Chakima Creek

Last updated • 2 min readFrom Wikipedia, The Free Encyclopedia
Chakima Creek
Canada British Columbia relief location map.jpg
Red pog.svg
Mouth of Chakima Creek
Location
Country Canada
Province British Columbia
District Cassiar Land District
Physical characteristics
SourceNear Cartoona Peak
  location Tahltan Highland
  coordinates 57°34′59″N130°37′45″W / 57.58306°N 130.62917°W / 57.58306; -130.62917 [1]
  elevation1,815 m (5,955 ft) [2]
Mouth Shaman Creek
  coordinates
57°36′41″N130°24′50″W / 57.61139°N 130.41389°W / 57.61139; -130.41389 [3] [2]
  elevation
780 m (2,560 ft) [2]
Length19 km (12 mi) [4]
Basin size100 km2 (39 sq mi) [5]
Discharge 
  average1.49 m3/s (53 cu ft/s) [5]
Basin features
Topo map NTS 104G9 Kinaskan Lake
NTS 104G10 Mount Edziza

Chakima Creek is a tributary of Shaman Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. [3] From its source in the mountains south of Mount Edziza, near Cartoona Peak and Tadeda Peak, it flows generally east for roughly 19 km (12 mi) [4] to empty into Shaman Creek, which flows to Kakiddi Creek, a tributary of the Klastline River, which in turn is a tributary of the Stikine River. [3]

Contents

Chakima Creek's mean annual discharge is estimated at 1.49 m3/s (53 cu ft/s). Its watershed covers 100 km2 (39 sq mi), and is mostly within Mount Edziza Provincial Park. The watershed's land cover is classified as 45.7% conifer forest, 26.6% shrubland, 14.0% barren, 9.6% herbaceous, and small amounts of other cover. [5]

The mouth of Chakima Creek is located about 55 km (34 mi) southeast of Telegraph Creek, British Columbia, about 70 km (43 mi) north of Bob Quinn Lake, British Columbia, and about 250 km (160 mi) east of Juneau, Alaska. [4]

Chakima Creek is in Mount Edziza Provincial Park, which lies within the traditional territory of the Tahltan First Nation, of the Tahltan people. [6] [7]

The name "Chakima" was created from the Talhtan words cha "beaver" and kima "house", referring to the maze of beaver dams and ponds in the area where Chakima Creek joins Shaman Creek. [3]

Geography

Chakima Creek originates in the high peaks south of Mount Edziza, north of Tadeda Peak and south of Cartoona Peak. From its source about 15 km (9.3 mi) south of the summit of Mount Edziza, Chakima Creek flows generally east for about 19 km (12 mi). It is joined by numerous unnamed tributaries which drain various mountains such as Esja Peak and Hoyaa Peak. [8] [9] In its lower reaches it makes a southward curve, coming close to Mowdade Lake, [10] then bending northward into a large wetland area. It flows through the northern end Mowchilla Lake, [11] then continues northeast through wetlands to empty into Shaman Creek. Mowchilla Lake and the various unnamed creeks that empty into it are part of Chakima Creek's watershed. [2] [5] [12]

Chakima Creek's watershed is part of the Mount Edziza volcanic complex. It is mostly within Mount Edziza Provincial Park. Chakima Creek itself is entirely within the park. Chakima Creek flows through Mowchilla Lake, and some of that lake's unnamed tributaries, which are part of Chakima Creek's watershed, drain areas to the south and east of Mowchilla Lake, outside of Mount Edziza Provincial Park. [2] [5] [12]

See also

Related Research Articles

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.

Hartz Creek is a tributary of the Tahltan River, part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally south and southwest for roughly 14 km (8.7 mi) to join the Tahltan River about 4.5 km (2.8 mi) north of Tahltan, British Columbia at the Tahltan River's confluence with the Stikine River. Hartz Creek's watershed covers 39.1 km2 (15.1 sq mi), and its mean annual discharge is estimated at 0.315 m3/s (11.1 cu ft/s). The mouth of Hartz Creek is located about 18 km (11 mi) northeast of Telegraph Creek, British Columbia, about 73 km (45 mi) southwest of Dease Lake, British Columbia, and about 200 km (120 mi) east of Juneau, Alaska. Hartz Creek's watershed's land cover is classified as 44.2% shrubland, 30.7% mixed forest, 20.8% conifer forest, and small amounts of other cover.

Riley Creek is a tributary of Middle Creek, which in turn is a tributary of the Tahltan River, part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally south for roughly 10 km (6.2 mi) to join Middle Creek about 1.5 km (0.93 mi) north of Middle Creek's confluence with the Tahltan River. Riley Creek's watershed covers 22.1 km2 (8.5 sq mi), and its mean annual discharge is estimated at 0.192 m3/s (6.8 cu ft/s). The mouth of Riley Creek is located about 22 km (14 mi) north of Telegraph Creek, British Columbia, about 74 km (46 mi) southwest of Dease Lake, British Columbia, and about 122 km (76 mi) east of Juneau, Alaska. Riley Creek's watershed's land cover is classified as 39.9% shrubland, 36.8% conifer forest, 20.3% mixed forest, and small amounts of other cover.

The Inhini 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 in the glaciers of Simma Mountain and Mount Rastus, the Inhini River flows north for about 25 km (16 mi) to the Iskut River just east of the Iskut's confluence with 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.

