Review of quantitative data, restricted range in gold content (rarely more than 10 ppb, generally below 5 ppb), mafic rocks have more, so do early crystallizing minerals, no use in exploration, factors other than concentration determine mineralization; examples
","language":"English","publisher":"American Geological Institute","doi":"10.2113/gsecongeo.68.2.168","usgsCitation":"Tilling, R.I., Gottfried, D., and Rowe, J., 1973, Gold abundance in igneous rocks; bearing on gold mineralization: Economic Geology, v. 68, no. 2, p. 168-186, https://doi.org/10.2113/gsecongeo.68.2.168.","productDescription":"19 p.","startPage":"168","endPage":"186","costCenters":[{"id":153,"text":"California Volcano Observatory","active":false,"usgs":true}],"links":[{"id":376228,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"68","issue":"2","noUsgsAuthors":false,"publicationDate":"1973-04-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Tilling, Robert I. 0000-0003-4263-7221 rtilling@usgs.gov","orcid":"https://orcid.org/0000-0003-4263-7221","contributorId":2567,"corporation":false,"usgs":true,"family":"Tilling","given":"Robert","email":"rtilling@usgs.gov","middleInitial":"I.","affiliations":[],"preferred":true,"id":792411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gottfried, David","contributorId":82295,"corporation":false,"usgs":true,"family":"Gottfried","given":"David","email":"","affiliations":[],"preferred":false,"id":792412,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowe, Jack J.","contributorId":117455,"corporation":false,"usgs":true,"family":"Rowe","given":"Jack J.","affiliations":[],"preferred":false,"id":792413,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1001627,"text":"1001627 - 1973 - Analysis of radiotracking data using digitized habitat maps","interactions":[],"lastModifiedDate":"2025-02-24T16:32:54.726748","indexId":"1001627","displayToPublicDate":"1973-07-06T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Analysis of radiotracking data using digitized habitat maps","docAbstract":"A method is described that provides a rapid and accurate analysis of habitat used by radio-equipped animals. The digitizer (basically an X-Y plotter in reverse) converts maps into digital form by describing each habitat unit as a polygon that closely approximates the actual shape of the unit. The coordinates of each polygon are then stored on magnetic tape. Habitat classification data and other information are coded and combined with the proper polygon coordinates. This results in one file containing all habitat data. A computer program with inputs of tracking data and habitat data provides a listing of the habitat used by the animals studied. Analysis of habitat used by radio-equipped ducks is demonstrated using this method.","language":"English","publisher":"Wiley","doi":"10.2307/3800133","usgsCitation":"Gilmer, D., Miller, S., and Cowardin, L., 1973, Analysis of radiotracking data using digitized habitat maps: Journal of Wildlife Management, v. 37, no. 3, p. 404-409, https://doi.org/10.2307/3800133.","productDescription":"6 p.","startPage":"404","endPage":"409","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130529,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"north-central Minnesota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -95.9482547291478,\n 48.36578955797768\n ],\n [\n -95.9482547291478,\n 46.745802177977566\n ],\n [\n -93.07791800075094,\n 46.745802177977566\n ],\n [\n -93.07791800075094,\n 48.36578955797768\n ],\n [\n -95.9482547291478,\n 48.36578955797768\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"37","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db6803fd","contributors":{"authors":[{"text":"Gilmer, D.S.","contributorId":22270,"corporation":false,"usgs":true,"family":"Gilmer","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":311375,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, S.E.","contributorId":31342,"corporation":false,"usgs":true,"family":"Miller","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":311376,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cowardin, L.M.","contributorId":106435,"corporation":false,"usgs":true,"family":"Cowardin","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":311377,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70241807,"text":"70241807 - 1973 - Hydraulics of sheetlike solution cavities","interactions":[],"lastModifiedDate":"2023-03-28T01:22:05.060537","indexId":"70241807","displayToPublicDate":"1973-07-01T20:17:14","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydraulics of sheetlike solution cavities","docAbstract":"The sheetlike solution cavities that supply water to most wells in central Tennessee are 100 to 2,500 feet wide and less than 0.2 inch high. These dimensions have a scale similar to those in Hele-Shaw models. Both logical and mathematical evidence indicate laminar ground-water flow, except close to pumping wells. The Theis nonequilibrium formula may be used to analyze aquifer-test data and to calculate significant values for transmissivity and storage. The Navier-Stokes equation and the Darcy equation for steady-state conditions may be used to estimate cavity dimensions.
