Coarse pyroclastic rock composed of rounded volcanic bombs 64 mm in a finer tuff matrix. Texture: Pyroclastic, coarse. Rock type: Igneous Pyroclastic. Grain size: Very coarse bombs 64 mm. Minerals present: Volcanic bombs, Lapilli, Ash matrix. Formation: Forms near volcanic vents from accumulation of ejected volcanic bombs and blocks during explosive eruptions. Common geological settings: Found near volcanic vents worldwide; Hawaii, Stromboli, Cascades. Common look-alikes and related entries: Volcanic Breccia, Conglomerate, Tuff.
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GeoMiner
Last updated
2026-03-30T14:39:31.91563+00:00
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Published; not independently peer-reviewed
Rocks — U.S. National Park Service. Authoritative overview of rock groups, the rock cycle, and geologic processes.
Coarse pyroclastic rock composed of rounded volcanic bombs 64 mm in a finer tuff matrix.
How can you identify Agglomerate?
Compare several properties rather than relying on colour alone. This entry records rock type: Igneous Pyroclastic; texture: Pyroclastic, coarse; grain size: Very coarse bombs 64 mm; common minerals: Volcanic bombs, Lapilli, Ash matrix. Confirm an important identification with additional field tests or qualified laboratory work.
How does Agglomerate form?
Forms near volcanic vents from accumulation of ejected volcanic bombs and blocks during explosive eruptions.
Where is Agglomerate commonly found?
Found near volcanic vents worldwide; Hawaii, Stromboli, Cascades.
What is Agglomerate commonly confused with?
Agglomerate may be confused with Volcanic Breccia, Conglomerate, Tuff. Compare multiple diagnostic properties because colour and surface appearance can overlap.
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