Serakol
In this article we are going to talk about Serakol, a topic that has been the subject of debate and discussion over the years. Serakol is a topic of great relevance in today's society, since it affects different areas of daily life, such as health, politics, culture and the economy. Throughout history, Serakol has played a fundamental role in forming identities and building communities. In this sense, it is important to analyze the impact that Serakol has had in different contexts and how it has evolved over time. Through this article, we aim to address different perspectives and aspects related to Serakol, in order to offer a comprehensive and enriching vision on this topic.
| Serakol | |
|---|---|
  Serakol | |
| Highest point | |
| Elevation | 2,153 m (7,064 ft) |
| Prominence | 5 m (16 ft) |
| Isolation | 174 m (571 ft) |
| Coordinates | 41°50′29″N 20°31′02″E / 41.84125°N 20.517093°E |
| Geography | |
| Country |  Albania |
| Region | Central Mountain Region |
| Municipality | Kukës |
| Parent range | Korab |
| Geology | |
| Rock age | Neogene |
| Mountain type | mountain |
| Rock type | shale |
Serakol (def. Serakoli) is a mountain in northeastern Albania, part of the Korab-Koritnik Nature Park. It lies south of the Shishtavec plateau, separated from the valley of the Çaja stream (Bushtricë). Its highest peak, Kulla e Zyberit, reaches a height of 2,153 m (7,064 ft).[1]
Geology
Composed almost entirely of shale, with a scaly and blocky structure, the mountain features an elongated shape with a northwest–southeast orientation. It is divided into two sections, the southeastern section, which represents the highest relief (Kulla e Zyberit – 2,153 m), and the northwestern section, which descends abruptly into the valley of the Black Drin. The northern slope of the mountain is modeled by glacial cirques, while the southeastern side drops steeply into the valley of Veleshicë. Its ridge exhibits a neogene erosive surface, resulting in an almost flat relief. The northwestern portion forms a gentle terrain, overly fragmented by erosive-denuding processes, gradually descending towards the Black Drin valley.[2]
See also
References
- ^ "Parku Natyror "Korab-Koritnik"". akzm.gov.al. Agjencia Kombëtare e Zonave të Mbrojtura. Retrieved 21 June 2023.
- ^ Kabo, Mevlan (1991). Gjeografia Fizike e Shqipërisë (1.2 ed.). Tiranë: Qendra e Studimeve Gjeografike. p. 126.