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) Siege of Breda (1624) The Siege of Breda of 1624–25 occurred during the Eighty Years' War. The siege resulted in Breda, a Dutch fortified city, falling into the control of the Army of Flanders. Following the orders of Ambrogio Spinola, Philip IV's army laid siege to Breda in August 1624. The siege was contrary to the wishes of Philip IV's government because of the already excessive burdens of the concurrent Eighty and Thirty Years' wars. The strategically located city was heavily fortified and strongly defended by a large and well prepared garrison of 7,000 men, that the Dutch were confident