The cast of Glacial Erratics - 2013 includes: Jon Levenson as Mr. Pierre Frances Mitchell as Principal Robyn Rikoon as Isabel Clarell
The debris of boulders eroded and carried down by glaciers will eventually form moraines (mounds) where the front of the glacier melts and retreats, leaving the debris behind. Moraines can be high and wide enough to form a dam, behind which glacial melt water is trapped and lakes are formed.
Erratics and drumlins are both types of geological formations associated with glacial activity. Erratics are large boulders transported and deposited by glaciers, often found in areas where the surrounding rock is different from the rock type of the erratic. Drumlins, on the other hand, are elongated hills formed from glacial till that has been shaped by the movement of ice. Both features provide evidence of past glacial movements and help in understanding the dynamics of glacial landscapes.
Erratic blocks or "erratics" for short.
Glacial deposits or glacial drift refer to all sediments of glacial origin. These deposits include materials such as till, moraines, outwash plains, and glacial erratics that are left behind by the movement of glaciers.
Erratics are distinctive because they are large boulders or rocks that have been transported and deposited by glacial ice, often far from their source location. Unlike other glacial features, such as moraines or drumlins, erratics can be composed of rock types that are not found in the surrounding area, highlighting their unique origin. Their irregular shapes and sizes also set them apart from more uniform glacial deposits. Additionally, erratics are often found in contrasting geological contexts, making them notable landmarks in the landscape.
On the rocks
Rocks that have been transported from their place of formation are known as erratics (these commonly occur in areas where glaciation has occurred and so are known as glacial erratics).
They are called glacial erratics if they are different from the local surrounding rocks.
Glacial erratics are mostly located in areas that were covered by glaciers during the last Ice Age, such as northern latitudes and high mountain regions. They can be found in places like Canada, Scandinavia, and parts of the United States where glaciers deposited large rocks as they receded.
Yes, there are glacial erratics and boulders in Georgia. These large rocks were transported by glaciers during the last Ice Age and are now found in various parts of the state, particularly in the northern regions. They serve as evidence of the region's glacial history.
Boulders that have been carried by a glacier have a couple names, but most commonly they are referred to as glacial boulders or erratics. If you're interested in learning more about glacial boulders, the Iowa Department of Natural Resources has a pretty good article about them; as Iowa and most of the American Midwest were covered by glaciers during the last Ice Age, glacial boulders are fairly common there. http://www.igsb.uiowa.edu/browse/boulders/boulders.htm