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Graham Cracker Model of Plate Tectonics
Graham Cracker Model of Plate Tectonics

... Graham Cracker Model of Plate Tectonics Background The Theory of Plate Tectonics states that the crust of the Earth is composed of seven major plates and numerous smaller plates. These plates “ride” on the hot plastic upper mantle known as the asthenosphere. This theory also says that most of these ...
CAN IMPACTS INDUCE VOLCANIC ERUPTIONS? by H. J. Melosh
CAN IMPACTS INDUCE VOLCANIC ERUPTIONS? by H. J. Melosh

Introductory Presentation on Earthquakes
Introductory Presentation on Earthquakes

... • Everyone should have personal disaster supplies kit. Keep one kit in your home, another in your car, and a third kit at work. • Store a household disaster supplies kit in an easily accessible location, with a threeday to one-week supply of essential items ...
Standards
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...  Why are there earthquakes, volcanoes and ridges at the plate boundaries?  How come you don’t see earthquakes at the midocean ridges so much?  Why are there earthquakes but not volcanoes in the Himalayas above India? All these questions are related to the differences in what is happening at each ...
Structural models of the Mediterranean lithospehre
Structural models of the Mediterranean lithospehre

... of  Apenninic  subduc7on,  as  a  result  of  the  global   westward  mo7on  of  the  lithosphere  with  respect  to  the   underlying  mantle.     ...
Earthquake Depths
Earthquake Depths

... Copy and define Key Terms in a foldable, or on index cards: plate tectonics, plates, lithosphere, asthenosphere, faults, earthquake, normal fault, reverse fault, strike-slip fault, seismic waves, focus, primary waves, secondary waves, surface waves, epicenter, seismograph, On page 154 read the poem ...
Fundamentals Of Physical Geography Class XI NCERT
Fundamentals Of Physical Geography Class XI NCERT

... different aspects of human life. Its imprints can be noticed on food, clothing, shelter and occupation. Human beings have come to terms with nature through adaptation and modification. As you already know, the present society has passed the stage of primitive societies, which were directly dependent ...
Teacher Period _____ Date
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... Background The main force that shapes our planet’s surface over long periods of time is the movement of Earth’s outer layer by the process of plate tectonics. The rigid outer layer of the Earth, called the lithosphere, is made of plates that fit together like a jigsaw puzzle. These plates are made o ...
new geophysical data about the inner structure of drake passage crust
new geophysical data about the inner structure of drake passage crust

... The analysis of the magnetic anomaly patterns in Drake Passage has allowed the reconstruction of the geological events since Late Oligocene [11]. The existent negative and positive magnetic anomaly distribution associated with different time of the oceanic floor areas formation corresponds with the ...
What is Density?
What is Density?

... Denser liquids help you float more easily. That is why it is easier to float in the ocean, than in a freshwater lake. ...
Grand Canyon National Park Geology Lesson Plans
Grand Canyon National Park Geology Lesson Plans

... hot, yielding upper mantle zone at very slow rates of a few centimeters per year. The crust is much thinner under the oceans than under the continents. Between 100 and 200 kilometers below the Earth’s surface, the temperature of the rock is near the melting point; molten rock erupted by some volcano ...
IgneousPet423-13Intro
IgneousPet423-13Intro

... To determine the proportion of the elements in the Sun, we make use of the energy levels between the electron orbitals of the atoms of the different elements. The electromagnetic spectra of the Sun was noted to contain dark lines in 1802 by Wollaston and later studied by Fraunhofer (early 1800's), i ...
Upper-mantle velocity structure beneath the North China Craton
Upper-mantle velocity structure beneath the North China Craton

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volcano hazards fact sheet
volcano hazards fact sheet

... thick. Some of the basaltic melt, or magma, produced by the hot spot accumulates near the base of the plate, where its heat melts rocks from the Earth's lower crust. These melts, in turn, rise closer to the surface to form large reservoirs of potentially explosive rhyolite magma. Catastrophic erupti ...
Click when ready
Click when ready

... • Background: Risk is a part of every landscape. When people select a site for a home, a factory, a fort, or a shopping center, they take many factors into consideration. One of those factors involves environmental Perception of the amount of danger may Readhazards. Background be wildly inaccurate. ...
The Theory of Plate Tectonics
The Theory of Plate Tectonics

... subduction zones forms magma, which rises to the Earth's sur­ face and erupts to form volcanic mountains. Volcanic mountains can also form under the sea. Sometimes, these mountains can rise above the ocean surface to become islands. The majority of tectonically active volcanic mountains on the Earth ...
Fall Final Exam Review
Fall Final Exam Review

... • Erosion: process in which the materials of Earth’s surface are loosened, dissolved, or worn away and transported from one place to another by a natural agent, such as wind, water, ice, or gravity • Mechanical weathering: produces smaller pieces • Chemical Weathering: Chemical alteration of mineral ...
Igneous Landforms and Geothermal Activity
Igneous Landforms and Geothermal Activity



... Ans: An earthquake is a sudden shaking or trembling of the earth lasting for a very short time. Q. What Causes an Earthquake? Ans: Earthquake is caused by a disturbance deep inside the earth’s crust created by motion of tectonic plate. Q. What could cause a disturbance inside the earth? Ans: Some ti ...
Plates on the Move
Plates on the Move

... under water. These rocks showed that molten material has erupted over and over along the mid-ocean ridge. ...
Geomorphic Processes and Evolution of Landforms
Geomorphic Processes and Evolution of Landforms

... colour of iron upon reduction turns to greenish or bluish grey. These weathering processes are interrelated. Hydration, carbonation and oxidation go hand in hand and hasten the weathering process. Can we give iron rusting as an example of oxidation? How essential is water in chemical weathering proc ...
It`s getting hot in here
It`s getting hot in here

... released onto the landscape, we say that the volcanic activity is extrusive(30), meaning it is on the exterior, or outside of the Earth. Magma that reaches the service is known as lava. Lava flows are extraordinarily hot, and destructive. In many cases, these lava flows are slow and continuous but v ...
Fig. 2.1 The change in temperature of a water parcel
Fig. 2.1 The change in temperature of a water parcel

... By virtue of their distinctive chemical and isotopic signatures, it is possible to track the flow of water masses and to infer how long ago water in various parts of the world’s oceans was in contact with the atmosphere. Such chemical analyses indicate the existence of a slow overturning characteriz ...
Alfred Wegener and continental drift
Alfred Wegener and continental drift

... On January 6th, 1912, Alfred Wegener presented his hypothesis of continental drift at the general assembly of the German Geological Union in Frankfurt. In the following months he published two papers whose contents are very similar: one in Petermann’s Mitteilungen, a geographical journal, and the ot ...
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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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