17, Qi Yunshan National Geopark in Anhui
Anhui Qiyun Shan National Geological Park is located in the scenic city of Huangshan in East and West-16 km, north-south width 6.9 km, area of 110 km2. Danxia Geopark in the typical landscape features, combined with dinosaur fossils, Taoism culture, Cliff stone in one. Qi Yunshan, Guchengbaiyue, Huguangshanse, scenery unlimited. Danxia landform complete its type, is Fengcong-Danxia landform, set extraordinary and dangerous, Sau, the United States in a region Qifeng ZHENG Rong, Guaishi rugged, Danya Chibi-risk legislation, re-stack Luan, Qianzibaitai. Represents about 90 million years ago Late Cretaceous since the terrain in the ongoing development of the geological model of the role. Qi Yunshan Danxia landform in the long geological history have, from evolution. In 9000 to 65 million years ago between the late Cretaceous sediments of the purple conglomerate, sandstone beds in the shallow lake - the foothills of the river sediments, Qiyun Shan group and formed a small rock group, has a base period of basalt eruption, Qi Yunshan Danxia landform constitute the material basis. And stable output into the basalt layer has also Danxia landform a beautiful mosaic "lace." 5300 million years ago at the Tertiary Himalayan basin comprehensive campaign to uplift into eroded area. Several million years in the uplift process, due to differences between movements, Qi Yunshan the uplift rate higher than the surrounding areas, relatively higher than the 100 ~ 300 m. Uplift developed in the course of the fracture, joint, formed a Qi Yunshan Danxia landform of the exhibition Bouguer; formation near the level of occurrence and lithologic differences, as a platform, Yadong, such as the formation of Danxia landscape has provided the conditions. Crustal uplift, water and gravity Qi Yunshan Danxia landscape is a direct form factors. The role of water of which the most significant erosion, ground water erosion washed away the rock, the first along the vertical joints of a gully development, water continued to scour erosion, gully widening will deepen a gully. Such as "Wulong peak" landscape, water is scouring the valley formed, tied for the formation of Wufeng wonders. Rock the edge of the valley, along under the gravity of the joint-caving, a cliff, the relative height difference dozens to several hundred meters, the highest cliffs of 300 m, such as "Zixiao wall" and "really Cavity House." Rock role in its own gravity load, tilt to the valley along the joint surface opened deep fissures and a peculiar form of "frontline" landscape, a rock caving Dan Wall, the collapse of a form of rock landscape. The next water erosion and crustal uplift the role of co-evolution of the valley for??Xiagu, such as "nanmu Valley." In addition, the park also has distribution of the Mesozoic Cretaceous Qi Yunshan Standard stratigraphic section relics, fossils of dinosaur bones, dinosaur egg fossils, fossils of dinosaur footprints, dinosaur fossil remains of trails and the Himalayan orogeny and new tectonic movement, and other relics.

18, Qinhuangdao in Hebei Liujiang National Geological Park

Qinhuangdao in Hebei Liujiang National Geological Park is located in Qinhuangdao City of Hebei Province, south Bohai Sea, according to the Yanshan North, East and bordering Liaoning, adjacent to the West and Tangshan. Area of 650 km2. Geological Park in paleontology fossils, remains of formation, karst landforms and geological features granite features. The core of the geological park, located in Qinhuangdao, north of Liujiang River basin, its southern edge from Qinhuangdao City 12 km, with 240 km2, includes a retrospective on the geological history of great scientific value of the typical profile of the type, fossils combination with stratigraphic section, the rock Construction of the section of rock and geological structure typical profile and structural features,
Rich content, for domestic rare. And the formation of its three sets of three rocks are widely distributed, both natural outcrop, stratigraphic integrity, clear boundaries, rocks complete fossil rich, sedimentary structure development, is recognized as "natural geological museum." Various types of structures. The folds of different sizes, different levels of fracture and kneading surface, traction, fissures, dykes, such as filling macro, micro-structure development, and acting clearly. Various types of structural features of the crustal movement on the development history of the region is of great significance. There are metal, non-metallic mineralization, the mine; karst formation of the CPS, the cave, the courtyard and stone bud, dissolved ditch; formed by water from the reactor Hill, or water, river terraces, and other geological relics. National Geological Park, a blend of many in the health, external deposits, but mostly because of small-scale mining and inappropriate, but suitable for popular science education, its causes and analysis has important significance. The fourth of the accumulation of holes, so that people can understand prehistoric biological communities, habitats and biological evolution, it is important to scientific research, popular science bases. 25 to 16 million years ago between the granite mixed Beidaihe, the Shanhaiguan well-known tourist area of geological background 5.4 to 2.5 billion years ago between ancient marine sediments in the limestone formation of the CPS, the cave, and so rare in North China's karst landscapes; ago 2.5 billion years to 65 million years between the Mesozoic granite tall majestic mountain, a steep difficult to form a mountain scenery; marine geological formation of modern China's largest coastal dunes and lagoon, formed a variety of sea, the marine landscape; nature The Guifushengong, created Qinhuangdao "open days Haiyue" Jingshi beauty.

