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The Rocky Mountains, often called the Rockies, are a broad mountain range in western North America. The Rocky Mountains stretch more than 4,800 kilometers (3,000 miles) from northernmost British Columbia, in Canada, to New Mexico, in the United States. The highest peak is Mount Elbert, in Colorado, which is 14,440 feet (4,401 meters) above sea level. Mount Robson in British Columbia, at 3,954 meters (12,972 feet) is the highest peak in the Canadian Rockies. The Rocky Mountain System within the United States is a United States physiographic region. Though part of the Pacific Cordillera, they are not to be confused with the Pacific Coast Ranges which are located immediately adjacent to the Pacific coast. In the United States, the more impressive rise above the Great Plains include the Front Range from northern Colorado to northern New Mexico, in Wyoming along the Wind River Range and Big Horn Mountains, and in Montana with the Crazy Mountains and along the Rocky Mountain Front which extends into extreme southwestern Alberta, Canada (known there as the Clark Range). The Wasatch Range near Salt Lake City, Utah divides the Great Basin from the mountains in the west.
Geography and geology
Image:PSP 021.jpg Mount Timpanogos, in the Wasatch Range, near Provo, Utah. The younger ranges of the Rocky Mountains uplifted during the late Cretaceous period (100 million-65 million years ago), although some portions of the southern mountains date from uplifts during the Precambrian (3,980 million-600 million years ago). The mountains' geology is a complex of igneous and metamorphic rock; younger sedimentary rock occurs along the margins of the southern Rocky Mountains, and volcanic rock from the Tertiary (65 million-1.8 million years ago) occurs in the San Juan Mountains and in other areas. Millennia of severe erosion in the Wyoming Basin transformed intermountain basins into a relatively flat terrain. The Tetons and other north-central ranges contain folded and faulted rocks of Paleozoic and Mesozoic age draped above cores of Proterozoic and Archean igneous and metamorphic rocks ranging in age from 1.2 billion (e.g., Tetons) to more than 3.3 billion years (Beartooth Mountains).[1][2][3] Periods of glaciation occurred from the Pleistocene Epoch (1.8 million-70,000 years ago) to the Holocene Epoch (fewer than 11,000 years ago). Recent episodes included the Bull Lake Glaciation that began about 150,000 years ago and the Pinedale Glaciation that probably remained at full glaciation until 15,000-20,000 years ago.[1][4] Ninety percent of Yellowstone National Park was covered by ice during the Pinedale Glaciation.[1][3]The little ice age was a period of glacial advance that lasted a few centuries from about 1550 to 1860. For example, the Agassiz and Jackson glaciers in Glacier National Park reached their most forward positions about 1860 during the little ice age.[1][5] Water in its many forms sculpted the present Rocky Mountain landscape.[1][6] Runoff and snowmelt from the peaks feed Rocky Mountain rivers and lakes with the water supply for one-quarter of the United States. The rivers that flow from the Rocky Mountains eventually drain into three of the world's Oceans: the Atlantic Ocean, the Pacific Ocean, and the Arctic Ocean.[1] These rivers include:
See also: Geology of the Rocky Mountains Human HistorySince the last great Ice Age, the Rocky Mountains were home first to Paleo-Indians and then to the Native American tribes of the Apache, Arapaho, Bannock, Blackfoot, Cheyenne, Crow, Flathead, Shoshoni, Sioux, Ute, Kutenai (Ktunaxa in Canada), Sekani, Dunne-za and others.[1][7] Paleo-Indians hunted the now-extinct mammoth and ancient bison (an animal 20% larger than modern bison) in the foothills and valleys of the mountains. Like the modern tribes that followed them, Paleo-Indians probably migrated to the plains in fall and winter for bison and to the mountains in spring and summer for fish, deer, elk, roots, and berries. In Colorado, along the crest of the Continental Divide, rock walls that Native Americans built for driving game date back 5,400-5,800 years.[1][8] A growing body of scientific evidence indicates that Native Americans had significant effects on mammal populations by hunting and on vegetation patterns through deliberate burning.