{"pageNumber":"5524","pageRowStart":"138075","pageSize":"25","recordCount":184904,"records":[{"id":70185168,"text":"70185168 - 1980 - Additional studies of competition and performance in OCS oil and gas sales, 1954-1975","interactions":[],"lastModifiedDate":"2017-03-27T14:14:22","indexId":"70185168","displayToPublicDate":"2000-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Additional studies of competition and performance in OCS oil and gas sales, 1954-1975","docAbstract":"

Economic rent is commonly defined in economics as any payment to a factor of production in excess of the minimum necessary to engage it in production. In the case of OCS lands owned by the federal government, the minimum supply price necessary to induce the federal government to lease production rights would be the costs of establishing and administering lease contracts. Assuming, for the sake of simplicity, that these costs are small enough to be ignored in the analysis, all payments to the federal government for use of OCS lands are forms of economic rent.

An ideal leasing system should transfer the full amount of economic rent implicit in OCS resources to the federal government. Whether such a complete transfer of economic rent occurs depends upon the conditions of competition in the market for OCS leases. The principal means for capturing economic rent under the bidding system employed by the federal government over the years 1954-1969 are the bonus paid by the highest bidder and a royalty payment which has historically been fixed at 16 2/3 percent of gross production value. Of less importance is an annual rental payment, usually about \\$3.00 per acre, which is paid as long as a tract under lease is not producing.

In the sections which follow, major factors affecting the capture of economic rent by the federal government are discussed and data are presented which demonstrate the importance of the different means used. In computing the amounts of economic rent captured by the federal government, the discounted cash flow technique is employed. This requires selection of an appropriate discount rate, in contrast to the internal rate of return analysis used in Part I, above.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70185168","usgsCitation":"Mead, W.J., and Sorensen, P.E., 1980, Additional studies of competition and performance in OCS oil and gas sales, 1954-1975, iii, 109 p., https://doi.org/10.3133/70185168.","productDescription":"iii, 109 p.","costCenters":[],"links":[{"id":337674,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70185168/report-thumb.jpg"},{"id":338393,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70185168/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58ca5301e4b0849ce97c8762","contributors":{"authors":[{"text":"Mead, Walter J.","contributorId":36564,"corporation":false,"usgs":true,"family":"Mead","given":"Walter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":684585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sorensen, Philip Edward","contributorId":103686,"corporation":false,"usgs":true,"family":"Sorensen","given":"Philip","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":684586,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37236,"text":"rp137 - 1980 - Handbook of acute toxicity of chemicals to fish and aquatic invertebrates : summaries of toxicity tests conducted at Columbia National Fisheries Research Laboratory, 1965-78","interactions":[],"lastModifiedDate":"2016-11-02T11:41:56","indexId":"rp137","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"137","title":"Handbook of acute toxicity of chemicals to fish and aquatic invertebrates : summaries of toxicity tests conducted at Columbia National Fisheries Research Laboratory, 1965-78","docAbstract":"

Acute toxicity is a major subject of research at Columbia National Fisheries Research Laboratory for evaluating the impact of toxic chemicals on fishery resources. The Laboratory has played a leading role in developing research technology for toxicity testing and data interpretation. In 1965-78, more than 400 chemicals were tested against a variety of invertebrates and fish species representative of both cold- and warm-water climates.

The use of acute toxicity tests for assessing the potential hazard of chemical contaminants to aquatic organisms is well documented (Boyd 1957; Henderson et al. 1960; Sanders and Cope 1966; Macek and McAllister 1970). Static acute toxicity tests provide rapid and (within limits) reproducible concentration-response curves for estimating toxic effects of chemicals on aquatic organisms. These tests provide a database for determining relative toxicity of a large number of chemicals to a variety of species and for estimating acute effects of chemical spills on natural aquatic systems; they also assist in determining priority and design of additional toxicity studies.

Acute toxicity tests usually provide estimates of the exposure concentration causing 50% mortality (LC50) to test organisms during a specified period of time. For certain invertebrates, the effective concentration is based on immobilization, or some other identifiable endpoint, rather than on lethality. The application of the LC50 has gained acceptance among toxicologists and is generally the most highly rated test for assessing potential adverse effects of chemical contaminants to aquatic life (Brungs and Mount 1978; American Institute for Biological Sciences 1978a).

The literature contains numerous papers dealing with the acute toxicity of chemicals to freshwater organisms. However, there is a tremendous need for a concise compendium of toxicity data covering a large variety of chemicals and test species. This Handbook is a compilation of a large volume of acute toxicity data from the Columbia Laboratory and its field laboratories. It presents definitive acute toxicity data on 271 chemicals tested against a variety of freshwater invertebrates and fishes. The chemicals represent all major groups of pesticides, as well as numerous industrial chemicals. This compilation should serve as a useful database for the many agencies and organizations dealing with research and management programs concerned with the impact of chemicals on aquatic resources.

The Columbia Laboratory has played a major role in developing currently used standard methodology for static acute toxicity testing. The use of standardized methodology greatly reduces variation in results. The data presented here have been carefully scrutinized to eliminate tests that failed to follow acceptable procedures. Handling of test organisms and procedures for static toxicity tests followed those described by Lennon and Walker (1964) and Macek and McAllister (1970), and conform well with those recommended by Brauhn and Schoettger (1975) and the Committee on Methods for Toxicity Tests with Aquatic Organisms (1975).

The species of fish and invertebrates that were tested are listed in phylogenetic order in Tables 1 and 2. Fish were obtained from Federal and State hatcheries as either eggs or fry. Original stocks of invertebrates were collected and cultured from wild populations with no known source of contamination; these populations were replenished regularly. The invertebrates were cultured in the Laboratory by methods similar to those described by Sanders and Cope (1966).

Test chemicals usually consisted of technical or analytical grade samples of known purity. Formulations of the chemicals were also tested when available. When purity of test chemicals was known, all calculated concentrations were based on percent active ingredients. Stock solutions were prepared immediately before each test, with commercial grade acetone as the carrier solvent. Occasionally, ethanol or dimethyl-formamide was substituted. Solvent concentrations did not exceed 0.5 mL/L in final dilution water.

