What Repairs Were Done At 1601 Burton Street, Rocky Mount Nc

Major mountain range in western North America

Rocky Mountains
The Rockies (en), Les montagnes Rocheuses (fr), Montañas Rocosas , Rocallosas (es)
Moraine Lake and the Valley of the Ten Peaks, Banff National Park, Alberta, Canada
Highest point
Height	Mount Elbert, Colorado, Us
Meridian	14,440 ft (iv,401 m)
Coordinates	39°07′04″Due north 106°26′43″W  /  39.11778°N 106.44528°Due west  / 39.11778; -106.44528
Dimensions
Length	4,800 km (3,000 mi)(straight-line distance)
Geography
Countries	Canada and United States
States/Provinces	British Columbia, Alberta, Washington, Idaho, Montana, Wyoming, Utah, Colorado and New Mexico
Range coordinates	43°44′28″N 110°48′09″W  /  43.741208°N 110.802414°Westward  / 43.741208; -110.802414 Coordinates: 43°44′28″N 110°48′09″W  /  43.741208°N 110.802414°West  / 43.741208; -110.802414
Parent range	North American Cordillera
Geology
Age of rock	Precambrian and Cretaceous
Type of rock	Igneous, sedimentary and metamorphic

The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mount organisation in N America. The Rocky Mountains stretch 3,000 mi (iv,800 km)^[i] in straight-line distance from the northernmost part of western Canada, to New Mexico in the southwestern United States. Depending on differing definitions between Canada and the United States, its northern terminus is located either in northern British Columbia'southward Concluding Range due south of the Liard River and east of the Trench, or in the northeastern foothills of the Brooks Range/British Mountains that face the Beaufort Sea coasts between the Canning River and the Firth River beyond the Alaska-Yukon edge.^[2] Its southernmost point is near the Albuquerque area adjacent to the Rio Grande Basin and north of the Sandia–Manzano Mountain Range. Being the easternmost portion of the North American Cordillera, the Rockies are distinct from the tectonically younger Cascade Range and Sierra Nevada, which both prevarication farther to its due west.

The Rocky Mountains formed fourscore 1000000 to 55 one thousand thousand years ago during the Laramide orogeny, in which a number of plates began sliding underneath the North American plate. The angle of subduction was shallow, resulting in a wide chugalug of mountains running downward western North America. Since then, further tectonic action and erosion by glaciers take sculpted the Rockies into dramatic peaks and valleys. At the end of the last ice historic period, humans began inhabiting the mount range. Afterward explorations of the range by Europeans, such as Sir Alexander Mackenzie, and Anglo-Americans, such as the Lewis and Clark expedition, natural resources such as minerals and fur drove the initial economic exploitation of the mountains, although the range itself never experienced a dense population.

Of the 100 highest major peaks of the Rocky Mountains, 78 (including the xxx highest) are located in Colorado, 10 in Wyoming, six in New United mexican states, three in Montana, and one each in Utah, British Columbia, and Idaho. Of the l about prominent summits of the Rocky Mountains, 12 are located in British Columbia,^[a] 12 in Montana, ten in Alberta,^[a] viii in Colorado, four in Wyoming, three in Utah, three in Idaho, and one in New Mexico. Public parks and forest lands protect much of the mountain range, and they are popular tourist destinations, especially for hiking, camping, mountaineering, fishing, hunting, mount biking, snowmobiling, skiing, and snowboarding.

Etymology [edit]

The name of the mountains is a translation of an Amerindian proper name that is closely related to Algonquian; the Cree name as-sin-wati is given equally, "When seen from across the prairies, they looked similar a rocky mass". The starting time mention of their present name past a European was in the journal of Jacques Legardeur de Saint-Pierre in 1752, where they were called " Montagnes de Roche ".^{[3] [iv]}

Geography [edit]

The Rocky Mountains are the easternmost portion of the expansive North American Cordillera. They are often defined every bit stretching from the Liard River in British Columbia^{[v] : xiii} due south to the headwaters of the Pecos River, a tributary of the Rio Grande, in New Mexico. The Rockies vary in width from 110 to 480 kilometres (70 to 300 mi). The Rocky Mountains comprise the highest peaks in fundamental N America. The range's highest elevation is Mountain Elbert located in Colorado at 4,401 metres (14,440 ft) to a higher place body of water level. Mountain Robson in British Columbia, at 3,954 metres (12,972 ft), is the highest peak in the Canadian Rockies.

