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Normal faults of four distinct systems cut the thrust plates, and in Late Cretaceous time, stocks of biotite granite, abnormally rich in beryllium, tin, boron and certain other trace elements, pierced the thrust plates. In part following the intrusion of the granites, a strong set of normal faults developed striking N. 60°-85° E. through the central York Mountains and locally these faults cut the granites. Dikes of granite, rhyolite porphyry, and lamprophyre were injected into some of these faults, the lamprophyres being younger. Trace elements in the lamprophyres prove they are mafic rocks probably derived from the lama, and that they cannot be related genetically to granite. Shortly after the intrusion of lamprophyre dikes, ore deposits of tin, beryllium, and fluorite were formed from solutions probably derived from deeply-buried hot granite where the granite was ruptured by normal faults. Ore shoots were localized beneath thrust faults where the faults are intruded by dikes, and a major ore-bearing structure, the Rapid River fault, is mineralized for half its length for a distance of eight miles. The tin deposits contain cassiterite and stannite in topaz greisen with abundant sulfides of copper, lead, zinc, and iron, as well as wolframite. The beryllium deposits contain fluorite, chrysoberyl, diaspore, muscovite, and tourmaline, with trace to small amounts of euclase, bertrandite, helvite, phenikite(?), todorokite and hematite. Beryl occurs sparingly in late veins of quartz and fluorite. Chrysoberyl is the earliest and commonest beryllium mineral, followed by euclase and bertrandite, and then phenakite(?) and beryl. Helvite is restricted to banded skarns near granite, and which consist of magnetite and fluorite. Throughout the district, a strong zonation is displayed from tin deposits in greisen through transitional veins of sulfide minerals with fluorite and chrysoberyl to fluorite-beryllium deposits and thence to barren veins of silica and fluorite with trace amounts of beryllium. This zonal arrangement of deposits probably will be found elsewhere in the world where greisen tin deposits occur in carbonate rocks. The geochemical cycle of the trace elements Be, Sn, W, B, Li, Cu, Pb, Zn and Nb shows that these elements were enriched in the biotite granites and were strongly fractionated among the minerals of granites. Fran the granites, these rare elements moved outward into contact rocks and ore deposits. During the supergene cycle, clear geochemical anomalies were formed in stream sediments, soils and plants near ore deposits, and geochemical prospecting led to the discovery of the beryllium lodes. With the possible exception of zinc and niobium, the rare elements that are associated in the rocks and ores remain associated in the supergene processes. Fixation of zinc in clay soil and tundra plants may account for the relatively small amount of zinc in strew sediments.</p><p>Datable Pleistocene events in the York Mountains begin with the Yarmouth Interglaciation when the York Terrace, a wide marine platform, was cut. In Illinoian time, the York Terrace was uplifted almost 400 feet, and during the Sangamon Interglaciation a second marine platform (Lost River Terrace) was cut and is not deformed. During Wisconsin time the widespread York Glaciation was followed by the more restricted Mint River Glaciation. Because uplift of the York Terrace extended into the Bering Strait, it is probable that prior to the uplift in Illinoian time the Bering Strait was a seaway and a barrier to land migration rather than a land bridge.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65142","usgsCitation":"Sainsbury, C., 1965, Geology and ore deposits of the central York Mountains, western Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 65-142, Report: 149 p.; 15 Plates: 20.55 x 27.89 inches or smaller; 8 Tables: 20.88 x 30.29 inches or smaller, https://doi.org/10.3133/ofr65142.","productDescription":"Report: 149 p.; 15 Plates: 20.55 x 27.89 inches or smaller; 8 Tables: 20.88 x 30.29 inches or 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,{"id":6111,"text":"pp474B - 1965 - Geology and uranium deposits of Elk Ridge and vicinity, San Juan County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"pp474B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"474","chapter":"B","title":"Geology and uranium deposits of Elk Ridge and vicinity, San Juan County, Utah","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1963","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp474B","usgsCitation":"Lewis, R., and Campbell, R., 1965, Geology and uranium deposits of Elk Ridge and vicinity, San Juan County, Utah: U.S. Geological Survey Professional Paper 474, p.  B1-B69, https://doi.org/10.3133/pp474B.","productDescription":"p.  