Test water (dilution water) was reconstituted from deionized water of at least 106 ohms resistivity by the addition of appropriate reagent grade chemicals (Marking 1969). Water was buffered to maintain a pH of 7.2 to 7.5, an alkalinity of 30 to 35 mg/L, and a hardness of 40 to 50 mg/L as CaCO3. Test water was mixed thoroughly and aerated before transfer into test chambers. Fish were acclimated to dilution water by gradually changing the water in acclimated tanks from 100% well water to 100% reconstituted water over a 1- to 3-day period at the desired testing temperature. Invertebrates were acclimated from well water to dilution water over a 4- to 6-h period. Toxicity tests were conducted under static conditions without aeration, and the organisms were not fed during acclimation or testing. Temperature of test solutions was maintained within ± 1°C of that required for a given test.

Toxicity tests with fish were conducted in 18.9-liter (5-gal) wide-mouthed jars containing 15 liters of test solution. Fingerling fish weighing 0.2 to 1.5 g were tested at each concentration. Caution was taken not to exceed 0.8 g of test organisms per liter of solution. Duplicate test chambers were used to accommodate larger fish. Test chambers varied in size for invertebrates, depending on the species used; volume of test solution ranged from 0.25 to 4 liters. At least 10 organisms were exposed to each concentration for all definitive tests. At least six concentrations were used per toxicity test.

The tests began upon initial exposure to the toxicant and continued for 96 h. Immobilization tests with invertebrates were conducted for only 48 h. The number of dead or affected organisms in each test chamber were recorded and the dead organisms were removed every 24 h; general observations on the condition of test organisms were also recorded at these times.

Toxicity data were analyzed by a statistical method described by Litchfield and Wilcoxon (1949) to determine LC50 (theoretical estimate of the concentration lethal to 50% of the test animals) and 95% confidence intervals. This method is recommended by the American Public Health Association (1971) and by Sprague (1969) for determining median lethal concentrations. The procedure is easily modified for computing a single LC50 when replicate tests are performed.

","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Johnson, W.W., and Finley, M.T., 1980, Handbook of acute toxicity of chemicals to fish and aquatic invertebrates : summaries of toxicity tests conducted at Columbia National Fisheries Research Laboratory, 1965-78: Resource Publication 137, v, 98 p.","productDescription":"v, 98 p.","numberOfPages":"106","temporalStart":"1965-01-01","temporalEnd":"1978-12-31","costCenters":[],"links":[{"id":330650,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":290334,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/37236/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a538","contributors":{"authors":[{"text":"Johnson, W. Waynon","contributorId":89581,"corporation":false,"usgs":true,"family":"Johnson","given":"W.","email":"","middleInitial":"Waynon","affiliations":[],"preferred":false,"id":511199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finley, Mack T.","contributorId":73250,"corporation":false,"usgs":true,"family":"Finley","given":"Mack","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":511198,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61000,"text":"mf1250 - 1980 - Maps showing coal resources of the Crumpler quadrangle, Mercer, McDowell, and Wyoming Counties, West Virginia","interactions":[],"lastModifiedDate":"2021-09-27T21:13:25.508938","indexId":"mf1250","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1250","title":"Maps showing coal resources of the Crumpler quadrangle, Mercer, McDowell, and Wyoming Counties, West Virginia","docAbstract":"

Coal Geology

The Crumpler quadrangle lies in the Appalachian Plateaus province, with the coal bearing Pocahontas and New River Formations of Pennsylvanian age having a gentle dip toward the northwest. Coal bed maps were prepared (figures 1-7) and resources were estimated (table 1) for seven of the many coal beds in the Crumpler quadrangle (Stricker, 1980, lists the names of the various coal beds in the quadrangle) following methods established by U.S. Bureau of Mines and U.S. Geological Survey, 1976. All of these coal beds crop out at the surface in the quadrangle, have a maximum thickness thickness of over-burden of less than 300 meters, and have been mined at the surface, or under-ground, or both. Resource estimates were not calculated for other coal beds in the Pocahontas and New River Formations, either because of insufficient data of because of the beds are too thin. Figure 8 is a generalized stratigraphic column of the coal-bearing sequence in the Crumpler quadrangle showing thickness and relative positions of the various coal beds. The Crumpler quadrangle originally contained about 498 million metric tons of coal. Approximately 326 million metric tons have been mined, or lost in mining, leaving remaining resources of 172 million metric tons.

Analyses of the mined coal beds in the Crumpler and adjacent quadrangle show the coal is medium - to low volatile bituminous (most are low volatile bituminous), containing 14-27 percent volatile matter (with an arithmetic mean of 18 percent), 2.1-22.4 percent ash (with an arithmetic mean of 7 percent), and 0.5-1.8 percent total sulfur (with an arithmetic mean of 0.8 percent). Heating values range from 6,380 to 8,610 Kcal/kg on an as-received basis. Trace element and major and minor oxide composition, of both whole coal and laboratory ash, for 59 samples within or near the quadrangle were obtained from USCHEM (Geochemical Data File or National Coal Resources Data System), (Kozey and others, 1980.) Neither elements of environmental concern such as arsenic, lead, mercury, and selenium nor potentially valuable elements such as germanium, uranium and thorium were found in significant amounts in the coal.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1250","usgsCitation":"Stricker, G.D., 1980, Maps showing coal resources of the Crumpler quadrangle, Mercer, McDowell, and Wyoming Counties, West Virginia: U.S. Geological Survey Miscellaneous Field Studies Map 1250, 1 Plate: 33.84 x 31.87 inches, https://doi.org/10.3133/mf1250.","productDescription":"1 Plate: 33.84 x 31.87 inches","costCenters":[],"links":[{"id":183369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1250.jpg"},{"id":389851,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6860.htm"},{"id":284425,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1250/plate-1.pdf"}],"country":"United States","state":"West Virginia","county":"Mcdowell County, Mercer County, Wyoming County","otherGeospatial":"Crumpler quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.375,37.375 ], [ -81.375,37.5 ], [ -81.25,37.5 ], [ -81.25,37.375 ], [ -81.375,37.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6623e4b0b290851008bd","contributors":{"authors":[{"text":"Stricker, Gary D. gstricker@usgs.gov","contributorId":87163,"corporation":false,"usgs":true,"family":"Stricker","given":"Gary","email":"gstricker@usgs.gov","middleInitial":"D.","affiliations":[{"id":165,"text":"Central Energy Resources Team","active":false,"usgs":true}],"preferred":false,"id":264807,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37374,"text":"ssrw230 - 1980 - Breeding biology and relation of pollutants to black skimmers and gull-billed terns in South Carolina","interactions":[],"lastModifiedDate":"2020-02-24T12:24:05","indexId":"ssrw230","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"230","title":"Breeding biology and relation of pollutants to black skimmers and gull-billed terns in South Carolina","docAbstract":"

