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TSUNAMI GLOSSARY
TSUNAMI GLOSSARY

Chapter 2 - Mineral and Rocks
Chapter 2 - Mineral and Rocks

... Metamorphic Textures • Foliated texture – platy and elongate minerals aligned parallel to one another – caused by differential pressure ...
Happy First Day of Februaryана2/1/12 1. Plate Tectonics Review 2
Happy First Day of Februaryана2/1/12 1. Plate Tectonics Review 2

... Plate Tectonics Review by Mrs. Holz ...
The rise Tibetan - Oxford Academic
The rise Tibetan - Oxford Academic

... strong outer layer through which heat is conducted, overlies a much weaker layer, the asthenosphere, in which convection transports heat most efficiently and maintains, on average, a gentle adiabatic temperature gradient and modest horizontal pressure gradients. Crust is merely the top part of the l ...
No Slide Title
No Slide Title

... • Earth’s internal heat – aids melting and metamorphism ...
Final Exam Review
Final Exam Review

...  Distinguish between the upper and lower mantle  Distinguish between the lithosphere and asthenosphere  Distinguish between the outer and inner core.  Relate plates to the mantle and crust of the Earth  Relationship between the continents, crust and plates  Know the major plates of the world; ...
Tomographic Pn velocity and anisotropy structure beneath
Tomographic Pn velocity and anisotropy structure beneath

... Iranian Long Period Array (ILPA) located in northern Iran (Figure 1). The uncertainty of the Pn phase readings is less than one second. To include these data in our inversion we required a minimum of 10 different events per station and a minimum of 5 stations recording a single event. The larger qu ...
B.Sc. Syllabus Geology Semester I Paper I (Introduction to Geology)
B.Sc. Syllabus Geology Semester I Paper I (Introduction to Geology)

... Paper II (Structural Geology) Unit I Scope and aim of Structural Geology, Concept of rock deformation: Types of forces, stress and strain. Stereographic projections and its use in structural analysis. Compass clinometers and its parts, method of using the instrument. Study of outcrops, identificati ...
Unit F791 - Global tectonics
Unit F791 - Global tectonics

Name
Name

... happens there?) happens there?) ...
Tectonics
Tectonics

Lesson 6. The work of moving ice, wind and sea waves
Lesson 6. The work of moving ice, wind and sea waves

... great that snow in lower layers becomes granular, hard and compact. The pressure also quickens the melting of some of the snow, which on refreezing starts turning into a granular ice. Again it is the pressure of the overlying layers which makes this solid mass of ice mobile. This great mass of ice m ...
Geochemistry of near-EPR seamounts: importance of source vs
Geochemistry of near-EPR seamounts: importance of source vs

... lavas erupted on the nearby EPR axis. These isotopic ratios correlate with each other, with the abundances and ratios of incompatible elements, with the abundances of measured major elements such as MgO, CaO, Na2 O and TiO2 contents, and with the abundances and ratios of major elements corrected for ...
SUPO_Earth_Science_Assessments_May09
SUPO_Earth_Science_Assessments_May09

... E5.1 A: Describe the position and motion of our solar system in our galaxy and the overall scale, structure, and age of the universe. 1. Periodically, there are spectacular meteor showers on Earth. These showers usually occur because the Earth’s orbit passes through the remains of____________. A. B. ...
Mantle hotspot neon in basalts from the Northwest Lau Back
Mantle hotspot neon in basalts from the Northwest Lau Back

... in the petrogenesis of basaltic magma in back-arc basins are topics of considerable interest. Isotopic tracers measured in basalts provide some of the most powerful insight to these tectonically complex regions. In this paper we investigate helium and neon isotope variations in lavas from the Northw ...
Geography-11 (Eng) - Punjab School Education Board | cPanel Login
Geography-11 (Eng) - Punjab School Education Board | cPanel Login

... Nuts. 1. Mercury : This planet is not only smallest one but also lies closest ...
Fractured Earth - Do plumes exist?
Fractured Earth - Do plumes exist?

... existence of mantle plumes. Instead, they argue for a ‘plate model’ that does not rely on mantle plumes, but rather on forces generated by the plates themselves. In this model LIPS are produced from simple decompression melting of the mantle during rifting, and the location of volcanism is fixed by ...
plates
plates

... In the 1960s, scientists developed a new theory that combined continental drift and seafloor spreading. According to the theory of Plate Tectonics, Earth’s crust and part of the upper mantel are broken into sections. These sections, called plates, move on a plastic-like layer of the mantle. The plat ...
U4-T2.8-Geology of Newfoundland
U4-T2.8-Geology of Newfoundland

... It is thought that the geology of Island Newfoundland resulted long ago when the Iapetus Ocean was closing. The North American plate collided with the African plate and as a result a portion of the Iapetus Ocean floor was sandwiched in between. Zone “A” is referred to as the Western (Humber) Zone an ...
Lithosphere, Earth`s Interior and Paleo-Environment
Lithosphere, Earth`s Interior and Paleo-Environment

A dynamic model of hot fingers in the mantle wedge in
A dynamic model of hot fingers in the mantle wedge in

... have been reported from many areas (Kuno, 1960; 1966; for summary, see Gill, 1981, p.209). Chemical analyses of basalt from 20 Quaternary volcanoes in NE Japan arc are reviewed to evaluate across- and along-arc variations. A plot of total alkalis (Na2O+K2O) against SiO2 of basalts in NE Japan (Fig. ...
Geology :: 8. Divergent plate margins
Geology :: 8. Divergent plate margins

... The relative speed of two spreading plates can be calculated on the magnetic pole reversals. The most recent magnetic reversal recorded near the crest of a mid-oceanic ridge occurred 730,000 years ago. The oldest reversal so far found in oceanic crust date back to the middle Jurassic, about 165 mill ...
Continental subduction and exhumation of high
Continental subduction and exhumation of high

... sedimentary layer, the crust made of a stronger material, and of a still stronger lithospheric mantle. The whole model is subjected to a constant vertical thermal gradient, causing the strength reduction with depth in each lithospheric layer. Subduction is driven by both push force and pull force. D ...
Geodynpub_files/Boutelier, 2004
Geodynpub_files/Boutelier, 2004

... sedimentary layer, the crust made of a stronger material, and of a still stronger lithospheric mantle. The whole model is subjected to a constant vertical thermal gradient, causing the strength reduction with depth in each lithospheric layer. Subduction is driven by both push force and pull force. D ...
Transition from continental break
Transition from continental break

... Processes controlling volcanicity at passive margins include the interaction of mantle plumes with the lithosphere [White, 1992], small thermal anomalies in the mantle with no mantle plumes [Anderson, 2000] and convective upwelling of mantle material into the melting zone during rifting (small-scale ...
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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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