The document discusses the history of theories of plate tectonics. It describes how early theories viewed the Earth's crust as rigid and unmoving, but accumulating evidence from seafloor mapping, core sampling, and studies across scientific disciplines demonstrated that the crust is made up of mobile tectonic plates that move and interact along boundaries. The modern theory of plate tectonics explains continental drift, mountain building, volcanism and earthquakes based on the dynamics of divergent, convergent, and transform plate boundaries.
Rigid Earth Theory. Plasticity. Isostacy. Alfred Wegener and Continental Drift. Wegener's lines of evidence. Harry Hess and more evidence. Power source = convection currents in the mantle. Theory of Plate Tectonics. Plate boundaries: Divergent (spreading centers), Convergent (subduction zones), Lateral (transform faults). Three types of subduction zones. Hot spots. Accreted Terranes. Cratons. Continental Shields. Topography. (maps for lab)
Rigid Earth Theory. Plasticity. Isostacy. Alfred Wegener and Continental Drift. Wegener's lines of evidence. Harry Hess and more evidence. Power source = convection currents in the mantle. Theory of Plate Tectonics. Plate boundaries: Divergent (spreading centers), Convergent (subduction zones), Lateral (transform faults). Three types of subduction zones. Hot spots. Accreted Terranes. Cratons. Continental Shields. Topography. (maps for lab)
Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle. This strong outer layer is called the lithosphere.
Plate Tectonic is a theory explaining the structure of the earth's crust and many associated phenomena as resulting from the interaction of rigid lithospheric plates which move slowly over the underlying mantle.
This Powerpoint Presentaion is used for my 11th Grade Earth Science Reporting as a major requirement for our sujbect. It talks about the tectonic processes and Plate boundaries with its theories..
Physical Geography Lecture 11 - The Lithosphere 111416angelaorr
Geologic time. Dating rocks. Earth's oldest rocks. Uniformitarianism. Earth's interior structure. The elements that make up Earth's solid material. What is a mineral? (The definition, broken down.) Mineraloid. Biogenic minerals. Non-organic formation: magma, vaporites, evaporites, precipitates. What is a rock? The rock cycle. The rock cycle's power source. Convection currents in the mantle. Igneous, sedimentary, and metamorphic rocks--details of each.
Study of plate tectonics of the earth, or plate movement, Jahangir Alam
a) Wegener’s Evidence (Continental Drift)
b) History of Plate Tectonics
c) Breakup and Appearence of Pangea
WHAT IS A PLATE?
Major continental and oceanic plates include:
Types of Earth’s Crust:
Plate tectonics (from the Late Latin tectonicus) is a scientific theory which describes the large scale motions of Earth's lithosphere.
THE DYNAMIC EARTH:
The earth is a dynamic planet, continuously changing both externally and internally. The earth’s surface is constantly being changed by endo-genetic processes resulting in volcanism and tectonism, and exogenetic processes such as erosion and deposition. These processes have been active throughout geological history. The processes that change the surface feature are normally very slow (erosion and deposition) except some catastrophic changes that occur instantaneously as in the case of volcanism or earthquakes. The interior of the earth is also in motion. Deeper inside the earth, the liquid core probably flows at a geologically rapid rate of a few tenths of mm/s. Several hypotheses attempted to explain the dynamism of the earth.
+ Horizontal movement hypothesis
+ Continental drift, displacement hypothesis
Development of the plate tectonic theory.
Plate tectonic theory arose out of the hypothesis of continental drift proposed by Alfred Wegener in 1912. He suggested that the present continents once formed a single land mass that drifted apart, thus releasing the continents from the Earth's core and likening them to "icebergs" of low density granite floating on a sea of denser basalt.
Seafloor Spreading
The first evidence that the lithospheric plates did move came with the discovery of variable magnetic field direction in rocks of differing ages.
Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle. This strong outer layer is called the lithosphere.
Plate Tectonic is a theory explaining the structure of the earth's crust and many associated phenomena as resulting from the interaction of rigid lithospheric plates which move slowly over the underlying mantle.
This Powerpoint Presentaion is used for my 11th Grade Earth Science Reporting as a major requirement for our sujbect. It talks about the tectonic processes and Plate boundaries with its theories..
