Trans-Sierran climatic contacts during the last 12,000 years [abstract]

EXTRACT (SEE PDF FOR FULL ABSTRACT): The early-Holocene warm period, ca. 9000 years ago, is a realistic analog for the possible effects of greenhouse warming. At that time the vegetation of the western Sierra Nevada resembled that currently found east of the crest. ... Tourism, water supply, and the logging industry will be negatively effected if climate changes during the next century are in the direction and magnitude of those of the early Holocene. Increased precipitation in the eastern Sierra could offset some of the effects.

Modeling the effect of snow on seasonal runoff within the Truckee River drainage basin

EXTRACT (SEE PDF FOR FULL ABSTRACT): We estimate monthly runoff for a 2-dimensional solution domain containing those areas tributary to Pyramid Lake, Nevada (the Truckee River drainage basin) at a 1-kilometer grid cell spacing. ... To calculate the effect of snow on the hydrologic system, we perform two experiments. In the first we assume that all precipitation falls as rain; in the second we assume that some precipitation falls as snow, thus available water is a combination of rain and snowmelt. We find that considering the effect of snow results in a more accurate representation of mean monthly flow rates, in particular the peak flow during the melt season in the Sierra Nevada. These preliminary results indicate that a relatively simple snow model can improve the representation of Truckee River basin hydrology, significantly reducing errors in modeled seasonal runoff.

The top ten California floods of the 20th century

The purpose of this paper is to summarize the biggest northern California floods of the 20th century. Flooding in California can occur from different causes. At least three types of floods occur: 1. Winter general floods, which cover a large area. 2. Spring and early summer snowmelt floods unique to the higher-elevation central and southern Sierra Nevada, which occur about once in 10 years on the average. 3. Local floods from strong thunderstorms, with intense rain over a relatively small area. These originate in moist tropical or subtropical air and include the flash floods of the desert and other areas of southern California when remnants of eastern Pacific hurricanes get carried into the state.

中国华北和美国加州地区地震层析成像研究

In recent years seismic tomography has become a powerful tool for studying the three-dimensional crust and mantle structure. In this study, we collected a large number of regional and teleseismic travel-time data and used seismic tomography method to study the relationship between earthquake occurrence and crustal heterogeneity for the 1992 Landers earthquake, heterogeneity and evolution of lithosphere under North China Craton and Southern California, and deep structure and origin of the Changbai intraplate volcano in Northeast China. Our results show a correlation between the seismic rupture zone and crustal heterogeneity. The distribution of the Landers aftershocks is cluster-like and separated or terminated in areas where low-velocity anomalies exist．Most of the large earthquakes with magnitudes >4.0 occurred in or around areas with high P-wave velocity．The possibility is that high-velocity areas are brittle and strong parts which can sustain seismogenic stress，and so can generate earthquakes. Our tomographic images show a very heterogeneous structure in the crust and upper mantle beneath Southern California. Three major anomalies in the upper mantle are revealed clearly beneath the southern Sierra Nevada, Transverse Ranges and Salton Trough. We consider that the high-velocity anomaly beneath the Transverse Ranges was formed through asymmetrical two-side convergence of subcrustal lithosphere and sinking to asthenosphere. Formation of the dense crust root and “drip structure” caused the high-velocity anomaly under the southern Sierra Nevada. The Salton Trough low is the response to the lithospheric extension when the Pacific plate was rifted away from the North American Plate. The tomograpic images beneath the North China Craton show that there exist different lithospheric structures under the different blocks. Complex, prominent low-velocity and high-velocity anomalies are imaged beneath the North China Basin, Trans-North China Orogen (TNCO), and Ordos Block which correspond to rifted, orogenic and cratonic lithospheres, respectively. The thickness of the three-type lithospheres is about 70, 90 and >250 km, respectively. Our results suggest that lithospheric thinning under the eastern part of North China Craton is due to long-term replacement and chemical and thermal erosion of the ancient lithosphere by the hot asthenosphere. The remains of ancient lithosphere exist either in the present upper mantle or have sunk into the mantle transition zone. Our tomographic result of the Changbai volcanic area suggests that the origin of the Changbai volcano is related to the deep dehydration of the subducted Pacific slab and corner flow in the big mantle wedge (BMW) above the stagnant Pacific slab.

Spa Rituales Ancestrales AüA S.A.S.

