Chapter 13 Earthquakes and Earth`s Interior
... Similar to how whales, bats and other animals use sound to ‘echolocate’ prey, seismologists can use waves generated by earthquakes to tell them about the shape and composition of the Earth’s interior. Similar to sound waves, P and S-waves will change speed and direction as they go from one area of ...
... Similar to how whales, bats and other animals use sound to ‘echolocate’ prey, seismologists can use waves generated by earthquakes to tell them about the shape and composition of the Earth’s interior. Similar to sound waves, P and S-waves will change speed and direction as they go from one area of ...
Brainpop - Earthquakes
... _____ 7. Why are surface waves more destructive to buildings than the initial seismic wave in an earthquake? a. it creates more sustained motion on the surface b. it reaches the surface faster c. it reaches deeper below the surface d. it travels farther from the epicenter _____ 8. What is the name o ...
... _____ 7. Why are surface waves more destructive to buildings than the initial seismic wave in an earthquake? a. it creates more sustained motion on the surface b. it reaches the surface faster c. it reaches deeper below the surface d. it travels farther from the epicenter _____ 8. What is the name o ...
Answers to the study guide
... 18. What evidence was gathered to explain the movements of the continents? a. The age of the sea floor gets older as you move away from the mid ocean ridge at divergent boundaries. The age of the floor gets older at the same rate on either side of the mid-ocean ridge b. The temperature and density ...
... 18. What evidence was gathered to explain the movements of the continents? a. The age of the sea floor gets older as you move away from the mid ocean ridge at divergent boundaries. The age of the floor gets older at the same rate on either side of the mid-ocean ridge b. The temperature and density ...
“I Can” – Plate Tectonics Objectives – Learning Target Analysis
... terms of crust, mantle, inner and outer cores) and where the magnetic field of the Earth is generated - section 6.1 (also know how these items relate to the causes of convergent and divergent plate boundaries) E 3.2C Describe the differences between oceanic and continental crust (including density, ...
... terms of crust, mantle, inner and outer cores) and where the magnetic field of the Earth is generated - section 6.1 (also know how these items relate to the causes of convergent and divergent plate boundaries) E 3.2C Describe the differences between oceanic and continental crust (including density, ...
Classroom Teacher Preparation Earth Science 2: Intro to Tectonics
... Lesson Objectives – SWBAT (“Students Will Be Able To…”): th ...
... Lesson Objectives – SWBAT (“Students Will Be Able To…”): th ...
Isostatic Adjustments
... in the rocks along a break it is called fracture. • When rocks do move at a break it is called a fault. ...
... in the rocks along a break it is called fracture. • When rocks do move at a break it is called a fault. ...
Sea Floor Spreading
... The heat from Earth's interior is released to the surface as heat flow. Current models indicate that heat moves to the surface with magma in convective motion. Most of the heat is carried to regions of mid-ocean ridges. Heat flow measurements at ocean ridges can be 8X greater than other parts of Ear ...
... The heat from Earth's interior is released to the surface as heat flow. Current models indicate that heat moves to the surface with magma in convective motion. Most of the heat is carried to regions of mid-ocean ridges. Heat flow measurements at ocean ridges can be 8X greater than other parts of Ear ...
Theory of Plate Tectonics
... BONUS FACTS: 2900 km below earth’s surface (7,250 laps around 400 meter track) ...
... BONUS FACTS: 2900 km below earth’s surface (7,250 laps around 400 meter track) ...
chapter_17. ppt - Louisiana State University
... Continental Glacier • Aerial view of the eastern margin of the continental glacier covering most of Greenland • It is much smaller than the ones in Antarctica, ...
... Continental Glacier • Aerial view of the eastern margin of the continental glacier covering most of Greenland • It is much smaller than the ones in Antarctica, ...
Theory of Plate Tectonics
... BONUS FACTS: 2900 km below earth’s surface (7,250 laps around 400 meter track) ...
... BONUS FACTS: 2900 km below earth’s surface (7,250 laps around 400 meter track) ...
II. THE ROCK CYCLE Chapter 5: Earth Kinematics
... overwhelming. For example, in the 1970s-80s NASA would have discovered continental drift by accident as a systematic ‘drift error’ while trying to track orbiting satellites from ground stations. Likewise, in 15 years ranchers in Australia will notice that all their property lines marked with a comme ...
... overwhelming. For example, in the 1970s-80s NASA would have discovered continental drift by accident as a systematic ‘drift error’ while trying to track orbiting satellites from ground stations. Likewise, in 15 years ranchers in Australia will notice that all their property lines marked with a comme ...
Monitoring Earthquakes - Hicksville Public Schools / Homepage
... pen remaining stationary occurs due to a basic principle of physics, “every object resists any change to its motion”. ...
... pen remaining stationary occurs due to a basic principle of physics, “every object resists any change to its motion”. ...
