The Molloy Deep (also known as the Molloy Hole) is a
bathymetric feature in the
Fram Strait, within the
Greenland Sea[1] east of Greenland and about 160
km west of
Svalbard. It is the location of the deepest point in the Arctic Ocean. 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.[2][3][4][5][6][7][8]
The outer rim of the trench is at a depth of 2,700 m (8,900 ft) and contains about 600 km2 inside the rim, descending to approximately 5,550 m (18,210 ft) at its greatest depth. The basin floor measures about 220 km2, and is the deepest point in the Arctic Ocean.[9][10] The only person to have reached the bottom of the Molloy Deep is American explorer
Victor Vescovo, as part of his
Five Deeps Expedition.
Topography
The Molloy Deep is a roughly rectangular, seismically active,[11] extensional,[12] sea-floor basin, that lies between the northwestern tip of the Molloy Fracture Zone,[13] (a right-lateral,[14] strike-slip fault[14]), and the Spitsbergen Fracture Zone (also a right-lateral, strike-slip fault). These two fracture zones connect the Knipovich Ridge (the actively spreading northern segment of the Mid-Atlantic Ocean ridge system), 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[15] which is the slowest spreading mid-ocean ridge on Earth,[16][17] and which stretches across the entire Arctic Oceans’ Eurasian Basin.[18]
Surveys
The Molloy Deep was discovered in September 1972 by the
USNS Hayes (T-AGOR-16), 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.[19]
Descents
The only person to reach the bottom of the Molloy Deep is
Victor Vescovo on 24 August 2019.[8][20] The
Five Deeps Expedition leader and chief submersible pilot, Vescovo, descended into the Molloy Deep in the Deep-Submergence Vehicle Limiting Factor (a Triton 36000/2 model submersible) from the support ship, the Deep Submersible Support Vessel DSSV Pressure Drop.[21] The Five Deeps Expedition established the depth of the Molloy Deep as 5,550 m (18,210 ft) ±14 m (46 ft) by direct
CTD pressure measurements.[22] This is shallower than previous estimations using earlier technology with less precise bathymetric methods.[23]
References
^"Fram Strait Bathymetry". Alfred Wegener Institute for Polar- and Marine Research. Archived from
the original on 14 May 2013. Retrieved 2 October 2012.
^Laderach, C., et al. (2011). Seismicity and active tectonic processes in the ultra-slow spreading Lena Trough, Arctic Ocean. Geophysical Journal International, v.184, pp. 1354–1370. doi.org/10.1111/j.1365-246X.2010.04926
^Baturin, D.G. (1990). "Structure and Geodynamics of the Molloy Transform Fracture Zones in the Mid-Ridge System of the Norway–Greenland Oceanic Basin". Okeanologiya. 30 (3): 436–443.
^
abChamov, N. P.; Sokolov, S. Yu.; Kostyleva, V. V.; Efimov, V. N.; Peive, A. A.; Aleksandrova, G. N.; Bylinskaya, M. E.; Radionova, E. P.; Stupin, S. I. (2010). "Structure and composition of the sedimentary cover in the Knipovich Rift valley and Molloy Deep (Norwegian-Greenland basin)". Lithology and Mineral Resources. 45 (6): 532–554.
doi:
10.1134/S0024490210060039.
S2CID56258200.