Fossils are depositions of dead animal imprints and/or bones. When an animal or plant dies, its skin rots away, leaving behind the bone or imprint.
The main types of fossils are cast, mold, petrified, trace, carbonized, and preserved fossils
fossils that are made from parts of an organism's body
Fossils are made naturally by Geological processes.
Probably a trace fossil; evidences of an organisms existence, without the body. Trace fossils include footprints, feces, burrow marks, and chemical signatures.
Fossils are what's left of ancient plants and animals. They are imprints in rock, generally sedimentary rock. The word "fossil"means "dug up" and it comes from Latin. Fossil fuels were made in the earth and took a long time to make.
Through the geophysical pressure on decomposed fossil shells deposited in deep underground layers. FOSSIL FULES ARE MADE UP OF PLANTS AND ANIMALS B- THE ORGANISM MUST BE BURIED IN SEDIMENT SOON AFTER IT DIES.
Fossil fuels are not made from the fossils of dinosaurs.
by freezing fossils in a freezer
theyre made out of dead stuff
fossils that are made from parts of an organism's body
fossil fuels are made from hydrocarbons of fossils of early life that has been locked away for millions of years
Fossils are made naturally by Geological processes.
It depends what fossil you're talking about but normally fossils are found in sedimentary rocks. But diatomaceous earth, and limestones contain fossils, or are made of fossils.
Fossil fuel is made from fossils that was under pressure for millions of years and turned into oil or coal. This can not be reproduced since there are no more fossils made from long extinct animals.
Because fossil fuels are fossils is the simple answer. Fossil fuels are just large collections of tiny fossils which have undergone a slightly different process which allows them to be flammable.
No, it is made from fossilisation of organic material.
Fossils can be made of any material that deteriorates slower than the sediment that forms the fossil hardens
Fossils can be made of any material that deteriorates slower than the sediment that forms the fossil hardens