B1-B69","costCenters":[],"links":[{"id":112708,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0474b/report.pdf","size":"11890","linkFileType":{"id":1,"text":"pdf"}},{"id":140174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0474b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6841d9","contributors":{"authors":[{"text":"Lewis, Richard Quintin","contributorId":91097,"corporation":false,"usgs":true,"family":"Lewis","given":"Richard Quintin","affiliations":[],"preferred":false,"id":152138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Russell H.","contributorId":91074,"corporation":false,"usgs":true,"family":"Campbell","given":"Russell H.","affiliations":[],"preferred":false,"id":152137,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65138,"text":"i460 - 1965 - Map showing foundation and excavation conditions in the Burtonville quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:05","indexId":"i460","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"460","subseriesTitle":"NONE","title":"Map showing foundation and excavation conditions in the Burtonville quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/i460","usgsCitation":"Dobrovolny, E., and Morris, R.H., 1965, Map showing foundation and excavation conditions in the Burtonville quadrangle, Kentucky: U.S. Geological Survey IMAP 460, 1 map., https://doi.org/10.3133/i460.","productDescription":"1 map.","costCenters":[],"links":[{"id":255300,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0460/plate-1.pdf","size":"9765","linkFileType":{"id":1,"text":"pdf"}},{"id":255301,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0460/report.pdf","size":"38","linkFileType":{"id":1,"text":"pdf"}},{"id":255302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0460/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.61749999999999,38.3675 ], [ -83.61749999999999,38.5 ], [ -83.5,38.5 ], [ -83.5,38.3675 ], [ -83.61749999999999,38.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae210","contributors":{"authors":[{"text":"Dobrovolny, Ernest","contributorId":45288,"corporation":false,"usgs":true,"family":"Dobrovolny","given":"Ernest","affiliations":[],"preferred":false,"id":272712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morris, R. H.","contributorId":91853,"corporation":false,"usgs":true,"family":"Morris","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":272713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41128,"text":"ofr6529 - 1965 - Preliminary geologic map of part of the Rapid City West quadrangle, South Dakota","interactions":[{"subject":{"id":41128,"text":"ofr6529 - 1965 - Preliminary geologic map of part of the Rapid City West quadrangle, South Dakota","indexId":"ofr6529","publicationYear":"1965","noYear":false,"title":"Preliminary geologic map of part of the Rapid City West quadrangle, South Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":63246,"text":"gq828 - 1969 - Geologic map of the Rapid City West quadrangle, Pennington County, South Dakota","indexId":"gq828","publicationYear":"1969","noYear":false,"title":"Geologic map of the Rapid City West quadrangle, Pennington County, South Dakota"},"id":1}],"supersededBy":{"id":63246,"text":"gq828 - 1969 - Geologic map of the Rapid City West quadrangle, Pennington County, South Dakota","indexId":"gq828","publicationYear":"1969","noYear":false,"title":"Geologic map of the Rapid City West quadrangle, Pennington County, South 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Richard W.","contributorId":106084,"corporation":false,"usgs":true,"family":"Bayley","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":224848,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52503,"text":"ofr65151 - 1965 - Water resources appraisal of the Anchorage area, Alaska","interactions":[],"lastModifiedDate":"2023-10-20T20:27:13.82275","indexId":"ofr65151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-151","title":"Water resources appraisal of the Anchorage area, Alaska","docAbstract":"<p>At the present, water use in the Anchorage area amounts to about 21 mgd (million gallons per day); of this amount ground water accounts for about 10 mgd. By 1980, 60 mgd may be required to meet the demand.</p><p>The greatest potential problem is overpumping the ground-water reservoir resulting in excessive declines in water levels, which, in turn, might lead to salt-water intrusion. A well-laid plan for conjunctive use of surface and ground water seems to be the most promising means of supplying the expected need of 60 mgd, and of preventing saltwater intrusion of the aquifers.</p><p>Total inflow into the Anchorage hydrologic system amounts to about 180 mgd. Of this amount Ship and South Fork Campbell Creeks contribute about 130 mgd, North Fork Campbell Creek and other streams contribute an estimated 24 mgd, and precipitation and ground-water inflow contribute an estimated 26 mgd.</p><p>Of the total outflow, which must be equivalent to the inflow, Ship and Chester Creeks contribute about 94 mgd, Campbell Creek about 25 mgd, and ground-water pumpage contributes an assumed amount of approximately 10 mgd. The difference of 50 mgd between inflow and outflow presumably is accounted for; by submarine discharge beneath Cook Inlet and evapotranspiration.