Skip to main content
Log in

The discovered deep-buried lake ice in source region of the Huanghe River

  • Published:
Chinese Geographical Science Aims and scope Submit manuscript

Abstract

The 4.45 m-thick pure ice lens have been discovered firstly at depth from 19.81–24.26 m in the bore No.6, which locates in north bank of the Ngoring Lake. In source region of the Huanghe (Yellow) River,14C dating, X-ray diffraction, pollen analysis, micropalaeontology, chemical components, environmental isotope2H,3H,18O and freezing point of the ice and water samples from the bore have been tested and microorganism in the ice have been also appraised with microscope. Combined with the research on geomorphy and Quaternary around the lake, the ice lens are determined as a kind of deep-buried lake ice, formed in 35,030–45,209 yr.B.P., and annual mean air temperature was about −10°C during that time.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  1. 王 绍令, 等. 环境同位素在青藏高原多年冻土区地 下冰研究中的应用. 冰川冻土, 1989, 11 (1): 53–60.

    Google Scholar 

  2. 王 平. 我国冰川的雪冰化学研究. 冰川冻土, 1986, 8(1): 40–41.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Wang, S., Li, W. The discovered deep-buried lake ice in source region of the Huanghe River. Chinese Geographical Science 3, 247–254 (1993). https://doi.org/10.1007/BF02664277

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02664277

Key Words

Navigation