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Creator:: Collier, Robert W., Dymond, Jack, and McManus, James
Abstract:: As a result of the past three years of field studies and our interpretation of these and other data from the literature, we conclude that there are inputs of hydrothermal fluids into the bottom of Crater Lake. The dissolved materials associated with these thermally and chemically enriched fluids, coupled with...
Resource Type:: Technical Report

Creator:: McManus, James, Collier, Robert W., Chen, Chen-Tung A., and Dymond, Jack
Abstract:: Active inputs of thermally and chemically enriched fluids at the bottom of Crater Lake create small vertical and horizontal heterogeneities in the deep-lake temperature and salt distribution. Using an internally recording CTD and a precise definition for salinity as a function of in situ conductivity and temperature, we assess the...
Resource Type:: Article
Full Text:: MCMANUS, JAMES, ROBERT W. COLLIER, CHEN-TIJNG A. CHEN, AND J

Creator:: Good, James W., Hildreth, Richard G., Rose, Robert E., Skillman, Skillman, Oregon State University. Marine Resource Management Program, University of Oregon. Ocean and Law Center, and Oregon. Dept. of Land Conservation and Development
Resource Type:: Technical Report
Full Text:: . Hildreth Associate Investigators Robert E. Rose Gregory Skillman June 30, 1987 This study was supported

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