1, Huangshan Mountain National Geopark in Anhui

Huangshan Geopark in Anhui top countries in the beautiful mountains of southern Anhui. North and South about 40 km, a width of things 30 km, an area of 154 km2. Huangshan Mountain National Geopark is a granite peak forest landscape. Huangshan to Xiongjunguiqi is known, the peak is 1,000 meters above 72, high-Qiaoba. Top mountain peaks and steep, Teluk-foot trough, in the form Qunfeng Qiaoba mountain terrain. Peak, the mountainside and valleys, etc., are widely distributed granite columns and Shilin. Since the center of the Huangshan to four weeks Chengfangshezhuang and distribution of the large number of "U"-shaped valley and the "V"-shaped valley. Qifeng the region stand, towering Xiongqi; Ching Chung green, tall and straight scene; Qiao Shi rugged, such as birds such as plastic; vast sea of clouds, the magnificent; Spa Plumbing, spewing Buxie. In about 1.4 billion years ago before the Late Jurassic, underground hot rocks along the crust of the weak areas of Huangshan on the transgression, in around 65 million years ago, the rock of Huangshan in a strong uplift. With the intermittent crustal uplift, underground rock and its follow-on the cover of weathering, erosion, but also from different directions by the various stress role in the rock created in a different direction of the joints. Since the Quaternary Period (175 million years ago) has formed a batch of three ancient increased erosion face, finally formed today's Huangshan. In these rock, because the mineral composition, crystallization of the mineral particle size, wind and the joint capacity of the nature, extent, such as multi-density differences caused??ax like a ghost-like beauty of Huangshan. In immediately Bridge, Tiandu Feng, the North Sea and other areas, be deemed to be famous Quaternary glaciers. Huangshan the existence of glaciers, more than half a century has been controversial, so far no conclusion. This is another attractive Huangshan Geopark is the charm. Huangshan "Qi Song, Guaishi, sea of clouds" three surprising and rich Waterscape as well as their mutual portfolio, showing the Huangshan natural harmony. Since ancient times, people have been longing for and praise. ?

2, Dunhuang, Gansu, Ya national geological park

Dunhuang, Gansu, Ya National Geological Park is located in Dunhuang City, northwest about 180 km, 100 km northwest Yumen Pass Office. Park area of 398 km2. Formed by wind erosion of Yadandemao. Geological parks focus on sectors-connecting to the peculiar shape of the wind erosion landforms, 1000-Baitai, Weimiaoweixiao, "yurts", "camel", "stone bird", "Shiren," "Danfo", "Shima" . It's like a medieval city, many of the world's famous buildings can find it in miniature, the world frightening. As night fell, defied stiff winds Jianli the issue of terror Xiaojiao, like 10 million animals in the roar, horrifying, so named after "Mo Guicheng." Dunhuang national geological parks are part of ancient Lop Nur, the desert plain area, sufficient light, low rainfall, evaporation, windy seasons, the biggest wind up to 12 above. In the new generation of geological (about 65 million years ago) Dunhuang - Shule faulted the center of the basin. Yadandemao constitute the rock formed in about 70 million years ago in the Pleistocene, for a deposition in rivers and lakes, the color was gray, green and yellow soil, the level of bedding, staggered bedding, local pest can see Trace fossils. As rock middle-level, vertical joint development, a soft rock blast in the nature of the long weathered heavy rain, wind erosion has led to various Ya landscape formation. Dunhuang Ya national geological park with its unique desert scenery, different forms of geological wonders, ancient folklore, has attracted countless brave explorers to the lifting of the "Mo Guicheng" the veil of mystery, exploring the mysteries of nature.

3, Inner Mongolia Keshi Ke Teng national geological parks ? ?

