Introducing Trabzon Province 12

Mountain Areas

Mountainous areas, the East-West line had been broken, the North Black Sea coast as springs which form an anticlinal axis. Character of the region's highest mountain, from the end of the Permian and Upper Cretaceous that lasted until the end of the regime of land and has formed as a result of the upper Pliyosen'deki vertical movements, took the form of Pleistocene.

East-West direction from the highest part of the water line is part of the Mountains to the east Haldizen. This is also the Eastern Black Sea Mountains, the highest mountains to the west part of the recent extensions of the Kaçkars. Upper Cretaceous rocks in oil revenues. Significant elevations; Demirkapı (3,376 meters), rest harrow (3156 m) and King (3139 m) hills.

One moves towards the glacial valleys of the peaks showing the distribution of almost every valley, about twenty, some of them one by one after another gideşenle interconnected glacial lakes located in areas ranging from 100-1900 m2 wide. Karagol, Sarigöl, Fish Lake and Stallion can be considered as the most important of lakes. Demirkapı, North slopes of these mountains are right and Multat streams resources. Each one of the board of the glacial valleys of the rivers undersized. Side starts to receive streams of approximately 2000 m. To the north, with the increasing levels of fluvial topography from the moving forces begin to announce themselves thoroughly. Important tributary creek to the east Solakli Haldizen Creek, Demirkapı, right, and brooks, with the participation of the North, 1,150 m. Multat Uzungöl reaches levels. Continuing on from here under the name Black Creek Solakli confused.

Further west of the fault is a thrust from the mass of bulbous mountains between the Upper Cretaceous-Eocene oil rhyolite and dacitic lava porfiridasitlerin infiltrate occurred. That make up the Great River Creek Creek Solakli Haldizen with an average of 2,500 m. High level of the plateau is located in a very large, bulbous mountains alçaldığı connecting these areas inland of the coast-Çaykara-Bayburt road is the gateway. Belt section of water line to the west, Mount (2746 m) and Visit Peak (2850 m) and continues. This line is also part of the water line in the south constitutes Karadere. Sector, which extends inland to the north junction of the right arm of Karadere Yağmurdere watershed, extending to the southwest to encompass the handle portion of the water line reaches Degirmendere Basin. Black Sea coast road south, along the left Karadere Dağbaşı Arakli-road, falling water, part of the area around Stone Bridge to the south line reaches Gümüşhane.