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ROCK CYCLE - Genesis Manansala

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ROCK CYCLE - Genesis Manansala

  1. 1. The Rock Cycle
  2. 2. Igneous
  3. 3. • Formed from molten rock (magma/lava) that has cooled • Literally means “from fire” Volcanic Eruption Igneous Rock
  4. 4. can become ***When the lava cools and turns into a solid, it can turn into quartz. Liquid hot lava As an example:
  5. 5. Formed on top of the crust. Small, hard to see crystals (cooled quickly) Ex: Pumice, Obsidian ***No visible crystals in either rock
  6. 6. When magma from below rises and punches through, the minerals don’t have time to crystallize – therefore, they produce rocks with small crystals. Magma (inside) Lava Flow (Outside) Boom! ash, gasses, volcanic glass, etc. The lava will quickly cool into solid rock! Other types of rock can be blasted out
  7. 7. IGNEOUS - Extrusive Little or NO Crystals!
  8. 8. IGNEOUS - Extrusive Little or NO Crystals!
  9. 9. IGNEOUS - Extrusive Little or NO Crystals!
  10. 10. IGNEOUS - Extrusive Little or NO Crystals!
  11. 11. IGNEOUS - Extrusive Little or NO Crystals!
  12. 12. Formed inside the crust/mantle. These types always have large visible crystals. (cooled slowly) Ex: Granite and Gabbro This is a special kind of Granite called: “Pink Granite” ***Notice that both rocks have easy to see crystals
  13. 13. Magma When magma from below rises up, but does not make it to the surface, the minerals start to crystallize slowly and form large crystals. Or not… This became Granite because it never made it to the surface! Notice the bulge that forms! There might be an eruption soon!
  14. 14. IGNEOUS - Intrusive Large Interlocking Crystals!
  15. 15. IGNEOUS - Intrusive Large Interlocking Crystals!
  16. 16. IGNEOUS - Intrusive Large Interlocking Crystals!
  17. 17. IGNEOUS - Intrusive Large Interlocking Crystals!
  18. 18. Sedimentary
  19. 19. Formed by sediments (pieces of rock, shells, and dead organisms) becoming “cemented” (stuck) together. Coal Limestone Sandstone Conglomerate ***You can see lots of different stuff stuck together in these rocks!
  20. 20. 1. Start at the Surface 4. Sedimentation & Deposition 5. Compaction & Cementation 2. Weather (Break Up) 3. Erode (Carry Away) © Beadle, 2009 Sediments worn away gather here Igneous rock Layers of sand and sediments Rain moves sand, dirt, and rocks down to the ocean Earth surface Ocean
  21. 21. Metamorphic
  22. 22.  To “Morph” means to change it! • They were once Igneous or Sedimentary rocks that got buried DEEP under ground. • The heat and pressure from being deep underground changed the rocks. • Has large, inter-grown crystals in thin “bands” (Foliated) or clusters (Non-Foliated).
  23. 23. 1. Get some pre-formed rock – Igneous or Sedimentary will do. 2a. Add Heat “cook it” 3. Cool & (Re)- Crystallize 4. Metamorphic Rock!!! Note: If it melts completely and cools; It will turn back into an Igneous Rock 2b. Squeeze (pressure) to “Foliate” Heat and pressure Rocks are “Morphed”
  24. 24. Rock Cycle

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