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No abstract available. 

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No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7324","usgsCitation":"Showen, C.R., and Williams, O.O., 1973, Index to water-quality data available from the U.S. Geological Survey in machine-readable form to December 31, 1972: Western region: U.S. Geological Survey Water-Resources Investigations Report 73-24, iii, 516 p. , https://doi.org/10.3133/wri7324.","productDescription":"iii, 516 p. ","costCenters":[],"links":[{"id":365503,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0024/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159789,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0024/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f2500","contributors":{"authors":[{"text":"Showen, Charles R.","contributorId":105717,"corporation":false,"usgs":true,"family":"Showen","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202009,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Owen O.","contributorId":108097,"corporation":false,"usgs":true,"family":"Williams","given":"Owen","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":202010,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29719,"text":"wri7321 - 1973 - Index to water-quality data available from the U.S. Geological Survey in machine-readable form to December 31, 1972; Northeastern region","interactions":[],"lastModifiedDate":"2023-01-23T21:27:15.010833","indexId":"wri7321","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-21","title":"Index to water-quality data available from the U.S. Geological Survey in machine-readable form to December 31, 1972; Northeastern region","docAbstract":"

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No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7325","usgsCitation":"Showen, C.R., and Stuthmann, N.G., 1973, Index to U.S. Geological Survey computer files containing daily values for water parameters to September 30, 1971 Northeastern region: U.S. Geological Survey Water-Resources Investigations Report 73-25, iii, 352 p., https://doi.org/10.3133/wri7325.","productDescription":"iii, 352 p.","costCenters":[],"links":[{"id":365566,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0025/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0025/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f2582","contributors":{"authors":[{"text":"Showen, Charles R.","contributorId":105717,"corporation":false,"usgs":true,"family":"Showen","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuthmann, Neil G.","contributorId":95106,"corporation":false,"usgs":true,"family":"Stuthmann","given":"Neil","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":202003,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29716,"text":"wri7322 - 1973 - Index to water-quality data available from the U.S. Geological Survey in machine-readable form to December 31, 1972: Southeastern Region","interactions":[],"lastModifiedDate":"2020-08-12T19:21:54.007024","indexId":"wri7322","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-22","title":"Index to water-quality data available from the U.S. Geological Survey in machine-readable form to December 31, 1972: Southeastern Region","docAbstract":"

This report lists water quality stations operated by the Geological Survey for what data are available in machine-readable form. The data are the results of analyses of water samples and indicate the chemical and physical characteristics of surface and ground water. The stations are listed according to station number within each State. The water quality data are identified by 5-digit parameter codes and are grouped into twenty-one parameter categories. The analytical results for all samples in any one year are then grouped within the parameter categories. The report lists the available retrieval options, the machine-readable output options user charges, and how to obtain the data.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7322","collaboration":"This index has been prepared as part of the cataloging activities of the Resources and Land Information Program (RALI)","usgsCitation":"Showen, C.R., and Williams, O.O., 1973, Index to water-quality data available from the U.S. Geological Survey in machine-readable form to December 31, 1972: Southeastern Region: U.S. Geological Survey Water-Resources Investigations Report 73-22, iii, 757 p., https://doi.org/10.3133/wri7322.","productDescription":"iii, 757 p.","costCenters":[],"links":[{"id":377419,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0022/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0022/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f24cd","contributors":{"authors":[{"text":"Showen, Charles R.","contributorId":105717,"corporation":false,"usgs":true,"family":"Showen","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Owen O.","contributorId":108097,"corporation":false,"usgs":true,"family":"Williams","given":"Owen","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":202002,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30326,"text":"wri7343 - 1973 - Flood of July 17, 1972 in Gallup, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri7343","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-43","title":"Flood of July 17, 1972 in Gallup, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division],","doi":"10.3133/wri7343","usgsCitation":"Waite, L.A., 1973, Flood of July 17, 1972 in Gallup, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 73-43, iv, 8 p. :maps ;27 cm., https://doi.org/10.3133/wri7343.","productDescription":"iv, 8 p. :maps ;27 cm.","costCenters":[],"links":[{"id":247338,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0043/report.pdf","size":"572","linkFileType":{"id":1,"text":"pdf"}},{"id":251806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0043/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eef2a","contributors":{"authors":[{"text":"Waite, Loyd A.","contributorId":79914,"corporation":false,"usgs":true,"family":"Waite","given":"Loyd","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":203062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29715,"text":"wri7328 - 1973 - Index to U.S. Geological Survey computer files containing daily values for water parameters to September 30, 1971: Western Region","interactions":[],"lastModifiedDate":"2019-07-16T09:06:32","indexId":"wri7328","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-28","title":"Index to U.S. Geological Survey computer files containing daily values for water parameters to September 30, 1971: Western Region","docAbstract":"

No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7328","usgsCitation":"Showen, C.R., and Stuthmann, N.G., 1973, Index to U.S. Geological Survey computer files containing daily values for water parameters to September 30, 1971: Western Region: U.S. Geological Survey Water-Resources Investigations Report 73-28, iii, 387 p., https://doi.org/10.3133/wri7328.","productDescription":"iii, 387 p.","costCenters":[],"links":[{"id":365567,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0028/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0028/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f25d9","contributors":{"authors":[{"text":"Showen, Charles R.","contributorId":105717,"corporation":false,"usgs":true,"family":"Showen","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuthmann, Neil G.","contributorId":95106,"corporation":false,"usgs":true,"family":"Stuthmann","given":"Neil","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":201999,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30493,"text":"wri7332 - 1973 - Appraisal of the quality of ground water in the Helena Valley, Montana","interactions":[],"lastModifiedDate":"2019-07-16T08:56:18","indexId":"wri7332","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-32","title":"Appraisal of the quality of ground water in the Helena Valley, Montana","docAbstract":"

