FLOOD Flashcards
Described as the volume of water moving
through a channel over a given time interval,
commonly measured in units such as cubic
feet per second (ft 3 /s)
Stream Discharge
to drain water off the landscape and to transport sediment
role of streams
a process where water flows through
stream channels
Runoff
precipitation reaching the land
surface moves downslope in thin sheets
Overland Flow
discharge of
groundwater into the surface environment
Groundwater baseflow
provide information about a
river or stream by simply plotting the discharge versus
time
Stream hydrographs
are a result of less deep infiltration in
arid areas resulting in a water table that is below the
level of most stream channels
Losing streams
are generally small and relatively fast
moving and occupy narrow valleys, but then evolve
Headwater streams
Individual systems are separated from one another by a
topographic high or crest in the landscape called a
drainage divide
represents the land area that collects water for an
individual stream or river.
drainage basin
are any smaller streams that feed larger streams within a
drainage basin
Tributaries
A method of classifying or
ordering the hierarchy of
natural channels
Strahler Stream Order
reflects downstream trade off between discharge
and slope in setting transport capacity (and thus ability to move
sediment and incise rock)
Longitudinal Profile
The
level below which a river or stream cannot incise
Base Level
Most commonly formed on horizontally
bedded and uniform sediments or on
uniformly resistant crystalline rocks.
Dendritic
Usually develops on moderate to steep slopes,
but also where regional structure, such as
outcropping resistant rock bands, are
elongated and parallel. All forms of transition
Parallel
Patterns most commonly on dipping or folded
sedimentary or weakly metamorphosed
sedimentary rocks; also areas of joints and
Trellis
Usually have a more or less
perpendicular turns mainly
caused by criss crossing
fractures.
Rectangular
Occurs around domes or cones, and
particularly common on volcanic areas.
Radial
Patterns also develop around domes, where
there exists alternating resistant and weak
beds, so that the major channels cut through
Annular
Can occur in a variety of conditions where local
hummocks and depressions inhibit a continuous
channel network.
Multibasinal
Incised into rocks with complicated structural
patterns. Associated with crystalline metamorphic
rocks with a history of intense folding, jointing,
intrusions, alterations, and faulting.
Contorted
all year agas na river
perennial