No abstract available.
","language":"English","doi":"10.3133/ofr5952","usgsCitation":"Hembree, C., Iorns, W., Oakland, G., and Phoenix, D.A., 1959, Chemical quality of water in the Lower Duchesne River drainage basin: U.S. Geological Survey Open-File Report 59-52, 22 p., https://doi.org/10.3133/ofr5952.","productDescription":"22 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":184535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Duchesne River drainage basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3b22","contributors":{"authors":[{"text":"Hembree, C. H.","contributorId":106866,"corporation":false,"usgs":true,"family":"Hembree","given":"C. H.","affiliations":[],"preferred":false,"id":254837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Iorns, W.V.","contributorId":56726,"corporation":false,"usgs":true,"family":"Iorns","given":"W.V.","affiliations":[],"preferred":false,"id":254835,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oakland, G.L.","contributorId":37324,"corporation":false,"usgs":true,"family":"Oakland","given":"G.L.","affiliations":[],"preferred":false,"id":254834,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Phoenix, D. A.","contributorId":92665,"corporation":false,"usgs":true,"family":"Phoenix","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":254836,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":56170,"text":"ofr5986 - 1959 - The action of heat and of superheated steam on the tuff of the Oak Spring formation","interactions":[],"lastModifiedDate":"2012-02-02T00:12:06","indexId":"ofr5986","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-86","title":"The action of heat and of superheated steam on the tuff of the Oak Spring formation","language":"ENGLISH","doi":"10.3133/ofr5986","usgsCitation":"Morey, G., 1959, The action of heat and of superheated steam on the tuff of the Oak Spring formation: U.S. Geological Survey Open-File Report 59-86, 13 p., 4 tables, https://doi.org/10.3133/ofr5986.","productDescription":"13 p., 4 tables","costCenters":[],"links":[{"id":100488,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1959/0086/report.pdf","size":"4616","linkFileType":{"id":1,"text":"pdf"}},{"id":181457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1959/0086/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d25e","contributors":{"authors":[{"text":"Morey, G.W.","contributorId":108155,"corporation":false,"usgs":true,"family":"Morey","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":254870,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2391,"text":"wsp1460G - 1959 - Ground-water resources of the lower Niobrara River and Ponca Creek basins, Nebraska and South Dakota","interactions":[{"subject":{"id":10806,"text":"ofr5794 - 1957 - Preliminary estimate of the underflow across the South Dakota-Nebraska State line in the Niobrara River and Ponca Creek drainage basins","indexId":"ofr5794","publicationYear":"1957","noYear":false,"title":"Preliminary estimate of the underflow across the South Dakota-Nebraska State line in the Niobrara River and Ponca Creek drainage basins"},"predicate":"SUPERSEDED_BY","object":{"id":2391,"text":"wsp1460G - 1959 - Ground-water resources of the lower Niobrara River and Ponca Creek basins, Nebraska and South Dakota","indexId":"wsp1460G","publicationYear":"1959","noYear":false,"chapter":"G","title":"Ground-water resources of the lower Niobrara River and Ponca Creek basins, Nebraska and South Dakota"},"id":1}],"lastModifiedDate":"2022-12-30T22:10:07.828778","indexId":"wsp1460G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1460","chapter":"G","title":"Ground-water resources of the lower Niobrara River and Ponca Creek basins, Nebraska and South Dakota","docAbstract":"This report describes the area in north-central Nebraska and south-central South Dakota drained by Ponca Creek and by the Niobrara River below Valentine, Nebr. The Niobrara River and Ponca Creek are neighboring eastward flowing tributaries of the Missouri River. The Dakota sandstone of Cretaceous age is the oldest formation tapped by wells; the water it yields to wells in small to moderate quantities is rather highly mineralized and very hard; it is unsuitable for irrigation and most domestic uses. Overlying the Dakota, in ascending order, are the following formations of Cretaceous age: the Graneros shale, Greenhorn limestone, Carlile shale, Niobrara formation, and Pierre shale. None of these is a source of water supply. The Niobrara is the oldest formation exposed, cropping out in only the deeper valleys at the eastern end of the area. The Pierre shale, which is exposed much more extensively, crops out in the deeper valleys throughout nearly all the area.
