A general term for any non-consolidated, clast-rich material that consists of >50% primary particles with diameters of 4-63 μm (American geologists), 2-63 μm (European geologists), or 2-50 μm (American soil scientists).
See siltstone
A general term for any non-consolidated, clast-rich material that consists of >50% primary particles with diameters of 4-63 μm (American geologists), 2-63 μm (European geologists), or 2-50 μm (American soil scientists).
See siltstone