{"pageNumber":"1772","pageRowStart":"44275","pageSize":"25","recordCount":46615,"records":[{"id":5200348,"text":"5200348 - 1974 - Relationships between chemical structure and rat repellency: II. compounds screened between 1950 and 1960","interactions":[],"lastModifiedDate":"2017-09-14T09:27:32","indexId":"5200348","displayToPublicDate":"2009-06-09T10:33:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":91,"text":"Technical Report","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"75-11-FEL.","title":"Relationships between chemical structure and rat repellency: II. compounds screened between 1950 and 1960","docAbstract":"Over 4,600 compounds, chiefly organic types, were evaluated using both a food acceptance test (Part A) and a barrier penetration bioassay (Part B), to correlate relationships between chemical structure and rodent repellency. These chemicals are indexed and classified according to the functional groups present and to the degree of substitution within their molecular structures. The results of reduction in food consumption for each compound appraised are calculated and their K values listed in Table 1.  The repellent activities of the functional groups represented, alone or in combinations, are expressed in Table II by a Functional Group Repellency Index.. A ranking of these indices suggests that acyclic and heteroyclic compounds containing tri- or pentavalent nitrogen would be a parent compound of choice for synthesizing novel repellents. Other molecular arrangements, spatial configurations and combinations of functional groups are compared.  There were 123 active, interesting or promising compounds included in the 699 having K values of 85 or greater, which were selected for the barrier appraisal study. These chemicals were formulated in selective solvents at several concentrations and applied to burlap.  Small food bags were fashioned using the fabric impregnated with the candidate formulation, and exposed to rodent attack following storage periods of varying intervals. The results of these tests are listed in Table III. Again, those compounds containing nitrogen in the functional groupings indicated a high order of effectiveness. Several commercial patents covering rodent repellents were issued using the data from the food acceptance and barrier studies. Organizations and cooperators which supplied samples for the program are listed in Appendix I. The Wiswesser cipher for compounds in Table I is used in Appendix II to facilitate location of chemicals by sample code number as they appear under the index headings, and for computer storage and analysis.","language":"English","publisher":" Food Engineering Laboratory, US Army Natick Laboratories","publisherLocation":"Natick, MA","collaboration":"OCLC: 2748732.  Project reference: 1T662713A031-07","usgsCitation":"Bowles, W.A., Adomaitis, V.A., DeWitt, J., and Pratt, J., 1974, Relationships between chemical structure and rat repellency: II. compounds screened between 1950 and 1960: Technical Report 75-11-FEL., iv, 375.","productDescription":"iv, 375","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92056,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://handle.dtic.mil/100.2/ADA005157"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db63472a","contributors":{"authors":[{"text":"Bowles, Walter A.","contributorId":101779,"corporation":false,"usgs":true,"family":"Bowles","given":"Walter","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":327580,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adomaitis, V. A.","contributorId":66198,"corporation":false,"usgs":true,"family":"Adomaitis","given":"V.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":327578,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeWitt, J.B.","contributorId":89080,"corporation":false,"usgs":true,"family":"DeWitt","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":327579,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pratt, J.J. Jr.","contributorId":40543,"corporation":false,"usgs":true,"family":"Pratt","given":"J.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":327577,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5200081,"text":"5200081 - 1974 - Optimal exploitation strategies for an animal population in a stochastic serially correlated environment","interactions":[],"lastModifiedDate":"2012-02-02T00:15:20","indexId":"5200081","displayToPublicDate":"2009-06-08T16:49:39","publicationYear":"1974","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Optimal exploitation strategies for an animal population in a stochastic serially correlated environment","docAbstract":"Optimal exploitation strategies were studied for an animal population in a stochastic, serially correlated environment.  This is a general case and encompasses a number of important cases as simplifications.  Data on the mallard (Anas platyrhynchos) were used to explore the exploitation strategies and test several hypotheses because relatively much is known concerning the life history and general ecology of this species and extensive empirical data are available for analysis.  The number of small ponds on the central breeding grounds was used as an index to the state of the environment.     Desirable properties of an optimal exploitation strategy were defined.  A mathematical model was formulated to provide a synthesis of the existing literature, estimates of parameters developed from an analysis of data, and hypotheses regarding the specific effect of exploitation on total survival.  Both the literature and the analysis of data were inconclusive concerning the effect of exploitation on survival.  Therefore, alternative hypotheses were formulated: (1) exploitation mortality represents a largely additive form of mortality, or (2 ) exploitation mortality is compensatory with other forms of mortality, at least to some threshold level.  Models incorporating these two hypotheses were formulated as stochastic dynamic programming models and optimal exploitation strategies were derived numerically on a digital computer.     Optimal exploitation strategies were found to exist under rather general conditions. Direct feedback control was an integral component in the optimal decision-making process.  Optimal exploitation was found to be substantially different depending upon  the hypothesis regarding the effect of exploitation on the population.  Assuming that exploitation is largely an additive force of mortality, optimal exploitation decisions are a convex function of the size of the breeding population and a linear or slightly concave function of the environmental conditions.  Optimal exploitation under this hypothesis tends to reduce the variance of the size of the population.  Under the hypothesis of compensatory mortality forces, optimal exploitation decisions are approximately linearly related to the size of the breeding population.     Environmental variables may be somewhat more important than the size of the breeding population to the production of young mallards. In contrast, the size of the breeding population appears to be more important in the exploitation process than is the state of the environment.  The form of the exploitation strategy appears to be relatively insensitive to small changes in the production rate.  In general, the relative importance of the size of the breeding population may decrease as fecundity increases.     The optimal level of exploitation in year t must be based on the observed size of the population and the state of the environment in year t unless the dynamics of the population, the state of the environment, and the result of the exploitation decisions are completely deterministic.  Exploitation based on an average harvest, harvest rate, or designed to maintain a constant breeding population size is inefficient.","language":"English","publisher":"Ph.D. Dissertation, University of Maryland","publisherLocation":"College Park","usgsCitation":"Anderson, D., 1974, Optimal exploitation strategies for an animal population in a stochastic serially correlated environment, 84.","productDescription":"84","numberOfPages":"84","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f400c","contributors":{"authors":[{"text":"Anderson, David R.","contributorId":8413,"corporation":false,"usgs":true,"family":"Anderson","given":"David R.","affiliations":[],"preferred":false,"id":326960,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011015,"text":"70011015 - 1974 - Preliminary results from a search for regional tectonomagnetic effects in California and western Nevada","interactions":[],"lastModifiedDate":"2025-08-29T16:13:30.649569","indexId":"70011015","displayToPublicDate":"2003-04-08T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Preliminary results from a search for regional tectonomagnetic effects in California and western Nevada","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>Physical theory and laboratory experiments both indicate that tectonomagnetic effects in seismically active areas should be detected with highly sensitive drift-free differential magnetometers. By using a pair of synchronized 0.25 7 absolute magnetometers to measure precisely field differences between 70 adjacent sites with a 10–15 km separation, more than 1,000 km of faults in California and western Nevada have been monitored for anomalous changes in the local magnetic field. Over a nine-month period, four sets of mea surements have been completed along 350 km of the San Andreas and two sets along the Excelsior Mountains, Mono Lake, and Owens Valley. Preliminary results show that significant changes have occurred between each subsequent data set and that these changes appear to be related to tectonic structure and seismicity. This method looks promising as a simple inexpensive scheme for indicating some hazardous sections of active faults, particularly in countries where extensive geophysics programs are not feasible.