Kutelo in the context of "Bansko"

A ridge is a long, narrow, elevated geomorphologic landform, structural feature, or a combination of both separated from the surrounding terrain by steep sides. The sides of a ridge slope away from a narrow top, the crest or ridgecrest, with the terrain dropping down on either side. The crest, if narrow, is also called a ridgeline. Limitations on the dimensions of a ridge are lacking. Its height above the surrounding terrain can vary from less than a meter to hundreds of meters. A ridge can be either depositional, erosional, tectonic, or a combination of these in origin and can consist of either bedrock, loose sediment, lava, or ice depending on its origin. A ridge can occur as either an isolated, independent feature or part of a larger geomorphological and/or structural feature. Frequently, a ridge can be further subdivided into smaller geomorphic or structural elements.

Koncheto (Bulgarian: Кончето [ˈkɔnt͡ʃɛto], lit. 'foal') is a name given to a knife-edge ridge in the Pirin Mountains in Bulgaria, at an elevation of approximately 2,810 metres, between the peaks Banski Suhodol (2,884 meters) and Kutelo (2,908 metres). There are steep slopes on either side: the northwestern side is almost vertical and 300–400 metres deep, while the southwestern side is less steep (approximately 30 degrees) but deeper (800 metres). There is a steel cable stretched along the top of the ridge to help hikers across. It is said that some less experienced hikers go through Koncheto by saddling the ridge edge like a horse and slowly advancing, hence its name.

The Banski Suhodol Glacier (Bulgarian: Ледника в Бански Суходол, Lednika v Banski Suhodol) is a glacieret in the Pirin Mountains of Bulgaria. It lies below the Kutelo peak (2908 m.) in the upper Banski Suhodol Valley (Bulgarian: Бански Суходол).

Banski Suhodol (Bulgarian: Бански Суходол [ˈbanski suxoˈdɔɫ]) is a peak in the Pirin mountain, south-western Bulgaria. It is located in the northern part of Pirin on the main ridge. Its height is 2,884 m which ranks it in third place in Pirin after Vihren (2,914 m) and Kutelo (2,908 m).

To the south-east of Banski Suhodol on the main ridge is located at the summit of Kutelo and the two peaks are linked by the Koncheto ridge — a dizzy karst ridge which on some places is only 70 cm wide.

41°46′16″N 23°24′17″E / 41.77111°N 23.40472°E / 41.77111; 23.40472

Golemiya Kazan (Bulgarian: Големия казан) is one of the two cirques that form an area called Kazanite (the Cauldrons), situated in Bulgaria's Pirin mountain range. Kazanite are located below the two highest summits Vihren (2,914 m) to the south and Kutelo (2,908 m) to the north. It is composed of two cirques, Malkiya Kazan (The Small Cauldron), which is the lower one (2,200 m) and is grassy, and Golemiya Kazan (The Big Cauldron), situated at 2,400 m and with stony slopes. The size of Golemiya Kazan is 1,200 m by 1,100 m. They were named like that because there is often fog rising from the cirques. Due to the karst in the region there are no lakes or streams in Kazanite. A 450 m-high face of Vihren begins from Golemiya Kazan and at its foot a small glacier called Snezhnika is located, whose size is 80x90 m in summer, with a latitude of 41°46′09″ N it is the southernmost glacial mass in Europe. Chamois are abundant in this area.