Continentality<span>, </span>a measure of the difference between continental and marine climates characterized by the increased range often peratures that occurs over land compared with water. This difference is a consequence of the much lower effective heat capacities of land surfaces as well as of their generally reduced evaporation rates.
Answer:
it is because, igneous and metamorphic form at temperatures and pressures which destroy the fossil remains. dead organisms may become sediments which may, under right conditions, become sedimentary rocks
Regions of the earth's waters, crust and atmosphere in which organisms can exist is the Biosphere
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The Ural Mountains and the Caucasus Mountains.
