Sedimentary rock deposited by turbidity currents in deep marine environments. Shows characteristic graded bedding Bouma sequence . Texture: Graded bedding. Rock type: Sedimentary Clastic. Grain size: Graded coarse at base to fine at top. Minerals present: Quartz, Feldspar, Clay minerals, Rock fragments. Formation: Deposited by submarine turbidity currents that flow down continental slopes into deep basins. Common geological settings: Found in flysch sequences worldwide; Alps, Appalachians, deep-sea fans. Common look-alikes and related entries: Greywacke, Sandstone, Siltstone.
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GeoMiner
Last updated
2026-03-30T14:39:17.16885+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.
Sedimentary rock deposited by turbidity currents in deep marine environments. Shows characteristic graded bedding Bouma sequence .
How can you identify Turbidite?
Compare several properties rather than relying on colour alone. This entry records rock type: Sedimentary Clastic; texture: Graded bedding; grain size: Graded coarse at base to fine at top; common minerals: Quartz, Feldspar, Clay minerals, Rock fragments. Confirm an important identification with additional field tests or qualified laboratory work.
How does Turbidite form?
Deposited by submarine turbidity currents that flow down continental slopes into deep basins.
Where is Turbidite commonly found?
Found in flysch sequences worldwide; Alps, Appalachians, deep-sea fans.
What is Turbidite commonly confused with?
Turbidite may be confused with Greywacke, Sandstone, Siltstone. Compare multiple diagnostic properties because colour and surface appearance can overlap.
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