{"pageNumber":"2314","pageRowStart":"57825","pageSize":"25","recordCount":68867,"records":[{"id":10854,"text":"ofr77150 - 1977 - A brief investigation of the surface-water hydrology of Yemen Arab Republic","interactions":[],"lastModifiedDate":"2019-04-26T09:10:54","indexId":"ofr77150","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-150","title":"A brief investigation of the surface-water hydrology of Yemen Arab Republic","docAbstract":"Yemen, near the southwest tip of the Arabian Peninsula, is a mountainous country bordered by a desert on the east and a coastal plain on the west. Rainfall is low and seasonal; consequently, most streams (wadis) are ephemeral. The natural flow regimens of many of the smaller wadis are modified by terracing for agriculture. The only streamflow data available in Yemen are short records on four large wadis. A brief field investigation and application of reconnaissance techniques are the bases for the largely qualitative description of the hydrology, and for the proposal to collect streamflow data needed for orderly development of the expanding economy. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77150","usgsCitation":"Riggs, H.C., 1977, A brief investigation of the surface-water hydrology of Yemen Arab Republic: U.S. Geological Survey Open-File Report 77-150, iv, 37 p. , https://doi.org/10.3133/ofr77150.","productDescription":"iv, 37 p. ","costCenters":[],"links":[{"id":363243,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0150/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0150/report-thumb.jpg"}],"country":"Yemen","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd497ae4b0b290850ef37d","contributors":{"authors":[{"text":"Riggs, Henry Chiles","contributorId":44129,"corporation":false,"usgs":true,"family":"Riggs","given":"Henry","email":"","middleInitial":"Chiles","affiliations":[],"preferred":false,"id":162078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8601,"text":"ofr77817 - 1977 - Late diagenetic indicators of buried oil and gas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr77817","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-817","title":"Late diagenetic indicators of buried oil and gas","docAbstract":"At least three hydrocarbon seepage mechanisms are interpreted to operate over oil and gas fields. These are: (1) effusion ofh ydrocarbons through inadequate caprocks and along faults and fractures, (2) low-molecular-weight hydrocarbons dissolved in water moving vertically through capping shales as a result of a hydrodynamic or chemical potential drive, and (3) diffusion of gases dissolved in water. Combinations of these mechanisms may also occur. \r\n\r\nSeeping hydrocarbons are oxidized near the earth's surface, and the resulting carbon dioxide reacts with water producing bicarbonate ions, which combine with calcium and magnesium dissolved in ground waters to yield isotopically distinctive pore-filling carbonate cements and surface rocks. The passage of hydrocarbons and associated compounds such as hydrogen sulfide through surface rocks causes a reducing environment and consequent reduction, mobilization, and loss of iron from iron-bearing minerals commonly resulting in a discoloration. Other metals such as manganese are also mobilized and redistributed. These changes in the physical and chemical properties of surface rocks correlate with the subsurface distribution of petroleum, and potentially can be detected from both airborne and spaceborne platforms.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77817","usgsCitation":"Donovan, T.J., and Dalziel, M.C., 1977, Late diagenetic indicators of buried oil and gas: U.S. Geological Survey Open-File Report 77-817, 44 leaves :ill., map ;28 cm.; (79 p. - PGS), https://doi.org/10.3133/ofr77817.","productDescription":"44 leaves :ill., map ;28 cm.; (79 p. - PGS)","costCenters":[],"links":[{"id":141034,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0817/report-thumb.jpg"},{"id":36198,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0817/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8be2","contributors":{"authors":[{"text":"Donovan, Terrence J.","contributorId":71529,"corporation":false,"usgs":true,"family":"Donovan","given":"Terrence","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158011,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dalziel, Mary C.","contributorId":103663,"corporation":false,"usgs":true,"family":"Dalziel","given":"Mary","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":158012,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8148,"text":"ofr77633 - 1977 - Surficial and applied surficial geology of the Belchertown Quadrangle, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr77633","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-633","title":"Surficial and applied surficial geology of the Belchertown Quadrangle, Massachusetts","docAbstract":"Till and stratified drift overlie maturely dissected topography in the Belchertown quadrangle, an area that straddles the New England Upland and Connecticut Valley Lowland in central Massachusetts. Lower Paleozoic, massive quartzo-feldspathic gneiss, quartzite and schist of the Pelham dome and Devonian granodiorite and quartz diorite of the Belchertown intrusive complex are in contact with Triassic arkosic fanglomerate and basalt along a lengthy normal fault separating the New England Upland from the Connecticut Valley Lowland. The orientation of striae, roches moutonnees, and streamline ridges indicate that the last Wisconsinian glacier advanced generally south 12? east. This glacier removed several meters of rock from the upland and an unknown larger quantity from the preglacial valley of the Connecticut River. Till is thin in the uplands, but several tens of feet of drift overlie bedrock in the lowland.\r\n\r\nThree lithic facies of sandy, clast-rich, non-compact, subarkosic till derived from the three major source rocks rest on bedrock or on highly weathered, compact, clast-poor, fissile probably older till. The mean for all upper till is 69.6% sand, 21.7% silt, and 8.8% clay; lower till consists of 48% sand, 23% silt and 29% clay. Mud-rich, compact, sparsely stony till in drumlins in and along the flank of the Connecticut Valley Lowland is composed of 51.5% sand, 28% silt, and 20.5% clay. Upper tills are facies equivalent deposits of the youngest Wisconsinian drift. Lower till is compact deeply weathered, jointed and stained suggesting it is correlative with other lower till in New England deposited by an earlier Wisconsinian glacier. Drumlin till may be a facies equivalent of a lower till or a mud-rich upper till derived from earlier glaciolacustrine deposits.\r\n\r\nUpper and lower till of the Belchertown quadrangle is texturally similar to other New England upper and lower tills to which they are equivalent. Both tills are interpreted as lodgment till derived from similar bedrock terrane by two different glaciers. The older glacier incorporated mud-rich saprolite producing a fine grained till, while the younger glacier eroded fresh bedrock or a thin regolith produced by mechanical weathering.\r\n\r\nDuring stagnation zone retreat of the last glacier, stratified drift was deposited by melt water in, on, alongside or down valley from stagnant ice. The absence of stratified drift along upland divides indicates that stagnation did not begin till large nunataks were emergent. Kame terraces, kame deltas, and ice channel fillings indicate that melt water flowed along stagnant ice and emptied into temporary proglacial lakes. As downwasting progressed, water was able to drain at lower elevation into expanding lakes, the last of which merged with northward-expanding proglacial Lake Hitchcock in the Connecticut Valley. Initial melt water drainage to the southeast was followed by drainage to the southwest to the ancestral Chicopee River. With the opening of the Narrows, Lake Hitchcock expanded northward and eastward to form the Amherst embayment into which melt water from the eastern uplands drained. Sand and gravel overlying varves in the Amherst embayment was deposited in late-glacial Lake Lawrence, which coalesced with equivalent Lake Hadley through cols between drumlins in the Connecticut Valley Lowland.\r\n\r\nDeglaciation of the Belchertown quadrangle probably occurred in a span of about 100 years in the interval 12,000 to 12,500 years B.P.\r\n\r\nUnconsolidated sediments of the Belchertown quadrangle are summarized as to their geologic and geotechnical properties for land use planning. Drift as it influences groundwater flow, yield, and quality and as a construction material is assessed. Some environmental degradation has occurred from the indiscriminant disposal of liquid and solid waste as well as injudicious use of road salt.