chapter 12 earths history and interior Flashcards
anthropocene
the age of human transformation of earths biological and physical systems
___ of earths land surface taken to grow food for people
40%
the universe began about ___ years ago with the big bang
13.8 billion
distances between and across galaxies are measured in _____ ____
light years
our solar system formed about ____ years ago
4.6 billion
crust
earths molten surface that cooled and hardened into a rigid surface
volcano
a mountain or hill formed by eruptions of lava and rock fragments
cyanobacteria
photosynthetic bacteria
stromatolites
colonies of cyanobacteria
how old is earth
4.6 billion years old
uniformitarianism
the principle that the same gradual and nearly imperceptible processes operating now have operated in the past
relative vs absolute age
relative- compares the age of one object with the age of another without specifying how old either is
absolute- an age that is specified in years before the present
superposition principle
in rock layers, the oldest rocks are located at the bottom and the youngest rocks are at the top
radiometric dating
assigning ages to materials based on the radiometric half life of unstable elements within the material
half life
the time it takes for half of the unstable elements to decay
geothermal gradient
temperature of earths interior increases with depth
seismic wave
energy released by earthquakes that travel through earths interior
earthquake
sudden shaking of the ground caused by movements of the earths crust
3 principle layers of earths interior
core
mantle
lithosphere
inner core vs outer core
inner- composed of solid iron and nickel, extends from earths center to about 5150 km below earths surface
outer- composed of liquid iron and nickel, extends to about 2900 km below earths surface
magnetic north pole vs geographic north pole
magnetic- found where the magnetic field enters the planet
geographic- found at earths axis of rotation
lower mantle
layer of heated and slowly deforming solid rock that lies between the base pf the crust and the outer core, lies 2900-200 km below earths surface
asthenosphere
found between depths of 100 and 200 km
lithosphere
the crust and the lithospheric mantle beneath it, extending to a depth of about 100 km on average
crust
the rigid outermost portion of the earth
continental crust vs oceanic crust
continental- makes up continents, composed mainly of granite
oceanic- beneath the oceans, composed mainly of basalt
granite vs basalt
granite- a silica rich rock made up of coarse grains
basalt- a dark heavy, fine grained volcanic rock
magma vs lava
magma- melted rock below earths surface
lava- magma that spills onto the surface of earths crust
moho
boundary that separates crust from lithospheric mantle; lies about 35 km deep
plate tectonics
theory addressing the origin, movement. and recycling of lithospheric plates and the landforms that result