Cette étude présente les architectures et la dynamique sédimentaire de la pente carbonatée au nord de Little Bahama Bank (Bahamas) à partir des données de sondeur multifaisceaux, de sondeur de sédiments (Chirp) et de sismique multitraces Haute Résolution (HR) issues de la mission Carambar 1(2010). Une analyse morpho-sédimentaire de surface permet de définir les grands domaines physiographiques et les éléments architecturaux de la pente et précise la répartition spatiale des sédiments dans le contexte actuel de haut niveau marin relatif. Elle révèle une pente dominée par de la boue de périplate-forme avec différents niveaux d’induration et entaillée par des glissements et des canyons sous marins.La variabilité spatiale du transfert de boue depuis la plate-forme vers la pente, couplée à l’évolution latérale de l’intensité du courant des Antilles est à l’origine de grandes différences morphologiques d’est en ouest. Dans la partie occidentale, la pente est environ deux fois plus étendue que dans la partie orientale,elle s’apparente à un système progradant. La pente orientale, quant à elle, est marquée par des processus de bypass. En effet, cette partie est caractérisée par de nombreux canyons sous-marins se poursuivant par des sillons distributaires alimentant des zones de dépôts distales confinées. Une étude intégrée permet la caractérisation à haute résolution des glissements et des canyons et la proposition d’un modèle déformation. Ces éléments architecturaux sont initiés par des déstabilisations intra-pente et leur évolution est contrôlée par des épisodes d’érosion régressive, la sédimentation pélagique et les écoulements gravitaires boueux. Enfin, une analyse sismo-stratigraphique permet de reconstituer l’évolution tectono-sédimentaire de la pente de l’Albien à l’Actuel en lien avec le contexte géodynamique des Caraïbes, l’eustatisme et la production carbonatée sur la plate-forme. / This study focuses on the architectures and the sedimentary dynamic of a carbonate slope located on the northern part of Little Bahama Bank (Bahamas) using a dataset composed of multibeam echo sounder,subbottom profiler (Chirp) and High-Resolution (HR) multichannel seismic collected during the Carambar 1cruise (2010). A morpho-sedimentary surface analysis defines the physiographic domains and the architectural elements of the slope and investigates the spatial distribution of sediments in the context of the current sea-level highstand. It reveals a slope dominated by periplatform ooze with several levels of induration and incised by numerous slides and submarine canyons. The spatial variability of off-bank transport, combined with the lateral variability of the Antilles Current intensity, are at the origin of a morphological evolution from west to east in the study area. In the western part, the slope is around twice as large as the eastern part and can be considered as a prograding system. The eastern slope is marked by bypass processes. Indeed, numerous submarine canyons are visible on the seafloor and are connected to several shallow distributary furrows feeding confined depositional areas. An integrated study allows a high resolution characterisation of slides and submarines canyons and enables us to propose a model of formation. These architectural elements are initiated by intra-slope destabilisations and their evolution is controlled by phases of retrogressive erosion,pelagic sedimentation and muddy gravity flows. Finally, a seismo-stratigraphic analysis allow to reconstitutethe tectonic and sedimentary evolution of the slope since the Albian to the present-day by establishing a link with the geodynamic context of Caraïbes, relative sea-level changes and the carbonate production on the platform.

Ce travail présente une analyse de la dynamique sédimentaire du système turbiditique actuel de l’Ogooué (Golfe de Guinée), secteur encore très peu exploré à l’heure actuelle. Il se base sur l’interprétation de données géo-acoustiques (sondeur multifaisceaux et sismique chirp), sédimentologiques (carottes küllenberg et interface) et courantométriques issues de campagnes océanographiques réalisées par le SHOM. L’analyse morpho-bathymétrique détaillée a révélé la diversité des structures morphologiques le long de la marge. Ces observations, associées aux données sédimentaires et courantométriques ont permis de préciser les différents processus de dépôt. La configuration du plateau continental, dont la largeur se réduit fortement vers le Nord va entraîner une variabilité des transferts sédimentaires en profondeur le long du système turbiditique de l’Ogooué. La très faible extension du plateau continental à l’extrémité de l’île Mandji et l’action de la dérive littorale favorisent une sédimentation gravitaire active sous la forme d’écoulements turbiditiques dans le canyon du Cap Lopez ou de glissements sous-marins. Grâce à la comparaison de données bathymétriques à différentes échelles de temps, il a été possible de documenter à très haute résolution les mécanismes d’initiation et de développement d’instabilités ainsi que les processus sédimentaires à l’origine du développement des méandres. En plus des apports détritiques, les écoulements gravitaires initiés dans ce secteur vont également transporter de grandes quantités de matière organique. / This work presents an analysis of the sedimentary dynamic in the Ogooué turbidite system (Gulf of Guinea), previously poorly studied. It is based upon the interpretation of geo-acoustic (multibeam bathymetry and imagery, seismic chirp), sedimentological (Küllenberg and interface cores) and current-meter data recovered during oceanographic cruises conducted by the SHOM. The detailed morpho-bathymetric analysis reveals the diversity of morphological structures along the margin. These observations, combined with current meter and sedimentological data allowed us to determine various depositional processes. The decreasing width of the continental shelf toward the North involves a variability of sediment transfer along the Ogooué turbidite system. The very small extension of the continental shelf at the extremity of the Mandji Island and the action of longshore drift promote active gravitary sedimentation dominated by turbiditic flows in the Cap Lopez canyon or submarine slides.By comparing bathymetric data at different time scales, we document the mechanisms responsible for the initiation and development of instabilities and the sedimentary processes related to meander growth. In addition to detrital fraction, the gravity flows initiated in this area also carry large amounts of organic matter.

