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.
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.
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.
Valley glaciers are typically advancing when their terminus is pushing forward, causing the glacier to grow in size. Conversely, they are retreating if the terminus is melting or receding, leading to a decrease in glacier size. Monitoring changes in the glacier front position over time can help determine if it is advancing or retreating.
khame
A boulder left behind by a retreating glacier is known as an erratic. A glacier is a moving river of ice and snow.
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 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.
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.
A retreating glacier is one that is diminishing more in length that its upper supply regions can compete with. The snout of the glacier is retreating, but the main body of the glacier is still moving forwards. If this situation continues, the glacier will disappear.
The material left behind by a retreating glacier, including boulders, sand, clay, and silt, is known as moraine.
Valley glaciers are typically advancing when their terminus is pushing forward, causing the glacier to grow in size. Conversely, they are retreating if the terminus is melting or receding, leading to a decrease in glacier size. Monitoring changes in the glacier front position over time can help determine if it is advancing or retreating.
Cape Cod is considered a terminal glacial moraine, meaning that it was created by debris left behind by a retreating glacier.
The glacier is melting faster than it is sliding down the valley.
Cape Cod is considered a terminal glacial moraine, meaning that it was created by debris left behind by a retreating glacier.