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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr92377B","usgsCitation":"Dolan, R., and Peatross, J., 1992, U.S. Geological Survey 1:2,000,000-scale map of shoreline erosion and accretion of the Mid-Atlantic coast; data supplement: U.S. Geological Survey Open-File Report 92-377, 114 p., https://doi.org/10.3133/ofr92377B.","productDescription":"114 p.","costCenters":[],"links":[{"id":422710,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_40488.htm","linkFileType":{"id":5,"text":"html"}},{"id":52309,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0377b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154233,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0377b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696230","contributors":{"authors":[{"text":"Dolan, Robert","contributorId":16405,"corporation":false,"usgs":true,"family":"Dolan","given":"Robert","email":"","affiliations":[],"preferred":false,"id":189103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peatross, Judith","contributorId":46561,"corporation":false,"usgs":true,"family":"Peatross","given":"Judith","email":"","affiliations":[],"preferred":false,"id":189104,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27564,"text":"wri914177 - 1992 - Geohydrology of, and simulation of ground-water flow in, the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri914177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"91-4177","title":"Geohydrology of, and simulation of ground-water flow in, the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire","docAbstract":"Hydrogeologic data collected since 1990 were assessed and a ground-water-flow model was refined in this study of the Milford-Souhegan glacial-drift aquifer in Milford, New Hampshire. The hydrogeologic data collected were used to refine estimates of hydraulic conductivity and saturated thickness of the aquifer, which were previously calculated during 1988-90. In October 1990, water levels were measured at 124 wells and piezometers, and at 45 stream-seepage sites on the main stem of the Souhegan River, and on small tributary streams overlying the aquifer to improve an understanding of ground-water-flow patterns and stream-seepage gains and losses. Refinement of the ground-water-flow model included a reduction in the number of active cells in layer 2 in the central part of the aquifer, a revision of simulated hydraulic conductivity in model layers 2 and representing the aquifer, incorporation of a new block-centered finite-difference ground-water-flow model, and incorporation of a new solution algorithm and solver (a preconditioned conjugate-gradient algorithm). Refinements to the model resulted in decreases in the difference between calculated and measured heads at 22 wells. The distribution of gains and losses of stream seepage calculated in simulation with the refined model is similar to that calculated in the previous model simulation. The contributing area to the Savage well, under average pumping conditions, decreased by 0.021 square miles from the area calculated in the previous model simulation. The small difference in the contrib- uting recharge area indicates that the additional data did not enhance model simulation and that the conceptual framework for the previous model is accurate.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914177","usgsCitation":"Harte, P., and Mack, T.J., 1992, Geohydrology of, and simulation of ground-water flow in, the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire: U.S. Geological Survey Water-Resources Investigations Report 91-4177, 1 v. (various pagings) :ill., maps ;28 cm. [PGS - 104 p.], https://doi.org/10.3133/wri914177.","productDescription":"1 v. (various pagings) :ill., maps ;28 cm. [PGS - 104 p.]","costCenters":[],"links":[{"id":122661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4177/report-thumb.jpg"},{"id":56425,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4177/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8782","contributors":{"authors":[{"text":"Harte, P. T. 0000-0002-7718-1204","orcid":"https://orcid.org/0000-0002-7718-1204","contributorId":36143,"corporation":false,"usgs":true,"family":"Harte","given":"P. T.","affiliations":[],"preferred":false,"id":198332,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mack, Thomas J. 0000-0002-0496-3918","orcid":"https://orcid.org/0000-0002-0496-3918","contributorId":39814,"corporation":false,"usgs":true,"family":"Mack","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198333,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":17818,"text":"ofr92409 - 1992 - Vitrinite reflectance and conodont color alteration index data from Alaska; data to accompany the Thermal maturity map of Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:21","indexId":"ofr92409","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-409","title":"Vitrinite reflectance and conodont color alteration index data from Alaska; data to accompany the Thermal maturity map of Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr92409","usgsCitation":"Johnsson, M.J., Pawlewicz, M., Harris, A., and Valin, Z., 1992, Vitrinite reflectance and conodont color alteration index data from Alaska; data to