![]() | MAP of the COUNTRIES on the SOUTH SEA from Panama to Guayquil Auteur(s) : Kitchin, Thomas, 1718-1784 Éditeur(s) : Strahan and Cadell ( London ) Résumé : Upper right margin: Vol II. (Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program. Panama Colombia South America South America South America Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide. 002625845 AMZ2553 http://ufdc.ufl.edu/UF00066650/00001 | Partager |
![]() | Étude géologique et géophysique des marges continentales passives : exemple du Zaïre et de l'Angola Auteur(s) : Moulin, Maryline Éditeur(s) : Université de Bretagne Occidentale Résumé : The objective of the present work is to study the formation of the passive continental margins of the Central Segment of the South Atlantic, most particularly the Congo and Angola margins. We propose a combined approach, which integrates structural constraints based on geological cross-sections (based on seismic data) and global constraints based on plate kinematic reconstructions. The structural study is based on : i) MCS and refraction data collected during the ZaiAngo programme (a joint project conducted by Ifremer and Total) ; ii) proprietary, industrial seismic data (courtesy of Total) from the Angola margin and iii) on all available seismic lines from the Africa and Brazil conjugated margins, between Walvis Ridge and the Equatorial Fracture Zones. Based on theses data, three structural domains (continental, transitional and oceanic) have been defined, the major characteristics of which are : Crustal thinning occurs abruptly, mostly below the continental slope, over a lateral distance of less than 50 km. The top of the crust deepens as the Moho shallows. Only a few extensional structures are observed ; tilted blocks are very few (one or two, depending on the profile), found only on the upper part of the slope and sealed by a discordance prior to salt deposition. The transitional domain is characterized by the existence of a pre-salt basin lying over a thin crustal layer. No tilted blocks are observed in this domain and reflectors within the pre-salt sediment series are parallel to the base of the Aptian salt, over distances greater than 100 km, precluding the possibility of any significant deformation that would imply large horizontal motions. Two types of crust are observed in the transitional domain. "Type I" crust is found below the undeformed pre-salt sediment series located below the eastern part of the basin ; it is characterized by an upper layer of thickness greater than 5 km and a abnormal velocity layer (7.2 - 7.6 km/s), up to 6 km thick. "Type II" crust is less than 5 km thick and found below the salt compressive front that affects the western part of the basin. The salt cover is continuous (no erosion surface is observed), from the continental shelf to the western termination of the basin. Salt was not deposited in a confined environment (like in the Mediterranean), but in a shallow water, lagunal environment. This imposes the zero-level and constrains the paleo-bathymetry at the time of salt deposition, which dates the latest stage of margin formation. Understanding the formation of a margin cannot be approached without studying the homolog margin. Therefore, it is of major importance to reconstruct the closure of the ocean bordered by these homolog margins and take into account the constraints imposed by the kinematic reconstructions on the lateral motions of the lithospheric plates. In order to assess the relative position of the plates at the ocean closure (prior to crustal thinning), a global study was thus performed, integrating all geophysical and geological constraints, in the ocean and on land. The role of african intra-plate deformation and its limits and their consequences have been thoroughly studied. To juxtapose the margins of the central segment of the Southern Atlantic, it is all the margins bordering the Equatorial Atlantic that need to be adjuste precisely. The kinematic study of this last region shows that