1. Earth’s interior is divided into layers. What are the four divisions, in order, of least dense to most dense? A.Atmosphere, Surface, interior, outside.

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1. Earth’s interior is divided into layers. What are the four divisions, in order, of least dense to most dense? A.Atmosphere, Surface, interior, outside B.Crust, mantle, outer core, inner core C.Mantle, Core, Atmosphere, Center D.Nucleus, Crust, Mantle, Core

2.The mantle is a layer of Earth. What is its density as compared to other layers? A. Most dense than all the other layers B. More dense than the crust, less dense than the core C. Less dense than the crust, more dense than the core D. the same as both the crust and the core. Continental Crust: 2.7 to 3.0 Oceanic Crust: 3.0 to 3.3 Mantle (silicates): 3.3 to 5.7 (increasing with depth?) Outer Core (liquid): 9.9 to 12.2 Inner Core (solid): 12.6 to 13.0

3. Which layer of the Earth is most dense? A. Crust B. Outer Core C. Mantle D. Inner Core Inner Core: Is the center of the Earth – 1200 km thick. Is the center of the Earth – 1200 km thick. It’s solidiron and nickel. Most dense layer (heaviest) It’s solid iron and nickel. Most dense layer (heaviest) The increased pressure causes the InnerCore to be solid The increased pressure causes the InnerCore to be solid

4. Why is air less dense than Earths rocks? A.The molecules in rock are larger than the molecules in air. B.The molecules in rock are smaller than the molecules in air. C.The molecules in air are further apart than in rocks. D.The molecules in air are closer together than in rocks. The particles of air are much further apart and not as closely packed as rock.

5.How does density affect the organization of Earth? A. The densest material is closest to the center. B. The density material is farthest from the center. C. The densest material is near the center. D. Density differences allow Earth materials to mix freely.

6.Earths rigid crust floats on the hot, plastic material of the mantle. What conclusion should be made about their density? The crust is A.denser and it floats B.denser and it sinks C.less dense and floats D.same density as the mantle

From Earth’s surface to its center, the layers of Earth’s interior differ in their composition, temperature and pressure. This diagram shows the layers. 7. What conclusion can you make about the density of Earth layers from the diagram? A. As temperature and pressure increases density increases B. As temperature and pressure increases, density decreases C. Temperature and pressure are unrelated to density D. Pressure and temperature are the only factors controlling density

8. Which layer is densest? A.Atmosphere B.Crust C.inner core D.Water

9. Why does the atmosphere float above the crust? A. the density of air increases when clouds form B. air is less dense than the crust C. air is more dense than the crust D. air has the same density as the crust

10. How are the materials making up the core different from those of the crust? A. they are harder B. they are more colorful C. they will dissolve in water D. they are more dense

11. Which substance would be the best model for the mantle? A. clay B. hard ball C. aluminum foil D. cotton balls The following materials are available to build a model of Earth: Clay, a hard ball, aluminum foil, cotton balls, cardboard Use this information to answer the next two questions: 12. Which substance would best model the thickness of the crust? A. cardboard B. hard ball C. aluminum foil D. cotton balls

13. A collection of rocks is used to model the kinds of materials found in Earth. Which rock should be labeled “core” rocks? A. iron/nickel B. aluminum/silicate C. water/salt D. coal/granite

14. Which model of Earth shows the most accurate shape and relative size of the continents? A. a road map B. a topographical map C. a globe D. a poster

15.Which parts of this model are accurate? A. The names of Earths layers B. The color of the layers C. The thickness of the layers D. The height of the mountains 16.How could the crust be more accurately represented? A. If the mountains were larger. B. If the location of India was moved. C. If it was not the outside layer. D. If it was thinner and flattened

Essay 1. Imagine that you are taking a journey through the center of Earth. You start in space over the crust. You are in a space ship that can withstand high temperature and pressure. You stop several times on your ship to collect data. Describe two characteristics of each layer as you go. Atmosphere, crust, water, mantle, outer core and inner core.

2. You are building a model of Earth based on the density of layers. What materials would you use for each layer? Include water and atmosphere.

Answers: 1. B 2. B 3. D 4. C 5. A 6. C 7. A 8. C 9. B 10. D 11. A 12. C 13. A 14. C 15. A 16. D Sample Answers: 1. Atmosphere: thin layer of gas, density increases as you get closer to the crust. Water: Floats on the crust. Warm on surface, gets colder as you go deeper, density increases and temperature decreases. Crust: Thin solid layer. Heat and pressure increases as you approach the mantle. Mantle: Trip through the mantle almost halfway to center of Earth. Heat and density increases as you travel through a sticky plastic liquid composed of silicon, oxygen, iron and magnesium. Outer Core: Hot liquid of iron nickel mixture. Increases in density and temperature as approach the inner core. Inner Core: Solid iron nickel mixture. Extreme heat and pressure. May be as hot as the Sun. Scoring Guide: 2 points for each layer. I point for heat and density. 1 point for describing material. Total 12 points. 2. Atmosphere - dry ice - gas Water - Water or Jell-O - liquid Crust - cookies - solid Mantle - molasses - thick plastic liquid Outer core - hot fudge - liquid Inner core - rock candy - solid

Sample Answers: 1. Atmosphere: thin layer of gas, density increases as you get closer to the crust. Water: Floats on the crust. Warm on surface, gets colder as you go deeper, density increases and temperature decreases. Crust: Thin solid layer. Heat and pressure increases as you approach the mantle. Mantle: Trip through the mantle almost halfway to center of Earth. Heat and density increases as you travel through a sticky plastic liquid composed of silicon, oxygen, iron and magnesium. Outer Core: Hot liquid of iron nickel mixture. Increases in density and temperature as approach the inner core. Inner Core: Solid iron nickel mixture. Extreme heat and pressure. May be as hot as the Sun. Scoring Guide: 2 points for each layer. I point for heat and density. 1 point for describing material. Total 12 points.

2. Atmosphere - dry ice - gas Water - Water or Jell-O - liquid Crust - cookies - solid Mantle - molasses - thick plastic liquid Outer core - hot fudge - liquid Inner core - rock candy - solid