</p><p>Surface and subsurface storage of excess stream discharge during periods of high flow can overcome the problem of water shortages during periods of greatest demand. Surface storage can be accomplished by construction of an additional dam on Ship Creek. Natural ground-water storage can be supplemented by spreading techniques to increase the amount of ground-water recharge. Additional recharge can be provided by returning air-conditioning water to the aquifer through recharge wells. Recharge along the coastline would be a means of maintaining a fresh-water barrier against salt-water intrusion.</p><p>The area with the greatest potential for ground-water development is along Ship Creek east and north of Mountain View. The alluvial fan east of Mountain View seems favorable for installation of deep wells; and withdrawal of ground water in this area is not likely to result in salt-water intrusion. Similar favorable conditions exist in the alluvial fan areas of North and South Forks Campbell Creek. Infiltration galleries in alluvial deposits along Ship Creek are a relatively inexpensive and convenient means of withdrawing water.</p><p>To plan for orderly and economical development of the Anchorage area's water resources, geologic and hydrologic studies are needed. An expanded network of stream-gaging stations and observation wells is needed. Deep wells near the coastline are needed to monitor any changes in chemical quality of ground water that would indicate impending salt-water intrusion. Borehole geophysical studies and pumping tests are needed to define the boundaries and hydraulic characteristics of the aquifers. The primary goal of these and other supplementing studies would be to provide the information needed to construct an electric-analog model of the Anchorage hydrologic system. Such a model would provide a means of assessing quantitatively alternative methods of water development.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65151","usgsCitation":"Sommers, D.A., and Marcher, M.V., 1965, Water resources appraisal of the Anchorage area, Alaska: U.S. Geological Survey Open-File Report 65-151, 34 p., https://doi.org/10.3133/ofr65151.","productDescription":"34 p.","costCenters":[],"links":[{"id":422019,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0151/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177656,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0151/report-thumb.jpg"}],"country":"United States","state":"Alaska","city":"Anchorage","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -150.0148756092472,\n              61.267767521656054\n            ],\n            [\n              -150.0148756092472,\n              61.119542274353336\n            ],\n            [\n              -149.69627209362233,\n              61.119542274353336\n            ],\n            [\n              -149.69627209362233,\n              61.267767521656054\n            ],\n            [\n              -150.0148756092472,\n              61.267767521656054\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f8302","contributors":{"authors":[{"text":"Sommers, David A.","contributorId":96761,"corporation":false,"usgs":true,"family":"Sommers","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":245455,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marcher, Melvin V.","contributorId":11590,"corporation":false,"usgs":true,"family":"Marcher","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":245454,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15753,"text":"ofr65141 - 1965 - Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","interactions":[{"subject":{"id":15753,"text":"ofr65141 - 1965 - Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"ofr65141","publicationYear":"1965","noYear":false,"title":"Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":6313,"text":"pp897 - 1977 - Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"pp897","publicationYear":"1977","noYear":false,"title":"Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska"},"id":1},{"subject":{"id":15754,"text":"ofr59106 - 1959 - Preliminary report on sedimentary and metamorphic rocks in part of the Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"ofr59106","publicationYear":"1959","noYear":false,"title":"Preliminary report on sedimentary and metamorphic rocks in part of the Romanzof Mountains, Brooks Range, northeastern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":15753,"text":"ofr65141 - 1965 - Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"ofr65141","publicationYear":"1965","noYear":false,"title":"Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska"},"id":2}],"supersededBy":{"id":6313,"text":"pp897 - 1977 - Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"pp897","publicationYear":"1977","noYear":false,"title":"Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska"},"lastModifiedDate":"2024-03-25T18:59:14.568941","indexId":"ofr65141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-141","title":"Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","docAbstract":"<p>This remote 700 square mile area in the Brooks Range is topographically rugged and geologically diverse; it contains a granitic pluton, low-grade metamorphic rocks, sedimentary rocks, and mafic igneous rocks, as well as glacial features.