\nExcept where the Niobrara River, its major tributaries, and Ponca Creek have cut their valleys into them, the Cretaceous rocks are overlain by semiconsolidated rocks of Tertiary age. Two Tertiary formations, the Brule and the Ogallala, are present in the area. The Brule formation underlies all the western part of the area and is exposed in the valleys of both the Niobrara and Keya Paha Rivers. The Ogallala formation, which overlaps the Brule, forms the upland on both sides of the river and is exposed in many places. The Brule is not a source of water supply, whereas the Ogallala yields small to moderately large quantities of water to many wells on the upland. The water in the Ogallala is of the calcium bicarbonate type and is moderately mineralized and hard.
\nUnconsolidated deposits of Quaternary age mantle the Tertiary rocks throughout nearly all the upland area south of the Niobrara River and in parts of the upland area north of the river. They also floor the Niobrara River valley. Where saturated, these sediments, which consist of stream-deposited sand and gravel and wind-deposited sand, yield small to large amounts of water to wells. The water in the Quaternary deposits is of the calcium bicarbonate type but is less mineralized and softer than that in the Ogallala.
\nThe only significant source of recharge to the Dakota sandstone in the report area is underflow from the west. Except for waiter yielded to wells tapping the Dakota, water in the formation is discharged from the area by underflow to the east. In the upland part of the area, the Ogallala formation and the overlying deposits of Quaternary age constitute a single aquifer, water moving from one Into the other without apparent hindrance. This aquifer is recharged principally by the direct infiltration of precipitation but in part also by underflow from the west and south and by seepage from intermittent streams and ponds. Water is discharged from the upland aquifer by outflow through springs or seepage into streams, through the process of evapotranspiration, and by wells when they are pumped. Ground water leaves the report area by underflow where the Quaternary deposits in the valleys of the Niobrara River and Ponca Creek merge with the Quaternary deposits in the Missouri River valley.
\nIn places where the Niobrara formation, the Pierre shale, or the Brule formation is at the surface or is mantled by thin deposits of the Ogallala or thin deposits of Quaternary age, only meager amounts of ground water can be obtained unless wells are deep enough to tap the Dakota sandstone. Elsewhere the Ogallala formation and the deposits of Quaternary age generally yield ample water for domestic and stock supplies, and in some places, notably in the vicinity of Ainsworth, they yield enough water for irrigation. Additional large supplies of ground water could be obtained on the upland in the southwestern and west-central parts of the area.
\nThe report contains an annotated bibliography of previous publications on the geology and ground-water resources of the area, brief descriptions of the Cretaceous, Tertiary, and Quaternary rocks, a map showing the contour of the water table, logs of test holes and wells not published elsewhere, results of analyses of ground- and surface-water samples, and records of all wells of large discharge and representative wells of small discharge.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","doi":"10.3133/wsp1460G","usgsCitation":"Newport, T., and Krieger, R.A., 1959, Ground-water resources of the lower Niobrara River and Ponca Creek basins, Nebraska and South Dakota: U.S. Geological Survey Water Supply Paper 1460, iv, 323 p., https://doi.org/10.3133/wsp1460G.","productDescription":"iv, 323 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":109946,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24392.htm","linkFileType":{"id":5,"text":"html"},"description":"24392"},{"id":28368,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1460g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139185,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1460g/report-thumb.jpg"}],"country":"United States","state":"Nebraska, North Dakota","otherGeospatial":"Niobrara River, Ponca Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -101.063232421875,\n 42.22851735620852\n ],\n [\n -101.063232421875,\n 43.29320031385282\n ],\n [\n -98.074951171875,\n 43.29320031385282\n ],\n [\n -98.074951171875,\n 42.22851735620852\n ],\n [\n -101.063232421875,\n 42.22851735620852\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a5ba","contributors":{"authors":[{"text":"Newport, Thomas G.","contributorId":93462,"corporation":false,"usgs":true,"family":"Newport","given":"Thomas G.","affiliations":[],"preferred":false,"id":145125,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krieger, Robert