The Breda Formation was deposited in the shallow sea that covered the Netherlands during the Miocene. It is mostly on top of the Oligocene clays of the Rupel Formation or late Oligocene sands and clays of the Veldhoven Formation. The Breda Formation can be a couple of meters (in the Roerdal Graben) to more than 700 metres (2,300 ft) thick. The top is formed by an erosionaldisconformity in the south and east of the Netherlands. In the west the contact with the PlioceneOosterhout Formation is more gradual. In the Roerdal Graben the mostly Pliocene Kiezeloolite Formation is sometimes on top of the Breda Formation.