학술논문

Transport and deposition in the May 18, 1980, Mount St. Helens blast flow
Document Type
Academic Journal
Source
Geology (Boulder). 26(2):155-158
Subject
24|Quaternary geology
Cascade Range
Cenozoic
explosive eruptions
field studies
Holocene
igneous rocks
Mount Saint Helens
pyroclastic flows
pyroclastic surges
pyroclastics
Quaternary
sampling
sedimentation
Skamania County Washington
southwestern Washington
statistical analysis
suspended materials
transport
turbulence
United States
volcanic rocks
volcaniclastics
volcanoes
volcanology
Washington
Language
English
ISSN
0091-7613
Abstract
A new, statistical sampling strategy for pyroclastic deposits has yielded data that reveal the depositional characteristics of the May 18, 1980, blast flow of Mount St. Helens. Samples were collected from each layer along a profile parallel to flow lines, as interpreted from tree blow-down directions. The decrease in the mass of sediment of different grain sizes with distance supports a turbulent-gravitational mechanism of suspended sedimentation, and transport within a dilute blast cloud having a density only slightly greater than that of the atmosphere. Traditional sampling strategies would have been unable to yield data suitable to test this settling mechanism hypothesis.