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What is a horizontal intrusive igneous body that forms between sedimentary rock layers?
A sill is a horizontal intrusive igneous body that forms between sedimentary rock layers. Sills are formed when magma intrudes parallel to the layering of the surrounding rocks and solidifies underground.
How would igneous rock be on a layer of sedimentary rock?
The igneous rock could have been erupted as lava on the surface, or intruded into the sedimentary rock layers as magma underneath the surface (a sill).
What kind of metamorphism occurs when intrusive magma forms a sill between two sedimentary rock strata?
contact metamorphism
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.
What is the word sill?
a tabular body of intrusive igneous rock, ordinarily between beds of sedimentary rocks or layers of volcanic ejecta.
What is a sentence for sedimentary rock?
Example sentences: Fossils are often found in sedimentary rock. It is easier to erode sedimentary rock than other forms of rock.
What feature of sedimentary rock is common to nearly every type of sedimentary?
Stratification.
What type of rock are the least common of the three types of rocks?
The most common chemical sedimentary rock is limestone.
Rock salt and rock gypsum are common examples of a group of chemical sedimentary rocks called .?
Rock salt and rock gypsum are common examples of a group of chemical sedimentary rocks called evaporities. When a sedimentary rock consists of angular, grave sized particles is breccia.
Is sedimentary rock the most common rock on planet surface?
yes
Is the rock breccia a clastic rock?
Breccias are a relatively common clastic sedimentary rock.
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.
