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A horizon
topsoil
B horizon
subsoil
C horizon
the least-weathered soil horizon, which always occurs beneath the B horizon and is similar to the parent material
CEC (cation exchange capacity)
the ability of a particular soil to absorb and release cations
chemical weathering
the process that breaks down rock through chemical changes
convergent
a tectonic plate boundary where two plates collide, come together, or crash into eachother
divergent
an area beneath the ocean where tectonic plates move away from each other
E horizon
the zone of leaching that forms under the O horizon or, less often, the A horizon
epicenter
the point on the earth’s surface directly above the focus of an earthquake
erosion
processes by which rock, sand, and soil, are broken down, and carried away (i.e. weathering, glaciation)
hot spot
an area where magma from deep within the mantle melts through the crust above it
humus
material formed from decaying leaves and other organic matter
igneous rocks
a type of rock that forms from the cooling of molten rock at or below the surface
lithosphere
a rigid layer made up of the uppermost part of the mantle and the crust
metamorphic rocks
a type of rock that forms from an existing rock that is changed by the heat, pressure, or chemical reactions
O horizon
the top layer of the surface containing inorganic solids, decaying organic matter, and living organisms
parent material
the rock material from which the inorganic components of a soil are derived
permeability
how easily substances can move through something
physical weathering
the mechanical breakdown of rocks and minerals
saturation point
the stage at which something can no longer hold more (usually water)
seafloor spreading
the process that creates new sea floor as plates move away from each other at the mid-ocean ridges
sedimentary rocks
a type of rock that forms when particles from other rocks or the remains of the plants and animals are pressed and cemented together
soil degradation
the loss of some air of a soil’s ability to support plant growth
subduction
the process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle at a convergent plate boundary
transform fault
boundary between two plates that are sliding past each other