Dean M. Chriss
Photography
Cathedral City Pinnacles
(Click image to enlarge)
These tufa towers formed underwater between 11,000 and 25,000 years ago. They
form when calcium-rich groundwater enters alkaline lake water causing calcium
carbonate to precipitate. This slowly forms a
calcium carbonate tube or pipe around the groundwater's entry point. Tufa towers
stop growing when their tops become exposed, either because they reach the
lake's surface or because lake level drops. The tallest of these towers is about
140 feet (43 m) high.