An extensive deposit of white, granular, massive gypsum has been discovered in central Thailand. The gypsum, a part of the Mesozoic Korat group, was deposited along with salt by evaporation of sea water in shallow basins extensively developed in Thailand and adjacent parts of Laos. It now occurs in a narrow, deep downfaulted block enclosed within a complex of Paleozoic sedimentary rocks and younger volcanic rocks, and is bounded to the east and west by north-trending high-angle faults. During downfaulting to its present position, the gypsum was altered to anhydrite. The upper part of the deposit has been reconverted to gypsum during the present cycle of erosion to depths of about 80-120 feet. Total reserves may exceed 25 million tons of gypsum with perhaps 10 times as much anhydrite.
","language":"English","publisher":"Thailand Department of Mineral Resources","issn":"0563-3532","usgsCitation":"Gardner, L.S., 1967, Phichit gypsum deposit, central Thailand: Report of Investigation - Thailand, Department of Mineral Resources, v. 9, 42 p.","productDescription":"42 p.","costCenters":[],"links":[{"id":367960,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Thailand","otherGeospatial":"Central Thailand","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[102.58493,12.18659],[101.68716,12.64574],[100.83181,12.62708],[100.97847,13.41272],[100.0978,13.40686],[100.01873,12.307],[99.47892,10.84637],[99.15377,9.96306],[99.2224,9.23926],[99.87383,9.20786],[100.27965,8.29515],[100.45927,7.42957],[101.01733,6.85687],[101.62308,6.74062],[102.14119,6.22164],[101.81428,5.81081],[101.15422,5.69138],[101.07552,6.20487],[100.2596,6.64282],[100.08576,6.46449],[99.69069,6.84821],[99.51964,7.34345],[98.98825,7.90799],[98.50379,8.38231],[98.33966,7.79451],[98.15001,8.35001],[98.25915,8.97392],[98.55355,9.93296],[99.03812,10.96055],[99.58729,11.89276],[99.19635,12.80475],[99.21201,13.26929],[99.09776,13.8275],[98.43082,14.62203],[98.19207,15.1237],[98.53738,15.3085],[98.90335,16.17782],[98.49376,16.83784],[97.85912,17.56795],[97.3759,18.44544],[97.79778,18.62708],[98.25372,19.7082],[98.95968,19.75298],[99.54331,20.1866],[100.11599,20.41785],[100.54888,20.10924],[100.60629,19.50834],[101.28201,19.46258],[101.03593,18.40893],[101.05955,17.5125],[102.11359,18.1091],[102.413,17.93278],[102.99871,17.96169],[103.20019,18.30963],[103.95648,18.24095],[104.71695,17.42886],[104.77932,16.44186],[105.58904,15.57032],[105.54434,14.72393],[105.21878,14.27321],[104.28142,14.41674],[102.98842,14.22572],[102.3481,13.39425],[102.58493,12.18659]]]},\"properties\":{\"name\":\"Thailand\"}}]}","volume":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gardner, Louis S.","contributorId":81581,"corporation":false,"usgs":true,"family":"Gardner","given":"Louis","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":772343,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221316,"text":"70221316 - 1967 - Test hold in aquifer with many water-bearing zones at Jacksonville, Florida","interactions":[],"lastModifiedDate":"2021-06-09T18:35:59.361297","indexId":"70221316","displayToPublicDate":"1967-10-01T13:30:27","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Test hold in aquifer with many water-bearing zones at Jacksonville, Florida","docAbstract":"One of the deepest water‐exploration wells in the southeastern United States was completed in 1966 at Jacksonville, Florida. It was drilled to a depth of nearly 2,500 feet to supply geologic and hydrologic information on the deeper unexplored part of the Floridan aquifer. This aquifer consists of a series of water producing zones separated by nonproducing zones. An important new fresh‐water producing zone was found, and the contact between the fresh water and salt water was located. The well was completed in three separate zones so that it could be used to monitor the the deeper part of the aquifer to detect any salt‐water encroachment. This paper describes the objectives, techniques, and results of drilling the test well.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01621.x","usgsCitation":"Leve, G., and Goolsby, D.A., 1967, Test hold in aquifer with many water-bearing zones at Jacksonville, Florida: Groundwater, v. 5, no. 4, p. 18-22, https://doi.org/10.1111/j.1745-6584.1967.tb01621.x.","productDescription":"5 p.","startPage":"18","endPage":"22","costCenters":[],"links":[{"id":386362,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","city":"Jacksonville","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.1337890625,\n 30.088107753367257\n ],\n [\n -81.2109375,\n 30.088107753367257\n ],\n [\n -81.2109375,\n 30.543338954230222\n ],\n [\n -82.1337890625,\n 30.543338954230222\n ],\n [\n -82.1337890625,\n 30.088107753367257\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Leve, G.W.","contributorId":64294,"corporation":false,"usgs":true,"family":"Leve","given":"G.W.","affiliations":[],"preferred":false,"id":817292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goolsby, D. A.","contributorId":50508,"corporation":false,"usgs":true,"family":"Goolsby","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":817293,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221313,"text":"70221313 - 1967 - New approaches to water‐resources investigations in upstate New York","interactions":[],"lastModifiedDate":"2021-06-09T18:00:54.224471","indexId":"70221313","displayToPublicDate":"1967-10-01T12:55:53","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"New approaches to water‐resources investigations in upstate New York","docAbstract":"The scope of area1 investigations of water resources in New York has changed within the last 4 years. Prior 1962, most investigations covered only counties or smaller areas and were mainly restricted to ground‐water resources Since 1762, investigarions have covered largebasin (2,000‐4,000 square miles) with the purpose of defining total water resources so that basin‐wldc comprehensive plans for water development can be prepared. Ground water has been intensively studied in the basin investigations, both because of its large potential for future development, and becaus e of it sinterre lation with the surface‐water resources. The latter reason is particularly important because the principal aquifers are numerous u nconnect edglacials and andgravel deposits that are crossed by streams. This ground‐water regimen to a large degree determines the flow characteristics and water quality of streams. Conversely, streamflow data provide acon‐venient means of assessing ground‐water availability.Some approaches used in basin studies are: (1)(1) numerous quantitative and qualitative observations of low streamflow to define the principal areas of ground‐water discharge and to define the quantity and quality of discharging ground water (2)estimation of total ground‐water dischar gepas stream gages from daily streamflow records by correlation with ground‐water levels and by analysis of the records (3) assessment of recharge to particular sand and gravel deposit swith inbroadlimits, using the data on ground‐water discharge to streams (4) estimation of a daily chemical quality hydrograph on the basis of quantity and quality of both ground‐water discharge and overland runoff.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01619.x","usgsCitation":"La Sala, A.M., 1967, New approaches to water‐resources investigations in upstate New York: Groundwater, v. 5, no. 4, p. 6-11, https://doi.org/10.1111/j.1745-6584.1967.tb01619.x.","productDescription":"6 p.","startPage":"6","endPage":"11","costCenters":[],"links":[{"id":386359,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"upstate New York","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.32202148437499,\n 42.97250158602597\n ],\n [\n -73.070068359375,\n 42.97250158602597\n ],\n [\n -73.070068359375,\n 45.01141864227728\n ],\n [\n -76.32202148437499,\n 45.01141864227728\n ],\n [\n -76.32202148437499,\n 42.97250158602597\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"La Sala, A. M. Jr.","contributorId":38199,"corporation":false,"usgs":true,"family":"La Sala","given":"A.","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":817289,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000180,"text":"1000180 - 1967 - Some oligochaetes from Lake Michigan","interactions":[],"lastModifiedDate":"2026-03-12T15:26:52.872993","indexId":"1000180","displayToPublicDate":"1967-10-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3625,"text":"Transactions of the American Microscopical Society","active":true,"publicationSubtype":{"id":10}},"title":"Some oligochaetes from Lake Michigan","docAbstract":"Twenty-six species of Tubificidae, 12 Naididae, and 1 Lumbriculidae were found in three regions of Lake Michigan- Green Bay, the southern end of the lake proper, and the harbor at Ludington, Michigan. One new naidid species is described. Methods of identification of some species are discussed and illustrated. The abundance of oligochaetes and distribution of certain species vary with depth and location. Data are presented on the effects of the environment on the distribution of certain species. The presence or absence of some species reflected the quality of the environment; some were prevalent in polluted waters whereas others were restricted or absent. Possible changes in composition and abundance of species are outlined if organic enrichment increases in Lake Michigan.
