Colorado Plateau - wikipedia Colorado Plateau A map of the Colorado Plateau. The Four Corners Monument is where the states of Colorado, New Mexico, Arizona, and Utah meet. ( The states are listed in clockwise order. ) The Colorado Plateau, also known as the Colorado Plateau Province, is a physiographic and desert region of the Intermontane Plateaus, roughly centered on the Four Corners region of the southwestern United States. The province covers an area of 337,000 km ( 130,000 mi ) within western Colorado, northwestern New Mexico, southern and eastern Utah, and northern Arizona. About 90 % of the area is drained by the Colorado River and its main tributaries : the Green, San Juan, and Little Colorado. Most of the remainder of the plateau is drained by the Rio Grande and its tributaries. The Colorado Plateau is largely made up of high desert, with scattered areas of forests. In the southwest corner of the Colorado Plateau lies the Grand Canyon of the Colorado River. Much of the Plateau 's landscape is related, in both appearance and geologic history, to the Grand Canyon. The nickname `` Red Rock Country '' suggests the brightly colored rock left bare to the view by dryness and erosion. Domes, hoodoos, fins, reefs, river narrows, natural bridges, and slot canyons are only some of the additional features typical of the Plateau. The Colorado Plateau has the greatest concentration of U.S. National Park Service ( NPS ) units in the country outside of the Washington, DC metropolitan area. Among its ten National Parks are Grand Canyon, Glen Canyon, Zion, Bryce Canyon, Capitol Reef, Canyonlands, Arches, Mesa Verde, and Petrified Forest. Among its 18 National Monuments are Bears Ears, Rainbow Bridge, Dinosaur, Hovenweep, Wupatki, Sunset Crater Volcano, Grand Staircase - Escalante, Natural Bridges, Canyons of the Ancients, Chaco Culture National Historical Park and the Colorado National Monument. Contents 1 Geography 2 Human history 3 Geology 4 Energy generation 5 Natural resources 5.1 Petroleum 5.2 Uranium 5.3 Coal 5.4 Gilsonite and uintaite 5.5 Scenic beauty 6 Protected lands 7 See also 8 References 8.1 Further reading Geography The Four Corners region and the Colorado Plateau. Click image to see state lines. The Book Cliffs of western Colorado. The Green River runs north to south from Wyoming, briefly through Colorado, and converges with the Colorado River in southeastern Utah. Sunset in Ojito Wilderness, near Albuquerque, NM The province is bounded by the Rocky Mountains in Colorado, and by the Uinta Mountains and Wasatch Mountains branches of the Rockies in northern and central Utah. It is also bounded by the Rio Grande Rift, Mogollon Rim and the Basin and Range Province. Isolated ranges of the Southern Rocky Mountains such as the San Juan Mountains in Colorado and the La Sal Mountains in Utah intermix into the central and southern parts of the Colorado Plateau. It is composed of six sections : Uinta Basin Section High Plateaus Section Grand Canyon Section Canyon Lands Section Navajo Section Datil Section As the name implies, the High Plateaus Section is, on average, the highest section. North - south trending normal faults that include the Hurricane, Sevier, Grand Wash, and Paunsaugunt separate the section 's component plateaus. This fault pattern is caused by the tensional forces pulling apart the adjacent Basin and Range province to the west, making this section transitional. Occupying the southeast corner of the Colorado Plateau is the Datil Section. Thick sequences of mid-Tertiary to late - Cenozoic - aged lava covers this section. Development of the province has in large part been influenced by structural features in its oldest rocks. Part of the Wasatch Line and its various faults form the western edge of the province. Faults that run parallel to the Wasatch Fault that lies along the Wasatch Range form the boundaries between the plateaus in the High Plateaus Section. The Uinta Basin, Uncompahgre Uplift, and the Paradox Basin were also created by movement along structural weaknesses in the region 's oldest rock. In Utah, the province includes