Ningxia Moon Lake Tourist Attractions Introduction Ningxia Moon Lake Scenic Area Address

What is the altitude of Moon Lake

Moon Lake is located in Alxa Left Banner, Alxa League, Inner Mongolia Autonomous Region. The terrain of Alxa Left Banner is high in the southeast and low in the northwest, with an average altitude of 800 to 1,500. meters, with a maximum altitude of 3556 meters. Moon Lake is a natural lake in the Tengger Desert. It is also one of the most influential desert in-depth tourism experience sites in the world, with a core area of ??150 square kilometers.

Moon Lake is 61 kilometers away from Bayanhot Town and 60 kilometers away from Guangzong Temple (South Temple) tourist area. Local herdsmen call it China Lake because from the east the lake looks like a crescent moon quietly telling ancient stories, and from the west the dunes look like a map of China, majestic.

The water surface of Moon Lake is about 2,000 acres. The water is 2 to 4 meters deep, 2 kilometers long from north to south, 1 kilometer wide from east to west, and 4 kilometers around the lake. The scenic area is divided into five major modules: folk customs area, club leisure area, hotel and villa area, ecological demonstration park and outdoor experience area. It can greatly meet the needs of the business, conference, adventure and leisure travel markets. Moon Lake is located in the hinterland of the Tengger Desert in Inner Mongolia. In recent years, with its unique wild luxury style, Moon Lake has become another high-profile leisure resort after Boao and Lijiang. Sacred mountains, deserts, Gobi and Tibetan Buddhism give Moon Lake, the pearl in the desert, endless charm.

Which province and place is Moon Lake located in?

Moon Lake is located in Alxa Left Banner, Alxa League, Inner Mongolia Autonomous Region. It is a natural lake in the Tengger Desert. It is also one of the most influential desert in-depth tourism experience sites in the world, with a core area of ??150 square kilometers.

Moon Lake is located in the hinterland of the Tengger Desert in Inner Mongolia. In recent years, with its unique wild luxury style, Moon Lake has become another high-profile leisure resort after Boao and Lijiang. Sacred mountains, deserts, Gobi and Tibetan Buddhism give Moon Lake, the pearl in the desert, endless charm. When you come here, you can enjoy the excitement of surfing in the sand sea, the excitement of sandboarding, the process of hiking through the desert, the unique charm of desert swimming, and you can also appreciate the emotion of the ancients "the sun sets in the desert with a round sun".

The formation and introduction of Moon Lake, or only its formation

Moon Lake is located in the hinterland of the Tengger Desert in Inner Mongolia. It is another high-end popular leisure resort. Sacred mountains, deserts, Gobi and Tibetan Buddhism give Moon Lake, the pearl in the desert, endless charm. When you come here, you can enjoy the excitement of surfing in the sand sea, the excitement of sandboarding, the process of hiking through the desert, the unique charm of desert swimming, and you can also appreciate the emotion of the ancients "the sun sets in the desert with a round sun".

On January 16, 2009, Moon Lake was also rated as one of the "Top Ten Charming Leisure Tourism Lakes in China" along with world-famous lakes such as West Lake and Xinjiang Tianchi, and won the title of "China's Most Romantic Lake" Beautiful title.

Ningxia Hui Autonomous Region Tengger Desert Moon Lake

Tengger Desert

Tengger Desert The fourth largest desert in China. It is located in the southeast of Alxa region, between 37°30′ and 40° north latitude, and 102°20′ and 106° east longitude. It covers an area of ??approximately 42,700 square kilometers. The administrative division mainly belongs to Alxa Left Banner, and the western and southeastern edges belong to Minqin and Wuwei in Gansu and Zhongwei City in Ningxia respectively. The desert includes Nanjiling in the north and Tengger in the south, and is commonly referred to as the Tengger Desert. Sand dunes, lake basins, mountains and flatlands are staggered in the interior of the desert. Among them, sand dunes account for 71%, lake basins account for 7%, and mountain residual hills and flat land account for 22%. Among the sand dunes, mobile sand dunes account for 93%, and the rest are fixed and semi-fixed sand dunes. The height is generally 10 to 20 meters, mainly grid-shaped dunes and grid-shaped dune chains, and crescent-shaped dunes are distributed in the edge areas. Tall complex dune chains are found in the northeastern part of the desert, with a height of about 50 to 100 meters. Fixed and semi-fixed sand dunes are mainly distributed on the periphery of the desert and on the edge of the lake basin, and the plants on them are mostly sagebrush and white thorns. On the moving sand dunes, there are Artemisia annua, Sand Bamboo, Phragmites australis, Phyllostachys sibiricum, Phyllostachys sibiricum, Phyllostachys sibiricum, Phyllostachys sibiricum, etc., which grow better than those in the Badain Jaran Desert. There are also large areas of ephedra in the Magang area in the northwest and southwest of the desert. There are natural secondary forests of Populus euphratica among the sand dunes around Wutongshu Lake. In Toudao Lake, Tonghu and other places, there are artificial forests built after 1949. The 31 kilometers (19 miles) of Baotou to Lanzhou railway pass through the southeastern edge of the Tengger Desert. An area of ??200_300 meters (656_984_) along the railway line has been treated and the original mobile sand dunes have been fixed, ensuring the safety of railway transportation. Edit this paragraph to form

