Granite domes are domical hills composed of granite with bare rock exposed over most of their surface; such domical features are generally known as bornhardts and can form in any plutonic rock, though they are typically granite or granitic gneiss. As granitic plutons cool kilometers below the surface, minerals crystallize under uniform confining pressure; as erosion brings the rock nearer the surface and the pressure above it decreases, the rock fractures along onion-like exfoliation joints parallel to the land surface, and under the right conditions these sheets of rock peel away to form a dome.
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Caused By
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: Granite Dome
In Discipline
Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Granite Dome
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Also in Geography Atlas: where this subject is found.
Source Wikidata: Granite Dome
Sources
Wikidata: Granite Dome
Wikidata Q49032693, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
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