Geological mapping using Landsat Thematic Mapper imagery in Almeria Province, South-east Spain in Special issue : Advances in geological remote sensing.
Geologic and topographic features of the Maritime territory control the loose material volume which comes from slopes to valleys floor as well as conditions of channel deformations development and floodplain-forming processes. Three types and eleven
sub-types of curves of the channel-forming discharges are distinguished according to geologic and geomorphic conditions of the drainage basins and order of streams. The data obtained permit to approach prognosis of changes in rivers channel-forming
layer reworked each year is 0.2 to 0.7 mm (up to 73.7 mm per year if ploughing effect is taken into account) which surpasses by far the total effect of all the rest geologic and geomorphic factors. - (L'A.).
geological past, the development of extensive truncation surfaces was increasingly restricted and superseded by the development of parapediments and by the accentuation of structural landforms.
The paper deals with the relationship of the relief to geological structure of the Murmansk Massif which is a large morphostructure at the NE Kola Peninsula and corresponds to the continental part of the Murmansk tectonic block. Analysis
Three subzones of different age are distinguished within the zone of neotectonic deformations at the Southern Khibini on the basis of space photoes and geological-geomorphological data. The zone as a whole is associated with the large regional
17 geological survey and supplementary studies made it possible to classify the remains of Pleistocene sandgravel terraces of the Weser River between Gieselwerder and Hehlen. Eleven terraces can be distinguished : the youngest (loess-free lower