{"pageNumber":"6875","pageRowStart":"171850","pageSize":"25","recordCount":184770,"records":[{"id":70212508,"text":"70212508 - 1958 - Mineralogy and petrology of the currant creek magnesite deposits and associated rocks of Nevada: New data","interactions":[],"lastModifiedDate":"2020-08-18T17:20:47.201955","indexId":"70212508","displayToPublicDate":"1958-08-18T12:16:09","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"title":"Mineralogy and petrology of the currant creek magnesite deposits and associated rocks of Nevada: New data","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[353:MAPOTC]2.0.CO;2","usgsCitation":"Faust, G., and Callaghan, E., 1958, Mineralogy and petrology of the currant creek magnesite deposits and associated rocks of Nevada: New data, v. 69, no. 3, p. 353-354, https://doi.org/10.1130/0016-7606(1958)69[353:MAPOTC]2.0.CO;2.","productDescription":"2 p.","startPage":"353","endPage":"354","costCenters":[],"links":[{"id":377622,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Faust, George T.","contributorId":15186,"corporation":false,"usgs":true,"family":"Faust","given":"George T.","affiliations":[],"preferred":false,"id":796631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Callaghan, Eugene","contributorId":79855,"corporation":false,"usgs":true,"family":"Callaghan","given":"Eugene","email":"","affiliations":[],"preferred":false,"id":796632,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212506,"text":"70212506 - 1958 - Flowtill in Southeastern Massachusetts","interactions":[],"lastModifiedDate":"2020-08-18T17:13:06.065905","indexId":"70212506","displayToPublicDate":"1958-08-18T11:58:08","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Flowtill in Southeastern Massachusetts","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[477:FISM]2.0.CO;2","usgsCitation":"Hartshorn, J.H., 1958, Flowtill in Southeastern Massachusetts: GSA Bulletin, v. 69, no. 4, p. 477-482, https://doi.org/10.1130/0016-7606(1958)69[477:FISM]2.0.CO;2.","productDescription":"6 p.","startPage":"477","endPage":"482","costCenters":[],"links":[{"id":377619,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Taunton","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.2847900390625,\n              41.76721469421018\n            ],\n            [\n              -70.91262817382812,\n              41.76721469421018\n            ],\n            [\n              -70.91262817382812,\n              42.11248648904184\n            ],\n            [\n              -71.2847900390625,\n              42.11248648904184\n            ],\n            [\n              -71.2847900390625,\n              41.76721469421018\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"69","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hartshorn, J. H.","contributorId":56247,"corporation":false,"usgs":true,"family":"Hartshorn","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":796630,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212102,"text":"70212102 - 1958 - Geology of the north half of the Mt. Abbot quadrangle, Sierra Nevada, California","interactions":[],"lastModifiedDate":"2020-08-14T13:50:08.504872","indexId":"70212102","displayToPublicDate":"1958-08-13T13:52:37","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology of the north half of the Mt. Abbot quadrangle, Sierra Nevada, California","docAbstract":"<p>The north half of the 15-minute Mt. Abbot quadrangle lies across the crest of the Sierra Nevada. The Cretaceous granitic rocks that underlie most of the area form eight large discordant plutons that range from quartz diorite to alaskite; the largest pluton is coarse prophyritic quartz monzonite. Pre-batholithic metasedimentary and metavolcanic rocks and metagabbro and metadiorite are minor.</p><p>The porphyritic quartz monzonite sent gently dipping dikes as much as 200 feet thick into its walls. These dikes in places make up more than half the height of exposed contact zones. A broad border zone of protoclastic flaser gneiss was formed in part of the pluton and in the adjacent wall rocks and dikes.</p><p>A contact between granodiorite and calcareous metasedimentary rocks swarms with dark inclusions. Their origin, puzzling in most places, is here clearly due to progressive hybridization of calc-silicate xenoliths; the changes take place within a few tens of yards of the contact. The xenoliths were amphibolitized concentrically and reconstituted to typical dark-inclusion texture and mineralogy and were drawn out from blocky xenoliths into spindle shapes.</p><p>Elsewhere, large irregular xenoliths of metadiorite were assimilated by alaskite. Within the resulting complex is a thick series of alaskite flow layers crowded with xenocrysts showing graded “bedding”.</p><p>All the granitic plutons were intrusive; assimilation of mafic wall rocks by felsic magmas may have caused much of the diversity.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[1245:GOTNHO]2.0.CO;2","usgsCitation":"Sherlock, D.G., and Hamilton, W., 1958, Geology of the north half of the Mt. Abbot quadrangle, Sierra Nevada, California: GSA Bulletin, v. 69, no. 10, p. 1245-1268, https://doi.org/10.1130/0016-7606(1958)69[1245:GOTNHO]2.0.CO;2.","productDescription":"24 p.","startPage":"1245","endPage":"1268","costCenters":[],"links":[{"id":377502,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sierra Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.39941406249999,\n              37.3002752813443\n            ],\n            [\n              -118.5205078125,\n              37.3002752813443\n            ],\n            [\n              -118.5205078125,\n              38.151837403006766\n            ],\n            [\n              -119.39941406249999,\n              38.151837403006766\n            ],\n            [\n              -119.39941406249999,\n              37.3002752813443\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"69","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sherlock, D. G.","contributorId":238257,"corporation":false,"usgs":false,"family":"Sherlock","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":796230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamilton, Warren","contributorId":14819,"corporation":false,"usgs":true,"family":"Hamilton","given":"Warren","affiliations":[],"preferred":false,"id":796231,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212095,"text":"70212095 - 1958 - Recent underwater surveys using low-frequency sound to locate shallow bedrock","interactions":[],"lastModifiedDate":"2020-08-14T13:57:52.366945","indexId":"70212095","displayToPublicDate":"1958-08-13T13:27:39","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Recent underwater surveys using low-frequency sound to locate shallow bedrock","docAbstract":"<p>Underwater investigations at Lake Mead, Chicago, Passamaquoddy Bay, and on Long Island established the characteristics of sound waves that can be used in shallow geophysical exploration by the sonar method.</p><p>At Lake Mead the sediments were for the most part clay of high water content which was easily penetrated by low-power sound at a frequency of 14.2 kilocycles. The greatest depth of penetration was 140 feet. Sound having frequencies of 50 and 80 kilocycles did not penetrate. At Chicago, sound at a frequecy of 11 kilocycles and an output power of 800 watts gave a satisfactory delineation of bedrock beneath Lake Michigan. The maximum distance to bedrock was about 135 feet. At Passamaquoddy Bay a sound frequency of 6 kilocycles and about 700 watts of output power gave much better delineation of bedrock. A frequency of 6 kilocycles at the lower output power was much better than 11 kilocycles at higher power. About 250 feet of penetration was attained. Pulsed power was used in each of these investigations. The pulse lengths were long—about 14–25 milliseconds.</p><p>Bedrock was mapped at Lake Mead, Chicago, and Passamaquoddy Bay. The methods of ordinary hydrographic surveying were used for horizontal and vertical positioning. For horizontal positions the ordinary three-point sextant-fix method was used. For vertical positioning, recording gages suitably placed and supplemented by staff gages were used. All data were tied into the third-order control net of the U. S. Coast and Geodetic Survey.</p><p>In connection with a study for a proposed Midwestern waterway, the technical problem was reviewed and the techniques considerably improved. New equipment was built and evaluated on Long Island Sound. It operated with pulsed power at a frequency of 6 kilocycles, and pulse length was controlled and variable from 1 to 9 milliseconds. Output acoustic power was about 2500 watts. With the transducer in ordinary operating positions as much as 400 feet of sediment was penetrated. With the transducer placed directly on the bottom of the water in Huntington Bay about 750 feet of penetration was attained. Several innovations in sonar techniques, which are desirable for sediment exploration, and which give much more detailed information than the earlier equipment are described.</p><p>The techniques required for stratigraphic interpretation of the sound records are described briefly. A method for the determination of sound velocities is discussed. Multiple echoes and other effects complicate the interpretation of records and are explained. The problems of geological control encountered also are mentioned.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[69:RUSULS]2.0.CO;2","usgsCitation":"Smith, W.O., 1958, Recent underwater surveys using low-frequency sound to locate shallow bedrock: GSA Bulletin, v. 69, no. 1, p. 69-98, https://doi.org/10.1130/0016-7606(1958)69[69:RUSULS]2.0.CO;2.","productDescription":"30 p.","startPage":"69","endPage":"98","costCenters":[],"links":[{"id":377501,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"Illinois, Maine, Nevada, New Brunswick, New York","city":"Chicago","otherGeospatial":"Lake Mead, Lake Michigan, Long Island Sound, Passamaquoddy Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.87579345703124,\n              35.980228800645676\n            ],\n            [\n              -114.071044921875,\n              35.980228800645676\n            ],\n            [\n              -114.071044921875,\n              36.47872381162464\n            ],\n            [\n              -114.87579345703124,\n              36.47872381162464\n            ],\n            [\n              -114.87579345703124,\n              35.980228800645676\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.00048828124999,\n              41.64007838467894\n            ],\n            [\n              -86.90185546874999,\n              41.64007838467894\n            ],\n            [\n              -86.90185546874999,\n              42.22851735620852\n            ],\n            [\n              -88.00048828124999,\n              42.22851735620852\n            ],\n            [\n              -88.00048828124999,\n              41.64007838467894\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -66.94656372070312,\n              45.02695045318546\n            ],\n            [\n              -66.88613891601562,\n              45.12974228438219\n            ],\n            [\n              -66.96372985839844,\n              45.18736044117691\n            ],\n            [\n              -67.06809997558592,\n              45.155895559488236\n            ],\n            [\n              -67.10243225097656,\n              45.11084634642854\n            ],\n            [\n              -67.15393066406249,\n              45.226546196265026\n            ],\n            [\n              -67.20817565917967,\n              45.23863511362128\n            ],\n            [\n              -67.203369140625,\n              45.1936513315257\n            ],\n            [\n              -67.17933654785156,\n              45.1389457307005\n            ],\n            [\n              -67.13264465332031,\n              45.04975516197155\n            ],\n            [\n              -67.05917358398438,\n              44.94438944516438\n            ],\n            [\n              -67.00286865234375,\n              44.90890028388591\n            ],\n            [\n              -66.983642578125,\n              44.93515465088411\n            ],\n            [\n              -66.94656372070312,\n              45.02695045318546\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.93798828125,\n              40.77430186363723\n            ],\n            [\n              -73.34747314453125,\n              40.88444793903562\n            ],\n            [\n              -73.06182861328125,\n              40.92388970852945\n            ],\n            [\n              -72.59765625,\n              40.96123389519331\n            ],\n            [\n              -72.25433349609375,\n              41.143501411390766\n            ],\n            [\n              -71.817626953125,\n              41.32938883149378\n            ],\n            [\n              -72.4713134765625,\n              41.308760782192856\n            ],\n            [\n              -72.91900634765625,\n              41.29844430929419\n            ],\n            [\n              -73.2183837890625,\n              41.18278832811288\n            ],\n            [\n              -73.49578857421875,\n              41.08142149109681\n            ],\n            [\n              -73.6578369140625,\n              41.02135510866602\n            ],\n            [\n              -73.93798828125,\n              40.77430186363723\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"69","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, W. O.","contributorId":53015,"corporation":false,"usgs":true,"family":"Smith","given":"W.