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Earth Science A study in Change: Rocks Watch for & It will tell you when/where information will be used in this unit!

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Presentation on theme: "Earth Science A study in Change: Rocks Watch for & It will tell you when/where information will be used in this unit!"— Presentation transcript:

1 Earth Science A study in Change: Rocks Watch for & It will tell you when/where information will be used in this unit!

2 Rocks  Any sold mass of minerals, or mineral like material.  Inorganic solid, crystalline structure, definite chemical composition.  Isn’t a rock, just a rock? So what?  They aren’t static objects. They change with the earth and can tell us about it. Their timeline is just different than ours!

3 Most Common Minerals (pg 35) Know these!

4 Main Types of Rock  Igneous  Sedimentary  Metamorphic  Processes that change rock  Melting & cooling  Weathering & erosion  Compaction & cementation  Heat & Pressure

5 Igneous Rocks  Form from the cooling of magma or lava.  Magma = molten rock below the surface of the earth (625 o C or 1032 o F, low end)  Intrusive igneous rock  Composed of silicon, oxygen, & gases like water vapor  Lava = molten rock above the surface of the earth  Extrusive igneous rock  Similar in composition to intrusive igneous, without the gases (low pressure = escape)

6 Igneous Characteristics  Texture  Course grained - large crystals caused by slow cooling of magma, usually intrusive  Fine grained - small interlocking crystals due to relatively fast cooling  Glassy - cools too quickly to form crystals, may appear glassy, may not (obsidian vs. pumice)pumice  Porphyritic - both large and small crystals due to varying rates of cooling

7 Igneous Characteristics  Composition  Granitic - made up of mostly quartz or feldspar  Tend to be light colored  Basaltic- made up of mostly dark silicates, rich in magnesium and iron  Tend to be dark colored  Other - either a combination of the above or ultramafic (really old rocks)

8 Igneous Rock Examples Obsidian Lava flow= basaltGranite AphaniticPorphyritic

9 Sedimentary Rocks  Form when existing rocks are broken down into sediments and the sediments are cemented together to form a “new” (recycled) rock.  Weathering - process by which existing rock is broken down.  Physical weathering - breaking of a large rock into smaller pieces(physical changes)  Chemical weathering - changing of rock composition due to chemical changes

10 Processes Forming Sedimentary Rocks  Weathering  Ice wedging, root action, acid rain  Faster when there is lots of water in environment  Erosion - process by which weathered sediment is transported away from original parent rock.  Wind, Water, Ice, Gravity  Deposition - fancy term for when the eroded particles are dropped!

11 Processes Forming Sedimentary Rocks  Compaction - process of squeezing or smashing of deposited sediments into a smaller volume  Usually due to the weight of new sediments being deposited above.  Cementation - process of gluing sediments together  Dissolved minerals precipitate out of solution and are deposited in the space between sediments.

12 Classification of Sedimentary Rocks  Clastic Sedimentary- composed of weathered sediments and minerals  Conglomerate, sandstone, shale  Bits and pieces stuck together.  Looks or feels chunky  Chemical Sedimentary - composed from precipitates of dissolved minerals  Limestone, rock salt, gypsum(drywall)

13 Sedimentary Rock Examples Sandstone- Clastic Limestone -Chemical Conglomerate - Clastic

14 Metamorphic Rock  Formed when existing rocks are changed by heat and pressure(causes chemical reactions).  Heat - provides energy for chemical reactions  Earth structure provides heat source  Amount required to change a rock depends upon its mineral composition  Chemical Reactions - hot water containing other substances that allow recrystallization  Pressure - from all directions, affected by depth

15 Types of metamorphic rock  Foliated - layered or banded appearance of metamorphic rocks  Due to parallel orientation of mineral crystals  Forms when sedimentary rock is smashed  Nonfoliated - does not have banded texture, usually made up of only one mineral.

16 Metamorphic Rock examples Sandstone, before/after, nonfoliated Slate (parent = shale) foliated

17 Metamorphic Examples Marble nonfoliated Quartzite nonfoliated

18 Rock Cycle (final exam)


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