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77633","usgsCitation":"Caggiano, J.A., 1977, Surficial and applied surficial geology of the Belchertown Quadrangle, Massachusetts: U.S. Geological Survey Open-File Report 77-633, ca. 150 leaves :ill., maps (4 fold., 2 col.) ;28 cm.; (122 p., 5 sheets - PGS), https://doi.org/10.3133/ofr77633.","productDescription":"ca. 150 leaves :ill., maps (4 fold., 2 col.) ;28 cm.; (122 p., 5 sheets - PGS)","costCenters":[],"links":[{"id":141468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0633/report-thumb.jpg"},{"id":35751,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0633/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35752,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0633/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35753,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0633/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35754,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0633/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35755,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0633/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35756,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0633/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689f1d","contributors":{"authors":[{"text":"Caggiano, Joseph A.","contributorId":38555,"corporation":false,"usgs":true,"family":"Caggiano","given":"Joseph","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":157228,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10005,"text":"ofr77624 - 1977 - Natural radioactivity in geothermal waters, Alhambra Hot Springs and nearby areas, Jefferson County, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr77624","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-624","title":"Natural radioactivity in geothermal waters, Alhambra Hot Springs and nearby areas, Jefferson County, Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77624","usgsCitation":"Leonard, R.B., and Janzer, V.J., 1977, Natural radioactivity in geothermal waters, Alhambra Hot Springs and nearby areas, Jefferson County, Montana: U.S. Geological Survey Open-File Report 77-624, iii, 20 leaves :ill., map ;27 cm.; (32 p. - PGS), https://doi.org/10.3133/ofr77624.","productDescription":"iii, 20 leaves :ill., map ;27 cm.; (32 p. - PGS)","costCenters":[],"links":[{"id":142599,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698100","contributors":{"authors":[{"text":"Leonard, Robert Benjamin","contributorId":15617,"corporation":false,"usgs":true,"family":"Leonard","given":"Robert","email":"","middleInitial":"Benjamin","affiliations":[],"preferred":false,"id":160662,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Janzer, Victor J.","contributorId":36119,"corporation":false,"usgs":true,"family":"Janzer","given":"Victor","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":160663,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11791,"text":"ofr77418 - 1977 - Water resources of the Weiser River basin, west-central Idaho","interactions":[{"subject":{"id":11791,"text":"ofr77418 - 1977 - Water resources of the Weiser River basin, west-central Idaho","indexId":"ofr77418","publicationYear":"1977","noYear":false,"title":"Water resources of the Weiser River basin, west-central Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":70047715,"text":"70047715 - 1977 - Water resources of the Weiser River basin, west-central Idaho","indexId":"70047715","publicationYear":"1977","noYear":false,"title":"Water resources of the Weiser River basin, west-central Idaho"},"id":1}],"supersededBy":{"id":70047715,"text":"70047715 - 1977 - Water resources of the Weiser River basin, west-central Idaho","indexId":"70047715","publicationYear":"1977","noYear":false,"title":"Water resources of the Weiser River basin, west-central Idaho"},"lastModifiedDate":"2013-08-20T10:35:57","indexId":"ofr77418","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-418","title":"Water resources of the Weiser River basin, west-central Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77418","usgsCitation":"Young, H., Harenberg, W.A., and Seitz, H.R., 1977, Water resources of the Weiser River basin, west-central Idaho: U.S. Geological Survey Open-File Report 77-418, 92, [96] leaves :ill., maps ;40 cm.; (188 p. - PGS), https://doi.org/10.3133/ofr77418.","productDescription":"92, [96] leaves :ill., maps ;40 cm.; (188 p. - PGS)","costCenters":[],"links":[{"id":144798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6985e2","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":163738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harenberg, William A.","contributorId":31773,"corporation":false,"usgs":true,"family":"Harenberg","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":163736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Seitz, Harold R.","contributorId":61814,"corporation":false,"usgs":true,"family":"Seitz","given":"Harold","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":163737,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8615,"text":"ofr7780 - 1977 - Ground-water data for 1974-75 in Joshua Tree National Monument, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr7780","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-80","title":"Ground-water data for 1974-75 in Joshua Tree National Monument, California","docAbstract":"This report, prepared at the request of the National Park Service, is part of a continuing inventory by the U.S. Geological Survey of general geohydrologic conditions at Joshua Tree National Monument, California. Tables of data for 1974-75 includes chemical analyses of ground water from selected wells and pumpage by Kaiser Steel Corporation from Pinto Basin. The table for yearly pumpage totals by Kaiser Steel Corporation includes years 1960-75. Water-level measurements are included for 22 observation wells. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7780","usgsCitation":"Downing, D., 1977, Ground-water data for 1974-75 in Joshua Tree National Monument, California: U.S. Geological Survey Open-File Report 77-80, iii, 34 leaves :ill., maps ;27 cm.; (39 p. - PGS), https://doi.org/10.3133/ofr7780.","productDescription":"iii, 34 leaves :ill., maps ;27 cm.; (39 p. - PGS)","costCenters":[],"links":[{"id":141083,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cfcf","contributors":{"authors":[{"text":"Downing, D.J.","contributorId":56217,"corporation":false,"usgs":true,"family":"Downing","given":"D.J.","email":"","affiliations":[{"id":16649,"text":"Oak Ridge National Laboratory, Environmental Sciences Division, Oak Ridge, TN 37831-6335, USA","active":true,"usgs":false}],"preferred":false,"id":158033,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8268,"text":"ofr76885 - 1977 - Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1975","interactions":[],"lastModifiedDate":"2017-06-14T13:27:01","indexId":"ofr76885","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"76-885","title":"Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1975","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76885","usgsCitation":"Choffel, K., Roddy, W., and Mitchell, R., 1977, Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1975: U.S. Geological Survey Open-File Report 76-885, 126 p., https://doi.org/10.3133/ofr76885.","productDescription":"126 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":140097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"Austin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683259","contributors":{"authors":[{"text":"Choffel, K.L.","contributorId":31254,"corporation":false,"usgs":true,"family":"Choffel","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":157459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roddy, W.R.","contributorId":27453,"corporation":false,"usgs":true,"family":"Roddy","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":157458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mitchell, R.N.","contributorId":94301,"corporation":false,"usgs":true,"family":"Mitchell","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":157460,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11808,"text":"ofr77744 - 1977 - Uranium mobility during interaction of rhyolitic glass with alkaline solutions: dissolution of glass","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr77744","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-744","title":"Uranium mobility during interaction of rhyolitic glass with alkaline solutions: dissolution of glass","docAbstract":"This report concerns investigations designed to identify the important physical and chemical parameters influencing the rate of release of uranium from glass shards of rhyolitic air-fall ash. Oxidizing, silica undersaturated, alkaline solutions are eluted through a column of rhyolitic glass shards at a carefully controlled temperature, pressure, and flow rate. The solutions are monitored for the concentration of uranium and selected additional elements (Si, K, Li, F), and the glass is recovered and examined for physical and/or chemical evidence of attack. The flushing mode is designed to mimic leaching of glass shards by intermittent, near-surface waters with which the glass is not in equilibrium. \r\n\r\nReported rates are applicable only to the experimental conditions (120?C, 7,000 psi), but it is assumed that the reaction mechanisms and the relative importance of rate-influencing parameters remain unchanged, at reduced temperature and pressure. Results of the above experiment indicate that silica and uranium are released from glass shards at comparable rates, while lithium and potassium are released faster and fluorine slower than either Si or U. Rates of release of silica and uranium correlate positively with the surface area of the shards. Rhyolitic shards release uranium at faster rates than rhyodacitic shards of comparable surface area. Changes in the shards resulting from experimental treatment and observed in the original glass separates from an Oligocene ash (compared to a Pleistocene ash) include; surface pitting, increased surface area, devitrification rinds (<1l micron wide) and reduced lithium contents. Future investigations will study the effect of temperature, pressure, solution composition, and flow rate on the relative mobility of U, Si, Li, F, and K.