Notes 9.29-10.8
· Apatite:
~ hardness 5
~ Ca3(PO4)3
· PO4 ~ comes from poop or apatite
· Fluorite:
~ hardness 4
~ CaF2
~ purity crystals (cubes on octahedron)
~ usually blue, green, purple, or clear
· Halite salt:
~ NaSl
~ slippery
~ dried salt
~ unusually perfect cubes
~ evaporate
· Pyrite:
~ FeS ß weathers quickly into Fe2O3
~ “fool’s gold”
~ brittle
~ not stable at Earth’s surface à rusts
~ usually comes out of mines
· Galieno:
~ PbS
~ main ore of lead; heavy
~ silvery, shinny, usually cube, dense
~ usually found with pyrite because of similar characteristics
· ore ~ economical term for rocks that have a substantial amount of certain minerals that have value
· hydrothermal deposit ~ both pyrite and galeno relates to volcanoes when both are dissolved by boiling water heated by volcanoes
· pegmatite veins:
~ last rocks to form when a big body of felsic magma cools
~ cools slowly
~ forms deep underground
· rocks transmit heat poorly
· composition “differentiates” because same elements are preferentially excluded or included from crystals à water is excluded because it is one of elements which is excluded from crystals
· plate tectonics occur because water decreases melting temperature of rocks
· amaenite:
~ occurred during Mesozoic period
~ helps dating
· halite:
~ found in deserts
· salt crystal:
~ different from calcite
~ identified by 60°/120° angles
~ rectangular
· Beryl:
~ emerald, aquamarine, morganite [gemstone varieties]
~ hardness 7.5-8
~ emerald ~ green
~ aquamarine ~ pale blue
~ morganite ~ catch-all term for other gemstone beryl-dear, yellowish
varieties of beryl emerald
aquamarine morganite
· Tourmaline:
~ black/brown is “schorl” (most common)
~ gems are usually pink, blue, or green (many colors)
~ parallel “striation” lines down long axis
schorl varieties of tourmaline
· Garnet:
~ burgundy, purple color (dark)
~ very common, small
~ large variety of colors
~ can grow very large
~ black - melonite
~ birthstone of January
garnet melonite
· Kunzite:
~ local variety - pink
~ spudomene
ß kunzite ß spudomene
· Climate:
~ energy entering air/water = sun + geothermal heat
~ sun is about 1km/m² of sunlight hits the earth
~ cross sectional area of Earth:
A = πr² = π(6.38 x 10^6m)² = 10^14m² = 10^117W of solar power ß rough estimate
~ geothermal heat ~ 32tw = 3 x 10^13W ß rough estimate
~ geothermal heat escapes through volcanoes
· the earth loses energy from reflection & radiation
· all objects radiate hear all the time
· as you heat something, you change the radiation & the total radiation
· Radiation:
~ energy out per m² = σeT^4
σ = constant
e = mother constant
T = temperature
(it can be really small of big because of the 4th power)
· The more an object is heated, the more energy is lost
· albedo ~ fraction of incoming light that is reflected à reflected light/absorbed light
· without the greenhouse effect, the earth would be freezing (like Mars)
· incoming sunlight mostly visible
· atmosphere is transparent in visible light
· Earth’s air: (mostly dry air)
~ N2 78%
~ O2 21%
~ Ar 1%
~ CO2 34%
· N2 & O2 are not considered greenhouse gasses because it doesn’t change in amount
· Ar & CO2 are green house gases
· H2O is usually between O2 & Ar; varies
· Humans have now doubled the amount of CO2 in the air
· Sun’s heat < inferred light heat
· If you freeze/boil the earth, the air will never come back
· Water vapor is a good greenhouse effect
· Climate feedback:
~ positive feedback - a change in a system that tends to lead to more of the same level of change
~ negative feedback - a change in a system that tends to prevent more of that same changes
· Positive feedback would be bad for the Earth because it would make earth into Mars or Venus