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(74)90026-2","issn":"00401951","usgsCitation":"Johnston, M., 1974, Preliminary results from a search for regional tectonomagnetic effects in California and western Nevada: Tectonophysics, v. 23, no. 3, p. 267-275, https://doi.org/10.1016/0040-1951(74)90026-2.","productDescription":"9 p.","startPage":"267","endPage":"275","costCenters":[],"links":[{"id":221715,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.57301703347488,\n              37.77611539118337\n            ],\n            [\n              -122.57301703347488,\n              34.6023069628598\n            ],\n            [\n              -115.30490121198801,\n              34.6023069628598\n            ],\n            [\n              -115.30490121198801,\n              37.77611539118337\n            ],\n            [\n              -122.57301703347488,\n              37.77611539118337\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"23","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8a5ee4b0c8380cd7e039","contributors":{"authors":[{"text":"Johnston, M.J.S. 0000-0003-4326-8368","orcid":"https://orcid.org/0000-0003-4326-8368","contributorId":104889,"corporation":false,"usgs":true,"family":"Johnston","given":"M.J.S.","affiliations":[],"preferred":false,"id":360091,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69544,"text":"hu39 - 1974 - Hydrologic Unit Map -- 1974, State of Pennsylvania","interactions":[],"lastModifiedDate":"2016-08-23T09:05:02","indexId":"hu39","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"39","subseriesTitle":"Pennsylvania 1974","title":"Hydrologic Unit Map -- 1974, State of Pennsylvania","docAbstract":"<p><span>This map and accompanying table show Hydrologic Units that are basically hydrographic in nature. &nbsp;The Cataloging Units shown will supplant the Cataloging Units previously used by the U.S. Geological Survey in its Catalog of Information on Water Data (1966-72). &nbsp;The previous U.S. Geological Survey Catalog-Indexing System was by map number and letter, such as 49M. 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,{"id":27698,"text":"wri7331 - 1974 - Evaluating pollution potential of land-based waste disposal, Santa Clara County, California: An application of earth-science data for planning","interactions":[],"lastModifiedDate":"2022-05-23T18:43:18.310967","indexId":"wri7331","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"73-31","title":"Evaluating pollution potential of land-based waste disposal, Santa Clara County, California: An application of earth-science data for planning","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7331","usgsCitation":"Hines, W.G., 1974, Evaluating pollution potential of land-based waste disposal, Santa Clara County, California: An application of earth-science data for planning: U.S. Geological Survey Water-Resources Investigations Report 73-31, 21 p., https://doi.org/10.3133/wri7331.","productDescription":"21 p.","costCenters":[],"links":[{"id":120051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0031/report-thumb.jpg"},{"id":400904,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49055.htm"},{"id":56548,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Santa Clara County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.2028,\n              36.8928\n            ],\n            [\n              -121.2033,\n              36.8928\n            ],\n            [\n              -121.2033,\n              37.4761\n            ],\n            [\n              -122.2028,\n              37.4761\n            ],\n            [\n              -122.2028,\n              36.8928\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db6297dc","contributors":{"authors":[{"text":"Hines, Walter G.","contributorId":100360,"corporation":false,"usgs":true,"family":"Hines","given":"Walter","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":198555,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56736,"text":"wdrMANHRIVT721 - 1974 - Water resources data for Massachusetts, New Hampshire, Rhode Island, and Vermont; water year 1972","interactions":[],"lastModifiedDate":"2025-12-02T15:32:01.803003","indexId":"wdrMANHRIVT721","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"MA-NH-RI-VT-72-1","title":"Water resources data for Massachusetts, New Hampshire, Rhode Island, and Vermont; water year 1972","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMANHRIVT721","collaboration":"Prepared in cooperation with the States of Massachusetts, New Hampshire, Rhode Island, and Vermont and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for Massachusetts, New Hampshire, Rhode Island, and Vermont; water year 1972: U.S. Geological Survey Water Data Report MA-NH-RI-VT-72-1, x, 394 p., https://doi.org/10.3133/wdrMANHRIVT721.","productDescription":"x, 394 p.","costCenters":[],"links":[{"id":496973,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1972/manhrivt-72-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182188,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1972/manhrivt-72-1/report-thumb.jpg"}],"country":"United States","state":"Massachusetts, New Hampshire, Rhode Island, Vermont","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.75815221267698,\n              41.97228971974073\n            ],\n            [\n              -72.05914450679514,\n              41.94783744910603\n            ],\n            [\n              -72.03721909861372,\n              41.17689376348471\n            ],\n            [\n              -69.54898870658968,\n              41.17689376348471\n            ],\n            [\n              -69.62571827814965,\n              42.66928063226206\n            ],\n            [\n              -70.66704818797406,\n              42.70956583410782\n            ],\n            [\n              -70.93013691979999,\n              45.43370116430904\n            ],\n            [\n              -71.6206949033691,\n              45.16384754432022\n            ],\n            [\n              -73.45123515505567,\n              45.15613160933199\n            ],\n            [\n              -73.75815221267698,\n              41.97228971974073\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4024","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":532852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69508,"text":"hu17 - 1974 - Hydrologic Unit Map -- 1974, State of Kentucky","interactions":[],"lastModifiedDate":"2022-04-26T19:38:09.602395","indexId":"hu17","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"17","subseriesTitle":"Kentucky 1974","title":"Hydrologic Unit Map -- 1974, State of Kentucky","docAbstract":"<p>This map and accompanying table show Hydrologic Units that are basically hydrographic in nature. &nbsp;The Cataloging Units shown will supplant the Cataloging Units previously used by the U.S. Geological Survey in its Catalog of Information on Water Data (1966-72). &nbsp;The previous U.S. Geological Survey Catalog-Indexing System was by map number and letter, such as 49M. 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,{"id":56757,"text":"wdrMS731 - 1974 - Water resources data for Mississippi, water year 1973","interactions":[],"lastModifiedDate":"2025-07-29T14:40:47.092271","indexId":"wdrMS731","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"MS-73-1","title":"Water resources data for Mississippi, water year 1973","docAbstract":"<p>Water resources data for the 1973 water year for Mississippi including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, and records of water-quality data on the chemical and physical characteristics of surface water, are given in this report. In Part 1, records are included for 79 gaging stations of which 75 are streamflow discharge stations, and 4 are reservoir or lake stations; also are included records for 58 low-flow partial-record stations, 139 crest-stage partial-record stations, and 79 miscellaneous sites. Locations of gaging stations are shown in Figure 1. In Part 2, data on the quality of surface water (chemical and temperature) were collected from designated sampling sites at predetermined intervals such as monthly, or less frequently. Records are given for 70 sampling stations of which 32 are continuous record stations, 26 are partial-record stations, and 12 are miscellaneous sites. Locations of water-quality stations are shown in Figure 1. A few pertinent stations (not included above) furnished by bordering States are also included in this report. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of L. E. Carroon, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Mississippi.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMS731","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for Mississippi, water year 1973: U.S. Geological Survey Water Data Report MS-73-1, vii, 184 p., https://doi.org/10.3133/wdrMS731.","productDescription":"vii, 184 p.","costCenters":[],"links":[{"id":493095,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1973/ms-73-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175275,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1973/ms-73-1/report-thumb.jpg"}],"country":"United 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,{"id":16210,"text":"ofr7458 - 1974 - South Carolina seismic program","interactions":[],"lastModifiedDate":"2023-12-06T21:13:16.29259","indexId":"ofr7458","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-58","title":"South Carolina seismic program","docAbstract":"<p>The principal objectives of the South Carolina Seismic Program are to: (1) provide essential high-quality raw seismic data for earthquakes in South Carolina; (2) compute accurate estimates of event and source parameters; (3) provide a catalog of events and source parameters that will be used in further evaluation of seismic hazard; and (4) respond with rapid estimates of event parameters if a large event occurs 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,{"id":59581,"text":"mf526 - 1974 - Availability of data on surface-water quantity and quality for the San Francisco Bay region, California with a summary of beneficial uses and implications for land use","interactions":[],"lastModifiedDate":"2021-11-22T19:09:58.299096","indexId":"mf526","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"526","title":"Availability of data on surface-water quantity and quality for the San Francisco Bay region, California with a summary of beneficial uses and implications for land use","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf526","usgsCitation":"Goss, J., 1974, Availability of data on surface-water quantity and quality for the San Francisco Bay region, California with a summary of beneficial uses and implications for land use: U.S. Geological Survey Miscellaneous Field Studies Map 526, Report; 17 p.; 1 Plate: 34.03 × 41.57 inches, https://doi.org/10.3133/mf526.","productDescription":"Report; 17 p.; 1 Plate: 34.03 × 41.57 inches","costCenters":[],"links":[{"id":391993,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3624.htm"},{"id":274548,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/0526/report.pdf"},{"id":274547,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0526/plate-1.pdf"},{"id":184869,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","country":"United States","state":"California","otherGeospatial":"San Francisco Bay region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.77197265625,\n              36.94111143010769\n            ],\n            [\n              -121.201171875,\n              36.94111143010769\n            ],\n            [\n              -121.201171875,\n              38.92522904714054\n            ],\n            [\n              -123.77197265625,\n              38.92522904714054\n            ],\n            [\n              -123.77197265625,\n              36.94111143010769\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f80","contributors":{"authors":[{"text":"Goss, Joseph","contributorId":70480,"corporation":false,"usgs":true,"family":"Goss","given":"Joseph","email":"","affiliations":[],"preferred":false,"id":262265,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67253,"text":"i830 - 1974 - Geologic map and sections of the Holy Cross quadrangle, Eagle, Lake, Pitkin, and Summit Counties, Colorado","interactions":[{"subject":{"id":16327,"text":"ofr58105 - 1958 - Geologic map of the southwestern part of the Holy Cross quadrangle, Colorado","indexId":"ofr58105","publicationYear":"1958","noYear":false,"title":"Geologic map of the southwestern part of the Holy Cross quadrangle, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":67253,"text":"i830 - 1974 - Geologic map and sections of the Holy Cross quadrangle, Eagle, Lake, Pitkin, and Summit Counties, Colorado","indexId":"i830","publicationYear":"1974","noYear":false,"title":"Geologic map and sections of the Holy Cross quadrangle, Eagle, Lake, Pitkin, and Summit Counties, Colorado"},"id":1},{"subject":{"id":46742,"text":"ofr71286 - 1971 - Geologic map of the Holy Cross Quadrangle, Eagle, Lake, Pitkin, and Summit counties, Colorado","indexId":"ofr71286","publicationYear":"1971","noYear":false,"title":"Geologic map of the Holy Cross Quadrangle, Eagle, Lake, Pitkin, and Summit counties, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":67253,"text":"i830 - 1974 - Geologic map and sections of the Holy Cross quadrangle, Eagle, Lake, Pitkin, and Summit Counties, Colorado","indexId":"i830","publicationYear":"1974","noYear":false,"title":"Geologic map and sections of the Holy Cross quadrangle, Eagle, Lake, Pitkin, and Summit Counties, Colorado"},"id":2}],"lastModifiedDate":"2022-04-12T20:52:43.881838","indexId":"i830","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"830","title":"Geologic map and sections of the Holy Cross quadrangle, Eagle, Lake, Pitkin, and Summit Counties, Colorado","docAbstract":"This map was first published as a printed edition in 1974. The geologic data have now been captured digitally and are presented here along with images of the printed map sheets. The map encompasses the area of four 7.5-minute quadrangles between 39º15' and 39º 30'N and 106º15' and 106º30'W in the Sawatch and Gore mountain ranges, and upper part of the Arkansas River drainage in central Colorado. The Holy Cross geologic map depicts in detail the complex geology at the north end of the Sawatch Range on the west at its junction with south end of the Gore Range on the east. The ranges are separated in the southern part of the map area by the upper reaches of the Arkansas River, and in the northeast part by the narrow valley of the upper Eagle River.  Sixty map units and numerous individual beds and thin units within the principal map units are shown. Paleoproterozoic and Mesoproterozoic metamorphic rocks are the principal rocks of the Sawatch Range. In the Gore Range, lower and upper Paleozoic sedimentary rocks rest unconformably on the Precambrian metamorphic rocks. Paleozoic rocks that range in age from Upper Cambrian though Middle Pennsylvanian support the Gore Range along the eastern quarter of the map. The sequence includes a basal quartzite overlain by interbedded, shale, dolomite, quartzite, and sandstone. The Leadville Dolomite, below the dark shale, is the host rock for the ore deposits at Leadville and the neighboring lead-zinc-silver districts. A wide range of Miocene to Cretaceous intrusive rocks dip east off the Sawatch Range. The Dry Union Formation of Pliocene and Miocene age fills the valley of the Arkansas River and is covered by Quaternary alluvium and glacial sediment. Glacial deposits of Bull Lake, Pinedale, and neoglacial age are present in many of the mountain valleys.  The geologic structure of the quadrangle is complex in geometry and time with a distinct structural and geographic break along the west front of the Gore Range in the eastern quarter of the quadrangle. In general, Paleozoic strata intruded by Tertiary and Cretaceous irregular linear plutons and sills of the Gore Range are tilted east from the Sawatch Range. These rocks are broken by major normal faults in a complex pattern commonly associated with Paleocene? and Cretaceous intrusive porphyries. In the Sawatch Range, two large Precambrian igneous complexes are separated by a broad shear zone of Precambrian age that extends northwest across the quadrangle and beneath Paleozoic rocks of the Gore Range. Down-to-valley normal faults define the margins of the Arkansas and upper Eagle River valleys.  The Leadville, Sugarloaf, and St. Kevin districts have produced significant amounts of silver. The Homestake mine at the head of West Tennessee Creek produced silver and lead from veins bearing siderite and barite. Scattered veins in shear zones along Homestake Creek are mainly argentiferous galena veins; some are quartz and copper. Veins at Holy Cross City produced gold. Other veins in the area have produced gold, silver, and minor amounts of copper.