Flyin Creek is a tributary of Walkout Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally northwest for roughly 7.7 km (4.8 mi) to join Walkout Creek, which flows into Raspberry Creek, then Mess Creek, which flows into the Stikine River about 3 km (1.9 mi) downriver from the community of Telegraph Creek. Flyin Creek's watershed covers 16.3 km2 (6.3 sq mi), and is entirely in Mount Edziza Provincial Park. The creek's mean annual discharge is estimated at 0.423 m3/s (14.9 cu ft/s). The mouth of Flyin Creek is located about 45 km (28 mi) south of Telegraph Creek, British Columbia, about 110 km (68 mi) southeast of Dease Lake, British Columbia, and about 230 km (140 mi) southeast of Juneau, Alaska. Flyin Creek's watershed's land cover is classified as 40.3% barren, 24,2% shrubland, 19.7% conifer forest, 13.8% herbaceous, and small amounts of other cover.

Stewbomb Creek is a tributary of the Little Iskut River and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally southeast for roughly 14 km (8.7 mi) to join the Little Iskut River, which flows into the Iskut River, the largest tributary of the Stikine River.

Artifact Creek is a tributary of Stewbomb Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally southeast for roughly 13 km (8.1 mi) to join Stewbomb Creek, which flows into the Little Iskut River. In turn the Little Iskut River flows to the Iskut River, the largest tributary of the Stikine River.

Bourgeaux Creek is a tributary of the Little Iskut River and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally east for roughly 17 km (11 mi) to join the Little Iskut River, a tributary of the Iskut River, which in turn is the largest tributary of the Stikine River. Gerlib Creek joins Bourgeaux Creek about 5 km (3.1 mi) upstream of Bourgeaux's confluence with the Little Iskut River.

Gerlib Creek is a tributary of Bourgeaux Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally east and south for roughly 10.5 km (6.5 mi) to join the Bourgeaux Creek, a tributary of the Little Iskut River, which in turn is a tributary of the Iskut River, the largest tributary of the Stikine River.

Crayke Creek is a tributary of Mess Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally west for roughly 7 km (4.3 mi) to join Mess Creek, a tributary of the Stikine River.

Kitsu Creek is a tributary of Mess Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally northwest and north for roughly 22.5 km (14.0 mi) to join Mess Creek, a tributary of the Stikine River.

Nagha Creek is a tributary of Kitsu Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally northwest and north for roughly 15 km (9.3 mi) to join Kitsu Creek, a tributary of Mess Creek, which in turn is a tributary of the Stikine River.

Tadekho Creek is a tributary of Mess Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows generally northwest for roughly 18 km (11 mi) to join Mess Creek just north of Mess Lake.

Nido Creek is a tributary of Kakiddi Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. It flows from Mount Edziza generally east for roughly 11 km (6.8 mi) to empty into Nuttlude Lake, an expansion of Kakiddi Creek, a tributary of the Klastline River, which in turn is a tributary of the Stikine River.

Sorcery Creek is a tributary of Kakiddi Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. From high peaks just south of Mount Edziza it flows generally east for roughly 13 km (8.1 mi) to empty into Kakiddi Lake, an expansion of Kakiddi Creek, a tributary of the Klastline River, which in turn is a tributary of the Stikine River.

Shaman Creek is a tributary of Kakiddi Lake, the source of Kakiddi Creek, and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. From its source in the glaciers south of Mount Edziza it flows generally east for roughly 20 km (12 mi) to empty into Kakiddi Lake, an expansion of Kakiddi Creek, a tributary of the Klastline River, which in turn is a tributary of the Stikine River.

Ball Creek is a tributary of the Iskut River and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. From its source in the mountains south of Mount Edziza, near Yeda Peak, it flows generally southeast and east for roughly 41 km (25 mi) to empty into the Iskut River, the largest tributary of the Stikine River.

More Creek is a tributary of the Iskut River and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada. From its source near Yeda Peak in the Spectrum Range south of Mount Edziza, it flows generally south and east for roughly 65 km (40 mi) to empty into the Iskut River, the largest tributary of the Stikine River.

The Tanzilla River is a tributary of the Stikine River in northwest part of the province of British Columbia, Canada.

References

  1. Derived from BCGNIS, topographic maps, and Toporama
  2. 1 2 3 4 5 "Toporama (on-line map and search)". Atlas of Canada . Natural Resources Canada . Retrieved 4 October 2023.
  3. 1 2 3 4 "Chakima Creek". BC Geographical Names .
  4. 1 2 3 Lengths and distances measured using BCGNIS coordinates, topographic maps, online map servers, and Toporama
  5. 1 2 3 4 5 "Northwest Water Tool". BC Water Tool. GeoBC, Integrated Land Management Bureau, Ministry of Agriculture and Lands, Government of British Columbia. Retrieved 10 October 2023.
  6. "Our Territory". Tahltan Central Government. Retrieved 29 September 2023.
  7. "Dah Ki Mi — "Our House"". Tahltan Band Council. Retrieved 29 September 2023.
  8. "Esja Peak". BC Geographical Names .
  9. "Hoyaa Peak". BC Geographical Names .
  10. "Mowdade Lake". BC Geographical Names .
  11. "Mowchilla Lake". BC Geographical Names .
  12. 1 2 Mussio, Russell; Mussio, Wesley (2018). Northern BC Backroad Mapbook. Mussio Ventures. pp. 99–100. ISBN   978-1-926806-87-7 . Retrieved 10 October 2023.