No abstract available.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp508","usgsCitation":"Balsley, J.R., and Bromery, R.W., 1965, Aeromagnetic map of part of the Lowville quadrangle, Lewis County, New York: U.S. Geological Survey Geophysical Investigations Map 508, 1 Plate: 18.40 x 22.36 inches, https://doi.org/10.3133/gp508.","productDescription":"1 Plate: 18.40 x 22.36 inches","costCenters":[],"links":[{"id":254279,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0508/report-thumb.jpg"},{"id":250807,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0508/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250806,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0508/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":485083,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3459.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"62500","country":"United States","state":"New York","county":"Lewis County","otherGeospatial":"Lowville quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -75.5,\n 44\n ],\n [\n -75.5,\n 43.75\n ],\n [\n -75.25,\n 43.75\n ],\n [\n -75.25,\n 44\n ],\n [\n -75.5,\n 44\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697986","contributors":{"authors":[{"text":"Balsley, James R.","contributorId":10010,"corporation":false,"usgs":true,"family":"Balsley","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":270289,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bromery, R. W.","contributorId":11676,"corporation":false,"usgs":true,"family":"Bromery","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":270290,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3038,"text":"wsp1610C - 1965 - Waterpower resources in Nehalem River basin, Oregon","interactions":[{"subject":{"id":16685,"text":"ofr59131 - 1959 - Waterpower resources in Nehalem River basin, Oregon, with geology of dam and reservoir sites","indexId":"ofr59131","publicationYear":"1959","noYear":false,"title":"Waterpower resources in Nehalem River basin, Oregon, with geology of dam and reservoir sites"},"predicate":"SUPERSEDED_BY","object":{"id":3038,"text":"wsp1610C - 1965 - Waterpower resources in Nehalem River basin, Oregon","indexId":"wsp1610C","publicationYear":"1965","noYear":false,"chapter":"C","title":"Waterpower resources in Nehalem River basin, Oregon"},"id":1}],"lastModifiedDate":"2023-01-03T22:05:42.967225","indexId":"wsp1610C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1610","chapter":"C","title":"Waterpower resources in Nehalem River basin, Oregon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1610C","usgsCitation":"Young, L.L., Colbert, J.L., Gaskill, D.L., and Piper, A., 1965, Waterpower resources in Nehalem River basin, Oregon: U.S. Geological Survey Water Supply Paper 1610, Report: v, 58 p.; 4 Plates: 26.00 x 19.77 inches or smaller, https://doi.org/10.3133/wsp1610C.","productDescription":"Report: v, 58 p.; 4 Plates: 26.00 x 19.77 inches or smaller","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":411302,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24799.htm","linkFileType":{"id":5,"text":"html"}},{"id":29879,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1610c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29878,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1610c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29881,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1610c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29880,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1610c/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29877,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1610c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139299,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1610c/report-thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Nehalem River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -123.81382726717416,\n 46.09485688632233\n ],\n [\n -123.81382726717416,\n 45.71849428512374\n ],\n [\n -123.041131977578,\n 45.71849428512374\n ],\n [\n -123.041131977578,\n 46.09485688632233\n ],\n [\n -123.81382726717416,\n 46.09485688632233\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485aa","contributors":{"authors":[{"text":"Young, Loyd L.","contributorId":14805,"corporation":false,"usgs":true,"family":"Young","given":"Loyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colbert, Jesse Lane","contributorId":9239,"corporation":false,"usgs":true,"family":"Colbert","given":"Jesse","email":"","middleInitial":"Lane","affiliations":[],"preferred":false,"id":146191,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gaskill, David L.","contributorId":53369,"corporation":false,"usgs":true,"family":"Gaskill","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146193,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Piper, Arthur M.","contributorId":65060,"corporation":false,"usgs":true,"family":"Piper","given":"Arthur M.","affiliations":[],"preferred":false,"id":146194,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":2626,"text":"wsp1810 - 1965 - Summary of floods in the United States during 1961","interactions":[],"lastModifiedDate":"2017-09-06T16:28:04","indexId":"wsp1810","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1810","title":"Summary of floods in the United States during 1961","docAbstract":"This report describes the most outstanding floods in the United States during 1961. The most damaging floods during the year were those caused by snowmelt in March and April in the upper Mississippi River basin and those accompanying Hurricane Carla in September.
