{"pageNumber":"2521","pageRowStart":"63000","pageSize":"25","recordCount":68788,"records":[{"id":70208390,"text":"70208390 - 1967 - Standards for water quality","interactions":[],"lastModifiedDate":"2020-02-06T15:32:41","indexId":"70208390","displayToPublicDate":"1967-04-30T15:29:42","publicationYear":"1967","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Standards for water quality","docAbstract":"

The quality which is necessary depends on the use to which the water will be put. Because uses vary, so also must quality standards. Maintaining any level of quality presents a problem of cost and depends on variations in natural water characteristics, in time and space, and variations in volume and types of wastes. For quality standards appropriate to a given water body, hydrologic network data can provide duration curves of flow, concentrations of dissolved oxygen, dissolved solids, including nutrients (nitrates and phosphates), turbidity, temperature, and other significant chemical, physical, and biological parameters. Standards can then be expressed as occurrences in percentage of time or with respect to flow.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"World petroleum congress proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"World Petroleum Congress","conferenceDate":"Apr 2-9, 1967","conferenceLocation":"Mexico City, Mexico","language":"English","publisher":"Curran Associates","usgsCitation":"Leopold, L., 1967, Standards for water quality, in World petroleum congress proceedings, v. 1967, Mexico City, Mexico, Apr 2-9, 1967, p. 271-275.","productDescription":"5 p.","startPage":"271","endPage":"275","costCenters":[],"links":[{"id":372126,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1967","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Leopold, Luna B.","contributorId":46582,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna B.","affiliations":[],"preferred":false,"id":781699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1001416,"text":"1001416 - 1967 - Stump and tree nesting by mallards and black ducks","interactions":[],"lastModifiedDate":"2025-02-12T16:26:36.899555","indexId":"1001416","displayToPublicDate":"1967-04-03T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Stump and tree nesting by mallards and black ducks","docAbstract":"

Studies conducted 1961-65 at the Montezuma National Wildlife Refuge in New York demonstrated that mallards (Anas platyrhynchos) and black ducks (Anas rubripes) make extensive use of stumps and dead snags for nest sites. Nest densities in timbered habitats compared favorably with those in untimbered habitats. Nest success was generally higher in timbered than in untimbered areas, except for a newly flooded impoundment where nest success was poor. A simple artificial nest structure was used to increase the number of available nest sites in some of the timbered habitats. Development of stump-nesting populations of ducks may furnish a means of increasing waterfowl production in forested areas.

","language":"English","publisher":"Wiley","doi":"10.2307/3798311","usgsCitation":"Cowardin, L.M., Cummings, G., and Reed, P., 1967, Stump and tree nesting by mallards and black ducks: Journal of Wildlife Management, v. 31, no. 2, p. 229-235, https://doi.org/10.2307/3798311.","productDescription":"7 p.","startPage":"229","endPage":"235","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487972,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3798311","text":"Publisher Index Page"},{"id":129254,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Montezuma National Wildlife Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.84477469582741,\n 43.092038474103845\n ],\n [\n -76.84477469582741,\n 42.94214802992465\n ],\n [\n -76.6614374815742,\n 42.94214802992465\n ],\n [\n -76.6614374815742,\n 43.092038474103845\n ],\n [\n -76.84477469582741,\n 43.092038474103845\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"31","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c59","contributors":{"authors":[{"text":"Cowardin, Lewis M.","contributorId":34574,"corporation":false,"usgs":true,"family":"Cowardin","given":"Lewis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":311004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, G.E.","contributorId":69926,"corporation":false,"usgs":true,"family":"Cummings","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":311002,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, P.B. Jr.","contributorId":87892,"corporation":false,"usgs":true,"family":"Reed","given":"P.B.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":311003,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221311,"text":"70221311 - 1967 - Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water","interactions":[],"lastModifiedDate":"2021-06-11T11:51:46.396788","indexId":"70221311","displayToPublicDate":"1967-04-01T12:45:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water","docAbstract":"

The Geological Survey has been the foremost agency in the investigation of ground‐water resources in the United States beginning about 1910. Most of the basic principles of modern ground‐water hydrology were developed in the Survey's program of cooperative investigations. Use of ground water in the United States in 1960 was about 17½ percent of all water uses, excluding water power. The use will probably increase, though at a decreasing rate. Although amount of use may level off, the need to know about it will not. While coordinating its activities with those of the Office of Water Data Coordination and the Office of Water Resources Research, the Survey expects to step up its work in all three areas of data collection, investigations, and research. However, there will be changes of emphasis. Collection of raw data will tend to stress key observation points, and more and more observation of temperature and quality, including contaminants. Investigations will be aimed at upgrading reconnaissance coverage to general coverage for most of the Nation. The areal basis will be stream drainage basins and special hydrologic terranes, rather than political units. There will be an increase in the preparation of analog models for representative ground‐water systems. In research, the problem‐oriented basis will continue. Stress will be on basic principles that pertain to artificial recharge, and the natural recharge and discharge of ground‐water reservoirs; and also on the application of geologic principles on a regional scale. These are critical elements in the management of surface‐water and ground‐water resources conjunctively in river basins.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01244.x","usgsCitation":"Upson, J., 1967, Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water: Groundwater, v. 5, no. 2, p. 13-19, https://doi.org/10.1111/j.1745-6584.1967.tb01244.x.","productDescription":"7 p.","startPage":"13","endPage":"19","costCenters":[],"links":[{"id":386408,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Upson, J. E.","contributorId":49342,"corporation":false,"usgs":true,"family":"Upson","given":"J. E.","affiliations":[],"preferred":false,"id":817408,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221310,"text":"70221310 - 1967 - Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water","interactions":[],"lastModifiedDate":"2021-06-09T17:49:06.328407","indexId":"70221310","displayToPublicDate":"1967-04-01T12:45:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water","docAbstract":"

