Mount Shasta has erupted, on the average, at least once per 800 years during the last 10,000 years, and about once per 600 years during the last 4,500 years. The last known eruption occurred about 200 radiocarbon years ago. Eruptions during the last 10,000 years produced lava flows and domes on and around the flanks of Mount Shasta, and pyroclastic flows from summit and flank vents extended as far as 20 km from the summit. Most of these eruptions also produced large mudflows, many of which reached more than several tens of kilometers from Mount Shasta. Future eruptions like those of the past may endanger the communities of Weed, Mount Shasta, McCloud, and Dunsmuir located on or near the flanks of Mount Shasta. This report describes the likely nature of future eruptions and the threat that they present to people and property situated around Mount Shasta; accompanying maps delineate areas likely to be affected during future eruptions in the vicinity of Mount Shasta. Future eruptions will most likely consist of lava flows, domes, and pyroclastic flows. Lava flows and pyroclastic flows may affect low and flat- lying ground almost anywhere within about 20 km of the summit of Mount Shasta, and mudflows may cover valley floors and other low areas as much as several tens of kilometers from the volcano. Mount Shasta is not likely to erupt large volumes of ash in the future; areas subject to the greatest risk from air-fall tephra are located mainly east and within about 50 km of the summit of the volcano.