A.","contributorId":99954,"corporation":false,"usgs":true,"family":"Krieger","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145124,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12752,"text":"ofr5910 - 1959 - The geology of the Jewel Cave SW quadrangle, South Dakota, and its bearing on the origin of the uranium deposits in the southern Black Hills","interactions":[{"subject":{"id":12752,"text":"ofr5910 - 1959 - The geology of the Jewel Cave SW quadrangle, South Dakota, and its bearing on the origin of the uranium deposits in the southern Black Hills","indexId":"ofr5910","publicationYear":"1959","noYear":false,"title":"The geology of the Jewel Cave SW quadrangle, South Dakota, and its bearing on the origin of the uranium deposits in the southern Black Hills"},"predicate":"SUPERSEDED_BY","object":{"id":33821,"text":"b1063G - 1963 - Geology of the Jewel Cave SW Quadrangle, Custer County, South Dakota","indexId":"b1063G","publicationYear":"1963","noYear":false,"chapter":"G","title":"Geology of the Jewel Cave SW Quadrangle, Custer County, South Dakota"},"id":1}],"supersededBy":{"id":33821,"text":"b1063G - 1963 - Geology of the Jewel Cave SW Quadrangle, Custer County, South Dakota","indexId":"b1063G","publicationYear":"1963","noYear":false,"title":"Geology of the Jewel Cave SW Quadrangle, Custer County, South Dakota"},"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr5910","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-10","title":"The geology of the Jewel Cave SW quadrangle, South Dakota, and its bearing on the origin of the uranium deposits in the southern Black Hills","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr5910","usgsCitation":"Braddock, W.A., 1959, The geology of the Jewel Cave SW quadrangle, South Dakota, and its bearing on the origin of the uranium deposits in the southern Black Hills: U.S. Geological Survey Open-File Report 59-10, xi, 197 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr5910.","productDescription":"xi, 197 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":144973,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d644","contributors":{"authors":[{"text":"Braddock, William A.","contributorId":61010,"corporation":false,"usgs":true,"family":"Braddock","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":166653,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56191,"text":"ofr59129 - 1959 - Floods and flood control on the Colorado River at Austin, Texas","interactions":[],"lastModifiedDate":"2017-06-14T17:24:17","indexId":"ofr59129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-129","title":"Floods and flood control on the Colorado River at Austin, Texas","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr59129","usgsCitation":"Yost, I.D., 1959, Floods and flood control on the Colorado River at Austin, Texas: U.S. Geological Survey Open-File Report 59-129, 9 p., https://doi.org/10.3133/ofr59129.","productDescription":"9 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":181679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"Austin","otherGeospatial":"Colorado River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.4102783203125,\n 30.209234673510014\n ],\n [\n -97.47482299804688,\n 30.23889993659824\n ],\n [\n -97.51602172851562,\n 30.256694798480346\n ],\n [\n -97.5640869140625,\n 30.26381184075493\n ],\n [\n -97.61627197265625,\n 30.276858411864904\n ],\n [\n -97.646484375,\n 30.28990324883237\n ],\n [\n -97.73025512695311,\n 30.310060039424812\n ],\n [\n -97.78106689453125,\n 30.36813582872057\n ],\n [\n -97.833251953125,\n 30.391830328088137\n ],\n [\n -97.87994384765625,\n 30.407228671741567\n ],\n [\n -97.90740966796875,\n 30.40485985382934\n ],\n [\n -97.93899536132812,\n 30.378799064289495\n ],\n [\n -97.96234130859375,\n 30.347990988731844\n ],\n [\n -97.95135498046875,\n 30.318358689813856\n ],\n [\n -97.93212890625,\n 30.30294635121175\n ],\n [\n -97.84011840820311,\n 30.28990324883237\n ],\n [\n -97.80990600585938,\n 30.281602189612\n ],\n [\n -97.79891967773438,\n 30.25194981710498\n ],\n [\n -97.7398681640625,\n 30.22940802598824\n ],\n [\n -97.69317626953125,\n 30.198552988693212\n ],\n [\n -97.62313842773438,\n 30.168875561169088\n ],\n [\n -97.54898071289062,\n 30.181934730780572\n ],\n [\n -97.47344970703124,\n 30.159376896356193\n ],\n [\n -97.44735717773438,\n 30.153439766137296\n ],\n [\n -97.41439819335938,\n 30.177186142075502\n ],\n [\n -97.4102783203125,\n 30.209234673510014\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e2e","contributors":{"authors":[{"text":"Yost, I. D.","contributorId":12833,"corporation":false,"usgs":true,"family":"Yost","given":"I.