Ulungur Lake is located in the north of Xinjiang. With a water area of 1,035 square kilometers, it is one of the top ten inland freshwater lakes in China. It has the only waterfront Yardang landform in China. At the same time, it is also an important node of the world's third migratory bird channel, with 23 famous fish species and more than 300 bird species.
Ulungu Lake (Golden Beach Scenic Area) is a concentrated tourist destination with both marine characteristics and landform diversity. The Golden Beach Scenic Area is an important part of the Ulungu Lake Scenic Area. The water area of Ulungu Lake is 1,035 square kilometers, consisting of Buluntohai (Dahaizi) and Jili Lake (Xiaohaizi). The Golden Beach Scenic Area is located on the east coast of Buluntohai in Ulungu Lake.
Ulungur Lake is also a "mirror of the sky" that makes people feel calm. Every year when the ice and snow on Ulungur Lake melts, the waters around the lake are wide and calm. When clouds float in the sky, their reflections appear in the lake, like a "mirror of the sky", attracting many photographers to come and create.
The Yardang landform of the Maritime Devil City, stretching for more than approximately 5 kilometers, is a rare spectacle in Xinjiang. The slopes are dome-shaped, with an average vertical height of 20 meters. The Yardang landform here, composed of Cretaceous sandshale formed over 100 million years ago, displays vibrant colors due to differences in rock layer materials. Shaped by long-term wind erosion and rainfall, it has been carved into countless strange forms, resembling skyscrapers, palaces, pagodas, and more.
Located at the estuary of Ulungur Lake on the eastern shore of Jili Lake, the Maritime Devil City combines the grandeur of a vast sea with the beauty of a serene lake. Travelers have hailed it as a "geological wonder of Yardang" and a "living Devil City."
Ulungur Lake developed on the basement of Paleozoic folds. It was eroded during the Mesozoic period, leading to the absence of sedimentary rock formations. The Tertiary rock system is relatively well-developed. Based on the distribution of sediments around the lake, lake terraces, lake erosion cliffs, and buried lacustrine sediments, the lake took shape in the Middle Pleistocene, with its basic pattern established in the Late Pleistocene. Observing Ulungur Lake helps understand the impact of crustal movement and glaciation (in paleogeological periods) on lake formation.
Geological and Geomorphological Research: Through field observations and wind erosion simulations at the Maritime Devil City, uncover how Yardang landforms are shaped by wind-water erosion and crustal movements.
Water Sports: Experience exciting water activities like surfing and enjoy holidays in the cool lake waters.