File
									
... • What is the driving force behind seafloor spreading? • How does the record of earth’s magnetic field support the theory of seafloor spreading? • What is a Hot Spot? ...
                        	... • What is the driving force behind seafloor spreading? • How does the record of earth’s magnetic field support the theory of seafloor spreading? • What is a Hot Spot? ...
									Plate Tectonics Internet Scavenger Hunt
									
... 18. As the seafloor spread apart, how does the magnetism of rocks oriented themselves with respect to the earth’s present magnetic field? Do the rocks forming (cooling & crystallizing) today show normal or reversed magnetism? ...
                        	... 18. As the seafloor spread apart, how does the magnetism of rocks oriented themselves with respect to the earth’s present magnetic field? Do the rocks forming (cooling & crystallizing) today show normal or reversed magnetism? ...
									Geology and Nonrenewable Minerals Chapter 14
									
... • 2000: Collapse of a dam retaining a cyanide leach pond • Impact on organisms and the environment ...
                        	... • 2000: Collapse of a dam retaining a cyanide leach pond • Impact on organisms and the environment ...
									Lesson 2 | Shaping Earth`s Surface
									
... polarity, the lines of force are arranged so magnetic north is close to Earth’s geographic north. Researchers discovered that Earth’s magnetic field periodically reverses; the north magnetic pole becomes the south pole and vice versa. Basaltic lavas contain minerals such as magnetite, which act like ...
                        	... polarity, the lines of force are arranged so magnetic north is close to Earth’s geographic north. Researchers discovered that Earth’s magnetic field periodically reverses; the north magnetic pole becomes the south pole and vice versa. Basaltic lavas contain minerals such as magnetite, which act like ...
									Document
									
... What are the layers of the Earth based on chemistry (in the correct order, from the center to the surface)? A. Crust, Mantle, Core B. Core, Mantle, Crust C. Mantle, Core, Crust D. Inner Core, Outer Core, Mantle, Crust ...
                        	... What are the layers of the Earth based on chemistry (in the correct order, from the center to the surface)? A. Crust, Mantle, Core B. Core, Mantle, Crust C. Mantle, Core, Crust D. Inner Core, Outer Core, Mantle, Crust ...
									What we`re gonna do today
									
... need to look to find the oldest rocks? What we’re gonna do today Video: Plate Tectonics Reflect Please write a one paragraph summary of the video. In your paragraph, please also give a critique of the video. Please be honest and appropriate. Homework Have a wonderful weekend! ...
                        	... need to look to find the oldest rocks? What we’re gonna do today Video: Plate Tectonics Reflect Please write a one paragraph summary of the video. In your paragraph, please also give a critique of the video. Please be honest and appropriate. Homework Have a wonderful weekend! ...
									Cooperative Institute for Dynamic Earth Research 2016 CIDER
									
...  Resulted in proposal to NSF/CSEDI->  co- funded 1st summer program with KITP (2004)  Funded summer at KITP in 2006, 2008, 2010 ...
                        	...  Resulted in proposal to NSF/CSEDI->  co- funded 1st summer program with KITP (2004)  Funded summer at KITP in 2006, 2008, 2010 ...
									Exam 1
									
... because: a. the break up of Panthalassa has destroyed all ancient seafloor b. all the older seafloor is layered under the present continental crust c. new seafloor eventually subducts and melts in deep-sea trenches; this process rarely takes longer than 200 million years., d. older seafloor is destr ...
                        	... because: a. the break up of Panthalassa has destroyed all ancient seafloor b. all the older seafloor is layered under the present continental crust c. new seafloor eventually subducts and melts in deep-sea trenches; this process rarely takes longer than 200 million years., d. older seafloor is destr ...
									Magnetic Field, Sea-floor Spreading, Deep
									
... MAGNETIC FIELD Some of our most important evidence of sea-floor spreading comes from magnetic reversals recorded on the ocean floor The magnetic poles can change place (called magnetic reversal) Magnetic mineral grains line up in opposite direction of magnetic field ...
                        	... MAGNETIC FIELD Some of our most important evidence of sea-floor spreading comes from magnetic reversals recorded on the ocean floor The magnetic poles can change place (called magnetic reversal) Magnetic mineral grains line up in opposite direction of magnetic field ...
									the geology of the moon
									
... are also mostly broad and flat and some have central peaks. A high proportion of the near side and most of the far side are covered with millions of craters. Most that have been named are after eminent scientists, philosophers and historical figures. On the near side there are about 30,000 craters l ...
                        	... are also mostly broad and flat and some have central peaks. A high proportion of the near side and most of the far side are covered with millions of craters. Most that have been named are after eminent scientists, philosophers and historical figures. On the near side there are about 30,000 craters l ...
									NOTES: IGNEOUS ROCKS
									
...  High temps may cause partial melting and re-crystallization  A “baked” zone is present along the edge of an igneous intrusion. This will contain contact metamorphosed rocks ...
                        	...  High temps may cause partial melting and re-crystallization  A “baked” zone is present along the edge of an igneous intrusion. This will contain contact metamorphosed rocks ...
									8. Earth`s Moving Plates
									
