This map of the Yakataga district is one of five maps at the same scale, showing the geology of the Gulf of Alaska Tertiary province (see index map). In this province, an accurate belt more than 300 miles long and 2 to 40 miles wide, sedimentary rocks of Tertiary age are exposed or inferred to underlie lowland areas covered by Quaternary unconsolidated deposits or ice (Miller, Payne, Gryc, 1959, p. 37-47). Field studies were carried out in the province intermittently from 1944 to 1960, under the Geological Survey's program of petroleum investigations in southern Alaska.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr61102","usgsCitation":"Miller, D.J., 1961, Geology of the Yakataga district, Gulf of Alaska Tertiary province, Alaska: U.S. Geological Survey Open-File Report 61-102, 2 Plates: 55.98 x 39.23 inches and 26.20 x 35.73 inches, https://doi.org/10.3133/ofr61102.","productDescription":"2 Plates: 55.98 x 39.23 inches and 26.20 x 35.73 inches","costCenters":[],"links":[{"id":134941,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0102/report-thumb.jpg"},{"id":414362,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0102/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414361,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0102/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"96000","country":"United States","state":"Alaska","otherGeospatial":"Gulf of Alaska Tertiary province, Yakataga district","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -143.5,60 ], [ -143.5,60.5 ], [ -141.5,60.5 ], [ -141.5,60 ], [ -143.5,60 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c912","contributors":{"authors":[{"text":"Miller, Don John","contributorId":77120,"corporation":false,"usgs":true,"family":"Miller","given":"Don","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":228063,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43363,"text":"ofr6199 - 1961 - Geology of the Katalla district, Gulf of Alaska Tertiary province, Alaska","interactions":[],"lastModifiedDate":"2022-04-05T20:20:50.001887","indexId":"ofr6199","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-99","title":"Geology of the Katalla district, Gulf of Alaska Tertiary province, Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6199","usgsCitation":"Miller, D.J., 1961, Geology of the Katalla district, Gulf of Alaska Tertiary province, Alaska: U.S. Geological Survey Open-File Report 61-99, 2 Plates: 28.90 × 41.88 inches and 28.78 × 35.96 inches, https://doi.org/10.3133/ofr6199.","productDescription":"2 Plates: 28.90 × 41.88 inches and 28.78 × 35.96 inches","costCenters":[],"links":[{"id":398149,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8013.htm"},{"id":81095,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0099/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81094,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0099/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"96000","country":"United States","state":"Alaska","otherGeospatial":"Katalla district","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -144.75,\n 59.783\n ],\n [\n -143.583,\n 59.783\n ],\n [\n -143.583,\n 60.586\n ],\n [\n -144.75,\n 60.586\n ],\n [\n -144.75,\n 59.783\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fb54","contributors":{"authors":[{"text":"Miller, Don John","contributorId":77120,"corporation":false,"usgs":true,"family":"Miller","given":"Don","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":228096,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68987,"text":"om209 - 1961 - Preliminary structure contour map on top of salt in the Paradox member of the Hermosa Formation in the salt anticline region, Colorado and Utah","interactions":[],"lastModifiedDate":"2021-12-29T13:53:26.271353","indexId":"om209","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":329,"text":"Oil and Gas Investigation Map","code":"OM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"209","title":"Preliminary structure contour map on top of salt in the Paradox member of the Hermosa Formation in the salt anticline region, Colorado and Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/om209","usgsCitation":"Elston, D.P., and Shoemaker, E.M., 1961, Preliminary structure contour map on top of salt in the Paradox member of the Hermosa Formation in the salt anticline region, Colorado and Utah: U.S. Geological Survey Oil and Gas Investigation Map 209, HTML Document, https://doi.org/10.3133/om209.","productDescription":"HTML Document","costCenters":[],"links":[{"id":187520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":104991,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5363.htm","linkFileType":{"id":5,"text":"html"},"description":"5363"}],"scale":"250000","country":"United States","state":"Colorado, Utah","otherGeospatial":"Paradox Member of the Hermosa Formation","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.88525390624999,\n 37.77071473849609\n ],\n [\n -107.93792724609375,\n 37.77071473849609\n ],\n [\n -107.93792724609375,\n 39.027718840211605\n ],\n [\n -109.88525390624999,\n 39.027718840211605\n ],\n [\n -109.88525390624999,\n 37.77071473849609\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aace4b07f02db66a544","contributors":{"authors":[{"text":"Elston, D. P.","contributorId":96334,"corporation":false,"usgs":true,"family":"Elston","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":279336,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":279335,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3468,"text":"cir437 - 1961 - Progress in the application of landform analysis in studies of semiarid erosion","interactions":[],"lastModifiedDate":"2018-01-02T20:09:48","indexId":"cir437","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"437","title":"Progress in the application of landform analysis in studies of semiarid erosion","docAbstract":"The analysis of topographic and hydrologic data gathered during studies of erosion in semiarid areas of Western United States show the following relation: (a) Mean annual sediment yield from small drainage basins is related to a ratio of basin relief to length; (b) mean annual runoff from small drainage basins is related to drainage density; (c) mean annual sediment yield per unit area decreases with increase in drainage area; (d) the form of some convex hill slopes is related to surficial creep; (e) asymmetry of drainage basins, including differences in hill-slope erosion and drainage density, is related to microclimatic variations on slopes of diverse exposure; .(f) the cutting of discontinuous gullies is closely related to steepening by deposition of the semiarid valley floor; (g) aggradation in ephemeral streams seems to be most prevalent in reaches where the ratio of contributing drainage area to channel length is relatively small; and (h) streamchannel shape, expressed as a width-depth ratio, is related to the percentage of silt-clay in bed and bank alluvium. The above relations cannot be detected without measurement of terrain characteristics. They further indicate the importance of quantitative terrain analysis in studies of erosion.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir437","usgsCitation":"Schumm, S.A., and Hadley, R.F., 1961, Progress in the application of landform analysis in studies of semiarid erosion: U.S. Geological Survey Circular 437, iii, 14 p. :diagrs., profile. ;27cm., https://doi.org/10.3133/cir437.","productDescription":"iii, 14 p. :diagrs., profile. ;27cm.","costCenters":[],"links":[{"id":30480,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0437/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118117,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0437/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649cc5","contributors":{"authors":[{"text":"Schumm, Stanley Alfred","contributorId":101652,"corporation":false,"usgs":true,"family":"Schumm","given":"Stanley","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":146984,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":146983,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3352,"text":"cir447 - 1961 - Selected sources of information on U.S. and world energy resources: An annotated bibliography","interactions":[],"lastModifiedDate":"2018-01-02T20:28:38","indexId":"cir447","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"447","title":"Selected sources of information on U.S. and world energy resources: An annotated bibliography","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir447","usgsCitation":"Trumbull, J., 1961, Selected sources of information on U.S. and world energy resources: An annotated bibliography: U.S. Geological Survey Circular 447, 8 p. ;27cm., https://doi.org/10.3133/cir447.","productDescription":"8 p. ;27cm.","costCenters":[],"links":[{"id":118206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0447/report-thumb.jpg"},{"id":30362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0447/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f8230","contributors":{"authors":[{"text":"Trumbull, James","contributorId":92233,"corporation":false,"usgs":true,"family":"Trumbull","given":"James","affiliations":[],"preferred":false,"id":146706,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23879,"text":"ofr6196 - 1961 - Water levels in observation wells in Santa Barbara County, California, in 1960","interactions":[{"subject":{"id":23879,"text":"ofr6196 - 1961 - Water levels in observation wells in Santa Barbara County, California, in 1960","indexId":"ofr6196","publicationYear":"1961","noYear":false,"title":"Water levels in observation wells in Santa Barbara County, California, in 1960"},"predicate":"SUPERSEDED_BY","object":{"id":95,"text":"wsp1770 - 1963 - Ground-water levels in the United States, 1956-60, southwestern states","indexId":"wsp1770","publicationYear":"1963","noYear":false,"title":"Ground-water levels in the United