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Holocene Environmental Changes and the Evolution of the Neolithic Cultures in China

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Landscapes and Societies

Abstract

China has three great topographic zones (Fig. 19.1). The first, in the eastern part of the mainland, contains plains ranging from a few tens of meters to ca. 100 m in elevation and hills and low mountains ranging from hundreds of meters to ca. 1000 m asl. The first zone passes gradually westwards into the second, which is characterized primarily by hills and mountains over 1000 m high and by deep river valleys. The third topographic zone is the Qinghai-Tibetan Plateaus with average altitude over 4000 m asl.

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  1. College of Environmental and Urban Sciences, Peking University, 100871, Beijing, China

    Duowen Mo

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  1. Duowen Mo
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  2. Zhijun Zhao
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  4. Minglin Li
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Correspondence to Duowen Mo .

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  1. School of Environmental Sciences, University of Guelph, Axelrod Building, Guelph, N1G 2W1, Ontario, Canada

    I. Peter Martini

  2. Axelrod Building, School of Environmental Sciences, University of Guelph, Guelph, N1G 2WI, Ontario, Canada

    Ward Chesworth

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Mo, D., Zhao, Z., Xu, J., Li, M. (2010). Holocene Environmental Changes and the Evolution of the Neolithic Cultures in China. In: Martini, I., Chesworth, W. (eds) Landscapes and Societies. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-9413-1_19

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