Pre-eruptive average SO2 emission rates (2-3?kt/d) were similar to the emission rates measured during the first part of the eruption (up to August 1995) in contrast with the effusive-explosive periods (March 1996-January 1998) during which SO2 emission rates were higher by a factor of ...
2. Choosing case study eruptions 3. Reconstructing PDC producing eruptions using Titan2D 4. Reconstructing the 1948 eruption 5. Results 6. Discussion 7. Concluding remarks Author contributions Declaration of Competing Interest Acknowledgements Appendix A. Supplementary data ReferencesShow full outline Cited...
Prediction of Volcanic Eruption with Polythionate Monitoring in Active Crater Lakes (II) : A Case Study at Poas Volcano, Costa Rica Ohsawa S. , Rowe G. L. , Brantley S. L. , Barquero J. , Fernandez M. , Fernandez J. F. , Takano B. Programme and abstracts the Volcanological Societ...
Characteristics of volcanic gas correlated to the eruption activity; Case study in the Merapi Volcano, periods of 1990-1994 来自 Semantic Scholar 喜欢 0 阅读量: 19 作者:Priatna Priatna,Eka Kadarsetia 摘要: http://dx.doi.org/10.17014/ijog.vol2no4.20074Volcanic gases, collected from Gendol and ...
Merapi as a case study, the authors apply the socio-psychological factors that might govern the social resilience of the community. The communities living around Mt. Merapi have developed capacities and adopted some ways for dealing with eruption consequences since they experience periodic volcanic ...
The morphology, dimensions and petrography of ancient lava flows can be used to extract the flow conditions during an eruption. Consequently, the study of a set of lava flows from a volcano can give important clues about the variations through time of such parameters as the effusion rate and ...
Sequence and eruptive style of the 1783 eruption of Asama Volcano, central Japan: a case study of an andesitic explosive eruption generating fountain-fed l... The 3-month long eruption of Asama volcano in 1783 produced andesitic pumice falls, pyroclastic flows, lava flows, and constructed a ...
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3A) and can be used to infer the extent and the shape of the surface carved by the by explosive eruption(s) that deeply cut into the pre-existing country rock (unit U1). The reflective area terminates indeed on an irregular, U-shaped unconformity, clearly recognizable on solf_1 that we...
Whakaari/White Island, island in the Bay of Plenty, 43 miles (69 km) west of Cape Runaway, eastern North Island, New Zealand. An active volcano, it is the top of a submarine vent at the northern end of the Taupo-Rotorua Volcanic Zone. An eruption of the