{"pageNumber":"6329","pageRowStart":"158200","pageSize":"25","recordCount":184914,"records":[{"id":70010248,"text":"70010248 - 1972 - Nimbus IV view of the major structural features of Alaska","interactions":[],"lastModifiedDate":"2026-01-23T22:32:08.618546","indexId":"70010248","displayToPublicDate":"1972-03-31T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Nimbus IV view of the major structural features of Alaska","docAbstract":"<p><span>Notwithstanding the relatively low degree of ground resolution, many of the major structural features of Alaska can be identified on the Nimbus IV IDCS image, exposed at an altitude of 600 nautical miles (1100 km). In addition, linears of regional extent that may be structurally controlled can be seen, many of which have not yet been recognized in surface mapping. The synoptic view provided by the image brings into focus an orthogonal set of fractures trending north-northeast and east-southeast and not heretofore apparent in regional maps of Alaska. This orthogonal fracture set may reflect a conjugate set of fractures within the crust, which has exerted significant control over the geologic history of the state. Increased resolution in other images from space platforms, such as the resolution of 200 to 650 feet (60 to 200 m) planned for the satellite television cameras of the ERTS program, will permit the discernment of finer detail and a greater accuracy in identifying and locating geologic features.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.175.4029.1423","issn":"00368075","usgsCitation":"Lathram, E., 1972, Nimbus IV view of the major structural features of Alaska: Science, v. 175, no. 4029, p. 1423-1427, https://doi.org/10.1126/science.175.4029.1423.","productDescription":"5 p.","startPage":"1423","endPage":"1427","costCenters":[],"links":[{"id":219601,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70010170,"text":"70010170 - 1972 - Rotational inertia of continents: A proposed link between polar wandering and plate tectonics","interactions":[],"lastModifiedDate":"2026-01-23T22:43:11.742324","indexId":"70010170","displayToPublicDate":"1972-03-24T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Rotational inertia of continents: A proposed link between polar wandering and plate tectonics","docAbstract":"A mechanism is proposed whereby displacement between continents and the earth's pole of rotation (polar wandering) gives rise to latitudinal transport of continental plates (continental drift) because of their relatively greater rotational inertia. When extended to short-term polar wobble, the hypothesis predicts an energy change nearly equivalent to the seismic energy rate.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.175.4028.1355","issn":"00368075","usgsCitation":"Kane, M.F., 1972, Rotational inertia of continents: A proposed link between polar wandering and plate tectonics: Science, v. 175, no. 4028, p. 1355-1357, https://doi.org/10.1126/science.175.4028.1355.","productDescription":"3 p.","startPage":"1355","endPage":"1357","costCenters":[],"links":[{"id":219669,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"175","issue":"4028","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aae9be4b0c8380cd8712a","contributors":{"authors":[{"text":"Kane, M. F.","contributorId":45708,"corporation":false,"usgs":true,"family":"Kane","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":358190,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001283,"text":"1001283 - 1972 - Movements and denning habits of a badger","interactions":[],"lastModifiedDate":"2025-03-10T15:32:13.066005","indexId":"1001283","displayToPublicDate":"1972-03-24T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Movements and denning habits of a badger","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Oxford Academic","doi":"10.2307/1378851","usgsCitation":"Sargeant, A., and Warner, D., 1972, Movements and denning habits of a badger: Journal of Mammalogy, v. 53, no. 1, p. 207-210, https://doi.org/10.2307/1378851.","productDescription":"4 p.","startPage":"207","endPage":"210","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128680,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Cedar Creek Natural History Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -93.2100945486041,\n              45.417181843336834\n            ],\n            [\n              -93.2100945486041,\n              45.37432553804044\n            ],\n            [\n              -93.15314198933328,\n              45.37432553804044\n            ],\n            [\n              -93.15314198933328,\n              45.417181843336834\n            ],\n            [\n              -93.2100945486041,\n              45.417181843336834\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"53","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b481f","contributors":{"authors":[{"text":"Sargeant, A.B.","contributorId":13171,"corporation":false,"usgs":true,"family":"Sargeant","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":310800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warner, D.W.","contributorId":63344,"corporation":false,"usgs":true,"family":"Warner","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":310801,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70208884,"text":"70208884 - 1972 - Geology of the massive sulfide deposits at Jerome, Arizona; A reinterpretation","interactions":[],"lastModifiedDate":"2020-03-04T11:25:26","indexId":"70208884","displayToPublicDate":"1972-03-04T10:51:52","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Geology of the massive sulfide deposits at Jerome, Arizona; A reinterpretation","docAbstract":"<p>The massive sulfide deposits at Jerome, consisting largely of pyrite, chalcopyrite, and sphalerite, are concordant stratabound lenses in massive quartz-bearing crystal tuffs of Precambrian age and overlying bedded tuffaceous rocks. The crystal tuffs were eraplaced as submarine pyroclastic flows. The evidence permits the interpretation that the massive sulfide lenses are essentially syngenetic and related to hydrothermal brines that discharged into a submarine basin. The host rocks and sulfide lenses were folded and metamorphosed. Two periods of folding can be recognized; during the second period, the older folds were deformed along vertical axes, and some of the chalcopyrite in the major lens migrated downward to form shoots of intersecting veins in the crystal tuff and chloritized tuff (black schist). Fluid inclusions in volcaniclastic and vein quartz appear to be related to deformation and metamorphism and provide no direct evidence on the nature of the primary fluids that presumably introduced the ore metals to the volcanic