Plate Tectonics - Cloudfront.net
... • Pacific Ocean is getting smaller and the Atlantic Ocean is getting wider due to seafloor spreading and subduction. ...
... • Pacific Ocean is getting smaller and the Atlantic Ocean is getting wider due to seafloor spreading and subduction. ...
Classifying Rocks
... Made of two or more different minerals that have been: • cemented together • squeezed and heated together • melted and cooled together. ...
... Made of two or more different minerals that have been: • cemented together • squeezed and heated together • melted and cooled together. ...
D o e I
... In geodesy, the size and shape of Earth’s surface can be mapped through a network of accurately surveyed points of geographic position using longitude, latitude and elevation, while taking into account the curvature of the earth through precise mathematical calculations. Developments over the last s ...
... In geodesy, the size and shape of Earth’s surface can be mapped through a network of accurately surveyed points of geographic position using longitude, latitude and elevation, while taking into account the curvature of the earth through precise mathematical calculations. Developments over the last s ...
File
... liquids, and gases. They cause slight vibrations (compression) that would rattle dishes on shelves, which provides a warning to people of the earthquake movement to come. Secondary (S) Waves - travel more slowly than P waves and can pass only through solids. Surface Waves - slowest of the three, but ...
... liquids, and gases. They cause slight vibrations (compression) that would rattle dishes on shelves, which provides a warning to people of the earthquake movement to come. Secondary (S) Waves - travel more slowly than P waves and can pass only through solids. Surface Waves - slowest of the three, but ...
Convection Model - Ocean First Education
... density increases. It sinks down toward where it was first heated and the process begins again. The circular movement up and down and back up again, over and over, is called a convection cell. Thi ...
... density increases. It sinks down toward where it was first heated and the process begins again. The circular movement up and down and back up again, over and over, is called a convection cell. Thi ...
3-D Earth Structure Model
... of no significant openings that would provide access to the deep interior of the planet, and caves or cavities at great depth are nearly impossible based on our knowledge of temperature and pressure within the Earth and the properties of Earth materials. However, Verne’s story is an interesting one ...
... of no significant openings that would provide access to the deep interior of the planet, and caves or cavities at great depth are nearly impossible based on our knowledge of temperature and pressure within the Earth and the properties of Earth materials. However, Verne’s story is an interesting one ...
To demonstrate how Young Fold Mountains are
... Fig. 6: Mark the wrinkling created by the ‘push’ of your fingers. This represents folding of the SIAL, SIMA, and also a bit of the Mantle. ...
... Fig. 6: Mark the wrinkling created by the ‘push’ of your fingers. This represents folding of the SIAL, SIMA, and also a bit of the Mantle. ...
Plate Tectonics
... At Mid-Ocean Ridges new oceanic crust is continuously built in the form of Sheeted Dikes und Pillow Lava. The upper part of the magma chamber solidifies as Gabbro. The Mohorovičič-Discontinuity (short form: Moho) is the boundary between crust and ...
... At Mid-Ocean Ridges new oceanic crust is continuously built in the form of Sheeted Dikes und Pillow Lava. The upper part of the magma chamber solidifies as Gabbro. The Mohorovičič-Discontinuity (short form: Moho) is the boundary between crust and ...
Grade 10 Informational Mini-Assessment
... spreading center, a ridge, to a subduction zone, a trench. Friction between the lithosphere and the underlying asthenosphere acts like glue, and the lithospheric plates are dragged along by the motion of the asthenosphere. To envision how Earth’s rocky mantle could flow almost like a fluid, think of ...
... spreading center, a ridge, to a subduction zone, a trench. Friction between the lithosphere and the underlying asthenosphere acts like glue, and the lithospheric plates are dragged along by the motion of the asthenosphere. To envision how Earth’s rocky mantle could flow almost like a fluid, think of ...
Chapter 13 Exploring the Oceans
... decreases with depth Deep zone—coldest Ocean as a Thermostat ...
... decreases with depth Deep zone—coldest Ocean as a Thermostat ...
