diatom shells settle on the ocean floor from the surface
diatom shells settle to the ocean floor after diatoms die
Sediments found in a sandbar of a river
In disturbed sediments without layers, the relative age of the sediments would be unknown.
Fossiliferous (yes, that is a word) limestone forms from organism rich sediments or coral reefs in usually shallow marine environments. Shells of small marine organisms are most often formed of calcium carbonate. In time, the weight of the accumulated shells and sediments cause a gradual sinking of the material. With additional sediments constantly accumulating, the weight from above causes compaction of those sediments, squeezing out air and fluids from the space between the shells and shell fragments. These particles are cemented together by the mineral calcite which precipitates out of the remaining fluids. The compaction and cementation are part of the process of lithification, or rock formation.
Natural gas is found in the sediments pertaining to Earth's crust.
Normally, the oldest rocks are found at the bottom of the layers, being the first of the sediments that were deposited.
Mostly in marine photic zones .
Yes, a diatom is a single celled organism. They are a major group of algae and usually found in all water environments.
Diatoms are usually found in marine areas like oceans.
Sediments found in a sandbar of a river
In disturbed sediments without layers, the relative age of the sediments would be unknown.
shells are found near the shore line
Sand.
its electrons that are found in the shells around an atom.
Electrons are found in the shells and clouds.
diatoms are tinny substances found in water that are living
Conch shells are found in the Florida Keys which are a group of more than1700 islands
Sediments