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The geology of Bermuda represents an isolated limestone island in the Atlantic at the edge of the shallow Bermuda Platform. This platform is part of the larger Bermuda Pedestal (other high points include the Challenger and Plantagenet banks, separated by water 1000 feet deep).
View history; Tools. Tools. move to sidebar hide. ... Bermuda: The Spencer's Point Formation is a geologic formation in Bermuda. It preserves fossils. See also
The Bermuda Pedestal is an oval geological feature in the northern Atlantic Ocean containing the topographic highs of the Bermuda Platform, the Plantagenet (Argus) Bank, and the Challenger Bank. The pedestal is 50 km (31 mi) long and 25 km (16 mi) wide at the 100 fathom line (-185 m), while the base measures 130 km by 80 km at -4200 m.
Bermuda (officially, The Bermuda Islands or The Somers Isles) is an overseas territory of the United Kingdom in the North Atlantic Ocean.Located off the east coast of the United States, it is situated around 1,770 km (1,100 mi) northeast of Miami, Florida, and 1,350 km (840 mi) south of Halifax, Nova Scotia, west of Portugal, northwest of Brazil, 1,759 km (1,093 mi) north of Havana, Cuba and ...
Bermuda is an archipelago consisting of 181 islands, although the most significant islands are connected by bridges and appear to form one landmass. It has a land area of 54 square kilometres (21 sq mi). Bermuda has a tropical climate, with warm winters and hot summers.
View history; Tools. Tools. move to sidebar hide. ... Bermuda: The Rocky Bay Formation is a geologic formation in Bermuda. It preserves fossils. See also
Pick any one of the more than 50 ships or 20 planes that have disappeared in the Bermuda Triangle in the last century. Each one has a story without an ending, leading to a litany of conspiracy ...
Bermuda rise Muir Seamount is a seamount ( underwater volcano ), located at 33°43.20′N 62°29.40′W / 33.72000°N 62.49000°W / 33.72000; -62.49000 It is located in the Bermuda rise , a seismically active region, and was the site of an earthquake on 24 March 1978.