Dilek Peninsula-Büyük Menderes Delta National Park Aegean Region in general. The peninsula was shaped into its current form over several geological eras with the tectonic merging of Paleozoic schist formations, Mesozoic limestone and marble deposits, and finally the accretion of large clays and other sediments during the Neogene period. This is partly because of Turkey's unstable fault block terrain, and because of the close proximity of the Anatolian-Aegean plate boundary, which generates massifs of mountains all across western Turkey. This includes the peninsula and the mountains surrounding the Büyük Menderes River, known collectively as the Menderes Massif. The peninsula is highly mountainous, with most of its
Anatolian languages Anatolian languages The Anatolian languages are an extinct family of Indo-European languages that were spoken in Asia Minor (ancient Anatolia), the best attested of them being the Hittite language. The list below gives the Anatolian languages in a relatively flat arrangement, following a summary of the Anatolian family tree by Robert Beekes (2010). This model recognizes only one clear subgroup, the Luwic languages. Modifications and updates of the branching order continue, however. A second version opposes Hittite to Western Anatolian, and divides the latter node into Lydian, Palaic, and a Luwian group (instead of Luwic). Hittite ("nešili") was the language