rocks accumulating on the sea floor. Liquid CO2-bearing inclusions are restricted to rocks and veins near the United Verde deposit and associated chalcopyrite ore shoots. Fluids at that time were CO2-rich, with temperatures of approximately 235 ø C and confining pressures of about 700 bars or less. </p>","language":"English","publisher":"GeoScienceWorld","doi":"10.2113/gsecongeo.67.7.845","usgsCitation":"Anderson, C., and Nash, J.T., 1972, Geology of the massive sulfide deposits at Jerome, Arizona; A reinterpretation: Economic Geology, v. 67, no. 7, p. 845-863, https://doi.org/10.2113/gsecongeo.67.7.845.","productDescription":"19 p.","startPage":"845","endPage":"863","costCenters":[],"links":[{"id":372893,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Jerome","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.2747802734375,\n              34.41144164327245\n            ],\n            [\n              -111.87377929687499,\n              34.41144164327245\n            ],\n            [\n              -111.87377929687499,\n              34.939985151560435\n            ],\n            [\n              -112.2747802734375,\n              34.939985151560435\n            ],\n            [\n              -112.2747802734375,\n              34.41144164327245\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"67","issue":"7","noUsgsAuthors":false,"publicationDate":"1972-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Anderson, C.A.","contributorId":105277,"corporation":false,"usgs":true,"family":"Anderson","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":783842,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nash, J. Thomas","contributorId":26306,"corporation":false,"usgs":true,"family":"Nash","given":"J.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":783843,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175803,"text":"70175803 - 1972 - Field trip guidebook for hydrogeology of the Twin Cities Artesian Basin","interactions":[],"lastModifiedDate":"2018-04-02T12:08:54","indexId":"70175803","displayToPublicDate":"1972-03-02T11:30:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5185,"text":"Guidebook","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"8","title":"Field trip guidebook for hydrogeology of the Twin Cities Artesian Basin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Minnesota Geological Survey","publisherLocation":"St. Paul, MN","usgsCitation":"Winter, T.C., and Norvitch, R., 1972, Field trip guidebook for hydrogeology of the Twin Cities Artesian Basin: Guidebook 8, 35 p.","productDescription":"35 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":326929,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Twin Cities Artesian Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82db6e4b03fd6b7da36a7","contributors":{"authors":[{"text":"Winter, T. C.","contributorId":23485,"corporation":false,"usgs":true,"family":"Winter","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":646375,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norvitch, R.F.","contributorId":107742,"corporation":false,"usgs":true,"family":"Norvitch","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":646376,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175445,"text":"70175445 - 1972 - An approach to the design of statewide or regional ground water information systems","interactions":[],"lastModifiedDate":"2018-04-02T12:05:27","indexId":"70175445","displayToPublicDate":"1972-02-01T13:00:00","publicationYear":"1972","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":"An approach to the design of statewide or regional ground water information systems","docAbstract":"<p><span>The design of water information or basic data systems must be flexible enough to provide information and data for a broad range of interests from national to local. The system must satisfy the need for information for accounting, surveillance, and areal synthesis purposes. The network is designed by identifying specific needs in terms of maps, analyses, and studies that will provide the basic knowledge for understanding each particular phase of the groundwater system. Each specific need is then analyzed with respect to whether it will provide information on accounting, surveillance, or areal synthesis. If a particular type of map, analysis, or observation can serve any of these three functions, a network of data collection or a program of studies is outlined in detail that will provide the information needed. The method of design necessitates the establishment of accuracy levels for maps, the density of data points, confidence limits, and so forth. The information system should be under the general guidance of a single agency, but much of the work and responsibility to carry out the details of the system must be shared by a number of agencies.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR008i001p00222","usgsCitation":"Winter, T.C., 1972, An approach to the design of statewide or regional ground water information systems: Water Resources Research, v. 8, no. 1, p. 222-230, https://doi.org/10.1029/WR008i001p00222.","productDescription":"9 p.","startPage":"222","endPage":"230","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":326402,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"57ada1afe4b0f412a62dfa36","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":645251,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206931,"text":"70206931 - 1972 - Suspended matter in surface waters of the northern Gulf of Mexico","interactions":[],"lastModifiedDate":"2019-11-27T17:10:28","indexId":"70206931","displayToPublicDate":"1972-01-31T17:05:51","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Suspended matter in surface waters of the northern Gulf of Mexico","docAbstract":"<p>Analyses of about 200 surface water samples collected during late fall 1966 show that concentrations of suspended matter greater than 1 mg/liter were restricted to within a few kilometers off Florida, but extended more than 100 km off Louisiana and Texas. Suspensates from areas farther than 100 km from shore contained mainly combustible organic matter, part of which was attributable to living plankton.</p><p>Organic aggregates encompassing appreciable amounts of inorganic detritus were particularly noteworthy in transitional areas. Zooplankton metabolism and fecal pellet production appears to be a geologically significant mechanism for depositing fine suspended matter and may contribute to the zonation of bottom sediments.</p><p>The mineral composition of surface suspensates ranges from a low magnesian calcite‐aragonite suite off Florida to montmorillonite‐kaolinite combinations from Alabama to Texas. The mineral composition of the suspensates resembles that of the bottom sediments in each area.