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This prgoram is sponsored primarily by the U.S. Geological Survey and the National Science Foundation and includes research by geologists, geophysicists, seismologists, engineers, sociologists, educators, and public policy experts.
\nIn the USGS program, there is a strong emphsis on effective communication of the results of research to a wide community of decision makers and users. This action is the key to implementation at all levels in federal, state, and local government, in the private sector, and on an individual basis.
\nThe U.S. Geological Survey convened a workshop involving approximately 65 people on May 22-24, 1978 in Denver, Colorado, to examine the communication problem. The purpose of the workshop was to evaluate critically the information-flow process for a number of past experiences, including:
\n(1) land use planning in Portola Valley, California,
\n(2) the seismic safety element, Santa Clara County, California
\n(3) earthquake preparedness, Puget Sound, Washington area,
\n(4) mitigation of geological hazards in Colorado,
\n(5) earthquake planning in the Mississippi-Arkansas-Tennessee area,
\n(6) water resource and land use planning in the northeast United States,
\n(7) acquiring and disseminating scientific and engineering information following an earthquake,
\n(8) development, use, and review of geologic and seismological data fro sitting of nuclear power plants,
\n(9) development and use of building codes that incorporate earthquake provisions,
\n(10) use of research products produced in the HUD/USGS San Francisco Bay region study, and\n
(11) achieving landslide hazard reduction.
\nThe objective was to identify the most significant lessons learned during the course of each experience and to develop recommendations for improving communication that might be incorporated in the search program of the USGS.
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E.","contributorId":84770,"corporation":false,"usgs":true,"family":"Hansen","given":"Dan","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":268032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Avery E.","contributorId":82383,"corporation":false,"usgs":true,"family":"Smith","given":"Avery","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":268031,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8723,"text":"ofr78811 - 1978 - Selected low-flow characteristics of streams in the vicinity of Warwick, Orange County, New York","interactions":[],"lastModifiedDate":"2023-09-12T21:44:55.403249","indexId":"ofr78811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File 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Discharge measurements at the partial-record sites were correlated with records from three suitable continuous-record gaging stations near the town to determine 7-day, 2-year low flows and 7-day, 10-year low flows. Measurement-site descriptions are included. The information presented provides a data base that planners and managers can use in making water-management decisions.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78811","collaboration":"Prepared in cooperation with the Town of Warwick","usgsCitation":"Eissler, B.B., 1978, Selected low-flow characteristics of streams in the vicinity of Warwick, Orange County, New York: U.S. Geological Survey Open-File Report 78-811, ii, 21 p., https://doi.org/10.3133/ofr78811.","productDescription":"ii, 21 p.","costCenters":[],"links":[{"id":420747,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0811/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141038,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0811/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Orange County","city":"Warwick","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.40317346376985,\n 41.276009317207354\n ],\n [\n -74.40317346376985,\n 41.22899934354564\n ],\n [\n -74.31350277830987,\n 41.22899934354564\n ],\n [\n -74.31350277830987,\n 41.276009317207354\n ],\n [\n -74.40317346376985,\n 41.276009317207354\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f8407","contributors":{"authors":[{"text":"Eissler, Benjamin B.","contributorId":77527,"corporation":false,"usgs":true,"family":"Eissler","given":"Benjamin","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":158212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20000,"text":"ofr781024 - 1978 - On the development of strong-motion instrument networks in the United States","interactions":[],"lastModifiedDate":"2023-03-13T18:51:22.842395","indexId":"ofr781024","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-1024","title":"On the development of strong-motion instrument networks in the United States","docAbstract":"This report outlines a plan for the distribution of strong-motion instrumentation throughout the United States. The present \"national\" network of strong-motion instrumentation has evolved through the merger of several programs initiated by different agencies and organizations with objectives ranging from research to regulation. It is the result of the coordination of instrument maintenance and record archival currently provided by the Seismic Engineering Branch of the U.S. Geological Survey (formerly the Seismological Field Survey of the U.S. Coast & Geodetic Survey, or the National Ocean Survey, or the National Oceanic and Atmospheric Administration). The USGS operates the program under funding from the National Science Foundation (NSF) in cooperation with other federal, state, and local agencies.
