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New Zealand Earthquake
• M 6.3 earthquake
• Shallow epicenter: 2-
3 miles
• Close to Christchurch,
city of 370,000
• After shock to the
September 4th M 7.1
What is the composition of
lava formed on oceanic crust?
High percentages Fe, Mg
Low percentages Si, O
DESCRIBE A CONVERGENT
PLATE BOUNDARY
What is the source of the lava
that forms oceanic crust?
the mantle or asthenosphere
What is the composition of
lava associated with
continental crust?
High percentages Si, O
Low percentages Fe, Mg
The Theory of Plate Tectonics
• Based on two hypotheses
– Continental Drift
– Seafloor spreading
Explain the development of the
theory of plate tectonics in
terms of the scientific method.
The
Scientific
Method
One or more ideas, statements or questions;
Single or multiple hypotheses
Collection of data
Observation of data or information
Theory
Not accepted Hypothesis
More Data
Continental drift hypothesis:
evidence?
• Proposed in 1911
• All evidence found on the continents
• Mechanism for moving the continents was
not known
• Alfred Wegener
proposed the
hypothesis of
continental drift in
1911
• He gathered
information from many
different sources and
used it as evidence for
his hypothesis
Continental Drift Hypothesis
• Fit of the continents
• Fossil evidence
• Ancient mountain ranges
• Past climate evidence
Continental Drift Hypothesis
Glaciers formed at the south pole
Swamps formed in tropical regions
• The
continental
drift
hypothesis
proposes that
the continents
were
assembled to
form the super
continent
Pangaea.
• Moved
through time
3:20
• Antonio Snider-Pelligrini
(1858), a geographer cut
out a map of Africa and
South America
suggesting they were
connected at one time
• Other physical evidence
based on observation
was used by Wegener
Fit of Continents
Fossil Evidence
• Similar terrestrial species were found on many
continents now separated by oceans.
• Information collected by paleontologists
Ancient Mountain Ranges
The same sequence of rocks is found in North America,
Great Brittan, and Norway. The pattern does not make
sense with the continents in their current configuration.
The Appalachian Mountains
Swamps
300 million years ago
Evidence of
Ancient Glaciers
•Glaciers carve the rock as they move.
•Scientists can determine the direction of movement (notice the
direction of movement noted in South America)
•As South America sits today, the pattern would not make sense.
(glaciers do not move from sea level to higher elevations)
Lack of mechanism to explain
continental movement.
• Evidence implied that the continents were at one
time assembled
• Wegener’s idea was not accepted by the
scientific community because he could not
explain how the continents moved
• With advances in technology, new information
was gathered in association with WWII
• What information do you know regarding
the seafloor that may be used to help
understand the hypothesis of seafloor
spreading?
Exploration of the Ocean Basins
Exploration of the Ocean Basins
• Seafloor features
• Composition of the seafloor
• Age of the seafloor
• Hot spots
• Seismicity
• Paleomagnetic pattern produced on the
seafloor
Exploration of Ocean Basins
Ocean basins contain a variety of landforms not discovered until WW II.
Support
• Echo sounding was used to map the seafloor
Seafloor features were
discovered using sonar.
4:26
Seafloor
features
• Mid-oceanic
ridges
• Trenches
• Volcanism
adjacent to
trenches
• Seamounts
• Fracture zones
Oceanic crust is composed of
volcanic rock.
• Basalt is volcanic rock with a mafic composition.
• Higher percentages of iron and magnesium, lower
percentages of silicon and oxygen.
Pillow basalts
Age of Ocean Crust
• Youngest at ridge
• Progressively older away from ridge
• Mirror image across the ridge
Seismicity
• Earthquakes are concentrated at what is
currently known as plate boundaries.
• Explain why there are broad bands of
seismicity associated with some areas.
Earth’s Magnetic Field
Bipolar:
acts like
a bar
magnet
Requirements for a magnetic
field
• An interior region of electrically conducting
fluid such as molten metal.
• Convection in that layer of fluid.
• At least moderately rapid rotation.
