Éditeur(s) : Service de géodésie et de cartographie ( Port-au-Prince? )
Résumé : Some maps printed by Army Map Service, Corps of Engineers.
Relief shown by contours and spot heights.
English and French.
Standard maps series designation: Series E632.
Some maps lack series statement.
Includes index to adjacent sheets, glossary, explanatory chart. Some maps have index to boundaries.
(Statement of Responsibility) compilée par le Service de Géodésie et de Cartographie et les Forces Armées d'Haiti sous le supervision du Département des Travaux Publics et avec la collaboration de la U.S. Army Inter American Geodetic Survey.
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.
12307066
http://ufdc.ufl.edu/UF00078625/00001

Éditeur(s) : United States Army Map Service ( Washington, D. C. )
Résumé : "Planimetric detail revised by AMS in 1965 by photo-planimetric methods from aerial photography dated April 1965."
Relief shown by contours and spot heights.
English and Spanish.
Alternate title: Santo Domingo and vicinity, Dominican Republic.
" ... 1,000 meter universal transverse Mercator grid, Zone 19 ..."
Standard map series designation: Series E931.
Includes index and glossary.
(Statement of Responsibility) prepared by the Army Map Service (AM), Corps of Engineers, U.S. Army.
Dominican Republic -- Santo Domingo
Santo Domingo (Dominican Republic)

Droits : This item is a work of the U.S. federal government and not protected by copyright pursuant to 17 U.S.C. §105.
12343948
85690393
001635947
http://ufdc.ufl.edu/UF00098759/00001

Éditeur(s) : A.M.S. ( Washington D.C )
Résumé : Relief shown by contours and spot heights. Depths shown by bathymetric isolines and soundings.
Contour interval 20 meters.
Index to adjoining sheets, elevation guide, and boundaries diagram in bottom margins.
Includes glossary.
Mixed set: Eds. 1-4.
Later eds. prepared variously by the U.S. Army Topographic Command, and the Instituto Cartográfico Militar in collaboration with the Defense Mapping Agency.
Standard map series designation: E733.
(Statement of Responsibility) prepared by the Army Map Service; control and field classification by the Instituto Cartográfico Universitario.
Dominican Republic
Dominican Republic

Droits : This item is a work of the U.S. federal government and not protected by copyright pursuant to 17 U.S.C. §105.
001747638
26406002
AJG0473
http://ufdc.ufl.edu/UF00079867/00001

Résumé : Árbol de tamaño mediano de hasta 6 m, copa redonda; ramas con espinas delgadas, flexibles, ocasionalmente ausentes. Hojas ampliamente elípticas de 6 a 11 cm de largo con el ápice obtuso o agudo, base cuneada a redondeada. Flores solitarias o en racimos cortos, blancas, aromáticas. Fruto globoso u oval, con 10 a 13 segmentos, pulpa amarillenta, dulce.
Arbre de taille moyenne pouvant atteindre 6 m, cime arrondie; branches avec épines fines, souples, parfois absentes. Feuilles très elliptiques de 6 à 11 cm de longueur avec une pointe obtuse ou aiguë, base rhomboïdale ou arrondie. Fleurs solitaires ou en grappes courtes, blanches, aromatiques. Fruit rond ou ovale, avec 10 à 13 segments, pulpe jaunâtre, sucrée.
Tree 6 -12 m tall with spines. Leaves ovate or oval-elliptic 5-15 cm x 2-8 cm, glabrous dark green above, margins serrate, petiole narrowly winged and articulate; flowers axillary, born single or in small racemes, 2-3cm in diameter, white, aromatic; fruit subglobose or oval, 4-12 cm in diameter, peel thick, ripening orange colour but often remaining green in the tropics, pulp sweet and juicy, seeds nil to many obovoid.
Nativa de Asia, ampliamente cultivada en regiones tropicales y subtropicales.
Originaire d’;Asie, cultivée dans de vastes régions tropicales et subtropicales.
Native to Asia, widely cultivated in tropical and subtropical regions.

http://www.tramil.net/fototeca/plant136

Éditeur(s) : University of Florida Press University of Florida Press ( Gainesville, FL )
Résumé : (Bibliography) Includes bibliographies and index.
"Series one, volume VI."
"A publication of the School of Inter-American Studies which contains the papers delivered at the sixth conference on the Caribbean held at the University of Florida, December 1, 2 and 3, 1955."
"Sixth volume in our Caribbean Conference series ..."--Foreword, p. vii.
(Statement of Responsibility) edited by A. Curtis Wilgus.
Caribe, ilhas ( e.u.)
Caribbean Area

