ENVIRONMENTAL ASSESSMENT
ENVIRONMENTAL ASSESSMENT
FOR THE CONSTRUCTION OF TWO DOCKS AND A BARGE
LANDING
ON GREAT ST. JAMES ISLAND
U.S. VIRGIN ISLANDS
PREPARED FOR
GREAT ST. JIM, LLC.
PREPARED BY
BIOIMPACT, INC.
BOX 132
KINGSHILL, ST. CROIX
U.S. VIRGIN ISLANDS 00851
[email protected]
REVISED JANUARY 2018
EFTA00802723
TABLE OF CONTENTS
SECTION
1.00 NAME AND ADDRESS OF APPLICANT PAGE
1
2.00 LOCATION OF PROJECT 1
2.00.1 Location and Agency Review Map 1
2.00.2 Vicinity Map 2
3.00 ABSTRACT 2
4.00 STATEMENT OF OBJECTIVES SOUGHT BY THE
PROPOSED PROJECT 4
5.00 DESCRIPTION OF PROJECT 4
5.01 Summary of Proposed Activity 5
5.OIa Purpose of Project 5
5.01b Presence and Location of Any Critical Areas and Possible Trouble Spots 6
5.OIc Method of Construction 10
5.OId Provisions to Limit Site Disturbance 11
5.OIe Sediment Control Methods to be Implemented 11
5.01 f Schedule for Construction Activities and Implementation
of Sediment Control Measures 11
5.OIg Maintenance of Sediment and Siltation Control Measures 11
5.02 Exhibits and Drawings 12
5.03 Project Work Plan/Schedule 18
6.00 ECOLOGICAL SETTING AND PROBABLE PROJECT IMPACT
ON THE NATURAL ENVIRONMENT 19
6.01 Climate and Weather 19
6.02 Landform, Geology, Soils and Historic Land Use 23
6.03 Drainage, Flooding and Erosion Control 28
6.04 Fresh Water Resource 32
6.05 Oceanography 32
6.06 Marine Resources and Habitat Assessment 40
6.07 Terrestrial Resources 50
6.08 Wetlands 52
6.09 Rare and Endangered Species 59
6.10 Air Quality 60
EFTA00802724
SECTION PAGE
7.00 IMPACT OF THE PROPOSE PROJECT ON THE HUMAN
ENVIRONMENT 62
7.01 Land and Water Use Plans 62
7.02 Visual Impacts 62
7.03 Impacts of Public Services and Utilities 62
7.04 Social Impacts 63
7.05 Economic Impacts 63
7.06 Impacts on Historical and Archaeological Resources 64
7.07 Recreational Use 64
7.08 Waste Disposal 64
7.09 Accidental Spills 64
7.10 Potential Adverse Effects, Which Cannot be Avoided 64
8.00 MITIGATION PLANS 64
9.00 ALTERNATIVES TO PROPOSED ACTION 64
10.00 RELATIONSHIP BETWEEN SHORT AND LONG TERM
USES OF MAN'S ENVIRONMENT 66
11.00 REFERENCES 66
Appendix A
Qualification Statements of Preparers
Bioimpact, Inc.
BCSC Dispova
Appendix B
Coral Relocation and Mitigation Plan
Appendix C
Water Quality Monitoring
Appendix D
Tree Boa Protection Plan
Appendix E
Pearson Artificial Reef Information
ii
EFTA00802725
1.0 NAME AND ADDRESS OF APPLICANT
Great St. Jim, LLC
9053 Estate St. Thomas, Suite 101
St. Thomas, VI 00802
2.0 LOCATION OF PROJECT
Great St. James Island is located to the southeast of the island of St. Thomas. The
geographic coordinates of the island are 18° 18.583' N and 64° 49.752' W. The
Temporary Barge Landing is located at 18° 18.902' N and 64° 49.802'W, the western
Christmas Cove Dock is located at 18° 18.804' N and 64° 49.876' W, and the southern
barge landing/dock is located at 18° 18.355' North L and 64° 49.659' W. The Location
and Agency Review Mao and Vicinity Map follow.
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Figure 2.01 Agency Review Map, the entire island of Great St. James is within CZM first
tier jurisdiction. The dock locations on the island are indicated.
EFTA00802726
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Figure 2.02 Vicinity Map showing Great St. James Island in relationship to the
surrounding area.
3.00 ABSTRACT
Great St. Jim, LLC is seeking to construct two docks, one of which is a combination
dock/ barge landing, and a temporary barge landing to provide access to Great St. James
Island.
There is currently a small pile-supported dock located within Shallow Bay on the north
side of the island. The bay is very shallow and vessels accessing the dock have damaged
the shallow seagrass beds within the bay. At one time, there had been a concrete
bulkhead at the shoreline with a small floating dock. The previous owner submitted an
application for the existing dock which was approved by DPNR's Division of Coastal
2
EFTA00802727
Zone Management but was not approved by the U.S. Army Corps of Engineers due to
objections by National Marine Fisheries because of the shallowness of the bay. The dock
was constructed by the previous owner despite not receiving the federal permit and
notices were issued by the USACE requesting the removal of the unpermitted structure.
