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Processes and Interactions of the Earths Systems

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Large, relatively flat areas. Coastal plains near the oceans. Can be called lowlands ... Moho Discontinuity. Boundary between the crust and the mantle ... – PowerPoint PPT presentation

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Title: Processes and Interactions of the Earths Systems


1
Unit 4
  • Processes and Interactions of the Earths Systems

2
Landforms
  • Three types of Landforms
  • Plains
  • Large, relatively flat areas
  • Coastal plains near the oceans
  • Can be called lowlands
  • Characterized by swamps, marshes, and low rolling
    hills
  • Examples Atlantic coastal plains Gulf coastal
    plains

3
Coastal Plains
4
Landforms
  • Interior plains middle of the land
  • Large center portion of the U.S. is called the
    Great Plains or High plains due to their
    elevation
  • covered with grass and few trees

5
Plains
6
Landforms
  • Plateaus
  • Relatively flat, raised areas
  • Made of nearly horizontal rocks that have been
    uplifted by Earth processes
  • Differ from plains because they rise sharply from
    their surroundings
  • Example Colorado Plateau has been cut through
    by the Colorado River to form the Grand Canyon

7
Plateau
8
Colorado Plateau
9
Landforms
  • Mountains
  • tallest mountain Mount Everest 8800m above
    sea level (28,871 feet)
  • Four types of mountains
  • Folded
  • Upwarped
  • Fault-block
  • Volcanic

10
Landforms
  • Folded Mountains
  • Resemble a rug pushed against a wall
  • Earth processes cause the land to be pushed
    together causing it to fold
  • Example Appalachian mountains

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12
Landforms
  • Upwarped Mountains
  • Earths crust pushed up by forces inside Earth
  • Composed of exposed metamorphic and igneous rocks
  • Example southern Rocky Mountains

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14
Landforms
  • Fault-Block Mountains
  • Huge tilted blocks of rocks that are separated
    from surrounding rock by faults
  • fault a large crack in rocks along which
    there is movement
  • one block of rock is pushed up while the other
    is pushed down
  • characterized by sharp jagged peaks
  • Example Sierra Nevada Mountains

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16
Landforms
  • Volcanic Mountains
  • Begin when magma reaches the Earths surface
    through a weak area in the crust
  • One layer builds on another until a cone is
    formed

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19
Weathering
  • Evidence of weathering
  • Sediments provide evidence for weathering
  • Natural elements break down rocks
  • Can lead to the formation of sedimentary rocks
    and soil
  • Weathering is the process that breaks down rocks
    into smaller and smaller fragments
  • Two types of weathering
  • Mechanical weathering
  • Chemical weathering

20
Weathering
  • Mechanical Weathering
  • Breaks apart rocks without changing their
    chemical composition
  • Each piece will retain the same composition as
    the original rock
  • Causes of mechanical weathering
  • Growing plants, expanding ice, growing crystals,
    lightning, and expansion and contraction with the
    freezing and thawing

21
Weathering
  • Chemical Weathering
  • Water, air, and other substance react with the
    rock to change the chemical composition of the
    rock fragments
  • Water
  • The oxygen and hydrogen in water react with
    chemicals in some rocks to form new compounds

22
Weathering
  • Acids
  • Water can mix with carbon dioxide to form
    carbonic acid
  • This is the same acid produced when soft drinks
    are carbonated
  • This is a weak acid
  • The weak acid breaks down the limestone and
    dissolves it

23
Weathering
24
Erosion
  • Erosion and Deposition
  • Erosion the movement of surface materials from
    one location to another
  • Major erosional forces
  • Gravity
  • Glaciers
  • Wind
  • Water
  • All require energy to move materials

25
Gravity erosion
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27
Wind Erosion
28
Water Erosion Grand Canyon
29
Erosion
  • Deposition the dropping of sediments
  • Occurs when the erosional force has lost its
    energy
  • Final stage of an erosional process
  • Erosion and Deposition by Gravity
  • Mass movement moves materials down slopes
  • Some are slow and some are very fast

30
Earthquakes
  • Earthquake focus
  • Focus the point in Earths interior where the
    energy waves are produced
  • Seismic waves
  • Seismic wave - the energy waves that move outward
    from the earthquake focus and make the ground
    quake
  • Epicenter
  • The point on Earths surface directly above the
    earthquake focus

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32
Using Seismic Waves to Map Earths Interior
  • The speed of the waves changes as the depth
    changes
  • The speed changes in accordance to the density of
    the layers of Earth

33
Using Seismic Waves to Map Earths Interior
  • Structure of Earth
  • Inner core
  • Solid and very dense
  • Composed of mostly nickel and iron
  • Outer core
  • Liquid layer that surrounds the inner core
  • Composed of nickel and iron

