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• 1935 Volume 2 Issue 3
  Published: 15 July 1935

    

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  On some examples of River Capture

  C.Y.Hsieh

  1935, 2(3): 1-11. https://doi.org/10.11821/xb193503006

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  In the course of stream development, each stream and its tributaries tend toincrease their length by headward erosion, or in other words to enlarge their catchment area.
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  ON THE DISTRIBUTION OF THERMAL SPHINGS IN CHINA

  H.T.Chang

  1935, 2(3): 13-22. https://doi.org/10.11821/xb193503007

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  The total number of thermal springs as mentioned in geographical records ofChinese provinces except Sinkiang together with those known through modernreports amounts to 512.
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  R閟ume d'etude sur la geographie urbaine d'Ou-si

  Wang Chung-chi

  1935, 2(3): 23-63. https://doi.org/10.11821/xb193503008

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  La situation d'Ou-si Le pays des canaux dans la plaine deltaique du Yang-tseu est la situation ou position g閚閞ale g閛gaphique d'Ou-si.
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  DIE BEDEUTUNG DER OZEANOGRAPHIE UND DER PLAN F躌 GR躈DUNG DER SEEWARTE

  Von John Lee

  1935, 2(3): 65-79. https://doi.org/10.11821/xb193503009

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  In dieser Abhandlung legt der Verfasser die Bedeutung der Ozeanographie sowie die Beziehungen zwischen ihr und anderen Wissensehaften dar.
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  THE FLOODS AND DROUGHTS OF THE LOWER YANGTZE VALLEY AND THEIR PREDICTIONS

  K.Y.Cheng

  1935, 2(3): 81-91. https://doi.org/10.11821/xb193503010

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  During Ching dynasty from 1644 to 1911, an interval of 268 years, there occurred in the lower Yangtze valley 197 floods and 156 droughts.
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  THE DEVELOPMENT OF GEOGRAPHY IN CHINA DURING LAST TWENTY YEARS

  G.Y.Chang

  1935, 2(3): 93-132. https://doi.org/10.11821/xb193503011

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  (1) Cartography (2) Geophysics (3) Physiography (4) Climatology