What important message does the above poem convey
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the VHP to respond to volcanic crises would be compromised by a lack of expertise in hazard assessment or volcano process studies.
One possible solution would be for VHP members to collaborate more on research projects with scientists outside the USGS, particularly those from universities and from laboratories of other government agencies. More active collaborations, coupled with an extramural grant program for academic researchers overseen partly or completely by the VHP, would help ensure that more investigations that are directly relevant to the program’s mission would be carried out.
HAZARD ASSESSMENT
Volcano hazard assessment aims to determine where and when future volcano hazards will occur and their potential severity. This kind of appraisal provides a long-term view of the locations and probabilities of large-scale eruptions and related phenomena, such as volcanic debris avalanches and tsunamis. The extensive range of hazards that must be evaluated requires the combined knowledge of a broad array of scientists, including geologists, hydrologists, geotechnical engineers, atmospheric physicists, and statisticians. Because assessment is inherently interdisciplinary, the VHP needs access to a very diverse set of expertise, either within its own ranks or through collaborations with outside groups.
Geologic mapping, stratigraphy, geochronology, and physical volcanology provide the backbone of volcanic hazard assessments by revealing past trends in eruption timing, volume, and explosivity. Historically the USGS has done an excellent job of incorporating geologic data into its assessments. The committee commends VHP efforts to integrate findings of geologic studies into volcanic hazard assessments. An ongoing challenge is to more effectively quantify geologic data in ways that optimize their use in such assessments.
Although mapping and dating of volcanic deposits can provide a good framework for hazard assessment, mechanical models of physical, chemical, and hydrologic processes help refine forecasts of the types and magnitudes of future eruptions. Both numerical models and laboratory simulations can relate the boundary conditions on a volcano to the likely consequences of any incipient eruptive activity. Although there has been some VHP participation in the development of these models, especially those related to hydrologic and sedimentologic phenomena, most have
One possible solution would be for VHP members to collaborate more on research projects with scientists outside the USGS, particularly those from universities and from laboratories of other government agencies. More active collaborations, coupled with an extramural grant program for academic researchers overseen partly or completely by the VHP, would help ensure that more investigations that are directly relevant to the program’s mission would be carried out.
HAZARD ASSESSMENT
Volcano hazard assessment aims to determine where and when future volcano hazards will occur and their potential severity. This kind of appraisal provides a long-term view of the locations and probabilities of large-scale eruptions and related phenomena, such as volcanic debris avalanches and tsunamis. The extensive range of hazards that must be evaluated requires the combined knowledge of a broad array of scientists, including geologists, hydrologists, geotechnical engineers, atmospheric physicists, and statisticians. Because assessment is inherently interdisciplinary, the VHP needs access to a very diverse set of expertise, either within its own ranks or through collaborations with outside groups.
Geologic mapping, stratigraphy, geochronology, and physical volcanology provide the backbone of volcanic hazard assessments by revealing past trends in eruption timing, volume, and explosivity. Historically the USGS has done an excellent job of incorporating geologic data into its assessments. The committee commends VHP efforts to integrate findings of geologic studies into volcanic hazard assessments. An ongoing challenge is to more effectively quantify geologic data in ways that optimize their use in such assessments.
Although mapping and dating of volcanic deposits can provide a good framework for hazard assessment, mechanical models of physical, chemical, and hydrologic processes help refine forecasts of the types and magnitudes of future eruptions. Both numerical models and laboratory simulations can relate the boundary conditions on a volcano to the likely consequences of any incipient eruptive activity. Although there has been some VHP participation in the development of these models, especially those related to hydrologic and sedimentologic phenomena, most have
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