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,{"id":70195900,"text":"70195900 - 1980 - Ground-water data for Billings, Golden Valley, and Slope Counties, North Dakota","interactions":[],"lastModifiedDate":"2018-03-07T13:45:55","indexId":"70195900","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5645,"text":"North Dakota Geological Survey Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"72","title":"Ground-water data for Billings, Golden Valley, and Slope Counties, North Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"North Dakota Geological Survey; North Dakota State Water Commission","usgsCitation":"Anna, L.O., 1980, Ground-water data for Billings, Golden Valley, and Slope Counties, North Dakota: North Dakota Geological Survey Bulletin 72, 241 p.","productDescription":"241 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352293,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publicComments":"North Dakota State Water Commission County Ground-Water Studies 29, pt. II, and North Dakota Geological Survey Bulletin 72, pt. II","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff476ce4b0da30c1bfdb71","contributors":{"authors":[{"text":"Anna, L. O.","contributorId":65472,"corporation":false,"usgs":true,"family":"Anna","given":"L.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":730421,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012329,"text":"70012329 - 1980 - Rate of mercury loss from contaminated estuarine sediments","interactions":[],"lastModifiedDate":"2017-12-14T16:35:31","indexId":"70012329","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Rate of mercury loss from contaminated estuarine sediments","docAbstract":"<p>The concentration of mercury in contaminated estuarine sediments of Bellingham Bay, Washington was found to decrease with a half-time of about 1.3 yr after the primary anthropogenic source of mercury was removed. <i>In situ</i> measurements of the mercury flux from sediments, in both dissolved and volatile forms, could not account for this decrease. This result suggests that the removal of mercury is associated with sediment particles transported out of the study area. This decrease was modeled using a steady-state mixing model.</p><p>Mercury concentrations in anoxic interstitial waters reached 3.5 μg/l, 126 times higher than observed in the overlying seawater. Mercury fluxes from these sediments ranged from 1.2 to 2.8 × 10<sup>−5</sup> ng/cm<sup>2</sup>/sec, all in a soluble form. In general, higher Hg fluxes were associated with low oxygen or reducing conditions in the overlying seawater. In contrast, no flux was measurable from oxidizing interstitial water having mercury concentrations of 0.01-0.06 μ/l.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(80)90137-4","issn":"00167037","usgsCitation":"Bothner, M., Jahnke, R., Peterson, M.L., and Carpenter, R., 1980, Rate of mercury loss from contaminated estuarine sediments: Geochimica et Cosmochimica Acta, v. 44, no. 2, p. 273-285, https://doi.org/10.1016/0016-7037(80)90137-4.","productDescription":"13 p.","startPage":"273","endPage":"285","costCenters":[],"links":[{"id":222132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9537e4b0c8380cd81892","contributors":{"authors":[{"text":"Bothner, Michael H. mbothner@usgs.gov","contributorId":139855,"corporation":false,"usgs":true,"family":"Bothner","given":"Michael H.","email":"mbothner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":363292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jahnke, R.A.","contributorId":33060,"corporation":false,"usgs":true,"family":"Jahnke","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":363290,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peterson, M. L.","contributorId":49930,"corporation":false,"usgs":false,"family":"Peterson","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":363291,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Carpenter, R.","contributorId":94793,"corporation":false,"usgs":true,"family":"Carpenter","given":"R.","affiliations":[],"preferred":false,"id":363293,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012256,"text":"70012256 - 1980 - A model to forecast short-term snowmelt runoff using synoptic observations of streamflow, temperature, and precipitation","interactions":[],"lastModifiedDate":"2018-02-05T12:29:02","indexId":"70012256","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"A model to forecast short-term snowmelt runoff using synoptic observations of streamflow, temperature, and precipitation","docAbstract":"<p><span>Snowmelt runoff is forecast with a statistical model that utilizes daily values of stream discharge, gaged precipitation, and maximum and minimum observations of air temperature. Synoptic observations of these variables are made at existing low- and medium-altitude weather stations, thus eliminating the difficulties and expense of new, high-altitude installations. Four model development steps are used to demonstrate the influence on prediction accuracy of basin storage, a preforecast test season, air temperature (to estimate ablation), and a prediction based on storage. Daily ablation is determined by a technique that employs both mean temperature and a radiative index. Radiation (both long- and short-wave components) is approximated by using the range in daily temperature, which is shown to be closely related to mean cloud cover. A technique based on the relationship between prediction error and prediction season weather utilizes short-term forecasts of precipitation and temperature to improve the final prediction. Verification of the model is accomplished by a split sampling technique for the 1960–1977 period. Short- term (5–15 days) predictions of runoff throughout the main snowmelt season are demonstrated for mountain drainages in western Washington, south-central Arizona, western Montana, and central California. The coefficient of prediction (</span><i>C</i><sub><i>p</i></sub><span>) based on actual, short-term predictions for 18 years is for Thunder Creek (Washington), 0.69; for South Fork Flathead River (Montana), 0.45; for the Black River (Arizona), 0.80; and for the Kings River (California), 0.80.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR016i004p00778","usgsCitation":"Tangborn, W.V., 1980, A model to forecast short-term snowmelt runoff using synoptic observations of streamflow, temperature, and precipitation: Water Resources Research, v. 16, no. 4, p. 778-786, https://doi.org/10.1029/WR016i004p00778.","productDescription":"9 p.","startPage":"778","endPage":"786","costCenters":[],"links":[{"id":222062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5059e482e4b0c8380cd46694","contributors":{"authors":[{"text":"Tangborn, Wendell V.","contributorId":32152,"corporation":false,"usgs":true,"family":"Tangborn","given":"Wendell","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":363107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012331,"text":"70012331 - 1980 - Gas and hydrogen isotopic analyses of volcanic eruption clouds in Guatemala sampled by aircraft","interactions":[],"lastModifiedDate":"2012-03-12T17:19:02","indexId":"70012331","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Gas and hydrogen isotopic analyses of volcanic eruption clouds in Guatemala sampled by aircraft","docAbstract":"Gas samples were collected by aircraft entering volcanic eruption clouds of three Guatemalan volcanoes. Gas chromatographic analyses show higher H2 and S gas contents in ash eruption clouds and lower H2 and S gases in vaporous gas plumes. H isotopic data demonstrate lighter isotopic distribution of water vapor in ash eruption clouds than in vaporous gas plumes. Most of the H2O in the vaporous plumes is probably meteoric. The data are the first direct gas analyses of explosive eruptive clouds, and demonstrate that, in spite of atmospheric admixture, useful compositional information on eruptive gases can be obtained using aircraft. ?? 