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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 wh
m the Atlantic flows through the islands. The westerly drift of the Caribbean Current sweeps into Pillsbury Sound from the Southeast, seeking a way North through the bather set up by the Cays to discharge along the North Shore of St. Thomas and out into the Atlantic. The current flows past Great St. J
rthern 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 effected by large seas and swells. However, there are no offshore structures other than the buoys and barges using the sit
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 wh
m the Atlantic flows through the islands. The westerly drift of the Caribbean Current sweeps into Pillsbury Sound from the Southeast, seeking a way North through the barrier set up by the Cays to discharge along the North Shore of St. Thomas and out into the Atlantic. The current flows past Great St.
rthern 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 sit
ed near the northeastern corner of the present Caribbean Plate, a relatively small trapezoidal-shaped plate which is moving eastward relative to the North and South American continents carried on the American plate. That arc of the I nser Antilles is an active volcanic arc above a subduction zone in w
se, office pavilion and mechanical building are all going through various stages of construction under previously obtained permits. EFTA00604283 (Pillsbury Sound E.2 EXISTING CABANA Caribbean Sea LAND USE LEGEND E=I EXISTING STRUCTURES 11.2 SCREEN CABANA 0.3 BEACH CABANA 11-1 OPEN CABANA B-S LOO
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