| Titre de série : |
U. S. Geological Survey Water-Supply Paper, 2273 |
| Titre : |
Polallic Creek debris flow and subsequent dam-break flood of 1980, East fort hood river basin, oregon |
| Type de document : |
texte imprimé |
| Auteurs : |
Ballino, G. L. ; Pierson, T. C. |
| Mention d'édition : |
U.S. Geological Survey |
| Editeur : |
U.S. Geological Survey |
| Année de publication : |
1985 |
| ISBN/ISSN/EAN : |
CI-04982 |
| Note générale : |
this report talks about approximately 9 p.m.on december 25, 1980, a intense rainstorn and the entremely wet antecedent conditions combined to trigger a landslide of approximately 5,000 yd3 at the head of polallie Creek Canyon on the northea..... plank of mount hood, oregon. the lands lide was transformed rappidly into a debris flow, which surged down the channel at iclocities of about 40-50 ft/s esowing and incorporating large volumes of channel fill and uprooted vegetation. When it readed the debris fan at the confluence with the East-fork Hood river, the debris flow de posited approximately 100,000 yd3 of satured, poorly sorted debris to a maximum thickness of 35 ft, forming a 750-ft-long temporavy dam accross the drannel... |
| Langues : |
Anglais (eng) |
| Mots-clés : |
Géographie Hydrologie Erosion Barrage Inondation Bassin versant |
| Index. décimale : |
551.48 Hydrologie : |
| Résumé : |
this report talks about approximately 9 p.m.on december 25, 1980, a intense rainstorn and the entremely wet antecedent conditions combined to trigger a landslide of approximately 5,000 yd3 at the head of polallie Creek Canyon on the northea..... plank of mount hood, oregon. the lands lide was transformed rappidly into a debris flow, which surged down the channel at iclocities of about 40-50 ft/s esowing and incorporating large volumes of channel fill and uprooted vegetation. When it readed the debris fan at the confluence with the East-fork Hood river, the debris flow de posited approximately 100,000 yd3 of satured, poorly sorted debris to a maximum thickness of 35 ft, forming a 750-ft-long temporavy dam accross the drannel... |
| Note de contenu : |
this report talks about approximately 9 p.m.on december 25, 1980, a intense rainstorn and the entremely wet antecedent conditions combined to trigger a landslide of approximately 5,000 yd3 at the head of polallie Creek Canyon on the northea..... plank of mount hood, oregon. the lands lide was transformed rappidly into a debris flow, which surged down the channel at iclocities of about 40-50 ft/s esowing and incorporating large volumes of channel fill and uprooted vegetation. When it readed the debris fan at the confluence with the East-fork Hood river, the debris flow de posited approximately 100,000 yd3 of satured, poorly sorted debris to a maximum thickness of 35 ft, forming a 750-ft-long temporavy dam accross the drannel... |
U. S. Geological Survey Water-Supply Paper, 2273. Polallic Creek debris flow and subsequent dam-break flood of 1980, East fort hood river basin, oregon [texte imprimé] / Ballino, G. L. ; Pierson, T. C. . - U.S. Geological Survey . - U.S. Geological Survey, 1985. ISSN : CI-04982 this report talks about approximately 9 p.m.on december 25, 1980, a intense rainstorn and the entremely wet antecedent conditions combined to trigger a landslide of approximately 5,000 yd3 at the head of polallie Creek Canyon on the northea..... plank of mount hood, oregon. the lands lide was transformed rappidly into a debris flow, which surged down the channel at iclocities of about 40-50 ft/s esowing and incorporating large volumes of channel fill and uprooted vegetation. When it readed the debris fan at the confluence with the East-fork Hood river, the debris flow de posited approximately 100,000 yd3 of satured, poorly sorted debris to a maximum thickness of 35 ft, forming a 750-ft-long temporavy dam accross the drannel... Langues : Anglais ( eng)
| Mots-clés : |
Géographie Hydrologie Erosion Barrage Inondation Bassin versant |
| Index. décimale : |
551.48 Hydrologie : |
| Résumé : |
this report talks about approximately 9 p.m.on december 25, 1980, a intense rainstorn and the entremely wet antecedent conditions combined to trigger a landslide of approximately 5,000 yd3 at the head of polallie Creek Canyon on the northea..... plank of mount hood, oregon. the lands lide was transformed rappidly into a debris flow, which surged down the channel at iclocities of about 40-50 ft/s esowing and incorporating large volumes of channel fill and uprooted vegetation. When it readed the debris fan at the confluence with the East-fork Hood river, the debris flow de posited approximately 100,000 yd3 of satured, poorly sorted debris to a maximum thickness of 35 ft, forming a 750-ft-long temporavy dam accross the drannel... |
| Note de contenu : |
this report talks about approximately 9 p.m.on december 25, 1980, a intense rainstorn and the entremely wet antecedent conditions combined to trigger a landslide of approximately 5,000 yd3 at the head of polallie Creek Canyon on the northea..... plank of mount hood, oregon. the lands lide was transformed rappidly into a debris flow, which surged down the channel at iclocities of about 40-50 ft/s esowing and incorporating large volumes of channel fill and uprooted vegetation. When it readed the debris fan at the confluence with the East-fork Hood river, the debris flow de posited approximately 100,000 yd3 of satured, poorly sorted debris to a maximum thickness of 35 ft, forming a 750-ft-long temporavy dam accross the drannel... |
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U. S. Geological Survey Water-Supply Paper, 2273. Polallic Creek debris flow and subsequent dam-break flood of 1980, East fort hood river basin, oregon