Éditeur(s) : Université des Antilles et de la Guyane IRD : Institut de Recherche pour le Développement
Extrait de : "Projet CARIBSAT, système caribéen d'information environnementale" : conférence, le 21 mars 2013. Université des Antilles et de la Guyane
Description : Malgré l'existence de systèmes d'alerte à l'échelle régionale, il n'y a pas de méthode pour aider à planifier les évacuations en cas de risques de tsunamis. La sensibilisation et la préparation sont pourtant essentielles. Itinéraire et destination, nombre de personnes en présence et temps de réaction doivent être calculés préalablement. Pour ce faire, des outils géographiques (MapInfo) permettent l'analyse optimale des réseaux routiers et des zones d'accessibilité.
Siècle(s) traité(s) : 21
Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Permalien : http://www.manioc.org/fichiers/V13102
V13102

Extrait de : La Montagne Pelée et l'effroyable destruction de Saint-Pierre (Martinique) le 08 mai 1902. Le brusque réveil du volcan en 1929 (En regard de la page 137)
Résumé : Cliché
Siècle(s) traité(s) : 20
Droits : Domaine public
Permalien : http://www.manioc.org/images/PAP110550196i1
PAP110550196i1

Résumé : At the outbreak of war with Spain in 1898, the U.S. Army was very small in numbers. This situation necessitated an immediate call for volunteers. President McKinley's appeal was overwhelmingly answered by a generation that had grown up in the shadow of their elders' Civil War glory. One group answering the call was the First Regiment of the U.S. Cavalry Volunteers, headed by Colonel Leonard Wood, a distinguished army doctor and Medal of Honor recipient. The regiment was actually the brainchild of Theodore Roosevelt, assistant secretary of the navy and Wood's friend. Roosevelt, realizing his own lack of military experience, suggested Wood for the command. The Rough Riders, as the regiment was soon known, comprised 1,250 men, including cowboys, Native Americans and eastern college athletes. Despite their dissimilarities, they were in excellent physical condition'a stark contrast to most of the other volunteer contingents. The Rough Riders departed from Tampa in mid-June without their horses. They landed at Daiquiri on June 22 and two days later served with distinction in a battle at Las Guásimas. Immediately prior to the conflict at San Juan, Colonel Wood was promoted to another field command, enabling Roosevelt as a full colonel to take command of the Rough Riders. On July 1, Roosevelt, having secured a horse, led his forces in a charge up Kettle Hill outside of Santiago. They achieved their goal and later in the day participated in the victory at San Juan Hill. By seizing these heights, American guns commanded the harbor at Santiago. The Spanish position was imperiled and an abortive attempt by the Spanish navy to escape from the harbor was halted with devastating results. Spanish land forces surrendered shortly thereafter. Roosevelt urged the Rough Riders' swift evacuation, fearing the continuing spread of disease. They returned to Montauk, Long Island, where they were held in quarantine before being mustered out in September. More than one-third of the Rough Riders were casualties in the Spanish-American War, a fact that has led some observers to criticize Roosevelt for unnecessary risk-taking. Nevertheless, the Rough Riders became heroes to the American public and Roosevelt emerged as a major national figure.
(Funding) Funded in part by the Institute for Museum and Library Services (IMLS), Ephemeral Cities Project.
Tampa |z 1271000 |2 ceeus
Hillsborough County |z 12057 |2 ceeus
United States of America -- Florida -- Hillsborough County -- Tampa
United States

