most people say that its called a moraine or it can be respiration but people or just say i prefer to called it a MORAINE. BY HG ;]
most people say that its called a moraine or it can be respiration but people or just say i prefer to called it a MORAINE. BY HG ;]
A boulder left behind by a retreating glacier is known as an erratic. A glacier is a moving river of ice and snow.
The material left behind by a retreating glacier, including boulders, sand, clay, and silt, is known as moraine.
A kettle is typically formed by deposition, when a block of ice left behind by a retreating glacier eventually melts. This process creates a depression in the landscape.
Till, moraine, and kettle are examples of glacial landforms. Till refers to unsorted material deposited by a glacier, moraine is a landform composed of till deposited by a glacier, and a kettle is a depression formed by the melting of a block of ice left behind by a retreating glacier.
A kame is a geological feature which means an unusual shaped mound or hill. It consists of sand, till or gravel. It is created in a depression on a retreating glacier and is then left on the land surface.
"Eskir"EskerA glacial ridge could be defined as several things:- An arête: a steep ridge formed by glaciers.- Corries: formed through glacier action.- Eskir/esker: a ridge of sand and gravel deposited by glacial movement.- Serac: a block of ice formed by intersecting crevasses on a glacier
This is likely referring to till, which is a mixture of unsorted materials (rock, sand, and silt) left behind by a retreating glacier. Till layers can vary in thickness and composition, and they are often seen in areas where glaciers have once existed.
Cape Cod is considered a terminal glacial moraine, meaning that it was created by debris left behind by a retreating glacier.
Cape Cod is considered a terminal glacial moraine, meaning that it was created by debris left behind by a retreating glacier.
A large boulder left behind by a glacier is called a glacial erratic. These erratics are often significantly different from the surrounding rocks, providing clues about the glacier's movement and the rocks it passed over during its journey.
The depressions left by melted blocks of ice in glacial deposits are called kettle holes. They are circular or oval-shaped depressions that form when large chunks of ice left behind by a retreating glacier become buried in sediment. When the ice eventually melts, it creates a hole in the ground.