Las practicas ancestrales de las culturas precolombinas cada día son mas validas en su aplicación actual para la medicina alternativa, orientada al bienestar y la salud, es un hecho que en los últimos años se observa un gran crecimiento de endemias de estrés que se presentan bajo determinadas circunstancias propias del sistema actual de vida urbana y actividades cotidianas, ocasionando recargas de tensión como respuesta a la supervivencia en un mundo agitado. La somatizacion del estrés se traduce en enfermedades fisiológicas, emocionales y anímicas, consideradas peligrosas y causantes de altos índices de morbilidad y mortalidad. AúA S.A.S. se crea como solución a este gran conflicto que azota a la humanidad, así se han incrementado las instalaciones de diversos Spa (Salud por agua) como establecimientos de bienestar y esparcimiento que incluyen terapias no solo físicas sino mentales y emocionales como un sistema holístico der salud. En los últimos años y gracias a las facilidades de movilidad y comunicaciones se observa un crecimiento acelerado del turismo de salud como sector de talla mundial, el cual apunta a un mayor desarrollo tanto a nivel nacional como internacional. Las visitas de turistas al país en interés de realizarse procedimientos tanto estéticos como médicos, permite identificar una gran oportunidad de negocio con visión sostenible y perdurable ante un futuro prometedor. En este sentido, se presenta la instauración de un Spa con rituales ancestrales como un establecimiento de salud (turismo de salud) que preste servicios a personas tanto colombianas como extranjeras interesadas en vivir una experiencia con tratamientos de relajación (turismo de bienestar). Si bien el gobierno ha impulsado nuevas políticas encaminadas al fomento de la competitividad en Colombia, a través de sectores de talla mundial, donde el turismo de salud se presenta con un fuerte potencial de crecimiento. El Programa de Transformación Productiva, es un ejemplo de lo anteriormente expresado como estrategia para lograr el desarrollo empresarial, crecimiento económico y la generación de más y mejores empleos en Colombia. AüA S.A.S ofrece servicios únicos con tiempos óptimos para resultados efectivos de relajación y bienestar, así como espacios adecuados, inspirados en los paisajes de la sierra nevada de Santa Marta y ecosistemas de la costa Caribe, teniendo un contacto más cercano con la naturaleza y sus elementos. Además de una atención y acompañamiento personalizado y servicios gratuitos de asesorías post-venta, creando un servicio nuevo de reeducación dentro del Spa y con material de cortesía dado, donde a través de libros, artículos, publicaciones, DVD y talleres a realizar el cliente cambiara su conciencia, como componentes diferenciadores y de valor agregado, saliendo de su estado patológico y con alto cubrimiento en la satisfacción de sus necesidades, creando fidelidad al cliente para que regrese. Así, en lo posible con esta información destacada de las encuestas, dentro de la investigación de mercados realizada, se puede determinar que la participación en el mercado es del 75%. El equipo emprendedor está conformado por Rosa Marina Lozano Socarrás, estudiante de Administración de Negocios Internacionales de la Universidad del Rosario. El proyecto arroja una rentabilidad del 58,22% promedio anual. El indicador VAN, determina que el proyecto arroja 60 Millones adicionales al invertir los recursos en este proyecto que en uno que rente el 33% anual, por lo tanto se sugiere continuar con el proyecto. Teniendo el indicador del Valor Presente Neto, para su cálculo es necesario la Tasa de descuento o Tasa de Interés de Oportunidad siendo del 33%, teniendo un valor de $ 60.278.254. La metodología empleada en el trabajo de grado se denota en la guía y lineamientos establecidos por el Centro de Emprendimiento de la Universidad del Rosario. Las fuentes primarias se destaca en la información de investigación de mercados a partir de encuestas, así como análisis del sector y competidores. La información secundaria se denota en el Plan de Negocios del subsector turismo de bienestar dado a conocer por el Ministerio de Industria, Comercio y Turismo.

La vida continúa: relatos de cómo se vive y se supera el ser víctima

Este trabajo es una colección de perfiles y crónicas sobre personas que tienen tres cosas en común: son víctimas de la violencia colombiana, el hecho de ser víctimas los afectó profundamente, y decidieron continuar con sus vidas pese a ello.

