Morphology and Dynamics of a Major Anastomosing Channel     System Riverine Plain, Australia
{'Code': '06030101', 'Directorate': {'Abbreviation': 'GEO', 'LongName': 'Directorate For Geosciences'}, 'Division': {'Abbreviation': 'EAR', 'LongName': 'Division Of Earth Sciences'}}
{'SignBlockName': 'John A. Maccini'}
Morphology and Dynamics of a Major Anastomosing Channel                    System Riverine Plain, Australia                                                     The Murray River is of hydrologic, geomorphic and                          sedimentologic interest because as it approaches the Cadell Fault               it bifurcates, and a major anastomosing-stream  develops on the                 alluvial Riverine Plain of southeastern Australia.  In this area                it  will be possible to study the characteristics of and reason                 for the deveolpment of anastomosing channel network and to                      determine if active tectonics is actively causing increased                     frequency of overband flooding and the problems of channel                      stability.                                                                           The study will determine how the morphological and                         sedimentary character of anastomosing system differs in channels                as well as factor in the local and regional tectonic effects.
{'FirstName': 'Stanley', 'LastName': 'Schumm', 'EmailAddress': 'stans@mussei.com', 'StartDate': '02/15/1988', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
{'Name': 'Colorado State University', 'CityName': 'Fort Collins', 'ZipCode': '805232002', 'PhoneNumber': '9704916355', 'StreetAddress': '601 S Howes St', 'CountryName': 'United States', 'StateName': 'Colorado', 'StateCode': 'CO'}
{'Code': '1571', 'Text': 'SCEC'}
{'url': 'https://www.nsf.gov/awardsearch/download?DownloadFileName=1987&All=true', 'xml': '8712287.xml'}