Physical-geographical description of the city of Sagarejo
The southern part of Sagarejo Municipality is spread on the plateau-hilly Iori plateau, which is built of Neogene and Quaternary sediments. Geologically it consists of monoclinic anticline heights and syncline vakefskery tuffs. Dry valleys, ravines, ravines and also terraces are built on the upper terrain.
Among the negative forms of relief are the Kachreti and Tsitsmatiani accumulation plains, which are tectonic depressions. Sakaraulo Mountain (594 m) separates the plains. Here is a desert plain (dimensions 8X5 km), which is filled with loose layers.
From the low ridges rising on the Iori plateau are distinguished: Sakari, Natakhtari, Tetri-Udabno and Yaila-Jikhi anticline ridges. Near Mount Natakhtari begins the Gareji low range, which in turn is built of Neogene limestones, clays, sandstones, and conglomerates. The Gareji series ends at the right bank of the Iori River within the municipality. On Gareji Ser there is a mountain desert (878 m on the Georgian-Azerbaijani border), on the northern slope of which is the Davitgareja monastery complex.
The following mountains are erected on the top of Iori: Teteli (769 m), Demurdaghi (991 m), Datvisser (583 m), Natakhtari (966 m), Naomari (972 m), Aklemisgora (946 m).
The northern part of the municipality is occupied by the south-western slope of the Gombori ridge. It is built of conglomerates, sandstones and clays. Mount Manavistsivi (1682 m) is distinguished. The ridge of Gombori ridge is smooth and its slopes are lined with a network of erosive ravines of the Iori Basin.
There are also Bedland and karst forms on the territory of the municipality, namely: the Bedland relief is found on the easily rocky outcrops of the cold waters, while the karst ridges are observed in the vicinity of Gombori Mountain.
The main hydrographic network of Sagarejo Municipality is formed by the Iori River, which divides the territory of the municipality into two parts. The upper Samgori main canal is taken out of the river Ivri, through which there is the "Tbilisi Sea".
The river Chailuri (length 30 km) flows on the territory of the municipality, which starts on the south-western slope of Gombori ridge. Alag-Alag Itoteba.
Also noteworthy is the river Lapiankhevi, which has flood features. It is a small and small river (length 11.5 km). Autumn is characterized by flooding. The river Gombori (length 12.4 km) also flows in the territory of the municipality, which originates in the mountains of Gombori and is distinguished by clean water and beautiful shores. The Gombor River has one direction and flows only to the west (except for the middle section of the river). It flows for a considerable distance in forested areas.
There are also lakes in the municipality, including A group of lakes near Ujarma is selected, which is rich in fish and popular with fishermen.
The route starts in Tbilisi and goes through Rustavi to Gareji desert. The first stop is the multi-spring colorful mountains and reservoir. Here you will have to walk a bit to get closer to the colorful mountains. If you decide to go it cheap and risk the low bandwidth you are only fooling yourself. After the colorful mountains, the route will pass the nearby monasteries of the martyr and John the Baptist and head to the David-Gareji monastery. The monastery of the martyr consists of senaks carved into the rock and you will have to walk to see it. Just 1 km before the Davit-Gareji Monastery, to the right of the road, you will notice a fortress-like column, this is the Chichkhituri Monastery. After that you will go to Davit-Gareji Monastery, where the first part of the tour ends. Take a good look at this beautiful complex, relax and get ready to visit Gareja Saberi.
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