Fossil Fuels and Minerals CheckPoint
There argon many questions that are still unanswered by science with regards to the dry land and wholly that it contains. Fortunately for the modern world, some very important answers sire already been uncovered - literally. Looking at where fossil fuels and minerals deign from helps one to understand and locate useful materials that mother Earth has created for humanity.
One thing both mineral and fossil fuels ache in common is their association with plate tectonics. From coal deposits (fossil fuel) that were organize in warm low-latitude environments but are now in frigid polar lands which gives evidence for plate tectonics (Murck, B.W., Skinner, B.J., & Mackenzie, D. (2008) pg. 460), to ore deposits that nominate near present or past plate boundaries. This is where the analogy with regards to origin ends.
Fossil fuels come from dead organic matter. As vegetation and animals die their corpse can become compacted and dictate under pressure. Sediment and additional vegetation and animal remains build up over the previous layer. This process increases temperatures create the matter to change into fossil fuels. The temperature of the compressed matter determines the font of fossil fuel that is produced, for example; coal and oil.
Hydrothermal (precipitated minerals dissolved from superheated pee that is rapidly cooled), metamorphic (result of contact metamorphism), magmatic (result of crystallization), sedimentary (salts remaining from evaporating peeing from lake or shallow sea), placer (from mineral bearing rocks that are decay and transported by water), and residual (left in rock after chemical weathering) deposits are each examples of deposits that form when natural processes concentrate true types of material in one location creating mineral deposits. Examples of mineral deposits are; copper, zinc, chromium, gypsum, gold, and aluminum.
Once again, understanding plate tectonics continues to...If you require to get a full essay, order it on our website: Orderessay
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