The investigation of the ground-water resources of Monmouth County is part of a Statewide water-resources program. This study was made by the U.S. Geological Survey in cooperation with the new Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply. It was under the general direction of Philip E. LaMoreaux, Chief of the Ground Water Branch of the U.S. Geological Survey, and under the direct supervision of Allen Sinnott, District Geologist.
This report presents data for most of the public-supply wells and for several irrigation wells in Monmouth County. The data for these wells are believed to be representative of large-capacity wells tapping the major aquifers present in the county. The information is released at this time in advance of an interpretive report because of its value to prospective users of ground water in Monmouth County. An earlier report presented data on small-capacity wells tapping both major and minor aquifers in the county. The data in these two reports form, in part, the basis for a comprehensive interpretive report on the ground-water resources of Monmouth County, now in preparation. Also to be included in the latter report are data for certain large-capacity industrial wells.
","language":"English","publisher":"State of New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply","usgsCitation":"Jablonski, L.A., 1960, Factual data for public-supply wells and selected irrigation wells in Monmouth County, New Jersey: New Jersey Division of Water Policy and Supply Water Resources Circular 4, iii, 29 p.","productDescription":"iii, 29 p.","numberOfPages":"33","costCenters":[],"links":[{"id":290118,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":290117,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114183/report.pdf"}],"country":"United States","state":"New Jersey","county":"Monmouth County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.613529,40.07913 ], [ -74.613529,40.478576 ], [ -73.972184,40.478576 ], [ -73.972184,40.07913 ], [ -74.613529,40.07913 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9dede4b065055fab1665","contributors":{"authors":[{"text":"Jablonski, Leo A.","contributorId":16324,"corporation":false,"usgs":true,"family":"Jablonski","given":"Leo","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":495256,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000358,"text":"1000358 - 1960 - The bottom fauna of Lake Huron","interactions":[],"lastModifiedDate":"2016-03-10T13:32:13","indexId":"1000358","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"The bottom fauna of Lake Huron","docAbstract":"The examination of 63 bottom samples, collected in Lake Huron in 1952 and 1956, revealed that Pontoporeia affinis was the dominant organism in both deep and shallow water. The next most abundant organisms in deep water were oligochaetes, fingernail clams, and midge larvae. Midge larvae were more numerous than either oligochaetes or fingernail clams in shallow water. The nmnber of organisms per square meter was similar to that determined from a similar study on Lake Michigan.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1960)89[193:TBFOLH]2.0.CO;2","usgsCitation":"Teter, H.D., 1960, The bottom fauna of Lake Huron: Transactions of the American Fisheries Society, v. 89, no. 2, p. 193-197, https://doi.org/10.1577/1548-8659(1960)89[193:TBFOLH]2.0.CO;2.","productDescription":"5 p.","startPage":"193","endPage":"197","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128938,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6696c7","contributors":{"authors":[{"text":"Teter, Howard D.","contributorId":22282,"corporation":false,"usgs":true,"family":"Teter","given":"Howard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":308449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000164,"text":"1000164 - 1960 - Age and growth of the whitefish Coregonus clupeaformis, of Munising Bay, Lake Superior","interactions":[],"lastModifiedDate":"2013-02-04T11:43:10","indexId":"1000164","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"Age and growth of the whitefish Coregonus clupeaformis, of Munising Bay, Lake Superior","docAbstract":"This study is based on a sample of 415 whitefish collected in 1953 from an unexploited population in Munising Bay, Lake Superior. Gill-net and trawl catches had different length-frequency distributions and age compositions, but estimates of growth from the two catches were very similar. The body-scale relation is a straight line with an intercept of 1.5 inches. Weight of Munising Bay whitefish captured in June increased as the 3.17 power of the length. Growth in length and weight of Munising Bay whitefish was the slowest yet reported from Great Lakes waters. Munising Bay whitefish required nearly 8 years to reach a length of 10 inches and a full 13 years to reach 15 inches. Slightly more than 8 years were required to reach a weight of 8 ounces and a little less than 14 years to reach 1 pound. The sex ratio of the Munising Bay whitefish exhibited no systematic change with an increase in age. The entire sample for which ages were determined contained 52 percent males. Munising Bay whitefish matured at much shorter lengths but at a greater age than reported for other Great Lakes whitefish populations. The smallest mature males were in the 11.5- to 11.9-inch length interval (age-group VII) and all males longer than 14.4 inches (age-group XII) were mature. The first mature females appeared at 12.0-12.4 inches (age-group X) and all females longer than 14.9 inches (age-group XII) were mature. The more rapidly growing individuals matured earlier than the slow-growing ones.