{"pageNumber":"6244","pageRowStart":"156075","pageSize":"25","recordCount":165658,"records":[{"id":16559,"text":"ofr55198 - 1955 - Preliminary geologic evaluation of the Chena area, Alaska","interactions":[],"lastModifiedDate":"2024-01-17T19:57:39.053257","indexId":"ofr55198","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-198","title":"Preliminary geologic evaluation of the Chena area, Alaska","docAbstract":"<p>It seems fitting at this session of the Alaska Science Conference, the first to be held in the Fairbanks area, to give a preliminary summary of the practical results of a geologic investigation of the Chena area east of Fairbanks. The work was done by the Geological Survey in 1950. One important objective of the study was to consider some of the geologic problems affecting development of the land for commercial and agricultural use -- especially to outline the parts of the area that are subject to possible ground subsidence and differential settling because of melting of ground ice masses in permafrost following clearing of the land for agriculture and for construction.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr55198","usgsCitation":"Williams, J.R., 1955, Preliminary geologic evaluation of the Chena area, Alaska: U.S. Geological Survey Open-File Report 55-198, 5 p., https://doi.org/10.3133/ofr55198.","productDescription":"5 p.","costCenters":[],"links":[{"id":424518,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0198/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148868,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1955/0198/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Chena area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -147.57123249956956,\n              64.90367711238932\n            ],\n            [\n              -147.57123249956956,\n              64.81616434255002\n            ],\n            [\n              -147.02328938433524,\n              64.81616434255002\n            ],\n            [\n              -147.02328938433524,\n              64.90367711238932\n            ],\n            [\n              -147.57123249956956,\n              64.90367711238932\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66982d","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":173054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16163,"text":"ofr55177 - 1955 - Pegmatites of the Middletown area, Connecticut","interactions":[{"subject":{"id":16163,"text":"ofr55177 - 1955 - Pegmatites of the Middletown area, Connecticut","indexId":"ofr55177","publicationYear":"1955","noYear":false,"title":"Pegmatites of the Middletown area, Connecticut"},"predicate":"SUPERSEDED_BY","object":{"id":36012,"text":"b1042Q - 1958 - Pegmatites of the Middletown area, Connecticut","indexId":"b1042Q","publicationYear":"1958","noYear":false,"chapter":"Q","title":"Pegmatites of the Middletown area, Connecticut"},"id":1}],"supersededBy":{"id":36012,"text":"b1042Q - 1958 - Pegmatites of the Middletown area, Connecticut","indexId":"b1042Q","publicationYear":"1958","noYear":false,"title":"Pegmatites of the Middletown area, Connecticut"},"lastModifiedDate":"2025-06-02T15:46:16.820927","indexId":"ofr55177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-177","title":"Pegmatites of the Middletown area, Connecticut","docAbstract":"<p>The pegmatites of the Middletown area in Connecticut have been mined almost continuously for feldspar and muscovite mica since about 1865, Pegmatites in this and other areas have recently become the subject of renewed interest because pegmatites are the potential source of beryl, the ore mineral of beryllium. During 1948 to 1950, the Geological Survey studied and mapped the pegmatites in an area of about 58 square miles near Middletown. The primary objectives of the mapping were to determine beryllium resources of the Middletown area, and to ascertain relationships of beryl-bearing pegmatites to non-beryl-bearing pegmatites and to type of wall rock.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr55177","usgsCitation":"Stugard, F., 1955, Pegmatites of the Middletown area, Connecticut: U.S. Geological Survey Open-File Report 55-177, Report: 92 p.; 2 Figures: 18.29 x 37.10 inches and 14.09 x 21.88 inches, https://doi.org/10.3133/ofr55177.","productDescription":"Report: 92 p.; 2 Figures: 18.29 x 37.10 inches and 14.09 x 21.88 inches","costCenters":[],"links":[{"id":489409,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1955/0177/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":489408,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1955/0177/figure-2.pdf","text":"Figure 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,{"id":42885,"text":"ofr55169 - 1955 - Preliminary geologic map of the Lothair quadrangle, Montana","interactions":[{"subject":{"id":42885,"text":"ofr55169 - 1955 - Preliminary geologic map of the Lothair quadrangle, Montana","indexId":"ofr55169","publicationYear":"1955","noYear":false,"title":"Preliminary geologic map of the Lothair quadrangle, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":35851,"text":"b1071E - 1959 - Geology of the lower Marias River area, Chouteau, Hill, and Liberty