Form background

The fourth largest desert in China. It is located in the southwest of Alxa Left Banner in Inner Mongolia Autonomous Region and on the border of central Gansu Province. The Great Wall of South Vietnam reaches Helan Mountain in the east and Yabulai Mountain in the west. The area is about 30,000 square kilometers. The altitude is about 1,200 to 1,400 meters.

Background Introduction

Tenggri means sky in Mongolian, which means the vast quicksand is like the boundless sky, hence the name. Inside the desert, sand dunes, lake basins, salt marshes, grasslands, mountains and plains are staggered. Among them, sand dunes account for 71%, of which 7% are fixed and semi-fixed sand dunes. Most of the southwest part of the desert is covered by vegetation, mainly ephedra and Artemisia spp.; in the depressions in the central, southern and northern parts of the desert, plants grow well, mainly Artemisia genus.

Mobile sand dunes are mainly grid-shaped dunes and grid-shaped dune chains, generally 10 to 20 meters high. There are also compound dune chains with a height of 10 to 100 meters, often moving southeast. There are 422 large and small lake basins in the desert, of which 251 have accumulated water. They are mainly for spring water supply and temporary water collection. Most of them are residual lakes from the Tertiary Period and are the main settlement areas for residents. Desertification control work began in 1958. Hundreds of protective forest belts were built and the sand was sealed to cultivate grass. This allowed the Baolan-Lanzhou Railway to pass through the desert without hindrance. This was a huge achievement in the science of desertification control in China. Reasons for editing this paragraph

Overgrazing in the Tengger Desert

The two main reasons for the formation of the Tengger Desert are drought and wind. In addition, people cut down forest trees and destroyed grasslands, leaving the surface of the land without plant coverage, and deserts were formed. In addition to arid climate conditions, deforestation and destruction of grasslands, the formation of deserts also requires rich sources of desert materials, which are mostly distributed in sediment-rich inland mountain basins and depressions and low flats on denuded plateaus. superior. Sand sources include fine-grained material from various sediments, ancient or modern. For example, the sand in China's Taklimakan Desert and Gurbantunggut Desert originates from ancient river alluvial deposits; most of the sand in the Tengger Desert, Mu Us Desert and Lesser Tengger Desert originates from ancient and modern alluvial deposits and lake deposits. The deserts in the middle reaches of the Tarim River and the lower reaches of the Korla Southwest Sliding River are all derived from modern river alluvial deposits; the sand dunes in the Tengger Desert and the Helan Mountains and Langshan-Bayinwula piedmont areas are derived from alluvial deposits; in the central and western parts of Ordos Sand dunes on the highlands are derived from the weathered residue of bedrock. Edit this paragraph's climate

The climate is controlled by westerly circulation all year round. It is a typical continental climate in the mid-temperate zone. Precipitation is scarce. The average annual precipitation is 102.9 mm, the maximum annual precipitation is 150.3 mm, and the minimum annual precipitation is 150.3 mm. 33.3 mm, the annual average temperature is 7.8℃, the absolute maximum temperature is 39℃, the absolute minimum temperature is -29.6℃, the average annual evaporation is 2258.8 mm, the frost-free period is 168 days, the sunlight is 3181 hours, the solar radiation is 150 kcal/cm2, and the temperature is greater than 10℃ The effective accumulated temperature is ?3289.1℃. Southwest wind prevails all year round. The main harmful wind is northwest wind. The wind is strong and the average annual wind speed is 4.1m/s. The hazard of wind and sand is the main natural disaster. However, it is rich in light and heat resources and has potential advantages in developing agriculture. Edit this paragraph's resources

