Conglomerates and sandstones representing bars deposited in the channel of a braided river. Note the lenticular bed geometry. The northward dip (to the left) is a result of folding during Pyrenean earth movements. | |
image credit: Roger Suthren. Paleocene, Albas, Corbières, S France |
sedshots
-- images of sediments and sedimentary rocks at virtual-geology.info
This page is maintained
by Roger Suthren. Last
updated
23 January, 2004 10:22