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The Dynamic Earth

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Title: The Dynamic Earth


1
The Dynamic Earth
2
The Dynamic Earth
  • Movement of the Earths crust (Ch 10)
  • Earthquakes and volcanoes (Ch 11)
  • Plate tectonics (Ch 12)
  • Rocks and minerals (Ch 13)
  • Weathering and soil formation (Ch 14)
  • Erosion and deposition (Ch 15)

3
Erosion and Deposition
  • Read pages 453-454

4
Erosion and Deposition
  • Erosion
  • The process by which weathered rock and soil
    particles are moved from one place to another
  • Erosion can be caused by
  • Gravity
  • Wind
  • Running water
  • Glaciers
  • Waves

5
Erosion and Deposition
  • Deposition
  • The process by which sediments are laid down in
    new locations

6
Section Review Questions
  • Section 15-1
  • What are the five agents of erosion?
  • How does erosion change the Earths surface?
  • What is deposition?
  • How does deposition change the surface of the
    Earth?

7
Gravity
  • Read pages 455-456

8
Erosion and Deposition
  • Gravity pulls rocks and soil down slopes
  • Called mass wasting
  • Can occur rapidly or slowly
  • Rapid
  • Landslide a tumbling of soil, rocks, and
    boulders
  • Mudflow usually occurs after a heavy rain
  • Slump block of rock or soil on the face of a
    steep slope that slips down so its upper surface
    is tilted back
  • Slow
  • Earthflow occurs after a heavy rain
  • Soil creep disturbance of soil particles by
    freezing, animal activity or water movement

9
Section Review Questions
  • Section 15-2
  • How does gravity cause erosion?
  • What is rapid mass wasting? Give two examples.
  • What is slow mass wasting? Give two examples.

10
Wind
  • Read pages 456-459

11
Erosion and Deposition
  • Wind
  • Wind is the most active agent of erosion in
    deserts, in plowed fields, and on the beaches

12
Types of Wind Erosion
  • Wind erodes the Earths surface in two ways
  • Deflation
  • Fine particles are carried many meters up into
    the air
  • Abrasion
  • When particles carried by the wind act like a
    sandblaster, cutting and polishing rocks

13
Deposits by Wind
  • The amount of rock and soil particles carried by
    the wind depends on the speed of the wind
  • As wind slows down, it cannot carry as many
    particles

14
Dunes
  • The deposits of windblown sand which occurs near
    bushes or rocks
  • As the dunes form, it slows the wind down and
    more sand is deposited
  • Eventually it will become a sand dune
  • This is a mound of sand deposited by the wind

15
Sand Dunes
  • Vary in size and shape
  • The side that faces the wind is a gentle slope
  • The side away from the wind is a steep slope
  • Sand dunes move by being eroded away on one side
    and deposited on the other

16
Loess
  • The deposits of fine particles of sand and silt
    deposited many miles away
  • These areas are very fertile
  • These deposits are light in color and may be many
    meters thick.

17
Windbreak
  • Is often used to decrease wind erosion and aid in
    wind deposition
  • A barrier that causes the wind to slow down
  • When wind speed is decreased, the load carried by
    the wind is dropped

18
Section Review Questions
  • Section 15-3
  • Where is wind the most active agent of erosion?
  • How are deflation and abrasion different?
  • What are two kinds of deposits caused by wind?

19
Running Water
  • Read pages 460-465

20
Running Water
  • Running water changes more of the Earths surface
    than any other agent of erosion
  • Running water is the major cause of erosion
  • Rivers, streams, and runoff are forms of running
    water

21
Runoff and Erosion
  • When rain falls on the surface of the Earth,
    three things can happen to the water
  • The rain can evaporate
  • It can sink into the ground
  • It can flow over the land surface as runoff

22
Runoff and Erosion
  • When water moves across the Earths surface as
    runoff, it picks up and carries particles of
    clay, sand, and gravel
  • This water and sediments move downhill as a
    result of gravity
  • While these particles are moving, they continue
    to wear away the soil and form grooves, called
    rills

23
Runoff and Erosion
  • Rills become wider and deeper and eventually form
    gullies
  • Gullies act as channels for runoff

