Unlike the Hudson's Bay Company, which maintained permanent forts in the wilderness and bartered with the native people for their furs, Ashley's group had no traders, no permanent forts, no Native American trappers. The mountain men more often than not gathered the furs themselves and brought their harvest to an annual rendezvous at some previously appointed spot in the fur country. There they received their year's wages and obtained new supplies for the fall hunt. Because they spent many years together in the mountains they were known then and thereafter as the mountain men. They were a tough and self-reliant crew, able to deal with and fight the Native Americans and to survive in the wilderness alone.
The mountain men were members of loose companies; after Ashley retired, the company of Smith, Jackson, and Sublette was formed, to be succeeded by the Rocky Mountain Fur Company. The annual rendezvous was an occasion of rough celebration—for many of the mountain men the nearest approach to civilization that they had for several years at a stretch. Prominent among the mountain men were Thomas Fitzpatrick, James Bridger, Jedediah S. Smith, Kit Carson, John Colter, William Sublette, Hugh Glass, W. S. (Old Bill) Williams, and Ceran St. Vrain. The country of the Southwest where Carson, the Bent brothers, Ewing Young, and others traded among the "civilized" Native Americans is also often considered part of the territory of the mountain men.
The Hudson's Bay Company from the Columbia River country also sent men into the mountains and the Great Basin, notably Alexander Ross and Peter Skene Ogden. In 1832 the American Fur Company began to send traders and trappers into the territory of the mountain men; some of their agents were outsmarted by their rivals and killed by the Native Americans, but the company persisted with its activities and ultimately employed many of the old mountain men.
With the expeditions of John C. Frémont (who was guided by mountain men) and the beginning of the wagon trains of settlers to Oregon (also guided by mountain men), the old life began to change. Its end was hastened by a change in fashions, which undermined the fur trade. In the late 1830s the beaver hat went out of style with the result that the price of beaver pelts declined to such a low point that it was no longer profitable for the mountain men to pursue their intense struggle with the wilderness. By the early 1840s their trapping activities had ceased.
See also fur trade.
See H. M. Chittenden, The American Fur Trade of the Far West (3 vol., 1902; repr. 1974); S. Vestal, The Mountain Men (1937); B. De Voto, Across the Wide Missouri (1947, repr. 1964); I. Stone, Men to Match My Mountains (1956); D. Berry, A Majority of Scoundrels (1961, repr. 1971); P. C. Phillips, The Fur Trade (1961); R. M. Utley, A Life Wild and Perilous (1997).
There are three types of mountain climbing. In the easiest, trail climbing, participants merely hike along trails to the top of a particular mountain. The trails generally are not very steep, and the mountains are relatively small. Rock climbing takes place on steeper slopes and larger mountains. Participants generally have to ascend on hands and feet, employing special equipment that may include thick rubber-soled boots or other special shoes, rope, and steel spikes, known as pitons, that are driven into the rock as an aid to climbing. Ice climbing is generally required only on extremely high mountains whose peaks are above the timber line. Equipment used in ice climbing includes the ice axe and attachable boot spikes, known as crampons, that are used on hard ice or snow.
Almost all the famous ascents have involved rock and ice climbing. The first significant achievements in mountain climbing were the ascents of Mont Blanc made by Jacques Balmat and Michel G. Paccard (1786) and by Horace B. de Saussure (1787). The ascent of other Alpine peaks, including the Ortles (1804), Jungfrau (1811), Finsteraarhorn (1812), and Mont Pelvou (1848) soon followed, and much useful information was gathered by geologists and topographers.
Modern mountain climbing may be dated from the ascent of Switzerland's Wetterhorn (1854). This feat was followed by a decade in which the popularity of mountain climbing grew tremendously, sparking the founding (1858) of the Alpine Club, in London, and the launching (1863) of its publication, the Alpine Journal. An elite class of professional guides soon established itself, and techniques for snow, ice, and rock climbing were developed to the point where highly hazardous ascents were possible for the experienced. This so-called golden age of mountain climbing came to an end with the conquest of the Matterhorn, the last of the great Alpine mountains, by Edward Whymper (1865).
