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  • Longitudinal changes in size and sorting of stream beds material in four English Rivers
  • Effects of the introduced wild English rabbit on the vegetation of central Australia. - (DWG)
  • Dictionary of earth science. English-French. French-English=Dictionnaire des sciences de la terre. Anglais-Français. Français-Anglais.
  • Airborne Thematic Mapper ; English Channel ; Géographie physique ; Infrarouge thermique ; Océanologie ; Royaume-Uni ; Température de la mer ; Télédétection
  • Les données ATM ont servi au calcul des températures de surface de l'ouest de l'English Channel. L'analyse des données infrarouges thermiques sont confrontées aux structures turbides et aux mesures sur bateau (boat trial). Aborde le problème de la
  • The Wolstonian stage of the British Pleistocene in and around its type area of the english Midlands
  • Modification of heavy mineral assemblages in english coversands by acid pedochemical weathering
  • Urbanization and natural Stream channel morphology: the Case of two English new towns in Man's impact on the hydrological cycle in the United Kingdom.
  • Typological classification of karren. The main types and subjoins the Czech, English, French, German, Spanish and Russian terms of these corrosional microforms of the karst surface. (MS).
  • Waterspouts in the English Channel
  • Télédétection des structures turbides en Manche. (Remote sensing of turbidity in the English Channel)
  • The authors give a regional classification of the individual glacialmorphological forms. The most important glacial relief forms of G.D.R. and Poland are adequatly discribed. There are given the special terms in German, Polish and English. - (IH)
  • of the last glacial age| and 3. humidity changes at the Japan Sea side of Japan in Postglacial Times. The 16 papers given are in Japanese with abstracts and figure captions in English. (P.A. Pirazzoli).
  • , and Razorbills due to oil pollution in the English Channel is emphasized.
  • and English Channel areas to the northeast. The sub-sedimentary structure between the Meriadzek Terrace and the Trevelyan escarpment is of continental origin having a block-faulted pattern and is interpreted as a southwestward prolongation of the continental