The dock however was never removed. The applicant understands the issues with the
existing dock and is proposing to remove the dock as soon as another dock is constructed
and usable.
A detailed study was done around the entire island to determine suitable locations for
dock location. All ESA listed corals were located and docks and barge landings were
designed to avoid these corals.
A temporary barge landing is being proposed on the northwestern facing beach. This site
is to the west of the salt pond and the associated wetlands. This a shoreline ramp which is
25 feet (ft) wide and 40ft in length extends to the Mean Water Line. The landing is free
of both coral and seagrass colonization. The landing is excellent for short term transfer of
material or equipment. The site is well protected from normal wave action but is
periodically impacted by wave action from ferries which travel through current cut
between Great St. James and St. Thomas. The wakes from these vessels make it an
unattractive site for mooring a barge for any length of time at the site. This landing can be
quickly constructed and utilized while the combination dock and barge landing on the
southeastern side of the island is constructed.
The western dock is proposed on the northern end of Christmas Cove. Historically there
was a dock in this location and there are still old concrete piles lying in the shallows of
this site. The proposed dock will be 10ft in width and 195ft in length extending 187ft
from mean low water (MLW) and 193ft from mean high water (MHW). The dock
extends beyond the nearshore hardbottom to a depth of 15ft out in the uncolonized sand
to allow for safe dockage for deeper vessels.
The southern dock is located off the point closest to Little St. James. The dock is "L"
shaped and is 20ft wide (to allow for barge landing) and 150ft in length extending 141ft
from MLW and I48ft from MHW, the "L" then turns east and extends 100ft by 20ft. A
wave attenuating/reef creating system is proposed beneath the dock which will allow for
more protected docking inside the dock when seas from the south are rough. The dock
has 9ft of water depth of the southern end and 711 to 8ft on the inside of the "L". The
dock has been designed so that barges can approach and land on the end of the dock
while vessels can dock along the "L".
After the hurricane Irma in 2017 the owner of the Great St. James assisted many of his
employees and their families who had lost their homes and housed people on the island.
In order to bring in emergency supplies, two small barge ramps were created near the
locations of both proposed docks; one in Christmas Cove and one off the closest point to
Little St. James. Both consisted of coral rubble and boulders pushed out into the water
approximately 10ft. and both were 15ft. wide. These were noticed by the USACE during
3
EFTA00802728
aerial surveillance and the USACE requested the removal of the structures as well as the
removal of some fill material which was deposited into the fringing wetland area while
creating access to the southern emergency ramp.
The southern ramp has been removed and the fill has been removed from the wetland
area and white mangrove seeds have been being spread in the wetland and seedlings are
beginning to sprout.
The applicant is requesting that he be allowed to keep the emergency ramp in Christmas
Cove until such time a permit is granted for the proposed barge ramp. This will facilitate
the bringing of materials and supplies to the island until such time a permanent ramp can
be built.
4.00 STATEMENT OF OBJECTIVES SOUGHT BY THE PROPOSED PROJECT
Great St. Jim, LLC is proposing to construct a temporary barge landing and an access
dock on the western side of the island to be used for worker and guest access to the island
and a combination barge landing/dock on the southeast side of the island on the point
closest to Little St. James. The existing dock in Shallow Bay will be removed as soon as
one of the docks is functional. The applicant is requesting to keep the emergency rubble
ramp in Christmas Cove until such time that the proposed barge landing can be permitted
and constructed.
5.0 SUMMARY OF PROPOSED ACTIVITY
Great St. Jim, LLC is seeking to construct two docks, one of which is a combination
dock/barge landing, and a temporary barge landing to provide access to Great St. James
Island. A detailed study was done around the entire island to determine suitable locations
for the dock locations and the sites with the least environmental impact were chosen.
A temporary barge landing is being proposed on the northwestern facing beach. This site
is to the west of the salt pond and the associated wetlands. This a shoreline ramp which
is 25 feet (ft) wide and 40ft in length extends to the Mean Water Line. Two bollards will
be placed to either side of the ramp and two moorings will be installed 75ft offshore on
either side of the ramp in just over 7ft of water depth. The mooring will be installed
using helix anchors and will use floating lines will be used to avoid seafloor disturbance
when the moorings are not in use. The landing is free of both coral and seagrass
colonization. The landing is excellent for short term pick up and drop off of material or
equipment. The site is well protected from normal wave action but is periodically
impacted by wave action from ferries which travel through current cut between Great St.
James and St. Thomas. The wakes from these vessels make it an unattractive site for
mooring a barge for any length of time at the site. This landing can be quickly
constructed and utilized while the combination dock and barge landing on the
southeastern side of the island is constructed.
4
EFTA00802729
The western dock is proposed on the northern end of Christmas Cove. Historically there
was a dock in this location and there are still old concrete piles lying in the shallows of
this site. The proposed dock will be 10ft in width and 195ft in length extending 187ft
from mean low water (MLW) and 193ft from mean high water (MHW). The dock will
connect to an access slab 12ft long and 2' thick. All the ESA listed coral species within
the area were located and the dock footprint avoids all ESA listed species. The dock
extends beyond the nearshore hardbottom to a depth of 15ft out in the uncolonized sand
to allow for safe dockage for deeper vessels.