The breeding biology and relation of pollutants to black skimmers (Ryn chops niger) and gull-billed terns (Gelochelidon nilotica) were investigated in South Carolina from 1969 through 1975. With few exceptions, the two species nested together in colonies located on barrier islands. We located 10 colonies, 7 of which were on the Cape Romain National Wildlife Refuge (Cape Romain); references were located that described nesting on seven other islands in South Carolina that no longer support colonies.

Gull-billed terns nested from early May through July; the skimmers started later (late May) but also continued later (early September). Both species nested in areas subject to tidal flooding, and the two species persisted in nesting in several colonies despite intense predation by rats and gulls. Estimated reproductive success varied greatly from year to year and colony to colony; success in most colonies seemed low, particularly for the gull-billed tern.

Residues of organochlorine pollutants in several eggs seemed of sufficient magnitude to induce adverse effects on reproductivity and eggshell thickness: however, the overall effect of organochlorines appeared negligible.

Maximum numbers of nests located in a single year were 790 for the skimmer and 340 for the gull-billed tern: the total breeding population in South Carolina is unknown. Although nesting islands at Cape Romain and Deveaux Bank are sanctuaries for nesting birds, both species will continue to lose nesting habitat as additional sea islands are developed and inhabited by man.

","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Blus, L.J., and Stafford, C.J., 1980, Breeding biology and relation of pollutants to black skimmers and gull-billed terns in South Carolina: Special Scientific Report - Wildlife 230, 18 p.","productDescription":"18 p.","costCenters":[],"links":[{"id":167351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South 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management","interactions":[],"lastModifiedDate":"2020-02-21T16:24:08","indexId":"ssrw229","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"229","title":"The Rocky Mountain population of the western Canada goose: Its distribution, habitats, and management","docAbstract":"

The western Canada goose (Branta canadensis moffitti) was divided into a Rocky Mountain population (RMP) and a Pacific population (PP) on the basis of band recovery patterns examined in this study and recovery data from other investigators. Habitat information obtained from nine cooperating wildlife agencies within the RMP's range provided a base line for evaluating future changes in nesting, molting, and wintering areas. The habitat inventory indicated that none of the seasonal habitats were currently limiting the size of the RMP. The RMP's range is divided into 15 reference areas and these are briefly described. Past studies of Canada geese in the Intermountain Region are reviewed. Topics covered in the discussion of breeding biology are nesting chronology, spring population composition, breeding age, clutch size, nesting success. artificial nesting structures, and gosling survival. Much of the mortality of Canada geese occurs before the birds are fledged. Man-made nesting structures reduce losses during incubation. but research is needed on the relations between brooding sites and gosling survival. Some western Canada geese, mainly prebreeders and unsuccessful nesters, make molt migrations to and from molting areas during and after the brood-rearing season. More than half of these molt-migrants are yearlings too young to nest; there are indications that even some successful nesters leave nesting areas to molt before the fledging of their offspring. Geese 2 years old or older may serve as guides to traditional molting areas for the first-time migrants (i.e., yearlings). Lack of disturbance appears to influence selection of specific molting areas within the nesting range of moffitti, whereas movements of molters out of the Intermountain Region may be related to the evolution of this subspecies. Apparently. molters of both the PP and RMP that leave the Region go to the Northwest Territories of Canada. Although the taxonomic status of moffitti as related to the giant Canada goose (B. c. maxima) is unclear. these two subspecies are closely related. as evidenced by similar molt migrations to subarctic Canada. similar blood serum proteins. and only dinal differences in body size ,!!nd color. Mean annual survival rates for birds banded on nesting areas averaged 53 ± 2% (X̿ ± SE) for immatures and 64 ± 1 % for adults. Mean annual survival rates of adults captured on molting areas averaged 70 ± 1 %. Sport hunting accounts for more than 86% of the mortality of fledged Rocky Mountain geese. and hunting may limit the population's growth. Because the number of waterfowl hunters in the Rocky Mountain West is increasing, the continued expansion or future maintenance of the RMP may require more restrictive hunting regulations. Other management recommendations include the refinement and standardization of spring and winter aerial surveys, and more accurate age and sex determinations when geese are banded and color-marked.

