
Rivers and Streams Self-paced lesson
Presentation
•
Science
•
8th Grade
•
Practice Problem
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Medium
+13
Standards-aligned
Brendan Ross
Used 11+ times
FREE Resource
17 Slides • 24 Questions
1
River/stream weathering, erosion, and deposition
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River systems are the result of weathering, erosion, and deposition done by water
The landforms and patterns that emerge from them are the result of varying amounts of energy in the river itself.
The energy is determined by how steep the river is (gravitational
potential energy)
Steeper=Faster water=more energy= More Weathering and erosion
Less steep=Slower water=less energy=more deposition
3
Mountain Stream-
steeper
Faster water
Erodes downwards
Meandering Stream-
less steep
slower water (but more of it)
Erodes horizontally.
REVIEW THE LANDFORMS FOUND IN BOTH
Two parts of a river system:
4
MOUNTAIN
Meandering
Source- where a river starts (usually in a mountain)
Confluence- Where two or more rivers join
Tributary- smaller river that connects to a larger river.
Meander- A curve in a river.
Oxbow lake- curved lake created from a cut off meander
Floodplain- flattened area near a meandering river. Created by horizontal erosion. Holds water that floods the banks of a river.
Delta- Area of deposited sediments at the end of a river, usually in a large body of water.
Estuary- area where river meets sea.
Mouth- area where a river ends, and opens into another larger body of slow-moving water.
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Categorize
Slower water
Faster water
horizontal erosion
downward erosion
Meanders
Oxbow lakes
Deposition
Floodplain
Estuary
Delta
Waterfall
Source
Steep gradient
Categorize the different characteristics and landforms of each stream type
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Labelling
Label the different parts of a river system with the correct label.
Meander
Source
Confluence
Mouth
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Multiple Choice
This diagram shows a _____________ .
Delta
Confluence
Source
mountain stream
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Meandering streams change shape back and forth due to the energy differences in them.
They curve and erode different areas over time.
The outer curve of a river is called the cutbank.
The inside curve of a river is called a point bar.
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Labelling
Label the part of the meandering stream.
Cutbank
Point Bar
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But why do these rivers curve?
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12
Multiple Select
Faster-moving water leads to (select all that apply)
Deposition
weathering
erosion
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Multiple Select
Slower-moving water leads to (select all that apply)
Deposition
weathering
erosion
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Multiple Choice
Weathering and erosion happen at the _______ curve(s).
inside
outside
both
left
right
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Multiple Choice
Deposition happens at the _______ curve(s).
inside
outside
both
left
right
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Many rivers end in a delta around the world. How do they form?
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18
Dropdown
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Awesome. Sediments can erode (move) or deposit (stop and lay down). But when do they deposit and when do they erode?
There are two main factors that affect this: Sediment size and water speed (velocity).
Larger sediments need more water speed to move them.
Smaller sediments will only deposit in calmer waters.
The graph that helps us predict what they will do is called the Hjulstrom Curve.
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River Speed
Sediment Size
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If something has a smaller size and/or more river speed, it will usually erode (except for clays, because they stick together)
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If something has a larger size and/or less river speed, it will usually deposit
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Multiple Choice
If a particle of gravel has size 10, and the river velocity is only 1 cm/sec, the gravel particle will
be transported
be deposited
be eroded
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Multiple Choice
If a particle of sand has size 1.0, and the river velocity is 100 cm/sec, the gravel particle will
be transported
be deposited
be eroded
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Multiple Choice
If a particle of silt has size 0.01, and the river velocity is 10 cm/sec, the gravel particle will
be transported
be deposited
be eroded
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Multiple Select
Based on the graph, if the stream speed is 1 cm/sec, which particle sizes would be deposited?
clay
sand
gravel
boulders
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The speed of a river is partially due to its slope. However, it can also change depending on friction. In a flood stage, rivers can have less in their way, and move faster.
One tool to track river levels (drought, normal, flooding) is a hydrograph.
A Hydrograph shows the volume of water passing a point in a river over time. As the amount of water increases (such as during a flood), the hydrograph line begins to peak.
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A horizontal line usually indicates where the "flood stage" for a particular river is. This isn't the same as height of the water. VOLUME does not equal HEIGHT of the water.
The peak height of a hydrograph happens AFTER a rainfall event. It takes time for the rain to fill the river, and so the peak discharge (most water passing the point) is always after the peak rainfall.
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Multiple Choice
According to the hydrograph, when was the peak volume of the river?
August 20
August 22
August 24
August 26
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Multiple Choice
According to the hydrograph, when did the river reach flood stage?
August 21
August 28
August 24
August 26
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Multiple Choice
What term likely describes the August 19 level of the river
flood
normal
drought
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Time to review what we learned.....
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Hotspot
Pick the area(s) of erosion in the river
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Hotspot
Which areas of the stream show a point bar? (Select 2)
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Labelling
Drag the labels for the fastest part of the river and the slowest part of the river
Slower water speed
Faster water speed
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Labelling
Drag the correct water speed to the correct part of the diagram. (For example, if you think the upper course has medium speed water, drag medium speed water below upper course).
Fastest Water
Slowest Water
Medium speed water
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Labelling
Label the features of the river.
Meanders
sediment
Delta
Tributary
Source
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Multiple Choice
Deltas are created when
Rivers deposit mud and sand at their end
Rivers erode mud and sand
Crystallization of minerals occurs in a river
Weathering occurs at the end of a river
40
Multiple Choice
If a particle of gravel has size 10, and the river velocity is only 500 cm/sec, the gravel particle will
be transported
be deposited
be eroded
41
Multiple Choice
How many days was the river at or above flood stage?
2
4
6
8
River/stream weathering, erosion, and deposition
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