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Study Guide / Notes 11
Study Guide / Notes 11

... chemical analyses of meteorites. Since the abundance of elements are similar we assume the composition of the earth to be similar. Therefore, elements not in the earth's outer layers can be expected to occur in the interior. (see p. 228) ...
Earth Science Chapter 5
Earth Science Chapter 5

... • Early 1900s German Scientist Alfred Wegener made a hypothesis: • All of the continents were once joined together in a single land mass and have since drifted apart. ...
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Geology and Layers of the Earth notes

... densities increase with depth as pressures increase so waves travel differently ...
A history of supercontinents on planet Earth
A history of supercontinents on planet Earth

... breaking up just 60 million years later and giving way to Pangaea, last of Earth's supercontinents. For the time being, at least. Continents are still on the move, and they'll almost certainly continue to move until the Sun vaporizes our planet in five billion years' time. In all likelihood, the con ...
Chapter 1: Meet Planet Earth
Chapter 1: Meet Planet Earth

...  Plate tectonics is a group of processes by which large fragments (plates) of lithosphere move horizontally across the surface of the Earth. Through their movements and interactions, they generate: ...
Name__________________________________  pd________ Use the links to help you answer the questions.
Name__________________________________ pd________ Use the links to help you answer the questions.

... 4. Describe in your own words how the Earth's layers were formed. "The Four Layers" will help you. ...
Rocks and The Earth`s Interior
Rocks and The Earth`s Interior

...  Velocities of compressional waves are reduced and shear waves disappear ...
Seventh Grade Geography and Economics Pre/Post Quarter One
Seventh Grade Geography and Economics Pre/Post Quarter One

... d. Changes in the core temperature of Earth 9. Moving from the outer-most layer to the inner-most layer, what is the correct order of the layers of the Earth? a. crust, mantle, core b. mantle, core, crust c. core, mantle, crust d. crust, core, mantle 10. Large chunks of the Earth’s crust called plat ...
Lecture 6 - Rocks and The Earth`s Interior
Lecture 6 - Rocks and The Earth`s Interior

...  Velocities of compressional waves are reduced and shear waves disappear ...
rocks and the earth`s interior - FAU
rocks and the earth`s interior - FAU

...  Velocities of compressional waves are reduced and shear waves disappear ...
CRCT Review Warm Ups
CRCT Review Warm Ups

... Monday ~ April 13th  Earth’s ...
Earth Science Text Assignments
Earth Science Text Assignments

... 9. What do scientists record and study to learn about the interior from these events? Scientists study these seismic waves and the speed of them reveals the structure of the planet. 10. What characteristics of these events, specifically, do they rely on? Scientists rely on the speed of the waves. 11 ...
Directed Reading A
Directed Reading A

... 18. Why are tectonic plates like the pieces of a jigsaw puzzle? ...
5th Gr Earth Science Template Completed
5th Gr Earth Science Template Completed

... Understand the origin (where they’re found), utilization (how they’re used), and concerns (depletion, pollution, transportation) associated with natural resources ...
Usually rocks are formed by heat, pressure, or both. Which of these
Usually rocks are formed by heat, pressure, or both. Which of these

... C. Creating mountains and trenches on land and in the oceans D. Rearranging the order of the Earth’s ...
Unit 3earthmoon part 1
Unit 3earthmoon part 1

... a belt of high-energy particles around Earth: Van Allen belts ...
Earth`s Interior (What`s down there below us?)
Earth`s Interior (What`s down there below us?)

... The “lithosphere” is the crust + part of the upper mantle. It is made of rock and is brittle. The “plates” of the earth’s crust make up the lithosphere. Below the lithosphere is a softer layer called the “asthenosphere”. In the asthenosphere, The rock is near it’s melting point, and flows very slowl ...
The Dynamic Earth Section 1 Erosion
The Dynamic Earth Section 1 Erosion

... largest magnitude ever recorded is 9.5. Magnitudes greater than 7.0 cause widespread damage. • Each increase of magnitude by one whole number indicates the release of 30.0 times more energy than the whole number below it. ...
Just how integrated is the Earth System
Just how integrated is the Earth System

... As components of the biosphere, humans are temporary receptacles of the matter and energy that flows through the Earth System “You are what you eat, drink, and breathe” Human health is, to some degree, a function of how this flow of matter and energy flows through, and interacts with, the human body ...
Part 1: The Layers of Earth
Part 1: The Layers of Earth

... http://www.livephysics.com/simulations/mechanics-sim/dig-hole-earth/ ...
Chap 20 Earth and Comparative Planetology
Chap 20 Earth and Comparative Planetology

... of high-energy particles around Earth: Van Allen belts ...
Studyguide
Studyguide

... o The edge of the denser plate is forced into the __________________, while the less dense plate is pushed up o If the plates are the _______________ density, both plates are pushed up Earthquakes  An __________________________ is movement of the ground caused by a sudden release of energy in the E ...
Name
Name

... 18) Why are Jupiter-sized planets easier to discover around other stars than Earthsized planets using the Doppler method? A) Jupiter-sized planets have extensive ring systems B) Jupiter-sized planets eject material into their star C) The higher masses of Jupiter-sized planets tend to produce smaller ...
Name
Name

... 18) Why are Jupiter-sized planets easier to discover around other stars than Earthsized planets using the Doppler method? A) Jupiter-sized planets have extensive ring systems B) Jupiter-sized planets eject material into their star C) The higher masses of Jupiter-sized planets tend to produce smaller ...
Ecology
Ecology

...  Fossils are commonly found in these types of rocks  Erosion and weathering break up the Earth to form sediments Metamorphic Rocks are rocks that have changed from one form to another by heat, pressure, and/or chemical processes  Igneous to Metamorphic  Sedimentary to Metamorphic  Metamorphic t ...
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