Original lakes

Tengger Desert - rich in resources

There are hundreds of thousands of preserved lakes scattered in the Tengger Desert The original ecological lake has existed for thousands of years. Under the blue sky, the desert is vast, desolate, and majestic. Thousands of miles of undulating sand dunes are scattered high and low like solidified waves. The soft lines show its extraordinary charm. Standing on the sand dunes high in Tengger Dalai, you will be surprised to find a strange original ecological lake, which resembles a map of China. The distribution of reeds marks all provinces and regions in the country one by one - this is Tengger Dalai Moon lake. According to testing, Moon Lake is half a freshwater lake and half a saltwater lake. The lake water contains more than 10 mineral trace elements such as selenium and iron oxide, and has great purification capabilities. The lake water has remained for millions of years without being turbid, despite the annual rainfall. It is only 220 millimeters, but instead of decreasing, the lake water has increased. Moon Lake is the only original ecological lake with a coastline among the many lakes in the Tengger Desert. On its 3-kilometer-long and 2-kilometer-wide coastline, if you dig out the thin surface layer, you can reveal tens of millions of years of black sand and mud. After testing, the unique black sand mud of Moon Lake is rich in more than a dozen trace elements. It is very similar to the medicated bath formula recommended by international health care organizations. Its quality is better than the black mud in the "Dead Sea". It can be said to be unique in Tengger Dalai. of pure ecological resources.

Lake Basins

There are as many as 422 large and small lake basins in the desert. Most of them are grass lakes without clear water, with an area ranging from 1 to 100 square kilometers. Distributed in a strip, the water source mainly comes from diving in the surrounding mountains. The vegetation types in the lake basin are mainly swamps, meadows and halophytes, which are the main pastures in the desert. Most of the mountains are scattered isolated mountains and hills covered by quicksand or divided by sand dunes, such as Alagu Mountain, Qingshan, Toudao Mountain, Erdao Mountain, Sandao Mountain, Sidao Mountain, Turantai Mountain, etc. The flat land inside the desert is mainly distributed between Chala Lake and Tong Lake in the southeast. A small area of ??land has been cultivated on the edge of the lake basin in the desert. The population density is higher than that of the Badain Jaran Desert. In the hinterland of the desert are Chahanbrug, Turantai, Iker and other townships, and residential areas are distributed on the periphery of the larger lake basin. There are residential areas such as Tonghu, Toudaohu, Wendurtu and Mengen on the edge of the desert, as well as some sand-fixing forest farms. Near Shapotou is a national nature reserve with an area of ??12,700 hectares. There are "ringing springs" in the desert that can predict earthquakes.

Rizhao Resources

The desert is rich in sunshine, with a maximum temperature of 39°C and an area of ??286.6 square kilometers. The main component of thermoelectric solar power generation is the solar collector. To reach the 280 degrees Celsius required for power generation. The collector must be focusing type. Taking the Chinese-made small single low-pressure steam turbine as an example, its generating power is 6,478 kilowatts, and the required solar collector area is 45,000 square meters. There are no fixed roads in the desert. Because the dunes are small and there are many residential areas, the east-west passage often passes directly through the desert. The Baotou-Lanzhou Railway passes through the southeastern edge of the desert. The Chahan Pond, Red Salt Pond and Tun Pond inside the desert are rich in salt. The residents are mainly Mongolian, who engage in animal husbandry and settle down to graze.

Edit this paragraph Geology and Hydrology

As far as the general terrain is concerned, it belongs to the alluvial plain of the Alxa Plateau, with an altitude of 1050m. In terms of geological structure, it is a fault basin, which is a fourth alluvial of fine sand and clay. It is covered by lake sediments, and is covered by alluvial, siltation and wind deposits. Most of them are mobile, semi-fixed and fixed sand dunes, gentle sandy land and inter-dune lowlands, which are distributed in multiple areas with heights ranging from 3 to 10 meters. . The Yellow River flows through the southeastern end of Dengkou County from south to north. The terrain of Dengkou Oasis slopes from southeast to northwest, with an altitude generally between 1048-1053m. The entire terrain of the Ulan Buh Desert is lower than the water level of the Yellow River, and there are conditions for diversion from the Yellow River for irrigation, thus making up for the disadvantages of low rainfall, high evaporation, and drought and water shortage. The underground water depth is 5-8 meters, the shallow water resources are abundant, and the water quality is good and suitable for irrigation. According to survey data from the Inner Mongolia Hetao General Administration, shallow confined and semi-confined water is extremely abundant, with a 100-meter aquifer and a total reserve of 5.7 billion cubic meters. The water quality is good, making it a high-quality water source for drainage and irrigation. Edit this section of tourism