The eastern edge of the Rockies rises dramatically above the Interior Plains of central North America, including the Sangre de Cristo Mountains of New Mexico and Colorado, the Front Range of Colorado, the Wind River Range and Large Horn Mountains of Wyoming, the Absaroka-Beartooth ranges and Rocky Mount Forepart of Montana and the Clark Range of Alberta.^{[ commendation needed ]}

Central ranges of the Rockies include the La Sal Range forth the Utah-Colorado border, the Uinta Range of Utah and Wyoming, and the Teton Range of Wyoming and Idaho.

The western border of the Rockies includes ranges such equally the Wasatch virtually Salt Lake Metropolis, the San Juan Mountains of New Mexico and Colorado, the Bitterroots along the Idaho-Montana border, and the Sawtooths in central Idaho. The Cracking Basin and Columbia River Plateau divide these subranges from distinct ranges further to the west. In Canada, the western edge of the Rockies is formed past the huge Rocky Mountain Trench, which runs the length of British Columbia from its beginning equally the Kechika Valley on the southward depository financial institution of the Liard River, to the middle Lake Koocanusa valley in northwestern Montana.^[6]

The Canadian Rockies are divers by Canadian geographers as everything south of the Liard River and east of the Rocky Mountain Trench, and do not extend into Yukon, Northwest Territories or primal British Columbia. They are divided into three main groups: the Muskwa Ranges, Hart Ranges (collectively called the Northern Rockies) and Continental Ranges. Other more northerly mountain ranges of the eastern Canadian Cordillera keep beyond the Liard River valley, including the Selwyn, Mackenzie and Richardson Mountains in Yukon as well every bit the British Mountains/Brooks Range in Alaska, but those are not officially recognized as part of the Rockies by the Geological Survey of Canada, although the Geological Society of America definition does consider them parts of the Rocky Mountains system equally the "Arctic Rockies".^[2]

The Continental Dissever of the Americas is located in the Rocky Mountains and designates the line at which waters flow either to the Atlantic or Pacific Oceans. Triple Divide Top (2,440 m or 8,020 ft) in Glacier National Park is and so named because water falling on the mountain reaches non merely the Atlantic and Pacific but Hudson Bay as well. Farther north in Alberta, the Athabasca and other rivers feed the basin of the Mackenzie River, which has its outlet on the Beaufort Body of water of the Arctic Ocean.

Human population is not very dense in the Rocky Mountains, with an average of four people per square kilometer and few cities with over fifty,000 people. Notwithstanding, the human population grew rapidly in the Rocky Mountain states between 1950 and 1990. The forty-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 xl years 1972–2012. Jackson, Wyoming, increased 260%, from one,244 to 4,472 residents, in those forty years.^[7]

The Front Range of the Rocky Mountains about Denver, Colorado

Geology [edit]

The rocks in the Rocky Mountains were formed before the mountains were raised by tectonic forces. The oldest stone is Precambrian metamorphic rock that forms the core of the N American continent. There is too Precambrian sedimentary argillite, dating dorsum to 1.7 billion years ago. During the Paleozoic, western North America lay underneath a shallow sea, which deposited many kilometers of limestone and dolomite.^{[5] : 76}

In the southern Rocky Mountains, well-nigh present-twenty-four hours Colorado, these ancestral rocks were disturbed by mountain edifice approximately 300 Ma, during the Pennsylvanian. This mountain-building produced the Ancestral Rocky Mountains. They consisted largely of Precambrian metamorphic stone forced upwards through layers of the limestone laid down in the shallow bounding main.^[8] The mountains eroded throughout the late Paleozoic and early Mesozoic, leaving extensive deposits of sedimentary rock.

