PPT-Thermal evolution of an early magma ocean in interaction wi

T Lebrun 1 H Massol 1 E Chassefière 1 A Davaille 2 E Marcq 3 P Sarda 1 F Leblanc 3 G Brandeis 4 1 Univ ParisSud Laboratoire IDES UMR8148 Univ ParisSud CNRS Bât 504 Orsay F91405 France. Principal Types of Ocean Principal Types of Ocean Basins Basalt Basins Basalt Table 10 Table 10 Common petrographic differences between tholeiitic and alkaline Common petrographic differences between tholeiitic and alkaline basalts basalts Tholeiiti Chapter 5. Rigid Earth to Plate Tectonics. Learning Objectives. Know the different types of volcanoes and their associated features. Understand the relationship of the volcanoes to plate tectonics. Know what geographic regions are at risk from volcanoes. Dave Stevenson. Caltech. . CIDER, KITP, July 18. Estimating Processes. Timescales, Energies, Mixing, . Unmixing. , Equilibration. Why is Earth (probably ) completely molten after a giant impact?. But. Evolution of the Earth. Cracks in the Earth’s Crust. The . crust. , when it is solid, acts as a . heat insulator. for the hot interior of the Earth.. The molten material in the mantle, . magma. , below the crust builds up tremendous heat and pressure. . IMPLORE. I. M. P. L. O. R. E. ust. redict. ocate. rganize. ead. /reread. xplore. PREDICT. Before reading the passage. Underline the title. Highlight any information in the title that I know. If the title has words you are familiar with highlight those words in the title, and each time they appear in the passage. Chapter 6: Section 2. Before the video…. Get out a sheet of paper.. Write an example of each type of thermal energy transfer discussed in the video.. Bill Nye Clip. After the video. Draw a diagram of each type of thermal energy transfer that you listed from the video. Include the heat source, where it is going, and what it is heating up. . Earth Science Fall . 2012 . Vocabulary: . aa. – jagged chunks of lava formed by rapid cooling on the surface of the lava flow . Vocabulary:. Caldera- large basin-shaped depression formed when an explosion destroys the upper part of a volcanic cone or when the magma chamber below a volcano is emptied during an eruption. Steven Ackleson. , Consortium for Ocean . Leadership. Data Assimilation and Modeling; . Bob . Arnone. , University of Southern . Mississippi. Modern Observatory Operations; . Collin . Roesler. , Bowdoin . Youtube. :. Volcano Eruption – The Eruption of Mount St Helens 1980. 22 minutes. VOLCANOES. . Lithosphere. Side vent. Pipe. Central vent. Lava flows. Dike. Sill. Magma. chamber. Magma, which originates in the asthenosphere.... three-layer . Titan. Michael Bland and William McKinnon. ?. C/MR. 2. . . 0.34. = . 1879.8 kg m. -3. .  . Fortes, 2012. Jacobson, 2006. Iess. et al. 2010. Constraints on Titan’s internal structure. Physical and . Geo Content. Before the video…. Get out a sheet of paper.. Write an example of each type of thermal energy transfer discussed in the video.. Bill Nye Clip. After the video. Draw a diagram of each type of thermal energy transfer that you listed from the video. Include the heat source, where it is going, and what it is heating up. . Magma Oceans in the Inner Solar System Linda T. Elkins- Tanton Magma Oceans Planetecimals accreted first 1.5M.A. of Solar System 1694- Gottfried Wilhelm Leibniz : Suggested Earth began as a uniform liquid and differentiated as it cooled I don’t expect you to know this, but knowing . the order of the geological periods can help . you make sense of what we’ll be discussing.. What helped me was this little mnemonic.. Come Over Some Day, Might Play Poker. Three. For much of human history, knowledge of the ocean and its currents was not recorded for many reasons - most sailors could not write and information was passed orally.. European nations began systematic ocean explorations but kept information secret between the 15.