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,{"id":68635,"text":"ha83 - 1964 - Water-table, surface-drainage, and engineering soils map of the Clayton area, Delaware","interactions":[],"lastModifiedDate":"2022-01-13T22:22:33.395377","indexId":"ha83","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"83","title":"Water-table, surface-drainage, and engineering soils map of the Clayton area, Delaware","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha83","usgsCitation":"Adams, J.K., Boggess, D.H., and Coskery, O.J., 1964, Water-table, surface-drainage, and engineering soils map of the Clayton area, Delaware: U.S. Geological Survey Hydrologic Atlas 83, 1 Plate: 46.00 × 29.50 inches, https://doi.org/10.3133/ha83.","productDescription":"1 Plate: 46.00 × 29.50 inches","costCenters":[],"links":[{"id":185781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90305,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/083/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394359,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16181.htm"}],"scale":"24000","country":"United States","state":"Delaware","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.767,\n              39.25\n            ],\n            [\n              -75.625,\n              39.25\n            ],\n            [\n              -75.625,\n              39.375\n            ],\n            [\n              -75.767,\n              39.375\n            ],\n            [\n              -75.767,\n              39.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4cc2","contributors":{"authors":[{"text":"Adams, John K.","contributorId":17700,"corporation":false,"usgs":true,"family":"Adams","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278608,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boggess, Durward H.","contributorId":28650,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278609,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coskery, O. J.","contributorId":8440,"corporation":false,"usgs":true,"family":"Coskery","given":"O.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278607,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":12938,"text":"ofr6433 - 1964 - Geology of the Andover Granite and surrounding rocks, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:06:56","indexId":"ofr6433","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-33","title":"Geology of the Andover Granite and surrounding rocks, Massachusetts","docAbstract":"Field and petrographic studies of the Andover Granite and surrounding rocks have afforded an opportunity for an explanation of its emplacement and crystallization. The investigation has contributed secondarily to an understanding of the geologic history of southeastern New England, particularly as it is revealed in the Lawrence, Wilmington, South Groveland, and Reading quadrangles of Massachusetts. \r\n\r\nThe Andover Granite and Sharpners Pond Tonalite together comprise up to 90 percent of the Acadian(?) subalkaline intrusive series cropping out within the area of study. The subalkaline series locally invades a sequence of early to middle Paleozoic and possibly Precambrian metasedimentary and metavolcanic rocks. Much of the subalkaline series and most of the Andover Granite is confined between two prominent east-northeast trending faults or fault systems. The northern fault separates the mildly metamorphosed Middle Silurian(?) Merrimack Group on the north from a highly metamorphosed and thoroughly intruded Ordovician(?) sequence on the south. The southern 'boundary '' fault is a major structural discontinuity characterized by penetrative, diffuse shearing over a zone one-half mile or more in width. \r\n\r\nThe magmatic nature of the Andover Granite is demonstrated by: (1) sharply crosscutting relationships with surrounding rocks; (2) the occurrence of tabular-shaped xenoliths whose long directions parallel the foliation within the granite and whose internal foliation trends at a high angle to that of the granite; (3) continuity with the clearly intrusive Sharpners Pond Tonalite; (4) the compositional uniformity of the granite as contrasted with the compositional diversity of the rocks it invades; (5) its modal and normative correspondence with (a) calculated norms of salic extrusives and (b) that of the ternary (\u001Cgranite\u001D) minimum for the system NaAlSi3O8-KAlSi3O8-SiO2. \r\n\r\nOrogenic granites, as represented by the Andover, contrast with post-orogenic granites, represented locally by the Peabody Granite, in their phase composition and texture. Unlike the Peabody, the Andover Granite is thought to have been thoroughly recrystallized through the unmixing of initially homogeneous phases with the concomitant development of extremely intricate, allotriomorphic textures. Textural relationships between potassium and plagioclase feldspars and among quartz and the two feldspars, suggest that the Andover Granite has evolved through exsolution of a single hypersolvus feldspar (or two coexisting subsolvus feldspars of only slightly disparate compositions) into discrete grains of plagioclase and potassium feldspar, much along the lines proposed by Tuttle (1952). \r\n\r\nA hypothesis is proposed for the origin of myrmekite whereby it is evolved indirectly through exsolution of a homogeneous, hypersolvus, calcalkali feldspar in the presence of a silica reservoir. Where the An 'molecule' is contained in the primary mix crystal, exsolution into potassium and plagioclase feldspar phases normally requires a paired exchange between Ca-Al and K-Si. Should the silicon requirements of the developing potassium feldspar be met by the matrix silica reservoir, the concomitantly evolving plagioclase may become stoichiometrically enriched in silicon and ultimately develop into myrmekite. Discrete unmixing of pure alkali feldspar proceeds through simple alkali ion exchange; ternary compostions high in An are more apt to fall initially in the two-feldspar field, thereby reducing the unmixing potential. General restriction of myrmekite to plagioclase of calcic albite to oligoclase composition is explained accordingly.