Zobrazeno 1 - 10
of 165
pro vyhledávání: '"M. Kervyn"'
Autor:
D. O'Hara, L. Goren, R. M. J. van Wees, B. Campforts, P. Grosse, P. Lahitte, G. Kereszturi, M. Kervyn
Publikováno v:
Earth Surface Dynamics, Vol 12, Pp 709-726 (2024)
The erosional state of a landscape is often assessed through a series of metrics that quantify the morphology of drainage basins and divides. Such metrics have been well explored in tectonically active environments to evaluate the role of different p
Externí odkaz:
https://doaj.org/article/c32e7ba842d84b3ca82f22a6a879a140
Autor:
M. Kervyn, F. Barette, S. Poppe, B. Smets, A. Syavulisembo Muhindo, J. Kambale Makundi, Y. Ngunzi Kahashi, J. Kambale Ndagana, S. Mossoux, F. Kervyn, C. Michellier
Publikováno v:
Journal of Applied Volcanology, Vol 13, Iss 1, Pp 1-22 (2024)
Abstract Assessing volcanic hazards in locations exposed to multiple central volcanoes requires to consider multiple potential eruption sources and their respective characteristics. While this is common practice in ashfall hazard assessment, this is
Externí odkaz:
https://doaj.org/article/f029e0f5db3b462a9e9cc428627415ac
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 23, Pp 933-953 (2023)
Risk perception is an essential element to consider for effective risk management at the time of eruption, especially in densely populated cities close to volcanoes like Goma in the east of the Democratic Republic of the Congo, which is highly expose
Externí odkaz:
https://doaj.org/article/5632b485976146d5802b8ffd3e90e027
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 19, Pp 1251-1263 (2019)
Development of hazard maps is one of the measures promoted by the international community to reduce risk. Hazard maps provide information about the probability of given areas to be affected by one or several hazards. As such they are useful tools to
Externí odkaz:
https://doaj.org/article/4c94221a797845c4a24588fb18f8d260
Autor:
S. Poppe, O. Galland, N. J. deWinter, S. Goderis, P. Claeys, V. Debaille, P. Boulvais, M. Kervyn
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 3, Pp n/a-n/a (2020)
Abstract Two end‐member conceptual models are used to describe deformation of the Earth's crust induced by magma intrusion. “Mode I” fracturing assumes tensile or opening‐mode, elastic deformation, while “Mode II” fracturing assumes plast
Externí odkaz:
https://doaj.org/article/3b2195c921b04938832ee6edb69f799c
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 18, Pp 105-124 (2018)
The inhabited zone of the Ugandan Rwenzori Mountains is affected by landslides, frequently causing loss of life, damage to infrastructure and loss of livelihood. This area of ca. 1230 km2 is characterized by contrasting geomorphologic, climatic an
Externí odkaz:
https://doaj.org/article/fc08d3a7378f4efd8a8b91ef9005e60c
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 16, Iss 1, Pp 135-147 (2016)
Natural disasters are too often presented as resulting from extreme natural phenomena affecting helpless populations, with people being insufficiently aware of the factors leading to disasters and of the existing strategies to mitigate their impacts.
Externí odkaz:
https://doaj.org/article/73539af699f14a7cb4ac2abcadecea2e
Publikováno v:
19th International Conference on AC and DC Power Transmission (ACDC 2023).
Autor:
D. Smittarello, B. Smets, J. Barrière, C. Michellier, A. Oth, T. Shreve, R. Grandin, N. Theys, H. Brenot, V. Cayol, P. Allard, C. Caudron, O. Chevrel, F. Darchambeau, P. de Buyl, L. Delhaye, D. Derauw, G. Ganci, H. Geirsson, E. Kamate Kaleghetso, J. Kambale Makundi, I. Kambale Nguomoja, C. Kasereka Mahinda, M. Kervyn, C. Kimanuka Ruriho, H. Le Mével, S. Molendijk, O. Namur, S. Poppe, M. Schmid, J. Subira, C. Wauthier, M. Yalire, N. d’Oreye, F. Kervyn, A. Syavulisembo Muhindo
Publikováno v:
Nature
Nature, 2022, 609 (7925), pp.83-88. ⟨10.1038/s41586-022-05047-8⟩
Nature, 2022, 609 (7925), pp.83-88. ⟨10.1038/s41586-022-05047-8⟩
Classical mechanisms of volcanic eruptions mostly involve pressure buildup and magma ascent towards the surface1. Such processes produce geophysical and geochemical signals that may be detected and interpreted as eruption precursors1,2,3. On 22 May 2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5c79d43d9cfb4083319c7cc7b246ff70
https://hal-insu.archives-ouvertes.fr/insu-03779616/file/s41586-022-05047-8.pdf
https://hal-insu.archives-ouvertes.fr/insu-03779616/file/s41586-022-05047-8.pdf
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