Résumé : The slides were taken on collecting trips sponsored by the William L. Bryant Foundation, where books, music and art indigenous to the regions were gathered. The are organized by geographical location.
View of Steamship (S.S.) Regina, a crowd of people, and automobiles on the pier in front of the Grenada Port Authority in Saint George’s, Saint George, Grenada. S.S. Regina, originally built in 1939, is docked at the port. S.S. Regina was christened S.S. Panama for Panama Line, formerly Panama Railroad Steamship Line. In 1941, the United States Army Transport Service converted her to a troop carrier and renamed her James Parker. By 1957, she was sold to American President Lines, formerly Dollar Steamship Lines. She was renamed President Hoover to replace another of American’s steamships by the same name. In 1964, she was acquired by Chandris Cruises and renamed Regina. She was scrapped in 1985 as S.S. Regina Prima. Passengers wait in automobiles, such as the Ford Zodiac, as the traffic is surrounded by pedestrians. A Royal Grenada Police Force officer, dressed in a white helmet and light blue shirt, is standing near one of the port facilities. In distance is a view of buildings in Saint George’s including the Cathedral of the Immaculate Conception which dates back to 1818. This Roman Catholic church also features Gothic arched windows and tower. Slide labeled Gren. 6
Grenada -- Caribbean region -- Saint George's, Saint George

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM1972_01a
Sheet 43:6
http://ufdc.ufl.edu/AA00029602/00001

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : This article considers economic risks which could potentially threaten the competitiveness and sustainability of cruise destinations such as New Zealand. Included in this article are those economic risks which are factored into cruise lines’ decisions as to whether to send their ships to a destination and the destination’s capacity to host these ships and their passengers. A cruise life-cycle framework has been developed to provide a structure for discussion: (a) product development; (b) infrastructure development; (c) distribution; (d) consumption; and (e) disposal. Five strategies for managing economic risks are presented: the formation of an adequately funded peak committee; the cultivation of a cruise culture; the provision of appropriate training; the creation of a national cruise manual; and the design, development and implementation of a cruise brand. Each of these strategies is based on an approach to risk management which calls for a positive view of risk and how it can be transformed into competitive success.
Cet article examine les risques économiques qui pourraient potentiellement menacer la compétitivité et la durabilité des destinations de croisière telle que la Nouvelle-Zélande. Les risques économiques inclus dans cet article relèvent des décisions compagnies de croisières que d'envoyer ou non leurs navires vers une destination et la capacité de la destination pour accueillir ces navires et leurs passagers. Un cadrage du cycle de vie de la croisière a été établi pour fournir de base de discussion: le développement de produits (a), le développement des infrastructures (b), la distribution(c) ; la consommation(d), et l'élimination(e). Cinq stratégies pour gérer les risques économiques sont présentées : la formation d'un comité de financement de pointe adéquat, le développement d'une culture de la croisière, la fourniture d'une formation appropriée, la création d'un manuel de croisière nationale et la conception, le développement et la mise en œuvre d'une marque « croisière ». Chacune de ces stratégies repose sur une approche de gestion des risques qui appelle à une vision positive du risque et de la façon dont il peut être appréhendé avec succès dans la compétition.
Nouvelle-Zélande

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.5134
http://journals.openedition.org/etudescaribeennes/5134

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : La mer des Caraïbes est un espace emblématique de la croisière. Au-delà de la réputation mondiale de ses destinations, des cartes postales qui vantent les charmes de la région, l’analyse de l’industrie de la croisière permet de souligner certaines limites et contradictions des modalités de développement actuelles. Le produit « croisière » a considérablement évolué : désormais c’est le paquebot en lui-même (temple de la consommation et enclave flottante) qui est devenu la destination du croisiériste. Ouverture au tourisme de masse, gigantisme des bateaux, rationalisation et optimisation des coûts dans le cadre d’un marché de plus en plus globalisé et capitalistique sont autant de données qui doivent être analysées pour comprendre l’évolution récente de la croisière et les défis renouvelés pour les territoires d’accueil.
The Caribbean Sea is emblematic of the cruise, it is known for its international routes, scenic postcards touting the charms of the region. The analysis of the cruise industry will highlight some limits and contradictions of current development patterns. The product "cruise" has evolved considerably. It’s now the cruise ship itself (temple of consumption and enclave floating) that became the object of the Cruise, the “Destination” of the cruise line.The cruise is part of mass tourism. It’s characterized by its huge boats, rationalization and cost optimization in the context of a market increasingly globalized capital. All data that must be analyzed to understand recent developments in the cruise and repeated challenges to the host territories.
El Mar Caribe es un emblema de la travesía. Esta conocido por sus rutas internacionales, postales escénicas explicando en detalle los encantos de la región. El análisis de la industria de los cruceros pondrán de relieve algunos límites y contradicciones de los patrones actuales de desarrollo. El producto "crucero" ha evolucionado considerablemente. Ahora es el crucero en sí (el templo del consumo y el enclave flotante) que se convirtió en el objeto del Crucero, el Destino "de la línea de cruceros. El crucero es parte del turismo de masas. Se caracteriza por sus grandes barcos, la racionalización y optimización de costes en el contexto de un mercado de capitales cada vez más globalizado. Todos los datos que se deben analizar para comprender la evolución reciente en el crucero y constantes desafíos a los territorios de acogida.
Caraïbes

