Abstract
Colorado's Cinnamon Gulch releases acid rock drainage (ARD) from anthropogenic and natural sources. In 2001, the total discharge from Cinnamon Gulch was measured at 1.02 cfs (29 L/s) at base flow and 4.3 cfs (122 L/s) at high flow (spring runoff). At base flow, natural sources account for 98% of the discharge from the watershed, and about 96% of the chemical loading. At high flow, natural sources contribute 96% of discharge and 92 to 95% of chemical loading. The pH is acidic throughout the Cinnamon Gulch watershed, ranging from 2.9 to 5.4. At baseflow, nearly all of the trace metals analyzed in the 18 samples exceeded state hardness-dependent water quality standards for aquatic life. Maximum dissolved concentrations of selected constituents included 16 mg/L aluminum, 15 mg/L manganese, 40 mg/L iron, 2 mg/L copper, 560 μg/L lead, 8.4 mg/L zinc, and 300 mg/L sulfate. Average dissolved concentrations of selected metals at baseflow were 5.5 mg/L aluminum, 5.5 mg/L manganese, 14 μg/L cadmium, 260 μg/L copper, 82 μg/L lead, and 2.8 mg/L zinc.
Similar content being viewed by others
References
Bookstrom AR, Naeser CW, Shannon JR (1987) Isotopic age determinations, unaltered and hydrothermally altered igneous rocks, north-central Colorado Mineral Belt. Isochron/West, no 49, pp 13–20
CGS (Colorado Geologic Survey) (2003) Ground water atlas of Colorado (in press)
CSU (Colorado State University) (2002) Colorado Water Resources Research Institute Website (http://waterknowledge.colostate.edu)
Emerick JC, Huskie WW, Cooper DJ (1988) Treatment of discharge from a high elevation metal mine in the Colorado Rockies using an existing wetland. Mine Drainage and Surface Mine Reclamation, Proceedings of a conference sponsored by the American Society for Surface Mining and Reclamation, The US Bureau of Mines, and the Office of Surface Mining and Reclamation and Enforcement, Pittsburgh, Pennsylvania, April 19–21, 1988, US Dept of the Interior, pp 345–352
Karlsson S, Allard B, Håkansson K (1988) Characterization of suspended solids in a stream receiving acid mine effluents, Bersbo, Sweden. Appl Geochem 3:345–356
Lovering TS (1935) Geology and ore deposits of the Montezuma quadrangle, Colorado. US Geol Surv Prof Pap 178
Meyer WA, Streufert RK, Williamson MA (1996) A comparison of natural acid rock drainage occurrences in Colorado. In: Bell RS, Cramer MH (compilers), Proceedings of the Symposium on the Application of geophysics to engineering and environmental problems (SAGEEP '96): April 28–May 2, 1996, Keystone, Colorado. Environmental and Engineering Geophysical Society (pub), Wheat Ridge, Colorado, USA (manuscript released as addendum to proceedings)
Neubert JT (2000) Naturally degraded surface waters associated with hydrothermally altered terrane in Colorado. Colorado Geol Surv Open-File Report 00–16, 153 pp
Neubert JT, Kurtz J P, Bove DJ, Sares MA (2003) Natural acid rock drainage associated with hydrothermally altered terrane in Colorado. Colorado Geol Surv (in press)
Neuerburg GJ (1971) Distribution of selected accessory minerals in the Montezuma stock, Summit County, Colorado. US Geol Surv Misc Geol Invest, map I-608, scale 1:31,680
Neuerburg GT, Botinelly T (1972) Map showing geologic and structural controls of ore deposits, Montezuma District, Central Colorado. US Geol Surv Misc Geol Invest, map I-750
Parkhurst DL, Appelo CAJ (1999) PHREEQC (version 2) - A computer program for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations. US Geol Surv Water-Resour Invest Rep 95–4259
Tweto O (compiler) (1979) Geologic map of Colorado. US Geol Surv Map, scale 1:500,000
Acknowledgments
The US Forest Service provided funding for the Cinnamon Gulch watershed characterization, and for the production of this paper. Thanks are due to Matt Sares and Bob Wood of CGS for critical reviews of the paper, and to Larry Scott of CGS for producing the figures.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Bird, D.A. Characterization of anthropogenic and natural sources of acid rock drainage at the Cinnamon Gulch abandoned mine land inventory site, Summit County, Colorado. Env Geol 44, 919–932 (2003). https://doi.org/10.1007/s00254-003-0835-9
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00254-003-0835-9