We had hoped to get all the way up to Mammoth Hot Springs on Monday, but, as usual, didn't have enough time. It made geographic sense to see Mammoth on the way out of the park, since it was near the exit we were planning to take.
Roadside Geology of Wyoming tell us that the water at Mammoth Hot Springs is not hot enough to form geysers. Instead, the area is "an excellent example of travertine terrace development." The book describes a complex chemical process whereby lime pours out over the limestone to create these lovely formations. "Geologists estimate that the waters of Mammoth Hot Springs carry more than 2 tons of dissolved lime to the surface each day, at a flow rate of 500 gallons per minute! In effect, Mammoth Hot Springs is a giant cement factory--about 8 inches of rock are deposited each year!" But it's not only geologically fascinating, it's beautiful, too.
While Mammoth was a beautiful and fascinating place, it was surprisingly crowded considering how far it was from the central areas of the park. We were annoyed by numerous examples of hogging multiple parking spaces, marching off the trail, and other poor behavior. By the time we left, we were ready to go on to a less crowded park.
Distance hiked: not sure, maybe 2 km
On to Glacier National Park.