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.3843
http://journals.openedition.org/etudescaribeennes/3843

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The Tyrrhenian Sea is usually interpreted to be a Neogene back-arc basin that opened by continental rifting and oceanic spreading caused by the eastward migration of the Apennine subduction system during Miocene and Pliocene times. Rifting of the southern Tyrrhenian Sea started first along the Eastern Sardinian margin during the middle to late Miocene times, including the Messinian. The "METYSS" project aims at better constraining the relationships between crustal tectonics, salt tectonics and sedimentation from Messinian times to present-day. The "METYSS 1" cruise (2009) allowed to acquire about 1200 km of HR seismic-reflection profiles along the Eastern Sardinian margin, Western Tyrrhenian Sea. This data set clearly illustrates that this area has been highly dissected during the rifting stage by N-S trending normal faults delineating ridges and basins, as previously described. The Messinian seismic markers (UU and MU) locally display fan-shaped stratal geometries, but the mechanism responsible for such geometries, salt tectonics or rifting, has yet to be carefully deciphered. We also mapped the spatial distribution of the mobile salt. The highly variable thickness of the small confined salt basins may be related to the initial pre-Messinian basin geometry, to the fact that salt deposition was syn-rift or to salt movement. Southeastward, salt tectonics is vigorous in unconfined basins and appears to have started early during the UU deposition. More surprisingly, our data demonstrate that some of the major faults have been significantly reactivated during the post-rift period, up to late Quaternary time, as shown by bathymetric scarps and associated debris flows. Moreover, some of this post-rift deformation can be evidenced within the Plio-Quaternary sequence by a regional unconformity. The post-Miocene deformation style varies greatly between different areas of the margin, and can also be strongly influenced by the presence or absence of mobile Messinian salt.
ISSN: 0040-1951

hal-00996665
https://hal.archives-ouvertes.fr/hal-00996665
DOI : 10.1016/j.tecto.2013.12.015

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
New outcrops in the Sinis peninsula (Sardinia, Italy) allow a detailed description of the Messinian erosion surface. The correlation between outcrops, industrial seismic data and data collected offshore Oristano from a recent cruise permits reconstruction of the geometry of this surface from presently emerged interfluves to the deep canyons offshore, with: - onshore: an eroded karstic plateau presently cropping out over a 20 km × 5 km area. Well-preserved karst structures occur locally and can form several metres high reliefs. The southernmost edge of the plateau is limited by a cliff. The karstic plateau and the cliff are sealed by transgressive deposits of Pliocene age; - offshore, an interfluve zone with a mostly flat and low-angle dipping plateau, westward dissected by paleovalleys which were identified down to a depth of 2000 m. In the Oristano Gulf, Messinian paleovalleys were also identified. The Capo San Marco paleocliff was probably located on the edge of a canyon. Onshore, only one major erosion surface was identified, located at the top the Messinian sequence. Offshore, this surface extends down to the abyssal plain. The surface was emplaced above deposits related to the Terminal Carbonate Complex. This indicates that the marginal evaporites are older than the major drawdown of the Mediterranean sea-level. The major drawdown is related to the deposition of the deep evaporites.
ISSN: 0037-0738

hal-00407864
https://hal.archives-ouvertes.fr/hal-00407864
DOI : 10.1016/j.sedgeo.2008.06.005