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6433","usgsCitation":"Castle, R.O., 1964, Geology of the Andover Granite and surrounding rocks, Massachusetts: U.S. Geological Survey Open-File Report 64-33, 550 p. ill., maps ;29 cm., https://doi.org/10.3133/ofr6433.","productDescription":"550 p. ill., maps ;29 cm.","costCenters":[],"links":[{"id":146979,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0033/report-thumb.jpg"},{"id":41382,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41383,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41384,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41385,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41386,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41387,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41388,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41389,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41390,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41391,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68353e","contributors":{"authors":[{"text":"Castle, Robert O.","contributorId":22741,"corporation":false,"usgs":true,"family":"Castle","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":166992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68621,"text":"ha90 - 1964 - Floods in Harvey quadrangle, Illinois","interactions":[],"lastModifiedDate":"2023-01-13T21:51:01.628461","indexId":"ha90","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"90","title":"Floods in Harvey quadrangle, Illinois","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha90","usgsCitation":"Allen, H., and May, V.J., 1964, Floods in Harvey quadrangle, Illinois: U.S. Geological Survey Hydrologic Atlas 90, 1 Plate: 53.00 x 32.50 inches, https://doi.org/10.3133/ha90.","productDescription":"1 Plate: 53.00 x 32.50 inches","costCenters":[],"links":[{"id":411928,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16189.htm","linkFileType":{"id":5,"text":"html"}},{"id":90282,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/090/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185645,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"Illinois","otherGeospatial":"Harvey quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.75,\n              41.5\n            ],\n            [\n              -87.75,\n              41.625\n            ],\n            [\n              -87.625,\n              41.625\n            ],\n            [\n              -87.625,\n              41.5\n            ],\n            [\n              -87.75,\n              41.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e70fa","contributors":{"authors":[{"text":"Allen, Howard E.","contributorId":17274,"corporation":false,"usgs":true,"family":"Allen","given":"Howard E.","affiliations":[],"preferred":false,"id":278584,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, V. Jeff","contributorId":80358,"corporation":false,"usgs":true,"family":"May","given":"V.","email":"","middleInitial":"Jeff","affiliations":[],"preferred":false,"id":278585,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68641,"text":"ha103 - 1964 - Water-table, surface-drainage, and engineering soils map of the Lewes area, Delaware","interactions":[],"lastModifiedDate":"2012-02-10T00:11:27","indexId":"ha103","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"103","title":"Water-table, surface-drainage, and engineering soils map of the Lewes area, Delaware","language":"ENGLISH","doi":"10.3133/ha103","usgsCitation":"Adams, J.K., Boggess, D.H., and Davis, C.F., 1964, Water-table, surface-drainage, and engineering soils map of the Lewes area, Delaware: U.S. Geological Survey Hydrologic Atlas 103, 1 map., https://doi.org/10.3133/ha103.","productDescription":"1 map.","costCenters":[],"links":[{"id":186590,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90312,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/103/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.25,38.75 ], [ -75.25,38.8675 ], [ -75.08333333333333,38.8675 ], [ -75.08333333333333,38.75 ], [ -75.25,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99d1","contributors":{"authors":[{"text":"Adams, John K.","contributorId":17700,"corporation":false,"usgs":true,"family":"Adams","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boggess, Durward H.","contributorId":28650,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, Christian F.","contributorId":84004,"corporation":false,"usgs":true,"family":"Davis","given":"Christian","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":278624,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68628,"text":"ha80 - 1964 - Water-table, surface-drainage, and engineering soils map of the Taylors bridge area, Delaware","interactions":[],"lastModifiedDate":"2012-02-10T00:11:26","indexId":"ha80","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"80","title":"Water-table, surface-drainage, and engineering soils map of the Taylors bridge area, Delaware","language":"ENGLISH","doi":"10.3133/ha80","usgsCitation":"Adams, J.K., and Boggess, D.H., 1964, Water-table, surface-drainage, and engineering soils map of the Taylors bridge area, Delaware: U.S. Geological Survey Hydrologic Atlas 80, col. map ;on sheet 74 x 92 cm., https://doi.org/10.3133/ha80.","productDescription":"col. map ;on sheet 74 x 92 cm.","costCenters":[],"links":[{"id":185698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90289,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/080/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.61749999999999,39.3675 ], [ -75.61749999999999,39.5 ], [ -75.5,39.5 ], [ -75.5,39.3675 ], [ -75.61749999999999,39.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c90","contributors":{"authors":[{"text":"Adams, John K.","contributorId":17700,"corporation":false,"usgs":true,"family":"Adams","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boggess, Durward H.","contributorId":28650,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278598,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68643,"text":"ha106 - 1964 - Water-table, surface-drainage, and engineering soils map of the Seaford East quadrangle, Delaware","interactions":[],"lastModifiedDate":"2012-02-10T00:11:27","indexId":"ha106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"106","title":"Water-table, surface-drainage, and engineering soils map of the Seaford East quadrangle, Delaware","language":"ENGLISH","doi":"10.3133/ha106","usgsCitation":"Adams, J.K., Boggess, D.H., and Coskery, O.J., 1964, Water-table, surface-drainage, and engineering soils map of the Seaford East quadrangle, Delaware: U.S. Geological Survey Hydrologic Atlas 106, 1 map., https://doi.org/10.3133/ha106.","productDescription":"1 map.","costCenters":[],"links":[{"id":186592,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90317,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/106/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.61749999999999,38.6175 ], [ -75.61749999999999,38.75 ], [ -75.5,38.75 ], [ -75.5,38.6175 ], [ -75.61749999999999,38.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ca8","contributors":{"authors":[{"text":"Adams, John K.","contributorId":17700,"corporation":false,"usgs":true,"family":"Adams","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278627,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boggess, Durward H.","contributorId":28650,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278628,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coskery, O. J.","contributorId":8440,"corporation":false,"usgs":true,"family":"Coskery","given":"O.