01892149

Résumé : Sufrútice erecto, con ramas ascendentes, tallos puberulentos con tricomas estrellados y diminutos. Hojas alternas, variando de rómbico-oblongas a ovado cuneadas u oblanceoladas, obtusas a redondeadas o subagudas en el ápice, cuneadas o redondeadas en la base. Pedicelos solitarios en las axilas y más o menos dispersos a lo largo del tallo; corola amarilla o amarilla-anaranjada. Frutos glabros, carpelos múticos o con 1 o 2 espinas; semillas de color café, glabras, excepto en el hilo.
Plante suffrutescente dressée, à branches ascendantes, tiges pubérulentes avec pubescencesen étoiles de très petite dimension. Feuilles alternes, rhomboïdale-oblongues à ovée- cunéiformes ou oblancéolées, obtuses à arrondies ou subaiguës à la pointe, cunéiformes ou arrondies à la base. Pédicelles axillaires solitaires et plus ou moins dispersés le long de la tige; corolle jaune ou jaune-orangée. Fruits glabres, carpelles mutiques ou avec 1 ou 2 épines; graines de couleur café, glabres, sauf sur le hile.
Erect bushy herb, 30-90 cm high with wiry branches. Stems stellate-puberulent, the hairs less than 1 mm long.  Leaves alternate, simple, 2-8 x 4 cm, lanceolate to rhombic-oblong, acute at the apex, narrowed or cordate at the base, margins serrate-dentate, blades discolorous, puberulent above and below; flowers pedicillate, solitary in axils, disperse along the stem, corolla, 7-10 mm yellow-orange, becoming pinkish; fruit with 9-14 glabrous carpels, 3-4 mm long including spine and 4-5 mm in diameter.
Regiones tropicales y subtropicales.
Régions tropicales et subtropicales.
Tropical and subtropical regions.

http://www.tramil.net/fototeca/plant322

Éditeur(s) : The Center ( Washington D.C )
Résumé : Relief shown by contours, and spot heights.
Depths shown by bathymetric isolines and soundings.
Mixed set: maps prepared by the Instituto Geográfico Nacional "Tommy Guardia," the Dirección de Cartográfico de Panamá, the Inter-American Geodetic Survey or the Army Map Service.
Some maps only in Spanish.
Standard map series designation: Series E762.
Includes index to adjoining sheets, boundaries and elevation guides.
(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 and published by the Defense Mapping Agency, Hydrographic/Topographic Center.
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.
21132987
http://ufdc.ufl.edu/UF00077003/00001

Éditeur(s) : National Geospatial Intelligence Agency ( Bethesda MD, Bethesda MD )
Résumé : (Language) Legend and glossary in English and Spanish.
"Map information as of 1968."
Relief shown by contours and spot heights ; soundings in feet at mean low water.
"Printed by U.S. Army Topographic Command (SX) 6-70".
"Reprint by NGA 1-04".
Includes indexes to numbered features and streets, and boundary diagram.
Standard map series designation: Series E931=Serie E931.
(Statement of Responsibility) prepared under the direction of the Department of Defense and published by the U.S. Army Topographic Command.
Dominican Republic -- barahona -- Santa Cruz de Barahona
Barahona (Dominican Republic : Province)
Santa Cruz de Barahona (Dominican Republic)

70627204
003590172
http://ufdc.ufl.edu/UF00096315/00001

Éditeur(s) : Elsevier
Résumé : We report on a multidisciplinary study of cold seeps explored in the Central Nile deep-sea fan of the Egyptian margin. Our approach combines in situ seafloor observation, geophysics, sedimentological data, measurement of bottom-water methane anomalies, pore-water and sediment geochemistry, and Th-230/U dating of authigenic carbonates. Two areas were investigated, which correspond to different sedimentary provinces. The lower slope, at similar to 2100 m water depth, indicates deformation of sediments by gravitational processes, exhibiting slope-parallel elongated ridges and seafloor depressions. In contrast, the middle slope, at similar to 1650 m water depth, exhibits a series of debris-flow deposits not remobilized by post-depositional gravity processes. Significant differences exist between fluid-escape structures from the two studied areas. At the lower slope, methane anomalies were detected in bottom-waters above the depressions, whereas the adjacent ridges show a frequent coverage of fractured carbonate pavements associated with chemosynthetic vent communities. Carbonate U/Th age dates (similar to 8 kyr BP), pore-water sulphate and solid phase sediment data suggest that seepage activity at those carbonate ridges has decreased over the recent past. In contrast, large (similar to 1 km(2)) carbonate-paved areas were discovered in the middle slope, with U/Th isotope evidence for ongoing carbonate precipitation during the Late Holocene (since similar to 5 kyr BP at least). Our results suggest that fluid venting is closely related to sediment deformation in the Central Nile margin. It is proposed that slope instability leads to focused fluid flow in the lower slope and exposure of 'fossil' carbonate ridges, whereas pervasive diffuse flow prevails at the unfailed middle slope.
Marine Geology (0025-3227) (Elsevier), 2009-06 , Vol. 261 , N. 1-4 , P. 92-104

