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No abstract available.

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No abstract available.

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The principal Middle Ordovician formations containing high-purity sands are the St. Peter Sandstone which crops out extensively from Minnesota to Arkansas; the Everton Formation principally of Arkansas; and the Oil Creek, McLish, and Tulip Creek Formations (all of the Simpson Group) of Oklahoma. The St. Peter and sandy beds in the other formations are commonly called \"sandstones,\" but a more appropriate term is \"sands\" for in most fresh exposures they are completely uncemented or very weakly cemented. On exposure to air, uncemented sands usually become \"case hardened\" where evaporating ground water precipitates mineral matter at the surface; but this is a surficial effect. 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No abstract available.

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B.","contributorId":31375,"corporation":false,"usgs":true,"family":"Simon","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146805,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":146806,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44116,"text":"ofr79901 - 1979 - Unevaluated reconnaissance map of the Arkansas River, Colorado, 1921","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"ofr79901","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-901","title":"Unevaluated reconnaissance map of the Arkansas River, Colorado, 1921","language":"ENGLISH","doi":"10.3133/ofr79901","issn":"ma","usgsCitation":"Jones, E., 1979, Unevaluated reconnaissance map of the Arkansas River, Colorado, 1921: U.S. Geological Survey Open-File Report 79-901, 1 map ;on 4 sheets smaller than 108 x 128 cm., https://doi.org/10.3133/ofr79901.","productDescription":"1 map ;on 4 sheets smaller than 108 x 128 cm.","costCenters":[],"links":[{"id":162333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":99133,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0901/plate-1.pdf","size":"2534","linkFileType":{"id":1,"text":"pdf"}},{"id":99134,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0901/plate-2.pdf","size":"1750","linkFileType":{"id":1,"text":"pdf"}},{"id":99135,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0901/plate-3.pdf","size":"3594","linkFileType":{"id":1,"text":"pdf"}},{"id":99136,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0901/plate-4.pdf","size":"2582","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f5cd","contributors":{"authors":[{"text":"Jones, E.E.","contributorId":49413,"corporation":false,"usgs":true,"family":"Jones","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":229180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29277,"text":"wri7927 - 1979 - Estimating the gas and dye quantities for modified tracer technique measurements of stream reaeration coefficients","interactions":[],"lastModifiedDate":"2019-11-14T14:50:03","indexId":"wri7927","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-27","title":"Estimating the gas and dye quantities for modified tracer technique measurements of stream reaeration coefficients","docAbstract":"Measuring the reaeration coefficient of a stream with a modified tracer technique has been accomplished by injecting either ethylene or ethylene and propane together and a rhodamine-WT dye solution into the stream. The movement of the tracers through the stream reach after injection is described by a one-dimensional diffusion equation. The peak concentrations of the tracers at the downstream end of the reach depend on the concentrations of the tracers in the stream at the injection site, the longitudinal dispersion coefficient, the mean water velocity, the length of the reach, and the duration of the injection period. The downstream gas concentrations also depend on the gas desorption coefficients of the reach. The concentrations of the tracer gases in the stream at the injection site depend on the flow rates of the gases through the injection diffusers, the efficiency of the gas absorption process, and the stream discharge. The concentration of dye in the stream at the injection site depends on the flow rate of the dye solution, the concentration of the dye solution, and the stream discharge. Equations for estimating the gas flow rates, the quantities of the gases, the dye concentration, and the quantity of dye together with procedures for determining the variables in these equations are presented. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7927","usgsCitation":"Rathbun, R.E., 1979, Estimating the gas and dye quantities for modified tracer technique measurements of stream reaeration coefficients: U.S. Geological Survey Water-Resources Investigations Report 79-27, viii, 42 p. , https://doi.org/10.3133/wri7927.","productDescription":"viii, 42 p. ","costCenters":[],"links":[{"id":369231,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0027/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0027/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc6f8","contributors":{"authors":[{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":201263,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4237,"text":"cir790 - 1979 - Assessment of geothermal resources of the United States: 1978","interactions":[],"lastModifiedDate":"2022-12-20T21:12:51.641683","indexId":"cir790","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"790","title":"Assessment of geothermal resources of the United States: 1978","docAbstract":"

The geothermal resource assessment presented in this Circular is a refinement and updating of USGS Circular 726. Nonproprietary information available in June 1978 is used to assess geothermal energy in the ground and, when possible, to evaluate the fraction that might be recovered at the surface. Five categories of geothermal energy are discussed:

a. Conduction-dominated regimes

b. Igneous-related geothermal systems

c. High-temperature (>1500C) and intermediate-temperature (90°-150°C) hydrothermal convection systems

d. Low-temperature (<900C) geothermal waters

e. Geopressured-geothermal energy (both thermal energy and energy from dissolved methane).