Terranes began colliding with the western edge of North America in the Mississippian (approximately 350 million years agone), causing the Antler orogeny.^[9] For 270 million years, the focus of the furnishings of plate collisions were nigh the edge of the North American plate purlieus, far to the west of the Rocky Mount region.^[nine] Information technology was not until eighty Ma these effects began reaching the Rockies.^[10]

The current Rocky Mountains arose in the Laramide orogeny from betwixt fourscore and 55 Ma.^[10] For the Canadian Rockies, the mountain building is coordinating to pushing a rug on a hardwood flooring:^{[11] : 78} the rug bunches up and forms wrinkles (mountains). In Canada, the terranes and subduction are the foot pushing the carpeting, the ancestral rocks are the rug, and the Canadian Shield in the center of the continent is the hardwood flooring.^{[eleven] : 78}

Further south, an unusual subduction may take acquired the growth of the Rocky Mountains in the United States, where the Farallon plate dove at a shallow angle below the North American plate. This depression angle moved the focus of melting and mountain building much farther inland than the normal 300 to 500 kilometres (200 to 300 mi). Scientists hypothesize that the shallow angle of the subducting plate increased the friction and other interactions with the thick continental mass higher up it. Tremendous thrusts piled sheets of crust on top of each other, building the broad, high Rocky Mountain range.^[12]

The current southern Rockies were forced upwards through the layers of Pennsylvanian and Permian sedimentary remnants of the Ancestral Rocky Mountains.^[13] Such sedimentary remnants were often tilted at steep angles along the flanks of the modern range; they are at present visible in many places throughout the Rockies, and are shown along the Dakota Hogback, an early Cretaceous sandstone formation running along the eastern flank of the modern Rockies.

Simply later the Laramide orogeny, the Rockies were similar Tibet: a high plateau, probably 6,000 metres (xx,000 ft) above sea level. In the terminal 60 1000000 years, erosion stripped away the high rocks, revealing the ancestral rocks beneath, and forming the current mural of the Rockies.^{[11] : 80–81}

Periods of glaciation occurred from the Pleistocene Epoch (1.8 million – 70,000 years agone) to the Holocene Epoch (fewer than xi,000 years agone). These water ice ages left their mark on the Rockies, forming extensive glacial landforms, such as U-shaped valleys and cirques. Recent glacial episodes included the Bull Lake Glaciation, which began about 150,000 years ago, and the Pinedale Glaciation, which peradventure remained at full glaciation until 15,000–xx,000 years agone.^[fourteen]

All of these geological processes exposed a complex prepare of rocks at the surface. For example, volcanic rock from the Paleogene and Neogene periods (66 million – two.six 1000000 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 due north-fundamental 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 ane.two billion (e.grand., Tetons) to more than three.3 billion years (Beartooth Mountains).^[7]

Environmental and climate [edit]

There are a wide range of environmental factors in the Rocky Mountains. The Rockies range in latitude betwixt the Liard River in British Columbia (at 59° Northward) and the Rio Grande in New Mexico (at 35° N). Prairie occurs at or below 550 metres (1,800 ft), while the highest top in the range is Mount Elbert at 4,400 metres (fourteen,440 ft). Atmospheric precipitation ranges from 250 millimetres (10 in) per twelvemonth in the southern valleys^[15] to 1,500 millimetres (60 in) per year locally in the northern peaks.^[16] Average Jan temperatures can range from −7 °C (20 °F) in Prince George, British Columbia, to 6 °C (43 °F) in Trinidad, Colorado.^[17] Therefore, there is not a single monolithic ecosystem for the entire Rocky Mountain Range.

