You've been talking about watanabe, and today mr. Ding used an article to show you how kop and tamayu were formed, and how seeds, mountains, mountain currents, goblins, etc. Were formed
I. The formation of yamada
The formation of watanabe began with the crust movement hundreds of millions of years ago:
The albino marble layers of the sea floor are invaded and baptized by hot magma from the ground。
In high-temperature and high-pressure environments, rock structures deteriorate, resulting in the formation of primary ore bodies of tanyu。
Ii. Formation and characteristics of the four main species
1. Mountain material (primary)
Mountain material formation: the primary jade mine, directly from the mountain, is the most primitive state。
Mountain characteristics: the size of the blocks varies, they are elliptical, they are rough on the surface and they vary in size. Textures are generally less favourable than seeds, but may also produce high-quality jade。
Mountain currents (secondary mines, upstream rivers)
Mountain currents form: raw jade mines fall by weather and are transported to the upper part of the river by floods and rivers。
Water characteristics of mountain currents: elliptical angles are slightly rounded, larger in size, smoother on the surface, often with water ripples, delicate in quality, between seeds and mountains。
Seeds (secondary mines, downstream rivers)
Seeds form: mountains are long-term weathered, collapsed, transported long distances by rivers, washed and eventually deposited downstream。
Seed characteristics: multiple pebbles, smooth surfaces, no angles, different sizes and different shapes. Because of their high quality, they are the highest price on the market today。
4. Gobi (secondary mine, gobi bay)
Gobiformation: primary or current water is transported to gobi by geological movement and exposed to the ground for long periods。
The goverine characteristics: long-term erosion by wind and sand, visible graft on the surface, and hard texture, clearly distinguishing from the other three。