Physical Geography Lecture 11 - The Lithosphere 111416angelaorr
Geologic time. Dating rocks. Earth's oldest rocks. Uniformitarianism. Earth's interior structure. The elements that make up Earth's solid material. What is a mineral? (The definition, broken down.) Mineraloid. Biogenic minerals. Non-organic formation: magma, vaporites, evaporites, precipitates. What is a rock? The rock cycle. The rock cycle's power source. Convection currents in the mantle. Igneous, sedimentary, and metamorphic rocks--details of each.
Study of plate tectonics of the earth, or plate movement, Jahangir Alam
a) Wegener’s Evidence (Continental Drift)
b) History of Plate Tectonics
c) Breakup and Appearence of Pangea
WHAT IS A PLATE?
Major continental and oceanic plates include:
Types of Earth’s Crust:
Plate tectonics (from the Late Latin tectonicus) is a scientific theory which describes the large scale motions of Earth's lithosphere.
THE DYNAMIC EARTH:
The earth is a dynamic planet, continuously changing both externally and internally. The earth’s surface is constantly being changed by endo-genetic processes resulting in volcanism and tectonism, and exogenetic processes such as erosion and deposition. These processes have been active throughout geological history. The processes that change the surface feature are normally very slow (erosion and deposition) except some catastrophic changes that occur instantaneously as in the case of volcanism or earthquakes. The interior of the earth is also in motion. Deeper inside the earth, the liquid core probably flows at a geologically rapid rate of a few tenths of mm/s. Several hypotheses attempted to explain the dynamism of the earth.
+ Horizontal movement hypothesis
+ Continental drift, displacement hypothesis
Development of the plate tectonic theory.
Plate tectonic theory arose out of the hypothesis of continental drift proposed by Alfred Wegener in 1912. He suggested that the present continents once formed a single land mass that drifted apart, thus releasing the continents from the Earth's core and likening them to "icebergs" of low density granite floating on a sea of denser basalt.
Seafloor Spreading
The first evidence that the lithospheric plates did move came with the discovery of variable magnetic field direction in rocks of differing ages.
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Movement and locations of water. Underground water. Soil water belt, subsurface flow. Percolation. Porosity and Permeability. Hydrologic Zones. Zone of aeration, zone of saturation, water table, effluent and influent condition. Zone of confined water, aquaclude, aquifer, artesian well. Waterless zone. Groundwater management. Groundwater management issues. Aquifer recharge, cone of depression, subsidence, groundwater contamination. The case of Venice Italy. Hydrothermal activity. Hot springs, geysers, fumaroles. Permafrost, melting permafrost. Glaciers, alpine and continental glaciers. Melting glaciers. Lakes. Destruction of the Aral Sea. Swamps and marshes. Streams.
Physical Geography Lecture 08 - Precipitation, Air Masses, and Storms 110216angelaorr
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Physical Geography Lecture 07 - Clouds and Transfer of Latent Heat 102616angelaorr
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Air pressure. Relationships between pressure, density, and temperature (confined vs. unconfined gases). Measuring air pressure. Isobars. The pressure gradient force. Wind. Convection cell diagram. Out of the high, into the low. Local winds (sea/land breezes, mountain/valley breezes, Chinook/Santa Ana winds).
Physical Geography Lecture 05 - Atmospheric Energy and Global Temps 101216angelaorr
Net radiation. Hypothetical radiation balance. Albedo, Conduction, Convection, Counterradiation. The Greenhouse Effect. Redistribution of energy. Sensible heat vs. Latent heat. Temperature lags. Factors influencing differences in global temperature. Review.
Review of last week's lecture. Air's composition. Particulates. Vertical structure of the atmosphere. Conduction, ELR, ozone. Review of today's material.
Physical Geography Lecture 04 - Earth's Energy and Seasons 10.03.16angelaorr
Earth In Space. Variations in Earth's Motion. Earth's Orbit. Axial Tilt. Solstices and Equinoxes. Properties of Electromagnetic Radiation. Insolation and the Solar Constant.
