{"pageNumber":"2466","pageRowStart":"61625","pageSize":"25","recordCount":68802,"records":[{"id":70039539,"text":"70039539 - 1970 - Serial publications commonly cited in technical bibliographies of the United States Geological Survey","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039539","displayToPublicDate":"2012-01-01T10:46:05","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Serial publications commonly cited in technical bibliographies of the United States Geological Survey","docAbstract":"A list of serial publications commonly cited by USGS technical bibliographies.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039539","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Serial publications commonly cited in technical bibliographies of the United States Geological Survey, 100 p., https://doi.org/10.3133/70039539.","productDescription":"100 p.","numberOfPages":"102","costCenters":[],"links":[{"id":261664,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039539/report.pdf"},{"id":261665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039539/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8d58e4b08c986b31835a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70046327,"text":"wdrNM691 - 1970 - Water resources data for New Mexico, water year 1969; Part 1. Surface water records","interactions":[],"lastModifiedDate":"2013-07-08T10:53:36","indexId":"wdrNM691","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NM-69-1","title":"Water resources data for New Mexico, water year 1969; Part 1. Surface water records","docAbstract":"Surface-water records for the 1969 water year for New Mexico, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report and their locations shown in figures 1, 2. Records for a few pertinent gaging stations in bordering states also are included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of W. E. Hale, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in New Mexico. Through September 30, 1960, the records of discharge and stage of streams and canals and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled Surface Water Supply of the United States.\"\nBeginning with the 1961 water year, surface-water records have been released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these reports is limited; they are designed primarily for rapid release of data shortly after the end of the water year to meet local needs. The discharge and reservoir storage records for 1961-65 also will be published in a Geological Survey water-supply paper series entitled \"Surface Water Supply of the United States 1961-65.\"","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Santa Fe, NM","doi":"10.3133/wdrNM691","collaboration":"Prepared in cooperation with the State of New Mexico and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Water resources data for New Mexico, water year 1969; Part 1. Surface water records: U.S. Geological Survey Water Data Report NM-69-1, 268 p., https://doi.org/10.3133/wdrNM691.","productDescription":"268 p.","costCenters":[],"links":[{"id":273456,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274525,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1969/nm-69/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.052,31.3322 ], [ -109.052,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.052,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b300eae4b01368e589e424","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535537,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70040710,"text":"70040710 - 1970 - Ground-water resources in the eastern Oswego River basin, New York","interactions":[],"lastModifiedDate":"2012-11-13T12:35:16","indexId":"70040710","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":241,"text":"Basin Planning Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"ORB-2","title":"Ground-water resources in the eastern Oswego River basin, New York","language":"English","publisher":"New York State Water Resources Commission","publisherLocation":"Albany, NY","usgsCitation":"Kantrowitz, I., 1970, Ground-water resources in the eastern Oswego River basin, New York: Basin Planning Report ORB-2, 129 p.; 6 Plates.","productDescription":"129 p.; 6 Plates","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263104,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a3ba68e4b0855e233c074a","contributors":{"authors":[{"text":"Kantrowitz, I.H.","contributorId":15646,"corporation":false,"usgs":true,"family":"Kantrowitz","given":"I.H.","affiliations":[],"preferred":false,"id":468856,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70040754,"text":"70040754 - 1970 - Time-of-travel studies in the Fall Creek basin, Tompkins County, New York, including low-flow characteristics","interactions":[{"subject":{"id":52458,"text":"ofr6547 - 1965 - Time of travel studies, Fall Creek basin, Tompkins County, New York","indexId":"ofr6547","publicationYear":"1965","noYear":false,"title":"Time of travel studies, Fall Creek basin, Tompkins County, New York"},"predicate":"SUPERSEDED_BY","object":{"id":70040754,"text":"70040754 - 1970 - Time-of-travel studies in the Fall Creek basin, Tompkins County, New York, including low-flow characteristics","indexId":"70040754","publicationYear":"1970","noYear":false,"title":"Time-of-travel studies in the Fall Creek basin, Tompkins County, New York, including low-flow characteristics"},"id":1}],"lastModifiedDate":"2017-09-13T18:25:06","indexId":"70040754","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5495,"text":"New York State Department of Environmental Conservation Report of Investigations","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"RI-11","title":"Time-of-travel studies in the Fall Creek basin, Tompkins County, New York, including low-flow characteristics","language":"English","publisher":"New York State Water Resources Commission","publisherLocation":"Albany, NY","usgsCitation":"Dunn, B., 1970, Time-of-travel studies in the Fall Creek basin, Tompkins County, New York, including low-flow characteristics: New York State Department of Environmental Conservation Report of Investigations RI-11, 21 p.","productDescription":"21 p.","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263188,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70040754.png"},{"id":274890,"type":{"id":15,"text":"Index Page"},"url":"https://archive.org/details/usgswaterresourcesnewyork-ri_11"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a61d6be4b0d446a665ca0e","contributors":{"authors":[{"text":"Dunn, Bernard","contributorId":61423,"corporation":false,"usgs":true,"family":"Dunn","given":"Bernard","email":"","affiliations":[],"preferred":false,"id":468961,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70001561,"text":"70001561 - 1970 - Water content of basalt erupted on the ocean floor","interactions":[],"lastModifiedDate":"2020-11-30T16:42:59.538015","indexId":"70001561","displayToPublicDate":"2010-09-28T23:09:22","publicationYear":"1970","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":"Water content of basalt erupted on the ocean floor","docAbstract":"

Deep sea pillow basalts dredged from the ocean floor show that vesicularity changes with composition as well as with depth. Alkalic basalts are more vesicular than tholeiitic basalts erupted at the same depth. The vesicularity data, when related to experimentally determined solubility of water in basalt, indicate that K-poor oceanic tholeiites originally contained about 0.25 percent water, Hawaiian tholeiites of intermediate K-content, about 0.5 percent water, and alkali-rich basalts, about 0.9 percent water. Analyses of fresh basalt pillows show a systematic increase of H2O+ as the rocks become more alkalic. K-poor oceanic tholeiites contain 0.06–0.42 percent H2O+, Hawaiian tholeiites, 0.31–0.60 percent H2O+, and alkali rich basalts 0.49–0.98 percent H2O+. The contents of K2O, P2O5, F, and Cl increase directly with an increase in H2O+ content such that at 1.0 weight percent H2O+, K2O is 1.58 percent, P2O5 is 0.55 percent, F is 0.07 percent, and Cl is 0.1 percent. The measured weight percent of deuterium on the rim of one Hawaiian pillow is −6.0 (relative to SMOW); this value, which is similar to other indications of magmatic water, suggests that no appreciable sea water was absorbed by the pillow during or subsequent to eruption on the ocean floor.