</p><p>Rocks of sedimentary origin include from oldest to youngest:</p><p>1.Neruokpuk Formation Middle and Upper Devonian(?), more than 4000 feet thick, a variety of units which represent the greenschist facies, including quartzitic- and schistose-feldspathic graywacke; phyllite, argillite, and slate, as well as dark limestone, sandy limestone, and silicified carbonate rocks. The succession of units in parts of the area is uncertain. Correlations between these units and with others in the eastern Brooks Range are provisional.</p><p>2.Kekiktuk Conglomerate and Kayak(?) Shale (Upper Devonian(?) to Upper Mississippian), a single map unit, from absent(?) to 400+ feet thick, containing dark shale Kayak(?) in its uppermost part and quartzite, interbedded dark shale, and some pebble- to boulder-conglomerate in the locally absent lower part (Kekiktuk). The unit overlies the Neruokpuk with angular unconformity, which may reflect either a pre-Kayak(?) or pre-Kekiktuk hiatus or both.</p><p>3.Lisburne Group, almost entirely carbonate rocks, and relatively thin in this area, 600 to 800 feet thick. Alapah Limestone (Upper Mississippian), to 560 feet thick, includes gray sandy, crystalline, and cherty limestone; minor dark shale; and dark cherty carbonate rocks in the upper part. The lower contact is gradational with the Kayak(?). Wahoo(?) Limestone (Pennsylvanian(?) to Permian) conformably overlies the Alapah, is absent to 200+ feet thick, and is characterized by light-gray crinoidal limestones in its upper part.</p><p>4. Sadlerochit Formation, consisting of three intraconformable units: ferruginous sandstone member (Permian) of ironstained orthoquartzite and dark slate, 175 to 240 feet thick which unconformably overlies the Wahoo(?) and Alapah Limestones; shale member of dark shale, slate, and minor quartzite averaging 400 feet in thickness; and quartzite member (Lower(?) Triassic), 700 feet thick, mostly orthoquartzite with minor shale and conglomerate. The basal clastics were probably shed from the north.</p><p>5.Shublik Formation (Middle(?) and Upper Triassic), 600 to 700 feet thick, with the thin phosphatic sandstone member overlain by dark phosphatic limestones and limy shales of the limestone member.</p><p>6.Kingak Formation (Jurassic), more than 1000 feet thick. The siltstone member, resistant sandstone and siltstone 75 to 150 feet thick, is overlain by an undetermined thickness of black shale. The basal part contrasts sharply with the underlying Shublik, indicating possible disconformity.</p><p>7.Ignek(?) Formation (Cretaceous), represented in the foothills where lithic graywacke, shale, and coaly shale constitute the few exposures examined.</p><p>8.Glacial and glaciofluvial materials of five advances recognized on the basis of morphology and position, which are tentatively correlated with five glaciations 15 miles west of the area.</p><p>9. Recent alluvial and colluvial deposits including fans which appear to represent at least three stages of encroachment.<br></p><p>The Ramanzof granite, exposed in the Okpilak batholith and Jago stock, is mostly light-gray quartz monzonite to granite, and contains essential quartz, perthitic microcline, albite-oligoclase, and partly chloritized biotite. Limited modal and chemical data are presented. Three textural facies are: 1) porphyritic (marginal), with abundant large microcline megacrysts; 2) variable (middle to marginal), which exhibits textural and mineralogical banding; and 3) coarse (inner to marginal), which is gneissoid to equigranular. Facies relationships appear to be mostly gradational but may be locally intrusive. Some schistose metasedimentary(?) rock occurs in the granite. Aplite dikes, inclusions, tourmaline veins and replacements, and chlorite and quartz veins are locally common, as well as quartz monzonite and mafic igneous dikes. Contacts with Neruokpuk Formation rocks are mostly abrupt, concordant to cross-cutting, and locally adjoin tactite and hornfels of the albite-epidote-hornfels and hornblende-hornfels facies. Contacts with Kekiktuk Conglomerate are apparently gradational through a schistoze zone. Both primary and secondary structural elements are present in the Romanzof in granite. Textural and mineralogical banding and, in general, feldspar foliation are considered to be primary in origin; biotite foliation, gneissic and schistose foliation, and schistose zones are considered secondary. Lead-alpha age of zircons appears to be Late Devonian, K-Ar age of biotite is Cretaceous, possibly indicating updating by later reheating. Field age relationships are inconclusive but suggest pre-Kayak(?) (Upper Devonian) granite emplacement. The pluton is interpreted to be essentially the product of melt crystallization, synorogenically emplaced by forceful injection with minor stoping, and may include marginally granitized rock.<br></p><p>Mafic igneous rocks of altered basaltic composition (greenstones) include dikes in granitic and Neruokpuk Formation rocks, and volcanics(?). A late Paleozoic age is suggested for them.