Willis Mountain is a narrow ridge of kyanite quartzite in Buckingham County, Virginia, about two miles long with steep rocky slopes rising some 150 meters above the adjacent valley to an elevation of 353 meters. The ridge originated as volcanic and volcanic-derived sediment that was hydrothermally altered by acidic fluids and then metamorphosed under high pressure and temperature into a rock unusually rich in kyanite, a mineral resistant enough to weathering that the ridge stands well above the surrounding, less resistant metamorphic terrain, its exposed rock characteristically etched with pits and furrows. Willis Mountain holds the largest of the region's kyanite deposits and has been mined since 1957.
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Source Willis Mountain (Wikipedia)
Source Willis Mountain (Wikipedia)
Source Willis Mountain (Wikipedia)
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Source Willis Mountain (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: Willis Mountain
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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: Willis Mountain
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Source Wikidata: Willis Mountain
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Wikidata: Willis Mountain
Wikidata Q2805142, class allow-list match (w-wdresolver-0926)View the Source Willis Mountain (Wikipedia)
Associated With: Quartzite, Lead paragraph
Willis Mountain is well known as the site of a large deposit of kyanite quartzite that has been actively mined for kyanite for decades.
Associated With: Quartzite, Article text, rock Quartzite
The kyanite quartzite and associated schist and gneiss consist of volcaniclastic sediments and volcanic rocks that have been altered by amphibolite grade metamorphism under pressure as high as 6.5 kb and temperatures as high as 600 °C.
Associated With: Schist, Article text, rock Schist
The kyanite quartzite and associated schist and gneiss consist of volcaniclastic sediments and volcanic rocks that have been altered by amphibolite grade metamorphism under pressure as high as 6.5 kb and temperatures as high as 600 °C.
Associated With: Gneiss, Article text, rock Gneiss
The kyanite quartzite and associated schist and gneiss consist of volcaniclastic sediments and volcanic rocks that have been altered by amphibolite grade metamorphism under pressure as high as 6.5 kb and temperatures as high as 600 °C.
Associated With: Cambrian, Article text, age Cambrian
The schists are enveloped by biotite-amphibole gneiss of the Cambrian Chopawamsic Formation.
Caused By: Metamorphism, Article text, process Metamorphism
The kyanite quartzite and associated schist and gneiss consist of volcaniclastic sediments and volcanic rocks that have been altered by amphibolite grade metamorphism under pressure as high as 6.5 kb and temperatures as high as 600 °C.
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