The Geological Survey has been the foremost agency in the investigation of ground‐water resources in the United States beginning about 1910. Most of the basic principles of modern ground‐water hydrology were developed in the Survey's program of cooperative investigations. Use of ground water in the United States in 1960 was about 17½ percent of all water uses, excluding water power. The use will probably increase, though at a decreasing rate. Although amount of use may level off, the need to know about it will not. While coordinating its activities with those of the Office of Water Data Coordination and the Office of Water Resources Research, the Survey expects to step up its work in all three areas of data collection, investigations, and research. However, there will be changes of emphasis. Collection of raw data will tend to stress key observation points, and more and more observation of temperature and quality, including contaminants. Investigations will be aimed at upgrading reconnaissance coverage to general coverage for most of the Nation. The areal basis will be stream drainage basins and special hydrologic terranes, rather than political units. There will be an increase in the preparation of analog models for representative ground‐water systems. In research, the problem‐oriented basis will continue. Stress will be on basic principles that pertain to artificial recharge, and the natural recharge and discharge of ground‐water reservoirs; and also on the application of geologic principles on a regional scale. These are critical elements in the management of surface‐water and ground‐water resources conjunctively in river basins.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01244.x","usgsCitation":"Upson, J., 1967, Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water: Groundwater, v. 5, no. 2, p. 13-19, https://doi.org/10.1111/j.1745-6584.1967.tb01244.x.","productDescription":"7 p.","startPage":"13","endPage":"19","costCenters":[],"links":[{"id":386357,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Upson, J. E.","contributorId":49342,"corporation":false,"usgs":true,"family":"Upson","given":"J. E.","affiliations":[],"preferred":false,"id":817287,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221352,"text":"70221352 - 1967 - The cone of depression and its use in solving water problems","interactions":[],"lastModifiedDate":"2021-06-11T12:55:49.318001","indexId":"70221352","displayToPublicDate":"1967-04-01T07:51:58","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"The cone of depression and its use in solving water problems","docAbstract":"

No abstract available. 

","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1967.tb01242.x","usgsCitation":"Schaefer, E.J., 1967, The cone of depression and its use in solving water problems: Groundwater, v. 5, no. 2, p. 2-4, https://doi.org/10.1111/j.1745-6584.1967.tb01242.x.","productDescription":"3 p.","startPage":"2","endPage":"4","costCenters":[],"links":[{"id":480345,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1745-6584.1967.tb01242.x","text":"Publisher Index Page"},{"id":386414,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Schaefer, Edward J.","contributorId":260170,"corporation":false,"usgs":false,"family":"Schaefer","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":817411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70196181,"text":"70196181 - 1967 - Artificial Recharge at Valley City, North Dakota, 1932 to 1965","interactions":[],"lastModifiedDate":"2018-03-22T14:07:24","indexId":"70196181","displayToPublicDate":"1967-04-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Artificial Recharge at Valley City, North Dakota, 1932 to 1965","docAbstract":"

Valley City, North Dakota, has an average daily water use of 750,000 gallons, which is obtained from wells tapping pattly confined gravel deposits in the Sheyenne River valley. These deposits at Valley City have a maximum thickness of more than 50 feet and an areal extent of approximately 1 square mile. The aquifer has been artificially recharged successfully since 1932 by diversion of water from the Sheyenne River to an abandoned gravel pit. During this time the piezometric surface in the aquifer has been raised more than 22 feet.

Prior to 1958, the recharge system was operated from January until June; however, when the piezometric surface rose to within about 8 feet of the surface, the recharge operation was discontinued. Between June and January the piezometric surface declined as ground water was withdrawn. During the recharge‐discharge cycle, the average annual fluctuation of the piezometric surface was 10 feet, amounting to a change in storage of about 1,000 acre‐feet of water. Since 1958, the recharge system has been operated throughout the year. There has been a gradual improvement in the quality of the water in the aquifer since the installation of the recharge system.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01245.x","usgsCitation":"Kelly, T.E., 1967, Artificial Recharge at Valley City, North Dakota, 1932 to 1965: Groundwater, v. 5, no. 2, p. 20-25, https://doi.org/10.1111/j.1745-6584.1967.tb01245.x.","productDescription":"6 p.","startPage":"20","endPage":"25","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352739,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","city":"Valley City","volume":"5","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","scienceBaseUri":"5aff5ed3e4b0da30c1bfdda9","contributors":{"authors":[{"text":"Kelly, T. E.","contributorId":63824,"corporation":false,"usgs":true,"family":"Kelly","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":731561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047453,"text":"70047453 - 1967 - Temperature and water-quality conditions for the period July 1963 to December 1965, Patuxent River Estuary, Maryland","interactions":[],"lastModifiedDate":"2013-09-19T13:13:44","indexId":"70047453","displayToPublicDate":"1967-01-06T13:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Temperature and water-quality conditions for the period July 1963 to December 1965, Patuxent River Estuary, Maryland","docAbstract":"Graphs and tables obtained from continuous records of surface-water temperature from five stations for the period july 1963 through December 1965 and of surface, salinity, dissolved oxygen, turbidity, tide-stage, wind data and bottom temperature from a single station are presented herein. Effects of powerplant cooling water on water temperature were obvious at a station near the plant's discharge point. Surface-water density at the Patuxent River Bridge varied from 1.0033 to 1.0127 with least change during the period May to September. Salinity ranged from 3 to 16.5 parts per thousand. Average salinity in the spring of 1965 was double that of spring 1964. Turbidity was high during the winter, and peak values were obtained during prolonged periods of high wind velocities. Dissolved oxygen values ranged from 386 to 15.0 parts per million, and percentage saturation of oxygen from 49 to 144 percent. The extreme tidal range was 5.7 feet; mean water levels were highest in summer and lowest in winter and spring.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","doi":"10.3133/70047453","usgsCitation":"Cory, R.L., and Nauman, J.W., 1967, Temperature and water-quality conditions for the period July 1963 to December 1965, Patuxent River Estuary, Maryland: Open-File Report, 72 p., https://doi.org/10.3133/70047453.","productDescription":"72 p.","numberOfPages":"83","costCenters":[],"links":[{"id":277876,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047453/report.pdf"},{"id":276130,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047453/report-thumb.jpg"}],"country":"United States","state":"Maryl","otherGeospatial":"Patuxent River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.709290,38.300176 ], [ -76.709290,38.638327 ], [ -76.389313,38.638327 ], [ -76.389313,38.300176 ], [ -76.709290,38.300176 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae9e4b0e21cafa49c97","contributors":{"authors":[{"text":"Cory, Robert L.","contributorId":77967,"corporation":false,"usgs":true,"family":"Cory","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":482070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nauman, Jon W.","contributorId":56232,"corporation":false,"usgs":true,"family":"Nauman","given":"Jon","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":482069,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70039370,"text":"70039370 - 1967 - Prospecting for gold in the United States","interactions":[],"lastModifiedDate":"2012-08-04T01:01:57","indexId":"70039370","displayToPublicDate":"1967-01-02T09:46:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Prospecting for gold in the United States","docAbstract":"Prospecting for gold is something that probably everyone dreams of trying at least once. To the person who is mainly concerned with this activity as a vacation diversion, prospecting offers a special excitement. There is a constant hope that the next pan of sediment may be \"pay dirt,\" and no other thrill can compare with that experienced when one sees even a few tiny flecks of gold glittering in the black sand at the bottom of his pan. The search itself is its own reward for the efforts expended by the vacation prospector. The would-be prospector hoping for financial gain, however, should carefully consider all the facts of the situation before deciding to set out on a prospecting expedition.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039370","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Prospecting for gold in the United States: General Information Product, 15 p., https://doi.org/10.3133/70039370.","productDescription":"15 p.","numberOfPages":"16","costCenters":[],"links":[{"id":261508,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039370/report.pdf"},{"id":261509,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039370/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8f50e4b0c8380cd7f6b5","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":535277,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70110392,"text":"wdrIN661 - 1967 - Water resources data for Indiana, 1966","interactions":[],"lastModifiedDate":"2014-06-11T09:46:03","indexId":"wdrIN661","displayToPublicDate":"1967-01-01T14:01:45","publicationYear":"1967","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":"IN-66-1","title":"Water resources data for Indiana, 1966","docAbstract":"

