Processes
Orogeny
oh-ROJ-uh-nee
Also Known As Mountain Building
Citation Formats
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BibTeX
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.
Facts
TimescaleTens of millions of years for a major mountain belt 1 Driving ForceThe collision of tectonic plates, principally continent-continent or continent-arc collision, which thickens and deforms the crust. 1 Resulting FeatureAn orogenic belt: one or more mountain ranges formed as the compressed plate crumples and is uplifted. 1 SignificanceOrogeny builds the world's major mountain ranges and is a principal way geologists identify ancient plate boundaries now buried deep within continental interiors. 1 Cross-Tradition Connections
Associated With
A fold belt is a common feature of orogenic zones.
Caused By
Mountain belts rise where converging plates collide or subduct.
In Discipline
Sources
1. Orogeny (Wikipedia)
Wikimedia FoundationIntroductionQuote, Introduction
An orogenic belt or orogen develops as the compressed plate crumples and is uplifted to form one or more mountain ranges.
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