Éditeur(s) : Gauthier-villars
Résumé : 69 new hydrothermal sites were discovered during the Naudur diving cruise. Dives were conducted between 17 degrees 5 and 18 degrees 40'5 on four segments showing marked contrast in morphology, volcanic, tectonic and hydrothermal activity. At 17 degrees 10'5, 17 degrees 25'5 and 18 degrees 37'5 the ridge has a dome shaped cross-section and is dominated by very active volcanic activity. Early widespread low temperature (<50 degrees C) diffuse hydrothermal discharge is followed by focused high temperature black smokers. At 18 degrees 15'S tectonic activity is dominant, no recent lava was observed, and only two of the 20 hydrothermal sites are active. At 18 degrees 32'5 recent lava representing a new volcanic episode partly covers the bottom of the graben. Deep hydrothermal convection is reactivated with new black smokers along the graben wall. Also, there is low temperature shimmering water from cooling lava flows. These three segments can be considered as successive volcanic/tectonic episodes typical of a fast spreading ridge. Further, the observations support a new model for the temporal evolution of episodic hydrothermal activity. Hydrothermal convection is unstable and superficial during the volcanic stage (dykes injection). At the beginning of the teaonic stage (graben formation) faults allow deep circulation and hot fluid to reach the surface. As the graben widens hydrothermal activity is less important and may cease. The heat of a new volcanic episode reactivates the deep hot water circulation along the graben faults completing a cycle.
69 nouveaux sites hydrothermaux ont été découverts entre 17'5 et 18'40'5 sur quatre segments présentant des activités volcaniques et tectoniques contrastées. A 17°10'S,17025'S et 18'37'5, la ride forme un dôme et l'activité volcanique est dominante. Les émissions hydrothermales sont d'abord diffuses et de basse température, puis focalisées et de haute température. A 18°15'S la majorité des sites hydrothermaux sont inactifs dans un graben axial dépourvu de laves récentes. A 18'32'5, des laves récentes s'épanchent au fond du graben. Les circuits hydrothermaux réactivés par le nouvel épisode volcanique se traduisent par des diffusions sur les laves récentes et par une reprise des émissions de haute température le long des murs du graben. Ces quatre segments traduisent des épisodes volcanoltectoniques successifs, caractéristiques de I'évolution temporelle des dorsales rapides. Les observations permettent de proposer un nouveau modèle de l'activité hydrothermale. Les circuits hydrothermaux sont diffus, peu structurés, instables et superficiels durant les épisodes volcaniques. Au début des épisodes tectoniques, les failles du graben drainent les fluides chauds en profondeur, puis lorsque le graben s'élargit, l'activité s'interrompt. La reprise de l'activité volcanique réamorce les circulations profondes le long des failles du graben.
Comptes Rendus de l'Academie des Sciences Serie II (1251-8069) (Gauthier-villars), 1994-12 , Vol. 319 , N. 11 , P. 1399-1406

Droits : Académie des Sciences
http://archimer.ifremer.fr/doc/00183/29455/27889.pdf
http://archimer.ifremer.fr/doc/00183/29455/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Ce texte pose les bases d’une réflexion sur les fondements de l’industrie de la croisière et sur l’importance et la portée de ce secteur d’activité. Il s’interroge notamment sur les relations entre les compagnies de croisières et le port récepteur des croisiéristes lors des excursions. Le produit croisière construit à partir des années 1970 a donné naissance à un tourisme de masse spécifique ; le bateau est à la fois le moyen de transport et la destination. Les escales n’ont qu’un rôle secondaire dans cette logique qui privilégie le gigantisme, la standardisation et l’uniformisation. Alors que le gigantisme touche certaines limites, l’offre croisière se recompose spatialement et innove sur les segments du haut de gamme et du luxe.
This paper proposes a reflection on the cruise industry, the importance and scope of this industry. One of the objectives is to examine in particular the relationship between cruise lines and ports that receive cruises and excursionists. The cruise product built from the 1970s engendred a specific mass tourism. And the boat is both the means of transport and the destination. The stops have a secondary role in this logic that favors gigantism, standardization and uniformity. While gigantism known some limits, cruise products reconstructs itself spatially and innovative segments of the high-end and luxury.

