Epstein Secrets

us) was seen off both the Christmas Cove and southern dock site. Methods The NOS St. John and St. Thomas Habitat map Tile 16 (Figure 6.06.1) of the Great St. James area shows the colonized rock pavement and bedrock as well as the offshore seagrass beds. The seagrass beds are not as continuous near the sh

Coastal Zone Permit to construct two docks, one of which is a combination dock and barge landing and a temporary barge landing to provide access to Great St. James Island. A temporary barge landing is being proposed on the northwestern facing beach. This site is to the west of the sand pond and the assoc

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 muc

B. SUPPORTING INFORMATION C. SITE PHOTOGRAPHS D. DATABASE SEARCH 3 EFTA00621970 I. SUMMARY An Environmental Site Assessment was conducted of Great St. James Island in January 2016. Great St. James is located off the southeastern end of the island of St. Thomas. Little St. James lies to the east.

lines running across the island. The island is comprised of 162 acres and rises to an elevation of 186 feet above sealevel. 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 wel

ts when they were surveyed. The southern ramp has been removed. Methods The NOS St. John and St. Thomas Habitat Map Tile 16 (Figure 6.06.1) of the Great St. James area shows the colonized rock pavement and bedrock as well as the offshore seagrass beds. The seagrass beds are not as continuous near the sh

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 muc