{"pageNumber":"2430","pageRowStart":"60725","pageSize":"25","recordCount":68807,"records":[{"id":70006516,"text":"70006516 - 1972 - Lake Erie: Effects of exploitation, environmental changes and new species on the fishery resources","interactions":[],"lastModifiedDate":"2012-11-21T14:00:48","indexId":"70006516","displayToPublicDate":"2012-11-21T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Lake Erie: Effects of exploitation, environmental changes and new species on the fishery resources","docAbstract":"In no other lake as large as Lake Erie (surface area, 25,690 km<sup>2</sup>) have such extensive changes taken place in the drainage basin, the lake environment, and the fish populations over the last 100 years. Deforestation and prairie burning led to erosion and siltation of valuable spawning grounds. Marsh spawning areas were drained. Lake-to-river spawning migrations were blocked by mill dams. Accelerated cultural nutrient loading increased total dissolved solids by nearly 50% (1920-70). Average summer water temperatures increased 1.1 C. Phytoplankton and zooplankton abundance increased severalfold. Severe oxygen depletion developed in the bottom waters of all three basins of the lake. Lake sturgeon were fished out as nuisance fish in the late 1800s. The commercial fisheries for lake trout, lake whitefish, and lake herring collapsed by 1940 and those for blue pike and walleye by 1960. Yellow perch production became unstable in the 1960s. The effects of exploitation, environmental changes, and new species on these fish populations are discussed.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Fisheries Research Board of Canada","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"NRC Research Press","publisherLocation":"Ottawa, ON","doi":"10.1139/f72-133","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Hartman, W.L., 1972, Lake Erie: Effects of exploitation, environmental changes and new species on the fishery resources: Journal of the Fisheries Research Board of Canada, v. 29, no. 6, p. 899-912, https://doi.org/10.1139/f72-133.","productDescription":"14 p.","startPage":"899","endPage":"912","numberOfPages":"13","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":263342,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":263341,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/f72-133"}],"country":"United States;Canada","otherGeospatial":"Lake Erie","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.4797,41.3971 ], [ -83.4797,43.2635 ], [ -78.8539,43.2635 ], [ -78.8539,41.3971 ], [ -83.4797,41.3971 ] ] ] } } ] }","volume":"29","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50adf7e9e4b03b26ec4d382d","contributors":{"authors":[{"text":"Hartman, Wilbur L.","contributorId":14763,"corporation":false,"usgs":true,"family":"Hartman","given":"Wilbur","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":354659,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70038678,"text":"wdrCA712 - 1972 - Water resources data for California, 1971; Part 2: Water quality records","interactions":[],"lastModifiedDate":"2012-06-13T01:01:48","indexId":"wdrCA712","displayToPublicDate":"2012-06-04T10:29:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-71-2","title":"Water resources data for California, 1971; Part 2: Water quality records","docAbstract":"Water-resources data for the 1971 water year for California include records of data for the chemical and physical characteristics of surface water. The distribution, type, and number of stations in each river or drainage basin are shown in figure 1. A few pertinent stations in bordering States are also included. The records were compiled by the Water Resources Division of the U.S. Geological Survey under the direction of R. Stanley Lord, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geololgical Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA712","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for California, 1971; Part 2: Water quality records: U.S. Geological Survey Water Data Report CA-71-2, xii, 512 p., https://doi.org/10.3133/wdrCA712.","productDescription":"xii, 512 p.","costCenters":[],"links":[{"id":257490,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/ca-71/WDR-1971-wq.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":257514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_71_2.jpg"}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc953e4b08c986b32ccdc","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":535193,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70038249,"text":"70038249 - 1972 - Water resources inventory of Connecticut Part 6: Upper Housatonic River basin","interactions":[],"lastModifiedDate":"2014-06-27T11:37:50","indexId":"70038249","displayToPublicDate":"2012-04-22T16:17:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"21","title":"Water resources inventory of Connecticut Part 6: Upper Housatonic River basin","docAbstract":"<p>The upper Housatonic River basin report area has an abundant supply of water of generally good quality, which is derived from precipitation on the area and streams entering the area. Annual precipitation has averaged about 46 inches over a 30-year period. Of this, approximately 22 inches of water is returned to the atmosphere each year by evaporation and transpiration; the remainder flows overland to streams or percolates downward to the water table and ultimately flows out of the report area in the Housatonic River or in smaller streams tributary to the Hudson River. During the autumn and winter precipitation normally is sufficient to cause a substantial increase in the amount of water stored in surface reservoirs and in aquifers, whereas in the summer, losses through evaporation and transpiration result in sharply reduced streamflow and lowered ground-water levels. Mean monthly storage of water in November is 2.8 inches more than it is in June.</p>\n<br/>\n<p>The amount of water that flows into, through, and out of the report area represents the total amount potentially available for use ignoring reuse. For the 30-year period 1931 through 1960, the annual runoff from precipitation has averaged 24 inches (294 billion gallons). During the same period, inflows from Massachusetts and New York have averaged 220 and 64 billion gallons per year, respectively. A total average annual runoff of 578 billion gallons is therefore available. Although runoff indicates the total amount of water potentially available, it is rarely feasible to use all of it. On the other hand, with increased development, some water may be reused several times.</p>\n<br/>\n<p>The water availability may be tapped as it flows through the area or is temporarily stored in streams, lakes, and aquifers. The amounts that can be developed differ from place to place and time to time, depending on the amount of precipitation, on the size of drainage area, on the thickness, transmissivity, and areal extent of aquifers, and on the variations in chemical and physical quality of water.</p>\n<br/>\n<p>Differences in precipitation cause differences in the amount of streamflow whereas differences in the proportion of stratified drift affect its timing.</p>\n<br/>\n<p>Water can be obtained from wells almost anywhere in the area, but the amount obtainable at any particular point depends on the type and water-bearing properties of the aquifers tapped.</p>\n<br/>\n<p>Stratified-drift aquifers are the only ones generally capable of yielding more than 100 gpm (gallons per minute) to individual wells. Drilled, screened wells tapping this unit yield from 17 to 1,400 gpm, with a median yield of 200 gpm.</p>\n<br/>\n<p>Till and bedrock are widespread but generally provide only small supplies of water. Till is tapped in a few places by dug wells, which can yield small supplies of only a few hundred gallons per day throughout all or most of the year. Bedrock is the chief aquifer for privately owned domestic and rural supplies; it is tapped by drilled wells, about 90 percent of which will supply at least 2 gpm. Only 1 of 10 bedrock wells, however, will supply more than 30 gpm.