{"pageNumber":"2257","pageRowStart":"56400","pageSize":"25","recordCount":68869,"records":[{"id":70199581,"text":"70199581 - 1979 - Variation of rain chemistry during storms at two sites in northern California","interactions":[],"lastModifiedDate":"2018-09-20T21:27:18","indexId":"70199581","displayToPublicDate":"1979-06-01T21:26:55","publicationYear":"1979","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":"Variation of rain chemistry during storms at two sites in northern California","docAbstract":"

The chemical composition of rainfall at Menlo Park, on San Francisco Bay, is compared with rainfall at Petrolia, which is near the coast about 500 km north of San Francisco. Sequential samples representing 1.35 to 5.4 mm of rain were collected from November 1971 to January 1972. At rural Petrolia the Cl:Na ratio was that of seawater for Cl concentrations ranging from 0.02 to 38 mg/l. In metropolitan Menlo Park the Cl:Na ratio in rain closely approximated that in seawater above about 0.5 mg/l Cl, but at lower Cl concentrations the ratio exceeded that in seawater, a fact attributed to the presence of anthropogenic Cl. Other constituents dissolved in Menlo Park rain (along with their concentration ranges in milligrams per liter), and believed to be derived in part from anthropogenic sources, were Ca (0.01–1.07), Mg (<0.01–1.08), Pb (0.003–0.035), Zn (0.002–0.013), Mn (0.0001–0.0057), Cu (0.0008–0.0024), NO3‐N (0.02–0.54), and Br (<0.01–0.12). The range of pH values was smaller in the rural than in the metropolitan areas; average H+ activity corresponded to a pH of 5.1 to 5.2 in both areas. At Petrolia, pH decreased with increased dissolved salts in rainfall, but no relation between pH and dissolved salts was evident at Menlo Park.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR015i003p00687","usgsCitation":"Kennedy, V.C., Zellweger, G.W., and Avanzino, R.J., 1979, Variation of rain chemistry during storms at two sites in northern California: Water Resources Research, v. 15, no. 3, p. 687-702, https://doi.org/10.1029/WR015i003p00687.","productDescription":"16 p.","startPage":"687","endPage":"702","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":357596,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","volume":"15","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","contributors":{"authors":[{"text":"Kennedy, V. C.","contributorId":46080,"corporation":false,"usgs":true,"family":"Kennedy","given":"V.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":745898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zellweger, Gary W.","contributorId":71171,"corporation":false,"usgs":true,"family":"Zellweger","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":745899,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Avanzino, Ronald J.","contributorId":24355,"corporation":false,"usgs":true,"family":"Avanzino","given":"Ronald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":745900,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70129074,"text":"70129074 - 1979 - Compressional velocities from multichannel refraction arrivals on Georges Bank: northwest Atlantic Ocean","interactions":[],"lastModifiedDate":"2017-08-23T12:50:45","indexId":"70129074","displayToPublicDate":"1979-06-01T15:18:39","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Compressional velocities from multichannel refraction arrivals on Georges Bank: northwest Atlantic Ocean","docAbstract":"

Velocities were obtained from unreversed, refracted arrivals on analog records from a 48‐channel, 3.6-km hydrophone cable (3.89 km from the airgun array to the last hydrophone array). Approximately 200 records were analyzed along 1500 km of ship track on Georges Bank, northwest Atlantic Ocean, to obtain regional sediment velocity distribution to a depth of 1.4 km below sea level. This technique provides nearly continuous coverage of refraction velocities and vertical velocity gradients. Because of the length of the hydrophone cable and the vertical velocity gradients, the technique is applicable only to the Continental Shelf and the shallower parts of the Continental Slope in water depths less than 300 m. Sediment diagenesis, the influence of overburden pressure on compaction, lithology, density, and porosity are inferred from these data.

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\n

Velocities of the sediment near the water‐sediment interface range from less than 1500 m/sec on the north edge of Georges Bank to 1830 m/sec for glacial deposits in the northcentral part of the bank. Velocity gradients in the upper 400 m range from 1.0km/sec/km(sec−1) on the south edge of the bank to 1.7sec−1 on the north. Minimum gradients of 0.8sec−1 were observed south of Nantucket Island. Velocities and velocity gradients are explained in relation to physical properties of the Cretaceous, Tertiary, and Pleistocene sediments. Isovelocity contours at 100-m/sec intervals are nearly horizontal in the upper 400 m. Isovelocity contours at greater depths show a greater difference from a mean depth because of the greater structural and lithological variation. Bottom densities inferred from the velocities range from 1.7 to 1.9g/cm3 and porosities range from 48 to 62 percent. The most significant factor controlling velocity distribution on Georges Bank is overburden pressure and resulting compaction. From the velocity data we conclude that Georges Bank has been partially overridden by a continental ice sheet.

","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","doi":"10.1190/1.1440992","usgsCitation":"McGinnis, L.D., and Otis, R.M., 1979, Compressional velocities from multichannel refraction arrivals on Georges Bank: northwest Atlantic Ocean: Geophysics, v. 44, no. 6, p. 1022-1033, https://doi.org/10.1190/1.1440992.","productDescription":"12 p.","startPage":"1022","endPage":"1033","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":295432,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Atlantic Ocean, Georges Bank","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71,\n 39.5\n ],\n [\n -65,\n 39.5\n ],\n [\n -65,\n 43\n ],\n [\n -71,\n 43\n ],\n [\n -71,\n 39.5\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"44","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5440de20e4b0b0a643c732c3","contributors":{"authors":[{"text":"McGinnis, L. D.","contributorId":28915,"corporation":false,"usgs":true,"family":"McGinnis","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":503421,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Otis, R. M.","contributorId":103603,"corporation":false,"usgs":true,"family":"Otis","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":503422,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185634,"text":"70185634 - 1979 - Monitoring of subsurface injection of wastes, Florida","interactions":[],"lastModifiedDate":"2020-01-26T10:14:59","indexId":"70185634","displayToPublicDate":"1979-05-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Monitoring of subsurface injection of wastes, Florida","docAbstract":"

Injection of waste liquids into Florida's subsurface is physically feasible in many places but should be accompanied by monitoring of the waste-receiving aquifer system in addition to the injection facility. Monitoring of the interaction of factors including hydrogeologic conditions, well construction, waste volumes and characteristics, and potable-water sources is desirable to assure that fresh-water resources are not being adversely affected. An effective aquifer-system monitoring program includes on-site wells located close to an injection well and open to the next-higher permeable stratum, satellite wells located hundreds to several thousands of feet from an injection well and open to the receiving aquifer, and regional wells located miles from individual injection wells and open to the receiving aquifer. An extensive aquifer-system monitoring program associated with two waste-injection facilities near Pensacola, Florida, has provided data which have aided hydrologists to understand the aquifer system's response to the injection and, accordingly, to evaluate the potential for affecting the area's fresh-water resources.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1979.tb03318.x","usgsCitation":"Vecchioli, J., 1979, Monitoring of subsurface injection of wastes, Florida: Groundwater, v. 17, no. 3, p. 244-249, https://doi.org/10.1111/j.1745-6584.1979.tb03318.x.","productDescription":"6 p. ","startPage":"244","endPage":"249","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338335,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.3193359375,\n 31.12819929911196\n ],\n [\n -87.4951171875,\n 30.29701788337205\n ],\n [\n -86.17675781249999,\n 30.259067203213018\n ],\n [\n -85.20996093749999,\n 29.76437737516313\n ],\n [\n -83.9794921875,\n 30.06909396443887\n ],\n [\n -82.9248046875,\n 28.69058765425071\n ],\n [\n -82.880859375,\n 27.566721430409707\n ],\n [\n -81.1669921875,\n 25.20494115356912\n ],\n [\n -80.5517578125,\n 25.085598897064752\n ],\n [\n -79.98046875,\n 26.745610382199022\n ],\n [\n -81.4306640625,\n 30.826780904779774\n ],\n [\n -87.3193359375,\n 31.12819929911196\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"17","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","scienceBaseUri":"58d63042e4b05ec79913112f","contributors":{"authors":[{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":686170,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70209766,"text":"70209766 - 1979 - Spectra of altered rocks in the visible and near infrared","interactions":[],"lastModifiedDate":"2020-04-24T17:34:41.724524","indexId":"70209766","displayToPublicDate":"1979-04-24T12:28:49","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Spectra of altered rocks in the visible and near infrared","docAbstract":"

