In 1970, the Chester County Water Resources Authority (Pennsylvania) and the U.S. Geological Survey (USGS) established a long-term water-quality network with the goal of assessing the quality of streams in the county and understanding stream changes in response to urbanization using benthic-macroinvertebrate data. This database represents one of the longest continuous water-quality data sets in the country. Benthic macroinvertebrates are aquatic insects, such as mayflies, caddisflies, riffle beetles, and midges, and other invertebrates that live on the stream bottom. Benthic macroinvertebrates are useful in evaluating stream quality because their habitat preference and low motility cause them to be affected directly by substances that enter the aquatic system. By evaluating the diversity and community structure of benthic-macroinvertebrate populations, a determination of stream quality can be made.
Between 1981 and 1997, the water-quality network consisted of 43 sites in 5 major basins in Chester County—Delaware, Schuylkill, Brandywine, Big Elk and Octoraro, and Red and White Clay. Benthicmacroinvertebrate, water-chemistry, and habitat data were collected each year in October or November during base-flow conditions. Using these data, Reif evaluates the overall water-quality condition of Chester County streams. This Fact Sheet summarizes the key findings from Reif for streams in the Red Clay and White Clay Creek Basins. These streams include East Branch Red Clay Creek (site 26), West Branch Red Clay Creek (site 27), East Branch White Clay Creek (site 28), the Middle Branch White Clay Creek (site 29), and West Branch White Clay Creek (site 30). This summary includes an analysis of stream conditions on the basis of benthic-macroinvertebrate samples and an analysis of trends in stream conditions for the 17-year study period.
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Pennsylvania Water Science Center
U.S. Geological Survey
215 Limekiln Road
New Cumberland, PA 17070
In 1970, the Chester County Water Resources Authority (Penn-sylvania) and the U.S. Geological Survey (USGS) established a long-term water-quality network with the goal of assessing the quality of streams in the county and understanding stream changes in response to urbanization using benthic-macroinvertebrate data. This database represents one of the longest continuous water-quality data sets in the country. Benthic macroinvertebrates are aquatic insects, such as mayflies, caddisflies, riffle beetles, and midges, and other invertebrates that live on the stream bottom. Benthic macroinvertebrates are useful in evaluating stream quality because their habitat preferences and low motility cause them to be affected directly by substances that enter the aquatic system. By evaluating the diversity and community structure of benthic-macroinvertebrate populations, a determination of stream quality can be made.
Between 1981 and 1997, the water-quality network consisted of 43 sites in 5 major basins in Chester County—Delaware, Schuylkill, Brandywine, Big Elk and Octoraro, and Red and White Clay. Benthic-macroinvertebrate, water-chemistry, and habitat data were collected each year in October or November during base-flow condition. Using these data, Reif evaluates the overall water-quality condition of Chester County streams. This Fact Sheet summarizes the key findings from Reif for streams in the Delaware River Basin. These streams include Darby Creek (site 17), Crum Creek (site 19), Ridley Creek (sites 20 and 21), East Branch Chester Creek (sites 22-24, and 51), and Goose Creek (site 25). This summary includes an analysis of stream conditions on the basis of benthic-macroinvertebrate samples and an analysis of trends in stream conditions for the 17-year study period.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs11602","collaboration":"Prepared in cooperation with the Chester County Water Resources Authority","usgsCitation":"Reif, A.G., 2002, Assessment of stream quality using biological indices at selected sites in the Delaware River basin, Chester County, Pennsylvania, 1981-97: U.S. Geological Survey Fact Sheet 116-02, 4 p., https://doi.org/10.3133/fs11602.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":120556,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0116/coverthb.jpg"},{"id":3745,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0116/fs20020116.pdf","text":"Report","size":"271 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 2002-0116"}],"contact":"Director, Pennsylvania Water Science Center
U.S. Geological Survey
215 Limekiln Road
New Cumberland, PA 17070
In 1970, the Chester County Water Resources Authority (Pennsylvania) and the U.S. Geological Survey (USGS) established a long-term water-quality network with the goal of assessing the quality of streams in the county and understanding stream changes in response to urbanization using benthic-macroinvertebrate data. This database represents one of the longest continuous water-quality data sets in the country. Benthic macroinvertebrates are aquatic insects, such as mayflies, caddisflies, riffle beetles, and midges, and other invertebrates that live on the stream bottom. Benthic macroinvertebrates are useful in evaluating stream quality because their habitat preferences and low motility cause them to be affected directly by substances that enter the aquatic system. By evaluating the diversity and community structure of benthic-macroinvertebrate populations, a determination of stream quality can be made.