</p>","language":"English","publisher":"Wiley","doi":"10.4319/lo.1972.17.1.0017","usgsCitation":"Manheim, F.T., Hathaway, J., and Uchupi, E., 1972, Suspended matter in surface waters of the northern Gulf of Mexico: Limnology and Oceanography, v. 17, no. 1, p. 17-27, https://doi.org/10.4319/lo.1972.17.1.0017.","productDescription":"11 p.","startPage":"17","endPage":"27","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":480673,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lo.1972.17.1.0017","text":"Publisher Index Page"},{"id":369762,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Northern Gulf of Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.5517578125,\n              25.20494115356912\n            ],\n            [\n              -83.0126953125,\n              29.19053283229458\n            ],\n            [\n              -84.19921875,\n              30.259067203213018\n            ],\n            [\n              -84.990234375,\n              29.76437737516313\n            ],\n            [\n              -86.484375,\n              30.372875188118016\n            ],\n            [\n              -88.11035156249999,\n              30.486550842588485\n            ],\n            [\n              -90.3076171875,\n              30.183121842195515\n            ],\n            [\n              -90.5712890625,\n              29.34387539941801\n            ],\n            [\n              -94.2626953125,\n              29.649868677972304\n            ],\n            [\n              -96.5478515625,\n              28.729130483430154\n            ],\n            [\n              -97.119140625,\n              27.839076094777816\n            ],\n            [\n              -97.55859375,\n              27.176469131898898\n            ],\n            [\n              -97.2509765625,\n              25.760319754713887\n            ],\n            [\n              -95.712890625,\n              22.998851594142913\n            ],\n            [\n              -89.3408203125,\n              22.67484735118852\n            ],\n            [\n              -81.6064453125,\n              24.046463999666567\n            ],\n            [\n              -80.5517578125,\n              25.20494115356912\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":776290,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hathaway, J.C.","contributorId":94280,"corporation":false,"usgs":true,"family":"Hathaway","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":776291,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Uchupi, Elazar","contributorId":79853,"corporation":false,"usgs":true,"family":"Uchupi","given":"Elazar","email":"","affiliations":[],"preferred":false,"id":776292,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010115,"text":"70010115 - 1972 - Lunar anorthosite 15415: Texture, mineralogy, and metamorphic history","interactions":[],"lastModifiedDate":"2026-01-26T16:13:46.226868","indexId":"70010115","displayToPublicDate":"1972-01-28T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Lunar anorthosite 15415: Texture, mineralogy, and metamorphic history","docAbstract":"Lunar anorthosite 15415 consists almost entirely of anorthite (homogeneous anorthite 96.6 molecule percent), with accessory diopsidic augite and traces of hypersthene, ilmenite, and a silica mineral. The rock has had a complex metamorphic history. The texture reflects at least two episodes of shearing (followed by intense and partial recrystallization, respectively), one episode of cataclastic deformation, and one or more episodes of shattering and fragmentation.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.175.4020.432","issn":"00368075","usgsCitation":"James, O., 1972, Lunar anorthosite 15415: Texture, mineralogy, and metamorphic history: Science, v. 175, no. 4020, p. 432-436, https://doi.org/10.1126/science.175.4020.432.","productDescription":"5 p.","startPage":"432","endPage":"436","costCenters":[],"links":[{"id":218779,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"175","issue":"4020","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4a8be4b0c8380cd68e53","contributors":{"authors":[{"text":"James, O.B.","contributorId":100526,"corporation":false,"usgs":true,"family":"James","given":"O.B.","email":"","affiliations":[],"preferred":false,"id":357987,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010114,"text":"70010114 - 1972 - Mariner 9 television reconnaissance of Mars and its satellites: Preliminary results","interactions":[],"lastModifiedDate":"2026-01-26T16:23:21.859169","indexId":"70010114","displayToPublicDate":"1972-01-21T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Mariner 9 television reconnaissance of Mars and its satellites: Preliminary results","docAbstract":"<div class=\"panel-pane pane-highwire-panel-tabs-container article__body\"><div class=\"pane-content\"><div id=\"panels-ajax-tab-container-highwire_article_tabs\" class=\"panels-ajax-tab-container\" data-panels-ajax-tab-preloaded=\"jnl_sci_tab_art\"><div class=\"panels-ajax-tab-wrap-jnl_sci_tab_art\"><div class=\"panel-display panel-1col clearfix\"><div class=\"panel-panel panel-col\"><div><div class=\"panel-pane pane-highwire-markup\"><div class=\"pane-content\"><div class=\"highwire-markup\"><div id=\"content-block-markup\" data-highwire-cite-ref-tooltip-instance=\"highwire_reflinks_tooltip\" data-highwire-glossary-tooltip-instance=\"highwire_reflinks_tooltip\"><div class=\"article abstract-view \"><div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-1\">At orbit insertion on 14 November 1971 the Martian surface was largely obscured by a dust haze with an extinction optical depth that ranged from near unity in the south polar region to probably greater than 2 over most of the planet. The only features clearly visible were the south polar cap, one dark, spot in Nix Olympica, and three dark spots in the Tharsis region. During the third week the atmosphere began to clear and surface visibility improved, but contrasts remained a fraction of their normal value. Each of the dark spots that apparently protrude through most of the dust-filled atmosphere has a crater or crater complex in its center. The craters are rimless and have featureless floors that, in the crater complexes, are at different levels. The largest crater within the southernmost spot is approximately 100 kilometers wide. The craters apparently were formed by subsidence and resemble terrestrial calderas. The south polar cap has a regular margin, suggesting very flat topography. Two craters outside the cap have frost on their floors; an apparent crater rim within the cap is frost free, indicating preferential loss of frost from elevated ground. If this is so then the curvilinear streaks, which were frost covered in 1969 and are now clear of frost, may be low-relief ridges. Closeup pictures of Phobos and Deimos show that Phobos is about 25 ±5 by 21 ±1 kilometers and Deimos is about 13.5 ± 2 by 12.0 ±0.5 kilometers. Both have irregular shapes and are highly cratered, with some craters showing raised rims. The satellites are dark objects with geometric albedos of 0.05.