Visible and near-infrared (0.35 to 2.5 mu m) bidirectional reflection spectra were recorded for a suite of well-characterized hydrothermally altered rock samples. The spectra typically display well-defined bands caused by both electronic and vibrational processes in the individual mineral constituents.Electronic transitions in the iron-bearing constituent minerals produce diagnostic minima near 0.43, 0.65, 0.85, and 0.93 mu m. Vibrational transitions in clay and water-bearing mineral constituents typically produce characteristic single or multiple features over limited spectral ranges near 1.4, 1.75, 1.9, 2.2, and 2.35 mu m. The most abundant feature-producing minerals present in these rocks are hematite, goethite, and alunite, while others frequently present are jarosite, kaolinite, potassium micas, pyrophyllite, montmorillonite, diaspore, and gypsum.This study shows that visible-near infrared spectrometry is a reliable and rapid technique for detecting and identifying clay minerals and alunite in rocks. Because these minerals are important constituents of altered rocks, the feasibility of using the visible and near infrared for detecting altered rocks by remote-sensing techniques is indicated. The spectral region near 2.2 mu m is particularly important for this purpose.

","language":"English","publisher":"GeoScienceWorld","doi":"10.2113/gsecongeo.74.7.1613","usgsCitation":"Hunt, G., and Ashley, R.P., 1979, Spectra of altered rocks in the visible and near infrared: Economic Geology, v. 74, no. 7, p. 1613-1629, https://doi.org/10.2113/gsecongeo.74.7.1613.","productDescription":"17 p.","startPage":"1613","endPage":"1629","costCenters":[],"links":[{"id":374265,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Goldfield","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.43286132812499,\n 38.112949789189614\n ],\n [\n -116.62536621093749,\n 38.112949789189614\n ],\n [\n -116.62536621093749,\n 38.805470223177466\n ],\n [\n -117.43286132812499,\n 38.805470223177466\n ],\n [\n -117.43286132812499,\n 38.112949789189614\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"7","noUsgsAuthors":false,"publicationDate":"1979-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hunt, G.R.","contributorId":7415,"corporation":false,"usgs":true,"family":"Hunt","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":787924,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ashley, Roger P. ashley@usgs.gov","contributorId":2749,"corporation":false,"usgs":true,"family":"Ashley","given":"Roger","email":"ashley@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":787925,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70120091,"text":"70120091 - 1979 - Habitat evaluation","interactions":[],"lastModifiedDate":"2014-08-12T10:30:24","indexId":"70120091","displayToPublicDate":"1979-04-01T10:27:54","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3725,"text":"Water Spectrum","active":true,"publicationSubtype":{"id":10}},"title":"Habitat evaluation","docAbstract":"

Ours has been a nation of rapid growth and development; our abundant water and other natural resources were quickly utilized to meet the needs of our expansion. Resources perceived to be “important” to the national interest were often exploited at the expense of others. Fish and wildlife, because of their apparent abundance and low priority status, were among those resources that historically received little attention or protection and were frequently \"traded off\" to other resource developments.

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\n

Ours has been a nation of rapid growth and development; our abundant water and other natural resources were quickly utilized to meet the needs of our expansion. Resources perceived to be “important” to the national interest were often exploited at the expense of others. Fish and wildlife, because of their apparent abundance and low priority status, were among those resources that historically received little attention or protection and were frequently \"traded off\" to other resource developments.

","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Spectrum","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"United States Army Corps of Engineers","publisherLocation":"Washington, D.C.","usgsCitation":"United States Army Corps of Engineers, 1979, Habitat evaluation: Water Spectrum, v. 11, no. 2, p. 26-34.","productDescription":"9 p.","startPage":"26","endPage":"34","numberOfPages":"9","costCenters":[],"links":[{"id":292005,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53eb2a78e4b0461e44764a39"} ,{"id":70120085,"text":"70120085 - 1979 - The composite dynamic method as evidence for age-specific waterfowl mortality","interactions":[],"lastModifiedDate":"2014-08-12T10:07:15","indexId":"70120085","displayToPublicDate":"1979-04-01T09:59:04","publicationYear":"1979","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":"The composite dynamic method as evidence for age-specific waterfowl mortality","docAbstract":"For the past 25 years estimation of mortality rates for waterfowl has been based almost entirely on the composite dynamic life table. We examined the specific assumptions for this method and derived a valid goodness of fit test. We performed this test on 45 data sets representing a cross section of banded sampled for various waterfowl species, geographic areas, banding periods, and age/sex classes. We found that: (1) the composite dynamic method was rejected (P <0.001) in 37 of the 45 data sets (in fact, 29 were rejected at P <0.00001) and (2) recovery and harvest rates are year-specific (a critical violation of the necessary assumptions). We conclude that the restrictive assumptions required for the composite dynamic method to produce valid estimates of mortality rates are not met in waterfowl data. Also we demonstrate that even when the required assumptions are met, the method produces very biased estimates of age-specific mortality rates. We believe the composite dynamic method should not be used in the analysis of waterfowl banding data. Furthermore, the composite dynamic method does not provide valid evidence for age-specific mortality rates in waterfowl.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wildlife Society","publisherLocation":"Washington, D.C.","doi":"10.2307/3800344","usgsCitation":"Burnham, K.P., and Anderson, D.R., 1979, The composite dynamic method as evidence for age-specific waterfowl mortality: Journal of Wildlife Management, v. 43, no. 2, p. 356-366, https://doi.org/10.2307/3800344.","productDescription":"11 p.","startPage":"356","endPage":"366","numberOfPages":"11","costCenters":[],"links":[{"id":291998,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291997,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2307/3800344"}],"volume":"43","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53eb2a90e4b0461e44764ad3","contributors":{"authors":[{"text":"Burnham, Kenneth P.","contributorId":95025,"corporation":false,"usgs":true,"family":"Burnham","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[{"id":189,"text":"Colorado Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":497888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, David R.","contributorId":92722,"corporation":false,"usgs":true,"family":"Anderson","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":497887,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001466,"text":"1001466 - 1979 - Use of prairie pothole habitat by breeding mallards","interactions":[],"lastModifiedDate":"2025-02-14T18:01:45.164294","indexId":"1001466","displayToPublicDate":"1979-04-01T00:00:00","publicationYear":"1979","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":"Use of prairie pothole habitat by breeding mallards","docAbstract":"

Detailed information on the use by mallards (Anas platyrhynchos) of prairie pothole habitat during the nesting season is necessary to interpret habitat needs of the species during the breeding period. Many data have been collected and published relating pair counts to habitat use and water conditions (e.g., Evans and Black 1956; Smith 1971; Stoudt 1971; Stewart and Kantrud 1973, 1974). However, use of pair-count data to assess wetland use tends to emphasize individual wetland units and does not consider total wetland habitat required to sustain a breeding pair on a daily or seasonal basis. We therefore attempted to determine habitat use by individually radio marked mallards during the breeding period. This paper describes home range characteristics and habitat use of a radiomarked sample of mallard hens breeding in North Dakota during 1973-75. Time budget data are also presented for 2 marked pairs of mallard pairs of mallards.