No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7332","usgsCitation":"Wilke, K., and Coffin, D.L., 1973, Appraisal of the quality of ground water in the Helena Valley, Montana: U.S. Geological Survey Water-Resources Investigations Report 73-32, Report: iii, 31 p.; 3 Plates: 16.44 x 15.57 inches or smaller, https://doi.org/10.3133/wri7332.","productDescription":"Report: iii, 31 p.; 3 Plates: 16.44 x 15.57 inches or smaller","costCenters":[{"id":400,"text":"Montana Water Science Center","active":false,"usgs":true}],"links":[{"id":160162,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0032/report-thumb.jpg"},{"id":365561,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1973/0032/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365562,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1973/0032/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365563,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1973/0032/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Helena Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.19238281249999,\n 46.521075663842865\n ],\n [\n -111.77490234375,\n 46.521075663842865\n ],\n [\n -111.77490234375,\n 46.7248003746672\n ],\n [\n -112.19238281249999,\n 46.7248003746672\n ],\n [\n -112.19238281249999,\n 46.521075663842865\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a352","contributors":{"authors":[{"text":"Wilke, K.R.","contributorId":60687,"corporation":false,"usgs":true,"family":"Wilke","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":203346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coffin, Donald L.","contributorId":90696,"corporation":false,"usgs":true,"family":"Coffin","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":203347,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29714,"text":"wri7326 - 1973 - Index to US Geological Survey computer files containing daily values for water parameters to September 30, 1971: Southeastern region","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri7326","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-26","title":"Index to US Geological Survey computer files containing daily values for water parameters to September 30, 1971: Southeastern region","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri7326","usgsCitation":"Showen, C.R., and Stuthmann, N.G., 1973, Index to US Geological Survey computer files containing daily values for water parameters to September 30, 1971: Southeastern region: U.S. Geological Survey Water-Resources Investigations Report 73-26, iii,206 p. :chiefly tables,map ;26 cm., https://doi.org/10.3133/wri7326.","productDescription":"iii,206 p. :chiefly tables,map ;26 cm.","costCenters":[],"links":[{"id":159777,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f25a2","contributors":{"authors":[{"text":"Showen, Charles R.","contributorId":105717,"corporation":false,"usgs":true,"family":"Showen","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":201998,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuthmann, Neil G.","contributorId":95106,"corporation":false,"usgs":true,"family":"Stuthmann","given":"Neil","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":201997,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29383,"text":"wri7319 - 1973 - Bolinas Lagoon, Marin County, California summary of sedimentation and hydrology, 1967-69","interactions":[],"lastModifiedDate":"2019-09-26T12:34:23","indexId":"wri7319","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-19","title":"Bolinas Lagoon, Marin County, California summary of sedimentation and hydrology, 1967-69","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7319","usgsCitation":"Ritter, J.R., and Brown, W.M., 1973, Bolinas Lagoon, Marin County, California summary of sedimentation and hydrology, 1967-69: U.S. Geological Survey Water-Resources Investigations Report 73-19, v, 74 p. , https://doi.org/10.3133/wri7319.","productDescription":"v, 74 p. 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John R.","contributorId":75508,"corporation":false,"usgs":true,"family":"Ritter","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":201442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, William M. III","contributorId":72365,"corporation":false,"usgs":true,"family":"Brown","given":"William","suffix":"III","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":201441,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":17559,"text":"ofr73191 - 1973 - Preliminary report on the geology along the Atlantic Continental margin of the northeastern United States","interactions":[{"subject":{"id":17559,"text":"ofr73191 - 1973 - Preliminary report on the geology along the Atlantic Continental margin of the northeastern United States","indexId":"ofr73191","publicationYear":"1973","noYear":false,"title":"Preliminary report on the geology along the Atlantic Continental margin of the northeastern United States"},"predicate":"SUPERSEDED_BY","object":{"id":70047583,"text":"70047583 - 1974 - Preliminary report on geology along Atlantic continental margin of northeastern United States","indexId":"70047583","publicationYear":"1974","noYear":false,"title":"Preliminary report on geology along Atlantic continental margin of northeastern United States"},"id":1}],"supersededBy":{"id":70047583,"text":"70047583 - 1974 - Preliminary report on geology along Atlantic continental margin of northeastern United States","indexId":"70047583","publicationYear":"1974","noYear":false,"title":"Preliminary report on geology along Atlantic continental margin of northeastern United States"},"lastModifiedDate":"2025-12-18T19:17:30.421311","indexId":"ofr73191","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-191","title":"Preliminary report on the geology along the Atlantic Continental margin of the northeastern United States","docAbstract":"