States, 1956-60, southwestern states"},"id":1}],"supersededBy":{"id":95,"text":"wsp1770 - 1963 - Ground-water levels in the United States, 1956-60, southwestern states","indexId":"wsp1770","publicationYear":"1963","noYear":false,"title":"Ground-water levels in the United States, 1956-60, southwestern states"},"lastModifiedDate":"2024-07-30T13:51:40.155402","indexId":"ofr6196","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-96","title":"Water levels in observation wells in Santa Barbara County, California, in 1960","docAbstract":"Investigation of the ground-water resources of Santa Barbara County was continued during 1960 by the U. S. Geological Survey in cooperation with the Santa Barbara County Water Agency. Monthly water-level measurements were made in 193 wells, in 9 of which automatic water-level recorders were operated. Earlier measurements, covering the period 1941 through 1955, have been published in Geological Survey Water-Supply Papers; those for 1956, 1957, 1958, and 1959 have been released locally in duplicated form. Water-Supply Paper 1068 contains tabulated descriptions of 2,246 wells in existence in 1942 in the several ground-water basins of the county. The same publication also contains many water-level measurements made prior to 1942 by the city of Santa Barbara, Santa Maria Valley Voter Conservation District, San Joaquin Power Division of the Pacific Gas and Electric Co., Union Sugar Co., Union Oil Co., and other organizations and individuals.
Comprehensive reports on the geology and ground-water resources of the Santa Ynez River basin (Upson and Thomasson, 1951, and Wilson, 1959), the south-coast basins (Upson, 1951), the Santa Maria Valley area (Worts, 1951), and the Cuyama Valley (Upson and Worts, 1951) have been published as Water-Supply Papers 1107, 1467, 1108, 1000, and 1110-B, respectively. A similar report on the San Antonio Creek Valley is in preparation. A report on stream runoff and ground-water storage capacity of the Santa Ynez River valley (Troxell and Wilson, 1952) was released to the open file on October 1952.
In addition to the water-level measurements made by the Geological Survey in 1960, measurements made by the Santa Maria Valley Water Conservation District are included in this report. Not, included in this report are miscellaneous measurements made by the Geological Survey in wells along the middle reach of the Santa Ynez River between Cachuma Dam and Rucker Crossing.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6196","issn":"0094-9140","collaboration":"Prepared in cooperation with the Santa Barba County Water Agency","usgsCitation":"Merritt, P., 1961, Water levels in observation wells in Santa Barbara County, California, in 1960: U.S. Geological Survey Open-File Report 61-96, 51 p., https://doi.org/10.3133/ofr6196.","productDescription":"51 p.","costCenters":[],"links":[{"id":156526,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0096/report-thumb.jpg"},{"id":431612,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1961/0096/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Santa Barabara County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.61474653419313,\n 35.107477322182945\n ],\n [\n -120.61474653419313,\n 33.603227658961316\n ],\n [\n -119.21258359397822,\n 33.603227658961316\n ],\n [\n -119.21258359397822,\n 35.107477322182945\n ],\n [\n -120.61474653419313,\n 35.107477322182945\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9d5f","contributors":{"authors":[{"text":"Merritt, P.M.","contributorId":45344,"corporation":false,"usgs":true,"family":"Merritt","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":190901,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3411,"text":"cir439 - 1961 - Time of travel of water in the Ohio River, Pittsburgh to Cincinnati","interactions":[],"lastModifiedDate":"2017-06-09T08:32:55","indexId":"cir439","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"439","title":"Time of travel of water in the Ohio River, Pittsburgh to Cincinnati","docAbstract":"This report presents a procedure for estimating the time of travel of water in the Ohio River from Pittsburgh, Pa., to Cincinnati, Ohio, under various river stage conditions. This information is primarily for use by civil defense officials and by others concerned with problems involving travel time of river water. \r\n\r\nTables and charts are presented to show, for a particular stage or discharge at Cincinnati, the average time it would take for water to travel through the entire reach from Pittsburgh, or through successive intermediate segments of the reach. For example, when the discharge at Cincinnati is 200,000 cfs, travel time from Pittsburgh to Cincinnati, a distance of 470 miles, averages about 7 days; and for discharges of more than 200,000 cfs, the travel time decreases very slowly with increasing discharge. When the discharge is 30,000 cfs, travel time is about 28 days; and for discharges of less than 