How to contact Dalinuoer Lake Natural Ecological Tourism Zone

Contact information of Dalinuoer Lake Natural Ecological Tourism Area: Dalinuoer Nature Reserve is about 90 kilometers away from Jingpeng Town, the seat of the Hexigten Banner People’s Government

Dalinuoer Lake Introduction to the attractions of the natural ecological tourist area:

Dalinuoer Nature Reserve is located in the west of Keshiketeng Banner, Chifeng City, Inner Mongolia Autonomous Region, about 90 kilometers away from Jingpeng Town, the seat of the Keshiketeng Banner People’s Government. The area spans the Dalai Nuori, Dalhan Ula and Aqi Ula three sumu. The northwest of the reserve is adjacent to Inner Mongolia's Xilin Gol Grassland Nature Reserve, the south is the eastern section of the Little Tengger Sandy Land, and the west is bounded by the Xilin Gol League. It is bounded by Chifeng City and about 80 kilometers away from Baiyin Aobao National Nature Reserve in the east. The geographical coordinates of the reserve are 1162211700 east longitude and 43114327 north latitude, with a total area of ??119413.55 hectares.

Dalinuoer National Nature Reserve is an important migration channel for migratory birds in northern China and one of the important distribution centers for migratory birds. Therefore, Dalinol Nature Reserve is a comprehensive nature reserve that mainly protects rare birds and the diverse ecosystems such as lakes, wetlands, sandy lands, grasslands and woodlands that they depend on for their survival. The special natural geographical conditions have given birth to the famous inland lake ecosystem on the Inner Mongolia Plateau. Lakes, rivers, swamps and wet meadows spread throughout the reserve constitute an important wetland ecosystem that accounts for 35.8% of the total area of ??the reserve. , which plays a leading role in the balance and stability of the regional ecosystem. The basalt platform and lake plain in the northwest of the reserve are broad and open prairie, where the most representative chestnut soil grass grassland of the Inner Mongolia Plateau develops. On the Little Tengger Sands in the south of the reserve is the unique elm sparse forest grassland landscape area, which is a special type of grassland area. In the corrugated sand dunes in the southeastern part of the reserve, sandy land vegetation and wetland vegetation are distributed in a mosaic. Sparse forests, shrubs, meadows, vegetation and swamp vegetation are distributed in a ring, thus forming a representative sandy grassland landscape type. .

Dalinol Nature Reserve has identified 160 species of birds in 36 families and 16 orders. Among the national key animals distributed in the reserve, those listed in the priority list of bird species diversity conservation in China’s Biodiversity Conservation Action Plan as Level A 1 include: black cheekbones, red-crowned cranes, white-naped cranes, great bustards, There are 6 species including Jade Belt Sea Eagle and Yellow-billed Egret; 3 species belonging to Level A 2 include: Gray Crane, Demoiselle Crane and Whooper Swan; 3 species belonging to Level B unique to China include: red-necked, little swan, kite, sparrow hawk, There are 11 species including common harrier, white-tailed harrier, merlin, red-horned falcon, yellow-clawed falcon, and long-eared trumpet.

The types and numbers of wading birds and migratory birds in the reserve dominate the rare birds. In spring and autumn, there are thousands of whooper swans and hundreds of white-naped cranes, gray cranes, Demoiselle cranes live here, and dozens of great bustards live and breed in the area.

The reserve has diverse ecosystems and rich resources of rare species. From the perspective of landscape ecosystem, the protected area has formed a landscape ecological pattern of basalt platform, lake basin plain, lake basin lowland and aeolian sandy land arranged in sequence from north to south. Correspondingly, it has platform plain and lake plain vegetation, low wetland vegetation and sandy land. The orderly distribution of sparse forest and grassland vegetation. In addition, the lake landscape centered on Dalinol and the mountainous landscape consisting of Dalhan Mountain and Zhenzi Mountain provide a diverse ecological environment for rich species resources. The reserve has identified 160 species of birds, 15 species of rodents, 21 species of fish, 72 species of phytoplankton, 36 species of zooplankton, more than 20 species of benthic animals, and about 434 species of higher plants. In addition, there are several small mammals in the reserve.

With its unique natural landscape and diverse species resources, the reserve attracts many experts and scholars from home and abroad as well as nature-loving tourists to come for inspection, visit and travel, and leaves a lasting impression on every visitor. Made a good impression. The protected area is not only an important base for scientific research, but also the best place to develop eco-tourism. There are scenery and pictures everywhere here. People can fully feel the infinite charm of nature when they come here.

