Core
Dense mass of solid nickel, iron, and radioactive elements that release massive amounts of heat
Mantle
Liquid layer of magma surrounding core, kept liquified by intense heat from core
Asthenosphere
Solid, flexible, outer layer of mantle, beneath the lithosphere
Lithosphere
Thin, brittle layer of rock floating on top of mantle
Crust
Very outer layer of the lithosphere, earth’s surface
Divergent
Plates move away from each other
Convergent
Plates move towards each other, leads to subduction
Transform
Plates slide past each other in opposite directions
Ring of Fire
Pattern of volcanoes all around pacific plate
Transform faults
Likely location of earthquakes
Hotspots
Areas of especially hot magma rising up to the lithosphere
Soil Horizon O
Organic, grass/leaves/plants, 0-0.1 meters
Soil Horizon A
Topsoil/humus, 0.1 m to 0.3 m
Soil Horizon E
Leaching, loss of organic matter/lighter in color, below A
Soil Horizon B
Subsoil, more clay than topsoil/lower levels of organic matter/blocky, .3 m to 1 m
Soil Horizon C
Weathered rock, 1 m to 1.3 m
Soil Horizon R
Bedrock
Three soil particles
Sand, silt, clay
Soil texture
The % of sand, silt, and clay in soil
Porosity
How much (volume of) water that a soil sample can hold
Permeability
How easily water drains through soil
Too sandy for growth
70%
Too much clay for growth
30%
Ideal soil for most plant growth
40-40-20
Percent of nitrogen in the Earth’s atmosphere
78%
Percent of oxygen in the earth’s atmosphere
21%
Percent of argon in the earth’s atmosphere
0.93%
Percent of water vapor in the earth’s atmosphere
0-4%
Percent of carbon dioxide in the earth’s atmosphere
0.04%
Exosphere
Outermost layer of the atmosphere where it merges with space
Thermosphere
Hottest temperature layer of the atmosphere, absorbs harmful radiation, aurora borealis
Mesosphere
Middle layer, 60-80km up
Stratosphere
Thickest O2 layer, 16-60 km
Troposphere
Weather occurs here, most of gas is here, 6-16 km
Coriolis effect
Deflection of the objects traveling through the atmosphere due to the spin of the earth
What direction does wind between 0-30 degrees move
E→W
What direction does wind from 30-60 degrees move
W→E
Hadley cells
Large-scale atmospheric circulation patterns
Watershed
A land area that drains water to a common body of water, such as a river, lake, or wetland
Insolation
Incoming solar radiation reaching a given area, measured in watts/m²
Albedo
Proportion of light
Asphalt has…
Low albedo because it absorbs heat
Windward side of rainshadows
Warm, most air from oceans hits the mountain. Full of greenery
Leeward side
Dry air descends down leeward side of the mountain warming as it sinks
Gyres
Large ocean circulation patterns due to global winds
Upwelling zones
Areas of ocean where winds blow warm surface water away from a land mass, drawing up colder war to replace it
Thermohaline circulation
Connects all the world oceans, mixing salt, nutrients, and transportation throughout
El Nino
Trade winds weaken, then reverse. W→E. Brings heat and precipitation to the Amazons, suppressed upwelling off the South Asian coast
La Nina
Stronger than normal trade winds, W←←←E, increased upwelling of the South Asian coast brings cooler than normal conditions