Alexander, W. H., Jr., Broadhurst, W. L., and White, W. N., Progress report on ground water In the High Plains in Texas, Tex. State Bd. Water Engrs., 12 pp., 7 tigs. (mimeogranhedl May 1944.
Ashley, George H.,and Graham, Jack B., Groundwater investigations in Pennsylvania Pa. Dep. Internal Affairs, Monthly Bull., v. 13, pp. 10–13 and 28, 1945.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i002p00274","usgsCitation":"Berdan, J.M., 1946, Appendix E—List of current publications concerning ground water: Eos, Transactions, American Geophysical Union, v. 27, no. 2, p. 274-278, https://doi.org/10.1029/TR027i002p00274.","productDescription":"5 p.","startPage":"274","endPage":"278","costCenters":[],"links":[{"id":379063,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Berdan, Jean M.","contributorId":34140,"corporation":false,"usgs":true,"family":"Berdan","given":"Jean","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":800513,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70214994,"text":"70214994 - 1946 - Report of Committee on Ground Water—1944–1945","interactions":[],"lastModifiedDate":"2020-10-05T18:16:42.707377","indexId":"70214994","displayToPublicDate":"1946-10-05T13:07:31","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of Committee on Ground Water—1944–1945","docAbstract":"Because of war‐imposed responsibilities of most agencies and individuals this year, no new programs were undertaken by the Committee, but the work of the Subcommittee on Permeability was continued, and a substantial progress report by C. E. Jacob, Acting Chairman, and by members of this Subcommittee follows this report as Appendices A to D.
Following a suggestion by Max Suter, copies of this year's Committee report were sent to each member prior to publication and it is planned to follow this procedure in the future.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i002p00236","usgsCitation":"Lohman, S.W., 1946, Report of Committee on Ground Water—1944–1945: Eos, Transactions, American Geophysical Union, v. 27, no. 2, p. 236-245, https://doi.org/10.1029/TR027i002p00236.","productDescription":"10 p.","startPage":"236","endPage":"245","costCenters":[],"links":[{"id":379062,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Lohman, S. W.","contributorId":45318,"corporation":false,"usgs":true,"family":"Lohman","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":800512,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70214990,"text":"70214990 - 1946 - Report of the Research Committee on Runoff, 1945–46","interactions":[],"lastModifiedDate":"2020-10-05T17:31:33.542479","indexId":"70214990","displayToPublicDate":"1946-10-05T12:23:07","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of the Research Committee on Runoff, 1945–46","docAbstract":"The variety of usage and even the confusion in the nomenclature and terminology of some fields of hydrology have been often remarked. The Committee on Runoff conceived the idea that it would be profitable to consider some of the terms which are especially pertinent to the field of runoff. That consideration was the principal Committee project of the past year and is featured in this report.
The Chairman sent a letter to the members of the Committee that was planned to draw out a symposium of opinions on the subject. A good starting point seemed to be the classification of water on the Earth. Meinzer's well‐known classification was given: atmospheric water, surface water, and subsurface or subterranean water. Comments were solicited.
","publisher":"American Geophysical Union","doi":"10.1029/TR027i006p00876","usgsCitation":"Davenport, R.W., 1946, Report of the Research Committee on Runoff, 1945–46: Eos, Transactions, American Geophysical Union, v. 27, no. 6, p. 876-878, https://doi.org/10.1029/TR027i006p00876.","productDescription":"3 p.","startPage":"876","endPage":"878","costCenters":[],"links":[{"id":379053,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Davenport, R. W.","contributorId":41798,"corporation":false,"usgs":true,"family":"Davenport","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":800508,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70214988,"text":"70214988 - 1946 - A generalized graphical method for evaluating formation constants and summarizing well‐field history","interactions":[],"lastModifiedDate":"2020-10-05T17:18:02.929995","indexId":"70214988","displayToPublicDate":"1946-10-05T12:13:43","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"A generalized graphical method for evaluating formation constants and summarizing well‐field history","docAbstract":"The capacities of a water‐bearing formation to transmit water under a hydraulic gradient and to yield water from storage when the water table or artesian pressure declines, are generally expressed, respectively, in terms of a coefficient of transmissibility and a coefficient of storage. Determinations of these two constants are almost always involved in quantitative studies of ground‐water problems.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i004p00526","usgsCitation":"Cooper, H., and Jacob, C.E., 1946, A generalized graphical method for evaluating formation constants and summarizing well‐field history: Eos, Transactions, American Geophysical Union, v. 27, no. 4, p. 526-534, https://doi.org/10.1029/TR027i004p00526.","productDescription":"9 p.","startPage":"526","endPage":"534","costCenters":[],"links":[{"id":379052,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Cooper, H.H.","contributorId":62573,"corporation":false,"usgs":true,"family":"Cooper","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":800505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacob, C. E.","contributorId":64504,"corporation":false,"usgs":true,"family":"Jacob","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":800506,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70214982,"text":"70214982 - 1946 - General principles of artificial ground-water recharge","interactions":[],"lastModifiedDate":"2020-10-05T16:23:23.989236","indexId":"70214982","displayToPublicDate":"1946-10-05T11:15:48","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"General principles of artificial ground-water recharge","docAbstract":"The natural subterranean reservoirs formed by the porous and permeable rocks differ from surface reservoirs chiefly in that they have complex structure and great internal resistanc• to the How of water. Their full utilization requires systematic development based on the geology and hydrology of the aquifer and the principles of hydraulics distinctive of ground water. The methods of increasing recharge are of two kinds: (1) Indirect methods, in which increased recharge is accomplished by locating production wells as close as practicable to areas of rejected recharge or natural discharge, and (2) direct methods, in which water from surface sources is conveyed to points from which it percolates into a body of ground water. The direct methods can also be divided into two groups: (1) Recharge by surface application, and (2) recharge through wells. This paper discusses the different methods in relation to geologic structure and ground-water hydraulics and gives numerous examples.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.41.3.191","usgsCitation":"Meinzer, O.E., 1946, General principles of artificial ground-water recharge: Economic Geology, v. 41, no. 3, p. 191-201, https://doi.org/10.2113/gsecongeo.41.3.191.","productDescription":"11 p.","startPage":"191","endPage":"201","costCenters":[],"links":[{"id":379046,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"3","noUsgsAuthors":false,"publicationDate":"1946-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":800497,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70214514,"text":"70214514 - 1946 - Artificial recharge of artesian limestone at Orlando, Florida","interactions":[],"lastModifiedDate":"2020-09-28T20:38:00.826699","indexId":"70214514","displayToPublicDate":"1946-09-28T15:28:45","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Artificial recharge of artesian limestone at Orlando, Florida","docAbstract":"The principal aquifer in the Orlando area consists of 900 feet or more of permeable artesian limestones of upper and middle Eocene age. As in most other parts of the Florida peninsula, these limestones are overlain by the Hawthorn formation of Miocene age which contains relatively impervious beds. The Hawthorn at Orlando is 45 to 200 feet thick and prevents or retards natural recharge to the lime. stones except where it is penetrated by what appear to be old sinkholes that are now filled with pervious material.
