Talking about the canyons in China In everyone's mind A series of familiar names will emerge 193km long Yangtze River Three Gorges It has attracted countless scholars and writers. (Xiling Gorge of the Three Gorges of the Yangtze River, photographer @魏启扬) ▼ The mountains are steep and majestic Taihang Mountain Canyons It was once an important transportation route for ancient people to cross mountains and ridges. (Please watch in horizontal mode, Taihang Mountain Grand Canyon in Linzhou, Henan Province, photographer @付有良) ▼ Draw a beautiful curve at the foot of Mount Nanga Bawa Yarlung Zangbo Grand Canyon With a length of 504.6 km and a depth of over 6000 m Ranked among the world's largest canyons (Nanga Bawa Peak and Yarlung Zangbo Grand Canyon, photographer @高一蒙) ▼ China is a mountainous country In contrast, there are countless canyons. They are widely distributed over 9.6 million square kilometers of land. Make China the world's One of the most beautiful canyon landscapes in the country (Distribution map of major famous canyons in China, drawn by @郑艺/Planet Research Institute) ▼ What is the power What shaped so many canyons? 01 The Creation of Rivers canyon The creation of the river It is a river that continuously cuts down The product of the collision with the rising earth However The Canyon at the Beginning It is not as magnificent as people imagine. In Mohe City, Heilongjiang Heilongjiang River bends into an exaggerated "Ω" shape Known as "The First Bay of Heilongjiang" Maybe it's hard to believe Such a winding river A whole new canyon may be brewing Beneath the calm waters The river water carries sand and gravel, wears away and cuts the bottom rocks Deepening the riverbed The entire river is embedded tens of meters below the surface If the Greater Khingan Range continues to rise Heilongjiang will maintain its current state and continue to cut Produces deeper canyons This kind of plain river The valley was formed due to the uplift of the land surface and the cutting of rivers. Pre-Creation River Canyon (Schematic diagram of the formation of the Xiancheng River Canyon, drawn by @Hanqing/Planetary Research Institute) ▼ In the last 100 million years Affected by the combined effects of plate movement Most of the Chinese mainland Rising to mountains and hills Many rivers once flowed here Cut down and deepen Forming various types of pre-formed river canyons In North China Taihang and Yanshan Mountains slowly rise Juma River, Yongding River, Hutuo River, etc. Carving the Xiancheng River Canyon into the Mountains (The Juma River Gorge in Yesanpo Scenic Area, Laishui County, Hebei Province, photographer @余明) ▼ At the junction of north and south The Qinling Mountains are rising rapidly The Han River and its tributaries cut into the mountains "Tai Chi City" in Xunyang City, Ankang City, Shaanxi Province The name comes from the Tai Chi-shaped Xiancheng River Canyon (The Xunhe River Gorge in Xunyang City, Ankang City, Shaanxi Province, where the Xunhe River flows right into the Han River. Photographer: Yang Wenzhong) ▼ In South China The southern hills have been in a state of uplift for a long time Several major tributaries of the Pearl River cut through the surface The formation includes Sanrong Gorge, Dading Gorge and Lingyang Gorge. Many pre-formed river canyons (Please watch in horizontal mode, Lingyang Gorge, Xijiang, Zhaoqing, Guangdong, photographer @吴勇强) ▼ In the Northwest Weigan River originates from Tianshan Mountain Cutting through the desolate mountains Leaving behind the curved pre-formed river canyon Finally it flows into the Tarim River (The Weigan River on the northern edge of the Tarim Basin cuts through the Queletag Mountains. Photographer: @仇梦涵) ▼ In the Southwest Long-term uplift of the Sichuan Basin and its surrounding mountains A series of rivers represented by the Jialing River Formation of a large number of pre-formed river canyons Among them, Libi Gorge, Wentang Gorge, Guanyin Gorge It is called "Little Three Gorges of Jialing River" (The Little Three Gorges of the Jialing River in Chongqing, image provided by Wu Xianghong, tagged @谢煜涵/Planet Research Institute) ▼ Tracing back from this The Jialing River and its tributaries flow through the valleys between the hills. Nanchong, Suining, Guangyuan Langzhong, Zhaohua and other towns They are all built in the wide areas of the Xiancheng River Canyon. (Please watch in horizontal mode, the ancient city of Langzhong in Sichuan and the surrounding hills, photographer @沈龙泉) ▼ In some areas on the southern slope of the Qinling Mountains