Plate Tectonics and Mountain Building – Study Guide Plate
... 7. What kind of plate boundary occurs where two plates grind past each other without destroying or producing lithosphere? 8. A divergent boundary at two oceanic plates can result in a ____. 9. What type of boundary occurs where two plates move together, causing one plate to descend into the mantle b ...
... 7. What kind of plate boundary occurs where two plates grind past each other without destroying or producing lithosphere? 8. A divergent boundary at two oceanic plates can result in a ____. 9. What type of boundary occurs where two plates move together, causing one plate to descend into the mantle b ...
Chapter 17 - MrFuglestad
... Wegener proposed that all continents were once joined in supercontinent called Pangea. He was one of the first to propose that the continents are drifting on the Earth’s surface. ...
... Wegener proposed that all continents were once joined in supercontinent called Pangea. He was one of the first to propose that the continents are drifting on the Earth’s surface. ...
Powerpoint Presentation Physical Geology, 10th ed.
... – Plates slide past one another – Fault zones, earthquakes mark boundary – San Andreas fault in California ...
... – Plates slide past one another – Fault zones, earthquakes mark boundary – San Andreas fault in California ...
Michael
... Turpin, the USGS head scientist of earthquake studies. You have asked many questions which I will answer in the following of this letter. The most recent earthquakes are occurring at the edges of Plate Boundaries. Plate Boundaries are the edges of the earth’s tectonic plates. The earth’s Tectonic Pl ...
... Turpin, the USGS head scientist of earthquake studies. You have asked many questions which I will answer in the following of this letter. The most recent earthquakes are occurring at the edges of Plate Boundaries. Plate Boundaries are the edges of the earth’s tectonic plates. The earth’s Tectonic Pl ...
PESPTprogramIntroContDrift12-13
... continents? 2. The temperature of earth’s interior ________________(increases/decreases) toward earth’s center where it may exceed _______________. 3. As you go deeper temperature ______________ (increases/decreases) and pressure ____________. Together with composition, this determines which layers ...
... continents? 2. The temperature of earth’s interior ________________(increases/decreases) toward earth’s center where it may exceed _______________. 3. As you go deeper temperature ______________ (increases/decreases) and pressure ____________. Together with composition, this determines which layers ...
Part I. The Layers of Earth - www .alexandria .k12 .mn .us
... Use the following sites to help you understand the Earth’s interior-http://www.mnh.si.edu/earth/main_frames.html (Select the “Multi-Media Version” and then the “Plate Tectonics and Volcanoes” tab. Now, click on “Inner Earth” and read the Introduction (2 slides) and then click on words CRUST, MANTLE ...
... Use the following sites to help you understand the Earth’s interior-http://www.mnh.si.edu/earth/main_frames.html (Select the “Multi-Media Version” and then the “Plate Tectonics and Volcanoes” tab. Now, click on “Inner Earth” and read the Introduction (2 slides) and then click on words CRUST, MANTLE ...
Chapter 2: Earth*s Structure
... • Transport: to carry from one place to another; Rivers can transport debris from one place to another. ...
... • Transport: to carry from one place to another; Rivers can transport debris from one place to another. ...
Plate Tectonics Resource Page - Western Reserve Public Media
... conclusion that the continents were once joined. These plants and animals could have lived on the continents when the continents when they were connected. Then when the continents divided, animals and plants from one area were stuck in other areas. Scientists believe that the continents had moved an ...
... conclusion that the continents were once joined. These plants and animals could have lived on the continents when the continents when they were connected. Then when the continents divided, animals and plants from one area were stuck in other areas. Scientists believe that the continents had moved an ...
Plate tectonics 2 - PAMS
... The Theory of Plate Tectonics, which links continental drift and seafloor spreading, explains how the Earth has evolved over time. It helps to explain the formation, movement, collisions, and destruction of the Earth’s crust ...
... The Theory of Plate Tectonics, which links continental drift and seafloor spreading, explains how the Earth has evolved over time. It helps to explain the formation, movement, collisions, and destruction of the Earth’s crust ...
inner core - Denton ISD
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
Post-glacial rebound
Post-glacial rebound (sometimes called continental rebound) is the rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period, through a process known as isostatic depression. Post-glacial rebound and isostatic depression are different parts of a process known as either glacial isostasy, glacial isostatic adjustment, or glacioisostasy. Glacioisostasy is the solid Earth deformation associated with changes in ice mass distribution. The most obvious and direct affects of post-glacial rebound are readily apparent in northern Europe (especially Scotland, Estonia, Latvia, Fennoscandia, and northern Denmark), Siberia, Canada, the Great Lakes of Canada and the United States, the coastal region of the US state of Maine, parts of Patagonia, and Antarctica. However, through processes known as ocean siphoning and continental levering, the effects of post-glacial rebound on sea-level are felt globally far from the locations of current and former ice sheets.