The surface-water records for the 1966 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering states.

\n
\n

The quality-of-water investigations of the U.S. Geological Survey are concerned with the chemical and physical characteristics of surface- and ground-water supplies of the Nation. The basic records for the 1966 water year for quality of surface waters within the State of Indiana are given in this report. For convenience and interest, there are also records for a few water quality stations in bordering states.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrIN661","collaboration":"Prepared in cooperation with Indiana Department of Natural Resources; Indiana State Board of Health; Indiana State Highway Commission; Corps of Engineers, U.S. Army","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Water resources data for Indiana, 1966: U.S. Geological Survey Water Data Report IN-66-1, viii, 252 p., https://doi.org/10.3133/wdrIN661.","productDescription":"viii, 252 p.","numberOfPages":"266","temporalStart":"1965-10-01","temporalEnd":"1966-09-30","costCenters":[],"links":[{"id":288276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288275,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/in-66-1/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"538052d2e4b0826cd5016a66","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":535660,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70114650,"text":"70114650 - 1967 - Results of the second phase of the drought-disaster test-drilling program near Morristown, N.J.","interactions":[],"lastModifiedDate":"2018-01-08T18:31:02","indexId":"70114650","displayToPublicDate":"1967-01-01T13:17:37","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":149,"text":"New Jersey Division of Water Policy and Supply Water Resources Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"17","title":"Results of the second phase of the drought-disaster test-drilling program near Morristown, N.J.","docAbstract":"

The continued drought in northeastern New Jersey through the summer of 1966 with its attendant water-supply problems resulted in an extension of the drought-disaster test-drilling program originally requested by the Office of Emergency Planning on August 30, 1965. Authorization to continue test drilling was fiven by the Office of Emergency Planning on September 26, 1966, with the stipulation that all field work be complete by January 31, 1977. Contractural costs were paid by the Office of Emergency Planning, whereas personnel costs were shared by the U.S. Geological Survey and the New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply.

The work undertaken in 1965 by the Geological Survey was \"...to preform the necessary drilling and testing of wells to identify the extent and nature of a reserve ground-water source in the vicinity of the Passaic River near the northern New Jersey metropolitan area.\" Results of this first phase were made available in the fall of 1966 in Water Resources Circular 16 of the New Jersey Department of Conservation and Economic Development. Three of the five areas tested (figure 1)--two in Parsippany-Troy Hills Township (areas 2 and 4) and one in East Hanover Township (area 1), Morris County--proved capable of providing an aggregate sustained yield of 7.5 million gallons daily (mgd) from wells constructed in sand and gravel deposits. Because significant supplies of ground water for emergency use were located in the first phase of the exploratory test-drilling program, it was though desirable to extend the originally planned studies so as to obtain maximum practicable information on emergency supplies.

During this second phase of the investigation, drilling was conducted in 16 sites in Chatham, Madison, and Florham Park Boroughs and in Hanover and East Hanover Townships, Morris County. (See figure 2.) The drilling in Hanover and East Hanover Townships, and part of the drilling done in Florham Park was to explore the availability of large undeveloped ground-water supplies. Drilling in Chatham, Madison, and Florham Park Boroughs was done primarily to determine the extent and continuity of buried valley-fill aquifers, so that a full evaluation of the effects of pumpage from other areas on these already heavily pumped areas could be made. In addition, it was anticipated that the drilling could help in defining the feasibility of artificial recharge of the heavily pumped areas and in the determination of the prospective method of recharge and points of emplacement.

Arrangements for easements with landowners, preparation of specifications for well drilling and seismic work, and supervision of well drilling and seismic contracts were all performed by the New Jersey District, Water Resources Division of the Geological Survey.

Prior to the test drilling, seismic exploration under contract with Alpine Geophysical Associates of Norwood, N. J. was conducted at five locations in the Chatham-Madison-Florham Park area and at one place in Parsippany-Troy Hills Township. The seismic work was done to determine the most favorable location for a test well at several potential test-well sites and to help in the interpretation of subsurface geology between test sites.

