Survey
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
Rocks and Minerals Minerals – What are they? • Inorganic solid • Crystal structure – Repeating atomic structure • Definite composition – Pure substance – elements Crystal structure of a diamond Mineral Formation • Come from magma (molten rock below ground) – Slow cooling: large crystals Mineral formation, con’t • Fast cooling: tiny crystals Mineral Formation, con’t • Above ground: magma called lava – May have no crystals if cools too fast Mineral formation, con’t • Crystals may form from dissolving out of liquid Calcite caves Salt caves Mineral Properties- distinguishing characteristics • Color • Luster- how light is reflected – Metal/nonmetal Mineral Properties, con’t • Hardness – Mohs Scale Mineral Properties, con’t • Streak Mineral Properties, con’t • Density d=m/v • Density = Mass/volume • Compare pumice and lead • Crystal shape Mineral properties, con’t • Cleavage – tendency to split along smooth surfaces Calcite has three directions of cleavage. The cleavage directions are not at right angles to each other, like salt, but are inclined. The resultant shape produced by the cleavage of calcite is called a rhombohedron Mineral properties, con’t • Fracture – tendency to split irregularly Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of weakness and break irregularly. Special properties • Magnetic – magnetite • Taste - halite Special properties, con’t • Fluorescence – glows under UV light Special Properties, con’t • Phosphorescence – continues to glow when UV light is removed Special Properties, con’t • Smell – sulfur • Fizzes – in response to acid: Calcite Special Properties, con’t • Radioactive - uranium uranite Mining for Uranium Metatorbernite contains uranium uranite Uses of minerals • Ores- minerals that can be re removed from rock in usable amounts – Metals- may be hammered, pressed, conduct electricity and heat Pressed metals hammered Copper and silver wire Uses of minerals, con’t • Non-metals – variety of uses: Sulfur: medicines, matches fertilizer Uses of Minerals, con’t • Gemstones – precious and valuable – Rubies, emeralds, diamonds, sapphires are considered precious stones – Semi-precious : garnet, topaz, onyx and others What is a Rock? • Composed of one or more minerals • May contain natural substances that are not minerals Types of Rock – classified by how they form Igneous Sedimentary Metamorphic Igneous • Means fire – from molten rock inside the earth – Classified by composition and texture • • • • Glassy: obsidian Granite Fine-grained: basalt Coarse-grained: granite Porphyritic – both large and small grains in one rock Obsidian Basalt Porphyritic granite Igneous, con’t • Classified by where it formed – Extrusive: formed from lava brought to the surface and cooled quickly – Intrusive: fomed in magma and cooled slowly (granite • Also known as plutonic rock or plutons (after Pluto: God to the Underworld) Extrusive - Basalt A glacial igneous boulder with intrusive sheet dikes Sedimentary rock – formed from particles that have been carried or deposited by wind or water Mesa Verde - Colorado Zion National Park - Utah 5% of the Earth’s surface is sedimentary rock Sedimentary, classification – Classic rocks – formed from fragments of existing rocks • Conglomerate – if over 1/3 is made of pebbles cemented together Sediment (A) may someday become a clastic rock (B) if compacted and cemented together. Coarse-grained clastic rock with mostly rounded clasts (conglomerate), Hopi Buttes, Arizona Sedimentary Rock, classification, Clastic con’t • Sandstones – made of sand-sized grains • Shale – made of particles smaller than sand Oil Shale Sandstone has stripes in it that show when the layer was made. This is a lot like rings in the trunk of a tree Black Shale Sedimentary classification, con’t • Organic Rocks – made from organisms – Example Limestone, chalk, coal White cliffs of Dover, England Sediment may have a biological or chemical origin. Shell fragments such as these are often found on beaches in tropical regions Coal Sedimentary Rock classification, con’t • Chemical Rocks- Formed when minerals dissolve out of water-Rock salt and gypsum The gypsum "cotton wool" is a rare phenomenon. The fibrous form of gypsum is called Anhydrite, meaning gypsum without water Gypsum flowers "grow" in profusion on the wall of the Puketiti Flower Cave in New Zealand. They are rocks, not living plants, despite the flower-like shape. They seem to grow and curve out of the wall, like toothpaste forced out of a tube. Some say they come out of cracks in the wall, Metamorphic Rock • Formed when chemical reactions, extreme heat or pressure change an existing rock form • May begin with either sedimentary or igneous rock Metamorphic classification – by texture • Foliated –(Latin word for leaf) – thin and flat, break in layers – Example slate and gneiss (nice) Kinked telephone book as an analogy for how kink bands form: a highly layered structure (phone book or foliated metamorphic rock) is compressed from the sides, resulting in kinking in order to accommodate the shortening of the pages/foliation. Red Slate Metamorphic classification – by texture con’t • Unfoliated – won’t break in layers – Example: Marble or quartzite Marble Nodular gray marble Dentritic Quartzite Rock Cycle