Mali i Konjakut
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| Mali i Konjakut | |
|---|---|
  Mali i Konjakut | |
| Highest point | |
| Elevation | 1,140 m (3,740 ft) |
| Prominence | 155 m (509 ft) |
| Isolation | 2.96 km (1.84 mi) |
| Coordinates | 40°02′40″N 19°54′22″E / 40.044361°N 19.906193°E |
| Geography | |
| Country |  Albania |
| Region | Southern Mountain Region |
| Municipality | Himarë |
| Parent range | Ceraunian Mountains |
| Geology | |
| Rock age(s) | Cretaceous, Paleogene, Neogene |
| Mountain type | mountain |
| Rock type(s) | limestone, flysch |
Mali i Konjakut is a massif in southern Albania, forming the central and most elevated section of the Lavan–Konjak–Galisht mountain chain. Rising between the Ionian coastal belt and the inland valleys of Delvinë and Borsh, it constitutes one of the dominant limestone formations of the Ceraunian Mountains range.[1]
Konjaku lies between Lavan to the southeast and Galisht to the northwest, reaching its highest point at Maja e Piksës (1,140 m) and Maja e Lugjeve (1,046 m). Along with Galisht, it forms the most elevated section of the chain, extending 18 km in length and 5–6 km in width.
The mountain is composed primarily of Cretaceous limestone, forming a prominent anticline, with Paleogene–Neogene flysch deposits appearing along the outer margins.
Its western slopes descend abruptly toward the Ionian shoreline and the valley of the Borsh river, whereas the eastern side declines more gradually into the upper Kalasa valley and the Delvinë basin. The summit ridge is comparatively broad and locally flattened, creating karstic plateaus known as ara ("fields").[2]