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":254900,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12559,"text":"ofr593 - 1959 - Coal fields of Alaska","interactions":[{"subject":{"id":12559,"text":"ofr593 - 1959 - Coal fields of Alaska","indexId":"ofr593","publicationYear":"1959","noYear":false,"title":"Coal fields of Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70043342,"text":"70043342 - 1960 - Coal fields of the United States","indexId":"70043342","publicationYear":"1960","noYear":false,"title":"Coal fields of the United States"},"id":1}],"supersededBy":{"id":70043342,"text":"70043342 - 1960 - Coal fields of the United States","indexId":"70043342","publicationYear":"1960","noYear":false,"title":"Coal fields of the United States"},"lastModifiedDate":"2013-02-12T11:52:58","indexId":"ofr593","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-3","title":"Coal fields of Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr593","usgsCitation":"Barnes, F.F., 1959, Coal fields of Alaska: U.S. Geological Survey Open-File Report 59-3, 5 p. :folded map ;27 cm., https://doi.org/10.3133/ofr593.","productDescription":"5 p. :folded map ;27 cm.","costCenters":[],"links":[{"id":111561,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/10623","linkFileType":{"id":5,"text":"html"}},{"id":145399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5ddb83","contributors":{"authors":[{"text":"Barnes, Farrell F.","contributorId":58624,"corporation":false,"usgs":true,"family":"Barnes","given":"Farrell","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":166337,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56167,"text":"ofr5982 - 1959 - Geology of the Marble exploration hole 4, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:12:06","indexId":"ofr5982","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-82","title":"Geology of the Marble exploration hole 4, Nevada Test Site, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/ofr5982","usgsCitation":"McKeown, F.A., and Wilmarth, V., 1959, Geology of the Marble exploration hole 4, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 59-82, 26 p., 3 figs., https://doi.org/10.3133/ofr5982.","productDescription":"26 p., 3 figs.","costCenters":[],"links":[{"id":180675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea2e","contributors":{"authors":[{"text":"McKeown, F. A.","contributorId":106100,"corporation":false,"usgs":true,"family":"McKeown","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":254867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilmarth, V.R.","contributorId":20803,"corporation":false,"usgs":true,"family":"Wilmarth","given":"V.R.","email":"","affiliations":[],"preferred":false,"id":254866,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":56178,"text":"ofr59109 - 1959 - General geology and structural features of the Birmingham red iron ore district, Alabama","interactions":[{"subject":{"id":56178,"text":"ofr59109 - 1959 - General geology and structural features of the Birmingham red iron ore district, Alabama","indexId":"ofr59109","publicationYear":"1959","noYear":false,"title":"General geology and structural features of the Birmingham red iron ore district, Alabama"},"predicate":"SUPERSEDED_BY","object":{"id":70047577,"text":"70047577 - 1963 - Structural geology of the Birmingham red iron ore district, Alabama","indexId":"70047577","publicationYear":"1963","noYear":false,"title":"Structural geology of the Birmingham red iron ore district, Alabama"},"id":1}],"supersededBy":{"id":70047577,"text":"70047577 - 1963 - Structural geology of the Birmingham red iron ore district, Alabama","indexId":"70047577","publicationYear":"1963","noYear":false,"title":"Structural geology of the Birmingham red iron ore district, Alabama"},"lastModifiedDate":"2018-01-08T18:17:43","indexId":"ofr59109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-109","title":"General geology and structural features of the Birmingham red iron ore district, Alabama","docAbstract":"No abstract available.
The Lake Mary quadrangle is in eastern Iron County, in the west part of the Upper Peninsula of Michigan. The quadrangle is underlain by Lower and Middle Precambrian rocks, formerly designated Archean and Algonkian rocks, and is extensively covered by Pleistocene glacial deposits. A few Upper Precambrian (Keweenawan) diabase dikes and two remnants of sandstone and dolomite of early Paleozoic age are also found in the area.
The major structural feature is the Holmes Lake anticline, the axis of which strikes northwest through the northeast part of the quadrangle. Most of the quadrangle, therefore, is underlain by rock of the west limb of the anticline. To the northwest along the fold axis, the Holmes Lake anticline is separated from the Amasa oval by a saddle of transverse folds in the vicinity of Michigamme Mountain in the Kiernan quadrangle.