","largerWorkTitle":"Wiley","language":"English","doi":"10.2307/3800366","usgsCitation":"Dwyer, T., Krapu, G., and Janke, D., 1979, Use of prairie pothole habitat by breeding mallards: Journal of Wildlife Management, v. 43, no. 2, p. 526-531, https://doi.org/10.2307/3800366.","productDescription":"6 p.","startPage":"526","endPage":"531","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":129388,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North 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Dakota\",\"nation\":\"USA \"}}]}","volume":"43","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604444","contributors":{"authors":[{"text":"Dwyer, T.J.","contributorId":56177,"corporation":false,"usgs":true,"family":"Dwyer","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":311079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krapu, Gary L.","contributorId":56994,"corporation":false,"usgs":true,"family":"Krapu","given":"Gary L.","affiliations":[],"preferred":false,"id":311080,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Janke, D.M.","contributorId":74709,"corporation":false,"usgs":true,"family":"Janke","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":311081,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70231538,"text":"70231538 - 1979 - Determination of sulfate in seawater and natural brines by 133Ba and membrane dialysis","interactions":[],"lastModifiedDate":"2022-05-12T15:21:24.613087","indexId":"70231538","displayToPublicDate":"1979-03-01T10:17:33","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Determination of sulfate in seawater and natural brines by 133Ba and membrane dialysis","title":"Determination of sulfate in seawater and natural brines by 133Ba and membrane dialysis","docAbstract":"

Dissolved sulfate is determined by precipitation with the radioisotope 133Ba and counting of the precipitate on a scintillation counter. Precipitation is carried out in dialysis bags; excess 133 Ba is removed via diffusion by soaking the bags in distilled water for 12 h, and the bags are then placed directly in the well of the scintillation counter. The procedure eliminates previous errors caused by washing and transferring of the precipitate and permits analysis of 0.5–3,000 µg·ml−1 sulfate in a 1.0-ml sample. The detection limit is increased by simply increasing the sample volume up to 5.0 ml. The technique is interference-free in natural waters ranging from freshwater to brines of 1.5 times the salinity of seawater.

","language":"English","publisher":"Association for the Sciences of Limnology and Oceanography","doi":"10.4319/lo.1979.24.2.0393","usgsCitation":"Seyfried, W.E., Rosenbauer, R.J., and Bischoff, J.L., 1979, Determination of sulfate in seawater and natural brines by 133Ba and membrane dialysis: Limnology and Oceanography, v. 24, no. 2, p. 393-396, https://doi.org/10.4319/lo.1979.24.2.0393.","productDescription":"4 p.","startPage":"393","endPage":"396","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":480604,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lo.1979.24.2.0393","text":"Publisher Index Page"},{"id":400581,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"2","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","contributors":{"authors":[{"text":"Seyfried, William E.","contributorId":291754,"corporation":false,"usgs":false,"family":"Seyfried","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":842960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenbauer, Robert J. brosenbauer@usgs.gov","contributorId":204,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"Robert","email":"brosenbauer@usgs.gov","middleInitial":"J.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":842961,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":842962,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70208415,"text":"70208415 - 1979 - Modern biogenic gas-generated craters (sea-floor “pockmarks”) on the Bering Shelf, Alaska","interactions":[],"lastModifiedDate":"2021-05-27T14:47:43.002387","indexId":"70208415","displayToPublicDate":"1979-02-07T13:57:15","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Modern biogenic gas-generated craters (sea-floor “pockmarks”) on the Bering Shelf, Alaska","docAbstract":"

As many as 1,340 small craters per square kilometre cover the sea floor of Norton Sound in the northeastern Bering Sea. The craters are circular pits, 1 to 10 m in diameter and less than 1 m deep, observed on sonographs over 20,000 km2 of northern Norton Sound sea floor. Craters typically are associated with acoustic anomalies, near-surface peaty mud, and gas-charged sediment.

The peaty mud is a thick (>1.5 m), nonmarine pre-Holocene deposit that is now covered by a 1- to 3-m-thick layer of Holocene marine mud in the area of the craters. The peaty mud (2% to 8% organic carbon) contains abundant biogenic methane [C1/(C2 + C3) = 256 to 7,669] with carbon isotope (δ13C) values of −69‰ to −75‰- Decomposition of organic debris in the peaty mud apparently charges the mud with gas. The peaty and gassy zones attenuate sound waves and cause acoustic anomalies on high-resolution seismic profiles in the area with craters.

The craters are forming now, as shown by the disruption of modern ice gouges by the craters. In the absence of storms, the gas apparently is trapped in the peaty mud in a saturated state by the cover of Holocene mud. Periodically, possibly during storms, the gas escapes through the thin Holocene cover and forms craters.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1979)90<1144:MBGCSP>2.0.CO;2","usgsCitation":"Hans, N.C., Thor, D., Sandstrom, M.W., and Kvenvolden, K.A., 1979, Modern biogenic gas-generated craters (sea-floor “pockmarks”) on the Bering Shelf, Alaska: GSA Bulletin, v. 90, no. 12, p. 1144-1152, https://doi.org/10.1130/0016-7606(1979)90<1144:MBGCSP>2.0.CO;2.","productDescription":"9 p.","startPage":"1144","endPage":"1152","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":372149,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Shelf","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -171.73828125,\n 62.75472592723178\n ],\n [\n -160.0048828125,\n 62.75472592723178\n ],\n [\n -160.0048828125,\n 65.93751437423593\n ],\n [\n -171.73828125,\n 65.93751437423593\n ],\n [\n -171.73828125,\n 62.75472592723178\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"90","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hans, Nelson C.","contributorId":26072,"corporation":false,"usgs":true,"family":"Hans","given":"Nelson","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":781782,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thor, D.R.","contributorId":79521,"corporation":false,"usgs":true,"family":"Thor","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":781783,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sandstrom, Mark W. 0000-0003-0006-5675 sandstro@usgs.gov","orcid":"https://orcid.org/0000-0003-0006-5675","contributorId":706,"corporation":false,"usgs":true,"family":"Sandstrom","given":"Mark","email":"sandstro@usgs.gov","middleInitial":"W.","affiliations":[{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"preferred":true,"id":781784,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kvenvolden, Keith A. kkvenvolden@usgs.gov","contributorId":3384,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"Keith","email":"kkvenvolden@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":781785,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70129075,"text":"70129075 - 1979 - Reply to discussion by Michael A. Collins, \"Fresh ground water stored in aquifers under the continental shelf: implications from a deep test, Nantucket Island, Massachusetts\"","interactions":[],"lastModifiedDate":"2018-02-02T10:59:29","indexId":"70129075","displayToPublicDate":"1979-02-01T15:29:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"Reply to discussion by Michael A. Collins, \"Fresh ground water stored in aquifers under the continental shelf: implications from a deep test, Nantucket Island, Massachusetts\"","docAbstract":"
We appreciate the comments made in the discussion by Michael A. Collins, regarding our paper about the anomalously low salinity of water underlying Nantucket Island. However, we feel that in his effort to justify the mathematical approach for solving salt water intrusion problems, he has overlooked several of the major points in this paper. We will try to amplify these points to establish that, indeed, the situation at Nantucket is anomalous, contrary to Collins’ negative conclusion (Collins, 1978).
","language":"English","publisher":"American Water Resources Association","doi":"10.1111/j.1752-1688.1979.tb00307.x","usgsCitation":"Kohout, F.A., and Delaney, D., 1979, Reply to discussion by Michael A. Collins, \"Fresh ground water stored in aquifers under the continental shelf: implications from a deep test, Nantucket Island, Massachusetts\": Water Resources Bulletin, v. 15, no. 1, p. 252-254, https://doi.org/10.1111/j.1752-1688.1979.tb00307.x.","productDescription":"3 p.","startPage":"252","endPage":"254","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":295434,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Nantucket Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.33172607421875,\n 41.20345619205131\n ],\n [\n -69.9169921875,\n 41.20345619205131\n ],\n [\n -69.9169921875,\n 41.425223482352656\n ],\n [\n -70.33172607421875,\n 41.425223482352656\n ],\n [\n -70.33172607421875,\n 41.20345619205131\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"15","issue":"1","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"5440de40e4b0b0a643c73309","contributors":{"authors":[{"text":"Kohout, F. A.","contributorId":11593,"corporation":false,"usgs":true,"family":"Kohout","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":503424,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Delaney, D.F.","contributorId":102128,"corporation":false,"usgs":true,"family":"Delaney","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":503423,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70231373,"text":"ofr791498 - 1979 - Regional geohydrology of the San Juan hydrologic basin of New Mexico, Colorado, Arizona, and Utah","interactions":[],"lastModifiedDate":"2022-05-10T14:03:36.437327","indexId":"ofr791498","displayToPublicDate":"1979-02-01T10:02:50","publicationYear":"1979","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":"79-1498","title":"Regional geohydrology of the San Juan hydrologic basin of New Mexico, Colorado, Arizona, and Utah","docAbstract":"