The southern dock is located off the point closest to Little St. James. Again, all of the
ESA corals were located, and the dock was designed to avoid these corals. The dock is
shaped and is 20ft wide (to allow for barge landing) and 150ft in length extending
141ft from MLW and 148ft from MHW, the "L" then turns east and extends 10011 by
20ft. A wave attenuating/reef creating system is proposed beneath the dock which will
allow for more protected docking inside the dock when seas from the south are rough.
The dock has 9ft of water depth of the southern end and 7ft to 8ft on the inside of the
"L". The dock has been designed so that barges can approach and land on the end of the
dock while vessels can dock along the "L".
The existing dock in the shallow northern bay will be removed as soon as one of the other
two docks is functional. The dock will have the decking removed, and then the stringers
and pile caps will be disassembled. This will all be done by workers from the shore.
Once only the piles remain, a shallow draft barge will come into the bay and pull the piles
out. If for some reason the piles cannot be pulled they will be cut off by commercial
divers at the mudline.
As soon as the proposed barge landing can be constructed the applicant will remove the
emergency ramp from Christmas Cove. This will be done from the shoreline using a
backhoe which will pull the cobble back on to the beach and spread it out along the back
beach. The larger riprap boulders will be taken inland to use in landscaping.
5.0Ia Purpose of Project
The purpose of this application is to provide access to the island of Great St. James.
Great St. Jim, LLC is proposing to construct a temporary barge landing to be used during
the construction of the other docks, an access dock on the western side of the island to be
used for worker and guest access to the island, and a combination barge landing/dock on
the southeast side of the island on the point closest to Little St. James. The existing dock
in Shallow Bay and emergency ramp in Christmas Cove will be removed as soon as one
of the docks and proposed barge ramp is functional.
5
EFTA00802730
5.01b Presence and Location of any Critical Areas and Possible Trouble Spots
The island of Great St. James is within the Vessup Bay/ East End Red Hook Area of
Particular Concern (APC) (Figure 5.01.1). The Vessup Bay/Red Hook APC is located on
the eastern end of St. Thomas and includes Nazareth, Muller, Vessup, Red Hook, Great
Bay, Cowpet Bay, Cabrita, Beck and Water Point, Great St. James, Little St, J, and Dog
Island.
Areas of Particular Concern in the STEER on St. Thomas
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Figure 5.01.1 Areas of Particular Conem (STEER (2011) St. Thomas East End Reserve
Management Plan. St. Thomas, USVI.
The island also lies within the St. Thomas East End Reverse (STEER). STEER was
developed to help protect coastal resources including seagrass beds and coral reef
communities. The island of Great St. James is in area C of the reserve and is referred to
as St. James (Figure 5.01.2).
6
EFTA00802731
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Management Plan. St. Thomas, USVI.
The regulations for the St. James are as follows:
St. James
Marine
Reserve and
Wildlife
Sanctuary Subchapter
96, Section
96-3 Prohibited Activities within the St. James MRWS:
• It is unlawful to remove any marine or other wildlife without
a permit or specific authorization from the Commissioner
Subchapter Permitted Activities within the St. James MRWS:
96, Section
96-4 Acts permitted, provided a permit is first obtained from the
Commissioner:
• Scientific collecting in support of and for use in a research
project with an approved protocol
• The use of castnet with a minimum square mesh size of X
inch to capture baitfish (fry) within 50 feet of the shoreline,
except for Cow and Calf rocks
• Fishing with hook and line
7
EFTA00802732
The marine habitats around Great St. James have abundant coral and seagrass resources.
There are numerous ESA listed corals species near the proposed dock locations.
Acropora palmata, Acropora. cervicornis, Orbicella annularis, Orbicella franksi and
Orbicella faveolata as well as Dendrogyra cylindrus are found off all the beach from
which the proposed docks and barge landings are planned. At the northern temporary
barge landing site, these corals are located primarily to the west in an area of coral
boulders and coral rubble. However, there are several small A. palmata and several 0.
annularis located on the shoreline cobble which extends out to a depth of 6.5ft. The
presence of these species as well as several non-ESA listed Porites astreoides has
dictated the location of the ramp. The proposed temporary barge landing position avoids
all coral and seagrass resources.
Location of the western dock has a cobble beach between two areas of emergent bedrock
and boulders. A. paknata occur on the emergent bedrock to the north. Offshore the
seafloor quickly gives way to exposed pavement. There is a long linear depression right
offshore and an old piling lies within this area. The fractured pavement then extends to
approximately 11.5ft of depth over the next 100ft heading offshore. The area has some
widely-scattered boulders and patchy coral colonization. There are scattered ESA corals
including Orbicella and Dendrogyra. During the first survey, there was a very large A.
palinata colony immediately seaward of where the old piling lay near shore. However,
upon the next visit by the island it was noted that an old boat was tied nearshore
apparently attached to the old piling. During a dive, several weeks later it was noted that
the boat was gone and the large A. cervicornis had been badly broken. The location of all
the ESA species has dictated the location of the dock. Approximately 75 corals will
require relocation to minimize impact, but no listed corals will need relocation.