</p></div></div><span id=\"related-urls\"></span></div></div></div></div></div></div></div></div></div></div></div>","language":"English","publisher":"AAAS","doi":"10.1126/science.175.4019.294","issn":"00368075","usgsCitation":"Masursky, H., Batson, R.M., McCauley, J., Soderblom, L., Wildey, R., Carr, M.H., Milton, D., Wilhelms, D., Smith, B., Kirby, T., Robinson, J., Leovy, C., Briggs, G., Duxbury, T.C., Acton, C., Murray, B.C., Cutts, J., Sharp, R., Smith, S., Leighton, R., Sagan, C., Veverka, J., Noland, M., Lederberg, J., Levinthal, E., Pollack, J.B., Moore, J., Hartmann, W., Shipley, E., De Vaucouleurs, G., and Davies, M.E., 1972, Mariner 9 television reconnaissance of Mars and its satellites: Preliminary results: Science, v. 175, no. 4019, p. 294-305, https://doi.org/10.1126/science.175.4019.294.","productDescription":"12 p.","startPage":"294","endPage":"305","costCenters":[],"links":[{"id":218778,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"175","issue":"4019","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a51f7e4b0c8380cd6c077","contributors":{"authors":[{"text":"Masursky, H.","contributorId":33823,"corporation":false,"usgs":true,"family":"Masursky","given":"H.","affiliations":[],"preferred":false,"id":357965,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Batson, R. M.","contributorId":76714,"corporation":false,"usgs":true,"family":"Batson","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":357978,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCauley, J.F.","contributorId":26310,"corporation":false,"usgs":true,"family":"McCauley","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":357963,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Soderblom, L.A. 0000-0002-0917-853X","orcid":"https://orcid.org/0000-0002-0917-853X","contributorId":6139,"corporation":false,"usgs":true,"family":"Soderblom","given":"L.A.","affiliations":[],"preferred":false,"id":357956,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wildey, R.L.","contributorId":9700,"corporation":false,"usgs":true,"family":"Wildey","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":357958,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":357980,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Milton, D.J.","contributorId":44121,"corporation":false,"usgs":true,"family":"Milton","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":357970,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Wilhelms, D.E.","contributorId":82302,"corporation":false,"usgs":true,"family":"Wilhelms","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":357979,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Smith, B.A.","contributorId":17616,"corporation":false,"usgs":true,"family":"Smith","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":357960,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Kirby, T.B.","contributorId":86643,"corporation":false,"usgs":true,"family":"Kirby","given":"T.B.","email":"","affiliations":[],"preferred":false,"id":357981,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Robinson, J.C.","contributorId":57726,"corporation":false,"usgs":true,"family":"Robinson","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":357974,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Leovy, C.B.","contributorId":95609,"corporation":false,"usgs":true,"family":"Leovy","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":357983,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Briggs, G.A.","contributorId":34242,"corporation":false,"usgs":true,"family":"Briggs","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":357966,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Duxbury, T. C.","contributorId":91983,"corporation":false,"usgs":true,"family":"Duxbury","given":"T.","email":"","middleInitial":"C.","affiliations":[{"id":36392,"text":"Jet Propulsion Laboratory","active":true,"usgs":false}],"preferred":false,"id":357982,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Acton, C.H. Jr.","contributorId":41291,"corporation":false,"usgs":true,"family":"Acton","given":"C.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":357968,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Murray, B. 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Jr.","contributorId":38431,"corporation":false,"usgs":true,"family":"Moore","given":"J.T.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":357967,"contributorType":{"id":1,"text":"Authors"},"rank":27},{"text":"Hartmann, W.K.","contributorId":96002,"corporation":false,"usgs":true,"family":"Hartmann","given":"W.K.","email":"","affiliations":[],"preferred":false,"id":357984,"contributorType":{"id":1,"text":"Authors"},"rank":28},{"text":"Shipley, E.N.","contributorId":66407,"corporation":false,"usgs":true,"family":"Shipley","given":"E.N.","email":"","affiliations":[],"preferred":false,"id":357975,"contributorType":{"id":1,"text":"Authors"},"rank":29},{"text":"De Vaucouleurs, G.","contributorId":108243,"corporation":false,"usgs":true,"family":"De Vaucouleurs","given":"G.","email":"","affiliations":[],"preferred":false,"id":357986,"contributorType":{"id":1,"text":"Authors"},"rank":30},{"text":"Davies, M. E.","contributorId":26050,"corporation":false,"usgs":true,"family":"Davies","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":357962,"contributorType":{"id":1,"text":"Authors"},"rank":31}]}}