19, the Yellow River Hukou Waterfall national geological parks ? ?

Yellow River Hukou Waterfall national geological parks in the Yellow River as the axis, across Shanxi and Shaanxi provinces. Hedong have Lvliang Shan, trying to Huanglong Mountain. Xiongzhi mountain here, the huge momentum of the Yellow River meandering river stretch. Their things from both sides of the boundary river on both sides were extended to the centerline of about 1.5 km. It was magnificent the Hukou waterfall as the main geological relics. Yellow River Hukou Waterfall on the Yellow River is the largest waterfall. It Feiliuzhixie, monstrous waves, Qitunshanhe, Zhen Tian Tao field, the two sides residual Cliff cliffs, become a world wonder. Falls the upper reaches of the Yellow River water-300 m, in less than 500 m long, was compressed to 20 ~ 30 m in width. 1000m3 / second of the river, from over 20 meters high and crash into Douya on, resulting in "a pot of a thousand miles to the Yellow River" spirit. Overwhelming impact of the waterfall as a rock "Valley Stream Xianglei" the roar; Jutao aroused Shushi Mi-spray, much as "water smoke," the landscape, the sun guide to the "Rainbow Forum" beauty. Falls are the bottom left-flowing water eroded the ground floor gallery can look up to waterfalls "The Yellow River water to the sky," the magnificent scenery. "Shili-tank" to the waterfall is the source of erosion cutting the results of a total length of 4200 m, width 30 ~ 50 m. Yellow River is the most narrow. Constraints in the river, the river Pentium growl, Zhuolang roller roundabout, magnificent. Falls from top to bottom on the bedrock, water erosion seen everywhere, big and small water trough and get to carry the gravel pit round loss, this is the famous "Danwobaojing": strong cut next to the river, the original shore of Mountain Hardware Heart Island into the river, and Bangladesh at the top of the island, the bottom of Huludao. "Bangladesh doors Yeyue" King is the full moon night, watching the sky river in two months Xiangying "floating on the spray as" Night. Hukou Waterfall of the formation and the local formation, construction, climate and hydrological conditions of the natural geographical factors. Hukou area of exposed bedrock is about 2 million years Triassic Zhifanggou group (Group), the upper part of the purple, green sandstone and mudstone inter-category, the lower part of the thick layer of sandstone, thin layer of sandstone and shale, because Soft and hard rock in the valley of the turn, so that water can exacerbate the erosion of the role. Hukou Waterfall formation of Indo-Chinese movement was due primarily to 2.3 billion years the role of the results, the formation of two joints, a group of straightening out the flow of the river; another set of joint development for the crossing. In addition, these two groups along the joints in the gestation of the waterfall, and the formation of the demise of a number of faults have emerged. As in Hukou and the mountains south of Bangladesh gate formation dip is very small, joint development, fault occasionally, and a stratigraphic level, so easy to cut structural role of the fragmentation. Therefore, the Hukou Waterfall is the formation of joint fault development and river erosion under strong cutting caused by two major factors.

20, Zhanjiang in Guangdong Hu Guangyan national geological parks ? ?

Hu Guangyan Zhanjiang City in southwest 20 km, Huguang Jinbuk West 4 km. An area of about 22 km2. Geological Park to ring the crater lake and geological remains the main hill fire. Kouhu similar to the volcano-shaped park, an area of about 2.30 km2, the largest water depth of 22 m, the water temperature gradually reduce the top down, from 27 ? to 17 ?, better water quality, crystal clear waters. Ring the fire were closed around the volcanic hills Kouhu, mainly from volcanic rocks constitute, in the hills ring the fire Chang Lin Hu side of a cliff Doubi, outside of the gentle slope. ? Hu Guangyan away 15 years ago after the eruption, volcanic mouth water into the lake depression. Eruption deposits kept very complete, the eruption of various mobile structure is very clear, diagenetic after the destruction of faults, can be seen everywhere, to study the volcanic diagenesis, the new tectonic movement provided a sufficient basis. Hu Guangyan is found that the typical domestic "Mallon Lake", the world is a rare, Hu Guangyan Mallon Lake lakebed sediment thickness 50 m, its real record of the Earth in modern times over 10 years since the ancient climate, ancient Changes in the environment in China is to study Mallon, and Mallon of the volcanic eruption of the lake formed an excellent venue.

