In reply to Submit to Gravity:
Definitely not deliberate; these sorts of deposits are bad news for local ecosystems - the reason the water was so clear is probably because just about everything in it is dead! The precipitated calcite smothers the ecosystem and the high pH of the water means that some metals can be transported in solution more easily - so not good for anything that might drink from the stream.
It's a similar process to the one which produces stalactites in caves but because quicklime is much more unstable than limestone, it dissociates in water much more readily - you get much more calcium in solution. The tufa deposits in your photos would have taken hundreds of thousands of years to form from rainwater in limestone.