30,000 cfs, the travel time increases very rapidly with decreasing discharge. Estimates of travel time at low discharge are subject to large errors. Statistical analysis of the possible variations of upstream discharge for a given discharge at Cincinnati indicates that the shortest probable travel time from Pittsburgh to Cincinnati ranges from 56 percent of that under average conditions when the discharge at Cincinnati is 15,000 cfs to 93 percent of that under average conditions when the discharge at Cincinnati is 894,000 cfs. \r\n\r\nA chart showing the time distribution of flow at Cincinnati is presented so that the probable travel time of Ohio River water can be determined for any time of the year. This chart provides information which, when applied to the time-of-travel chart, shows that the most probable travel time of water from Pittsburgh to Cincinnati ranges from 160 hours in February to 1,250 hours in September. Also presented is a flow-duration curve that can be used to predict future discharges and, subsequently, times of travel, for use in long-range planning. The procedure used to compute time of travel is described in sufficient detail to make it usable as a guide for similar studies of other rivers that have deans and pools in the reach being studied. \r\n\r\nThe computations for the time-of-travel charts were made as follows: (a) by dividing the reach between Pittsburgh and Cincinnati into four subreaches with a full-range streamgaging station at or near the ends of each; (b) by computing for each subreach mean velocities corresponding to various discharges at Cincinnati, using data obtained from river survey maps and data available from gaging station operations; (c) by assuming that any mass of contaminated water would travel at a rate equal to that of the mean velocity of the river water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir439","usgsCitation":"Steacy, R.E., 1961, Time of travel of water in the Ohio River, Pittsburgh to Cincinnati: U.S. Geological Survey Circular 439, iii, 14 p. :map, diagrs., tables. ;27cm., https://doi.org/10.3133/cir439.","productDescription":"iii, 14 p. :map, diagrs., tables. ;27cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":30428,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0439/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0439/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Ohio River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.957275390625,\n 38.272688535980976\n ],\n [\n -79.8046875,\n 38.272688535980976\n ],\n [\n -79.8046875,\n 40.73893324113601\n ],\n [\n -84.957275390625,\n 40.73893324113601\n ],\n [\n -84.957275390625,\n 38.272688535980976\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b6e4b07f02db533c35","contributors":{"authors":[{"text":"Steacy, Robert E.","contributorId":71162,"corporation":false,"usgs":true,"family":"Steacy","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146848,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4057,"text":"cir442 - 1961 - Ground-water resources--Development and management","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"cir442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"442","title":"Ground-water resources--Development and management","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir442","usgsCitation":"Conover, C.S., 1961, Ground-water resources--Development and management: U.S. Geological Survey Circular 442, 7 p. ;27 cm., https://doi.org/10.3133/cir442.","productDescription":"7 p. ;27 cm.","costCenters":[],"links":[{"id":117098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0442/report-thumb.jpg"},{"id":31151,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0442/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a3ab","contributors":{"authors":[{"text":"Conover, Clyde Stuart","contributorId":42197,"corporation":false,"usgs":true,"family":"Conover","given":"Clyde","email":"","middleInitial":"Stuart","affiliations":[],"preferred":false,"id":148086,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43371,"text":"ofr61167 - 1961 - Geology of the Poverty Bay quadrangle, Washington","interactions":[{"subject":{"id":43371,"text":"ofr61167 - 1961 - Geology of the Poverty Bay quadrangle, Washington","indexId":"ofr61167","publicationYear":"1961","noYear":false,"title":"Geology of the Poverty Bay quadrangle, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":61899,"text":"gq158 - 1961 - Geology of the Poverty Bay quadrangle, Washington","indexId":"gq158","publicationYear":"1961","noYear":false,"title":"Geology of the Poverty Bay quadrangle, Washington"},"id":1}],"supersededBy":{"id":61899,"text":"gq158 - 1961 - Geology of the Poverty Bay quadrangle, Washington","indexId":"gq158","publicationYear":"1961","noYear":false,"title":"Geology of the Poverty Bay quadrangle, Washington"},"lastModifiedDate":"2019-06-21T15:29:14","indexId":"ofr61167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-167","title":"Geology