The Lower Precambrian rocks are represented by the Dickinson group and by porphyritic red granite whose relation to the Dickinson group is uncertain, but which may be older. The rocks of the Dickinson group are chiefly green to black metavolcanic schist and red felsite, some of the latter metarhyolite. The dark schist is commonly magnetic. The Dickinson group underlies the core area of the Holmes Lake anticline, which is flanked by steeply dipping Middle Precambrian formations of the Animikie series.
A major unconformity separates the Lower Precambrian rocks from the overlying Middle Precambrian rocks. In ascending order the formations of the Middle Precambrian are the Randville dolomite, the Hemlock formation, which includes the Mansfield iron-bearing slate member, and the Michigamme slate. An unconformity occurs between the Hemlock formation and Michigamme slate. The post-Hemlock unconformity is thought to be represented in the Lake Mary quadrangle by the absence of iron-formation of the Amasa formation, which is known to lie between the Hemlock and the Michigamme to the northwest of the Lake Mary quadrangle in the Crystal Falls quadrangle. Post-Hemlock erosion may account also for the absence of iron-formation of the Fence River formation on the east limb of the Holmes Lake anticline within the Lake Mary quadrangle.
The Randville dolomite is not exposed and is known only from diamond drilling in the northeast part of the area where it occurs in the east and west limbs of the Holmes Lake anticline. The formation has a maximum thickness of about 2,100 feet; this includes a lower arkosic phase, some of which is quartz pebble conglomerate, a medial dolomitic phase, and an upper slate phase. The triad is gradational. Included within the formation are a few beds of chloritic schist thought to be of volcanic origin. An unconformity between the Randville and the succeeding Hemlock is not indicated in the quadrangle, but is probably present.
The Hemlock formation is best exposed in the northwest and south-central parts of the area. The apparent thickness of the formation is 10,000- 17,000 feet. It is composed mainly of mafic metavolcanic rocks and intercalated slate and iron-formation. In the north part of the quadrangle the volcanic rocks are greenstone, which includes altered basaltic flow rocks, volcanic breccia, tuff, and slate. Pillow structures are common in the metabasalt. It is not certain if any Hemlock rocks are present in the east limb of the Holmes Lake anticline. In the south part of the quadrangle, the rocks of the Hemlock are chiefly chlorite and hornblende schist and hornfels. Pyroxene hornfels is sparingly present.
At least two sedimentary slate belts are included in the Hemlock formation. One of these, the Mansfield iron-bearing slate member, includes in its upper part an altered chert-siderite iron-formation 30 to over 150 feet thick from which iron ore has been mined at the Mansfield location. The position of the iron-bearing rocks has been determined magnetically, and past explorations for iron ore are discussed.
Though probably; unconformable, the contact between the Hemlock and the Michigamme formations appears conformable. The Michigamme slate consists of at least 4,000 feet of interbedded mica schist and granulite, the altered equivalents of the slate and graywacke characteristic of the Michigamme in adjacent areas. The Michigamme rocks are best exposed in the south part of the quadrangle in the vicinity of Peavy Pond.
Two periods of regional metamorphism have resulted in the alteration of almost all of the rocks of the quadrangle. The Lower Precambrian rocks underwent at least one period of metamorphism, uplift, and erosion before the deposition of the Randville dolomite. After the deposition of the Michigamme slate, a post-Middle Precambrian period of regional metamorphism occurred with attending deformation and igneous intrusion. The grade of metamorphism rises toward the south in the area. The rocks in the northern two-thirds of the quadrangle are representative of greenschist facies of regional metamorphism, whereas the rocks in the southern onethird of the quadrangle are representative of the albite-epidote-amphibolite, the amphibolite, and the pyroxene hornfels facies, the metamorphic node centering about the intrusive Peavy Pond complex in the Peavy Pond area.
The Precambrian sedimentary and volcanic rocks are cut by intrusive igneous rocks of different types and several different ages. Gabbroic sills and dikes invaded the Hemlock rocks at some time after the Hemlock was deposited and before the post-Middle Precambrian orogeny and metamorphism. Some contact metamorphism attended the intrusion of the major sills. One of the sills, the West Kiernan sill, is well differentiated. A syntectonic igneous body, composed of gabbro and minor ultramafic parts and fringed with intermediate and felsic differentiates and hybrids, the Peavy; Pond complex, was intruded into the Hemlock and Michigamme formations during the post-Middle Precambrian orogeny. The complex is situated in the Peavy Pond area at the crest of the regional metamorphic node. Contact-altered sedimentary and volcanic rocks margin the complex.