The tourism department has arranged many special activities for tourists, such as desert picnics, desert camping, stargazing and moongazing, searching for water in the desert, visiting desert nomads, visiting the desert "Bird Lake", "Fish Lake" and viewing ancient rock paintings are the "specialties" of roaming the Tengger Desert. In addition, the tourism department also provides guests with vehicles, food, camel drivers, guides, camping equipment and, of course, the most important ones, camels. Camels for tourism,

Tengger Desert-Swan Lake

In addition to elegant saddles and pedals, there are also pancake bags for fruits and food, and cameras for guests. , telescopes, etc. can be placed in the earthen sack stretched across the camel's back. In addition to the camels for the tourists, the camel team also includes the guide camels that lead the way, the guides' accompanying camels, and the logistics camels that follow the trail. The tinkling camel bells equipped in the camel team can ring ten miles away at night, giving people a sense of safety and stability. At the same time, it also plays a role in regulating the camels' pace. Swan Lake: Tengger Desert Swan Lake is located in Alxa Left Banner (Bayanhot Town), Alxa League, Inner Mongolia Autonomous Region. It is located on the eastern edge of the Tengger Desert. It is about 1,500 meters long from north to south and 500 meters wide from east to west. About 3.2 square kilometers. Swan Lake and Moon Lake are about 35 kilometers apart from north to south, and Bayanhot Town, where the banner government is located, is also about 35 kilometers apart from east to west. The three form an obtuse isosceles triangle. Swan Lake is surrounded by vast desert, with undulating sand dunes and billowing sand waves. The scene is majestic and refreshing. Swan Lake and Moon Lake, one large and one small, are a pair of outstanding sisters among the more than 190 lakes in Tengger. They complement each other and have their own charms, attracting a large number of tourists. Edit this paragraph: Moon Lake in the Tengger Desert

Moon Lake in the Tengger Desert

Located in the hinterland of the Tengger Desert in the Alxa League of Inner Mongolia, China, the Moon Lake is a short distance from major cities in the country. The desert adventure camp with the shortest radius is the best trip for modern urbanites looking for thrills and complete relaxation outside of the tense competitive life. Moon Lake has three unique features: first, its shape resembles a map of China: standing on a high sand dune, a complete map of China is displayed in front of you, and the distribution of reeds marks each province and region one by one; second, the lake's natural medicine Bath formula: The lake water with an area of ??three square kilometers is rich in potassium salts, manganese salts, a small amount of nitrate, natural soda, trona, iron oxide and other trace elements. It is very similar to the medicated bath formula recommended by international health care organizations. The lake water has great biological purification capabilities and can quickly improve and restore the natural original ecological qualities. The third is the Thousands of Years Black Beach: a natural bathing beach that is one kilometer long and nearly 100 meters wide. Pushing aside its surface layer, underneath is more than ten meters thick pure black sand and mud. Its texture is far superior to the black mud of the Dead Sea, and it is a natural mud therapy treasure. The scenic area has complete water, electricity and communication facilities, and convenient transportation. There is a black oil road directly leading to the scenic area reception station. It is about 130 kilometers away from Yinchuan Airport and Railway Station. Edit this section of industries

Tengger Desert - Animal Husbandry

Mainly include Cistanche deserticola, Cynomorium Cynomorium, sophora seeds, etc. The alliance currently has 15 million acres of natural Haloxylon ammodendron forest, a concentrated distribution area of ??5.787 million acres of Cistanche deserticola, and an annual collection volume of 150 tons; 28.25 million acres of white thorns, a concentrated distribution area of ??18.33 million acres of Cynomorium Cynomorium, and an annual collection volume of more than 500 tons; natural The distribution area of ??bitter bean seeds is 1.34 million acres, the resource output is 400,000 tons, and the annual collection is 1,000 tons. In terms of soil and vegetation in the Tengger Desert, the zonal soils of the Tengger Desert are gray desert soil and brown zeem soil. The vegetation is dominated by sandy shrubs and semi-shrubs. A large amount of gypsum often accumulates in the gravel and sandy loam soil layers; a large area of ??saline-alkali soil develops in the lake basin, among which meadow saline soil is the most widely distributed and grows a large number of halophytes. Aeolian sand soil is the largest soil type in the territory and is distributed from the edge of the lake basin to the piedmont plain. It is the foundation on which oasis plants rely. Large areas of mobile dunes have almost no vegetation, with a coverage of less than 1%; semi-fixed dunes have a higher vegetation coverage of 15%-20%. Mainly are sand bamboo and Artemisia seed; fixed sand dune plants grow densely, mainly Artemisia ordosica; in widely distributed lake basins, due to better water conditions, salinized meadows and swamp vegetation are dominant.

