aim: unit 8 review do now: –power on your laptops and download the test corrections template....
TRANSCRIPT
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Aim: Unit 8 Review • Do Now:
– Power on your laptops and download the test corrections template.
– H.W. Finish your unit 8 test corrections.
![Page 2: Aim: Unit 8 Review Do Now: –Power on your laptops and download the test corrections template. –H.W. Finish your unit 8 test corrections](https://reader036.vdocuments.net/reader036/viewer/2022062719/56649ed95503460f94be7016/html5/thumbnails/2.jpg)
Sorting of Sediments and Deposition
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Agents of Deposition
• The agents of erosion are also agents of deposition.
• Depositional rate depends on sediment size, shape and density.
• Depositional rate also depends on characteristics of the depositional agent.
Speed or velocity
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Agents of Deposition
• Stream sediments and wind sediments get deposited when the speed or velocity of the eroding agent decreases enough so that the agent can no longer carry the sediment.
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Settling Rate Vs. Velocity
• As the velocity (speed) of the wind or stream decreases, deposition begins – usually with the largest, heaviest, most dense, most rounded, particles settling out first.
Velocity
Sett
ling
Rate
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Settling Rate Vs. Density
• Particle density affects settling rate. Particles with similar size and shape should settle at the same rate, but particles with a higher density will settle faster.
Density
Sett
ling
Rate
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Settling Time Vs. Rate
• Be oh-so-careful when answering questions about which particles settle fastest. There is a HUGE difference between settling time and settling rate.
Settling Time
Sett
ling
Rate
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Mountain side
Stream
Lake
As the stream enters the lake or an ocean, the stream velocity decreases
and sediments are deposited.
Stream velocity
decreases
Sediments are deposited in size order horizontally.
Horizontal Sorting
BouldersCobbles
PebblesSand Silt Clay
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Region of maximum stream velocity changes when streams bend or turn. There is an interface between regions of erosion and deposition…
Stream
BouldersCobblesPebblesSand
Vertical SortingClay
Silt
Vertical Sorting
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Vertical Sorting
•During vertical sorting the largest, roundest, most dense particles settle to the bottom with the smallest, flattest, least dense particles settling at the top.
Vertical Sorting
Latest layer
Earliest layerLater layer
•Vertical sorting can occur as a single depositional event in still water or a series of events as when a stream’s velocity decreases through the seasons allowing particles to settle in a graded bed.
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Vertical Sorting
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Where a stream or river enters a lake or ocean, deposition begins at the mouth forming a delta.
Named for the Greek letter
Stream
Ocean
Deltas
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Mississippi Delta• Sediment-laden
river water mixes with cold, deep-sea currents, creating a nutrient rich zone where both salt and freshwater fish flourish.
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• Wind-born particles are generally sorted by size, but are small. Cross bedding is common in sand dunes.
• Sediments eroded and deposited by gravity are unsorted.
Deposition by other agents of erosion
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Crossbeds in a Sand Dune
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Unsorted Sediments
• Unsorted till left behind by a Glacier.
• Unsorted sediments due to Mass Movement.
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Final Question
• What are the factors that affect the settling rates of sediments?