{"pageNumber":"6506","pageRowStart":"162625","pageSize":"25","recordCount":184904,"records":[{"id":67930,"text":"ha300 - 1968 - Availability of ground water in the northern part, Tenmile and Taunton River basins, southeastern Massachusetts","interactions":[],"lastModifiedDate":"2021-11-16T19:19:06.170274","indexId":"ha300","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"300","title":"Availability of ground water in the northern part, Tenmile and Taunton River basins, southeastern Massachusetts","docAbstract":"<p>The northern part of the Tenmile and Taunton River basins occupies an area of about 195 square miles. It includes some of the rapidly growing suburbs of Boston, Attleboro, and Brockton and lies along major highways connecting Boston with Fall River and Providence, Rhode Island. (See location map.)</p>\n<p>The purpose of this report is to delineate the extent of and to estimate the annual sustained yield and pumpage of the principal aquifers that are suitable for exploration for high-yielding wells to meet the needs of municipal water systems and industry. Lesser aquifers providing water for industrial, commercial, domestic, and some municipal supplies are also outlined.</p>\n<p>This report is based on geologic mapping, records of about 2,200 wells and test borings, seismic records, and discussion of water problems with municipal and corporate officials, drillers, and consulting engineers. Selected test borings and wells, including most municipal and industrial&nbsp; wells, are located on the map. They indicate areas from which water is pumped, saturated thickness and texture of materials, yield of wells, and areas in which exploratory work has already been done. Additional subsurface data are listed in a separate report (Williams and Willey, 1967).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha300","usgsCitation":"Williams, J.R., 1968, Availability of ground water in the northern part, Tenmile and Taunton River basins, southeastern Massachusetts: U.S. Geological Survey Hydrologic Atlas 300, 1 Plate: 42.87 x 40.50 inches, https://doi.org/10.3133/ha300.","productDescription":"1 Plate: 42.87 x 40.50 inches","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":187695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha300.JPG"},{"id":391754,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15672.htm"},{"id":89129,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/300/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"scale":"31680","country":"United States","state":"Massachusetts","otherGeospatial":"Taunton River, Ten Mile River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.36749999999999,41.8675 ], [ -71.36749999999999,42.1175 ], [ -71,42.1175 ], [ -71,41.8675 ], [ -71.36749999999999,41.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8bb","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":277345,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68128,"text":"ha278 - 1968 - Water resources of the Mississippi Headwaters Watershed, North-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T10:41:10","indexId":"ha278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"278","title":"Water resources of the Mississippi Headwaters Watershed, North-central Minnesota","docAbstract":"<p>The Mississippi Headwaters watershed is a 7,608 square mile area in north-central Minnesota which includes all land drained by the Mississippi River above the Crow Wing River.</p>\n<p>From its source in Lake Itasca, 1,460 feet above mean sea level, the Mississippi River follows a semicircular 376 mile course to where it leaves the watershed at an altitude of 1,150 feet. The origin of the river is in glacial moraine. The river flows through end moraines and rolling till plains, across an extensive outwash plain occupied by large reservoir lakes, and finally across an extensive marshy plain which is the bed of an ancient glacial lake.</p>\n<p>Glacial deposits in the watershed include till, lenses of sand and gravel in till, outwash deposits of sand and gravel, and lake deposits of fine sand, silt, and clay. Beneath the glacial drift is an uneven surface of Precambrian bedrock. Bedrock consists of igneous intrusives and metamorphosed sedimentary formations.</p>\n<p>Water resources in the area are abundant. Lakes and streams occupy about 8 percent of the surface of the area. 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,{"id":67358,"text":"i534D - 1968 - Transcontinental geophysical survey (35°-39° N) seismic refraction profiles of the crust and upper mantle from 87° to 100° W longitude","interactions":[],"lastModifiedDate":"2021-10-21T16:09:00.311508","indexId":"i534D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"534","chapter":"D","title":"Transcontinental geophysical survey (35°-39° N) seismic refraction profiles of the crust and upper mantle from 87° to 100° W longitude","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i534D","usgsCitation":"Warren, D.H., 1968, Transcontinental geophysical survey (35°-39° N) seismic refraction profiles of the crust and upper mantle from 87° to 100° W longitude: U.S. Geological Survey IMAP 534, Report: 4 p.; 1 Plate: 47.82 × 27.69 inches, https://doi.org/10.3133/i534D.","productDescription":"Report: 4 p.; 1 Plate: 47.82 × 27.69 inches","costCenters":[],"links":[{"id":390740,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1734.htm"},{"id":256377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0534d/report-thumb.jpg"},{"id":256376,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0534d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256375,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0534d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100,35 ], [ -100,39 ], [ -87,39 ], [ -87,35 ], [ -100,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626e5f","contributors":{"authors":[{"text":"Warren, D. H.","contributorId":101327,"corporation":false,"usgs":true,"family":"Warren","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":276050,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67033,"text":"i564 - 1968 - Preliminary geologic map of the Roberts Mountain quadrangle, Lewis and Clark County, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:11:18","indexId":"i564","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"564","subseriesTitle":"NONE","title":"Preliminary geologic map of the Roberts Mountain quadrangle, Lewis and Clark County, Montana","language":"ENGLISH","doi":"10.3133/i564","usgsCitation":"Schmidt, R.G., and