of the Poverty Bay quadrangle, Washington","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr61167","usgsCitation":"Waldron, H.H., 1961, Geology of the Poverty Bay quadrangle, Washington: U.S. Geological Survey Open-File Report 61-167, 2 Plates: 22.79 x 31.08 inches and 23.22 x 24.61 inches, https://doi.org/10.3133/ofr61167.","productDescription":"2 Plates: 22.79 x 31.08 inches and 23.22 x 24.61 inches","costCenters":[],"links":[{"id":364926,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0167/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364927,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0167/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161903,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0167/report-thumb.jpg"}],"country":"United States","state":"Washington","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e818","contributors":{"authors":[{"text":"Waldron, Howard Hamilton","contributorId":21927,"corporation":false,"usgs":true,"family":"Waldron","given":"Howard","email":"","middleInitial":"Hamilton","affiliations":[],"preferred":false,"id":228106,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39780,"text":"pp387A - 1961 - Botanical Evidence of the Modern History of Nisqually Glacier, Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"pp387A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"387","chapter":"A","title":"Botanical Evidence of the Modern History of Nisqually Glacier, Washington","docAbstract":"A knowledge of the areas once occupied by mountain glaciers reveals at least part of the past behavior of these glaciers. From this behavior, inferences of past climate can be drawn. The maximum advance of Nisqually Glacier in the last thousand years was located, and retreat from this point is believed to have started about 1840. The maximum downvalley position of the glacier is marked by either a prominent moraine or by a line of difference between stands of trees of strikingly different size and significantly different age. The thousand-year age of the forest beyond the moraine or line between abutting stands represents the minimum time since the surface was glaciated. This age is based on the age of the oldest trees, plus an estimated interval required for the formation of humus, plus evidence of an ancient fire, plus an interval of deposition of pyroclastics. The estimate of the date when Nisqually Glacier began to retreat from its maximum advance is based upon the ages of the oldest trees plus an interval of 5 years estimated as the time required for the establishment of trees on stable moraines. This interval was derived from a study of the ages of trees growing at locations of known past positions of the glacier.\r\n\r\nReconnaissance studies were made on moraines formed by Emmons and Tahoma Glaciers. Preliminary analyses of these data suggest that Emmons Glacier started to recede from its maximum advance in about 1745. Two other upvalley moraines mark positions from which recession started about 1849 and 1896. Ages of trees near Tahoma Glacier indicate that it started to recede from its position of maximum advance in about 1635. About 1835 Tahoma Glacier started to recede again from another moraine formed by a readvance that ter minated near the 1635 position.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp387A","usgsCitation":"Sigafoos, R.S., and Hendricks, E.L., 1961, Botanical Evidence of the Modern History of Nisqually Glacier, Washington: U.S. Geological Survey Professional Paper 387, p. A1-A20, https://doi.org/10.3133/pp387A.","productDescription":"p. A1-A20","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":124576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0387a/report-thumb.jpg"},{"id":12475,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/pp/387-a/index.htm","linkFileType":{"id":5,"text":"html"}},{"id":67649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0387a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122,46.666666666666664 ], [ -122,47 ], [ -121.25,47 ], [ -121.25,46.666666666666664 ], [ -122,46.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7276","contributors":{"authors":[{"text":"Sigafoos, Robert S.","contributorId":82379,"corporation":false,"usgs":true,"family":"Sigafoos","given":"Robert","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":222150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":222149,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":41102,"text":"ofr61168 - 1961 - Preliminary geologic map of Seattle and vicinity, Washington","interactions":[{"subject":{"id":41102,"text":"ofr61168 - 1961 - Preliminary geologic map of Seattle and vicinity, Washington","indexId":"ofr61168","publicationYear":"1961","noYear":false,"title":"Preliminary geologic map of Seattle and vicinity, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":64584,"text":"i354 - 1962 - Preliminary geologic map of Seattle and