Relevant bibliographies by topics / Comité Regional de la Sierra

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Academic literature on the topic 'Comité Regional de la Sierra'

Author: Grafiati
Published: 4 June 2021
Last updated: 4 February 2022

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Journal articles on the topic "Comité Regional de la Sierra"

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Gómez Flores, Carlos Jesús. "Un documento transdisciplinario para llamar a la acción." HORIZONTE SANITARIO 11, no. 1 (August 18, 2014): 32. http://dx.doi.org/10.19136/hs.a11n1.109.

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Biodiversidad: bases de información para la Sierra de Tabasco, libro cuyo principal autor es el Doctor Eduardo López Hernández, a la par de otros colegas y de ex discípulos, se compone de nueve capítulos que se arropan con amplias notas científicas. El texto fue editado en el marco de la Colección José N. Rovirosa. En el esfuerzo se vincula El Colegio de Investigadores de Tabasco A.C. de cuyo Comité Editorial formo parte.
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Gómez Flores, Carlos Jesús. "Un documento transdisciplinario para llamar a la acción." HORIZONTE SANITARIO 11, no. 1 (August 18, 2014): 32. http://dx.doi.org/10.19136/hs.v11i1.109.

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Biodiversidad: bases de información para la Sierra de Tabasco, libro cuyo principal autor es el Doctor Eduardo López Hernández, a la par de otros colegas y de ex discípulos, se compone de nueve capítulos que se arropan con amplias notas científicas. El texto fue editado en el marco de la Colección José N. Rovirosa. En el esfuerzo se vincula El Colegio de Investigadores de Tabasco A.C. de cuyo Comité Editorial formo parte.
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Unemi, Editor. "COMITÉ EVALUADOR." CIENCIA UNEMI 10, no. 23 (October 4, 2017): 5–6. http://dx.doi.org/10.29076/issn.2528-7737vol10iss23.2017pp5-6p.