The U.S. Geological Survey is conducting a geological and geophysical study of the northeastern United States Outer Continental Shelf and the adjacent slope from Georges Bank to Cape Hatteras. The study also includes the adjacent Coastal Plain because it is a more accessible extension of the shelf. The total study area is about 324,000 sq km, of which the shelf and slope constitute about 181,000 sq km and the Coastal Plain constitutes 143,000 sq km. The shelf width ranges from about 30 km at Cape Hatteras to about 195 km off Raritan Bay and on Georges Bank. Analyses of bottom samples make it possible to construct a preliminary geologic map of the shelf and slope to a water depth of 2,000 m. The oldest beds cropping out in the submarine canyons and on the slope are of early Late Cretaceous age. Beds of Early Cretaceous and Jurassic age are present in deep wells onshore and probably are present beneath the shelf in the area of this study. Such beds are reported beneath the Scotian Shelf to the northeast where they include limestone, salt, and anhydrite. Preliminary conclusions suggest a considerably thicker Mesozoic sedimentary sequence than has been previously described. The region is large; the sedimentary wedge is thick; structures seem favorable, and the hydrocarbon potential may be considerable.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73191","usgsCitation":"Minard, J.P., Perry, W.J., Weed, E.G., Rhodehamel, E., Robbins, E.I., and Mixon, R.B., 1973, Preliminary report on the geology along the Atlantic Continental margin of the northeastern United States: U.S. Geological Survey Open-File Report 73-191, 34 p., https://doi.org/10.3133/ofr73191.","productDescription":"34 p.","costCenters":[],"links":[{"id":497686,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0191/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149906,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0191/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c91e","contributors":{"authors":[{"text":"Minard, James P.","contributorId":84761,"corporation":false,"usgs":true,"family":"Minard","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":176871,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perry, W. J. Jr.","contributorId":64266,"corporation":false,"usgs":true,"family":"Perry","given":"W.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":176870,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weed, Elaine G. A.","contributorId":91496,"corporation":false,"usgs":true,"family":"Weed","given":"Elaine","email":"","middleInitial":"G. A.","affiliations":[],"preferred":false,"id":176872,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rhodehamel, E. C.","contributorId":91517,"corporation":false,"usgs":true,"family":"Rhodehamel","given":"E. C.","affiliations":[],"preferred":false,"id":176873,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Robbins, E. I.","contributorId":101269,"corporation":false,"usgs":true,"family":"Robbins","given":"E.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":176874,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mixon, R. B.","contributorId":11235,"corporation":false,"usgs":true,"family":"Mixon","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":176869,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70120891,"text":"70120891 - 1973 - Interstitial water studies on small core samples, Deep Sea Drilling Project: Leg 10","interactions":[],"lastModifiedDate":"2019-12-16T14:33:13","indexId":"70120891","displayToPublicDate":"1975-01-01T11:39:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, Deep Sea Drilling Project: Leg 10","docAbstract":"

Leg 10 interstitial water analyses provide new indications of the distribution of rock salt beneath the floor of the Gulf of Mexico, both confirming areas previously indicated to be underlain by salt bodies and extending evidence of salt distribution to seismically featureless areas in the Sigsbee Knolls trend and Isthmian Embayment. The criterion for presence of salt at depth is a consistent increase in interstitial salinity and chlorinity with depth.

Site 86, on the northern margin of the Yucatan Platform, provided no evidence of salt at depth. Thus, our data tend to rule out the suggestion of Antoine and Bryant (1969) that the Sigsbee Knolls salt was squeezed out from beneath the Yucatan Scarp. Cores from Sites 90 and 91, in the central Sigsbee Deep, were not obtained from a great enough depth to yield definite evidence for the presence of buried salt.

Site 86, on the northern margin of the Yucatan Platform, provided no evidence of salt at depth. Thus, our data tend to rule out the suggestion of Antoine and Bryant (1969) that the Sigsbee Knolls salt was squeezed out from beneath the Yucatan Scarp. Cores from Sites 90 and 91, in the central Sigsbee Deep, were not obtained from a great enough depth to yield definite evidence for the presence of buried salt.

","language":"English","publisher":"Integrated Ocean Drilling Program Management International","publisherLocation":"College Station, TX","doi":"10.2973/dsdp.proc.10.121.1973","usgsCitation":"Manheim, F., Sayles, F.L., and Waterman, L.S., 1973, Interstitial water studies on small core samples, Deep Sea Drilling Project: Leg 10: Initial reports of the Deep Sea Drilling Project, v. 10, p. 615-623, https://doi.org/10.2973/dsdp.proc.10.121.1973.","productDescription":"9 p.","startPage":"615","endPage":"623","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488226,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/dsdp.proc.10.121.1973","text":"Publisher Index Page"},{"id":292419,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Gulf Of Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.86,18.18 ], [ -97.86,30.4 ], [ -81.04,30.4 ], [ -81.04,18.18 ], [ -97.86,18.18 ] ] ] } } ] }","volume":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fe7e4b0333418718930","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":45294,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank T.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":498570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sayles, Fred L.","contributorId":88279,"corporation":false,"usgs":true,"family":"Sayles","given":"Fred","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":498571,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waterman, Lee S.","contributorId":30151,"corporation":false,"usgs":true,"family":"Waterman","given":"Lee","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":498569,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70106983,"text":"70106983 - 1973 - Geology and water resources of the Wharton Tract and the Mullica River basin in southern New Jersey","interactions":[],"lastModifiedDate":"2015-10-17T19:24:16","indexId":"70106983","displayToPublicDate":"1975-01-01T10:47:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":135,"text":"Special Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"36","title":"Geology and water resources of the Wharton Tract and the Mullica River basin in southern New Jersey","docAbstract":"

The Wharton Tract is an area of 150 square miles located in the Mullica River basin in southern New Jersey's Pine Barrens region. The tract is a relatively flat, low-lying, generally sandy area containing shallowly incised streams. The larger streams are commonly bordered by swamps. The tract was purchased by the State primarily as a water-supply preserve, but also for conservation and recreational purposes.

\n

Mean streamflow at three continuous record gaging stations in the Wharton Tract is: Mullica River near Batsto (46.1-square mile drainage area), 6 mgd (million gallons per day); Batsto River at Batsto (70.5-square mile drainage area), 81 mgd; Oswego River at Harrisville (64.0-square mile drainage area), 55 mgd. Thus mean discharge from this 180.6-sq mi (square mile) area is 202 mgd or 1.12 mgd per sq mi.

