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The chemical weathering of feldspars (granites), which release ions. |
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Where pools of water containing the appropriate ions in concentration dry out. Typically a very arid (dry) climate. |
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Water runoff from mountains collects in rapidly drying desert lakes. eg. Death Valley; Great Salt Lake |
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high water areas along arid coastlines eg. Persian Gulf, Saudi Arabia |
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found on continents that fill with marine water eg. Michigan Basin; Gulf of Mexico |
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non-marine evaporite (Boron) once used as a cleaning agent eg. 20 Mule Team Borax |
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the salt layers are less dense than the other sediments and slowly flow upward, forming a dome or diapir. |
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ionic bond - salt of our blood and tears used in food production and preservation, water softening, to melt snow and ice |
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used to make plaster eg. frescos |
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occurs as a native element near the fumeroles of volcanoes more commonly mined by sending hot water into salt domes to melt the sulfur |
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used in war - suffocating gases; gunpowder today most used to manufacture drugs, fertilizers, explosives, and pesticides |
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comes from the evaporite mineral borax mined in Death Valley used in glass products (Pyrex), laundry and cleaning products, food preservatives, ceramic glazes |
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nitrogen, phosphorous, and potassium are the main materials in modern fertilizers |
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the numbers (eg. 5-10-10) on fertilizer bags refer to % of nitrogen (N), phosphorous (P), and potassium (K) (N) - green leaf growth (P) - roots + flowers (K) - fruit |
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natural nitrate evaporite deposits that are extremely rare - very soluble occur in very dry regions (eg. Atacoma desert in Chile) or caves produced from manure and urine |
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mostly obtained synthetically from atmospheric nitrogen and natural gas by the Haber Process - produces ammonia most important chemical process of 20th century - prolonged WWI and led to the population explosion as fertilizers increased food production |
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found in guano deposits from birds and in bone pilgrims learned from Indians to bury fish and bones with corn - bone meal problem: insoluble when dissolved in sulfuric acid, becomes soluble (superphosphate) |
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comes from evaporite materials such as sylvite huge deposits in Canada, New Mexico, Texas, Oklahoma, and Kansas |
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ability to be easily shaped |
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combines with other elements to take on significant new properties tend to have superior properties to the original metal |
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accounts for more than 95% by weight of all metals consumed because: - abundance - 3rd most abundant metallic element after silicon and aluminum
- ease of smelting - separating metal from its ore
- easily alloyed - results in tempered, sharpened, and welded objects that are exceptionally strong and durable
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an alloy of iron and other elements - corrosion resistance - add nickel
- high temp. hardness - add chromium, cobalt, tungsten, molybdenum
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Iron ores can be formed in igneous plutons such as: (2 examples) |
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- magnetite crystallizes in pluton's magma and settles to bottom of the deep magma chamber forming thick layers
- hydrothermal deposits - hot water-rich fluids escape from magma chamber or come from groundwater into fractures surrounding rock crystallizing iron minerals
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Iron ores can be formed by sedimentary activities such as: (3 examples) |
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- Bog Iron Deposits - (Revolutionary War) smallest deposits; occur in formerly glaciated and coastal regions where bogs with decaying vegatations interact with iron-rich clays
- Ironstones - (Civil War) many sandstones and shale contain hematite cements that originally from the leaching of huge quantities of iron from old soil
- Banded Iron Formations - most abundant source of iron (nonrenewable); consists of alternating bands of hematite and red chert; Lake Superior area
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most is done by open pit (surface) mining; removed in a series of steps called benches most iron ore must be further concentrated (beneficiation) - removing impurities and packed into small pellets to be shipped to the smelters |
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process of separating a metal from the impurites in the ore |
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began more than 4000 years ago in Anatolia, Egypt, and Mesopotamia Iron Age replaced Bronze Age around 1200 BC |
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ingredients: - coke (C) - heating coal in absence of air
- limestone - used to absorb/separate undesirable elements; creates slag
- iron ore
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a glassy-like material recycled as concrete aggregate and railroad ballast |
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second most abundant metallic element in earth's crust very hard to free from the minerals in which it occurs lightweight and resistant to weathering less effective in conducting electricity |
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found at pyramid on top of Washington monument (once worth more than gold) - used in packaging and containers (35%)
- transportation - over 150lb in avg. car (20%)
- building (18%)
- electrical wire (9%)
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in many silicate minerals (feldspar micas); rarely found concentrated enough to make an ore Bauxite - ore of aluminum; forms as part of a soil in tropical climates |
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any rock that contains a sufficient concentration of a material to be economically and legally extracted |
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requires abundant, cheap electricuty (usually shipped to Norway, Canada, US) mixed with cryolite and electrodes; electricity is passed through, and molten aluminum forms around electrodes |
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making a new aluminum can from old ones requires only 5% of the energy needed to make a new one from bauxite |
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occurs as a native element Copper Age brought humans out of Stone Age around 6000 years ago |
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- during WWII, copper so important pennies were made of steel
- electrical wires
- pipes for plumbing
- alloys bronze (copper + tin) and brass (copper + zinc)
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Bingham Copper Mine - Utah |
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porphyry copper formed from igneous hydrothermal solutions largest man-made excavation in the world - 2.5 miles wide and .5 miles deep 15 million tons of copper have been removed |
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soft and resists corrosion and rusting - used for galvanizing steel used to make brass used as zinc oxide in paint pigments, ointments, and lotions to prevent sunburns |
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very dense, soft, and has a low melting temperature used in automobile batteries, additive in gasoline, in paint pigments, ammunition, in electrical and plumbing solder, and for x-ray and radioactive shielding more malleable than gold |
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metallic gold is soft, malleable, dense and corrosion-free (noble metal) |
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gold deposits first form as hydrothermal solutions, typically in altered country rock (rock that was there before magma) around granite magmas |
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are water-rich fluids containing lots of left-over quartz, feldspars, even micas from the granitic magma along with much heavier elements (gold, silver, copper, etc) often form veins in the country rock with very large crystals called pegmatites |
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original gold deposit (the dream find of every prospector) |
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Placers or Placer deposits |
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where most gold is found the mother lode erodes and the gold survives, transported by water gold settles-out on stream bottoms (in unconsolidated sands and gravels) which can be shoveled or dredged in pans or into long sluiceways.
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