the reconstruction obtained are reliable, unambiguous with a quantifiable precision The best fitting poles (obtained using the PLACA software), show that it is impossible to close the margins beyond the superposition of the salt fronts, from the Angola and Brazil margins. The geological cross-sections based on seismic data from the homolog margins indicate that a 330 km wide basin with thin (< 12 km) crust was present at the time of the fit. This basin cannot result from horizontal movement related to pure stretching or simple shear, or any model implying conservative volume. This conclusion is consistent with the existence of presalt reflectors parallel to the salt layer wich extends to the platform: the formation of the pre-salt basin must be related to vertical motions. The scenario that we propose for the evolution of the Congo-Angola margin consist in four stages: the first phase corresponds to extensional deformation limited to the few tilted blocks observed on the upper part of the slope. During the second phase, the main crustal thinning occurs, vertical motions prevailes, resulting in the formation of the continental slope and in the subsidence of the basin. The third phase corresponds to the first stress striction: deformation is concentrated in a limited section of the basin, which corresponds to the salt compression front. A proto-oceanic crust is formed, probably composed of thinned continental crust intruded by mantle material. The second stress striction corresponds to the finale phase, resulting in oceanisation senso stricto. The evolution described shows that we can not apply conservative models for margin formation (such as McKenzie and Wernicke or any of their avatars). In order to explain this thinning, one should investigate non-conservative models (implying geochemical transformation, small scale convection, intrusion...) such as those proposed in marginal or continental basins with no horizontal movments. Ce travail de thèse aborde la formation des marges continentales passives dans le segment central de l'océan Atlantique Sud (plus particulièrement au Congo et en Angola), en intégrant une étude en coupe (étude structurale à partir des coupes sismiques) et une étude en plan (étude cinématique). L'étude structurale de la marge a été réalisée à partir des données de sismique réflexion et réfraction de la campagne Zaïango et d'une compilation de données sismiques réflexion existantes sur toutes les marges africaine et brésilienne entre les zones de fracture équatoriales et la ride de Walvis. L'interprétation de ces données a permis d'individualiser la structure de la marge en trois domaines : continental, transitionnel et océanique et de déterminer quelques points majeurs sur la structuration de la marge. L'amincissement est abrupt, localisé dans la zone de pente continentale et restreint à 50 km. La marge montre peu de structures distensives : seuls un ou deux blocs basculés sont observés en haut de pente continentale. Le domaine transitionnel est caractérisé par la géométrie particulière de la sédimentation anté-salifère, l'absence de blocs basculés et la faible épaisseur de croûte. La couche sédimentaire anté-salifère montre des réflecteurs plans jusqu'à la base du sel, continus sur 100 km, éliminant toutes possibilités de déformation du socle pendant et après son dépôt. La croûte du domaine transitionnel peut-être divisée en deux types : une croûte de type I sur laquelle se déposent les sédiments non déformés, et une croûte de type II sur laquelle se superposent les limites du « front compressif salifère » bien exprimé dans les séries postsalifères. Enfin le sel, que l'on observe depuis la plate-forme jusqu'au bassin profond, ne se dépose pas dans un bassin confiné (comme en Méditerranée) mais à un niveau proche de 0 m (ressemblant probablement à un dépôt de type lagunaire) et donne la paléo-bathymétrie au moment de son dépôt qui marque la fin de la période de formation de la marge. La compréhension de la genèse d'une marge ne peut