The San Juan Basin in the southeastern part of the Colorado Plateau, southwest of the San Juan Mountains, broadly includes the Acoma and Gallup Sags in its southern part and the small Chama Basin in its northeastern part. Regionally, the water-yielding strata (aquifers) dip inward toward the center of San Juan Basin or toward the axes of the adjoining structural sags. Aquifers exposed or at shallow depths along the margin of the basin are deeply buried in the center of the basin.

The occurrence and movement of ground water is strongly influenced by the structural configuration of the basin; fractures along joints and faults, particularly the Puerco fault belt; distribution and lithology of the rock strata, and the relationship of the uplands recharge areas of the aquifers to the lowland areas where the most ground-water discharges.

The aggregate thickness of sedimentary rocks is more than 10,000 feet in the deepest part of the basin. In order of decreasing abundance, these rocks consist of mudstone, claystone, siltstone, sandstone, silty sandstone, coal, limestone, conglomerate, and gypsum. The main aquifers consist of sandstone or sandstone containing lenses of conglomerate except for the San Andres Limestone.

The principal aquifers, listed in descending stratigraphic order, are the Tertiary Cuba Mesa and Llaves Members of the San Jose Formation and the Ojo Alamo Sandstone; the Pictured Cliffs, Cliff House, Point Lookout, Gallup, and Dakota Sandstones; the Westwater Canyon and Salt Wash Sandstone Members of the Morrison Formation, the Cow Springs Sandstone, the Zuni Sandstone, and the Entrada Sandstone; and the San Andres Limestone, Glorieta Sandstone, and De Chelly Sandstone. These aquifer are separated by formations, that do not readily transmit water between the aquifers.

Regional movement of ground water is mainly to the San Juan and Chaco s Rivers, the Puerco River, the Rio Puerco, and their main tributaries. Ground water from aquifers overlying the Dakota Sandstone discharge within the confines of the San Juan hydrologic basin. Part of the ground water in the Dakota Sandstone, Morrison Formation, and underlying formations moves across the interbasin divide into the Black Mesa, the Blanding Basin, or to the Rio Grande Trough.

","language":"English","publisher":"U.S. Department of Interior","doi":"10.3133/ofr791498","collaboration":"San Juan Basin Regional Uranium Study Working Paper No. 11C","usgsCitation":"Cooley, M.E., and Weist, W., 1979, Regional geohydrology of the San Juan hydrologic basin of New Mexico, Colorado, Arizona, and Utah: U.S. Geological Survey Open-File Report 79-1498, vii, 39 p., https://doi.org/10.3133/ofr791498.","productDescription":"vii, 39 p.","numberOfPages":"78","costCenters":[],"links":[{"id":400384,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1498/report-thumb.jpg"},{"id":400383,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1498/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona, Colorado, New Mexico, Utah","otherGeospatial":"San Juan hydrologic basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110,\n 34.5\n ],\n [\n -106,\n 34.5\n ],\n [\n -106,\n 38\n ],\n [\n -110,\n 38\n ],\n [\n -110,\n 34.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cooley, Maurice E.","contributorId":8077,"corporation":false,"usgs":true,"family":"Cooley","given":"Maurice","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":842539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weist, William G.","contributorId":21526,"corporation":false,"usgs":true,"family":"Weist","given":"William G.","affiliations":[],"preferred":false,"id":842540,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70206953,"text":"70206953 - 1979 - Genesis of ore deposits in the San Juan Volcanic Field, Southwestern Colorado-lead isotope evidence","interactions":[],"lastModifiedDate":"2020-07-15T00:06:21.948413","indexId":"70206953","displayToPublicDate":"1979-01-02T16:48:18","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Genesis of ore deposits in the San Juan Volcanic Field, Southwestern Colorado-lead isotope evidence","docAbstract":"

In the San Juan volcanic area of southwestern Colorado, the isotopic composition of lead in ores and ore prospects of Cenozoic age ranges widely: 17.72 to 21.13 for 206Pb/ 204Pb; 15.50 to 15.81 for 207Pb/ 204Pb; and 37.21 to 38 for 208Pb/ 204Pb. Examination of the lead isotope data indicates that once deposition of lead minerals begins, further exchange of lead between fluid and wall rock is insignificant. This conclusion is supported by the relatively constant isotopic composition of the lead in these ores, which is not affected by the grade of ore mineralization or type of wall rock. The values of 206Pb/ 204Pb in some vein-type deposits exceed the maximum value known for all Mesozoic and Cenozoic igneous rocks of the Rocky Mountain region. These isotopic relations show that if ore-forming solutions are composed of meteoric water, as indicated in studies of light stable isotopes, they must have penetrated deep enough to acquire lead from Pre-cambrian rocks or sediments derived from them. The fact that some of these vein ores are now in Cenozoic igneous rocks indicates the ore fluid had an upward vertical component to its movement. The lead isotope data therefore support a circulating cell hypothesis for these kinds of ores, as suggested by many recent studies of light stable isotopes as related to mineralization. Some other deposits (Summitville, Jasper, Red Mountain district) have values of 206Pb/ 204Pb similar to those of the large volumes of altered rock that enclose them ( 206Pb/ 204Pb ∼ 18.5), suggesting that in places the lead may have been locally derived by leaching of the adjacent rocks or from magmatogenic fluids. When the lead isotope data are treated in detail, the rocks and galenas of the Platoro caldera complex, of the central San Juan caklera complex, and of the Baughman Creek center appear to contain significant components derived from 1,400- to l,500-m.y.-old and 1,700- to 1,800 m.y.-old source materials. These also are the ages of the two main groups of rocks that comprise the Precambrian basement under the San Juan volcanic area. Although the data from the western San Juan caldera complex scatter considerably, the only obvious source for the lead seems to be the 1,700- to l,800-m.y.-old rocks or detritus of such age in Phanerozoic sediments. Where the involvement of 1,400- to l,500-m.y.-old sources is greatest, the Th/U ratio in the source material is small (calculated to be about 0.7), whereas the Th/U ratio of the 1,700- to l,800-m.y.-old source material appears to be 2.3 to 3.3. The largest Th/U values are from the western San Juan caldera complex. © 1979 Society of Economic Geologists, Inc.