Contracts for the drilling of the test holes were awarded during November and drilling commences on November 30. Kaye Well drilling, Inc. of Jackson, N. J. was the recipient of a contract for eight of the test holes, and a second contract was awarded to Rinbrand Well Drilling Co., Inc. of Glen Rock, N. J.--also for eight test holes.

Acknowledgment is due to the many public officials of Chatham, Madison, Florham Park, Morristown, and East Hanover Township as well as officials of the Braidburn Corporation and Esso Research and Engineering Co., who cooperated by making their lands available for exploration.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Trenton, NJ","collaboration":"Prepared by the State of New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply, in cooperation with United States Department of the Interior Geological Survey","usgsCitation":"Vecchioli, J., Nichols, W., and Nemickas, B., 1967, Results of the second phase of the drought-disaster test-drilling program near Morristown, N.J.: New Jersey Division of Water Policy and Supply Water Resources Circular 17, Report: v, 23 p.; 3 Plates: 34.65 x 21.48 inches or smaller.","productDescription":"Report: v, 23 p.; 3 Plates: 34.65 x 21.48 inches or smaller","numberOfPages":"30","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":290164,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327417,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70114650/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":327415,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70114650/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":327416,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70114650/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":290163,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114650/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey","city":"Morristown","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.501444,40.780231 ], [ -74.501444,40.818361 ], [ -74.456181,40.818361 ], [ -74.456181,40.780231 ], [ -74.501444,40.780231 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ad40f9e4b0729c154181d6","contributors":{"authors":[{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":495394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nichols, William D.","contributorId":98296,"corporation":false,"usgs":true,"family":"Nichols","given":"William D.","affiliations":[],"preferred":false,"id":495395,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nemickas, Bronius","contributorId":105733,"corporation":false,"usgs":true,"family":"Nemickas","given":"Bronius","email":"","affiliations":[],"preferred":false,"id":495396,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70039249,"text":"70039249 - 1967 - Mountains and plains Denver's geologic setting","interactions":[],"lastModifiedDate":"2012-08-03T01:02:04","indexId":"70039249","displayToPublicDate":"1967-01-01T13:01:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Mountains and plains Denver's geologic setting","docAbstract":"A slice of geologic history is exposed to view in the Denver, Colorado area. Denver is situated on the High Plains near the east front of the Rocky Mountains. As one travels westward from Denver toward the mountains, successively older rocks are crossed from the geologically young rocks of the High Plains and the South Platte River valley to the older rocks of the foothills and the ancient rocks of the mountains. Thus, within a few miles,the journey turns back the pages of time in a lifesized textbook that vividly illustrates the geologic events that shaped the landscape.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039249","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Mountains and plains Denver's geologic setting: General Information Product, 23 p., https://doi.org/10.3133/70039249.","productDescription":"23 p.","numberOfPages":"24","costCenters":[],"links":[{"id":261472,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039249/report.pdf"},{"id":261473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039249/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Denver","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.25,38.833333333333336 ], [ -106.25,40.583333333333336 ], [ -103.5,40.583333333333336 ], [ -103.5,38.833333333333336 ], [ -106.25,38.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ebae4b0c8380cd70c33","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":535271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221309,"text":"70221309 - 1967 - An electrical analog study of the geometry of limestone solution","interactions":[],"lastModifiedDate":"2021-06-09T17:42:25.755466","indexId":"70221309","displayToPublicDate":"1967-01-01T12:38:36","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"An electrical analog study of the geometry of limestone solution","docAbstract":"

This study of the geometry of limestone solution is based on the following conditions: (1) the limestone is impermeable but contains and transmits water in joints, fractures, bedding‐plane partings, and solution channels; (2) at depth, the limestone aquifer is underlain by impermeable rock; (3) ground water in the limestone is under water‐table conditions; (4) recharge to the limestone is by infiltration of precipitation through the overlying rock to the zone of saturation; (5) discharge from the aquifer is by seeps and springs; and (6) ground water dissolves the limestone through which it flows, continuously modifying the flow pattern and the hydrologic properties of the medium. These conditions commonly are found in limestone terranes in the eastern and central United States. An electrical analog was constructed conforming to this description of the ground‐water flow system and has been used to define the pattern, velocity, and density of ground‐water flow and the relative length of time of contact of water with the aquifer. Successive models are used to illustrate progressive limestone solution and changes in ground‐water flow in the aquifer. The initial analog indicates a strongly convex water table with the greatest density of flow at shallow depths beneath the water table near the point of discharge. Successive models indicate greater concentration of flow near and on the level of ground‐water discharge, an overall lowering of the water table, and a pronounced flattening of the water table near the discharge point. Results of the analog study support the following conclusions: (1) The most active zone of solution is at shallow depths beneath the water table and near the point of ground‐water discharge. Consequently, the size of channels generally decreases with depth and increases with proximity to the point of ground‐water discharge. (2) Generally, solution channels have a greater lateral than vertical extent.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01235.x","usgsCitation":"Bedinger, M.S., 1967, An electrical analog study of the geometry of limestone solution: Groundwater, v. 59, no. 12, p. 24-24, https://doi.org/10.1111/j.1745-6584.1967.tb01235.x.","productDescription":"1 p.","startPage":"24","endPage":"24","costCenters":[],"links":[{"id":386356,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"12","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":817286,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25259,"text":"25259 - 1967 - Water quality at Patuxent River Bridge, MD","interactions":[],"lastModifiedDate":"2014-08-01T11:54:03","indexId":"25259","displayToPublicDate":"1967-01-01T11:50:02","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesNumber":"C819t","title":"Water quality at Patuxent River Bridge, MD","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","doi":"10.3133/25259","issn":"0364-7064","usgsCitation":"Cory, R.L., and Nauman, J.W., 1967, Water quality at Patuxent River Bridge, MD, https://doi.org/10.3133/25259.","costCenters":[],"links":[{"id":291521,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Maryl","city":"Patuxent","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.763695,38.531239 ], [ -76.763695,38.548694 ], [ -76.731681,38.548694 ], [ -76.731681,38.531239 ], [ -76.763695,38.531239 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53dca9cfe4b07615786377ac","contributors":{"authors":[{"text":"Cory, Robert L.","contributorId":77967,"corporation":false,"usgs":true,"family":"Cory","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":193355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nauman, Jon W.","contributorId":56232,"corporation":false,"usgs":true,"family":"Nauman","given":"Jon","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":193354,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70170953,"text":"70170953 - 1967 - Geochemistry and ground-water movement in northwestern Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T10:00:51","indexId":"70170953","displayToPublicDate":"1967-01-01T11:15:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry and ground-water movement in northwestern Minnesota","docAbstract":"

