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Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more cases of similar organisms separated by oceans 1912 Proposed single supercontinent Pangaea

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Page 1: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Continental Drift Theory

• Alfred Wegener• German meteorologist

• Found papers describing similar fossils on opposite sides of the Atlantic

• Researched more cases of similar organisms separated by oceans

• 1912 Proposed single supercontinent Pangaea

Page 2: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Continental Drift Theory5 Types of Evidence

• Fit of the Continents• Distribution of Fossils• Sequence of Rocks• Glacier Scraping Patterns• Ancient Climates and

Wandering Polar Regions

http://library.thinkquest.org/3669/media/map2dd.GIF

Page 3: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Wegener’s Continental Drift Evidence:

• Continents ‘fit’ together in a single land mass 250 mya

• CLICK Simulations

http://www.ucmp.berkeley.edu/geology/anim1.html

http://www.eoearth.org/upload/thumb/f/fb/Plate_tectonics_over_time.gif/400px-Plate_tectonics_over_time.gif

Page 4: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Wegener’s Continental Drift Evidence: Plant and animal fossils of the same species were found on

several different continents.

Page 5: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Wegener’s Continental Drift Evidence: Similar sequence of rock or

rock formations have the same age

Page 6: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Wegener’s Continental Drift Evidence: Glacial deposits, striations,

and scraping patterns

Page 7: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Wegener’s Continental Drift Evidence: Climate distribution

Past Present

Coal exists under the ice in the rock of Antarctica – yet coal can only form from plants that grow in warm climates.

Page 8: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Wegener’s Theory Problems

1) Wegener had no convincing mechanism (did not explain the forces) of how the continents might move. Continents plowing through the crust would destroy the crust.

2) Continents are not moving apart at the speed Wegener proposed.

Wegener = 250cm/yr

Actual = 2 cm/yr

Page 9: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Holmes Breakthrough: Heat trapped in the Earth caused

convection currents in the mantle.

• As a substance is heated its density decreases and rises to the surface until it is cooled and sinks again.

Page 10: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Convection Currents

• Gravity causes the heated mantle to sink

• The mantle heats up near the core and then rises again

• Conduction is the transfer of heat between 2 materials in direct contact with each other

library.thinkquest.org/C003124/images/convect.jpg

http://www.wisc-online.com/objects/index_tj.asp?objID=SCE304Click animation

Page 11: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Volcanic rocks on the seafloor have magnetization because, as they cool,

magnetic minerals within the rock align to the Earth’s magnetic field.

New Evidence: Magnetic pattern of rock

Page 12: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

North Magnetic Pole in No. Hemi

Page 13: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

North Magnetic Pole in So. Hemi

Page 14: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Present DayNorth Magnetic Pole in No. Hemi

Page 15: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Sea-Floor Spreading Hypothesis by Hess & Deitz

CLICK Animation: http://www.uwsp.edu/geo/faculty/ritter/glossary/s_u/sea_flr_spread.html

Page 16: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Plate Tectonics Theory

Plates ‘float’ on the AsthenospherePlates have oceanic and continental crust

www.wiley.com/college/herenow/ptect/pt-map1.gif

Page 17: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Earth’s Layers

• Inner Core• Outer Core• Mantle• Crust• Atmosphere

• Lithosphere – crust and upper mantle, plates move independently

• Asthenosphere-region below the Lithosphere

http://library.thinkquest.org/04oct/01724/images/Earth-crust-cutaway-english.png

Page 18: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Continental Crust

• Cooling rate - slow• Crystal size - large• Density – less dense• Thickest portion of the Earth’s outer layer• Composition – made mainly of granite rock

http://www.amonline.net.au/geoscience/images/earth_diagrams/cont_oceanic_crust.gif

Page 19: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Oceanic Crust

• Cooling rate - fast• Crystal size - small• Density – more dense• Thinnest portion of the Earth’s outer layer• Composition – Made mainly of basalt rock

http://faculty.weber.edu/bdattilo/parks/plume_ocean.jpg

Page 20: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Volcano - opening or rupture in the Earth’s crust that allows molten rock to escape

http://cgz.e2bn.net/e2bn/leas/c99/schools/cgz/accounts/staff/rchambers/GeoBytes%20GCSE%20Blog%20Resources/Images/Plate%20Tectonics/Plate%20Tectonics/VolcanoStructure.jpg

Page 21: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Earthquake - result of sudden energy release in the Earth’s crust creating seismic waves.