The basalt plateau and lake plain in the west and north of the reserve are endless grassland landscapes. Here, there are green grass, flowers in bloom, cattle and sheep walking on the grass, and the simple scenery between the blue sky and green grass. The yurt reminds people of the yurt sung in the Mongolian song. The smoke from the yurt floats gently into the blue sky, making people really feel that the blue sky is so close to us.

Darkhan Mountain in the southern part of the reserve is lined with green trees and strange rocks. When you stand on the top of the mountain, you can have a panoramic view of the reserve. To the south is the rolling Little Tengger Sand Land, where sparse elm forests, lowlands between hills, and water bubbles of varying sizes are inlaid, forming a beautiful sandy grassland landscape. At the western foot of Darhan is the sparkling Dali Lake, which looks like the sea and the sky. Zhanzi Mountain in the distance seems to be floating on the water. The willow bushes and beaches beside the lake at the foot of the mountain are the best for swimming and fishing. place.

The Yingchang Road Site, also known as King Lu City, is located in the west of the protected area, bordering Subur to the west and the Huolai River to the south. It is surrounded by mountains and rivers and has an elegant environment. It has been listed as a key cultural relic of the autonomous region. Protective unit. This city was the place where Huizong Tuohuan Tiemuer fled from Dadu in the late Yuan Dynasty and died of illness in the second year of his life. Emperor Xuanguang accepted the throne, Shilidala succeeded to the throne in Yingchang, and the history books called it Zhaoyuan. Yingchang Wei was built in the early Ming Dynasty. During Zhu Bei's expedition, Zhu Zongzheng stationed in Yingchang four times and renamed it Qingping Town. The back city was destroyed by fire.

To the west from Yingchang Road is Liyupaozi. It is surrounded by mountains, has an elegant environment, and is full of springs at the bottom of the lake. The sandy land on the southern bank of the lake is covered with dense elm forests, and the northern bank is stony low mountains. Legend has it that Emperor Kangxi once fished here.

The Xiulai River connecting Liyupao and Dali Lake is a small river that supplies water to Dali Lake all year round. This river can be called the thinnest river in the world, with its thinnest point only about 12cm.

Nangengnuoer in the southeastern part of the reserve is often covered by shallow water and has a large area of ??willow bushes and reeds. It is an important place for nesting and breeding of birds in the reserve. All species of birds occupy their respective territories. This is the best place for bird watching tours in spring and autumn.

The reserve is located in the high plains of Inner Mongolia. The landforms in the area are mainly composed of four types: basalt platform, windy sand landform, lake landform and river landform.

From the perspective of formation type, the lakes in the reserve are mainly structural barrier lakes. They are an east-west lake group centered on Dali Lake and are located on the deep fault zone of the Xilamulun River. It is a lake formed by tectonic subsidence and dammed by basalt flow. At present, the shore of the ancient lake basin in the protected area has good lakeside topography, such as lakeshore terraces, lake erosion cliffs, lake erosion pillars, lake erosion platforms, land-connected islands and multiple lakeshore sand embankments. There are still two levels of lake erosion cliffs preserved on the Dalhan Mountain in the southern part of the reserve. The first level is 30 meters above the lake level, and the other is 60 meters above the water level. The deepest depth of Dali Lake today is 13 meters, which shows that the water depth of the ancient lake was approximately 6070 meters.

There are four rivers in the reserve: Gongger River, Liangzi River, Shali River, and Huolai River. These rivers are all inland rivers on the Inner Mongolia Plateau. They are characterized by: small water volume, silt There are also few, the river bed is gentle and the erosion base level is also high. The river is a meandering river bed with extremely developed meanders, which eventually flow into the lake. Wet meadows are often developed on both sides of the river.

The Little Tengger Sand Land in the southern part of the reserve has a relatively dry climate, with low annual precipitation, high evaporation, and strong winds. The main wind directions are west, northwest, or southwest. Due to differences in water content, vegetation, and sand consolidation degrees, sand belts mostly spread east-west on satellite images. The dune types are mainly composite longitudinal sand ridges and sand hills, and crescent-shaped dune chains and parabolic dunes are widely distributed.

