{"pageNumber":"2496","pageRowStart":"62375","pageSize":"25","recordCount":68760,"records":[{"id":70161925,"text":"70161925 - 1968 -  The administration of sulfonamide drugs to adult salmon","interactions":[],"lastModifiedDate":"2016-02-08T16:55:47","indexId":"70161925","displayToPublicDate":"2011-01-09T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":" The administration of sulfonamide drugs to adult salmon","docAbstract":"<p>The artificial propagation of salmon starts with the capture of adults as they ascend rivers to spawn. After capture, they are retained in specially constructed holding areas until sexually mature. Though holding periods vary with species, the spring chinook (<i>Oncorhynchus tshawytsca</i>) may be held as long as 4 months before they are spawned. During this interval the fish are often closely confined at unfavorable water temperatures and fatal diseases sometimes reach epizootic proportions. It is important that methods be devised to control or prevent infectious diseases in adult salmon while they are in the holding ponds.</p>\n<p>Mass treatment is the most convenient way to combat fish diseases. For example, drugs can be administered per os in diets, or chemicals can be added to the water. These methods are mostly ineffective in treating systemic infections of adult salmon because mature salmon do not feed, and many fish diseases cannot be controlled by chemical baths. Thus, effective treatment would require administering drugs to each individual.</p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8640(1968)30[168:TAOSDT]2.0.CO;2","usgsCitation":"Amend, D., and Fryer, J.L., 1968,  The administration of sulfonamide drugs to adult salmon: Progressive Fish-Culturist, v. 30, no. 3, p. 168-172, https://doi.org/10.1577/1548-8640(1968)30[168:TAOSDT]2.0.CO;2.","productDescription":"5 p.","startPage":"168","endPage":"172","numberOfPages":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314074,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5694e039e4b039675d005dd3","contributors":{"authors":[{"text":"Amend, D.F.","contributorId":63082,"corporation":false,"usgs":true,"family":"Amend","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":588093,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fryer, J. L.","contributorId":21900,"corporation":false,"usgs":true,"family":"Fryer","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":588094,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5220074,"text":"5220074 - 1968 - Collecting and rearing black flies","interactions":[],"lastModifiedDate":"2023-02-21T17:24:10.637782","indexId":"5220074","displayToPublicDate":"2010-06-16T12:17:39","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":798,"text":"Annals of the Entomological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Collecting and rearing black flies","docAbstract":"<p><span>This paper, based on a study carried out at the Seney National Wildlife Refuge, Seney, Michigan, and the Patuxent Wildlife Research Center, Laurel, Maryland, describes methods and techniques for collecting, storing, and rearing 8 species of Simuliidae. Included in the study were&nbsp;</span><i>Cnephia dacotensis</i><span>&nbsp;(Dyar &amp; Shannon),&nbsp;</span><i>C. mutata</i><span>&nbsp;(Malloch),&nbsp;</span><i>Prosimulium fuscum</i><span>&nbsp;Syme &amp; Davies,&nbsp;</span><i>Simulium aureum</i><span>&nbsp;Fries,&nbsp;</span><i>S. decorum</i><span>&nbsp;(Walker),&nbsp;</span><i>S. venustum</i><span>&nbsp;Say,&nbsp;</span><i>S. verecundum</i><span>&nbsp;Stone &amp; Jamnback, and&nbsp;</span><i>S. vittattum</i><span>&nbsp;Zetterstedt. Simuliid eggs collected from a variety of habitats, packed with wet materials in plastic bags and held at 4°C, have remained viable, thus far, up to 424 days. Eggs held at 0° to −70°C failed to hatch when placed in rearing aquariums. Air-dried eggs held at 4°C for 339–535 days failed to hatch after being held in aquariums for 166 days. Immature stages of black flies were successfully reared in 1¼-gallon Pyrex jars and 15-gallon plexiglas aquariums in which the water was agitated by compressed air and aquarium pumps. Water velocities of 0.250–0.542 feet per second were obtained in streams of air bubbles created by use of air stones. Of 21 larval diets used, one consisting of Purina Dog Chow (60-mesh or finer), brain-heart infusion broth, and brewer's yeast powder, and a second consisting of Wayne's dog chow (60-mesh or finer) and brain-heart infusion broth without brewer's yeast powder, were most satisfactory. Larvae were fed 1 gram of diet per 1¼- gallon aquarium and 2 grams per 15-gallon aquarium biweekly. In most of the 225 cultures of&nbsp;</span><i>S. aureum, S. decorum, S. verecundum, S. venustum,</i><span>&nbsp;and&nbsp;</span><i>S. Vittatum</i><span>&nbsp;it took from 1 to 5 days for the development of eggs to larvae (165 cultures,&nbsp;</span><i>73%)</i><span>&nbsp;and the same number of days for the development of pupae to adults (172 cultures, 76%). Development time for larvae to pupae was fairly closely divided between 11–15 days (63 cultures, 28%) and 16–20 days (53 cultures, 23.6%). The entire period for development from egg to adult after placement of eggs in rearing aquariums was from 21 to 25 days for 26.7% of the cultures.</span></p>","language":"English","publisher":"Oxford Academic Press","doi":"10.1093/aesa/61.5.1072","usgsCitation":"Tarshis, I., 1968, Collecting and rearing black flies: Annals of the Entomological Society of America, v. 61, no. 5, p. 1072-1083, https://doi.org/10.1093/aesa/61.5.1072.","productDescription":"12 p.","startPage":"1072","endPage":"1083","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194321,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","issue":"5","noUsgsAuthors":false,"publicationDate":"1968-09-16","publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae904","contributors":{"authors":[{"text":"Tarshis, I.B.","contributorId":83625,"corporation":false,"usgs":true,"family":"Tarshis","given":"I.B.","email":"","affiliations":[],"preferred":false,"id":331296,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220073,"text":"5220073 - 1968 - Use of fabrics in streams to collect black fly larvae","interactions":[],"lastModifiedDate":"2023-02-21T17:17:19.373363","indexId":"5220073","displayToPublicDate":"2010-06-16T12:17:39","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":798,"text":"Annals of the Entomological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Use of fabrics in streams to collect black fly larvae","docAbstract":"<p><span>A technique is described for using strips of gauze to collect large numbers of larvae of&nbsp;</span><i>Cnephia dacotensis</i><span>&nbsp;(Dyar &amp; Shannon),&nbsp;</span><i>Simulium decorum</i><span>&nbsp;(Walker),&nbsp;</span><i>S. venustuni</i><span>&nbsp;Say,&nbsp;</span><i>S. vcrecundum</i><span>&nbsp;Stone &amp; Jamnback, and&nbsp;</span><i>S. vittatum</i><span>&nbsp;Zetterstedt from various water habitats.</span></p>","language":"English","publisher":"Oxford Academic Press","doi":"10.1093/aesa/61.4.960","usgsCitation":"Tarshis, I., 1968, Use of fabrics in streams to collect black fly larvae: Annals of the Entomological Society of America, v. 61, no. 4, p. 960-961, https://doi.org/10.1093/aesa/61.4.960.","productDescription":"2 p.","startPage":"960","endPage":"961","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194274,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","issue":"4","noUsgsAuthors":false,"publicationDate":"1968-07-15","publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6045e4","contributors":{"authors":[{"text":"Tarshis, I.B.","contributorId":83625,"corporation":false,"usgs":true,"family":"Tarshis","given":"I.B.","email":"","affiliations":[],"preferred":false,"id":331295,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220597,"text":"5220597 - 1968 - Blood parasites in North American waterfowl","interactions":[],"lastModifiedDate":"2012-02-02T00:15:12","indexId":"5220597","displayToPublicDate":"2010-06-16T12:17:38","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3638,"text":"Transactions of the North American Wildlife and Natural Resources Conference","active":true,"publicationSubtype":{"id":10}},"title":"Blood parasites in North American waterfowl","docAbstract":"One thing seems to stand out in the overall knowledge we have of the blood parasites of waterfowl, as previously noted by Herman and Wehr, (1954): the greatest potential of losses is in the younger age groups, usually those birds 5-10 weeks old. In Leucocytozoon infections, death occurs as early as the first or second week of the bird's life. As a conclusion to this presentation, I wish to emphasize that there are many gaps in our knowledge of these parasites and that the answers are to be obtained by further studies in the young birds.  