
Originally Posted by
yuzuha
Chert is what glues most sandstones and even arkansas stones together. It is basically quartz/silica, the same as agate, jasper, quartzite, opal,flint or novaculite etc. Silica is partially soluble in warm alkaline water and forms flocculant precipitates when the pH goes down. Hydrothermal action often partially dissolves sand (quartzite and sandstone), diatomacious earth (novaculite) and reprecipitates between the grains cementing them together, or silica laden waters dissolve and replace grains of carbonate or other mineral or form a dense cement around impurities (flint, jasper or agate etc). It varies like novaculite... the black stuff is full of manganese dioxide and dense chert cement around heavily dissolved diatom shells (which come in nearly every shape from little 5 micron balls to 200 micron long rods)... in the coarser novaculite stones the shells just less dissolved and not as heavily cemented together.