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77744","usgsCitation":"Zielinski, R.A., 1977, Uranium mobility during interaction of rhyolitic glass with alkaline solutions: dissolution of glass: U.S. Geological Survey Open-File Report 77-744, 36, [5] leaves of plates :ill. ;28 cm.; (41 p. - PGS), https://doi.org/10.3133/ofr77744.","productDescription":"36, [5] leaves of plates :ill. ;28 cm.; (41 p. - PGS)","costCenters":[],"links":[{"id":145048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0744/report-thumb.jpg"},{"id":39701,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0744/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60541a","contributors":{"authors":[{"text":"Zielinski, Robert A. 0000-0002-4047-5129 rzielinski@usgs.gov","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":1593,"corporation":false,"usgs":true,"family":"Zielinski","given":"Robert","email":"rzielinski@usgs.gov","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":163765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10849,"text":"ofr78123 - 1977 - Atlantic Margin Coring Project 1976: Preliminary Report on Shipboard and Some Laboratory Geotechnical data","interactions":[],"lastModifiedDate":"2018-06-18T15:28:59","indexId":"ofr78123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"78-123","title":"Atlantic Margin Coring Project 1976: Preliminary Report on Shipboard and Some Laboratory Geotechnical data","docAbstract":"<p>This report presents reduced shipboard geotechnical data collected during the 1976 Atlantic Margin Coring Project; results of laboratory tests of specific gravity, water content, bulk density, and Atterberg limits; and sedimentation-compression e log p curves showing consolidation. A description of the procedures used at sea and in the laboratory and a short preliminary summary of the shipboard results also is included.</p><p>The involvement of Marine Geotechnical Laboratory (MGL), Lehigh University, personnel in the 1976 Atlantic Margin Coring Project can be divided into two phases. In Phase One, the Lehigh nuclear-transmission densitometer was rebuilt to process cores at sea more rapidly than previously had been done in the laboratory, the equipment was assembled and tested aboard the Glomar Conception, and at-sea geotechnical measurements were made during the duration of the cruise.</p><p>Data sheets were prepared for both unopened core sections (Appendix III) and split-core samples (Appendix IV). Completed data forms are on file at the MGL and at the Geological Survey in Woods Hole.</p><p>Phase Two included reduction of the shipboard data, testing of all geotechnical samples taken from cores split aboard the ship, and certain other analytical work ashore utilizing the geotechnical measurements. Water content and weight/volume bulk density tests were performed at the MGL. Specific gravity and Atterberg limit tests and certain calculations were performed by Geological Survey personnel at the Corpus Christi, Texas, laboratory.</p><p>During Phase One, 37 unopened, 1.5-m-long core sections were selected by Lehigh personnel for subsequent static and dynamic triaxial and consol­idation testing ashore. The disposition of these cores is controlled by Geological Survey Project personnel; they are not further discussed in this report.</p><p>A depth convention has been adopted in this report for the convenience of labeling core sections and analyzing the data. Each 9.2-m-long (30 ft) core liner had a maximum penetration depth referenced to the water-sediment interface; these data are given in Hathaway, et al. (1976). Each 9.2-m-long core liner was cut into six or fewer sections, each 1.5 m (5 ft) in length, aboard the ship. To the maximum penetration depth, 0.2 m was subtracted to obtain the depth at the bottom of the first 1.5 m section above the core catcher. To obtain values at the bottom of the remaining 1.5 m sections, an additional 1.5 m was added for each section. The depth of the bottom of each core section was used for all values obtained using the nuclear densitometer. Tests within core sections and samples collected from core sections were assigned depths based on the location of the test or sample within the core section. It should be clearly recognized that all depths within a 9.2-m-long core are estimates of the true depth, which cannot be uniquely calculated because of the uncertainty of the relationship of sediment contained within the core liner to true in situ depths.</p><p>This report is considered to be preliminary because the author has not had access to the final lithologic logs or paleontological results, upon which a more accurate description of geotechnical results could be based. It would be inappropriate to comment on geological hazards until this information is made available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr78123","usgsCitation":"Richards, A.F., 1977, Atlantic Margin Coring Project 1976: Preliminary Report on Shipboard and Some Laboratory Geotechnical data: U.S. Geological Survey Open-File Report 78-123, 165 p. in various pagings :ill. ;28 cm.; (166 p. - PGS), https://doi.org/10.3133/ofr78123.","productDescription":"165 p. in various pagings :ill. ;28 cm.; (166 p. - PGS)","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":144827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259889,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0123/ofr1978123.pdf","text":"Report","size":"4.06 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1978-123"}],"country":"United States","otherGeospatial":"Atlantic Ocean","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.88,25.0 ], [ -82.88,42.64 ], [ -67.0,42.64 ], [ -67.0,25.0 ], [ -82.88,25.0 ] ] ] } } ] }","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>Foreword&nbsp;</li><li>Introduction&nbsp;</li><li>Core quality evaluation</li><li>Shipboard geotechnical tests</li><li>Laboratory geotechnical tests</li><li>Downhole density logging</li><li>Sedimentation-compression curve analysis</li><li>Results&nbsp;</li><li>References</li><li>Appendices</li><li><br data-mce-bogus=\"1\"></li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b33b","contributors":{"authors":[{"text":"Richards, Adrian F.","contributorId":91114,"corporation":false,"usgs":true,"family":"Richards","given":"Adrian","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":162071,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11813,"text":"ofr7756 - 1977 - Ground-water resources and geology of Colquitt County, Georgia","interactions":[],"lastModifiedDate":"2016-12-14T10:12:07","indexId":"ofr7756","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-56","title":"Ground-water resources and geology of Colquitt County, Georgia","docAbstract":"<p>Limestone beds of Eocene, Oligocene, and lower Miocene age, called the principal artesian aquifer, are the chief source of ground water for Colquitt County. Because streams are small, undependable and relatively inaccessible to most users, ground water is the most important source for increased industrial and agricultural water use. Southeast of Moultrie the principal artesian aquifer is very productive, and has transmissivity in excess of 145,000 feet squared per day (13,500 meters squared per day). A structural or paleogeographic feature called the Suwannee strait traverses the county from near the southwest corner to the northeast corner. In this strait, limestone in the principal artesian aquifer is partly replaced by fine-grained clastic sediment, impairing transmissivity and making wells hard to construct. Transmissivity is much lower northwest of the strait than it is southeast, probably because of facies changes in the aquifer.</p>\n<p>In the belt of the hypothesized Ochlockonee fault, water containing greater-than-usual concentrations of dissolved solids is produced. This anomaly could be the result of the fault having acted as a conduit when the vertical hydraulic gradient was upward from a deeper aquifer, or be the result of the movement of ground water from a sulfate-rich source in the sediments of the Suwannee strait. In south-central Colquitt County, clay-capped permeable beds extending above potentiometric surfaces create conditions favorable for breathing wells.</p>\n<p>Predominantly clastic beds of Miocene age overlie the Suwannee Limestone. These beds have a transmissivity of about 2,280 feet squared per day (215 meters squared per day), but they are of comparatively little importance because larger yields can be obtained from the underlying principal artesian aquifer. Moreover, wells are difficult to construct in the poorly consolidated clastic sediments, and water from these shallow beds is likely to be depleted during droughts.</p>\n<p>The ground water is generally hard, but is otherwise of good quality. One exception is near the hypothesized Ochlockonee fault where water contains higher-than-usual concentrations of various ions, especially sulfate. Another exception occurs along the axis of the Suwannee strait where clay minerals in the channel facies may soften the water by ion exchange.