L’été est passé et le numéro de l’automne est arrivé. Je pose la fiche ici avec son sommaire et je repasse pour y laisser mes notes.
Au sommaire :
- L’actualité culturelle
Page 4-5
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Bellier, V., Legendre, Y., Carazzo, G., Michaud-Dubuy, A., Traineau, H., & Vittecoq, B. (2026). Carte pédagogique de la montagne Pelée [Map]. BRGM Éditions.
- L’actualité éruptive du troisième trimestre 2026
Page 6-8
L’éruption la plus marquante de l’été 2026 est incontestablement celle de l’Anak Krakatau, qui a produit de spectaculaires fontaines de lave atteignant possiblement plus de 1000 mètres ! Des journalistes venus couvrir l’éruption sont malheureusement portés disparus… Également le Sinabung (Indonésie), le Fuego (Guatemala) et l’Etna (Italie).
- L’actualité scientifique du troisième trimestre 2026
Page 8-15
Au menu ce trimestre : l’augmentation du dégazage de CO2 dans les monts Dore ; la nouvelle caldeira du Hunga Tonga ; une première étude sur l’éruption du Hayli Gubbi ; des datations aux méthodes inhabituelles ; un nouveau champ volcanique en Idaho ; la hauteur des fontaines de lave du Kīlauea…
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- Dossier : Sur les mondes aux volcans de glace
Page 16-23
Les volcans que nous connaissons sur Terre ne constituent qu’une des formes possibles de volcanisme, où c’est de la roche qui fond pour former du magma. Mais dans le système solaire externe, plusieurs mondes gelés présentent une autre forme de volcanisme, dans laquelle c’est de la glace qui fond et érupte. Enfilez votre combinaison spatiale, nous vous emmenons à la découverte des cryovolcans.
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- Volcans utiles : Quand les volcans servent à entraîner les astronautes
Page 24-30
Quel est le paysage terrestre qui ressemble le plus à la Lune ? Un volcan ! Rien de tel qu’un bon champ de lave pour simuler la surface rocailleuse de notre satellite. Partant de ce constat, la NASA a utilisé plusieurs régions volcaniques pour former les hommes du programme Apollo à la géologie. Alors que son successeur Artemis est en cours, le ballet des astronautes a repris sur plusieurs volcans.
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Pesquet, T. (2023).
The detective. Caves & Pangaea Blog.
Schaber, G. G. (2005).
The U.S. Geological Survey, branch of Astrogeology—A chronology of activities from conception through the end of Project Apollo (1960-1973) (Open-File Report Nos. 2005–1190). U.S. Geological Survey.
https://doi.org/10.3133/ofr20051190
- La méthode : Mesurer la température des phénomènes volcaniques
Page 31-35
La chaleur est une caractéristique majeure des différents phénomènes volcaniques. Qu’il s’agisse des vapeurs s’échappant d’une fumerolle, du mélange gaz–particules d’un écoulement pyroclastique, ou de la lave d’une coulée, les températures atteignent plusieurs centaines de degrés. Combien exactement ? Comment effectue-t-on ces mesures, et quelles informations nous apportent-elles ?
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- L’image : Max Fleischer, un artiste et botaniste à Java
Page 36-39
Peut-on mener deux carrières de concert ? Et surtout, peut-on réussir dans les deux ? Assurément oui pour l’Allemand Max Fleischer, qui fut à la fois un botaniste reconnu et un artiste de talent. Entre deux échantillonnages de mousses tropicales, il a notamment peint les paysages volcaniques de Java.
- La vie : La faune volcanique des îles Galápagos
Page 40-45
Dans l’océan Pacifique, une poignée de terres isolées abrite des animaux ayant évolué pendant des millions d’années, divergeant progressivement de leurs ancêtres continentaux. Parfaitement adaptée aux paysages volcaniques qui l’entourent, cette faune possède quelques espèces étonnantes. Présentations.
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Steinfartz, S. (2011).
When Hotspots Meet: The Galápagos Islands: A Hotspot of Species Endemism Based on a Volcanic Hotspot Centre. In F. E. Zachos & J. C. Habel (Eds.),
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Boersma, P. D., Steinfurth, A., Merlen, G., Jiménez-Uzcátegui, G., Vargas, F. H., & Parker, P. G. (2013). Galápagos Penguin (Spheniscus mendiculus). In P. G. Borboroglu & P. D. Boersma (Eds.), Penguins: natural history and conservation. University of Washington Press.
Tapia Aguilera, W., & Gibbs, J. P. (2023).
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- La question : À quoi ressemblera la prochaine éruption du Vésuve ?
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La dernière éruption du Vésuve s’est produite il y a plus de 80 ans, en 1944, après plus de trois siècles d’activité presque ininterrompue. Une telle pause n’est cependant pas inhabituelle dans l’histoire du volcan napolitain. Et s’il est impossible de prévoir sa durée, elle devrait conditionner la nature de la future éruption.
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