The Glacial till plains are a till plain landform in Northern Ohio, located near the shore of Lake Erie and produced by the retreat of the Wisconsin glaciation...

and northern Ohio (see Glacial till plains (Ohio)). Till plains are large flat or gently sloping areas of land on which glacial till has been deposited...

bordered on the west by glacial till plains in the north, generally north of the Ohio River, and the Bluegrass Region south of the Ohio River. Elevations vary...

rock scouring and scratching, glacial moraines, drumlins, valley cutting, and the deposition of till or tillites and glacial erratics. Successive glaciations...

the last glacial maximum, also known as the Late Wisconsin in North America. This glaciation radically altered the geography north of the Ohio River, including...

A glacial erratic is a glacially deposited rock differing from the type of rock native to the area in which it rests. Erratics, which take their name from...

glacier melts or partially retreats. Fluvio-glacial landforms and erosional surfaces include: outwash plains, kames, kame terraces, kettle holes, eskers...

rock and soil were scraped from the glacial centers to its margins by slowly moving ice and redeposited as drift or till. Much of this drift was dumped into...

glacial outwash. Glacial outwash is generated when streams of meltwater flow away from the glacier and deposit sediment to form broad outwash plains called...

of the till plains, they determine the course of many streams and rivers, which as a whole are consequent upon the surface form of the glacial deposits...