</p><p>Structural grain strikes east-northeast; south-dipping elements are common. Structures include the major positive nature of the area (first order), relatively broad folds (second order) which contain small tight folds (third order). Related south-dipping cleavage, schistosity, and biotite foliation in granite in the northern part of the area are cut by prominent sets of transverse joints and faults. Other features are longitudinal normal and reverse faults, at least one large-scale overthrust fault, and sheared zones in granite with possible attendant retrograde metamorphism.</p><p>Although Mesozoic and Tertiary deformational features are dominant in northern Alaska, the Romanzof area may have been part of a Late Devonian orogenic belt continuous with one in northern Canada. Three alternate trends of such a belt in northern Alaska are discussed, but evidence is inconclusive.</p><p>The mineral potential of the area is largely unknown. Minor amounts of metallic sulfides and oxides are present in granite and Neruokpuk Formation rocks. Analyses of stream silt samples suggest the possibility of tin and beryllium potential. 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,{"id":33935,"text":"b1198B - 1965 - Geochemical prospecting investigations in the Copper Belt of Vermont","interactions":[],"lastModifiedDate":"2012-02-02T00:09:27","indexId":"b1198B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1198","chapter":"B","title":"Geochemical prospecting investigations in the Copper Belt of Vermont","language":"ENGLISH","publisher":"U.S. Gov. Print. Off.,","doi":"10.3133/b1198B","usgsCitation":"Canney, F.C., 1965, Geochemical prospecting investigations in the Copper Belt of Vermont: U.S. Geological Survey Bulletin 1198, p. B1-B28, ill. ;23 cm., https://doi.org/10.3133/b1198B.","productDescription":"p. B1-B28, ill. ;23 cm.","costCenters":[],"links":[{"id":163696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1198b/report-thumb.jpg"},{"id":61816,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1198b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adeb0","contributors":{"authors":[{"text":"Canney, Frank Cogswell","contributorId":70776,"corporation":false,"usgs":true,"family":"Canney","given":"Frank","email":"","middleInitial":"Cogswell","affiliations":[],"preferred":false,"id":212193,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32747,"text":"pp392B - 1965 - Mineralogy and stratigraphy of the lower part of the Pierre Shale, South Dakota and Nebraska","interactions":[{"subject":{"id":32747,"text":"pp392B - 1965 - Mineralogy and stratigraphy of the lower part of the Pierre Shale, South Dakota and Nebraska","indexId":"pp392B","publicationYear":"1965","noYear":false,"chapter":"B","title":"Mineralogy and stratigraphy of the lower part of the Pierre Shale, South Dakota and Nebraska"},"predicate":"IS_PART_OF","object":{"id":5635,"text":"pp392 - 1976 - Studies of the Pierre Shale in the Northern Great Plains","indexId":"pp392","publicationYear":"1976","noYear":false,"title":"Studies of the Pierre Shale in the Northern Great Plains"},"id":1}],"isPartOf":{"id":5635,"text":"pp392 - 1976 - Studies of the Pierre Shale in the Northern Great Plains","indexId":"pp392","publicationYear":"1976","noYear":false,"title":"Studies of the Pierre Shale in the Northern Great Plains"},"lastModifiedDate":"2017-08-09T14:35:09","indexId":"pp392B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"392","chapter":"B","title":"Mineralogy and stratigraphy of the lower part of the Pierre Shale, South Dakota and Nebraska","language":"ENGLISH","doi":"10.3133/pp392B","usgsCitation":"Schultz, L., 1965, Mineralogy and stratigraphy of the lower part of the Pierre Shale, South Dakota and Nebraska: U.S. Geological Survey Professional Paper 392, p. B1-B19, https://doi.org/10.3133/pp392B.","productDescription":"p. B1-B19","costCenters":[],"links":[{"id":119252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0392b/report-thumb.jpg"},{"id":60677,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0392b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60678,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0392b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60679,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0392b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699df3","contributors":{"authors":[{"text":"Schultz, L.G.","contributorId":62617,"corporation":false,"usgs":true,"family":"Schultz","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":209087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57052,"text":"b1181H - 1965 - Geologic reconnaissance along the Alaska Highway, Delta River to Tok Junction, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:12:04","indexId":"b1181H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1181","chapter":"H","title":"Geologic reconnaissance along the Alaska Highway, Delta River to Tok Junction, Alaska","language":"ENGLISH","doi":"10.3133/b1181H","usgsCitation":"Holmes, G., 1965, Geologic reconnaissance along the Alaska Highway, Delta River to Tok Junction, Alaska: U.S. Geological Survey Bulletin 