 Parts of Moslavačka gora, along with igneous landforms on Papuk and Požeška gora mountains in Slavonia to the east, are possibly remnants of a volcanic arc from the same tectonic plate collision that caused the Dinaric Alps.The region is a part of the Dinaric Alps, linked to a Late Jurassic to recent times fold and thrust belt, itself part of the Alpine orogeny, extending southeast from the southern Alps.The Dinaric Alps in Croatia encompass the entire Gorski Kotar and Lika regions, as well as considerable parts of Dalmatia, with their northeastern edge running from Žumberak to the Banovina region, along the Sava River, and their westernmost landforms being Ćićarija and Učka mountains in Istria.