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Revision as of 07:38, 28 October 2005 editSkookum1 (talk | contribs)Autopatrolled89,945 editsNo edit summary  Revision as of 07:39, 28 October 2005 edit undoSkookum1 (talk | contribs)Autopatrolled89,945 editsNo edit summaryNext edit →
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It and the neighbouring ] line the east bank of the Fraser River north of the town of . The Clear Range extends as far as the town of ] and is bounded by the south wall of ] on the north. The southeast flank of the Clear Range is the ] between ] and ], while to its northeast are the and ], and beyond them the ] of the ]. The range is horseshoe-shaped, facing the high rangeland-plateau basin of ], which drains northeast to join the ], a tributary of the ] All of these areas, including the ] are classified by geographers as belonging to the Cariboo Plateau, itself part of the greater ]. It and the neighbouring ] line the east bank of the Fraser River north of the town of . The Clear Range extends as far as the town of ] and is bounded by the south wall of ] on the north. The southeast flank of the Clear Range is the ] between ] and ], while to its northeast are the and ], and beyond them the ] of the ]. The range is horseshoe-shaped, facing the high rangeland-plateau basin of ], which drains northeast to join the ], a tributary of the ] All of these areas, including the ] are classified by geographers as belonging to the Cariboo Plateau, itself part of the greater ].


Terrain: ==Terrain==


Yhe outer flanks of the range are extremely steep, particularly on the side of the Fraser, where the northerly peaks are a high plateau-edge almost 7000' above the river below. The core of the range is extremely rugged and has a complex series of interlocking valley. Karst formations throughout the area suggest caves, though none have been discovered, and there are scores of intermittent waterfalls and subalpine swamps. The area is heavily logged by thereby interlaced with logging roads and other trails. Yhe outer flanks of the range are extremely steep, particularly on the side of the Fraser, where the northerly peaks are a high plateau-edge almost 7000' above the river below. The core of the range is extremely rugged and has a complex series of interlocking valley. Karst formations throughout the area suggest caves, though none have been discovered, and there are scores of intermittent waterfalls and subalpine swamps. The area is heavily logged by thereby interlaced with logging roads and other trails.
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The highest summits are Blustry Mountain 2334 m (7657 ft), its neighbour Cairn Peak 2328 m (7638 ft), and north of them Moore Peak 2223 m (7293 ft) and Chipuin Mountain 2170 m (7119 ft). The highest peak in the southern part of the range is ] 2077 m (6814 ft), but higher in the centre of the range is Mount Murray 2153 m (7064 ft). The highest summits are Blustry Mountain 2334 m (7657 ft), its neighbour Cairn Peak 2328 m (7638 ft), and north of them Moore Peak 2223 m (7293 ft) and Chipuin Mountain 2170 m (7119 ft). The highest peak in the southern part of the range is ] 2077 m (6814 ft), but higher in the centre of the range is Mount Murray 2153 m (7064 ft).


Flora and Fauna: ==Flora and Fauna==


The climate is varied, though mostly dry, especially on the west and southeast. The interior of the range gets more waterfall and was heavily-treed relative to the canyons flanking it The climate is varied, though mostly dry, especially on the west and southeast. The interior of the range gets more waterfall and was heavily-treed relative to the canyons flanking it
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Typical boreal forest and mountain wlidlife prevail: grizzly, black bear, black-tail deer, moose, and various rodents. The range's reptile populations includes several varieties of dryland lizard and also the timber rattlesnake; the Clear Range is the farthest northwest extent of the rattlesnake. Typical boreal forest and mountain wlidlife prevail: grizzly, black bear, black-tail deer, moose, and various rodents. The range's reptile populations includes several varieties of dryland lizard and also the timber rattlesnake; the Clear Range is the farthest northwest extent of the rattlesnake.


History and Culture ==History and Culture==


The Clear Range is largely the domain of the ] or ''Nlaka'pamux'', although the northwest edge of the range is occupied by communities of the ]. There are no urban settlements in the range although it is skirted by three major highways and also three rail lines (the ], ] and ]). Due to its location, it overlooked the great movement of goldseekers during the ] and ] although no major mines or deposits were found on its slopes. The Clear Range is largely the domain of the ] or ''Nlaka'pamux'', although the northwest edge of the range is occupied by communities of the ]. There are no urban settlements in the range although it is skirted by three major highways and also three rail lines (the ], ] and ]). Due to its location, it overlooked the great movement of goldseekers during the ] and ] although no major mines or deposits were found on its slopes.

Revision as of 07:39, 28 October 2005

The Clear Range is a small mountain range located in the angle of the Fraser and Thompson Rivers|Thompson River]] in south-central British Columbia. It has a small subdivision just northeast of that confluence named the Scarped Range.

It and the neighbouring Marble Range line the east bank of the Fraser River north of the town of . The Clear Range extends as far as the town of Pavilion and is bounded by the south wall of Marble Canyon on the north. The southeast flank of the Clear Range is the Thompson River between Ashcroft, British Columbia and Lytton, British Columbia, while to its northeast are the and Trachyte Hills, and beyond them the Arrowstone Hills of the Bonaparte Plateau. The range is horseshoe-shaped, facing the high rangeland-plateau basin of Hat Creek, British Columbia, which drains northeast to join the Bonaparte River, a tributary of the Thompson All of these areas, including the Clear Range are classified by geographers as belonging to the Cariboo Plateau, itself part of the greater Fraser Plateau.

Terrain

Yhe outer flanks of the range are extremely steep, particularly on the side of the Fraser, where the northerly peaks are a high plateau-edge almost 7000' above the river below. The core of the range is extremely rugged and has a complex series of interlocking valley. Karst formations throughout the area suggest caves, though none have been discovered, and there are scores of intermittent waterfalls and subalpine swamps. The area is heavily logged by thereby interlaced with logging roads and other trails.

The highest summits are Blustry Mountain 2334 m (7657 ft), its neighbour Cairn Peak 2328 m (7638 ft), and north of them Moore Peak 2223 m (7293 ft) and Chipuin Mountain 2170 m (7119 ft). The highest peak in the southern part of the range is [[Botanie Mountain, just north of Lytton 2077 m (6814 ft), but higher in the centre of the range is Mount Murray 2153 m (7064 ft).

Flora and Fauna

The climate is varied, though mostly dry, especially on the west and southeast. The interior of the range gets more waterfall and was heavily-treed relative to the canyons flanking it

Typical boreal forest and mountain wlidlife prevail: grizzly, black bear, black-tail deer, moose, and various rodents. The range's reptile populations includes several varieties of dryland lizard and also the timber rattlesnake; the Clear Range is the farthest northwest extent of the rattlesnake.

History and Culture

The Clear Range is largely the domain of the Thompson First Nation or Nlaka'pamux, although the northwest edge of the range is occupied by communities of the St'at'imc First Nation. There are no urban settlements in the range although it is skirted by three major highways and also three rail lines (the BCR, CPR and CNR). Due to its location, it overlooked the great movement of goldseekers during the Fraser Canyon and Cariboo Gold Rushes although no major mines or deposits were found on its slopes.