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Q: When ancient decaying bones and organisms become compressed together what type of sedimentary rock would form?
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Related questions

What rock is formed when debris is buried and compressed together?

sedimentary


Is chalk sedimentary?

Yes,!! Chalk is fine grains of limestone compressed together and limestone is sedimentary, so chalk has to sedimentary.


What rock is formed when debris is buried compressed and cemented together?

sedimentary


Rock is formed when debris is buried compressed and cemented together?

Sedimentary


Rock is formed when debris is buried compressed and cemented together.?

Sedimentary


What rock is formed when debris is buried compressed and cemented together.?

sedimentary


Which type of rock is formed when layers of rock partials carried by wind and water are compressed and cemented together?

sedimentary


What types of rock are form when layers of rock particles carried by wind and water are compressed and cemented together?

Sedimentary


What are compressed and cemented together to form sedimentary rock?

Sedimentary rocks are formed by the compaction from overlying sediments and by the cementation resulting from the replacement of fluids with minerals, in a process of rock formation known as lithification.


How do fossils end up in sedimentary rocks?

fossils are small living organisms that existed millions of years ago. They mostly have a shell which is the fossil that you can sea. Sedimentary rock is formed when lots of small particles and pieces of rock and often dead organisms, (the fossils) drift down to the sea bed and over millions of years get compressed together to form the rock. The fossil that you see was once a living shelled organism which dies and was preserved as the sedimentary rock formed


Sandstone is in what class?

Siltstone is a sedimentary rock. It forms on river beds when silt compressed together.


Is sandstone igneous or sedimentary or metamorphic?

Sandstone is a sedimentary rock which is made up of sand grains which have been compressed to form a rock that has very weak bonds holding the grains together. The grains themselves can be igneous, sedimentary or metamorphic depending on which rock the grains were eroded from.