","language":"English","publisher":"Wiley","doi":"10.2307/3224267","usgsCitation":"Hiltunen, J.K., 1967, Some oligochaetes from Lake Michigan: Transactions of the American Microscopical Society, v. 86, no. 4, p. 433-454, https://doi.org/10.2307/3224267.","productDescription":"22 p.","startPage":"433","endPage":"454","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":130511,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois, Indiana, Michigan, Wisconsin","otherGeospatial":"Lake Michigan","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -87.97025984791705,\n 45.20587410008886\n ],\n [\n -88.14054252464355,\n 41.50726553497216\n ],\n [\n -86.33381625694446,\n 41.50940165221235\n ],\n [\n -85.83636960569008,\n 44.47722673256698\n ],\n [\n -85.09881343279604,\n 44.956609541015666\n ],\n [\n -84.6020024557969,\n 45.768004056882816\n ],\n [\n -84.97649940103136,\n 46.22260358684156\n ],\n [\n -86.6882000784625,\n 46.0039491403779\n ],\n [\n -87.97025984791705,\n 45.20587410008886\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"86","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e8e4b07f02db5e8f3f","contributors":{"authors":[{"text":"Hiltunen, Jarl K.","contributorId":27820,"corporation":false,"usgs":true,"family":"Hiltunen","given":"Jarl","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":308199,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206898,"text":"70206898 - 1967 - Chemical Composition of Ectoprocta (Bryozoa)","interactions":[],"lastModifiedDate":"2019-11-26T11:00:51","indexId":"70206898","displayToPublicDate":"1967-09-30T10:57:18","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2412,"text":"Journal of Paleontology","active":true,"publicationSubtype":{"id":10}},"title":"Chemical Composition of Ectoprocta (Bryozoa)","docAbstract":"Published data on the elemental composition of the Ectoprocta (Bryozoa) are supplemented by new chemical analyses of 28 ectoproct samples, distributed among 13 species, for organic matter, CO2 calcium, magnesium, strontium, barium, phosphorus and iron. The new data, in addition to the 25 fairly complete analyses previously published (distributed among 19 other species) suggest the existence of 3 species groupings that are based on composition and are related to habitat. Group I consists of genera that have more than 50 percent organic matter (dry weight). It includes all species of the entirely freshwater Phylactolaemata and the commonly brackish-water and freshwater Ctenostomata. Group II includes Cheilostomata having from 25 to 50 percent organic matter (dry weight). These genera are bush-like in growth habit and may be anchored to fine-grained sediment bottoms. Genera in Group II contain appreciable amounts of P2O5 (1.0-2.0 percent) and Fe2O3 (0.4-1.0 percent) in the ash. Only calcite has been observed in the mineralized portion of the skeleton of Group II species. Group III includes Cheilostomata and Cyclostomata that have less than 25 percent organic matter. These forms require stable surfaces for colonization. They contain a lesser amount of P2O5 (0.1-0.6 percent) and of Fe2O3 (less than 0.4 percent) than Group II genera. About 15 percent of Group III species have aragonitic skeletons. \"Pure\" aragonitic hard parts contain about 1.0 percent SrO (1.4 wt. percent SrCO3 and 0.3 percent MgO (0.6 wt. percent MgCO3) whereas \"pure\" calcitic skeletons contain less than 0.4 percent SrO (0.6 wt. percent SrCO3) and more than 3.5 percent MgO (7.4 wt. percent MgCO3). Based on the few species analyzed, some additional taxonomic and ecologic generalizations are suggested. Calcitic cheilostomes contain more magnesium than do calcitic cyclostomes. Warm water calcitic species have higher magnesium concentrations than do cold water calcitic species. Specimens from an estuary contain more P2O5 and less strontium than do specimens from areas of normal marine salinity, and specimens from nearshore areas have more iron than do specimens from deeper offshore areas. The order of concentration of elements in ectoprocts relative to the composition of sea water is 105 for phosphorus and iron, 103 for barium, 102 for calcium and strontium, and 101 for magnesium. However, the elements that are highly enriched in ectoprocts, especially iron and phosphorus, may be supplied to a considerable extent by sources other than normal sea water, such as food (diatoms in particular), and occluded matter of terrigenous origin. Twenty-eight protein and chitin amino acids were studied in three representative marine ectoproct species: Bugula simplex, a calcitic cheilostome, Parasmittina nitida, an aragonitic cheilostome, and Tubulipora liliacea, a calcitic cyclostome. Similar proportions but widely different amounts (from 0.6 to 11 percent organism dry weight) of amino acids occur in these species. Obvious variations in amino acid proportions relate more directly to degree of calcification and to mineralogy than to species classification. Chitin amino acids recoverable in residues after leaching with acid form less than 2 percent of the total organic content of the organism.
