王屋山世界地质公园，位于豫西北济源市境内，是一座以裂谷构造、地质工程景观为主，地质地貌、水体景观为辅，以生态和人文相互辉映为特色的综合型地质公园。地理坐标为：东经112°01′10″-112°31′50″，北纬34°57′00″-35°16′45″，分为天坛山、黑龙峡、西滩和黄河三峡四个景区，面积约986平方公里。
Located in jiyuan City,northwest of Henan,Wangwushan Nationg Geopark is a comprehensive geopark mainly composed of rift valley structures and geologic engineering landscapes and also of geologic landforms and watery landscapes as well as typical geologic section,paleontology fossil and geologic landform landscapes,characterized by inter–reflecting ecologic and humanistic landscapes.The geographic coordinates are: 34°57′00″-35°16′45″N and 112°01′10″-112°31′50″E,divided into 4 scenic spots such as Tiantan Maintain,Heilong Gorge,Xitan and Yellow River Three Gorges with an area of about 986 square kilometers.
公园概况
王屋山的总体地貌分为中山、低山、丘陵、盆地和平原五部分，中山区起伏多变的远峰近峦，险峻恢宏的悬崖峭壁、深邃幽静的沟谷溪潭，各种动态的飞瀑走泉，在低山、丘陵的衬托下，有时像琵琶遮面，雄伟中又不失几分朦胧与神秘；而它与开阔、规则、整齐、坦荡的平川田园风光则形成了鲜明的对比，总体特征表现为统一中有变化，变化中有统一，节奏感强，颇赋诗的旋律，画的韵味，它的航测鸟瞰效果为明暗对比强烈，阴阳交替复杂；肌理清晰，立体轮廓明显；旷中有奥，奥中有旷，旷奥兼具，其美学价值是很高的。
王屋山世界地质公园是由一系列具有特殊科学意义、稀有性和美学价值的，能够代表本区乃至整个华北地区的地质历史。特定阶段的地质事件和地质作用的典型地质遗迹所组成。主要表现在：①王屋山分布的太古宇林山群、古元古界银鱼沟群、长城系西阳河群、蓟县系汝阳群地层和嵩阳运动、中条运动、晋宁运动系统地反映了古大陆增生、拼接和裂解的全过程，是这一时期极为重要的超大陆地质事件，具有世界对比意义。②王屋山出露齐全的太古宇、元古宇、古生界、中生界河新生界地层层序完好的自嵩阳运动以来的八次造陆、造山运动遗迹，详细地记录了自25亿年以来，华北地区地壳的海陆变迁过程，依然一部记录于石头上的、天然的“地质史书”。③复杂的地质地理背景，系统的地层层序、岩石组合、结构构造和古生物化石以及丰富的矿产资源、生态资源和人文资源，使王屋山成为储存地质信息的“数据库”。④在古大陆碰撞拼接的背景下，导致王屋山在中条期褶皱构造十分发育。⑤在王屋山的天坛山，由不整合面形成的大绝壁虽经改造，残迹犹存；尤其是两期不整合面的“T”形交汇，更是国内少有、世界罕见。⑥在下元古界银鱼沟群的大理岩中，发育了一种与硅化木形状相似的典型构造遗迹，我们称之为“席筒状构造”这种构造截止目前在地质文献中尚未记载。
The overall land feature of Wangwushan is divided into five parts as medium mountain,low mountain,hill,basin and plain.In the medium area the rolling peaks,perilous cliffs,deep valleys and various rough waterfalls and springs,against the low mountains and hills,are sometimes like red sun out of the sea and sometimes like shy girls,showing some nebulosity and mysteries;and it forms a remarkable contract against the open,regular,order and plain field scene with the gross property of variance in unification and vice versa,strong rhythm,and pocetic cadence as pictorial taste.The aviation surveyed bird’s–eyes effect is of strong contrast in brighrness effect,intercrossed and complicated,lt has distinct texfure,mysrery and unconstraint,outstanding stereo profile,boasting very high aesthetic value.
Wangwushan National geopark is composed of aseries typical reics with particularly scientific significance,rarity and aesthetic value,able to represent the area and even all North China’s geologic history,geologic functions in particular periods,which mainly shows:1.The Archeam Forestry Mourth Group,paleoproterozoic Whitebait Valley Group,Changcheng System’s Xiyang River Group,jixian System’s Ruyang Group Stratum,and the orogenies of songyang,Zhongtiao,Wangwushan and jinning distributed in Wangwushan reflect systematically the whole process of acctetion,matching and cracking of rhe ancient continents,which are extremely important supercontinent events with worldwide conteasting significance.2,The complete outcrop of A rcheam,Proterozoic,Palaeozoic Mesozoic and Cenozoic stratigraphic successions and perfectly conserved relics of the eight large–scale epeirogenesis and orogenies in Wangwushan since the Songyang Orogeny have recorded the crust’s changes of sea level in detail in North China in the past 2.5 binllion years,just like a “natural geologic history book” recorded in rocks.3.The complicated geologic and geographic backgrounds,the systematic ctratigraphic successions,rock assemblage,structures,paleontology fossils,and the abundant mineral resources,ecological resources,and humanistic resources make Wangwushan become a “database” of conserved geologic information.4.Against the background of collision and matching of the ancient continents,the folded structures in Wangwushan in the zhongtiao stage were greatly developed.5.ln the Tiantan Mountain of Wangwushan,the residual relics are still reserved due to the plane of unconformity of the latge beetling walls;especially the “T”—shape cross of the planes of unconformity of the fwo stages are rare both at home and abroad.6.ln the marble of Neoproterozoic.
Whitebait Valley Group,a typical structure relic like silicified wood was developed,which we call “mat—roll structure” and rhere has been no record of this kind of structure in geologic literatures so far.
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