Chapter 14 Flashcards
Internal Drainage Basin
Water leaves the basin through
evaporation, transpiration or
subsurface gravitational flow
Gradient
drop in elevation per unit distance
Stage
height of river
Base level
level below which a stream cannot erode its valley;
In general, the ultimate base level is sea level
Discharge
Volume of flow over time
Urbanization
can increase peak flow and shorten lag time between storm peak and stream discharge peak
Exotic streams
Discharge of most streams increase downstream because the area being drained increases
Hydrograph
A graph of stream discharge over time for a specific place
This material is then transported to new locations ____________, where it is laid down in the process of _________
Fluvial transport
Deposition
Erosion, transport, and deposition are affected by
discharge and
channel gradient
(Three types of load in streams)
Dissolved load (solution)
Chemical solution
(Three types of load in streams)
Suspended load
fine-grained particles
(Three types of load in streams)
Bed load
coarser materials
Braided Channels/Streams
Multiple-thread channels
Excess sediment
Channels and islands are not
static
Maze of interconnected
channels
Straight
areas where gradient is high