Skip to Main Content
Chemical fluxes and sensitivity to acidification of two high elevation catchments in southern WyomingAuthor(s): J. O. Reuss; F. A. Vertucci; R. C. Musselman; R. A. Sommerfeld
Source: Journal of Hydrology. 173: 165-189.
Publication Series: Scientific Journal (JRNL)
Station: Rocky Mountain Research Station
PDF: View PDF (1.47 MB)
DescriptionHydrological and chemical fluxes were examined for East and West Glacier Lakes and their adjacent high-elevation (3200-3700 m) catchments in the Snowy Range of southern Wyoming. Both lakes are approximately 3 ha, but the East Glacier catchment (29 ha) is about half the size of West Glacier. Bedrock is primarily quartzite that has been heavily fractured and crossed with mafic intrusions.
- You may send email to email@example.com to request a hard copy of this publication.
- (Please specify exactly which publication you are requesting and your mailing address.)
- We recommend that you also print this page and attach it to the printout of the article, to retain the full citation information.
- This article was written and prepared by U.S. Government employees on official time, and is therefore in the public domain.
CitationReuss, J. O.; Vertucci, F. A.; Musselman, R. C.; Sommerfeld, R. A. 1995. Chemical fluxes and sensitivity to acidification of two high elevation catchments in southern Wyoming. Journal of Hydrology. 173: 165-189.
Keywordschemical fluxes, acidification, high elevation catchments, bedrock
- Appendix B: Phytoplankton Species
- Spatial and temporal patterns in water chemistry of two high elevation lakes in southeast Wyoming
- Soils [Chapter 5]
XML: View XML