The reserve has a medium-temperature continental climate, characterized by dramatic changes in cold and heat on the plateau, with large temperature differences between day and night, dry climate, long sunshine hours, strong solar radiation, heavy wind and sand, and rich thermal and wind energy resources. The annual average temperature is 1~2℃. January is the coldest month with an average temperature of -23℃~24℃. The extreme minimum temperature reaches -45℃. The number of days with annual minimum temperature below -20℃ exceeds 100 days. July is the hottest month. , the average temperature is 16~18℃, and the accumulated temperature at 10℃ is 1300~1700℃. Both ground temperature changes and air temperature changes are unimodal, and the maximum frozen soil thickness is 191 cm. Spring temperatures rise quickly, wind speeds are high, precipitation is low, and the climate is dry. It is the windiest season in the year, with instantaneous wind speeds up to level 11. The climate in summer is warm and cool, precipitation is concentrated, rain and heat occur in the same season, precipitation is unevenly distributed, and heavy rains and droughts occur from time to time.

Dalinuoer Nature Reserve and the surrounding areas belong to the Neocatastrophic uplift zone of the Greater Khingan Range in terms of geotectonic structure, and have strong neotectonic movements. The east-west fault from the end of the Tertiary to the beginning of the Quaternary, as well as multiple volcanic eruptions, etc., established the development pattern of this landform and laid the foundation for the distribution of water resources. In addition, the zonal differences in climate, soil and vegetation, etc. A variety of natural and geographical factors have had a positive impact on the generation, distribution, storage and movement of water resources in the reserve. Among various natural conditions, precipitation is the main supply source of water resources in the region. The amount of precipitation and regional differences directly affect the development degree of surface water and river characteristics. They also determine the distribution and abundance of groundwater, especially shallow water. degree.

The special landform types and geographical conditions of the reserve have formed its diverse ecosystems. From a landscape level, the reserve is mainly composed of three large landscape areas: the northwest is the majestic, broad and open platform grassland and lake plain grassland landscape, the south is the rolling sandy landscape, and the central and eastern parts are It is a unique plateau inland lake landscape dominated by Dalinuoer Lake and a wetland landscape formed by the development of rivers and wetlands. Distributed in these different areas are woodland, grassland, wetland and farmland ecosystems.

The forest ecosystems in the reserve are relatively concentrated. Except for small areas of artificial forests around the fishing grounds and several larger villages, the rest are distributed in the small Tengri Sand in the south of the reserve. The land and the Darkhan Mountain. Due to the special climate and water and heat conditions of the Little Tengger Sand Land, a unique elm sparse forest ecosystem has been formed in the reserve. The vegetation here is well developed and highly concealed. The vertical structure is clearly divided into three layers. The tree layer is mainly composed of elm trees. The shrub layer is mainly composed of Caragana microphylla, Siberian apricot, Northeastern polygonum, Inner Mongolia mugwort, small yellow willow, etc.; the grass layer is There are wheatgrass, Cryptophylla, Leymus chinensis, Carex and some annual grasses and sandy miscellaneous species. The distribution area of ??elm sparse forest in the reserve is 25,492 hectares, accounting for 21.3% of the total area of ??the reserve. A variety of birds are distributed in the woodland ecosystem, and white storks and black storks, national first-level protected birds, breed here.

The vegetation in the reserve is grassland, which is widely distributed in the west and north of the reserve, covering an area of ??54,446 hectares, accounting for 45.65% of the total area of ??the reserve. The main representative community is Leymus chinensis. Leymus chinensis grassland and Stipa macrophylla grassland with Stipa macrophylla as the founding species. Due to overgrazing in most grasslands in the area, some grasslands have been degraded. On the Stipa macrophylla grassland, Stipa macrophylla, Caragana microphylla, and Cryptophylla gracilis grassland and Stipa macrophylla, Wolfsbane, and Cryptophylla gracilis grassland were formed; in the Leymus chinensis grassland, Artemisia frigidum became the dominant species and was seriously degraded. The lot has become an established species.

The grassland ecosystem of this reserve has a large area and flat terrain, and is home to many wild animals. The great bustard, a national first-level protected bird, lives here.

The unique topography and abundant water resources of the reserve have formed a large area of ??wetland. The wetland ecosystem occupies an absolute advantage in the reserve, covering an area of ??42,737 hectares, accounting for 35.8% of the total area of ??the reserve. . The wetland ecosystem in the reserve mainly includes three types: lake system, river system and marsh system. The total lake area of ??the reserve is 25,644 hectares, the river area is 1,502 hectares, and the biogas system area is 15,591 hectares. More than 60 species of birds in the reserve inhabit and breed in the wetlands, and the numbers are large. The largest cluster can reach tens of thousands.