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H.","contributorId":15204,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":189766,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":24583,"text":"ofr80929 - 1980 - Preliminary interpretations of geologic results obtained from boreholes UE25a-4,-5,-6, and -7, Yucca Mountain, Nevada Test Site","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr80929","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-929","title":"Preliminary interpretations of geologic results obtained from boreholes UE25a-4,-5,-6, and -7, Yucca Mountain, Nevada Test Site","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ; Open-File Services Section, Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/ofr80929","issn":"0094-9140","usgsCitation":"Spengler, R., and Rosenbaum, J.G., 1980, Preliminary interpretations of geologic results obtained from boreholes UE25a-4,-5,-6, and -7, Yucca Mountain, Nevada Test Site: U.S. Geological Survey Open-File Report 80-929, iii, 35 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr80929.","productDescription":"iii, 35 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":155132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0929/report-thumb.jpg"},{"id":53624,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0929/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53625,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0929/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673223","contributors":{"authors":[{"text":"Spengler, Richard W.","contributorId":91498,"corporation":false,"usgs":true,"family":"Spengler","given":"Richard W.","affiliations":[],"preferred":false,"id":192200,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenbaum, J. G.","contributorId":96685,"corporation":false,"usgs":true,"family":"Rosenbaum","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":192201,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23936,"text":"ofr80975 - 1980 - Selected water-level records for Oklahoma, 1979-80","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"ofr80975","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-975","title":"Selected water-level records for Oklahoma, 1979-80","docAbstract":"A systematic program to collect water-level records in Oklahoma began in 1937. The objectives of this program are (1) to provide long-term records of water-level fluctuations in representative wells, (2) to facilitate the prediction of water-level trends and indicate future availability of ground-water supplies, and (3) to provide information for use in basic research.\nWater-level data in table 1 are from wells that are measured annually, prior to the irrigation season to achieve the most natural representation of the static water level. Water level measurements listed in the column under 1979 may have been made during December 1978 or January, February, March, April, or May 1979. Measurements listed in the column 1980 may have been made during December 1979 or January, February, March, or April 1980. Figure 1 shows the counties and number of wells therein, where data were obtained for this report.\n\nRecords of water levels in Oklahoma are obtained through a cooperative program by the Oklahoma Water Resources Board and the U.S. Geological Survey. The Oklahoma Water Resources Board collects water level data for all counties in the State and the records are tabulated and published by the U.S. Geological Survey on an annual basis.\n\nThe stratigraphic nomenclature and age determinations used in this report are those accepted by the Oklahoma Geological Survey and do not necessarily agree with those at the U.S. Geological Survey except for the Cheyenne Sandstone which is considered to be Purgatoire Sandstone by the Oklahoma Geological Survey (Robert O. Fay, Personal Communication, August 9, 1979).","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80975","issn":"0094-9140","usgsCitation":"Mills, W.B., and Spiser, D.E., 1980, Selected water-level records for Oklahoma, 1979-80: U.S. Geological Survey Open-File Report 80-975, v, 59 p. :map ;26 cm., https://doi.org/10.3133/ofr80975.","productDescription":"v, 59 p. :map ;26 cm.","costCenters":[],"links":[{"id":94509,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015048180643?urlappend=%3Bseq=3"},{"id":156590,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d26","contributors":{"authors":[{"text":"Mills, Willard B.","contributorId":29390,"corporation":false,"usgs":true,"family":"Mills","given":"Willard","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":191003,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spiser, Dannie E.","contributorId":42214,"corporation":false,"usgs":true,"family":"Spiser","given":"Dannie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":191004,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11652,"text":"ofr801018 - 1980 - Chemical character of water in the Red River alluvial aquifer, Louisiana","interactions":[],"lastModifiedDate":"2023-03-14T22:44:57.106324","indexId":"ofr801018","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1018","title":"Chemical character of water in the Red River alluvial aquifer, Louisiana","docAbstract":"

The Red River alluvial aquifer of Louisiana underlies approximately 2,000 square miles in the Red River Valley of Louisiana. The aquifer is Pleistocene in age and consists of clay, silt, sand, and gravel deposited by the Red River. Sand and gravel constitute the lower two-thirds of the deposit, the most productive part of the aquifer. The aquifer ranges from 40 to 150 feet in thickness and reaches its maximum thickness in Avoyelles and Catahoula Parishes. Fine sand, silt, and clay of Holocene age overlie and generally confine the aquifer. These fine-grained deposits generally do not exceed 50 feet in thickness.

The aquifer is recharged by downward seepage of rainfall in the valley, by lateral movement of water from adjacent Pleistocene and Tertiary formations, and by upward movement of water from underlying formations of Tertiary age. When large quantities of seepage occur locally within short periods of time, a temporary reduction in mineralization takes place in the upper part of the aquifer. Lateral recharge from Pleistocene and Tertiary formations generally upgrades water in the alluvial aquifer near the edge of the valley. Recharge from underlying aquifers may upgrade or downgrade the quality of water in the lower part of the alluvial aquifer.

The Red River and its major tributaries recharge the Red River alluvial aquifer in local zones near the river during high stream stages, but noticeable water-quality changes occur only following periods of prolonged high stages.

Ground water in the alluvium generally moves toward the streams and down the valley. Water levels fluctuate seasonally and are generally less than 30 feet below land surface. Annual water-level fluctuations have a maximum range of about 30 feet near the Red River, and a minimum range of only a few feet in some interstream areas.

The Red River alluvial aquifer can yield 2,000 gallons per minute or more of water to individual wells where thick beds of coarse sand and gravel occur in the southern part of the study area. Aquifer tests indicate that the transmissivity ranges from 2,000 to 27,000 feet squared per day. The hydraulic conductivity ranges from 100 to 300 feet per day. Storage coefficients range from 6.0x10-4 to 1.0x10-3.

Water in the aquifer typically is of the calcium magnesium bicarbonate type. The water is hard to very hard, ranging in hardness from about 100 to 2,300 mg/L (milligrams per liter). However, hardness generally is in the 200- to 600-mg/L range. The ions that appear to be most variable in occurrence and sensitive to change with time are calcium, magnesium, iron, sulfate, and chloride. Iron concentrations range from less than 0.3 mg/L to as high as 49 mg/L but generally are 1 to 10 mg/L. In areas where rapid recharge occurs, shallow wells may have iron concentrations of less than 0.3 mg/L. Sulfate concentrations generally range from 0.5 to 50 mg/L but locally exceed 250 mg/L. The highest concentration detected was 1,900 mg/L. Chloride concentrations typically are less than 50 Mg/L. However, concentrations of chloride exceed 250 mg/L locally and are as high as 4,400 mg/L in a few areas. For this report, water with chloride concentrations greater than 250 mg/L is considered salty.

