Choquette Hot Springs, also known as Stikine River Hot Springs or Fowler Hot Springs, are located on the eastern bank of the Stikine River, approximately 23 kilometers (14 miles) from the Canada–U.S. border and about 1 kilometer (0.6 miles) north of the Choquette River. They are the northernmost of three spring systems along the lower Stikine and the only one situated in Canadian territory. The area consists of a series of hot springs and beaver ponds. Due to significant beaver activity and associated flooding, use of the springs has declined in recent years. As a result, most river travelers continue past this site and visit Chief Shakes Hot Springs farther downstream.
Access to Choquette Hot Springs is only possible by boat via the Stikine River. The springs can be reached by maneuvering a kayak or shallow-draft boat through a narrow side channel of the river. This channel lies almost directly across from an old cabin, once part of the Fowler homestead, which gave rise to the local name “Fowler Hot Springs.” The site is remote and requires precise navigation to locate the entry point and safely reach the springs.
Over 15 individual springs emerge from cracks in the bedrock walls along the flat valley floor, spanning about 60 meters (197 feet) along the cliffs. Many of these springs now drain into large beaver ponds, while several remain above pond level. The spring water is clear, odorless, and low in mineral content, composed mainly of chloride, sulfate, sodium, and silica. Water temperatures range between 50°C and 60°C (122°F to 140°F), with some historical reports noting temperatures as high as 66°C (151°F). Within the beaver ponds, the water is significantly cooler, averaging around 25°C (77°F), and some visitors have used these areas for swimming. In the southern portion of the main pond, submerged springs can be identified by visible gas bubbles and the upwelling of warmer water.
Choquette Hot Springs offer a remote and natural hot spring experience along the upper reaches of the Stikine River. The site is shaped by natural forces, including beaver activity, and features a mix of hot spring sources and cooler ponds. While difficult to access and rarely visited, the springs remain a striking example of the region’s geothermal landscape for those experienced and adventurous enough to reach them.