Keshiketeng Banner National Geological Park, south of Chifeng City, northwest even Xilinhot. National Geological Park to the Quaternary Bingjiu group, granite stone forest, geological structure and volcanic landscape for the group characteristics. The core zone of about 90 km2. Geological Park is located in the Greater Xing'an Mountains and the southern tip of the Yanshan Mountains junction, since the Quaternary Period (about 175 million years ago) since the multi-phase development of ancient glaciers, Castle Peak has nearly 1,000 ancient Bingjiu; preserve their integrity, the typical form, is the world On rare ancient Bingjiu large group at the same time there are Bingdou, glaciers "U"-shaped valley, traces of the glacier-lateral moraine, to end moraine ancient glaciers, and other relics. Spur of the Greater Xing'an Mountains in the mountains of Beijing University, granite stone forest landscape patterns of different groups, like people of like, Weimiaoweixiao, lifelike. Granite-intensive level of joints and vertical joints. Density of different vertical joints of the rock is separated into different wind capacity of the block, the long-term weathering eventually evolved into today
Days to see the granite stone forest. Park Kwan Dalinuoer volcanic landscape is China's northeast region one of the nine volcanoes, volcanic cone of different forms, known as the "five major volcanic Lotus miniature landscape." Geological park there are hot springs, desert, grasslands, lakes, rivers, mountains and valleys of prehistoric relics of human activities.

4, Yunnan Tengchong Volcano National Geological Park of geothermal

Yunnan Tengchong Volcano National Geological Park of geothermal and in Tengchong County in the Lianghe. Geological Park in geological relics and ancient volcanic accompanied by the Health and hot spring features. Core area of about 100 km2. Park has 97 of the volcano. Which preserved the crater and volcanic cone is 25, various types of volcanic cone. Park a few lava-class platform, the main Central crater lava platform, large area, the gentle slope. Various types of volcanic cone, crater, lava platform, lava flows and other volcanic features Yanse Hu parked very significant Head, a spectacular volcanic scenery. Tengchong Volcano lava landscape constructed mainly empty lava, lava collapse, lava flows and original joint structure; pyroclastic that sets rock melting, melting and melting guitar tuff breccia. Spectacular volcanic bombs, of various shapes, the main spindle-shaped, bread-and-Serratula. Park formed in the volcano about 340 million years ago to 10,000 years between the Pliocene to the Holocene in the Alps - the eastern section of the Himalayan Tethys structural belt, the Indian Plate and Eurasian Plate landing two continental plates - continental collision With the east, to development of faults, the younger of volcanic activity and a strong show of its geothermal features. Experienced a long geological evolution, Canghaisangtian changes, several magmatic eruption and a series of tectonic cycle, leaving a large number of geological relics, formed a Qili of the natural landscape. Tengchong Volcano epiphytic very rich geological phenomena, and a typical tropical, geothermal field, geothermal, hot spring, and so on. One show features into the hot jet hole, to take gas ground, boiling hot surface, fountains, gas-, water-chuen, and the explosion of hot water, such as six landscape. Water-chuen, landscape-chuen, another platform, Quan, embankment, Wah-chuen, a heap-chuen, Doubi, Quan, mass graves, Quan, fans-chuen, mushrooms, beans, Quan, Quan, grapes, Tung Wah-chuen, as well as inside, 10 minutes Milk, the goose-chuen, and so on. The contents of the rich and the beautiful colors, rare in the world.

5, Guangdong Danxia Mountain National Geopark

Guangdong Danxia Mountain National Geopark in Shaoguan City of northeast Renhua and Qujiang County border. Geopark things wide 17.5 km, north and south of 22.9 km, a total area of 290 km2, which Danxia landform concentrated distribution of 180 km2. The world from a red terrestrial sandstone and conglomerate to Chibi Danya for the characteristics of a class of landscape are called Danxia landform, this type of Danxia Mountain is named to the special landscape. A
Danxia landform of the rock is formed in 9000 dated back about 7,000 years ago to the Late Cretaceous of rivers and lakes of red sandstone and conglomerate. In about 65 million years ago, the area affected by the tectonic movements, have many faults and joints, but also the entire basin into Danxia erosion areas. About 23 million years ago in the Himalayan movement started making rapid uplift of the area. During the long years of intermittent role in the uplift of the area's topography makes earthshaking changes have taken place, this area will Geologic role in shaping such a beautiful scene. Save the whole mountain, a relatively good Subtropical the evergreen forest, the Four Seasons lush, green to drop. The Danxia the show, the main show in Jinjiang. Yu Ye Jin Jiang green, from 000 in the Nanling dumping Lin Hai, in Danxia Group in the circuitous Nanliu, all the way Tsui Chuk Gaan, trees mother-in-law, near Shek Daoying, Yuan-Shan Wei Yi. In addition to national geological parks breathtaking Danxia geological relics, there are well-preserved ecological environment and patchy distribution of the Peak, the original ecological community in the valley and old and valuable trees and wild animals, and the history of human use of the Danxia landform Remains of ancient species. All this attracts numerous tourists to pour in at home and abroad.