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Comité EditorialDr. Richard Iván RamírezAnormalizaUniversidad Estatal de Milagro, UNEMIrramireza@unemi.edu.ecMilagro, Ecuador Dr. Vicenc FernándezUniversidad Politécnica de Cataluñavicenc.fernandez@upc.eduBarcelona, España Dr. Ahmed YanguiField Crop Regional Research Centerahmed.yangui@yahoo.frBeja, Tunisia Dra. Mayra D’Armas RegnaultUniversidad Politécnica Antonio José deSucre, UNEXPOmdarmas@unexpo.edu.vePuerto Ordaz, Venezuela Dr. Thiago Duarte PimentelUniversidade Federal de Juiz de Forathiagodpimentel@gmail.comMinas Gerais, Brazil Dr. Rodrigo Romo MuñozUniversidad del Bio-Biorromo@ubiobio.clConcepción, Chile Dr. Ángel Barrasa NotarioUniversidad de Zaragozaabarrasa@unizar.esZaragoza, España Dr. David Benavides CuevasUniversidad de Sevillabenavides@us.esSevilla, España Máster Ángela Laguna CaicedoUniversidad Tecnológica de Panamáangela.laguna@utp.ac.paPanamá, Panamá Dr. Simón Pérez MartínezUniversidad Estatal de Milagro, UNEMIsimonpm2006@gmail.comMilagro, Ecuador Dr. Amr R. A. RadwanUniversidad de El Cairoamrradwan2010@yahoo.com El Cairo,Egipto Dr. Fernando Guilherme TenórioEscuela Brasileira de Administración Públicay de Empresas de la Fundación GetulioVargasfernando.tenorio@fgv.brRío de Janeiro, Brazil Dra. Carmen HernándezDomínguezUniversidad Estatal de Milagro, UNEMIcarmen.hernandez.dominguez@gmail.comMilagro, Ecuador Dr. Iván EsparragozaUniversidad de Pensilvaniaiee1@psu.eduFiladelfia, USA Máster Alexandra AnormalizaDirector Affinity Group Field Support Centerat NYC Department of Educationaanorma@schools.nyc.gov New York, USA Dr. Mario Pérez-MontoroGutiérrezUniversidad de Barcelonaperez-montoro@ub.eduBarcelona, España Dr. Humberto R. Álvarez A.Universidad Tecnológica de Panamáhumberto.alvarez@utp.ac.paPanamá, Panamá Dra. Beatriz CarvajalUniversidad Centro Occidental “LisandroAlvarado”, UCLAbecar777@yahoo.esBarquisimeto, Venezuela Dr. Islam HassounehPalestine Polytechnic University (PPU).islamh@ppu.eduHebrón, Palestina Comité de Evaluadores ExternosMáster Pepita Alarcón ParraMáster en Planificación, Evaluación yAcreditación en la Educación SuperiorDocente investigadoraEscuela Superior Politécnica deChimborazopepita.alarcon@espoch.edu.ecRiobamba, Ecuador Dra. Gina Álvarez ReyesMáster en Administración AmbientalJefe Laboratorio Análisis del AguaEscuela Superior Politécnica deChimborazogalvarez101@yahoo.esRiobamba, Ecuador Máster Guido Asencio GallardoMBA © Latinoamericano,Magíster © en Ciencias SocialesAcadémico del Departamento deCiencias Administrativas y EconómicasUniversidad de Los Lagosguido.asencio@gmail.comOsorno, Chile Máster Fernando Molina GranjaMáster en Informática AplicadaMáster en Educación a DistanciaDocente investigador Facultad deIngenieríaUniversidad Nacional de Chimborazo,UNACHfemolinag@yahoo.esRiobamba, Ecuador Máster Carlos Montalvo PatiñoMáster en Educación SuperiorAcademic Consultantcarlosmontalvo2000@yahoo.comGuayaquil, Ecuador Máster Javier Ortiz RojasMáster en Sistemas de InformaciónGerencialDocente investigadorUniversidad Politécnica Salesianajortiz@ups.edu.ecQuito, Ecuador Máster Washington Padilla AriasMáster en Gerencia de SistemasDocente investigadorUniversidad Politécnica Salesianawpadillaa@ups.edu.ecQuito, Ecuador Dr. Oscar Parada GutiérrezDoctor en Ciencias EconómicasDocente investigadorEscuela Superior Politécnica deChimborazoospg2012@gmail.comRiobamba, Ecuador Máster Ninfa Pilozo SalavarríaMáster en Desarrollo EducativoEx revisora de estiloExperta en Lenguaje y Comunicaciónnpilozos@hotmail.comMilagro, Ecuador Máster Diego Ramiro BarbaBayasMáster en Gerencia de Proyectos deEcoturismoEscuela Superior Politécnica delChimborazod_barba@espoch.edu.ecRiobamba, Ecuador Máster Segundo Camino MogroMáster en EconomíaInvestigador EconómicoEspecializado en economía industrial,productividad y competenciasegundo.camino@gmail.comGuayaquil, Ecuador Máster Tania Crespo VacaMáster en Docencia y Gerencia enEducación SuperiorEnglish teachertcrespo2@hotmail.comGuayaquil, Ecuador Dr. Amilkar Puris CáceresDoctor en Ciencias TécnicasDocente investigadorUniversidad Técnica Estatal de Quevedoapuris@uteq.edu.ecQuevedo, Ecuador Dra. Gisela Quintero ChacónDoctora en Ciencias PedagógicasDocente InvestigadoraUniversidad Nacional de EducaciónGisela.quintero@unae.edu.ecAzoguez, Ecuador Máster Carmita Ramírez CalixtoMagister en Educación y Gerencia SuperiorDocente investigadoraUniversidad de Guayaquilcarmita.ramirezc@ug.edu.ecGuayaquil, Ecuador Máster Luis Fernando SolórzanoÁlavaMáster Salud PúblicaMáster en MicrobiologíaDocente investigadorUniversidad de Guayaquilluis.solorzanoa@ug.edu.ecGuayaquil, Ecuador Máster Leyla Nury VelardePinargotteMáster en Comunicación y DesarrolloDocente investigadoraUniversidad San Francisco de Quitoleylanury@hotmail.comQuito, Ecuador Máster Fernando Veloz NavarreteMáster en Dirección de EmpresasDocente investigadorEscuela Superior Politécnica deChimborazoferveloz@yahoo.esRiobamba, Ecuador Máster Manuel GonzálezGonzálezMáster en VirologíaDirector TécnicoFomento y Transferencia del ConocimientoInstituto Nacional de Investigaciónen Salud Pública, INSPImgonzales@inspi.gob.ecGuayaquil, Ecuador Máster Betzabé Maldonado MeraMáster en Gestión de OrganizacionesUniversidad de las Fuerzas Armadasbrmaldonado@espe.edu.ecQuito, Ecuador Dr. Marek Michalski MichalskaDoctor en EconomíaUniversidad San Francisco de Quitommichalski@usfq.edu.ecQuito, Ecuador Dr. Víctor H. Villao ReyesEspecialista en CirugíaDirector Hospital San CarlosDocente Facultad de Medicina UEESvvillao@isc.com.ecGuayaquil, Ecuador Máster Jimena Viteri OjedaMáster en Informática AplicadaDocente-InvestigadoraEscuela Superior Politécnica deChimborazojcviteri@espoch.edu.ecRiobamba, Ecuador Máster Scandra Mora SaadoMáster en Ingeniería IndustrialUniversidad Nacional ExperimentalPolitécnicasmora@unexpo.edu.vePuerto Ordaz, Venezuela Dr. Edgar Alexander PiñeroDoctor en Administración y Dirección deEmpresasUniversidad Experimental de Guayanaalexanderpinero12@gmail.comPuerto Ordaz, Venezuela
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García Flórez, Manuel. "Editorial." RFS Revista Facultad de Salud 2, no. 1 (January 11, 2010): 7–8. http://dx.doi.org/10.25054/rfs.v2i1.90.

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La tercera entrega de la Revista Facultad de Salud se destaca por la conveniencia y pluralidad de temas abordados. Se exponen adelantos de investigación en ciencias básicas, en ciencias clínicas, se actualizan temas y se abre espacio para la presentación de casos clínicos, con todo esto se crea un escenario para el acercamiento de diferentes áreas en búsqueda de la integración del conocimiento. En este número reconocemos la valiosa participación de los miembros salientes del comité científico y damos la bienvenida a los nuevos integrantes: doctores, Paola Andrea Tejada y Dagoberto Santofimio Sierra del Hospital Hernando Moncaleano Perdomo de la ciudad de Neiva, doctor Gustavo Adolfo Vallejo del Departamento de Biología de la Universidad del Tolima y la doctora Heloisa Helena Della Colleta, adscrita al Instituto de Ciencias Biológicas de la Universidad Federal de Minas Gerais de Brasil. Su inclusión en el comité se fundamenta en su gran experiencia académica y logros científicos, sin duda ellos contribuirán con el fortalecimiento de nuestra joven publicación.
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Burga, Manuel. "La Sierra Central Peruana (1821-1870) una Economía Regional Andina." Allpanchis 15, no. 22 (October 2, 2020): 103–24. http://dx.doi.org/10.36901/allpanchis.v15i22.912.