Droits : 2009 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/2009/publication-6586.pdf
DOI:10.1016/j.margeo.2008.10.008
http://archimer.ifremer.fr/doc/00000/6586/

Éditeur(s) : HAL CCSD Elsevier
Résumé : Several nuclides of the ;238;U (;234;U, ;230;Th, ;226;Ra, ;210;Pb) and ;235;U (;231;Pa, ;227;Ac) decay series have been measured through gamma spectrometry in the U-bearing episyenites of the Bernardan mine (northwest Massif Central, France), in order to study recent mobilizations in the U-deposit and their time-scales. (;230;Th/;238;U) and (;231;Pa/;235;U) ratios show that U has been little affected during the last 350 ky, especially in the U-rich samples. In contrast, ;226;Ra was subjected to a general redistribution, with a clear tendency for Ra to be lost from the U-rich samples and added to U-poor samples. The highest Ra excesses are present in low-U samples, and are related to adsorption onto iron hydroxides. Ra appears to have been redistributed within the mineralised episyenitic bodies, which seem to remain in ;226;Ra–;238;U radioactive equilibrium, a result consistent with the earlier study of Leroy [1984. Episyénitisation dans le gisement d'uranium du Bernardan (Marche): Comparaison avec des gisements similaires du Nord-Ouest du Massif Central français. Miner. Depos. 19, 26–35]. As shown by the ;226;Ra and ;210;Pb data, the Ra redistribution was very active between 8 and 0.1 ky, and this might be a consequence of the hydrological changes in groundwater circulation accompanying the Holocene climate warming.
ISSN: 0009-2541

hal-00407600
https://hal.archives-ouvertes.fr/hal-00407600
DOI : 10.1016/j.chemgeo.2007.06.020

Éditeur(s) : University of Florida Press University of Florida Press ( Gainesville, FL )
Résumé : (Bibliography) Includes bibliographies and index.
"Series one, volume III."
"A publication of the School of Inter-American Studies which contains the papers delivered at the third annual conference on the Caribbean held at the University of Florida, December 18, 19, and 20, 1952."
(Statement of Responsibility) edited by A. Curtis Wilgus.
Caribe, ilhas ( e.u.)
Caribe, ilhas ( e.u.)
Caribe, ilhas ( e.u.)
Caribbean Area
Caribe, Ilhas ( E.U.) (TendÊncias)

02473722

Éditeur(s) : U.S. Dept. of State U.S. Dept. of State ( Washington, DC )
Résumé : (System Details) Master and use copy. Digital master created according to Benchmark for Faithful Digital Reproductions of Monographs and Serials, Version 1. Digital Library Federation, December 2002.
Title from PDF cover (LLMC Digital, viewed on Sept. 27, 2010)
"Excerpts of testimony, speeches, and remarks by U.S. Secretary of State Madeleine K. Albright on Colombia, economic issues, Panama, Mexico, Cuba, Caribbean Ministerial, and Haiti."
"March 2000"--P. 2 of cover.