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":796229,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212088,"text":"70212088 - 1958 - Reply to Kuenen's letter","interactions":[],"lastModifiedDate":"2020-08-13T17:51:13.256646","indexId":"70212088","displayToPublicDate":"1958-08-13T12:45:04","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1369,"text":"Deep Sea Research Part A, Oceanographic Research Papers","active":true,"publicationSubtype":{"id":10}},"title":"Reply to Kuenen's letter","docAbstract":"<p>No abstract&nbsp; available.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0146-6291(58)80013-2","usgsCitation":"Ladd, H.S., and Tracey, J.I., 1958, Reply to Kuenen's letter: Deep Sea Research Part A, Oceanographic Research Papers, v. 5, no. 1, p. 79-80, https://doi.org/10.1016/S0146-6291(58)80013-2.","productDescription":"2 p.","startPage":"79","endPage":"80","costCenters":[],"links":[{"id":377500,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ladd, H. S.","contributorId":95537,"corporation":false,"usgs":true,"family":"Ladd","given":"H.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":796227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracey, J. I. Jr.","contributorId":17205,"corporation":false,"usgs":true,"family":"Tracey","given":"J.","suffix":"Jr.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":796228,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212081,"text":"70212081 - 1958 - The relation of phosphorites to ground water in Beaufort County, North Carolina","interactions":[],"lastModifiedDate":"2020-08-14T13:59:30.7653","indexId":"70212081","displayToPublicDate":"1958-08-13T12:28:37","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The relation of phosphorites to ground water in Beaufort County, North Carolina","docAbstract":"<p><span>Recent ground-water studies undertaken by the U.S. Geological Survey in cooperation with the North Carolina Division of Mineral Resources have delineated phosphorite deposits, tentatively regarded as being of middle Miocene age, in Beaufort County. These deposits lie unconforma-bly on limestone of Eocene age and are unconformably overlain by late Miocene marl. The phosphorites, buried beneath strata ranging in thickness from 45 to 250 feet, underlie an area approximating 450 square miles. The total thickness of the phosphorite column throughout the area ranges from several feet to nearly 90 feet. </span></p><p><span>The phosphorite column consists of phosphatic sands and intercalated shell limestones. The sands, composed of pellets of brown sand-size collophane (probably carbonate-fluorapatite) and sand-size, flat-sided angular quartz with some silt, clay, and organic material, have a median diameter between 0.50 and 0.25 mm. Chemical analyses of representative samples of the raw sand show a variation in PaOs content from 8 to 31 percent. The P2O5 content is apparently proportionate to the collophane content throughout the area. Reconstruction of the geologic history suggests that the phosphorites were deposited as chemical precipitates and as in situ replacements in a restricted marine basin where the pH of the water acted as the primary depositional control. </span></p><p><span>Reconstruction of the hydrologic history of the phosphorites indicates that the deposits were preserved under artesian conditions; they were never subjected to alteration under water-table conditions. The absence of postpositional alteration makes this area a potentially classic one for studies of phosphorite genesis. </span></p><p><span>Chemical analyses of artesian waters from the phosphorites and from limestones overlain by phosphorites reveal significantly greater concentrations of iodide and bromide in solution than are present in water from overlying sediments or from underlying limestones not overlain by phosphorites. Such anomalies, if present in other similar terranes, may indicate the presence of buried phosphorites. The depth and size distribution of the material suggest a recovery method utilizing wells constructed to \"pump sand.\"</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.53.1.85","usgsCitation":"Brown, P., 1958, The relation of phosphorites to ground water in Beaufort County, North Carolina: Economic Geology, v. 53, p. 85-101, https://doi.org/10.2113/gsecongeo.53.1.85.","productDescription":"17 p.","startPage":"85","endPage":"101","costCenters":[],"links":[{"id":377499,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","county":"Beaufort","otherGeospatial":"Beaufort  County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.8109130859375,\n              35.46514408578589\n            ],\n            [\n              -76.75048828125,\n              35.84008157153468\n            ],\n            [\n              -77.310791015625,\n              35.91129848822746\n            ],\n            [\n              -77.7667236328125,\n              35.78662688467009\n            ],\n            [\n              -77.8436279296875,\n              35.55010533588552\n            ],\n            [\n              -77.3162841796875,\n              35.28150065789119\n            ],\n            [\n              -76.97021484375,\n              35.28150065789119\n            ],\n            [\n              -76.86035156249999,\n              35.40696093270201\n            ],\n            [\n              -77.27783203125,\n              35.594785665487244\n            ],\n            [\n              -77.14599609375,\n              35.60818490437746\n            ],\n            [\n              -76.8109130859375,\n              35.46514408578589\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"53","noUsgsAuthors":false,"publicationDate":"1958-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, P.M.","contributorId":46324,"corporation":false,"usgs":true,"family":"Brown","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":796226,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212077,"text":"70212077 - 1958 - Minerals of the cassiterite-bearing veins at Irish Creek, Virginia, and their paragenetic relations","interactions":[],"lastModifiedDate":"2020-08-14T14:04:28.947002","indexId":"70212077","displayToPublicDate":"1958-08-13T12:10:52","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Minerals of the cassiterite-bearing veins at Irish Creek, Virginia, and their paragenetic relations","docAbstract":"<p><span>Major rock types of the Irish Creek district are gneisses and schists, intruded by granodiorite. All these rocks are believed to be Precambrian. The ore deposits are fissure veins consisting largely of quartz veins bordered by greisen, and enriched by recurrent deposition. From field and microscopic evidence six stages of mineral formation have been deduced: </span></p><p><span>1. Crystallization of the granodiorite with the formation of hypersthene, augite, hornblende, andesine, orthoclase, microcline, and quartz; and accessory apatite, rutile, ilmenite, titanomagnetite, and zircon. </span></p><p><span>2. Metamorphism of the granodiorite and gneiss with formation of uralitic actinolite, epidote, and sphene. </span></p><p><span>3. A period of fracturing and formation of quartz veins. </span></p><p><span>4. Greisenization of the host rock producing first: coarse muscovite, brown biotite, cassiterite, beryl, wolframite, and quartz; then producing a second group of minerals-fluorite, green biotite, chlorite, phenakite, siderite, ankerite, parisite, sphalerite, sulfides, including aikinite and galeno-bismutite, leucoxene, fine muscovite, and quartz. </span></p><p><span>5. Formation of late vein minerals, clinozoisite, calcite, nontronite, and montmorillonite. </span></p><p><span>6. Formation of surficial alteration products, kaolinite, vermiculite, hematite, limonite, and scorodite. </span></p><p><span>The italicized mineral names indicate the minerals heretofore unreported from Irish Creek; parisite, aikinite, and galenobismutite are new minerals for Virginia. Included in the detailed descriptions of all the minerals is a chemical analysis of beryl.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.53.1.65","usgsCitation":"Glass, J.J., Koschmann, A.H., and Vhay, J.S., 1958, Minerals of the cassiterite-bearing veins at Irish Creek, Virginia, and their paragenetic relations: Economic Geology, v. 53, no. 1, p. 65-84, https://doi.org/10.2113/gsecongeo.53.1.65.","productDescription":"20 p.","startPage":"65","endPage":"84","costCenters":[],"links":[{"id":377498,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","otherGeospatial":"Irish Creek","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-79.1574,37.8923],[-79.1545,37.8882],[-79.1499,37.8814],[-79.147,37.8732],[-79.1476,37.8678],[-79.1424,37.8623],[-79.1424,37.8596],[-79.1483,37.856],[-79.1576,37.8438],[-79.1572,37.8261],[-79.1718,37.8039],[-79.1783,37.7994],[-79.1952,37.7917],[-79.2004,37.7908],[-79.2045,37.7927],[-79.2132,37.7963],[-79.23,37.814],[-79.2329,37.8136],[-79.237,37.8104],[-79.2452,37.8086],[-79.2505,37.8018],[-79.2563,37.7973],[-79.2651,37.7964],[-79.2709,37.7964],[-79.2732,37.7937],[-79.2721,37.7855],[-79.2721,37.7788],[-79.2768,37.7715],[-79.2838,37.7638],[-79.2972,37.7516],[-79.3036,37.7407],[-79.3025,37.733],[-79.3042,37.7294],[-79.3159,37.7204],[-79.3182,37.7172],[-79.3171,37.7063],[-79.3206,37.7004],[-79.3346,37.6864],[-79.3404,37.6796],[-79.3428,37.6733],[-79.341,37.6678],[-79.3393,37.6637],[-79.3422,37.6619],[-79.3527,37.6597],[-79.3568,37.656],[-79.3597,37.6515],[-79.3661,37.6483],[-79.3754,37.6461],[-79.3794,37.6443],[-79.3876,37.6366],[-79.3923,37.633],[-79.3992,37.6298],[-79.412,37.6284],[-79.4196,37.6262],[-79.4324,37.6153],[-79.4358,37.6208],[-79.4422,37.6189],[-79.4544,37.6094],[-79.455,37.6058],[-79.4539,37.5999],[-79.4504,37.5936],[-79.4463,37.5881],[-79.4457,37.5822],[-79.4446,37.5804],[-79.4394,37.5791],[-79.4347,37.5786],[-79.4341,37.5777],[-79.4376,37.5686],[-79.4411,37.5664],[-79.4487,37.5641],[-79.4521,37.5632],[-79.4556,37.5614],[-79.4574,37.5596],[-79.462,37.555],[-79.4643,37.5537],[-79.4725,37.5519],[-79.4777,37.5496],[-79.4794,37.5487],[-79.4939,37.5415],[-79.5003,37.5365],[-79.5787,37.5822],[-79.5764,37.5849],[-79.5741,37.5895],[-79.5706,37.599],[-79.652,37.6474],[-79.6829,37.6655],[-79.6748,37.675],[-79.6702,37.6864],[-79.6678,37.6968],[-79.6684,37.6991],[-79.6754,37.7036],[-79.6842,37.7398],[-79.679,37.7453],[-79.6767,37.7516],[-79.6744,37.7643],[-79.6634,37.777],[-79.6512,37.8002],[-79.6448,37.8133],[-79.6373,37.8179],[-79.6332,37.8197],[-79.6233,37.8333],[-79.6192,37.8424],[-79.6169,37.8514],[-79.607,37.8601],[-79.607,37.8628],[-79.6081,37.8637],[-79.6117,37.865],[-79.6155,37.8662],[-79.6194,37.8681],[-79.6242,37.8714],[-79.6267,37.8742],[-79.6274,37.8745],[-79.6339,37.8759],[-79.6365,37.8751],[-79.6376,37.8745],[-79.6387,37.8735],[-79.6406,37.872],[-79.6422,37.8715],[-79.6427,37.8716],[-79.646,37.8736],[-79.6473,37.8744],[-79.6476,37.8744],[-79.6374,37.8895],[-79.6269,37.9122],[-79.6118,37.9321],[-79.5745,37.9612],[-79.5552,37.9816],[-79.5231,38.0205],[-79.5115,38.035],[-79.5231,38.0423],[-79.5202,38.0464],[-79.5015,38.0591],[-79.4887,38.0777],[-79.4805,38.0867],[-79.4197,38.0513],[-79.3211,37.995],[-79.2004,37.9291],[-79.19,37.9213],[-79.1801,37.9132],[-79.1673,37.9023],[-79.1574,37.8923]]],[[[-79.3493,37.755],[-79.3427,37.7618],[-79.3339,37.7594],[-79.3332,37.7618],[-79.3286,37.7602],[-79.332,37.7427],[-79.3333,37.743],[-79.3328,37.7383],[-79.3393,37.7317],[-79.3335,37.7298],[-79.334,37.728],[-79.3409,37.7291],[-79.3555,37.7087],[-79.3609,37.7048],[-79.3603,37.7026],[-79.3699,37.6962],[-79.3723,37.6977],[-79.3732,37.6967],[-79.3826,37.7062],[-79.3752,37.712],[-79.3759,37.7222],[-79.3691,37.7271],[-79.3668,37.7267],[-79.3669,37.7281],[-79.372,37.7298],[-79.3776,37.7269],[-79.3749,37.7394],[-79.3815,37.7406],[-79.3809,37.7435],[-79.372,37.7457],[-79.3647,37.7443],[-79.361,37.7514],[-79.3571,37.7545],[-79.3493,37.755]]],[[[-79.4351,37.7776],[-79.448,37.7685],[-79.4532,37.7658],[-79.4607,37.7749],[-79.4549,37.7821],[-79.4619,37.788],[-79.4543,37.7957],[-79.4497,37.7957],[-79.4415,37.8012],[-79.4147,37.7912],[-79.4351,37.7776]]]]},\"properties\":{\"name\":\"Rockbridge\",\"state\":\"VA\"}}]}","volume":"53","issue":"1","noUsgsAuthors":false,"publicationDate":"1958-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Glass, Jewell