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"London, UK","doi":"10.1577/1548-8659(1960)89[323:AAGOTW]2.0.CO;2","collaboration":"Out-of-print","usgsCitation":"Edsall, T.A., 1960, Age and growth of the whitefish Coregonus clupeaformis, of Munising Bay, Lake Superior: Transactions of the American Fisheries Society, v. 89, no. 4, p. 323-332, https://doi.org/10.1577/1548-8659(1960)89[323:AAGOTW]2.0.CO;2.","productDescription":"10 p.","startPage":"323","endPage":"332","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266924,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1960)89[323:AAGOTW]2.0.CO;2"}],"volume":"89","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db6899a5","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":308172,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000367,"text":"1000367 - 1960 - First-year growth of the walleye, Stizostedion vitreum vitreum (Mitchill), and associated factors in the Red Lakes, Minnesota","interactions":[],"lastModifiedDate":"2016-03-10T13:41:12","indexId":"1000367","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"First-year growth of the walleye, Stizostedion vitreum vitreum (Mitchill), and associated factors in the Red Lakes, Minnesota","docAbstract":"First-year growth of the walleye, Stizostedion vitreum vitreum (Mitchill), was studied from 4,544 fish collected during the first summer of life in the Red Lakes in six seasons and from back calculations on 4,474 fish one year or more in age representing 17 year classes. Sexes did not differ in growth rate. Growth within the season varied greatly in different years and total growth deviated as much as 15.3% from the mean of the entire period. Water temperature, size of brood, and abundance of large walleyes and perch did not affect growth rate. Very early or late spawning influenced total growth during the season and final size and goodness or poorness of a season's growth was determined by the middle of July. Growth rate of young-of-the-year perch and total use of perch as food did not significantly influence growth. Incidence of perch in walleye stomachs ranged from 10.9 to 98.0% and spottail shiner was a more important food item in most years than perch. Total first- year growth of the walleye was apparently determined before fish became a major item in the diet.
","language":"English","publisher":"Wiley","doi":"10.4319/lo.1960.5.3.0281","usgsCitation":"Smith, L.L., and Pycha, R.L., 1960, First-year growth of the walleye, Stizostedion vitreum vitreum (Mitchill), and associated factors in the Red Lakes, Minnesota: Limnology and Oceanography, v. 5, no. 3, p. 281-290, https://doi.org/10.4319/lo.1960.5.3.0281.","productDescription":"10 p.","startPage":"281","endPage":"290","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":480391,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lo.1960.5.3.0281","text":"Publisher Index Page"},{"id":130458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"3","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f33d9","contributors":{"authors":[{"text":"Smith, Lloyd L. Jr.","contributorId":103618,"corporation":false,"usgs":true,"family":"Smith","given":"Lloyd","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308466,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pycha, Richard L.","contributorId":17175,"corporation":false,"usgs":true,"family":"Pycha","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308465,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7000045,"text":"7000045 - 1960 - A primer on water","interactions":[],"lastModifiedDate":"2017-03-23T15:30:33","indexId":"7000045","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"A primer on water","docAbstract":"When you open the faucet you expect water to flow. And you expect it to flow night or day, summer or winter, whether you want to fill a glass or water the lawn. It should be clean and pure, without any odor.
You have seen or read about places where the water doesn't have these qualities. You may have lived in a city where you were allowed to water the lawn only during a few hours of certain days. We know a large town where the water turns brown after every big rainstorm.
Beginning shortly after World War II, large areas in the Southwestern United States had a 10-year drought, and newspapers published a lot of information about its effects. Some people say that the growing demand for water will cause serious shortages over much of the country in the next 10 to 40 years. But it has always been true that while water wells and springs dry up in some places, floods may be occurring in other places at the same time.
Nearly every month news stories are published describing floods somewhere in the country. In fact, every year, on the average, 75,000 persons are forced from their homes by floods. In some years, as in 1951 when the lower Kansas River experienced a great flood, half a million people are affected. To understand the reasons for such recurring distress, it is necessary to know something about rivers and about the flat land or flood plain that borders the river.
Interest in water and related problems is growing as our population increases and as the use of water becomes steadily greater. To help meet this heightened interest in general information about water and its use and control is the reason this primer was written. The primer is in two parts. The first part tells about hydrology, or the science that concerns the relation of water to our earth, and the second part describes the development of water supplies and the use of water. The Geological Survey is publishing this primer in nontechnical language in the hope that it will enable the general reader to understand the facts about water as a part of nature, and that by having this understanding the people can solve their water problems.