1980.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Rose, W., Cadle, R., Heidt, L., Friedman, I., Lazrus, A., and Huebert, B., 1980, Gas and hydrogen isotopic analyses of volcanic eruption clouds in Guatemala sampled by aircraft: Journal of Volcanology and Geothermal Research, v. 7, no. 1-2, p. 1-10.","startPage":"1","endPage":"10","numberOfPages":"10","costCenters":[],"links":[{"id":222190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14bfe4b0c8380cd54b4b","contributors":{"authors":[{"text":"Rose, W.I. Jr.","contributorId":25275,"corporation":false,"usgs":true,"family":"Rose","given":"W.I.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":363298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cadle, R.D.","contributorId":64804,"corporation":false,"usgs":true,"family":"Cadle","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":363300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heidt, L.E.","contributorId":61168,"corporation":false,"usgs":true,"family":"Heidt","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":363299,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":363302,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lazrus, A.L.","contributorId":92426,"corporation":false,"usgs":true,"family":"Lazrus","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":363301,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Huebert, B.J.","contributorId":6189,"corporation":false,"usgs":true,"family":"Huebert","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":363297,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70012083,"text":"70012083 - 1980 - Impact of horse traffic on trails in Rocky Mountain National Park.","interactions":[],"lastModifiedDate":"2013-03-15T20:50:39","indexId":"70012083","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2456,"text":"Journal of Soil and Water Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Impact of horse traffic on trails in Rocky Mountain National Park.","docAbstract":"Disturbances related to the impact of horses on trails in Rocky Mountain National Park vary across the landscape. Geomorphic monitoring of permanent sites suggests that horse traffic is not the single, dominant process active on trails, nor is degredation always a direct result of horse use. Instead, amounts and rates of change are a function of geomorphic and biologic characteristics of the terrain interacting with horse traffic of varying degrees. The most influential landscape factors governing trail deteriortion, rockiness, stoniness, vegetation, and drainage. - from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Soil and Water Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Soil and Water Conservation Society","usgsCitation":"Summer, R., 1980, Impact of horse traffic on trails in Rocky Mountain National Park.: Journal of Soil and Water Conservation, v. 35, no. 2, p. 85-87.","startPage":"85","endPage":"87","numberOfPages":"3","costCenters":[],"links":[{"id":222636,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a38bee4b0c8380cd61690","contributors":{"authors":[{"text":"Summer, R.M.","contributorId":56800,"corporation":false,"usgs":true,"family":"Summer","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":362687,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012355,"text":"70012355 - 1980 - Nearshore current pattern off south Texas: an interpretation from aerial photographs.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:07","indexId":"70012355","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"Nearshore current pattern off south Texas: an interpretation from aerial photographs.","docAbstract":"Current patterns in a 4-km-wide zone along the south Texas coast were interpreted from patterns of water turbidity visible in aerial photographs taken during a winter day of moderate northerly winds. Features of the turbidity pattern remained recognizable on photographs taken 25 min apart. Currents measured from the movements of these features were southward and nearly parallel to shore, increasing from about 17 cm/sec in an offshore zone to about 40 cm/sec at the line of breaking waves. - from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Remote Sensing of Environment","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0034-4257(80)90010-3","issn":"00344257","usgsCitation":"Hunter, R.E., and Hill, G.W., 1980, Nearshore current pattern off south Texas: an interpretation from aerial photographs.: Remote Sensing of Environment, v. 10, no. 2, p. 115-134, https://doi.org/10.1016/0034-4257(80)90010-3.","startPage":"115","endPage":"134","numberOfPages":"20","costCenters":[],"links":[{"id":205170,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0034-4257(80)90010-3"},{"id":221945,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6414e4b0c8380cd7287b","contributors":{"authors":[{"text":"Hunter, R. E.","contributorId":48148,"corporation":false,"usgs":true,"family":"Hunter","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":363349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, G. W.","contributorId":85551,"corporation":false,"usgs":true,"family":"Hill","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":363350,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012188,"text":"70012188 - 1980 - The mass balance approach: application to interpreting the chemical evolution of hydrologic systems","interactions":[],"lastModifiedDate":"2019-12-06T07:08:14","indexId":"70012188","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"The mass balance approach: application to interpreting the chemical evolution of hydrologic systems","docAbstract":"<p>Mass balance calculations are applied to observed chemical and isotopic data of three natural water systems involving carbonate reactions in order to define mineral stoichiometry of reactants and products, relative rates of reactions, and mass transfer. One study evaluates reactions in a lagoon on the east coast of the Yucatan Peninsula, Mexico.