several higher fault - separated plateaus : Awapa Plateau Aquarius Plateau Kaiparowits Plateau Markagunt Plateau Paunsaugunt Plateau Sevier Plateau Fishlake Plateau Pavant Plateau Gunnison Plateau and the Tavaputs Plateau. Some sources also include the Tushar Mountain Plateau as part of the Colorado Plateau, but others do not. The mostly flat - lying sedimentary rock units that make up these plateaus are found in component plateaus that are between 1,500 to 3,350 metres ( 4,900 to 11,000 ft ) above sea level. A supersequence of these rocks is exposed in the various cliffs and canyons ( including the Grand Canyon ) that make up the Grand Staircase. Increasingly younger east - west trending escarpments of the Grand Staircase extend north of the Grand Canyon and are named for their color : Chocolate Cliffs, Vermillion Cliffs, White Cliffs, Gray Cliffs, and the Pink Cliffs. Within these rocks are abundant mineral resources that include uranium, coal, petroleum, and natural gas. Study of the area 's unusually clear geologic history ( which is laid bare due to the arid and semiarid conditions ) has greatly advanced that science. A rain shadow from the Sierra Nevada far to the west and the many ranges of the Basin and Range means that the Colorado Plateau receives 15 to 40 centimetres ( 6 to 16 in ) of annual precipitation. Higher areas receive more precipitation and are covered in forests of pine, fir, and spruce. Though it can be said that the Plateau roughly centers on the Four Corners, Black Mesa in northern Arizona is much closer to the east - west, north - south midpoint of the Plateau Province. Lying southeast of Glen Canyon and southwest of Monument Valley at the north end of the Hopi Reservation, this remote coal - laden highland has about half of the Colorado Plateau 's acreage north of it, half south of it, half west of it, and half east of it. Human history The Ancestral Puebloan People lived in the region from around 2000 to 700 years ago. A party from Santa Fe led by Fathers Dominguez and Escalante, unsuccessfully seeking an overland route to California, made a five - month out - and - back trip through much of the Plateau in 1776 - 1777. Despite having lost one arm in the American Civil War, U.S. Army Major and geologist John Wesley Powell explored the area in 1869 and 1872. Using wooden oak boats and small groups of men the Powell Geographic Expedition charted this largely unknown region of the United States for the federal government. Construction of the Hoover Dam in the 1930s and the Glen Canyon Dam in the 1960s changed the character of the Colorado River. Dramatically reduced sediment load changed its color from reddish brown ( Colorado is Spanish for `` red '' ) to mostly clear. The apparent green color is from algae on the riverbed 's rocks, not from any significant amount of suspended material. The lack of sediment has also starved sand bars and beaches but an experimental 12 - day - long controlled flood from Glen Canyon Dam in 1996 showed substantial restoration. Similar floods are planned for every 5 to 10 years. Geology The Redwall Limestone cliffs of the Colorado Plateau tower above the northern Mojave Desert. The Permian through Jurassic stratigraphy of the Colorado Plateau area of southeastern Utah that makes up much of the famous prominent rock formations in protected areas such as Capitol Reef National Park and Canyonlands National Park. From top to bottom : Rounded tan domes of the Navajo Sandstone, layered red Kayenta Formation, cliff - forming, vertically jointed, red Wingate Sandstone, slope - forming, purplish Chinle Formation, layered, lighter - red Moenkopi Formation, and white, layered Cutler Formation sandstone. Picture from Glen Canyon National Recreation Area, Utah. Erosion - resistant sandstones of Mesozoic age result in bands of continuous cliffs, central Colorado Plateau. MODIS satellite image of Grand Canyon, Lake Powell ( black, left of center ) and the Colorado Plateau. White areas are snow - capped. One of the most geologically intriguing features of the Colorado Plateau is its remarkable stability. Relatively