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The state of Georgia wants you to Identify surface features caused by constructive and deconstructive processes. Constructive vs. Destructive Land forms are the ... – PowerPoint PPT presentation

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Title: The%20state%20of%20Georgia%20wants%20you%20to


1
The state of Georgia wants you to
  • Identify surface features caused by constructive
    and deconstructive processes.

2
Constructive vs. Destructive
  • Land forms are the result of a combination of
    constructive and destructive forces. Constructive
    forces affect the earth's surface by building it
    up to form new landforms like mountains and
    islands. Destructive forces affect the earth's
    surface by breaking down landforms to form new
    ones.

3
Deposition deltas sand dunes
  • The dunes are the product of the wind and rain
    eroding nearby mountains. The dunes collect here
    because the prevailing winds across the valley
    blow in this direction and meet winds blowing in
    the opposite direction. The sand drops to the
    valley floor and begins to collect. So over the
    course of millennia, the dunes have build.
    Tomorrow they will be different because the wind
    still blows, the sand still moves and the
    deposits of sand still grow.

4
Western Sand Dune
5
Delta
  • A delta is a low, watery land formed at the mouth
    of a river. It is formed from the silt, sand and
    small rocks that flow downstream in the river and
    are deposited in the delta.
  • A delta is often (but not always) shaped like a
    triangle (hence its name, delta, a Greek letter
    that is shaped like a triangle).

6
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7
  • NASA view of a delta from space.

8
Faults
  • Faults are usually caused by the Earth's crust
    bending and breaking in the middle because of the
    forces pressing on it. These bends and breaks can
    form faults where the earth's crust is able to
    move. 
  • Faults also mark plate boundaries. There are
    three main types of faults and each are
    constructive in their own way.

9
Divergent Fault Line
  • Divergent Fault is where two plates are moving
    away from each other. (For more)
  • As plates pull apart from each other the earth's
    crust spreads apart. This usually causes rifts or
    rift valleys. The majority of this activity takes
    place deep within the oceans along plate
    boundaries. As the plates pull apart hot magma is
    pushed toward the surface and volcanoes occur.
    This affects the Earth's surface by adding new
    material to the surface.

10
Convergent Fault Line
  • Convergent Fault is when two plates come
    together.
  • Not only can this cause destruction it can also
    cause construction. When two plates collide in a
    collision zone the result is mountains. The
    pressure of these two plates hitting each other
    causes the crust of the earth to rise. This can
    occur in the oceans of the world and on land.
    Mountain building is a very slow process but it
    is caused by convergent faults.

11
Transform Fault is when two plates slide past
each other.
  • Notice how the delta spreads in a fan shape.

12
Earthquakes
  • What is an earthquake?Earthquakes are the
    shaking, rolling or sudden shock of the earths
    surface. They are the Earth's natural means of
    releasing stress. More than a million earthquakes
    rattle the world each year.

13
  • Earthquakes most commonly occur along faults in
    the crust.   

Sometimes new landforms are created. Earthquakes
can happen on land and in water. An earthquake
can destroy everything that gets into its path.
It destroys buildings, bridges, dams, and other
structures.
14
Where do earthquakes happen?
15
Why?
Most naturally occurring earthquakes are related
to the tectonic nature of the Earth. Such
earthquakes are called tectonic earthquakes. The
Earth's lithosphere is a patchwork of plates in
slow but constant motion caused by the release to
space of the heat in the Earth's mantle and core.
16
Why continued
  • The heat causes the rock in the Earth to warm so
    that the plates move slowly but surely. Plate
    boundaries lock as the plates move past each
    other, creating frictional stress. When the
    frictional stress exceeds a critical value,
    called local strength, an earthquake happens.

17
  • The West Coast is most at risk of having an
    earthquake, but earthquakes can happen in the
    Midwest and along the East Coast. Earthquakes can
    be felt over large areas although they usually
    last less than one minute. Earthquakes cannot be
    predicted - although scientists are working on
    it!

18
Quit pushing!!
19
Largest Fault in the US The San Andreas Fault
20
  • Natural Disasters - Earthquakes - Fault Lines 

21
Technology and Earthquakes
  • Earthquakes generate seismic waves which can be
    detected with a sensitive instrument called a
    seismograph. Advances in seismograph technology
    have increased our understanding of both
    earthquakes and the Earth itself.
  • Perhaps the earliest seismograph was invented in
    China A.D. 136 by a m an named Choko.

22
Volcanoes
  • A volcano is a mountain or hill formed by the
    accumulation of magma or molten rock. Magma is
    typically produced at depths of 50 to 60 miles
    below the surface because liquid magma is less
    dense than solid rock, it is pushed out of cracks
    in the Earth's surface. Volcanic eruptions can be
    deadly, damaging property and infrastructure.

23
Volcano Types
  • Volcanoes are one of the most powerful forces in
    nature. A volcano is a hole in the earths crust.
    The hollow holes that are in volcanoes are called
    craters. There are different types of volcanoes 
    shield-volcanoes, cinder cone volcanoes, lava
    domes and the most common - composite volcanoes.

24
Volcanoes are basically hollowed-out mountains
with connections to the Earths magma core. There
are over 500 volcanoes in the world. The
volcanoes are contained in a circle called the
Ring of Fire.
25
  • Volcanic eruptions start in a magma chamber. The
    high pressure of the steams and gasses make the
    magma fill the magma chamber.
  • When the chamber is full, the type of eruption
    depends on the amount of gases and silica in the
    magma.
  • The amount of silica determines how sticky the
    magma is and the amount of water determines the
    explosive potential of the steam.