The main economic vegetation includes reeds, Splendens splendens, white thorns, salt thorns, etc., with a coverage of 20%-60%. It is the main grazing land and mowing grassland in the desert. There is a certain regularity in the distribution of plants from quicksand to the belly of the lake basin; in the desert The main feed and medicinal plants in the piedmont alluvial plains on the edge and the island hills and mountain valleys in the desert include red sand, pearl, ephedra, holly, Bawang, Tibetan golden pheasant, pigweed, and eucalyptus. Chenopodium, bindweed, shrubs, tansy, etc. There are a large number of small grasses mixed in the grass group, showing the characteristics of grassland. Based on the above situation, in the future, grazing should still be the main use area in desert areas. It is necessary to strengthen the protection and utilization of existing grasslands and control grazing on fixed sand dunes. A rotational grazing system should be established for fixed sand dunes and lake basins. In areas with better water sources, establish Artificial and semi-artificial pastures that combine forest and grass. Edit this paragraph Desert deterioration

According to the relevant person in charge of the Wuhai Forestry Bureau, in the past 40 years, due to the dual reasons of natural climate warming and man-made destruction, the Ulan Buh Desert has expanded eastward and southward at a rapid rate Very amazing. According to relevant records, in the early 1960s, the eastern edge of the Ulan Bhe Desert was nearly 30 kilometers away from Wuhai. In less than 40 years since then, nearly one-third of the land in Uda District has been swallowed up by the Ulan Buh Desert. The eastern edge of the Ulan Buh Desert has expanded from Alxa League on the west bank of the Yellow River to Haibowan area on the east bank of the Yellow River. The erosion area is nearly 100 square kilometers, and all of them have formed crescent-shaped and half-moon shaped flowing sand dunes. Some of the sand dunes are The relative height is more than 50 meters. The rapid advancement of the Ulan Buh Desert has seriously affected the daily lives of people in surrounding areas. According to the third desertification and sandification land monitoring report of the autonomous region, the desertification and sandification area in Wuhai City accounts for 80.12% of the city's total land area. Severe desertification and desertification have resulted in a poor natural ecological environment in Wuhai. The average annual precipitation is less than 160 mm (only 81.5 mm in 2005), while the evaporation is as high as 3,500 mm; sand and dust weather and sandstorms occur frequently, and the average daily wind speed The maximum number of days greater than 3 m/s is 301 days. Wuhai City has become one of the cities with the most severe desertification in the Inner Mongolia Autonomous Region and even in China. Edit this paragraph Management and Utilization

