Glaciers are the agent of erosion that deposit irregular mounds of unsorted sediment with parallel scratches on rounded particles. This type of deposit is called a moraine, which is formed as the glacier moves and carries a mixture of different-sized sediments that get deposited when the glacier melts.
The process that carries sediments into rivers is called erosion. Erosion occurs when weathering and other factors break down rocks and soil, which are then transported by water, wind, or ice and deposited into rivers.
A drumlin is primarily a landform that results from glacial deposition, where sediments are deposited and shaped by the movement of glaciers. Erosion can also play a role in shaping drumlins, but their characteristic streamlined shape is primarily influenced by deposition processes.
Erosion transports sediments from the original source through processes like wind, water, or ice. As the sediments are eroded, they are carried away and eventually deposited in a new location, forming sedimentary deposits.
When the energy of an agent of erosion decreases, such as when a river slows down or a glacier melts, it drops the sediments it was carrying. This process is known as deposition, where the sediments are deposited in new locations, leading to the formation of new landforms. On the other hand, when the energy of the agent of erosion increases, it can pick up and transport more sediments.
Glacial ice is the most probable agent of erosion that deposited unsorted sediments in deposit B. Glaciers can transport a wide range of sediment sizes and mix them together as they move, resulting in unsorted sediments.
in erosion sediments are are deposited, in weathering sediments are taken away
Glaciers are the agent of erosion that deposit irregular mounds of unsorted sediment with parallel scratches on rounded particles. This type of deposit is called a moraine, which is formed as the glacier moves and carries a mixture of different-sized sediments that get deposited when the glacier melts.
Erosion of sediments on a mountain range will eventually lead to the formation of sedimentary rock. As sediments are transported and deposited in layers, they undergo compaction and cementation over time. This process transforms loose sediments into solid rock, typically resulting in formations such as sandstone, shale, or limestone, depending on the composition of the sediments.
Floodplains are typically formed by the deposition of sediments carried and deposited by rivers during floods, rather than erosion. Erosion can shape the landscape, but floodplains are mostly a result of the sediment deposition process.
Deposition: Sediments must be deposited on a surface, such as a rock layer or land surface. Erosion: The deposited sediments must then be removed through processes like weathering and erosion, exposing the underlying surface to create an unconformity.
The process that carries sediments into rivers is called erosion. Erosion occurs when weathering and other factors break down rocks and soil, which are then transported by water, wind, or ice and deposited into rivers.
well first is weathering, then the sediments ,then erosion takes the sediments to a new place ,then they are deposited there for a new land form to come
The unsorted rock material deposited directly by a melting glacier is called till. Wind erosion that removes dry soil particles is known as deflation. Together, these processes can create a landscape called a desert pavement where larger rocks are left behind due to deflation.
A drumlin is primarily a landform that results from glacial deposition, where sediments are deposited and shaped by the movement of glaciers. Erosion can also play a role in shaping drumlins, but their characteristic streamlined shape is primarily influenced by deposition processes.
Erosion transports sediments from the original source through processes like wind, water, or ice. As the sediments are eroded, they are carried away and eventually deposited in a new location, forming sedimentary deposits.
Sediments in sedimentary rocks may be made of fragments of other rocks, minerals, and organic material like remains of plants and animals. These sediments are typically transported and deposited by processes such as erosion, weathering, and deposition.