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前言望城崗,位于南昌市西部偏南,距北火車站约八公里余。本文所指望城崗附近,系西起烏井,东抵贛江,南北以十公里的一线作为范圍。本区地貭基础古老,震旦紀千枚岩系分布极广,其上复第四紀紅土及近代冲积层,从整个地貌来看,实为波状起伏的准平原,相对高度一般在60公尺以內,个別岡阜可逾60公尺,望城崗即其中之一,登岡巒高处,可远眺南昌旧城,望城崗的名称,即由此而来。
Foreword Wangcheng Gang, Nanchang in the western part of the south, about eight kilometers from the North Railway Station. This article is expected around the city post, the Department of West wells, east of Gan River, north and south to 10 km of the line as a range. In this area, the ancient basement and the Sinian phyllite series are widely distributed. The Quaternary laterites and the alluvial layers of modern alluvium are undulating plains in the whole landform. The relative height is generally 60 km Within a foot, individual Gang Fu can be more than 60 meters, Wang Cheng Gang is one of them, Deng Gangluan height, overlooking the old city of Nanchang, Wangchenggang name, that is from.