Metamorphism Flashcards
Regional metamorphism
During mountain building, great quantities of rocks are subjected to pressures and high temps associated with large scale deformation
Contact metamorphism
Parents rock baked by magma rising from
below
Confining pressure
Forces are equally applied in all directions
Differential stress
Forces unequally and in different directions
Foliated Texture
Any nearly flat arrangement of mineral grains or structural features within a rock
Non foliated texture
A result of contact metamorphism
Theory of plate tectonics - The earth’s interior can be divided into layers based on
Chemical properties and physical properties
Continental drift hypothesis
Prior to the late 1960’s, most geologists held the view that the ocean basins and continents had fixed geological positions
Lithosphere
Rigid
Responds to energy by cracking or breaking
Divided into seven different plates
Plate boundaries = where plates meet
Plates not defined entirely by a single contine
Lithosphere Plates rest on plastic (fluid) Asthenosphere
Asthenosphere - solid, but mobile
Less rigid (plastic)
Responds to energy by flowing
Convection current
With boiling water
Hot water less dense - rises
Cooler water denser - sinks
Divergent plate boundaries
Where plates move apart
Results in
Ocean floor spreading - at oceanic plate boundaries
Rift lake/valley formation - at continental plate boundaries
Convergent plate boundaries
Where two plates move toward each other
Resulting in
Collision of oceanic lithosphere and continental crust - oceanic lithosphere descends beneath an overriding plate eventually to be reabsorbed into the mantle; or
Collision of two continental blocks = mountain building
Transform plate boundaries
Where two plates grind past each other
Can cause earthquakes
Plates are constantly changing
Earth’s total surface area does not change, the size and shape of individual plates are constantly changing