The Solomon D-6 15- by 30-minute quadrangle lies 20 miles northeast of Nome, Alaska, and adjoins on the east the Nome D-l quadrangle mapped by Hummel (1962b) and on the west the Solomon D-5 quadrangle mapped by Smith (1910).
Placer gold has been produced from Iron Creek and many of its tributaries, and a small amount of copper was shipped from the Wheeler mine. Many lode prospects contain small amounts of copper in silicified limestone within and near the base of thrust plates of carbonate rocks. Other lodes consist of well-defined veins containing gold and base-metal sulfide minerals, but none has been commercially productive.
Mapped rock units include the \"York Slate,\" of Precambrian age, which consists of a highly deformed and thick sequence of graphitic calcareous siltite, which contains thin limestone beds and intercalated(?) volcaniclastic rocks, and Paleozoic carbonate rocks, which have been converted largely to marble and schistose marble. Along and near the Kigluaik Mountains in the north part of the quadrangle, quartzo-feldspathic gneisses of Precambrian age are intruded by fine-grained granite. A very thick sequence of schistose thin-bedded argillaceous and dolomitic limestone overlies the York Slate and is correlative with a similar rock originally mapped in the York Mountains.
Surficial deposits, consisting principally of moraine and stream-reworked moraine, mantle large parts of the quadrangle.
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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"1971, At Palmer Seismology Observatory the countdown ends at earthquake +15: Earthquake Information Bulletin (USGS), v. 3, no. 5, p. 20-25.","productDescription":"6 p.","startPage":"20","endPage":"25","numberOfPages":"6","costCenters":[],"links":[{"id":329704,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","volume":"3","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5807351de4b0841e59e288d3","contributors":{"editors":[{"text":"Posey, Carl A.","contributorId":175126,"corporation":false,"usgs":false,"family":"Posey","given":"Carl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":651259,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":70156927,"text":"70156927 - 1971 - Calculated in situ rock density from gravity observations, UA-1 (Cannikin) emplacement hole, Amchitka Island, Alaska","interactions":[],"lastModifiedDate":"2019-11-12T16:13:41","indexId":"70156927","displayToPublicDate":"2015-09-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Calculated in situ rock density from gravity observations, UA-1 (Cannikin) emplacement hole, Amchitka Island, Alaska","docAbstract":"Gravity observations were made on the ground surface and at a depth of 5,854 feet in drill hole UA-1. Two attempts to measure the free-air gradient utilizing the headframe over the drill hole were unsuccessful owing to mechanical vibrations in the structure. Because of the uncertainty in the measured free-air gradients these values were discarded and the average value (0.09406 mgal/ft) was used in the calculations. The calculated in situ bulk density is 2.36 g/cc. The weighted average bulk density determined from 47 core samples taken in the adjacent UAE-1 drill hole is also 2.36 g/cc. An analysis of selected portions of density logs provides an in situ bulk density of 2.37 g/cc.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70156927","usgsCitation":"Healey, D., 1971, Calculated in situ rock density from gravity observations, UA-1 (Cannikin) emplacement hole, Amchitka Island, Alaska, 10 p., https://doi.org/10.3133/70156927.","productDescription":"10 p.","numberOfPages":"12","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307826,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr474106.JPG"},{"id":308546,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70156927/report.pdf","text":"Report","size":"1,510 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka Island, Aleutian Islands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 178.584136963,\n 51.63677159243599\n ],\n [\n 178.592376709,\n 51.61290019118336\n ],\n [\n 179.21585083,\n 51.3254629443313\n ],\n [\n 179.508361816,\n 51.37520943448463\n ],\n [\n 179.057922363,\n 51.587309751245456\n ],\n [\n 178.628082275,\n 51.67936786087718\n ],\n [\n 178.584136963,\n 51.63677159243599\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f2a9b1e4b0dacf699ec6ac","contributors":{"authors":[{"text":"Healey, D.L.","contributorId":52964,"corporation":false,"usgs":true,"family":"Healey","given":"D.L.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":571167,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70156919,"text":"70156919 - 1971 - Marine terraces of the western Aleutian Islands, Alaska","interactions":[],"lastModifiedDate":"2019-11-12T16:51:00","indexId":"70156919","displayToPublicDate":"2015-09-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Marine terraces of the western Aleutian Islands, Alaska","docAbstract":"The islands of the Rat Islands group, which includes Amchitka Island, have active sea cliffs, well-developed intertidal platforms, and a prominent submarine platform at -100 m. These features have not been disturbed by tectonic activity for the past 17,000 years. The islands of the Delarof Islands group, located east of Amchitka Pass, have inactive sea cliffs and emergent low terraces that indicate relatively recent uplift, possibly as much as 4 m. Higher and older marine terraces on the islands of both groups cannot be correlated, and some tectonic adjustment between the island groups is suggested.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70156919","usgsCitation":"Morris, R.H., 1971, Marine terraces of the western Aleutian Islands, Alaska, ii, 23 p., https://doi.org/10.3133/70156919.","productDescription":"ii, 23 p.","numberOfPages":"28","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308058,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70156919.JPG"},{"id":308543,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70156919/report.pdf","text":"Report"}],"country":"United States","state":"Alaska","otherGeospatial":"Aleutian Islands","tableOfContents":"Measurements of the microwave emission from Arctic Sea ice were made with aircraft at 8 wavelengths ranging from 0.510 to 2.81 cm. The expected contrast in emissivities between ice and water was observed at all wavelengths. Distributions of sea ice and open water were mapped from altitudes up to 11 km in the presence of dense cloud cover.