Estrategias Populistas en Colombia: Las elecciones Presidenciales de 2014

La presente investigación analiza las estrategias populistas empleadas por los candidatos para las presidenciales colombianas de 2014. Se asume el populismo como discurso desde los planteamientos de Ernesto Laclau, considerando que el populismo actúa en forma de discurso movilizador, cuya lógica implica la construcción de una perspectiva antagónica de la realidad, la cual identifica positivamente a las mayorías frente un enemigo que encarna valores y prácticas negativas. Las estrategias populistas constituyen el medio para proponer una visión dicotómica de la realidad y una demanda hegemónica, donde el candidato aparece como parte positiva del antagonismo y constituye la solución de la demanda más importante en términos sociales. La tesis se concentra en responder a la pregunta: ¿Cómo se emplearon las estrategias populistas en las elecciones presidenciales de 2014? Para esto se construyó un índice de estrategias populistas en el cual se ubicó el discurso de cada candidato, donde un antagonismo adecuadamente estructurado y una demanda hegemónica representativa para la sociedad, representa beneficios electorales para el candidato. Se concluye que una adecuada articulación discursiva entre frontera antagónica (receptor positivo y contraparte negativa) y demanda hegemónica, puede significar para el candidato una mayor probabilidad de éxito, en la medida que los ciudadanos interioricen su discurso y se adhieran a él.

Incidencia de los actores internacionales no estatales en los conflictos internos. Estudio de caso: la participación de las empresas militares privadas “Executive Outcomes” y “Sandline International” en la guerra civil de Sierra Leona (1991-2002)

La Participación de las Empresas Militares Executive Outcomes y Sandline International en el conflicto de Sierra Leona fue una de las primeras veces en las que se vieron en escena a estos actores confluyendo en un nuevo orden internacional; y este estudio de caso busca determinar la manera de actuar de estas empresas y su incidencia en el conflicto. El caso de Sierra Leona es uno de los principales acercamientos a este nuevo fenómeno, que empezó a ejercer funciones que tradicionalmente le correspondían a los Estados y que han llevado a una privatización de la seguridad. Por medio de este estudio de caso se busca también determinar cuáles son las falencias y los retos que acarrean a las Empresas Militares Privadas en cuanto a su intervención en los conflictos internos. El caso de Sierra Leona es fundamental en tanto fue uno de los conflictos más intensos desarrollados en África en la década de los 90; y fue el momento en el cual las Empresas Militares Privadas empezaron a estar en la mira internacional a causa de estas intervenciones que generaron tanto críticas negativas como positivas.

Bogotá no tiene mar pero tiene playa: el vallenato y sus intérpretes costeños en Bogotá

La Playa es un sector de la ciudad de Bogotá, donde se encuentra la oferta de músicos informales más grande de Colombia: mariachis, tríos de cuerda y grupos vallenatos. En esta investigación, se analiza la migración de músicos vallenatos provenientes del Caribe colombiano a este sector de la capital del país; se examina el trabajo de estos músicos en La Playa; y se revisa el proceso de consolidación del vallenato como música nacional.

Safeguarding livelihoods or exacerbating poverty?: Artisanal mining and formalization in West Africa

In recent years, policy mechanisms to support a formalized artisanal and small-scale mining (ASM) sector in sub-Saharan Africa have gained increasing currency. Proponents of formalization argue that most social and environmental problems associated with the sector stem from the fact that ASM is predominantly unregulated and operates outside the legal sphere. This paper critically examines recent efforts to formalize artisanal and small-scale mining inWest Africa, drawing upon recent fieldwork carried out in Sierra Leone, Ghana and Mali. In exploring the sector’s livelihood dimensions, the analysis suggests that bringing unregulated, informal mining activities into the legal domain remains a considerable challenge. The paper concludes by confirming the urgent need to refocus formalization strategies on the main livelihood challenges and constraints of small-scale miners themselves, if poverty is to be alleviated and more benefits are to accrue to depressed communities in mineral-rich regions.

Emplacement mechanism of the main granite pluton of the Lavras do Sul intrusive complex, South Brazil, determined by magnetic anisotropies