NSF supports a data management function and the operation of a network of about 200 accelerographs and 300 seismoscopes utilized for studies of ground motion and building response. The State of California is developing its own strong-motion instrumentation program (CSMIP), which includes measurements of ground motion as well as the response of representative types of structures. The CSMIP network is the largest network operated by a single agency anywhere in the world. Eventually it will contain a total of about 1000 accelerographs. The Army Corps of Engineers (COE) is developing a program for monitoring the response of earth dams, which eventually will include as many as 400 instruments on over 100 dams. Other agencies and organizations are developing networks appropriate to their missions or objectives. At present the number of instruments owned by these other agencies is less than 100 in each case, although several agencies are still expanding their networks. The present distribution of accelerographs in the United States is indicated in Figure 1 (see: USGS, 1977, also).
In 1964 the cities of Los Angeles and Beverly Hills, California passed ordinances which required 3 accelerographs to be installed in all high-rise buildings. Initially, these instruments were installed and maintained as a part of the strong-motion program of the Seismological Field Survey (SFS). As the number of installations required by such codes increased, it became apparent that the maintenance of these instruments placed an inordinate burden on and created an imbalance in the SFS operated program (in 1972, 50 percent of the \"national\" program was concentrated in Los Angeles). With the transfer of the SFS program responsibility to the NSF and with the development of the CSMIP, the responsibility for maintenance of code required instruments has reverted to the city building officials and the building owners.
As the coordinated network of strong-motion instruments has grown, the maintenance of the instruments has required a larger staff than the USGS could provide under existing personnel ceilings. This situation has been resolved by the agencies with the larger networks performing their own installation and maintenance. The USGS maintains an archive of first class copies of all records, whereas other agencies maintain archives of their own records, only. In addition, the USGS coordinates the routine processing of all of the significant records, although other agencies will process their own data if they consider it to have a higher priority than does the USGS. In response to a recent change in their legislated charter, the CSMIP is beginning to develop a capability to process the data collected under that program.
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Such relations often follow power laws, the exponents in which are called hydraulic exponents. The Langbein (1964) minimum-variance theory is examined in regard to its validity and its ability to predict observed hydraulic exponents. The variables used with the theory were velocity, depth, width, bed shear stress, friction factor, slope (energy gradient), and stream power. Slope is often constant, in which case only velocity, depth, width, shear and friction factor need be considered. The theory was tested against a wide range of field data from various geographic areas of the United States. The original theory was intended to produce only the average hydraulic exponents for a group of cross sections in a similar type of geologic or hydraulic environment. The theory does predict these average exponents with a reasonable degree of accuracy. An attempt to forecast the exponents at any selected cross section was moderately successful. Empirical equations are more accurate than the minimum variance, Gauckler-Manning, or Chezy methods. Predictions of the exponent of width are most reliable, the exponent of depth fair, and the exponent of mean velocity poor. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1029","usgsCitation":"Williams, G.P., 1978, Hydraulic geometry of river cross sections; theory of minimum variance: U.S. Geological Survey Professional Paper 1029, 47 p., https://doi.org/10.3133/pp1029.","productDescription":"47 p.","costCenters":[],"links":[{"id":123811,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1029/report-thumb.jpg"},{"id":34006,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1029/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a22c","contributors":{"authors":[{"text":"Williams, Garnett P.","contributorId":100361,"corporation":false,"usgs":true,"family":"Williams","given":"Garnett","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":152870,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8682,"text":"ofr78943 - 1978 - Proceedings of Conference VI: Methodology for identifying seismic gaps and soon-to-break gaps: Convened under auspicies of National Earthquake Hazards Reduction Program, 25-27 May, 1978","interactions":[],"lastModifiedDate":"2016-02-17T10:09:51","indexId":"ofr78943","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-943","title":"Proceedings of Conference VI: Methodology for identifying seismic gaps and soon-to-break gaps: Convened under auspicies of National Earthquake Hazards Reduction Program, 25-27 May, 1978","docAbstract":"The fifth conference in the continuing series under the Earthquake Hazard Reduction Program was held at Massachusetts Institute of Technology on May 25- 27, 1978. Its theme was \"Methodology for Defining Seismic Gaps and Soon-to-Break Seismic Gaps.