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,{"id":957,"text":"wsp2372 - 1991 - Method for estimating low-flow characteristics of ungaged streams in Indiana","interactions":[{"subject":{"id":12474,"text":"ofr86323 - 1986 - Method for estimating low-flow characteristics of ungaged streams in Indiana","indexId":"ofr86323","publicationYear":"1986","noYear":false,"title":"Method for estimating low-flow characteristics of ungaged streams in Indiana"},"predicate":"SUPERSEDED_BY","object":{"id":957,"text":"wsp2372 - 1991 - Method for estimating low-flow characteristics of ungaged streams in Indiana","indexId":"wsp2372","publicationYear":"1991","noYear":false,"title":"Method for estimating low-flow characteristics of ungaged streams in Indiana"},"id":1}],"lastModifiedDate":"2024-01-09T21:54:06.600443","indexId":"wsp2372","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2372","title":"Method for estimating low-flow characteristics of ungaged streams in Indiana","docAbstract":"<p>Equations for estimating the 7-day, 2-year and 7oday, 10-year low flows at sites on ungaged streams are presented. Regression analysis was used to develop equations relating basin characteristics and low-flow characteristics at 82 gaging stations. Significant basin characteristics in the equations are contributing drainage area and flow-duration ratio, which is the 20-percent flow duration divided by the 90-percent flow duration. Flow-duration ratio has been regionalized for Indiana on a plate. Ratios for use in the equations are obtained from the plate. Drainage areas are determined from maps or are obtained from reports. The predictive capability of the method was determined by tests of the equations and of the flow-duration ratios on the plate. The accuracy of the equations alone was tested by estimating the low-flow characteristics at 82 gaging stations where flow-duration ratio is already known. In this case, the standard errors of estimate for 7-day, 2-year and 7-day, 10-year low flows are 19 and 28 percent. When flow-duration ratios for the 82 gaging stations are obtained from the map, the standard errors are 46 and 61 percent. However, when stations having drainage areas of less than 10 square miles are excluded from the test, the standard errors decrease to 38 and 49 percent. Standard errors increase when stations with small basins are included, probably because some of the flow-duration ratios obtained for these small basins are incorrect. Local geology and its effect on the ratio are not adequately reflected on the plate, which shows the regional variation in flow-duration ratio. In all the tests, no bias is apparent areally, with increasing drainage area or with increasing ratio. Guidelines and limitations should be considered when using the method. The method can be applied only at sites in the northern and central physiographic zones of the State. Low-flow characteristics cannot be estimated for regulated streams unless the amount of regulation is known so that the estimated low-flow characteristic can be adjusted. The method is most accurate for sites having drainage areas ranging from 10 to 1,000 square miles and for predictions of 7-day, 10-year low flows ranging from 0.5 to 340 cubic feet per second.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2372","collaboration":"Indiana State Board of Health","usgsCitation":"Arihood, L.D., and Glatfelter, D.R., 1991, Method for estimating low-flow characteristics of ungaged streams in Indiana: U.S. Geological Survey Water Supply Paper 2372, Report: iv, 18 p.; 1 Plate: 17.50 x 29.00 inches, https://doi.org/10.3133/wsp2372.","productDescription":"Report: iv, 18 p.; 1 Plate: 17.50 x 29.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":424241,"rank":4,"type":{"id":36,"text":"NGMDB Index 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,{"id":2449,"text":"wsp2346 - 1991 - Geohydrology and ground-water resources of Philadelphia, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-20T09:51:18","indexId":"wsp2346","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2346","title":"Geohydrology and ground-water resources of Philadelphia, Pennsylvania","docAbstract":"The aquifers underlying the 134.6-square-mile city of Philadelphia are divided by the Fall Line into the unconsolidated aquifers (chiefly sand and gravel) of the Coastal Plain and the consolidated-rock aquifers (chiefly schist of the Wissahickon Formation) of the Piedmont. Ground water is present under confined and unconfined conditions. The principal units of the confined-aquifer system are the lower and middle sands of the Potomac-Raritan-Magothy aquifer system. The lower sand unit is the most productive aquifer in Philadelphia. The median yield of wells screened in the lower sand unit is 275 gal/min (gallons per minute), and yields of some wells are as high as 1,350 gal/min. The median specific capacity is 16 (gal/min)/ft (gallons per minute per foot of drawdown). The principal units of the unconsolidated unconfined-aquifer system are the upper sand unit of the Potomac-Raritan-Magothy aquifer system and the informally named Trenton gravel. The median yield of wells tapping these two undifferentiated units is 90 gal/min, and yields of some wells are as high as 1,370 gal/min. The median specific capacity is 