26
Evidence of Steam Magma
27
  • Volcanoes can form on land but they can also form
    in water. Volcanoes can help build up the Earth's
    surface (constructive) like the developing
    Hawaiian Islands, but volcanoes can also be very
    destructive to the Earth's surface.

28
Destructive Volcanoes
  • Volcanoes can endanger anything that happens to
    be in the vicinity of an erupting volcano such as
    humans, property, and agriculture. 
  • Volcanoes are destructive because when they erupt
    not only  can they spew hot ash and lava but they
    can also cause other destructive activities to
    occur.

29
Volcanic DiagramNotice the difference in
destruction on either side of the volcano.
30
Volcanic Landslide step 1
Mud flows also may occur with a volcano eruption
engulfing everything in its path..
  • Volcanic Landslide step 2

31
  • Volcanoes are destructive because when they erupt
    not only  can they spew hot ash and lava but they
    can also cause other destructive activities to
    occur.
  • Lava flows can destroy homes, grass, trees, and
    anything else in its destructive path.   The lava
    which is hot melted rock flows from one place to
    another burning everything it touches.

32
Tsunamis and Earthquakes
  • Two main destructive forces can be triggered by a
    volcano tsunamis and earthquakes.
  • Damage to the Earth's surface caused by a volcano
    is often not repairable but over many, many years
    some new growth may begin to appear.

33
Good Thing/Bad thing
  • There are many constructive properties of
    volcanoes. For example, volcanoes help the
    rock-cycle by bringing rocks to the surface to
    form new landforms like islands.  All of the
    Hawaiian Islands were created by volcanoes. There
    is even a new island forming right now.

34
  • Another example of a volcanoes' constructive
    force is that if there are enough eruptions or a
    constant lava flow a mountain can form. Some of
    these mountains form on land but many build from
    the bottom of oceans.

35
Here are other ways a volcano can be
constructive...
  • volcanic ash can be used as an abrasive or
    cleaning agent
  • volcanic ash can act as a mulch
  • volcanoes can create geothermal energy
  • ashes can make more fertile soil
  • To see an animation of an erupting volcano  click
    here.

36
Erosion
  • Erosion is a process in which rock and soil are
    broken loose from the earth's surface at one
    location and moved to another.

37
Water Erosion
  • Moving water (like a stream) is an important
    agent in the erosion process. Dirt and other
    sediment get in the water and then the moving
    water moves it to a new location.  
  • Gravity plays an important role as well in
    erosion gravity pulls down dirt and other stuff
    from the hills and causes erosion.

38
Wind Erosion
  • Wind erosion occurs mostly in flat, dry areas and
    close to bodies of water.  Wind erosion removes
    the most fertile part of soil and lowers the soil
    production. That means most crops and plants will
    not make it to harvest time. All that is left
    after wind erosion in soil is the clayish soil
    and silts.

39
  • In the 1930s a long dry spell got bad enough it
    turned into dust storms. They called it the Black
    Blizzards and it became known as  the Dust Bowls.
  • Want to know more? Click here

40
Weathering
  • Weathering is the process of decomposition or
    disintegration of rocks and their minerals. That
    is why it is considered a destructive force. The
    rocks and their minerals break down into smaller
    pieces like silt, clay and sand.

41
  • The weathering process occurs at or near the
    surface of the earth. In fact, the soil we depend
    on for much of our food is a mixture of bits and
    pieces of weathered rock.

42
Weathering and Water
  • One of the major causes of weathering is water.
    Moving waters such as rivers and oceans can
    permanently change the Earth's surface. The
    waters and rivers can carve deep canyons or
    weather cliffs along the seashore causing them to
    fall into the waters.

43
  • Rain water can also cause weathering. As it
    rains, rain water can seep into holes and cracks
    in rocks causing weathering and if this water
    freezes inside the rock, this can cause the rock
    to break into smaller pieces.

44
Extreme Heat
  • Extreme heat is an example of weathering that can
    cause destructive changes to the surface of the
    earth.
  • Rocks that become heated at the surface of the
    earth can expand and then contract. If this
    happens often enough the expansion and
    contraction of rock would eventually cause
    weathering.

45
Plants
  • Plant roots grow in cracks of rocks. As they
    grow, they force open the cracks. This is another
    way pieces of rock can be broken off.

46
Weathering and Erosion
  • Weathering and erosion often occur at the same
    time. After weathering has broken the rocks into
    smaller pieces, other processes like erosion and
    deposition move the broken pieces to other
    places.
  • Weathering is a destructive force because it
    changes rocks by breaking them into smaller
    pieces.

47
Weathering processes are divided into three
categories
  •    Physical or Mechanical Weathering
  •    Chemical Weathering
  •    Biological Weathering

48
  • Physical or Mechanical Weathering   breaks
    larger rocks into smaller rocks without changing
    what the rock is made of. Examples
  • Chemical Weathering   involves changing what the
    rock is made of. Chemical weathering causes the
    rocks to become weak and eventually crumble.
    Examples
  • Biological Weathering is the actual molecular
    breakdown of minerals.
  • Example Lichens live on rocks and they slowly
    eat away at the surface of rocks

49
Technology and Flood Control
  • http//www.gcwallace.com/ServicesLasVegasFloodCont
    rol.asp

50
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51
European Flood Control
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