\n

Principal aquifers in the Wharton Tract and Mullic River basin are in the Kirkwood Formation of middle Miocene age, Cohansey Sand of Miocene(?) and Pliocene(?) age, and in overlying hydraulically connected deposits of Quaternary age.

\n

The Kirkwood Formation is composed of sand, silt, and clay. Diverse lithologies represent deposition in different environments such as nearshore marine, barrier bar, lagoonal, estuarine, and tidal marsh. Hydraulic characteristics of the Kirkwood in the Mullica River basin are virtually unknown. Most Kirkwood aquifers in the basin are believed to be hydraulically connected with the overlying Cohansey Sand.

\n

The Cohansey Sand is dominantly a quartz sand containing minor amounts of pebbly sand, silty sand, and interbedded clay. Almost all of the Wharton Tract and most of the Mullica River basin lie within the sandier area of the Cohansey, which contains approximately 75 percent sand beds and 25 percent silt and clay beds. Data from test drilling show that the upper 100 feet of sediments in the Wharton Tract contain about 93 percent sand beds, 3.5 percent clay beds, and 3.5 percent silt beds. The Cohansey in the Tract ranges in thickness from less than 50 feet to about 180 feet; the average thickness is about 125 feet.

\n

The Cohansey Sand is believed to be, in overall aspect, a deltaic deposit. It contains materials that were deposited locally in nearshore-marine, fluvial, estuarine, lagoonal, and beach environments.

\n

The hydraulic conductivity of Cohansey aquifer material ranges from about 90 to 250 feet per day (660 to 1,885 gallons per day per square foot) in southern New Jersey. One aquifer test in the Wharton Tract gives an average value of 130 feet per day (1,000 gallons per day per square foot). The transmissivity of the Cohansey Sand aquifer through most of the Wharton Tract is typically between 10,000 and 20,000 square feet per day (75,000 and 150,000 gallons per day per foot).

\n

Deposits of Quaternary age form a discontinuous veneer lying unconformably above the Cohansey Sand. The most important hydrologic function of most of these deposits is to absorb precipitation and transmit the water to the underlying Cohansey Sand. Thicker deposits of estuarine sand and clay of the Cape May Formation fill a channel in the underlying Cohansey Sand along the lower reaches of the Mullica River. This channel deposit is 85 feet thick near Batsto.

\n

Ground water and surface water in the Mullica River basin are low in dissolved solids, generally less than 50 mg/1 (milligrams per liter). Iron concentrations are generally high, up to 49,000 micrograms per liter (49 mg/1) in ground water and up to 7,100 micrograms per liter (7.1 mg/1) in the streams. The water is acidic as indicated by typical pH values of from 4.5 to 6.5. Color of the surface water is commonly high, ranging from 3 - 150 platinum-cobalt units. After appropriate treatment these waters are acceptable for most uses.

\n

The Wharton Tract is well situated to support the growing water needs of nearby New Jersey communities. Maximum development of water can be achieved by conjunctive use of ground and surface water. During most of the year, some water would be withdrawn either directly from streams or from adjacent wells. During periods of low flow during summer or fall water would be pumped from wells farther from the stream~. From analysis of flow-duration curves it is estimated that 70 mgd of water could be developed with minimal effect upon low flows in the half of the tract above the gaging stations on the Mullica and Batsto Rivers. The quantity available in the entire tract is greater, possibly in the order of 150 mgd. With augmentation of streamflow by pumping from ground water, it is likely that considerably more water could be safely used on a perennial basis.

\n

A possibility exists for multiple use of the water resources of the Mullica River through construction of an inexpensive tide barrier at the Garden State Parkway. This would create a fresh water lake in a State forest, park, and recreational area, which would also provide a flexible and economical water supply for much of the Atlantic coastal resort development.

","language":"English","publisher":"State of New Jersey Department of Environmental Protection, Division of Water Resources","collaboration":"Prepared in cooperation with United States Department of the Interior Geological Survey","usgsCitation":"Rhodehamel, E.C., 1973, Geology and water resources of the Wharton Tract and the Mullica River basin in southern New Jersey: Special Report 36, 58 p.","productDescription":"58 p.","numberOfPages":"65","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":287918,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":287917,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70106983/report.pdf"}],"country":"United States","state":"New Jersey","otherGeospatial":"Mullica River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.7768,38.8517 ], [ -75.7768,40.7423 ], [ -73.8448,40.7423 ], [ -73.8448,38.8517 ], [ -75.7768,38.8517 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"537b27f4e4b0929ba496ab78","contributors":{"authors":[{"text":"Rhodehamel, Edward C.","contributorId":38135,"corporation":false,"usgs":true,"family":"Rhodehamel","given":"Edward","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":493827,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70107931,"text":"70107931 - 1973 - Sediment discharge in the Lake Tahoe basin, California, 1972 water year","interactions":[],"lastModifiedDate":"2014-06-11T09:39:44","indexId":"70107931","displayToPublicDate":"1974-01-01T11:15:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Sediment discharge in the Lake Tahoe basin, California, 1972 water year","docAbstract":"

Streamflow and fluvial-sediment discharge data are being collected at selected streams and highway gutters in the Lake Tahoe basin to determine the extent of erosion from highway cuts and to evaluate the effects of various land treatment practices to reduce erosion.

\n
\n

Precipitation in the Lake Tahoe area during 1972 was 77 percent of normal; consequently, runoff was well below normal. Seventy-six percent of the total annual runoff during the 1972 water year occurred from March through June 1972.

