Ice on rivers and lakes has many important influences on design and construction of structures, operation of shipping, flow and circulation, water quality, and other factors related to the use of the water resources. Human interest in understanding these influences has led to many programs of data collection, research, and investigations for a century or more. The body of literature reporting on these studies includes several thousand items in textbooks, proceedings, journals, and technical reports. By far, the largest part of the studies were in the United States, Canada, and the Soviet Union. For the sake of this bibliography, the literature can be classified as dealing with basic characteristics of ice; freezing and melting processes and their prediction and control on rivers, and on lakes; effects of river and lake ice on navigation, flow, and structures; and influences of ice on chemical, biological, and the thermal characteristics of water quality.
This bibliography cites about 750 publications dealing with ice. Literature prior to the mid 1960's is summarized in several earlier bibliographies, and therefore this paper concentrates mainly on work over the past decade or so, plus some background from a few earlier reports. The body of literature is large, and this bibliography is not exhaustive; it does provide, however, a representative cross section of the scope of recent work in the field.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1590","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532552,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27206,"text":"wri77137 - 1977 - Trophic conditions in Lake Winnisquam, New Hampshire","interactions":[],"lastModifiedDate":"2019-11-01T12:07:02","indexId":"wri77137","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-137","title":"Trophic conditions in Lake Winnisquam, New Hampshire","docAbstract":"Lake Winnisquam has received treated domestic sewage for approximately 50 years and since June 1961 has been treated with copper sulfate to control the growth of nuisance algae. The Laconia City secondary sewage-treatment plant was upgraded in 1975 to include phosphorus removal. Phosphorus was not removed effectively until early 1976, and, therefore, the 1976 data are considered baseline or pre-phosphorus removal with respect to anticipated changes in the trophic condition of the lake. Effluent from the Laconia State School primary-treatment plant was diverted to the Laconia City plant in October 1976. Dissolved oxygen concentrations showed marked differences between the two basins comprising Lake Winnisquam. Phytoplankton samples showed similarities by algal group for all stations but algal genera varied between the upper and lower basins. Total phosphorus concentrations in the epilimnion ranged from 0.01 to 0.10 milligram per liter, and accumulation of total phosphorus in the hypolimnion resulted in concentrations up to 0.59 milligrams per liter. Chemical states of nutrients varied among the stations corresponding to the degree of depletion of hypolimnetic dissolved oxygen. Dissolved oxygen profiles were used to illustrate zones of algal production, respiration, and bacterial decomposition. The rate of depletion of dissolved oxygen in the hypolimnion was linearly related to time. Because change in the rate of hypolimnetic dissolved oxygen depletion is more easily measured than change of nutrient load in the lake, it is suggested it be used as an indicator of the response of the lake to change in trophic condition.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd187","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533130,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29208,"text":"wri7790 - 1977 - Techniques for Estimating Flood-Depth Frequency Relations on Natural Streams in Georgia","interactions":[],"lastModifiedDate":"2017-01-24T08:01:19","indexId":"wri7790","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-90","title":"Techniques for Estimating Flood-Depth Frequency Relations on Natural Streams in Georgia","docAbstract":"Regional relations are defined for estimating the depth of floods having recurrence intervals of 10, 50, and 100 years on streams with natural flow in Georgia.\r\n\r\nMultiple-regression analysis of station data is used to define the relations between flood depths and frequency for streams draining from 1 to 1,000 square miles, and for 10 climatological and physical basin characteristics.\r\n\r\nThe analysis indicates that the drainage area of the basin is the most significant variable. Five regions having distinct flood-depth frequency characteristics are delineated.\r\n\r\nThe developed relations, expressed as equations and graphs, are considered usable for any site in Georgia where the drainage area is between 1 and 1,000 square miles, and the flow is natural; exceptions include streams that are urbanized, regulated, tide affected, channelized, or where manmade structures significantly affect peak stages.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wri7790","usgsCitation":"Price, M., 1977, Techniques for Estimating Flood-Depth Frequency Relations on Natural Streams in Georgia: U.S. Geological Survey Water-Resources Investigations Report 77-90, iii, 33 p., https://doi.org/10.3133/wri7790.","productDescription":"iii, 33 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":119788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_77_90.gif"},{"id":12592,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri77-90/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db686095","contributors":{"authors":[{"text":"Price, McGlone","contributorId":42964,"corporation":false,"usgs":true,"family":"Price","given":"McGlone","email":"","affiliations":[],"preferred":false,"id":201148,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28390,"text":"wri7748 - 1977 - Low-flow characteristics of Minnesota streams","interactions":[],"lastModifiedDate":"2018-03-12T13:24:24","indexId":"wri7748","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-48","title":"Low-flow characteristics of Minnesota streams","docAbstract":"Low-flow frequency data for 161 continuous-record gaging stations having eight or more complete years of record are presented for 1-, 7-, 14-, 30-, 60-, 90-, 120-, 183-, and 365-day low flows for frequencies ranging from once in 2 years to once in 100 years. In addition, 8,146 low-flow measurements at 1,515 sites are given. Included are measurements at 623 partial-record stations where correlations with nearby continuous-record gaging stations eventually will be completed, and at 892 miscellaneous-measurement sites where only a few measurements were made.