Instead, ecologists carve up the Rocky Mountain into a number of biotic zones. Each zone is defined past whether it can back up copse and the presence of 1 or more indicator species. 2 zones that do non support trees are the Plains and the Tall tundra. The Swell Plains lie to the east of the Rockies and is characterized past prairie grasses (below roughly 550 metres (1,800 ft)). Alpine tundra occurs in regions above the treeline for the Rocky Mountains, which varies from 3,700 metres (12,000 ft) in New United mexican states to 760 metres (2,500 ft) at the northern end of the Rocky Mountains (near the Yukon).^[17]

Bighorn sheep (such equally this lamb in Alberta) take declined dramatically since European-American settlement of the mountains

The USGS defines ten forested zones in the Rocky Mountains. Zones in more than southern, warmer, or drier areas are divers by the presence of pinyon pines/junipers, ponderosa pines, or oaks mixed with pines. In more northern, colder, or wetter areas, zones are defined by Douglas firs, Cascadian species (such equally western hemlock), lodgepole pines/quaking aspens, or firs mixed with spruce. Near treeline, zones can consist of white pines (such as whitebark pine or bristlecone pine); or a mixture of white pine, fir, and spruce that appear as shrub-like krummholz. Finally, rivers and canyons can create a unique wood zone in more barren parts of the mount range.^[7]

The Rocky Mountains are an important habitat for a keen deal of well-known wildlife, such as wolves, elk, moose, mule and white-tailed deer, pronghorn, mount goats, bighorn sheep, badgers, black bears, grizzly bears, coyotes, lynxes, cougars, and wolverines.^{[vii] [eighteen]} For example, North America'due south largest herds of moose are in the Alberta–British Columbia foothills forests.

The status of most species in the Rocky Mountains is unknown, due to incomplete information. European-American settlement of the mountains has adversely impacted native species. Examples of some species that have declined include western toads, greenback cutthroat trout, white sturgeon, white-tailed ptarmigan, trumpeter swan, and bighorn sheep. In the United States portion of the mount range, noon predators such as grizzly bears and wolf packs had been extirpated from their original ranges, simply have partially recovered due to conservation measures and reintroduction. Other recovering species include the bald hawkeye and the peregrine falcon.^[7]

History [edit]

Ethnic people [edit]

Since the final great ice age, the Rocky Mountains were home outset to ethnic peoples including the Apache, Arapaho, Bannock, Blackfoot, Cheyenne, Coeur d'Alene, Kalispel, Crow Nation, Flathead, Shoshone, Sioux, Ute, Kutenai (Ktunaxa in Canada), Sekani, Dunne-za, and others. Paleo-Indians hunted the now-extinct mammoth and aboriginal bison (an animal 20% larger than mod bison) in the foothills and valleys of the mountains. Similar the modern tribes that followed them, Paleo-Indians probably migrated to the plains in autumn and winter for bison and to the mountains in spring and summer for fish, deer, elk, roots, and berries. In Colorado, along with the crest of the Continental Split up, stone walls that Native Americans built for driving game engagement back 5,400–5,800 years. A growing body of scientific evidence indicates that indigenous people had significant effects on mammal populations past hunting and on vegetation patterns through deliberate burning.^[7]

European exploration [edit]

Recent human history of the Rocky Mountains is 1 of more rapid alter. The Spanish explorer Francisco Vázquez de Coronado—with a grouping of soldiers, missionaries, and African slaves—marched into the Rocky Mountain region from the south in 1540.^[19] In 1610, the Spanish founded the metropolis of Santa Fe, the oldest continuous seat of regime in the United States, at the pes of the Rockies in present-day New Mexico. The introduction of the horse, metallic tools, rifles, new diseases, and different cultures profoundly changed the Native American cultures. Native American populations were extirpated from well-nigh of their historical ranges by affliction, warfare, habitat loss (eradication of the bison), and continued assaults on their culture.^[7]

In 1739, French fur traders Pierre and Paul Mallet, while journeying through the Great Plains, discovered a range of mountains at the headwaters of the Platte River, which local American Indian tribes called the "Rockies", condign the kickoff Europeans to report on this uncharted mountain range.^[20]

Sir Alexander MacKenzie in 1800

Sir Alexander MacKenzie (1764 – March 11, 1820) became the first European to cross the Rocky Mountains in 1793.^[21] He establish the upper reaches of the Fraser River and reached the Pacific coast of what is now Canada on July 20 of that twelvemonth, completing the start recorded transcontinental crossing of N America northward of United mexican states.^[22] He arrived at Bella Coola, British Columbia, where he first reached saltwater at Due south Bentinck Arm, an inlet of the Pacific Sea.