J.","contributorId":106948,"corporation":false,"usgs":true,"family":"Glass","given":"Jewell","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":796223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koschmann, A. H.","contributorId":55455,"corporation":false,"usgs":true,"family":"Koschmann","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":796224,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vhay, John Stewart","contributorId":97920,"corporation":false,"usgs":true,"family":"Vhay","given":"John","email":"","middleInitial":"Stewart","affiliations":[],"preferred":false,"id":796225,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70212070,"text":"70212070 - 1958 - Uranium deposits under conglomeratic sandstone of the Morrison Formation, Colorado and Utah","interactions":[],"lastModifiedDate":"2020-08-14T14:05:19.628286","indexId":"70212070","displayToPublicDate":"1958-08-13T11:40:12","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Uranium deposits under conglomeratic sandstone of the Morrison Formation, Colorado and Utah","docAbstract":"<p><span>In southwestern Colorado and southeastern Utah, strata of conglomeratic sandstone are localized at the base of the Brushy Basin Member of the Morrison Formation of Jurassic age. These discrete lithologic units contain sedimentary structures oriented in a prevailing easterly direction. They are believed to cover about one-third of the underlying Salt Wash Member in southwestern Colorado and southeastern Utah, and they locally rest on ore-bearing sandstone in the Salt Wash Member. Eastward-trending planar cross-stratification and trough cross-stratification and a general westward coarsening of sediments in the conglomeratic sandstone strata suggest that they are the products of stream aggradation from westerly source areas. Uranium-vanadium deposits in the uppermost, almost continuous, layer of sandstone of the Salt Wash Member are classified according to their association with the conglomerate strata. Of the 363 deposits studied in the uppermost sandstone layer of the Salt Wash Member, 101 are known to be directly beneath conglomeratic sandstone strata, 211 are below the projected extension of conglomeratic sandstone strata, 33 are beyond the safe limits of such projection, and 18 are lateral to the margins of conglomeratic sandstone strata. At places, near clusters of deposits in the uppermost sandstone of the underlying Salt Wash Member, conglomeratic sandstone strata of the Brushy Basin Member are also mineralized. It is postulated that ground-water movement during deposition of the Morrison Formation in Late Jurassic time localized the uranium and vanadium. The direction of this ground-water movement is believed to have been related to streams that deposited the conglomeratic strata, so that in the ore-bearing sandstone metal ions contained in the ground water were localized in places of high transmissibility and in the vicinity of decaying organic debris. According to the age of the ores, precipitation of the metals was much later than their localization, probably during Late Cretaceous or early Tertiary time.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[403:UDUCSO]2.0.CO;2","usgsCitation":"Phoenix, D.A., 1958, Uranium deposits under conglomeratic sandstone of the Morrison Formation, Colorado and Utah: GSA Bulletin, v. 69, no. 4, p. 403-418, https://doi.org/10.1130/0016-7606(1958)69[403:UDUCSO]2.0.CO;2.","productDescription":"16 p.","startPage":"403","endPage":"418","costCenters":[],"links":[{"id":377497,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Morrison Formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.0830078125,\n              37.020098201368114\n            ],\n            [\n              -108.160400390625,\n              37.020098201368114\n            ],\n            [\n              -108.160400390625,\n              39.16414104768742\n            ],\n            [\n              -110.0830078125,\n              39.16414104768742\n            ],\n            [\n              -110.0830078125,\n              37.020098201368114\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"69","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Phoenix, D. A.","contributorId":92665,"corporation":false,"usgs":true,"family":"Phoenix","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":796222,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212066,"text":"70212066 - 1958 - Stratigraphy of Upper Pennsylvanian and lower Permian rocks in the Sand Canyon area, Otero County, New Mexico","interactions":[],"lastModifiedDate":"2020-08-13T16:39:30.26643","indexId":"70212066","displayToPublicDate":"1958-08-13T11:13:10","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphy of Upper Pennsylvanian and lower Permian rocks in the Sand Canyon area, Otero County, New Mexico","docAbstract":"<p><span>The Magdalena Group of Pennsylvanian age and, in ascending order, the lower tongue of the Abo Sandstone (herein named the Danley Ranch Tongue), the Hueco Limestone, the upper tongue of the Abo Sandstone (herein named the Lee Ranch Tongue), and the Yeso Formation of Permian age are well displayed in the southern part of the Sacramento Mountains. The contact of the Pennsylvanian rocks with the overlying Permian rocks is unconformable throughout the area. Locally the relief before deposition of the Abo was so great that in places the Danley Ranch Tongue of the Abo is absent because of nondeposition. At these places there is prominent angular discordance between the Pennsylvanian and Permian rocks.</span></p><p><span> The red beds of the Danley Ranch Tongue interfinger with and grade southward into the overlying Hueco Limestone. Red beds of the Lee Ranch Tongue of the Abo Sandstone also grade southward into the Hueco and cannot be traced south of the southern part of the Sacramento Mountains. The Lee Ranch Tongue is believed to be stratigraphically lower than the Deer Mountain Red Shale Member of the type Hueco Limestone. The herein named Otero Mesa Member of the Yeso Formation is believed to occupy an intermediate stratigraphic position between the Lee Ranch Tongue and the Deer Mountain Red Shale.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[689:SOUPAL]2.0.CO;2","usgsCitation":"Bachman, G.O., and Hayes, P., 1958, Stratigraphy of Upper Pennsylvanian and lower Permian rocks in the Sand Canyon area, Otero County, New Mexico: GSA Bulletin, v. 69, no. 6, p. 689-700, https://doi.org/10.1130/0016-7606(1958)69[689:SOUPAL]2.0.CO;2.","productDescription":"12 p.","startPage":"689","endPage":"700","costCenters":[],"links":[{"id":377495,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Otero County","otherGeospatial":"Sand Canyon","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-105.314,33.1323],[-105.3136,33.0485],[-105.3142,33.0044],[-105.3143,32.9629],[-105.3512,32.9628],[-105.3514,32.9276],[-105.3536,32.5218],[-105.3165,32.5221],[-105.2997,32.522],[-105.2828,32.5219],[-105.266,32.5218],[-105.2497,32.5217],[-105.2301,32.5216],[-105.2138,32.5219],[-105.1801,32.5217],[-105.1627,32.5215],[-105.1436,32.5214],[-105.1441,32.5241],[-105.1376,32.5241],[-105.0083,32.5208],[-104.9767,32.5205],[-104.9593,32.5203],[-104.9436,32.5202],[-104.9403,32.5201],[-104.9338,32.5201],[-104.924,32.52],[-104.9164,32.5199],[-104.9071,32.5194],[-104.8658,32.519],[-104.8566,32.5189],[-104.849,32.5188],[-104.8491,32.5124],[-104.8495,32.4427],[-104.8492,32.4286],[-104.8496,32.399],[-104.8493,32.3839],[-104.8495,32.2554],[-104.8457,32.2554],[-104.8461,32.1533],[-104.8463,32.1378],[-104.8462,32.1104],[-104.8464,32.0958],[-104.8466,32.0031],[-104.8612,32.003],[-104.9115,32.0029],[-104.9201,32.0029],[-104.9282,32.0029],[-104.9449,32.0029],[-104.9606,32.003],[-105.0114,32.0026],[-105.0276,32.0028],[-105.0439,32.0029],[-105.0601,32.0027],[-105.0775,32.0028],[-105.1445,32.0025],[-105.1521,32.0025],[-105.1643,32.0024],[-105.1853,32.0022],[-105.2145,32.002],[-105.2486,32.0017],[-105.2534,32.0017],[-105.2619,32.0017],[-105.3015,32.002],[-105.3177,32.0021],[-105.335,32.0023],[-105.3528,32.0019],[-105.3701,32.002],[-105.4204,32.0023],[-105.4372,32.0024],[-105.454,32.0021],[-105.4713,32.0021],[-105.5216,32.0024],[-105.572,32.0022],[-105.6219,32.0022],[-105.6391,32.0022],[-105.6467,32.0018],[-105.6662,32.0019],[-105.7169,32.002],[-105.7337,32.002],[-105.7548,32.0016],[-105.7738,32.0016],[-105.7953,32.0017],[-105.8228,32.0018],[-105.8393,32.0019],[-105.8622,32.0019],[-105.879,32.0019],[-105.9281,32.0019],[-105.9444,32.0019],[-105.9978,32.002],[-106.0439,32.002],[-106.1662,32.0023],[-106.2214,32.0021],[-106.314,32.0018],[-106.3733,32.0017],[-106.3724,32.0523],[-106.3719,32.0669],[-106.3715,32.0811],[-106.373,32.169],[-106.3728,32.2565],[-106.3727,32.3436],[-106.3723,32.3759],[-106.373,32.6493],[-106.3731,32.6643],[-106.3746,32.8692],[-106.3737,32.8979],[-106.3745,32.9598],[-106.3368,32.9604],[-106.3372,33.0537],[-106.3378,33.1898],[-106.3403,33.3913],[-106.1028,33.3918],[-106.0935,33.3923],[-106.0676,33.3923],[-106.0594,33.3923],[-106.0495,33.3923],[-106.0418,33.3923],[-106.0313,33.3923],[-106.0143,33.3923],[-105.9978,33.3923],[-105.9879,33.3927],[-105.9285,33.3927],[-105.8774,33.3918],[-105.8411,33.3922],[-105.7218,33.3924],[-105.7221,33.3069],[-105.5179,33.308],[-105.4157,33.3075],[-105.3125,33.3065],[-105.314,33.1323]]]},\"properties\":{\"name\":\"Otero\",\"state\":\"NM\"}}]}","volume":"69","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bachman, George O.","contributorId":25070,"corporation":false,"usgs":true,"family":"Bachman","given":"George","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":796191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, Philip T.","contributorId":43098,"corporation":false,"usgs":true,"family":"Hayes","given":"Philip T.","affiliations":[],"preferred":false,"id":796192,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211931,"text":"70211931 - 1958 - Hydrologic education","interactions":[],"lastModifiedDate":"2020-08-11T20:25:05.15528","indexId":"70211931","displayToPublicDate":"1958-08-11T15:22:42","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Hydrologic education","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"Taylor & Francis Online","doi":"10.1080/02626665809493108","usgsCitation":"Langbein, W., 1958, Hydrologic education: International Association of Scientific Hydrology - Bulletin , v. 3, no. 3, p. 27-30, https://doi.org/10.1080/02626665809493108.","productDescription":"4 p.","startPage":"27","endPage":"30","costCenters":[],"links":[{"id":486942,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626665809493108","text":"Publisher Index Page"},{"id":377389,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Langbein, Walter B.","contributorId":98294,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter B.","affiliations":[],"preferred":false,"id":795851,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211930,"text":"70211930 - 1958 - Contact metamorphism adjacent to a teschenite intrusion","interactions":[],"lastModifiedDate":"2020-08-12T15:10:37.713101","indexId":"70211930","displayToPublicDate":"1958-08-11T15:10:30","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6005,"text":"Journal of the Geological Society of Australia","onlineIssn":"0016-7614","active":false,"publicationSubtype":{"id":10}},"title":"Contact metamorphism adjacent to a teschenite intrusion","docAbstract":"<p><span>Shale adjacent to the upper contact of an annular teschenite intrusion was converted to andalusite hornfels in an aureole 2–4 feet wide. At some points along the contact there is no evidence of anhydrous recrystallization. Rarely, magmatic reaction with small shale xenoliths resulted in formation of cordierite‐sillimanite (?) hornfelses, and locally a very small‐scale movement of magmatic constituents took place across the contact before consolidation of the teschenite. Very severe deuteric alteration of teschenite adjacent to the contact resulted in large losses of Si, Fe, Mg, alkalis, and probably Ca, some of which were recombined in clays and carbonates in the more porous shales and in joints, but analyses of uniformly fine‐grained shales indicate little change in bulk composition. Mineralogical evidence indicates a maximum contact temperature within the range 500°‐600° C, and a maximum intrusion temperature within the range 1000°‐1200° C.