Granule (geology)
A granule is a
Krumbein phi scale of sedimentology. Granules are generally considered to be larger than sand (0.0625 to 2 millimetres diameter) and smaller than pebbles (4 to 64 millimetres diameter). A rock made predominantly of granules is termed a granule conglomerate.[1]
See also
- Gravel
- Particle size (grain size)
References
- ISBN 0-914696-14-9