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  • A comparison of bunter sandstone scarps in the Black Forest and the Vosges in Landforms and landform evolution in West Germany.
  • This paper concentrates on a description of scarps in two structurally and lithologically comparable areas : the Kniebis area of the Black Forest and the Donon area of the Vosges. Differences in the geomorphodynamics can be attributed to differences
  • Discussion of methods and techniques for the quantitative description of landforms particular in high mountains and application of these methods to several digital elevation models of the Turtmanntal in Valais. The absence of adequate methods
  • for the parameterisation of complex landforms is particularly evident for high mountain landforms. Therefore this study wants to contribute methodologically and in application to the description of geomorphometric structure in high mountain environments. - (IFL)
  • Classroom simulation of small-scale solutional landforms
  • Description of a classroom experiment to illustrate terrain-forming processes. - (DWG)
  • Following the description of evolution history, the mountainous landforms (6 volcanic subtypes and 4 non-volcanic subtypes) and the hill and basin landforms (4 various subtypes) are presented and mapped in the two north Hungarian Mountains. (DLO).
  • Landform replication experiments on quarried limestone rock slopes in the English Peak District
  • This paper describes the land surface changes resulting from limestone quarrying and considers the nature of landform evolution on quarried limestone rock slopes. This is followed by a description of a new technique known as restoration blasting
  • and its application in a serie of landform replication experiments.
  • Landforms and structures of the waterlain west end of St. Thomas moraine, SW Ontario, Canada
  • St Thomas moraine is one of the late Wisconsinan recessional moraines in southwest Ontario and is waterlain. Description of the visible St. Thomas moraine with the mesoform ridges. Description of Lake Erie bluff section and correlation of Lake Erie
  • Geomorphogenesis ; Geomorphology ; Hungary ; Karst ; Karstic landform ; Typology
  • A geological and geomorphological description of the open karst regions of Hungary. - (JS)
  • Description of four lesson places for use in primary schools to teach geographical concepts related to landforms. - (DWG)
  • Following an outline of palaeogeography, author gives an overall geomorphological description and map of the landscape. The landforms are primarily controlled by fluvial accumulation, derasion and tectonic processes. (DLO).
  • Données sur l'évolution des dolines du karst anthigène, allogène et couvert avec utilisation de ses fonctions descriptives
  • Doline ; Geomorphogenesis ; Hungary ; Karst ; Karstic landform ; Landform evolution ; Mathematics ; Romania
  • representation of the real land surface. This can be achieved by the use of Digital Elevation models. The power of this tool is demonstrated by some examples in landform description, landform analysis and spatial modelling.
  • Erosion surface ; Erosion surfaces ; Landform description ; Landform evolution ; Monographs
  • Late quaternary landforms and environmental change in northwest Botswana: the evidence of Lake Ngami and the Mababe Depression
  • Evolution du Lac Ngami, partie du Paléo-Makgadikgadi, et variations du niveau lacustre| connexion avec la dépression de Mababe. Description des formes du relief et des stages| chronologie. Delta de l'Okovango, Botswana.
  • The A. presents a geomorphological description about the landforms of the badland areas of Alberta province, Canada. - (JS)
  • Alluvial cone ; Cold desert ; Front moraine ; Geomorphology ; Ice sheet ; Periglacial landform ; Poland ; Sandur
  • The main result of this study is detailed description of some classical, described by Schwarzbach, and some new sections. - (Equipe IH)
  • Hydrogeology ; Karst ; Karstic landform ; Polje ; Pollution ; Portugal ; Water pollution
  • Description du poljé de Minde et de son évolution géomorphologique. Analyse des problèmes de pollution des eaux du poljé. - (DBF)
  • Description d'une surface de karstification verticale
  • Dating ; Geomorphology ; Karst ; Karstic landform ; Karstification ; Model
  • In this paper the terminology used in long-term geomorphology is evaluated. Long-term geomorphology is the study of landforms that are mostly pre-Quaternary, Cenozoic, Mesozoic or even Palaeozoic age. Many terms have been introduced to name the long
  • -term scale landforms that persist to the present. The definitions of many of these terms are ambiguous, have changed over time, and their use and meaning is consequently often unclear. An attempt is made to clarify definitions. Long-term geomorphology
  • deals in great parts with the lowering of a land surface to the base level (mostly sea level), leaving a new land surface. The largest group of terms concerns descriptions and genetic models for these kinds of new land surfaces collectively called base
  • level surfaces here. Other terms dicussed here relate to relict and preglacial landforms and regional terms for stepped surfaces. Terminology is discussed with particular reference to examples from and its use in Scandinavia. Scandinavia is unique
  • in the respect that pre-Quaternary landforms were repeatedly covered by Quaternary ice sheets but often survived with different degrees of glacial modification.
  • The relationship between geology and landforms along a coastal mountain front, Northern Calabria, Italy
  • processes operative in a Mediterranean climate. The AA. provide a detailed description of the geomorphologic elements; however, their effort was dedicated mostly to the fans because their history may offer clues for the understanding of the recent
  • Jotunheimen Research Expeditions, Contribution No. 84. Boulder-paved river channels : a case study of a fluvio-periglacial landform
  • Résultats d'une approche quantitative, analytique et sédimentologique adoptée pour l'étude d'un lit fluvial façonné par une combinaison unique de processus fluviaux et périglaciaires dans l'étage alpin de Jotunheimen. Description morphologique du