Data obtained from studies of birds shot by hunters or from specimens taken during fall or winter banding operations can be expected to be far less rewarding and significanf than studies of goslings and ducklings. We need much more knowledge of these parasites and their vectors and other relationships before we can develop management procedures to combat or contain them. It will require many more studies in depth to achieve this goal, but the facts are there waiting to be uncovered.  These parasites will have to be regulated along with breeding habitat, hunter take, and other factors that all add up to maintenance and management of waterfowl.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the North American Wildlife and Natural Resources Conference","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Herman, C.M., 1968, Blood parasites in North American waterfowl: Transactions of the North American Wildlife and Natural Resources Conference, v. 33, p. 348-359.","productDescription":"348-359","startPage":"348","endPage":"359","numberOfPages":"12","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196344,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607762","contributors":{"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":332086,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70159222,"text":"70159222 - 1968 - Geology and ground-water resources of Burlington County, New Jersey","interactions":[],"lastModifiedDate":"2015-11-12T13:58:35","indexId":"70159222","displayToPublicDate":"2010-02-02T05:15:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":126,"text":"New Jersey Division of Water Policy and Supply Special Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"26","title":"Geology and ground-water resources of Burlington County, New Jersey","docAbstract":"<p>Burlington County, which lies between Trenton, Atlantic City and Camden, has an area of 827 square miles. The county is in the Atlantic Coastal Plain physiographic province, has moderate temperatures and a dependable rainfall of 44 inches per year. The area is attracting new industries and additional population. Water usage is increasing with this economic growth; 26 mgd (million gallons per day) of ground water were used in 1960.</p>\n<p>The Raritan and Magothy Formations are the most prolific producers, but the Cohansey Sand and Kirkwood Formation have a great and, as yet, untapped potential. Small to moderately large supplies have been obtained from other aquifers. The maximum average potential recharge to the ground-water reservoirs is estimated to be about 790 mgd. Presently, most of it is rejected because the aquifers are essentially full. On this basis, it is believed that ground-water supplies in Burlington County are sufficient for the foreseeable future. However, well spacing must be planned to avoid local overdevelopment.&nbsp;</p>","language":"English","publisher":"State of New Jersey Department of Convservation and Economic Development, Division of Water Policy and Supply","publisherLocation":"Trenton, N.J.","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the State of New Jersey","usgsCitation":"Rush, F.E., 1968, Geology and ground-water resources of Burlington County, New Jersey: New Jersey Division of Water Policy and Supply Special Report 26, Report: ix, 66 p.;12 Plates: 20.86 x 12.88 inches or smaller.","productDescription":"Report: ix, 66 p.;12 Plates: 20.86 x 12.88 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":310065,"rank":14,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70159222.jpg"},{"id":311234,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-10.pdf","text":"Plate 10","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 10"},{"id":311235,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-11.pdf","text":"Plate 11","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 11"},{"id":311236,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-18.pdf","text":"Plate 18","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 18"},{"id":311237,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-20.pdf","text":"Plate 20","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 20"},{"id":311238,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-22.pdf","text":"Plate 22","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 22"},{"id":311214,"rank":13,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70159222/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":311228,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":311227,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":311229,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 5"},{"id":311230,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 6"},{"id":311231,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-7.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 7"},{"id":311232,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-8.pdf","text":"Plate 8","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 8"},{"id":311233,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159222/plate-9.pdf","text":"Plate 9","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 9"}],"country":"United States","state":"New Jersey","county":"Burlington County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.739990234375,\n              40.189364913019006\n            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,{"id":5210051,"text":"5210051 - 1968 - Values of the South Atlantic and Gulf Coast marshes and estuaries to waterfowl","interactions":[],"lastModifiedDate":"2012-02-02T00:15:13","indexId":"5210051","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1968","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Values of the South Atlantic and Gulf Coast marshes and estuaries to waterfowl","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the Marsh and Estuary Management Symposium","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Louisiana State University","publisherLocation":"Baton Rouge, LA","usgsCitation":"Lynch, J., 1968, Values of the South Atlantic and Gulf Coast marshes and estuaries to waterfowl, chap. <i>of</i> Proceedings of the Marsh and Estuary Management Symposium, p. 52-63.","startPage":"52","endPage":"63","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602c6b","contributors":{"authors":[{"text":"Lynch, J.J.","contributorId":40295,"corporation":false,"usgs":true,"family":"Lynch","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":327685,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38821,"text":"pp544E - 1968 - Seismic seiches from the March 1964 Alaska earthquake","interactions":[],"lastModifiedDate":"2021-08-17T20:30:42.561793","indexId":"pp544E","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1968","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":"544","chapter":"E","title":"Seismic seiches from the March 1964 Alaska earthquake","docAbstract":"Seismic seiches caused by the Alaska earthquake of March 27, 1964, were recorded at more than 850 surface-water gaging stations in North America and at 4 in Australia. In the United States, including Alaska and Hawaii, 763 of 6,435 gages registered seiches. Nearly all the seismic seiches were recorded at teleseismic distance. This is the first time such far-distant effects have been reported from surface-water bodies in North America. The densest occurrence of seiches was in States bordering the Gulf of Mexico. The seiches were recorded on bodies of water having a wide range in depth, width, and rate of flow. In a region containing many bodies of water, seiche distribution