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Doraville, Georgia","doi":"10.3133/ofr7756","collaboration":"Prepared in cooperation with Georgia Department of Natural Resources, Geologic and Water Resources Division","usgsCitation":"Zimmerman, E.A., 1977, Ground-water resources and geology of Colquitt County, Georgia: U.S. Geological Survey Open-File Report 77-56, vi, 41 p., https://doi.org/10.3133/ofr7756.","productDescription":"vi, 41 p.","numberOfPages":"52","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":144821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr7756.jpg"},{"id":325511,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","county":"Colquitt 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E. A.","contributorId":75533,"corporation":false,"usgs":true,"family":"Zimmerman","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":163774,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10840,"text":"ofr77154 - 1977 - Water-quality data for Nassau and Suffolk counties, New York: July 1974 through September 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr77154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-154","title":"Water-quality data for Nassau and Suffolk counties, New York: July 1974 through September 1975","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77154","usgsCitation":"Reynolds, R.J., and Ragone, S.E., 1977, Water-quality data for Nassau and Suffolk counties, New York: July 1974 through September 1975: U.S. Geological Survey Open-File Report 77-154, 99 leaves :ill., maps (some fold., 1 in pocket) ;28 cm.; (38 p. - PGS), https://doi.org/10.3133/ofr77154.","productDescription":"99 leaves :ill., maps (some fold., 1 in pocket) ;28 cm.; (38 p. - PGS)","costCenters":[],"links":[{"id":145727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6a7a","contributors":{"authors":[{"text":"Reynolds, Richard J. 0000-0001-5032-6613 rjreynol@usgs.gov","orcid":"https://orcid.org/0000-0001-5032-6613","contributorId":1082,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rjreynol@usgs.gov","middleInitial":"J.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":162058,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ragone, Stephen E.","contributorId":74374,"corporation":false,"usgs":true,"family":"Ragone","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":162059,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11346,"text":"ofr77204 - 1977 - Index of published surface-water quality data for Oklahoma 1946-1975","interactions":[],"lastModifiedDate":"2017-09-29T08:05:10","indexId":"ofr77204","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-204","title":"Index of published surface-water quality data for Oklahoma 1946-1975","docAbstract":"Surface-water-quality data for Oklahoma have been published by the U.S. Geological Survey in cooperation with various State agencies on an annual basis since 1949. The published data represents 2,733 station-years of data from 527 stations, ranging from one sample from a station once during the thirty--year period to a continuously operating daily station were more than one hundred samples were collected in a year. The last comprehensive index was published in 1963; since that time various unpublished indexes have been in use, none of which were complete.\r\nMost of the water-quality data collected and published prior to 1970 was for the common inorganic constituents such as, calcium, magnesium, sodium, alkalinity, chloride and sulfate. Since 1970 other types of data such as the minor or trace metals, organic compounds including pesticides, nutrients, oxygen resources, and biologic information have been collected and published with ever increasing frequency.\r\n\r\nThis index was designed to provide the data user a means of rapid search for stations by downstream order (Table 2), county (Table 4), and alphabetically by stream or station name (Table 1). Table 1 also provides a breakdown of the data into 10 broad water-quality categories.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77204","usgsCitation":"Stoner, J.D., 1977, Index of published surface-water quality data for Oklahoma 1946-1975: U.S. Geological Survey Open-File Report 77-204, 212 p., https://doi.org/10.3133/ofr77204.","productDescription":"212 p.","numberOfPages":"219","costCenters":[],"links":[{"id":143323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0204/report-thumb.jpg"},{"id":346199,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0204/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efa79","contributors":{"authors":[{"text":"Stoner, Jerry D.","contributorId":38611,"corporation":false,"usgs":true,"family":"Stoner","given":"Jerry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":162971,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8675,"text":"ofr77487 - 1977 - Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma","interactions":[{"subject":{"id":8675,"text":"ofr77487 - 1977 - Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma","indexId":"ofr77487","publicationYear":"1977","noYear":false,"title":"Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70046142,"text":"70046142 - 1986 - Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water","indexId":"70046142","publicationYear":"1986","noYear":false,"title":"Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water"},"id":1}],"supersededBy":{"id":70046142,"text":"70046142 - 1986 - Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water","indexId":"70046142","publicationYear":"1986","noYear":false,"title":"Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water"},"lastModifiedDate":"2017-09-29T07:58:43","indexId":"ofr77487","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-487","title":"Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma","docAbstract":"<p>Most of the data presented in this report were collected by the U.S. Geological Survey as part of a study of the geohydrology of the Vamoosa aquifer, in east-central Oklahoma, in cooperation with the Oklahoma Geological Survey. Some of the data listed in the tables were collected by Bingham and Moore (1975) and Bingham and Bergman (in press).</p><p>Acknowledgment is extended to city officials and individuals who provided the data for this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77487","usgsCitation":"D’Lugosz, J.J., and McClaflin, R.G., 1977, Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma: U.S. Geological Survey Open-File Report 77-487, iii, 38 p., https://doi.org/10.3133/ofr77487.","productDescription":"iii, 38 p.","numberOfPages":"43","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"links":[{"id":142224,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0487/report-thumb.jpg"},{"id":346195,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0487/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oklahoma","otherGeospatial":"Vamoosa Aquifer","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.3006,36.1632],[-96.3002,36.1577],[-96.2991,36.0778],[-96.085,36.0773],[-96.0281,36.0764],[-96.0288,36.0006],[-96.0286,35.9906],[-96.0304,35.9026],[-96.0326,35.9027],[-96.0319,35.8565],[-96.1928,35.8589],[-96.1936,35.6365],[-96.1944,35.553],[-96.0898,35.5532],[-96.0892,35.3756],[-95.9803,35.3751],[-95.9809,35.2896],[-96.4413,35.2902],[-96.4393,35.1158],[-96.4932,35.116],[-96.4944,35.0275],[-96.4961,34.9076],[-96.5043,34.8978],[-96.5046,34.8878],[-96.5128,34.8775],[-96.5237,34.8678],[-96.5344,34.8671],[-96.5437,34.875],[-96.5585,34.9026],[-96.5572,34.9085],[-96.5608,34.919],[-96.5675,34.9205],[-96.5749,34.9156],[-96.585,34.9163],[-96.5872,34.9159],[-96.5924,34.911],[-96.5975,34.9088],[-96.6045,34.9031],[-96.6186,34.9006],[-96.6337,34.8996],[-96.646,34.9016],[-96.6559,34.9068],[-96.658,34.9123],[-96.6615,34.9274],[-96.6726,34.9312],[-96.6831,34.9364],[-96.6932,34.9357],[-96.7017,34.9314],[-96.7081,34.9242],[-96.715,34.9189],[-96.7146,34.9139],[-96.7074,34.9092],[-96.6986,34.9036],[-96.6927,34.8953],[-96.6891,34.8866],[-96.6921,34.8776],[-96.6951,34.8726],[-96.7032,34.8646],[-96.706,34.8633],[-96.7151,34.858],[-96.732,34.8566],[-96.7391,34.8612],[-96.7411,34.8694],[-96.7465,34.8782],[-96.7529,34.8906],[-96.7549,34.897],[-96.7626,34.9026],[-96.7681,34.9054],[-96.7783,34.9015],[-96.7823,34.8988],[-96.7896,34.899],[-96.7912,34.9004],[-96.7989,34.9087],[-96.8005,34.9119],[-96.7998,34.9142],[-96.7998,34.9332],[-96.8013,34.9396],[-96.8035,34.9419],[-96.8197,34.9431],[-96.8237,34.9428],[-96.8311,34.9393],[-96.8329,34.9357],[-96.8346,34.9348],[-96.8397,34.9326],[-96.8419,34.9336],[-96.843,34.9354],[-96.8446,34.9363],[-96.8599,34.9294],[-96.8668,34.9268],[-96.8785,34.9265],[-96.8902,34.9295],[-96.8991,34.9337],[-96.9041,34.937],[-96.9051,34.9406],[-96.9033,34.9456],[-96.906,34.9497],[-96.9087,34.952],[-96.9086,34.9548],[-96.9096,34.9598],[-96.914,34.963],[-96.9218,34.9654],[-96.933,34.9665],[-96.9431,34.9658],[-96.9494,34.9618],[-96.9563,34.9533],[-96.9627,34.9448],[-96.9662,34.9403],[-96.9685,34.9376],[-96.9709,34.935],[-96.9817,34.9265],[-96.9921,34.9176],[-97.0068,34.9106],[-97.0147,34.9094],[-97.0169,34.9099],[-97.0253,34.9104],[-97.0453,34.918],[-97.0537,34.9205],[-97.0621,34.9202],[-97.0715,34.9244],[-97.0797,34.9318],[-97.0859,34.9328],[-97.1027,34.9313],[-97.1161,34.9356],[-97.1285,34.9344],[-97.1432,34.9305],[-97.1433,35.2021],[-97.1405,35.202],[-97.1442,35.3742],[-97.1437,35.4645],[-97.1452,35.6361],[-97.1436,35.7246],[-97.1438,35.8112],[-97.1433,35.8988],[-97.1405,35.8988],[-97.1409,35.9283],[-97.1428,35.9442],[-97.1423,35.9641],[-97.1557,35.9485],[-97.1729,35.9428],[-97.1872,35.9426],[-97.2013,35.9469],[-97.2163,35.9576],[-97.2252,35.9677],[-97.236,35.9683],[-97.2461,35.9721],[-97.2523,35.9744],[-97.2734,35.9734],[-97.2841,35.9767],[-97.2863,35.9795],[-97.2862,35.9835],[-97.2883,35.9931],[-97.2927,36.0004],[-97.2982,36.0091