The relation between water quality and water movement within the ground-water reservoir may be better understood if studies of flow systems are used in conjunction with hydrochemical methods. Within small watersheds, local, intermediate, and regional flow systems may develop, depending upon the shape, the relief, and the thickness of the ground-water reservoir. Lateral and vertical variations of water quality in the ground-water reservoir reflect the difference in length of flow paths within a system. The relative ion concentration of the major ions in solution in ground waters change as water moves from recharge areas to discharge areas. These changes are used to interpret the direction and rate of ground-water movement.

\n

Ground-water types mapped in the Two Rivers watershed of northwestern Minnesota indicate that calcium bicarbonate type water occurs near the source of recharge and progressively changes to the sulfate type as water moves downgradient toward the discharge area. Local recharge areas are indicated by the greater penetration of calcium bicarbonate waters into the ground-water reservoir. The calcrum bicarbonate type water of surface streams during low flow indicates that water moves into the stream from the upper part of the ground-water reservoir. Chloride type water moves from the Paleozoic rocks and mixes with water in the glacial drift probably at places where permeable zones in the Paleozoic rocks are in contact with the overlying drift.

","language":"English","publisher":"National Groundwater Association","publisherLocation":"Herndon, VA","doi":"10.1111/j.1745-6584.1967.tb01233.x","usgsCitation":"Maclay, R., and Winter, T.C., 1967, Geochemistry and ground-water movement in northwestern Minnesota: Groundwater, v. 5, no. 1, p. 11-19, https://doi.org/10.1111/j.1745-6584.1967.tb01233.x.","productDescription":"9 p.","startPage":"11","endPage":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321174,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","volume":"5","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","scienceBaseUri":"5735a938e4b0dae0d5df5115","contributors":{"authors":[{"text":"Maclay, R.W.","contributorId":72804,"corporation":false,"usgs":true,"family":"Maclay","given":"R.W.","affiliations":[],"preferred":false,"id":629203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winter, T. C.","contributorId":23485,"corporation":false,"usgs":true,"family":"Winter","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":629204,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70270905,"text":"70270905 - 1967 - Water resources of the Guanica area, Puerto Rico: A preliminary appraisal, 1963","interactions":[],"lastModifiedDate":"2025-08-29T14:38:32.636793","indexId":"70270905","displayToPublicDate":"1967-01-01T10:37:37","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources of the Guanica area, Puerto Rico: A preliminary appraisal, 1963","docAbstract":"

Guánica and the lower Rio Loco valley lie between the extensive agricultural development in Lajas Valley to the west and the industrial development at Guayanilla to the east. Having a protected deep-water port, the Guánica area is particularly well suited to further development. The economic growth of the area depends, in important degree, on the amount of water available-water in the immediate area or water to be brought in from other areas.

The purpose of the study of the Guánica area was to evaluate the water supply in the immediate area. How much water is there? How much water moves through the area and what are the factors that control the movement? What is the composition of the water? And how much more water can be used?

The study itself took one year. Active data collection included measurements of streamflow, measurements of water levels in wells, measurements of well discharge, chemical analyses of surface and ground water, geologic reconnaissance, and considerable interviewing. Information for more than one year was obtained for rainfall and other weather data, well pumpage, water leaving Lago loco, and water used by the Southwestern Puerto Rico project.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70270905","collaboration":"In cooperation with the Commonwealth of Puerto Rico","usgsCitation":"McClymonds, N.E., 1967, Water resources of the Guanica area, Puerto Rico: A preliminary appraisal, 1963, Report: 43 p.; 2 Figures: 13.90 x 22.82 inches and 13.89 x 8.24 inches, https://doi.org/10.3133/70270905.","productDescription":"Report: 43 p.; 2 Figures: 13.90 x 22.82 inches and 13.89 x 8.24 inches","costCenters":[],"links":[{"id":495081,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70270905/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":495080,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70270905/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":495082,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70270905/figure-7.pdf","text":"Figure 7","linkFileType":{"id":1,"text":"pdf"}},{"id":495079,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70270905/report-thumb.jpg"}],"country":"Puerto Rico","city":"Guanica","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -67.41782863900221,\n 18.61812040597721\n ],\n [\n -67.41782863900221,\n 17.80333089063508\n ],\n [\n -65.56416750050371,\n 17.80333089063508\n ],\n [\n -65.56416750050371,\n 18.61812040597721\n ],\n [\n -67.41782863900221,\n 18.61812040597721\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McClymonds, Neal E.","contributorId":360640,"corporation":false,"usgs":false,"family":"McClymonds","given":"Neal","middleInitial":"E.","affiliations":[],"preferred":false,"id":947337,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2000010,"text":"2000010 - 1967 - Physical limnology of Saginaw Bay, Lake Huron","interactions":[],"lastModifiedDate":"2012-02-02T00:15:00","indexId":"2000010","displayToPublicDate":"1967-01-01T01:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"12","title":"Physical limnology of Saginaw Bay, Lake Huron","docAbstract":"Water temperature and the distribution of various chemicals measured during surveys from June 7 to October 30, 1956, reflect a highly variable and rapidly changing circulation in Saginaw Bay, Lake Huron. The circulation is influenced strongly by local winds and by the stronger circulation of Lake Huron which frequently causes injections of lake water to the inner extremity of the bay. The circulation patterns determined at six times during 1956 reflect the general characteristics of a marine estuary of the northern hemisphere. The prevailing circulation was counterclockwise; the higher concentrations of solutes from the Saginaw River tended to flow and enter Lake Huron along the south shore; water from Lake Huron entered the northeast section of the bay and had a dominant influence on the water along the north shore of the bay.\nThe concentrations of major ions varied little with depth, but a decrease from the inner bay toward Lake Huron reflected the dilution of Saginaw River water as it moved out of the bay. Concentrations in the outer bay were not much greater than in Lake Huron proper. The proportions of various cations and anions were similar to the average proportions for the freshwaters of the world.\nThe average flushing time was 186 days, but was 113 days during the period of peak river discharge. The lakeward transport of Saginaw River water ranged from 619 to 2,294 feet per day in the inner bay to 1,410 to 3,000 feet per day in the outer bay on June 7 and October 30, respectively.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"Beeton, A.M., Smith, S.H., and Hooper, F.F., 1967, Physical limnology of Saginaw Bay, Lake Huron: Technical Report 12, 56 p.","productDescription":"56 p.","startPage":"0","endPage":"56","numberOfPages":"56","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92062,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr12.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685b43","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":324922,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":324921,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hooper, Frank F.","contributorId":97847,"corporation":false,"usgs":true,"family":"Hooper","given":"Frank","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":324923,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70156254,"text":"70156254 - 1967 - Devonian of the Northern Rocky Mountains and plains","interactions":[],"lastModifiedDate":"2015-08-17T12:47:04","indexId":"70156254","displayToPublicDate":"1967-01-01T01:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Devonian of the Northern Rocky Mountains and plains","docAbstract":"