We, as representatives of the Geological Survey, acknowledge with thanks the helpful suggestions made on an early draft by Marion Loizeaux, Maria Lord Converse, Constance Foley, Laura R. Langbein, and Bruce C. Leopold. We are also indebted to various geologists and engineers of the Survey for their discerning critical reviews.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/7000045","usgsCitation":"Leopold, L.B., and Langbein, W.B., 1960, A primer on water: General Interest Publication, iv, 50 p., https://doi.org/10.3133/7000045.","productDescription":"iv, 50 p.","numberOfPages":"57","costCenters":[],"links":[{"id":261217,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/7000045/report.pdf"},{"id":261218,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/7000045/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8fa7","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":344013,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langbein, Walter Basil","contributorId":40581,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter","email":"","middleInitial":"Basil","affiliations":[],"preferred":false,"id":344014,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185592,"text":"70185592 - 1960 - Water and the Southwest","interactions":[],"lastModifiedDate":"2017-03-24T10:51:59","indexId":"70185592","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5332,"text":"Landscape","active":true,"publicationSubtype":{"id":10}},"title":"Water and the Southwest","docAbstract":"In a pluvial period associated with Wisconsin glaciation the closed basin of the Estancia valley in New Mexico held a lake which, at its maximum extent, was 150 feet deep and had a surface area of 450 square miles. This basin, with an elevation of about 6,000 feet, has at present an annual precipitation of about 16 inches.
Estimates have been made of the Pleistocene precipitation necessary to maintain this pluvial lake. Instead of the present annual average of 14 inches, it has been variously estimated that the precipitation must have been 20 to 24 inches. Lakes existed during Pleistocene time in many places in Western United States which are now true deserts. There is evidence in many places in this area that early man lived on the shores of these lakes. He must have adapted himself to the increasing aridity. Some of the forms of this adaptation can be seen even at present in the form of flood-water farming practices highly developed by the Hopi Indians.
","language":"English","usgsCitation":"Leopold, L.B., 1960, Water and the Southwest: Landscape, v. 10, no. 1, p. 27-31.","productDescription":"5 p.","startPage":"27","endPage":"31","costCenters":[],"links":[{"id":338280,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"10","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d6304de4b05ec79913114f","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1013698,"text":"1013698 - 1960 - Neutralizing chlorine in city water for use in fish-distribution tanks","interactions":[],"lastModifiedDate":"2025-07-31T15:28:06.644472","indexId":"1013698","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Neutralizing chlorine in city water for use in fish-distribution tanks","docAbstract":"No abstract available.
","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8659(1960)22[30:NCICWF]2.0.CO;2","usgsCitation":"Pyle, E.A., 1960, Neutralizing chlorine in city water for use in fish-distribution tanks: Progressive Fish-Culturist, v. 22, no. 1, p. 30-33, https://doi.org/10.1577/1548-8659(1960)22[30:NCICWF]2.0.CO;2.","productDescription":"4 p.","startPage":"30","endPage":"33","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129332,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697a66","contributors":{"authors":[{"text":"Pyle, E. A.","contributorId":51243,"corporation":false,"usgs":true,"family":"Pyle","given":"E.","middleInitial":"A.","affiliations":[],"preferred":false,"id":319075,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70176005,"text":"70176005 - 1959 - Geology and ground-water resources of Clay County, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T13:47:36","indexId":"70176005","displayToPublicDate":"2015-12-21T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Clay County, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Walters, K., and Bayne, C., 1959, Geology and ground-water resources of Clay County, Kansas: Kansas Geological Survey Bulletin, v. 136, 106 p. .","productDescription":"106 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327692,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327691,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"136","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73d7e4b03fd6b7df2cc5","contributors":{"authors":[{"text":"Walters, K.L.","contributorId":105765,"corporation":false,"usgs":true,"family":"Walters","given":"K.L.","affiliations":[],"preferred":false,"id":646786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bayne, C.K.","contributorId":173976,"corporation":false,"usgs":false,"family":"Bayne","given":"C.K.","email":"","affiliations":[],"preferred":false,"id":646787,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70176007,"text":"70176007 - 1959 - Ground-water levels in observation wells in Kansas, 1958","interactions":[],"lastModifiedDate":"2016-08-23T13:57:47","indexId":"70176007","displayToPublicDate":"2015-12-20T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Ground-water levels in observation wells in Kansas, 1958","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Fishel, V., Gulley, E., and Reavis, E., 1959, Ground-water levels in observation wells in Kansas, 1958: Kansas Geological Survey Bulletin, v. 141, 146 p. .","productDescription":"146 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327696,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327695,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"141","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dde4b03fd6b7df2d0c","contributors":{"authors":[{"text":"Fishel, V.C.","contributorId":6126,"corporation":false,"usgs":true,"family":"Fishel","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":646789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gulley, E.L.","contributorId":173982,"corporation":false,"usgs":false,"family":"Gulley","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":646790,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reavis, E.L.","contributorId":70246,"corporation":false,"usgs":true,"family":"Reavis","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":646791,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70160534,"text":"70160534 - 1959 - Etiology of sockeye salmon 'virus' disease","interactions":[],"lastModifiedDate":"2018-02-22T13:48:41","indexId":"70160534","displayToPublicDate":"2015-10-12T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"296","title":"Etiology of sockeye salmon 'virus' disease","docAbstract":"Violent epizootics among hatchery reared sockeye salmon fingerlings (Oncorhynchus nerka) caused by a filterable agent have occurred. In 1954, one source of this infectious, filterable agent was found to be adult sockeye viscera used in the diet for the fingerlings. The results of observations on an epizootic in 1958 indicate that the infection may be transmitted to fingerlings from a water supply to which adult sockeye salmon have access.