606510569

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The Jacupiranga Complex is one of several Meso-Cenozoic alkaline intrusive complexes along the margins of the intracratonic Paraná Basin in southern Brazil. The complex encompasses a wide range of rock-types, including dunites, wehrlites, clinopyroxenites, melteigites-ijolites, feldspar-bearing rocks (diorites, syenites, and monzonites), lamprophyres and apatite-rich carbonatites. While carbonatites have been extensively investigated over the last decades, little attention has been paid to the silicate rocks. This study presents new geochonological and geochemical data on the Jacupiranga Complex, with particular emphasis on the silicate lithotypes. 40Ar/39Ar ages for different lithotypes range from 133.7 ± 0.5 Ma to 131.4 ± 0.5 Ma, while monzonite zircon analyzed by SHRIMP yields a U-Pb concordia age of 134.9 ± 1.3 Ma. These ages indicate a narrow time frame for the Jacupiranga Complex emplacement, contemporaneous with the Paraná Magmatic Province. Most of the Jacupiranga rocks are SiO2-undersaturated, except for a quartz-normative monzonite. Based on geochemical compositions, the Jacupiranga silicate lithotypes may be separated into two magma-evolution trends: (1) a strongly silica-undersaturated series, comprising part of the clinopyroxenites and the ijolitic rocks, probably related to nephelinite melts and (2) a mildly silica-undersaturated series, related to basanite parental magmas and comprising the feldspar-bearing rocks, phonolites, lamprophyres, and part of the clinopyroxenites. Dunites and wehrlites are characterized by olivine compositionally restricted to the Fo83-84 interval and concentrations of CaO (0.13–0.54 wt%) and NiO (0.19–0.33 wt%) consistent with derivation by fractional crystallization, although it is not clear whether these rocks belong to the nephelinite or basanite series. Lamprophyre dikes within the complex are considered as good representatives of the basanite parental magma. Compositions of calculated melts in equilibrium with diopside cores from clinopyroxenites are quite similar to those of the lamprophyres, suggesting that at least a part of the clinopyroxenites is related to the basanite series. Some feldspar-bearing rocks (i.e. meladiorite and monzonite) show petrographic features and geochemical and isotope compositions indicative of crustal assimilation, although this may be relegated to a local process. Relatively high CaO/Al2O3 and La/Zr and low Ti/Eu ratios from the lamprophyres and calculated melts in equilibrium with cumulus clinopyroxene point to a lithospheric mantle metasomatized by CO2-rich fluids, suggesting vein-plus-wall-rock melting mechanisms. The chemical differences among those liquids are thought to reflect both variable contributions of melting resulting from veins and variable clinopyroxene/garnet proportions of the source.
ISSN: 0895-9811

hal-01583547
https://hal.archives-ouvertes.fr/hal-01583547
DOI : 10.1016/j.jsames.2017.05.009

Éditeur(s) : Direction Générale des Travaux Publics Direction Générale des Travaux Publics ( Haiti )
Résumé : This collection of over 5,000 black and white photographs held by the National Archives of Haiti dates from 1918 to 1945. It contains images of public buildings before and after restoration, public works, monuments, and the visits of U.S. Presidents and other officials.
Haiti

Droits : All rights reserved by the National Archives of Haiti.
11518

Éditeur(s) : G.P.O. G.P.O. ( Washington, D.C., U.S.A )
Résumé : (System Details) Digital master created according to Benchmark for Faithful Digital Reproductions of Monographs and Serials, Version 1. Digital Library Federation, December 2002.
(Language) English and French.
Title from PDF t.p. (LLMC Digital, viewed on Sept. 8, 2011).
Found also in U.S. 52d Cong., 1st sess. Senate. Ex. doc. 8, pt. X: Tariffs of the American republics, v. 2.
Haiti
Haïti
Haiti

Droits : No restrictions on access copy.
657161050
ocn657161050

Éditeur(s) : United States Army Topographic Command ( Washington, D. C. )
Résumé : "Map information as of 1968."
Relief shown by contours and spot heights.
Alternate title: San Francisco de Macorís.
"Grid 1,000 meter, UTM: Zone 19 (black numbered lines), 1,000 meter, Lambert for Dominican Republic (blue numbered ticks)."
Standard map series designation: Series E931 -- Serie E931.
Includes indexes, indexed boundary diagram, and glossary.
(Statement of Responsibility) prepared under the direction of the Department of Defense and published by the U.S. Army Topographic Command.
Dominican Republic -- San Francisco de Macoris
San Francisco de Macorís (Dominican Republic)

Droits : This item is a work of the U.S. federal government and not protected by copyright pursuant to 17 U.S.C. §105.
31209763
001949863
http://ufdc.ufl.edu/UF00098756/00001

