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The cooling effect of reduced pressure on air as it rises higher in the atmosphere and expands
Polar Cells
Hadley Cells
Adiabatic Cooling
Chemical Weathering
Metamorphic Rocks
Stratosphere
Convergent Plate Boundaries
Parent Material
A convection current in the atmosphere that cycles between the equator and 30N and 30S
Polar Cells
Hadley Cells
Adiabatic Cooling
Chemical Weathering
Metamorphic Rocks
Stratosphere
Convergent Plate Boundaries
Parent Material
A convection cell in the atmosphere formed by air that rises at 60N and 60S and sinks at the poles, 90N and 90S
Polar Cells
Hadley Cells
Adiabatic Cooling
Chemical Weathering
Metamorphic Rocks
Stratosphere
Convergent Plate Boundaries
Parent Material
The Layer of the atmosphere above the troposphere, extending roughly 16 to 50 km (10-31 miles) above the surface of the Earth
Polar Cells
Hadley Cells
Adiabatic Cooling
Chemical Weathering
Metamorphic Rocks
Stratosphere
Convergent Plate Boundaries
Parent Material
Rock material underlying a soil
Polar Cells
Hadley Cells
Adiabatic Cooling
Chemical Weathering
Metamorphic Rocks
Stratosphere
Convergent Plate Boundaries
Parent Material
Plates move towards one another. Continental + Continental = Mountains. Oceanic goes under land, forms mountains and volcanoes. Oceanic goes under other oceanic
Polar Cells
Hadley Cells
Adiabatic Cooling
Chemical Weathering
Metamorphic Rocks
Stratosphere
Convergent Plate Boundaries
Parent Material
Other rick types subjected to high temps and pressure causing physical and chemicals changes. Pressure creates distorted bands called foliation
Polar Cells
Hadley Cells
Adiabatic Cooling
Chemical Weathering
Metamorphic Rocks
Stratosphere
Convergent Plate Boundaries
Parent Material
Breakdown of rocks and minerals by chemical reactions ad dissolving of a rocks chemical elements. Alters newly exposed/primary minerals to make secondary minerals
Polar Cells
Hadley Cells
Adiabatic Cooling
Chemical Weathering
Metamorphic Rocks
Stratosphere
Convergent Plate Boundaries
Parent Material
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