By Tianjin Library
A Pictorial list of the Qing Dynasty - Rivers and websites, contains significant different types of maps: river maps and maps of ancient sites.China was once an agrarian society in the course of medieval instances, and harnessing rivers performed a huge function in maintaining social improvement. A Compendium on Harnessing Rivers, which used to be accomplished within the forty second 12 months of Emperor Kangxi s reign (1703), includes a huge variety of invaluable photographs compiled and edited via Zhang Penghe, the governor-general answerable for rivers. The publication additionally comprises maps of varied rivers drawn by way of nameless artists. They list the vicissitudes of rivers and parts alongside the banks whereas while realistically tracing the shapes of urban partitions, areas of old curiosity, and wonder spots alongside the rivers.As a mom river of the chinese language country, the Yellow River has continually been the point of interest of a lot recognition, leading to extra historical chinese language maps of this river than the other in China. This ebook collects many maps of the Yellow River made in the course of the overdue Qing interval, such a lot of which additionally checklist in writing the dates of the crevasse and the closure of a undeniable portion of the river and the deployment of infantrymen guarding it. an entire Map of the Yellow River inside Shandong, A Map of the Yellow River in the entire Province of Shandong, A Concise whole Map of the Yellow River inside of Shandong are one of the maps awarded during this book.Other maps to be had contain Maps of the Rivers less than Baoding Prefecture, Maps of the Rivers below Zhengding Prefecture, and Maps of the Rivers less than the 5 Prefectures of Zhili Ji, Zhao, Shen, Ding, and Yi.In addition, there are 3 maps of old curiosity: Maps of His Majesty s transitority residing Palaces on His go back trip, Maps of Dagu Batteries, and Illustrations of Wendeng, Weihai, and different historic Sites..KEY gains- Rivers and websites is the 3rd booklet in A Pictorial checklist of the Qing Dynasty sequence. the opposite 3 books are entitled company records (Released might 2008), outdated Manchu Capital (Released June 2008), and Manchurian Railway (to be free up November 2008).- inclusive of over four hundred maps that seem in chronological order in ten different types, every one embellished with coloured drawings.- unique photographs and entire colour
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Additional resources for A Pictorial Record of the Qing Dynasty - Rivers and Sites
Major tributaries of the Ganga in the Punjab were captured by the Indus. Either northeastward advance of the tributaries of the Indus resulted in the capture of the tributaries of the Ganga, or tectonic episodes of the Main Central Thrust and early Miocene uplift of the Salt Range may have caused this major drainage reorganization (Clift and Blusztajn, 2005). For the main part, hinterland tectonics and focused denudation because of uplift driven by erosional unloading appear to be the main influential factors in the growth and development of the large river system sourced in the Himalaya; base level changes modulate the large river system(s) in this region in a framework determined by coupled hinterland tectonic-climatic processes.
2 TECTONIC SETTINGS OF LARGE RIVER SYSTEMS Most modern large river systems have their headwaters in the uplifted zones of large orogens, and flow through extensive continental-scale cratonic areas. 2. Large continental-scale masses such as those of the Indian (drained by the Ganga, Brahmaputra), N. American (Mississippi, Rio Grande), African (Congo, Zambezi, Orange) and Australian (Murray-Darling) Shields adjoining major compressional belts on the globe provide the necessary ‘scale’ constraints for the formation of these rivers, and their sustenance through a long period of time.
Its source region in the Precambrian Guinean Shield is just 240 km from the Atlantic Ocean but the river flows away from the sea into the Sahara Desert and then takes a sharp right turn to southeast to flow into the Gulf of Guinea. , 1990; Gasse, 2000). 3g) tend to develop as dome-flank systems (Cox, 1989). , 1973; White and McKenzie, 1989) postulates that the fracturing of the domal structure formed by mantle plumes may produce rifts and volcanism. Cox (1989) suggested that the rivers rising close to the escarpment mark the flank of the remnant dome; they drain away from the continental edge and the failed arms of the rift system leads the drainage towards the new ocean.