accompany the Thermal maturity map of Alaska (Version 1.1): U.S. Geological Survey Open-File Report 92-409, 3 computer disks ;3 1/2 in., https://doi.org/10.3133/ofr92409.","productDescription":"3 computer disks ;3 1/2 in.","costCenters":[],"links":[{"id":150022,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1071,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/dds/dds-54/Data/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdb04","contributors":{"authors":[{"text":"Johnsson, Mark J.","contributorId":58631,"corporation":false,"usgs":true,"family":"Johnsson","given":"Mark","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":177978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pawlewicz, M. J.","contributorId":75111,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"M. J.","affiliations":[],"preferred":false,"id":177979,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harris, A. G.","contributorId":39791,"corporation":false,"usgs":true,"family":"Harris","given":"A. G.","affiliations":[],"preferred":false,"id":177977,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Valin, Z. C. 0000-0001-6199-6700","orcid":"https://orcid.org/0000-0001-6199-6700","contributorId":75165,"corporation":false,"usgs":true,"family":"Valin","given":"Z. C.","affiliations":[],"preferred":false,"id":177980,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":23325,"text":"ofr92401 - 1992 - A test to evaluate the earthquake prediction algorithm, M8","interactions":[],"lastModifiedDate":"2017-05-09T15:35:56","indexId":"ofr92401","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-401","title":"A test to evaluate the earthquake prediction algorithm, M8","docAbstract":"A test of the algorithm M8 is described. The test is constructed to meet four rules, which we propose to be applicable to the test of any method for earthquake prediction:
1. An earthquake prediction technique should be presented as a well documented, logical algorithm that can be used by investigators without restrictions.
2. The algorithm should be coded in a common programming language and implementable on widely available computer systems.
3. A test of the earthquake prediction technique should involve future predictions with a black box version of the algorithm in which potentially adjustable parameters are fixed in advance. The source of the input data must be defined and ambiguities in these data must be resolved automatically by the algorithm.
4. At least one reasonable null hypothesis should be stated \u0001 in advance of testing the earthquake prediction method, and it should be stated how this null hypothesis will be used to estimate the statistical significance of the earthquake predictions.
The M8 algorithm has successfully predicted several destructive \u0001 earthquakes, in the sense that the earthquakes occurred inside regions with linear dimensions from 384 to 854 km that the algorithm had identified as being in times of increased probability for strong earthquakes. In addition, M8 has successfully \"post predicted\" high percentages of strong earthquakes in regions to which it has been applied in retroactive studies. The statistical significance of previous predictions has not been established, however, and post-prediction studies in general are notoriously subject to success-enhancement through hindsight. Nor has it been determined how much more precise an M8 prediction might be than forecasts and probability-of-occurrence estimates made by other techniques. We view our test of M8 both as a means to better determine the effectiveness of M8 and as an experimental structure within which to make observations that might lead to improvements in the algorithm or conceivably lead to a radically different approach to earthquake prediction.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr92401","issn":"0094-9140","usgsCitation":"Healy, J., Kossobokov, V.G., and Dewey, J.W., 1992, A test to evaluate the earthquake prediction algorithm, M8: U.S. Geological Survey Open-File Report 92-401, Report: 23 p., Appendixes, https://doi.org/10.3133/ofr92401.","productDescription":"Report: 23 p., Appendixes","numberOfPages":"117","costCenters":[],"links":[{"id":156197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0401/report-thumb.jpg"},{"id":340530,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0401/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5b7e","contributors":{"authors":[{"text":"Healy, John H.","contributorId":19562,"corporation":false,"usgs":true,"family":"Healy","given":"John H.","affiliations":[],"preferred":false,"id":189906,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kossobokov, Vladimir G.","contributorId":84794,"corporation":false,"usgs":true,"family":"Kossobokov","given":"Vladimir","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":189907,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dewey, James W. 0000-0001-8838-2450 jdewey@usgs.gov","orcid":"https://orcid.org/0000-0001-8838-2450","contributorId":5819,"corporation":false,"usgs":true,"family":"Dewey","given":"James","email":"jdewey@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":189905,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":38310,"text":"ofr92300B - 1992 - Preliminary geomagnetic data, College