The small, above-ground masonry structures of northwestern New Mexico called "pueblitos" first came to the attention of anthropologists in over a century ago. In 1920, the noted archaeologist A.V. Kidder hypothesized that these masonry structures might have been built by Puebloan refugees fleeing Spanish reprisals in the wake of the Spanish reconquest of New Mexico after the Pueblo Revolt, and he proposed that this hypothesis be tested. Over the next several decades, however, the hypothesis remained untested, but it became both accepted as established fact and the basis for most anthropological, archaeological, and historical reconstructions of Navajo history and cultural development.

Beginning in the tenth century, Chaco Canyon emerged as an important center whose influence shaped subsequent cultural developments throughout the Four Corners area of the American Southwest. Archaeologists investigating the prehistory of Chaco Canyon have long been impressed by its massive architecture, evidence of widespread trading activities, and ancient roadways that extended across the region. Research on Chaco Canyon today is focused on what the remains indicate about the social, political, and ideological organization of the Chacoan people. Communities with great houses located some distance away are of particular interest, because determining how and why peripheral areas became associated with the central canyon provides insight into the evolution of the Chacoan tradition. This volume brings together twelve chapters by archaeologists who suggest that the relationship between Chaco Canyon and outlying communities was not only complex but highly variable. Their new research reveals that the most distant groups may have simply appropriated Chacoan symbolism for influencing local social and political relationships, whereas many of the nearest communities appear to have interacted closely with the central canyon--perhaps even living there on a seasonal basis. The multifaceted approach taken by these authors provides different and refreshing perspectives on Chaco. Their contributions offer new insight into what a Chacoan community is and shed light on the nature of interactions among prehistoric communities. "The multifaceted approach . . . provides different and sometimes refreshing perspectives on Chaco. Their contributions offer new insight into what a Chacoan community is, and they shed new light on the nature of interactions among prehistoric communities." —Traditional Dwellings & Settlements Review

Social contact norms are used by managers to establish standards for regulating visitation of wilderness areas so that visitors can attain adequate experiences of solitude. This study expanded on current conceptions of social contact norms to provide a theoretical and empirical basis for understanding how such norms are formed. Using person perception, stereotyping, and socialization theory and the concept of cognitive schemata, a conceptual framework was built to explain how visitors come to judge certain groups as appropriate or inappropriate in a wilderness area. Seven research hypotheses were proposed and tested using a database consisting of responses to a mail questionnaire survey of 800 permit requestors and 95 interviews with visitors at Aravaipa Canyon Wilderness, Arizona. The first hypothesis, that wilderness visitors would regard some types of groups as appropriate and other types of groups as inappropriate in the wilderness area, was supported. Norms for encountering 13 types of groups were estimated from written questions and drawings, and paired picture comparisons allowed ranking of six types of groups. Encounters with lone hikers, small groups, medium-sized groups, birdwatchers, youth groups, school classes, and rangers were considered more appropriate than encounters with hunters, horseback riders, packstock users, and nude bathers. Logit and multinomial logit models were used to test the six remaining hypotheses, which concerned the influences of socialization and other processes on development of social contact norms. To test the hypotheses, norms for encountering six types for groups were predicted from demographic and other variables. The results indicated that norms for encountering small groups were not affected by social class or race; affiliation with a small group during a wilderness visit was associated with a dislike of large groups, membership in a conservation organization had no such association; members of conservation organizations preferred fewer encounters with hunters; membership in a conservation organization also prompted the respondents to dislike encounters with horseback riders; females, older visitors, and people with children disliked encountering nude bathers; and inexperienced and less self-reliant visitors enjoyed encounters with rangers. Theoretical, managerial, and social implications of these results were then discussed.

The coal-bearing Dakota Sandstone at Coal Canyon, Arizona, which is located in the western portion of the Black Mesa basin, has yielded abundant, diverse, and generally well-preserved spores, pollen, and microplankton. The formation is characterized by high frequencies of fern spores, especially striate spores belonging to the Schizaeaceae, and angiospermous pollen consisting primarily of simple tricolpate and tricolporate grains. Gymnospermous pollen is comparatively uncommon. The microflora assemblage contains many exclusively Cretaceous species previously reported from Australia, western Europe, Siberia, and other localities of North America. A microflora which compares closely with the Dakota assemblage occurs in the Woodbine strata of Oklahoma. On the basis of palynologic evidence, the age of the Dakota Sandstone at Coal Canyon, is interpreted as lowermost Upper Cretaceous (Cenomanian).

