|
000
| 01972cam 2200337za 4500 |
|---|
| 001 | 9.852678 |
|---|
| 003 | CaOODSP |
|---|
| 005 | 20221107154636 |
|---|
| 007 | cr ||||||||||| |
|---|
| 008 | 180301s1984 oncab||#ob|||f001 0 eng d |
|---|
| 020 | |q(paper)|z0660117290 |
|---|
| 040 | |aCaOODSP|beng |
|---|
| 041 | |aeng|bfre |
|---|
| 043 | |an-cn-ab|an-cn-bc |
|---|
| 086 | 1 |aM44-84/16E-PDF|zM44-84/16E |
|---|
| 100 | 1 |aEisbacher, Gerhard H. |
|---|
| 245 | 10|aDestructive mass movements in high mountains |h[electronic resource] : |bhazard and management / |cG.H. Eisbacher and J.J. Clague. |
|---|
| 260 | |aOttawa : |bGeological Survey of Canada : |bEnergy, Mines and Resources Canada, |cc1984. |
|---|
| 300 | |a230 p. : |bill., maps |
|---|
| 490 | 1 |aPaper / Geological Survey of Canada ;|v84-16 |
|---|
| 500 | |aDigitized edition from print 2017 [produced by Saskatchewan Polytechnic Library]. |
|---|
| 504 | |aIncludes bibliographical references and index. |
|---|
| 520 | |a"Most destructive mass movements are complex and are related to mountain torrent systems and instabilities in steep bedrock slopes. They are controlled by unique combinations of geological, topographic, meteorological, and seismic factors and by human activity (e.g mining, logging, urban and recreational development). The major groups of mass movements considered in this report are debris flows from surficial deposits, debris flows from bedrock failures, mass movements on volcanoes, glacier-related mass movements, and rockfalls and rock avalanches"--Summary, p. 2. |
|---|
| 546 | |aIncludes abstract and summary in French. |
|---|
| 692 | 07|2gccst|aGeology |
|---|
| 700 | 1 |aClague, J. J. |q(John Joseph), |d1946- . |
|---|
| 710 | 1 |aCanada. |bEnergy, Mines and Resources Canada. |
|---|
| 710 | 2 |aGeological Survey of Canada. |
|---|
| 830 | #0|aGeological Survey of Canada. Paper ;|v84-16|w(CaOODSP)9.815431 |
|---|
| 856 | 40|qPDF|s136.27 MB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/M44-84-16-eng.pdf |
|---|