21, Hebei Fuping Tianshengqiao national geological parks ?
Hebei Fuping Tianshengqiao national geological parks, the county seat from the West about 25 km, area of 32 km2, to Zhu Baicao-long camp to the waterfall group, Yaotai Galaxy waterfall on the rocks and metamorphic rock landscape of geological features section. Scenic areas for the type of metamorphic rock geological features tectonic erosion block Hill, wins mountain range overlap, Cangshan sea. Geological Park in two parts: First, Zhu camp Tianshengqiao Falls Scenic Area and the other is about 25 billion years away from the ancient sector Longquanguan standard geological sections. Tianshengqiao is located in the 112 m waterfall top surface, the peculiar structure of the bridge deck, under a micro-arch bridge, a metamorphic rock to the Tianshengqiao rare in China. Visitors to walk the bridge, the water underneath the river, the bridge before the Baizhang abyss, the bridge after a clear water lake. People both daunting and Liulianwangfan. Tianshengqiao long bridge trees, water underneath, the upper reaches close to 60 m gap between the eighth waterfall, waterfall 8, 9 waterfall connected, Li Bao Shui Kiu wait-and-see, waterfall splashing into the culvert to spend, the more Chuandong over the abyss, mountains, water , Trees, bridges among Ying Chen. If curtain of water from top to bottom, before and after Hill Bili, around the tree Congcong, the wet period Feiliu , such as Wanmabenteng, thundering sound; dry season, Chan Chan flowing water, such as spreading Chu Yu-throwing, Shengyun clear. Pushui into the winter ice, crystal icicles; different attitude, the phenomenon is to watch the winter. Stand the meantime, can fully enjoy the beauty of nature. Fuping Tianshengqiao National Geological Park Set geology, geomorphology, water resources, ecosystems, human history, such as integration of tourism resources, it has a high scientific value, ornamental value, the value of ecological protection model.

22, Sichuan County Reef Geological State Park ? ?

Sichuan County Reef Geological State Park is located in the northwest county, mountain forest, the valley aspect, Podou a deep valley, the higher ground, the ridge above sea level in more than 1200 ~ 2000 m between the Qianfo Shan peak elevation 2922 m, area of 508 km2. Geological Park to Sham siliceous limestone reef sponge reefs and the formation of geological features features. County in the area, about 2.3 billion years late Triassic formation of the reefs of the six radio siliceous sponges, sponge has identified six new branches, 31 are new, new species 55. 6 radio Qianzibaitai siliceous sponges, colorful, a goblet, bowl, pot-shaped, straw hat-shaped, honeycomb-shaped, petal-shaped, and so dozens of forms, the smallest to the shortage 1 mm, the largest diameter of up to 80 cm, is currently the world's Found that the biggest sponge. County sponge reefs of the reef high 40 ~ 60 m, while Europe's largest Jurassic sponge reefs only about 20 m high. Currently County and nearby surface that the reef is more than 100, reef distance ranging from 100 ~ 2000 m, in a landscape on the Rock Hill processes, as shown in the Piedmont LONGMENSHAN distribution, the distribution area of about 266 km2, buried in the ground The reef more than 700 of these have fully reflected the sponge area at the time of the extremely prosperous group. The world's reefs in shallow water main, Deep Water reefs rare. Sponge reefs are usually mainly calcium, silica rare; County found for a typical rare Sham siliceous sponge reefs, growth depth of 100 ~ 200 m. The rest of the world have found that the six-launched siliceous sponges very scarce, mainly fossil fragments, are far from complete, do not form a reef. Jurassic sponge animals in the sudden proliferation of Europe, which in the past is a mystery. Research has proved that China's County along the six-launched siliceous sponges may be the ancestors of the European siliceous sponges. County sponge reefs grow at about 2.3 billion years late Triassic ancient Mediterranean east coast of the Gulf, and later gradually ancient Mediterranean retreat westward to Europe, the sponge animals such as land and sea changes in the migration westward, after a few million years across the Euro-Asian migration and the evolution of large, settled only in Europe. County sponge reefs around the discovery, filled a sponge in the history of animal evolution of the gaps, but also remove the ancient Mediterranean Sea Change and the European Jurassic sponge origin of the mystery.

