by U.S. Dept. of the Interior, U.S. Geological Survey, U.S. Geological Survey, Branch of Information Services [distributor] in Troy, N.Y, Denver, CO .
Written in English
Includes bibliographical references (p. 13-14).
|Statement||by Peter S. Murdoch and Charles R. Barnes.|
|Series||U.S. Geological Survey open-file report ;, 96-221|
|Contributions||Barnes, Charles R., Geological Survey (U.S.)|
|LC Classifications||TD427.A27 M87 1996|
|The Physical Object|
|Pagination||iv, 14 p. :|
|Number of Pages||14|
|LC Control Number||97158953|
and recent monitoring of stream chemistry in the Catskill Mountains of New York indicate, however, that nitric acid has a significant and increasing role in surface water acidification that. Excerpt from Notes on the Mammals of the Catskill Mountains, New York, With General Remarks on the Fauna and Flora of the Region Owing to the character of the geological formation, there are but few shells in the Catskills. The following list includes all of the species which we found by: 3. The watersheds included in this study were the Neversink and Rondout reservoir watersheds located in the southeastern portion of the Catskill Mountains in southeastern New York area of the Catskill Mountains is particularly vulnerable to the effects of acid deposition because it is characterized by thin soils overlying sedimentary bedrock composed of shale, siltstone, sandstone and Cited by: Results from both long‐term (up to 70 years) and recent monitoring of stream chemistry in the Catskill Mountains of New York indicate, however, that nitric acid has a significant and increasing role in surface water acidification that, during high‐flow periods, rivals the role of sulfuric by:
Catskill Streams provide billion gallons of clean drinking water each day to over nine million residents in New York City and some smaller municipalities (nearly half the population of New York State). Catskill Mountains, dissected segment of the Allegheny Plateau, part of the Appalachian Mountain system, lying mainly in Greene and Ulster counties, southeastern New York, U.S. Bounded north and east by the valleys of the Mohawk and Hudson rivers, respectively, the mountains are drained by headstreams of the Delaware River and by numerous small creeks. Results from both long-term (up to 70 years) and recent monitoring of stream chemistry in the Catskill Mountains of New York indicate, however, that nitric acid has a significant and increasing. Work Plan of the Neversink Watershed Study in the Catskill Mountains of Southeastern New York By Gregory B. Lawrence, Douglas A. Burns, Peter S. Murdoch, Barry Baldigo, and Yvonne H. Baevsky Prepared in cooperation with the New York City Department of Environmental Protection U.S. Geological Survey Open-File Report Cited by: 7.
Catskill Fly Fishing Center & Museum Stream Ecology site > National Ground Water Association > Center for Watershed Protection > Wetlands in the Watersheds of the New York City Water Supply System > WATERSHED The Surfrider Foundation shares an animated overview of how a watershed works. Published in August , this book is the result of more than 40 years of research on the Catskill forest. It includes 25 maps showing the distribution of species and forest-products industries in addition to a full-color, large, fold-out map that shows the extent of the first growth forest, second and third growth forest, agricultural lands, burned areas, reforested areas, and landslides.5/5(4). Discharge to concentration relationships for eight streams studied by the U.S. Geological Survey (USGS) as part of the U.S. Environmental Protection Agency's (U.S. EPA) Long-Term Monitoring Project (–89) indicate acidification of some streams by H2SO4 and HNO3 in atmospheric deposition and by organic acids in soils. Concentrations of major ions in precipitation were similar to those Cited by: Restoring Geomorphic Stability and Biodiversity in Streams of the Catskill Mountains, New York, USA Abstract.—Many stream and river channels in North America have been straightened, widened, and hardened to stabilize channel banks and beds, but these efforts have typically.