Uniformitarianism. Eratosthenes. Earth's size and shape. Centrifugal force. Earth's rotation and revolution. Navigation: great circles and small circles. The geographic grid. Time zones. Review
Physical Geography Lecture 01 - What Is Geography 092616angelaorr
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3. Rigid Earth Theory
• It was once believed that Earth’s crust was
hard and brittle and could not bend
4. Rigid Earth Theory
• It was once believed that Earth’s crust was
hard and brittle and could not bend
5. Rigid Earth Theory
• It was once believed that Earth’s crust was
hard and brittle and could not bend
• Plasticity
6. Rigid Earth Theory
• It was once believed that Earth’s crust was
hard and brittle and could not bend
• Plasticity
– We now know that Earth’s crust can bend (like
a tough plastic) before breaking
7. Isostacy
• “The maintenance of hydrostatic
equilibrium in the crust”
– hydrostatics—branch of physics related to the
pressure and equilibrium of liquids (hydro)
• statics—bodies not active; at rest; in equilibrium;
as opposed to dynamics
9. Isostacy
• Addition or removal of crustal material causes a sinking
or rebounding of crust
10. Isostacy
• Addition or removal of crustal material causes a sinking
or rebounding of crust
– Add or remove continental mass and the crust will sink
or rise to accommodate the added/removed weight
11. Isostacy
• Addition or removal of crustal material causes a sinking
or rebounding of crust
– Add or remove continental mass and the crust will sink
or rise to accommodate the added/removed weight
• a glacier growing or remelting, crust eroding off the
surface, sediment deposits, water bodies on land,
esp. those created by dams
13. Alfred Wegener and
His Continental Drift Theory
• German meteorologist, 1920s
“The present continents were
originally connected as one
enormous landmass that has
broken up and drifted apart over
the last few 100 million years.
The drifting continues….”
14. Alfred Wegener and
His Continental Drift Theory
• German meteorologist, 1920s
“The present continents were
originally connected as one
enormous landmass that has
broken up and drifted apart over
the last few 100 million years.
The drifting continues….”
• Pangaea (Gk. “whole land”)
15. Alfred Wegener and
His Continental Drift Theory
• German meteorologist, 1920s
“The present continents were
originally connected as one
enormous landmass that has
broken up and drifted apart over
the last few 100 million years.
The drifting continues….”
• Pangaea (Gk. “whole land”)
17. Wegener’s Lines of Evidence
• Similar geology (rocks and rock structures)…
18. Wegener’s Lines of Evidence
• Similar geology (rocks and rock structures)…
• …petrology (rock chemistry),
19. Wegener’s Lines of Evidence
• Similar geology (rocks and rock structures)…
• …petrology (rock chemistry),
• …paleontology (fossilized plants and animals),
20. Wegener’s Lines of Evidence
• Similar geology (rocks and rock structures)…
• …petrology (rock chemistry),
• …paleontology (fossilized plants and animals),
• …matching glacial features (U-shaped valleys,
glacial deposits, etc.) on continents separated by
oceans
21. Wegener’s Lines of Evidence
• Similar geology (rocks and rock structures)…
• …petrology (rock chemistry),
• …paleontology (fossilized plants and animals),
• …matching glacial features (U-shaped valleys,
glacial deposits, etc.) on continents separated by
oceans
• …continent shapes that seem to fit together,
22. Wegener’s Lines of Evidence
• Similar geology (rocks and rock structures)…
• …petrology (rock chemistry),
• …paleontology (fossilized plants and animals),
• …matching glacial features (U-shaped valleys,
glacial deposits, etc.) on continents separated by
oceans
• …continent shapes that seem to fit together,
• …patterns in the locations of volcanoes
23. Wegener’s Lines of Evidence
• Similar geology (rocks and rock structures)…
• …petrology (rock chemistry),
• …paleontology (fossilized plants and animals),
• …matching glacial features (U-shaped valleys,
glacial deposits, etc.) on continents separated by
oceans
• …continent shapes that seem to fit together,
• …patterns in the locations of volcanoes
24. Wegener’s Lines of Evidence
• Similar geology (rocks and rock structures)…
• …petrology (rock chemistry),
• …paleontology (fossilized plants and animals),
• …matching glacial features (U-shaped valleys,
glacial deposits, etc.) on continents separated by
oceans
• …continent shapes that seem to fit together,
• …patterns in the locations of volcanoes
Ex.: S. America/Africa, Madagascar/India, Australia/Antarctica
27. …but no one bought it.