23, Shandong Zaozhuang XIONGERSHAN national geological parks ? ?
Shandong Zaozhuang XIONGERSHAN national geological parks with a total area of 98 km2, a karst geological features and Bao Dugu landscape features. Zhi-mountain region stacked, vertical and horizontal Gully, a small hill over 40 blocks, elevation 211 ~ 584 m in between. Mountains were flying geese-shaped array. To XIONGERSHAN and Bao Dugu as the basis, the Great Rift Valley-Ssangyong, the cave group, (Long grasp Cliff), (failure), Springs and the most typical Gushan-shaped landscape as one. Bao Dugu for the first summit, elevation 584 m, with its unique ancient times the "male" and "surprising" and "dangerous", "show" and known in the first Lunan 72 Gushan, known as "Lunan on the Mount Tai" This is known as "Tianxiadiyi Gushan." XIONGERSHAN elevation 481 m, is a unique Shandong Province, North China's karst geological features rare natural wonders. Karst region, the variety of cave group, Qixingguaizhuang the stalactite, Ssangyong Tiancheng Qijue the Great Rift Valley, wonderful changes. Hand Qingtian Stone Forest such as small, Yousi blooming lotus, grasping Yaxia giant dragon-shaped limestone spelled at the Rolling Stones, all demonstrate the power of nature. Gengjian Springs Congcong, Huguang charming. Constitutes a geological park XIONGERSHAN unique geological landscape. Construction along some form of giant cave was never turned into a sigh of small canyon. XIONGERSHAN Ssangyong such as the Great Rift Valley, about 500 m, depth of about 40 m, a width of 15 m. Stalactites in the development of rock can be seen on the tectonic breccia. Valley has its holes, holes have holes, the formation of stalactite cave-Qianzibaitai, Wei Cheng-concept. In the valley, rock, water Infiltration karst fissures encountered Geshui-emission, a large number of Springs. Rock and wind in the region of the balance of the ability to form a common development of the region and at home and abroad typical Cambrian limestone table-shaped mountain - Gushan-shaped landscape, is also carbonate Qifeng. At the same time, structural karst development in the region, limestone, shale, sandstone weathering the difference between the seismic, gravity and other factors role, the local mountain collapsed in landslides and rock, such as cleft mountain valley west of the landslide and the east Long grasp of the Maya (rock collapse) is a typical geological disaster relics. Not only that, the region also has a profound historical and cultural background, weed trees, a rare natural habitats, wild diverse plant and animal species. Discovered deep forest, stunning is that people are a good place for leisure travel.

24, Fushan National Geopark in Anhui ? ?

Anhui Fushan National Geological Park is located in Anqing City, Anhui Province Cong Yangxian in from the Congyang Xian city 36 km, from Tongcheng 40 km, its direct access to the Yangtze River waterway, the total area of 76 km2. Geopark type of volcanic features. Fushan preserved volcanic features, typical patterns, nearly circular plane, a diameter of about 4 km2, an area of about 14 km2, while the ground was high, middle and lower basin Au, a typical collapse volcanic depression, choose a type of rock, structural features clearly visible . Qiong, a composite Qiu, crater, the volcano bell, volcanic residue (pumice) and lava flows, ring and radial fracture, turtles, such as crack. Fushan in the ladder to Lotus Peak area, formed by volcanic ash-melting guitar tuff the weak level, the common area exposed to the irregular polygon cracking structures, shows the layered rocks at cooling contraction of specific sites, crack vertical rock Level under the rules of the extension, the formation of columnar joint, this group along the joint leaching weathered steep peaks have formed a landscape. Ash flows in the form of melting guitar tuff, were found with a vertical dimension of the pore structure. This is the pore structure of the volatile hot volcanic ash rocks in the stream in the consolidation process, the volatile form of escape. Fushan area of the "islands Xuelang" attractions, to a more typical profile of the natural flow of volcanic ash, each representing a volcanic-ash eruption. Fushan is 1.35 billion years to the Cretaceous period 65 million years of breaking a volcanic eruption the volcano, is now in its original form volcanoes cone collapse disintegration of the results. Volcanic rocks of the characteristics of the rhythmic sequence of Fushan period reflects the characteristics of the volcanic activity and the formation of the volcano. Fushan volcanic rhythm sequence integrity, and typical geological phenomenon, domestic and foreign Mesozoic volcanic areas most representative of Iwata. Fushan volcanic formation Code China has been identified as "Fushan cycle" typical of volcanic rocks in the geology of the legislation with the Code of significance. In short, Fushan national geological parks, possession You Donghe, the cliff air; Guaidan Qifeng, a Fengzi. Gengjian clear water circuitous, vertical and horizontal valley, the beauty of Tiancheng, it is amazing. In addition, the human landscape of Fushan colorful, left many precious cultural relics.