is more dependent on geologic and seismic factors than on hydro-dynamic ones. The concept that seiches are caused by the horizontal acceleration of water by seismic surface waves has been extended in this paper to show that the distribution of seiches is related to the amplitude distribution of short-period seismic surface waves. These waves have their greatest horizontal acceleration when their periods range from 5 to 15 seconds. Similarly, the water bodies on which seiches were recorded have low-order modes whose periods of oscillation also range from 5 to 15 seconds. Several factors seem to control the distribution of seiches. The most important is variations of thickness of low-rigidity sediments. This factor caused the abundance of seiches in the Gulf Coast area and along the edge of sedimentary overlaps. Major tectonic features such as thrust faults, basins, arches, and domes seem to control seismic waves and thus affect the distribution of seiches. Lateral refraction of seismic surface waves due to variations in local phase-velocity values was responsible for increase in seiche density in certain areas. For example, the Rocky Mountains provided a wave guide along which seiches were more numerous than in areas to either side. In North America, neither direction nor distance from the epicenter had any apparent effect on the distribution of seiches. Where seismic surface waves propagated into an area with thicker sediment, the horizontal acceleration increased about in proportion to the increasing thickness of the sediment. In the Mississippi Embayment however, where the waves emerged from high rigidity crust into the sediment, the horizontal acceleration increased near the edge of the embayment but decreased in the central part and formed a shadow zone. Because both seiches and seismic intensity depend on the horizontal acceleration from surface waves, the distribution of seiches may be used to map the seismic intensity that can be expected from future local earthquakes.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: effects on the hydrologic regimen (Professional Paper 544)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp544E","usgsCitation":"McGarr, A., and Vorhis, R.C., 1968, Seismic seiches from the March 1964 Alaska earthquake: U.S. Geological Survey Professional Paper 544, Report: 43 p.; 1 Plate: 39.97 inches x 27.98 inches, https://doi.org/10.3133/pp544E.","productDescription":"Report: 43 p.; 1 Plate: 39.97 inches x 27.98 inches","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":388056,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4595.htm"},{"id":65745,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0544e/pp544e_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65744,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0544e/pp544e_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0544e/report-thumb.jpg"},{"id":104508,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0544e/index.html","linkFileType":{"id":5,"text":"html"},"description":"4595"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8,24.5 ], [ -124.8,49.383333 ], [ -66.95,49.383333 ], [ -66.95,24.5 ], [ -124.8,24.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa889","contributors":{"authors":[{"text":"McGarr, Arthur","contributorId":102548,"corporation":false,"usgs":true,"family":"McGarr","given":"Arthur","affiliations":[],"preferred":false,"id":220498,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vorhis, Robert C.","contributorId":52555,"corporation":false,"usgs":true,"family":"Vorhis","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":220497,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38770,"text":"pp585B - 1968 - Evapotranspiration and the water budget of prairie potholes in North Dakota","interactions":[],"lastModifiedDate":"2018-03-16T14:16:46","indexId":"pp585B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"585","chapter":"B","title":"Evapotranspiration and the water budget of prairie potholes in North Dakota","docAbstract":"<p> The mass-transfer method was used to study the hydrologic behavior of 10 prairie potholes in central North Dakota during the 5-year period 1960-64. Many of the potholes went dry when precipitation was low. The average evapotranspiration during the May to October period each year was 2.11 feet, and the average seepage was 0.60 foot. These averages remained nearly constant for both wet and dry years. </p><p>The greatest source of water for the potholes was the direct rainfall on the pond surface; this supplied 1.21 feet per year. Spring snowmelt supplied 0.79 foot of water and runoff from the land surface during the summer supplied 0.53 foot. Even though the water received from snowmelt was only 31 percent of the total, it was probably the most vital part of the annual water supply. This water was available in the spring, when waterfowl were nesting, and generally lasted until about July 1, even with no additional direct rainfall on the pond or runoff from the drainage basin. The average runoff from the land surface into pothole 3 was found to be 1.2 inches per year- 1 inch from snowmelt and 0.2 inch from rainfall.</p><p>'The presence of growing aquatic plants, such as bulrushes and cattails, was a complicating factor in making measurements. New computation procedures had to be devised to define the variable mass-transfer coefficient. Rating periods were divided into 6-hour units for the vegetated potholes. The instruments had to be carefully maintained, as water levels had to be recorded with such accuracy that changes of 0.001 foot could be detected. In any research project involving the measurements of physical quantities, the results are dependent upon the accuracy and dependability of the instruments used; this was especially true during this project. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of prairie potholes in North Dakota","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp585B","usgsCitation":"Shjeflo, J., 1968, Evapotranspiration and the water budget of prairie potholes in North Dakota: U.S. Geological Survey Professional Paper 585, vi, 49 p., https://doi.org/10.3133/pp585B.","productDescription":"vi, 49 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":65642,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0585b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122259,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0585b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9be7","contributors":{"authors":[{"text":"Shjeflo, J.B.","contributorId":30509,"corporation":false,"usgs":true,"family":"Shjeflo","given":"J.B.","affiliations":[],"preferred":false,"id":220424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38785,"text":"pp545C - 1968 - Effects of the earthquake of March 27, 1964, on the Alaska highway system","interactions":[{"subject":{"id":38785,"text":"pp545C - 1968 - Effects of the earthquake of March 27, 1964, on the Alaska highway system","indexId":"pp545C","publicationYear":"1968","noYear":false,"chapter":"C","title":"Effects of the earthquake of March 27, 1964, on the Alaska highway system"},"predicate":"IS_PART_OF","object":{"id":70048241,"text":"pp545 - 1967 - The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","indexId":"pp545","publicationYear":"1967","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities"},"id":1}],"isPartOf":{"id":70048241,"text":"pp545 - 1967 - The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","indexId":"pp545","publicationYear":"1967","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities"},"lastModifiedDate":"2022-02-15T20:27:32.761478","indexId":"pp545C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"545","chapter":"C","title":"Effects of the earthquake of March 27, 1964, on the Alaska highway system","docAbstract":"The great earthquake that struck Alaska about 5:36 p.m., Alaska standard time, Friday, March 27, 1964 (03:36:1.3.0, Greenwich mean time, March 28, 1964), severely crippled the highway system in the south-central part of the State. All the major highways and most secondary roads were impaired. Damage totaled more than $46 million, well over $25 million to bridges and nearly $21 million to roadways. Of