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DUBAWNT, or DOOBAUNT ( See also: river of See also: Mackenzie and See also: Keewatin districts, See also: Canada
.
It rises in Wholdaia (or See also: Daly) Lake, in 104° 20' W. and 60° 15' N., and flows northward to its confluence with the Thelon river, and thence eastward to Chesterfield Inlet, an arm of Hudson See also: Bay
.
It passes through numerous lake-expansions, including Dubawnt Lake, with an See also: area of 1700 sq. m. and an altitude of 500 ft. above the See also: sea; See also: Aberdeen, altitude 130 ft.; and See also: Baker, 30 ft
.
From the See also: head of Wholdaia Lake to the head of Chesterfield Inlet is 750 M. and thence to the west See also: coast of Hudson Bay 125 M
.
The river is shallow, and See also: banks and See also: bed are chiefly composed of boulders; grassy slopes, however, occur at intervals along its banks, especially on the shores of Dubawnt Lake, and are the feeding grounds of large bands of cariboo
.
Discovered in 1770 by See also: Samuel Hearne, the Dubawnt'was explored by J
.
B
.
Tyrrell in 1893, and the Thelon by See also: David Hanbury in' 1899
.
See See also: Annual Report of the See also: Geological Survey of Canada for 1896 (printed 1898)
.
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