Lake Sobygaard, Denmark : a shallow lake in recovery after a reduction in phosphorus loading in Shallow lakes environment. (L'environnement des lacs eutrophes)
A Balaton idegenforgalmanak néhany jellemzoje. (Main features of tourism around Lake Balaton)
As Lake Balaton has strengthened its position in the geographical distribution of Hungarian tourism it is absolutely necessary to determine the balance between the receptional capacity and the actual number of guests received and to urge early
restrictions in order that the lake could preserve its place in tourism. (CK).
Administration ; Conflit ; England ; Géographie de l'Europe ; Lake District National Park ; Marché immobilier ; Office public ; Parc naturel ; Politique du logement ; Pouvoir local ; Royaume-Uni ; Résidence secondaire
L'existence de nombreuses résidences secondaires dans le Lake District National Park est à l'origine de deux politiques de logement. L'A. pose le problème d'intervention sur le marché libre immobilier par la planification et de la résolution
Physical geographic conditions of the natron lakes of the Kiskunsag National Park
Natron lakes cover an about 10 km area in the western part of the structural valley of the Danube on the Danube-Tisza Interfluve. Blow-out depressions form their floors. Their isolation is a consequence of human intervention into landscape
. The chemical properties of the lakes are in close correlation with climatic features (evaporation). (DLO).
Freeze-up and break-up of lakes as an index of temperature changes during the transition seasons : a case study for Finland
The statistical relationships between lake freeze-up/lake break-up dates and air temperatures means over various time periods are analyzed for 63 lakes in Finland. Freeze-up/break-up dates provide a useful proxy for air temperature estimates in data
Lake Rimigliano, located on the coastal plain of Tuscany was dried out in the first half of the 20th century. The paper presents the unpublished description of the old lake given by Paolo Savi. A recent geological and morphological study of the lake
has led to hypotheses that differ from earlier accounts: Lake Rimigliano acted as a coastal barrier lake only along its lower transverse stretch, near the sea. The entire length was filled during the rise in sea-level that followed on the last period
A Balaton kialakulasa. (The origin of Lake Balaton)
The AA., on the basis of their recent geomorphological studies, consider Lake Balaton to be a polygeneous depression formed by sinking periodical both in space and time. Its slow sinking started in the Riss, became more active in the Würm, mainly
De Zevenambachtspolder of Nieuwkoopse droogmakerij, een negentiende-eeuws staatsproject van formaat. (Lake reclamation in the nineteenth century: the Zevenambachtspolder)
The lake reclamation of the nineteenth century stands on whole in bad repute in relevant literature. The lake reclamation (1797-1812) of Nieuwkoop doesn't fit into this existing negative image. Except for some short periods with draining problems
A morahalmi Madarasz-to foldtani és vizfoldtani viszonyai. (The geological and hydrogeological conditions of Lake Madarasz near Morahalom)
Boreholes indicate that the loess surface sinks below 10 m towards the west and partly retains groundwater percolating in the direction of the eastern slope. This is the origin of the parallel waterlogged depressions, among them of the Lake Madarasz
. The lake shores are favourable for recreation and angling sites, a proposal is made for appropriate utilization. (DLO).
Radiocarbon dating of transitions between marine and lacustrine sediments and their relation to the development of lakes
at isolation/ingression contacts for lakes of the same altitude above present sea-level. The dating errors are connected to periods with more oligotrophic conditions with isoetides. The isoetide vegetation and the dating errors disappear when the lakes become