995 resultados para Lluís Companys
Resumo:
Two unknown volcanic outcrops in the Alt Emporda (Girona) are described in this paper . We present their exact situation and a description of their occurrence and their mineralogical and petrological characteristics. Bothhave been classified as alkali-olivine basalts and they probably extruded during the Neogen period
Resumo:
Two decay rates are distinguished in the discharge hydrograph of the Onyar River, using Maillet's formula. In this way, we can know which Kina of influence is made by geomorphology and rainfall distribution on fluvial processes
Resumo:
The unconfined compression strength is a geotechnical parameter frequently used to determine the bearing capacity of foundations on clayey soils. Its value can be obtained from the unconfined compression test and, among several in situ tests, the standard penetration test (SPT). However, a comparison between the values of such a strength determined by both tests in CL, CL-ML and CH soils shows that it does not exist an approximate relationship. In any case it is remarkable that values of the test conducted in the laboratory fit between the lower and the higher ones calculated from the standard penetration number. This is very important for those geotechnical reports in which the unconfined compression strength is only based on the SPT. In this way, if the lower value is taken to evaluate the ultimate soilbearing capacity the result will not be very accurate but it will probably be by the side of safety
Resumo:
Estudi morfològic de la Costa Brava
Resumo:
S’analitza la formació de la ‘Pedra Alta’, a Sant Feliu de Guíxols, a partir de les característiques morfològiques, macroscòpiques, microscòpiques i tectòniques
Resumo:
It is a contribution to the study of the terraces of the river Ter along its mid-course in the town of Girona, since that is the last speace where it is still possible to observe four of these terraces with clear characteristics of climatical deposition. Itsmorphological peculiarities are described as well as the morphometrical and lithological parameters of its pebbles. These terraces are compared with others which have been studied in other areas of the regions and conclusions are drawn concerning deposition, source àrea and chronology
Resumo:
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
Resumo:
The behaviour of 21 natural springs in a granític massif is studied in this survey. Geomorphological features of the zone are described as well as water circulation and rising 25 parametres of each of them are analysed ans conclusions are withdrawn regarding geological conditions of rising, course, chemism and potability
Resumo:
The Bac Grillera nappe (Prepirenean of Girona) shows a stratigraphic section composed of two unconformi ty-bounded units. The lower unit is composed by rethian (marly limestones) and liassic (brechoid marly limestones and limestones). The upper unit (sandstones and marly limestones) belongs to the upper Cretaceous (Campanian)
Resumo:
Sobre els mapes del medi natural terrestre que aglutinaran els trets del rocam, la disposició dels materials i les seves formes i que reuniran la informació suficient per poder ser utilitzats per als estudis sobre la prevenció de la contaminació
Resumo:
Ressenya del llibre 'La Vall de Llémena' d' Albert Pujadas i Pigem, editat per la Diputació de Girona dins la col·lecció 'Els Espais Naturals de les Comarques Gironines' i publicat l'any 1995 i en el que s'ofereix un material didàctic-educatiu als professors d'ensenyament secundari
Resumo:
Ressenya del llibre 'Itinerari geològic de Banyoles : descoberta del funcionament del sistema lacustre' de David Brusi, Joan Bach i Miquel Sanz, editat per l' Ajuntament de Banyoles i Eumo Editorial l'any 1990
Resumo:
Descripció del volcà anomenat 'Palou' a 1Km. al Sud d' Amer
Resumo:
Descripció del sistema càrstic de Sant Martí de Llémena
Resumo:
With the aim of radiocarbon dating Llora travertines, chemical and isotopic data of strearn water and present travertines have been analyzed. The purpose is to determine the radiocarbon activity of present travertines in order to assign an initial radiocarbon activity to the old ones. Applying this methodology we conclude that travertines are from Holocen age around 4.000 years BP