Gilan Tourism

Virgin and untouched nature

Gilan includes the western end of the Alborz mountain range and the western part of Iran's Caspian margin. The deep white river valley breaks the mountain belt between Manjil and Imamzadeh Hashem. In the northwest, the Talesh heights extend in the form of continuous basins and separate Gilan from Azerbaijan. Except for the northern end of the Ayuran, at the end of the Astara Chacha valley, which does not exceed 1600 m above sea level, the altitudes of all those regions are above 2000 m, and three peaks above 3000 m high (3197 m), Ajam (3009 m) and Shah Teacher Hot Masuleh (3050 meters). In the eastern and northeastern parts of the country, there are parallel flows going down to the sea, leading to a pattern of shapes. The western Alborz in the east of the Sefidrud Valley is wider and more prominent and has three parallel slopes; the representative of the southern and southern ones is in the Gilan mountain range (2375 m) in the Amarlou region; the median amplitude is steeper; from Dorfak Mountain (2733 m) to the Creek Mountain 3389 m), while the valley of the Pelorud Kalachai clearly divides the northern slopes into the magnificent (2387 m) and Mount Semam or Samavos (3689 m), the highest point of the Gilan. There are more than 40 rivers in Gilan, most notably Seychelles. Other important rivers are Gilan Astara Chay, Korgranrood, Asalem, Dinakal, Shihrood, Vakir, Vazirkadeh, Hasankayeh, Dehkah, Chamkhaleh, Kianrood, Khashbijjari and Pilehrood. Although all these mountains have more area than plains, plains are the most important feature of the province, and the term Gilan is often referred to as plain or especially to the central plain. This low-rise, 35-km wide, 90-kilometer long, heterogeneous, can be divided into two main parts: the Sefidrud delta in the east and the Fouman plain in the west. The former is entirely created by white sand, a high-flowing river (450 million cubic meters averaged) and high alluvium content. On top of the river, there is a thick, old, alluvial content, but at the bottom, north of the Astana, the river often has mud and mud, and its route has changed from the former north-easterly direction to the sea at the top of the plain at the glance of the plain, and now The north flows and the smaller living delta makes it between the beautiful and the port of Kishash as it crosses the sea. The Foumanate plain in the west tries to capture alluvial deposits of the sea and sandy beaches with abundant deposits from the numerous rivers flowing through the heights. They do not go directly to the sea, they are gathered in the Anzali lagoon or an outlet to the sea. They are gathering sandy beaches along the coastline. The wetland has been steadily shrinking and posting as a result of sedimentation. In contrast, the northern Talesh and eastern Gilan flows, which are even more plentiful than the Pelorud, are not enough to neutralize the flow of coastal waters flowing to the east, and can not be just a narrow ribbon of the low-lying area with only a few kilometers wide between Astara and Sefidrud, and in the east of Ghasemabad With a width of about 10 km in the Polroud crater around the clutch.

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