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Tectonic Plates

Learn about the tectonic plates!

TermDefinition
Divergent Plates move apart to create new crust
Divergent Boundary Features Ridges, rift valleys, and ocean basins form here
Convergent Plates move toward each other, destroying or uplifting crust
Convergent Boundary Features Mountains, trenches, volcanoes, and earthquakes
Transform Plates slide past each other causing faults and earthquakes
Where are ridges formed? Formed at divergent boundaries where magma rises
What are ridges? Common at oceanic-oceanic boundaries
earthquakes Occur at all boundary types due to plate movement
ocean basins Form at divergent oceanic-oceanic boundaries
rift valleys Form on land when continental crust splits apart
volcanoes Form at convergent or divergent boundaries when magma reaches surface
mountains Form at convergent continental-continental boundaries
trenches Deep ocean depressions where subduction occurs
faults Cracks in the crust where plates slide past each other
seafloor spreading Process that forms new oceanic crust at ridges
Plate Boundaries Summary Divergent = divide, Convergent = collide, Transform = slide
Subduction Process where denser oceanic crust sinks beneath lighter crust
Collision When two continental plates push up mountains
Rifting When crust thins and pulls apart creating valleys
Pacific Plate Large oceanic plate under the Pacific Ocean
North American Plate Includes North America and part of the Atlantic seafloor
South American Plate Includes South America and Atlantic seafloor
Eurasian Plate Covers Europe and most of Asia
African Plate Covers Africa and surrounding ocean floor
Indo-Australian Plate Covers Australia and Indian Ocean region
Antarctic Plate Covers Antarctica and surrounding seafloor
Nazca Plate Oceanic plate off west coast of South America
Cocos Plate Oceanic plate off coast of Central America
Philippine Plate Oceanic plate near the Philippines
Caribbean Plate Plate beneath the Caribbean region
Arabian Plate Plate beneath the Middle East region
Yellowstone Supervolcano and hotspot under North America
Hawaii Hotspot forming volcanic island chain in Pacific Ocean
Iceland Hotspot and divergent ridge above the Mid-Atlantic Ridge
Galapagos Islands Hotspot near Ecuador forming volcanic islands
Toba Supervolcano in Indonesia that erupted ~74,000 years ago
Taupo Supervolcano in New Zealand
Hotspot Rising plume of hot mantle forming volcanoes away from boundaries
Continental Drift Theory Continents once formed Pangaea and drifted apart
Plate Tectonics Theory Lithospheric plates move on the semi-fluid asthenosphere
Seafloor Spreading Theory New crust forms at mid-ocean ridges and moves outward
Subduction Theory Old crust sinks beneath lighter continental crust
Law of Superposition Oldest rock layers at bottom, youngest on top
Uniformitarianism Earth’s processes today are the same as in the past
Isostasy Crust floats in balance on denser mantle
Paleomagnetism Magnetic patterns in rocks prove seafloor spreading
Theory of Continental Drift Wegener’s idea that continents were once joined as Pangaea
Evidence for Continental Drift Fossils, continental fit, glaciers, and rock formations across oceans
Fossil Evidence Similar fossils found on now-separated continents
Continental Fit Continents like South America and Africa fit together
Glacial Evidence Glacial marks found in tropical regions show past movement
Landform and Rock Evidence Matching mountain ranges and rocks across oceans
Alfred Wegener Proposed the Continental Drift Theory
Harry Hess Discovered seafloor spreading supporting Wegener’s idea
Harry Hess Discovery Mountains, valleys, and volcanoes on the ocean floor
Plate Movement Cause Mantle convection currents move tectonic plates
Divergent Boundary Examples Mid-Atlantic Ridge, East African Rift Valley
Convergent Ocean-Ocean Forms trenches and volcanic island arcs (Mariana Trench)
Convergent Ocean-Continent Forms trenches and volcanic mountains (Andes)
Convergent Continent-Continent Forms folded mountains (Himalayas)
Transform Boundary Example San Andreas Fault where plates slide past
Oceanic Crust Dense crust that subducts under continental crust
Sea-floor Spreading New crust forms at ridges as magma rises and cools
Earth’s Surface Stability Crust destroyed at subduction zones balances new crust creation
Conduction Heat transfer by direct contact
Radiation Heat transfer through electromagnetic waves
Convection Heat transfer by movement of fluids
Convection in the Mantle Hot mantle rises, cool mantle sinks—drives plate motion
Convection Example - Macaroni Macaroni rises and falls in boiling water due to convection
Conduction Example - Spoon Metal spoon heats up in hot liquid
Radiation Example - Sun Sunlight warms your skin without contact
Hot Air Balloon Rises because hot air is less dense
Warm Air Moves upward and collects near ceilings
Lava Lamp Example Wax rises when heated and sinks when cooled
Sidewalk Heating Sunlight warms concrete through radiation
Sidewalk Burns Feet Heat transfers to skin by conduction
Hot Fluid Less dense and rises upward
Cold Fluid More dense and sinks downward
Thermal Equilibrium Heat moves from hot to cold until temperatures are equal
Created by: JudeBellingham
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