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  • Fluvial palaeohydrology : the morphometric contribution
  • The use of morphometric parameters in tectonic geomorphology (on the example of the Western Beskydy Mts.)
  • The application of some morphometric parameters for morphometric research of the culmination area of the outer Western Carpathians. Potential zones of neotectonic activity are delimited. - (MS)
  • The morphology of the Aegean Sea: a discussion of morphometrical data
  • Morphometric features of drumlins in Western Pomerania
  • In connection with the large number and regular shape of drumlins within particular fields, many students have used morphometric and geometric methods in order to find similarities in the features and in the spatial distribution of forms
  • . On the basis of the measurements of six morphometric parameters of drumlins in Western Pomerania, regions were defined having concentrations of the forms having similar features within one field, from the analysis of the frequency of occurrence. Besides, from
  • multiple regression analysis it was possible to define such independent variables as individual features of drumlins. The morphometric analysis used was treated as an initial stage for further field investigations in order to explain the morphogenesis
  • Morphometric controls and geomorphic responses on fans in the Southern Alps, New Zealand
  • Morphometric variables associated with 41 debris-flow and 18 fluvial fans and their basins in the Southern Alps of New Zealand are examined. The specific objectives are to test for significant differences between debris-flow and fluvial fans
  • and determine which morphometric variables can best differentiate the fans according to process; to investigate the relations between some morphometric variables at each type of fan; to attempt to explain the results of the morphometric analyses on the basis
  • of the underlying processes; and to explore the usefulness of morphometric thresholds for identification of debris-flow potential on fans.
  • Fractals and morphometric measures : is there a relationship?
  • This paper examines the application of fractal concepts to geomorphometry. The correlations between the fractal dimension (D) and the 24 traditional morphometric parameters used in this study are all very weak. This suggests that the fractal
  • Morfometrické charakteristiky sklonove asymetrickych udoli vybranych uzemi severni Moravy. (Morphometrical characteristics of valley asymmetry in some North Moravian regions)
  • The study deals with morphometrical data on asymetric valleys in the regions of Nizky Jesenik highland, Moravian Gate and hilly land of Hlucin in Northern Moravia and Silesia. Especially is shown the dependance between the index of asymetry
  • A comparison of two river basins, the Limnitis and Evdhimou, using the water balance and drainage basin morphometric techniques
  • Spatial scale and drainage basin morphometric interaction
  • Aeolian dust ripples : their occurrence, morphometrical characteristics, dynamics and origin
  • In this paper, the main morphometric and dynamic properties of aeolian ripples formed in a wind tunnel during the deposition of natural, silt-sized dust particles over a flat horizontal surface are investigated. Two different (but counteracting
  • Variability of the morphometric characteristics of valley networks caused by variations in a scale
  • This article indicates the quantitative tools, with assistance of which it is possible to characterize the morphology (shape) of the valley network and determine their variability caused by the scale change. The monitored morphometric
  • The use of GIS-based digital morphometric techniques in the study of cockpit karst
  • The Cockpit Country is the type area for cockpit karst landforms. A detailed analysis of cockpit karst terrain is carried out using the latest GIS-based digital morphometric techniques in order to assess the nature of such terrain and provide
  • High-magnitude landslide events on a limestone-scarp in central Germany : morphometric characteristics and climatic controls
  • parameters of different temporal scales (annual rainfall to extreme short-time rainfall events) are analyzed in the context of the given morphostructural, morphometric and geological setting.
  • Morphometric analysis of the drainage network in the Modena and Reggio Emilia Apennines (Northern Italy)
  • basins of central Italy. The aim of the research is to carry out a preliminary morphometric characterisation of the Emilia Basin that, if supported by sample monitoring, should allow the correct management of these fluvial basins. - (NF)
  • Morphometric controls and basin response in the Cascade Mountains
  • Morphometric variables associated with 36 debris torrent, 78 snow avalanche, 45 composite debris torrent and snow avalanche and 14 streamflow basins in the Cascade Mountains of southwestern British Columbia, Canada are examined. The results show
  • different nature of these processes. The AA. explore the usefulness of selected morphometric characteristics for preliminary identification of debris torrent hazard.
  • The identification of debris torrent basins using morphometric measures derived within a GIS
  • The aim of this study is to explore the potential of DEM-derived morphometric measures within a GIS to advance the identification of drainage basins subject to debris torrent activity. Logistic regression and discriminant analysis indicate
  • that the standard deviations of slope gradient and slope aspect are the strongest predictors of the variables tested. The results suggest that important morphometric indicators of debris torrent activity can be derived from DEMs, thus providing a systematic basis
  • Geomorphology and structure of the Bear River Range, north eastern Utah: a morphometric approach
  • Morphometric investigation of dolines in Bükk mountains
  • New morphometrical parameters for explanation of karst development
  • Areas of land-cover forms and calculation of their morphometric parameters
  • Selected vector quantitative methods evaluate areas or regions. Calculations of spatial morphometric parametres, namely of frequency, area and circumference, spatial orientation of a region are presented. The mentioned methods are shown