little rock deformation such as faulting and folding has affected this high, thick crustal block within the last 600 million years or so. In contrast, provinces that have suffered severe deformation surround the plateau. Mountain building thrust up the Rocky Mountains to the north and east and tremendous, earth - stretching tension created the Basin and Range province to the west and south. Sub ranges of the Southern Rocky Mountains are scattered throughout the Colorado Plateau. The Precambrian and Paleozoic history of the Colorado Plateau is best revealed near its southern end where the Grand Canyon has exposed rocks with ages that span almost 2 billion years. The oldest rocks at river level are igneous and metamorphic and have been lumped together as `` Vishnu Basement Rocks '' ; the oldest ages recorded by these rocks fall in the range 1950 to 1680 million years. An erosion surface on the `` Vishnu Basement Rocks '' is covered by sedimentary rocks and basalt flows, and these rocks formed in the interval from about 1250 to 750 million years ago : in turn, they were uplifted and split into a range of fault - block mountains. Erosion greatly reduced this mountain range prior to the encroachment of a seaway along the passive western edge of the continent in the early Paleozoic. At the canyon rim is the Kaibab Formation, limestone deposited in the late Paleozoic ( Permian ) about 270 million years ago. A 12,000 - to - 15,000 - foot high ( 3,700 to 4,600 m ) extension of the Ancestral Rocky Mountains called the Uncompahgre Mountains were uplifted and the adjacent Paradox Basin subsided. Almost 4 mi. ( 6.4 km ) of sediment from the mountains and evaporites from the sea were deposited ( see geology of the Canyonlands area for detail ). Most of the formations were deposited in warm shallow seas and near - shore environments ( such as beaches and swamps ) as the seashore repeatedly advanced and retreated over the edge of a proto - North America ( for detail, see geology of the Grand Canyon area ). The province was probably on a continental margin throughout the late Precambrian and most of the Paleozoic era. Igneous rocks injected millions of years later form a marbled network through parts of the Colorado Plateau 's darker metamorphic basement. By 600 million years ago North America had been leveled off to a remarkably smooth surface. Throughout the Paleozoic Era, tropical seas periodically inundated the Colorado Plateau region. Thick layers of limestone, sandstone, siltstone, and shale were laid down in the shallow marine waters. During times when the seas retreated, stream deposits and dune sands were deposited or older layers were removed by erosion. Over 300 million years passed as layer upon layer of sediment accumulated. It was not until the upheavals that coincided with the formation of the supercontinent Pangea began about 250 million years ago that deposits of marine sediment waned and terrestrial deposits dominate. In late Paleozoic and much of the Mesozoic era the region was affected by a series of orogenies ( mountain - building events ) that deformed western North America and caused a great deal of uplift. Eruptions from volcanic mountain ranges to the west buried vast regions beneath ashy debris. Short - lived rivers, lakes, and inland seas left sedimentary records of their passage. Streams, ponds and lakes created formations such as the Chinle, Moenave, and Kayenta in the Mesozoic era. Later a vast desert formed the Navajo and Temple Cap formations and dry near - shore environment formed the Carmel ( see geology of the Zion and Kolob canyons area for details ). The area was again covered by a warm shallow sea when the Cretaceous Seaway opened in late Mesozoic time. The Dakota Sandstone and the Tropic Shale were deposited in the warm shallow waters of this advancing and retreating seaway. Several other formations were also created but were mostly eroded following two major periods of uplift. The Laramide orogeny closed the seaway and uplifted a large belt of crust from Montana to Mexico, with the Colorado Plateau region being the