Nagha Creek Explained

Nagha Creek
Pushpin Map:British Columbia
Pushpin Map Caption:Mouth of Nagha Creek
Subdivision Type1:Country
Subdivision Name1:Canada
Subdivision Type2:Province
Subdivision Name2:British Columbia
Subdivision Type3:District
Subdivision Name3:Cassiar Land District
Length:15km (09miles)
Discharge1 Avg:1.43m3/s
Source1:Kitsu Peak
Source1 Location:Spectrum Range
Source1 Coordinates:57.4164°N -130.7167°W[1]
Source1 Elevation:1800m (5,900feet)
Mouth:Kitsu Creek
Mouth Coordinates:57.5058°N -130.8558°W
Mouth Elevation:690m (2,260feet)
Basin Size:46.6km2
Custom Label:Topo map

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.[2] It flows generally northwest and north for roughly 15km (09miles)[3] to join Kitsu Creek, a tributary of Mess Creek, which in turn is a tributary of the Stikine River.

Nagha Creek's mean annual discharge is estimated at 1.43m3/s. Its watershed covers 46.6km2 and is entirely in Mount Edziza Provincial Park. The watershed's land cover is classified as 38.5% barren, 29.8% conifer forest, 13.4% shrubland, 11.9% snow/glacier, 5.5% herbaceous, and small amounts of other cover.[4]

The mouth of Nagha Creek is located about 48km (30miles) south of Telegraph Creek, British Columbia, about 115km (71miles) southwest of Dease Lake, British Columbia, and about 228km (142miles) southeast of Juneau, Alaska.[3]

Nagha Creek is in Mount Edziza Provincial Park, which lies within the traditional territory of the Tahltan First Nation, of the Tahltan people.[5] [6]

The name "Nagha" comes from a Tahltan word for wolverine. According to BC Geographical Names, the creek was named "Nagha" because during time of survey a wolverine frequently visited a sheep carcass on the ice near the surveying party.

Geography

Nagha Creek originates from Nagha Glacier near Kitsu Peak and Yeda Peak in the Spectrum Range, about 33km (21miles) south of Mount Edziza.

From its source, Nagha Creek flows between Yagi Ridge, to the south, and the Kitsu Plateau, to the north. It then flows through conifer forests to join Kitsu Creek near Mess Lake. After its confluence with Nagha Creek, Kitsu Creek flows about 1km (01miles) before emptying into Mess Creek.[3] Nagha Creek's watershed is in the southern part of the Mount Edziza volcanic complex.[7] [8]

The steep, south-facing side of Nagha Creek contains a conical, 60m (200feet) and 400m (1,300feet) volcanic crater called The Ash Pit. This is the youngest and southernmost volcanic vent in the Mess Lake Lava Field, as well as possibly the youngest volcanic feature in the entire Mount Edziza volcanic complex.[9]

See also

Notes and References

  1. Derived from BCGNIS, topographic maps, and Toporama
  2. JAPYT. Nagha Creek.
  3. Lengths and distances measured using BCGNIS coordinates, topographic maps, online map servers, and Toporama
  4. Web site: Northwest Water Tool . BC Water Tool . GeoBC, Integrated Land Management Bureau, Ministry of Agriculture and Lands, Government of British Columbia . 4 October 2023.
  5. Web site: Our Territory . Tahltan Central Government . 29 September 2023.
  6. Web site: Dah Ki Mi — "Our House" . Tahltan Band Council . 29 September 2023.
  7. Web site: Toporama (on-line map and search) . . . 28 September 2023.
  8. Book: Mussio . Russell . Mussio . Wesley . Northern BC Backroad Mapbook . 28 September 2023 . 2018 . Mussio Ventures . 978-1-926806-87-7 . 99.
  9. Souther. J. G.. Jack Souther. The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia. Geological Survey of Canada. Canada Communication Group. Memoir 420. 1992. 235. 0-660-14407-7. 10.4095/133497. free.