it's called a slump.
The benthic zone is the lowest level of a body of water such as an ocean or a lake. It includes the sediment surface sediment and some sub-surface layers.
The building up of layers of sediment is known as sedimentation. This process occurs when particles of rocks, minerals, and organic matter settle and accumulate on the Earth's surface over time, forming layers of sediment. Over millions of years, these layers can become compressed and cemented together to form sedimentary rocks.
ecological region at the lowest level of an ocean with the sediment surface and some sub-surface layers
Sediment is laid down in flat layers because gravity causes particles to settle evenly and compact together, forming a flat surface. Additionally, water or wind currents tend to distribute sediment horizontally, creating uniform layers. The flat layers of sediment can provide important clues about past environments and geological processes.
When sediment collects in an area, it is called sedimentation. This process occurs when particles settle out of a fluid and accumulate on a surface, forming layers of sediment over time.
The settling of particles on a sediment or other surface is known as sedimentation. This process occurs when particles in a fluid, such as water or air, lose their kinetic energy and come to rest due to gravity or other forces. Over time, sedimentation can lead to the formation of layers of sediment on the surface.
Gravity causes layers of sediment to be horizontal because as sediment deposits, it settles evenly due to gravity pulling the particles downwards. Over time, as more sediment accumulates, the weight of the new layers causes the underlying layers to compact and settle into a horizontal orientation.
When erosion stops and transported sediment settles on a surface, it is called deposition. This process involves the laying down of sediment by natural agents like water, wind, or ice, leading to the formation of sedimentary rock layers over time.
Horizontal layers of rocks are rock layers that are parallel to the Earth's surface. These layers are typically formed over time through sedimentary processes, such as deposition of sediment in water or air. The horizontal orientation of these layers indicates the original horizontal position in which they were deposited.
The process that builds up sediment over millions of years is called sedimentation. It involves the accumulation of weathered rocks, minerals, and organic material that settle in layers on the Earth's surface. Over time, these layers of sediment can become compressed and cemented together to form sedimentary rocks.
The squeezing of layers of sediment is called compaction. This process reduces the volume of sediment and removes water between particles, resulting in the formation of sedimentary rocks.
Deposition