</p>","language":"English","publisher":"ASJ","doi":"10.2475/ajs.280.2.130","issn":"00029599","usgsCitation":"Plummer, N., and Back, W., 1980, The mass balance approach: application to interpreting the chemical evolution of hydrologic systems: American Journal of Science, v. 280, no. 2, p. 130-142, https://doi.org/10.2475/ajs.280.2.130.","productDescription":"13 p. ","startPage":"130","endPage":"142","numberOfPages":"13","costCenters":[],"links":[{"id":488827,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2475/ajs.280.2.130","text":"Publisher Index Page"},{"id":222059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico ","otherGeospatial":"Yucatan Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.62597656249999,\n              18.114529138838503\n            ],\n            [\n              -86.429443359375,\n              18.114529138838503\n            ],\n            [\n              -86.429443359375,\n              22.471954507739227\n            ],\n            [\n              -91.62597656249999,\n              22.471954507739227\n            ],\n            [\n              -91.62597656249999,\n              18.114529138838503\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"280","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505badbee4b08c986b323dc6","contributors":{"authors":[{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":362957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Back, W.","contributorId":33839,"corporation":false,"usgs":true,"family":"Back","given":"W.","email":"","affiliations":[],"preferred":false,"id":362956,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010385,"text":"70010385 - 1980 - The age curves of sulfur and oxygen isotopes in marine sulfate and their mutual interpretation","interactions":[],"lastModifiedDate":"2014-08-19T11:33:04","indexId":"70010385","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"The age curves of sulfur and oxygen isotopes in marine sulfate and their mutual interpretation","docAbstract":"Three hundred new samples of marine evaporite sulfate, of world-wide distribution, were analyzed for δ<sup>34</sup>S, and 60 of these also for δ<sup>18</sup>O in the sulfate ion. Detailed δ<sup>34</sup>S age curves for Tertiary—Cretaceous, Permian—Pennsylvanian, Devonian, Cambrian and Proterozoic times document large variations in δ<sup>34</sup>S. A summary curve forδ<sup>18</sup>O also shows definite variations, some at different times than δ<sup>34</sup>S, and always smaller. The measured δ<sup>34</sup>S and δ<sup>18</sup>O correspond to variations in these isotopes in sulfate of the world ocean surface. The variations of δ<sup>18</sup>O are controlled by input and output fluxes of sulfur in the ocean, three of which are the same that control δ<sup>34</sup>S: deposition and erosion of sulfate, and deposition of sulfide. Erosion of sulfide differs in its effect on the S and O systems. δ<sup>18</sup>O in the sulfate does not seem to be measurably affected by equilibration with either seawater or with subsurface waters after crystallization. In principle, the simultaneous application of both δ<sup>34</sup>S and δ<sup>18</sup>O age curves should help reduce the number of assumptions in calculations of the cycles of sulfur and oxygen through geological time, and a new model involving symmetrical fluxes is introduced here to take advantage of the oxygen data. However, all previously published models as well as this one lead to anomalies, such as unreasonable calcium or oxygen depletions in the ocean—atmosphere system. In addition, most models are incapable of reproducing the sharp rises of the δ<sup>34</sup>S curve in the late Proterozoic, the Devonian and the Triassic which would be the result of unreasonably fast net sulfide deposition. This fast depletion could result from an ocean that has not always been mixed (as previously assumed in all model calculations).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"New York, NY","doi":"10.1016/0009-2541(80)90047-9","issn":"00092541","usgsCitation":"Claypool, G.E., Holser, W.T., Kaplan, I.R., Sakai, H., and Zak, I., 1980, The age curves of sulfur and oxygen isotopes in marine sulfate and their mutual interpretation: Chemical Geology, v. 28, no. C, p. 199-260, https://doi.org/10.1016/0009-2541(80)90047-9.","productDescription":"62 p.","startPage":"199","endPage":"260","numberOfPages":"62","costCenters":[],"links":[{"id":218864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266126,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(80)90047-9"}],"volume":"28","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba9ade4b08c986b32241d","contributors":{"authors":[{"text":"Claypool, George E.","contributorId":76312,"corporation":false,"usgs":true,"family":"Claypool","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":358802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holser, William T.","contributorId":12131,"corporation":false,"usgs":true,"family":"Holser","given":"William","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":358799,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaplan, Isaac R.","contributorId":8218,"corporation":false,"usgs":true,"family":"Kaplan","given":"Isaac","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":358798,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sakai, Hitoshi","contributorId":30639,"corporation":false,"usgs":true,"family":"Sakai","given":"Hitoshi","email":"","affiliations":[],"preferred":false,"id":358800,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zak, Israel","contributorId":48697,"corporation":false,"usgs":true,"family":"Zak","given":"Israel","email":"","affiliations":[],"preferred":false,"id":358801,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70012372,"text":"70012372 - 1980 - Geologic history of Grecian Rocks, Key Largo Coral Reef Marine Sanctuary.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:01","indexId":"70012372","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1106,"text":"Bulletin of Marine Science","active":true,"publicationSubtype":{"id":10}},"title":"Geologic history of Grecian Rocks, Key Largo Coral Reef Marine Sanctuary.","docAbstract":"Two transects were drilled across the major ecologic zones of the c. 750 by 200 m reef, whose accumulation was controlled by a local Pleistocene topographic feature. The Reef is composed of 5 major ecologic zones: 1) a deep seaward rubble zone, 6-8 m depth; 2) a poorly developed spur and groove zone composed of massive head corals and Millepora (4-6 m water depth); 3) a characteristic high-energy oriented Acropora palmata zone extending from the surface down to 4 m; 4) a distinct broad reef flat composed of in situ A. palmata and coral rubble, followed by 5) a narrow low- energy back-reef zone of unoriented A. palmata, thickets of A. cervicornis, and various massive head corals in water 0-3 m deep. An extensive grass-covered carbonate sand flat 3-4 m deep extends in a landward direction from zone 5. - from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Marine Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00074977","usgsCitation":"Shinn, E., 1980, Geologic history of Grecian Rocks, Key Largo Coral Reef Marine Sanctuary.: Bulletin of Marine Science, v. 30, no. 3, p. 646-656.","startPage":"646","endPage":"656","numberOfPages":"11","costCenters":[],"links":[{"id":222250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a197be4b0c8380cd559dd","contributors":{"authors":[{"text":"Shinn, E.A.","contributorId":38610,"corporation":false,"usgs":true,"family":"Shinn","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":363400,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012183,"text":"70012183 - 1980 - Chemical mass-wasting of the northern Yucatan Peninsula by groundwater dissolution","interactions":[],"lastModifiedDate":"2019-12-06T07:10:02","indexId":"70012183","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Chemical mass-wasting of the northern Yucatan Peninsula by groundwater dissolution","docAbstract":"<p>The northern part of the Yucatan Peninsula is a relatively flat, low-lying carbonate terrane with no geomorphic expressions of stream channels. It is estimated that mean annual recharge to the groundwater system is 150 mm. For the 65,500 km<sup>2</sup><span>&nbsp;</span>study area, mean annual discharge (equivalent to recharge) is 9.8 × 10<sup>9</sup><span>&nbsp;</span>m<sup>3</sup>, or 8.6 × 10<sup>6</sup><span>&nbsp;</span>m<sup>3</sup><span>&nbsp;</span>for each 1 km of the 1,100-km-long coastline. In the interior of the peninsula, the recharging water annually dissolves about 37.5 t (metric tons) of calcite per 1 km<sup>2</sup>. When the groundwater has become saturated with calcite, little additional water-rock interaction occurs until the active mixing (dispersion) zone is reached near the coastline.