|
Mount Tilley (Canada)
Mount Tilley is a mountain summit located in the Gold Range of the Monashee Mountains in British Columbia, Canada. Situated west of the Columbia River and Upper Arrow Lake, this peak is visible from the Trans-Canada Highway, Revelstoke, and Revelstoke Mountain Resort ski area. Its nearest higher peak is Mount Begbie, to the east, with Tilley Lake set in the saddle between the two peaks. History Mount Tilley was named for Sir Samuel Leonard Tilley (1818–1896), a Canadian politician and one of the Fathers of Confederation. The mountain's name was officially adopted in 1924 by the Geographical Names Board of Canada, although this toponym had appeared in publications as early as 1887, if not earlier. The first ascent of the mountain was made in 1968 by Bruce Haggerstone and David P. Jones. Climate Based on the Köppen climate classification, Mount Tilley is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below − ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monashee Mountains
The Monashee Mountains are a mountain range lying mostly in British Columbia, Canada, extending into the U.S. state of Washington. They stretch from north to south and from east to west. They are a sub-range of the Columbia Mountains. The highest summit is Mount Monashee, which reaches . The name is from the Scottish Gaelic ''monadh'' and ''sìth,'' meaning "moor" and "peace". Geography The Monashee Mountains are limited on the east by the Columbia River and Arrow Lakes, beyond which lie the Selkirk Mountains. They are limited on the west by the upper North Thompson River and the Interior Plateau. The northern end of the range is Canoe Mountain at the south end of the Robson Valley, near of the town of Valemount, British Columbia. The southern extremity of the range is in Washington State, where the Kettle River Range reaches the confluence of the Kettle River and the Columbia, and reaches west to the southern extremity of the Okanagan Highland (spelled Okanogan Hig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Samuel Leonard Tilley
Sir Samuel Leonard Tilley (May 8, 1818June 25, 1896) was a Canadian politician and one of the Fathers of Confederation. Tilley was descended from United Empire Loyalists on both sides of his family. As a pharmacist, he went into business as a druggist. Personal life Born in Gagetown, New Brunswick, Tilley was the son of storekeeper Thomas Morgan Tilley and Susan Ann Peters. He was a descendant of American loyalists on both sides of his family. On May 6, 1843 he married Julia Ann Hanford in Saint John, New Brunswick; they had eight children. Hanford died in 1862, leaving Tilley a widower. On October 22, 1867, he married Alice Starr Chipman in St. Stephen, New Brunswick; they had two children, including future New Brunswick premier Leonard Percy de Wolfe Tilley. Samuel Leonard Tilley died in 1896 on June 25. Political career Samuel Leonard Tilley entered politics as an activist in the temperance movement. As a result of the 1848 recession, caused in part by Britain's e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Macpherson (Canada)
Mount Macpherson is a mountain summit located in the Gold Range of the Monashee Mountains in British Columbia, Canada. Situated southwest of Revelstoke and west of the Columbia River and Upper Arrow Lake, this peak is visible from Revelstoke, the Trans-Canada Highway, and Revelstoke Mountain Resort ski area. Its nearest higher peak is Mount Tilley, to the south, and Mount Begbie is to the south-southeast. __NOTOC__ History Mount Macpherson was named for Sir David Lewis Macpherson (1818–1896)), a Canadian businessman, member of the Senate of Canada, and Minister of the Interior. The mountain's name was officially adopted September 30, 1932, by the Geographical Names Board of Canada, although this toponym had appeared in publications as early as 1887, if not earlier. Climate Based on the Köppen climate classification, Mount Macpherson is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount English
Mount English is a mountain summit located in the Gold Range of the Monashee Mountains of British Columbia, Canada. Situated southwest of Revelstoke, this peak is visible from the Trans-Canada Highway and Revelstoke Mountain Resort ski slopes. Neighbors include Mount Macpherson to the northeast, Mount Tilley to the east, and Mount Begbie is to the east. Precipitation runoff from Mount English drains into tributaries of the Eagle River. Topographic relief is significant as the summit rises 1,540 meters (5,052 ft) above Wap Creek in . Etymology Mount English was named to remember George Melville English (1918–1943), a Canadian Army Sergeant from Revelstoke. He served with the Royal Canadian Artillery, but he died September 15, 1943, age 24, in an automobile accident. The mountain's toponym was officially adopted April 29, 1965, by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Mount English is located in a subarctic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fraser River