By examining halokinetics and channel evolution in a deep-water system, we investigate how submarine channel morphology is affected by changing seascape linked to diapirism. The study area is located in Mississippi Canyon, Gulf of Mexico (GOM), situated directly off the continental slope in a prominent salt dome region. Interactions of salt domes with submarine channels in the GOM are poorly documented. Utilizing 3D seismic data and seismic geomorphology techniques, a long-lived Plio-Pleistocene submarine channel system has been investigated to develop a relationship between variable phases of salt movement and plan-form morphology of preserved channels. We suggest that halokinetics acts as a driver for topographic-channel evolution in the study area. We show how submarine channel morphology can be directly controlled by halokinetics, where salt movement can act as a structural control on both location and morphology of meandering channel complexes. Channels are able to move towards an equilibrium state only when holokinetics decreases.

Dendroarchaeological samples can contain three kinds of information: chronological, behavioral, and environmental. The decisions of past people regarding species selection, beam size, procurement and modification techniques, deadwood use, and stockpiling are the most critical factors influencing an archaeological date distribution. Using dendrochronological samples from prehistoric and historic period sites in the same area of eastern Utah, this paper examines past human behavior as the critical factor in dendroarchaeological date distributions.

Les systèmes radar à synthèse d’ouverture (RSO) sont utilisés depuis de nombreuses années pour des applications militaires telles que la détection des cibles cachées. L’amélioration constante de la résolution de ces capteurs permet aujourd’hui d’accéder à un niveau de détail élevé dans la scène imagée. Cependant, l’interprétation de ces images demeure particulièrement compliquée dans le cas des milieux urbains. En effet, ces milieux particuliers sont sièges de nombreux phénomènes physiques et d’interactions multiples qui rendent la tâche de détection difficile et parfois erronée. C’est dans ce contexte que s’inscrit cette thèse. L’objectif est d’étudier la faisabilité de détection d’une cible en non visée directe du capteur à l’intérieur d’une scène simple et représentative du milieu urbain: le canyon urbain. Une étude sur la phénoménologie de propagation électromagnétique à l’intérieur des canyons urbains est menée à l’aide de mesures en environnement contrôlé à échelle réduite. Ces mesures ont permis la validation d’un outil électromagnétique commercial pour l’étude de la propagation d’une configuration à échelle réelle. Se basant sur les résultats de simulation du code électromagnétique validé, un outil maison, dédié à la prédiction des zones de détection d’une cible à l’intérieur d’un canyon urbain et à l’analyse de la signature électromagnétique correspondante, a été développé et validé. En outre, ce code contribue à l’interprétation complète de données radiométriques et interférométriques d’une scène urbaine réelle. / Synthetic Aperture Radar (SAR) systems have been used since many years for military applications such as the detection of hidden targets. With improved resolutions of these systems, high level of details can be distinguished in the corresponding images. However, some difficulties are encountered when analyzing the SAR images of urban areas. In particular, in these areas, many physical phenomena and interactions occur that make the detection of a target a challenging task. In this framework, the goal of the thesis is to investigate the feasibility of detecting Non Line Of Sight targets inside a simple and representative scene: the urban canyon. A study of the electromagnetic (EM) phenomenology of propagation inside urban canyons has been performed using indoor data at a reduced scale. These data allowed the validation of an EM commercial tool that studies the EM propagation at a real scale. Based on the results of simulation of this code, an in-house code was developed dedicated to predict the detection of a target inside an urban canyon and to analyze the corresponding EM signature. Moreover, this code contributed to a full interpretation of InSAR data of a real complex urban scene with targets.

The Canyon Range Formation (informal new name), formerly mapped as the Indianola Group within the Canyon Range, is divisible into two distinct, mappable units, A and B. Unit A is nearly all conglomerate strata, and conglomerate texture and sedimentary structures suggest an alluvial fan depositional environment. Precambrian and basal Cambrian quartzite clasts represent the erosional debris from the allochthonous Canyon Range thrust. Unit B is composed of interbedded fluvial sandstone and conglomerates with lacustrine limestones, commonly micritic and/or oncolitic. Conglomerate clasts indicate a Paleozoic carbonate provenance. Unit A, previously mapped as the Indianola, underlies Unit B and correlates with the Price River-lower North Horn Formations of the Pavant Range and Long Ridge. Marginal paleontologic and stratigraphic indicators suggest Unit B to be equivalent to the Paleocene-Eocene North Horn and Flagstaff Formations rather than the Cretaceous Indianola Group. Stratigraphic and structural relationships indicate the last major phase of "Sevier" thrusting ended by Price River (?) time.