Earth Materials презентация

3- 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

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Environmental Geology Chapter 3 Earth Materials


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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


Слайд 3Basic 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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Слайд 4Basic Building Blocks
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Слайд 5
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http://chemistry.about.com/library/pdfs/PeriodicTableMuted.pdf


Слайд 6Basic Building Blocks
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Minerals
Naturally occurring
Inorganic
1 or more element
Solid, crystalline structure, atoms in a fixed

pattern

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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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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

Слайд 10Rock 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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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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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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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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Physical Weathering


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Chemical Weathering


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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







Слайд 17Two 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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Слайд 18Sedimentary Rocks
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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.

Слайд 20Contact Metamorphism
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Слайд 21Regional Metamorphism
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Слайд 22Foliation
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Figure 3.27, page 84


Слайд 233-
Rock Cycle


Слайд 243-
Rocks as Indicators of the Past
Figure 3.30, page 87
Figure 3.31, page

88

Слайд 25Minerals
1A sulfur
2A native copper
3A graphite
4A galena (lead sulfide)
6A pyrite (fool’s

gold)
7A hematite
9A magnetite
11A halite
13A calcite
18A feldspar
20A quartz
21 A quartz
23 A mica, muscovite

Rocks
1B granite
2B granite, pegmatite
5B gabbro (oceanic crust)
8B basalt
12B obsidian
13B volcanic breccia
15B sandstone, siliceous
16B sandstone, arkose
17B shale
20B limestone, chalk
22B limestone, travertine
24B coal, bituminous
25B slate
30B quartzite
31B marble
32B anthracite coal

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