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278626,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":46386,"text":"ofr64133 - 1964 - Map of the lower portion of the Teton Glacier, Grand Teton National Park, Wyoming","interactions":[],"lastModifiedDate":"2026-01-16T22:07:34.632127","indexId":"ofr64133","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-133","title":"Map of the lower portion of the Teton Glacier, Grand Teton National Park, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr64133","usgsCitation":"Reed, J.C., 1964, Map of the lower portion of the Teton Glacier, Grand Teton National Park, Wyoming: U.S. Geological Survey Open-File Report 64-133, 1 map., https://doi.org/10.3133/ofr64133.","productDescription":"1 map.","costCenters":[],"links":[{"id":168403,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db658561","contributors":{"authors":[{"text":"Reed, John Calvin Jr.","contributorId":8460,"corporation":false,"usgs":true,"family":"Reed","given":"John","suffix":"Jr.","email":"","middleInitial":"Calvin","affiliations":[],"preferred":false,"id":233198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35069,"text":"b1161C - 1964 - Nonopaque heavy minerals in sandstone of Jurassic and Cretaceous age in the Black Hills, Wyoming and South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:09:45","indexId":"b1161C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1161","chapter":"C","title":"Nonopaque heavy minerals in sandstone of Jurassic and Cretaceous age in the Black Hills, Wyoming and South Dakota","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1161C","usgsCitation":"Mapel, W.J., Chisholm, W.A., and Bergenback, R.E., 1964, Nonopaque heavy minerals in sandstone of Jurassic and Cretaceous age in the Black Hills, Wyoming and South Dakota: U.S. Geological Survey Bulletin 1161, p. C1-C59, ill., maps (2 fold. in pocket) ;24 cm., https://doi.org/10.3133/b1161C.","productDescription":"p. C1-C59, ill., maps (2 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":166988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1161c/report-thumb.jpg"},{"id":63015,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1161c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63016,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1161c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63017,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1161c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e97","contributors":{"authors":[{"text":"Mapel, W. J.","contributorId":92225,"corporation":false,"usgs":true,"family":"Mapel","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":214067,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chisholm, Wayne A.","contributorId":43343,"corporation":false,"usgs":true,"family":"Chisholm","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":214065,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bergenback, Richard E.","contributorId":65897,"corporation":false,"usgs":true,"family":"Bergenback","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":214066,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2983,"text":"wsp1499E - 1964 - Water resources of the Flint area, Michigan","interactions":[],"lastModifiedDate":"2017-02-06T15:45:12","indexId":"wsp1499E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1499","chapter":"E","title":"Water resources of the Flint area, Michigan","docAbstract":"<p>This report describes the water resources of Genesee County, Mich., whose principal city is Flint. The sources of water available to the county are the Flint and Shiawassee Rivers and their tributaries, inland lakes, ground water, and Lake Huron. The withdrawal use of water in the county in 1958 amounted to about 45 mgd. Of this amount, 36 mgd was withdrawn from the Flint River by the Flint public water-supply system. The rest was supplied by wells. At present (1959) the Shiawassee River and its tributaries and the inland lakes are not used for water supply.</p><p>&nbsp;Flint River water is used for domestic, industrial, and waste-dilution requirements in Flint. About 60 percent of the water supplied by the Flint public water system is used by Flint industry. At least 30 mgd of river water is needed for waste dilution in the Flint River during warm weather.</p><p>Water from Holloway Reservoir, which has a storage capacity of 5,760 million gallons, is used to supplement low flows in the Flint River to meet water-supply and waste-dilution requirements. About 650 million gallons in Kearsley Reservoir, on a Flint River tributary, is held in reserve for emergency use. Based on records for the lowest flows during the period 1930-52, the Flint River system, with the two reservoirs in operation, is capable of supplying about 60 mgd at Flint, less evaporation and seepage losses. The 1958 water demands exceeded this amount. Development of additional storage in the Flint River basin is unlikely because of lack of suitable storage sites. Plans are underway to supply Flint and most of Genesee County with water from Lake Huron.</p><p>The principal tributaries of the Flint River in and near Flint could furnish small supplies of water. Butternut Creek, with the largest flow of those studied, has an estimated firm yield of 0.054 mgd per sq mi for 95 percent of the time. The Shiawassee River at Byron is capable of supplying at least 29 mgd for 95 percent of the time.</p><p>Floods are a serious problem in Flint. The April 1947 flood, the largest on record, caused nearly $4 million flood damage in Flint. A proposed flood-control plan for Flint calls for channel, floodwall, and levee improvements and the removal or modification of some bridges.</p><p>Analyses of water samples taken from selected streams and lakes in the Flint area indicate that the waters are of the calcium bicarbonate type and generally hard to very hard. Flint River water is relatively uniform in quality although a progressive increase in iron, sodium, and chloride concentrations was noted between Otisville and Montrose. Downstream from Flint, the dissolved oxygen</p><p>content may be low during low flows. At times, concentrations of iron, manganese, phenols, color, and turbidity in Flint River water exceed the limits recommended in drinking water standards. Water temperatures ranged from freezing to 86°F in a 4-year period. The finished water supplied by the Flint water-treatment plant is fairly uniform in quality, moderately soft, alkaline, and low in color and turbidity. The pH is nearly always above 10. Further softening and removal of iron and related minerals would be desirable for certain industrial uses.</p><p>The quality of the water sampled in the Flint River tributaries was generally similar to that of the Flint River. However, no phenols or oils and waxes were found. Softening and other treatment dependent upon use would be required if these streams were developed for water supply.</p><p>Waters sampled in the Shiawassee River and selected lakes were generally less mineralized than Flint River water. Water from the lakes showed the lowest concentrations of dissolved solids. Softening would be required for nearly all uses. Additional treatment would depend upon contemplated use.</p><p>Shallow deposits of sand and gravel deposited as outwash along glacial meltwater streams and as deltas in the glacial lakes that covered the northwestern part of the county are sources of water to moderate- and large-capacity wells. Thick deposits of sand and gravel also fill some of the valleys in the bedrock surface and yield moderate to large supplies of water. Production from public supply wells tapping the drift aquifers in the area ranges from about 50 to 1,200 gpm. The water from the drift aquifer is hard or very hard and commonly contains objectionable amounts of iron.