The Davis Strait is underlain by complex geological features of buried grabens (basins) and ridges, formed by strike-slip faulting of the Ungava Fault Zone during Paleogene times about 45 million to 62 million years ago. The strike-slip faulting transferred plate-tectonic motions in the Labrador Sea to Baffin Bay. It is the world's broadest strait.
Depth
With a water depth of between one and two thousand meters the strait is substantially shallower than the Labrador Sea to the south.
Tides
The strait is famous for its fierce tides that can range from 30 to 60 ft (9.1 to 18.3 m), which discouraged many earlier explorers.[citation needed]
US Geological Survey has estimated that at least 13% of the world's undiscovered oil deposits and 30% of the world's undiscovered gas pockets are located in the Arctic, with the seas around Greenland potentially holding large amounts of natural gas and lesser amounts of crude oil and natural gas liquids.[2][3] This has led Greenland's minister and provincial council to offer a large number of off-shore concessions to potential hydrocarbon (oil and gas) extraction. The largest concessions areas are located in seas west of Greenland, primarily the Davis Strait and Baffin Bay, but with several smaller concessions in the Greenland Sea in the east also.[4][5][6][7]
Boertmann, David. Mapping of Oil Spill Sensitive Areas in the Davis Strait, West Greenland A Review of Biological Data in Relation to Oil Spill Sensitivity Mapping, with an Identification of Data Gaps. Copenhagen, Denmark: Greenland Environmental Research Institute, 1992.
Crawford, R. E. Life History of the Davis Strait Greenland Halibut, with Reference to the Cumberland Sound Fishery. Winnipeg: Dept. of Fisheries and Oceans, 1992.
Jørgensen, O. A.; Hvingel, C.; Møller, P. R.; Treble, M. A. (2005). "Identification and mapping of bottom fish assemblages in Davis Strait and southern Baffin Bay". Canadian Journal of Fisheries and Aquatic Sciences. 62 (8): 1833–1852. doi:10.1139/f05-101.