[1][9] Recent human history of the Rocky Mountains is one of more rapid change.[1][10][3]The Spanish explorer Francisco Vásquez de Coronado — with a group of soldiers, missionaries, and African slaves — marched into the Rocky Mountain region from the south in 1540. The introduction of the horse, metal tools, rifles, new diseases, and different cultures profoundly changed the Native American cultures. Native American populations were extirpated from most of their historical ranges by disease, warfare, habitat loss (eradication of the bison), and continued assaults on their culture.[1] Image:Rockies USA1.jpg Colorado Rockies Sir Alexander MacKenzie (1764 - March 11, 1820) became the first European to cross the Rocky Mountains in 1793. He found the upper reaches of the Fraser River and reached what is now the Pacific coast of Canada on July 20 of that year, completing the first recorded transcontinental crossing of North America north of Mexico. He arrived at Bella Coola, British Columbia, where he first reached saltwater at South Bentinck Arm, an inlet of the Pacific Ocean. The Lewis and Clark Expedition (1804-1806) was the first scientific reconnaissance of the Rocky Mountains. Specimens were collected for contemporary botanists, zoologists, and geologists.[1][11] The expedition was said to have paved the way to (and through) the Rocky Mountains for European-Americans from the East, although Lewis and Clark met at least 11 European-American mountain men during their travels.[1] Mountain men, primarily French, Spanish, and British roamed the Rocky Mountains from 1720 to 1800 seeking mineral deposits and furs. The fur-trading Northwest Company established Rocky Mountain House as a trading post in what is now the Rocky Mountain foothills of Alberta in 1799, and their business rivals the Hudson's Bay Company established Acton House nearby. These posts served as bases for most European activity in the Canadian Rockies in the early 1800s, most notably the expeditions of David Thompson (explorer), the first European to follow the Columbia River to the Pacific Ocean. After 1802, American fur traders and explorers ushered in the first widespread white presence in the Rockies south of the 49th parallel. The more famous of these include Americans included William Henry Ashley, Jim Bridger, Kit Carson, John Colter, Thomas Fitzpatrick, Andrew Henry, and Jedediah Smith. On July 24, 1832, Benjamin Bonneville led the first wagon train across the Rocky Mountains by using Wyoming's South Pass.[1] The Mormons began to settle near the Great Salt Lake in 1847. In 1859, gold was discovered near Cripple Creek, Colorado, and the regional economy of the Rocky Mountains was changed forever. The transcontinental railroad was completed in 1869, and Yellowstone National Park was established in 1872. While settlers filled the valleys and mining towns, conservation and preservation ethics began to take hold. President Harrison established several forest reserves in the Rocky Mountains in 1891-1892. In 1905, President Theodore Roosevelt extended the Medicine Bow Forest Reserve to include the area now managed as Rocky Mountain National Park.[1].[8] Economic development began to center on mining, forestry, agriculture, and recreation, as well as on the service industries that support them.[1].[10] Tents and camps became ranches and farms, forts and train stations became towns, and some towns became cities.[1] Industry and developmentEconomic resources of the Rocky Mountains are varied and abundant. Minerals found in the Rocky Mountains include significant deposits of copper, gold, lead, molybdenum, silver, tungsten, and zinc. The Wyoming Basin and several smaller areas contain significant reserves of coal, natural gas, oil shale, and petroleum. For example, the Climax mine, located near Leadville, Colorado, was the largest producer of Molybdenum in the world. Molybdenum is used in heat-resistant steel in such things as cars and planes. The Climax mine employed over 3,000 workers. The Coeur d’Alene mine of northern Idaho produces silver, lead, and zinc. Canada's largest coal mines are in the Crowsnest Pass near Sparwood, British Columbia and Elkford, British Columbia; additional coal mines exist near