Hudson Strait

Definition and stakes

A. P. Low,  Report on the Dominion Government Expedition to Hudson Bay and the Arctic Islands on board the D.G.S. Neptune…

“ Ships entering Hudson strait from the Atlantic during the early part of the season, when ice is present in the strait, should keep in the northern half of the channel between Resolution and the Button islands. Care should be taken to keep some miles from Resolution, as the strong currents close to the island cause the ice to come together and open again with considerable violence. The north side of the strait should be followed as far as Big island, keeping at a respectful distance from the land in order to avoid the pressure when the ice is pressed on the land by southerly winds. ”
Source: Gutenberg

A. P. Low,  Report on the Dominion Government Expedition to Hudson Bay and the Arctic Islands on board the D.G.S. Neptune…

“ The limestone country terminates some distance north of King cape, which marks the western limit of Hudson strait on its north side, and the coast is again formed of crystalline rock, with its characteristic broken outline and fringe of islands. The northern shores of Hudson strait along its western half although bold are not high, and the interior probably does not reach a general elevation of 1,000 feet. To the eastward of Big island the coast becomes higher, and the land rises slowly inland to elevations of 2,000 to 3,000 feet. ”
Source: Gutenberg

A. P. Low,  Report on the Dominion Government Expedition to Hudson Bay and the Arctic Islands on board the D.G.S. Neptune…

“ When the eastern mouth of Hudson strait is left, a change is soon seen in following the eastern side of Baffin island northward. The hills are less rounded, and talus lies on the slopes of the cliffs; about Cumberland gulf and Cyrus Field bay there is evidence of a universal ice-cap having been present, but the rounding, polishing and striation of the rocks are markedly less than to the south and westward. In these places it is exceedingly difficult to find striæ upon the rock surfaces, and these when found show that the movement was local and from the highlands towards the open sea. ”
Source: Gutenberg

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