Geology and Geochronology of Silica Sands of Coastal Plain of Thiruvananthapuram District, Kerala,India,With Special reference to Late Quaternary Environment

Department of Marine Geology & Geophysics, Cochin University of Science & Technology

The Engineering Geology of the Landslides on the North Coast of the Isle of Wight and their Stabilisation

Transfer thesis

Science 3 : biology and geology.

Ofrece los contenidos del currículo oficial de biología y geología de tercero de la ESO en inglés. Esta opción es para los centros que deseen incorporar el desarrollo del idioma inglés en la enseñanza de otras materias escolares. Facilita la integración de los conocimientos y fomenta el desarrollo del razonamiento. Permite cumplir los objetivos curriculares tanto en España como en el Reino Unido.

Science 3. Teacher's book : biology and geology.

Ofrece los contenidos del currículo oficial de biología y geología de tercero de la ESO en inglés. El propósito principal de este manual del profesor, es proporcionar apoyo en las aulas, desde un punto de vista científico y claro. El material que ha sido desarrollado desde una perspectiva científica, facilita la integración de los conocimientos y fomenta el desarrollo del razonamiento. Permite cumplir los objetivos curriculares tanto en España como en el Reino Unido.

Science 4 : biology and geology.

Ofrece los contenidos del currículo oficial de biología y geología del cuarto curso de la ESO en inglés. Esta opción es para los centros que deseen incorporar el desarrollo del idioma inglés en la enseñanza de otras materias escolares. Facilita la integración de los conocimientos y fomenta el desarrollo del razonamiento. Permite cumplir los objetivos curriculares tanto en España como en el Reino Unido.

Science 4. Teacher's book : biology and geology.

Ofrece los contenidos del currículo oficial de biología y geología del cuarto curso de la ESO en inglés. El propósito principal de este manual del profesor, es proporcionar apoyo en las aulas, desde un punto de vista científico y claro. El material que ha sido desarrollado desde una perspectiva científica, facilita la integración de los conocimientos y fomenta el desarrollo del razonamiento. Permite cumplir los objetivos curriculares tanto en España como en el Reino Unido.

OCR AS-A2 Geology

Texto de Geología para los cursos específicos del General Certificate of Education Advanced level (A,A2). Proporciona definiciones de términos clave importante de las especificaciónes. Incluye consejos sobre cómo mejorar los conocimientos para ayudar a los alumnos a prepararse para la evaluación práctica. La publicación está estructurada en cuatro unidades con preguntas de examen al final de cada una de ellas: Tectónica de la tierra; Rocas; Geología Ambiental; Evolución de la Vida, Tierra y Clima; y dos de habilidades prácticas para los niveles A y AS respectivamente. Tiene las soluciones a las cuestiones .

Physical geology : the science of Earth.

Es una herramienta de aprendizaje para entender los fundamentos científicos de la geología, así como las consecuencias de las acciones humanas sobre nuestro planeta. Ofrece a los estudiantes un marco para aprender y pensar de forma crítica y ayudarles a tomar decisiones sobre cuestiones tan importantes como: el calentamiento global, la superpoblación, el problema del agua dulce y otros.

An excursion guide to the Moine : geology of the northern highlands of Scotland.

Guía geológica con catorce excursiones de fácil acceso para conocer la amplia variedad de rocas y estructuras existente en la zona de Moine Supergroup. Contiene mapas geológicos de cada ruta y datos sobre el itinerario de cada excursión, así como datos adicionales (tipo de terreno, distancia y tiempo). La guía ha sido escrita por aquellos que tienen algún conocimiento previo de geología, por ejemplo, estudiantes graduados y geólogos profesionales. También se menciona que es necesario llevar calzado, ropa de abrigo e impermeable para realizar estas curiosas rutas.

