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C. DEPOSITION The _____________ of particles and fragments.
It is also called
___________________
The agents of deposition are:
____________________
____________________
____________________
RATES OF DEPOSITION DEPEND ON:
1. Particle size: ________ particles (clay,silt) settle more slowly than larger particles.
________ do not settle out of solution unless the solution
becomes _______________
_____________ __________ are the ions that come out of solution.
&
2. Particle shape:
____________ between water and the surface of particles _______ settling.
As the surface area ___________ the time it takes to settle __________
3. Particle Density:
____________ particles settle faster.
Complete the graphs: label each axis
What is the relationship between settling rate and
particle size?
Settling rate
Particle size
What is the relationship between settling rate and
shape?
Settling rate
Particle gets flatter
What is the relationship between settling rate and
density?
Settling rate
density
Settling Rate and Settling Time:
Settling time
settling
As the rate of settling
The settling time
Complete the graph: this relationship is
indirect
rate
VELOCITY OF TRANSPORTING
MEDIUM: The slower the velocity of the water the ________ particles will settle. It takes longer for particles to settle
in ___________ water.
SORTING OF SEDIMENTS:
Horizontal Sorting: a gradual change in the size,shape and density
(of deposited particles) when a stream slows down
…………… ……………. ……………. ……………. Ions in solution
boulders
cobbles
sand
silt
Horizontal Sorting
clay
pebbles Roundest and densest
Smallest flattest least dense
(colloids)
Precipitation
Mississippi River Delta
Nile River Delta
Vertical Sorting &
Graded Bedding:
Largest at bottom
smallest at top
Each layer represents a single event of deposition
EROSIONAL-DEPOSITIONAL
SYSTEM:
___________ or
___________ are examples of this kind of system.
Within a stream system
energy transforms from
____________
to ____________
energy.
Erosion ______________Will dominate in the steeper section and
Deposition ______________ In places of less gradient or slope.
Kinetic Energy depends on
__________________ velocity increases Kinetic energy increases more erosion occurs
Slope-
Potential Energy depends
on__________ not Slope energy is stored and deposition occurs
height
Dynamic Equilibrium
When the rate of erosion equals rate of deposition:
___________________ is reached
Erosion occurs more often on _______
And Deposition occurs in large
bodies of _______
land
water
Ocean
lake A B
C D
Side View
lake
Ocean
A B C
D
Top View
Streams that flow over flat valleys
may develop meandering paths
because of erosion and deposition.
Glaciers
Sediments left by glaciers are:
_______________
Glacial erratics are large rocks that have been transported by glacial ice without being broken into
pieces
Some Glacial Features include: U-shaped valleys Moraines unsorted sediments drumlins kettle lakes finger lakes outwash plains erratics
Drumlins
outwash plain
Kettle lakes
WIND:
Sediments left by wind are
________________
Sand dunes may form with a gentle slope facing into the wind ________________ Windward side
And a steep slope on the opposite side___________
leeward side
When wind direction changes sand dunes cross each other creating a feature known as ________________ Cross bedding
Most sand dunes are well ___________
in sloping ____________ sorted
layers
Deposition on Coastlines by
Ocean Waves and Currents:
The sand grains are _____________ &
______________
rounded
frosted
_______ Generates
Waves
Wind
Waves move sand __________ to the shore parallel
Barrier beaches may form like Jones Beach or Fire Island
Wave action rounds sediments as a result of __________ abrasion