China National Geological Parks
 


25, the Beijing Yanqing Guihua Mu national geological parks ? ?

Beijing Yanqing Guihua Mu National Geological Park is located in Yanqing County northeast of cross-strait Shirakawa, surrounded by mountains. Yanqing County from the southwest city about 30 km, from the city about 100 km. Park along the cross-strait Shirakawa, things of 26 km, north and south-6 ~ 8 km, an area of about 226 km2, to 1.4 to 1.8 billion years between the Upper Jurassic Guihua Mu characterized. Yanqing Guihua Mu fossils in the middle between 1.4 to 1.8 billion years of the Upper Jurassic Tuchengzi group, the exposed surface of Guihua Mu currently has 57, fossil texture clear, firm texture, ring width can be argued. Cheng Qian brown the surface more yellow or off-white, fresh section for more black ash, as its shape was Juduan the stump of a tree trunk, the general diameter of 0.6 ~ 1.5 m, the largest diameter of 2.5 m, and more perpendicular to the ground, revealing the ground generally high 0.4 ~ 0.5m, up to 1 m, only a small amount of Hengwo or tilt, for a maximum of 15 m. Geological park west of Fort Shirakawa reservoir of the North Eastern region of the village of Shirakawa Fort Reservoir and the East 600 m, sporadic Guihua Mu, for the formation Upper Jurassic Tuchengzi group, in flower pots Cundong 1.5 km, the occurrence of animals and plants Fossil formation lithology is the Upper Jurassic Tuchengzi group Ash Green fine sandstone. At the same time there are fossil bivalves are the main Lufeng Zhubang, Geshizhubeng, Mengyin, such as mussels, especially Zhubang is based. Fossils of different shape, single, double hull has, in general preserved shell valve more complete. Yanqing Guihua Mu group with a large number intact, and other characteristics, especially the Muhua Dan Kwan all produced in the original layer, in the eastern region to facilitate traffic into the only film preservation Guihua Mu origin. In addition, the geopark is also available in animal and plant fossils categories, landscape, structural features and mineral sites, hydrological landscape, natural eco-tourism, customs and cultural landscape, and so on.

26, in rural Henan-day mantle national geological parks ?

Henan Province in the township-day mantle National Geological Park is located in Neixiang County to Ma Fu cottage Yamaguchi prefecture, north of the frontline mountain. An area of 1087 km2. Park to a record 30 billion years since the formation of rock, tectonic and geological landscape features. Geological Park in the mountains Songzhi, Stubbs and Tang Xiao,
Throughout the metamorphic stratigraphy, the dynamic geological, geomorphological structure and erosion, karst caves, waterfalls, and other precious Canyon geological relics, Gengjian Maolin Dicui, rolling streams, rare flora and fauna rich people understand nature, ideal for tourism . From the perspective of Geology, Park is located in Qinling Orogen, it is experiencing long-term orogenic several different roles in the formation of continental Orogen, in the Chinese mainland in the formation and evolution occupies an important position. It records the orogen to 30 billion years of evolutionary history, the occurrence of rich, system, continuous, full of continental dynamics research information, research Qinling Orogen, research and Tethys tectonic domain retrospective of the global land mass of discrete groups, Clustering, hyperplasia, pieced together, orogenic evolution, such as the ideal place. Qinling Orogen has been the research results for the mainland Orogen of the world has set a good example. Geological Park in North China Orogen almost won the southern margin of the land mass of all the stratigraphic sequence and structural features, the study of the formation and evolution of orogenic belts, the formation and evolution of the Chinese mainland, the retrospective of the evolution of Earth history, a very important scientific value.

27, Zhejiang Linhai national geological parks ? ?