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/00167615808728492","usgsCitation":"Wilshire, H.G., 1958, Contact metamorphism adjacent to a teschenite intrusion: Journal of the Geological Society of Australia, v. 6, no. 1, p. 11-20, https://doi.org/10.1080/00167615808728492.","productDescription":"11 p.","startPage":"11","endPage":"20","costCenters":[],"links":[{"id":377387,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wilshire, Howard G.","contributorId":68346,"corporation":false,"usgs":true,"family":"Wilshire","given":"Howard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":795850,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211929,"text":"70211929 - 1958 - Radiotracer experiments in the Mohawk River, New York, to study sewage path and dilution","interactions":[],"lastModifiedDate":"2020-08-11T20:01:06.769149","indexId":"70211929","displayToPublicDate":"1958-08-11T14:40:57","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Radiotracer experiments in the Mohawk River, New York, to study sewage path and dilution","docAbstract":"<p><span>Sewage from the Knolls Atomic Power Laboratory near Schenectady, N. Y., was dosed with 4.53 curies of P prior to discharge into the Mohawk River. Its pattern of diffusion was measured in the river with immersible GM‐tubes and by sampling. The initial path of sewage was strongly influenced by differences in density between sewage and river due to temperature. During warm months relatively cold sewage moved on the river bottom perpendicularly to river current. For at least the first 800 ft of travel the maximum sewage concentration decreased logarithmically with distance from outfall. The term ‘half‐distance’ (here about 110 ft) is proposed to describe the concentration change. During cold months sewage rose to the river surface and at times was moved upstream by wind. However, when the river temperature was near freezing, the sewage first rose and then sank as the temperature of the sewage‐river mixture approached 39° F.</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/TR039i003p00427","usgsCitation":"Simpson, E.S., Beetem, W., and Ruggles, F.H., 1958, Radiotracer experiments in the Mohawk River, New York, to study sewage path and dilution: Eos, Transactions, American Geophysical Union, v. 39, no. 3, p. 427-433, https://doi.org/10.1029/TR039i003p00427.","productDescription":"7 p.","startPage":"427","endPage":"433","costCenters":[],"links":[{"id":377384,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Lower Mohawk River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.05059814453125,\n              42.69252994883861\n            ],\n            [\n              -73.56857299804688,\n              42.69252994883861\n            ],\n            [\n              -73.56857299804688,\n              43.072900581493215\n            ],\n            [\n              -74.05059814453125,\n              43.072900581493215\n            ],\n            [\n              -74.05059814453125,\n              42.69252994883861\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"39","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Simpson, Eugene S.","contributorId":116654,"corporation":false,"usgs":true,"family":"Simpson","given":"Eugene","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":795847,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beetem, W. Arthur","contributorId":34831,"corporation":false,"usgs":true,"family":"Beetem","given":"W. Arthur","affiliations":[],"preferred":false,"id":795848,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ruggles, F. H.","contributorId":105805,"corporation":false,"usgs":true,"family":"Ruggles","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":795849,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70211928,"text":"70211928 - 1958 - Application of statistical methods to the analysis of ground‐water levels","interactions":[],"lastModifiedDate":"2020-08-11T19:31:46.319712","indexId":"70211928","displayToPublicDate":"1958-08-11T14:23:06","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Application of statistical methods to the analysis of ground‐water levels","docAbstract":"<p><span>Valuable hydrologic information can be obtained from statistical analysis of water‐level trends. The time‐series and the functional‐equation approaches are applied to New Jersey well records representing different hydrologic conditions. The results are valuable as concise summaries of the records, for extrapolating observed data, for interpolating between measurements, and for estimating hydrologic factors such as coefficients of transrnissibility and storage, evapotranspiration, and ground‐water discharge.&nbsp;</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/TR039i001p00075","usgsCitation":"Remson, I., and Randolph, J., 1958, Application of statistical methods to the analysis of ground‐water levels: Eos, Transactions, American Geophysical Union, v. 39, no. 1, p. 75-83, https://doi.org/10.1029/TR039i001p00075.","productDescription":"9 p.","startPage":"75","endPage":"83","costCenters":[],"links":[{"id":377381,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Remson, Irwin","contributorId":89115,"corporation":false,"usgs":true,"family":"Remson","given":"Irwin","email":"","affiliations":[],"preferred":false,"id":795845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randolph, J.R.","contributorId":19532,"corporation":false,"usgs":true,"family":"Randolph","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":795846,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211918,"text":"70211918 - 1958 - Reconnaissance study of erosion and deposition produced by the flood of August 1955 in Connecticut","interactions":[],"lastModifiedDate":"2020-08-11T19:16:55.176465","indexId":"70211918","displayToPublicDate":"1958-08-11T14:08:12","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Reconnaissance study of erosion and deposition produced by the flood of August 1955 in Connecticut","docAbstract":"<p><span>A large area in the valley bottoms in Connecticut was inundated by the flood of August 1955. Relative to the total area flooded that part permanently modified by the flow was surprisingly small. Although great in some places, the distribution of these permanent modifications of channel and flood plain was spotty. Erosion of the channel and valley bottom appears to have been most severe in narrow, steep valleys. Environments of deposition were diverse. They appeared to be related to rate and direction of flow, quantity and size of sediments locally available, and in some cases to the presence of vegetation. Most of the coarse sediment deposited in the valley appears to have been derived from local sources such as valley walls and terraces composed of glacial outwash and till and flood plains containing considerable gravel. Fine sand predominated in most of the sediment deposited. Considering the magnitude of the runoff, the quantity of fine sediment transported or deposited by the flood was small. The maximum observed concentration was 473 parts per million in Scantic River at Broad Brook. Newly deposited fine sediments are thin or absent on the flood plains of many valleys which were beneath 20 ft of slow‐moving flood waters. The paucity of deposition in such ideal depositional environments also indicates that the flow did not have a high concentration of fine sediments. A number of boulders five to seven feet in diameter were moved by flood waters in reaches in which smaller gravels were undisturbed. Severe erosion in the uplands was minor. In this reconnaissance we saw little evidence of newly formed gullies and no areas of severe sheet erosion. This was the case in both woodland and pasture land. Large amounts of subsurface flow and relatively unerodible ground are presumed to be responsible for the absence of erosion.</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/TR039i001p00001","usgsCitation":"Wolman, M.G., and Eiler, J., 1958, Reconnaissance study of erosion and deposition produced by the flood of August 1955 in Connecticut: Eos, Transactions, American Geophysical Union, v. 39, no. 1, p. 1-14, https://doi.org/10.1029/TR039i001p00001.","productDescription":"14 p.","startPage":"1","endPage":"14","costCenters":[],"links":[{"id":377372,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-71.799242,42.008065],[-71.797922,41.935395],[-71.797649,41.928556],[-71.794161,41.841101],[-71.794161,41.840141],[-71.792786,41.80867],[-71.792767,41.807001],[-71.791062,41.770273],[-71.789678,41.724734],[-71.789672,41.724569],[-71.786994,41.655992],[-71.787637,41.639917],[-71.789356,41.59691],[-71.789359,41.596852],[-71.797683,41.416709],[-71.81839,41.419599],[-71.839649,41.412119],[-71.842563,41.409855],[-71.843472,41.40583],[-71.842131,41.395359],[-71.833443,41.384524],[-71.831613,41.370899],[-71.837738,41.363529],[-71.835951,41.353935],[-71.829595,41.344544],[-71.839013,41.334042],[-71.860513,41.320248],[-71.859566,41.3224],[-71.868235,41.330941],[-71.886302,41.33641],[-71.91671,41.332217],[-71.922092,41.334518],[-71.923282,41.335113],[-71.936284,41.337959],[-71.945652,41.337799],[-71.956747,41.329871],[-71.970955,41.324526],[-71.979447,41.329987],[-71.982194,41.329861],[-71.988153,41.320577],[-72.021898,41.316838],[-72.084487,41.319634],[-72.094443,41.314164],[-72.09982,41.306998],[-72.11182,41.299098],[-72.134221,41.299398],[-72.16158,41.310262],[-72.173922,41.317597],[-72.177622,41.322497],[-72.184122,41.323997],[-72.191022,41.323197],[-72.201422,41.315697],[-72.203022,41.313197],[-72.204022,41.299097],[-72.212924,41.291365],[-72.225276,41.299047],[-72.235531,41.300413],[-72.248161,41.299488],[-72.251895,41.29862],[-72.250515,41.294386],[-72.251323,41.289997],[-72.261487,41.282926],[-72.31776,41.277782],[-72.327595,41.27846],[-72.333894,41.282916],[-72.34146,41.28011],[-72.348643,41.277446],[-72.348068,41.269698],[-72.386629,41.261798],[-72.398688,41.278172],[-72.40593,41.278398],[-72.451925,41.278885],[-72.472539,41.270103],[-72.485693,41.270881],[-72.499534,41.265866],[-72.506634,41.260099],[-72.51866,41.261253],[-72.521312,41.2656],[-72.529416,41.264421],[-72.533247,41.26269],[-72.536746,41.256207],[-72.537776,41.255646],[-72.546833,41.250718],[-72.547235,41.250499],[-72.570655,41.267744],[-72.571076,41.268054],[-72.571136,41.268098],[-72.583336,41.271698],[-72.585181,41.271321],[-72.585934,41.271168],[-72.586674,41.271017],[-72.587926,41.270761],[-72.589818,41.270375],[-72.590967,41.270141],[-72.598036,41.268698],[-72.607863,41.270387],[-72.610236,41.270795],[-72.617237,41.271998],[-72.617521,41.27194],[-72.617983,41.271845],[-72.631363,41.269092],[-72.641001,41.267108],[-72.641538,41.266998],[-72.642811,41.266884],[-72.650697,41.266178],[-72.653838,41.265897],[-72.653931,41