</p><p>The Saginaw formation is a source of water to wells supplying some of the small communities and industries in the county. The Saginaw, which is the uppermost bedrock formation in the area, underlies most of the county. It is composed of layers of sandstone, shale, and limestone and some beds of coal. The formation is composed principally of sandstone in some areas of the county, and shale in others. Production from wells tapping the Saginaw ranges from a few to about 500 gpm. The water produced is generally moderately hard or hard and commonly contains objectionable amounts of chloride. The quality of the water limits its development for water supply. Overdrafts from the Saginaw result in a lowering of the piezometric surface and commonly cause an upward migration of water high in chloride.</p><p>The Michigan and Marshall formations are generally not sources of fresh water where they are overlain by the Saginaw formation. In the southern and eastern parts of the county where they are overlain by glacial deposits, they are a source of water of good quality. The quantity of water obtainable from these formations is not fully known. However, the Marshall may be a source of large supplies of water in the southeastern part of the county.</p><p>An ample supply of water is available in lakes, ponds, and streams in the metropolitan area of Flint to meet requirements for domestic, sanitary, and firefighting use in civil defense emergencies. The extent of emergency use of water from these sources would depend upon the pumping, distribution, and treatment facilities available. Enough private industrial and commercial, and public wells are present in the area normally supplied by the Flint public water system to meet emergency requirements for domestic and sanitary use. Use of these wells would also depend upon available pumping and distribution facilities. Water from many of these wells contains objectionable amounts of chloride, but it could be used without treatment in an emergency.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1499E","usgsCitation":"Wiitala, S.W., Vanlier, K., and Krieger, R.A., 1964, Water resources of the Flint area, Michigan: U.S. Geological Survey Water Supply Paper 1499, Document: viii, 86 p.; 6 Plates: 20.00 x 18.29 inches or smaller, https://doi.org/10.3133/wsp1499E.","productDescription":"Document: viii, 86 p.; 6 Plates: 20.00 x 18.29 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":139431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1499e/report-thumb.jpg"},{"id":29743,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29744,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29745,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29746,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29747,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29748,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29749,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1499e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","county":"Genesee County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-83.4607,43.2235],[-83.4593,43.1425],[-83.4589,43.1365],[-83.455,42.9681],[-83.4553,42.9617],[-83.4546,42.8798],[-83.4541,42.8766],[-83.5737,42.8744],[-83.6902,42.871],[-83.6863,42.7822],[-83.9225,42.7812],[-83.928,42.8677],[-83.9309,42.9574],[-83.9283,43.0451],[-83.9294,43.1334],[-83.9318,43.2204],[-83.8154,43.2212],[-83.694,43.2223],[-83.5809,43.2226],[-83.4607,43.2235]]]},\"properties\":{\"name\":\"Genesee\",\"state\":\"MI\"}}]}\n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602df3","contributors":{"authors":[{"text":"Wiitala, Sulo Werner","contributorId":20315,"corporation":false,"usgs":true,"family":"Wiitala","given":"Sulo","email":"","middleInitial":"Werner","affiliations":[],"preferred":false,"id":146097,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vanlier, K.E.","contributorId":24332,"corporation":false,"usgs":true,"family":"Vanlier","given":"K.E.","affiliations":[],"preferred":false,"id":146098,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krieger, Robert A.","contributorId":99954,"corporation":false,"usgs":true,"family":"Krieger","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146099,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61291,"text":"mf295 - 1964 - Geologic map of the Hay Meadow Reservoir quadrangle, Sublette, Fremont, and Sweetwater Counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"mf295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"295","title":"Geologic map of the Hay Meadow Reservoir quadrangle, Sublette, Fremont, and Sweetwater Counties, Wyoming","language":"ENGLISH","doi":"10.3133/mf295","usgsCitation":"Zeller, H.D., and Stephens, E., 1964, Geologic map of the Hay Meadow Reservoir quadrangle, Sublette, Fremont, and Sweetwater Counties, Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 295, 1 map ;58 x 44 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf295.","productDescription":"1 map ;58 x 44 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104066,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2715.htm","linkFileType":{"id":5,"text":"html"},"description":"2715"},{"id":182976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.11749999999999,42.25 ], [ -109.11749999999999,42.3675 ], [ -109,42.3675 ], [ -109,42.25 ], [ -109.11749999999999,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69808b","contributors":{"authors":[{"text":"Zeller, H. D.","contributorId":104872,"corporation":false,"usgs":true,"family":"Zeller","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":265335,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, E. V.","contributorId":31054,"corporation":false,"usgs":true,"family":"Stephens","given":"E. V.","affiliations":[],"preferred":false,"id":265334,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35469,"text":"b1161D - 1964 - Geologic reconnaissance of the Antelope-Ashwood area, north-central Oregon, with emphasis on the John Day Formation of late Oligocene and early Miocene age","interactions":[],"lastModifiedDate":"2022-07-05T21:10:38.994709","indexId":"b1161D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1161","chapter":"D","title":"Geologic reconnaissance of the Antelope-Ashwood area, north-central Oregon, with emphasis on the John Day Formation of late Oligocene and early Miocene age","docAbstract":"This report briefly describes the geology of an area of about 750 square miles in Jefferson, Wasco, Crook, and Wheeler Counties, Oregon. About 16,000 feet of strata that range in age from pre-Tertiary to Quaternary are exposed. These include the following units: pre-Tertiary slate, graywacke, conglomerate, and meta-andesite; Clarno Formation of Eocene age - lava flows, volcanic breccia, tuff, and tuffaceous mudstone, chiefly of andesitic composition; John Day Formation of late Oligocene and early Miocene age - pyroclastic rocks, flows, and domes, chiefly of rhyolitic composition; Columbia River Basalt of middle Miocene age - thick, columnar jointed flows of very fine grained dense dark-gray basalt; Dalles Formation of Pliocene age - bedded tuffaceous sandstone, siltstone, and conglomerate; basalt of Pliocene or Pleistocene age - lava flows of porous-textured olivine basalt; and Quaternary loess, landslide debris, and alluvium. Unconformities separate pre-Tertiary rocks and Clarno Formation, Clarno and John Day Formations, John Day Formation and Columbia River Basalt, and Columbia River Basalt and Dalles Formation.