Different forms of ice also exhibited strong contrasts in emissivity. Emissivity differences of up to 0.2 were observed between two types of ice at the 0.811-cm wavelength. The higher emissivity ice type is tentatively identified as having been formed more recently than the lower emissivity ice.
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M.","contributorId":33336,"corporation":false,"usgs":true,"family":"Pinckney","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":178803,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":178805,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":13221,"text":"ofr7182 - 1971 - Cretaceous plutonic rocks of St. Lawrence Island, Alaska; a preliminary report","interactions":[{"subject":{"id":13221,"text":"ofr7182 - 1971 - Cretaceous plutonic rocks of St. Lawrence Island, Alaska; a preliminary report","indexId":"ofr7182","publicationYear":"1971","noYear":false,"title":"Cretaceous plutonic rocks of St. Lawrence Island, Alaska; a preliminary report"},"predicate":"SUPERSEDED_BY","object":{"id":39571,"text":"pp750D - 1971 - Geological Survey research 1971, Chapter D","indexId":"pp750D","publicationYear":"1971","noYear":false,"chapter":"D","title":"Geological Survey research 1971, Chapter D"},"id":1}],"supersededBy":{"id":39571,"text":"pp750D - 1971 - Geological Survey research 1971, Chapter D","indexId":"pp750D","publicationYear":"1971","noYear":false,"title":"Geological Survey research 1971, Chapter D"},"lastModifiedDate":"2023-12-11T21:55:27.97203","indexId":"ofr7182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-82","title":"Cretaceous plutonic rocks of St. Lawrence Island, Alaska; a preliminary report","docAbstract":"Reconnaissance mapping on St. Lawrence Island, Alaska has revealed seven epizonal granitic plutons of mid-Cretaceous age with a combined outcrop area of about 350 square miles. The plutonic rocks are dominantly quartz monzonite, but include minor amounts of granodiorite, monzonite, syenite, syenodiorite, and alaskite.
The plutons are structurally and petrologically similar to and about the same age as plutons on the Chukotsky Peninsula, U.S.S.R. and in western Alaska. They suggest tectonic continuity between Siberia and Alaska since at least Cretaceous time.
Several mineralized areas containing molybdenum, copper, lead, and zinc sulfides are associated with the plutonic bodies in the western part of the island.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7182","usgsCitation":"Csejtey, B., Patton, W.W., and Miller, T.P., 1971, Cretaceous plutonic rocks of St. Lawrence Island, Alaska; a preliminary report: U.S. Geological Survey Open-File Report 71-82, Report: 17 p.; 4 Plates: 27.32 x 12.98 inches or smaller, https://doi.org/10.3133/ofr7182.","productDescription":"Report: 17 p.; 4 Plates: 27.32 x 12.98 inches or smaller","costCenters":[],"links":[{"id":423416,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0082/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":423415,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0082/figure-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":423414,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0082/figure-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":423413,"rank":4,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1971/0082/table-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":423412,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0082/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146114,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0082/report-thumb.jpg"},{"id":395108,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8665.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"St. Lawrence Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -171.93603515625,\n 62.694309593663185\n ],\n [\n -168.64013671875,\n 62.694309593663185\n ],\n [\n -168.64013671875,\n 64.06259063688063\n ],\n [\n -171.93603515625,\n 64.06259063688063\n ],\n [\n -171.93603515625,\n 62.694309593663185\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6833e8","contributors":{"authors":[{"text":"Csejtey, Bela Jr.","contributorId":61008,"corporation":false,"usgs":true,"family":"Csejtey","given":"Bela","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":167427,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patton, William Wallace Jr.","contributorId":72346,"corporation":false,"usgs":true,"family":"Patton","given":"William","suffix":"Jr.","email":"","middleInitial":"Wallace","affiliations":[],"preferred":false,"id":167428,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":167426,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":6286,"text":"pp705A - 1971 - Inventory of Glaciers in the North Cascades, Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"pp705A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"705","chapter":"A","title":"Inventory of Glaciers in the North Cascades, Washington","docAbstract":"Perennial bodies of ice in the North Cascades having areas of at least 0.1 km2 (square kilometer) are tabulated and classified. The inventory, a contribution to the International Hydrological Decade, includes 756 glaciers, covering 267 km2, about half of the glacier area in the United States south of Alaska. Listings include each glacier's location, drainage basin, area, length, orientation, altitude, and classification as to form, source, surface, nature of terminus, and activity. These glaciers contribute annually about 800 million cubic meters of water to streamflow in the State of Washington.