","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Guenther, R.W., Watson, S., Rucker, R., and Ross, A.J., 1959, Etiology of sockeye salmon 'virus' disease: Special Scientific Report - Fisheries 296, iv, 10 p.","productDescription":"iv, 10 p.","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312721,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":312720,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://spo.nmfs.noaa.gov/SSRF/SSRF296.pdf","text":"pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567a823be4b0a04ef490fce4","contributors":{"authors":[{"text":"Guenther, Raymond W.","contributorId":39343,"corporation":false,"usgs":false,"family":"Guenther","given":"Raymond","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":729299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watson, S.W.","contributorId":150802,"corporation":false,"usgs":false,"family":"Watson","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":729300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rucker, R.R.","contributorId":104000,"corporation":false,"usgs":true,"family":"Rucker","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":729301,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ross, A. J.","contributorId":105267,"corporation":false,"usgs":true,"family":"Ross","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":729302,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70176008,"text":"70176008 - 1959 - Geology and ground-water resources of Cloud County, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T14:04:49","indexId":"70176008","displayToPublicDate":"2015-10-05T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Cloud County, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Bayne, C., and Walters, K., 1959, Geology and ground-water resources of Cloud County, Kansas: Kansas Geological Survey Bulletin, v. 139, 144 p. .","productDescription":"144 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327699,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327698,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"139","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73d7e4b03fd6b7df2cc7","contributors":{"authors":[{"text":"Bayne, C.K.","contributorId":173976,"corporation":false,"usgs":false,"family":"Bayne","given":"C.K.","email":"","affiliations":[],"preferred":false,"id":646792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, K.L.","contributorId":105765,"corporation":false,"usgs":true,"family":"Walters","given":"K.L.","affiliations":[],"preferred":false,"id":646793,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70176006,"text":"70176006 - 1959 - Kansas streamflow characteristics, part 1, Flow duration","interactions":[],"lastModifiedDate":"2016-08-23T13:54:05","indexId":"70176006","displayToPublicDate":"2015-09-15T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesTitle":{"id":414,"text":"Technical Report","active":false,"publicationSubtype":{"id":9}},"title":"Kansas streamflow characteristics, part 1, Flow duration","language":"English","publisher":"State of Kansas Water Resources Board ","publisherLocation":"Topeka, Kansas","usgsCitation":"Furness, L., 1959, Kansas streamflow characteristics, part 1, Flow duration: Technical Report, v. 1, 213.","productDescription":"213","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327694,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73e2e4b03fd6b7df2d28","contributors":{"authors":[{"text":"Furness, L.W.","contributorId":16908,"corporation":false,"usgs":true,"family":"Furness","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":646788,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70160575,"text":"70160575 - 1959 - Vibrio infections among marine and fresh-water fish","interactions":[],"lastModifiedDate":"2021-04-02T15:13:30.918528","indexId":"70160575","displayToPublicDate":"2015-09-13T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Vibrio infections among marine and fresh-water fish","docAbstract":"In 1951. B. J. Earpio found a vibrio infection among salmon fingerlings being reared in saltwater at the Deception Pass Biological Station of the Washington State Department of Fisheries. The disease waa characterized by erythema at the base of fins and on the sides of the fish, necrotic areas in the Inusculature, inflammation of the intestinal tract, and general septicernia. The disease reappeared the next year, killing nearly all of the churn salmon (Oncorhynchus keta) fingerlings, killing about half of the pink salmon (O. gorbuscha) fingerlings, and affecting to a lesser degree the chinook salmon (O. tshawytscha) fingerlings. Also, late in 1952. R. R. Rucker and E. J. Ordal found the same disease at a rainbow trout hatchery of the Washington State Department of Game at Vancouver. The disease caused severe losses there among the rainbow trout (Salmo gairdneri) and among the sea-run form of the same species (called steelhead trout). The disease was manifested by bloody, necrotic areas in the musculature and inflammation of the viscera, відоіШат to furumaculoвiв,
\nThe main object of this paper is to bring vibrio infections of fish to the attention of the American fish-culturist.
