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CONFIRMATORY EVIDENCE OF PLEISTOCENE GLACIATION FROM THE HUANGSHAN, SOUTHERN ANHUI*

CONFIRMATORY EVIDENCE OF PLEISTOCENE GLACIATION FROM THE HUANGSHAN, SOUTHERN ANHUI* CONFIRMATORY EVIDENCE OF PLEISTOCENE GLACIATION FROM THE HUANGSHAN, SOUTHERN ANHUI* BY J. S. LEE (p) (Academia Sinica) A body óf facts gathered a few years ago from the Lower Yangtze Valley compelled the writer to draw the conclusion that glaciation occurred n parts of this region some time during the Pleistocene period. So radically this explanation differs from the "orthodox" view that "scientific bcepticism" has tended to do all what it can to keep such a disturbing hiterpretation in the background. A few geologists however may have been anxiously waiting for further evidence. For their consideration I In this short note I shall endeavour to jenture to offer the present case. call attention to a number of crucial points which have a fundamental bearing on the problem, leaving the detailed consideration to a later occasion. According to the 'New Atlas of China' (Ting, Wong and Tseng) the position of the Huangshan is located at about long. 118° 8' E. and tat. 300 10' N. Barometric readings by different observers vary consi.. The figures recorded by Dr. Lishouhua derably as regards its altitude. According to this observer the appear to represent the happy mean. Lienhuafeng which is the highest peak, http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Geologica Sinica (English Edition) Wiley

CONFIRMATORY EVIDENCE OF PLEISTOCENE GLACIATION FROM THE HUANGSHAN, SOUTHERN ANHUI*

Lee, J. S.
Acta Geologica Sinica (English Edition) , Volume 15 (3) – Sep 1, 1936
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Publisher
Wiley
Copyright
Copyright © 1936 Wiley Subscription Services, Inc., A Wiley Company
ISSN
1000-9515
eISSN
1755-6724
DOI
10.1111/j.1755-6724.1936.mp15003002.x
Publisher site
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Abstract

CONFIRMATORY EVIDENCE OF PLEISTOCENE GLACIATION FROM THE HUANGSHAN, SOUTHERN ANHUI* BY J. S. LEE (p) (Academia Sinica) A body óf facts gathered a few years ago from the Lower Yangtze Valley compelled the writer to draw the conclusion that glaciation occurred n parts of this region some time during the Pleistocene period. So radically this explanation differs from the "orthodox" view that "scientific bcepticism" has tended to do all what it can to keep such a disturbing hiterpretation in the background. A few geologists however may have been anxiously waiting for further evidence. For their consideration I In this short note I shall endeavour to jenture to offer the present case. call attention to a number of crucial points which have a fundamental bearing on the problem, leaving the detailed consideration to a later occasion. According to the 'New Atlas of China' (Ting, Wong and Tseng) the position of the Huangshan is located at about long. 118° 8' E. and tat. 300 10' N. Barometric readings by different observers vary consi.. The figures recorded by Dr. Lishouhua derably as regards its altitude. According to this observer the appear to represent the happy mean. Lienhuafeng which is the highest peak,

Journal

Acta Geologica Sinica (English Edition) – Wiley

Published: Sep 1, 1936

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