First, the current situation and characteristics of the climate, hydrology, soil and vegetation in the Tengger Desert provide the prerequisite and ideas for the management and utilization of the Tengger Desert. From the perspective of climate and hydrological conditions, the Tengger Desert has significant continental climate characteristics; it is close to lake basins and rivers, and has good water conditions. The Tengger Desert has a dryness degree of 4-12, an annual average temperature of 7-9 to (2, greater than 10 degrees, an accumulated temperature of 3200 to 36000 degrees, an annual sunshine duration of 3100-3200 hours, and a frost-free period of 145-165 days. It is the largest desert in Inner Mongolia. It is one of the areas with the longest sunshine and the highest accumulated temperature in Ningxia. The annual precipitation is 1.16-148 mm. Although the rainfall is small, it is mostly concentrated in July-August. The rain and heat are in the same season. It is an annual grass in summer. It provides good hydrothermal conditions for the growth of grasses and other small grasses. The annual evaporation is 3000-3600 mm, the annual average wind speed is 3-4 meters/second, there are level 8 storms in February and March, and the number of windy days per year is 30--. --50 days, is one of the areas rich in wind energy resources. This provides a prerequisite for the use of wind energy. Secondly, the Yellow River flows through the southeast edge of the Tengger Desert, and has been diverted for irrigation since ancient times, with good results, especially The area in Zhongwei County has good harvests despite droughts and floods. It can be said to be "blocked in the south of the Yangtze River." The Yellow River diversion irrigation system there should be continued to improve and expand, and the oasis along the Yellow River should be consolidated and expanded. To achieve this goal, a protective forest should be built in the northern part of the oasis to block it. The stagnant desert is expanding to the south. Third, there are 422 large and small lake basins widely distributed in the Tengger Desert, with a total area of ??503,400 hectares. Most of them are Splendens splendens, Malan and other grass lakes with no water or very small water area. The lake basin in the Geli Desert has sufficient light and heat, good water conditions, rich groundwater, and a burial depth of 1-2 meters. It is an oasis in the desert and has become a place where herders have lived for generations. The distribution characteristics of this lake are: in the desert. The lake basins in the central and southern parts generally extend 20-30 kilometers long, 1-3 kilometers wide, and cover an area of ??4000-5000 hectares. The lake basins are distributed in a regular north-south parallel arrangement, surrounded by flowing sand dune belts 3-5 kilometers wide. Separation; most of the lake basins on the western and southern edges are irregularly distributed and vary in size. The larger ones are 5,000-10,000 hectares, and the smaller ones are less than 100 hectares. They are fed by many lakes and springs, with good water quality and vegetation. Although the area is small, it is a local animal husbandry base with abundant water and grass. From the above situation, the Tengger Desert, especially in the south, is dotted with lake basins and has some flat and open land with the Yellow River flowing through it. Therefore, The potential for irrigation from the Yellow River is great. It is necessary to strengthen the comprehensive development and utilization of the lake basin beach. While building the existing oasis base, other oases can be built. Fourthly, as far as the soil and vegetation of the Tengger Desert are concerned, the Tengger Desert has great potential. The desert zonal soil is gray desert soil and brown calc soil. The vegetation is dominated by sandy shrubs and semi-shrubs. A large amount of gypsum often accumulates in the gravelly and sandy loamy soil layers; large areas of saline-alkali soil develop in the lake basin. Among them, meadow salt soil is the most widely distributed and grows a large number of halophytes. Aeolian sand soil is the largest soil type in the territory. It is distributed from the edge of the lake basin to the piedmont plain and is the basis for the large flow of oasis plants. There are almost no plants growing on sand dunes, and the coverage is less than 1%; the vegetation coverage of semi-fixed sand dunes is as high as 15%-20%.

Mainly are sand bamboo and Artemisia seed; fixed sand dune plants grow densely, mainly Artemisia ordosica; in widely distributed lake basins, due to better water conditions, saline meadows and swamp vegetation are dominant. The main economic vegetation includes reeds, Splendens splendens, white thorns, salt thorns, etc., with a coverage of 20%-60%. It is the main grazing land and mowing grassland in the desert. There is a certain regularity in the distribution of plants from quicksand to the belly of the lake basin; in the desert The main feed and medicinal plants in the piedmont alluvial plains on the edge and the island hills and mountain valleys in the desert include red sand, pearl, ephedra, holly, Bawang, Tibetan golden pheasant, pigweed, and eucalyptus. Chenopodium, bindweed, shrubs, tansy, etc. There are a large number of small grasses mixed in the grass group, showing the characteristics of grassland. Based on the above situation, in the future, grazing should still be the main use area in desert areas. It is necessary to strengthen the protection and utilization of existing grasslands and control grazing on fixed sand dunes. A rotational grazing system should be established for fixed sand dunes and lake basins. In areas with better water sources, establish Artificial and semi-artificial pastures that combine forest and grass. Fifth, the Tengger Desert is a scientific research demonstration area for desertification control in desert areas across the country. It has achieved significant results in desertification prevention and control, and has been hailed as "a miracle in the history of human desertification control" - one of the world's most valuable desertification areas. It is said to be a first-class desert control project and was awarded the honor of "Global Environmental Protection 500" by the United Nations. In the Zhongwei Shapotou area on the southern edge of the desert, a national nature reserve has been established, and there is the world's first desert railway - the Zhongwei section of the Baotou-Lanzhou Railway. In the future, in terms of management and development, railway sand control should be the focus. Give full play to the advantages of scientific research and production institutions and promote scientific research results and applicable technologies for desertification control. Sixth, continue to aerially sow forage in the desert grasslands on the eastern edge of the Tengger Desert. Alxa Left Banner has aerially sown locally grown fine grass seeds Artemisia annua and Shaguai Zao from the northwest to the edge of the Tengger Desert in the southwest of Bayanhot Town, where the banner government is seated, and has received good ecological benefits. After aerial sowing of pasture, obvious changes occurred in the sowing area, exposing undulating moving sand. The hills and sandy land have become a green grassland, and the quicksand has been fixed or semi-fixed, so that the desert with no grass available has suddenly become the first-class pasture in the whole flag, so that the plant area rate, plant coverage and pasture yield have improved. The growth has doubled, and most of the sowing areas have been opened as winter and spring grazing pastures or as drought- and disaster-resistant grazing bases, and some have been used as grass seed collection bases. In view of the important role of aerial sowing of pasture in Alxa Left Banner in the development of livestock production and wind protection and sand fixation, especially in renovating the land, controlling deserts, and improving the ecological environment, it is necessary to continue to aerially sow forage there and intensify the work. .

