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What are the Earths chemical layers
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APES Unit 4

QuestionAnswer
What are the Earths chemical layers -Crust -Mantle -Core
Crust The outermost layer, composed of oxygen, silicon, aluminum, magnesium, iron, etc
Mantle The layer of Earth above the ocre, composed of silicate rocks, magnesium, and iron
Core The innermost zone of Earth's interior, composed mostly of iron and nickel
Earths Physical Layers -Lithosphere -Asthenosphere -Mesosphere -Outer core -Inner core
Lithosphere Solid
Astehnosphere Semi-molten rock
Mesosphere Composed of molten rock (Magma) that slowly circulates in convection cells
Outer Core Liquid metal; movement is responsible for earth's magnetic field
Inner core Solid metal due to pressure
Hot Spots When heat causes plumes of hot Magma to well upward from the mantle
Transform Fault Boundary An area where tectonic plates move sideways past each other leading to a fault or a fracture in the rock of the crust
Divergent plate boundary An area beneath the ocean where tectonic plates move away from each other
Seafloor spreading The formation of new ocean crust as a result of Magma pushing upward and outward from Earth's mantle to the surface
Convergent Plate Boundary An area where plates move towards one another and collide
Subduction When one plate goes under another plate
Igneous rocks Rock formed directly from cooled magma EX: Granite
What rock is the main type in the ocean Basalt
What rock is the main type in continental Granite
Sedimentary Rocks Rock that forms when sediments such as muds, sands, or gravels are compressed by overlying sediments EX: Conglomerate
Metamorphic Rocks Rock that forms when sedimentary rock, igneous rocks, or other metamorphic rock is subjected to high temps and pressure EX: Gneiss
Physical weathering Mechanical breakdown of rocks and minerals, usually caused by water, wind, or variations in temperature such as seasonal freeze thaw cycles
Chemical weathering Breakdown of rocks and minerals by chemical reactions, the dissolving of chemical elements from rocks, or both these processes
Erosion Physical removal of rock fragments form a landscape or ecosystem
Soils in order from highest to lowest -O -A -E -B -C
O horizon Organic horizon at the surface, with organic detritus in various stages of decomposition, the bottom layer composed of humus
A horizon The top layer of soil, compromising organic material and minerals that have been mixed together, sometimes called topsoil
E horizon A zone of leaching or eluviation, found in some acidic soils under the O horizon, or less often, the A horizon
B horizon Commonly known as subsoil, primarily mineral material with very little organic matter
C horizon The least weathered soil horizon, always below the b horizon, similar to he parent material
REMINDER MOST SOILS HAVE EITHER AN O HORIZON OR AN A HORIZON AND USUALLY NOT BOTH
Water holding capacity Amount of water soil can hold against the draining force of gravity
Watershed Area of land that drains into a particular body of water
Albedo Areas of the earth that reflect more solar energy
High albedo Ice, snow, light color
Low albedo Asphalt, dark colors
How much is the earth tilted 23.5 degrees
What are the 2 primary gasses in the atmosphere Nitrogen and Oxygen
Layers of the Earth's atmosphere -Troposphere -Stratosphere -Ozone layer -Mesosphere -Mesosphere, Thermosphere, Exosphere
Trophosphere Layer of the atmosphere closest to the surface of the Earth and is the densest layer -Where Earth's weather occurs -Where we live
Stratosphere Layer of the atmosphere above the troposphere -Where you fly a plane
Ozone layer Located between the troposphere and stratosphere that absorbs most of the suns UV ryas
Adiabatic Cooling The cooling effect of reduced pressure on air as it rises in the atmosphere and expands
Adiabatic Heating Increased pressure on air as it sinks toward the surface of the earth and decreases in volume
Latent Heat Release The release of energy when weather vapor in the atmosphere condenses into liquid water
Atmospheric Convection currents Global patterns of air movement that are initiated by the unequal heating of the Earth-regions near the earth receive more solar radiation than regions near the poles
Hadley cells Convection currents that cycle between the equator and 30 degrees N and 30 degrees S
Polar Cells Convection currents formed by air rising at 60 degrees N and 60 degrees S
Ferrell Cells Convection currents found between Hadley and polar Cells fitting in like a gear
Coriolis effect The deflection of an object's path due to the rotation of the earth
Gyre A large-scale pattern of water circulation on the oceans surface that moves clockwise in the northern hemisphere and counterclockwise in the southern hemisphere
Thermohaline Temperature and Salt
Created by: sydeboswell
 

 



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