Glacials
Moraines are deposits of rock, gravel, and dirt that have been left behind by glaciers as they advance and retreat. Glaciers pick up rocks and other debris as they move, and when they melt or retreat, this material is deposited as moraines.
drumlin
Kames. Many are found in areas of kettles and moraines.
The four types of moraines are lateral, medial, terminal, and ground moraines. Lateral moraines form along the sides of a glacier, medial moraines are formed when two glaciers merge and their lateral moraines combine, terminal moraines mark the furthest extent of a glacier's advance, and ground moraines are the debris left behind beneath a glacier as it retreats.
Flat deposits of rocks are called sedimentary layers or strata. These layers are formed over time through the accumulation and compaction of sediments.
moraines
Moraines are deposits of rock, gravel, and dirt that have been left behind by glaciers as they advance and retreat. Glaciers pick up rocks and other debris as they move, and when they melt or retreat, this material is deposited as moraines.
The depressions left behind are called kettles. The raised areas are called moraines.
drumlin
Kames. Many are found in areas of kettles and moraines.
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.
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.
Unsorted deposits refer to sedimentary deposits that have not been sorted or arranged by size or weight. This means that the particles or materials within the deposit have not undergone any sorting process based on their characteristics, such as size, shape, or density. Examples of unsorted deposits include moraines left by glaciers or alluvial fan deposits.
Some deposits of alpine glaciers include moraines (such as lateral, medial, and terminal moraines), drumlins, eskers, and outwash plains. These deposits are created as the glacier erodes, transports, and deposits sediment during its movement.
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.
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.
Kames. Many are found in areas of kettles and moraines.