Magnetic fabric and rock magnetism studies were performed on apparently isotropic granite facies from the main intrusion of the Lavras do Sul Intrusive Complex pluton (LSIC, Rio Grande do Sul, South Brazil). This intrusion is roughly circular (similar to 12 x 13.5 km), composed of alkali-calcic and alkaline granitoids, with the latter occupying the margin of the pluton. Magnetic fabrics were determined by applying both anisotropy of low-field magnetic susceptibility (AMS) and anisotropy of anhysteretic remanent magnetization (AARM). The two fabrics are coaxial. The parallelism between AMS and AARM tensors excludes the presence of a single domain (SD) effect on the AMS fabric of the granites. Several rock-magnetism experiments performed in one specimen from each sampled site show that for all sites the magnetic susceptibility is dominantly carried by ferromagnetic minerals, while mainly magnetite carries the magnetic fabrics. Lineations and foliations in the granite facies were successful determined by applying magnetic methods. Magnetic lineations are gently plunging and roughly parallel to the boundaries of the pluton facies, except at the few sites in the central facies which have a radial orientation pattern. In contrast, the magnetic foliations tend to follow the contacts between the different granite facies. They are gently outerward-dipping inside the pluton, and become either steeply southwesterly dipping or vertical towards its margin. The lack of solid-state and subsolidus deformations at outcrop scale and in thin sections precludes deformation after full crystallization of the pluton. This evidence allows us to interpret the observed magnetic fabrics as primary in origin (magmatic) acquired when the rocks were solidified as a result of processes reflecting magma flow. The foliation pattern displays a dome-shaped form for the main LSIC-pluton. However, the alkaline granites which outcrop in the southern part of the studied area have an inward-dipping foliation, and the steeply plunging magnetic lineation suggests that this area could be part of a feeder zone. The magma ascent probably occurred due to ring-diking. (C) 2008 Elsevier B.V. All rights reserved.

CONTROLLING YELLOW-BILLED MAGPIES (Pica nuttalli)

The yellow-billed magpie is a little smaller than the American or black-billed magpie, but the difference in size is very slight. The birds look exactly alike, except one has a black beak and the other has a yellow bill and a bit of yellow skin back of the eye.There are concentrated populations in the Los Banos area, Gustine area, and along the course of the Merced River comprising about 19,100 acres. They are occasionally seen in other areas of the County, but only infrequently observed in the southwestern portion of the County. The heaviest populations are in walnut orchards, dairy farms, almond orchards, turkey ranches and areas adjacent to river bottoms.The yellow-billed magpie may represent a dying ancient race. Since scientific interest has been directed toward its habits and distribution, its range has become more restricted. There are reports that 50 or 60 years ago it was common in many places close to the Coast, where the observer would now look for it in vain. It inhabits only the interior of California west of the Sierra Nevada, chiefly in the Sacramento and San Joaquin Valleys. It haunts stock ranches, because food to its liking is usually plentiful in such places. When cattle and sheep are butchered the refuse attracts magpies. They gather about any dead animal. They feed on grasshoppers, worms and grubs, and of course always look for a reasonable supply of eggs.

Ordovician klippen structures of the Sierra de Umango: New insights on Tectonic evolution of the Western Sierras Pampeanas, Argentina

The basement rock of the Pampean flat-slab (Sierras Pampeanas) in the Central Andes was uplifted and rotated in the Cenozoic era. The Western Sierras Pampeanas are characterised by meta-igneous rocks of Grenvillian Mesoproterozoic age and metasedimentary units metamorphosed in the Ordovician period. These rocks, known as the northern Cuyania composite terrane, were derived from Laurentia and accreted toward Western Gondwana during the Early Paleozoic. The Sierra de Umango is the westernmost range of the Western Sierras Pampeanas.This range is bounded by the Devonian sedimentary rocks of the Precordillera on the western side and Tertiary rocks from the Sierra de Maz and Sierra del Espinal on the eastern side and contains igneous and sedimentary rocks outcroppings from the Famatina System on the far eastern side. The Sierra de Umango evolved during a period of polyphase tectonic activity, including an Ordovician collisional event, a Devonian compressional deformation, Late Paleozoic and Mesozoic extensional faulting and sedimentation (Paganzo and Ischigualasto basins) and compressional deformation of the Andean foreland during the Cenozoic. A Nappe System and an important shear zone, La Puntilla-La Falda Shear Zone (PFSZ), characterise the Ordovician collisional event, which was related to the accretion of Cuyania Terrane to the proto-Andean margin of Gondwana. Three continuous deformational phases are recognised for this event: the D1 phase is distinguished by relics of 51 preserved as internal foliation within interkinematic staurolite por-phyroblasts and likely represents the progressive metamorphic stage; the D2 phase exhibits P-T conditions close to the metamorphic peak that were recorded in an 52 transposition or a mylonitic foliation and determine the main structure of Umango; and the D3 phase is described as a set of tight to recumbent folds with S3 axial plane foliation, often related to thrust faults, indicating the retrogressive metamorphic stage. The Nappe System shows a top-to-the S/SW sense direction of movement, and the PFSZ served as a right lateral ramp in the exhumation process. This structural pattern is indicative of an oblique collision, with the Cuyania Terrane subducting under the proto-Andean margin of Gondwana in the NE direction. This continental subduction and exhumation lasted at least 30 million years, nearly the entire Ordovician period, and produced metamorphic conditions of upper amphibolite-to-granulite facies in medium- to high-pressure regimes. At least two later events deformed the earlier structures: D4 and D5 deformational phases. The D4 deformational phase corresponds to upright folding, with wavelengths of approximately 10 km and a general N-S orientation. These folds modified the S2 surface in an approximately cylindrical manner and are associated with exposed, discrete shear zones in the Silurian Guandacolinos Granite. The cylindrical pattern and subhorizontal axis of the D4 folds indicates that the S2 surface was originally flat-lying. The D4 folds are responsible for preserving the basement unit Juchi Orthogneiss synformal klippen. This deformation corresponds to the Chanica Tectonic during the interval between the Devonian and Carboniferous periods. The D5 deformational phase comprehends cuspate-lobate shaped open plunging folds with E W high-angle axes (D5 folds) and sub-vertical spaced cleavage. The D5 folds and related spaced cleavage deformed the previous structures and could be associated with uplifting during the Andean Cycle. (C) 2012 Elsevier Ltd. All rights reserved.