.265931],[-72.654715,41.266219],[-72.662203,41.268964],[-72.662838,41.269197],[-72.667176,41.268192],[-72.671673,41.267151],[-72.672339,41.266997],[-72.674319,41.26552],[-72.684939,41.257597],[-72.685414,41.252607],[-72.685539,41.251297],[-72.689446,41.247629],[-72.690237,41.246887],[-72.690439,41.246697],[-72.693441,41.245493],[-72.694744,41.24497],[-72.69547,41.244948],[-72.701806,41.244752],[-72.706236,41.244615],[-72.707212,41.244585],[-72.708658,41.24454],[-72.708963,41.24453],[-72.709193,41.244523],[-72.710595,41.24448],[-72.710821,41.244812],[-72.713674,41.249007],[-72.711208,41.251018],[-72.71246,41.254167],[-72.722439,41.259138],[-72.732813,41.254727],[-72.754444,41.266913],[-72.757477,41.266913],[-72.786142,41.264796],[-72.818737,41.252244],[-72.819372,41.254061],[-72.826883,41.256755],[-72.847767,41.25669],[-72.85021,41.255544],[-72.854055,41.24774],[-72.861344,41.245297],[-72.881445,41.242597],[-72.895445,41.243697],[-72.900803,41.245864],[-72.904345,41.247297],[-72.905245,41.248297],[-72.903045,41.252797],[-72.902808,41.252894],[-72.894745,41.256197],[-72.89473,41.25626],[-72.893845,41.259897],[-72.89637,41.263949],[-72.903129,41.274794],[-72.907962,41.282549],[-72.9082,41.282932],[-72.916827,41.282033],[-72.917037,41.281905],[-72.920062,41.280056],[-72.920658,41.271574],[-72.920714,41.27078],[-72.920846,41.268897],[-72.931887,41.261139],[-72.933472,41.260024],[-72.935646,41.258497],[-72.956984,41.25292],[-72.959633,41.252228],[-72.961345,41.25178],[-72.962047,41.251597],[-72.983751,41.235364],[-72.985095,41.234358],[-72.986247,41.233497],[-72.997948,41.222697],[-73.003639,41.215287],[-73.007548,41.210197],[-73.013465,41.205479],[-73.013988,41.205062],[-73.014948,41.204297],[-73.020149,41.204097],[-73.020167,41.204237],[-73.020195,41.204446],[-73.02021,41.204568],[-73.020254,41.204906],[-73.020449,41.206397],[-73.022549,41.207197],[-73.024783,41.207435],[-73.045602,41.209658],[-73.05065,41.210197],[-73.054947,41.208468],[-73.05935,41.206697],[-73.07761,41.195176],[-73.07945,41.194015],[-73.09122,41.184153],[-73.092,41.1835],[-73.092147,41.183377],[-73.104328,41.17317],[-73.105483,41.172203],[-73.105493,41.172194],[-73.107987,41.168738],[-73.110352,41.159697],[-73.109952,41.156997],[-73.108352,41.153718],[-73.111052,41.150797],[-73.130253,41.146797],[-73.16437,41.158565],[-73.170074,41.160532],[-73.170701,41.164945],[-73.177774,41.166697],[-73.202656,41.158096],[-73.228295,41.142602],[-73.235058,41.143996],[-73.247958,41.126396],[-73.262358,41.117496],[-73.286759,41.127896],[-73.296359,41.125696],[-73.31186,41.116296],[-73.33066,41.109996],[-73.372296,41.10402],[-73.392162,41.087696],[-73.400154,41.086299],[-73.41367,41.073258],[-73.435063,41.056696],[-73.450364,41.057096],[-73.468239,41.051347],[-73.477364,41.035997],[-73.493327,41.048173],[-73.516903,41.038738],[-73.516766,41.029497],[-73.522666,41.019297],[-73.528866,41.016397],[-73.531169,41.021919],[-73.530189,41.028776],[-73.532786,41.03167],[-73.535338,41.03192],[-73.551494,41.024336],[-73.561968,41.016797],[-73.567668,41.010897],[-73.570068,41.001597],[-73.583968,41.000897],[-73.584988,41.010537],[-73.595699,41.015995],[-73.603952,41.015054],[-73.643478,41.002171],[-73.651175,40.995229],[-73.657336,40.985171],[-73.659671,40.987909],[-73.658772,40.993497],[-73.659372,40.999497],[-73.655571,41.007697],[-73.654671,41.011697],[-73.655371,41.012797],[-73.662672,41.020497],[-73.670472,41.030097],[-73.679973,41.041797],[-73.687173,41.050697],[-73.694273,41.059296],[-73.716875,41.087596],[-73.722575,41.093596],[-73.727775,41.100696],[-73.639672,41.141495],[-73.632153,41.144921],[-73.614391,41.152915],[-73.564941,41.17517],[-73.514617,41.198434],[-73.509487,41.200814],[-73.482709,41.21276],[-73.518384,41.256719],[-73.550961,41.295422],[-73.548929,41.307598],[-73.549574,41.315931],[-73.548973,41.326297],[-73.544728,41.366375],[-73.543425,41.376622],[-73.543415,41.376754],[-73.541169,41.405994],[-73.537673,41.433905],[-73.537469,41.43589],[-73.536969,41.441094],[-73.536067,41.451331],[-73.535986,41.45306],[-73.535885,41.455236],[-73.535857,41.455709],[-73.535769,41.457159],[-73.534369,41.475894],[-73.534269,41.476394],[-73.534269,41.476911],[-73.53415,41.47806],[-73.534055,41.478968],[-73.533969,41.479693],[-73.530067,41.527194],[-73.521041,41.619773],[-73.520017,41.641197],[-73.518238,41.666734],[-73.516785,41.687581],[-73.511921,41.740941],[-73.510961,41.758749],[-73.505008,41.823773],[-73.504944,41.824285],[-73.501984,41.858717],[-73.498304,41.892508],[-73.496527,41.92238],[-73.492975,41.958524],[-73.489615,42.000092],[-73.487314,42.049638],[-73.432812,42.050587],[-73.29442,42.046984],[-73.293097,42.04694],[-73.231056,42.044945],[-73.229798,42.044877],[-73.127276,42.041964],[-73.053254,42.039861],[-73.008745,42.03886],[-72.999549,42.038653],[-72.863733,42.03771],[-72.863619,42.037709],[-72.847142,42.036894],[-72.813541,42.036494],[-72.816741,41.997595],[-72.774757,42.002129],[-72.766739,42.002995],[-72.766139,42.007695],[-72.763265,42.009742],[-72.763238,42.012795],[-72.761238,42.014595],[-72.759738,42.016995],[-72.761354,42.018183],[-72.76231,42.019775],[-72.762151,42.021527],[-72.760558,42.021846],[-72.758151,42.020865],[-72.757467,42.020947],[-72.754038,42.025395],[-72.751738,42.030195],[-72.753538,42.032095],[-72.757538,42.033295],[-72.755838,42.036195],[-72.714134,42.036608],[-72.695927,42.036788],[-72.643134,42.032395],[-72.607933,42.030795],[-72.606933,42.024995],[-72.590233,42.024695],[-72.582332,42.024695],[-72.573231,42.030141],[-72.528131,42.034295],[-72.509192,42.034217],[-72.45668,42.033999],[-72.317148,42.031907],[-72.249523,42.031626],[-72.135715,42.030245],[-72.135687,42.030245],[-72.102162,42.028899],[-72.063496,42.027347],[-71.987326,42.02688],[-71.89078,42.024368],[-71.80065,42.023569],[-71.799242,42.008065]]]},\"properties\":{\"name\":\"Connecticut\",\"nation\":\"USA  \"}}]}","volume":"39","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Wolman, M. Gordon","contributorId":85163,"corporation":false,"usgs":true,"family":"Wolman","given":"M.","email":"","middleInitial":"Gordon","affiliations":[],"preferred":false,"id":795803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eiler, J.P.","contributorId":238011,"corporation":false,"usgs":false,"family":"Eiler","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":795804,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211917,"text":"70211917 - 1958 - Lower ordovician section near Chambersburg, Pennsylvania","interactions":[],"lastModifiedDate":"2020-08-11T19:02:08.031196","indexId":"70211917","displayToPublicDate":"1958-08-11T13:56:39","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Lower ordovician section near Chambersburg, Pennsylvania","docAbstract":"<p>The Lower Ordovician series (Beekmantown group) is at least 3500 feet thick near Chambersburg, Pennsylvania, approximately 1200 feet thicker than was earlier estimated. Reverse faulting in the upper part of the section may have obscured the youngest Early Ordovician and oldest Middle Ordovician beds in the area, so that the total thickness of the Lower Ordovician series may be comparable to the thickness measured in Maryland.</p><p>The Beekmantown group is represented by the Stonehenge limestone and the Rockdale Run formation. Moving the base of the Stonehenge downward to include about 200 feet of strata previously referred to the underlying Conococheague formation facilitates regional correlation without impairing mappability. Newly discovered fossils from the Rockdale Run formation add notably to the faunas of the upper part of that formation. Comparison of a trilobite-brachiopod faunule near the top of the Diparelasma zone (Cotter-Powell equivalent) with similar fossils in Zone J of the Utah-Nevada sequence suggests that Zone J may be no younger than the Powell dolomite of the Ozark region. Difficulty in recognizing correlatives of the Smithville and Black Rock formations suggests the need for restudy of these units in the Ozark region.</p><p>Evidence from the Chambersburg section neither proves nor contradicts the hypothesis of continuous deposition from Early Ordovician to Middle Ordovician time in the central Appalachian area.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[837:LOSNCP]2.0.CO;2","usgsCitation":"Sando, W.J., 1958, Lower ordovician section near Chambersburg, Pennsylvania: GSA Bulletin, v. 69, no. 7, p. 837-854, https://doi.org/10.1130/0016-7606(1958)69[837:LOSNCP]2.0.CO;2.","productDescription":"18 p.","startPage":"837","endPage":"854","costCenters":[],"links":[{"id":377369,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Chambersburg","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.673095703125,\n              39.74943369178247\n            ],\n            [\n              -77.025146484375,\n              39.74943369178247\n            ],\n            [\n              -77.025146484375,\n              40.47202439692057\n            ],\n            [\n              -78.673095703125,\n              40.47202439692057\n            ],\n            [\n              -78.673095703125,\n              39.74943369178247\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"69","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sando, William Jasper","contributorId":8524,"corporation":false,"usgs":true,"family":"Sando","given":"William","email":"","middleInitial":"Jasper","affiliations":[],"preferred":true,"id":795802,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211916,"text":"70211916 - 1958 - Technique for the extraction and partial chemical analysis of fluid-filled inclusions from minerals","interactions":[],"lastModifiedDate":"2020-08-11T18:54:58.544298","indexId":"70211916","displayToPublicDate":"1958-08-11T13:47:36","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Technique for the extraction and partial chemical analysis of fluid-filled inclusions from minerals","docAbstract":"<p><span>A method has been developed for the extraction and limited chemical analysis of the materials in solution in the fluid from the very minute fluid-filled inclusions such as commonly occur in whitish or milky quartz. The method may also be applied, with some reservations, to a variety of other minerals. As the amounts of substances in the fluid are small compared with possible contaminants, great care is needed in sample purification and cleaning; an electrolytic method has been found to be the only satisfactory final cleaning step. Following this, the inclusions are opened by ball milling of the cleaned sample, with deionized water, in an alumina ball mill using alumina grinding media. The ions present in the resultant slurry are separated from the ground quartz by electrodialysis and analyzed. Other methods, such as the decrepitation of a sample in an absorption train, are used to estimate the amount of H2O and CO2 in the inclusions. The most significant part of the analytical work has been to determine the ratios between the alkali metals. </span></p><p><span>The materials in solution in the fluid-filled inclusions from 11 samples of quartz have been analyzed by the ball milling-electrodialysis method. Although there are large differences between samples, the average weights of the alkali metal ions found, for all samples, in milligrams per kilogram of quartz, are: Li+-0.92, Na+-99, K+-133, Rb+-0.45, Cs+-0.38 (atomic ratios, in the same sequence: 0.03/1.00/0.79/0.001/0.0007). In addition, 27 to 193 milligrams of CI\", and 5 to 140 milligrams of SOr were found, per kilogram of quartz. H2O and COa were determined on only one sample. Six of the samples were from gold-quartz veins in the Grass Valley district, California. In these six the Na+/K+ ratios were all very similar, but the amounts of Li+, Rb+ and Cs+ found varied greatly. Although there are serious limitations to this and to all other techniques developed, it is felt that the results presented are sufficiently encouraging to warrant further study and possible application to specific geologic problems, such as the identification of epochs of quartz deposition</span></p>","language":"English","publisher":"GeoScienceWorld","doi":"10.2113/gsecongeo.53.3.235","usgsCitation":"Roedder, E., 1958, Technique for the extraction and partial chemical analysis of fluid-filled inclusions from minerals: Economic Geology, v. 53, no. 3, p. 235-269, https://doi.org/10.2113/gsecongeo.53.3.235.","productDescription":"35 p.","startPage":"235","endPage":"269","costCenters":[],"links":[{"id":377367,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"3","noUsgsAuthors":false,"publicationDate":"1958-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Roedder, Edwin","contributorId":25571,"corporation":false,"usgs":true,"family":"Roedder","given":"Edwin","affiliations":[],"preferred":false,"id":795801,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211915,"text":"70211915 - 1958 - Design of simple punched card systems with reference to geochemical problems","interactions":[],"lastModifiedDate":"2020-08-11T18:26:53.691124","indexId":"70211915","displayToPublicDate":"1958-08-11T13:24:01","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Design of simple punched card systems with reference to geochemical problems","docAbstract":"<p><span>A number of critical factors should be considered in the&nbsp;</span><span class=\"ScopusTermHighlight\">design</span><span>&nbsp;of files using marginally&nbsp;</span><span class=\"ScopusTermHighlight\">punched</span><span>&nbsp;cards. These factors are discussed in general terms and exemplified by&nbsp;</span><span class=\"ScopusTermHighlight\">reference</span><span>&nbsp;to a&nbsp;</span><span class=\"ScopusTermHighlight\">system</span><span>&nbsp;developed for use in geo-chemical studies.