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Mount Shadowfax
Mount Shadowfax is a mountain summit in southwest British Columbia, Canada. Description Mount Shadowfax is located in the Cadwallader Range which is a subrange of the Coast Mountains. It is situated north of Pemberton and northeast of Mount Gandalf. Most precipitation runoff from the peak drains south to Birkenhead Lake via Phelix Creek, however a portion of the north slope drains to Cadwallader Creek, which is a tributary of the Hurley River. Shadowfax is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising over 800 meters (2,625 ft) above Phelix Creek in approximately . History The first ascent of the mountain was made May 7, 1972, by Peter Jordan and Fred Thiessen.UBC Varsity Outdoor Club Journal, vol 15, 1972, pp 52-55 This climbing party also made the first ascents of nearby Mount Gandalf and Mount Aragorn. The names Aragorn, Gandalf, and Shadowfax were taken from ficti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cadwallader Range
The Cadwallader Range, originally named the Cadwallader Mountains, is a sub-range of the Pacific Ranges of the Coast Mountains in the Bridge River-Lillooet Country of the South-Central Interior of British Columbia, Canada, located between the south end of Anderson Lake (E) and the Hurley River. According to the provincial basemap, the precise alpine boundaries of the range are McGilliray Pass, at its eastern extremity and beyond which is the Bendor Range, and the pass between Noel and Sockeye Creeks on its west, which is immediately north of the lower end of Birkenhead Lake. The officially unnamed range west of that has been called the Noel Range, after its main peak Mount Noel. At the foot of the range along its northeast flank is Cadwallader Creek, scene of the historic and once-rich Bralorne and Pioneer Mines and the ghost town of Bralorne (a.k.a. Bralorne-Pioneer). The range was named Cadwallader Mountains in 1917, and was renamed the Cadwallader Range in 1951. The name ... [...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] |
Two-thousanders Of British Columbia
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor (2,369&n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tolkien Peak
Tolkien Peak is a mountain summit located in the Cadwallader Range in southwestern British Columbia, Canada. It is situated in Birkenhead Lake Provincial Park, north of Pemberton, and south of Mount Gandalf, which is its nearest higher peak. The peak is named for J. R. R. Tolkien (1892–1973), author of the novels '' The Hobbit'' and ''The Lord of the Rings''. The names for nearby Mount Aragorn, Mount Gandalf, and Mount Shadowfax were taken from fictional characters in his books, which were read while waiting out stormy weather during the 1972 first ascents of those mountains. Precipitation runoff from the peak drains into tributaries of the Fraser River. Climate Based on the Köppen climate classification, Tolkien Peak is located in a subarctic climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains The Coast Mountains (french: La chaîne Côtière) are a major mountain range in the Pacific Co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of British Columbia
British Columbia is the westernmost province of Canada, bordered by the Pacific Ocean. With an area of it is Canada's third-largest province. The province is almost four times the size of the United Kingdom and larger than every United States state except Alaska. It is bounded on the northwest by the U.S. state of Alaska, directly north by Yukon and the Northwest Territories, on the east by Alberta, and on the south by the U.S. states of Washington, Idaho, and Montana. Formerly part of the British Empire, the southern border of British Columbia was established by the 1846 Oregon Treaty. The province is dominated by mountain ranges, among them the Canadian Rockies but dominantly the Coast Mountains, Cassiar Mountains, and the Columbia Mountains. Most of the population is concentrated on the Pacific coast, notably in the area of Vancouver, located on the southwestern tip of the mainland, which is known as the Lower Mainland. It is the most mountainous province of Canada. Statist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orographic Lift
Orographic lift occurs when an air mass is forced from a low elevation to a higher elevation as it moves over rising terrain. As the air mass gains altitude it quickly cools down adiabatically, which can raise the relative humidity to 100% and create clouds and, under the right conditions, precipitation. Orographic lifting can have a number of effects, including precipitation, rain shadowing, leeward winds, and associated clouds. Precipitation Precipitation induced by orographic lift occurs in many places throughout the world. Examples include: * The Mogollon Rim in central Arizona * The western slope of the Sierra Nevada range in California * The mountains near Baja California North – specifically La Bocana to Laguna Hanson. * The windward slopes of Khasi and Jayantia Hills (see Mawsynram) in the state of Meghalaya in India. * The Western Highlands of Yemen, which receive by far the most rain in Arabia. * The Western Ghats that run along India's western coast. * The Grea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weather Front
A weather front is a boundary separating air masses for which several characteristics differ, such as air density, wind, temperature, and humidity. Disturbed and unstable weather due to these differences often arises along the boundary. For instance, cold fronts can bring bands of thunderstorms and cumulonimbus precipitation or be preceded by squall lines, while warm fronts are usually preceded by stratiform precipitation and fog. In summer, subtler humidity gradients are known as dry lines can trigger severe weather. Some fronts produce no precipitation and little cloudiness, although there is invariably always a wind shift. Cold fronts generally move from west to east, whereas warm fronts move poleward, although any direction is possible. Occluded fronts are a hybrid merge of the two, and stationary fronts are stalled in their motion. Cold fronts and cold occlusions move faster than warm fronts and warm occlusions because the dense air behind them can lift as well as push ... [...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 ave ... [...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'' indi ... [...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 Observation), Pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Club Of Canada
The Alpine Club of Canada (ACC) is an amateur athletic association with its national office in Canmore, Alberta that has been a focal point for Canadian mountaineering since its founding in 1906. The club was co-founded by Arthur Oliver Wheeler, who served as its first president, and Elizabeth Parker, a journalist for the '' Manitoba Free Press''. Byron Harmon, whose 6500+ photographs of the Canadian Rockies in the early 20th century provide the best glimpse of the area at that time, was official photographer to the club at its founding. The club is the leading organization in Canada devoted to climbing, mountain culture, and issues related to alpine pursuits and ecology. It is also the Canadian regulatory organization for climbing competition, sanctioning local, regional and national events, and assembling, coaching and supporting the national team. The ACC is divided into 24 regional sections across Canada that serve local members and focus on local issues and access, linkin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gandalf
Gandalf is a protagonist in J. R. R. Tolkien's novels ''The Hobbit'' and ''The Lord of the Rings''. He is a Wizards (Middle-earth), wizard, one of the ''Istari'' order, and the leader of the Fellowship of the Ring (characters), Fellowship of the Ring. Tolkien took the name "Gandalf" from the Old Norse Dvergatal, "Catalogue of Dwarves" (''Dvergatal'') in the ''Völuspá''. As a wizard and the bearer of one of the Three Rings, Gandalf has great power, but works mostly by encouraging and persuading. He sets out as Gandalf the Grey, possessing great knowledge and travelling continually. Gandalf is focused on the mission to counter the Dark Lord Sauron by destroying the One Ring. He is associated with fire; his ring of power is Narya, the Ring of Fire. As such, he delights in fireworks to entertain the hobbits of the Shire, while in great need he uses fire as a weapon. As one of the Maiar, he is an immortal spirit from Valinor, but his physical body can be killed. In ''The Hobbit' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_-_11.jpg "Click for more on -> First Ascent")
