Shuswap Highland
From Wikipedia, the free encyclopedia
The Shuswap Highland is in essence a foothill (or transitional) area between the much broader interior plateaus southwest and west of it, and the mountainous terrain of the northern Monashee and Cariboo Mountains on the east/north-east.
Climates here range from sub-alpine in the mountains, especially further north, to a semi-arid, more temperate, continental climate that is found around Shuswap Lake. Coordinates: 51°15′N 119°20′W / 51.250°N 119.333°W
See also
- Okanagan Highland
- Quesnel Highland
- Geography of British Columbia
- Geology of British Columbia
- Geology of the Pacific Northwest
References
- ↑ "Shuswap Highland". Peakbagger. Retrieved 2011-01-14.
- ↑ "Dunn Peak, British Columbia". Peakbagger.com.
- S. Holland, Landforms of British Columbia, Province of British Columbia, 1976
- "Shuswap Highland". BC Geographical Names. http://apps.gov.bc.ca/pub/bcgnws/names/19477.html.
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