 
									
								
									Monday 4/1 - cloudfront.net
									
... • Use the notes on Pg. 55 to answer the questions. 1. Where do most earthquakes occur? 2. The ______is the point in the crust where movement occurs first. 3. ______ waves can travel through the earth’s interior. 4. _______ waves move perpendicular to the motion of the wave. 5. _______ waves can move ...
                        	... • Use the notes on Pg. 55 to answer the questions. 1. Where do most earthquakes occur? 2. The ______is the point in the crust where movement occurs first. 3. ______ waves can travel through the earth’s interior. 4. _______ waves move perpendicular to the motion of the wave. 5. _______ waves can move ...
									The E.S.S Project - Laconia School District
									
... lithosphere. They float on the mantle and move at extremely slow rates. They move from convection. Convection is when something is hot it rises and then when it cools it will sink. When the mantle is moving from convection it pulls the lithosphere with it and that causes that plates to move. The pla ...
                        	... lithosphere. They float on the mantle and move at extremely slow rates. They move from convection. Convection is when something is hot it rises and then when it cools it will sink. When the mantle is moving from convection it pulls the lithosphere with it and that causes that plates to move. The pla ...
									Read Full Press Release
									
... • These defense systems and components will continue to rely on these foreign sources based on their life cycles and lack of effective substitutes; and • In anticipation of these identified supply risks, some defense contractors and government agencies have begun taking initial steps to limit this d ...
                        	... • These defense systems and components will continue to rely on these foreign sources based on their life cycles and lack of effective substitutes; and • In anticipation of these identified supply risks, some defense contractors and government agencies have begun taking initial steps to limit this d ...
									Landforms depend on types of crust that meet
									
... continental drift? continents • 2. climate clues: tropical plants were found in cold Antarctica & glacial deposits found in Africa • 3. rock clues: similar rock structures found on different continents • 4. Pangaea: continents fit together like puzzle pieces ...
                        	... continental drift? continents • 2. climate clues: tropical plants were found in cold Antarctica & glacial deposits found in Africa • 3. rock clues: similar rock structures found on different continents • 4. Pangaea: continents fit together like puzzle pieces ...
									Ch02%20outline
									
... ocean floor provides a method for determining plate motions • Both the direction and rate of seafloor spreading can be established ...
                        	... ocean floor provides a method for determining plate motions • Both the direction and rate of seafloor spreading can be established ...
									Slide 1 - Cloudfront.net
									
... – Logarithmic scale: for each increase of 1 point, the earthquake is 10 times stronger  A 5.0 earthquake is 10x stronger than a 4.0  A 8.0 earthquake is 100x stronger than a 6.0 ...
                        	... – Logarithmic scale: for each increase of 1 point, the earthquake is 10 times stronger  A 5.0 earthquake is 10x stronger than a 4.0  A 8.0 earthquake is 100x stronger than a 6.0 ...
									Notes - Plate Tectonics
									
... 4. Oceanic-Continental or Oceanic-Oceanic Convergent Boundary a subduction zone where one plate overrides and the other is forced down into the mantle a. lighter continental plate or oceanic plate overrides the denser oceanic plate b. oceanic plate edge is subducted down into the asthenosphere and ...
                        	... 4. Oceanic-Continental or Oceanic-Oceanic Convergent Boundary a subduction zone where one plate overrides and the other is forced down into the mantle a. lighter continental plate or oceanic plate overrides the denser oceanic plate b. oceanic plate edge is subducted down into the asthenosphere and ...
									the Exciting World of Earthquakes Part I
									
... volcanic eruption, or event by manmade explosions. Most destructive quakes, however, are caused by dislocations of the crust. The crust may first bend and then, when the stress exceeds the strength of the rocks, break and "snap" to a new position. In the process of breaking, vibrations called "seism ...
                        	... volcanic eruption, or event by manmade explosions. Most destructive quakes, however, are caused by dislocations of the crust. The crust may first bend and then, when the stress exceeds the strength of the rocks, break and "snap" to a new position. In the process of breaking, vibrations called "seism ...
									convection current demonstration
									
... toward the edges of the container. This cooling increases the density of the fluid and causes it to sink. The sinking fluid pushes the fluid below it back toward the center of the dish and the cycle begins again. o Add three pieces of balsa wood as shown in Figure 2 to the pan to demonstrate plate m ...
                        	... toward the edges of the container. This cooling increases the density of the fluid and causes it to sink. The sinking fluid pushes the fluid below it back toward the center of the dish and the cycle begins again. o Add three pieces of balsa wood as shown in Figure 2 to the pan to demonstrate plate m ...
									YOU Crazy Earth
									
... Well, it should seem obvious to you at this point… you don’t have to be a geologist to figure it out: the Earth is out of control! To better understand why this is so, let’s further analyze the Earth by heading to www.learner.org/interactives/dynamicearth/. You’ll know you’re where you need to be if ...
                        	... Well, it should seem obvious to you at this point… you don’t have to be a geologist to figure it out: the Earth is out of control! To better understand why this is so, let’s further analyze the Earth by heading to www.learner.org/interactives/dynamicearth/. You’ll know you’re where you need to be if ...
									Surfaces and features of the Earth 4th.notebook
									