The Lewis and Clark Expedition (1804–1806) was the outset scientific reconnaissance of the Rocky Mountains.^[23] Specimens were collected for gimmicky botanists, zoologists, and geologists. The trek was said to accept paved the style to (and through) the Rocky Mountains for European-Americans from the E, although Lewis and Clark met at least 11 European-American mount men during their travels.^[7]

Mountain men, primarily French, Castilian, and British, roamed the Rocky Mountains from 1720 to 1800 seeking mineral deposits and furs. The fur-trading North West Company established Rocky Mount House as a trading post in what is now the Rocky Mount Foothills of present-day Alberta in 1799, and their business organization rivals the Hudson's Bay Company established Acton Business firm nearby.^[24] These posts served as bases for most European activity in the Canadian Rockies in the early on 19th century. Amongst the most notable are the expeditions of David Thompson, who followed the Columbia River to the Pacific Ocean.^[25] On his 1811 expedition, he camped at the junction of the Columbia River and the Snake River and erected a pole and observe challenge the expanse for the United Kingdom and stating the intention of the North West Company to build a fort at the site.^[26]

By the Anglo-American Convention of 1818, which established the 49th parallel northward as the international boundary west from Lake of the Forest to the "Stony Mountains";^[27] the U.k. and the U.s.a. agreed to what has since been described equally "joint occupancy" of lands farther due west to the Pacific Ocean. Resolution of the territorial and treaty bug, the Oregon dispute, was deferred until a afterward time.

In 1819, Spain ceded their rights n of the 42nd Parallel to the United States, though these rights did non include possession and also included obligations to U.k. and Russia concerning their claims in the same region.

Settlement [edit]

After 1802, fur traders and explorers ushered in the kickoff widespread American presence in the Rockies south of the 49th parallel. The more than famous of these include William Henry Ashley, Jim Bridger, Kit Carson, John Colter, Thomas Fitzpatrick, Andrew Henry, and Jedediah Smith. On July 24, 1832, Benjamin Bonneville led the offset wagon railroad train across the Rocky Mountains by using South Laissez passer in the present State of Wyoming.^[seven] Similarly, in the wake of Mackenzie's 1793 expedition, fur trading posts were established west of the Northern Rockies in a region of the northern Interior Plateau of British Columbia which came to be known as New Caledonia, beginning with Fort McLeod (today'due south customs of McLeod Lake) and Fort Fraser, but ultimately focused on Stuart Lake Post (today'southward Fort St. James).

Negotiations betwixt the United kingdom of great britain and northern ireland and the United States over the next few decades failed to settle upon a compromise boundary and the Oregon Dispute became important in geopolitical diplomacy between the British Empire and the new American Republic. In 1841, James Sinclair, Main Factor of the Hudson'due south Bay Company, guided some 200 settlers from the Reddish River Colony west to bolster settlement around Fort Vancouver in an endeavor to retain the Columbia District for Britain. The party crossed the Rockies into the Columbia Valley, a region of the Rocky Mount Trench near nowadays-day Radium Hot Springs, British Columbia, and then traveled south. Despite such efforts, in 1846, United kingdom ceded all claim to Columbia District lands s of the 49th parallel to the United States; as resolution to the Oregon boundary dispute by the Oregon Treaty.^[28]

