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Plate Boundaries
Plate Boundaries

... c. forms deep trenches and islands ...
Key to Investigation 2: Plate Tectonics
Key to Investigation 2: Plate Tectonics

... 1b. It is the moving of plates rubbing against each other that cause earthquakes. Subduction zones are primarily the cause of volcanoes. Converging or colliding plates push up mountains. If plates are not locally interacting with each other, there is little geologic activity, such as in Central Aust ...
What type of boundary is…
What type of boundary is…

Geochemical cycle of volatiles during plate
Geochemical cycle of volatiles during plate

... stability field expands to lower pressures by up to 1 GPa. When these results are combined with phase relations in the Mg2SiO4–Fe2SiO4 system, the significant effects on the pressure and pressure interval of this phase transformation are only expected in colder mantle regions (< 1400 °C) and for H2O ...
Type of Boundary, type of crust
Type of Boundary, type of crust

... earthquakes and eruptions of basaltic lava, earthquake focus depth increases as you move away from the trench over the subducting plate. ...
LITHOSPHERIC BUOYANCY - Lunar and Planetary Institute
LITHOSPHERIC BUOYANCY - Lunar and Planetary Institute

... While a variety of interpretations of the Venusian cratering record have been proposed [1,2,3,4,5], the simplest interpretation is a relatively rapid, global resurfacing about 300-500 Myr ago. Mechanisms that could cause catastrophic and perhaps episodic global scale mantle overturn with consequent ...
Section 11-3
Section 11-3

The Layers of the EarthPowerPoint Fill-in-the
The Layers of the EarthPowerPoint Fill-in-the

... The crust is composed of two rocks. The continental crust is mostly _______________. The oceanic crust is ________________. Basalt is much ___________________ than the granite. Because of this the ___________________ dense continents ride on the denser oceanic plates. The ___________________ is the ...
The Layer`s Of The Earth! - Mrs. V. Murphy`s Science Class
The Layer`s Of The Earth! - Mrs. V. Murphy`s Science Class

... Transform Boundaries Where plates slide past each other ...
Class 9 - Earth and Atmospheric Sciences
Class 9 - Earth and Atmospheric Sciences

... Tectonic Plates and Their Boundaries — The lithosphere is divided into about a dozen major tectonic plates defined by boundaries of three types: spreading ridges, subduction zones, and transform faults, as shown in accompanying diagrams. The Earth’s Internal (Endogenic) Heat Engine What’s A Heat Eng ...
Chapter 7, Section 1 Directed Reading A
Chapter 7, Section 1 Directed Reading A

... while the densest compounds make up the core? _______________________________________________________________ _______________________________________________________________ 4. List the three layers of the Earth, based on their chemical composition. A. B. C. 5. Complete Sentence - What three element ...
oceanic ridges
oceanic ridges

... Collison zones form where both sides of a convergent boundary consist of continental (buoyant) material. Modern example: Himalayas ...
ch7 answers to SG
ch7 answers to SG

... 23. When continental plates collide with oceanic plates, what happens? Subduction – the oceanic plate subducts under the continental plate. 24. What type of fault occurs on a transform boundary? Strike-slip Fault 25. The core of the earth is divided into a liquid outer core and a solid inner core, b ...
Chapter 9 Plate Tectonics
Chapter 9 Plate Tectonics

...  Convection currents within Earth drive plate motion  Hot material deep in the mantle moves upward by convection  At the same time, cooler, denser slabs of oceanic lithosphere sink into the mantle ...
The Earths Crust Quick Key
The Earths Crust Quick Key

Earth`s+Interior+Structure
Earth`s+Interior+Structure

... As rocks in the interior of the Earth are heated enough, their density decreases. The less dense rock rises slowly over time. The most likely source of the Earth’s internal heat is the decay of radioactive elements in the core. ...
ANSWER KEY Name - Riverdale Middle School
ANSWER KEY Name - Riverdale Middle School

