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                    <text>Remote Survey of a Near-Coastal Archaeological Alignment at Kualoa, Hawai'i
Using Worldview 2 Satellite, LiDAR and UAV Imagery
Damion Sailors
University of Hawai'i at Mānoa, Department of Anthropology
Saunders Hall 808-349-9426, USA
Email: sailors@hawaii.edu
Scott S. Honda
University of Hawai'i at Mānoa, Department of Geography, Saunders Hall 808-351-3096
USA
Email: sshonda@hawaii.edu
Abstract
By using World View 2 multispectral satellite imagery, LiDAR, and unmanned aerial
vehicles, a large submerged archaeological stone alignment, that is likely part of an
ancient Hawaiian fishpond, was detected off the coast of Kualoa, Hawai’i during a
remote survey of the area. Principal component analysis, ratio indices, and LiDAR
interpretation were utilized in a GIS to help detect this archaeological stone feature that
is located in shallow coastal waters. Because threats of modern development, sea-level
fluctuations, and complications inherent to coastal-maritime environments have
generally challenged the survey of cultural resources located within the coastal strand,
this method holds promise for future spatial analyses and provides an accessible and
cost efficient means of shoreline assessment. This paper aims to show how remote
sensing methods can assist in the study of archaeological features that are located
within difficult to access coastal and near-coastal areas.
Key words: Remote Sensing, Coastal Survey, Fishponds, Archaeology, GIS

Introduction
On the windward side of the island of O'ahu, an archaeological alignment was detected
utilizing remote sensing techniques in the near-shore coastal flats of the northwest
section of Kane'ohe Bay near Kualoa Regional Park. Kualoa is a culturally significant
ahupua'a (land division) with a rich, traditional prehistory associated with social elites of
old Hawai'i and today it is maintained by the City and County of Honolulu. Kualoa is also
a pu'uhonua (ceremonial center) that was governed by the kahuna nui (high priests) of
Hawai'i who maintained close relationships with the neighboring watersheds of Hakipu'u
on the west and Ka'a'awa on the north as seen in (Figs.1-2) (Sterling and Summers,
1962; Gunness, 1987). Traditionally, these land divisions possessed stone-walled
1

�fishponds that were typical of an intensified form of aquaculture practiced in early
Hawai'i (Kikuchi, 1976). However, the spatial data that exists on this subject matter is
limited. Accordingly, this paper provides an efficient means of surveying submerged,
archaeological features located in shallow, coastal waters using satellite, LiDAR and
digital camera imagery.

Fig. 1 Area on O'ahu, Hawai'i Where Offshore Stone Alignment Was Detected. (Damion Sailors,
2013)
The Site Location - Kualoa
The first archaeological survey of Kualoa was performed by J. G. McAllister in 1933 and
included the documentation of Mōli'i fishpond, 'Āpua Pond, Mokoli'i Pond, Koholālele
Pond, and Niuola'a Heiau. McAllister learned through interviews and translations that
Kualoa is a pu'uhonua (ceremonial center) where large ceremonies dedicated to Lono
(the god of harvest) were performed and that the area was also well-known for its
association with ancient Polynesian genealogies. Kualoa is also respected for its
2

�ancient burial caves reserved for social elites and its unique access to palaoa (sperm
whale ivory) which, because of its wealth, afforded Kualoa political power in precontact
Hawai'i (Gunness, 1987). McAllister also collected a reference from a local informant
about an ancient fish pond named Pilihe'e that was destroyed by a tsunami sometime
prior to the mid-19th century (Sterling and Summers, 1962). This fishpond was then
located and mapped during a student pedestrian survey during the Kualoa
Archaeological Research Project (1975-1985) using a rough “tape and compass”
method but was not explored further. As a consequence, this fishpond is not well-known
in either academic or local communities and management of this archaeological
resource has not occurred (Gunness, 1987; Carson and Athens, 2007).

Fig. 2 Aerial photograph of Kualoa Beach Park taken from an airplane showing Mōli'i Pond
(large pond on left) and 'Āpua Pond (small pond on right), shoreline accretion at south end of
Kualoa, and coral reef development in area. (John O’Connor, 2013)
There have been other, more recent archaeological studies conducted at Kualoa Park,
and to summarize the findings thus far, there have been 44 shoreline burials recovered
to date and a large amount of material artifacts consisting of large proportions of basalt
tools, kapa (bark cloth) making utensils, and gaming stones. The recovery of these
artifacts support the inference that Kualoa was a ceremonial center associated with the
Makahiki festivals honoring the god Lono. Interestingly, fishing gear was poorly
represented (only 3.62% of total artifacts) as were household items (2.89%) (Barrera,
1974; Gunness, 1987). The survey of this offshore alignment at Kualoa is significant
3

�because of the wall’s probable antiquity and what it might add to the overall
anthropological discussion regarding maritime coastal adaptation in an island
environment (Kikuchi, 1976). The absolute age of this feature is unknown but because
this stone alignment is of substantial size, it can be inferred that an organized social
effort was invested in its construction and maintenance (Kirch, 2010). Oral traditions
and geomorphological studies also support the idea that Kualoa was not only a sacred
land-division with an extensive royal history, but that it was particularly vulnerable to
damage from tsunamis that periodically strike the islands (Gunness, 1987; Carson and
Athens, 2007). Considering that the coastal zone of this windward part of O'ahu is highly
dynamic in terms of its coastal geomorphology, this stone wall may have also served as
a type of break-water constructed in an effort to modify the coastline or it may have
functioned as an aggregate for fishing (Kikiloi, 2003).
Pacific Island Fishponds
At the time of Captain Cook’s arrival to Hawai'i in 1778 there were an estimated total of
360 fishponds of varying size and function located throughout the archipelago. On
average, these fishponds were each thought to have produced a total of 3000 kg of fish
per year (Kikuchi, 1976; Kikiloi, 2003). At first, this may seem rather industrious, but if
we consider that the population in old Hawai'i may have conservatively been around
300,000 people, there would have been very little fish to go around (Schmitt, 1971;
Wyban and Wyban, 1989). It is estimated that fishpond technology in Hawai'i may be at
least seven centuries old after results from analyses made of the Alekoko and Kekupua
Ponds on Kaua'i revealed a radiocarbon range from 1140 - 1280 AD (Burney and
Burney, 2003). This is the oldest radiometric evidence there is for fishpond use in
Hawai'i but it is possible that the origin of this technology extends further back in time.
Hawaiian fishpond types can be separated amongst those that are dependent upon
freshwater, brackish water, and seawater. The primary fish harvested in Hawaiian
fishponds were mullet and milkfish and at least 22 species of edible marine life also
flourished in these ponds as secondary domesticates (Kikiloi, 2003). Based on the
available evidence, it could be argued that in contrast to the rest of Oceania, the
Hawaiian Islands claimed a more sophisticated aquacultural system (Kikuchi, 1976).
This argument is bolstered by the apparent large numbers of fishponds in Hawai'i, their
4

�larger acreage, variation in the types of sites, and in the technological complexity of the
system. However, there is evidence that other areas such as in the Society Islands,
Micronesia, and Western Polynesia, fish pond technologies were just as elaborate and
intensified as those found in Hawai'i (Dieudonne, 2002).
Remote Sensing methods
The advancements in both passive and active sensors used in remote sensing allow for
the collection of data or imagery with greater spatial, temporal, spectral, and radiometric
resolution. One example of advancements made with passive sensors is the
multispectral sensors on board some of today’s satellites (World View 2, Landsat MSS,
IKONOS). Multispectral sensors break up the electromagnetic spectrum into multiple
bands allowing for a finer analysis of an object’s reflectance value than previous
sensors. Hyper-spectral sensors allow for an even finer analysis, breaking up the
electromagnetic spectrum into hundreds of spectral bands (Jensen, 2005). Also an
active sensor technology that has seen increasing use is LiDAR (short for light and
radar). LiDAR is useful in detecting changes in elevation of an area at a relatively high
resolution. The Worldview 2 satellite is a commercial satellite that was launched in 2009
and is capable of collecting 8-band multispectral imagery at a high resolution with an
average revisit time of 1.1 days. The spatial resolution of the images is 1.85 m for the 8band multispectral images and 0.46 m for the panchromatic image. There are 8-bands
that the satellite groups into different parts of wavelengths (nm) within the
electromagnetic spectrum. The 8-bands and sections are the coastal band (400 - 450
nm), blue band (450 - 510 nm), green band (510 - 580 nm), yellow band (585 - 625 nm),
red band (630 - 690 nm), red edge (705 -745 nm), near-infrared 1 (770 - 895 nm), and
near-Infrared (860 - 1040 nm) (Digital Globe, 2013). Since each band collects at
different sections of the electromagnetic spectrum, each band can contain different
information based on the material an object or feature is made of. Each band also
interacts differently with water. The least amount of absorption and scattering takes
place in the wavelengths between 400 - 500 nm. Thus the two lowest bands, the coastal
band and blue band, are the most suitable bands to detect underwater features. In
contrast, the wavelengths represented by the red and near-infrared bands are highly
absorbed by water (Jensen, 2007). In passive remote sensing techniques, there are
5

�multiple operations that can be done to multispectral satellite imagery in order to
produce analyzable results.
Processing
The first process tree began by pan-sharpening the satellite imagery. Pan-sharpening
was done so the multispectral bands could have a higher resolution of the panchromatic
band, which was 0.46 m (Padwick, 2010). The terrestrial areas were then masked out of
the image. This was done to ensure that the full range of digital numbers in the imagery
belonged to pixels of offshore areas which could then be analyzed with greater detail.
An index ratio called the non-homogenous feature difference (NHFD) was then
performed. The NHFD takes the red-edge and coastal bands into the following formula:
(red-edge - coastal) / (red-edge + coastal) (Wolf, 2010). Index ratios, such as the NHFD,
enhance the contrast between two bands (Zeinelabdeina and Albielyb, 2008). The
reason why this formula works well in detecting offshore features is because the rededge and coastal bands interact with water very differently. The energy in the spectrum
of the red-edge band is highly absorbed by water where the energy in the spectrum of
the coastal band is not. When two bands have very different reactions to a phenomenon
(e.g. water) the ratio of those two bands will usually have a substantial amount of
information (Jensen, 2005). This creates an image that visualizes the contrast between
objects closer or above the surface of the water to objects towards the bottom of the
sea floor.
The second process tree started with the pan-sharpening and masking out of the
terrestrial areas of the satellite imagery followed by a principal component analysis
(PCA). PCA is an image enhancement technique that transforms the multispectral
imagery into principal components (PCs). Each principal component represents the
spatially correlated brightness values of each band in the multispectral imagery, while
being uncorrelated to other derived principal components. From the 8 multispectral
bands, 8 PCs are derived. The first PC will have the most information and the last PC
will usually have the least. The goal of PCA is to reduce the amount of spatially
repeated data throughout the 8 bands of the multispectral imagery into principal
components that are quite easy to interpret (Jensen, 2005). Once PCA was executed,
PCs 1 and 2 were visualized in the GIS platform well-known as ArcMap.
6

�LiDAR has the ability to gather elevation data on land and the bathymetry of areas in
shallow waters with relatively high accuracy (Jensen, 2007). LiDAR, that was made
available through the 2013 National Science Foundation - Research Experience for
Undergraduates, was also utilized to help detect the Kualoa fishpond wall. A LiDAR
point cloud (0.25 m resolution) was used to create a continuous surface or bathymetric
image using Inverse Distance Weighted and Natural Neighbor tools in ArcGIS (Bolstad,
2012). 3D geovisualization in ArcGIS of the LiDAR point cloud readily displayed the
shape of the offshore feature. To visualize the point cloud in 3D, graduated colors
based on the Z (elevation) value were first given to each point. Then the point cloud was
exaggerated to 30 times of its Z value, to best show the variation in depth of the
offshore area.
Unmanned aerial vehicle (UAV) technology was also utilized to collect imagery of the
offshore feature. Although there are many UAV platforms available, a DJI Phantom
Quad-Copter was used as it was made available via the National Science FoundationResearch Experiences for Undergraduates program mentioned previously. A Pentax
Optio camera was attached to the Phantom to collect imagery. Due to the weight of the
camera, the flying time of the UAV was limited to approximately two minutes. The UAV
coupled with the camera allowed for up-to-date imagery within the visible light spectrum
of the feature. However, there were some difficulties with the UAV/Pentax combo. The
first difficulty was the manipulation of the UAV’s elevation and position to ensure that
useful imagery over the correct feature was being acquired. Another difficulty was that
the Pentax captures imagery only in the visible light spectrum, so in order for
submerged features to be detected, a substantial amount of sunlight is needed (P.
Nesbit, Personal Communication 2013). Unfortunately, because the weather was
uncooperative, only a limited amount of useful images were acquired in the time allotted.
Finally, an underwater pedestrian survey shown in (Fig. 3), using snorkel gear and
underwater cameras, was also performed at a high tide in order to visually inspect,
measure, and photograph this feature. The wall sections observed on this day were
heavily encrusted with coral, algae, and other marine growth, but it was clear that this
alignment was indeed a purposefully constructed stone wall of some sort. Its function
though remains speculative.
7

�Fig. 3 (left) Underwater survey of offshore alignment at Kualoa Beach Park. Basalt stones used
in the wall’s construction are heavily encrusted with marine growth but can be easily discerned
as an articulated feature. (Chuck DeVaney, 2012)
Fig. 4 (right) Imagery from the steps taken in two “process trees” used to discern the offshore
alignment. A) Non-Homogenous Feature Difference (Red-Edge - Coastal) / (Red-Edge + Coastal),
B) Principal Component Analysis (Symbolized as PC1: Green and Blue, PC2: Red), C) Inverse
Distance Weighted interpolation of LiDAR point cloud, D) Natural Neighbor interpolation of
LiDAR point cloud. (Scott Honda, 2013)
Results
Due to the combination of difficulties in maneuvering the UAV, the varying availability of
sunlight, and the changing tides, the number of useful images captured by the
UAV/Pentax was limited. Given more flying time, stable conditions, and additional
equipment, like a field of view camera mounted to the UAV, more useful imagery could
have been attained. However, a mosaic was attempted in PhotoScan and Microsoft ICE
of the collected UAV/Pentax imagery. Although PhotoScan is capable of producing an
accurate and georeferenced image, it could not produce a mosaic image from the
collected UAV/Pentax imagery. Microsoft ICE was able to create a mosaic using some
of the images taken via UAV, but the resulting mosaic had no ground control points
available in the imagery that were usable for georeferencing. The software used for
manipulating and visualizing the data for analysis was ERDAS Imagine and ArcGIS.
ERDAS Imagine is image analysis software that has the ability to execute many remote
sensing and image analysis techniques (Intergraph, 2013). Principal component
analysis, ratio Indices, pan-sharpening, and masking of the satellite multispectral
8

