Bedrock type determines size of river meanders, impacting landscape diversity.
Bedrock meanders in the Appalachian Valley and Ridge province vary in size due to differences in the type of rock they are formed in. Meanders in shaly rocks are larger than those in non-shaly rocks. Other factors don't explain these size differences. Meanders in shaly rocks are about twice as long and have wider valley floors compared to meanders in non-shaly rocks. In plateau regions, meander shapes can change as erosion happens, leading to unusual relationships between meander size and rock type.