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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. 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,{"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":33913,"text":"b1028L - 1959 - Geology of Umnak and Bogoslof Islands, Aleutian Islands, Alaska","interactions":[{"subject":{"id":12861,"text":"ofr5522 - 1955 - The petrology of Umnak and Bogoslof Islands, Alaska","indexId":"ofr5522","publicationYear":"1955","noYear":false,"title":"The petrology of Umnak and Bogoslof Islands, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":33913,"text":"b1028L - 1959 - Geology of Umnak and Bogoslof Islands, Aleutian Islands, Alaska","indexId":"b1028L","publicationYear":"1959","noYear":false,"chapter":"L","title":"Geology of Umnak and Bogoslof Islands, Aleutian Islands, Alaska"},"id":1}],"lastModifiedDate":"2012-02-02T00:09:28","indexId":"b1028L","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":"1028","chapter":"L","title":"Geology of Umnak and Bogoslof Islands, Aleutian Islands, Alaska","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1028L","usgsCitation":"Byers, F., 1959, Geology of Umnak and Bogoslof Islands, Aleutian Islands, Alaska: U.S. Geological Survey Bulletin 1028, p. 267-369, ill., maps ;23 cm., https://doi.org/10.3133/b1028L.","productDescription":"p. 267-369, ill., maps ;23 cm.","costCenters":[],"links":[{"id":109178,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20598.htm","linkFileType":{"id":5,"text":"html"},"description":"20598"},{"id":96186,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1028l/report.pdf","size":"10553","linkFileType":{"id":1,"text":"pdf"}},{"id":163062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1028l/report-thumb.jpg"},{"id":61803,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1028l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61804,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1028l/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61805,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1028l/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61806,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1028l/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61807,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1028l/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b96e","contributors":{"authors":[{"text":"Byers, F.M. Jr.","contributorId":78338,"corporation":false,"usgs":true,"family":"Byers","given":"F.M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":212164,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33740,"text":"b1077 - 1959 - Geology of the Lake Mary quadrangle, Iron County, Michigan","interactions":[{"subject":{"id":12610,"text":"ofr565 - 1956 - Preliminary report on the geology of Lake Mary quadrangle, Iron County, Michigan","indexId":"ofr565","publicationYear":"1956","noYear":false,"title":"Preliminary report on the geology of Lake Mary quadrangle, Iron County, Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":33740,"text":"b1077 - 1959 - Geology of the Lake Mary quadrangle, Iron County, Michigan","indexId":"b1077","publicationYear":"1959","noYear":false,"title":"Geology of the Lake Mary quadrangle, Iron County, Michigan"},"id":1}],"lastModifiedDate":"2016-08-26T14:32:11","indexId":"b1077","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":"1077","title":"Geology of the Lake Mary quadrangle, Iron County, Michigan","docAbstract":"<p>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. </p><p>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. </p><p>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. </p><p>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. </p><p>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&nbsp;unconformity between the Randville and the succeeding Hemlock is not indicated in the quadrangle, but is probably present. </p><p>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. </p><p>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. </p><p>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. </p><p>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. </p><p>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. </p><p>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. </p><p>A few diabase dikes, probably of Keweenawan age, have intruded the deformed and altered Animikie rocks. </p><p>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.</p>","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":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":33961,"text":"b1046K - 1959 - Results of geologic exploration by core drilling, 1953, land-pebble phosphate district, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:09:22","indexId":"b1046K","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":"K","title":"Results of geologic exploration by core drilling, 1953, land-pebble phosphate district, Florida","language":"ENGLISH","publisher":"Govt. print. off.,","doi":"10.3133/b1046K","usgsCitation":"Cathcart, J.B., and McGreevy, L.J., 1959, Results of geologic exploration by core drilling, 1953, land-pebble phosphate district, Florida: U.S. Geological Survey Bulletin 1046, p. 221-298  :map, col. diagr., profiles, tables., https://doi.org/10.3133/b1046K.","productDescription":"p. 221-298  :map, col. diagr., profiles, tables.","costCenters":[],"links":[{"id":163947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1046k/report-thumb.jpg"},{"id":61857,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61858,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61859,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61860,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61861,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61862,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61863,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61864,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61865,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61866,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61867,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61868,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61869,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61870,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61871,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61872,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61873,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61874,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61875,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046k/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61876,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1046k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fa19","contributors":{"authors":[{"text":"Cathcart, James Bachelder","contributorId":19540,"corporation":false,"usgs":true,"family":"Cathcart","given":"James","email":"","middleInitial":"Bachelder","affiliations":[],"preferred":false,"id":212238,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGreevy, L. J.","contributorId":108124,"corporation":false,"usgs":true,"family":"McGreevy","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":212239,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35987,"text":"b1046M - 1959 - Reconnaissance investigation of uranium occurrences in the Saratoga area, Carbon County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:09:41","indexId":"b1046M","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":"M","title":"Reconnaissance investigation of uranium occurrences in the Saratoga area, Carbon County, Wyoming","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1046M","usgsCitation":"Stephens, J.G., and Bergin, M.J., 1959, Reconnaissance investigation of uranium occurrences in the Saratoga area, Carbon County, Wyoming: U.S. Geological Survey Bulletin 1046, p. 321-338  :maps (2 fold.) ;24 cm., https://doi.org/10.3133/b1046M.","productDescription":"p. 321-338  :maps (2 fold.) ;24 cm.","costCenters":[],"links":[{"id":109226,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20653.htm","linkFileType":{"id":5,"text":"html"},"description":"20653"},{"id":167457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1046m/report-thumb.jpg"},{"id":63934,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046m/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63935,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046m/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63936,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1046m/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e9a0","contributors":{"authors":[{"text":"Stephens, James Gilbert","contributorId":37803,"corporation":false,"usgs":true,"family":"Stephens","given":"James","email":"","middleInitial":"Gilbert","affiliations":[],"preferred":false,"id":215565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergin, M. J.","contributorId":77144,"corporation":false,"usgs":true,"family":"Bergin","given":"M.","middleInitial":"J.","affiliations":[],"preferred":false,"id":215566,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34836,"text":"b1046R - 1959 - Uranium in Sharon Springs member of Pierre shale, South Dakota and northeastern Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:27","indexId":"b1046R","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":"R","title":"Uranium in Sharon Springs member of Pierre shale, South Dakota and northeastern Nebraska","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1046R","usgsCitation":"Kepferle, R.C., 1959, Uranium in Sharon Springs member of Pierre shale, South Dakota and northeastern Nebraska: U.S. Geological Survey Bulletin 1046, p. 577-604, ill., maps (fold. in pocket) ;24 cm., https://doi.org/10.3133/b1046R.","productDescription":"p. 577-604, ill., maps (fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":109228,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20656.htm","linkFileType":{"id":5,"text":"html"},"description":"20656"},{"id":163976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1046r/report-thumb.jpg"},{"id":62785,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046r/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62786,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046r/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62787,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046r/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62788,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046r/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1046r/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6054ce","contributors":{"authors":[{"text":"Kepferle, Roy Clark","contributorId":46072,"corporation":false,"usgs":true,"family":"Kepferle","given":"Roy","email":"","middleInitial":"Clark","affiliations":[],"preferred":false,"id":213667,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39043,"text":"pp321 - 1959 - Cenozoic echinoids of eastern United States","interactions":[],"lastModifiedDate":"2013-02-26T14:56:35","indexId":"pp321","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"321","title":"Cenozoic echinoids of eastern United States","language":"ENGLISH","doi":"10.3133/pp321","usgsCitation":"Cooke, C.W., 1959, Cenozoic echinoids of eastern United States: U.S. Geological Survey Professional Paper 321, 106 p., https://doi.org/10.3133/pp321.","productDescription":"106 p.","costCenters":[],"links":[{"id":165559,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0321/report-thumb.jpg"},{"id":268409,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0321/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6a52","contributors":{"authors":[{"text":"Cooke, C. Wythe","contributorId":81538,"corporation":false,"usgs":true,"family":"Cooke","given":"C.","email":"","middleInitial":"Wythe","affiliations":[],"preferred":false,"id":220847,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4051,"text":"cir418 - 1959 - Floods of January-February 1959 in Ohio","interactions":[],"lastModifiedDate":"2018-02-19T21:28:50","indexId":"cir418","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"418","title":"Floods of January-February 1959 in Ohio","docAbstract":"<p>No abstract available.