Between 1981 and 1997, the network consisted of 43 sites in 5 major basins in Chester County—Delaware, Schuylkill, Brandywine, Big Elk and Octoraro, and Red and White Clay. Benthic-macroinvertebrate, water-chemistry, and habitat data were collected each year in October or November during base-flow conditions. Using these data, Reif evaluated the overall water-quality condition of Chester County streams. This Fact Sheet summarizes the key findings from Reif for streams in the Schuylkill River Basin. These streams include Pigeon Creek (site 10), Stony Run (site 6), French Creek (sites 12-16), Pickering Creek (sites 1-5), Little Valley Creek (site 49), and Valley Creek (site 50). This summary includes an analysis of stream conditions based on benthic-macroinvertebrate samples and an analysis of trends in stream conditions for the 17-year study period.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs11402","collaboration":"Prepared in cooperation with the Chester County Water Resources Authority","usgsCitation":"Reif, A.G., 2002, Assessment of stream quality using biological indices at selected sites in the Schuylkill River basin, Chester County, Pennsylvania, 1981-97: U.S. Geological Survey Fact Sheet 114-02, 4 p., https://doi.org/10.3133/fs11402.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":120554,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0114/coverthb.jpg"},{"id":3743,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0114/fs20020114.pdf","text":"Report","size":"264 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 2002-0114"}],"contact":"Director, Pennsylvania Water Science Center
U.S. Geological Survey
215 Limekiln Road
New Cumberland, PA 17070
This digital map database, compiled from previously published and unpublished data, and new mapping by the authors, represents the general distribution of bedrock and surficial deposits in the mapped area. Together with the accompanying text file (wsomf.ps, wsomf.pdf, wsomf.txt), it provides current information on the geologic structure and stratigraphy of the area covered. The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The scale of the source maps limits the spatial resolution (scale) of the database to 1:62,500 or smaller.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2402","usgsCitation":"Blake, M., Graymer, R., and Stamski, R., 2002, Geologic map and map database of western Sonoma, northernmost Marin, and southernmost Mendocino counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 2402, 45 p. and 1 sheet, https://doi.org/10.3133/mf2402.","productDescription":"45 p. and 1 sheet","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":187454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110357,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52762.htm","linkFileType":{"id":5,"text":"html"},"description":"52762"},{"id":6333,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2002/2402/","linkFileType":{"id":5,"text":"html"}}],"scale":"1","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.53416666666666,38.25 ], [ -123.53416666666666,38.85027777777778 ], [ -122.75,38.85027777777778 ], [ -122.75,38.25 ], [ -123.53416666666666,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4947","contributors":{"authors":[{"text":"Blake, M.C. 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W.","affiliations":[],"preferred":false,"id":280310,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stamski, R.E.","contributorId":81574,"corporation":false,"usgs":true,"family":"Stamski","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":280312,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":69392,"text":"mf2408 - 2002 - Surficial Geologic Map of the Hughes Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:25","indexId":"mf2408","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2408","title":"Surficial Geologic Map of the Hughes Quadrangle, Alaska","docAbstract":"This dataset represents surficial geologic mapping of the Hughes quadrangle, Alaska. It is used to create the mapsheet in MF-2408, which shows surficial deposits of the 1:250,000 scale Hughes quadrangle in north central Alaska.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/mf2408","usgsCitation":"Hamilton, T.D., 2002, Surficial Geologic Map of the Hughes Quadrangle, Alaska (Version 1.0): U.S. Geological Survey Miscellaneous Field Studies Map 2408, Map: 42 x 25 inches; Pamphlet; Digital Database; Metadata, https://doi.org/10.3133/mf2408.","productDescription":"Map: 42 x 25 inches; Pamphlet; Digital Database; Metadata","additionalOnlineFiles":"Y","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":110365,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_53758.htm","linkFileType":{"id":5,"text":"html"},"description":"53758"},{"id":187455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9543,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2002/2408/","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -156,66 ], [ -156,67 ], [ -153,67 ], [ -153,66 ], [ -156,66 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a45c","contributors":{"authors":[{"text":"Hamilton, Thomas D.","contributorId":91474,"corporation":false,"usgs":true,"family":"Hamilton","given":"Thomas","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":280313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44934,"text":"wri20024292 - 2002 - Estimates of median flows for streams on the Kansas surface water register","interactions":[{"subject":{"id":44934,"text":"wri20024292 - 2002 - Estimates of median flows for streams on the Kansas surface water register","indexId":"wri20024292","publicationYear":"2002","noYear":false,"displayTitle":"Estimates of Median Flows for Streams on the Kansas Surface Water Register","title":"Estimates of median flows for streams on the Kansas surface water register"},"predicate":"SUPERSEDED_BY","object":{"id":55232,"text":"sir20045032 - 2004 - Estimates of median flows for streams on the 1999 Kansas Surface Water Register","indexId":"sir20045032","publicationYear":"2004","noYear":false,"title":"Estimates of median flows for streams on the 1999 Kansas Surface Water Register"},"id":1}],"supersededBy":{"id":55232,"text":"sir20045032 - 2004 - Estimates of median flows for streams on the 1999 Kansas Surface Water Register","indexId":"sir20045032","publicationYear":"2004","noYear":false,"title":"Estimates of median flows for streams on the 1999 Kansas Surface Water Register"},"lastModifiedDate":"2019-05-28T10:09:50","indexId":"wri20024292","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4292","displayTitle":"Estimates of Median Flows for Streams on the Kansas Surface Water Register","title":"Estimates of median flows for streams on the Kansas surface water register","docAbstract":"The Kansas State Legislature, by enacting Kansas Statute KSA 82a-2001 et. seq., mandated the criteria for determining which Kansas stream segments would be subject to classification by the State. One criterion for the selection as a classified stream segment is based on the statistic of median flow being equal to or greater than 1 cubic foot per second. As specified by KSA 82a-2001 et. seq., median flows were determined from U.S. Geological Survey streamflow-gaging-station data by using the most-recent 10-years of gaged data (KSA) for each streamflow-gaging station. Median flows also were determined by using gaged data from the entire period of record (all-available hydrology, AAH).
Least-squares multiple regression techniques were used, along with Tobit analyses, to develop equations for estimating median flows for uncontrolled stream segments. The drainage area of the uncontrolled gaging stations used in the regression analyses ranged from 2.06 to 12,004 square miles. A logarithmic transformation of the data was needed to develop the best linear relation for computing median flows. In the regression analyses, the significant climatic and basin characteristics, in order of importance, were drainage area, mean annual precipitation, mean basin permeability, and mean basin slope. Tobit analyses of KSA data yielded a root mean square error of 0.285 logarithmic units, and the best equations using Tobit analyses of AAH data had a root mean square error of 0.247 logarithmic units.
These equations and an interpolation procedure were used to compute median flows for the uncontrolled stream segments on the Kansas Surface Water Register. Measured median flows from gaging stations were incorporated into the regression-estimated median flows along the stream segments where available. The segments that were uncontrolled were interpolated using gaged data weighted according to the drainage area and the bias between the regression-estimated and gaged flow information. On controlled reaches of Kansas streams, the median flow information was interpolated between gaging stations using only gaged data weighted by drainage area.
