Bear River (Portland Canal)
Bear River | ||
Strohn Lake and Bear River Glacier in the headwaters of the Bear River |
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Data | ||
location | British Columbia ( Canada ) | |
River system | Bear River | |
origin |
Strohn Lake , glacial fringing lake of Bear River Glacier 56 ° 6 ′ 26 ″ N , 129 ° 40 ′ 33 ″ W |
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Source height | approx. 550 m | |
muzzle |
Portland Canal Coordinates: 55 ° 55 ′ 3 " N , 129 ° 59 ′ 21" W 55 ° 55 ′ 3 " N , 129 ° 59 ′ 21" W |
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Mouth height | 0 m | |
Height difference | approx. 550 m | |
Bottom slope | approx. 14 ‰ | |
length | 38 km | |
Catchment area | approx. 660 km² | |
Discharge at level 08DC006 A Eo : 350 km² Location: 16 km above the mouth |
MQ 1968/1998 Mq 1968/1998 |
25.2 m³ / s 72 l / (s km²) |
Left tributaries | Bitter Creek | |
Right tributaries | Rufus Creek, American Creek | |
Small towns | Stewart |
The Bear River (English for "Bear River") is a 38 km long tributary of the Portland Canal in the Canadian province of British Columbia .
The Bear River forms the outflow of Strohn Lake , the 550 m high glacial edge lake of the Bear River Glacier . The British Columbia Highway 37A (Glacier Highway) follows the course up to the mouth in the small town Stewart . The Bear River initially flows eight miles west. The Bear River takes in the meltwater from the Erickson Glacier further north via Rufus Creek . The American Creek flows from the north into the Bear River. This now turns towards the south-southwest. The Bear River Ridge flanks the river valley to the west. The glaciated mountain range of the Cambria Range lies in the southeast . The Bitter Creek , outflow of the Bromley Glacier , flows into the Bear River after a further 9 km from the east.
The Bear River drains an area of about 660 km². The mean discharge above the mouth of Bitter Creek , 16 km above the mouth, is 25.2 m³ / s. The highest monthly outflows occur during the melting of the glaciers in the summer months of July and August.
Web links
- Bear River . In: BC Geographical Names (English)