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Description Crust Mantle Liquid Outer Core Solid
Description Crust Mantle Liquid Outer Core Solid

... Moho discontinuity (40km)- separates low density silicates (rich in Al+K) from high density silicates (rich in Mg+Fe) ...
Plate Tectonics: Types of Plate Margins
Plate Tectonics: Types of Plate Margins

Lecture 6 Review Sheet
Lecture 6 Review Sheet

... boundary, mid-ocean ridge, continental rift, rift valley, rift volcano, rift range or rift mountain, island arc, subduction, magma, volcano, collision zone, orogenic belt, volcanic arc, accretionary wedge, forearc basin, terrigenous/terrestrial sediment, subduction trench, magmatic arc, mountain cha ...
Convection in the mantle is commonly related to plate tectonic
Convection in the mantle is commonly related to plate tectonic

The layers of the Crust
The layers of the Crust

... The outermost layer of the Earth, the Crust, can be divided by its physical properties into the Lithosphere and Asthenosphere. The Lithosphere (stone sphere) is the rigid outer-most layer of the Earth. The Lithosphere is the relatively cool, rigid shell of the Earth that consists of the Crust and th ...
Ch 9 4 Testing Plate Tectonics
Ch 9 4 Testing Plate Tectonics

... earthquakes along the oceanic ridge system was shown to be consistent with the new theory  Scientists have found that intermediate and deep focus earthquakes occur within the subducting plate as it goes into the mantle  Shallow-focus earthquakes are produced as the descending slab reacts with the ...
26 Sep: Volcano Processes
26 Sep: Volcano Processes

...  May someday be possible to predict EQs; need improved understanding of physics & MUCH better measurements Today: • Volcanism ...
Chapter 5-Study Questions
Chapter 5-Study Questions

... made of several large segments that are slowly moving. ___12. Earth’s rigid outer shell, called the crust, lies over a hotter, weaker zone known as the athenosphere. ___13. Sea floor spreading is the mechanism responsible for producing ocean-floor material at the crest of oceanic ridges. ___14. The ...
Formative Assessment - Western Reserve Public Media
Formative Assessment - Western Reserve Public Media

... is the mantle. It is composed of rock that flows very slowly. The outermost layer is the crust. There is oceanic crust and continental crust. The crust and the upper part of the mantle (which is cooler and more rigid than the lower part) together make up the lithosphere. The lithosphere is broken in ...
Theory of Plate Tectonics
Theory of Plate Tectonics

... The Plate Tectonic Theory states that Earth’s surface is broken into large plates that move apart and then rejoin, sliding over the semi-fluid rock below. There are about 12 major tectonic plates and many smaller ones. Mantle convection is thermal energy transfer in the mantle where hot, light magma ...
CH 9 Plate tectonics
CH 9 Plate tectonics

... * Subduction occurs and one plate dives down * Ocean trench forms * Volcanic island arcs * Ex: Japan, Aleutians ...
Chapter 7 Vocabulary List
Chapter 7 Vocabulary List

Plate Tectonics Review Worksheet
Plate Tectonics Review Worksheet

... Plate Tectonics Review Worksheet 1. Continental Drift: A theory proposed by Alfred Wegner that said all continents were once joined 300 million years ago in a single land mass called Pangaea. Over time the continents moved to their present day locations. 2. What are four pieces of evidence for conti ...
Eighth Grade ScienceEarth`s HistoryStudy Guide
Eighth Grade ScienceEarth`s HistoryStudy Guide

... 6. What is subduction? When one plate goes under another plate and it is melted back into the mantle. 7. The Earth’s plates are made of what layer(s)? inner core, outer core, mantle (asthenosphere—upper mantle), crust (lithosphere) 8. Explain convection currents. Fluids when heated become less dense ...
– Circle the response that best answers the question.
– Circle the response that best answers the question.

... 23 Sequencing - Place these terms in correct order so they begin at Earth’s surface and move toward the center: inner core, asthenosphere, lower mantle, lithosphere, outer core. ...
Long term geomagnetic variations and whole
Long term geomagnetic variations and whole

... The geomagnetic field is generated by the convection of molten metal in the Earth’s outer core that is itself controlled by heat flowing across the core-mantle boundary. It has long been suspected that palaeomagneticallyobserved variations in geomagnetic behaviour occurring over tens to hundreds of ...
Spreading Ridge Axis, Divergent Plate Boundary Subduction Zone
Spreading Ridge Axis, Divergent Plate Boundary Subduction Zone

Digestive System Study Guide
Digestive System Study Guide

... called the A________. ...
Lessons 4 and 5 Vocabulary
Lessons 4 and 5 Vocabulary

... Lesson 5 Continued Lithosphere – the cool, solid outer shell of the earth. It consists of the crust and the rigid uppermost part of the mantle and is broken up into segments, or plates. Mantle – the layer of the earth beneath the crust. It is about 2900 km thick, and it makes up about 83 percent of ...
Document
Document

... AKA Slabpull ...
Ch. 8 Vocab Study Guide
Ch. 8 Vocab Study Guide

... 2. The ________________________ is located directly under the lithosphere. This is a layer of hotter and softer rock in the mantle. 3. The switch in the Earth’s magnetic field is called: _______________________________________ 4. A solid sphere of metal at the Earth’s center: _______________________ ...
Study Guide Chapter 3 – Plate Tectonics GPS: S6E5. Students will
Study Guide Chapter 3 – Plate Tectonics GPS: S6E5. Students will

... 8. The transfer of energy through space is called ________________________. 9. Heat transfer within a material or between materials that are touching is called _____________________. 10. _________________ is heat transfer by movement of currents with a fluid – which can be a liquid or a gas. 11. In ...
CH 9 Plate tectonics
CH 9 Plate tectonics

... • Thinner and more sweet • Holds up better to washings • Able to leap tall buildings in a single bound. • Makes Jessica Alba look like a ho. ...
Plate tectonics vocab
Plate tectonics vocab

... 1.Crust- the thin and solid outermost layer of the Earth above the mantle. 2.Mantle- the layer of rock between the Earth’s crust and core. 3.Core- the central part of the Earth below the mantle. 4.Lithosphere- the solid, outer layer of the Earth that consists of the crust and the rigid upper part of ...
The Structure of Earth - Mrs. wolfe`s 6th grade​ science classroom
The Structure of Earth - Mrs. wolfe`s 6th grade​ science classroom

... earthquake was caused by the movement of tectonic plates at the San Andreas Fault. ...
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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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