\r\n\r\nThe John Day Formation, the only unit studied in detail, consists of about 4,000 feet of tuff, lapilli tuff, strongly to weakly welded rhyolite ash flows, and less abundant trachyandesite flows and rhyolite flows and domes. The formation was divided into nine mappable members in part of the area, primarily on the basis of distinctive ledge-forming welded ash-flow sheets. Most of the sheets are composed of stony rhyolite containing abundant lithophysae and sparse phenocrysts. One sheet contains 10 to 20 percent phenocrysts, mostly cryptoperthitic soda sanidine, but including less abundant quartz, myrmekitic intergrowths of quartz and sanidine, and oligoclase. The rhyolitic ash flows and lava flows were extruded from nearby vents, in contrast to some of the interbedded air-fall tuff and lapilli tuff of dacitic and andesitic composition that may have been derived from vents in an ancestral Cascade Range. The John Day is dated on the basis of a late Oligocene flora near the base of the formation and early Miocene faunas near the top of the formation.\r\n\r\nThe middle Miocene and older rocks in the Antelope-Ashwood area are broadly folded and broken along northeast-trending faults. Over much of the area the rocks dip gently eastward from the crest of a major fold and are broken along a series of steeply dipping antithetic strike faults. Pliocene and Quaternary strata appear to be undeformed.\r\n\r\nAt the Priday agate deposit, chalcedony-filled spherulites (thunder-eggs) occur in the lower part of a weakly welded rhyolitic ash flow. The so-called thunder-eggs are small spheroidal bodies, about 3 inches in average diameter; each consists of a chalcedonic core surrounded by a shell of welded tuff that is altered to radially oriented fibers of cristobalite and alkalic feldspar.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to general geology (Bulletin 1161)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1161D","collaboration":"Prepared in cooperation with the State of Oregon, Department of Geology ande Mineral Industries","usgsCitation":"Peck, D.L., 1964, Geologic reconnaissance of the Antelope-Ashwood area, north-central Oregon, with emphasis on the John Day Formation of late Oligocene and early Miocene age: U.S. Geological Survey Bulletin 1161, Report: iii, 26 p.; 1 Plate: 31.50 × 13.00 inches, https://doi.org/10.3133/b1161D.","productDescription":"Report: iii, 26 p.; 1 Plate: 31.50 × 13.00 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":63365,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1161d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109435,"rank":699,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20913.htm","linkFileType":{"id":5,"text":"html"},"description":"20913"},{"id":63366,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1161d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166225,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1161d/report-thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Antelope-Ashwood area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121,\n              44.5\n            ],\n            [\n              -120.449,\n              44.5\n            ],\n            [\n              -120.449,\n              45\n            ],\n            [\n              -121,\n              45\n            ],\n            [\n              -121,\n              44.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a83d6","contributors":{"authors":[{"text":"Peck, Dallas L.","contributorId":60187,"corporation":false,"usgs":true,"family":"Peck","given":"Dallas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":214693,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59818,"text":"mf287 - 1964 - Geology of the Irwin quadrangle, Bonneville County, Idaho","interactions":[],"lastModifiedDate":"2012-02-10T00:10:26","indexId":"mf287","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"287","title":"Geology of the Irwin quadrangle, Bonneville County, Idaho","language":"ENGLISH","doi":"10.3133/mf287","usgsCitation":"Jobin, D., and Schroeder, M., 1964, Geology of the Irwin quadrangle, Bonneville County, Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 287, 1 map., https://doi.org/10.3133/mf287.","productDescription":"1 map.","costCenters":[],"links":[{"id":104058,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2706.htm","linkFileType":{"id":5,"text":"html"},"description":"2706"},{"id":182561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.36749999999999,43.3675 ], [ -111.36749999999999,43.5 ], [ -111.25,43.5 ], [ -111.25,43.3675 ], [ -111.36749999999999,43.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fe96","contributors":{"authors":[{"text":"Jobin, D. A.","contributorId":41062,"corporation":false,"usgs":true,"family":"Jobin","given":"D. A.","affiliations":[],"preferred":false,"id":262649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schroeder, M.L.","contributorId":71243,"corporation":false,"usgs":true,"family":"Schroeder","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":262650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59817,"text":"mf277 - 1964 - Geology of the Conant Valley quadrangle, Bonneville County, Idaho","interactions":[],"lastModifiedDate":"2012-02-10T00:10:26","indexId":"mf277","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"277","title":"Geology of the Conant Valley quadrangle, Bonneville County, Idaho","language":"ENGLISH","doi":"10.3133/mf277","usgsCitation":"Jobin, D., and Schroeder, M., 1964, Geology of the Conant Valley quadrangle, Bonneville County, Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 277, 1 map :col. ;58 x 42 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf277.","productDescription":"1 map :col. ;58 x 42 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":182560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":104051,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2696.htm","linkFileType":{"id":5,"text":"html"},"description":"2696"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.5,43.3675 ], [ -111.5,43.5 ], [ -111.36749999999999,43.5 ], [ -111.36749999999999,43.3675 ], [ -111.5,43.