être approchée sans son homologue. Cette simple constatation, cette évidence, montre toute l'importance que l'on doit apporter à la reconstruction cinématique initiale de l'océan qui borde ces marges homologues et aux contraintes imposées par les reconstructions cinématiques sur les mouvements horizontaux des plaques lithosphériques. Afin d'étudier la position des marges au moment de cette fermeture, c'est-à-dire avant amincissement, une étude globale intégrant l'ensemble des données disponibles, géophysiques et géologiques, océaniques et continentales, a été réalisée. Le rôle de la déformation intraplaque africaine, ses limites et leurs conséquences a, en particulier, été l'objet d'une attention poussée. Pour juxtaposer les marges du segment central, ce sont toutes les marges de l'océan Atlantique Equatorial qui doivent être ajustées précisément. L'étude cinématique réalisée de la région équatoriale montre que l'on obtient une reconstruction fiable et sans ambiguïté, avec une précision que l'on peut quantifier. Les pôles issus de cette étude (et calculés avec le Logiciel PLACA) indiquent qu'il est impossible d'obtenir une fermeture plus serrée que celle qui conduit à la superposition des fronts salifères brésilien et angolais : les coupes issues de la sismique réflexion des deux marges indiquent qu'il subsiste un bassin aminci, large de plus de 330 km et dont la croûte n'excède jamais 13 kilomètres d'épaisseur. La formation de ce bassin ne peut résulter de mouvements horizontaux, ce qui exclut un amincissement par étirement (pure stretching) ou par l'existence d'une faille de détachement (simple shear) ou par quelque modèle conservatif que ce soit. Cette constatation corrobore l'observation de la présence d'horizons anté-salifère parallèles, entre eux et au sel, couche salifère que l'on retrouve sur la plate-forme : la création de ce bassin anté-salifère ne peut être que liée à un mouvement vertical. Le schéma d'évolution que nous proposons à partir des données structurales et des contraintes cinématiques présente quatre étapes : le premier stade correspond à une phase de déformation distensive limitée aux quelques rares blocs basculés observés en haut de pente continentale. C'est durant la deuxième étape que se déroule la phase d'amincissement principal, les mouvements verticaux prévalent, aboutissant à la formation de la pente continentale et à la subsidence du bassin. La troisième phase correspond à une première striction des contraintes : la déformation se concentre sur une partie réduite du bassin, coïncidant avec le front salifère compressif. Une proto-croûte océanique se forme, probablement composée de croûte continentale amincie et intrudée de matériel mantellique. La seconde striction correspond à la phase finale de formation de la marge et aboutit à l'océanisation sensu stricto. L'étude cinématique et la description de l'évolution de la marge à partir des données sismiques montre donc que l'on ne peut envisager l'application d'un modèle de genèse des marges avec conservation de volume (type McKenzie ou Wernicke et leurs avatars) : pour expliquer l'amincissement du bassin, il faudrait probablement nous intéresser aux modèles non-conservatifs (impliquant transformation, convection à petite échelle, ...) qui sont déjà invoqués pour la formation des bassins marginaux ou continentaux, sans mouvements horizontaux. Droits : info:eu-repo/semantics/openAccess http://archimer.ifremer.fr/doc/2003/these-82.pdf http://archimer.ifremer.fr/doc/00000/82/ | Partager |
![]() | Begræbnissplatz der Opfer ; Burial place of the temple offerings ; Burial place of the victims ; Allgemeine historie der reisen zu wasser und lande Éditeur(s) : [s.n.] Résumé : Title from upper margin. Believed to have been published in: Allgemeine historie der reisen zu wasser und lande, v.13. "No. 22"--right upper margin. (Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program. Mexico Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide. 002356711 ALW1139 http://ufdc.ufl.edu/UF00000006/00001 | Partager Voir aussi |
