the rock cycle
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Analyzing how rocks are formed Presented by Austin Prater, III. The Rock Cycle. What’s so special about a rock?. Can you think of any ways rocks are used in your everyday life? Aren’t all rocks pretty much the same? How will knowing the types of rocks help me in the future? - PowerPoint PPT PresentationTRANSCRIPT
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The Rock CycleAnalyzing how rocks are formedPresented by Austin Prater, III
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What’s so special about a rock? Can you think of any ways rocks are
used in your everyday life? Aren’t all rocks pretty much the
same? How will knowing the types of rocks
help me in the future? Did you know the all the rocks on
Earth get recycled over time?
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Mass of Land, Sky, & Sea in kg
Earth100%
Water0%
Sky0%
Earth's Spheres by Mass
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State Goals 12.11.82 Indicate that the earth's crust is made
from mostly igneous and metamorphic materials and was formed as a result of partial melting of part of the mantle rock. Know that there is a thin layer of sedimentary rock on top in many places.
12.11.87 Identify the properties of rocks and minerals based on the physical and chemical conditions in which they are formed, including plate tectonic processes.
12.E.4a Explain how external and internal energy sources drive Earth processes (e.g., solar energy drives weather patterns; internal heat drives plate tectonics).
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Learning Objectives
After this unit’s activities students should be able to:
Identify the 3 types of rocks based on their physical characteristics
Describe the processes involved with the formation of the types of rock
Classify samples of rocks based on their features and informational tables
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The Rock Cycle
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Here is another version of the Rock Cycle
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IGNEOUS ROCKS
Form by solidification (crystallization) of melted minerals
At the surface, LAVA hardens to form EXTRUSIVE rocks with tiny (FINE-GRAINED) crystals or GLASSY (no crystal) TEXTURES
Beneath the surface, MAGMA hardens to form INTRUSIVE rocks with easily visible (COARSE-GRAINED) crystal texture.
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Granite
Light-colored, coarse- grained, no pattern
Mostly quartz, feldspar, mica, and hornblende
Often used for buildings and monuments
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Basalt Dark-colored, fine-
grained, extrusive Formed where lava
erupted onto surface Most widespread
igneous rocks Found locally in the
Palisades along west shore of Hudson River, Connecticut River valley
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Gabbro
Dark-colored, coarse- grained intrusive
Similar composition to basalt—plagioclase feldspar with some pyroxene and olivine
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Obsidian
Natural volcanic glass
Forms when lava cools very quickly
Usually dark, but small pieces may be clear
Fractures along curved (conchoidal) surface
Used as spear and arrow points, kniveshttp://www.volcanoworld.org/vwdocs/vwlessons/lessons/Slideshow/Igrocks/Igrock7.html
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Pumice and other igneous rocks
Light colored, frothy (many air spaces)
Same minerals as in granite, but finer in grain size
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Sedimentary RocksSedimentary rocks may be made of rock fragments—sediments—or by chemical reactions. The classification of sediments is shown below.
http://www.volcanoworld.org/vwdocs/vwlessons/lessons/Sedrocks/Sedrocks6.html
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Clastic rocks–made of cemented sediments—are classified by their grain sizes.
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Non-clastic rocks form by chemical precipitation (settling out from a solution.) Limestone is made from calcite, chert from quartz, and halite is rock salt.
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Biologic sedimentary rocks come from the remains of organic matter.
The most important of these is coal. Anthracite coal results from the greatest pressure and releases the most energy when burned. Other varieties are bituminous and lignite. “Petrified” (permineralized) wood is another organic rock.
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More about sedimentary rocks
Shale is the most common sedimentary rock
Sedimentary rocks cover about three-quarters of the land surface
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Metamorphic Rocks
Formed by heat and pressure changing existing rocks
REGIONAL METAMORPHIC affects a large area and results from plate tectonics
CONTACT METAMORPHISM affects rocks on a local scale, such as “baking” sedimentary rocks next to magma or lava
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“Foliated” rocks contain much mica and other rocks that produce layering or banding
Gneisses and schists are examples of layering within rocks
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Non-foliated metamorphic rocks include marble, which comes from limestone, and quatzite, which comes from sandstone
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Illinois layers of rock