�imagery were done in ERDAS Imagine. ArcGIS has a variety of tools and applications
that can be used to analyze, extract, manipulate, and manage geospatial data but was
primarily used for interpolating and visualizing the LiDAR point cloud data.
The image analysis, as seen in (Fig. 4), of this offshore alignment revealed the remnant
articulation of a discrete, walled structure that may be part of the aquacultural complex
in this area that includes Mōli'i fishpond, 'Āpua Pond, Mokoli'i Pond, and Koholālele
Pond. This alignment may be part of the Pilihe'e fishpond mentioned by local informants
in McAllister’s early twentieth century survey. Alternatively, it may be part of some sort
of antiquated breakwater or fish aggregation device placed there long ago. Further
study is required in order to understand more about this feature’s origin and function.
What we do know from this survey is that this alignment is purposefully constructed
from basalt boulders, stones, and pebbles, is approximately 550 m in length, three
meters wide, and is less than a meter tall on average being exposed at the lowest of
tides when it appears to be part of the natural reef formation of the area. It is a large
alignment that if proven to be a fishpond wall, would add many hectares to the
traditional aquacultural area of Kualoa. Considering the dynamic nature of Kualoa’s
shoreline, whether it is due to tsunami, tectonic processes and/or sea-level fluctuations,
this feature must have been an important variable in the recent social and
geomorphological history of this part of Kane'ohe Bay, O'ahu.
Discussion
Based on the non-homogenous feature difference, the principal component analysis
imagery, and the LiDAR point cloud, the use of remote sensing techniques (both active
and passive) to locate the offshore wall were useful in mapping this near-coastal
alignment. Because only the contrast of the wall from the surrounding reef was being
sought after, the NHFD was utilized here with the digital number values of the two
bands (coastal and red-edge) to demonstrate this contrast. If one were attempting to
derive the health or biomass of vegetation, the use of radiance would be more
appropriate (Jensen, 2005). Although more sophisticated UAV systems are available,
the hobbyist grade Phantom Quad-Copter was capable of imaging the offshore
alignment. The post processing of the UAV imagery in photogrammetry based software
like PhotoScan could be a useful method of finding and surveying coastal features.
9

�However, in this case study, not all images were usable in PhotoScan. This is probably
due to distortions introduced by water. Perhaps if a multispectral camera, with bands
that could penetrate water (i.e. coastal blue) were used, PhotoScan would be capable of
creating an orthophoto and a digital surface model of underwater features. Kualoa is an
area of chronic erosion and accretion, and has had frequent and intense coastal
modifications occur over the course of human occupation in the area. How the ancient
people of Kualoa adapted to, and perhaps influenced these changes can be seen
archaeologically, and thus remote sensing and survey at a high resolution can assist
anthropological endeavors in this region (Hunt and Lipo, 2008). Knowledge then gained
may shed light on issues of sustainability and how limited resources, such as those
found in the Pacific islands, are managed by complex societies (Ladefoged and Graves,
2000; Erlandson, 2010). In a contemporary context, threats of inundation causing the
potential loss of cultural resources in coastal areas are immediate and severe. These
cultural resources, in the form of archaeological features, can be identified within the
coastal strand using the methods we have discussed here in this report. For future
study, questions regarding the automation of extracting linear features from remote
imagery as well as improvements on data management can be readily explored.
Maritime adaptations may be more easily understood using these spatial methods and
considering the accessibility and efficiency of this type of non-invasive technique, we
propose further similar survey in coastal-maritime regions.
Acknowledgments
Special thanks go to Drs. Carl Lipo, Suzanne Wechsler, Chris Lee, Matt Becker, and
teaching assistants of the 2013 NSF-REU G.R.A.M Field Program, at California State
University at Long Beach. We would like to thank Dr. Terry Hunt, University of Oregon
and Drs. Christian Peterson and Matt McGranahan, University of Hawai'i at Mānoa.
Obligations are extended as well to John O’Connor and Chuck DeVaney for photo
contributions. And a final mahalo or “thank you” is given to the National Science
Foundation (Grant # DGE-1329626) and to those who assisted in reviewing the paper.
References
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�Bolstad, P., 2012. GIS Fundamentals: A first text on geographic information systems.
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A new synthesis in oceanic domestication: The Symbiotic

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Damion Sailors is a graduate student in the Anthropology Department at the University
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Geography, with a Minor in Information and Computer Sciences.

12

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                  <text>The Pacific Ocean contains a wealth of underwater cultural heritage. Underwater sites in Oceania span human history from the Stone Age to the Atomic Age. Due to the cultural richness of underwater heritage in the region and its complex history, the protection of these sites is of high importance for the region. Moreover, the potential for sustainable tourism in partnership with diving industry has been attracting a growing attention.&#13;
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                <text>By using World View 2 multispectral satellite imagery, LiDAR, and unmanned aerial vehicles, a large submerged archaeological stone alignment, that is likely part of an ancient Hawaiian fishpond, was detected off the coast of Kualoa, Hawaiâ€™i during a remote survey of the area. Principal component analysis, ratio indices, and LiDAR interpretation were utilized in a GIS to help detect this archaeological stone feature that is located in shallow coastal waters. Because threats of modern development, sea-level fluctuations, and complications inherent to coastal-maritime environments have generally challenged the survey of cultural resources located within the coastal strand, this method holds promise for future spatial analyses and provides an accessible and cost efficient means of shoreline assessment. This paper aims to show how remote sensing methods can assist in the study of archaeological features that are located within difficult to access coastal and near-coastal areas.</text>
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                    <text>Jōmon Sea: Navigation in the Origins of Japan
Daniele Petrella (IRIAE, daniele.petrella@iriae.com)
Irene Ciulla (IRIAE, ciullairene@gmail.com)
Diego M. Mezzapelle (IRIAE, halfskin@hotmail.it)
Giuseppe Avola (IRIAE, peppeavola95@gmail.com)
ABSTRACT
Japanese neolithic, the so called Jōmon Period, represents a vast terrain in which to develop new and exciting
research in the archaeological field. This is because there are still many questions that need to be answered to
better clarify the evolutionary dynamics of the cultures that characterized it. The project Jōmon Sea: Navigation
in the Origins of Japan aims to study and understand the use of the sea and waterways during the Japanese
Neolithic period, both in terms of movements within the archipelago and contacts with the surrounding
territories. In its first phase, the project will focus on the analysis of the nature and dynamics behind the first
relations with the Korean peninsula. For this reason, International Research Institute for Archaeology and
Ethnology (IRIAE) has developed a new project of maritime archaeological investigation on land and
underwater. The project identifys the island of Tsushima (Nagasaki Prefecture) as a crucial point. The activities
will begin at the sites of Meotoishimae and Ongaura, both overlook the Korean coast and have geomorphological
characteristics of possible landings and/or coastal settlements. Among these, those most under analysis are
related to the origins of the Jōmon culture, a topic that cannot be separated from human environment interaction:
the relationship with the Korean populations and that with the sea. What was the role of the sea in the life of the
Jōmon People? How did they move and what boats did they use? What were kaizuka really and what did they
mean? How did they adapt to the environmental changes at the advent of the Holocene?
List of Figures
Figure 1: Flowchart of the Adaptation Cycle
Figure 2: Waniura Bay and Shishimi Bay
Figure 3: Ongasaki / Ongaura Site
Figure 4: ‘Meotoishimae’ Site

INTRODUCTION
The topic of this abstract fits best into the session ‘History and Current Trends of Underwater
Archaeology around East Asia’ because it aims to address the study of the relationships between
Jōmon communities and the sea, its use and exploitation of resources, and the role it played in the
relations between them and continental populations, not neglecting the importance of other waterways
in internal movements and communications. All this through a new methodological proposal based on
the simultaneous investigation of land and underwater sites with the aid of innovative technologies and
computer systems. Our methodology is the study of coastal sites in relation to the adjacent seabed, in
GIS, to bring together archaeological data from the various sites under investigation. This will open up
new research perspectives in the complex field of movement and settlement choice during the
Japanese Neolithic.
As there are clear cultural differences in the archipelago during the Jōmon Period (14,000 BC and
9,500 BC and end around 1000 BC), we prefer to identify this period as the 'Japanese Neolithic’ and
use the term jōmon to indicate the cultural faces that characterised it. The identification and
'development' of cultural faces is based on changes in the relationship between man and his
environment and how he adapted to it. In the circular flowchart (Figure 1) the environment inevitably
influences the lifestyle of human groups, which produces a 'material culture' that, in turn, favours and
enables the adaptation necessary to survive climatic and environmental changes (Renfrew et al. 1991).

1

�Figure 1: Flowchart of the Adaptation Cycle

The advent of the Holocene brought about great changes that conditioned and forced human groups in
the area to modify their 'habits' (Barnes 2015).
Climatic change characterised the Holocene. On the one hand, on land evergreens and deciduous
broadleaf trees produced acorns and hard fruits (Teshigawa 2022; Williams et al. 1982) and the
ecological process of insularisation led to an increase in the populations of smaller mammals such as
wild boar and deer. This followed the extinction of larger animals that could not migrate to places with
more suitable temperatures. All this allowed for a constant seasonal food supply for gathering and
hunting (Habu 2022). On the other hand, in the water the sea level rise separated Japan from the
continent. This led to the development of navigation, both for marine and terrestrial travel. On land the
presence of the great mountains over the entire surface of the archipelago make overland travel
extremely complex.
Rivers represented the main inland communication routes, while lakes were an important source of
supply for inland areas further from the coasts (Hornell 1946). Over the sea people performed
cabotage and inter-island boating.
Moreover, water products, such as molluscs, fish, and marine mammals, represented a new source of
food supply that not only contributed to the general needs of the populations, but also compensated for
seasonal food fluctuations (Habu et al. 2011; Koike 1980; Teshigawara 2021; Teshigawara 2022).
Excavations conducted in various areas of Japan, related to the various phases of the Jōmon Period,
have brought to light bones of large marine mammals and large fish, such as whales and tuna. Such
animals require complex organisation, strategy, and technology of evolved societies (Hosoya et al.
2014).
The waterways became the main communication routes for the 'flow of goods, people and information'
(Mizoguchi 2013) not only within the archipelago itself, but also from outside.
Japan, in fact, with the advent of the Holocene, became a territory with a temperate climate, rich in
vegetation and raw materials and particularly suited to both fishing and hunting (Teshigawara 2016).
This 'oasis' was a destination for migratory flows of foreign cultures that greatly influenced the
development of local communities (Mizoguchi 2002). Namely, from the north populations of Siberia
and the American territories; from the south-west populations of Korea; and from the south
populations of the Southeast Asian Archipelago (Nakagome et al. 2020).
The reconsideration of all these elements led to the project 'Jōmon Sea: Navigation in the Origins of
Japan' by the International Research Institute for Archaeology and Ethnology (IRIAE). The project is
divided into three phases. Jōmon Sea 1 will focus on understanding the nature of early relations with
Korea and how these influenced the evolution of Jōmon cultures. Jōmon Sea 2 will deal with relations
with northern cultures. Jōmon Sea 3 will address the study of internal contacts within the country.

2

�The first phase will focus on relations with the Korean peninsula to investigate the island of Tsushima
(Nagasaki Prefecture). The island is located in the centre of the Sea of Japan, on the route between
Kyūshū and Korea, from whose coastline it is only 47 km away. It is likely that this island was
intercepted by explorers from the peninsula in search of richer territories. Tsushima represents a
veritable 'treasure chest' for archaeological research because since ancient times it has been the
crossroads of all cultural dynamics between Japan and the surrounding cultures; just as Sicily, Italy is
at the centre of the Mediterranean. Numerous investigations were conducted on the island in recent
decades by Japanese scholars, which confirmed the strong Korean presence and exchanges with
northern Kyūshū, but also the mutual influence between Korean and local populations (Shōbayashi
1995). The project is carried out in collaboration with Tokyo University of Marine Science and
Technology and the Asian Research Institute of Underwater Archaeology (ARIUA), which has been
carrying out archaeological investigations on Tsushima Island for years.
CASE STUDIES
After analysing the reports of all the excavations and investigations conducted on the island, we chose
to start with the north-western area, which faces Korea. Two extremely interesting sites can be found
in this area (Figure 2). These are the Waniura Bay, located in the far north, and the Shishimi Bay area,
slightly further south (Nagasaki 2019), which represent the case studies examined.

Figure 2: Waniura Bay and Shishimi Bay

The Ongasaki / Ongaura Site
This is the first of the inlets, coming from the south, in Waniura Bay and facing the Korean coast. It is
part of the Yabitsu area, which is being investigated by ARIUA; where the first, and so far, only,
Jōmon landing site has been identified, as well as numerous Korean Neolithic evidence (Hayashida
2019).

3

�The investigations focused on the Ongasaki promontory that closes the inlet to the north (around 20
metres above sea level) and in the stretch of sea that bathes Ongaura (Figure 3).

Figure 3: Ongasaki / Ongaura Site

The surface survey of Ongasaki revealed the presence of three obsidian points and significant
quantities of obsidian, quartz crystals and shell waste. Considering the particular purity of the obsidian
found, the absence of quarrying pits on Tsushima Island and the morphological characteristics of the
tips found, we assume that it came from the Koshidake quarry in northern Kyūshū. The shape and
quality of these finds is absolutely superimposable to those found along the southern coast of Korea
and, mainly, in the Busan area. The route of obsidian is likely: raw obsidian arrives on the island from
northern Kyūshū reaching Ongasaki for processing, from there, the finished products are sent to the
Korean coast. In addition, the presence of hundreds of quartz crystals, shell waste and numerous traces
of charcoal make Ongasaki an important processing and sorting site for obsidian products and other
valuable materials. We also found archaeological evidence related to later periods, such as fragments
of iron swords (dated to the Late Yayoi and the Kofun Period), bronze-finished weapons and armour, a
bronze coin from the Edo Period and some fragments of medieval pottery (including celadon) that
testify to the long life of the Ongasaki site and the strategic importance of its location.
The underwater survey carried out on the seabed of Ongaura Bay revealed the presence of fragments
of amphorae, still to be chronologically framed, and three lithic anchors whose typology can be
ascribed between the Jōmon and medieval periods.
The 'Meotoishimae' Site
The geomorphology of Meotoishimae and the documented importance of the bay were the elements
that prompted us to investigate this inlet. This site is located opposite the important site of Meotoishi
in Shishimi Bay (Figure 4), which has always been known to Koreans and mentioned in the text
Haedong Jegukgi (Adachi 1999). It was excavated between the end of the 1970s and 1993 and brought
to light a very large number of Neolithic Korean pottery of the Sugari type and only a few fragments
of Ataka-style pottery dated to the Middle Jōmon (Kiyoura 1992).