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : International audience
The Ama Drime range located at the transition between the high Himalayan range and south Tibet is a N-S active horst that offsets the South Tibetan Detachment System (STDS). Within the horst, a paragneissic unit, possibly attributed to the upper Himalayan crystalline series, overly the lower Himalayan crystalline series Ama Drime orthogneissic unit containing large metabasite layers and pods that have experienced pressure >= 1.4 GPa. Combining structural analysis with new and published pressure-temperature (P-T) estimates as well as U-Th/Pb, Ar-39/Ar-40 and (U-Th)/He ages, the P-T-deformation-time (P-T-D-t) paths of the main units within and on both sides of the horst are reconstructed. They imply that N-S normal faults initiated prior to 11 Ma and have accounted for a total exhumation <= 0.6 GPa (22 km) that probably occurred in two phases: the first one until similar to 9 Ma and the second one since 6 to 4 Ma at a rate of similar to 1 mm/yr. In the Ama Drime unit, 1 to 1.3 GPa (37 to 48 km) of exhumation occurred after partial melting since similar to 30 Ma until similar to 13 Ma, above the Main Central Trust (MCT) and below the STDS when these two fault systems were active together. The switch from E-W (STDS) to N-S (Ama Drime horst) normal faulting between 13 and 12 Ma occurs at the time of propagation of thrusting from the MCT to the Main Boundary Thrust. These data are in favor of a wedge extrusion or thrust system rather than a crustal flow model for the building of the Himalaya. We propose that the kinematics of south Tibet Cenozoic extension phases is fundamentally driven by the direction and rate of India underthrusting.
ISSN: 0278-7407

hal-00486405
https://hal.archives-ouvertes.fr/hal-00486405
DOI : 10.1029/2009TC002551

Éditeur(s) : University of Florida Press Walter B. Fraser Publication Fund University of Florida Press ( Gainesville, FL ) Walter B. Fraser Publication Fund
Résumé : (Bibliography) Bibliographical footnotes and index.
"Series one, volume IV."
"A publication of the School of Inter-American Studies which contains the papers delivered at the fourth annual conference on the Caribbean held at the University of Florida, December 3, 4, and 5, 1953."
(Statement of Responsibility) edited by A. Curtis Wilgus.
Caribe, ilhas ( e.u.)
Caribbean Area

02473766

Éditeur(s) : HAL CCSD Springer Verlag (Germany) Springer Verlag
Résumé : International audience
We report here U-series and trace element data for an olivine-melilitite lava flow, erupted in 1957 in the Virunga volcanic field and known as the Mugogo eruption. Petrological and geochemical data show that the Mugogo magma represents a primary mantle melt, derived from a low degree of melting of a metasomatised mantle source. It is highly enriched in very incompatible trace elements (e.g. more than 300-fold compared to primitive mantle for Th), with a distinctly lower enrichment in Rb, Ba and Sr. The high Th/U and low (230Th/232Th) ratios (4.4 and 0.750, respectively, with a (230Th/238U) ratio of 1.09) are close to the values found for the Nyamuragira basanites. But the most striking feature is the very low (226Ra/230Th) ratio of 0.48, the lowest ever measured in a mafic volcanic rock. The most probable origin of this Ra deficit is the presence of phlogopite (having a high Ra partition coefficient) in the lithospheric mantle, either as a residual phase during low-degree isobaric melting (in batch-melting or a diffusion-controlled melting models), or in a phlogopite-bearing upper mantle through which the melt migrates and equilibrates (in an equilibrium porous flow model commonly used to describe adiabatic melting). The disequilibrium pattern (230Th) > (238U) > (210Pb) ≫ (226Ra), reversed compared to the pattern observed in the Oldoinyo Lengai natrocarbonatite, suggests that a carbonatite melt might have been involved to explain the Ra deficit. We thus discuss the possibility of an early separation of a Ra-enriched carbonate melt either from the olivine-melilitite melt or from a carbonated mantle source, followed by the production of a low-degree melt of olivine-melilitite composition, but the lack of available experimental, petrological and geochemical evidences makes this process somewhat speculative at present. Further studies of recent (<5 ky) olivine-melilitites are needed to check whether the large Ra deficit is a general characteristic of this type of magma that can be used to constrain models of its formation.
ISSN: 0010-7999

hal-01174173
https://hal.archives-ouvertes.fr/hal-01174173
DOI : 10.1007/s00410-015-1124-9

Éditeur(s) : United States Army Topographic Command United States Army Topographic Command ( Washington, D. C. )
Résumé : "Map information as of 1968."
Relief shown by contours and spot heights.
Alternate title: Mao.
Standard map series designation: Series E931 = Serie E931.
"Grid 1,000 meter, UTM: Zone 19 (black numbered lines), 1,000 meter, Lambert for Dominican Republic (blue numbered ticks)."
Includes indexes, indexed boundary diagram, and glossary.
(Statement of Responsibility) prepared under the direction of the Department of Defense and published by the U.S. Army Topographic Command.
Dominican Republic -- Mao
Mao (Dominican Republic)

12611884
85690395
001933086