In an extraordinarily bold move, he then turned south and went around the island to M'Clure Strait at its northern end, experiencing unprecedented danger from the heavy Beaufort Sea ice.
McClintock (1873) ended the dispute by observing that he had seen both M'Clure Strait and Victoria Strait and was convinced that neither would ever be navigated.
(22) Between the islands lie a number of possible shipping routes connecting the Atlantic and Arctic Oceans (and later the Pacific Ocean), with the widest and deepest route running from Lancaster Sound through Barrow Strait into Viscount Melville Sound and onwards through M'Clure Strait into the Beaufort Sea.
It seems inevitable that the deeper, wider routes further north will eventually open as well, as even M'Clure Strait briefly did in September 2007 and again in September 2008.
Areas near the edges of the CAA, including the periphery of the Western High Arctic, Amundsen Gulf, M'Clure Strait, Lancaster Sound, Prince Regent Inlet and the Gulf of Boothia, were land fast for the shortest amount of time each year (Fig.
Region Sub-region Onset Onset Breakup Breakup trend [rho]-value trend [rho]-value Baffin E Baffin Bay 0.44 0.47 -0.15 0.71 Bay NW Baffin Bay 0.52 0.39 -0.68 0.09 W Baffin Bay 0.62 0.12 -0.92 0.05 Kane Basin 1.15 0.13 -1.72 0.06 Beaufort Alaska 2.88 0.005 -0.62 0.1 Sea Banks 0.97 0.44 -1.17 0.14 Mackenzie 2.80 0.0007 -0.34 0.16 CAA-West Amundsen 0.56 0.59 -0.78 0.56 Amundsen Mouth 0.096 0.93 -0.22 0.79 Coronation-Maud 0.85 0.03 -0.13 0.64 Franklin 0.44 0.43 -0.50 0.14 M'Clintock 0.48 0.36 -0.56 0.09 Channel M'Clure Strait 1.25 0.17 -1.16 0.14 West Barrow - V.
In 2001, the Kapitan Khlebnikov traversed route 1, the northerly route through Viscount Melville Sound, M'Clure Strait and into the Beaufort Sea, in both easterly and westerly directions.
The most direct route through the Northwest Passage is via Viscount Melville Sound into the M'Clure Strait and around the coast of Banks Island.
It was deposited by the last ice entering Liddon Gulf from M'Clure Strait
. In the chronology of Banks Island, ice last filled M'Clure Strait
in the M'Clure Stade (the penultimate stade) of Early Wisconsinan age of the Amundsen Glaciation (the last glaciation) (Hodgson et al., 1984:24).
They spent much of their time offshore, near or beyond the shelf break and in the polar pack ice of the estuary, or in Amundsen Gulf, M'Clure Strait, and Viscount Melville Sound.
Amundsen Gulf, M'Clure Strait, and Viscount Melville Sound are comparatively deep bodies of water (maximum depths = ca.
In the west, the highest dwell-times were in the Mackenzie Estuary and within a deep trench located within M'Clure Strait
and Viscount Melville Sound.