One condition that best increases the chance that an organism will become fossilized is if the burial happens rapidly. Another condition that can increase the chance of an organism becoming fossilized is if the organism has hard body parts.
Fossil Fuels =)
fossil.
Fossils are proof of organisms that lived long ago
Examples of biogeologic processes include soil formation through the weathering of rocks, the deposition of sediments by rivers and glaciers, and the formation of fossil fuels from the remains of organisms over millions of years. These processes involve interactions between living organisms and the Earth's geology.
Fossil formation typically requires the rapid burial of an organism in sediment, which helps protect it from decomposition and scavenging. The organism's remains undergo a process of mineralization over time, where minerals replace the original organic material, preserving the structure of the organism as a fossil.
dead organisms
Fossil Fuels =)
i think rock and sea is the habitat of fossil becaus these are the remains of organisms
Yes, coal, petroleum, and natural gas are formed over millions of years from the remains of dead organisms that were buried and subjected to heat and pressure. In a laboratory setting, it is possible to simulate the conditions required for the formation of these fossil fuels, but it would not be practical to produce them on a large scale. Instead, these fossil fuels are extracted from the earth where they naturally occur.
fossil.
Fossil fuel
they decayed
Fossils are proof of organisms that lived long ago
Fossil Fuels =)
Examples of biogeologic processes include soil formation through the weathering of rocks, the deposition of sediments by rivers and glaciers, and the formation of fossil fuels from the remains of organisms over millions of years. These processes involve interactions between living organisms and the Earth's geology.
Fossil formation typically requires the rapid burial of an organism in sediment, which helps protect it from decomposition and scavenging. The organism's remains undergo a process of mineralization over time, where minerals replace the original organic material, preserving the structure of the organism as a fossil.
fossil