1181, p. H1-H19, https://doi.org/10.3133/b1181H.","productDescription":"p. H1-H19","costCenters":[],"links":[{"id":109470,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20950.htm","linkFileType":{"id":5,"text":"html"},"description":"20950"},{"id":100600,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1181h/report.pdf","size":"1518","linkFileType":{"id":1,"text":"pdf"}},{"id":100601,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1181h/plate-1.pdf","size":"6968","linkFileType":{"id":1,"text":"pdf"}},{"id":181978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1181h/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68854b","contributors":{"authors":[{"text":"Holmes, G.W.","contributorId":69215,"corporation":false,"usgs":true,"family":"Holmes","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":256181,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52497,"text":"ofr65140 - 1965 - Floods in New York-1964","interactions":[],"lastModifiedDate":"2012-02-02T00:11:23","indexId":"ofr65140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-140","title":"Floods in New York-1964","language":"ENGLISH","doi":"10.3133/ofr65140","usgsCitation":"Robison, F., 1965, Floods in New York-1964: U.S. Geological Survey Open-File Report 65-140, 22 p., https://doi.org/10.3133/ofr65140.","productDescription":"22 p.","costCenters":[],"links":[{"id":179513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db5453f3","contributors":{"authors":[{"text":"Robison, F.L.","contributorId":41889,"corporation":false,"usgs":true,"family":"Robison","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":245442,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52491,"text":"ofr65125 - 1965 - Records of wells and test holes, materials tests, and chemical analyses of water in the Assabet River basin, Massachusetts","interactions":[],"lastModifiedDate":"2019-06-04T14:52:43","indexId":"ofr65125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-125","title":"Records of wells and test holes, materials tests, and chemical analyses of water in the Assabet River basin, Massachusetts","docAbstract":"<p>The Assabet River, located in Worcester and Middlesex Counties in eastern Massachusetts, drains an area of approximately 177 square miles. The area includes all or a portion of the following towns: Acton, Boxborough, Carlisle, Concord, Hudson, Littleton, Marlborough, Maynard, Stow, Sudbury, and Westford in Middlesex County; Berlin, Bolton, Boylston, Clinton, Grafton, Harvard, Northborough, Shrewsbury, and Westborough in Worcester County (see plate 1 in pocket).</p><p>This report presents data collected as part of an investigation of the ground-water resources in the Assabet River basin by the U.S. Geological Survey in cooperation with the Massachusetts Water Resources Commission. The data have been prepared for release in order to make available to the public basic ground-water data that will be useful in the planning of water-resources development.</p><p>The data in this report were collected intermittently from 1939 to 1964 by H. A. Wilde, H. L. Pree, H. N. Halberg, J. A. Baker, R. W. Macomber, W. B. Fleck, and S. J. Pollock. The selected data in tables 2, 3, 4, and 5 represent those wells, test wells, and borings that were deemed representative of any given location. Data of some one hundred wells and test wells and over one thousand bridge and roadway borings are not included in this report, but may be inspected at the U.S. Geological Survey, Ground Water Branch, 211 Congress Street, Boston, Massachusetts. Tables 6-9 include data on chemical analyses of water samples, physical and hydrologic properties of materials samples, and water-table measurements made during the years 1961 through 1964. The geologic units used in tables 2 and 3 are described in table 1. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65125","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Water Resources Commission","usgsCitation":"Pollock, S., and Fleck, W.B., 1965, Records of wells and test holes, materials tests, and chemical analyses of water in the Assabet River basin, Massachusetts: U.S. Geological Survey Open-File Report 65-125, Report: 45 p.; 1 Plate: 41.16 x 54.13 inches, https://doi.org/10.3133/ofr65125.","productDescription":"Report: 45 p.; 1 Plate: 41.16 x 54.13 inches","costCenters":[],"links":[{"id":364337,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0125/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364338,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0125/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0125/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Massachusetts","otherGeospatial":"Assabet River basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635624","contributors":{"authors":[{"text":"Pollock, Samuel J.","contributorId":27555,"corporation":false,"usgs":true,"family":"Pollock","given":"Samuel J.","affiliations":[],"preferred":false,"id":245432,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleck, William B.","contributorId":17587,"corporation":false,"usgs":true,"family":"Fleck","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":245431,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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