Prehistory of Transylvania Prehistory of Transylvania The Prehistory of Transylvania describes what can be learned about the region known as Transylvania through archaeology, anthropology, comparative linguistics and other allied sciences. Transylvania proper is a plateau or tableland in northwest central Romania. It is bounded and defined by the Carpathian Mountains to the east and south, and the Apuseni Mountains to the west. As a diverse and relatively protected region, the area has always been rich in wildlife, and remains one of the more ecologically diverse areas in Europe. The mountains contain a large number of caves, which attracted both human and animal residents.
1537 Transylvania 1537 Transylvania 1537 Transylvania, provisional designation , is a carbonaceous asteroid and long-lost minor planet from the outer regions of the asteroid belt, approximately 17 kilometers in diameter. Discovered by Gyula Strommer in 1940, it was later named after region of Transylvania, where the discoverer was born. "Transylvania" was discovered on 27 August 1940, by Hungarian astronomer Gyula Strommer at the Konkoly Observatory near Budapest, Hungary. Observations of the asteroid continued at Konkoly until February 1942. It became a lost minor planet until Spring 1981, when astronomer Leif Kahl Kristensen at the University of Aarhus rediscovered it based on contemporary