12 (gal/min)/ft. The consolidated unconfined-aquifer system consists mainly of the Wissahickon Formation. The median yield of nondomestic wells that tap the Wissahickon Formation is 45 gal/min, and yields are as high as 350 gal/min. The median specific capacity is 0.5 (gal/min)/ft. \r\n\r\nUrbanization has considerably modified the hydrologic cycle in Philadelphia. Impervious surfaces have reduced recharge areas and evapotranspiration and have increased direct runoff. Leakage from the water-distribution system, which is supplied from the Delaware and Schuylkill Rivers, was about 60 to 72 Mgal/d (million gallons per day) in 1980. Groundwater infiltration to sewers is estimated to be as much as 135 Mgal/d when the water table is high. The potentiometric surface of the lower sand unit has been lowered substantially by pumping. By 1954, cones of depression were more than 50 ft (feet) below sea level at the U.S. Naval Base and more than 70 ft below sea level along the Delaware River northeast of the naval base. As a result of withdrawals, declining heads in the lower sand unit caused water to flow downward from the overlying unconsolidated deposits and the water table to decline below sea level along the Delaware River. Beginning in the mid1960's, ground-water withdrawals from the lower sand unit decreased, and, by 1979, water levels had risen 25 ft at the U.S. Naval Base and 45 ft farther north along the Delaware River. As of 1985, water levels in the lower sand unit were controlled largely by pumping in nearby parts of New Jersey. \r\n\r\nUrbanization also has caused substantial degradation of the quality of ground water in Philadelphia. By 1945, the quality of water in the unconfined aquifer system began to deteriorate as contaminants present at the land surface migrated down- ward. Withdrawal of water from the deeper confined aquifers caused a head decline that resulted in downward movement of contaminated water from the overlying unconfined aquifer system. Consequently, water in the confined aquifers deteriorated progressively in chemical quality so it resembles water in the unconfined aquifer system. \r\n\r\nThe concentration of dissolved solids in water samples collected during 1979-80 ranged from 90 to 4,480 mg/L (milligrams per liter). The average concentration of 778 mg/L was 45 percent higher than that of samples collected during 1945-58. Water from the unconfined unconsolidated aquifers generally had the highest dissolved-solids concentration. The concentration of dissolved iron in water samples collected during 197980 ranged from 0 to 220 mg/L and exceeded 0.30 mg/L in 71 percent of the samples. The average concentration of 17 mg/L was nearly 30 percent higher than that of samples collected during 1945-58. Many wells have been abandoned because of elevated iron concentrations. The concentration of dissolved manganese in water ","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp2346","usgsCitation":"Paulachok, G.N., 1991, Geohydrology and ground-water resources of Philadelphia, Pennsylvania: U.S. Geological Survey Water Supply Paper 2346, vii, 79 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wsp2346.","productDescription":"vii, 79 p. :ill., maps (some col.) ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":138129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2346/report-thumb.jpg"},{"id":28524,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2346/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d1f","contributors":{"authors":[{"text":"Paulachok, Gary N. gnpaulac@usgs.gov","contributorId":3500,"corporation":false,"usgs":true,"family":"Paulachok","given":"Gary","email":"gnpaulac@usgs.gov","middleInitial":"N.","affiliations":[],"preferred":true,"id":145222,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40257,"text":"ofr91640 - 1991 - Complete Bouguer gravity map of the Bagdad 0.5° x 1° quadrangle, Arizona","interactions":[],"lastModifiedDate":"2021-11-19T20:16:39.015064","indexId":"ofr91640","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-640","title":"Complete Bouguer gravity map of the Bagdad 0.5° x 1° quadrangle, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr91640","usgsCitation":"Hendricks, J.D., Plescia, J.B., and Matic, A.K., 1991, Complete Bouguer gravity map of the Bagdad 0.5° x 1° quadrangle, Arizona: U.S. Geological Survey Open-File Report 91-640, 1 Plate: 44.86 × 27.42 inches, https://doi.org/10.3133/ofr91640.","productDescription":"1 Plate: 44.86 × 27.42 inches","costCenters":[],"links":[{"id":173212,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":71332,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1991/0640/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391945,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18186.htm"}],"country":"United States","state":"Arizona","otherGeospatial":"Bagdad 0.5° x 1° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114,\n              34.5\n            ],\n            [\n              -113,\n              34.5\n            ],\n            [\n              -113,\n              35\n            ],\n            [\n              -114,\n              35\n            ],\n            [\n              -114,\n              34.