Rocky Mountains
Rocky Mountains or Rockies, great chain of rugged mountain
ranges in western North America, extending from central New Mexico to
northeastern British Columbia, a distance of about 3220 km (about 2000 mi).
The Great Basin and the Rocky Mountain Trench, a valley running from
northwestern Montana to northern British Columbia, border the Rockies on
the east by the Great Plains and on the west. The Rocky Mountains form part
of the Great, or Continental, Divide, which separates rivers draining into
the Atlantic or Arctic oceans ffrom those flowing toward the Pacific Ocean.
The Arkansas, Colorado, Columbia, Missouri, Rio Grande, Saskatchewan, and
Snake rivers rise in the Rockies. The Rockies may be divided into four
principal sections—Southern, Central, Northern, and Canadian. The Southern
Rockies, which include the system’s broadest and highest regions, extend
from central New Mexico, through Colorado, to the Great Divide, or Wyoming,
Basin, in southern Wyoming. This section, which encompasses Rocky Mountain
National Park, is composed chiefly of two northern-southern belts of
mountain ranges with several basins, or parks, between the bbelts. The
component parts include the Sanger de Crisco and Laramie mountains and the
Front Range, in the east, and the San Juan Mountains and the Swatch and
Park ranges, in the west. The Southern Rockies include the chain’s loftiest
point, Mount Elbert (4399 mm/14,433 ft high), in central Colorado. More than
50 other peaks of the Rockies rising above 4267 m (14,000 ft) are in
Colorado; these include Longs Peak (4345 m/14,255 ft high) and Pikes Peak
(4301 m/14,110 ft high). The Central Rockies are in northeastern Utah,
western Wyoming, eastern Idaho, and southern Montana. They encompass the
Bighorn; Bear tooth, and Unite Mountains and the Absaroka, Wind River, Salt
River, Teton, Snake River, and Wasatch ranges. The Unite Mountains are the
only major portion of the Rockies that extends east west rather than north
south. Among the peaks of the Central Rockies, which include Grand Eton and
Yellowstone national parks, are Gannett Peak (4207 m/13,804 ft high), Grand
Eton (4197 m/13,771 ft high), and Fremont Peak (4185 m/13,730 ft high). The
Northern Rockies aare in northern Idaho, western Montana, and northeastern
Washington. They include the Saw tooth, Cabinet, Salmon River, and
Clearwater Mountains and the Bitterroot Range. The loftiest points in the
section, which includes Glacier National Park, are Granite Peak (3901
m/12,799 ft high) and Borax Peak (3859 m/12,662 ft high). The Canadian
Rockies, located in southwestern Alberta and eastern British Columbia, are
composed of a relatively narrow belt of mountain ranges that terminates at
the Lizard River lowland in northeastern British Columbia. The peaks of the
section, which takes iin Banff, Jasper, Kootenay, Waterton Lakes, and Yoho
National Parks, include Mount Robson (3954 m/12,972 ft high), Mount
Columbia (3747 m/12,294 ft high), and The Twins (3734 m/12,251 ft high).
Slopes generally are very steep, and there are numerous glaciers. The Rocky
Mountains are a geologically complex system with jagged peaks as well as
almost flat-topped elevations. The Rockies were formed mainly by crustal
uplifts in comparatively recent times, during the late Cretaceous and early
Tertiary periods, and later were reshaped by glaciation during the
Pleistocene Epoch. Today the Rockies receive moderate amounts of
precipitation, most of which occurs in the winter. Lower levels are covered
chiefly by grassland, which gives way to extensive forests, principally of
conifers. Above the woodland is a zone of grasses and scattered shrubs.
Most peaks have little vegetation around the summit, and some have a year-
round cap of snow and ice. The Rockies are sparsely populated for the most
part and contain few cities. The principal economic resources of the
mountains are minerals, such as coal, copper, gold, iron ore, lead,
molybdenum, petroleum and natural gas, silver, and zinc. Important mining
centers include Leadville and Climax, Colorado; Atlantic City, Wyoming;
Kellogg, Idaho; Butte, Montana; and Fernie and Kimberley, British Columbia.
