THE SHERMAN CRATER ERUPTIVE PERIOD AT MOUNT BAKER, NORTH CASCADES--A.D. 1843 TO PRESENT--IMPLICATIONS FOR RESERVOIRS AT THE BASE OF THE VOLCANO
The phreatomagmatic phase of the eruptive period ceased before 1891, as the crater was then "ice-filled." Thermal activity continued at reduced levels until approximately the 1930's. Thereafter, aerial photos record loss of ice and snow in the crater, climaxing with the well-documented tenfold increase in aseismic thermal activity in March 1975. Activity declined by 1976, but not subsequently to pre-1975 levels. Continuing significant gas emissions, mainly CO2, are monitored by the USGS.
Collapse probability will rise with significantly increased activity at Sherman Crater. Volume of the 1845-1847 lahar was 15-25 million m3; volumes of 3 collapse lahars from the same, hydrothermally altered sector of the volcano during the mid-Holocene were 50-200 million m3, substantially greater than believed possible in 1975. Based on these case histories and assessment of any renewed activity, rapid drawdown to reduce spillway-level capacities (total storage of Baker Lake: 390 million m3; Lake Shannon: 200 million m3) is recommended when authorities are advised by scientists. Drawdown, also done in 1975, can accomodate potential lahar inflows, thus minimizing risks of downstream flooding from displaced water as well as those of shoreline inundation by lahar-induced waves.