</p>\n<br/>\n<p>The amount of ground water potentially available in the report area depends upon the thickness and hydraulic properties of aquifers, the amount of salvageable natural discharge of ground water, and the quantity of water available by induced infiltration from streams and lakes. From data on transmissivity, thickness, recharge, well performance, and streamflow, preliminary estimates of ground-water availability can be made for most stratified-drift aquifers in the report area. Long-term yields estimated for eight areas of stratified drift especially favorable for development of large ground-water supplies ranged from 0.6 to 5 mgd (million gallons per day). Detailed site studies are needed to verity these estimates and to determine optimum yields, drawdowns, and spacing of individual wells before major ground-water development is undertaken in these or other areas.</p>\n<br/>\n<p>The chemical quality of water in the report area is generally good; carbonate-bedrock units exert considerable local influence on water quality. Samples of naturally occurring surface water collected at 24 sites during low flow averaged 90 mg/l (milligrams per liter) dissolved solids and 60 mg/l hardness. Water from wells is generally more highly mineralized than naturally occurring water from streams. About 37 percent of the wells sampled yielded water with more than 200 mg/l dissolved solids and 50 percent yielded water with more than 120 mg/l hardness. These concentrations reflect the high degree of mineralization of ground water in carbonate bedrock and unconsolidated deposits derived from this bedrock. The larger streams, which transport varying amounts of industrial and domestic effluents, averaged about 150 mg/l dissolved solids and 90 mg/l hardness.</p>\n<br/>\n<p>Iron and manganese concentrations in both ground water and surface water at some places exceed recommended limits for domestic and industrial use. Most wells in the report area yield water with little or no iron or manganese. In certain localities however, the probability is high of encountering water with excessive concentrations of these constituents. Schists, especially the unit in the northwestern corner of the basin, are the likely sources of water with excessive iron and manganese.</p>\n<br/>\n<p>Iron concentrations in naturally occurring stream water exceed 0.3 mg/l under low-flow conditions at 29 percent of the sites sampled. These excessive concentrations result from discharge of iron-bearing water from aquifers or from swamps where iron is released from decaying vegetation.</p>\n<br/>\n<p>Water temperature in the larger streams ranges from 0°C (degrees Celsius) to about 28°C. Ground water between 30 feet and 200 feet below the land surface has a relatively constant temperature, usually between 8°C and 11°C.</p>\n<br/>\n<p>The quantity of suspended sediment transported by streams under natural conditions is negligible. Even in streams affected by man, turbidity is rarely a problem.</p>\n<br/>\n<p>The total amount of water used in the report area for all purposes during 1967 was about 6,360 million gallons, or 140 gpd per person. Public supplies furnished the domestic needs of nearly half the population of the area. All of the 14 public supplies sampled provided water that meets the drinking water standards of the U.S. Public Health Service.</p>","language":"English","publisher":"Connecticut Department of Environmental Protection","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Cervione, M.A., Mazzaferro, D.L., and Melvin, R.T., 1972, Water resources inventory of Connecticut Part 6: Upper Housatonic River basin: Connecticut Water Resources Bulletin 21, Report: viii, 82 p.; 6 Plates: 31.73 x 39.58 inches and smaller.","productDescription":"Report: viii, 82 p.; 6 Plates: 31.73 x 39.58 inches and smaller","numberOfPages":"92","costCenters":[],"links":[{"id":258809,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0021/report.pdf","size":"26735","linkFileType":{"id":1,"text":"pdf"}},{"id":258810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0021/report-thumb.jpg"},{"id":285991,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038249/plate-b-2.pdf"},{"id":285992,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038249/plate-b-3.pdf"},{"id":285989,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038249/plate-a.pdf"},{"id":285990,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038249/plate-b-1.pdf"},{"id":285993,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038249/plate-c.pdf"},{"id":285994,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038249/plate-d.pdf"}],"scale":"125000","country":"United States","state":"Connecticut","otherGeospatial":"Housatonic River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.566667,41.25 ], [ -73.566667,42.066667 ], [ -73.166667,42.066667 ], [ -73.166667,41.25 ], [ -73.566667,41.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb7ce4b08c986b32d699","contributors":{"authors":[{"text":"Cervione, Michael A. Jr.","contributorId":23988,"corporation":false,"usgs":true,"family":"Cervione","given":"Michael","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mazzaferro, David L.","contributorId":89539,"corporation":false,"usgs":true,"family":"Mazzaferro","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":463736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Melvin, Robert T.","contributorId":99808,"corporation":false,"usgs":true,"family":"Melvin","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":463737,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039169,"text":"70039169 - 1972 - Surface-water investigations at Barrow, Alaska","interactions":[],"lastModifiedDate":"2012-07-24T01:01:47","indexId":"70039169","displayToPublicDate":"2012-01-01T11:36:52","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":347,"text":"Basic Data Report","active":false,"publicationSubtype":{"id":6}},"title":"Surface-water investigations at Barrow, Alaska","docAbstract":"The U.S. Public Health Service is currently developing plans for a long-term water supply and sewage treatment system for the village of Barrow, Alaska. To assist in planning, the U.S. Geological Survey was requested to initiate a cooperative streamflow data-collection program with the U.S. Public Health Service in June 1972 to determine the availability of surface water and the areal distribution of runoff in the Barrow area. This basic-data report summarizes the streamflow data collected from June 1 through July 10, 1972, at three gaging stations in the Barrow area (fig. 1) and discusses the future data-collection program.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Anchorage, AK","doi":"10.3133/70039169","collaboration":"Prepared in cooperation with the United States Public Health Service","usgsCitation":"Jones, S.H., 1972, Surface-water investigations at Barrow, Alaska: Basic Data Report, 16 p., https://doi.org/10.3133/70039169.","productDescription":"16 p.","numberOfPages":"18","costCenters":[{"id":109,"text":"Alaska District Water Resources Division","active":false,"usgs":true}],"links":[{"id":261324,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039169/report.pdf"},{"id":261325,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039169/report-thumb.jpg"}],"country":"United States","state":"Alaska","city":"Barrow;Browerville","otherGeospatial":"Emaiksoun Lake;Esatkuat Lagoon;Esatkuat Creek;Nunavak Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -156.88333333333333,71.21666666666667 ], [ -156.88333333333333,71.35 ], [ -156.63333333333333,71.35 ], [ -156.63333333333333,71.21666666666667 ], [ -156.88333333333333,71.21666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba190e4b08c986b31f176","contributors":{"authors":[{"text":"Jones, Stanley H.","contributorId":98729,"corporation":false,"usgs":true,"family":"Jones","given":"Stanley","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":465718,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70001480,"text":"70001480 - 1972 - Microcrystalline sphalerite in resin globules suspended in Lake Kivu, East Africa","interactions":[],"lastModifiedDate":"2020-12-21T23:53:54.917661","indexId":"70001480","displayToPublicDate":"2010-09-28T23:09:22","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2746,"text":"Mineralium Deposita","active":true,"publicationSubtype":{"id":10}},"title":"Microcrystalline sphalerite in resin globules suspended in Lake Kivu, East Africa","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>The origin and chemical nature of micron-sized spheres found as suspended particles in Lake Kivu are examined. It can be shown that the hollow spheres, with a wall thickness of 500 Å, consist of a complex polymeric resinous material which has little functionality, except for hydroxyl groups. The spheres arise in the process of degassing of water samples at depth. Tiny gas bubbles, about 1 micron in size, act as scavengers of dissolved resinous material. The newly created resinous membrane promotes the selective coordination of zinc dissolved in the water column. In the prevailing H<sub>2</sub>S regime, formation of sphalerite crystals in induced. The size range of the crystals, 5 to 50 Å, corresponds to 1 to 10 unit cells and suggests that the resinous membrane also acts as a template in sphalerite growth processes. The sources of the zinc and dissolved gases (CO<sub>2</sub>, CH<sub>4</sub>, H<sub>2</sub>S) are hydrothermal springs seeping from the lake bottom into the basin. Water discharge is substantial; about 100 years are required to fill the lake to its present level (ca. 550 km<sup>3</sup><span>&nbsp;</span>water). The average Kivu water contains 2 ppm zinc. Thus, 1 million tons of zinc are contained in Lake Kivu in the form of sphalerite.