Pennsylvania Geology, v. 39, no. 4 - Pennsylvania Department of
Pennsylvania Master Naturalists Geology Workshop part 1 April 2012.
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Transcript of Pennsylvania Master Naturalists Geology Workshop part 1 April 2012.
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Pennsylvania Master Naturalists Geology Workshop
part 1 April 2012
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Sources • Chet & Maureen Raymo, Written in Stone, 1989• Joel Arem, Rocks & Minerals, Bantam Books, 1973• Bruce Goodwin, Geology of the Philadelphia Area, 1966• Commonwealth of Pennsylvania, Topographic and
Geologic Survey, Dept of Environmental Resources• Sarah West, “Gems of the Wissahickon,” 1995 • Wissahickon Photos by Sarah West• Aron Sando, Neree Wissahickon Worth Preserving 2007• Tarbuck & Lutgens, Earth, An Introduction to Physical
Geology, 2004• Stepanski & Snow Gem Trails of Pennsylvania and New
Jersey 1996
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Program Overview
Minerals:
Rocks:
The Rock Cycle
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Minerals• About 4000 different minerals have been identified• About 25 different minerals are common.• Over 90% are silicates• The building blocks of
rocks
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MineralsMinerals are• Inorganic substances• Naturally occurring• Solid• Possess and orderly internal structure• Have a definite chemical composition, a definite
formula, such as NaCl or SiO2
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Silicate Minerals
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Identification of Minerals
• By Crystal Form
• By Hardness
• By Streak Color
• By Luster
• By Cleavage
• By Specific Gravity
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Crystal FormIf space is available minerals form crystals
with a characteristic shape
Clear Quartz Garnet
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Table Salt, NaCl
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By Hardness
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Fracture vs Cleavage• Cleavage: the tendency of a mineral to
break along a plane of weak bonding leaving a relatively smooth surface. Minerals that cleave will break into similarly shaped pieces.
• Fracture: Minerals that do not show cleavage will fracture into pieces with irregular surfaces. Minerals that fracture will break into dissimilar pieces.
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Muscovite Mica & Biotite Mica cleave into thin sheets
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Orthoclase Feldspar. Cleaves in 2 planes at close to a 90o angle
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Fracture: Uneven breakage Concoidal Fracture Smooth fracture
glass or quartz Hematite
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Types of Luster
Metallic
Non-Metallic
• Dull
• earthy
• Glassy
• Pearly
• Silky
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Galena: metallic luster on right. Dull luster on left.
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Asbestos: Silky luster
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Orthoclase Feldspar: pearly luster
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Plagioclase Feldspar
(showing striations)
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Mineral Color is NOT a reliable identification property.
The color of a mineral depends on the inclusions that are present in the mineral crystal.
• Varieties of Quartz
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Streak Color is used for identification• The color left from rubbing a mineral along a ceramic
plate may be very different from the apparent color of the mineral
• Some minerals leave no streak color• Pyrite has a metallic luster but a dark gray streak
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Specific Gravity
• Ratio of the weight of a mineral to the weight of an equal volume of water
• Common rocks and minerals have a specific gravity of 2.5-3.0
• Metallic minerals have specific gravities 2 or 3 times greater. (Galena specific=7.6. Pure Gold =20)
• galena
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Other Properties used in Identification
• Reaction with Acid: Identifies Carbonates such as calcite & dolomite
• Magnetism: identifies Magnetite
• Flourescence
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Flourescence
• Sterling Hill Mine “Christmas Tree Ore”, Franklinite• Calcite fluoresces bright orange• Willemite: bright green• Hydrozincite: blue
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Rocks are mixtures of Minerals. They will not have a single formula representing their composition
.
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Rocks are classified according to the way they form as…
• Igneous
• Sedimentary
• Metamorphic
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Two Major Categories of Igneous Rock
Felsic: Are highest in Silica, Feldspar & Quartz. Form viscous, explosive magma– Granite, Andesite, Rhyolite
Basaltic: Are lowest in silica. High in Iron and Magnesium. Form less viscous, more liquid magma– Basalt, Diorite, Gabbro
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Felsic Igneous Rock
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Basaltic (Mafic) Igneous Rock
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Igneous Rocks are identified by
Component minerals
Texture
• Coarse Grained:
• Fine grained: Glassy
• Pyroclastic:
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Glassy or Frothy Textures result when cooling is very rapid as in explosive lava eruptions
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Texture reflects cooling rate or magma water content
When water content is high or cooling is very slow mineral crystals can grow large.
Pegmatite
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Process of Sedimentary Rock Formation
• Sediment deposition or precipitation– In water or blown by wind
• Sediment Burial– Sediments pile up over time
• Compaction– Weight of overlying layers compress the lower layers
• Cementation– Dissolved substances fill in spaces and join or cement
the particles
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Sedimentary Rocks are Identified by
Types of Sediments
• Detrital
• Chemical
• Organic
Particle Size
Presence of Fossils
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Detrital Sedimentary Rocksvary according to particle size
• Shale: mud particles predominate
• Sandstone: sand particles predominate
• Breccia :gravel particles predominate
• Conglomerate: gravel particles predominate
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Sediment Sorting by Particle Size
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Heavy Particles can settle in turbulent water.
The lightest particles settle only in still water
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Sandstone
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Breccia & Conglomerate
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Grand Canyon Bright Angel Shale
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Crossbedding indicates formation from c wind blown sediments
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Shale with fern fossil
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Chemical Sedimentary Rock forms from material that is carried in solution and later precipitates
Inorganic Chemical sedimentary rock• Vein Quartz
• Geodes
• Chert
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ChertAgate Jasper Flint
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Geodes
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Biochemical (organic) Sedimentary Rock
• Limestone CaCO3
• Dolomite CaMg(CO3)2
• Coral
• chalk
• Coquina
• Coal
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Coquina
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Chalk Cliffs of Dover
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CoalFormation
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Metamorphism produces:
• Layering
• Deformation– Uplift– Folding
• Recrystalization of minerals. Formation of gems such as mica, garnet. Staurolite, tourmaline etc.
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Eroded Folds, Marcia Jones King
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Metamorphic Rocks are classified by
Texture
• Foliated: layered
• nonfoliated
Grain Size
Folding or other deformation
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Metaconglomerate: Note elongation of pebbles and beginning of alignment into
layers
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Metamorphic Grades• Low
– Slate, phyllite
• Medium– Schist
• High– Gneiss, migmatite
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The Rock Cycle
• illustrates the origin of the basic rock types
• explains how rocks can be transformed from one type to another
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Rock Cycle
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Metamorphosis occurs at subduction zones when crustal plates collide
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Two Forces Drive the Rock CyclePart II
Plate Tectonics
• Produces new igneous rock
• Produces metamorphism of preexisting rocks
Weathering
• Produces sediments that are later compressed into sedimentary rocks
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Seeing is BelievingOne important objective of our field trip is to
appreciate and enjoy the natural beauty all
around us.