</span></p>","language":"English","publisher":"GeoScienceWorld","doi":"10.2113/gsecongeo.53.3.325","usgsCitation":"Breger, I., 1958, Design of simple punched card systems with reference to geochemical problems: Economic Geology, v. 53, no. 3, p. 325-338, https://doi.org/10.2113/gsecongeo.53.3.325.","productDescription":"14 p.","startPage":"325","endPage":"338","costCenters":[],"links":[{"id":377362,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"3","noUsgsAuthors":false,"publicationDate":"1958-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Breger, Irving A.","contributorId":41901,"corporation":false,"usgs":true,"family":"Breger","given":"Irving A.","affiliations":[],"preferred":false,"id":795800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211914,"text":"70211914 - 1958 - The solubility of solids in gases","interactions":[],"lastModifiedDate":"2020-08-11T18:20:46.318446","indexId":"70211914","displayToPublicDate":"1958-08-11T13:11:39","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The solubility of solids in gases","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"GeoScienceWorld","doi":"10.2113/gsecongeo.53.3.348","usgsCitation":"Morey, G., 1958, The solubility of solids in gases: Economic Geology, v. 53, no. 3, p. 348-349, https://doi.org/10.2113/gsecongeo.53.3.348.","productDescription":"2 p.","startPage":"348","endPage":"349","costCenters":[],"links":[{"id":377360,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"3","noUsgsAuthors":false,"publicationDate":"1958-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Morey, G.W.","contributorId":108155,"corporation":false,"usgs":true,"family":"Morey","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":795799,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211913,"text":"70211913 - 1958 - Limestone aquifers of Maryland","interactions":[],"lastModifiedDate":"2020-08-11T18:08:28.465533","indexId":"70211913","displayToPublicDate":"1958-08-11T13:02:12","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Limestone aquifers of Maryland","docAbstract":"<p><span>Limestone rocks are an important source of ground water in the Piedmont and Appalachian areas of Maryland. The major limestone aquifers are the Cockeysville and Wakefield marbles and the Silver Run, Tomstown, Frederick, Grove, Waynesboro, Elbrook, Conococheague, Beekmantown, Stones River, Tonoloway, Helderberg and Greenbrier formations. Drilled and dug wells and springs are common sources of water supply in the limestone areas. The depths of 298 limestone wells range from 8.7 to 1,800 feet and average about 150 feet. The yields of these wells range from 0.1 to 575 gpm. Specific capacities, or yield per foot of drawdown, range in 137 wells from 0.1 to 43 gpm per foot. Springs are common in the limestone areas and their flow varies widely at different times. Most of the known springs are of the 5th magnitude or lower, and therefore have a mean flow of less than 100 gpm. The quality of water from the limestone aquifers is satisfactory for most purposes, but is commonly hard and slightly alkaline. The limestone aquifers are large essentially untapped ground-water reservoirs whose hydrologic character is only partially understood.&nbsp;</span></p>","language":"English","publisher":"GeoScienceWorld","doi":"10.2113/gsecongeo.53.6.722","usgsCitation":"Otton, E.G., and Richardson, C.A., 1958, Limestone aquifers of Maryland: Economic Geology, v. 53, no. 6, p. 722-736, https://doi.org/10.2113/gsecongeo.53.6.722.","productDescription":"15 p.","startPage":"722","endPage":"736","costCenters":[],"links":[{"id":377358,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Limestone aquifers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.508056640625,\n              38.762650338334154\n            ],\n            [\n              -75.59692382812499,\n              38.762650338334154\n            ],\n            [\n              -75.59692382812499,\n              39.76632525654491\n            ],\n            [\n              -79.508056640625,\n              39.76632525654491\n            ],\n            [\n              -79.508056640625,\n              38.762650338334154\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"53","issue":"6","noUsgsAuthors":false,"publicationDate":"1958-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Otton, Edmond G.","contributorId":96989,"corporation":false,"usgs":true,"family":"Otton","given":"Edmond","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":795797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richardson, Claire A.","contributorId":33299,"corporation":false,"usgs":true,"family":"Richardson","given":"Claire","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":795798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211904,"text":"70211904 - 1958 - Titaniferous sedimentary rocks in the Cuyuna district, central Minnesot","interactions":[],"lastModifiedDate":"2020-08-11T18:00:21.979979","indexId":"70211904","displayToPublicDate":"1958-08-11T12:49:55","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Titaniferous sedimentary rocks in the Cuyuna district, central Minnesot","docAbstract":"<p><span>The ore-yielding main iron-formation of the Cuyuna district is strati-graphically overlain by approximately 300 feet of titaniferous sedimentary rocks, and a field test for titahia has been an effective supplement to customary stratigraphic studies. The titanium is in leucoxene.</span></p><p><span> The sedimentary rocks of the district are highly folded, and the main iron-formation serves as the reference for relative stratigraphic position. The strata older than the main iron-formation are light-gray argillite and siltstone with local lenses of quartzite near the upper contact; the older strata contain about 0.5 percent titania. The main iron-formation is a persistent layer of chemically precipitated ferruginous sediments that contain about 0.2 percent titania. The strata younger than the main iron-formation are gray or black argillite, partly carbonaceous, partly ferruginous, and are transitional into lenses of lean upper iron-formation. At the base of the younger strata, 250-350 feet of argillite and slate contain 1-3.7 percent titania and average 2.0 percent. This titaniferous argillite is similar to argillite higher in the younger sequence which contains less than 1.5 percent titania and averages about 1 percent. There are weathered rocks interpreted as tuffs and basalt flows locally interlayered near the bottom of the titaniferous zone. The basalt contains 1-2 percent titania. The high titania content of the 250-350-foot zone suggests a volcanic origin; the argillite probably is reworked basaltic pyroclastics. A few titaniferous bodies have been found in rocks below, within, and above the main iron-formation and thin titaniferous argillaceous layers occur within the main iron-formation.</span></p>","language":"English","publisher":"GeoScienceWorld","doi":"10.2113/gsecongeo.53.6.708","usgsCitation":"Schmidt, R.G., 1958, Titaniferous sedimentary rocks in the Cuyuna district, central Minnesot: Economic Geology, v. 53, no. 6, p. 708-721, https://doi.org/10.2113/gsecongeo.53.6.708.","productDescription":"14 p.","startPage":"708","endPage":"721","costCenters":[],"links":[{"id":377356,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Cuyuna District","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.3173828125,\n              45.82879925192134\n            ],\n            [\n              -93.36181640625,\n              45.82879925192134\n            ],\n            [\n              -93.36181640625,\n              47.07012182383309\n            ],\n            [\n              -95.3173828125,\n              47.07012182383309\n            ],\n            [\n              -95.3173828125,\n              45.82879925192134\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"53","issue":"6","noUsgsAuthors":false,"publicationDate":"1958-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Schmidt, R. G.","contributorId":107690,"corporation":false,"usgs":true,"family":"Schmidt","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":795734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211899,"text":"70211899 - 1958 - Terrain diagrams in isometric projection – Simplified","interactions":[],"lastModifiedDate":"2020-08-11T17:46:33.788731","indexId":"70211899","displayToPublicDate":"1958-08-11T12:26:47","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":797,"text":"Annals of the Association of American Geographers","active":true,"publicationSubtype":{"id":10}},"title":"Terrain diagrams in isometric projection – Simplified","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Taylor & Francis Online","doi":"10.1111/j.1467-8306.1958.tb01577.x","usgsCitation":"Stacy, J., 1958, Terrain diagrams in isometric projection – Simplified: Annals of the Association of American Geographers, v. 48, no. 3, p. 22-236, https://doi.org/10.1111/j.1467-8306.1958.tb01577.x.","productDescription":"5 p.","startPage":"22","endPage":"236","costCenters":[],"links":[{"id":377347,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stacy, J.R.","contributorId":105803,"corporation":false,"usgs":true,"family":"Stacy","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":795724,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010454,"text":"70010454 - 1958 - Dating of Zawi Chemi, an early village site at Shanidar, northern Iraq","interactions":[],"lastModifiedDate":"2026-02-27T17:23:37.107094","indexId":"70010454","displayToPublicDate":"1958-06-20T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Dating of Zawi Chemi, an early village site at Shanidar, northern Iraq","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.127.3312.1446.a","issn":"00368075","usgsCitation":"Solecki, R., and Rubin, M., 1958, Dating of Zawi Chemi, an early village site at Shanidar, northern Iraq: Science, v. 127, no. 3312, p. 1446-1446, https://doi.org/10.1126/science.127.3312.1446.a.","productDescription":"1 p.","startPage":"1446","endPage":"1446","costCenters":[],"links":[{"id":218869,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Iraq","otherGeospatial":"Shanidar, northern Iraq","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              44.15165755288794,\n              36.95913896955399\n            ],\n            [\n              44.15165755288794,\n              36.781048118532254\n            ],\n            [\n              44.50784554807424,\n              36.781048118532254\n            ],\n            [\n              44.50784554807424,\n              36.95913896955399\n            ],\n            [\n              44.15165755288794,\n              