Section Review
... 8. Explain how scientists know about the structure of the Earth’s interior. _______________________________________________________________ _______________________________________________________________ INTERPRETING GRAPHICS ...
... 8. Explain how scientists know about the structure of the Earth’s interior. _______________________________________________________________ _______________________________________________________________ INTERPRETING GRAPHICS ...
Inside the Restless Earth
... 12. For each of the boundaries diagramed above, explain what happens at each of these boundaries and give a real-world example of each one. ...
... 12. For each of the boundaries diagramed above, explain what happens at each of these boundaries and give a real-world example of each one. ...
Earth Science Concepts
... Plate Tectonics are a puzzle or plates that all apply pressure to each other in the earths lithosphere. Plate tectonics also describes the forming and movement of oceanic and continental plates A subduction zone is when two crustal plates collide forcing one of them to submerge into the m ...
... Plate Tectonics are a puzzle or plates that all apply pressure to each other in the earths lithosphere. Plate tectonics also describes the forming and movement of oceanic and continental plates A subduction zone is when two crustal plates collide forcing one of them to submerge into the m ...
Earthquake when the ground shakes suddenly and violently caused
... seismic wave,move through body of an object ...
... seismic wave,move through body of an object ...
NAME - Thomas C. Cario Middle School
... 23.) What happens to p-waves when they enter the liquid outer core? Bend and Slow down S-Waves? They don’t enter the Outer Core 24.) Which seismic waves are the fastest? Primary 25.) What is the name for the part of the Earth where no seismic waves are detected from a given earthquake? Shadow Zone 2 ...
... 23.) What happens to p-waves when they enter the liquid outer core? Bend and Slow down S-Waves? They don’t enter the Outer Core 24.) Which seismic waves are the fastest? Primary 25.) What is the name for the part of the Earth where no seismic waves are detected from a given earthquake? Shadow Zone 2 ...
Physics - WordPress.com
... 4.8 Explain why scientists find it difficult to predict earthquakes and tsunami waves even with available data © Pearson Education Ltd 2011. Copying permitted for purchasing institution only. This material is not copyright free. This document may have been altered from the original. ...
... 4.8 Explain why scientists find it difficult to predict earthquakes and tsunami waves even with available data © Pearson Education Ltd 2011. Copying permitted for purchasing institution only. This material is not copyright free. This document may have been altered from the original. ...
Earthquake Text Worksheet
... Name ________________________________________________ Period ______ Date _____________ ...
... Name ________________________________________________ Period ______ Date _____________ ...
The layers of the Crust
... Lithosphere is the relatively cool, rigid shell of the Earth that consists of the Crust and the upper 80 to 100 km of the Mantle (which adheres to the crust.) The Lithosphere is approximately 200 km thick (under continental crust) and breaks up into tectonic plates. The Lithosphere is the "plate" of ...
... Lithosphere is the relatively cool, rigid shell of the Earth that consists of the Crust and the upper 80 to 100 km of the Mantle (which adheres to the crust.) The Lithosphere is approximately 200 km thick (under continental crust) and breaks up into tectonic plates. The Lithosphere is the "plate" of ...
Plate Tectonics Review Guide 08-09
... b. plate carrying oceanic crust collides with a plate carrying continental crust ____________________ c. 2 plates carrying continental crust collide _______________________________________________ 2. What is the difference between a seismograph and a seismogram? 3. Explain, in detail, how plate tect ...
... b. plate carrying oceanic crust collides with a plate carrying continental crust ____________________ c. 2 plates carrying continental crust collide _______________________________________________ 2. What is the difference between a seismograph and a seismogram? 3. Explain, in detail, how plate tect ...
EES Chapter 8 and Plate Tectonics Review - Bennatti
... _____________________13. Older scale used to measure the energy released by earthquakes _____________________14. More accurate scale used to measure the energy released by earthquakes ______________________15. Seismic waves that move through the Earth but not through the outer core _________________ ...
... _____________________13. Older scale used to measure the energy released by earthquakes _____________________14. More accurate scale used to measure the energy released by earthquakes ______________________15. Seismic waves that move through the Earth but not through the outer core _________________ ...
key
... 1. 200 million years ago, all the continents were one called Pangaea. Evidence is continents fitting together, fossils of same organism on two different continents, similar mountain ranges on diff. continents. 2. Seismic waves tell us that the inside of the Earth is made up of layers. 3. Continental ...
... 1. 200 million years ago, all the continents were one called Pangaea. Evidence is continents fitting together, fossils of same organism on two different continents, similar mountain ranges on diff. continents. 2. Seismic waves tell us that the inside of the Earth is made up of layers. 3. Continental ...
Plate Tectonics Homework Packet
... - What Greek word does this name come from? 9. Earth’s crust must be moving for the continents to change. What might be causing the plates to move? ...
... - What Greek word does this name come from? 9. Earth’s crust must be moving for the continents to change. What might be causing the plates to move? ...
Earthquakes
... Elastic Rebound- the sudden return of elastically deformed rock to its original shape Seismic Waves- waves of energy that travel through the earth P-Waves- the fastest type of seismic waves S-Waves- the 2nd fastest type of seismic waves ...