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a83dd","contributors":{"authors":[{"text":"Hendricks, J. D.","contributorId":40187,"corporation":false,"usgs":true,"family":"Hendricks","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":223189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plescia, J. B.","contributorId":15689,"corporation":false,"usgs":true,"family":"Plescia","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":223188,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Matic, A. K.","contributorId":64319,"corporation":false,"usgs":true,"family":"Matic","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":223190,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17358,"text":"ofr91589 - 1991 - Mineral resource studies of national forest roadless areas in Idaho","interactions":[],"lastModifiedDate":"2024-12-17T21:23:18.377494","indexId":"ofr91589","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-589","title":"Mineral resource studies of national forest roadless areas in Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr91589","usgsCitation":"Johnson, K.M., and Worl, R., 1991, Mineral resource studies of national forest roadless areas in Idaho: U.S. Geological Survey Open-File Report 91-589, iii, 84 p., 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,{"id":58780,"text":"mf2182 - 1991 - Reconnaissance photogeologic map of young faults in the Las Vegas 1 degree by 2 degrees quadrangle, Nevada, California, and Arizona","interactions":[],"lastModifiedDate":"2025-06-04T20:00:30.317911","indexId":"mf2182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"2182","title":"Reconnaissance photogeologic map of young faults in the Las Vegas 1 degree by 2 degrees quadrangle, Nevada, California, and Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2182","usgsCitation":"Dohrenwend, J.C., Menges, C., Schell, B.A., and Moring, B.C., 1991, Reconnaissance photogeologic map of young faults in the Las Vegas 1 degree by 2 degrees quadrangle, Nevada, California, and Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 2182, 1 Plate: 36.42 x 28.47 inches, https://doi.org/10.3133/mf2182.","productDescription":"1 Plate: 36.42 x 28.47 inches","costCenters":[],"links":[{"id":489659,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5811.htm","linkFileType":{"id":5,"text":"html"}},{"id":182427,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/2182/report-thumb.jpg"},{"id":282150,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2182/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Arizona, California, Nevada","otherGeospatial":"Las Vegas 1 degree by 2 degrees quadrangle,","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116,36 ], [ -116,37 ], [ -114,37 ], [ -114,36 ], [ -116,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636871","contributors":{"authors":[{"text":"Dohrenwend, J. C.","contributorId":40960,"corporation":false,"usgs":true,"family":"Dohrenwend","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":260773,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Menges, C.M.","contributorId":71200,"corporation":false,"usgs":false,"family":"Menges","given":"C.M.","affiliations":[],"preferred":false,"id":260774,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schell, B. A.","contributorId":77151,"corporation":false,"usgs":true,"family":"Schell","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":260775,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moring, B. C.","contributorId":91462,"corporation":false,"usgs":true,"family":"Moring","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":260776,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":16823,"text":"ofr91271 - 1991 - Analytical results and sample locality map of stream-sediment and panned-concentrate samples from the Garberville 1:100,000 quadrangle, (southwest quarter of the Redding, California 1:250,000 quadrangle) Humboldt, Trinity, Shasta, Tehama, and Mendocino Counties, California","interactions":[],"lastModifiedDate":"2022-07-08T21:45:49.715037","indexId":"ofr91271","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-271","title":"Analytical results and sample locality map of stream-sediment and panned-concentrate samples from the Garberville 1:100,000 quadrangle, (southwest quarter of the Redding, California 1:250,000 quadrangle) Humboldt, Trinity, Shasta, Tehama, and Mendocino Counties, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr91271","usgsCitation":"Smith, S.M., Silberman, M., O’Leary, R.M., and Hopkins, R.T., 1991, Analytical results and sample locality map of stream-sediment and panned-concentrate samples from the Garberville 1:100,000 quadrangle, (southwest quarter of the Redding, California 1:250,000 quadrangle) Humboldt, Trinity, Shasta, Tehama, and Mendocino Counties, California: U.S. Geological Survey Open-File Report 91-271, Report: 86 p.; 1 Plate: 35.85 × 26.57 inches, https://doi.org/10.3133/ofr91271.","productDescription":"Report: 86 p.; 1 Plate: 35.85 × 26.57 inches","costCenters":[],"links":[{"id":403330,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18101.htm","linkFileType":{"id":5,"text":"html"}},{"id":45900,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0271/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45899,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1991/0271/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149599,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0271/report-thumb.jpg"}],"country":"United