\n
\n

Sediment samples were collected during the year at streamflow gaging stations and at gutter stations at highway cuts to define the range of transport conditions. The major part (87 percent) of the annual suspended-sediment discharge during the 1972 water year occurred during the snowmelt runoff period, March through June.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/70107931","collaboration":"Prepared in cooperation with the California Department of Transportation Division of Highways","usgsCitation":"Kroll, C.G., 1973, Sediment discharge in the Lake Tahoe basin, California, 1972 water year, iv, 33 p., https://doi.org/10.3133/70107931.","productDescription":"iv, 33 p.","numberOfPages":"38","temporalStart":"1971-10-01","temporalEnd":"1972-09-30","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":288274,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70107931/report-thumb.jpg"},{"id":288273,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70107931/report.pdf"}],"country":"United States","state":"California","otherGeospatial":"Lake Tahoe","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.2862,38.6007 ], [ -120.2862,39.3786 ], [ -119.6624,39.3786 ], [ -119.6624,38.6007 ], [ -120.2862,38.6007 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"537dcb14e4b05ed6215c08b8","contributors":{"authors":[{"text":"Kroll, Carl G.","contributorId":72389,"corporation":false,"usgs":true,"family":"Kroll","given":"Carl","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":493937,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70038039,"text":"70038039 - 1973 - Hydrologic Data of the Neponset and Weymouth River Basins, Massachusetts","interactions":[],"lastModifiedDate":"2015-02-09T09:17:45","indexId":"70038039","displayToPublicDate":"1974-01-01T10:48:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":367,"text":"Massachusetts Hydrologic - Data Report","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"14","title":"Hydrologic Data of the Neponset and Weymouth River Basins, Massachusetts","docAbstract":"

The Neponset, Weymouth Fore, and Weymouth Back River basins occupy an area of 183 square miles in eastern Massachusetts south of Boston and Braintree, Brockton, Canton, Dedham, Dover, Foxborough, Hingham, Holbrook, Medfield, Milton, Norwood, Quincy, Randolph, Rockland, Sharon, Stoughton, Walpole, Westwood, and Weymouth.

\n

Hydrologic data presented in this report were collected during an investigation of the water resources in the areas of these basins that are upstream from tide effect or heavy urbanization. This investigation was conducted by the U.S. Geological Survey in cooperation with the Massachusetts Water Resources Commission. The data are released in order to make available to the public basic hydrologic and related information that will facilitate the planning of water-resources development and will complement an interpretive report, \"Hydrology and water resources of the Neoponset and Weymouth River basins, Massachusetts\" (HA-484).

\n

The well and boring data contained herein were selected from a larger group of data in order to minimize redundancy of information for intensely drilled areas. All of the data are on filed and available for inspection at the office of the U.S. Geological Survey, Water Resources Division, Boston, Massachusetts.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boston, Massachusetts","doi":"10.3133/70038039","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Water Resources Commission","usgsCitation":"Brackley, R., Fleck, W.B., and Willey, R.E., 1973, Hydrologic Data of the Neponset and Weymouth River Basins, Massachusetts: Massachusetts Hydrologic - Data Report 14, Report: 51 p.; Plate: 47.12 x 35.64 inches, https://doi.org/10.3133/70038039.","productDescription":"Report: 51 p.; Plate: 47.12 x 35.64 inches","numberOfPages":"56","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":264632,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038039/plate-1.pdf","size":"16.2 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":264633,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70038039/report.pdf","size":"4.3 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":264634,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70038039/report-thumb.jpg"}],"scale":"31680","country":"United States","state":"Massachusetts","otherGeospatial":"Neponset River, Weymouth River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.29852294921875,\n 42.06968462804663\n ],\n [\n -71.29852294921875,\n 42.35245491952619\n ],\n [\n -70.8837890625,\n 42.35245491952619\n ],\n [\n -70.8837890625,\n 42.06968462804663\n ],\n [\n -71.29852294921875,\n 42.06968462804663\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3510e4b0c8380cd5fc27","contributors":{"authors":[{"text":"Brackley, R. A.","contributorId":16851,"corporation":false,"usgs":true,"family":"Brackley","given":"R. A.","affiliations":[],"preferred":false,"id":463316,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleck, William B.","contributorId":17587,"corporation":false,"usgs":true,"family":"Fleck","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":463317,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Willey, Richard E.","contributorId":30972,"corporation":false,"usgs":true,"family":"Willey","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463318,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70174291,"text":"70174291 - 1973 - The benthic fauna of the Northern Bering Sea","interactions":[],"lastModifiedDate":"2016-07-08T09:44:40","indexId":"70174291","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"The benthic fauna of the Northern Bering Sea","docAbstract":"

The shelled benthic fauna of the northern Bering Sea has been extensively sampled and the taxonomy, distribution and functional role of 105 species of mollusks, two species of barnacles, two species of echinoids and one species of brachiopod havet4pen examined: The major benthic communities were evaluated by cluster analysis. They are:

\n
    \n
  1. the Balanus rostratus alaskensis community which inhabits cobble or gravel substrates;
    2. \n
  2. the Tellina lutea alternidentata community which is limited to areas of clean sand;
    3. \n
  3. the Clinocardium ciliatum community which is found on silty-sand substrates; and
    4. \n
  4. the Macoma balthica community which inhabits the brackish coastal lagoons.
    5. \n
\n