The Fraser River is the longest river within British Columbia, Canada, rising at Fraser Pass near Blackrock Mountain in the Rocky Mountains and flowing for , into the Strait of Georgia just south of the City of Vancouver. The river's annual discharge at its mouth is or , and it discharges 20 million tons of sediment into the ocean. Naming The river is named after Simon Fraser, who led an expedition in 1808 on behalf of the North West Company from the site of present-day Prince George almost to the mouth of the river. The river's name in the Halqemeylem (Upriver Halkomelem) language is , often seen archaically as Staulo, and has been adopted by the Halkomelem-speaking peoples of the Lower Mainland as their collective name, . The river's name in the Dakelh language is . The ''Tsilhqot'in'' name for the river, not dissimilar to the ''Dakelh'' name, is , meaning Sturgeon ''()'' River ''()''. Course The Fraser drains a area. Its source is a dripping spring at Fras ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eagle River (Shuswap Lake)
The Eagle River is a river in the Canadian province of British Columbia. The river was named by Walter Moberly after following the flight of eagles and finding Eagle Pass. Course The Eagle River originates in the mountains west of Revelstoke and flows west and southwest, entering Shuswap Lake at Sicamous. The Eagle River is part of the Fraser River drainage basin, via the Thompson River. The Perry River is a major tributary, joining Eagle River near Malakwa. See also *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 th ... References Rivers of British Columbia {{BritishColumbia-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surface Runoff
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'', ''Dwd'' and ''Dsd''. Description This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below and in summer, the temperature may exceed . However, the summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least to fall into this category of climate, and the coldest month should a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
First Ascent
In mountaineering, a first ascent (abbreviated to FA in guide books) is the first successful, documented attainment of the top of a mountain or the first to follow a particular climbing route. First mountain ascents are notable because they entail genuine exploration, with greater risks, challenges and recognition than climbing a route pioneered by others. The person who performs the first ascent is called the first ascensionist. In free climbing, a first ascent (or first free ascent, abbreviated FFA) of a climbing route is the first successful, documented climb of a route without using equipment such as anchors or ropes for aiding progression or resting. History The details of the first ascents of even many prominent mountains are scanty or unknown; sometimes the only evidence of prior summiting is a cairn, artifacts, or inscriptions at the top. Today, first ascents are generally carefully recorded and usually mentioned in guidebooks. The term is also used when referrin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geographical Names Board Of Canada
The Geographical Names Board of Canada (GNBC) is a national committee with a secretariat in Natural Resources Canada, part of the Government of Canada, which authorizes the names used and name changes on official federal government maps of Canada created since 1897. The board consists of 27 members, one from each of the provinces and territories, and others from departments of the Government of Canada. The board also is involved with names of areas in the Antarctic through the Antarctic Treaty. Structure The secretariat is provided by Natural Resources Canada. In addition to the provincial and territorial members are members from the following federal government departments: Aboriginal Affairs and Northern Development Canada, Canada Post Corporation, Fisheries and Oceans Canada, Elections Canada, Library and Archives Canada, Department of National Defence, Natural Resources Canada (including Geological Survey of Canada and Canada Centre for Mapping and Earth Observatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Father Of Confederation
The Fathers of Confederation are the 36 people who attended at least one of the Charlottetown Conference of 1864 (23 attendees), the Quebec Conference of 1864 (33 attendees), and the London Conference of 1866 (16 attendees), preceding Canadian Confederation. Only eleven people attended all three conferences. Table of participation The following table lists the participants in the Charlottetown, Quebec, and London Conferences and their attendance at each stage. Group photographs Other possible claimants to title Four other individuals have been labelled as Fathers of Confederation. Hewitt Bernard, who was the recording secretary at the Charlottetown Conference, is considered by some to be a Father of Confederation. The leaders most responsible for bringing three specific provinces into Confederation after 1867 are also referred to as Fathers of Confederation. * The provisional government established by Louis Riel ultimately negotiated the terms under which Manitoba ent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_-_11.jpg "Click for more on -> First Ascent")