","language":"English","publisher":"The Groundwater Association","doi":"10.1111/j.1745-6584.1973.tb02976.x","usgsCitation":"Moore, G.K., 1973, Hydraulics of sheetlike solution cavities: Groundwater, v. 11, no. 4, p. 4-11, https://doi.org/10.1111/j.1745-6584.1973.tb02976.x.","productDescription":"8 p.","startPage":"4","endPage":"11","costCenters":[],"links":[{"id":414793,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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\"}}]}","volume":"11","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Moore, Gerald K.","contributorId":14377,"corporation":false,"usgs":true,"family":"Moore","given":"Gerald","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":867771,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70236457,"text":"70236457 - 1973 - Mapping of the 1973 Mississippi River floods from the Earth Resources Technology Satellite (ERTS)","interactions":[],"lastModifiedDate":"2022-09-07T14:02:16.358177","indexId":"70236457","displayToPublicDate":"1973-06-01T08:51:03","publicationYear":"1973","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Mapping of the 1973 Mississippi River floods from the Earth Resources Technology Satellite (ERTS)","docAbstract":"On March 31, and May 4 and 5, 1973, the first Earth Resources Technology Satellite (ERTS-1) obtained multispectral scanner imagery over the Mississippi River below St. Louis, Missouri. The river was in flood, and the ERTS data provided the first opportunity for regional synoptic mapping of the extent of flooding at the time the imagery was obtained along a 1200 river-mile reach and some of its tributaries. The flood data were compared with imagery collected by ERTS on October 1 and 2, 1972, when the rivers were confined to their normal channels. The specially processed data were analyzed by additive-color techniques, and special enhancements were prepared to aid in interpretation of the data. The extent of flooding was delineated by additive-color, temporal composites of MSS band 7 infrared images. The temporal composites vividly depict, on a single scene, the flooded areas in relation to the normal channel. Color composites of the two near-infrared bands, which usually accentuate surface water, were enlarged to a scale of 1:250,000. Excellent registration was obtained between the image and transparencies of the 1:250,000 topographic maps used as overlays. The resulting image maps were then used as an interim product for preparation of maps showing the extent of flooding at the same scale.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Remote sensing and water resources management","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"American Water Resources Association","usgsCitation":"Deutsch, M., Ruggles, F.H., Guss, P., and Yost, E., 1973, Mapping of the 1973 Mississippi River floods from the Earth Resources Technology Satellite (ERTS), in Remote sensing and water resources management, p. 39-55.","productDescription":"17 p.","startPage":"39","endPage":"55","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":406303,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Illinois, Kentucky, Missouri, Tennessee","otherGeospatial":"Mississippi River-Ohio River confluence","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.06591796875,\n 35.33529320309328\n ],\n [\n -88.65966796875,\n 35.33529320309328\n ],\n [\n -88.65966796875,\n 37.75334401310656\n ],\n [\n -90.06591796875,\n 37.75334401310656\n ],\n [\n -90.06591796875,\n 35.33529320309328\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":851082,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruggles, F. H.","contributorId":105805,"corporation":false,"usgs":true,"family":"Ruggles","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":851083,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guss, Philip","contributorId":296268,"corporation":false,"usgs":false,"family":"Guss","given":"Philip","email":"","affiliations":[],"preferred":false,"id":851084,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yost, Edward","contributorId":296269,"corporation":false,"usgs":false,"family":"Yost","given":"Edward","email":"","affiliations":[],"preferred":false,"id":851085,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":5220562,"text":"5220562 - 1973 - Pen-reared fulvous tree ducks used in movement studies of wild populations","interactions":[],"lastModifiedDate":"2025-02-24T16:41:57.924627","indexId":"5220562","displayToPublicDate":"1973-04-06T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Pen-reared fulvous tree ducks used in movement studies of wild populations","docAbstract":"To obtain movement data on wild fulvous tree ducks (Dendrocygna bicolor) 165 immature pen-reared fulvous tree ducks were color-marked and released in three southeast Texas counties in July October 1969/70. Nine (5 percent) of the marked birds were recovered from 3 days to 9 months after release, and an additional 15 birds provided sight records. Many released birds apparently became integrated into the wild population; all of those observed were with wild flocks. Six birds were recovered over 50 miles from the release sites. Four released in late July to mid-September had moved eastward and two went southward in September or later. Five were still in the Texas-Louisiana rice belt (three in late November). The sixth bird was recovered in October in Veracruz, which supports the assumption that U.S. Gulf Coast nesting populations winter in southern Mexico.
