© Mark E. Damon - All Rights Reserved © Mark E. Damon - All Rights Reserved Round 1 Round 2 Final Jeopardy $ $ p i l l i h P D a p h n e $ y h t a K © Mark E. Damon - All Rights Reserved Scientific Method Basic Chemistry Minerals Rocks Earth’s Structure Round 2 $100 $100 $100 $100 $100 $100 Final Jeopardy $200 $200 $200 $200 $200 $200 Scores $300 $300 $300 $300 $300 $300 $400 $400 $400 $400 $400 $400 $500 $500 $500 $500 $500 $500 Metric Measurement © Mark E. Damon - All Rights Reserved $100 Used by scientists to measure volumes of liquids. © Mark E. Damon - All Rights Reserved $100 Graduated Cylinders Scores © Mark E. Damon - All Rights Reserved $200 Use this to measure the mass of a mineral sample. © Mark E. Damon - All Rights Reserved $200 A Cent-0-Gram or Digital Balance Scores © Mark E. Damon - All Rights Reserved $300 Measures metric length in centimeters. © Mark E. Damon - All Rights Reserved $300 A Centimeter Ruler Scores © Mark E. Damon - All Rights Reserved $400 Determined by dividing an object’s mass by its volume. © Mark E. Damon - All Rights Reserved $400 Density Scores © Mark E. Damon - All Rights Reserved $500 Newtons are the units for this metric measurement. © Mark E. Damon - All Rights Reserved $500 Force Scores © Mark E. Damon - All Rights Reserved $100 Involves using sight, hearing, smell and sometimes taste to gather information. © Mark E. Damon - All Rights Reserved $100 Observations Scores © Mark E. Damon - All Rights Reserved $200 The variable the scientist changes, also called the “manipulated variable.” © Mark E. Damon - All Rights Reserved $200 The Independent Variable Scores © Mark E. Damon - All Rights Reserved $300 An interpretation based on observation and prior knowledge. © Mark E. Damon - All Rights Reserved $300 An Inference Scores © Mark E. Damon - All Rights Reserved © Mark E. Damon - All Rights Reserved $400 This variable changes in response to the independent variable. © Mark E. Damon - All Rights Reserved $400 The Dependent Variable Scores © Mark E. Damon - All Rights Reserved $500 “The diverse way that scientists solve problems and seek to answer questions about the natural world.” © Mark E. Damon - All Rights Reserved $500 Scientific Inquiry Scores © Mark E. Damon - All Rights Reserved $100 This “number” is equal to the number of protons in the nucleus of an atom. © Mark E. Damon - All Rights Reserved $100 The Atomic Number Scores © Mark E. Damon - All Rights Reserved $200 Subtract the atomic number from the mass number to determine the number of these. © Mark E. Damon - All Rights Reserved $200 Neutrons Scores © Mark E. Damon - All Rights Reserved $300 Form when two or more different kinds of elements are chemically bonded together. © Mark E. Damon - All Rights Reserved $300 Compounds Scores © Mark E. Damon - All Rights Reserved $400 This phase of matter has “free movement’ of molecules making it the most energetic phase of matter. © Mark E. Damon - All Rights Reserved $400 Gas Scores © Mark E. Damon - All Rights Reserved $500 When these “changes” occur, a new substance is produced. © Mark E. Damon - All Rights Reserved $500 Chemical Changes Scores © Mark E. Damon - All Rights Reserved $100 The Field Scale of Mineral Hardness states that minerals that scratch this, have a hardness of six. © Mark E. Damon - All Rights Reserved $100 Window Glass Scores © Mark E. Damon - All Rights Reserved $200 Minerals can’t be composed of anything that is living, or ever was living. In other words, they are all: © Mark E. Damon - All Rights Reserved $200 Inorganic Scores © Mark E. Damon - All Rights Reserved $300 Said to be the least reliable physical property in the identification of an unknown mineral. © Mark E. Damon - All Rights Reserved $300 Mineral Color Scores © Mark E. Damon - All Rights Reserved $400 A brick, diamond, coal, and glass. Of these, only this one is a mineral. © Mark E. Damon - All Rights Reserved $400 Answer: Diamond Why not these three? •Brick (man-made) •Coal (organic) •Glass (man-made & no crystals) Scores © Mark E. Damon - All Rights Reserved $500 Use this process to determine the volume of a mineral sample. © Mark E. Damon - All Rights Reserved $500 Water Displacement Scores © Mark E. Damon - All Rights Reserved $100 These rocks would be found in or near a volcano. © Mark E. Damon - All Rights Reserved $100 Igneous Rocks Scores © Mark E. Damon - All Rights Reserved $200 This mineral has a density of 2.6 g/ml, a glassy luster, and a hardness of 2.5. © Mark E. Damon - All Rights Reserved $200 Halite Scores © Mark E. Damon - All Rights Reserved $300 Metamorphism means “change in form.” An existing rock or “protolith” is changed into a Metamorphic Rock. The protolith is subjected to these to bring that change about. © Mark E. Damon - All Rights Reserved $300 Heat and Pressure Scores © Mark E. Damon - All Rights Reserved $400 These threaten public health by polluting streams and rivers. © Mark E. Damon - All Rights Reserved $400 Coal Mines Scores © Mark E. Damon - All Rights Reserved $500 Weathering of rocks, erosion and transportation of rock the fragments, deposition, compaction and cementation of those rock fragments, form this type of sedimentary rock. © Mark E. Damon - All Rights Reserved $500 Clastic or Fragmental Sedimentary Rocks Scores © Mark E. Damon - All Rights Reserved $100 This is the extremely hot, central portion of the Earth’s interior. © Mark E. Damon - All Rights Reserved $100 The Core Scores © Mark E. Damon - All Rights Reserved $200 The upper part of the Earth’s mantle and the crust on top are referred to as this. © Mark E. Damon - All Rights Reserved $200 The Lithosphere Scores © Mark E. Damon - All Rights Reserved $300 Because temperature differences in rock create density differences, large convection currents are created in this area of the Earth’s structure. © Mark E. Damon - All Rights Reserved $300 The Asthenosphere (Upper Mantle) Scores © Mark E. Damon - All Rights Reserved $400 By studying these, scientists have been able to determine that the structure of the Earth’s interior is layered. © Mark E. Damon - All Rights Reserved $400 Seismic or Earthquake Waves Scores © Mark E. Damon - All Rights Reserved $500 These both INCREASE as the depth below the Earth’s surface INCREASES. © Mark E. Damon - All Rights Reserved $500 The Temperature & Pressure Scores © Mark E. Damon - All Rights Reserved Divergent Boundaries Convergent Boundaries Transform Boundaries $200 $200 $200 $200 $200 $200 Final Jeopardy $400 $400 $400 $400 $400 $400 Scores $600 $600 $600 $600 $600 $600 $800 $800 $800 $800 $800 $800 Relative Ages Plate Tectonics Pot Luck $1000 $1000 $1000 $1000 $1000 $1000 Round 1 © Mark E. Damon - All Rights Reserved $200 Fossils are usually found in this type of rock. © Mark E. Damon - All Rights Reserved $200 Sedimentary Rocks Scores © Mark E. Damon - All Rights Reserved $400 This “principle” states that rock layers on the bottom of the stack are older than the ones on the top. © Mark E. Damon - All Rights Reserved $400 Superposition Scores © Mark E. Damon - All Rights Reserved $600 The youngest layer of rock pictured above has a fossil of this type in it. © Mark E. Damon - All Rights Reserved $600 A Fern Fossil (The fern fossil is in the top layer.) Scores © Mark E. Damon - All Rights Reserved $800 Which rock layer is older, the one with the clam fossil or the one with the trilobite fossil? © Mark E. Damon - All Rights Reserved $800 The layer with the Trilobite fossil. Scores © Mark E. Damon - All Rights Reserved $1000 Based on the fossils found, the location pictured was most likely this kind of environment for much of the past. © Mark E. Damon - All Rights Reserved $1000 Ocean or Marine Scores © Mark E. Damon - All Rights Reserved $200 Basaltic rock is added to the ocean floor along these landforms. © Mark E. Damon - All Rights Reserved $200 Mid-Ocean Ridges Scores © Mark E. Damon - All Rights Reserved © Mark E. Damon - All Rights Reserved $400 This process occurs along mid-ocean ridges. © Mark E. Damon - All Rights Reserved $400 Sea-Floor Spreading Scores © Mark E. Damon - All Rights Reserved $600 Scientists discovered that rocks farther from mid-ocean ridges were older than the rocks at the ridge by doing this. © Mark E. Damon - All Rights Reserved $600 Drilling Core Samples from the Ocean Floor. Scores © Mark E. Damon - All Rights Reserved $800 Because basaltic lava cools and congeals rapidly at the bottom of the ocean, the basaltic rocks that form take the shape of these. © Mark E. Damon - All Rights Reserved $800 Pillows (Pillow Basalts) Scores © Mark E. Damon - All Rights Reserved $1000 As oceanic crust moves away from a mid-ocean ridge, it becomes: © Mark E. Damon - All Rights Reserved $1000 Cooler and Denser Scores © Mark E. Damon - All Rights Reserved $200 This stress force occurs along convergent margins. © Mark E. Damon - All Rights Reserved $200 Compression Scores © Mark E. Damon - All Rights Reserved $400 For this reason, plates of lithosphere that contain ocean crust sink into the mantle or are “subducted” when colliding with plates of lithosphere containing continental crust. © Mark E. Damon - All Rights Reserved $400 Because oceanic