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La Intendencia de Tarma, a fines del siglo XVIII, correspondía casi íntegramente a lo que se considera la región central. Luego de la Independencia, en 1825, esta intendencia toma el nombre de departamento de Junín y se le asignan las provincias de Tarma, Jauja, Huancayo y Cerro de Pasco. Esta misma demarcación política permanecerá inalterable en este departamento durante el periodo que nos interesa.
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Galan, Juanjo, and Daniela Perrotti. "Incorporating Metabolic Thinking into Regional Planning: The Case of the Sierra Calderona Strategic Plan." Urban Planning 4, no. 1 (February 21, 2019): 152–71. http://dx.doi.org/10.17645/up.v4i1.1549.

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The metabolic study of the southeastern part of the Calderona Mountain Range (Sierra Calderona) was developed over an area of 200 square kilometers. Due to its location on the outskirt of the Metropolitan Area of Valencia (Spain), the Calderona Mountain Range presents most of the metabolic challenges and potentials that characterize peri-urban areas. The main goal of the study was to increase the sustainability levels of the region by optimizing the flows of materials and energy, as well as flows related to the transport of people within and in/outside the region. The following article includes a methodological introduction to regional and urban metabolic studies. Secondly, it presents the specific application of those principles in the Sierra Calderona case and the qualitative and quantitative results of the assessed regional flows. Moreover, the use of Metabolic Functional Areas (FMAs) is proposed to better integrate metabolic studies with land-use and spatial planning. In its second section, the article also presents the potential for shifting toward an optimized metabolism of the studied area, as well as a set of strategies and actions for their achievement. Finally, in the conclusions, we present a critical reflection on the methods, data, exportability and scalability of the results produced in the Sierra Calderona Case. Due to its regional character, the metabolic performance of the Sierra Calderona is connected to a wide range of land uses, productive functions and stakeholders. That is the reason why the formulated strategies and actions are deeply interlinked with different sectors and why they were supported by the results of an open participatory process. However, and in spite of its regional scope, the urban systems of the Sierra Calderona proved to be an essential lever for improving the regional and local sustainability, due to their varied morphological structures, distinctive ways of functioning, and different types of interaction with the surroundings.
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Yamamoto, Jaime. "Actividad microsísmica en el área de Canatlán, Durango y su relación con la geología regional." Geofísica Internacional 32, no. 3 (July 1, 1993): 501–10. http://dx.doi.org/10.22201/igeof.00167169p.1993.32.3.525.

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Los hipocentros de 22 microsismos (-0.09≤Mc≤1.1) que ocurrieron en el área de Canatlán, Durango (24°38'N, 105°W) del 30 de abril al 2 de mayo del 1972 fueron determinados. Los eventos se localizan entre la Laguna de Santiaguillo y el flanco oriental de la Sierra de la Magdalena perteneciente a la Sierra Madre Occidental a una profundidad de 1.0 a 5.5 km. La distribución espacial de los epicentros presenta dos tendencias lineales de sismicidad orientadas N21°W y N71°E de longitud 7.2 y 5.4 km respectivamente, que sugiere la existencia de un sistema de fallas conjugadas sísmicamente activas. La tendencia N21°W coincide con la dirección de las antiguas fallas normales longitudinales asociadas con la Sierra Madre Occidental. Aunque no se tiene registro gráfico de los eventos principales ocurridos el 18 de marzo de 1972 al inicio de la secuencia, el radio de perceptibilidad indica que probablemente tuvieron una magnitud mb de 3.1.
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Lopez, Leslie, and Victoria Chenaut. "Procesos rurales e historia regional (sierra y costa totonacas de Veracruz)." Journal of the Royal Anthropological Institute 5, no. 2 (June 1999): 318. http://dx.doi.org/10.2307/2660739.

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Rogers, Paul C., Wayne D. Shepperd, and Dale L. Bartos. "Aspen in the Sierra Nevada: Regional Conservation of a Continental Species." Natural Areas Journal 27, no. 2 (April 2007): 183–93. http://dx.doi.org/10.3375/0885-8608(2007)27[183:aitsnr]2.0.co;2.

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Craib, Raymond B. "Procesos rurales e historia regional (sierra y costa totonacas de Veracruz)." Hispanic American Historical Review 79, no. 1 (February 1, 1999): 160–62. http://dx.doi.org/10.1215/00182168-79.1.160.

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Dissertations / Theses on the topic "Comité Regional de la Sierra"

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Bartolini, Claudio. "Regional Structure and Stratigraphy of Sierra El Aliso, Central Sonora, Mexico." Thesis, The University of Arizona, 1988. http://hdl.handle.net/10150/244082.

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Assemblages of Paleozoic age and less significant Triassic and possibly Cretaceous-Tertiary volcanic rocks constitute the Sierra El Aliso, 186 km east-southeast of Hermosillo, Sonora. The Paleozoic section consists of approximately 2000 m of allochthonous Ordovician to Permian pelagic and hemipelagic deposits that accumulated in continental slope, continental rise and ocean floor (?) environments. The lower Paleozoic is characterized by graptolitic black shale and radiolarian chert, quartzite, argillite and local limestone. The upper Paleozoic is predominantly turbidite carbonates rich in benthonic foraminifera, and conodont faunas, subordinate bedded chert, siltstone, sandstone and chert-clast conglomerate. After Early Permian time, but prior to the deposition of the Late Triassic Barranca Group the Paleozoic section was imbricated along south-southeast vergent thrust faults. The Triassic rocks unconformably overlie the Paleo-zoic strata and all thrust faults. The Triassic and older rocks are overlain by the Cretaceous-Tertiary volcanics.
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Gross, Deanna Katherine, and deanna gross@adelaide edu au. "POLITICS AND PLUNDER: Civil war and regional intervention in Africa." Flinders University. School of Political and International Studies, 2007. http://catalogue.flinders.edu.au./local/adt/public/adt-SFU20080502.111658.

