引用本文:
【打印本页】   【下载PDF全文】   View/Add Comment  Download reader   Close
←前一篇|后一篇→ 过刊浏览    高级检索
本文已被:浏览 1594次   下载 1678 本文二维码信息
码上扫一扫!
分享到: 微信 更多
美国科德角半岛地貌
李 凡1, 唐宝珏1
中国科学院海洋研究所
摘要:
关键词:  
DOI:
分类号:
基金项目:
INTRODUCTION TO THE GEOMORPHOLOGICAL PATTERN ON THE CAPE COD PENINSULA
Abstract:
Cape Cod peninsula, located in the southeast of the massachusetts state, was formed by the accumulation of the moraine after the glacier melted in the late pleistocene and early Holocene. The moraine knobs, moraine plane, accumulated sand and gravel coast, erosional coast such as sea scarp and coastal dune etc. geomorphological patterns were evolved on the Cape Cod peninsula. Some part of the coast were effectively protected and utilized fay the resident but most of it still not been protected.
Key words:  
Copyright ©  Editorial Office for Marine Sciences Copyright©2008 All Rights Reserved
Supervised by: Chinese Academy of Sciences (CAS)   Sponsored by: Institute of Oceanology, CAS
Address: 7 Nanhai Road, Qingdao, China.  Postcode: 266071  Tel: 0532-82898755  E-mail: bjb@qdio.ac.cn
Technical support: Beijing E-Tiller Co.,Ltd.