\nExamples are given for determining low-flow characteristics at partial-record stations and miscellaneous-measurement sites. Where the number of measurements are adequate to develop a relation line, they alone are related to concurrent daily flows at a continuous-record gaging station. Where the number of measurements are too few to define a relation with flows at nearby gaging stations, an equal-yield line can be helpful for estimating a relation line. The relation line may be used to transfer low-flow characteristics from a continuous-record gaging station to a site where only discharge measurements are available .
\nSpecific conductance of streams, where available, is listed with the discharge measurements at partial-record stations and miscellaneous-measurement sites. Observed conductivity values range from less than 50 micromhos per centimeter at 25° Celsius in the northeast to greater than 1,000 for parts of west-central Minnesota.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64862d","contributors":{"authors":[{"text":"Lindskov, K.L.","contributorId":91077,"corporation":false,"usgs":true,"family":"Lindskov","given":"K.L.","affiliations":[],"preferred":false,"id":199718,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7838,"text":"ofr77258 - 1977 - Aeromagnetic maps with geologic interpretations for the Tularosa Valley, south-central New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr77258","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-258","title":"Aeromagnetic maps with geologic interpretations for the Tularosa Valley, south-central New Mexico","docAbstract":"An aeromagnetic survey of the Tularosa Valley in south-central New Mexico has provided information on the igneous rocks that are buried beneath alluvium and colluvium. \r\n\r\nThe data, compiled as residual magnetic anomalies, are shown on twelve maps at a scale of 1:62,500. Measurements of magnetic properties of samples collected in the valley and adjacent highlands give a basis for identifying the anomaly-producing rocks. Precambrian rocks of the crystalline basement have weakly induced magnetizations and produce anomalies having low magnetic intensities and low magnetic gradients. Late Cretaceous and Cenozoic intrusive rocks have moderately to strongly induced magnetizations. \r\n\r\nPrecambrian rocks produce prominent magnetic anomalies having higher amplitudes and higher gradients. The Quaternary basalt has a strong remanent magnetization of normal polarity and produces narrow anomalies having high-magnetic gradients. Interpretations include an increase in elevation to the top of buried Precambrian rock in the northern part of the valley, a large Late Cretaceous and Cenozoic intrusive near Alamogordo, and a southern extension of the intrusive rock exposed in the Jarilla Mountains. Evidence for the southern extension comes from a quantitative analysis of the magnetic anomalies..","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77258","usgsCitation":"Bath, G.D., 1977, Aeromagnetic maps with geologic interpretations for the Tularosa Valley, south-central New Mexico: U.S. Geological Survey Open-File Report 77-258, ii, 16 p. :ill., 18 maps (12 fold. in 2 envelopes) ;27 cm., https://doi.org/10.3133/ofr77258.","productDescription":"ii, 16 p. :ill., 18 maps (12 fold. in 2 envelopes) ;27 cm.","costCenters":[],"links":[{"id":140550,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0258/report-thumb.jpg"},{"id":35351,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35352,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35353,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35354,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35355,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35356,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35357,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35358,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35359,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35360,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35361,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35362,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0258/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35363,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0258/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689e7d","contributors":{"authors":[{"text":"Bath, G. D.","contributorId":71968,"corporation":false,"usgs":true,"family":"Bath","given":"G.