Zhejiang Linhai National Geological Park is located in Linhai City, about 50 km east of the coastal zone, between the years 9500 to 6500 formed the Late Cretaceous intrusive volcanic eruption rocks landscape characterized. Geological formation as the main park on the Lower Cretaceous rooftop Group, an eastern Zhejiang coast late Mesozoic volcanic eruption zone component. Geological park there with volcanic rocks, faults and vertical column joints of lava formed a unique platform, Fengcong, Shilin and other landscape. The highest mountain in the park for white Yanshan elevation 508 m, an altitude generally peaks in the 200 ~ 300 m between. Kan first major volcanic dome of intrusive rocks in the eastern part of the even-Kan Village near the crater area of about 2 km2, as its center of the invasive form of advanced acidic volcanic lava dome structure, cooling lava formed about 15 million columns. Stonehenge pentagons and hexagons very rules of geometry, like removing artificial carving. Stonehenge vertical extension 300 ~ 500 m, ranging from highly exposed. Or vertical columns arranged in an orderly manner or Xiewo, layers of piles, the magnificent, extraordinary momentum, Lin pillar is 000. In addition, the 000-peak, 1,000-Maya, the fence wall, giant Road, coral rock, spectacular landscape Majestic Shilin, a different attitude Feibaoliuquan, constitute a natural picture, it is delightful. There are acid spray excess of lava, forming a large number of mobile transgression to the movement of tectonic, and a level-tower-like distribution, rhyolite traces of both size. There are composed of volcanic channel Tazhuangyanfeng (Taozhu a natural three Juta), rock cliffs tower, top-ping, higher than the mountains around 150 ~ 200 m, is located in the coastal and spectacular special significantly, the concept of different directions such as "Tap "For instance, the" castle ", such as" screen?"such as" Lotus ", is to watch the sunrise, the better to Wuhai. Acidic lava platform experience tectonic uplift, weathering and erosion and water erosion, a peak-geomorphological features and sea caves. - Rural Ao, on the northern part of the 1 km-Ao, on the pterosaur fossil bird with long tail buried in the volcanic eruption during the intermittent-tuff, found that six of the pterosaur fossil preservation of integrity, was identified as a pterosaur teeth Branch, the characteristics of For a very long beak and no teeth, short tail, with the spine. Pterosaur age of about 76 to 83 million years. Late Cretaceous of ancient biology, ecology and ancient volcanic disaster on the biological effects of the study are of great significance. The geopark is China's invasion ? Mesozoic Cretaceous volcanic eruption rocks typical one of the regions, Central Pacific volcanic activity is also an important component of the band. The role of acidic volcanic lava invasion to overflow and volcanic eruptions accumulation of debris, after a long period of geological history of internal and external driving force formed by the large number of natural geological relics.

28, the Loess Plateau in Shaanxi Luochuan national geological parks ? ?

Luochuan Loess Plateau in Shaanxi National Geological Park is located in Luochuan County, Yan'an City in the south, a total area of 5.9 km2. Luochuan County, Yan'an revolutionary sites Beiju 135 km, the ancient capital of Xi'an Nanju 240 km; Huangdi Ling ancestor of the Chinese nation from another 35 km, from the famous Hukou Waterfall 130 km, from the history of Sima Qian's hometown of St. Hancheng 140 km, have a good surrounding environment of tourism. The geological park in the Loess stratigraphic section and geological features of the Loess characteristics. Geoparks the highest elevation 1136 m, China's Loess Plateau is the source of loess landscape of the typical region. Cut deep valley in between 80 ~ 140 m, a steep-slope, surface and underground water by gravity, within the valley loess landslides and the collapse of development, erosion ditch head back strongly. And a steep slope-valley, "V"-valley, on both sides of more landslides, the slope of the hanging groove, and groove wood loess section clearly exposed, for complete formation, the ancient soil layer clear, comparability strong, with very High academic value. In addition, the micro-topography of the Loess Gounei, such as: loess landslides, collapse, the Loess hanging ditch, the Loess La Shuidong, loess Bridge, the Loess column, such as the Loess wall. These micro-structure peculiar topography, natural-Fun to watch and strong. Luochuan County, black-ditch Loess geological relics is geological history and internal forces outside the integrated product of geological processes, is 240 years since the Earth's crust structure, tectonic movement and landscapes shape a true portrayal of evolution. During the formation of the Loess exposed complete, stable layer, the true record of the Quaternary since ancient climate, ancient environment, the ancient geography, vegetation and ancient geological events important areas such as information, is a standard loess stratigraphic section. Loess landscape in the long-term erosion of the geological formation of the next. The unique shape, people intoxicated with natural talent, the beauty of art created in??. The protection of the natural landscape, will enable more people to understand nature and enjoy the beautiful nature to human sacrifice.