The horizontal changes of the Jialing River Gorge are more prominent The river water continues to erode the mountains on the concave bank Widen the river channel laterally At the same time, the silt is deposited on the convex bank This phenomenon means that the uplift of the mountain has slowed down or even stopped. (Jialing River Gorge in Hui County, Longnan, Gansu Province, the river flows from the top to the bottom of the picture, photographer @杨文忠, tagged @汉青/星球研究院) ▼ Wait until the mountain rises rapidly again When the river cuts down and becomes faster again The previously accumulated silt and riverbed were cut again. On both sides of the Xiancheng River Canyon Forming a landscape called "terrace" (Please watch in horizontal screen, the terrace landscape of the Suosong Village section of the Yarlung Zangbo River Gorge, photographer @贾纪谦, tagged @汉青/星球研究院) ▼ Terraces are step-shaped landforms on the hillsides on both sides of the canyon. It is in the continuous period of rise and rest. The product of mountain rivers constantly transforming canyons Witnessed the intermittent uplift of the earth (Schematic diagram of the formation of canyon terraces, drawn by @Hanqing/Planetary Research Institute) ▼ They provide fertile river sediment and at an altitude far above the river For the survival and development of mankind Created favorable conditions (Farmlands and villages on the terraces of the Lancang River Canyon, photographer @李小糖, tagged @汉青/星球研究院) ▼ So far Rivers can grow in two basic ways: by deepening and by widening. Creating a canyon And beyond the creation of the river The Earth Continues to Rise It also helps at the macro level Creating a richer canyon landscape 02 The Earth's Help In the karst area of southwest China There is often a canyon with a unique shape Deeply embedded in carbonate mountains Like a "crack in the earth" It is called a karst canyon. (Maliang River Canyon in Xingyi, Guizhou is a karst fissure canyon, photographer @笑飞雪) ▼ The rocks in karst areas are mainly composed of calcium carbonate. These rocks are dissolved by the carbon dioxide in the water. Makes rivers cut faster Soon a deep and narrow "ground crack" was formed. (Huangying Grand Canyon in Wulong, Chongqing, photographer @胡兴波) ▼ Chongqing Fengjie has The longest and most densely populated canyon in the world The most typical karst canyon group Among them, Tianjingxia fissure is particularly typical. (Interior view of Tianjingxia Ground Crack, photographer @黄雪峰) ▼ More special is The river at the bottom of Tianjing Gorge has turned to flow underground Become an underground river (Schematic diagram of the origin of karst fissure canyons, drawn by @Hanqing/Planetary Research Institute) ▼ Underground rivers sometimes encounter cliffs Incarnation Waterfall (Hubei Enshi Qingjiang Butterfly Spring, the two waterfalls correspond to the valley river and the underground river respectively, photographer @李云飞, tagged @汉青/星球研究院) ▼ More often The underground river creates a large number of underground caves When the roof of a series of caves collapses Forming several interconnected tiankengs It also forms a large karst canyon (Chongqing Wulong Tiankeng Canyon, the tiankengs are separated by natural bridges, and the bottom of the canyon is a river that has seen the sun again. Photographer @陈小羊) ▼ The dark river has since seen the light of day Continue to flow among the peaks and peaks Scouring and dissolving out larger canyons To the karst region of southwest China Add a touch of softness and beauty (Please watch in horizontal mode, Lijiang River Gorge in Yangshuo, Guilin, Guangxi, photographer @何旭龙) ▼ If the intrinsic chemical properties of rocks Participated in creating the most beautiful canyon in China Then the fracture zone produced by the rock being broken by external force They often help shape the most majestic canyons. 65 million years ago The Indian Plate and the Eurasian Plate collide violently As the Qinghai-Tibet Plateau gradually rises A huge force tears the earth apart In and around the Qinghai-Tibet Plateau Formed a stretch of hundreds of kilometers Super fault zone (Sketch of the topography and large faults in the southeastern Qinghai-Tibet Plateau, drawn by @Zheng Yi/Planet Research Institute) ▼ The water converges along a section of the fault zone Forming a super river Rivers cut down to form super canyons Thus, the most spectacular canyon group in China was born. At the foot of Mount Nanga Bawa Several fault zones are connected to each other Turning a big bend around the snowy mountains The