","language":"English","publisher":"SEPM Society for Sedimentary Geology","usgsCitation":"Schopf, T., and Manheim, F.T., 1967, Chemical Composition of Ectoprocta (Bryozoa): Journal of Paleontology, v. 41, no. 5, p. 1197-1225.","productDescription":"29 p.","startPage":"1197","endPage":"1225","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":369636,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":369635,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/1302092"}],"volume":"41","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schopf, T.J.M.","contributorId":106754,"corporation":false,"usgs":true,"family":"Schopf","given":"T.J.M.","email":"","affiliations":[],"preferred":false,"id":776187,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":776188,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70205374,"text":"70205374 - 1967 - Compilation of surface water records of Nepal through December 31, 1965","interactions":[],"lastModifiedDate":"2019-09-16T12:28:36","indexId":"70205374","displayToPublicDate":"1967-09-17T12:23:55","publicationYear":"1967","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":15,"text":"Monograph"},"title":"Compilation of surface water records of Nepal through December 31, 1965","docAbstract":"No Abstract available
","language":"English","publisher":"Kathmandu H.S.D.","usgsCitation":" Nepal Hydrological Survey Department., 1967, Compilation of surface water records of Nepal through December 31, 1965, 66 p.","productDescription":"66 p.","numberOfPages":"66","costCenters":[],"links":[{"id":367437,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://202.45.147.158/cgi-bin/koha/opac-detail.pl?biblionumber=1396"},{"id":367438,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Nepal","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"compilers":[{"text":"Evett, W. W.","contributorId":218997,"corporation":false,"usgs":false,"family":"Evett","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":770958,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"authors":[{"text":" Nepal Hydrological Survey Department.","contributorId":218998,"corporation":true,"usgs":false,"organization":" Nepal Hydrological Survey Department.","id":770957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70205377,"text":"70205377 - 1967 - Exploration for artesian water in the Sokoto Basin, Nigeria","interactions":[],"lastModifiedDate":"2024-03-22T00:11:13.530478","indexId":"70205377","displayToPublicDate":"1967-09-16T13:20:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Exploration for artesian water in the Sokoto Basin, Nigeria","docAbstract":"The Sokoto basin in semiarid northwestern Nigeria contains Cretaceous and Tertiary semiconsolidated deposits that dip gently northwest off an oldland of pre-Cretaceous crystalline rocks. Until recent years the dug well has been the chief source of ground water for the Hausa cultivators and the pastoral Fulani inhabitants of the region. Borehole exploration sponsored by US AID and the Geological Survey of Nigeria with technical guidance from the writers of the U. S. Geological Survey has revealed that the basal section of the Gwandu Formation contains a productive artesian sand aquifer throughout a 5,700 square mile area. Transmissibilities of the aquifer proved to be as high as 180,000 Imperial gallons a day per foot but generally decrease towards the west. The free flow areas total about 1,000 square miles with pressure heads in boreholes up to + 83 feet above land surface and individual flows as great as 12,000 gallons per hour. Beneath the Gwandu, pressure aquifers in the Rima Group and the Gundumi Formation also produce flowing water in the lowland (fadama) of the Sokoto River. In the southern part of the basin, however, only one aquifer is present in the Cretaceous sequence, because the Gundumi aquifer is absent and the Rima aquifer apparently grades into the upper permeable section of the Illo Group. The quality of the water from all the pressure aquifers is generally quite good, although the iron content is high in places and salinity increases in the very deep aquifers.
","language":"English","publisher":"National Groundwater Association","doi":"10.1111/j.1745-6584.1967.tb03670.x","usgsCitation":"Anderson, H., and Ogilbee, W., 1967, Exploration for artesian water in the Sokoto Basin, Nigeria: Groundwater, v. 5, no. 3, p. 42-46, https://doi.org/10.1111/j.1745-6584.1967.tb03670.x.","productDescription":"5 p.","startPage":"42","endPage":"46","costCenters":[],"links":[{"id":367442,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Nigeria","otherGeospatial":"Sokoto Province","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[8.50029,4.77198],[7.46211,4.41211],[7.0826,4.46469],[6.69807,4.24059],[5.89817,4.26245],[5.3628,4.88797],[5.03357,5.6118],[4.32561,6.27065],[3.57418,6.2583],[2.6917,6.25882],[2.74906,7.87073],[2.72379,8.50685],[2.91231,9.13761],[3.22035,9.44415],[3.70544,10.06321],[3.60007,10.33219],[3.79711,10.73475],[3.57222,11.32794],[3.61118,11.66017],[3.68063,12.5529],[3.96728,12.95611],[4.10795,13.53122],[4.36834,13.74748],[5.44306,13.86592],[6.44543,13.49277],[6.82044,13.11509],[7.33075,13.09804],[7.80467,13.34353],[9.01493,12.82666],[9.52493,12.8511],[10.11481,13.27725],[10.70103,13.24692],[10.98959,13.38732],[11.5278,13.32898],[12.30207,13.03719],[13.08399,13.59615],[13.3187,13.55636],[13.99535,12.46157],[14.18134,12.48366],[14.57718,12.08536],[14.46819,11.90475],[14.41538,11.57237],[13.57295,10.79857],[13.30868,10.16036],[13.1676,9.64063],[12.95547,9.41777],[12.75367,8.71776],[12.21887,8.30582],[12.06395,7.79981],[11.83931,7.39704],[11.74577,6.98138],[11.05879,6.64443],[10.49738,7.05536],[10.11828,7.03877],[9.52271,6.45348],[9.23316,6.44449],[8.75753,5.47967],[8.50029,4.77198]]]},\"properties\":{\"name\":\"Nigeria\"}}]}","volume":"5","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Anderson, H. R.","contributorId":67487,"corporation":false,"usgs":true,"family":"Anderson","given":"H. R.","affiliations":[],"preferred":false,"id":770966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ogilbee, William","contributorId":106093,"corporation":false,"usgs":true,"family":"Ogilbee","given":"William","email":"","affiliations":[],"preferred":false,"id":770967,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70214101,"text":"70214101 - 1967 - Compilation of hydrologic data Green Creek, Brazos River basin, Texas, 1967","interactions":[],"lastModifiedDate":"2024-09-13T13:26:07.152429","indexId":"70214101","displayToPublicDate":"1967-09-12T11:42:37","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Compilation of hydrologic data Green Creek, Brazos River basin, Texas, 1967","docAbstract":"The U.S. Soil Conservation Service is actively engaged in the installation of flood and soil erosion reducing measures in Texas under the authority of \"The Flood Control Act of 1936 and 1944\" and \"Watershed Protection and Flood Prevention Act\" (Public Law 566), as amended. The Soil Conservation Service has found a total of 3,438 floodwater-retarding structures to be physically and economically feasible in Texas. As of September 30, 1967, 1,196 of these structures had been built.
This watershed-development program will have varying but important effects on the natural surface- and ground-water resources of river basins, especially where a large number of the floodwater-retarding structures are built. Basic hydrologic data under natural and developed conditions are needed to appraise the effects of the structures on the yield and mode of occurrence of runoff.