Droits : info:eu-repo/semantics/openAccess
http://journals.openedition.org/etudescaribeennes/5623

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : La croisière en Polynésie est une pratique assez peu développée et fragile. L’éloignement, le manque d’infrastructures, le manque de souplesse de la règlementation ont longtemps été montrés du doigt pour expliquer ses difficultés. Mais parler de la croisière en Polynésie française est chose complexe, car elle regroupe des pratiques assez diversifiées dans leurs formes, les profils des touristes, les lieux investis, et les enjeux sociaux et économiques qui en découlent. Depuis quelques années, il semble que la croisière soit un des axes de développement touristique choisi par le pouvoir local. Papeete a été ainsi au cœur d’une série d’aménagements qui ont à la fois servi la croisière et renforcé l’urbanité de cette ville.
Cruise in French Polynesia is a rather little developed and fragile practise. The distance, the lack of infrastructures, the lack of flexibility of the rules was pointed for a long time to explain its difficulties. The analysis of cruise in French Polynesia is difficult because it includes diversified practices as in their forms, the profile of the tourists, the explored places, and social and economic impacts. Cruise seems to become one of the axes of tourist development policies set by the local government. Papeete is in the heart of developments which have also served cruise and strengthened the “urbanity” of this city.
Polynésie française

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.5143
http://journals.openedition.org/etudescaribeennes/5143

Éditeur(s) : HAL CCSD AGU and the Geochemical Society
Résumé : International audience
Rainbow is a dome-shaped massif at the 36°14′N nontransform offset along the Mid-Atlantic Ridge. It hosts three ultramafic-hosted hydrothermal sites: Rainbow is active and high temperature; Clamstone and Ghost City are fossil and low temperature. The MoMARDREAM cruises (2007, 2008) presented here provided extensive rock sampling throughout the massif that constrains the geological setting of hydrothermal activity. The lithology is heterogeneous with abundant serpentinites surrounding gabbros, troctolites, chromitites, plagiogranites, and basalts. We propose that a W dipping detachment fault, now inactive, uplifted the massif and exhumed these deep-seated rocks. Present-day deformation is accommodated by SSW-NNE faults and fissures, consistent with oblique teleseismic focal mechanisms and stress rotation across the discontinuity. Faults localize fluid flow and control the location of fossil and active hydrothermal fields that appear to be ephemeral and lacking in spatiotemporal progression. Markers of high-temperature hydrothermal activity (∼350°C) are restricted to some samples from the active field while a more diffuse, lower temperature hydrothermal activity (<220°C) is inferred at various locations through anomalously high As, Sb, and Pb contents, attributed to element incorporation in serpentines or microscale-sulfide precipitation. Petrographic and geochemical analyses show that the dominant basement alteration is pervasive peridotite serpentinization at ∼160–260°C, attributed to fluids chemically similar to those venting at Rainbow, and controlled by concomitant alteration of mafic-ultramafic units at depth. Rainbow provides a model for fluid circulation, possibly applicable to hydrothermalism at oceanic detachments elsewhere, where both low-temperature serpentinization and magmatic-driven high-temperature outflow develop contemporaneously, channeled by faults in the footwall and not along the detachment fault.
ISSN: 1525-2027

hal-01115281
https://hal.archives-ouvertes.fr/hal-01115281
https://hal.archives-ouvertes.fr/hal-01115281/document
https://hal.archives-ouvertes.fr/hal-01115281/file/Andreani_et_al-2014-Geochemistry%2C_Geophysics%2C_Geosystems.pdf
DOI : 10.1002/2014GC005269

Éditeur(s) : Wiley InterScience
Résumé : This paper reports on the status and design of the operational remotely operated vehicle Victor 6000, rated for 6000 m depth and of the 3000 m depth autonomous underwater vehicle Asterxx operated by Ifremer the French Institute for Sea Exploitation. Victor 6000 is part of a global system built of subsystems, scientific modules, winch and cable, dead weight and umbilical, positioning subsystem using acoustic ultra short base line (USBL) techniques, and software for data and dive management. In 2005 the system was equipped with a second toolsled dedicated to high resolution mapping of the sea bed, with both acoustical and optical devices. Asterxx, the first autonomous underwater vehicle (AUV) developed by IFREMER, is 4.5 m in length with a diameter of 0.69 m. Depending on the payload, its weight is between 600 and 800 kg in air,with a diving depth of 3000 m. Its cruising speed is between 0.5 and 2.5 ms. The AUV is capable of carrying various payloads for a wide spectrum of applications. The vehicle can cruise up to 100 km. For coastal applications this vehicle is operable by a limited crew potentially from a nonspecialized vessel. Both vehicles are used for oceanography as well as to continually evolve underwater systems to address new scientific challenges.
Journal of Field Robotics (1556-4959) (Wiley InterScience), 2007-06 , Vol. 24 , N. 6 , P. 449-459

Droits : 2007 Wiley InterScience
http://archimer.ifremer.fr/doc/2007/publication-2806.pdf
DOI:10.1002/rob.20195
http://archimer.ifremer.fr/doc/00000/2806/

