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Fossils

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1) There are two types of fossils, Type I which consists of the remains of the dead animal or plant or the imprint left from the remains.This could include teeth, bones, skin impressions and hair. It could also include the hardened shell of an animal without a backbone. Type II consists of something that was made by the animal while it was living that has hardened into stone which is called trace fossils. Trace fossils include burrows, footprints, coprolite, and even animal poop. Permineralization is when liquid minerals are filled into open space in the bones. Therefore fossils are formed through permineralization when bones are turned into some sort of crystal. By the bone material being replaced by different minerals contained in the liquid of the sediments that buried it. This can also be done with shells, exoskeletons, and wood.

2) The slow movement of Earth’s plates can push and pull on the rock in the crust. These forces can crack the rock making a fault. A fault is a crack in the crust where slabs of rock can slip past one another. the largest faults are at the boundaries of the plates. Sometime part of one plate gets caught on the rough edge of another. Pressure builds and the plates can break, which causes an Earthquake to begin.Earthquakes happen in Japan.

3) Scientist measure Earthquakes by using a magnitude scale. A magnitude scale measures the amount of energy that comes from an earthquake. Earthquakes with a low magnitude release little energy and do little damage. Earthquakes can’t be predicted to any degree, it’s been tested several times, and it just never worked.

5) A volcano is a mountain that opens downward to a pool of molten rock below the surface of the earth. Eruptions occur from pressure being built up. Volcanoes are formed when hardened lava turns into solid rock, built up over time the rock forms into a mountain. Sometimes,

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