No abstract available.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8640(1936)323[14:TIITAO]2.0.CO;2","usgsCitation":"Hile, R., 1937, The increase in the abundance of the yellow pike perch, Stizostedion vitreum (Mitchill), in Lakes Huron and Michigan, in relation to the artificial propagation of the species: Progressive Fish-Culturist, v. 66, p. 143-159, https://doi.org/10.1577/1548-8640(1936)323[14:TIITAO]2.0.CO;2.","productDescription":"16 p.","startPage":"143","endPage":"159","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"66","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a85e4b07f02db64d783","contributors":{"authors":[{"text":"Hile, Ralph","contributorId":48510,"corporation":false,"usgs":true,"family":"Hile","given":"Ralph","email":"","affiliations":[],"preferred":false,"id":308235,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000424,"text":"1000424 - 1937 - The Artificial propagation of the commercial species of fish of the Great Lakes","interactions":[],"lastModifiedDate":"2016-02-04T10:54:49","indexId":"1000424","displayToPublicDate":"1937-01-01T00:00:00","publicationYear":"1937","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":"The Artificial propagation of the commercial species of fish of the Great Lakes","docAbstract":"No abstract available.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8640(1937)428[8:TAPOTC]2.0.CO;2","usgsCitation":"Van Oosten, J., 1937, The Artificial propagation of the commercial species of fish of the Great Lakes: Progressive Fish-Culturist, v. 2, p. 605-612, https://doi.org/10.1577/1548-8640(1937)428[8:TAPOTC]2.0.CO;2.","productDescription":"8 p.","startPage":"605","endPage":"612","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":129043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c2c","contributors":{"authors":[{"text":"Van Oosten, John","contributorId":23479,"corporation":false,"usgs":true,"family":"Van Oosten","given":"John","email":"","affiliations":[],"preferred":false,"id":308536,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000425,"text":"1000425 - 1937 - Doom of the Great Lakes fisheries","interactions":[],"lastModifiedDate":"2012-02-02T00:04:12","indexId":"1000425","displayToPublicDate":"1937-01-01T00:00:00","publicationYear":"1937","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":720,"text":"American Forests","active":true,"publicationSubtype":{"id":10}},"title":"Doom of the Great Lakes fisheries","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Forests","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Van Oosten, J., 1937, Doom of the Great Lakes fisheries: American Forests, v. 43, no. 3, p. 103, 144-105,145.","productDescription":"p. 103-105,144-145","startPage":"103, 144","endPage":"105,145","numberOfPages":"5","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":129044,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63603e","contributors":{"authors":[{"text":"Van Oosten, John","contributorId":23479,"corporation":false,"usgs":true,"family":"Van Oosten","given":"John","email":"","affiliations":[],"preferred":false,"id":308537,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70196443,"text":"70196443 - 1937 - Disease relationship of domestic stock and wildlife","interactions":[],"lastModifiedDate":"2018-04-06T13:47:57","indexId":"70196443","displayToPublicDate":"1937-01-01T00:00:00","publicationYear":"1937","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Disease relationship of domestic stock and wildlife","docAbstract":"From the time that western civilization established itself on the North American continent until very recent years, little thought was given to the diseases, or other forms of loss, in game. In the process of bringing civilization and the incidental domestic arts and trades to the United States it appears to have been the policy to establish domestic farm stock on the land just as abundantly as the carrying capacity of land would tolerate. And judged by the low quality of many of our present farm animals, it is evident that in many cases the land was, and is now, overstocked and undermanaged. In traveling over this country one is impressed by the lack of uniformity, imperfect physical development, and poor state of nutrition of much of the domestic livestock. It would appear that the wild animals unhampered by fencing and other restraint such as controlled mating, feed selection, and enforced habitat in contaminated or polluted environment, have a better chance for perfect growth and complete development to a size and proportion normal for those species.