A compass has a different
declination depending on the
location on the Earth’s surface
Earth’s Magnetic Field
• Strength varies with location
– Red- stronger
– Blue weaker
Iron-rich rocks are magnetized as
they cool to the current magnetic
field.
• Basalt= iron rich volcanic rock; oceanic
crust
Paleomagnetic pattern across the
mid-oceanic ridge
Mirror image across the ridge and correlative with age
Positive
anomalies=
normal
polarities
Negative
anomalies =
reverse
polarities
Polar
Reversals
• Correlated to time
• Scientists dated iron-
rich volcanic rocks on
land
• Developed
technology to
measure the
paleomagnetic
reading
Polar Reversals
• Timescale of polar
reversals
• Possibly related to
flow in the outer
core
Paleomagnetic Evidence
• Positive and negative recordings of the
oceanic crust create a symmetrical pattern
across the mid-oceanic trench
• In the 1963, Harry
Hess developed the
idea of seafloor
spreading to explain
the seafloor’s
formation
• Continental
movement is the
result of ocean floor
movement
Seafloor Spreading
Seafloor Spreading
• Mafic lava is extruded along the mid-oceanic ridge to
produce ocean floor.
• New material is added, the cooler material is split and is
“pushed” away from the ridge
Driving Mechanisms
Convection cells within
the mantle
Pushing at the mid-
oceanic ridges
Pulling at the subduction
zones
Push
Pull
Convection
The theory of plate tectonics
• Explains that the Earth’s lithosphere is
broken into distinct units that move as a
coherent package. Where the tectonic
plates meet, produces distinct physical
characteristics on the Earth’s surface.
The Scientific Method
Continental Drift Hypothesis
Collection of data
Observation of data or information
Theory of Plate Tectonics
Mechanism for plate movement
Not accepted
Seafloor Spreading Hypothesis
Associated
with the
continents
Ocean
basins
key
Information to understand:
• The evidence used by Wegener to describe
the continental drift hypothesis.
• The evidence associated with technology that
was used to collect information about ocean
basins.
• The hypothesis of seafloor spreading
• The accepted tectonic plate driving
mechanism.
Earthquakes and volcanoes outline
the tectonic plate boundaries

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continentahjjjjjjjjjghghhjghuyldrift.ppt

  • 1. New Zealand Earthquake • M 6.3 earthquake • Shallow epicenter: 2- 3 miles • Close to Christchurch, city of 370,000 • After shock to the September 4th M 7.1
  • 2. What is the composition of lava formed on oceanic crust? High percentages Fe, Mg Low percentages Si, O
  • 4. What is the source of the lava that forms oceanic crust? the mantle or asthenosphere
  • 5. What is the composition of lava associated with continental crust? High percentages Si, O Low percentages Fe, Mg
  • 6. The Theory of Plate Tectonics • Based on two hypotheses – Continental Drift – Seafloor spreading
  • 7. Explain the development of the theory of plate tectonics in terms of the scientific method.
  • 8. The Scientific Method One or more ideas, statements or questions; Single or multiple hypotheses Collection of data Observation of data or information Theory Not accepted Hypothesis More Data
  • 9. Continental drift hypothesis: evidence? • Proposed in 1911 • All evidence found on the continents • Mechanism for moving the continents was not known
  • 10. • Alfred Wegener proposed the hypothesis of continental drift in 1911 • He gathered information from many different sources and used it as evidence for his hypothesis Continental Drift Hypothesis
  • 11. • Fit of the continents • Fossil evidence • Ancient mountain ranges • Past climate evidence Continental Drift Hypothesis Glaciers formed at the south pole Swamps formed in tropical regions
  • 12. • The continental drift hypothesis proposes that the continents were assembled to form the super continent Pangaea. • Moved through time 3:20
  • 13. • Antonio Snider-Pelligrini (1858), a geographer cut out a map of Africa and South America suggesting they were connected at one time • Other physical evidence based on observation was used by Wegener Fit of Continents
  • 14. Fossil Evidence • Similar terrestrial species were found on many continents now separated by oceans. • Information collected by paleontologists
  • 15. Ancient Mountain Ranges The same sequence of rocks is found in North America, Great Brittan, and Norway. The pattern does not make sense with the continents in their current configuration.
