Duba wurin da ke ƙasa sannan ka amsa tambayar daga baya a cikin harshe ɗaya kamar yadda wurin yake:  Passage: Bayyanar da aka yi daga baya na kayan pyroclastic daga fashewar da rushewar ƙasa ta bar ya ƙunshi yawancin sabbin tarkace magmatic maimakon gutsuttsura na dutsen mai aman wuta. Sakamakon ajiyar da aka samu ya samar da wani nau'i mai kama da fan na shimfidawa, harsuna da lobes. Aƙalla raƙuman pyroclastic 17 daban-daban sun faru a lokacin fashewar 18 ga Mayu, kuma jimlarsu ta kasance kusan 0.05 cubic miles (0.21 km3). Ruwan da ke gudana har yanzu yana da kusan 570 zuwa 790 ° F (300 zuwa 420 ° C) makonni biyu bayan fashewar. Fashewar fashewar tururi na biyu da wannan zafi ya haifar da ramuka a gefen arewacin ramin pyroclastic-flow, a kudancin bakin Tekun Ruhu, da kuma saman ɓangaren Kogin North Fork Toutle. Waɗannan fashewar fashewar tururi sun ci gaba a lokaci-lokaci na makonni ko watanni bayan sanyawar kwararar pyroclastic, kuma aƙalla ɗaya ya faru shekara guda daga baya, a ranar 16 ga Mayu, 1981.  Tambaya: Wane irin yanayi ne ya kasance bayan ambaliyar?
wani fan-kamar zane na overlapping zanen gado, harsuna da lobes