PPT-GY111 Physical Geology Deformation of the Earth’s Crust
Author : rodriguez | Published Date : 2023-09-26
Stress amp Strain Stress a force applied to an area Example tire pressure in psi Strain a change in original shape or volume produced by stress Elastic strain analogous
Presentation Embed Code
Download Presentation
Download Presentation The PPT/PDF document "GY111 Physical Geology Deformation of th..." is the property of its rightful owner. Permission is granted to download and print the materials on this website for personal, non-commercial use only, and to display it on your personal computer provided you do not modify the materials and that you retain all copyright notices contained in the materials. By downloading content from our website, you accept the terms of this agreement.
GY111 Physical Geology Deformation of the Earth’s Crust: Transcript
Stress amp Strain Stress a force applied to an area Example tire pressure in psi Strain a change in original shape or volume produced by stress Elastic strain analogous to a steel spring or rubber band. Liz LaRosa for use with my 5. th. Grade Science Class . http://www.middleschoolscience.com. 2009 . Earth’s Layers. The Earth's rocky outer crust solidified billions of years ago, soon after the Earth formed. . I. t . S. haped the World. b. y Josh . I. rving. What is Geology?. Geology is the study of rocks, gems, and minerals and the study of the structure of these materials. An important part is how they were formed and how they change over time.. UNIT 1. What is Geology. Geology is the study of Earth, including the materials that it is made of, the physical and chemical changes that take place on its surface and in its interior and the history of the planet and its life form. Lithosphere. Earth’s Systems (spheres) . Lithosphere - . Earth’s crust and upper . mantle. Atmosphere - . Layers of gases surrounding . Earth . Lower Crust . and . Upper Mantle: Evidence . from . Rock Mechanics, Geodesy, and . Field Observations. Roland . Burgmann. . and Georg . Dresen. Key Purposes. Concerned . with describing material properties through constitutive equations that relate . How Rocks Deform. Deformation. . . = bending, tilting, or breaking Earth’s crust.. Isostasy. Deformation can be due to two opposing forces:. gravity, or weight, of the . lithosphere. pressing down on the . Solar System. Nebular Hypothesis. Nebular Hypothesis: Solar System was produced by the gravitational collapse of a gas cloud – the remnant of a supernova . explosion.. Concentration of heavy elements in inner . UNIT 1. What is Geology. Geology is the study of Earth, including the materials that it is made of, the physical and chemical changes that take place on its surface and in its interior and the history of the planet and its life form. https://. www.youtube.com/watch?v=rQx2wLyagk4. . Essential Question:. How are layers of the Earth different from one another?. Standard:. S6E5a. Compare and contrast the Earth’s crust, mantle, and core including temperature, density, and composition.. https://. www.youtube.com/watch?v=rQx2wLyagk4. . Essential Question:. How are layers of the Earth different from one another?. Standard:. S6E5a. Compare and contrast the Earth’s crust, mantle, and core including temperature, density, and composition.. Instructor: Dr. Scott T. Marshall. All . Science . is . Based . on . The Scientific Method. Today’s . Theme:. What is Geology?. The study of the Earth. Composition. Behavior. History. Geology is often called geoscience or Earth science. for engineers. Geology and Geophy. sics Department. King Saud University. Importance of Geology in Civil Engineering. Geology is the study of earth, the materials of which it is made, the structure of those materials and the effects of the natural forces acting upon them . Mount Erebus. Mount Erebus. to. McMurdo Station. 36 km. Planetary . Surfaces I. Planetary Surfaces. Why look at the surface?. 1. formation history (composition). 2. past geologic activity. 3. current geologic activity. Important Terms. Craton: interior of continents made of stable Precambrian and Paleozoic rocks.. Shield: portion of Craton composed of older Precambrian rocks.. Platform: portion of Craton made of younger relatively undeformed Paleozoic sediments..
Download Document
Here is the link to download the presentation.
"GY111 Physical Geology Deformation of the Earth’s Crust"The content belongs to its owner. You may download and print it for personal use, without modification, and keep all copyright notices. By downloading, you agree to these terms.
Related Documents