4

�Figure 4: ‘Meotoishimae’ Site

Our investigations on the Meotoishimae site revealed an interesting similarity with the structures in
Koshitaka, which is located on the same side of the island only three kilometers to the north and
currently being investigated by the Tsushima Museum team. If this structure similarity is confirmed by
subsequent investigations, one could hypothesise their repeated pattern during the Neolithic period, as
well as location choice of the island's bays overlooking the stretch of sea facing Korea. The
archaeological excavations at the Koshitaka site uncovered 2461 fragments of Neolithic Korean
pottery and only seven fragments of Maebira-style Jōmon pottery (Shōbayashi 1995), as well as a
Korean-style kiln. This discrepancy between the amount of Korean and indigenous evidence leaves
little doubt these were Korean settlements.
We hypothesize groups from Korea sailed in search of richer territories and then settled in Tsushima.
Over time, they influenced and merged with the small local populations, and, from this fusion
developed a hybrid culture. During the Early/Middle Jōmon this hybrid culture looked further east,
towards the Kyūshū coast, which they reached by cultural exchanges.
RESOURCES
The resources that will be deployed to implement the project will come, in addition to the specific
skills and expertise present in IRIAE, from the collaboration with Tokyo University of Marine Science
and Technology. They supply the technological approach to underwater investigations, and the
ARIUA. Moreover, the project already enjoys the patronage of UNESCO Underwater Heritage and the
financial support of the Italian Ministry of Foreign Affairs and International Cooperation.
FRAMEWORK
The project aims to answer a series of interconnected questions. These questions are based on the use
and exploitation of the sea, waterways and coastal settlements in bays. First, in Jōmon Sea the aim is
to understand the structure and location-choice of coastal settlements in bays. We aim to contextualize
this with the seasonal cycle of food supply and storage methods. Second, we aim to collect data on the
5

�types and level of nautical knowledge of the Neolithic communities that exploited the bays, along with
their transportation of raw materials, related trade and cultural exchange.
The methodological approach is simultaneous archaeological investigation and comparison of data
from land and underwater. Further, we will use both sonar equipment for scanning the seabed and
high-resolution satellite reading software. The latter will be used to obtain a clearer visualisation of the
geomorphology of the areas and the identification of anthropic evidence that might otherwise be
difficult to identify.
Of extreme importance, moreover, is the creation of a GIS platform that collects data from the sites we
have investigated and from those investigated by other research groups. The GIS facilitates site
comparison to obtain a more complete reading of the historical dynamics that characterised the area
starting from the Neolithic period. The GIS platform georeferences elements necessary for the
management and analysis of the survey results (reconnaissance, excavation, protection, etc.). The GIS
can be used for the planning and design of subsequent excavation work. Within GIS, we plan to carry
out distributional-typological analyses of finds and fragments characterised with different symbology
on the basis of the type of material (stone, metal, wood, etc.) and the type of artefact (e.g., scrap,
arrowhead, blade, etc.). In this way it is possible to visualise and interpret the dynamics of distribution,
concentration, isolation and thinning of specific typological groups and compare them simultaneously.
RESULTS
The results obtained during the spring 2023 survey campaign were the identification that the Ongasaki
site is a processing and sorting site for valuable materials, and what routes these raw materials took to
reach Ongasaki and from there to Korea. The existence of the Ongasaki processing site suggests a
settlement or logistical support site in its vicinity. Therefore, future investigations and excavations will
aim to find and understand site organisation.
Another important outcome the research team is aiming for is the identification of repeated patterns in
bay structure and their location, so that these may serve as a proto-type for future identifications of
other anthropized bays. Finally, it is our intention that the GIS platform created can be constantly
implemented with data from other research in order to achieve a comparison of data that facilitates a
broad and syncretic reading of the periods under analysis. The GIS would become a baseline tool
available to the scientific community and all researchers.

Acknowledgements
We would like to thank our Japanese colleagues at Tokyo University of Marine Science and Technology and the ARIUA,
whose input was essential to access Japan's difficult administrative mechanisms. As well as the Tsushima Board of Education
and the Nagasaki Prefecture for granting us the necessary authorisations. In addition, we would like to thank the Ministry of
Foreign Affairs and International Cooperation of the Italian Republic, which has supported all IRIAE projects with great
enthusiasm for years. Finally, we would like to thank all the IRIAE team members without whose professionalism and
dedication the project would not have been possible.

6

�Bibliography
Adachi, H. Nihon no Fune. Tokyo: Fune no Kagakukan, 1999.
Barnes, L. G. Vulnerable Japan: The Tectonic Life Setting of Life in the Archipelago. In P. C. Brown and B. L. 2015
Habu, J. “Jōmon Collectors and Foragers: Regional Interaction and Long-Term Changes in Settlement System among
Prehistoric Hunter-gatherers in Japan.” In J. Habu and B. Fitzhugh (Eds.), Beyond Foraging and Collecting: Evolutionary
Change in Hunter-gatherer Settlement Systems, New York: Kluwer-Plenum Publishing Corporation, (2002): 53-72.
Habu, J., Matsui, A., Yamamoto, N. and Kanno, T. “Shell Midden Archaeology in Japan: Aquatic Food Acquisition and
Long-term Change in the Jōmon Culture.” Quaternary International 239 (2011): 19-27.
Hayashida, K. “2018 Nendo Yabitsu B Chiten Chōsa no Gaiyō.” ARIUA Newsletter 8 (2019): 27-33.
Hornell, J. Water Transport, Origins and Early Evolution. Cambridge: Cambridge University Press, 1946.
Hosoya, L. A., Nakamura, O., Seguchi, S. and Shibutani, A. “What Did Jōmon People Eat in Fact? Jōmon Subsistence and
Society Chronological Shifts in Japanese Jōmon Subsistence Strategies on the Basis of Local Characteristics of North Tohoku
Area.” Proceeding of the 6th Worldwide Conference of the Society for East Asian Archaeology (2014): 6-10.
Kiyoura, G. “Meotoishi Iseki.” Nagasaki-ken Maizō Bunkazai Chōsashūhō 15 (1992): 1-38.
Koike, H. Seasonal Dating by Growth-line Counting of the Clam, Meretrix Lusoria: Toward a Reconstruction of Prehistoric
Shell Collecting Activities in Japan. Tokyo: University of Tokyo Press. 1980
Mizoguchi, K. An Archaeological History of Japan, 30000 B.C. to A.D. 700. Philadelphia: University of Pennsylvania Press,
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Mizoguchi, K. The Archaeology of Japan. Cambridge: Cambridge University Press, 2013
Nagasaki, A.”Tsushima Hokubu no Iseki no Yōsō.” ARIUA Newsletter 8 (2019): 2-10.
Nakagome, S., Gakuhari, T. and Rasmussen, S. “Ancient Jomon Genome Sequence Analysis Sheds Light on Migration
Patterns of Early East Asian Populations.” Common Biol 3 (2020): 437-456.
Renfrew, C. and Bahn, P. Archaeology: Theories, Methods, and Practice. London: Thames and Hudson. 1991
Shōbayashi, M. Kōdai Kikō, Vol.1: Tsushima. Nagasaki: Town News-sha, 1995
Teshigawara, A. Jōmon Jidai-shi. Tokyo: Shinsenn sha, 2016
Teshigawara, A. Jōmon Jidai o Shiru Tame no 110 Mondai. Tokyo: Shinsen-sha, 2021
Teshigawara, A. Jōmon Jidai Gaido Bukku. Tokyo: Shinsen-sha, 2022
Williams, M. N. and Hunn, S. E. Resource Managers: North American and Australian Hunter-gatherers. Boulder: Westview
Press. 1982

7

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territories. In its first phase, the project will focus on the analysis of the nature and dynamics behind the first&#13;
relations with the Korean peninsula. For this reason, International Research Institute for Archaeology and&#13;
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                <text>Petrella, Daniele. 2023. “Jōmon Sea: Navigation in the Origins of Japan.” Edited by Jennifer Craig, Jay Mok, T. Kurt Knoerl, Akifumi Iwabuchi, and Kotaro Yamafune. In Proceedings of Fifth Asia Pacific Regional Conference on Underwater Cultural Heritage: Gwangju, The Republic of Korea, November 13-18 2023. The Museum of Underwater Archaeology. URL: https://apconf.omeka.net/exhibits/show/apconfproceedings/item/1891</text>
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                    <text>Geophysical techniques for non-intrusive documentation of UCH:
Comparative analysis of the methodology developed in three study areas in Spain.
Soledad Solana Rubio,1 Felipe Cerezo Andreo2, Sebastián Federico Ramallo,3 Dario Bernal Casasola,4
Miguel Ángel Cau Ontiveros,5 Francisco López-Castejón6
1

(University of Cádiz, Researcher) 0000-0001-5571-7453
(University of Cádiz, Associate Professor) 0000-0003-0025-1726
3
Asensio (University of Murcia, Professor) 0000-0003-1828-3996
4
(University of Cádiz, Professor) 0000-0003-1107-5318
5
(ICREA, and IAUB, University of Barcelona, Professor) 0000-0002-1138-157X
6
(Cartagena Oceanographic Research Institute and Polytechnic University of Cartagena, Researcher) 0000-00024196-4100
2

ABSTRACT
Generally, the combined use of different geophysical instruments and archaeological fieldwork provides enough
information for the classification and preliminary study of sites. However, the application of these techniques in
detailed analysis of specific archaeological sites is still in its early stages. In this paper, we present the results of
the geophysical survey work carried out in three different underwater contexts, as part of three research projects,
in three areas of Spain: Algeciras (Cádiz), Cartagena (Murcia) and Palma de Mallorca (Balearic Islands).
Geophysical survey allows for the application of non-intrusive techniques to achieve the documentation
of UCH, as recommended by the 2001 UNESCO Convention on the Protection of the Underwater Heritage,
without altering the archaeological material in any way. Therefore, we have used the Sub Bottom Profiler in several
archaeological works, with varying depths and conservation conditions, to address our research questions of how
much information can we obtain non-intrusively on the UCH and how can we best use the equipment to innovate
in the development of non-intrusive methodology. Based on the results obtained in each area, we can draw several
methodological conclusions that lay the groundwork for a method that can be applied to other case studies.
Keywords: non-intrusive techniques, geophysical survey, Sub Bottom Profiler, monitoring UCH.
List of figures
Figure 1 – Location of the case studies and surveyed areas.
Figure 2 – Equipment used on board the vessel for fieldwork.
Figure 3 – Signal processing example using ISE 2.9 INNOMAR software.
Figure 4 – Types of anomalies recorded.

1. INTRODUCTION
We present an innovative and non-intrusive method of monitoring and documenting Underwater
Cultural Heritage (UCH), in which we have taken advantage of the opportunities offered by the
development of new technologies. We analyse the methodology implemented in three case studies, in
which we have surveyed the UCH in different areas using a Sub Bottom Profiler (SBP). This is an
equipment that emits acoustic pulses that penetrate the sediment, resulting in the image of a stratigraphic
profile of the seabed and the artefacts or anomalies that may be buried beneath it. In this way, without
disturbing the seabed, we can see what is buried, what is anomalous and how deep it is. This research
has been the result of a collaborative effort of the University of Cádiz (Spain), through three different
projects, with the universities of Murcia, Cartagena, Barcelona, Balearic Islands and the Consell de
Mallorca.

1

�2. CASE STUDIES
This methodological study took into consideration three case studies (see figure 1), each with different
characteristics related to the archaeological heritage to be studied and the geological conditions of the
environment in which it is located. Furthermore, although the research goals of each project were
distinct, they all shared the methodological questions that we aim to address in this paper.
2.1. HERAKLES Project (Algeciras, Cádiz)
As a pioneering project for this research, the HERAKLES Project (FEDER-UCA18-107327)7 was the
first scenario to test the SBP techniques. We undertook the geophysical survey in a specific zone of the
Bay of Algeciras: the harbour area (see figure 1.1). As the main objectives of the HERAKLES project
were to document the UCH of Algeciras Bay and to assess the impact of port and industrial constructions
on it, the goals of this survey were two:
1. To determine the existence of anomalies buried under the sediment.
2. To understand the stratigraphy of the area and how successive dredging and harbour works have
modified the natural sedimentation processes.
2.2. ALADROQUE Project (Cartagena, Murcia)
The second scenario was the harbour area of Cartagena, which differed significantly from the previous
case study. The zone of intervention covers the mouth of the Benipila Rambla (stream) and the
Algameca Chica, up to a depth of approximately -50 m, an area of detrital and rocky seabed with plenty
of archaeological materials (see figure 1.2). The ALADROQUE project8 arises after the high impact
weather event known as coold drop (Depresión aislada en niveles altos – DANA) that affected the
Region of Murcia in September 2019. One of the most serious consequences of this episode was the
overflowing of the streams, such as the Benipila, causing a large amount of sediment and rubbish to be
dragged into the sea. Thus, the ALADROQUE project aimed to assess the impact of this event on the
seabed and on the UCH. The objectives of the geophysical survey were therefore two:
1. To identify possible anomalies that might correspond either to UCH or to objects dragged by the
floods.
2. To evaluate the rate of sedimentation caused by floods and sea currents by monitoring the burial
process in two known archaeological sites.
2.3. ARQUEOMALLORNAUTA Project (Palma de Mallorca, Balearic Islands)
The third case study involved the Ses Fontanelles shipwreck (Munar et al., 2022; Soler et al. 2021),
located in shallow waters, with sandy seabed, offering ideal conditions for studying its state of
preservation and the probable dispersion of its materials. The ARQUEOMALLORNAUTA project9
aimed to document and excavate this unique Late Roman shipwreck, and a geophysical survey was
conducted as a preliminary activity before archaeological fieldwork (see figure 1.3). Therefore, our
objectives were threefold:
1. To obtain a three-dimensional visualization of the shipwreck that would allow the evaluation of its
state of preservation.
“Entre las Columnas de Hércules, Arqueología Subacuática de un espacio privilegiado. La bahía de Algeciras” (FEDERUCA18-107327 HERAKLES)
8 “ALADROQUE: El impacto de los eventos climáticos tipo DANA en la conservación de los entornos subacuáticos de los
accesos al puerto de Cartagena (España)”, an initiative of the Cartagena Oceanographic Research Institute (CORI), in
collaboration with the University of Murcia (UM), the University of Cadiz (UCA) and the Navy Diving Centre (CBA),
9 Joint project of the Consell de Mallorca and the universities of Barcelona, the Balearic Islands and Cádiz.
7

2

�2. To provide stratigraphic details especially about the characteristics of marine sedimentary levels.
3. To detect the existence of anomalies that can be analysed in the interpretation phase of the results of
the archaeological fieldwork.

Figure 1 – Location of the case studies and surveyed areas: 1. Bay of Algeciras;
2. Harbour of Cartagena; 3. Palma de Mallorca.

3. RESOURCES
The resources available to conduct the work include the equipment used (see figure 2), property of the
Laboratory of Archaeology and Prehistory (LABAP) of the University of Cádiz (UCA), consists of:
- Sub Bottom Profiler (SBP) model SES-2000 standard, manufactured by the German company
INNOMAR. It is parametric in nature, which allows a high resolution in the detection of strata and
layers of sediments. The signal penetrates, on average, twice the depth at which it probes.
- Motion correction sensor (MRU) to correct and improve precision of the spatial location of the signal.
- Mobile RTK GNSS Leica GS18 Antenna, which ensures the positioning of the data readings with a
millimetre error margin.
Besides, different boats were used in each case study. For the survey in Algeciras, we used the Tarpán,
a fiberglass rigid boat with inboard motor, and a draft of 0.5 m. Secondly, in Cartagena we had two
fiberglass vessels from the University of Murcia, the Betsaida, with 0.3 m draught, and the Universitas,
with 0.6 m draught. In the third case study, a semi-rigid inflatable boat with an outboard motor was
used, with a draft of 0.4 m, named Mustelus. A very important variable for the reliability of the results
in geophysical surveying with SBP is the expertise of the boat captain. In the three case studies, they

3

�were very skilled, showing great ability, not only in handling each boat, but also in understanding what
the team needed.
Regarding the human team, the works were performed by two archaeologists from the University of
Cádiz, trained in the use of geophysical techniques thanks to the activities coordinated by the Nautical
and Underwater Archaeology Line.

Figure 2 – Equipment used on board the vessel for fieldwork.

4. FRAMEWORK
Given the three case studies presented, the methodological inquiries of this research aim to determine
the limitations of the SBP technique. Furthermore, we have identified various types of anomalies in all
three geophysical surveys, which have been subsequently cross-checked with other techniques such as
historical information, magnetic anomalies, test pits, and visual surveys. This has allowed us to create a
comprehensive catalogue of anomalies that can be utilized in future SBP surveys (Cerezo Andreo et all,
2022; Higueras-Milena and Cerezo Andreo, 2021).
Following the principles established by UNESCO in the 2001 Convention (Maarleveld, Guérin and
Egger, 2013; VVAA., 2010), surveying with SBP allows prioritising in situ conservation of UCH,
exploration over recovery and non-destructive techniques.
The precision of the transects over the area to be studied is fundamental for the interpretation of the
data, so once the working areas have been defined, the density level of each survey grid must be planned,
considering the objectives proposed for each survey.
In the framework of the HERAKLES project, given the large extension of the Bay of Algeciras, we have
focused on understanding the general stratigraphy and the degree of preservation of original sediments
in “El Saladillo”, one of the ancient harbour spaces.

