Acitivity 1 review Flashcards
change in the original shape and size of a rock.
Deformation
deformation of materials from stress; ratio of changes in length to the original length
strain
successive stages of deformation ( 3 enumerate )
elastic, ductile, fracture
irereversible strain wherein the material breaks.
fracture
process of rock formations ( 2 enumerate )
folding and faulting
wherein the strain is reversible
elastic
wherein the strain is irreversible
ductile
occurs when rock pushed towards each other from opposite sides, become ductile solids, produced by horizontal comprehensive stresses
folding
force acting on a material that produces a strain
stress
stress where the forces act equally from all directions.
pressure
refers to the stress that is not equal from all directions
differential stress
common types of folds ( 2 enumerate )
anticline, syncline
fold that is arched upward, ridge
anticline
fold that is arched downward, through
syncline
fracturing and displacement of brittle rocks along a fault plane
faulting
types of stress ( enumerate 3 )
tension, compression, shearing
stretched rocks
tension
pushes rocks together
compression
causes masses of rocks to slip
shearing
the blocks are pulled apart
normal fault
the blocks are pushed together
reverse fault
two blocks slide past each other
transform fault
seafloor on other side of ridges spread away from the crest
SEAFLOOR SPREADING
contains crust and uppermost part of mantle
LITHOSPHERE
composed of partially melted rocks in upper mantle that acts in a plastic manner.
ASTHENOSPHERE
Plates of lithosphere are moved around by underlying hot mantle.
PLATE MOVEMENT
concept of horizontal or upwards and downward movement of mantle.
CONVECTION CELLS
tectonic plates moving away from each other
DIVERGENT BOUNDARIES
tectonic plates converging
CONVERGENT BOUNDARIES
shearing forces causes rocks to slide past one another.
TRANSFORM BOUNDARIES
stretching and thinning of rocks resulting in faulting
TENSIONAL FORCES
forms mountain but has no volcanism.
CONTINENT - CONTINENT
results in chain of volcanoes
CON TINENT - OCEANIC
Causes to sink into mantle forming subduction zone
OCEAN - OCEAN
very deep depresssion in the ocean floor
TRENCH
An astronomer used biology and geology to describe pangea and continental drift
ALFRED WEGENER
single landmass out of all earth’s continent
PANGEA
located near the south pole during the assembly of Pangea exhibit evidence of glaciation
PALEOCLIMATES
rich placer deposits of gold are found on the ghana coast but the source are in brazil
PLACER DEPOSITS
sedimentary rocks formed out of deposits of glaciers
TILLITE DEPOSITS
helpful for exploring and mapping the ocean by sound wave
SONAR
canadian geophysicist combined continetal drift and seafloor spreading
JOHN TUZO