vicinity, Washington","indexId":"i354","publicationYear":"1962","noYear":false,"title":"Preliminary geologic map of Seattle and vicinity, Washington"},"id":1}],"supersededBy":{"id":64584,"text":"i354 - 1962 - Preliminary geologic map of Seattle and vicinity, Washington","indexId":"i354","publicationYear":"1962","noYear":false,"title":"Preliminary geologic map of Seattle and vicinity, Washington"},"lastModifiedDate":"2019-06-21T15:38:28","indexId":"ofr61168","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-168","title":"Preliminary geologic map of Seattle and vicinity, Washington","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr61168","usgsCitation":"Waldron, H.H., 1961, Preliminary geologic map of Seattle and vicinity, Washington: U.S. Geological Survey Open-File Report 61-168, 3 Plates: 41.00 x 35.31 inches or smaller, https://doi.org/10.3133/ofr61168.","productDescription":"3 Plates: 41.00 x 35.31 inches or smaller","costCenters":[],"links":[{"id":364933,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0168/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0168/report-thumb.jpg"},{"id":364934,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0168/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364935,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0168/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","city":"Seattle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.56347656249999,\n 47.45780853075031\n ],\n [\n -121.9482421875,\n 47.45780853075031\n ],\n [\n -121.9482421875,\n 47.724544549099676\n ],\n [\n -122.56347656249999,\n 47.724544549099676\n ],\n [\n -122.56347656249999,\n 47.45780853075031\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf7c","contributors":{"authors":[{"text":"Waldron, Howard Hamilton","contributorId":21927,"corporation":false,"usgs":true,"family":"Waldron","given":"Howard","email":"","middleInitial":"Hamilton","affiliations":[],"preferred":false,"id":224499,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2401,"text":"wsp1619A - 1961 - Hydrogeology of a spring in a glacial terrane near Ashland, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1619A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1619","chapter":"A","title":"Hydrogeology of a spring in a glacial terrane near Ashland, Ohio","language":"ENGLISH","publisher":"U.S. GPO,","doi":"10.3133/wsp1619A","usgsCitation":"Norris, S.E., 1961, Hydrogeology of a spring in a glacial terrane near Ashland, Ohio: U.S. Geological Survey Water Supply Paper 1619, 17 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1619A.","productDescription":"17 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":139034,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619a/report-thumb.jpg"},{"id":28390,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db685160","contributors":{"authors":[{"text":"Norris, Stanley Eugene","contributorId":24772,"corporation":false,"usgs":true,"family":"Norris","given":"Stanley","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":145140,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":958,"text":"wsp1608A - 1961 - Effects of phosphate mining on the ground water of Anguar, Palau Islands, Trust Territory of the Pacific Islands","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1608A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1608","chapter":"A","title":"Effects of phosphate mining on the ground water of Anguar, Palau Islands, Trust Territory of the Pacific Islands","docAbstract":"Mining of phosphate ore on Angaur Island by mechanized methods created large water-table lakes, which became filled with brackish or saline water. A hydrologic investigation was started in 1949 to determine whether the saline water in the lakes would spread to surrounding areas and cause damage to agricultural lands and the water supply. \r\n\r\nAngaur, which is in the Palau Islands in the southwestern part of Micronesia, is administered as part of the Trust Territory of the Pacific Islands, under a trusteeship granted to the United States by the United Nations. The island has an area of 3.2 square miles and has a maximum altitude of about 150 feet. The climate is tropical oceanic. The average annual temperature is 82 ? F; the average annual rainfall is about 125 inches; and the average relative humidity is about 80 percent. \r\n\r\nThe northwestern third of Angaur (province A) consists topographically of a series of concentric ridges and depressions which are underlain largely by well-cemented coralline limestone of Pliocene, Pleistocene, and Recent ages. The remaining two-thirds of Angaur (province B} is a low plain underlain in the northern and central parts by a low platform of coralline rubble of Pleistocene and Recent age and in the southern part by sandy and rubbly beach deposits of Recent age. Province A contained extensive phosphate deposits of which more than 3 million tons were mined in 1909-55. \r\n\r\nWeekly water-level measurements