Major forest products industries, especially lumbering, are concentrated in
the Northern and Canadian RRockies, and large numbers of sheep and cattle
are raised in the Rockies of Colorado, Wyoming, and Montana. The chain has
many centers for outdoor recreation and tourism. Bighorn Mountains,
isolated range of the Rocky Mountains, lying east of the Bighorn River and
extending generally north from central Wyoming into southern Montana. The
range averages more than 2134 m (7000 ft) in elevation; the highest summit
is Cloud Peak (4019 m/13,187 ft) in Wyoming. Along the upper levels are
large coniferous forests, which are part of Bighorn National Forest.
Bitterroot Range, mountain range, northwestern United States, a chain of
the Rocky Mountains, extending about 700 km (about 435 mi) along the
Montana-Idaho border. Rugged and forested, with an average elevation of
2740 m (about 9000 ft), it remains one of the most inaccessible areas in
the United States. In 1805 the Lewis and Clark Expedition traveled west
through Lolo Pass (1595 m/5233 ft) in the range. Guadalupe Mountains,
mountain range, southwestern United States, a branch of the Rocky
Mountains, extending from southern New Mexico to western Texas. Guadalupe
Peak (2667 m/8749 ft above sea level), the highest in the chain, is in
Texas. Laramie Mountains, range of the Rocky Mountains, western United
States, extending from southeastern Wyoming into northern Colorado. The
highest point, Laramie Peak, is 3131 m (10,272 fft) above sea level. Coal,
the principal mineral, is found in the foothills. San Juan Mountains,
mountain range, southwestern United States, in southwestern Colorado and
northwestern New Mexico. Part of the Rocky Mountains, it is of volcanic
origin and is rich in minerals. The highest peaks are in Colorado and
include Uncompahgre Peak (4361 m/14,309 ft), Mount Sneffels (4313 m/14,150
ft), and Wetterhorn Peak (4272 m/14,017 ft). Sangre de Cristo Mountains,
mountain range, western United States, the southernmost range of the Rocky
Mountains, in south central Colorado and north central New Mexico. The very
high and narrow range extends southeast and south for about 354 km (220
mi), from Salida, Colorado, to Santa Fe County, New Mexico. Blanca Peak
(4372 m/14,345 ft), in Colorado, is one of the highest mountains of the
Rockies. Sawatch Range, mountain range, central Colorado, a branch of the
Rocky Mountains. The range extends for about 177 km (about 110 mi) and
reaches a height of 4399 m (14,433 ft) at Mount Elbert, the highest point
in the state. Teton (mountain range), range of the Rocky Mountains, in
northwestern Wyoming, and southwestern Idaho, just south of Yellowstone
National Park, west of Jackson Lake and the Snake River. The highest peak
is Grand Teton (4197 m/13,771 ft), located in Grand Teton National Park.