Of the 2,232 total stream segments on the Kansas Surface Water Register, 30 percent of the segments had an estimated median streamflow of less than 1 cubic foot per second when the KSA analysis was used. When the AAH analysis was used, 40 percent of the segments had an estimated median streamflow of less than 1 cubic foot per second.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri20024292","collaboration":"Prepared in cooperation with the Kansas Department of Health and Environment","usgsCitation":"Perry, C.A., Wolock, D.M., and Artman, J.C., 2002, Estimates of median flows for streams on the Kansas surface water register (Superseded by SIR 2004-5032): U.S. Geological Survey Water-Resources Investigations Report 2002-4292, vi, 107 p., https://doi.org/10.3133/wri20024292.","productDescription":"vi, 107 p.","numberOfPages":"114","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":360235,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4292/wrir20024292.pdf","text":"Report","size":"29.0 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRIR 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\"}}]}","edition":"Superseded by SIR 2004-5032","contact":"Director, Kansas Water Science Center
U.S. Geological Survey
1217 Biltmore Drive
Lawrence, KS 66049
The U.S. Geological Survey, U.S. Environmental Protection Agency, and Illinois Environmental Protection Agency began a study of the hydrogeology, flow system, and distribution of contaminants in the aquifers underlying Belvidere, Ill., and vicinity in 1992. As part of the study, the ancestral Troy Bedrock Valley, located about 1.5 miles west of Belvidere, was identified as an important part of the ground-water-flow system. In the deepest parts of the valley, the basal Glenwood confining unit may be absent; thick deposits of sand and gravel that infill part of the valley may directly overlie the sandstone St. Peter aquifer, a regionally important source of water for public supply. With few deep wells open to the St. Peter aquifer present in the valley to provide necessary geologic information, tritium and other water-chemistry data were collected from eight wells to possibly delineate areas where the confining unit may be absent; the data also provide baseline water-quality information for an area expecting changes in land use and increases in water withdrawal. Also as part of the study, particle-tracking analysis was done using an available flow model to (1) identify possible discharge locations of ground water and contaminants and (2) delineate areas contributing recharge to the Belvidere municipal wells.
This report presents and interprets water-chemistry data collected during December 2000 and presents results of particle-tracking analysis. Ground water in samples from two of four wells open to the St. Peter aquifer appears to have recharged after 1954, suggesting that the Glenwood confining unit may be absent near the wells. Other hydrogeologic and water-chemistry data, however, were inconclusive or contradictory. Concentrations of iron, manganese, and lead exceeded maximum contaminant levels in five or less samples, but materials associated with the water-distribution systems appear to contribute to the elevated concentrations above natural levels.
Particle-tracking analysis indicates that most ground-water flow beneath possible contaminant-source areas discharges from the glacial drift aquifer to the Kishwaukee River. Most of the source areas are in or near Belvidere and are within 1,500 feet of the river. The analysis also indicates the possibility that in parts of the study area, some ground water does not discharge to the river, but flows beneath the Kishwaukee River in the underlying carbonate Galena-Platteville aquifer. Ground water that discharges to the one municipal well open to the glacial drift aquifer is estimated to travel over 1 mile in less than 25 years. Simulated residence (travel) times of ground water from the base of the glacial drift aquifer to the six municipal wells open, in part, to the Galena-Platteville aquifer, are estimated at less than about 40 years. Because fractures in this aquifer are unaccounted for in the flow model, actual areas contributing recharge are likely larger and travel times faster than those simulated for most of the municipal wells. Tritium data indicate that, in general, travel times from the land surface to the deepest parts of the Galena-Platteville aquifer are less than 46 years. Methyl tertiary-butyl ether data indicate that travel times to the upper part of the aquifer may be less than 16 years. The water-quality-based estimates of travel time generally are consistent with the estimates from particle-tracking analysis.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri024062","collaboration":"Prepared in cooperation with the Illinois Environmental Protection Agency U.S. Environmental Protection Agency","usgsCitation":"Mills, P., Halford, K.J., and Cobb, R., 2002, Delineation of the Troy Bedrock Valley and particle-tracking analysis of ground-water flow underlying Belvidere, Illinois: U.S. Geological Survey Water-Resources Investigations Report 2002-4062, v, 46 p., https://doi.org/10.3133/wri024062.","productDescription":"v, 46 p.","costCenters":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"links":[{"id":5984,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4062/wrir02_4062.pdf","text":"Report","size":"4.43 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRIR 02–4062"},{"id":183897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4062/coverthb.jpg"}],"country":"United States","state":"Illinois","county":"Boone County","city":"Belvidere","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.9385,42.4984],[-88.7737,42.4958],[-88.7719,42.4957],[-88.7059,42.4972],[-88.705,42.4167],[-88.7041,42.329],[-88.7057,42.2418],[-88.7061,42.1564],[-88.8224,42.1557],[-88.94,42.1549],[-88.9406,42.2408],[-88.9405,42.3284],[-88.9392,42.4161],[-88.9385,42.4984]]]},\"properties\":{\"name\":\"Boone\",\"state\":\"IL\"}}]}","contact":"Director, Central Midwest Water Science Center
U.S. Geological Survey
405 North Goodwin
Urbana, IL 61801
Land subsidence associated with ground-water-level declines has been recognized as a potential problem in Coachella Valley, California. Since the early 1920s, ground water has been a major source of agricultural, municipal, and domestic supply in the valley. Pumping of ground water resulted in water-level declines as large as 15 meters (50 feet) through the late 1940s. In 1949, the importation of Colorado River water to the lower Coachella Valley began, resulting in a reduction in ground-water pumping and a recovery of water levels during the 1950s through the 1970s. Since the late 1970s, demand for water in the valley has exceeded deliveries of imported surface water, resulting in increased pumping and associated ground-water-level declines and, consequently, an increase in the potential for land subsidence caused by aquifer-system compaction.