While all of the factors mentioned produce a definitely deleterious result on the welfare of animal life, that of contaminated or polluted environment is by no means the least. The stunting action of disease on the growth of the young is too well known to admit of controversy. The impairment of function of vital organs due to minute cellular changes resulting from sub-acute or chronic infections prevents normal growth. Through centuries of enforced survival in densely congested pastures, pens, and stables, a certain degree of acquired resistance to many diseases has been built up in farm stock. If it were not so, very few barnyard animals would ever survive the conditions generally seen in our agricultural districts. Manure heaps, quantities of partly spoiled feed, and decaying masses of vegetation and refuse have come to be regarded as a natural part of the barnyard scene.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Transactions of the second north american wildlife conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Second north american wildlife conference","conferenceDate":"March 1-4, 1937","conferenceLocation":"St. Louis, MO","language":"English","publisher":"American Wildlife Institute","publisherLocation":"Washington, D.C.","usgsCitation":"Shillinger, J., 1937, Disease relationship of domestic stock and wildlife, in Transactions of the second north american wildlife conference, St. Louis, MO, March 1-4, 1937, p. 298-302.","productDescription":"5 p.","startPage":"298","endPage":"302","costCenters":[],"links":[{"id":353235,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6f71e4b0da30c1bfe575","contributors":{"authors":[{"text":"Shillinger, J.E.","contributorId":47879,"corporation":false,"usgs":true,"family":"Shillinger","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":732926,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70200389,"text":"70200389 - 1937 - Plan of Muddy River, Nevada: above a point 3 miles below Overton, miscellaneous dam sites","interactions":[],"lastModifiedDate":"2018-10-17T13:11:14","indexId":"70200389","displayToPublicDate":"1934-01-01T14:10:54","publicationYear":"1937","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Plan of Muddy River, Nevada: above a point 3 miles below Overton, miscellaneous dam sites","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70200389","usgsCitation":"U.S. Geological Survey, 1937, Plan of Muddy River, Nevada: above a point 3 miles below Overton, miscellaneous dam sites, 2 Plates: 27.94 x 22.02 inches and 27.73 x 21.90 inches, https://doi.org/10.3133/70200389.","productDescription":"2 Plates: 27.94 x 22.02 inches and 27.73 x 21.90 inches","costCenters":[],"links":[{"id":358485,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70200389/plate-2.pdf","text":"Sheet B","linkFileType":{"id":1,"text":"pdf"}},{"id":358483,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70200389/report-thumb.jpg"},{"id":358484,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70200389/plate-1.pdf","text":"Sheet A","linkFileType":{"id":1,"text":"pdf"}}],"scale":"31680","country":"United States","state":"Nevada","otherGeospatial":"Muddy River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.949951171875,\n 36.52067329034796\n ],\n [\n -114.400634765625,\n 36.52067329034796\n ],\n [\n -114.400634765625,\n 36.80598611937673\n ],\n [\n -114.949951171875,\n 36.80598611937673\n ],\n [\n -114.949951171875,\n 36.52067329034796\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128240,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":748864,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206349,"text":"70206349 - No Year - Origin of the bedding replacement deposits of fluorspar in the Illinois field","interactions":[],"lastModifiedDate":"2019-10-30T17:45:13","indexId":"70206349","displayToPublicDate":"1937-05-01T17:41:22","publicationYear":"1937","noYear":true,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Origin of the bedding replacement deposits of fluorspar in the Illinois field","docAbstract":"The banded fluorspar deposits of the Cave In Rock district are attributed to replacement of limestone and the preservation of bedding and cross-bedding of the rock. The solutions contained hydrofluoric acid which reacted with CaCO 3 . The replacement was stoichiometrical, with consequent reduction of volume, but continued deposition of calcium fluoride, brought in from other points, partly or completely filled the voids. Thus, the pure bands display a comb structure, and represent replacement of pure limestone laminae. The less pure granular bands, devoid of comb structure, reflect the alternating, impure bands of the rock in which the fine-grained impurities (ferriferous carbonate, clay, et al) were disseminated. Recrystallization of clastic quartz grains in some calcareous sandstone layers resulted in the formation of bands of quartz grains. The writer dissents from the views of Bastin who believes the banding is due to rhythmic precipitation. Chemistry and controlling structural conditions are discussed.
