
Universe 8e Lecture Chapter
... 1960s and early 1970s and from more recent observations by unmanned spacecraft. Analysis of seismic waves and other data indicates that the Moon has a crust thicker than that of the Earth (and thickest on the far side of the Moon), a mantle with a thickness equal to about 80% of the Moon’s radius, a ...
... 1960s and early 1970s and from more recent observations by unmanned spacecraft. Analysis of seismic waves and other data indicates that the Moon has a crust thicker than that of the Earth (and thickest on the far side of the Moon), a mantle with a thickness equal to about 80% of the Moon’s radius, a ...
Identifying Plate Tectonics Lab 1-34
... 41. The sediments found in this sediment core are evidence that supports the theory of plate tectonics. To see why, suppose that the ocean floor did not move away from the midocean ridge. (In other words, suppose that the theory of plate tectonics was incorrect.) In this case, what would the sedimen ...
... 41. The sediments found in this sediment core are evidence that supports the theory of plate tectonics. To see why, suppose that the ocean floor did not move away from the midocean ridge. (In other words, suppose that the theory of plate tectonics was incorrect.) In this case, what would the sedimen ...
Kevin
... • Definition : The cycle of movement in the asthenosphere that causes the plates of the lithosphere to move. Heated material in the asthenosphere becomes less dense and rises toward the solid lithosphere, through which it cannot rise further. It therefore begins to move horizontally, dragging the li ...
... • Definition : The cycle of movement in the asthenosphere that causes the plates of the lithosphere to move. Heated material in the asthenosphere becomes less dense and rises toward the solid lithosphere, through which it cannot rise further. It therefore begins to move horizontally, dragging the li ...
Plate Tectonics and the Rock Cycle
... Volcanism within the continents is complex and not well understood. Two origins have been suggested for these volcanic regions (Figure 2-6). One model suggests that some of the continental flood basalts are the result of magmas generated by a hotspot underneath the continent (i.e. Yellowstone). The ...
... Volcanism within the continents is complex and not well understood. Two origins have been suggested for these volcanic regions (Figure 2-6). One model suggests that some of the continental flood basalts are the result of magmas generated by a hotspot underneath the continent (i.e. Yellowstone). The ...
Oceanography Questions for Test 1
... Design a research program (ship-, land- or space based) to illustrate three convincing lines of evidence for plate tectonics. You could design an oceanographic research cruise to map the midocean ridges by any ...
... Design a research program (ship-, land- or space based) to illustrate three convincing lines of evidence for plate tectonics. You could design an oceanographic research cruise to map the midocean ridges by any ...
Minerals Give Clues To Their Environment Of Formation Also Rocks
... !! Volcanic activity is concentrated along plate margins. Andesitic volcanoes are found at subduction margins, and basaltic volcanoes are concentrated along spreading margins. Rhyolitic volcanoes occur at collision margins and in places where rising basaltic magma causes the continental crust to me ...
... !! Volcanic activity is concentrated along plate margins. Andesitic volcanoes are found at subduction margins, and basaltic volcanoes are concentrated along spreading margins. Rhyolitic volcanoes occur at collision margins and in places where rising basaltic magma causes the continental crust to me ...
Physics of Terrestrial Planets and Moons: An
... geophysical properties of the Earth-like planets and moons, those bodies that consist largely of rock, iron, and water, and the processes occurring in their interiors and on their surfaces. But it goes further by discussing the giant planets and asteroids and comets as well and other extrasolar plan ...
... geophysical properties of the Earth-like planets and moons, those bodies that consist largely of rock, iron, and water, and the processes occurring in their interiors and on their surfaces. But it goes further by discussing the giant planets and asteroids and comets as well and other extrasolar plan ...
Document
... 2) a given petrogenetic process can produce magmas with different chemical and isotopic composition; 3) tomographic studies do not furnish unique results (i.e., different models can give contrasting conclusions); ...