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i830","usgsCitation":"Tweto, O., and Brandt, T., 1974, Geologic map and sections of the Holy Cross quadrangle, Eagle, Lake, Pitkin, and Summit Counties, Colorado (Originally posted in 1974; Digital edition July 19, 2013): U.S. Geological Survey IMAP 830, Report: 9 p.; 1 Plate: 36.00 x 50.05; Downloads Directory, https://doi.org/10.3133/i830.","productDescription":"Report: 9 p.; 1 Plate: 36.00 x 50.05; Downloads Directory","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":189301,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/i830.gif"},{"id":398599,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9660.htm"},{"id":275187,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/830/downloads/I-830_map.pdf"},{"id":275186,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/830/"},{"id":275188,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/830/downloads/I-830textonly_508.pdf"},{"id":275189,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/imap/830/downloads/"}],"scale":"24000","country":"United States","state":"Colorado","county":"Eagle County. Lake County, Pitkin County, Summit County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.5,39.25 ], [ -106.5,39.5 ], [ -106.25,39.5 ], [ -106.25,39.25 ], [ -106.5,39.25 ] ] ] } } ] }","edition":"Originally posted in 1974; Digital edition July 19, 2013","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db672287","contributors":{"authors":[{"text":"Tweto, Ogden","contributorId":52939,"corporation":false,"usgs":true,"family":"Tweto","given":"Ogden","affiliations":[],"preferred":false,"id":275854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brandt, Theodore R.","contributorId":102336,"corporation":false,"usgs":true,"family":"Brandt","given":"Theodore R.","affiliations":[],"preferred":false,"id":275855,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12427,"text":"ofr741003 - 1974 - Statistical summary of geochemical data furnished by 85 laboratories for for six geochemical exploration reference samples","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr741003","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-1003","title":"Statistical summary of geochemical data furnished by 85 laboratories for for six geochemical exploration reference samples","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr741003","usgsCitation":"Allcott, G., and Lakin, H.W., 1974, Statistical summary of geochemical data furnished by 85 laboratories for for six geochemical exploration reference samples: U.S. Geological Survey Open-File Report 74-1003, 103 p. ;29 cm., https://doi.org/10.3133/ofr741003.","productDescription":"103 p. ;29 cm.","costCenters":[],"links":[{"id":144875,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dce4b07f02db5e1776","contributors":{"authors":[{"text":"Allcott, G.H.","contributorId":94676,"corporation":false,"usgs":true,"family":"Allcott","given":"G.H.","affiliations":[],"preferred":false,"id":166122,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lakin, H. W.","contributorId":11594,"corporation":false,"usgs":true,"family":"Lakin","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":166121,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28391,"text":"wri746 - 1974 - Movement and dispersion of soluble materials in Salem Creek, Muddy Creek, and Yadkin River between Winston-Salem and Salisbury, North Carolina","interactions":[],"lastModifiedDate":"2018-11-16T09:55:04","indexId":"wri746","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-6","title":"Movement and dispersion of soluble materials in Salem Creek, Muddy Creek, and Yadkin River between Winston-Salem and Salisbury, North Carolina","docAbstract":"<p>Wastes entering the Yadkin River from the Winston-Salem area, particularly during heavy rains, resulted in several major fish kills in the late 1960's and early 1970's. The actions undertaken to solve this problem, included the collection of data on the time of travel and dispersion characteristics of the tributaries draining the Winston-Salem area and of the main stem of the Yadkin below their confluence.</p><p>Fluorescent dye was used to simulate the movement of waterborne wastes under four different flow conditions over a reach of about 41 miles (66 kilometers) beginning at the sewage-treatment plant on Salem Creek and ending on the Yadkin River at High Rock Lake near Salisbury. Total travel time for the entire reach ranges from about 28 hours during periods of high streamflow to about 47 hours during periods of low flow. A soluble substance released as a slug at the sewage-treatment plant disperses longitudinally and laterally as it moves downstream. Longitudinal dispersion, expressed as the time required for a substance released as a slug at the sewage-treatment plant to pass a downstream point, ranges from about 8 hours at the upper end of High Rock Lake during periods of high flow to about 15 hours during periods of low flow. The rate of lateral dispersion also depends on the rate of flow of the Yadkin. During high-flow conditions wastes entering the Yadkin from Winston-Salem disperse across the river in a few miles. Under low-flow conditions lateral dispersion is still incomplete more than 10 miles (16 kilometers) downstream.</p><p>Longitudinal dispersion casues the maximum concentrations resulting from slug injections to decrease significantly as the traveltime increases. A relation is presented so the maximum concentration can be estimated at any location downstream from a point of injection at flow rates between about 80 and 500 cubic feet per second (2 and 14 cubic meters per second) at the Muddy Creek gaging station and between about 1,500 and 10,000 cubic feet per second (42 and 280 cubic meters per second) at the Yadkin College gaging station.</p><p>Water entering the Yadkin River from Muddy Creek during low-flow periods does not completely disperse laterally for more than 10 miles (16 kilometers) below the confluence, but, when the Yadkin River discharge is above 5,000 cubic feet per second (140 cubic meters per second), lateral mixing is complete within a few miles below the confluence.</p>","language":"English","publisher":"U. S. Geological Survey","doi":"10.3133/wri746","usgsCitation":"Lindskov, K., 1974, Movement and dispersion of soluble materials in Salem Creek, Muddy Creek, and Yadkin River between Winston-Salem and Salisbury, North Carolina: U.S. Geological Survey Water-Resources Investigations Report 74-6, iv, 26 p., https://doi.org/10.3133/wri746.","productDescription":"iv, 26 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":359496,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159381,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0006/report-thumb.jpg"}],"country":"United States","state":"North Carolina","city":"Salisburg, Winston-Salem","otherGeospatial":"Muddy Creek, Salem Creek, Yadkin River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.1667,\n              35.70693497582502\n            ],\n            [\n              -80.1667,\n              36\n            ],\n            [\n              -80.5,\n              36\n            ],\n            [\n              -80.5,\n              35.70693497582502\n            ],\n            [\n              -80.1667,\n              35.70693497582502\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4802","contributors":{"authors":[{"text":"Lindskov, K.L.","contributorId":91077,"corporation":false,"usgs":true,"family":"Lindskov","given":"K.L.","affiliations":[],"preferred":false,"id":199719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3598,"text":"cir699 - 1974 - Gold in the Black Hills, South Dakota, and how new deposits might be found","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"cir699","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"699","title":"Gold in the Black Hills, South Dakota, and how new deposits might be found","docAbstract":"Of the recorded production of 34,694,552 troy ounces of gold mined in South Dakota through 1971, about 90 percent has come from Precambrian ore bodies in the Homestake mine at Lead in the northern Black Hills. Most of the rest has come from ore deposited in the Deadwood Formation (Cambrian) by hydrothermal replacement during early Tertiary igneous activity. About 99 percent of the total production has been within a radius of 5 miles (8 km) of Lead. Elsewhere, prospecting has been intense, both in the Precambrian rocks, which are exposed over an area 61 by 26 miles (98 by 42 km), and in nearby Paleozoic rocks. \r\n\r\nAll the known ore bodies have been found either at the surface or in subsurface workings of operating mines. Efforts to find totally new deposits have been modest and sporadic; no comprehensive and systematic program has ever been attempted. \r\n\r\nObviously, any exploration program should be aimed at finding a new deposit resembling the Homestake in the Precambrian, but discovery in the Deadwood of a new group of ore bodies containing several hundred thousand ounces of gold would certainly be worthwhile. \r\n\r\nEvidence has long been available that the Deadwood deposits and the Homestake deposit are somehow related. Current opinion is that (1) the Homestake ore is mainly Precambrian, (2) a trivial amount of Homestake ore is Tertiary, (3)gold in Deadwood basal conglomerate is largely of placer origin, and (4) the gold of replacement deposits in the Deadwood and in other rock units came originally from sources similar to the Homestake deposit or its parent materials. \r\n\r\nHomestake ore is virtually entirely contained in a unit of iron-formation locally known as the Homestake Formation, which seemingly had more gold in the original sediments than similar rocks exposed elsewhere in the Black Hills. Gold, sulfur, and other constituents were subsequently concentrated in ore shoots in zones of dilation caused by cross folds that deformed earlier major folds. These ore shoots are in metamorphic rocks of a grade just above the garnet isograd, in a zone where the principal iron-magnesium mineral of the iron-formation changes from a carbonate (sideroplesite) to a silicate (cummingtonite). This metamorphic reaction would release carbon dioxide to the fluid that presumably formed the ore bodies. \r\n\r\nIn short, three controls over localization of the ore have been identified: (1) the cross folds; (2) the so-called Homestake Formation, which passes beneath Paleozoic rocks north of Lead and has not been proved to reappear anywhere else in the Black Hills (Other units of iron-formation less enriched in gold might locally become more like the Homestake Formation beneath the cover of Paleozoic rocks.