Thick sequence of alternating sandstone/greywacke and shale deposited in deep marine foreland basins during mountain building. Texture: Interbedded coarse and fine. Rock type: Sedimentary Clastic. Grain size: Alternating sand and mud. Minerals present: Quartz, Feldspar, Clay minerals, Lithic fragments. Formation: Deposited by repeated turbidity currents in deep marine foreland basins during orogenic events. Common geological settings: Alps, Carpathians, Pyrenees, Appalachians; classic synorogenic sedimentary sequence. Common look-alikes and related entries: Turbidite, Greywacke, Molasse.
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
2026-03-30T14:39:38.828767+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.
Thick sequence of alternating sandstone/greywacke and shale deposited in deep marine foreland basins during mountain building.
How can you identify Flysch?
Compare several properties rather than relying on colour alone. This entry records rock type: Sedimentary Clastic; texture: Interbedded coarse and fine; grain size: Alternating sand and mud; common minerals: Quartz, Feldspar, Clay minerals, Lithic fragments. Confirm an important identification with additional field tests or qualified laboratory work.
How does Flysch form?
Deposited by repeated turbidity currents in deep marine foreland basins during orogenic events.