","language":"English","publisher":"Wiley","doi":"10.2307/3798899","usgsCitation":"Flickinger, E.L., King, K.A., and Heyland, O., 1973, Pen-reared fulvous tree ducks used in movement studies of wild populations: Journal of Wildlife Management, v. 37, no. 2, p. 171-175, https://doi.org/10.2307/3798899.","productDescription":"5 p.","startPage":"171","endPage":"175","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193943,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana, Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -98.76367548777017,\n 29.90549728304535\n ],\n [\n -98.76367548777017,\n 26.074023755177024\n ],\n [\n -89.74477546304901,\n 26.074023755177024\n ],\n [\n -89.74477546304901,\n 29.90549728304535\n ],\n [\n -98.76367548777017,\n 29.90549728304535\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"37","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5860","contributors":{"authors":[{"text":"Flickinger, Edward L.","contributorId":48907,"corporation":false,"usgs":true,"family":"Flickinger","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":332019,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Kirk A.","contributorId":9203,"corporation":false,"usgs":true,"family":"King","given":"Kirk","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":332018,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heyland, O.","contributorId":57970,"corporation":false,"usgs":true,"family":"Heyland","given":"O.","email":"","affiliations":[],"preferred":false,"id":332020,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70208891,"text":"70208891 - 1973 - Fluid-inclusion studies of the fluorspar and gold deposits, Jamestown district, Colorado","interactions":[],"lastModifiedDate":"2020-03-04T12:15:28","indexId":"70208891","displayToPublicDate":"1973-03-04T12:03:02","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Fluid-inclusion studies of the fluorspar and gold deposits, Jamestown district, Colorado","docAbstract":"The Jamestown district, Boulder County, Colorado, is a major producer of fluorspar; prior to 1940, gold, gold-telluride, and lead-silver ores were mined. Fluorite occurs as a primary mineral in phases of the composite sodic granite stock at Jamestown and in breccia zones, stockworks, and pipe-shaped bodies in and adjacent to the stock. Gold and telluride mineralization occurs with and without fluorite in veins peripheral to the stock. A great variety of fluid-inclusion types is present in the district, reflecting chemically and physically diverse fluids. Fluid inclusions in early-stage quartz from the fluorspar deposits have filling temperatures of 250 degrees to 375 degrees C, salinities of 20 to 30%, and boiling is indicated at many locations. Most inclusions associated with the main fluorite stage have salinities of at least 26% to more than 50% and filling temperatures in the range of 250 degrees to 350 degrees C. Probable cognate fluorite on the inclusion walls and as many as ten daughter minerals precipitated from some primary inclusions in fluorite attest to the presence of salt and CaF 2 -rich polycomponent fluorspar-depositing fluids. Carbon dioxide-rich liquids and vapors were present during and after the main period of fluorspar deposition.
Gold-bearing veins contain fluid inclusions indicating that two fundamentally different types of fluids were present. Inclusions in pregold quartz and fluorite have filling temperatures which range up to 375 degrees C, and most have very high salinities comparable to those from the fluorspar deposits, suggesting that early quartz and fluorite of the gold-bearing veins was roughly contemporaneous with the main period of fluorspar deposition. Fluid inclusion and other thermometric data (Kelly and Goddard, 1969) suggest that gold and telluride deposition occurred at temperatures below 300 degrees C. Fluid inclusions most directly associated with gold deposition have filling temperatures in the range 205 degrees to 270 degrees C and have about 4% salinity. These data suggest that the gold-bearing fluids either evolved from the fluorite-bearing fluids or were later unrelated hydrothermal pulses introduced on reopened structures.
Boiling occurred at many locations that were at relatively high elevations or adjacent to the sodic granite stock. From the interpretation that boiling occurred and from the heterogeneity of CO 2 contents, we deduce that fluid pressures were low and variable, commonly near 150 bars, but ranging to as much as approximately 500 bars when CO 2 pressures were high; these determinations are compatible with the depth of cover estimated from geomorphic reconstruction using the Flattop peneplain. The absence of strong thermal or salinity zonation of fluids relative to the outcropping stock suggests that fluids were emanating from a larger intrusive body at depth.
","language":"English","publisher":"GeoScienceWorld","doi":"10.2113/gsecongeo.68.8.1247","usgsCitation":"Nash, J.T., and Cunningham, C.G., 1973, Fluid-inclusion studies of the fluorspar and gold deposits, Jamestown district, Colorado: Economic Geology, v. 68, no. 8, p. 1247-1262, https://doi.org/10.2113/gsecongeo.68.8.1247.","productDescription":"16 p.","startPage":"1247","endPage":"1262","costCenters":[],"links":[{"id":372903,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Jamestown district","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.44746398925781,\n 40.06913905733146\n ],\n [\n -105.32936096191406,\n 40.06913905733146\n ],\n [\n -105.32936096191406,\n 40.14948820651523\n ],\n [\n -105.44746398925781,\n 40.14948820651523\n ],\n [\n -105.44746398925781,\n 40.06913905733146\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"68","issue":"8","noUsgsAuthors":false,"publicationDate":"1973-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Nash, J. Thomas","contributorId":26306,"corporation":false,"usgs":true,"family":"Nash","given":"J.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":783850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cunningham, C. G.","contributorId":76741,"corporation":false,"usgs":true,"family":"Cunningham","given":"C.","middleInitial":"G.","affiliations":[],"preferred":false,"id":783851,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70208822,"text":"70208822 - 1973 - Basement ages and basement depths in the eastern equatorial pacific from Deep Sea Drilling Project Legs 5, 8, 9, and 16","interactions":[],"lastModifiedDate":"2020-03-02T13:53:51","indexId":"70208822","displayToPublicDate":"1973-03-02T13:52:39","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Basement Ages and Basement Depths in the Eastern Equatorial Pacific from Deep Sea Drilling Project Legs 5, 8, 9, and 16","title":"Basement ages and basement depths in the eastern equatorial pacific from Deep Sea Drilling Project Legs 5, 8, 9, and 16","docAbstract":"Recent literature contains numerous references to basement ages and basement depths determined by the Deep Sea Drilling Project. The data are derived from a variety of sources, many of them inadequately documented or preliminary, and are not uncommonly inaccurate or conflicting. In this paper we present tabulations of basement ages and depths from DSDP Legs 5, 8, 9, and 16 in the eastern equatorial Pacific, refer them to the latest biostratigraphic time scale, and document and discuss their error limits. We recommend that in future use of this type of data a similar practice be adopted and that the precise source of data, time scale used, and procedures for determining ages and errors be clearly identified in order to avoid confusion. Based on the data presented here, we also give the relations between basement age, distance from the spreading center, and basement depth. The errors inherent in the data cause these relations to be very general and to have less resolution than ascribed to them by some previous investigators.