The southern dock also extends from a cobble beach which gives way to rock pavement
and has emergent bedrock and boulders on either side of the beach. There are Acropora
colonies to the east and farther to the south on the bedrock and boulders. There are
Orbicella and Dendrogyra within the embayment and their locations have dictated the
location of the dock. The dock avoids all ESA listed corals but will require the relocation
of approximately 75 corals.
This southern dock will include a combination wave attenuator and reef building system.
A mitigation plan has been prepared and is found in Appendix B.
Because of the rock occurring in the area, some of the pilings may require socketing and
if this is required special water quality measures will be taken. If at all possible a vibra-
hammer will be used to drive the piles. A water quality monitoring program has been
proposed and the plan is found in Appendix C.
The area is known habitat to protect sea turtles and marine mammals and as such
NOAA's Sea Turtle and Smalltooth Sawfish Construction Conditions will be followed as
well as NOAA's Vessel Strike Avoidance Measures and Reporting for Mariners.
8
EFTA00802733
The property contains 6 salt ponds. The wetland around the salt ponds have been
delineated and the delineations were approved by the U.S. ACOE during a previous
application for development of the island. This delineation is more than 5 years old, but
no wetland disturbance will occur as a result of this project.
The island is known to be habitat to the St. Thomas Tree Boa that is a listed rare and
endangered species. The boa as well as another species of snake have been seen during
the field studies. There will be special corridors and preservation areas set aside on the
island for these species. The access ways to the western and southern docks already
exist, but the branch that will need to be developed to the temporary barge landing will be
cleared by hand to limit impacts to the tree boas. A tree boa mitigation plan is found in
Appendix D.
Both emergency barge ramps consisted of cobble and boulders pushed out from the
shoreline to create landings so that the barge would have sufficient water depth to land
the supplies. Both ramps were pushed out over the uncolonized coral rubble and neither
extend deep enough to encounter coral resources. No turbidity impacts were noted
during the survey of the ramps. The southern ramp has since been removed.
5.OIc Method of Construction
The temporary barge ramp will be the first feature constructed. The landing slab will be
framed and poured from shore and the bollards will be installed near the shoreline. The
cobble will be excavated with a small machine and silt fencing will be placed seaward off
all excavation prior to any work. Divers utilizing a small boat will install the offshore
moorings. As soon as this ramp is in the emergency barge ramp will be removed. The
emergency barge ramp will be removed by backhoe from the shoreline. The cobble will
be pulled in and spread on the back beach. The riprap will be taken inland to use in
landscaping.
The western and southern docks will both be constructed from a barge. A vibratory
hammer will be used to drive all the piles if the hardness of the rock allows. If the rock
proves to be too hard, the piles will be socketed, placed, and grouted in. All corals will be
transplanted out of the footprint and area of impact prior to the start of construction and
all turbidity control will be installed prior to any in-water work that day. If rocketing is
required, seafloor length curtains will be used and monitored and not removed until water
quality within the curtains has fallen to acceptable limits. All corals within the curtain
limits will be removed to prevent damage by settling sediments. Once the pilings have
been placed, re-enforcing steel will be placed, and concrete poured. Turbidity controls
will be installed, and water quality monitoring will occur during all concrete pouring.
Once the piles are completed the pile caps and decking will be placed.
1O
EFTA00802734
Access slabs will be constructed from shore and silt fencing will be placed seaward of all
excavations.
The existing dock will be removed as soon as one of the access docks is functional. The
decking and pile caps will be removed from shore. The pilings will be pulled by a small
barge and if the pilings proved to hard to pull they will be cut off at mudline.
5.0Id Provisions to Limit Site Disturbance
The dock locations have been located to minimize impact on the marine environment by
avoiding all ESA listed corals and seagrass beds. Corals which cannot be avoided will be
relocated out of the footprint and potential area of impact and turbidity control and water
quality monitoring will be implemented. The branch of the road to the temporary barge
landing will be first cleared by hand to minimize impact to the VI Tree Boa. A Tree Boa
protection plan is found in Appendix D.
5.00e Sedimentation Control Methods to be Implemented.
Silt fencing will be placed seaward of all upland excavation and construction. Turbidity
bathers will be installed around all areas of in-work, including pile driving and concrete
pouring overwater. If pile socketing is required two rows of turbidity bathers will be
installed and these curtains will be seafloor length. These curtains will be maintained
until the interior water quality has fallen to acceptable levels.
5.00f Schedule for Construction Activities and Implementation of Sediment Control
Measures
Silt fencing will be installed prior to any upland excavation and maintained throughout
construction. All construction will be occurring in cobble areas without vegetation, so
fencing will be maintained until such time no exposed soil is within the area.
Silt fencing will be installed during the new access road clearing and maintained until
such time the roadway is stabilized.