29, the Tibetan Yigong national geological parks ? ?

Tibetan Yigong National Geological Park is located in Bomi County, Nyingchi Prefecture and at the junction, the main Yigong Township in Bomi County. A total area of 2160 km2, Yigong huge mountain to the collapse of geological relics, modern glaciers and alpine valleys features. Park for the deep mountain valley landscape, resulting in a significant vertical climate change. Nival from the mountains down cold, sub-alpine boreal, temperate mountain, hot-temperate, subtropical and tropical climate, such as different vertical banding. Yigong giant mountain collapsed into the District happened with the accumulation area, the biggest gap between the collapse of 2580 m, the accumulation of side amounted to 300 million m3, including high-speed sliding Cahen, high-speed water slide unique take sand pit, knoll group; And Yigong Yanse Hu, Yan Sehu breaches, Yan Sehu break formation of secondary collapses, landslides ruins, relics and ancient glacial activity corresponding geo-ecological environment. Yigong giant mountain collapsed ? the unique types of landslides is extremely rare. A typical mountain valley landscape terrain conditions of regional and global structure to the entire Qinghai-Tibet Plateau uplift the result of sustained, since the formation of this region for more tolerance of weathering the hard rock, and rivers along the lines of structure, not only easy to deep, A strong driving force for the conditions of water erosion, resulting in higher than the terrain continue to increase, making a further weakening of slope stability. The climate in this region is unique, not only by the southwest monsoon rainfall the impact of the Indian Ocean and there Daguai Wan warm and wet air currents along the Yarlung Zangbo River and its white base Gallas-Hengduan Mountains and the valley between the north Shenru, abundant rainfall , In the region blocked by mountains, forming China's largest group of marine glaciers, sea ice freezing and thawing on the one hand exacerbated by the high mountain region of the wedge of rock fissures split, and increase the flow of the river valley and the erosion of cutting capacity, Further exacerbated by both sides of the valley slope instability and collapse, landslides and in the formation. As rock hard by the role of faults, fractures inevitable development. The cracks also restrict the development direction of the collapse of the formation of the fractured decision was a degree of connectivity in the frequency of collapse. The role of faults and makes a long time there have been broken and a rock collapse. In short, the giant landslide ? Yigong landslide is the unique role of the internal and external dynamic geological comprehensive long-term role in the outcome, formed by the collapse - Landslide - Jiang blocking weir Cypriots into Lake - the lake outburst - terrain of the valley - the valley of secondary collapse, landslides geological Disaster chain in the world is extremely difficult to see. Yigong national geological park-giant landslide, Yan Sehu, Glacier, Grand Canyon landscape, Tibetan customs and the human species as one is that people are understanding of nature's good place.

30, eight of Huainan in Anhui Mountain National Geopark ? ?

Huainan of Anhui eight National Geological Park, the area of 120 km2, in order to form since about 5.4 to 5.1 billion years before the Cambrian, in the EC profile, rich in fossils and karst landscape features. Park mainly hilly areas, mountain ranges north-south extension of the Huaihe River Park in the northwest mountains and winding stream, the water in the region posed a Raoshan turn, the unique landscapes dependencies landscape. As the special geographical geological conditions, such as the region Shilin Karst topography, Qifengyishi throughout the region. Douya erosion along the river such as Li Ren-wall 1000, dangerous Qingxiu. Cambrian region, the EC profile in the formation and development, abundant fossils, outcrop, and concentrate, without deformation, deterioration. Implied in the ancient geography and ancient sedimentary environment, the ancient geochemistry, paleontology, paleomagnetism, the ancient structure information is revealed in the area as well as many weeks o-geological mysteries of the key. North China is also to study the geological evolution of Taiwan, South China, North Cambrian contrast provide an important basis for the geological. Yidikala first in Australia, South Africa, Huainan of the Bechtel Group found that epigenetic animals will advance the history of the origin of the two billion years. Geological parks with international or domestic large regional formation (tectonic) compared the significance of the typical profile, and fossils of origin, typical of international or national significance to the landscape and geological phenomena, regional and global geological evolution of major historical events provide an important geological evidence .

31, Hunan Chenzhou Flying Mountain National Geopark ? ?

