Road to the Spring
Afton is a friendly place offering an assortment of Western shops, a few small motels and one new chain hotel (Fairfield Inn
). The signposted road (2nd Avenue) to Periodic Spring forks off Highway 89 in the town center, soon becoming unpaved and entering thick woodland, part of the Bridger-Teton National Forest
. It passes a shady USFS campground then follows the narrow canyon of Swift Creek
into the mountains (the Salt River Range
) for 4 miles to a parking area, where the track ends. For most of the way, the road parallels a large, green, newly constructed water pipe, which provides an improved supply to the nearby town. Some sections of the canyon walls show impressively jagged rock formations, composed of twisted strata inclined near vertically, though most is covered by dense forest - a mixture of fir, oak and aspen, some of which turn bright red/orange colors in the fall.
A wide, stony trail continues upstream from the parking area, climbing gently and staying close to the creek for nearly a mile until arriving at the base of the short side ravine that contains the spring.
The path splits, with one branch starting to ascend the steep hillside on the north side, and the other crossing the creek on a footbridge then going up the ravine to the spring; the last section is over boulders kept moist by spray from the exit stream, and so is liable to be slippery. The cliffs above are sheer, angular, dark and crumbling, enclosing the spring on three sides to create a cool, sheltered alcove. The actual source is less exciting to look at, since it has been modified to prevent rocks falling into the vent, and now has a concrete roof, metal baffles and assorted pipework, resulting in a rather unnatural appearance. The water typically flows normally for 15 to 20 minutes, decreases in intensity during the next few minutes and stops completely for several minutes more. The current resumes quickly, preceded by muffled subterranean noises, though without the sudden surge that characterizes a geyser. The cycle is best observed during mid to late summer, as at other times the periodicity is less evident. Intermittent springs are similar to cold water geysers in that they are not associated with geothermal activity, but such geysers derive their power from expansion of trapped carbon dioxide, so are quite different to the springs. Afton's spring was (re)discovered early in the 20th century by a local sawmill owner who observed the regular fluctuations of Swift Creek, and tracked up the canyon to find the cause, though long before this the location was known to the native Shoshone Indians.