Owing to the lack of adequate surface drainage, more than 200 wells have been drilled into the limestones in the Orlando area to drain streets, control lake levels, and dispose of sewage and other waste liquids. Generally the piezometric surface of the water in the limestones is fat enough below the land surface to allow drainage by gravity. As the limestones are cavernous, most of the wells have large capacities for receiving water and seldom become clogged although a considerable amount of rubbish is carried into them.
The piezometric surface is conspicuously higher where drainage wells are concentrated, probably because of recharge through wells. However, the effect of the artificial recharge cannot be clearly differentiated from that of natural recharge. A deep-well current meter was used to determine the horizons at which the polluted surface water enters the limestones.
The investigation was made in cooperation with the Florida Geological Survey and the Corps of Engineers of the U.S. Army.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.41.4.293","usgsCitation":"Unklesbay, A., and Cooper, H., 1946, Artificial recharge of artesian limestone at Orlando, Florida: Economic Geology, v. 41, no. 4, p. 293-307, https://doi.org/10.2113/gsecongeo.41.4.293.","productDescription":"15 p.","startPage":"293","endPage":"307","costCenters":[],"links":[{"id":378829,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","city":"Orlando","otherGeospatial":"Orlando","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.97998046875,\n 28.110748760633534\n ],\n [\n -81.01318359375,\n 28.110748760633534\n ],\n [\n -81.01318359375,\n 29.046565622728846\n ],\n [\n -81.97998046875,\n 29.046565622728846\n ],\n [\n -81.97998046875,\n 28.110748760633534\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"41","issue":"4","noUsgsAuthors":false,"publicationDate":"1946-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Unklesbay, A.G.","contributorId":241622,"corporation":false,"usgs":false,"family":"Unklesbay","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":799767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, H.H.","contributorId":62573,"corporation":false,"usgs":true,"family":"Cooper","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":799768,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70214511,"text":"70214511 - 1946 - Artificial recharge of glacial sand and gravel with filtered river water at Louisville, Kentucky","interactions":[],"lastModifiedDate":"2020-09-28T19:57:27.735045","indexId":"70214511","displayToPublicDate":"1946-09-28T14:46:59","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Artificial recharge of glacial sand and gravel with filtered river water at Louisville, Kentucky","docAbstract":"Records obtained by the Geological Survey, United States Department of the Interior, and the Geological Division, Kentucky Department of Mines and Minerals, indicate that industries at Louisville pumped about 62 million gallons of water per day from wells in 1943. This was over 20 million gallons a day more than the natural recharge to the glacial outwash sand and gravel from which the wells draw the water. The ground water is especially in demand because of its uniformly low temperature throughout the year. In order to stop the resulting serious decline of water levels and decrease in yields of wells, the pumpage is now gradually being reduced. Also, the recharge has been increased about 2 million gallons a day by introducing water into the aquifer through wells.
During the spring of 1944 the Seagram and National distilleries helped solve a local shortage of ground water by recharging the underground reservoir with 1.7 million gallons a day of cold water from the municipal river-water supply. While this water was being added to the aquifer through several supply wells the plants were operated with additional city water, and the rest of the supply wells were kept idle. In this way, the large cone of depression in the water table that had been created by heavy pumping from the wells was practically filled with cold water from a combination of natural and artificial recharge. As a result, during the summer when the city water became too warm to be used in the plants, an increased and ample supply of cold water was available from the wells. It has been suggested that other industries at Louisville might adopt similar procedures for insuring adequate supplies of cold water during the summers.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.41.6.644","usgsCitation":"Guyton, W., 1946, Artificial recharge of glacial sand and gravel with filtered river water at Louisville, Kentucky: Economic Geology, v. 41, no. 6, p. 644-658, https://doi.org/10.2113/gsecongeo.41.6.644.","productDescription":"13 p.","startPage":"644","endPage":"658","costCenters":[],"links":[{"id":378826,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"Louisville","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.011962890625,\n 38.017803980061124\n ],\n [\n -85.4351806640625,\n 38.017803980061124\n ],\n [\n -85.4351806640625,\n 38.42777351132902\n ],\n [\n -86.011962890625,\n 38.42777351132902\n ],\n [\n -86.011962890625,\n 38.017803980061124\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"41","issue":"6","noUsgsAuthors":false,"publicationDate":"1946-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Guyton, W.F.","contributorId":11688,"corporation":false,"usgs":true,"family":"Guyton","given":"W.F.","affiliations":[],"preferred":false,"id":799763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70214508,"text":"70214508 - 1946 - Artificial recharge of productive ground-water aquifers in New Jersey","interactions":[],"lastModifiedDate":"2020-09-28T19:34:12.53488","indexId":"70214508","displayToPublicDate":"1946-09-28T14:21:42","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Artificial recharge of productive ground-water aquifers in New Jersey","docAbstract":"Artificial recharge by water spreading is practiced in several places in New Jersey. Rates of recharge ranging from 3,000 to 125,000 gallons per acre per day have been measured at the Perth Amboy Water Works, where artificial recharge of the Old Bridge sand, of upper Cretaceous age, has been practiced for more than 40 years. At the Duhernal development, which also draws from the Old Bridge sand, four or five million gallons daily is now derived from artificial recharge. This rate will probably increase with further lowering of the water table near the lake. For many years the Princeton Water Company has pumped water from a stream for recharging the Stockton sandstone, of Triassic age. The Lake Mohawk-Sparta Water Company spreads water underground by means of covered, gravel-filled ditches to recharge a shallow aquifer in its well field. The City of East Orange spreads the water from several small streams over parts of the intake area of the Quaternary beds supplying its wells. The estimated total recharge there is about two million gallons daily. Closely related to artificial recharge are those instances wherein well sites are chosen to take advantage of potential recharge from existing bodies of surface water. At the Borough of Manville no water spreading operations are conducted, but about three quarters of the water from its wells is derived by recharge from the Raritan River. The silting of water spreading areas may impair their effectiveness considerably. In some instances the growth of aquatic vegetation seems to reduce the ill effects of silting.