... a.) Name the feature shown at A. Mid-Ocean Ridge b.) What is occurring at B? Sea-floor spreading c.) What process is shown occurring at C, and why does it occur? Subduction, because the ocean floor is so much heavier (denser) than the land ...
Constraints on the evolution of oceanic lithosphere from surface
Constraints on the evolution of oceanic lithosphere from surface

... Geological Museum Room 310, 24 Oxford Street ...
Chapter 8 Volcanoes Section 1, Why Volcanoes Form
Chapter 8 Volcanoes Section 1, Why Volcanoes Form

... Earth’s mantle, the rock is subjected to greater heat and pressure. • As a result, the plate releases fluids, which causes surrounding rock to melt. • Magma then moves upward through cracks in the Earth to form a volcano. ...
Plate Tectonics and Mountain Building – Study Guide Plate
Plate Tectonics and Mountain Building – Study Guide Plate

... 8. A divergent boundary at two oceanic plates can result in a ____. 9. What type of boundary occurs where two plates move together, causing one plate to descend into the mantle beneath the other plate? 10. The San Andreas fault is a geographic example of what type of fault boundary? 11. New ocean cr ...
PLATE TECTONICS
PLATE TECTONICS

... indicates continents split apart Recent Evidence for Continental Drift • Fitting continents at continental slope rather than shoreline • Refined matches of rocks between continents • Isotopic ages support matches • Glacial evidence • Matches between Africa and South America are particularly convinci ...
The Changing Earth
The Changing Earth

...  Divergent boundaries on continents produce rift valleys.  Magma rises through cracks and forms volcanoes. ...
Changing Earth`s Surface
Changing Earth`s Surface

Instructor`s Notes: Chapter 17 Earth`s Interior Earth`s Interior Indirect
Instructor`s Notes: Chapter 17 Earth`s Interior Earth`s Interior Indirect

... Density calculation of the earth indicate that the core is 11 g/cm3; 14 times denser than water (crustal rock is 2.8 X denser than water) Meteorites (metallic) high percentage of iron and nickel in solar system (crust and mantle have relatively small amount of iron)- iron and nickel have same seismi ...
Name: Pd: Plate Tectonics Unit Test Study Guide S6E5a. Compare
Name: Pd: Plate Tectonics Unit Test Study Guide S6E5a. Compare

... 11. Most geologists rejected Alfred Wegener’s idea of continental drift because he could not explain HOW they moved or the force that caused them to move 12. What causes the movement of tectonic plates? Convection currents below the lithosphere 13. What is Pangaea? The name of the super continent wh ...
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Mantle plume



A mantle plume is a mechanism proposed in 1971 to explain volcanic regions of the earth that were not thought to be explicable by the then-new theory of plate tectonics. Some such volcanic regions lie far from tectonic plate boundaries, for example, Hawaii. Others represent unusually large-volume volcanism, whether on plate boundaries, e.g. Iceland, or basalt floods such as the Deccan or Siberian traps.A mantle plume is posited to exist where hot rock nucleates at the core-mantle boundary and rises through the Earth's mantle becoming a diapir in the Earth's crust. The currently active volcanic centers are known as ""hot spots"". In particular, the concept that mantle plumes are fixed relative to one another, and anchored at the core-mantle boundary, was thought to provide a natural explanation for the time-progressive chains of older volcanoes seen extending out from some such hot spots, such as the Hawaiian–Emperor seamount chain.The hypothesis of mantle plumes from depth is not universally accepted as explaining all such volcanism. It has required progressive hypothesis-elaboration leading to variant propositions such as mini-plumes and pulsing plumes. Another hypothesis for unusual volcanic regions is the ""Plate model"". This proposes shallower, passive leakage of magma from the mantle onto the Earth's surface where extension of the lithosphere permits it, attributing most volcanism to plate tectonic processes, with volcanoes far from plate boundaries resulting from intraplate extension.
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