core
dense mass of nickel, iron, and radioactive elements that release massive amounts of heat; inner core is solid outer core is liquid
mantle
soft solid of magma surrounding core, kept soft by intense heat from the core
asthensphere
solid, flexible outer layer of mantle, beneath the lithosphere
lithosphere
thin, brittle layer or rock floating on top of mantle (broken up into tectonic plates)
crust
very outer layer of the lithosphere
convergent tectonic plate
mostly granitic rock
divergent tectonic plate
mostly basaltic rock
divergent plate boundary
plates move away from each other, rising magma plume from mantle forces plates apart, forms mid- oceanic ridges, volcanos, seafloor spreading, and rift vallys (on land)
transform fault plate boundary
plates slide past each other in opposite directions, forms earthquakes
convergent plate boundary
plates move toward each other, leads to subduction (one plate being forced beneath another) when one plate is oceanic, forms mountains, islands, arcs, earthquakes, and volcanos
magma
heated by the earth's core, rises toward the lithosphere, when cooled and expanded it forces oceanic plates apart (subduction zone), leads to mid-ocean ranges, volcanos, or seafloor spreading
oceanic- oceanic
one plate subducts underneath the other
oceanic- continental
dense oceanic plate subducts beneath cont. plate melts back into magma
continental- continental
one plate subducts underneath other, forcing surface crust (mountains)
ring of fire
pattern of volcanos all around pacific plate
transform faults
likely location of earthquakes
hotspots
areas of esp. hot magma rising up to lithosphere
soil
mix of geologic (rock) and organic (living) components, sand, silt, clay
humus
main organic part of soil (broken down biomass like leaves, dead animals, waste, etc.)
nutrients
ammonium, phosphates, nitrates
water
filters rain water+ runoff by traping pollutants in pore spaces+ plant roots
nutrient recycling
home to decomposers that break down dead organic matter+ return nutrients to the soil
habit
provides habit for organisms like earthworms, fungi, bacteria, moles, slugs
weathering
breakdown of rocks into smaller pieces physical, biological (roots of trees cracks rocks), chemical (acid rain, acids from moss/ lichen)
erosion
transport of weathered rock fragments by wind and rain,carried to new location and deposited (deposition)
parent materials
soil pH, nutrient content
topography
steep slope= too much erosion; more level ground= deposition
climate
warmer= faster breakdown of organic matter; more precipitation= more weathering, erosion and deposition
organisms
soil organisms like bacteria, fungi, worms breakdown organic matter
o- horizon
a layer of organic matter (plant roots, dead leaves, animal waste, etc) on top soil
a- horizon
aka top soil (layer of humus (decomposed organic matter) and minerals from parent material)
b- horizon
aka subsoil; lighter layer below topsoil, mostly made of minerals with little to no organic matter
c- horizon
least weathered soil that is closest to the parent material, sometimes called bedrock
loss of topsoil
tiling (turning soil for ag.) and loss of vegetation disturb soil and make it more easily eroded by wind and rain
soil degration
the loss of the ability of soil to support plant growth
compaction
compression of soil by machines( tractors, bulldozers, etc) grazing livestock, and humans reduces ability to hold moisture
nutrient depition
repeatedly growing crops on the same soil removes key nutrients (N, P, K, Na, Mg) over time
geologic rock portion of soil
made up of 3 particles (sand> silt> clay)
soil texture
The percent of sand silt and clay in soil (always adds to 100%)
porosity
The amount of pore space a soil has more sand in soil= more porous/ higher porosity (easier for water and air to enter) more clay in soil= less porous/ higher porosity (harder for water and air to enter) nthe pore space within a soil
permebility
How easily water drains through soil, more porous/ higher porosity= more permeable/ higher permeability
H20 holding capacity
how well water is retained or held by soil, more porous/ higher permeability= lower H20 holding capacity
soil fertility
ability of soil to support plant growth