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What feature of sedimentary rock is common to nearly every type of sedimentary rock?
The feature common to nearly every type of sedimentary rock is layering, known as stratification, which is formed by the accumulation and compaction of sediments over time. This layering provides information about the environment in which the rock was formed.
Is sedimentary rock the only type of layered rock?
No. Extrusive igneous rocks are usually layered. Some metamorphic rocks have foliation, which resembles layering, but it is not the same thing.
Is a metamorphic rock with no banding a nonfoliated rock?
Yes, a metamorphic rock with no banding is classified as a nonfoliated rock. Nonfoliated rocks do not exhibit the layering or banding commonly seen in foliated rocks due to the recrystallization process they undergo during metamorphism.
What is stratification and what type of rock does it apply to?
Stratification refers to the layering of rock formations caused by sediment deposition over time. It commonly applies to sedimentary rocks, such as sandstone, shale, and limestone, which are formed through the accumulation and compaction of sedimentary particles.
Clay minerals cement layers of sediment together to form what?
Clay minerals can cement layers of sediment together to form shale, a type of sedimentary rock characterized by its fine-grained nature and distinct layering.
What feature of sedimentary rock is common to nearly every type of sedimentary rock?
The feature common to nearly every type of sedimentary rock is layering, known as stratification, which is formed by the accumulation and compaction of sediments over time. This layering provides information about the environment in which the rock was formed.
What type of rock forms from layering of eroded rock?
Sedimentary rock forms from the layering of eroded rock material, which accumulates and undergoes compaction and cementation over time. Examples of sedimentary rocks include sandstone, shale, and limestone.
Is sedimentary rock the only type of layered rock?
No. Extrusive igneous rocks are usually layered. Some metamorphic rocks have foliation, which resembles layering, but it is not the same thing.
What shows how rocks change one type to other?
The rock cycle
What is a diagram that shows how roks change from one type to another?
rock cycle
WHAT TYPE OF MAP SHOWS THE ROCK LAYERS INSID A LANDFORM?
a road map
Intrusive igneous rock body that is tabular and concordant?
A sill is a type of intrusive igneous rock body that is tabular and concordant, meaning it is parallel to the layering of the surrounding rock. Sills are formed when magma is injected into existing rock layers and solidifies underground. They are often found in sedimentary rock formations.
Is a model that shows how rocks are recycled from one type to another?
the rock cycle is correct
Is a metamorphic rock with no banding a nonfoliated rock?
Yes, a metamorphic rock with no banding is classified as a nonfoliated rock. Nonfoliated rocks do not exhibit the layering or banding commonly seen in foliated rocks due to the recrystallization process they undergo during metamorphism.
What is stratification and what type of rock does it apply to?
Stratification refers to the layering of rock formations caused by sediment deposition over time. It commonly applies to sedimentary rocks, such as sandstone, shale, and limestone, which are formed through the accumulation and compaction of sedimentary particles.
Is an intrusive igneous rock body that is tabular and concordant parallel to adjacent sedimentary rocks?
This type of intrusive igneous rock body is called a sill. Sills are tabular igneous bodies that form parallel to the layering of existing sedimentary rocks. They are concordant, meaning they intrude along bedding planes without disrupting the original layering of the surrounding rocks.
What is the type of rock made from layers of rock and other materials that are cemented together?
The type of rock that is made from layers of rock and other materials cemented together is called sedimentary rock. This process of layering and cementation usually occurs over long periods of time, often through the accumulation and compaction of sediments. Examples of sedimentary rocks include sandstone, limestone, and shale.
