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Murtle River
The Murtle River is a river in east-central British Columbia, Canada. It rises from a large unnamed glacier in the Cariboo Mountains at an elevation of and flows southwest for to the head of gigantic Murtle Lake. The river also drains Murtle Lake then flows southwest for into the Clearwater River. The Murtle River is the longest and largest tributary to the Clearwater. The Murtle River is known for having many waterfalls along its course. Between Murtle Lake and the Clearwater River, the Murtle drops over seven named waterfalls: McDougall, Meadow, Horseshoe, Majerus, Dawson, The Mushbowl and Helmcken Falls. Discovery and naming There are no records about the Murtle River being known by First Nations. The river was discovered by Joseph Hunter, a surveyor working for the future Canadian Pacific Railway, on May 25, 1874. Hunter's expedition rafted across the Clearwater River near The Horseshoe, headed east for about , and reached the Murtle River upstream from Majerus Falls. H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McDougall Falls
McDougall Falls is a waterfall on the Murtle River in Wells Gray Provincial Park, east-central British Columbia, Canada. McDougall Falls is located 5 km downstream from the Diamond Lagoon of Murtle Lake. It is 14 m high. A hiking trail follows the south shore of the Murtle River from the lagoon. This trail is only accessible by canoeing across Murtle Lake. The waterfall was discovered by Joseph Hunter, a surveyor working for the future Canadian Pacific Railway, on May 27, 1874. Hunter did not name the falls, but he did name the Murtle River and Murtle Lake for his birthplace in Scotland, Milton of Murtle, near Aberdeen. McDougall Falls and McDougall Lake McDougall Lake is a lake in Wells Gray Provincial Park in east-central British Columbia, Canada. It drains through File Creek into Murtle Lake. Naming McDougall Lake and McDougall Falls on the Murtle River were named for Pete McDougal who homeste ..., north of here, were named for Pete McDougal who homesteaded in the Clearw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meadow Falls
Meadow Falls is one of seven waterfalls on the Murtle River west of Murtle Lake in Wells Gray Provincial Park, east-central British Columbia, Canada. Meadow Falls is high.Neave, Roland (2015). ''Exploring Wells Gray Park'', 6th edition. Wells Gray Tours, Kamloops, BC. . The waterfall was discovered by Joseph Hunter, a surveyor working for the future Canadian Pacific Railway, on May 26, 1874. Hunter did not name the falls, but he did name the Murtle River and Murtle Lake for his birthplace in Scotland, Milton of Murtle, near Aberdeen. The Meadow Falls name refers to nearby marshes along the otherwise slow-moving Murtle River, a section known as The Stillwater. Visitors to Meadow Falls are rare because there is no road or trail access and the nearby marshes make cross-country travel difficult. The nearest trail ends at Horseshoe Falls Horseshoe Falls is the largest of the three waterfalls that collectively form Niagara Falls on the Niagara River along the Canada–United Sta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Horseshoe Falls (British Columbia)
Horseshoe Falls is one of seven waterfalls on the Murtle River west of Murtle Lake in Wells Gray Provincial Park, east-central British Columbia, Canada. Horseshoe Falls has two steps, apart; the upper drop is high and the lower and much wider drop is high.Neave, Roland (2015). ''Exploring Wells Gray Park'', 6th edition. Wells Gray Tours, Kamloops, BC. . The waterfall was discovered by Joseph Hunter, a surveyor working for the future Canadian Pacific Railway, on May 26, 1874. Hunter did not name the falls, but he did name the Murtle River and Murtle Lake for his birthplace in Scotland, Milton of Murtle, near Aberdeen. Horseshoe Falls was named in 1914 by land surveyor Robert Henry Lee, who mapped homesteaders' lots along the south side of the Murtle River. The river is slow-moving between Horseshoe Falls and Meadow Falls, upstream, and Lee marked a "raft crossing" on his map. Horseshoe Falls can be reached by a hiking trail from Pyramid Campground on Clearwater Valley Road. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dawson Falls
Dawson Falls is one of seven waterfalls on the Murtle River in Wells Gray Provincial Park, British Columbia, Canada. Name origin Dawson Falls was named in 1913 by land surveyor Robert Henry Lee after George Herbert Dawson, the Surveyor-General for British Columbia from 1912-1917.Neave, Roland (2015). ''Exploring Wells Gray Park'', 6th edition. Wells Gray Tours, Kamloops, BC. . Lee and his crew camped near Dawson Falls during the summers of 1913 and 1914 while they surveyed homesteaders' lots along the south side of the Murtle River. On July 24, 1913, Lee was surveying west from Dawson Falls when he discovered Helmcken Falls. Description The Wells Gray Park road (Clearwater Valley Road) passes close to Dawson Falls. The main viewpoint is a 10-minute walk and it is another few minutes to the top of the waterfall. A rough trail on the north side of the Murtle River provides a different vantage point. Pyramid Campground, one of four campgrounds in Wells Gray Park, is just northeast ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mahood Lake
Mahood Lake is a lake in the South Cariboo region of the Interior of British Columbia in Wells Gray Provincial Park. It is drained by the Mahood River, a tributary of the Clearwater River which has cut a deep canyon into Cambrian rocks and Pleistocene glacial moraines. Mahood Lake is fed by the short Canim River, which drains nearby Canim Lake to the west via Canim Falls and Mahood Falls.Neave, Roland (2015). ''Exploring Wells Gray Park'', 6th edition. Wells Gray Tours, Kamloops, BC. . The lake is 629 metres in elevation, 197 metres deep at its deepest point, approximately 33.5 km² in area, in length (east to west) and a maximum of in width. Mount Mahood is immediately south of the lake and rises to . Discovery and naming There are no written records about First Nations visits to Mahood Lake, but they did use this valley because pictographs can be seen about halfway along the south shore. The Mahood Lake area was the centre of considerable attention between 1872 and 187 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of British Columbia Rivers