Assessment data are presented on three colored maps prepared in cooperation with the National Oceanic and Atmospheric Administration.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir790","collaboration":"Prepared in cooperation with the Department of Energy","usgsCitation":"Muffler, L.P., 1979, Assessment of geothermal resources of the United States: 1978: U.S. Geological Survey Circular 790, Report: iv, 163 p.; 3 Plates: 34.51 x 46.16 inches and smaller, https://doi.org/10.3133/cir790.","productDescription":"Report: iv, 163 p.; 3 Plates: 34.51 x 46.16 inches and smaller","costCenters":[],"links":[{"id":410818,"rank":6,"type":{"id":36,"text":"NGMDB Index 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Patrick 0000-0001-6638-7218 pmuffler@usgs.gov","orcid":"https://orcid.org/0000-0001-6638-7218","contributorId":3322,"corporation":false,"usgs":true,"family":"Muffler","given":"L.J.","email":"pmuffler@usgs.gov","middleInitial":"Patrick","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":148524,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48423,"text":"ofr79417 - 1979 - Suspended- and bedload-sediment transport in the Snake and Clearwater rivers in the vicinity of Lewiston, Idaho, August 1976 through July 1978","interactions":[],"lastModifiedDate":"2014-06-18T10:51:50","indexId":"ofr79417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-417","title":"Suspended- and bedload-sediment transport in the Snake and Clearwater rivers in the vicinity of Lewiston, Idaho, August 1976 through July 1978","docAbstract":"

Impoundment of water in the Snake River and Clearwater River arms behind Lower Granite Dam (see cover map) began in June 1975. At this time, Lower Granite Reservoir and Lock facilities, constructed by the USACE (U.S. Army Corps of Engineers), Walla Walla District, became operational. Construction and operation of this facility necessitated collection of hydrologic data that did not exist prior to construction. The USACE requested the USGS (U.S. Geological Survey) to collect hydraulic- and channel-geometry data and describe sediment-transport characteristics, beginning in the spring of 1972.

\n
\n

This report summarizes information collected during August 1976 through July 1978 and is the fifth in a series of reports designed to release hydrologic data on a timely basis. Although some of the data were collected during the late summer and fall periods (August through December) of 1976 and 1977, most were collected during the spring runoff periods of 1977 and 1978. Therefore, for convenience, data contained in this report will be referred to as the 1977-78 data. Because this is primarily a basic-data report, no interpretation of the data is provided.

\n
\n

This report presents tables of selected data collected and computations compiled since the 1976 report (Seitz, 1976). Most of the tabular data are also presented on graphs. Some of the graphs show plots of data since 1972~ others show plots of only the 1977-78 data.

\n
\n

Relatively minor amounts of bedload were transported during the 1977 drought period. Therefore, regular scheduled sampling of the bedload was impractical. Only two bedload samples were collected from the Clearwater River in 1977. The resultant data are included in tables 10, 12, and 14, and figure 6. All bedload data in this report should be considered tentative, pending completion of sampler-calibration studies and possible adjustment of the data to\ncorrect for sampler efficiency.

\n
\n

An analysis of the middle Snake River streamflow record was made during 1977. The streamflow rating for the Snake River near Anatone, Washington, gage was found to be in error at high stages. The streamflow record for water years 1974 and 1975 was revised and published with 1976 water-year data (Water Resources Data for Idaho, Water Year 1976). The revised Snake River near Anatone streamflow rating was used to recompute the sediment-discharge rating curve (fig. 3).

\n
\n

This study program is funded by the USACE through a cooperative agreement with the USGS. All field work, laboratory analysis, and compilation of data are being conducted by the USGS.

\n
\n

Data collection is scheduled to terminate at the end of the 1979 runoff season. A reanalysis of all data collected since the start of the program will correct all provisional records since 1972, including the 1974, 1975, and 1976 years for the Snake River near Anatone station.

