Relative Dating Of Rocks Ppt

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Relative Dating Principles 2 . The Cross-cutting Law Any feature that cuts across a body of sediment or rock is younger than the body of sediment or rock that it cuts across . Cross-cutting Igneous Rock Cross Cutting Relationships - Geologic features that cut through and across rocks are younger than those rocks . Relative Dating Principles 1 .
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Relative and Absolute Dating There are two major ways to date geologic events: Relative dating -how old a rock is compared to surrounding rocks Absolute dating -actual number of years since the rock was formed Relative Dating The various relative dating methods tell you whether a specific rock or layer of rocks is younger or older as compared to surrounding rocks This type of dating does not give an exact age for the rock The Law of Superposition states that in an undisturbed sequence of . . .
1 . IV . Relative Dating 2 . Relative dating tells us the sequence in which events occurred, not how long ago they occurred . Chronological order - relational 3 . a . Law of Superposition The law of superposition states that in an undeformed, undisturbed sequence of sedimentary rocks , each bed is older than the one above it and younger than the one below it . 4 . Undistrubed Rock Layer
10 . Using Fossils to Date Rocks β’ To date rock layers, geologists first give a relative age to a layer of rock at one location . Then they can give the same age to matching layers of rock at other locations . 11 . Example using Silly Bandz Points of agreement:β’ Silly Bandz were popular between July-Oct 2010 .β’ .
E5 .3g Identify a sequence of geologic events using relative -age dating principles . Relative Dating In the same way that a history book shows an order of events, layers of rock (called strata) show the sequence of events that took place in the past . Using a few basic principles, scientists can determine the order in which rock layers formed .
Igneous rock (magma) from the Earth's interior that squeezes/burns its way into existing rock then cools and hardens . *Folding- Occurs when rock layers bend and buckle from Earth's internal forces . *Tilting-occurs when Earth's forces move rock layers until they become slanted . *Cross cutting law .
Section 4 .2 . The relative age of a rock is its age compared to the ages of other rocks . Ex . Mrs . Herrscher is older than her sister and brother . The absolute age of a rock is the number of years that have passed since the rock formed . Ex . Mrs . Herrscher is 33 years old .
Types of Rock Sedimentary rock forms from sediment (sediment- solid particles of rock produced by weathering and erosion by water and wind) * Igneous rock forms from volcanic lava flows * Metamorphic rock - forms from intense heat and pressure Relative Dating of Rocks The relative age of rocks determines the age of rock layers as younger or older, but does not give the exact age .
Relative dating Process of placing object or events in their proper sequence in time . Principle of superposition Oldest rocks in an undisturbed sequence of rock layers are at the bottom of the sequence Unconformities Gaps in rock record where erosion occurred Fossils
6 .2 .2 Relative Dating The Law of Superposition In any undisturbed sequence of strata, the oldest layer is at the bottom of the sequence, and the youngest layer is at the top of the sequence . The Cross-Cutting Law Any feature that cuts across a body of sediment or rock is younger than the body of sediment or rock that it cuts across . NOTE:
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Relative Dating Of Rocks Ppt














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