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.41.7.726","usgsCitation":"Barksdale, H., and DeBuchananne, G., 1946, Artificial recharge of productive ground-water aquifers in New Jersey: Economic Geology, v. 41, no. 7, p. 726-737, https://doi.org/10.2113/gsecongeo.41.7.726.","productDescription":"7 p.","startPage":"726","endPage":"737","costCenters":[],"links":[{"id":378824,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey","otherGeospatial":"Perth Amboy Water Works","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.46533203125,\n 40.66813955408042\n ],\n [\n -74.058837890625,\n 40.66813955408042\n ],\n [\n -74.058837890625,\n 41.075210270566636\n ],\n [\n -74.46533203125,\n 41.075210270566636\n ],\n [\n -74.46533203125,\n 40.66813955408042\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"41","issue":"7","noUsgsAuthors":false,"publicationDate":"1946-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Barksdale, H.C.","contributorId":65912,"corporation":false,"usgs":true,"family":"Barksdale","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":799760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeBuchananne, G.D.","contributorId":91166,"corporation":false,"usgs":true,"family":"DeBuchananne","given":"G.D.","affiliations":[],"preferred":false,"id":799761,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70170446,"text":"70170446 - 1946 - Ground water in the Fargo-Moorhead area, North Dakota and Minnesota","interactions":[],"lastModifiedDate":"2018-03-05T12:14:25","indexId":"70170446","displayToPublicDate":"1946-01-01T16:00:00","publicationYear":"1946","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Ground water in the Fargo-Moorhead area, North Dakota and Minnesota","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70170446","usgsCitation":"Byers, A., Wenzel, L., Laird, W.M., and Dennis, P., 1946, Ground water in the Fargo-Moorhead area, North Dakota and Minnesota, 72 p., https://doi.org/10.3133/70170446.","productDescription":"72 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"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":320322,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Minnesota, North Dakota","otherGeospatial":"Fargo-Moorhead area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.07176208496094,\n 46.72056392864264\n ],\n [\n -97.07176208496094,\n 46.979315418679995\n ],\n [\n -96.56501770019531,\n 46.979315418679995\n ],\n [\n -96.56501770019531,\n 46.72056392864264\n ],\n [\n -97.07176208496094,\n 46.72056392864264\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5718a842e4b0ef3b7caba58a","contributors":{"authors":[{"text":"Byers, A.C.","contributorId":168773,"corporation":false,"usgs":false,"family":"Byers","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":627229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wenzel, L.K.","contributorId":18733,"corporation":false,"usgs":true,"family":"Wenzel","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":627230,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Laird, Wilson M.","contributorId":53473,"corporation":false,"usgs":true,"family":"Laird","given":"Wilson","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":627231,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dennis, P.E.","contributorId":73627,"corporation":false,"usgs":true,"family":"Dennis","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":627232,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1473,"text":"1473 - 1946 - Ground-water resources of the southwestern part of the Louisville area, Kentucky","interactions":[],"lastModifiedDate":"2014-07-11T14:26:17","indexId":"1473","displayToPublicDate":"1946-01-01T14:24:03","publicationYear":"1946","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Ground-water resources of the southwestern part of the Louisville area, Kentucky","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Louisville, KY","doi":"10.3133/1473","collaboration":"Prepared in cooperation with the Rubber Reserve Company, the City of Louisville, and Jefferson County.","usgsCitation":"Rorabaugh, M.I., 1946, Ground-water resources of the southwestern part of the Louisville area, Kentucky, 3 p., https://doi.org/10.3133/1473.","productDescription":"3 p.","numberOfPages":"3","costCenters":[],"links":[{"id":289803,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Kentucky","city":"Louisville","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.948441,37.9971 ], [ -85.948441,38.38051 ], [ -85.4051,38.38051 ], [ -85.4051,37.9971 ], [ -85.948441,37.9971 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c0ec3de4b065ccca5fe3b6","contributors":{"authors":[{"text":"Rorabaugh, Matthew Irvin","contributorId":19152,"corporation":false,"usgs":true,"family":"Rorabaugh","given":"Matthew","email":"","middleInitial":"Irvin","affiliations":[],"preferred":false,"id":143756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70160867,"text":"70160867 - 1946 - Geology and ground-water resources of the island of Hawaii","interactions":[],"lastModifiedDate":"2024-03-18T22:07:12.867365","indexId":"70160867","displayToPublicDate":"1946-01-01T11:15:00","publicationYear":"1946","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":"9","title":"Geology and ground-water resources of the island of Hawaii","docAbstract":"Hawaii, the largest island in the Hawaiian group, is 93 miles long, 76 miles wide, and covers 4,030 square miles. Mauna Loa Volcano is 13,680 feet high and Mauna Kea is 13,784 feet high. Plate 1 shows the geology, wells, springs, and water-development tunnels. Plate 2 is a map and description of points of geologic interest along the main highways. Plate 3 (same sheet as plate 2) shows highways and points of geologic interest in Hawaii National Park area. The volcanic terms used in the report are defined.