6, Hai Luogou National Geological Park in Sichuan

Sichuan Hai Luogou National Geological Park is located in the southeast margin of the Qinghai-Tibet Plateau, the middle section of the Gongga Mountain Snowy Mountains east slope, Luding County of Sichuan Province, something about 29 km, north-south width of 17 km, area of 350 km2. Hai Luogou national geological park with modern glaciers, hot springs and mountain valleys as the main features. Gongga Mountain peak elevation of 7514 m, peak shape of a pyramid, known as "King of Shushan," for the world's 11 peaks. Park complex landform types: high-mountain, alpine mountains, and so on. 4900 m above sea level in Mountain high above the snow line for the region, mainly to the granite bedrock nudity, Kok Fung, the blade, such as chiropractors and Bingdou Bingshi landscape development. Gongga Mountain peak, unnamed peak, the three peaks, such as pyramid-shaped peak angle with the blade in the watershed above the ridge. Development of modern glaciers firn pots. - Hung, Ki, insurance, the completion Qifeng unexpected heavy snow mountains, towering and magnificent, magnificent, aesthetic value, ornamental strong. At 5.4 billion years ago, Hong Gongga Mountain region is part of the ancient land of Yunnan, for the well-eroded land. In ago 500000000 to 2.5 billion years between (the Ordovician to the Triassic), the area most in Kangdian ancient land west of the area, in this long period, formed a thick 20000 Meters of marine-based land and sea cross each other strata; about 2.2 billion years ago before the Indo-Chinese movement, so that the whole western Sichuan large-scale uplift fold, the end of the marine period, the formation of ancient snow mountains. Yanshan movement and the subsequent movement of the Himalayas further uplift fold, from long-term erosion. About 180 million years ago until the late Tertiary the end of ancient mountain snow was razed to become part of China's quasi-Plain. 340 million years ago orogeny to the Gongga Mountain uplift Qian Yumi, and the first time in the region glacier ice cap (Flower & Ice Age). To the Pleistocene (248 million years ago), glaciers to go days, a Moroccan Kong Ling Ice Age, glaciers off the assembly line up to 1800 ~ 1900 m above sea level the ancient Dadu River area. 130 million years ago, Yuanmou movement of the end of a regional lake sediment and into the river to the main role of the period, the formation of the Dadu River today, the Yalong river valley. At the same time, the alpine zone of a number of glaciers. In the 24,930 to 19,700 years ago before the last Ice Age, in the upper reaches of the Hai Luogou formed a 10 km km to a thickness of 200 m lateral moraine of the embankment. After further shrinking of glaciers, in 1560, 940 years of ice into two, at an altitude of 2750 m of modern glacier front of a cut at the end of the moraine of the glacier ice thickness of 20 ~ 60 m of the two end moraine embankment. The two ice into the era of China in 5000 is equivalent to climate change to the second and third cold period, called the new Ice Age. Geological parks in addition to modern glaciers, hot mineral spring group has a complete vertical natural Daipu and diversity of mountain ecosystems strong combination of many different forms of pictographic rocks, many types of biological landscape. Glacier coexistence with the hot spring, cold and warm compatible with this rare spectacle, the world's attention.

