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Plate Tectonics
A Brief History of a Unifying Theory
Accumulation of Observations -
Evidence· Patterns of continents
· Paleontology· Geology
· Patterns of sea floor ages· Patterns of seafloor depth· Patterns of seafloor sediments · Patterns of magnetism· Patterns of volcanoes· Patterns of earthquakes
Plate Tectonics as the Unifying Concept of Earth Science
http://pubs.usgs.gov/gip/dynamic/historical.html
Earth’s Great Puzzle Pieces
• 1620 – Sir Francis Bacon observed similarities of coasts of Africa and South America … “no mere accidental occurrence.” A few years later it was suggested that they were once one, but had been separated by the Flood.
• 1782 – Benjamin Franklin, based on observed oyster shells on mountain tops “The crust of the Earth must be a shell floating on a fluid interior.... Thus the surface of the globe would be capable of being broken and distorted by the violent movements of the fluids on which it rested.”
• 1799 – Alexander Von Humbolt, German explorer and naturalist, observed the similarities in the geology and features of the west coast of Africa and east coast of South America (separated by a valley filled by the flood)
1858 - Geographer Antonio Snider-Pellegrini made these two maps showing his version of how
the American and African continents may once have fit together, then later separated
A Man and His Model
• Current: Contracting Earth• 1912: Continental Drift• Observations
• Fit of Continents• Geology• Paleontology• Climate belts
• Pangea (“all lands”) 300 -200 Ma• Breakup 180 Ma
• Rigid bodies moving through yielding seafloorAlfred Wegener
Eduard Seuss
The same land plant and animal fossils are found on separate continents!
• 1926• Based on
glossopteris fern
Fossils Match!
Geology Matches, Too!
Scientific Community says:
Scientific Community says:
No mechanism to make continental drift happen
Mechanism for Plate Movement!• Arthur Holmes (Late 1920’s)
• Interior of Earth has sluggish convection (transport of heat from core); hot stuff rises, cool stuff sinks
• New ocean crust injected into ocean floor
But from where?
Maurice Ewing
• Mapping the seafloor 1947-1959
• Lockney Texas
• Rice University Trained
• UTMB - Division of Earth and Planetary Sciences of the Marine Biomedical Institute
Maurice Ewing
• Mapping the seafloor 1947-1959• Surprises:
• Thin sediment• Basalt crust – glasses• Age less than 150 Ma
(hadn’t identified a pattern yet)
• Ridges – later shown to circle globe
• Valley within ridge (Tharp)• Earthquakes along ridges• High heat flow (Bullard)
Harry Hess and Seafloor Spreading
• 1962 – startling new theory “History of the Oceans”
• New ocean crust at mid-ocean ridges
• Ocean crust dragged down at trenches; mountains form here
• Continental crust too light; remains at surface
• Earthquakes occur where crust descends
“It explains everything….”
Rocks and Magnetism - Tools• When magma cools, takes on signature
of Earth’s prevailing magnetic field
• Three magnetic measurements can be taken from rocks
• Inclination - ~ latitude ~distance to the pole
• Declination - ~ direction to the pole
• Positive (normal) or negative (reversed) - depending on what Earth’s field is doing
• Add age = powerful tool
• Earth’s present magnetic field is called normal• magnetic north near the north geographic pole • magnetic south near the south geographic pole
• At various times in the past, Earth’s magnetic field has completely reversed• magnetic south near the north geographic pole • magnetic north near the south geographic pole
• 171 times in last 76 million years … takes 5,000 to 10,000 per reversal. Lasts 10’s of thousands to millions of years
Magnetic Reversals
Symmetric patterns of magnetism on either side of mid-ocean ridge
Vine and Matthews The Final Push – 1962-1963
Seafloor as a magnetic tape recorder
Magnetic Stripes on Seafloor
When magma cools, it takes on signature of Earth’s prevailing magnetic field
magnetic iron-bearing minerals align with Earth’s magnetic field
Oceanic Crust Is Young
Age of Continents
Original copyrighted image removed; there is an image available at http://
www.lithosphere.info/TC1-2006/TC1_Fig2-ages-062006.jpg
that may be copyrighted.
Tuzo Wilson
• Transform faults: opposite sense of movement than expected.
• Proven correct (Sykes)• Sealed theory of sea-floor spreading and plate tectonics
for most scientists • 1960s-1970s
Hydrothermal Vents
• The result of seawater percolating down through fissures in the ocean crust in the vicinity of spreading centers or subduction zones
• The cold seawater is heated by hot magma and reemerges to form the vents. Seawater in hydrothermal vents may reach temperatures of over 340°C (700°F)
• Discovered in 1977 while exploring an oceanic spreading ridge near the Galapagos Islands
Theory of Plate Tectonics• The upper mechanical layer of Earth (lithosphere) is divided into rigid
plates that move away from, toward, and along each other
• Most deformation of Earth’s crust occurs at plate boundaries
How can you calculate the rate of plate movement?
Calculating Plate Movement
• Pick an object and watch it … • Better on glaciers than on slow moving
plates …
• Use magnetic reversals … long time periods
• Date rocks across a mid-ocean ridge really really carefully … tedious
Northern Pacific Basin
Hawaii
HawaiianRidgeMidway
EmperorSeamount
Chain
Hot Spots
• Stationary magma chambers under mobile plates …
Prominent Hot Spots
Plate Movement Rates using Hot Spots
http://www.classzone.com/books/earth_science/terc/content/investigations/es0810/es0810page01.cfm?chapter_no=investigation
Tectonics on Other Planets?
Do you recognize either of these locations?
Mars Topography
Mars Magnetic Field