","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1973)84<2361:BAABDI>2.0.CO;2","usgsCitation":"Van Andel, T.H., and Bukry, D., 1973, Basement ages and basement depths in the eastern equatorial pacific from Deep Sea Drilling Project Legs 5, 8, 9, and 16: GSA Bulletin, v. 84, no. 7, p. 2361-2379, https://doi.org/10.1130/0016-7606(1973)84<2361:BAABDI>2.0.CO;2.","productDescription":"9 p.","startPage":"2361","endPage":"2379","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":372784,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Pacific Ocean","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -125.859375,\n 41.64007838467894\n ],\n [\n -157.32421875,\n 40.3130432088809\n ],\n [\n -156.62109374999997,\n -1.0546279422758742\n ],\n [\n -90.703125,\n 5.266007882805498\n ],\n [\n -95.80078125,\n 23.241346102386135\n ],\n [\n -125.859375,\n 41.64007838467894\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"84","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Van Andel, T. H.","contributorId":68038,"corporation":false,"usgs":true,"family":"Van Andel","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":783496,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bukry, David 0000-0003-4540-890X dbukry@usgs.gov","orcid":"https://orcid.org/0000-0003-4540-890X","contributorId":3550,"corporation":false,"usgs":true,"family":"Bukry","given":"David","email":"dbukry@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":783497,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70200643,"text":"70200643 - 1973 - Stages in the P-T path of ascending basalt magma: an example from San Quintin, Baja California","interactions":[],"lastModifiedDate":"2018-10-25T14:32:33","indexId":"70200643","displayToPublicDate":"1973-03-01T14:31:24","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Stages in the P-T path of ascending basalt magma: an example from San Quintin, Baja California","docAbstract":"Late Pleistocene or Recent lavas from San Quintin, Baja California are basanitoids and alkali basalts. The surface quench temperatures of the lavas average 1 005° C with log
Hydraulic sand models are useful physical tools in the investigation of the transition zone that occurs between salt and fresh ground water in coastal aquifers. Such models are used to demonstrate the effects of transport mechanisms that influence the dynamic behavior and the shape of the transition zone. The techniques employed in obtaining in-place measurements of solute concentrations are generally the stumbling block in generating data for two-dimensional dispersion systems. Two in-place measurement techniques were used in the studies described: (1) conductivity probes when salt was used as a tracer; and (2) photoelectric cells when organic dye was used as a tracer. Results indicate that conductivity methods are more reliable; however, care must be exercised inasmuch as the probes tend to disturb the fluid flow.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Cahill, J., 1973, Hydraulic sand-model studies of miscible-fluid flow: Journal of Research of the U.S. Geological Survey, v. 1, no. 2, p. 243-250.","productDescription":"8 p.","startPage":"243","endPage":"250","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311972,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":311971,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1973/vol1issue2/report.pdf","text":"Report","size":"26.1 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States of America","volume":"1","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"566418c7e4b06a3ea36c7afb","contributors":{"authors":[{"text":"Cahill, J.M.","contributorId":12509,"corporation":false,"usgs":true,"family":"Cahill","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":581421,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70160717,"text":"70160717 - 1973 - Can satellite photography contribute to topographic mapping?","interactions":[],"lastModifiedDate":"2015-12-29T12:43:06","indexId":"70160717","displayToPublicDate":"1973-03-01T02:30:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Can satellite photography contribute to topographic mapping?","docAbstract":"Photographs taken on early space missions, in the Gemini-Apollo series, demonstrated the usefulness of the long view for cartography despite acknowledged shortcomings. Later developments, such as ERTS and Skylab, will provide far more data about Earth, but mostly in planimetric form. The third dimension, height, which makes the map representation topographic, is not easy to measure at orbital altitudes. The capability of current and near-future systems is not likely to do much for topographic mapping at scales larger than 1:250,000, but the benefits in planimetric mapping may be better than even the optimists hoped for.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Doyle, F.J., 1973, Can satellite photography contribute to topographic mapping?: Journal of Research of the U.S. Geological Survey, v. 1, no. 3, p. 315-325.","productDescription":"11 p.","startPage":"315","endPage":"325","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":312993,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":312992,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1973/vol1issue3/report.pdf","text":"Report","size":"23.61 MB","linkFileType":{"id":1,"text":"pdf"}}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5683bcbae4b0a04ef4925e4b","contributors":{"authors":[{"text":"Doyle, Frederick J.","contributorId":46380,"corporation":false,"usgs":true,"family":"Doyle","given":"Frederick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":583674,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70179368,"text":"70179368 - 1973 - Summary of ground-water hydrological data in Michigan for 1971","interactions":[],"lastModifiedDate":"2016-12-29T14:03:28","indexId":"70179368","displayToPublicDate":"1973-03-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Summary