Earth science 6.1

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6.1 Running Water

Transcript of Earth science 6.1

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6.1 Running Water

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Water Cycle

• The constant movement of water among the oceans, the atmosphere, geosphere, and the biosphere.

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Infiltration

• The movement of surface water into rock or soil through cracks and pore spaces

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transpiration

• When plants absorb water and release it into the atmosphere

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Gradient

• The slope of a stream over a certain distance

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Stream channel

• The course that the water in a stream follows

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Discharge

• The quantity of water in a stream that passes a given point in a period of time

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tributary

• A stream that empties itself into another stream

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Base level

• The lowest point to which a stream can erode its channel

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Meander

• A looplike bend in the course of a stream

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Key Concept

• Water constantly moves along the oceans, the atmosphere, the solid earth, and the biosphere. This unending circulation of Earth’s water supply is the water cycle.

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Key Concept

• Balance in the water cycle means the average annual precipitation over Earth equals the amount of water that evaporates.

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Key Concept

• The ability of a stream to erode and transport materials depends largely on its velocity.

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Key Concept

• While gradient decreases between a stream’s headwaters and mouth, discharge increases.