Lillooet Ranges
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Lillooet Ranges
The Lillooet Ranges are the southeasternmost subdivision of the Pacific Ranges of the Coast Mountains of British Columbia. They are located between the drainage of the Lillooet River and Harrison Lake on the west and the canyon of the Fraser River on the east, and by the lowland coastal valley of that river on the south. The Lillooet Ranges are approximately 8100 square kilometres (3150 mi²) in area. The range is extremely rugged and varied in terrain, and includes some of the highest peaks in southwestern British Columbia. The highest is Skihist Mountain, , crowning the Cantilever Range in the heart of the area to the west of the community of Lytton at the confluence of the Thompson and Fraser Rivers. The northernmost subdivision of the Lillooet Ranges is the Cayoosh Range, which includes the second-highest summit in the Lillooet Ranges, an unnamed peak just south of Seton Lake and about WSW of the town of Lillooet. To the northeast of Harrison Lake, Mount Breakenri ...
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Mount Marriott
Mount Marriott is a mountain located in British Columbia, Canada. It is a dry peak near the head of the Cayoosh Creek. It is easily reached by trail, and the best time to climb the mountain is in the month of July. There are a few lakes in close proximity to the mountain peak that are swimmable during the months of August and September. The lake was named in honor of RCAF Flying Officer Terrence James Marriott, who was killed in 1943, while fighting in World War II. References {{Reflist, refs= {{cite bivouac, id=1052, name=Mount Marriott, accessdate=2017-04-27 Marriott Marriott may refer to: People *Marriott (surname) Corporations * Marriott Corporation, founded as Hot Shoppes, Inc. in 1927; split into Marriott International and Host Marriott Corporation in 1993 * Marriott International, international hote ... Pacific Ranges Lillooet Land District ...
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Cayoosh Range
The Cayoosh Range is the northernmost section of the Lillooet Ranges, which are a subrange of the Pacific Ranges of the Coast Mountains in British Columbia, Canada. The range covers an area of c. 3770 km² (1455 sq mi) and is approximately 65 km (40 mi) SW to NE and about 20 km (12 mi) SE to NW. In some classification systems the Lillooet Ranges are considered to form their own group, rather than being a subdivision of the Pacific Ranges, although the Bendor Range, north of the Cayoosh Range across Anderson Lake, is classified as part of the Pacific Ranges which would tend to imply that the Cayoosh and Lillooet Ranges are as well. The Cayoosh Range is defined by the valley of Cayoosh Creek on the south, which is followed by the Duffey Lake Road section of Highway 99, from Pemberton- Mount Currie to Lillooet, which are at the respective western and eastern ends of the range. Cayoosh Pass, between the head of Duffey Lake and the descent to the Pemberto ...
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Silver River (British Columbia)
The Silver River, aka the Big Silver River and Big Silver Creek, or zácta in the St'at'imcets language of the In-SHUCK-ch people, is the second-largest stream entering Harrison Lake in the Lower Mainland of British Columbia, Canada (the largest is the Lillooet River, at the head of the lake). Rising in the central Lillooet Ranges to the east of the lake, it is approximately 40 km in length; its main tributary is the Little Silver River. A logging camp at its mouth was once a thriving community named Silver River, British Columbia, Silver River. References

* Rivers of the Pacific Ranges Rivers of the Lower Mainland Lillooet Ranges {{BritishColumbia-river-stub ...
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Nahatlatch River
The Nahatlatch River is a tributary of the Fraser River in the Canadian province of British Columbia. It originates in the Lillooet Ranges of the Coast Mountains and empties into the Fraser River in the Fraser Canyon, north of Boston Bar. Course The Nahatlatch's River originates in the Lillooet Ranges. It flows southeast, the northeast, collecting tributaries such as Mehatl Creek, Tachewana Creek, and Squakum Creek. It flows through Nahatlatch Lake, Hannah Lake, and Frances Lake. After the lakes the Nahatlatch River flows generally east to join the Fraser River in the Fraser Canyon. The Mehatl Creek watershed is within Mehatl Creek Provincial Park. The Nahatlatch Provincial Park and Protected Area encompasses the Nahatlatch River's valley from Mehall Creek to Nahatlatch, Hannah, and Frances Lakes. See also * List of tributaries of the Fraser River * List of rivers of British Columbia The following is a partial list of rivers of British Columbia, organized by watershed. Some l ...
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Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ...
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Mount Currie, British Columbia
Mount Currie is in the Squamish-Lillooet region of southwestern British Columbia. On BC Highway 99, the locality is by road about north of Vancouver, northeast of Whistler, and southwest of Lillooet. The Lillooet Tribal Council governs the First Nations portion. The relatively smaller freehold part is an unincorporated community. The latter business centre approximately encompasses an area where the Macrea Road/Highway 99 intersection forms the southwest corner and the Pemberton Portage Road/Highway 99 intersection forms the northeast corner. The First Nations reserves straddle the Birkenhead River. The eastern portion of the reserves extends north to the same latitude as the Owl Creek community but is well back from the river at that point. First Nations Early community In 1846, Alexander Caulfield Anderson visited Lillooet Village (not to be confused with later named Lillooet). On a grassy island above Lillooet Lake, the residents numbered 50 men (plus women and children). ...