Éditeur(s) : Ieee
Résumé : The Momareto cruise was held from August 6 to September 6, 2006 on the new French oceanographic vessel Pourquoi pas? The ROV Victor 6000 visited three vent fields, ranging from 850m to 2300m, on the Mid-Atlantic Ridge. The scientific objective of the cruise was to study the spatial and temporal dynamics of hydrothermal communities colonizing these active vent sites. Aside scientific and technological objectives, one of the major goals of this cruise was to share the excitement of our science with the public. For this, the results of the project were shared through different media. The most challenging and exciting communication event remains the real-time transmission of images acquired by the ROV Victor at 1700m depth to a 250 person audience on land.
Oceans 2007 - Europe, Vols 1-3 (Ieee), 2007 , P. 707-710

Droits : 2007 IEEE
http://archimer.ifremer.fr/doc/2007/publication-3599.pdf
http://archimer.ifremer.fr/doc/00000/3599/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
At the North-Ecuadorian convergent margin (1°S–1.5°N), the subduction of the rough Nazca oceanic plate leads to tectonic erosion of the upper plate and complex seismogenic behavior of the megathrust. We used three selected pre-stack depth migrated, multi-channel seismic reflection lines collected during the SISTEUR cruise to investigate the margin structure and decipher the impact of the subducted Atacames seamounts on tectonic erosion, interseismic coupling, and seismogenesis in the region of the 1942 Mw7.8 earthquake.This dataset highlights a subducted ∼30×40 km∼30×40 km, double-peak seamount that belongs to the Atacames seamount chain and that is associated with a deep morphologic re-entrant containing mass transport deposits.The seamount subduction uplifted the margin basement by ∼1.6 km and pervasively broke the margin by deep and intense reverse faulting ahead of the seamount, a process that is likely to weaken considerably the margin. In the seamount wake, the basement reverse fault system rotated counter-clockwise. This faulted basement is overlain with slope sediment sliding along listric normal faults that sole out onto the BSR. This superposition of deep tectonic contraction within the basement and shallow gravitational extension deformation within the sediment highlights the key role of gas hydrate on outer slope erosion.In addition to long-term regional basal erosion, the margin basement has thinned locally by an extra 0.8–1 km in response to the subduction of the Atacames seamount chain and hydrofracturing by overpressured fluids at the margin toe. This pervasively and deeply fractured margin segment is associated with a seismically quiet and GPS-modeled low interseismic coupling corridor that terminates downdip near the 1942 epicenter and locked zone. We suggest that the deeply buried double-peak Atacames seamount triggered the 1942 earthquake ahead of its leading flank. This result supports previous studies proposing that subducted seamounts provide unfavorable conditions for locking the updip segment of the plate boundary limiting the updip extent of seismogenic zones, but may favor large subduction earthquakes at greater depths.
ISSN: 0012-821X

hal-01256399
https://hal.archives-ouvertes.fr/hal-01256399
DOI : 10.1016/j.epsl.2015.10.043

Éditeur(s) : HAL CCSD IODP
Résumé : Integrated Ocean Drilling Program (IODP) Expedition 335 (14 April–4 June 2011) will be the fourth ocean cruise of the "Superfast" campaign to drill a deep hole into intact oceanic basement and will return to Ocean Drilling Program (ODP) Hole 1256D to deepen this scientific reference penetration a significant distance into cumulate gabbros. Cores and data recovered during the Superfast 4 expedition will provide hitherto unavailable observations that will test models of the accretion and evolution of the oceanic crust. Site 1256 was specifically located on oceanic crust that formed at a superfast spreading rate (>200 mm/y) to exploit the observed relationship between spreading rate and depth to axial low velocity zones, thought to be magma chambers, seismically imaged at active mid-ocean ridges. This was a deliberate strategy to reduce the drilling distance to gabbroic rocks because thick sequences of lavas and dikes have proved difficult to penetrate in past. ODP Leg 206 (2002) initiated operations at Site 1256, including the installation in Hole 1256D of a reentry cone with 16 inch casing inserted through the 250 m thick sedimentary cover and cemented into basement to facilitate deep drilling. The hole was then cored ~500 m into basement. IODP Expeditions 309 and 312 (2005) successfully completed the first sampling of an intact section of upper oceanic crust from lavas, through the sheeted dikes, and into the upper gabbros. Hole 1256D now penetrates >1500 meters below seafloor (mbsf) and >1250 m subbasement and currently resides in the dike–gabbro transition zone. The first gabbroic rocks were encountered at 1407 mbsf. Below this lies a ~100 m complex zone of fractionated gabbros intruded into contact metamorphosed dikes. Although previous cruises achieved the benchmark objective of reaching gabbro in intact ocean crust, critical scientific questions remain. These include the following: 1. Does the lower crust form by the recrystallization and subsidence of a high-level magma chamber (gabbro glacier), crustal accretion by intrusion of sills throughout the lower crust, or some other mechanism? 2. Is the plutonic crust cooled by conduction or hydrothermal circulation? 3. What is the geological nature of Layer 3 and the Layer 2/3 boundary at Site 1256? 4. What is the magnetic contribution of the lower crust to marine magnetic anomalies? Hole 1256D is poised at a depth where samples that should conclusively address these questions can be obtained, possibly with only a few hundred meters of drilling. Importantly, as of the end of Expedition 312, the hole was clear of debris and open to its full depth. Increased rates of penetration (1.2 m/h) and enhanced core recovery (>35%) in the gabbros indicate that this return to Hole 1256D could deepen the hole >300 m into plutonic rocks, past the transition from dikes to gabbro, and into a region of solely cumulate gabbroic rocks.
https://hal.archives-ouvertes.fr/hal-00564953

