Spatsizi River

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Spatsizi River
Spatsizi plateau.jpg
Canada British Columbia relief location map.jpg
Red pog.svg
Location of the mouth of the Spatsizi River in BC
Physical characteristics
Source Mount Gunanoot
  locationNear Spatsizi Headwaters Provincial Park
  elevation1,900 m (6,200 ft)
Mouth Stikine River
  location
Hyland Post
  coordinates
57°42′27″N128°06′11″W / 57.70750°N 128.10306°W / 57.70750; -128.10306 [1]
Length132 km (82 mi) [2]
Basin size3,516 km2 (1,358 sq mi) [3]
Discharge 
  average60.8 m3/s (2,150 cu ft/s) [3]

The Spatsizi River is a tributary of the Stikine River, rising near Mount Gunanoot in the southeastern Spatsizi Plateau, British Columbia.

Contents

Etymology

"Spatsizi" is a phrase from the Sekani language meaning "red goat", a reference to the habit of mountain goats in the region of rolling in the red dust of a particular mountain, making their coat-hair red.

Geography

The Spatsizi River emerges near the foot of Mount Gunanoot in the Skeena Mountains of north-central British Columbia. It then flows downslope and enters Spatsizi Headwaters Provincial Park from the south. The river continues north, leaving the park to enter a broad valley in the heart of the Spatsizi Plateau. The flat-bottomed topography of the valley allows the river to meander considerably along much of its northwestward flow until it reaches the Stikine River in Stikine River Provincial Park. [4]

See also

Related Research Articles

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Spatsizi Headwaters Provincial Park is a provincial park in the Stikine Region of British Columbia, Canada. It was established on January 25, 2001 to protect the headwaters of the Spatsizi River while providing recreational facilities for visitors.

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The Spatsizi Plateau is a plateau in the upper basin of the Stikine River in north-central British Columbia, Canada. Most of the plateau, which is a sub-plateau of the Stikine Plateau, is enshrined in either Spatsizi Plateau Wilderness Provincial Park or Spatsizi Headwaters Provincial Park. It is flanked on the south and southwest by the Skeena Mountains, on the southeast by the Omineca Mountains, on the northeast by the Stikine Ranges of the Cassiar Mountains, and on the west by the Klastline Plateau.

Spatsizi Mountain is a mountain in the Spatsizi Plateau, a sub-plateau of the Stikine Plateau in north-central British Columbia, Canada. The name "Spatsizi" derives from the Sekani language and means "red goat", as mountain goats in this region are known to roll on a particular red mountain, resulting in a red colour to their coats.

Mount Gunanoot is a mountain in the Spatsizi Plateau of the North-Central Interior of British Columbia, Canada, located just east of the headwaters of the Spatsizi River. It is named for Simon Gunanoot, a Gitxsan packer, entrepreneur and erstwhile fugitive who was hunted for several years before turning himself in for trial and being acquitted. Gunanoot is responsible for "opening up" most of the country in this region.

The Craig River is a transboundary river tributary of the Iskut River in Southeast Alaska, United States, and the northwest part of the province of British Columbia, Canada. Originating in Alaska, where it is sometimes called the South Fork Craig River, the Craig flows into British Columbia, generally in a northeast then northwest direction for about 50 km (31 mi) to join the Iskut River about 2 km (1.2 mi) east of the confluence of the Iskut and Hoodoo River. Its main tributary is the Jekill River.

The Tuya River is a major tributary of the Stikine River in northwest part of the province of British Columbia, Canada. From its source at High Tuya Lake in Tuya Mountains Provincial Park just south of Ash Mountain, the highest peak of the Tuya Range, the Tuya River flows south about 200 km (120 mi) to meet the Stikine River in the Grand Canyon of the Stikine. The Tuya River's main tributary is the Little Tuya River. The Tuya River divides the Tanzilla Plateau on the east from the Kawdy Plateau, to the northwest, and the Nahlin Plateau, to the southwest. All three are considered sub-plateaus of the Stikine Plateau. The Tuya River's watershed covers 3,575 km2 (1,380 sq mi), and its mean annual discharge is estimated at 36.9 m3/s (1,300 cu ft/s). The mouth of the Tuya River is located about 24 km (15 mi) northeast of Telegraph Creek, British Columbia, about 67 km (42 mi) southwest of Dease Lake, British Columbia, and about 210 km (130 mi) east of Juneau, Alaska. The Tuya River's watershed's land cover is classified as 35.7% shrubland, 31.4% conifer forest, 14.0% mixed forest, 7.2% herbaceous, and small amounts of other cover.

Raspberry Creek is a tributary of Mess Creek, which in turn is a tributary of the Stikine River in northwest part of the province of British Columbia, Canada. It flows generally northwest for at least 12 km (7.5 mi) to join Mess Creek about 6 km (3.7 mi) north of Mess Creek's confluence with Kitsu Creek. Raspberry Creek's watershed covers 129 km2 (50 sq mi) and its mean annual discharge is estimated at 3.472 m3/s (122.6 cu ft/s). The mouth of Raspberry Creek is located about 40 km (25 mi) southeast of Telegraph Creek, about 61 km (38 mi) southwest of Iskut and about 110 km (68 mi) southwest of Dease Lake. Raspberry Creek's watershed's land cover is classified as 35.1% barren, 24.9% shrubland, 20.7% conifer forest, 16.8% herbaceous, and small amounts of other cover.

Beatty Creek is a tributary of the Tahltan River in northwest part of the province of British Columbia, Canada. It flows generally south about 62 km (39 mi) to join the Tahltan River a few kilometres downstream from the Little Tahltan River confluence. The Tahltan River is one of the main tributaries of the Stikine River.

The Little Iskut River is a tributary of the Iskut River in the northwest part of the province of British Columbia, Canada, in Cassiar Land District. From its source at Little Ball Lake in Mount Edziza Provincial Park, the Little Iskut River flows about 45 km (28 mi), generally north to the vicinity of Mowdale Lake, then southeast and south to the Iskut River just below Cascade Falls. The Little Iskut River is part of the Stikine River drainage basin, as the Iskut River is a major tributary of the Stikine.

The Klastline River is a tributary of the Stikine River in northwestern British Columbia, Canada. It flows generally northwest about 70 km (43 mi) to join the Stikine River, which flows southwest across the Canada–United States border into Alaska where it empties into various straits of the Inside Passage. The Klastline River flows through Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people. Klastline means "confluence" or "junction of waters" in the Tahltan language.

References

  1. "Spatsizi River". BC Geographical Names. Retrieved 2022-06-26.
  2. Lehner, B., Verdin, K., Jarvis, A. (2008): New global hydrography derived from spaceborne elevation data. Eos, Transactions, AGU, 89(10): 93–94.
  3. 1 2 "Northwest Water Tool". BC Water Tool. GeoBC, Integrated Land Management Bureau, Ministry of Agriculture and Lands, Government of British Columbia. Retrieved 2022-06-26.
  4. "Management Direction Statement for Spatsizi Headwaters Provincial Park" (PDF). bcparks.ca. 2003-03-01. Retrieved 2020-10-23.