Dit rapport presenteert de resultaten van deze analyses, waarbij een belangrijk eindproduct gevormd wordt door de hoger vernoemde erosie/sedimentatie-kaarten. Deze resultaten worden in dit rapport bondig besproken, daar waar mogelijk wordt gewezen op een mogelijke oorzaak van de waargenomen trend (baggeren, storten, invloed van harde structuren zoals strandhoofden). Een van de opvallendste resultaten is de waarneming van een erosietrend van de vooroevervoet (waar de steilere vooroever overgaat in de vlakkere zeebodem) op verschillende locaties langsheen de Belgische kust.
Naast de resultaten wordt in dit rapport ook uitvoerig aandacht besteed aan de technische kant van de uitgevoerde analyses: niet alleen wordt de methodologie toegelicht (kort geformuleerd komt de trendanalyse neer op een enkelvoudige lineaire regressie met kleinste-kwadratenbenadering van de dieptewaarden (morfologische trendanalyse) of volumes (volumetrische trendanalyse)), maar eveneens wordt aangegeven hoe de methodologie geïmplementeerd kan worden in ArcGIS software. Als dusdanig zijn delen van het rapport op te vatten als mogelijke leidraad voor het uitvoeren van morfologische trendanalyse m.b.v. 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