These associations were compared with the classic boreal benthic communities of Peterson & Thorson. Although the Bering Sea fauna is compositionally similar to the Scandinavian, the species associations differ markedly. These differences are believed to be due to substrate differences. The Bering Sea sediments are more poorly sorted and patchily distributed than those of Scandinavian waters.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70174291","usgsCitation":"Rowland, R.W., 1973, The benthic fauna of the Northern Bering Sea: Open-File Report, vi, 234 p., https://doi.org/10.3133/70174291.","productDescription":"vi, 234 p.","numberOfPages":"236","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":324811,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70174291.PNG"},{"id":324883,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70174291/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"577f7d33e4b0ef4d2f45facf","contributors":{"authors":[{"text":"Rowland, Robert W.","contributorId":42200,"corporation":false,"usgs":true,"family":"Rowland","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":641712,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207474,"text":"70207474 - 1973 - Interstitial water studies on small core samples, leg 19","interactions":[],"lastModifiedDate":"2019-12-19T18:10:35","indexId":"70207474","displayToPublicDate":"1973-12-31T18:05:09","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, leg 19","docAbstract":"

The sediments cored on Leg 19 consist primarily of diatomaceous oozes with variable proportions of volcanic material and terrigenous clays and silts. With a few exceptions, deposition rates are high at these sites, usually exceeding 5cm/103y. The interstitial solutions sampled exhibit compositional changes which previously have been found to characterize rapidly deposited terrigenous sediments. Some of the largest changes in Na+, K+, Mg2+, Cl-, and HCO3 yet found in DSDP samples occur in the pore waters studied from this leg (see Table 1).

","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.19.133.1973","usgsCitation":"Sayles, F., Waterman, L., and Manheim, F.T., 1973, Interstitial water studies on small core samples, leg 19: Initial reports of the Deep Sea Drilling Project, v. 19, p. 871-874, https://doi.org/10.2973/dsdp.proc.19.133.1973.","productDescription":"4 p.","startPage":"871","endPage":"874","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488853,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/dsdp.proc.19.133.1973","text":"Publisher Index Page"},{"id":370533,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sayles, F.L.","contributorId":77657,"corporation":false,"usgs":true,"family":"Sayles","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":778185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waterman, L.S.","contributorId":25474,"corporation":false,"usgs":true,"family":"Waterman","given":"L.S.","affiliations":[],"preferred":false,"id":778186,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":778187,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70207473,"text":"70207473 - 1973 - Interstitial water studies on small core samples, legs 16, 17, and 18","interactions":[],"lastModifiedDate":"2019-12-19T18:02:56","indexId":"70207473","displayToPublicDate":"1973-12-31T17:52:08","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, legs 16, 17, and 18","docAbstract":"

Legs 16, 17, and 18 encountered three groups of sediment types: rapidly deposited biogenic deposits, showing marked changes in interstitial calcium, magnesium, and strontium; slowly deposited biogenic deposits, showing little variability in pore fluids other than elevated silica concentrations; and terrigenous deposits. The latter showed the usual loss of sulfate and combination of diagenetic reactions culminating in loss of Na+ , K+ , Mg++, with variable changes in Ca++. Very high barium concentrations (to 59 mg/kg) occurred at Site 178 (Leg 18).

","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.18.app2.1973","usgsCitation":"Waterman, L., Sayles, F., and Manheim, F.T., 1973, Interstitial water studies on small core samples, legs 16, 17, and 18: Initial reports of the Deep Sea Drilling Project, v. 18, p. 1001-1012, https://doi.org/10.2973/dsdp.proc.18.app2.1973.","productDescription":"12 p.","startPage":"1001","endPage":"1012","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488844,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/dsdp.proc.18.app2.1973","text":"Publisher Index Page"},{"id":370532,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Waterman, L.S.","contributorId":25474,"corporation":false,"usgs":true,"family":"Waterman","given":"L.S.","affiliations":[],"preferred":false,"id":778182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sayles, F.L.","contributorId":77657,"corporation":false,"usgs":true,"family":"Sayles","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":778183,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":778184,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70206974,"text":"70206974 - 1973 - Phosphate in interstitial waters of anoxic sediments: Oxidation effects during sampling procedure","interactions":[],"lastModifiedDate":"2019-12-02T12:16:27","indexId":"70206974","displayToPublicDate":"1973-12-31T12:11:38","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Phosphate in interstitial waters of anoxic sediments: Oxidation effects during sampling procedure","docAbstract":"

Oxidation during sampling procedures significantly decreases the inorganic phosphate concentrations of interstitial water rich in iron (II). All sampling and analytical procedures must be carried out in an inert atmosphere. Orthophosphate in the interstitial water of Cheaspeake Bay sediments, in equilibrium with vivianite, is a potential nutrient source for the overlying water.

","language":"English","doi":"10.1126/science.180.4093.1362","issn":"00368075","usgsCitation":"Bray, J., Bricker, O., and Troup, B., 1973, Phosphate in interstitial waters of anoxic sediments: Oxidation effects during sampling procedure: Science, v. 180, no. 4093, p. 1362-1364, https://doi.org/10.1126/science.180.4093.1362.","productDescription":"3 p. ","startPage":"1362","endPage":"1364","costCenters":[],"links":[{"id":369806,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Chesapeake Bay ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.88232421875,\n 37.87051721701939\n ],\n [\n -75.56396484375,\n 37.87051721701939\n ],\n [\n -75.56396484375,\n 39.614152077002664\n ],\n [\n -76.88232421875,\n 39.614152077002664\n ],\n [\n -76.88232421875,\n 37.87051721701939\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"180","issue":"4093","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bray, J.T.","contributorId":220977,"corporation":false,"usgs":false,"family":"Bray","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":776433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bricker, O.P.","contributorId":33717,"corporation":false,"usgs":true,"family":"Bricker","given":"O.P.","affiliations":[],"preferred":false,"id":776434,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Troup, B.N.","contributorId":220976,"corporation":false,"usgs":false,"family":"Troup","given":"B.N.","email":"","affiliations":[],"preferred":false,"id":776435,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70156684,"text":"70156684 - 1973 - Notes on the bromine pentafluoride technique of oxygen extraction","interactions":[],"lastModifiedDate":"2015-08-25T17:34:01","indexId":"70156684","displayToPublicDate":"1973-12-28T19:45:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Notes on the bromine pentafluoride technique of oxygen extraction","docAbstract":"