Thousands passed through the Rocky Mountains on the Oregon Trail beginning in the 1840s.^[29] The Mormons began settling nearly the Nifty Common salt Lake in 1847.^[30] From 1859 to 1864, gilt was discovered in Colorado, Idaho, Montana, and British Columbia, sparking several gilt rushes bringing thousands of prospectors and miners to explore every mountain and canyon and to create the Rocky Mountains' first major industry. The Idaho gold rush alone produced more gilt than the California and Alaska gilt rushes combined and was important in the financing of the Union Army during the American Civil War. The transcontinental railroad was completed in 1869,^[31] and Yellowstone National Park was established as the world's offset national park in 1872.^[32] Meanwhile, a transcontinental railroad in Canada was originally promised in 1871. Though political complications pushed its completion to 1885, the Canadian Pacific Railway eventually followed the Kick Horse and Rogers Passes to the Pacific Ocean.^[33] Canadian railway officials likewise convinced Parliament to gear up aside vast areas of the Canadian Rockies as Jasper, Banff, Yoho, and Waterton Lakes National Parks, laying the foundation for a tourism manufacture which thrives to this day. Glacier National Park (MT) was established with a similar relationship to tourism promotions by the Groovy Northern Railway.^[34] While settlers filled the valleys and mining towns, conservation and preservation ideals began to take hold. U.Southward. President Harrison established several forest reserves in the Rocky Mountains in 1891–1892. In 1905, U.Southward. President Theodore Roosevelt extended the Medicine Bow Forest Reserve to include the surface area at present managed every bit Rocky Mountain National Park. Economic development began to centre on mining, forestry, agriculture, and recreation, too as on the service industries that support them. Tents and camps became ranches and farms, forts and railroad train stations became towns, and some towns became cities.^[7]

Economy [edit]

Industry and evolution [edit]

Economical resource of the Rocky Mountains are varied and abundant. Minerals constitute in the Rocky Mountains include significant deposits of copper, gilded, 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 most 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 iii,000 workers. The Coeur d'Alene mine of northern Idaho produces silver, lead, and zinc. Canada's largest coal mines are near Fernie, British Columbia and Sparwood, British Columbia; additional coal mines be nearly Hinton, Alberta, and in the Northern Rockies surrounding Tumbler Ridge, British Columbia.^[7]

Abandoned mines with their wakes of mine tailings and toxic wastes dot the Rocky Mountain landscape. In one major example, lxxx years of zinc mining profoundly polluted the river and depository financial institution near Eagle River in north-cardinal 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 h2o quality, and the loss of recreational opportunities. The analysis also revealed that cleanup of the river could yield $ii.3 million in boosted revenue from recreation. In 1983, the former owner of the zinc mine was sued past the Colorado Attorney General for the $4.viii million cleanup costs; five years later on, ecological recovery was considerable.^{[7] [35]}

The Rocky Mountains incorporate several sedimentary basins that are rich in coalbed methane. Coalbed methane is natural gas that arises from coal, either through bacterial action or through exposure to high temperature. Coalbed methane supplies 7 percent of the natural gas used in the United States. The largest coalbed methane sources in the Rocky Mountains are in the San Juan Basin in New United mexican states and Colorado and the Powder River Basin in Wyoming. These two basins are estimated to contain 38 trillion cubic feet of gas. Coalbed marsh gas can exist recovered past dewatering the coal bed, and separating the gas from the water; or injecting water to fracture the coal to release the gas (so-called hydraulic fracturing).^[36]

Agriculture and forestry are major industries. Agriculture includes dryland and irrigated farming and livestock grazing. Livestock are oft moved between high-elevation summertime pastures and depression-elevation winter pastures, a practice known as transhumance.^[7]

Tourism [edit]

Every twelvemonth the scenic areas of the Rocky Mountains draw millions of tourists.^[vii] The main linguistic communication of the Rocky Mountains is English. But at that place are also linguistic pockets of Spanish and indigenous languages.

People from all over the world visit the sites to hike, campsite, or engage in mountain sports.^{[7] [37]} In the summer season, examples of tourist attractions are:

In the United States:

• Yellowstone National Park
• Glacier National Park
• Grand Teton National Park
• Rocky Mountain National Park
• Bang-up Sand Dunes National Park and Preserve
• Sawtooth National Recreation Area
• Flathead Lake

In Canada, the mountain range contains these national parks:

• Banff National Park
• Jasper National Park
• Kootenay National Park
• Waterton Lakes National Park
• Yoho National Park

Glacier National Park in Montana and Waterton Lakes National Park in Alberta border each other and are collectively known equally Waterton-Glacier International Peace Park

In the winter, skiing is the main attraction, with dozens of Rocky Mountain ski areas and resorts.