\nHawaii was built by five volcanoes. All the rocks are volcanic, except for minor amounts of sedimentary rock derived from them. Mauna Loa and Kilauea volcanoes erupt often; Hualalai Volcano last erupted in 1801; Mauna Kea has had Recent but no historic eruptions; Kohala Mountain has long been extinct.
\nKohala Mountain constitutes the northern end of the island. It is built largely of rocks of the Pololu volcanic series which are dominantly olivine basalt with a few thin intercalated beds of vitric basaltic ash. After the eruption of this series, Kohala Volcano was deeply eroded on the windward (northeastern) side, and a deep soil formed on its other slopes. Later, oligoclase andesite and trachyte lava flows, named the Hawi volcanic series, were erupted. They rest on soil at the top of the Pololu series, and lie in the valleys cut into the Pololu lavas on the windward slope. Both the Pololu and Hawi volcanics were erupted from three rift zones trending N. 35° W., S. 65° E., and S. 50° W. from the summit of the mountain. The rift zones are marked at the surface by rows or cinder cones, and beneath the surface by innumerable dikes. A caldera occupied the summit of the mountain at the beginning of the eruption of the Hawi lavas, and for a time confined the flows. It was gradually filled and the lava escaped northeastward into the large valleys. Some of the caldera faults can still be traced. A shallow graben indents the summit now.
\nSouth of Kohala Mountain lies the much larger volcano of Mauna Kea. The early rocks of Mauna Kea constitute the Hamakua volcanic series. The lower member of this series consists chiefly of olivine basalt flows with intercalated thin beds of vitric basaltic ash. The olivine basalt of the lower member changes gradationally into the upper member, in which basalt and olivine basalt arc still abundant, but andesite also is present. Lavas of the upper member interfinger with Hawi lavas of Kohala Mountain. The Hamakua volcanic series is mantled with Pahala ash 5 to 20 feet thick, above which lie the rocks of the Laupahoehoe volcanic series. Locally the two series are separated by erosional unconformity, The Laupahoehoe lavas are dominantly andesite. The andesites erupted after the last glacial epoch are mapped separately on plate 1. The Laupahoehoe volcanic series, and probably also the Hamakua volcanic series, were erupted principally from three rift zones, trending west, northeast and south-southeast from the summit of the mountain. The upper slopes are studded with many large cinder cones, lying principally along the rift zones. Late in its geologic history, Mauna Kea was capped by a small glacier, presumably contemporaneous with the Wisconsin stage of glaciation in North America, which left conspicuous terminal, lateral, and ground moraines. Deposits exposed in canyons on the southern slope, formerly believed to be of glacial origin, are now believed to be volcanic explosion breccias.
\nThe main bulk of Hualalai Volcano is built of basalts of the Hualalai volcanic series. One flow of andesite has been found. The cinder and spatter cones lie principally along three rift zones which trend northwest, north, and southeast from the summit. On the northern slope of Hualalai Volcano lies the large trachyte pumice cone of Puu Waawaa, and its thick flow of trachyte. These are grouped together as the Waawaa volcanics. They are partly buried by later basalts from both Hualalai and Mauna Loa. The last eruption of Hualalai Volcano, in 1800–1801, produced olivine basalt.
\nThe earliest exposed rocks of Mauna Loa comprise the Ninole volcanic series. Several beds of altered vitric ash are intercalated with the lavas. Following eruption of the Ninole series, a long period or quiescence occurred, during which deep amphitheater-headed valleys were cut. This was followed by the eruption of the Kahuku volcanic series, consisting mostly of lavas with some thin beds of ash. The Rahuku series is overlain by the Pahala ash, which overlies also the Hilina volcanic series on Kilauea, the Hamakua volcanic series on Mauna Kea, and the Hawi volcanic series on Kohala, providing a rough datum for correlation of the lavas of the four mountains. Deposition of the Pahala ash was followed on Mauna Loa by eruption of the Kau volcanic series, which has continued until the present time. The historic and flaws of the Kau series are mapped separately on plate 1. The historic eruptions and volcanic activity of Mauna Loa are briefly described. The western and southern slopes of Mauna Loa are cut by normal faults along which the lower flanks of the mountain have slipped seaward.
\nThe Kau volcanic series and presumably also the Kahuku and Ninole volcanic series were erupted principally from vents along two rift zones which extend northeast and southwest from the summit caldera. The lavas of all three series are preponderantly olivine basalt. Many of the lavas contain small amounts of hypersthene.
\nThe Pahala ash on the northeastern and eastern slopes of Mauna Loa was derived largely from Mauna Kea. West and south of Kilauea Caldera, however, it was derived principally from Kilauea. Minor amounts were contributed by eruptions of Mauna Loa. It is a vitric basaltic ash, now generally altered to palagonite.
\nThe earliest exposed lavas and thin intercalated ash beds of Kilauea Volcano comprise the Hilina volcanic series. These are capped by the Pahala ash, which in turn, is overlain by the lavas and thin ash beds of the Puna volcanic series. The volcanics of both series were erupted along two rift zones, one extending southwestward from Kilauea Caldera, and the other extending southeastward for 5 miles and then bending sharply east by north. The lavas of both series are very largely olivine basalt. A few flows contain hypersthene. Augite phenocrysts are common in Mauna Loa lavas, but rare in those of Kilauea, indicating that crystallization has not progressed as far in the magma chamber of Kilauea Volcano as in that of Mauna Loa. Eruption of the Puna volcanic series has continued until the present time, the historic flows being separated from the prehistoric ones on plate 1. The historic eruptions and volcanic activity of Kilauea are briefly described.
\nKilauea Volcano originated on the southern slope of Mauna Loa where faults intersected the Eastern Fundamental Fissure of the Hawaiian Archipelago. The southern flank of Kilauea is cut by normal faults, along which the southern part is sliding seaward.
