我国某些历史地貌学问题的刍议  

SOME QUESTIONS ON THE HISTORICAL GEOMORPHOLOGY PROBLEM OF CHINA

作　　者：曾昭璇[1] 

机构地区：[1]华南师范大学地理系

出　　处：《地理研究》1983年第2期12-19,共8页Geographical Research

摘　　要：本文提出历史地貌学是地貌学的一个组成部分,它主要研究人类历史时期地貌的变迁。它在理论上能对地貌学上一些基本理论给予证实或提供重要依据;在生产上能按历史演变过程提出一些建设性意见,为有关建设部门参考。并举珠江三角洲水道及黄河下游的整治意见为例。说明历史地貌学能对生产建设提供科学依据。Historical geomorphology is normally a study of the changes of landformsin the historical period.It has developed rapidly with its growing needs in the. production and construction of our country .Geologists, pedologists, by draulicengineers, archeologists and conservationists often consult historical geomor-phologic knowledge.In theory, we know that the river meandering channel would migrate on the flood plain,but when did it cut off the meander neck? The gully would be elongated continually,but how many meters has it been elongatedyThe piedmont would be buried by debris and sand coming down from the mountain slopes, but how many meters per 100 years? Historical geomorphology answers such kind of questions.Therefore, after researches on historical geomorphology, one would get some good ideas,which are helpful to the production and construction in our country. For example, the yellow River was not in one channel during the historical time.The present single channel form is the result of building dykes by human beings,so it must be noted,that its floods have destroyed the dykes and chan-nged its course.And thus,in this article, the author suggests that the Yellow River might be branched into a fan-like channel system instead of one channel at the present day.For the fan-like channel system can make all the soil and water stay in the great, thirsty North China plain.

关 键 词：历史地貌学 西江 黄河 地貌学研究 古河道 古地貌 平原 三角洲 济水 河床 

分 类 号：P9[天文地球—自然地理学]