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
Sant Salvador, Breda Sant Salvador, Breda Sant Salvador de Breda is a parish church and former Benedictine monastery in Breda, Province of Girona, Catalonia, Spain. Very little of the original Romanesque architecture remains. The 11th-12th century bell tower, reconstructed later, is the best preserved building. It is a slender tower, in height, and rectangular in shape. It consists of five floors with windows in the top four. The Gothic-style church, built between the 14th and 16th centuries, serves as parish church. It has a late Romanesque cloister which was partially destroyed in 1877. Annexed to the cloister is an ancient abbey house with