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":156704,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11636,"text":"ofr77402 - 1977 - Well records, water-level measurements, logs of test holes, and chemical analyses of ground water in the Cache River alluvial aquifer-stream system, northeast Arkansas, 1946-76","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr77402","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-402","title":"Well records, water-level measurements, logs of test holes, and chemical analyses of ground water in the Cache River alluvial aquifer-stream system, northeast Arkansas, 1946-76","docAbstract":"Most of the ground-water data for the Cache River alluvial aquifer-stream system in northeast Arkansas were collected between March 1973 and April 1976, but some were collected as early as April 1946. The data includes records of 363 wells and test holes, water-level measurements of 295 wells, logs of 32 test holes, and chemical analyses of water samples from 85 wells. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77402","usgsCitation":"Westerfield, P.W., 1977, Well records, water-level measurements, logs of test holes, and chemical analyses of ground water in the Cache River alluvial aquifer-stream system, northeast Arkansas, 1946-76: U.S. Geological Survey Open-File Report 77-402, iii, 166 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr77402.","productDescription":"iii, 166 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":144952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ace4b07f02db5c641e","contributors":{"authors":[{"text":"Westerfield, Paul W.","contributorId":30599,"corporation":false,"usgs":true,"family":"Westerfield","given":"Paul","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":163483,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56383,"text":"wdrFL763 - 1977 - Water resources data for Florida, water year 1976; Volume 3, southwest Florida","interactions":[],"lastModifiedDate":"2024-04-04T22:47:44.568825","indexId":"wdrFL763","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"FL-76-3","title":"Water resources data for Florida, water year 1976; Volume 3, southwest Florida","docAbstract":"Water resources data for the 1975 water year in southwest Florida consist of discharge records for 70 streams, stage-only records for 31 streams, elevations for 107 lakes, and daily water level measurements for 352 wells. Water quality data for approximately 220 surface sites and 700 wells are included; as are miscellaneous measurement and crest-stage partial records.
These data represent the National Water Daya System records collected by the U.S. Geological Survey and cooperating local, state and federal agencies in Florida.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL763","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Water resources data for Florida, water year 1976; Volume 3, southwest Florida: U.S. Geological Survey Water Data Report FL-76-3, xvii, 460 p., https://doi.org/10.3133/wdrFL763.","productDescription":"xvii, 460 p.","costCenters":[],"links":[{"id":185022,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1976/fl-76-3/report-thumb.jpg"},{"id":427476,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1976/fl-76-3/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"southwest Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.78457237569292,\n 29.029313869037665\n ],\n [\n -82.78457237569292,\n 26.872712576892866\n ],\n [\n -81.80582106070898,\n 26.872712576892866\n ],\n [\n -81.80582106070898,\n 29.029313869037665\n ],\n [\n -82.78457237569292,\n 29.029313869037665\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f730c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7594,"text":"ofr77585 - 1977 - Use of imaging in the 0.46-2.36 [micrometers] spectral region for alteration mapping in the Cuprite mining district, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"ofr77585","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-585","title":"Use of imaging in the 0.46-2.36 [micrometers] spectral region for alteration mapping in the Cuprite mining district, Nevada","docAbstract":"Color composites of Landsat MSS ratio images that display variations in the intensity of ferric-iron absorption bands are highly effective for mapping limonitic altered rocks, but ineffective for mapping nonlimonitic altered rocks. Analysis of 0.45-2.5 ?m field and laboratory spectra shows that iron-deficient opalites in the Cuprite mining district, Nevada, have an intense OH-absorption band near 2.2 ?m owing to their clay mineral and alunite contents and that this spectral feature is absent or weak in adjacent unaltered tuff and basalt. To evaluate the usefulness of this spectral feature for discriminating between altered and unaltered rocks, we generated color-ratio composite images from multispectral (0.46-2.36 ?m) aircraft data. The altered rocks in the district can be discriminated from unaltered rocks with few ambiguities; in addition, some effects of mineralogical zoning can be discriminated within the altered area. Only variations in amounts of limonite can be discerned in shorter wavelength aircraft data, Landsat MSS bands, and color aerial photographs.