4

�Before conducting the survey in the port of Cartagena, we had access to valuable information that aided
in our planning process. Specifically, we were aware of certain anomalies that had been detected during
a previous survey conducted in 2008 by the National Museum of Underwater Archaeology (ARQVA).
During our SBP surveys, undertaken in 2021 and 2022, we detected new anomalies and checked the
levels of burying or unearthing in sites. Some of the anomalies were documented by diving or using a
ROV. We also verified their archaeological potential and established a protocol for the periodic
monitoring of their state of preservation.
For the ARQUEOMALLORNAUTA project, two work areas were surveyed: the one where the Ses
Fontanelles shipwreck is preserved and a larger one to document its general sedimentation dynamics
and to detect anomalies that could be related to the site. The seabed in the study area is generally sandy
but with a strong muddy matrix that allowed the signal to penetrate several metres below, reaching - 5.5
m in some profiles. The Ses Fontanelles shipwreck was protected by sandbags, resulting in a 2.5 m deep
tumulus. That makes the water column between the transducer and the shipwreck very small.
After the data analysis and processing (see figure 3), we obtained a series of anomalies that we classified
according to their archaeological interest and their accessibility. Subsequently, a fieldwork season to
check the most significant anomalies was planned.

Figure 3 – Signal processing example using ISE 2.9 INNOMAR software.

5. RESULTS
5.1. HERAKLES Project (Algeciras, Cádiz)
On the El Saladillo research area we have successfully identified the paleochannel from the Last Glacial
Maximum period (see figure 4.A). This unknown geological feature was not easily silted by sediments,
so it kept its depth for a long time, which explains why this area was used as an anchorage throughout
history.
Our surveys led to notable discoveries, including the identification of the basement levels of Isla Verde
Island. This now-destroyed island was once one of the main landmarks on the maritime landscape in the
ancient Bay and provided a reliable source of fresh water.

5

�5.2. ALADROQUE Project (Cartagena, Murcia)
The intensive use of the SBP in the port of Cartagena has yielded high-resolution stratigraphic profiles,
enabling the documentation of the impact of the flooding caused by the 2019 DANA. The resulting data
about the impact of the flood on the UCH holds potential for advancing monitoring and conservation
efforts. In addition, we have assessed the burial or erosion factor that some archaeological sites are
suffering, especially the Cartagena 1 shipwreck, located at 63 m depth, one of the best-preserved
shipwrecks from the 2nd century BC in the Iberian Mediterranean. Cross-checking data between 20082021-2022, we have been able to verify that the shipwreck has been unearthed between 70 and 80 cm.
The cargo is now scattered over a space twice the size it was in 2008, which means that the tumulus is
falling apart (see figure 4.B). On the contrary, there are areas that have been significantly buried, hiding
known elements since the 2008 surveys. This process is partly positive because burial offers good
guarantees for the conservation of the heritage, but also it makes access to it impossible.
Finally, dives to verify the selected anomalies have revealed the presence of rubbish and other debris
which are altering the structural integrity of some objects.

Figure 4 – Types of anomalies recorded. A) Paleochannel with continental sedimentation; B) Shipwreck C) Pipeline
D) Buried object (in this case an amphora) E) Natural anomaly corresponding to the bottom of a paleochannel.

5.3. ARQUEOMALLORNAUTA Project (Palma de Mallorca, Balearic Islands)
The results have been very positive, as we have achieved a stratigraphic visualisation of both the Ses
Fontanelles shipwreck and its surroundings. Among the 31 significant anomalies detected, those of
special archaeological or stratigraphic interest were selected. Thus, we configured three categories of
priority for intervention according to their accessibility: size, morphology, and depth below the seabed.
After the second processing of the signals and the comparative analysis of the anomalies, three of them
were identified with paleochannels, one with the Ses Fontanelles shipwreck, five provided relevant
information on the stratigraphy and six were considered to be a pipeline (see figure 4.C). Therefore, we
made eight archaeological test pits to verify this interpretation. Only one test pit was positive as far as
the presence of archaeological material was concerned, finding a fragment of ancient pottery. The
artefact was found under a layer of shells and coarse gravel, covered by another layer of dead seagrass.

6

�The hyperboles shown by the acoustic signal corresponded to points where the archaeological material
was buried (see figure 4.D).
The anomalies of natural origin correspond to a layer of rubble, coarse gravel, and pebble rocks that we
consider to be the seabed of a paleochannel, with continental sedimentation phases (see figure 4.E). This
provides interesting information about the palaeolandscape in the pre-Holocene period.
With respect to the anomaly identified as the Ses Fontanelles shipwreck, collected in 53 stratigraphic
profiles, we could document the different levels that comprised the shipwreck's protective tumulus.
5.4. Conclusions
The results achieved in the three case studies demonstrate that the use of the SBP has been proven
effective for UCH surveying, providing high-resolution stratigraphic profiles and detailed information
on the morphology of the seafloor and any anomalies present. Overall, the use of the SBP is a useful
tool in the field of UCH research, allowing for non-intrusive and precise surveying of underwater
archaeological sites.
To conclude, here are some generalities regarding the use of the SBP for the UCH surveying, although
each site and its characteristics, the equipment used and the objectives of each research will determine
the configuration and final results.
-

-

-

-

-

-

Regarding the type of seabed, the signal penetrates better in mud than in sand, where there is
usually more noise.
The boat used for the survey should be small, to ensure manoeuvrability, but stable and with
rigid gunwale, as vertical as possible to the water surface. The most important thing is to prevent
engine vibrations from being transmitted to the SBP.
The recommended speed for conducting SBP surveys is typically less than 4 knots. We have
achieved optimal results at speeds between 2 and 2.5 knots. It should be noted that slower survey
speeds can result in longer survey durations and increased vulnerability to wave interference,
ship vibration, and reduced ability to correct heading.
It is important to note that obtaining accurate and reliable results with the SBP is highly
dependent on the sea state. It has been observed that waves exceeding 30-40 cm significantly
impact the quality of the data collected, rendering them unreliable.
In theory, the penetration distance of the SBP signal is twice the water column below the
transducer. Nevertheless, at greater depths, the number of pulses emitted must be increased due
to the prolonged time it takes for the signal to return. From our experience, optimal results are
obtained at depths ranging between 10 to 20 meters.
Regarding frequency, increasing it will yield higher resolution, but at the expense of losing
penetration depth. Conversely, lowering the frequency will increase penetration depth, but
reduce resolution. Finding the optimal frequency setting requires thorough testing and
experimentation on a case-by-case basis.
As for the research objectives, this technique is highly recommended for anomaly detection or
for monitoring known sites. It is very useful for surveying UCH at different times and for
analysing, by comparing the signals, the rate of sedimentation. It is also very useful for the study
of the paleolandscape or to check the impact of dredging on the seabed, but for stratigraphic
studies it must be combined with geotechnical cores (Torres et al, 2022).

In the future we have planned more surveys to test this methodology in new and different case studies,
therefore we will add more conclusions to this research. A methodology based on the results obtained
here will undoubtedly contribute not only to a better knowledge of the UCH, but also to a greater
awareness and impact of the research at the international level.

7

�ACKNOWLEDGEMENTS
The work in the Bay of Algeciras has been co-financed by the 2014-2020 ERDF Operational Programme and by the Department
of Economy, Knowledge, Business and University of the Regional Government of Andalusia. Project reference: FEDERUCA18-107327.
The Cartagena case study has been co-financed by CORI and the ARQUEOTOPOS III Project, Grant HAR201785726-C2-1-P (Carthago Nova desde su entorno litoral: Paleotopografía y evolución medioambiental del Sector central del
Sureste Ibérico. Dinámica poblacional y productiva) funded by MCIN.
The case of Ses Fontanelles is part of the activities of the research group ERAAUB of the Institute of Archaeology
of the University of Barcelona (IAUB), Consolidated Group (2021 SGR 00696), thanks to the support of the Comissionat per
a Universitats i Recerca del DIUE de la Generalitat de Catalunya. Some of the activities have been possible thanks to the
synergies created with the projects “Arqueología y Arqueometría aplicadas al estudio de la cerámica y el poblamiento de la
ciudad romana de Pollentia y su hinterland (Mallorca, islas Baleares)” (ARQCERPOL) (PID2021-123223NB-I00)
(ARQCERPOL) (PID2021-123223NB-I00), funded by MCIN/AEI/ 10.13039/501100011033 and by “ERDF A way of making
Europe”, GARVM III (PID2019-108948RB-I00/AEI/10.13039/501100011033), Gobierno de España/FEDEAR;
ARQUEOSTRA (FEDER-UCA18-104415) Programa Operativo FEDER 2014-2020 and Consejería de Transformación
Económica, Industria, Conocimiento y Universidades, Junta de Andalucía; and ARQUEOFISH (P18-FR-1483) Programa de
Ayudas a la I+D+I, Plan Andaluz de Investigación, Desarrollo e Innovación (PAIDI 2020).
We thank this conference for accepting us and for providing a methodological session, which is important for the
whole scientific community. Thanks to the three projects, the four universities and the LABAP, which provided us with the
equipment. To the owners and captains of the boats. To all the researchers who seek knowledge underwater.
BIBLIOGRAPHY
Cerezo Andreo, Felipe, Solana Rubio, Soledad, López-Castejón, Francisco and Ramallo Asensio, Sebastián Federico. “El
impacto de los eventos climáticos tipo Dana en la conservación de los entornos subacuáticos de los accesos al puerto de
Cartagena (España). Primeros datos del proyecto Aladroque.”, NANS: Noticiario de Arqueología Naútica y Subacuática, ISSNe 2952-1149, Nº. 0 (7), (2022): 4-18. Available in: &lt;https://dialnet.unirioja.es/servlet/articulo?codigo=8758191&gt;.
Higueras-Milena Castellano, Aurora and Cerezo Andreo, Felipe. “Investigaciones arqueológicas mediante métodos geofísicos
marinos en el entorno de La Caleta Antecedentes y novedades de la campaña de 2019”. In La Caleta (Cádiz): Entre la Tierra
y el Mar. Un estudio diacrónico de uso, edited by en Alberto Gullón Abao, Lilyan Padrón Reyes and Carlota Pérez-Reverte
Mañas, 19-34. Sevilla: Aconcagua, 2021.
Maarleveld, Thijs, Guérin, Ulrike and Egger, Barbara. Manual para actividades dirigidas al patrimonio cultural subacuático:
directrices para el Anexo de la Convención de la UNESCO de 2001. Paris: UNESCO, 2013. Available in:
&lt;https://unesdoc.unesco.org/ark:/48223/pf0000220716&gt;.
Munar Llabrés, Sebastià, Cardell Perelló, Jaume, de Juan, Carlos, Cau Ontiveros, Miguel Ángel, Bernal-Casasola, Darío,
Picornell, Llorenç and García Riaza, Enrique. “Ses Fontanelles Shipwreck (Mallorca, Balearic Islands): An Exceptional Late
Roman Vessel and Its Cargo”, Journal of Maritime Archaeology, 17 (2022):
487–505. Available in:
&lt;https://doi.org/10.1007/s11457-022-09331-6&gt;.
Soler i Nicolau, Antònia, Font Jaume, Alexandre, Berni Millet, Piero, García Riaza, Enrique, Bernal-Casasola, Darío, Cau
Ontiveros, Miguel Ángel, Cardell Perelló, Jaume and Munar Llabrés, Sebastià. “El singular conjunto de tituli picti del pecio
de Ses Fontanelles (Mallorca, islas Baleares) y su contribución a la epigrafía anfórica tardorromana hispánica”, Cuadernos de
Arqueología y Prehistoria de la Universidad Autónoma de Madrid (CUPAUAM) 47(1), (2021): 287-317. Available in:
&lt;https://doi.org/10.15366/cupauam2021.47.1.010&gt;.
Torres, Trinidad, Ortiz, José E., Ramallo, Sebastián, Ros, Milagros, Sánchez Palencia, Yolanda, Blázquez, Ana, Cerezo, Felipe,
López-Cilla, Ignacio, Galán, Luis, A., Borrego, Ángeles G., Ruiz Zapata, Blanca, Gil, María José, Manteca Ignacio and
Rodríguez-Estrella, Tomás. “Development of the marine Holocene environment in a drowned paleovalley with final anthropic
influence in the Cartagena Bay (Murcia, SE Spain)”, The Holocene, 32 (6), (2022): 554–568. Available in:
&lt;https://doi.org/10.1177/09596836221080759&gt;.
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Cultura, 2010. Available in: &lt; https://www.calameo.com/read/000075335b012b37e3d4b&gt;.

8

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                <text>Generally, the combined use of different geophysical instruments and archaeological fieldwork provides enough&#13;
information for the classification and preliminary study of sites. However, the application of these techniques in&#13;
detailed analysis of specific archaeological sites is still in its early stages. In this paper, we present the results of&#13;
the geophysical survey work carried out in three different underwater contexts, as part of three research projects,&#13;
in three areas of Spain: Algeciras (Cádiz), Cartagena (Murcia) and Palma de Mallorca (Balearic Islands).&#13;
Geophysical survey allows for the application of non-intrusive techniques to achieve the documentation&#13;
of UCH, as recommended by the 2001 UNESCO Convention on the Protection of the Underwater Heritage,&#13;
without altering the archaeological material in any way. Therefore, we have used the Sub Bottom Profiler in several&#13;
archaeological works, with varying depths and conservation conditions, to address our research questions of how&#13;
much information can we obtain non-intrusively on the UCH and how can we best use the equipment to innovate&#13;
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                <text>Solana Rubio, Soledad , Felipe Cerezo Andreo, Sebastián Federico Ramallo Asensio, Darío Bernal Casasola, Miguel Ángel Cau Ontiveros, Francisco López-Castejón. 2023. “Geophysical techniques for non-intrusive documentation of UCH: comparative analysis of the methodology developed in different study areas at various depths.” Edited by Jennifer Craig, Jay Mok, T. Kurt Knoerl, and Carlota Perez-Reverte. In Proceedings of Fifth Asia Pacific Regional Conference on Underwater Cultural Heritage: Gwangju, The Republic of Korea, November 13-18 2023. The Museum of Underwater Archaeology. URL: https://apconf.omeka.net/exhibits/show/apconfproceedings/item/2000 </text>
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                    <text>Recent Efforts in Underwater Cultural Heritage Management
on the Pacific Outer Continental Shelf

Dave Ball
Pacific Outer Continental Shelf Region, Bureau of Ocean Energy Management
Camarillo, California 93010, USA
Email: david.ball@boem.gov
Abstract
The Bureau of Ocean Energy Management (BOEM) is responsible for managing
the nation’s energy and mineral resources on the federal Outer Continental Shelf
(OCS). These resources include conventional energy (oil and gas), renewable
energy (wind and hydrokinetic) and sand and gravel extraction for beach
restoration. As with any federal action or undertaking, an assessment of potential
impacts to the environment, including cultural resources, is required to make an
informed decision. The BOEM Pacific OCS Region is taking a proactive
approach to cultural resources management on the OCS by funding research
efforts that provide baseline information on known and potential underwater
cultural resources, and by identifying best practices for incorporating information
from indigenous communities in the planning process.
Key words: Bureau of Ocean Energy Management, Cultural Landscape, Offshore
Renewable Energy, Outer continental Shelf, Submerged Landform, Tribe
Introduction
The Bureau of Ocean Energy Management (BOEM) is responsible for managing over
1.76 billion acres of seafloor off the coast of the United States (U.S.) and is charged
with regulatory oversight of offshore conventional energy (oil and gas), renewable
energy (wind, wave and ocean currents) and marine minerals (primarily sand and gravel
resources for coastal restoration). The Bureau’s jurisdiction begins 3 nautical miles
offshore and extends approximately 200 nautical miles, to the extent of the Exclusive
Economic Zone1. BOEM’s authority over conventional energy and marine minerals was
established through the Outer Continental Shelf Lands Act (OCSLA) of 1953, which
gave the Secretary of the Interior authority over mineral exploration and development on
the Outer Continental Shelf (OCS). Through the Energy Policy Act (EPAct) of 2005
BOEM (then operating as the Minerals Management Service) also has authority over
offshore renewable energy. The EPAct significantly expanded the bureau’s offshore
energy responsibilities and renewed interest in energy development on the Atlantic and
Pacific OCS. For any federal action or undertaking within the Bureau’s authority, BOEM
1

�must comply with the National Environmental Policy Act (NEPA), the National Historic
Preservation Act (NHPA) and other legislative and regulatory environmental
requirements. Included in those requirements is the obligation to consult with federally
recognized tribal governments, as mandated through Executive Order 13175 and
Secretarial Order 3317. Additionally, the NHPA requires consultation with federally
recognized tribes and Native Hawaiian Organizations for cultural resources that are
considered eligible for listing on the National Register of Historic Places. As BOEM’s
offshore renewable energy program has developed, and applications for construction of
offshore facilities are increasing, it is important that the Bureau properly engage with the
nation’s coastal indigenous communities.

