{"pageNumber":"7238","pageRowStart":"180925","pageSize":"25","recordCount":184828,"records":[{"id":70171144,"text":"70171144 - 1935 - Some general considerations of plankton and plankton problems with reference to water supplies","interactions":[],"lastModifiedDate":"2016-05-24T09:07:15","indexId":"70171144","displayToPublicDate":"1935-01-01T00:00:00","publicationYear":"1935","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Some general considerations of plankton and plankton problems with reference to water supplies","docAbstract":"

No abstract available.

","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Papers presented at Ninth Annual Michigan Conference on Water Purification","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Ninth Annual Michigan Conference on Water Purification","language":"English","publisher":"Michigan State College of Agriculture and Applied Science","usgsCitation":"Deason, H.J., 1935, Some general considerations of plankton and plankton problems with reference to water supplies, in Papers presented at Ninth Annual Michigan Conference on Water Purification, p. 5-14.","productDescription":"10 p.","startPage":"5","endPage":"14","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321577,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d6651e4b07e28b6684e7a","contributors":{"authors":[{"text":"Deason, Hilary J.","contributorId":66628,"corporation":false,"usgs":true,"family":"Deason","given":"Hilary","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180103,"text":"70180103 - 1934 - Stream measurement work: Appendix 4 in Nineteenth biennial report of the State Engineer to the governor of Utah: 1933-1934","interactions":[],"lastModifiedDate":"2017-01-24T12:26:39","indexId":"70180103","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1934","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5276,"text":"Utah State Engineer Biennial Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"19","chapter":"Appendix 4","title":"Stream measurement work: Appendix 4 in Nineteenth biennial report of the State Engineer to the governor of Utah: 1933-1934","docAbstract":"

Stream measurement work under the usual co-operative agreement between the U.S. Geological Survey and the State Engineer continued during the biennium for the purpose of determining the water resources of the State. This work in Utah is part of the general plan for a systematic determination of the water resources of the United States begun by the Geological Survey in 1888. Records of stream flow on a few rivers in the West were taken as part of special studies on irrigation, in which connection gaging stations were established on the Bear, Weber, Provo, and Sevier rivers. The Bear River station at Collinston has been maintained continuously since that date.

","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Nineteenth biennial report of the State Engineer to the governor of Utah: 1933-1934","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","usgsCitation":"Purton, A., 1934, Stream measurement work: Appendix 4 in Nineteenth biennial report of the State Engineer to the governor of Utah: 1933-1934: Utah State Engineer Biennial Report 19, 4.","productDescription":"4","startPage":"57","endPage":"60","numberOfPages":"4","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333810,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333809,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-364","text":"Full Text of Biennial Report"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5888770de4b05ccb964bab6d","contributors":{"authors":[{"text":"Purton, A.B.","contributorId":18338,"corporation":false,"usgs":true,"family":"Purton","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":660338,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006897,"text":"70006897 - 1934 - Ulcer disease of trout","interactions":[],"lastModifiedDate":"2015-12-21T07:49:01","indexId":"70006897","displayToPublicDate":"2012-01-01T14:26:22","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Ulcer disease of trout","docAbstract":"During the summer of 1933, lesions of a disease were noted among some fingerling brook, rainbow, blackspotted, and lake trout at the Cortland (New York) trout hatchery. Although these lesions bore a marked superficial resemblance to those of furunculosis, they were sufficiently atypical to warrant further investigation. A more detailed examination of the lesions proved them to be of a distinct disease, which for lack of a better name is herein called \"ulcer disease,\" for the lesions closely resemble those described by Calkins (1899) under this name. Because of the marked resemblance to furunculosis, ulcer disease has not been generally recognized by trout culturists, and any ulcer appearing on fish has been ascribed by them to furunculosis without further question.","language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","doi":"10.1577/1548-8659(1934)64[252:UDOT]2.0.CO;2","usgsCitation":"Fish, F.F., 1934, Ulcer disease of trout: Transactions of the American Fisheries Society, v. 64, no. 1, p. 252-258, https://doi.org/10.1577/1548-8659(1934)64[252:UDOT]2.0.CO;2.","productDescription":"7 p.","startPage":"252","endPage":"258","numberOfPages":"7","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":258315,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258304,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1934)64[252:UDOT]2.0.CO;2","linkFileType":{"id":5,"text":"html"}}],"volume":"64","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbbfbe4b08c986b328954","contributors":{"authors":[{"text":"Fish, F. F.","contributorId":82572,"corporation":false,"usgs":true,"family":"Fish","given":"F.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":355426,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006896,"text":"70006896 - 1934 - A fungus disease in fishes of the Gulf of Maine","interactions":[],"lastModifiedDate":"2016-01-04T12:29:28","indexId":"70006896","displayToPublicDate":"2012-01-01T13:12:07","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3011,"text":"Parasitology","active":true,"publicationSubtype":{"id":10}},"title":"A fungus disease in fishes of the Gulf of Maine","docAbstract":"