The Devonian System, represented predominantly by shallow-water marine carbonate, is widespread in Montana, Wyoming, eastern Idaho, North Dakota, South Dakota, and northwestern Nebraska. It comprises cratonic rocks in the east and miogeosynclinal rocks in the west.

\n

The cratonic rocks thicken generally northward from their southern limit in Wyoming across a broad shelf that occupies most of Wyoming and Montana. In northern Montana, they are as much as 1,250 feet thick. Cratonic rocks also thicken eastward from areas of Early Mississippian erosional thinning in central and eastern Montana to as much as 2,000 feet in the intracratonic Williston basin centered in northwestern North Dakota.

\n

The miogeosynclinal rocks, which moved eastward on low-angle thrust faults, abut against cratonic rocks along a north-trending disturbed belt in western Wyoming, western Montana and eastern Idaho. The miogeosynclinal rocks thicken abruptly westward from 1,000 feet near this belt to about 3,000 feet near the east edge of the Idaho batholith. Farther west they have been buried beneath younger rocks, altered by the batholith, or eroded.

\n

Five subdivisions of the Devonian System are treated separately:

\n

1. Upper Lower Devonian (Coblenzian) marginal and nearshore marine carbonate rocks and related continental and estuarine discontinuous sinkhole and channel-fill deposits.

\n

2. Upper Middle Devonian (Givetian) carbonate rocks that contain a 525-foot-thick evaporitic sequence in the Williston basin.

\n

3. Lower Upper Devonian (Frasnian, toI) cyclically deposited carbonate rocks that include thick beds of dolarenite and dolomitized calcarenite on the west.