,{"id":70010294,"text":"70010294 - 1972 - Mariner 9 science experiments: Preliminary results","interactions":[],"lastModifiedDate":"2026-01-26T16:18:28.205601","indexId":"70010294","displayToPublicDate":"1972-01-21T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Mariner 9 science experiments: Preliminary results","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.175.4019.293","issn":"00368075","usgsCitation":"Steinbacher, R., Kliore, A., Lorell, J., Hipsher, H., Barth, C., Masursky, H., Munch, G., Pearl, J., and Smith, B., 1972, Mariner 9 science experiments: Preliminary results: Science, v. 175, no. 4019, p. 293-294, https://doi.org/10.1126/science.175.4019.293.","productDescription":"2 p.","startPage":"293","endPage":"294","costCenters":[],"links":[{"id":219225,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"175","issue":"4019","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a51f6e4b0c8380cd6c068","contributors":{"authors":[{"text":"Steinbacher, R.H.","contributorId":88478,"corporation":false,"usgs":true,"family":"Steinbacher","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":358548,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kliore, A.","contributorId":44424,"corporation":false,"usgs":true,"family":"Kliore","given":"A.","email":"","affiliations":[],"preferred":false,"id":358544,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lorell, J.","contributorId":8344,"corporation":false,"usgs":true,"family":"Lorell","given":"J.","email":"","affiliations":[],"preferred":false,"id":358540,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hipsher, H.","contributorId":82183,"corporation":false,"usgs":true,"family":"Hipsher","given":"H.","email":"","affiliations":[],"preferred":false,"id":358547,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Barth, C.A.","contributorId":26468,"corporation":false,"usgs":true,"family":"Barth","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":358541,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Masursky, H.","contributorId":33823,"corporation":false,"usgs":true,"family":"Masursky","given":"H.","affiliations":[],"preferred":false,"id":358542,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Munch, G.","contributorId":53241,"corporation":false,"usgs":true,"family":"Munch","given":"G.","email":"","affiliations":[],"preferred":false,"id":358545,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Pearl, J.","contributorId":39652,"corporation":false,"usgs":true,"family":"Pearl","given":"J.","affiliations":[],"preferred":false,"id":358543,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Smith, B.","contributorId":53740,"corporation":false,"usgs":true,"family":"Smith","given":"B.","affiliations":[],"preferred":false,"id":358546,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70010281,"text":"70010281 - 1972 - Magma supply rate at Kilauea volcano, 1952-1971","interactions":[],"lastModifiedDate":"2026-01-26T16:35:00.159804","indexId":"70010281","displayToPublicDate":"1972-01-14T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Magma supply rate at Kilauea volcano, 1952-1971","docAbstract":"<div class=\"panel-pane pane-highwire-panel-tabs-container article__body\"><div class=\"pane-content\"><div id=\"panels-ajax-tab-container-highwire_article_tabs\" class=\"panels-ajax-tab-container\" data-panels-ajax-tab-preloaded=\"jnl_sci_tab_art\"><div class=\"panels-ajax-tab-wrap-jnl_sci_tab_art\"><div class=\"panel-display panel-1col clearfix\"><div class=\"panel-panel panel-col\"><div><div class=\"panel-pane pane-highwire-markup\"><div class=\"pane-content\"><div class=\"highwire-markup\"><div id=\"content-block-markup\" data-highwire-cite-ref-tooltip-instance=\"highwire_reflinks_tooltip\" data-highwire-glossary-tooltip-instance=\"highwire_reflinks_tooltip\"><div class=\"article abstract-view \"><div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-1\">The three longest Kilauea eruptions since 1952 produced lava at an overall constant rate of about 9 x 10<sup>6</sup><span>&nbsp;</span>cubic meters per month (vesicle-free). This is considered to represent the rate of magma supply from a deep source, probably the mantle, because little or no summit deformation indicating high-level storage accompanied any of the three eruptions.</p></div></div><span id=\"related-urls\"></span></div></div></div></div></div></div></div></div></div></div></div>","language":"English","publisher":"AAAS","doi":"10.1126/science.175.4018.169","issn":"00368075","usgsCitation":"Swanson, D.A., 1972, Magma supply rate at Kilauea volcano, 1952-1971: Science, v. 175, no. 4018, p. 169-170, https://doi.org/10.1126/science.175.4018.169.","productDescription":"2 p.","startPage":"169","endPage":"170","costCenters":[],"links":[{"id":219061,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.3192138671875,\n              19.374636239520235\n            ],\n            [\n              -155.20797729492188,\n              19.374636239520235\n            ],\n            [\n              -155.20797729492188,\n              19.449759112405612\n            ],\n            [\n              -155.3192138671875,\n              19.449759112405612\n            ],\n            [\n              -155.3192138671875,\n              19.374636239520235\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"175","issue":"4018","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4b3ee4b0c8380cd693bd","contributors":{"authors":[{"text":"Swanson, D. A.","contributorId":34102,"corporation":false,"usgs":true,"family":"Swanson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":358513,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206714,"text":"70206714 - 1972 - Borehole activation analysis by delayed and capture gamma rays using a 252Cf neutron source","interactions":[],"lastModifiedDate":"2019-11-18T14:25:13","indexId":"70206714","displayToPublicDate":"1972-01-08T14:19:50","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Borehole activation analysis by delayed and capture gamma rays using a 252Cf neutron source","docAbstract":"<p><span>Theoretical analysis and experimental comparison of the radiative capture and delayed gamma-ray activation techniques indicate the latter to be more efficient for the detection of copper, whereas the radiative capture method is preferable for nickel. A conservative lower detection limit for both copper and nickel is '-0.5%. Borehole spectra by both techniques were made in a copper- and nickel-bearing gabbro, utilizing a Ge(Li) propane-cooled detector. Al, Mn, Na, Mg, Cu, and V were readily activated and detected by the delayed method. H, Fe, Si, and Ni were not usually present in the delayed spectra but they responded well in the capture mode. It is shown that the borehole sonde can be configured to permit simultaneous delayed and capture spectra, permitting detection of all of these elements. Simulated borehole experiments indicate that, in the delayed gamma-ray mode, an infinite sample is achieved when the ore layer has a vertical thickness of ∼20 cm and a horizontal distance of '10 cm into the wallrock. The depth resolution is thus relatively good but horizontal penetration through the wallrock is limited. © 1972 Society of Economic Geologists, Inc.