PPT-Composition of the Earth’s inner core from high pressure

sound velocity measurements of FeNiSi alloys S Dominijanni 1 C McCammon 1 E Ohtani 2 D Ikuta 2 T Sakamaki 2 T Ishii 1 SerenaDominijanniunibayreuthde 1 Bayerisches Geoinstitut University of Bayreuth Germany . 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!. (they are trivially simple, but they do give some interesting results if you ask the right questions). The Physical Principal – . Conservation of Mass. Bulk Silicate Earth . (the hypothetical homogeneous composition of the solid silicate Earth after core formation, but before any other differentiation process). The National Weather Service counts on two sources for information:. Radar. Weather Balloon. Data collected from the atmosphere. Data collected from the Earth’s surface . In order to forecast the weather, meteorologists make measurements of:. 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.. It’s going to be . a WILD RIDE!. Journey to the Center of the Earth. Imagine if you will…... You are a Geologist* and have been given the task of traveling to the center of the Earth. You have a specially designed Earthship that will take you to the core. Your Earthship, . GLY 4200 . Fall, . 2016. 2. Interior of the Earth. Earth’s interior is divided into zones, with differing properties and compositions. Since we live on the crust, it is the most studied. The core and mantle are very important in understanding the behavior of the earth. GLY 4200 . Fall. , . 2017. 2. Interior of the Earth. Earth’s interior is divided into zones, with differing properties and compositions. Since we live on the crust, it is the most studied. The core and mantle are very important in understanding the behavior of the earth. 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.. Weather Systems Unit. By the end of this class, you will be able to:. *Compare and contrast high and low pressure systems. *Identify areas of high and low pressure on a weather map. DO NOW: What’s in a letter?. 6th Grade 2015-2016. By: Katherine Pease. Objective: . Students will compare and contrast the different layers of the Earth to create a informative diagram.. TEK: 6.10 The student understands the structure of Earth, the rock cycle, and plate tectonics.. , physical properties, and thermal state of the core.  . Eiji. Ohtani,. Graduate . school of Science, Tohoku University, Sendai 980-8578, Japan . 1. Recent development of High Pressure . Experiments. 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!. (they are trivially simple, but they do give some interesting results if you ask the right questions). The Physical Principal – . Conservation of Mass. Bulk Silicate Earth . (the hypothetical homogeneous composition of the solid silicate Earth after core formation, but before any other differentiation process).