Byname:
the Rockies

Serious problems have arisen as a result of timber harvesting, grazing, oil exploration, mining, and reservoir operations in the Rockies. Logging and oil exploration have been responsible for accelerated slope erosion, both from the operations themselves and from the access roads built to reach them. Erosion has stripped away the often thin soil cover and caused serious silting of streams. Trace quantities of harmful metals have been released into streams and groundwater from mining operations, particularly from the leaching of mill tailings. Reservoir operations have disrupted fisheries by altering the temperature and flow patterns of streams and by disrupting riparian (streamside) vegetation communities. Wildlife habitat has been lost through the development of lands for agriculture and livestock grazing. Thus, the degree to which land in the Rocky Mountains remains natural generally declines as elevation decreases.

Study and exploration

The Rocky Mountains were one of the last regions in North America to be explored by Europeans, because of the inaccessibility and ruggedness of the terrain. Roman Catholic missionaries worked their way northward from Mexico into New Mexico in the 17th and 18th centuries. In 1776–77 Silvestre Vélez de Escalante and his party explored and documented their travels into what is now Utah, reaching almost to the Great Salt Lake. The Scottish explorer Alexander Mackenzie, searching for a river course to the Pacific Ocean from the Canadian prairie, crossed the Rockies (1792–93) at a latitude higher than any other expedition until the early 19th century. The Lewis and Clark Expedition in 1804–06 explored and charted a route up the Missouri River into Montana and thence across Idaho and Oregon to the Pacific. The English explorer and fur trader David Thompson explored the headwaters of the Saskatchewan and Columbia rivers in the Canadian Rockies in 1807–11, setting up the first trading posts in that region and producing the first survey of the entire length of the Columbia River.

Possibly the most remarkable of all western explorations were those of Jedediah Smith in 1822–31. Following the Missouri River into east-central Montana, Smith first worked his way southward into the Bighorn Basin and thence into southeastern Idaho, northern and southwestern Utah, and southern Nevada, around the Sierra Nevada, and back to the Great Salt Lake across the Great Basin. Also important were the expeditions of John C. Frémont in the 1840s. Frémont followed the North Platte River into Wyoming, went up the Sweetwater River to the south end of the Wind River Range (South Pass), and thence traveled southwestward into Utah. This was an important scientific survey because he charted distances, determined latitudes, longitudes, and elevations, and recorded objectively in some detail what he saw.

Four great western surveys were organized by the U.S. government following the American Civil War: the survey of the 40th parallel led by Clarence King (1867–78), the geologic survey of Nebraska and Wyoming led by Ferdinand Hayden (1867–78), the 100th-meridian survey led by George Wheeler (1872–79), and the expeditions to the Green and Colorado rivers in Wyoming, Utah, Arizona, and southern Nevada led by John Wesley Powell (1871–79). The maps and preliminary observations of these important surveys laid the groundwork for the great mass of scientific research that followed. The Rocky Mountains, with their abundant deposits of fossil fuels, uranium, and other minerals, continue to attract the attention of geologists.

Armand J. Eardley Richard A. Marston

Rocky Mountain National Park, spectacular mountainous region of north-central Colorado, U.S. It lies just west of the town of Estes Park and adjoins Arapaho National Recreation Area, which surrounds two lakes formed by the impounding of the Colorado River, to the southwest; the eastern entrance of the park lies about 70 miles (115 km) northwest of Denver. Established in 1915 and designated a UNESCO Biosphere Reserve in 1976, the national park has an area of 415 square miles (1,075 square km).

Rocky Mountain National Park includes part of the Front Range, a line of mountains trending north-south that marks the eastern edge of the Southern Rocky Mountains. Dozens of peaks exceed 12,000 feet (3,650 metres) in elevation, the highest being Longs Peak at 14,259 feet (4,346 metres). Also notable are the broad glacier-carved valleys and gorges, numerous alpine lakes, and plunging streams. Ice Age glacial deposition is evidenced by meadows and rolling moraines. The Continental Divide runs roughly northwest-southeast through the centre of the park. The source of the Colorado River is in the northwestern corner; the river flows southward along the park’s western edge and into Arapaho National Recreation Area before turning to the southwest.

Rocky Mountain National Park supports three ecosystems: montane, subalpine, and alpine tundra. Tundra makes up one-third of the park’s area. A great variety of plant life, more than 700 species, can be seen. Trees characteristic of the area include aspen, fir, pine, and spruce. The tundra in the park’s high country is an island of arctic vegetation surrounded by plants of lower latitudes. Animal life includes bighorn, deer, mountain lions, bobcats, black bears, elk, moose, and a variety of birds.

The park is accessible in summer via Trail Ridge Road, which bisects it east-west and reaches an elevation of 12,183 feet (3,713 metres); it is one of America’s most scenic highways. The Continental Divide National Scenic Trail also passes through. The park has some 350 miles (565 km) of hiking trails. Popular activities are snowshoeing and cross-country skiing in winter and hiking, fishing, rock climbing, and horseback riding in summer. Several of the visitor centres have cultural and natural history exhibits.

The Editors of Encyclopaedia BritannicaThis article was most recently revised and updated by Alicja Zelazko.