The base of freshwater in the Red River Valley generally coincides with the base of the alluvium at depths of 80 to 150 feet. However, locally, the aquifer contains salty water, and the base of freshwater occurs within the aquifer; in parts of Rapides, Caddo, and Natchitoches Parishes, the base of freshwater extends below the alluvium. The largest occurrence of salty water is in Natchitoches Parish, with other smaller bodies occurring in Red River, Caddo, and Bossier Parishes.

Water quality in the aquifer varies both areally and with depth; the quality also varies with time, depending on the quantity and chemical character of the recharge water.

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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80793","usgsCitation":"Karl, S.M., Berg, H.C., Grybeck, D., and Abramson, B.S., 1980, Preliminary map and tables describing metalliferous and selected nonmetalliferous mineral deposits in the Petersburg and eastern Port Alexander quadrangles, Alaska: U.S. Geological Survey Open-File Report 80-793, Report: 17 p.; 4 Plates: 34.56 × 31.86 inches or smaller, https://doi.org/10.3133/ofr80793.","productDescription":"Report: 17 p.; 4 Plates: 34.56 × 31.86 inches or smaller","costCenters":[],"links":[{"id":404295,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75434.htm","linkFileType":{"id":5,"text":"html"}},{"id":80398,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0793/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80397,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0793/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80396,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0793/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80395,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0793/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80394,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0793/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173193,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0793/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Petersburg and Port Alexander quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -134.5,\n 56\n ],\n [\n -132,\n 56\n ],\n [\n -132,\n 57\n ],\n [\n -134.5,\n 57\n ],\n [\n -134.5,\n 56\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d90b","contributors":{"authors":[{"text":"Karl, Susan M. 0000-0003-1559-7826 skarl@usgs.gov","orcid":"https://orcid.org/0000-0003-1559-7826","contributorId":502,"corporation":false,"usgs":true,"family":"Karl","given":"Susan","email":"skarl@usgs.gov","middleInitial":"M.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":226836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berg, H. C.","contributorId":36130,"corporation":false,"usgs":true,"family":"Berg","given":"H.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":226839,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grybeck, Donald","contributorId":8066,"corporation":false,"usgs":true,"family":"Grybeck","given":"Donald","affiliations":[],"preferred":false,"id":226837,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Abramson, B. S.","contributorId":29045,"corporation":false,"usgs":true,"family":"Abramson","given":"B.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":226838,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":11526,"text":"ofr801234 - 1980 - Where on Earth is all the lithium?; with a section on uranium isotope studies","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr801234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1234","title":"Where on Earth is all the lithium?; with a section on uranium isotope studies","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801234","usgsCitation":"Vine, J.D., and Dooley, J.R., 1980, Where on Earth is all the lithium?; with a section on uranium isotope studies: U.S. Geological Survey Open-File Report 80-1234, iii, 114 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr801234.","productDescription":"iii, 114 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":146379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1234/report-thumb.jpg"},{"id":39389,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1234/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e491e","contributors":{"authors":[{"text":"Vine, James David","contributorId":52147,"corporation":false,"usgs":true,"family":"Vine","given":"James","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":163303,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dooley, J. R. Jr.","contributorId":8110,"corporation":false,"usgs":true,"family":"Dooley","given":"J.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":163302,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":41293,"text":"ofr80424 - 1980 - Preliminary bathymetry of McCarty Fiord and Neoglacial changes of McCarty Glacier, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:49","indexId":"ofr80424","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-424","title":"Preliminary bathymetry of McCarty Fiord and Neoglacial changes of McCarty Glacier, Alaska","docAbstract":"Preliminary bathymetry (at 1:20,000 scale) and other scientific studies of McCarty Fiord, Alaska, Conducted by the Research Vessel Growler in 1978, showed this 15 mile-long waterway to be a narrow, deeply scoured basin enclosed by a terminal-moraine shoal. This valley was formerly filled by McCarty Glacier, which began a drastic retreat shortly after 1909; the glacier reached shallow water at the head of the fiord around 1960. The relative rate of retreat in deep water and on land is disclosed by the slower melting of stagnent ice left in a side valley. Soundings and profiles show the main channel to extend to a depth as great as 957 feet and to have the typical ' U ' shape of a glacier-eroded valley; since the glacier 's retreat, sediments have formed a nearly level deposit in the deepest part of the fiord. Old forest debris dated by carbon-14 indicates that a neoglacial advance of the glacier began before 3,395 years B.P. (before present); by 1,500 B.P. the glacier filled most of the fiord, and before the glacier culminated its advance around 1860 , two glacier-dammed lakes were formed in side valleys. (USGS)","language":"ENGLISH","doi":"10.3133/ofr80424","usgsCitation":"Post, A., 1980, Preliminary bathymetry of McCarty Fiord and Neoglacial changes of McCarty Glacier, Alaska: U.S. Geological Survey Open-File Report 80-424, 4 maps ;89 x 67 cm., https://doi.org/10.3133/ofr80424.","productDescription":"4 maps ;89 x 67 cm.","costCenters":[],"links":[{"id":171520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":19997,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19998,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19999,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20000,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c836","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":224787,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24046,"text":"ofr80952 - 1980 - Hydrogeology of the Seldovia area, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:10","indexId":"ofr80952","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-952","title":"Hydrogeology of the Seldovia area, Alaska","docAbstract":"Surficial materials in the Seldovia area, Alaska, are mapped as glacial drift over sedimentary bedrock, glacial drift over igneous and metamorphic bedrock, valley-bottom, alluvium, alluvial fan deposits, beach and intertidal deposits, and peat. Unconsolidated materials are generally less than 10 feet thick except in well-drained glacial deposits along the Seldovia-Jakolof Bay Road and in depressions in the bedrock surface. These depressions are poorly drained and commonly contain peat bogs. Development of domestic wells (1-15 gallons per minute) may be possible from unconsolidated materials and sedimentary bedrock, but larger water requirements must be met from surface-water sources. In areas having the water table or top of bedrock at shallow depths, effluent from sewage disposal systems may cause pollution of the land surface and nearby surface water. Seepage from hillside aquifers and unstable land along the coast of Kachemak Bay may adversely affect roads and structures. (USGS)","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr80952","issn":"0094-9140","usgsCitation":"Nelson, G.L., and Danskin, W.R., 1980, Hydrogeology of the Seldovia area, Alaska (WRI/OFR): U.S. Geological Survey Open-File Report 80-952, 1 map ;63 x 35 cm., in envelope 31 x 23 cm., https://doi.org/10.3133/ofr80952.","productDescription":"1 map ;63 x 35 cm., in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":108085,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11840.htm","linkFileType":{"id":5,"text":"html"},"description":"11840"},{"id":156318,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":53215,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0952/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53216,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0952/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614d21","contributors":{"authors":[{"text":"Nelson, Gordon L.","contributorId":55443,"corporation":false,"usgs":true,"family":"Nelson","given":"Gordon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Danskin, Wesley R. 0000-0001-8672-5501 wdanskin@usgs.gov","orcid":"https://orcid.org/0000-0001-8672-5501","contributorId":1034,"corporation":false,"usgs":true,"family":"Danskin","given":"Wesley","email":"wdanskin@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":191215,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23933,"text":"ofr801195 - 1980 - Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978","interactions":[],"lastModifiedDate":"2013-08-02T08:00:06","indexId":"ofr801195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1195","title":"Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978","docAbstract":"This report describes the observation-well network in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough Counties, Florida. Data obtained in 1978 from the network in and adjacent to the two well fields, as well as rainfall and pumpage records, are presented. The Southwest Florida Water Management District has established regulatory water-level limits in four observation wells and water-quality limits in three observation wells. Water levels dropped below regulatory limits in the spring of 1978 in three wells. Chloride concentrations in 1978 remained above regulatory limits for the entire year in one well and exceeded the limit during the late spring in the other two deep wells, both west of Eldridge-Wilde well field. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr801195","issn":"0094-9140","usgsCitation":"Mills, L.R., 1980, Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978: U.S. Geological Survey Open-File Report 80-1195, iv, 27 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr801195.","productDescription":"iv, 27 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":156575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1195/report-thumb.jpg"},{"id":275925,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1195/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606973","contributors":{"authors":[{"text":"Mills, L. R.","contributorId":26281,"corporation":false,"usgs":true,"family":"Mills","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":190997,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42673,"text":"ofr801270 - 1980 - Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah","interactions":[{"subject":{"id":42673,"text":"ofr801270 - 1980 - Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah","indexId":"ofr801270","publicationYear":"1980","noYear":false,"title":"Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66445,"text":"i1445 - 1983 - Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah","indexId":"i1445","publicationYear":"1983","noYear":false,"title":"Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah"},"id":1}],"supersededBy":{"id":66445,"text":"i1445 - 1983 - Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah","indexId":"i1445","publicationYear":"1983","noYear":false,"title":"Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah"},"lastModifiedDate":"2022-04-07T17:46:28.532055","indexId":"ofr801270","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1270","title":"Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah","docAbstract":"

