Earth Science, Tarbuck Chap 7 Flashcards
force applied equally in
all directions is called
Confining Pressure
What does Confining pressure do to rocks
compacts mineral grains to reduce the volume of rock bodies. Note that Confining Pressure does not cause Deformation
Deformation is caused by
Differential Stress
3 types of differential Stress
Compressional, Tensional, Shear
What is compressional Stress
squeezes a rock mass. Associated with convergent boundaries
What is Tensional Stress
pulls apart rock bodies. Associated with Divergent boundaries
What is Shear Stress
movement of one part of a
rock body past another. Associated with transform boundaries
What is Strain?
When differential stress changes a rock’s shape, the resulting deformation is called strain.
What is another way other than strain Mineral Grains change responding to Differential Stress
Recrystallization of the Crystals caused by movement of atoms from high to low stress
What are the types of deformation that lead to strain
elastic, brittle, and ductile
What is elastic deformation
A temporary shape change that is self-reversing after the force is removed, so that the object returns to its original shape
What is Brittle Deformation
When a rock is deformed beyond its ability to respond elastically, rocks that break into smaller pieces undergo Brittle deformation
What is Ductile Deformation
slippage along surfaces of weakness within the rock and the gradual reshaping of mineral
grains. This can cause some rocks to flow very slowly
Temperatures are higher,
Rocks can undergo Ductile deformation more easily
Order from smallest to largest temperature gradients and why: Mid-ocean Ridge, Hot spots, Subduction zones
Subduction zones(Cool oceanic crust goes deeper into the mantle, leading to small temperature gradients), Hot Spots(Both Mid-ocean ridges and Hot spots have large temperature gradients but mid-ocean ridges typically have the most elevated geotherms because their unusually thin crust allows hot mantle to push up near the surface), Mid-ocean Ridges
When temperatures a lower,
Brittle Deformation is common
As confining pressure increases,
Rocks are harder to break
What are Folds
Along convergent plate boundaries, rock strata are often
bent into a series of wavelike undulations
What is an anticline fold
arching of sedimentary layers
What is a Syncline Fold
Downfolds or troughs