... 2) a given petrogenetic process can produce magmas with different chemical and isotopic composition; 3) tomographic studies do not furnish unique results (i.e., different models can give contrasting conclusions); ...
Evolution of helium and argon isotopes in a convecting mantle
... depth, but varied in the deeper mantle to reflect present uncertainties. Cases are presented that focus on the influence of two uncertain physical parameters: the density of subducted eclogite in the deep mantle, and the partition coefficient for helium. Results indicate that the system self-consist ...
... depth, but varied in the deeper mantle to reflect present uncertainties. Cases are presented that focus on the influence of two uncertain physical parameters: the density of subducted eclogite in the deep mantle, and the partition coefficient for helium. Results indicate that the system self-consist ...
Melting under the Colorado Plateau, USA
... of mantle asthenosphere (Carlson and Nowell, 2001, and references therein), and geochemical evidence for melting above the garnet-spinel transition zone (Asmerom, 1999, and references therein) suggest melt generation in CP lithosphere. Thermal relaxation of lithosphere adjacent to warmer asthenosphe ...
... of mantle asthenosphere (Carlson and Nowell, 2001, and references therein), and geochemical evidence for melting above the garnet-spinel transition zone (Asmerom, 1999, and references therein) suggest melt generation in CP lithosphere. Thermal relaxation of lithosphere adjacent to warmer asthenosphe ...
Evidence for both crustal and mantle earthquakes in the subducting
... [15] In a recent study, Hacker et al. [2002a, 2002b] tested the hypothesis that the intermediate-depth earthquakes in the upper and lower seismic zones are related to dehydration reactions. Based on thermal-petrological models, they predict eclogite transformation and associated seismicity in the up ...
... [15] In a recent study, Hacker et al. [2002a, 2002b] tested the hypothesis that the intermediate-depth earthquakes in the upper and lower seismic zones are related to dehydration reactions. Based on thermal-petrological models, they predict eclogite transformation and associated seismicity in the up ...
Earth Science Chapter 9 Section 2 Review
... ____ 11. What type of boundary occurs where two plates move together, causing one plate to descend into the mantle beneath the other plate? a. transform fault boundary c. convergent boundary b. divergent boundary d. transitional boundary ____ 12. Which of the following is a geographic example of a t ...
... ____ 11. What type of boundary occurs where two plates move together, causing one plate to descend into the mantle beneath the other plate? a. transform fault boundary c. convergent boundary b. divergent boundary d. transitional boundary ____ 12. Which of the following is a geographic example of a t ...
Lesson 1 - Earth`s Oceans and the Ocean Floor - Hitchcock
... • Satellites can measure variations in the height of the ocean’s surface. The ocean floor’s features can affect the height of the water above them. • To explore the oceans, scientists use underwater vessels, some of which have pilots and researchers. Other vessels are remotely operated. • Using equi ...
... • Satellites can measure variations in the height of the ocean’s surface. The ocean floor’s features can affect the height of the water above them. • To explore the oceans, scientists use underwater vessels, some of which have pilots and researchers. Other vessels are remotely operated. • Using equi ...
Lesson 1 - Earth`s Oceans and the Ocean Floor - Hitchcock
... • Satellites can measure variations in the height of the ocean’s surface. The ocean floor’s features can affect the height of the water above them. • To explore the oceans, scientists use underwater vessels, some of which have pilots and researchers. Other vessels are remotely operated. • Using equi ...
... • Satellites can measure variations in the height of the ocean’s surface. The ocean floor’s features can affect the height of the water above them. • To explore the oceans, scientists use underwater vessels, some of which have pilots and researchers. Other vessels are remotely operated. • Using equi ...
Subduction zone backarcs, mobile belts, and orogenic heat
... We include one oceanic backarc (Bering Sea) and one former continental backarc (the northern Canadian Cordillera that was cut off by transform faulting in the Eocene) that give very similar thermal results to the current continental backarcs. The heat flow averages range from 70 to 85 mW/m2; Pn velo ...
