A series of hot springs adjacent to the Lillooet River valley, such as the Harrison, Sloquet, Clear Creek and Skookumchuck springs, are not known to occur near areas with recent volcanic activity. Instead, many are located near 16-26 million year old intrusions of the Pemberton Volcanic Belt. The relationship of these hot springs to the Garibaldi Volcanic Belt is not clear. However, a few hot springs are known to exist in areas that have experienced relatively recent volcanic activity. About five hot springs exist at the Mount Cayley massif and two small groups of hot springs are present at the Mount Meager massif. The springs at Meager might be evidence of a shallow magma chamber beneath the surface. No hot springs are known to exist at Mount Garibaldi like those found at the Mount Meager and Mount Cayley massifs, although there is evidence of abnormal high heat flow at the adjacent Table Meadows and other locations. Abnormal warm water adjacent to Britannia Beach could be geothermal activity linked to the Watts Point volcanic centre.