Ch. 14 Flashcards
sea floor spreading
midocean ridges are formed by currents of magma rising up from the mantle; volcanic eruptions create new basaltic ocean floor that then spreads away laterally fro the ridge. mid ocean ridges contain the newest crust formed.
subduction
at oceanic trenches, older lithosphere descends into the asthenosphere where is is recycled. sediments furthers from the ridges are the oldest
plate tectonics
a framework with which we can understand and relate a wide range of internal processes and topographic patters
plates
move slowly over the asthenosphere. cold and rigid and therefore deformed significantly only at the edges and only where one plate interacts with another
divergent plate boundaries
magma from the asthenosphere wells up in the opening between places, this upward flow of molten material produces a line of volcanic vents that spill out basaltic lava onto the ocean floor. plates move away. usually represented by a mid ocean ridge
convergent boundary
plates collide and are sometimes referred to as destructive boundaries. removal or compression of the surface of the crust. mountain ranges, volcanoes, and oceanic trenches oceanic lithosphere is more dense than continental so it always under rides the continental plate
oceanic-oceanic convergence
subduction also takes place, one plate goes beneath the other and a trench is formed. volcanic arc is typical here
continental-continental convergence
no subduction takes place, forms mountain ranges,
transform boundaries
two plates slip past each other, fault lines
volcanism
a general term that refers to all the phenomena connected to the origin and movement of molten rock
magma
molten material below the surface
shield volcanos
basaltic lava tends to flow quite easily over the surrounding surface forming broad low lying shelf volcanos built up of later upon layer of solidified lava flow. little pyroclastic material, mountains with gentle sloping side
composite volcano
emit higher silica “intermediate” lava such as andesite often erupt ant explosively and tend to develop into symmetrical steep sided volcanoes
lava domes
plug domes, masses of very think viscous lava that does not flow very well. lava that bulges from a vent. some form inside of composite volcanoes.
cinder cones
the smallest peak, cone shaped peaks built by the unconsolidated pyroclastic materials that are ejected from the vent.