1. A fungus disease of epidemic proportions was found in the common sea herring (Clupea harengus) throughout the Gulf of Maine.

\n

2. The fungus was also found to infect the common winter flounder (Pseudopleuronectes americanus) and the alewife (Pomobolus pseudoharengus).

\n

3. The causative agent was found to be a species of fungus belonging to the genus Ichthyosporidium Caullery and Mesnil (1905). The specific name is tentatively accepted as hoferi Plehn and Muslow (1911).

\n

4. The organism is believed to be a normal parasite to the herring and reaches epidemic proportions only when certain unknown factors are operative.

\n

5. The causative organism was found in herring preserved in 1926, and it is believed that the epidemic has been increasing in severity since that time.

\n

6. It is believed that such an epidermic,once initiated, increases in severity, reaches a peak, and subsides to a subpatent level. The peak is believed to have been reached in 1931.

\n

7. The life history and effects of the organism in the herring and flounder are described.

\n

8. The herring is believed to acquire the infection by the ingestion of parasites liberated from fish in the same school.

\n

9. The flounder is believed to acquire the infection by the consumption of infected herring.

\n

10. The alewife is believed to acquire the infection by ingestion of the parasite during its infrequent association with the herring.

\n

11. Infection is believed to be established by way of the alimentary canal and, once established, to spread throughout the host by way of the blood stream or the lymphatics.

\n

12. Direct cross infection from the herring to the flounder establishes the theory that the parasites in these two hosts are one and the same organism.

\n

13. Direct cross infection experiments from the herring to the flounder eliminate the necessity of an intermediate host.

\n

14. There is no reason to believe that this parasite is capable of infecting warm-blooded animals.

","largerWorkTitle":"Parasitology","language":"English","publisher":"Cambridge University Press","publisherLocation":"Cambridge, U.K.","doi":"10.1017/S003118200002326X","usgsCitation":"Fish, F.F., 1934, A fungus disease in fishes of the Gulf of Maine: Parasitology, v. 26, no. 1, p. 1-16, https://doi.org/10.1017/S003118200002326X.","productDescription":"16 p.","startPage":"1","endPage":"16","numberOfPages":"16","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":258369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258359,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1017/S003118200002326X","linkFileType":{"id":5,"text":"html"}}],"country":"United States, Canada","state":"Maine, New Hampshire, Massachusetts, New Brunswick, Nova Scotia","otherGeospatial":"Gulf Of Maine","volume":"26","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-04-06","publicationStatus":"PW","scienceBaseUri":"5059e3e5e4b0c8380cd462b1","contributors":{"authors":[{"text":"Fish, F. F.","contributorId":82572,"corporation":false,"usgs":true,"family":"Fish","given":"F.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":355425,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3471,"text":"cir10 - 1934 - The McCoy mining district and gold veins in Horse Canyon, Lander County, Nevada","interactions":[],"lastModifiedDate":"2019-05-10T08:56:25","indexId":"cir10","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1934","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"10","title":"The McCoy mining district and gold veins in Horse Canyon, Lander County, Nevada","docAbstract":"

