PPT-Mantle

Transition Zone Discontinuities beneath the Contiguous United States Stephen S Gao and Kelly H Liu sgaomstedu httpwwwmstedusgao Missouri University of Science and Technology . MINERALS DOWN UNDER NATIONAL RESEARCH FLAGSHIP. Steve Barnes, . CSIRO Earth Science and Resource Engineering. GA Mineral Systems June . 2012. Fertility (as applied to magmas). Do particular kinds of magmas have a tendency to give rise to ore deposits?. Richard Carlson. CIDER, July 2012. Molecular Cloud, M16. NASA/ESA. Protoplanetary Disk,. Hubble Telescope. When did planetary chemical differentiation begin?. Before there were planets!. Not Everything was Volatilized!. Explore: p. 672 - 678. Learning Targets. I can use simple models to simulate the forces acting on tectonic plates.. I can compare directions of plate motions with locations of hot spots, spreading ridges, and trenches. O. h We Wonder . W. hat . Y. ou Are. By Alex . Hornby. , Ross Findlay, . Adam . Lewi. s. , . Libby Rose, David . Redpath. , . Megan . Roberts, Emma Reynolds.. Afar, Ethiopia. Afar is at a triple tectonic junction.. . Christian Garvey, James King and Charlie Mason. . (Simon Crosbie, Andrew Knott, George Lodwick, Ben Taylor, Jonathon Taylor) . Time history of volcanism . The Azores was onset with a flood basalt eruption, creating a 600Km wide plateau. . An Introduction to Ch 11&12. Regions of the Earth. The Earth is made up predominantly of two major regions:. A predominantly molten, central core. A mostly solid outer mantle and crust. Hydrosphere and Crust . Kevin Burgee. Teuthowenia. . pellucida. Phylum: Mollusca. Class: . Cephalopoda. Order: . Teuthida. Family: . Cranchiidae. Contains about 60 species of . squid. also known as cockatoo squid, . cranchiid. CHRISTIAN, JACK. , FRASER, BEN, JAMES M . &. JAM W. BACKGROUND. Located in the North Atlantic the Azores is an autonomous region of Portugal, 850 miles to the west.. The Azores lie at a triple junction between the Eurasian, North American and African Plate.. The Earth is divided into three layers based on the compounds that makeup each layer. They are:. 1. Crust. 2. Mantle. 3. Core. The Crust. The Crust is the :. 1. outer most layer of the Earth.. 2. It is the thinnest layer.. : mechanical . boundary . layer,. dry-mostly, stable . for 10. 8. -10. 9. a, possessing a steady-state conductive . geotherm. with base. in . cratons. at . 4-7 . GPa. (170–250 km. ), shallower (ca 100-150km) in off-. Mountain-Building Geology. Mountains Distant from Subducting Plate Boundaries. Mueller State Park. Version 2.0. October 8, 2015. North America. In moving west, the . North American Plate . slid over several ancient plates, pushing up the . ‘. assemble or gather together’. . Jews go to the Synagogue to . meet. together with other Jews, to . worship. God and . learn. more about their religion. . Look at the pictures that follow. . 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.. Garnero. 2007. McNamara & . Zhong. 2005. Mantle seismic heterogeneity as a function of depth. Romanowicz. , 2003. We expect a thermal boundary layer at the CMB. Lay et al., 2008. We expect denser mantle “dregs” to settle to the bottom.