The hydrosphere and lithosphere are primarily involved in the process of erosion. The hydrosphere, which includes water bodies like rivers and oceans, transports sediment and wears away at rocks through processes like abrasion and hydraulic action. The lithosphere, which includes the Earth's crust and land formations, is the surface being eroded by the movement of water, ice, and wind.
The two spheres that are responsible for erosion are the hydrosphere and the atmosphere. These spheres interact all of the time.
Cementing is not a process involved in the formation of sedimentary rock.
Creeps are a type of slow, ongoing mass movement of soil and rock downhill, typically due to gravity. While they are involved in the process of erosion by gradually moving material down a slope, they are not agents of erosion themselves. Instead, creeps primarily contribute to the process of soil creep, which does not necessarily involve significant erosion.
Yes, Earth's spheres interact with each other in various ways. For example, the geosphere (solid Earth) influences the hydrosphere (water) through erosion and sedimentation, while the atmosphere interacts with the lithosphere through weathering and erosion. These interactions are essential for maintaining Earth's systems and processes.
Deposition is the opposite of erosion. Deposition is the process where sediments and rocks are added to a landform or landmass, while erosion is the process where sediment and rocks are removed from a landform.
The two spheres that are responsible for erosion are the hydrosphere and the atmosphere. These spheres interact all of the time.
The two geological processes involved in changing an igneous rock to a sedimentary rock are weathering and erosion. Weathering is the process of decomposing rocks, while erosion refers to the process of wearing away the surface of rocks by the action of water, glaciers and winds.
Cementing is not a process involved in the formation of sedimentary rock.
The Lithosphere.
Geosphere, hydrosphere and atmosphere are involved. Water travels through these spheres.
The three basic steps are erosion (weathering), transport (carrying silt), and deposition (carried load settles out).
Creeps are a type of slow, ongoing mass movement of soil and rock downhill, typically due to gravity. While they are involved in the process of erosion by gradually moving material down a slope, they are not agents of erosion themselves. Instead, creeps primarily contribute to the process of soil creep, which does not necessarily involve significant erosion.
Erosion
Erosion is a mechanical process.
The answer is Erosion.
Weathering or erosion.
Erosion