],[-97.3055,36.011],[-97.3203,36.0108],[-97.3329,36.0078],[-97.3359,36.0024],[-97.34,35.9947],[-97.3475,35.9885],[-97.3556,35.9841],[-97.3569,36.1583],[-97.1426,36.1588],[-97.1417,36.245],[-96.9277,36.246],[-96.9276,36.3313],[-97.0338,36.3326],[-97.0333,36.5059],[-97.0116,36.506],[-97.0109,36.5105],[-97.0096,36.5155],[-97.0083,36.5204],[-97.0025,36.5249],[-96.9978,36.5275],[-96.9915,36.5292],[-96.988,36.531],[-96.9828,36.5327],[-96.977,36.5344],[-96.9667,36.5352],[-96.9564,36.535],[-96.9506,36.5367],[-96.946,36.538],[-96.939,36.5424],[-96.9355,36.5455],[-96.929,36.5513],[-96.9261,36.554],[-96.9243,36.554],[-96.9175,36.5529],[-96.906,36.5536],[-96.9003,36.554],[-96.8968,36.5553],[-96.8921,36.5597],[-96.8909,36.5634],[-96.8873,36.5683],[-96.8866,36.5732],[-96.8876,36.5792],[-96.8932,36.5824],[-96.9034,36.5867],[-96.9162,36.6001],[-96.9387,36.5959],[-96.9468,36.5911],[-96.9526,36.5889],[-96.9549,36.589],[-96.9612,36.5882],[-96.974,36.5843],[-96.982,36.583],[-96.986,36.5827],[-96.9952,36.5837],[-97.0032,36.5839],[-97.0153,36.5827],[-97.029,36.5847],[-97.0415,36.5858],[-97.0512,36.5883],[-97.0568,36.5929],[-97.055,36.5979],[-97.0532,36.601],[-97.0469,36.6018],[-97.0473,36.6054],[-97.049,36.6068],[-97.0547,36.6106],[-97.0551,36.6165],[-97.0528,36.6364],[-97.0617,36.651],[-97.0656,36.6547],[-97.067,36.6656],[-97.0666,36.6829],[-97.0606,36.6918],[-97.0548,36.6926],[-97.0491,36.6939],[-97.0253,36.7012],[-97.0238,36.6953],[-97.017,36.6907],[-97.0038,36.6909],[-96.994,36.6903],[-96.9878,36.6875],[-96.9682,36.6889],[-96.958,36.6865],[-96.9477,36.6836],[-96.9345,36.6852],[-96.9263,36.691],[-96.9262,36.6937],[-96.9267,36.6982],[-96.9254,36.7014],[-96.9206,36.7085],[-96.9204,36.7176],[-96.9151,36.7216],[-96.9061,36.7351],[-96.8907,36.7525],[-96.8786,36.7536],[-96.8689,36.7521],[-96.8604,36.7483],[-96.849,36.7445],[-96.8404,36.7434],[-96.8248,36.7472],[-96.8218,36.7531],[-96.821,36.7589],[-96.822,36.7662],[-96.8133,36.7665],[-96.8041,36.7663],[-96.7967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Joseph J.","contributorId":71172,"corporation":false,"usgs":true,"family":"D’Lugosz","given":"Joseph","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McClaflin, Roger G.","contributorId":50157,"corporation":false,"usgs":true,"family":"McClaflin","given":"Roger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":158137,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11194,"text":"ofr7783 - 1977 - Hydrologic data for Little Elm Creek, Trinity River basin, Texas, 1975","interactions":[],"lastModifiedDate":"2022-02-04T19:35:43.046325","indexId":"ofr7783","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-83","title":"Hydrologic data for Little Elm Creek, Trinity River basin, Texas, 1975","docAbstract":"<p>This report contains rainfall, runoff, and storage data collected during the 1975 water year for a 75.5 sq mi area above the stream-gaging station Little Elm Creek near Aubrey, Texas. Floodflows from 35.7 sq mi of the area are regulated by 16 floodwater-retarding structures constructed by the Soil Conservation Service. Six storm periods were selected for detailed computations and analyses. Water-quality data is given for Little Elm Creek. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7783","collaboration":"Prepared in cooperation with the city of Dallas and the Texas Water Development Board","usgsCitation":"Slade, R., and Taylor, J., 1977, Hydrologic data for Little Elm Creek, Trinity River basin, Texas, 1975: U.S. Geological Survey Open-File Report 77-83, 108 p., https://doi.org/10.3133/ofr7783.","productDescription":"108 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":144714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0083/report-thumb.jpg"},{"id":395466,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0083/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Little Elm Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e927","contributors":{"authors":[{"text":"Slade, R.M. Jr.","contributorId":40595,"corporation":false,"usgs":true,"family":"Slade","given":"R.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":162707,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, J.M.","contributorId":42587,"corporation":false,"usgs":true,"family":"Taylor","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":162706,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10138,"text":"ofr77618 - 1977 - Seepage tests on No Name Creek, Colville Indian Reservation, Washington, May 12-13, 1977","interactions":[],"lastModifiedDate":"2019-04-26T09:27:20","indexId":"ofr77618","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-618","title":"Seepage tests on No Name Creek, Colville Indian Reservation, Washington, May 12-13, 1977","docAbstract":"To gain information for a water-management situation, a seepage test was performed on May 12-13, 1977, on a reach of No Name Creek on the Colville Indian Reservation in north-central Washington. On May 13, injection of a concentrated brine at the head of the test reach permitted chloride-concentration data to be combined with the discharge measurements made to define the pattern of gain and loss along the reach. Equations describing discharge and chloride mass balance were used to determine this pattern of gain and loss. The seepage tests showed that the streamflow gain of at least 0.58 cfs from springflow contributions was offset by losses of at least 0.59 cfs over the same reach. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77618","usgsCitation":"MacNish, R.D., 1977, Seepage tests on No Name Creek, Colville Indian Reservation, Washington, May 12-13, 1977: U.S. Geological Survey Open-File Report 77-618, iii, 9 p., https://doi.org/10.3133/ofr77618.","productDescription":"iii, 9 p.","costCenters":[],"links":[{"id":143619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0618/report-thumb.jpg"},{"id":363249,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0618/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Coville Indian Reservation, No Name Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb99a","contributors":{"authors":[{"text":"MacNish, Robert D.","contributorId":6061,"corporation":false,"usgs":true,"family":"MacNish","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":160878,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8701,"text":"ofr76880 - 1977 - Directory of local assistance centers of the National Water Data Exchange (NAWDEX)","interactions":[{"subject":{"id":8701,"text":"ofr76880 - 1977 - Directory of local assistance centers of the National Water Data Exchange (NAWDEX)","indexId":"ofr76880","publicationYear":"1977","noYear":false,"title":"Directory of local assistance centers of the National Water Data Exchange (NAWDEX)"},"predicate":"SUPERSEDED_BY","object":{"id":48608,"text":"ofr801193 - 1980 - Directory of assistance centers of the National Water Data Exchange (NAWDEX)","indexId":"ofr801193","publicationYear":"1980","noYear":false,"title":"Directory of assistance centers of the National Water Data Exchange (NAWDEX)"},"id":1}],"supersededBy":{"id":48608,"text":"ofr801193 - 1980 - Directory of assistance centers of the National Water Data Exchange (NAWDEX)","indexId":"ofr801193","publicationYear":"1980","noYear":false,"title":"Directory of assistance centers of the National Water Data Exchange (NAWDEX)"},"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr76880","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"76-880","title":"Directory of local assistance centers of the National Water Data Exchange (NAWDEX)","docAbstract":"The National Water Data Exchange (NAWDEX), managed by the U.S. Geological Survey, has established a network of Local Assistance Centers throughout the United States and Puerto Rico to assist users of water data in identifying and locating the data they need. This Directory provides the information needed to contact any of the established Centers. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76880","usgsCitation":"Edwards, M.D., 1977, Directory of local assistance centers of the National Water Data Exchange (NAWDEX): U.S. Geological Survey Open-File Report 76-880, iv, 11 p. ;27 cm.; (10 p. - PGS), https://doi.org/10.3133/ofr76880.","productDescription":"iv, 11 p. ;27 cm.; (10 p. - PGS)","costCenters":[],"links":[{"id":141791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b464a","contributors":{"authors":[{"text":"Edwards, Melvin D.","contributorId":94305,"corporation":false,"usgs":true,"family":"Edwards","given":"Melvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":158179,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9482,"text":"ofr7755 - 1977 - Uranium and thorium in the middle Precambrian Estes Conglomerate, Nemo District, Lawrence County, South Dakota: a preliminary report","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr7755","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-55","title":"Uranium and thorium in the middle Precambrian Estes Conglomerate, Nemo District, Lawrence County, South Dakota: a preliminary report","docAbstract":"The Estes Conglomerate, which is exposed in the Nemo District on the northeastern flank of the Black Hills, South Dakota, is inferred to be of early middle Precambrian age (early Precambrian X or Paleoaphebian) and to be resting on late early Precambrian (late Precambrian W) granitic continental crust. The Estes contains beds of quartzite and quartz-pebble conglomerate (oligomictic conglomerate) with matrices of micaceous quartzite that locally contain 5 to 25 percent dispersed pyrite. Highly oxidized outcrop samples of the oligomictic conglomerate have anomalously high contents of both uranium (10 to 40 ppm) and thorium (20 to 800 ppm). High thorium values in the oligomictic conglomerate favor a placer mechanism for the concentration of radioactive minerals and appear to eliminate the possibility of epigenetic processes, such as reduction of uranium by pyrite. The presence of abundant old prospect pits and of several abandoned mines suggests that these conglomerates may also contain some gold. Early prospectors may have been attracted by the gossan produced by oxidation of pyrite. Uranium in the Estes Conglomerate may be of similar origin to the economically very important uranium deposits in the Matinenda Formation of the Elliot Lake District, Ontario. Because uranium is rapidly dissolved in acidic, oxygenated ground water, such as is present where pyrite is weathering, most of the uranium originally present in the analyzed samples has probably been leached out. Conglomerate located below the zone of weathering and oxidation has good potential for economic uranium deposits.