... Elastic Rebound- the sudden return of elastically deformed rock to its original shape Seismic Waves- waves of energy that travel through the earth P-Waves- the fastest type of seismic waves S-Waves- the 2nd fastest type of seismic waves ...
Earthquake Notes
... Intraplate quakes occur far from plate edges and happen when stress builds up and the Earth's crust is stretched or squeezed together until it rips. ...
... Intraplate quakes occur far from plate edges and happen when stress builds up and the Earth's crust is stretched or squeezed together until it rips. ...
Vocabulary for Earth`s Structure and Note Cards Crust – the
... Core – the Earth’s layer that extends from below the mantle to the center of the Earth. Outer core – liquid part of the core, made of molten iron and nickel Inner core – solid part of the core, mostly made of solid iron and nickel Asthenosphere – a plastic layer of the mantle on which pieces of the ...
... Core – the Earth’s layer that extends from below the mantle to the center of the Earth. Outer core – liquid part of the core, made of molten iron and nickel Inner core – solid part of the core, mostly made of solid iron and nickel Asthenosphere – a plastic layer of the mantle on which pieces of the ...
Dynamic Earth Review Sheet
... Layers of the Earth o Be able to use the chart on page 10 to determine the different properties of the layers of the Earth. o Describe the major differences between continental and oceanic crust? ...
... Layers of the Earth o Be able to use the chart on page 10 to determine the different properties of the layers of the Earth. o Describe the major differences between continental and oceanic crust? ...
Earthquake Test Study Guide
... 1) What is the cause of earthquakes? 2) What is a fault? 3) Where is the focus of an earthquake? 4) Where is the epicenter of the earthquake? 5) Name the three types of earthquake waves. 6) Which seismic wave has a push-pull movement? 7) Which seismic wave has a wriggling side to side motion? 8) Whi ...
... 1) What is the cause of earthquakes? 2) What is a fault? 3) Where is the focus of an earthquake? 4) Where is the epicenter of the earthquake? 5) Name the three types of earthquake waves. 6) Which seismic wave has a push-pull movement? 7) Which seismic wave has a wriggling side to side motion? 8) Whi ...
Dynamic Earth Review Sheet Plate Tectonics Be able to use the
... Layers of the Earth o Be able to use the chart on page 10 to determine the different properties of the layers of the Earth. o Describe the major differences between continental and oceanic crust? ...
... Layers of the Earth o Be able to use the chart on page 10 to determine the different properties of the layers of the Earth. o Describe the major differences between continental and oceanic crust? ...
Plate Teconics Study Guide
... 4. Name four pieces of evidence that supports the theory of continental drift. 5. What provides us with knowledge about the interior of the earth? 6. What is evidence of sea-floor spreading? 7. What forces cause the earth’s plates to move? 8. Give an example of each type of tectonic plate boundary a ...
... 4. Name four pieces of evidence that supports the theory of continental drift. 5. What provides us with knowledge about the interior of the earth? 6. What is evidence of sea-floor spreading? 7. What forces cause the earth’s plates to move? 8. Give an example of each type of tectonic plate boundary a ...
Rising Plumes in Earth`s Mantle: Phantom or Real?
... that “it’s difficult to argue these things are real” in either P or S renditions. A fundamental problem, say many researchers, is a dearth of data. Everyone agrees that some finite-frequency technique is the way to go, but many argue that even it is being overwhelmed by the limited data available. M ...
... that “it’s difficult to argue these things are real” in either P or S renditions. A fundamental problem, say many researchers, is a dearth of data. Everyone agrees that some finite-frequency technique is the way to go, but many argue that even it is being overwhelmed by the limited data available. M ...
Snack-Tectonics Lab
... Make category headings for each section in bold and then use full sentences to answer each question. Purpose: What is the purpose of this lab? Background Information: Write 1-3 paragraphs about plate boundaries. You may use any source (internet, textbook book, etc.) but it MUST BE IN YOUR OWN WORDS! ...
... Make category headings for each section in bold and then use full sentences to answer each question. Purpose: What is the purpose of this lab? Background Information: Write 1-3 paragraphs about plate boundaries. You may use any source (internet, textbook book, etc.) but it MUST BE IN YOUR OWN WORDS! ...
Frederick Simons
... Geology 5640/6640 15 Feb 2017 Introduction to Seismology Last time: Seismology as Investigative Tool Deep-Earth investigations use earthquakes as sources, three-component broadband seismometers as receivers, and analysis tools include: • Normal modes • Precursors • Waveforms • Receiver Functions • T ...
... Geology 5640/6640 15 Feb 2017 Introduction to Seismology Last time: Seismology as Investigative Tool Deep-Earth investigations use earthquakes as sources, three-component broadband seismometers as receivers, and analysis tools include: • Normal modes • Precursors • Waveforms • Receiver Functions • T ...
Introduction to Plate Tectonics California Geology 20
... and has gained acceptance within the scientific community but has not yet been decisively proven. Or…… ...
... and has gained acceptance within the scientific community but has not yet been decisively proven. Or…… ...
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.