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77585","usgsCitation":"Abrams, M.J., Ashley, R.P., Rowan, L.C., Goetz, A.F., and Kahle, A., 1977, Use of imaging in the 0.46-2.36 [micrometers] spectral region for alteration mapping in the Cuprite mining district, Nevada: U.S. Geological Survey Open-File Report 77-585, ii, 19 leaves :ill., map ;27 cm., https://doi.org/10.3133/ofr77585.","productDescription":"ii, 19 leaves :ill., map ;27 cm.","costCenters":[],"links":[{"id":139947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0585/report-thumb.jpg"},{"id":35093,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0585/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69881a","contributors":{"authors":[{"text":"Abrams, Michael J.","contributorId":15192,"corporation":false,"usgs":true,"family":"Abrams","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":156252,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ashley, R. P.","contributorId":50513,"corporation":false,"usgs":true,"family":"Ashley","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":156256,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowan, L. C.","contributorId":40584,"corporation":false,"usgs":true,"family":"Rowan","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":156254,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Goetz, Alexander F.H.","contributorId":43747,"corporation":false,"usgs":true,"family":"Goetz","given":"Alexander","middleInitial":"F.H.","affiliations":[],"preferred":false,"id":156255,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kahle, A.B.","contributorId":36928,"corporation":false,"usgs":true,"family":"Kahle","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":156253,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":8548,"text":"ofr77769 - 1977 - Analyses of native water, core material, and elutriate samples collected from the Atchafalaya River and Atchafalaya Bay","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr77769","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-769","title":"Analyses of native water, core material, and elutriate samples collected from the Atchafalaya River and Atchafalaya Bay","docAbstract":"During October and November 1976 the U.S. Geological Survey, in cooperation with the U.S. Army Corps of Engineers, collected native water and core material from 14 sites along the Atchafalya River in Louisiana (from the head of Whiskey Bay Pilot Channel to American Pass) and 5 sites in Atchafalya Bay for evaluation of possible environmental effects of a proposed channel-enlargement project. Core material from all river sites and one bay site was collected to a depth of 50 feet (15 meters). At the remaining bay sites, samples were collected to a depth of less than 6 inches (15 centimeters) using a pipe dredge. Core material and native water were analyzed (separately and as elutriate samples prepared from mixtures) for selected metals, nutrients, organic compounds, and physical characteristics. No interpretation of the data is given. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77769","usgsCitation":"Demas, C.R., 1977, Analyses of native water, core material, and elutriate samples collected from the Atchafalaya River and Atchafalaya Bay: U.S. Geological Survey Open-File Report 77-769, iv, 17 p. :fold. map ;27 cm.; (27 p., 1 sheet - PGS), https://doi.org/10.3133/ofr77769.","productDescription":"iv, 17 p. :fold. map ;27 cm.; (27 p., 1 sheet - PGS)","costCenters":[],"links":[{"id":141722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680df2","contributors":{"authors":[{"text":"Demas, Charles R.","contributorId":36121,"corporation":false,"usgs":true,"family":"Demas","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157918,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4133,"text":"cir747 - 1977 - Environmental geology, Allegheny County and vicinity, Pennsylvania: Description of a program and its results","interactions":[],"lastModifiedDate":"2022-12-20T22:56:31.236756","indexId":"cir747","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"747","title":"Environmental geology, Allegheny County and vicinity, Pennsylvania: Description of a program and its results","docAbstract":"Past land-use practices, including mining, in Allegheny County, Pa., have resulted in three principal environmental problems, exclusive of air and water contamination. They are flooding, landsliding, and subsidence over underground mines. In 1973, information was most complete relative to flooding and least complete relative to landsliding.
Accordingly, in July 1973, the U.S. Geological Survey (USGS) and The Appalachian Regional Commission (ARC) entered into an agreement by which the USGS undertook studies chiefly aimed at increasing knowledge of landsliding and mine subsidence relative to land use, but having other ramifications as well, as part of a larger ARC 'Land-use and physical-resource analysis' (LUPRA) program. The chief geographic focus was Allegheny County, but adjacent areas were included in some investigations.