7, Shandong Wang Shan National Geological Park

Shandong Wang Shan National Geological Park is located in Shandong Province Lin Quxian Chengdong about 22 km, an area of about 13 km2, to the world-famous mountain-wang fossils and reflect its formation environment for the characteristics of the volcanic features. Park fossils mainly deposited in the Miocene Shan Mong group diatomite layer (about 14 million years ago), many of the types, preservation of the integrity of the world's rare fossils have been found in a dozen categories 600 Variety. Animal fossils, including insects, fish, spiders, amphibians, reptiles, birds and mammals. Fossils of winged insects veins clear, completely preserved, and some reservations brilliant colors, has studied the identification of the 11 heads of 46 Section 100 of 182 kinds. Shan Wang bird fossils found so far is China's most abundant fossil birds integrity of origin. 1.30 fossils of deer and the original ancient Oriental ancestors Xiong Miocene fossil is the world's most complete preservation of the fossil specimens. Plant fossils have moss, ferns, gymnosperms and angiosperms and algae. In addition to 100 species of algae, other plants, 46 Section 98 of 143 kinds. They study ancient global ecology, ancient climate, such as plants and animals have an important evolution of the position. Chinese and foreign experts were called on the Miocene "Laboratory." Wang Shan region is China's output of fossils of one of diatomite origin. Unique "million rolls on," said higher research and ornamental value. Fossils of volcanic origin surrounding geology, geomorphology volcanic eruption geological parks is important geological sites, mainly distributed in the basin external Huangshan, Yao Shan, Lingshan, wiping Masan, and other places. At present there can be observed from the crater ancient geological landscape, Mallon-volcanic basin topography, volcanic lava structure, is to study new generation of volcanic activity in North China, the volcanic basin formation and evolution of the important bases. At the same time the new generation of Shandong is also to the provisional Linqu-profile location of the group, the retrospective geological history is of great scientific value.

8, Tianjin, North China National Geological Park

Tianjin, North China National Geological Park is located in the North mountain thistle, ranking third in Fuxin Beijing-Tianjin-Tangshan area, known as Beijing, Tianjin, Tang "Golden Triangle" said. Geological parks with the core area of 9 km2, long from north to south 24 km, things the average width of 350 m. Geological park to the main geological relics in the ancient Spring community profile and fossils. Jixian ancient profession in the Spring section (18 to 8 million years ago), complete with rock, exposed continuous, well-preserved, simple structure, the top and bottom limits of clear, shallow and degenerate very blessed. Changzhou House from the mountains to the village only 24 km distance, on behalf of the 18 billion years to 8 billion years up to 10 million years of geological history of the continuous deposition of a complete land and sea changes in the process. Abundant fossils, found the fossils of more macro, so that more cells of the internationally recognized from the 9 billion years earlier to 17 billion years. In addition, there are still some of the world's most ancient geological phenomena, such as formed in the 12 to 13 million years ago between the sedimentary deposits and sepiolite Tieling group found the world's oldest jet hole structure. Spring in Jixian ancient profession is the profile of human nature left to the valuable natural heritage, found a number of important fossils of early life on Earth and the evolution of the formation process is important. Earth's ancient times to open many of the mysteries of science plays an irreplaceable position. Geological parks Qunfeng Junxiu, Canyon??, fresh air pleasant, charming scenery, natural mysteries attractive, convenient transportation, leisure, vacation, travel, pay homage to the good place, is also exploring the mysteries of the rare natural places.
 
9, Sichuan Dadu River Gorge National Geological Park

Sichuan Dadu River Gorge National Geological Park is located in Leshan City, Sichuan Province Jinkouhe, Ya'an City Hanyuan Xian and the Liangshan Yi Autonomous Prefecture of Ganluo County, bordering site, a total area of 404 km2. Geological park to the Grand Canyon and the Dadu River Mountain basalt geological features tile features. Geological park to the river mouth in - us r. between the Dadu River Grand Canyon as the mainstay, is typical of the river valley landscape erosion Valley, about 26 km, Gu-70 ~ 150 m, fall 1000 ~ 1500 m, the largest deep valley 2600 m, as the Yangtze River Three Gorges of the double than the United States Grand Canyon deeper 860 m, momentum magnificent, beautiful spectacular, dangerous You Magic, on both sides of Bili 1000 Ren, Qianzibaitai, such as the picturesque Thai, and cutting out of the top Sinian (5.4 million years ago) E Edge Group to Emei Mountain basalt Permian (about 3 million years ago) thick several thousand meters a perfect cross-section, more than 10 billion years to record the geological evolution of history. Emei Mountain basalt constitute the roof of Pingdingshan, Peak platform area of about 1.6 km2, around the perilous rock rugged, cliffs Gaoxuan, height difference of 800 ~ 1000 m, Yuan Wang as castles in the air, and if imbricate review in the mountains above the stack, and Mount Emei, Wa Wushan echoes, a tripartite confrontation of powerful, scenery Qijue, very spectacular. Tile in the mountains, save a complete U-shaped glacial valley, Kok Fung, Bingdou, Bingshi Lake, such as the late Pleistocene ice of ancient glacial landscape, a beautiful water color and five Qixingguaizhuang the "stoning Park." Other geological relics are: Pool Five ancient glaciers, dingmugou Late Permian to the ancient community profile, Ping Shui Jingkuang pheasant, and many have special significance to the hydro-geological landscape, and so on.

