What kind of car do I need to go to Tibet? What are the characteristics of the Tibetan sandgrouse?

The climate in Tibet in August is very comfortable, with temperatures between 10° and 25°. It is neither dry nor humid, nor as stuffy as in the mainland. You can wear thin long clothes and trousers during the day. Comfortable cotton underwear is recommended, so that you won't feel sticky even if you sweat a little. High-top outdoor shoes are recommended. At night, the temperature in these places will drop to several degrees below zero. At this time, sweaters and down jackets should be added. A fleece windbreaker can achieve a good warming effect. So what kind of car do you need to go to Tibet? What are the characteristics of the Tibetan hairy-legged sandgrouse? Let's take a look at the introduction of the Encyclopedia Knowledge Network!

Contents of this article

1. What kind of car do I need to go to Tibet?

2. What are the characteristics of the Tibetan sandgrouse?

3. The largest lake in Tibet

What kind of car do I need to go to Tibet?

It is best to drive an off-road vehicle. Many mountain roads in Tibet are unpaved gravel roads. When it rains, cars are basically unable to cope with it. Small mudslides frequently occur in Tibet. Although the possibility of destroying the road is very low, it is easy to block the way of cars. Therefore, off-road vehicles are the first choice. Four-wheel or all-wheel drive is a necessary function for all off-road vehicles. Even if those fashionable SUVs designed specifically for cities have four-wheel drive functions, their frames are often low. It is easy to break down when driving on undulating roads. At that time, no one can help. Use professional off-road tires. The shoulder tread blocks of professional off-road tires are arranged in a toothed shape, which has the effect of digging mud, sand and gravel.

What are the characteristics of the Tibetan sandgrouse?

The Tibetan Sandgrouse is a bird of the genus Sandgrouse of the family Sandgrouse. It is commonly known as the Sandgrouse. The Tibetan Sandgrouse inhabits deserts, grasslands, semi-deserts, alpine meadows and grasslands near lakes at an altitude of 3,500 to 5,100 meters. It likes to gather in groups. In summer, it moves in groups of more than a dozen. In winter, it often gathers in large groups of hundreds. It forages in open areas. It flies fast but flies low. It feeds mostly on the flowers, leaves, buds, seeds of leguminous plants and seeds of other plants. Sometimes it also eats small insects of the order Coleoptera. It digs holes in the ground and lays 3 eggs per nest.

It is a bird of plateau forests and shrubs. In summer, it likes to live in spruce, dense forests (with mosses on the ground under the forest) and understory shrubs. In autumn, it migrates to riverside forests and sparse forest belts with lower altitudes. It is highly gregarious, and the largest group ever seen was 31. It occasionally moves in mixed groups with blue pheasants. It is omnivorous, but mainly feeds on plant food. In summer and autumn, it mainly feeds on young spruce branches and leaves, mosses, seeds of Polygonum stems and early grass, and in winter it almost exclusively feeds on mosses. It occasionally feeds on animal food. In the 13 stomachs we dissected, we found fly larvae once. In early July, we obtained three chicks about 4-6 days old, and at the end of July, we saw a female chick leading four chicks to forage. The blood-sucking pheasant begins to lay eggs and reproduce in May in the Qilian Mountains.

The largest lake in Tibet

Selin Co., which means "the devil's lake with majestic light" in Tibetan, was once named Qilin Lake and Selindong Co. It is the largest lake in Tibet and the second largest saltwater lake in China. It is a tectonic lake formed during the formation of the Qinghai-Tibet Plateau and is a large deep-water lake.

The Selin Co and Bange Co lake basins are newly developed fault basins based on the Bange fault basin that began to develop in the early Paleogene of the Cenozoic Era and were activated and developed in the Quaternary Period. The long axis of the basin is nearly EW-oriented, and new structures are developed on the north and south margins. It has been uplifted along with the overall uplift of the Qinghai-Tibet Plateau since the Middle and Late Pleistocene. The large lakes have gradually shrunk, and due to local uplift differences, the large lakes have been divided, gradually forming the modern distribution pattern of multiple lakes. [5] Before the late Late Pleistocene, Selin Co and Bange Co were a unified large lake with an east-west long axis. In the late Late Pleistocene, they were divided into two lakes, which are distributed in an east-west direction. There is still a narrow waterway connecting the two.