","language":"English ","doi":"10.2113/gsecongeo.32.3.364","issn":" 03610128","usgsCitation":"Currier, L., 1937, Origin of the bedding replacement deposits of fluorspar in the Illinois field: Economic Geology, v. 32, no. 3, p. 364-386, https://doi.org/10.2113/gsecongeo.32.3.364.","productDescription":"23 p. 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\"}}]}","volume":"32","issue":"3","noUsgsAuthors":false,"publicationDate":"1937-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Currier, L.W.","contributorId":61489,"corporation":false,"usgs":true,"family":"Currier","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":774250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180145,"text":"70180145 - 1936 - Ground water investigations in Utah to June 30, 1936: A part of Chapter 8 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","interactions":[],"lastModifiedDate":"2017-01-24T15:25:32","indexId":"70180145","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5276,"text":"Utah State Engineer Biennial Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"20","chapter":"8","title":"Ground water investigations in Utah to June 30, 1936: A part of Chapter 8 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","docAbstract":"During the past few years of drouth the importance of ground-water supplies has become more fully appreciated. During this time, because of subnormal replenishment of the ground-water reservoirs and the increased withdrawals from wells, the ground-water levels have declined in most developed areas in the State, a condition which has made the well owners acutely aware that ground water is not inexhaustible. Numerous cases of contention between well owners resulted in increased demands for adequate regulation of the appropriation and use of ground water. Realizing that more information concerning the ground water of the State was imperative, not only to administer the ground-water regulations but to prepare for the conservation and replenishment of existing supplies and development of new supplies, the State Legislature enacted, during its 1935 session, Senate Bill 206, which authorized the State Engineer to make an investigation of the ground water of the State. To provide for the expenses of the investigation, the bill allotted /$10,000 to the State Engineer, this sum to be matched by a State or Federal organization, and the investigation to be carried out co-operatively during the biennium beginning July 1, 1935. A co-operative agreement between the State Engineer and the United States Geological Survey was made on July 1, 1935.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Taylor, G., and Thomas, H.E., 1936, Ground water investigations in Utah to June 30, 1936: A part of Chapter 8 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936: Utah State Engineer Biennial Report 20, 16 p.","productDescription":"16 p.","startPage":"91","endPage":"106","numberOfPages":"16","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333855,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333854,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-365","text":"Full Text of Biennial Report"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5888770de4b05ccb964bab69","contributors":{"authors":[{"text":"Taylor, G.H.","contributorId":85158,"corporation":false,"usgs":true,"family":"Taylor","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":660502,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":660503,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70180141,"text":"70180141 - 1936 - Stream-gaging work: Section 2 of Chapter 6 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","interactions":[],"lastModifiedDate":"2017-01-24T15:11:23","indexId":"70180141","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5276,"text":"Utah State Engineer Biennial Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"20","chapter":"6","title":"Stream-gaging work: Section 2 of Chapter 6 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","docAbstract":"Stream gaging is primarily the work of collecting basic data relating to the surface-water supplies of the State. These records are used as the basis for all developments involving the use of water.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","usgsCitation":"Purton, A., 1936, Stream-gaging work: Section 2 of Chapter 6 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936: Utah State Engineer Biennial Report 20, 10 p.","productDescription":"10 p.","startPage":"51","endPage":"60","numberOfPages":"10","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333850,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333849,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-365","text":"Full Text of Biennial Report"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5888770de4b05ccb964bab6b","contributors":{"authors":[{"text":"Purton, A.B.","contributorId":18338,"corporation":false,"usgs":true,"family":"Purton","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":660483,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039566,"text":"70039566 - 1936 - Stream flow, suspended, and dissolved matter in streams on and near soil conservation project, La Crosse, WI","interactions":[],"lastModifiedDate":"2012-08-12T01:01:45","indexId":"70039566","displayToPublicDate":"2012-01-01T23:11:52","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Stream flow, suspended, and dissolved matter in streams on and near soil conservation project, La Crosse, WI","docAbstract":"Measurements of stream flow and movement of suspended natter have been obtained at stations on the La Crosse project as indicated below: Little La Crosse River near Leon, Wis. Drainage area 77.1 square miles. The station is in sec. 3, T. 16 N., R. 4 W., 2 miles northwest of Leon, Monroe County; established March 14, 1934; suspended matter determined from April 1, 1934. Coon Creek at Coon Valley, Wis. Drainage area 77.2 square miles. The station is in sec. 7, T. 14 N., R. 5 W., in the village of Coon Valley, Vernon County; established March 16, 1934; suspended matter determined from April 6, 1934. Coon Creek near Stoddard, Wis. Drainage area 115 square miles. The station is in sec. 25, T. 14 N., R. 7 W., 3 1/4 miles east of Stoddard, Vernon County; established March 28, 1934; suspended matter determined from April 6, 1934.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039566","collaboration":"Prepared in cooperation with the Soil Conservation Service, U.S. Department of Agriculture","usgsCitation":"Grover, N., 1936, Stream flow, suspended, and dissolved matter in streams on and near soil conservation project, La Crosse, WI, 21 p., *66 p.; Tables; Worksheets, https://doi.org/10.3133/70039566.","productDescription":"21 p., *66 p.; Tables; Worksheets","numberOfPages":"109","costCenters":[],"links":[{"id":261079,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039566/report.pdf"},{"id":261080,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039566/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","city":"La Crosse","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9a72e4b08c986b31c946","contributors":{"authors":[{"text":"Grover, N.C.","contributorId":65453,"corporation":false,"usgs":true,"family":"Grover","given":"N.C.","email":"","affiliations":[],"preferred":false,"id":466490,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006903,"text":"70006903 - 1936 - Founders of fish culture - European origins","interactions":[],"lastModifiedDate":"2015-12-21T08:08:13","indexId":"70006903","displayToPublicDate":"2012-01-01T12:47:00","publicationYear":"1936","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":"Founders of fish culture - European origins","docAbstract":"Just where true fish culture appeared in history depends entirely upon what one considers fish culture to be. If the transportation of fishes from regions of plenty to those of few is to be regarded as fish culture - as it is by some even today - then this story should start in remotest antiquity and deal with an amazing series of failures. However, fish culture to be classed as a science must include far more than mere transportation, it must include a deliberate effort on the part of man to master a technique of fish raising which will yield results far superior to Nature's. Accordingly, the wheel of history must be spun forward to the fifteenth century, A. D., when man first conceived the idea that with care and exactitude, he could improve upon Nature. The fish cultural efforts of the Chinese, the Egyptians, the Greeks, and the Romans may be skipped over in a hurry, for they represented little more than the transportation and rearing of wild fish. With the renaissance of modern civilization in Europe came the birth of scientific fish culture.","language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1577/1548-8640(1936)316[8:FOFCEO]2.0.CO;2","usgsCitation":"Fish, F.F., 1936, Founders of fish culture - European origins: Progressive Fish-Culturist, v. 16, p. 8-10, https://doi.org/10.1577/1548-8640(1936)316[8:FOFCEO]2.0.CO;2.","productDescription":"3 p.","startPage":"8","endPage":"10","numberOfPages":"3","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":258373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258343,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8640(1936)316[8:FOFCEO]2.0.CO;2","linkFileType":{"id":5,"text":"html"}}],"volume":"16","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1391e4b0c8380cd546cb","contributors":{"authors":[{"text":"Fish, F. F.","contributorId":82572,"corporation":false,"usgs":true,"family":"Fish","given":"F.