largest block. Thrust faults in Colorado are thought to have formed from a slight clockwise movement of the region, which acted as a rigid crustal block. The Colorado Plateau Province was uplifted largely as a single block, possibly due to its relative thickness. This relative thickness may be why compressional forces from the orogeny were mostly transmitted through the province instead of deforming it. Pre-existing weaknesses in Precambrian rocks were exploited and reactivated by the compression. It was along these ancient faults and other deeply buried structures that much of the province 's relatively small and gently inclined flexures ( such as anticlines, synclines, and monoclines ) formed. Some of the prominent isolated mountain ranges of the Plateau, such as Ute Mountain and the Carrizo Mountains, both near the Four Corners, are cored by igneous rocks that were emplaced about 70 million years ago. Minor uplift events continued through the start of the Cenozoic era and were accompanied by some basaltic lava eruptions and mild deformation. The colorful Claron Formation that forms the delicate hoodoos of Bryce Amphitheater and Cedar Breaks was then laid down as sediments in cool streams and lakes ( see geology of the Bryce Canyon area for details ). The flat - lying Chuska Sandstone was deposited about 34 million years ago ; the sandstone is predominantly of eolian origin and locally more than 500 meters thick. The Chuska Sandstone caps the Chuska mountains, and it lies unconformably on Mesozoic rocks deformed during the Laramide orogeny. Younger igneous rocks form spectacular topographic features. The Henry Mountains, La Sal Range, and Abajo Mountains, ranges that dominate many views in southeastern Utah, are formed about igneous rocks that were intruded in the interval from 20 to 31 million years : some igneous intrusions in these mountains form laccoliths, a form of intrusion recognized by Grove Karl Gilbert during his studies of the Henry Mountains. Ship Rock ( also called Shiprock ), in northwestern New Mexico, and Church Rock and Agathla, near Monument Valley, are erosional remnants of potassium - rich igneous rocks and associated breccias of the Navajo Volcanic Field, produced about 25 million years ago. The Hopi Buttes in northeastern Arizona are held up by resistant sheets of sodic volcanic rocks, extruded about 7 million years ago. More recent igneous rocks are concentrated nearer the margins of the Colorado Plateau. The San Francisco Peaks near Flagstaff, south of the Grand Canyon, are volcanic landforms produced by igneous activity that began in that area about 6 million years ago and continued until 1064 C.E., when basalt erupted in Sunset Crater National Monument. Mount Taylor, near Grants, New Mexico, is a volcanic structure with a history similar to that of the San Francisco Peaks : a basalt flow closer to Grants was extruded only about 3000 years ago ( see El Malpais National Monument ). These young igneous rocks may record processes in the Earth 's mantle that are eating away at deep margins of the relatively stable block of the Plateau. Tectonic activity resumed in Mid Cenozoic time and started to unevenly uplift and slightly tilt the Colorado Plateau region and the region to the west some 20 million years ago ( as much as 3 kilometers of uplift occurred ). Streams had their gradient increased and they responded by downcutting faster. Headward erosion and mass wasting helped to erode cliffs back into their fault - bounded plateaus, widening the basins in - between. Some plateaus have been so severely reduced in size this way that they become mesas or even buttes. Monoclines form as a result of uplift bending the rock units. Eroded monoclines leave steeply tilted resistant rock called a hogback and the less steep version is a cuesta. Cliffs of Navajo Sandstone in Zion National Park Great tension developed in the crust, probably related to changing plate motions far to the west. As the crust stretched, the Basin and Range province broke up into a multitude of down - dropped valleys and elongate mountains. Major faults, such