</p></div></div><div id=\"Abs2-section\" class=\"c-article-section\"><br></div>","language":"English","publisher":"Springer","doi":"10.1007/BF00206891","issn":"00264598","usgsCitation":"Degens, E., Okada, H., Honjo, S., and Hathaway, J., 1972, Microcrystalline sphalerite in resin globules suspended in Lake Kivu, East Africa: Mineralium Deposita, v. 7, no. 1, p. 1-12, https://doi.org/10.1007/BF00206891.","productDescription":"12 p.","startPage":"1","endPage":"12","costCenters":[],"links":[{"id":203675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Democratic Republic of Congo, Rwanda","otherGeospatial":"Lake Kivu","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              28.707275390624996,\n              -2.58640142780824\n            ],\n            [\n              29.53125,\n              -2.58640142780824\n            ],\n            [\n              29.53125,\n              -1.491225656518564\n            ],\n            [\n              28.707275390624996,\n              -1.491225656518564\n            ],\n            [\n              28.707275390624996,\n              -2.58640142780824\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"7","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bc81","contributors":{"authors":[{"text":"Degens, E.T.","contributorId":76321,"corporation":false,"usgs":true,"family":"Degens","given":"E.T.","email":"","affiliations":[],"preferred":false,"id":346774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Okada, H.","contributorId":14097,"corporation":false,"usgs":true,"family":"Okada","given":"H.","email":"","affiliations":[],"preferred":false,"id":346773,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Honjo, S.","contributorId":97227,"corporation":false,"usgs":true,"family":"Honjo","given":"S.","email":"","affiliations":[],"preferred":false,"id":346776,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hathaway, J.C.","contributorId":94280,"corporation":false,"usgs":true,"family":"Hathaway","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":346775,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70001459,"text":"70001459 - 1972 - Metamorphic assemblages and the direction of flow of metamorphic fluids in four instances of serpentinization","interactions":[],"lastModifiedDate":"2022-11-18T16:36:23.524509","indexId":"70001459","displayToPublicDate":"2010-09-28T23:09:21","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Metamorphic assemblages and the direction of flow of metamorphic fluids in four instances of serpentinization","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>Fluids related to Serpentinization are of at least three types. The first reported (Barnes and O'Neil, 1969) is a fluid of local meteoric origin, the chemical and thermodynamic properties of which are entirely controlled by olivine, orthopyroxene, brucite, and serpentine reactions. It is a Ca<sup>+2</sup>-OH<sup>−1</sup><span>&nbsp;</span>type and is shown experimentally to be capable of reacting with albite to yield calcium hydroxy silicates. Rodingites may form where the Ca<sup>+2</sup>-OH<sup>−1</sup><span>&nbsp;</span>type waters flow across the ultramafic contact and react with siliceous country rock.</p><p>The second type of fluid has its chemical composition largely controlled before it enters the ultramafic rocks, but reactions within the ultramafic rocks fix the thermodynamic properties by reactions of orthopyroxene, olivine, calcite, brucite, and serpentine. The precipitation of brucite from this fluid clearly shows that fluid flow allows reaction products to be deposited at a distance from the point of solution. Thus, textural evidence for volume relations during Serpentinization may not be valid.</p><p>The third type of fluid has its chemical properties fixed in part before the reactions with ultramafic rocks, in part by the reactions of orthopyroxene, olivine, and serpentine and in part by reactions with siliceous country rock at the contact. The reactions of the ultramafic rock and country rock with the fluid must be contemporaneous and require flow to be along the contact. This third type of fluid is grossly supersaturated with talc and tremolite, both found along the contact. The occurrence of magadiite, kenyaite, mountainite, and rhodesite along the contact is probably due to a late stage low-temperature reaction of fluids of the same thermodynamic properties as those that formed the talc and tremolite at higher temperatures. Oxygen isotope analyses of some of these minerals supports this conclusion.</p><p>Rodingites form from Ca<sup>+2</sup>-rich fluids flowing across the contact; talc and tremolite form from silica-rich fluids flowing along the contact.</p><p>Isotopic analyses of the fluids indicate varied origins including unaltered local meteoric water and connate water. Complexion Spring water may be a sample of only slightly altered Jurassic or Cretaceous sea water.</p></div></div><div id=\"cobranding-and-download-availability-text\" class=\"note test-pdf-link\"><br></div>","language":"English","publisher":"Springer","doi":"10.1007/BF00371220","issn":"00107999","usgsCitation":"Barnes, I., Rapp, J., O’Neil, J.R., Sheppard, R., and Gude, A.J., 1972, Metamorphic assemblages and the direction of flow of metamorphic fluids in four instances of serpentinization: Contributions to Mineralogy and Petrology, v. 35, no. 3, p. 263-276, https://doi.org/10.1007/BF00371220.","productDescription":"14 p.","startPage":"263","endPage":"276","costCenters":[],"links":[{"id":203777,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":409453,"rank":2,"type":{"id":12,"text":"Errata"},"url":"https://doi.org/10.1007/BF00371728","linkFileType":{"id":5,"text":"html"}}],"volume":"35","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db62878e","contributors":{"authors":[{"text":"Barnes, I.","contributorId":23678,"corporation":false,"usgs":true,"family":"Barnes","given":"I.","affiliations":[],"preferred":false,"id":346764,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rapp, John B.","contributorId":32028,"corporation":false,"usgs":true,"family":"Rapp","given":"John B.","affiliations":[],"preferred":false,"id":346766,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Neil, J. R.","contributorId":69633,"corporation":false,"usgs":true,"family":"O’Neil","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":346767,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sheppard, R.A.","contributorId":22361,"corporation":false,"usgs":true,"family":"Sheppard","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":346763,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gude, A. J. III","contributorId":25554,"corporation":false,"usgs":true,"family":"Gude","given":"A.","suffix":"III","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":346765,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":5210161,"text":"5210161 - 1972 - Biological data on PCBs in animals other than man","interactions":[],"lastModifiedDate":"2012-02-02T00:15:16","indexId":"5210161","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1972","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Biological data on PCBs in animals other than man","docAbstract":"SUMMARY:  Polychlorinated biphenyls have become ubiquitous in the world ecosystem in quantities similar to those of DDE.      