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what ideas supported Wegener’s idea of continental drift
jigsaw puzzle fit of continents, linked fossil patterns across continents, paleoclimate indicators like glacier movement, matching geologic units of age and composition
The energy that drives Plate Tectonics and is responsible for earthquakes and volcanic eruptions comes from
the Earth's internal heat energy from the core and mantle
describe earth’s lithosphere
cold, rigid, strong, solid
all plate boundaries are associated with
presence of earthquakes
what features are associated with subduction zones
volcanoes, trenches, plates subducting into mantle, large earthquakes
what do you find at divergent plate boundaries?
volcanoes and mostly small earthquakes
the Himalayas are at what plate boundary
continent-continent convergence
The point on Earth's surface directly above the point where an earthquake occurs
epicenter
_______ travel the fastest of energy waves produced by earthquakes and can travel through _______, whereas _______ are slower and can travel through _______.
p-waves; solids, liquids, or gases; s-waves; solids
criticism of wegener’s work
couldn’t explain how or why plates moved
who provided mechanism for continental drift and how?
harry hess, national defense sonar
why did continents move apart?
seafloor spreading
where does magma come up to make new material
midocean ridges
youngest rocks are ___ , older rocks are ____ from the ridge
near, far
describe the magnetism pattern of earth
flips over time, symmetric, barcode pattern, iron points N vs S
inner core composition
solid iron ball
outer core composition
molten iron
mantle composition
silicate rock, peridolite, <3% melt (magma)
crust composition
silicate rock, granite, basalt, sandstone, shale, gneiss
lithosphere
rigid outer layer composed of crust and upper mantle
asthenosphere
beneath lithosphere, mostly solid, flows slightly
what melts rocks?
increased temperature, decreased pressure on hot rocks, chemical reactions with water
what happens during convection?
colder, denser rock from crust sinks; hotter, less dense rock from mantle rises
divergent plate boundary
how pangea broke apart, continental drift, not many volcanoes
convergent plate boundary- oceanic-oceanic
older, cooler, denser descends into subduction zone, volcanic islands on overriding plate
convergent plate boundary- oceanic-continental
denser oceanic crust subducts below continental crust, volcanoes/mountains form on continental plate, violent volcanoes and earthquakes
convergent plate boundary- continental-continental
2 continental collide, none go down, high mountains, no volcanoes
transform fault boundary
plates move laterally past each other between sea floor spreading centers, little volcanism, shallow, damaging earthquakes