5 Enhancing Professional Development for Earth Science Teachers (Posters)
Monday, 14 March 2005
8:00 AM - 12:00 PM
SITES OF GEOLOGIC INTEREST IN THE MCKAY WILDLIFE PRESERVE AND NATURE TRAIL IN CALEDONIA, NEW YORK
Paper number: 5-14
Program: THEME SESSIONS
Time: 8:00 AM – 12:00 PM
Authors
Abstract
The Devonian Onondaga Formation is exposed in the park, which contains marine fossils, such as brachiopods, corals, and crinoids. Dark chert from the Onondaga, which was used by Native Americans for implements and projectile points, is also common. Glaciation and karst are the erosional processes that have formed the modern landscape. Glacial erratics exist throughout the park, and originated in the Canadian Shield and western New York State. These erratics are commonly gneiss, granite, and sandstones. Additionally, glacial polishing is evident along the Onondaga bedrock. Several mushroom-shaped boulders and a large sinkhole indicate the presence of karst.