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Tectonic Plates
Tectonic Plates

... Pangea- A super continent that held all our modern continents. ...
Skinner Chapter 4
Skinner Chapter 4

... Read each question carefully before answering. Work at a steady pace, and you should have ample time to finish. _____________________________________________ 1. Rocks deep inside the Earth are so hot that it is possible for them to flow like sticky liquids. 2. Radiation is the process by which heat ...
Volcano PowerPoint
Volcano PowerPoint

... * most volcanoes on Earth are dormant (not active) *There are about 600 active volcanoes on Earth. ...
Mountain Formation
Mountain Formation

... is the longest mountain ...
lecture 01s - Kean University
lecture 01s - Kean University

... A star more than 9 times the mass of our sun burns faster, then expands into a red super giant star. Betelgeuse, for example. Pressure is high enough to also produce the heavier elements including silicon, magnesium, and iron. ...
Powerpoint Presentation Physical Geology, 10/e
Powerpoint Presentation Physical Geology, 10/e

... Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. ...
Document
Document

... earth’s crust consists of solid inorganic elements and compounds called minerals that can sometimes be used as resources. ...
Monday - Houston ISD
Monday - Houston ISD

... periodic table. Each student must write on an index card the element's ...
Continental Drift - The Cyberworld of Deepsea Dawn, Oregon
Continental Drift - The Cyberworld of Deepsea Dawn, Oregon

... century yet the validity of continental drift was not generally recognized until the late 1960’s”  It took ocean floor data to solidify ideas and convince scientific community!  The oceans rule! ...
THE OCEAN FLOOR
THE OCEAN FLOOR

Chapter 10: Section 1 Continental Drift
Chapter 10: Section 1 Continental Drift

... • Geologic evidence shows that ice once covered most of Earth’s continental surfaces. As continents began to drift around the globe, however, global temperatures changed and much of the ice sheet melted. • As continents rift or as mountains form, populations of organisms are separated. When populati ...
plate tectonics
plate tectonics

... Plate Tectonics- theory that Earth’s crust and upper mantle (lithoshphere) are broken into sections called plates that move on top of the asthenosphere. ...
The Earth`s Layers and Plate Tectonics Study Guide #1 Unit 3
The Earth`s Layers and Plate Tectonics Study Guide #1 Unit 3

... Site in which convection currents are found ...
and Wilson cycle tectonics
and Wilson cycle tectonics

... 12) Substutuing this integral into (11) we get an expression for the water depth : ...
File
File

... • These two split again to form the current continents ...
Chemical Elements
Chemical Elements

... Al2SiO5. Three different minerals have this same composition, but the coordination of oxygens around the Al in the structure is dependent upon the pressure and temperature conditions during formation. In fact, this change in crystal structure makes a very useful indicator of geologic conditions! Kya ...
mid-ocean ridge
mid-ocean ridge

... lithosphere is broken into large pieces called plates that are separated by cracks. Below the lithosphere, the material is hotter and under increasing pressure. As a result, the part of the mantle just beneath the lithosphere is less rigid than the rock above, although it is still solid. This softer ...
Evidence after wegener: seafloor spreading and
Evidence after wegener: seafloor spreading and

... • this proved that oceanic crust is created at different times, supporting seafloor spreading ...
Earth`s Crust in Motion
Earth`s Crust in Motion

File
File

... 19. Evidence suggests that Earth is about 4.6 billion years old, even though no Earth rocks have been found that can be dated at more than 4 billion years old. This discrepancy is most likely caused by earth’s original crust being a. Difficult to date so precisely b. Subject to extensive erosion c. ...
Chapter 11 Mountain Building 11.1 Rock Deformation Factors
Chapter 11 Mountain Building 11.1 Rock Deformation Factors

... Orogenesis is the collection of processes that result in the forming of mountains. Mountains that are formed primarily by folding are called folded mountains. A folded mountain is caused by extreme force pushing from both sides of the plates. This great pressure causes mountain to break, bend, and f ...
How accurately can we measure density within the Earth?
How accurately can we measure density within the Earth?

... • high spatial resolution • good absolute accuracy • determines boundaries • does not measure density directly • elastic properties correlated with density • more money –> better results ...
How thick is Continental crust?
How thick is Continental crust?

... on top to about 1600 degrees Fahrenheit in the deepest parts of the crust. You can bake a loaf of bread in your oven at 350 degrees F., at 1,600 degrees F. rocks begin to melt. ...
Chapter 18
Chapter 18

... • The core has been found to have 2 parts: 1. A liquid outer core 2. A solid inner core • The core makes up about 15% of the earth’s total volume and about 1/3 of its mass. • The core has been found to be mostly iron. This is believed because the magnetic field which is produced indicates that it is ...
Folds, Faults and Mountain Belts (Con`t.)
Folds, Faults and Mountain Belts (Con`t.)

... Produced metamorphic rocks found in the Alps, Himalaya, and Appalachian Mountains. Also produced the greatly eroded metamorphic rocks in the Great Lakes region. These rocks are exposed by uplift (faulting) and rapid erosion. The process doesn’t reverse itself. ...
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Geochemistry

Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans. The realm of geochemistry extends beyond the Earth, encompassing the entire Solar System and has made important contributions to the understanding of a number of processes including mantle convection, the formation of planets and the origins of granite and basalt.
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