The volcanoes of the island of Hawaii are believed to have started their activity in the Tertiary period. The great erosional period which followed deposition of the Pololu and Ninole volcanic series is placed near the end of the Pliocene. The Hilina and Hamakua volcanic series were probably erupted in the late Pliocene and earlier Pleistocene. The Hawi volcanic series and the Waawaa volcanics are probably early or middle Pleistocene in age. The main period of deposition of the Pahala ash was probably late in the middle Pleistocene or early in the upper Pleistocene. The Laupahoehoe volcanic series is late Pleistocene and Recent in age, most of the flows antedating the Wisconsin glaciation. The Hualalai volcanic series probably extends from Tertiary to historic time, and the Kau and Puna volcanic series from late Pleistocene to the present. A chapter is devoted to the petrography of the rocks in which are listed all reliable chemical rock analyses.
The rocks of the island are highly permeable. Most of the rainfall sinks quickly into the ground. Perennial streams are present only on the windward slopes of Kohala Mountain and Mauna Kea. Most of the water sinks rapidly to the basal water table, where it floats on salt water according to the Ghyben-Herzberg principle. Basal water escapes in springs at or near sea level all along the coast. Only a very small proportion of it is recovered in wells. Along the windward coasts the basal water is of good quality and large supplies await development. Along the leeward coasts most of the basal water is brackish.
\nIn Kohala Mountain, much water is perched on ash beds in the Pololu volcanic series and on ash and soil at the base of the Hawi volcanic series. It escapes in perched springs in the big valleys and along the windward sea cliff and is recovered in tunnels. Along the windward slope of Mauna Keu, small amounts of water are perched by ash beds and dense lava flows in the Hamakua volcanic series. Small perched springs issue from these structures and water is recovered by tunnels. In the Kau District ash beds perch considerable water, which is recovered by many tunnels. On the southern slope of Mauna Kea small springs are perched by beds of hill wash.
Dikes in the rift zones are relatively impermeable, but enclose masses of permeable rock. Water is confined at high level in the interdike compartments in Kohala Mountain, and probably in the other volcanoes. It escapes in high-level springs in the deep valleys on Kohala Mountain; some of it is recovered by tunnels.
It is estimated that an average of about 13,085 million gallons of water a day falls as rain over the whole island. Of this only about 2.5 percent is visibly discharged from wells, tunnels, and springs. Large supplies of basal groundwater await development. Projects for development of additional water for the city of Hilo and the Kona District are described.
\nChemical analyses of water, water supplies of towns and villages, descriptions of wells, springs, and tunnels, and discharge records of numerous springs and tunnels are given in tabulated form.
","language":"English","publisher":"Hawaii Division of Hydrography","publisherLocation":"Honolulu","collaboration":"Prepared in cooperation with the Geological Survey, United States Department of the Interior","usgsCitation":"Stearns, H.T., and Macdonald, G., 1946, Geology and ground-water resources of the island of Hawaii: Bulletin 9, xiii, 363 p.","productDescription":"xiii, 363 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":221,"text":"Division of Hydrography","active":false,"usgs":true}],"links":[{"id":426757,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19533.htm","linkFileType":{"id":5,"text":"html"}},{"id":313178,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/stearns/Hawaii.pdf","text":"Report","size":"92.6 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A.","contributorId":52273,"corporation":false,"usgs":true,"family":"Macdonald","given":"Gordon A.","affiliations":[],"preferred":false,"id":584091,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70195896,"text":"70195896 - 1946 - Ground water in beach deposits of glacial Lake Agassiz near Mountain, Pembina County, North Dakota","interactions":[],"lastModifiedDate":"2018-03-07T13:30:20","indexId":"70195896","displayToPublicDate":"1946-01-01T00:00:00","publicationYear":"1946","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5646,"text":"North Dakota Ground Water Studies","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"2","title":"Ground water in beach deposits of glacial Lake Agassiz near Mountain, Pembina County, North Dakota","docAbstract":"No abstract available.
","language":"English","publisher":"North Dakota State Water Conservation Commission","usgsCitation":"Akin, P., 1946, Ground water in beach deposits of glacial Lake Agassiz near Mountain, Pembina County, North Dakota: North Dakota Ground Water Studies 2, 24 p.","productDescription":"24 p.","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":352289,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6d84e4b0da30c1bfe568","contributors":{"authors":[{"text":"Akin, P.D.","contributorId":104471,"corporation":false,"usgs":true,"family":"Akin","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":730418,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70198526,"text":"70198526 - 1945 - Industrial limestones and dolomites in Virginia: northern and central parts of the Shenandoah Valley","interactions":[],"lastModifiedDate":"2018-08-06T16:49:43","indexId":"70198526","displayToPublicDate":"2018-01-01T16:47:16","publicationYear":"1945","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Industrial limestones and dolomites in Virginia: northern and central parts of the Shenandoah Valley","docAbstract":"The area described in this report includes the northern and central parts of Shenandoah Valley in Virginia extending from the West Virginia line southwestward to the vicinity of Greenville, Augusta County. It contains extensive deposits of high-calcium limestone averaging more than 97 per cent calcium carbonate. The Mosheim limestone, composed largely of high-calcium limestone, is the important \"quarry rock\" of the area. Other formations containing high-calcium limestone include locally a part of the Lenoir, the upper part of the Chambersburg in the western belts of Shenandoah County, and relatively thin units in the Beekmantown along the eastern side of the Massanutten Mountain syncline north of Rockingham County. Some of the thickest deposits of high-calcium limestone near railroads are in Frederick, Shenandoah, Rockingham, and Augusta counties.
Extensive exposures of the Tomstown (Shady) dolomite, containing more than 42 per cent magnesium carbonate, occur in the eastern part df Clarke County. Locally near the North Mountain fault in parts of Shenandoah and Rockingham counties, 80 feet or more of brecciated dolomite in the Elbrook formation contains about 43.5 per cent magnesium
carbonate and generally less than 2 per cent silica. Most of the sampled dolomite units in the Elbrook, Conococheague, and Beekmantown formations contain less than 40 per cent magnesium carbonate.
