Chapter 6 Running Water and Groundwater Flashcards
The water cycle is the
unending circulation of Earth’s water supply.
Balance in the water cycle means that
the average annual precipitation over Earth equals the
amount of water that evaporates.
The ability of a stream to erode and transport material
depends largely on its
velocity.
A stream’s discharge
increases between its source and mouth.
Base level is
the lowest point to which a stream can erode its channel.
Most streams carry the largest part of their load
in suspension.
A depositional feature that forms where a stream enters a
lake or an ocean is a
delta.
The most prominent features of a narrow V-shaped valley
where the stream profile drops quickly are
rapids and waterfalls.
A floodplain forms where a stream
cuts mainly side to side.
One major cause of floods is
rapid spring snowmelt.
Limiting development on floodplains is effective because it
allows floodplains to absorb floodwaters with little harm
to structures.
A drainage basin is
the land that contributes water to a stream.
Groundwater is found underground in the zone of
saturation.
Springs form where
the water table intersects the ground surface.
Permeable rock layers or sediments that freely transmit
groundwater are
aquifers.