Diapositiva 1 - Zanichelli online per la scuola
									
... Endogenous processes occur inside Earth and generate the ocean floors and continents. ...
                        	... Endogenous processes occur inside Earth and generate the ocean floors and continents. ...
									Causes and effects of Earthquakes| sample answer
									
... The earth’s crust is broken into slabs, they are called plates. These plates are constantly moving because of convectional currents in the mantle (asthenosphere). There movements cause earthquakes. Earthquake are vibrations in the earth’s crust that occur when strain in the crust is suddenly release ...
                        	... The earth’s crust is broken into slabs, they are called plates. These plates are constantly moving because of convectional currents in the mantle (asthenosphere). There movements cause earthquakes. Earthquake are vibrations in the earth’s crust that occur when strain in the crust is suddenly release ...
									Unit 1.4 Earthquakes
									
... Where do earthquakes Occur? • Earthquakes can occur near the Earth’s surface or far below the surface. • Most earthquakes occur at plate boundaries, but some happen at faults located in the middle of tectonic plates. ...
                        	... Where do earthquakes Occur? • Earthquakes can occur near the Earth’s surface or far below the surface. • Most earthquakes occur at plate boundaries, but some happen at faults located in the middle of tectonic plates. ...
									P-2, Advanced Proficiency, 6th Grade, Earth Science
									
... volcanoes, and midocean ridges; and the distribution of fossils, rock types, and ancient climatic zones. (1) 1c - Students know lithospheric plates the size of continents and oceans move at rates of centimeters per year in response to movements in the mantle. (1) 1e - Students know major geologic ev ...
                        	... volcanoes, and midocean ridges; and the distribution of fossils, rock types, and ancient climatic zones. (1) 1c - Students know lithospheric plates the size of continents and oceans move at rates of centimeters per year in response to movements in the mantle. (1) 1e - Students know major geologic ev ...
									• Haiti is on a transform boundary between the Caribbean and North
									
...  Sewage pipes were damaged leading to some water being contaminated. This made 28 people ill.  The biggest aftershock measured 6.3 on the Richter Scale.  It cost the New Zealand economy around $4 billion ...
                        	...  Sewage pipes were damaged leading to some water being contaminated. This made 28 people ill.  The biggest aftershock measured 6.3 on the Richter Scale.  It cost the New Zealand economy around $4 billion ...
									chapter 1 - Solution Manuals
									
... dense, dark rock, which in some places can flow. The crust is solid, rigid rock. The density decreases from the core to the mantle and crust. 14. Uniformitarianism states that the natural processes operating in today’s world are the same processes, with the same underlying physical principles, that ...
                        	... dense, dark rock, which in some places can flow. The crust is solid, rigid rock. The density decreases from the core to the mantle and crust. 14. Uniformitarianism states that the natural processes operating in today’s world are the same processes, with the same underlying physical principles, that ...
									Powerpoint
									
... around the Sun, (b) has sufficient mass for its selfgravity to overcome rigid body forces so that it assumes a hydrostatic equilibrium (nearly round) shape, and (c) has cleared the neighbourhood around its orbit. (2) A “dwarf planet” is a celestial body that (a) is in orbit around the Sun, (b) has s ...
                        	... around the Sun, (b) has sufficient mass for its selfgravity to overcome rigid body forces so that it assumes a hydrostatic equilibrium (nearly round) shape, and (c) has cleared the neighbourhood around its orbit. (2) A “dwarf planet” is a celestial body that (a) is in orbit around the Sun, (b) has s ...
									Climate - Humble ISD
									
... Not all human alteration have been positive. We have caused deforestation, over farmed the land, and polluted the environment. ...
                        	... Not all human alteration have been positive. We have caused deforestation, over farmed the land, and polluted the environment. ...
									Happy Lesson
									
... 5. What happens when these plates move? • [A] They can collide. (correct answer) • [B] They can move apart. (correct answer) • [C] They can slide past each other. (correct answer) • [D] They can combine to form one plate ...
                        	... 5. What happens when these plates move? • [A] They can collide. (correct answer) • [B] They can move apart. (correct answer) • [C] They can slide past each other. (correct answer) • [D] They can combine to form one plate ...
									File
									
... show HOW the plates move. • Back then, we had no GPS (global position satellites) nor did we know much about atomic radiation nor CONVECTION! ...
                        	... show HOW the plates move. • Back then, we had no GPS (global position satellites) nor did we know much about atomic radiation nor CONVECTION! ...
									Earth`s Moving Plates
									
... when compared to the outer layers, though its thickness does vary. It is thinnest under the oceans and thickest through the continents. ...
                        	... when compared to the outer layers, though its thickness does vary. It is thinnest under the oceans and thickest through the continents. ...
									Chapter 21 - Bemidji State University
									
