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Unlike most subduction zones around the world, Cascadia does not have a deep oceanic trench along its continental margin. Although no hot springs are known in the Garibaldi area, there is evidence of abnormally high heat flux at Table Meadows just south of Mount Price and elsewhere. Mount Price reaches an elevation of 2,049 meters (6,722 feet) and is one of several Garibaldi Belt volcanoes that were volcanically active during the Quaternary. There is also little seismic evidence of active subduction of the Juan de Fuca Plate. It could otherwise be attributed to explosive volcanism, but there is no fragmentary material around the rim to confirm this. Peléan eruptions can cause short- and long-term water supply problems for the city of Vancouver and much of the Lower Mainland. One of the common methods used to predict how much demand there will be for a particular commodity in the future is called market analysis.
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The basin was probably formed as a result of glacial action, as the northern side appears almost certainly covered by glacier. Like other volcanoes in the Garibaldi Volcanic Belt, Mount Price formed as a result of subduction zone volcanism. Both are at least 300 meters (980 feet) thick and 6 kilometers (3.7 miles) long and extend northwest and southwest. This basin consists of a granite wall surrounding the volcano on its western and southwestern sides. The northwest lava flow forms a volcanic dam known as the Barrier. Both lava flows form steep cliffs; The current face of the Barrier is the result of a landslide that occurred in the mid-19th century. The volcano was later overtaken by the Cordilleran Ice Sheet, which covered much of western North America during the glacial periods of the Quaternary. Their unusually large thickness results from their ponding and cooling against the Cordilleran Ice Sheet as they fill valleys at lower altitudes. As the Juan de Fuca Plate moves beneath the North American Plate in the Cascadia subduction zone, it creates volcanoes and volcanic eruptions. Following the retreat of the Cordilleran Ice Sheet from high altitudes less than 15,000 years ago, andesite eruptions of the third eruptive phase occurred from a satellite vent in Price Bay.