Quiz over Chapter 10 Flashcards
(41 cards)
Deformation
refers to all changes in the shape or position of a rock body in response to stress
Rock or geologic Structures
features that result from forces generated by the interactions of tectonic plates
(includes folds, faults, and joints)
Stress
the force that deforms rocks
Magnitude
a function of the amount of force applied to a given area
When stresses on a rock exceed its strength….
the rock deforms by flowing, folding, fracturing, or faulting
Confining pressure
stress applied to uniformity in all directions
squeezes rocks, making them stronger and harder to break
differential stress
Stress applied unequally in different directions
Types of Stress
Compressional
Tensional
Shear
Compressional Stress
squeezes a rock and shortens a rock body
tensional stress
pulls apart a rock unit and lengthens it
Shear stress
Produces a motion similar to slippage that occurs between individual playing cards when the top of the stack is moved relative to the bottom
Strain
change in shape of a rock caused by differential stress
strained bodies lose their original configuration during deformation
Elastic deformation
rock returns to nearly its original size and shape when the stress is removed
ductile deformation
bends
brittle deformation
breaks
Temperature
Higher temp deform by ductile deformation {deep}
Cooler rocks form by brittle deformation {on surface or high up in crust}
Factors that affect rock strength
Rock type
Time
Temperature
Pressure
Rock type
Crystalline igneous rocks generally experience brittle deformation, whereas sedimentary and metamorphic rocks experience ductile deformation
Time
forces applied over a long period of time generally result in ductile deformation
Joints
cracks in the rocks resulting from the rock being stretched and pulled apart
created columns
Faults
fractures in the rocks where rocks on one side of the fault are displaced relative to the rocks on the other side of the fault
Folds are evidence
that rocks can bend without breaking
result of deformation in high temp high pressure environments
Most folds are
result from compressional stresses that result in a shortening and thickening of the crust
Anticlines
upfolded or arched sedimentary layers
Oldest strata in the center