Is it a natural phenomenon that rare ice wonders appear in Burqin County, Xinjiang?

Ice landscape is a natural landscape. On the lawn of a green land in the north of Burqin County, Xinjiang, a large-scale ice spectacle appeared, which lasted for 5 hours. The ice hockey formed in the grass is inlaid all over the ground like white pearls, and the thick icicles are wrapped around the branches, just like a dreamy fairy tale world.

There is also a spectacular icing spectacle in Hukou Waterfall of the Yellow River, which attracts many tourists to watch this beautiful scenery. The ice of Yuqiao Reservoir in Tianjin expands due to the cold expansion, and the ice landscape here presents a winding shape.

Also in Xinjiang, the difference is that the ice in Sailimu Lake in Xinjiang hangs upside down on the lake and is set off by snow. Lakes and mountains are like fairyland on earth.

The formation of ice is that when the temperature difference between indoor and outdoor is large, the indoor temperature near the window will become moisture, and then it will condense into ice flowers on the glass.

When the temperature of ice in nature is below zero, water will condense into ice, which can form three forms of ice landscape, including deposited ice, glacier ice and water-formed ice. The ice landscape of Hukou Waterfall on the Yellow River is directly frozen by water, and the phenomenon that water turns into ice can be found in rivers and seawater.

In the process of snow disaster falling in the atmosphere, due to the continuous drop of temperature, deposited ice is finally formed, and glacier ice is also formed by the change and freezing of snow under the influence of temperature.

River ice should be common in our life. Once the temperature of river ice drops to freezing point due to the action of water flow, the temperature of the whole water body will also drop, so the formation of river ice is not only the surface, but also the inside of the water body and the river bottom. However, lakes generally freeze because only the surface of the water body is affected and will condense into ice, while the temperature inside the water body will still be higher than the freezing point, so the ice on the lake surface is generally only a layer on the surface.