Many rocks can contain fossil organisms. Generally speaking, sedimentary rocks are the rock type that contains the most fossil organisms. Coquina, a type of limestone, is formed nearly completely by the shells of marine organisms. And coal is a sedimentary rock composed of the remains of ancient swamp plants.
They are called sedimentary rocks, formed by the remains of dead organisms, sand, etc
Coral.
In some rare areas there are still living stromatolites.
There are several sedimentary rocks that are made of the compressed remains of organisms. That's actually how fossils are made. One example of this type of rock would be limestone.
Organic sedimentary rocks.
Fossil
A biogenic rock is a rock made from the remains of living organisms, which collected during sedimentation.
Organic sedimentary rock is comprised of the remains of once living organisms.
Limestone
Coquina is a sedimentary rock fitting that description.
sedimentary rock is formed by you are stupid if you dont know that
sedimentary rock
this would be organic sedimentary
Organic sedimentary rock is comprised of the remains of once living organisms.
Organic sedimentary rock is comprised of the remains of once living organisms.
Organic sedimentary rock is comprised of the remains of once living organisms.
this would be organic sedimentary
Chalk would fit this description.
no. it is the other way around. living organisms are important to the rock cycle.
Any link of uranium with the living organisms.
organic/biochemical sedimentary rocks are formed of once-living organisms
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
Asphalt is not a rock, but is produced from the remains of fossilized organisms.