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Elfin Lakes
Elfin Lakes are two lakes in Garibaldi Provincial Park that are popular for hiking, snowshoeing, skiing, and mountain bicycling trail located east of Squamish, British Columbia, Squamish, British Columbia, Canada. History The name was adopted in 1978 when it was identified in a pamphlet for the local lodge. However, a 1946 letter from W.H. Matthews, a Vancouver City Archivist notes that the lakes were once called Crystal Lakes but were never found on any maps."Elfin Lakes." Crown Registry and Geographic Base. GeoBC. Web. 22 Oct 2011. The area has always been a popular destination for hikers and skiers since the creation of the park in the 1927. Then a local lodge was built in the early 1940s by Joan Mathews, Ottar Brandvold, and his brother Emil and was called the Diamond Head Chalet, but it is now unused and decaying. It attracted many hikers and backcountry skiers. Eventually the owners retired, and ownership was transferred to BC Parks. They chose to not maintain it and built t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Opal Cone
Opal Cone is a cinder cone located on the southeast flank of Mount Garibaldi in the Coast Mountains of British Columbia, Canada. It is the source of a long broad dacite lava flow with prominent wrinkled ridges. The lava flow is unusually long for a silicic lava flow. Opal Cone is a member of the Cascade Volcanoes, but it is located in the Garibaldi Ranges in the Coast Mountains and not in the Cascade Range proper. See also * List of volcanoes in Canada * Volcanism of Canada * Volcanism of Western Canada * Cascade Volcanoes * Garibaldi Volcanic Belt * Garibaldi Lake volcanic field The Garibaldi Lake volcanic field is a volcanic field, located in British Columbia, Canada. It was formed by a group of nine small andesitic stratovolcanoes and basaltic andesite vents in the scenic Garibaldi Lake area immediately north of Mount ... External links Opal Conein the Canadian Mountain Encyclopedia Hiking Opal Cone- Online guide for hiking to the summit References Catalogue of Canadia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Garibaldi Provincial Park
Garibaldi Provincial Park, also called Garibaldi Park, is a wilderness park located on the coastal mainland of British Columbia, Canada, 70 kilometres (43.5 mi) north of Vancouver. It was established in 1920 and named a Class A Provincial Park of British Columbia in 1927. The park is a popular destination for outdoor recreation, with over 30,000 overnight campers and over 106,000 day users in the 2017/2018 season. Garibaldi Park spans an area of over 1,950 square kilometres (753 sq mi), encompassing a majority of the Garibaldi Range mountains. The western side of the park is highly trafficked by the public due to access provided by the nearby Sea to Sky Highway to destinations in the park such as Elfin Lakes, Garibaldi Lake, The Black Tusk, Cheakamus Lake, and Wedgemount Lake. The eastern wilderness of the park is harder to access and therefore more remote than its western counterpart. To the south, Garibaldi Park connects with Golden Ears Provincial Park and Pi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia
British Columbia (commonly abbreviated as BC) is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, forests, lakes, mountains, inland deserts and grassy plains, and borders the province of Alberta to the east and the Yukon and Northwest Territories to the north. With an estimated population of 5.3million as of 2022, it is Canada's third-most populous province. The capital of British Columbia is Victoria and its largest city is Vancouver. Vancouver is the third-largest metropolitan area in Canada; the 2021 census recorded 2.6million people in Metro Vancouver. The first known human inhabitants of the area settled in British Columbia at least 10,000 years ago. Such groups include the Coast Salish, Tsilhqotʼin, and Haida peoples, among many others. One of the earliest British settlements in the area was Fort Victoria, established ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Squamish, British Columbia
Squamish (; Squamish language, Sḵwx̱wú7mesh sníchim: Sḵwx̱wú7mesh, ; 2016 census population 19,512) is a community and a district municipality in the Provinces and territories of Canada, Canadian province of British Columbia, located at the north end of Howe Sound on the British Columbia Highway 99, Sea to Sky Highway. The population of the Squamish census agglomeration, which includes Indian reserve, First Nation reserves of the Squamish Nation although they are not governed by the municipality, is 19,893. Indigenous Squamish people have lived in the area for thousands of years. The town of Squamish had its beginning during the construction of the BC Rail, Pacific Great Eastern Railway in the 1910s. It was the first southern terminus of that railway (now a part of Canadian National Railway, CN). The town remains important in the operations of the line and also the port. Forestry has traditionally been the main industry in the area, and the town's largest employer was the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-bloc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canada
Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Columnar Peak
Mount Garibaldi (known as Nch'kaý to the indigenous Squamish people) is a dormant stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has a maximum elevation of and rises above the surrounding landscape on the east side of the Cheakamus River in New Westminster Land District. Mount Garibaldi contains three summits, two of which are individually named. Atwell Peak is a sharp, conical summit slightly higher than the more rounded summit of Dalton Dome. Both summits were volcanically active at different times throughout Mount Garibaldi's eruptive history. The northern and eastern flanks of Mount Garibaldi are obscured by the Garibaldi Névé, a large snowfield containing several radiating glaciers. Flowing from the steep western face of Mount Garibaldi is the Cheekye River, a tributary of the Cheakamus River. Opal Cone on the southeastern flank is a small volcanic cone from which a lengthy lava flow descends. The western face is a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Gargoyles
The Gargoyles are two mountain peaks in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. The highest peak has an elevation of whereas the lowest peak has an elevation of . A deeply eroded obsidian dome remnant at The Gargoyles contains 77% silica content and is the only Quaternary high-silica rhyolite identified anywhere in the Cascade Volcanic Arc north of the Three Sisters. The age of this rhyolite is poorly known. The Gargoyles were originally mapped as the ''Lava Peaks'' by William Henry Mathews William Henry Mathews (1919–2003) was a Canadian geologist, volcanologist, engineer, and professor. He is considered a pioneer in the study of subglacial eruptions and volcano-ice interactions in North America. Many of his publications continu ... in 1958. The current name was suggested and adopted in 1978. Another name applied to The Gargoyles is ''Lava Peak''. References External links * Garibaldi Ranges New Westminster Land District ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Atwell Peak
Atwell Peak is a dramatic pyramid shaped volcanic peak located at the southern edge of Mount Garibaldi, British Columbia, Canada. Atwell Peak was the source of many pyroclastic flows during Garibaldi's development. Frequent landslides on its west face drops steeply into the Cheekye River. Atwell Peak is often mistakenly called Mount Garibaldi when viewed from Squamish, since the main peak is hidden. The peak is usually climbed during winter or early spring when the rock is frozen because it is very loose and rotten. Atwell Peak contains three ridges, the north, east, and south. The two most visible routes are the north and south ridges. Atwell Peak consists of three ridges, the north, east, and south. The east ridge connects with the north ridge about 100 horizontal metres north of the summit. All ridges, with the possible exception of the upper east ridge, are sharp and heavily corniced in winter and spring. The north ridge is the shortest climbing route. Several gullies on the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Garibaldi
Mount Garibaldi (known as Nch'kaý to the indigenous Squamish people) is a dormant stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has a maximum elevation of and rises above the surrounding landscape on the east side of the Cheakamus River in New Westminster Land District. Mount Garibaldi contains three summits, two of which are individually named. Atwell Peak is a sharp, conical summit slightly higher than the more rounded summit of Dalton Dome. Both summits were volcanically active at different times throughout Mount Garibaldi's eruptive history. The northern and eastern flanks of Mount Garibaldi are obscured by the Garibaldi Névé, a large snowfield containing several radiating glaciers. Flowing from the steep western face of Mount Garibaldi is the Cheekye River, a tributary of the Cheakamus River. Opal Cone on the southeastern flank is a small volcanic cone from which a lengthy lava flow descends. The western face is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diamond Head (British Columbia)
Diamond Head is a subsidiary peak of Mount Garibaldi in southwestern British Columbia, Canada. It is located west of Mamquam Lake on the south side of Mount Garibaldi in Garibaldi Provincial Park. It was possibly named by Canadian volcanologist William Henry Mathews for its resemblance to Diamond Head in Hawaii. The peak consists of tuff breccia Breccia () is a rock composed of large angular broken fragments of minerals or rocks cemented together by a fine-grained matrix. The word has its origins in the Italian language, in which it means "rubble". A breccia may have a variety of di ... ranging in size from dust to enormous blocks. References External links * Garibaldi Ranges New Westminster Land District Two-thousanders of British Columbia {{BritishColumbiaCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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