Introduction to Thousand Layer Stone

Melaleuca: Also known as cumulite, it is a crystalline dolomite of marine sedimentation. The stone is hard and dense, with a thin weathered layer on the surface and is relatively soft. The texture on the stone is clear, and it is mostly concave and convex. Straight, with a certain rhythm, smooth lines, sometimes with twists and turns; the color is gray-black, gray-white, gray, and brown, with the brown color being slightly more prominent, and the color and texture are more harmonious, making it look natural and smooth; the shape is peculiar, There are many changes, including natural landscapes such as mountains and caves, as well as pagodas, columns, figures, animals and other images. They are both concrete and abstract, with beautiful, quiet, elegant and dignified charm. The original stone is black and gray-black thin-layered strips of limestone, interbedded with white and gray-white strips of dolomite, and is alternately black and white, commonly known as "Black and White Road". Due to the difference in lithology between the two, different dissolution conditions are created, forming a shape with clear bedding and distinct concave and convex strips, often presenting a landscape of mountains, caves, holes, and ravines. Varieties include black and white stone, dragon scale stone, turtle stone, lotus stone, bamboo leaf stone, caviar stone, etc. Black and White Road is a unique thin-layered gray-black micrite-microcrystalline limestone produced in the Wangshan Formation in the upper part of the Sinian System, which is interbedded with thin-layered yellow-green, light gray, and gray-white powdery fine-crystalline limestone. Appears as a combination of black and white parallel strips. Produced in the Guoji area of ??Tongshan; dragon scale stone is also called the "money stone". Turret stone is produced in the medium-thin dolomite layers of the Jiudingshan Formation and Niyuan Formation of the Sinian System. Most of them are layer structures formed by mud cracks, forming crack textures and complex interlayer textures; Lianhua Stone is produced In the upper section of the Fengshan Formation of the Upper Cambrian, geological technicians commonly call it "Da Wo Juan", which is a stratigraphic marker layer. It can be seen in places such as Tongshan Hanwang; bamboo leaf stone is a block of stone formed by weathering and karstification of gravel limestone. Produced in the mountains around Banjing Village, Hanwang Town, caviar stone is an oolitic limestone. It is named because the rock is rich in caviar-like oolitic grains. It was formed in a warm shallow sea environment with small water depth and strong current activity.