![]() | Le Partie Francoise De l"Isle de Saint Domingue ; Le Petit Atlas Maritime Recueil De Cartes et Plans des Quatre Parties du Monde en Cinq Volumes Auteur(s) : Bellin, Jacques Nicolas, 1703-1772 Éditeur(s) : Chez Didot ( Paris ) Résumé : "Tome 1 No.67" in upper right margin Haiti West Indies Haiti West Indies West Indies Haiti Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide. AAA5880 http://ufdc.ufl.edu/UF00004626/00001 | Partager |
![]() | Carte des Provinces de Cartagene, S Marthe et Venezuela Auteur(s) : Bellin, Jacques Nicolas, 1703-1772 Prévost, 1697-1763 Éditeur(s) : Didot ( Paris ) Résumé : From: Histoire Generale Des Voyages ou Nouvelle Collection de Toutes Les Relations de Voyages. Prime meridian: Paris and Ferro. Relief shown pictorially. Map extends beyond neat line on lower left. In lower right margin: "Tom. XII No 4." Map shows watermark with flower and text. (Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program. (Statement of Responsibility) Par M. B. Ing. de la Marine, 1754. Venezuela Colombia Venezuela Colombia Venezuela Colombia Venezuela Colombia Venezuela Colombia Colombia Venezuela Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide. 002604623 AMX1101 141188694 http://ufdc.ufl.edu/UF00066655/00001 | Partager Voir aussi Maps -- Early works to 1800 ( lcsh ) Maps -- Early works to 1800 ( lcsh ) Early maps -- No scale -- 1754 ( local ) Early maps -- No scale -- 1754 ( local ) Early works to 1800 -- No scale -- 1754 ( local ) Early works to 1800 -- No scale -- 1754 ( local ) No scale -- 1754 ( local ) No scale -- 1754 ( local ) Early maps -- No scale -- 1754 ( local ) Early maps -- No scale -- 1754 ( local ) |
![]() | Le Port au Prince dans l'Isle de St. Domingue Auteur(s) : Bellin, Jacques Nicolas, 1703-1772 Bellin, Jacques Nicolas, 1703-1772 Éditeur(s) : Bellin, Jacques Nicolas ( Paris ) Résumé : From: Le Petit Atlas Maritime Recueil De cartes Et Plans Des Quatre Parties Du Monde. "Tome I, no. 52." Philips No. 3508. Relief shown by hachures. Depths shown by fathoms. Oriented with north toward the lower right. Map shows location of the "Ville du Port au Prince". Partial circle watermark on left margin. (Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program. Haiti Port-au-Prince Port-au-Prince (Haiti) Port-au-Prince (Haiti) Port-au-Prince (Haiti) Port-au-Prince (Haiti) Port-au-Prince (Haiti) Port-au-Prince (Haiti) Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide. 002567846 AMT4144 05409752 http://ufdc.ufl.edu/UF00066653/00001 | Partager |
![]() | Haiti city maps 1:12,500 : Jérémie ; Aquin ; Series E935 Auteur(s) : United States -- Defense Mapping Agency. -- Hydrographic/Topographic Center United States -- National Imagery and Mapping Agency Éditeur(s) : Defense Mapping Agency Hydrographic/Topographic Center ( Washington D.C, Washington D.C ) Résumé : (Language) Parallel text in English and French. Relief shown by contours and spot heights. Contour interval 20 meters. Title from upper margin. Includes index to streets, guide to numbered features, location and boundaries maps, and glossary. "NIMA STOCK NO. E935XAQUIN." "NSN 7643014045079." (Statement of Responsibility) prepared and published by the Defense Mapping Agency Hydrographic/Topographic Center. Haiti -- Aquin Aquin (Haiti) Aquin (Haiti) Droits : This item is a work of the U.S. federal government and not protected by copyright pursuant to 17 U.S.C. §105. 49847439 002802628 http://ufdc.ufl.edu/UF00096314/00001 | Partager |
![]() | Código civil : esta obra contiene el texto del código español, hecho extensivo a Cuba por R.D. de 31 de julio de 1889, con las modificaciones ... /Có ; Código civil (1889) Auteur(s) : Betancourt y Miranda, Angel C. Éditeur(s) : Rambla, Bouza Rambla, Bouza ( La Habana, Cuba ) Résumé : This book had no title page. 3rd edition, authorized with corrections [3a. ed. autorizada y corregida]. The margins are extensively annotated by Mario Diaz Cruz. Droits : All rights reserved by the source institution. 25579347 | Partager |
