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Skarn identification and geology

Skarn rock reference specimen

Coarse-grained metamorphic rock formed by metasomatic replacement at the contact between igneous intrusions and carbonate rocks. Texture: Coarse-grained, variable. Rock type: Metamorphic Contact/Metasomatic. Grain size: Coarse. Parent rock: Limestone/Dolostone. Minerals present: Garnet grossular/andradite, Pyroxene diopside, Epidote, Wollastonite, Vesuvianite. Formation: Forms at intrusion-carbonate contacts where hot fluids cause metasomatic exchange, creating calc-silicate minerals. Common geological settings: Worldwide; major ore deposits Cu, Fe, W, Sn, Mo form in skarn environments. Common look-alikes and related entries: Marble, Hornfels, Calc-silicate rock.

Sources, scope & corrections

These authoritative resources support category-level nomenclature, terminology, identification methods, and safety. When a specimen-specific safety warning appears, the public-health source listed here directly supports that precaution. They are not line-by-line citations for every other property on this entry, and natural specimens vary.

Editorial owner
GeoMiner
Last updated
2026-03-30T14:39:10.705332+00:00
Review status
Published; not independently peer-reviewed
  • Rocks — U.S. National Park Service. Authoritative overview of rock groups, the rock cycle, and geologic processes.
  • Can you identify my rock or mineral? — U.S. Geological Survey. Identification limitations and routes to in-person professional verification.

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Common questions

What is Skarn?
Coarse-grained metamorphic rock formed by metasomatic replacement at the contact between igneous intrusions and carbonate rocks.
How can you identify Skarn?
Compare several properties rather than relying on colour alone. This entry records rock type: Metamorphic Contact/Metasomatic; texture: Coarse-grained, variable; grain size: Coarse; common minerals: Garnet grossular/andradite, Pyroxene diopside, Epidote, Wollastonite, Vesuvianite. Confirm an important identification with additional field tests or qualified laboratory work.
How does Skarn form?
Forms at intrusion-carbonate contacts where hot fluids cause metasomatic exchange, creating calc-silicate minerals.
Where is Skarn commonly found?
Worldwide; major ore deposits Cu, Fe, W, Sn, Mo form in skarn environments.
What is Skarn commonly confused with?
Skarn may be confused with Marble, Hornfels, Calc-silicate rock. Compare multiple diagnostic properties because colour and surface appearance can overlap.

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