... Cracks in the Earth's Crust The solid crust acts as a heat insulator for the hot interior of the earth. Below the crust, in the mantle, is the molten material called magma. Tremendous heat and pressure within the earth cause the hot magma to flow in convection currents. Periodically it rises to the ...
                        	... Cracks in the Earth's Crust The solid crust acts as a heat insulator for the hot interior of the earth. Below the crust, in the mantle, is the molten material called magma. Tremendous heat and pressure within the earth cause the hot magma to flow in convection currents. Periodically it rises to the ...
									Earth Science
									
... Prepare “Earth putty” by mixing honey, water and powdered milk in a 1:1:10 ratio by volume. If it is too crumbly, add more water. If it is too wet, add more powdered milk. Take one heaping tablespoon of “Earth putty”. Form it into a ball. Use your thumb to make a deep indentation into the ball. Half ...
                        	... Prepare “Earth putty” by mixing honey, water and powdered milk in a 1:1:10 ratio by volume. If it is too crumbly, add more water. If it is too wet, add more powdered milk. Take one heaping tablespoon of “Earth putty”. Form it into a ball. Use your thumb to make a deep indentation into the ball. Half ...
									Geology ppt
									
... • 2000: Collapse of a dam retaining a cyanide leach pond • Impact on organisms and the environment ...
                        	... • 2000: Collapse of a dam retaining a cyanide leach pond • Impact on organisms and the environment ...
									Plate Tectonics Review Key
									
... 25. What is the ‘conveyor belt’ for the lithospheric plates? Convection currents which are located in the upper mantle. 26. What is the asthenosphere? It is the ‘plastic-like’ layer in the upper mantle. The lithospheric plates ride atop the asthenosphere. 27. Refer to your plate tectonics map. Which ...
                        	... 25. What is the ‘conveyor belt’ for the lithospheric plates? Convection currents which are located in the upper mantle. 26. What is the asthenosphere? It is the ‘plastic-like’ layer in the upper mantle. The lithospheric plates ride atop the asthenosphere. 27. Refer to your plate tectonics map. Which ...
									The Rock Cycle - Science A 2 Z
									
... Basalt is the most common type of extrusive igneous rock and the most common rock type at the Earth's surface. ...
                        	... Basalt is the most common type of extrusive igneous rock and the most common rock type at the Earth's surface. ...
									Module Title: Code: Level: Credits:
									
... 4. Explain the generation of hydrocarbons within sedimentary basins, use simple exploration techniques, and compare technologies for hydrocarbon exploration and extraction; 5. Describe the roles of glacial, fluvial, hill slope, coastal and submarine processes in forming the natural environment, and ...
                        	... 4. Explain the generation of hydrocarbons within sedimentary basins, use simple exploration techniques, and compare technologies for hydrocarbon exploration and extraction; 5. Describe the roles of glacial, fluvial, hill slope, coastal and submarine processes in forming the natural environment, and ...
									of the same age is form in southern Africa, South America, India, and
									
... igneous rock is created, any magnetic minerals in that rock crystalize and align themselves within the Earth’s current magnetic field. This is important because if the continents had not moved, igneous rocks on every continent should point towards the current magnetic North Pole. However, this is no ...
                        	... igneous rock is created, any magnetic minerals in that rock crystalize and align themselves within the Earth’s current magnetic field. This is important because if the continents had not moved, igneous rocks on every continent should point towards the current magnetic North Pole. However, this is no ...
									Plate Tectonics
									
... three types of plate boundaries.  I will list and describe three causes of plate movement. ...
                        	... three types of plate boundaries.  I will list and describe three causes of plate movement. ...
									Structure of the upper mantle beneath the Alps and Apennines as
									
... continuing to the southwest into Sicily and merging into the Maghrebides of northwestern Africa. Alps and Apennines developed along opposite subductions, in an area characterized by strong variability of tectonic signatures. This variability, coupled to the incompleteness of ...
                        	... continuing to the southwest into Sicily and merging into the Maghrebides of northwestern Africa. Alps and Apennines developed along opposite subductions, in an area characterized by strong variability of tectonic signatures. This variability, coupled to the incompleteness of ...
									Continental-Drift-and-Seafloor-Spreading
									
... 3. Glossopteris- plant fossils found on different continents- Plant fossils 4. Tropical plant fossils that were found on an island in Artic Ocean! (Scratches in rocks made by glaciers in South Africa) The continental drift theory was NOT accepted because Wegener could not explain HOW the continents ...
                        	... 3. Glossopteris- plant fossils found on different continents- Plant fossils 4. Tropical plant fossils that were found on an island in Artic Ocean! (Scratches in rocks made by glaciers in South Africa) The continental drift theory was NOT accepted because Wegener could not explain HOW the continents ...
									Seismological Analysis and the Effect of Earthquakes in the New
									
... a larger area than those on the West coast, since these conditions allow seismic waves to travel further, but they do so with less force. Seismic wave velocities are also related to the type of rock, the temperature, and the pressure conditions under which they occur (Weidner 1999). Studies of earth ...
                        	... a larger area than those on the West coast, since these conditions allow seismic waves to travel further, but they do so with less force. Seismic wave velocities are also related to the type of rock, the temperature, and the pressure conditions under which they occur (Weidner 1999). Studies of earth ...
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.