Tepehan: Fissure and Landslide

A landslide and a fissure give Tepehan a distinct geological focus. During an earthquake, more than 180,000 cubic metres of material shifted, and a wide-ranging fissure formed in an olive grove. The landslide also developed in a Neogene rock unit. Together, these features draw attention to movement, soil and rock. The wider travel region of Hatay also offers its own landscape and cultural themes.

Geology at Different Scales

The landslide in the village of Tepehan affected an area of 12,000 square metres. During the earthquake, more than 180,000 cubic metres of material shifted. The area and the volume of material moved describe two different measurements of the same event. The landslide is also a concrete example of how earthquakes can trigger mass movements such as landslides. The event can therefore be understood in terms of both its scale and the geological process involved.

The landslide developed in a Neogene geological unit composed of sandstone, clayey limestone, claystone and marl. For those interested in geology, two perspectives converge here: the mass movement associated with the earthquake, and the rock types in the unit. Looking at the rocks thus complements the landslide figures with a specific geological context.

A second geological feature is a fissure in an olive grove in the village of Tepehan. It is 400 metres long and 200 metres wide. The split-open grove looked like a canyon. This comparison complements the measurements with an image of the formation; both draw attention to different aspects of the same olive grove.

Landscape and History in the Wider Hatay Region

In the area of the village of Kozkalesi, Kursat (Koz) Kalesi stands on a commanding hill beside the Altınözü (Kuseyr)–Antakya road, which has been used since antiquity. The castle is said to have been built during the Principality of Antioch to secure the road. A prominent location and a possible historical explanation are thus linked to the same route. This regional context complements Tepehan’s geological themes with a distinct historical perspective.

At Gelinler Dağı, between Yunushan, Kamberli, Kozkalesi and Akamber, rock formations are known as Peri Bacaları. The name adds a landscape theme to the Hatay context. Together with the castle, this offers a regional perspective that distinguishes between the historic road and the named rock formations, without treating either as part of Tepehan’s geology.

Minibus Connections and Holiday Apartment Search

For the Tepehan–Antakya minibus route, the municipal fare schedule for 2026 lists fares of 70 or 50 Turkish lira. For Tepehan–Enek, it lists 35 or 20 Turkish lira. Check current departure times before travelling. These amounts give you specific cost points for the two routes mentioned to help plan your trip.

If you are looking for a holiday apartment in Tepehan, you can plan your trip around your interests: geological themes take centre stage in Tepehan, while the castle and rock formations are distinct themes of the wider Hatay region. Consider whether the village itself or a broader regional perspective should be your starting point for planning your trip.

Discover more destinations: Hatay, Madenli Belediyesi, Atik, Arsuz, Başlamış Köyü, Harbiye, Karahüseyinli Köyü, Iskenderun.

Go to the wider travel overview: Hatay.