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Mount Baker (Waputik Mountains)
Mount Baker is a mountain on the Continental Divide, in Alberta and British Columbia, in the Waputik Mountains of the Canadian Rockies. It was named in 1898 by J. Norman Collie after his friend and climbing partner George Percival Baker (1855–1951), textile manufacturer, plantsman and gardener, and keen mountaineer. Baker described his visit to this area which took place in 1897.Mountaineering memories of the past. Privately printed 1951 In this small volume Baker noted that Collie also proposed to name a pass after him. Collie and Baker were accompanied by Peter Sarbach, and for the first week by H. B. Dixon as well as American members of the Appalachian Mountain Club. Mount Sarbach was named at the same time, as well as several other peaks: "We now named the peaks, after presidents of the Club of our time, Freshfield, Dent, Pilkington, and Walker." The mountain has been wrongly identified as "Stremotch Mountain" on subsequent maps and documents after a first map that was su ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Weed
Mount Weed is a mountain summit located in the Mistaya River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Mount Weed is situated at the confluence of Silverhorn Creek and Mistaya River, 3.5 kilometres southwest of Mount Noyes, 4.5 km east of Mistaya Lake, and 14 km north of Bow Lake. Its nearest higher peak is Mount Patterson, to the southwest. Patterson stands directly across the Mistaya River valley from Weed, and both are prominent features seen from the Icefields Parkway. History The mountain was named by J. Norman Collie in 1902 for George Marsten Weed (1864-1948) of the Appalachian Mountain Club, who climbed in the Rockies and made several first ascents. Collie and Weed were together in a party which made the first ascent of Mount Forbes on August 10, 1902. The mountain's name was officially adopted in 1928 by the Geographical Names Board of Canada. The first ascent of the peak was made in 1936 by L. Gest, Mr. and Mrs. H. King ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Pilkington
Mount Pilkington is located on the border of Alberta and British Columbia, between Mount Freshfield and Waitabit Peak. It was named in 1898 after Charles Pilkington. Mount Pilkington is located on the Continental Divide between the Campbell Icefield and the Freshfield Icefield. The Pilkington Ascent On August 5, 2019, Dr. Matthew B.G. Pilkington, Charles Pilkington's great-great-grandnephew, became the first Pilkington to summit the peak. Matthew's ascent was followed by his son, Dante G.M. Pilkington, who became the second Pilkington to summit Mount Pilkington. See also * List of peaks on the British Columbia–Alberta border * List of mountains in the Canadian Rockies A list of highest peaks in the Canadian Rockies is shown below: References ;Notes {{reflist, group=notes *• Canadian Rockies The Canadian Rockies (french: Rocheuses canadiennes) or Canadian Rocky Mountains, comprising both the A ... References Mountains of Banff National Park Thre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Three-thousanders Of British Columbia
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Andes) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trapper And Baker
Animal trapping, or simply trapping or gin, is the use of a device to remotely catch an animal. Animals may be trapped for a variety of purposes, including food, the fur trade, hunting, pest control, and wildlife management. History Neolithic hunters, including the members of the Cucuteni-Trypillian culture of Romania and Ukraine (c. 5500–2750 BCE), used traps to capture their prey. An early mention in written form is a passage from the self-titled book by Taoist philosopher Zhuangzi describes Chinese methods used for trapping animals during the 4th century BCE. The Zhuangzi reads, "The sleek-furred fox and the elegantly spotted leopard ... can't seem to escape the disaster of nets and traps." "Modern" steel jaw-traps were first described in western sources as early as the late 16th century. The first mention comes from Leonard Mascall's book on animal trapping. It reads, "a griping trappe made all of yrne, the lowest barre, and the ring or hoope with two clickets." ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Peaks On The Alberta–British Columbia Border
This is a list of peaks on the Alberta–British Columbia border, being the spine of the Continental Divide from the Canada–United States border The border between Canada and the United States is the longest international border in the world. The terrestrial boundary (including boundaries in the Great Lakes, Atlantic, and Pacific coasts) is long. The land border has two sections: Can ... to the 120th meridian, which is where the boundary departs the Continental Divide and goes due north to the 60th parallel. Peaks are listed from north to south and include the four peaks not on the Continental Divide but which are on the 120th Meridian, stretching approximately due north from Intersection Mountain, which as its name implies is located at the intersection of the Divide and the Meridian. See also * List of Boundary Peaks of the Alaska-British Columbia/Yukon border * Extreme points of British Columbia References {{DEFAULTSORT:List Of Peaks On The British Columbi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Habel