at 35 wells, test holes, and lakes indicate that the water table averages about 2 feet above mean sea level in the beach deposits, about half a foot above mean sea level in the rubble deposits, and about 1.35 feet above mean sea level in the coralline limestone. Water samples obtained weekly at the observation sites indicate that the ground water in province A is not of uniform quality, as large variations in salinity occur throughout the area. In contrast, the ground water in province B is of relatively uniform quality, and contains less than 1,000 ppm (parts per million) of chloride in most places. \r\n\r\nIn province A removal of earthy phosphate which had acted as a seal allowed the infiltration of saline water through solution channels exposed at the bottom of several of the lakes. The sampling program showed no indication of large-scale movement of saline water out of the lakes into adjacent ground water. Provinces A and B apparently function as independent ground-water units, and the quality of the ground water in province B has not been noticeably affected by mining activities in province A. \r\n\r\nThe lakes were backfilled with limestone rubble to reduce the possibility of underground movement of saline water out of the lakes. The gross permeability of the backfill material is less than that of the surrounding limestone in province A, and, as the rate of influx of saline water was curtailed, the recharge of fresh water from rainfall tended to reduce the salinity of the ground water in the fill. In parts of the backfilled area the salinity of the water at the water table decreased rapidly in less than 1 year, as a layer of fresh water was built up at the water table.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1608A","usgsCitation":"Arnow, T., 1961, Effects of phosphate mining on the ground water of Anguar, Palau Islands, Trust Territory of the Pacific Islands: U.S. Geological Survey Water Supply Paper 1608, iv, 39 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1608A.","productDescription":"iv, 39 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608a/report-thumb.jpg"},{"id":25481,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611a74","contributors":{"authors":[{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":142917,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35687,"text":"b1081F - 1961 - Geology of the southern part of the Lemhi Range, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:09:35","indexId":"b1081F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1081","chapter":"F","title":"Geology of the southern part of the Lemhi Range, Idaho","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1081F","usgsCitation":"Ross, C.P., 1961, Geology of the southern part of the Lemhi Range, Idaho: U.S. Geological Survey Bulletin 1081, p.189-260, ill., map (1 fold. col.in pocket) ;24 cm., https://doi.org/10.3133/b1081F.","productDescription":"p.189-260, ill., map (1 fold. col.in pocket) ;24 cm.","costCenters":[],"links":[{"id":109301,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20743.htm","linkFileType":{"id":5,"text":"html"},"description":"20743"},{"id":166555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1081f/report-thumb.jpg"},{"id":63587,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1081f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63588,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1081f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c797","contributors":{"authors":[{"text":"Ross, Clyde Palhemus","contributorId":12324,"corporation":false,"usgs":true,"family":"Ross","given":"Clyde","email":"","middleInitial":"Palhemus","affiliations":[],"preferred":false,"id":215058,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40579,"text":"ofr61138 - 1961 - Claim map, Egnar quadrangle, San Miguel County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:11:10","indexId":"ofr61138","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-138","title":"Claim map, Egnar quadrangle, San Miguel County, Colorado","language":"ENGLISH","doi":"10.3133/ofr61138","usgsCitation":"Sample, R.D., and Albee, H., 1961, Claim map, Egnar quadrangle, San Miguel County, Colorado: U.S. Geological Survey Open-File Report 61-138, 1 map., https://doi.org/10.3133/ofr61138.","productDescription":"1 map.","costCenters":[],"links":[{"id":176400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0138/report-thumb.jpg"},{"id":76819,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0138/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76820,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1961/0138/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e0573","contributors":{"authors":[{"text":"Sample, Raymond Dewey","contributorId":50587,"corporation":false,"usgs":true,"family":"Sample","given":"Raymond","email":"","middleInitial":"Dewey","affiliations":[],"preferred":false,"id":223561,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Albee, Howard