KSIĄŻKI POWIĄZANE ZE SŁOWEM «LAHAR»
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1
Postglacial lahars and potential hazards in the White ... - Halaman 24
Clay-sized minerals detected by X-ray diffractioni in lahar, debris avalanche, and glacial deposits Sample2 Location Minerals identified by x-ray diffraction3 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. 17. 18. 19. 20. 21. 22. 23. 1921 debris ...
2
Volcanic Hazards - Bhgn 3 - Halaman 16
Sequential changes in flow type and particle-support mechanisms in the transformation of a lahar to lahar-runout flow, and then to normal streamflow (Scott, 1988; Table 9). Flow direction and decreasing, sediment concentration are left to right ...
3
Debris-flow Hazards and Related Phenomena - Halaman 269
Stratigraphic relation of lahars to one another, weathering pro®les between deposits, and geomorphic relations where deposits form successive terraces within a valley provide relative age determinations. Stratigraphic units can also be dated ...
Matthias Jakob, Oldrich Hungr,
2007
4
Debris Flows/avalanches: Process, Recognition, and ...
The North Fork Toutle River lahar was unique because it did not begin to move downvalley until approximately 1310 PDT, more than 4.5 hr after the eruption started. It was an extremely long and large lahar that lasted until approximately 2120 ...
John E. Costa, Gerald F. Wieczorek,
1987
5
Western Cordillera and Adjacent Areas - Halaman 212
Concern about future lahars on Mount Rainier spurred the mapping and dating of the volcano's Holocene lahar deposits (Crandell, 1971; Scott et al., 1995). This work shows that Mount Rainier produced both clay-rich and clay-poor flows ...
6
The Encyclopedia of Volcanoes - Halaman 654
The mobility of lahar mixtures can thus be viewed as the product of an energy cascade that begins with the bulk gravitational potential energy of sediment and water poised at high elevations. The next step of the cascade entails transformation ...
Haraldur Sigurdsson, Bruce Houghton, Steve McNutt,
2015
7
Floods, Faults, and Fire: Geological Field Trips in ... - Halaman 93
The contact between deposits of two nineteenth century lahars is knife-sharp in the stream bank at the Boulder Creek campground, 120 m below the highway bridge (Stop 4). Boulder-size clasts of Baker andesite dominate the coarse phase of ...
Peter L. Stelling, David Samuel Tucker,
2007
8
Early Warning Systems for Natural Disaster Reduction - Halaman 42
Having witnessed the destructive effects of dangerous lahar and mudflows in the aftermath of an eruption the population's awareness of the possibility of becoming victims was once more heightened. The displacement of people, destruction, ...
Jochen Zschau, Andreas N. Küppers,
2013
9
Neogene-Quaternary Continental Margin Volcanism: A ...
After the eruption, this material was quickly removed in the form of rain lahars that extensively flooded the Puebla Basin and destroyed several important settlements such as Totimehuacan, Cholula, Huejotzingo, Xochitécatl, and Cacaxtla.
Claus Siebe, José Luis Macías, Gerardo J. Aguirre-Díaz,
2006
10
Monitoring, Simulation, Prevention and Remediation of ... - Halaman 105
Lahar flow is the mixture of water and erupted volcanic material that slides down through the river valleys or grooves (Houghton et al. [2]). Hazards caused by lahar flows have been generated by rain, after or during eruption, and or a dam ...
C. A. Brebbia, D. De Wrachien, S. Mambretti,
2012