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Name Student ID Exam 2b – GEOL 1113 Fall 2009 ____
Name Student ID Exam 2b – GEOL 1113 Fall 2009 ____

... _____ 32. A Benioff earthquake zone is significant in plate tectonic theory because it a. locates rift valleys on continents b. coincides with mid-oceanic ridges c. traces the descent of a sea-floor slab subducting into an oceanic trench or under a continent d. may predict quake locations under tran ...
Exam 2a – GEOL 1113 Fall 2009
Exam 2a – GEOL 1113 Fall 2009

Geologic Time Scale
Geologic Time Scale

... Geologic Time Scale The History of Our Earth ...
chapter 8 - Team Strength
chapter 8 - Team Strength

... Completion: Using the word bank below, complete each sentence or statement. (2 Pts Each) 35. The location on Earth’s surface above the point where an earthquake starts is the ____________________. 36. Movements that follow a major earthquake often produce smaller earthquakes called ________________. ...
Earthquakes
Earthquakes

... of the damage done by earthquakes.  Body waves are of two types, compressional and shear. Both types pass through the Earth's interior from the focus of an earthquake to distant points on the surface, but only compressional waves travel through the Earth's molten core. Because compressional waves t ...
Earth/Environmental Science Review Packet
Earth/Environmental Science Review Packet

... C. change in direction of the axis, but without any change in tilt—this changes the stars near (or not near) the Pole D. wobbling around the axis (This occurs over an 18 year period) E. the center of mass where two or more celestial bodies orbit each other(This is the point about which the Earth and ...
GEOL 1080 I - Research at UVU
GEOL 1080 I - Research at UVU

Concept Test
Concept Test

... Recent evidence suggests that Mars, like Earth, once had a stronger magnetic field. Assuming this is true, which of the following could explain why Mars lacks a global magnetic field like that of Earth? a. Because Mars's interior is cooler than Earth's, its liquid core layer may not be undergoing co ...
Skinner Chapter 5
Skinner Chapter 5

... 47. (modified Mercalli) OR (modified Mercalli intensity) 48. shape...volume 49. Earthquakes cause damage by (1) ground motion; (2) faulting and surface rupturing; (3) fires; (4) land movement and slope collapse; (5) liquefaction; and (6) tsunami. 50. Seismic gaps are places along seismically active ...
The Structure of the Earth and Plate Tectonics
The Structure of the Earth and Plate Tectonics

... Ocean-Ocean Plate Collision • WHEN TWO OCEANIC PLATES COLLIDE, ONE RUNS OVER THE OTHER WHICH CAUSES IT TO SINK INTO THE MANTLE FORMING A SUBDUCTION ZONE. • THE SUBDUCTING PLATE IS BENT DOWNWARD TO FORM A VERY DEEP DEPRESSION IN THE OCEAN FLOOR CALLED A TRENCH. • THE WORLDS DEEPEST PARTS OF THE OCEA ...
Themes in Regional Geography
Themes in Regional Geography

... Causes of Global Warming • Emission of anthropogenic (human-caused) ...
1. Continental drift? What evidence did Alfred Wagner use to
1. Continental drift? What evidence did Alfred Wagner use to

... 1. Continental drift? What evidence did Alfred Wagner use to support his theory of? He thought that continents were an only piece of land but then they were separated. 2. Why do you think people didn't believe continental drift theory when Wagner first explained it? Because he didn’t prove why conti ...
Oreo Cookie Plate Tectonics
Oreo Cookie Plate Tectonics

Chapt12RHS2014
Chapt12RHS2014

... • Most mineral prices are kept artificially low. • Extraction of lower grades of ore is possible due to technological advances. Good idea? • Biomining (in-place, or in situ) -use or microorganisms to break down rock material and extract minerals. • Importance of rare earth metals – see p. 291 ...
Layers of the Moon - Challenger Center
Layers of the Moon - Challenger Center

... Knowledge of the Moon’s interior is limited; however, scientists have developed  a model based on available data. The current model suggests that the Moon has a  partially  molten  iron‐rich  core.  Seismic  equipment  left  by  Apollo  astronauts  indicates that inner parts may be partially molten. ...
Section 1 Review
Section 1 Review

Tectonic Plate Motions
Tectonic Plate Motions

... Convection within the Earth’s mantle causes the plates to move. Mantle material is heated above the core. The hot mantle rises up toward the surface ( Figure 1.2). As the mantle rises, it cools. At the surface, the material moves horizontally away from a mid-ocean ridge crest. The material continues ...
EarthquakesHnrs2
EarthquakesHnrs2

... build strain on rocks again)  Monitor to look for patterns – Parkfield, California had earthquakes every 22 years – In anticipation of the next one, seismographs were put into place, but it has not yet occurred (overdue by 16 years since last one was in 1966)  Seismic gaps: sections of active faul ...
Research Activities:  Jer-Ming Chiu
Research Activities: Jer-Ming Chiu

... high-resolution images of 3-D structure in Taiwan region and their tectonic evolution seismic wave propagation within subduction zones and 3-D geometry and internal structure of subduction zones deformation and tectonic evolution of converging continental and oceanic plates images of anomalous areas ...
Slide 1
Slide 1

... • Sediments moved by wind, water, ice or gravity • Heavy sediments press down on the layers beneath (compaction) • Dissolved minerals flow between particles and cement them together (cementation) ...
Trivial Pursuit File
Trivial Pursuit File

Lab 2: The Interior of the Earth
Lab 2: The Interior of the Earth

... • Vibrations of the earths crust are earthquakes. • When an earthquake occurs energy waves radiate out in all directions. These waves are called seismic waves. • Scientist cannot see seismic waves traveling through the Earth but they can detect them with a seismograph. • Seismologists, scientists th ...
chapter 14 - TeamCFA school
chapter 14 - TeamCFA school

... CORE CASE STUDY: The crucial importance of rare-earth metals. Few people have heard of rare-earth metals and oxides that are crucial to the major technologies that support today’s lifestyles and economies. Without affordable supplies of rare-earth metals, industrialized nations could not develop the ...
Climate Zones - Lourdes Academy
Climate Zones - Lourdes Academy

... Natural Resources in History • Natural resources affected the location and growth of settlements all through history.  • Asians and Europeans came into contact with one another partly because Europeans wanted the silks and spices of Asia that had been cultivated.  • Modern industry started in cou ...
3D Imaging of the Earth`s Lithosphere Using Noise from Ocean Waves
3D Imaging of the Earth`s Lithosphere Using Noise from Ocean Waves

... Seismic tomography is the main technique available to image the subsurface structure of the Earth across a range of scales. This technique is similar in principle to CT scans that are used in medicine. Based on a CT scan, doctors can “see” organs and bones inside human bodies. Likewise, through seis ...
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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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