Turbidity barriers will be installed before any in-water work and maintained until interior
water quality is within acceptable levels. Double turbidity bathers will be required if pile
socketing is required.
5.00g Maintenance of Sediment and Siltation Control Measures
All silt fencing and turbidity bathers will be inspected and maintained through the
construction period. Silt fencing will be inspected daily even when no construction is in
progress (over weekends/holidays). Turbidity bathers will be monitored throughout the
II
EFTA00802735
day and will be repaired and adjusted as necessary as part of the water quality monitoring
plan. Curtains will be maintained throughout the day and removed or secured as
necessary when no in-water work is ongoing.
5.02 EXHIBITS AND DRAWINGS
Drawing Page
Proposed Temporary Barge Landing 11
Western Access 12
Southern Access Dock/Barge Access 13
As-built Drawings for Existing Dock 14
As-built Drawings for Existing Dock 15
12
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EFTA00802741
5.03 Project Work Plan/Schedule
• Temporary Barge Landing
I. Placement of silt fencing
2. Excavation of footings
3. Framing of slab
4. Placement of bollards
5. Pouring of concrete
6. Removal of silt fencing once all areas are stabilized
7. Placement of moorings
8. Remove emergency barge ramp
• Southern Dock
I. Placement of turbidity bathers
2. Placement of piles - vibra-hammer or socketing
3. Placement of re-enforcing steel and pouring of concrete
4. Placement of pile cabs and deck slabs
5. Turbidity barriers moved/removed as necessary once interior water quality is
acceptable
6. Placement of silt fencing
7. Excavation of footing
8. Framing of slab
9. Pouring of concrete
10. Removal silt fencing once all areas are stabilized
• Western Dock
11. Placement of turbidity bathers
12. Placement of piles/vibra-hammer or socketing
13. Placement of re-enforcing steel and pouring of concrete
14. Placement of pile cabs and deck slabs
15. Turbidity barriers moved/removed as necessary once interior water quality is
acceptable
16. Placement of silt fencing
17. Excavation of footing
18. Framing of slab
19. Pouring of concrete
20. Remove silt fencing once all areas are stabilized
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18
EFTA00802742
6.00 ENVIRONMENTAL SETTING AND PROBABLE PROJECT IMPACTS
6.01 Climate and Weather
Prevailing Winds
The Virgin Islands lie in the "Easterlies" or "Trade Winds" which traverse the southern
part of the "Bermuda High" pressure area, thus the predominant winds are usually from
the east-northeast and east (IRF, 1977). These trade winds vary seasonally (Figure
6.01.1) and are broadly divided into 4 seasonal modes: I) December to February; 2)
March to May; 3) June to August; and 4) September to November. Below are the
characteristics of these modes as taken from Marine Environments of the Virgin Islands
Technical Supplement No. I (IRF, 1977).
December - February
During the winter the trade winds reach a maximum and blow with great regularity from
the east-northeast. Wind speeds range from eleven to twenty-one knots about sixty
percent of the time in January. This is a period when the Bermuda High is intensified
with only nominal compensation pressure changes in the Equatorial Trough. The trade
winds during this period are interrupted by "Northerners" or "Christmas Winds" which
blow more than twenty knots from a northerly direction in gusts from one to three days.
Such outbreaks average about thirty each year. They are created by strengthening of
high-pressure cells over the North American continent, which, in turn, allow weak cold
fronts to move southeastward over the entire Caribbean region. Intermittent rains, clouds
and low visibility accompany these storms.
March - May
During the spring, the trade winds are reduced in speed and blow mainly from the east.
Winds exceed twenty knots only thirteen percent of the time in April. The change in
speed and direction is the result of a decrease of the Equatorial Trough.
June - August
Trade winds reach a secondary maximum during this period and blow predominantly
from the east to east-southeast. Speeds exceed twenty knots twenty-three percent of the
time during July. The trend for increasing winds results from the strengthening of the
Bermuda High and a concurrent lowering of the pressure in the Equatorial Trough. Trade
winds during this period are interrupted by occasional hurricanes.
September - November
During the fall, winds blow mainly from the east or southeast and speeds reach an annual
minimum. Only seven percent of the winds exceed twenty knots in October. The low
wind speeds result from a decrease in the Equatorial Trough. During this period,
19
EFTA00802743
especially during late August through mid-October, the normal trade wind regime is often
broken down by easterly waves, tropical storms, and hurricanes.
Storm and Hurricanes
There are numerous disturbances during the year, especially squalls and thunderstorms.
These occur most frequently during the summer, lasting only a few hours, and causing no
pronounced change in the trade winds.
A tropical cyclone whose winds exceed 74 miles per hour is termed a hurricane in the
northern hemisphere, and significantly affects the area. These hurricanes occur most
frequently between August and mid-October (Figure 5) with their peak activity occurring
in September. The annual probability of a cyclone is one in sixteen years (Bowden,
1974).
