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Scientists are constantly striving to understand the Earth; it can be divided into ____ parts |
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The study of the solid earth including minerals, rocks, and fossils. |
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The study of movement of water, lakes, and streams. |
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The study of the shape and composition of ocean water, tides and currents, and plants and animals. |
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The study of earth’s atmosphere including weather and climate. |
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The study of the planets, the sun and stars. |
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an organized manner to solve a problem |
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Steps of the Scientific Method |
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1. Making observations2. Forming a hypothesis3. Conducting experiments test hypothesis using a variable and a control4. Drawing conclusions – statements about original hypothesis |
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statement that explains why things happen the way they do. |
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describes what happens in a given situation |
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Used to help scientist understand how things work. Models show relationships of data gathered models are refined constantly as new data allows. |
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What are the two types of data |
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sight, touch, smell, hearing, and taste. |
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distance, volume, and time |
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Symbol for Meter, Liter, Kilogram, and Newton |
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The variable that is changed by the experimenter. |
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The variable that responds to the independent variable. |
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Those items in an experiment that remains the same |
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The group that receives everything but the independent variable. All results are compared to this group. |
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The number of times an experiment is performed. |
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- Title: the effect of IV on the DV - Hypothesis – If…. Then. …. |
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Breakage of a mineral along planes of weakness in the crystal structure |
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Visible light spectrum radiation reflected from a mineral |
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Geometric shape of a crystal or mineral |
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Breakage of a mineral, not along planes of weakness in the crystral structure |
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Resistance to scratching or abrasion. |
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Character of the light reflected by a mineral. |
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force generated by an object or electrical field. |
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Chemical interaction of hydrochloric acid and calcium carbonate (CaCO3 |
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Ratio of the mass of a mineral to the mass of an equal volume of water |
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Color of the mineral when it is powdered |
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Nerve ending reaction in the tongue to different chemicals |
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Large areas that are flat, or nearly flat. |
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Large areas that are flat, or nearly flat that are elevated. |
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Par of Earth’s crust that are not horizontal, may be bent of broken. May be volcanic. |
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Science of map making. Based on information from explorers. More art in the beginning |
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Second century astronomer, and first to put North at top information based on a round map. |
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Since 1807 USGS has conducted surveys to improve maps. Place benchmarks or bronze marker to establish elevation; about 3000. |
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– lines that run east – west around the Earth 0°- 90°0° latitude – equator – divides into N and S hemispheres also called: “parallels” always include direction: ex. 23°N or 45°S |
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run from N. pole to S. pole. Not parallel touch at the poles, also called “meridian” |
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Prime Meridian – crosses trough Greenwich, England. 0° longitude indicates E or W hemisphere. Can be used to measure distance and time. -180° meridian separates consecutive days – International Date Line. |
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Scales – They show relationship between distance on map to that on Earth. |
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1. Verbal scale – equates two different units. Ex. -1cm = 100km |
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Representative faction (Rf) |
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2. Representative faction (Rf) – shows ratio of representative distance on map to acual distance on Earth. Ex. – 1cm = 100km or 1: 100,000 |
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Contour interval – difference in elevation between consecutive contour lines. |
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A naturally occurring, inorganic solid with a definite chemical composition and crystal structure. |
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Silicates – consists of silicon and oxygen 92% of Earth’s crust. |
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Tetrahedron – 4 sided structure long chains form quartz |
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1. Carbonates – 8% if Earth’s crust (non silicates) -Made of 3 oxygen + 1 Carbon - example – Calcite (carbon + calcium) Dolomite (magnesium + oxygen |
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sulfates – 4 Oxygen + 1 Sulfur - Gypsum – sulfate bonded to calcium and H20 |
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Oxides – O bonded to another element example – Fe or Al |
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Halides and Sulfides – contain no Oxygen example Halite – NaCl or Pyrite – Iron Sulfide |
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rare minerals that contain element Example – gold, silver, and copper |
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Diamond and graphite – pure carbon |
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1. Color – not very reliable 2. Streak – color left on porcelain surface 3. Luster – appearance in reflected light metallic or non metallic, waxy, pearly, glassy, dull, brilliant, silky 4. Hardness – Mohs’ scale of mineral harness 1(softest)-------------------------------------------(hardest) 10 Talc Diamond 5. Cleavage – tendency to break along smooth, define surfaces Fracture – breaks along rough or jagged surfaces 6. Others – Density and Crystal shaped Special Properties – Loadstone-magnetic Calcite – fizzes with HCI Halite – taste salty Sulfur – smells like eggs 7. Specific gravity – comparison weight and water. |
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a. Crystal – 3 dimensional structure with each surface face having definite shape. |
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a. Gem – Mineral that has beauty, durability, and value |
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a. Ores- Term used to describe minerals from which metal and non-metals can be removed in usable amounts; separate by a process of smelting. |
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Copper can be used for..... |
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a. Copper can be used in pipes and electrical wires |
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Silverand gold can be used as..... |
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a. Silver and gold can be used for jewelry and dental fillings |
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a. Sulfur is of the most useful non-metals; used in matches medicines and fertilizers |
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- Rocks – Naturally occurring combination of minerals
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- Magma – molten rock in the Earth
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Molten rock reaches the surface |
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1. Igneous – formed from lava or magma |
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2. Sedimentary – compressed sediments through weathering and erosion |
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Metamorphic forms from.... |
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3. Metamorphic – igneous, sedimentary are warmed and put under pressure; formed new combinations or crystals. |
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Igneous rocks form under 2 conditions |
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a) chemicals in magma ex. Basalt (iron) b) rate at which lava cools |
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- extrusive – fine small crystals
ex. Rhyolite |
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- coarse – large crystal
ex. Granite |
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contains dense minerals usually black or green. |
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low density, usually light in color |
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Rocks which don't form crystals |
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What are the 3 types of sedimentary rock |
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Clastic, Chemical, Organic |
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Clastic Sedimentary Pieces of rock exposed to heat, water, and freezing. Conglomerate – composed of large round fragments Breccias – sharp edge pieces; sandstone, siltstone, shale. |
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Chemical sedimentary -
- Formed when minerals dissolve in water and evaporate, compaction occurs to form rock.
Evaporates – form when chemical is left out of solution, usually deposited on ocean floor; rock salt and gypsum. Precipitate – form when substances fall out of solution, deposit on ocean flow; compact limestone, and chert. |
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- Organic Sedimentary
Formed from once living organisms which contained an element carbon. Organic limestone forms from skeleton of corals, also coal formation. Vast supply in eastern and western part of U.S. Southwest has deposits of coal. Coal forms from decaying plant material at bottom of swamps or bogs. Peat forms first form buried sediments, pressure increases and temperature rises. This forms lignite (know as brown coal). Next is bituminous coal (soft brown coal), most common. Last is anthracite (hard compact, black coal). Used to produce electricity. Resrvoir rocks are formed when oil droplets seep through limestone or sandstone and pool. Fossil fuels – coal, oil, natural gas. |
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used in industrial or construction projects. Examples; shale and limestone. Used in sewer pipes, buildings are made of sandstone and rock gypsum is used for drywall. Porcelain – used in sinks, china, china made of clay, feldspar and quartz. |
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A. Formation -form when heat and pressure cause chemical and structural changes. Mountain building forces and heat form large; bodies of magma that form metamorphic rocks. B. Classification of Metamorphic Rocks: Foliated – have obvious layers, often are shiny. Example: slate, phylitite No foliated: contain no layers Example: marble. |
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Shale à slate Sandstone à quartzite Granite à gneiss Mica à Schist Limestone à Marble |
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