Location of the Buda Hills proper (Budai-hegyek) within physical subdivisions of Hungary. The Buda Hills in broader sense (Budai-hegység) include also southerly situated Budaörs and Budakeszi Basin (Budaörsi- és Budakeszi-medence) and Tétény Plateau (Tétényi-fennsík).
During the period from the terminal Cretaceous to Priabonian, the area was a karstic terrestrial environment displaying distinct relief differences. It was also the time when Triassic formations were eroded. The continental period (ended by the transgression in Late Eocene) was characterized by the formation of small fans at the slope foot. The fans contained substantial quantities of andesiteclasts thanks to the fans' close location to the andesite source rocks. The clasts could have been then transported by periodic streams along the valleys. The Late Eocene transgression reworked accumulated terrestrial sediments.[6]
Juhász Árpád [in Hungarian] (1988). dr. Gál Éva: A budai hegyvidék. Képzőművészeti Kiadó. Képzőművészeti Kiadó. ISBN 963-336-436-1.
Magyarország kistájainak katasztere. Szerk.: Dövényi Zoltán. MTA Földrajztudományi Kutatóintézet. Budapest. 2010. ISBN 978-963-9545-29-8.{{cite book}}: CS1 maint: location missing publisher (link)
Dr. Pápa Miklós [in Hungarian] (1956). Budai hegyek útikalauz, Sport Lap- és Könyvkiadó. Budapest. Archived from the original on 2020-10-22. Retrieved 2020-06-10.{{cite book}}: CS1 maint: location missing publisher (link)
Dr. Pápa Miklós [in Hungarian] (1966). Budai-hegység útikalauz, Sport. Budapest.{{cite book}}: CS1 maint: location missing publisher (link)
References
Wikimedia Commons has media related to Buda Hills.
^Haas, János; Budai, Tamás; Dunkl, István; Farics, Éva; Józsa, Sándor; Kövér, Szilvia; Götz, Annette; Piros, Olga; Szeitz, Péter (2017-09-13). "The Budaörs-1 well revisited: Contributions to the Triassic stratigraphy, sedimentology, and magmatism of the southwestern part of the Buda Hills". Central European Geology. 60 (2): 201–229. Bibcode:2017CEJGl..60..201H. doi:10.1556/24.60.2017.008. hdl:10831/67494. ISSN 1788-2281.
^Balogh, K. (1981). "Correlation of the Hungarian Triassic". Acta Geologica Hungarica. 24 (1): 3–48.
^Kozur, Heinz; Mock, Rudolf (October 1991). "New Middle Carnian and Rhaetian conodonts from Hungary and the Alps. Stratigraphic importance and tectonic implications for the Buda Mountains and adjacent areas" (PDF). Jahrbuch Geologischen Bundesanstalt. 134: 271–297. Archived from the original (PDF) on 2021-06-09. Retrieved 2018-03-07.
^Kósa, Gábor; Mindszenty, Andrea; Mohai, Rita (2003). "Eocene alluvial fan prograding over a highly dissected palaeokarst surface built up by Upper Triassic dolomites. New details on the early Palaeogene evolution of the Buda-Hills" (PDF). Bulletin of the Hungarian Geological Society. 133 (2): 271–285.
^Magyari, Árpád (1994). "Late Eocene Transpression in the Budaörs Hills". Bulletin of the Hungarian Geological Society. 124 (2): 155–173.
^Farics, Éva; Farics, Dávid; Kovács, József; Haas, János (2017-10-28). "Interpretation of sedimentological processes of coarse-grained deposits applying a novel combined cluster and discriminant analysis". Open Geosciences. 9 (1): 525–538. Bibcode:2017OGeo....9...40F. doi:10.1515/geo-2017-0040. hdl:10831/66854. ISSN 2391-5447.