Hydrologic investigations of these small watersheds, both developed and undeveloped, were begun by the Geological Survey in 1951 and are now being made in 11 areas (fig. 1). These studies are being made in cooperation with the Texas Water Development Board, the Soil Conservation Service, the San Antonio River Authority, the city of Dallas and the Tarrant County Water Control and Improvement District No. 1. The 11 study areas were chosen to sample watersheds having different rainfall, topography, geology, and soils. In four of the study areas (North, Little Elm, Mukewater, and Pin Oak Creeks), streamflow and rainfall records were collected prior to construction of the floodwater-retarding structures, thus affording the opportunity for analyses of the conditions \"before and after\" development. Structures have now been built in three of these study areas. A summary of the development of the floodwater-retarding structures in each study area as of September 30, 1967, is shown in table 1.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70214101","collaboration":"Prepared in cooperation with Texas Water Development Board and Soil Conservation Service","usgsCitation":"U.S. Geological Survey, 1967, Compilation of hydrologic data Green Creek, Brazos River basin, Texas, 1967: Open-File Report, iii, 34 p., https://doi.org/10.3133/70214101.","productDescription":"iii, 34 p.","costCenters":[],"links":[{"id":425045,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70214101/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":425044,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70214101/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW"} ,{"id":70207355,"text":"70207355 - 1967 - Applications of factor analysis in study of chemistry of groundwater quality, Mojave River Valley, California","interactions":[],"lastModifiedDate":"2019-12-19T07:41:52","indexId":"70207355","displayToPublicDate":"1967-06-30T09:51:59","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Applications of factor analysis in study of chemistry of groundwater quality, Mojave River Valley, California","docAbstract":"Factor analysis is applied to results of chemical analyses of 103 water samples from wells in the Upper and Middle Mojave River valley, San Bernardino County, California. Chemical analyses showed that there are three principal chemical types of water, calcium bicarbonate, sodium sulfate, and sodium chloride, as well as many mixtures of the three. Data were studied by factor analysis to learn the relative importance of each principal ion in determining the variations among the samples, and to examine the possibility of chemical equilibrium between aqueous and solid phases in the aquifers. Most of the covariance in the system may be accounted for by variances of Ca+2, Mg+2, Na+1, SO4−2, and Cl−1. There is almost identical loading on the constituents Na+1 and Cl−1. The variance in chemical composition of the hydrochemical system is governed largely by sources of sodium chloride. None of the components is controlled by equilibrium between ions in the water and minerals in the aquifers. Concentrations of NO3−1 and F−1 vary independently of other constituents. Geographic distribution of statistical loadings of the principal constituents at individual wells does not reveal sources of the constituents, which must be deduced from geologic and hydrologic evidence. Factor analysis, however, furnished the critical information on chemical relationships basic to the deduction.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR003i002p00505","issn":"00431397","usgsCitation":"Dawdy, D., and Feth, J.H., 1967, Applications of factor analysis in study of chemistry of groundwater quality, Mojave River Valley, California: Water Resources Research, v. 3, no. 2, p. 505-510, https://doi.org/10.1029/WR003i002p00505.","productDescription":"6 p. ","startPage":"505","endPage":"510","costCenters":[],"links":[{"id":370397,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":" Mojave River Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.6845703125,\n 32.565333160841035\n ],\n [\n -114.5654296875,\n 32.565333160841035\n ],\n [\n -114.5654296875,\n 36.2265501474709\n ],\n [\n -121.6845703125,\n 36.2265501474709\n ],\n [\n -121.6845703125,\n 32.565333160841035\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"3","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","contributors":{"authors":[{"text":"Dawdy, D.R.","contributorId":99956,"corporation":false,"usgs":true,"family":"Dawdy","given":"D.R.","affiliations":[],"preferred":false,"id":777798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777799,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221315,"text":"70221315 - 1967 - Second session occurrence of ground water in different geologic environments","interactions":[],"lastModifiedDate":"2022-11-22T18:03:25.629766","indexId":"70221315","displayToPublicDate":"1967-06-01T13:17:29","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2126,"text":"JAWRA","active":true,"publicationSubtype":{"id":10}},"title":"Second session occurrence of ground water in different geologic environments","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1967.tb05879.x","usgsCitation":"McGuinness, C.L., 1967, Second session occurrence of ground water in different geologic environments: JAWRA, v. 3, no. 2, https://doi.org/10.1111/j.1752-1688.1967.tb05879.x.","productDescription":"1 p.","startPage":"3","costCenters":[],"links":[{"id":386361,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","contributors":{"authors":[{"text":"McGuinness, C. L.","contributorId":20313,"corporation":false,"usgs":true,"family":"McGuinness","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":817291,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221312,"text":"70221312 - 1967 - Effects on ground‐water quality and induced infiltration of wastes disposed into the Hocking River at Lancaster, Ohio","interactions":[],"lastModifiedDate":"2021-06-09T17:54:59.74169","indexId":"70221312","displayToPublicDate":"1967-06-01T12:50:42","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Effects on ground‐water quality and induced infiltration of wastes disposed into the Hocking River at Lancaster, Ohio","docAbstract":"Watercourse aquifer systems in many areas are adversely affected by wastes disposed into surface‐water sources, resulting in either reduced streambed permeability, infiltration of wastes into the aquifer, or both. These conditions are illustrated at Lancaster, Ohio, where low streambed permeability in the vicinity of the municipal well field, resulting from the discharge of wastes to the Hocking River, seriously retards the infiltration of surface water and lessens the available yield of the wells. The wastes consist of brine and iron‐laden effluent from the municipal treatment plant, discharged within the area of influence of the pumped wells to a stream already carrying much organic waste and other debris. Upstream from the discharge sewer, muck and organic debris have accumulated thickly on the streambed, while downstream from the sewer the streambed sediments have become tightly cemented by iron and other constituents in the waste water. There is evidence that, despite reduced streambed permeability, wastes have entered the aquifer and have materially contributed to declines in well efficiency and to recurring problems of well maintenance. Conditions such as those illustrated at Lancaster occur also at Dayton and are not uncommon elsewhere in Ohio. Indirect contamination of aquifers and adverse physical and chemical alteration of streambed sediments, resulting from surface‐water waste disposal, may in many places pose a threat to the ground‐water supply. This fact should not be overlooked in determining water‐quality standards to be established under the Water Quality Act of 1965.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb03662.x","usgsCitation":"Norris, S., 1967, Effects on ground‐water quality and induced infiltration of wastes disposed into the Hocking River at Lancaster, Ohio: Groundwater, v. 5, no. 3, p. 15-19, https://doi.org/10.1111/j.1745-6584.1967.tb03662.x.","productDescription":"5 p.","startPage":"15","endPage":"19","costCenters":[],"links":[{"id":386358,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Ohio","city":"Lancaster","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.85888671875,\n 39.605688178320804\n ],\n [\n -82.24365234375,\n 39.605688178320804\n ],\n [\n -82.24365234375,\n 39.85072092501597\n ],\n [\n -82.85888671875,\n 39.85072092501597\n ],\n [\n -82.85888671875,\n 39.605688178320804\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Norris, S.E.","contributorId":43771,"corporation":false,"usgs":true,"family":"Norris","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":817288,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221306,"text":"70221306 - 1967 - Epifauna of the Patuxent River Estuary, Maryland, for 1963 and 1964","interactions":[],"lastModifiedDate":"2021-06-09T16:38:55.813498","indexId":"70221306","displayToPublicDate":"1967-06-01T11:32:11","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1228,"text":"Chesapeake Science","active":true,"publicationSubtype":{"id":10}},"title":"Epifauna of the Patuxent River Estuary, Maryland, for 1963 and 1964","docAbstract":"Methods of collection and analysis of epifaunal