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The Rock Cycle

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Presentation on theme: "The Rock Cycle"— Presentation transcript:

1 The Rock Cycle http://www.windows.ucar.edu/tour/link=/earth/geology/rocks_intro.html

2 Rock Cycle  Rock: Earth material made of minerals, glass or organic matter  Rock Cycle: the process by which, over many years, Earth materials change back and forth among magma, igneous rocks, sediments, sedimentary rocks and metamorphic rocks

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4 Igneous Rocks: rock formed when magma or lava cools

5  Lava: molten rock from a volcano flowing on Earth’s surface  Magma: molten rock beneath Earth’s surface  Intrusive: igneous rocks that form below Earth’s surface (plutonic)  Extrusive: igneous rocks that form when magma extrudes onto Earth’s surface and cools as lava (volcanic)

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7 Igneous Rocks  Basaltic or Mafic: dark- colored igneous rocks that form from magma rich in iron & magnesium (high ferromagnesium minerals; low silica)  Granitic or Felsic: light- colored igneous rocks, form from magma rich in silicon and oxygen (low ferromagnesium minerals; high silica)

8 Igneous Rock Textures A rock’s texture depends on the - size, - shape, and - arrangement of crystals A crystal’s size and shape depends: - rate of cooling - amount of dissolved gasses   Composition – types of minerals within a rock   Structure – orientation of minerals or rock fragments in a rock

9 Coarse Grained  Mineral grains large enough to be seen with the unaided eye (Phaneritic): Granite or Gabbro Granite or Gabbro

10 Fine Grained  Mineral grains too small to be seen with the unaided eye (Aphanitic):  For example: Rhyolite or Basalt

11 Glassy  Cooled so quickly that no crystals were able to be formed Obsidian Scoria or Pumice or Pumice

12 Porphyritic Texture Displays two stages of cooling… slow and then fast (or quenched)

13   Composition – types of minerals within a rock   Structure – orientation of minerals or rock fragments in a rock

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15 Sedimentary Rocks: rock formed when sediments become pressed or cemented together

16  Sediments: loose materials such as rock fragments and mineral grains that have been transported by wind, water, or glacier  Weathering: the breaking of rocks into smaller pieces, either mechanically or chemically  Erosion: the process that moves weathered rocks from one location to another  Deposition: the build up of sediments on the bottoms of lakes, valleys and the ocean floor usually in layers

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18  Compaction: sedimentary rock- forming process that occurs when layers of sediment become compressed by the weight of layers above them  Cementation: sedimentary rock- forming process in which sediments are glued together by minerals deposited between the sediments

19 Three types of Sedimentary Rocks:  Clastic Sedimentary Rock: made of broken fragments of plants, animals, and primarily other rocks

20 Examples of Clastic Sedimentary Rocks Conglomerate- composed of rounded, pebble-sized fragments that are held together by a cement

21 Examples of Clastic Sedimentary Rocks Breccia - composed of angular, pebble- sized fragments that are held together by a cement

22 Examples of Clastic Sedimentary Rocks Sandstone – composed of small mineral grains (usually quartz) that are cemented together.

23 Examples of Clastic Sedimentary Rocks Shale – made of flaky clay particles that compress into flat layers

24 Chemical Sedimentary Rocks made from minerals precipitated from a solution or are left behind when a solution evaporates – minerals left behind form rocks called evaporites Rock salt (halite)  Rock salt (halite) 

25 Organic Sedimentary Rock  primarily made from the remains of once living things

26 Examples of Organic Sedimentary Rock  Limestone  Fossiliferous Limestone  Chalk

27 Example of Organic Sedimentary Rock Coal - forms from plant remains that are buried before they decay. The plant layers are then compacted into matter that is composed mostly of carbon

28 Metamorphic Rock: rock formed from existing rock when the temperature or pressure changes

29 Textures of Metamorphic Rocks  Foliated: a texture of metamorphic rock, created when mineral grains flatten and line up in parallel bands  Nonfoliated: texture of metamorphic rock, created when mineral grains change, grow, & rearrange but don’t form bands

30 Local Metamorphism  metamorphism that affects relatively small volumes of rock (less than 100 km³)

31 Regional Metamorphism  metamorphism that affects thousands of ( km³ ) cubic kilometers of rock

32 Contact Metamorphism metamorphism where temperature is the primary agent http://academic.brooklyn.cuny.edu/geology/grocha/monument/images/metheat.gif  Limestone  Marble  Basalt  Marble  Limestone

33 Dynamic Metamorphism Dynamic Metamorphism metamorphism where pressure is the primary agent (aka deformational metamorphism) http://www.indiana.edu/~g103/G103/wk5/week5.htm

34 Result of Dynamic Metamorphism

35 http://www.indiana.edu/~g103/G103/wk5/week5.htm

36 Examples of Metamorphic Rocks  Gneiss – metamorphosed granite, displays foliation and banding; a result of high grade metamorphism (foliated texture) kinked gneiss 

37 Examples of Metamorphic Rocks  Slate – pressure exerted on shale (claystone/ mudstone) mudstone)  Schist – high heat and pressure exerted on slate (both with foliated texture) http://library.thinkquest.org/05aug/00461/images/slate.jpg http://www.windows.ucar.edu/tour/link=/earth/geology/images/Schist_mica_jpg_image.html

38 Examples of Metamorphic Rocks  Quartzite – metamorphosed quartz sandstone (looks like fine crystalline structure)  Marble – formed from the compression of limestone (looks like numerous calcite crystals) http://www.answersincreation.org/curriculum/geology/images/Quartzite_2_jpg.jpg http://www.answersincreation.org/curriculum/geology/images/Marble_2_jpg.jpg (both with nonfoliated texture)

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40 On your hiking tour of the west, your travel group decides to take a break at a nearby stream. You get one look at that clean, cool water and quickly figure out that this would be an awesome spot to soak your tired feet. As you place your feet in the water, you notice some shiny stuff in the bottom of the stream. “Is it gold?” you think to yourself. How could you determine if it is? What tests would you use? Which tests would not be good to use to identify this as gold?

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44  http://www.eastchester.k12.ny.us/sc hools/hs/teachers/fermann/Links1.ht m http://www.eastchester.k12.ny.us/sc hools/hs/teachers/fermann/Links1.ht m http://www.eastchester.k12.ny.us/sc hools/hs/teachers/fermann/Links1.ht m

45 Map

46 Data Table 1 Station No. # of visitsStation No. # of visits 17 28 39 410 511 6

47 Data Table 2 Station 1 - Compaction and Cementation (write information/draw diagrams regarding station 1 here) Station 2 - High Temperature and Pressure (write information/draw diagrams regarding station 2 here)

48 List of Stations 1. 1. Compaction and Cementation 2. 2. High Temperature and Pressure 3. 3. Sediments 4. 4. Igneous rock 5. 5. To the surface 6. 6. Metamorphic rock 7. 7. Sedimentary rock 8. 8. Melting 9. 9. Cooling and hardening (solidification/crystallization) 10. 10. Magma 11. 11. Weathering and Erosion

49 Rock Cycle Roulette – write-up 1. Entire lab is to be typed. 2. Map: create 3 long boxes on the computer and HAND DRAW the arrows. 3. Data Table 1: Create a table (either in Microsoft Word or Excel) with tally marks to indicate how many times you went to each station. 4. Data Table 2: type the information at each of the stations IN ORDER (Station 1 – Station 11) AND recreate the diagrams (by hand) at the appropriate stations. 5. Answer the questions and conclusion questions fully, with the question implied in the answer 5. Answer the questions and conclusion questions fully, with the question implied in the answer.

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