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Pemberton, British Columbia
Pemberton is a village municipality in the Squamish-Lillooet region of southwestern British Columbia. This Pemberton Valley community is on the southwest shore of the Lillooet River and northeast shore of Pemberton Creek. On BC Highway 99, the locality is by road about north of Vancouver, northeast of Whistler, and southwest of Lillooet. First Nations The valley lies in the traditional territory of the Lil'wat First Nation, who have resided for thousands of years, but are now concentrated at Mount Currie. During the hunting season, the people journeyed into the headwaters of the Lillooet River. The absence of trails indicates travel was mostly by canoe. Indigenous farmers introduced potato growing to the area, having received seed potatoes either from passing early traders or from visiting the Lower Mainland. Early European exploration Hudson's Bay Company (HBC) employees were among the first outsiders to venture into the valleys of the Birkenhead River and Lillooet Rive ...
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Stein River
The Stein River is a tributary of the Fraser River in the Canadian province of British Columbia. The name is derived from the Nlaka'pamux word Stagyn, meaning "hidden place", referring to the fact that the size and extent of the Stein River valley is not very noticeable from the river's confluence with the Fraser. It is one of only 2 unlogged watersheds with an area greater than 50 km south of Prince George, BC Prince George is the largest city in northern British Columbia, Canada, with a population of 74,004 in the metropolitan area. It is often called the province's "northern capital" or sometimes the "spruce capital" because it is the hub city for .... Course The Stein River and its tributaries are contained in Stein Valley Nlaka'pamux Heritage Park. The river originates in remote Tundra Lake and flows generally east, joining the Fraser River north of Lytton. See also * List of British Columbia rivers References Tributaries of the Fraser River Fraser Ca ...
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Stein Valley Nlaka'pamux Heritage Park
Stein Valley Nlaka'pamux Heritage Park is a provincial park in British Columbia, Canada. It was established on November 22, 1995 by BC Parks and the Lytton First Nation to protect the ecological and cultural significance of the Stein River valley. Etymology The name "Stein" comes from the Nlaka'pamux word "stagyn", which means "hidden place". This land is an important spiritual land for the First Nations in the area. History In the 1980s there was a plan to log the valley. This was protested by the environmentalists who argued that this was the last untouched watershed in the southern Coast Mountains. In 1988 Fletcher Challenge announced a moratorium on logging the Stein. After strong public support, and an annual music festival that raised awareness, the Stein Valley was finally protected as a park on July 12, 1995. In June 2017, the park board suspended kayaking and rafting activities in order to better determine their long-term impacts on the ecological integrity of the park. ...
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Megatsunami
A megatsunami is a very large wave created by a large, sudden displacement of material into a body of water. Megatsunamis have quite different features from ordinary tsunamis. Ordinary tsunamis are caused by underwater tectonic activity (movement of the earth's plates) and therefore occur along plate boundaries and as a result of earthquakes and the subsequent rise or fall in the sea floor that displaces a volume of water. Ordinary tsunamis exhibit shallow waves in the deep waters of the open ocean that increase dramatically in height upon approaching land to a maximum run-up height of around in the cases of the most powerful earthquakes. By contrast, megatsunamis occur when a large amount of material suddenly falls into water or anywhere near water (such as via a meteor impact or volcanic activity). They can have extremely large initial wave heights ranging from hundreds and possibly up to thousands of metres, far beyond the height of any ordinary tsunami. These giant wave hei ...
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Mount Breakenridge
Mount Breakenridge, , is a mountain in the Lillooet Ranges of southwestern British Columbia, Canada, located on the east side of upper Harrison Lake in the angle of mountains formed by that lake and the Big Silver River. Name The name was conferred by Lieutenant Palmer RE for Archibald T. Breakenridge RE, a member of his party, during a reconnaissance survey by the Royal Engineers from the north end of Harrison Lake to Four Mile House in the Douglas Road along the Lillooet River in 1859. In Ucwalmícwts, the language of the Lower Lillooet people, the mountain's name is ''mólkwcen'' (no translation given), which is also the name of a fishing camp located near the mouth of Stokke Creek, a creek feeding Harrison Lake from its origins on the flank of Breakenridge. Potential landslide and tsunami hazard Mount Breakenridge is the subject of intensive study by government geologists due to the location of a fracture or shear zone on the mountainside above Harrison Lake. Researcher ...
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Lillooet, British Columbia
Lillooet () is a district municipality in the Squamish-Lillooet Regional District, Squamish-Lillooet region of southwestern British Columbia. The town is on the west shore of the Fraser River immediately north of the Seton River mouth. On British Columbia Highway 99, BC Highway 99, the locality is by road about northeast of Pemberton, British Columbia, Pemberton, northwest of Lytton, British Columbia, Lytton, and west of Kamloops. First Nations A main population centre of the Stʼatʼimc (Lillooet Nation), who comprise just over 50 per cent of the Lillooet area residents, it is one of the southernmost communities in North America where Indigenous peoples in Canada, indigenous people form the majority. First Nations in Canada, First Nations communities assert the land is traditional territory, having been continuously inhabited for thousands of years. The confluence of several main streams with the Fraser attracted large seasonal and permanent indigenous populations. Situated in ...
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