communities from six stations in the Patuxent estuary are described. The stations were distributed from Solomons near the mouth of the estuary, upstream to Lower Marlboro, near the limit of salt water intrusion. Species composition and abundance, seasons of attachment, and production of the epifaunal community were determined on material collected from panels submerged for 1, 3, and 12 month periods covering the years 1963 and 1964. Salinity was highest downstream, as was the number of species. Salinity decreased rapidly between the Patuxent River Bridge station and Lower Marlboro, where the number of species was reduced to half. Seasons of attachment corresponded with seasonal temperature changes, with the greatest attachment taking place during the summer months. Over 40 species were identified with 7 of them comprising the bulk of the biomass produced. For the 7 most productive species, seasons of attachment and total numbers collected from areas of one square decimeter from monthly and quarterly panels from each station are shown. The seven species were the barnacle Balanus improvisus; the tunicate, Molgula manhattensis; the hydroids, Cordylophora lacustris and Bimeria franciscana; the amphipod, Corophium lacustre; the anemone Sagartia leucolena; the tubeworm, Polydora ligni. Their respective importance varied with seasons of attachment and location. Comments on the distribution and abundance of the less significant forms are included. Dry and ash-free dry weight (organic carbon) production of the epifaunal community varied from month to month depending on the seasons of attachment of the various species. The highest production for a single month was observed at the upriver station, Lower Marlboro, where barnacles and amphipods produced 2,754 g/m2/30 days dry weight and 351 gc/m2/30 days organic weight during August 1963. At the same station, barnacles, amphipods, and hydroids produced, on quarterly panels, the highest yearly average weight of about 1150 gc/m2/yr organic carbon and on monthly panels, about 6,500 g/m2/yr dry weight or about 3.5 times the least organic weight and 8 times the least dry weight produced at the downriver Station, Queentree Landing.
","language":"English","publisher":"Estuarine Research Federation","doi":"10.2307/1351152","usgsCitation":"Cory, R.L., 1967, Epifauna of the Patuxent River Estuary, Maryland, for 1963 and 1964: Chesapeake Science, v. 8, no. 2, p. 71-89, https://doi.org/10.2307/1351152.","productDescription":"19 p.","startPage":"71","endPage":"89","costCenters":[],"links":[{"id":386353,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.80541992187499,\n 38.238180119798635\n ],\n [\n -76.39617919921875,\n 38.238180119798635\n ],\n [\n -76.39617919921875,\n 38.839707613545144\n ],\n [\n -76.80541992187499,\n 38.839707613545144\n ],\n [\n -76.80541992187499,\n 38.238180119798635\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"8","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cory, R. L.","contributorId":49456,"corporation":false,"usgs":true,"family":"Cory","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":817282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206895,"text":"70206895 - 1967 - Evidence for submarine discharge of water on the Atlantic continental slope of the southern United States, and suggestions for further search","interactions":[],"lastModifiedDate":"2019-11-26T10:48:32","indexId":"70206895","displayToPublicDate":"1967-05-31T10:40:16","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5892,"text":"Transactions of the New York Academy of Sciences","active":false,"publicationSubtype":{"id":10}},"title":"Evidence for submarine discharge of water on the Atlantic continental slope of the southern United States, and suggestions for further search","docAbstract":"No abstract available.
","language":"English","publisher":"New York Academy of Sciences","doi":"10.1111/j.2164-0947.1967.tb02825.x","usgsCitation":"Manheim, F.T., 1967, Evidence for submarine discharge of water on the Atlantic continental slope of the southern United States, and suggestions for further search: Transactions of the New York Academy of Sciences, v. 29, no. 7 , p. 839-853, https://doi.org/10.1111/j.2164-0947.1967.tb02825.x.","productDescription":"15 p.","startPage":"839","endPage":"853","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":369631,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"7 ","noUsgsAuthors":false,"publicationDate":"2012-04-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":776181,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010484,"text":"70010484 - 1967 - Geochemical evidence of present-day serpentinization","interactions":[],"lastModifiedDate":"2026-02-09T16:33:24.542339","indexId":"70010484","displayToPublicDate":"1967-05-12T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical evidence of present-day serpentinization","docAbstract":"Ultrabasic (pH > 11) water issues from some fresh ultramafic bodies. The properties of the ultrabasic solutions are believed to be due to current reactions yielding serpentine from primary olivines and pyroxenes. The low concentrations of divalent iron. divalent magnesium, and dissolved silica from the serpentinization require an increase in rock volume.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.156.3776.830","issn":"00368075","usgsCitation":"Barnes, I., LaMarche, V.C., and Himmelberg, G., 1967, Geochemical evidence of present-day serpentinization: Science, v. 156, no. 3776, p. 830-832, https://doi.org/10.1126/science.156.3776.830.","productDescription":"3 p.","startPage":"830","endPage":"832","costCenters":[],"links":[{"id":219239,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"156","issue":"3776","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1634e4b0c8380cd550b3","contributors":{"authors":[{"text":"Barnes, I.","contributorId":23678,"corporation":false,"usgs":true,"family":"Barnes","given":"I.","affiliations":[],"preferred":false,"id":359028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaMarche, Valmore C. Jr.","contributorId":101719,"corporation":false,"usgs":true,"family":"LaMarche","given":"Valmore","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359030,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Himmelberg, G.","contributorId":29565,"corporation":false,"usgs":true,"family":"Himmelberg","given":"G.","affiliations":[],"preferred":false,"id":359029,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70208390,"text":"70208390 - 1967 - Standards for water quality","interactions":[],"lastModifiedDate":"2020-02-06T15:32:41","indexId":"70208390","displayToPublicDate":"1967-04-30T15:29:42","publicationYear":"1967","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Standards for water quality","docAbstract":"The quality which is necessary depends on the use to which the water will be put. Because uses vary, so also must quality standards. Maintaining any level of quality presents a problem of cost and depends on variations in natural water characteristics, in time and space, and variations in volume and types of wastes. For quality standards appropriate to a given water body, hydrologic network data can provide duration curves of flow, concentrations of dissolved oxygen, dissolved solids, including nutrients (nitrates and phosphates), turbidity, temperature, and other significant chemical, physical, and biological parameters. Standards can then be expressed as occurrences in percentage of time or with respect to flow.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"World petroleum congress proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"World Petroleum Congress","conferenceDate":"Apr 2-9, 1967","conferenceLocation":"Mexico City, Mexico","language":"English","publisher":"Curran Associates","usgsCitation":"Leopold, L., 1967, Standards for water quality, in World petroleum congress proceedings, v. 1967, Mexico City, Mexico, Apr 2-9, 1967, p. 271-275.","productDescription":"5 p.","startPage":"271","endPage":"275","costCenters":[],"links":[{"id":372126,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1967","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Leopold, Luna B.","contributorId":46582,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna B.","affiliations":[],"preferred":false,"id":781699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1001416,"text":"1001416 - 1967 - Stump and tree nesting by mallards and black ducks","interactions":[],"lastModifiedDate":"2025-02-12T16:26:36.899555","indexId":"1001416","displayToPublicDate":"1967-04-03T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Stump and tree nesting by mallards and black ducks","docAbstract":"Studies conducted 1961-65 at the Montezuma National Wildlife Refuge in New York demonstrated that mallards (Anas platyrhynchos) and black ducks (Anas rubripes) make extensive use of stumps and dead snags for nest sites. Nest densities in timbered habitats compared favorably with those in untimbered habitats. Nest success was generally higher in timbered than in untimbered areas, except for a newly flooded impoundment where nest success was poor. A simple artificial nest structure was used to increase the number of available nest sites in some of the timbered habitats. Development of stump-nesting populations of ducks may furnish a means of increasing waterfowl production in forested areas.
