noun[mass noun] Geology
Layering within a stratum and at an angle to the main bedding plane.
- Lower Cretaceous tides revealed by cross-bedding with mud drapes.
- Intra-sedimentary faults, palaeochannels, and cross-bedding in sandstones and conglomerates are locally abundant.
- Intervals of siltstone and fine sandstone show climbing ripple lamination and low-angle cross-bedding.
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