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Tsecha Creek

Coordinates: 57°49′41″N 130°25′55″W / 57.82806°N 130.43194°W / 57.82806; -130.43194
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Tsecha Creek
Tsecha Creek is located in British Columbia
Tsecha Creek
Mouth of Tsecha Creek
Location
CountryCanada
ProvinceBritish Columbia
DistrictCassiar Land District
Physical characteristics
SourceMount Edziza
 • locationBig Raven Plateau
 • coordinates57°46′00″N 130°37′13″W / 57.76667°N 130.62028°W / 57.76667; -130.62028[1]
 • elevation2,093 m (6,867 ft)[1]
MouthKakiddi Creek
 • location
Stikine Plateau
 • coordinates
57°49′41″N 130°25′55″W / 57.82806°N 130.43194°W / 57.82806; -130.43194[1]
 • elevation
716 m (2,349 ft)[1]
Length16 km (9.9 mi)[1]
Basin size23.1 km2 (8.9 sq mi)[2]
Discharge 
 • average0.423 m3/s (14.9 cu ft/s)[2]
Basin features
Topo mapNTS 104G15 Buckley Lake
NTS 104G9 Kinaskan Lake

Tsecha Creek is a tributary of Kakiddi Creek, which in turn is a tributary of the Klastline River, part of the Stikine River watershed in northwest part of the province of British Columbia, Canada.[3] It flows generally west for about 16 km (9.9 mi) to join Kakiddi Creek about 5 km (3.1 mi) south of Kakiddi Creek's confluence with the Klastline River.[3][1] Tsecha Creek's watershed covers 23.1 km2 (8.9 sq mi) and its mean annual discharge is estimated at 0.423 m3/s (14.9 cu ft/s).[2] The mouth of Tsecha Creek is located about 44 km (27 mi) east-southeast of Telegraph Creek, about 26 km (16 mi) west of Iskut and about 73 km (45 mi) south-southwest of Dease Lake.[1] Tsecha Creek's watershed's land cover is classified as 47.8% barren, 27.5% conifer forest, 13.1% shrubland, 10.3% snow/glacier, and small amounts of other cover.[2]

Tsecha Creek is in Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people.[4][5]

Geography

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Tsecha Creek originates from the northern slope of Mount Edziza, a massive glaciated mountain in the middle of the Big Raven Plateau.[4][6] From its source between Pillow Ridge and The Pyramid, Tsecha Creek flows northwest about 8 km (5.0 mi) to the northwestern edge of the Big Raven Plateau. It then flows about 8 km (5.0 mi) east-northeast down the northwestern side of the plateau into Kakiddi Valley where Tsecha Creek drains into Kakiddi Creek at the northeastern boundary of Mount Edziza Provincial Park.[1][4]

Geology

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The head of Tsecha Creek lies in an area covered by loose black cinders and ash from Williams Cone, the youngest cinder cone in the Desolation Lava Field.[3][7] This lava field is one of the youngest volcanic features of the Mount Edziza volcanic complex which consists of a linear group of volcanoes on the Tahltan Highland.[4][7]

History

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The name of the creek was chosen by surveyors of the Geological Survey of Canada for the creek's association with cinders and ash from Williams Cone. It was first adopted 2 January 1980 on the National Topographic System map 104G/16.[3] Tsecha is a combination of the Tahltan words "tse" and "cha", which mean "rock" and "rain", respectively.[3][7]

See also

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References

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  1. ^ a b c d e f g h Elevation, length and coordinates derived from Google Earth and the Canadian Geographical Names Database
  2. ^ a b c d "Northwest Water Tool". BC Water Tool. GeoBC, Integrated Land Management Bureau, Ministry of Agriculture and Lands, Government of British Columbia. Retrieved 2023-09-26.
  3. ^ a b c d e "Tsecha Creek". BC Geographical Names. Retrieved 2023-10-04.
  4. ^ a b c d "A 502" (Topographic map). Telegraph Creek, Cassiar Land District, British Columbia (3 ed.). 1:250,000. 104 G (in English and French). Department of Energy, Mines and Resources. 1989. Archived from the original on 2021-05-02. Retrieved 2021-09-25.
  5. ^ Markey, Sean; Halseth, Greg; Manson, Don (2012). Investing in Place: Economic Renewal in Northern British Columbia. University of British Columbia Press. p. 242. ISBN 978-0-7748-2293-0.
  6. ^ "Mount Edziza". BC Geographical Names. Retrieved 2023-10-01.
  7. ^ a b c Souther, J. G. (1992). The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia. Geological Survey of Canada (Report). Memoir 420. Canada Communication Group. doi:10.4095/133497. ISBN 0-660-14407-7.
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