hal-00564953
https://hal.archives-ouvertes.fr/hal-00564953
DOI : 10.2204/iodp.sp.335.2010

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Le secteur de la croisière connaît un essor considérable dans l’espace méditerranéen. Si pour l’heure cette croissance profite essentiellement à la rive nord, qui dispose des infrastructures nécessaires, le potentiel de développement est immense dans les pays de la rive sud. Avec la croisière, ces derniers peuvent trouver l’occasion de diversifier leur offre touristique et de valoriser économiquement leurs villes portuaires, qui, pour la plupart, bénéficient d’un patrimoine culturel très important. Cet article étudie la manière dont l’essor de l’activité sur la rive sud de la Méditerranée peut être mis au service d’un projet de développement. L’étude de cas porte sur la ville de Casablanca, capitale économique du Maroc, qui, bien que mal valorisée sur le plan touristique, s’impose spontanément comme la première destination du tourisme de croisière au Maroc. Le développement de l’activité est l’occasion pour les autorités locales de mettre en œuvre une stratégie d’intégration du port dans la ville qui redéfinit entièrement la fonction du port dans la métropole.
The cruise industry has grown considerably in the Mediterranean. this growth benefits mainly to the north shore, which has the necessary infrastructure development but the potential is immense in the countries of the southern shore. With the cruise, they may find the opportunity to diversify their tourism offer and enhance their economically port cities, which for the most part, have a very important cultural heritage. This article examines how the rise of activity on the southern shore of the Mediterranean can be put at the service of a development project. The case study focuses on the city of Casablanca, the economic capital of Morocco, which, although poorly valued on the tourist map, is necessary spontaneously as the first destination of cruise tourism in Morocco. Development activity is an opportunity for local authorities to implement an integration strategy in the port city that completely redefines the function of the port in the city.
Casablanca

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.5167
http://journals.openedition.org/etudescaribeennes/5167

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Sur la terre ferme, la sécurité est devenue un thème récurrent de la vie politique, des imaginaires voire de la réalité. Dans le monde de la croisière au contraire, la communication vend un univers idyllique. Or la réalité de la vie à bord du navire n’est pas faite que de bonheur, et les armateurs, les voyagistes, les équipages et les autorités administratives anticipent des situations qui mettent en péril les passagers. La gestion des épidémies ne se limite pas à la grippe H1N1, moment exceptionnel qui cache la réalité fréquente des épidémies de gastro-entérite. Le quotidien sécuritaire est aussi constitué par les risques plus traditionnels : le feu et le naufrage. La croisière également s’accompagne de viols et violences sur des croisiéristes, voire de disparitions de passagers. Ces trois dangers de la croisière font l’objet de mesures de santé publique, de définition de normes de sécurité internationales depuis 1914, et de mesures législatives récentes, puisque le dernier texte a été promulgué par le président Obama en juillet 2010. L’Europe montre un retard important dans l’organisation de cette politique, gage de développement de l’industrie de la croisière.
On land, security has become a recurring theme in the political life of the imagination or reality. In the world of cruising the contrary, communication sells idyllic world. The reality of life on the ship is not made that happiness, and shipowners, operators, crews and administrative authorities anticipate situations that endanger passengers. Outbreak management is not limited to the H1N1 exceptional moment that hides the reality of frequent outbreaks of gastroenteritis. The daily safe is also constituted by the more traditional risks: fire and sinking. The cruise also accompanied by rape and violence on cruise or disappearances of passengers. These three dangers of the cruise are the subject of public health measures, definition of international safety standards since 1914, and recent legislation, since the final text was issued by President Obama in July 2010. Europe shows a significant delay in the organization of the political guarantee for the development of the cruise industry.