  • 17. Evidence of Ancient Glaciers •Glaciers carve the rock as they move. •Scientists can determine the direction of movement (notice the direction of movement noted in South America) •As South America sits today, the pattern would not make sense. (glaciers do not move from sea level to higher elevations)
  • 18. Lack of mechanism to explain continental movement. • Evidence implied that the continents were at one time assembled • Wegener’s idea was not accepted by the scientific community because he could not explain how the continents moved • With advances in technology, new information was gathered in association with WWII
  • 19. • What information do you know regarding the seafloor that may be used to help understand the hypothesis of seafloor spreading? Exploration of the Ocean Basins
  • 20. Exploration of the Ocean Basins • Seafloor features • Composition of the seafloor • Age of the seafloor • Hot spots • Seismicity • Paleomagnetic pattern produced on the seafloor
  • 21. Exploration of Ocean Basins Ocean basins contain a variety of landforms not discovered until WW II.
  • 22. Support • Echo sounding was used to map the seafloor Seafloor features were discovered using sonar. 4:26
  • 23. Seafloor features • Mid-oceanic ridges • Trenches • Volcanism adjacent to trenches • Seamounts • Fracture zones
  • 24. Oceanic crust is composed of volcanic rock. • Basalt is volcanic rock with a mafic composition. • Higher percentages of iron and magnesium, lower percentages of silicon and oxygen. Pillow basalts
  • 25. Age of Ocean Crust • Youngest at ridge • Progressively older away from ridge • Mirror image across the ridge
  • 26.
  • 27. Seismicity • Earthquakes are concentrated at what is currently known as plate boundaries. • Explain why there are broad bands of seismicity associated with some areas.
  • 28.
  • 30.
  • 31.
  • 32. Requirements for a magnetic field • An interior region of electrically conducting fluid such as molten metal. • Convection in that layer of fluid. • At least moderately rapid rotation.
  • 33. A compass has a different declination depending on the location on the Earth’s surface
  • 34. Earth’s Magnetic Field • Strength varies with location – Red- stronger – Blue weaker
  • 35. Iron-rich rocks are magnetized as they cool to the current magnetic field. • Basalt= iron rich volcanic rock; oceanic crust
  • 36. Paleomagnetic pattern across the mid-oceanic ridge Mirror image across the ridge and correlative with age Positive anomalies= normal polarities Negative anomalies = reverse polarities
  • 37. Polar Reversals • Correlated to time • Scientists dated iron- rich volcanic rocks on land • Developed technology to measure the paleomagnetic reading
  • 38. Polar Reversals • Timescale of polar reversals • Possibly related to flow in the outer core
  • 39. Paleomagnetic Evidence • Positive and negative recordings of the oceanic crust create a symmetrical pattern across the mid-oceanic trench
  • 40. • In the 1963, Harry Hess developed the idea of seafloor spreading to explain the seafloor’s formation • Continental movement is the result of ocean floor movement Seafloor Spreading
  • 41. Seafloor Spreading • Mafic lava is extruded along the mid-oceanic ridge to produce ocean floor. • New material is added, the cooler material is split and is “pushed” away from the ridge
  • 42. Driving Mechanisms Convection cells within the mantle Pushing at the mid- oceanic ridges Pulling at the subduction zones Push Pull Convection
  • 43. The theory of plate tectonics • Explains that the Earth’s lithosphere is broken into distinct units that move as a coherent package. Where the tectonic plates meet, produces distinct physical characteristics on the Earth’s surface.
  • 44. The Scientific Method Continental Drift Hypothesis Collection of data Observation of data or information Theory of Plate Tectonics Mechanism for plate movement Not accepted Seafloor Spreading Hypothesis Associated with the continents Ocean basins key
  • 45. Information to understand: • The evidence used by Wegener to describe the continental drift hypothesis. • The evidence associated with technology that was used to collect information about ocean basins. • The hypothesis of seafloor spreading • The accepted tectonic plate driving mechanism.
  • 46. Earthquakes and volcanoes outline the tectonic plate boundaries