PPT-Integrating geologic maps with fault mechanics

John Singleton George Mason University NSF Cutting Edge Workshop 2012 Exercise overview Relate basic stress concepts and fault mechanics Andersonian theory MohrCoulomb failure frictional . Tips on how to integrate textual support smoothly into your own writing. 2. What works?. INEFFECTIVE. . Rodriguez writes, “My parents, who are no longer my parents in a cultural sense.” He expresses the alienation from his family that has resulted from his assimilation into English-speaking American culture.. Topographic Maps. Contouring. Topographic contours indicating surface relief. Image taken from US Army training manual.. Solid yellow lines represent surface isobars, line of equal air pressure. Green dashed lines are geopotential heights, the altitude at which 500 millibars of air pressure are attained. These types of contour maps are used by meteorologists. The weather system shown is the Storm of the Century, a powerful winter storm called a nor’easter.. Chapter 7 lesson 4. What is the geologic time scale?. Geologists use the geologic time scale to show Earth’s history.. It is a record of the geologic events and the evolution of life forms as shown by the fossil record.. In depth: chapter 19. Geologic Time Scale. Examining layers of sedimentary rock, scientists have put together a chronology of Earth’s history.. It is divided into 4 Eras:. 1. Precambrian (3.5 . bya. Geological “Clocks”. Geologic time determination is subdivided into 2 categories:. Relative Dating: simply determines whether or not an event occurs before or after another event (e.g. a granite dike is younger than the surrounding sandstone since it intrudes across the sandstone in an outcrop).. America. Dane S. VanDervoort. 1. , Chong Ma. 2. , Mark G. Steltenpohl. 2. , Joshua J. Schwartz. 3. 1. Geologic Investigations Program, Geological Survey of Alabama, Tuscaloosa, Alabama . 35486. 2. Department of Geosciences, Auburn University, Auburn, Alabama . a. Fossils. 3. Geologic Time Scale. 4. Geologic Belts. 5. NC Geologic History. How do we know . geologic . history. ?. Earth's History. Earth's history spans over a length of . 4.5 billion . years. Geologists have divided that time into units based on major geologic events and life forms. . Presenter: Alicia McGee. Email: . amcgee@mobilemcps.org. Make a copy of this to take notes!. Maps and Geography . We want students to become global students….. So….. Students should be able to:. Carlo Fabricatore is a computer scientist and game designer. He specializes in videogame development and the study of human-computer interactions in the area of digital games. He is the founder and CE Time: Wed. 1 – 3 pm 3 UNITS. COURSE OUTLINE. MODULE 1. Map reading and interpretation of structural features and geological history in simple geological maps.. . MODULE . 2. Practical recording of geological features on base maps.. Visualizing 3D Surfaces. Carol J. Ormand. , . SERC, Carleton College. Eric Riggs, Texas A&M University. Overview. What do we mean when we talk about “reading” contour maps?. Example: the Topographic Map Assessment. How to read a map. Maps . are pictures of the Earth's . surface. Reference maps . just . show natural features like rivers, cities, political subdivisions and highways. .. Thematic maps . use these items only . The oldest map?. Konya . town map, Turkey, c. 6200 BC. Milestones Project. http://www.math.yorku.ca/SCS/Gallery/milestone/. The First World Map. Anaximander of Miletus, Turkey, c. 550 BC. Milestones Project. The use of one’s body to produce motion that is safe, energy conserving, and anatomically and physiologically efficient and that leads to the maintenance of a person's body balance and control. Benefits of Proper Body Mechanics.