Flooding Flashcards
What is the main role of streams and rivers?
Drain the water and transport sediments
A stream overflow occurs if its ability to carry water is overwhelmed.
Flood
The volume of water moving through a channel over a period of time.
Stream discharge
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 the river or stream by plotting the discharge and time.
Stream hydrographs
Amount of time for a water to move across the landscape and into channels.
Lag time
Continuous input of groundwater baseflow allows stream in many areas to keep flowing at minimum levels.
Baseflow conditions
More water infiltration causes groundwater to be higher than stream channels.
Gaining streams
Result of less deep infiltration in arid areas resulting in a water table below the streams.
Losing streams
Large streams serve as the principal channel within the drainage system.
River
Upper portion of the drainage system.
Headwaters
Found in the lower part of the system where a river empties into an ocean.
Mouth
Individual system separated from one another by topographic high or crest.
Drainage divide
Land area that collects water for an individual stream or river.
Drainage basin/ Watershed
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
The longitudinal profile reflects a downstream trade-off between discharge and slope in setting transport capacity.
Stream Longitudinal Profile
The limiting level below which a stream cannot erode is called _________.
Base level
Approximately equals the inverse of the source basin length.
Drainage density
True or False. Steep terrain has high drainage density while gentle terrains have low drainage density.
TRUE
Drainage pattern that forms horizontally bedded and uniform sediments or on uniformly resistant crystalline rocks.
Dendritic
Drainage pattern that develops on moderate to steep slopes, but also where regional structure, such as outcropping resistant rock bands.
Parallel
Patterns most commonly on dipping or folded sedimentary or weakly metamorphosed sedimentary rock; also areas of joints and faults which intersect with right angles and old sand dunes with parallel alignment.
Trellis
Usually have more or less perpendicular turns mainly caused by crisscrossing fractures.
Rectangular
Occurs around domes or cones and is particularly common in volcanic areas.
Radial
Patterns also develop around domes, where there exist alternating resistant and weak beds.
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, intrusion, alterations, and faulting.
Contorted
Types flowing streams.
Perennial, intermittent, & ephemeral
Types of linearity of river.
Straight, meandering and braided