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The geology of the U.S. Virgin Islands includes mafic volcanic rocks, with complex mineralogy that first began to erupt in the Mesozoic overlain and interspersed with carbonate and conglomerate units.
The Virgin Islands (Spanish: Islas Virgenes) are an archipelago in the Caribbean Sea. They are geologically and biogeographically the easternmost part of the Greater Antilles, the northern islands belonging to the Puerto Rico Trench and St. Croix being a displaced part of the same geologic structure.
The islands' terrain is mostly hilly to rugged and mountainous with little level land. Crown Mountain, on Saint Thomas, is the highest point in the U.S. Virgin Islands at 1,555 ft (474 m).
These include various types of dry to moist forests, salt ponds, beaches, mangroves, seagrass beds and coral reefs. The land is mountainous, with average slopes being 30 percent. Bordeaux mountain, 1286 feet high, plunges sharply to the sea.
(l) For Assignments of Mortgage and Leasehold Interest for several properties, the recording fees shall be $25.00 for the document and $4.00 for each property or unit attached; for certified copies, the recording fees shall be $10.00 for the first page and $1.00 for each additional page; for Certificates of Death, the ...
Formal transfer of the islands occurred on March 31, 1917, along with a U.S. payment to Denmark of $25,000,000 in gold coin. United States colonial policy distinguished between citizens and "nationals," or inhabitants of colonies to whom the rights of U.S. citizenship were not conferred.
Its terrain consists of coral islands, and is relatively flat. It has volcanic islands and is steep and hilly. Its lowest point is the Caribbean Sea and its highest point is Mount Sage at 521 metres (1,709 ft) above sea level. Its natural resources are negligible.
The USVI is an organized, unincorporated territory of the United States, meaning it follows U.S. laws but also has its own local government. It also means that not all of the U.S. Constitution applies to the people living there.