Concentrations of volatile constituents in the alkali basalt melts relative to tholeiitic melts can be explained by varying degrees of partial melting of mantle material or by fractional crystallization of a magma batch.

","language":"English","publisher":"Springer","doi":"10.1007/BF00388949","issn":"00107999","usgsCitation":"Moore, J., 1970, Water content of basalt erupted on the ocean floor: Contributions to Mineralogy and Petrology, v. 28, no. 4, p. 272-279, https://doi.org/10.1007/BF00388949.","productDescription":"8 p.","startPage":"272","endPage":"279","costCenters":[],"links":[{"id":203746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489f4f","contributors":{"authors":[{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":346801,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220067,"text":"5220067 - 1970 - Mass movement of black fly larvae on silken threads (Diptera: Simuliidae)","interactions":[],"lastModifiedDate":"2023-02-21T17:09:10.94562","indexId":"5220067","displayToPublicDate":"2010-06-16T12:18:02","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":798,"text":"Annals of the Entomological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Mass movement of black fly larvae on silken threads (Diptera: Simuliidae)","docAbstract":"

Stoppage of waterflow in a stream resulted in the migration of massive numbers of black fly larvae on silken threads. Larvae were found on single silken threads, but the heaviest concentrations were on “cables” composed of 25-50 individual silken threads. The larvae were attached in concentric rings around the silken threads and cables.

","language":"English","publisher":"Oxford Academic Press","doi":"10.1093/aesa/63.2.607","usgsCitation":"Tarshis, I., and Neil, W., 1970, Mass movement of black fly larvae on silken threads (Diptera: Simuliidae): Annals of the Entomological Society of America, v. 63, no. 2, p. 607-610, https://doi.org/10.1093/aesa/63.2.607.","productDescription":"4 p.","startPage":"607","endPage":"610","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193574,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"2","noUsgsAuthors":false,"publicationDate":"1970-03-16","publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fd98","contributors":{"authors":[{"text":"Tarshis, I.B.","contributorId":83625,"corporation":false,"usgs":true,"family":"Tarshis","given":"I.B.","email":"","affiliations":[],"preferred":false,"id":331286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neil, W.","contributorId":86063,"corporation":false,"usgs":true,"family":"Neil","given":"W.","email":"","affiliations":[],"preferred":false,"id":331287,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5220066,"text":"5220066 - 1970 - Two species of Simuliidae (Diptera), Cnephia ornithophilia and Prosimulium vernale, from Maryland","interactions":[],"lastModifiedDate":"2023-02-13T22:58:14.366194","indexId":"5220066","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":798,"text":"Annals of the Entomological Society of America","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Two species of Simuliidae (Diptera), Cnephia ornithophilia and Prosimulium vernale, from Maryland","title":"Two species of Simuliidae (Diptera), Cnephia ornithophilia and Prosimulium vernale, from Maryland","docAbstract":"

The finding of Cnephia ornithophilia Davies, Peterson, & Wood and Prosimulium vernale Shewell for the first time at the Patuxent Wildlife Research Center, Laurel, Maryland, is described. Larvae of C. ornithophilia were collected Nov. 15, pupae Feb. 14, and adult flies Feb. 28. No immature or adult specimens were found between Apr. 2 and Nov. 14. The greatest number of immature stages was found in a 3- to 5-foot-wide stream several hundred feet long, 1-8 inches deep, with a stream flow between 0.49 and 3.30 feet per second. The water temperature varied from 0.5° to 4.0°C, the oxygen content was 10-13 ppm; and the pH varied from 6.9 to 7.4. Larvae of P. vernale were collected Nov. 30 through March, pupae from February through Apr. 1, and adult flies from Feb. 26 through Apr. 1. No immature or adult specimens were found between Apr. 2 and Nov. 29. The largest number of immature stages of P. vernale was found in a 6- to 16-foot-wide stream, 100 feet long, and 1.2 inches deep. The stream flow was between 0.92 and 1.36 feet per second. The water temperature was 0.5°C; pH was 6.7; and oxygen content was 7 ppm.

