Sediment forms through the weathering and erosion of rocks and minerals, which breaks down larger materials into smaller particles. These particles are then transported by natural forces such as water, wind, or ice, and eventually deposited in various environments like rivers, lakes, and oceans. Over time, layers of sediment accumulate and can become compacted and cemented, leading to the formation of sedimentary rock.
A two smaller, more stable nuclei
igneous rock
The loss of edges on sediment grains best describes the process of sediment abrasion or weathering, where particles collide and rub against one another, leading to the rounding of their edges. This process typically occurs in environments with high energy, such as rivers or beaches, where sediment is continuously transported and reworked. As a result, grains become smoother and more rounded over time, reflecting their transport history and the conditions of their depositional environment.
It is known as moraine.
When sediment is compressed over time, it forms sedimentary rock. This process, known as lithification, involves the compaction of sediment layers and the cementation of particles by minerals precipitating from water. As pressure increases, the sediment grains are forced closer together, leading to the formation of solid rock structures. Common examples of sedimentary rocks include sandstone, limestone, and shale.
The term that best describes the study of how energy is transferred to different locations and forms is "thermodynamics." Thermodynamics is the branch of physics that deals with the relationships between heat and other forms of energy.
Sediment sorting refers to the uniformity of grain size within a deposit, layering refers to the horizontal stratification of sediment, texture describes the size, shape, and arrangement of grains within a sediment, and grain roundness indicates the relative smoothness or angularity of sediment grains.
levee
One atom pulls an electron from another atom.
A two smaller, more stable nuclei
Reduced chemistry
not a hydrogenous sediment?
no they do not
The ocean floor generally consists of basalt cooled from magma, and the overlying layers of sediment, both inorganic and organic.
Deposition is the process by which sediment settles out of water and is deposited on the bottom of a body of water.
A sediment deposit called a windward slope forms when sediment is blown against an obstacle and settles behind it. This deposit is characterized by a gradual slope facing into the prevailing wind direction.
forms a sediment when it sinks to the bottom of a liquid.