云台山是第三大地质山貌公园。
12亿年前的海滩遗迹
我们脚下这一片色调鲜艳,纹理优美的红色岩石,为石英砂岩,它是在距今12亿年前后的滨海沙滩环境下形成的,伴随着当时海平面的上升与下降,潮涨与潮落,云台山一带时而沉入海底,时而露出海面,岩石中保留的交错层理及波痕、泥裂等丰富的沉积构造遗迹,就是当时古海洋存在的证据。
1.2 Billion-Year-Old Seashore Vestige
The bright colored and beautifully textured red rock under our feet was formed out of a seushore 1.2 billion years ago.With the rise and fall of sea level, and the ebb and flow of tide,Yuntal Mountain sometimes sinks into the sea, and sometimes rises out of sea. leaving abundant sedimentary structure vestiges, such as cross strata and ripple marks, mudcracks, in the rocks. These vestiges are the evidence for the existence of the ancient sea.
34亿年锆石采集地
地球形成距今已有46亿年的历史,研究地球演化历史、探索地球形成原因,一直是科学家们长期以来所关注的重要领域之一。2005年地质学家在开展云台地貌景观形成的地学背景研究过程中,在此地采集了太古宙的岩石样品,由北京离子探针中心对其中的锆石年龄测定,获得了3398±8Ma(34亿年)的定年数据,这是目前河南省境内发现的最古老的地质年龄值,对研究地球早期古陆分布以及演化具有重要意义。 Site Where 3.4 Billion-Year-Old Zircons Were Unearthed
The Earth came into being 46 billion years ago. Its evolutionary history and how it was formed have long been one of the main focuses of the scientific research. The zircon in the rock samples collected by geologists who were conducting geoscientific research on the formation of the topography of Yuntai Mountain in 2005 is dated at3398±8Ma (34 billion years) by Beijing SHRIMP Center. It is the oldest rock ever found in Henan province so far and of significance to the research on the plate distribution in the early years of the earth and the evolution of plates.
幸福渠
现在您的脚下便是幸福渠,1958年春开始修建,历时十七年建成,全长92.3公里。它的修建解决了云台山及周边地区老百姓饮水灌溉难的困境。幸福渠横跨崇山峻岭,迂回曲折于悬崖峭壁间,施工环境十分艰险,是修武县人民战天斗地的结果和智慧的结晶。今天大家的旅游仍然在享受着幸福渠的恩泽。 Happy Channel
You are standing on Happy Channel, which, running 92.3 kilometers, began to be built in the spring of 1958 and took 17 years to complete. The completion of the channel has solved the drinking and irrigation problems on Yuntai Mountain and its surrounding area. As Happy Channel runs through high mountains and treacherous ridges and winds along the cliffs, the working condition at the channel construction site is dangerous. The channel is the fruit of the wisdom of local Xiuwu citizens and their struggle against nature
赤壁丹崖的成因
赤壁丹崖是云台山的典型景观之一 长250米,高1
米,其岩石为距今12亿年前后形成的紫红色石英砂岩,在太行山形成过程中,由于断层的错断和风化剥蚀作用,使得这套古老的岩石能够出露于地表。犹如大自然的鬼斧神工给云台山在这里开了一扇天窗,才有了红石峡的美景和壮观的赤壁丹崖。赤壁丹崖就是断层活动形成的断层面。 Cause of Formation of Red Danxia Cliff
Red Danxia Cliff, 250 meters long and 150 meters high, is one of the imposing landscapes on Yuntai Mountain, with purplish red quartz sandstone which formed 1.2 billion years ago. Due to the faulting and weathering during the formation of Taihang Mountain, the rocks are surfaced to shape the beautiful Red Stone Gorge and Red Danxia Cliff, as if nature skillfully carved a sun-roof on Yuntai Mountain. Red Danxia Cliff is a fault plane resulted from the faulting.