","language":"English","publisher":"Oxford Academic Press","doi":"10.1093/aesa/63.2.587","usgsCitation":"Tarshis, I., and Stuht, J., 1970, Two species of Simuliidae (Diptera), Cnephia ornithophilia and Prosimulium vernale, from Maryland: Annals of the Entomological Society of America, v. 63, no. 2, p. 587-590, https://doi.org/10.1093/aesa/63.2.587.","productDescription":"4 p.","startPage":"587","endPage":"590","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193573,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","city":"Laurel","otherGeospatial":"Patuxent Wildlife Research Center","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.83910511083083,\n 39.056967490820995\n ],\n [\n -76.83651187120617,\n 39.0518361946026\n ],\n [\n -76.83322710101596,\n 39.05022509750219\n ],\n [\n -76.82855926969188,\n 39.04646572801187\n ],\n [\n -76.82631179535134,\n 39.04592865889336\n ],\n [\n -76.82147108138619,\n 39.04727132403269\n ],\n [\n -76.81282694930492,\n 39.048479700836594\n ],\n [\n -76.80694893949003,\n 39.047539853997534\n ],\n [\n -76.79865057269289,\n 39.04324325205229\n ],\n [\n -76.7958844504265,\n 39.04055774312775\n ],\n [\n -76.79380985872771,\n 39.03679785913823\n ],\n [\n -76.78827761419562,\n 39.033037775075485\n ],\n [\n -76.77928771683158,\n 39.02954608930375\n ],\n [\n -76.7766944772076,\n 39.02780018172879\n ],\n [\n -76.77098935003441,\n 39.025785619401375\n ],\n [\n -76.76874187569324,\n 39.01906999698835\n ],\n [\n -76.7644198096526,\n 39.016786540051754\n ],\n [\n -76.74972478511539,\n 39.035857856879545\n ],\n [\n -76.74159930095931,\n 39.042840432221624\n ],\n [\n -76.73917894397707,\n 39.04646572801187\n ],\n [\n -76.73641282171135,\n 39.05334273405077\n ],\n [\n -76.7338195820867,\n 39.05777296705838\n ],\n [\n -76.72984328132952,\n 39.059920858768635\n ],\n [\n -76.72742292434728,\n 39.061665972670056\n ],\n [\n -76.72258221038211,\n 39.063813745948806\n ],\n [\n -76.71964320547467,\n 39.066901055558276\n ],\n [\n -76.71428384358431,\n 39.068914445600285\n ],\n [\n -76.70771430320318,\n 39.07589375308592\n ],\n [\n -76.70235494131279,\n 39.07924894368335\n ],\n [\n -76.69976170168883,\n 39.08569046238466\n ],\n [\n -76.71912455754948,\n 39.08971611288936\n ],\n [\n -76.72292797566492,\n 39.08756912787962\n ],\n [\n -76.75300955530629,\n 39.088911001169436\n ],\n [\n -76.76753169720179,\n 39.09696170478483\n ],\n [\n -76.77773177305731,\n 39.114535880241874\n ],\n [\n -76.80107092967515,\n 39.09682753392198\n ],\n [\n -76.82786773912561,\n 39.07441741867859\n ],\n [\n -76.83910511083083,\n 39.056967490820995\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"63","issue":"2","noUsgsAuthors":false,"publicationDate":"1970-03-16","publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db62397a","contributors":{"authors":[{"text":"Tarshis, I.B.","contributorId":83625,"corporation":false,"usgs":true,"family":"Tarshis","given":"I.B.","email":"","affiliations":[],"preferred":false,"id":331285,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuht, J.N.","contributorId":72680,"corporation":false,"usgs":true,"family":"Stuht","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":331284,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5210074,"text":"5210074 - 1970 - Aims and methods of waterfowl research in North America","interactions":[],"lastModifiedDate":"2012-02-02T00:15:14","indexId":"5210074","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1970","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"30","title":"Aims and methods of waterfowl research in North America","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"VIII International Congress of Game Biologists","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","collaboration":"August 22-27, 1967, Helsinki, Finland","usgsCitation":"Crissey, W., 1970, Aims and methods of waterfowl research in North America, chap. of VIII International Congress of Game Biologists, p. 37-46.","startPage":"37","endPage":"46","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688efb","contributors":{"authors":[{"text":"Crissey, W.F.","contributorId":21656,"corporation":false,"usgs":true,"family":"Crissey","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":327714,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71005,"text":"wdrMN7012 - 1970 - Water resources data for Minnesota, water year 1970, Part 1. Surface water records and Part 2. Water quality records","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"wdrMN7012","displayToPublicDate":"2005-08-09T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MN-70-1-2","title":"Water resources data for Minnesota, water year 1970, Part 1. Surface water records and Part 2. Water quality records","language":"ENGLISH","doi":"10.3133/wdrMN7012","usgsCitation":"Geological Survey, U., 1970, Water resources data for Minnesota, water year 1970, Part 1. Surface water records and Part 2. Water quality records: U.S. Geological Survey Water Data Report MN-70-1-2, 307 p., https://doi.org/10.3133/wdrMN7012.","productDescription":"307 p.","costCenters":[],"links":[{"id":185751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1970/mn-70-1-2/report-thumb.jpg"},{"id":90533,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1970/mn-70-1-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3e99","contributors":{"authors":[{"text":"Geological Survey, U.S.","contributorId":26017,"corporation":false,"usgs":true,"family":"Geological Survey","given":"U.S.","affiliations":[],"preferred":false,"id":283481,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":54138,"text":"ofr7010 - 1970 - A proposed streamflow data program for Ohio","interactions":[],"lastModifiedDate":"2017-01-18T14:39:13","indexId":"ofr7010","displayToPublicDate":"2004-04-01T00:00:00","publicationYear":"1970","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":"70-10","title":"A proposed streamflow data program for Ohio","docAbstract":"

A streamflow data program is proposed for Ohio which consists of both data collection and data analysis. The program is proposed after a study which (1) established long-term objectives and goals for streamflow information, (2) examined and analyzed available data to determine its adequacy for meeting the established goals, and (3) considered alternate methods and data requirements for providing information to meet unfulfilled goals.

The program is designed to provide data (1) for current use, (2) for planning and design, (3) for definition of long-term trends, and (4) on the characteristics of stream environment. At present 141 gaging stations provide adequate data for current use. Multiple- regression relations have been defined that accurately estimate many flow characteristics needed for planning and design on natural-flow streams. A systems approach is required to define flow characteristics of regulated streams. A network of 13 existing gages is proposed for indefinite operation to define long-term flow trends, and additional data collection is proposed on the characteristics of stream environment. Studies of available data and of data to become available are suggested.

The proposed program may be modified in the future to reflect the degree of information that becomes available from new and improved data analyses.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7010","usgsCitation":"Anttila, P.W., 1970, A proposed streamflow data program for Ohio: U.S. Geological Survey Open-File Report 70-10, Report: iv, 62 p.; 2 Figures: 17.79 x 19.50 inches and 16.86 x 18.89 inches, https://doi.org/10.3133/ofr7010.","productDescription":"Report: iv, 62 p.; 2 Figures: 17.79 x 19.50 inches and 16.86 x 18.89 inches","numberOfPages":"68","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":174092,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":333372,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0010/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":333373,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0010/figure-2.pdf","text":"Figure 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9acb","contributors":{"authors":[{"text":"Anttila, Peter W.","contributorId":27423,"corporation":false,"usgs":true,"family":"Anttila","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":249302,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010413,"text":"70010413 - 1970 - Coastal currents and mass transport of surface sediments over the shelf regions of Monterey Bay, California","interactions":[],"lastModifiedDate":"2025-04-16T15:08:04.716543","indexId":"70010413","displayToPublicDate":"2003-04-04T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Coastal currents and mass transport of surface sediments over the shelf regions of Monterey Bay, California","docAbstract":"

In Monterey Bay, the highest concentrations of medium and fine sands occur nearshore between ten and thirty fathoms. Silt and clay accumulate in greater depths. Contours of median diameter roughly parallel the isobaths.