The effects of regional metamorphism have been superposed on the contact metamorphic rocks peripheral to the complex and on the igneous rocks of the complex as well. The mafic augite-bearing rocks of the complex emplaced early in the orogeny were deformed by granulation at the peak of the deformation and subsequently metamorphosed to hornblende rocks. Some of the intermediate and felsic rocks of the complex were foliated by the deformation, while the more fluid, felsic parts of the complex were intruded under orogenic stress and crystallized after the peak of deformation. The deformation culminated in major faulting during which the formations were dislocated, and some of the granite of the complex was extremely brecciated.
A few diabase dikes, probably of Keweenawan age, have intruded the deformed and altered Animikie rocks.
The only known metallic resource is iron ore. The Mansfield mine produced 1¥2 million tons of high-grade iron ore between the years 1890 and 1913. Sporadic exploration since 1913 has failed to reveal other ore deposits of economic importance.
","language":"English","publisher":"U. S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b1077","collaboration":"Prepared in cooperation with the Geological Survey Division Michigan Department of Conservation","usgsCitation":"Bayley, R.W., 1959, Geology of the Lake Mary quadrangle, Iron County, Michigan: U.S. Geological Survey Bulletin 1077, Document: v, 112 p.; 7 Plates: 38.91 x 33.74 inches or smaller, https://doi.org/10.3133/b1077.","productDescription":"Document: v, 112 p.; 7 Plates: 38.91 x 33.74 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":96076,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1077/plate-1.pdf","size":"5234","linkFileType":{"id":1,"text":"pdf"}},{"id":96077,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1077/plate-2.pdf","size":"3204","linkFileType":{"id":1,"text":"pdf"}},{"id":96078,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1077/plate-3.pdf","size":"3526","linkFileType":{"id":1,"text":"pdf"}},{"id":96079,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1077/plate-4.pdf","size":"981","linkFileType":{"id":1,"text":"pdf"}},{"id":96080,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1077/plate-5.pdf","size":"2776","linkFileType":{"id":1,"text":"pdf"}},{"id":96081,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1077/plate-6.pdf","size":"2526","linkFileType":{"id":1,"text":"pdf"}},{"id":96082,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1077/plate-7.pdf","size":"289","linkFileType":{"id":1,"text":"pdf"}},{"id":109296,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20736.htm","linkFileType":{"id":5,"text":"html"},"description":"20736"},{"id":61608,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1077/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1077/report-thumb.jpg"}],"country":"United States","state":"Michigan","county":"Iron County","otherGeospatial":"Lake Mary quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.25,\n 46.125\n ],\n [\n -88.25,\n 46\n ],\n [\n -88.125,\n 46\n ],\n [\n -88.125,\n 46.125\n ],\n [\n -88.25,\n 46.125\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f91d","contributors":{"authors":[{"text":"Bayley, Richard W.","contributorId":106084,"corporation":false,"usgs":true,"family":"Bayley","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":211857,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35851,"text":"b1071E - 1959 - Geology of the lower Marias River area, Chouteau, Hill, and Liberty Counties, Montana","interactions":[{"subject":{"id":41413,"text":"ofr55166 - 1955 - Preliminary geologic map of the Goose Mountain No. 1 quadrangle, Montana","indexId":"ofr55166","publicationYear":"1955","noYear":false,"title":"Preliminary geologic map of the Goose Mountain No. 1 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},{"subject":{"id":41414,"text":"ofr55167 - 1955 - Preliminary geologic map of the Goose Mountain No. 2 quadrangle, Montana","indexId":"ofr55167","publicationYear":"1955","noYear":false,"title":"Preliminary geologic map of the Goose Mountain No. 2 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":2},{"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":3},{"subject":{"id":42894,"text":"ofr55168 - 1955 - Preliminary geologic map of the Lonesome Lake No. 2 quadrangle, Montana","indexId":"ofr55168","publicationYear":"1955","noYear":false,"title":"Preliminary geologic map of the Lonesome Lake No. 2 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":4}],"lastModifiedDate":"2012-02-02T00:09:46","indexId":"b1071E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1071","chapter":"E","title":"Geology of the lower Marias River area, Chouteau, Hill, and Liberty Counties, Montana","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1071E","usgsCitation":"Smith, J.F., Witkind, I.J., and Trimble, D.E., 1959, Geology of the lower Marias River area, Chouteau, Hill, and Liberty Counties, Montana: U.S. Geological Survey Bulletin 1071, p. 121-155, ill., maps (3 fold. in pocket) ;24 cm., https://doi.org/10.3133/b1071E.","productDescription":"p. 121-155, ill., maps (3 