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... Oikawa et al. 2010 ...
Lecture 4 Igneous Rocks - University of Illinois
Lecture 4 Igneous Rocks - University of Illinois

... • magma: igneous rocks form from the cooling of molten (or partially molten) rock materials called magma, which consists liquid, dissolved gas, and crystals. • lava: magma that reaches Earth's surface • extrusive or volcanic: igneous rocks that form when molten rock solidifies at the surface • intru ...
Part2platetectonics BEST!
Part2platetectonics BEST!

... Challenger Deep got its name from the British survey ship Challenger II, which pinpointed the deep water off the Marianas Islands in 1951. Then in 1960, the US Navy sent the Trieste (a submersible - a mini-submarine designed to go really deep) down into the depths of the Marianas trench to see just ...
Lecture 4 Igneous Rocks
Lecture 4 Igneous Rocks

... “... Pahoehoe forms ropy features on the surface but aa forms a rough jagged blocky surface. Pahoehoe shows a relatively smooth surface. This illustrates that pahoehoe is the more fluid of the two lavas and it yields thinner individual flows.” ...
The long-term strength of continental lithosphere: “jelly sandwich” or
The long-term strength of continental lithosphere: “jelly sandwich” or

Mineral Environments of Formation
Mineral Environments of Formation

... bottom of the magma chamber to form ore deposits. ...
Session 4
Session 4

... The theory of plate tectonics has been built from observations of local phenomena (e.g., volcanoes and earthquakes) that indicate patterns at a global scale. Yet many students do not live in places where such observable phenomena occur. And, it’s hard to appreciate the global patterns that exist (e. ...
Study-Questions3
Study-Questions3

... 20. What U.S. state has the most earthquakes? What type of plate boundary generates many of these earthquakes? 21. Could an earthquake similar to the one that triggered the 2004 tsunami in the Indian Ocean and the 2011 tsunami that devastated parts of Japan also occur on west coast of the U.S.? Exp ...
Word - CDE
Word - CDE

... What components of a plant or animal could cease to function and still allow the organism to survive? What components of a plant or animal could cease to function that would cause the organism to die? What adaptations or characteristics help humans to ...
Slide 1
Slide 1

... • Much of the sediments formed by the wind and water erosion are deposited into the sea, where new sedimentary rocks will be formed. • The grinding movement of the Earth’s tectonic plates also recycles rocks. Pieces of igneous and seabed sedimentary rock get broken off and are added to the cycle. • ...
Lithological Processes, Hazards and Management (1)
Lithological Processes, Hazards and Management (1)

...  Age and thickness of sedimentation increases with increasing distance Subduction:  Hypothesis: crust destruction  Supporting evidence o Most intense seismic activity o Pattern of earthquake foci  More recent activity at shallow depth  Benioff zone about 45 degree angle: marks line of disturban ...
Eastern Klamath Mountains - College of the Siskiyous
Eastern Klamath Mountains - College of the Siskiyous

Can a Horizontal Astronomical Driving Force and an
Can a Horizontal Astronomical Driving Force and an

... corresponds to the mean semidiurnal lunar wave M2, which is responsible first of all for the generation of tidal bulge; the solid Earth tides have a well-known vertical oscillation of 300–400 mm/12 h25′, but they also have a relevant 150–200 mm/12 h25′ horizontal swinging. Under a permanent torque, t ...
No Slide Title
No Slide Title

... • By the time this Archean event ended – several cratons had formed that are found – in the older parts of the Canadian shield ...
EPSL Effects of relative plate motion on the deep structure and
EPSL Effects of relative plate motion on the deep structure and

... the Mariana arc. The age of subducting lithosphere is an important control in the subduction process [19], but the increase from about 135 Ma at the northern Izu-Bonin trench to over 150 Ma at the Mariana trench [20] is too small to explain the lateral variations in the Wadati-Benioff zones. We note ...
Bell Ringer 1-5-10
Bell Ringer 1-5-10

... Bell Ringer 2-4-11 1. Classify each of the following layers as liquid, solid, or solid but able to flow slowly: lithosphere, asthenosphere, lower mantle, out core, inner core. 2. What is conduction? 3. What is the role of gravity in creating convection currents? 4. What are the three types of heat ...
PEUXENOS
PEUXENOS

... second largest plateau on Earth. It has an average eleva-tion of nearly 4000 m, a crustal thickness of at least 65 km, and covers an area of over 600,000 km2. The plaetau is part of the central Andean mountain belt associated with the subduction of the Nazca plate beneath the South American plate. C ...
Earth Science - Adventist Education
Earth Science - Adventist Education

... Recognize God as the Designer and Creator of our earth within the universe. Introduce and relate terminology appropriate to Earth Science. Demonstrate understanding of the structure and composition of earth (geologic time table, plate tectonics, rocks and minerals). Become acquainted with the geolog ...
First order of relief
First order of relief

... Explanations for the Crustal Dichotomy Endogenous explanations ...
Question paper - Unit F791 - Global tectonics
Question paper - Unit F791 - Global tectonics

... (a) In 1915, Alfred Wegener published his book The Origin of Continents and Oceans. This put forward the first strong case for the movement of continents. Using the subheadings below, outline evidence for continental drift. (i) ...
Plate Tectonic: Plates and Their Consequences [8th grade]
Plate Tectonic: Plates and Their Consequences [8th grade]

... lithosphere and the mantle. Using their knowledge of this relationship, students will then be engaged in exploring how tectonic plates work and their interactions along plate boundaries. Students will also be able to predict the resulting geologic activity given a specific plate boundary type. Lastl ...
Dynamic Earth Unit 4 lesson 5 Earthquakes
Dynamic Earth Unit 4 lesson 5 Earthquakes

... What are some effects of earthquakes? • Most earthquakes do not cause damage, but some strong earthquakes can cause major damage and loss of life, especially in areas closest to the epicenter. • When the shaking of an earthquake is more than ...
THE ORIGIN AND GROWTH OF CONTINENTS 1 Geophysical
THE ORIGIN AND GROWTH OF CONTINENTS 1 Geophysical

... (5) Erosion of shield areas removes K, U and Th and reduces the heat flow to levels below those of present erogenic areas. INTRODUCTION The origin of continents is a basic problem in geology and there have been two opposing schools of thought since the subject received scientific attention. The firs ...
Plate boudaries
Plate boudaries

... The oceanic plate descends under the continental plate because it is denser. As the plate descends it starts to melt due to the friction caused by the movement between the plates. This melted plate is now hot, liquid rock (magma). The magma rises through the gaps in the continental plate. If it reac ...
Crustal Features
Crustal Features

... Crustal Features 8.9B relate plate tectonics to the formation of crustal features ...
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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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