Climate
No rainfall data is available for Great St. James. However, based on the vegetation on the
island the island which is dry adapted, it is probable that the island gets between 36-45
inches of rainfall a year. Rainfall usually occurs in brief, intense showers of less than a
few tenths of an inch and major rainfall events are associated with weather systems
(USGS 1998). The Virgin Islands have no sharply defined wet season. The wettest
period generally is from September to November, and the driest period is from January to
June (USGS 1998). The Cruz Bay which is the closest monitored station receives
between 39 inches of rainfall annually. The average rainfall received between 1972 and
2012 is found in the table below.
CRUZ BAY, VIRGIN ISLANDS (671980)
Period of Record Monthly Climate Summary
Period of Record : 1/ 1/1972 to 3/31/2012
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Annual
Average Max. 83.8 84.0 84.1 84.9 86.4 88.0 88.9 89.2 89.0 88.2 86.7 84.6 86.5 Temperature (F)
Average MM. 69.6 69.5 69.7 71.7 74.0 75.8 75.9 75.9 75.1 74.2 72.7 70.6 72.9 Temperature (F)
Average Total
Precipitation (in.) 2.65 1.89 1.89 3.49 4.18 2.50 3.41 4.65 6.02 4.81 6.28 3.25 45.02
Average Total 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 SnowFall (in.)
Average Snow Depth
(in.) 0 0 0 0 0 0 0 0 0 0 0 0 0
Percent of possible observations for period of record.
Max. Temp.: 71.2% Min. Temp.: 71.8% Precipitation: 88.2% Snowfall: 93.3% Snow Depth: 93.2%
Check Station Metadata or Metadata graphics for more detail about data completeness.
Table 6.01.1 Climate data from the Southeast Regional Climate Center, University of
North Carolina at Chapel Hill.
20
EFTA00802744
The difference between the mean temperatures of the coolest and warmest month is only
5 to 7 degrees F. The highest temperatures August or September and the lowest are in
January or February. The highest average daytime temperature in the warmest months is
about 88 degrees F, and in the coolest months is in the low 80's. Nighttime lows are
usually in the mid 70's during the warmer months and in the high 60's during the cooler
months (USGS 1998). In general, air temperature in the Virgin Islands ranges between
77 degrees and 85 degrees.
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Figure 6.01.1. Prevailing Winds in the U.S. Virgin Islands, January through June
21
EFTA00802745
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Figure 6.01.2. Prevailing Winds, U.S. Virgin Islands July through December.
12
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ATLANTIC BASIN 9 SYSTEMS
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SYSTEMS PER YEAR
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Figure 6.01.3. Tropical Hurricane Frequencies in the Virgin Islands (National Weather
Service .
22
EFTA00802746
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Hurricanes O O
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NOAA
Figure 6.01.4. Tropical Storm and Hurricane Occurrences in the Atlantic (National
Weather Service)
6.02 Landforms, Geology, Soils, and Historic Use
GEOLOGY OF ST. THOMAS, ST JOHN AND SURROUNDING CAYS
The Virgin Islands are near the northeastern corner of the present Caribbean Plate, a
relatively small trapezoidal -shaped plate that is moving eastward relative to the North and
South American continents carried on the American plate. The arc of the Lesser Antilles
is an active volcanic arc above a subduction zone in which the Atlantic oceanic crust of
the American Plate is carried downward under the Caribbean Plate. The closest volcano
to the Virgin Islands that is still active is Saba, about 160 km. to the east.
St. John is 7 miles long and 3 miles wide for a total of 12,000 acres or 19 square miles.
The oldest rocks of St. John are submarine lavas (keratophyre and spilite), beds of
volcanic debris and chert. Associated intrusive rocks of the Water Island Formation is
overlain by andesitic volcanic and volcanoclastic rocks of the Louisenhoj Formation
which underlies the island of St. Thomas to the east and much of the northwestern portion
of St. John. Donnelly (1966) suggested that the Louisenhoj Formation was deposited
unconformably on the Water Island Formation after a period of emergence, tilting and
erosion, on the slopes and environs of a subaerial volcanic island located roughly
between St. Thomas and St. John, an area now occupied by Pillsbury Sound. The
youngest layered deposits on St. Thomas are volcaniclastic rocks of the Tutu Formation.
Fossils contained in the Tutu Formation suggest that those deposits are of the Early
Cretaceous (Albain) Age (Donnelly et. al. 1971). It appears that all of the volcaniclastic
rocks of St. Thomas and St. John were deposited in a relatively short period of time
spanning 10 to 15 million years approximately 100 million years ago (D. Rankin 1988).
23
EFTA00802747
GEOLOGY OF GREAT ST. JAMES
The island which lies off the eastern tip of St. Thomas is irregularly shaped, and has two
fault lines running across the island. The island is comprised of 162 acres and rises to an
elevation of 186 feet above sea level. The island is a part of the Water Island Formation
that was lain down in the Lower Cretaceous. The northern tip is tonalite, gabbro and
granite from the tertiary period, the north-western tip as well as the southeastern tip of the
island is basalt, and the southwestern tip is undivided, mostly keratophyra. The central
portion of the island and the northeastern point is part of the Louisenhoj Formation. The
shorelines are a combination of sandy beach, cobble beach and shear rocky cliffs. There
are 6 salt ponds on the island.