10, the Fujian Jinhu national geological parks ? ?

Fujian large Jinhu national geological parks in Sanming City of Fujian Province in Taining County, a total area of 461 km2. Danxia to geological relics and granite landscape features. Geological Park is the major geological fault running water erosion sites, the fault collapsed, caving and other geological weathering erosion formed, Danxia landform a meandering, peak and valley (water Yixian Tian, the second-line days, slashes days), Valley Lane, Fort Rock , Stone walls, stone pillars, Yan Feng, Fengcong, Danya Chibi, Tianshengqiao, Chuandong, rock groove, flat holes, with holes for peak-like holes in Waterloo, Pot-hole, caving Yanse Hu, Shek Zhongru, waterfalls, etc. 26 landscape types. Nature created the Lake area Qianyanwanhe, shape million, magnificent, Wei-concept for the Danxia landform, especially ZHONG Ling Commission show, Yanbo Hao-miao of Jinhu clear water, Shanguangshuise making the other more beautiful, static and dynamic The proper coordination, created a lake in the mountains, a lake in the mountains, the Central Mountain water, water Raoshan, scattered in the mountains of the Qifengyidan linked together by the lake, a unique vitality and charm of the water program in the world Jia Jing. Another granite landscapes, such as granite stone pillars, stone forests, pneumatic-and-egg shape the landscape, caves, waterfalls and the surrounding ecological environment. Also in Danxia landform of the region are rare animals and plants, such as Chen Shui-bian tree, and Fangzhu, such as temples, tombs, rock coffin, Xuanguan, historical and cultural sites, and so on.

11, Jiaozuo, Henan Yuntaishan national geological parks

Henan Jiaozuo Yuntai Mountain National Geopark in Henan province Xiuwu County in Jiaozuo City, south of the northern part of the Taihang Mountains. Because of the mountain Gao Jun, Qunfeng Sidaoqiaoya Taiwan, common Baiyun wind around, Gu Ming. Yuntaishan the construction of the park to one side and bluffs overlooking the mountain landscape and glens Chingchuankang Feibao characterized. The core zone of about 80 km2. Landscape park complex, undulating terrain, Zhongshan, hilly Piedmont and gently inclined-alluvial plains, mountains due to strong erosion cutting, broken terrain, more than a deep ditch canyon, cliffs, rolling ups and downs, for a typical Tectonic denudation landscape. Park, Qunfeng Songzhi, inline sky, the mountain-special, Stubbs and Forum, bluffs overlooking Feibao, glens Chingchuankang, Tam Chi Hui Ying, Feng vary Shiqi, the ecological vegetation, embellished mountains, cultural landscape, long history, Paleontology fossils, competing Zhengyan, geological sites, rich and varied mineral resources, the full range. Here are formed in the exposed since about 14 to 3 billion years between the full stratigraphic section; Swire-yu - Early Proterozoic basement, a typical structure remains, in particular the new tectonic movement remains, throughout the entire park, is very typical . 23 years ago began in the Himalayan movement makes Yuntai Mountain area further uplift the geological formation of the current landscape.

12, Gansu Liujiaxia Dinosaur National Geological Park ? ?