<br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir418","usgsCitation":"Cross, W.P., and Brooks, H.P., 1959, Floods of January-February 1959 in Ohio: U.S. Geological Survey Circular 418, 54 p., https://doi.org/10.3133/cir418.","productDescription":"54 p.","costCenters":[],"links":[{"id":117583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1959/0418/report-thumb.jpg"},{"id":31144,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1959/0418/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfc25","contributors":{"authors":[{"text":"Cross, William Perry","contributorId":21137,"corporation":false,"usgs":true,"family":"Cross","given":"William","email":"","middleInitial":"Perry","affiliations":[],"preferred":false,"id":148071,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooks, Harold Phillips","contributorId":28958,"corporation":false,"usgs":true,"family":"Brooks","given":"Harold","email":"","middleInitial":"Phillips","affiliations":[],"preferred":false,"id":148072,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3095,"text":"wsp1469 - 1959 - Ground-water conditions and storage capacity in the San Joaquin Valley, California","interactions":[{"subject":{"id":22843,"text":"ofr5636 - 1956 - Ground-water conditions and storage capacity in the San Joaquin Valley, California","indexId":"ofr5636","publicationYear":"1956","noYear":false,"title":"Ground-water conditions and storage capacity in the San Joaquin Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":3095,"text":"wsp1469 - 1959 - Ground-water conditions and storage capacity in the San Joaquin Valley, California","indexId":"wsp1469","publicationYear":"1959","noYear":false,"title":"Ground-water conditions and storage capacity in the San Joaquin Valley, California"},"id":1},{"subject":{"id":44087,"text":"ofr5466 - 1954 - Table showing estimated ground-water storage capacity of the San Joaquin Valley, California, and map showing ground-water storage units in the San Joaquin Valley","indexId":"ofr5466","publicationYear":"1954","noYear":false,"title":"Table showing estimated ground-water storage capacity of the San Joaquin Valley, California, and map showing ground-water storage units in the San Joaquin Valley"},"predicate":"SUPERSEDED_BY","object":{"id":3095,"text":"wsp1469 - 1959 - Ground-water conditions and storage capacity in the San Joaquin Valley, California","indexId":"wsp1469","publicationYear":"1959","noYear":false,"title":"Ground-water conditions and storage capacity in the San Joaquin Valley, California"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"wsp1469","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":"1469","title":"Ground-water conditions and storage capacity in the San Joaquin Valley, California","docAbstract":"The San Joaquin Valley includes roughly the southern two-thirds of the Great \r\nCentral Valley of California. It is a broad structural trough surrounded by \r\nmountains. The northern part of the valley drains through the San Joaquin \r\nRiver northward to San Francisco Bay ; the southern part of the valley normally \r\nis a basin of interior drainage tributary to evaporation sumps in the trough of \r\nthe valley, chiefly Tulare and Buena Vista Lake beds. \r\nIn years of normal discharge most of the streamflow in the southern part of \r\nthe valley not diverted for irrigation finds its way to Tulare and Buena Vista \r\nLake beds. In the historic past, however, during years of heavy floods the low \r\ndivide between Buena Vista and Tulare Lakes and the low divide between \r\nTulare Lake and the San Joaquin River were overtopped and through-flowing \r\ndrainage occurred over the full length of the valley. Because the Tulare Lake \r\nbed is the lowest point and also the largest sump, this whole basin of interior \r\ndrainage is commonly referred to as the Tulare Lake drainage basin. \r\nAverage annual precipitation ranges from more than 15 inches in the north- \r\neastern part of the valley to less than 4 inches in the southwestern part. The \r\nprecipitation decreases from north to south and from east to west across the \r\nvalley. Streamflow, the critical quantity in the water supply, depends almost \r\nwholly on the amount and distribution of precipitation in the Sierra Nevada to \r\nthe east. Much of this precipitation falls as snow, and the snowpack acts as a \r\nnatural reservoir retaining much of the annual runoff until late spring and early \r\nsummer. \r\nThe mean seasonal runoff to the San Joaquin Valley is nearly 10 million acre- \r\nfeet, of which about two-thirds is tributary to the San Joaquin River; the remaining third is tributary to Tulare Lake drainage basin. In 1952 about 8.5 \r\nmillion acre-feet of surface water was diverted for irrigation. Withdrawals of \r\nground water for irrigation in 1952 approximated 7.5 million acre-feet. \r\nThe surface of the San Joaquin Valley is not a featureless plain but is characterized by various types of physiography such as dissected uplands, low \r\nalluvial plains and fans, river flood plains and channels, and overflow lands \r\nand lake bottoms. \r\nThe dissected uplands fringe the valley along its mountain borders. They are \r\nunderlain by unconsolidated to semiconsolidated continental deposits of late \r\nTertiary and early Quaternary age which have been moderately tilted and \r\nfolded. The topography of these uplands ranges from deeply dissected hill land \r\nhaving a relief of several hundred feet to gently rolling land whose relief Is only \r\na few feet. \r\nThe low