Quaternary glacio-erosional landforms in Laoshan Mountain and their constraints on the origin of Jiaozhou Bay, Qingdao, east of China

Hongbo Lu; Shiyong Yan; Yue Zhang

doi:10.1007/s00343-007-0139-0

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Quaternary glacio-erosional landforms in Laoshan Mountain and their constraints on the origin of Jiaozhou Bay, Qingdao, east of China

OriginalPaper | Updated：2023-05-16

- Quaternary glacio-erosional landforms in Laoshan Mountain and their constraints on the origin of Jiaozhou Bay, Qingdao, east of China
- Quaternary glacio-erosional landforms in Laoshan Mountain and their constraints on the origin of Jiaozhou Bay, Qingdao, east of China
- 海洋湖沼学报（英文） 2007年25卷第2期页码：139-148
- Affiliations：
  
  1. Department of Earth Sciences China University of Petroleum
  2. Library of China University of Petroleum
- Author bio：
- Funds：
  
  Sponsored by Doctorate Research Program of China University of Petroleum (No. Y020109)
- DOI：10.1007/s00343-007-0139-0
  中图分类号：
- 纸质出版：2007
- Accepted：
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Quaternary glacio-erosional landforms in Laoshan Mountain and their constraints on the origin of Jiaozhou Bay, Qingdao, east of China[J]. 海洋湖沼学报（英文）, 2007,25(2):139-148.

Lu, H., Yan, S. & Zhang, Y. Quaternary glacio-erosional landforms in Laoshan Mountain and their constraints on the origin of Jiaozhou Bay, Qingdao, east of China., Chin. J. Ocean. Limnol. 25, 139–148 (2007). https://doi.org/10.1007/s00343-007-0139-0
Quaternary glacio-erosional landforms in Laoshan Mountain and their constraints on the origin of Jiaozhou Bay, Qingdao, east of China[J]. 海洋湖沼学报（英文）, 2007,25(2):139-148. DOI： 10.1007/s00343-007-0139-0.

Lu, H., Yan, S. & Zhang, Y. Quaternary glacio-erosional landforms in Laoshan Mountain and their constraints on the origin of Jiaozhou Bay, Qingdao, east of China., Chin. J. Ocean. Limnol. 25, 139–148 (2007). https://doi.org/10.1007/s00343-007-0139-0 DOI：

摘要

Abstract

A field investigation on Quaternary glacial landforms in Laoshan Mountain has discovered many glacial potholes

scouring grooves on top of granite ridges

and large boulders. These erosional landforms were formed by the meltwater from the overlying ice cap

suggesting that there was at least an ice cap covering Laoshan Mountain and the surrounding areas or even a continental ice sheet over the vast area of Shandong Province in the Late Pleistocene. The ice sheet was obstructed by the Laoshan Mountain

Dazhu Mountain and Xiaozhu Mountain in the coastal areas as it moved toward the Yellow Sea. The ice flows eroded the bedrock and carved the weak intersection of the fault systems in the NE and NW directions into a deep channel

which gradually formed a fjord in the area of the Jiaozhou Bay basin by 20.00 ka BP. The seawater gradually invaded the fjord from the beginning of the Holocene (11.00 ka BP) and Jiaozhou Bay was eventually formed. Similar fjords are easily found along the east of China and they share a similar origin because of the Quaternary glaciation in the region.

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references

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