Mount Habel is a mountain summit located in Banff National Park on the Continental Divide along the border of Alberta and British Columbia in the Waputik Mountains, part of the Canadian Rockies. It was named in 1986 after Jean Habel. Jean Habel was a German geographer who explored the Canadian Rockies and in 1897 was the first to set foot on the Wapta Icefield which surrounds Mount Habel. __NOTOC__ Geology Like other mountains in Banff Park, Mount Habel 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. Climate Based on the Köppen climate classification, Mount Habel is located in a 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 moderati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trapper Peak (Alberta)
Trapper Peak is a mountain in Alberta and British Columbia, Canada, located on their border along the Continental Divide in the Wapta Icefield. Trapper Peak has two summits, one accessible from Baker. Peyto Peak is located to the north-east. The peak was originally named in 1892 by Walter D. Wilcox to honor his guide, trapper Bill Peyto, and the first ascent was in 1933 by Conrad Kain and party. Geology Trapper Peak 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. Climate Based on the Köppen climate classification, Trapper Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below . See also * List of peaks on the Alberta–British Columbia border This is a list of peaks on the Alberta–British Columbia border, being the s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Line Parent
A peak's line parent is the closest higher peak on the highest ridge leading away from the peak's "key col". A col is the lowest point on the ridge between two summits and is roughly synonymous with pass, gap, saddle and notch. The highest col of a peak is its key col. If there is more than one ridge which can be followed to a higher peak then the line parent is the peak closest to the key col. Usually, a line parent must meet some prominence criteria, which might vary depending on the author and the location of the peak. There are at least two other kinds of peak parentage. Island parentage, which is also referred to as encirclement or topographic parentage; and source parentage. See also * Topographic prominence In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest cont ... References ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Patterson
Mount Patterson is a peak in the Waputik Range of the Canadian Rockies. It is located within Banff National Park in Alberta of Western Canada. Mount Patterson stands across the Mistaya River Valley from Mount Weed, and both are prominent features seen from the Icefields Parkway. Its nearest higher peak is Howse Peak, to the northwest. It was named in 1917 after John Duncan Patterson who was president of the Alpine Club of Canada from 1914 to 1920. Geology Like other mountains in Banff Park, Mount Patterson 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. Climate Based on the Köppen climate classification, Mount Patterson is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below with wind chill factors below . Precipitation runoff from Mount Patterson drain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canadian Alpine Journal
The ''Canadian Alpine Journal'' is the yearly magazine of the Alpine Club of Canada. It serves as a worldwide journal of record for achievements in climbing, mountaineering, ski mountaineering, and exploration of mountains. The magazine is headquartered in Toronto, Ontario. Each issue contains feature stories about notable climbs, written by the participants, as well as short notes by climbers about new and noteworthy achievements. Some general articles about mountaineering, mountain medicine, the mountain environment, or other topics are also sometimes included. Each issue includes book reviews, memorials of deceased members, and club activities. History The journal was founded in 1907, and during the early decades some volumes covered more than one year. Since 1947 (volume 30), the journal has been published annually. Similar journals Other magazines of record for climbing include the ''American Alpine Journal'' published by the American Alpine Club, the ''Alpine Journal' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wapta Icefield
The Wapta Icefield is located on the Continental Divide in the Waputik Mountains of the Canadian Rockies, in the provinces of British Columbia and Alberta. The icefield is shared by Banff and Yoho National Parks and numerous outlet glaciers extend from the icefield, including the Vulture, Bow and Peyto Glaciers. Runoff from the icefields and outlet glaciers supply water to both the Kicking Horse and Bow Rivers, as well as numerous streams and lakes. The icefield is one of the most studied in the Canadian Rockies and all evidence supports the conclusion that the icefield is shrinking in area, especially near the lowest altitudes of its outlet glaciers, including Peyto Glacier, in which the glacier has become both shorter in length and thinner in thickness. In the 1980s the icefield covered an area of approximately . The icefield is easily accessible by mountaineers in both the summer and winter. Both ski trips in the winter and glacier hiking trips in the summer often combine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