</p><p>Theoretical calculations and laboratory experiments have shown that when two waters, each calcite saturated and with different salinities, are mixed, the resulting solution generally becomes undersaturated with calcite and, therefore, is capable of dissolving additional calcite. On the basis of our study of the Xel Ha lagoon on the east coast of Yucatan, we calculate that as much as 1.2 mmol/L additional calcite can be dissolved in the brackish groundwater zone of dispersion. This indicates that if the total solution potential of the amount of water discharging at Xel Ha has focused within the lagoon area, the lagoon could be chemically incised in less than 3,000 yr. We postulate that chemical mass wasting by dissolution in the zone of groundwater mixing is an important geomorphic process in coastal areas of limestone terranes.</p>","language":"English","publisher":"GeoScienceWorld","doi":"10.1130/0091-7613(1980)8<222:CMOTNY>2.0.CO;2","issn":"00917613","usgsCitation":"Hanshaw, B., and Back, W., 1980, Chemical mass-wasting of the northern Yucatan Peninsula by groundwater dissolution: Geology, v. 8, no. 5, p. 222-224, https://doi.org/10.1130/0091-7613(1980)8<222:CMOTNY>2.0.CO;2.","productDescription":"3 p. ","startPage":"222","endPage":"224","numberOfPages":"3","costCenters":[],"links":[{"id":221996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico ","otherGeospatial":"Yucatan Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.62597656249999,\n              18.114529138838503\n            ],\n            [\n              -86.429443359375,\n              18.114529138838503\n            ],\n            [\n              -86.429443359375,\n              22.471954507739227\n            ],\n            [\n              -91.62597656249999,\n              22.471954507739227\n            ],\n            [\n              -91.62597656249999,\n              18.114529138838503\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f57fe4b0c8380cd4c272","contributors":{"authors":[{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":362942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Back, W.","contributorId":33839,"corporation":false,"usgs":true,"family":"Back","given":"W.","email":"","affiliations":[],"preferred":false,"id":362943,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012113,"text":"70012113 - 1980 - About forty last-glacial Lake Missoula jokulhlaups through southern Washington","interactions":[],"lastModifiedDate":"2024-04-26T16:14:48.885907","indexId":"70012113","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2309,"text":"Journal of Geology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"About forty last-glacial Lake Missoula jökulhlaups through southern Washington","title":"About forty last-glacial Lake Missoula jokulhlaups through southern Washington","docAbstract":"<p><span>The rhythmic Touchet Beds in the Walla Walla and lower Yakima valleys resulted from many separate backfloodings by hydraulically ponded glacial Lake Missoula water. At least once this episodic lake briefly contained half the&nbsp;</span><span class=\"NLM_tex-math\"><img src=\"https://www.journals.uchicago.edu/na101/home/literatum/publisher/uchicago/journals/content/jg/1980/i30063875/628553/20180625/images/eqs/eq-00001.gif\" alt=\"\" data-mce-src=\"https://www.journals.uchicago.edu/na101/home/literatum/publisher/uchicago/journals/content/jg/1980/i30063875/628553/20180625/images/eqs/eq-00001.gif\"></span><span>&nbsp;of water that catastrophically drained the largest glacial Lakes Missoula. Evidence that the Touchet Beds rhythmites originated from brief backfloodings includes up-valley thinning and fining of locally derived bedload, upvalley paleocurrents, and upvalley transport of erratics derived from Cordilleran ice. Evidence that a lengthy nonflood environment followed the emplacement of each of about 40 Touchet Beds rhythmite includes inferred eolian and slopewash sediment overlying many rhythmites, uncontaminated Mount St. Helens \"set S\" tephra couplet atop one rhythmite as much as 220 m below the maximum level of backflooding, filled semiconsolidated rodent burrows throughout the 30 m of the thickest section, and dispersed skeletons of mammals. The lack of weathering or soil within the Touchet Beds suggests that all rhythmites are late Wisconsin. Bottom sediment of glacial Lake Missoula in Montana consists of rhythmites each interpreted as the record of a gradually deepening lake. Forty superposed rhythmites record about 40 late-Wisconsin fillings and emptyings of glacial Lake Missoula. The complementary records of about 40 separate glacial Lakes Missoula and about 40 great floods in southern Washington and in the Willamette Valley, Oregon indicate that the Missoula floods were great jokulhlaups. The last several floods were smaller than earlier ones because the controlling dam of Cordilleran ice thinned during deglaciation.</span></p>","language":"English","publisher":"University of Chicago Press","doi":"10.1086/628553","issn":"00221376","usgsCitation":"Waitt, R.B., 1980, About forty last-glacial Lake Missoula jokulhlaups through southern Washington: Journal of Geology, v. 88, no. 6, p. 653-679, https://doi.org/10.1086/628553.","productDescription":"27 p.","startPage":"653","endPage":"679","numberOfPages":"27","costCenters":[],"links":[{"id":222051,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e644e4b0c8380cd472d5","contributors":{"authors":[{"text":"Waitt, R. B. Jr.","contributorId":48558,"corporation":false,"usgs":true,"family":"Waitt","given":"R.","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":362762,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70140583,"text":"70140583 - 1980 - Plant stress detection by remote measurement of fluorescence","interactions":[],"lastModifiedDate":"2017-01-18T15:04:56","indexId":"70140583","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3868,"text":"Applied Optics","active":true,"publicationSubtype":{"id":10}},"title":"Plant stress detection by remote measurement of fluorescence","docAbstract":"<p><span>Chlorophyll fluorescence of mature lemon trees was measured with a Fraunhofer line discriminator (FLD). An increase in fluorescence was correlated with plant water stress as measured by stomatal resistance and twig water potential.