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Visualizing Earth Science
Visualizing Earth Science

... • Explain the connection between earthquakes and plate tectonics. • Identify several earthquake-related hazards. • Define body waves and surface waves. • Explain how the materials in Earth’s interior affect seismic waves. • Define and describe the composition of Earth’s crust, mantle and core. ...
Plate Tectonics Vocabulary Terms
Plate Tectonics Vocabulary Terms

... fragments of lithosphere move toward one another and collide. As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries ...
Earthquakes
Earthquakes

...  They speed up or slow down or are refracted (bent), depending on what layer they are travelling through ...
Name____________________________
Name____________________________

... Latitude: Measurement in degrees north or south (of equator). Hemisphere: One-half of a sphere (N-hemi, S-hemi). Equator: Line that divides N-hemi and S-hemi (longest parallel). Rheology: The study of the deformation and flow of matter. Convection: Transfer of heat within a liquid or gas. Conduction ...
1 REVIEW Exam #2. GG101 Below are some example questions to
1 REVIEW Exam #2. GG101 Below are some example questions to

... 4) What are the three types of magma produced by volcanoes? 5) How does magma style influence the type of volcanic eruption? 6) What are the three primary types of mountain systems? 7) Draw seismic waves in Earths interior and clearly label all components 8) Using the crustal cross-section in the fo ...
12.2 Note Outline
12.2 Note Outline

... Earth is composed of layers, including the lithosphere (surface) and asthenosphere (just below the surface) The asthenosphere is partly molten, and allows the tectonic plates of the lithosphere to “float” on the convection currents of hot magma. When tectonic plates meet (converge), one plate may sl ...
12.2 Note Outline key.jnt
12.2 Note Outline key.jnt

... Earth is composed of layers, including the lithosphere (surface) and asthenosphere (just below the surface) The asthenosphere is partly molten, and allows the tectonic plates of the lithosphere to “float” on the convection currents of hot magma. When tectonic plates meet (converge), one plate may sl ...
Section 20.1 - CPO Science
Section 20.1 - CPO Science

...  A moving line of grocery carts is a good analogy of a moving lithospheric plate.  Although a plate may be moving as a single unit, its boundaries act like they were made of many small sections like the line of carts. ...
EARTHQUAKES
EARTHQUAKES

... discovered in about 1910. From the lack of S waves and a great slowing of the P wave velocity (by about 40%) it was deduced that the outer core is made of liquid. The shadow zone also defined the diameter of the core. ...
Plate Tectonics
Plate Tectonics

... plates  Fit together  Difference ...
Earthquakes PPT
Earthquakes PPT

... A FAULT is a BREAK in the Earth’s CRUST. Most Earthquakes occur along FAULT LINES. **Not all cracks in rocks are faults. A FAULT IS DEFINED BY THE MOVEMENT OF ROCK OCCURINGON EITHER SIDE. When the MOVEMENT is SUDDEN, the ENERGY released causes an EARTHQUAKE. ...
Vocab-Chapter 7 - Wachter Middle School
Vocab-Chapter 7 - Wachter Middle School

... ____________________________ 3. The theory that the Earth’s lithosphere is divided into tectonic plates that move around on top of the asthenosphere. ____________________________ 4. The amount of force per unit area that is put on a given material. ____________________________ 5. The bending of rock ...
Powerpoint
Powerpoint

... tectonic plates. They are like broken ice fragments that float on the surface of water. Any sudden shifting of the tectonic plates results in earthquakes. The tectonic plates may slide past each other, push apart, or collide together. The interactions at the plate boundaries are important to conside ...
Earth`s interio
Earth`s interio

... – P waves travel + 6 Km/Sec • “Moho” (Mohorovicic Discontinuity) – Boundary between Crust and Mantle Mantle • P-wave velocity 8 Km/sec & higher • Made of ultramafic rock – Low in silica, high in Fe, Mg – Denser than basalt • Lithosphere – rigid uppermost part of mantle plus crust – tectonic plates – ...
geol_15_patton_fall_..
geol_15_patton_fall_..

... distance from the fault)? Where are some places that I discussed examples of earthquakes? What type of plate boundaries and what type of earthquakes were they (Denali 2002, San Francisco 1906, Aleutians 2013, Sea of Okhotsk, 2013, Pakistan 2013)? Where do earthquakes occur (related to depth of hypoc ...
Inside the Restless Earth
Inside the Restless Earth

... a. Tip of the iceberg -Differences between oceanic and continental crust are …………(discuss thickness and density) Continental crust stands higher than oceanic crust because it is thicker and less dense. Continental crust “floats” on the asthenosphere. ...
EGU2008-A-05921 - Copernicus Meetings
EGU2008-A-05921 - Copernicus Meetings

... also included, but these are derived from laboratory experiments. These properties are included to provide a reference database as a common standard of material properties necessary for performing realistic simulations of rock behaviour during geological and geodynamic processes. The model fits the ...
Chapter 6 – Plate Tectonics and Earthquakes
Chapter 6 – Plate Tectonics and Earthquakes

... 1. There are 7 major plates named after their associated continents, or surface features (Ex. North American plate, South American plate) ...
25.1 Notes
25.1 Notes

... EQ notes 25.2 Earthquake -A sudden movement or vibration of the ground that occurs when rocks slip or slide along cracks in the Earth - corresponds closely with plate boundaries -usually shallow EQ’s (70km or lower) occur at divergent boundaries -deep EQ’s (70km or more) occur at convergent boundari ...
GEOL 106 Earthquake Country Mid Term I Study
GEOL 106 Earthquake Country Mid Term I Study

... first, second, third, to arrive and why? What is refraction? What does the plot of the seismic wave velocity vs. depth into the earth tell us? What is the difference between earthquakes in California and Virginia? How can one locate an earthquake with seismologic data? How can one determine the magn ...
GEOL 106 Earthquake Country Mid Term I Study
GEOL 106 Earthquake Country Mid Term I Study

... is first, second, third, to arrive and why? What is refraction? What does the plot of the seismic wave velocity vs. depth into the earth tell us? What is the difference between earthquakes in California and Virginia? How can one locate an earthquake with seismologic data? How can one determine the m ...
Mid Term I - earthjay science
Mid Term I - earthjay science

Document
Document

... The asthenosphere can deform like stiff putty. ...
Earth`s Structures and Earthquake Study Guide
Earth`s Structures and Earthquake Study Guide

... 21. Evidence used to support the theory of continental drift included that the continents seem to fit together like pieces of a puzzle, there are similar fossils on different continents and mountain ranges in South America and Africa line up. 22. Scientists think that convection currents flow in Ear ...
REVIEW Earth`s Interior
REVIEW Earth`s Interior

... Use the following terms to label the diagram below. Then, use the terms to fill in the blanks in the sentences that follow. Terms may be used more than once. crust outer core mantle inner core mesosphere asthenosphere tectonic plate core lithosphere ...
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Earthscope



Earthscope is an earth science program using geological and geophysical techniques to explore the structure and evolution of the North American continent and to understand the processes controlling earthquakes and volcanoes. The project has three components: USARRAY, the Plate Boundary Observatory, and the San Andreas Fault Observatory at Depth.The project is funded by the National Science Foundation (NSF), and the data produced is publicly accessible in real-time. Organizations associated with the project include UNAVCO, the Incorporated Research Institutions for Seismology (IRIS), Stanford University, the United States Geological Survey (USGS) and National Aeronautics and Space Administration (NASA). Several international organizations also contribute to the initiative.
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