Certainly, yes.
True
Overcome intermolecular forces
This organic material is made up of living organisms such as plants and animals, dead plants and animals, and nutrients that have come from decomposed plants and animals.
A horizon B horizon C horizon O horizon
They were formed from the remains of the prolific plant material growing in vast marshy areas in the Carboniferous. The plant remains did not rot in their shallow water environment and formed layer after layer of sediment which was eventually covered with subsequent layers of additional sediments resulting in their compaction and cementation in a process of lithification.
answ2. Conditions favourable for good preservation of a fossil include:-. quick burial. a fine silt cover (Though lignite or similar often contain good fossils). little or no decomposition. stable geological environment - no metamorphism, folding, crushing.Some good fossils are found to have had their internal structure replaced by mineral solution. Quite common with wood.Very occasionally, an insect or animal is preserved in an inaccessible environment, such as the tar pits of la Brea, or Baltic Amber.Wooly Mamoths and similar are not considered fossils.Fossils are formed by microorganisms decomposing the remains of an animal or plant. These microorganisms need oxygen to respire, so fossils are left when the material is to hard for the microorganisms to decay when there is a lack of oxygen.
While solubility is undergoing changes in their substances wheather it could be from a mechanical deformation, exposure to another substance, or any of a number other alterations. If the same substance remains after the change, a physical change has taken place.
Study of cilization through the material remains is archaelogy
solid material
"MR 7 material" remains undefined in the English language.
Overcome intermolecular forces
When two balls collide, energy is transferred into sound and deformation, but momentum remains the same. The mass times velocity of the balls is constant.
colon
Organic material contains organic compounds from the remains of dead organisms and their waste products.
55
A scientist who studies the material remains of past human life.
weathered remains of other rocks
coal