Ideas about Evolution of Earth (static to dynamic) - PowerPoint PPT Presentation

1 / 34
About This Presentation
Title:

Ideas about Evolution of Earth (static to dynamic)

Description:

Mohorovicic discontinuity: large jump in seismic P-waves 6-8 km/sec = base of crust. ... E-W motion due to tidal forces of sun and moon. ... – PowerPoint PPT presentation

Number of Views:71
Avg rating:3.0/5.0
Slides: 35
Provided by: geolo52
Category:

less

Transcript and Presenter's Notes

Title: Ideas about Evolution of Earth (static to dynamic)


1
Ideas about Evolution of Earth(static to dynamic)
  • Pre-Renaissance (Static Earth).
  • Renaissance to 20th Century (Geophysics
    Continental Drift).
  • 20th Century (Sea Floor Spreading).
  • Present-Day Perspective (Plate Tectonics
    Paradigm).

Important
2
Nature of Earth from the Greeks through the Dark
Ages.
  • Pre-1600 Myth and Religious view of Earth
  • Catastrophism catastrophic events due to angry
    gods.
  • Poseidon (Neptune) god of earthquakes
  • Typhon many-headed monster, source of storms
  • Zeus sky and weather god
  • Hades (Pluto) - god of the underworld
  • Vulcan god of fire, volcanoes
  • Center of Earth Hades

Important
3
(No Transcript)
4
Dantes Map of Hell
Geologists
Geophysicists?
5
Greek Science
Important
  • Knew the Earth was round.
  • Assumed that continents were fixed.
  • No information about ocean floor or earths
    interior.
  • Natural processes (not gods) formed geologic
    features.
  • Herodotus (484-426 B.C.), Empedocles (?), Pliny
    (23-79 A.D.) all studied geology, the latter two
    died while observing volcanoes.

6
The Development of Geophysics(internal structure
earth)
  • Renaissance to 20th century

7
Changing Views of Earth Earths Magnetic Field.
  • 1600 William Gilbert, Physician to Queen
    Elizabeth I, Published De Magnete. Earths
    magnetic field two-pole bar magnet.

8
Changing Views of Earth Earth Structure.
  • 1596-1650 Descartes proposed earth had
    metallic interior, middle shell of heavy rock and
    thin surface of sands and clays.

9
Changing Views of Earth Beginning of
Geophysics.
Important
  • 1687 Newtons laws of motion gravity.
  • 1650-1750 Start of Geologic mapping.
  • Combine into Start of Geophysics.

10
Changing Views of Earth
Important
  • Late 1700s Average density of earth 5.5
    g/cm3.
  • Since surface rocks 2.7 g/cm3 inner earth must
    be more dense.
  • 1785-1795 James Hutton Founder of modern
    geology
  • Dynamic view of earth as internal heat engine
    rather than static.
  • Magmatism melted rocks coming from depth.
  • Uniformitarianism steady state evolution of
    earth.

11
Changing Views of Earth
Important
  • 1873 J.D. Dana meteorites inner core of
    planets
  • Chondritic core (iron and nickle).
  • Stony outer parts (Fe,Mg silicates).
  • 1900s By turn of century recognized three-fold
    division of earth into core, mantle, and
    lithosphere.

12
How Do We Determine Internal Structure and
Composition Today?
  • Look at rocks exposed at surface (0-30 km and
    rarely100 km, China).
  • Drill holes (15 km, Khola Peninsular, Russia).
  • Magmatism (0-200 km deepest diamond bearing
    kimberlites).
  • Meteorites
  • Chondritic core
  • Stony outer parts.
  • Geophysics
  • Gravity
  • Magnetics
  • Heat Flow
  • Seismic Waves
  • Earth precession