To ensure that the Bureau is consulting

properly, BOEM is funding several projects that seek to be more proactive in developing
the best practices for identifying appropriate information gathering protocols and survey
measures in order to avoid or mitigate adverse effects during development on the OCS.
Each of these projects is rooted in the cultural landscape concept, which seeks to
develop a more holistic understanding of areas that could be affected by a proposed
action

or

undertaking

by

integrating

environmental

science

with

historical,

archaeological and traditional knowledge.
Cultural Landscape Approach
The concept of cultural landscapes is not new.

According to the United Nations

Educational, Scientific and Cultural Organization (UNESCO), “[I]n 1992, the World
Heritage Convention became the first international legal instrument to recognize and
protect cultural landscapes” (Mitchell et al., 2009: 19). UNESCO defines a cultural
landscape as embracing…
“…a diversity of manifestations of the interaction between humankind and
its natural environment.
Cultural landscapes often reflect specific
techniques of sustainable land-use, considering the characteristics and
limits of the natural environment they are established in, and a specific
spiritual relation to nature…Cultural landscapes are illustrative of the
evolution of human society and settlement over time” (Mitchell et al., 2009:
19-20).
In recent years the cultural landscape approach has also gained traction and
acceptance within the federal historic preservation program in the U.S. For example,
the U.S. National Park Service’s Bulletin 36 defines a cultural landscape as, “a
2

�geographic area, including both cultural and natural resources and the wildlife or
domestic animals therein, associated with a historic event, activity, or person or
exhibiting other cultural or aesthetic values” (NPS, 1994). More recently, the U.S.
National Oceanic and Atmospheric Administration’s (NOAA) Marine Protected Areas
Federal Advisory Committee issued a white paper in 2011, which recommended
incorporating a cultural landscape approach to “strengthen conservation of resources
that cross the land/sea interface, promote sustainability of those resources and improve
the socio-economic resilience of communities which depend upon them” (MPAFAC,
2011: 4). Additionally, in 2011 the Advisory Council on Historic Preservation (ACHP)
released the Native American Traditional Cultural Landscapes Action Plan, which is
designed to:


Promote the recognition and protection of Native American traditional
cultural landscapes both within the federal government and the historic
preservation community



Address the challenges of the consideration of Native American
traditional cultural landscapes in the Section 106 review process as
well as in NEPA reviews (ACHP, 2012).

This plan was adopted by the ACHP in November 2011 and announced by the White
House on June 28, 2012 (Donaldson, 2012).
BOEM Environmental Studies
Established in 1973 under the former Minerals Management Service, the Environmental
Studies Program (ESP) is an applied science program that was created to develop,
conduct and oversee scientific research specifically to inform policy decisions regarding
offshore energy and marine minerals activities on the OCS.

Research conducted

through the BOEM ESP covers physical oceanography, atmospheric sciences, biology,
protected species, social sciences and economics, submerged cultural resources and
environmental fates and effects. The primary goal of the ESP is to provide information
needed for the assessment and management of environmental impacts on the human,
marine and coastal environments of the OCS and the potentially affected coastal areas.
As a result, BOEM is a leading contributor to the growing body of scientific knowledge
about the nation’s marine and coastal environment. Through BOEM’s ESP, baseline
3

�analysis of underwater cultural heritage resources has been updated off the Atlantic,
Gulf of Mexico and Pacific coasts (Pearson et al., 2003; TRC, 2012; ICF International et
al., 2014, respectively). Each of these studies includes a database of identified and
reported historic shipwrecks and a predictive model of high probability areas that could
be associated with submerged prehistoric landforms, areas that would have been
exposed thousands of years ago during the Last Glacial Maximum (LGM). Additionally,
in support of potential offshore renewable energy development, initial baseline
assessments have been completed along the Atlantic and Pacific coasts of historic
properties that could be affected by alteration of the seascape from construction of
offshore facilities (TRC, 2012; ICF International et al., 2014, respectively).
BOEM held the first commercial offshore renewable energy lease sale for an area off of
Rhode Island in July 2013, and a second sale was held off Virginia in September.
Interest for developing offshore renewable energy has also been expressed elsewhere
on the Atlantic OCS, as well as off the coasts of Hawaii and Oregon within the BOEM
Pacific OCS Region. Offshore renewable energy siting could have an affect on
submerged prehistoric sites and coastal sites that are important to indigenous groups.
Expected impacts to the seafloor will occur from the installation of individual wind, wave
or ocean current generators and associated transmission cable corridors. Additionally,
wind turbines, which can stand 300-500 feet above the ocean surface, will have a
definite visual signature. Depending on how far offshore wind turbines are constructed,
many of these facilities will be visible to some extent from the coast, and therefore will
have some level of affect to the offshore view.
Therefore, as BOEM reviews applications for offshore renewable energy projects, it is
critical that the Bureau not only develop protocols that honor the unique relationship
between the federal government, sovereign tribal nations and indigenous communities,
but also incorporates traditional knowledge and oral tradition into the decision-making
process. To meet these challenges, BOEM has awarded several research studies that
seek to develop best-practices protocols for working with federally recognized tribes and
Native Hawaiian communities, as well as incorporating information from these groups
into the analysis of offshore geophysical survey data. Some of these projects are briefly

4

�highlighted below and two of these efforts will be detailed further in this session by
Valerie Grussing and Hans Van Tilburg.
Submerged Paleocultural Landscapes Project
Off the Atlantic coast of the U.S., where interest in offshore wind energy has been more
prominent, BOEM has entered into a cooperative agreement with the University of
Rhode Island, in partnership with the Narragansett Indian Tribal Historic Preservation
Office, to develop a science-based, standardized best practices methodology for
incorporating tribal knowledge into a predictive model for identifying submerged
landforms.

Developing

Protocols

for

Reconstructing

Submerged

Paleocultural

Landscapes and Identifying Ancient Native American Archaeological Sites in
Submerged Environments seeks to enhance and refine the Bureau’s understanding of
submerged paleocultural landscape distribution on the Atlantic OCS and to better
understand and identify paleocultural landscapes of importance to regional tribes
through collaborative research. Specifically, the project is designed to incorporate
Narragansett Indian Tribal oral history and traditional knowledge with remote sensing
surveys off the coast of Rhode Island in order to develop a geospatial predictive model
that will identify offshore environments with varying archaeological sensitivity for
containing ancient Native American archaeological resources.
The first phase of the project was completed in the spring of 2013, which consisted of a
2-day workshop between invited tribal representatives and archaeologists from Europe
and the U.S. The workshop reviewed current theories on submerged landform
identification and discussed how to respectfully engage Native American tribes. The
second phase of the project will synthesize the information obtained at the workshop,
along with published sources, to develop a methodology aimed at incorporating tribal
knowledge into best practices protocols for developing a model to identify submerged
landforms. Once a working model is developed, researchers will conduct field
investigations and data acquisition, combined with tribal traditional knowledge in order
to validate the model and create a more complete understanding of the paleocultural
landscape off Rhode Island. The project also includes an outreach component with the
Narragansett Tribe and will develop training materials and a documentary film. This
project was awarded as a cooperative agreement through the North Atlantic Coast
5

�Cooperative Ecosystem Studies Unit in July 2012 and should be completed in
September, 2016.
Characterization of Tribal Cultural Landscapes
At the time of this writing, the BOEM Pacific OCS office has received two applications
for offshore renewable energy projects off the Oregon coast. These proposed projects
include a commercial floating wind lease off of Coos Bay and a marine hydrokinetic
(MHK) research lease off of Newport. Prior to receiving these lease requests, the BOEM
Pacific OCS office entered into an interagency agreement with NOAA’s Marine
Protected Areas Center and the Maritime Heritage Program to develop best practices
protocols for working with west coast tribes to incorporate information on tribal cultural
landscapes into the Bureau’s decision-making process. The goal of this project,
Characterizing Tribal Cultural Landscapes, is to develop a proactive approach to
working with Native American communities in order to identify areas of tribal
significance that need to be considered in the planning process.

A more detailed

discussion of this project is provided elsewhere in this session by Dr. Valerie Grussing
in her paper, Characterizing Tribal Cultural Landscapes for Resource Preservation and
Protection.
Hawaii Maritime Heritage
The BOEM Pacific OCS Region office has not yet received any completed applications
for renewable energy projects offshore Hawaii, however, interest has been expressed
for offshore wind development. In May 2012, the BOEM Pacific OCS Region signed an
inter-agency agreement with NOAA’s Office of National Marine Sanctuaries to provide
baseline information on underwater cultural heritage resources off the eight main
Hawaiian Islands. The project, Assessing Historic Properties and Cultural Resources in
the Main Hawaiian Islands, will develop a database of underwater and land-based
cultural resources that could be affected by construction of offshore renewable energy
facilities. The project also seeks to develop a best practices methodology for engaging
Native Hawaiian communities, similar to the Tribal Cultural Landscapes project, so that
information important to Native Hawaiians is included in the planning and review
process for any future offshore renewable energy applications. This is the first cultural
resources-related project that BOEM has undertaken for Hawaii and the information
6

�collected through this effort will provide critical information for taking into consideration
the effects of offshore renewable energy development on cultural resources near the
eight main Hawaiian Islands. Further information on this effort is discussed elsewhere
in this session by Dr. Hans Van Tilburg in his paper, Assessing Historic Properties and
Cultural Resources in the Main Hawaiian Islands.
Submerged Landforms on the Pacific OCS
With the completion of the updated baseline study on underwater cultural heritage for
the BOEM Pacific OCS Region, BOEM developed this follow-up study to further
investigate submerged landforms off the U.S. west coast and to refine the predictive
model for where these landforms might be expected. Archaeological and Biological
Assessment of Submerged Landforms off the Pacific Coast is a multi-disciplinary effort
that will examine existing data sets from areas off the southern California and central
Oregon coastlines that have been identified as having a high potential to be associated
with previously exposed landforms. The project will develop and field test a geospatial
model that will aid in the identification and classification of potential submerged cultural
landforms from existing remote sensing data and seafloor maps in areas along the
Pacific coast. Similar to the Narragansett project on the Atlantic OCS, this project will
evaluate existing remote sensing data and review current theories on sea level rise
during the Last Glacial Maximum (LGM) on the Pacific OCS in order to identify high
probability areas for further testing. Biological indicators, such as hard-bottom features,
will also be assessed to see if these features correlate with possible submerged
landforms. The project will also conduct fine-scale survey and ground-truthing of
identified features and analyze new data for possible indicators of prehistoric human
activity. This project should be completed in 2017.
Pacific Region Ocean Uses Atlas
The last project that the BOEM Pacific Region office is currently undertaking, which has
the potential to incorporate cultural use information from indigenous communities, is the
Pacific Region Ocean Use Atlas (PROUA). The PROUA project was developed through
an inter-agency agreement with NOAA’s National Ocean Service and is designed to
document where coastal communities use the ocean across a full range of typical
human activities and sectors. The primary objective of the project is to enhance ocean
7

�planning for offshore renewable energy development and inform other ocean planning
strategies that require insight on how and where ocean areas are used for recreational,
commercial and industrial types of activity. One component of this project is to conduct
interactive participatory mapping workshops in order to capture the knowledge of
community experts about the patterns of ocean uses occurring off the coasts of Hawaii,
Oregon and Washington. Though the previously discussed efforts have not yet been
completed to fully develop protocols for engagement with coastal indigenous
communities, efforts have been made to invite these groups into the process
appropriately.
Conclusion
With the passage of the 2005 Energy Policy Act, BOEM’s mandate over offshore energy
and marine minerals expanded to include offshore renewable energy. In an attempt to
improve BOEM’s environmental review process and better fulfill the Bureau’s obligation
to consult with federally recognized tribes and Native Hawaiian Organizations, BOEM is
developing a more proactive approach to engage indigenous communities in the
decision-making process in support of offshore renewable energy. Information on each
of the studies described in this paper, as well as other research funded by the Bureau,
can be found on our website at: www.boem.gov\studies\.
Acknowledgement
Funding for the research projects identified above has been provided through the
Bureau of Ocean Energy Management.

The author would like to thank the Tribal

Historic Preservation Offices of the Confederated Tribes of Grand Ronde, the Makah
Tribe, and the Yurok Tribe for their efforts on the Tribal Cultural Landscapes project, as
well as the Narragansett Indian Tribal Historic Preservation Office for their efforts on the
Submerged Paleocultural Landscapes project.
Endnote
1

OCSLA and the Submerged Lands Act define the OCS as all submerged lands lying seaward of state
coastal waters. For most coastal states federal waters begin 3 nautical miles past the mean low tide line,
the exception to this rule includes offshore Texas and the west coast of Florida, whose state waters
extend 9 nautical miles offshore.

8

�References
ACHP (Advisory Council on Historic Preservation), 2012. The ACHP’s Native American
Traditional Cultural Landscapes Action Plan. http://www.achp.gov/traditional-culturallandscape.pdf, accessed 05 December 2013.
Donaldson, M. W., 2012.Native American Traditional Cultural Landscapes Action Plan –
Better

Decisions

for

Historic

Properties.

http://www.whitehouse.gov/blog/2012/06/28/native-american-traditional-culturallandscapes-action-plan-better-decisions-histo-0, accessed 05 December 2013.
ICF International Davis Geoarchaeological Research and Southeastern Archaeological
Research, 2013. Inventory and Analysis of Coastal and Submerged Archaeological Site
Occurrence, Pacific OCS. U.S. Department of the Interior, Bureau of Ocean Energy
Management, Pacific OCS, Camarillo, CA OCS Study BOEM 2013-0115, pp. 363.
Mitchell, N., Mechtild Rössler, and Pierre-Marie Tricaud., (Eds.), 2009. World Heritage
Cultural Landscapes: A Handbook for Conservation and Management
http://whc.unesco.org/documents/publi_wh_papers_26_en.pdf, accessed 04 December
2013.
NPS (National Park Service), 1994. Bulletin 36 Protecting Cultural Landscapes:
Planning,

Treatment

and

Management

of

Historic

Landscapes.

http://www.nps.gov/tps/how-to-preserve/preservedocs/preservation-briefs/36PreserveBrief-Landscapes.pdf, accessed 04 December 2013.
MPAFAC (Marine Protected Areas Federal Advisory Committee), 2011. White Paper
and Recommendations of Managing Marine Resources across the Land/Sea Interface.
http://marineprotectedareas.noaa.gov/pdf/helpfulresources/mpafac_rec_protected_landsea_12_11.pdf, accessed 04 December 2013.
Pearson, C. E., James, Jr., S. R., Krivor, M. C., El Darragi, S. D., and Cunningham, L.,
2003. Refining and Revising the Gulf of Mexico Outer Continental Shelf Region HighProbability Model for Historic Shipwrecks: Final Report. U. S. Dept. of the Interior,
Minerals Management Service, Gulf of Mexico OCS Region, New Orleans, LA. OCS
Study MMS 2003-060, 2003-061, 2003-062, 3 Volumes.
TRC Environmental Corporation, 2012. Inventory and Analysis of Archaeological Site
Occurrence on the Atlantic Outer Continental Shelf. U.S. Dept. of the Interior, Bureau of
9

�Ocean Energy Management, Gulf of Mexico OCS Region, New Orleans, LA. OCS
Study BOEM 2012-008, pp. 324.
Dave Ball is the Pacific Region Historic Preservation Officer and Diving Safety Officer
for the Bureau of Ocean Energy Management (BOEM). Before joining BOEM he worked
for several archaeological firms in the Pacific Northwest. He received a BA in
anthropology from Sonoma State University in 1992 and an MA in anthropology from
Florida State University in 1998. Dave has over 20 years’ experience in archaeology
and has directed field research on both terrestrial and underwater archaeological sites
across the country, including inundated prehistoric sites, World War II shipwrecks, and
deepwater shipwrecks in the Gulf of Mexico. He is currently serving on the Board of
Directors for the Advisory Council on Underwater Archaeology.

