Epstein Secrets

e Anchorage Associates, which deed was recorded April 24, 1978 in Book Page 52, Ho. 1114 in the Office of the Recorder of needs for Sr. Thorns and St. John; TOGETHER WITH = :“in-exciusive easement in perpetuity, appurtenant to and running with the premises herein conveyed, an, over and across the Esta

the Estate of Karen Elisabeth Kjaer a/k/a Karin Lis Kjaer dated October IS. 1987, recorded at the office of the Recorder of Deeds for St. Thomas and St. John on October 21. 1987. in Book No. 31-I). Page 54. Doe. No. 5090. TOGETHER WITH any improvements thereon. and the rights. privileges and appurtenanc

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

e 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 overl

e 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 s

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

e 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 overl

e 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 s

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

on despite the fact being considered a nature park with beautiful walks acclaimed by naturalists from the States as superior to the national park on St. John. Owner, Kjaer family, is looking to construct and sell 53 individual home units priced at about $750,000 each. Existing terrain conditions where s

GREAT ST. JAMES - U.S. VIRGIN ISLANDS • PROJECT FEASIBILITY REPORT • APRIL 2016 %-1 w to g. MONTEGAN A & D Inc. EFTA00599527 Great St. James Island USVI Estate Great Saint James Island is a Civil in St. Thomas County, VI with an elevation of 125 feet, or 38 meters above sea level.