plains and fans border the dissected uplands along their valley- \r\nward margins. They are generally fiat to gently undulating and featureless and are underlain by undeformed to slightly deformed alluvial deposits of \r\nQuaternary age. \r\nThe river flood plains and channels lie along the San Joaquia and Kings \r\nRivers in the axial part of the valley and along the major east-side streams. \r\nWhere the rivers are incised below the general land surface, the flood plains are \r\nwell defined; but in the axial trough of the valley, where the rivers are flanked \r\nby low-lying overflow lands, the flood-plain and channel deposits are confined to \r\nthe stream channel and to the natural levees that slope away from the river. \r\nOverflow lands and lake bottoms include the historic beds of Tulare, Buena \r\nVista, and Kern Lakes in the southern part of the valley, and the low-lying lands \r\nin the axial trough between the low alluvial plains and fans and the natural \r\nlevees of the San Joaquin River and its major tributaries. They are level and \r\nfeatureless and are underlain by lake and swamp deposits of Recent age. \r\nThe San Joaquin Valley is a great structural downwarp between the tilted \r\nblock of the Sierra Nevada on the east and the complexly folded and faulted \r\nCoast Ranges on the we","language":"ENGLISH","publisher":"U.S. Govt. Print. 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,{"id":692,"text":"wsp1501 - 1959 - Surface water supply of the United States, 1957, Part I-A, North Atlantic slope basins, Maine to Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp1501","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":"1501","title":"Surface water supply of the United States, 1957, Part I-A, North Atlantic slope basins, Maine to Connecticut","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1501","usgsCitation":"Wells, J.V., 1959, Surface water supply of the United States, 1957, Part I-A, North Atlantic slope basins, Maine to Connecticut: U.S. Geological Survey Water Supply Paper 1501, viii, 257 p. ;23 cm., https://doi.org/10.3133/wsp1501.","productDescription":"viii, 257 p. ;23 cm.","costCenters":[],"links":[{"id":137484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1501/report-thumb.jpg"},{"id":25255,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1501/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696150","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":142620,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61389,"text":"mf218 - 1959 - Diagrammatic restored section of the Inyan Kara group, Morrison formation, and Unkpapa sandstone of the western side of the Black Hills, Wyoming and South Dakota","interactions":[],"lastModifiedDate":"2024-04-22T15:33:14.528141","indexId":"mf218","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"218","title":"Diagrammatic restored section of the Inyan Kara group, Morrison formation, and Unkpapa sandstone of the western side of the Black Hills, Wyoming and South Dakota","docAbstract":"<p>The Inyan Kara group of Early Cretaceous age and the underlying Morrison formation and Unkpapa sandstone of Late Jurassic age comprise about 300 to 850 feet of gently dipping predominantly nonmarine rocks that crop out along the flanks of the Black Hills in northeastern Wyoming and western South Dakota. Detailed mapping and stratigraphic studies of these rocks were made from 1952 to 1957 by the U.S. Geological Survey on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission. One of the results of the studies is a correlation of formational and intraformational units along the western side of the Black Hills for a distance of about 140 miles. The generalized section above, which has a greatly exaggerated vertical scale, shows the main lithologic units that have been traced and correlated, and the stratigraphic position of uranium deposits in various parts of the Black Hills in relation to these units. Geologists who have contributed to the diagrammatic section are listed on another part of this sheet and the areas for which each is responsible are shown on the accompanying map. The brief text below summarizes some of the broad stratigraphic relations within the Inyan Kara group and underlying formations.</p>","language":"English","publisher":"U. S. Geological Survey","publisherLocation":"Washington, DC","doi":"10.3133/mf218","isbn":"0607796855","usgsCitation":"Mapel, W.J., and Gott, G.B., 1959, Diagrammatic restored section of the Inyan Kara group, Morrison formation, and Unkpapa sandstone of the western side of the Black Hills, Wyoming and South Dakota: U.S. Geological Survey Miscellaneous Field Studies Map 218, 1 Plate: 50.66 x 27.58 inches, https://doi.org/10.3133/mf218.","productDescription":"1 Plate: 50.66 x 27.58 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":327596,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0218/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183373,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf218.PNG"}],"scale":"250000","country":"United States","state":"South Dakota, Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.86666666666666,43.416666666666664 ], [ -104.86666666666666,45 ], [ -103.51666666666667,45 ], [ -103.51666666666667,43.416666666666664 ], [ -104.86666666666666,43.416666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65db7d","contributors":{"authors":[{"text":"Mapel, W. J.","contributorId":92225,"corporation":false,"usgs":true,"family":"Mapel","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":265562,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gott, G. B.","contributorId":94281,"corporation":false,"usgs":true,"family":"Gott","given":"G.","middleInitial":"B.","affiliations":[],"preferred":false,"id":265563,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1844,"text":"wsp1459A - 1959 - Survey of ferrous-ferric chemical equilibria and redox