The Fort Beauséjour road and the relict of the base of a running dyke located below the Fort. A running dyke is a dyke that stretches from one aboiteau to the next aboiteau.Cut sods ("parements" ) on the base of an old dyke on the Tantramar Salt Marsh.Hatvany, Matthew G. (2002). The Origins of the Acadian Aboiteau: An Environmental-Historical Geography of the Northeast. Historical Geography 30, Also available at http://www.historical-geography.net/volume_30_2002/hatvany.pdf. Hatvany, Matthew George. 2003. Marshlands : four centuries of environmental change on the shores of the St. Lawrence, Aboiteaux of Kamouraska. Sainte-Foy, Quebec : Presses de l'Université Laval. Rippon, Stephen. 2000. The transformation of coastal wetlands : exploitation and management of marshland landscapes in North West Europe during the Roman and medieval periods, British Academy postdoctoral fellowship monograph. Oxford ; New York: Oxford University Press. Rippon, Stephen, Nigel Cameron, and Council for British Archaeology. 2006. Landscape, community and colonisation : the north Somerset levels during the 1st to 2nd millennia AD. York: Council for British Archaeology. Sebold, Kimberly R. (1992) FROM MARSH TO FARM: The Landscape Transformation of Coastal New Jersey. National Park Service, [cited 7 July 2010. Available from http://www.nps.gov/history/history/online_books/nj3/contents.htm. |