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primary limestone chemical
calcium carbonate
calcium carbonate formula
CaCO3
karst
landscape with sinkholes, caves, and springs
how karsts form
water dissolves carbonate rocks
water + carbon dioxide → carbonic acid
H20+CO2→H2CO3
carbonic acid → hydrogen ion + bicarbonate ion
H2CO3→H*HC03
hydrogen ion + bicarbonate ion + calcium carbonate (in limestone)
H*+HCO3→Ca**+2HCO3
speleothems
travertine formations
flowstone
travertine sheets on walls
mammoth cave setting
mississippian limestone
zone of saturation for speleothems
unsaturated zone
exposure spring
aquifer exposed at surface
hypocrene spring
spring just below surface
gushet spring
waterfall on cliff face
helocrene spring
gentle slope trickle
limnocrene spring
pool by a fault
rheocrene spring
stream flows from fault
4 components of a geyser
heat, water, earthquakes, plumbing
eccentricity
changes in orbit roundness, 100,000 yrs
obliquity/tilt
changes in rotational axis, 41,000 yrs
precession
wobbles in axis, 23,000 yrs
3 ice ages
late proterozoic, permian, pleistocine
cold glacial record
low 18/16 ratio
zone of ablation
ice is melted or sublimated
glacial advance
accumulation greater than ablation
glacial retreat
ablation greater than accumulation
crevasse
fracture in glacier
terminus
end of glacier
moraine
sediment pile from glacier
eskers
snake channel for sediment under glacier
drumlins
tear-drop mound
paternoster lakes
chain of lakes going up (from glacier)
aretes
two glaciers make a ridge
horn
3+ glaciers carve a mountain peak
cirque
depression where glacier sits