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7755","usgsCitation":"Hills, F.A., 1977, Uranium and thorium in the middle Precambrian Estes Conglomerate, Nemo District, Lawrence County, South Dakota: a preliminary report: U.S. Geological Survey Open-File Report 77-55, ii, 27 leaves :ill., maps ;27 cm.; (26 p. - PGS), https://doi.org/10.3133/ofr7755.","productDescription":"ii, 27 leaves :ill., maps ;27 cm.; (26 p. - PGS)","costCenters":[],"links":[{"id":141906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0055/report-thumb.jpg"},{"id":37190,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0055/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605c0b","contributors":{"authors":[{"text":"Hills, F. Allan","contributorId":90309,"corporation":false,"usgs":true,"family":"Hills","given":"F.","email":"","middleInitial":"Allan","affiliations":[],"preferred":false,"id":159767,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10150,"text":"ofr77461 - 1977 - Water-level records for Adams, Larimer, Logan, Morgan, Sedgwick, Washington, and Weld Counties, Colorado, 1973-77","interactions":[],"lastModifiedDate":"2018-11-02T14:14:46","indexId":"ofr77461","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-461","title":"Water-level records for Adams, Larimer, Logan, Morgan, Sedgwick, Washington, and Weld Counties, Colorado, 1973-77","docAbstract":"<p>Water levels measured during March 1977 in 350 wells tapping alluvial aquifers in Adams, Larimer, Logan, Morgan, Sedgwick, Washington, and Weld Counties, Colo., are included in this report. Water-level records for the 4 preceding years also are included to serve as references illustrating declining or rising water levels.</p><p>Water-level measurements made in March 1977 do not reflect the precipitation deficiencies of the winter of 1976-77.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77461","usgsCitation":"Major, T.J., and Vaught, K.D., 1977, Water-level records for Adams, Larimer, Logan, Morgan, Sedgwick, Washington, and Weld Counties, Colorado, 1973-77: U.S. Geological Survey Open-File Report 77-461, iii, 19 p., https://doi.org/10.3133/ofr77461.","productDescription":"iii, 19 p.","costCenters":[],"links":[{"id":359125,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0461/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0461/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Adams 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,{"id":10803,"text":"ofr77565 - 1977 - Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region","interactions":[{"subject":{"id":10803,"text":"ofr77565 - 1977 - Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region","indexId":"ofr77565","publicationYear":"1977","noYear":false,"title":"Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region"},"predicate":"SUPERSEDED_BY","object":{"id":38698,"text":"pp813K - 1978 - Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","indexId":"pp813K","publicationYear":"1978","noYear":false,"chapter":"K","title":"Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region"},"id":1}],"supersededBy":{"id":38698,"text":"pp813K - 1978 - Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","indexId":"pp813K","publicationYear":"1978","noYear":false,"title":"Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region"},"lastModifiedDate":"2016-01-15T16:15:22","indexId":"ofr77565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-565","title":"Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region","docAbstract":"<p>A broad-perspective analysis of the ground-water resources and present and possible future water development and management in the Souris-Red-Rainy Region is presented. The region includes the basins of the Souris River within Montana and North Dakota; the Red River of the North in South Dakota, North Dakota, and Minnesota; and the Rainy River within Minnesota. The region includes 59,645 square miles, mostly in North Dakota and Minnesota.</p>\n<p>The terrain is relatively flat, but ranges in altitude from 2,541 to 750 feet. Annual average precipitation ranges from 14 inches in the west to 28 inches in the east and about 75 percent of it is rain. The mean annual snow fall ranges from 32 inches in the west to 64 inches in the east. Temperatures range from -55&deg; to 118&deg;F (-48.3&deg; to 47.8&deg;C). Irrigation is needed at least part of the time to assure crop production, particularly in the western part of the region.</p>\n<p>Sand and gravel deposits in the drift form the most important fresh-water aquifers. Other aquifers are found in at least parts of the region in the Precambrian, Paleozoic, Cretaceous, and Tertiary rocks. The potentiometric surface in the bedrock generally decreases in altitude toward the Red River of the North, indicating that the general direction of ground-water movement is toward the river. Ground-water with less than 3,000 milligrams per liter dissolved solids is available throughout the region.</p>\n<p>Ground water with less than 1,000 milligrams per liter occurs in most of the region east of the Red River of the North and in most of the shallow aquifers west of the river. The total volume of water available from storage having less than 3,000 milligrams per liter dissolved solids is estimated to be 5 x 10<sup>8</sup> acre-feet. In addition to the fresh and slightly saline water, the region has abundant highly mineralized water that can be considered as a resource. Yields of wells in individual bedrock aquifers are generally less than 100 gallons per minute but locally yields may be as much as 500 gallons per minute and more. Yields in drift aquifers are frequently less than 100 gallons per minute but range from 5 to 1,000 gallons per minute. In a few places outwash yields more than 1,000 gallons per minute.</p>\n<p>Ground water is the sole or a primary source of water supply in much of the region, including supplies for irrigation, domestic and livestock, municipal, and industrial needs. Reportedly, the potential irrigation development is 1,550,000 acres, as compared with 50,200 acres in 1975. Both ground- and surface-water supplies would be required to meet these demands. Rural domestic and livestock water supplies are derived almost entirely from ground-water sources. Smaller communities and towns generally rely on ground water, and the cities and industries use ground water, surface water, or both. The municipalities using surface water generally depend upon reservoir storage. Water quality rather than quantity is the greater water-supply problem for many communities in the region.</p>\n<p>Increased demands on both ground-water and surface-water supplies likely will be made in the future. Storage of surface water in the ground-water reservoirs during times of surplus for withdrawal during times of scarcity would aid in meeting these demands. The surplus (flood) water is of better chemical quality than underlying ground water in parts of the western half of the region. Fresh water could be stored in saline- or fresh-water aquifers, and pumped out later, as needed. Thus, the ground-water reservoirs have a definite present and potential role in water management.</p>\n<p>To understand the hydrologic system for management purposes there is a need to determine more adequately the geologic and hydrologic characteristics of existing aquifers and the location of new aquifers. Also, as pumping and other stresses on any part of the hydrologic system affect other parts of the system, monitoring programs ideally should be started and maintained to detect changes and determine effects of the stresses.</p>\n<p>Many alternatives are available for managing water in the region. Some of these are operational and others are undergoing research. Adequate hydrologic information is needed to aid in solving problems of water supply, use and pollution.