The spatial distribution of low flows in Poland not exceeded at an assumed probability
This paper presents the results of a fitting of most frequently-applied probability distributions to a series of minimum yearly flows. Specifically, the series of minimal annual discharges derived from 119 stream gauges located throughout Poland
and relating to the period 1971-1990. The main task was to adjust one of the probability distribution functions applied most frequently. Maps generated provide for the identification of several regularities.
Cartografía de zonas probables de salida de aludes en el Alto Gállego (Pirineo Central Aragonés) mediante el empleo de Sistemas de Información Geográfica
Cartographie des zones probables de départ d'avalanches dans le Alto Gallego (Pyrénées centrales aragonaises) au moyen de Systèmes d'Information Géographiques
Les AA. étudient les zones probables de départ d’avalanches dans la vallée du Alto gallego (Pyrénées centrales aragonaises) à partir d’un Système d’Information Géographique. Pour ce faire, ils utilisent les facteurs suivants : l’altitude mensuelle
Cartografía de zonas probables de salida de aludes en el Alto Gállego (Pirineo Central Aragonés) mediante el empleo de Sistemas de Información Geográfica
Cartographie des zones probable des départs d'avalanches dans le Alto Gallego (Pyrénées centrales aragonaises) au moyen de Systèmes d'Information Géographique
Les AA présentent une cartographie des zones probables de départs d’avalanches dans la vallée du Alto Gallego (Pyrénées centrales aragonaise) au moyen de SIG. Pour ce faire, ils utilisent comme mesure la variation mensuelle de l’isotherme 0 (de
Les AA. décrivent des structures sédimentaires observées à proximité du village de Terreti (Calabre) dans des dépôts plio-pléistocènes. Leur très probable lien avec l’intense activité sismique locale et régionale est ensuite confrontée aux autres
processus pouvant déclencher la formation de telles structures. Des structures en bol et des fentes y sont observées ; il s’agit probablement de sismites au sens strict du terme, présentant un lien indirect avec l’activité sismique régionale qui aurait été
An analysis of the statistical distribution of event soil loss was carried out using the data collected in the period 1999–2008 at the microplots and plots of the Sparacia experimental area (Sicily, Italy). In particular, the theoretical probability
actuelle du finage de cette commune de Bourgogne est un héritage, probablement une construction médiévale et moderne adossée à une potentialité antique. Les opérations foncières successives se sont coulées dans le moule planimétrique préexistant.
. The AA. demonstrate here that lithalsas were formed only on weathered quartzitic rocks of the Cambro-Ordovician massif of Stavelot, and probably are associated with local hydrological conditions.
similarity between the samples collected from the occurrences. In the environment of both locations some boulders are found composed of quartzite. In the opinion of the author these boulders were very probably transported by floating frozen ice floes. - (AM)
mapping. The author concluded that on the basis of geological considerations and geophysical measurements an anthropogenic origin seems to be most probable. - (AM)
fans in the northern, western and south-eastern foreland of the Mátra Mountains and from alluvial fans of the Sajó and Hernád Rivers as well as probably of the Maros River. The distribution of boulders and their deposition pattern point to fluvial
Italy plans to erect two gas terminals (LNG terminals) in immediate vicinity of the Slovenian state border. No cross-border impact is indicated in the reports produced by the Italian side, despite high probability of cross-border impacts. The paper
to avoid the endogeneity problem associated with designating PFA, probability of being PFA for each census tract is estimated using a probit model. Residential parcel development continues to expand at the outside of the PFA in the smart growth era.
Cu and Cd, 2) to delineate areas with a high probability of exceeding critical sanitation thresholds, and 3) to determine the potential sources responsible for the identified patterns. Mostly areas with known industrial activities (such as lead
characteristics. The author's primary objectives are to present some physical and chemical symptoms of meromixis at selected localities, to discuss the mutual interaction between the physical and chemical characteristics of lake water and to explore some probable
. Facito area. It is possible to distinguish synsedimentary, synorogenic and postorogenic mélange. The abundance of mélanges in the outcrops of Mt. Facito fm. probably lead to misinterpret it as a unique, huge olistostroma.- (NF)
with the structure of the Tuscan Metamorphic «basement», in terms of geometry, stacking pattern and timing, suggesting a probable common structural evolution even if a different structural levels. - (NF)