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19-Dec-2019 16:46

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The principle of faunal succession is based on the appearance of fossils in sedimentary rocks.

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As he continued his job as a surveyor, he found the same patterns across England.Explanations: A – folded rock strata cut by a thrust fault; B – large intrusion (cutting through A); C – erosional angular unconformity (cutting off A & B) on which rock strata were deposited; D – volcanic dyke (cutting through A, B & C); E – even younger rock strata (overlying C & D); F – normal fault (cutting through A, B, C & E).The principle of cross-cutting relationships pertains to the formation of faults and the age of the sequences through which they cut.Geologists still use the following principles today as a means to provide information about geologic history and the timing of geologic events.

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The principle of Uniformitarianism states that the geologic processes observed in operation that modify the Earth's crust at present have worked in much the same way over geologic time.Faults are younger than the rocks they cut; accordingly, if a fault is found that penetrates some formations but not those on top of it, then the formations that were cut are older than the fault, and the ones that are not cut must be younger than the fault.



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