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Caught Between Spaces Socio-Environmental Vulnerability in Formal and Informal Peri-Urban Bogotá and Soacha, Colombia Valencia, Sandra
Caught Between Spaces Socio-Environmental Vulnerability in Formal and Informal Peri-Urban Bogotá and Soacha, Colombia Valencia, Sandra 2016 Document Version: Publisher's PDF, also known as Version of record Link to publication Citation for published version (APA): Valencia, S. (2016). Caught Between Spaces: Socio-Environmental Vulnerability in Formal and Informal Peri- Urban Bogotá and Soacha, Colombia. Lund University. Total number of authors: 1 General rights Unless other specific re-use rights are stated the following general rights apply: Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal Read more about Creative commons licenses: https://creativecommons.org/licenses/ Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. LUND UNIVERSITY PO Box 117 221 00 Lund +46 46-222 00 00 Caught Between Spaces: Socio-Environmental Vulnerability in Formal and Informal Peri-Urban Bogotá and Soacha, Colombia Sandra C. Valencia DOCTORAL DISSERTATION by due permission of the Faculty of Social Science, Lund University, Sweden. -
4.4 Drilling Exploration 1) Quaternary Drilling Exploration the Study
The Study on the Sustainable Groundwater Development for Bogotá Plain, Colombia 4.4 Drilling Exploration 1) Quaternary Drilling Exploration The Study Team carried out Quaternary exploratory drilling to know geological condition and to install groundwater level observation wells. (a) Location of Drilling Location of six drilling is shown in Table-4.5 and Figure-4.12. In site selection, items below were considered. • To be suitable to know hydrogeological characteristics of Quaternary • To be suitable to know representative groundwater level of Quaternary Table-4.5 Location of Quaternary Exploratory Drilling Coordinates Well No. E N No.1 Gibraltar (Soacha) 988,439 1,005,845 No.2 Tisquesusa (Facatativa) 976,639 1,022,020 No.3 Siberia (Tabio) 991,462 1,017,974 No.4 Sopo (Sopo) 1,011,020 1,037,638 No.5 Diana 1,013,170 1,038,429 No.6 Choconta 1,049,874 1,067,343 Well Structure Total drilling depth of six wells is 1,022m, and average depth of each well is 200m. The final diameter of casing of six wells is 8 inch. Groundwater level recorders were installed for every well. After installation of the recorders, groundwater level is being automatically observed. Six observation have screens for sand and gravel aquifer distributing in clayey formation, which can be called multiple screen structure. Therefore, these wells show mixed groundwater level of different aquifers of Quaternary. Result of Drilling Result of drilling is shown in Table-4.6. Pumping tests were carried out immediately after drilling completion. After pumping test of 48 hours pumping, recovery tests were carried out. -
Mammals and Stratigraphy : Geochronology of the Continental Mammal·Bearing Quaternary of South America
MAMMALS AND STRATIGRAPHY : GEOCHRONOLOGY OF THE CONTINENTAL MAMMAL·BEARING QUATERNARY OF SOUTH AMERICA by Larry G. MARSHALLI, Annallsa BERTA'; Robert HOFFSTETTER', Rosendo PASCUAL', Osvaldo A. REIG', Miguel BOMBIN', Alvaro MONES' CONTENTS p.go Abstract, Resume, Resumen ................................................... 2, 3 Introduction .................................................................. 4 Acknowledgments ............................................................. 6 South American Pleistocene Land Mammal Ages ....... .. 6 Time, rock, and faunal units ...................... .. 6 Faunas....................................................................... 9 Zoological character and history ................... .. 9 Pliocene-Pleistocene boundary ................................................ 12 Argentina .................................................................... 13 Pampean .................................................................. 13 Uquian (Uquiense and Puelchense) .......................................... 23 Ensenadan (Ensenadense or Pampeano Inferior) ............................... 28 Lujanian (LuJanense or Pampeano lacus/re) .................................. 29 Post Pampean (Holocene) ........... :....................................... 30 Bolivia ................ '...................................................... ~. 31 Brazil ........................................................................ 37 Chile ........................................................................ 44 Colombia -