\n","language":"English","publisher":"Department of Commerce, Bureau of Fisheries","doi":"10.1577/1548-8659(1959)21[22:VIAMAF]2.0.CO;2","usgsCitation":"Rucker, R.R., 1959, Vibrio infections among marine and fresh-water fish: Progressive Fish-Culturist, v. 21, no. 1, p. 22-25, https://doi.org/10.1577/1548-8659(1959)21[22:VIAMAF]2.0.CO;2.","productDescription":"4 p.","startPage":"22","endPage":"25","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312784,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567bd3bae4b0a04ef491a1ea","contributors":{"authors":[{"text":"Rucker, Robert R.","contributorId":69615,"corporation":false,"usgs":true,"family":"Rucker","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":813463,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71569,"text":"tei545 - 1959 - Gravity and seismic exploration in Yucca Valley, Nevada test site, January-April, 1959","interactions":[],"lastModifiedDate":"2015-10-20T13:04:38","indexId":"tei545","displayToPublicDate":"2013-07-18T11:22:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"545","title":"Gravity and seismic exploration in Yucca Valley, Nevada test site, January-April, 1959","docAbstract":"
The thickness of the alluvial and tuffaceous deposits that overlie bedrock in Yucca Valley has been inferred from gravity and seismic measurements. Preliminary interpretations indicate that these deposits are thickest in a narrow north-trending trough in the eastern part of the valley. The gravity data delineate a buried north-trending ridge of bedrock that extends from Mine Mountain almost to Quartzite Ridge.
\nSeismic refraction measurements confirm the existence of the bedrock ridge and indicate that the bedrock is as close as 100 feet to the surface. The buried bedrock high is important because it may alter concepts of the movement of groundwater within the valley.
\nA single seismic-refraction profile was located near the area of thickest alluvium and tuff to determine the feasibility of using refraction techniques for determining the depth to bedrock where it is covered with several thousand feet of alluvium and tuff. The results are encouraging but not enough data were acquired to give a reliable depth estimate.
\nSeismic-refraction measurements were used successfully to determine the thickness of alluvium in narrow valleys partly filled with alluvium.
\nThis work was in the northwestern part of Yucca Valley and was done to choose drilling sites for studies of ground-water movement.
\n","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei545","collaboration":"Work done on behalf of the Albuquerque Operations Office, U.S. Atomic Energy Commission.","usgsCitation":"Diment, W.H., Healey, D., and Roller, J., 1959, Gravity and seismic exploration in Yucca Valley, Nevada test site, January-April, 1959: U.S. Geological Survey Trace Elements Investigations 545, Report: 41 p.; 1 Plate: 21.26 x 34.69 inches, https://doi.org/10.3133/tei545.","productDescription":"Report: 41 p.; 1 Plate: 21.26 x 34.69 inches","numberOfPages":"44","onlineOnly":"N","additionalOnlineFiles":"Y","temporalStart":"1959-01-01","temporalEnd":"1959-04-30","costCenters":[],"links":[{"id":290451,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei545.jpg"},{"id":310154,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/545/report.pdf","text":"Report","size":"14.70 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":310155,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/545/plate-1.pdf","text":"Plate 1","size":"12.50 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"}],"country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"Yucca Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-115.9082,39.1615],[-115.5191,38.9578],[-115.4725,38.9325],[-115.4433,38.9162],[-115.3694,38.8769],[-115.363,38.874],[-115.242,38.8093],[-115.0969,38.7309],[-115.0777,38.721],[-115.0604,38.7107],[-115.0291,38.6937],[-114.999,38.6777],[-114.9996,38.592],[-114.9997,38.4315],[-114.9994,38.3894],[-115.0004,38.0507],[-115.1185,38.0508],[-115.1436,38.0508],[-115.326,38.0515],[-115.3453,38.0514],[-115.4003,38.051],[-115.4587,38.0506],[-115.6394,38.0512],[-115.6581,38.051],[-115.8404,38.0504],[-115.8931,38.0507],[-115.8938,37.723],[-115.8969,37.5498],[-115.8975,37.2796],[-115.8982,37.1926],[-115.8942,36.8425],[-115.8941,36.686],[-115.8945,36.6702],[-115.8949,36.598],[-115.8949,36.5962],[-115.8946,36.5858],[-115.8947,36.5005],[-115.8945,36.4806],[-115.8949,36.462],[-115.8944,36.457],[-115.8948,36.3087],[-115.8945,36.2923],[-115.8943,36.1957],[-115.8945,36.1608],[-115.8948,36