\" One of the proposed strategies for acquiring critical data on earthquake prediction is to identify soon-to-break gaps and to deploy a variety of instruments in the expected epicentral region. The Conference had as one of its major purposes the evaluation of our present capability to define gaps in general and soon-to-break gaps in particular, and thus to determine if the first step in the strategy proposed above could be fulfilled today.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78943","usgsCitation":"Isacks, B.L., and Plafker, G., 1978, Proceedings of Conference VI: Methodology for identifying seismic gaps and soon-to-break gaps: Convened under auspicies of National Earthquake Hazards Reduction Program, 25-27 May, 1978: U.S. Geological Survey Open-File Report 78-943, 924 p., https://doi.org/10.3133/ofr78943.","productDescription":"924 p.","numberOfPages":"938","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":142656,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr78943.PNG"},{"id":318083,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0943/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6608a8","contributors":{"authors":[{"text":"Isacks, Bryan L.","contributorId":93912,"corporation":false,"usgs":true,"family":"Isacks","given":"Bryan","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":158147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":158146,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8737,"text":"ofr78782 - 1978 - Estuarine research: An annotated bibliography of selected literature, with emphasis on the Hudson River estuary, New York and New Jersey","interactions":[],"lastModifiedDate":"2023-02-24T17:28:54.454175","indexId":"ofr78782","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-782","title":"Estuarine research: An annotated bibliography of selected literature, with emphasis on the Hudson River estuary, New York and New Jersey","docAbstract":"Abstracts of 177 selected publications on water movement in estuaries, particularly the Hudson River estuary, are compiled for reference in Hudson River studies. Subjects represented are the hydraulic, chemical, and physical characteristics of estuarine waters, estuarine modeling techniques, and methods of water-data collection and analysis. Summaries are presented in five categories: Hudson River estuary studies; hydrodynamic-model studies; water-quality-model studies; reports on data-collection equipment and methods; and bibliographies, literature reviews, conference proceedings, and textbooks. An author index is included. Omitted are most works published before 1965, environmental-impact statements, theses and dissertations, policy or planning reports, regional or economic reports, ocean studies, studies based on physical models, and foreign studies.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78782","collaboration":"Prepared in cooperation with the Water Resources Council for the Hudson River Level-B Study Group","usgsCitation":"Embree, W.N., and Wiltshire, D.A., 1978, Estuarine research: An annotated bibliography of selected literature, with emphasis on the Hudson River estuary, New York and New Jersey: U.S. Geological Survey Open-File Report 78-782, ii, 58 p., https://doi.org/10.3133/ofr78782.","productDescription":"ii, 58 p.","costCenters":[],"links":[{"id":142873,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0782/report-thumb.jpg"},{"id":413406,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0782/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey, New York","otherGeospatial":"Hudson River estuary","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.03137207031247,\n 40.551374198715166\n ],\n [\n -73.74023437499999,\n 40.551374198715166\n ],\n [\n -73.74023437499999,\n 42.90413649491736\n ],\n [\n -74.03137207031247,\n 42.90413649491736\n ],\n [\n -74.03137207031247,\n 40.551374198715166\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb173","contributors":{"authors":[{"text":"Embree, William N.","contributorId":41428,"corporation":false,"usgs":true,"family":"Embree","given":"William","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":158238,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiltshire, Denise