Strong, C., 1968, Preliminary geologic map of the Roberts Mountain quadrangle, Lewis and Clark County, Montana: U.S. Geological Survey IMAP 564, 1 map ;58 x 40 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i564.","productDescription":"1 map ;58 x 40 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106837,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9351.htm","linkFileType":{"id":5,"text":"html"},"description":"9351"},{"id":188221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,47 ], [ -112.25,47.1175 ], [ -112.11749999999999,47.1175 ], [ -112.11749999999999,47 ], [ -112.25,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67acce","contributors":{"authors":[{"text":"Schmidt, R. G.","contributorId":107690,"corporation":false,"usgs":true,"family":"Schmidt","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":275485,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strong, C.P. Jr.","contributorId":20021,"corporation":false,"usgs":true,"family":"Strong","given":"C.P.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":275484,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5844,"text":"pp590 - 1968 - A descriptive catalog of selected aerial photographs of geologic features in the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp590","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"590","title":"A descriptive catalog of selected aerial photographs of geologic features in the United States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp590","usgsCitation":"Denny, C.S., Warren, C., Dow, D., and Dale, W., 1968, A descriptive catalog of selected aerial photographs of geologic features in the United States: U.S. Geological Survey Professional Paper 590, 79 p., https://doi.org/10.3133/pp590.","productDescription":"79 p.","costCenters":[],"links":[{"id":112635,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0590/report.pdf","size":"44031","linkFileType":{"id":1,"text":"pdf"}},{"id":140248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0590/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aee64","contributors":{"authors":[{"text":"Denny, Charles Storrow","contributorId":86331,"corporation":false,"usgs":true,"family":"Denny","given":"Charles","email":"","middleInitial":"Storrow","affiliations":[],"preferred":false,"id":151670,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warren, C.R.","contributorId":80663,"corporation":false,"usgs":true,"family":"Warren","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":151669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dow, D.H.","contributorId":97898,"corporation":false,"usgs":true,"family":"Dow","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":151671,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dale, W.J.","contributorId":28590,"corporation":false,"usgs":true,"family":"Dale","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":151668,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":14001,"text":"ofr68119 - 1968 - Redefinition of the terms Kingsport Formation and Mascot Dolomite and subdivisions of the upper part of the Knox Group in eastern Tennessee","interactions":[],"lastModifiedDate":"2025-06-17T16:42:56.511921","indexId":"ofr68119","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-119","title":"Redefinition of the terms Kingsport Formation and Mascot Dolomite and subdivisions of the upper part of the Knox Group in eastern Tennessee","docAbstract":"<p>Upper part of the Knox Group has previously been divided into three formations; however, because of the lack of regionally recognizable boundaries, there has been a marked inconsistency as to the rocks assigned by different workers to the Longview Dolomite, Kingsport Formation and Mascot Dolomite. Regional stratigraphic studies have pointed out that there are only two recognizable major gross lithologic divisions. Because of this limitation, the term Longview, which has been used as a fossil zone, is abandoned; the term Kingsport is redefined to include the limestone and medium to coarsely crystalline dolomite unit, and Mascot is redefined to include the silty to very-finely crystalline dolomite unit from the top of the Kingsport to the unconformity at the top of the Knox Group.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68119","usgsCitation":"Harris, L.D., 1968, Redefinition of the terms Kingsport Formation and Mascot Dolomite and subdivisions of the upper part of the Knox Group in eastern Tennessee: U.S. Geological Survey Open-File Report 68-119, Report: ii, 52 p.; 6 Figures: 62.53 x 21.41 inches or smaller, https://doi.org/10.3133/ofr68119.","productDescription":"Report: ii, 52 p.; 6 Figures: 62.53 x 21.41 inches or 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,{"id":62521,"text":"gq761 - 1968 - Geologic map of the Ackerman Canyon quadrangle, Lander and Eureka Counties, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:10:44","indexId":"gq761","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"761","title":"Geologic map of the Ackerman Canyon quadrangle, Lander and Eureka Counties, Nevada","language":"ENGLISH","doi":"10.3133/gq761","usgsCitation":"McKee, E.H., 1968, Geologic map of the Ackerman Canyon quadrangle, Lander and Eureka Counties, Nevada: U.S. Geological Survey Geologic Quadrangle 761, 1 map., https://doi.org/10.3133/gq761.","productDescription":"1 map.","costCenters":[],"links":[{"id":103481,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2067.htm","linkFileType":{"id":5,"text":"html"},"description":"2067"},{"id":248684,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0761/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":253911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0761/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.75,39.5 ], [ -116.75,39.75 ], [ -116.5,39.75 ], [ -116.5,39.5 ], [ -116.75,39.