| Description |
The Kirkham Hot Spring is easily accessible on foot from the nearby national forest Kirkham campground. Summer season is usually quite busy and nightly closure from 10:00 p.m. to 6:00 a.m. is strictly enforced. Steamy waterfalls and hot pools make this site very inviting to the weary traveler.
The Kirkham Hot Spring is part of the South Fork Payette Geothermal System (SFPGS). This series of thermal springs is located along faults that fracture the Atlanta lobe of the Idaho Batholith. Seismic activity helps to keep the hydrothermal systems in this region active. A magnitude 7.3 earthquake, the highest magnitude ever recorded in Idaho, occurred as recently as 1983. Noticeable changes in flow rates of the springs were recorded near the epicenter which was located just north of the SFPGS.
The Idaho batholith is comprised of Cretaceous period micaceous granites, leucogranites, and gradiorites. Tertiary plutons of granite and diorite are also present (Druschel et al., 2001). |