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Mountain formation

Mountain formation occurs due to a variety of geological processes associated with large-scale movements of Earth's crust (tectonic plates). Folding, faulting, volcanic activity, igneous intrusion and metamorphism can all be parts of the orogenic process of mountain building. The formation of mountains is not necessarily related to the geological…

Art, Types of mountains & Models

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Types of mountains

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Mountain formation

Nodes65
Edges64
Triples8
Avg. degree1.97
Density0.030769
Components1

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mountains mountain volcanoes plate volcanic tectonic movements crust formation block fold folding continental earth's plates passive margins blocks example associated

Entity relationships Subject–Predicate–Object triples

SubjectPredicateObjectConfidenceSrc
the Scandinavian Mountainsinstance ofa horst forming a massive anticline situated between the complex graben valleys of the Struma and Mesta rivers.Uplifted passive marginsUnlike orogenic mountains there is no wide…0.80text
eastern Greenlandinstance ofa horst forming a massive anticline situated between the complex graben valleys of the Struma and Mesta rivers.Uplifted passive marginsUnlike orogenic mountains there is no wide…0.80text
the Brazilian Highlandsinstance ofa horst forming a massive anticline situated between the complex graben valleys of the Struma and Mesta rivers.Uplifted passive marginsUnlike orogenic mountains there is no wide…0.80text
or Australia's Great Dividing Rangeinstance ofa horst forming a massive anticline situated between the complex graben valleys of the Struma and Mesta rivers.Uplifted passive marginsUnlike orogenic mountains there is no wide…0.80text
the Scandinavian Mountainsinstance ofUplifted passive marginsUnlike orogenic mountains there is no widely accepted geophysical model that explains elevated passive continental margins0.80text
eastern Greenlandinstance ofUplifted passive marginsUnlike orogenic mountains there is no widely accepted geophysical model that explains elevated passive continental margins0.80text
the Brazilian Highlandsinstance ofUplifted passive marginsUnlike orogenic mountains there is no widely accepted geophysical model that explains elevated passive continental margins0.80text
or Australia's Great Dividing Rangeinstance ofUplifted passive marginsUnlike orogenic mountains there is no widely accepted geophysical model that explains elevated passive continental margins0.80text

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