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Chapter 10

Permeability
ability of a substance to transmit fluid
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Gaining Stream
stream gains water from inflow of groundwater through streambed
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Losing Stream
streams lose water to the groundwater system by outflow through the streambed
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Darcy's Law
Gradient, Conductivity, Discharge
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Porosity
percentage of void or pore space in a rock body
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Types of porosity
Intergranular= due to space btw grains Bedding Plane= due to space btw bedding of rock layers Solution= due to cavities w/in rocks that have dissolved from mild acids
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Aquifer
Permeable rock strata or sediment that transmit groundwater freely
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Aquitard
Impermeable layer that hinders or prevents water movement
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Cave Formation
groundwater that dissolves soluble rock below the surface, have delicate balance of solution and dissolution and are called living caves- continuously making new cave formations; rock type- travertine
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Karst Topography
dissolved limestone that is very close to the surface, results in landscape features
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Karst Topography Features
Sinkholes, Natural Bridges, Karst Towers
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Hot Springs
water is 11-16 degrees F warmer than average annual air temp of locality. Heated by cooling of igneous rocks below 95% located near active volcanoes
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Geysers
Intermittent hot springs where water erupts with great force
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How do geysers work?
Extensive underground chambers collect water which is heated by igneous rock below
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Thermophiles
Yellowstone; organisms that can survive and thrive in extreme heat environments
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