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,{"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":"<p><span>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&nbsp;</span><sub>3</sub><span>&nbsp;. 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.&nbsp;</span></p>","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":70180141,"text":"70180141 - 1936 - Stream-gaging work: Section 2 of Chapter 6 in <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>","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 <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>","docAbstract":"<p>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.</p>","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 <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>: 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":70180145,"text":"70180145 - 1936 - Ground water investigations in Utah to June 30, 1936: A part of Chapter 8 in <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>","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 <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>","docAbstract":"<p>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.</p>","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 <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>: 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":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":"<p>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.</p>\n<p>The 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.</p>\n<p>In 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</p>\n<p>The 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.</p>\n<p>The 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.</p>\n<p>The 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.</p>\n<p>At 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, &nbsp;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.</p>","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      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.49554443359375,\n              39.528407312645825\n            ],\n            [\n              -74.29229736328125,\n              39.49874248613119\n            ],\n            [\n              -74.33624267578125,\n              39.4255858195144\n            ],\n            [\n              -74.38842773437499,\n              39.37677199661635\n            ],\n            [\n              -74.47219848632812,\n              39.31623792008409\n            ],\n            [\n              -74.54360961914062,\n              39.299236474818194\n            ],\n            [\n              -74.59854125976562,\n              39.24182610848299\n            ],\n            [\n              -74.70840454101561,\n              39.118341154165186\n            ],\n            [\n              -74.73175048828124,\n              39.11407918425643\n            ],\n            [\n              -74.77294921875,\n              39.132190775931036\n            ],\n            [\n              -74.77706909179688,\n              39.14603767446419\n            ],\n            [\n              -74.63973999023438,\n              39.301361881349244\n            ],\n            [\n              -74.5697021484375,\n              39.42346418978382\n            ],\n            [\n              -74.49554443359375,\n              39.528407312645825\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5623712fe4b06217fc47deab","contributors":{"authors":[{"text":"Barksdale, Henry 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":32823,"text":"pp185H - 1936 - The flora of the New Albany shale: Part 1, Diichnia kentuckiensis, a new representative of the Calamopityeae","interactions":[],"lastModifiedDate":"2013-01-31T11:24:36","indexId":"pp185H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"185","chapter":"H","title":"The flora of the New Albany shale: Part 1, Diichnia kentuckiensis, a new representative of the Calamopityeae","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1934-35","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp185H","usgsCitation":"Read, C., 1936, The flora of the New Albany shale: Part 1, Diichnia kentuckiensis, a new representative of the Calamopityeae: U.S. Geological Survey Professional Paper 185, p. 149-161, https://doi.org/10.3133/pp185H.","productDescription":"p. 149-161","costCenters":[],"links":[{"id":166027,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0185h/report-thumb.jpg"},{"id":266808,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0185h/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65db27","contributors":{"authors":[{"text":"Read, C.B.","contributorId":77202,"corporation":false,"usgs":true,"family":"Read","given":"C.B.","affiliations":[],"preferred":false,"id":209246,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34924,"text":"b870 - 1936 - Geology and ore deposits of the Bayard area, Central Mining District, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:09:30","indexId":"b870","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"870","title":"Geology and ore deposits of the Bayard area, Central Mining District, New Mexico","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b870","usgsCitation":"Lasky, S.G., 1936, Geology and ore deposits of the Bayard area, Central Mining District, New Mexico: U.S. Geological Survey Bulletin 870, vi, 144 p. :incl. tables, diagrs. 17 pl. (part fold., part col. ; incl. maps.) ;28 cm., https://doi.org/10.3133/b870.","productDescription":"vi, 144 p. :incl. tables, diagrs. 