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.2113/gsecongeo.67.5.579","issn":"03610128","usgsCitation":"Moxham, R., Senftle, F.E., and Boynton, G.R., 1972, Borehole activation analysis by delayed and capture gamma rays using a 252Cf neutron source: Economic Geology, v. 67, no. 5, p. 579-591, https://doi.org/10.2113/gsecongeo.67.5.579.","productDescription":"13 p.","startPage":"579","endPage":"591","costCenters":[],"links":[{"id":369297,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"5","noUsgsAuthors":false,"publicationDate":"1972-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":775521,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":775522,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boynton, G. R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":775523,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010127,"text":"70010127 - 1972 - Iron-rich basal sediments from the eastern equatorial pacific: Leg 16, deep sea drilling project","interactions":[],"lastModifiedDate":"2026-01-26T16:41:16.281831","indexId":"70010127","displayToPublicDate":"1972-01-07T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Iron-rich basal sediments from the eastern equatorial pacific: Leg 16, deep sea drilling project","docAbstract":"Iron-rich sediments chemically similar to those forming at present on the crest of the East Pacific Rise have been found just above basement at widely separated drill sites in the eastern equatorial Pacific, including three sites of Leg 16 of the Deep Sea Drilling Project. These sediments were probably formed when the basement was at the crest of this rise and have moved to their present location as a result of sea-floor spreading.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.175.4017.61","issn":"00368075","usgsCitation":"Cronan, D., Van Andel, T.H., Heath, G.R., Dinkelman, M., Bennett, R., Bukry, D., Charleston, S., Kaneps, A., Rodolfo, K., and Yeats, R., 1972, Iron-rich basal sediments from the eastern equatorial pacific: Leg 16, deep sea drilling project: Science, v. 175, no. 4017, p. 61-63, https://doi.org/10.1126/science.175.4017.61.","productDescription":"3 p.","startPage":"61","endPage":"63","costCenters":[],"links":[{"id":218989,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"175","issue":"4017","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3ef9e4b0c8380cd6418f","contributors":{"authors":[{"text":"Cronan, D.S.","contributorId":57324,"corporation":false,"usgs":true,"family":"Cronan","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":358032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Andel, T. H.","contributorId":68038,"corporation":false,"usgs":true,"family":"Van Andel","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":358033,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heath, G. Ross","contributorId":84635,"corporation":false,"usgs":true,"family":"Heath","given":"G.","middleInitial":"Ross","affiliations":[],"preferred":false,"id":358035,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dinkelman, M.G.","contributorId":83392,"corporation":false,"usgs":true,"family":"Dinkelman","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":358034,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bennett, R.H.","contributorId":34649,"corporation":false,"usgs":true,"family":"Bennett","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":358029,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bukry, D.","contributorId":15338,"corporation":false,"usgs":true,"family":"Bukry","given":"D.","affiliations":[],"preferred":false,"id":358027,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Charleston, S.","contributorId":23816,"corporation":false,"usgs":true,"family":"Charleston","given":"S.","email":"","affiliations":[],"preferred":false,"id":358028,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kaneps, A.","contributorId":37211,"corporation":false,"usgs":true,"family":"Kaneps","given":"A.","email":"","affiliations":[],"preferred":false,"id":358030,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Rodolfo, K.S.","contributorId":96156,"corporation":false,"usgs":true,"family":"Rodolfo","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":358036,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Yeats, R.S.","contributorId":48990,"corporation":false,"usgs":true,"family":"Yeats","given":"R.S.","affiliations":[],"preferred":false,"id":358031,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":32539,"text":"32539 - 1972 - National Atlas, Central Pacific states","interactions":[],"lastModifiedDate":"2017-03-29T11:27:40","indexId":"32539","displayToPublicDate":"1972-01-01T16:47:35","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"National Atlas, Central Pacific states","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/32539","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, National Atlas, Central Pacific states (Rev. 1972.), 1 map, https://doi.org/10.3133/32539.","productDescription":"1 map","numberOfPages":"1","costCenters":[],"links":[{"id":291552,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.17,33.35 ], [ -127.17,47.45 ], [ -112.21,47.45 ], [ -112.21,33.35 ], [ -127.17,33.35 ] ] ] } } ] }","edition":"Rev. 1972.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53dca9c4e4b0761578637736","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":529406,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047704,"text":"70047704 - 1972 - Annual water-resources review, White Sands Missile Range: 1971","interactions":[],"lastModifiedDate":"2013-11-13T12:44:59","indexId":"70047704","displayToPublicDate":"1972-01-01T15:46:00","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":"Annual water-resources review, White Sands Missile Range: 1971","docAbstract":"This report presents water-resource information that was collected at White Sands Missile Range during 1971 and early 1972 by personnel of the U.S. Geological Survey, Water Resources Division. Data on ground-water pumpage and resulting water-level fluctuation, chemical quality, percipitation, and surface-water runoff are summarized in the report. The data were obtained as a result of the continuing water-resources basic-data collection program sponsored by the Facilities Engineering Directorate, White Sands Missile Range.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Albuquerque, NM","doi":"10.3133/70047704","collaboration":"Prepared in cooperation with White Sands Missile Range","usgsCitation":"Cruz, R.R., 1972, Annual water-resources review, White Sands Missile Range: 1971: Open-File Report, 35 p., https://doi.org/10.3133/70047704.","productDescription":"35 p.","numberOfPages":"35","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":276785,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047704.jpg"},{"id":278727,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047704/report.pdf"}],"country":"United States","state":"New Mexico","otherGeospatial":"White Sands Missile Range","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,31.0 ], [ -109.0,37.0 ], [ -103.0,37.0 ], [ -103.0,31.0 ], [ -109.0,31.