Category Archives: Place

Mount Jarvis

Alberta-BC boundary. Mount: Fraser River drainage
N of Kakwa Lake near BC-Alberta boundary
54.0736 N 120.1669 W — Map 93I/1 — GoogleGeoHack
Earliest known reference to this name is 1877 (CPR Report)
Name officially adopted in 1917
Official in BCCanada

Adopted by the Geographic Board of Canada in 1917, as identified in the 1877 Canadian Pacific Railway report. Edward Worrell Jarvis [1846–1894], with his assistant Charles Francis Hanington [1848–1930], explored the region in 1875 in connection with CPR surveys.

References:

Encampment Creek

British Columbia. Creek: Columbia River drainage
Flows E into Columbia Reach, Kinbasket Lake
52.15 N 118.5167 W — Map 83D/2 — GoogleGeoHack
Name officially adopted in 1939
Official in BCCanada

Adopted in 1939 for BC Lands’ map 5D, Revelstoke-Golden, “flowing E into Columbia River at junction with Canoe River”. Location description and coordinates of mouth subsequently adjusted after flooding behind Mica Dam.

Camp Creek labelled on BC Reference Map 42 was likely adjusted to Encampment Creek to avoid duplication and to retain a historic reference: this creek originally flowed into the apex of the great bend [Big Bend] of the Columbia River at approximately 52°8′ N 118°27’15” W opposite Boat Encampment, the place where David Thompson [1770–1857] wintered in 1811. Following flooding of these valleys behind Mica Dam, this creek now flows into Kinbasket Lake.

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Canoe Encampment

British Columbia. Locality: Columbia River drainage
Confluence of Canoe River and Columbia River (now submerged in Kinbasket Lake)
52.1167 N 118.4333 W — Map 83D01 — GoogleGeoHack
Earliest known reference to this name is 1811 (David Thompson)
Not currently an official name.
This locality appears on:
Map North America 1817 [A NWC post indicated here]
John Arrowsmith’s map BC 1859

On John Arrowsmith’s 1859 map of British Columbia, “Canoe Encampment” is the name for the Boat Encampment established by David Thompson [1770–1857] in 1811.

Lac l’Orignal

British Columbia. : Fraser River drainage
Former name for Moose Lake
Detail of Tête Jaune Cache area, John Arrowsmith map,1859

Detail of Tête Jaune Cache area, John Arrowsmith map,1859
Colonial Dispatches, Uvic

“Orignal” is Canadian French for “moose,” derived from Basque oreina “deer” via orignac, the form that the Basque word took on in the Basque-Mi’kmaq pidgin used by the Mi’kmaq and visiting Basque fishermen and whalers.

On Arrowsmith’s 1859 map, Moose Lake appears as “Lac L’Original [sic],” and the two sections of Yellowhead Lake are called Moose Lake and Cow dung Lake.

References:

  • Arrowsmith, John [1790–1873]. Provinces of British Columbia and Vancouver Island; with portions of the United States and Hudson’s Bay Territories. 1859. UVic

Kettle Lakes

British Columbia. Lakes: Fraser River drainage
W of Yellowhead Lake
52.85 N 118.5833 W — Map 83D/15 — GoogleGeoHack
Name officially adopted in 1985
Official in BCCanada

A kettle (also known as a kettle lake, kettle hole, or pothole) is a hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake. When the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than 10 m deep and eventually become filled with sediment.
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Jackman Flats Park

British Columbia. Provincial Park
SE of Tête Jaune Cache
52.9358 N 119.3861 W GoogleGeoHack
Name officially adopted in 2002
Official in BCCanada

Jackman Flats Provincial Park was established in 2000. At the end of the last ice age, some 11,000 years ago, winds from the main trench of the Fraser River and from, what is now, Kinbasket Lake, deposited vast quantities of sand in the Jackman Flats area. This created an ecosystem considered unique in British Columbia. Rare plant communities and shifting sand dune structures now exist in this rather small park (614 ha).

References:

Mount Terry Fox Park

British Columbia. Provincial Park
Adjacent to SW side of Mount Robson Park
52.95 N 119.25 W — Map 83D/14 — GoogleGeoHack
Name officially adopted in 1982
Official in BCCanada

Established on 23 June 1982, containing 1930 hectares more or less.

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