The
crust is
too
rigid!
28. …but no one bought it.
The So why don’t we
crust is see the crust
too ripping apart
rigid! right now?
29. …but no one bought it.
The So why don’t we
crust is see the crust
too ripping apart
rigid! right now?
What do you
mean, “The
continents are
floating???”
30. …but no one bought it.
The So why don’t we
crust is see the crust
too ripping apart
rigid! right now?
And hey, what’s the
What do you power source driving
mean, “The these movements of all
continents are the land masses,
floating???” anyway???
31. …but no one bought it.
The So why don’t we
crust is see the crust
too ripping apart
rigid! right now?
And hey, what’s the
What do you power source driving
mean, “The these movements of all
continents are the land masses,
floating???” anyway???
What a
knucklehead.
37. The evidence continued to mount…
• Military seafloor mapping: Seafloor geology—
structure, chemistry, and age
38. The evidence continued to mount…
• Military seafloor mapping: Seafloor geology—
structure, chemistry, and age
– Oceanic crust: only 100 m.y.o
39. The evidence continued to mount…
• Military seafloor mapping: Seafloor geology—
structure, chemistry, and age
– Oceanic crust: only 100 m.y.o
– Continental crust: 4.1 b.y.o.
40. The evidence continued to mount…
• Military seafloor mapping: Seafloor geology—
structure, chemistry, and age
– Oceanic crust: only 100 m.y.o
– Continental crust: 4.1 b.y.o.
• Core sampling
41. The evidence continued to mount…
• Military seafloor mapping: Seafloor geology—
structure, chemistry, and age
– Oceanic crust: only 100 m.y.o
– Continental crust: 4.1 b.y.o.
• Core sampling
• Seafloor sediment
42. The evidence continued to mount…
• Military seafloor mapping: Seafloor geology—
structure, chemistry, and age
– Oceanic crust: only 100 m.y.o
– Continental crust: 4.1 b.y.o.
• Core sampling
• Seafloor sediment
• Rigid Earth folks retired—paradigm shift to plasticity
43. The evidence continued to mount…
• Military seafloor mapping: Seafloor geology—
structure, chemistry, and age
– Oceanic crust: only 100 m.y.o
– Continental crust: 4.1 b.y.o.
• Core sampling
• Seafloor sediment
• Rigid Earth folks retired—paradigm shift to plasticity
• Convection currents as mechanism/power source
44. The evidence continued to mount…
• Military seafloor mapping: Seafloor geology—
structure, chemistry, and age
– Oceanic crust: only 100 m.y.o
– Continental crust: 4.1 b.y.o.
