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
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