","language":"English","publisher":"Wiley","doi":"10.2307/3798311","usgsCitation":"Cowardin, L.M., Cummings, G., and Reed, P., 1967, Stump and tree nesting by mallards and black ducks: Journal of Wildlife Management, v. 31, no. 2, p. 229-235, https://doi.org/10.2307/3798311.","productDescription":"7 p.","startPage":"229","endPage":"235","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487972,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3798311","text":"Publisher Index Page"},{"id":129254,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Montezuma National Wildlife Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.84477469582741,\n 43.092038474103845\n ],\n [\n -76.84477469582741,\n 42.94214802992465\n ],\n [\n -76.6614374815742,\n 42.94214802992465\n ],\n [\n -76.6614374815742,\n 43.092038474103845\n ],\n [\n -76.84477469582741,\n 43.092038474103845\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"31","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c59","contributors":{"authors":[{"text":"Cowardin, Lewis M.","contributorId":34574,"corporation":false,"usgs":true,"family":"Cowardin","given":"Lewis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":311004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, G.E.","contributorId":69926,"corporation":false,"usgs":true,"family":"Cummings","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":311002,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, P.B. Jr.","contributorId":87892,"corporation":false,"usgs":true,"family":"Reed","given":"P.B.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":311003,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221311,"text":"70221311 - 1967 - Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water","interactions":[],"lastModifiedDate":"2021-06-11T11:51:46.396788","indexId":"70221311","displayToPublicDate":"1967-04-01T12:45:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water","docAbstract":"The Geological Survey has been the foremost agency in the investigation of ground‐water resources in the United States beginning about 1910. Most of the basic principles of modern ground‐water hydrology were developed in the Survey's program of cooperative investigations. Use of ground water in the United States in 1960 was about 17½ percent of all water uses, excluding water power. The use will probably increase, though at a decreasing rate. Although amount of use may level off, the need to know about it will not. While coordinating its activities with those of the Office of Water Data Coordination and the Office of Water Resources Research, the Survey expects to step up its work in all three areas of data collection, investigations, and research. However, there will be changes of emphasis. Collection of raw data will tend to stress key observation points, and more and more observation of temperature and quality, including contaminants. Investigations will be aimed at upgrading reconnaissance coverage to general coverage for most of the Nation. The areal basis will be stream drainage basins and special hydrologic terranes, rather than political units. There will be an increase in the preparation of analog models for representative ground‐water systems. In research, the problem‐oriented basis will continue. Stress will be on basic principles that pertain to artificial recharge, and the natural recharge and discharge of ground‐water reservoirs; and also on the application of geologic principles on a regional scale. These are critical elements in the management of surface‐water and ground‐water resources conjunctively in river basins.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01244.x","usgsCitation":"Upson, J., 1967, Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water: Groundwater, v. 5, no. 2, p. 13-19, https://doi.org/10.1111/j.1745-6584.1967.tb01244.x.","productDescription":"7 p.","startPage":"13","endPage":"19","costCenters":[],"links":[{"id":386408,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Upson, J. E.","contributorId":49342,"corporation":false,"usgs":true,"family":"Upson","given":"J. E.","affiliations":[],"preferred":false,"id":817408,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221310,"text":"70221310 - 1967 - Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water","interactions":[],"lastModifiedDate":"2021-06-09T17:49:06.328407","indexId":"70221310","displayToPublicDate":"1967-04-01T12:45:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water","docAbstract":"The Geological Survey has been the foremost agency in the investigation of ground‐water resources in the United States beginning about 1910. Most of the basic principles of modern ground‐water hydrology were developed in the Survey's program of cooperative investigations. Use of ground water in the United States in 1960 was about 17½ percent of all water uses, excluding water power. The use will probably increase, though at a decreasing rate. Although amount of use may level off, the need to know about it will not. While coordinating its activities with those of the Office of Water Data Coordination and the Office of Water Resources Research, the Survey expects to step up its work in all three areas of data collection, investigations, and research. However, there will be changes of emphasis. Collection of raw data will tend to stress key observation points, and more and more observation of temperature and quality, including contaminants. Investigations will be aimed at upgrading reconnaissance coverage to general coverage for most of the Nation. The areal basis will be stream drainage basins and special hydrologic terranes, rather than political units. There will be an increase in the preparation of analog models for representative ground‐water systems. In research, the problem‐oriented basis will continue. Stress will be on basic principles that pertain to artificial recharge, and the natural recharge and discharge of ground‐water reservoirs; and also on the application of geologic principles on a regional scale. These are critical elements in the management of surface‐water and ground‐water resources conjunctively in river basins.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01244.x","usgsCitation":"Upson, J., 1967, Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water: Groundwater, v. 5, no. 2, p. 13-19, https://doi.org/10.1111/j.1745-6584.1967.tb01244.x.","productDescription":"7 p.","startPage":"13","endPage":"19","costCenters":[],"links":[{"id":386357,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Upson, J. E.","contributorId":49342,"corporation":false,"usgs":true,"family":"Upson","given":"J. E.","affiliations":[],"preferred":false,"id":817287,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221352,"text":"70221352 - 1967 - The cone of depression and its use in solving water problems","interactions":[],"lastModifiedDate":"2021-06-11T12:55:49.318001","indexId":"70221352","displayToPublicDate":"1967-04-01T07:51:58","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"The cone of depression and its use in solving water problems","docAbstract":"No abstract available.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1967.tb01242.x","usgsCitation":"Schaefer, E.J., 1967, The cone of depression and its use in solving water problems: Groundwater, v. 5, no. 2, p. 2-4, https://doi.org/10.1111/j.1745-6584.1967.tb01242.x.","productDescription":"3 p.","startPage":"2","endPage":"4","costCenters":[],"links":[{"id":480345,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1745-6584.1967.tb01242.x","text":"Publisher Index Page"},{"id":386414,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Schaefer, Edward J.","contributorId":260170,"corporation":false,"usgs":false,"family":"Schaefer","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":817411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70196181,"text":"70196181 - 1967 - Artificial Recharge at Valley City, North Dakota, 1932 to 1965","interactions":[],"lastModifiedDate":"2018-03-22T14:07:24","indexId":"70196181","displayToPublicDate":"1967-04-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Artificial Recharge at Valley City, North Dakota, 1932 to 1965","docAbstract":"Valley City, North Dakota, has an average daily water use of 750,000 gallons, which is obtained from wells tapping pattly confined gravel deposits in the Sheyenne River valley. These deposits at Valley City have a maximum thickness of more than 50 feet and an areal extent of approximately 1 square mile. The aquifer has been artificially recharged successfully since 1932 by diversion of water from the Sheyenne River to an abandoned gravel pit. During this time the piezometric surface in the aquifer has been raised more than 22 feet.
