The Molloy Deep is a bathymetric feature in the Fram Strait, within the Greenland Sea east of Greenland and about 160 km west of Svalbard. It is the location of the deepest point in the Arctic Ocean. The outer rim of the trench is at a depth of and contains about 600 km2 inside the rim, descending to approximately at its greatest depth. The basin floor measures about 220 km2, and is the deepest point in the Arctic Ocean. The first and only person to have reached the bottom of the Molloy Deep is American explorerVictor Vescovo, as part of his Five Deeps Expedition.
Geology
The Molloy Deep is a roughly rectangular, seismically active, extensional, sea-floor basin, that lies between the northwestern tip of the Molloy Fracture Zone,, and the Spitsbergen Fracture Zone. These two fracture zones connect the Knipovich Ridge, with the Lena Trough, an actively spreading mid-ocean ridge region north of the Spitsbergen Fracture Zone. The Lena Trough joins the southwestern end of the Arctic Ocean's Gakkel Ridge which is the slowest spreading mid-ocean ridge on Earth, and which stretches across the entire Arctic Oceans’ Eurasian Basin.
History
The Molloy Deep was discovered in September 1972 by the USNS Hayes, the first of a new class of catamaran-hulled oceanographic research vessels. The Molloy Deep, Molloy Hole, Molloy Fracture Zone, and Molloy Ridge were named after Arthur E. Molloy, a U.S. Navy research scientist who worked in the North Atlantic, North Pacific and Arctic Oceans in the 1950s-1970s.
Manned descent
The first, and so far only, person to reach the bottom of the Molloy Deep is Victor Vescovo on 24 August 2019. The Five Deeps Expedition leader and chief submersible pilot, Vescovo, descended into the Malloy Deep in the Deep-Submergence VehicleDSV Limiting Factor from the support ship, the Deep Submersible Support VesselDSSV Pressure Drop. The Five Deeps Expedition established the depth of the Molloy Deep as ± by direct CTD pressure measurements. This is shallower than previous estimations using earlier technology with less precise bathymetric methods.