Geologically, Moravia covers a transitive area between the Bohemian Massif and the Carpathians (from (north)west to southeast), and between the Danube basin and the North European Plain (from south to northeast). Its core geomorphological features are three wide valleys, namely the Dyje-Svratka Valley (Dyjsko-svratecký úval), the Upper Morava Valley (Hornomoravský úval) and the Lower Morava Valley (Dolnomoravský úval). The first two form the westernmost part of the Outer Subcarpathia, the last is the northernmost part of the Vienna Basin. The valleys surround the low range of Central Moravian Carpathians. The highest mountains of Moravia are situated on its northern border in Hrubý Jeseník, the highest peak is Praděd (1491 m). Second highest is the massive of Králický Sněžník (1424 m) the third are the Moravian-Silesian Beskids at the very east, with Smrk (1278 m), and then south from here Javorníky (1072). The White Carpathians along the southeastern border rise up to 970 m at Velká Javořina. The spacious, but moderate Bohemian-Moravian Highlands on the west reach 837 m at Javořice.