Hunan's Chenzhou Flying Mountain National Geopark in Hunan Province in the south, the main stream Lei Xiangjiang river water tributaries of the middle reaches of the East, a total area of about 110 km2, to Danxia landform and karst cave for the main features. Park main Danxia landform types Walled (Fort), which is located in an orderly manner, Walled are steep, Redcliffe Chibi, Walled top tree when Huagai. Walled dissolution into many top-shaped depression Hunyuan pit. Walled area within the gods for one of the main King. During embellished a gorge, Shihmen, Tianshengqiao, Yixian Tian, caves and dissolution from the top of the Walled catchment depression (Tianchi); form a stockade (Fort) for the center, two rivers of water as a link, Hongyan green water, Chibi Danxia, Canyon Qidong, Gumuzhuhai the "four out of Castle Peak Tsui Ping", "Hong Kong is well spent to" the wonderful Danxia landscape. Park, the Huayan cave million, in development since the formation of about 3.5 to 3.2 billion years ago the Lower Carboniferous limestone; is about 9 km, for an underground Underground River, the main tunnel of 2245 m, inside a 13 Different characteristics of the hall, the largest can accommodate thousands of people; Dong Wai-chuen, there are, inside one day, there are holes holes, holes have River. Travertine inside various types of deposition, Ishida, stalagmite and stone Zhongru, stone pillars, Shiman, stone screens clouds, shape and have different Qixiangwanqian. In particular, is "underwater crystal cone" is the second time that the world's natural-odd. More "stone eggs Health and bamboo shoots" for the first time that the world's singular treasures. Dongwai landscape is also very spectacular, the general Falls more than 50 m from the roof on Feiliu??, to hang up the hole a silver drencher. This shows that the Southern Song Dynasty, through its well-known physical-Zhang Nanxuan Inscription on the roof, "Hua Yan million," the three Chinese characters. Walled in Lei Yue Fung-shaped cliffs and mountains west of more than 200 meters from the river surface Shushi Mi Linjiang in the caves in the cliffs, placed two wooden Xuanguan, a must for the Shonan landscape. To give people the ancients how to Muguan placed on the cliff Doubi unlimited Xiaxiang, very humane profound meaning. Scenic areas more complicated geological structure. Various types of local landscapes, both typical Danxia landform, there karst cave landscape, Danxia set Hongyan, the cave, clear water, one in the spring, both ancient landscape of the background figures. Castle Peak, green water, Redcliffe Chibi, bamboo deeply, a one-hung, extraordinary and dangerous, Sau, Meilunmeihuan natural picture.

32, Hunan Scopalia japonica maxin Mountain National Geopark ? ?

Hunan Scopalia japonica maxin National Geological Park is located in the new County in Southwest Hunan, Nanjing county from the new 11 km, area of 108 km2, Danxia Geopark in landscape features. Scopalia japonica maxin Mountain Danxia landform types, a total of more than 60 main geological features scenic spots, respectively, of the belt wedge-shaped, split-the massive, slope-style wall-like, cross-cut the line, scattered and arch-columnar - And embedded router during the groove and cliffs, such as wandering profiling. One out again cascading into the wedge-shaped features and processes during the peak Village Head landscape significantly. Not only that, Danxia landform of the "body steep, Lu ease, top-ping" and the basic characteristics of a typical structure (such as "Yi Xiantian," Tianshengqiao) in this performance is outstanding, but a large scale, groups Obviously, the high frequency. Scopalia japonica maxin from the Green Mountain Danxia landform (David) year, their prime time period from the remains of old age have developed. Danxia landform Scopalia japonica maxin a mountain of rock is formed in 9000 to 65 million years ago between the late Cretaceous continental red rocks of the (conglomerate, sandstone and conglomerate), grid-like rock in the vertical joints extremely development, these are A Scopalia japonica maxin Mountain Danxia landform of the material basis and space conditions. As a humid subtropical climate, abundant rainfall, surface runoff and development, and its water erosion induced by the gravitational effect, Danxia landform is formed outside the main camp of the conditions. Scopalia japonica maxin area, the accumulation of gravity, they often constitute the slope attractions, and some also form a boulder to watch the value of attractions, such as the Ham stone, stone image of beauty toiletry, and so on. However, many attractions because of the vertical joints of rock layers with monoclinic grounds, and there invading perilous rock, some with the direction of the invading bedding, some with the direction of the invading joints, such as Cloak Walled, General Shi, candle - And so on. Scopalia japonica maxin Mountain Danxia landform of China Danxia landform of abundance and grade of the most representative and one of the most beautiful scenic spots. Scopalia japonica maxin Mountain Danxia landform, modeling colorful, Guiqi insurance online, is a rare large-scale "Danxia landform Museum", for dedication to the human nature of the natural resources of gems.

 

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