10

�</text>
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                  <text>Video interview with Session 2 chair Dr. Hans Van Tilburg and links to the papers included in the session.</text>
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                  <text>In 2009, responding to the effort to protect the significant natural and cultural resources within the marine environment for the benefit of present and future generations, the U.S. National Marine Protected Areas Center formed a Cultural Heritage Resources Working Group to provide expert advice on improving the conservation and management of maritime heritage resources. The resulting White Paper provided a series of recommendations to both the U.S. Department of Commerce and the Department of the Interior, including new definitions for cultural heritage, marine cultural resources, tribes, indigenous peoples, and cultural landscapes. Central to these recommendations was a strong endorsement for the Cultural Landscape Approach in the understanding and management of maritime heritage resources (or UCH). Subsequently, the National Oceanic and Atmospheric Administrationâ€™s (NOAA) Maritime Heritage Program has adopted the recommendations of this paper and is implementing a â€œmaritime cultural landscapeâ€ approach to the management of cultural resources within the National Marine Sanctuary System. Also as a part of this initiative, NOAA and the Bureau of Ocean Energy and Management (BOEM) have teamed up to support maritime cultural landscape studies of heritage resources by Native American Tribes and Native Hawaiian communities in the Pacific region. These projects on the U.S. West Coast and in the Hawaiian Islands demonstrate the necessity of adapting a broader range of recognized cultural resources and a more inclusive and participatory management and preservation process. Charismatic resources like historic shipwrecks will always provide unique information for archaeologists and historians, but we do ourselves a disservice if we focus solely on these types of properties, and neglect other perspectives and the broader nature of all types and traces of human existence that lie underwater.&#13;
Participants in this session will focus on the status of these ongoing ground-breaking projects, the advantages of a broader and more inclusive approach compared to the previous cultural heritage management paradigm in the U.S., and the challenges that this creates.</text>
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                <text>The Bureau of Ocean Energy Management (BOEM) is responsible for managing the nationâ€™s energy and mineral resources on the federal Outer Continental Shelf (OCS). These resources include conventional energy (oil and gas), renewable energy (wind and hydrokinetic) and sand and gravel extraction for beach restoration. As with any federal action or undertaking, an assessment of potential impacts to the environment, including cultural resources, is required to make an informed decision. The BOEM Pacific OCS Region is taking a proactive approach to cultural resources management on the OCS by funding research efforts that provide baseline information on known and potential underwater cultural resources, and by identifying best practices for incorporating information from indigenous communities in the planning process.</text>
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                    <text>Assessing Historic Properties and Cultural Resources
in the Main Hawaiian Islands
Hans Van Tilburg
NOAA Office of National Marine Sanctuaries, Honolulu, Hawaii 96825, USA
Email: hans.vantilburg@noaa.gov
Dave Ball
BOEM Environmental Assessment Section, Camarillo, California 93010, USA
Email: david.ball@boem.gov
Abstract
Understanding the types and locations of significant archaeological and cultural
resources is essential to their protection. NOAA and the Bureau of Ocean Energy and
Management (BOEM) have teamed up to support an assessment of historic properties
and cultural resources in the main Hawaiian Islands. Objectives for this project include:
1) a database of verified, reported, and potential submerged cultural resources in the
Hawai`i Outer Continental Shelf; 2) a database of historic properties that could be
adversely impacted by alteration of the ocean viewshed; and 3) a management tool for
engaging Native Hawaiian communities in identifying significant marine areas for
offshore energy development planning purposes.
Key words: Resource Management, Hawaiian Islands, Indigenous community,
Mitigation, Viewshed
Origin of the Project
The remote main eight Hawaiian Islands are approximately 3,900 km from the North
American continent, 6,000 km from Japan, and 7,000 km from Papua New Guinea.
Their coasts and near shore waters represent, for the most part, a high-energy marine
environment subject to the prevailing northeasterly Trade Winds, open ocean swells,
Pacific storms, quake-generated tsunami, and passing hurricanes. There are few
natural harbors or safe anchorages, though fringing and barrier reefs provide some
protection. The warm clear waters are home to the Teredonavalis shipworm, and
currents and surge contribute to sand scouring and marine weathering of all artifacts.
However, compared to continents, the waters around the Hawaiian Islands drop off very
quickly. For instance, 300-600 m are typical depths for the three-mile limit around the

1

�island of O‘ahu. At these depths, historic wreck sites are little affected by the recurring
storms and tsunami events that impact the upper ocean levels.
Initiating a comprehensive and systematic documentation of cultural resources for the
marine environment of the main Hawaiian Islands (survey does not include the remote
Northwestern atolls) is a challenging and daunting task. No such comprehensive survey
has yet been completed, though some progress has been made in gathering specific
information regarding historic properties such as shipwrecks and submerged aircraft.
Hawai‘i’s high-energy marine environment has long been hazardous for mariners, and
hundreds of ships have been reported lost. But one of the most interesting challenges
for understanding underwater cultural heritage (UCH) in the islands is the fact that, until
recent years, the overall definition of cultural resources in Hawai‘i generally did not
included historic properties like shipwrecks, so commonly recognized as UCH in other
locations.
In general, the main focus of cultural resource efforts in Hawai‘i has been the
maintenance and preservation of indigenous cultural access, traditional practices, and
active human connections and relationships to marine species and culturally significant
natural resources. These are issues of immediate importance to local communities,
dynamic issues that bear directly on maintaining cultural practices and cultural identity.
The fact that shipwreck archaeology is relatively new to the islands is not due to a lack
of attention to cultural resources; just the opposite, it is due to the fact that cultural
resources and resource preservation, in the broadest sense, have been and are
overwhelmingly important in Hawai‘i. Historic properties like shipwrecks represent the
new element or “player” brought into an existing and much older discussion.
Historic wreck sites are obviously important to archaeologists and historians as unique
and non-renewable sources of information. They have also been important to Hawai‘i’s
recreational diving industry and even to fishermen as productive fishing sites.
Yethistoric wreck sites have not been part of the cultural resource discussion at a
program or agency level until more recent years. For instance, while cultural resources
are a large part of the 2012 Hawaii Ocean Resources Public Management Plan (Anon,
2012), shipwrecks or submerged historic properties are not mentioned within the

2

�document. Sensitivity to Hawai‘i’s unique history and a special sense of place is
required for understanding cultural resource governance in the islands.
This presentation focuses on a new and innovative resource management three-year
inventory project, the Maritime Cultural Resource Site Assessment in the Main Hawaiian
Islands, funded by the U.S. Department of the Interior, Bureau of Ocean Energy
Management (BOEM), through an Interagency Agreement with the U.S. Department of
Commerce, National Oceanic and Atmospheric Administration (NOAA), National Ocean
Service. This project proposes new ways of conducting cultural resource inventory work,
methods that are better suited to recording information in a manner that recognizes
Hawai‘i’s investment in cultural resource management, and better suited to engaging
Native Hawaiian Organizations and communities, as well as accounting for the existing
values that archaeologists and historians bring to the mix.
The origin of this project is actually the State of Hawai‘i’s effort to reduce greenhouse
gas emissions and develop local energy independence. The State supports a mandate
to achieve 70% “green” energy independence by the year 2040. Offshore renewable
energy development will be a part of the effort to meet this goal. Understanding the
types and locations of significant archaeological and cultural resources will be essential
to their protection in the context of this coming development. Therefore, NOAA and the
Bureau of Ocean Energy and Management (BOEM) have teamed up to support the site
assessment project, producing the tools of the desk-based assessment for the entire
main eight Hawaiian Islands, prior to the specific proposal of any single specific
development project.
There are three main objectives for this project: 1) create a database of verified,
reported, and potential submerged cultural resources in the Hawai`i Outer Continental
Shelf; 2) create a database of historic properties on shore that could be adversely
impacted by alteration of the ocean viewshed; and 3) create a management tool for
engaging Native Hawaiian communities in identifying significant marine areas for
offshore energy development planning purposes. There are a number of important
benefits stemming from the overall goal of resource protection from potential impacts.
For NOAA the project will help meet the agency’s mandate to inventory historic
properties, and most importantly build on two decades of growing social awareness of
3

�maritime heritage properties in Hawai‘i. For BOEM the project will obviously facilitate
decision-making for offshore renewable energy development by providing the
groundwork for cultural resources review, helping make siting decisions more efficiently.
Finally, for Native Hawaiian stakeholders the project will (hopefully) better engage
communities with agencies prior to the proposal of activities that may impact resources.
Objective 1: Database of Verified and Potential Submerged Cultural Resources on
the Outer Continental Shelf
(Note: the volcanic islands of Hawai‘i originate in a denser oceanic tectonic plate, not a
lighter continental plate; hence, they have no actual continental shelf. Here the term
OCS is used to designate the main study zone from 3-200 miles offshore).
Objective 1, the inventory of verified, reported, and potential submerged cultural
resources on the Hawai`i outer continental shelf, will be the most familiar to maritime
archaeologists as it replicates, in part, the standard desk-based assessment tool
highlighted in UNESCO’s UCH Foundation courses, and published in the Training
Manual for the UNESCO Foundation Course on the Protection and Management of
Underwater Cultural Heritage in Asia and the Pacific (UNESCO, 2012). NOAA
sanctuary staff are currently examining primary and secondary archival sources and
developing a Microsoft Access database of confirmed, reported, and potential
submerged archaeological resources within the survey area. The project specifies the 3200 mile offshore Federal waters zone, but existing data for the near shore 0-3 mile
zone may be included as well, in order to make a more usable inventory. The targeted
archival sources include: the Hawai‘i State Historic Preservation Division records; State
and Federal shipwreck databases; the Bernice Pauahi Bishop Museum; internet
sources; maritime insurance companies records; the National Archives (e.g., customs
house records, wreck reports, Federal Admiralty court records, etc.); public, private, and
academic libraries; public and private maritime museums; historic newspapers
(including currently available translations of Hawaiian language newspapers), private
papers and collections; historic maps and navigation charts; archaeological site reports;
and federal, state, and private hangs and obstructions databases.
Though the shipwreck topics relatively new here in Hawai‘i, there is existing field
information in a variety of forms: numerous shallow water maritime archaeology site
4

�plans and surveys (SCUBA depths) by NOAA and University of Hawai‘i divers as part of
the Maritime Archaeology Survey Techniques courses; discoveries, images, and
informal reports by sport and technical divers; and multiple deep water site discoveries,
including high-definition video surveys, by the Hawai‘i Undersea Research Lab (HURL).
HURL was established in 1980 as a joint NOAA/University of Hawai‘i center with the
primary responsibility of advancing knowledge of the nation’s deepwater resources and
marine processes which are crucial for effective ecosystem-based management. HURL
has two three-person research submersibles; Pisces IV and Pisces V (Fig. 1).These are
battery-powered, one-atmosphere submersibles with a maximum operating depth of
2000 m (6,280 ft). They offer scientists direct observation through three view ports,
high-definition

video

cameras,

instrument

placement,

sample

collecting,

and

environmental monitoring. Though maritime archaeology and cultural resource
management has usually not been a priority for fully-funded missions, HURL has
investigated numerous maritime heritage properties during their pre-season training
dives, preparing both submersibles and pilots prior to the dive season (Fig. 2). Maritime
archaeologists have been able to take advantage of the excellent working relationship
between NOAA and the University of Hawai‘i, and the generosity and professionalism of
HURL Operations Director Terry Kerby and his staff, to gain unique data on deep water
discoveries.

Fig. 1 HURL 3-man research submersible PISCES V launching from
the submerged LRT.(C. Wollerman, HURL)
5

�Fig. 2 Deep water discoveries of naval aircraft circa 1938, one of many types
of resources found by the HURL team. (H. Van Tilburg, NOAA ONMS)
Several important documents and collections provide critical background information for
the UCH inventory, though some include only near shore (0-3mi) information. The 19891990 Hawaiian Fishpond Study including the islands of O‘ahu, Moloka‘i, Maui, Lāna‘i,
Kaua‘i, and Hawai‘i is the largest state-wide statistical survey of coastal fishpond field
data, supported by the Bishop Museum (DHM: 1989; 1990). Mifflin Thomas’s Hawaiian
Registered Vessels lists statistical and service data for selected ships of both the
historic Kingdom period 1800-1893 and subsequent Territory of Hawai‘i period 18931959 (Thomas, 1982). Thrum’s Hawaiian Annual 1842-1932, Honolulu features an
annual summary of marine casualties. Specific shipwreck losses can also be traced
through newspaper issues of the Pacific Commercial Advertiser (1856-1912) (later the
Honolulu Advertiser), as well as the local Star Bulletin (1912-2001).

Finally, naval

shipwreck and aircraft losses have been detailed in U.S. Shipwrecks in Hawaiian
Waters: an Inventory of Submerged Naval Properties (Van Tilburg, 2002) produced by a
grant from the Naval Historical Center in Washington DC (now known as the Naval
History and Heritage Command). Inventory work is continuing to build upon this
foundation.