the 204 bridges in south-central Alaska, 141 were damaged; 92 were severely damaged or destroyed. The earthquake damaged 186 of the 830 miles of roadway in south-central Alaska, 83 miles so severely that replacement or relocation was required. Earthquake damage to the roadways and bridges was chiefly by (1) seismic shaking, (2) compaction of fills as well as the underlying sediments, (3) lateral displacement of the roadway and bridges, (4) fractures, (5) landslides, (6) avalanches, (7) inundation by seismic sea waves, (8) scouring by seismic sea waves, (9) regional tectonic subsidence, causing inundation and erosion by high tides in subsided areas. The intensity of damage was controlled primarily by the geologic environment (including the depth of the water table) upon which the highway structures rested, and secondarily by the engineering characteristics of the structures. Structures on bedrock were only slightly damaged if at all, whereas those on unconsolidated sediments were slightly to severely damaged, or were completely destroyed by seismic shaking. The low-lying areas underlain by saturated sediments, such as the Snow River Crossing and Turnagain Arm sections of the Seward-Anchorage Highway, were the most severely damaged stretches of the highway system in south-central Alaska. At Snow River and Turnagain Arm, the sediments underlying the roadway are fine grained and the water table is shallow. These factors were responsible for the intense damage along this stretch of the highway. All the bridges on the Copper River Highway except for one on bedrock were damaged by seismic shaking. Lateral displacement of sediments toward a free face, which placed the bridges in compression, was the chief cause for the damage. This type of failure was extensive and widespread throughout the highway system. The chief engineering characteristics responsible for the type and intensity of damage include (1) thickness of roadway fills, (2) type of pile bents and masonry piers, (3) the weight ratio between the substructure and superstructure, and (4) the tie between the substructure and superstructure. The thicker the roadway fills, the more severe the damage. Wood piles did not break as extensively as piles constructed of three railroad rails welded together. Bridges that had relatively heavy superstructures, for example those with concrete decks on wood piles, were more severely damaged than those with all-wood or concrete decks or concrete piers. Failure first occurred at the tie between the superstructure and the substructure; the poorer this tie, the sooner the failure. Seismic sea waves destroyed 12 bridges on the Chiniak Highway on Kodiak Island, one bridge on Point Whitshed road near Cordova, and about 14 miles of roadway. The combination of regional tectonic subsidence and local subsidence and compaction of sediments caused inundation of many miles of highway by high tides, especially around Turnagain Arm. Total subsidence in some places amounted to more than 13 feet.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Effects on transportation, communications, and utilities (Professional Paper 545)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp545C","usgsCitation":"Kachadoorian, R., 1968, Effects of the earthquake of March 27, 1964, on the Alaska highway system: U.S. Geological Survey Professional Paper 545, vi, 66 p., https://doi.org/10.3133/pp545C.","productDescription":"vi, 66 p.","numberOfPages":"74","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":169457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0545c/report-thumb.jpg"},{"id":113232,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0545c/pp545c_text.pdf","size":"14502","linkFileType":{"id":1,"text":"pdf"}},{"id":111459,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0545c/index.html","linkFileType":{"id":5,"text":"html"}},{"id":395998,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_99038.htm"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -154.8193359375,\n              56.68037378950137\n            ],\n            [\n              -145.72265625,\n              56.68037378950137\n            ],\n            [\n              -145.72265625,\n              63.93737246791484\n            ],\n            [\n              -154.8193359375,\n              63.93737246791484\n            ],\n            [\n              -154.8193359375,\n              56.68037378950137\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db61024b","contributors":{"authors":[{"text":"Kachadoorian, Reuben","contributorId":24336,"corporation":false,"usgs":true,"family":"Kachadoorian","given":"Reuben","email":"","affiliations":[],"preferred":false,"id":220441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38757,"text":"pp605A - 1968 - Ground-water hydrology and geology of the lower Great Miami River valley, Ohio","interactions":[{"subject":{"id":52504,"text":"ofr65152 - 1965 - Hydrogeologic aspects of an analog model study of the Fairfield-New Baltimore area, Ohio","indexId":"ofr65152","publicationYear":"1965","noYear":false,"title":"Hydrogeologic aspects of an analog model study of the Fairfield-New Baltimore area, Ohio"},"predicate":"SUPERSEDED_BY","object":{"id":38757,"text":"pp605A - 1968 - Ground-water hydrology and geology of the lower Great Miami River valley, Ohio","indexId":"pp605A","publicationYear":"1968","noYear":false,"chapter":"A","title":"Ground-water hydrology and geology of the lower Great Miami River valley, Ohio"},"id":1},{"subject":{"id":52629,"text":"ofr67205 - 1967 - Bedrock contour maps of the Lower Great Miami River valley, Ohio","indexId":"ofr67205","publicationYear":"1967","noYear":false,"title":"Bedrock contour maps of the Lower Great Miami River valley, Ohio"},"predicate":"SUPERSEDED_BY","object":{"id":38757,"text":"pp605A - 1968 - Ground-water hydrology and geology of the lower Great Miami River valley, Ohio","indexId":"pp605A","publicationYear":"1968","noYear":false,"chapter":"A","title":"Ground-water hydrology and geology of the lower Great Miami River valley, Ohio"},"id":2}],"lastModifiedDate":"2012-02-02T00:09:54","indexId":"pp605A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"605","chapter":"A","title":"Ground-water hydrology and geology of the lower Great Miami River valley, Ohio","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Ground water in the lower Great Miami River Valley, Ohio","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp605A","usgsCitation":"Spieker, A.M., 1968, Ground-water hydrology and geology of the lower Great Miami River valley, Ohio: U.S. Geological Survey Professional Paper 605, p. A1-A37, https://doi.org/10.3133/pp605A.","productDescription":"p. A1-A37","costCenters":[],"links":[{"id":165852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0605a/report-thumb.jpg"},{"id":22016,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0605a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":22017,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0605a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":22018,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0605a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674136","contributors":{"authors":[{"text":"Spieker, A. M.","contributorId":22824,"corporation":false,"usgs":true,"family":"Spieker","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":220400,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38755,"text":"pp600B - 1968 - Geological Survey research 1968, Chapter B","interactions":[],"lastModifiedDate":"2025-08-25T20:08:39.266373","indexId":"pp600B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"600","chapter":"B","title":"Geological Survey research 1968, Chapter B","docAbstract":"<p>This collection of 44 short papers is the first published chapter of \"Geological Survey Research 1968.\" The papers report on scientific and economic results of current work by 1ne1nbers of the Geologic, Topographic, and Water Resources Divisions of the U.S. Geological Survey.</p><p>Chapter A, to be published later in the year, will present a summary of significant results of work done during fiscal year 1968, together with lists of investigations in progress, reports published, cooperating agencies, and Geological Survey offices.