Unsorted and not layered
A terminal moraine and a delta are both landforms created by deposition of sediment. However, a terminal moraine is formed by glacial ice depositing till at the end of a glacier, whereas a delta is formed by a river depositing sediment at its mouth where it meets a body of water.
Glacial till is unsorted and unstratified sediment deposited directly by a glacier, while stratified drift is sorted and stratified sediment deposited by glacial meltwater. An example of glacial till is a moraine, which is a ridge of mixed debris left behind by a moving glacier. An example of stratified drift is an outwash plain, which is a flat, gently sloping area formed by the deposition of sorted sediments carried by glacial meltwater.
Moraines are formed by the deposition of glacial debris as a glacier moves and erodes the land. As the glacier melts, it leaves behind ridges and mounds of unsorted sediment. The size and shape of a moraine can vary depending on the glacier's movement and the type of sediment deposited.
Glacial moraine could dam and prevent glacial meltwater from escaping. Glacial lakes usually form behind the moraine as the thawing glacier retreats.
The glacial landform for mounds or ridges of till is called moraines. Moraines are formed when glaciers deposit rock material and sediment that they have eroded and carried as they move. They can be found along the sides, in the middle, or at the terminus of a glacier.
A moraine is another name for glacial sediment. There are four common types: Lateral, Terminal, Medial and Ground Moraine.
The rock and soil debris accompanying the glacier is moraine. lateral moraine at the sides where avalanches have dropped it, terminal moraine where the glacier finishes, and medial moraine formed from the lateral moraines of two contributory glaciers when they join.
A terminal moraine and a delta are both landforms created by deposition of sediment. However, a terminal moraine is formed by glacial ice depositing till at the end of a glacier, whereas a delta is formed by a river depositing sediment at its mouth where it meets a body of water.
Glacial till is unsorted and unstratified sediment deposited directly by a glacier, while stratified drift is sorted and stratified sediment deposited by glacial meltwater. An example of glacial till is a moraine, which is a ridge of mixed debris left behind by a moving glacier. An example of stratified drift is an outwash plain, which is a flat, gently sloping area formed by the deposition of sorted sediments carried by glacial meltwater.
Moraine and outwash are both glacial deposits formed by the movement of glaciers. Moraine consists of debris, such as rocks and sediment, that accumulates at the edges or base of a glacier, while outwash is the sediment deposited by meltwater streams flowing from a glacier. Both features provide important insights into past glacial activity and landscape evolution. Additionally, they contribute to the geological and ecological characteristics of the areas they occupy.
Moraines are formed by the deposition of glacial debris as a glacier moves and erodes the land. As the glacier melts, it leaves behind ridges and mounds of unsorted sediment. The size and shape of a moraine can vary depending on the glacier's movement and the type of sediment deposited.
Glacial moraine could dam and prevent glacial meltwater from escaping. Glacial lakes usually form behind the moraine as the thawing glacier retreats.
glacial till.
Glacial Till (used to be called 'Boulder Clay'). Sometimes Moraine Debris, but terms like 'moraine' refer to the topography of the deposit rather than the material itself.
The glacial landform for mounds or ridges of till is called moraines. Moraines are formed when glaciers deposit rock material and sediment that they have eroded and carried as they move. They can be found along the sides, in the middle, or at the terminus of a glacier.
A moraine forms by sediment ridges. 👍 or 👎
Glacial weathering forms till moraine kettles and also kettles lakes. More specifically the acts of glacial depositionforms these.