Special study was made of the carbonate rocks suitable for chemical use and favorably located near railroads. Limestones, containing less than 95 per cent calcium carbonate, were studied locally in some detail. Descriptions of the belts of industrial limestone and dolomite are supplemented by geologic maps and sections, and chemical analyses.
","largerWorkTitle":"Virginia Division of Mineral Resources Bulletin","publisher":"Virginia Geological Survey","publisherLocation":"Charlottesville, VA","usgsCitation":"Edmundson, R., 1945, Industrial limestones and dolomites in Virginia: northern and central parts of the Shenandoah Valley, v. 65, 195 p.","productDescription":"195 p.","costCenters":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"links":[{"id":356224,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":356223,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.dmme.virginia.gov/commercedocs/BUL_65.pdf","text":"Document"}],"country":"United States","state":"Virginia","otherGeospatial":"Shenandoah Valley","volume":"65","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Edmundson, R.S.","contributorId":206778,"corporation":false,"usgs":false,"family":"Edmundson","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":741787,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70178707,"text":"70178707 - 1945 - The Ogden Valley artesian reservoir","interactions":[],"lastModifiedDate":"2016-12-09T11:30:45","indexId":"70178707","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1945","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"2","title":"The Ogden Valley artesian reservoir","docAbstract":"Ogden Valley, in Weber County, Utah, contains an artesian reservoir from which the city of Ogden obtains all except a small part of its municipal water supply. A detailed investigation of the ground-water resources of Ogden Valley, and particularly of this artesian reservoir, was made by the Geological Survey, United States Department of the Interior, in cooperation with the city of Ogden between 1932 and 1934, and the results of this investigation have been reported by Leggette and Taylor.1 The present paper, which might be termed a sequel to that report, is based on data collected during those years, augmented by records that have been obtained (1935-1940) by the Geological Survey as part of a State-wide project in cooperation with the Utah State Engineer. The conclusions drawn from the study of these records and presented in detail in the following pages are as follows: (1) The artesian reservoir is filled to capacity nearly every year during the spring run-off from melting snow; (2) after the annual freshet, the recharge to the reservoir is insufficient to balance the discharge from artesian wells, which ordinarily is at a maximum during the summer; the reservoir is depleted and is not filled again until the following spring; (3) during the periods when the artesian reservoir is not full the rate of recharge is more or less proportional to the inflow to the valley by streams, except that rain on the recharge area may be of sufficient intensity to contribute some water by infiltration and deep penetration; and (4) the artesian reservoir thus serves to store water that would otherwise be lost to Great Salt Lake in the excess spring overflow, and available records indicate that water used by increased draft from wells would be replenished in normal years by increased recharge during the spring freshet.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Thomas, H.E., 1945, The Ogden Valley artesian reservoir: Technical Publication 2, 37 p.","productDescription":"37 p.","numberOfPages":"39","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331476,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331475,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w9200081.pdf"},{"id":331474,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-070"}],"country":"United States","state":"Utah","county":"Weber County","otherGeospatial":"Ogden Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.84562683105469,\n 41.25148375190403\n ],\n [\n -111.74606323242188,\n 41.23134745732574\n ],\n [\n -111.74400329589844,\n 41.29276955352782\n ],\n [\n -111.80992126464844,\n 41.313918406594375\n ],\n [\n -111.84906005859375,\n 41.29586493605656\n ],\n [\n -111.84562683105469,\n 41.25148375190403\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58468af0e4b04fc80e5236e3","contributors":{"authors":[{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":654889,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70160494,"text":"70160494 - 1945 - Columnaris as a disease of cold-water fishes","interactions":[],"lastModifiedDate":"2016-01-04T08:17:39","indexId":"70160494","displayToPublicDate":"2015-06-22T00:00:00","publicationYear":"1945","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3623,"text":"Transactions of the American Entomological Society","active":true,"publicationSubtype":{"id":10}},"title":"Columnaris as a disease of cold-water fishes","docAbstract":"A natural outbreak of columnaris disease among wild adult and hatchery-reared fingerling salmon in the State of Washington is described. The disease is identified by the recovery of the causative organism, Bacillus columnaris Davis, which may be readily identified by its characteristic action in forming columns on the surfaces of infected material held in a water mount on a microscope slide. The gross lesions vary in appearance according to the particular organ affected but are formed, essentially, by the progressive necrosis and disintegration of the tissues. The tissues primarily affected are skin, body musculature, and the gills. Cultivation of the causative organism in tryptone solutions is recorded. Controlled, laboratory-induced infections indicate that among the cold-water fishes, columnaris disease is of little consequence to fingerlings at water temperatures below 55° F., but becomes highly pathogenic at temperatures in excess of 70° F. Between these temperature thresholds, the degree and severity of the infection is markedly influenced by factors adverse to the host. No effective control measures have been found.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1943)73[32:CAADOC]2.0.CO;2","usgsCitation":"American Fisheries Society, 1945, Columnaris as a disease of cold-water fishes: Transactions of the American Entomological Society, v. 73, no. 1, p. 32-36, https://doi.org/10.1577/1548-8659(1943)73[32:CAADOC]2.0.CO;2.","productDescription":"5 p.","startPage":"32","endPage":"36","numberOfPages":"5","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312571,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.02636718749999,\n 48.951366470947725\n ],\n [\n -117.00439453125,\n 46.46813299215554\n ],\n [\n -116.8505859375,\n 46.01222384063236\n ],\n [\n -119.0478515625,\n 46.027481852486645\n ],\n [\n -120.52001953124999,\n 45.69083283645816\n ],\n [\n -122.10205078125,\n 45.583289756006316\n ],\n [\n -122.49755859375,\n 45.55252525134013\n ],\n [\n -123.11279296875001,\n 46.13417004624326\n ],\n [\n -123.99169921875,\n 46.164614496897094\n ],\n [\n -124.01367187499999,\n 46.875213396722685\n ],\n [\n -124.8486328125,\n 48.38544219115483\n ],\n [\n -123.96972656249999,\n 48.25394114463431\n ],\n [\n -123.28857421875,\n 48.42920055556841\n ],\n [\n -123.22265625000001,\n 48.79239019646406\n ],\n [\n -123.31054687499999,\n 49.05227025601607\n ],\n [\n -122.58544921875,\n 49.009050809382046\n ],\n [\n -117.02636718749999,\n 48.951366470947725\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567930c2e4b0da412f4fb541"} ,{"id":70040233,"text":"70040233 - 1945 - Record of wells in Suffolk County, N.Y., Supplement 1","interactions":[],"lastModifiedDate":"2012-10-09T17:16:16","indexId":"70040233","displayToPublicDate":"2012-01-01T14:55:05","publicationYear":"1945","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-9","title":"Record of wells in Suffolk County, N.Y., Supplement 1","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","usgsCitation":"Roberts, C., and Brashears, M., 1945, Record of wells in Suffolk County, N.Y., Supplement 1: Bulletin GW-9, 155 p.; 1 Plate.","productDescription":"155 p.; 1 Plate","numberOfPages":"155","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262495,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.7600,40.4800 ], [ -79.7600,45.0200 ], [ -71.8600,45.0200 ], [ -71.8600,40.4800 ], [ -79.7600,40.4800 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a27be4b0e8fec6cdb60a","contributors":{"authors":[{"text":"Roberts, C.M.","contributorId":75107,"corporation":false,"usgs":true,"family":"Roberts","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":467940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brashears, M.L. Jr.","contributorId":23212,"corporation":false,"usgs":true,"family":"Brashears","given":"M.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":467939,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70040266,"text":"70040266 - 1945 - Correlation of ground-water levels and precipitation on Long Island, New York","interactions":[],"lastModifiedDate":"2021-01-28T21:10:31.346353","indexId":"70040266","displayToPublicDate":"2012-01-01T10:51:17","publicationYear":"1945","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-14","title":"Correlation of ground-water levels and precipitation on Long Island, New York","docAbstract":"No abstract available.
","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","usgsCitation":"Jacob, C.E., 1945, Correlation of ground-water levels and precipitation on Long Island, New York: Bulletin GW-14, 24 p.","productDescription":"24 p.","numberOfPages":"24","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.992919921875,\n 40.54720023441049\n ],\n [\n -73.42163085937499,\n 40.543026009955014\n ],\n [\n -72.476806640625,\n 40.78885994449482\n ],\n [\n -71.7791748046875,\n 41.054501963290505\n ],\n [\n -72.21313476562499,\n 41.19105625669688\n ],\n [\n -72.6361083984375,\n 41.025499378313754\n ],\n [\n -73.157958984375,\n 41.0130657870063\n ],\n [\n -73.6907958984375,\n 40.925964939514294\n ],\n [\n -73.927001953125,\n 40.78054143186033\n ],\n [\n -74.0313720703125,\n 40.718119379753446\n ],\n [\n -74.0313720703125,\n 40.59727063442024\n ],\n [\n -73.992919921875,\n 40.54720023441049\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50d9cbd1e4b07a5aecdeea0a","contributors":{"authors":[{"text":"Jacob, C. E.","contributorId":64504,"corporation":false,"usgs":true,"family":"Jacob","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":467981,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70040264,"text":"70040264 - 1945 - The water table in the western and central parts of Long Island, New York","interactions":[],"lastModifiedDate":"2012-10-11T17:16:22","indexId":"70040264","displayToPublicDate":"2012-01-01T10:37:03","publicationYear":"1945","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-12","title":"The water table in the western and central parts of Long Island, New York","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","usgsCitation":"Jacob, C.E., 1945, The water table in the western and central parts of Long Island, New York: Bulletin GW-12, 24 p.; 2 Plates.","productDescription":"24 p.; 2 Plates","numberOfPages":"24","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e54c84e4b0a4aa5bb01030","contributors":{"authors":[{"text":"Jacob, C. E.","contributorId":64504,"corporation":false,"usgs":true,"family":"Jacob","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":467978,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175642,"text":"70175642 - 1945 - Geology and ground-water resources of Thomas County, Kansas","interactions":[],"lastModifiedDate":"2016-08-19T11:41:10","indexId":"70175642","displayToPublicDate":"2010-06-30T10:30:00","publicationYear":"1945","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 Thomas County, Kansas","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lawrence, KS","usgsCitation":"Frye, J., 1945, Geology and ground-water resources of Thomas County, Kansas: Kansas Geological Survey Bulletin, v. 59, Report: 110 p.","productDescription":"Report: 110 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":326730,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":326729,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"59","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58acfe4b03bcb0104bba7","contributors":{"authors":[{"text":"Frye, J.C.","contributorId":35067,"corporation":false,"usgs":true,"family":"Frye","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":645912,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5230032,"text":"5230032 - 1945 - Some recent publications on management and propagation of waterfowl","interactions":[],"lastModifiedDate":"2014-07-21T10:11:50","indexId":"5230032","displayToPublicDate":"2009-06-09T11:33:00","publicationYear":"1945","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"267","title":"Some recent publications on management and propagation of waterfowl","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Nestler, R.B., 1945, Some recent publications on management and propagation of waterfowl: Wildlife Leaflet 267, 5 p.","productDescription":"5 p.","numberOfPages":"5","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":112332,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015007538500?urlappend=%3Bseq=463"},{"id":202797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e7e4b07f02db5e851d","contributors":{"authors":[{"text":"Nestler, R. B.","contributorId":43866,"corporation":false,"usgs":true,"family":"Nestler","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":343395,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5230017,"text":"5230017 - 1945 - Plant-food resources for waterfowl in the Pacific Northwest","interactions":[],"lastModifiedDate":"2012-02-02T00:15:22","indexId":"5230017","displayToPublicDate":"2009-06-09T09:33:22","publicationYear":"1945","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":235,"text":"Washington Department of Game, Biological Bulletin","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"No. 7","title":"Plant-food resources for waterfowl in the Pacific Northwest","language":"English","collaboration":"OCLC 18806095","usgsCitation":"Scheffer, T., and Hotchkiss, N., 1945, Plant-food resources for waterfowl in the Pacific Northwest: Washington Department of Game, Biological Bulletin No. 7, 