A.","contributorId":78717,"corporation":false,"usgs":true,"family":"Wiltshire","given":"Denise","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":158239,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6438,"text":"pp1030 - 1978 - Erosion and sediment yields in the Transverse Ranges, Southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp1030","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1030","title":"Erosion and sediment yields in the Transverse Ranges, Southern California","docAbstract":"Major-storm and long-term erosion rates in mountain watersheds of the western Transverse Ranges of Ventura County, Calif., are estimated to range from low values that would not require the construction of catchments or channel-stabilization structures to values as high as those recorded anywhere for comparable bedrock erodibilities. A major reason for this extreme variability is the high degree of tectonic activity in the area--watersheds are locally being uplifted by at least as much as 25 feet per 1,000 years, yet the maximum extrapolated rate of denudation measured over the longest available period of record is 7.5 feet per 1,000 years adjusted to a drainage area of 0.5 square mile. Evidence of large amounts of uplift continuing into historic time includes structurally overturned strata of Pleistocene age, active thrust faulting, demonstrable stream antecedence, uplifted and deformed terraces, and other results of base-level change seen in stream channels. Such evidence is widespread in the Transverse Ranges, and aspects of the landscape are locally more a function of tectonic activity than of the denudational process. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1030","usgsCitation":"Scott, K.M., and Williams, R.P., 1978, Erosion and sediment yields in the Transverse Ranges, Southern California: U.S. Geological Survey Professional Paper 1030, 38 p., https://doi.org/10.3133/pp1030.","productDescription":"38 p.","costCenters":[],"links":[{"id":123898,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1030/report-thumb.jpg"},{"id":33847,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1030/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdf73","contributors":{"authors":[{"text":"Scott, Kevin M.","contributorId":88331,"corporation":false,"usgs":true,"family":"Scott","given":"Kevin","email":"","middleInitial":"M.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":152723,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Rhea P.","contributorId":87114,"corporation":false,"usgs":true,"family":"Williams","given":"Rhea","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":152722,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8616,"text":"ofr78854 - 1978 - Ground-water data for 1976-77 in Joshua Tree National Monument, California","interactions":[],"lastModifiedDate":"2024-01-31T20:39:05.016885","indexId":"ofr78854","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-854","title":"Ground-water data for 1976-77 in Joshua Tree National Monument, California","docAbstract":"A continuing study of ground water in Joshua Tree National Monument shows that during 1976-77 water levels fluctuated seasonally; slight declines were detected in the Oasis of Mara and the Pinto Basin. Water quality was generally good, with a high concentration of fluoride in one well in the southern part of the Monument.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78854","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Downing, D., 1978, Ground-water data for 1976-77 in Joshua Tree National Monument, California: U.S. Geological Survey Open-File Report 78-854, iv, 34 p., https://doi.org/10.3133/ofr78854.","productDescription":"iv, 34 p.","costCenters":[],"links":[{"id":141084,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0854/report-thumb.jpg"},{"id":425167,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0854/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Joshua Tree National Monument","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116.09899195770373,\n 34.08392494796759\n ],\n [\n -116.09899195770373,\n 33.70568354156441\n ],\n [\n -115.40727607556032,\n 33.70568354156441\n ],\n [\n -115.40727607556032,\n 34.08392494796759\n ],\n [\n -116.09899195770373,\n 34.08392494796759\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cdee","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":158034,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40046,"text":"ofr78653 - 1978 - Coal resource occurrence and coal development potential maps of the Forks Ranch quadrangle, Big Horn County, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:18","indexId":"ofr78653","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-653","title":"Coal resource occurrence and coal development potential maps of the Forks Ranch quadrangle, Big Horn County, Montana","language":"ENGLISH","doi":"10.3133/ofr78653","usgsCitation":"Culbertson, W.C., Robinson, L.N., and Gaffke, T., 1978, Coal resource occurrence and coal development potential maps of the Forks Ranch quadrangle, Big Horn County, Montana: U.S. Geological Survey Open-File Report 78-653, 58 maps and 1 data sheet ;58 x 42 cm.; 31 p., https://doi.org/10.3133/ofr78653.","productDescription":"58 maps and 1 data sheet ;58 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William Craven","contributorId":43765,"corporation":false,"usgs":true,"family":"Culbertson","given":"William","email":"","middleInitial":"Craven","affiliations":[],"preferred":false,"id":222911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, L. N.","contributorId":16840,"corporation":false,"usgs":true,"family":"Robinson","given":"L.