{{Ligam web | last = Schilling | first = Steve P. | coauthors = David W. Ramsey, James A. Messerich, and Ren A. Thompson | títol = USGS Scientific Investigations Map 2928: Rebuilding Mount St. Helens | url= http://pubs.usgs.gov/sim/2006/2928/ | date = 2006-08-08 | accessdate = 2007-03-07 }}</ref>
Amb la recenta activitat volcanica que comencèt en 2004, los lòbes del glacièr son butats suls costats e cap amont per la creissença del dòma volcanic novèl. La superfícia del glacièr s'es ara asladaasclada e presenta [[crebassa]]s e [[serac]]s amor del movement del sòl del cratèr. Lo dòma volcanic novèl a desseparat lo glacièr en un lòbe oèst e un lòbe èst. Malgrat l'activitat volcanica, lo tèrme del glacièr a sempre avaçat, amb una avança considerabla del costat èst, situat a l'ombra de la paret del cratèr. DuePr'amor tode the advancel'avança, twolos lobesdos oflòbes thedel glacierglacièr joinedse togetherson inrejonh lateen Maymai de 2008 ande thusara thelo glacierglacièr completelyenroda surroundscompletament thelo lavadòma domesvolcanic.<ref name="NT">{{Ligam web|títol=MSH08_aerial_st_helens_crater_from_north_05-30-08|url=http://vulcan.wr.usgs.gov/Imgs/Jpg/MSH/MSH08/MSH08_crater_glacier_arms_touching_05-30-08_med.jpg|publisher=[[United States Geological Survey]]|first=Steve|last=Schilling|date=2008-05-30|accessdate=2008-06-07}} - Glacier arms touch on North end of glacier.</ref> In addition, since 2004, new glaciers have formed on the crater wall above Crater Glacier feeding rock and ice onto its surface below; there are two rock glaciers to the north of the eastern lobe of Crater Glacier.