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1968","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp600B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1968, Geological Survey research 1968, Chapter B: U.S. Geological Survey Professional Paper 600, v, 235 p., https://doi.org/10.3133/pp600B.","productDescription":"v, 235 p.","numberOfPages":"240","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":494788,"rank":16,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27411.htm","text":"Localization and control of uranium deposits in the southern San Juan basin mineral belt, New Mexico - an hypothesis"},{"id":494787,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_45567.htm","text":"Intrusive rocks of north-central Puerto Rico","linkFileType":{"id":5,"text":"html"}},{"id":494786,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27422.htm","text":"The source of travertine in the Creede Formation, San Juan Mountains, Colorado","linkFileType":{"id":5,"text":"html"}},{"id":494785,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27421.htm","text":"Phosphate nodules from the Wills Point Formation, Hopkins County, Texas","linkFileType":{"id":5,"text":"html"}},{"id":494783,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27419.htm","text":"Preliminary assessment of ground water in the Green River Formation, Uinta Basin, Utah","linkFileType":{"id":5,"text":"html"}},{"id":494782,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27418.htm","text":"Dark mineral accumulations in beach and dune sands of Cape Cod and vicinity","linkFileType":{"id":5,"text":"html"}},{"id":494780,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27416.htm","text":"Late Tertiary syncline in the southern Absaroka Mountains, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":494779,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27415.htm","text":"Recent fault scarps in Independence Valley near Tuscarora, Elko County, Nevada","linkFileType":{"id":5,"text":"html"}},{"id":403316,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27410.htm","text":"Radioelement composition of surface soil in Adams County, Colorado","linkFileType":{"id":5,"text":"html"}},{"id":113225,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0600b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165851,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0600b/report-thumb.jpg"},{"id":494778,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27414.htm","text":"Gravity anomalies in the Ruby Mountains, northeastern Nevada","linkFileType":{"id":5,"text":"html"}},{"id":494777,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27413.htm","text":"Seismic-refraction studies of the Loveland Basin landslide, Colorado","linkFileType":{"id":5,"text":"html"}},{"id":494776,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27412.htm","text":"Thickness of valley fill in the Jordan Valley east of the Great Salt Lake, Utah","linkFileType":{"id":5,"text":"html"}},{"id":494781,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27417.htm","text":"Geology and radiocarbon ages of Late Pleistocene lacustrine clay deposits, southern part of San Joaquin Valley, California","linkFileType":{"id":5,"text":"html"}},{"id":494784,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27420.htm","text":"Occurrence and composition of biotites from the Cartridge Pass pluton of the Sierra Nevada batholith, California","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6877b3","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":529879,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35191,"text":"b1254G - 1968 - Carbonate rocks of Cambrian and Ordovician age in the Lancaster quadrangle, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-21T10:41:50","indexId":"b1254G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1254","chapter":"G","title":"Carbonate rocks of Cambrian and Ordovician age in the Lancaster quadrangle, Pennsylvania","docAbstract":"<p>Detailed mapping has shown that the carbonate rocks of Cambrian and Ordovician age in the Lancaster quadrangle, Pennsylvania, can be divided into 14 rock-stratigraphic units. These units are defined primarily by their relative proportions of limestone and dolomite. The oldest units, the Vintage, Kinzers, and Ledger Formations of Cambrian age, and the Conestoga Limestone of Ordovician age are retained in this report. The Zooks Corner Formation, of Cambrian age, a dolomite unit overlying the Ledger Dolomite, is named here for exposures along Conestoga Creek near the village of Zooks Corner. The Conococheague (Cambrian) and Beekmantown (Ordovician) Limestones, as mapped by earlier workers, have been elevated to group rank and subdivided into formations that are correlated with and named for geologic units in Lebanon and Berks Counties, Pa. These formations, from oldest to youngest, are the Buffalo Springs, Snitz Creek, Millbach, and Richland Formations of the Conococheague Group, and the Stonehenge, Bpler, and Ontelaunee Formations of the Beekmantown Group. The Annville and Myerstown Limestones, which are named for lithologically similar units in Dauphin and Lebanon Counties, Pa., overlie the Beekmantown Group in one small area in the quadrangle. </p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1254G","usgsCitation":"Meisler, H., and Becher, A.E., 1968, Carbonate rocks of Cambrian and Ordovician age in the Lancaster quadrangle, Pennsylvania: U.S. Geological Survey Bulletin 1254, p. G1-G14, illus., maps. ;24 cm., https://doi.org/10.3133/b1254G.","productDescription":"p. G1-G14, illus., maps. ;24 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":63068,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1254g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1254g/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f00b9","contributors":{"authors":[{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":214226,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Becher, Albert E.","contributorId":82979,"corporation":false,"usgs":true,"family":"Becher","given":"Albert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":214227,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48203,"text":"ofr73278 - 1968 - Ground-water resources investigation program for the Kinshasa area, Democratic Republic of the Congo","interactions":[],"lastModifiedDate":"2012-02-02T00:10:38","indexId":"ofr73278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-278","title":"Ground-water resources investigation program for the Kinshasa area, Democratic Republic of the Congo","language":"ENGLISH","doi":"10.3133/ofr73278","usgsCitation":"Tibbitts, G.C., 1968, Ground-water resources investigation program for the Kinshasa area, Democratic Republic of the Congo: U.S. Geological Survey Open-File Report 73-278, 43 p.  ill. ; 27 cm., https://doi.org/10.3133/ofr73278.","productDescription":"43 p.  ill. ; 27 cm.","costCenters":[],"links":[{"id":172396,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db66103f","contributors":{"authors":[{"text":"Tibbitts, G. Chase Jr.","contributorId":30601,"corporation":false,"usgs":true,"family":"Tibbitts","given":"G.","suffix":"Jr.","email":"","middleInitial":"Chase","affiliations":[],"preferred":false,"id":236963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67345,"text":"i541 - 1968 - Reconnaissance geologic map of the Ochoco Reservoir quadrangle, Crook County, Oregon","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i541","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"541","subseriesTitle":"NONE","title":"Reconnaissance geologic map of the Ochoco Reservoir quadrangle, Crook County, Oregon","language":"ENGLISH","doi":"10.3133/i541","usgsCitation":"Waters, A.C., and Vaughan, R., 1968, Reconnaissance geologic map of the Ochoco Reservoir quadrangle, Crook County, Oregon: U.S. Geological Survey IMAP 541, 1 map., https://doi.org/10.3133/i541.","productDescription":"1 map.","costCenters":[],"links":[{"id":103208,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1700.htm","linkFileType":{"id":5,"text":"html"},"description":"1700"},{"id":188105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.75,44.25 ], [ -120.75,44.5 ], [ -120.5,44.5 ], [ -120.5,44.25 ], [ -120.75,44.