Breda Formation Formation. The Breda Formation can be a couple of meters to (in the Roerdal Graben) more than thick. The top is formed by an erosional nonconformity in the south and east of the Netherlands. In the west the contact with the Pliocene Oosterhout Formation is more gradual. In the Roerdal Graben the mostly Pliocene Kiezeloolite Formation is sometimes on top of the Breda Formation. Locally the Breda Formation can be subdivided into members: the Aalten Member (silty calcareous clay, rich in shells), the Eibergen Member (clay alternating with thin sand layers, with a basal conglomerate in which shark teeth and
NAC Breda area, NAC were forced to move. "Period: 30 August 1931 – 1 August 1940." Due to the City Council’s decision to zone the grounds of ‘t Ploegske as a residential area and the city of Breda had no new grounds available, NAC were forced to move out Breda. The town of Princenhage offered NAC a terrain, where NAC built a state-of-the-art stadium with a capacity of 5,500. The main disadvantage was that the stadium was located far from Breda’s city centre. Nevertheless, NAC’s golden decennium in the thirties, when NAC was considered to be one of the top clubs in