Hurricane Carla traveled northward along the east edge of Texas and then northeastward through southeastern Oklahoma, northwestern Arkansas, southeastern Missouri, and central Illinois. Heavy rains and floods occurred east of the hurricane's path in Texas and west of its path for the remainder of its journey.
Mississippi, Alabama, and Georgia had moderate to severe floods in February and March from a series of large-area rainstorms. Many maximum peak discharges occurred, and streams remained at high stages for periods longer than any known before. Property damage was high and four lives were lost.
Extensive flooding took place in May from southeastern Kansas and northeastern Oklahoma through northern Arkansas, southern Missouri, northern Kentucky, and the southern parts of Illinois, Indiana, and Ohio. Maximum discharges occurred at many sites throughout the area.
Heavy flooding was experienced on Kootenai River at Bonners Ferry, Idaho, in May and June. These floods were noteworthy for their duration.
The most tragic flood of the year was in July in Charleston, W. Va. A small area cloudburst flood caused 22 deaths and damage of more than \\$1 million.
Severe flooding occurred in December in the Tombigbee River, Pearl River, and Pascagoula River basins in Mississippi, Louisiana, and Alabama. Much damage resulted, and from two to three thousand persons were evacuated from large flooded areas.
In addition to the floods mentioned above, 19 others of lesser magnitude are considered important enough to be included in this annual summary.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1809Q","usgsCitation":"Sever, C.W., 1965, Ground-water resources and geology of Seminole, Decatur, and Grady Counties, Georgia: U.S. Geological Survey Water Supply Paper 1809, Report: iv, 30 p.; 2 Plates: 35.50 × 22.50 inches and 18.00 × 25.00 inches, https://doi.org/10.3133/wsp1809Q.","productDescription":"Report: iv, 30 p.; 2 Plates: 35.50 × 22.50 inches and 18.00 × 25.00 inches","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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Charles W.","contributorId":102056,"corporation":false,"usgs":true,"family":"Sever","given":"Charles","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145596,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2169,"text":"wsp1644 - 1965 - Quality of surface waters of the United States, 1959, Parts 7 & 8, lower Mississippi River Basin and western Gulf of Mexico Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1644","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1644","title":"Quality of surface waters of the United States, 1959, Parts 7 & 8, lower Mississippi River Basin and western Gulf of Mexico Basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1644","usgsCitation":"Love, S.K., 1965, Quality of surface waters of the United States, 1959, Parts 7 & 8, lower Mississippi River Basin and western Gulf of Mexico Basins: U.S. Geological Survey Water Supply Paper 1644, xi, 508 p. :ill. ;25 cm., https://doi.org/10.3133/wsp1644.","productDescription":"xi, 508 p. :ill. ;25 cm.","costCenters":[],"links":[{"id":138307,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1644/report-thumb.jpg"},{"id":27780,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1644/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651c04","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144764,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2537,"text":"wsp1662B - 1965 - Specific yield - laboratory experiments showing the effect of time on column drainage","interactions":[],"lastModifiedDate":"2018-06-13T11:36:21","indexId":"wsp1662B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1662","chapter":"B","title":"Specific yield - laboratory experiments showing the effect of time on column drainage","docAbstract":"The increasing use of ground water from many major aquifers in the United States has required a more thorough understanding of gravity drainage, or specific yield. This report describes one phase of specific yield research by the U.S. Geological Survey's Hydrologic Laboratory in cooperation with the California Department of Water Resources.
An earlier phase of the research concentrated on the final distribution of moisture retained after drainage of saturated columns of porous media. This report presents the phase that concentrated on the distribution of moisture retained in similar columns after drainage for various periods of time.
Five columns, about 4 cm in diameter by 170 cm long, were packed with homogenous sand of very fine, medium, and coarse sizes, and one column was packed with alternating layers of coarse and medium sand. The very fine materials were more uniform in size range than were the medium materials. As the saturated columns drained, tensiometers installed throughout the length recorded changes in moisture tension. The relation of tension to moisture content, determined for each of the materials, was then used to convert the tension readings to moisture content. Data were then available on the distribution of retained moisture for different periods of drainage from 1 to 148 hours. Data also are presented on the final distribution of moisture content by weight and volume and on the degree of saturation.
