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- W1001450847 abstract "The seafloor of Hudson Bay is characterized by a major basin about 250 m deep, with two separate arms in its southern half. The dividing topographic high is called “Midbay Bank,” which is a broad promontory that extends northerly almost half the length of the bay from the south coast between Winisk and Severn Rivers. Around the flanks of the basin at 80 to 100 m of water depth, the isobaths are parallel with the general configuration of the coast, as well as with the basin. The valleys are characterized by re-entrant contours that head in the vicinity of existing rivers on land and depressions at high submarine elevations on Midbay Bank. The valleys also have smooth V-shaped profiles in echograms. Sediments are coarse near shore, where they consist of gravels of Precambrian and Paleozoic origins. Quartz sands are also common on the beaches around the mainland coasts in the northwestern and eastern parts of the bay. Most sediment enters the bay from several large rivers and is dispersed." @default.
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- W1001450847 date "1986-01-01" @default.
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- W1001450847 title "Chapter 8 Seafloor Morphology and Sediments" @default.
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- W1001450847 doi "https://doi.org/10.1016/s0422-9894(08)70901-2" @default.
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