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":222910,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gaffke, T. M.","contributorId":58641,"corporation":false,"usgs":true,"family":"Gaffke","given":"T. M.","affiliations":[],"preferred":false,"id":222912,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":66572,"text":"i1072 - 1978 - Reconnaissance map of potential volcanic hazards from Cotopaxi Volcano, Ecuador","interactions":[],"lastModifiedDate":"2012-02-10T00:11:14","indexId":"i1072","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1072","subseriesTitle":"NONE","title":"Reconnaissance map of potential volcanic hazards from Cotopaxi Volcano, Ecuador","language":"ENGLISH","doi":"10.3133/i1072","usgsCitation":"Miller, C., Mullineaux, D.R., and Hall, M., 1978, Reconnaissance map of potential volcanic hazards from Cotopaxi Volcano, Ecuador: U.S. Geological Survey IMAP 1072, 1 map : col. ;88 x 50 cm. on sheet 101 x 74 cm., https://doi.org/10.3133/i1072.","productDescription":"1 map : col. ;88 x 50 cm. on sheet 101 x 74 cm.","costCenters":[],"links":[{"id":115178,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1072/report.pdf","size":"82","linkFileType":{"id":1,"text":"pdf"}},{"id":115179,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1072/plate-1.pdf","size":"13057","linkFileType":{"id":1,"text":"pdf"}},{"id":188807,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1072/report-thumb.jpg"}],"scale":"1","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78.75,0.16666666666666666 ], [ -78.75,1 ], [ -78.25,1 ], [ -78.25,0.16666666666666666 ], [ -78.75,0.16666666666666666 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63eaf5","contributors":{"authors":[{"text":"Miller, C.D.","contributorId":34504,"corporation":false,"usgs":true,"family":"Miller","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":274726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mullineaux, D. 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The Precambrian intrusives were emplaced in a sequence of high-grade interlayered felsic gneisses, amphibolites, and pelitic schists of sedimentary and volcanic origin. These rocks are cut by a major northeast-trending Precambrian shear zone where mainly left lateral movement of 1/ 2 to 1 mile is certain. Cumulative movement of many miles is possible. The Precambrian intrusives consist of a batholith, the Mount Ethel pluton, a smaller Buffalo Pass pluton, and small dikes or lenses of fine-grained porphyry, pegmatites, and ultramafics.
The Mount Ethel pluton is an oval shaped body 7 miles wide by about 40 miles long (shown by geophysical data to extend beneath younger sediments in North Park). Outer batholithic contacts are sharp and dip steeply outward at about 85°. Five mappable internal variants consist, in order of decreasing age, of granodiorite, quartz monzonite porphyry of Rocky Peak, quartz monzonite of Roxy Ann Lake, granite and quartz monzonite, and. leucogranite. Internal contacts between these plutonic variants are sharp, and evidence of liquid-solid relationships abounds; despite this, all rocks except the granodiorite contribute to an Rb-Sr whole-rock isochron indicating emplacement about 1.4 b.y. (billion years) ago. The most important variants volumetrically are: the quartz monzonite porphyry of Rocky Peak, which forms an irregular 2-mile-thick carapace or mapped band around the west edge of the pluton and is lithologically similar to nearby Sherman Granite, and the quartz monzonite of Roxy Ann Lake, which forms most of the rest of the pluton and is lithologically similar to Silver Plume Granite. An apparent Sherman -Silver Plume dichotomy with similar rock types and similar relative ages is noted throughout Colorado plutons of that age.
The Buffalo Pass pluton consists of the quartz monzonite and gra- nodiorite augen gneiss of Buffalo Mountain and equigranular quartz monzonite gneiss. Internal contacts are not exposed. These rocks contribute to an Rb-Sr whole-rock isochron indicating syntectonic emplacement 1.7-1.8 b.y. ago, essentially the same as the metamorphism of the felsic gneiss wallrocks in the area of this report, and of rocks of Boulder Creek age elsewhere in Colorado.
