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Age and Movement of Rocks
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How old is old? Relative Dating a method of determining if an object is older or younger than another object.
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Layer upon Layers a principle that states younger rock layers lay on top older rock layers. Superposition
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Column of Ages geologic column the arrangement of rock layers with the oldest at the bottom.
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Disturbing Forces Geologic Columns are not always horizontal. Forces from inside the Earth often disturb the layers. There are 4 types of disturbed rock layers.
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Disturbed Rock Layers A fault is a break in the Earth’s crust that moves rock layers in different directions.
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Disturbed Rock Layers Folding occurs when rock layers are bent and buckle.
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Disturbed Rock Layers Intrusions are when lava from inside Earth squeezes into cracks in rock layers and cool.
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Disturbed Rock Layers Tilting of rock layers occur when internal forces cause the rocks to slant one direction.
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are breaks in the geologic column. 3 types: a. Disconformity (missing sedimentary rock layers) b. Nonconformity (sedimentary on Igneous) c. Angular Unconformities
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http://www.wwnorton.com/college/geo/ani mations/geologic_history.htmhttp://www.wwnorton.com/college/geo/ani mations/geologic_history.htm http://www.wwnorton.com/college/geo/ani mations/types_of_unconformity.htmhttp://www.wwnorton.com/college/geo/ani mations/types_of_unconformity.htm
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