stu said:
Water (I know obvious) and oxygen levels are what count. Opening up passage ways usually blocked can lead to increase rate of growth.
So would be the concentration of calcium in the water, the availability of carbon dioxide, the evaporation co-efficient (hence your opened passage observation), and quite a few other variables.
For instance, take a cave under a limestone pavement, or very thin soils, like Swinstow or Simpsons in Yorkshire. Very little soils above = less nitrogen absorbed into the water (which now becomes very weak nitric acid) = less chemical erosion of the limestone = less calcium to come out of solution = less stall formation.
Or take St. Cuthberts or GB in the Mendips, where glaciation did not remove the soil and you get more profuse stal formation.
Or go to Jamaica under the tropical forests, where you will be lucky to see the roof for stal in many caves!
It's a very complex subject realy, but I will ask one question to the forum.
On flowstone and sometimes on stals you get micro-gours forming, and despite the angle of the slope they are forming on, the vertical period of the gours is predominantly 1cm. Why?