SOILS OF THE PROJECT SITE
The Custom Soil Survey of the Unites State Virgin Islands has classified 6 soil types on
the islands of Great St. James. Cinnamon Bay gravelly loam (CgC), 5 to 12 percent
slopes, occasionally flooded is usually found on alluvial fans and terraces adjacent to
volcanic uplands. It has a surface layer which is 0 to 5 inches deep that is a very dark
grayish brown gravelly loam, the subsurface is 5 to 10 inches deep and is a dark brown
gravelly loam. Redhook extremely stony sand (RdB), 0 to 5 percent slopes, rubbly,
rarely flooded is usually found on coast beaches that are composed of calcareous sand. It
has a surface layer 0 to 7 inches deep of dark brown extremely stony sand, underlain with
7 to 10 inches of brown very stony and 10 to 16 inches of very pale brown very gravelly
sand below which is 16 to 60 inches of white very gravelly sand. Salt flats ponded
(SaA) consist of area of unvegetated saline flats, saline marshes and salt ponds. The soils
are very deep and poorly drained, strongly saline and frequently ponded for very long
periods. Southgate -Rock outcrop complex (SrE), 20 to 40 percent slopes is found on
the summits and side slopes of volcanic hills and mountains. It has a surface layer of 0 to
5 inches of brown gravelly loam and a subsoil of 5 to 10 inches of brown very gravelly
loam underlain by 10 to 17 inches of weathered igneous bedrock and 17 to 60 inches of
unweathered igneous bedrock. Southgate -Rock outcrop complex (SrF), 40 to 60
percent slopes is found on the summits and side slopes of volcanic hills and mountains. It
has a surface layer of 0 to 5 inches of brown gravelly loam and a subsoil of 5 to 10 inches
of brown very gravelly loam underlain by 10 to 17 inches of weathered igneous bedrock
and 17 to 60 inches of unweathered igneous bedrock. Solitude gravelly fine sandy loan
(SoA), is found in areas that are adjacent to saline marshes, flats and salt ponds and are a
mixture of terrestrial and marine sediments.
24
EFTA00802748
MOM
I
I
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I
I
I
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I g QS Iliecume Rag
Sal lap
WOOS 1 02000•••••••••••Ore @MOM
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A n—ess i • I—. —a.°'twig.= noses owes .•• mos wanes•oloi
Figure 6.02.1 Custom Soils map of the project area (USGS Custom Soil Survey
(https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx)
HISTORIC USE I
I
I
I
I
I
I
I
The archeological survey found no evidence of prehistoric habitation. There are no
structures shown on the island before 1760 on any of the historic maps. The island is
reported to have been under cultivation since the 1760. Around 1770, a cotton plantation
was established and cotton was cultivated until approximately 1815. Great St. James was
continuous occupied between 1760 and 1911. Today there is a house and complex
located off the northern bay which is often referred to as Shallow Bay
ADVERSE SITE CONDITIONS
The island is protected by its location between St. Thomas and St. John and the
surrounding cays. The northern temporary barge landing is protected by the other cays to
the north, and St. Thomas and St. John to the west and east. Waves do attenuate in
Pillsbury Sound and the area can be affected by large seas and swells. However, there
are no offshore structures other than the buoys and barges using the site should be
moored no more than a couple of hours.
Under normal sea conditions the Christmas Cove Dock and the Southeastern Dock/Barge
Landing are well protected by their locations in relation to the prevailing seas which are
25
EFTA00802749
usually from the east, southeast or northeast. During storms and during some periods of
the winter, seas can approach from the southwest. The Christmas Cove dock could be
effected by waves approaching between 220° to 250° and the Southwest dock would be
effected by waves coming from 210' to 240'. Waves occur from this direction primarily
during storm events. When seas become extremely rough or storms approach vessels
would be taken to more protected anchorages.
All three sites lie with area VE elevation 8ft where FEMA has determined that the 100-
year flood elevation with velocity will be 8ft as shown on FIRM maps 45 and 30 below.
Figure 6.02.2. FEMA FIRM Map Panel 45 of 94.
26
EFTA00802750
Figure 6.02.3 FEMA FIRM Map Panel 30 of 94.
The U.S. Virgin Islands lie in one of the most earthquake prone areas of the world, and
are susceptible to ground shaking, earthquake -induced ground failures, surface fault
ruptures and tsunamis (tidal waves) (Hays, 1984). The activity is mostly associated with
large-scale tectonic activity or faulting, originating in the Anegada Trough to the
northeast of the islands. The trough and its related scarp apparently were thrown up by
block faulting during the late Pliocene or early Pleistocene. It is oriented generally
northeast to southwest, separating St. Croix from Puerto Rico and the other Virgin
Islands. Based on shallow focus earthquakes, the Anegada Fault Trough is estimated to
be more than 400 miles in length. There are indications that strike slip movement is
occurring, with St. Croix shifting northeast relative to Puerto Rico (Puerto Rico Water
Authority 1970). The year 2018 marks the 151th anniversary of the last major
earthquake in the islands. This quake, which occurred on November 18, 1867 had an
identified intensity of VIII on the Modified Mercalli Scale. Earthquakes of this
magnitude have generally been associated with epicentral ground accelerations of
between 0.05 and 0.35 gravities. Since the 1868 quake, there has been continuous low
intensity activity, all below 6.0 Richter. Thousands of tiny earthquakes are encountered
every year on the island.