The fine-grained porphyry dikes cut the Buffalo Pass pluton, the ultramafics, and some pegmatites. The dikes are within the age range of the Mount Ethel pluton and are older than the mylonite and shear zones. They occur in both an older northwest-trending and a somewhat younger northeast-trending set but do not appear to change compositionally from one set to the other. Regional considerations indicate that they were emplaced between about 1.1 and 1.5 b.y. ago, a time when intermediate to mafic dikes were commonly emplaced throughout Colorado, Wyoming, and southwestern Montana. The pegmatite and ultramafic bodies are not dated directly, but clustering of many pegmatites outside the contacts of the Mount Ethel pluton may indicate a genetic relation of the pegmatites to the Mount Ethel rocks.
Fluorite is a common accessory mineral in the rocks of the Mount Ethel pluton; it has not been observed in this area in the petrographically similar rocks of the Buffalo Pass pluton. Fluorite was precipitated most abundantly from the Precambrian magma that formed the quartz monzonite of Roxy Ann Lake. In 70 percent of these rocks fluorite is observed in amounts as great as 2 percent and is successively less abundant in both older and younger plutonic phases. Textural evidence indicates that, although most fluorite is intergrown with and contemporaneous with other magmatic minerals, some fluorite is associated with alteration minerals in a manner demonstrating its mobility since its initial deposition.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1041","usgsCitation":"Snyder, G.L., and Hedge, C.E., 1978, Intrusive rocks northeast of Steamboat Springs, Park Range, Colorado: U.S. Geological Survey Professional Paper 1041, Report: iii, 42 p.; 1 Plate: 37.00 × 34.00 inches, https://doi.org/10.3133/pp1041.","productDescription":"Report: iii, 42 p.; 1 Plate: 37.00 × 34.00 inches","costCenters":[],"links":[{"id":395421,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4693.htm"},{"id":33837,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1041/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33836,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1041/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Steamboat Springs","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.9333,\n 40.5\n ],\n [\n -106.575,\n 40.5\n ],\n [\n -106.575,\n 40.75\n ],\n [\n -106.9333,\n 40.75\n ],\n [\n -106.9333,\n 40.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49bee4b07f02db5d1213","contributors":{"authors":[{"text":"Snyder, George L.","contributorId":6843,"corporation":false,"usgs":true,"family":"Snyder","given":"George","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":152704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedge, Carl E.","contributorId":76299,"corporation":false,"usgs":true,"family":"Hedge","given":"Carl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":152705,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19990,"text":"ofr781033 - 1978 - Preliminary report on the coal resources of the National Petroleum Reserve in Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:37","indexId":"ofr781033","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-1033","title":"Preliminary report on the coal resources of the National Petroleum Reserve in Alaska","docAbstract":"NPR-A, located on the Arctic slope of Northern Alaska, is underlain by a thick sequence of sedimentary rocks of Cretaceous age which attain a thickness of as much as 4600 m (15,000 feet). The bulk of the coal resources occurs in rocks of the Nanushuk Group of Early and Late Cretaceous age. The Nanushuk Group is a wedge-shaped unit of marginal marine and nonmarine rocks that is as thick as 3300 m (11,000 feet) just west of NPR-A. Within the reserve, coal occurs primarily in the middle and thicker portions of this clastic wedge and occurs stratigraphically in the upper half of the section. Specific data on individual coal beds or zones are scarce, and estimates of identified coal resources of about 49.5 billion tons represent a sampling of coal resources too small to give a realistic indication of the potential resources for an area so large. Estimates of undiscovered resources suggest hypothetical resources of between 330 billion and 3.3 trillion tons. The wide range in the undiscovered resource estimates reflects the scarcity and ambiguity of the available data but also suggests the presence of a potentially large coal resource.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr781033","usgsCitation":"Martin, G.C., and Callahan, J.E., 1978, Preliminary report on the coal resources of the National Petroleum Reserve in Alaska: U.S. Geological Survey Open-File Report 78-1033, ii, 23 leaves :ill., maps ;28 cm.; (29 p., 2 sheets, scale 1:471,680 - PGS), https://doi.org/10.3133/ofr781033.","productDescription":"ii, 23 leaves :ill., maps ;28 cm.; (29 p., 2 sheets, scale 1:471,680 - PGS)","costCenters":[],"links":[{"id":152169,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1033/report-thumb.jpg"},{"id":49513,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49514,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1033/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49515,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"47680","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696c3c","contributors":{"authors":[{"text":"Martin, G. C.","contributorId":102854,"corporation":false,"usgs":true,"family":"Martin","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":181863,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Callahan, James E.","contributorId":7273,"corporation":false,"usgs":true,"family":"Callahan","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":181862,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8744,"text":"ofr78290 - 1978 - Sediment transport in the Tanana River in the vicinity of Fairbanks, Alaska, 1977","interactions":[],"lastModifiedDate":"2018-10-31T14:10:09","indexId":"ofr78290","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-290","title":"Sediment transport in the Tanana River in the vicinity of Fairbanks, Alaska, 1977","docAbstract":"Measurements of suspended- and bedload-sediment transport for the Tanana River in the vicinity of Fairbanks, Alaska, show that suspended-sediment load, G in tons per day, relates to water discharge, Q, in cubic feet per scond, as:
GS = 1.66 x 10-8 Q2.83
The bedload transport rate is approximately one percent of the suspended-sediment transport rate.
