|
Mount Aragorn (2,435m)
Mount Aragorn is a mountain summit located in the Cadwallader Range in southwestern British Columbia, Canada. It is situated north of Pemberton, west of Lillooet, and immediately north of Mount Gandalf. Precipitation runoff from the peak drains into tributaries of the Fraser River. History The first ascent of the mountain was made in 1972 by Peter Jordan, Fred Thiessen, and Eric White.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 Shadowfax. The names Aragorn, Gandalf, and Shadowfax were taken from fictional characters in the novels The Hobbit and The Lord of the Rings by J. R. R. Tolkien, which were read while waiting out stormy weather during the 1972 outing. The mountain's name was proposed in 1978 by Karl Ricker of the Alpine Club of Canada, and was officially adopted January 23, 1979, by the Geographical Names Board of Canada. Climate Based on the Köppen climate classificat ... [...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] |
The Hobbit
''The Hobbit, or There and Back Again'' is a children's fantasy novel by English author J. R. R. Tolkien. It was published in 1937 to wide critical acclaim, being nominated for the Carnegie Medal and awarded a prize from the '' New York Herald Tribune'' for best juvenile fiction. The book remains popular and is recognized as a classic in children's literature. ''The Hobbit'' is set within Tolkien's fictional universe and follows the quest of home-loving Bilbo Baggins, the titular hobbit, to win a share of the treasure guarded by a dragon named Smaug. Bilbo's journey takes him from his light-hearted, rural surroundings into more sinister territory. The story is told in the form of an episodic quest, and most chapters introduce a specific creature or type of creature of Tolkien's geography. Bilbo gains a new level of maturity, competence, and wisdom by accepting the disreputable, romantic, fey, and adventurous sides of his nature and applying his wits and common s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gandolf And Aragorn
Gandulf or Gandolf (Latin ''Gandolphus'', French ''Gandolphe'', Italian ''Gandolfo'') is a masculine given name of Germanic origin, common in the Middle Ages. The roots of the name are ''gand'' (literally "wand" or "magic wand", by extension "sorcery") and ''wolf'' ("wolf").Rosa and Volker Kohlheim, ''Lexikon der Vornamen: Herkunft, Bedeutung und Gebrauch von über 8 000 Vornamen'' (Berlin: Dudenverlag, 2016)here/ref> *Gandulf of Piacenza (10th century), Italian count * Gandulf (11th century), bishop of Reggio nell'Emilia * Gandulf (died 1184), bishop of Alba * Gandulf of Bologna (died after 1185), theologian * Gandulf (died 1229), abbot of Saint-Sixte and cardinal * Gandulf of Binasco (died 1260), Franciscan saint * Gandolphus Siculus (''floruit'' 1438–44), Sicilian papal legate to India See also * Gandalf (other) * Gandolfi *Gundulf Gundulf and its variants (Gondulf, Gundulph, Kundolf, Gondulphus, Gundulfus, Gundolfo, Gondon) is a Germanic given name, from ''gund'', "b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of British Columbia
The geology of British Columbia is a function of its location on the leading edge of the North American continent. The mountainous physiography and the diversity of rock types and ages hint at the complex geology, which is still undergoing revision despite a century of exploration and mapping. The country's most prominent geological features are mountain ranges, including the North American Cordillera, which stretches from Southern Mexico to Alaska. Terrane theory Terrane theory was first proposed by Jim Monger of the Geological Survey of Canada and Charlie Rouse in 1971 as an explanation for a set of fusulinid fossils found in central British Columbia. Rather than use facies changes or seaways (which were common explanations at the time), the two geologists proposed that the fossils in question had been part of an assemblage of rocks that had migrated across the Pacific Ocean to their present location. This theory was then developed by Porter Irwin and Davy Jones of the US ... [...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] |
Pacific Ocean
The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean (or, depending on definition, to Antarctica) in the south, and is bounded by the continents of Asia and Oceania in the west and the Americas in the east. At in area (as defined with a southern Antarctic border), this largest division of the World Ocean—and, in turn, the hydrosphere—covers about 46% of Earth's water surface and about 32% of its total surface area, larger than Earth's entire land area combined .Pacific Ocean . '' Britannica Concise.'' 2008: Encyclopædia Britannica, Inc. The centers of both the |
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] |
North America
North America is a continent in the Northern Hemisphere and almost entirely within the Western Hemisphere. It is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the southeast by South America and the Caribbean Sea, and to the west and south by the Pacific Ocean. Because it is on the North American Plate, North American Tectonic Plate, Greenland is included as a part of North America geographically. North America covers an area of about , about 16.5% of Earth's land area and about 4.8% of its total surface. North America is the third-largest continent by area, following Asia and Africa, and the list of continents and continental subregions by population, fourth by population after Asia, Africa, and Europe. In 2013, its population was estimated at nearly 579 million people in List of sovereign states and dependent territories in North America, 23 independent states, or about 7.5% of the world's population. In Americas (terminology)#Human ge ... [...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] |
Mount Aragorn (2,435m)
Mount Aragorn is a mountain summit located in the Cadwallader Range in southwestern British Columbia, Canada. It is situated north of Pemberton, west of Lillooet, and immediately north of Mount Gandalf. Precipitation runoff from the peak drains into tributaries of the Fraser River. History The first ascent of the mountain was made in 1972 by Peter Jordan, Fred Thiessen, and Eric White.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 Shadowfax. The names Aragorn, Gandalf, and Shadowfax were taken from fictional characters in the novels The Hobbit and The Lord of the Rings by J. R. R. Tolkien, which were read while waiting out stormy weather during the 1972 outing. The mountain's name was proposed in 1978 by Karl Ricker of the Alpine Club of Canada, and was officially adopted January 23, 1979, by the Geographical Names Board of Canada. Climate Based on the Köppen climate classificat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Mount Aragorn (2,435m)")
.jpg "Click for more on -> Pacific Ocean")
.jpg "Click for more on -> North America")