Droits : All rights reserved. 2005.
D20-012

Éditeur(s) : HAL CCSD
Résumé : International audience
This study aims at assessing the population vulnerability in the Pasig-Potrero River basin threatened by the recurrent lahars of Mt Pinatubo volcano (Philippines) subsequent to its 1991 eruption. A survey carried out between February and March 1998 enabled us to define and to map different levels of risk perception, the quality of the potential behaviors in the event of further lahars and of the demeanors in case of evacuation order. It was then possible to work out a typology and a cartography of human vulnerability in this study area.This study points out that, even though the risk perception is quite high, some problems remain, notably concerning warning and behaviors in case of evacuation.This work is part of a larger framework including population vulnerability assessment around Mt Pinatubo (social and institutional vulnerability). It also aims at estimating the effects, notably the territorial consequences, occurred as a result of a crisis linked to the volcano and its lahars, and that has been lasting for eight years. These results should allow to elaborate some risk and disaster scenarios. They are intended to be used as operational purposes in crises management such as relief arrangement, land use planning.
Cette étude a pour objectif d'évaluer la vulnérabilité des populations du bassin de la rivière Pasig-Potrero menacé par les lahars récurrents du volcan Pinatubo (Philippines) suite à l'éruption de 1991. A partir d'une campagne d'enquêtes sur le terrain, réalisée entre février et mars 1998, on a pu définir et cartographier différents niveaux de perception du risque, la qualité des comportements potentiels face aux lahars ainsi que des attitudes en cas d'ordre d'évacuation. Ces données ont ensuite permis de réaliser une typologie et une cartographie de la vulnérabilité dans le secteur d'étude.Il en ressort que si la perception du risque est assez élevée, des problèmes subsistent, notamment en matière d'alerte et de comportements en cas d'évacuation. La qualité de l'alerte a aussi montré, dans le passé, des carences qu'il convient aujourd'hui de combler.Ce travail s’inscrit dans un cadre plus large d'évaluation de la vulnérabilité des populations face au volcan Pinatubo (vulnérabilité sociale, institutionnelle...) el des conséquences, notamment territoriales, de huit années de crises liées à l'éruption, puis aux lahars.Ces conclusions peuvent guider l'élaboration de scénarios de risque et de catastrophe, utiles à des fins opérationnelles (planification des secours, aide à la gestion des crises, aménagement du territoire...).
Pangea

hal-01169313
https://hal.archives-ouvertes.fr/hal-01169313
https://hal.archives-ouvertes.fr/hal-01169313/document
https://hal.archives-ouvertes.fr/hal-01169313/file/Gaillard%20D%27Ercole%20Leone%201998%20-%20Cartographie%20de%20la%20vuln%C3%A9rabilit%C3%A9%20des%20populations%20Pinatubo%20Philippines.pdf

Éditeur(s) : HAL CCSD Groupe français de géomorphologie (GFG)
Résumé : International audience
This study aims at assessing the vulnerability of populations in the Pasig-Potrero River basin, who are threatened by the recurrent lahars of Mt Pinatubo volcano (Philippines) in the aftermath of its 1991 eruption. A survey, carried out between February and March 1998, enabled us to define and to map different levels of risk perception, the quality of potential behavioural patterns in the event of further lahars, and attitudes in the event of an evacuation order. It was then possible to work out a classification and to map the patterns of human vulnerability in the study area. This study points out that, while risk perception is quite high, some problems remain, notably concerning the warning systems and the behaviour of the population in the case of an evacuation. Theses results should assist in elaborating risk and disaster scenarios. They are intended to be used for operational purposes in crisis management such as the organization of disaster relief, and in land use planning.
ISSN: 1266-5304

hal-01169334
https://hal.archives-ouvertes.fr/hal-01169334
https://hal.archives-ouvertes.fr/hal-01169334/document
https://hal.archives-ouvertes.fr/hal-01169334/file/article_morfo_1266-5304_2001numéro 7_3_1103.pdf
DOI : 10.3406/morfo.2001.1103

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : During the 2003 summer monsoon, the Hi-CLIMB seismological stations deployed across the Himalayan Range detected bursts of high-frequency seismic noise that lasted several hours to days. On the basis of the cross correlation of seismic envelopes recorded at 11 stations, we show that the largest transient event on 15 August was located nearby a village partially destroyed on that day by a devastating debris flow. This consistency in both space and time suggests that high-frequency seismic noise analysis can be used to monitor debris flow generation as well as the evacuation of the sediment. A systematic study of one year of seismic noise, focusing on the detection of similar events, provides information on the spatial and temporal occurrence of mass movements at the front of the Himalayas. With a 50% probability of occurrence of a daily event, a total of 46 debris flows are seismically detected. Most of them were generated in regions of steep slopes, large gullies, and loose soils during the 2003 summer monsoon storms. These events are compared to local meteorological data to determine rainfall thresholds for slope failures, including the cumulative rainfall needed to bring the soil moisture content to failure capacity. The inferred thresholds are consistent with previous estimates deduced from soil studies as well as sediment supply investigations in the area. These results point out the potential of using seismic noise as a dedicated tool for monitoring the spatiotemporal occurrence of landslides and debris flows on a regional scale.
ISSN: 0148-0227

hal-00464177
https://hal.archives-ouvertes.fr/hal-00464177
DOI : 10.1029/2008JF001198

