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Published byOliver Wade Modified over 9 years ago
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Watersheds/ Stream Drainage Patterns
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WATERSHEDS / DRAINAGE BASINS Watershed: The area of land drained by any one stream REMEMBER: a stream is running water that ’ s confined to a channel---this channel can be any size: SMALL MEDIUM LARGE
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Q:Where does water go once it hits the surface of the earth? A: Some gets absorbed into the ground (infiltration) some flows along the surface (runoff) Q:Where does water go once it hits the surface of the earth? A: Some gets absorbed into the ground (infiltration) some flows along the surface (runoff)
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Water always flows from HIGH elevation to LOW elevation. Along the way, this water combines with other water, so the size of the stream gets bigger and bigger. A B The smaller streams are called tributaries.
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These watershed regions are pretty small because the streams they feed into are pretty small The rivers of New York State obtain their water from very distinct regions. The state is divided into the following DRAINAGE BASINS (WATERSHEDS): In what drainage basin is Valhalla?
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This side, all water flows to PACIFIC OCEAN This side, all water flows to ATLANTIC OCEAN The UNITED STATES is split into two LARGE drainage basins
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Stream Drainage Pattern: -The shape of a stream’s course in an area as viewed from the sky or -what the pattern of stream flow is when looking from above *The formation of the pattern a stream creates is determined by the shape of the underlying bedrock structure
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a)dendritic: homogeneous rock b)trellised pattern: alternating weak and strong rock c)radial: dome uplift or volcano.
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d) centripetal: converging to a central basin e) rectangular: intersecting fractures in bedrock f) deranged: retreat of glaciers
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Dendritic Drainage -Consists of many tributaries flowing into one river -Occurs in a humid climate -Looks like branching tree roots
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Trellis Drainage -Looks like a trellis. -WHAT IS A TRELLIS???
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Trellis drainage -occurs when tributaries flow at right angles to rivers
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Rectangular drainage -Occurs in regions of faulting -Water flows along path of least resistance -Right angles form from the offsetting of faults (land is shifting left/right up/down at right angles)
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Radial Drainage -develops around a central elevated point (Mountain Peak) -Tributary “ roots ” start at the high elevation
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Centripetal Drainage -Opposite of Radial Drainage -Streams flow to a central depression or basin
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Deranged Drainage -No apparent pattern -Streams flow with the landscape left behind from a glacier -Water is from the retreat of the glacier
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Question: –What determines the shape of a stream drainage pattern???? The landscape of the underlying bedrock
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