Observatory, Fairbanks","interactions":[],"lastModifiedDate":"2012-02-02T00:09:48","indexId":"ofr92300B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-300","chapter":"B","title":"Preliminary geomagnetic data, College Observatory, Fairbanks","language":"ENGLISH","doi":"10.3133/ofr92300B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Preliminary geomagnetic data, College Observatory, Fairbanks (February): U.S. Geological Survey Open-File Report 92-300, v. 10p. :ill. ;28 cm., https://doi.org/10.3133/ofr92300B.","productDescription":"v. 10p. :ill. ;28 cm.","costCenters":[],"links":[{"id":165249,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0300b/report-thumb.jpg"},{"id":64680,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0300b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"February","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69782b","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":529854,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29430,"text":"wri904124 - 1992 - Sediment transport, particle sizes, and loads in lower reaches of the Chippewa, Black, and Wisconsin Rivers in Western Wisconsin","interactions":[],"lastModifiedDate":"2022-02-08T19:43:13.597235","indexId":"wri904124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"90-4124","title":"Sediment transport, particle sizes, and loads in lower reaches of the Chippewa, Black, and Wisconsin Rivers in Western Wisconsin","docAbstract":"Hydraulic and sediment data were collected at three sites on the Chippewa River (near Caryville, at Durand, and near Pepin); at one site near Galesville on the Black River; and at one site at Muscoda on the Wisconsin River during water years 1976-83. This report summarizes an interpretation of those data by providing (1) a description of the relation of suspended sediment, bedload, and total-sediment discharge to water discharge; (2) a description of particle-size characteristics of bed material, bedload, and suspended sediment; and (3) estimates of annual and average annual suspended load, bedload, and total-sediment load for water years 1974-83. Direct measurement with a Helley-Smith bedload sampler and calculations by the modified-Einstein procedure were used to estimate bedload.
\nSingle equations describe the suspended- and totalsediment transport-rate relations for Chippewa River at Durand and main channel at Pepin, and the Black River near Galesville. Two equations were needed to define the transport- rate relations for the Chippewa River near Caryville and Wisconsin River at Muscoda.
\nBed material at all sites except Chippewa River near Caryville were of similar particle size and exhibited little variation with time or location in the river cross sections. Median diameter at these sites ranged from 0.35 to 0.84 mm (millimeter). At Chippewa River near Caryville, median diameter ranged from 0.42 to 15 mm. Helley-Smith bedload at Chippewa River at Durand and near Pepin, Black River near Galesville, and Wisconsin River at Muscoda were of similar particle size. About 57 to 65 percent of bedload at all sites except Chippewa River near Caryville was in the 0.4- to 0.6- mm size range. About 50 percent of bedload at Chippewa River near Caryville was in the 0.5- to 1.0-mm size range. Suspended sediment at all sites except Chippewa River near Caryville was in the sand-size range; the average median diameters were between 0.17 and 0.22 mm. At Chippewa River near Caryville, 60 percent (on the average) of suspended sediment was finer than 0.062 mm.
\nAverage annual total-sediment load and the percentage transported as bedload were determined for a 10-year period (water years 1974-83)(October 1,1973-September 30, 1982). These loads and percentages were, respectively, 123,000 tons and 35 percent at Chippewa River near Caryville; 1,073,000 tons and 61 percent at Chippewa River at Durand; 940,000 tons and 44 percent at Chippewa River near Pepin; 277,000 tons and 43 percent at Black River near Galesville; and 558,000 tons and 49 percent at Wisconsin River at Muscoda.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904124","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Rose, W.J., 1992, Sediment transport, particle sizes, and loads in lower reaches of the Chippewa, Black, and Wisconsin Rivers in Western Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 90-4124, vi, 38 p., https://doi.org/10.3133/wri904124.","productDescription":"vi, 38 p.","numberOfPages":"44","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":58278,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4124/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":395643,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47385.htm"},{"id":159780,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4124/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Black River, Chippewa River, Wisconsin River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.333,\n 43\n ],\n [\n -89,\n 43\n ],\n [\n -89,\n 46\n ],\n [\n -92.333,\n 46\n ],\n [\n -92.333,\n 43\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbe93","contributors":{"authors":[{"text":"Rose, W. J.","contributorId":14433,"corporation":false,"usgs":true,"family":"Rose","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":201515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17050,"text":"ofr92598AB - 1992 - Descriptions of seismic array components; Part 3, Software modules for data conversion","interactions":[],"lastModifiedDate":"2012-02-02T00:07:10","indexId":"ofr92598AB","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-598","chapter":"A,B","title":"Descriptions of seismic array components; Part 3, Software modules for data conversion","language":"ENGLISH","publisher":"U.S. Department of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section, distributor, 1992","doi":"10.3133/ofr92598AB","usgsCitation":"Lee, W., 1992, Descriptions of seismic array components; Part 3, Software modules for data conversion: U.S. Geological Survey Open-File Report 92-598, 106, [5] p. ;28 cm. +1 computer disk ; 3 1/2 in., https://doi.org/10.3133/ofr92598AB.","productDescription":"106, [5] p. ;28 cm. +1 computer disk ; 3 1/2 in.","costCenters":[],"links":[{"id":149620,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0598a-b/report-thumb.jpg"},{"id":46190,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0598a-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668dcc","contributors":{"authors":[{"text":"Lee, W.H.","contributorId":81901,"corporation":false,"usgs":true,"family":"Lee","given":"W.H.","affiliations":[],"preferred":false,"id":174738,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":49607,"text":"ofr92602B - 1992 - Earthquake data report, February 1992","interactions":[],"lastModifiedDate":"2013-03-27T07:44:31","indexId":"ofr92602B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-602","chapter":"B","title":"Earthquake data report, February 1992","language":"ENGLISH","doi":"10.3133/ofr92602B","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Earthquake data report, February 1992: U.S. Geological Survey Open-File Report 92-602, Three 5 1/4 inch diskettes, https://doi.org/10.3133/ofr92602B.","productDescription":"Three 5 1/4 inch diskettes","costCenters":[],"links":[{"id":175934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":270268,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1992/0602b/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a92d","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":531996,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4726,"text":"twri03B7 - 1992 - Analytical solutions for one-, two-, and three-dimensional solute transport in ground-water systems with uniform flow","interactions":[{"subject":{"id":16509,"text":"ofr8956 - 1989 - Analytical solutions for one-, two-, and three-dimensional solute transport in ground-water systems with uniform flow","indexId":"ofr8956","publicationYear":"1989","noYear":false,"title":"Analytical solutions for one-, two-, and three-dimensional solute transport in ground-water systems with uniform flow"},"predicate":"SUPERSEDED_BY","object":{"id":4726,"text":"twri03B7 - 1992 - Analytical solutions for one-, two-, and three-dimensional solute transport in ground-water systems with uniform flow","indexId":"twri03B7","publicationYear":"1992","noYear":false,"title":"Analytical solutions for one-, two-, and three-dimensional solute transport in ground-water systems with uniform flow"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"twri03B7","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-B7","title":"Analytical solutions for one-, two-, and three-dimensional solute transport in ground-water systems with uniform flow","docAbstract":"Analytical solutions to the advective-dispersive solute-transport equation are useful in predicting the fate of solutes in ground water. Analytical solutions compiled from available literature or derived by the author are presented for a variety of boundary condition types and solute-source configurations in one-, two-, and three-dimensional systems having uniform ground-water flow. A set of user-oriented computer programs was created to evaluate these solutions and to display the results in tabular and computer-graphics format. These programs incorporate many features that enhance their accuracy, ease of use, and versatility. Documentation for the programs describes their operation and required input data, and presents the results of sample problems. Derivations of selected solutions, source codes for the computer programs, and samples of program input and output also are included.","language":"ENGLISH","publisher":"U.S. G.P.O. ;Book and Open-File Report Sales [distributor],","doi":"10.3133/twri03B7","issn":"0565-596X","usgsCitation":"Wexler, E.J., 1992, Analytical solutions for one-, two-, and three-dimensional solute transport in ground-water systems with uniform flow: U.S. Geological Survey Techniques of Water-Resources Investigations 03-B7, x, 190 p. :ill. ;28 cm., https://doi.org/10.3133/twri03B7.","productDescription":"x, 190 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":139099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":354,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri3-b7/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c35c","contributors":{"authors":[{"text":"Wexler, Eliezer J.","contributorId":99963,"corporation":false,"usgs":true,"family":"Wexler","given":"Eliezer","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":149689,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":49624,"text":"ofr92611A - 1992 - Earthquake data report, November 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr92611A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-611","chapter":"A","title":"Earthquake data report, November 1992","language":"ENGLISH","doi":"10.3133/ofr92611A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Earthquake data report, November 1992: U.S. Geological Survey Open-File Report 92-611, 420 p., https://doi.org/10.3133/ofr92611A.","productDescription":"420 p.","costCenters":[],"links":[{"id":176927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0611a/report-thumb.jpg"},{"id":86226,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0611a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a250","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":532013,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38311,"text":"ofr92300C - 1992 - Preliminary geomagnetic data, College Observatory, Fairbanks","interactions":[],"lastModifiedDate":"2012-02-02T00:09:48","indexId":"ofr92300C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-300","chapter":"C","title":"Preliminary geomagnetic data, College Observatory, Fairbanks","language":"ENGLISH","doi":"10.3133/ofr92300C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Preliminary geomagnetic data, College Observatory, Fairbanks (March): U.S. Geological Survey Open-File Report 92-300, v. 11p. :ill. ;28 cm., https://doi.org/10.3133/ofr92300C.","productDescription":"v. 11p. :ill. ;28 cm.","costCenters":[],"links":[{"id":165250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0300c/report-thumb.jpg"},{"id":64681,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0300c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"March","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db67350b","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":529855,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17073,"text":"ofr92601A - 1992 - Earthquake data report, January 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr92601A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-601","chapter":"A","title":"Earthquake data report, January 1992","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, National Earthquake Information Center :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr92601A","usgsCitation":"National Earthquake Information Center, 1992, Earthquake data report, January 1992: U.S. Geological Survey Open-File Report 92-601, 340 p., https://doi.org/10.3133/ofr92601A.","productDescription":"340 p.","costCenters":[],"links":[{"id":148615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0601a/report-thumb.jpg"},{"id":46202,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0601a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a8b0","contributors":{"authors":[{"text":"National Earthquake Information Center","contributorId":128066,"corporation":true,"usgs":false,"organization":"National Earthquake Information Center","id":529000,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21401,"text":"ofr92405 - 1992 - Late Pliocene pollen assemblages from Ocean Drilling Project Hole 646B; census data and paleoclimatic estimates","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr92405","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-405","title":"Late Pliocene pollen assemblages from Ocean Drilling Project Hole 646B; census data and paleoclimatic estimates","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr92405","usgsCitation":"Willard, D.A., 1992, Late Pliocene pollen assemblages from Ocean Drilling Project Hole 646B; census data and paleoclimatic estimates: U.S. Geological Survey Open-File Report 92-405, 12 p. ill. ;28 cm., https://doi.org/10.3133/ofr92405.","productDescription":"12 p. ill. ;28 cm.","costCenters":[],"links":[{"id":153843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0405/report-thumb.jpg"},{"id":50970,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0405/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b49","contributors":{"authors":[{"text":"Willard, Debra A. 0000-0003-4878-0942 dwillard@usgs.gov","orcid":"https://orcid.org/0000-0003-4878-0942","contributorId":2076,"corporation":false,"usgs":true,"family":"Willard","given":"Debra","email":"dwillard@usgs.gov","middleInitial":"A.","affiliations":[{"id":411,"text":"National Climate Change and Wildlife Science Center","active":true,"usgs":true},{"id":24693,"text":"Climate Research and Development","active":true,"usgs":true}],"preferred":true,"id":184361,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":59812,"text":"mf2205 - 1992 - A geochemical investigation of selected areas in Greenville and Laurens Counties, South Carolina: Implications for mineral resources","interactions":[],"lastModifiedDate":"2022-09-15T20:27:37.582435","indexId":"mf2205","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2205","title":"A geochemical investigation of selected areas in Greenville and Laurens Counties, South Carolina: Implications for mineral resources","docAbstract":"The purpose of this study is to geochemically evaluate three areas within the Greenville 1° x 2° quadrangle (see index map) that have been shown by previous studies to contain anomalously high