13
Modern ViewInternal structure of Earth
Core
14
Internal structure of Earth
Asthenosphere
Mantle
Mesosphere
15
Internal structure of Earth
Important
Lithosphere
16
Changing Views of Earth 1800-1940
Important
1934 W.M. Elsasser flow in outer core causes
magnetic field.
17
Changing Views About the Continents The
Beginnings of Continental Drift
Important
18
Maps of Floating Continents
  • 1596 Abraham Ortelius (Dutch Cartographer)
    first suggested that continents joined together
    then separated.
  • 1620 Sir Francis Bacon Often thought to be the
    first to suggest continental drift, but really
    only noted similarity in shapes of continents.
  • 1846 Dana (geologist) continents and oceans
    stable and never change place.
  • 1846 Forbes (biologist) plant and animal
    evolution required continents to be connected at
    some time in the past.
  • 1858 Antonio Snider (Frenchman) noticed similar
    plant fossils in the coal seams of North America
    Europe. Made map of floating continents.
  • 1872 Reclus proposed that continental drift
    might be the cause of mountain building.
  • 1885 Suess (Swiss) plant fossils and glaciation
    in South America Africa similar (Gondwana).

19
1858 Antonio Sniders map of floating continents.
20
Scientists also recognized series of mountain
belts on edges of continents
Important
21
The cores of these mountain belts have been
strongly deformed Called Orogenic Belts.
Early reconstruction of European Alps
Big Folds
Big Faults
22
Fit of Continents?Why did mountains form?
  • EARLY IDEAS
  • A cooling ( shrinking) Earth...
  • Continental Drift Theory

23
LORD KELVIN AND THE SHRINKING EARTH
As cooled, it shrank!
Didnt know about all heat sources
24
1908-1910 F. B. Taylor (American)
Important
  • 1908 Published private pamphlet arguing for
    continental drift. Trying to explain formation
    and distribution of orogenic belts. Recently
    discovered mid-atlantic ridge as breaking point?
  • 1910 Publication proposed that continents moved
    like huge landslides from the poles towards the
    equators.
  • Suggested that
  • Moon captured in Cretaceous.
  • Initially closer to earth.
  • That gravitational forces would move continents.
  • Quickly disregarded because
  • Only needed 40 km displacement to explain
    mountain belts, not 1000s.
  • Tidal effect should stop rotation and/or rip
    apart earth within one year.

Continents Sliding off south pole
Continents Sliding off north pole
Collisions
25
1910 Alfred Wegener German meteorologist largely
working in southern hemisphere.
Important
  • Evidence of Africa and South America and other
    southern continents being together.
  • Shapes of continents fit back together.
  • Shared glacial and other geologic features.
  • Shared animal and plant fossils.
  • Shared climatic zones.

26
Fit of Africa and South America
27
(No Transcript)
28
Fit of old mountain belts in Africa and South
America
29
Distribution of glacial deposits
Match of Glacial/Stratigraphic data known by 1937
30
Fossil data by 1937 (almost)
Glossopteris leaves
Mesosaurus
31
Wegeners continental drift
Important
Wegeners reconstruction of Pangea (Greek all
land) Laurentia (northern landmass). Gondwana
(southern landmass). Only moderately different
from Sniders 1858 maps.
Laurentia
Gondwana
32
Important
Wegeners continental drift
  • Shapes of continents dont change with time.
  • Continents move through ocean basins.
  • Continental drift young (Pleistocene) to explain
    young orogeny.
  • NS movement due to gravitational attraction of
    equatorial bulge.
  • E-W motion due to tidal forces of sun and moon.
  • Front edges continents crumpled, forming orogenic
    belts.
  • Oceanic islands parts of continents left behind.

33
Wegeners continental drift
  • Above idea not generally accepted because
  • No accepted mechanism for moving continents
    through oceans.
  • Arguments about timing of orogenies, thus
    continental movements.
  • He was a meteorologist working in southern
    hemisphere.

34
What is the Solution?
  • Our Next Topics
  • Sea Floor Spreading
  • Plate Tectonics
Write a Comment
User Comments (0)
About PowerShow.com