6

�The existing and somewhat scattered field and archival inventory data is focused on 0-3
mile near shore resources and suggestive of three broad categories of cultural heritage
resources: 1) pre-western contact Native Hawaiian archaeological sites such as coastal
fishponds and fish traps; 2) 19th and early 20th century commercial transportation,
including whaling and sealing ships, Pacific cargo vessels, and inter island steamships
servicing the (former) Hawaiian plantations; and 3) military vessels, including surface
ships, submarines, and submerged naval aircraft. The offshore 3-200 mile OCS
inventory brings a new focus and new dataset to the fore.
Objective 2: Database of Historic Properties that could be adversely impacted by
Alteration of the Ocean View Shed
For Objective 2, NOAA sanctuary staff will conduct research in the office of the Hawai‘i
State Historic Preservation Division and develop a database of terrestrial properties that
could be visually affected from offshore renewable energy siting. The data to be
collected includes historic and archaeological information related to properties that are
nominated to, or are eligible for, listing on the U.S. National Register of Historic Places.
This may seem like an odd task for maritime archaeologists. For preservationists and
cultural practitioners, however, the connection is clear.
The National Register establishes criteria for measuring historical significance, an
important step in valuing and preservation heritage resources. Traditional Cultural
Properties, or locations associated with traditional beliefs or religious ceremonies, or
economic or artistic practices central in maintaining a community’s identity, may meet
National Register criteria and be protected (Shrimpton, 1990). Recently, the viewshed
or view plane of the ocean itself was interpreted as a type of historical “property” (Fig. 3).
Precedence was set in the review of the proposed Cape Wind (offshore turbine wind
farm) energy project in Nantucket Sound, Massachusetts (MMS, 2010). The Aquinnah
and Mashpee Wampanoag Native Tribes claimed that the proposed wind turbines had
the potential to degrade their essential view of the sunrise for religious ceremonies and
also the view of the ocean central in other rituals. In an island state like Hawai‘i, with an
active and engaged host culture, it is only natural that federal agencies begin to address
the issue of viewsheds of the ocean as they pertain to the cultural significance of
specific areas of the marine environment.
7

�Fig. 3 The raised Hawaiian temple at Pu`ukoholāHeiau National Historic
Site on the Island of Hawai`i, a place where cultural practices continue.
(H. Van Tilburg, NOAA ONMS)
Objective 3: Management Tool for Engaging Native Hawaiian Communities in
Identifying Significant Marine Areas
For objective 3, NOAA sanctuary staff will work with a Native Hawaiian Project
Facilitator to develop a consultative working group. The group will include members of
NOAA’s Maritime Heritage Program, the Facilitator, the BOEM contracting office
representative, and representatives from each of the main Hawaiian Islands (including
island districts and/or counties). The working group will coordinate and facilitate the
development of an analysis guide through a series of workshops, meetings, trainings,
and consultations, as necessary, held during the project. This analysis guide or
management tool will identify community heritage resource leaders, define common
terminology, establish protocols for handling sensitive issues, establish reciprocal datasharing for information validation, develop a list of topics that should be consistently
asked for by project proponents, and create a template for Hawaiian communities to
collect and hold information that can be queried internally with the ability to provide
summary results to external parties. That is a major paradigm shift. The project
proposes to grant communities greater ability to manage and control their own sensitive
8

�cultural resource information rather than automatically require them to reveal sensitive
information to government agencies. Information obtained from this project will provide
baseline information for Native Hawaiian communities, helping to recognize and
document marine areas of cultural importance. In short, the working group will develop
a guidance tool that will help local communities navigate through cultural management
discussions, particularly where those discussions involve sensitive resources and
critical marine areas.
The working group will then test the analysis document tool by conducting independent
case studies, identifying indigenous cultural landscapes within a pre-defined study area.
At its most basic, cultural landscapes are specific places where combinations of human
activity and natural forces have left a discernable mark or footprint on the environment
(Jensen et al., 2011). The landscape studies will begin with a Traditional Cultural
Property (TCP) and Traditional Ecological Knowledge (TEK) analysis of Native
Hawaiian sites and resources within the selected areas (Fig. 4). These case studies will
focus on areas that include coastal land-based, as well as offshore, areas of Native
Hawaiian significance. Each case study will incorporate an area of one or more
traditional Hawaiian ahupua`a, a land division developed by ruling chiefs of the islands
in the 15th century which typically runs from the mountain ridge to the fringing reef,
usually encompassing an entire watershed. The types of cultural resource information to
be identified include traditional cultural properties in a maritime context, information
related to traditional gathering, hunting, fishing and other subsistence and commerce
activities, as well as those related to spiritual and ceremonial sites and activities. The
working group, workshops, and case studies provide an analysis guidance tool that
(hopefully) will assist local communities in conducting their own maritime cultural
landscape assessments. Familiar heritage resources like shipwrecks do not
automatically rise to the fore here, unless those types of resources are valued by the
community itself. Significance, in this instance, is not defined by government mandates
and enforced from above, but rather is more reflective of local values and generated at
the grass-roots community level.

9

�Fig. 4 The emergent walls of the Hawaiian stone fish traps and fish pond at
Kaloko-Honokōhau National Historic Park. (H. Van Tilburg, NOAA ONMS)
Project Challenges and Questions
The ambitious and innovative approach represented by this maritime resource
assessment project raises interesting challenges for Hawai‘i’s cultural preservation
efforts. The project will not be easy to complete. Discussions regarding cultural
resources are always lengthy and highly charged in Hawai‘i, and this is a complicated
project inclusive of a large amount of public input in a process that has no precedent
among the islands. The fact that local communities, in Hawai‘i and elsewhere, often feel
disenfranchised by development interests and may perceive that their access to cultural
resources deteriorates over time, engenders an understandable amount of wariness
among the public. Those who are familiar with Hawai‘i’s history also know that the
United States was clearly implicated in the illegal overthrow of the Hawaiian Islands in
1893, for which the presidential executive office issued a formal apology 100 years after
the fact. They also know that the diseases that flourished in the wake of the Western
discovery of Hawai‘i in 1778, followed by subsequent social and economic upheaval,
devastated the Hawaiian population, cultural practices and traditions, and very fabric of
Hawaiian society. Cultural practices, identity, and cultural resources are therefore
inseparable, and managing cultural resources is a complex and critical challenge in the
islands.
10

�For exactly these reasons, this project attempts what may be an improvement on the
way that cultural resources have been assessed, managed, and ultimately protected in
the United States thus far. If successful, local communities may be more empowered in
resource management decisions that affect their islands.

Because the underwater

cultural heritage falls under the larger definition of cultural resources, and UCH does
include a wide variety of historic and prehistoric properties, BOEM has therefore
included project support for the Asia Pacific Conference on UCH 2014 and is one of the
main APCONF conference sponsors. The project obviously has a contribution to make
in understanding the underwater cultural heritage of Hawai‘i, and just as obviously, parts
of the project go way beyond the definition of “underwater cultural heritage”. Or do they?
Considering the intense level of cultural resource engagement locally in Hawai‘i, and
also considering the passage of the international UNESCO 2001 Convention on the
Protection of the Underwater Cultural Heritage, one might ask “where is the intersection
between these two efforts? Is there any? How much of what is considered “cultural
resources” in Hawai‘i is really included in the definition of UCH: “…all traces of human
existence that lie or were lying underwater and have a cultural or historical character”?
Clearly, shipwrecks are part of the UCH, whether or not they are popularly regarded as
cultural resources in Hawai‘i. And clearly, pre-Western contact lithic remains of stone
fishponds and traps, along with canoe anchors, artifacts associated with coastal villages,
and specific accumulations of ancient fishing tools, are part of the UCH resource base,
under “objects of prehistoric character.”But humans have been intentionally and
inadvertently shaping their environment, both terrestrial and marine, for a very long
time...much, much longer than the existence of any written definition of “traditional
cultural properties” or criteria from the National Register of Historic Places (Fig. 5). This
has led to the cultural landscape approach being used as the interpretive tool to
understand cumulative impacts to the environment in a more holistic fashion. Canall
these landscapes be UCH as well?

11

�Fig. 5 The plantation-era ruins of the industrial harbor at Mahukona, once
the entry port for the Kingdom of Hawai`i. The submerged steamship wreck
from 1913 lies to the left. The whole environment, harbor, and wreck, make
up the cultural landscape here.(H. Van Tilburg, NOAA ONMS)
One could pursue the merit of including or excluding a given resource as cultural
heritage for a long time. That is something of a theoretical exercise. Perhaps it would
be better, for our efforts in Hawai‘i, to approach the question from the local perspective
of the intended results. Definitions of landscapes and underwater cultural heritage and
cultural resources all serve a similar purpose: they are intended to promote the
understanding and preservation of resources that are valued for a number of reasons,
including maintaining cultural identity. Is it worthwhile to understand the cultural
resources and long-term impacts associated with traditional hunting, fishing, and
gathering activities in the context of potential UCH? Is it worthwhile to think broadly
about the definition of UCH, beyond the familiar shipwreck sites? The local answer is a
pragmatic “yes,” if by doing so, those “traces of human existence” that are valued by
communities as significant may have a better chance at being understood and protected.
Acknowledgements
The authors would like to thank the Bureau of Ocean Energy and Management for
making the project possible, and the dedicated staff of the National Marine Protected
Area Center for providing the impetus for the development of the cultural landscape
approach as it pertains to maritime heritage resources.

12

�References
Anon., 2012. Hawaii Ocean Resources Management Plan, Public Review Draft. Hawaii
CZM Program State Office of Planning, Honolulu.
DHM Planners Inc., 1989. Hawaiian fishpond study: islands of Oahu, Molokai, and
Hawaii / prepared by DHM Planners, Inc. and Public Archaeology Section, Applied
Research Group, Bernice Pauahi Bishop Museum, Honolulu.
DHM Planners Inc., 1990. Hawaiian fishpond study: islands of Hawaii, Maui, Lanai and
Kauai / prepared by DHM Inc., Public Archaeology Section, Applied Research Group,
Bishop Museum and Moon, O'Connor, Tam &amp; Yuen, Honolulu.
Honolulu Star Bulletin 1912-2001, Honolulu, Hawaii daily newspaper.
Jensen, J. O., Mather, R. and Gray, J., 2011. Viewing the Future through the Lens of the
Maritime Cultural Landscape. Sanctuary Watch, Fall: 2-3.
MMS (U.S. Minerals Management Service), 2010.Record of Decision: Cape Wind
Energy Project, Horseshoe Shoal, Nantucket Sound. U.S. Department of Interior,
Washington DC.
Pacific Commercial Advertiser 1856-1921, (becomes Honolulu Advertiser), Honolulu
Hawaii daily newspaper.
Shrimpton, R. H., (Ed.), 1990. National Register Bulletin: How to Apply the National
Register Criteria for Evaluation. U.S. Department of the Interior, National Park Service,
Washington DC.
Thomas, M., 1982. Hawaiian Interisland Vessels and Hawaiian Registered Vessels.
Seacoast Press, Santa Barbara.
Thrum’s Hawaiian Annual 1842-1932. Star-Bulletin Press, Honolulu.
UNESCO, 2012. Training Manual for the UNESCO Foundation Course on the
Protection and Management of Underwater Cultural Heritage in Asia and the Pacific.
UNESCO Bangkok Asia and Pacific Regional Bureau for Education, Bangkok.
Van Tilburg, H., 2002. U.S. Shipwrecks in Hawaiian Waters: an Inventory of Submerged
Naval Properties. Naval Historical Center, Washington DC.
Hans Van Tilburg holds a BA in geography from University of California Berkeley, an
MA in maritime archaeology/history from East Carolina University and a PhD in history
from the University of Hawai‘i, where he ran the graduate program in maritime
archaeology and history. Hans has taught courses in world maritime history and
13

�published over 30 articles and book reviews, as well as several books. He has served
as a consultant for UNESCO’s cultural heritage program and instructor for UNESCO’s
UCH Foundation courses. He is currently the maritime heritage coordinator and unit
diving supervisor for NOAA’s Office of National Marine Sanctuaries in the Pacific.
Dave Ball is the Pacific Region Historic Preservation Officer and Diving Safety Officer
for the Bureau of Ocean Energy Management (BOEM). Before joining BOEM he worked
for several archaeological firms in the Pacific Northwest. He received a BA in
anthropology from Sonoma State University in 1992 and an MA in anthropology from
Florida State University in 1998. Dave has over 20 years’ experience in archaeology
and has directed field research on both terrestrial and underwater archaeological sites
across the country, including inundated prehistoric sites, World War II shipwrecks, and
deepwater shipwrecks in the Gulf of Mexico. He is currently serving on the Board of
Directors for the Advisory Council on Underwater Archaeology.

14

�</text>
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                  <text>In 2009, responding to the effort to protect the significant natural and cultural resources within the marine environment for the benefit of present and future generations, the U.S. National Marine Protected Areas Center formed a Cultural Heritage Resources Working Group to provide expert advice on improving the conservation and management of maritime heritage resources. The resulting White Paper provided a series of recommendations to both the U.S. Department of Commerce and the Department of the Interior, including new definitions for cultural heritage, marine cultural resources, tribes, indigenous peoples, and cultural landscapes. Central to these recommendations was a strong endorsement for the Cultural Landscape Approach in the understanding and management of maritime heritage resources (or UCH). Subsequently, the National Oceanic and Atmospheric Administrationâ€™s (NOAA) Maritime Heritage Program has adopted the recommendations of this paper and is implementing a â€œmaritime cultural landscapeâ€ approach to the management of cultural resources within the National Marine Sanctuary System. Also as a part of this initiative, NOAA and the Bureau of Ocean Energy and Management (BOEM) have teamed up to support maritime cultural landscape studies of heritage resources by Native American Tribes and Native Hawaiian communities in the Pacific region. These projects on the U.S. West Coast and in the Hawaiian Islands demonstrate the necessity of adapting a broader range of recognized cultural resources and a more inclusive and participatory management and preservation process. Charismatic resources like historic shipwrecks will always provide unique information for archaeologists and historians, but we do ourselves a disservice if we focus solely on these types of properties, and neglect other perspectives and the broader nature of all types and traces of human existence that lie underwater.&#13;
Participants in this session will focus on the status of these ongoing ground-breaking projects, the advantages of a broader and more inclusive approach compared to the previous cultural heritage management paradigm in the U.S., and the challenges that this creates.</text>
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                <text>Understanding the types and locations of significant archaeological and cultural resources is essential to their protection. NOAA and the Bureau of Ocean Energy and Management (BOEM) have teamed up to support an assessment of historic properties and cultural resources in the main Hawaiian Islands. Objectives for this project include: 1) a database of verified, reported, and potential submerged cultural resources in the Hawai`i Outer Continental Shelf; 2) a database of historic properties that could be adversely impacted by alteration of the ocean viewshed; and 3) a management tool for engaging Native Hawaiian communities in identifying significant marine areas for offshore energy development planning purposes.</text>
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                    <text>DISCOVERY AND MANAGEMENT OF THE WRECK OF USS ALBACORE (SS-218)
1

Ivor Mollema (Naval History and Heritage Command, Archaeologist)
Tamaki Ura, PhD (University of Tokyo, Professor Emeritus)
3
David Johnston (Naval History and Heritage Command, Naval Photographic Interpreter)
4
Stephen Katona (Naval History and Heritage Command, Independent Researcher)
2

ABSTRACT
The wreck of USS Albacore (SS-218) was discovered on 25 May 2022 and resurveyed in October by Dr Tamaki
Ura’s team of researchers at La Plongée Deep Sea Engineering Society. Following the initial discovery,
volunteer researchers for the Naval History and Heritage Command (NHHC) examined recorded footage of the
wreckage to identify the wrecked boat. Key features identified the wreckage as belonging to an American
submarine from the Second World War. Further investigation and archival research identified the submarine as
the American Albacore, a Gato class submarine lost in action in Japanese waters on 7 November 1944. The U.S.
Navy formally confirmed the identity of the wrecksite as the Albacore in February 2023.
After an overview of the vessel’s history, this paper covers the initial search and discovery of Albacore during
2022. In particular, the use of a Remotely Operated Vehicle demonstrates the viability of this approach for
initial identification assessments of deep wrecks. An outline of the identification process is provided that covers
key features of Albacore observed on both the underwater footage and archival imagery. The identity
confirmation process and media outreach efforts surrounding the discovery are covered, followed by a
discussion on the continuing management and treatment of Albacore.
Key Words: Submarine, Second World War, Japan, US Navy

LIST OF IMAGES
Figure 1. Albacore at the final stages of its final refit at Mare Island Naval Shipyard, completed in May, 1944 (USN
Photograph 19-N-65354).
Figure 2. The vent holes that allowed researchers to identify the wreck as Albacore as captured during the 2022 survey led
by Dr. Tamaki Ura (Niconico Live, October 2022).
Figure 3. The SJ Radar Mast that helped confirm the identity of Albacore as captured during the 2022 survey led by Dr.
Tamaki Ura (Niconico Live, Oct. 2022).