Yarlung Zangbo River flows through it This has created one of the longest and deepest onshore canyons in the world. Yarlung Zangbo Grand Canyon (Overlooking the Yarlung Zangbo Grand Canyon from high altitude, photographer @小风) ▼ In the heart of the Hengduan Mountains Several fault zones are arranged approximately in parallel Guide the Nujiang River, Lancang River and Jinsha River Forming three deep canyons Including Nujiang Grand Canyon (The First Bay of Nujiang River, photographer @崔永江) ▼ Lancang River Grand Canyon (Lancang River Grand Canyon in Yanjing Township, Mangkang, Tibet, photographer @胡澍) ▼ and Jinsha River Grand Canyon Together they form the world-famous Three Parallel Rivers (Please watch in horizontal mode, the canyon of the first bend of the Jinsha River, photographer @崔永江) ▼ In these majestic mountains and deep valleys There are also countless narrow terraces hidden They are like pearls in the canyon. Raising a home (Yajiang County in the Yalong River Gorge in Sichuan, photographer @见书) ▼ These Grand Canyons on the Fault Zone Bringing the magnificence of China's canyons to a climax But that's not the whole story of the canyon. As our gaze continues upward Towards the source of rivers where the surface is rising more dramatically What else is exciting here? 03 Source of rivers Rivers of China There are at least two different sources Thus, two different canyon systems are formed. In the mountains and hills at lower altitudes Precipitation gathers along the slope The mud, sand and rocks washed away the hillside along the way. Forming grooves of varying sizes Ravine landform Loess Plateau in Northern China The spectacular valley landscape They vary in size From a width and depth of only a few meters Small grooves and shallow grooves (Valley landscape of the Loess Plateau in Gansu, photographer @Teng Hongliang, tagged @Hanqing/Planet Research Institute) ▼ Up to tens of meters in width and depth Thousands of meters in length Large cuts and gullies (On the Loess Plateau after the snow, the tree-like valleys are particularly clear, photographer @吴玮) ▼ They follow the law of evolution from small to large Under the wash of rain and snow Forming a complex network of gullies (Schematic diagram of valley landform evolution, drawn by @Hanqing/Planetary Research Institute) ▼ Eventually the plateau was cut into pieces Producing a landscape with thousands of ravines and gullies (Aerial photography of the Loess Plateau in Gaolan, Gansu, photographer @何旭龙) ▼ In the concept of geomorphology There is perennial water flowing at the bottom of the canyon The valleys are formed by repeated erosion of intermittent water flows. There is no stable river at the bottom Based on this distinction The true face of some internet celebrity "canyons" It is actually a larger valley. "Yucha Grand Canyon" in Yan'an, Shaanxi There is no stable river at the bottom There is only water and gravel left by mountain torrents. This shows that it is a valley formed by repeated erosion by mountain torrents. (Yucha Grand Canyon in Yan'an, Shaanxi Province. The white substance at the bottom is ice formed by accumulated water. Photographer: @李源) ▼ High up in the narrow valley walls Sometimes stuck dead wood can be seen They mark the heights that flash floods once reached. It can be seen that its momentum is strong (In the Yucha Grand Canyon, a strong mountain torrent stuck a dead tree between the rock walls. Photographer: @石耀臣) ▼ The "Mysterious Grand Canyon of Tianshan" in Kuche, Xinjiang A larger scale But there is no stable river at the bottom of the valley Just a huge ravine (There is no perennial river at the bottom of the mysterious Tianshan Grand Canyon in Kuche, Xinjiang, and it is also a huge valley. Photographer @蒋涵) ▼ When looking down from a high altitude A vast network of ravines carved into the reddish-brown mountain They are seasonal rain and snow The result of carving the hillside (Overlooking the mysterious Grand Canyon of Tianshan from high altitude, photographer @李珩) ▼ Only when the valley continues to cut down When the area groundwater is touched Water can flow out continuously Forming a stable river (Diagram of streams generated by deepening valleys, drawn by @Hanqing/Planetary Research Institute) ▼ So far The valley turns into a river source Mountains and hills at medium and low altitudes across China Giving life to rivers (The snow-covered Qinling Mountains, the valleys carved out by snow water give birth to rivers, photographer @刘忠文) ▼ The river flows from its origin in the valley to the distance Cut a