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : International audience
Parapneumonic pleural effusions represent the main cause of pleural infections. Their incidence is constantly increasing. Although by definition they are considered to be a “parapneumonic” phenomenon, the microbial epidemiology of these effusions differs from pneumonia with a higher prevalence of anaerobic bacteria. The first thoracentesis is the most important diagnostic stage because it allows for a distinction between complicated and non-complicated parapneumonic effusions. Only complicated parapneumonic effusions need to be drained. Therapeutic evacuation modalities include repeated therapeutic thoracentesis, chest tube drainage or thoracic surgery. The choice of the first-line evacuation treatment is still controversial and there are few prospective controlled studies. The effectiveness of fibrinolytic agents is not established except when they are combined with DNase. Antibiotics are mandatory; they should be initiated as quickly as possible and should be active against anaerobic bacteria except for in the context of pneumococcal infections. There are few data on the use of chest physiotherapy, which remains widely used. Mortality is still high and is influenced by underlying comorbidities.
Les épanchements pleuraux parapneumoniques représentent la principale étiologie des pleurésies infectieuses. Leur incidence est en constante augmentation. Bien qu’ils soient qualifiés de « parapneumoniques », l’épidémiologie microbienne est différente de celle des pneumonies avec notamment une plus grande fréquence des germes anaérobies. La ponction pleurale exploratrice représente l’étape diagnostique centrale qui permet de distinguer les épanchements parapneumoniques compliqués et non compliqués. Seuls les épanchements parapneumoniques compliqués doivent faire l’objet d’un traitement évacuateur reposant sur la mise en œuvre de ponctions pleurales répétées (PPR), d’un drainage thoracique ou d’une prise en charge chirurgicale. Le choix de la technique évacuatrice première reste débattu car il existe peu d’études prospectives comparatives. L’utilisation d’agents fibrinolytiques n’a pas fait la preuve de son efficacité sauf lorsqu’ils sont utilisés en association à la DNAse. L’antibiothérapie doit être systématique, précoce et couvrir les germes anaérobies, sauf en cas d’infection à pneumocoque. Il existe peu de données sur la place de la kinésithérapie qui reste largement utilisée. La mortalité est élevée et directement influencée par les comorbidités sous-jacentes.
ISSN: 0761-8425

hal-01117905
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01117905
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01117905/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01117905/file/Les%20%C3%A9panchements%20pleuraux%20parapneumoniques_accepted.pdf
DOI : 10.1016/j.rmr.2014.12.001

Éditeur(s) : HAL CCSD Springer Verlag (Germany)
Résumé : International audience
Mount Pinatubo volcano erupted in June 1991 in the main island of Luzon belonging to the Philippines archipelago. Huge economic losses and population exodus have followed. This major crisis has been relayed with other crises due to rainfed lahars which have been supplied with eruption deposits. These lahars have occurred every year since 1991 during the rainy season. They will probably last until 2005. After a brief presentation of the Philippine official response system to disasters, this paper draws up a critical analysis of the different kinds of institutional and social responses deployed to manage the different crisis and post-crisis phases of this event. Based on three viewpoints: from population, media and other actors, this analysis attempts to point out the strengths and weaknesses of the official management system, especially by studying the efficiency and the range of the solutions taken. So, it appears that the management of the June 1991 main crisis (eruption) was a success. On the other hand, difficulties have occurred with lahars risk management. Indeed, these lahars have obliged the authorities to protect and relocate thousands of people. In spite of persistent problems, the management system (monitoring/warning/evacuation) of lahar crises improves year after year. Failures appear especially within the rehabilitation program (protection/rehousing). Many direct (lack of means, preparedness, coordination, dialog,
etc.) and indirect (politico-administrative, socio-economic, cultural contexts) factors come together to lock the wheels of
the institutional response system. They defer the socio-economic start of this vital northern Philippines area.
GeoJournal

halshs-00119436
https://halshs.archives-ouvertes.fr/halshs-00119436
https://halshs.archives-ouvertes.fr/halshs-00119436/document