The location, extent, and magnitude of the vertical land-surface changes in Coachella Valley between 1998 and 2000 were determined using Global Positioning System (GPS) and interferometric synthetic aperture radar (InSAR) methods. GPS measurements made at 15 geodetic monuments in the lower Coachella Valley indicate that -34 to +60 millimeters ± 45 millimeters (-0.11 to +0.20 foot ± 0.15 foot) of vertical change in the land surface occurred during the 2-year period. Changes at three of the monuments exceeded the maximum uncertainty of ± 45 millimeters (± 0.15 foot) at the 95-percent confidence level, which indicates that small amounts of uplift occurred at these monuments between October 1998 and August 2000. Water-level measurements made at wells near the three uplifted monuments during this 2-year period indicate that the water levels fluctuate seasonally; water-level measurements made at these wells in September 1998 and September 2000 indicate that the water levels rose slightly near two monuments and declined slightly near the third. The relation between the seasonally fluctuating, but fairly stable, water levels between September 1998 and September 2000 and the slight uplift at the monuments may indicate that the water levels are fluctuating in the elastic range of stress and that the preconsolidation stress of the aquifer system was not exceeded during the 2-year period.
Results of the InSAR measurements made between June 17, 1998, and October 4, 2000, indicate that land subsidence, ranging from about 40 to 80 millimeters (0.13 to 0.26 foot), occurred in three areas of the Coachella Valley; near Palm Desert, Indian Wells, and La Quinta. Measurements made between June 17, 1998, and June 2, 1999, indicate that about 15 millimeters (0.05 foot) occurred southeast of Lake Cahuilla. All the subsiding areas coincide with or are near areas where ground-water levels declined between 1998 and 2000; some water levels in 2000 were at the lowest levels in their recorded histories. The coincident areas of subsidence and declining water levels suggest that aquifer-system compaction may be causing subsidence. If the stresses imposed by the historically lowest water levels exceeded the preconsolidation stress, the aquifer-system compaction and associated land subsidence may be permanent. Although the localized character of the subsidence signals look typical of the type of subsidence characteristically caused by localized pumping, the subsidence also may be related to tectonic activity in the valley.
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Michelle 0000-0002-8180-382X micsneed@usgs.gov","orcid":"https://orcid.org/0000-0002-8180-382X","contributorId":155,"corporation":false,"usgs":true,"family":"Sneed","given":"Michelle","email":"micsneed@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222676,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stork, Sylvia V. 0000-0002-1994-5560 svstork@usgs.gov","orcid":"https://orcid.org/0000-0002-1994-5560","contributorId":5096,"corporation":false,"usgs":true,"family":"Stork","given":"Sylvia","email":"svstork@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":true,"id":222677,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ikehara, Marti E.","contributorId":53757,"corporation":false,"usgs":true,"family":"Ikehara","given":"Marti","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":222678,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":50495,"text":"ofr02202 - 2002 - The Central Kentucky Prototype; an object-oriented geologic map data model for the National Geologic Map Database","interactions":[],"lastModifiedDate":"2012-02-02T00:11:19","indexId":"ofr02202","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-202","title":"The Central Kentucky Prototype; an object-oriented geologic map data model for the National Geologic Map Database","language":"ENGLISH","doi":"10.3133/ofr02202","usgsCitation":"Soller, D.R., Brodaric, B., Hastings, J.T., Wahl, R., and Weisenfluh, G.A., 2002, The Central Kentucky Prototype; an object-oriented geologic map data model for the National Geologic Map Database: U.S. Geological Survey Open-File Report 2002-202, p. 38, illus. incl. 1 table, 21 refs, https://doi.org/10.3133/ofr02202.","productDescription":"p. 38, illus. incl. 1 table, 21 refs","costCenters":[],"links":[{"id":176061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4311,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-202/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad2e4b07f02db681ab7","contributors":{"authors":[{"text":"Soller, David R. 0000-0001-6177-8332 drsoller@usgs.gov","orcid":"https://orcid.org/0000-0001-6177-8332","contributorId":2700,"corporation":false,"usgs":true,"family":"Soller","given":"David","email":"drsoller@usgs.gov","middleInitial":"R.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true}],"preferred":true,"id":241603,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brodaric, Boyan","contributorId":80341,"corporation":false,"usgs":true,"family":"Brodaric","given":"Boyan","affiliations":[],"preferred":false,"id":241606,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hastings, Jordan T.","contributorId":6119,"corporation":false,"usgs":true,"family":"Hastings","given":"Jordan","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":241604,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wahl, Ron","contributorId":105791,"corporation":false,"usgs":true,"family":"Wahl","given":"Ron","email":"","affiliations":[],"preferred":false,"id":241607,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Weisenfluh, Gerald A.","contributorId":51832,"corporation":false,"usgs":true,"family":"Weisenfluh","given":"Gerald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":241605,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":47513,"text":"ofr2002300 - 2002 - Water-Resources Investigations in Wisconsin, 2002","interactions":[],"lastModifiedDate":"2015-10-15T13:53:40","indexId":"ofr2002300","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-300","title":"Water-Resources Investigations in Wisconsin, 2002","docAbstract":"The statewide average precipitation of 34.83 inches for the 2001 water year was 3.15 inches greater than the normal annual precipitation of 31.68 inches for water years 1961–90. Average precipitation values affecting streamflow conditions ranged from 92 percent in northeast Wisconsin to 122 percent in southwest Wisconsin with a statewide average of 110 percent (summary tables provided by Lyle Anderson and Ed Hopkins, State Climatology Office, University of Wisconsin, Madison, written commun., 2002).
\nThe year started out very dry with all regions of the state below 50% of the long-term October average. November precipitation, which was approximately normal, was followed by a December which had record-setting snowfall in most of southern Wisconsin and heavier than normal snowfall the rest of the state. This snowfall total was boosted by the colder than normal temperatures that increased the snowfall depth for water content. The state had the first emergency snow declaration since 1979 with 14 counties receiving aid for December snow clean-up (Wisconsin State Journal, Dec. 15, 2001). Statewide precipitation in January was close to normal. February precipitation was above normal in northwest, north central and all of southern Wisconsin. Elsewhere in the state precipitation was close to normal. In March all regions of the state were very dry with total precipitation below 50% of the long-term March average. In April, the northwest corner of the state had precipitation over three times normal, north central had more than double normal and west central also had precipitation significantly above normal. The rest of the state was also above normal. In May, precipitation in the southern and central parts of the state was about 160 percent of normal. From mid June to mid July there was a statewide dry spell, with most of the state receiving less than 1 inch of rain. August precipitation was close to normal for most of the state with some localized very heavy rains of over 11 inches in southwest and south central Wisconsin. In September, the southern part of the state was above normal, the northwest part of the state was below normal and the rest of the state was about normal.