The adjacent Columbia Mountains in British Columbia contain major resorts such as Panorama and Kicking Horse, as well as Mount Revelstoke National Park and Glacier National Park.

There are numerous provincial parks in the British Columbia Rockies, the largest and most notable being Mount Assiniboine Provincial Park, Mountain Robson Provincial Park, Northern Rocky Mountains Provincial Park, Kwadacha Wilderness Provincial Park, Rock Mountain Provincial Park and Muncho Lake Provincial Park.

See also [edit]

• Arabian Rocky Mountains
• Canadian Rocky Mountains, mountain range between British Columbia and Alberta
• Geology of the Rocky Mountains
• List of mountain peaks of the Rocky Mountains
• Little Rocky Mountains, mountain range in north-central Montana
• Mountain human being
• Rocky Mountains subalpine zone
• Southern Rocky Mountains

Notes [edit]

1. ^ ^{a b} Three of these peaks lie on the Alberta-British Columbia edge.

References [edit]

1. ^ "Rocky Mountains | Location, Map, History, & Facts". Encyclopedia Britannica . Retrieved July 2, 2022.
2. ^ ^{a b} Madole, Richard F.; Bradley, William C.; Loewenherz, Deborah Southward.; Ritter, Dale F.; Rutter, Nathaniel West.; Thorn, Colin E. (1987). "Rocky Mountains". In Graf, William 50. (ed.). Geomorphic Systems of Due north America. Decade of North American Geology. Vol. two (Centennial Special ed.). Geological Society of America (published January 1, 1987). pp. 211–257. doi:x.1130/DNAG-CENT-v2.211. ISBN9780813754147 . Retrieved June 22, 2022.
3. ^ Ak rigg, Chiliad.P.Five.; Akrigg, Helen B. (1997). British Columbia Place Names (3rd ed.). Vancouver, BC: UBC Printing. p. 229. ISBN978-0-7748-0636-seven . Retrieved September 2, 2022.
4. ^ Mardon, Ernest G.; Mardon, Austin A. (2010). Community Identify Names of Alberta (third ed.). Edmonton, AB: Golden Meteorite Press. p. 283. ISBN978-one-897472-17-0 . Retrieved September 2, 2022.
5. ^ ^{a b} Gadd, Ben (1995). Handbook of the Canadian Rockies. Corax Press. ISBN9780969263111.
6. ^ Cannings, Richard (2007). The Rockies: A Natural History. Greystone/David Suzuki Foundation. p. 5. ISBN978-1-55365-285-4.
7. ^ ^{a b c d e f g h i j k l chiliad northward o}  This article incorporates public domain material from the Us Geological Survey certificate: T.J. Stohlgren. "Rocky Mountains".
8. ^ Chronic, Halka (1980). Roadside Geology of Colorado. ISBN978-0-87842-105-3.
9. ^ ^{a b} Blakely, Ron. "Geologic History of Western U.s.". Archived from the original on June 22, 2022.
10. ^ ^{a b} English language, Joseph M.; Johnston, Stephen T. (2004). "The Laramide Orogeny: What Were the Driving Forces?" (PDF). International Geology Review. 46 (9): 833 838. Bibcode:2004IGRv...46..833E. doi:10.2747/0020-6814.46.9.833. S2CID 129901811. Archived (PDF) from the original on June 7, 2022.
11. ^ ^{a b c} Gadd, Ben (2008). Canadian Rockies Geology Road Tours. Corax Press. ISBN9780969263128.
12. ^  This commodity incorporates public domain material from the The states Geological Survey document: "Geologic Provinces of the United States: Rocky Mountains". Retrieved December x, 2006.
13. ^ Lindsey, D.A. (2010). "The geologic story of Colorado's Sangre de Cristo Range" (PDF). U.Southward. Geological Survey. Round 1349. Archived (PDF) from the original on May ii, 2022.
14. ^ Pierce, K.L. (1979). History and dynamics of glaciation in the northern Yellowstone National Park area. Washington, DC: U.S. Geological Survey. pp. 1 90. Professional Paper 729-F.
15. ^ "Southern Rocky Mountains". Woods Encyclopedia Network. Archived from the original on October vii, 2022. Retrieved Baronial 22, 2022.