Experimental studies have shown that PCBs have a toxicity to mallards, pheasants, bobwhite quail, coturnix quail, red-winged blackbirds, starlings, cowbirds, and grackles that is of the same order as the toxicity of DDE to these species. Overt signs of poisoning also are similar to those caused by compounds of the DDT group. Toxic effects of DDE and Aroclor 1254 to coturnix chicks were additive, but not synergistic.      PCBs containing higher percentages of chlorine are more toxic to birds than those containing lower percentages. PCBs of foreign manufacture contained contaminants to an extent that greatly increased their toxicity.      Residues of PCBs in the brains of birds killed by these compounds measure in the hundreds of parts per million. PCBs may have contributed to mortality of some birds in the field.      Toxicity to insects of PCBs of different degrees of chlorination is the reverse of the pattern in birds: the lower chlorinations are more toxic to insects. PCBs enhanced the toxicity of dieldrin and DDT to insects.      Shrimp are very sensitive to PCBs and most will die as a result of 20-day exposure to a concentration of 5 ppb. PCBs also inhibit shell growth of oysters. Crabs are less sensitive; all accumulate residues to many times the concentrations in the water, and a test with crabs showed that they lost the residues very slowly.      Growth of certain species of marine diatoms was experimentally inhibited by PCBs, but algae were not affected.      The small marine crustacean, Gammarus, is sensitive to PCBs in concentrations of thousandths to tenths of a part per billion.        Exposure to 5 ppb of Aroclor 1254 caused mortality of two species of fish in 14-45 days. Onset of death was delayed and was accompanied by fungus-like lesions.      Rainbow trout were quickly killed by terphenyls at 10 ppb under normal oxygen conditions and at 2 ppb with reduced oxygen.      Metabolic changes of PCBs have been suggested by environmental observations of different isomeric patterns in animals of different trophic levels. Quantitative differences also are pronounced, with magnifications of hundreds to thousands of times.      Laboratory studies have shown no metabolic changes of PCBs by crabs and shrimps, minimal changes by fish, and pronounced changes by birds.        PCBs induce microsomal enzyme activity in birds. Exposure to PCBs increased the susceptibility of mallard ducklings to duck hepatitis virus.      Offspring of pheasants whose parents received high dosages of PCBs made poor choices in visual cliff tests. Egg production and hatching after pipping also were affected. Migratory restlessness was increased in English robins exposed to PCBs.      Long-term studies of the reproductive effects of Aroclor 1254 on mallards and bobwhite quail and of Aroclor 1254 plus DDE on quail showed no significant differences from controls. In studies of chickens, however, egg production and hatchability were impaired by high doses of Aroclor 1254 and by low doses of Aroclor 1242.      Statistical evaluations of the role that different chemicals may play in thinning eggshells of brown pelicans showed that DDE residues correlate better with shell thinning than do residues of dieldrin or PCBs, confirming observations with cormorants and white pelicans.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Polychlorinated Biphenyls and the Environment","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Interdepartmental Task Force on PCBs","publisherLocation":"Washington, D.C.","collaboration":"OCLC:  6261205 ; OCLC:  1165099 ; distributed by NTIS, stock No. COM-72-10419","usgsCitation":"Stickel, L., 1972, Biological data on PCBs in animals other than man, chap. <i>of</i> Polychlorinated Biphenyls and the Environment, p. 158-172.","productDescription":"vii, 181","startPage":"158","endPage":"172","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c473","contributors":{"authors":[{"text":"Stickel, L.F.","contributorId":41095,"corporation":false,"usgs":true,"family":"Stickel","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":327875,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047554,"text":"70047554 - 1972 - Hydraulic testing of hole UA-1-HTH-1, Amchitka Island, Alaska","interactions":[],"lastModifiedDate":"2013-09-19T13:11:24","indexId":"70047554","displayToPublicDate":"2009-01-01T09:10:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Hydraulic testing of hole UA-1-HTH-1, Amchitka Island, Alaska","docAbstract":"Total depth of the hole was 1,054 meters (3,458 feet) but, because of borehole erosion and bridging, only about 198 meters (650 feet) of the hole was·hydraulically tested with straddle packers. Some information was obtained on the lower part of the hole by use of the pressure recorders which are used with the straddle packers. The heads below land surface in that part of the hole tested with. straddle packers. ranged from·3.9 meters {12.7 feet) in the ..\ninterval 80.5 to 125. 0. meters (264- to 410 feet), the uppermost zone tested with straddle packers, to 5.1 meters (18.6 feet) in the interval 227.4 to 278.6 meters (.746 to 914 feet), the lowermost part of the hole tested with straddle packers. The composite static water level obtained following a pumping test.was 5.5 meters (18,0 feet). The composite head below 278.6 meters (914 feet), determined from a pressure recorder, was about 12.2 meters (40 feet). The head distribution. indicates a decreasing· head with depth. Water samples were collected from two intervals for chemical, radiochemical, and C-14 analysis. The unadjusted age of water in the interval 183.5 to 234.7 meters (602 to 770. feet) was determined to be 8,410 years, and for the interval 227.4 to 278.6 meters (746 to 914 feet) was 17,880 years. After adjustment the.ages of the waters may be less; however, they would still be. in the thousands of years and the relative difference probably would still be real.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/70047554","usgsCitation":"Ballance, W.C., and Dinwiddie, G., 1972, Hydraulic testing of hole UA-1-HTH-1, Amchitka Island, Alaska, 27 p., https://doi.org/10.3133/70047554.","productDescription":"27 p.","numberOfPages":"32","costCenters":[],"links":[{"id":277872,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047554/report.pdf"},{"id":276298,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047554/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 178.6158,51.3092 ], [ 178.6158,51.6665 ], [ 179.4688,51.6665 ], [ 179.4688,51.3092 ], [ 178.6158,51.3092 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03efe4b0026c2bc11b96","contributors":{"authors":[{"text":"Ballance, Wilbur C.","contributorId":50436,"corporation":false,"usgs":true,"family":"Ballance","given":"Wilbur","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":482395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dinwiddie, G.A.","contributorId":49798,"corporation":false,"usgs":true,"family":"Dinwiddie","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":482394,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039440,"text":"70039440 - 1972 - Channel erosion surveys along proposed TAPS route, Alaska, July 1971","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039440","displayToPublicDate":"2008-11-18T14:45:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Channel erosion surveys along proposed TAPS route, Alaska, July 1971","docAbstract":"The U.S. Geological Survey has the threefold responsibility along the proposed route of the Trans-Alaska Pipeline System (TAPS): to investigate possible hydroloqic hazards to the pipeline, to investigate possible impacts of the pipeline on water resources, and to develop a better understanding of Arctic hydrology. Because the proposed pipeline route lies within many stream channels, one of the obvious hydrologic hazards is channel erosion. It was considered a major hazard in a report by Hadley (1969) after a short reconnaissance of the proposed pipeline route and also in a national assessment of water resources by the Water Resources Council (1968). The U.S. Department of Interior has also recognized the channel erosion problems in considering the environmental impacts of TAPS and has stipulated conditions for their control (U.S. Dept. of Interior, 1972a, b). The Alyeska Pipeline Service Company (APSC), who would build and operate TAPS, has described methods for complying with the Department of Interior stipulations for channel and erosion control (APSC, 1971).","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039440","usgsCitation":"Childers, J.M., 1972, Channel erosion surveys along proposed TAPS route, Alaska, July 1971, 79 p., https://doi.org/10.3133/70039440.","productDescription":"79 p.","numberOfPages":"87","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":261578,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039440/report.pdf"},{"id":261579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039440/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173,54.666666666666664 ], [ 173,71.83333333333333 ], [ -130,71.83333333333333 ], [ -130,54.666666666666664 ], [ 173,54.