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Ch 06.1: Running Water

Ch 06.1: Running Water

Assessment

Presentation

Science

11th Grade

Practice Problem

Easy

NGSS
MS-ESS1-1, MS-ESS2-4, MS-ESS2-1

+15

Standards-aligned

Created by

Sarah Rock

Used 3+ times

FREE Resource

25 Slides • 15 Questions

1

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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media

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?

1

water balance

2

base level

3

water cycle

4

transpiration

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Labelling

Correctly label each portion of the Water Cycle.

Drag labels to their correct position on the image

runoff

infiltration

evaporation

precipitation

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Fill in the Blanks

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Multiple Choice

The water cycle is the...

1

...distribution of drinking water on Earth.

2

...unending circulation of Earth's water supply.

3

...the recycling of water after industrial use.

4

...the evaporation of water from Earth's surface.

14

Multiple Choice

Balance in the water cycle means that...

1

...the average annual precipitation over Earth equals the amount of water that evaporates.

2

...water that falls to Earth only enters oceans.

3

...the amount of water that falls to Earth weighs the same as the amount that condenses in clouds.

4

...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

20

Multiple Select

Which of the following are factors that determine the velocity of a stream?

1

gradient

2

channel shape

3

channel size

4

channel roughness

5

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 ___.

1

width

2

density

3

velocity

4

length

26

Multiple Choice

A stream's discharge...

1

...decreases between its source and mouth.

2

...remains the same throughout its course.

3

...is greatest during times of drought.

4

...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

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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.

1

true

2

false

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Multiple Choice

From its headwaters to its mouth, a stream's gradient increases.

1

true

2

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

38

Multiple Choice

The lowest point to which a stream can erode its channel is its ___.

1

base level

2

headwaters

3

valley

4

mouth

39

Multiple Choice

A bend in a stream is called a ___.

1

meander

2

tributary

3

mouth

4

valley

40

Multiple Choice

Base level is...

1

...the lowest point to which a stream can erode its channel.

2

...any part of the stream that is below sea level.

3

...the source from which the stream flows.

4

...the elevation of a stream's largest tributary.

Ch 06.1: Running Water

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