![]() | Vitzliputzli vornehmster Götze der Mexicaner ; Vitzliputzli - most prominent priest of the Mexicans, copperplate engraving 1755 ; Vitzliputzli the chief god of the Mexicans ; Allgemeine historie der reisen zu wasser und lande Éditeur(s) : [s.n.] Résumé : Title from upper margin. Believed to have been published in: Allgemeine historie der reisen zu wasser und lande, v.13. "No. 23" -- right upper margin. "J.13.D." -- right lower margin. (Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program. Mexico Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide. 002356791 ALW1219 http://ufdc.ufl.edu/UF00000007/00001 | Partager Voir aussi |
![]() | Seamount subduction at the North-Ecuadorian convergent margin: Effects on structures, inter-seismic coupling and seismogenesis, Auteur(s) : Marcaillou, B. Collot, J-Yves Ribodetti, A. d'Acremont, Elia Mahamat, A. Alvarado, A. Auteurs secondaires : Géoazur (GEOAZUR) ; Université Côte d'Azur (UCA) - Centre National de la Recherche Scientifique (CNRS) - Observatoire de la Côte d'Azur - Institut national des sciences de l'Univers (INSU - CNRS) - Université Nice Sophia Antipolis (UNS) ; Université Côte d'Azur (UCA) Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) instituto Geofísico ; Escuela Politécnica Nacional Institut des Sciences de la Terre de Paris (iSTeP) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Centre National de la Recherche Scientifique (CNRS) 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 | Partager |
![]() | Haiti city graphic 1:10,000 : Petit Goâve ; Petit Goâve ; Series E935 Auteur(s) : United States -- Defense Mapping Agency. -- Hydrographic/Topographic Center Éditeur(s) : United States Defense Mapping Agency, Hydrographic / Topographic Center ( Washington, D.C. ) Résumé : (Language) Parallel text in English and French. "Printed by DMAHTC 7-88." Relief shown by contours and spot heights. Contour interval 20 meters. Title from upper margin. "Compiled in 1988 from best available sources." Includes guide to numbered features, location and boundaries maps, and glossary. "DMA STOCK NO. E935XPETITGOAVE." (Statement of Responsibility) prepared and published by the Defense Mapping Agency Hydrographic/Topographic Center. Haiti -- Petit Goâve Petit Goâve (Haiti) Petit Goâve (Haiti) Droits : This item is a work of the U.S. federal government and not protected by copyright pursuant to 17 U.S.C. §105. 49847430 002787116 http://ufdc.ufl.edu/UF00098797/00001 | Partager |
![]() | La Partie Francoise de L'isle de Saint Domingue ; The French part of the Isle of Santo Domingo Auteur(s) : Bellin, Jacques Nicolas, 1703-1772 Bellin, Jacques Nicolas, 1703-1772 Éditeur(s) : Bellin, Jacques Nicolas ( Paris ) Résumé : From: Le Petit Atlas Maritime Recueil De cartes Et Plans Des Quatre Parties Du Monde."Tome. I, No. 67" Philips No. 3508. Map shows the region of today's Haiti. Relief shown pictorially. Depths shown by fathoms. Prime meridian: Paris. Map shows frames with coordinates only in lower and left margins. Map includes compass rose close to the center. Map shows watermark with text. (Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program. Haiti Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide. 002734399 ANL2212 123414576 http://ufdc.ufl.edu/UF90000251/00001 | Partager |
![]() | Republic of Panama Special Map no. 2. Auteur(s) : United States -- Army. -- Corps of Engineers Panama -- Dirección de Cartografía Éditeur(s) : Printed by Army Map Service, Corps of Engineers ( Washington ) Résumé : "Transverse Mercator projection." Relief shown by gradient tints. Marginal maps: Index to adjoining sheets. Accompanied by index map on sheet 27 x 41 cm. (Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program. (Statement of Responsibility) prepared under the direction of the Engineer, USARCARIB ... 3-56. Compilation by the Direción de Cartografía, Ministerio de Obras Públicas, República de Panamá in collaboration with the Inter American Geodetic Survey. Panama Panama Droits : This item is a work of the U.S. federal government and not protected by copyright pursuant to 17 U.S.C. §105. 06928011 map68000414 http://ufdc.ufl.edu/UF00077002/00001 | Partager |