Fine-grained materials are supplied to the bay region from erosion of cliffs which partly surround Monterey Bay, from sediment laden river discharge, and from continual reworking of widespread Pleistocene and Recent sea floor sediments. These sediments in turn are picked up by coastal currents and distributed over the shelf regions by present day current regimes.

Studies of bottom currents over the shelf regions and in Monterey Canyon have revealed patterns which vary with seasonal changes. Current patterns during August and September exhibit remarkable symmetry about the axis of Monterey Submarine Canyon. Central Shelf currents north and south of Monterey Canyon flowed northwest at an average rate of 0.2 knots and south at 0.3 knots respectively. On the North Shelf between January and March currents flowed east to southeast at 0.3–0.5 knots with mirror image patterns above the South Shelf during the same period.

Irregular current flow in the canyon indicates a complex current structure with frequent shifts in counterclockwise and clockwise direction over very short periods of time. Bottom topography of the canyon complex often causes localization of canyon currents. One particular observation at a depth of 51 fathoms indicated up-canyon flow at a rate of 0.2 knots. Most of the observed currents are related to seasonal variations, upwelling, ocean swell patterns, and to changes in the California and Davidson currents.

Changes in current regimes are reflected in the patterns of sediment distribution and transport. Sediment transport is chiefly parallel to the isobaths, particularly on the North and South Shelf regions. Complex dispersal patterns are observed near Monterey Canyon and Moss Landing Harbor jetties. Longshore currents move sediments southward except near Monterey Canyon which acts as a physiographic barrier and the extreme southern end of the bay where currents are non persistent.

Some sediments are also transported offshore by rip currents and other agencies and deposited in deeper, quieter waters. Supply of sediments to the canyon head results in over-filling and steepening with subsequent mass movement of sediments seaward followed by deposition in channels and on the broad deep sea fan.

","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(70)90029-0","issn":"00253227","usgsCitation":"Wolf, S.C., 1970, Coastal currents and mass transport of surface sediments over the shelf regions of Monterey Bay, California: Marine Geology, v. 8, no. 5, p. 321-336, https://doi.org/10.1016/0025-3227(70)90029-0.","productDescription":"16 p.","startPage":"321","endPage":"336","costCenters":[],"links":[{"id":219302,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Monterey Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.23388671874999,\n 36.507428541837264\n ],\n [\n -121.57745361328125,\n 36.507428541837264\n ],\n [\n -121.57745361328125,\n 37.04202441635081\n ],\n [\n -122.23388671874999,\n 37.04202441635081\n ],\n [\n -122.23388671874999,\n 36.507428541837264\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"8","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f780e4b0c8380cd4cb4f","contributors":{"authors":[{"text":"Wolf, Stephen C.","contributorId":38148,"corporation":false,"usgs":true,"family":"Wolf","given":"Stephen","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":358862,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010436,"text":"70010436 - 1970 - The structure and origin of the large submarine canyons of the Bering Sea","interactions":[],"lastModifiedDate":"2025-04-16T15:21:45.429592","indexId":"70010436","displayToPublicDate":"2003-04-02T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"The structure and origin of the large submarine canyons of the Bering Sea","docAbstract":"

Three exceptionally large and long submarine canyons — Bering, Pribilof, and Zhemchug — incise the continental slope underlying the southeastern Bering Sea. Bering Canyon, the world's longest known slope valley, is approximately 400 km long and has a volume of 4,300 km3. The volume of Pribilof Canyon is 1,300 km3 and that of Zhemchug is 8,500 km3; Zhemchug Canyon may well be the world's largest slope valley; most other large submarine canyons have volumes less than 500 km3. Pribilof and Zhemchug canyons are further distinguished by the headward bifurcation of their slope axes to form elongated trough-shaped basins behind the regionally projected position of the shelf edge. These troughs are superimposed over structural depressions formed by down-faulted basement rocks of Mesozoic and older ages. Prior to canyon cutting these depressions were filled with as much as 2,600 m of shallow-water diatomaceous, tuffaceous, and detrital sediments largely of Tertiary age. Deposition of these sediments took place concurrently with general margin subsidence of at least 2,000 m.

The data and conclusions presented in this paper stress that the location, trend, and shape of the enormous submarine canyons cutting the Bering margin are structurally determined. However, axial cutting and headward erosion within the relatively unconsolidated Tertiary strata and the older, lithified basement rock is thought to have been caused by basinward-sliding masses of sediment; these unstable sediment bodies accumulated on the upper continental slope and outer shelf, probably near the mouths of major Alaskan rivers.

Bering Canyon was periodically cut and filled by axial sedimentation during Late Tertiary and Quaternary time. Pribilof and Zhemchug canyons, however, are thought to have been excavated entirely during the Pleistocene. It is presumed that, during one or more periods of glacially lowered sea level, the Kuskokwim and Yukon rivers emptied into or near the heads of Pribilof and Zhemchug canyons. The enormous size and unusual shape of Zhemchug Canyon resulted from the breaching of the seaward wall of an outer-shelf basement depression and the subsequent removal of nearly 4,500 km3 of Tertiary deposits filling it.