No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801270","usgsCitation":"Machette, M., and Steven, T., 1980, Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah: U.S. Geological Survey Open-File Report 80-1270, 1 Plate: 42.74 x 27.50 inches, https://doi.org/10.3133/ofr801270.","productDescription":"1 Plate: 42.74 x 27.50 inches","costCenters":[],"links":[{"id":398325,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1270/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175563,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1270/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Beaver Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.75,38.3675 ], [ -112.75,38.5 ], [ -112.61749999999999,38.5 ], [ -112.61749999999999,38.3675 ], [ -112.75,38.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db67426e","contributors":{"authors":[{"text":"Machette, Michael N.","contributorId":28963,"corporation":false,"usgs":true,"family":"Machette","given":"Michael N.","affiliations":[],"preferred":false,"id":226916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steven, Thomas A.","contributorId":57529,"corporation":false,"usgs":true,"family":"Steven","given":"Thomas A.","affiliations":[],"preferred":false,"id":226917,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23957,"text":"ofr80581 - 1980 - Ground-water models for water resources planning","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr80581","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-581","title":"Ground-water models for water resources planning","docAbstract":"In the past decade hydrologists have emphasized the development of computer-based mathematical models to aid in the understanding of flow, the transport of solutes, transport of heat, and deformation in the groundwater system. These models have been used to provide information and predictions for water managers. Too frequently, groundwater was neglected in water-resource planning because managers believed that it could not be adequately evaluated in terms of availability, quality, and effect of development on surface water supplies. Now, however, with newly developed digital groundwater models, effects of development can be predicted. Such models have been used to predict hydrologic and quality changes under different stresses. These models have grown in complexity over the last 10 years from simple one-layer flow models to three-dimensional simulations of groundwater flow which may include solute transport, heat transport, effects of land subsidence, and encroachment of salt water. This paper illustrates, through case histories, how predictive groundwater models have provided the information needed for the sound planning and management of water resources in the United States. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80581","issn":"0094-9140","usgsCitation":"Moore, J.E., 1980, Ground-water models for water resources planning: U.S. Geological Survey Open-File Report 80-581, 25 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr80581.","productDescription":"25 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0581/report-thumb.jpg"},{"id":53155,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0581/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69807b","contributors":{"authors":[{"text":"Moore, John E.","contributorId":33688,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":191040,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23998,"text":"ofr802039 - 1980 - Surficial geology of Central Square quadrangle, Oswego County, New York","interactions":[],"lastModifiedDate":"2022-09-14T21:50:01.013787","indexId":"ofr802039","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-2039","title":"Surficial geology of Central Square quadrangle, Oswego County, New York","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr802039","usgsCitation":"Muller, E.H., and Miller, T.S., 1980, Surficial geology of Central Square quadrangle, Oswego County, New York (WRI/OFR): U.S. Geological Survey Open-File Report 80-2039, 1 Plate: 24.25 × 27.36 inches, https://doi.org/10.3133/ofr802039.","productDescription":"1 Plate: 24.25 × 27.36 inches","costCenters":[],"links":[{"id":156306,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":397652,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75392.htm","linkFileType":{"id":5,"text":"html"}},{"id":53180,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/2039/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New York","county":"Oswego County","otherGeospatial":"Central Square quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.125,\n 43.25\n ],\n [\n -76.25,\n 43.25\n ],\n [\n -76.25,\n 43.375\n ],\n [\n -76.125,\n 43.375\n ],\n [\n -76.125,\n 43.25\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c15","contributors":{"authors":[{"text":"Muller, Ernest Hathaway","contributorId":96297,"corporation":false,"usgs":true,"family":"Muller","given":"Ernest","email":"","middleInitial":"Hathaway","affiliations":[],"preferred":false,"id":191119,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Todd S. tsmiller@usgs.gov","contributorId":1190,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"tsmiller@usgs.gov","middleInitial":"S.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":191118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24116,"text":"ofr80958 - 1980 - January 1980 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2017-09-29T08:45:22","indexId":"ofr80958","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-958","title":"January 1980 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"

