USGS Weekly Update 2008-Feb-29 10:26
Summary The pause in lava dome growth continues, and all our monitoring instruments show trifling or nil volcanic-related activity. This pause, which began in late January 2008, was recognized by absence of measurable growth among successive fixed-camera images, nearly quiescent seismicity, and the absence of tilt signals that might characterize extrusion of lava from the conduit.
We continue to monitor closely for evidence of renewed extrusion or other activity. The new lava dome remains hot in places; thus, it is capable of producing hot avalanches or small steam explosions that could cause hazardous conditions in and around the crater. Sudden melting of snow and ice could send small lahars onto the Pumice Plain and perhaps down the Toutle River as far as the Sediment Retention Structure (SRS). Ash clouds from explosions could affect aircraft.
Recent Observations: On a daily basis, a small steam plume rises above the active spine but usually dissipates before reaching crater-rim height. Under optimal atmospheric conditions this plume may ascend above the rim and be visible to residents and travelers in southwest Washington and northwest Oregon. This morning a small lenticular cloud formed above the volcano, owing to a changing weather system.
This past week field crews took advantage of good weather to repair a GPS antenna at Johnston Ridge Observatory, improve a radio connection for data transmission from Coldwater Ridge visitor center, and replace a bent antenna at one of our voice-communication repeater sites.
For the past month, locatable earthquakes at Mount St. Helens have been fewer than one per day, all smaller than magnitude 2. Ground tilt measurements show an overall sluggish subsidence in the area of the new dome. A GPS receiver on the active spine settles about 2 cm daily on a southward path.
Mt. Fitzherbert