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Blackfoot River (Idaho)


FieldValue
nameBlackfoot River
imageBlackfoot River Idaho.jpg
image_captionBlackfoot River
image_size300
map_size300
pushpin_mapIdaho#USA
pushpin_map_size300
pushpin_map_captionLocation of the mouth of the Blackfoot River in Idaho
subdivision_type1Country
subdivision_name1United States
subdivision_type2State
subdivision_name2Idaho
subdivision_type4Counties
subdivision_name4Caribou County, Idaho, Bingham County, Idaho
length135 mi
discharge1_locationnear Blackfoot
discharge1_min0 cuft/s
discharge1_avg210 cuft/s
discharge1_max2130 cuft/s
source1_locationnortheast of Soda Springs, Caribou County, Idaho
source1_coordinates
source1_elevation6443 ft
mouthSnake River
mouth_locationsouthwest of Blackfoot, Bingham County, Idaho
mouth_coordinates
mouth_elevation4413 ft
basin_size1097 sqmi

The Blackfoot River is a tributary of the Snake River in the U.S. state of Idaho. Formed by the confluence of Diamond Creek and Lanes Creek, it flows 135 mi to its mouth at the Snake River. The river is part of the Columbia River Basin.

The Blackfoot River's drainage basin is approximately 1097 sqmi in area. Its mean annual discharge, as measured at by USGS gage 13068501 (Combination Blackfoot River and Bypass Channel near Blackfoot, Idaho), is 210 cuft/s, with a maximum daily recorded flow of 2130 cuft/s, and a minimum of zero flow.

The river is named for the Blackfoot people even though they never lived in the area. It was first mapped by the Lewis and Clark expedition.

Course

The Blackfoot River is formed by the joining of Diamond and Lanes creeks, in the Caribou-Targhee National Forest in Caribou County near Soda Springs, Idaho. It flows northwest through the Blackfoot Reservoir, which is used for irrigation and flood control, then west to join the Snake River in Bingham County.

The Blackfoot River's headwaters are very close to the headwaters of the Bear River and the Portneuf River. All three begin in a few square miles of relatively flat land near Soda Springs, from which some headwater streams flow north to the Blackfoot River, others south to the Bear River, and others west to the Portneuf River.

Watershed

The region the Blackfoot River flows through is covered in all its lowest portions with flows of basalt which had their origin in the Blackfoot – Gem Valley lava field. The Blackfoot River flows from open marsh and grasslands near its source into the Blackfoot Narrows. The Blackfoot Narrows traverses a desert canyon of primarily sagebrush and juniper habitat: an excellent place to view birds of prey. Fishing for trout is usually good.

References

References

  1. "National Hydrography Dataset". United States Geological Survey.
  2. "Blackfoot River".
  3. Source elevation derived from [[Google Earth]] search using GNIS source coordinates.
  4. [http://www.nwcouncil.org/fw/subbasinplanning/uppersnake/plan/Assessment/1IntroOverview.pdf Upper Snake, Headwaters, Closed Basin Subbasins Plan Plan] {{Webarchive. link. (2012-02-13 , Northwest Power and Conservation Council)
  5. [https://pubs.usgs.gov/wdr/2005/wdr-id-05-1/pdf/ID05v1-09.pdf Upper Snake River basin between Idaho Falls and Neeley (includes Willow Creek, Blackfoot and Portneuf River basins)], Water Resources Data, Idaho, 2005
Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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