as the Hurricane Fault, developed that separate the two regions. The dry climate was in large part a rainshadow effect resulting from the rise of the Sierra Nevada further west. Yet for some reason not fully understood, the neighboring Colorado Plateau was able to preserve its structural integrity and remained a single tectonic block. A second mystery was that while the lower layers of the Plateau appeared to be sinking, overall the Plateau was rising. The reason for this was discovered upon analyzing data from the USARRAY project. It was found that the asthenosphere had invaded the overlying lithosphere, as a result of an area of mantle upwelling stemming from either the disintegration of the descending Farallon Plate, or the survival of the subducted spreading center connected to the East Pacific Rise and Gorda Ridge beneath western North America, or possibly both. The asthenosphere erodes the lower levels of the Plateau. At the same time, as it cools, it expands and lifts the upper layers of the Plateau. Eventually, the great block of Colorado Plateau crust rose a kilometer higher than the Basin and Range. As the land rose, the streams responded by cutting ever deeper stream channels. The most well - known of these streams, the Colorado River, began to carve the Grand Canyon less than 6 million years ago. The Pleistocene epoch brought periodic ice ages and a cooler, wetter climate. This increased erosion at higher elevations with the introduction of alpine glaciers while mid-elevations were attacked by frost wedging and lower areas by more vigorous stream scouring. Pluvial lakes also formed during this time. Glaciers and pluvial lakes disappeared and the climate warmed and became drier with the start of Holocene epoch. Energy generation Castle Gate Power Plant near Helper, UT. Coal mine in Carbon County, UT. Oil well in the Uinta Basin, Utah. Electrical power generation is one of the major industries that takes place in the Colorado Plateau region. Most electrical generation comes from coal fired power plants. Natural resources Petroleum The rocks of the Colorado Plateau are a source of oil and a major source of natural gas. Major petroleum deposits are present in the San Juan Basin of New Mexico and Colorado, the Uinta Basin of Utah, the Piceance Basin of Colorado, and the Paradox Basin of Utah, Colorado, and Arizona. Uranium Main article : Uranium mining in Utah The Colorado Plateau holds major uranium deposits, and there was a uranium boom in the 1950s. The Atlas Uranium Mill near Moab has left a problematic tailings pile for cleanup, which is soon to happen. Coal Major coal deposits are being mined in the Colorado Plateau in Utah, Arizona, Colorado, and New Mexico, though large coal mining projects, such as on the Kaiparowits Plateau, have been proposed and defeated politically. The ITT Power Project, eventually located in Lynndyl, Utah, near Delta, was originally suggested for Salt Wash near Capitol Reef National Park. After a firestorm of opposition, it was moved to a less beloved site. In Utah the largest deposits are in aptly named Carbon County. In Arizona the biggest operation is on Black Mesa, supplying coal to Navajo Power Plant. Gilsonite and uintaite Perhaps the only one of its kind, a gilsonite plant near Bonanza, southeast of Vernal, Utah, mines this unique, lustrous, brittle form of asphalt, for use in `` varnishes, paints,... ink, waterproofing compounds, electrical insulation,... roofing materials. '' Scenic beauty The scenic appeal of this unique landscape had become, well before the end of the twentieth century, its greatest financial natural resource. The amount of commercial benefit to the four states of the Colorado Plateau from tourism exceeded that of any other natural resource. Protected lands North Rim of the Grand Canyon National Park, Arizona. Painted Desert seen from Blue Mesa, Petrified Forest National Park Erosional features within Glen Canyon National Recreation Area. Cliff Palace at Mesa Verde National Park, Colorado. This relatively high semi-arid province produces many distinctive erosional features such as