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.5220
http://journals.openedition.org/etudescaribeennes/5220

Éditeur(s) : Amer Geophysical Union
Résumé : The Algerian margin has originated from the opening of the Algerian basin about 25-30 Ma ago. The central margin provides evidence for large-scale normal faults of Oligo-Miocene age, whereas transcurrent tectonics characterizes the western margin. A set of NW-SE oriented dextral transform faults was active during basin opening and divided the 600 km long central margin into segments of similar to 120-150 km. The upper Miocene, Plio-Quaternary, and present-day tectonic setting is, however, compressional and supports the occurrence of a margin inversion, a process still poorly documented worldwide. We show that the central Algerian margin represents a rare example of inverted margin, where the process of subduction inception is particularly well expressed and helps understand how extensional and transtensive structures are involved in margin shortening. Using multibeam bathymetry and multichannel seismic reflection sections from the MAR-ADJA 2003 and 2005 cruises, we evidence Pliocene-Pleistocene shortening with contrasting styles along the margin between west (Khayr Al Din bank) and east (Boumerdes-Dellys margin) of Algiers. Pre-Miocene structures such as basement highs and transform faults appear to control changes of the deformation pattern along this part of the margin, resulting in different widths, geometries, and relative positions of folds and faults. Plio-Quaternary and active blind thrust faults do not reuse Oligo-Miocene normal and transform faults during inversion, but instead grow within the continental margin (as testified for instance by the 21 May 2003 M-w 6.8 Boumerdes-Zemmouri earthquake), at the foot of the continental slope and at the northern sides of basement highs interpreted as stretched continental blocks of the rifted margin. The inherited structures of the margin appear, therefore, to determine this deformation pattern and ultimately the earthquake and tsunami sizes offshore. The complex geometry of the fault system along the Algerian margin suggests a process of initiation of subduction in its central and eastern parts.
Tectonics (0278-7407) (Amer Geophysical Union), 2010-03 , Vol. 29 , N. TC2008 , P. 1-22

Droits : 2010 American Geophysical Union
http://archimer.ifremer.fr/doc/00008/11883/9286.pdf
http://archimer.ifremer.fr/doc/00008/11883/9287.pdf
DOI:10.1029/2009TC002547
http://archimer.ifremer.fr/doc/00008/11883/

Éditeur(s) : Gauthier-villars
Résumé : 70 hydrothermal sites were observed during the 23 dives of the French submersible Nautile (''Naudur'' cruise, December 1993), at 17-degrees-19-degrees-S on the East Pacific Rise. Large vent-animal communities are present around these sites. The zoological composition of these communities is the same as that of the communities at 11-degrees-13-degrees-N and 21-degrees-N on the East Pacific Rise. However, the distribution of the species on the sites is different from all the other hydrothermal communities; large anemone fields of several hundred square metres, associated with colonies of Bathymodiolus and Calyptogena, have been observed. Fresh lava areas seem to bear the most important biological activity.
70 sites hydrothermaux actifs ont été découverts lors des 23 plongées du submersible français Nautile (campagne « Naudur », décembre 1993) sur la dorsale Est Pacifique, entre 17°S et 19°S. D'importantes communautés animales leur sont associées, et bien que les animaux qui les constituent soient analogues à ceux observés sur cette même dorsale à 1 r-13°N et 21°N, les structures des peuplements sont différentes de celles connues par ailleurs. Des champs d'anémones et de bivalves (Bathymodiolus et Calyptogena) de plusieurs centaines de mètres carrés ont été observés (17°25'S). Les zones de laves les plus récentes paraissent les plus riches biologiquement
Comptes Rendus de l'Academie des Sciences Serie II (1251-8069) (Gauthier-villars), 1995-01 , Vol. 320 , N. 1 , P. 47-54

Droits : Académie des Sciences
http://archimer.ifremer.fr/doc/00183/29454/27856.pdf
http://archimer.ifremer.fr/doc/00183/29454/

