A Note to the Lignite occurrence in Lukundol, Kathmandu

Authors

  • R. M. Tuladhar Department of Mines and Geology, Lainchaur, Kathmandu

DOI:

https://doi.org/10.3126/jngs.v2i1.32529

Keywords:

Lignites, Lukundol Formation, Quaternary fluvio-lacustrine, Kathmandu valley

Abstract

The Quaternary fluvio-lacustrme sediments of Kathmandu Valley arc characterized by the occurrence of low quality lignite. The lignites are more confined to the lower part of this deposition in the Lukundol Formation, consisting of clay, silt, sand and coarse sand. These lignites show ambivalent characters between lignite and peat.

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Published

1982-06-30

How to Cite

Tuladhar, R. M. (1982). A Note to the Lignite occurrence in Lukundol, Kathmandu. Journal of Nepal Geological Society, 2(1), 47–51. https://doi.org/10.3126/jngs.v2i1.32529

Issue

Vol. 2 No. 1 (1982)

Section

Articles

License

© Nepal Geological Society