Kinzers Formation
The Kinzers Formation is a geologic formation in Pennsylvania. It preserves fossils dating back to the Cambrian Period. The base of the Kinzers Formation is primarily a dark-brown shale. The middle is a gray and white spotted limestone and, locally, marble having irregular partings. The top is a sandy limestone which weathers to a fine-grained, friable, porous, sandy mass. Type section. Named from exposures at a railroad cut at Kinzers, Lancaster County, Pennsylvania. Other outcrops. The Kinzers overlies the Vintage Dolomite at the type section of the Vintage at a railroad cut at Vintage, Pennsylvania. High  quality fossil specimens ("Lagerstätte") were obtained from the Noah Getz Quarry, one mile north of Rohrerstown, Pennsylvania, but the quarry location is overgrown and disturbed by development. The fossils are from the Emigsville Member, and include the trilobite "Olenellus thompsoni", the arthropod "Anomalocaris pennsylvanica", the bivalve "Tuzoia getzi", and the green algae "Margaretia dorus".