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Over recent decades, civil wars in Africa have taken millions of lives and caused widespread destruction of whole states and regions. The living standards of peoples residing in such states in Africa which have been devastated by war are often deplorable, with violence, disease and poverty characterising life there. Lawlessness is another feature of such wars, making these states optimal places for international terrorist groups to operate in, and from. For both the above reasons, the West should not turn a blind eye to this issue. These wars that have occurred in a number of African states, including Rwanda, Sierra Leone, the Democratic Republic of Congo (DRC) and Sudan, have often become regionalised with surrounding states increasingly becoming involved. This is particularly the case when economic gain can be sought through involvement in the civil war. The introduction of regional actors into domestic civil wars frequently serves to intensify and prolong the conflict, through an increase of arms and troops entering the fighting. The surrounding state actors largely claim to be involved for political reasons, namely to provide security to their own state. However, numerous credible reports have shown that vast plundering of natural resources has been carried out in war-time by surrounding states in the war-torn state. Consequently, this thesis examines the motives of surrounding state actors when deciding to participate in domestic civil wars of their neighbours. To do this, I compile case studies on both Sierra Leone and the Democratic Republic of Congo since both states had been ravaged by violent and drawn-out civil wars involving regional actors. Furthermore, the regional actors in both cases (Liberia in Sierra Leone, and particularly Rwanda, Uganda, Zimbabwe in the DRC) have been accused of participating in the wars for economic gain. The case studies showed that while political motivations largely drive the initial decision by regional actors to participate in civil wars in their region, it is subsequently economic gain that both allows and compels them to continue their involvement in the civil war. Henceforth, in the final chapter, I put investigate policy suggestions for the future including: prevention of resources being used to fuel warfare through controlling their access to legitimate channels; the use of aid to reduce the likelihood of those in poverty turning to war in pursuit of sustenance, including opportunities to target aid and use compliance with particular peace agreements as a prerequisite for attaining the funding; diversification of the economies of these weak states through development assistance to reduce risks produced by a high dependency on primary commodity exports for income and financial sanctions in the form of freezing of assets or asset blocking. These policy suggestions seek to address both the political and economic motivations of the surrounding state actors in participating in civil wars in Africa.
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Vargas, Marco Antonio Moreno 1976, Ivo Marcos 1960 Theis, and Universidade Regional de Blumenau Programa de Pós-Graduação em Desenvolvimento Regional. "Oportunidades e ameaças para o desenvolvimento regional de Santa Cruz de La Sierra, Bolívia : uma análise institucional do plano de desenvolvimento socioeconômico /." reponame:Biblioteca Digital de Teses e Dissertações FURB, 2018. http://www.bc.furb.br/docs/TE/2018/364481_1_1.pdf.

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PAULA, Rodolfo Reis de. "Geologia estrutural das serras Curamalal e Bravard, porção oeste do cinturão móvel paleozóico Sierra de la Ventana, Argentina." reponame:Repositório Institucional da CPRM, 2014. http://rigeo.cprm.gov.br/xmlui/handle/doc/1284.

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Submitted by maria carolina coutinho barrozo de freitas (maria.barrozo@cprm.gov.br) on 2014-07-28T18:46:20Z No. of bitstreams: 1 Geologia estrutural das serras Curamalal e Bravard, porção oeste do Cinturão móvel paloezoico Sierra de la Ventana (Argen~1.pdf: 42296946 bytes, checksum: 81eb20f0ba11e8d8833cd93be7579d89 (MD5)
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O presente trabalho apresenta novos dados geológicos adquiridos na porção oeste do cinturão móvel Sierra de la Ventana, localizada 550 Km a sul de Buenos Aires, Argentina. Geologicamente está inserida sobre a porção sul do Cráton Rio de La Plata. As rochas análogas a este cinturão gonduânico encontram-se nas Ihas Malvinas, na África do Sul, na Antártica e na Austrália. A Sierra de La Ventana é constituida por um embasamento meta-ígneo do fim do Neoproterozoico ao Cambriano, e rochas metassedimentares depositadas entre o Ordoviciano e o Permiano. Ambas unidades foram deformadas e metamorfisadas durante o Paleozoico Superior formando o orógeno Gondwanides. A analise das estruturas deformacionais permitiu a caracterização de duas fases de deformação na área. A primeira fase (D1) de caráter dúctil-rúptil, gerou dobras e falhas reversas NW-SE, concomitantemente a um metamorfismo de baixo grau com temperatura máxima em torno de 300°C, estimada pelas microestruturas de deformação em quartzo. Três clivagens metamórficas na escala microscópica foram descritas nos meta-pelitos, interpretadas como produto da primeira fase de deformação (D1). Nenhuma feição de redobramento foi observada na macro-escala. A partir da análise cinemática e do cálculo dos vetores de compressão s1, s2 e s3, foi possível reconhecer planos de falha que não se adequam ao regime de esforços vigentes durante a fase de deformação (D1), cuja a compressão tem orientação NE-SW. Por isso foram interpretados como pertencentes a uma segunda fase de deformação (D2), puramente rúptil e bem menos expressiva que a primeira fase (D1) com compressão de orientação NW-SE. A análise cinemática e dinâmica das estruturas das fases D1 e D2 indicam que ambas se desenvolveram em um regime de deformação coaxial, sem rotação. Houve uma mudança de quase 90° em torno do eixo X cartesiano no sentido anti-horário em relação a posição de s1 e s2 nas duas fases, e em torno de 30° no eixo Y também no sentido anti-horário em relação a s1 e s3. A ausência de estruturas intermediárias aos campos de tensão das fases D1 e D2, sugere que são fases deformacionais distintas.
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PAULA, Rodolfo Reis de. "Geologia estrutural das serras Curamalal e Bravard, porção oeste do cinturão móvel paleozoico Sierra de la Ventana, Argentina." reponame:Repositório Institucional da CPRM, 2014. http://rigeo.cprm.gov.br/xmlui/handle/doc/1770.