canyon in the mountains And continue from the valleys on both sides of the canyon Gathering water (Please watch in horizontal mode, the valleys on the mountains on both sides of the Jinsha River Canyon, photographer @陈小羊) ▼ In this way A vast gully-river-canyon system Appearing on the earth Leading rivers to the sea (Diagram of the gully-river-canyon system, drawn by @Zheng Borong/Planetary Research Institute) ▼ But this system is not complete In western China, where the ground is rising rapidly On those peaks and plateaus that reach the sky There is also a world ruled by ice and snow (Glaciers and canyons around Gongga Snow Mountain, photographer @向文军) ▼ Glaciers are like frozen rivers Flowing down the gullies and canyons around the mountains Crushing rocks and reshaping valleys (Valley glacier landscape of Kunlun Mountains, photographer @仇梦涵) ▼ When the climate warms Glacier retreat U-shaped valley with a wide bottom Left behind in the depths of the snowy mountains (Schematic diagram of the formation of a glacial U-shaped valley, drawn by @王朝阳&张靖/Planetary Research Institute) ▼ Glacier meltwater flows into streams Flowing and cutting along the U-shaped valley (Qiangningcuo moraine lake and stream under Qiangyong Glacier, photographer @李珩) ▼ Continue to U-shaped valley Transformed into a "V"-shaped river canyon (The meltwater from the Laigu Glacier formed streams, transforming the U-shaped valley of the glacier into a "V"-shaped canyon. Photographer: @张政) ▼ Gradually build a complete Glacier-valley-river-canyon system (Sketch of the glacier-valley-river-canyon system, drawn by @Zheng Borong/Planetary Research Institute) ▼ Xinjiang Tianshan For such a huge system Provides a classic miniature case At the top of Tianshan Mountain, more than 5,000 meters above sea level Glacier meltwater flows in the U-shaped valley Gathered into messy streams (Glacier valley and river canyon under Bogda Peak in Tianshan Mountains, Xinjiang, photographer @赣州七爷) ▼ The stream receives water from the valley along its way. Converge into large rivers Cutting mountains to form valleys And finally rushed out of the valley Deposit silt at the foot of the mountain Forming continuous alluvial fans (Snow-capped mountains, glaciers, valleys, canyons and alluvial fans of Tianshan Mountain in Xinjiang, photographer @陆雨春) ▼ The rise of the Tianshan Mountains continues The river is still cutting rapidly Forming a deep pre-familiar river canyon in front of the mountain (Please watch horizontally, Anjihai Grand Canyon in Xinjiang, photographer @崔华明) ▼ On the walls of these canyons The flat terrace is eye-catching Records the history of intermittent uplift of the Tianshan Mountains It also records the history of the canyon's intermittent deepening. (Terraces on both sides of the Dushanzi Grand Canyon in Xinjiang, photographer @张波) ▼ In addition to the continuous terraces formed on both sides of the canyon It is also constantly washed away by rainfall. Produced dense valley groups (The dense gullies on the side walls of Dushanzi Grand Canyon, photographer @张波) ▼ Precipitation gathers in the valley At the end it joins the canyon river (The gully system on the side wall of Dushanzi Grand Canyon in Xinjiang, photographer @一乙) ▼ finally Meltwater from glaciers and precipitation from the clouds At the foot of the rising Tianshan Mountains Creates a glacier-valley-river-canyon system (Please watch in horizontal mode, alluvial fan canyon group in the northern foothills of Tianshan Mountains, map by @Zheng Yi/Planetary Research Institute) ▼ This system connects the mountains and the foothills. But the Tianshan Mountains themselves It is still the watershed between northern and southern Xinjiang. Separated into two different worlds Facing the ultimate obstacle of the watershed Can the canyon continue to be connected? 04 Through the Earth Yangtze River and Yellow River Provides us with a definite answer More than 100 million years ago Wushan was once an ancient watershed Separated the ancient Yangtze River in the east and the ancient Chuan River in the west But as the sources of the two rivers continue to cut through the mountains Finally cross the watershed (Please watch in horizontal mode, the Yangtze River Three Gorges are connected. The time of the connection is still controversial, ranging from tens of millions to hundreds of thousands of years ago; map by @郑伯蓉&风沉郁&陈志浩/Planetary Research Institute) ▼ The two rivers merge into one in the canyon The Three Gorges Project of the Yangtze River came into being (Chongqing Fengjie Kuimen is the