The necessity to use a dry box when loading silicate samples into reaction vessels prior to fluorination is eliminated by the use of a simple loading technique. Data presented show the reproducibility of the fluorination reaction using this technique. Sodium fluoride, when added to saline waters prior to fluorination, improves the precision of the overall technique.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Friedman, I., and Gleason, J.D., 1973, Notes on the bromine pentafluoride technique of oxygen extraction: Journal of Research of the U.S. Geological Survey, v. 1, no. 6, p. 679-680.","productDescription":"2 p.","startPage":"679","endPage":"680","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307489,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307488,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1973/vol1issue6/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"volume":"1","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55dd91bce4b0518e354dd1a7","contributors":{"authors":[{"text":"Friedman, Irving","contributorId":90664,"corporation":false,"usgs":true,"family":"Friedman","given":"Irving","email":"","affiliations":[],"preferred":false,"id":569950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gleason, Jim D.","contributorId":82322,"corporation":false,"usgs":true,"family":"Gleason","given":"Jim","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":569951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70121273,"text":"70121273 - 1973 - Interstitial water studies on small core samples, Leg 15","interactions":[],"lastModifiedDate":"2019-12-16T14:46:47","indexId":"70121273","displayToPublicDate":"1973-12-01T14:16:24","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, Leg 15","docAbstract":"

Analyses of pore fluids from reducing environments demonstrate that reduction of SO4 is accompanied by large increases in alkalinity and strong depletion of Ca and Mg. The data are compatible with a model of replacement of Fe3+ in clay lattices by Mg from the interstitial solutions and the precipitation of pyrite. Depletions of Na in the interstitial solutions are related to Mg losses by a ratio of approximately 1:3. Pore fluids from oxidizing pelagic sediments exhibit little SO4 depletion. Losses of Mg are accompanied by the addition of Ca to the pore solutions on a nearly 1:1 basis. Strong Sr enrichment is also found in these solutions. The magnitude of the Sr increase suggests that considerable carbonate recrystallization has occurred.

\n
\n

As part of an extensive interlaboratory and analytical calibration, the effect of squeezing sediment at different temperatures has been studied in depth. Samples of a variety of lithologies have been included. Enrichment of K by as much as 24 percent and depletion of Mg and Ca by up to 7 percent occurs during warming. However, no significant effect upon Cl and SO4 could be detected. The strongest effects are seen in the minor constituents studied. On warming, Sr, Si, and B are enriched as much as 19, 40, and 60 percent, respectively. The size of the observed concentration changes varies with the mineralogy of the sediment, but is significant in all types studied, particularly with regards to Mg and K.

","language":"English","publisher":"Integrated Ocean Drilling Program Management International","publisherLocation":"College Station, TX","doi":"10.2973/dsdp.proc.20.207.1973","usgsCitation":"Sayles, F.L., Manheim, F., and Waterman, L.S., 1973, Interstitial water studies on small core samples, Leg 15: Initial reports of the Deep Sea Drilling Project, v. 15, p. 783-804, https://doi.org/10.2973/dsdp.proc.20.207.1973.","productDescription":"22 p.","startPage":"783","endPage":"804","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488220,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2973/dsdp.proc.20.207.1973","text":"Publisher Index Page"},{"id":292690,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Caribbean Sea","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.0,8.0 ], [ -82.0,20.0 ], [ -61.0,20.0 ], [ -61.0,8.0 ], [ -82.0,8.0 ] ] ] } } ] }","volume":"15","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f5b655e4b09d12e0e8e6e7","contributors":{"authors":[{"text":"Sayles, Fred L.","contributorId":88279,"corporation":false,"usgs":true,"family":"Sayles","given":"Fred","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":498904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":45294,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank T.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":498903,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waterman, Lee S.","contributorId":30151,"corporation":false,"usgs":true,"family":"Waterman","given":"Lee","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":498902,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70241488,"text":"70241488 - 1973 - Resistivity, self‐potential, and induced‐polarization surveys of a vapor‐dominated geothermal system","interactions":[],"lastModifiedDate":"2023-03-21T19:16:07.390216","indexId":"70241488","displayToPublicDate":"1973-12-01T14:07:13","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Resistivity, self‐potential, and induced‐polarization surveys of a vapor‐dominated geothermal system","docAbstract":"