Detrital U–Pb Provenance, Mineralogy, and Geochemistry of the Cretaceous Colombian Back–Arc Basin
Volume 2 Quaternary Chapter 8 Neogene https://doi.org/10.32685/pub.esp.36.2019.08 Detrital U–Pb Provenance, Mineralogy, and Published online 25 November 2020 Geochemistry of the Cretaceous Colombian Back–Arc Basin Paleogene Javier GUERRERO1* , Alejandra MEJÍA–MOLINA2 , and José OSORNO3 1 [email protected] Abstract The geology of the Cretaceous Colombian back–arc basin is reviewed con- Universidad Nacional de Colombia Cretaceous sidering detrital U–Pb provenance ages, mineralogy, and geochemistry of samples Sede Bogotá Departamento de Geociencias collected from outcrop sections and wells at several localities in the core of the Eastern Carrera 30 n.° 45–03 Bogotá, Colombia Cordillera, Middle Magdalena Valley, and Catatumbo areas. The data set supports previ- 2 [email protected] ous studies indicating a basin with main grabens in the present–day Eastern Cordillera Universidad Yachay Tech Hacienda Urcuquí s/n y Proyecto Yachay Jurassic between the Guaicáramo/Pajarito and Bituima/La Salina border faults, which operated Urcuquí, Ecuador as normal faults during the Cretaceous. Limestones are common on the western and 3 [email protected] Agencia Nacional de Hidrocarburos northern sides of the basin, whereas terrigenous strata predominate on the eastern Calle 26 n.° 59–65, segundo piso and southern sides. After the Berriasian, grabens were connected by marine flooding Bogotá, Colombia during the Valanginian, with two main source areas documented by distinct element * Corresponding author Triassic and mineral contents, one in the Central Cordillera magmatic arc and the other in the Guiana Shield. Some elements present in Lower Cretaceous shales, including scan- Supplementary Information: dium, vanadium, and beryllium, are not related to the sediment supply areas for the S: https://www2.sgc.gov.co/ LibroGeologiaColombia/tgc/ basin but instead are linked to Valanginian to Cenomanian hydrothermal activity and sgcpubesp36201908s.pdf Permian dikes of gabbro, diorite, and tonalite emplaced during the main phase of extension in the basin. -
Lithology and Geochemistry of the Guadalupe Group Base Around Tunja, This Work Is Distributed Under the Creative Commons Attribution 4.0 License
Boletín Geológico, 47, 35-65, 2020 https://doi.org/10.32685/0120-1425/ boletingeo.47.2020.494 Lithology and geochemistry of the Guadalupe Group base around Tunja, This work is distributed under the Creative Commons Attribution 4.0 License. Boyacá, Colombia Received: May 12, 2020 Revised: July 27, 2020 Accepted: September 17, 2020 Litología y geoquímica de la base del Grupo Guadalupe, en los Published online: December 28, 2020 alrededores de Tunja, Boyacá, Colombia German Martínez Aparicio1, Pedro Patarroyo2 and Roberto Terraza Melo1 1. Servicio Geológico Colombiano, (SGC), Bogotá, Colombia. 2. Universidad Nacional de Colombia, (UNAL), Bogotá, Colombia. Corresponding author: German Martínez Aparicio, [email protected] Abstract The base of the Guadalupe Group, in the Tunja area of Colombia, contains cherts, porcellanites, mudstones, and siltstones with subordinate quartz arenites. The lithostratigraphic description of two stratigraphic sections showed that the dominant facies have fine granular textures and siliceous compositions, which considerably differ from those of the prevailing sandy terrigenous facies described in the type locality in the Eastern Hills of Bogotá, in the Arenisca Dura Formation, the basal unit of the Guadalupe Group in this sector. The units that form the Guadalupe Group (base of the Guadalupe Group, Plaeners, and Arenisca Tierna) markedly differ from each other morphologically, which facilitates their mapping because the base and top units generate a steep morphology, and the intermediate units form surface depressions or valleys, similar to the morphology of the Guadalupe Group in its type locality in the Eastern Hills of Bogotá. The base of the Guadalupe Group consists of cherts and porcellanites toward the NW of the study area (Alto del Gavilán section), with mudstones, siltstones, quartz arenites, and to a lesser extent porcellanites and cherts prevailing toward the SE (Vereda Salitre section). -
