摘要
清华校园建立在古清河故道和海淀台地交界之处,拥有河谷和台地双重地貌。校园内万泉河水从中流过,河湖纵横,水流充沛。清华地貌何以形成?三百年前熙春园(清华园前身)何以选址在此?当地人地关系何以建立?清华园虽然已经繁荣了三百年,但却很少有人注意这些问题,而这正是今天我们了解校园、保护校园、利用校园、开发校园的重要基础。追寻清华校园的形成与利用,具有重要的文化意义。
Tsinghua University was built at the intersection between the ancient Qinghe River old course and Haidian platform, with both characteristic geomorphologies of the valley and platform. The Wanquan river runs across the campus. Lakes and rivers are interspersed. How was the geomorphology of Tsinghua campus formed? Why was it selected for the Xichun Park three hundred years ago in which the Qinghua Park is situated now? How was the local man-land relationship built up? Although the Qinghua Park has been prosperous for 300 years, few people care about these questions. The answers to these questions are keys to understand, protect, harness, and develop the campus. This paper is aimed to study the geomorphological formation of the Tsinghua campus and buildup of new man-land relationship. Pursuit of the formation history and value of University campus has important cultural significance.
出处
《北京社会科学》
CSSCI
北大核心
2010年第3期34-39,共6页
Social Sciences of Beijing
关键词
古清河故道
海淀台地
万泉河水系
清华校园地貌
ancient Qinghe River old course
Haidian platform
Wanquan river system
geomorphology of Tsinghua campus