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Mineral Formation

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Mineral Formation

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  1. In 2008, crystals up to 39 feet long were found in a cave in Mexico at a depth of 1000 feet. The cave is extremely hot, with air temperatures reaching 136 °F with 90 to 99 % humidity. The cave is relatively unexplored due to these conditions. Without proper protection, people can only endure about ten minutes of exposure at a time. See the suits Mineral Formation

  2. Video https://www.youtube.com/watch?v=jb1bL8xTqAs Mineral Formation

  3. Scoria Gneiss Coal The Earth’s crust is made up of two things: Minerals and Rocks Rocksare combinations of minerals Minerals are individual crystals of all the same stuff ***You should see lots of different minerals in every single rock

  4. What is a mineral? Main Concept: Minerals are the building blocks of rocks! There are five main criteria for something to be a mineral: a) It must be solid b) It must occur naturally (not man-made) c) It is made of non-living material (never alive) d) It has a definite chemical formula (NaCl=salt) e) It has a crystal structure (Precious?)

  5. Examples: ***Notice how each is one single type of crystal! • Amethyst Calcite Garnet • Galena Gold Pyrite

  6. From stuff dissolved in liquids (Evaporation & Hot Water) From Cooling molten material Where do minerals come from? • Mineral crystals can form in two main ways:

  7. Minerals & Crystals fromMagma & Lava “Extrusive” Cooling: Lava cools Fast (Short Time = Small Crystals) • Minerals form from hot magma as it cools inside the crust, or as lava cools on the surface. • When these liquids cool to a solid, they form crystals (minerals). • Size of the crystal depends on time it takes to freeze into a solid. “Intrusive” Cooling: Magma cools slowly (Long Time = Large Crystals)

  8. Minerals Crystal Size When the hot material cools fast, it has smaller crystal size. When it cools slowly, it has large crystals. Granite Rhyolite You can see individual crystals in Granite = cooled slowly You can’t see many individual crystals in Rhyolite = cooled very fast

  9. Minerals formed by Evaporation • Some minerals form when solutions/mixtures evaporate: • When water evaporates, it leaves behind the stuff that’s dissolved in it. • The longer it takes to evaporate, the larger the crystal. • i.e. salt & water – ocean, • Halite, Gypsum, Calcite. ***All the white stuff = salt mineral crystals that formed when the water of this lake evaporated. The mineral material was left behind

  10. These salt crystals formed from salt water because as the water evaporated, the salt wasn’t dissolved anymore. So the chemical energy in salt takes over and crystals form. Do you notice the characteristic cubic crystalline shapes?

  11. How do we identify Minerals? We use the different physical and chemical properties of the mineral to identify it from other different minerals Luster:Describes how light is reflected from a minerals surface. Streak: Is the color of the minerals powder when dragged across a surface. Crystal shape: Different minerals make different crystal shapes Hardness: Hardness is determined by a “scratch test”. Color: Every mineral has some natural color…ex: Gold, Blue, Clear… Etc: There are many other types of properties we use but these are the big ones

  12. Special Properties • Some minerals display strange properties. • These can include: Magnetism, fluorescence, and reactivity. Fizzing! These minerals glow in the dark. A black light really brings it out! The minerals in this rock react with acid The particles of minerals of this rock act like magnets

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