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Yes. It is true.

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Q: IS stratigraphy is a method to determine the relative age of rock strata?
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Related questions

Is it true that Stratigraphy is a method to determine the relative age of rock strata?

Yes, stratigraphy is a method to determine the relative age of rock strata. Stratigraphy is a branch of geology which studies rock layers.


What can be used to date fossils in rocks to give an approximate age.?

The study of strata is called stratigraphy. Stratigraphy can be used to determine an approximate age of fossils in rocks.


What can be used to date fossils in rocks to give an approximate age?

The study of strata is called stratigraphy. Stratigraphy can be used to determine an approximate age of fossils in rocks.


Can be used to date fossils in rocks to give an approximate age.?

The study of strata is called stratigraphy. Stratigraphy can be used to determine an approximate age of fossils in rocks.


The study of layers of the earth in order to date strata?

Stratigraphy.


How is the term Stratigraphy properly defined?

Stratigraphy, or formation, refers to the study of strata, or rock layers. Stratigraphy is often used for geologic time markers, and it serves many uses in the scientific world.


Who proposed the principles of stratigraphy to relatively date rock layers?

William (Strata) Smith


What are the principles of seismic stratigraphy?

Seismic stratigraphy is a geologic approach to the interpretation of seismic data, allowing their application based on physical stratigraphy. Primary seismic reflections parallel the surface and nonconforming surface of the strata.


What minerals are found in a rock determine?

strata


What minerals found in a rock determine?

strata


What is the Application of sequence stratigraphy?

Depositional environments, geologic ages, and sometimes catastrophic event ages can be determined by a careful examination of the individual strata in sedimentary rock.


Where does the word strata originate from?

Strata is the plural of stratum.In geology and related fields, a stratum is a layer of sedimentary rock or soil with internally consistent characteristics that distinguish it from other layers. The "stratum" is the fundamental unit in a stratigraphic column and forms the basis of the study of stratigraphy.