Process

Orogeny

oh-ROJ-uh-nee
Also Known As Mountain Building
Geology

The building of mountain belts where converging plates crumple, thicken and uplift the crust. The Himalaya, still rising as India drives into Asia, the Alps, and the ancient worn-down Appalachians each record an orogeny, and reading deformed rock for the mountain belts it once belonged to is one of geology's oldest skills. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Timescale
Tens of millions of years for a major mountain belt 1
Driving Force
The collision of tectonic plates, principally continent-continent or continent-arc collision, which thickens and deforms the crust. 1
Resulting Feature
An orogenic belt: one or more mountain ranges formed as the compressed plate crumples and is uplifted. 1
Significance
Orogeny builds the world's major mountain ranges and is a principal way geologists identify ancient plate boundaries now buried deep within continental interiors. 1
Driving Force
Driving Force (category)
Tectonic 1
Timescale
Timescale (category)
Years to Decades 1
Orogeny
Filter Results2 entries
Connections

Associated With

Folding, Processes

A fold belt is a common feature of orogenic zones.

Source Fold, Geology (Wikipedia)

Caused By

Mountain belts rise where converging plates collide or subduct.

Source Orogeny (Wikipedia)

Causes

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Lassen Peak
Source Laurentia (Wikipedia)

Wikidata P31 (Q1479638) mapped to formative process Orogeny via earth5 extended reviewed judgment map; source citation is this entity's own cited Wikidata item.

Source Wikidata: Lewis Overthrust

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Liathach

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Liberty Cap

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mahagnao Volcano

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Malubiting

Wikidata P31 (Q9381142) mapped to formative process Orogeny via earth5 extended reviewed judgment map; source citation is this entity's own cited Wikidata item.

Source Wikidata: Malvern Hills

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Masherbrum

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Matobo Hills
Source Wikipedia: McMurdo Dry Valleys, Wikipedia

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mont Megantic

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Monte Pissis

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Moro Rock

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Agamenticus

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Ascutney

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Asgard

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Banahaw

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Berlin

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Bisoke

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Buffalo

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Cameroon

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Chiperone

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Conner

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Cooroora

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Danxia

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Discovery

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Elgon

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Erongo

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Fentale

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Guiting-Guiting

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Halcon

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Hombori

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Iriga

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Isarog

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Jianglang

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Kadam

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Kailash

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Karisimbi

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Kenya

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Kilimanjaro

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Kinabalu

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Kirkpatrick

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Kitanglad

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Kulal

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Langshan

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Ledang

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Mount Lico

Showing 101 to 150 of 247 in Causes, page 3 of 5.