\n

4. Upper Upper Devonian (Famennian, toII-IV) evaporitic rocks overlain by fossilferous open-marine shale and limestone.

\n

5. Undivided uppermost Devonian (Famennian, to V-VI) and lowermost Mississippian (Tournaisian, cuI-lower cuIIα) carbonaceous and clastic rocks deposited in six shallow basins interspersed among areas uplifted during the penecontemporaneous Antler orogeny.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"International symposium on the Devonian system","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"International symposium on the Devonian system","conferenceLocation":"Calgary, Alberta, Canada","language":"English","publisher":"Alberta Society of Petroleum Geologists","publisherLocation":"Calgary, Alberta","usgsCitation":"Sandberg, C.A., and Mapel, W., 1967, Devonian of the Northern Rocky Mountains and plains, in International symposium on the Devonian system, v. I, Calgary, Alberta, Canada, p. 843-877.","productDescription":"35 p.","startPage":"843","endPage":"877","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":306804,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho, Montana, Nebraska, North Dakota, South Dakota, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.83984375,\n 41.83682786072714\n ],\n [\n -115.83984375,\n 49.210420445650286\n ],\n [\n -96.240234375,\n 49.210420445650286\n ],\n [\n -96.240234375,\n 41.83682786072714\n ],\n [\n -115.83984375,\n 41.83682786072714\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"I","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d305b1e4b0518e35468ceb","contributors":{"authors":[{"text":"Sandberg, Charles A. sandberg@usgs.gov","contributorId":2362,"corporation":false,"usgs":true,"family":"Sandberg","given":"Charles","email":"sandberg@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":568253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mapel, William J.","contributorId":89796,"corporation":false,"usgs":true,"family":"Mapel","given":"William J.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":568254,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2198,"text":"wsp1832 - 1967 - Hydrology of the Valley-fill and carbonate-rock reservoirs, Pahrump Valley, Nevada-California","interactions":[],"lastModifiedDate":"2023-03-14T20:27:11.946442","indexId":"wsp1832","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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":"1832","title":"Hydrology of the Valley-fill and carbonate-rock reservoirs, Pahrump Valley, Nevada-California","docAbstract":"This is the second appraisal of the water supply of Pahrump Valley, made 15 years after the first cooperative study. In the first report the average recharge was estimated to be 23,000 acre-feet per year, only 1,000 acre-feet more than the estimate made in this report. All this recharge was considered to be available for development. Because of the difficulty in salvaging the subsurface outflow from the deep carbonate-rock reservoir, this report concludes that the perennial yield may be only 25,000 acre-feet. \r\n\r\nIn 1875, Bennetts and Manse Springs reportedly discharged a total of nearly 10,000 acre-feet of water from the valley-fill reservoir. After the construction of several flowing wells in 1910, the spring discharge began to decline. In the mid-1940's many irrigation wells were drilled, and large-capacity pumps were installed. During the 4-year period of this study (1959-62), the net pumping draft averaged about 25,000 acre-feet per year, or about twice the estimated yield. In 1962 Bennetts Spring was dry, and the discharge from Marse Spring was only 1,400 acre-feet. \r\n\r\nDuring the period February 1959-February 1962, pumping caused an estimated storage depletion of 45,000 acre-feet, or 15,000 acre-feet per year. If the overdraft is maintained, depletion of stored water will continue and pumping costs will increase. Water levels in the vicinity of the Pahrump, Manse, and Fowler Ranches declined more than ]0 feet in response to the pumping during this period, and they can be expected to continue to decline at ,the projected rate of more than 3 feet per year. \r\n\r\nThe chemical quality of the pumped water has been satisfactory for irrigation and domestic use. Recycling of water pumped or irrigation, however, could result in deterioration of the water quality with time.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1832","usgsCitation":"Malmberg, G.T., 1967, Hydrology of the Valley-fill and carbonate-rock reservoirs, Pahrump Valley, Nevada-California: U.S. Geological Survey Water Supply Paper 1832, iv, 47 p., https://doi.org/10.3133/wsp1832.","productDescription":"iv, 47 p.","costCenters":[],"links":[{"id":414133,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25037.htm","linkFileType":{"id":5,"text":"html"}},{"id":27854,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1832/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138285,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1832/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Pahrump Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116.25,\n 36.467\n ],\n [\n -116.25,\n 35.617\n ],\n [\n -115.517,\n 35.617\n ],\n [\n -115.517,\n 36.467\n ],\n [\n -116.25,\n 36.467\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca1e","contributors":{"authors":[{"text":"Malmberg, Glenn T.","contributorId":11196,"corporation":false,"usgs":true,"family":"Malmberg","given":"Glenn","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":144812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000348,"text":"1000348 - 1967 - Growth of lake trout in Lake Superior before the maximum abundance of sea lampreys","interactions":[],"lastModifiedDate":"2012-02-02T00:04:41","indexId":"1000348","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Growth of lake trout in Lake Superior before the maximum abundance of sea lampreys","docAbstract":"The growth in length of lake trout (Salvelinus namaycush) from the inshore water of Lake Superior in 1953 increased with age from the 3rd to 9th year, and was nearly constant from the 9th to the 12th year. Growth was greatest in the 1st year (4.0 inches) and least in the 2nd and 3rd years (2.3 inches). Between the 4th and 9th years the increments increased from 2.6 to 3.5 inches. Growth was calculated from a curvilinear body-scale relation. Intraseasonal growth in length extended from late April until well after October; most growth was in late summer and fall. The younger fish started growth earlier, and some mature fish did not increase in length until after the October spawning. Lake trout reached the minimum legal weight (1.5 pounds) in the 7th year of life and the average size taken in the commercial fishery (about 3 pounds) in the 8th year. The annual increase in weight in the 8th year of life was over 64%. Fish used in this study grew more slowly than those from Lakes Michigan and Huron taken during the period when sea lamprey abundance was increasing, but at about the same rate as lake trout of Lake Michigan before the sea lamprey appeared.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Rahrer, J.F., 1967, Growth of lake trout in Lake Superior before the maximum abundance of sea lampreys: Transactions of the American Fisheries Society, v. 96, no. 3, p. 268-277.","productDescription":"p. 268-277","startPage":"268","endPage":"277","numberOfPages":"9","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e3c7","contributors":{"authors":[{"text":"Rahrer, Jerold F.","contributorId":76679,"corporation":false,"usgs":true,"family":"Rahrer","given":"Jerold","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308435,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000166,"text":"1000166 - 1967 - Biology of the freshwater drum in western Lake Erie","interactions":[],"lastModifiedDate":"2013-02-11T14:40:39","indexId":"1000166","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2938,"text":"Ohio Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Biology of the freshwater drum in western Lake Erie","docAbstract":"Information on the biology of the freshwater drum or sheepshead (Aplodinotus grunniens) was collected in Lake Erie during a fishery and limnological study made by the Bureau of Commercial Fisheries in 1957 and 1958. Growth of the sheepshead in 1958 was slower than in 1927, and slower than the growth in most other waters. Males and females grew at the same rate through the 4th year of life, but thereafter the females grew faster. Males required more than 13 years and females 11 years to reach 17 inches. A weight of 2 pounds was attained in the 12th year of life by males and in the 10th year by females. Annulus formation extended from mid-June to early August for age-groups I-IV (2nd through 5th year of life). Younger fish started growth earlier in the season than the older fish, and the larger, faster growing members of an age group began growth earlier than the smaller fish.\nThe growing season in 1958 ended in early October. Bottom-water temperatures were about 65A?F when growth started (mid-June) and 58A°F when growth ended. Growth was most rapid in August when temperatures were highest for the year (72A?F). Growth of young of the year, but not of older fish, was positively correlated with temperature during the 1951-57 growing seasons. The sex ratio of the 1958 samples shifted with age; age-groups I-IV contained 54% males, but older age groups had 75% males. Males matured between 7.0 and 15.9 inches (age-groups II-V) and females between 9.0 and 13.4 inches (age-groups III-VII). Spawning in 1958 reached a peak in early July, but extended from mid-June to early August.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ohio Journal of Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Ohio Academy of Science","collaboration":"Out-of-print","usgsCitation":"Edsall, T.A., 1967, Biology of the freshwater drum in western Lake Erie: Ohio Journal of Science, v. 67, no. 6, p. 321-340.","productDescription":"20 p.","startPage":"321","endPage":"340","numberOfPages":"20","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267215,"type":{"id":15,"text":"Index Page"},"url":"https://hdl.handle.net/1811/5342"}],"volume":"67","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db6231a7","contributors":{"authors":[{"text":"Edsall, Thomas A.","contributorId":84302,"corporation":false,"usgs":true,"family":"Edsall","given":"Thomas","email":"","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":false,"id":308174,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000456,"text":"1000456 - 1967 - Fishery picture changing in Lake Erie: pollution a major factor, survey shows","interactions":[],"lastModifiedDate":"2013-04-05T10:48:34","indexId":"1000456","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1330,"text":"Conservationist","active":true,"publicationSubtype":{"id":10}},"title":"Fishery picture changing in Lake Erie: pollution a major factor, survey shows","docAbstract":"The objectives of these cruises of the research vessel Musky II in 1965 and 1966 were: To determine changes in the fish population and environmental conditions in recent years; to determine if the geographic and depth distributions of certain species of fish in the summer differed from that in the autumn; and, to obtain much-needed information on the selectivity of experimental gill nets, particularly for the fresh-water drum (sheepshead) and the walleye. In general, the kinds of fishes, and the geographic and depth distribution of the catches in the eastern basin in June, 1966 did not differ greatly from those in September of the preceding year. The numbers of some fishes, however, had changed- the so-called trash fish were more abundant and the more desirable commercial species were less numerous than in 1965. Yellow perch was by far the most abundant species in the catches. Other fishes taken frequently included white suckers, stonecats, white bass, smelt, and walleyes. Sizeable populations of small-mouth bass and fresh-water drum were also found.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Conservationist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Van Meter, H.D., and Shepherd, W.F., 1967, Fishery picture changing in Lake Erie: pollution a major factor, survey shows: Conservationist, v. 22, no. 2, p. 2-3.","productDescription":"p. 2-3","startPage":"2","endPage":"3","numberOfPages":"1","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df7b7","contributors":{"authors":[{"text":"Van Meter, Harry D.","contributorId":36887,"corporation":false,"usgs":true,"family":"Van Meter","given":"Harry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":308569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shepherd, William F.","contributorId":50857,"corporation":false,"usgs":true,"family":"Shepherd","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308570,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046372,"text":"70046372 - 1967 - Serial publications commonly cited in technical bibliographies of the United States Geological Survey","interactions":[],"lastModifiedDate":"2013-07-08T12:49:35","indexId":"70046372","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Serial publications commonly cited in technical bibliographies of the United States Geological Survey","docAbstract":"This compilation is a listing of the serial publications cited in the following publications of the United States Geological Survey: Geophysical Abstracts, Abstracts of North American Geology, Bibliography of North American Geology, and Bibliography of Hydrology of the United States. A supplement of publications added since the main list was compiled begins on page 83. New journals cited in Geophysical . Abstracts are listed in each monthly issue. Serial publications cited in each annual bibliography are listed in that volume.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70046372","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Serial publications commonly cited in technical bibliographies of the United States Geological Survey (1967 edition), 93 p., https://doi.org/10.3133/70046372.","productDescription":"93 p.","numberOfPages":"96","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274617,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70046372/report.pdf"},{"id":273561,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70046372/report-thumb.jpg"}],"edition":"1967 edition","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b6f56ce4b0097a7158e5f2","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":535544,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70046378,"text":"70046378 - 1967 - The Amazon, measuring a mighty river","interactions":[],"lastModifiedDate":"2013-07-08T12:46:58","indexId":"70046378","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"The Amazon, measuring a mighty river","docAbstract":"The Amazon, the world's largest river, discharges enough water into the sea each day to provide fresh water to the City of New York for over 9 years. Its flow accounts for about 15 percent of all the fresh water discharged into the oceans by all the rivers of the world. By comparison, the Amazon's flow is over 4 times that of the Congo River, the world's second largest river. And it is 10 times that of the Mississippi, the largest river on the North American Continent.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/70046378","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, The Amazon, measuring a mighty river, 16 p., https://doi.org/10.3133/70046378.","productDescription":"16 p.","numberOfPages":"16","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":273572,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70046378/report-thumb.jpg"},{"id":274613,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70046378/report.pdf"}],"country":"Brazil","otherGeospatial":"Amazon River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -60.89,-4.55 ], [ -60.89,0.71 ], [ -49.99,0.71 ], [ -49.99,-4.55 ], [ -60.89,-4.55 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b6f56de4b0097a7158e5ff","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":535548,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70196333,"text":"70196333 - 1967 - Hydrologic applications of lithofacies clastic-ratio maps","interactions":[],"lastModifiedDate":"2018-06-04T10:30:26","indexId":"70196333","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Hydrologic applications of lithofacies clastic-ratio maps","docAbstract":"