Résumé : Une expérience a été réalisée en conditions hivernales dans six bassins de terre pour déterminer l'effet des taux de renouvellement sur la production de crevettes Penaeus stylirostris, sur les caractéristiques de l'eau et du sédiment des enceintes d'élevage. Les budgets d'azote ont été établis en prenant en compte les différentes formes azotées dans l'eau, dans le sédiment, dans l'aliment et dans les crevettes. Un épisode de mortalité a été obserVé en cours d'élevage et peut être attribué à une epizootie dénommée "syndrome 93». Ce dernier était concomitant à une phase de croissance phytoplantonique et a été d'autant plus important que la biomasse phytoplanctonique dans le bassin d'élevage était élevée. Bien qu'une dilution importante de la colonne d'eau se soit avérée bénéfique pour la santé du cheptel pendant l'épisode de mortalité, l'augmentation des taux de renouvellement n'a en revanche pas permis d'améliorer de manière significative la qualité de l'environnement crevette sur toute la saison d'élevage (eau et sédiment). Une augmentation des échanges d'eau ne s'est pas accompagnée d'une meilleure exportation des déchets par les effluents. Cependant, les résultats montrent que cette augmentation accroît la productivité primaire. Les composés issus de la minéralisation de la matière organique et du métabolisme sont ainsi exportés sous forme particulaire plutôt que sous forme soluble. Les budgets d'azote montrent que la quantité de déchets rejetés par les effluents vers l'environnement côtier est faible. Ainsi, 10,1% à 16,90/o de l'azote introduit dans le milieu d'élevage sous forme d'aliment est exporté dans les effluents. Seulement 17,3% à 21,4% de l'azote d'origine alimentaire est retrouvé dans la chair des crevettes. L'augmentation des échanges d'eau implique une augmentation de l'accumulation azotée dans les sédiments de 21,0% à 50,1%. Parallèlement, le calcul de la proportion d'azote évacué par diffusion ou par dénitrification vers l'atmosphère diminue de 43,1% à 19,5% avec l'augmentation des taux de renouvellement.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00079/19066/16661.pdf
http://archimer.ifremer.fr/doc/00079/19066/

Éditeur(s) : HAL CCSD AGU and the Geochemical Society
Résumé : Geochemistry, Geophysics, Geosystems, v. 9, p. Q12001, 2008. http://dx.doi.org/10.1029/2008GC002098
International audience
Rb/Sr, 40Ar/39Ar, and Sm/Nd isotopic data are reported in Caledonian eclogites from the Lindås Nappe, Bergen Arcs, Norway, in order to investigate processes controlling isotopic equilibrium at mineral scale in polymetamorphic rocks. The Bergen Arcs exposes Sveconorwegian ∼950–930 Ma granulites, partially overprinted by Caledonian eclogite-facies metamorphism at ∼425 Ma and amphibolite-facies metamorphism at ∼410 Ma. Geochemical and Rb-Sr data from more than 10 phengite fractions separated from one sample reflect the composition of the microdomain (a few hundred microns in size) in which phengite crystallized. Phengite crystallized after garnet or plagioclase by dissolution-precipitation processes yield apparent age between 700 and 600 Ma. At the time of their crystallization, these phengites inherited the isotopic composition of their precursor minerals, at a microdomain scale. Phengite from quartz veins, which crystallized from elements mobilized by the circulating fluid, yield an age closer to the eclogite-facies metamorphic age. The closed system evolution of the eclogitizing fluid, the segregation of textural and reactional microdomains, the high Sr content of the studied phengite, and the short duration of the recrystallization processes (<1Ma) are interpreted as the main factors responsible for the lack of a Rb/Sr isotopic equilibrium, at the scale of hand samples. Such equilibrium is nevertheless reached in quartz veins where the crystallization of minerals implies that the fluid circulation acted as a factor of isotopic homogenization. The in situ single mineral Ar/Ar datings revealed that both eclogite- and amphibolite-facies minerals are characterized by an excess of radiogenic argon (ages between 425 and 520 Ma). The excess of argon has been inherited from the previous granulite and has been only partially evacuated from the system by the circulating fluid. The apparent Sm/Nd ages from garnets inherited from the granulite-facies metamorphism (c. 930 Ma) are in agreement with previous estimates. This result confirms that the diffusion of Nd in garnet does not occur at temperatures lower than 700°C. This study highlights the complexity of radiochronometer behavior during HP metamorphism and demonstrates that coupling different radiochronometers, such as Ar/Ar and Rb/Sr, does not always guarantee the validity of the geochronological results.
ISSN: 1525-2027

hal-00407885
https://hal.archives-ouvertes.fr/hal-00407885
DOI : 10.1029/2008GC002098