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
Siege of Breda (1624) Spain wanted to have a strong position in potential peace negotiations. The conquest of Breda would enable Spain to put forward stronger demands concerning religious freedom for Catholics in the Republic and lifting the blockade of the Scheldt. Breda was one of the strongest cities in the defence of the Republic between the States of Holland and royal Brabant. The city was strategically located on a navigable river, Mark, and near several roads. Henry III of Nassau, Lord of Breda from 1509 to 1538, had been commissioned by Charles V to travel through Europe. In Italy, he came into contact