","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(70)90043-5","issn":"00253227","usgsCitation":"Scholl, D., Buffington, E.C., Hopkins, D., and Alpha, T.R., 1970, The structure and origin of the large submarine canyons of the Bering Sea: Marine Geology, v. 8, no. 3-4, p. 187-210, https://doi.org/10.1016/0025-3227(70)90043-5.","productDescription":"24 p.","startPage":"187","endPage":"210","costCenters":[],"links":[{"id":219758,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -168.48632812499997,\n 54.77534585936447\n ],\n [\n -154.16015625,\n 54.77534585936447\n ],\n [\n -154.16015625,\n 60.19615576604439\n ],\n [\n -168.48632812499997,\n 60.19615576604439\n ],\n [\n -168.48632812499997,\n 54.77534585936447\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"8","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb096e4b08c986b324f56","contributors":{"authors":[{"text":"Scholl, D.W.","contributorId":106461,"corporation":false,"usgs":true,"family":"Scholl","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":358927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buffington, E. C.","contributorId":13948,"corporation":false,"usgs":true,"family":"Buffington","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":358924,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hopkins, D.M.","contributorId":103646,"corporation":false,"usgs":true,"family":"Hopkins","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":358926,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Alpha, T. R.","contributorId":20715,"corporation":false,"usgs":true,"family":"Alpha","given":"T.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":358925,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70009840,"text":"70009840 - 1970 - Submarine basalt from the Revillagigedo Islands region, Mexico","interactions":[],"lastModifiedDate":"2025-04-16T15:03:40.797211","indexId":"70009840","displayToPublicDate":"2003-01-04T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Submarine basalt from the Revillagigedo Islands region, Mexico","docAbstract":"

Ocean-floor dredging and submarine photography in the Revillagigedo region off the west coast of Mexico reveal that the dominant exposed rock of the submarine part of the large island-forming volcanoes (Roca Partida and San Benedicto) is a uniform alkali pillow basalt; more siliceous rocks are exposed on the upper, subaerial parts of the volcanoes. Basalts dredged from smaller seamounts along the Clarion fracture zone south of the Revillagigedo Islands are tholeiitic pillow basalts. Pillows of alkali basalts are more vesicular than Hawaiian tholeiitic pillows collected from the same depths. This difference probably reflects a higher original volatile content of the alkali basalts.

Manganese-iron oxide nodules common in several dredge hauls generally contain nucleii of rhyolitic pumice or basalt pillow fragments. The pumice floated to its present site from subaerial eruptions, became waterlogged and sank, and was then coated with manganese-iron oxides. The thickness of palagonite rinds on the glassy pillow fragments is proportional to the thickness of manganese-iron oxide layers, and both are a measure of the age of the nodule. Both oldest basalts (10–100 m.y.) and youngest (less than 1 m.y.) are along the Clarion fracture zone, whereas basalts from Roca Partida and San Benedicto volcanoes are of intermediate age.

","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(70)90022-8","issn":"00253227","usgsCitation":"Moore, J., 1970, Submarine basalt from the Revillagigedo Islands region, Mexico: Marine Geology, v. 9, no. 5, p. 331-345, https://doi.org/10.1016/0025-3227(70)90022-8.","productDescription":"15 p.","startPage":"331","endPage":"345","numberOfPages":"15","costCenters":[],"links":[{"id":218761,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.0498046875,\n 22.268764039073968\n ],\n [\n -105.2490234375,\n 22.268764039073968\n ],\n [\n -105.2490234375,\n 24.84656534821976\n ],\n [\n -111.0498046875,\n 24.84656534821976\n ],\n [\n -111.0498046875,\n 22.268764039073968\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"9","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d1fe4b08c986b31d65a","contributors":{"authors":[{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":357264,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70200882,"text":"wdrID691 - 1970 - Water resources data for Idaho, water year 1969: Part 1. Surface water records","interactions":[],"lastModifiedDate":"2025-05-22T20:26:18.01434","indexId":"wdrID691","displayToPublicDate":"1999-01-01T12:16:06","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ID-69-1","title":"Water resources data for Idaho, water year 1969: Part 1. Surface water records","docAbstract":"

Surface-water records for the 1969 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Idaho are given in this report and their locations shown in figures 2 and 3. Records for a few selected gaging stations in bordering States also are included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of W. L. Burnham, district chief, Water Resources Division.

Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Idaho were contained in Parts 10, 12, and 13 of that series.

Beginning with the 1961 water year, streamflow records and related data have been released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports is limited and primarily for local needs. Records will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of conterminous United States will be further subdivided.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrID691","collaboration":"Prepared in cooperation with the State of Idaho and with other agencies","usgsCitation":"U.S. Geological Survey, 1970, Water resources data for Idaho, water year 1969: Part 1. 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Print. Off.,","doi":"10.3133/twri03C2_1970","issn":"0565-596X","usgsCitation":"Guy, H., and Norman, V.W., 1970, Field methods for measurement of fluvial sediment (1970): U.S. Geological Survey Techniques of Water-Resources Investigations 03-C2, vi, 59 p. :ill. ;26 cm. Reprinted in 1982., https://doi.org/10.3133/twri03C2_1970.","productDescription":"vi, 59 p. :ill. ;26 cm. Reprinted in 1982.","costCenters":[],"links":[{"id":94735,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/twri/03c02-1970/report.pdf","size":"11967","linkFileType":{"id":1,"text":"pdf"}},{"id":139160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/twri/03c02-1970/report-thumb.jpg"}],"edition":"1970","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f56cb","contributors":{"authors":[{"text":"Guy, Harold P.","contributorId":6434,"corporation":false,"usgs":true,"family":"Guy","given":"Harold P.","affiliations":[],"preferred":false,"id":149620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norman, Vernon W.","contributorId":22325,"corporation":false,"usgs":true,"family":"Norman","given":"Vernon","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":149621,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2512,"text":"wsp1888 - 1970 - Hydrology of the Upper Malad River basin, southeastern Idaho","interactions":[],"lastModifiedDate":"2013-11-21T13:44:23","indexId":"wsp1888","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1970","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":"1888","title":"Hydrology of the Upper Malad River basin, southeastern Idaho","docAbstract":"The report area comprises 485 square miles in the Basin and Range physiographic province. It includes most of eastern' Oneida County and parts of Franklin, Bannock, and Power Counties of southeastern Idaho. Relief is about 5,000 feet; the floor of the Malad Valley is at an average altitude of about 4,400 feet. Agriculture is, by far, ,the principal economic .activity. In 1960 the population of the upper Malad River basin was about 3,600, of which about 60 percent resided in Malad City, the county seat of Oneida County. \n\n

The climate is semiarid throughout the Malad Valley and its principal tributary valleys; ,above 6,500 feet the climate is subhumid. Annual precipitation ranges from about 13 inches in the lower Malad Valley to more than 30 inches on the highest peaks of the Bannock and Malad ranges. Owing to ,the normally clear atmospheric conditions, large daily and seasonal temperature fluctuations are common. Topography, distance from the Pacific Ocean, .and the general atmospheric circulation are the principal factors governing the climate of the Malad River basin. The westerlies transport moisture from the P.acific Ocean toward southeastern Idaho. The north-south tren4ing mountains flanking the basin are oriented orthogonally to the moisture flux so that they are very effective in removing precipitable water from the air. A minimum uplift of 6,000 feet is required to transport moisture from the Pacific source region; accordingly, most air masses are desiccated long before they reach the Malad basin. Heaviest precipitation is generally associated with steep pressure gradients in the midtroposphere that are so oriented as to cause a deep landward penetration of moisture from the Pacific Ocean.

