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29-563: In 1907, Dr. Donaldson Bogart Dowling, an engineer with the Geological Survey of Canada , named the mountain for John Alfred (Fred) Kidd, who was a resident of nearby Morley , Alberta. From 1902 to 1907, Kidd ran the Morley general store and outfitted expeditions and geological survey crews such as Dowling's with supplies. The first ascent of the mountain was made in 1947 by R. C. Hind and J. F. Tarrant. The mountain's name

58-569: A 5.8 route called The Fold on the south peak. In 1985, Rudi Kranabitter and Ferdl Taxbock made the first ascent of this now-classic route. Ice Climbing Routes with grades on Mount Kidd: Mount Bogart Mount Bogart is a 3,144-metre (10,315-foot) summit located in Kananaskis Country in the Canadian Rockies of Alberta , Canada . Mount Bogart's nearest higher peak is Wind Mountain, 4.7 km (2.9 mi) to

87-619: A dry winter, are found in parts of East Asia, like China, where the Siberian High makes the winters colder than places like Scandinavia or Alaska interior but extremely dry (typically with around 5 millimeters (0.20 in) of rainfall equivalent per month), meaning that winter snow cover is very limited. The Dwc climate can be found in: In the Southern Hemisphere, small pockets of the Lesotho Highlands and

116-469: A subarctic climate, receives an average rain-equivalent of 101.91 inches (2,588.5 mm) of precipitation per year. Coastal areas of Khabarovsk Krai also have much higher precipitation in summer due to orographic influences (up to 175 millimetres (6.9 in) in July in some areas), whilst the mountainous Kamchatka peninsula and Sakhalin island are even wetter, since orographic moisture isn't confined to

145-523: Is a tributary of the Bow River , and thence the Saskatchewan River . Mount Kidd has two summits, a north and south peak, each with scramble routes. The more massive north peak is the true summit at 2,958 m (9,705 ft), whereas the lesser south peak rises to 2,895 m (9,498 ft). Additionally, Mount Kidd has a class 5.7 rock climbing route on its northeast buttress, as well

174-507: Is excessive. The frost-free season is very short, varying from about 45 to 100 days at most, and a freeze can occur anytime outside the summer months in many areas. The first D indicates continentality, with the coldest month below 0 °C (32 °F) (or −3 °C (27 °F)). The second letter denotes precipitation patterns: The third letter denotes temperature: Most subarctic climates have little precipitation, typically no more than 380 mm (15 in) over an entire year due to

203-676: Is found in the following areas: Further north and east in Siberia, continentality increases so much that winters can be exceptionally severe, averaging below −38 °C (−36 °F), even though the hottest month still averages more than 10 °C (50 °F). This creates Dfd climates, which are mostly found in the Sakha Republic : In the Southern Hemisphere , the Dfc climate is found only in small, isolated pockets in

232-529: Is located in a subarctic climate zone with cold snowy winters and mild summers. Temperatures can drop below −20 °C (−4 °F) with wind chill factors below −30 °C (−22 °F). Weather conditions during winter make Mount Kidd one of the better places in the Rockies for ice climbing . Precipitation runoff from the mountain drains into the Kananaskis River which

261-781: The Pacific Ocean , resulting in increased precipitation, especially during the winter months. This climate zone supports the presence of temperate rainforests, mostly on highest areas of the Valdivian rainforest in Chile and the subantarctic forest in Argentina. Climates classified as Dsc or Dsd , with a dry summer, are rare, occurring in very small areas at high elevation around the Mediterranean Basin , Iran , Kyrgyzstan , Tajikistan , Alaska and other parts of

290-666: The Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny . The Lewis Overthrust extends over 450 km (280 mi) from Mount Kidd south to Steamboat Mountain, located west of Great Falls, Montana. Mount Kidd marks the northern end of the Lewis Thrust Fault. Based on the Köppen climate classification , Mount Kidd

319-713: The Snowy Mountains of Australia , the Southern Alps of New Zealand , and the Lesotho Highlands . In South America , this climate occurs on the western slope of the central Andes in Chile and Argentina , where climatic conditions are notably more humid compared to the eastern slope. The presence of the Andes mountain range contributes to a wetter climate on the western slope by capturing moisture from

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348-420: The humid continental climates . Like other Class D climates, they are rare in the Southern Hemisphere, only found at some isolated highland elevations. 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 . This type of climate offers some of

377-667: The northwestern United States ( Eastern Washington , Eastern Oregon , Southern Idaho , California's Eastern Sierra ), the Russian Far East , Akureyri, Iceland , Seneca, Oregon , and Atlin, British Columbia . Turkey and Afghanistan are exceptions; Dsc climates are common in Northeast Anatolia , in the Taurus and Köroğlu Mountains , and the Central Afghan highlands . In the Southern Hemisphere,

406-416: The subpolar oceanic climate , as the sea is approached where winter temperatures average near or above freezing despite maintaining the short, cool summers. In China and Mongolia, as one moves southwestwards or towards lower elevations, temperatures increase but precipitation is so low that the subarctic climate grades into a cold semi-arid climate . The Dfc climate, by far the most common subarctic type,

