Are there any fish in the water of Huata Village in Lingqiu?

Zhangjiakou city is characterized by its high northwest and low southeast. It is divided into two natural areas, namely, the northern dam and the southern dam, with the boundary of the Malaysian Mountains watershed. The northern dam includes all the three counties of Zhangbei, Kangbao and Guyuan and most of shangyi county. It belongs to the southern edge of the Inner Mongolia Plateau, with an altitude of 1,3-1,6 meters. The terrain is open, the grassland factory is wide, and there are many inland lakes (Nao). Gangliang, lake, beach and grass slope are distributed alternately, showing a typical undulating plateau landscape. The total land area of the four counties is 13,8 square kilometers, of which Bashang Plateau covers an area of 12,9 square kilometers. The southern dam is located in the transitional zone between the North China Plain and the Inner Mongolia Plateau, and the terrain is relatively complex, which can be divided into three types: one is the river area dominated by Yanghe River, Sanggan River and its tributaries, with an altitude of 5-6 meters and a total land area of 6,119 square kilometers; The second is the shallow hilly area formed at the foot of the deep mountain area, with an altitude of 8-14 meters and a total land area of 4387 square kilometers; The third is the deep mountain area around the hilly area, with an altitude of more than 12 meters and a total land area of 1345 square kilometers. According to the landform, Zhangjiakou Bashang Plateau accounts for 35%, rivers and basins under the dam account for 16.6%, hills account for 11.9%, and mountains account for 36.5%. The landform and landform are complex, and the land resources are rich and diverse. There are obvious differences in microclimate between regions, which is beneficial to the cultivation of various crops? Datong is located at the junction of Shanxi platform anticline and Yinshan uplift of North China platform. Beikou Uplift in the north, Datong-Jingle Depression in the southwest and Sanggan River New Fault Depression in the southeast. In this area, a series of tectonic traces have been formed during the multi-stage crustal tectonic changes, especially the Yanshan movement and Himalayan movement, with well-developed neotectonic movement and frequent seismic activity. In the east, Datong Volcano Group, a famous geological wonder in the world, and Tengchong, Yunnan, constitute two major volcanic groups in the north and south. Form a basin, commonly known as Datong basin. In terms of landform, the mountainous area of Datong is 278 square kilometers, accounting for 13.4% of the total area; The hilly area is 1177 square kilometers, accounting for 56.6% of the total area; Pingchuan covers an area of 626 square kilometers, accounting for only 3% of the total area. Among them, mountains and hills are mainly concentrated in the west, north and northeast, while Pingchuan District is located in the southeast. This constitutes the main characteristics of Datong city, which is high in the northwest and low in the southeast, and the terrain is inclined from northwest to southeast. Datong is located in the intersection of Yinshan Mountain in the south, Yanshan Mountain in the east, Luliang Mountain in the north and Taihang Mountain in the north, and it is the passage for birds in the central part to move south headed by geese. The northwest mountains belong to the yinshan mountains and Lvliang mountains, mainly including Baideng Mountain, Shuang Shan, Erlang Mountain, Yunmen Mountain and Cailiang Mountain. The mountains in the southeast belong to Taihang Mountains, mainly including Hengshan Mountain, Taibai Mountain and Liuling Mountain. The general elevation of the whole city is between 1 and 15 meters, the highest point is Huangyangjian of Liuling Mountain in Yanggao County (242 meters above sea level), and the lowest point is the exit of Ranhe River in Huata Village in Lingqiu County (558 meters above sea level). Sanggan River runs through the city from southwest to northeast, forming a trough-shaped basin with high periphery, low middle and two mountains and one river. Besides Sanggan River, the main rivers in China are Yuhe River, Nanyang River, Huliu River, Tanghe River and Cangtou River, which belong to Haihe River system.