24
Runoff and Erosion
  • The amount of runoff is affected by several
    factors
  • The amount of rainfall
  • In areas of high average rainfall, there is a lot
    of runoff, there is a lot of erosion
  • The amount of plant growth in an area
  • Plant roots hold soil particles in place and help
    to absorb some of the water
  • Areas with little plant growth have greater
    runoff and therefore greater erosion

25
Runoff and Erosion
  • The amount of runoff is affected by several
    factors
  • The shape of the land
  • Steep slopes have the greatest amount of runoff
  • Water moves too fast to soak into the ground
  • As the water moves rapidly down the hill, a lot
    of erosion takes place

26
Streams and Erosion
  • When the water from several gullies comes
    together, a stream forms
  • Streams carry large amounts of sediments
  • The soil particles and rock materials carried
    along by the stream are called the streams load

27
Streams and Erosion
  • Sediments are carried different ways
  • Large, heavy sediments, such as pebbles and
    boulders, are pushed or rolled downstream
  • Lighter sediments, such as silt or clay, are
    picked up and carried along by the force of the
    moving water
  • There sediments, such as salts, dissolve in the
    water

28
Streams and Erosion
  • Streams cause erosion by abrasion
  • Sediments carried by streams constantly collide
    with rocks, chipping away pieces and wearing down
    the rocks
  • Different types of rock layers will result in
    different types of abrasion

29
Development of a River System
  • Runoff forms rills, rills deepen and widen into
    gullies, gullies form streams, streams join to
    form rivers
  • Rivers usually begin in mountains and hills
  • Rivers affect large areas by erosion

30
Development of a River System
  • The network of rills, gullies, streams, and
    rivers in an area is called a drainage system
  • A tributary is a main source of water for a river
  • Many tributaries feed the river

31
Development of a River System
  • The area drained by a main river and its channels
    is called a drainage basin
  • The land that separates one drainage basin from
    another is called a divide
  • One of the larges divides is called the
    Continental Divide
  • This is a divide that passes down the center of
    the Rocky Mountains
  • West of the divide, water goes to the Pacific
  • East of the divide, water goes to the Atlantic

32
Development of a River System
  • The divide may start off wide, but as the
    drainage system of a river develops, the divide
    becomes narrower

33
Life Cycle of a River
  • An immature river, or a young river, is a river
    in an early stage of development
  • Water flows very rapidly over the surface
  • This is able to move large rocks and produce a
    lot of runoff

34
Life Cycle of a River
  • A river that has been developing for many
    thousands of year is called a mature river
  • Because of continuous erosion, the rapids and
    waterfalls have largely disappeared
  • The river is curved and winding, forming loops
    called meanders
  • The water has slowed down so erosion has slowed
    down

35
Deposits by Rivers
  • A stream or river carries a large amount of
    sediments
  • Deposits are left where a stream bends or curves
  • The outside of the curve receives the full impact
    of the current

36
Oxbow Lakes
  • This is a U-shaped lake that forms when a river
    meanders in a curve and eventually cuts off the
    ends forming a lake

37
Alluvial Fans
  • When the sediments carried by a rapid moving
    river are dropped because the river slows down
  • This deposit forms a fan-like shape

38
Deltas
  • Large amounts of sediments deposited at the mouth
    of a large river that flows into a lake or an
    ocean form a delta
  • Sediments can build up near the mouth of a river

39
Flood Plains and Levees
  • Flood plains form when a river overflows and
    sediments are deposited in the area around the
    river
  • Flood plains are very fertile
  • The ridgelike deposits along the sides of the
    river are called levees

40
Section Review Questions
  • Section 15-4
  • What is the major cause of erosion?
  • What factors affect the amount of runoff?
  • What is a drainage system? A drainage basin?
  • Compare an immature river to a mature river.
  • How are deltas and flood plains formed?

