contact
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.
A convergent plate boundary would likely form a mountain chain of sedimentary rock. As tectonic plates collide, one plate may be forced beneath the other, leading to the uplift of sedimentary layers and their subsequent compression and deformation, forming mountain ranges.
It is called sedimentary rock.
When layers of sediment get squeezed together, they form a rock type called sedimentary rock. This process, known as lithification, involves the compression and cementation of sediment particles over time. Sedimentary rocks can include materials such as sandstone, shale, and limestone.
The sedimentary rock formed from tiny particles of clay in thin, flat layers is called shale. I hope this was helpful:)
bedding plane
The boundary between any two different layers of sediment is called a "sedimentary contact" or "stratum contact." This contact represents a change in sediment characteristics, such as composition, texture, or depositional environment. Understanding these boundaries is crucial for interpreting the geological history recorded in sedimentary rock formations.
A laccolith is an igneous formation between two sedimentary layers
The layers of any sedimentary rock are called strata.
sedimentary
The layers of any sedimentary rock are called strata.
The layers found in sedimentary rocks are called strata. These are horizontal layers of sediment that have been deposited over time and then compacted and cemented together to form rock. Each layer represents a different time period in Earth's history.
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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.
the rock layers were eroded at the interface between the igneous intrusion and the sedimentary rocks.
sedimentary
Strata (singular: stratum)