{"refrec":{"BRefID":27094,"RR":"<b>Ameryckx, J.</b> (1952). Ontstaan en evolutie van het Zwin in België. <i>Natuurwet. Tijdschr. 34(4-5)</i>: 99-110","BEntID":27094,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":". <i>Natuurwet. Tijdschr. 34(4-5)</i>: 99-110","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":1,"TerrestrialFlag":0,"Authorstring":"Ameryckx, J.","OrigTitleTranslFlag":1,"Authorstringtrunc":"Ameryckx, J.","Englishabstract":null,"AbstractOtherLang":"Après quelques brèves considérations sur la littérature concernant l'histoire du Zwin, l'auteur traite les points suivants : 1. <i>Endiguements</i>. Une étude détaillée des endiguements, indispensable pour pouvoir suivre l'évolution du Zwin, a été faite. Le Zwin a été formé au Xme siècle au cours de la transgression dunkerquienne III A. Les endiguements commencés au XIIme siècle ont diminué progressivement l'étendue de son aire d'inondation; aujourd'hui il n'en reste qu'une schorre de quelques centaines d'hectares à la frontière belgo-hollandaise. 2. <i>Cours d'eau principaux</i>. Une mise au point a été faite en ce qui concerne la distinction entre les cours d'eau naturels et artificiels. 3. <i>Ruptures de digues</i>. 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