The final zone of capillary saturation was approximately 12 cm for coarse sand, 13 cm for medium sand, and 52 cm for very fine sand. The data showed these zones were 92 to 100 percent saturated.
Most of the outflow from the columns occurred in the earlier hours of drainage--90 percent in 1 hour for the coarse materials, 50 percent for the medium, and 60 percent for the very fine. Although the largest percentage of the specific yield was reached during the early hours of drainage, this study amply demonstrates that a very long time would be required to reach drainage equilibrium.
In the layered columns the middle (medium sand) layer functioned as a hanging water column accelerating the drainage of the overlying coarse-sand layer. After the middle layer started to drain, the moisture distribution as retained in all three layers showed trends similar to that obtained when the same materials were tested in homogenous columns.
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1662B","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Prill, R.C., Johnson, A., and Morris, D.A., 1965, Specific yield - laboratory experiments showing the effect of time on column drainage: U.S. Geological Survey Water Supply Paper 1662, iv, 55 p., https://doi.org/10.3133/wsp1662B.","productDescription":"iv, 55 p.","costCenters":[],"links":[{"id":138581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1662b/report-thumb.jpg"},{"id":28778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1662b/report.pdf","text":"Report","size":"1.51 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64853b","contributors":{"authors":[{"text":"Prill, Robert C.","contributorId":86317,"corporation":false,"usgs":true,"family":"Prill","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":145365,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morris, Donald Arthur","contributorId":13960,"corporation":false,"usgs":true,"family":"Morris","given":"Donald","email":"","middleInitial":"Arthur","affiliations":[],"preferred":false,"id":145364,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3039,"text":"wsp1787 - 1965 - Ground-water conditions and storage in the Central Sevier Valley, Utah","interactions":[{"subject":{"id":52149,"text":"ofr60161 - 1960 - Ground-water areas and well logs, Central Sevier Valley, Utah","indexId":"ofr60161","publicationYear":"1960","noYear":false,"title":"Ground-water areas and well logs, Central Sevier Valley, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3039,"text":"wsp1787 - 1965 - Ground-water conditions and storage in the Central Sevier Valley, Utah","indexId":"wsp1787","publicationYear":"1965","noYear":false,"title":"Ground-water conditions and storage in the Central Sevier Valley, Utah"},"id":1},{"subject":{"id":52226,"text":"ofr6226 - 1962 - Records of selected wells and springs, chemical analyses of ground water, water-level measurements of selected wells, selected drillers' logs of wells, and logs of test holes, Central Sevier Valley, Sanpete, Sevier, and Piute Counties, Utah","indexId":"ofr6226","publicationYear":"1962","noYear":false,"title":"Records of selected wells and springs, chemical analyses of ground water, water-level measurements of selected wells, selected drillers' logs of wells, and logs of test holes, Central Sevier Valley, Sanpete, Sevier, and Piute Counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3039,"text":"wsp1787 - 1965 - Ground-water conditions and storage in the Central Sevier Valley, Utah","indexId":"wsp1787","publicationYear":"1965","noYear":false,"title":"Ground-water conditions and storage in the Central Sevier Valley, Utah"},"id":2},{"subject":{"id":52308,"text":"ofr6314 - 1963 - Records of selected wells and springs, chemical analyses of ground water, water-level measurements of selected wells, selected drillers' logs of wells, and logs of test holes, Central Sevier Valley, Sanpete, Sevier, and Piute Counties, Utah","indexId":"ofr6314","publicationYear":"1963","noYear":false,"title":"Records of selected wells and springs, chemical analyses of ground water, water-level measurements of selected wells, selected drillers' logs of wells, and logs of test holes, Central Sevier Valley, Sanpete, Sevier, and Piute Counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3039,"text":"wsp1787 - 1965 - Ground-water conditions and storage in the Central Sevier Valley, Utah","indexId":"wsp1787","publicationYear":"1965","noYear":false,"title":"Ground-water conditions and storage in the Central Sevier Valley, Utah"},"id":3}],"lastModifiedDate":"2017-09-06T16:06:56","indexId":"wsp1787","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1787","title":"Ground-water conditions and storage in the Central Sevier Valley, Utah","docAbstract":"The central Sevier Valley, in the central part of Utah, extends from the town of Kingston to the Yuba Dam and from the Tushar and Valley Mountains and the Pavant Range to the Sevier, Fishlake, Wasatch, and Gunnison Plateaus. A geologic and hydrologic investigation of the valley was made to determine the relation between surface water and ground water and to determine if ground water can be used for irrigation supplies without affecting existing water uses. During the investigation, data were collected for about 700 wells and 26 springs. Monthly water-level measurements were made at 93 observation wells, and automatic recording gages were maintained at 6 additional wells. Chemical analyses were made of water collected from 68 wells and springs. Test holes were drilled at 21 sites to determine the thickness and hydrologic properties of the waterbearing materials. Consumption of ground water by vegetation was estimated on the basis of area and applied rates of evapotranspiration.