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f452e4b0c8380cd4bc79","contributors":{"authors":[{"text":"Childers, Joseph M.","contributorId":14379,"corporation":false,"usgs":true,"family":"Childers","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":466241,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039525,"text":"70039525 - 1972 - A land use classification scheme for use with remote sensor data","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039525","displayToPublicDate":"2008-01-16T14:25:00","publicationYear":"1972","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"A land use classification scheme for use with remote sensor data","docAbstract":"The needs of Federal agencies for a broad overview of national land use patterns, trends, and environmental impacts, with data inputs from both conventional sources and some of the more exotic sensors in high altitude aircraft and satellite platforms led to the formation in early 1971 of an Inter-Agency Steering Committee on Land Use Information and Classification. The work of this Committee, composed of representatives from the Geological Survey of the U.S. Department of the Interior, the Earth Observations Program of the National Aeronautics and Space Administration, the Soil Conservation Service of the U.S. Department of Agriculture, as well as the Association of American Geographers and the International Geographical Union, has been supported by NASA and the EROS Program of the Interior Department and coordinated by the USGS Geographic Applications Program. The Chairman of the Inter-Agency Committee was Dr. Arch C. Gerlach, Chief Geographer of the Geological Survey until his death in May 1972. Shortly before Dr. Gerlach's death, Dr. James R. Anderson was appointed Acting Chairman of the Committee.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, A land use classification scheme for use with remote sensor data, v, 205 p.","productDescription":"v, 205 p.","numberOfPages":"215","costCenters":[],"links":[{"id":261650,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/confpub/70039525/report.pdf"},{"id":261651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/confpub/70039525/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e42fe4b0c8380cd46498","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":535338,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039552,"text":"70039552 - 1972 - U.S. Geological Survey National Center, Reston, Virginia","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039552","displayToPublicDate":"2008-01-07T13:04:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"U.S. Geological Survey National Center, Reston, Virginia","docAbstract":"In 1917 the Geological Survey moved into the newly built Interior Building near the White House in Washington, D. C. Twenty years later a larger building was constructed nearby to house the expanding U. S. Department of the Interior. Height restrictions reduced the planned size of the new building, and the Geological Survey was compelled to remain in the older Interior Building now identified as the General Services Administration Building. Expansion of the Survey's programs, and particularly the overall government need for additional office space in downtown Washington, has resulted in the Survey's activities being presently housed in 30 different buildings, at 17 widely scattered locations throughout the Washington Metropolitan Area.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039552","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, U.S. Geological Survey National Center, Reston, Virginia, 25 p., https://doi.org/10.3133/70039552.","productDescription":"25 p.","numberOfPages":"29","costCenters":[],"links":[{"id":261676,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039552/report.pdf"},{"id":261677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039552/report-thumb.jpg"}],"country":"United States","state":"Virginia","city":"Reston","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.36666666666666,38.95 ], [ -77.36666666666666,38.93333333333333 ], [ -77.35,38.93333333333333 ], [ -77.35,38.95 ], [ -77.36666666666666,38.95 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bba78e4b08c986b3281ba","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":535349,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010171,"text":"70010171 - 1972 - Middle pleistocene mollusks from St. Lawrence Island and their significance for the paleo-oceanography of the Bering Sea","interactions":[],"lastModifiedDate":"2025-07-11T16:07:00.57417","indexId":"70010171","displayToPublicDate":"2004-11-19T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Middle pleistocene mollusks from St. Lawrence Island and their significance for the paleo-oceanography of the Bering Sea","docAbstract":"<p>Drift, evidently of Illinoian age, was deposited on St. Lawrence Island at the margin of an ice cap that covered the highlands of the Chukotka Peninsula of Siberia and spread far eastward on the continental shelf of northern Bering Sea. Underlying the drift on the northwestward part of the island are mollusk-bearing beds deposited during the Kotzebuan Transgression.</p><p>A comparison of mollusk faunas from St. Lawrence Island, Chukotka Peninsula, and Kotzebue Sound suggests that the present northward flow through Bering and Anadyr Straits was reversed during the Kotzebuan Transgression. Cold arctic water penetrated southward and southwestward bringing an arctic fauna to the Gulf of Anadyr. Warmer Pacific water probably entered eastern Bering Sea, passed eastward and northeastward around eastern and northern St. Lawrence Island, and then became entrained in the southward currents that passed through Anadyr Strait.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0033-5894(72)90033-6","issn":"00335894","usgsCitation":"Hopkins, D., Rowland, R., and Patton, W.W., 1972, Middle pleistocene mollusks from St. Lawrence Island and their significance for the paleo-oceanography of the Bering Sea: Quaternary Research, v. 2, no. 2, p. 119-134, https://doi.org/10.1016/0033-5894(72)90033-6.","productDescription":"16 p.","startPage":"119","endPage":"134","costCenters":[],"links":[{"id":219670,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"St. Lawrence Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -172.62707116583636,\n              64.0488182952663\n            ],\n            [\n              -172.62707116583636,\n              62.80972983412474\n            ],\n            [\n              -168.38785991048877,\n              62.80972983412474\n            ],\n            [\n              -168.38785991048877,\n              64.0488182952663\n            ],\n            [\n              -172.62707116583636,\n              64.0488182952663\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"2","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505a56eae4b0c8380cd6d8f7","contributors":{"authors":[{"text":"Hopkins, D.M.","contributorId":103646,"corporation":false,"usgs":true,"family":"Hopkins","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":358193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowland, R.W.","contributorId":36153,"corporation":false,"usgs":true,"family":"Rowland","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":358192,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patton, W. W. Jr.","contributorId":11231,"corporation":false,"usgs":true,"family":"Patton","given":"W.