Gansu Liujiaxia Dinosaur National Geological Park is located in Yongjing County of salt pan Gap Reservoir north shore. Park covers an area of 15 km2. Geological park to groups of dinosaur footprints as the main body. Liujiaxia Dinosaur Footprint group, save a complete and clear. At the same time, the same level of rock lying on the preservation of dinosaur tracks, drag marks and the Department of fecal traces, which form the footprint, horizontal tracks, drag marks and feces trace coexistence scenes. 710 m2 in the rock surface found Class 8 30 Group 270 Avenue, including two giant Xijiao Lei, two legs like a beast, a similar class Long Island and three other unique shape, have not yet vested in the footprint, On behalf of eight species. At the same place in such a variety of plant food category and carnivorous dinosaur footprints, the first of its kind in the country in the world is also extremely rare. Liujiaxia the largest group of dinosaur footprints of a group of Xijiao Lei Avenue after the Avenue of 150 cm, width 120 cm, before the Avenue of 70 cm, width 110 cm, Stride 375 cm, the lateral margin of spacing around the Avenue 345 cm, the most in the world, But such small footprint foot before and after foot, before and after the printing of a full and regularly review of the stack, for the first time at home and abroad. Park also found the fossils of dinosaur bones. To further study and research the type of dinosaur footprints and relics made of the relationship between the track provides an important clue. Dinosaur footprint fossils of dinosaur physiology is the study and living habits of precious materials, its form, composition and arrangement of features can truly reflect a considerable part of living habits and physiological characteristics, such as body size, four-legged walking foot or two sports, or Qunju Single way of life, at the same time to study dinosaurs living environment and provide an important basis for biological categories. As diverse types of dinosaurs, strange patterns, and is known to Tiqu great, successfully rule the Earth for 1.6 billion years, to about 65 million years ago all but disappeared. Happened to the dinosaurs from the boom, from the decline to extinction of the whole evolution process is full of legends and mystery. Gansu believe that the Liujiaxia Dinosaur National Geological Park will attract many students and the community visited, making it the most popular, with great relish and the general concern of geoparks. ?

13, Heilongjiang Jiayin Dinosaur National Geological Park ?

Heilongjiang Jiayin Dinosaur National Geological Park north of Heilongjiang, and Russia's Basikewo the sea, the gentle mountain, according to Jiang's standing total area of 38 km2. Geological Park to the Late Cretaceous dinosaur fossils and fossils of plants and animals associated mainly. Geological Park in 8800 to have 65 million years ago between the rich Late Cretaceous dinosaurs, abdominal-footed, fish, insects, plants and Yubie like fossils, producing fossil stratigraphic section complete, the sequence clear, stable layer; keel Hill Dinosaur fossils found in China is the first dinosaur fossil is a flat-Yazui Long subfamily, is the Late Cretaceous large Yazui Long representatives, so far, only found in China's Heilongjiang River. In addition, also found that the carnivorous Tyrannosaurus rex. Park found the plant fossils, was named Jiayin angiosperms, is the Late Cretaceous of China's pan-Arctic angiosperm plants in the typical representative, was first discovered in China, northern China to fill the Late Cretaceous history of the development of plant A blank for the Late Cretaceous ancient geography and ancient climate research also provided new evidence, a natural??the Late Cretaceous geological museum. Geological park surrounded Sanshui, Linjiang standing singular beautiful natural landscape. Mountaineering Yuan Wang, Gully aspect, the Peaks of Zhu; overlooking the other side, Woyeqianli, the vast open; overlooking the foot of the mountain, such as with Jiangping, slowly east. In summer, Danxiancenglin stacked?, linked by mountains and rivers, Lin Cui Feng Qing, wildflowers Zhengyan, scenery Qili, to winter, the snow everywhere Ai Ai, the snow-wrapped, the forest's surface ice, Qianhuhouyong, cupola-shore, it is Spectacular. Is a rare popularization of science, a good place for tourism and leisure. ? ?

14, Beijing Shihua Dong national geological parks ? ?

