glacier
drumlin
Moraines are found in regions where glaciers have occurred, such as mountain ranges, polar regions, and areas with high elevations. They are commonly found at the edges of glaciers or in valleys where glaciers have advanced and retreated, leaving behind deposits of rock, sediment, and debris.
Unsorted sediments refer to a mixture of different sizes of particles that have not been sorted or arranged by any natural process like water or wind. These sediments lack any distinct pattern in their arrangement and can be found in deposits such as till or moraines left behind by glaciers.
Glacial moraines are accumulations of rock, soil, and debris carried and deposited by a glacier. They form as the glacier flows, picking up material from the land surface and carrying it along. Once the glacier retreats, it leaves behind these deposits, creating distinctive ridges and mounds.
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.
drumlin
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.
The depressions left behind are called kettles. The raised areas are called moraines.
Moraines are found in regions where glaciers have occurred, such as mountain ranges, polar regions, and areas with high elevations. They are commonly found at the edges of glaciers or in valleys where glaciers have advanced and retreated, leaving behind deposits of rock, sediment, and debris.
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 sediments refer to a mixture of different sizes of particles that have not been sorted or arranged by any natural process like water or wind. These sediments lack any distinct pattern in their arrangement and can be found in deposits such as till or moraines left behind by glaciers.
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.
Glacial moraines are accumulations of rock, soil, and debris carried and deposited by a glacier. They form as the glacier flows, picking up material from the land surface and carrying it along. Once the glacier retreats, it leaves behind these deposits, creating distinctive ridges and mounds.
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.
The soil and rocks left behind by a glacier are called moraine. Moraines can be classified as lateral, medial, or terminal, depending on where they are deposited in relation to the glacier. These deposits play a vital role in shaping the landscape and providing insights into glacial history.
When a glacier melts it deposits the sediment it eroded from the land, creating various landforms.
Glacial deposits are layers of rock, above the bedrock, as produced by the recent ice age(s), the glaciers as they moved across the planet, would pick up debris along the way, and as they moved, to say the area of, Washington State, besides, forming the Puget Sound Basin, called, a Fjord, later melting and leaving behind the various deposits, possibly gem material, gold, diamod's, etc. So theoretically, there could be, deposits, left by recent glaciation, rich in valuable minerals,