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Mike Richards's avatar

The mud pots around the bottom end of the Imperial Valley always fascinated me, although I've never got to this one. There's quite a group of them at the Davis Schrimpf Seep Field at the SE of the Salton Sea - though from decades-old memories, it is a pretty miserable hot, dusty, muddy, smelly walk to get close to them.

These aren't actually geothermal features, they're driven by carbon dioxide rather than boiling water. Water and carbon dioxide are rising up along a zone of compression and liquifying the sediments to produce goop. Why the Niland Geyser moves is not clear as most of these features stay in one place. Maybe it wants to go swim in the Salton?

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