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The Colorado orogeny was an episode of mountain building (an orogeny) in Colorado and surrounding areas. This took place from 1780 to 1650 million years
Colorado_orogeny
Period of mountain building in North America
The Laramide orogeny was a time period of mountain building in western North America, which started in the Late Cretaceous, 80 to 70 million years ago
Laramide_orogeny
Mountain-building episode in North America
The Sevier orogeny was a mountain-building event that affected western North America from northern Canada to the north to Mexico to the south. The Sevier
Sevier_orogeny
Craton in the west-central United States and western Canada
Paleoproterozoic Colorado orogeny. The Colorado orogen collided with the Wyoming Craton at 1.78–1.75 Ga. Collision of the Colorado orogen and the Trans-Hudson
Wyoming_Craton
marked today by the Laramie Mountains. The Colorado orogeny was likely part of the larger Yavapai orogeny, which extended across North America and probably
Geology of the Rocky Mountains
Geology_of_the_Rocky_Mountains
Mountain building event 1.7 billion years ago in the southwestern United States
belt, the Colorado province or Colorado orogeny at 1780–1700 Mya. Metasomatic tourmalinites dated to 1680 Mya found within the Cerro Colorado Tusas Mountains
Yavapai_orogeny
Area of ore deposits in Colorado, United States
Igneous rocks intruded about 60 to 70 million years ago during the Laramide orogeny are associated with the belt and once were thought to be responsible for
Colorado_Mineral_Belt
several cratons Barramundi Orogeny (c. 1.8 Gyr) influences MacArthur Basin in Northern Australia. c. 1,780 Ma – Colorado Orogeny (1.78 – 1.65 Gyr) influences
Timeline_of_Earth
Major river in the western United States and Mexico
years ago in a mountain-building episode known as the Laramide orogeny. The Colorado River first formed as a west-flowing stream draining the southwestern
Colorado_River
Mountain-building event in North America
The Trans-Hudson orogeny or Trans-Hudsonian orogeny was the major mountain building event (orogeny) that formed the Precambrian Canadian Shield and the
Trans-Hudson_orogeny
Collision of tectonic plates resulting in the creation of mountains
The Variscan orogeny or Hercynian orogeny was a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia)
Variscan_orogeny
Plateau in southwestern United States
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
Colorado_Plateau
Mountain-building event in North America
The Mazatzal orogeny was an orogenic event in what is now the Southwestern United States from 1650 to 1600 Mya in the Statherian Period of the Paleoproterozoic
Mazatzal_orogeny
Tectonic event from the Late Devonian into the Mississippian and early Pennsylvanian
The Antler orogeny was a tectonic event which occurred in Nevada during the Mississippian subperiod of the Carboniferous. A great volume of conglomeratic
Antler_orogeny
Steep-sided canyon in Arizona, US
the Colorado Plateau, starting about 65 million years ago (during the Laramide orogeny). This uplift has steepened the stream gradient of the Colorado River
Grand_Canyon
Geologic structural basin in the U.S.
basin started forming as early as 300 million years ago, during the Colorado orogeny that created the Ancestral Rockies. Rocks formed during this time include
Denver_Basin
Mountain-building event in what is now the Southwestern US
The Berthoud orogeny of Colorado, which emplaced the Berthoud Plutonic Suite, took place in the same time frame as the Picuris Orogeny. A number of quartzite-rhyolite
Picuris_orogeny
Mountain range in eastern North America
their relatives themselves were created by a series of three distinct orogenies beginning approximately 480 million years ago, making them one of the
Appalachian_Mountains
Major mountain range in western North America
Rockies formed 55 million to 80 million years ago during the Laramide orogeny, in which a number of plates began sliding underneath the North American
Rocky_Mountains
American mountain range
rocks formed during the Colorado orogeny some 1.7 billion years ago and then uplifted more recently during the Laramide orogeny. The Blanca Massif is also
Sangre_de_Cristo_Range
the U.S. State of Colorado was assembled from island arcs accreted onto the edge of the ancient Wyoming Craton. The Sonoma orogeny uplifted the ancestral
Geology_of_Colorado
Colorado Colorado orogeny Colorado Parks and Wildlife website commons:Category:State parks of Colorado Colorado Piedmont Colorado places Colorado places
Index of Colorado-related articles
Index_of_Colorado-related_articles
Mountain in Colorado, United States
Precambrian, approximately 1.05 billion years ago, during the Grenville orogeny. Through the process of uplifting, the hardened rock pushed through the
Pikes_Peak
Origin theory for geologic formation in the U.S.
