Plate Tectonics
1 / 31

Plate Tectonics and the Ocean Floor - PowerPoint PPT Presentation

  • Uploaded on

Plate Tectonics and the Ocean Floor. Continental Drift. Theory proposed by Alfred Wegener in 1912 Continents once formed a single landmass. Early Evidence. Age of Oceanic Crust. Courtesy of Paleomagnetism. Plate Tectonics – 1960’s. Explains HOW the plates moved.

I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
Download Presentation

PowerPoint Slideshow about ' Plate Tectonics and the Ocean Floor' - barton

An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.

- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript

Plate Tectonics


the Ocean Floor

Continental drift
Continental Drift

  • Theory proposed by Alfred Wegener in 1912

  • Continents once formed a single landmass

Age of Oceanic Crust

Courtesy of

Plate tectonics 1960 s
Plate Tectonics – 1960’s

  • Explains HOW the plates moved

The crust
The Crust

  • Continental Crust

  • thick (10-70km)- buoyant (less dense than oceanic crust) - mostly old

Oceanic Crust

- thin (~7 km)- dense (sinks under continental crust)- young

Plate movement
Plate Movement

  • “Plates” of lithosphere are moved around by the underlying hot mantle convection cells

Three types of plate boundary

  • Divergent

  • Convergent

  • Transform

Divergent Boundaries

  • Spreading ridges

    • As plates move apart new material is erupted to fill the gap

Mid ocean ridge
Mid-Ocean Ridge

  • Underwater mountain ranges

  • Due to plates pulling away from each other

  • A Rift Valley forms in the middle where magma comes out

  • Have many fracture zones which break the ridge up

Iceland: Atlantic.An example of continental rifting

  • Iceland has a divergent plate boundary running through its middle

Convergent Boundaries Atlantic.

  • There are three styles of convergent plate boundaries

    • Continent-continent collision

    • Continent-oceanic crust collision

    • Ocean-ocean collision

Continent-Continent Collision Atlantic.

  • Forms mountains,e.g. European Alps, Himalayas

Himalayas Atlantic.

Continent-Oceanic Crust Collision Atlantic.



Subduction Atlantic.

  • Oceanic lithosphere subducts underneath the continental lithosphere

  • Oceanic lithosphere heats and dehydrates as it subsides

  • The melt rises forming volcanism

  • E.g. The Andes

Trenches Atlantic.

  • Due to one plate subducting (going below) another plate

  • Earthquakes

  • Many volcanoes and volcanic island arcs form here

Ocean-Ocean Plate Collision Atlantic.

  • When two oceanic plates collide, one runs over the other which causes it to sink into the mantle forming a subduction zone.

  • The subducting plate is bent downward to form a very deep depression in the ocean floor called a trench.

  • The worlds deepest parts of the ocean are found along trenches.

    • E.g. The Mariana Trench is 11 km deep!

Transform Boundaries Atlantic.

  • Where plates slide past each other

Above: View of the San Andreas transform fault

Pacific Ring of Fire Atlantic.

Volcanism is mostly focused at plate margins

Continental shelf
Continental Shelf Atlantic.

  • Part of a continent covered by water

  • Gentle slope

  • Average depth is 60 m

  • Amount exposed changes with sea level

Continental slope
Continental Slope Atlantic.

  • Steep

  • May be cut by submarine canyons

  • Sediment piles up at the bottom and forms continental rise

Abyssal plains
Abyssal Plains Atlantic.

  • Flattest area on earth

  • Cover ½ of deep ocean

  • Covered with fine sediment

Seamounts Atlantic.

  • Submerged volcanic mountains

  • Called oceanic island if they rise above water

Guyot Atlantic.

  • Seamounts that have been eroded and are now flat on top