Prior to 1958, the recharge system was operated from January until June; however, when the piezometric surface rose to within about 8 feet of the surface, the recharge operation was discontinued. Between June and January the piezometric surface declined as ground water was withdrawn. During the recharge‐discharge cycle, the average annual fluctuation of the piezometric surface was 10 feet, amounting to a change in storage of about 1,000 acre‐feet of water. Since 1958, the recharge system has been operated throughout the year. There has been a gradual improvement in the quality of the water in the aquifer since the installation of the recharge system.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01245.x","usgsCitation":"Kelly, T.E., 1967, Artificial Recharge at Valley City, North Dakota, 1932 to 1965: Groundwater, v. 5, no. 2, p. 20-25, https://doi.org/10.1111/j.1745-6584.1967.tb01245.x.","productDescription":"6 p.","startPage":"20","endPage":"25","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352739,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","city":"Valley City","volume":"5","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","scienceBaseUri":"5aff5ed3e4b0da30c1bfdda9","contributors":{"authors":[{"text":"Kelly, T. E.","contributorId":63824,"corporation":false,"usgs":true,"family":"Kelly","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":731561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047453,"text":"70047453 - 1967 - Temperature and water-quality conditions for the period July 1963 to December 1965, Patuxent River Estuary, Maryland","interactions":[],"lastModifiedDate":"2013-09-19T13:13:44","indexId":"70047453","displayToPublicDate":"1967-01-06T13:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Temperature and water-quality conditions for the period July 1963 to December 1965, Patuxent River Estuary, Maryland","docAbstract":"Graphs and tables obtained from continuous records of surface-water temperature from five stations for the period july 1963 through December 1965 and of surface, salinity, dissolved oxygen, turbidity, tide-stage, wind data and bottom temperature from a single station are presented herein. Effects of powerplant cooling water on water temperature were obvious at a station near the plant's discharge point. Surface-water density at the Patuxent River Bridge varied from 1.0033 to 1.0127 with least change during the period May to September. Salinity ranged from 3 to 16.5 parts per thousand. Average salinity in the spring of 1965 was double that of spring 1964. Turbidity was high during the winter, and peak values were obtained during prolonged periods of high wind velocities. Dissolved oxygen values ranged from 386 to 15.0 parts per million, and percentage saturation of oxygen from 49 to 144 percent. The extreme tidal range was 5.7 feet; mean water levels were highest in summer and lowest in winter and spring.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","doi":"10.3133/70047453","usgsCitation":"Cory, R.L., and Nauman, J.W., 1967, Temperature and water-quality conditions for the period July 1963 to December 1965, Patuxent River Estuary, Maryland: Open-File Report, 72 p., https://doi.org/10.3133/70047453.","productDescription":"72 p.","numberOfPages":"83","costCenters":[],"links":[{"id":277876,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047453/report.pdf"},{"id":276130,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047453/report-thumb.jpg"}],"country":"United States","state":"Maryl","otherGeospatial":"Patuxent River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.709290,38.300176 ], [ -76.709290,38.638327 ], [ -76.389313,38.638327 ], [ -76.389313,38.300176 ], [ -76.709290,38.300176 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae9e4b0e21cafa49c97","contributors":{"authors":[{"text":"Cory, Robert L.","contributorId":77967,"corporation":false,"usgs":true,"family":"Cory","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":482070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nauman, Jon W.","contributorId":56232,"corporation":false,"usgs":true,"family":"Nauman","given":"Jon","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":482069,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70039370,"text":"70039370 - 1967 - Prospecting for gold in the United States","interactions":[],"lastModifiedDate":"2012-08-04T01:01:57","indexId":"70039370","displayToPublicDate":"1967-01-02T09:46:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Prospecting for gold in the United States","docAbstract":"Prospecting for gold is something that probably everyone dreams of trying at least once. To the person who is mainly concerned with this activity as a vacation diversion, prospecting offers a special excitement. There is a constant hope that the next pan of sediment may be \"pay dirt,\" and no other thrill can compare with that experienced when one sees even a few tiny flecks of gold glittering in the black sand at the bottom of his pan. The search itself is its own reward for the efforts expended by the vacation prospector. The would-be prospector hoping for financial gain, however, should carefully consider all the facts of the situation before deciding to set out on a prospecting expedition.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039370","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Prospecting for gold in the United States: General Information Product, 15 p., https://doi.org/10.3133/70039370.","productDescription":"15 p.","numberOfPages":"16","costCenters":[],"links":[{"id":261508,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039370/report.pdf"},{"id":261509,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039370/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8f50e4b0c8380cd7f6b5","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535277,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70110392,"text":"wdrIN661 - 1967 - Water resources data for Indiana, 1966","interactions":[],"lastModifiedDate":"2014-06-11T09:46:03","indexId":"wdrIN661","displayToPublicDate":"1967-01-01T14:01:45","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IN-66-1","title":"Water resources data for Indiana, 1966","docAbstract":"The surface-water records for the 1966 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering states.
