Browse

洛東江 上流와 王澼川의 河岸段丘
River Terraces of the Upper Nakdong River and Wangpi Stream

Cited 0 time in Web of Science Cited 0 time in Scopus
Authors
孫明遠
Issue Date
1993-08
Publisher
서울대학교 국토문제연구소
Citation
지리학논총 별호, Vol.17, pp. 1-120
Keywords
river terraceterrace depositslocal crustal movementriver captureQuatenary Paleoenvironment하안단구단구퇴적물국지적 지반융기하천쟁탈제4기 고환경
Abstract
River terrace is the main subject of Quaternary research in the nonglaciated

area such as Korean Peninsular. Much information about geomorphological events such as the Quaternary paleoclimate and the crustal movement is recorded in river terraces. Therefore, to study river terrace Will be helpful to understaand the history of geomorphological development and Quaternary paleoenvironment.

This dissertation is an attempt to elucidate the relationships among c1imatic changes, crustal movements, and the development of river terrace at the upper

reach of the great rivers in Korean Peninsular. I selected the drainage basins of

Nakdong River and Banbeon Stream which flows through the western side of,

and Wangpi Steram which flows through the western side of Taebaik

Mountains, where river terraces were typically developed. And by ana1ysing the

spatial distribution of terraces formed at each basin, the physical and chemical

characterics of terraces deposite, depositional structures of outcrops, I clarified

the morphogenetic processes of terraces.
Language
Korean
URI
http://hdl.handle.net/10371/89831
Files in This Item:
Appears in Collections:
College of Social Sciences (사회과학대학)Institute for Korean Regional Studies (국토문제연구소)지리학논총 별호지리학논총 별호 Volume 16/17 (1993)
  • mendeley

Items in S-Space are protected by copyright, with all rights reserved, unless otherwise indicated.

Browse