\n\n

Annual water yields in the project area range from about 0.8 inch in the, lower Malad Valley to more than 19 inches on the high peaks north and east of Malad City. The mean annual water yield for the entire basin is 4 inches, or about 115,000 acre-feet. Evaporation is greatest in July when about 7 inches is lost from lakes, reservoirs, and waterlogged areas; losses from free-water surfaces may be as much .as 38 inches annually.

\n\n

An extensive ground-water reservoir consisting of sand and gravel interbedded with relatively impermeable beds of silt .and clay underlies much of the Malad Valley. Wells near the center of the valley exceeding 700 feet in depth do not reach bedrock. The Woodruff fault, which transects the constricted lower Malad Valley, is one of the main factors creating artesian conditions south of the latitude of Malad City. Recharge is obtained principally from mountain runoff which flows onto highly permeable alluvial fans surrounding the valley and from streams that flow across the valley floor. On the basis of a water balance analysis, under flow from the project area was estimated to be 28,000 acre-feet annually, surface-water outflow was 51,000 acre-feet, and transbasin imports were about 4,000 acre-feet.

\n\n

The principal tributaries of the Malad River are perennial along their upper and middle reaches and have well-sustained low flows. During the growing season, all surface water entering the Malad Valley is used for irrigation. Spine irrigation is practiced in the principal tributary valleys; however, a shortage of suitable reservoir sites has hampered surface-water development in these areas. The highly porous deposits underlying the Malad Valley tend to attenuate flood peaks. An unusual combination of meteorologic events early in 1962 effectively counteracted the high absorptive capacity of the valley and predisposed the basin to high flood risk. Subsequent rapid snowmelt combined with frozen ground produced the extraordinary flood of February 12, 1962.

\n\n

Calcium and bicarbonate commonly are the most abundant ions in the surface waters of the upper Malad River basin. In August 1967, the dissolved-solids content of streamflow ranged from 200 to 350 milligrams per liter in the middle and upper parts of the basin; however, much greater values were measured in the Malad River between Woddruff and Cherry Creek Lane. With the exception of that reach, the surface water of the project area is suitable for irrigating all but the most sensitive crops.