![]() | Carte des observations qui ont été faites sur la Frégate de Roi l'Emeraude en 1753 sur la Caye d'Argent Auteur(s) : Bellin, Jacques Nicolas, 1703-1772 Bellin, Jacques Nicolas, 1703-1772 Éditeur(s) : Didot ( [Paris ) Résumé : (Citation/Reference) Philips, From: Description geographique des débouquemens qui sont au nord de L'Isle de Saint Domingue.... "Pl. XXV" Map shows keys to the north of the Dominican Republic. Watermark with text on right margin. Prime meridian: Paris. (Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program. Turks and Caicos Islands West Indies Bahamas Turks and Caicos Islands Turks and Caicos Islands Turks and Caicos Islands Turks and Caicos Islands Turks and Caicos Islands Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide. 002567940 AMT4239 162533761 http://ufdc.ufl.edu/UF00071891/00001 | Partager Voir aussi Maps -- Early works to 1800 ( lcsh ) Maps -- Early works to 1800 ( lcsh ) Maps -- Early works to 1800 ( lcsh ) Early works to 1800 -- 1:400,000 -- 1753 ( local ) Early maps -- 1:400,000 -- 1753 ( local ) 1:400,000 -- 1753 ( local ) Early works to 1800 -- 1:400,000 -- 1753 ( local ) Early maps -- 1:400,000 -- 1753 ( local ) |
![]() | Haiti 1:50,000 Auteur(s) : United States -- Army Map Service Éditeur(s) : The Service ( Washington ) Résumé : Relief shown by contours and spot heights. "Transverse mercator projection." Includes legend, glossary, and index to adjoining sheets in margins. Some sheets prepared by Service de Géodésie des Forces Armées d'Haiti. (Statement of Responsibility) prepared by the Army Map Serivce, Corps of Engineers, U.S. Army. Haiti Haiti Droits : This item is a work of the U.S. federal government and not protected by copyright pursuant to 17 U.S.C. §105. 06885972 http://ufdc.ufl.edu/UF00078623/00001 | Partager |
![]() | Journal du siège de la Martinique par l'armée et la flotte anglaise commandées du g.al Grey et du vice amiral Joh. Jervis Auteur(s) : Rochambeau, Donatien Marie Joseph de Vimeur, 1750-1813 Résumé : Title from PDF caption (LLMC Digital, viewed on Nov. 11, 2011) Manuscript. "Ce mémoire est écrit de la main du général Rochambeau"--Margin note on leaf 1. Signed and dated at end: Philadelphie, 14 Fuctidor an 2e, Le General Rochambeau. Martinique France Great Britain Martinique France 760307396 ocn760307396 | Partager |
![]() | Crustal structure of the rifted volcanic margins and uplifted plateau of Western Yemen from receiver function analysis Auteur(s) : Ahmed, Abdulhakim Tiberi, Christel Leroy, Sylvie Stuart, Graham Keir, Derek Sholan, Jamal Khanbari, Khaled Al-Ganad, Ismael Auteurs secondaires : Seismological and Volcanological ; Observatory Center Institut des Sciences de la Terre de Paris (iSTeP) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Centre National de la Recherche Scientifique (CNRS) Manteau et Interfaces ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) School of Earth and Environment [Leeds] (SEE) ; University of Leeds National Ocenalography Centre Southampton ; University of Southampton [Southampton] Yemen Remote Sensing Center and Department of Earth and Environmental Science ; Université de Sana'a Yemen Geological Survey & Mineral Ressources Board ; GSMRB Éditeur(s) : HAL CCSD Oxford University Press (OUP) Résumé : International audience We analyse P-wave receiver functions across the western Gulf of Aden and southern Red Sea continental margins in Western Yemen to constrain crustal thickness, internal crustal structure and the bulk seismic velocity characteristics in order to address the role of magmatism, faulting and mechanical crustal thinning during continental breakup. We analyse teleseismic data from 21 stations forming the temporary Young Conjugate Margins Laboratory (YOCMAL) network together with GFZ and Yemeni permanent stations. Analysis of computed