States","state":"California","county":"Humboldt County, Mendocino County, Shasta County, Tehama County, Trinity County","otherGeospatial":"Garberville quadrangle, Redding quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124,\n              40\n            ],\n            [\n              -123,\n              40\n            ],\n            [\n              -123,\n              40.5\n            ],\n            [\n              -124,\n              40.5\n            ],\n            [\n              -124,\n              40\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4814e4b07f02db4dac38","contributors":{"authors":[{"text":"Smith, S. M.","contributorId":27859,"corporation":false,"usgs":true,"family":"Smith","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":173764,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silberman, M.L.","contributorId":10013,"corporation":false,"usgs":true,"family":"Silberman","given":"M.L.","affiliations":[],"preferred":false,"id":173763,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Leary, R. M.","contributorId":44894,"corporation":false,"usgs":true,"family":"O’Leary","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":173765,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hopkins, R. T. Jr.","contributorId":70743,"corporation":false,"usgs":true,"family":"Hopkins","given":"R.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":173766,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":16805,"text":"ofr91380B - 1991 - Analytical results and sample locality map of moss, moss-sediment, and willow samples from the Iditarod Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:18","indexId":"ofr91380B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-380","chapter":"B","title":"Analytical results and sample locality map of moss, moss-sediment, and willow samples from the Iditarod Quadrangle, Alaska","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr91380B","usgsCitation":"Arbogast, B., Erickson, B., Gray, J.E., and McNeal, J., 1991, Analytical results and sample locality map of moss, moss-sediment, and willow samples from the Iditarod Quadrangle, Alaska: U.S. Geological Survey Open-File Report 91-380, 1 computer disk ;5 1/4 in., https://doi.org/10.3133/ofr91380B.","productDescription":"1 computer disk ;5 1/4 in.","costCenters":[],"links":[{"id":150550,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e4db","contributors":{"authors":[{"text":"Arbogast, B. F.","contributorId":60623,"corporation":false,"usgs":true,"family":"Arbogast","given":"B. F.","affiliations":[],"preferred":false,"id":173684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, B.M.","contributorId":53389,"corporation":false,"usgs":true,"family":"Erickson","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":173683,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gray, J. E.","contributorId":49363,"corporation":false,"usgs":true,"family":"Gray","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":173682,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McNeal, J.M.","contributorId":61817,"corporation":false,"usgs":true,"family":"McNeal","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":173685,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":58784,"text":"mf1060 - 1991 - Seismicity map of the state of Georgia","interactions":[],"lastModifiedDate":"2017-05-10T11:15:44","indexId":"mf1060","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"1060","title":"Seismicity map of the state of Georgia","docAbstract":"<p>This map is one of a series of seismicity maps produced by the U.S. Geological Survey that show earthquake data of individual states or groups of states at the scale of 1:1,000,000. This maps shows only those earthquakes with epicenters located within the boundaries of Georgia, even though earthquakes in nearby states or countries may have been felt or may have cause damage in Georgia.</p><p> The data in table 1 were used to compile the seismicity map; these data are a corrected, expanded, and updated (through 1987) version of the data used by Algermissen (1969) for a study of seismic risk in the United States. The locations and intensities of some earthquakes were revised and intensities were assigned where none had been before. Many earthquakes were added to the original list from new data sources as well as from some old data sources that has not been previously used. The data in table 1 represent best estimates of the location of the epicenter, magnitude, and intensity of each earthquake on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed, but not all, especially for earthquakes that occurred before seismic instruments were universally used. </p><p>The latitude and longitude coordinates of each epicenter were rounded to the nearest tenth of a degree and sorted so that all identical locations were grouped and counted. These locations are represented on the map by a triangle. The number of earthquakes at each location is shown on the map by the Arabic number to the right of the triangle. A Roman numeral to the left of a triangle is the maximum Modified Mercoili intensity (Wood and Neumann, 1931) of all earthquakes at that geographic location, The absence of an intensity value indicates that no intensities have been assigned to earthquakes at that location. The year shown below each triangle is the latest year for which the maximum intensity was recorded.