\n\n

The total water yield is not sufficient to meet all the water needs of the basin. A comprehensive water-management plan is required to ensure optimal use of the water resource.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington D.C.","doi":"10.3133/wsp1888","usgsCitation":"Pluhowski, E.J., 1970, Hydrology of the Upper Malad River basin, southeastern Idaho: U.S. Geological Survey Water Supply Paper 1888, v, 89 p., https://doi.org/10.3133/wsp1888.","productDescription":"v, 89 p.","numberOfPages":"94","costCenters":[],"links":[{"id":138716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1888/report-thumb.jpg"},{"id":28673,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1888/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Upper Malad River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdb62","contributors":{"authors":[{"text":"Pluhowski, Edward J.","contributorId":87911,"corporation":false,"usgs":true,"family":"Pluhowski","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145318,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3144,"text":"wsp1926 - 1970 - Surface water supply of the United States, 1961-65, Part 9. Colorado River basin, Volume 3. Lower Colorado River basin","interactions":[],"lastModifiedDate":"2021-12-03T20:30:05.371112","indexId":"wsp1926","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1926","title":"Surface water supply of the United States, 1961-65, Part 9. Colorado River basin, Volume 3. Lower Colorado River basin","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1926","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Surface water supply of the United States, 1961-65, Part 9. Colorado River basin, Volume 3. Lower Colorado River basin: U.S. Geological Survey Water Supply Paper 1926, Report; 571 p.; 1 Plate: 24.50 × 32.62 inches, https://doi.org/10.3133/wsp1926.","productDescription":"Report; 571 p.; 1 Plate: 24.50 × 32.62 inches","costCenters":[],"links":[{"id":30091,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1926/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30090,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1926/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1926/report-thumb.jpg"},{"id":110042,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25150.htm","linkFileType":{"id":5,"text":"html"},"description":"25150"}],"country":"United States","state":"Arizona, Baja California, California, Nevada, Sonora","otherGeospatial":"lower Colorado River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.01562499999999,\n 31.3348710339506\n ],\n [\n -112.47802734375,\n 31.3348710339506\n ],\n [\n -112.47802734375,\n 36.98500309285596\n ],\n [\n -116.01562499999999,\n 36.98500309285596\n ],\n [\n -116.01562499999999,\n 31.3348710339506\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db692480","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528104,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3087,"text":"wsp1923 - 1970 - Surface water supply of the United States, 1961-65: Part 8, western Gulf of Mexico basins: Volume 2, basins from Lavaca River to Rio Grande","interactions":[],"lastModifiedDate":"2022-12-09T21:15:35.313638","indexId":"wsp1923","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1923","title":"Surface water supply of the United States, 1961-65: Part 8, western Gulf of Mexico basins: Volume 2, basins from Lavaca River to Rio Grande","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1923","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Surface water supply of the United States, 1961-65: Part 8, western Gulf of Mexico basins: Volume 2, basins from Lavaca River to Rio Grande: U.S. Geological Survey Water Supply Paper 1923, Report: ix, 786 p.; 1 Plate: 30.00 × 36.24 inches, https://doi.org/10.3133/wsp1923.","productDescription":"Report: ix, 786 p.; 1 Plate: 30.00 × 36.24 inches","costCenters":[],"links":[{"id":110040,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25147.htm","linkFileType":{"id":5,"text":"html"},"description":"25147"},{"id":138639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1923/report-thumb.jpg"},{"id":29966,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1923/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29965,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1923/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"western Gulf of Mexico basins","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -96,\n 26\n ],\n [\n -96,\n 38.376\n ],\n [\n -108.444,\n 38.376\n ],\n [\n -108.444,\n 26\n ],\n [\n -96,\n 26\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db69294a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528068,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3146,"text":"wsp1965 - 1970 - Quality of surface waters of the United States, 1965. Parts 9-11, Colorado River basin to Pacific slope basins in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1965","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1965","title":"Quality of surface waters of the United States, 1965. Parts 9-11, Colorado River basin to Pacific slope basins in California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1965","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Quality of surface waters of the United States, 1965. Parts 9-11, Colorado River basin to Pacific slope basins in California: U.S. Geological Survey Water Supply Paper 1965, xiv, 678 p. ;23 cm., https://doi.org/10.3133/wsp1965.","productDescription":"xiv, 678 p. ;23 cm.","costCenters":[],"links":[{"id":138879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1965/report-thumb.jpg"},{"id":30094,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1965/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6519d0","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528105,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3088,"text":"wsp1925 - 1970 - Surface water supply of the United States, 1961-65, Part 9. Colorado River basin, Volume 2. Colorado River basin from Green River to Compact Point","interactions":[],"lastModifiedDate":"2021-12-03T20:25:13.975014","indexId":"wsp1925","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1925","title":"Surface water supply of the United States, 1961-65, Part 9. Colorado River basin, Volume 2. Colorado River basin from Green River to Compact Point","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1925","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Surface water supply of the United States, 1961-65, Part 9. Colorado River basin, Volume 2. Colorado River basin from Green River to Compact Point: U.S. Geological Survey Water Supply Paper 1925, Report: 618 p.; 1 Plate: 19.00 × 32.15 inches, https://doi.org/10.3133/wsp1925.","productDescription":"Report: 618 p.; 1 Plate: 19.00 × 32.15 inches","costCenters":[],"links":[{"id":138640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1925/report-thumb.jpg"},{"id":29967,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1925/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29968,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1925/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392463,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25149.htm"}],"country":"United States","state":"Arizona, Colorado, Idaho, New Mexico, Utah","otherGeospatial":"Colorado River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.250,\n 35.525\n ],\n [\n -106.692,\n 35.525\n ],\n [\n -106.692,\n 43.396\n ],\n [\n -112.250,\n 43.396\n ],\n [\n -112.250,\n 35.525\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af6e4b07f02db692a93","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528069,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2477,"text":"wsp1608M - 1970 - Hydrographic and sedimentation survey of Kajakai Reservoir, Afghanistan","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1608M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"M","title":"Hydrographic and sedimentation survey of Kajakai Reservoir, Afghanistan","docAbstract":"A hydrographic and sedimentation survey of Band-e Kajakai (Kajakai Reservoir) on the Darya-ye Hirmand (Helmand River) was carried out during the period September through December 1968. Underwater mapping techniques were used to determine the reservoir capacity as of 1968. Sediment range lines were established and monumented to facilitate future sedimentation surveys. Afghanistan engineers and technicians were trained to carry out future reservoir surveys. Samples were obtained of the reservoir bed and in the river upstream from the reservoir. Virtually no sediments coarser than about 0.063 millimeter were found on the reservoir bed surface. The median diameter of sands being transported into the reservoir ranged from 0.040 to 0.110 millimeter. The average annual rate of sedimentation was 7,800 acre-feet. Assuming an average density of 50 pounds per cubic foot (800 kilograms per cubic meter), the estimated average sediment inflow to the reservoir was about 8,500,000 tons (7,700,000 metric tons) per year. \r\n\r\nThe decrease in capacity at spillway elevation for the period 1953 to 1968 due to sediment deposition was 7.8 percent, or 117,700 acre-feet. Redefinition of several contours above the fill area resulted in an increase in capacity at spillway elevation of 13,600 acre-feet; thus, the net change in capacity was 7.0 percent, or 104,800 acre-feet. \r\n\r\nBased on current data and an estimated rate of compaction of deposited sediment, the assumption of no appreciable change in hydrologic conditions in the drainage area, the leading edge of the principal delta will reach the irrigation outlet in 40-45 years. \r\n\r\nIt is recommended that a resurvey of sediment range lines be made during the period 1973-75.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1608M","usgsCitation":"Perkins, D.C., and Culbertson, J.K., 1970, Hydrographic and sedimentation survey of Kajakai Reservoir, Afghanistan: U.S. Geological Survey Water Supply Paper 1608, iv, 43 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1608M.","productDescription":"iv, 43 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608m/report-thumb.jpg"},{"id":28553,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608m/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6146cd","contributors":{"authors":[{"text":"Perkins, Don C.","contributorId":59429,"corporation":false,"usgs":true,"family":"Perkins","given":"Don","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Culbertson, James K.","contributorId":31371,"corporation":false,"usgs":true,"family":"Culbertson","given":"James","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":145258,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2479,"text":"wsp01B - 1970 - Detergents and associated contaminants in ground water at three public-supply well fields in southwestern Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp01B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"2001","chapter":"B","title":"Detergents and associated contaminants in ground water at three public-supply well fields in southwestern Suffolk County, Long Island, New York","docAbstract":"Sampling of groups of small-diameter shallow observation wells and nearby public-supply wells screened in the upper glacial aquifer at three well fields showed that detergents (MBAS) were distributed through almost the entire saturated thickness of the aquifer. Concentrations of MBAS in water from all the wells sampled ranged from less than 0.02 to nearly 5 mg/l (milligrams per liter), whereas MBAS concentrations in water pumped from shallow public supply wells ranged from about 0.1 mg/l to about 1.3 mg/l. Upward trends in MBAS concentrations, which were observed at most of the shallow observation wells from 1961 to 1966, nearly stabilized or declined to some extent by 1968. A slight to distinct upward trend in the MBAS content of water pumped from shallow public-supply wells was observed during the same period at two of the three well fields investigated. \r\n\r\nChloride concentrations in the upper glacial aquifer, which ranged from about 5 to 80 mg/l, had a distinct upward trend at some wells apparently due to infiltration of both sewage effluent and deicing salts which were applied to roads in the winter. Nitrate concentrations also increased slightly but remained below the recommended limit for drinking water. \r\n\r\nNo MBAS was detected in water from public-supply wells tapping deeper zones in the underlying Magothy aquifer, and significant amounts of MBAS and associated contaminants are unlikely to reach those zones for many years, if present flow patterns and head relationships are not markedly changed.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp01B","usgsCitation":"Perlmutter, N., and Guerrera, A., 1970, Detergents and associated contaminants in ground water at three public-supply well fields in southwestern Suffolk County, Long Island, New York: U.S. Geological Survey Water Supply Paper 2001, iv, 22 p. :illus. (2 fold. in pocket) ;23 cm., https://doi.org/10.3133/wsp01B.","productDescription":"iv, 22 p. :illus. (2 fold. in pocket) ;23 cm.","costCenters":[],"links":[{"id":138763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2001b/report-thumb.jpg"},{"id":28562,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2001b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28563,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2001b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28564,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2001b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6679cb","contributors":{"authors":[{"text":"Perlmutter, Nathaniel M.","contributorId":32139,"corporation":false,"usgs":true,"family":"Perlmutter","given":"Nathaniel M.","affiliations":[],"preferred":false,"id":145262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guerrera, A.A.","contributorId":86751,"corporation":false,"usgs":true,"family":"Guerrera","given":"A.A.","affiliations":[],"preferred":false,"id":145263,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3079,"text":"wsp1904 - 1970 - Surface water supply of the United States, 1961-65, Part 2. South Atlantic slope and eastern Gulf of Mexico, Volume 1. Basins from James River to Savannah River","interactions":[],"lastModifiedDate":"2021-10-20T18:19:29.410377","indexId":"wsp1904","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1904","title":"Surface water supply of the United States, 1961-65, Part 2. South Atlantic slope and eastern Gulf of Mexico, Volume 1. Basins from James River to Savannah River","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1904","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Surface water supply of the United States, 1961-65, Part 2. South Atlantic slope and eastern Gulf of Mexico, Volume 1. Basins from James River to Savannah River: U.S. Geological Survey Water Supply Paper 1904, Report: x, 942 p.; 1 Plate: 27.00 × 26.50 inches, https://doi.org/10.3133/wsp1904.","productDescription":"Report: x, 942 p.; 1 Plate: 27.00 × 26.50 inches","costCenters":[],"links":[{"id":29952,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1904/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390687,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25129.htm"},{"id":29953,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1904/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139417,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1904/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.644,\n 32.05\n ],\n [\n -75.517,\n 32.05\n ],\n [\n -75.517,\n 38.33\n ],\n [\n -83.644,\n 38.33\n ],\n [\n -83.644,\n 32.05\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db69420c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528060,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3148,"text":"wsp1903 - 1970 - Surface water supply of the United States, 1961-65: Part 1. North Atlantic slope basins: Volume 3. Basins from Maryland to York River","interactions":[],"lastModifiedDate":"2022-11-02T19:47:50.663475","indexId":"wsp1903","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1903","title":"Surface water supply of the United States, 1961-65: Part 1. North Atlantic slope basins: Volume 3. Basins from Maryland to York River","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1903","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Surface water supply of the United States, 1961-65: Part 1. North Atlantic slope basins: Volume 3. Basins from Maryland to York River: U.S. Geological Survey Water Supply Paper 1903, ix, 850 p., https://doi.org/10.3133/wsp1903.","productDescription":"ix, 850 p.","costCenters":[],"links":[{"id":409076,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25128.htm","linkFileType":{"id":5,"text":"html"}},{"id":30096,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1903/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1903/report-thumb.jpg"}],"country":"United States","state":"Delaware, Maryland, New Jersey, New York, Pennsylvania, Virginia, West Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -79.5,\n 42.936\n ],\n [\n -79.5,\n 37\n ],\n [\n -75.067,\n 37\n ],\n [\n -75.067,\n 42.936\n ],\n [\n -79.5,\n 42.936\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db69424c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528106,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37213,"text":"rp93 - 1970 - Common marsh plants of the United States and Canada","interactions":[],"lastModifiedDate":"2016-11-09T11:47:32","indexId":"rp93","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"93","title":"Common marsh plants of the United States and Canada","docAbstract":"