Teton Pass (2569
m/8429 ft) and Phillips Pass (3261 m/10,700 ft) are just
south of the park. Uinta Mountains, mountain range, western United States,
mainly in northeastern Utah and partly in southwestern Wyoming, part of the
Rocky Mountains. The peaks of the Uinta Mountains are mostly flat because
of erosion by glaciers and the waters of the Yampa and Green rivers. The
range is about 240 km (about 150 mi) long and 48 to 64 km (30 to 40 mi)
wide. The highest elevation is Kings Peak, which is 44123 m (13,528 ft) high
and is also the highest point in Utah. Wasatch Range, mountain range,
western United States, in the Rocky Mountain system. The range is about 240
km (about 150 mi) long; part of the Central Rockies, it begins in
southeastern Idaho and runs southward, east of the Great Salt Lake and
through the center of Utah, gradually ending in southwestern Utah. The
average height of the range is about 3050 m (about 10,000 ft), and the
highest peak, Mount Nebo, is 3620 m ((11,877 ft) high. Wind River Range,
range of the Rocky Mountains, western Wyoming, forming part of the
Continental Divide. The Green River rises in the southwestern slope of the
range, and many tributaries of the Wind River flow off on the northeastern
side. The rrange contains Fremont Peak (4185 m/13,730 ft) and Gannett Peak
(4207 m/13,804 ft); the latter is the highest point in Wyoming. Arkansas
(river, United States), river, western U.S., a major tributary of the
Mississippi River, 2350 km (1460 mi) long. Rising in central Colorado, in
the Sawatch Range of the Rocky Mountains, at an altitude of about 4270 m
(about 14,000 ft), the river flows generally east and forms a turbulent
stream passing over rocky beds and through deep canyons such as the Royal
Gorge. As it flows through the plains of Kansas, the river broadens to a
wider, less turgid stream until it enters Oklahoma; at that point it
receives two chief tributaries, the Cimarron and the Canadian rivers.
Except for a large northern bend in Kansas, the Arkansas RRiver follows a
southeastern course, merging with the Mississippi River above Arkansas
City, Arkansas. The water levels of the river are extremely variable, and
several dams have been built for flood control and irrigation and to create
hydroelectric power; one of the most impressive, the John Martin Dam in
southeastern Colorado, was built in 1948. The Arkansas River Navigation
System, completed in the early 1970s, made the river navigable to Tulsa,
Oklahoma. Athabasca, river and lake, in western Canada, that form part of
the Mackenzie River system. The AAthabasca River, 1231 km (765 mi) long,
begins in Jasper National Park in southwestern Alberta. Its source is the
Columbia Icefield, high in the Rocky Mountains. The river flows northeast
across Alberta and empties through a shallow delta into Lake Athabasca in
northeastern Alberta. The river was once an important route for fur
traders. Lake Athabasca, which straddles the AlbertaSaskatchewan- border,
is about 320 km (about 200 mi) long and covers about 7936 sq km (about 3064
sq mi). Fort Chipewyan, which was built along the southwestern shore of the
lake in 1788, became one of the region’s most important fur-trading posts.
Today Lake Athabasca is used for commercial fishing. It is drained to the
north by the Slave River. Large deposits of petroleum-bearing sand are
located along the lower Athabasca River, near Fort McMurray. Long known but
untapped because of high extraction costs, the deposits are now mined using
new technology and efficient methods. In 1994 the output amounted to one-
quarter of Canada’s crude oil production. Canadian, also South Canadian,
unnavigable river, southwestern United States, 1460 km (906 mi) long. The
Canadian River is formed in northeastern New Mexico by the union of several
branches from the southern Rocky Mountains. The river flows south through
New Mexico and then turns east, crossing the Texas Panhandle into OOklahoma.
