
Tashkent Train Station, Uzbekistan, Uzbekistan, Uzbekistan
These locations were historically submerged beneath the waves of the ocean. Over millions of years, they have evolved into geological formations characterized by the presence of Jurassic marble stones. These marbles formed during the Paleozoic era, approximately 150 million years ago, when the Earth's surface experienced a period of relative warmth and shallower marine conditions.
The Arashan Lakes System comprises six interconnected lakes situated at an elevation exceeding 3350 meters above sea level, primarily within the northern portion of the plateau. These lakes, including Khoja Arashan, Big Arashan, and Small Arashan, along with two smaller unnamed bodies of water, are fed exclusively through melting ice during the summer months between mid-July and September. They are characterized by being moraine-type high-mountain lakes ranging in altitude from 2770 to 3350 meters above sea level.
The route commences with a journey from Tashkent, traversing approximately 50 kilometers via off-road terrain to reach the Arashan Lakes. Upon arrival, visitors have the opportunity to witness numerous activities such as the annual relocation of over 1000 sheep to the shores of the lake, providing insight into the traditional shepherd lifestyle and interactions with local communities. Additionally, the region offers the chance to swim in its thermal spring waters, offering therapeutic benefits and unique hydrothermal experiences.
Starting from the thermal spring, the next stop is Khoja Arashan, the smallest of the lakes, which begins to dry up once the temperature rises significantly. Proceeding further, one encounters Lake Arashan (also known as Big Arashan), measuring approximately 1 kilometer in length and boasting a maximum width of 250 meters. Its immediate vicinity features a massive pile of gravel, initially mistaken for ice due to its unusual appearance. Located slightly higher at an altitude of 2780 meters above sea level, another small lake named Arashan is found nearby, showcasing a rectangular shape.
Continuing on the trail, travelers arrive at the Upper Arashan, situated at an elevation of 2795 meters above sea level and nearly identical in size to Big Arashan. Finally, reaching the summit of the mountain, four distinct lakes—Khoja Arashan, Big Arashan, Small Arashan, and Upper Arashan—are accessible. Among these, the highest lake, Khoja Arashan, stands out at an elevation of 3,365 meters above sea level. A striking feature at this location is the presence of two glacial lakes near the base of the mountain's slope.
Upon descending back towards Ertash Village and returning to Tashkent, travelers conclude their exploration of the Arashan Lakes System.
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Duration 12 hours
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Live tour guide
Russian
Pickup included
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Private group
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Tashkent Train Station, Uzbekistan, Uzbekistan, Uzbekistan
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0.19 mi
1.68 mi
2.73 mi
2.49 mi
2.55 mi
3.36 mi
5.59 mi
Over millions of years, the Arashan Lakes were formed due to the evolution of geological formations characterized by the presence of Jurassic marble stones. These marbles formed during the Paleozoic era, approximately 150 million years ago, when the Earth's surface experienced a period of relative warmth and shallower marine conditions.
The Arashan Lakes System comprises six interconnected lakes situated at an elevation exceeding 3350 meters above sea level.
The Arashan Lakes System includes Khoja Arashan, Big Arashan, and Small Arashan, along with two smaller unnamed bodies of water.
The lakes in the Arashan Lakes System are primarily fed through melting ice during the summer months between mid-July and September.
Visitors can witness numerous activities such as the annual relocation of over 1000 sheep to the shores of the lake, providing insight into the traditional shepherd lifestyle and interactions with local communities. Additionally, the region offers the chance to swim in its thermal spring waters, offering therapeutic benefits and unique hydrothermal experiences.
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