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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.
What is the relationship
  between settling rate and
       particle size?
                           Complete the graphs:
                              label each axis

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:
                            As the rate of settling

settling                    The settling time
  rate
                            Complete the graph:
                            this relationship is
            Settling time         indirect
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
Horizontal Sorting
           boulders


                cobbles

Roundest              pebbles
and                        sand
densest

                                                      Precipitation
                                                      ……………
                                  silt
                                                      …………….
                                                        Ions in
                                                      …………….
                                         (colloids)
                                           clay       …………….
                                                        solution
               Smallest
               flattest
               least dense
Mississippi River Delta
Nile River Delta
Vertical Sorting &
Graded Bedding:
          Each layer
           represents
           a single
           event of
           deposition

           Largest
            at
            bottom
           smallest
            at top
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
       Slope-
 __________________
velocity increases
Kinetic energy increases
more erosion occurs
Potential Energy
    depends
    height
 on__________
not Slope
energy is stored and
deposition occurs
When the rate of
 erosion equals rate of
 deposition:

 Dynamic Equilibrium
___________________
is reached
Erosion occurs more
      often on
       land
     _______
  And Deposition
  occurs in large
     bodies of
     water
    _______
Side View
lake
       A   B



               C
                              D
                                   Ocean


                   Top View
       A   B
               C
lake


                               D      Ocean
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
                             Drumlins




finger lakes
outwash plains
                                        Kettle lakes


erratics           outwash
                    plain
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      leeward side
  side___________
When wind direction changes
 sand dunes cross each other
 creating a feature known as
 Cross bedding
 ________________
Most sand dunes are well
      sorted
  ___________
              layers
in sloping ____________
Deposition on
  Coastlines by
Ocean Waves and
    Currents:
The sand grains are
  rounded
_____________
&

   frosted
______________
Wind
_______
Generates
 Waves
Waves move
sand
 parallel
__________
to the shore
Barrier beaches may form
like Jones Beach or Fire Island
Wave action
rounds sediments
as a result
    abrasion
of __________

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Deposition

  • 1.
  • 2. C. DEPOSITION The _____________ of particles and fragments. It is also called ___________________
  • 3. The agents of deposition are:   ____________________   ____________________   ____________________
  • 4. RATES OF DEPOSITION DEPEND ON: 1. Particle size: ________ particles (clay,silt) settle more slowly than larger particles.
  • 5. ________ do not settle out of solution unless the solution becomes _______________ _____________& __________ are the ions that come out of solution.
  • 6. 2. Particle shape: ____________ between water and the surface of particles _______ settling. As the surface area ___________ the time it takes to settle __________
  • 7. 3. Particle Density: ____________ particles settle faster.
  • 8. What is the relationship between settling rate and particle size? Complete the graphs: label each axis Settling rate Particle size
  • 9. What is the relationship between settling rate and shape? Settling rate Particle gets flatter
  • 10. What is the relationship between settling rate and density? Settling rate density
  • 11. Settling Rate and Settling Time: As the rate of settling settling The settling time rate Complete the graph: this relationship is Settling time indirect
  • 12. VELOCITY OF TRANSPORTING MEDIUM: The slower the velocity of the water the ________ particles will settle. It takes longer for particles to settle in ___________ water.
  • 13. SORTING OF SEDIMENTS: Horizontal Sorting: a gradual change in the size,shape and density (of deposited particles) when a stream slows down
  • 14. Horizontal Sorting boulders cobbles Roundest pebbles and sand densest Precipitation …………… silt ……………. Ions in ……………. (colloids) clay ……………. solution Smallest flattest least dense
  • 18. Graded Bedding: Each layer represents a single event of deposition Largest at bottom smallest at top
  • 19. EROSIONAL -DEPOSITIONAL SYSTEM: ___________ or ___________ are examples of this kind of system.
  • 20. Within a stream system energy transforms from ____________ to ____________ energy.
  • 21. Erosion _____________ _Will dominate in the steeper section and
  • 22.
  • 23. Deposition ______________ In places of less gradient or slope.
  • 24.
  • 25. Kinetic Energy depends on Slope- __________________ velocity increases Kinetic energy increases more erosion occurs
  • 26.
  • 27.
  • 28. Potential Energy depends height on__________ not Slope energy is stored and deposition occurs
  • 29. When the rate of erosion equals rate of deposition: Dynamic Equilibrium ___________________ is reached
  • 30. Erosion occurs more often on land _______ And Deposition occurs in large bodies of water _______
  • 31. Side View lake A B C D Ocean Top View A B C lake D Ocean
  • 32. Streams that flow over flat valleys may develop meandering paths because of erosion and deposition.
  • 34. Sediments left by glaciers are: _______________
  • 35.
  • 36. Glacial erratics are large rocks that have been transported by glacial ice without being broken into pieces
  • 37. Some Glacial Features include: U-shaped valleys Moraines unsorted sediments drumlins kettle lakes Drumlins finger lakes outwash plains Kettle lakes erratics outwash plain
  • 38. WIND:
  • 39. Sediments left by wind are ________________
  • 40.
  • 41.
  • 42. Sand dunes may form with a gentle slope facing into the wind ________________ Windward side And a steep slope on the opposite leeward side side___________
  • 43.
  • 44.
  • 45.
  • 46. When wind direction changes sand dunes cross each other creating a feature known as Cross bedding ________________ Most sand dunes are well sorted ___________ layers in sloping ____________
  • 47. Deposition on Coastlines by Ocean Waves and Currents:
  • 48. The sand grains are rounded _____________ & frosted ______________
  • 49.
  • 52.
  • 53. Barrier beaches may form like Jones Beach or Fire Island
  • 54. Wave action rounds sediments as a result abrasion of __________