Table of Content

15 July 1934, Volume 1 Issue 2 Previous Issue    Next Issue

An Attempt at a NEW Classification of the Natural Regions of China F. HUNG 1934, 1 (2):  1-19.  doi: 10.11821/xb193402001 Abstract ( )   PDF (3161KB) ( )   Save The major division of China is into two regions with marked contrasts in their geographical environment: the Eastern Monsoon Regions and the Central Asiatic Plateaus, the physiographic boundary of which follows approximately the Kbingan Mountains, the In Shan, the Szech-wanese Alps and the edge of Yunnan Plateau. Related Articles | Metrics

An Analytica1 Study on the Scenic Regions in Chekiang G.YUN CHANG 1934, 1 (2):  62-69.  doi: 10.11821/xb193402004 Abstract ( )   PDF (527KB) ( )   Save 1. Orography 2. Geology 3. Drainage 4. Vegetation 5. Historical Remains. Related Articles | Metrics

A Comparlson between North Shensi basin&Szechuan basin C.Y.HSIEH 1934, 1 (2):  70-85.  doi: 10.11821/xb193402005 Abstract ( )   PDF (2760KB) ( )   Save One of the most conspicuous feature in Chinese geomorphology is the similardevelopment of some topographic forms such as basins, plateaus etc. Related Articles | Metrics

Geology and Human Relations in the Upper Huangho Region T.F.HOU, C.C.SUN 1934, 1 (2):  86-97.  doi: 10.11821/xb193402006 Abstract ( )   PDF (1901KB) ( )   Save The different geological formations and their ecouomie sigmficances. Related Articles | Metrics

The Aridity of North China:its Causes&Consequences COCHING CHU 1934, 1 (2):  98-109.  doi: 10.11821/xb193402007 Abstract ( )   PDF (3005KB) ( )   Save The rainfall of China is scanty when compared with the northeas ern partof the United States of Ameriea, almost identical in location and in latitude,The aridity of north China was found to be due to the following four causes. Related Articles | Metrics

Notes on Soils in China CHIN-KWEI LEE 1934, 1 (2):  110-128.  doi: 10.11821/xb193402008 Abstract ( )   PDF (3325KB) ( )   Save The classification of soils in China is essentially following Marbut's system2.It is first grouped into Pedocals and Pedalfers depending upon their lime content in the soil profiles. Pedocals are predominant in North China where precipitation is not enough to leach out the lime in the soils. While Pedalfers arepredominant in South China where the rainfall is higher. Related Articles | Metrics

A Model Map of China Under Preparation S.Y.TSENG 1934, 1 (2):  129-134.  doi: 10.11821/xb193402009 Abstract ( )   PDF (1976KB) ( )   Save Following the completion of the New Atlas of China compiled by V. K.Ting, W. H. Wong and S. Y. Tseng, the modeling of a relief map of China hasbeen undertaken by the National Geological Survey of China under the directionof the writer since late winter of 1933. Related Articles | Metrics