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641915","contributors":{"authors":[{"text":"Waters, A. C.","contributorId":13304,"corporation":false,"usgs":true,"family":"Waters","given":"A.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":276021,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vaughan, R.H.","contributorId":65169,"corporation":false,"usgs":true,"family":"Vaughan","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":276022,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67217,"text":"i543 - 1968 - Reconnaissance geologic map of the Lookout Mountain quadrangle, Crook and Wheeler Counties, Oregon","interactions":[],"lastModifiedDate":"2012-02-10T00:11:18","indexId":"i543","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"543","subseriesTitle":"NONE","title":"Reconnaissance geologic map of the Lookout Mountain quadrangle, Crook and Wheeler Counties, Oregon","language":"ENGLISH","doi":"10.3133/i543","usgsCitation":"Swinney, C., Waters, A.C., and Miller, C.P., 1968, Reconnaissance geologic map of the Lookout Mountain quadrangle, Crook and Wheeler Counties, Oregon: U.S. Geological Survey IMAP 543, 1 map., https://doi.org/10.3133/i543.","productDescription":"1 map.","costCenters":[],"links":[{"id":103204,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1696.htm","linkFileType":{"id":5,"text":"html"},"description":"1696"},{"id":187494,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.5,44.25 ], [ -120.5,44.5 ], [ -120.25,44.5 ], [ -120.25,44.25 ], [ -120.5,44.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db6418c5","contributors":{"authors":[{"text":"Swinney, C.M.","contributorId":24423,"corporation":false,"usgs":true,"family":"Swinney","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":275793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waters, A. C.","contributorId":13304,"corporation":false,"usgs":true,"family":"Waters","given":"A.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":275792,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, C. P.","contributorId":106855,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":275794,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":32713,"text":"pp448D - 1968 - Tertiary aquifers in the Mississippi embayment, with discussions of quality of the water","interactions":[],"lastModifiedDate":"2021-09-02T19:22:07.683203","indexId":"pp448D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"448","chapter":"D","title":"Tertiary aquifers in the Mississippi embayment, with discussions of quality of the water","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water resources of the Mississippi embayment","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp448D","usgsCitation":"Hosman, R., Long, A.T., Lambert, T., and Jeffery, H., 1968, Tertiary aquifers in the Mississippi embayment, with discussions of quality of the water: U.S. Geological Survey Professional Paper 448, Report: iii, 29 p.; 8 Plates: 54.25 × 35.50 inches or smaller, https://doi.org/10.3133/pp448D.","productDescription":"Report: iii, 29 p.; 8 Plates: 54.25 × 35.50 inches or smaller","costCenters":[],"links":[{"id":95925,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448d/plate-7.pdf","size":"5406","linkFileType":{"id":1,"text":"pdf"}},{"id":95924,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448d/plate-6.pdf","size":"4161","linkFileType":{"id":1,"text":"pdf"}},{"id":95923,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448d/plate-5.pdf","size":"4044","linkFileType":{"id":1,"text":"pdf"}},{"id":95922,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448d/plate-4.pdf","size":"4604","linkFileType":{"id":1,"text":"pdf"}},{"id":60627,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448d/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60626,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60625,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95921,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0448d/report.pdf","size":"4103","linkFileType":{"id":1,"text":"pdf"}},{"id":388457,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4447.htm"},{"id":119710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0448d/report-thumb.jpg"},{"id":95926,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448d/plate-8.pdf","size":"4252","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alabama, Arkansas, Kentucky, Louisiana, Mississippi, Missouri, Oklahoma, Tennessee, Texas","otherGeospatial":"Mississippi embayment","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.75,\n              32.00\n            ],\n            [\n              -87.00,\n              32.00\n            ],\n            [\n              -87.00,\n              37.3333\n            ],\n            [\n              -94.75,\n              37.3333\n            ],\n            [\n              -94.75,\n              32.00\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f043d","contributors":{"authors":[{"text":"Hosman, R. L.","contributorId":42978,"corporation":false,"usgs":true,"family":"Hosman","given":"R.","middleInitial":"L.","affiliations":[],"preferred":false,"id":209000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, A. T. along@usgs.gov","contributorId":20744,"corporation":false,"usgs":true,"family":"Long","given":"A.","email":"along@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":false,"id":208999,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lambert, T. W.","contributorId":74733,"corporation":false,"usgs":true,"family":"Lambert","given":"T. W.","affiliations":[],"preferred":false,"id":209002,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jeffery, H. G.","contributorId":74353,"corporation":false,"usgs":true,"family":"Jeffery","given":"H. G.","affiliations":[],"preferred":false,"id":209001,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":68107,"text":"ha274 - 1968 - Patterns of runoff in the Willamette Basin, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:25:30","indexId":"ha274","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"274","title":"Patterns of runoff in the Willamette Basin, Oregon","language":"ENGLISH","doi":"10.3133/ha274","usgsCitation":"Oster, E.A., 1968, Patterns of runoff in the Willamette Basin, Oregon: U.S. Geological Survey Hydrologic Atlas 274, 1 map., https://doi.org/10.3133/ha274.","productDescription":"1 map.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":186512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89377,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/274/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.5,43.25 ], [ -124.5,46.333333333333336 ], [ -121.5,46.333333333333336 ], [ -121.5,43.25 ], [ -124.5,43.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688a71","contributors":{"authors":[{"text":"Oster, E. A.","contributorId":24785,"corporation":false,"usgs":true,"family":"Oster","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32633,"text":"pp593E - 1968 - Late Eocene nonmarine diatoms from the Beaver Divide area, Fremont County, Wyoming","interactions":[],"lastModifiedDate":"2020-02-28T09:21:21","indexId":"pp593E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"593","chapter":"E","title":"Late Eocene nonmarine diatoms from the Beaver Divide area, Fremont County, Wyoming","docAbstract":"<p>The Beaver Divide is a high escarpment of Tertiary nonmarine strata in central Wyoming separating the Sweetwater Plateau from the relatively low-lying Wind River Basin. The Wagon Bed Formation of middle and late Eocene age and the Beaver Divide Conglomerate Member of the White River Formation-this member being of early Oligocene (Chadronian) age--are exposed near the top of the Beaver Divide in Fremont County, Wyo., about 23 miles southeast of Riverton. The upper part of the Wagon Bed Formation, dated as late Eocene (Uintan) age by Van Houten on the basis of vertebrate fossils, contains a highly silicified fresh-water limestone stratigraphically high in the section with a poorly preserved diatom assemblage. The Beaver Divide Conglomerate Member contains large blocks of similar white limestone, some of which have an assemblage of diatoms