Beijing Shi Huadong National Geological Park is located in Fangshan District of Beijing, Hebei and the town of Dover Township in the cross-strait Shihe, from the Beijing City 50 km, from the Fangshan 30 km. Geoparks include Shihua Dong and Yin Hudong, a karst cave inside and secondary chemical deposition landscape. Dan Huadong is the current domestic karst caves found in the large-scale, multi-layer, all types of deposition, the large number of secondary chemical sediments of the cave. Multi-hole of more than sticks to the floor structure, there are seven from top to bottom, 1 to 5-hole, a total length of 5000 m, 6,7 Underground River of underground water and filling the tunnel layer. Entrance altitude 251 m, diving from the region of 160 m, a cave-diving near. Shihua Dong 1, 2, two long-1362 m, there are 12 tall and 16 Dongting cavern formed. There are different forms of size-hole 63. Dan Huadong inside secondary chemical sediment types, modeling the United States, Qianzibaitai stone flower, stone sticks and stone Zhongru; typical beautiful stone pagodas and stone shields, stone lamps, stone terrace; Majestic Shiman, stone flags, Stone Falls; dazzling white, milk and flashing LED stone wall of the IPL, Dan Huadong brings together the best of karst cave sediments. Dan Huadong not only deposition type, shape the United States, but also holes in solid, structured, inside fresh air, good environment. As the deep hole of a greater space and underground Underground River, creating a cycle of self-regulation holes in climate and environment. ? Yinhu Dong (also known as the British three holes) of Dover Township, Fangshan District in the United Kingdom under the water 100 m at the South Village. Yin Hudong-lateral body to form a single, 90 meters deep hole total of about 4000 m. Inside there are eight large halls and more than 40 attractions and the Underground River water underground hole, the hole-general, 5 ~ 10 m, an average of about 8 m-high, inside an area of about 30,000 m2. Shihua Dong Yin Hudong is yet another miracle in the region, King-for-hole walking, people Mubuxiajie. David Kistler particular block, about 2 m, snow leopard Toulian Silver Fox body, the shape of an "inverted Silver Fox", it Tongti surfaced about the long white as snow Liangcun the burr, Mimizhazha to as crystal clear as cashmere , Dazzling white, beautiful touching. Also inside are rough-tall stalagmite and stone pillars, the typical stone flag, with stone, crystal of the geese, flashing LED stone waterfall, the white stone pillars too busy, Ishige, stone and other flowers. Although Tung Yin Hudong of a single, but inside the deposition colorful miniature landscape has its own characteristics, coupled with nearly 800 m long tunnel, Qingqing of clear water, clear bottoming out of the underground river. Park in the karst cave of high density, good conditions-dong, a complicated process. These tall halls and exquisite landscape, nature is in the long geological time, the sculpture by carefully. For example, Dan Huadong this multi-storey structure of the cave is the earliest form of Dongding. At that time, a hole on top of the standard surface water table, where there are underground water erosion, transportation, material taken away holes, caves formed after a rise in the crust, the crust of the cave with the underground water level is rising relative decline later , The local stability in the shell, groundwater and the formation of the new site for corrosion removal, it formed a second tier cave. In this way, the crust up several times, it formed a multi-storey cave. Clearly, Dan Huadong 7 of the existence of different heights cave, signs in the region at least six times intermittent rise. At present, groundwater is still the lowest dissolution caves. Beijing Shihua Dong national geological parks, with the exception of part of the underground karst cave and deposited inside the secondary chemical landscape, there are some ground stratigraphic section and geological structure acting and other geological relics of the ancient landscape and history of landscape architecture and the humanities, and so on. ?

15, Zhejiang Changshan national geological parks ? ?

Zhejiang Changshan National Geological Park is located in the territory of Changshan County, located in the upper reaches of Qiantang River, the park area of 82 km2. Park in the development of a major retrospective of the geological history of great scientific value of a typical stratigraphic section, fossils combination with stratigraphic section. HUANGNITANG Daruiweier bands to the line of the global profile of the most important. HUANGNITANG Daruiweier band is the lower profile of the global profile of point (GSSP), the only global Daruiweier band contrast standards, the establishment of a permanent mark profile (that is, and academics known as the "Golden Nail" ) Due to the formation of the scientific profile on the international community have a comparative and research value. Park, the geological formation remains to Ordovician fossils, algae reef limestone karst landscape features and structural geology, to a large number of Gangnam District Paleozoic strata of the profile of these strata and fossils in the main output. Particularly early in the Ordovician (4.6 to 5 million years ago) and the T-formation, conodont animal fossils known for the good of the world. Late Ordovician (4.4 to 4.6 million years ago) Three Mountain limestone reef was also its karst landforms, rock and biological characteristics of the uniqueness of the change is known. Watts Hill ? Ruo Yan River structural deformation with Ordovician rocks Thick light structural features, a good Ornamental Stones - known for its flower stone. There is also a multi-stage development of the various micro-topography unit and the Changshan River geological landscape. Broad River floodplain, and Chang Feng Hu Yanglin bands on the weather along the domestic landscape, and so are rare.

