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A ripple mark is not a kind of rock in and of itself, but a feature found in some sedimentary rocks, usually sandstones.
Through observation of sedimentary rocks, geologists are able to analyze rock layers and date the rocks by testing the carbon in each sample.
600 million years
They are called clastic sedimentary rocks.
Rocks are to geologists as stars are to astronomers.
Sedimentary rocks show fossils, because of pre-existing life forms. They also show ripple marks due to weathering and erosion...
Ripple marks
Ripple marks
"Ripple marks" (but you could also say cross bedding and dune bedding sort of do this too).
sedimentary,metormorphic , igneous .........
Sedimentary, metamorphic and igneous.
A ripple mark is not a kind of rock in and of itself, but a feature found in some sedimentary rocks, usually sandstones.
Through observation of sedimentary rocks, geologists are able to analyze rock layers and date the rocks by testing the carbon in each sample.
Ripple marks in sedimentary rock were emplaced in sediments by near shore wave action, covered by additional sediments, and eventually lithified into a solid rock which becomes exposed by weathering and erosion of overlying material over large expanses of time.
The investigative process by which geologists identify and match sedimentary strata and other rocks of the same ages in different areas is referred to as correlation.
600 million years
They are called clastic sedimentary rocks.