Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern...

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Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University

Transcript of Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern...

Page 1: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Rock Identification

Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University

Page 2: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Characterizing RocksCharacterizing Rocks

There are 3 major types of rocks

IGNEOUS – formed from molten magma

SEDIMENTARY – formed from sediment (soil, sand, etc,)

METAMORPHIC – formed by applying heat and pressure to other existing rocks

Page 3: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

The Rock Cycle – a representation of the interrelationship between different types of rocks.

Page 4: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Characterizing RocksCharacterizing Rocks

The three major characterizing features of The three major characterizing features of rocks are:rocks are:

• • ColorColor

•• Composition (Mineralogy/Chemistry)Composition (Mineralogy/Chemistry)

•• TextureTexture

Note: Even the most sophisticated Note: Even the most sophisticated geological classification schemes are geological classification schemes are based on these featuresbased on these features

Page 5: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Characterizing RocksCharacterizing Rocks

Classification by ColorClassification by Color

Color Index (used mainly for igneous rocks)Color Index (used mainly for igneous rocks)

• • Leucocratic – light colorLeucocratic – light color • • Mesocratic – intermediate colorMesocratic – intermediate color • • Melanocratic – dark colorMelanocratic – dark color

and/orand/or • • Felsic – rich in light colored mineralsFelsic – rich in light colored minerals • • Mafic – rich in dark colored mineralsMafic – rich in dark colored minerals

Page 6: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Igneous RocksIgneous Rocks

Textures of Igneous RocksTextures of Igneous Rocks

•• Aphanitic – fine-grained. Individual grains Aphanitic – fine-grained. Individual grains can’t be seen with naked eyecan’t be seen with naked eye

•• PhaneriticPhaneritic - grains easily seen with the - grains easily seen with the naked naked eyeeye

•• Porphyritic – larger grains in finer grainsPorphyritic – larger grains in finer grains •• Inclusions Inclusions

> > XenolithsXenoliths

>> Xenocrysts Xenocrysts

Page 7: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.
Page 8: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.
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Page 10: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Vesicular & Glassy Textures

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Xenoliths

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Xenocryst

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Sedimentary RocksSedimentary Rocks

Detrital & Chemical Rock ClassificationDetrital & Chemical Rock Classification

Detrital RocksDetrital Rocks Chemical RocksChemical Rocks

ConglomerateConglomerate LimestoneLimestone

SandstonesSandstones Chert Chert (Flint)(Flint)

SiltstoneSiltstone Salt Salt (Evaporite)(Evaporite)

ShaleShale

Page 16: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Detrital Sedimentary RocksDetrital Sedimentary Rocks

Detrital rocks are classified based on particle Detrital rocks are classified based on particle size and grain shapesize and grain shape

Page 17: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Detrital Sedimentary RocksDetrital Sedimentary Rocks

ConglomeratesConglomerates

– Poorly Sorted particle sizesPoorly Sorted particle sizes

– Well-rounded particlesWell-rounded particles

– Usually particles are gravel sizedUsually particles are gravel sized

Page 18: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.
Page 19: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.
Page 20: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.
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Detrital Sedimentary RocksDetrital Sedimentary Rocks

BrecciaBreccia

– Poorly sorted grainsPoorly sorted grains

– Angular grainsAngular grains

– Gravel sized grainsGravel sized grains

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Detrital Sedimentary RocksDetrital Sedimentary Rocks

SandstoneSandstone

– Well sorted particlesWell sorted particles

– Particles can be angular to roundedParticles can be angular to rounded

– Sand-sized ParticlesSand-sized Particles

Page 25: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.
Page 26: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.
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Detrital Sedimentary RocksDetrital Sedimentary Rocks

ShaleShale

– Microscopic grain sizeMicroscopic grain size

– Consist of silt and clay size grainsConsist of silt and clay size grains

– Cannot see grains with naked eyeCannot see grains with naked eye

– Occur in “quiet” depositional environmentsOccur in “quiet” depositional environments

Page 28: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.
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Chemical Sedimentary RocksChemical Sedimentary Rocks

ClassificationClassification

– Inorganic - Not produced by living things.Inorganic - Not produced by living things.

