Editing Flowstone (section)

==Formation==
[[File:Tropfsteine.svg|right|thumb|Diagram of dripstone cave structures (flowstone labelled AB)]]
Flowing films of water that move along floors or down positive-sloping walls build up layers of [[calcium carbonate]] (calcite), [[aragonite]], [[gypsum]],<ref>Hill, C A, and Forti, P, (1997). Cave Minerals of the World,  (2nd edition). [Huntsville, Alabama: National Speleological Society Inc.] pp 193 and 196</ref><ref>Szablyár, P., (1981) “Morphogenetics of Umm al Massabih Cave (Libya)”, Karszt és Barlang, No. 1, P27-34. In Hungarian.</ref> or other cave [[mineral]]s. These minerals are dissolved in the water and are deposited when the water loses its dissolved [[carbon dioxide]] through the mechanism of agitation, meaning it can no longer hold the minerals in solution. The flowstone forms when thin layers of these deposits build on each other, sometimes developing more rounded shapes as the deposit gets thicker.

There are two common forms of flowstones, [[tufa]] and [[travertine]].  Tufa is usually formed via the precipitation of calcium carbonate, and is spongy or porous in nature.  Travertine is a calcium carbonate deposit often formed in creeks or rivers; its nature is laminated, and it includes such structures as [[stalagmite]]s and [[stalactite]]s.

The deposits may grade into thin sheets called "[[drapery (geology)|draperies]]" or "curtains" where they descend from overhanging portions of the wall. Some draperies are translucent, and some have brown and beige layers that look much like [[bacon]] (often termed "cave bacon").

Though flowstones are among the largest of [[speleothem]]s, they can still be damaged by a single touch. The [[sebum|oil from human fingers]] causes the flowing water to avoid the area, which then dries out.  Flowstones are also good identifiers of periods of past droughts, since they need some form of water to develop; the lack of that water for long periods of time can leave traces in the rock record via the absence or presence of flowstones, and their detailed structure.<ref name=Drysdale/>

===Concrete derived flowstone===
Flowstone derived from concrete, lime or mortar, can form on manmade structures, much more rapidly than in the natural cave environment due to the different chemistry involved.<ref name=Hill&Forti1997>Hill, C A, and Forti, P, (1997). Cave Minerals of the World,  (2nd edition). [Huntsville, Alabama: National Speleological Society Inc.] pp. 217 and 225</ref>
On concrete structures, these secondary deposits are the result of [[concrete degradation]],<ref>Macleod, G, Hall, A J and Fallick, A E, (1990). "An applied mineralogical investigation of concrete degradation in a major concrete road bridge". Mineralogical Magazine, Vol.54, 637–644</ref><ref name=SmithGK2016>Smith G.K., (2016). "Calcite straw stalactites growing from concrete structures", Cave and Karst Science, Vol.43, No.1, P.4-10, (April 2016), British Cave Research Association, ISSN 1356-191X</ref> when calcium ions have been leached from the concrete in solution and redeposited on the structure's surface to form flowstone, stalactites and stalagmites.<ref name=Hill&Forti1997 /> [[Carbon dioxide]] (CO<sub>2</sub>) is absorbed into the hyperalkaline leachate solution as it emerges from the concrete. This facilitates the chemical reactions which deposits [[calcium carbonate]] (CaCO<sub>3</sub>) on vertical or sloping surfaces, in the form of flowstone.<ref name=Hill&Forti1997 /><ref name=SmithGK2016 />

Concrete derived secondary deposits are classified as "[[calthemite]]s".<ref name=SmithGK2016 /> These calcium carbonate deposits mimic the forms and shapes of [[speleothem]]s, created in caves. e.g. [[stalagmite]]s, [[stalactite]]s, flowstone etc. It is most likely that calthemite flowstone is precipitated from leachate solution as [[calcite]], "in preference to the other, less stable [[polymorphism (materials science)|polymorphs]], [[aragonite]] and [[vaterite]]."<ref name=SmithGK2016 />

Other trace elements such as iron from rusting reinforcing or copper oxide from pipework may be transported by the leachate and deposited at the same time as the CaCO<sub>3</sub>.<ref name=SmithGK2016 /> This may cause the calthemites to take on colours of the leached oxides.<ref>White W.B., (1997), “Color of Speleothems”, Cave Minerals of the World, (2nd Edition) Hill C. and Forti P. [Huntsville, Alabama: National Speleological Society Inc.] 239-244</ref><ref name=SmithGK2016 />