Title: WATERSHEDS / DRAINAGE BASINS
1WATERSHEDS / DRAINAGE BASINS
Def The area of land drained by any one stream
REMEMBER a stream is running water thats
confined to a channel---this channel can be any
size
2QWhere 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)
3Water 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.
4The rivers of New York State obtain their water
from very distinct regions. The state is divided
into the following DRAINAGE BASINS (WATERSHEDS)
These watershed regions are pretty small because
the streams they feed into are pretty small
In what drainage basin is Hyde Park?
5Watersheds Continental Divide and Appalachian
Mountains
Water goes from high sea level to low sea level
6The UNITED STATES is split into two LARGE
drainage basins.
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10Drainage Patterns of Watersheds
- Dendritic
- Radial
- Rectangular
- Trellis
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12Dendritic Drainage Patterns
- Dendritic drainage pattern is the most common
form and looks like the branching pattern of tree
roots. - It develops in regions underlain by homogeneous
material. - The subsurface bedrock all has a similar
resistance to weathering so there is not a path
of least resistance, the resistance is equal in
every direction the tributaries take. - Tributaries joining larger streams at acute angle
(less than 90 degrees).
13Drainage Patterns of Watersheds
- Dendritic
- Radial
- Rectangular
- Trellis
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15Radial Drainage Patterns
- radial drainage pattern develops around a central
elevated point. - This pattern is common to cone shaped features
such as volcanoes. - The tributary streams originate at the highest
points toward the top of the volcano or cone.
16Drainage Patterns of Watersheds
- Dendritic
- Radial
- Rectangular
- Trellis
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18Rectangular Drainage Patterns
- rectangular drainage pattern is found in regions
that have undergone faulting. - Streams follow the path of least resistance and
thus are concentrated in places where exposed
rock is the weakest. - Movement of the surface due to faulting off-sets
the direction of the stream. - As a result, the tributary streams make sharp
bends and enter the main stream at high angles.
19Drainage Patterns of Watersheds
- Dendritic
- Radial
- Rectangular
- Trellis
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21Trellis Drainage Patterns
- Trellis drainage patterns look similar to their
namesake, the common garden trellis. - Trellis drainage develops in folded topography
like that found in the Appalachian Mountains of
North America. - Down-turned folds called synclines form valleys
in which the main channel of the stream flows. - Short tributary streams enter the main channel at
sharp angles, as the tributaries run down sides
of parallel ridges called anticlines. - Tributaries join the main stream at nearly right
angles.