Minerals Building Blocks of Rocks Minerals Building Blocks of Rocks.
ROCKS AND MINERALS Chapters 2 & 3 Test 2 material Begin.
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Transcript of ROCKS AND MINERALS Chapters 2 & 3 Test 2 material Begin.
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ROCKS AND MINERALS
Chapters 2 & 3Test 2 material
Begin
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Grand Canyon
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RELATIVE TIME
TIME IN RELATIONSHIP WHILE COMPARING ONE ROCK LAYER WITH ANOTHER
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GEOLOGIC LAWS - SUPERPOSITION
EACH LAYER OF ROCK IS OLDER THAN THE LAYER ABOVE IT AND YOUNGER THAN THE LAYER BELOW IT
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GEOLOGIC LAWS - CROSS CUTTING
WHEN ROCKS CUT THROUGH OTHER ROCKS, THEY ARE ASSUMED TO BE YOUNGER THAN THE ROCKS THEY CUT THROUGH
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GEOLOGIC LAW - INCLUSIONS
PIECES OF OLDER ROCK CONTAINED WITHIN A YOUNGER ROCK
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TYPES OF FOSSILSPETRIFICATION - TURNED TO STONEINDIRECT EVIDENCE - TRACE OF ITS EXISTENCE (COPROLITE)ACTUAL REMAINS - SHELLIMPRINT - BIRD TRACKS OR WORM BURROWSONLY FOUND IN SEDIMENTARY ROCK
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PETRIFICATION
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COPROLITE - INDIRECT
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SHARK TOOTH – ACTUAL
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IMPRINT
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OPPOSING THOUGHT - UNIFORMITARIANISM
SAME PHYSICAL PROCESSES ACTIVE TODAY HAVE BEEN OPERATING THROUGHOUT GEOLOGIC TIMEPRESENT HOLDS KEY TO PASTJAMES HUTTON - FATHER OF MODERN GEOLOGY
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OPPOSING THOUGHT - CATASTROPHISM
CATASTROPHIC OR CATACLYSMIC EVENTS HAVE ALTERED DEPOSITION AND EROSION THROUGHOUT TIMESCABLANDS OF IDAHO - 100,000 YEARS OF EROSION TOOK PLACE IN A 30 DAY PERIOD
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HOW ROCK DIFFERS ACROSS THE EARTH’S
CRUST
CONTINENTAL ROCK - GRANITE - SIAL WHICH IS COMPOSED OF SILICA AND ALUMINUM AND LIGHTER THAN OCEAN ROCKOCEAN ROCK - BASALT - SIMA WHICH IS HEAVIER AND COMPOSED OF SILICA AND MAGNESIUM
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GEOLOGIC CONCEPT - ISOSTACY
EQUILIBRIUM STATE IN EARTH’S CRUST FORMED BY THE RELATIONSHIP OF PORTIONS OF THE LITHOSPHERE & ASTHENOSPHERELOG FLOATING IN RIVER
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GEOLOGIC CYCLESHYDROLOGIC CYCLEROCK CYCLETECTONIC CYCLE
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MINERALINORGANIC SOLID NATURAL COMPOUND HAVING A SPECIFIC CHEMICAL FORMULA AND POSSESSING A CRYSTALLINE STRUCTURE THAT IS FIXED OR VARIES WITHIN A DEFINITE RANGE
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EXAMPLES OF MINERALSTALCGYPSUMCALCITEQUARTZSULFURHALITEGRAPHITE
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GALENAFLUORITEAPATITEMAGNETITEDIAMOND
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PHYSICAL PROPERTIES LUSTER - APPEARANCE OF LIGHT REFLECTED FROM A MINERAL - METALLIC OR NONMETALLICCOLOR - INHERENT OR EXOTICSTREAK - AFTER RUBBING MINERAL ACROSS A PORCELAIN PLATE THE LEFTOVER POWDER RESIDUE
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STREAK PLATE
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SPECIFIC GRAVITY - WEIGHT OF MINERAL TO EQUAL VOLUME OF WATERCLEAVAGE - ABILITY TO BREAK OR CLEAVE IN CERTAIN DIRECTIONS MORE READILY THAN OTHERSFRACTURE - DOES NOT BREAK IN CERTAIN DIRECTIONS
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CLEAVAGE
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FRACTURE
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MAGNETISM - CAN PICK UP WITH MAGNETTASTE - HALITEFEEL - TALC (SOAPY) GRAPHITE (OILY OR GREASY)ACID TEST - WILL FIZZ OR BUBBLEHARDNESS - SCRATCHING RESISTANT
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MOH’S SCALE OF HARDNESS
1 = TALC2 = GYPSUM2.5 = HUMAN FINGERNAIL3 = CALCITE4 = FLUORITE5 = APATITE5.5 = GLASS
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7 = QUARTZ10 = DIAMONDIF YOU SCRATCH IT WITH YOUR FINGER NAIL = LESS THAN 2.5CAN’T SCRATCH IT AND IT WON’T SCRATCH GLASS = 2.5-5.5SCRATCHES GLASS = GREATER 5.5
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MINERAL GROUPSSILICATES
OXYGEN & SILICON ATOMSSILICON-OXYGEN TETRAHEDRON [4 OXYGEN ATOMS SURROUNDING A MUCH SMALLER SILICON ATOM]FELDSPARS, QUARTZ, MICAS, HORNBLENDE, OLIVINE, AUGITE