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2619","contributors":{"authors":[{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":267491,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16105,"text":"ofr68258 - 1968 - The Mt. Montro kyanite deposit, Grand Bassa County, Liberia","interactions":[],"lastModifiedDate":"2021-12-23T15:59:36.556716","indexId":"ofr68258","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-258","title":"The Mt. Montro kyanite deposit, Grand Bassa County, Liberia","docAbstract":"<p>The Mt. Montro kyanite deposit, 14 miles north of Buchanan, Grand Bassa County, Liberia, is near the middle of a belt of kyanite-bearing gneisses and schists that is 9 miles long and 1 mile wide. The deposit, which seems to be the most persistent and the largest single body of kyanite rocks in the belt, is approximately 12, 600 feet long, as much as 480 feet in outcrop width, and from 25 to 350 feet thick. Kyanite-quartz-biotite-feldspar-garnet-muscovite gneiss, local interbeds of kyanite-mica schist, and lesser amounts of biotite-quartz gneiss, are the principal rocks in the deposit. Other rocks in the kyanite belt include garnet-biotite gneiss, undifferentiated quartzo-feldspathic gneiss, quartzite, and amphibolite. The rocks are the product of regional metamorphism to almandine amphibolite facies. The regional strike is northwest and dips are southwest.</p><p>Kyanite crystals are as much as 3 inches long. The kyanite content ranges from 5. 8 to 46. 7 percent, but most rocks contain between 10 and 35 percent. Garnetiferous beds contain as much as 15 percent red garnets that range to half an inch in diameter. In general, the garnet-rich beds are found in the upper part of the deposit.</p><p>he total reserves of the Mt. Montro kyanite deposit are estimated at about 10 million tons of kyanitic rock containing approximately 2.5 million tons of kyanite. These estimates include measured, indicated, and inferred reserves, calculated to depths of 25 to 100 feet, on the assumption that open-cut mining to those depths would be feasible. The largest part of the deposit underlies Mt. Montro and contains about 8 million tons of kyanitic rock containing nearly 1.9 million tons of kyanite. Residual soil overlying the deposit averages about 5 feet in thickness and is estimated to comprise slightly more than 400,000 cubic yards of material containing about 186,000 tons of kyanite.</p><p>The proximity of the kyanite deposit to a paved highway, to port facilities at Buchanan, and to water, electrical power, and timber resources are considered favorable factors relevant to possible development. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68258","usgsCitation":"Stanin, S.A., and Cooper, B.R., 1968, The Mt. Montro kyanite deposit, Grand Bassa County, Liberia: U.S. Geological Survey Open-File Report 68-258, Report: 33 p.; 4 Plates: 13.24 x 8.92 inches or smaller; 1 Table, https://doi.org/10.3133/ofr68258.","productDescription":"Report: 33 p.; 4 Plates: 13.24 x 8.92 inches or smaller; 1 Table","costCenters":[],"links":[{"id":393367,"rank":7,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1968/0258/table-3.pdf","text":"Table 3","linkFileType":{"id":1,"text":"pdf"}},{"id":393366,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0258/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393364,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0258/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393363,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0258/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393365,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0258/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393362,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0258/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149780,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0258/report-thumb.jpg"}],"country":"Liberia","county":"Grand Bassa County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -10.079269409179688,\n              6.071255645661511\n            ],\n            [\n              -10.020904541015625,\n              6.071255645661511\n            ],\n            [\n              -10.020904541015625,\n              6.1146113285641635\n            ],\n            [\n              -10.079269409179688,\n              6.1146113285641635\n            ],\n            [\n              -10.079269409179688,\n              6.071255645661511\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b3c4","contributors":{"authors":[{"text":"Stanin, S. Anthony","contributorId":57853,"corporation":false,"usgs":true,"family":"Stanin","given":"S.","email":"","middleInitial":"Anthony","affiliations":[],"preferred":false,"id":172242,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, Bismark R.","contributorId":100409,"corporation":false,"usgs":true,"family":"Cooper","given":"Bismark","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":172243,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63776,"text":"gp627 - 1968 - Aeromagnetic map of the Worthington quadrangle and parts of the Plainfield and Peru quadrangles, Berkshire and Hampshire Counties, Massachusetts","interactions":[],"lastModifiedDate":"2025-06-18T18:18:55.986911","indexId":"gp627","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"627","title":"Aeromagnetic map of the Worthington quadrangle and parts of the Plainfield and Peru quadrangles, Berkshire and Hampshire Counties, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp627","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1968, Aeromagnetic map of the Worthington quadrangle and parts of the Plainfield and Peru quadrangles, Berkshire and Hampshire Counties, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 627, 1 Plate: 20.68 x 31.87 inches, https://doi.org/10.3133/gp627.","productDescription":"1 Plate: 20.68 x 31.87 inches","costCenters":[],"links":[{"id":490937,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5994.htm","linkFileType":{"id":5,"text":"html"}},{"id":253469,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0627/report-thumb.jpg"},{"id":249972,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0627/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249971,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0627/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Berkshire County, Hampshire County","otherGeospatial":"Worthington quadrangle and parts of the Plainfield and Peru quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.0083,\n              42.5\n            ],\n            [\n              -73.0083,\n              42.375\n            ],\n            [\n              -72.875,\n              42.375\n            ],\n            [\n              -72.875,\n              42.5\n            ],\n            [\n              -73.0083,\n              42.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b9cf","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533246,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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