This report contains hydrologic data on water-level measurements in observation wells in western and south-central Kansas. The measurements were made in mid-winter, mostly in January, when pumping was minimal and water levels had recovered from the effects of pumping during the previous irrigation season. This report also provides basic hydrologic data for relating water-level changes from a \"base-reference year\" (pre-development year), a year of abnormally high rainfall and minimum pumpage (1966), and the previous year (1979). The \"base-reference year\" i s designated as 1950 for the northwestern and west-central areas, 1940 for the southwestern area, and 1944 for the south-central area. Water-level data in the south-central area also are compared with data for 1974. \"Base-reference-year\" water levels are based on measurements made during that year and on interpretation of water-table-contour maps.

Tables in the report show the depths to water level in 1940, 1944, or 1950 (pre-development years), 1966, 1974, 1979, and 1980; water-level changes from 1940-80,1944-80,1950-80,1966-80,1974-80, and 1979-80; and the average annual changes from 1940-80, 1944-80, 1950-80, 1966-80, and 1974-80. Also shown are saturated thicknesses of the deposits in 1940, 1944, or 1950, and in 1980, as well as the percentage change in saturated thickness from 1940-80, 1944-80, or 1950-80.

Maps in the report, drawn by digital plotter, show the location of observation wells where water-level measurements are made. The water-level rise or decline, 1979-80, is given to the nearest 0.01 foot; two values at the same location indicate separate wells in the same 10-acre tract.

The annual water-level measurements are made by personnel of the Division of Water Resources of the Kansas State Board of Agriculture and of the U.S. Geological Survey. State-agency support for this program is provided through the Kansas Geological Survey.

Wells in this report are numbered according to the Bureau of Land Manage- ment's system of land subdivision. In this system, the first set of digits of a well number indicates the township; the second set, the range east or west of the sixth principal meridian; and the third set, the section in which the well is situated. The first letter denotes the 160-acre tract within the section; the second, the 40-acre tract, and the third, the 10-acre tract. The letters, A, B, C, or D, are designated in a counterclockwise direction beginning in the northeast quadrant. Because there may be more than one well in a 10-acre tract, consecutive numbers, beginning with \"1\", are added in the order in which the data from the wells are collect.

Explanation of geologic units in tables 1 and 2 are: QA, Quaternary alluvium; QU, undifferentiated Quaternary deposits; TO, Ogallala Formation; KN, Niobrara Formation; KU, undifferentiated Lower Cretaceous rocks; KJ, undiffer-rentiated Lower Cretaceous and Upper Jurassic rocks.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80958","issn":"0094-9140","usgsCitation":"Pabst, M., 1980, January 1980 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 80-958, 166 p., https://doi.org/10.3133/ofr80958.","productDescription":"166 p.","numberOfPages":"170","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":346230,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0958/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0958/report-thumb.jpg"}],"country":"United 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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801208","usgsCitation":"Muller, E.H., and Miller, T.S., 1980, Surficial geology of New Haven quadrangle, Oswego County, New York (WRI/OFR): U.S. Geological Survey Open-File Report 80-1208, 1 Plate: 24.07 × 26.99 inches, https://doi.org/10.3133/ofr801208.","productDescription":"1 Plate: 24.07 × 26.99 inches","costCenters":[],"links":[{"id":157491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":397654,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75368.htm"},{"id":53182,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1208/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New York","county":"Oswego County","otherGeospatial":"New Haven quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.375,\n 43.5\n ],\n [\n -76.25,\n 43.5\n ],\n [\n -76.25,\n 43.375\n ],\n [\n -76.375,\n 43.375\n ],\n [\n -76.375,\n 43.5\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c10","contributors":{"authors":[{"text":"Muller, Ernest Hathaway","contributorId":96297,"corporation":false,"usgs":true,"family":"Muller","given":"Ernest","email":"","middleInitial":"Hathaway","affiliations":[],"preferred":false,"id":191124,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Todd S. tsmiller@usgs.gov","contributorId":1190,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"tsmiller@usgs.gov","middleInitial":"S.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":191123,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23919,"text":"ofr801114 - 1980 - Surficial geology of part of Sandy Creek quadrangle, Oswego County, New York","interactions":[],"lastModifiedDate":"2022-03-25T21:38:12.899738","indexId":"ofr801114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1114","title":"Surficial geology of part of Sandy Creek quadrangle, Oswego County, New York","docAbstract":"