\nRunoff for rivers in the state ranged from 67 percent of the average annual runoff (1964–2001) at the Kewaunee River site in the northeast part of the state to 160 percent of the average annual runoff (1944–2001) at the Eau Galle River at Spring Valley site in the west central part of the state. Departures of runoff in the 2001 water year as a percent of long-term average runoff in the state (determined using stations with drainage areas greater than 150 square miles and at least 20 years of record) are shown in figure 4.
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\"}}]}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4786e4b07f02db4851cb","contributors":{"authors":[{"text":"Hueschen, K. A. (compiler)","contributorId":54068,"corporation":false,"usgs":true,"family":"Hueschen","given":"K.","suffix":"(compiler)","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":235599,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, S.Z.","contributorId":73875,"corporation":false,"usgs":true,"family":"Jones","given":"S.Z.","email":"","affiliations":[],"preferred":false,"id":235600,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fuller, J. A.","contributorId":29838,"corporation":false,"usgs":true,"family":"Fuller","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":235598,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70178215,"text":"70178215 - 2002 - Contaminants without borders: A regional assessment of the Colorado River Delta ecosystem","interactions":[],"lastModifiedDate":"2019-07-23T10:45:48","indexId":"70178215","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"chapter":"111","title":"Contaminants without borders: A regional assessment of the Colorado River Delta ecosystem","docAbstract":"The Colorado River Delta Region (CRDR) is comprised of large agricultural areas in the U.S. (Imperial and Yuma districts) and Mexico (Mexicali and San Luis districts), the Salton Sea, and the Lower Colorado River from southern Arizona to the Gulf of California (Valdés-Casillas et al., 1998). Before agricultural development, the lower delta comprised large riparian and wetland areas (Sykes, 1937; Glenn et al., 1999). Currently, most water from the Colorado River below Imperial Dam is used for irrigation in California and Mexico, and only remnants of the former CRDR wetlands remain. However, the Cienega de Santa Clara and the Rio Hardy wetlands (Figure 111.1) provide important habitat for many resident and migratory birds, including endangered species such as the desert pupfish (scientific names are provided in Table 111.1) and the Yuma clapper rail (Abarca et al., 1993; Mellink et al., 1997). Detailed descriptions of the CRDR and its wetlands are provided elsewhere (Sykes, 1937; Glenn et al., 1995; 1999; Friederici, 1998; Valdés-Casillas et al., 1998).
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Managing for healthy ecosystems","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"CRC Press","isbn":"9781566706124","usgsCitation":"Mora, M.A., Garcia, J., de la Paz Carpio-Obeso, M., and King, K.A., 2002, Contaminants without borders: A regional assessment of the Colorado River Delta ecosystem, chap. 111 of Managing for healthy ecosystems, p. 1125-1134.","productDescription":"10 p.","startPage":"1125","endPage":"1134","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":330851,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":330850,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.crcpress.com/Managing-for-Healthy-Ecosystems/Rapport-Lasley-Rolston-Nielsen-Qualset-Damania/p/book/9781566706124"}],"country":"Mexico, United States","state":"California","otherGeospatial":"Colorado River Delta Region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.56494140625001,\n 31.203404950917395\n ],\n [\n -113.75244140624999,\n 31.203404950917395\n ],\n [\n -113.75244140624999,\n 33.293803558346596\n ],\n [\n -116.56494140625001,\n 33.293803558346596\n ],\n [\n -116.56494140625001,\n 31.203404950917395\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5821a0dee4b02f1a881de97c","contributors":{"authors":[{"text":"Mora, Miguel A. 0000-0002-8393-0216","orcid":"https://orcid.org/0000-0002-8393-0216","contributorId":46643,"corporation":false,"usgs":true,"family":"Mora","given":"Miguel","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":653296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garcia, Jaqueline","contributorId":176724,"corporation":false,"usgs":false,"family":"Garcia","given":"Jaqueline","email":"","affiliations":[],"preferred":false,"id":653297,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"de la Paz Carpio-Obeso, Maria","contributorId":176725,"corporation":false,"usgs":false,"family":"de la Paz Carpio-Obeso","given":"Maria","email":"","affiliations":[],"preferred":false,"id":653298,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"King, Kirke A.","contributorId":17727,"corporation":false,"usgs":true,"family":"King","given":"Kirke","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":653299,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":48855,"text":"ofr02440 - 2002 - Estimated use of water in South Dakota, 2000","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"ofr02440","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-440","title":"Estimated use of water in South Dakota, 2000","docAbstract":"During 2000, the total amount of water withdrawn from ground- and surface-water sources in South Dakota was about 528 Mgal/d (million gallons per day). Of this amount, about 222 Mgal/d, or 42 percent of the total, was from ground water. Surface-water withdrawals were about 306 Mgal/d, or 58 percent of the total.\r\n\r\nTotal withdrawals for six categories of offstream use in South Dakota during 2000 were compiled. The withdrawals include: 93.3 Mgal/d for public supply, 9.53 Mgal/d for self-supplied domestic, 5.12 Mgal/d for industrial, 372.7 Mgal/d for irrigation, 5.24 Mgal/d for thermoelectric power, and 42.0 Mgal/d for livestock.\r\n\r\nWater use for hydroelectric power was the only instream use compiled in this report. About 57,794 Mgal/d was used by the hydroelectric powerplants to generate about 6,151 gigawatt-hours of electricity during 2000.","language":"ENGLISH","doi":"10.3133/ofr02440","usgsCitation":"Amundson, F.D., 2002, Estimated use of water in South Dakota, 2000: U.S. Geological Survey Open-File Report 2002-440, iii, 17 p. : col. ill., col. map ; 28 cm., https://doi.org/10.3133/ofr02440.","productDescription":"iii, 17 p. : col. ill., col. map ; 28 cm.","costCenters":[],"links":[{"id":4075,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr02440","linkFileType":{"id":5,"text":"html"}},{"id":169927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a033","contributors":{"authors":[{"text":"Amundson, Franklin D.","contributorId":99206,"corporation":false,"usgs":true,"family":"Amundson","given":"Franklin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":238440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44697,"text":"fs11502 - 2002 - Assessment of stream quality using biological indices at selected sites in the Big Elk and Octoraro Creek basins, Chester County, Pennsylvania, 1981-97","interactions":[],"lastModifiedDate":"2018-02-09T12:44:53","indexId":"fs11502","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"115-02","title":"Assessment of stream quality using biological indices at selected sites in the Big Elk and Octoraro Creek basins, Chester County, Pennsylvania, 1981-97","docAbstract":"In 1970, the Chester County Water Resources Authority (Pennsylvania) and the U.S. Geological Survey (USGS) established a long-term water-quality network with the goal of assessing the quality of streams in the county and understanding stream changes in response to urbanization using benthic-macroinvertebrate data. This database represents one of the longest continuous water-quality data sets in the country. Benthic macroinvertebrates are aquatic insects, such as mayflies, caddisflies, riffle beetles, and midges, and other invertebrates that live on the stream bottom. Benthic macroin-vertebrates are useful in evaluating stream quality because their habitat preference and low motility cause them to be affected directly by substances that enter the aquatic system. By evaluating the diversity and community structure of benthic-macroinvertebrate populations, a determination of stream quality can be made.