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":358191,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70188907,"text":"70188907 - 1972 - An inventory of suspended sediment stations and type of data analysis for Pennsylvania streams, 1947-1970","interactions":[],"lastModifiedDate":"2017-07-12T15:17:55","indexId":"70188907","displayToPublicDate":"2000-03-11T00:00:00","publicationYear":"1972","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":"An inventory of suspended sediment stations and type of data analysis for Pennsylvania streams, 1947-1970","docAbstract":"<p>Data concerning suspended sediment concentrations and loads, frequency of occurrence of suspended sediment concentrations, and long-term trends of annual suspended sediment loads are important tools for today's environmental manager. These data are required background for those concerned with establishing and enforcing erosion and sedimentation control regulations and sediment concentration or turbidity standards for water-quality criteria, or those concerned with designing for adequate long-term water storage in reservoirs (sediment load), for efficient municipal and industrial plant operation (sediment concentration frequency), etc.<br></p><p>This is a compilation of the location, period of record, sampling frequency and type of data synthesis for suspended sediment carried by Pennsylvania streams. Figures 1 and 2 show the approximate locations of sediment sampling stations in Pennsylvania. All of the sediment data listed were collected by the U. S. Geological Survey mainly in cooperation with the following Federal, State, and local agencies.<br></p><p style=\"padding-left: 60px;\" data-mce-style=\"padding-left: 60px;\">Pennsylvania Department of Environmental Resources<br>&nbsp; &nbsp; &nbsp;Bureau of Engineering and Construction<br>&nbsp; &nbsp; &nbsp;Soil and Water Conservation Commission<br>Pennsylvania Department of Transportation<br>City of Philadelphia<br>Brandywine Valley Association<br>Delaware Geological Survey<br>Conestoga Valley Association<br>Lehigh County Soil and Water Conservation District<br>Corps of Engineers, U. S. Army</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, Pennsylvania","doi":"10.3133/70188907","usgsCitation":"Ott, A.N., and Commings, A.B., 1972, An inventory of suspended sediment stations and type of data analysis for Pennsylvania streams, 1947-1970: Open-File Report, ii, 24 p., https://doi.org/10.3133/70188907.","productDescription":"ii, 24 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":343746,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70188907/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":342968,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70188907/report-thumb.jpg"}],"country":"United 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,{"id":65715,"text":"i711 - 1972 - Geologic map of Yellowstone National Park","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i711","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1972","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":"711","subseriesTitle":"NONE","title":"Geologic map of Yellowstone National Park","language":"ENGLISH","doi":"10.3133/i711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Geologic map of Yellowstone National Park: U.S. Geological Survey IMAP 711, 1 map :col. ;87 x 86 cm. on sheet 98 x 104 cm. folded in envelope 31 x 24 cm., https://doi.org/10.3133/i711.","productDescription":"1 map :col. ;87 x 86 cm. on sheet 98 x 104 cm. folded in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":106926,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9475.htm","linkFileType":{"id":5,"text":"html"},"description":"9475"},{"id":189430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.16666666666667,44.13333333333333 ], [ -111.16666666666667,45.11666666666667 ], [ -109.8,45.11666666666667 ], [ -109.8,44.13333333333333 ], [ -111.16666666666667,44.13333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2b02","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":534087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70202873,"text":"70202873 - 1972 - Water quality at Miami International Airport, Miami, Florida, 1971–72","interactions":[],"lastModifiedDate":"2025-04-24T18:44:36.007127","indexId":"70202873","displayToPublicDate":"1994-04-01T14:44:18","publicationYear":"1972","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}},"seriesNumber":"FL 72-023","displayTitle":"Water quality at Miami International Airport, Miami, Florida, 1971–72","title":"Water quality at Miami International Airport, Miami, Florida, 1971–72","docAbstract":"<p>The quality of water, sediment, and biota was determined at four sites in canals and drainage ditches at Miami International Airport (MIA) during high- and low-water periods and during summer and winter 1971–72. Concentrations of common ions, such as calcium, sodium, chloride, and magnesium, tended to be above average for fresh water because of periodic salt-water intrusion. Nitrogen, phosphorus, and pesticides were in higher concentrations than typical for undisturbed areas of south Florida, but not higher than usual for the urban coastal area, so it is not known to what extent these chemicals are attributable to surrounding urbanization. Heavy metals, oil and grease, and PCB's (polychlorinated biphenyls) were the best indicators of the effects of MIA on water quality. Concentations of the above were quite variable, high values for each were recorded and were probably associated with recent discharges from industrial sources. Arsenic, lead, iron, and chromium all exceeded, in one or more samples, the U.S. Public Health Service's recommended upper limits for metals in water. Only iron normally exceeds these standards in the natural waters of south Florida. PCB's were detected in most samples and were in concentrations up to 1,000 micrograms per kilogram in fish. In addition to pesticides and PCB's, another group of persistant chlorinated compounds, PCN's (polychlorinated naphthalenes) were detected in water, sediment, and fish. This is the first known detection of these compounds in the environment.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70202873","usgsCitation":"Freiberger, H.J., and McPherson, B.F., 1972, Water quality at Miami International Airport, Miami, Florida, 1971–72: Open-File Report FL 72-023, 50 p., https://doi.org/10.3133/70202873.","productDescription":"50 p.","numberOfPages":"50","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":362649,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70202873/ofr72023.pdf","text":"Report","size":"1.28 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":362648,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70202873/coverthb.jpg"}],"contact":"<p><a href=\"https://www.usgs.gov/locations/st-petersburg-coastal-and-marine-science-center\" data-mce-href=\"https://www.usgs.gov/locations/st-petersburg-coastal-and-marine-science-center\">St. Petersburg Coastal and Marine Science Center</a><br>U.S. Geological Survey<br>600 4th Street South<br>St. Petersburg, FL 33701</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Sampling sites</li><li>Methods</li><li>Streamflow</li><li>Rainfall</li><li>Water quality</li><li>Summary and conclusions</li><li>References</li></ul>","publishedDate":"1972-10-01","noUsgsAuthors":false,"publicationDate":"1972-10-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Freiberger, Herbert J.","contributorId":84404,"corporation":false,"usgs":true,"family":"Freiberger","given":"Herbert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":760363,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McPherson, Benjamin F.","contributorId":17965,"corporation":false,"usgs":true,"family":"McPherson","given":"Benjamin","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":760364,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56496,"text":"wdrIN711 - 1972 - Water resources data for Indiana, water year 1971","interactions":[],"lastModifiedDate":"2014-06-11T10:28:04","indexId":"wdrIN711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IN-71-1","title":"Water resources data for Indiana, water year 1971","docAbstract":"Water resources data for the 1971 water year for Indiana, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, and records of water-quality data on the chemical and physical characteristics of surface water are given in this report. Records for a few pertinent gaging and water-quality stations in bordering States also are included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of J. L. Cook, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Indiana.