PPT-The Earth’s Layers

Density of rocks 1 Find the mass of each rock sample on the electric balance Record measurement in data table g 2Pour 50 mL of water from beaker into the graduated cylinder Use dropper to get the exact amount of 50 . First Layer Height=.35 & Solid Layers Bottom=3. Layer Height. Solid Layers Top=3. If Solid Layer Top=3 the top. Three layers will be printed solid. Based on the . Infill:Top. /Bottom Fill. Pattern. In the image on the right . Radioactive decay is the most referenced “evidence” for the earth being old. We will now examine the other evidences . that are popularly used. We must keep in must the Biblical framework of the flood when addressing these issues. On Monday and Tuesday…. We found the density of liquids and rocks. . We learned that denser materials sink, and lighter materials float.. We learned that granite is lighter than basalt and that iron is denser than both.. Learning Objectives. BTEOTLIWBAT. ….. Set up layers and assign colors and line types to them.. Load different line types needed for the templates.. Identify and use the toggles found on the Layers toolbar. . . Plate . techtonics. Continental Drift. The theory discovered by Alfred Wegener that states the continents were once connected but later drifted apart to their current locations.. Evidence supporting continental drift. Radioactive decay is the most referenced “evidence” for the earth being old. We will now examine the other evidences . that are popularly used. We must keep in . mind the . Biblical framework of the flood when addressing these issues. This week we will look at a few more . commonly used “evidences” that . the earth is old. Again we need to keep in mind the flood if we are going to explain these observations in a young world, and the observations tend to give strong evidence for the flood . Presented by Kesler Science. What are the main characteristics of the Earth’s layers?. How can the Earth’s layers be illustrated?. Essential Questions:. Earth's Layers. Earth’s Crust. The outer layer 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.. Jerome E. . Mitchell. 2013 NASA Earth and Space Science Fellow. Ph.D. Thesis Proposal. Advisor: Geoffrey C. Fox . Committee: David J. Paden, Judy . Qiu. , . Minje. Kim, and John D. Paden*. Introduction. Do Now. SWBAT identify and explain the layers of the Earth . Enter . silently. Grab materials, folders, notebooks. Begin . Do . Now. Write a hypothesis in an if-then-because . statement for the following question:. Inner Core. Outer Core. Mantle. Crust. The Layers of the Earth. 3. Crust. Thinnest layer; density 3 g/cm. 3. The Earth's . outermost. . layer of the 4 main layers. The crust is typically about . 30-40 km thick beneath continents. LAYERS of the Interior. THE CORE- . Nuclear Fusion occurs. Diameter- 400,000 km. The Radiation Zone- . region of compressed gas and energy is transferred by electromagnetic waves.. Thickness- 300,000 km . Crust. Mantle . Core. The Crust. Hard , solid, and strong. Cooler than other layers. Thinner beneath the oceans and made of basalt. Thicker beneath the continents and made of granite. The Mantle. Composed of two layers: the upper mantle and lower mantle.