The location and extent of 11 kinds of surficial deposits in part of Sandy Creek quadrangle, Oswego County, N.Y., are mapped on a 7.5-minute U.S. Geological Survey topographic map. The map was compiled to indicate the lithology and potential for groundwater development at any specific location.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801114","usgsCitation":"Miller, T.S., 1980, Surficial geology of part of Sandy Creek quadrangle, Oswego County, New York (WRI/OFR): U.S. Geological Survey Open-File Report 80-1114, 1 Plate: 23.61 × 26.58 inches, https://doi.org/10.3133/ofr801114.","productDescription":"1 Plate: 23.61 × 26.58 inches","costCenters":[],"links":[{"id":157039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":397648,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75344.htm"},{"id":53129,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1114/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New York","county":"Oswego County","otherGeospatial":"Sandy Creek quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76,\n 43.7167\n ],\n [\n -76.125,\n 43.7167\n ],\n [\n -76.125,\n 43.625\n ],\n [\n -76,\n 43.625\n ],\n [\n -76,\n 43.7167\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e481ee4b07f02db4e00ee","contributors":{"authors":[{"text":"Miller, Todd S. tsmiller@usgs.gov","contributorId":1190,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"tsmiller@usgs.gov","middleInitial":"S.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":190976,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41290,"text":"ofr80426 - 1980 - Preliminary bathymetry— Esther Passage and channels east to Eaglek Island, Alaska","interactions":[],"lastModifiedDate":"2021-11-17T19:48:58.829524","indexId":"ofr80426","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-426","title":"Preliminary bathymetry— Esther Passage and channels east to Eaglek Island, Alaska","docAbstract":"

A map, scale 1:20,000, shows water depths, rocks, and hazards to navigation. These data are noted on track lines run by the Research Vessel Growler in Alaskan waters, where data on navigation shown on published charts are nonexistant, preliminary, or out dated.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80426","usgsCitation":"Post, A., 1980, Preliminary bathymetry— Esther Passage and channels east to Eaglek Island, Alaska: U.S. Geological Survey Open-File Report 80-426, 1 Plate: 52.00 × 36.00 inches, https://doi.org/10.3133/ofr80426.","productDescription":"1 Plate: 52.00 × 36.00 inches","costCenters":[],"links":[{"id":171517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20001,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0426/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391812,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11631.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Eagle Island, Esther Passage","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -148.033,\n 60.783\n ],\n [\n -147.667,\n 60.783\n ],\n [\n -147.667,\n 60.925\n ],\n [\n -148.033,\n 60.925\n ],\n [\n -148.033,\n 60.783\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9ec","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":224784,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41289,"text":"ofr80428 - 1980 - Preliminary bathymetry: Approaches to Unakwik Inlet, Alaska","interactions":[],"lastModifiedDate":"2021-12-09T20:14:21.720437","indexId":"ofr80428","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-428","title":"Preliminary bathymetry: Approaches to Unakwik Inlet, Alaska","docAbstract":"

A map, scale 1:20,000, shows water depths, rocks, and hazards to navigation. These data are noted on track lines run by the Research Vessel Growler in Alaskan waters, where data on navigation shown on published charts are nonexistant, preliminary, or out dated. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80428","usgsCitation":"Post, A., 1980, Preliminary bathymetry: Approaches to Unakwik Inlet, Alaska: U.S. Geological Survey Open-File Report 80-428, 1 Plate: 39.00 × 46.00 inches, https://doi.org/10.3133/ofr80428.","productDescription":"1 Plate: 39.00 × 46.00 inches","costCenters":[],"links":[{"id":108034,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11633.htm","linkFileType":{"id":5,"text":"html"},"description":"11633"},{"id":20002,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0428/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Unakwik Inlet","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -147.6947021484375,\n 60.86764961744716\n ],\n [\n -147.35687255859375,\n 60.86764961744716\n ],\n [\n -147.35687255859375,\n 61.01572481397616\n ],\n [\n -147.6947021484375,\n 61.01572481397616\n ],\n [\n -147.6947021484375,\n 60.86764961744716\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9f4","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":224783,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41360,"text":"ofr80245 - 1980 - Preliminary geologic map of the La Honda and San Gregorio quadrangles, San Mateo County, California","interactions":[],"lastModifiedDate":"2018-06-14T11:28:01","indexId":"ofr80245","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-245","title":"Preliminary geologic map of the La Honda and San Gregorio quadrangles, San Mateo County, California","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80245","usgsCitation":"Brabb, E.E., 1980, Preliminary geologic map of the La Honda and San Gregorio quadrangles, San Mateo County, California: U.S. Geological Survey Open-File Report 80-245, Map: 59 x 89 cm., https://doi.org/10.3133/ofr80245.","productDescription":"Map: 59 x 89 cm.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":172935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110619,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75236.htm","linkFileType":{"id":5,"text":"html"},"description":"75236"},{"id":79114,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0245/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b1c0","contributors":{"authors":[{"text":"Brabb, Earl E.","contributorId":48939,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":224895,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24002,"text":"ofr801113 - 1980 - Surficial geology of West of Texas quadrangle, Oswego County, New York","interactions":[],"lastModifiedDate":"2022-03-25T22:18:53.51598","indexId":"ofr801113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1113","title":"Surficial geology of West of Texas quadrangle, Oswego County, New York","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801113","usgsCitation":"Muller, E.H., 1980, Surficial geology of West of Texas quadrangle, Oswego County, New York (WRI/OFR): U.S. Geological Survey Open-File Report 80-1113, 1 Plate: 18.60 × 26.75 inches, https://doi.org/10.3133/ofr801113.","productDescription":"1 Plate: 18.60 × 26.75 inches","costCenters":[],"links":[{"id":157493,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":397656,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75343.htm"},{"id":53184,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1113/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New York","county":"Oswego County","otherGeospatial":"West of Texas quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.375,\n 43.5\n ],\n [\n -76.4333,\n 43.5\n ],\n [\n -76.4333,\n 43.5333\n ],\n [\n -76.375,\n 43.5333\n ],\n [\n -76.375,\n 43.5\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b72","contributors":{"authors":[{"text":"Muller, Ernest Hathaway","contributorId":96297,"corporation":false,"usgs":true,"family":"Muller","given":"Ernest","email":"","middleInitial":"Hathaway","affiliations":[],"preferred":false,"id":191127,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}