\nThe quality-of-water investigations of the U.S. Geological Survey are concerned with the chemical and physical characteristics of surface- and ground-water supplies of the Nation. The basic records for the 1966 water year for quality of surface waters within the State of Indiana are given in this report. For convenience and interest, there are also records for a few water quality stations in bordering states.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrIN661","collaboration":"Prepared in cooperation with Indiana Department of Natural Resources; Indiana State Board of Health; Indiana State Highway Commission; Corps of Engineers, U.S. Army","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Water resources data for Indiana, 1966: U.S. Geological Survey Water Data Report IN-66-1, viii, 252 p., https://doi.org/10.3133/wdrIN661.","productDescription":"viii, 252 p.","numberOfPages":"266","temporalStart":"1965-10-01","temporalEnd":"1966-09-30","costCenters":[],"links":[{"id":288276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288275,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/in-66-1/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"538052d2e4b0826cd5016a66","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535660,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70114650,"text":"70114650 - 1967 - Results of the second phase of the drought-disaster test-drilling program near Morristown, N.J.","interactions":[],"lastModifiedDate":"2018-01-08T18:31:02","indexId":"70114650","displayToPublicDate":"1967-01-01T13:17:37","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":149,"text":"New Jersey Division of Water Policy and Supply Water Resources Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"17","title":"Results of the second phase of the drought-disaster test-drilling program near Morristown, N.J.","docAbstract":"The continued drought in northeastern New Jersey through the summer of 1966 with its attendant water-supply problems resulted in an extension of the drought-disaster test-drilling program originally requested by the Office of Emergency Planning on August 30, 1965. Authorization to continue test drilling was fiven by the Office of Emergency Planning on September 26, 1966, with the stipulation that all field work be complete by January 31, 1977. Contractural costs were paid by the Office of Emergency Planning, whereas personnel costs were shared by the U.S. Geological Survey and the New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply.
The work undertaken in 1965 by the Geological Survey was \"...to preform the necessary drilling and testing of wells to identify the extent and nature of a reserve ground-water source in the vicinity of the Passaic River near the northern New Jersey metropolitan area.\" Results of this first phase were made available in the fall of 1966 in Water Resources Circular 16 of the New Jersey Department of Conservation and Economic Development. Three of the five areas tested (figure 1)--two in Parsippany-Troy Hills Township (areas 2 and 4) and one in East Hanover Township (area 1), Morris County--proved capable of providing an aggregate sustained yield of 7.5 million gallons daily (mgd) from wells constructed in sand and gravel deposits. Because significant supplies of ground water for emergency use were located in the first phase of the exploratory test-drilling program, it was though desirable to extend the originally planned studies so as to obtain maximum practicable information on emergency supplies.
During this second phase of the investigation, drilling was conducted in 16 sites in Chatham, Madison, and Florham Park Boroughs and in Hanover and East Hanover Townships, Morris County. (See figure 2.) The drilling in Hanover and East Hanover Townships, and part of the drilling done in Florham Park was to explore the availability of large undeveloped ground-water supplies. Drilling in Chatham, Madison, and Florham Park Boroughs was done primarily to determine the extent and continuity of buried valley-fill aquifers, so that a full evaluation of the effects of pumpage from other areas on these already heavily pumped areas could be made. In addition, it was anticipated that the drilling could help in defining the feasibility of artificial recharge of the heavily pumped areas and in the determination of the prospective method of recharge and points of emplacement.
Arrangements for easements with landowners, preparation of specifications for well drilling and seismic work, and supervision of well drilling and seismic contracts were all performed by the New Jersey District, Water Resources Division of the Geological Survey.
Prior to the test drilling, seismic exploration under contract with Alpine Geophysical Associates of Norwood, N. J. was conducted at five locations in the Chatham-Madison-Florham Park area and at one place in Parsippany-Troy Hills Township. The seismic work was done to determine the most favorable location for a test well at several potential test-well sites and to help in the interpretation of subsurface geology between test sites.
Contracts for the drilling of the test holes were awarded during November and drilling commences on November 30. Kaye Well drilling, Inc. of Jackson, N. J. was the recipient of a contract for eight of the test holes, and a second contract was awarded to Rinbrand Well Drilling Co., Inc. of Glen Rock, N. J.--also for eight test holes.
Acknowledgment is due to the many public officials of Chatham, Madison, Florham Park, Morristown, and East Hanover Township as well as officials of the Braidburn Corporation and Esso Research and Engineering Co., who cooperated by making their lands available for exploration.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Trenton, NJ","collaboration":"Prepared by the State of New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply, in cooperation with United States Department of the Interior Geological Survey","usgsCitation":"Vecchioli, J., Nichols, W., and Nemickas, B., 1967, Results of the second phase of the drought-disaster test-drilling program near Morristown, N.J.: New Jersey Division of Water Policy and Supply Water Resources Circular 17, Report: v, 23 p.; 3 Plates: 34.65 x 21.48 inches or smaller.","productDescription":"Report: v, 23 p.; 3 Plates: 34.65 x 21.48 inches or smaller","numberOfPages":"30","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":290164,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327417,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70114650/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":327415,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70114650/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":327416,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70114650/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":290163,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114650/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey","city":"Morristown","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.501444,40.780231 ], [ -74.501444,40.818361 ], [ -74.456181,40.818361 ], [ -74.456181,40.780231 ], [ -74.501444,40.780231 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ad40f9e4b0729c154181d6","contributors":{"authors":[{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":495394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nichols, William D.","contributorId":98296,"corporation":false,"usgs":true,"family":"Nichols","given":"William D.","affiliations":[],"preferred":false,"id":495395,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nemickas, Bronius","contributorId":105733,"corporation":false,"usgs":true,"family":"Nemickas","given":"Bronius","email":"","affiliations":[],"preferred":false,"id":495396,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70039249,"text":"70039249 - 1967 - Mountains and plains Denver's geologic setting","interactions":[],"lastModifiedDate":"2012-08-03T01:02:04","indexId":"70039249","displayToPublicDate":"1967-01-01T13:01:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Mountains and plains Denver's geologic setting","docAbstract":"A slice of geologic history is exposed to view in the Denver, Colorado area. Denver is situated on the High Plains near the east front of the Rocky Mountains. As one travels westward from Denver toward the mountains, successively older rocks are crossed from the geologically young rocks of the High Plains and the South Platte River valley to the older rocks of the foothills and the ancient rocks of the mountains. Thus, within a few miles,the journey turns back the pages of time in a lifesized textbook that vividly illustrates the geologic events that shaped the landscape.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039249","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Mountains and plains Denver's geologic setting: General Information Product, 23 p., https://doi.org/10.3133/70039249.","productDescription":"23 p.","numberOfPages":"24","costCenters":[],"links":[{"id":261472,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039249/report.pdf"},{"id":261473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039249/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Denver","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.25,38.833333333333336 ], [ -106.25,40.583333333333336 ], [ -103.5,40.583333333333336 ], [ -103.5,38.833333333333336 ], [ -106.25,38.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ebae4b0c8380cd70c33","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}