It has been preliminarily identified that there are 434 species of wild vascular plants in 250 genera and 67 families in the reserve, accounting for 19% of the wild vascular plants in the area. From the perspective of plant life forms, perennial herbs have an absolute advantage, with 280 species, accounting for 65% of all vascular plants, followed by monophyletic and biennial herbs, with 108 species accounting for 25%, and shrubs accounting for 25%. 6%, semi-shrubs account for 2%, and trees account for 2%. From the perspective of water ecological types of plants, mesophytes account for the most, with 260 species accounting for 53% of all vascular plants, 151 species of xerophytes accounting for 35% of all plants, and 40 species of hygrophytes accounting for 53% of all vascular plants. 9%, 13 species of aquatic plants, accounting for 3%. Judging from the floristic and geographical composition of plants, temperate plant genera have a clear advantage, with 157 genera in Japan, accounting for 63% of all plant genera, and 71 tropical plant genera, accounting for 3%. Central Asia, Central Asia, and the Mediterranean There are 22 genera in etc., accounting for 0.9%. There is also a genus unique to China.

The rich plant resources in the reserve contain a large number of plants of economic significance. Preliminary statistics include 294 species of medicinal plants, accounting for 68% of all vascular plants in the reserve. Common species include: licorice , ephedra, parsnip, bupleurum, motherwort, skullcap, cattail, reed root, dioscorea, polygonatum, Yiyeqiu, costus, fragrant blue orchid, orchid potted flower, etc. There are approximately 183 species of pastures of medium or above quality in the reserve, of which 83 species are excellent forages. There are also rich ornamental plants in the reserve, such as about 75 species of Limonium bicolor, delphinium, catfish, mountain elixir, dianthus, and wild chestnut. In addition, there are many kinds of edible plants in the reserve, such as wild vegetables such as amaranth, amaranth retroflexus, wild leek, day lily, etc., and wild fruits such as hawthorn, mountain vitex, and autumn pear.

There are also a large number of phytoplankton in the reserve. It is measured that the annual average phytoplankton content in Dalinol Lake is 1.6 mg/L, with 5 phyla and 72 species. Among them, there are 19 species of Cyanophyta, 24 species of Chlorophyta, 20 species of Diatoms, 7 species of Euglena, and 2 species of Dinoflagellates.

The reserve has recorded 133 species of birds in 16 orders, 33 families, among which the passerines contain the most families and species, with 44 species in 9 families, accounting for 27 of all bird families. % and 33% of the number of species; including families and species, there are storks, cranes, and birds. The above three orders have 3 families respectively, with ***35 species of birds, accounting for 10% of the total number of species. 26% of the number of species; orders containing 2 families include Falcon-type order and Columbine-type order, and the rest are single orders and single families, with 10 orders and 10 families. The largest family of birds in the reserve is Anatidae, with a total of 20 species of birds, accounting for 15% of all bird species in the reserve, constituting the main body of birds in the reserve. In spring and autumn, thousands of birds rest here, especially geese, ducks and gulls. The number of whooper swans in the reserve is also quite large. In spring and autumn, thousands of whooper swans can be seen, like snow-white flocks. There are also a relatively large number of great bustards on the grasslands in the northwest of the reserve. It is initially estimated that there are about 30 to 40 great bustards in this area.

Due to the influence of environmental factors such as climate conditions and water chemical composition, the fish species in Dalinol Lake are relatively monotonous, but the fish production is relatively large, among which crucian carp and Vacheronian carp are the largest. , is the main economic fish species in Dalinol Lake.

The protected area has a population of more than 4,000 people, with a distribution density of 3.4 people/square kilometer. Fishery and animal husbandry are the main economic activities in the area. The total number of livestock in the territory is about 90,000, and the total output value of animal husbandry is 5 to 6 million yuan. Dalinol has a long history of fishery production. There are records of fishing as far back as the 16th year of Mongolian Taizu in the Yuan Dynasty (1221 AD). The total fishery output value in 1998 was 5.2 million yuan. As early as 1983-1985, the Inner Mongolia Environmental Protection Office, Inner Mongolia Normal University, Chifeng Municipal Environmental Protection Office and other units conducted an investigation and study on the bird resources here, determined the status of Dalinol in the migration of migratory birds, and proposed the establishment of Dalinol. Recommendations for the Knoll Nature Reserve.