Presencia del paleogeno bajo los sedimentos neogénicos de Vilablareix (Girona)

This study makes clear the existence of a paleogenical red basal level (Pontils Fm.) in the Vilablareix àrea, under the mio-pliocenical cover of the Girona plain, enlargening the surface known go far of that level

Calibration of uncertain flood inundation models using remotely sensed water levels

A traditional method of validating the performance of a flood model when remotely sensed data of the flood extent are available is to compare the predicted flood extent to that observed. The performance measure employed often uses areal pattern-matching to assess the degree to which the two extents overlap. Recently, remote sensing of flood extents using synthetic aperture radar (SAR) and airborne scanning laser altimetry (LIDAR) has made more straightforward the synoptic measurement of water surface elevations along flood waterlines, and this has emphasised the possibility of using alternative performance measures based on height. This paper considers the advantages that can accrue from using a performance measure based on waterline elevations rather than one based on areal patterns of wet and dry pixels. The two measures were compared for their ability to estimate flood inundation uncertainty maps from a set of model runs carried out to span the acceptable model parameter range in a GLUE-based analysis. A 1 in 5-year flood on the Thames in 1992 was used as a test event. As is typical for UK floods, only a single SAR image of observed flood extent was available for model calibration and validation. A simple implementation of a two-dimensional flood model (LISFLOOD-FP) was used to generate model flood extents for comparison with that observed. The performance measure based on height differences of corresponding points along the observed and modelled waterlines was found to be significantly more sensitive to the channel friction parameter than the measure based on areal patterns of flood extent. The former was able to restrict the parameter range of acceptable model runs and hence reduce the number of runs necessary to generate an inundation uncertainty map. A result of this was that there was less uncertainty in the final flood risk map. The uncertainty analysis included the effects of uncertainties in the observed flood extent as well as in model parameters. The height-based measure was found to be more sensitive when increased heighting accuracy was achieved by requiring that observed waterline heights varied slowly along the reach. The technique allows for the decomposition of the reach into sections, with different effective channel friction parameters used in different sections, which in this case resulted in lower r.m.s. height differences between observed and modelled waterlines than those achieved by runs using a single friction parameter for the whole reach. However, a validation of the modelled inundation uncertainty using the calibration event showed a significant difference between the uncertainty map and the observed flood extent. While this was true for both measures, the difference was especially significant for the height-based one. This is likely to be due to the conceptually simple flood inundation model and the coarse application resolution employed in this case. The increased sensitivity of the height-based measure may lead to an increased onus being placed on the model developer in the production of a valid model

Field meeting: Romney Marsh - its churches and geology, 22 May 2004

The building fabrics of seven churches situated either on Romney Marsh or the marshland fringe were examined briefly. These revealed important differences in the relative abundance of the two principal building stones. Ragstones from the Hythe Formation occurred more frequently in the northeast, while sandstones from the Ashdown 'Beds' were more common in the west. In the Romney Marsh area, both stones were quarried mainly from their adjoining coastlines, with, up to the thirteenth century, opportunist collection of beach boulders generally preceding the exploitation or hewn stone. Other building stones, possible distribution routes and impacts of the quarrying upon coastline development were also discussed.

The effect of a large freshwater perturbation on the glacial north Atlantic Ocean using a coupled general circulation model

The commonly held view of the conditions in the North Atlantic at the last glacial maximum, based on the interpretation of proxy records, is of large-scale cooling compared to today, limited deep convection, and extensive sea ice, all associated with a southward displaced and weakened overturning thermohaline circulation (THC) in the North Atlantic. Not all studies support that view; in particular, the "strength of the overturning circulation" is contentious and is a quantity that is difficult to determine even for the present day. Quasi-equilibrium simulations with coupled climate models forced by glacial boundary conditions have produced differing results, as have inferences made from proxy records. Most studies suggest the weaker circulation, some suggest little or no change, and a few suggest a stronger circulation. Here results are presented from a three-dimensional climate model, the Hadley Centre Coupled Model version 3 (HadCM3), of the coupled atmosphere - ocean - sea ice system suggesting, in a qualitative sense, that these diverging views could all have occurred at different times during the last glacial period, with different modes existing at different times. One mode might have been characterized by an active THC associated with moderate temperatures in the North Atlantic and a modest expanse of sea ice. The other mode, perhaps forced by large inputs of meltwater from the continental ice sheets into the northern North Atlantic, might have been characterized by a sluggish THC associated with very cold conditions around the North Atlantic and a large areal cover of sea ice. The authors' model simulation of such a mode, forced by a large input of freshwater, bears several of the characteristics of the Climate: Long-range Investigation, Mapping, and Prediction (CLIMAP) Project's reconstruction of glacial sea surface temperature and sea ice extent.