Between 1981 and 1997, the water-quality network consisted of 43 sites in 5 major basins in Chester County—Delaware, Schuylkill, Brandywine, Big Elk and Octoraro, and Red and White Clay. Benthic-macroinvertebrate, water-chemistry, and habitat data were collected each year in October or November during base-flow conditions. Using these data, Reif evaluates the overall water-quality condition of Chester County streams. This Fact Sheet summarizes the key findings from Reif for streams in the Big Elk and Octoraro Creek Basins. These streams include East Branch Big Elk Creek (site 31), West Branch Big Elk Creek (site 32), East Branch Octoraro Creek (site 33) and Valley Creek (site 34). This summary includes an analysis of stream conditions based on benthic-macroinvertebrate samples and an analysis of trends in stream conditions for the 17-year study period.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs11502","collaboration":"Prepared in cooperation with the Chester County Water Resources Authority","usgsCitation":"Reif, A.G., 2002, Assessment of stream quality using biological indices at selected sites in the Big Elk and Octoraro Creek basins, Chester County, Pennsylvania, 1981-97: U.S. Geological Survey Fact Sheet 115-02, 4 p., https://doi.org/10.3133/fs11502.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":120555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0115/coverthb.jpg"},{"id":3744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0115/fs20020115.pdf","text":"Report","size":"232 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 2002-0115"}],"contact":"Director, Pennsylvania Water Science Center
U.S. Geological Survey
215 Limekiln Road
New Cumberland, PA 17070
In 1970, the Chester County Water Resources Authority (Pennsylvania) and the U.S. Geological Survey (USGS) established a longterm water-quality network with the goal of assessing the quality of streams in the county and understanding stream changes in response to urbanization using benthic-macroinvertebrate data. This database represents one of the longest continuous water-quality data sets in the country. Benthic macroinvertebrates are aquatic insects, such as mayflies, caddisflies, riffle beetles, and midges, and other invertebrates that live on the stream bottom. Benthic macroinvertebrates are useful in evaluating stream quality because their habitat preferences and low motility cause them to be affected directly by substances that enter the aquatic system. By evaluating the diversity and community structure of benthic-macroinvertebrate populations, a determination of stream quality can be made.
Between 1981 and 1997, the water-quality network consisted of 43 sites in 5 major basins in Chester County—Delaware, Schuylkill, Brandywine, Big Elk and Octoraro, and Red and White Clay. Benthicmacroinvertebrate, water-chemistry, and habitat data were collected each year in October or November during base-flow conditions. Using these data, Reif evaluated the overall water-quality condition of Chester County streams. This Fact Sheet summarizes the key findings from Reif for streams in the Brandywine Creek Basin. These streams include West Branch Brandywine Creek (sites 37 and 38), Buck Run (site 46), Doe Run (site 45), East Branch Brandywine Creek (sites 48, 42, 36, and 39), Indian Run (site 47), West Valley Creek (site 44), and Main Stem Brandywine Creek (site 40). This summary includes an analysis of stream conditions based on benthic-macroinvertebrate samples and an analysis of trends in stream conditions for the 17-year study period.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs11702","collaboration":"Prepared in cooperation with the Chester County Water Resources Authority","usgsCitation":"Reif, A.G., 2002, Assessment of stream quality using biological indices at selected sites in the Brandywine Creek basin, Chester County, Pennsylvania, 1981-97: U.S. Geological Survey Fact Sheet 117-02, 4 p., https://doi.org/10.3133/fs11702.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":3746,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0117/fs20020117.pdf","text":"Report","size":"291 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 2002-0117"},{"id":122027,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0117/coverthb.jpg"}],"contact":"Director, Pennsylvania Water Science Center
U.S. Geological Survey
215 Limekiln Road
New Cumberland, PA 17070
No abstract available.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0e2f","contributors":{"authors":[{"text":"Daniels, David L. 0000-0003-0599-8036 dave@usgs.gov","orcid":"https://orcid.org/0000-0003-0599-8036","contributorId":1792,"corporation":false,"usgs":true,"family":"Daniels","given":"David","email":"dave@usgs.gov","middleInitial":"L.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":241897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snyder, Stephen L. ssnyder@usgs.gov","contributorId":4753,"corporation":false,"usgs":true,"family":"Snyder","given":"Stephen","email":"ssnyder@usgs.gov","middleInitial":"L.","affiliations":[{"id":5068,"text":"Midwest Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":241898,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":69673,"text":"mf2405 - 2002 - Geologic map of the Santa Ana Pueblo quadrangle, Sandoval County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:22","indexId":"mf2405","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2405","title":"Geologic map of the Santa Ana Pueblo quadrangle, Sandoval County, New Mexico","docAbstract":"The Santa Ana Pueblo quadrangle is located in the northern part of the Albuquerque basin, which is the largest\r\n basin or graben within the Rio Grande rift. The quadrangle is underlain by poorly consolidated sedimentary\r\n rocks of the Santa Fe Group and is dominated by Santa Ana Mesa, a volcanic tableland underlain by basalt flows\r\n of the San Felipe volcanic field. The San Felipe volcanic field is the largest area of basaltic lavas exposed\r\n in the Albuquerque basin. The structural fabric of the quadrangle is dominated by dozens of generally north\r\n striking, east- and west-dipping normal faults associated with the Neogene Rio Grande rift.","language":"ENGLISH","doi":"10.3133/mf2405","usgsCitation":"Personius, S.F., 2002, Geologic map of the Santa Ana Pueblo quadrangle, Sandoval County, New Mexico (Online Version 1.1): U.S. Geological Survey Miscellaneous Field Studies Map 2405, 1 map : col. ; 58 x 48 cm., on sheet 84 x 117 cm., https://doi.org/10.3133/mf2405.","productDescription":"1 map : col. ; 58 x 48 cm., on sheet 84 x 117 cm.","costCenters":[],"links":[{"id":110374,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54137.htm","linkFileType":{"id":5,"text":"html"},"description":"54137"},{"id":188080,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6342,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2002/mf-2405/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.61749999999999,35.3675 ], [ -106.61749999999999,35.5 ], [ -106.5,35.5 ], [ -106.5,35.3675 ], [ -106.61749999999999,35.3675 ] ] ] } } ] }","edition":"Online Version 1.1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a127","contributors":{"authors":[{"text":"Personius, Stephen F. personius@usgs.gov","contributorId":1214,"corporation":false,"usgs":true,"family":"Personius","given":"Stephen","email":"personius@usgs.gov","middleInitial":"F.