Ticket price for Moon Lake Scenic Area: 160 yuan (including 15-kilometer adventure vehicle, battery boat for lake tour) Ticket price for Shapotou Scenic Area: 90 yuan for adults, 90 yuan for children, children under 120cm are free of charge but need to buy 2 yuan insurance !

Where is the Moon Lake Scenic Area

The Moon Lake Scenic Area is located in Alxa Left Banner, Alxa League, Inner Mongolia Autonomous Region. It is a natural lake in the Tengger Desert.

The water surface of Moon Lake is about 2,000 acres. The water is 2 to 4 meters deep, 2 kilometers long from north to south, 1 kilometer wide from east to west, and 4 kilometers around the lake. The scenic area is divided into five major modules: folk customs area, club leisure area, hotel and villa area, ecological demonstration park and outdoor experience area. It can greatly meet the needs of the business, conference, adventure and leisure travel markets.

Moon Lake in the Tengger Desert advocates the advanced concept of "combination of modern civilization and ecological protection", takes "ecological education" as its purpose, and builds a healthy development environment in which humans and nature coexist harmoniously. It is the current domestic desert tourism The scenic spot relies on environmental resources and project implementation to combine "ecological tourism" and "environmental education" into the best desert ecological adventure tourism base.

Natural resources of Moon Lake:

The reeds in the lake are swaying, the lawns on the lakeshore are like carpets, the lake water is rippling with blue waves, water birds are playing, and fish are swimming on the shallow bottom.

A variety of shrubs and grasses such as flower sticks, caraganas, saguai dates, and Haloxylon ammodendron grow around the lake, as well as scattered elms, poplars and Elaeagnus trees. Hundreds of wild animals such as yellow sheep, hares, badgers and pigs are the owners here. Rare white swans, yellow and white ducks, shelducks and other groups live here. The sand peaks and lakes complement each other, making it a fairyland on earth.

The Moon Lake Scenic Area is a desert eco-tourism area with complete water, electricity and communication equipment, convenient transportation, the largest scale and the richest tourism content. The scenic area is located in the hinterland of the Tengger Desert in Alxa Left Banner, Inner Mongolia Autonomous Region, with black The oil road leads directly to the reception station of the scenic spot. It is affiliated to Inner Mongolia Jiuhan Tiancheng Tourism Development Company. It is the desert adventure camp with the shortest radius from major domestic cities and can fully meet the personalized travel needs of tourists.

The combination of resources in the scenic spot is extremely unique. It not only contains the traditional culture of the grassland nomads, but also integrates the desert scenery, Gobi charm, original ecological lakes and Tibetan Buddhism, so that the magic of nature and the inner spiritual needs of human beings are integrated. An extremely perfect blend.

Is there a sea in the desert?

There is a sea

A lake in the desert - Moon Lake in the Tengger Desert

Moon Lake in the Tengger Desert

Pictures of Moon Lake:

Introduction to Moon Lake:

Moon Lake tourist area is located on the eastern edge of the Tengger Desert, in Chaogetu Huresumu, Alxa Left Banner within the territory.

