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...

of Sec. 21, Township 20, Range 1, West 5th Meridian. Big Rock is a glacial erratic that is part of a 930 km (580 mi) long, narrow (1.00 to 22.05 km (0...

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

250 kilometres (150 miles) away in Wales, either through glaciation (glacial erratic theory) or through humans organizing their transportation. A summary...

period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology...

Glacial erratic boulders of Estonia are large boulders of rock which have been formed and moved into Estonia by glacial action during previous ice ages...

Pennsylvania, which was founded by Quaker settlers from Soulbury. A glacial erratic lies in a road in the parish. The stone originated in Derbyshire, and...

Trygław (IPA: [trɨg.wav]) is the largest glacial erratic in Poland and one of the largest in Europe. It is located in the town of Tychowo, in Gmina Tychowo...

The Last Glacial Maximum (LGM), also referred to as the Last Glacial Coldest Period, was the most recent time during the Last Glacial Period where ice...

are glacial erratics that lie upon a surficial blanket of Late Wisconsin glacial till. The largest glacial erratic within the Foothills Erratics Train...