Matches in DBpedia 2015-10 for { ?s ?p "'Earth Surface Processes and Landforms' is the journal of the British Society for Geomorphology (BSG), formerly the British Geomorphological Research Group (BGRG) and is an international journal of geomorphology, publishing on all aspects of Earth Surface Science. The journal was founded in 1976 as Earth Surface Processes and obtained its present name in 1981. The Journal primarily publishes original research papers that will have a sustained impact upon geomorphological science and cognate disciplines. It also publishes Earth Surface Exchanges which include commentaries on issues of particular geomorphological interest, discussions of published papers, shorter journal articles suitable for rapid publication and specially-commissioned reviews on key aspects of geomorphological science. Foci include the physical geography of rivers, valleys, glaciers, mountains, hills, slopes, coasts, deserts, and estuary environments, along with research into Holocene, Pleistocene, or Quaternary science."@en }
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- Earth_Surface_Processes_and_Landforms abstract "'Earth Surface Processes and Landforms' is the journal of the British Society for Geomorphology (BSG), formerly the British Geomorphological Research Group (BGRG) and is an international journal of geomorphology, publishing on all aspects of Earth Surface Science. The journal was founded in 1976 as Earth Surface Processes and obtained its present name in 1981. The Journal primarily publishes original research papers that will have a sustained impact upon geomorphological science and cognate disciplines. It also publishes Earth Surface Exchanges which include commentaries on issues of particular geomorphological interest, discussions of published papers, shorter journal articles suitable for rapid publication and specially-commissioned reviews on key aspects of geomorphological science. Foci include the physical geography of rivers, valleys, glaciers, mountains, hills, slopes, coasts, deserts, and estuary environments, along with research into Holocene, Pleistocene, or Quaternary science.".