starting point of the Three Gorges, and the foreground is Baidi City. Photographer: Li Qiong) ▼ On the upper reaches of the Yangtze River Countless watersheds, big and small, have also been connected Forming countless canyons The Yangtze River eventually reaches the Qinghai-Tibet Plateau Created the rolling Yangtze River flowing eastward (Tiger Leaping Gorge on the Jinsha River, photographer @Lu Wen) ▼ Different from the Yangtze River The Yellow River was originally a series of lakes and rivers. They are blocked by many ancient watersheds. The eastern mountains of the Loess Plateau were once one of them. When it is finally penetrated Formed the magnificent Shanxi-Shaanxi Grand Canyon (The Yellow River Jin-Shaan Grand Canyon, photographer @许兆超) ▼ In the upper reaches of the Yellow River The power of penetration is also very powerful The ancient lake systems that were originally blocked by the watershed It is also connected by rivers and canyons. The scattered water systems are integrated into a large river That’s why the Yellow River water comes from the sky (Longyangxia and Longyangxia Reservoir of the Yellow River, photographer @李珩) ▼ In the history of the evolution of the Chinese land Ravines and canyons Nurture and help rivers connect the earth When humans walked into the canyon It further enriches the connotation of the canyon. In vertical direction A canyon is a land passage through the mountains Countless merchants and troops shuttled through it Countless dangerous passes are hidden in it Stirring up the heroic spirit of war (Beijing Jundu Grand Canyon, one of the Eight Gorges of Taihang Mountains, with Juyongguan Great Wall stretching across it, was an important military pass in ancient times. Photographer: @Greatwj) ▼ The canyon is also an important shipping channel. The boat passes through the mountains To deliver wealth and goods to all directions (Please watch in horizontal mode, Qutang Gorge of the Three Gorges of the Yangtze River, photographer @王正坤) ▼ But the canyon also blocks traffic Bringing isolation Create a relatively closed environment (A village in the Taihang Mountain Grand Canyon in Linzhou, Henan Province, photographer @李建斌) ▼ For thousands of years People fleeing war and looking for a new home Migrating into the mountains along the canyon On the slopes or terraces on both sides of the canyon Building a paradise (Yanjin County in the Guanhe Gorge in Zhaotong, Yunnan, photographer @Yu Ming) ▼ To communicate with the outside world People living in the canyon Create multiple modes of transportation For example, zip line (Zipline bridge in Nujiang Gorge, photographer @张伊华) ▼ Hanging wall highway (Taihang Mountain Cliff Road, photographer @朱金华) ▼ now People use the power of technology Build bridges in valleys and dig holes in mountains (In the Taihang Mountains of Zezhou County, Jincheng City, Shanxi Province, the Xianshen River Bridge crosses the canyon. Photographer: Zhao Yaping) ▼ Roads and railways run along the canyon Leading to a home in the mountains (Guozigou Bridge in Yili, Xinjiang, photographer @赖宇宁) ▼ The earth has been connected for billions of years Connected with thousands of years of civilization So intertwined This is the canyon of China. Rich, magnificent, incomparable Deep Zone (Peach Blossom Valley in Bomi, Nyingchi, Tibet, photographer @张静) ▼ This article was created by Chief Writer: Yunwukongcheng Editor: Director Image: Imayama Map: Zhengyi Design: Han Qing & Zheng Borong Reviewer: Fengzi & Ding Hao Cover Photographer: Ren Jialing Main references of this article [1] Fang Shi. Study on the coupling of Songliao Basin and Daxinganling in Mesozoic and Cenozoic periods[D]. Jilin University, 2003. [2] Shu Liangshu. General Geology[M]. Geological Publishing House, 2010. [3] Liu Fenliang, Gao Hongshan, Li Zongmeng, et al. Terrace development and valley geomorphic evolution in the Qiaojia-Menggu section of the Jinsha River[J]. Acta Geographica Sinica, 2020, v.75(05):209-219. [4] Zhang Bin, Ai Nanshan, Huang Zhengwen, et al. The morphology and origin of the Jialing River meander in China[J]. Chinese Science Bulletin, 2007, 052(022):2671-2682. [5] Qiu Weili, Zhang Jiafu, Zhou Liping, et al. A preliminary study on the Yellow River terrace sequence in Hequ, Shanxi Province[J]. Quaternary Sciences, 2008, 28(4):544-552. [6] Liu Shangren. Distribution and characteristics of river terraces in western Guangdong[J]. Tropical Geography, 2007, 27(001):6-10. [7] Chen Weihai, Zhu Xuewen, Zhu Dehao, et al. Karst geological relics and development and evolution of the