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683099","contributors":{"authors":[{"text":"Jobin, D. A.","contributorId":41062,"corporation":false,"usgs":true,"family":"Jobin","given":"D. A.","affiliations":[],"preferred":false,"id":262647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schroeder, M.L.","contributorId":71243,"corporation":false,"usgs":true,"family":"Schroeder","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":262648,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59816,"text":"mf284 - 1964 - Geologic map of the Thompson Peak quadrangle, Bonneville County, Idaho","interactions":[],"lastModifiedDate":"2012-02-10T00:10:26","indexId":"mf284","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"284","title":"Geologic map of the Thompson Peak quadrangle, Bonneville County, Idaho","language":"ENGLISH","doi":"10.3133/mf284","usgsCitation":"Jobin, D., and Soister, P., 1964, Geologic map of the Thompson Peak quadrangle, Bonneville County, Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 284, 1 map ;58 x 42 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf284.","productDescription":"1 map ;58 x 42 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104055,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2703.htm","linkFileType":{"id":5,"text":"html"},"description":"2703"},{"id":182559,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.25,43.3675 ], [ -111.25,43.5 ], [ -111.11749999999999,43.5 ], [ -111.11749999999999,43.3675 ], [ -111.25,43.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a552","contributors":{"authors":[{"text":"Jobin, D. A.","contributorId":41062,"corporation":false,"usgs":true,"family":"Jobin","given":"D. A.","affiliations":[],"preferred":false,"id":262646,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Soister, P.E.","contributorId":32986,"corporation":false,"usgs":true,"family":"Soister","given":"P.E.","affiliations":[],"preferred":false,"id":262645,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3012,"text":"wsp1656 - 1964 - Geology and ground-water features of the Edison-Maricopa area, Kern County, California","interactions":[],"lastModifiedDate":"2023-03-08T21:55:27.26962","indexId":"wsp1656","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1656","title":"Geology and ground-water features of the Edison-Maricopa area, Kern County, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1656","usgsCitation":"Wood, P.R., and Dale, R.H., 1964, Geology and ground-water features of the Edison-Maricopa area, Kern County, California: U.S. Geological Survey Water Supply Paper 1656, Report: vi, 108 p.; 12 Plates: 40.00 x 26.50 inches or smaller, https://doi.org/10.3133/wsp1656.","productDescription":"Report: vi, 108 p.; 12 Plates: 40.00 x 26.50 inches or smaller","costCenters":[],"links":[{"id":29819,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29818,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413890,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24848.htm","linkFileType":{"id":5,"text":"html"}},{"id":29821,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1656/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29820,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29814,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29813,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29812,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29811,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29810,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29809,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139530,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1656/report-thumb.jpg"},{"id":29817,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29816,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29815,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1656/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Kern County","otherGeospatial":"Edison-Maricopa area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.589,\n              34.876\n            ],\n            [\n              -118.589,\n              35.458\n            ],\n            [\n              -119.5,\n              35.458\n            ],\n            [\n              -119.5,\n              34.876\n            ],\n            [\n              -118.589,\n              34.876\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685f6e","contributors":{"authors":[{"text":"Wood, Perry Rowley","contributorId":10787,"corporation":false,"usgs":true,"family":"Wood","given":"Perry","email":"","middleInitial":"Rowley","affiliations":[],"preferred":false,"id":146145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dale, R. H.","contributorId":98711,"corporation":false,"usgs":true,"family":"Dale","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":146146,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59807,"text":"mf291 - 1964 - Preliminary geologic map of the Hot Sulphur Springs SW quadrangle, Grand County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:26","indexId":"mf291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"291","title":"Preliminary geologic map of the Hot Sulphur Springs SW quadrangle, Grand County, Colorado","language":"ENGLISH","doi":"10.3133/mf291","usgsCitation":"Izett, G., and Barclay, C., 1964, Preliminary geologic map of the Hot Sulphur Springs SW quadrangle, Grand County, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 291, 1 map ;57 x 44 cm. on sheet 77 x 86 cm. folded to 26 x 22 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/mf291.","productDescription":"1 map ;57 x 44 cm. on sheet 77 x 86 cm. folded to 26 x 22 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104062,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2711.htm","linkFileType":{"id":5,"text":"html"},"description":"2711"},{"id":183550,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.25,40 ], [ -106.25,40.1175 ], [ -106.11749999999999,40.1175 ], [ -106.11749999999999,40 ], [ -106.25,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b22c","contributors":{"authors":[{"text":"Izett, G. A.","contributorId":21131,"corporation":false,"usgs":true,"family":"Izett","given":"G. A.","affiliations":[],"preferred":false,"id":262629,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barclay, C.S.V.","contributorId":41523,"corporation":false,"usgs":true,"family":"Barclay","given":"C.S.V.","email":"","affiliations":[],"preferred":false,"id":262630,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16911,"text":"ofr64153 - 1964 - Astrogeologic studies, annual progress report, August 25, 1962, to July 1, 1963","interactions":[],"lastModifiedDate":"2012-02-02T00:07:12","indexId":"ofr64153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-153","title":"Astrogeologic studies, annual progress report, August 25, 1962, to July 1, 1963","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr64153","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Astrogeologic studies, annual progress report, August 25, 1962, to July 1, 1963: U.S. Geological Survey Open-File Report 64-153, 578 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr64153.","productDescription":"578 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":149679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c9b0","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":528992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39171,"text":"pp272F - 1964 - Methods to compute long-wave radiation from the atmosphere and reflected solar radiation from a water surface","interactions":[],"lastModifiedDate":"2012-02-02T00:09:55","indexId":"pp272F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"272","chapter":"F","title":"Methods to compute long-wave radiation from the atmosphere and reflected solar radiation from a water surface","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Studies of evaporation","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp272F","usgsCitation":"Koberg, G.E., 1964, Methods to compute long-wave radiation from the atmosphere and reflected solar radiation from a water surface: U.S. Geological Survey Professional Paper 272, p. 107-136, https://doi.org/10.3133/pp272F.","productDescription":"p. 107-136","costCenters":[],"links":[{"id":120797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0272f/report-thumb.jpg"},{"id":66704,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0272f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62cedc","contributors":{"authors":[{"text":"Koberg, G. E.","contributorId":30212,"corporation":false,"usgs":true,"family":"Koberg","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":221078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47064,"text":"ofr64123 - 1964 - Geologic map of the Catskill SW quadrangle, Colfax County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:10:40","indexId":"ofr64123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-123","title":"Geologic map of the Catskill SW quadrangle, Colfax County, New Mexico","language":"ENGLISH","doi":"10.3133/ofr64123","usgsCitation":"Pillmore, C., 1964, Geologic map of the Catskill SW quadrangle, Colfax County, New Mexico: U.S. Geological Survey Open-File Report 64-123, 1 map, https://doi.org/10.3133/ofr64123.","productDescription":"1 map","costCenters":[],"links":[{"id":170629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":106334,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8051.htm","linkFileType":{"id":5,"text":"html"},"description":"8051"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d24f","contributors":{"authors":[{"text":"Pillmore, Charles L.","contributorId":27123,"corporation":false,"usgs":true,"family":"Pillmore","given":"Charles L.","affiliations":[],"preferred":false,"id":234579,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47226,"text":"ofr6415 - 1964 - Gamma-ray logs from central Bluegrass Region, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:10:58","indexId":"ofr6415","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-15","title":"Gamma-ray logs from central Bluegrass Region, Kentucky","language":"ENGLISH","doi":"10.3133/ofr6415","usgsCitation":"Black, D.F., and Cressman, E.R., 1964, Gamma-ray logs from central Bluegrass Region, Kentucky: U.S. Geological Survey Open-File Report 64-15, 1 diagram :photocopy ;on sheet 64 x 93 cm., https://doi.org/10.3133/ofr6415.","productDescription":"1 diagram :photocopy ;on sheet 64 x 93 cm.","costCenters":[],"links":[{"id":168722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b13f3","contributors":{"authors":[{"text":"Black, Douglas F. B.","contributorId":106498,"corporation":false,"usgs":true,"family":"Black","given":"Douglas","email":"","middleInitial":"F. B.","affiliations":[],"preferred":false,"id":234859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cressman, Earle Rupert","contributorId":43324,"corporation":false,"usgs":true,"family":"Cressman","given":"Earle","email":"","middleInitial":"Rupert","affiliations":[],"preferred":false,"id":234858,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13544,"text":"ofr6449 - 1964 - Copper determinations on samples of alluvium and caliche from the rocky Range, Beaver County, Utah","interactions":[],"lastModifiedDate":"2025-06-12T19:43:38.919414","indexId":"ofr6449","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-49","title":"Copper determinations on samples of alluvium and caliche from the rocky Range, Beaver County, Utah","docAbstract":"<p>A study of the distribution of copper in transported alluvium on a pediment of the Rocky Range, Beaver County, Utah, undertaken to determine whether known copper deposits in bedrock concealed by alluvium could be detected by geochemical methods, was reported in Geological Survey Research 1960 ( Erickson, R.L., and Marrenzino, A.P., 1960, Geochemical prosecting for copper in the Rocky Range, Beaver County, Utah; U.S. Geol. 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The attached map and table supplement that paper by giving the locations at which the samples were collected and the analytical determinations of copper in the samples.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6449","usgsCitation":"Erickson, R.L., and Marranzino, A.P., 1964, Copper determinations on samples of alluvium and caliche from the rocky Range, Beaver County, Utah: U.S. Geological Survey Open-File Report 64-49, Report: 5 p.; 1 Plate: 24.26 x 19.36 inches, https://doi.org/10.3133/ofr6449.","productDescription":"Report: 5 p.; 1 Plate: 24.26 x 19.36 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,{"id":39109,"text":"pp305L - 1964 - Core tests, Simpson area, Alaska, with a section on temperature measurement studies","interactions":[],"lastModifiedDate":"2012-02-02T00:10:14","indexId":"pp305L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"305","chapter":"L","title":"Core tests, Simpson area, Alaska, with a section on temperature measurement studies","language":"ENGLISH","doi":"10.3133/pp305L","usgsCitation":"Robinson, F.M., and Brewer, M., 1964, Core tests, Simpson area, Alaska, with a section on temperature measurement studies: U.S. Geological Survey Professional Paper 305, p. 645-730, https://doi.org/10.3133/pp305L.","productDescription":"p. 645-730","costCenters":[],"links":[{"id":120011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0305l/report-thumb.jpg"},{"id":66559,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66560,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66561,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66562,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66563,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66564,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66565,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66566,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0305l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688e50","contributors":{"authors":[{"text":"Robinson, F. M.","contributorId":84830,"corporation":false,"usgs":true,"family":"Robinson","given":"F.