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp705A","collaboration":"A contribution to the International Hydrological Decade","usgsCitation":"Post, A., Richardson, D., Tangborn, W.V., and Rosselot, F., 1971, Inventory of Glaciers in the North Cascades, Washington: U.S. Geological Survey Professional Paper 705, 25 p., https://doi.org/10.3133/pp705A.","productDescription":"25 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":139707,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0705a/report-thumb.jpg"},{"id":12507,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/pp/705-A/index.htm","linkFileType":{"id":5,"text":"html"}},{"id":22066,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0705a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":22067,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0705a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":22068,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0705a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":22069,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0705a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,47 ], [ -123,49 ], [ -120,49 ], [ -120,47 ], [ -123,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49afe4b07f02db5c8c65","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":152449,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richardson, Don","contributorId":64238,"corporation":false,"usgs":true,"family":"Richardson","given":"Don","email":"","affiliations":[],"preferred":false,"id":152448,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tangborn, Wendell V.","contributorId":32152,"corporation":false,"usgs":true,"family":"Tangborn","given":"Wendell","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":152446,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rosselot, F.L.","contributorId":42955,"corporation":false,"usgs":true,"family":"Rosselot","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":152447,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":6197,"text":"pp715A - 1971 - Combined Ice and Water Balances of Gulkana and Wolverine Glaciers, Alaska, and South Cascade Glacier, Washington, 1965 and 1966 Hydrologic Years","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"pp715A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"715","chapter":"A","title":"Combined Ice and Water Balances of Gulkana and Wolverine Glaciers, Alaska, and South Cascade Glacier, Washington, 1965 and 1966 Hydrologic Years","docAbstract":"Glaciers occur in northwestern North America between lat 37 deg and 69 deg N. in two major mountain systems. The Pacific Mountain System, near the west coast, receives large amounts of precipitation, has very mild temperatures, and contains perhaps 90 percent of the glacier ice. The Rocky Mountain or Eastern System, on the other hand, receives nearly an order of magnitude less precipitation, has temperatures that range from subpolar to subtropic, and contains glaciers that are much smaller in both size and total area.\r\n\r\nAs a contribution to the International Hydrological Decade program on combined balances at selected glaciers, the U.S. Geological Survey is conducting studies of ice and water balance on four glaciers in the Pacific Mountain System: Wolverine and Gulkana Glaciers in Alaska, South Cascade Glacier in Washington, and Maclure Glacier in California. Similar data are being collected by other organizations at five glaciers in western Canada, including two in the Rocky Mountain System, and at one glacier in the Rocky Mountain System in northern Alaska.\r\n\r\nGulkana, Wolverine, South Cascade, and Maclure Glaciers have dissimilar mass balances, and each is fairly representative of the glaciers for its particular region. Gulkana Glacier (lat 63 deg 15' N., Alaska Range, Alaska) normally has an equilibrium line at an altitude of 1,800 m (meters), an activity index of about 6 mm/m (millimeters per meter), a winter balance of about 1.0 m, and an annual exchange of about 2.2 m. (Balance values are given in terms of water-equivalent measure; the winter balance of 1 m, for example, indicates a volume of ice equal in mass to a volume of water 1 m in depth covering the area of the glacier.) The normal approximate parameters for the other glaciers studied are as follows: Wolverine Glacier (lat 60 deg 24' N., Kenai Mountains, Alaska) - equilibrium-line altitude 1,200 m, activity index 9 mm/m, winter balance 2.5 m, and annual exchange 5.5 m; South Cascade Glacier (lat 48 deg 22' N., North Cascades, Wash.) - equilibrium-line altitude 1,900 m, activity index 17 mm/m, winter balance 3.1 m, and annual exchange 6.6 m; and Maclure Glacier (lat 37 deg 45' N., Sierra Nevada, Calif.) - equilibrium-line altitude 3,600 m, activity index 23 mm/m, winter balance 2.3 m, and annual exchange 4.6 m.\r\n\r\nMass balances of these four glaciers and their drainage basins are measured annually by standard glaciological techniques. In addition, the hydrologic balance is calculated using streamflow and precipitation measurements. Combining these independent measurements results in fairly well defined values of water and ice balance for the glaciers and drainage basins. A revision of the standard International Hydrological Decade mass-balance system permits combination of annual and stratigraphic terms.