tiankeng and ground fissure in Fengjie, Chongqing[J]. Journal of Mountain Science, 2004, 22(1):22-22. [8] Wei Yuelong, Li Chengzhan, Chen Weihai, et al. Analysis of karst landscape characteristics and its formation and evolution in the Fengjie Tiankeng and Difeng scenic area in Chongqing[J]. Acta Geoscientia Sinica, 2019(5). [9] Lin C, Peng M, Tan H, et al. Crustal structure beneath Namche Barwa, eastern Himalayan syntaxis: New insights from three-dimensional magnetotelluric imaging[J]. Journal of Geophysical Research: Solid Earth, 2017, 122(7): 5082-5100. [10] M. Singh and A. Kumar, "Active Deformation Measurements at Mishmi Complex of Eastern Himalayan Syntaxis," International Journal of Geosciences, Vol. 4 No. 4, 2013, pp. 746-758. [11] Chang Zufeng, Chang Hao, Zang Yang, et al. New activity characteristics of the Weixi-Qiaohou fault and its relationship with the Red River fault [J]. Chinese Journal of Geomechanics, 2016, 22(003):517-530. [12] Zhang Zhiwei, Cheng Wanzheng, Ruan Xiang, et al. Seismicity and tectonic stress field characteristics of the Longmenshan fault zone before the Wenchuan earthquake with a magnitude of 8.0[J]. Acta Seismologica Sinica, 2009. [13] Wu Shufang, Liu Boyang, Lei Qi, et al. Study on the evolution process of slope rill erosion based on three-dimensional reconstruction technology[J]. Transactions of the Chinese Society of Agricultural Engineering, 2019, 035(009):114-120. [14] Luo Zehua. Research on the characteristics of gully systems and their disaster-causing effects in the Loess Plateau[D]. Lanzhou University, 2016. [15] Wu Yongqiu, Liu Baoyuan. Gullied erosion and prediction[J]. Journal of Basic Science and Engineering, 2000, 08(2):134-142. [16] Liu Baoyuan, Yang Yang, Lu Shaojuan. Analysis of several commonly used soil erosion terms and their significance in production practice[J]. Chinese Journal of Soil and Water Conservation, 2018, 016(001):9-16. [17] CHEN Yongzong. Valley types in the loess hilly area of the middle reaches of the Yellow River[J]. Geographical Science, 1984(04):35-41. [18] Liu Nanwei. Physical Geography-3rd Edition[M]. Science Press, 2014. [19] Zha Fangyong, Guo Wei, Luo Qianzhou, et al. Preliminary investigation of Danxia landform landscape resources in the Ordos Basin (Shaanxi) [C]// Proceedings of the 32nd Annual Meeting of the Tourism Geology and Geopark Research Branch of the Geological Society of China and the Tongren Geopark International Academic Symposium (Tourism Geology Proceedings Volume 24). 2017. [20] Ren Fang. Study on the genetic model of Danxia landform in Longhushan Geopark[D]. China University of Geosciences (Beijing), 2009. [21] Yang Wangtun. Study on the formation mechanism of Danxia landform in the southwestern margin of Ordos Basin[D]. Chang'an University. [22] Peng Xiaohua, Wu Hao, Li Yichao, et al. Preliminary study on the formation mechanism of the wave-like Danxia landform in Longzhou, Jingbian, Shaanxi Province[J]. Acta Geoscientia Sinica, 2020, 041(003):443-451. [23] Hu Guiming, Chen Jie, Qin Jintang, et al. Rapid incision of the Anjihai River Grand Canyon in the northern Tianshan Mountains since 3.7 ka[J]. Chinese Science Bulletin, 2020(15):1506-1518. [24] Zheng Hongbo, Wei Xiaochun, Wang Ping, et al. The past and present of the Yangtze River[J]. Science China: Earth Sciences, 2017, 047(004): P.385-393. [25] Baotian Pan; Huai Su; Zhenbo Hu; Xiaofei Hu; Hongshan Gao; Jijun Li; Eric Kirby (2009). Evaluating the role of climate and tectonics during non-steady incision of the Yellow River: evidence from a 1.24Ma terrace record near Lanzhou, China. , 28(27-28), 0–3290. doi:10.1016/j.quascirev.2009.09.003 Source: Planet Research Institute A group of National Geographic fans, focusing on exploring the extreme world |
<<: Why is the most peculiar appearance of the Yangtze River at its source?
Community operation is the product of the Interne...
[[139209]] Microsoft CEO Satya Nadella mentioned ...
This activity was based on the WeChat service acc...
Everyone knows how to use Facebook to attract tra...
An excellent short video often requires a good pl...
Reliable Axing: Today is different from the past,...
As one of ByteDance's popular apps, Toutiao i...
I have been in charge of advertising since the en...
When it comes to BOSE and SONY, all friends who h...
According to Business Insider, experts say self-d...
[[324038]] April 26th news: Recently, domestic iP...
Commercial illustration system course basics + ad...
There is a logic that says that we should use the...
How much is the quote for customized fitness in Z...