Éditeur(s) : HAL CCSD Elsevier
Résumé : The Gulf of Aigues-Mortes (NW Mediterranean Sea) is a midshelf zone whose scale is an intermediate between the nearshore scale (0–10 m depth) and the coastal scale (including the whole continental shelf). Its hydrodynamics is investigated for the first time. ADCP, CTD and thermosalinograph data were collected during three short cruises (HYGAM; March 6–7, 20–21, April 5–6, 2005). They were scheduled approximately every 15 days to sample the gulf circulation under different weather conditions. Moreover, the cruise data were used to validate the Symphonie model, a 3D primitive equations circulation model. The circulation features displayed by in situ data were well reproduced by Symphonie. A downscaling modelling approach was implemented, the largest scale being obtained by the replay of the MFSTEP regional model of the North-Western Mediterranean Sea. The analysis, closely coupling in situ measurements and model results, provides information that would not have been obtained using data separately. The great variability of the oceanic circulation at this scale is well evidenced. Winds are the main forces, not only locally but also at a larger scale. North winds generate coherent structures interacting with the general Mediterranean circulation. The explanation of the induced currents is then not straightforward, some of them being, for example, northward. South and southeast winds reinforce the sloping surface, the latter allowing the geostrophic equilibrium with longshore currents. This study, focused on the end of winter 2004–2005, also enhances the heat fluxes from offshore to nearshore, as well as the initiation of shelf dense waters. The knowledge of the midshelf oceanic circulation is then applied to run a numerical experiment which describes both the dispersion of a fictive contaminant from a point S (at the centre of the GAM), and evaluates the risk of contamination of the beaches along the GAM shores.
ISSN: 0278-4343

hal-00196620
https://hal.archives-ouvertes.fr/hal-00196620
DOI : 10.1016/j.csr.2007.06.006

Éditeur(s) : Gauthier-villars
Résumé : The aim of the joint French-British CYAPORC submersible cruise was the exploration and sampling of the Porcupine and Goban Escarpments. A paleozoic mesozoic sedimentary cover has been evidenced abov ea caledonian or older cristalline basement on the Porcupine scarp. On the Goban scarp, the observed outcrops are mainly lower Cretaceous carbonates overlying paleozoic sandstones
La campagne de plongée franco-britannique CYAPORC avait pour objet l'exploration et l'échantillonnage des escarpements de Porcupine et de Goban. Sur l'escarpement de Porcupine au Nord, on a mis en évidence, au-dessus d'un socle cristallin calédonien ou plus ancien, une couverture sédimentaire paléozoïque puis mésozoïque. Sur l'escarpement de Goban, les affleurements observés sont des séries du Crétacé inférieur reposantsur des niveaux de grès paléozoïques.
Comptes Rendus de l'Academie des Sciences Serie II (1251-8069) (Gauthier-villars), 1987-04 , Vol. 304 , N. 16 , P. 1003-1008

Droits : Académie des Sciences
http://archimer.ifremer.fr/doc/00184/29489/27853.pdf
http://archimer.ifremer.fr/doc/00184/29489/

Éditeur(s) : Elsevier
Résumé : During the Fanindien 2006 cruise of R/V 'Beautemps-Beaupre', high resolution multibeam bathymetry, sub-bottom profiling and sediment coring was carried out along the East African margin, offshore Tanzania and Mozambique (Indian Ocean). The newly acquired data reveal the presence of a giant deep-sea valley (the Tanzania channel) that is more than 10 km wide at 4000 m water depth, along the continental rise. The valley remains similar to 70 m deep and 7 km wide at 800 km from the Tanzania coast. Morphological comparison with worldwide submarine channels show that the Tanzania channel is one of the largest known submarine valleys. This discovery brings new light on development of submarine valleys that drain sediments originated from the East African Rift System (EARS) highlands (i.e. the Tanzania channel and its neighbor Zambezi channel located similar to 1000 km southward). Both of the systems have a morphology markedly different to the classical sinuous, V-shaped channels located at similar latitudes (e.g. the Zaire or Amazon channels). Their submarine drainage system consists of a downslope converging tributary canyons joining a central trunk channel in the continental rise. The presence of such giant deep-sea drainage systems is probably linked to a strong structural control on the sediment pathway, associated to a massive sediment transfer towards the Indian Ocean in relation with the tectonic activity of the East African Rift System (i.e. the uplift periods trough mid-Miocene and Plio-Pleistocene times) and its interplay with the East African equatorial climate changes.
Marine Geology (0025-3227) (Elsevier), 2008-12 , Vol. 255 , N. 3-4 , P. 179-185

Droits : 2008 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/00324/43491/42958.pdf
DOI:10.1016/j.margeo.2008.09.002
http://archimer.ifremer.fr/doc/00324/43491/