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O presente trabalho apresenta novos dados geológicos adquiridos na porção oeste do cinturão móvel Sierra de la Ventana, localizada 550 Km a sul de Buenos Aires, Argentina. Geologicamente está inserida sobre a porção sul do Cráton Rio de La Plata. As rochas análogas a este cinturão gonduânico encontram-se nas Ihas Malvinas, na África do Sul, na Antártica e na Austrália. A Sierra de La Ventana é constituida por um embasamento meta-ígneo do fim do Neoproterozoico ao Cambriano, e rochas metassedimentares depositadas entre o Ordoviciano e o Permiano. Ambas unidades foram deformadas e metamorfisadas durante o Paleozoico Superior formando o orógeno Gondwanides. A analise das estruturas deformacionais permitiu a caracterização de duas fases de deformação na área. A primeira fase (D1) de caráter dúctil-rúptil, gerou dobras e falhas reversas NW-SE, concomitantemente a um metamorfismo de baixo grau com temperatura máxima em torno de 300°C, estimada pelas microestruturas de deformação em quartzo. Três clivagens metamórficas na escala microscópica foram descritas nos meta-pelitos, interpretadas como produto da primeira fase de deformação (D1). Nenhuma feição de redobramento foi observada na macro-escala. A partir da análise cinemática e do cálculo dos vetores de compressão s1, s2 e s3, foi possível reconhecer planos de falha que não se adequam ao regime de esforços vigentes durante a fase de deformação (D1), cuja a compressão tem orientação NE-SW. Por isso foram interpretados como pertencentes a uma segunda fase de deformação (D2), puramente rúptil e bem menos expressiva que a primeira fase (D1) com compressão de orientação NW-SE. A análise cinemática e dinâmica das estruturas das fases D1 e D2 indicam que ambas se desenvolveram em um regime de deformação coaxial, sem rotação. Houve uma mudança de quase 90° em torno do eixo X cartesiano no sentido anti-horário em relação a posição de s1 e s2 nas duas fases, e em torno de 30° no eixo Y também no sentido anti-horário em relação a s1 e s3. A ausência de estruturas intermediárias aos campos de tensão das fases D1 e D2, sugere que são fases deformacionais distintas. Palavras-chave: Paleozóico, Deformação dúctil-rúptil, Gondwanides, Sierra de La Ventana, microestruturas em quartzo.
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Velasco, Juliana. "Regional Organizations and the Durability of Peace." Master's thesis, University of Central Florida, 2013. http://digital.library.ucf.edu/cdm/ref/collection/ETD/id/5882.

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This thesis investigates the role of regional organizations in peacemaking and peacekeeping, particularly on the effects of peace agreement duration. This is important because the United Nations has been traditionally seen as the default international peacekeeping force but recently, more responsibility is being given to regional organizations. This study hypothesizes that regional organizations' ability to clear commitment problems, create specific agreements, and willingness to enforce agreements make them the most effective third parties to deal with many conflicts. However, the study also hypothesizes that regional organizations are less fit to mediate conflicts based around ethnicity, identity, or religious disparities. By utilizing a mixture of logistic regression and case studies, the results illustrate that regional organizations are an essential asset to creating agreements that elongate the duration of peace. In testing for the partiality of regional organizations, the specifics of agreements made, the willingness and capabilities of enforcement, the reason for the conflict and the institutionalization of the organization, quantitative and qualitative results illustrate that regional organizations are a valid tool for conflict management.
M.A.
Masters
Political Science
Sciences
Political Science; International Studies
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7

Villanueva, Rabanal Jorge Armando. "Participación y co-gestión al interior del Área de Conservación Regional Alto Nanay Pintuyacu Chambira en Loreto: el caso del Comité de Gestión." Master's thesis, Pontificia Universidad Católica del Perú, 2020. http://hdl.handle.net/20.500.12404/17659.