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":220976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brewer, M.C.","contributorId":54994,"corporation":false,"usgs":true,"family":"Brewer","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":220975,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14011,"text":"ofr6473 - 1964 - Preliminary surficial geology of the Bashbish Falls quadrangle, Massachusetts-Connecticut-New York","interactions":[],"lastModifiedDate":"2025-06-17T13:50:40.301139","indexId":"ofr6473","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-73","title":"Preliminary surficial geology of the Bashbish Falls quadrangle, Massachusetts-Connecticut-New York","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6473","usgsCitation":"Hartshorn, J.H., and Atherton, J.S., 1964, Preliminary surficial geology of the Bashbish Falls quadrangle, Massachusetts-Connecticut-New York: U.S. Geological Survey Open-File Report 64-73, Report: 16 p.; 1 Plate: 33.60 x 27.47 inches, https://doi.org/10.3133/ofr6473.","productDescription":"Report: 16 p.; 1 Plate: 33.60 x 27.47 inches","costCenters":[],"links":[{"id":490821,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0073/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":490820,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0073/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397538,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8071.htm"},{"id":146640,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0073/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Connecticut, Massachusetts, New York","otherGeospatial":"Bashbish Falls quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.5,\n              42\n            ],\n            [\n              -73.375,\n              42\n            ],\n            [\n              -73.375,\n              42.125\n            ],\n            [\n              -73.5,\n              42.125\n            ],\n            [\n              -73.5,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db66998c","contributors":{"authors":[{"text":"Hartshorn, Joseph H.","contributorId":89862,"corporation":false,"usgs":true,"family":"Hartshorn","given":"Joseph","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":168786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atherton, J. S.","contributorId":98737,"corporation":false,"usgs":true,"family":"Atherton","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":168787,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3221,"text":"cir489 - 1964 - A magnetic anomaly of possible economic significance in southeastern Minnesota","interactions":[],"lastModifiedDate":"2018-01-02T19:49:02","indexId":"cir489","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"489","title":"A magnetic anomaly of possible economic significance in southeastern Minnesota","docAbstract":"An aeromagnetic survey in southeastern Minnesota by the U. S. Geological Survey in cooperation with the State of Minnesota has revealed a high-amplitude, linear, and narrow magnetic feature that suggests a possible source of Precambrian iron-formation of economic value. \r\n\r\nFor the past few years the U. S. Geological Survey has been conducting detailed geophysical studies of the midcontinent gravity anomaly--a broad, high-amplitude feature that extends from Lake Superior through the States of Minnesota, Iowa, Nebraska, and part of Kansas. As part of this study an aeromagnetic survey of the southern part of the State was made in cooperation with the State of Minnesota during the summer of 1963, in which a linear high-amplitude anomaly of the order of 4,000 gammas was discovered. Because of the high amplitude, the linearity, and the narrowness of the magnetic feature, it is believed the source may be Precambrian iron-formation of possible economic value. \r\n\r\nThe anomalous area is in Fillmore County, approximately between the towns of Lanesboro and Peterson in the extreme southeastern part of the State. (See figures 1 and 2.) At the site of the anomaly, Cambrian sedimentary rocks occur in the valley of the Root River, and Ordovician rocks (nearly flat lying) mantle the upland areas. \r\n\r\nThe uplands are largely covered by glacial deposits, which are relatively thin (Paul K. Sims, written communication, 1964). Depths to the Precambrian are estimated to range from 500 feet to 1,000 feet below the surface. \r\n\r\nThe aeromagnetic map shown in figure 2 was compiled from continuous magnetic profiles made along east-west flight lines 1,000 feet above ground, and spaced approximately 1 mile apart. Contour intervals of 20, 100, and 500 gammas were used depending on the intensity. The instrument for the survey was a flux-gate type magnetometer (AN/ASQ-3A) which measures total-field variations. The contour map displays variations in magnetic pattern which are typical of shallow Precambrian rocks. Anomalies of the order of 1,000 gammas are shown along the east and west edges of the map. The outstanding feature is the previously mentioned linear positive anomaly that trends northeast and reaches a peak of 3,960 gammas. The positive anomaly is contoured from data on four consecutive profiles, but only two show high amplitudes. The high-amplitude anomalies along traverses 1 and 2 are shown in figure 3. \r\n\r\nDepth calculations suggest that the source of the anomaly lies about 1,000 feet below the surface. Assuming a dikelike source and magnetization resulting entirely from induction in the earth's field, several calculations were made in an attempt to fit the magnetic profile taken along the line AA' (see figs. 2 and 4), considered to be a typical cross-section of the magnetic anomaly. Comparisons are shown between observed and computed profiles. The fixed parameters used were (a) distance from detector to source of 2,000 ft; width of dike of 5,000 ft; dip of dike of 75?, 90?, 105? , and 120? , as shown. The best fit occurs when the dike is vertical or dips 75? to the southwest. For these cases, the susceptibility, k, is computed to be 0.016 c.g.s, units, and is comparable to k = 0.02+ calculated by Bath (1962) for the relatively unmetamorphosed iron-formation of the Main Megabi district in Minnesota where the induced magnetization was most likely the dominant magnetization. If the dominant magnetization for the anomaly in Fillmore County were remanent rather than induced, the economic importance of the anomaly would be greatly reduced. \r\n\r\nThis anomaly seems sufficiently promising to warrant further geologic and geophysical investigation. Detailed ground magnetic and electrical studies would be useful to delineate the feature. In the final analysis, however, the presence of iron-formation can be determined only by the drill.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir489","usgsCitation":"Zietz, I., 1964, A magnetic anomaly of possible economic significance in southeastern Minnesota: U.S. Geological Survey Circular 489, 5 p. :maps ;27 cm., https://doi.org/10.3133/cir489.","productDescription":"5 p. :maps ;27 cm.","costCenters":[],"links":[{"id":138944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1964/0489/report-thumb.jpg"},{"id":30214,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1964/0489/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae1de","contributors":{"authors":[{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":146462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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