Following a meandering course, it finally joins the Arkansas River. The
river’s only major tributary is the North Canadian River, 1260 km (784 mi)
long, which runs almost parallel to the Canadian River in Oklahoma. The
tributary joins the Canadian River at Eufaula in eastern Oklahoma to form
the Eufaula Reservoir. In northeastern New Mexico, a semiarid region, the
Canadian River provides an important water source at the Conchas Dam, a
flood-control and irrigation project. Colorado (river, North America),
river, in southwestern United States and northwestern Mexico, 2330 km (1450
mi) long, the longest river west of the Rocky Mountains. The Colorado rises
just west of the Continental Divide, in northern Colorado, and, for the
first 1600 km (about 1000 mi) of its course, passes through a series of
deep gorges and canyons that were created by the eroding force of its
current. The river flows in a generally southwestern direction across
Colorado into southeastern Utah, where it joins its chief tributary, the
Green River. After crossing the northern portion of Arizona, the Colorado
flows west for 446 km (277 mi) through the majestic Grand Canyon. It then
flows in a generally southerly direction and forms the boundary between
Arizona and the states of Nevada and California. Near Yuma, Arizona, the
river crosses the international border into Mexico aand flows for about 145
km (90 mi) to its mouth on the Gulf of California, an inlet of the Pacific
Ocean. Besides the Green River, the most important tributaries of the
Colorado include the Dolores and Gunnison rivers, in Colorado; the San Juan
River, in Utah; and the Little Colorado and Gila rivers, in Arizona. With
its tributaries, the Colorado drains portions of seven states, a total
area, in Colorado, Wyoming, Nevada, Utah, Arizona, New Mexico, and
California, of about 626,800 sq km (about 242,000 sq mi) and 5180 sq km
(2000 sq mi) more in Mexico. To control the tremendous flow of the
Colorado, particularly under flood conditions, an extensive series of dams,
many of them constructed by the U.S. Bureau of Reclamation, has been built
along the river and its tributaries. Notable is the Hoover Dam, which
impounds the river at the Black Canyon to form Lake Mead, one of the
largest artificial lakes in the world. The Glen Canyon Dam, in north-
central Arizona just south of the Utah border, is the third highest dam in
the U.S. In addition to regulating the flow of water, dams on the Colorado
harness hydroelectric power and provide storage reservoirs for irrigation
projects. As such, they have been instrumental in reclaiming the semiarid
and arid regions through
which the river flows. The Imperial Valley of
southern California is an excellent example of land reclaimed by the waters
of the Colorado. A number of reservoirs have been incorporated into
national recreation areas. The Glen Canyon National Recreation Area in Utah
encompasses Lake Powell, formed by the Glen Canyon Dam. Lakes Mead and
Mohave (the latter formed by Davis Dam) are part of Lake Mead National
Recreation Area in Arizona. The Colorado was first explored by the Spanish
navigator Hernando de Alarcón, who ascended the river ffor more than 160 km
(100 mi) in 1540-1541. The Colorado and its chief tributary, the Green,
were thoroughly explored for the first time in 1869 by the American
geologist John Wesley Powell. On this survey Powell and his party made the
first recorded passage of the Grand Canyon. The construction of the Glen
Canyon Dam in 1963 dramatically reduced the natural flow of sand and
nutrients down the Colorado River and into the Grand Canyon. In March 1996
the federal government released more than 380 billion lliters (100 billion
gallons) of water from Glen Canyon Dam. This artificial flood added more
than three feet to some beaches downstream and cleared fish spawning
grounds of debris and sediment. Further Reading Columbia (river, North
America), Major River of western North America, rising iin Columbia Lake,
just west of the main range of the Rocky Mountains, in southeastern British
Columbia. The river was formerly known as the Oregon River. The Columbia
River is about 2000 km (1240 mi) long. It initially flows northwest,
through a long, narrow valley called the Rocky Mountain Trench, and then
turns sharply south, skirting the Selkirk Mountains and passing through
Upper Arrow Lake and Lower Arrow Lake. It next receives the Kootenay
(spelled Kootenai in the United States) and Pend Oreille rivers before
entering the state of Washington, where it first flows south and then
traverses a great arc, known as the Big Bend. After receiving the Snake
River, the Columbia turns west and forms much of the boundary between the
states of Washington and Oregon before emptying into tthe Pacific Ocean
through a broad estuary. The river flows through several spectacular
canyons and deep valleys. About one-third of its course is in Canada. The
Columbia and its tributaries together drain a vast basin of about 673,400