","language":"English","publisher":"Society of Economic Geology","doi":"10.2113/gsecongeo.74.1.1","usgsCitation":"Doe, B.R., Steven, T.A., Delevaux, M., Stacey, J.S., Lipman, P.W., and Fisher, F.S., 1979, Genesis of ore deposits in the San Juan Volcanic Field, Southwestern Colorado-lead isotope evidence: Economic Geology, v. 74, no. 1, p. 1-26, https://doi.org/10.2113/gsecongeo.74.1.1.","productDescription":"26 p.","startPage":"1","endPage":"26","costCenters":[],"links":[{"id":369779,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"San Juan volcanic field","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.7481689453125,\n 37.046408899699564\n ],\n [\n -105.31494140625,\n 37.046408899699564\n ],\n [\n -105.31494140625,\n 38.47939467327645\n ],\n [\n -108.7481689453125,\n 38.47939467327645\n ],\n [\n -108.7481689453125,\n 37.046408899699564\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"1","noUsgsAuthors":false,"publicationDate":"1979-02-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Doe, B. R.","contributorId":52173,"corporation":false,"usgs":true,"family":"Doe","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":776363,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steven, T. A.","contributorId":42575,"corporation":false,"usgs":true,"family":"Steven","given":"T.","middleInitial":"A.","affiliations":[],"preferred":false,"id":776364,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Delevaux, M.H.","contributorId":27853,"corporation":false,"usgs":true,"family":"Delevaux","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":776365,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stacey, J. S.","contributorId":72785,"corporation":false,"usgs":true,"family":"Stacey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":776366,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lipman, P. W.","contributorId":93470,"corporation":false,"usgs":true,"family":"Lipman","given":"P.","middleInitial":"W.","affiliations":[],"preferred":false,"id":776367,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fisher, F. S.","contributorId":34146,"corporation":false,"usgs":true,"family":"Fisher","given":"F.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":776368,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":10362,"text":"ofr791543 - 1979 - Hydrologic and geologic data from the Upper East Coast Planning Area, southeast Florida","interactions":[],"lastModifiedDate":"2022-01-05T15:17:36.702962","indexId":"ofr791543","displayToPublicDate":"1979-01-01T22:05:00","publicationYear":"1979","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":"79-1543","title":"Hydrologic and geologic data from the Upper East Coast Planning Area, southeast Florida","docAbstract":"The Upper East Coast Planning Area, one of five designated planning areas in the South Florida Water Management District, consists of St. Lucie, Martin, and eastern Okeechobee Counties. Existing hydrologic and geologic data have been compiled as a base for additional investigations to determine the water-bearing characteristics of the shallow aquifer system in the area. These data include lithologic logs from 51 wells in excess of 90 feet in depth, periodic ground-water levels from 100 wells, and ground-water levels from 100 wells, and ground-water quality data from 93 wells. (Kosco-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr791543","collaboration":"Prepared in cooperation with the South Florida Water Management District","usgsCitation":"Miller, W.L., 1979, Hydrologic and geologic data from the Upper East Coast Planning Area, southeast Florida: U.S. Geological Survey Open-File Report 79-1543, iii, 99 p., https://doi.org/10.3133/ofr791543.","productDescription":"iii, 99 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":968,"rank":99,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1543/ofr791543.pdf","text":"Report","size":"1.87 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":143398,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1543/coverthb.jpg"}],"country":"United States","state":"Florida","county":"Martin County, Okeechobee County, St. Lucie County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.77766418457031,\n 27.563069215397533\n ],\n [\n -80.84564208984375,\n 27.56367792633874\n ],\n [\n -80.85525512695312,\n 27.15936422843682\n ],\n [\n -80.84220886230469,\n 27.15019980940818\n ],\n [\n -80.82984924316406,\n 27.178301644674047\n ],\n [\n -80.82984924316406,\n 27.1923499094294\n ],\n [\n -80.79345703125,\n 27.20212157179689\n ],\n [\n -80.73989868164062,\n 27.174025734723248\n ],\n [\n -80.70556640625,\n 27.142867732886465\n ],\n [\n -80.68702697753906,\n 27.12147976230783\n ],\n [\n -80.68016052246092,\n 27.101921467004363\n ],\n [\n -80.66642761230469,\n 27.086639170923554\n ],\n [\n -80.63690185546875,\n 27.024877476307523\n ],\n [\n -80.61836242675781,\n 26.974709325134718\n ],\n [\n -80.61355590820312,\n 26.952065151373972\n ],\n [\n -80.06767272949219,\n 26.95022893777318\n ],\n [\n -80.08827209472656,\n 27.011419925555597\n ],\n [\n -80.10818481445312,\n 27.06279462605336\n ],\n [\n -80.13771057128906,\n 27.12147976230783\n ],\n [\n -80.1507568359375,\n 27.158142349342786\n ],\n [\n -80.15419006347656,\n 27.18502060071115\n ],\n [\n -80.16860961914062,\n 27.21311366818236\n ],\n [\n -80.1947021484375,\n 27.259512784361693\n ],\n [\n -80.27091979980469,\n 27.42846138179594\n ],\n [\n -80.28739929199219,\n 27.47598882050083\n ],\n [\n -80.3155517578125,\n 27.561851783388512\n ],\n [\n -80.77766418457031,\n 27.563069215397533\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"

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","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611832","contributors":{"authors":[{"text":"Miller, Wesley L.","contributorId":91859,"corporation":false,"usgs":true,"family":"Miller","given":"Wesley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161257,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7847,"text":"ofr791258 - 1979 - Hydrologic conditions in Broward County, Florida, 1976","interactions":[],"lastModifiedDate":"2022-05-10T18:45:36.869462","indexId":"ofr791258","displayToPublicDate":"1979-01-01T22:05:00","publicationYear":"1979","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":"79-1258","title":"Hydrologic conditions in Broward County, Florida, 1976","docAbstract":"During the 1976 water year, rainfall was 3.6 percent below average in Broward County, Fla. Water levels in the Pompano Beach and Dixie well fields were lower during the peak of the 1976 dry season than the peak of the record low dry season in 1971. Flow in the major canals was variable during the 1976 water year compared to 1962-75 averages. Flows in Cypress Creek, Middle River, and Snake Creek at S-29 were higher than the average. Flows in Plantation Canal and South New River were equal to the 1962-75 averages, while Hillsboro, North New River, and Snake Creek at N.W. 67th Avenue were below the long-term averages. The concentrations of principal mineral constituents in surface water in Broward County were within limits established by Florida State Water Standards, with the exception of iron at one station. Total coliforms were equal to or within permissible limits for class III water and waters for public supply in Broward canals at all sites during the 1976 water year. Fecal coliform did not exceed the permissible limit for public water supply at any of the sites during the 1976 water year. (Kosco-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr791258","usgsCitation":"Beaven, T., 1979, Hydrologic conditions in Broward County, Florida, 1976: U.S. Geological Survey Open-File Report 79-1258, viii, 93 p., https://doi.org/10.3133/ofr791258.","productDescription":"viii, 93 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":955,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1258/ofr791258.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":400448,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75067.htm"},{"id":141285,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1258/coverthb.jpg"}],"country":"United States","state":"Florida","county":"Broward 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","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db6115b5","contributors":{"authors":[{"text":"Beaven, T.R.","contributorId":84757,"corporation":false,"usgs":true,"family":"Beaven","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":156725,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70199344,"text":"70199344 - 1979 - Lakes of Oregon, Volume 6: Douglas County","interactions":[],"lastModifiedDate":"2018-09-21T14:58:50","indexId":"70199344","displayToPublicDate":"1979-01-01T15:58:37","publicationYear":"1979","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":"Lakes of Oregon, Volume 6: Douglas County","docAbstract":"