The Central Plains orogeny was a mountain building event in the Proterozoic from 1630 to 1800 million years ago, preserved in the subsurface of Nebraska
Central_Plains_orogeny
Highest mountain in Colorado, United States
Mount Elbert is part of the Sawatch Range, an uplift of the Laramide Orogeny which separated from the Mosquito Range to the east around 28 million years
Mount_Elbert
Craton forming the geological core of North America
included the Yavapai orogeny at 1.71 to 1.68 Gya, which welded the 1.8 to 1.7 Gya Yavapai province to Laurentia; the Mazatzal orogeny at 1.65 to 1.60 Gya
Laurentia
Earthquake in Colorado, US
Colorado. It is the largest earthquake in Colorado's history. The Southern Rocky Mountains are still actively growing due to the Laramide orogeny. The
1882_Fort_Collins_earthquake
Prehistory of Colorado provides an overview of the activities that occurred prior to Colorado's recorded history. Colorado experienced cataclysmic geological
Prehistory_of_Colorado
Ridge in the Rocky Mountains, US
sandstone beds that cap the ridge. The hogback was formed during the Laramide orogeny, approximately 50 million years (50 my) ago, when the modern Rockies were
Dakota_Hogback
Concert venue near Morrison, Colorado, U.S.
colloquially as Red Rocks) is an open-air amphitheater near Morrison, Colorado, approximately ten miles (16 km) southwest of Denver. It is owned and operated
Red_Rocks_Amphitheatre
Supercontinent from the late Paleozoic to early Mesozoic eras
collided with Laurentia, forming Euramerica, an event called the Caledonian orogeny. As Avalonia inched towards Laurentia, the seaway between them, a remnant
Pangaea
Caldera in the state of Utah
shallowed considerably. The shallowing was also responsible for the Laramide Orogeny which created the Rocky Mountains. Once slab rollback strengthened, this
Wah_Wah_Springs_Caldera
Tasman Sea Predates uplift of Great Escarpment Colorado 75 Gulf of California Uplift during Laramide orogeny, see Geology of the Grand Canyon area Murrumbidgee
List_of_rivers_by_age
National monument in Colorado and Utah, United States
mountain building forces that formed the Uinta Mountains during the Laramide orogeny. Erosion later exposed the layers at the surface to be found by paleontologists
Dinosaur_National_Monument
Mountain range in New Mexico, United States
p. 75. Cather, Steven M. (2004). "Laramide orogeny in central and northern New Mexico and southern Colorado". In Mack, G.H.; Giles, K.A. (eds.). The geology
Zuñi_Mountains
Mountain in the American state of Colorado
of the Town of Crested Butte in Gunnison County, Colorado, United States. During the Laramide Orogeny the area near Matchless Mountain was lifted and Precambrian
Matchless_Mountain_(Colorado)
Mountain range in Colorado, US
faulted anticlines formed as part of the Sawatch Uplift during the Laramide orogeny around 65 million years ago (Mya). The mountains were originally contiguous
Mosquito_Range
Mountain range in Colorado and New Mexico, United States
located in southern Colorado and northern New Mexico in the United States. The mountains run from Poncha Pass in South-Central Colorado, trending southeast
Sangre_de_Cristo_Mountains
Mountain pass and archaeological site in Colorado, USA
planking used for snowsheds. The Front Range was created by the Laramide Orogeny, the last of three major mountain-building events, which occurred between
Rollins_Pass
was overwritten during the Yavapai and Mazatzal orogenies in the Proterozoic. The Grenville orogeny to the east caused Arizona to fill with sediments
Geology_of_Arizona
Geologic formation in Emery County, Utah, United States
shale, and limestone that was pushed up during the Paleocene Laramide Orogeny 40–60 million years ago. Since that time, infrequent but powerful flash
San_Rafael_Swell
Mazatzal orogenies 1750 to 1650 million years ago (Mya). This was followed by 200 million years of tectonic quiescence that ended in the Picuris orogeny. This
Geology_of_New_Mexico
Aspect of geology
Laramide orogeny; a mountain-building event that is largely responsible for creating the Rocky Mountains to the east. In total, the Colorado Plateau was