Stra Tigraphy
EARTH SCIENCES RESEARCH JOURNAL Earth Sci. Res. J. Vol. 20, No. 3 ( September, 2016 ) : B1 - B9 STRATIGRAPHY Lithofacies cyclicity determination in the guaduas formation (Colombia) using Markov chains Mariño M. Jorge E.1, Amaya Erika2 1 Universidad Pedagógica y Tecnológica de Colombia- Escuela de Ingeniería Geológica; [email protected] 2 Universidad Pedagógica y Tecnológica de Colombia- Escuela de Ingeniería Geológica; [email protected] ABSTRACT Keywords: Litofacies, Lithofacies, reservoir Statistical embedded Markov Chain processes were used to analyze facies transitions and to determine environment, facies maps, Guaduas, the stacking pattern of the lithofacies of the Guaduas formation. Twelve Lithofacies were found lithofacies maps. and characterized based on lithology and sedimentary structures in four stratigraphic sections. The findings were compared with a previous assemblage of lithofacies, interpretations of sedimentary environments, and depositional systems. As a result, four depositional Systems were established. Through the statistical analyses of facies transitions it was found that tidal facies are prevalent in the Socota section, more specifically in the upper part. Whereas in the Sogamoso, Umbita and Peñas de Sutatausa sections, fluvial facies are prevalent in the upper part of the sections, and follow a regressive sequence with more continental deposits around the upper part of the sections. For each of these sections the Markov Chain transition matrices illustrate a strong interaction between tidal facies and fluvial facies, especially in the Peñas de Sutatausa matrix, where facies 6, made up of tidal deposits, appears several times. From the facies model and Markov Chain analyses, it is evident that the Guaduas formation is a cyclic sequence in which the Markov facies repetitions are consistent with the lithofacies analyses conducted in previous stratigraphic studies. -
Los Vertebrados Cenozoicos De Colombia: Yacimientos, Faunas, Problemas Planteados
LOS VERTEBRADOS CENOZOICOS DE COLOMBIA: YACIMIENTOS, FAUNAS, PROBLEMAS PLANTEADOS (Con dos mapas de Iocalidades) ROBERT HOFFSTETTER 1 ADVERTENCIA El presente informe fue presentado en el IV Congreso Latinoamericano de Zoologia (Caracas, 10-16 de noviembre de 1968). Desgraciadamente la puhlicacion del mismo, que corria a cargo de la Universidad Central de Venezuela, no pudo realizarse hasta la Iecha, Dado el tiempo transcurrido, hemos creido conveniente completar la version original con adiciones hihliografieas posteriores al citado Congreso, y con algunas modificaciones del texto, teniendo en cuenta los trabajos recientes. Estos corres- ponden esencialmente a Ia descripcion del pircterio Colombitherium tolimense (HOFFSTETTER 1970), al descubrimiento de un mono en el Oligoceno inferior suda- mericano (Branisella: HOFFSTETTER 1969a) y sohre todo a las opiniones modernas al respecto del origen de los varios grupos de Mamiferos implantados en America del Sur antes del Mioceno. INTRODUCCION Debido a su situacion geografica y a sus caracteres fisiografieos, Colombia representa un campo de estudio particularmente interesante en 10 que respecta a los Vertebrados Cenozoicos sudamericanos. 'Institut de Paleontologie, Museum National d'Histoire Naturelle, 8 rue de Buffon, Paris (59). - 37- En efecto, nuestro conocimiento de dichos vertehrados se basa esencialmente en la sucesidn de faunas recolectadas en Argentina, 0 sea en una zona marginal del continente sudamericano; Colomhia se encuentra al extremo opuesto, en el NW del continente, y ademas corresponde a la zona intertropical; de manera que la comparacion tiene que ser muy instructiva. Por su misma posicion geografica, Colomhia es c1 primer territorio interesado por los eventuales intercamhios faunicos con Norte America. ASl, representa un lugar privilegiado para rebuscar las feehas, naturaleza y modalidades de tales Intercamhios. -
University of Florida Thesis Or Dissertation Formatting
