Formerly, the gate was called in Latin: Porta Hungarica and in Hungarian: Dévényi kapu.
In a wider sense it begins below Bratislava Castle (in which case the gate is 11.5 km long and 2 to 7 km wide) and in a narrower sense it begins below Devín Castle. It ends near Hundsheimer Berg, the highest peak of the Austrian Carpathians at 480 meters AMSL, in Austria on the right bank of the Danube. To the east, it borders another natural gate, the Lamač Gate.
Geologically, Devín Gate was created during the Pleistocene epoch. A large part of its core consists of granite massifs from the Carboniferous period. It also features limestones and dolomites from the Cenozoic era. Neogene period sediments include conglomerates, gravels and others. On the Upper Danube, comprising the section between the springs where the river begins and Devín Gate upstream of Bratislava, the extension of the morphological floodplain is smaller as compared to the rest of the river.4
dubious
Neolithic farmers settled in the area approximately 5000 - 3500 BC, establishing continuous human settlement which lasts until present time.5
48°10′30.29″N 16°58′42.96″E / 48.1750806°N 16.9786000°E / 48.1750806; 16.9786000
Britannica: Hungarian Gates https://www.britannica.com/place/Hungarian-Gates ↩
International Commission for the Protection of the Danube River (ICPDR): Danube Basin/River Basin, Section: Middle Basin https://www.icpdr.org/main/danube-basin/river-basin ↩
"Vyhliadková plavba: Tri hrady v Devínskej bráne". panorama.sk. Retrieved 3 July 2012. http://www.panorama.sk/sk/sprievodca/vyhliadkova-plavba-devinska-brana/2218 ↩
Schneider, Dister and Dopke, 2009 ↩
"NPR Devínska Kobyla". geomuz-devkob.blogspot.sk. Retrieved 3 July 2012. http://geomuz-devkob.blogspot.sk/ ↩