In Discipline

Geology, Disciplines
Source Orogeny (Wikipedia)
Sources
1. Orogeny (Wikipedia)
Wikimedia Foundation
  • Introduction
    An orogenic belt or orogen develops as the compressed plate crumples and is uplifted to form one or more mountain ranges.
  • Introduction, definition sentence
    is a mountain-building process that takes place at a convergent plate margin when plate motion compresses the margin.
View the Source
Jura Mountains (Wikipedia)
Causes: Jura Mountains, Article text
Quote, Causes: Jura Mountains, Article text
This deformation accommodates the compression from alpine folding as the main Alpine orogenic front moves roughly northwards.
View the Source
Stone Mountain (Wikipedia)
Causes: Stone Mountain, Geology
Quote, Causes: Stone Mountain, Geology
The granite intruded into the metamorphic rocks of the Piedmont region during the last stages of the Alleghenian Orogeny
View the Source
Caledonian orogeny (Wikipedia)
  • Causes: Caledonian Orogeny, Lead, process Orogeny
    The Caledonian orogeny encompasses events that occurred from the Ordovician to Early Devonian, roughly 490-390 million years ago (Ma).
  • Causes: Caledonian Orogeny, Lead paragraph
    The Caledonian orogeny was a mountain-building cycle recorded in the northern parts of the British Isles, the Scandinavian Caledonides, Svalbard, eastern Greenland and parts of north-central Europe
View the Source
Carpathian Mountains (Wikipedia)
Causes: Carpathian Mountains, Article text, process Orogeny
Quote, Causes: Carpathian Mountains, Article text, process Orogeny
The Carpathian mountains were formed during the Alpine orogeny in the Mesozoic and Cenozoic by moving the ALCAPA (Alpine-Carpathian-Pannonian), Tisza and Dacia plates over subducting oceanic crust.
View the Source
Chicamocha Canyon (Wikipedia)
Causes: Chicamocha Canyon, Lead, process Orogeny
Quote, Causes: Chicamocha Canyon, Lead, process Orogeny
The Chicamocha Canyon started forming in the Early Oligocene, when Colombia was undergoing a tectonically active phase of the Andean orogeny.
View the Source
Ellsworth Mountains (Wikipedia)
Causes: Ellsworth Mountains, Article text, process Orogeny
Quote, Causes: Ellsworth Mountains, Article text, process Orogeny
Liptak Formation of quartzites, and the Mount Wyatt Earp Formation of quartzites. Major deformation of the sedimentary rocks occurred during the Gondwanide orogeny, followed by later uplift.
View the Source
Gawler Craton (Wikipedia)
Causes: Gawler Craton, Lead, process Orogeny
Quote, Causes: Gawler Craton, Lead, process Orogeny
Prior to 1550 Ma the craton comprised a number of active Proterozoic orogenic belts extending back in time to at least 2450 Ma.
View the Source
Great Glen Fault (Wikipedia)
Causes: Great Glen Fault, Article text, process Orogeny
Quote, Causes: Great Glen Fault, Article text, process Orogeny
It formed towards the end of the Caledonian orogeny associated with the collision between the Laurentia and Baltic tectonic plates at the end of the Silurian continuing into the Early Devonian (likely age range 430-390 Ma (million years)).
View the Source
Laurentia (Wikipedia)
Causes: Laurentia, Lead, process Orogeny
Quote, Causes: Laurentia, Lead, process Orogeny
During other times in its past, Laurentia has been part of larger continents and supercontinents and consists of many smaller terranes assembled on a network of early Proterozoic orogenic belts.
View the Source
Wikipedia: McMurdo Dry Valleys, Wikipedia
Causes: McMurdo Dry Valleys, Article text, process Orogeny
Quote, Causes: McMurdo Dry Valleys, Article text, process Orogeny
The Palaeozoic Granite Harbour intrusives include granitoid plutons and dykes, which intruded into the metasedimentary Skelton Group in the Late Cambrian-Early Ordovician during the Ross orogeny.
View the Source
Mount Roraima (Wikipedia)
Causes: Mount Roraima, Article text, process Orogeny
Quote, Causes: Mount Roraima, Article text, process Orogeny
These rocks sit on a granite and gneiss base and were originally covered by layers of Mesozoic clay, conglomerate, and diorite, but have been exposed by erosion and by orogeny over the past 180 million years, eroded by precipitation to form strange shapes.
View the Source
San Rafael Swell (Wikipedia)
Causes: San Rafael Swell, Lead, process Orogeny
Quote, Causes: San Rafael Swell, Lead, process Orogeny
Measuring approximately 75 by 40 miles (121 by 64 km), the swell consists of a giant dome-shaped anticline of sandstone, shale, and limestone that was pushed up during the Paleocene Laramide Orogeny 40-60 million years ago.
View the Source
São Francisco Craton (Wikipedia)
Causes: São Francisco Craton, Lead, process Orogeny
Quote, Causes: São Francisco Craton, Lead, process Orogeny
The Paleoproterozoic (about 2.5 to 2.0 Ga) was the source of orogenic belts and the current configuration of the craton.
View the Source
Shetland (Wikipedia)
Causes: Shetland, Article text, process Orogeny
Quote, Causes: Shetland, Article text, process Orogeny
These islands are the northern outpost of the Caledonian orogeny, and there are outcrops of Lewisian, Dalradian and Moine metamorphic rocks with histories similar to their equivalents on the Scottish mainland.
View the Source
Illimani (Wikipedia)
Causes: Illimani, Lead paragraph
Quote, Causes: Illimani, Lead paragraph
Its formation results from the ancient folding associated with the Andean orogeny, as with the majority of the neighboring mountains in the cordillera
View the Source
Muddus plains (Wikipedia)
Causes: Muddus Plains, Lead paragraph
Quote, Causes: Muddus Plains, Lead paragraph
The plains formed in connection to the uplift of the northern Scandinavian Mountains in the Paleogene
View the Source
Vasquez Rocks (Wikipedia)
Causes: Vasquez Rocks, Lead section (caused-by Orogeny)
Quote, Causes: Vasquez Rocks, Lead section (caused-by Orogeny)
It is known for its rock formations, the result of sedimentary layering and later tectonic uplift.
View the Source
Trans-Hudson orogeny (Wikipedia)
Causes: Trans-Hudson Orogen, Lead, process Orogeny
Quote, Causes: Trans-Hudson Orogen, Lead, process Orogeny
The Trans-Hudson orogeny or Trans-Hudsonian orogeny was the major mountain building event (orogeny) that formed the Precambrian Canadian Shield and the North American Craton (also called Laurentia), forging the initial North American continent.
View the Source
Mountain chain (Wikipedia)
Causes: Mountain chain, Lead sentence
Quote, Causes: Mountain chain, Lead sentence
Elongated mountain chains occur most frequently in the orogeny of fold mountains, (that are folded by lateral pressure), and nappe belts (where a sheetlike body of rock has been pushed over another rock mass).
View the Source
Hill chain (Wikipedia)
Causes: Hill chain, Lead sentence
Quote, Causes: Hill chain, Lead sentence
The chain-like arrangement of hills in a chain is a consequence of their collective formation by mountain building forces or ice age earth movements.
View the Source
Chink (geology) (Wikipedia)
Causes: Chink (geology), Lead sentence
Quote, Causes: Chink (geology), Lead sentence
Chinks may also result from tectonic uplifts.
View the Source
Piedmonttreppen (Wikipedia)
Causes: Piedmonttreppen, Lead sentence
Quote, Causes: Piedmonttreppen, Lead sentence
A piedmonttreppen or piedmont benchland is a conceived landform consisting in a succession of benches at different heights and that forms in sequence during the uplift of a geological dome.
View the Source
Central Valley (California) (Wikipedia)
Causes: Central Valley (California), Article text
Quote, Causes: Central Valley (California), Article text
The valley was enclosed by the uplift of the Coast Ranges, with its original outlet into Monterey Bay.
View the Source
Spiti (Wikipedia)
Causes: Spiti, Article text
Quote, Causes: Spiti, Article text
Over millennia, the Spiti River and its tributaries such as the Pin River, have cut deep gorges in the uplifted sedimentary strata.
View the Source
Fort Valley (Virginia) (Wikipedia)
Causes: Fort Valley (Virginia), Article text
Quote, Causes: Fort Valley (Virginia), Article text
The Fort Valley and Massanutten mountain range is the result of the Alleghanian Orogeny, the geologic process where a continental plate crumples and is pushed upwards to form mountain ranges.
View the Source
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