36.95913896955399\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"127","issue":"3312","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fde1e4b0c8380cd4e9b6","contributors":{"authors":[{"text":"Solecki, R.S.","contributorId":99284,"corporation":false,"usgs":true,"family":"Solecki","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":358965,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":358964,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175839,"text":"70175839 - 1958 - Correlation of ground-water levels and air temperatures in the winter and spring in Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T10:16:49","indexId":"70175839","displayToPublicDate":"1958-06-17T12:45:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5181,"text":"Technical Paper","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"1","title":"Correlation of ground-water levels and air temperatures in the winter and spring in Minnesota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Minnesota Department of Conservation, Division of Waters","publisherLocation":"St. Paul, MN","usgsCitation":"Schneider, R., 1958, Correlation of ground-water levels and air temperatures in the winter and spring in Minnesota: Technical Paper 1, 17 p.","productDescription":"17 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":327022,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-92.204691,46.704041],[-92.205192,46.698341],[-92.183091,46.695241],[-92.176091,46.686341],[-92.204092,46.666941],[-92.201592,46.656641],[-92.207092,46.651941],[-92.242493,46.649241],[-92.256592,46.658741],[-92.270592,46.650741],[-92.274392,46.657441],[-92.286192,46.660342],[-92.287392,46.667342],[-92.291292,46.668142],[-92.292192,46.663308],[-92.294033,46.074377],[-92.332912,46.062697],[-92.35176,46.015685],[-92.372717,46.014198],[-92.410649,46.027259],[-92.428555,46.024241],[-92.442259,46.016177],[-92.453373,45.992913],[-92.464512,45.985038],[-92.461138,45.980216],[-92.469354,45.973811],[-92.527052,45.983245],[-92.548459,45.969056],[-92.551186,45.95224],[-92.60246,45.940815],[-92.614314,45.934529],[-92.638824,45.934166],[-92.638474,45.925971],[-92.659549,45.922937],[-92.676167,45.912072],[-92.675737,45.907478],[-92.707702,45.894901],[-92.734039,45.868108],[-92.739278,45.84758],[-92.765146,45.830183],[-92.757815,45.806574],[-92.776496,45.790014],[-92.784621,45.764196],[-92.809837,45.744172],[-92.869193,45.717568],[-92.870025,45.697272],[-92.875488,45.689014],[-92.887929,45.639006],[-92.882529,45.610216],[-92.886442,45.598679],[-92.883749,45.575483],[-92.871082,45.567581],[-92.823309,45.560934],[-92.770223,45.566939],[-92.726082,45.541112],[-92.726677,45.514462],[-92.702224,45.493046],[-92.680234,45.464344],[-92.653549,45.455346],[-92.646602,45.441635],[-92.650422,45.398507],[-92.664102,45.393309],[-92.676961,45.380137],[-92.678223,45.373604],[-92.70272,45.358472],[-92.698967,45.336374],[-92.709968,45.321302],[-92.737122,45.300459],[-92.761013,45.289028],[-92.760615,45.278827],[-92.751659,45.26591],[-92.760249,45.2496],[-92.751708,45.218666],[-92.763908,45.204866],[-92.767408,45.190166],[-92.764872,45.182812],[-92.752404,45.173916],[-92.757707,45.155466],[-92.739584,45.115598],[-92.744938,45.108309],[-92.791528,45.079647],[-92.803079,45.060978],[-92.793282,45.047178],[-92.770362,45.033803],[-92.76206,45.02432],[-92.771231,45.001378],[-92.769445,44.97215],[-92.754603,44.955767],[-92.750645,44.937299],[-92.758701,44.908979],[-92.774571,44.898084],[-92.773946,44.889997],[-92.764133,44.875905],[-92.769102,44.862167],[-92.765278,44.837186],[-92.78043,44.812589],[-92.785206,44.792303],[-92.805287,44.768361],[-92.807988,44.75147],[-92.787906,44.737432],[-92.737259,44.717155],[-92.700948,44.693751],[-92.660988,44.660884],[-92.632105,44.649027],[-92.619779,44.634195],[-92.621456,44.615017],[-92.601516,44.612052],[-92.586216,44.600088],[-92.569434,44.603539],[-92.549777,44.58113],[-92.549957,44.568988],[-92.540551,44.567258],[-92.518358,44.575183],[-92.493808,44.566063],[-92.481001,44.568276],[-92.455105,44.561886],[-92.433256,44.5655],[-92.399281,44.558292],[-92.361518,44.558935],[-92.336114,44.554004],[-92.314071,44.538014],[-92.302466,44.516487],[-92.302215,44.500298],[-92.291005,44.485464],[-92.232472,44.445434],[-92.195378,44.433792],[-92.124513,44.422115],[-92.111085,44.413948],[-92.078605,44.404869],[-92.056486,44.402729],[-92.038147,44.388731],[-91.970266,44.365842],[-91.941311,44.340978],[-91.92559,44.333548],[-91.918625,44.322671],[-91.913534,44.311392],[-91.924613,44.291815],[-91.896388,44.27469],[-91.896008,44.262871],[-91.88704,44.251772],[-91.892698,44.231105],[-91.877429,44.212921],[-91.872369,44.199167],[-91.829167,44.17835],[-91.808064,44.159262],[-91.751747,44.134786],[-91.721552,44.130342],[-91.710597,44.12048],[-91.708207,44.105186],[-91.69531,44.09857],[-91.68153,44.0974],[-91.667006,44.086964],[-91.647873,44.064109],[-91.638115,44.063285],[-91.610487,44.04931],[-91.59207,44.031372],[-91.507121,44.01898],[-91.48087,44.008145],[-91.463515,44.009041],[-91.432522,43.996827],[-91.407395,43.965148],[-91.385785,43.954239],[-91.366642,43.937463],[-91.357426,43.917231],[-91.347741,43.911964],[-91.338141,43.897664],[-91.320605,43.888491],[-91.310991,43.867381],[-91.284138,43.847065],[-91.262436,43.792166],[-91.244135,43.774667],[-91.255431,43.744876],[-91.255932,43.729849],[-91.268455,43.709824],[-91.273252,43.666623],[-91.271749,43.654929],[-91.262397,43.64176],[-91.268748,43.615348],[-91.232707,43.583533],[-91.232812,43.564842],[-91.243214,43.550722],[-91.243183,43.540309],[-91.232941,43.523967],[-91.218292,43.514434],[-91.217706,43.50055],[-96.453049,43.500415],[-96.453067,45.298115],[-96.489065,45.357071],[-96.521787,45.375645],[-96.562142,45.38609],[-96.617726,45.408092],[-96.680454,45.410499],[-96.692541,45.417338],[-96.731396,45.45702],[-96.76528,45.521414],[-96.857751,45.605962],[-96.844211,45.639583],[-96.835769,45.649648],[-96.760866,45.687518],[-96.745086,45.701576],[-96.662595,45.738682],[-96.641941,45.759871],[-96.627778,45.786239],[-96.583085,45.820024],[-96.574517,45.843098],[-96.561334,45.945655],[-96.57035,45.963595],[-96.57794,46.026874],[-96.559271,46.058272],[-96.554507,46.083978],[-96.557952,46.102442],[-96.56692,46.11475],[-96.563043,46.119512],[-96.571439,46.12572],[-96.56926,46.133686],[-96.579453,46.147601],[-96.577952,46.165843],[-96.587408,46.178164],[-96.584372,46.204155],[-96.59755,46.227733],[-96.598645,46.241626],[-96.590942,46.250183],[-96.59887,46.26069],[-96.595014,46.275135],[-96.60136,46.30413],[-96.599761,46.330386],[-96.619991,46.340135],[-96.618147,46.344295],[-96.629211,46.352654],[-96.644335,46.351908],[-96.646341,46.360982],[-96.655206,46.365964],[-96.658436,46.373391],[-96.666028,46.374566],[-96.669132,46.390037],[-96.680687,46.407383],[-96.688082,46.40788],[-96.701358,46.420584],[-96.703078,46.429467],[-96.718074,46.438255],[-96.715557,46.463232],[-96.73627,46.48138],[-96.737798,46.489785],[-96.733612,46.497224],[-96.737702,46.50077],[-96.738475,46.525793],[-96.744341,46.533006],[-96.743003,46.54294],[-96.74883,46.558127],[-96.744436,46.56596],[-96.746442,46.574078],[-96.772446,46.600129],[-96.774094,46.613288],[-96.78995,46.631531],[-96.790663,46.649112],[-96.798823,46.658071],[-96.792958,46.677427],[-96.784339,46.685054],[-96.790906,46.70297],[-96.779252,46.727429],[-96.784279,46.732993],[-96.781216,46.740944],[-96.787466,46.756753],[-96.784314,46.766973],[-96.796195,46.789881],[-96.795756,46.807795],[-96.801446,46.810401],[-96.80016,46.819664],[-96.787657,46.827817],[-96.789663,46.832306],[-96.779347,46.843672],[-96.781358,46.879363],[-96.768458,46.879563],[-96.767358,46.883663],[-96.773558,46.884763],[-96.776558,46.895663],[-96.759241,46.918223],[-96.761757,46.934663],[-96.78312,46.925482],[-96.79038,46.929398],[-96.791558,46.944464],[-96.797734,46.9464],[-96.798737,46.962399],[-96.821852,46.969372],[-96.82318,46.999965],[-96.834221,47.006671],[-96.829499,47.021537],[-96.818557,47.02778],[-96.821422,47.032842],[-96.819321,47.0529],[-96.824479,47.059682],[-96.818175,47.104193],[-96.827344,47.120144],[-96.824807,47.124968],[-96.831547,47.142017],[-96.822377,47.162744],[-96.829637,47.17497],[-96.826962,47.182802],[-96.838806,47.197894],[-96.832789,47.203911],[-96.838806,47.22502],[-96.832946,47.237588],[-96.83766,47.240876],[-96.835368,47.250428],[-96.841672,47.258164],[-96.838997,47.267716],[-96.842531,47.269531],[-96.844088,47.289981],[-96.832884,47.30449],[-96.841958,47.316907],[-96.835845,47.321014],[-96.835845,47.335914],[-96.852417,47.366241],[-96.848907,47.370565],[-96.852676,47.374973],[-96.846925,47.376891],[-96.840621,47.389881],[-96.845492,47.394179],[-96.844919,47.399815],[-96.863593,47.418775],[-96.85748,47.440457],[-96.859868,47.470926],[-96.85471,47.478281],[-96.85853,47.489934],[-96.851653,47.497098],[-96.851367,47.509037],[-96.866363,47.524893],[-96.85471,47.535973],[-96.859153,47.566355],[-96.853689,47.570381],[-96.856373,47.575749],[-96.851293,47.589264],[-96.856903,47.602329],[-96.855421,47.60875],[-96.873671,47.613654],[-96.871005,47.616832],[-96.879496,47.620576],[-96.882393,47.633489],[-96.888573,47.63845],[-96.882376,47.649025],[-96.88697,47.653049],[-96.887126,47.666369],[-96.895271,47.67357],[-96.899352,47.689473],[-96.908928,47.688722],[-96.907266,47.693976],[-96.920119,47.710383],[-96.923544,47.718201],[-96.919471,47.722515],[-96.932809,47.737139],[-96.928505,47.748037],[-96.934173,47.752412],[-96.939179,47.768397],[-96.9644,47.782995],[-96.957283,47.790147],[-96.966068,47.797297],[-96.975131,47.798326],[-96.980579,47.805614],[-96.979327,47.824533],[-96.986685,47.837639],[-96.998295,47.841724],[-96.998144,47.858882],[-97.005557,47.863977],[-97.002456,47.868677],[-97.023156,47.874978],[-97.019355,47.880278],[-97.024955,47.886878],[-97.019155,47.889778],[-97.024955,47.894978],[-97.020155,47.900478],[-97.024955,47.908178],[-97.017254,47.905678],[-97.015354,47.910278],[-97.023754,47.915878],[-97.018054,47.918078],[-97.035754,47.930179],[-97.036054,47.939379],[-97.054554,47.946279],[-97.052454,47.957179],[-97.061454,47.96358],[-97.053553,47.991612],[-97.064289,47.998508],[-97.066762,48.009558],[-97.063012,48.013179],[-97.072239,48.019107],[-97.068987,48.026267],[-97.072257,48.048068],[-97.097772,48.07108],[-97.103052,48.071669],[-97.099431,48.082106],[-97.105226,48.09044],[-97.104872,48.097851],[-97.109535,48.104723],[-97.123205,48.106648],[-97.120702,48.114987],[-97.131956,48.139563],[-97.141401,48.14359],[-97.138911,48.157793],[-97.146745,48.168556],[-97.141474,48.179099],[-97.146233,48.186054],[-97.134372,48.210434],[-97.136304,48.228984],[-97.141254,48.234668],[-97.135763,48.237596],[-97.138765,48.244991],[-97.127276,48.253323],[-97.131846,48.267589],[-97.11657,48.279661],[-97.12216,48.290056],[-97.128862,48.292882],[-97.122072,48.300865],[-97.132443,48.315489],[-97.127601,48.323319],[-97.134854,48.331314],[-97.131145,48.339722],[-97.147748,48.359905],[-97.140106,48.380479],[-97.145592,48.394195],[-97.135012,48.406735],[-97.142849,48.419471],[-97.1356,48.424369],[-97.139173,48.430528],[-97.134229,48.439797],[-97.137689,48.447583],[-97.132746,48.459942],[-97.144116,48.469212],[-97.141397,48.476256],[-97.144981,48.481571],[-97.140291,48.484722],[-97.138864,48.494362],[-97.148133,48.503384],[-97.153076,48.524148],[-97.150481,48.536877],[-97.163105,48.543855],[-97.160863,48.549236],[-97.152459,48.552326],[-97.158638,48.564067],[-97.149616,48.569876],[-97.14974,48.579516],[-97.142915,48.583733],[-97.143684,48.597066],[-97.137504,48.612268],[-97.132931,48.61338],[-97.130089,48.621166],[-97.125639,48.620919],[-97.125269,48.629694],[-97.108466,48.632658],[-97.111921,48.642918],[-97.100551,48.658614],[-97.102652,48.664793],[-97.097708,48.68395],[-97.118286,48.700573],[-97.116185,48.709348],[-97.136083,48.727763],[-97.139488,48.746611],[-97.151289,48.757428],[-97.147478,48.763698],[-97.154854,48.774515],[-97.157093,48.790024],[-97.163535,48.79507],[-97.165624,48.809627],[-97.180028,48.81845],[-97.177747,48.824815],[-97.181116,48.832741],[-97.173811,48.838309],[-97.175618,48.853105],[-97.187362,48.867598],[-97.185738,48.87222],[-97.197982,48.880341],[-97.197982,48.898332],[-97.210541,48.90439],[-97.211161,48.916649],[-97.217992,48.919735],[-97.218666,48.931781],[-97.224505,48.9341],[-97.232147,48.948955],[-97.230859,48.960891],[-97.239209,48.968684],[-97.237297,48.985696],[-97.230833,48.991303],[-97.229039,49.000687],[-95.153711,48.998903],[-95.15335,49.383079],[-95.126467,49.369439],[-95.058404,49.35317],[-95.014415,49.356405],[-94.988908,49.368897],