Hinton, Alberta[1] and in the Northern Rockies surrounding Tumbler Ridge, British Columbia. Abandoned mines with their wakes of mine tailings and toxic wastes dot the Rocky Mountain landscape. In one major example, eighty years of zinc mining profoundly polluted the river and bank near Eagle River in north-central Colorado. High concentrations of the metal carried by spring runoff harmed algae, moss, and trout populations. An economic analysis of mining effects at this site revealed declining property values, degraded water quality, and the loss of recreational opportunities. The analysis also revealed that cleanup of the river could yield $2.3 million in additional revenue from recreation. In 1983, the former owner of the zinc mine was sued by the Colorado Attorney General for the $4.8 million cleanup costs; 5 years later, ecological recovery was considerable.[1][12] Agriculture and forestry are major industries. Agriculture includes dryland and irrigated farming and livestock grazing. Livestock are frequently moved between high-elevation summer pastures and low-elevation winter pastures,[1] a practice known as transhumance. Human population is not very dense in the Rocky Mountains, with an average of four people per square kilometer (10 per square mile) and few cities with over 50,000 people. However, the human population grew rapidly in the Rocky Mountain states between 1950 and 1990. The 40-year statewide increases in population range from 35% in Montana to about 150% in Utah and Colorado. The populations of several mountain towns and communities have doubled in the last 40 years. Jackson Hole, Wyoming, increased 260%, from 1,244 to 4,472 residents, in 40 years.[1] TourismImage:Reservoir in the Rocky Mountains.jpg Snowmelt runoff fills a reservoir in the Rocky Mountains near Dillon, Colorado. Image:Longs Peak.jpg Snowpack accumulation at 14,255 ft. on Longs Peak in Rocky Mountain National Park (photo courtesy of USDA). Every year the scenic areas and recreational opportunities of the Rocky Mountains draw millions of tourists.[1] The main language of the Rocky Mountains is English. But there are also linguistic pockets of Spanish and Native American languages. People from all over the world visit the sites to hike, camp, or engage in mountain sports.[1] In the summer, main tourist attractions are: In the United States:
In Canada, the mountain range contains these national parks:
Glacier National Park in Montana and Waterton Lakes National Park in Alberta border each other and collectively are known as Waterton-Glacier International Peace Park. (See also International Peace Park.) In the winter, skiing is the main attraction. The major ski resorts are:
The adjacent Columbia Mountains in British Columbia and Idaho contain major resorts such as Schweitzer, Panorama and Kicking Horse, as well as Mount Revelstoke National Park. See also: List of U.S. Rocky Mountain ski resorts, List of Alberta ski resorts, List of B.C. ski resorts ClimateImage:Rocky Mountains.aerial view.no snow.jpg Aerial view of the Colorado Rocky Mountains in summer Image:Aerial Section of Snow Covered Rocky Mountain at Colorado.jpg Aerial view of the Colorado Rocky Mountains in winter The Rocky Mountains have a highland climate. The average annual temperature in the valley bottoms of the Colorado Rockies near the latitude of Boulder is 43 °F (6 °C). July is the hottest month there with an average temperature of 82 °F (28 °C). In January, the average monthly temperature is 7 °F (−14 °C), making it the region's coldest month. The average precipitation per year there is approximately 14 inches (360 mm). The summers in this area of the Rockies are warm and dry, because the western fronts impede the advancing of water-carrying storm systems. The average temperature in summer is 59 °F (15 °C) and the average precipitation is 5.9 inches (150 mm). Winter is usually wet and very cold, with an average temperature of 28 °F (−2 °C) and average snowfall of 11.4 inches (29.0 cm). In spring, the average temperature is 40 °F (4 °C) and the average precipitation is 4.2 inches (107 mm). And in the fall, the average precipitation is 2.6 inches (66 mm) and the average temperature is 44 °F (7 °C). References
See also
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