APES Unit 4: Earth Systems and Resources

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Key terms to know for AP Environmental Science Unit 4: Earth Systems and Resources.

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54 Terms

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core

dense mass of solid nickel, iron, and radioactive elements that release massive amounts of heat

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mantle

liquid layer of magma surrounding core, kept liquified from core’s intense heat

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asthenosphere

solid, flexible outer layer of mantle

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lithosphere

thin, brittle layer of rock floating on top of mantle

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crust

earth’s surface, very outer layer of lithosphere

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divergent plate boundary

plates move away from each other bc of magma rising

  • forms mid-oceanic ridges, volcanoes, seafloor spreading, rift valleys

<p>plates move away from each other bc of magma rising</p><ul><li><p>forms mid-oceanic ridges, volcanoes, seafloor spreading, rift valleys</p></li></ul><p></p>
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convergent plate boundary

plates move toward each other, leads to subduction

  • forms mountains, island arcs, earthquakes, volcanoes

<p>plates move toward each other, leads to <u>subduction</u></p><ul><li><p>forms mountains, island arcs, earthquakes, volcanoes</p></li></ul><p></p>
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transform fault boundary

plates slide past each other in opposite directions

  • forms earthquakes

<p>plates slide past each other in opposite directions</p><ul><li><p>forms earthquakes</p></li></ul><p></p>
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oceanic-oceanic subduction zone

one oceanic plate subducts under another

  • forms mid-ocean volcanoes, island arcs, off-shore trenches

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oceanic-continental subduction zone

oceanic plate subducts under continental plate, melts back into magma

  • forms coastal mountains, volcanoes on land, trenches, tsunamis

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continental-continental subduction zone

one continental plate subducts under another, forces surface crust up

  • forms mountains

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Ring of Fire

pattern of volcanoes all around Pacific plate

<p>pattern of volcanoes all around Pacific plate</p>
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hotspots

areas of hot magma constantly rising up to lithosphere 

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soil

mix of geological and organic components

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humus

main organic part of soil, broken down organic matter

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weathering

breakdown of rocks in 3 ways (physical, biological, chemical), forms soil

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erosion

transport of weathered rock carried by wind and rain

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parent material

sometimes called bedrock, rock that underlies soil

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O-horizon

layer of organic matter on top of soil

  • provides nutrients and limits H2O loss to evaporation

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A-horizon

topsoil, layer of humus from parent material

  • has most biological activity, breaking down organic matter

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B-horizon

subsoil, lighter layer below topsoil

  • contains some nutrients, little to no organic matter

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C-horizon

least weathered soil closest to parent material

  • most intact rock

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soil degradation

loss of ability of soil to support plant growth

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compaction

compression of soil by machines, grazing livestock, and humans

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nutrient depletion

repeatedly growing crops on same soil, removing key nutrients over time

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soil texture

% of sand, silt, and clay in soil, always adds up to 100%

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porosity

amount of pore space a soil has

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permeability

water’s ability to drain through soil 

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H2O holding capacity

how well water is retained/held by soil

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troposphere

0-16 km, change in weather occurs here, most dense, temp decreases 

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stratosphere

16-60 km, thickest layer of O3 here, absorbs UV rays, temp increases

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mesosphere

60-80 km, even less dense, coldest place on Earth, temp decreases

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thermosphere

80-800 km, hottest place on Earth, absorbs x-rays, temp increases

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Coriolis effect

makes objects traveling long distances around Earth appear to move at a curve rather than straight line due Earth’s spin

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watershed

body of land that drains into a body of water

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Chesapeake Bay Watershed

6 state region that drains into a series of streams/rivers and eventually into Chesapeake Bay

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cover crops

a buffer plant to hold soil in place, prevents runoff

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topographic map

2D representation of 3D space, each line represents elevation

<p>2D representation of 3D space, each line represents elevation</p>
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elevation

distance above sea level

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relief

distance between point A and point B

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insolation

amount of solar radiation reaching an area, measured in Watts/m²

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latitude

distance from equator

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solstice

North or South hemispheres maximally tilted toward sun (Summer/Winter)

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equinox

North and South hemispheres equally face sun

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albedo

proportion of light that’s reflected by surface

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urban heat island

urban areas are hotter than surrounding rural area

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rain shadow effect

warm, moist air from ocean hits windward side of mountain, dry air descends down leeward side of mountain

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gyres

large ocean circulation patterns due to global wind (clockwise North, counter South)

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upwelling zones

areas of ocean where winds blow warm surface water away from land, drawing up colder, deeper water to replace

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thermohaline circulation

connects all world’s oceans, mixing salt, nutrients, and temp

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El Nino Southern Oscillation

pattern of shifting atmospheric pressure and oceancurrents in Pacific between South Amer and Australia/Southeast Asia

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normal year

trade winds blow hot equator water W ← E, productive fisheries

<p>trade winds blow hot equator water W ← E, productive fisheries</p>
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El Niño year

trade winds weaken and reverse W → E, suppressed upwelling off South Amer coast, damaged fisheries

<p>trade winds weaken and reverse W → E, suppressed upwelling off South Amer coast, damaged fisheries</p>
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La Niña year

stronger than normal trade winds W ← E, increased upwelling off South Amer coast, productive fisheries

<p>stronger than normal trade winds W ← E, increased upwelling off South Amer coast, productive fisheries</p>