A moving mass of rock fragments, soil, and mud, more than half of the particles being larger than sand size. Slow debris flows may move less than 1 m per year; rapid ones reach 160 km per hour. Debris flows are very fluid and contain a high content of water.Neuendorf, K.K.E., Mehl, J.P., Jr., and Jackson, J.A., ed., 2005, Glossary of Geology: American Geological Institute, 799 p.
Below is a list of publications related to Debris Flow. Select a publication number to access more detailed information and their respective files available for download.
- P 1732-B
- Coombs, M.L., Neal, C.A., Wessels, R.L., and McGimsey, R.G., 2006, Geothermal disruption of summit glaciers at Mount Spurr Volcano, 2004-6: An unusual manifestation of volcanic unrest, in Haeussler, P.J. and Galloway, J.P., ed., Studies by the U.S. Geological Survey in Alaska, 2005: U.S. Geological Survey Professional Paper 1732-B, 33 p.
- RI 2013-2
- Reger, R.D. and Burns, P.A.C., 2013, Surficial-geologic map of the Livengood area, central Alaska: Alaska Division of Geological & Geophysical Surveys Report of Investigation 2013-2, 1 sheet, scale 1:50,000.