As the Alps became familiar, climbers ventured to other mountainous areas. The English Lake District, Wales, and the Scottish Highlands offered climbing challenges of all degrees of difficulty. William C. Slingsby led the way to the Norwegian mountains; Douglas W. Freshfield was one of the pioneer climbers in the Caucasus, soon followed by Albert F. Mummery. In Africa, Kilimanjaro (1889) and Mt. Kenya (1899) were climbed; the duke of the Abruzzi explored the Ruwenzori group in 1906. In the United States, Grand Teton in the Teton Range was climbed in 1872. In the 1860s and 70s Clarence King and John Muir ranged through the Sierra Nevada. In Alaska, Mt. St. Elias was climbed by the duke of the Abruzzi in 1897; Mt. Blackburn and Mt. McKinley were ascended in 1912 and 1913, respectively. In South America, Whymper climbed Chimborazo (1880) and Aconcagua and Tupungato (both: 1897). Gongga (Minya Konka), in China, was climbed in 1932.
The most challenging of all have proved to be the mountain systems of the Himalayas. Conway of Allington explored the Karakorum range in 1892; in 1895 J. Norman Collie, C. G. Bruce, Geoffrey Hastings, and Albert Mummery attempted Nanga Parbat, but the effort was given up after Mummery's disappearance on the mountain's western face. It was not until 58 years later that Nanga Parbat was climbed by Herman Buhl. In 1950, Maurice Herzog scaled Annapurna. The three towering giants—Mt. Everest, K2 (Mt. Godwin-Austen), and Mt. Kanchenjunga—were conquered in the 1950s: Edmund Hillary and Tenzing Norgay were the first to ascend Everest, the world's tallest mountain, in 1953; an Italian team led by Ardito Desio climbed K2 in 1954; and in 1955 a British expedition led by Charles Evans surmounted Kanchenjunga. With the Chinese claim of an ascent of Gosainthan in 1964, the world's ten tallest mountains, all in the Himalayas, were finally conquered. Two other notable events in mountaineering were the scaling (1961) of the south face of Mt. McKinley and the winter ascent (1961) of the north wall of the Eiger in the Alps.
Many mountain climbing clubs have been formed, notably the Schweizer Alpen Club, Club Alpino Italiano, Club Alpin Français, the Himalayan Club, the Alpine Club (London), the Alpine Club of Canada, and the American Alpine Club. Most of these render valuable service by building and maintaining shelter huts and providing information concerning topography, routes, and mountain craft.
There is a rich and extensive literature of mountain climbing. See E. Whymper, Scrambles amongst the Alps (1871, 6th ed. 1936, repr. 1966); D. W. Freshfield, The Exploration of the Caucasus (2d ed. 1902); H. W. Tilman, The Ascent of Nanda Devi (1937) and Mount Everest, 1938 (1948); H. E. G. Tyndale, Mountain Paths (1949); W. R. Irwin, ed., Challenge: An Anthology of the Literature of Mountaineering (1950); Sir Arnold H. M. Lunn, A Century of Mountaineering, 1857-1957 (1958); J. Bernstein, Ascent (1965); S. Styles, Foundations of Climbing (1966) and On Top of the World (1967); A. J. Huxley, ed., Standard Encyclopedia of the World's Mountains (1969); F. Fleming, Killing Dragons: The Conquest of the Alps (2000).
Most of the great mountain systems now in existence were developed fairly late in geologic history. The greatest mountain masses are in North and South America, including the Andes, Rockies, Sierra Nevada, and Coast Ranges of the United States, Canada, and Alaska; and the Eurasian mountain belt, in which lie the Pyrenees, Atlas, Alps, Balkans, Caucasus, Hindu Kush, Himalayas, and other ranges. Among notable single peaks are Everest, K2 (Godwin-Austen), and Kanchenjunga in Asia; Aconcagua, Chimborazo, and Cotopaxi in South America; McKinley, Logan, and Popocatepetl in North America; Mont Blanc and Elbrus in Europe; Kilimanjaro, Kenya, and Ruwenzori in Africa.
Mountains have important effects upon the climate, population, economy, and state of civilization of the regions in which they occur. By intercepting prevailing winds they cause precipitation; regions on the windward side of a great range thus have plentiful rainfall, while those on its lee side are arid. Mountains are in general thinly populated, not only because the cold climate and rarefied atmosphere of high regions are unfavorable to human life, but also because the higher reaches of mountains are unfit for agriculture. Mountains frequently contain valuable mineral ores, deposited out of solution by water or by gases. Mountains act as natural barriers between countries and peoples; they determine the routes followed by traders, migrants, and invading armies. The difficulties of travel and communication in mountain regions tend to favor political disunity.
