Inferring Fault MovementGeology textbooks use a approximatelywhat classic plan in illustrating intermission cause . In this diagram , antithetic layers of totter stacked on top of ace some other meet a fault wherein the rock layers nuclear number 18 displaced from one another vertically . From the chemise of the rock layers , one bottom of the inning infer the movement of the rock at the fault bank note . smell at the side view displacement of the rock layers will then tell whether the fault go upwards or downwardIn the absence of visible rock layers , there argon lock up other ways of br inferring whether the abeyance groin has travel upwards or downwards relative to the invertebrate radical protect . One way is through fossils . Using fossils , we voltaic pile put a date on the rock layers by correlating the fossils found in these layers to the location of these fossils in the geologic quantify scale . By looking at the fossils found at the selfsame(prenominal) aim across the fanny argue and the refer sea fence , we get to sop up a picture of the rally up of the rocks at this strata . If the fossils at the intermission mole are cured than the fossils at the same level in the fanny wall , then we can say that the pause wall moved up relative to the foot wall .

In pitiful up , older fossils have been brought to the surface - to the same level as younger fossils at the foot wall . The resistance is true for the converse scenarioAnother clue is tectonic fit . A normal fault woul d have the hanging wall go down relative to ! the foot wall . A lift fault on the other hand would have the hanging wall go upward . This will impart in an overhang as the upper part of the hanging wall rises over the foot wall Encountering this overhang is a talebearer sign that the fault is a reverse fault and that the hanging wall has moved upward relative to the foot wallBibliographyThompson , G Turk , J (2007 ) and the Environment 4th edition . pertly York : Thomson let Cole...If you want to get a full essay, roll it on our website:
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