arches, arroyos, canyons, cliffs, fins, natural bridges, pinnacles, hoodoos, and monoliths that, in various places and extents, have been protected. Also protected are areas of historic or cultural significance, such as the pueblos of the Anasazi culture. There are nine U.S. National Parks, a National Historical Park, sixteen U.S. National Monuments and dozens of wilderness areas in the province along with millions of acres in U.S. National Forests, many state parks, and other protected lands. In fact, this region has the highest concentration of parklands in North America. Lake Powell, in foreground, is not a natural lake but a reservoir impounded by Glen Canyon Dam. National parks ( from south to north to south clockwise ) : Petrified Forest National Park Grand Canyon National Park Zion National Park Bryce Canyon National Park Capitol Reef National Park Canyonlands National Park Arches National Park Black Canyon of the Gunnison National Park Mesa Verde National Park Chaco Culture National Historical Park National Monuments ( alphabetical ) : Aztec Ruins National Monument Canyon De Chelly National Monument Canyons of the Ancients National Monument Cedar Breaks National Monument Colorado National Monument Dinosaur National Monument Grand Canyon - Parashant National Monument Grand Staircase - Escalante National Monument El Malpais National Monument El Morro National Monument Hovenweep National Monument Navajo National Monument Natural Bridges National Monument Rainbow Bridge National Monument Sunset Crater National Monument Vermilion Cliffs National Monument Walnut Canyon National Monument Wupatki National Monument Wilderness areas : Kachina Peaks Wilderness Strawberry Crater Wilderness Kendrick Mountain Wilderness Beaver Dam Mountains Wilderness Paiute Wilderness Grand Wash Cliffs Wilderness Mount Logan Wilderness Mount Trumbull Wilderness Kanab Creek Wilderness Cottonwood Point Wilderness Paria Canyon - Vermilion Cliffs Wilderness Saddle Mountain Wilderness Mount Baldy Wilderness Escudilla Wilderness Black Ridge Canyons Wilderness Flat Tops Wilderness Uncompahgre Wilderness Mount Sneffels Wilderness Lizard Head Wilderness Weminuche Wilderness South San Juan Wilderness Cebolla Wilderness Ojito Wilderness West Malpais Wilderness Bisti / De-Na - Zin Wilderness Pine Valley Mountain Wilderness Ashdown Gorge Wilderness Box - Death Hollow Wilderness Dark Canyon Wilderness High Uintas Wilderness Other notable protected areas include : Glen Canyon National Recreation Area, Dead Horse Point State Park, Goosenecks State Park, the San Rafael Swell, the Grand Gulch Primitive Area, Kodachrome Basin State Park, Goblin Valley State Park, Monument Valley, and Barringer Crater. Sedona, Arizona and Oak Creek Canyon lie on the south - central border of the Plateau. Many but not all of the Sedona area 's cliff formations are protected as wilderness. The area has the visual appeal of a national park, but with a small, rapidly growing town in the center. See also Deserts Rocky Mountains Mojave Desert Great Basin Sonoran Desert References Jump up ^ `` Colorado Plateau plateau, United States ''. Encyclopedia Britannica. Retrieved 2017 - 06 - 05. Jump up ^ Leighty, Robert D. ( 2001 ). `` Colorado Plateau Physiographic Province ''. Contract Report. Defense Advanced Research Projects Agency ( DOD ) Information Sciences Office. Archived from the original on 2004 - 09 - 26. Retrieved 2007 - 12 - 25. ^ Jump up to : Kiver, Eugene P. ; Harris, David V. ( 1999 ). Geology of U.S. Parklands ( 5th ed. ). John Wiley & Sons. ISBN 0 - 471 - 33218 - 6. Jump up ^ Crampton, Gregory ( 1964 ). Standing Up Country. New York : Alfred Knopf. pp. 43 -- 46. ^ Jump up to : This article incorporates public domain material from the United States Geological Survey document : `` Colorado Plateau Province ''. Geologic Provinces of the United States. Retrieved 2017 - 07 - 04. Jump up ^ `` Why is the Colorado Plateau Rising ? ''. Geology.com. Archived from the original on 2011 - 05 - 05. Retrieved 9 May 2011. Jump up ^ Utah : A Guide to the State. 