plates are more dense. Scores © Mark E. Damon - All Rights Reserved $600 When two plates carrying continental crust collide, these form. © Mark E. Damon - All Rights Reserved $600 Folded Mountains (Example: The Himalaya Mountains) Scores © Mark E. Damon - All Rights Reserved $800 Deep-ocean trenches form along Subduction zones. This deep-ocean trench boasts being the world’s deepest. © Mark E. Damon - All Rights Reserved $800 The Mariana Trench Scores © Mark E. Damon - All Rights Reserved $1000 As an oceanic plate is subducted under a continental plate, these form. © Mark E. Damon - All Rights Reserved $1000 Folded Mountains and Volcanoes Scores © Mark E. Damon - All Rights Reserved $200 This Transform Boundary represents a major fault line that runs through most of California. © Mark E. Damon - All Rights Reserved $200 The San Andreas Fault Scores © Mark E. Damon - All Rights Reserved $400 This stress force exists along Transform Boundaries and Strike-Slip Faults. © Mark E. Damon - All Rights Reserved $400 Shearing Scores © Mark E. Damon - All Rights Reserved © Mark E. Damon - All Rights Reserved $600 Because “Fault E” does this to “Intrusion D,” we know that the intrusion is older. © Mark E. Damon - All Rights Reserved $600 Cross-Cuts Scores © Mark E. Damon - All Rights Reserved $800 During the lab where you used the “Fault Laboratory,” the hooked-Velcro strips were used to increase the resistance along the fault. In nature, the hookedVelcro represent these along an actual fault line. © Mark E. Damon - All Rights Reserved $800 Kinks and Twists Along the Fault Line Scores © Mark E. Damon - All Rights Reserved $1000 The San Andreas Fault runs 800 miles through this U.S. state. © Mark E. Damon - All Rights Reserved $1000 California Scores © Mark E. Damon - All Rights Reserved $200 Compression of rock layers occurs at convergent margins. When rock layers are compressed, these form. © Mark E. Damon - All Rights Reserved $200 Folded Rock Layers Scores © Mark E. Damon - All Rights Reserved $400 This stress force exists along Divergent Margins. © Mark E. Damon - All Rights Reserved $400 Tension Scores © Mark E. Damon - All Rights Reserved $600 Evidence supporting the Theory of Continental Drift includes: fit of the continents, glacial remains in Africa, coal deposits in Antarctica, evidence from landforms, and fossil evidence. Who was the scientist that proposed the Theory of Continental Drift? © Mark E. Damon - All Rights Reserved $600 Alfred Wegener Scores © Mark E. Damon - All Rights Reserved $800 The theory of Plate Tectonics states that the Earth’s plates are in this kind of motion. © Mark E. Damon - All Rights Reserved $800 Constant, Slow Motion Scores © Mark E. Damon - All Rights Reserved $1000 Geologists rejected the Theory of Continental Drift for this reason. © Mark E. Damon - All Rights Reserved $1000 Wegener was unable to explain how the continents moved or drifted over time. Scores © Mark E. Damon - All Rights Reserved $200 The Atomic Number of Tungsten is 74 and its Mass Number is 184. That means there are this many neutrons in the nucleus of a Tungsten atom. © Mark E. Damon - All Rights Reserved $200 110 Scores © Mark E. Damon - All Rights Reserved $400 In the lower mantle of the Earth, warmer, less dense liquid rock rises as cooler, more dense liquid rock sinks. This creates large cells of motion that geologists believe drag the Earth’s plates along with them. What are these cells of motion called? © Mark E. Damon - All Rights Reserved $400 Convection Currents Scores © Mark E. Damon - All Rights Reserved $600 These are areas of land where all of the rain that falls drains off of it to the same place. © Mark E. Damon - All Rights Reserved $600 Watersheds Scores © Mark E. Damon - All Rights Reserved $800 The thermometer indicates a temperature of this many degrees Celsius. © Mark E. Damon - All Rights Reserved $800 24°C Scores © Mark E. Damon - All Rights Reserved $1000 Because the bonds of a liquid are attracted to the bonds of a graduated cylinder, measured liquids “sag” or have a “belly down” appearance. Measurements are always made from the lowest part of this curvature. This is the name given to the curvature. © Mark E. Damon - All Rights Reserved $1000 The Meniscus Scores © Mark E. Damon - All Rights Reserved Ocean-Floor Structures Scores Final Jeopardy Question © Mark E. Damon - All Rights Reserved These formations were first discovered at the bottom of a mid-ocean ridge in 1977 by Robert Ballard while inside the submarine Alvin. © Mark E. Damon - All Rights Reserved Black Smokers or Chimneys Scores