Resulting products, exclusive of this report, are:
1. Forty-three provisional maps of landslide, distribution and susceptibility and of land modified by man in Allegheny County, 1:24,000 scale, 7½ -minute quadrangle format, released to open files.
2. Four USGS Miscellaneous Field Studies (MF) maps of Allegheny County showing (a) bedrock, MF685A; (b) susceptibility to landsliding, MF-685B ; (c) coal-mining features, MF-685C; and (d) zones that can be affected by flooding, landsliding and undermining, MF-685D; all at the scale of 1:50,000.
3. Two MF maps showing coal-mining activity and related information and sites of recorded mine-subsidence events, and one MF map classifying land surface by relative potentiality of mine subsidence, in Allegheny, Washington, and Westmoreland Counties, Pa., at a scale of 1:125,000--MF-693A through MF-693C.
4. A companion report to the Allegheny County map of susceptibility to landsliding--USGS Circular 728.
5. Five MF maps, largely in chart form, describing interaction of the shallow ground-water regime with mining-related problems, landsliding, heavy storm precipitation, and other features and processes, largely in Allegheny County--MF-641A through MF-641E.
Map products are directly applicable to general classification of land for susceptibility to landsliding and mine subsidence and, to a lesser extent, flooding and engineering characteristics. The hydrogeologic charts enable greater understanding of environmental effects of ground water. All products are guides to expected conditions, but none are substitutes for detailed investigations of specific sites by competent technical personnel on the ground.
Specific results and findings are:
1. Knowledge of .susceptibility to landsliding in Allegheny County now is adequate for application to countywide land-use planning.
2. About 110 mi2 (285. km2), or 15 percent, of the county has some significant degree of susceptibility to landsliding.
3. Although a general classification of land in Allegheny, Washington, and Westmoreland Counties relative to mine-subsidence incidents was prepared, data are wholly inadequate for even moderately precise prediction of subsidence events over previously mined-out areas; the accumulation of adequate data might not repay the effort in terms of damage prevention.
4. Commonwealth-of-Pennsylvania regulations, have been very successful in limiting mine-subsidence damage over areas mined after 1966.
5. Undermining and consequent subsidence may have affected the ground-water regime more widely than heretofore believed.
Except for the earth-disturbance inventory that resulted in the maps of susceptibility to landsliding and man-modified land, methods used in the studies largely were conventional. The inventory and ensuing analysis combined aerial photographic interpretation with field work and incorporation of existing data. The method worked very well for the purposes of defining distribution of landslides and areas having different susceptibilities to landsliding. However, if susceptibility to landsliding alone had been the goal, this could have been determined adequately by using photographs at smaller scales and appreciably less expenditure of effort per unit of ground area.
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/cir747","usgsCitation":"Briggs, R.P., 1977, Environmental geology, Allegheny County and vicinity, Pennsylvania: Description of a program and its results: U.S. Geological Survey Circular 747, iv, 25 p., https://doi.org/10.3133/cir747.","productDescription":"iv, 25 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":410830,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23801.htm","linkFileType":{"id":5,"text":"html"}},{"id":31240,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0747/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118109,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0747/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","county":"Allegheny 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Reginald Peter","contributorId":78723,"corporation":false,"usgs":true,"family":"Briggs","given":"Reginald","email":"","middleInitial":"Peter","affiliations":[],"preferred":false,"id":148264,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56400,"text":"wdrFL761 - 1977 - Water resources data for Florida, water year 1976; Volume 1, northeast Florida","interactions":[],"lastModifiedDate":"2024-04-04T22:46:37.592208","indexId":"wdrFL761","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"FL-76-1","title":"Water resources data for Florida, water year 1976; Volume 1, northeast Florida","docAbstract":"Water resources data for the 1975 water year in northeast Florida consists of discharge records for 59 streams, stage—only records for 12 streams, elevations for 67 lakes, and daily water level measurements for 98 wells. Water quality data for approximately 220 surface sites and 700 wells are included; as are 2 miscellaneous measurements, 25 crest—stage partial records, and 8 annual maximum flood profile measurements.
These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, state and federal agencies in Florida.