1982. p. 590. Further reading Wikimedia Commons has media related to Colorado Plateau. Prickly pear cactus are common throughout the Colorado Plateau region. Baars, Donald L. ( 1972 ). Red Rock Country : The Geologic History of the Colorado Plateau. Doubleday. ISBN 0 - 385 - 01341 - 8. Baars, Donald L. ( 2002 ). Traveler 's Guide to the Geology of the Colorado Plateau. University of Utah Press. ISBN 0 - 87480 - 715 - 8. Baldridge, W. Scott ( 2004 ). Geology of the American Southwest : A Journey Through Two Billion Years of Plate - Tectonic History. Cambridge University Press. ISBN 0 - 521 - 01666 - 5. Fillmore, Robert ( 2011 ). Geological Evolution of the Colorado Plateau of Eastern Utah and Western Colorado. University of Utah Press. ISBN 978 - 1 - 60781 - 004 - 9. Harris, Ann G. ; Tuttle, Esther ; Tuttle, Sherwood D. ( 1997 ). Geology of National Parks ( Fifth ed. ). Iowa : Kendall / Hunt Publishing. pp. 2 -- 3, 19 -- 20, 25. ISBN 0 - 7872 - 5353 - 7. Plummer, Charles C. ; McGeary, David ; Carlson, Diane H. ( 1999 ). Physical Geology ( Eighth ed. ). Boston : McGraw - Hill. p. 320. ISBN 0 - 697 - 37404 - 1. Stanley, Steven M. ( 1999 ). Earth System History. W.H. Freeman and Company. pp. 511 -- 513,537. ISBN 0 - 7167 - 2882 - 6. Foos, Annabelle. Geology of the Colorado Plateau ( PDF ). National Park Service. Archived from the original ( PDF ) on 2004 - 06 - 10. Retrieved 2005 - 12 - 21. Roylance, Ward ( 1982 ). Utah : A Guide to the State. Salt Lake City : Utah : A Guide to the State Foundation. OL 3508093M. Look, Al ( 1947 ). A Thousand Million Years on the Colorado Plateau. Golden Bell Publications. OCLC 254673147. Trimble, Stephen ( 1979 ). The Bright Edge : A Guide to the National Parks of the Colorado Plateau. Museum of Northern Arizona Press. OCLC 768218015. 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Aurora - Lakewood, CO Metropolitan Statistical Area Eastern Plains Front Range Grand Valley High Plains High Rockies Mineral Belt Northern Colorado Northwestern Colorado Piedmont Plateau Roan Plateau Roaring Fork Valley San Luis Valley Sangre de Cristo Mountains South - Central Colorado Southwest Colorado Uinta Mountains Uintah Basin Western Slope Municipalities Akron Alamosa Arvada Aspen Aurora Boulder Breckenridge Brighton Broomfield Cañon City Castle Rock Centennial Colorado Springs Commerce City Cortez Craig Delta Denver Durango Englewood Erie Evans Fairplay Federal Heights Fort Collins Fort Morgan Fountain Golden Glenwood Springs Grand Junction Greeley Greenwood Village Gunnison La Junta Lafayette Lakewood Lamar Leadville Littleton Longmont Louisville Loveland Montrose Northglenn Parker Platteville Pueblo Salida Steamboat Springs Sterling Superior Thornton Trinidad Vail Westminster Wheat Ridge Windsor Counties Adams Alamosa Arapahoe Archuleta Baca Bent Boulder Broomfield Chaffee Cheyenne Clear Creek Conejos Costilla Crowley Custer Delta Denver Dolores Douglas Eagle El Paso Elbert Fremont Garfield Gilpin Grand Gunnison Hinsdale Huerfano Jackson Jefferson Kiowa Kit Carson La Plata Lake Larimer Las Animas Lincoln Logan Mesa Mineral Moffat Montezuma Montrose Morgan Otero Ouray Park Phillips Pitkin Prowers Pueblo Rio Blanco Rio Grande Routt Saguache San Juan San Miguel Sedgwick Summit Teller Washington Weld Yuma State of Utah Salt Lake City ( capital ) Topics Cities Congressional districts Counties Flag Geography Government Governors Healthcare History People Portal State fair Symbols Tourist attractions Society Culture Crime Demographics Economy Education Politics Regions Cache Valley Colorado Plateau Dixie Great Basin Great Salt Lake Great Salt Lake Desert Mojave Desert Monument Valley San Rafael Swell Uinta Basin Uinta Mountains Wasatch Back Wasatch Front Wasatch Range Largest cities American Fork Bountiful Cedar City Clearfield Cottonwood Heights Draper Holladay Kaysville Layton Lehi Logan Midvale Millcreek Murray Ogden Orem Pleasant Grove Provo Riverton Roy St. George Salt Lake City Sandy South Jordan South Salt Lake Spanish Fork Springville Taylorsville Tooele West Jordan West Valley City Counties Beaver Box Elder Cache Carbon Daggett Davis Duchesne Emery Garfield Grand Iron Juab