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A feature of the analysis, differing from techniques used for previous editions of the national chart, is that analytic models define the regional magnetic field and are used to contour the magnetic charts.\r\n\r\nAn overall rms (root mean square) fit of less than 235 nT was obtained for the horizontal and vertical intensities; for the chart of magnetic declination, the rms deviation was on the order of 0.5 degrees. The models of annual change, derived from data at repeat stations and observatories operated by the U.S. Geological Survey, yielded an rms deviation of approximately 6 nT/yr in the force components and 0.7 min/yr in magnetic declination.","language":"ENGLISH","publisher":"Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir810","usgsCitation":"Fabiano, E.B., Jones, W.J., and Peddie, N.W., 1979, The magnetic charts of the United States for Epoch 1975: U.S. Geological Survey Circular 810, iii, 15 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir810.","productDescription":"iii, 15 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":124791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1979/0810/report-thumb.jpg"},{"id":31052,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1979/0810/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6990ed","contributors":{"authors":[{"text":"Fabiano, Eugene B.","contributorId":9234,"corporation":false,"usgs":true,"family":"Fabiano","given":"Eugene","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":147912,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, W. J.","contributorId":79088,"corporation":false,"usgs":true,"family":"Jones","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":147914,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peddie, Norman W.","contributorId":68711,"corporation":false,"usgs":true,"family":"Peddie","given":"Norman","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":147913,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":36773,"text":"fwsobs79_27 - 1979 - Cooperative Instream Flow Service Group, September 1977-December 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:10:00","indexId":"fwsobs79_27","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"79/27","title":"Cooperative Instream Flow Service Group, September 1977-December 1978","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"U.S. Fish and Wildlife Service, 1979, Cooperative Instream Flow Service Group, September 1977-December 1978: FWS/OBS 79/27, 16 p. : ill.; 27 cm.","productDescription":"16 p. : ill.; 27 cm.","costCenters":[],"links":[{"id":165393,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68650e","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529586,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36770,"text":"fwsobs79_24 - 1979 - Decline of submerged aquatic plants in Chesapeake Bay","interactions":[],"lastModifiedDate":"2012-02-02T00:10:00","indexId":"fwsobs79_24","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"79/24","title":"Decline of submerged aquatic plants in Chesapeake Bay","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Stevenson, J.C., Confer, N., and Pieper, C.B., 1979, Decline of submerged aquatic plants in Chesapeake Bay: FWS/OBS 79/24, 12 p.","productDescription":"12 p.","costCenters":[],"links":[{"id":165390,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db67273a","contributors":{"authors":[{"text":"Stevenson, J. 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During 1978 twenty dredge sites were occupied and successfully dredged from the R.V. S.P. LEE along the eastern Bering Sea continental margin (Fig. 1). A total of several tons of rock were collected using a chain-bag dredge. Samples were recovered in water depths ranging from 750 to 2,750 meters from exposures along the continental slope bordering the large Bering Sea shelf.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791139","usgsCitation":"Marlow, M.S., Cooper, A.K., Scholl, D.W., Vallier, T.L., and McLean, H., 1979, Description of dredge samples from the Bering Sea continental margin: U.S. Geological Survey Open-File Report 79-1139, 6 p., https://doi.org/10.3133/ofr791139.","productDescription":"6 p.","costCenters":[],"links":[{"id":141536,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1139/report-thumb.jpg"},{"id":424697,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -185.15090325261252,\n 57.09189815353466\n ],\n [\n -185.15090325261252,\n 50.777014004737026\n ],\n [\n -160.1657690351336,\n 50.777014004737026\n ],\n [\n -160.1657690351336,\n 57.09189815353466\n ],\n [\n -185.15090325261252,\n 57.09189815353466\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dbf5","contributors":{"authors":[{"text":"Marlow, Michael S.","contributorId":72775,"corporation":false,"usgs":true,"family":"Marlow","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":154280,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, Alan K. acooper@usgs.gov","contributorId":2854,"corporation":false,"usgs":true,"family":"Cooper","given":"Alan","email":"acooper@usgs.gov","middleInitial":"K.