历山石是属于黄河中游偏下的黄河石的主要构成。它形成于长城系底部,相当于常州沟的沉积地层,其同位素年龄在17-17.5亿年之间。它是当年的滨海沙滩、沙堤、沙坪环境下沉积而成。久经海水淘洗磨蚀,已成单矿砂岩,石英砂含量在90%-98%之间。人们利用它在成岩作用同时成稍后的地下水携带的铁锰质胶体,从沙粒间的空隙和岩石裂隙渗入凝结下来棕色、铁锈色、红色的环带构成行云流水、崇山怒涛。 Lishan stone is the main part of the Yellow River stone which is below the middle reaches of the Yellow River. It is formed at the bottom of the Great Wall System, which is equivalent to the sedimentary stratum of Changzhou Gully. Its isotopic age is 17-17.5 billion years. It is the year beachfront sand, sand embankment, Shaping environment deposited. Long after the sea washing erosion, has become a single mineral sandstone, quartz sand content of 90% -98%. People use it in the diagenesis at the same time into a later groundwater carrying ferromanganese colloid, sand and grain from the gaps and rock cracks into the condensation of brown, rust-colored, red belts constitute the clouds, water, mountains.