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrIN711","collaboration":"Prepared in cooperation with Indiana Department of Natural Resources; Indiana State Board of Health; Indiana State Highway Commission; Corps of Engineers, U.S. Army","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Indiana, water year 1971: U.S. Geological Survey Water Data Report IN-71-1, xi, 355 p., https://doi.org/10.3133/wdrIN711.","productDescription":"xi, 355 p.","numberOfPages":"371","temporalStart":"1970-10-01","temporalEnd":"1971-09-30","costCenters":[],"links":[{"id":288288,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288287,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/in-71-1/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6cd3","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":532677,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6121,"text":"pp708 - 1972 - Ground-Water Hydraulics","interactions":[],"lastModifiedDate":"2012-02-02T00:05:56","indexId":"pp708","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"708","title":"Ground-Water Hydraulics","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp708","usgsCitation":"Lohman, S.W., 1972, Ground-Water Hydraulics: U.S. Geological Survey Professional Paper 708, Report: viii, 70 p.; 9 Plates, https://doi.org/10.3133/pp708.","productDescription":"Report: viii, 70 p.; 9 Plates","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":117745,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0708/report-thumb.jpg"},{"id":22065,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0708/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33180,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0708/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33181,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0708/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33182,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0708/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33183,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0708/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33184,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0708/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33185,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0708/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33186,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0708/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33187,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0708/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33188,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0708/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69902e","contributors":{"authors":[{"text":"Lohman, Stanley William","contributorId":53361,"corporation":false,"usgs":true,"family":"Lohman","given":"Stanley","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":152153,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56574,"text":"wdrKS712 - 1972 - Water resources data for Kansas, water year 1971; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2018-11-05T15:16:33","indexId":"wdrKS712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"KS-71-2","title":"Water resources data for Kansas, water year 1971; Part 2, Water quality records","docAbstract":"<p>Water-resources data for the 1971 water year for Kansas include records of data for the chemical and physical characteristics of surface and ground water. Data on the quality of surface water (chemical, microbiological, temperature, and sediment) were collected from designated sampling sites at predetermined intervals such as once daily, weekly, monthly, or less frequently. Records are given for 66 sampling stations of which 9 are partial-record stations, and 52 are miscellaneous sites. Records of chemical analyses are given for 46 ground-water sites. Locations of surface water-quality stations are shown in Figure 1, page 2. Records for pertinent water-quality stations in bordering States are also included. The records were collected by the Water Resources Division of the U.S. Geological Survey under the direction of C. W. Lane, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Kansas.</p><p>The Geological Survey has published records of chemical quality, suspended sediment, and water temperatures since 1941 in annual series of water-supply papers entitled, \"Quality of Surface Waters of the United States.\" Beginning with the 1964 water year, water-quality records also have been released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these reports is limited; they are designed primarily for rapid release of data shortly after the end of the water year to meet local needs. These records will be published later in Geological Survey water-supply papers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrKS712","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Kansas, water year 1971; Part 2, Water quality records: U.S. Geological Survey Water Data Report KS-71-2, v, 140 p., https://doi.org/10.3133/wdrKS712.","productDescription":"v, 140 p.","numberOfPages":"150","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":181590,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/ks-71-2/report-thumb.jpg"},{"id":359195,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/ks-71-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":56576,"text":"wdrPA712 - 1972 - Water resources data for Pennsylvania, water year 1971; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2020-12-31T22:22:04.056302","indexId":"wdrPA712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"PA-71-2","title":"Water resources data for Pennsylvania, water year 1971; Part 2, Water quality records","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrPA712","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Pennsylvania, water year 1971; Part 2, Water quality records: U.S. Geological Survey Water Data Report 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,{"id":3150,"text":"wsp2015 - 1972 - Quality of surface waters of the United States, 1967, Parts 9-11, Colorado River basin to Pacific Slope basin in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp2015","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2015","title":"Quality of surface waters of the United States, 1967, Parts 9-11, Colorado River basin to Pacific Slope basin in California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2015","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Quality of surface waters of the United States, 1967, Parts 9-11, Colorado River basin to Pacific Slope basin in California: U.S. Geological Survey Water Supply Paper 2015, xv, 702 p. :ill. ;23 cm., https://doi.org/10.3133/wsp2015.","productDescription":"xv, 702 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":138883,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2015/report-thumb.jpg"},{"id":30098,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2015/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6519b3","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":528108,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23460,"text":"ofr72191 - 1972 - Radiochemical analyses of surface water from U.S. Geological Survey hydrologic bench-mark stations","interactions":[],"lastModifiedDate":"2017-09-04T11:41:15","indexId":"ofr72191","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-191","title":"Radiochemical analyses of surface water from U.S. Geological Survey hydrologic bench-mark stations","docAbstract":"<p>The U.S. Geological Survey's program for collecting and analyzing surface-water samples for radiochemical constituents at hydrologic bench-mark stations is described. Analytical methods used during the study are described briefly and data obtained from 55 of the network stations in the United States during the period from 1967 to 1971 are given in tabular form.</p><p>Concentration values are reported for dissolved uranium, radium, gross alpha and gross beta radioactivity. Values are also given for suspended gross alpha radioactivity in terms of natural uranium. Suspended gross beta radioactivity is expressed both as the equilibrium mixture of strontium-90/yttrium-90 and as cesium-137.