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
Capture of Breda (1590) conditions of the surrender of the city, that was decided according to the following terms: The taking of Breda on the part of the Dutch and English troops, a city in the eyes of the Spaniards that was assumed to be safe, was a disagreeable surprise for the Spanish authorities. The Duke of Parma - Alexander Farnese was enraged by the cowardice of the Italian troops in charge of the defense of the city. He ordered three captains responsible for the garrison of Breda to be executed and a fourth official was expelled from the army. Finally the recriminations ended