... We include one oceanic backarc (Bering Sea) and one former continental backarc (the northern Canadian Cordillera that was cut off by transform faulting in the Eocene) that give very similar thermal results to the current continental backarcs. The heat flow averages range from 70 to 85 mW/m2; Pn velo ...
True polar wander
... Polar wander should not be confused with precession or nutation, which is where the axis of rotation moves, in other words the North Pole points toward a different star. These are caused by the gravitational attraction of the Moon and Sun, and occurs all the time and at a much faster rate than polar ...
... Polar wander should not be confused with precession or nutation, which is where the axis of rotation moves, in other words the North Pole points toward a different star. These are caused by the gravitational attraction of the Moon and Sun, and occurs all the time and at a much faster rate than polar ...
Lecture Outlines PowerPoint Chapter 7 Earth Science, 12e Tarbuck
... Hot spots and mantle plumes • Caused by rising plumes of mantle material • Volcanoes can form over them (Hawaiian ...
... Hot spots and mantle plumes • Caused by rising plumes of mantle material • Volcanoes can form over them (Hawaiian ...
The westward drift of the lithosphere
... grouped hotspots into three main families that have very little internal relative motion (Pacific, Indo-Atlantic, and Iceland). In his analysis, Pacific hotspots have remained nearly fixed relative to each other during the last 80 m.y. We do not yet have a reliable constraint on the source depth of ...
... grouped hotspots into three main families that have very little internal relative motion (Pacific, Indo-Atlantic, and Iceland). In his analysis, Pacific hotspots have remained nearly fixed relative to each other during the last 80 m.y. We do not yet have a reliable constraint on the source depth of ...
Plate C Plate D
... Activity 4: Ocean Depth and Age of Crust We have seen that as ocean crust moves away from mid-ocean ridge it gets older and deeper. We now can derive a relationship between water depth and age. 1. Make a plot of the Water Depth (D) vs. T 1/2 (where T = age of oceanic crust) on the graph below. First ...
... Activity 4: Ocean Depth and Age of Crust We have seen that as ocean crust moves away from mid-ocean ridge it gets older and deeper. We now can derive a relationship between water depth and age. 1. Make a plot of the Water Depth (D) vs. T 1/2 (where T = age of oceanic crust) on the graph below. First ...
Chapter 12.2
... Describing Earthquakes (continued) • Seismometers are used to measure seismic wave energy. Early seismometers just measured whether the ground shook. Some seismometers measure horizontal movement, others vertical movement. A seismogram is produced, showing when an earthquake started, how long ...
... Describing Earthquakes (continued) • Seismometers are used to measure seismic wave energy. Early seismometers just measured whether the ground shook. Some seismometers measure horizontal movement, others vertical movement. A seismogram is produced, showing when an earthquake started, how long ...
end of course earth science
... accumulating in shallow swamps. The EY10D202 墍 weight of the sediments caused the C area beneath them to sink, allowing more sediments to accumulate. The process continued until many layers ...
... accumulating in shallow swamps. The EY10D202 墍 weight of the sediments caused the C area beneath them to sink, allowing more sediments to accumulate. The process continued until many layers ...
toward
... In Selinsgrove, which of these forces are we likely to see: plate tectonics, weathering, erosion, volcanic eruption, or deposition? ...
... In Selinsgrove, which of these forces are we likely to see: plate tectonics, weathering, erosion, volcanic eruption, or deposition? ...
tectonic plates
... At ocean ridges, the plates are hot and magma pushes up between the plates forcing them apart. At trenches, an oceanic plate is cold and dense. Gravity pulls the plate edge down into the mantle, dragging the rest of the plate after it. This explanation of plate movement takes account of: • ridges • ...
... At ocean ridges, the plates are hot and magma pushes up between the plates forcing them apart. At trenches, an oceanic plate is cold and dense. Gravity pulls the plate edge down into the mantle, dragging the rest of the plate after it. This explanation of plate movement takes account of: • ridges • ...
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.