APES Ch 8- Earth Systems

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Created by:

annav18  on April 30, 2012

Subjects:

APES, AP Environmental Science

Description:

This is vocabulary from Chapter 8 of Friedland and Relyea AP Textbook

Classes:

APES, APES Elmore, Mastbaum APES 2013

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APES Ch 8- Earth Systems

mantle
the layer of the earth between the crust and the core
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Definitions

mantle the layer of the earth between the crust and the core
magma molten rock
asthenosphere located in the outer part of the mantle and is composed of semi-molten, ductile rock
lithosphere a 60 mile think layer that includes the solid upper mantle as well as the crust
crust the outermost layer of the lithosphere
hot spots places where molten material from the mantle reaches the lithosphere
plate tectonics Earth's lithosphere is divided into plates, most of which are in constant motion
tectonic cycle the sum of the processes that build up and break down the lithosphere
subduction the process of one plate passing under another
volcano a vent in Earth's surface that emits ash, gases, and molten lava
divergent plate boundaries when oceanic plates move apart as if on a giant conveyor belt
seafloor spreading when the magma rises up and outward, forming new rock. This process brings important elements such as copper & lead to the surface of the Earth
convergent plate boundaries when plates move toward one another and collide, and the lighter layer goes on top of the heavier, subducted layer
transform boundary a plate boundary where two plates move/slide past each other in opposite directions
fault a fracture in rock across which there is movement
fault zones large expanses of rock where movement has occurred
earthquakes sudden movements of Earth's crust followed by a series of shocks
seismic activity another word for fault zones
epicenter the exact point on the surface of Earth directly above the location where the rock ruptures
richter scale a measure of the largest ground movement that occurs during an earthquake
minerals solid chemical substances with uniform structures that form under specific temperatures and pressures They are usually compounds
igneous rocks rocks that form directly from magma. They are classified as basaltic or granitic [i.e granite, basalt]
sedimentary rocks rocks that form when sediments like mud, sand, or gravel are compressed by overlying sediments. It forms over long periods of time. This layer often holds fossils [i.e. sandstone, limestone]
metamorphic rocks rocks that form when sedimentary rocks, igneous rocks, or other metamorphic rocks are subjected to high temperatures and pressures [i.e. marble, quartzite]
physical weathering Weathering in which solid rock is fragmented by mechanical processes that do not change its chemical composition.
chemical weathering The process that breaks down rock through chemical changes
acid rain rain containing acids that form in the atmosphere when industrial gas emissions (especially sulfur dioxide and nitrogen oxides) combine with water
erosion the physical removal of rock fragments from a landscape or ecosystem
deposition the accumulation or depositing if eroded material such as sediment, rock fragments, or soil
soil a mix of geologic and organic compounds. Often called "Earth's dynamic membrane"
parent material the rock material underlying soil from which its inorganic components are derived
horizons soil layers
O horizon the top-most soil layer that has organic matter in various stages of decomposition
A horizon the topsoil layer that is a zone of overlying organic material and underlying mineral material
B Horizon a zone of accumulation of metals and nutrients, commonly known as subsoil
C horizon the least weathered soil horizon that is similar to the parent material
cation exchange capacity the ability of a particular soil to absorb and release cations. This is sometimes referred to as the nutrient holding capacity
base saturation a measure of the proportion of soil bases to soil acids, expressed as a percentage
soil degradation the loss of some or all of the ability of soils to support plant growth
ores concentrated accumulations of minerals from which economically valuable materials can be extracted
metals elements with properties that allow them to conduct electricity and heat energy and perform other important functions
reserve he known quantity of a resource that can be economically recovered
strip mining the removal of "strips" of soil and rock to expose ore and is used when the desired ore is relatively close to Earth's surface and runs parallel to it
tailings mining spoils
open pit mining the creation of a large pit or hole in the ground that is visible from Earth's surface, and is used when the resource is close to the surface but extends beneath the surface both horizontally and vertically
mountaintop removal when miner remove the entire top of a mountain with explosives, this is really bad for the Earth
placer mining the process of looking for metals and precious stones in river sediments
subsurface mining begins with a horizontal tunnel dug into the side of a mountain or other feature containing the resource. From here, vertical shafts are drilled and elevators are used to bring miners down to the resource and back to the surface

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