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En los últimos años, el Comité de Gestión del Área de Conservación Regional Alto Nanay-Pintuyacu-Chambira en Loreto, ha logrado consolidarse como un espacio de participación y representación de las comunidades de la zona, sugiriendo que el modelo de co-gestión en las ACR resulta beneficioso para los diversos actores involucrados y constituiría una herramienta de participación eficaz en un entorno donde la gestión de los recursos naturales resulta fundamental para la vida de las comunidades de la zona. Parece tratarse de una experiencia de creación de capital social que crece y se fortalece con su uso. La presente investigación constituye un estudio de caso que busca identificar las principales características de la participación del Comité de Gestión del Área de Conservación Regional Alto Nanay-Pintuyacu-Chambira (Loreto), como actor involucrado en el proceso de elaboración del Plan Maestro y como facilitador de la participación eficaz de los actores sociales, políticos y económicos del ACR, a través del análisis de su funcionamiento y de sus interrelaciones con otros actores de la zona, con el fin de contribuir al conocimiento de las dinámicas de participación formal de comunidades campesinas y nativas en áreas de gran biodiversidad de la Amazonía peruana. Asimismo, de manera general, la investigación explora los vínculos entre la participación comunitaria y la gestión de un Área de Conservación Regional, poniendo énfasis en los conceptos de co-gestión, institucionalidad y capital social, los cuales sirven de paraguas para realizar el análisis del Comité de Gestión como actor social que permite el involucramiento de la población en la gestión de un territorio con gran biodiversidad. La institucionalidad-legitimidad, los conocimientos-capacidades, así como la articulación interinstitucional, son las tres dimensiones empleadas para conocer el desempeño real del Comité de Gestión en términos de co-gestión del ACR-ANPCH, así como los principales problemas o retos que enfrenta. De esta manera, puede apreciarse que el Comité de Gestión constituye una figura de participación que goza de institucionalidad y legitimidad en al ACR-ANPCH, cuyos miembros poseen conocimientos vinculados principalmente al proceso de elaboración del Plan Maestro y que han cumplido un importante rol articulador entre las diferentes instancias de gestión del ACR. Sin embargo, también queda claro que el Comité de Gestión enfrenta serios retos, relacionados especialmente con su sostenibilidad financiera y con la etapa de implementación del Plan Maestro una vez que sea aprobado.
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Álvarez, Rogel Yolanda. "Aplicación de tecnología S.I.G. al Estudio del Riesgo y Prevención de Incendios Forestales en el área de Sierra Espuña-Gebas (Región de Murcia)." Doctoral thesis, Universidad de Murcia, 2000. http://hdl.handle.net/10803/10878.

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El trabajo aborda el problema de los incendios forestales, utilizando como área piloto del Parque Regional de Sierra Espuña y su entorno, generando un Sistema de Información Geográfica (SIG) que incorpora variables climáticas, topográficas, de vegetación y humanas vinculadas directa o indirectamente con los incendios forestales; se implementan índices y modelos de riesgo y simulaciones del comportamiento del fuego con fines predictivos. Se estudian los incendios forestales desde una doble perspectiva: por un lado se confecciona una cartografía detallada del riesgo de incendios en la zona, estableciendo niveles de riesgo en función de un índice resultante de la combinación de los factores que intervienen en el inicio y posterior desarrollo del incendio. Por otro se realizan simulaciones sobre el comportamiento más previsible del fuego, bajo las condiciones particulares del área. También se analizan las posibilidades que ofrecen las imágenes de satélite como complemento para el estudio de incendios forestales.
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Douglas, John Elmer. "Regional interaction in the Northern Sierra: An analysis based on the late prehistoric occupation of the San Bernardino Valley, southeastern Arizona." Diss., The University of Arizona, 1990. http://hdl.handle.net/10150/185011.

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The terms "core" and "periphery" have a long history of use for describing regional variability in the archaeological record. Contemporary theories for the late prehistoric in the Greater Southwest often follow this tradition, postulating underlying social processes that created this division. This dissertation examines the assumptions and the evidence for theories of long-distance social interaction by considering the prehistory of the Northern Sierra, a region in the south-central Greater Southwest located in northwestern Chihuahua, northeastern Sonora, southwestern New Mexico, and southeastern Arizona. Paquime (sometimes called Casas Grandes) in Chihuahua is widely considered to be the core of late prehistoric developments in the Northern Sierra. The history of research and interpretation of the region are carefully considered, an analysis that demonstrates the inadequacies of current data and theory. New frameworks will be needed to resolve disputed issues. Towards this end, evidence of interaction at Paquime is examined by analyzing the quantity and distribution of nonlocal ceramics within the site. These probable exchange items are found to be relatively rare and their distribution diffuse, indicating acquisition was largely casual and infrequent. Attention is then focused on the postulated periphery by examining the upper San Bernardino Valley in the extreme southeastern corner of Arizona. Data collected for this examination includes survey within the Valley and excavation of the late prehistoric Boss Ranch Site (AZ FF:7:10 (ASM)). The interpretive concerns that are addressed include (1) population movements, (2) external influences on settlement systems, (3) trade and interaction, and (4) the influences of subsistence systems. The analysis revealed no evidence of population intrusion from the "core" and few aspects of local material culture that could be ascribed to Paquime. Exchange items are rare, and the probable sources include many areas besides the zone around Paquime. Furthermore, excavation data suggest that settlements may have been occupied repeatedly for short periods. This undermines notions of stable core and periphery interaction by indicating the absence of surplus crops, stable social alliances, and hierarchical settlement systems in the region.
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Araos, Espinoza José Miguel. "Glacial geomorphology and paleoglacial behavior estimation in Sierra Baguales (50° S): Paleoclimatic factors that controlled glacier variations within the pleistocene - holocene regional context." Tesis, Universidadn de Chile, 2016. http://repositorio.uchile.cl/handle/2250/142482.

