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THIS IS With Your Host... Column A Column B Column C Column D Column E Column F 100 100 100 100 100 100 200 200 200 200 200 200 300 300 300 300 300 300 400 400 400 400 400 400 500 500 500 500 500 500 Rocks that form from Magma or Lava cooling. A 100 Igneous A 100 Clastic sedimentary rock made of the sediment size Clay. A 200 Shale A 200 Metamorphic Rocks can form from what type of rock? A 300 Any type!!! A 300 What type of Sedimentary Rock is Coal? A 400 Organic A 400 What process forms detrital sedimentary rocks? A 500 WECC Weathering Erosion Compaction Cementation A 500 Extrusive rocks form from _________. B 100 Lava B 100 What processes form Metamorphic Rocks. B 200 Heat and Pressure Or…Contact with heated fluids. B 200 What process creates chemical sedimentary rocks? B 300 Evaporation B 300 Metamorphic rock that will from from the heating and pressuring of Limestone. B 400 Marble B 400 A Detrital Sedimentary Rock is named based upon what? B 500 Sediment Size Examples: Clay, Silt. Sand, Gravel B 500 What do we call molten rock UNDER Earth’s Surface and what type of rock would it form? C 100 Magma Intrusive Igneous Rock C 100 What rate of cooling produces BIG crystals in Igneous Rocks? C 200 Slow Cooling - intrusively C 200 What process forms sediments? C 300 Weathering and Erosion C 300 DAILY Place A Wager DOUBLE C 400 Name the three things that form rocks. Give an example of a rock that satisfies each. C 400 Minerals (many) Organic Material (chalk,coal) Volcanic Glass (obsidian) C 400 In an undisturbed layer of sedimentary rocks, where can the oldest rocks be found? C 500 At the bottom C 500 Determining the age of rocks by examining a layer of sedimentary rocks is known as the law of ________. D 100 Superposition D 100 What makes Rhyolite and Granite similar? What makes them different? D 200 1. Similar: Both granitic – light color – lower density – high in Si and O – low in Fe and Mg 2. Different: Where they formed – intrusive vs. extrusive – crystal size – Lava/magma D 200 Name any metamorphic rock, its parent rock and whether it is foliated or non-foliated. D 300 Quartzite – sandstone (n) Gneiss – granite (f) Slate – shale (f) Marble – Limestone (n) Schist – many parent rocks (f) D 300 What are three things that can be used to classify an igneous rock? D 400 Crystal size Color Specific Gravity Elements D 400 How do you know that pumice and scoria are extrusive? How can you tell them apart? D 500 Gas Pockets Color D 500 Two examples of organic rocks are: E 100 Chalk Coquina Coal “Fossil-rich” limestone E 100 Two Clastic sedimentary rocks made of gravel sized sediments. E 200 Conglomerate and Breccia E 200 An example of a foliated igneous rock is: E 300 NONE!!! Only metamorphic can be foliated or nonfoliated E 300 What are two ways that two rocks made of the same minerals could look so different? E 400 The minerals exist in different proportions (think choc. chip cookie example) Intrusive/Extrusive so they have different crystal sizes. E 400 This is why magma rises to the surface and becomes lava. E 500 Because it is warmer and therefore less dense than the surrounding rocks. E 500 Name one of the clastic Sedimentary Rocks made of a medium size sediment. F 100 Siltstone or sandstone F 100 What does the color tell us about the speed at which an igneous rock formed? F 200 Absolutely Nothing!!! Only crystal size can tell us that, silly! F 200 These rocks form by applying heat or pressure to a preexisting rock. F 300 Metamorphic F 300 Name a chemical sedimentary rock. F 400 Limestone Rock Salt F 400 This Igneous Rock has large crystals, cools from magma, and makes up the center of the continents. Hint: made of mica, quartz, feldspar and hornblende. F 500 Granite F 500 Final Jeopardy Please record your wager. (I wouldn’t recommend wagering a lot – it is pretty impossible). Click on screen to begin Name Mr. Hayden’s FAV path through the rock cycle! Click on screen to continue Sedimentary, Sedimentary, Igneous, Metamorphic, Igneous, Sedimentary!!! Click on screen to continue Thank You for Playing Jeopardy! Game Designed By C. Harr-MAIT