potentials","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1459A","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":"1459","chapter":"A","title":"Survey of ferrous-ferric chemical equilibria and redox potentials","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1459A","usgsCitation":"Hem, J.D., and Cropper, W., 1959, Survey of ferrous-ferric chemical equilibria and redox potentials: U.S. Geological Survey Water Supply Paper 1459, iii, 31 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1459A.","productDescription":"iii, 31 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1459a/report-thumb.jpg"},{"id":27050,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1459a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688869","contributors":{"authors":[{"text":"Hem, John David","contributorId":42577,"corporation":false,"usgs":true,"family":"Hem","given":"John","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":144241,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cropper, W.H.","contributorId":93029,"corporation":false,"usgs":true,"family":"Cropper","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":144242,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39140,"text":"pp280K - 1959 - Part 4. Submarine topography and shoal-water ecology","interactions":[],"lastModifiedDate":"2022-02-17T22:43:58.618476","indexId":"pp280K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"280","chapter":"K","title":"Part 4. Submarine topography and shoal-water ecology","docAbstract":"<p>The topography of the sea floor within 10 miles of Saipan broadly resembles that of the land. Eastward, toward the Mariana trench, slopes are about 6&deg;, without prominent benches or scarps. This is inferred to indicate easterly continuation of generally pyroclastic bedrock. The westward slope averages 2&deg; to 3&deg; and consists mainly of nearly flat benches and westfacing scarps. This is taken to imply westward continuation of a limestone bench-and-fault-scarp topography. Projection of known faults to sea and through Tinian, on the basis of topographic trends, suggests a pattern of west-dipping normal faults that parallel the strike of the Mariana ridge and affect the shape and position of islands at the crest of the ridge.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology of Saipan, Mariana Islands","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp280K","usgsCitation":"Cloud, P.E., 1959, Part 4. Submarine topography and shoal-water ecology: U.S. Geological Survey Professional Paper 280, Report: 134 p.; 4 Plates: 27.31 x 35.94 inches or smaller; Table 6; Chart 1, https://doi.org/10.3133/pp280K.","productDescription":"Report: 134 p.; 4 Plates: 27.31 x 35.94 inches or smaller; Table 6; Chart 1","startPage":"361","endPage":"445","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":122170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0280k/report-thumb.jpg"},{"id":66639,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0280k/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":321976,"rank":306,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/pp/0280k/table-6.pdf","text":"Table 6","linkFileType":{"id":1,"text":"pdf"}},{"id":321975,"rank":305,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0280k/plate-122.pdf","text":"Plate 122","linkFileType":{"id":1,"text":"pdf"}},{"id":321974,"rank":304,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0280k/plate-121.pdf","text":"Plate 121","linkFileType":{"id":1,"text":"pdf"}},{"id":321973,"rank":303,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0280k/plate-120.pdf","text":"Plate 120","linkFileType":{"id":1,"text":"pdf"}},{"id":321972,"rank":302,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0280k/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":321971,"rank":301,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/0280k/chart-1.pdf","text":"Chart 1","linkFileType":{"id":1,"text":"pdf"}},{"id":396148,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_44665.htm"}],"country":"Saipan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              145.6835174560547,\n              15.088698509791715\n            ],\n            [\n              145.6835174560547,\n              15.295444914728776\n            ],\n            [\n              145.83457946777344,\n              15.295444914728776\n            ],\n            [\n              145.83457946777344,\n              15.088698509791715\n            ],\n            [\n              145.6835174560547,\n              15.088698509791715\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683ba0","contributors":{"authors":[{"text":"Cloud, Preston E. Jr.","contributorId":59861,"corporation":false,"usgs":true,"family":"Cloud","given":"Preston","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":221028,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1622,"text":"wsp1517 - 1959 - Surface water supply of the United States, 1957, part 13, Snake River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp1517","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":"1517","title":"Surface water supply of the United States, 1957, part 13, Snake River Basin","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp1517","usgsCitation":"Wells, J.V., 1959, Surface water supply of the United States, 1957, part 13, Snake River Basin: U.S. Geological Survey Water Supply Paper 1517, vii, 256 p. :tables., https://doi.org/10.3133/wsp1517.","productDescription":"vii, 256 p. :tables.","costCenters":[],"links":[{"id":137185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1517/report-thumb.jpg"},{"id":26687,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1517/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6960c4","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":143904,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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