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":109274,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20711.htm","linkFileType":{"id":5,"text":"html"},"description":"20711"},{"id":97084,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1071e/report.pdf","size":"2886","linkFileType":{"id":1,"text":"pdf"}},{"id":165572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1071e/report-thumb.jpg"},{"id":63809,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1071e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63810,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1071e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63811,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1071e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c827","contributors":{"authors":[{"text":"Smith, J. Fred Jr.","contributorId":106482,"corporation":false,"usgs":true,"family":"Smith","given":"J.","suffix":"Jr.","email":"","middleInitial":"Fred","affiliations":[],"preferred":false,"id":215333,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witkind, Irving Jerome","contributorId":87517,"corporation":false,"usgs":true,"family":"Witkind","given":"Irving","email":"","middleInitial":"Jerome","affiliations":[],"preferred":false,"id":215332,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trimble, Donald E.","contributorId":75910,"corporation":false,"usgs":true,"family":"Trimble","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":215331,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":35009,"text":"b1046N - 1959 - Preliminary study of radioactive limonite in Colorado, Utah, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:09:46","indexId":"b1046N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1046","chapter":"N","title":"Preliminary study of radioactive limonite in Colorado, Utah, and Wyoming","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1046N","usgsCitation":"Lovering, T., and Beroni, E.P., 1959, Preliminary study of radioactive limonite in Colorado, Utah, and Wyoming: U.S. Geological Survey Bulletin 1046, p. 339-384, ill. ;24 cm., https://doi.org/10.3133/b1046N.","productDescription":"p. 339-384, ill. ;24 cm.","costCenters":[],"links":[{"id":165569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1046n/report-thumb.jpg"},{"id":62950,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1046n/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db669f57","contributors":{"authors":[{"text":"Lovering, T.G.","contributorId":55014,"corporation":false,"usgs":true,"family":"Lovering","given":"T.G.","affiliations":[],"preferred":false,"id":213974,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beroni, Ernest Pete","contributorId":15181,"corporation":false,"usgs":true,"family":"Beroni","given":"Ernest","email":"","middleInitial":"Pete","affiliations":[],"preferred":false,"id":213973,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":35028,"text":"b1079 - 1959 - Geology of the Charleston phosphate area, South Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:09:49","indexId":"b1079","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1079","title":"Geology of the Charleston phosphate area, South Carolina","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1079","usgsCitation":"Malde, H.E., 1959, Geology of the Charleston phosphate area, South Carolina: U.S. Geological Survey Bulletin 1079, 105 p. illus., maps, diagrs., profile, tables ;25 cm., https://doi.org/10.3133/b1079.","productDescription":"105 p. illus., maps, diagrs., profile, tables ;25 cm.","costCenters":[],"links":[{"id":109298,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20738.htm","linkFileType":{"id":5,"text":"html"},"description":"20738"},{"id":165256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1079/report-thumb.jpg"},{"id":62961,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1079/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62962,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1079/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62963,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1079/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62964,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1079/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62965,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1079/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62966,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1079/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae81a","contributors":{"authors":[{"text":"Malde, Harold E.","contributorId":45706,"corporation":false,"usgs":true,"family":"Malde","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":214006,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36122,"text":"b1081B - 1959 - Stratigraphy of the Inyan Kara group in the Black Hills","interactions":[],"lastModifiedDate":"2012-02-02T00:09:37","indexId":"b1081B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1081","chapter":"B","title":"Stratigraphy of the Inyan Kara group in the Black Hills","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1081B","usgsCitation":"Waage, K.M., 1959, Stratigraphy of the Inyan Kara group in the Black Hills: U.S. Geological Survey Bulletin 1081, p. 11-90, ill. ;24 cm., https://doi.org/10.3133/b1081B.","productDescription":"p. 11-90, ill. ;24 