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The mesa is about 9.5 square miles in area and reaches a maximum altitude of 7,679 feet. The mesa is underlain by welded tuff, friable-bedded tuff, and zeolitized-bedded tuff of the Piapi Canyon Group and the Indian Trail Formation of Tertiary age. The tuff--2,000 to 9,000 feet thick--rests unconformably upon thrust-faulted miogeosynclinal rocks of Paleozoic age. \r\n\r\nZeolitic-bedded tuff at the base of the tuff sequence controls the recharge rate of ground water to the underlying and more permeable Paleozoic aquifers. The zeolitic tuff--600 to 800 feet thick--is a fractured aquitard with high interstitial porosity, but with very low interstitial permeability and fracture transmissibility. The interstitial porosity ranges from 29 to 38 percent, the interstitial permeability is generally less than 0.009 gpd/ft3, and the fracture transmissibility ranges from 10 to 100 gpd/ft for 900 feet of saturated rock. The tuff is generally fully saturated interstitially hundreds of feet above the regional water table, yet no appreciable volume of water moves through the interstices because of the very low permeability. The only freely moving water observed in miles of underground workings occurred in fractures, usually fault zones.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr66130","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Thordarson, W., 1965, Perched Ground Water in Zeolitized-Bedded Tuff, Rainier Mesa and Vicinity, Nevada Test Site, Nevada: U.S. Geological Survey Open-File Report 66-130, 94 p., https://doi.org/10.3133/ofr66130.","productDescription":"94 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":173079,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0130/report-thumb.jpg"},{"id":80723,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0130/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80724,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0130/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80725,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0130/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80726,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0130/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68859a","contributors":{"authors":[{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":227412,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32725,"text":"pp456B - 1965 - Diabase sheets of the Taylor Glacier region, Victoria Land, Antarctica, with sections on petrography and sections on chemistry","interactions":[],"lastModifiedDate":"2012-02-02T00:09:09","indexId":"pp456B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"456","chapter":"B","title":"Diabase sheets of the Taylor Glacier region, Victoria Land, Antarctica, with sections on petrography and sections on chemistry","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the geology of Antarctica","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp456B","usgsCitation":"Hamilton, W., Hayes, P.T., Calvert, R., Smith, V.C., Elmore, P., Barnett, P., and Conklin, N., 1965, Diabase sheets of the Taylor Glacier region, Victoria Land, Antarctica, with sections on petrography and sections on chemistry: U.S. Geological Survey Professional Paper 456, p. 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1965 - Bedrock geologic map of the Milford quadrangle, Fairfield and New Haven Counties, Connecticut","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq427","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"427","title":"Bedrock geologic map of the Milford quadrangle, Fairfield and New Haven Counties, Connecticut","language":"ENGLISH","doi":"10.3133/gq427","usgsCitation":"Fritts, C., 1965, Bedrock geologic map of the Milford quadrangle, Fairfield and New Haven Counties, Connecticut: U.S. Geological Survey Geologic Quadrangle 427, 1 map., https://doi.org/10.3133/gq427.","productDescription":"1 map.","costCenters":[],"links":[{"id":102447,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_896.htm","linkFileType":{"id":5,"text":"html"},"description":"896"},{"id":249159,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0427/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":252160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0427/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.11749999999999,41.1175 ], [ -73.11749999999999,41.25 ], [ -73,41.25 ], [ -73,41.1175 ], [ -73.11749999999999,41.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db6362fe","contributors":{"authors":[{"text":"Fritts, Crawford E.","contributorId":87619,"corporation":false,"usgs":true,"family":"Fritts","given":"Crawford E.","affiliations":[],"preferred":false,"id":268216,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}