• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/10

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

10 Cards in this Set

  • Front
  • Back
hdrologic cycle
The hydrologic cycle is a summary of the circulation of Earth’s water supply
Processes Involved
Processes involved in the hydrologic cycle
-Evaporation
-Transpiration
-Precipitation
-Infiltration
-Runoff
running water - begins as sheet flow
Infiltration capacity is controlled by
-Intensity and duration of rainfall
-Prior wetted condition of the soil
-Soil texture
-Slope of the land
-Nature of the vegetative cover
-Sheet flow develops into tiny channels called rills
Running water - drainage networks
Drainage networks
-The land area that contributes water to a stream is called the drainage basin
-The drainage pattern consists of the interconnected network of streams in an area
-A drainage basin of one stream is separated from the drainage basin of another by an imaginary line called a divide
running water - streamflow
Streamflow
-Two types of flow determined primarily by velocity
-Laminar flow
-Turbulent flow
-Factors that determine velocity
-Gradient, or slope
-Channel characteristics including shape, size, and roughness
-Discharge – the volume of water moving past a given point in a certain amount of time
narrow valleys
Narrow valleys
V-shaped
Downcutting toward base level
Features often include rapids and waterfalls
wide valleys
Wide valleys
Stream is near base level
Downward erosion is less dominant
Stream energy is directed from side to side forming a floodplain
Features of wide valleys often include
Floodplains
Erosional floodplains
Depositional floodplains
Meanders
Cut bank and point bar
Cutoffs and oxbow lakes
floods and flood control
Floods are the most common and most destructive geologic hazard
Causes of flooding
Result from naturally occurring and human-induced factors
types of floods
Types of floods
Regional floods
Flash floods
Ice-jam floods
Dam failure
flood control
Flood control
Engineering efforts
Artificial levees
Flood-control dams
Channelization – Mississippi River flow path shortened by more than 240 km.

Nonstructural approach through sound floodplain management