}; (3} proximity to the garnet isograd--nearly all the exposed Precambrian rocks in the Black Hills are at a metamorphic grade higher than this isograd--and occurrence of this isograd zone mostly beneath Paleozoic rocks. \r\n\r\nIn searching for new deposits, one can guess from existing data where Precambrian rocks of suitable nature may be concealed. The usefulness of such guesses can be increased if they are made with information about the distribution of gold in younger rocks. Gold in the Deadwood basal conglomerate would be the simplest indicator of a deposit once exposed on the pre-Deadwood surface. Tertiary replacement deposits in the Deadwood or other rocks, which obtained their gold from Precambrian sources that may be nearby or far away, can also be helpful; they, like anomalies found by geochemical sampling, at least outline the regions of mineralizing activity. \r\n\r\nA suitable approach to exploration is to make a thorough study of the stratigraphy, the structure, and the metals geochemistry of the Deadwood Formation and associated rocks, chiefly in the northern Black Hills but to a lesser extent elsewhere in localities where the Precambrian geology seems promising and where gold has been found nearby. Such a program, even if it does not yield","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir699","usgsCitation":"Norton, J.J., 1974, Gold in the Black Hills, South Dakota, and how new deposits might be found: U.S. Geological Survey Circular 699, iii, 22 p. :maps ;26 cm., https://doi.org/10.3133/cir699.","productDescription":"iii, 22 p. :maps ;26 cm.","costCenters":[],"links":[{"id":126412,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1974/0699/report-thumb.jpg"},{"id":30631,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1974/0699/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a493d","contributors":{"authors":[{"text":"Norton, James Jennings","contributorId":59412,"corporation":false,"usgs":true,"family":"Norton","given":"James","email":"","middleInitial":"Jennings","affiliations":[],"preferred":false,"id":147232,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56315,"text":"wdrSC731 - 1974 - Water resources data for South Carolina, water year 1973","interactions":[],"lastModifiedDate":"2020-05-12T16:54:45.748533","indexId":"wdrSC731","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"SC-73-1","title":"Water resources data for South Carolina, water year 1973","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrSC731","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for South Carolina, water year 1973: U.S. Geological Survey Water Data Report SC-73-1, x, 210 p. , https://doi.org/10.3133/wdrSC731.","productDescription":"x, 210 p. 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,{"id":61370,"text":"mf626 - 1974 - Faults and their potential hazards in Santa Cruz County, California","interactions":[],"lastModifiedDate":"2025-05-12T17:29:17.497542","indexId":"mf626","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"626","title":"Faults and their potential hazards in Santa Cruz County, California","docAbstract":"<p>This report and map area designed to provide Santa Cruz County with basic data on the location, pattern, recency of movement, potential for future surface rupture, and anticipated earthquake magnitudes and recurrence intervals for several of the faults located there for consideration in the county's land-use planning program and the preparation of its seismic safety element.&nbsp; This report does not consider other seismic hazards such as ground shaking, seismically induced ground failure, or tsunamis (seismically generated sea waves) that can accompany offshore earthquakes of large magnitude.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf626","usgsCitation":"Hall, N.T., Sarna-Wojcicki, A.M., and Dupre, W.R., 1974, Faults and their potential hazards in Santa Cruz County, California: U.S. Geological Survey Miscellaneous Field Studies Map 626, 3 Sheets: 47.81 x 35.67 inches or smaller, https://doi.org/10.3133/mf626.","productDescription":"3 Sheets: 47.81 x 35.67 inches or smaller","costCenters":[],"links":[{"id":485723,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3741.htm","linkFileType":{"id":5,"text":"html"}},{"id":359999,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0626/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359997,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0626/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":186853,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0626/report-thumb.jpg"},{"id":359998,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0626/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"California","county":"Santa Cruz County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.31666666666666,36.85 ], [ -122.31666666666666,37.28333333333333 ], [ -121.58333333333333,37.28333333333333 ], [ -121.58333333333333,36.85 ], [ -122.31666666666666,36.85 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f73b7","contributors":{"authors":[{"text":"Hall, N. Timothy","contributorId":78014,"corporation":false,"usgs":true,"family":"Hall","given":"N.","email":"","middleInitial":"Timothy","affiliations":[],"preferred":false,"id":265528,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sarna-Wojcicki, Andrei M. 0000-0002-0244-9149 asarna@usgs.gov","orcid":"https://orcid.org/0000-0002-0244-9149","contributorId":1046,"corporation":false,"usgs":true,"family":"Sarna-Wojcicki","given":"Andrei","email":"asarna@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":265527,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dupre, William R.","contributorId":80712,"corporation":false,"usgs":true,"family":"Dupre","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":265526,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":6375,"text":"pp782 - 1974 - Geology of the San Francisco North quadrangle, California","interactions":[{"subject":{"id":42241,"text":"ofr54274 - 1954 - Preliminary bedrock-surface map of the San Francisco City area, California","indexId":"ofr54274","publicationYear":"1954","noYear":false,"title":"Preliminary bedrock-surface map of the San Francisco City area, California"},"predicate":"SUPERSEDED_BY","object":{"id":6375,"text":"pp782 - 1974 - Geology of the San Francisco North quadrangle, California","indexId":"pp782","publicationYear":"1974","noYear":false,"title":"Geology of the San Francisco North quadrangle, California"},"id":1}],"lastModifiedDate":"2025-01-10T14:47:54.601025","indexId":"pp782","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"782","title":"Geology of the San Francisco North quadrangle, California","docAbstract":"<p>San Francisco is a heavily built up city in a region of active faults and is subject to earthquakes and landslides. In such an area careful selection of building sites and foundations is imperative. This geologic investigation of the San Francisco North quadrangle was carried out to obtain basic geologic data to aid in construction and other civil engineering problems. The study also contributes to a better understanding of the geology of this part of the Coast Ranges in general and of the Franciscan Formation and surficial deposits in particular.</p><p>On the geologic map (pl. 1) , consolidated rocks are delineated by their composition, age, and origin. Such a classification also gives an approximate indication of the engineering properties of each formation. To make the map more useful to the civil engineer, unconsolidated deposits are shown where thick enough to be depicted. This report and the accompanying map should be a useful guide for planning foundation studies necessary in engineering design.