Kane Millard Morgan Piute Rich Salt Lake San Juan Sanpete Sevier Summit Tooele Uintah Utah Wasatch Washington Wayne Weber Attractions Festivals Sundance Film Festival Utah Shakespeare Festival National Monuments Bears Ears National Monument Cedar Breaks National Monument Dinosaur National Monument Grand Staircase - Escalante National Monument Hovenweep National Monument Natural Bridges National Monument Rainbow Bridge National Monument Timpanogos Cave National Monument National parks Arches National Park Bryce Canyon National Park Canyonlands National Park Capitol Reef National Park Zion National Park National Recreation Areas Flaming Gorge National Recreation Area Glen Canyon National Recreation Area Ski resorts Alta Ski Area Beaver Mountain Brian Head Ski Resort Brighton Ski Resort Cherry Peak Resort Deer Valley Park City Mountain Resort Powder Mountain Snowbasin Snowbird Ski Resort Solitude Mountain Resort Sundance Resort Wolf Mountain Other Bonneville Salt Flats Golden Spike National Historic Site Great Salt Lake Lagoon ( amusement park ) Temple Square State of Arizona Phoenix ( capital ) Topics Index Climate Delegations Geography Government History World War II Museums Music People Transportation Tourist attractions Society Culture Crime Demographics Economy Education Politics Regions Arizona Strip Arizona Sun Corridor Coconino Plateau Colorado Plateau Grand Canyon Kaibab Plateau Mogollon Plateau Mogollon Rim Mojave Desert Monument Valley North Central Arizona Northeast Arizona Northern Arizona Oak Creek Canyon Phoenix Metropolitan Area Safford area San Francisco Volcanic Field Sonoran Desert Southern Arizona ( Traditional Arizona ) Transition zone Verde Valley White Mountains Counties Apache Cochise Coconino Gila Graham Greenlee La Paz Maricopa Mohave Navajo Pima Pinal Santa Cruz Yavapai Yuma Cities Chandler Flagstaff Gilbert Glendale Kingman Lake Havasu City Mesa Peoria Phoenix Prescott Scottsdale Sierra Vista Tempe Tucson Yuma State of New Mexico Santa Fe ( capital ) Topics Index Delegations Geography Government History World War II Landmarks Military Nuevomexicanos New Mexicans Paleontology Municipalities Census - designated places Symbols Transportation Tribes Tourist attractions New Mexican cuisine Society Crime Culture Demographics Economy Education Politics Regions Central New Mexico Colorado Plateau Eastern New Mexico Llano Estacado Northern New Mexico Permian Basin San Luis Valley Sangre de Cristo Mountains Southwestern New Mexico Cities Alamogordo Albuquerque Artesia Carlsbad Clovis Corrales Deming Española Farmington Gallup Grants Hobbs Las Cruces Las Vegas Los Alamos Los Lunas Lovington Portales Raton Rio Rancho Roswell Ruidoso Santa Fe Silver City Socorro Sunland Park Taos Tucumcari Counties See : List of counties in New Mexico Bernalillo Catron Chaves Cibola Colfax Curry De Baca Doña Ana Eddy Grant Guadalupe Harding Hidalgo Lea Lincoln Los Alamos Luna McKinley Mora Otero Quay Rio Arriba Roosevelt San Juan San Miguel Sandoval Santa Fe Sierra Socorro Taos Torrance Union Valencia Coordinates : 37 ° N 110 ° W ﻿ / ﻿ 37 ° N 110 ° W ﻿ / 37 ; - 110 VIAF : 233666076 LCCN : sh85028685 GND : 4010409 - 6 Retrieved from `` https://en.wikipedia.org/w/index.php?title=Colorado_Plateau&oldid=801297545 '' Categories : Colorado Plateau Hidden categories : Wikipedia articles incorporating text from the United States Geological Survey All articles with unsourced statements Articles with unsourced statements from December 2011 Coordinates on Wikidata Wikipedia articles with VIAF identifiers Wikipedia articles with LCCN identifiers Wikipedia articles with GND identifiers Talk Contents About Wikipedia Беларуская Български Čeština Deutsch Eesti Español Esperanto فارسی Français Gàidhlig 한국어 Հայերեն Bahasa Indonesia Italiano עברית ಕನ್ನಡ Кыргызча Lietuvių Magyar 日本 語 Oʻzbekcha / ўзбекча Polski Português Русский Suomi Türkçe Українська 中文 Edit links This page was last edited on 18 September 2017, at 21 : 20. 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Question: the colorado plateau covers northern new mexico and what other state
Answer: Colorado