the same as that of the Wagon Bed Formation but showing excellent preservation. Both the Wagon Bed limestone and the limestone blocks from the Beaver Divide Conglomerate Member have virtually the same assemblages of nonmarine gastropods. A study of the local geology indicates that a marked erosional topography formed on the Wagon Bed strata before deposition of the Beaver Divide sediments. The Beaver Divide limestone blocks were derived from nearby exposures of the Wagon Bed Formation. The diatom assemblage under consideration was originally deposited in the Wagon Bed limestone and is, therefore, late Eocene rather than early Oligocene in age. This represents the earliest known assemblage of nonmarine diatoms from North America. </p><p>The diatom assemblage of the Wagon Bed Formation consists of 27 new species, two species known previously from the upper Miocene of France, and five species still found in living assemblages. One new genus containing two species also occurs in the deposit. The Wagon Bed diatom assemblage is strikingly distinct from later Tertiary fresh-water assemblages in that many diatom genera common to the younger deposits are totally lacking in this Eocene formation. These genera may be absent because of a highly specialized paleoecology during deposition of the Wagon Bed limestone, but the meager evidence provided by the few still-living species suggests nothing more specific than deposition in a temperate circumneutral lake. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to paleontology, 1967","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp593E","usgsCitation":"Lohman, K.E., and Andrews, G., 1968, Late Eocene nonmarine diatoms from the Beaver Divide area, Fremont County, Wyoming: U.S. Geological Survey Professional Paper 593, 38 p., https://doi.org/10.3133/pp593E.","productDescription":"38 p.","costCenters":[],"links":[{"id":119206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0593e/report-thumb.jpg"},{"id":60509,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0593e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","country":"United States","state":"Wyoming","county":"Fremont County","otherGeospatial":"Beaver Divide","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.15490722656249,\n              42.44778143462245\n            ],\n            [\n              -106.5399169921875,\n              42.44778143462245\n            ],\n            [\n              -106.5399169921875,\n              43.03677585761058\n            ],\n            [\n              -108.15490722656249,\n              43.03677585761058\n            ],\n            [\n              -108.15490722656249,\n              42.44778143462245\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8c42","contributors":{"authors":[{"text":"Lohman, K. 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,{"id":63788,"text":"gp628 - 1968 - Aeromagnetic map of the Westhampton quadrangle and part of the Woronoco quadrangle, Hampshire County, Massachusetts","interactions":[],"lastModifiedDate":"2022-09-28T19:22:01.564556","indexId":"gp628","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"628","title":"Aeromagnetic map of the Westhampton quadrangle and part of the Woronoco quadrangle, Hampshire County, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp628","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1968, Aeromagnetic map of the Westhampton quadrangle and part of the Woronoco quadrangle, Hampshire County, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 628, Report: 1 p.; 1 Plate: 20.78 × 32.79 inches, https://doi.org/10.3133/gp628.","productDescription":"Report: 1 p.; 1 Plate: 20.78 × 32.79 inches","costCenters":[],"links":[{"id":249992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0628/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407538,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5995.htm","linkFileType":{"id":5,"text":"html"}},{"id":249993,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0628/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0628/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Hampshire County","otherGeospatial":"Westhampton quadrangle, Woronocco quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.875,42.25 ], [ -72.875,42.375 ], [ -72.75,42.375 ], [ -72.75,42.25 ], [ -72.875,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68be6d","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":533257,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68109,"text":"ha321 - 1968 - Water resources of Wisconsin, Fox-Wolf River basin","interactions":[],"lastModifiedDate":"2022-12-19T21:35:52.233908","indexId":"ha321","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"321","title":"Water resources of Wisconsin, Fox-Wolf River basin","docAbstract":"<p><span>PURPOSE AND SCOPE</span></p>\n<p><span>The purposes of this report are to (1) describe the geohydrology of the basin, (2) describe and relate the surface- and ground-water systems, (3) discuss existing and possible future water problems in the basin, and (4) to suggest means of possible solutions. The scope of the study was to interpret and relate streamflow, climatic, geologic, and ground-water information. Because of its reconnaissance nature, this report should serve as background information. More specific water information for many areas of the Fox-Wolf River basin is available at the offices of the U.S. Geological Survey and the University of Wisconsin Geological and Natural History Survey in Madison. This study is part of a planned investigation of the geology and water resources of the rapidly developing Fox River valley industrial complex and municipal region extending from Green Bay to Fond du Lac. The related studies in this region cover Fond du Lac County (Newport, 1962), Outagamie County (LeRoux, 1957), Brown County (Drescher, 1953), the Green Bay area (Knowles and others, 1964; Knowles, 1964), Waupaca County (Berkstresser, 1964), Waushara County (Summers, 1965), and Winnebago County (Olcott, 1966).</span></p>\n<p>&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha321","usgsCitation":"Olcott, P.G., 1968, Water resources of Wisconsin, Fox-Wolf River basin: U.S. Geological Survey Hydrologic Atlas 321, 4 Sheets: 38.50 x 29.00 or smaller, https://doi.org/10.3133/ha321.","productDescription":"4 Sheets: 38.50 x 29.00 or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":186514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410739,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15695.htm","linkFileType":{"id":5,"text":"html"}},{"id":89382,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/321/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89381,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/321/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89380,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/321/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89379,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/321/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","otherGeospatial":"Fox River, Wolf River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.142822265625,\n              43.74728909225906\n            ],\n            [\n              -90.142822265625,\n              46.2330529447983\n            ],\n            [\n              -87.945556640625,\n              46.2330529447983\n            ],\n            [\n              -87.945556640625,\n              43.74728909225906\n            ],\n            [\n              -90.142822265625,\n              43.74728909225906\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f070f","contributors":{"authors":[{"text":"Olcott, Perry G.","contributorId":17249,"corporation":false,"usgs":true,"family":"Olcott","given":"Perry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277658,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67346,"text":"i542 - 1968 - Reconnaissance geologic map of the Post quadrangle, Crook County, Oregon","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i542","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"542","subseriesTitle":"NONE","title":"Reconnaissance geologic map of the Post quadrangle, Crook County, Oregon","language":"ENGLISH","doi":"10.3133/i542","usgsCitation":"Waters, A.C., 1968, Reconnaissance geologic map of the Post quadrangle, Crook County, Oregon: U.S. Geological Survey IMAP 542, 1 map., https://doi.org/10.3133/i542.","productDescription":"1 map.","costCenters":[],"links":[{"id":103210,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1702.htm","linkFileType":{"id":5,"text":"html"},"description":"1702"},{"id":188106,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.5,44 ], [ -120.5,44.25 ], [ -120.25,44.25 ], [ -120.25,44 ], [ -120.5,44 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641443","contributors":{"authors":[{"text":"Waters, A. C.","contributorId":13304,"corporation":false,"usgs":true,"family":"Waters","given":"A.