A MONOGRAPH OF THE GENUS LOCKHARTIA (ORCHIDACEAE: ONCIDIINAE) By MARIO ALBERTO BLANCO-COTO A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2011 1 © 2011 Mario Alberto Blanco-Coto 2 To my parents, who have always supported and encouraged me in every way. 3 ACKNOWLEDGMENTS Many individuals and institutions made the completion of this dissertation possible. First, I thank my committee chair, Norris H. Williams, for his continuing support, encouragement and guidance during all stages of this project, and for providing me with the opportunity to visit and do research in Ecuador. W. Mark Whitten, one of my committee members, also provided much advice and support, both in the lab and in the field. Both of them are wonderful sources of wisdom on all matters of orchid research. I also want to thank the other members of my committee, Walter S. Judd, Douglas E. Soltis, and Thomas J. Sheehan for their many comments, suggestions, and discussions provided. Drs. Judd and Soltis also provided many ideas and training through courses I took with them. I am deeply thankful to my fellow lab members Kurt Neubig, Lorena Endara, and Iwan Molgo, for the many fascinating discussions, helpful suggestions, logistical support, and for providing a wonderful office environment. Kurt was of tremendous help in the lab and with Latin translations; he even let me appropriate and abuse his scanner. Robert L. Dressler encouraged me to attend the University of Florida, provided interesting discussions and insight throughout the project, and was key in suggesting the genus Lockhartia as a dissertation subject. -
Estratigrafía Física, Palinológica, Sedimentológica Y Secuencial Del Cretácico Superior Y Paleoceno Del Piedemonte Llanero. Implicaciones En Exploración Petrolera
Geología Colombiana 20, 1996 Estratigrafía Física, Palinológica, Sedimentológica y Secuencial del Cretácico Superior y Paleoceno del Piedemonte Llanero. Implicaciones en Exploración Petrolera. JAVIER GUERRERO Departamento de Geociencias, Universidad Nacional de Colombia, Apartado Aéreo 14490, Santafé de Bogotá GUSTAVO SARMIENTO Subdirección de Geología, INGEOMINAS, Apartado Aéreo 4865, Santafé de Bogotá GUERRERO, J. & SARMIENTO, G. (1996) : Estratigrafía Física, Palinológica, Sedimentológica y Secuencial del Cretácico Superior y Paleoceno del Piedemonte Llanero. Implicaciones en Exploración Petrolera.- Geología Colombiana, n. 20, p. 3-66, 9 Figs., Bogotá. Palabras claves: Estratigraffa Secuencial, Palinología, Piedemonte Llanero, Cordillera Oriental, Exploración, Petróleo, Ambientes Sedimentarios, Chipaque, Guadalupe, Guaduas, Socha Inferior, Cretácico, Paleoceno. RESUMEN de San Luis de Gaceno y parte inferior de la Formación Guaduas) y ST2 (Formaciones Socha Inferior y Socha Se discute la estratigrafía de la Formación Chipaque, Superior). Grupo Guadalupe, Formación Guaduas y Formación Finalmente, presentamos una discusión de las Socha Inferior en proximidades de San Luis de Gaceno. implicaciones en exploración petrolera, producto de la El Grupo Guadalupe del Piedemonte Llanero se divide integración del marco estratigráfico, sedimentológico en tres nuevas unidades litoestratigráficas que de base y geocronológico aquí propuesto. a tope sedenominan Formación Aren itas de San Antonio (Guadalupe Inferior, Campaniano temprano), Formación ABSTRACT -
Structural Styles of the Eastern Cordillera of Colombia
Volume 3 Quaternary Chapter 6 Neogene https://doi.org/10.32685/pub.esp.37.2019.06 Structural Styles of the Eastern Cordillera Published online 29 May 2020 of Colombia Paleogene Andreas KAMMER1*, Alejandro PIRAQUIVE2 , Cristhian GÓMEZ3, Andrés MORA4, and Antonio VELÁSQUEZ5 1 [email protected] Universidad Nacional de Colombia Abstract The Eastern Cordillera of Colombia is bracketed between the moderately Departamento de Geociencias Carrera 30 n.° 45–03 Cretaceous west–dipping flank of the Central Cordillera on its western side and the little disturbed Bogotá, Colombia to gently bent Guiana Shield on its eastern side. Unlike other Andean foreland–orient- 2 [email protected] Servicio Geologico Colombiano ed belts, it is completely disconnected from the main Andean trunk system. Transverse Dirección de Asuntos Nucleares shortening of 4 mm/y records a considerable displacement transfer to the upper plate; Carrera 50 n.° 26–20 Bogotá, Colombia this is twice the long–term rate of 2.2 mm/y, which is the average for a shortening of Jurassic 3 [email protected] 65 km over a period of 30 Ma and suggests an increased recent shortening phase. We Universidad Nacional de Colombia Departamento de Geociencias differentiate three structural domains. The southern domain records significant short- Carrera 30 n.° 45–03 ening by penetrative strain at lower structural levels and folding at higher structural Bogotá, Colombia 4 [email protected] levels, which supports the idea of partitioning into pure–shear deformation within Ecopetrol S.A Triassic the pre–Cretaceous basement and into buckling in the Upper Cretaceous to Paleo- Vicepresidencia de Exploración Bogotá, Colombia gene units. -
