Salmon River (Shuswap Lake)

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Salmon River
Salmon River not far from the estuary

Salmon River not far from the estuary

Data
location British Columbia (Canada)
River system Fraser River
Drain over Little River  → South Thompson River  → Thompson River  → Fraser River  → Pacific Ocean
Headwaters to the east of the Thompson Plateau
50 ° 18 ′ 11 ″  N , 119 ° 41 ′ 16 ″  W
Source height approx.  1700  m
muzzle Salmon Arm, Shuswap Lake Coordinates: 50 ° 42 ′ 57 "  N , 119 ° 18 ′ 8"  W 50 ° 42 ′ 57 "  N , 119 ° 18 ′ 8"  W
Mouth height approx.  346  m
Height difference approx. 1354 m
Bottom slope approx. 10 ‰
length approx. 135 km
Catchment area 1550 km²
Discharge
A Eo : 1550 km²
Location: 5 km above the mouth
MQ 1974/2015
Mq 1974/2015
4.97 m³ / s
3.2 l / (s km²)
Communities Falklands

The Salmon River is an approximately 135 km long tributary of Shuswap Lake in the southeast of the Canadian province of British Columbia .

River course

The Salmon River rises in the east of the Thompson Plateau at an altitude of about 1700  m . It initially flows 20 km to the west. Not far from the north shore of Salmon Lake , the Salmon River turns north and later northeast. At river kilometer 50 it passes the municipality of Falkland and turns to the southeast. For the lower 38 km, the Salmon River flows north and flows into the head end of Salmon Arm , a part of Shuswap Lake. The small town of Salmon Arm is east of the river mouth. The British Columbia Highway 97 runs east of Westwold over a distance of 30 km along the river.

Hydrology

The Salmon River drains an area of ​​1550 km². The mean discharge near the mouth is 4.97 m³ / s. The highest monthly discharges usually occur in May and June with an average of 18.8 and 12.2 m³ / s, respectively.

Fish fauna

Prior to the 1914 landslide at Hells Gate on the Fraser River , the Salmon River was the spawning area of a larger salmon population . Since then, salmon migration into the Salmon River has decreased significantly and fishing has been banned. At the level of the Westwold settlement, west of Falkland, the Salmon River flows through a deep gravel bed several kilometers long. Above-ground runoff only occurs in this area during the spring floods . Thus this section of the river is an insurmountable obstacle for the salmon for most of the year.

Web links

Individual evidence

  1. ^ Government of Canada: Historical Hydrometric Data Search Results: Station 08LE070
  2. a b c d e Government of Canada: Historical Hydrometric Data Search Results: Station 08HD006