34
Using Seismic Waves to Map Earths Interior
  • Mantle
  • Largest layer located above the inner core
  • Composed of silicon, oxygen, magnesium, and iron
  • Crust
  • Outermost layer
  • Solid and similar in composition to the mantle

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36
Using Seismic Waves to Map Earths Interior
  • Moho Discontinuity
  • Boundary between the crust and the mantle
  • Seismic waves speed up as they reach this area
  • Seismic waves speed up as they reach more dense
    areas and slow down when the reach less dense
    areas
  • The more solid the layer the more dense

37
Weather
  • What is weather and what are the factors that
    affect it?
  • Weather
  • The present daily atmospheric conditions
  • Factors that affect weather
  • Air pressure, wind, temperature, and air moisture

38
Weather
  • Describe what causes lightning and thunder during
    a thunderstorm.
  • Lightning
  • Occurs when a rapid uplift of air builds up
    electric charges in the clouds and there is flow
    of current between the regions of positive areas
    and negative areas
  • Can be cloud-cloud, cloud-ground, or ground-cloud
  • Thunder
  • The rapid expansion of air due to the rapid
    warming of the air caused by lightning then it
    cools rapidly making a noise

39
Weather
  • Explain how a tornado forms.
  • Wind shear occurs, which is wind at different
    altitudes blow in opposite directions and at
    different speeds
  • A strong updraft causes the wind shear to tilt,
    which causes rotation
  • If the rotation gets fast enough the funnel will
    reach the ground, which is then a tornado

40
Weather
  • Describe how a hurricane forms.
  • SE trade winds meet with the NE trade winds
    causing a low pressure system to form
  • Air masses begin to rotate counterclockwise in
    the northern hemisphere around 5-20 north
    latitude
  • Warm air rises and water vapor condenses
  • The longer the low pressure system is over warm
    water the stronger the hurricane

41
Climate
  • Define climate and list what is used to determine
    climate.
  • Climate is the weather averages over several
    years in a given area
  • Temperature, precipitation, air pressure,
    humidity, and days of sunshine

42
Climate
  • List and describe the factors that affect
    climate.
  • Latitude determines the amount of direct
    sunlight
  • Topography mountain windward side receives more
    rain due to the warm air rising and cooling
  • Location of lakes and oceans water warms and
    cools slower than land
  • Availability of moisture the more moisture in
    the air the wetter the area remains
  • Global wind patterns does the wind blow onto
    land or out to sea (onto land wet out to sea
    dry)

43
Climate
  • Ocean currents warm oceans cause warmer
    climates cooler oceans cause cooler climates
  • Location of air masses large cities heat up the
    air more than surrounding areas and cause the
    climate to be different

44
Atmosphere
  • The atmosphere is divided vertically into four
    layers on the basis of temperature
  • Troposphere
  • Stratosphere
  • Mesosphere
  • Thermosphere

45
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46
Troposphere
  • Layer in which we live, where nearly all weather
    occurs
  • Temperature decreases with an increase in
    altitude
  • Environmental lapse rate name given to the
    temp. decrease
  • (normal lapse rate- 6.5o per kilometer)

47
Stratosphere
  • The boundary between the stratosphere and
    troposphere is called the tropopause
  • Temperatures rise through the stratosphere
  • This is due to ozone absorbing UV rays
  • Although the ozone is thinner at top of strat.,
    it absorbs enough energy to keep the warmer temp

48
Mesosphere
  • Stratopause marks the end of the stratosphere
  • Temp begins to decrease with height after
    stratopause
  • The coldest temps in the atmosphere occur in the
    mesosphere

49
Thermosphere
  • The mesopause marks the end of the mesosphere and
    the beginning of the thermosphere
  • No well-defined upper limit
  • Although the temp is hot, it would not feel hot
    because there are very few air molecules

50
Ionosphere
  • Lower portion of the thermosphere
  • Here molecules of nitrogen and oxygen are ionized
  • Electrons are then free to travel as electric
    current
  • The aurora borealis and aurora australis are
    found here

51
Plate Tectonics
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53
Evidence for Pangaea
  • Climate Clues
  • Rock Clues
  • Glacial Clues
  • Fossil Clues

54
Fossil Clues
55
Seafloor Spreading
  • The floor spreads at a divergent
  • boundary
  • this boundary is also known
  • as a rift or mid ocean ridge

56
Plate boundaries
  • 3 types
  • divergent boundaries
  • convergent boundaries
  • transform fault boundaries

57
Divergent Boundary
  • Divergent Boundary is where
  • 2 plates are moving away
  • from each other

58
Convergent Boundary
  • Convergent Boundary is where 2 plates collide

59
Transform fault boundaries
  • Plates slide past each other no
    production/destruction of material

60
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