</span></p>","language":"English","publisher":"The Optical Society","doi":"10.1364/AO.19.003287","usgsCitation":"McFarlane, J.C., Watson, R.D., Theisen, A.F., Jackson, R.D., Ehrler, W.L., Pinter, P.J., Idso, S.B., and Reginato, R.J., 1980, Plant stress detection by remote measurement of fluorescence: Applied Optics, v. 19, p. 3287-3289, https://doi.org/10.1364/AO.19.003287.","productDescription":"3 p.","startPage":"3287","endPage":"3289","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":297865,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","noUsgsAuthors":false,"publicationDate":"1980-10-01","publicationStatus":"PW","scienceBaseUri":"54dd2c26e4b08de9379b3664","contributors":{"authors":[{"text":"McFarlane, J. C.","contributorId":139140,"corporation":false,"usgs":false,"family":"McFarlane","given":"J.","email":"","middleInitial":"C.","affiliations":[{"id":6914,"text":"U.S. Environmental Protection Agency","active":true,"usgs":false}],"preferred":false,"id":540189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watson, Robert D.","contributorId":62605,"corporation":false,"usgs":true,"family":"Watson","given":"Robert","email":"","middleInitial":"D.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":540190,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Theisen, Arnold F.","contributorId":12052,"corporation":false,"usgs":true,"family":"Theisen","given":"Arnold","email":"","middleInitial":"F.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":540191,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jackson, R. D.","contributorId":30758,"corporation":false,"usgs":false,"family":"Jackson","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":6622,"text":"US Department of Agriculture","active":true,"usgs":false}],"preferred":false,"id":540192,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ehrler, W. L.","contributorId":139141,"corporation":false,"usgs":false,"family":"Ehrler","given":"W.","email":"","middleInitial":"L.","affiliations":[{"id":6622,"text":"US Department of Agriculture","active":true,"usgs":false}],"preferred":false,"id":540193,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pinter, P. J. Jr.","contributorId":100535,"corporation":false,"usgs":false,"family":"Pinter","given":"P.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[{"id":6622,"text":"US Department of Agriculture","active":true,"usgs":false}],"preferred":false,"id":540194,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Idso, S. B.","contributorId":139142,"corporation":false,"usgs":false,"family":"Idso","given":"S.","email":"","middleInitial":"B.","affiliations":[{"id":6622,"text":"US Department of Agriculture","active":true,"usgs":false}],"preferred":false,"id":540195,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Reginato, R. J.","contributorId":20082,"corporation":false,"usgs":false,"family":"Reginato","given":"R.","email":"","middleInitial":"J.","affiliations":[{"id":6622,"text":"US Department of Agriculture","active":true,"usgs":false}],"preferred":false,"id":540196,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":27573,"text":"wri80101 - 1980 - Ground water in the Springfield-Salem plateaus of southern Missouri and northern Arkansas","interactions":[],"lastModifiedDate":"2023-03-10T22:42:37.12126","indexId":"wri80101","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"80-101","title":"Ground water in the Springfield-Salem plateaus of southern Missouri and northern Arkansas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri80101","usgsCitation":"Harvey, E.J., 1980, Ground water in the Springfield-Salem plateaus of southern Missouri and northern Arkansas: U.S. Geological Survey Water-Resources Investigations Report 80-101, iv, 66 p., https://doi.org/10.3133/wri80101.","productDescription":"iv, 66 p.","costCenters":[],"links":[{"id":263307,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0101/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":263306,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0101/report-thumb.jpg"},{"id":413985,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35380.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arkansas, Missouri","otherGeospatial":"Springfield-Salem plateaus","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -94.582,\n              39\n            ],\n            [\n              -94.582,\n              36\n            ],\n            [\n              -89.5,\n              36\n            ],\n            [\n              -89.5,\n              39\n            ],\n            [\n              -94.582,\n              39\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d839","contributors":{"authors":[{"text":"Harvey, Edward Joseph","contributorId":32131,"corporation":false,"usgs":true,"family":"Harvey","given":"Edward","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":198353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175086,"text":"70175086 - 1980 - The behavior of <sup>14</sup>C and <sup>13</sup>C in estuarine water: Effects of In situ CO<sub>2</sub> production and atmospheric exchange","interactions":[],"lastModifiedDate":"2016-07-28T14:11:48","indexId":"70175086","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3225,"text":"Radiocarbon","active":true,"publicationSubtype":{"id":10}},"title":"The behavior of <sup>14</sup>C and <sup>13</sup>C in estuarine water: Effects of In situ CO<sub>2</sub> production and atmospheric exchange","docAbstract":"<p>The effects of nonconservative sources (inputs) and sinks (outputs) of carbon are indicated by the behavior of &Delta;<sup>14</sup>C and &delta;<sup>13</sup>C of the total dissolved inorganic carbon (&Sigma;CO<sub>2</sub>) in San Francisco Bay and Chesapeake Bay. Isotopic distributions and model calculations indicate that in North San Francisco Bay the net CO<sub>2</sub>&nbsp;flux to the atmosphere and carbon utilization in the water column are balanced by benthic production. Municipal waste appears to be a dominant source in South San Francisco Bav. In Chesapeake Bay, atmospheric exchange has increased the &Delta;<sup>14</sup>C and &delta;<sup>13</sup>C in the surface water. Decomposition of organic matter in the water column is indicated to be the dominant source of excess &Sigma;CO<sub>2</sub>&nbsp;in the deep water.