of ground-water hydrological data in Michigan for 1971","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70179368","usgsCitation":"Huffman, G., and Thompson, T., 1973, Summary of ground-water hydrological data in Michigan for 1971: Open-File Report, 88 p., https://doi.org/10.3133/70179368.","productDescription":"88 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":332646,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United 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\"}}]}\n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58662f1fe4b0cd2dabe7c4f1","contributors":{"authors":[{"text":"Huffman, G.C.","contributorId":44150,"corporation":false,"usgs":true,"family":"Huffman","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":656942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, T.","contributorId":68362,"corporation":false,"usgs":true,"family":"Thompson","given":"T.","affiliations":[],"preferred":false,"id":656943,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70207210,"text":"70207210 - 1973 - Ground water in perspective","interactions":[],"lastModifiedDate":"2019-12-13T07:40:55","indexId":"70207210","displayToPublicDate":"1973-02-28T09:55:12","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2126,"text":"JAWRA","active":true,"publicationSubtype":{"id":10}},"title":"Ground water in perspective","docAbstract":"Owing to their enormous capacity, ground‐water reservoirs are at least equal in importance to the ground water itself. As regulators of water movement in the hydrological cycle, these reservoirs surpass all lakes combined, natural and manmade. While many aquifers are not well understood, data on many others are adequate for long‐range broad‐scale planning. An example is the basalt aquifer of the Snake River Plain in Idaho. However, the area has managerial problems which concern the time, the place and the feasibility of manipulations of water. All continents of the world contain great aquifers. For every huge aquifer, however, hundreds of smaller ones occur, and even these contain astonishing amounts of water. Aquifers in the Ohio River Basin of the United States are good examples. Management of total water resources is a difficult problem at many places. But many problems could be met and many water shortages alleviated or eliminated by use of aquifers, not merely as sources of water, but as reservoirs for management of water.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1973.tb01707.x","issn":"1093474X","usgsCitation":"Nace, R.L., 1973, Ground water in perspective: JAWRA, v. 9, no. 1, p. 18-24, https://doi.org/10.1111/j.1752-1688.1973.tb01707.x.","productDescription":"7 p.","startPage":"18","endPage":"24","costCenters":[],"links":[{"id":370204,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"Idaho, Wyoming, Montana, Oregon","otherGeospatial":"Snake River Plain ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.26806640625,\n 47.62097541515849\n ],\n [\n -120.08056640625,\n 44.94924926661153\n ],\n [\n -121.1572265625,\n 44.26093725039923\n ],\n [\n -119.61914062499999,\n 43.89789239125797\n ],\n [\n -116.21337890625,\n 43.24520272203356\n ],\n [\n -114.12597656249999,\n 42.97250158602597\n ],\n [\n -111.73095703125,\n 44.11914151643737\n ],\n [\n -111.29150390625,\n 42.5530802889558\n ],\n [\n -109.27001953125,\n 42.08191667830631\n ],\n [\n -108.3251953125,\n 42.69858589169842\n ],\n [\n -107.666015625,\n 43.43696596521823\n ],\n [\n -108.65478515625,\n 44.731125592643274\n ],\n [\n -109.77539062499999,\n 46.14939437647686\n ],\n [\n -110.36865234374999,\n 47.68018294648414\n ],\n [\n -112.19238281249999,\n 48.04870994288686\n ],\n [\n -117.26806640625,\n 47.62097541515849\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"9","issue":"1","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","contributors":{"authors":[{"text":"Nace, R. L.","contributorId":11332,"corporation":false,"usgs":true,"family":"Nace","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":777277,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70214099,"text":"70214099 - 1973 - Annual compilation and analysis of hydrologic data for Pin Oak Creek, Trinity River basin, Texas, 1971","interactions":[],"lastModifiedDate":"2021-11-09T21:57:29.087585","indexId":"70214099","displayToPublicDate":"1973-01-01T16:56:36","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Annual compilation and analysis of hydrologic data for Pin Oak Creek, Trinity River basin, Texas, 1971","docAbstract":"The U.S. Soil Conservation Service is actively engaged in the installation of flood- and soil-erosion reducing measures in Texas under the authority of \"The Flood Control Act of 1936 and 1944\" and \"Watershed Protection and Flood Prevention Act\" (Public Law 566), as amended. The Soil Conservation Service has found a total of approximately 3,500 floodwater-retarding structures to be physically and economically feasible in Texas. As of September 30, 1971, 1,496 of these structures had been built.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70214099","collaboration":"Prepared in cooperation with the Texas Water Development Board","usgsCitation":"Hampton, B., 1973, Annual compilation and analysis of hydrologic data for Pin Oak Creek, Trinity River basin, Texas, 1971: Open-File Report, iii, 18 p., https://doi.org/10.3133/70214099.","productDescription":"iii, 18 p.","numberOfPages":"26","costCenters":[],"links":[{"id":391548,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70214099/report-thumb.jpg"},{"id":391549,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70214099/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Pin Oak Creek","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hampton, B.B.","contributorId":43362,"corporation":false,"usgs":true,"family":"Hampton","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":826491,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047467,"text":"70047467 - 1973 - Lake Okeechobee seepage monitoring network","interactions":[],"lastModifiedDate":"2025-04-10T17:47:21.905845","indexId":"70047467","displayToPublicDate":"1973-01-01T16:11:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"FL 73-018","displayTitle":"Lake Okeechobee Seepage Monitoring Network","title":"Lake Okeechobee seepage monitoring network","docAbstract":"This report summarizes the data collected at the five original monitoring sites along the south shore of Lake Okeechobee from January 29, 1970 to June 28, 1972. In order to use the hydrographs in this report to full advantage, they should be studied in conjunction with Meyer's graphs and text (1971). During steady-state conditions, water seeps from the lake through the filtercake and through the aquifers beneath the dike. At those sites where the filtercake is missing, or has about the same permeability as the aquifers, the seepage from the lake is about equivalent to the flow through the aquifers. Present data are insufficient to determine whether or not filtercake buildup has reduced seepage. No appreciable change in drainage occurred during the observed period.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tallahassee, FL","doi":"10.3133/70047467","usgsCitation":"McKenzie, D.J., 1973, Lake Okeechobee seepage monitoring network: Open-File Report FL 73-018, 64 p., https://doi.org/10.3133/70047467.","productDescription":"64 p.","numberOfPages":"64","costCenters":[],"links":[{"id":277873,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047467/coverthb.jpg"},{"id":276140,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047467/ofr-fl-73018.pdf","text":"Report","size":"14.6 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR FL 73-018"}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.143229,26.624789 ], [ -81.143229,27.207276 ], [ -80.568544,27.207276 ], [ -80.568544,26.624789 ], [ -81.143229,26.624789 ] ] ] } } ] }","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
An inventory of lakes and reservoirs in Oregon has been needed for many years. Records have long been collected throughout the State to assess the quantity and quality of water from streams, but few data have been collected on water stored in Oregon's lakes and reservoirs. Such data are essential for a complete evaluation of the total surface-water supply of the State and to provide a basis for answering questions about Oregon's lakes. Much of the information on lakes and reservoirs previously collected by Federal and State agencies has never been published. These data were compiled and used as a basis for collecting additional information. This report provides information for use by city, county, and State planning groups as well as for sportsmen, tourists, and others interested in preserving the recreational value of Oregon's lakes.
Because of the large number of lakes and reservoirs in Oregon, a single report covering the State would be bulky. Therefore, the best approach seemed to be to publish several volumes on a county or multicounty basis, and Clatsop, Columbia, and Tillamook Counties were selected for the first report. (See fig. 1.)
In addition to office compilation of existing data, most lakes were visited at least once. Visits were made in late summer or early fall when lakes were most accessible and when water temperature and biological activity are at a maximum. Some lakes previously studied by other Federal or State agencies and included in this report were not visited during the study.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70199338","collaboration":"Prepared in cooperation with the Oregon State Engineer","usgsCitation":"Sanderson, R., Shulters, M., and Curtiss, D.A., 1973, Lakes of Oregon, Volume 1: Clatsop, Columbia, and Tillamook Counties: Open-File Report, iii, 95 p., https://doi.org/10.3133/70199338.","productDescription":"iii, 95 p.","costCenters":[],"links":[{"id":357626,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70199338/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":357625,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70199338/report-thumb.jpg"}],"country":"United States","state":"Oregon","county":"Clatsop County, Columbia County, Tillamook County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.0411376953125,\n 45\n ],\n [\n -123,\n 45\n ],\n [\n -123,\n 46.2824277013447\n ],\n [\n -124.0411376953125,\n 46.2824277013447\n ],\n [\n -124.0411376953125,\n 45\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sanderson, R.B.","contributorId":169982,"corporation":false,"usgs":false,"family":"Sanderson","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":746018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shulters, M.V.","contributorId":54583,"corporation":false,"usgs":true,"family":"Shulters","given":"M.V.","email":"","affiliations":[],"preferred":false,"id":746019,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Curtiss, D. A.","contributorId":27862,"corporation":false,"usgs":true,"family":"Curtiss","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":746020,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70241799,"text":"70241799 - 1973 - Value and validity of earth resources observations from space","interactions":[],"lastModifiedDate":"2023-03-27T19:34:22.92267","indexId":"70241799","displayToPublicDate":"1973-01-01T14:29:15","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1926,"text":"Hydrological Sciences Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Value and validity of earth resources observations from space","docAbstract":"Observations of the earth from space can provide overall repetitive views in various regions of the electromagnetic spectrum. Data from such surveys can be used as the basis for more detailed observations from aircraft and on the ground to guide resource exploration, development, and conservation activities.