In 1985, the "Inner Mongolia Grassland Nature Reserve Plan" compiled by the Inner Mongolia Environmental Protection Science Institute included the Dalinuor area in the planned nature reserve plan. In 1986, the People's Government of Keshiketeng Banner in Chifeng City approved the establishment of Dalinuoer Nature Reserve. The management of the reserve is handled by Dalinore Fisheries. With the progress of society and the improvement of people's environmental awareness, Dalinol, a treasure land, is valued by more and more people. Its scientific value, conservation value and the social and economic benefits it will bring have become increasingly clear. Show it to the world. The construction and development of Dalinuoer Nature Reserve has attracted widespread social attention. In 1995, the Inner Mongolia Autonomous Region Urban and Rural Development and Environmental Protection Department and the Chifeng Municipal Environmental Protection Office commissioned the Inner Mongolia Environmental Monitoring Center Station to further develop the Dalinuoer Nature Reserve. Based on the investigation and research, the "Dalinol Nature Reserve Plan" was compiled. In 1996, the Chifeng Municipal People's Government submitted an application to the Inner Mongolia Autonomous Region People's Government to upgrade Dalinuoer Nature Reserve to an autonomous region-level nature reserve. In 1996, the Autonomous Region People's Government approved the promotion of Dalinuoer Nature Reserve to an autonomous region-level nature reserve. . In May of the same year, the People's Government of the Autonomous Region submitted an application to the State Council for the promotion of Dalinuoer Nature Reserve to a national nature reserve. In December 1996, the National Nature Reserve Review Committee approved the promotion of Dalinuoer Nature Reserve to a national nature reserve. Relevant materials and applications for national nature reserves. In December 1997, the State Council approved the promotion of Dalinuoer Nature Reserve to a national nature reserve.

In the early days of the establishment of Dalinuoer Nature Reserve, the management agency was located at Dalinuoer Fishing Ground and was managed by Dalinuoer Fishing Ground.

After being promoted to an autonomous region-level nature reserve in 1995, the People's Government of Keshiketeng Banner approved the establishment of the Dalinuoer Nature Reserve Management Bureau. Since the establishment of the reserve, a large amount of publicity work has been carried out, extensive publicity has been carried out through the use of news media, and videos and brochures introducing the reserve have been produced. Organized and compiled the "Comprehensive Investigation Report of Dalinuoer Nature Reserve", completed the "Dalinuoer Nature Reserve Project Proposal" (19962000), carried out the work of confirming the land rights of the protected area, delimited the boundaries, and handled the core area Land use certificate. In order to strengthen the management of the protected area, the management agency of the protected area has formulated management measures for the protected area and strictly investigated and punished poaching and damage to the resources and environment of the protected area. In order to strengthen the management and protection of the core area and restore the ecological environment of the lake area, the nature reserve has enclosed part of the core area. After several years of efforts, the surrounding environment of the lake area has been restored, and the types and numbers of birds have increased significantly. Fish production is also stable. The scientific research and monitoring work in the reserve has also achieved gratifying results, and the Dalinuoer Wetland ecological environment re-research project has passed expert appraisal. The protected area has strengthened the management of tourism resource development activities, delineated tourism areas, and standardized tourism behavior. Enjoy the lake and water color and bird watching tour

The night in the grassland is quiet and charming, and the melodious and resonant sound of the matouqin will take you into a green dreamland. With your smile picked from nature, a ray of morning light has first appeared in the east. Please keep everything yesterday in your memory. Let's go to the lake to watch the sunrise with thousands of rays of light, watch the golden-scaled fish leaping, and enjoy the hundreds of flowers. Birds sing and sing at the prairie pearl of Bird Paradise - Dalinuoer Lake

Walk in the morning breeze to the shore of Dalinuoer Lake. The lake surface is like a makeup mirror, with white swans, gray cranes, red-crowned cranes, wild geese, and swan geese migratory birds here. Make up and bathe. The morning sun in the east welcomes the sun, it is as red as red, the breeze is blowing, the clouds are in the water, the waves are in the sky, the sky is low and the water is wide, fish are jumping and gulls are slapping, flying flowers are dotted, and the golden waves are shining, it is spectacular. When you inadvertently look up, the vast lake in front of you is the famous prairie pearl Dalinuoer, which is translated into Chinese as sea-like lake, so Dalinuoer is also called Dalinuoer Lake. Dalinol Lake has a total area of ??240 square kilometers and a water depth of 10 to 13 meters. The water quality is chloride, bicarbonate, calcium and magnesium type water, and the salt content is mainly carbonate. The pH range is between 9.4 and 9.6. It is a closed Suda-type brackish water lake. Dalinuoer Lake is an inland lake on the plateau with no leakage. It is close to four rivers and springs: Gongger River, Liangzi River, Huolai River and Shali River. supply. Due to years of drought and other reasons, evaporation is greater than recharge, and the paste surface has shrunk. The water of Dalinuoer Lake contains 5% salt, a certain amount of alkali, and is smooth. It is the second largest freshwater lake in the Inner Mongolia Autonomous Region. Due to the unique water quality, it is difficult for exotic fish species to survive. There are only two types of fish in the lake, namely carp and Chinese squid (Wasiyaro), with an annual output of 600,000 kilograms of fresh fish. The fish produced in Dalinol Lake are tender and delicate in texture. Rich in nutrients, it is a good gift for entertaining guests and friends and as a gift to relatives and friends.