</p>\n<p>&nbsp;</p>","language":"English","publisher":"The American Journal of Science","doi":"10.1017/S0033822200010018","usgsCitation":"Spiker, E.C., 1980, The behavior of <sup>14</sup>C and <sup>13</sup>C in estuarine water: Effects of In situ CO<sub>2</sub> production and atmospheric exchange: Radiocarbon, v. 22, no. 3, p. 647-654, https://doi.org/10.1017/S0033822200010018.","productDescription":"8 p.","startPage":"647","endPage":"654","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":480595,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1017/s0033822200010018","text":"Publisher Index Page"},{"id":325789,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2016-07-18","publicationStatus":"PW","scienceBaseUri":"579b2cb5e4b0589fa1c980df","contributors":{"authors":[{"text":"Spiker, Elliott C.","contributorId":50174,"corporation":false,"usgs":true,"family":"Spiker","given":"Elliott","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":643857,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2002123,"text":"2002123 - 1980 - Human disturbance at water sources of desert bighorn sheep","interactions":[],"lastModifiedDate":"2012-02-02T00:14:54","indexId":"2002123","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":91,"text":"Technical Report","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"CPSU/UNLV 010/12","title":"Human disturbance at water sources of desert bighorn sheep","docAbstract":"No abstract available at this time","language":"English","publisher":"National Park Service","usgsCitation":"Leslie, D., and Douglas, C.L., 1980, Human disturbance at water sources of desert bighorn sheep: Technical Report CPSU/UNLV 010/12.","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":198444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a631","contributors":{"authors":[{"text":"Leslie, David M. Jr.","contributorId":52514,"corporation":false,"usgs":true,"family":"Leslie","given":"David M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":326005,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Douglas, C. L.","contributorId":64586,"corporation":false,"usgs":true,"family":"Douglas","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":326006,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":64774,"text":"i1254A - 1980 - Map showing water circulation and rates of sedimentation in the Port Isabel 1 degree by 2 degrees quadrangle, Texas","interactions":[],"lastModifiedDate":"2023-08-29T18:31:13.927695","indexId":"i1254A","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"1254","subseriesTitle":"MGA","chapter":"A","title":"Map showing water circulation and rates of sedimentation in the Port Isabel 1 degree by 2 degrees quadrangle, Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1254A","usgsCitation":"Berryhill, H.L., and Trippet, A., 1980, Map showing water circulation and rates of sedimentation in the Port Isabel 1 degree by 2 degrees quadrangle, Texas: U.S. Geological Survey IMAP 1254, Report: 1 p.; 1 Plate: 46.83 x 24.80 inches, https://doi.org/10.3133/i1254A.","productDescription":"Report: 1 p.; 1 Plate: 46.83 x 24.80 inches","costCenters":[],"links":[{"id":255197,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1254a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255198,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1254a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420252,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9078.htm","linkFileType":{"id":5,"text":"html"}},{"id":255199,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1254a/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Texas","otherGeospatial":"Port Isabel 1 degree x 2 degrees quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.5,\n              28\n            ],\n            [\n              -97.5,\n              27\n            ],\n            [\n              -96,\n              27\n            ],\n            [\n              -96,\n              28\n            ],\n            [\n              -97.5,\n              28\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640e0a","contributors":{"authors":[{"text":"Berryhill, H. L. Jr.","contributorId":35361,"corporation":false,"usgs":true,"family":"Berryhill","given":"H.","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":272129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trippet, A. R.","contributorId":105377,"corporation":false,"usgs":true,"family":"Trippet","given":"A. R.","affiliations":[],"preferred":false,"id":272130,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012395,"text":"70012395 - 1980 - Speculations on processes responsible for mesoscale current lineations on the continental shelf, southern California","interactions":[],"lastModifiedDate":"2014-11-14T11:52:37","indexId":"70012395","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Speculations on processes responsible for mesoscale current lineations on the continental shelf, southern California","docAbstract":"<p>A side-scan sonar survey of San Pedro shelf, California, reveals areas of mesoscale current lineations oriented approximately north-northeast in water depths of 20-25 m. Widths of sand ribbons range from 40 to 120 m and intervening erosional furrows, from 15 to 50 m. A conceptual model shows that the scale and orientation of current lineations agree with the dimensions and axial directions of Langmuir circulations theoretically generated by a combination either of southerly and southwesterly winds with regular trains of swell from the southern hemisphere or of two sets of wave trains crossing from the south and west. These longitudinal bedforms indicate shore-normal sediment transport at the times and on the areas of the shelf when and where they have been observed.</p>","language":"English","doi":"10.1016/0025-3227(80)90132-2","issn":"00253227","usgsCitation":"Karl, H.A., 1980, Speculations on processes responsible for mesoscale current lineations on the continental shelf, southern California: Marine Geology, v. 34, no. 1-2, p. M9-M18, https://doi.org/10.1016/0025-3227(80)90132-2.","productDescription":"10 p.","startPage":"M9","endPage":"M18","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":222533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Pedro shelf","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.32275390624999,\n              33.780288785150866\n            ],\n            [\n              -118.3172607421875,\n              33.46008845688024\n            ],\n            [\n              -117.88467407226561,\n              33.46008845688024\n            ],\n            [\n              -117.89840698242188,\n              33.78371305547283\n            ],\n            [\n              -118.32275390624999,\n              33.780288785150866\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b95b7e4b08c986b31b094","contributors":{"authors":[{"text":"Karl, Herman A.","contributorId":80649,"corporation":false,"usgs":true,"family":"Karl","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":363439,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012239,"text":"70012239 - 1980 - Tectonic stresses in the lithosphere: constraints provided by the experimental deformation of rocks.","interactions":[],"lastModifiedDate":"2024-07-16T16:58:51.265202","indexId":"70012239","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Tectonic stresses in the lithosphere: constraints provided by the experimental deformation of rocks.","docAbstract":"<p><span>The strengths of rocks clearly place an upper limit on the stress that can be sustained by the upper half of the lithosphere. Laboratory data on rock rheology are generally lacking at intermediate temperatures and pressures on the important rock types expected in the lithosphere, so a definitive accounting of the strength distribution with depth in the upper lithosphere is presently unattainable. Analogies are drawn between the fragmentary strength data on silicates at intermediate temperature and the more extensive experimental data on marble and limestone, and several tentative conclusions are drawn: First, brittle processes, such as faulting and cataclasis, are expected to control rock strength at low pressures and temperatures. The strengths associated with these brittle mechanisms increase rapidly with increasing effective pressure