5
$\begingroup$

Near Prague,Czech Republic is old lime mine. Most of it is closed but one short transport tunnel under one hill is publicly accessible. Tunnel has profile around 2,5x2,5m and it's slightly bended and it's about 100m long. I estimate that hill above it is about 50m high from floor of tunnel. Aproximate location: 50°02'28.0"N 14°22'32.1"E

In middle of tunnel this immediately caught my attention, as it was reflecting light from my headlamp a lot. Its like some very wet yellow coating on rock side of tunnel.

Area on photo is 2m wide and 1-1,5m high. Tunnel was completely dark, and only source of light was headlamp and flash in my camera so the photo is quite dark

According to geological map of area the base rock is Lime and Hornblende from lower devon,emsian

What is this coating? I found this site post-trip, so I tried to answer all question in quide as best I can and I can go into that tunnel again and provide all needed information

Strange coating in old lime mine shaft

$\endgroup$
  • $\begingroup$ blue portions could be some sort of bacteria?? $\endgroup$ – Always Confused Aug 9 '16 at 14:54
  • 1
    $\begingroup$ @AlwaysConfused the blue/black portions is rock without coating $\endgroup$ – Rfilip Aug 10 '16 at 8:10
5
$\begingroup$

Given your description of the base rock and the age of the mine I would suggest that what you are seeing is what in a cave we would refer to as flow stone (A deposit of Calcium Carbonate in one or more of many crystal structures).

Simplified Process:

Ground water often has varying degrees of dissolved carbon dioxide in it. This carbon dioxide within the water creates a mild acid, carbonic acid. The acid in the ground water will corrode out Calcium Carbonate in the base rock. Most ground water will be saturated with Calcium Carbonate, the lime, depending on the concentration of dissolved carbon dioxide in the water. When the water seeps out of the walls of the mine it has an opportunity to off gas some of the dissolved carbon dioxide. When this occurs the water can no longer hold as much dissolved Calcium Carbonate and the excess is deposited on the walls in various forms. The mechanism of dissolving the rock and re-deposition is driven by various equilibrium reactions( involving temperature, water mixing, partial pressures of the gases...). A karst hydrologist/geologist would be able to give you much more detailed information on the processes. It is this process that forms caves and causes the formations with the caves to form.

The following web site gives a pretty straight forward explanation of what I believe you are seeing. https://en.wikipedia.org/wiki/Karst

|improve this answer|||||
$\endgroup$

Your Answer

By clicking “Post Your Answer”, you agree to our terms of service, privacy policy and cookie policy

Not the answer you're looking for? Browse other questions tagged or ask your own question.