A stratum.
geologists call an area where is one type of topography is a landform
When sand, clay, or silt gradually turn into stone, we call them sedimentary rocks. These rocks are formed through the accumulation and compaction of sediment over time.
Geologists call the process of tectonic plates breaking apart "rifting." It occurs when the Earth's lithosphere is being pulled apart, causing the plates to separate, creating new ocean basins. Rifting is a key stage in the formation of new tectonic boundaries.
permafrost
Scientists call the top layer of a soil profile the "O horizon" or "organic horizon." This layer consists of organic material such as leaves, twigs, and other plant debris that are in the process of decomposing.
A single layer with consistent characteristics is referred to as a stratum.
Geologists refer to substances found in the Earth's crust as "minerals." Minerals are naturally occurring, inorganic solids with a definite chemical composition and crystalline structure. They can also refer to rocks, which are composed of one or more minerals or mineraloids. Additionally, geologists may categorize materials based on their properties, such as igneous, sedimentary, or metamorphic rocks.
Geologists call an area where there is one type of topography a landform region.
geologists call an area where is one type of topography is a landform
geologists call an area where is one type of topography is a landform
Geologists
Mesozoic
uh, chemicals.
Geologists refer to the crust and the uppermost mantle collectively as the "lithosphere." This layer is rigid and solid, lying above the more pliable asthenosphere. The lithosphere varies in thickness and is divided into oceanic and continental types, which play a crucial role in tectonic processes.
Direct Answer: AsthenosphereExplained Answer: Earthquake waves normally go faster with increasing depth. However, below the lithosphere, the upper mantle contains a curious layer in which earthquake waves unexpectedly slow down. Geologists call this layer the asthenosphere.
Sedimentary rock layers. your welcome
lithosphere