Unit 1 - Plate Tectonics Flashcards
(31 cards)
crust
solid, thin outermost layer
mantle
- two parts (upper and lower)
- solid that behaves like a liquid (it flows)
- thickest layer of the Earth
outer core
- liquid layer of iron and nickel
inner core
- solid dense ball of mostly iron
- innermost layer of earth
solar nebula
- a disc of gas and dust that surround all new stars
- Earth formed from the accretion of metal from a solar nebula
why inner core is solid and outer core is liquid
- denser elements (like iron) sink to the center
- formed inner core, intense pressure from the rest of the Earth keeps inner core from melting
differentiation
- the sinking of metals to form the core and the rising of materials to form the crust/mantle comes from different densities of liquid
- also happens because of the force of gravity
plate tectonics
the process by which pieces of of a strong lithosphere (rigid plates) move around over a weak asthenosphere (weaker substrate)
lithosphere
- Aka rigid plate, made up of crust/upper mantle
- Earth’s surface is a mosaic of 18 plates
- Very rigid/strong
asthenosphere
- weak substrate, allows plates/lithosphere to move
- crust is solid, but asthenosphere acts like a liquid to allow them to move (like silly putty)
why hotter mantle below asthenosphere doesn’t flow as easily
The hotter mantle beneath the asthenosphere does not flow as easily because of the significantly higher pressure at that depth
evidence of continental drift by Alfred Wegener
- North and South America coastlines fit with Europe and Africa
- identical volcanic rocks appear on both sides of the Atlantic
- Fossils of non-swimming animals found on both sides of the modern oceans
why few scientists accepted Wegener’s theory of continental drift
- it requires strong oceanic crust to get out of the way of the moving continents
- was not clear what force would cause continents to move
magnetic reversal
- crystals in lava flows act like tiny compasses and show that the north and south magnetic poles often switched places
- volcanic rocks have allowed us to track magnetic reversals back hundreds of millions of years
observation that led to theory of plate tectonics
- magnetic reversals in volcanic oceanic crustal rocks on the seafloor were found
- allowed us to use the volcanic rock on land to determine their age
- revealed spreading centers on seafloor where new ocean crust forms and moves
- mobility of ocean crust meant that continents could move around without plowing into oceans
mid-ocean ridge
magma from below reaches the surface, cools to form new ocean lithosphere, then moves outwards from the ridge
subduction zone
-Earth isn’t growing, so ocean crust must also be destroyed
- happens at subduction zones where ocean plates dive (subduct) back into the Earth’s interior
- give rise to the highest mountains, deepest trenches, largest earthquakes, and most of earth’s volcanoes
kind of plate boundary San Andreas is
- San Andreas fault is a transform plate boundary between the Pacific and North American plates
- not all boundaries between continental and oceanic crust are plate boundaries (called passive margins)
transform plate boundary
tectonic plates that slide past each other on the surface of the Earth horizontally
conduction
heat transfer through a solid through the spread of vibrations on the atomic scale
convection
- heat transfer through fluid motions of liquids and gasses & solids that flow like a liquid
- leads to fluid circulation as hot volumes rise and cool volumes sink
radioactive heat
heat transfer through electromagnetic waves (light) through a transparent (clear) medium
when a solid can convect
- Earth’s mantle is a solid (crystalline structure) but flows like a fluid and thus transfer heat through convection
- called solid state convection
what drives plate tectonics
- plate tectonics is the surface expression of mantle convection (circulation of hot/cold fluid)