F.","contributorId":64252,"corporation":false,"usgs":true,"family":"Albee","given":"Howard F.","affiliations":[],"preferred":false,"id":223562,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":40581,"text":"ofr61140 - 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1961 - Filter-press method of extracting water samples for chloride analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1544A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1544","chapter":"A","title":"Filter-press method of extracting water samples for chloride analysis","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1544A","usgsCitation":"Lusczynski, N.J., 1961, Filter-press method of extracting water samples for chloride analysis: U.S. Geological Survey Water Supply Paper 1544, v. :ill. ;23 cm. ;8 p., https://doi.org/10.3133/wsp1544A.","productDescription":"v. :ill. ;23 cm. ;8 p.","costCenters":[],"links":[{"id":138113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1544a/report-thumb.jpg"},{"id":30181,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1544a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f483d","contributors":{"authors":[{"text":"Lusczynski, Norbert J.","contributorId":93465,"corporation":false,"usgs":true,"family":"Lusczynski","given":"Norbert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":146416,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43407,"text":"ofr61166 - 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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr61166","usgsCitation":"Waldron, H.H., 1961, Geology of the Des Moines quadrangle, Washington: U.S. Geological Survey Open-File Report 61-166, 2 Plates: 23.62 x 34.51 and 18.06 x 34.89 inches, https://doi.org/10.3133/ofr61166.","productDescription":"2 Plates: 23.62 x 34.51 and 18.06 x 34.89 inches","costCenters":[],"links":[{"id":135028,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0166/report-thumb.jpg"},{"id":365168,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0166/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365167,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0166/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":496169,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7996.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","otherGeospatial":"Des Moines quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.25,\n 47.5\n ],\n [\n -122.375,\n 47.5\n ],\n [\n -122.375,\n 47.375\n ],\n [\n -122.25,\n 47.375\n ],\n [\n -122.25,\n 47.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f55","contributors":{"authors":[{"text":"Waldron, Howard Hamilton","contributorId":21927,"corporation":false,"usgs":true,"family":"Waldron","given":"Howard","email":"","middleInitial":"Hamilton","affiliations":[],"preferred":false,"id":228169,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52265,"text":"ofr6299 - 1961 - Floods in Arkansas, magnitude and frequency","interactions":[{"subject":{"id":52265,"text":"ofr6299 - 1961 - Floods in Arkansas, magnitude and frequency","indexId":"ofr6299","publicationYear":"1961","noYear":false,"title":"Floods in Arkansas, magnitude and frequency"},"predicate":"SUPERSEDED_BY","object":{"id":70047418,"text":"70047418 - 1971 - Floods in Arkansas, magnitude and frequency characteristics through 1968","indexId":"70047418","publicationYear":"1971","noYear":false,"title":"Floods in Arkansas, magnitude and frequency characteristics through 1968"},"id":1}],"supersededBy":{"id":70047418,"text":"70047418 - 1971 - Floods in Arkansas, magnitude and frequency characteristics through 1968","indexId":"70047418","publicationYear":"1971","noYear":false,"title":"Floods in Arkansas, magnitude and frequency characteristics through 1968"},"lastModifiedDate":"2017-03-09T12:38:22","indexId":"ofr6299","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"62-99","title":"Floods in Arkansas, magnitude and frequency","docAbstract":"This report presents methods by which the magnitude and frequency of expected floods for most streams in Arkansas may be determined. Flood data have been used to define flood-frequency curves applicable to the State.
Composite frequency curves have been defined showing the relation of the mean annual flood to floods having recurrence intervals of 1. 2 to 50 years. Other curves express the relation of the mean annual flood to drainage basin characteristics. For the northern part of the State, it was found that the slope of the composite frequency curve varies with drainage area size, and an adjustment curve was drawn for use in conjunction with the composite curve for this area.
By combining data from the composite and mean annual flood curves a flood-frequency curve may be drawn for any stream in Arkansas, not materially affected by works of man, within the limits of drainage area and recurrence interval defined by base data.
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