Mountains and mountain ranges have varied origins. Some are the erosional remnants of plateaus; others are cones built up by volcanoes, such as Mt. Rainier in Washington, or domes pushed up by intrusive igneous rock (see rock), such as the Black Hills of South Dakota and the Henry Mts., Utah. Fault-block mountains (see fault) are formed by the raising of huge blocks of the earth's surface relative to the neighboring blocks. The Basin and Range region of Nevada, Arizona, New Mexico, and Utah is one of the most extensive regions of fault-block mountains.
All the great mountain chains of the earth are either fold mountains or complex structures in whose formation folding, faulting, or igneous activity have taken part. The growth of folded or complex mountain ranges is preceded by the accumulation of vast thicknesses of marine sediments. It was first suggested in the late 1800s that these sediments accumulated in elongated troughs, or geosynclines, that were occupied by arms of the sea. While some of the sediment was derived from the interior of the continent, great quantities of sediment were apparently derived from regions now offshore from the continent. For examples, sedimentary rocks of the Appalachian Mts. formed in a vast geosyncline that extended from the Gulf states northeastward through the eastern states and New England, and into E Canada. It is now recognized that great thicknesses of sediment can occur wherever there is subsidence (lowering of the earth's crust).
The best modern analogues of geosynclines appear to be the thick deposits of sediment making up the continental shelves and continental rises (see ocean). Most geologists now believe that the geosynclinal sediments found in mountain ranges were initially deposited under similar conditions. The period of sedimentation is followed by folding and thrust faulting, with most high mountain ranges uplifted vertically subsequent to folding. The movements of the earth's surface that result in the building of mountains are compression, which produces folding, thrust faulting, and possibly some normal faulting; tension, which produces most normal faulting; and vertical uplift. Mountains are subject to continuous erosion during and after uplift. Sharp peaks are formed and are subsequently attacked and leveled. Mountains may be entirely base-leveled, or they may be rejuvenated by new uplifts.
The ultimate cause of mountain-building forces has been a source of controversy, and many hypotheses have been suggested. An old hypothesis held that earth movements were adjustments of the crust of the earth to a shrinking interior that contracted and set up stresses due either to heat loss or gravitational compaction. Another hypothesis suggested that earth movements were primarily isostatic, i.e., adjustments that kept the weights of sections of the crust nearly equal (see continent). A third hypothesis, popular from the early 1960s to today, ascribed mountain-building stresses to convection currents in a hot semiplastic region in the earth's mantle.
According to the plate tectonics theory, the lithosphere is broken into several plates, each consisting of oceanic crust, continental crust, or a combination of both. These plates are in constant motion, sideswiping one another or colliding, and continually changing in size and shape. Where two plates collide, compressional stresses are generated along the margin of the plate containing a continent. Such stresses result in the deformation and uplift of the continental shelf and continental rise sediments into complex folded and faulted mountain chains (see seafloor spreading; continental drift).
See W. M. Bueler, Mountains of the World (1970); K. Hsu, Mountain Building Processes (1986); A. J. Gerrard, Mountain Environments (1990).
After three days (Sept. 8-11) of defending themselves behind their wagons, the emigrants were approached under a flag of truce by the Mormons, who offered to protect them in a retreat to Cedar City but instructed them to go unarmed and on foot, ostensibly to allay the suspicions of the Paiute. While following these instructions, the entire party, with the exception of 18 young children, were massacred. The Mormons were charged with inciting and directing the attack, and anti-Mormon feeling was intensified; Mormons attempted to blame the attack on the Paiutes. Several investigations were made, but it was not until 1874 that Lee, a fanatical Mormon and adopted son of Brigham Young, was arrested. In 1875, Lee and three associates accused of complicity were excommunicated. Lee was convicted of murder and in 1877 was put to death at the Mountain Meadows site. No other members of the raiding party were ever charged. Into the 1990s the Paiutes continued to be widely blamed for the massacre, which remains a controversial event in the history of the American West.
See studies by J. Brooks (2d ed. 1962, repr. 1970), W. Bagley (2002), and S. Denton (2003).
See biography by J. G. T. Spink (1947).
Acute reaction to a change from low altitudes to altitudes above 8,000 ft (2,400 m). Most people gradually adapt, but some have a severe reaction that can be fatal unless they return to low altitude. Normal adaptations to the reduced oxygen at high altitude (e.g., breathlessness, racing heartbeat) are exaggerated; other manifestations include headache, gastrointestinal upsets, and weakness. Pulmonary edema is quickly reversed with oxygen and evacuation to a lower area.
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Bighorn sheep (Ovis canadensis).