• Core sampling
• Seafloor sediment
• Rigid Earth folks retired—paradigm shift to plasticity
• Convection currents as mechanism/power source
• Geologists, geophysicists, seismologists,
oceanographers, physicists, and paleontologists all
agree the theory fits the evidence gathered within
their respective fields
45. The Theory of Plate Tectonics
Tectonic (crustal) plates
• Pulling apart (spreading/diverging)
• Slamming together and sinking
(subducting/converging)
• Sliding laterally (sideways)
50. Convergent Plate Boundaries
• Subduction zones
– Crust being forced together
– Lightest material rises (mountain-building) while
the heaviest stuff sinks (pushed back into the
mantle)
51. Convergent Plate Boundaries
• Subduction zones
– Crust being forced together
– Lightest material rises (mountain-building) while
the heaviest stuff sinks (pushed back into the
mantle)
– Remelting (mostly from friction) creates volcanoes
52. Convergent Plate Boundaries
• Subduction zones
– Crust being forced together
– Lightest material rises (mountain-building) while
the heaviest stuff sinks (pushed back into the
mantle)
– Remelting (mostly from friction) creates volcanoes
– Intense, deep-focus earthquakes
55. Three Types of Subduction Zones
1. Continental crust meets oceanic crust
56. Three Types of Subduction Zones
1. Continental crust meets oceanic crust
– Oceanic crust sinks
57. Three Types of Subduction Zones
1. Continental crust meets oceanic crust
– Oceanic crust sinks
– Big trench offshore
58. Three Types of Subduction Zones
1. Continental crust meets oceanic crust
– Oceanic crust sinks
– Big trench offshore
– Volcanoes on the continental margin
59. Three Types of Subduction Zones
1. Continental crust meets oceanic crust
– Oceanic crust sinks
– Big trench offshore
– Volcanoes on the continental margin
– Big earthquakes (potential for tsunamis)
63. Three Types of Subduction Zones
2. Oceanic crust meets oceanic crust
64. Three Types of Subduction Zones
2. Oceanic crust meets oceanic crust
– The older and colder crust will probably sink
65. Three Types of Subduction Zones
2. Oceanic crust meets oceanic crust
– The older and colder crust will probably sink
– Big earthquakes and volcanic islands (called
“island arcs”)
66. Three Types of Subduction Zones
2. Oceanic crust meets oceanic crust
– The older and colder crust will probably sink
– Big earthquakes and volcanic islands (called
“island arcs”)
– Deep ocean trench
67. Three Types of Subduction Zones
2. Oceanic crust meets oceanic crust
– The older and colder crust will probably sink
– Big earthquakes and volcanic islands (called
“island arcs”)
– Deep ocean trench
– Potential for tsunamis
70. Three Types of Subduction Zones
3. Continental crust meets continental crust
71. Three Types of Subduction Zones
3. Continental crust meets continental crust
– Too light to subduct
72. Three Types of Subduction Zones
3. Continental crust meets continental crust
– Too light to subduct
– Mountain-building
73. Three Types of Subduction Zones
3. Continental crust meets continental crust
– Too light to subduct
– Mountain-building
– Big earthquakes
74. Three Types of Subduction Zones
3. Continental crust meets continental crust
– Too light to subduct
– Mountain-building
– Big earthquakes
– Little if any volcanism (mostly intrusive)
78. Transform Fault Boundaries
• Tectonic plates slide past one another
– Earthquakes are less intense than subduction
79. Transform Fault Boundaries
• Tectonic plates slide past one another
– Earthquakes are less intense than subduction
– No volcanoes
80. Transform Fault Boundaries
• Tectonic plates slide past one another
– Earthquakes are less intense than subduction
– No volcanoes
– Little or no mountain-building
83. “Hot spots”
• Also called magma plumes
• Generally occur some distance from any
other type of plate boundary
84. “Hot spots”
• Also called magma plumes
• Generally occur some distance from any
other type of plate boundary
• Unrelated to convergent, divergent, or
transform boundaries
85. “Hot spots”
• Also called magma plumes
• Generally occur some distance from any
other type of plate boundary
• Unrelated to convergent, divergent, or
transform boundaries
• Anomalous (odd) “balloons” of rising magma
86. “Hot spots”
• Also called magma plumes
• Generally occur some distance from any
other type of plate boundary
• Unrelated to convergent, divergent, or
transform boundaries
• Anomalous (odd) “balloons” of rising magma
– Hot spot stays in one position as the moving,
island-covered crustal plate rides away from it
87.
88.
89. Accreted Terranes
• A moving continent may
pick up new land material
as lighter (felsic) material
scrapes off of a
subducting plate
90. Accreted Terranes
• A moving continent may
pick up new land material
as lighter (felsic) material
scrapes off of a
subducting plate
91. Craton
• These terranes were added to the original
material first formed from magma that rose
out of Earth’s earliest crust
– Craton--the name given to these ancient proto-
continents
cratons
29
92. Continental Shields
• More magma material was added to the
cratons, forming continents.
– Continental shields: Where the earliest
continental material still exists intact and is
exposed at the surface.
30
94. Topography
• Right from the very beginning, the crust
was affected by stresses and strains that
caused crustal deformations
• Over time, the crust has continued to be
folded, faulted, broken, eroded and further
built upon, creating the topography, the
ups and downs of land relief, that we see
today
32