The Mud Volcano area in Yellowstone National Park provides an example of a vapor‐dominated geothermal system. A test well drilled to a depth of about 347 ft penetrated the vapor‐dominated reservoir at a depth of less than 300 ft. Subsequently, 16 vertical electrical soundings (VES) of the Schlumberger type were made along a 3.7‐mile traverse to evaluate the electrical resistivity distribution within this geothermal field. Interpretation of the VES curves by computer modeling indicates that the vapor‐dominated layer has a resistivity of about 75–130 ohm‐m and that its lateral extent is about 1 mile. It is characteristically overlain by a low‐resistivity layer of about 2–6.5 ohm‐m, and it is laterally confined by a layer of about 30 ohm‐m. This 30‐ohm‐m layer, which probably represents hot water circulating in low‐porosity rocks, also underlies most of the survey at an average depth of about 1000 ft. Horizontal resistivity profiles, measured with two electrode spacings of an AMN array, qualitatively corroborate the sounding interpretation. The profiling data delineate the southeast boundary of the geothermal field as a distinct transition from low to high apparent resistivities. The northwest boundary is less distinctly defined because of the presence of thick lake deposits of low resistivities. A broad positive self‐potential anomaly is observed over the geothermal field, and it is interpretable in terms of the circulation of the thermal waters. Induced‐polarization anomalies were obtained at the northwest boundary and near the southeast boundary of the vapor‐dominated field. These anomalies probably are caused by relatively high concentrations of pyrite.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.1190/1.1440400","usgsCitation":"Zohdy, A., Anderson, L.A., and Muffler, L.P., 1973, Resistivity, self‐potential, and induced‐polarization surveys of a vapor‐dominated geothermal system: Geophysics, v. 38, no. 6, p. 1130-1144, https://doi.org/10.1190/1.1440400.","productDescription":"15 p.","startPage":"1130","endPage":"1144","costCenters":[],"links":[{"id":414486,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Mud Volcano, Yellowstone National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -110.60905607728807,\n 44.706407927367536\n ],\n [\n -110.60905607728807,\n 44.57802847588391\n ],\n [\n -110.29948543173212,\n 44.57802847588391\n ],\n [\n -110.29948543173212,\n 44.706407927367536\n ],\n [\n -110.60905607728807,\n 44.706407927367536\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"38","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zohdy, A.A.R.","contributorId":43503,"corporation":false,"usgs":true,"family":"Zohdy","given":"A.A.R.","affiliations":[],"preferred":false,"id":867002,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, L. A.","contributorId":22763,"corporation":false,"usgs":true,"family":"Anderson","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":867003,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Muffler, L.J. Patrick 0000-0001-6638-7218 pmuffler@usgs.gov","orcid":"https://orcid.org/0000-0001-6638-7218","contributorId":3322,"corporation":false,"usgs":true,"family":"Muffler","given":"L.J.","email":"pmuffler@usgs.gov","middleInitial":"Patrick","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":867004,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70241868,"text":"70241868 - 1973 - Geologic factors affecting compaction of deposits in a land-subsidence area","interactions":[],"lastModifiedDate":"2023-03-29T13:52:19.535178","indexId":"70241868","displayToPublicDate":"1973-12-01T08:47:29","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geologic factors affecting compaction of deposits in a land-subsidence area","docAbstract":"

In the west-central San Joaquin Valley, California, pumping of ground water has changed water levels, thereby increasing the stresses that tend to compact alluvium by as much as 50 percent and creating a large area of intense land subsidence.

The estimated 1943–1960 specific unit compaction (compaction during a time period, per unit thickness, per unit applied-stress increase) of the deposits in a northern subarea is four times that of a southern subarea, which suggests marked differences in the compressibility of the deposits. A third of the compressibility difference is real and is due to less prior total applied stress in the northern than in the southern subarea.

The other two-thirds of the compressibility difference is only apparent and is attributed to different water-expulsion rates in the clayey beds of different depositional environments. In the northern subarea, the deposits are mainly flood-plain sediments that contain extensive sand beds and thin clayey beds that are dewatered relatively quickly under increasing effective stress. In the southern subarea, the sediments are mainly alluvial-fan deposits that contain thick clayey sequences adjacent to lensing sandy beds. These deposits are de-watered more slowly than those in the northern subarea.

Variations of mean lithology in the chief compacting zone could not be correlated with variations in the specific unit compaction of the deposits.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1973)84<3783:GFACOD>2.0.CO;2","usgsCitation":"Bull, W.B., 1973, Geologic factors affecting compaction of deposits in a land-subsidence area: Geological Society of America Bulletin, v. 84, no. 12, p. 3783-3802, https://doi.org/10.1130/0016-7606(1973)84<3783:GFACOD>2.0.CO;2.","productDescription":"20 p.","startPage":"3783","endPage":"3802","costCenters":[],"links":[{"id":414895,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.35746288036006,\n 38.13312825895784\n ],\n [\n -120.53105995747384,\n 38.256520706440995\n ],\n [\n -121.70181326512369,\n 37.802004789813125\n ],\n [\n -121.50865485274531,\n 37.556878251392675\n ],\n [\n -120.58094260405235,\n 36.354060008522765\n ],\n [\n -120.24252200430453,\n 35.65038148239793\n ],\n [\n -119.51694986254691,\n 34.94145470111849\n ],\n [\n -118.77718624215447,\n 34.88440116587513\n ],\n [\n -118.47954946198888,\n 35.513980851524835\n ],\n [\n -118.78601558017306,\n 36.40932502176584\n ],\n [\n -119.48617719748387,\n 37.205195140576066\n ],\n [\n -120.35746288036006,\n 38.13312825895784\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"84","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bull, William B.","contributorId":8919,"corporation":false,"usgs":true,"family":"Bull","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":868015,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70241797,"text":"70241797 - 1973 - What about ground water?","interactions":[],"lastModifiedDate":"2023-03-27T19:05:53.425851","indexId":"70241797","displayToPublicDate":"1973-11-01T13:58:25","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"What about ground water?","docAbstract":"

No abstract available.

","language":"English","publisher":"The Groundwater Association","doi":"10.1111/j.1745-6584.1973.tb02992.x","usgsCitation":"Heath, R., 1973, What about ground water?: Groundwater, v. 11, no. 6, p. 50-51, https://doi.org/10.1111/j.1745-6584.1973.tb02992.x.","productDescription":"2 p.","startPage":"50","endPage":"51","costCenters":[],"links":[{"id":414783,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North 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