No abstract available.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings, South Dakota Academy of Science","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"South Dakota Academy of Science","usgsCitation":"Pettyjohn, W.A., and Randich, P.G., 1967, Hydrologic applications of lithofacies clastic-ratio maps, in Proceedings, South Dakota Academy of Science, p. 48-60.","productDescription":"13 p.","startPage":"48","endPage":"60","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":353065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff5ed3e4b0da30c1bfddab","contributors":{"authors":[{"text":"Pettyjohn, Wayne A.","contributorId":20724,"corporation":false,"usgs":true,"family":"Pettyjohn","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":732353,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randich, Phillip G.","contributorId":93071,"corporation":false,"usgs":true,"family":"Randich","given":"Phillip","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":732354,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70190814,"text":"70190814 - 1967 - Hydrologic and climatologic data, 1966, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2018-03-26T15:43:24","indexId":"70190814","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"13","title":"Hydrologic and climatologic data, 1966, Salt Lake County, Utah","docAbstract":"

An investigation of the water resources of Salt Lake County, Utah, was undertaken by the Water Resources Division of the U.S. Geological Survey in July 1963. This investigation is a cooperative project financed equally by the State of Utah and the Federal Government in accordance with an agreement between the State Engineer and the Geological Survey. The Utah Water and Power Board, Utah Fish and Game Commission, Salt Lake County Water Conservancy District, Metropolitan Water District of Salt Lake City, Salt Lake County, Kennecott Copper Corporation, Utah Power and Light Company, Salt Lake City Chamber of Commerce, and the Central Utah Water Conservancy District contributed funds to the State Engineer's office toward support of the project.

The investigation encompasses the collection and interpretation of a large variety of climatologic, hydrologic, and geologic data in and near Salt Lake County. Utah Basic-Data Releases 11 and 12 contain data collected through 1965. This release contains climatologic and surface-water data for the 1966 water year (October 1965 to September 1966) and groundwater data collected during the 1966 calendar year. Similar annual releases will contain data collected during the remainder of the investigation, and interpretive reports will be prepared as the investigation proceeds. Organizations that furnished data are acknowledged in station descriptions and footnotes to tables.

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