– Biochemical - Are produced by or are Biochemical - Are produced by or are

remnants of living things (e.g. shell remnants of living things (e.g. shell

fragments, coral reefs, etc)fragments, coral reefs, etc)

Page 31: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Chemical Sedimentary RocksChemical Sedimentary Rocks

LimestoneLimestone

– Most abundant chemical rockMost abundant chemical rock

– Inorganic (oolitic limestone, Inorganic (oolitic limestone,

Travertine) or Biochemical (Chalk, Travertine) or Biochemical (Chalk,

Coquina)Coquina)

Page 32: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Limestone (Chemical Rocks)Limestone (Chemical Rocks)

Travertine Travertine

– Common in cavesCommon in caves

– Happen when Happen when

calcium carbonate calcium carbonate

is precipitated out is precipitated out

of groundwaterof groundwater

Page 33: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Limestone (Chemical Rocks)Limestone (Chemical Rocks)

CoquinaCoquina– Consists of Consists of

loosely loosely cemented shell cemented shell fragmentsfragments

Page 34: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Fossiliferous limestone Limestone

Page 35: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Fine-grained limestone

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Chemical Sedimentary RocksChemical Sedimentary Rocks

Chert (Flint)Chert (Flint)

– Consists of Microcrystalline SilicaConsists of Microcrystalline Silica

– Two major occurrences of chertTwo major occurrences of chertIrregular shaped nodules in limestoneIrregular shaped nodules in limestone

layers of rocklayers of rock

– Most likely BiochemicalMost likely Biochemical

Page 37: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Cross-section through a geoid showing silica layering

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Flint

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Metamorphic RocksMetamorphic Rocks

Classified into two main groupsClassified into two main groups

– Foliated RocksFoliated Rocks

– Non-foliated RocksNon-foliated Rocks

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Page 42: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Foliated RocksFoliated Rocks

Progression of Shale to GneissProgression of Shale to Gneiss– SlateSlate Low Metamorphic GradeLow Metamorphic Grade– PhyllitePhyllite– SchistSchist– GneissGneiss High Metamorphic GradeHigh Metamorphic Grade

Metamorphic Rocks

Page 43: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Foliated TexturesFoliated Textures

Slaty - very fine-grained, fissileSlaty - very fine-grained, fissile

Phyllitic - fine-grained, foliated, shinnyPhyllitic - fine-grained, foliated, shinny

Schistose - foliated, large grains visibleSchistose - foliated, large grains visible

Gneissic - light and dark bandsGneissic - light and dark bands

Metamorphic Rocks

Page 44: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

SlateSlate

Parent RockParent Rock– ShaleShale

Slaty CleavageSlaty Cleavage

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PhyllitePhyllite

Parent Rock– Slate

Characteristic sheen/shine

Phyllitic Texture

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SchistSchist

Parent RockParent Rock– PhyllitePhyllite

Characteristic Characteristic scaly appearance scaly appearance

SchistositySchistosity

Page 47: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

GneissGneiss

Parent RockParent Rock– SchistSchist

Characteristic Characteristic of light and of light and dark bandingdark banding

Gneissic Gneissic TextureTexture

Page 48: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Non-foliated RocksNon-foliated Rocks

Rocks that show no FoliationRocks that show no Foliation

– Crystalline RocksCrystalline Rocks

– MarbleMarble

– QuartziteQuartzite

– Anthracite (coal)Anthracite (coal)

Metamorphic Rocks

Page 49: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

MarbleMarble

Parent RockParent Rock– Limestone Limestone

or Dolostoneor DolostoneReacts to AcidReacts to Acid

Page 50: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.
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QuartziteQuartzite

Parent RockParent Rock– SandstoneSandstone

Moderate to Moderate to high high metamorphismmetamorphism

Very HardVery Hard

Page 52: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.

Anthracite (coal)

Parent materialParent material– Plant matterPlant matter

High High metamorphismmetamorphism

Shinny and hardShinny and hard

Page 53: Rock Identification Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.