moraines
glacier
Kames. Many are found in areas of kettles and moraines.
Glacial ice erosion will form: * Corries (cirques) * Aretes * Pyramidal Peaks * U-shaped troughs * Hanging Valleys * Truncated Spurs * Rouche Moutonees * Striations * Rock Steps Sediment deposition (resulting from glacial processes) will form: * Ice-transported boulders * Erratics * Lateral moraines * Medial moraines * Terminal moraines * Recessional moraines * Push moraines * Varves * Eskers * Delta kames * Kame terraces * Braided streams * Flat bottoms to U-shaped valleys
Moraines are the deposited remains that are left when a glacier melts and retreats. Therefore, erosion must have first taken place further up the glacier, and the debris carried down to be left at the melting point as stoney mounds.
moraines
moraines
The depressions left behind are called kettles. The raised areas are called moraines.
Kames. Many are found in areas of kettles and moraines.
Apron: Defined as an area covered by sand and gravel deposited at the front of a glacial moraine Outwash material/sandur. Or if into water a varve.
When deposits of till build up, they can leave behind various landforms such as moraines, drumlins, eskers, and outwash plains. These features are created by the movement of glaciers and the deposition of sediments as the glacier retreats.
Moraines form when a glacier moves down a mountain until it reaches temperatures warm enough to melt. As the ice melts, it deposits sediment. This sediment form ridges called moraines. Sources: My earth science book.
glacier
moraines
Kames. Many are found in areas of kettles and moraines.
Glacial ice erosion will form: * Corries (cirques) * Aretes * Pyramidal Peaks * U-shaped troughs * Hanging Valleys * Truncated Spurs * Rouche Moutonees * Striations * Rock Steps Sediment deposition (resulting from glacial processes) will form: * Ice-transported boulders * Erratics * Lateral moraines * Medial moraines * Terminal moraines * Recessional moraines * Push moraines * Varves * Eskers * Delta kames * Kame terraces * Braided streams * Flat bottoms to U-shaped valleys
Moraines are the deposited remains that are left when a glacier melts and retreats. Therefore, erosion must have first taken place further up the glacier, and the debris carried down to be left at the melting point as stoney mounds.