The following geologic sketch is based on a two-day visit made to the McCoy district in September 1930. For valuable information and aid generously extended, the writer would express his thanks to the miners and prospectors of the district and especially to Mr. Joseph H. McCoy, a well-known mining man of Nevada and discoverer and founder of the district.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir10","usgsCitation":"Schrader, F.C., 1934, The McCoy mining district and gold veins in Horse Canyon, Lander County, Nevada: U.S. Geological Survey Circular 10, 13 p. , https://doi.org/10.3133/cir10.","productDescription":"13 p. ","numberOfPages":"19","costCenters":[],"links":[{"id":363658,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0010/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0010/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Lander County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b989","contributors":{"authors":[{"text":"Schrader, Frank Charles","contributorId":77917,"corporation":false,"usgs":true,"family":"Schrader","given":"Frank","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":146988,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35653,"text":"b854 - 1934 - Geology and ore deposits of the Casto quadrangle, Idaho","interactions":[],"lastModifiedDate":"2015-12-17T15:24:32","indexId":"b854","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1934","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"854","title":"Geology and ore deposits of the Casto quadrangle, Idaho","docAbstract":"

The study of the Casto quadrangle was undertaken as the first item in a project to obtain more thorough knowledge of the general geology of southcentral Idaho on which to base study of the ore deposits of t he region. The quadrangle conta ins fragmentary exposures of Algonkian and Paleozoic sedimentary rocks, extensive deposits of old volcanic strata, presumably Permian, not heretofore recognized in this part of Idaho, and a thick succession of Oligocene(?) lava and pyroclastic rocks. The Idaho batholith and its satellites extend into the quadrangle, and in addition there a re large masses of Tertiary granitic rock, not previously distinguished in Idaho, and many Tertiary dikes, some of which are genetically associated with contact-metamorphic deposits. The area contains injection gneiss of complex origin, largely related to the Idaho batholith but in part resulting from injection by ~he Tertiary granitic rocks under relatively light load. Orogenic movement took place in Algonkian, Paleozoic, and Tertiary time. There is a summit peneplain or par tial peneplain of Tertiary, perhaps Pliocene age, and the erosional history since its elevation has been complex. The ore deposits include lodes and placers. The lodes are related to both the Idaho batholith and the Tert iary intrusive rocks and have yielded gold and copper ore of a total value of about 1,000,000. Placers, largely formed in an interglacial inter val, have yielded about an equal amount. There has been some prospecting but almost no production since 1916.

","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b854","usgsCitation":"Ross, C.P., 1934, Geology and ore deposits of the Casto quadrangle, Idaho: U.S. Geological Survey Bulletin 854, Report: 135 p.; 1 Plate: 18.48 x 27.70 inches, https://doi.org/10.3133/b854.","productDescription":"Report: 135 p.; 1 Plate: 18.48 x 27.70 inches","numberOfPages":"149","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":167466,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/b854.jpg"},{"id":109521,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21026.htm","linkFileType":{"id":5,"text":"html"},"description":"21026"},{"id":312483,"rank":701,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0854/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":312484,"rank":702,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0854/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Challis National Forest, Salmon National Forest","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.16918945312499,\n 43.16512263158296\n ],\n [\n -117.16918945312499,\n 46.604167162931844\n ],\n [\n -112.91748046874999,\n 46.604167162931844\n ],\n [\n -112.91748046874999,\n 43.16512263158296\n ],\n [\n -117.16918945312499,\n 43.16512263158296\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68464d","contributors":{"authors":[{"text":"Ross, Clyde P.","contributorId":10473,"corporation":false,"usgs":true,"family":"Ross","given":"Clyde","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":215010,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1340,"text":"wsp660 - 1934 - Artesian water in Somervell County, Texas","interactions":[],"lastModifiedDate":"2016-08-22T10:08:31","indexId":"wsp660","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1934","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"660","title":"Artesian water in Somervell County, Texas","docAbstract":"