41
Glaciers
  • Read pages 466-470

42
Glaciers
  • A large mass of moving ice and snow
  • Review chapter 7

43
Glacial Ice and Erosion
  • Glacial ice erodes by abrasion and by plucking
    away at the rock beneath it
  • Rock materials carried by a glacier are called
    glacial debris
  • Particles in the glacier scrapes along rocks and
    leaves scratches

44
Deposits by Glaciers
  • As a glacier comes to warmer climates, it begins
    to melt and leave behind rocks and debris
  • This debris is called till

45
Moraines
  • When a glacier melts and retreats, it leaves
    behind till
  • Till forms a ridge called a moraine
  • Till at the front side of the glacier is called
    terminal moraine
  • Till at the sides of the glacier is called a
    lateral moraine
  • Scientists study tills to find where the glacier
    formed

46
Drumlins
  • An oval-shaped mound of till
  • Formed as deposits of till are rounded by glacial
    ice

47
Meltwater Deposits
  • Meltwater forms when the glacier stops moving and
    begins to melt
  • These rivers of melted water carry sediments and
    deposit them along a stream beds called valley
    trains
  • These deposits form areas called outwash plains
  • These plains are very fertile
  • Many farms today can be found in these areas

48
Iceberg Deposits
  • Icebergs may contain rocks and debris picked up
    from land
  • As the iceberg melts, the rocks and debris are
    deposited on the ocean floor

49
Glacial Lakes
  • Glaciers form many lakes including the Finger
    Lakes in New York, the Great Lakes and other
    smaller lakes

50
Glacial Lakes
  • Glaciers can form lakes in two ways
  • Glacial till piles up in low-lying river channels
    and other areas
  • These deposits keep water from flowing away from
    land
  • Ice blocks are surrounded or covered with
    sediments deposited by the glaciers
  • When the ice melts, it leaves a depression, or
    hole, in the ground
  • These lakes are known as kettle lakes

51
Section Review Questions
  • Section 15-5
  • How does a glacier erode the Earths surface?
  • Compare a valley glacier and a continental
    glacier.
  • What is till? A moraine? A drumlin?
  • What are two meltwater deposits?
  • How are glacial lakes formed?

52
Waves
  • Read pages 470-474

53
Waves
  • The powerful force of waves constantly erodes and
    shapes the shoreline

54
Waves and Erosion
  • Waves cause erosion in several ways
  • The force of waves hitting the rocks
  • The particles in the waves rubbing against the
    rocks
  • Forcing water up into cracks and making the
    cracks bigger
  • Salt water dissolving some minerals

55
Waves and Erosion
  • Erosion at a shoreline can occur at different
    rates
  • The size and the force of the waves hitting the
    shoreline have an effect on the rate of erosion
  • Certain rocks erode more quickly than others

56
Sea Cliffs and Terraces
  • Steep faces of rock that are formed by wave
    erosion are called sea cliffs
  • The flat place at the bottom of a sea cliff is
    called the terrace
  • This area is made up of the ground up particles
    of the sea cliff

57
Sea Stacks and Caves
  • The columns of resistant rock left behind from
    sea cliffs are called sea stacks
  • A sea cave is a hollowed out portion of a sea
    cliff

58
Deposits by Waves
  • Waves carry large amounts of sand, rock particles
    and pieces of shells
  • Beaches
  • Are made up of eroded rock particles deposited on
    the shoreline
  • The color of beach sand depends on the source
    rock from which it came

59
Sand Bars and Spits
  • When water currents turn and flow parallel to the
    shoreline it is called a longshore current
  • If the shoreline bends or curves, materials
    carried by waves in a longshore current is
    deposited in open water and forms a sand bar
  • If the sandbar is connected to the curving
    shoreline, it is called a spit

60
The Shape of the Shoreline
  • The shape of the shoreline often results from
    changes in the level of the sea
  • A drop in the ocean forms more sea cliffs
  • A rise in the ocean forms more harbors and bays

61
Section Review Questions
  • Section 15-6
  • How do waves affect a shoreline?
  • What is a sea cliff? A sea stack?
  • Why do different beaches have different colored
    sand?
  • How does a longshore current form sand bars and
    spits?

62
Chapter Review
  • Pages 478-479
  • Multiple Choice
  • 1-10
  • True or False
  • 1-7
  • Concept Mapping
  • Extra Credit
  • Concept Mastery
  • Answer 5 of the 9 questions
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