The value of earth resource observations from space has been demonstrated by the practical use of photographs from the Gemini and Apollo spaceflights and particularly by a series of multispectral photographs taken during the flight of Apollo 9. The analysis of those photographs has shown that the performance of the planned Earth Resources Technology Satellite will meet the needs of the resource and environmental community for small-scale repetitive images of the earth in the visible and solar infrared portions of the spectrum and has provided a limited base of material for earth scientists to work with in order to ready themselves for the ERTS data.
The validity of earth resource observations from space can be derived by analogy from the successively closer observations of the moon, culminating in repeated physical sampling of the moon's surface. The method of inductive reasoning and analysis used for the moon is the opposite of the normal deductive analysis used on the earth. Adoption of the inductive methods and reasoning for earth observations will provide a framework of broad observations and conclusions leading to the identification of target areas for more detailed observation and will, in time, reduce the costs and time required for surveys dealing with resource and environmental problems.
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Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
The purpose of this report is to present daily precipitation (see table A) and continual incremental (5-minute duration) rainfall data through entire storm periods (see table B) at four of the longest first-order National Weather Service station records in Missouri. These basic data can be used in model studies, unit-hydrographic techniques, and other rainfall-intensity studies.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70199681","collaboration":"Prepared in cooperation with U.S. Federal Highway Administration and Missouri State Highway Commission","usgsCitation":"Hauth, L.D., 1973, Selected storm events in 5-minute increments from Missouri rainfall stations at Kansas City, St. Louis, Springfield, and Columbia, Mo., for the period 1892-1970: Open-File Report, 369 p., https://doi.org/10.3133/70199681.","productDescription":"369 p.","costCenters":[],"links":[{"id":400992,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70199681/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":357700,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70199681/report-thumb.jpg"}],"country":"United States","state":"Missouri","city":"Columbia, Kansas City, Springfield, St. Louis","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.625732421875,\n 37.204081555898526\n ],\n [\n -92.46093749999999,\n 37.204081555898526\n ],\n [\n -92.46093749999999,\n 37.309014074275915\n ],\n [\n -92.625732421875,\n 37.309014074275915\n ],\n [\n -92.625732421875,\n 37.204081555898526\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.28515625,\n 38.79904887985135\n ],\n [\n -92.13409423828125,\n 38.79904887985135\n ],\n [\n -92.13409423828125,\n 38.89958342598271\n ],\n [\n -92.28515625,\n 38.89958342598271\n ],\n [\n -92.28515625,\n 38.79904887985135\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.45318603515625,\n 38.72194763292809\n ],\n [\n -90.31036376953125,\n 38.72194763292809\n ],\n [\n -90.31036376953125,\n 38.826870521380634\n ],\n [\n -90.45318603515625,\n 38.826870521380634\n ],\n [\n -90.45318603515625,\n 38.72194763292809\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.63623046875,\n 39.10022600175347\n ],\n [\n -94.5208740234375,\n 39.10022600175347\n ],\n [\n -94.5208740234375,\n 39.20033381963202\n ],\n [\n -94.63623046875,\n 39.20033381963202\n ],\n [\n -94.63623046875,\n 39.10022600175347\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hauth, Leland D.","contributorId":17219,"corporation":false,"usgs":true,"family":"Hauth","given":"Leland","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":746176,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70160680,"text":"70160680 - 1973 - Evaluating the reliability of specific-yield determinations","interactions":[],"lastModifiedDate":"2015-12-28T18:24:44","indexId":"70160680","displayToPublicDate":"1973-01-01T01:15:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Evaluating the reliability of specific-yield determinations","docAbstract":"The specific yield of the alluvial aquifer in the Gila River flood plain in southeastern Arizona has been determined using two methods of analysis - the time-drawdown method and the soil-moisture-content method. Time-drawdown data measured at 17 observation wells during a 3.5-day aquifer test define an average apparent specific yield of 0.13. Soil-moisture-content data measured at nine access holes during the aquifer test indicate that complete gravity drainage had not been attained in the cone of depression by the end of the drawdown period. The moisture-content data were therefore extrapolated with time to define an average specific yield in the range 0.13 to 0.15. The results obtained by the two methods arc in close agreement. However, the significantly lower standard deviation of the results from the moisture-content analysis indicates that extrapolation of the apparent values derived by this method may provide a more reliable estimate of the true specific yield than the apparent values derived by the time-drawdown method. Reliable estimates of specific yield in the zone of seasonal water-level fluctuations are also possible from an evaluation of the soil-moisture change in the spring and summer recession period.