地肱:大伾山与古代黄河河道变迁  

Digong: Dapi Mountain and the Changes of the YellowRiver Course in Ancient Times

作　　者：陈东川 CHEN Dongchuan(Center for Historical Geographical Studies,Fudan University,ShangHai 200433,China)

机构地区：[1]复旦大学历史地理研究中心,上海200433

出　　处：《平顶山学院学报》2024年第3期58-62,共5页Journal of Pingdingshan University

摘　　要：作为黄河下游起始河段的标志性地物之一,“大伾”指的是位于今郑州巩义、荥阳两市北部的大伾山。自洛口至于汜水口间的大伾山与其东侧的广武山一线,自古便被称作“地肱”。这一称号正反映了黄河下游首段河道的基本流向与大伾、广武两山顶托作用之间的密切关系。不仅如此,大伾山至今仍是郑州与黄淮大平原城市安全的天然保障。As one of the landmark of the beginning of the lower reaches of the Yellow River,Dapi refers to Dapi Mountain located in the north of Gongyi and Xingyang of present Zhengzhou.The line between Dapi Mountain and Guangwu Mountain from Luokou to Sishuikou has been called Digong since ancient times.This title reflects the close relationship between the basic flow direction of the first section of the lower reaches of the Yellow River and the supporting role of Dapi Mountain and Guangwu Mountain.More than that,Dapi Mountain is still a natural guarantee for the city safety of Zhengzhou and Huanghuai Plain.

关 键 词：地肱 大伾山 广武山 郑州 

分 类 号：K901[历史地理—人文地理学]