An inventory of lakes and reservoirs in Oregon is useful in evaluating the surface-water supply of the State and in providing answers to questions about Oregon's lakes. Much of the information on lakes and reservoirs previously collected by Federal and State agencies has never been published. Those data were compiled and used as a basis for collecting additional information. This report provides information for use by city, county, and State planning groups in planning interpretative studies. The information also will be useful to sportsmen, tourists, and others interested in preserving the recreational value of Oregon's lakes.

Because of the large number of lakes and reservoirs in Oregon, a single report covering the State would be bulky. Therefore, lake information is being issued in several volumes on a county or multicounty basis. Volume 1, released in 1973 covered Clatsop, Columbia, and Tillamook Counties; volume 2 (1974) included Benton, Lincoln, and Polk Counties; volume 3 (1975) included Hood River, Multnomah, Washington, and Yamhill Counties; volume 4 (1976) included Clackamas County; and volume 5 (1977) included Marion County. Douglas County was selected for volume 6. (See figure 1.)

In addition to office compilation of existing data, each lake was visited. Most visits were made in summer or early fall when lakes were most accessible and when water temperature and biological activity were near maximum.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70199344","collaboration":"Prepared in cooperation with the Douglas County Water Resources Survey and Oregon Water Resources Department","usgsCitation":"Rinella, J.F., 1979, Lakes of Oregon, Volume 6: Douglas County: Open-File Report, iii, 123 p., https://doi.org/10.3133/70199344.","productDescription":"iii, 123 p.","costCenters":[],"links":[{"id":357639,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70199344/report-thumb.jpg"},{"id":357640,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70199344/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Douglas County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.2,\n 42.75\n ],\n [\n -122,\n 42.75\n ],\n [\n -122,\n 44\n ],\n [\n -124.2,\n 44\n ],\n [\n -124.2,\n 42.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Rinella, Joseph F. jrinella@usgs.gov","contributorId":1371,"corporation":false,"usgs":true,"family":"Rinella","given":"Joseph","email":"jrinella@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":746034,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70120124,"text":"70120124 - 1979 - The use of habitat structure preferenda for establishing flow regimes necessary for maintenance of fish habitat","interactions":[],"lastModifiedDate":"2014-08-12T13:30:21","indexId":"70120124","displayToPublicDate":"1979-01-01T13:28:32","publicationYear":"1979","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The use of habitat structure preferenda for establishing flow regimes necessary for maintenance of fish habitat","docAbstract":"The pursuit of simplicity in the complex management of instream and out-of-stream water uses very early led to the minimum, or “base,” flow concept and the myth that a consistent methodology could be used to establish the desired minimum flow. Such a single flow value has not proven to be practical. As water becomes fully appropriated to upstream use and storage, the minimum flow, if not violated, tends to become the average condition. This situation is manifest in a flat or stepped but fixed hydrograph throughout the stream reach of concern for much of the year.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Ecology of Regulated Streams","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Plenum Press","publisherLocation":"New York, NY","doi":"10.1007/978-1-4684-8613-1_19","usgsCitation":"Stalnaker, C., 1979, The use of habitat structure preferenda for establishing flow regimes necessary for maintenance of fish habitat, chap. of The Ecology of Regulated Streams, p. 321-337, https://doi.org/10.1007/978-1-4684-8613-1_19.","productDescription":"17 p.","startPage":"321","endPage":"337","numberOfPages":"17","costCenters":[],"links":[{"id":292032,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292031,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/978-1-4684-8613-1_19"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53eb2a90e4b0461e44764ade","contributors":{"authors":[{"text":"Stalnaker, Clair B.","contributorId":30871,"corporation":false,"usgs":true,"family":"Stalnaker","given":"Clair B.","affiliations":[],"preferred":false,"id":497935,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25142,"text":"25142 - 1979 - CEL, index to current earthquake literature","interactions":[],"lastModifiedDate":"2014-07-14T13:23:21","indexId":"25142","displayToPublicDate":"1979-01-01T13:22:08","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"CEL, index to current earthquake literature","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/25142","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, CEL, index to current earthquake literature, https://doi.org/10.3133/25142.","costCenters":[],"links":[{"id":289920,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c4fbf4e4b0b58d96eeb554","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":529182,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70120106,"text":"70120106 - 1979 - Development of techniques and procedures for monitoring the effectiveness of fish and wildlife measures associated with U.S. Army Corps of Engineers water resource development projects","interactions":[],"lastModifiedDate":"2014-08-12T11:34:18","indexId":"70120106","displayToPublicDate":"1979-01-01T11:31:35","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Development of techniques and procedures for monitoring the effectiveness of fish and wildlife measures associated with U.S. Army Corps of Engineers water resource development projects","docAbstract":"No abstract available.","language":"English","publisher":"Enviro Control","publisherLocation":"Rockville, MD","usgsCitation":"Horak, G.C., and Olson, J.E., 1979, Development of techniques and procedures for monitoring the effectiveness of fish and wildlife measures associated with U.S. Army Corps of Engineers water resource development projects.","costCenters":[],"links":[{"id":292016,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53eb2a63e4b0461e447649e3","contributors":{"authors":[{"text":"Horak, Gerry C.","contributorId":88656,"corporation":false,"usgs":true,"family":"Horak","given":"Gerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":497916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, J. E.","contributorId":24800,"corporation":false,"usgs":true,"family":"Olson","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":497915,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001664,"text":"1001664 - 1979 - Fall foods of migrant common snipe in North Dakota","interactions":[],"lastModifiedDate":"2025-02-14T16:35:27.887348","indexId":"1001664","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"Fall foods of migrant common snipe in North Dakota","docAbstract":"

Studies of foods consumed by common snipe (Capella gallinago) during fall migration (Sperry 1940, Erickson 1941, Choate in Tuck 1972, Tuck 1972) have shown that diets vary among habitats. More recently, Fogarty and Arnold (1977) expressed the need for more detailed information on snipe food habits and more refined knowledge of the snipe's range and adaptability to various food situations. There is a paucity of information on snipe feeding ecology in the prairie pothole region of North America where unstable and unpredictable hydrological conditions affect abundance and availability of aquatic foods. The objectives of study were to (1) identify foods consumed by common snipe during fall migration in south-central North Dakota, and (2) describe changes in diet during years with different water regimes.