.1163],[-115.8948,36.0927],[-115.895,36.0015],[-115.9178,36.0192],[-115.9518,36.0457],[-115.9925,36.0773],[-116.049,36.1211],[-116.0624,36.1314],[-116.1039,36.1636],[-116.1287,36.1829],[-116.1702,36.2152],[-116.173,36.2174],[-116.2311,36.2626],[-116.2834,36.3028],[-116.2954,36.3122],[-116.3752,36.373],[-116.5107,36.4764],[-116.5247,36.4871],[-116.5589,36.5131],[-116.574,36.5245],[-116.5946,36.54],[-116.6556,36.5867],[-116.6583,36.5888],[-116.6764,36.6024],[-116.706,36.6248],[-116.7895,36.6877],[-116.8424,36.7276],[-116.8453,36.7298],[-116.8806,36.7568],[-116.8912,36.7648],[-116.9237,36.7891],[-116.9641,36.8193],[-116.9783,36.8299],[-116.981,36.8319],[-117.0046,36.8495],[-117.164,36.9688],[-117.1639,36.9698],[-117.1637,37.0182],[-117.164,37.0894],[-117.1642,37.171],[-117.1641,37.1909],[-117.1641,37.1936],[-117.1665,37.6995],[-117.1664,37.714],[-117.1663,37.7285],[-117.1663,37.7435],[-117.1662,37.7585],[-117.1657,38.0019],[-117.2198,38.0482],[-117.2397,38.0483],[-117.239,38.0641],[-117.2408,38.0705],[-117.2653,38.0932],[-117.6896,38.4731],[-118.0197,38.7599],[-118.197,38.9154],[-118.1972,38.9993],[-117.8559,39.0746],[-117.7748,39.092],[-117.7008,39.1058],[-117.6409,39.1149],[-117.5946,39.1231],[-117.4742,39.1431],[-117.3823,39.1562],[-117.3609,39.1585],[-117.3318,39.1629],[-117.3063,39.1634],[-117.2849,39.1633],[-117.1995,39.1632],[-117.0856,39.1628],[-117.0322,39.1626],[-117.0144,39.1626],[-116.9871,39.1625],[-116.9158,39.1631],[-116.7562,39.1622],[-116.7301,39.1625],[-116.5996,39.1616],[-116.5859,39.162],[-116.4815,39.1616],[-116.3497,39.1618],[-116.2358,39.1616],[-116.0548,39.1624],[-115.9082,39.1615]]]},\"properties\":{\"name\":\"Nye\",\"state\":\"NV\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5f19e4b0b290850fc1de","contributors":{"authors":[{"text":"Diment, William H.","contributorId":78797,"corporation":false,"usgs":true,"family":"Diment","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":284407,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healey, D.L.","contributorId":52964,"corporation":false,"usgs":true,"family":"Healey","given":"D.L.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":284406,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roller, J.C.","contributorId":12507,"corporation":false,"usgs":true,"family":"Roller","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":284405,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70046988,"text":"70046988 - 1959 - Ground-water levels and related hydrologic data from selected observation wells in Nassau County, Long Island, New York","interactions":[{"subject":{"id":56157,"text":"ofr5969 - 1959 - Ground-water levels and related hydrologic data from selected observation wells in Nassau County, Long Island, New York","indexId":"ofr5969","publicationYear":"1959","noYear":false,"title":"Ground-water levels and related hydrologic data from selected observation wells in Nassau County, Long Island, New York"},"predicate":"SUPERSEDED_BY","object":{"id":70046988,"text":"70046988 - 1959 - Ground-water levels and related hydrologic data from selected observation wells in Nassau County, Long Island, New York","indexId":"70046988","publicationYear":"1959","noYear":false,"title":"Ground-water levels and related hydrologic data from selected observation wells in Nassau County, Long Island, New York"},"id":1}],"lastModifiedDate":"2013-07-11T15:57:43","indexId":"70046988","displayToPublicDate":"2013-01-01T15:43:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"GW-41","title":"Ground-water levels and related hydrologic data from selected observation wells in Nassau County, Long Island, New York","docAbstract":"Nassau County has experienced a rapid growth in population and industry in the past 20 years that has resulted in increased development of its ground-water resources. The county is located in west-central Long Island and its boundaries enclose a land area of 274 square miles. The climate is relatively mild and precipitation averages 43 inches a year. The precipitation is the ultimate source of natural replenishment to the ground-water reservoir. Ground water is found in the pore spaces of unconsolidated sands, gravels, and clays which overlay a basement of crystalline bedrock.","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the New York State Water Power and Control Commission and the Nassau County Department of Public Works","usgsCitation":"Isbister, J., 1959, Ground-water levels and related hydrologic data from selected observation wells in Nassau County, Long Island, New York: Bulletin GW-41, 42 