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| Mount Baker Stratovolcano last erupted |
Label
1975 - Increased Heat and Signs of Activity
By Mount Baker
In March 1975, local observers noted a dark column rising from Sherman Crater that sharply contrasted with previous white steam emissions. Over the next year numerous ashy plumes resulted in the formation of several small near-vent lahars.
In Spring 1975, scientists measured a ten-fold increase in thermal activity and detected magmatic gases, increasing concern that an eruption could occur. This was the first hint of volcanic activity in the Cascades since the 1914-1917 eruption of Lassen Peak in northern California. By the fall of 1975, melting of Sherman Crater glacier resulted in a snow-free area three times larger than typical summer exposure and revealed a shallow lake and previously unknown fumaroles.
Sherman Crater glacier's hole and enclosing lake, which melted during the 1975 increase in heat production from Mount Baker. Sulfurous fumarole to right of hole. (Spurgeon, Terry. Public domain.)
Sources/Usage: Public Domain.
Mount Baker's crater lake in 1976 formed due to glacial and snow melt as a result of increased heat from magma beneath the surface. Fumarole on left ejecting gas at a velocity of 268 kph (167 mph). (Credit: Kiver, Gene. Public domain.)
A major concern was that an eruption might cause the walls of Sherman Crater to collapse, sending lahars into Baker Lake reservoir and cause a wave to overtop, or significantly damage, the Upper Baker Dam. Either event would result in a large volume of water rushing into the Lake Shannon reservoir and potentially cause a surge of water over, or failure of, the Lower Baker Dam. Failure of the Lower Baker Dam would result in catastrophic flooding down the Skagit River with little to no warning. This was an especially worrying scenario for the town of Concrete, WA, which lies at the foot of the Lower Baker Dam.
As a result of the activity and hazard concerns, all potential monitoring tools available at the time were employed and the Baker Lake reservoir was lowered to accommodate possible lahars. This was truly the first extensive and modern monitoring campaign at a Cascade volcano. Monitoring techniques included installation of a seismic network, tilt monitoring, temperature measurements, fumarole and airborne gas sampling, crater meltwater analysis, and gravity measurements.
Fumaroles steaming within Sherman Crater, Mount Baker, Washington. (Scurlock, John. Public domain.)
Baker Lake shorelines were closed during 1975 increase in Mount Baker activity. This notice informed visitors of the reasoning and hazards associated with the renewed activity. (Public domain.)
As time passed, no clear signs of rising magma – earthquakes, significant changes in gas composition or emission rates, or surface deformation – appeared. The activity gradually declined over the following two years, but the amount of heat escaping from the ground stabilized at a higher level than before 1975. Field observations and on-site monitoring occurred sporadically in the 1990s and more regularly in the 2000s, which provides for a relatively long-term data set regarding the behavior of Mount Baker. The data collected suggests that magma may have intruded beneath the volcano in 1975, but it did not have enough energy to erupt. The magma stalled, likely in the form of a dike, and has been cooling since. The shallow magma heated the overlying hydrothermal system, which caused the observed increases in heat and gas emissions as well as providing energy for the steam explosions.
