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The Geomorphologic and Geological Characteristics of China Qinling Mountain Based on DEM

Received: 29 November 2016    Accepted:     Published: 7 December 2016
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Abstract

The Qinling Mountain plays an important role in the formation and evolution of China continent, which is the North-Southdivide of China in physical geography. It constitutes three parts: East-Qinling, Central-Qinling and Western-Qinling Mountains. The paper was aimed at analyzing the different geomorphic characteristics based on DEM and the relation between the landforms and geology. Some topographic parameters were calculated, such as mean elevation, summit and base level, local relief and mean slope. The DEM data was the SRTM DEM with spatial resolution of 90m. The swath profiles method was used, which the profiles were divided into 5-km -wide segments. For each segment, max, min and mean elevation data of 100-km-long swath were projected onto the profile. Three swath profiles were constructed across the eastern, central and western part through the Qinling Mountains. The results show that: elevation is higher in the west traverse comparing the central and east traverse. The area of granitite by high values of local relief which are related to the deeply incised valleys prevailing in the Taibai Mountain. Lithology and drainage network influence the geomorphology pattern in Qinling Mountain which is the reason that different geomorphology from the south to north.

Published in Earth Sciences (Volume 5, Issue 6)
DOI 10.11648/j.earth.20160506.13
Page(s) 104-110
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Geomorphologic, Qinling Mountain, DEM, Relief

References
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Cite This Article
  • APA Style

    Ye Baoying. (2016). The Geomorphologic and Geological Characteristics of China Qinling Mountain Based on DEM. Earth Sciences, 5(6), 104-110. https://doi.org/10.11648/j.earth.20160506.13

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    ACS Style

    Ye Baoying. The Geomorphologic and Geological Characteristics of China Qinling Mountain Based on DEM. Earth Sci. 2016, 5(6), 104-110. doi: 10.11648/j.earth.20160506.13

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    AMA Style

    Ye Baoying. The Geomorphologic and Geological Characteristics of China Qinling Mountain Based on DEM. Earth Sci. 2016;5(6):104-110. doi: 10.11648/j.earth.20160506.13

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  • @article{10.11648/j.earth.20160506.13,
      author = {Ye Baoying},
      title = {The Geomorphologic and Geological Characteristics of China Qinling Mountain Based on DEM},
      journal = {Earth Sciences},
      volume = {5},
      number = {6},
      pages = {104-110},
      doi = {10.11648/j.earth.20160506.13},
      url = {https://doi.org/10.11648/j.earth.20160506.13},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20160506.13},
      abstract = {The Qinling Mountain plays an important role in the formation and evolution of China continent, which is the North-Southdivide of China in physical geography. It constitutes three parts: East-Qinling, Central-Qinling and Western-Qinling Mountains. The paper was aimed at analyzing the different geomorphic characteristics based on DEM and the relation between the landforms and geology. Some topographic parameters were calculated, such as mean elevation, summit and base level, local relief and mean slope. The DEM data was the SRTM DEM with spatial resolution of 90m. The swath profiles method was used, which the profiles were divided into 5-km -wide segments. For each segment, max, min and mean elevation data of 100-km-long swath were projected onto the profile. Three swath profiles were constructed across the eastern, central and western part through the Qinling Mountains. The results show that: elevation is higher in the west traverse comparing the central and east traverse. The area of granitite by high values of local relief which are related to the deeply incised valleys prevailing in the Taibai Mountain. Lithology and drainage network influence the geomorphology pattern in Qinling Mountain which is the reason that different geomorphology from the south to north.},
     year = {2016}
    }
    

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  • TY  - JOUR
    T1  - The Geomorphologic and Geological Characteristics of China Qinling Mountain Based on DEM
    AU  - Ye Baoying
    Y1  - 2016/12/07
    PY  - 2016
    N1  - https://doi.org/10.11648/j.earth.20160506.13
    DO  - 10.11648/j.earth.20160506.13
    T2  - Earth Sciences
    JF  - Earth Sciences
    JO  - Earth Sciences
    SP  - 104
    EP  - 110
    PB  - Science Publishing Group
    SN  - 2328-5982
    UR  - https://doi.org/10.11648/j.earth.20160506.13
    AB  - The Qinling Mountain plays an important role in the formation and evolution of China continent, which is the North-Southdivide of China in physical geography. It constitutes three parts: East-Qinling, Central-Qinling and Western-Qinling Mountains. The paper was aimed at analyzing the different geomorphic characteristics based on DEM and the relation between the landforms and geology. Some topographic parameters were calculated, such as mean elevation, summit and base level, local relief and mean slope. The DEM data was the SRTM DEM with spatial resolution of 90m. The swath profiles method was used, which the profiles were divided into 5-km -wide segments. For each segment, max, min and mean elevation data of 100-km-long swath were projected onto the profile. Three swath profiles were constructed across the eastern, central and western part through the Qinling Mountains. The results show that: elevation is higher in the west traverse comparing the central and east traverse. The area of granitite by high values of local relief which are related to the deeply incised valleys prevailing in the Taibai Mountain. Lithology and drainage network influence the geomorphology pattern in Qinling Mountain which is the reason that different geomorphology from the south to north.
    VL  - 5
    IS  - 6
    ER  - 

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Author Information
  • Institute of Geological Survey, China University of Geosciences, Beijing, China

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