and are relatively insensitive to temperature and strain rate. Second, the transitions between brittle and ductile processes occur at critical values of the least principal stress σ</span><sub>3</sub><span>. I suggest that the concept of the deformation mechanism map of Ashby (1972) be extended to brittle-ductile transitions by normalizing the applied differential stress σ by σ</span><sub>3</sub><span>, i.e., the transitions occur at critical values of σ/σ</span><sub>3</sub><span>. Third, the high temperature flow law of olivine, widely applied to problems involving flow in the asthenosphere, is inappropriate to the conditions of temperature found in the lithosphere, because different dislocation flow mechanisms dominate at low to intermediate temperatures. The fragmentary rheological data suggest the following rheological structure of the lithosphere where it is inelastically deforming: A rapid pressure-driven increase in rock strength with depth culminates with a shear strength maximum of up to 8 kbar at depths that depend on the state of stress and on the temperature distribution. A review of the mechanisms of weakening associated with water suggests that water weakening effects are probably not important in the oceanic lithosphere but are likely to be controlling in the continental crust.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB085iB11p06353","issn":"01480227","usgsCitation":"Kirby, S.H., 1980, Tectonic stresses in the lithosphere: constraints provided by the experimental deformation of rocks.: Journal of Geophysical Research Solid Earth, v. 85, no. B11, p. 6353-6363, https://doi.org/10.1029/JB085iB11p06353.","productDescription":"11 p.","startPage":"6353","endPage":"6363","numberOfPages":"11","costCenters":[],"links":[{"id":221811,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"B11","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505ba47ee4b08c986b3203a1","contributors":{"authors":[{"text":"Kirby, S. H.","contributorId":51721,"corporation":false,"usgs":true,"family":"Kirby","given":"S.","middleInitial":"H.","affiliations":[],"preferred":false,"id":363061,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012279,"text":"70012279 - 1980 - Extraction and concentration of phenolic compounds from water and sediment","interactions":[],"lastModifiedDate":"2017-03-16T09:07:51","indexId":"70012279","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Extraction and concentration of phenolic compounds from water and sediment","docAbstract":"Continuous liquid-liquid extractors are used to concentrate phenols at the ??g l-1 level from water into dichloromethane; this is followed by Kuderna-Danish evaporative concentration and gas chromatography. The procedure requires 5 h for 18 l of sample water. Overall concentration factors around 1000 are obtained. Overall concentration efficiencies vary from 23.1 to 87.1%. Concentration efficiencies determined by a batch method suitable for sediments range from 18.9 to 73.8%. ?? 1980.","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(01)93181-2","issn":"00032670","usgsCitation":"Goldberg, M.C., and Weiner, E.R., 1980, Extraction and concentration of phenolic compounds from water and sediment: Analytica Chimica Acta, v. 115, no. C, p. 373-378, https://doi.org/10.1016/S0003-2670(01)93181-2.","productDescription":"6 p.","startPage":"373","endPage":"378","numberOfPages":"6","costCenters":[],"links":[{"id":222402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"115","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0e5ce4b0c8380cd533f5","contributors":{"authors":[{"text":"Goldberg, Marvin C.","contributorId":26066,"corporation":false,"usgs":true,"family":"Goldberg","given":"Marvin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":363166,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weiner, Eugene R.","contributorId":23280,"corporation":false,"usgs":true,"family":"Weiner","given":"Eugene","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363165,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012323,"text":"70012323 - 1980 - Quantile estimation with more or less floodlike distributions","interactions":[],"lastModifiedDate":"2018-02-05T12:29:45","indexId":"70012323","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"Quantile estimation with more or less floodlike distributions","docAbstract":"<p><span>The desirable properties of an estimator relative to a hypothetical population may be irrelevant in practice unless the population at issue more or less resembles the hypothetical population. Evidence that floods are distributed with long, stretched upper tails suggests that use of the more common distributions results in a rather precise underestimation of the extreme quantiles and thereby in the underdesign of flood protection measures.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR016i003p00547","usgsCitation":"Landwehr, J.M., Matalas, N., and Wallis, J., 1980, Quantile estimation with more or less floodlike distributions: Water Resources Research, v. 16, no. 3, p. 547-555, https://doi.org/10.1029/WR016i003p00547.","productDescription":"9 p.","startPage":"547","endPage":"555","costCenters":[],"links":[{"id":222068,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505a91f4e4b0c8380cd8057c","contributors":{"authors":[{"text":"Landwehr, J. Maciunas","contributorId":13962,"corporation":false,"usgs":false,"family":"Landwehr","given":"J.","email":"","middleInitial":"Maciunas","affiliations":[],"preferred":false,"id":363276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matalas, N.C.","contributorId":25173,"corporation":false,"usgs":true,"family":"Matalas","given":"N.C.","affiliations":[],"preferred":false,"id":363275,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wallis, J.R.","contributorId":79236,"corporation":false,"usgs":true,"family":"Wallis","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":363277,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1014004,"text":"1014004 - 1980 - Effect of leaching on apparent digestion coefficients of feedstuffs for salmonids","interactions":[],"lastModifiedDate":"2025-08-13T15:17:14.505038","indexId":"1014004","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Effect of leaching on apparent digestion coefficients of feedstuffs for salmonids","docAbstract":"<p><span>Fecal excretions were collected from rainbow trout (Salmo gairdneri) in metabolism chambers. In this method of collection the daily excretion is suspended in about 1 L of water. Aliquots of the suspension were separated into solid and liquid fractions by settling, centrifuging, or filtering. Solid and liquid fractions and the unseparated suspension were analyzed for total nitrogen. Digestion coefficients for protein were calculated on the basis of solids and on total suspension. More than half of the fecal nitrogen was in the liquid fraction. Digestion coefficients for protein based only on solids were about 10 percentage points higher than those based on the total suspension, apparently because of leaching when the fecal matter was exposed to water. Digestibility and metabolizable energy of 55 diet ingredients, obtained by the metabolism chamber method, were tabulated.