water, wind, ice, etc. do transport sediment.
lava does not transport sediment
Weathering, erosion, and deposition are the three processes that contribute to the formation of sediments. Weathering breaks down rocks into smaller pieces, erosion transports the sediments to new locations, and deposition is the settling of these sediments in new areas.
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 are formed in the natural environment through the process of weathering and erosion. Weathering breaks down rocks into smaller pieces, while erosion transports these pieces to new locations where they settle and accumulate as sediments. Over time, these sediments can be compacted and cemented together to form sedimentary rocks.
Weathering breaks down rocks into smaller fragments. Erosion transports the sediments from their source to a new location. Deposition occurs when the sediments settle and accumulate in a new area. Compaction and cementation transform the sediments into solid rock through pressure and mineral precipitation.
The combination of weathering and movement of resulting sediments of rocks is known as erosion. Weathering breaks down rocks into smaller pieces, while erosion transports these sediments to new locations through the action of water, wind, ice, or gravity.
Sediments enter oceans through various processes, primarily from river runoff, which transports eroded materials from land. Additionally, sediments can be delivered by wind, which carries fine particles that settle into the ocean. Coastal erosion and the movement of sediment along shorelines also contribute to ocean sedimentation. Furthermore, underwater volcanic activity and tectonic processes can introduce sediments directly from the seafloor.
Turbulent flow transports more sediment than laminar flow due to the increased velocity and mixing of particles in turbulent flow. This helps to keep sediments suspended and advected downstream more effectively.
Sediment is created through the process of weathering and erosion. Weathering breaks down rocks into smaller pieces, while erosion transports these pieces to new locations where they accumulate and form sediment layers. Over time, pressure and cementation can turn these sediments into sedimentary rocks.
Any type of rock, such as igneous, metamorphic, or sedimentary, can be changed into sediments by weathering and erosion processes. Weathering breaks down rocks into smaller pieces, while erosion transports these sediments to new locations where they can eventually become part of sedimentary rocks through processes like compaction and cementation.
Glacial deposits may form when glaciers move along mountains and break off sediments. These deposits can include a variety of sediment types such as till, moraines, and erratic boulders. As the glacier moves, it erodes and transports these sediments, eventually depositing them once the glacier melts.
The process in the rock cycle that causes sediments to form is called weathering and erosion. Weathering breaks down rocks into smaller particles through physical, chemical, or biological processes, while erosion transports these particles away from their original location. Over time, these sediments can accumulate and undergo lithification, eventually forming sedimentary rocks.
A metamorphic rock can be transformed into sediments through the processes of weathering and erosion. Weathering breaks down the rock into smaller particles through physical, chemical, or biological means, while erosion transports these particles away from their original location. Over time, these sediments can accumulate and eventually become compacted and cemented to form sedimentary rock.