In early spring, the warm sun awakens sleeping creatures, and the ice melts and the snow melts. It is said that April 18th every year is the day when the Sea Dragon King gathers for a banquet, so the lake that has been frozen for half a year will burst suddenly overnight, and with the help of the breeze, it will magically pile up to the shore, layer upon layer, crystal clear and exquisite. At this time, there is a vast bay of spring water in front of you, the cold icebergs are around you, and deep in the grassland behind you is the early summer dotted with green grass and flowers. This wonderful scene of winter, spring and summer coexisting in one place is rare among the many lakes in the north. This is the ingenious masterpiece of Dalinol Lake.

In this rare scenery, you will find thousands of birds chirping loudly, rising like gods riding in the mist, and falling like goddesses scattering flowers, with graceful and extraordinary postures.

Dalinoor Lake's sister lake - Ganggennuoer Lake

With the melody of the rolling waves of Dalinnuoer Lake, walk 15 kilometers east of the lake and you will arrive at Ganggennuoer Lake. Lake Nuoer (Chinese translation means Eternal Lake). Ganggennuoer Lake has a total area of ??17 square kilometers, a water depth of 1 to 5 meters, and an altitude of 1,240 meters. The lake is rich in carp, crucian carp, and Chinese carp. A large reed nearly 2 meters high grows in the southeast of Ganggennuoer Lake. It conserves water and is fed by the crystal clear Tuoli River. Along the southern edge of Ganggennuoer Lake, at the northern end of the Hunshandake Sandy Land, there are several springs gurgling into the lake all year round. There is an inconspicuous Dagennuoer on the west side of Lake Ganggennuoer, from which an unknown stream gurgls into Lake Ganggennuoer. Ganggennuoer Lake is surrounded by red willow trees, which are like low water towers conserving water.

The beauty of Ganggennuoer Lake lies in the vast expanse of green grassland beside the lake, and the beauty lies in the rippling golden scales in the lake water. If it's a sunny day and the sea is calm, you can see thousands of fish jumping around and the crackling sound is endless. Carp weighing several kilograms or more will jump out of the water, which will dazzle you. Some of them actually fall into the cabin. He tried to jump over the dragon gate but failed, so he fell into the soup pot under the cabin. Under the setting sun or in the morning light, you may be on the shore of a glimmering lake, or go boating on the lake, or go fishing. The trivial matters of the city will naturally drift away with the waves of the water, and a feeling of leisure and tranquility will come to your heart.

September to October every year is the best time to watch birds and lakes. In the distance are lush green grasslands dotted with yellow flowers, and large tracts of reeds more than 1 meter high grow on the shore near the water. Various baby birds are toddling in the grass. If you approach quietly, you will see a red-crowned crane with a red crown on its head, gentle steps and full of gentlemanly demeanor, walking happily, followed by a little gentleman learning to walk.

Looking up, thousands of migratory birds are flying and singing on the lake. White swans, red-crowned cranes, and gray cranes are circling the lake, floating like immortals, just like the flying fairies in Dunhuang murals, with graceful movements. This picture of birds, fish and lake light drawn by nature is intoxicating and fascinating, making you linger and forget to leave.

Dalinore Lake's sister lake - Dolennore Lake

Go west 16 kilometers from Dalinore Lake to Dolennore Lake. Lake Dolenor has a total area of ??2.2 square kilometers. There are many springs in the lake and the water quality is excellent. It is famous for its abundance of carp. According to legend, there was no carp in Dolenol Lake. After fishing in Dalinol Lake, Emperor Kangxi came to Dolenol Lake and saw that there were no fish in the lake and the huge water surface was empty, so he ordered people to use camels to fish from the Yellow River. Dozens of carp were brought and released into the lake. To this day, people still refer to Dolenol as Carp Paozi. The descendants of dozens of carp carried in cowhide bags have continued to multiply and become inexhaustible wealth for the people here.