Ch._19
... Seismic belts are relatively narrow and tend to follow tectonic plate boundaries. 1. True 2. False ...
... Seismic belts are relatively narrow and tend to follow tectonic plate boundaries. 1. True 2. False ...
Unit 1: Review of Science and Math Skills
... 1) Recognize the evidence for the theory of plate tectonics. 2) Be able to explain the occurrence of most major geographic features such as mountain ranges, island arcs, deep sea trenches, mid- ocean ridges, and hot spots using the theory of plate tectonics. 3) Understand the mechanisms that drive p ...
... 1) Recognize the evidence for the theory of plate tectonics. 2) Be able to explain the occurrence of most major geographic features such as mountain ranges, island arcs, deep sea trenches, mid- ocean ridges, and hot spots using the theory of plate tectonics. 3) Understand the mechanisms that drive p ...
DP - quakes
... Encourage participants to develop their own PowerPoint presentations as a way to prepare for this event. Suggest that participants first enter the event topics into their PowerPoint presentations similar to an outline. As participants search the web for specific topics they will frequently fin ...
... Encourage participants to develop their own PowerPoint presentations as a way to prepare for this event. Suggest that participants first enter the event topics into their PowerPoint presentations similar to an outline. As participants search the web for specific topics they will frequently fin ...
Dynamic Planet power point 2017
... Encourage participants to develop their own PowerPoint presentations as a way to prepare for this event. Suggest that participants first enter the event topics into their PowerPoint presentations similar to an outline. As participants search the web for specific topics they will frequently fin ...
... Encourage participants to develop their own PowerPoint presentations as a way to prepare for this event. Suggest that participants first enter the event topics into their PowerPoint presentations similar to an outline. As participants search the web for specific topics they will frequently fin ...
Flexural Isostatic Analysis of Loading (western U.S. example)
... refraction data and estimated mass variations for both crustal thickness variations and internal density variations • Note we need to know Te to turn mass variation (loading) into elevation! • Uncertainties reflect interpolation error, uncertainties in seismic velocity structure, errors in regressio ...
... refraction data and estimated mass variations for both crustal thickness variations and internal density variations • Note we need to know Te to turn mass variation (loading) into elevation! • Uncertainties reflect interpolation error, uncertainties in seismic velocity structure, errors in regressio ...
Review Test 2 - Course World
... Tectonic plates, sometimes called lithospheric plates, are large, irregularly shaped slabs of oceanic and/or continental crust. Much like a flagstone sidewalk, plates come in many sizes. The largest plates, the Pacific and Antarctic Plate, measure thousands of miles across. Smaller plates, such as t ...
... Tectonic plates, sometimes called lithospheric plates, are large, irregularly shaped slabs of oceanic and/or continental crust. Much like a flagstone sidewalk, plates come in many sizes. The largest plates, the Pacific and Antarctic Plate, measure thousands of miles across. Smaller plates, such as t ...
Crustal Deformation
... How Geologists Use These Clues • We can mentally fill out the sketch to get an idea of the shape of the fold. • Note that we still have no idea how big the fold is, only what kind it is. 3. Small structures provide clues to much larger structures ...
... How Geologists Use These Clues • We can mentally fill out the sketch to get an idea of the shape of the fold. • Note that we still have no idea how big the fold is, only what kind it is. 3. Small structures provide clues to much larger structures ...
First Exam - Practice Test
... d. andesite and diorite. e. All of the above Plutons are a. magma bodies within the deep crust. b. intrusive igneous rocks in the lower mantle. c. magma bodies produced by volcanism. d. igneous rocks produced by fissure eruptions. e. made by contact metamorphism Plate tectonics is important to igneo ...
... d. andesite and diorite. e. All of the above Plutons are a. magma bodies within the deep crust. b. intrusive igneous rocks in the lower mantle. c. magma bodies produced by volcanism. d. igneous rocks produced by fissure eruptions. e. made by contact metamorphism Plate tectonics is important to igneo ...
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.