Biología de la conservación de endemismos vagetales de los parques nacionales canarios

[ES]El presente proyecto se centra en aplicar técnicas de biología molecular, demográficas y de biología reproductiva en cuatro endemismos canarios amenazados que se encuentran total o parcialmente localizados en los parques nacionales de Canarias: Silene nocteolens Webb & Berthel. (Parque Nacional del Teide, Tenerife); Ilex perado ssp. lopezlilloi (G. Kunkel) A. Hansen & Sunding (Parque Nacional Garajonay, La Gomera), Sorbus aria (L.) Crantz (Parque Nacional de la Caldera de Taburiente, La Palma) y Bencomia exstipulata Svent. (parques nacionales del Teide y Caldera de Taburiente). Se estableció un estudio genético a través de marcadores moleculares hipervariables, microsatélites, y se determinó para cada taxón la variación genética de sus poblaciones, para su posterior aplicación en la gestión en el ámbito de la Biología de la conservación de estos taxones.

Biofilms on exposed monumental stones: mechanism of formation and development of new control methods

Within the stone monumental artefacts artistic fountains are extremely favorable to formation of biofilms, giving rise to biodegradation processes related with physical-chemical and visual aspect alterations, because of their particular exposure conditions. Microbial diversity of five fountains (two from Spain and three from Italy) was investigated. It was observed an ample similarity between the biodiversity of monumental stones reported in literature and that one found in studied fountains. Mechanical procedures and toxic chemical products are usually employed to remove such phototrophic patinas. Alternative methods based on natural antifouling substances are recently experimented in the marine sector, due to their very low environmental impact and for the bio settlement prevention on partially immersed structures of ships. In the present work groups of antibiofouling agents (ABAs) were selected from literature for their ability to interfere, at molecular level, with the microbial communication system “quorum sensing”, inhibiting the initial phase of biofilm formation. The efficacy of some natural antibiofoulants agents (ABAs) with terrestrial (Capsaicine - CS, Cinnamaldehyde - CI) and marine origin (Zosteric Acid - ZA, poly-Alkyl Pyridinium Salts – pAPS and Ceramium botryocarpum extract - CBE), incorporated into two commercial coatings (Silres BS OH 100 - S and Wacker Silres BS 290 - W) commonly used in stone conservation procedures were evaluated. The formation of phototrophic biofilms in laboratory conditions (on Carrara marble specimens and Sierra Elvira stone) and on two monumental fountains (Tacca’s Fountain 2 - Florence, Italy and Fountain from Patio de la Lindaraja - Alhambra Palace, Granada, Spain) has been investigated in the presence or absence of these natural antifouling agents. The natural antibiofouling agents, at tested concentrations, demonstrated a certain inhibitory effect. The silane-siloxane based silicone coating (W) mixing with ABAs was more suitable with respect to ethyl silicate coating (S) and proved efficacy against biofilm formation only when incompletely cured. The laboratory results indicated a positive action in inhibiting the patina formation, especially for poly-alkyl pyridinium salts, zosteric acid and cinnamaldehyde, while on site tests revealed a good effect for zosteric acid.