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp782","usgsCitation":"Schlocker, J., 1974, Geology of the San Francisco North quadrangle, California: U.S. Geological Survey Professional Paper 782, Report: vii, 109 p.; 3 Plates: 41.96 x 27.10 inches or smaller, https://doi.org/10.3133/pp782.","productDescription":"Report: vii, 109 p.; 3 Plates: 41.96 x 27.10 inches or smaller","costCenters":[],"links":[{"id":117541,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0782/report-thumb.jpg"},{"id":33748,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0782/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109060,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19768.htm","linkFileType":{"id":5,"text":"html"},"description":"19768"},{"id":465885,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0782/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":465886,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0782/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":465887,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0782/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"California","otherGeospatial":"San Francisco North quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.5,\n              37.758333\n            ],\n            [\n              -122.375,\n              37.758333\n            ],\n            [\n              -122.375,\n              37.875\n            ],\n            [\n              -122.5,\n              37.875\n            ],\n            [\n              -122.5,\n              37.758333\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      },\n      \"id\": 0\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e65b","contributors":{"authors":[{"text":"Schlocker, Julius","contributorId":47357,"corporation":false,"usgs":true,"family":"Schlocker","given":"Julius","email":"","affiliations":[],"preferred":false,"id":152605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36367,"text":"b1313D - 1974 - Use of Dar Zarrouk curves in the interpretation of vertical electrical sounding data","interactions":[],"lastModifiedDate":"2012-02-02T00:09:32","indexId":"b1313D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1313","chapter":"D","title":"Use of Dar Zarrouk curves in the interpretation of vertical electrical sounding data","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1313D","usgsCitation":"Zohdy, A.A., 1974, Use of Dar Zarrouk curves in the interpretation of vertical electrical sounding data: U.S. Geological Survey Bulletin 1313, iv, 41 p. :illus. ;23 cm., https://doi.org/10.3133/b1313D.","productDescription":"iv, 41 p. :illus. ;23 cm.","costCenters":[],"links":[{"id":247659,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1313d/report.pdf","size":"1854","linkFileType":{"id":1,"text":"pdf"}},{"id":247660,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1313d/plate-1.pdf","size":"954","linkFileType":{"id":1,"text":"pdf"}},{"id":252060,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1313d/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6051e9","contributors":{"authors":[{"text":"Zohdy, Adel A. R.","contributorId":61799,"corporation":false,"usgs":true,"family":"Zohdy","given":"Adel","email":"","middleInitial":"A. R.","affiliations":[],"preferred":false,"id":216207,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11184,"text":"ofr77643 - 1974 - Some aspects of remote sensing for consideration in planning for environmental monitoring of the Alyeska Pipeline, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr77643","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"77-643","title":"Some aspects of remote sensing for consideration in planning for environmental monitoring of the Alyeska Pipeline, Alaska","docAbstract":"Remote sensing data were taken along a line surveyed for the building of the Alyeska Pipeline, Alaska, in the winter of 1973-74. The portion considered in this report is the area from the Yukon River south to Isabel Pass in the Alaska Range. \r\n\r\nThe occurrences of aufeis gave the appearance of four rather distinct modes of formation. In the area south of Big Delta, the icings occurred as seepage at the toes of the terraces and along the bottoms of the stream channels cutting into the terraces. In the Yukon-Tanana uplands, the icings occurred generally as seepage at the lowest points in the U-shaped valleys and along the surfaces of the streams in the tributary valleys incised into the rolling hills. The icings formed in the stream channels in both regions have similar hydraulic considerations as do the icings formed in the lower part of the valleys at the toes of the terraces. \r\n\r\nAerial techniques of collecting data by photography and thermal imagery were tested in this setting as a basis for consideration in planning for potential environmental monitoring of the pipeline.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77643","usgsCitation":"Skibitzke, H.E., 1974, Some aspects of remote sensing for consideration in planning for environmental monitoring of the Alyeska Pipeline, Alaska: U.S. Geological Survey Open-File Report 77-643, 32 leaves, 11 fold. ill. :ill., maps ;28 cm.; (33 p., 9 sheets - PGS), https://doi.org/10.3133/ofr77643.","productDescription":"32 leaves, 11 fold. ill. :ill., maps ;28 cm.; (33 p., 9 sheets - PGS)","costCenters":[],"links":[{"id":144517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0643/report-thumb.jpg"},{"id":38951,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0643/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38952,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0643/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38953,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0643/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38954,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0643/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38955,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0643/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38946,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0643/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38947,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0643/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38948,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0643/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38949,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0643/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38950,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0643/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e9e4b07f02db5e94c6","contributors":{"authors":[{"text":"Skibitzke, Herbert E.","contributorId":32142,"corporation":false,"usgs":true,"family":"Skibitzke","given":"Herbert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":162687,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2673,"text":"wsp2031 - 1974 - Influence of recharge basins on the hydrology of Nassau and Suffolk Counties, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp2031","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"2031","title":"Influence of recharge basins on the hydrology of Nassau and Suffolk Counties, Long Island, New York","docAbstract":"An investigation of recharge basins on Long Island was made by the U.S. Geological Survey in cooperation with the New York State Department of Environmental Conservation, Nassau County Department of Public Works, Suffolk County Department of Environmental Control, and Suffolk County Water Authority. The major objectives of the study were to (1) catalog basic physical data on the recharge basins in use on Long Island, (2) measure quality and quantity of precipitation and inflow, (3) measure infiltration rates at selected recharge basins, and (4) evaluate regional effects of recharge basins on the hydrologic system of Long Island. The area of study consists of Nassau and Suffolk Counties -- about 1,370 square miles -- in eastern Long Island, N.Y. \r\n\r\nRecharge basins, numbering more than 2,100 on Long Island in 1969, are open pits in moderately to highly permeable sand and gravel deposits. These pits are used to dispose of storm runoff from residential, industrial, and commercial areas, and from highways, by infiltration of the water through the bottom and sides of the basins. \r\n\r\nThe hydrology of three recharge basins on Long Island -- Westbury, Syosset, and Deer Park basins -- was studied. The precipitation-inflow relation showed that the average percentages of precipitation flowing into each basin were roughly equivalent to the average percentages of impervious areas in the total drainage areas of the basins. Average percentages of precipitation flowing into the basins as direct runoff were 12 percent at the Westbury basin, 10 percent at the Syosset basin, and 7 percent at the Deer Park basin. Numerous open-bottomed storm-water catch basins at Syosset and Deer Park reduced the proportion of inflow to those basins, as compared with the Westbury basin, which has only a few open-bottomed catch basins. \r\n\r\nInflow hydrographs for each basin typify the usual urban runoff hydrograph -- steeply rising and falling limbs, sharp peaks, and short time bases. Unit hydrographs for the Westbury and the Syosset basins are not expected to change; however, the unit hydrograph for the Deer Park basin is expected to broaden somewhat as a result of additional future house construction within the drainage area. \r\n\r\nInfiltration rates averaged 0.9 fph (feet per hour) for 63 storms between July 1967 and May 1970 at the Westbury recharge basin, 0.8 fph for 22 storms from July 1969 to September 1970 at the Syosset recharge basin, and 0.2 fph for 24 storms from March to September 1970 at the Deer Park recharge basin. Low infiltration rates at Deer Park resulted mainly from (1) a high percentage of eroded silt, clay, and organic debris washed in from construction sites in the drainage area, which partly filled the interstices of the natural deposits, and (2) a lack of a well-developed plant-root system on the floor of the younger basin, which would have kept the soil zone more permeable. \r\n\r\nThe apparent rate of movement of storm water through the unsaturated zone below each basin averaged 5.5 fph at Westbury, 3.7 fph at Syosset, and 3.1 fph at Deer Park. The rates of movement for storms during the warm months (April through October) were slightly higher than average, probably because the recharging water was warmer than it was during the rest of the year, and therefore, was slightly less viscous.