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8659(1980)42[195:EOLOAD]2.0.CO;2","usgsCitation":"Smith, R.R., Peterson, M.C., and Allred, A.C., 1980, Effect of leaching on apparent digestion coefficients of feedstuffs for salmonids: Progressive Fish-Culturist, v. 42, no. 4, p. 195-199, https://doi.org/10.1577/1548-8659(1980)42[195:EOLOAD]2.0.CO;2.","productDescription":"5 p.","startPage":"195","endPage":"199","numberOfPages":"5","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129753,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6255b0","contributors":{"authors":[{"text":"Smith, R. R.","contributorId":31699,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":319606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, M. C.","contributorId":104438,"corporation":false,"usgs":true,"family":"Peterson","given":"M.","middleInitial":"C.","affiliations":[],"preferred":false,"id":319608,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allred, A. C.","contributorId":87094,"corporation":false,"usgs":true,"family":"Allred","given":"A.","middleInitial":"C.","affiliations":[],"preferred":false,"id":319607,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012382,"text":"70012382 - 1980 - Mixing models and ionic geothermometers applied to warm (up to 60°C) springs: Jordan Rift Valley, Israel","interactions":[],"lastModifiedDate":"2015-06-12T16:11:44","indexId":"70012382","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Mixing models and ionic geothermometers applied to warm (up to 60°C) springs: Jordan Rift Valley, Israel","docAbstract":"<p id=\"\">Mixing models and evaluation of SiO<sub>2</sub>&nbsp;contents of warm-water manifestations in the Jordan&mdash;Dead Sea Rift Valley indicate that these waters are fed by aquifers with estimated temperatures of up to 68&deg;C. These calculations and Na/K ratios, concentrations of Na, K and Ca, concentrations of atmospheric Ne, Ar, Kr and Xe; and concentrations of the stable hydrogen and oxygen isotopes all indicate below-boiling temperatures.</p>\n<p id=\"\">No indications are available for the existence of above-boiling geothermal systems in the Jordan Rift Valley. Slightly higher than observed temperatures are concluded for a deep component at the springs of Hammat Gader (67&deg;C), Gofra (68&deg;C), the Russian Garden (40&deg;C), and the Yesha well (53&ndash;65&deg;C). These temperatures may encourage further developments for spas and bathing installations and, to a limited extent, for space heating, but are not favorable for geothermal power generation.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(80)90002-5","issn":"00221694","usgsCitation":"Mazor, E., Levitte, D., Truesdell, A., Healy, J., and Nissenbaum, A., 1980, Mixing models and ionic geothermometers applied to warm (up to 60°C) springs: Jordan Rift Valley, Israel: Journal of Hydrology, v. 45, no. 1-2, p. 1-19, https://doi.org/10.1016/0022-1694(80)90002-5.","productDescription":"19 p.","startPage":"1","endPage":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":222350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5b86e4b0c8380cd6f5fb","contributors":{"authors":[{"text":"Mazor, E.","contributorId":18104,"corporation":false,"usgs":true,"family":"Mazor","given":"E.","email":"","affiliations":[],"preferred":false,"id":363416,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Levitte, D.","contributorId":102630,"corporation":false,"usgs":true,"family":"Levitte","given":"D.","email":"","affiliations":[],"preferred":false,"id":363419,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":363417,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Healy, J.","contributorId":80822,"corporation":false,"usgs":true,"family":"Healy","given":"J.","affiliations":[],"preferred":false,"id":363418,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nissenbaum, A.","contributorId":103008,"corporation":false,"usgs":true,"family":"Nissenbaum","given":"A.","email":"","affiliations":[],"preferred":false,"id":363420,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1007447,"text":"1007447 - 1980 - Foods of breeding tricolored blackbirds in agricultural areas of Merced County, California","interactions":[],"lastModifiedDate":"2023-11-26T15:12:53.632401","indexId":"1007447","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1318,"text":"Condor","active":true,"publicationSubtype":{"id":10}},"title":"Foods of breeding tricolored blackbirds in agricultural areas of Merced County, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Oxford Academic","doi":"10.2307/1367578","usgsCitation":"Skorupa, J.P., Hothem, R.L., and DeHaven, R.W., 1980, Foods of breeding tricolored blackbirds in agricultural areas of Merced County, California: Condor, v. 82, no. 4, p. 465-467, https://doi.org/10.2307/1367578.","productDescription":"3 p.","startPage":"465","endPage":"467","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":503048,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/condor/vol82/iss4/22","text":"External Repository"},{"id":130352,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de4c5","contributors":{"authors":[{"text":"Skorupa, J. P.","contributorId":93002,"corporation":false,"usgs":false,"family":"Skorupa","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":315369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hothem, R. L.","contributorId":82633,"corporation":false,"usgs":true,"family":"Hothem","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":315368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeHaven, R. W.","contributorId":31711,"corporation":false,"usgs":true,"family":"DeHaven","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":315367,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":41821,"text":"ofr80997 - 1980 - Aeromagnetic map of the Little Dog-Pup Canyon area, New Mexico","interactions":[],"lastModifiedDate":"2023-03-01T20:39:39.140401","indexId":"ofr80997","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"80-997","title":"Aeromagnetic map of the Little Dog-Pup Canyon area, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80997","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Aeromagnetic map of the Little Dog-Pup Canyon area, New Mexico: U.S. Geological Survey Open-File Report 80-997, 1 Plate: 32.70 x 33.96 inches, https://doi.org/10.3133/ofr80997.","productDescription":"1 Plate: 32.70 x 33.96 inches","costCenters":[],"links":[{"id":168030,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413553,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11854.htm","linkFileType":{"id":5,"text":"html"}},{"id":79544,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0997/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","otherGeospatial":"Little Dog-Pup Canyon area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.819,\n              32.479\n            ],\n            [\n              -105.168,\n              32.479\n            ],\n            [\n              -105.168,\n              32.153\n            ],\n            [\n              -104.819,\n              32.153\n            ],\n            [\n              -104.819,\n              32.479\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691ebc","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":530646,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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