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77565","usgsCitation":"Reeder, H.O., 1977, Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region: U.S. Geological Survey Open-File Report 77-565, 125 p., https://doi.org/10.3133/ofr77565.","productDescription":"125 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":143865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0565/report-thumb.jpg"},{"id":38598,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0565/report.pdf","text":"Report","size":"2.98 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Minnesota, Montana, North Dakota, South Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.40283203124999,\n              49.03786794532644\n            ],\n            [\n              -95.185546875,\n              49.06666839558117\n            ],\n            [\n              -95.1416015625,\n              49.52520834197442\n            ],\n            [\n              -94.74609375,\n              49.32512199104001\n            ],\n            [\n              -94.482421875,\n              48.864714761802794\n            ],\n            [\n              -93.69140625,\n              48.69096039092549\n            ],\n            [\n              -93.0322265625,\n              48.719961222646276\n            ],\n            [\n              -92.28515625,\n              48.516604348867475\n            ],\n            [\n              -91.845703125,\n              48.40003249610685\n            ],\n            [\n              -91.3623046875,\n              48.19538740833338\n            ],\n            [\n              -90.7470703125,\n              48.28319289548349\n            ],\n            [\n              -89.384765625,\n              48.1367666796927\n            ],\n            [\n              -90,\n              47.724544549099676\n            ],\n            [\n              -91.2744140625,\n              47.15984001304432\n            ],\n            [\n              -92.373046875,\n              46.70973594407157\n            ],\n            [\n              -94.5703125,\n              45.73685954736049\n            ],\n            [\n              -95.712890625,\n              45.398449976304086\n            ],\n            [\n              -97.0751953125,\n              45.30580259943578\n            ],\n            [\n              -98.525390625,\n              45.82879925192134\n            ],\n            [\n              -99.5361328125,\n              46.10370875598026\n            ],\n            [\n              -100.81054687499999,\n              46.89023157359399\n            ],\n            [\n              -101.953125,\n              47.07012182383309\n            ],\n            [\n              -103.3154296875,\n              47.54687159892238\n            ],\n            [\n              -104.150390625,\n              47.84265762816538\n            ],\n            [\n              -105.2490234375,\n              48.3416461723746\n            ],\n            [\n              -105.40283203124999,\n              49.03786794532644\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6995d7","contributors":{"authors":[{"text":"Reeder, Harold O.","contributorId":14381,"corporation":false,"usgs":true,"family":"Reeder","given":"Harold","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":161995,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9478,"text":"ofr77457 - 1977 - Paleomagnetic investigation of late Quaternary sediments of south San Francisco Bay, California","interactions":[],"lastModifiedDate":"2017-03-06T16:07:55","indexId":"ofr77457","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-457","title":"Paleomagnetic investigation of late Quaternary sediments of south San Francisco Bay, California","docAbstract":"<p>Paleomagnetic inclinations of the Late Quaternary sediments of South San Francisco Bay were determined from bore hole samples collected near Dumbarton Bridge. The sediments consist of estuarine muds and nonmarine sand deposits, floored by bedrock of the Mesozoic Franciscan Formation. - Beneath Dumbarton Bridge the entire sedimentary fill is normally polarized; therefore, the fill postdates the Brunhes-Matayama polarity reversal (700,000 y. B.P.). Magnetic time lines such as the Mono Lake excursion (24,000 y. B.P.) and the reversed Blake event (110,000 y B.P.) were not found in this bore hole. In addition to Holocene and modern deposits of San Francisco Bay, an older estuarine unit occurs in the stratigraphic section. The older unit was deposited during a period of high sea level, tentatively correlated with the Sangamon interglacial period. Because evidence of the Blake event is not present in the older estuarine unit, the proposed age of this unit could not be confirmed. Although the Holocene estuarine deposits of South San Francisco Bay carry stable remanent magnetization, a reliable record of geomagnetic secular variation could not be recovered because the water-saturated sdiment was deformed by drilling. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77457","usgsCitation":"Hillhouse, J.W., 1977, Paleomagnetic investigation of late Quaternary sediments of south San Francisco Bay, California: U.S. Geological Survey Open-File Report 77-457, 13 p., https://doi.org/10.3133/ofr77457.","productDescription":"13 p.","numberOfPages":"31","costCenters":[],"links":[{"id":335817,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0457/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0457/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.43850708007811,\n              37.421435292172944\n            ],\n            [\n              -121.92352294921874,\n              37.421435292172944\n            ],\n            [\n              -121.92352294921874,\n              37.792422407988575\n            ],\n            [\n              -122.43850708007811,\n              37.792422407988575\n            ],\n            [\n              -122.43850708007811,\n              37.421435292172944\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689c48","contributors":{"authors":[{"text":"Hillhouse, John W. 0000-0002-1371-4622 jhillhouse@usgs.gov","orcid":"https://orcid.org/0000-0002-1371-4622","contributorId":2618,"corporation":false,"usgs":true,"family":"Hillhouse","given":"John","email":"jhillhouse@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":159758,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11363,"text":"ofr7774 - 1977 - Evaporation and radiation measurements at Salton Sea, California","interactions":[{"subject":{"id":11363,"text":"ofr7774 - 1977 - Evaporation and radiation measurements at Salton Sea, California","indexId":"ofr7774","publicationYear":"1977","noYear":false,"title":"Evaporation and radiation measurements at Salton Sea, California"},"predicate":"SUPERSEDED_BY","object":{"id":2770,"text":"wsp2053 - 1978 - Evaporation and radiation measurements at Salton Sea, California","indexId":"wsp2053","publicationYear":"1978","noYear":false,"title":"Evaporation and radiation measurements at Salton Sea, California"},"id":1}],"supersededBy":{"id":2770,"text":"wsp2053 - 1978 - Evaporation and radiation measurements at Salton Sea, California","indexId":"wsp2053","publicationYear":"1978","noYear":false,"title":"Evaporation and radiation measurements at Salton Sea, California"},"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr7774","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-74","title":"Evaporation and radiation measurements at Salton Sea, California","docAbstract":"Evaporation from the Salton Sea, Calif., was computed for a 539-day period between July 14, 1967, and January 2, 1969, by use of energy-budget, mass-transfer, and water budget methods. The total evaporation computed by the three methods agreed within 5 percent. The values of heat transfer to and from the bed were used in the energy-budget computations. Monthly evaporation computed by the energy-budget method for 1968 showed that the Salton Sea exhibited a double wave evaporation similar to that of oceans in the same latitude. Weekly and montly comparisons were made to determine if radiation measured by the flat-plate radiometer is seasonally biased. These comparisons indicate that the measurements of radiation by the flat-plate radiometer are not seasonally biased, and that the Cummings Radiation Integrator gives reliable measurements of radiation for periods as short as 1 week. An empirical mass-transfer coefficient, N, as determined from energy-budget measurements. The value of this coefficient to give evaporation in inches per day is 0.00245 when the windspeed is expressed in miles per hour and the vapor pressure expressed in millibars. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7774","usgsCitation":"Sturrock, A.M., 1977, Evaporation and radiation measurements at Salton Sea, California: U.S. Geological Survey Open-File Report 77-74, xii, 42 p. :ill., map ;28 cm.; (49 p. - PGS), https://doi.org/10.3133/ofr7774.","productDescription":"xii, 42 p. :ill., map ;28 cm.; (49 p. - PGS)","costCenters":[],"links":[{"id":142541,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9d19","contributors":{"authors":[{"text":"Sturrock, Alex M.","contributorId":48948,"corporation":false,"usgs":true,"family":"Sturrock","given":"Alex","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":163004,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9463,"text":"ofr77802 - 1977 - Hydrogeologic data for the McKay Creek subsurface waste-injection test site, Pinellas County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr77802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-802","title":"Hydrogeologic data for the McKay Creek subsurface waste-injection test site, Pinellas County, Florida","docAbstract":"Lithologic, hydraulic, geophysical, and water-quality data collected at the McKay Creek subsurface waste-injection test site in Pinellas County, Florida, are reported. Data were collected to determine the possibility of subsurface injection of waste-treatment plant effluent. One exploratory hole, one test injection well, and eight observation wells were constructed between May 1973 and February 1976. The exploratory hole was drilled to a depth of 1,750 feet below land surface; the test injection well is open in dolomite between 952 and 1 ,040 feet; and the observation wells are open to intervals above , in, and below the test injection zone. The lithology of the upper 100 feet is predominantly clay. From 100 to 1,750 feet below land surface, limestone and dolomite predominate. Gypsum is present 1,210 feet below land surface. Laboratory analyses of cores taken during drilling are given for vertical intrinsic permeability, porosity, interval transit time, and compressibility. Specific capacities tested during drilling range from 4 to 2,500 gallons per minute per foot of drawdown. An 83-hour withdrawal test at 4,180 gallons per minute and a 2-month injection test at 650 gallons per minute were run. Small water-quality changes were observed in one observation well immediately above the test injection zone during and after the injection test. Formation water in all of the wells with the exception of the shallowest observation wells is saline. The vertical position of saltwater is estimated to be at about 280 feet below land surface. Thirteen wells within a 1-mile radius of the test site were located and sampled for water quality. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77802","usgsCitation":"Hickey, J.D., 1977, Hydrogeologic data for the McKay Creek subsurface waste-injection test site, Pinellas County, Florida: U.S. Geological Survey Open-File Report 77-802, [105] leaves in various foliations :ill. (1 fold. in pocket), map ;27 cm.; (119 p. - PGS), https://doi.org/10.3133/ofr77802.","productDescription":"[105] leaves in various foliations :ill. (1 fold. in pocket), map ;27 cm.; (119 p. - PGS)","costCenters":[],"links":[{"id":142890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db628a2a","contributors":{"authors":[{"text":"Hickey, John D.","contributorId":34925,"corporation":false,"usgs":true,"family":"Hickey","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":159731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10781,"text":"ofr77619 - 1977 - Ground-water investigations at U.S. Air Force Launch Control Facility E-0, Ramsey County, North Dakota","interactions":[],"lastModifiedDate":"2018-03-12T16:02:40","indexId":"ofr77619","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-619","title":"Ground-water investigations at U.S. Air Force Launch Control Facility E-0, Ramsey County, North Dakota","docAbstract":"<p>U.S. Air Force Launch Control Facility E-0 is located in Ramsey County, North Dakota. Geohydrologic and water-quality data indicate that the fractured Pierre Shale is the only aquifer in the vicinity of the facility that will supply acceptable water at the required rate of 5 gallons per minute (0.32 liters per second}. The chemical quality of the water is generally considered marginally satisfactory for the intended use due to the presence of high concentrations of dissolved solids, and chloride or sulfate.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77619","usgsCitation":"Randich, P., 1977, Ground-water investigations at U.S. Air Force Launch Control Facility E-0, Ramsey County, North Dakota: U.S. Geological Survey Open-File Report 77-619, iv, 23 p., https://doi.org/10.3133/ofr77619.","productDescription":"iv, 23 p.","onlineOnly":"N","additionalOnlineFiles":"N","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":145076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr77619.jpg"},{"id":310507,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0619/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota","county":"Ramsey County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.3196,48.5433],[-98.3191,48.4556],[-98.318,48.3683],[-98.2915,48.3684],[-98.2931,48.2812],[-98.2954,48.195],[-98.4221,48.1946],[-98.4242,48.0214],[-98.5249,48.0214],[-98.5254,47.9159],[-98.5881,47.9154],[-98.5914,47.9178],[-98.6056,47.918],[-98.6198,47.9177],[-98.6246,47.915],[-98.6272,47.9183],[-98.633,47.9248],[-98.6362,47.9322],[-98.6273,47.9358],[-98.6278,47.9418],[-98.6418,47.9484],[-98.6524,47.9559],[-98.659,47.9629],[-98.6641,47.9727],[-98.6666,47.9778],[-98.6656,47.9916],[-98.6681,47.9981],[-98.674,48.0023],[-98.6841,48.0047],[-98.699,48.004],[-98.7071,48.0027],[-98.7146,47.9996],[-98.7208,47.9969],[-98.7276,47.9933],[-98.7311,47.9883],[-98.7361,47.981],[-98.7423,47.9755],[-98.7477,47.9742],[-98.76,47.9707],[-98.7702,47.9666],[-98.7764,47.9626],[-98.7881,47.9517],[-98.7929,47.9508],[-98.7956,47.9508],[-98.7982,47.9527],[-98.7995,47.9555],[-98.7988,47.9587],[-98.7933,47.9623],[-98.7877,47.9682],[-98.7801,47.976],[-98.7576,47.9849],[-98.754,47.9913],[-98.7553,47.9946],[-98.7566,47.996],[-98.7619,47.9997],[-98.7639,48.0016],[-98.7624,48.0066],[-98.7637,48.0089],[-98.767,48.0118],[-98.7704,48.0118],[-98.7711,48.0081],[-98.77,48.0017],[-98.7747,48.0008],[-98.7801,48.0018],[-98.786,48.006],[-98.7864,48.0175],[-98.7861,48.0277],[-98.796,48.0388],[-98.8025,48.0481],[-98.8031,48.0509],[-98.7996,48.0541],[-98.7989,48.0545],[-98.7955,48.0573],[-98.7975,48.0582],[-98.8016,48.0583],[-98.8116,48.0611],[-98.8217,48.0631],[-98.8238,48.0608],[-98.828,48.0554],[-98.8328,48.0503],[-98.8356,48.0476],[-98.8439,48.0422],[-98.8513,48.0418],[-98.852,48.0414],[-98.8568,48.0391],[-98.8657,48.0355],[-98.8752,48.0324],[-98.8799,48.0352],[-98.8845,48.0385],[-98.8885,48.0386],[-98.8894,48.033],[-98.8808,48.0228],[-98.8865,48.0141],[-98.8906,48.0096],[-98.894,48.0087],[-98.8973,48.011],[-98.9005,48.0193],[-98.8998,48.0207],[-98.9079,48.0227],[-98.918,48.0205],[-98.9208,48.0173],[-98.9183,48.0099],[-98.9157,48.0052],[-98.9232,48.0012],[-98.932,48.0004],[-98.9475,48.0037],[-98.9536,48.0038],[-98.9569,48.0038],[-98.9678,48.0021],[-98.9787,47.9986],[-98.9916,47.9941],[-98.9943,47.9932],[-98.9983,47.996],[-98.9934,48.0047],[-98.9892,48.0125],[-98.9843,48.0166],[-98.9877,48.018],[-98.9945,48.0149],[-99.0024,48.0237],[-99.0017,48.0255],[-99.0015,48.032],[-99.0028,48.0352],[-99.0034,48.0398],[-99.0012,48.0458],[-99.0018,48.0504],[-99.0126,48.0519],[-99.0213,48.052],[-99.0289,48.0484],[-99.0377,48.0457],[-99.0446,48.0398],[-99.0509,48.0311],[-99.0531,48.0238],[-99.0625,48.0234],[-99.0706,48.0235],[-99.0711,48.0341],[-99.0713,48.053],[-99.0735,48.1065],[-99.1175,48.1069],[-99.1187,48.1134],[-99.1206,48.1217],[-99.1272,48.1278],[-99.1292,48.1301],[-99.1298,48.1324],[-99.1311,48.1356],[-99.133,48.1389],[-99.1371,48.1408],[-99.154,48.1386],[-99.1621,48.1415],[-99.1668,48.1447],[-99.1708,48.1452],[-99.1762,48.1462],[-99.1836,48.1486],[-99.1924,48.1505],[-99.1977,48.1538],[-99.201,48.157],[-99.2023,48.1949],[-99.2032,48.2511],[-99.203,48.259],[-99.2033,48.2811],[-99.2029,48.3697],[-99.137,48.3704],[-99.1261,48.3703],[-99.1044,48.3706],[-99.0935,48.37],[-99.0793,48.3699],[-99.0738,48.3698],[-99.063,48.3697],[-98.9726,48.3701],[-98.9713,48.5432],[-98.6138,48.543],[-98.6029,48.5428],[-98.5811,48.543],[-98.3196,48.5433]]]},\"properties\":{\"name\":\"Ramsey\",\"state\":\"ND\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668b28","contributors":{"authors":[{"text":"Randich, P.G.","contributorId":69953,"corporation":false,"usgs":true,"family":"Randich","given":"P.G.","affiliations":[],"preferred":false,"id":161952,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8709,"text":"ofr77259 - 1977 - The National Water Data Exchange (NAWDEX)","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr77259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-259","title":"The National Water Data Exchange (NAWDEX)","docAbstract":"The National Water Data Exchange (NAWDEX) was established in 1976 to assist users of water data to identify, locate, and acquire needed data. NAWDEX is a confederation of water-oriented organizations working together to provide more timely and convenient access to their data. A directory of sources of water data and a nationwide index of available water data are maintained for the storage and dissemination of information on available water data. Assistance services are provided through a nationwide network of Local Assistance Centers. This network consists of 51 Centers located in 45 states and Puerto Rico. The Centers provide convenient access to NAWDEX services as well as making local-area expertise available in the identification and location of needed data. Additional Centers will be added to the network, as needed, to meet demands. NAWDEX is centrally managed by a Program Office located within the U.S. Geological Survey 's Water Resources Division in Reston, Virginia. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77259","usgsCitation":"Edwards, M.D., 1977, The National Water Data Exchange (NAWDEX): U.S. Geological Survey Open-File Report 77-259, 5 p. ;27 cm.; (9 p. - PGS), https://doi.org/10.3133/ofr77259.","productDescription":"5 p. ;27 cm.; (9 p. - PGS)","costCenters":[],"links":[{"id":94869,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0259/report.pdf","size":"465","linkFileType":{"id":1,"text":"pdf"}},{"id":143567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0259/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67afcc","contributors":{"authors":[{"text":"Edwards, Melvin D.","contributorId":94305,"corporation":false,"usgs":true,"family":"Edwards","given":"Melvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":158193,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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