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":154278,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scholl, David W. 0000-0001-6500-6962 dscholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6500-6962","contributorId":3738,"corporation":false,"usgs":true,"family":"Scholl","given":"David","email":"dscholl@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":154282,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vallier, Tracy L.","contributorId":28857,"corporation":false,"usgs":true,"family":"Vallier","given":"Tracy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":154279,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McLean, Hugh","contributorId":73977,"corporation":false,"usgs":true,"family":"McLean","given":"Hugh","affiliations":[],"preferred":false,"id":154281,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":36909,"text":"fwsobs77_19 - 1979 - Guidelines for preparing expert testimony in water management decisions related to instream flow issues. IFIP No. 1","interactions":[],"lastModifiedDate":"2018-10-01T19:55:26","indexId":"fwsobs77_19","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"77/19","title":"Guidelines for preparing expert testimony in water management decisions related to instream flow issues. IFIP No. 1","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Sweetman, D.A., 1979, Guidelines for preparing expert testimony in water management decisions related to instream flow issues. IFIP No. 1 (Revised Edition): FWS/OBS 77/19, 32 p.; 27 cm.","productDescription":"32 p.; 27 cm.","costCenters":[],"links":[{"id":92229,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015017874655?urlappend=%3Bseq=5"},{"id":166707,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revised Edition","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a2ab","contributors":{"editors":[{"text":"Lamb, Berton L.","contributorId":6919,"corporation":false,"usgs":true,"family":"Lamb","given":"Berton L.","affiliations":[],"preferred":false,"id":747071,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Sweetman, Debra A.","contributorId":35377,"corporation":false,"usgs":true,"family":"Sweetman","given":"Debra","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":217156,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10250,"text":"ofr79934 - 1979 - Paleoecological evaluation of Late Eocene biostratigraphic zonations on the west coast","interactions":[{"subject":{"id":10250,"text":"ofr79934 - 1979 - Paleoecological evaluation of Late Eocene biostratigraphic zonations on the west coast","indexId":"ofr79934","publicationYear":"1979","noYear":false,"title":"Paleoecological evaluation of Late Eocene biostratigraphic zonations on the west coast"},"predicate":"SUPERSEDED_BY","object":{"id":70043180,"text":"70043180 - 1980 - Paleoecological evaluation of Late Eocene biostratigraphic zonations of the Pacific Coast of North America","indexId":"70043180","publicationYear":"1980","noYear":false,"title":"Paleoecological evaluation of Late Eocene biostratigraphic zonations of the Pacific Coast of North America"},"id":1}],"supersededBy":{"id":70043180,"text":"70043180 - 1980 - Paleoecological evaluation of Late Eocene biostratigraphic zonations of the Pacific Coast of North America","indexId":"70043180","publicationYear":"1980","noYear":false,"title":"Paleoecological evaluation of Late Eocene biostratigraphic zonations of the Pacific Coast of North America"},"lastModifiedDate":"2013-02-06T18:27:39","indexId":"ofr79934","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-934","title":"Paleoecological evaluation of Late Eocene biostratigraphic zonations on the west coast","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79934","usgsCitation":"McDougall, K.A., 1979, Paleoecological evaluation of Late Eocene biostratigraphic zonations on the west coast: U.S. Geological Survey Open-File Report 79-934, ix, 215 p. :ill., map., https://doi.org/10.3133/ofr79934.","productDescription":"ix, 215 p. :ill., map.","costCenters":[],"links":[{"id":143092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d14","contributors":{"authors":[{"text":"McDougall, Kristin A.","contributorId":69146,"corporation":false,"usgs":true,"family":"McDougall","given":"Kristin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161077,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28327,"text":"wri7957 - 1979 - Map showing ground-water conditions in the Virgin River, Grand Wash, and Shivwits areas, Mohave County, Arizona, 1976","interactions":[],"lastModifiedDate":"2019-07-26T15:50:41","indexId":"wri7957","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-57","title":"Map showing ground-water conditions in the Virgin River, Grand Wash, and Shivwits areas, Mohave County, Arizona, 1976","docAbstract":"The Virgin River, Grand Wash, and Shivwits areas include about 3 ,250 square miles in northwestern Arizona. Ground water is obtained mainly from the alluvium, conglomerate, and basalt; however, several other formations yield small amounts of water to some wells. In the Virgin River area, most wells are less than 200 feet deep, water levels range from 17 to 310 feet below the land surface, and well yields range from a few gallons per minute to as much as 2,000 gallons per minute. Springs in the Littlefield area contribute about 70 cubic feet per second of water to the Virgin River. In the Grand Wash area wells are from 35 to 850 feet deep, and water levels range from 5 to 759 feet below the land surface. In the Shivwits area wells are from 10.5 to 300 feet deep, and water levels range from 10 to 256 feet below the land surface. The chemical quality of the water varies with location and aquifer in the report area. Information shown on the map (scale 1:125,000) includes the principal aquifer that furnishes water to wells and springs, depth to water, altitude of the water level, and specific conductance and fluoride concentrations. 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