Geology of the Grand Canyon area
Geology_of_the_Grand_Canyon_area
National park in Colorado, United States
located approximately 55 mi (89 km) northwest of Denver in north-central Colorado, within the Front Range of the Rocky Mountains. The park is situated between
Rocky_Mountain_National_Park
Protected rock formation near Colorado Springs, Colorado
Niitko’usi’i) is a 1,341.3-acre (542.8 ha) public park located in Colorado Springs, Colorado, United States. 862 acres (349 ha) of the park was designated
Garden_of_the_Gods
Mountain park in Jefferson County, Colorado, US
eroded during the Pennsylvanian epoch. Later, uplift during the Laramide orogeny tilted the rocks to the angle at which they sit today. An Army expedition
Red_Rocks_Park
Long, narrow ridge
years ago. The Black Hills are the easternmost segment of the Laramide orogeny. The Dakota hogback rim separates the surrounding flat plains from the
Hogback_(geology)
High-altitude basin in Colorado and New Mexico in the United States
The San Luis Valley is a region in south-central Colorado with a small portion overlapping into New Mexico. The valley is approximately 122 miles (196 km)
San_Luis_Valley
Mountain range of the Southern Rocky Mountains of North America
million years ago, the Front Range began to rise again due to the Laramide Orogeny in the western half of the state, draining from being at the bottom of
Front_Range
North American region east of the range
heavily deformed by faulting, folding, and overthrusting. During the Sevier orogeny mountain-building event about 115 and 55 million years ago, what is known
Rocky_Mountain_Front
Rock formation in the western United States
to Alberta and Saskatchewan in the north, was formed during the Nevadan orogeny, a precursor event to later orogenic episodes that created the Rocky Mountains
Morrison_Formation
Mountain range in Arizona and New Mexico, US
years ago). If so, then major uplift of the central Colorado Plateau may postdate the Laramide orogeny. Minette of the Navajo Volcanic Field intruded and
Chuska_Mountains
Rock formations near Boulder, Colorado, US
present orientation between 80 and 35 million years ago, during the Laramide Orogeny. The Flatirons were subsequently exposed by erosion. Other manifestations
The_Flatirons
Continental rift zone in the southwest United States
separates the Colorado Plateau in the west from the interior of the North American craton on the east. The rift extends from central Colorado in the north
Rio_Grande_rift
Hypothetical Neoproterozoic supercontinent
[failed verification] Examples are the Grenville orogeny in North America and the Dalslandian orogeny in Europe. Since then, many alternative reconstructions
Rodinia
Mountain, highest point in Tennessee, United States
tectonism during the Taconic orogeny. Later, Devonian-Mississippian metamorphism of these strata occurred during the Acadian orogeny and additional Pennsylvanian
Kuwohi
River basin in southwestern Wyoming, United States
deposits. The GGRB is host to many anticlines created during the Laramide Orogeny trapping many of its hydrocarbon resources. It is bounded by the Rawlins
Greater_Green_River_Basin
Geologic feature in Utah, United States
Utah, United States. The geologic structure, formed during the Laramide orogeny, is a south-southeast trending fold in which the east side is dropped relative
Waterpocket_Fold
Geologic structural basin in eastern Utah, US
(also known as the Uintah Basin) is a physiographic section of the larger Colorado Plateaus province, which in turn is part of the larger Intermontane Plateaus
Uinta_Basin
Prehistoric inland sea that split the continent of North America
the west coast of the Americas had commenced, resulting in the Laramide orogeny, the early phase of growth of the modern Rocky Mountains. The Western Interior
Western_Interior_Seaway
Fifth period of the Paleozoic Era
Variscan-Alleghanian-Ouachita orogeny. Today their remains stretch over 10,000 km from the Gulf of Mexico in the west to Turkey in the east. The orogeny was caused by
Carboniferous
Geographic area containing several geologically related mountains
structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most
Mountain_range
Common high-grade metamorphic rock
Whitney, D.L.; Teyssier, C.; Siddoway, C.S. (eds.). Gneiss domes in orogeny: Boulder, Colorado, Geological Society of America Special Paper 380. Retrieved 5
Gneiss
Geological process at tectonic plate boundaries
ridge. The Laramide Orogeny in the Rocky Mountains of the United States is attributed to flat-slab subduction. During this orogeny, a broad volcanic gap
Subduction
Highest mountain in North Carolina, United States
These metasedimentary rocks were later uplifted during the Alleghenian orogeny. The soils are well drained, dark brown and stony with fine-earth material
Mount_Mitchell
National park in Utah, United States
Laramide orogeny started to uplift the Rocky Mountains 70 million years ago and with it, the Canyonlands region. Erosion intensified and when the Colorado River
Canyonlands_National_Park
Mountain range in Wyoming and Colorado, United States
eastern Wyoming. The mountains in turn give their name to the Laramide orogeny, the uplift of the North American Plate approximately 70 million years
Laramie_Mountains
Geologic formation in the United States
uplift of the Rocky Mountains (late Cretaceous Sevier orogeny and the Paleogene Laramide orogeny). Tectonic highlands supplied the Eocene sedimentary basins
Green_River_Formation
Structural basin in the Southwestern United States
Gondwana and Laurentia resulted in the Alleghanian and Ouachita orogenies. The Alleghanian Orogeny was the collision of Africa with the current-day southeastern
San_Juan_Basin
Mountain in Gunnison County, Colorado, United States
mountain is located in Gunnison County, Colorado, and in the Gunnison National Forest. During the Laramide Orogeny the area near Fairview Peak was lifted
Fairview Peak (Gunnison County, Colorado)
Fairview_Peak_(Gunnison_County,_Colorado)
Mountain in Larimer County, Colorado, United States
formed as sedimentary rock was uplifted and folded during the Laramide orogeny. The mountain itself is on property owned by the Bureau of Land Management
Goat Hill (Larimer County, Colorado)
Goat_Hill_(Larimer_County,_Colorado)
Geologic feature in California and Arizona
of mountain ranges of California List of mountain ranges of the Lower Colorado River Valley Spencer, Jon; Reynolds, S. J. (1990). "Relationship between
Maria_fold_and_thrust_belt
Mountain range in Utah and Colorado in the United States
uplift of the mountain range. The uplift of the range dates to the Laramide orogeny, about 70 to 50 million years ago, when compressive forces produced high-angle
Uinta_Mountains
From 1.75 to 1.65 billion years ago, Utah was impacted by the Mazatzal orogeny. Thick sequences of sedimentary rock from the Neoproterozoic, including
Geology_of_Utah
Summit in Capitol Reef National Park, Utah, USA
during the Laramide Orogeny. Ferns Nipple from west Ferns Nipple from west Ferns Nipple in the distance Mountains portal Colorado Plateau Geology of the
Ferns_Nipple
Landform in Utah and Arizona, United States
Laramide orogeny, which has increased the ability of the Colorado River to cut its channel to make individual plateaus out of the Colorado Plateaus region
Grand_Staircase
Geological formation in Colorado, United States
Laramide orogeny, that eventually formed the Rocky Mountains and raised Pikes Peak to its current height. Pikes Peak, like other portions of Colorado Rockies
Pikes_Peak_granite
Geological formation in the American state of Utah
which formed between 50 and 70 million years ago during the Laramide Orogeny. South aspect North aspect Looking WNW at Chimney Rock, Hwy 24, and trailhead
Chimney Rock (Capitol Reef National Park)
Chimney_Rock_(Capitol_Reef_National_Park)
(Jurassic to Cenozoic Periods). The last mountain building event, the Laramide orogeny, (about 70-40 million years ago) the last of the three episodes, is responsible
Geology_of_the_United_States
Mesozoic–Cenozoic plateau in North America
Nevadaplano probably formed as part of either the Sevier or the Laramide Orogeny during the Mesozoic and persisted into the Paleogene. Its growth began
Nevadaplano
Sub-range of the Rocky Mountains in the western United States