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Doctor en Ciencias, Mención Geología
The Sierra Baguales Mountain Range (SBMR) forms the eastern foothills of the Patagonian Andes located between 50º and 51º S, topographically isolated from the Southern Patagonian Icefield (SPIF) and under the influence of the Westerly Winds. Its landscape shows glacial deposits and morphologies, potentially useful for the reconstruction of the Pleistocene Holocene glaciations, which occurred in the vicinity of the Patagonian Ice Cap, and possibly showed individual responses to environmental change after the Last Glacial Maximum (LGM). Using simple and multivariate statistical methods, the morphometry of 143 glacial cirques, distributed between the current eastern limit of the SPIF and the easternmost SBMR, approximately 200 km from the Pacific coast, was analyzed. For the latter sector, using photo-interpretation, Geographic Information Systems (GIS) and field work, the first glacial and periglacial geomorphological map of the area was constructed. The relationship between the Geological Strength Index (GSI), rainfall gradient, and cirque areas, which were occupied and eroded by former alpine glaciers, was also established. To this end, theoretical profiles of the ice topography, based on a perfect plasticity model, were developed. Ages of local environmental changes were estimated using 14C dating. Equilibrium Line Altitude (ELA) variations were interpreted based on geomorphological evidence and the accumulation area ratio (AAR).The lowering of the ELA was converted to the change in temperature by multiplying it with an average atmospheric lapse rate. For the SBMR, it is possible to recognize two glaciation levels which rise towards the interior of continent. Their spatial distribution and elevation were controlled by tectonic factors (Andean uplift), the rainfall gradient and the climate contrast from east (temperate maritime) to west (dry cold), present in southern Patagonia since the LGM. The lower group of glacial cirques is distributed in the lower areas of the main valleys. These have no current evidence of snow or glacial processes and have been subject to fluvial erosion and gravitational processes. These cirques can be associated with outlet glacier advance of the Patagonian Ice Cap during the Holocene, and were probably partially or completely covered with ice during the LGM or prior glaciations. On the other hand, the upper group of glacial cirques is located east of the SPIF and mainly in the eastern section of the SBMR. Their size is reduced progressively to the east due to the increased resistance of the rocks on which they developed and the regional rainfall gradient. These cirques show evidence of lateral and frontal moraines of alpine glaciers, some of which are currently active. This cirque group corresponds to those glaciers that remained after the middle Holocene, favored by a gentle slope and aspect, in addition to low temperatures prevailing in the highest marginal sections of the SPIF and particularly the SBMR. Radiocarbon ages can be considered as evidence of environmental change linked to the temperature decrease and rainfall increment resulting from the latitudinal shift and the increase in strength of the Westerly Winds during the middle Holocene. For the SBMR, where the local atmospheric temperature from the Tardiglacial was approximately 3.8±0.8°C colder than today, temperatures possibly remained lower in relation to the regional context, mainly due to the cold and dry climate prevailing towards the interior of the continent, and the elevation of the basins where the former alpine glaciers were located, which eventually advanced and coalesced to form a small Icefield. Such advances could be related to variations in the Frias Lobe, at the same latitude of the SBMR but closer to the SPIF eastern margin.
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Books on the topic "Comité Regional de la Sierra"

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Las montañas como regiones: La sierra de El Cuale. Zapopan, Jalisco, México: Universidad de Guadalajara, Centro Universitario de Ciencias Económico Administrativas, Departmento de Estudios Regionales, 2009.

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Hernández, Jorge Enríquez. Análisis geoeconómico del sistema regional de la Sierra Tarahumara. México: Universidad Nacional Autónoma de México, Facultad de Filosofía y Letras, Colegio de Geografía, 1988.

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Liisa, North, and FLACSO (Organization) Sede Ecuador, eds. Vamos dando la vuelta: Iniciativas endógenas de desarrollo local en la Sierra ecuatoriana. Quito, Ecuador: FLACSO Ecuador, 2009.

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King, Rodney. Zur Strategie der Entwicklungszentren in den Provinzen Sierra Leones: Möglichkeiten und Grenzen. Stuttgart: Institut für Raumordnung und Entwicklungsplanung, 1992.

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Abrego, Daniela Gaya. Santa Cruz de la Sierra, entre el aislamiento y la autonomía: Análisis sociológico de la historia del oriente boliviano, 1561-1825. Santa Cruz, Bolivia: Fondo Editorial Municipal de Santa Cruz de la Sierra, 2000.

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Québec (Province). Comité sur les agglomérations urbaines. Document de réflexion des membres représentant les municipalités de la périphérie au sein du Comité sur les agglomérations urbaines. Québec]: Le Comité, 1996.

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Carrillo, Luis A. Ramírez. Chilchota, un pueblo al pie de la sierra: Integración regional y cambio económico en el noroeste de Michoacán. Zamora, Mich. [i.e. Michoacán]: Colegio de Michoacán, 1986.

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Iglesias, Horacio Morales. Zonas afectadas por el Huracán Stan en las regiones Istmo-Costa, Sierra y Soconusco: (investigación para su ordenamiento), 2008. San Cristóbal de Las Casas, Chiapas, Mexico: El Colegio de la Frontera Sur, Laboratorio de Análisis de Información Geográfica y Estadística, 2008.

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United States. Congress. House. Committee on International Relations. Subcommittee on Africa. Elections in Sierra Leone: A step toward regional stability? : hearing before the Subcommittee on Africa of the Committee on International Relations, House of Representatives, One Hundred Seventh Congress, second session, May 16, 2002. Washington: U.S. G.P.O., 2002.

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Así nació el Cuzco rojo. [S.l: s.n.], 1986.

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Book chapters on the topic "Comité Regional de la Sierra"

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Sickman, James O., and John M. Melack. "Nitrogen and Sulfate Export from High Elevation Catchments of the Sierra Nevada, California." In Biogeochemical Investigations at Watershed, Landscape, and Regional Scales, 217–26. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-017-0906-4_21.

