|2003 Seattle Annual Meeting (November 2–5, 2003)|
|Paper No. 116-10|
|Presentation Time: 1:30 PM-5:30 PM|
MERCURY DEPOSITION IN A TIDAL MARSH DOWNSTREAM OF THE HISTORIC NEW ALMADEN MINING DISTRICT, CALIFORNIA
CONAWAY, C.H., Department of Environmental Toxicology, Univ of California Santa Cruz, 1156 High Street, Santa Cruz, CA 95064, firstname.lastname@example.org, WATSON, E.B., Department of Geography, Univ of California Berkeley, 507 McCone Hall, Berkeley, CA 94720, FLANDERS, J.R., Environmental Toxicology, Univ of California Santa Cruz, 1156 High Street, Santa Cruz, CA 95064, and FLEGAL, A.R.|
A record of mercury deposition was provided by sediment recovered from piston cores of a south San Francisco Bay tidal marsh that is 30-km downstream of the New Almaden mining district, formerly the largest mercury mining district in North America. Pre-mining sediment mercury concentrations were 80±30 ng/g, which are similar to pre-mining concentrations in cores taken from other parts of San Francisco Estuary. Concentrations in the core increase to a maximum of about 1200 ng/g, corresponding to a period in the mid-20th century, nearly 50 years after the peak in mercury production at the mines. The extent of contamination from upstream mining activity appears to reflect the amount of processed ore disposed of at the surface, and also periods when mercury was recovered from reworking these surface ore dumps and open cuts. Transport of this contaminant mercury to the tidal marsh appears to be influenced by hydrologic modifications in the watershed, including dam building and subsidence related to groundwater withdrawal. Although San Francisco Estuary is contaminated with mercury from numerous historic mining sources, including late 19th century hydraulic gold mining in the Sierra Nevada, there is little evidence of pre-mining contamination from natural mercury sources in the southern reach of San Francisco Estuary.
2003 Seattle Annual Meeting (November 2–5, 2003)
|Session No. 116--Booth# 46|
Environmental Geoscience (Posters) II
Washington State Convention and Trade Center: Hall 4-F
1:30 PM-5:30 PM, Monday, November 3, 2003
Geological Society of America Abstracts with Programs, Vol. 35, No. 6, September 2003, p. 238
© Copyright 2003 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.