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":355432,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70040178,"text":"70040178 - 1936 - Withdrawal of ground water on Long Island, N.Y.","interactions":[],"lastModifiedDate":"2012-10-03T17:16:16","indexId":"70040178","displayToPublicDate":"2012-01-01T10:21:47","publicationYear":"1936","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-1","title":"Withdrawal of ground water on Long Island, N.Y.","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","usgsCitation":"Thompson, D.G., and Leggette, R., 1936, Withdrawal of ground water on Long Island, N.Y.: Bulletin GW-1, 28 p.; 1 Plate.","productDescription":"28 p.; 1 Plate","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262267,"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\": [ [ [ -79.75138888888888,40.48444444444444 ], [ -79.75138888888888,45.00111111111111 ], [ -71.78388888888888,45.00111111111111 ], [ -71.78388888888888,40.48444444444444 ], [ -79.75138888888888,40.48444444444444 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e58739e4b0a4aa5bb09f96","contributors":{"authors":[{"text":"Thompson, D. G.","contributorId":95050,"corporation":false,"usgs":true,"family":"Thompson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":467832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":467831,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70159187,"text":"70159187 - 1936 - Supplementary report on the ground-water supplies of the Atlantic City region","interactions":[],"lastModifiedDate":"2015-11-12T13:46:31","indexId":"70159187","displayToPublicDate":"2010-02-02T05:15:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":135,"text":"Special Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"6","title":"Supplementary report on the ground-water supplies of the Atlantic City region","docAbstract":"This report is the second progress report on the ground-water investigations in the Atlantic City region. Many important problems still remain to be solved, however, and it is in no sense a final report.
\nThe report covers the area immediately surrounding Atlantic City, extending from Brigantine to Sea Isle City along the coast and from Absecon to Somers Point on the mainland. In addition to this, a few data are presented bearing on the area along the coast as far south as Wildwood. The area lies in the southern part of the New Jersey Coastal Plain, and the water-bearing formations considered are all unconsolidated and of Miocene or more recent age. The major formations in the region dip gently toward the ocean and possibly extend out under the ocean to the edge of the Continental Shelf, about 100 miles from Atlantic City. The principal ground-water supplies in the area are derived from the so-called \"800-foot sand,\" a member of the Kirkwood formation, and from the overlying Cohansey sands. The 800-foot sand is of wide extent and apparently fairly uniform. The Cohansey sands, on the other hand, cover a wide area but are by no means uniform. At the Atlantic City Water Works two Cohansey sands are recognized-the so-called \"100-foot\" and \"200-foot\" sands. Neither of these sands can be differentiated from the other sands of the Cohansey formation over a distance greater than 4 or 5 miles in any direction.
\nIn addition to the supplies derived from ground water, some surface water is used at present by two of the public water supplies. The quality of the water from all the sources of supply now used is satisfactory. The total consumption of water in the region has increased gradually over the entire period of record, except for a moderate decline from 1929 to 1934. Additional water supplies can be obtained from either of two fairly large streams near the region, and possibly also from a more widespread development of the Cohansey sands. The 800-foot sand should not be counted upon as a source of additional water supply, in view of its liability to salt-water contamination. The same danger also exists in the Cohansey sands on the mainland near the shore, but farther inland it is not a serious menace to the supply from these sands
\nThe 100-foot sand at the Atlantic City Water Work has been overdeveloped since 1930, with the result that the head of the water in it has been lowered materially and salt water has been drawn into it through holes in the overlying clay beneath the nearby salt marshes. Three of the five new large-capacity wells drilled to this sand in 1930 have been temporarily or permanently abandoned on account of salt-water intrusion, and the two others will probably have to be abandoned also, unless suitable remedial measures are promptly adopted. It is recommended that the wells to the 100-foot sand be used only when needed to supply the seasonal peak demand and that consideration be given to a project to transform the tidal marshes into a fresh-water pond by means of a suitable dam in order to protect the formation from further contamination. If detailed study proves that the dam and fresh-water pond would not be economically justified, a smaller pond and an embankment and tide gates on the main stream to keep the salt water from flooding the marshes are recommended as less effective but less expensive remedial measures. In view of the experience with the 100-foot sand at the Atlantic City Water Works, it is further recommended that any additional development of the Cohansey sands be preceded by a comprehensive test-well program that will indicate not only the capacity of the sands, but the location of salt water in them and the possibility of its being drawn into existing wells or the proposed new wells.
