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The volcano that built the island's basement is inferred to be mid-plate hotspot volcanism, and was formed when a disturbance in the transition zone led magma from the zone toward Earth's surface. [1] [2] [3] Eolian limestone and hills dominates much of the surface geology of Bermuda, interbedded with layers of paleosols. [4]
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.
Bermuda is a group of low-forming volcanoes in the Atlantic Ocean, in the west of the Sargasso Sea, roughly 578 nmi (1,070 km; 665 mi) ...
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 ...
Volcanoes of Bermuda — an Atlantic island dependency of the United Kingdom in North America. Pages in category "Volcanoes of Bermuda" The following 3 pages are in ...
During the Second World War Great Sound was the location several military installations: The United States Navy's Naval Operating Base, the Royal Naval Dockyard, on Ireland Island, RAF Darrell's Island, and Royal Naval Air Station Bermuda, on Boaz island.
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.
A seamount is a large submarine landform that rises from the ocean floor without reaching the water surface (), and thus is not an island, islet, or cliff-rock.Seamounts are typically formed from extinct volcanoes that rise abruptly and are usually found rising from the seafloor to 1,000–4,000 m (3,300–13,100 ft) in height.