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":280863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70156308,"text":"70156308 - 2002 - Assimilation and retention of selenium and other trace elements from crustacean food by juvenile striped bass (Morone saxatilis)","interactions":[],"lastModifiedDate":"2016-07-26T15:32:00","indexId":"70156308","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Assimilation and retention of selenium and other trace elements from crustacean food by juvenile striped bass (Morone saxatilis)","docAbstract":"Estimates of the assimilation and retention of trace elements from food by fish are useful for linking toxicity with the biogeochemical cycling of these elements through aquatic food webs. Here we use pulse-chase radiotracer techniques to estimate the assimilation and retention of Se and four trace metals, Ag, Am, Zn, and Cd, by 43- and 88-d-old juvenile striped bass, Morone saxatilis, from crustacean food. Brine shrimp nauplii, Artemia franciscana, or adult copepods,Acartia tonsa, were fed radiolabeled diatoms and then fed to juvenile striped bass. Assimilation efficiencies (AEs ± SD) for 43-d-old fish were 18 ± 2%, 6 ± 1%, 23 ± 4%, 33 ± 3%, and 23 ± 2% for Ag, Am, Cd, Se, and Zn, respectively. For 88-d-old fish, the AEs were 28 ± 1%, 42 ± 5%, and 40 ± 5% for Cd, Se, and Zn, respectively. The higher AEs in the older fish may result from longer gut passage times for larger fish. The 44-d-old fish excreted 5 ± 0.8%, 4 ± 2.0%, 7 ± 0.3%, 9 ± 0.4%, and 1.3 ± 0.9% of the Ag, Am, Cd, Se, and Zn, respectively, they ingested from food per day, whereas the 88-d-old fish excreted 3 ± 1.0%, 8 ± 0.5%, and 3 ± 0.5% of the assimilated Cd, Se, and Zn per day, respectively. Predictions of steady state Se concentrations in juvenile striped bass tissues made using a biokinetic model and the measured AE and efflux rates ranged from 1.8 to 3.0 mg Se g-1dry wt for muscle tissue and 6.8 to 11.6 mg Se g-1 dry wt for gut tissue. These predictions agreed well with average values of 2.1 and 13 mg Se g-1 dry wt measured independently in North San Francisco Bay, where elevated Se concentrations are of concern. The model results imply that the planktonic food web, including juvenile striped bass, does not transfer Se as efficiently to top consumers as does the benthic food web.
","publisher":"American Society of Limnology and Oceanography","doi":"10.4319/lo.2002.47.3.0646","usgsCitation":"Baines, S.B., Fisher, N.S., and Stewart, A.R., 2002, Assimilation and retention of selenium and other trace elements from crustacean food by juvenile striped bass (Morone saxatilis): Limnology and Oceanography, v. 47, no. 3, p. 647-655, https://doi.org/10.4319/lo.2002.47.3.0646.","productDescription":"10 p.","startPage":"647","endPage":"655","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":478597,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.5090","text":"External Repository"},{"id":306944,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"3","noUsgsAuthors":false,"publicationDate":"2002-05-07","publicationStatus":"PW","scienceBaseUri":"55d5a8ade4b0518e3546a4b3","contributors":{"authors":[{"text":"Baines, Stephen B.","contributorId":146650,"corporation":false,"usgs":false,"family":"Baines","given":"Stephen","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":568626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, Nicholas S.","contributorId":75022,"corporation":false,"usgs":true,"family":"Fisher","given":"Nicholas","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":568627,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stewart, A. Robin 0000-0003-2918-546X arstewar@usgs.gov","orcid":"https://orcid.org/0000-0003-2918-546X","contributorId":1482,"corporation":false,"usgs":true,"family":"Stewart","given":"A.","email":"arstewar@usgs.gov","middleInitial":"Robin","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":40553,"text":"WMA - Office of the Chief Operating Officer","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true}],"preferred":true,"id":568628,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44564,"text":"wri024220 - 2002 - Potential effects of structural controls and street sweeping on stormwater loads to the lower Charles River, Massachusetts","interactions":[],"lastModifiedDate":"2023-01-05T21:38:12.204066","indexId":"wri024220","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4220","title":"Potential effects of structural controls and street sweeping on stormwater loads to the lower Charles River, Massachusetts","docAbstract":"The water quality of the lower Charles River is periodically impaired by combined sewer overflows (CSOs) and non-CSO stormwater runoff. This study examined the potential non-CSO load reductions of suspended solids, fecal coliform bacteria, total phosphorus, and total lead that could reasonably be achieved by implementation of stormwater best management practices, including both structural controls and systematic street sweeping. Structural controls were grouped by major physical or chemical process; these included infiltration-filtration (physical separation), biofiltration-bioretention (biological mechanisms), or detention-retention (physical settling). For each of these categories, upper and lower quartiles, median, and average removal efficiencies were compiled from three national databases of structural control performance. Removal efficiencies obtained indicated a wide range of performance. Removal was generally greatest for infiltration-filtration controls and suspended solids, and least for biofiltration-bioretention controls and fecal coliform bacteria.