Conglomerate (geology)
Appearance
![](http://upload.wikimedia.org/wikipedia/commons/thumb/9/99/Carmelo_Formation_at_Point_Lobos.jpg/200px-Carmelo_Formation_at_Point_Lobos.jpg)
![](http://upload.wikimedia.org/wikipedia/commons/thumb/0/0b/Puddingstone_outcrop_on_Coppet_Hill_-_geograph.org.uk_-_465829.jpg/230px-Puddingstone_outcrop_on_Coppet_Hill_-_geograph.org.uk_-_465829.jpg)
A conglomerate is a rock consisting of individual clasts within a finer-grained matrix that have become cemented together.
Conglomerates are sedimentary rocks consisting of rounded fragments and are thus differentiated from breccias, which consist of angular clasts.[1] Both conglomerates and breccias have clasts larger than sand (>2 mm).
References
[change | change source]- ↑ "Conglomerate Rocks." Conglomerate Rocks on Rock Hound. Archived 2010-07-26 at the Wayback Machine Rock Hounds. Retrieved on July 29, 2007.