砂岩红色之谜
形成红石峡的这套红色石英砂岩的总厚度,在云台山地区达150米,它构成了红石峡谷岩石的主体。砂岩的红色是岩石中铁质成分氧化形成,由于铁质含量不均匀导致砂岩颜色的深浅程度不一样,构成了造型优美的各种图案。 The Riddles of Red Rocks
The red quartz sandstone that forms Red Stone Gorge and makes up the main constituent of Red Stone Gorge is 150m thick on Yuntai Mountain. The redness of the rocks is resulted from the oxidation of the element iron that occurs inside the rocks. An uneven distribution of the element iron among the rocks leads to a diversity in the shade of the rocks, and thus beautiful patterns are formed.
红石峡苑区
红石峡是一条距今14-10亿年之间沉积的红色石英砂岩在地质作用下形成的线状峡谷。2300万年以来,由于新构造运动的强烈
抬升和水蚀作用的深度切割,使此处的红色石英砂岩形成了高达 United Nation Yuntai
150余米的丹崖断墙和高悬于丹崖断墙之上,长2000米,深达百余 Educational,Scientific and Cultural Organization Global UNES
米,宽仅数米一数十米的碧水丹峡。峡内瀑泉飞泻,溪潭珠串,
谩步崖壁栈道,悠尽可领略丹崖、碧水、蓝天构成的一幅幅经典画卷,还可欣赏砂岩层p的交错层理、层面波痕、龟裂构造等丰富的沉积遗迹。
Red-stone Gorge Scenic Area
Red-stone Gorge is a lnear gorge formed by rea quartz sandstone deposited under the geology structure about 14-10 illin years ago With strong uplift of neotectonic movement and deep incision under water erosion, the kind of sandetone foms a red cliff with the hight of more than 150 meters and a red gorge with the length of 1500 meters, the depth of more than 100 muaters and the width of only several meters to tens meters. in the scenic area. Waterfalls are pouring down. srings fowing and streams gurgling, and ponds are calm, appearing a string of beads. When tambling over plank road hn in jlmg a uth the vpitors will catch a charming landstape formed by red ciff clear water and, blue sh cah geolony tove. includint some chipracteristic sediments, like red quartzose sandstone one bllion yan ago, and hoe strucruse like bedding plant structure. stracture the cos buiding. Again, the ylators can
黑龙王庙断层
黑龙王庙断层是景区内最主要的断层,长度约10千米,最大断距可达700米,它控制了云台山地区风景地貌的格局,红石峡和百家岩的丹崖断墙景观就是典型的黑龙王庙断层面。
Black Dragon Temple Fault
Black Dragon Temple fault, the main fault in this tourist attraction, is 10 kilometers long with a maximumfault displacement of 700 meters . It dominates the landscape and topography of Yuntai Mountain, and is typified by Red Stone Gorge and Danyia Cliff of Baijia Rocks.
以上是红石峡的一处风景,用手去触摸千亿年的岩石,让你的灵魂都充满坚韧性,我慢慢扑捉大自然的神韵,见证者自然界的鬼斧神工。
做在大巴车上,当长长的巴士穿越在陡峭悬崖之间时,自己的心脏感觉都不淡定,但是看到司机师傅的高超的开车技术时,心情慢慢打开,随着巴士车在环形山路间攀岩而上,感觉人间奇迹。
真的感谢司机师傅的开车水平,让我看了景,好像捡了一条生命。灵魂震撼的同时,生命也成了自然界的部分,感到人在34亿年前活化石前的渺小,体会着她带给我生命的坚韧性。
在抬眼望去的山峰之间,你看到一个词,水墨山水,在吴冠中的笔下总是能感觉山水的水墨丹青,总以为是文人墨客的笔作,不会想到世间真是这样的有着在山峰上有种忽隐忽现的泼墨山水,第一次深切的感到画作和真实之间原来如此贴切和生动。
谢谢你修武云台山。
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