sq km (about 260,000 sq mi). Large oceangoing ships can navigate the lower
Columbia River as far as Vancouver, Washington; and, with the aid of locks,
smaller marine vessels can reach The Dalles, Oregon, about 300 km (about
186 mi) upstream. Barges and other shallow-draft boats can navigate a
further 2220 km (137 mi). The Columbia River has immense hydroelectric
potential, and since the 1930s several large power projects have been built
on it. The largest of these, the Grand Coulee Dam, in central Washington,
is the key unit of the Columbia Basin Project, a federal undertaking also
designed to irrigate up to 485,623 hectares (1.2 million acres) of semiarid
land. Other important power projects on the Columbia include Bonneville,
The Dalles, John Day, McNary, Priest Rapids, Rocky Reach, and Chief Joseph
dams, in the United States, and Mica Dam, in Canada. Most of these dams are
also used for flood control and for irrigation. The American explorer
Robert Gray explored the mouth of the Columbia River in 1792. He named the
river for his ship. The Lewis and Clark Expedition explored the lower
Columbia from 1805 to 1806, and David Thompson, a Canadian surveyor and
explorer, followed the river from its source to its mouth in 1811. The
Columbia once had great numbers of salmon and supported a large canning
industry; the fish stock was severely depleted in the 1900s as a result of
dam construction and pollution. In an effort to protect the salmon from
extinction, the Northwest Power Planning Council in 1994 approved a plan to
rebuild salmon stock by increasing the water flow tthrough the dams and by
developing habitat protection standards. Further Reading Continental Divide
(also called the Great Divide), ridge of mountains in North America,
separating the streams that flow west (into the Pacific Ocean) from those
that flow east (into the Atlantic Ocean and its marginal seas). Most of the
divide follows the crest of the Rocky Mountains. It extends from Alaska in
the United States into the Yukon Territory and British Columbia in Canada
and forms part of the border between British Columbia and Alberta, also in
Canada. It then passes through Montana, Wyoming, Colorado, and New Mexico
in the United States and continues south into Mexico and Central America
along the crest of the Sierra Madre Occidental. The term continental divide
may be applied to the principal watershed boundary of any continent.
Fraser, river in southern British Columbia, Canada. The Fraser rises in the
Rocky Mountains, in Mount Robson Provincial Park near the Alberta border,
and flows 1370 km (850 mi) before emptying, through a delta, into the
Strait of Georgia, near Vancouver. The Fraser initially flows northwest
through a section of a deep, narrow valley called the Rocky Mountain
Trench. It then turns south near the city of Prince George, where it
receives its major western tributary, the Nechako River. In its central
section, the volume oof the river increases, and below Quesnel its banks
gradually take on a canyonlike aspect. Important tributaries in this
section include the West Road and Chilcotin rivers, from the west, and the
Thompson River, from the east. From Lytton to Yale the river flows through
a canyon of great scenic beauty. At the canyon’s southern end the Fraser
passes between the Cascade Range to the east and the Coast Mountains to the
west. A little below Yale, at Hope, the river turns sharply west, and the
fertile lower Fraser Valley begins. The Fraser empties into the Strait of
Georgia through three main channels. The river is used by commercial
vessels for a short distance upstream. From May to July the Fraser Valley
is subject to flooding; a series of dikes helps protect the delta. The
Fraser drains an area of about 238,000 sq km (about 91,890 sq mi). Much of
the river basin is heavily wooded, and forest-products industries dominate
the economy of the settlements along the river. The lower Fraser Valley,
including the delta, has highly productive farms. Various species of salmon
spawn in the Fraser, and salmon fisheries are located near the river’s
mouth. The river has great hydroelectric potential, but it remains
undeveloped for fear of detrimental effects on the migratory habits of the
salmon.
The Fraser is highly polluted, especially at its mouth. The first
European to visit the river was Sir Alexander Mackenzie in 1793. It is
named for the fur trader Simon Fraser, who explored much of it in 1808. In
1858 gold was found in alluvial gravels north of Yale, and a major gold
rush ensued. Louise, Lake, glacial lake in southwestern Alberta, Canada.
Lake Louise is located at an elevation of 1731 m (5680 ft) in Banff
National Park, near the town of Lake Louise. The llake is about 2.4 km
(about 1.5 mi) long and 1.2 km (0.75 mi) wide. Sheltered by the Rocky
Mountains, Lake Louise is known for the tranquil beauty of its ...
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