
These acidic hot springs have a limited supply of water. More water leads to less viscose “paint.”

In drier conditions the mudpots are thick and sluggish, bubbling slowly and belching clouds of gas - a bit like bucks night revellers after their 2am kebab.

The hottest surface vents are fumaroles. Their underground systems contain very little water, but reach far down into hot rock masses. When water does drain into the fumaroles’ plumbing, it converts instantly into steam and bursts out of the vent. The fumaroles above are actually shape shifters. When there's more water around, they're paint pots. When they dry out a bit, they turn into constant steam jets. I kept well clear of these vents. I’m still afraid of death by scalding.
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