Counties, Montana","indexId":"b1071E","publicationYear":"1959","noYear":false,"chapter":"E","title":"Geology of the lower Marias River area, Chouteau, Hill, and Liberty Counties, Montana"},"id":1}],"supersededBy":{"id":35851,"text":"b1071E - 1959 - Geology of the lower Marias River area, Chouteau, Hill, and Liberty Counties, Montana","indexId":"b1071E","publicationYear":"1959","noYear":false,"title":"Geology of the lower Marias River area, Chouteau, Hill, and Liberty Counties, Montana"},"lastModifiedDate":"2019-06-21T12:11:58","indexId":"ofr55169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-169","title":"Preliminary geologic map of the Lothair quadrangle, Montana","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr55169","usgsCitation":"Smith, J.F., 1955, Preliminary geologic map of the Lothair quadrangle, Montana: U.S. Geological Survey Open-File Report 55-169, 1 Plate: 27.49 x 33.26 inches, https://doi.org/10.3133/ofr55169.","productDescription":"1 Plate: 27.49 x 33.26 inches","costCenters":[],"links":[{"id":364903,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1955/0169/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1955/0169/report-thumb.jpg"}],"country":"United States","state":"Montana","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b12c","contributors":{"authors":[{"text":"Smith, J. Fred","contributorId":65522,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"","middleInitial":"Fred","affiliations":[],"preferred":false,"id":227328,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20703,"text":"ofr55153 - 1955 - Geology and ore deposits in the Reid Inlet area, Glacier Bay, Alaska, with added notes on a mineralized zone near Lituya Bay","interactions":[{"subject":{"id":20703,"text":"ofr55153 - 1955 - Geology and ore deposits in the Reid Inlet area, Glacier Bay, Alaska, with added notes on a mineralized zone near Lituya Bay","indexId":"ofr55153","publicationYear":"1955","noYear":false,"title":"Geology and ore deposits in the Reid Inlet area, Glacier Bay, Alaska, with added notes on a mineralized zone near Lituya Bay"},"predicate":"SUPERSEDED_BY","object":{"id":47363,"text":"b1058B - 1959 - Geology and ore deposits in the Reid Inlet area, Glacier Bay, Alaska","indexId":"b1058B","publicationYear":"1959","noYear":false,"chapter":"B","title":"Geology and ore deposits in the Reid Inlet area, Glacier Bay, Alaska"},"id":1}],"supersededBy":{"id":47363,"text":"b1058B - 1959 - Geology and ore deposits in the Reid Inlet area, Glacier Bay, Alaska","indexId":"b1058B","publicationYear":"1959","noYear":false,"title":"Geology and ore deposits in the Reid Inlet area, Glacier Bay, Alaska"},"lastModifiedDate":"2023-10-02T19:21:15.399065","indexId":"ofr55153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-153","title":"Geology and ore deposits in the Reid Inlet area, Glacier Bay, Alaska, with added notes on a mineralized zone near Lituya Bay","docAbstract":"<p>A gold-bearing area of about 7 1/2 square miles, first discovered by Mr. Joseph Ibach in 1924, exists near the head of Glacier Bay between Reid and Lamplugh glaciers.</p><p>The dominant rock type in the area is granodiorite which is intruded into bedded rocks that may be of Paleozoic age. The bedded rocks consist of conglomerate, limestone, and black graphitic schist. A light-colored quartz diorite younger than the granodiorite crops out south of the mapped area.</p><p>Most of the ore deposits are found in fissure type quartz veins. These occur in both the granodiorite and in the older bedded rocks. The mineralizing solutions which brought in the gold have altered the country rock for as much as a few tens of feet to each side of the fissures. Locally, this altered rock is gold-bearing, but in the places sampled the gold content was found to be too low to permit profitable mining.</p><p>Most of the quartz veins tend to be lenticular, both horizontally and vertically, and the gold tends to be concentrated in discrete spots along the veins. These factors tend to make the ore spotty and its location unpredictable. This has given rise to the concept that the ore in the area has a tendency not to continue below the surface. Geologically there appears to be no reason to believe that gold mineralization is confined to surface outcrop.</p><p>The Leroy and Rainbow properties are the only two that have yielded significant quantities of gold within the mapped area, but the veins on the Highland Chief and probably the Rambler claims appear to be of sufficient size and grade to be potential ore producers.&nbsp;</p><p>The LeRoy mine is the largest in the area. The ore body consisted of a fissure type quartz vein averaging between 2 and 3 feet in width with a length of about 60 feet, but in 1954, all of the ore in the main vein had been mined out above the main working level. Ore probably amounting to several hundreds of tons was mined and milled from the Rainbow vein.</p><p>The results of an investigation of a mineralized area near Lituya Bay is included in this report. The mineralized material consists of hydrothermally altered rock found in volcanic rocks believed to be of Mesozoic age. 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