• http://news.bbc.co.uk/nol/shared/spl/hi/world/04/earthquake/img/earthquake.gif

Page 22: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

More Evidence: Location of mountain ridges, rift valleys, mid-ocean ridges, and

trenches on plate boundaries. Convergent, Divergent and Transform

http://www.ifa.hawaii.edu/~barnes/ast110_06/tprai/Tectonic_plate_boundaries.png

SIMULATIONS ON ALL BOUNDARY TYPESCLICK http://www.pbs.org/wgbh/aso/tryit/tectonics/shockwave.html

Page 23: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Andes MountainsConvergent Oceanic & Continental

Plates move toward each other

blue.utb.edu/paullgj/images/Conv_Cont_Ocean.JPG

CLICK http://www.pbs.org/wgbh/aso/tryit/tectonics/convergent.html

A trench, a steep walled valley on the sea floor, forms here.

Denser oceanic crust subducts under less dense continental crust

Page 24: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Convergent BoundaryOceanic & Continental

CLICK http://geology.com/nsta/convergent-boundary-oceanic-continental.gif

Page 25: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Japan or Aleutian IslandsConvergent Oceanic & Oceanic

ceeps.colostate-pueblo.edu/.../smM1P1Fig15.gif

Denser oceanic crust subducts under less dense oceanic crust

Page 26: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Convergent BoundaryOceanic & Oceanic

http://geology.com/nsta/convergent-boundary-oceanic-oceanic.gif

Page 27: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

HimalayasConvergent Continental & Continental:

http://www.pbs.org/wgbh/aso/tryit/tectonics/crush.html

Faulting and Folding

Page 28: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Convergent BoundaryContinental & Continental

http://geology.com/nsta/convergent-boundary.gif

Page 29: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Mid Atlantic RidgeDivergent Oceanic

At a divergent boundary lithosphere plates move away from each other

Page 30: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Divergent BoundaryOceanic

• Mid-Ocean Ridges – a structure formed from seafloor spreading.

CLICK http://geology.com/nsta/divergent-boundary-oceanic.gif

Page 31: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

East African Rift ValleyDivergent Continental

Rift Valley – Pulling apart of crust due to tensional forces

ceeps.colostate-pueblo.edu/.../smM1P1Fig15.gif

Page 32: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Divergent BoundaryContinental

• Rift Valley

http://geology.com/nsta/divergent-boundary-continental.gif

Page 33: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

San Andreas FaultTransform Plate Boundary

Plates slide past each other

www.wiley.com/college/herenow/ptect/pt-map1.gif

Page 34: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Transform Boundary

TRANSFORM SIMUALTIONSCLICK http://geology.com/nsta/transform-boundary.gifCLICK http://www.pbs.org/wgbh/aso/tryit/tectonics/transform.htm

Page 35: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

http://vulcan.wr.usgs.gov/Imgs/Gif/PlateTectonics/Maps/map_plate_tectonics_world.gif

Evidence - Location of earthquakes and volcanoes

Page 36: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Hot Spots

Page 37: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

The Hawaiian-Emperor volcanic chain is the result of the drifting of the

Pacific Plate over a fixed hot spot.

http://geology.com/nsta/plate-tectonics-cover.gif

Page 38: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

The bend in the (Hawaiian – Emperor) volcanic chain is the result of a major change in the direction of the movement of the Pacific Plate.

Page 39: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Location of Hot Spots

Hot spots result from hot, narrow plumes of material that rise deep within the mantle.

Page 40: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Plate Movement in the future• http://www.scotese.com/earth.htm

It is even possible to measure the speed of continentalplates extremely accurately, using satellite technology.

Page 41: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

External Energy For Earth

• Sun & Moon keeps air and sea in motion, shapes surface

• Sun warms atmosphere & crust unevenly creating winds

• Winds drive ocean currents and water cycle• Erosion from winds, rains, rivers, glaciers, and

waves shape surface• Weathering from winds and rains• Sun & Moon Gravitational Energy, produces tides• Planetesimal collisions

Page 42: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Internal Energy for Earth

• Radioactive element decay

• Core heat from layers pressure

• Convection currents

• Volcanoes

• Hot Springs

• Earthquakes

Page 43: Continental Drift Theory Alfred Wegener German meteorologist Found papers describing similar fossils on opposite sides of the Atlantic Researched more

Evidence for Plate Tectonics

• Continents fit together• Fossil distribution• Common rock formations: same age• Glacier evidence: deposits, striations, scraping• Climate distribution

New evidence • Magnetic pattern of rock• Location of earthquakes and volcanoes • Location of mountain ridges, rift valleys,

mid-ocean ridges, and trenches

First evidence used for Continental Drift Theory