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SILICON-OXYGEN TETRAHEDRON
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NON-SILICATE MINERALSCARBONATES - CALCITE & DOLOMITEHALIDES - HALITE & FLUORITENATIVE ELEMENTS - GOLD, COPPER, DIAMOND, GRAPHITE, SILVERSULFATES - GYPSUMSULFIDES - GALENA & PYRITEOXIDES - MAGNETITE & HEMATITE
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USES OF NON-METALLIC MINERALS
APATITE - FERTILIZERSASBESTOS - FIBERSCALCITE - CHEMICALS, CEMENTCLAY [KAOLINITE] CHINA, KAOPECTATEFLUORITE - GLASS, CHEMICALSGRAPHITE - PENCIL LEAD
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GYPSUM - PLASTER OF PARISHALITE - TABLE SALTMUSCOVITE - ELECTRICAL INSULATORSULFUR - CHEMICALSTALC - BABY POWDER, PAINTS
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GEMSTONESPRECIOUS
DIAMONDEMERALD [BERYL]OPALRUBY [CORUNDUM]SAPPHIRE [CORUNDUM]
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DIAMONDS
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EMERALDS
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GEMSTONESSEMIPRECIOUS
AMETHYST - QUARTZCAT’S EYE - QUARTZGARNETJADE - JADEITEMOONSTONE - FELDSPARTOPAZTURQUOISEZIRCON
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AMETHYST
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METALLIC MINERAL RESOURCES
ALUMINUM, CHROMIUM, COPPER, GOLD, IRON, LEAD, MAGNESIUM, MERCURY, NICKEL, PLATINUM, SILVER, TIN, TITANIUM, TUNGSTEN, URANIUM, ZINC
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ROCK TYPESIGNEOUSSEDIMENTARYMETAMORPHIC
ROCK CYCLE
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IGNEOUS ROCKSFORM WHEN MAGMA OR LAVA COOLS AND CRYSTALLIZESCOOLS RAPIDLY HAVE SMALL CRYSTALS - EXTRUSIVECOOLS SLOWLY HAVE LARGE CRYSTALS - INTRUSIVE
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INTRUSIVE IGNEOUS ROCKS COOL SLOWLY IN THE CRUST (MAGMA)EXTRUSIVE IGNEOUS ROCKS COOL RAPIDLY AT THE SURFACE (LAVA)WHICH WILL HAVE THE LARGE CRYSTAL SIZE?
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CLASSIFYING IGNEOUS ROCKS
MINERAL COMPOSITIONTEXTURE - OVERALL APPEARANCE OF ROCK BASED ON SIZE & ARRANGEMENT OF CRYSTALS
FINE-GRAINEDCOARSE-GRAINEDPORPHYRITICGLASSY
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GLASSY
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FINE-GRAINED
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COARSE-GRAINED
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PORPHYRITIC
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IGNEOUS ROCKSGRANITEBASALTPUMICEOBSIDIANRHYOLITE
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RHYOLITE
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SEDIMENTARY ROCKSBITS AND PIECES OF EXISTING ROCK ARE TRANSPORTED THEN LITHIFIED BY COMPRESSION, COMPACTION, AND CEMENTATIONLAID DOWN IN HORIZONTALLY LAYERED BEDSONLY ROCK TYPE TO CONTAIN FOSSILS
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CLASSIFYING SEDIMENTARY ROCKS
DETRITAL SEDIMENTARY ROCKS - ORIGINATE AS SOLID PARTICLES FROM WEATHERED ROCKSCHEMICAL SEDIMENTARY ROCKS - SOLUBLE MATERIAL PRODUCED BY CHEMICAL WEATHERING
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CLASSIFICATION BY PARTICLE SIZE - DETRITALBOULDER, COBBLE, PEBBLE = GRAVEL = CONGLOMERATE OR BRECCIASAND = SAND = SANDSTONESILT = MUD = SILTSTONECLAY = MUD = SHALE
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GRAVEL-SIZED
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SAND-SIZED
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SILT-SIZED
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CLAY-SIZED
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SEDIMENTARY ROCKSCONGLOMERATESANDSTONESILTSTONESHALELIMESTONEPEAT MOSS & LIGNITE COALBITUMINOUS COAL
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METAMORPHIC ROCKSTRANSFORMED FROM PRE-EXISTING ROCKS BY EITHER HEAT, PRESSURE, OR CHEMICAL ACTIONFOLIATED (BANDS OR LAYERS) AND NON-FOLIATED
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FOLIATED METAMORPHIC ROCKS
SLATESCHISTSGNEISS
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FOLIATED ROCK
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NON-FOLIATEDMETAMORPHIC ROCKS
MARBLEQUARTZITE
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NON-FOLIATED ROCK
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OLD ROCK TO METAMORPHIC EQUIVALENT
GRANITE BECOMES GNEISSMICA BECOMES SCHISTSHALE BECOMES SLATELIMESTONE BECOMES MARBLESANDSTONE BECOMES QUARTZITEBITUMINOUS COAL BECOMES ANTHRACITE COAL
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Yosemite Valley