... d. Trac..s<.fossils - imprint by a moving animal including footprints, burrowing and etc. II. Relative Geological Time - Geological events are recorded in the rocks and are placed in chronological order without regard for the actual dates. A. Superposition - in a sequence of undisturbed sedimentary ...
                        	... d. Trac..s<.fossils - imprint by a moving animal including footprints, burrowing and etc. II. Relative Geological Time - Geological events are recorded in the rocks and are placed in chronological order without regard for the actual dates. A. Superposition - in a sequence of undisturbed sedimentary ...
									Land Formations - Library Video Company
									
... mantle of the Earth. At this point, the mantle is not covered by any crust. 2. Prepare your mid-ocean ridge and your two deep trenches. Using the scissors, carefully cut a slit vertically in the side of the oatmeal carton that’s about 12 centimeters, or five inches, long. This slit represents your m ...
                        	... mantle of the Earth. At this point, the mantle is not covered by any crust. 2. Prepare your mid-ocean ridge and your two deep trenches. Using the scissors, carefully cut a slit vertically in the side of the oatmeal carton that’s about 12 centimeters, or five inches, long. This slit represents your m ...
									Plate Boundaries
									
... 100 km thick, although its thickness is age dependent (older lithosphere is thicker).The lithosphere below the crust is brittle enough at some locations to produce earthquakes by faulting, such as within a subducted oceanic plate. Locked fault—a fault that is not slipping because frictional resistan ...
                        	... 100 km thick, although its thickness is age dependent (older lithosphere is thicker).The lithosphere below the crust is brittle enough at some locations to produce earthquakes by faulting, such as within a subducted oceanic plate. Locked fault—a fault that is not slipping because frictional resistan ...
									Word format
									
... A. rocks on one side of the ridge have the opposite magnetic polarity to the other side B. Earth’s magnetic field reverses about every half million years C. older oceanic crust is slowly pushed away from ridge D. continents plow through the oceanic crust E. all of the above 23. The oldest oceanic cr ...
                        	... A. rocks on one side of the ridge have the opposite magnetic polarity to the other side B. Earth’s magnetic field reverses about every half million years C. older oceanic crust is slowly pushed away from ridge D. continents plow through the oceanic crust E. all of the above 23. The oldest oceanic cr ...
									Chapter 34: The Changing Face of the Earth
									
... itself abrade the land but it also carries embedded rocks of all sizes, and thus acts very much like sandpaper. Valley glaciers gouge and scoop out the valleys they occupy, modifying them into U-shaped troughs. The topography between adjacent glaciated valleys is often angular and sharp. Continental ...
                        	... itself abrade the land but it also carries embedded rocks of all sizes, and thus acts very much like sandpaper. Valley glaciers gouge and scoop out the valleys they occupy, modifying them into U-shaped troughs. The topography between adjacent glaciated valleys is often angular and sharp. Continental ...
									When drilling stopped in 1994, the hole was over seven miles deep
									
... scientist was heard to comment, “Every time we drill a hole we find the unexpected. That’s exciting, but disturbing.” To the surprise of the researchers, they did not find the expected transition from granite to basalt at 3-6 kilometers beneath the surface. Data had long shown that seismic waves tra ...
                        	... scientist was heard to comment, “Every time we drill a hole we find the unexpected. That’s exciting, but disturbing.” To the surprise of the researchers, they did not find the expected transition from granite to basalt at 3-6 kilometers beneath the surface. Data had long shown that seismic waves tra ...
									Title
									
... Seamount chains trail away from oceanic plateaus and result from material behind and below the head of the rising plume material. Because the plumes are relatively fixed, and the overlying tectonic plates drift horizontally on the surface of the planet, the subsequent eruptions in the mountain chain ...
                        	... Seamount chains trail away from oceanic plateaus and result from material behind and below the head of the rising plume material. Because the plumes are relatively fixed, and the overlying tectonic plates drift horizontally on the surface of the planet, the subsequent eruptions in the mountain chain ...
									Rocks
									
... silt, clay, or other materials. The grains in this sample are mostly the feldspar and quartz minerals, which probably accumulated near the granite from which they were eroded. ...
                        	... silt, clay, or other materials. The grains in this sample are mostly the feldspar and quartz minerals, which probably accumulated near the granite from which they were eroded. ...
									notes
									
... silt, clay, or other materials. The grains in this sample are mostly the feldspar and quartz minerals, which probably accumulated near the granite from which they were eroded. ...
                        	... silt, clay, or other materials. The grains in this sample are mostly the feldspar and quartz minerals, which probably accumulated near the granite from which they were eroded. ...
									Growing and Shrinking Oceans
									
... the subducted crust gets pushed deeper and deeper below the Earth, it gets hotter and hotter and eventually melts back into magma. Due to the processes of seafloor spreading and subduction, which happen at the same time in different parts of the Earth, rock is constantly being both created and destr ...
                        	... the subducted crust gets pushed deeper and deeper below the Earth, it gets hotter and hotter and eventually melts back into magma. Due to the processes of seafloor spreading and subduction, which happen at the same time in different parts of the Earth, rock is constantly being both created and destr ...
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.