\r\n\r\nOn the average, a 1-inch rainfall resulted in a peak rise of the water table directly below each basin of 0.5 foot; a 2-inch rainfall resulted in a peak rise of about 2 feet. The mound commonly dissipated within 1 to 4 days at Westbury, 7 days to more than 15 days at Syosset, and 1 to 3 days at Deer Park, depending on the magnitude of the peak buildup. \r\n\r\nAverage annual ground-water recharge was estimated to be 6.4 acre-feet at the Westbury recharge basin, 10.3 acre-feet at the Syosset recharge basin, and 29.6 acre-feet at the Deer Park recharge basin. \r\n\r\nChemical composition of precipitation at Westbury, Syosset, and Deer Park drainage areas was similar: ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2031","usgsCitation":"Seaburn, G., and Aronson, D.A., 1974, Influence of recharge basins on the hydrology of Nassau and Suffolk Counties, Long Island, New York: U.S. Geological Survey Water Supply Paper 2031, vi, 66 p. :ill. (1 fold. in pocket) ;23 cm., https://doi.org/10.3133/wsp2031.","productDescription":"vi, 66 p. :ill. (1 fold. in pocket) ;23 cm.","costCenters":[],"links":[{"id":138260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2031/report-thumb.jpg"},{"id":247234,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2031/plate-1.pdf","size":"1142","linkFileType":{"id":1,"text":"pdf"}},{"id":29023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5ede49","contributors":{"authors":[{"text":"Seaburn, G.E.","contributorId":42193,"corporation":false,"usgs":true,"family":"Seaburn","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":145593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aronson, D. A.","contributorId":20308,"corporation":false,"usgs":true,"family":"Aronson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145592,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66509,"text":"i878 - 1974 - Availability of ground water for irrigation, municipal, or industrial use in the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah","interactions":[],"lastModifiedDate":"2025-08-13T19:30:55.69324","indexId":"i878","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"878","title":"Availability of ground water for irrigation, municipal, or industrial use in the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah","docAbstract":"<p>The Navajo and Hopi Indian reservations are located mainly in northeastern Arizona, although the Navajo Indian reservation extends into northwestern New Mexico and southeastern Utah (see location map). The area of this report coincides with the areas of the Navajo and Hopi Indian reservations except in part of New Mexico, where the areas was extended eastward to longitude 108° and southward to Interstate Highway 40 and in southeastern Utah.</p><p>This investigation was conducted by the U.S. Geological Survey at the request of the Bureau of Indian Affairs. The study was undertaken to evaluate the potential for large-scale ground-water development in the Navajo and Hope Indian Reservations. The results given in this report are intended as preliminary guidelines for the development of ground water in sufficient quantity and of suitable quality for irrigation, municipal, and industrial uses. Data are not included for areas in which less than 25 gal min<sup>-1</sup> (gallons per minute) or 95 l min<sup>-1 </sup>(litres per minute) can be developed.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i878","collaboration":"Prepared in cooperation with the Bureau of Indian Affairs","usgsCitation":"McGavock, E.H., and Edmonds, R.J., 1974, Availability of ground water for irrigation, municipal, or industrial use in the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah: U.S. Geological Survey IMAP 878, 4 Sheets: 48.74 x 34.30 inches or smaller; Cover: 9.15 x 11.92 inches, https://doi.org/10.3133/i878.","productDescription":"4 Sheets: 48.74 x 34.30 inches or smaller; Cover: 9.15 x 11.92 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":494052,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9778.htm","linkFileType":{"id":5,"text":"html"}},{"id":255953,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-2.pdf","text":"Sheet 2: Areas where wells will yield at least 200 gallons per minute","size":"18.36 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":255957,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0878/report-thumb.jpg"},{"id":255956,"rank":2,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/0878/report.pdf","text":"Folio Cover","size":"30 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":255955,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-4.pdf","text":"Sheet 4: Areas where wells will yield at least 25 gallons per minute","size":"14.86 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":255952,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-1.pdf","text":"Sheet 1: Areas where wells will yield at least 500 gallons per minute","size":"19.92 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":255954,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0878/plate-3.pdf","text":"Sheet 3: Areas where wells will yield at least 75 gallons per minute","size":"17.89 MB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"375000","country":"United States","state":"Arizona, New Mexico, Utah","otherGeospatial":"Navajo Indian Reservations, Hopi Indian Reservations","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,35 ], [ -112,37.5 ], [ -108,37.5 ], [ -108,35 ], [ -112,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667eda","contributors":{"authors":[{"text":"McGavock, E. H.","contributorId":40679,"corporation":false,"usgs":true,"family":"McGavock","given":"E.","middleInitial":"H.","affiliations":[],"preferred":false,"id":274633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edmonds, R. J.","contributorId":78825,"corporation":false,"usgs":true,"family":"Edmonds","given":"R.","middleInitial":"J.","affiliations":[],"preferred":false,"id":274634,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30433,"text":"wri7448 - 1974 - Index to maps of flood-prone areas in Indiana","interactions":[],"lastModifiedDate":"2018-10-30T15:06:07","indexId":"wri7448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-48","title":"Index to maps of flood-prone areas in Indiana","docAbstract":"<p>A listing of flood maps for Indiana prepared by the U.S. Geological Survey through 1974 is presented by county. The list provides information on the type of flooding depicted and the reliability of the delineation.</p><p>The list was prepared from a computer file, and an available program allows retrieval of data by land-line location, State and county, and Standard Metropolitan Statistical Area (SMSA). The file will be continuously updated.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7448","usgsCitation":"Weist, W.G., 1974, Index to maps of flood-prone areas in Indiana: U.S. Geological Survey Water-Resources Investigations Report 74-48, 27 p., https://doi.org/10.3133/wri7448.","productDescription":"27 p.","costCenters":[],"links":[{"id":159753,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0048/report-thumb.jpg"},{"id":358978,"rank":2,"type":{"id":11,"text":"Document"},"url":" https://pubs.usgs.gov/wri/1974/0048/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f24dd","contributors":{"authors":[{"text":"Weist, William G. Jr.","contributorId":21527,"corporation":false,"usgs":true,"family":"Weist","given":"William","suffix":"Jr.