Waitt R B, Pierson T C, Macleod N S, Janda R J, Voight B, Holcomb R T
Science. 1983 Sep 30;221(4618):1394-7. doi: 10.1126/science.221.4618.1394.
An explosive eruption of Mount St. Helens on 19 March 1982 had substantial impact beyond the vent because hot eruption products interacted with a thick snowpack. A blast of hot pumice, dome rocks, and gas dislodged crater-wall snow that avalanched through the crater and down the north flank. Snow in the crater swiftly melted to form a transient lake, from which a destructive flood and lahar swept down the north flank and the North Fork Toutle River.
1982年3月19日圣海伦斯火山的一次爆发产生了巨大影响,远超火山口范围,因为炽热的喷发物与厚厚的积雪相互作用。一股炽热的浮石、穹顶岩石和气体冲击,使火山口壁上的积雪松动,积雪顺着火山口崩塌并沿北坡滑落。火山口内的雪迅速融化形成一个临时湖泊,一场毁灭性的洪水和火山泥流从该湖泊沿北坡和图特尔河的北支流奔涌而下。