Breda Formation whale bones were found), the Zenderen Member (green, glauconiferous fine sand) and the Delden Member (sandy, glauconite and goethite bearing clay and loam. The Breda Formation corresponds largely with the Berchem Formation of northern Belgium. Breda Formation The Breda Formation (; abbreviation: BR) is a geologic formation in the subsurface of the Netherlands. The formation consists of marine glauconiferous sands and clays that were deposited during the Miocene epoch. Although the formation is not very rich in fossils, sometimes bones of fishes, mammals ("Leptophoca cf. proxima", "Protophocaena minima"), shells and shark teeth (a.o of Megalodon) are found. The Breda Formation
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