","language":"English","publisher":"Wiley","doi":"10.2307/3800667","usgsCitation":"Fritzell, E., Swanson, G., and Meyer, M., 1979, Fall foods of migrant common snipe in North Dakota: Journal of Wildlife Management, v. 43, no. 1, p. 253-257, https://doi.org/10.2307/3800667.","productDescription":"5 p.","startPage":"253","endPage":"257","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130344,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North 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Dakota\",\"nation\":\"USA \"}}]}","volume":"43","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f79a1","contributors":{"authors":[{"text":"Fritzell, E.K.","contributorId":35685,"corporation":false,"usgs":true,"family":"Fritzell","given":"E.K.","email":"","affiliations":[],"preferred":false,"id":311473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swanson, G.A.","contributorId":49299,"corporation":false,"usgs":true,"family":"Swanson","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":311474,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, M.I.","contributorId":56584,"corporation":false,"usgs":true,"family":"Meyer","given":"M.I.","email":"","affiliations":[],"preferred":false,"id":311475,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2000146,"text":"2000146 - 1979 - Distribution and status of marine birds breeding along the coasts of the Chukchi and Bering seas","interactions":[],"lastModifiedDate":"2017-09-11T10:50:01","indexId":"2000146","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":74,"text":"Research Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"11","title":"Distribution and status of marine birds breeding along the coasts of the Chukchi and Bering seas","docAbstract":"The Alaska coast fronting on the Chukchi and Bering seas, exclusive of the Aleutian Islands, supports seven complexes of marine bird colonies numbering more than 1 million birds each, nine colonies of 100,000 to almost 1 million birds, and many smaller colonies. Colonies are found on most headlands and islands and are dominated numerically by alcids and kittiwakes (Rissa sp.). Estuarine habitats (mainly the lowlands of northern Seward Peninsula, Yukon-Kuskokwim delta, and the north side of the Alaska Peninsula) are extremely important for breeding and migrating marine waterfowl, shorebirds, gulls (Larus sp.), and terns (Sterna sp.). Information on population size and distribution of breeding marine birds within this area is extensive for only a few of the more heavily hunted species of waterfowl. Except for the intensive and systematic censusing of a few colonies in this region, population data on cliff-, burrow-, and crevice-nesting birds are such that all but gross changes in numbers may go unnoticed, and if noticed they could not be measured.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Conservation of marine birds of northern North America","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Bartonek, J., and Sealy, S., 1979, Distribution and status of marine birds breeding along the coasts of the Chukchi and Bering seas: Research Report 11, 11 p.","productDescription":"11 p.","startPage":"21","endPage":"31","numberOfPages":"11","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199255,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495c0","contributors":{"authors":[{"text":"Bartonek, James C.","contributorId":38085,"corporation":false,"usgs":true,"family":"Bartonek","given":"James C.","affiliations":[],"preferred":false,"id":325170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sealy, S.G.","contributorId":59908,"corporation":false,"usgs":true,"family":"Sealy","given":"S.G.","affiliations":[],"preferred":false,"id":325171,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001439,"text":"1001439 - 1979 - Second North Dakota record of Louisiana waterthrush","interactions":[],"lastModifiedDate":"2017-10-20T10:59:05","indexId":"1001439","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3111,"text":"Prairie Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Second North Dakota record of Louisiana waterthrush","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Prairie Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Faanes, C.A., 1979, Second North Dakota record of Louisiana waterthrush: Prairie Naturalist, v. 11, no. 3, p. 91-92.","productDescription":"2 p.","startPage":"91","endPage":"92","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":129013,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685fad","contributors":{"authors":[{"text":"Faanes, C. A.","contributorId":8790,"corporation":false,"usgs":true,"family":"Faanes","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":311029,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012589,"text":"70012589 - 1979 - International cooperation in water resources","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70012589","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1746,"text":"GeoJournal","active":true,"publicationSubtype":{"id":10}},"title":"International cooperation in water resources","docAbstract":"Advancements in hydrology proceeded slowly until the late 1800's when new ventures created a surge of interest and accomplishment. Progress waned again until the middle 20th century when an International Hydrological Decade was conceived, eventually receiving wide multinational support from governmental agencies and nongovernmental institutions. Organized by UNESCO, the Decade program was launched January 1, 1965. Participation included 107 nations, six United Nations agencies, and more than a dozen international scientific organizations. The initial program emphasized scientific research, and international cooperation; the second half of the Decade, emphasized technical assistance and technology transfer, largerly through education, training and demonstration. The success of the Decade led to the establishment of the International Hydrological Program, again under the aegis of UNESCO, to continue the work of the Decade indefinitely. The five major program activities, now involving about 90 countries and several international organizations, include: the scientific program, the promotion of education and training, the enhancement of information exchange, support of technical assistance, and the enlargement of regional cooperation. A significant amount of activity related to hydrological data networks and forecasting is carried on in an Operational Hydrology Programme by the WMO, chiefly through its Commission for Hydrology. Other international governmental organizations with a strong interest in water include the UN, the UN Development Programme, the FAO, the WHO, the International Atomic Energy Agency, the UN Environment Programme, the International Standardization Organization, and developmental institutions such as the World Bank. The specialized interests of researchers outside of the governmental structure, are met through association in various scientific and technical organizations which are world wide in scope and membership. Notwithstanding a sometimes bewildering variety of organizations, there certainly exists, for any nation, group, or individual, a demonstrated mechanism for almost any conceivable form of international cooperation in hydrology and water resources. ?? 1979 Akademische Verlagsgesellschaft.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"GeoJournal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00455987","issn":"03432521","usgsCitation":"Jones, J., Beall, R., and Giusti, E., 1979, International cooperation in water resources: GeoJournal, v. 3, no. 5, p. 481-487, https://doi.org/10.1007/BF00455987.","startPage":"481","endPage":"487","numberOfPages":"7","costCenters":[],"links":[{"id":222025,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205185,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00455987"}],"volume":"3","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3d39e4b0c8380cd633d1","contributors":{"authors":[{"text":"Jones, J.R.","contributorId":15967,"corporation":false,"usgs":true,"family":"Jones","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":363987,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beall, R.M.","contributorId":88392,"corporation":false,"usgs":true,"family":"Beall","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":363989,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Giusti, E.V.","contributorId":51342,"corporation":false,"usgs":true,"family":"Giusti","given":"E.V.","affiliations":[],"preferred":false,"id":363988,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70012617,"text":"70012617 - 1979 - Probability weighted moments: Definition and relation to parameters of several distributions expressable in inverse form","interactions":[],"lastModifiedDate":"2018-02-05T12:28:50","indexId":"70012617","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"Probability weighted moments: Definition and relation to parameters of several distributions expressable in inverse form","docAbstract":"

Distributions whose inverse forms are explicitly defined, such as Tukey's lambda, may present problems in deriving their parameters by more conventional means. Probability weighted moments are introduced and shown to be potentially useful in expressing the parameters of these distributions.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR015i005p01049","usgsCitation":"Greenwood, J., Landwehr, J.M., Matalas, N., and Wallis, J., 1979, Probability weighted moments: Definition and relation to parameters of several distributions expressable in inverse form: Water Resources Research, v. 15, no. 5, p. 1049-1054, https://doi.org/10.1029/WR015i005p01049.","productDescription":"6 p.","startPage":"1049","endPage":"1054","costCenters":[],"links":[{"id":222486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505a8cbde4b0c8380cd7e875","contributors":{"authors":[{"text":"Greenwood, J. Arthur","contributorId":87031,"corporation":false,"usgs":false,"family":"Greenwood","given":"J. Arthur","affiliations":[],"preferred":false,"id":364076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landwehr, J. Maciunas","contributorId":13962,"corporation":false,"usgs":false,"family":"Landwehr","given":"J.","email":"","middleInitial":"Maciunas","affiliations":[],"preferred":false,"id":364074,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Matalas, N.C.","contributorId":25173,"corporation":false,"usgs":true,"family":"Matalas","given":"N.C.","affiliations":[],"preferred":false,"id":364073,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wallis, J.R.","contributorId":79236,"corporation":false,"usgs":true,"family":"Wallis","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":364075,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70012604,"text":"70012604 - 1979 - Submarine thermal springs on the Galapagos Rift","interactions":[],"lastModifiedDate":"2015-06-15T09:48:53","indexId":"70012604","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Submarine thermal springs on the Galapagos Rift","docAbstract":"