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52136e30e4b0b08f446198b8","contributors":{"authors":[{"text":"Cruz, R. R.","contributorId":97496,"corporation":false,"usgs":true,"family":"Cruz","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482772,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120944,"text":"70120944 - 1972 - Distribution and isotopic composition of uranium in lower Nueces River, Nueces Bay and Corpus Christi Bay, Texas","interactions":[],"lastModifiedDate":"2014-08-18T15:20:51","indexId":"70120944","displayToPublicDate":"1972-01-01T15:11:18","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1871,"text":"Gulf Coast Association of Geological Societies Transactions","active":true,"publicationSubtype":{"id":10}},"title":"Distribution and isotopic composition of uranium in lower Nueces River, Nueces Bay and Corpus Christi Bay, Texas","docAbstract":"The uranium concentration and isotopic composition of water and suspended sediment from the Nueces River, Nueces Bay and Corpus Christi Bay were determined by alpha-spectroscopy. The average dissolved uranium concentration and radioactivity ratio (U<sup>234</sup>/U<sup>238</sup>) of Nueces River water were determined to be 2.44 µg/1 and 1.15 respectively. Water from a tributary of the Nueces River, Cayamon Creek, was found to contain an average dissolved uranium concentration of 42.8 µg/1 with an isotopic radioactivity ratio of 1.56. Close inspection of the lateral concentration and isotopic activity ratio of uranium revealed an increase below the confluence of Cayamon Creek with the Nueces River. A model was derived based on equations used in isotopic dilution analysis, which predicts these increases within analytical error. This model may be useful in future studies to locate anomalous uranium within the hydrologic environment.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Gulf Coast Association of Geological Societies Transactions","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Gulf Coast Association of Geological Societies","publisherLocation":"New Orleans, LA","usgsCitation":"Holmes, C.W., and Slade, E.A., 1972, Distribution and isotopic composition of uranium in lower Nueces River, Nueces Bay and Corpus Christi Bay, Texas: Gulf Coast Association of Geological Societies Transactions, v. 22, p. 315-322.","productDescription":"8 p.","startPage":"315","endPage":"322","numberOfPages":"8","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292476,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292475,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/gcags/data/022/022001/0315.htm"}],"country":"United States","state":"Texas","otherGeospatial":"Corpus Christi Bay;Nueces Bay;Nueces River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.0,27.6409 ], [ -98.0,28.124 ], [ -97.0,28.124 ], [ -97.0,27.6409 ], [ -98.0,27.6409 ] ] ] } } ] }","volume":"22","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f31349e4b0094694f9d82b","contributors":{"authors":[{"text":"Holmes, Charles W.","contributorId":31071,"corporation":false,"usgs":true,"family":"Holmes","given":"Charles","email":"","middleInitial":"W.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":498656,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slade, Elizabeth Ann","contributorId":28537,"corporation":false,"usgs":true,"family":"Slade","given":"Elizabeth","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":498655,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70121102,"text":"70121102 - 1972 - Acoustic reflection profiles, East Margin, Yucatan Peninsula: Leg 2, 1971 cruise, UNITEDGEO I","interactions":[],"lastModifiedDate":"2014-08-19T14:46:23","indexId":"70121102","displayToPublicDate":"1972-01-01T14:23:43","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Acoustic reflection profiles, East Margin, Yucatan Peninsula: Leg 2, 1971 cruise, UNITEDGEO I","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/70121102","collaboration":"USGS-GD-72-003, PB-207-595","usgsCitation":"Vedder, J.G., 1972, Acoustic reflection profiles, East Margin, Yucatan Peninsula: Leg 2, 1971 cruise, UNITEDGEO I, 15 p., https://doi.org/10.3133/70121102.","productDescription":"15 p.","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292581,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"otherGeospatial":"Gulf Of Mexico;Yucatan Peninsula","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.46,16.05 ], [ -91.46,22.65 ], [ -84.94,22.65 ], [ -84.94,16.05 ], [ -91.46,16.05 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f464c8e4b073ff773a7cd0","contributors":{"authors":[{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":498802,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168638,"text":"70168638 - 1972 - Water resources data for Iowa, water year 1971","interactions":[],"lastModifiedDate":"2016-02-22T12:56:36","indexId":"70168638","displayToPublicDate":"1972-01-01T14:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Iowa, water year 1971","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/70168638","usgsCitation":"U.S. Geological Survey, 1972, Water resources data for Iowa, water year 1971, https://doi.org/10.3133/70168638.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":318275,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United 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,{"id":70214098,"text":"70214098 - 1972 - Annual compilation and analysis of hydrologic data for Honey Creek, Trinity River Basin, Texas, 1970","interactions":[],"lastModifiedDate":"2021-12-20T18:54:34.337147","indexId":"70214098","displayToPublicDate":"1972-01-01T13:53:48","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":"Annual compilation and analysis of hydrologic data for Honey Creek, Trinity River Basin, Texas, 1970","docAbstract":"<p>The U.S. Soil Conservation Service is actively engaged in the installation of flood- and soil-erosion reducing measures in Texas under the authority of \"The Flood Control Act of 1936 and 1944\" and \"Watershed Protection and Flood Prevention Act\" (Public Law 566), as amended. The Soil Conservation Service has found a total of approximately 3,500 floodwater-retarding structures to be physically and economically feasible in Texas. As of September 30, 1970, 1,439 of these structures had been built.</p><p>This watershed-development program will have varying but important effects on the natural surface- and ground-water resources of river basins, especially where a large number of the floodwater-retarding structures are built. Basic hydrologic data under natural and developed conditions are needed to appraise the effects of the structures on the yield and mode of occurrence of runoff.