The median particle size of suspended sediment is generally silt (<0.062 mm), but at some low-water discharges, the median particle size is very fine sand. The median particle size of bedload is generally gravel (>2.0 mm, and often in the range of 10 to 20 mm), but at some low transport rates, the median particle size is medium sand. At all water discharges and sediment-transport rates, the particles constituting the suspended load are significantly smaller than the particles constituting the bedload.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78290","usgsCitation":"Emmett, W.W., Burrows, R.L., and Parks, B., 1978, Sediment transport in the Tanana River in the vicinity of Fairbanks, Alaska, 1977: U.S. Geological Survey Open-File Report 78-290, v, 28 p., https://doi.org/10.3133/ofr78290.","productDescription":"v, 28 p.","costCenters":[],"links":[{"id":359042,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0290/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142682,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0290/report-thumb.jpg"},{"id":94473,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015018204977?urlappend=%3Bseq=3"}],"country":"United States","state":"Alaska","city":"Fairbanks","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbeb6","contributors":{"authors":[{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158251,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burrows, Robert L.","contributorId":79473,"corporation":false,"usgs":true,"family":"Burrows","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":158252,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parks, Bruce","contributorId":87542,"corporation":false,"usgs":true,"family":"Parks","given":"Bruce","email":"","affiliations":[],"preferred":false,"id":158253,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":67931,"text":"ha560 - 1978 - Water resources of the coastal drainage basins of southeastern Massachusetts, northwest shore of Buzzards Bay","interactions":[{"subject":{"id":16563,"text":"ofr75651 - 1975 - Water resources of the coastal drainage basins of southeastern Massachusetts, northwest shore of Buzzards Bay","indexId":"ofr75651","publicationYear":"1975","noYear":false,"title":"Water resources of the coastal drainage basins of southeastern Massachusetts, northwest shore of Buzzards Bay"},"predicate":"SUPERSEDED_BY","object":{"id":67931,"text":"ha560 - 1978 - Water resources of the coastal drainage basins of southeastern Massachusetts, northwest shore of Buzzards Bay","indexId":"ha560","publicationYear":"1978","noYear":false,"title":"Water resources of the coastal drainage basins of southeastern Massachusetts, northwest shore of Buzzards Bay"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:21","indexId":"ha560","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"560","title":"Water resources of the coastal drainage basins of southeastern Massachusetts, northwest shore of Buzzards Bay","language":"ENGLISH","doi":"10.3133/ha560","usgsCitation":"Williams, J.R., 1978, Water resources of the coastal drainage basins of southeastern Massachusetts, northwest shore of Buzzards Bay: U.S. Geological Survey Hydrologic Atlas 560, 5 maps : col. ;on 2 sheets 94 x 131 cm. and 82 x 104 cm. --, https://doi.org/10.3133/ha560.","productDescription":"5 maps : col. ;on 2 sheets 94 x 131 cm. and 82 x 104 cm. --","costCenters":[],"links":[{"id":187696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89130,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/560/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89131,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/560/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.08333333333333,41.5 ], [ -71.08333333333333,42 ], [ -70.66666666666667,42 ], [ -70.66666666666667,41.5 ], [ -71.08333333333333,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f026d","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":277346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":62975,"text":"gq1316 - 1978 - Geologic map of the Leitchfield quadrangle, Grayson County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:44","indexId":"gq1316","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1316","title":"Geologic map of the Leitchfield quadrangle, Grayson County, Kentucky","language":"ENGLISH","doi":"10.3133/gq1316","usgsCitation":"Gildersleeve, B., 1978, Geologic map of the Leitchfield quadrangle, Grayson County, Kentucky: U.S. Geological Survey Geologic Quadrangle 1316, 1 map : col. ;58 x 46 cm. on sheet 78 x 86 cm. --, https://doi.org/10.3133/gq1316.","productDescription":"1 map : col. ;58 x 46 cm. on sheet 78 x 86 cm. --","costCenters":[],"links":[{"id":107743,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10851.htm","linkFileType":{"id":5,"text":"html"},"description":"10851"},{"id":249113,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1316/report.pdf","size":"36","linkFileType":{"id":1,"text":"pdf"}},{"id":252114,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1316/report-thumb.jpg"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.36749999999999,37.3675 ], [ -86.36749999999999,37.5 ], [ -86.25,37.5 ], [ -86.25,37.3675 ], [ -86.36749999999999,37.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696f51","contributors":{"authors":[{"text":"Gildersleeve, Benjamin","contributorId":14468,"corporation":false,"usgs":true,"family":"Gildersleeve","given":"Benjamin","email":"","affiliations":[],"preferred":false,"id":268124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8636,"text":"ofr78259 - 1978 - Report of the annual yield of the Arkansas River basin for the Arkansas River Basin Compact, Arkansas--Oklahoma 1977 water year","interactions":[],"lastModifiedDate":"2022-09-27T16:34:34.087594","indexId":"ofr78259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-259","title":"Report of the annual yield of the Arkansas River basin for the Arkansas River Basin Compact, Arkansas--Oklahoma 1977 water year","docAbstract":"The computed annual yields for subbasins in the Arkansas River basin as defined in the Arkansas River Basin Compact, Arkansas-Oklahoma, 1972, are presented in this report. The area bounded by the Compact is shown in figure 1.
This report was prepared by the Water Resources Division of the U.S. Geological Survey in cooperation with the Arkansas Division of Soil and Water Resources. Streamflow data were furnished by the Arkansas and Oklahoma Districts of the Water Resources Division, Geological Survey, and the U.S. Army Corps of Engineers, Tulsa District. The Tulsa District also provided data from the Webbers Falls, Tenkiller Ferry, Robert S. Kerr, and Wister Reservoirs.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78259","collaboration":"Prepared in cooperation with the Arkansas Division of Soil and Water Resources","usgsCitation":"Ducret, G., 1978, Report of the annual yield of the Arkansas River basin for the Arkansas River Basin Compact, Arkansas--Oklahoma 1977 water year: U.S. Geological Survey Open-File Report 78-259, ii, 25 p., https://doi.org/10.3133/ofr78259.","productDescription":"ii, 25 p.","costCenters":[],"links":[{"id":407415,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0259/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143453,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0259/report-thumb.jpg"}],"country":"United States","state":"Arkansas, Oklahoma","otherGeospatial":"Arkansas River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.03173828125,\n 34.994003757575776\n ],\n [\n -93.75732421875,\n 34.994003757575776\n ],\n [\n -93.75732421875,\n 35.64836915737426\n ],\n [\n -95.03173828125,\n 35.64836915737426\n ],\n [\n -95.03173828125,\n 34.994003757575776\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5be4b07f02db630e5c","contributors":{"authors":[{"text":"Ducret, G. Louis","contributorId":32531,"corporation":false,"usgs":true,"family":"Ducret","given":"G. Louis","affiliations":[],"preferred":false,"id":158066,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}