Earth Materials

Содержание

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3- Basic Building Blocks Atoms Nucleus contains protons and neutrons Electrons

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Basic Building Blocks

Atoms
Nucleus contains protons and neutrons
Electrons orbit the nucleus
Elements
Atoms with

the same number of protons
Hydrogen has one proton, Helium has two
Periodic Table of Elements
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Basic Building Blocks Isotope – an atom with varying number of

Basic Building Blocks

Isotope – an atom with varying number of neutrons,

some are unstable = radioactive decay
Ion – atom has gained or loss and electron and is positively or negatively charged
Sodium Na+
Iron Fe 3+
Chlorine Cl-
Oxygen 02

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Basic Building Blocks 3-

Basic Building Blocks

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3- http://chemistry.about.com/library/pdfs/PeriodicTableMuted.pdf

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http://chemistry.about.com/library/pdfs/PeriodicTableMuted.pdf

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Basic Building Blocks 3-

Basic Building Blocks

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3- Minerals Naturally occurring Inorganic 1 or more element Solid, crystalline

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Minerals

Naturally occurring
Inorganic
1 or more element
Solid, crystalline structure, atoms in a fixed

pattern
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3- Minerals 4,000+ minerals Each has unique chemical and physical properties

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Minerals

4,000+ minerals
Each has unique chemical and physical properties (for ex. -

graphite vs diamonds are both almost all C but different crystalline structures)
Physical properties controlled by structure and composition
Building blocks of rocks
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3- Rock Forming Minerals Approximately 12 common minerals make up crust

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Rock Forming Minerals

Approximately 12 common minerals make up crust
Pyroxene and Amphibole

are ferromagnesian silicates
Feldspars – aluminum rich silicates
Clay minerals – result from weathering of silicates, broken down by rainwater
Quartz – almost pure silicon and oxygen
Calcite - limestone
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Rock Forming Minerals Minerals classified on type of negatively charged ion

Rock Forming Minerals

Minerals classified on type of negatively charged ion within

crystalline structure
Sulfides contain sulfur bonded to positive Pb, Zn or Fe
Carbonates bonded to C and O
Oxides – negative charged O
Sulfates – negative charged SO4
Silicates – largest class, negatively charged Si and O4
Si and O make up 75% of crust by weight

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3- Rocks Aggregate or assemblage of one or more types of

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Rocks

Aggregate or assemblage of one or more types of minerals; many

are composed of several different minerals and some are one type of mineral
Texture is studied, way mineral grains are arranged. Coarse, fine or mixed grains and shape of grain.
Formed when magma cools, minerals precipitate out of solution; grains can grow. Or exposure to heat/pressure.
Three types
Igneous
Sedimentary
Metamorphic
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3- Igneous Rocks Form via cooling magma Intrusive cooled Coarse grained

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Igneous Rocks

Form via cooling magma
Intrusive cooled
Coarse grained
When magma breaches Earth’s

surface it is called lava.
Extrusive cooled
Fine grained
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3- Weathering Breaking down of rocks Physical weathering Frost wedging Plant

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Weathering

Breaking down of rocks
Physical weathering
Frost wedging
Plant roots
Crystal growth – minerals precipitate

out of solution
Fluctuations in daily temperature
Chemical
Dissolution
Hydrolysis
Oxidation / reduction
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3- Physical Weathering

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Physical Weathering

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3- Chemical Weathering

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Chemical Weathering

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3- Sedimentary Rocks Weathering results in sediment Compacted and cemented sediment

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Sedimentary Rocks

Weathering results in sediment
Compacted and cemented sediment = sedimentary

rocks
Erosion – sediment and ions removed from given area.
Rock or sediment dissolved, picked up by wind or water, or abraded
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Two Types of Sedimentary Rocks Detrital – made of preexisting rock

Two Types of Sedimentary Rocks

Detrital – made of preexisting rock &

mineral fragments that have cemented together
Material was deposited in low lying areas
Shale, sandstone
Table 3.2, page 80
Chemical – dissolved ions precipitate out of solution
Limestone, rock salt (halite)
Table 3.3, page 81

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Sedimentary Rocks 3-

Sedimentary Rocks

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3- Metamorphic Rocks Changes through heat and pressure, not enough to

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Metamorphic Rocks

Changes through heat and pressure, not enough to melt rock.


Contact metamorphism
Heat, low pressure
Nonfoliated texture, marble and quartzite
Regional metamorphism
heat, high pressure
Foliated texture due to pressure. Minerals reorient into parallel structure. Slate and gneiss.
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Contact Metamorphism 3-

Contact Metamorphism

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Regional Metamorphism 3-

Regional Metamorphism

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Foliation 3- Figure 3.27, page 84

Foliation

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Figure 3.27, page 84

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3- Rock Cycle

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Rock Cycle

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3- Rocks as Indicators of the Past Figure 3.30, page 87 Figure 3.31, page 88

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Rocks as Indicators of the Past

Figure 3.30, page 87

Figure 3.31, page

88