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REPORT:
Rockslide-debris Avalanche of May 18, 1980, Mount St. Helens Volcano, Washington


-- Harry Glicken, 1996,
Rockslide-debris Avalanche of May 18, 1980, Mount St. Helens Volcano, Washington: U.S. Geological Survey Open-File Report 96-677

Table of Contents

Abstract
Introduction
Acknowledgments
Geology of the source area
General Statement
Description of rock units
Older dacite unit
Andesite and basalt unit
Modern dacite unit
Cryptodome
Pre-eruption structure
Geology of the slide blocks
Geometry of the deposit
Volume and thickness
Morphology of hummocks
Orientation of elongate hummocks
Hummock types
Formation of the hummocks
Interpretation of size data
Geologic maps of the deposit
General statement
Morphologic map of the debris-avalanche deposit
North Fork unit
Johnston Ridge unit
Spirit Lake unit
Marginal unit
Proximal unit
Distal unit
Lithologic map
Block facies units
Older dacite unit
Andesite and basalt unit
Modern dacite unit
Modern undifferentiated unit
Mixed block and matrix facies unit
Contacts between lithologic units
Other deposits of the May 18, 1980 eruption
Blast deposits
Lahar deposits
Pyroclastic flow deposits of the afternoon of May 18
Tertiary bedrock
Texture of the deposit
General statement
Terminology
Scales of study
Textural interpretation of map relations
East of the break-in-slope
West of the break-in-slope
Lateral variation in debris-avalanche block size
Textural interpretation of exposures
General statement
Description of windows
Block-facies windows
Block- and matrix-facies windows
Matrix-facies windows
Discussion of windows
Density measurements
Grain-size analysis
Methods
Results
General statement
Distribution plots
Cumulative plots
Statistical parameters
Lateral variations of statistical parameters
Conclusions
Slide and blast events
Slide block I
Slide block II and blast surge
Slide block III
Final events
Water budget
Transition to flow and disintegration of material
Fluidization and fluids in the flow
Turbulence
The base of the debris avalanche
Mobility of the debris avalanche
References cited


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08/23/99, Lyn Topinka