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1060","usgsCitation":"Reagor, B.G., Stover, C.W., Algermissen, S.T., and Long, L., 1991, Seismicity map of the state of Georgia (Revision - 1991): U.S. Geological Survey Miscellaneous Field Studies Map 1060, 36.03 X 28.23 inches, https://doi.org/10.3133/mf1060.","productDescription":"36.03 X 28.23 inches","costCenters":[],"links":[{"id":183328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1060/report-thumb.jpg"},{"id":278826,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1060/plate-1.pdf","text":"Plate","size":"7.10 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"}],"scale":"1000000","country":"United 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,{"id":54697,"text":"wdrMN901 - 1991 - Water Resources Data, Minnesota, Water Year 1990. Volume 1. Great Lakes and Souris-Red-Rainy River Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:11:56","indexId":"wdrMN901","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MN-90-1","title":"Water Resources Data, Minnesota, Water Year 1990. Volume 1. Great Lakes and Souris-Red-Rainy River Basins","language":"ENGLISH","doi":"10.3133/wdrMN901","usgsCitation":"Gunard, K., Hess, J., Zirbel, J., and Cornelius, C., 1991, Water Resources Data, Minnesota, Water Year 1990. Volume 1. Great Lakes and Souris-Red-Rainy River Basins: U.S. Geological Survey Water Data Report MN-90-1, 140 p., https://doi.org/10.3133/wdrMN901.","productDescription":"140 p.","costCenters":[],"links":[{"id":180700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1990/mn-90-1/report-thumb.jpg"},{"id":87903,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1990/mn-90-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb601","contributors":{"authors":[{"text":"Gunard, K.T.","contributorId":103733,"corporation":false,"usgs":true,"family":"Gunard","given":"K.T.","affiliations":[],"preferred":false,"id":251226,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, J.H.","contributorId":100465,"corporation":false,"usgs":true,"family":"Hess","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":251225,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zirbel, J.L.","contributorId":70837,"corporation":false,"usgs":true,"family":"Zirbel","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":251224,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cornelius, C.E.","contributorId":106190,"corporation":false,"usgs":true,"family":"Cornelius","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":251227,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":54711,"text":"wdrMO901 - 1991 - Water resources data, Missouri, water year 1990","interactions":[],"lastModifiedDate":"2023-01-04T19:04:38.902976","indexId":"wdrMO901","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MO-90-1","title":"Water resources data, Missouri, water year 1990","docAbstract":"<p>The U.S. Geological Survey, in cooperation with local, State, and Federal agencies and organizations, obtains a large quantity of data pertaining to the water resources of Missouri each water year (October 1 to September 30). These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of Missouri. To make these data readily available to interested parties outside the U.S. Geological Survey, the data are published annually in this report series, entitled \"WATER RESOURCES DATA FOR MISSOURI.\" This volume contains records for water discharge at 107 gaging stations; stage and contents at 11 lakes and reservoirs; water level records for 58 ground-water monitoring wells; water quality at 43 sampling stations (including 2 lakes); and data for 13 crest-stage stations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMO901","collaboration":"Prepared in cooperation with the Missouri Department of Natural Resources, Division of Geology and Land Survey and Division of Environmental Quality; Missouri State Highway and Transportation Commission; and with other State and Federal agencies","usgsCitation":"Reed, H., Hatten, D., Perkins, T., Gray, G., and Davis, J.V., 1991, Water resources data, Missouri, water year 1990: U.S. Geological Survey Water Data Report 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Jr.","contributorId":43850,"corporation":false,"usgs":true,"family":"Gray","given":"G.