cm.","costCenters":[],"links":[{"id":167425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1081b/report-thumb.jpg"},{"id":64085,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1081b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a60e9","contributors":{"authors":[{"text":"Waage, Karl M.","contributorId":29863,"corporation":false,"usgs":true,"family":"Waage","given":"Karl","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":215794,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36288,"text":"b1087A - 1959 - Geology of the Garo uranium-vanadium-copper deposit, Park County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:09:48","indexId":"b1087A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1087","chapter":"A","title":"Geology of the Garo uranium-vanadium-copper deposit, Park County, Colorado","language":"ENGLISH","publisher":"U.S. Govt. Print. Office,","doi":"10.3133/b1087A","usgsCitation":"Wilmarth, V., 1959, Geology of the Garo uranium-vanadium-copper deposit, Park County, Colorado: U.S. Geological Survey Bulletin 1087, p. 1-21, ill., maps ;23 cm., https://doi.org/10.3133/b1087A.","productDescription":"p. 1-21, ill., maps ;23 cm.","costCenters":[],"links":[{"id":109313,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20759.htm","linkFileType":{"id":5,"text":"html"},"description":"20759"},{"id":97338,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1087a/report.pdf","size":"1618","linkFileType":{"id":1,"text":"pdf"}},{"id":97339,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1087a/plate-1.pdf","size":"2657","linkFileType":{"id":1,"text":"pdf"}},{"id":97340,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1087a/plate-2.pdf","size":"177","linkFileType":{"id":1,"text":"pdf"}},{"id":97341,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1087a/plate-3.pdf","size":"1321","linkFileType":{"id":1,"text":"pdf"}},{"id":97342,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1087a/plate-4.pdf","size":"740","linkFileType":{"id":1,"text":"pdf"}},{"id":97343,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1087a/plate-5.pdf","size":"269","linkFileType":{"id":1,"text":"pdf"}},{"id":165157,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1087a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db68035d","contributors":{"authors":[{"text":"Wilmarth, Verl R.","contributorId":89951,"corporation":false,"usgs":true,"family":"Wilmarth","given":"Verl R.","affiliations":[],"preferred":false,"id":216076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46093,"text":"ofr59127 - 1959 - Map of Hillsborough County, Florida, showing contours on the piezometric surface in the principal artesian aquifer","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"ofr59127","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-127","title":"Map of Hillsborough County, Florida, showing contours on the piezometric surface in the principal artesian aquifer","language":"ENGLISH","doi":"10.3133/ofr59127","usgsCitation":"Wetterhall, W., 1959, Map of Hillsborough County, Florida, showing contours on the piezometric surface in the principal artesian aquifer: U.S. Geological Survey Open-File Report 59-127, 1 map., https://doi.org/10.3133/ofr59127.","productDescription":"1 map.","costCenters":[],"links":[{"id":162001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655712","contributors":{"authors":[{"text":"Wetterhall, W.S.","contributorId":10468,"corporation":false,"usgs":true,"family":"Wetterhall","given":"W.S.","affiliations":[],"preferred":false,"id":232603,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":34534,"text":"b1097A - 1959 - Evaluation of the lead-alpha (Larsen) method for determining ages of igneous rocks","interactions":[],"lastModifiedDate":"2012-02-02T00:09:30","indexId":"b1097A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1097","chapter":"A","title":"Evaluation of the lead-alpha (Larsen) method for determining ages of igneous rocks","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1097A","usgsCitation":"Gottfried, D., Jaffe, H.W., and Senftle, F.E., 1959, Evaluation of the lead-alpha (Larsen) method for determining ages of igneous rocks: U.S. Geological Survey Bulletin 1097, p. 1-63, ill. ;24 cm., https://doi.org/10.3133/b1097A.","productDescription":"p. 1-63, ill. ;24 cm.","costCenters":[],"links":[{"id":167366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1097a/report-thumb.jpg"},{"id":62414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1097a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65da7a","contributors":{"authors":[{"text":"Gottfried, David","contributorId":82295,"corporation":false,"usgs":true,"family":"Gottfried","given":"David","email":"","affiliations":[],"preferred":false,"id":213127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jaffe, Howard W.","contributorId":6501,"corporation":false,"usgs":true,"family":"Jaffe","given":"Howard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":213125,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Senftle, Frank E.","contributorId":49401,"corporation":false,"usgs":true,"family":"Senftle","given":"Frank","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":213126,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}