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42877,"text":"ofr741020 - 1974 - Preliminary potassium-argon age data on volcanic rocks of Long Valley Caldera and vicinity, Mono County, California","interactions":[],"lastModifiedDate":"2025-07-31T20:35:34.185545","indexId":"ofr741020","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-1020","title":"Preliminary potassium-argon age data on volcanic rocks of Long Valley Caldera and vicinity, Mono County, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741020","usgsCitation":"Dalrymple, G.B., and Lanphere, M.A., 1974, Preliminary potassium-argon age data on volcanic rocks of Long Valley Caldera and vicinity, Mono County, California: U.S. Geological Survey Open-File Report 74-1020, Report: 1 p.; 3 Plates: 16.17 x 20.95 inches or smaller, https://doi.org/10.3133/ofr741020.","productDescription":"Report: 1 p.; 3 Plates: 16.17 x 20.95 inches or smaller","costCenters":[],"links":[{"id":80701,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/1020/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80700,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/1020/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80699,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/1020/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":493286,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8844.htm","linkFileType":{"id":5,"text":"html"}},{"id":80702,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/1020/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169153,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/1020/report-thumb.jpg"}],"scale":"65000","country":"United States","state":"California","county":"Mono County","otherGeospatial":"Long Valley Caldera and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.25,\n              38\n            ],\n            [\n              -119.25,\n              37.5\n            ],\n            [\n              -118.75,\n              37.5\n            ],\n            [\n              -118.75,\n              38\n            ],\n            [\n              -119.25,\n              38\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696665","contributors":{"authors":[{"text":"Dalrymple, G. B.","contributorId":10407,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":227313,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lanphere, M. A.","contributorId":35298,"corporation":false,"usgs":true,"family":"Lanphere","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":227314,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66499,"text":"i766M - 1974 - Map showing the thickness of loosely packed sediments and the depth to bedrock in the Sugar House quadrangle, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2022-12-12T21:02:14.211744","indexId":"i766M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"766","chapter":"M","title":"Map showing the thickness of loosely packed sediments and the depth to bedrock in the Sugar House quadrangle, Salt Lake County, Utah","docAbstract":"<p>This map provides information on the location and distribution of three general types of geologic materials in part of Salt Lake County, including the southeastern part of Salt Lake City, Utah. These materials have different physical properties that are pertinent to comprehensive planning and zoning, land-use studies, and engineering usage. The map should be of use in preliminary studies to determine the depth to different &nbsp;general types of foundation material and to determine the potential for settlement of the ground surface during major earthquakes, which could result in damage to waterlines, gaslines, large buildings, and other major engineering structures.</p><p>The lines on the map are generalized. Lines showing the thickness of loosely packed sediments are based on drillers’ logs of 27 water wells in and near the 35-square-mile part of the quadrangle west of the mountains – less than one data point for each square mile. Lines showing the depth to bedrock are based on indirect geophysical data, and the data points are more widely scattered. The map may be useful as a general guide in planning, but investigations by qualified specialists should be made for detailed evaluations of specific areas.</p><p>references to other reports of possible interest to the reader are included at the end of this text.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i766M","usgsCitation":"McGregor, E.E., Van Horn, R., and Arnow, T., 1974, Map showing the thickness of loosely packed sediments and the depth to bedrock in the Sugar House quadrangle, Salt Lake County, Utah: U.S. Geological Survey IMAP 766, Cover : 1 p.; 1 Plate: 40.53 x 27.68 inches, https://doi.org/10.3133/i766M.","productDescription":"Cover : 1 p.; 1 Plate: 40.53 x 27.68 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":410314,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9532.htm","linkFileType":{"id":5,"text":"html"}},{"id":255945,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0766m/report-thumb.jpg"},{"id":255943,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0766m/plate-1.pdf","text":"Map I-766-M","linkFileType":{"id":1,"text":"pdf"}},{"id":255944,"rank":1,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/0766m/report.pdf","text":"Folio Cover","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Utah","county":"Salt Lake County","otherGeospatial":"Sugar House quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.875,40.625 ], [ -111.875,40.75 ], [ -111.75,40.75 ], [ -111.75,40.625 ], [ -111.875,40.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a25c5","contributors":{"authors":[{"text":"McGregor, Edward E.","contributorId":95886,"corporation":false,"usgs":true,"family":"McGregor","given":"Edward","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":274616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Horn, Richard","contributorId":52169,"corporation":false,"usgs":true,"family":"Van Horn","given":"Richard","email":"","affiliations":[],"preferred":false,"id":274617,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":274618,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":67248,"text":"i856A - 1974 - Map showing potential sources of gravel and crushed-rock aggregate in the greater Denver area, Front Range Urban Corridor, Colorado","interactions":[],"lastModifiedDate":"2022-09-20T20:13:14.327141","indexId":"i856A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"856","chapter":"A","title":"Map showing potential sources of gravel and crushed-rock aggregate in the greater Denver area, Front Range Urban Corridor, Colorado","docAbstract":"<p>Gravel and (or) crushed-rock aggregates are essential commodities for urban development, but supplies in many places are exhausted or otherwise eliminated by urban growth. Gravel resources may be exhausted by exploitation, covered by urban spread, or eliminated from production by zoning. this conflict between a growing need and a progressively reduced supply can be forestalled by informed land-use planning. Fundamental to intelligent decisions on land use is knowledge of the physical character, distribution, and quantity of the gravel resources of an area, and of the alternative resource of rock suitable for crushing. This map has been prepared to supply data basic to land-use planning in the&nbsp;<span>Front Range Urban Corridor.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i856A","usgsCitation":"Trimble, D.E., and Fitch, H.R., 1974, Map showing potential sources of gravel and crushed-rock aggregate in the greater Denver area, Front Range Urban Corridor, Colorado: U.S. Geological Survey IMAP 856, Cover sheet: 1 p.; Plate: 44.35 x 37.21 inches, https://doi.org/10.3133/i856A.","productDescription":"Cover sheet: 1 p.; Plate: 44.35 x 37.21 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":407088,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9738.htm","linkFileType":{"id":5,"text":"html"}},{"id":256252,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0856a/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"},{"id":256254,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0856a/report-thumb.jpg"},{"id":256253,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0856a/report.pdf","text":"Cover sheet","linkFileType":{"id":1,"text":"pdf"},"description":"Cover sheet"}],"country":"United States","state":"Colorado","city":"Denver","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.375,\n              39.375\n            ],\n            [\n              -104.625,\n              39.375\n            ],\n            [\n              -104.625,\n              40\n            ],\n            [\n              -105.375,\n              40\n            ],\n            [\n              -105.375,\n              39.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a92e4b07f02db6579a8","contributors":{"authors":[{"text":"Trimble, D. E.","contributorId":11581,"corporation":false,"usgs":true,"family":"Trimble","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":275846,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fitch, H. R.","contributorId":73282,"corporation":false,"usgs":true,"family":"Fitch","given":"H.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":275847,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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