Quiz 10 Flashcards
Absolute Geologic Age
precise dates of many types of geologic events
Relative Geologic Age
the age of one event relative to another
Principle of Original Horizontality
-sediments are deposited in horizontal or near-horizontal layers
-therefore, non horizontal layers have generally been folded or tilted from their original positions
Principle of Superposition
-in any given succession of sedimentary rock layers lying in their original horizontal position the rocks at the bottom of the sequence are older than those lying above
Principle of Original Lateral Continuity
-sediments are deposited in layers that continue laterally in all directions until they thin out as a result of nondeposition
-or until they reach the edge of the basin in which they are deposited
-therefore, if you find a layer that abruptly ends, something has cut this layer after it was deposited (faults, dikes, and erosion) can truncate otherwise laterally continuous layers
Principle of Cross-Cutting Relations
any geologic feature is younger than any feature that it cuts
Principle of Inclusions
an inclusion in a rock is older than the rock containing it
Compressive stress
causes shortening and is an important type of stress at convergent tectonic plate boundaries
Tensional stress
the principal stress at divergent boundaries, causes stretching
Shear stress
causes one side of a body to slide past the other, and is the principal type of stress along transform-fault plate boundaries
Elastic strain
temporary; if the stress is removed, the object snaps back to its original shape (think stretched rubber band)
Plastic strain
permanent; if the stress is removed, the original size or shape is not restored (bending a piece of soft wire)
Brittle deformation
a rock undergoing elastic strain which can suddenly break (a dry stick)
Ductile
a rock that undergoes much plastic strain without rupturing (bent wire)
Outcrop
visible exposures of bedrock or other geologic formations at the surface of the earth