\nThe salt-water intrusion into the 100-foot sand was effectively studied by means of driven-well points, which, it was found, could easily be driven to a depth of about 100 feet. The fact that the screen of these wells was driven with the casing and that no water was used in the drilling process made it possible to collect true samples of water from every sand encountered in them. This, in turn, made it possible to study the vertical distribution of salt water in each well. The interpretation of the vertical distribution of salt water in these wells was very helpful in arriving at a final decision as to the source of the salt water.
\nThe 200-foot sand at the Atlantic City Water Works has also been subjected to a considerably increased draft since 1930. Although there is no evidence at present that this sand has been overdeveloped, a study of its characteristics suggests that it may not be capable of yielding permanently the capacity of the present wells that tap it. Three test wells have been installed between the well field and the source from which this sand might derive salt water, and they should be sampled regularly to determine the danger of salt-water intrusion into the sand. In a landward direction this sand merges into the other Cohansey sands. It is therefore advisable that any additional development of the Cohansey sands should be undertaken so far inland that the pumping from it will not affect the present wells to the 200-foot sand and thereby increase the danger of salt-water contamination in them.
\nAt present more potable water is taken from the Atlantic City 800-foot sand than from any other source of supply for the region. This sand is the sole source for some of the smaller communities on the barrier beaches. The original static head of the water in it at Atlantic City was between 20 and 25 feet above sea level. The head has been lowered more than 50 feet over much of the region, and in parts of Atlantic City it has been lowered considerably more than 100 feet. A consideration of the principles governing the relation between salt water and fresh water in water-bearing sands indicates that the 800-foot sand probably contained salt water at a distance of 5 or 10 miles out from Atlantic City before any water was pumped from it. The evidence collected in this investigation indicates that the cone of depression created by the pumping from this sand in the Atlantic City region has probably extended inland to the intake area of the sand, the nearest part of which is probably about 40 miles from Atlantic City. If this is so, the conclusion is almost inescapable that it has also extended oceanward for a distance considerably greater than the 5 or 10 miles to the original zone of contact between the fresh and salt waters, and that salt water is probably being drawn toward the Atlantic City region through this sand. The time of its arrival will depend primarily upon the rate of pumping in the region and upon how much of the fresh water that originally lay between the region and the zone of contact must be removed before the salt water can reach the region. It may arrive in the near future if it advances in the form of a narrow tongue. On the other hand, if it advances along a broader front; so that more of the intervening fresh water must be pumped out of the formation, its arrival may be delayed for some time.
","language":"English","publisher":"State of New Jersey State Water Policy Commission","collaboration":"Prepared in cooperation with the U.S. Geological Survey","usgsCitation":"Barksdale, H.C., Sundstrom, R.W., and Brunstein, M.S., 1936, Supplementary report on the ground-water supplies of the Atlantic City region: Special Report 6, 150 p.","productDescription":"150 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":310010,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70159187.jpg"},{"id":311253,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70159187/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"New Jersey","otherGeospatial":"Atlantic City, Brigantine, Somers Point, Sea Isle City, Absecon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n 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C.","contributorId":11463,"corporation":false,"usgs":true,"family":"Barksdale","given":"Henry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":577791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sundstrom, Raymond W.","contributorId":8080,"corporation":false,"usgs":true,"family":"Sundstrom","given":"Raymond","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":577792,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brunstein, Maurice S.","contributorId":149293,"corporation":false,"usgs":false,"family":"Brunstein","given":"Maurice","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":577793,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":38153,"text":"wsp773A - 1936 - Geology and ground-water resources of the Elizabeth City area, North 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