The submarine hydrothermal activity on and near the Galápagos Rift has been explored with the aid of the deep submersible Alvin. Analyses of water samples from hydrothermal vents reveal that hydrothermal activity provides significant or dominant sources and sinks for several components of seawater; studies of conductive and convective heat transfer suggest that two-thirds of the heat lost from new oceanic lithosphere at the Galápagos Rift in the first million years may be vented from thermal springs, predominantly along the axial ridge within the rift valley. The vent areas are populated by animal communities. They appear to utilize chemosynthesis by sulfur-oxidizing bacteria to derive their entire energy supply from reactions between the seawater and the rocks at high temperatures, rather than photosynthesis

","language":"English","publisher":"AAAS","doi":"10.1126/science.203.4385.1073","issn":"00368075","usgsCitation":"Corliss, J., Dymond, J., Gordon, L., Edmond, J., Von Herzen, R.P., Ballard, R.D., Green, K., Williams, D., Bainbridge, A., Crane, K., and Van Andel, T.H., 1979, Submarine thermal springs on the Galapagos Rift: Science, v. 203, no. 4385, p. 1073-1083, https://doi.org/10.1126/science.203.4385.1073.","productDescription":"11 p.","startPage":"1073","endPage":"1083","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":222268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"203","issue":"4385","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d36e4b08c986b31d6ea","contributors":{"authors":[{"text":"Corliss, J.B.","contributorId":108253,"corporation":false,"usgs":true,"family":"Corliss","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":364038,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dymond, J.","contributorId":98461,"corporation":false,"usgs":true,"family":"Dymond","given":"J.","email":"","affiliations":[],"preferred":false,"id":364037,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gordon, L.I.","contributorId":28370,"corporation":false,"usgs":true,"family":"Gordon","given":"L.I.","email":"","affiliations":[],"preferred":false,"id":364030,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edmond, J.M.","contributorId":24920,"corporation":false,"usgs":true,"family":"Edmond","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":364029,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Von Herzen, R. P.","contributorId":87662,"corporation":false,"usgs":true,"family":"Von Herzen","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":364036,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ballard, Richard D.","contributorId":40729,"corporation":false,"usgs":true,"family":"Ballard","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":364032,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Green, K.","contributorId":63949,"corporation":false,"usgs":true,"family":"Green","given":"K.","affiliations":[],"preferred":false,"id":364033,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Williams, D.","contributorId":31908,"corporation":false,"usgs":true,"family":"Williams","given":"D.","affiliations":[],"preferred":false,"id":364031,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Bainbridge, A.","contributorId":81639,"corporation":false,"usgs":true,"family":"Bainbridge","given":"A.","affiliations":[],"preferred":false,"id":364035,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Crane, K.","contributorId":14117,"corporation":false,"usgs":true,"family":"Crane","given":"K.","email":"","affiliations":[],"preferred":false,"id":364028,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Van Andel, T. H.","contributorId":68038,"corporation":false,"usgs":true,"family":"Van Andel","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":364034,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}} ,{"id":27965,"text":"wri7995 - 1979 - Hydrology and water quality in the Nederlo Creek Basin, Wisconsin, before construction of two water-retention structures","interactions":[],"lastModifiedDate":"2023-03-29T19:49:27.118639","indexId":"wri7995","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-95","title":"Hydrology and water quality in the Nederlo Creek Basin, Wisconsin, before construction of two water-retention structures","docAbstract":"

The Nederlo Creek basin, in the \"Driftless Area\" of southwest Wisconsin, is geographically and hydrologically similar to other small basins in the area. Topography is rugged, with approximately 400 feet of relief between the boundary ridge tops and the valley floor. The water-retention structures (a dry floodwater- retention structure and a 43-acre reservoir) are to provide recreation and flood protection for the basin.

\n

Streamflow, springflow, precipitation, and groundwater levels were monitored at several sites to describe the hydrologic system. Streamflow is fairly constant at base flow, but rapid changes in discharge occur during periods of snowmelt or heavy rain; recession to base-flow discharge following these events is rapid. Surface runoff is a significant contributor to Streamflow only 10 percent of the time.

\n

The mean annual hydrologic budget for water years 1968-72 shows that of the 32.5 inches of precipitation on the basin, 6.4 inches left as runoff and 25.9 inches as evapotranspiration; ground-water storage increased an average of 0.2 inches per year.

\n

The water is a hard calcium magnesium bicarbonate type. Concentrations of major constituents in ground water and streams at base flow are similar, but concentrations in the stream generally decrease during periods when surface runoff contributes to Streamflow. Dissolved-oxygen concentrations in the stream are generally lowest during the summer; nighttime lows are generally between 7 and 8 milligrams per liter and daily maximums between 11 and 12.5 milligrams per liter. Diurnal water-temperature fluctuations of several degrees are common in streams during summer; daily maximum water temperatures as high as 26°C have been measured in some areas, but temperatures this high seldom persist for more than 2 hours. Estimates of mean annual total phosphorus and total nitrogen loads during 1967-74 fall within the ranges of 0.02 to 0.07 and 0.4 to 0.8 tons per square mile, respectively; 70 to 80 percent of the total phosphorus and 35 to 55 percent of the total nitrogen are transported during periods when surface runoff contributes to Streamflow.

\n

Mean annual suspended-sediment loads during 1968-74 range from 13 to 60 tons per square mile, with 74 to 86 percent of the total transported during periods when surface water contributes to streamflow. These sediment loads are at the low end of the range previously reported for streams in the \"Driftless Area\".

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7995","usgsCitation":"Kammerer, P.A., and Sherrill, M.G., 1979, Hydrology and water quality in the Nederlo Creek Basin, Wisconsin, before construction of two water-retention structures: U.S. Geological Survey Water-Resources Investigations Report 79-95, v, 34 p., https://doi.org/10.3133/wri7995.","productDescription":"v, 34 p.","numberOfPages":"41","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":414907,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35374.htm","linkFileType":{"id":5,"text":"html"}},{"id":123633,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0095/report-thumb.jpg"},{"id":56783,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0095/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","otherGeospatial":"Nederlo Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.01554870605469,\n 43.308941276170124\n ],\n [\n -91.01554870605469,\n 43.40429919674392\n ],\n [\n -90.86242675781249,\n 43.40429919674392\n ],\n [\n -90.86242675781249,\n 43.308941276170124\n ],\n [\n -91.01554870605469,\n 43.308941276170124\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688073","contributors":{"authors":[{"text":"Kammerer, Phil A. Jr.","contributorId":85993,"corporation":false,"usgs":true,"family":"Kammerer","given":"Phil","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":198975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sherrill, Marvin G.","contributorId":91469,"corporation":false,"usgs":true,"family":"Sherrill","given":"Marvin","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":198976,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}