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... a. At the edge of a continent b. Half way between a ridge and a trench c. At a mid-ocean ridge d. At a deep sea trench 14. Which of the following is used as evidence of seafloor spreading? a. Fossil evidence b. Rock clues c. Climate clues d. Magnetic pole reversals 15. Which is a source of evidence ...
Document
Document

... Travel through the crust of the earth and attenuate (gradually disappear); Scientists have found that attenuation occurs more slowly in older rock (like the eastern US, but more quickly in younger rock ...
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SAI109 Dealing 4 Dynamic Response Earths Surface

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REVISED EXAM 3 STUDY GUIDE – PHYSICAL GEOGRAPHY
REVISED EXAM 3 STUDY GUIDE – PHYSICAL GEOGRAPHY

... Describe the four basic principles of Relative Dating in geology. Describe the Absolute Dating techniques in geology What is Geologic Time? What is the Geologic Time Scale? What are Eons? What are Periods? What are Epochs? When was the “Age of the Reptile? Age of Mammals? ...
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12.710: Introduction to Marine Geology and Geophysics Solutions to

... Xe’s volatility means that were accretion to occur after all of the 129I had decayed, all of the daughter 129Xe would have degassed and been lost from the Earth during accretion. Likewise, were accretion to happen before the 129I in the solar system decayed to extinction, the remaining 129I in the ...
Continental Drift and Sea-Floor Spreading 7.2
Continental Drift and Sea-Floor Spreading 7.2

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Curriculum Map Template

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Geology 101

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Plate Tectonics

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Regents Earth Science – Unit 11: The Dynamic Crust

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Astronomy 1: Midterm 2 Practice Exam

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WELCOME BACK! - Year 6 and 7 Mathematics, Science and

... The Mesosphere is where you can find falling stars and meteors. True Satellite signals are found within the exosphere. False Planes fly in this layer, called the stratosphere. True ...
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MOVEMENT OF EARTH’S CRUST

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...  Destruction of sea floor occurs in subduction zones  Seismicity is the frequency. Magnitude, and distribution of earthquakes  Earthquakes are concentrated along oceanic ridges, transform faults, trences and island arcs  Tectonism refers to the deformation of Earth’s crust  Benioff Zone is an a ...
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Tectonic Plates

... Basic Premise of Plate Tectonics • Earth’s crust is divided into plates • Plates move relative to one another (at 1-15 cm/yr) • Deformation is concentrated at plate boundaries • There are 3 types of tectonic boundaries ...
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GR. 6 EARTH SCIENCE CURRICULUM GUIDE Enduring

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... • Mantle: thickest layer, mostly solid except for upper mantle being able to flow like “thick toothpaste” • ____________core: liquid iron and nickel • ____________core: mostly iron, the tremendous pressure keeps it solid. – Heat from Earth’s core helps produce convection currents and hot-spot activi ...
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Jeopardy Game (ppt 9 MB)

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Print › Earthquakes: Chapter 5 | Quizlet

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Earthquakes

...  The area between 105-140 degrees from the epicenter  Area in which seismic waves can’t be detected  What is the cause?  Secondary waves can’t be transmitted through liquid layers  Primary waves are slowed and deflected by the outer core and speed up again when the reach the solid inner core ...
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Unit 3 Vocabulary

... Slab pull – force created by sinking of a plate, or slab, that pulls on the rest of the plate Subduction – sinking of a denser plate below a more buoyant plate at a convergent plate boundary Transform plate boundary – where two plates slide by each other Fault zone - area of many fractured pieces of ...
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Geophysics



Geophysics /dʒiːoʊfɪzɪks/ is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. The term geophysics sometimes refers only to the geological applications: Earth's shape; its gravitational and magnetic fields; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial relations; and analogous problems associated with the Moon and other planets.Although geophysics was only recognized as a separate discipline in the 19th century, its origins go back to ancient times. The first magnetic compasses were made from lodestones, while more modern magnetic compasses played an important role in the history of navigation. The first seismic instrument was built in 132 BC. Isaac Newton applied his theory of mechanics to the tides and the precession of the equinox; and instruments were developed to measure the Earth's shape, density and gravity field, as well as the components of the water cycle. In the 20th century, geophysical methods were developed for remote exploration of the solid Earth and the ocean, and geophysics played an essential role in the development of the theory of plate tectonics.Geophysics is applied to societal needs, such as mineral resources, mitigation of natural hazards and environmental protection. Geophysical survey data are used to analyze potential petroleum reservoirs and mineral deposits, locate groundwater, find archaeological relics, determine the thickness of glaciers and soils, and assess sites for environmental remediation.
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