INTRODUCTION
The USS Albacore (SS-218) is one of 52 American submarines lost during WWII. She served on ten
war patrols and sank at least 10 enemy vessels, with a potential for three more unconfirmed sinkings.
This includes six enemy combatant ships and ties Albacore for the most sinkings of enemy combatant
ships by any American submarine during WWII. Reported lost at the end of 1944, Albacore
was discovered by a team of researchers from the University of Tokyo in May 2022 (Johnston,
Katona, and Iwasaki 2022). A team of researchers associated with the Naval History and Heritage
Command (NHHC) reviewed the collected footage and compared it with archival imagery and
records to determine the identity of wreckage as belonging to Albacore. NHHC archaeologists
verified the identity of the wrecksite and corroborated the initial assessment of the wreck’s
identity. The discovery, investigation, and announcement (NHHC 2023) laid out a template for
approaching wreck sites in the future, with particular relevance to contemporary submarines.
HISTORY OF USS ALBACORE (SS-218)
Albacore was laid down on 21 April 1941 at Groton, Connecticut by the Electric Boat
Company (“Albacore II (SS-218)”). It was launched on 17 February 1942 and commissioned on 1
June of the same year. Following the submarine’s shakedown cruise, it crossed the Panama Canal
and arrived in Pearl Harbor in mid-1942. She departed for her first of 11 war patrols on 28
August 1942 in the waters surrounding Truk. This patrol ended on 20 October 1942 with Albacore’s
return to Midway for a refit. During her inaugural
war patrol, Albacore experienced her first
1
combat actions when she

�engaged two enemy cargo vessels on 13 September 1942 with damage to the leading vessel, but
missed the second. She then proceeded to make a night surface attack on an enemy tanker on 1
October 1942, and heavily damaged it. On 9 October, three Japanese warships, including one Zuikaku
class carrier, pursued Albacore for most of the day. The next day, Albacore crew sank an enemy
freighter after shaking off pursuers. Two Japanese submarine chasers, supported from the air,
encountered Albacore on 11 October but broke off the chase after seven hours of silent running by
Albacore. She departed the area the next day and headed to Midway Atoll for the first refit.
Departing Midway for her second war patrol on 11 November 1942, Albacore set out for the waters
off New Britain and New Guinea. Rebuffed from her first assigned patrol area by Japanese destroyers,
she started patrolling the area around Madang harbour in New Guinea. Two enemy vessels were
spotted: one destroyer and one suspected transport. Releasing a salvo of torpedoes, the Albacore crew
sank the transport on 18 December 1942. On her arrival in Brisbane on 30 December 1942 her crew
learned they had sunk the Japanese light cruiser Tenyru of 3300 tons. This was only the second
Japanese cruiser sunk by an American submarine during WWII, and succeeded in weakening the
enemy hold on New Guinea. This engagement was certainly one of Albacore’s most significant.
After receiving an overhaul on her main engines, Albacore departed for her third patrol on 20 January
1943. During this patrol, the crew sank one destroyer and one frigate, with suspected damage to
another vessel. Her fourth patrol achieved no confirmed enemy sinkings, although she reportedly
engaged several enemy convoys. The next war patrol, this time under the command of Lt. CmDr
Oscar Hagberg, achieved similar results. Albacore’s crew sank the ship Heijo Maru on 4 September
1943. Her seventh patrol would see Albacore come close to destruction. She pursued a Japanese
convoy, but was accidentally bombed by a plane from the US 5th Air Force on 6 November. Although
she received no damage during this attack, Albacore did lose contact with her quarries. On 10
November 1943, she was once again the victim of friendly fire when she was bombed by an American
aircraft and suffered significant damage. All auxiliary power was knocked out, and the main induction
valve was broken. For two and a half hours, she continued to move between 30 and 400 feet before
restoring her trim and returning to the surface. She completed her patrol and returned to Brisbane on 5
December 1943, where she also received a new commander in Lt. Cmdr. James Blanchard. She
completed one more patrol, before setting sail for Pearl Harbor on 22 February 1944. Three days later,
she sailed for Mare Island Navy Yard for her final overhaul.
She arrived back in Pearl Harbor on 13 May and departed for her ninth war patrol on 29 May in
waters west of the Marianas Islands. She engaged no enemy ships during this patrol. Albacore shifted
her position to the south on 18 June to support the American landings on Saipan. Admiral Nimitz
planned to get the submarine, along with several others, to intercept a Japanese relief force. Albacore
encountered a large concentration of Japanese Navy ships, and torpedoed near the aviation gasoline
tanks of the aircraft carrier Taiho. The loss of one of Japan’s largest and newest aircraft carriers, along
with a second sunk by USS Cavalla that same morning, caused the rest of the Japanese fleet to retreat
to the relative safety of Okinawa, facilitating the subsequent landing of the U.S. forces in Guam,
Tinian, and Saipan. Albacore would go on to sink two more ships after this action.
Albacore departed Midway Atoll for her final war patrol on 28 October 1944. This was the last time
anyone received any communications from the submarine. A Japanese report, issued by the Japanese
Ominato District Guard Unit, references an underwater explosion off of Hokkaido, Japan. Forces at
Ezan Lighthouse and aboard Fukuei Maru #7, both reported an explosion a few miles off the coast on
7 November 1944. NHHC volunteer researchers Yutaka Iwasaki and Stephen Katona triangulated
these two sightings to develop a predicted location for the wreckage. The same records reported
details of surface debris found at the explosion site. One winter jacket or jumper was found with the
marking “ALB-5” on the back. This is presumed to be an abbreviated form of Albacore and used to
identify the clothing as belonging to the submarine. A pair of white shorts, labelled with “ASK,” was
also found. These initials match those of Arthur Star Kruger, a Seaman 2 nd Class who was listed as a
member of the crew of Albacore at the time of her demise. Associated with the clothing items were
also large amounts of heavy oil, cork, bedding, and American food supplies. This evidence, coupled
2

�with later video evidence collected by Dr Ura and reviewed by David Johnston and Steve Katona,
later confirmed the identity of this wreck as belonging to Albacore. With no outgoing
communications received from Albacore, she was ultimately declared lost on 21 December 1944 and
stricken from the Naval Vessel Register on 30 March 1945.
Over her relatively short career, Albacore conducted 11 war patrols and is credited with 10 sinkings
against enemy vessels, with another three not yet confirmed. She earned nine battle stars and four
Presidential Unit Citations (PUC). The submarine received the PUC for her second, third, eighth, and
ninth patrols. Six of her 10 sinkings were against enemy combatant ships, ranking her as one of the
most successful submarines against enemy combatants during WWII.
DISCOVERY OF SITE USS ALBACORE
Following archival research and location data in Japanese records, Dr Tamaki Ura and his team
developed a survey pattern covering the suspected area of Albacore’s sinking. They completed
surveys in the Shiriyaski Sea between Honshu and Hokkaido, Japan (Johnston, Katona, and Iwasaki
2022). On 25 May 2022 two multibeam systems were used to develop a bathymetric map of the area,
while a towed system equipped with side scan sonar was used to develop a clearer image of the
seafloor and any wreckage still located there. Dr Ura’s team found a wreck, about 50 metres in length.
After identifying a shipwreck site, Dr Ura’s team conducted underwater surveys using ROVs on 26
May and 2 October 2022 (Johnston, Katona, and Iwasaki 2022). All survey activity was broadcasted
live via internet (Nico Nico News, May and October 2022). The initial survey attempts in May
encountered difficulties brought on by the harsh underwater surroundings and poor visibility. The
depth, over 200 metres, also complicated matters. Despite difficulties, several images suggested the
discovery of an American submarine. The confirmed location of the shipwreck was within one
nautical mile of the location of the underwater explosion reported by Japanese forces off Hokkaido on
7 November 1944. Dr Ura’s team returned with volunteer researchers and archaeologists from NHHC,
in October 2022 with a larger and more powerful ROV to confirm the identity of the wreck as
Albacore.
The data collected on these two trips showed a shipwreck split, as the fore part was lost and the aft
end was buried in the sand. The break occurred forward of the conning tower fairwater. The centre
section, including the conning tower and its aft part, was surveyed by the ROV. The shipwreck is
heeled over to starboard about 5 degrees. The bridge has been smashed down to the port side of the
submarine. Many fishing nets and marine concretions cover the wreck.
ANALYSIS OF ALBACORE FOOTAGE
Unlike surface vessels, there are a number of challenges facing those attempting the identification of
American submarine wrecks. WWII submarines typically had little to no markings to distinguish
themselves. Surface vessels usually have their name and assigned numbers marked in several
locations. In this case, only the visual modifications, outlined below, and some deductive reasoning
guided NHHC researchers who relied heavily on historic photographs from the Mare Island Navy
Shipyard.
Volunteer researcher David Johnston reviewed the footage collected by Dr Ura’s team with location
data derived from Japanese historical reports. As mentioned above, the official ship history provided
by the Dictionary of American Naval Fighting Ships (DANFS) alongside archival material confirmed
that Albacore underwent its last major refit at the Mare Island Navy Yard in California starting on 25
February 1944. She departed Mare Island Navy Yard on 5 May 1944. A collection of U.S. Navy
photographs shows Albacore during its final overhaul at Mare Island Navy Yard. Figure 1 shows
several modifications made to the submarine and highlights three as they relate to the video analysis

3

�Figure 1. Albacore at the final stages of its final refit at Mare Island Naval Shipyard, completed in May, 1944 (USN
Photograph 19-N-65354).

Figure 2. The vent holes that allowed researchers to identify the wreck as Albacore as captured during the 2022
survey led by Dr. Tamaki Ura (Niconico Live, October 2022).

4

�Figure 3. The SJ Radar Mast that helped confirm the identity of Albacore as captured during the 2022 survey led by
Dr. Tamaki Ura (Niconico Live, Oct. 2022).

(Katona and Johnston 2022). A watertight gun ammunition locker, containing rounds for the deck
gun. This can be seen on the aft port side of the conning tower fairwater, shown as feature four in the
accompanying photograph. It is likely that an identical locker existed on the starboard side as well.
Second, NHHC researchers noticed the removal of steel plates on the upper edge of the fairwater. The
removal revealed the structural I-beam ribs shown as feature six in the photograph. Finally, one of the
most important aspects is labelled as feature seven in the image. A line of vent holes drilled along the
upper corner of the superstructure on both sides of the submarine allowed air to escape the
superstructure faster, speeding diving times (Figure 2). Another key identifying feature is the SJ
Radar antenna mounted on Gato class submarines like Albacore. Based on the Mare Island overhaul
photographs, the SJ radar mast was mounted forward of the periscope shears, and this is where it was
found on the wreck (Figure 3). SJ Radar systems were installed on most USN submarines between
1942 and 1944. This system was key to differentiating Albacore from any submarines of different
nationalities in the area. The SJ Radar dish was unique to American submarines in the Pacific theatre,
and clearly differentiated it from British, Dutch, and Soviet submarines that could also have operated
in the same area as Albacore.
All of the aforementioned features were identified by co-author Johnston during his review of the
footage collected by Dr Ura’s team. The most informative features included the SJ Radar system and
the vent holes along the upper edge of the superstructure. Researchers also identified one of
Albacore’s 20 mm anti-aircraft gun mounts, affixed during a previous refit, and the exposed ribs

5

�revealed in the conning tower during her final refit. Some additional features, including possible
hatches and ladders, were also documented.
These observed features, many which clearly differentiated Albacore from any other contemporary
submarine lost in the area, provided sufficient evidence for archaeologists at NHHC to confirm the
identity of Albacore’s remains. The SJ radar system established the remains as those of an American
submarine, while features installed/opened during its final refit in early 1944 set it apart from any
other American submarines lost in the area. The combination of archaeological documentation,
historical records, and location data provided the necessary confidence for NHHC to assert the
submarine wreck’s identity.
ANNOUNCEMENT AND OUTREACH
Coupled with the first press release (NHHC 2023) were announcements on Facebook, Instagram,
Twitter, and LinkedIn. The total number of views in the first four days reached 269,657 across all
NHHC platforms. The largest number of responses was on Twitter, followed by Facebook and
Instagram. The press’ response to the NHHC announcement was also encouraging. Several domestic
and international outlets, including NPR, CNN, Fox News, Popular Mechanics, and Science, ran
features. Outside the United States, the story was picked up by Spanish, Hungarian, Polish, Italian,
French, Japanese, and Vietnamese publications.
NHHC’s volunteer researchers also coordinated with a number of organisations focused on research
and preservation of the history of lost WWII submarines and their crewmen. In particular, those
involved in the organisation On Eternal Patrol (OEP), website that records lost servicemen of
American submarines, worked to find next of kin of Albacore’s crew members (OEP 2023). NHHC
supported these efforts by issuing a letter on the discovery signed by the Command’s Director that
could be forwarded to any next of kin on the website. Efforts are underway to organise a memorial
event involving next of kin in the near future.
MOVING FORWARD: WHAT’S NEXT?
The NHHC’s experience with Albacore has illustrated the effectiveness of collaboration when
addressing future submarine discoveries. Research partners, such as Dr Ura, spearheaded research
efforts that led to the discovery of a wreck of interest, while he gained experience with submarine
wreck investigations. NHHC volunteer researchers, lending their time and analytical skills, also
gained valuable experience and insight into the methods used to identify submarines. Finally, NHHC
archaeologists, historians and archivists lead to the wreck identity confirmation. In tandem with
partners, NHHC then coordinated the associated public announcement. This collaborative approach
allowed for a pooling of knowledge, expertise, time and resources that increased confidence in and
accelerated the official confirmation of the identity of the wreck. Both of these facets are crucial,
allowing for the public to be informed in a timely manner of the site’s importance, while at the same
time ensuring protective measures can be applied, which now constitutes a sunken military craft under
the jurisdiction of the Department of the Navy. Further disturbance must be sanctioned by NHHC.
At present, NHHC has no plans to recover Albacore, or any part of it. The sea is considered a fit and
final resting place for U.S. Navy sailors. The focus now shifts to the continued preservation of this
war grave.

6

�BIBLIOGRAPHY
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II
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April

28,

2023.

The Society La Plongee for Deep Sea Engineering. “Find US Submarine ‘Albacore’ Sunk off Hokkaido.” Academist.
Accessed April 29, 2023. https://academist-cf.com/projects/187?lang=en.
Johnston, David, and Steve Katona. 2022. “Addendum to the Report ‘Evaluation of the Wreckage of USS Albacore (SS218)’ Dated October 2022.” Washington DC.
Johnston, David, Steve Katona, and Yutaka Iwasaki. 2022. “Evaluation of the Wreckage of the USS Albacore (SS-218).”
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Katona, Stephen J., and David L. Johnston. 2022. “Critical Features for Identification of USS Albacore (SS-218).”
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Nico Nico News. “Niconico Live: Finding the Lost Submarine “ALBACORE.” May 25-26, 2022. Accessed April 28, 2023.
https://live.nicovideo.jp/watch/lv326919568.
Nico Nico News. Niconico Live: Finding the Lost Submarine “ALBACORE.” October 2, 2022. Accessed April 28, 2023.
https://live.nicovideo.jp/watch/lv336612796.
OEP On Eternal Patrol. “On Eternal Patrol.” Accessed April 29, 2023. https://www.oneternalpatrol.com/.
NHHC Naval History and Heritage Command. “Wreck Site Identified as WWII Submarine USS Albacore (SS 218).”
Accessed April 28, 2023. https://www.history.navy.mil/news-and-events/news/2023/nhhc-identifies-albacore-wrecksite.html.

7

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