amounts of tin. Jackson and Moore (1992) reported the presence of cassiterite (SnO2)-bearing heavy-mineral concentrates from stream sediment samples that were collected during a regional geochemical reconnaissance of the Greenville 1° x 2° quadrangle. The data reported here confirm identified in selected heavy-mineral concentrate samples. In addition, anomalously high concentrations of barium, beryllium, lanthanum, and thorium are also reported for parts of the same areas. No significant mineral deposits are known to occur in the study areas. There was, however, minor production of monazite from several nearby localities (Sloan, 1908), and gold was produced from deposits in the northeastern part of Greenville County and nearby Spartanburg County (McCauley and Butler, 1966). The three areas selected for resampling are located in the Inner Piedmont physiographic province of South Carolina (see index map). The generalized tectonic setting of the region and the locations of the study is just north of Greenville, S.C. Much of it is within the moderately to steeply sloped terrane of Paris Mountain State Park where elevations reach approximately 600 m. Simpsonville, S.C., is neat the center of the second study area, and the southernmost study area is near Hickory Tavern, S.C. Both the Simpsonville and Hickory Tavern study areas are in more gently rolling Piedmont terrane. Each of the sampled areas is drained by tributaries of the Enoree and Reedy Rivers. Parts of three different thrust sheets underlie the region covered by this study (fig. 1); in ascending structural position, they are the Six Mile, Paris Mountain, and Laurens thrust sheets (Nelson and others, 1987). Nelson (1988, p. 7) described the contacts between these sheets as being along unnamed faults. The rocks in and around the study areas have undergone sillimanite-muscovite-grade metamorphism (Nelson, 1988, p. 9). Nelson (1988, p. 13) reports that the Six Mile thrust sheet was metamorphosed about 344 Ma. The geology of these sheets as described in this study, including geologic contacts, rock descriptions, and unit names, generally follows that of Nelson and others (1987, 1989). Within the Paris Mountain study area, rocks of the Paris Mountain thrust sheet predominate (fig. 2) and consist of a biotite-muscovite-sillimanite schist (EZsp) that has extensive lenses of fine- to medium- grained biotite granite gneiss (Pzgp). Areas of biotite granite gneiss that occur in the southern part of the Paris Mountain study area contain extensive pegmatitic and leucogranitic phases. These pegmatitic zones consist mostly of coarse-grained microcline feldspar and quartz with minor amounts of muscovite, biotite, and garnet. Smaller pegmatite lenses (<0.5 m thick) that occur within the biotite-muscovite-sillimanite schist of the Paris Mountain study area are generally of similar mineralogy, although some contain tourmaline crystals up to 5 cm in length. The Six Mile thrust sheet underlies the northern edge of the Paris Mountain study area, where it is composed of gneissic biotitic granites of the Caesars Head Granite (figs. 1 and 2). The northwestern part of the Simpsonville study area (figs. 1 and 3), within the Paris Mountain thrust sheet, is underlain by a biotite-muscovite-sillimanite schist (EZsp) that contains lenses of biotite granite gneiss (Pzgp). In the southeastern part of the Simpsonville study area, within the Laurens thrust sheet, biotite gneiss (EZgl), biotite granite gneiss (Pzgf), and minor amphibolite (EZal) are interlayered biotite (EZgl), granite gneiss (Dgg), and amphibolite (EZal) of the Laurens thrust sheet (fig. 4).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf2205","usgsCitation":"Jackson, J.C., 1992, A geochemical investigation of selected areas in Greenville and Laurens Counties, South Carolina: Implications for mineral resources: U.S. Geological Survey Miscellaneous Field Studies Map 2205, 2 Plates: 48.27 x 29.72 inches and 42.00 x 36.70 inches, https://doi.org/10.3133/mf2205.","productDescription":"2 Plates: 48.27 x 29.72 inches and 42.00 x 36.70 inches","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":182455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2205.jpg"},{"id":406790,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5837.htm","linkFileType":{"id":5,"text":"html"}},{"id":284442,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2205/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":284443,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2205/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","datum":"National Geodetic Datum of 1929","country":"United States","state":"South Carolina","county":"Greenville County, Laurens County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.45,\n 34.625\n ],\n [\n -82.125,\n 34.625\n ],\n [\n -82.125,\n 35\n ],\n [\n -82.45,\n 35\n ],\n [\n -82.45,\n 34.625\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd49dce4b0b290850ef6d6","contributors":{"authors":[{"text":"Jackson, John C. jjackson@usgs.gov","contributorId":2652,"corporation":false,"usgs":true,"family":"Jackson","given":"John","email":"jjackson@usgs.gov","middleInitial":"C.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":262638,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}