Moon Lake is about 130 kilometers away from Yinchuan Railway Station and Airport, and 80 kilometers away from Bayanhot. There is a 48-kilometer-long tourist road southward from 18 kilometers of Yinba Highway, passing through the Tengger Desert directly to the reception of Moon Lake Scenic Area stop, and then transfer to a "Shunliulun" (a desert bus converted from a military truck) or an off-road vehicle to cross the desert to Moon Lake. Moon Lake has rippling blue waves, surrounded by a desert oasis with abundant water and grass. The lake has a history of 60 million years. The entire lake covers an area of ??4.5 square kilometers and is 1.5 kilometers wide from east to west. It competes with the desert together with several similar lakes, tenaciously performing the miracle of life.

The total area of ??the Moon Lake tourist area is 157 square kilometers, of which the oasis area around the lake is 7 square kilometers, and the rest are mobile desert areas. Moon Lake Tourist Area is invested and developed by Inner Mongolia Jiuhan Tiancheng Tourism Development Co., Ltd. After several years of construction, the entire scenic area has formed relatively complete tourism service facilities. The reception area has naturally formed two areas, namely the transfer station and Moon Lake. tourist resort, the two are 15 kilometers apart.

The transfer station

is located on an oasis 15 kilometers east of Moon Lake. The terrain here is flat and open, surrounded by continuous sand dunes. There is a transfer parking lot here with an area of ??about 1,000 square meters. A tourist reception service center is set up to provide tourists with services such as rest, consultation, ticketing and waiting. The tourist area is equipped with modified military "shun six-wheel" trucks and off-road vehicles suitable for driving in the desert, transporting tourists across 15 kilometers of desert, becoming a unique and exciting tourist activity - thrilling surfing. "Shun Liulun" is a modified military vehicle. It is driven by high horsepower in the desert. It can climb over sand and gorges as if there is no one around. It can also be called a cruiser in the vast sea. Plowing through the layers of sand waves, sometimes jumping to the top of the sand waves, and sometimes falling into the valley of the waves, people can enjoy the thrill and excitement of sand sea surfing and the vastness, roughness and boldness of Tengger.

Moon Lake Tourist Resort

Moon Lake is located in the hinterland of the Tengger Desert and has rich tourism resources. The uncanny workmanship of nature gives Moon Lake three unique landscapes. First, the shape of Moon Lake resembles a map of China: when you look at it from a high place, a map of China covering several square kilometers is displayed in front of you. The divisions of reeds make up the provinces and regions. One is marked; the other is that the lake water is a natural medicinal bath formula: the lake water with an area of ??4.5 square kilometers is rich in potassium salts, manganese salts, a small amount of Glauber's salt, natural soda, trona, ferric chloride and other trace elements, and is recommended by an international health care organization. The formula of bath medicine is very similar. The lake water has great biological purification ability and can quickly improve and restore the true nature of the natural ecology; the third is the black sand that has been in existence for millions of years: the Tianse Bathing Beach beach is one kilometer long and nearly one hundred meters wide. Pushing away its surface layer, the bottom layer is more than ten meters thick. The pure black mud of rice has a texture that far exceeds the black mud of the Dead Sea. It is a natural mud therapy treasure.

Tourism service and leisure facilities such as yurts, holiday cabins, and villas have been built on the oasis beside Moon Lake. White yurts are spread out in a criss-cross pattern on the oasis, like mushrooms that have just broken through the ground. In order to meet the needs of different tourists, the scenic spot also has elegant leisure cabins, villas and presidential suites, as well as glass conference halls. The quaint yurts are also equipped with modern facilities such as air conditioning, closed-circuit television, and telephones, allowing tourists to experience a comfortable vacation environment in the yurts with ethnic characteristics.

The scenery in Tengger in July is even more pleasant, with yellow sand, blue water, green grass, melodious songs, and intoxicating wine. Tourists who come for a hike think it is a fairyland on earth, as if Stepping into the mirage, it is quiet and peaceful. There are many fun activities during the day: sand sea surfing, go-kart racing in the desert, horseback riding in the wilderness, dancing in the clear water with swans, gazing at the stars by the bonfire, falling asleep with camel bells, leisurely paddling in the reeds, medicinal baths in the original ecological sacred lake, and Black sand mud therapy. Moon Lake is quiet and gorgeous at night. Colorful floor lamps, street lamps, and corridor lamps decorate the entire scenic spot into a fairyland on earth. The morin fiddle played and the bonfire was lit. Accompanied by the melodious tune, people who knew each other or had never met before held hands and danced, intoxicated against the background of the desert.

At Moon Lake in the Tengger Desert, people