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":276023,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68124,"text":"ha281 - 1968 - Hydrology and water resources of the Housatonic River Basin, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:13:38","indexId":"ha281","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"281","title":"Hydrology and water resources of the Housatonic River Basin, Massachusetts","language":"ENGLISH","doi":"10.3133/ha281","usgsCitation":"Norvitch, R.F., Farrell, D., Pauszek, F.H., and Petersen, R., 1968, Hydrology and water resources of the Housatonic River Basin, Massachusetts: U.S. Geological Survey Hydrologic Atlas 281, 4 col. maps ;73-95 x 86-119 cm., https://doi.org/10.3133/ha281.","productDescription":"4 col. maps ;73-95 x 86-119 cm.","costCenters":[],"links":[{"id":186192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89400,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/281/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89401,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/281/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89402,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/281/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89403,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/281/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89404,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/281/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89405,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/281/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604d26","contributors":{"authors":[{"text":"Norvitch, Ralph F.","contributorId":65456,"corporation":false,"usgs":true,"family":"Norvitch","given":"Ralph","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":277687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrell, D.F.","contributorId":91163,"corporation":false,"usgs":true,"family":"Farrell","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":277688,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pauszek, F. H.","contributorId":61399,"corporation":false,"usgs":true,"family":"Pauszek","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277686,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Petersen, R.G.","contributorId":35807,"corporation":false,"usgs":true,"family":"Petersen","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":277685,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":55877,"text":"ofr68301 - 1968 - Compilation of hydrologic data, Escondido Creek, San Antonio River basin, Texas, 1966","interactions":[],"lastModifiedDate":"2017-06-27T15:24:30","indexId":"ofr68301","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"68-301","title":"Compilation of hydrologic data, Escondido Creek, San Antonio River basin, Texas, 1966","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68301","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1968, Compilation of hydrologic data, Escondido Creek, San Antonio River basin, Texas, 1966: U.S. Geological Survey Open-File Report 68-301, 44 p., https://doi.org/10.3133/ofr68301.","productDescription":"44 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":182222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6a9f79","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":532413,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55876,"text":"ofr68299 - 1968 - Compilation of hydrologic data, Deep Creek, Colorado River basin, Texas, 1966","interactions":[],"lastModifiedDate":"2017-06-27T15:27:09","indexId":"ofr68299","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"68-299","title":"Compilation of hydrologic data, Deep Creek, Colorado River basin, Texas, 1966","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68299","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1968, Compilation of hydrologic data, Deep Creek, Colorado River basin, Texas, 1966: U.S. Geological Survey Open-File Report 68-299, 54 p., https://doi.org/10.3133/ofr68299.","productDescription":"54 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":182221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6a9f08","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":532412,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55868,"text":"ofr68248 - 1968 - An appraisal of the ground-water resources of the Upper Susquehanna River basin in Pennsylvania","interactions":[],"lastModifiedDate":"2016-10-21T10:49:18","indexId":"ofr68248","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"68-248","title":"An appraisal of the ground-water resources of the Upper Susquehanna River basin in Pennsylvania","docAbstract":"<p>This report describes the availability, quantity, quality, variability, and cost of development of the ground-water resources in the Upper Susquehanna River basin in Pennsylvania, which is the entire drainage area in Pennsylvania above the confluence of the West Branch and the main stem of the Susquehanna River at Northumberland. The report has been prepared for and under specifications established by the Corps of Engineers, U. S. Army, and is intended to serve the specific needs for ground-water information for all Federal and State agencies participating in the comprehensive study of the basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68248","usgsCitation":"Seaber, P.R., 1968, An appraisal of the ground-water resources of the Upper Susquehanna River basin in Pennsylvania: U.S. Geological Survey Open-File Report 68-248, Report: v, 75 p.; Plate: 24.63 x 17.70 inches, https://doi.org/10.3133/ofr68248.","productDescription":"Report: v, 75 p.; Plate: 24.63 x 17.70 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":184103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr68248.PNG"},{"id":330306,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0248/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330307,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0248/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Upper Susquehanna River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.7225341796875,\n              40.62646106367355\n            ],\n            [\n              -76.0308837890625,\n              40.901057866884024\n            ],\n            [\n              -75.7232666015625,\n              41.0130657870063\n            ],\n            [\n              -75.50354003906249,\n              41.31907562295139\n            ],\n            [\n              -75.443115234375,\n              41.66470503009207\n            ],\n            [\n              -75.4815673828125,\n              42.0125705565935\n            ],\n            [\n              -78.0084228515625,\n              42.004407212963585\n            ],\n            [\n              -78.4259033203125,\n              41.623655390686395\n            ],\n            [\n              -78.8214111328125,\n              41.17038447781618\n            ],\n            [\n              -78.8653564453125,\n              40.65980593837852\n            ],\n            [\n              -78.7225341796875,\n              40.62646106367355\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6856bb","contributors":{"authors":[{"text":"Seaber, Paul R.","contributorId":67492,"corporation":false,"usgs":true,"family":"Seaber","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":254394,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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