This is the fourth of a series of publications on field identification of North American marsh and water plants. It describes the emergent and semiemergent plants most likely to be found in inland and coastal marshes. It omits hundreds of uncommon marsh plants and plants less characteristic of marshes than of marsh edges, lake and stream shores, or wet meadows.

\n
\n

The first of the series, \"Pondweeds and Pondweedlike Plants of Eastern North America,\" Circular 187, was broadened in scope as Resource Publication 44, \"Underwater and Floating-leaved Plants of the United States and Canada,\" and is superseded by it. The present publication, widens the scope of \"Bulrushes and Bulrushlike Plants of Eastern North America,\" Circular 221, and contains most of the species listed therein.

\n
\n

This guide is designed for identification of marsh plants without recourse to technical botanical keys. To use it, read pages 1 to 4 and then look at the drawings. To identify a plant, find the group in which it fits, then find a drawing and description that match it.

","language":"English","publisher":"Bureau of Sport Fisheries and Wildlife","publisherLocation":"Washington, D.C.","usgsCitation":"Hotchkiss, N., 1970, Common marsh plants of the United States and Canada: Resource Publication 93, v, 99 p.","productDescription":"v, 99 p.","numberOfPages":"106","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":289882,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":289881,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/rp/0093/report.pdf"}],"country":"Canada;United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173.0,16.916667 ], [ 173.0,83.1 ], [ -52.6,83.1 ], [ -52.6,16.916667 ], [ 173.0,16.916667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae5da","contributors":{"authors":[{"text":"Hotchkiss, Neil","contributorId":93544,"corporation":false,"usgs":true,"family":"Hotchkiss","given":"Neil","email":"","affiliations":[],"preferred":false,"id":217673,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}