39.","productDescription":"39","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200863,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf48","contributors":{"authors":[{"text":"Scheffer, T.H.","contributorId":87256,"corporation":false,"usgs":true,"family":"Scheffer","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":343371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hotchkiss, N.","contributorId":48655,"corporation":false,"usgs":true,"family":"Hotchkiss","given":"N.","affiliations":[],"preferred":false,"id":343370,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5200007,"text":"5200007 - 1945 - The aquatic and marsh vegetation of Minnesota and its value to waterfowl","interactions":[],"lastModifiedDate":"2012-02-02T00:15:22","indexId":"5200007","displayToPublicDate":"2009-06-09T09:33:21","publicationYear":"1945","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":221,"text":"Technical Bulletin","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"No. 3.","title":"The aquatic and marsh vegetation of Minnesota and its value to waterfowl","language":"English","publisher":"Minnesota Department of Conservation.","usgsCitation":"Moyle, J., and Hotchkiss, N., 1945, The aquatic and marsh vegetation of Minnesota and its value to waterfowl: Technical Bulletin No. 3., 122.","productDescription":"122","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669747","contributors":{"authors":[{"text":"Moyle, J.B.","contributorId":54323,"corporation":false,"usgs":true,"family":"Moyle","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":326809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hotchkiss, N.","contributorId":48655,"corporation":false,"usgs":true,"family":"Hotchkiss","given":"N.","affiliations":[],"preferred":false,"id":326808,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":57118,"text":"ofr45110 - 1945 - Water facts for Oklahoma","interactions":[],"lastModifiedDate":"2014-05-14T13:03:03","indexId":"ofr45110","displayToPublicDate":"1995-01-01T07:00:00","publicationYear":"1945","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"45-110","title":"Water facts for Oklahoma","docAbstract":"Water descends from the clouds, and forms rivers, lakes, and seas. It is delivered to the earth absolutely free, not in accordance with man-made specifications or orders but at the caprice of the elements. Hence man to realize fully the benefits of this incomparable and recurring resource must have full knowledge of its erratic occurrence before ways and means may be devised for putting water to beneficial use and for preventing it from doing harm. Water facts are essential for the effective and efficient utility of water.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington D.C.","doi":"10.3133/ofr45110","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1945, Water facts for Oklahoma: U.S. Geological Survey Open-File Report 45-110, 35 p., https://doi.org/10.3133/ofr45110.","productDescription":"35 p.","costCenters":[],"links":[{"id":287133,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1945/0110/report.pdf"},{"id":287134,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1945/0110/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0025,33.6158 ], [ -103.0025,37.0023 ], [ -94.4307,37.0023 ], [ -94.4307,33.6158 ], [ -103.0025,33.6158 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628dea","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":533038,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55535,"text":"ofr4524 - 1945 - Water utilization in the Nooksack River, Washington","interactions":[],"lastModifiedDate":"2017-06-21T10:43:00","indexId":"ofr4524","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1945","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"45-24","title":"Water utilization in the Nooksack River, Washington","docAbstract":"The primary purpose of the investigation of the water resources\nof the Nooksack River was land classification. The\nNooksack basin lies largely within the Mt. Baker National Forest\nand a considerable area of public lands will be involved\nin any plan for the ultimate development of its water power.\nSurveys on a scale of 1:24,000 and 1:31,680 were made from the\nmouth of the Nooksack River upstream to include such stretches\nof ell streams in the basin as appear to have sufficient flow\nand head or storage possibilities to attract future power development.\nA dam site on the main stream and one on South Fork\nwere mapped on a scale of 400 feet to the inch. A dam site on\nthe main stream near Deming was mapped in 1938 by the U.S. Engineers.\nAreas within the basin not covered by these surveys\nare largely shown on quadrangle maps, The lower basin has been\nmapped on a scale of one inch to the mile, and the upper basin\non a scale of one quarter inch to the mile (Mt. Baker district).\nThese surveys and a brief record of discharge on the principal \nstreams of the basin together with a general reconnaissance\nform the basis of this report. It outlines roughly a plan of\ndevelopment showing the potential power of the Nooksack River\nand its tributaries, and considers briefly the problems of flood\ncontrol and irrigation within the basin.","language":"English","doi":"10.3133/ofr4524","usgsCitation":"Helland, R., 1945, Water utilization in the Nooksack River, Washington: U.S. Geological Survey Open-File Report 45-24, 86 p., https://doi.org/10.3133/ofr4524.","productDescription":"86 p.","costCenters":[],"links":[{"id":287119,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1945/0024/report-thumb.jpg"},{"id":287118,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1945/0024/report.pdf"}],"country":"United States","state":"Washington","otherGeospatial":"Nooksock River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681db8","contributors":{"authors":[{"text":"Helland, R.O.","contributorId":72458,"corporation":false,"usgs":true,"family":"Helland","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":253659,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2435,"text":"wsp965 - 1945 - Surface water supply of Hawaii : July 1, 1941, to June 30, 1942","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp965","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1945","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":"965","title":"Surface water supply of Hawaii : July 1, 1941, to June 30, 1942","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp965","usgsCitation":"Parker, G., and Carson, M.H., 1945, Surface water supply of Hawaii : July 1, 1941, to June 30, 1942: U.S. Geological Survey Water Supply Paper 965, iv, 134 p. :ill. ;24 cm., https://doi.org/10.3133/wsp965.","productDescription":"iv, 134 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0965/report-thumb.jpg"},{"id":28505,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0965/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697831","contributors":{"authors":[{"text":"Parker, Glenn L.","contributorId":42944,"corporation":false,"usgs":true,"family":"Parker","given":"Glenn L.","affiliations":[],"preferred":false,"id":145195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carson, Max H.","contributorId":21132,"corporation":false,"usgs":true,"family":"Carson","given":"Max","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145194,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}