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Hanson, R.L., 1973, Evaluating the reliability of specific-yield determinations: Journal of Research of the U.S. Geological Survey, v. 1, no. 3, p. 371-376.","productDescription":"6 p.","startPage":"371","endPage":"376","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":312956,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":312955,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1973/vol1issue3/report.pdf","text":"Report","size":"23.61 MB"}],"country":"United States of America","state":"Arizona","otherGeospatial":"Gila River flood plain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.77239990234375,\n 33.02363335727839\n ],\n [\n -110.73394775390625,\n 33.09269208341614\n ],\n [\n -110.64468383789062,\n 33.15364887320584\n ],\n [\n -110.41259765625,\n 33.244430403478276\n ],\n [\n -110.24642944335938,\n 33.2191589278251\n ],\n [\n -110.115966796875,\n 33.17893926058104\n ],\n [\n -110.03631591796875,\n 33.109948297894285\n ],\n [\n -109.89349365234374,\n 33.02017899916362\n ],\n [\n -109.87289428710938,\n 32.95912969356239\n ],\n [\n -109.918212890625,\n 32.9372338139709\n ],\n [\n -110.04318237304688,\n 33.06622597514673\n ],\n [\n -110.25878906249999,\n 33.17664043594348\n ],\n [\n -110.379638671875,\n 33.19732768648875\n ],\n [\n -110.77239990234375,\n 33.02363335727839\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"1","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56826b3de4b0a04ef4925b2f","contributors":{"authors":[{"text":"Hanson, Ronald L.","contributorId":65054,"corporation":false,"usgs":true,"family":"Hanson","given":"Ronald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":583543,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2000135,"text":"2000135 - 1973 - A preliminary classification of wetland plant communities in north-central Minnesota","interactions":[],"lastModifiedDate":"2017-09-14T10:26:49","indexId":"2000135","displayToPublicDate":"1973-01-01T01:00:00","publicationYear":"1973","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":"168","title":"A preliminary classification of wetland plant communities in north-central Minnesota","docAbstract":"A classification of wetland plant communities was developed for a study area in north-central Minnesota in order to analyze data on waterfowl use of habitat that were gathered by radio telemetry. The classification employs features of several earlier classifications in addition to new classes for bogs and lakeshore communities. Brief descriptions are given for each community, and the important plant species are listed. Discriminant function analysis was used for 40 plant species. Seventy-five percent of the stands studied were classified correctly by this technique. Average probabilities of assignment to communities were calculated and helped to identify distinct and poorly defined communities as well as the relationship among communities.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Cowardin, L., and Johnson, D.H., 1973, A preliminary classification of wetland plant communities in north-central Minnesota: Special Scientific Report - Wildlife 168, 34 p.","productDescription":"34 p.","startPage":"0","endPage":"33","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":112157,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015077581075?urlappend=%3Bseq=3"},{"id":198621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6aad5b","contributors":{"authors":[{"text":"Cowardin, L.M.","contributorId":106435,"corporation":false,"usgs":true,"family":"Cowardin","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":325157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Douglas H. 0000-0002-7778-6641","orcid":"https://orcid.org/0000-0002-7778-6641","contributorId":70327,"corporation":false,"usgs":true,"family":"Johnson","given":"Douglas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":325156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046404,"text":"70046404 - 1973 - Floods in New York, 1971","interactions":[],"lastModifiedDate":"2019-06-11T15:18:47","indexId":"70046404","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Floods in New York, 1971","docAbstract":"This report, for the calendar year 1971, was prepared at the request of the New York State Department of Transportation under provisions of an agreement between the New York State Department of Environmental Conservation and the U.S. Geological Survey fore a cooperative statewide program investigate the water resources of the State. The report was complied in the New York, Water Resources Division, U.S. Geological Survey, under the direction of Robert J. Dingman, District Chief. The information was obtained from newspaper clippings, publications of the National Weather Service, and the Environmental Data Service, and the Environmental Data Service of the National Oceanic and Atmospheric Administration (\"Climatological Data\" and \"Storm Data\"), and records of the U.S. Geological Survey.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Albany, NY","doi":"10.3133/70046404","collaboration":"Prepared in cooperation with the New York State Department of Transportation and New York State Department of Environmental Conservation","usgsCitation":"Robison, F.L., 1973, Floods in New York, 1971: Open-File Report, iii, 33 p., https://doi.org/10.3133/70046404.","productDescription":"iii, 33 p.","numberOfPages":"40","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":273607,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274607,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70046404/report.pdf"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.765000,40.494444 ], [ -79.765000,45.011667 ], [ -71.790278,45.011667 ], [ -71.790278,40.494444 ], [ -79.765000,40.494444 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b846e6e4b03203c522b1cf","contributors":{"authors":[{"text":"Robison, F. Luman","contributorId":103264,"corporation":false,"usgs":true,"family":"Robison","given":"F.","email":"","middleInitial":"Luman","affiliations":[],"preferred":false,"id":479621,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}