Granule (geology)

In this article, we will explore the fascinating world of Granule (geology) and all the implications this topic has in today's environment. From its history to its impact on society, through its different perspectives and applications, we will analyze in depth all the relevant aspects of Granule (geology). In addition, we will delve into the latest research and discoveries on this topic, as well as the opinions of experts on the subject. Without a doubt, Granule (geology) is an exciting and constantly evolving topic, so this article aims to be a guide to better understand its importance and meaning today.

A granule is a clast of rock with a particle size of 2 to 4 millimetres based on the 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.

See also

References

  1. ^ Folk, R.L. (1980) The Petrology of Sedimentary Rocks. Austin, Texas, Hemphill Publishing Company. 182 pp. ISBN 0-914696-14-9