receiver functions shows that (1) the thickness of unextended crust on the Yemen plateau is ∼35km; (2) this thins to ∼22km in coastal areas and reaches less than 14km on the Red Sea coast, where presence of a high-velocity lower crust is evident. The average Vp/Vs ratio for the western Yemen Plateau is 1.79, increasing to ∼1.92 near the Red Sea coast and decreasing to 1.68 for those stations located on or near the granitic rocks. Thinning of the crust, and by inference extension, occurs over a ∼130-km-wide transition zone from the Red Sea and Gulf of Aden coasts to the edges of the Yemen plateau. Thinning of continental crust is particularly localized in a <30-km-wide zone near the coastline, spatially co-incident with addition of magmatic underplate to the lower crust, above which on the surface we observe the presence of seaward dipping reflectors (SDRs) and thickened Oligo-Miocene syn-rift basaltic flows. Our results strongly suggest the presence of high-velocity mafic intrusions in the lower crust, which are likely either synrift magmatic intrusion into continental lower crust or alternatively depleted upper mantle underplated to the base of the crust during the eruption of the SDRs. Our results also point towards a regional breakup history in which the onset of rifting was synchronous along the western Gulf of Aden and southern Red Sea volcanic margins followed by a second phase of extension along the Red Sea margin. ISSN: 0956-540X hal-00825194 https://hal.archives-ouvertes.fr/hal-00825194 https://hal.archives-ouvertes.fr/hal-00825194/document https://hal.archives-ouvertes.fr/hal-00825194/file/RF_Hakim2012_GJI.pdf DOI : 10.1093/gji/ggt072 | Partager |
![]() | Trinidad 1:62,500 Auteur(s) : United States -- Army Map Service Éditeur(s) : [s.n.] ( Washington ) Résumé : Complete in 8 sheets. "Polyconic projection." Military grid. "Contour interval 25, 50 feet changing to 100 feet at 100 foot contour." Six classes of roads or trails are shown. Provisional edition, 1940, by U.S. Army, Corps of Engineers, has title "Trinidad and Tobago .. Tactical map." Marginal map: Index to sheets. Trinidad and Tobago Trinidad Trinidad 002631426 06455957 AMZ8170 http://ufdc.ufl.edu/UF00065429/00002 | Partager |
![]() | Plan du port du Carenage ou petit cul de sac de l'Isle Se. Lucie Auteur(s) : Bellin, Jacques Nicolas, 1703-1772 Bellin, Jacques Nicolas, 1703-1772 Éditeur(s) : [s.n.] ( Paris ) Résumé : (Citation/Reference) Philips From: Le Petit Atlas Maritime Recueil De cartes Et Plans Des Quatre Parties Du Monde, "Tome I, no. 96," 1764. Relief shown pictorially and by hachures. Depths shown in fathoms. Includes graphic scale in toises. "Voyez la carte de l'isle de Se. Lucie, no. 95"--Lower margin. Oriented with North towards the left. Vertical watermark with text on right margin. (Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program. Saint Lucia Castries Castries (Saint Lucia) Castries (Saint Lucia) Castries (Saint Lucia) Saint Lucia Castries Castries (Saint Lucia) Castries (Saint Lucia) Castries (Saint Lucia) Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide. 002568025 AMT4324 05416030 http://ufdc.ufl.edu/UF00071892/00001 | Partager Voir aussi Harbors -- Maps -- Early works to 1800 ( lcsh ) Harbors -- No scale -- 1764 ( local ) Early maps -- No scale -- 1764 ( local ) Early works to 1800 -- No scale -- 1764 ( local ) No scale -- 1764 ( local ) Harbors -- No scale -- 1764 ( local ) Early maps -- No scale -- 1764 ( local ) Early works to 1800 -- No scale -- 1764 ( local ) |
![]() | British Guiana 1:125,000 Auteur(s) : United States -- Army Map Service Éditeur(s) : [s.n.] ( Washington ) Résumé : "Polyconic projection." Military grid. Relief shown by hachures with spot heights in feet. Five classes of roads or trails are shown. Marginal map: Index to adjoining sheets. Guyana Guyana Droits : This item is a work of the U.S. federal government and not protected by copyright pursuant to 17 U.S.C. §105. 06453929 002632176 http://ufdc.ufl.edu/UF00082555/00001 | Partager |