Stylolite
From Wikipedia, the free encyclopedia
A stylolite is a fracture in limestone rocks, caused by dissolution from groundwater flow. Sylolites appear as jagged discontinuities in outcrops and hand samples; often cutting through fossils.
A stylolite is a fracture in limestone rocks, caused by dissolution from groundwater flow. Sylolites appear as jagged discontinuities in outcrops and hand samples; often cutting through fossils.