17 pl. (part fold., part col. ; incl. maps.) ;28 cm.","costCenters":[],"links":[{"id":92989,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0870/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92990,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0870/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92991,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0870/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92992,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0870/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92993,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0870/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92994,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0870/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0870/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6846b4","contributors":{"authors":[{"text":"Lasky, Samuel Grossman","contributorId":35380,"corporation":false,"usgs":true,"family":"Lasky","given":"Samuel","email":"","middleInitial":"Grossman","affiliations":[],"preferred":false,"id":213818,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39336,"text":"pp186A - 1936 - New Upper Cretaceous Ostreidae from the Gulf region","interactions":[],"lastModifiedDate":"2013-01-31T11:25:08","indexId":"pp186A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"186","chapter":"A","title":"New Upper Cretaceous Ostreidae from the Gulf region","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1936","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp186A","usgsCitation":"Stephenson, L.W., 1936, New Upper Cretaceous Ostreidae from the Gulf region: U.S. Geological Survey Professional Paper 186, p. 1-12, https://doi.org/10.3133/pp186A.","productDescription":"p. 1-12","costCenters":[],"links":[{"id":170062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":266809,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0186a/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697838","contributors":{"authors":[{"text":"Stephenson, L. W.","contributorId":70349,"corporation":false,"usgs":true,"family":"Stephenson","given":"L.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":221323,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2137,"text":"wsp773D - 1936 - Ground-water resources of Kleberg County, Texas","interactions":[],"lastModifiedDate":"2016-08-16T11:38:47","indexId":"wsp773D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"773","chapter":"D","title":"Ground-water resources of Kleberg County, Texas","docAbstract":"<p>Abundant supplies of fresh water are obtained from deep artesian wells In all parts of Kleberg County. The water is derived from a stratum of sand, 10 to 150 feet thick, which usually has been referred to the Goliad sand but possibly may be at the base of the LIssie formation. The top of the sand Is reached at depths of around 400 feet In the western part of the county, 600 to 700 feet In the locality of Klngsville, and 1,250 to 1,450 feet In the eastern part of the county. Small supplies of fairly good water are obtained from shallow wells In very sandy areas in the eastern and southern parts of the county, but with this exception, so far as known, no good water has been obtained In the county either above or below the artesian fresh-water horizon.</p>\n<p>The fresh artesian water Is supplied by percolation from the outcrop of the water-bearing sands, which is many miles to the west In Jim Wells, Brooks, and Duval Counties. The estimated average replenishment from the outcrop to the wells of Kleberg County is 3,000,000 gallons a day.</p>\n<p>Available Information regarding most of the wells of the county Is given in the table of well records. Of the 43V wells listed 34 are not In use, and the water supplies from the others are used as follows: , Entirely for stock, 151; domestic use and stock, 241; public supply, 3; Industrial supply, 2; Irrigation, 4; railroad supply, 1; unrecorded, 1. About 80 are flowing wells In the southern and eastern parts of the county.</p>\n<p>It is concluded that the total withdrawal from those wells averages about 4,000,000 gallons a day. Some water is wasted, but the amount is not very great.</p>\n<p>There has been a general decline In the artesian head throughout the county. The largest decline has been in the western part of the county and In the vicinity of Klngsville, where the water level is now 15 to 45 feet below the surface in wells that once had a strong flow. Wells continue to flow in the southern and eastern parts of the county, but under less head than formerly. There was a small net loss in head in most parts of the county between the winters of 1932-33 and 1934-35, indicating that the decline is slowly continuing. Originally the artesian pressure In the fresh-water sands was much higher than the pressure In the overlying saltwater sands, but this relation has been reversed in the western part of the county and In the district around Klngsville, as a result of the decline in artesian head.</p>\n<p>Water obtained from the fresh-water horizon is comparatively fresh in the western and central parts of the county but contains a somewhat higher proportion of chlorides toward the Gulf. Samples obtained from about 100 wells, located for the most part in the central part of the county, showed a. higher chloride content than is normal for the freshwater beds in the area. These wells are believed in large part to be defective and to be admitting salt water. This was demonstrated and the leaks located in several wells that were tested. No evidence was found of salt-water contamination by percolation through the formations, however. The leaky wells should be repaired, If practicable, or sealed to prevent them from contaminating the fresh-water sand. The chances of leaks developing can be largely eliminated If the wells are properly drilled and provided with casing of good grade, and the casing is adequately seated.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp773D","usgsCitation":"Livingston, P.P., and Bridges, T.W., 1936, Ground-water resources of Kleberg County, Texas: U.S. Geological Survey Water Supply Paper 773, 197-232 p., https://doi.org/10.3133/wsp773D.","productDescription":"197-232 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0773d/report-thumb.jpg"},{"id":27737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0773d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fca","contributors":{"authors":[{"text":"Livingston, Penn Poore","contributorId":79452,"corporation":false,"usgs":true,"family":"Livingston","given":"Penn","email":"","middleInitial":"Poore","affiliations":[],"preferred":false,"id":144722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bridges, Thomas W.","contributorId":106870,"corporation":false,"usgs":true,"family":"Bridges","given":"Thomas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144723,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2807,"text":"wsp677 - 1936 - Ground water in south-central Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp677","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"677","title":"Ground water in south-central Tennessee","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp677","usgsCitation":"Theis, C., 1936, Ground water in south-central