p.","productDescription":"42 p.","numberOfPages":"62","costCenters":[],"links":[{"id":274899,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046988.png"},{"id":274898,"type":{"id":15,"text":"Index Page"},"url":"https://archive.org/details/usgswaterresourcesnewyork-bull_gw_41"}],"country":"United States","state":"New York","county":"Nassau County","otherGeospatial":"Long Island","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.767,40.5732 ], [ -73.767,40.9093 ], [ -73.4204,40.9093 ], [ -73.4204,40.5732 ], [ -73.767,40.5732 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51dfd3e3e4b0d332bf22f38a","contributors":{"authors":[{"text":"Isbister, John","contributorId":97074,"corporation":false,"usgs":true,"family":"Isbister","given":"John","email":"","affiliations":[],"preferred":false,"id":480811,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047487,"text":"70047487 - 1959 - Ground-water resources of the Oakland Park area of eastern Broward County, Florida","interactions":[{"subject":{"id":24519,"text":"ofr5891 - 1958 - Ground-water resources of the Oakland Park area of eastern Broward County, Florida","indexId":"ofr5891","publicationYear":"1958","noYear":false,"title":"Ground-water resources of the Oakland Park area of eastern Broward County, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70047487,"text":"70047487 - 1959 - Ground-water resources of the Oakland Park area of eastern Broward County, Florida","indexId":"70047487","publicationYear":"1959","noYear":false,"title":"Ground-water resources of the Oakland Park area of eastern Broward County, Florida"},"id":1}],"lastModifiedDate":"2017-09-13T17:55:10","indexId":"70047487","displayToPublicDate":"2013-01-01T15:18:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5489,"text":"Florida Geological Survey Report of Investigations","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"20","title":"Ground-water resources of the Oakland Park area of eastern Broward County, Florida","docAbstract":"The Biscayne aquifer is the source of all fresh ground water in the Oakland Park area of eastern Broward County, Florida. This aquifer extends from the land surface to more than 215 feet below mean sea level and is composed chiefly of sandy marine limestone, calcareous sandstone, and beds of fine to medium quartz sand. The aquifer differs from place to place, but, in general, most of the layers of limestone and sandstone occur at depths below 60 feet. The permeability of the aquifer increases with depth.","language":"English","publisher":"Florida Geological Survey","publisherLocation":"Tallahassee, FL","collaboration":"Prepared by the United States Geological Survey in cooperation with the City of Fort Lauderdale and the Florida Geological Survey","usgsCitation":"Sherwood, C., 1959, Ground-water resources of the Oakland Park area of eastern Broward County, Florida: Florida Geological Survey Report of Investigations 20, vii, 40 p.","productDescription":"vii, 40 p.","costCenters":[],"links":[{"id":276179,"type":{"id":11,"text":"Document"},"url":"https://ufdc.ufl.edu/UF00001204/00001/pdf?search=report+%3dinvestigations"},{"id":276180,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047487.PNG"}],"country":"United States","state":"Florida","county":"Broward County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.881389,25.95675 ], [ -80.881389,26.334667 ], [ -80.015276,26.334667 ], [ -80.015276,25.95675 ], [ -80.881389,25.95675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5203a379e4b02bdb1bc63fa6","contributors":{"authors":[{"text":"Sherwood, C. B.","contributorId":27888,"corporation":false,"usgs":true,"family":"Sherwood","given":"C. B.","affiliations":[],"preferred":false,"id":482173,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047665,"text":"70047665 - 1959 - Annual water-level measurements in observation wells, 1951-1955, and atlas of maps showing changes in water levels for various periods from beginning of record through 1954, New Mexico","interactions":[],"lastModifiedDate":"2013-08-16T15:01:14","indexId":"70047665","displayToPublicDate":"2013-01-01T14:53:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":138,"text":"Technical Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"13","title":"Annual water-level measurements in observation wells, 1951-1955, and atlas of maps showing changes in water levels for various periods from beginning of record through 1954, New Mexico","docAbstract":"This report tabulates the annual measurements of water level in the observation wells in the various irrigated areas, primarily from 1951 