Ophthalmoplax (Decapoda: Brachyura: Portunoidea) from the Late Campanian, Upper Cretaceous, of Colombia 93 Boletín De La Sociedad Geológica Mexicana
Ophthalmoplax (Decapoda: Brachyura: Portunoidea) from the late Campanian, Upper Cretaceous, of Colombia 93 Boletín de la Sociedad Geológica Mexicana Volumen 68, núm. 1, 2016, p. 93-103 D GEOL DA Ó E G I I C C O A S 1904 M 2004 . C EX . ICANA A C i e n A ñ o s Ophthalmoplax (Decapoda: Brachyura: Portunoidea) from the late Campanian, Upper Cretaceous, of Colombia Walter Guzmán1, Hermann Darío Bermúdez1, Arley de Jesús Gómez-Cruz2, Francisco J. Vega3,* 1 Grupo de Investigación Paleoexplorer, Calle 98bis 71D-20 Bogotá D.C. Colombia. 2 Universidad de Caldas, Facultad de Ciencias, Departamento de Ciencias Geológicas, Calle 65 No. 26-10, Manizales, Caldas, Colombia. 3 Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, Coyoacán, 04510 CDMX, México. * [email protected] Abstract A new species of the brachyuran Ophthalmoplax is documented based upon two specimens collected from shales of the Lodolitas de Aguacaliente Formation, Guadalupe Group, (Cordillera Oriental, Colombian Andes), which represents a regional transgressive event. The small crustaceans were found in the uppermost parasequences with retrogradational stacking pattern, near to the maximum flooding surface (MFS), at the end of the late Campanian Transgressive Systems Tract (TST). This is the oldest record forOphthalmo - plax in America. Morphological affinities with other species of the genus are discussed, including size reduction related with anoxia events and paleotemperature. Keywords: Crustacea, Portunoidea, Ophthalmoplax andina n. sp., Campanian, anoxia, Colombia. Resumen Se documenta la presencia de una nueva especie del braquiuro Ophthalmoplax con base en dos especimenes recolectados en lutitas de la Formación Lodolitas de Aguacaliente, parte media del Grupo Guadalupe, (Cordillera Oriental, Andes de Colombia), la cual registra un evento transgresivo regional. -
El Gran Libro De Los Páramos
El gran ElEl grangran librolibro libro de los dede loslos páramos páramospáramos El gran libro de los páramos El gran libro de los páramos © El gran libro de los páramos Agradecimientos Instituto de Investigación de Recursos Biológicos Alexander von Humboldt A Brigitte LG Baptiste, Eugenia Ponde de León, Carlos Tapia y María Paula Quiceno. A los docentes y estudiantes de instituciones educativas en los cuatro sitios piloto del Proyecto Páramo Andino, quienes con sus Comité Editorial Fotografía Ilustraciones aportes, contribuyeron a la revisión y ajuste de este material pedagógico validado y socializado durante el proceso de elaboración. Brigitte LG Baptiste Adolfo Correa Eduard Martínez Su valiosa participación permitió incorporar sugerencias en el diseño de “El Gran libro de los páramos”. María Susana Ruggiero Alberto Rojas Ilustraciones regiones Alejandra Osejo naturales de Colombia En el páramo de Rabanal, a las instituciones educativas Nuestra Señora del Carmen, sede Tibita el Carmen en Lenguazaque, Insti- tución Educativa La Libertad en Samacá, Institución Educativa Francisco de Paula Santander, sede Mata Negra en Ventaquemada. Dirección editorial, Textos y Andrea C. Buitrago Castro Cortesía cartilla Planeta Azul, Mediación del lenguaje Andrés Vélez Agenda del mar En el páramo el Duende, a las instituciones educativas Simón Bolívar (9 sedes), municipio de Calima el Darién; Antonio José de Adriana Vásquez Cerón Banco de Imágenes IAvH Sucre (6 sedes) en el corregimiento de Andinápolis, municipio de Trujillo; San Isidro (3 sedes), municipio de Trujillo. Andrea C. Buitrago Castro Bibiana Duarte Ilustración carátula Cornelio Botta En el páramo de Chiles, al Centro Educativo La Calera, vereda La Calera, Centro Educativo Cristo Rey, vereda Cristo rey, ubicadas Mónica Rubio Torgler Expertos invitados David Marín en el resguardo indígena de Chiles.