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":251270,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Davis, Jerri V. jdavis@usgs.gov","contributorId":99149,"corporation":false,"usgs":true,"family":"Davis","given":"Jerri","email":"jdavis@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":false,"id":251272,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1698,"text":"wsp2376 - 1991 - Tidal-flow, circulation, and flushing changes caused by dredge and fill in Hillsborough Bay, Florida","interactions":[{"subject":{"id":19113,"text":"ofr8876 - 1991 - Tidal-flow, circulation, and flushing changes caused by dredge and fill in Hillsborough Bay, Florida","indexId":"ofr8876","publicationYear":"1991","noYear":false,"title":"Tidal-flow, circulation, and flushing changes caused by dredge and fill in Hillsborough Bay, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":1698,"text":"wsp2376 - 1991 - Tidal-flow, circulation, and flushing changes caused by dredge and fill in Hillsborough Bay, Florida","indexId":"wsp2376","publicationYear":"1991","noYear":false,"title":"Tidal-flow, circulation, and flushing changes caused by dredge and fill in Hillsborough Bay, Florida"},"id":1}],"lastModifiedDate":"2022-12-29T20:55:21.579955","indexId":"wsp2376","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2376","title":"Tidal-flow, circulation, and flushing changes caused by dredge and fill in Hillsborough Bay, Florida","docAbstract":"Hillsborough Bay, Florida, underwent extensive physical changes between 1880 and 1972 because of the construction of islands, channels, and shoreline fills. These changes resulted in a progressive reduction in the quantity of tidal water that enters and leaves the bay. Dredging and filling also changed the magnitude and direction of tidal flow in most of the bay. \r\n\r\nA two-dimensional, finite-difference hydrodynamic model was used to simulate flood, ebb, and residual water transport for physical conditions in Hillsborough Bay and the northeastern part of Middle Tampa Bay during 1880, 1972, and 1985. The calibrated and verified model was used to evaluate cumulative water-transport changes resulting from construction in the study area between 1880 and 1972. The model also was used to evaluate water-transport changes as a result of a major Federal dredging project completed in 1985. \r\n\r\nThe model indicates that transport changes resulting from the Federal dredging project are much less areally extensive than the corresponding transport changes resulting from construction between 1880 and 1972. Dredging-caused changes of more than 50 percent in flood and ebb water transport were computed to occur over only about 8 square miles of the 65-square-mile study area between 1972 and 1985. Model results indicate that construction between 1880 and 1972 caused changes of similar magnitude over about 23 square miles. Dredging-caused changes of more than 50 percent in residual water transport were computed to occur over only 17 square miles between 1972 and 1985. Between 1880 and 1972, changes of similar magnitude were computed to occur over an area of 45 square miles. \r\n\r\nModel results also reveal historical tide-induced circulation patterns. The patterns consist of a series of about 8 interconnected circulatory features in 1880 and as many as 15 in 1985. Dredging- and construction-caused changes in number, size, position, shape, and intensity of the circulatory features increase tide-induced circulation throughout the bay. Circulation patterns for 1880, 1972, and 1985 levels of development differ in many details, but all exhibit residual landward flow of water in the deep, central part of the bay and residual seaward flow in the shallows along the bay margins. This general residual flow pattern is confirmed by both computed transport of a hypothetical constituent and long-term salinity observations in Hillsborough Bay. The concept has been used to estimate the average time it takes a particle to move from the head to the mouth of the bay. The mean transit time was computed to be 58 days in 1880 and 29 days in 1972 and 1985. \r\n\r\nThis increase in circulation and decrease in transit time since 1880 is estimated to have caused an increase in average salinity of Hillsborough Bay of about 2 parts per thousand. Dredge and fill construction is concluded to have significantly increased circulation and flushing between 1880 and 1972. Little circulation or flushing change is attributed to dredging activity since 1972.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2376","usgsCitation":"Goodwin, C., 1991, Tidal-flow, circulation, and flushing changes caused by dredge and fill in Hillsborough Bay, Florida: U.S. Geological Survey Water Supply Paper 2376, vi, 49 p., https://doi.org/10.3133/wsp2376.","productDescription":"vi, 49 p.","costCenters":[],"links":[{"id":411192,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25263.htm","linkFileType":{"id":5,"text":"html"}},{"id":137052,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2376/report-thumb.jpg"},{"id":26779,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2376/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"Hillsborough Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.3886755773811,\n              27.953098360693957\n            ],\n            [\n              -82.49596993271051,\n              27.953098360693957\n            ],\n            [\n              -82.49596993271051,\n              27.782592090617385\n            ],\n            [\n              -82.3886755773811,\n              27.782592090617385\n            ],\n            [\n              -82.3886755773811,\n              27.953098360693957\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699bfa","contributors":{"authors":[{"text":"Goodwin, Carl R.","contributorId":76284,"corporation":false,"usgs":true,"family":"Goodwin","given":"Carl R.","affiliations":[],"preferred":false,"id":143984,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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