The following is a partial list of rivers of British Columbia, organized by watershed. Some large creeks are included either because of size or historical importance (See Alphabetical List of British Columbia rivers ). Also included are lakes that are "in-line" connecting upper tributaries of listed rivers, or at their heads. Arctic drainage Arctic Ocean via Mackenzie River drainage :''(NB Liard tributaries on Yukon side of border omitted)'' Liard River watershed * Liard River ** Petiewewtot River **Fort Nelson River *** Sahtaneh River ****Snake River ***Muskwa River ****Prophet River ***** Minaker River *****Besa River **** Tetsa River **** Chischa River ****Tuchodi River ***Sikanni Chief River ****Buckinghorse River ***Fontas River ** Dunedin River ** Beaver River **Toad River ***West Toad River *** Racing River *** Schipa River **Grayling River ** Trout River **Vents River ** Smith River ** Coal River ** Rabbit River *** Gundahoo River **Kechika River *** Red River ***Turnag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subglacial Mound
A subglacial mound (SUGM) is a type of subglacial volcano. This type of volcano forms when lava erupts beneath a thick glacier or ice sheet. The magma forming these volcanoes was not hot enough to melt a vertical pipe right through the overlying glacial ice, instead forming hyaloclastite and pillow lava deep beneath the glacial ice field. Once the glaciers had retreated, the subglacial volcano would be revealed, with a unique shape as a result of their confinement within glacial ice. They are somewhat rare worldwide, being confined to regions which were formerly covered by continental ice sheets and also had active volcanism during the same period. They are found throughout Iceland, Antarctica and the Canadian province of British Columbia. Subglacial mounds can be mistaken for cinder cones because they may have a similar shape. An example of this confusion is Pyramid Mountain in the Wells Gray-Clearwater volcanic field The Wells Gray-Clearwater volcanic field, also called the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyramid Mountain (volcano)
Pyramid Mountain is a subglacial mound located on the Murtle River, Murtle Plateau in Wells Gray Provincial Park, east-central British Columbia, Canada. Formation Pyramid Mountain erupted about 12,000 years ago. It was once mistaken for a cinder cone and is now known to have erupted underneath about of glacial ice. The volcano erupted vigorously and cooled rapidly when the hot lava contacted the surrounding ice and melted it, creating an envelope of water around the rising volcano. The result was a cement-like surface with smoothed cobbles of granite, schist, phyllite and other non-volcanic pebbles which were carried by the ice from many kilometers distant. As a result of this type of eruption, Pyramid Mountain has no crater and no lava flows stretching away from its base. The secondary cone to the east (best seen from Clearwater Valley Road near Hemp Creek) was not formed by a separate eruption, but was simply a slump when the ice melted away from Pyramid, releasing the pressure ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McLeod Hill
McLeod Hill is a tuya, located north of Clearwater in the Wells Gray-Clearwater volcanic field in Wells Gray Provincial Park, east-central British Columbia, Canada. McLeod Hill last erupted about 12,000 years ago when the Murtle Plateau was still covered by ice. However, it may also be the oldest volcano in the Clearwater Valley, dating to about 200,000 years ago when it was the source of the vast quantity of lava that comprises the Murtle Plateau. Viewed from Green Mountain, it looks like a low rounded dome, quite different from nearby Pyramid Mountain.Goward, Trevor and Hickson, Cathie (1995). ''Nature Wells Gray'', 2nd edition. Lone Pine Publishing, Edmonton, AB. .Neave, Roland (2015). ''Exploring Wells Gray Park'', 6th edition. Wells Gray Tours, Kamloops, BC. . The Wells Gray Loppet Trail, a popular cross-country ski route, goes over McLeod Hill. It starts at the Murtle River near Dawson Falls and ends at Helmcken Falls Lodge, a distance of . The ski trail is tracked by B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fissure Vent
A fissure vent, also known as a volcanic fissure, eruption fissure or simply a fissure, is a linear volcanic vent through which lava erupts, usually without any explosive eruption, explosive activity. The vent is often a few metres wide and may be many kilometres long. Fissure vents can cause large flood basalts which run first in lava channels and later in lava tubes. After some time, the eruption tends to become focused at one or more spatter cones. Small fissure vents may not be easily discernible from the air, but the crater rows (see Laki) or the canyons (see Eldgjá) built up by some of them are. The Dike_(geology)#Magmatic_dikes, dikes that feed fissures reach the surface from depths of a few kilometers and connect them to deeper magma chamber, magma reservoirs, often under volcanic centers. Fissures are usually found in or along rifts and rift zones, such as Iceland and the East African Rift. Fissure vents are often part of the structure of shield volcanoes. Icelan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arthur Wellesley Gray
Arthur Wellesley Gray (1876 – 7 May 1944) was a British Columbia cabinet minister and mayor. He is particularly noted for his work creating some of British Columbia's early provincial parks and Wells Gray Provincial Park is named for him. His colleagues usually called him by his nickname, "Wells".Neave, Roland (2015). ''Exploring Wells Gray Park'', 6th edition. Wells Gray Tours, Kamloops, BC. . Early life Gray was born in New Westminster, British Columbia, in 1876. As a youth, he achieved distinction in lacrosse and was a member of the New Westminster Salmonbelly Club which won the world lacrosse championship in 1900. Career At age 30, Gray was elected alderman of New Westminster and at age 36 he became mayor, a post he held from 1913 to 1919 and again from 1927 to 1930. In 1927, he was also elected to the British Columbia Legislature in Victoria and was re-elected at the next four provincial elections with significant majorities. In 1933, Premier Duff Pattullo appointed Gray ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