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Mountain range, southern Montana and northern Wyoming, U.S. It is a range of the northern Rocky Mountains extending 120 mi (193 km), rising abruptly 4,000–5,000 ft (1,200–1,500 m) above the Great Plains and Bighorn Basin. The highest summit is Wyoming's Cloud Peak, at 13,165 ft (4,013 m). Bighorn National Forest covers part of the range. On Medicine Mountain is the Medicine Wheel, a prehistoric stone-spoked circle 70 ft (20 m) in diameter.
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Species (Puma concolor) of large, graceful cat that lives in a wide variety of habitats in the Americas, from southern Alaska to Patagonia. In many regions, the species is restricted to wilderness areas, and some subspecies are considered endangered. Cougars' coloration ranges from pale buff to reddish brown, with dark ears and tail tip and white rump and belly. The adult weighs from 77 to more than 220 lb (35 to 100 kg). A male may be about 9 ft (3 m) long, one-third of which is tail, and stand 24–30 in. (60–75 cm) tall at the shoulder. Since the cougar occasionally kills livestock, it has been intensively hunted by farmers, especially in North America, and has been basically exterminated from the eastern U.S. It is valuable for preventing overpopulation of prey animals (mostly deer, in North America). In North America, cougar attacks on humans occur a few times per year, some being fatal.
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Mountain goat (Oreamnos americanus)
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Sport of attaining, or attempting to attain, high points in mountainous regions, mainly for the joy of the climb. The pleasures of mountaineering lie not only in the conquest of the peak but also in the physical and spiritual satisfactions brought about through intense personal effort, ever-increasing proficiency, and contact with natural grandeur. The greater rewards do not come without considerable risk and danger. The first great peak ascended in modern times was Mont Blanc, in 1786. Other Alpine peaks followed, capped by the ascent of the Matterhorn in 1865. By the 1910s, most peaks of the Andes, the Rockies, and other Western Hemisphere ranges had been climbed, including Mount McKinley (1913). Beginning in the 1930s a series of successful ascents of mountains in the Himalayas occurred; the summits of many of the Himalayan mountains were not reached until the 1950s, however. Of these climbs, the best known is the 1953 ascent of Mount Everest by Edmund Hillary and Tenzing Norgay. In the 1960s mountaineering became an increasingly technical sport, emphasizing the use of specialized anchoring, tethering, and grappling gear in the ascent of vertical rock or ice faces.
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Any of several shrubs or trees of the genus Sorbus, in the rose family, native to the Northern Hemisphere. They are widely cultivated as ornamentals for their white flower clusters and bright-orange fruits. Most noteworthy are the handsome American mountain ash, or dogberry (S. americana), and European mountain ash (S. aucuparia), also called rowan, or quickbeam. The European species grows to 60 ft (18 m), twice as high as the American species.
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Landform that rises well above its surroundings, generally exhibiting steep slopes, a relatively confined summit area, and considerable local relief (inequalities of elevation). Mountains are considered larger than hills, but the term has no standardized geologic meaning. Mountains are formed by the folding, faulting, or upwarping of the Earth's surface due to the movement of plates (see plate tectonics) or by the emplacement of volcanic rock onto the surface. For example, the Himalayan Mountains where India meets the Eurasian Plate were formed by a collision between plates that caused extreme compressional folding and the uplifting of large areas. The mountain ranges around the Pacific basin are attributed to the sinking of one plate beneath another. Seealso plateau.
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Typhus-like disease first seen in the Rocky Mountain region, caused by the bacterium Rickettsia rickettsii (see rickettsia) and transmitted by various ticks. In severe cases the rash bleeds more and is especially prominent on the wrists and ankles. Central nervous system involvement causes restlessness, insomnia, and delirium. Prostration may progress to coma, with death possible in a week or more. Mortality increases with age. Recovery is slow but usually complete as visual disturbances, deafness, and mental confusion pass. Prompt antibiotic treatment hastens it and reduces mortality. Prevention depends on avoiding tick bites, by wearing long, light-coloured clothing and insect repellent and inspecting for ticks. A vaccine reduces the risk of infection somewhat and of death greatly.
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Landis, 1928
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Landis, 1928
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Breed of Swiss working dog brought to Switzerland over 2,000 years ago by invading Romans. The hardy breed was widely used to pull carts and to drive cattle to and from their pastures. It has a broad chest, hanging V-shaped ears, and a long, silky, black coat. Markings include brown spots on the chest and forelegs and over the eyes, and sometimes white on the chest, nose, feet, and tail tip. The breed stands 21–28 in. (53–70 cm) high and weighs about 90 lbs (40 kg).
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