The main group of springs is located about from the river. According to a U.S. government geologist in 1915, "At Democrat Springs, which are 5 miles below
Delonegha Springs, hot water issues on the southwest side of Kern River, within 150 feet of its edge, but 50 or 75 feet above its surface. In 1908 there was a substantial hotel, having accommodations for 100 people...The waters of these springs are sulphureted, but they do not seem to carry notable amounts of other mineral matter...With reference to the fault origin of these springs, it was learned that although the
earthquake of April 18, 1906, was not severely felt here, the main spring ceased flowing at that time. It was reopened a few months later by making a cut into the slope about 8 feet below the former point of issuance of the spring". The spring waters do contain "iron, sodium and other salts". According to
Kern River Country (1979), the resort had five springs. One that produced at was used for bathing while the other four were piped to a reservoir near the hotel that was used as a swimming pool. According to an earlier source, "At a third place another small spring forms a drinking pool." == See also ==