\r\n\r\nThe annual balance of South Cascade Glacier at the end of the 1965 hydrologic year was slightly positive (+0.07 m averaged over the glacier), but continued ablation and deficient accumulation in October 1965 resulted in slightly negative net balances for both the glacier and the drainage basin. Factors tending to produce this near-zero balance were the above-average late-winter balance (3.48 m) and the numerous summer snowfalls. Ice ablation averaged about 39 mm of water per day during the main melt season. Runoff during the summer ablation season was lower than the 1958-64 average.\r\n\r\nThe South Cascade Glacier annual balance in 1966 (-0.94 m) was considerably more negative mainly owing to the deficient winter snowpack (the late-winter balance was only 2.52 m) and the warm dry summer. Ice ablation averaged about 44 mm of water per day during the melt season. The loss in storage of this and other glaciers in the North Cascades increased the runoff of many valley streams by approximately 50 percent during August and September.\r\n\r\nThe 1966 Gulkana Glacier annual balance was slightly positive (+0.06 m); on the basis of past observations and the rapid terminus ret","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp715A","collaboration":"A contribution to the International Hydrological Decade","usgsCitation":"Meier, M.F., Tangborn, W.V., Mayo, L.R., and Post, A., 1971, Combined Ice and Water Balances of Gulkana and Wolverine Glaciers, Alaska, and South Cascade Glacier, Washington, 1965 and 1966 Hydrologic Years: U.S. Geological Survey Professional Paper 715, 22 p., https://doi.org/10.3133/pp715A.","productDescription":"22 p.","temporalStart":"1964-10-01","temporalEnd":"1966-09-30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":140787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0715a/report-thumb.jpg"},{"id":12506,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/pp/715-A/index.htm","linkFileType":{"id":5,"text":"html"}},{"id":33352,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33353,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33354,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33355,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33356,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33357,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33358,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0715a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae731","contributors":{"authors":[{"text":"Meier, Mark Frederick","contributorId":30982,"corporation":false,"usgs":true,"family":"Meier","given":"Mark","email":"","middleInitial":"Frederick","affiliations":[],"preferred":false,"id":152278,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tangborn, Wendell V.","contributorId":32152,"corporation":false,"usgs":true,"family":"Tangborn","given":"Wendell","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":152279,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mayo, Lawrence R.","contributorId":98344,"corporation":false,"usgs":true,"family":"Mayo","given":"Lawrence","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":152281,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":152280,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":21432,"text":"ofr71328 - 1971 - Geochemical reconnaissance of the McCarthy B-6 quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ofr71328","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-328","title":"Geochemical reconnaissance of the McCarthy B-6 quadrangle, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr71328","usgsCitation":"Winkler, G., MacKevett, E., and Smith, J., 1971, Geochemical reconnaissance of the McCarthy B-6 quadrangle, Alaska: U.S. Geological Survey Open-File Report 71-328, 8 leaves :map ;28 cm.; 1 sheet, scale 1:63,360, https://doi.org/10.3133/ofr71328.","productDescription":"8 leaves :map ;28 cm.; 1 sheet, scale 1:63,360","costCenters":[],"links":[{"id":106519,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8646.htm","linkFileType":{"id":5,"text":"html"},"description":"8646"},{"id":154726,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0328/report-thumb.jpg"},{"id":51001,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0328/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":51002,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0328/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"63360","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade8b","contributors":{"authors":[{"text":"Winkler, Gary R.","contributorId":75513,"corporation":false,"usgs":true,"family":"Winkler","given":"Gary R.","affiliations":[],"preferred":false,"id":184418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacKevett, E.M. Jr.","contributorId":58613,"corporation":false,"usgs":true,"family":"MacKevett","given":"E.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":184417,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, James G.","contributorId":98712,"corporation":false,"usgs":true,"family":"Smith","given":"James G.","affiliations":[],"preferred":false,"id":184419,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":13081,"text":"ofr7172 - 1971 - Metallic mineral resources map of the Mt. McKinley quadrangle, Alaska","interactions":[{"subject":{"id":13081,"text":"ofr7172 - 1971 - Metallic mineral resources map of the Mt. McKinley quadrangle, Alaska","indexId":"ofr7172","publicationYear":"1971","noYear":false,"title":"Metallic mineral resources map of the Mt. 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