the rock cycle
DESCRIPTION
THE ROCK CYCLE. BY: DANIELLE PERRY. INTRODUCTION. This slide show is intended to help you understand important types of rocks. The diagram in the next slide represents the ROCK CYCLE-a scheme that represents the processes of changes that connect the three major groups of rocks: SEDIMENTARY - PowerPoint PPT PresentationTRANSCRIPT
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THE ROCK CYCLEBY: DANIELLE PERRY
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This slide show is intended to help you understand important types of rocks.
The diagram in the next slide represents the ROCK CYCLE-a scheme that represents the processes of changes that connect the three major groups of rocks:
SEDIMENTARY IGNEOUS METAMORPHIC It also shows two other important parts of the “Rock
Cycle”-SEDIMENTS and molten LAVA and MAGMA Source: http://www.canadianrockhound.com/junior/rock
cycle.html
INTRODUCTION
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CLASSIFICATION OF ROCKS
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EXAMPLES OF NON-CLASTIC ROCKS
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Sedimentary rocks may be made of rock fragments-sediments-or by chemical reactions. The classification is shown below:
SEDIMENTARY ROCKS
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Shale is the most common sedimentary rock.
Sedimentary rocks cover about three quarters of the land surface.
For more about sedimentary rocks http:||www.rolcanoworld.org|vw docs
SHALE ROCK
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The most important of this is coal.
SEDIMENTARY ROCKS
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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 {COURSE-GRAINED} crystal texture.
IGNEOUS ROCKS
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Light-colored, coarse-grained, no pattern. Mostly quartz, feldspar, mica, and
hornblende. Often used for buildings and monuments.
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Dark-colored, fine-grained, extrusive. Formed where lava erupted onto surface. Found locally in Palisades along west shore
of Hudson River, Connecticut River valley.
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Dark-colored coarse-grained intrusive Similar composition to basalt-plagioclase
feldspar with some pyroxene, and olivine.
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Natural volcanic glass. Forms when lava cools very quickly. Usually dark, but small pieces may be clear. Fractures along curved {conchoidal} . Used as spear, and arrow points,and knives.
Obsidian
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PUMICE and RHYOLITE
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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.
For more information: http:/www.volcanoworld.org/vwdocs/vwdocs
lessons/lessonsMetrocks/Metrocks1.html
METAMORPHIC ROCKS
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FOLIATES, SLATE,GNEISS,SCHIST
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NON- FOLIATES