27
EFTA00802751
IMPACT OF SITE GEOLOGY ON THE DOCK
The site geology will have little impact on the construction and placement of the
temporary barge landing. Both other docks will be impacted by the site geology which
will dictate how the pilings can be installed. It is probable that the pile in the pavement
areas will have to be socketed. Once beyond the pavement a vibratory hammer can be
utilized.
IMPACT OF THE PROJECT ON GEOLOGICAL RESOURCES
No dredging or filling is proposed, therefore there will be negligible impact on the
geology of the area. The emergency ramp will be removed as soon as the proposed barge
landing is constructed and the shoreline will be restored to pre-ramp conditions.
6.03 Drainage, Flooding, and Erosion Control
6.03a Impacts of Terrestrial and Shoreline Erosion
The project includes the construction of 3 landing or access pads on cobble beaches
between rocky headlands. These pads are all limited in size the largest being just over
1000sqft. Due to the small size of these introduced impervious surfaces none should
result in any notable change in terrestrial runoff. Both docks are pile supported and in
areas of rocky or cobble beaches. Neither dock site has sand deposition on the beach and
the cobbles found on both beachesare moved by wave action rather than littoral transport.
The construction of the docks should not result in any shoreline erosion.
6.03b Relationship of the Project to the Coastal Flood Plain
All three sites lie with area VE elevation 8ft. where FEMA has determined that the 100-
year flood elevation with velocity will be 8ft as shown on FIRM maps 45 and 30
provided in Section 6.02.
6.03c Presence and Location of any Critical Areas and Possible Trouble Spots
The island of Great St. James is within the Vessup Bay/ East End Red Hook Area of
Particular Concern (APC) (Figure 5.01.1). The Vessup Bay/Red Hook APC is located on
the eastern end of St. Thomas and includes Nazareth, Muller, Vessup, Red Hook, Great
Bay, Cowpet Bay, Cabrita, Beck and Water Point, Great St. James, Little St, J, and Dog
Island.
28
EFTA00802752
Figure 5.01.1 Areas of Particular Conem (STEER (2011) St. Thomas East End Reserve
Management Plan. St. Thomas, USVI.
The island also lies within the St. Thomas East End Reverse (STEER). STEER was
developed to help protect coastal resources including seagrass beds and coral reef
communities. The island of Great St. James is in area C of the reserve and is referred to
as St. James (Figure 5.01.2).
29
EFTA00802753
(
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Figure 5.01.2 STEER boundaries. (STEER (2011) St. Thomas East End Reserve
Management Plan. St. Thomas, USVI.
30
EFTA00802754
The regulations for the St. James are as follows:
St. lames
Marine
Reserve and
Wildlife
Sanctuary Subchapter
96, Section
96-3 Prohibited Activities within the St. James MRWS:
• It is unlawful to remove any marine or other wildlife without
a permit or specific authorization from the Commissioner
Subchapter Permitted Activities within the St. James MRWS:
96, Section
964 Acts permitted, provided a permit is first obtained from the
Commissioner:
• Scientific collecting in support of and for use in a research
project with an approved protocol
• The use of castnet with a minimum square mesh size of X
inch to capture baldish (fry) within 50 feet of the shoreline,
except for Cow and Calf rocks
• Fishing with hook and line
The marine habitats around Great St. James have abundant coral and seagrass resources.
There are numerous ESA listed corals species near the proposed dock locations.
Acropora palmata, Acropora. cervicornis, Orbicella amzularis, Orbicella franksi and
Orbicella faveolata as well as Dendrogyra cylinders are found off all the beach from
which the proposed docks and barge landings are planned. At the northern temporary
barge landing site, these corals are located primarily to the west in an area of coral
boulders and coral rubble. However, there are several small A. palmata and several 0.
amiularis located on the shoreline cobble which extends out to a depth of 6.5ft. The
presence of these species as well as several non-ESA listed Porites astreoides has
dictated the location of the ramp. The proposed temporary barge landing position avoids
all coral and seagrass resources.
Location of the western dock has a cobble beach between two areas of emergent bedrock
and boulders. A. palmata occur on the emergent bedrock to the north. Offshore the
seafloor quickly gives way to exposed pavement. There is a long linear depression right
offshore and an old piling lies within this area. The fractured pavement then extends to
approximately 11.5ft of depth over the next 100ft heading offshore. The area has some
widely-scattered boulders and patchy coral colonization. There are scattered ESA corals
including Orbicella and Dendrogyra. During the first survey, there was a very large A.
pabnata colony immediately seaward of where the old piling lay near shore. However,
upon the next visit by the island it was noted that an old boat was tied nearshore
apparently attached
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