[-94.957465,49.370186],[-94.854245,49.324154],[-94.816222,49.320987],[-94.824291,49.308834],[-94.82516,49.294283],[-94.797244,49.214284],[-94.797527,49.197791],[-94.773223,49.120733],[-94.750221,49.099763],[-94.750218,48.999992],[-94.718932,48.999991],[-94.683069,48.883929],[-94.684217,48.872399],[-94.692527,48.86895],[-94.693044,48.853392],[-94.685681,48.840119],[-94.701968,48.831778],[-94.704284,48.824284],[-94.694974,48.809206],[-94.694312,48.789352],[-94.690889,48.778066],[-94.651765,48.755913],[-94.645164,48.749975],[-94.645083,48.744143],[-94.61901,48.737374],[-94.58715,48.717599],[-94.549069,48.714653],[-94.533057,48.701262],[-94.452332,48.692444],[-94.438701,48.694889],[-94.416191,48.710948],[-94.384221,48.711806],[-94.342758,48.703382],[-94.308446,48.710239],[-94.290737,48.707747],[-94.260541,48.696381],[-94.251169,48.683514],[-94.254643,48.663888],[-94.250497,48.656654],[-94.224276,48.649527],[-94.091244,48.643669],[-94.065775,48.646104],[-94.035616,48.641018],[-94.006933,48.643193],[-93.944221,48.632294],[-93.91153,48.634673],[-93.840754,48.628548],[-93.824144,48.610724],[-93.806763,48.577616],[-93.811201,48.542385],[-93.818253,48.530046],[-93.794454,48.516021],[-93.656652,48.515731],[-93.643091,48.518294],[-93.628865,48.53121],[-93.612844,48.521876],[-93.60587,48.522472],[-93.594379,48.528793],[-93.547191,48.528684],[-93.467504,48.545664],[-93.460798,48.550552],[-93.456675,48.561834],[-93.465199,48.590659],[-93.438494,48.59338],[-93.405269,48.609344],[-93.395022,48.603303],[-93.371156,48.605085],[-93.362132,48.613832],[-93.35324,48.613378],[-93.349095,48.624935],[-93.254854,48.642784],[-93.207398,48.642474],[-93.178095,48.623339],[-93.088438,48.627597],[-92.984963,48.623731],[-92.954876,48.631493],[-92.95012,48.630419],[-92.949839,48.608269],[-92.929614,48.606874],[-92.909947,48.596313],[-92.894687,48.594915],[-92.728046,48.53929],[-92.657881,48.546263],[-92.634931,48.542873],[-92.625739,48.518189],[-92.631117,48.508252],[-92.627237,48.503383],[-92.636696,48.499428],[-92.654039,48.501635],[-92.661418,48.496557],[-92.698824,48.494892],[-92.712562,48.463013],[-92.687998,48.443889],[-92.656027,48.436709],[-92.507285,48.447875],[-92.475585,48.418793],[-92.456325,48.414204],[-92.456389,48.401134],[-92.47675,48.37176],[-92.469948,48.351836],[-92.437825,48.309839],[-92.416285,48.295463],[-92.369174,48.220268],[-92.336831,48.235383],[-92.269742,48.248241],[-92.273706,48.256747],[-92.294541,48.27156],[-92.292999,48.276404],[-92.301451,48.288608],[-92.294527,48.306454],[-92.306309,48.316442],[-92.304561,48.322977],[-92.295412,48.323957],[-92.288994,48.342991],[-92.26228,48.354933],[-92.222813,48.349203],[-92.216983,48.345114],[-92.206803,48.345596],[-92.203684,48.352063],[-92.178418,48.351881],[-92.177354,48.357228],[-92.145049,48.365651],[-92.143583,48.356121],[-92.083513,48.353865],[-92.077961,48.358253],[-92.055228,48.359213],[-92.045734,48.347901],[-92.046562,48.33474],[-92.037721,48.333183],[-92.030872,48.325824],[-92.000133,48.321355],[-92.01298,48.297391],[-92.006577,48.265421],[-91.989545,48.260214],[-91.976903,48.244626],[-91.971056,48.247667],[-91.971779,48.252977],[-91.954432,48.251678],[-91.952209,48.244394],[-91.957683,48.242683],[-91.957798,48.232989],[-91.941838,48.230602],[-91.915772,48.238871],[-91.89347,48.237699],[-91.884691,48.227321],[-91.867882,48.219095],[-91.864382,48.207031],[-91.815772,48.211748],[-91.809038,48.206013],[-91.79181,48.202492],[-91.789011,48.196549],[-91.756637,48.205022],[-91.749075,48.198844],[-91.741932,48.199122],[-91.742313,48.204491],[-91.714931,48.19913],[-91.711611,48.1891],[-91.721413,48.180255],[-91.724584,48.170657],[-91.705318,48.170775],[-91.70726,48.153661],[-91.698174,48.141643],[-91.699981,48.13184],[-91.712226,48.116883],[-91.703524,48.113548],[-91.682845,48.122118],[-91.687623,48.111698],[-91.676876,48.107264],[-91.665208,48.107011],[-91.653261,48.114137],[-91.653571,48.109567],[-91.640175,48.096926],[-91.559272,48.108268],[-91.552962,48.103012],[-91.569746,48.093348],[-91.575471,48.066294],[-91.575672,48.048791],[-91.567254,48.043719],[-91.488646,48.068065],[-91.45033,48.068806],[-91.437582,48.049248],[-91.429642,48.048608],[-91.391128,48.057075],[-91.370872,48.06941],[-91.365143,48.066968],[-91.340159,48.073236],[-91.332589,48.069331],[-91.26638,48.078713],[-91.214428,48.10294],[-91.190461,48.124891],[-91.183207,48.122235],[-91.176181,48.125811],[-91.137733,48.14915],[-91.139402,48.154738],[-91.092258,48.173101],[-91.082731,48.180756],[-91.024208,48.190072],[-90.976955,48.219452],[-90.914971,48.230603],[-90.88548,48.245784],[-90.875107,48.237784],[-90.847352,48.244443],[-90.839176,48.239511],[-90.836313,48.176963],[-90.832589,48.173765],[-90.821115,48.184709],[-90.817698,48.179569],[-90.804207,48.177833],[-90.796596,48.159373],[-90.777917,48.163801],[-90.778031,48.148723],[-90.79797,48.136894],[-90.787305,48.134196],[-90.789919,48.129902],[-90.76911,48.116585],[-90.761555,48.100133],[-90.751608,48.090968],[-90.641596,48.103515],[-90.626886,48.111846],[-90.59146,48.117546],[-90.582217,48.123784],[-90.55929,48.121683],[-90.555845,48.117069],[-90.569763,48.106951],[-90.567482,48.101178],[-90.556838,48.096008],[-90.487077,48.099082],[-90.467712,48.108818],[-90.438449,48.098747],[-90.403219,48.105114],[-90.374542,48.090942],[-90.367658,48.094577],[-90.344234,48.094447],[-90.330052,48.102399],[-90.312386,48.1053],[-90.289337,48.098993],[-90.224692,48.108148],[-90.188679,48.107947],[-90.176605,48.112445],[-90.136191,48.112136],[-90.116259,48.104303],[-90.073873,48.101138],[-90.023595,48.084708],[-90.015057,48.067188],[-90.008446,48.068396],[-89.997852,48.057567],[-89.99305,48.028404],[-89.97718,48.023501],[-89.968255,48.014482],[-89.954605,48.011516],[-89.95059,48.015901],[-89.934489,48.015628],[-89.915341,47.994866],[-89.897414,47.987599],[-89.873286,47.985419],[-89.868153,47.989898],[-89.847571,47.992442],[-89.842568,48.001368],[-89.830385,48.000284],[-89.820483,48.014665],[-89.797744,48.014505],[-89.763967,48.022969],[-89.724048,48.018996],[-89.721038,48.017965],[-89.724044,48.013675],[-89.716114,48.016441],[-89.716417,48.010251],[-89.702528,48.006325],[-89.673798,48.01151],[-89.667128,48.007421],[-89.657051,48.009954],[-89.649057,48.003853],[-89.617867,48.010947],[-89.611678,48.017529],[-89.607821,48.006566],[-89.594749,48.004332],[-89.582117,47.996314],[-89.564288,48.00293],[-89.489226,48.014528],[-89.495344,48.002356],[-89.541521,47.992841],[-89.551555,47.987305],[-89.555015,47.974849],[-89.572315,47.967238],[-89.58823,47.9662],[-89.611412,47.980731],[-89.624559,47.983153],[-89.631825,47.980039],[-89.640129,47.96793],[-89.638285,47.954275],[-89.697619,47.941288],[-89.793539,47.891358],[-89.85396,47.873997],[-89.87158,47.874194],[-89.923649,47.862062],[-89.930844,47.857723],[-89.92752,47.850825],[-89.933899,47.84676],[-89.974296,47.830514],[-90.072025,47.811105],[-90.075559,47.803303],[-90.1168,47.79538],[-90.16079,47.792807],[-90.178755,47.786414],[-90.187636,47.77813],[-90.248794,47.772763],[-90.323446,47.753771],[-90.332686,47.746387],[-90.437712,47.731612],[-90.441912,47.726404],[-90.458365,47.7214],[-90.537105,47.703055],[-90.551291,47.690266],[-90.735927,47.624343],[-90.86827,47.5569],[-90.907494,47.532873],[-90.914247,47.522639],[-90.939072,47.514532],[-91.032945,47.458236],[-91.045646,47.456525],[-91.097569,47.413888],[-91.128131,47.399619],[-91.146958,47.381464],[-91.156513,47.378816],[-91.188772,47.340082],[-91.238658,47.304976],[-91.262512,47.27929],[-91.288478,47.26596],[-91.326019,47.238993],[-91.357803,47.206743],[-91.418805,47.172152],[-91.477351,47.125667],[-91.497902,47.122579],[-91.518793,47.108121],[-91.573817,47.089917],[-91.591508,47.068684],[-91.626824,47.049953],[-91.644564,47.026491],[-91.666477,47.014297],[-91.704649,47.005246],[-91.780675,46.945881],[-91.806851,46.933727],[-91.841349,46.925215],[-91.883238,46.905728],[-91.914984,46.883836],[-91.952985,46.867037],[-92.094089,46.787839],[-92.088289,46.773639],[-92.06449,46.745439],[-92.025789,46.710839],[-92.01529,46.706469],[-92.020289,46.704039],[-92.03399,46.708939],[-92.08949,46.74924],[-92.10819,46.74914],[-92.13789,46.73954],[-92.14329,46.73464],[-92.141291,46.72524],[-92.146291,46.71594],[-92.167291,46.719941],[-92.189091,46.717541],[-92.204691,46.704041]]]},\"properties\":{\"name\":\"Minnesota\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82db2e4b03fd6b7da3663","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":646433,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220584,"text":"5220584 - 1958 - Aspergillosis in waterfowl","interactions":[],"lastModifiedDate":"2025-07-25T15:39:28.787199","indexId":"5220584","displayToPublicDate":"1958-06-16T12:18:25","publicationYear":"1958","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Aspergillosis in waterfowl","docAbstract":"<p>No abstract available.</p>","conferenceTitle":"Twenty-third North American Wildlife Conference","conferenceDate":"March 3-5, 1958","conferenceLocation":"St. Louis, MO","language":"English","publisher":"Wildlife Management Institute","usgsCitation":"Herman, C.M., and Sladen, W.J., 1958, Aspergillosis in waterfowl, Twenty-third North American Wildlife Conference, St. Louis, MO, March 3-5, 1958, p. 187-191.","productDescription":"5 p.","startPage":"187","endPage":"191","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":492912,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wildlifemanagement.institute/conference/transactions/1958","linkFileType":{"id":5,"text":"html"}},{"id":196157,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672b46","contributors":{"authors":[{"text":"Herman, Carlton M.","contributorId":88718,"corporation":false,"usgs":true,"family":"Herman","given":"Carlton","email":"","middleInitial":"M.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":332052,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sladen, William J.L.","contributorId":85676,"corporation":false,"usgs":false,"family":"Sladen","given":"William","email":"","middleInitial":"J.L.","affiliations":[],"preferred":false,"id":332051,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221316,"text":"5221316 - 1958 - Mass control of insects: The effects on fish and wildlife","interactions":[],"lastModifiedDate":"2023-08-30T16:28:53.825439","indexId":"5221316","displayToPublicDate":"1958-06-16T12:18:25","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1122,"text":"Bulletin of the Entomological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Mass control of insects: The effects on fish and wildlife","docAbstract":"<p><span>The mass control of insects carried on during the past ten years has made possible the economical suppression and, in a few instances, the near eradication of pest insect populations over widespread areas. These large operations, usually featuring the use of the airplane for applying insecticides quickly and cheaply, have proven to be the means of effectuating control programs which never could have been carried on through use of the techniques and equipment of early-day economic entomology. With the development of the methods employed in modern mass control came the introduction of new toxicants, well-adapted for use against insects because of their potency, low cost and wide availability. The present-day entomologist is thus armed with the means to carry on a control task of almost any magnitude.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1093/besa/4.2.52","usgsCitation":"Cope, O.B., and Springer, P.F., 1958, Mass control of insects: The effects on fish and wildlife: Bulletin of the Entomological Society of America, v. 4, no. 2, p. 52-56, https://doi.org/10.1093/besa/4.2.52.","productDescription":"5 p.","startPage":"52","endPage":"56","numberOfPages":"5","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196945,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605a48","contributors":{"authors":[{"text":"Cope, Oliver B.","contributorId":13290,"corporation":false,"usgs":true,"family":"Cope","given":"Oliver","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":333546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Springer, Paul F.","contributorId":70445,"corporation":false,"usgs":true,"family":"Springer","given":"Paul","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":333547,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}