high country views. The Wasatch Range's origins are rooted in the Sevier Orogeny. As the Farallon plate subducted under the North American plate between
Wasatch_Range
(1980). "Summary of Laramide orogeny in Colorado" (PDF). Rocky Mountain Association of Geologists 1980 Symposium. Colorado Geological Survey. Retrieved
White_River_Plateau
Mountain range in the Western United States
northern Colorado into southern Wyoming. The northern extent of this range is the sub-range the Snowy Range. From the northern end of Colorado's Never Summer
Medicine_Bow_Mountains
Ridge in Colorado, United States
Mesaverde Formation. The ridge formed towards the end of the Laramide orogeny during the middle to late Eocene. "Grand Hogback". Geographic Names Information
Grand_Hogback
Geologic dome in Texas, United States
resulting mountain formation, globally called the Grenville orogeny, and locally called the Llano Orogeny, tectonically shoved and interleaved together these
Llano_Uplift
Mountain range in South Dakota and Wyoming, United States
the Black Hills was emplaced by magma generated during the Trans-Hudson orogeny and contains abundant pegmatite. The core of the Black Hills has been dated
Black_Hills
Marble from Colorado
the result of regional metamorphism, a process more associated with the orogeny and erosion of mountain ranges on a regional scale. Geologists still debate
Yule_Marble
Country in South Asia
up in sheets (or nappes) ahead of the subduction zone. This created the orogeny, or process of mountain building, of the Himalayas. The middle and stiffer
India
Mountain monument under construction in South Dakota
midcrustal Proterozoic and Archean metapelites during the Trans-Hudson orogeny and dated to 1.715 ± 0.003Ga from U-Pb and Th-Pb monazite dating. The leucogranite
Crazy_Horse_Memorial
Protected area in southwestern Colorado, US
The Weminuche Wilderness is a wilderness area in southwest Colorado managed by the United States Forest Service as part of the San Juan National Forest
Weminuche_Wilderness
National monument in the United States
sedimentary geologic formation outcropping around Florissant, Teller County, Colorado. The formation is noted for the abundant and exceptionally preserved insect
Florissant_Formation
associated with the Grenville orogeny. During the Proterozoic terranes were accreted onto the province. During the Taconic orogeny 445 to 435 million years
Geology_of_North_America
Major river in central United States
Montana at the headwaters of the Missouri River first rose in the Laramide Orogeny, a mountain-building episode that occurred from around 70 to 45 million
Missouri_River
Geologic uplift of Earth's surface that is attributed to plate tectonics
lithosphere bends under the action of forces such as the weight of a growing orogeny or changes in ice thickness related to glaciation. The lithosphere rests
Tectonic_uplift
Granitic rock
complex (Grenville orogeny of Proterozoic age), the Paleozoic Appalachian orogeny in Maine, and the currently active Himalayan orogeny. The leucogranite
Leucogranite
Sedimentary rock exposure in Colorado and Utah, U.S.
Basin. Uplift and folding associated with the later stages of the Laramide Orogeny subsequently tilted them into a nearly vertical position. Raven Ridge is
Raven_Ridge
Group of mountain ranges
Earth's lithosphere (crust and uppermost mantle). For example, the Laramide orogeny changed the topography of the central Rocky Mountains and adjoining Laramide
North_American_Cordillera
Summit in Utah, United States
which formed between 50 and 70 million years ago during the Laramide Orogeny. Spring and fall are the most favorable seasons to visit Navajo Dome. According
Navajo_Dome
Mountain range in Argentina
of arms of La Rioja Province. Famatina Department, La Rioja Famatinian orogeny Reicheocactus famatimensis (Speg.) Schlumpb. 29°00′52″S 67°47′58″W / 29
Sierra_de_Famatina
together with the Superior Craton and Hearne Craton during the Trans-Hudson Orogeny. The Wyoming Craton was a separate continent until it joined the proto-North
Geology_of_Wyoming
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