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Hot spots can be used to track plate movements.
Hot spots can be used to track plate movements.

... as the African Plate splits apart. This huge valley is thousands of kilometers long and as much as 1800 meters (5900 ft) deep. ...
Plate tectonics explains the movement of large
Plate tectonics explains the movement of large

... lithosphere = asthenosphere • The plates of the lithosphere float on the asthenosphere ...
PLATES OF THE EARTH`S CRUST
PLATES OF THE EARTH`S CRUST

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5) Types of Boundaries

... The melted rock rises up through the continental plate, causing more earthquakes and forming volcanic eruptions where it finally reaches the surface. An oceanic trench is a consistent feature. Most dangerous place to live ...
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What is a Volcano?

... Area where large numbers of earthquakes and volcanic eruptions occur in a 40,000km horseshoe shape. Contains 452 volcanoes, with over 75% of worlds active and dormant volcanoes. ...
File - Bruner science
File - Bruner science

...  Earthquakes often form from the ______________ between moving tectonic plates.  This accounts for _____ percent of all earthquakes.  The _________ _____ _________ convergent plate boundary west of Vancouver Island has many earthquakes. ...
PLATE TECTONICS - Cockeysville Middle
PLATE TECTONICS - Cockeysville Middle

... Activity 1: What Is Plate Tectonics? • The Earth’s surface is broken up into 15 lithospheric plates. • These plates are composed of the top part of the mantle and the crust. • There are oceanic plates (more dense) and continental plates (less dense). • These plates “float” on the asthenosphere, the ...
Plate Motion
Plate Motion

...  East Pacific ...
Earth`s Interior
Earth`s Interior

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Plate Tectonics
Plate Tectonics

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Plate Tectonics
Plate Tectonics

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OCEAN BASINS, GEOGRAPHY AND GEOLOGY OF THE OCEANS
OCEAN BASINS, GEOGRAPHY AND GEOLOGY OF THE OCEANS

... Continental crust or lithosphere – 100km thick Heat driven motion at the core creates convection currents and causes flowing and movement. HISTORY 200 million years ago – supercontinent Pangaea –Sea was Panthalassa – ancestor of Pacific –Tethy's sea separated Eurasia and Africa 180mya – Pangaea spli ...
Plate Tectonics - Coventry Local Schools
Plate Tectonics - Coventry Local Schools

... POSSIBLE CAUSES OF TECTONIC PLATE MOTION ______11. When rock is heated, it becomes less dense and tends to a. rise. b. sink. c. move sideways. d. erupt. ______12. When rock cools, it becomes more dense and tends to a. rise to the surface. b. sink below the surface. c. move sideways. d. push against ...
Chapter 3 Plate Tectonics Study Guide – Test Friday Oct 21
Chapter 3 Plate Tectonics Study Guide – Test Friday Oct 21

... A divergent boundary on land produces… ...
IGNEOUS ROCK FACTS Igneous rock is formed when melted rock
IGNEOUS ROCK FACTS Igneous rock is formed when melted rock

... surface of the earth. It cools slowly, so there is more time for mineral grains to form. The mineral grains mineral in intrusive igneous rock are medium in size. Extrusive igneous rock is formed when lava cools and solidifies on the surface of the earth. It cools quickly, so there is less time for m ...
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Plate Tectonics and the Rock Cycle
Plate Tectonics and the Rock Cycle

... related to the rifting apart of the continental lithosphere. The East Africa Rift is one such setting in which this is actively occurring today, and it may be considered to be a young divergent plate margin. Both these types of continental intra-plate volcanism produce predominantly basalts. This is ...
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ppt

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Chapter 5 Notes: Plate Tectonics  Earth’s Interior Direct
Chapter 5 Notes: Plate Tectonics Earth’s Interior Direct

... o Plates: a section of the lithosphere that slowly moves over the Asthenosphere carrying pieces of the continental and oceanic crust  Combined continental drift and sea floor spreading into a scientific theory o Scientific Theory: well tested concept that explains a wide range of observations  Ide ...
First Quarter Exam Review Sheet Name
First Quarter Exam Review Sheet Name

... What is the relationship between the age of rocks on the seafloor and their distance from the mid-ocean ridge? Where do most earthquake faults occur? Describe the pattern of magnetic polarity (the magnetic patterns in the crust rocks) on each side of a mid-ocean ridge. Where is the oldest oceanic cr ...
Physical Earth Science Semester 1 Mid
Physical Earth Science Semester 1 Mid

... 39. What is the color of the powdered form of a mineral called? streak 40. Differences in elevation are best shown using what kind of map? A topographic map 41. What is the current geologic period? Quaternary 42. Where is new ocean crust formed? At divergent boundaries 43. What happened to all the c ...
Slide 1 - My Teacher Pages
Slide 1 - My Teacher Pages

... ridge forming new oceanic crust • Tectonic plates spread apart and magma fills the gap. • As new crust forms older crust moves away from the M.O.R. ...
Chapter 3: Plate Tectonics
Chapter 3: Plate Tectonics

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Name - Middletown Public Schools
Name - Middletown Public Schools

... SECOND, read the worksheet “A MOVING JIGSAW PUZZLE” and complete three fill-in questions. THIRD, show the teacher the work you have completed. _______________________ FOURTH, begin the lab by following the PROCEDURE in “EDIBLE TECTONICS”. FIFTH, answer the questions under “QUESTIONS/CONCLUSIONS”. 1. ...
Convection currents
Convection currents

...  The Mantle is the largest layer of the Earth.  The middle mantle is composed of very hot dense rock that flows like asphalt.  The movement of the middle mantle (asthenosphere) is the reason that the crustal plates of the Earth move. ...
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Large igneous province



A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.
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