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Dynamic Earth. Class 5 24 January 2006. Any Questions?. Interacting Earth Systems Volcanoes contribute gases to the atmosphere . This is how the oceans were formed 3-4 Billion years ago. Lithosphere Hydrosphere Atmosphere Biosphere.

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dynamic earth

Dynamic Earth

Class 5

24 January 2006

slide3
Interacting Earth SystemsVolcanoes contribute gases to the atmosphere. This is how the oceans were formed 3-4 Billion years ago
slide4

Lithosphere

Hydrosphere

Atmosphere

Biosphere

plate tectonics
Plate Tectonics
  • Fundamental Concept and Unifying Theory in Earth Science
  • Idea is > 100 yrs old
  • Acceptance only within the past 30 years
plate tectonics1
Plate Tectonics
  • How and why did it come about?
  • During the 1800’s geologists recognized many strange things that seemed to imply that the continents had once been together.
the fit of the continents
The fit of the continents

1915: Alfred Wegener Origin of the Continents and Oceans

fit of the continents
Fit of the continents

Alexander du Toit:

Continuity of rocks between Africa and South America

the same kinds of fossils appear on both sides of the atlantic mesosaurs lived in fresh water
The same kinds of fossils appear on both sides of the Atlantic(Mesosaurs lived in fresh water)
slide16

There is evidence that huge glaciers occupied large parts of the southern continents about 250 million years ago.

slide17

This distribution is very difficult to explain if the continents were in this position during the time of glaciation.

slide20

The Theory of “Continental Drift” proposed that Pangea began to break upin the Triassic (200 Million Years Ago)

slide21

Gondwanaland (southern continent) began to break up in the Jurassic Period(135 Million Years Ago)

acceptance of continental drift
Acceptance of Continental Drift?
  • Evidence for continental drift purely descriptive
    • Description is not an explanation
  • Theory must explain how continents move
    • No plausible explanation for driving force
  • Wegener thought that continents floated like boats across the solid ocean crust, dragged along by the tidal forces of the Sun and Moon
holmes explanation of continental drift 1928
Holmes’ explanation of continental drift (1928)

Convection deep in the Earth could push and pull the continents apart, creating new oceanic crust through the process of seafloor spreading.

slide27

Convection

Water boiling in a pan on your stove is an example of convection

slide28

Convection

Hot water rises

Cold water sinks

holmes explanation of continental drift 19281
Holmes’ explanation of continental drift (1928)

Holmes’ proposed convection currents “dragged the two halves of the original continents apart, with consequent mountain building in the front where the currents are descending, and the ocean floor development in the site of the gaps, where the currents are ascending.”

Holmes’ theory was almost universally ignored because of the influence of Sir Harold Jeffreys…

Jeffreys thought the idea crazy! His observations of earthquakes suggested that Earth’s interior far too rigid – as rigid as steel.

holmes explanation of continental drift 19282
Holmes’ explanation of continental drift (1928)

Holmes conceded that “purely speculative ideas of this kind, specifically invented to match the requirements, can have no scientific value until they acquire support from independent evidence.”

slide31

Why was Continental Drift

not accepted?

  • Because it was difficult to under-stand how continents could move.
  • What did we learn to make us more willing to accept the idea that the continents have moved?
jump ahead to the 1960s
Jump ahead to the 1960s

Maps and paintings by Marie Tharp allowed geologists to visualize the newly available bathymetry

drilling into the seafloor provided m ore evidence supporting sea floor spreading
Drilling into the seafloor provided more evidence supporting sea-floor spreading
  • Micropaleontology of sediments
  • Dating of the underlying lavas

Drilling ship Glomar Challenger

slide39

Earth’s Magnetic Field

Another key to understanding the puzzle.

slide40

Earth’s Magnetic Field

The Earth behaves like a magnet whose poles are nearly coincident with the spin axis (i.e., the geographic poles).

slide41

Earth’s Magnetic Field

Magnetic lines of force emanate from the magnetic poles.

A suspended magnet is inclined due to the magnetic field.

slide42

A compass points North because theneedle is made of iron. It becomes aligned in the Earth’s magnetic field.

slide43

Magma formed at spreading centers contains minute pieces of iron that become aligned in the direction of the Earth’s magnetic field.

slide44

When the magma cools, the iron pieces remain frozen in this alignment, pointing toward the Earth’s magnetic North Pole.

slide46

Magnetic reversals

  • A special property of the Earth’s magnetic field is that it has reversed its direction many times in the past.
  • When this happens, rocks formed at that time are magnetized pointing toward the South Pole.
magnetic reversals
Magnetic reversals
  • The last reversal was about 700,000 years ago.
  • These reversals appear to be abrupt (probably only take about 1000 years or so).
magnetic reversals1
Magnetic reversals
  • A period of time in which magnetism is dominantly of one polarity is called a magnetic epoch.
  • We call north polarity normal and south polarity reversed.
the geomagnetic time scale
The GeomagneticTime Scale

Based on determining the magnetic characteristics of rocks of known age (from both the oceans and the continents).

We have a good record of geomagnetic reversals back to about 60 Million years ago.

t hur sday
Thursday
  • Continue with Sea Floor Spreading and Plate Tectonics
  • Please finish reading Chapter 2
homework 2 due january 31 st

Homework #2Due January 31st

Find it on the Web Site