Epstein Secrets

up to 1.3ft (IRF 1977). There are no notable locally driven tidal currents due to the lack of confinement within the area. NOAA has a tide gauge in Charlotte Amalie which is a southern exposure which has been recording water levels since 1975. The high tide recorded on September 18, 1989 (Hurricane Hugo) was +3

ording water levels since 1975. The high tide recorded on September 18, 1989 (Hurricane Hugo) was +3.35ft, and in 1995 during Hurricane Marilyn the Charlotte Amalie tide station recorded the highest tide height 3.98ft above Mean Lower Low Water (MLLW). The lowest tide recorded was on February 6, 1985 and was -1

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

mark (hereinafter collectively referred to as "Grantors") and GSJ Properties Corp., a Virgin Islands Corporation, Time Center Building, 4600 Fstate Charlotte Amalie, St. Thomas, VI 00802, (hereinafter referred to as "Grantee"). WITNESSETH: That the Grantors, for and in consideration of the sum of WAtcee. WAVWy

Attached is a copy of the deed from James A. Evans, Jr., William H. Evans and Cowpet Bay Corporation to Karen Lis Kjaer, recorded on EFTA00805274 Great St. lint. LLC, v. /gate, et at Motion to Dismiss the First Amended Complaint Page 4 October II, 1979. A copy of the 1979 deed is attached as Exhibit 3

rever, all of their right, title and interest in and to the following described real pro- perty: "CS a te , 3 y 76' • — 1. The Island known as Great St. James Island / 74. in the United States Virgin islands and being located off the southeastern tip of the Island of St. Thomas, United States vir

up to 1.3ft (IRF 1977). There are no notable locally driven tidal currents due to the lack of confinement within the area. NOAA has a tide gauge in Charlotte Amalie which is a southern exposure which has been recording water levels since 1975. The high tide recorded on September 18, 1989 (Hurricane Hugo) was +3

ording water levels since 1975. The high tide recorded on September 18, 1989 (Hurricane Hugo) was +3.35ft, and in 1995 during Hurricane Marilyn the Charlotte Amalie tide station recorded the highest tide height 3.98ft above Mean Lower Low Water (MLLW). The lowest tide recorded was on February 6, 1985 and was -1

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