EFTA01102170.pdf
dataset_9 pdf 1.1 MB • Feb 3, 2026 • 7 pages
MARINE RESOURCES
The island of Great St. James is located off the eastern end of St. Thomas. The island is
surrounded by seagrass beds, coral colonized bed rock, and coral colonized pavement. The
northeastern bay is shallow and has very dense seagrass beds the bay terminates in a sandy beach.
There are scattered hard bottom areas along the west shoreline and a shallow cobble/seagrass area
along the eastern shoreline.
Survey Methods
Surveys were conducted with snorkeling equipment and scuba to evaluate the habitats present. Aerial
photographs were utilized to help provide an overview of the habitats and changes over time. The NOS
Benthic Habitat map was reviewed and was found to accurately depict the near shore habitat types
present around Great St. James. The environmental consultant was very familiar with the bay have
done numerous surveys in the bay in the past. The recent damage to the dense seagrass beds was
immediately apparent.
Figure 1: LOCATION OF GREAT ST. JAMES DOCK 18° 18.745'N64° 49.589'W
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Figure 2 NOAA Benthic Habitat Map
Legend
NE Bay Benthic Habitats C Cobble/Seagrass
Exestna Dock Location O Coloinzed Hardbottom
• Seagrass beds - Tbalassa - Syrin9aclum
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onot 2016 Da4000be
LIDO ft
Figure 3. Benthic Habitat Map
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Findings
During a due diligence survey in January prior to Great St. Jim, LLC taking possession of the island it was
noted that there appeared to be a considerable amount of seagrass disturbance offshore. During survey
in February and March of 2016, this damage was document.
The northeastern bay is a well-protected shallow northern bay where the existing dock is located. This
bay is colonized by seagrass, Thalassic testudinum, Syringodium filiforme and Halodule wrightii. The
densest beds lay near shore and to the east of the dock. The peninsula to the east of this point is
surrounded by rocky headlands and is a very exposed environment. The rocky cliffs extend below the
sea surface and due to the intense wave action the shallowest areas are not colonized. By a depth of 8'-
10' the rocky substrate becomes colonized by a wide variety of corals and sponges. The slope is steep
offshore and the water reaches a depth of 40' to 50' relatively close to shore. The rocky slope gives way
to a cobbly then sandy bottom and there are sparse to moderately dense seagrass beds that extend
seaward.
When surveys of the bay were done in 2006 the seagrass extended under the dock. In 2016 there are
now large depressions around the dock as much as 9' in depth off the end of the dock and there are
large blowouts in the beds along the shoreline to the north. This appears to have been happening over
time as documented by the Google aerial photographs.
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Google earth N
Inag. • 2onsogratgad. 400 ft
GSJ 3.13.2014
Enating Dock
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:O16Ogtar.. 400
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The blowouts are now far worse than what is shown in the latest photograph.
Beds now from end of dock
xisting dock, note poor water quality
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arge blow outs
here were dense Thalassia beds under the dock in
2006.
here is no longer any seagrass immediately around the
dock.
here is loose seagrass detritus rolling in the surf along
the beach.
IMPACT OF DOCK MAINTENANCE AND INSTALLATIN OF RO LINE
The maintenance of the existing dock and the installation of the RO line should have no impact to the
existing environment.
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We however felt it was extremely important to document the condition the bay was found in when the
new owner took possession of the island. The bay which previously had dense seagrass beds up and
around the dock and along the shoreline, now had poor water quality and huge blowouts and
depressions along the shoreline. The new owner is in no way responsible for these impacts that
occurred over the last several years the previous owner had the island, especially over the last several
month when they took equipment off the island by barge.
here are large amounts of loose seagrass in the middle
of the depressions.
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- Feb 3, 2026