
Ch 06.1: Running Water
Presentation
•
Science
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11th Grade
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Practice Problem
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Easy
+15
Standards-aligned
Sarah Rock
Used 3+ times
FREE Resource
25 Slides • 15 Questions
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Ch 06.1: Running Water
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Objectives:
6.1: Explain how the water cycle circulates Earth’s water supply in an unending cycle.
6.2: Explain how the water cycle is kept in balance.
6.3: Describe the ability of a stream to erode and transport material.
6.4: Compare and contrast the changes in gradient and discharge between a stream’s headwaters and mouth.
6.5: Define base level.
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Water is found everywhere on EArth.
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The Water Cycle
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Water constantly moves among the oceans, the atmosphere, the geosphere, and the hydrosphere.
water cycle - unending circulation of Earth’s water supply
possible because water readily changes from one state of
matter to another at temperatures and pressures common on Earth’s surface
worldwide system powered by energy from the sun and by gravity
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Water evaporates into the atmosphere from the ocean.
Condensation causes moisture to form clouds.
Precipitation causes water to fall back to the surface of the Earth.
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When precipitation falls on land:
infiltration - the movement of surface water into rock or soil through cracks and pore spaces
runoff - the process by which excess water flows over the surface of Earth into lakes and streams when the rate of rainfall exceeds Earth’s absorption ability
transpiration - the process through which plants absorb water and release it into the atmosphere
in cold areas, precipitation may become part of a glacier
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Balance in the water cycle means the average annual precipitation over Earth equals the amount of water that evaporates and transpires.
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Multiple Choice
Which term describes the ending circulation of Earth's water supply?
water balance
base level
water cycle
transpiration
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Labelling
Correctly label each portion of the Water Cycle.
runoff
infiltration
evaporation
precipitation
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Fill in the Blanks
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Multiple Choice
The water cycle is the...
...distribution of drinking water on Earth.
...unending circulation of Earth's water supply.
...the recycling of water after industrial use.
...the evaporation of water from Earth's surface.
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Multiple Choice
Balance in the water cycle means that...
...the average annual precipitation over Earth equals the amount of water that evaporates.
...water that falls to Earth only enters oceans.
...the amount of water that falls to Earth weighs the same as the amount that condenses in clouds.
...water taht evaporates from Earth's surface remains forever in the atmosphere.
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Streamflow
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Gravity influences the way water makes its way to the oceans:
Streams and rivers carry water downhill from the land to the sea.
The time this takes depends on the velocity of the steam.
Velocity is the distance that water travels in a period of time.
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straight stretches - higher steam velocity is near the center of the channel just below the surfacee
center of the channel is where friction is the lowest
curved stretches - zone of maximum velocity shifts toward its outer bank
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Fill in the Blanks
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The ability of a steam to erode and transport materials depends largely on its velocity.
factors determining stream velocity include: gradient; shape, size, and roughness of the channel; and discharge
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Multiple Select
Which of the following are factors that determine the velocity of a stream?
gradient
channel shape
channel size
channel roughness
stream discharge
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Gradient
stream channel - the course the water in a stream follows
gradient - the slope or steepness of a stream channel
usually expressed as the horizontal drop of a steam over a certain distance
varies over a stream’s length and between streams
the steeper the gradient, the more energy the stream has as it flows downhill
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Channel Characteristics
Friction slows the forward movement of water.
shape, size, and roughness of the channel affect the amount of friction
water in a smoother channel flows more easily than water in a rougher channel
water in a larger channel flows more easily than water in a smaller channel
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Discharge
discharge - the volume of water flowing past a certain point in a given unit of time
usually measured in cubic meters per second
increases with rainfall and snowmelt
as discharge increases, channel widens and deepens to handle additional water
as size of channel incrases, there is less friction and water
flows more swiftly
construction can cover soil that once absorbed water; decreased water absorption can increase runoff, leading to an increase in magnitude and frequency of floods
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Multiple Choice
The ability of a stream to erode and transport material depends largely on its ___.
width
density
velocity
length
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Multiple Choice
A stream's discharge...
...decreases between its source and mouth.
...remains the same throughout its course.
...is greatest during times of drought.
...increases between its source and its mouth.
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Changes from Upstream to Downstream
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Match
Match each term with the correct definition.
course that water in a stream follows
volume of water flowing past a certain point in a given unit of time
steepness of a stream channel
distance that water travels in a period of time
stream channel
discharge
gradient
velocity
stream channel
discharge
gradient
velocity
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stream profile - a cross-sectional view of a stream or river from its headwaters to its mouth
headwaters - the source or starting point of a stream or river
mouth - the point downstream where a stream or river empties into another body of water
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While gradient decreases between a stream's headwaters and mouth, discharge increases.
the amount of discharge increases because more and more tributaries enter the main channel as it moves downstream
tributary - a stream that empties into another stream
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Multiple Choice
A stream's discharge increases between the headwaters and mouth of the stream.
true
false
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Multiple Choice
From its headwaters to its mouth, a stream's gradient increases.
true
false
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Base Level
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Base level is the lowest point to which a stream can erode its channel.
the base level at which the mouth of a stream enters the ocean, a lake, or another stream
ultimate base level - sea level - the lowest level that stream erosion can lower the land
temporary base level - lakes, resistant layers of rock, and main streams that act as base level for their tributaries
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meander - the many bends in a stream in a broad, flat-bottomed valley that is near its base level
downcutting - occurs when a stream erodes the bottom of a channel, resulting in a deepening of the channel
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Multiple Choice
The lowest point to which a stream can erode its channel is its ___.
base level
headwaters
valley
mouth
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Multiple Choice
A bend in a stream is called a ___.
meander
tributary
mouth
valley
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Multiple Choice
Base level is...
...the lowest point to which a stream can erode its channel.
...any part of the stream that is below sea level.
...the source from which the stream flows.
...the elevation of a stream's largest tributary.
Ch 06.1: Running Water
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