</p><p>Other physical parameters reported which describe the samples include the concentrations of dissolved and suspended solids, the water temperature and stream discharge at the time of the sample collection.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72191","issn":"0094-9140","usgsCitation":"Janzer, V., and Saindon, L., 1972, Radiochemical analyses of surface water from U.S. Geological Survey hydrologic bench-mark stations: U.S. Geological Survey Open-File Report 72-191, 41 p., https://doi.org/10.3133/ofr72191.","productDescription":"41 p.","numberOfPages":"44","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":156794,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0191/report-thumb.jpg"},{"id":113005,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0191/report.pdf","size":"1482","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649c73","contributors":{"authors":[{"text":"Janzer, V.J.","contributorId":31777,"corporation":false,"usgs":true,"family":"Janzer","given":"V.J.","affiliations":[],"preferred":false,"id":190144,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saindon, L.G.","contributorId":103281,"corporation":false,"usgs":false,"family":"Saindon","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":190145,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24148,"text":"ofr72294 - 1972 - Digest of the catalog of information on water data","interactions":[],"lastModifiedDate":"2012-02-02T00:08:02","indexId":"ofr72294","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-294","title":"Digest of the catalog of information on water data","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, Office of Water Data Coordination,","doi":"10.3133/ofr72294","issn":"0094-9140","usgsCitation":"Pauszek, F.H., 1972, Digest of the catalog of information on water data: U.S. Geological Survey Open-File Report 72-294, vii, 70 p. :ill., maps ;26 cm., https://doi.org/10.3133/ofr72294.","productDescription":"vii, 70 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":155936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611b22","contributors":{"authors":[{"text":"Pauszek, F. H.","contributorId":61399,"corporation":false,"usgs":true,"family":"Pauszek","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":191404,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23465,"text":"ofr72192 - 1972 - Stream depletion factors, Arkansas River valley, southeastern Colorado; A basis for evaluating plans for conjunctive use of ground and surface water","interactions":[],"lastModifiedDate":"2019-02-06T13:25:21","indexId":"ofr72192","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-192","title":"Stream depletion factors, Arkansas River valley, southeastern Colorado; A basis for evaluating plans for conjunctive use of ground and surface water","docAbstract":"<p>The Arkansas River valley is a stream-aquifer system that consists of the Arkansas River and the associated valley-fill deposits. The hydrology, geology, and water-resources development in the valley have been described by Moore and Wood (1967). The history of delivery of irrigation water by canals indicates that the supply has been inadequate during some seasons and some years. The shortage can be reduced by carefully designed conjunctive use of ground and surface water. An analog model of the Arkansas River valley in Colorado was constructed to facilitate such designs (Moore and Wood, 1967).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72192","issn":"0094-9140","usgsCitation":"Jenkins, C., and Taylor, O., 1972, Stream depletion factors, Arkansas River valley, southeastern Colorado; A basis for evaluating plans for conjunctive use of ground and surface water: U.S. Geological Survey Open-File Report 72-192, Report: ii, 8 p.; 4 Plates: 40.92 x 22.26 inches or smaller, https://doi.org/10.3133/ofr72192.","productDescription":"Report: ii, 8 p.; 4 Plates: 40.92 x 22.26 inches or smaller","costCenters":[],"links":[{"id":52776,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0192/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0192/report-thumb.jpg"},{"id":52777,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0192/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52778,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0192/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52779,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0192/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52780,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0192/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Arkansas River Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-102.7445,37.6428],[-103.0766,37.6417],[-103.183,37.6424],[-103.2917,37.6426],[-103.4039,37.6423],[-103.5092,37.6432],[-103.5778,37.6432],[-103.6016,37.6437],[-103.8109,37.644],[-103.8929,37.644],[-103.9661,37.6439],[-104.0591,37.6436],[-104.0597,37.7316],[-104.3518,37.8148],[-104.3889,37.8248],[-104.4978,37.8556],[-104.6074,37.886],[-104.6527,37.8982],[-104.7175,37.8949],[-104.9375,37.8834],[-104.9545,37.8822],[-104.9737,37.881],[-105.0017,37.8794],[-105.0041,37.8794],[-105.0093,37.879],[-105.0122,37.8799],[-105.0209,37.8859],[-105.0313,37.8919],[-105.0295,37.8964],[-105.03,37.9],[-105.0346,37.9055],[-105.0468,37.9115],[-105.0474,37.9967],[-105.0481,38.0855],[-105.0481,38.173],[-105.0483,38.202],[-105.0487,38.2582],[-104.9391,38.2587],[-104.9402,38.3448],[-104.9392,38.4178],[-104.939,38.43],[-104.9397,38.5003],[-104.9427,38.5003],[-104.943,38.5175],[-104.8295,38.5183],[-104.736,38.5183],[-104.7171,38.5186],[-104.6071,38.5187],[-104.4971,38.5192],[-104.3759,38.52],[-104.2836,38.5201],[-104.2794,38.5205],[-104.2759,38.5204],[-104.1629,38.5215],[-104.054,38.523],[-103.9411,38.523],[-103.8328,38.523],[-103.7228,38.5223],[-103.6116,38.5225],[-103.6118,38.5171],[-103.5089,38.5159],[-103.508,38.4366],[-103.5066,38.3409],[-103.5019,38.3408],[-103.5004,38.2646],[-103.3972,38.2647],[-103.2787,38.2649],[-103.1691,38.2647],[-103.0571,38.2647],[-102.741,38.2654],[-102.6154,38.2661],[-102.5075,38.2662],[-102.396,38.2662],[-102.2858,38.2665],[-102.1749,38.2668],[-102.0443,38.2676],[-102.0443,38.2627],[-102.0432,37.7384],[-102.043,37.6429],[-102.089,37.643],[-102.199,37.6429],[-102.3071,37.6435],[-102.4182,37.6432],[-102.5281,37.6432],[-102.6363,37.6435],[-102.7445,37.6428]]]},\"properties\":{\"name\":\"Bent\",\"state\":\"CO\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a52cf","contributors":{"authors":[{"text":"Jenkins, C.T.","contributorId":106099,"corporation":false,"usgs":true,"family":"Jenkins","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":190153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, O.J.","contributorId":71584,"corporation":false,"usgs":true,"family":"Taylor","given":"O.J.","email":"","affiliations":[],"preferred":false,"id":190152,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2665,"text":"wsp1663H - 1972 - Origin of mineralized water in Precambrian rocks of the Upper Paraiba Basin, Paraiba, Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1663H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1663","chapter":"H","title":"Origin of mineralized water in Precambrian rocks of the Upper Paraiba Basin, Paraiba, Brazil","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1663H","usgsCitation":"Schoff, S., 1972, Origin of mineralized water in Precambrian rocks of the Upper Paraiba Basin, Paraiba, Brazil: U.S. Geological Survey Water Supply Paper 1663, iv, H1-H38 p. :maps (1 fold. in pocket) ;24 cm., https://doi.org/10.3133/wsp1663H.","productDescription":"iv, H1-H38 p. :maps (1 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":138231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1663h/report-thumb.jpg"},{"id":29005,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1663h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29006,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1663h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a62d","contributors":{"authors":[{"text":"Schoff, Stuart L.","contributorId":104467,"corporation":false,"usgs":true,"family":"Schoff","given":"Stuart L.","affiliations":[],"preferred":false,"id":145577,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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