16. ^ "Northern Rocky Mountains". Forest Encyclopedia Network. Archived from the original on July 21, 2022. Retrieved August 22, 2022.
17. ^ ^{a b} Sheridan, Scott. "United states & Canada: Rocky Mountains (Affiliate fourteen)" (PDF). Geography of the U.s. and Canada form notes. Kent State University. Archived from the original (PDF) on September 1, 2006.
18. ^ "Rocky Mountains | mountains, N America". Encyclopædia Britannica. Archived from the original on August 12, 2022. Retrieved August 12, 2022.
19. ^ "Events in the West (1528–1536)". PBS. 2001. Archived from the original on April 10, 2022. Retrieved April 15, 2022.
20. ^ "The West: Events from 1650 to 1800". PBS. Archived from the original on July six, 2022.
21. ^ "Mackenzie: 1789, 1792–1797". Archived from the original on January 17, 2022. Retrieved April 15, 2022.
22. ^ "Commencement Crossing of North America National Celebrated Site of Canada". Archived from the original on May 12, 2022. Retrieved April xv, 2022.
23. ^ "Lewis and Clark Expedition: Scientific Encounters". Archived from the original on April 9, 2022. Retrieved April fifteen, 2022.
24. ^ "Rocky Mountain House National Historic Site of Canada". February 28, 2022. Archived from the original on May xiii, 2022. Retrieved April 15, 2022.
25. ^ "Guide to the David Thompson Papers 1806–1845". 2006. Retrieved April 15, 2022.
26. ^ Oldham, kit (January 23, 2003). "David Thompson plants the British flag at the confluence of the Columbia and Snake rivers on July 9, 1811". Archived from the original on March 26, 2022. Retrieved April fifteen, 2022.
27. ^ "Treaties in Force" (PDF). November one, 2007. Retrieved April 15, 2022.
28. ^ "Historical Context and American Policy". Archived from the original on May thirteen, 2022. Retrieved April xv, 2022.
29. ^ "Oregon Trail Interpretive Eye". Archived from the original on March 4, 2022. Retrieved Apr 15, 2022.
30. ^ "The Mormon Trail". Archived from the original on April 5, 2022. Retrieved April 15, 2022.
31. ^ "The Transcontinental Railroad". 2022. Archived from the original on April 12, 2022. Retrieved April xv, 2022.
32. ^ "Yellowstone National Park". April iv, 2022. Archived from the original on July 7, 2022. Retrieved April 15, 2022.
33. ^ "Canadian Pacific Railway". Archived from the original on Nov 20, 2022. Retrieved April fifteen, 2022.
34. ^ "Glaciers and Glacier National Park". 2022. Archived from the original on January 17, 2022. Retrieved April 15, 2022.
35. ^ Brandt, Eastward. (1993). "How much is a gray wolf worth?". National Wildlife. 31: 412.
36. ^ "Coal-Bed Gas Resources of the Rocky Mountain Region". USGS. USGS fact sheet 158-02. Archived from the original on June 28, 2022.
37. ^ "Rocky Mount National Park". National Park Foundation. Archived from the original on Oct 4, 2022. Retrieved August 12, 2022.

Further reading [edit]

• Businesswoman, Jill (2002). Rocky Mountain futures: an ecological perspective. Isle Press. ISBNane-55963-953-9.
• Newby, Rick (2004). The Rocky Mountain region. Greenwood Press. ISBN0-313-32817-X.

External links [edit]

• Colorado Rockies Forests ecoregion images at bioimages.vanderbilt.edu (slow modem version)
• North Central Rockies Forests ecoregion images at bioimages.vanderbilt.edu (deadening modem version)
• South Central Rockies Forests ecoregion images at bioimages.vanderbilt.edu (deadening modem version)
• Dusk on the Tiptop of the Rocky Mountains, CO, Historical Gild of Pennsylvania

Source: https://en.wikipedia.org/wiki/Rocky_Mountains

Posted by: ferrisapere1969.blogspot.com

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