Another is that limestone is primarily
precipitated from seawater, as explained on pages 263 — 268.
Not exact matches
Usually, marine algae scavenge mercury
from seawater and
precipitate it onto the sea floor, where it no longer threatens most marine species.
Sulphate composition of
seawater is constant so that has no effect (it's
precipitated out as Calcium Sulphate) and change in CO2 is predominantly
from the atmosphere not volcanoes.
Finally, the reaction leaves behind a highly alkaline warm solution, between pH 9 and 11, which when vented
precipitates carbonate
from the
seawater, building white carbonate limestone - like «chimneys» that can grow to great heights.