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Joffre Lakes Provincial Park is a class A provincial park located 35 kilometres (22 mi) east of Pemberton in British Columbia, Canada. It was established in 1996, when Joffre Lakes Recreation Area (created 1988) was upgraded to park status.
Slalok Mountain, originally known as Rex's Pillar, is a 2,653-metre (8,704-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the third-highest point of the Joffre Group, which is a subset of the Lillooet Ranges. [3]
Mount Taylor is a 2,318-metre (7,605-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is part of the Joffre Group, which is a subset of the Lillooet Ranges. [3] It is situated 21 km (13 mi) east of Pemberton, and 7 km (4 mi) northeast of Lillooet Lake.
Mount Matier is a prominent 2,783-metre (9,131-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the highest point of the Joffre Group, which is a subset range of the Coast Mountains . [ 3 ]
Joffre Peak is a 2,721-metre (8,927-foot) mountain summit located in the Coast Mountains, in Joffre Lakes Provincial Park, in southwestern British Columbia, Canada. It is the second-highest point of the Joffre Group, which is a subset of the Lillooet Ranges . [ 2 ]
Based on the Köppen climate classification, Mount Hartzell is located in a subarctic climate zone of western North America. [4] Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.
The largest and most important is the Stein Valley Nlaka'pamux Heritage Park, which takes in the entire Stein River basin, immediately west of Lytton and east of Pemberton-Mount Currie. "The Stein" is the largest unlogged watershed in the southern Coast Mountains and, like the rest of the Lillooet Ranges, varies from coastal-type alpine in the ...
Based on the Köppen climate classification, Mount Spetch is located in a subarctic climate zone of western North America. [4] Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.