大寨石的原岩生成于4.39亿年前的奥陶纪,地层单元属奥陶系中统、峰峰组;岩性为中厚层状海相沉积石灰岩,俗称青石;在漫长的地质历史中,经地壳运动和长 期的流水侵蚀、风化,发生形变。由于当地雨量充沛,坡陡流急,石头被雕刻得千姿百态,横七竖八地半露在山表。奥陶系石灰岩在山西境内分布广泛,仅在大寨及 周边较小的地理区域内,形成孔洞发育,形态奇特,呈大小不等具天然造型的单体岩块群。
垣曲石,产于山西省垣曲县。该石主要为历山石和黄河彩石,有造形石、图纹石。其图纹石色泽鲜艳,形象逼真,石上纹理构成山水、文字、动植物等图案。垣曲石大多采自山岭、河溪、沟岔。黄河流经垣曲县有48公里,县内的历山亦多奇石。黄河水研磨出的黄河奇石,加上县境内另有5条河流,使卵石遍布,千姿百态,奇石资源十分丰富。
河曲黄河石,主要产于山西省河曲县黄河滩头。河曲县境内,出露地层有奥陶系、石炭系、二叠系、三叠系等,基岩多见于沟谷之中,地质多为砂页岩构造。黄河由北 环西向南流经河曲县蜿蜒70多公里,河床最宽处约五华里。河曲地表直入黄河的较大支流有4条,中小河沟37条。
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