Till and stratified drift :D
Did you get this from Portola MS in 6th grade workbook for Science?
The two main types of glacial drift are till and moraine. Till refers to the mixture of sediments deposited directly by the ice, while moraine refers to the accumulation of till along the edges or underneath a glacier.
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.
Glacial drift refers to the material, such as rocks, sand, and clay, that is carried and deposited by glaciers as they move across the land. It includes both till, which is material directly deposited by the glacier, and stratified drift, which is material sorted and deposited by meltwater from the glacier. Glacial drift plays a crucial role in shaping the landscape and can be used by geologists to understand past glacial activity.
Glacial drift is material that has been eroded, transported, and deposited by glaciers. It includes a mix of rock fragments, sediments, and debris that are carried along by ice and then left behind as the glacier melts or retreats. Glacial drift can vary in size and composition, depending on the location and movement of the glaciers.
Glacial drift refers to the debris and sediments (such as rocks, sand, and gravel) that are transported and deposited by glaciers as they move. This process can shape the land, create moraines and drumlins, and leave behind distinctive landforms like valleys and ridges. Glacial drift plays a significant role in shaping the Earth's landscape and influencing the geology of regions that have been covered by glaciers in the past.
The two main types of glacial drift are till and moraine. Till refers to the mixture of sediments deposited directly by the ice, while moraine refers to the accumulation of till along the edges or underneath a glacier.
Glacial Drift
Glacial Drift
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.
It was a continental drift .
till is the name of the material. In most cases all glacial-related deposits are unsorted and unstratified.
Alphine
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.
Glacial drift refers to the material, such as rocks, sand, and clay, that is carried and deposited by glaciers as they move across the land. It includes both till, which is material directly deposited by the glacier, and stratified drift, which is material sorted and deposited by meltwater from the glacier. Glacial drift plays a crucial role in shaping the landscape and can be used by geologists to understand past glacial activity.
It's a stratified drift.
Glacial drift is material that has been eroded, transported, and deposited by glaciers. It includes a mix of rock fragments, sediments, and debris that are carried along by ice and then left behind as the glacier melts or retreats. Glacial drift can vary in size and composition, depending on the location and movement of the glaciers.
Glacial Drift