Somervell County is part of the Grand Prairie region of north-central Texas. An excellent supply of artesian water is available from the Trinity reservoir at no great depth. The first flowing well in Somervell County was drilled in 1880, and the first flowing well in Glen Rose, the county seat, was drilled in 1881. Since 1880 more than 500 wells have been constructed, probably more than half of them prior to 1900. Many of these early wells have been abandoned, either because the well hole caved in as a result of the absence or deterioration of casing or because the wells ceased to yield water by natural flow. The artesian water has always been used chiefly for domestic supply and for watering stock. Only a comparatively small area of farm land is now irrigated. The quantity used to supply the needs of tourist camps and outdoor swimming pools forms a relatively large percentage of the total amount withdrawn from the artesian reservoir in Somervell County. The artesian water is contained chiefly in the permeable sandstone beds--the basal sands for the Trinity group. Some shallow wells of small capacity are supplied by water in the crevices and solution channels in limestone that apparently is near the base of the Glen Rose formation and probably derives its water by leakage from the underlying Trinity reservoir. The wells encounter from one to three aquifers, the number depending upon their depth and location. At and around Glen Rose, the area in which most of the flowing wells are concentrated, the first aquifer is the creviced portion of the limestone, which is encountered at about 50 feet but does not everywhere yield water. The second and third aquifers, both of which are part of the 'basal sands' of the Trinity group, are much more uniform and persistent; the second is encountered at Glen Rose at depths of 100 to 135 feet, and the third at depths of about 275 to 330 feet. The artesian reservoir is supplied by water that falls as rain or snow upon the outcrop of the 'basal sands' on the higher lands west and north of Somervell County. These permeable beds dip eastward and southeastward beneath the county and are covered by the less permeable beds of the overlying Glen Rose formation. As the water that reaches the zone of saturation percolates down the dip of the beds it is confined under artesian pressure, and wells that penetrate these beds at lower altitudes yield water by natural flow. Originally the artesian pressure was sufficient to raise the water in tightly cased wells in the northwestern part of Somervell County to a maximum altitude of about 750 feet above sea level, but at Glen Rose the original artesian head was probably not more than 710 feet. From the information avail- able it would appear that the original head of the water in the upper aquifers was not nearly as great as that of the lower aquifer. The head has declined generally throughout the county. At Glen Rose in June 1930 the artesian head of the water from the deepest aquifer of the Trinity reservoir was about 639 feet above sea level, and the head of the water from the upper aquifers was about 15 feet less. The decline in head still continues, but at a very much slower rate than formerly. With the decline in head the size of the area of artesian flow has decreased, though in recent years the shrinkage has been comparatively little. The draft from the artesian reservoir in Somervell County during the summer is estimated at about 1,000,000 gallons a day, distributed as follows: Domestic use, 150,000 gallons; stock use, 60,000 gallons; recreation pools, 250,000 gallons; irrigation, 180,000 gallons; and waste, not including underground leakage, 360,000 gallons. In winter the daily draft is probably about 370,000 gallons less than in summer. The 360,000 gallons a day permitted to flow from wells without being used for any beneficial purposes is an unnecessary drain upon the artesian reservoir. The head of many of the flowing wells in Glen R

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp660","usgsCitation":"Fiedler, A.G., 1934, Artesian water in Somervell County, Texas: U.S. Geological Survey Water Supply Paper 660, iv, 86 p., https://doi.org/10.3133/wsp660.","productDescription":"iv, 86 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0660/report-thumb.jpg"},{"id":26404,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0660/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c4a","contributors":{"authors":[{"text":"Fiedler, Albert George","contributorId":62192,"corporation":false,"usgs":true,"family":"Fiedler","given":"Albert","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":143592,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1589,"text":"wsp737 - 1934 - Surface water supply of the United States, 1932 : Part 12. North Pacific slope basins : A. Pacific slope basins in Washington and upper Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp737","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1934","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"737","title":"Surface water supply of the United States, 1932 : Part 12. North Pacific slope basins : A. Pacific slope basins in Washington and upper Columbia River basin","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp737","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1934, Surface water supply of the United States, 1932 : Part 12. North Pacific slope basins : A. 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This report presents the preliminary results of the authors' field work in 1931 and 1932 in the drainage basin of the South Fork of Clearwater River and just south of the divide between that stream and Salmon River.

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