Hydrologic Cycle
River Streams
Drainage Patterns
Streamflow Characteristics
Running Water Work
100

The circulation of water on and below Earth’s surface

Hydrologic cycle

100

Land area where streams drain into a main river

Drainage basin (watershed)

100

Drainage pattern that resembles the branches of a tree

Dendritic pattern

100

Smooth, slow-moving water with little mixing

Laminar flow

100

Invisible material carried in solution

Dissolved load

200

Surplus water flowing over Earth’s surface

Runoff

200

Boundary separating drainage basins

Divide

200

Drainage pattern controlled by faults or joints in bedrock

Rectangular pattern

200

Fast, chaotic flow that causes more erosion

Turbulent flow

200

Visible sediment carried within the water

Suspended load

300

Release of water vapor from plants into the atmosphere

Transpiration

300

Expansion of a river’s head due to erosion

Headward erosion

300

Drainage pattern that flows outward from a central high area

Radial pattern

300

Vertical drop of a river over a given distance

Gradient

300

Large rocks rolling along the stream bottom

Bed load

400

The combined processes of evaporation and transpiration

Evapotranspiration

400

River zone where erosion and deposition are roughly balanced

Zone of sediment transport

400

Drainage pattern formed by alternating bands of resistant and weak rock

Trellis pattern

400

Volume of water flowing past a point per unit time

Discharge

400

Jumping motion of sediment along the stream floor

Saltation

500

Water soaking into the ground

Infiltration

500

River zone where sediment is deposited and deltas form

Zone of sediment deposition

500

Most common drainage pattern on uniform material

Dendritic pattern

500

Stream that flows only after heavy rainstorms

Ephemeral stream

500

A stream’s ability to transport particles of a given size

Competence

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