... Plate tectonics is the theory that the Earth's crust is broken into huge plates that shift and move on the molten layers below the crust. Where two plates come together = fault zones Along these zones mountains, volcanoes, and earthquakes occur. ...
                        	... Plate tectonics is the theory that the Earth's crust is broken into huge plates that shift and move on the molten layers below the crust. Where two plates come together = fault zones Along these zones mountains, volcanoes, and earthquakes occur. ...
									Plate Tectonics - Cloudfront.net
									
... HOW? – Alfred Wegener proposed that the continents were moving on a more fluid layer under the crust that could possibly be moving due to internal heat . . . ...
                        	... HOW? – Alfred Wegener proposed that the continents were moving on a more fluid layer under the crust that could possibly be moving due to internal heat . . . ...
									Earthquakes
									
... • A type of seismic wave that compresses and expands the ground • The first wave to arrive at an earthquake http://daphne.meccahosting.com/~a0000e89/insideearth2.htm ...
                        	... • A type of seismic wave that compresses and expands the ground • The first wave to arrive at an earthquake http://daphne.meccahosting.com/~a0000e89/insideearth2.htm ...
									Passing Plates I
									
... Wegener developed this theory after noticing that the bulge of Brazil on the eastern coast of South America appeared to match up with the dent of the southwestern coast of Africa. From his observation he argued that the two continents were once together, but they drifted apart. He also believed that ...
                        	... Wegener developed this theory after noticing that the bulge of Brazil on the eastern coast of South America appeared to match up with the dent of the southwestern coast of Africa. From his observation he argued that the two continents were once together, but they drifted apart. He also believed that ...
									Changing Earth
									
... surface. If magma reaches a weak spot in Earth’s crust, a volcano will form. As more magma comes to the surface, the volcano erupts. Lava is magma that has reached the surface. Some eruptions are more violent than others. Sometimes the magma’s gases explode. Hot rocks, gases, and ash burst from the ...
                        	... surface. If magma reaches a weak spot in Earth’s crust, a volcano will form. As more magma comes to the surface, the volcano erupts. Lava is magma that has reached the surface. Some eruptions are more violent than others. Sometimes the magma’s gases explode. Hot rocks, gases, and ash burst from the ...
									Plate Tectonics - Open Earth Systems
									
...  At a transform fault boundary, plates grind past each other without destroying the lithosphere.  Transform faults • Most join two segments of a mid-ocean ridge. • At the time of formation, they roughly parallel the direction of plate movement. • They aid the movement of oceanic crustal material. ...
                        	...  At a transform fault boundary, plates grind past each other without destroying the lithosphere.  Transform faults • Most join two segments of a mid-ocean ridge. • At the time of formation, they roughly parallel the direction of plate movement. • They aid the movement of oceanic crustal material. ...
									platetectonics-1232003374497953-1 - RCPL
									
... diameter-was known by the ancient Greeks, but it was not until the turn of the 20th century that scientists determined that our planet is made up of three main layers: crust, mantle, and core. ...
                        	... diameter-was known by the ancient Greeks, but it was not until the turn of the 20th century that scientists determined that our planet is made up of three main layers: crust, mantle, and core. ...
									Going Their Separate Ways
									
... north (as measured by a compass) differs from the geographic north that corresponds to the planet’s axis of rotation. At present, the lines of force of the Earth’s magnetic field are arranged as shown in Figure 2; the present orientation of Earth’s magnetic field is referred to as normal polarity. I ...
                        	... north (as measured by a compass) differs from the geographic north that corresponds to the planet’s axis of rotation. At present, the lines of force of the Earth’s magnetic field are arranged as shown in Figure 2; the present orientation of Earth’s magnetic field is referred to as normal polarity. I ...
									Document
									
... Earthquakes: Vibrations (seismic waves) within Earth materials are produced by the rapid release of energy  Earth’s crust is in constant motion because of tectonic forces  Earth’s crust can store elastic energy  When forces exceed the elastic limits and structural strength of the rocks, the rocks ...
                        	... Earthquakes: Vibrations (seismic waves) within Earth materials are produced by the rapid release of energy  Earth’s crust is in constant motion because of tectonic forces  Earth’s crust can store elastic energy  When forces exceed the elastic limits and structural strength of the rocks, the rocks ...
									Document
									
... Earthquakes: Vibrations (seismic waves) within Earth materials are produced by the rapid release of energy  Earth’s crust is in constant motion because of tectonic forces  Earth’s crust can store elastic energy  When forces exceed the elastic limits and structural strength of the rocks, the rocks ...
                        	... Earthquakes: Vibrations (seismic waves) within Earth materials are produced by the rapid release of energy  Earth’s crust is in constant motion because of tectonic forces  Earth’s crust can store elastic energy  When forces exceed the elastic limits and structural strength of the rocks, the rocks ...
									Minerals, Rocks and Resources
									
... • Minerals can be tested by scratching the unknown mineral with the edge or point of other materials of known harness ...
                        	... • Minerals can be tested by scratching the unknown mineral with the edge or point of other materials of known harness ...
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.
 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									