16, Hebei Lai Yuen Baishi Shan National Geological Park ?

Hebei Lai Yuen Baishi Shan national geological parks, including the Laiyuan County Juma source domain and Baishi Shan area of 60 km2. Geological Park in Dali Bai Shishan characterized Yan Feng Lin, accompanied by 10 granite waterfall Gap Falls group and Juma source Quanqun and other geological tectonic ruins. Bai Shishan red meat to the lower part of the granite base, central to the white marble Wei Yao, the top of the pyramid peaks for the grey, red, white, grey colour one, the unique landscape. Bai Shishan main high-2096 m, more than 10% peak Cong, Qiao wall, shape vary. Most of the straight-wall , Prism has Kok, steep Bili, it seems Daoxuefupi. Peaks of different forms, some under small-large, rather than dumping some down, some Zhuangru stacked blocks, some so unpredictable and ever. In granite in the area also is a landscape of muddy garden majestic mountains, towering Guaidan, 1000 Zibai Tai, fun. Bai Shishan 10 waterfall Gap in the stream flow was 4000 m, Qianshan between stone, even the 10-stack the waterfall, a waterfall Tan, Tan Hui Cheng waterfall, waterfall spray flying. Dragon waterfall drop 48 m, broad waterfall 3 m, such as the Galaxy hung upside down, the pet thundering sound, the momentum of the magnificent waterfall at Ssangyong levels fall, the gap between 60 m, big difference. Drought, the water fine, in the very Xiuqi; wet period, silver screens Gaoxuan, attractive scenery. Even stacked constant stream waterfall in the background of green vegetation Cangyu, showing a more dynamic, so that visitors Liulianwangfan. "Scale slope" for the granite joints, in the shape of a weathered, peeling off, the shape of scale, Manliu Valley streams, crystal attractive. 11 billion years ago before the formation of the Mesoproterozoic Jixian Ji Wumishan of dolomite have the effect of regional metamorphism. Yanshan to the Mesozoic period (about 1.4 billion years ago) the intrusion of granite, dolomite degeneration, the more near the granite, stronger role in eradicating corruption, formed a fading white dolomitic marble, a local contact metamorphic minerals - radial wollastonite . This is Baishi Shan peak forest landform created the material basis, hence the name will Baishi Shan. Dolomitic marble-like flattening of the yield, nearly level for the formation of the peak level of vertical rock Overlay stability. Construction of the future role of dolomitic marble of the two vertical joints, control of the Dangerous Yanfengbili the development of the long-term surface water erosion, weathering and gravity collapse, then formed a marble peak forest landscape of today's wonders. 10 waterfall Gap water from the 1400 m above sea level Longhu-chuen, it is fractured granite in the water, is along the rocks in the joints of the outflow. Bai Shishan how the granite joint development group, but with 10 waterfall Gap is closely related to the formation of the three original joint, a waterfall and the gap is due to the Department of joint development. 10 waterfall Gap is the origin of the formation of the springs in the mountains, in Xiaxie process, the granite of the three original joint control of the flow direction, as part of a group of special joints to form the base level of the river, in the long In the process, as a partial gap formed a number of waterfalls, this is what we now see the 10 Gorge waterfall landscape. Juma source Lai Kwan including water, easy source of water and Juma He is the source of Beijing Juma He formed about 1.4 billion years ago in the Yanshan movement, for the control of the increase in tectonic fault-chuen. This water-chuen, a large, steady flow, spring, as thousands of years "to the endless rolling Chung" Jumaquanqun, is another in North China, "Springs." ? Hebei Lai Yuen Baishi Shan National Geological Park Set metamorphic rock peaks, topography, mineral resources, water landscapes, ecosystems, human history, and many other tourist resources as one. Accessibility, landscape focus.

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