</p><p>Hydrologic investigations of these small watershed study areas were begun by the U.S. Geological Survey in 1951 and are now being made in 12 areas (fig. 1). These investigations are being made in cooperation with the Texas Water Development Board, the Soil Conservation Service, the San Antonio River Authority, the city of Dallas, and the Tarrant County Water Control and Improvement District No. 1. The 12 study areas were chosen to sample watersheds having different rainfall, topography, geology, and soils. In five of the study areas (North, Little Elm, Mukewater, Little Pond-North Elm, and Pin Oak Creeks), streamflow and rainfall records were collected prior to construction of the floodwater-retarding structures, thus affording the opportunity for analyses of the conditions 'before and after\" development. Structures have now been built in four of these study areas. A summary of the development of the floodwater-retarding structures in each study area as of September 30, 1970, is shown in table 1.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70214098","collaboration":"Prepared in cooperation with the Texas Water Development Board and Soil Conservation Service","usgsCitation":"Hampton, B., 1972, Annual compilation and analysis of hydrologic data for Honey Creek, Trinity River Basin, Texas, 1970: Open-File Report, iv, 66 p., https://doi.org/10.3133/70214098.","productDescription":"iv, 66 p.","costCenters":[],"links":[{"id":393110,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70214098/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393109,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70214098/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Honey Creek, Trinity River Basin","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hampton, B.B.","contributorId":43362,"corporation":false,"usgs":true,"family":"Hampton","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":828720,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":70231050,"text":"70231050 - 1972 - Aerospace methods of revealing and evaluating Earth resources","interactions":[],"lastModifiedDate":"2022-04-29T15:42:50.886235","indexId":"70231050","displayToPublicDate":"1972-01-01T10:34:39","publicationYear":"1972","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Aerospace methods of revealing and evaluating Earth resources","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"International Workshop in Earth Resources Survey Systems","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"International Workshop in Earth Resources Survey Systems","conferenceDate":"May 3-7, 1971","conferenceLocation":"University of Michigan, Michigan, United States","language":"English","publisher":"National Aeronautics and Space Administration","usgsCitation":"Fischer, W., 1972, Aerospace methods of revealing and evaluating Earth resources, <i>in</i> International Workshop in Earth Resources Survey Systems, v. 1, University of Michigan, Michigan, United States, May 3-7, 1971, p. 39-54.","productDescription":"16 p.","startPage":"39","endPage":"54","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":399910,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":399909,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://ntrs.nasa.gov/citations/19730007621"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fischer, William A.","contributorId":47787,"corporation":false,"usgs":true,"family":"Fischer","given":"William A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":841805,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70121227,"text":"70121227 - 1972 - Acoustic-reflection profiles, eastern Greater Antilles: Leg 3, 1971 cruise, UNITEDGEO I","interactions":[],"lastModifiedDate":"2018-06-21T10:13:22","indexId":"70121227","displayToPublicDate":"1972-01-01T10:17:57","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Acoustic-reflection profiles, eastern Greater Antilles: Leg 3, 1971 cruise, UNITEDGEO I","docAbstract":"<h1>Introduction</h1><p>As part of a cooperative marine research program designated the Internataional Decade of Ocean Exploration (IDOE), the United states Geological Survey is participating in an investigation of the geologic framework and resource potential of continental margins and small ocean basins in the Gulf of Mexico, Caribbean Sea, and west African continental shelf areas. These studies are funded through the National Science Foundation. Legs 1 and 2, completed June 22 and July 8, respectively, were concerned with subbottom features of the Bay of Campeche and with the tectonic framework of the continental margin east of the Yucatan Peninsula. Leg 3, described in this report was conducted in the Antilles region of the northeastern Caribbean between July 17 and August 4, 1971.</p><p>This report presents the unedited records of the approximately 5840 km of acoustic reflection profiling made during Leg 3. Magnetic and gravity data were collected also but are being reported elsewhere in conjunction with the results of the study.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70121227","collaboration":"USGS-GD-72-004, PB-207-596","usgsCitation":"Garrison, L.E., 1972, Acoustic-reflection profiles, eastern Greater Antilles: Leg 3, 1971 cruise, UNITEDGEO I, 19 p., https://doi.org/10.3133/70121227.","productDescription":"19 p.","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292665,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":355152,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/89839/report.pdf","text":"Report","size":"20.2 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Unumbered Series 89839"}],"otherGeospatial":"Caribbean Sea;Greater Antilles","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.37,16.44 ], [ -79.37,23.38 ], [ -65.22,23.38 ], [ -65.22,16.44 ], [ -79.37,16.44 ] ] ] } } ] }","contact":"<p><a href=\"https://woodshole.er.usgs.gov/\" data-mce-href=\"https://woodshole.er.usgs.gov/\">Coastal and Marine Geology Program</a><br> U.S. Geological Survey<br> 384 Woods Hole Road<br> Woods Hole, MA 02543</p>","tableOfContents":"<ul><li>Introduction</li><li>Scientific Party</li><li>Ship Schedule</li><li>Objectives of Investigation</li><li>Geologic Setting</li><li>Preliminary Results</li><li>References</li><li>Operational Data</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f5b64ae4b09d12e0e8e650","contributors":{"authors":[{"text":"Garrison, Louis E.","contributorId":91793,"corporation":false,"usgs":true,"family":"Garrison","given":"Louis","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":498830,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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