through 1955. It summarizes changes in water level by discussion and with an atlas of nearly all the maps of change of water level for the period of record to 1955 for each area in which observations are being made. Included also are hydrographs for the period of record through 1954 of several selected wells in the various areas irrigated from ground-water sources. The annual measurements of water level before 1951, seasonal measurements, and daily records of water levels in wells equipped with recording gages have been published in an annual series of U. S. Geological Survey water-supply papers.","language":"English","publisher":"New Mexico Office of the State Engineer","publisherLocation":"Santa Fe, NM","collaboration":"Prepared in cooperation with the United States Geological Survey","usgsCitation":"Reeder, H.O., 1959, Annual water-level measurements in observation wells, 1951-1955, and atlas of maps showing changes in water levels for various periods from beginning of record through 1954, New Mexico: Technical Report 13, Parts A-C: Variously Paginated.","productDescription":"Parts A-C: Variously Paginated","costCenters":[],"links":[{"id":276713,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047665.JPG"},{"id":276709,"type":{"id":11,"text":"Document"},"url":"https://www.ose.state.nm.us/PDF/Publications/Library/TechnicalReports/TechReport-013A.pdf"},{"id":276711,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://www.ose.state.nm.us/PDF/Publications/Library/TechnicalReports/TechReport-013B.pdf"},{"id":276712,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://www.ose.state.nm.us/PDF/Publications/Library/TechnicalReports/TechReport-013C.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.05,31.33 ], [ -109.05,37.0 ], [ -103.0,37.0 ], [ -103.0,31.33 ], [ -109.05,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520f49e0e4b0fc50304bc4a0","contributors":{"authors":[{"text":"Reeder, Harold O.","contributorId":14381,"corporation":false,"usgs":true,"family":"Reeder","given":"Harold","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":482671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047579,"text":"70047579 - 1959 - Water-resources reconnaissance of Gambell and Savoonga villages, St. Lawrence Island, Alaska","interactions":[{"subject":{"id":56143,"text":"ofr58107 - 1958 - Water-resources reconnaissance of Gambell and Savoonga villages, St. Lawrence Island, Alaska","indexId":"ofr58107","publicationYear":"1958","noYear":false,"title":"Water-resources reconnaissance of Gambell and Savoonga villages, St. Lawrence Island, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70047579,"text":"70047579 - 1959 - Water-resources reconnaissance of Gambell and Savoonga villages, St. Lawrence Island, Alaska","indexId":"70047579","publicationYear":"1959","noYear":false,"title":"Water-resources reconnaissance of Gambell and Savoonga villages, St. Lawrence Island, Alaska"},"id":1}],"lastModifiedDate":"2013-08-12T15:02:07","indexId":"70047579","displayToPublicDate":"2013-01-01T14:50:00","publicationYear":"1959","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":"Water-resources reconnaissance of Gambell and Savoonga villages, St. Lawrence Island, Alaska","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70047579","collaboration":"Prepared in cooperation with the Alaska Department of Health and the Alaska Rural Development Board; 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Observations made in 1955, 1956 and 1957, showed that this species was probably most abundant in the vicinity of Mamou, Evangeline Parish, and Roanoke, Jefferson Davis Parish. Tree ducks arrive in the rice country as the rice is planted in the spring and usually depart following fall harvest. A few winter in the coastal marshes. The nesting period extends from late May well into August. Thirteen and 20 pairs were found nesting in two separate five-square-mile areas. All nests observed were in rice fields. Clutch size in several nests found by John J. Lynch averaged about 13 eggs. A clutch of 23 eggs was probably a dump nest. Several investigators have reported incubation periods varying from 24 to 26 days. Nests were constructed of rice or other plants that occurred in the rice fields; they usually had a canopy and ramp; none was lined with down. Renesting compensated for some first attempt losses. Depredations on rice plantings sometimes occurred in spring in water-planted rice fields. Favorite foods were seeds of grasses and sedges found in rice fields. 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