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Sickman, James O., John M. Melack, and John L. Stoddard. "Regional analysis of inorganic nitrogen yield and retention in high-elevation ecosystems of the Sierra Nevada and Rocky Mountains." In The Nitrogen Cycle at Regional to Global Scales, 341–74. Dordrecht: Springer Netherlands, 2002. http://dx.doi.org/10.1007/978-94-017-3405-9_10.

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McNamee, Terence, and Monde Muyangwa. "Introduction." In The State of Peacebuilding in Africa, 3–14. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-46636-7_1.

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Abstract The introduction briefly summarizes the thematic chapters in the book (conflict prevention, mediation and management; post-conflict reconstruction, justice and DDR; the role of women, religion, humanitarianism, grassroots organizations and early warning systems; and regional and continental bodies) as well as the country/region case studies (the Democratic Republic of Congo, Rwanda, Sierra Leone, Sudan/South Sudan, Mozambique and the Sahel/Mali). The introduction also outlines the key conceptual and definitional challenges and explains what sets this volume apart from others in the ever-expanding literature on peacebuilding in Africa. Of several recurrent themes in the book that merit closer scrutiny, the introduction highlights: funding challenges; managing expectations; tensions between grassroots dynamics and peace-building at the elite level; varying effectiveness of regional economic communities and the African Union; and frequent lack of coordination between donors and partners on the ground.
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Hocquenghem, Anne-Marie. "Contribución a una historia regional." In Los Guayacundos de Caxas y la sierra piurana, 155–62. Institut français d’études andines, 1990. http://dx.doi.org/10.4000/books.ifea.1114.

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"Sierra Leone’s war in a regional context: lessons from interventions." In A Human Security Doctrine for Europe, 111–38. Routledge, 2006. http://dx.doi.org/10.4324/9780203020005-13.

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Martínez-Flener, Milagros. "Violencia en la sierra de Piura colonial durante el siglo XVIII." In El norte en la historia regional, siglos XVIII-XIX, 325–44. Institut français d’études andines, 1998. http://dx.doi.org/10.4000/books.ifea.3311.

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Hernan, González-Osorio. "El humus en la zona cafetera colombiana: Contenido calidad y su relación con algunas propiedades físicas y químicas del suelo." In Materia orgánica biología del suelo y productividad agrícola: Segundo seminario regional comité regional eje cafetero, 11–32. Cenicafé, 2009. http://dx.doi.org/10.38141/10791/0003_1.

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R. D., Zapata-Hernández. "El compostaje y los índices para evaluar su estabilidad." In Materia orgánica biología del suelo y productividad agrícola: Segundo seminario regional comité regional eje cafetero, 33–42. Cenicafé, 2009. http://dx.doi.org/10.38141/10791/0003_2.

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N. W., Osorio-Vega. "Microorganismos del suelo y su efecto sobre la disponibilidad y absorción de nutrientes por las plantas." In Materia orgánica biología del suelo y productividad agrícola: Segundo seminario regional comité regional eje cafetero, 43–71. Cenicafé, 2009. http://dx.doi.org/10.38141/10791/0003_3.

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S., Sadeghian. "La materia orgánica en agroecosistemas cafeteros de Colombia." In Materia orgánica biología del suelo y productividad agrícola: Segundo seminario regional comité regional eje cafetero, 72–99. Cenicafé, 2009. http://dx.doi.org/10.38141/10791/0003_4.

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Conference papers on the topic "Comité Regional de la Sierra"

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Margason, Andy, Gilles V. Tagne, Aleksandr Glavnik, Claire Browning, Rylee Norris, Katie Mesa, and Benjamin Robbins. "REGIONAL AND LOCAL CONTROLS ON GROUNDWATER QUALITY IN SIERRA LEONE, WEST AFRICA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-333560.

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Kylander-Clark, Andrew, and Scott Johnston. "Detrital Titanite Petrochonology of Sierra Nevada Modern Sands: Tracing Local and Regional-Scale Arc Processes." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1392.

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Gevedon, Michelle L., Juliet Ryan-Davis, Jaime D. Barnes, Jade Star Lackey, Michael G. Prior, Kouki Kitajima, and John W. Valley. "REGIONAL IMPLICATIONS OF LOW-δ18O SKARNS OF THE JURASSIC MOJAVE SEGMENT OF THE SIERRA NEVADA ARC." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274510.

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Johnston, Scott M., Andrew R. C. Kylander-Clark, and Andrew P. Barth. "DETRITAL ZIRCON AS A TRACER FOR TIME-TRANSGRESSIVE, REGIONAL-SCALE ARC PROCESSES: A CASE STUDY FROM MODERN SIERRA NEVADA SANDS." In 116th Annual GSA Cordilleran Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020cd-347509.

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Johnston, Scott, Andrew R. C. Kylander-Clark, and Andrew P. Barth. "DETRITAL ZIRCON AS A TRACER FOR TIME-TRANSGRESSIVE, REGIONAL-SCALE ARC PROCESSES: A CASE STUDY FROM MODERN SIERRA NEVADA SANDS." In Cordilleran Section-117th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021cd-363206.

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Reports on the topic "Comité Regional de la Sierra"

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J.A. Rodriguez-Pineda, P. Goodell, P.F. Dobson, J. Walton, R. Oliver, De La Garza, and S. Harder. REGIONAL HYDROLOGY OF THE NOPAL I SITE, SIERRA DE PENA BLANCA, CHIHUAHUA, MEXICO. Office of Scientific and Technical Information (OSTI), July 2005. http://dx.doi.org/10.2172/859183.

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