435-823: The Dsc climate is present in South America as a subarctic climate influenced by Mediterranean characteristics, often considered a high-altitude variant of the Mediterranean climate. It is located on the eastern slopes of the central Argentine Andes and in some sections on the Chilean side. While there are no major settlements exhibiting this climate, several localities in the vicinity experience it, such as San Carlos de Bariloche , Villa La Angostura , San Martín de los Andes , Balmaceda , Punta de Vacas , and Termas del Flaco . Climates classified as Dwc or Dwd , with

464-430: The coldest month should average below 0 °C (32 °F) (or −3 °C (27 °F)). Record low temperatures can approach −70 °C (−94 °F). With 5–7 consecutive months when the average temperature is below freezing, all moisture in the soil and subsoil freezes solidly to depths of many feet. Summer warmth is insufficient to thaw more than a few surface feet, so permafrost prevails under most areas not near

493-406: The long summer days at such latitudes do permit some agriculture. In some areas, ice has scoured rock surfaces bare, entirely stripping off the overburden. Elsewhere, rock basins have been formed and stream courses dammed, creating countless lakes. Should one go northward or even toward a polar sea, one finds that the warmest month has an average temperature of less than 10 °C (50 °F), and

522-423: The long winters and make use of the short summers. Trees are mostly limited to conifers , as few broadleaved trees are able to survive the very low temperatures in winter. This type of forest is also known as taiga , a term which is sometimes applied to the climate found therein as well. Even though the diversity may be low, the area and numbers are high, and the taiga (boreal) forest is the largest forest biome on

551-425: The low temperatures and evapotranspiration . Away from the coasts, precipitation occurs mostly in the summer months, while in coastal areas with subarctic climates the heaviest precipitation is usually during the autumn months when the relative warmth of sea vis-à-vis land is greatest. Low precipitation, by the standards of more temperate regions with longer summers and warmer winters, is typically sufficient in view of

580-418: The most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below −50 °C (−58 °F) and in summer, the temperature may exceed 26 °C (79 °F). 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 10 °C (50 °F) to fall into this category of climate, and

609-478: The mountain drains east into the Kananaskis River and west into Spray Lakes Reservoir which both empty to the Bow River . Subarctic climate The subarctic climate (also called subpolar climate , or boreal climate ) is a continental 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°N to 70°N, poleward of

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638-613: The north. Mount Bogart is situated northwest of Mount Kidd , and both can be seen from Highway 40 near the Kananaskis Village junction. Mount Bogart was named by Donaldson Bogart Dowling (1858-1925), after his mother, whose maiden name was Bogart. Donaldson Dowling, an engineer with the Geological Survey of Canada , explored the area in 1904. The first ascent of the peak was made in 1930 by Kate Gardiner and Walter Feuz. The duo also made first ascents of Mount Lyautey and Mount Galatea in 1930. The mountain's name

667-460: The planet, with most of the forests located in Russia and Canada . The process by which plants become acclimated to cold temperatures is called hardening . Agricultural potential is generally poor, due to the natural infertility of soils and the prevalence of swamps and lakes left by departing ice sheets , and short growing seasons prohibit all but the hardiest of crops. Despite the short season,

696-453: The southern boundary of this climate zone. Seasonal thaw penetrates from 2 to 14 ft (0.6 to 4.3 m), depending on latitude, aspect, and type of ground. Some northern areas with subarctic climates located near oceans (southern Alaska , northern Norway , Sakhalin Oblast and Kamchatka Oblast ), have milder winters and no permafrost, and are more suited for farming unless precipitation

725-403: The subarctic climate grades into a tundra climate not at all suitable for trees. Southward, this climate grades into the humid continental climates with longer summers (and usually less-severe winters) allowing broadleaf trees ; in a few locations close to a temperate sea (as in northern Norway and southern Alaska ), this climate can grade into a short-summer version of an oceanic climate ,

754-428: The very low evapotranspiration to allow a water-logged terrain in many areas of subarctic climate and to permit snow cover during winter, which is generally persistent for an extended period. A notable exception to this pattern is that subarctic climates occurring at high elevations in otherwise temperate regions have extremely high precipitation due to orographic lift . Mount Washington , with temperatures typical of

783-519: The warmer months and creates large glaciers in Kamchatka. Labrador , in eastern Canada, is similarly wet throughout the year due to the semi-permanent Icelandic Low and can receive up to 1,300 millimetres (51 in) of rainfall equivalent per year, creating a snow cover of up to 1.5 metres (59 in) that does not melt until June. Vegetation in regions with subarctic climates is generally of low diversity, as only hardy tree species can survive

812-563: Was officially adopted in 1953 by the Geographical Names Board of Canada . In June 1986, Mount Kidd was the scene of the first of three related airplane crashes known as the Rescue 807 Crashes . In August 2010, James Hoshizaki stepped onto a snow cornice to pose for a photo when it gave way, resulting in an avalanche that swept him down about 200 metres to his death. Mount Kidd is composed of sedimentary rock laid down during

841-553: Was officially adopted in 2006 by the Geographical Names Board of Canada . Mount Bogart is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny . Based on the Köppen climate classification , Mount Bogart is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from

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