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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 Results5 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: Ritigala

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: Roque Nublo

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: Ruwenzori Mountains

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: Salkantay

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: San Rafael Swell

Wikidata P31 (Q1437459) mapped to formative process Orogeny via earth5 extended reviewed judgment map; source citation is this entity's own cited Wikidata item.

Source Wikidata: Scandinavian Mountains

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: Sia Kangri

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: Sierra Nevada de Santa Marta

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: Simien Mountains

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: Sivalik 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: Skil Brum

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: Slover Mountain
Source Spiti (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: Stac Pollaidh

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: Suilven

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: Taka Mountains

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: Tendaguru Formation

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: The Hazards

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: Thicketty Mountain

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: Þórisjökull

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: Tian Shan
Source Trans-Hudson orogeny (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: Trivor

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: Ultar Sar

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: Ulvetanna

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: Ural Mountains
Source Vasquez Rocks (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: Vingerklip

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: Virunga Mountains

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: Wase 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: Waterfall

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: Willis Mountain

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: Yerupaja

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: You Yangs

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: Zagros Mountains

Showing 201 to 238 of 238 in Causes, page 5 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
Caledonian orogeny (Wikipedia)
Causes: Caledonian Orogeny, Lead paragraph
Quote, 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
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
Quote, Causes: Trans-Hudson Orogen, Lead
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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