Generally speaking, after physical weathering, primary sediments are mainly produced on hillsides and buried in sand or gravel layers. Water-rock mainly refers to riverbed deposition.
The jadeite original stones in Myanmar mainly include rocks, water stones, water-eroded sandstone and primary skinless stones. Rock refers to jadeite wool formed by weathering and accumulation. After physical weathering of general primary sediments.
It is mainly produced on hillsides and buried in sandy soil layer or gravel layer.
Shi Shui mainly refers to the jadeite raw materials deposited in the river bed; Half mountain and half water shell is between rock and water stone; Water-to-sandstone has a thick weathering crust, which is often spherical or oval; Primary skinless stone refers to jadeite raw stone with bare and unweathered skin, which occurs in primary mineral deposits.
Emerald wool accumulated by weathering of rocks. Generally speaking, after physical weathering, primary deposits are mainly produced on hillsides and buried in sand or gravel layers. Generally, the primary surface of this kind of rock is covered with a layer of sandy and muddy weathered skin with different thickness and uneven thickness, which is polygonal or semi-angular in shape and has thin skin with different colors.