Tennessee: U.S. Geological Survey Water Supply Paper 677, v, 182 p. :ill., tables, maps. ;23 cm., https://doi.org/10.3133/wsp677.","productDescription":"v, 182 p. :ill., tables, maps. ;23 cm.","costCenters":[],"links":[{"id":138246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0677/report-thumb.jpg"},{"id":29309,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0677/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66da1d","contributors":{"authors":[{"text":"Theis, C.V.","contributorId":101641,"corporation":false,"usgs":true,"family":"Theis","given":"C.V.","email":"","affiliations":[],"preferred":false,"id":145826,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2139,"text":"wsp773B - 1936 - Water resources of the Edwards limestone in the San Antonio area, Texas","interactions":[],"lastModifiedDate":"2016-08-22T11:44:21","indexId":"wsp773B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"773","chapter":"B","title":"Water resources of the Edwards limestone in the San Antonio area, Texas","docAbstract":"<p>The water discharged from the large springs of San Antonio and most of the deep wells of the San Antonio area comes from a common reservoir in fissures and solution channels in the Edwards limestone.</p>\n<p>The water enters the limestone in a zone of outcrop along the Balcones escarpment, which crosses the northern parts of Bexar and Medina Counties and extends a long distance both to the east and west of these counties. It is estimated that the combined annual losses into the limestone from the Medina, Prio, Dry Prio, Nueces, and Sabinal Rivers and Hondo Creek may average as much as 150,000 acre-feet a year, the equivalent of a continuous flow of about 134,000,000 gallons a day. Smaller streams also contribute to the underground reservoir, and additional recharge is provided from rainfall on the outcrop of the limestone by direct penetration and by seepage from innumerable storm-water channels.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp773B","usgsCitation":"Livingston, P., Sayre, A., and White, W.N., 1936, Water resources of the Edwards limestone in the San Antonio area, Texas: U.S. Geological Survey Water Supply Paper 773, 59-113 p. :ill., 1 folded map ;24 cm., https://doi.org/10.3133/wsp773B.","productDescription":"59-113 p. :ill., 1 folded map ;24 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137793,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0773b/report-thumb.jpg"},{"id":27739,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0773b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602d9e","contributors":{"authors":[{"text":"Livingston, Penn","contributorId":104977,"corporation":false,"usgs":true,"family":"Livingston","given":"Penn","affiliations":[],"preferred":false,"id":144727,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sayre, A.N.","contributorId":84339,"corporation":false,"usgs":true,"family":"Sayre","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":144728,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, W. N.","contributorId":69954,"corporation":false,"usgs":true,"family":"White","given":"W.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":144726,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":33910,"text":"b855 - 1936 - Geology and mineral resources of the Bellefonte quadrangle, Pennsylvania","interactions":[],"lastModifiedDate":"2022-03-30T20:00:40.764893","indexId":"b855","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"855","title":"Geology and mineral resources of the Bellefonte quadrangle, Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b855","usgsCitation":"Butts, C., and Moore, E.S., 1936, Geology and mineral resources of the Bellefonte quadrangle, Pennsylvania: U.S. Geological Survey Bulletin 855, Report: vi, 111 p.; 2 Plates: 21.22 × 20.26 inches and 23.94 × 8.06 inches, https://doi.org/10.3133/b855.","productDescription":"Report: vi, 111 p.; 2 Plates: 21.22 × 20.26 inches and 23.94 × 8.06 inches","costCenters":[],"links":[{"id":92472,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0855/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92471,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0855/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92473,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0855/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162979,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0855/report-thumb.jpg"},{"id":397897,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21027.htm"}],"scale":"62500","country":"United States","state":"Pennsylvania","otherGeospatial":"Bellefonte quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78,\n              40.75\n            ],\n            [\n              -77.75,\n              40.75\n            ],\n            [\n              -77.75,\n              41\n            ],\n            [\n              -78,\n              41\n            ],\n            [\n              -78,\n              40.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4708","contributors":{"authors":[{"text":"Butts, Charles","contributorId":75988,"corporation":false,"usgs":true,"family":"Butts","given":"Charles","email":"","affiliations":[],"preferred":false,"id":212160,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, Elwood S.","contributorId":62466,"corporation":false,"usgs":true,"family":"Moore","given":"Elwood","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":212159,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4550,"text":"wsp793 - 1936 - Surface water supply of the United States, 1935 : Part 13 Snake River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:51","indexId":"wsp793","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"793","title":"Surface water supply of the United States, 1935 : Part 13 Snake River basin","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp793","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1936, Surface water supply of the United States, 1935 : Part 13 Snake River basin: U.S. Geological Survey Water Supply Paper 793, 197 p. ;24 cm., https://doi.org/10.3133/wsp793.","productDescription":"197 p. ;24 cm.","costCenters":[],"links":[{"id":139800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0793/report-thumb.jpg"},{"id":31607,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0793/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db69701b","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":528248,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45324,"text":"b847B - 1936 - The Rosebud coal field, Rosebud and Custer Counties, Montana","interactions":[{"subject":{"id":45324,"text":"b847B - 1936 - The Rosebud coal field, Rosebud and Custer Counties, Montana","indexId":"b847B","publicationYear":"1936","noYear":false,"chapter":"B","title":"The Rosebud coal field, Rosebud and Custer Counties, Montana"},"predicate":"IS_PART_OF","object":{"id":35011,"text":"b847 - 1937 - Contributions to economic geology (short papers and preliminary reports), 1934-36","indexId":"b847","publicationYear":"1937","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1934-36"},"id":1}],"isPartOf":{"id":35011,"text":"b847 - 1937 - Contributions to economic geology (short papers and preliminary reports), 1934-36","indexId":"b847","publicationYear":"1937","noYear":false,"title":"Contributions to economic geology (short papers and preliminary reports), 1934-36"},"lastModifiedDate":"2021-08-17T20:41:43.236121","indexId":"b847B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"847","chapter":"B","title":"The Rosebud coal field, Rosebud and Custer Counties, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b847B","usgsCitation":"Pierce, W.G., 1936, The Rosebud coal field, Rosebud and Custer Counties, Montana: U.S. Geological Survey Bulletin 847, 78 p., https://doi.org/10.3133/b847B.","productDescription":"78 p.","startPage":"43","endPage":"120","costCenters":[],"links":[{"id":93994,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0847b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0847b/report-thumb.jpg"},{"id":388061,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20517.htm"}],"country":"United States","state":"Montana","county":"Custer County, Rosebud County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.3359375,\n              45.37530235052552\n            ],\n            [\n              -104.666748046875,\n              45.37530235052552\n            ],\n            [\n              -104.666748046875,\n              47.39834920035926\n            ],\n            [\n              -109.3359375,\n              47.39834920035926\n            ],\n            [\n              -109.3359375,\n              45.37530235052552\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e26","contributors":{"authors":[{"text":"Pierce, W. G.","contributorId":11267,"corporation":false,"usgs":true,"family":"Pierce","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":231424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35597,"text":"b873 - 1936 - Geology and mineral resources of the Butler and Zelienople quadrangles, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:09:43","indexId":"b873","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"873","title":"Geology and mineral resources of the Butler and Zelienople quadrangles, Pennsylvania","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b873","usgsCitation":"Richardson, G.B., 1936, Geology and mineral resources of the Butler and Zelienople quadrangles, Pennsylvania: U.S. Geological Survey Bulletin 873, v, 93 p., 1 l. incl. illus., tables. :maps (5 fold., 4 in pocket) 3 fold. diagr. ;23 cm., https://doi.org/10.3133/b873.","productDescription":"v, 93 p., 1 l. incl. illus., tables. :maps (5 fold., 4 in pocket) 3 fold. diagr. ;23 cm.","costCenters":[],"links":[{"id":93411,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0873/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93412,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0873/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93413,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0873/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0873/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0873/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6849d7","contributors":{"authors":[{"text":"Richardson, George Burr","contributorId":102458,"corporation":false,"usgs":true,"family":"Richardson","given":"George","email":"","middleInitial":"Burr","affiliations":[],"preferred":false,"id":214915,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2752,"text":"wsp775 - 1936 - Records of wells on the Snake River Plain, southeastern Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp775","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"775","title":"Records of wells on the Snake River Plain, southeastern Idaho","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp775","usgsCitation":"Stearns, H.T., Crandall, L., and Steward, W.G., 1936, Records of wells on the Snake River Plain, southeastern Idaho: U.S. Geological Survey Water Supply Paper 775, 1 p. l., 139 p. incl. tables. ;23 cm., https://doi.org/10.3133/wsp775.","productDescription":"1 p. l., 139 p. incl. tables. ;23 cm.","costCenters":[],"links":[{"id":137813,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0775/report-thumb.jpg"},{"id":29178,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0775/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635521","contributors":{"authors":[{"text":"Stearns, Harold T.","contributorId":65831,"corporation":false,"usgs":true,"family":"Stearns","given":"Harold","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":145717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crandall, Lynn","contributorId":7690,"corporation":false,"usgs":true,"family":"Crandall","given":"Lynn","email":"","affiliations":[],"preferred":false,"id":145716,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Steward, Willard G.","contributorId":99126,"corporation":false,"usgs":true,"family":"Steward","given":"Willard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145718,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39330,"text":"pp182 - 1936 - The Tertiary floras of Alaska, with a chapter on the geology of the Tertiary deposits","interactions":[],"lastModifiedDate":"2023-09-19T20:08:35.614329","indexId":"pp182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"182","title":"The Tertiary floras of Alaska, with a chapter on the geology of the Tertiary deposits","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp182","usgsCitation":"Hollick, A., and Smith, P.S., 1936, The Tertiary floras of Alaska, with a chapter on the geology of the Tertiary deposits: U.S. Geological Survey Professional Paper 182, Report: iii, 185 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