Water resources data for the 1976 water year for northwest Florida consist of records of stage, discharge, and water quality of streams; elevation and water quality of lakes and reservoirs; water-levels and water quality of wells; and discharge and water quality of springs. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating state and federal agencies in Florida.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL764","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Water resources data for Florida, water year 1976; Volume 4. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f7336","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532582,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10493,"text":"ofr77404 - 1977 - Catalog of seismograph stations operated in support of the ERDA Nevada Operations Office, January 1964 thru June 1976","interactions":[],"lastModifiedDate":"2013-11-07T12:25:19","indexId":"ofr77404","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-404","title":"Catalog of seismograph stations operated in support of the ERDA Nevada Operations Office, January 1964 thru June 1976","docAbstract":"The seismograph stations listed in this catalog were established over the period January 1964 through June 1976 in support of the Energy Research and Development Administration, Nevada (ERDA/NV) underground weapons testing program at the Nevada Test Site (NTS), central Nevada, and Amchitka, Alaska. For station listings before 1964 see Coast and Geodetic Survey publication, \"Seismic Data Summary Nuclear Detonation Program 1961 through 1963\", by W. V. Mickey and T. R. Shugart, January 1964. Coordinates of stations instrumented for ERDA's Industrial Application Division (IAD, Plowshare) events are published in separate reports (Appendix A, page 66). In addition to the stations for monitoring the testing program, other stations established for specific seismicity studies, such as the Aleutian Seismicity Network, are also listed.","language":"English","publisher":"U.S. Geological Survey,","publisherLocation":"Reston, VA","doi":"10.3133/ofr77404","collaboration":"This report is preliminary and has not been edited or reviewed for conformity with Geological Survey standards and nomenclatures","usgsCitation":"Navarro, R., Wuollet, G.M., and Bradley, B., 1977, Catalog of seismograph stations operated in support of the ERDA Nevada Operations Office, January 1964 thru June 1976: U.S. Geological Survey Open-File Report 77-404, 74 p ., https://doi.org/10.3133/ofr77404.","productDescription":"74 p .","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":144946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":270151,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0404/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7263","contributors":{"authors":[{"text":"Navarro, R.","contributorId":32148,"corporation":false,"usgs":true,"family":"Navarro","given":"R.","email":"","affiliations":[],"preferred":false,"id":161491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wuollet, Geraldine M.","contributorId":36561,"corporation":false,"usgs":true,"family":"Wuollet","given":"Geraldine","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":161492,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradley, B.R.","contributorId":39387,"corporation":false,"usgs":true,"family":"Bradley","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":161493,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28880,"text":"wri7773 - 1977 - Digital computer simulation model of the Englishtown aquifer in the northern coastal plain of New Jersey","interactions":[],"lastModifiedDate":"2020-06-24T22:32:33.329655","indexId":"wri7773","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-73","title":"Digital computer simulation model of the Englishtown aquifer in the northern coastal plain of New Jersey","docAbstract":"Continued decline of water levels in the Englishtown aquifer, in New Jersey, has caused considerable concern regarding the ability of the aquifer to meet future yield demands. A detailed study of the capability of the aquifer to yield water entailed the use of a digital computer simulation model to evaluate aquifer and confining layer coefficients and to test alternative concepts of the hydrodynamics of the flow system. The modeled area includes about 750 square miles of the northern Coastal Plain of New Jersey and encompasses all the major centers of pumping from the Englishtown aquifer. The simulation model was calibrated by matching computed declines with historical water-level declines over the 12-year period, 1959-70. The volume of transient and steady leakage into the Englishtown aquifer from and through the adjacent confining layers equaled more than 90 percent of the total volume of water withdrawn from the aquifer between 1959 and 1970. The analytical estimate of transient leakage indicates that about 60 percent of the water withdrawn from the Englishtown between 1959 and 1970 was replaced by water released from storage in the adjacent confining beds. An additional 34 percent of the withdrawal over this time period was supported by steady leakage through the overlying confining bed from the Mount Laurel aquifer. Of the more than 30 billion gallons withdrawn from the aquifer over the 12-year period, about 2 billion gallons were obtained from storage in the aquifer. The values of aquifer and confining-layer coefficients used in the model are nearly the same as the average values obtained from field and laboratory data. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7773","usgsCitation":"Nichols, W.D., 1977, Digital computer simulation model of the Englishtown aquifer in the northern coastal plain of New Jersey: U.S. Geological Survey Water-Resources Investigations Report 77-73, ix, 101 p., https://doi.org/10.3133/wri7773.","productDescription":"ix, 101 p.","costCenters":[],"links":[{"id":159615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0073/report-thumb.jpg"},{"id":375879,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Coastal New Jersey","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.267578125,\n 40.59727063442024\n ],\n [\n -74.37744140625,\n 40.413496049701955\n ],\n [\n -74.2236328125,\n 40.245991504199026\n ],\n [\n -74.619140625,\n 39.41922073655956\n ],\n [\n -75.08056640625,\n 39.487084981687495\n ],\n [\n -75.52001953125,\n 39.791654835253425\n ],\n [\n -75.52001953125,\n 39.40224434029275\n ],\n [\n -75.16845703124999,\n 38.993572058209466\n ],\n [\n -74.77294921875,\n 38.736946065676\n ],\n [\n -73.85009765625,\n 39.9434364619742\n ],\n [\n -73.8720703125,\n 40.49709237269567\n ],\n [\n -74.267578125,\n 40.59727063442024\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b464d","contributors":{"authors":[{"text":"Nichols, W. D.","contributorId":73220,"corporation":false,"usgs":true,"family":"Nichols","given":"W.","middleInitial":"D.","affiliations":[],"preferred":false,"id":200552,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9281,"text":"ofr77594 - 1977 - Graded layering in the Al Hadah pluton near At Ta'if, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr77594","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-594","title":"Graded layering in the Al Hadah pluton near At Ta'if, Kingdom of Saudi Arabia","docAbstract":"To assess urban storm-water-quality characteristics in the metropolitan area of Portland, Oreg., seven drainage basins were selected with varying drainage areas, basin slopes, impervious areas, land uses, and active construction areas. Automatic water-quality samplers, rain gages, and stream gages were installed in each basin. From September 1, 1975, to May 1, 1976, data were collected to determine rainfall intensities and stream discharge. Almost 500 samples from the seven basins were analyzed to describe pollutants for at least four complete storms on each of the basins. In addition to the storm samples, several base-flow samples were collected and analyzed for each site. Stream discharge and water-quality data are tabulated. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77594","usgsCitation":"Hadley, D.G., and Greenwood, W., 1977, Graded layering in the Al Hadah pluton near At Ta'if, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 77-594, iv, 39 leaves :ill., maps ;28 cm., https://doi.org/10.3133/ofr77594.","productDescription":"iv, 39 leaves :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0594/report-thumb.jpg"},{"id":36993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0594/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673f65","contributors":{"authors":[{"text":"Hadley, Donald G.","contributorId":19527,"corporation":false,"usgs":true,"family":"Hadley","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":159414,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Greenwood, William R.","contributorId":53789,"corporation":false,"usgs":true,"family":"Greenwood","given":"William R.","affiliations":[],"preferred":false,"id":159415,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9657,"text":"ofr77677 - 1977 - Station location map and audio-magnetotelluric data log for the area around Coso Hot Springs, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr77677","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-677","title":"Station location map and audio-magnetotelluric data log for the area around Coso Hot Springs, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77677","usgsCitation":"Jackson, D.B., Gregory, D.I., and Kucks, R., 1977, Station location map and audio-magnetotelluric data log for the area around Coso Hot Springs, California: U.S. Geological Survey Open-File Report 77-677, 19 leaves :map ;27 cm., https://doi.org/10.3133/ofr77677.","productDescription":"19 leaves :map ;27 cm.","costCenters":[],"links":[{"id":140961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3e96","contributors":{"authors":[{"text":"Jackson, Dallas B.","contributorId":19947,"corporation":false,"usgs":true,"family":"Jackson","given":"Dallas","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":160066,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gregory, Daniel I.","contributorId":98723,"corporation":false,"usgs":true,"family":"Gregory","given":"Daniel","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":160068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kucks, R.P.","contributorId":53758,"corporation":false,"usgs":true,"family":"Kucks","given":"R.P.","affiliations":[],"preferred":false,"id":160067,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}