\r\n\r\nStreet sweeping has received renewed interest as a water-quality control practice because of reported improvements in sweeper technology and the recognition that opportunities for implementing structural controls are limited in highly urbanized areas. The Stormwater Management Model that was developed by the U.S. Geological Survey for the lower Charles River Watershed was modified to simulate the effects of street sweeping in a single-family land-use basin. Constituent buildup and washoff variable values were calibrated to observed annual and storm-event loads. Once calibrated, the street sweeping model was applied to various permutations of four sweeper efficiencies and six sweeping frequencies that ranged from every day to once every 30 days.\r\n\r\nReduction of constituent loads to the lower Charles River by the combined hypothetical practices of structural controls and street sweeping was estimated for a range of removal efficiencies because of their inherent variability and uncertainty. This range of efficiencies, with upper and lower estimates, provides reasonable bounds on the load that could be removed by the practices examined. The upper estimated load reduction from combined street sweeping and structural controls, as a percentage of the total non-CSO load entering the lower Charles River downstream of Watertown Dam, was 44 percent for suspended solids, 34 percent for total lead, 14 percent for total phosphorus, and 17 percent for fecal coliform bacteria. The lower estimated load reduction from combined street sweeping and structural controls from non-CSO sources downstream of Watertown Dam, was 14 percent for suspended solids, 11 percent for total lead, 4.9 percent for total phosphorus, and 7.5 percent for fecal coliform bacteria. Load reductions by these combined management practices can be a small as 1.4 percent for total phosphorus to about 4 percent for the other constituents if the total load above Watertown Dam is added to the load from below the dam. Although the reductions in stormwater loads to the lower Charles River from the control practices examined appear to be minor, these practices would likely provide water-quality benefits to portions of the river during those times that they are most impaired-during and immediately after storms. It should also be recognized that only direct measurements of changes in stormwater loads before and after implementation of control practices can provide definitive evidence of the beneficial effects of these practices on water-quality conditions in the lower Charles River.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024220","usgsCitation":"Zarriello, P.J., Breault, R., and Weiskel, P.K., 2002, Potential effects of structural controls and street sweeping on stormwater loads to the lower Charles River, Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 2002-4220, v, 42 p., https://doi.org/10.3133/wri024220.","productDescription":"v, 42 p.","costCenters":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":411454,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54163.htm","linkFileType":{"id":5,"text":"html"}},{"id":134974,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3780,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024220/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Massachusetts","otherGeospatial":"lower Charles River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -71.0667,\n 42.3861\n ],\n [\n -71.225,\n 42.3861\n ],\n [\n -71.225,\n 42.2667\n ],\n [\n -71.0667,\n 42.2667\n ],\n [\n -71.0667,\n 42.3861\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6838ff","contributors":{"authors":[{"text":"Zarriello, Phillip J. 0000-0001-9598-9904 pzarriel@usgs.gov","orcid":"https://orcid.org/0000-0001-9598-9904","contributorId":1868,"corporation":false,"usgs":true,"family":"Zarriello","given":"Phillip","email":"pzarriel@usgs.gov","middleInitial":"J.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breault, Robert F. 0000-0002-2517-407X rbreault@usgs.gov","orcid":"https://orcid.org/0000-0002-2517-407X","contributorId":2219,"corporation":false,"usgs":true,"family":"Breault","given":"Robert F.","email":"rbreault@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230005,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiskel, Peter K. pweiskel@usgs.gov","contributorId":1099,"corporation":false,"usgs":true,"family":"Weiskel","given":"Peter","email":"pweiskel@usgs.gov","middleInitial":"K.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230003,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":39953,"text":"wri024217 - 2002 - Streamflow in the Quinnipiac River Basin, Connecticut— Statistics and Trends, 1931–2000","interactions":[],"lastModifiedDate":"2021-10-22T18:28:14.785672","indexId":"wri024217","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4217","title":"Streamflow in the Quinnipiac River Basin, Connecticut— Statistics and Trends, 1931–2000","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024217","usgsCitation":"Ahearn, E.A., 2002, Streamflow in the Quinnipiac River Basin, Connecticut— Statistics and Trends, 1931–2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4217, 42 p., https://doi.org/10.3133/wri024217.","productDescription":"42 p.","costCenters":[],"links":[{"id":390833,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_53972.htm"},{"id":258679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4217/report-thumb.jpg"},{"id":258678,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4217/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Connecticut","otherGeospatial":"Quinnipac River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73,\n 41.2892\n ],\n [\n -72.7097,\n 41.2892\n ],\n [\n -72.7097,\n 41.6981\n ],\n [\n -73,\n 41.6981\n ],\n [\n -73,\n 41.2892\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4dc0","contributors":{"authors":[{"text":"Ahearn, Elizabeth A. 0000-0002-5633-2640 eaahearn@usgs.gov","orcid":"https://orcid.org/0000-0002-5633-2640","contributorId":194658,"corporation":false,"usgs":true,"family":"Ahearn","given":"Elizabeth","email":"eaahearn@usgs.gov","middleInitial":"A.","affiliations":[{"id":196,"text":"Connecticut Water Science Center","active":true,"usgs":true},{"id":377,"text":"Massachusetts-Rhode Island Water Science Center","active":false,"usgs":true}],"preferred":false,"id":222674,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}