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These publications showcase the significant science conducted in our Science Centers.

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Water resources data for New Hampshire and Vermont, water year 2002 Water resources data for New Hampshire and Vermont, water year 2002

The Water Resources Division of the U.S. Geological Survey, in cooperation with State agencies, obtains a large amount of data pertaining to the water resources of New Hampshire and Vermont each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the States. To make these data...
Authors
Richard G. Kiah, Chandlee Keirstead, Robert O. Brown, Gregory S. Hilgendorf

Introduction Introduction

No abstract available.
Authors
D. J. Hoffman, Barnett A. Rattner, G.A. Burton, J. Cairns

Coastal erosion and wetland change in Louisiana: selected USGS products Coastal erosion and wetland change in Louisiana: selected USGS products

This Digital Data Series (DDS) report is primarily a selection of USGS science products that were previously published as paper atlases and maps but are no longer available in their original form. We have made an attempt to preserve the paper atlases by having them scanned in an efficient compressed digital format that provides a print-on-demand as well as a programmed viewing capability...
Authors
S. Jeffress Williams, Jamey M. Reid, VeeAnn A. Cross, Christopher F. Polloni

Effects of ultraviolet radiation on toad early life stages Effects of ultraviolet radiation on toad early life stages

Background
Authors
E. E. Little, R.D. Calfee, D. L. Fabacher, C. Carey, V. S. Blazer, E.M. Middleton

Characterization of limestone reacted with acid-mine drainage in a pulsed limestone bed treatment system at the Friendship Hill National Historical Site, Pennsylvania, USA Characterization of limestone reacted with acid-mine drainage in a pulsed limestone bed treatment system at the Friendship Hill National Historical Site, Pennsylvania, USA

Armoring of limestone is a common cause of failure in limestone-based acid-mine drainage (AMD) treatment systems. Limestone is the least expensive material available for acid neutralization, but is not typically recommended for highly acidic, Fe-rich waters due to armoring with Fe(III) oxyhydroxide coatings. A new AMD treatment technology that uses CO2 in a pulsed limestone bed reactor...
Authors
Jane M. Hammarstrom, Philip Sibrell, Harvey E. Belkin

Wisconsin potential field grids, derivative maps, and tectonic interpretations Wisconsin potential field grids, derivative maps, and tectonic interpretations

No abstract available.
Authors
David L. Daniels, S. L. Snyder, D.W. Geister, C. P. Ervin, M.G. Mudrey, W.F. Cannon, Connie Dicken

Arsenic in midwestern glacial deposits — Occurrence and relation to selected hydrogeologic and geochemical factors Arsenic in midwestern glacial deposits — Occurrence and relation to selected hydrogeologic and geochemical factors

Ground-water-quality data collected as part of 12 U.S. Geological Survey National Water-Quality Assessment studies during 1996-2001 were analyzed to (1) document arsenic occurrence in four types of gla-cial deposits that occur in large areas of the Midwest, (2) identify hydrogeologic or geochemical factors asso-ciated with elevated arsenic concentrations, and (3) search for clues as to...
Authors
Mary Ann Thomas

Streamflow and water-quality characteristics of the Ottawa River and selected tributaries in Allen, Hardin, and Putnam counties, Ohio Streamflow and water-quality characteristics of the Ottawa River and selected tributaries in Allen, Hardin, and Putnam counties, Ohio

Streamflow and water-quality measurements were made on the Ottawa River and selected tributaries between 1999 to 2002. Ten sets of streamflow measurements were made at an index station on the Auglaize River at Fort Jennings (station 04186500) and at 19 other sites along the Ottawa River and selected tributaries. These data were collected to relate daily mean streamflow at the Auglaize...
Authors
Kimberly Shaffer

Historical trend in ice thickness on the Piscataquis River in central Maine. Historical trend in ice thickness on the Piscataquis River in central Maine.

We analyzed a long-term record of ice thickness on the Piscataquis River in central Maine to determine whether there were temporal trends that were associated with climate warming. Trends in ice thickness were compared and correlated with regional time series of winter air temperature, heating degree days (HDD) , date of river ice-out, seasonal center-of-volume date (SCVD) (date on which...
Authors
Thomas G. Huntington, Robert W. Dudley, Glenn A. Hodgkins

Streamer resistivity surveys in delmarva coastal bays Streamer resistivity surveys in delmarva coastal bays

No abstract available.
Authors
Frank T. Manheim, David E. Krantz, Donald S. Snyder, Brian Sturgis

Synimpact-postimpact transition inside Chesapeake Bay crater Synimpact-postimpact transition inside Chesapeake Bay crater

The transition from synimpact to postimpact sedimentation inside Chesapeake Bay impact crater began with accumulation of fallout debris, the final synimpact deposit. Evi dence of a synimpact fallout layer at this site comes from the presence of unusual, millimeter- scale, pyrite microstructures at the top of the Exmore crater-fill breccia. The porous geometry of the pyrite...
Authors
Claude (Wylie) Poag

New shoreline change data and analysis for the Massachusetts shore with emphasis on Cape Cod and the islands: Mid-1800s to 1994 New shoreline change data and analysis for the Massachusetts shore with emphasis on Cape Cod and the islands: Mid-1800s to 1994

That shorelines change, oftentimes dramatically in short periods of time, is an accepted fact for those who live along the shore. However, when two-thirds or approximately 512 miles of a state's ocean-facing shore exhibits a long-term erosional trend, in some locations eroding at an average annual rate of 12 feet per year, as is the case in Massachusetts, shoreline property owners...
Authors
James F. O’Connell, E. Robert Thieler, Courtney Schupp
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