In a sandy, riverside location in Wisconsin, my family has a farm, once abandoned by a previous owner because it would not produce much corn. By the time we bought it – for a pittance – only a few remnants of white pine remained from the magnificent stands made famous by the Paul Bunyan legend. In this part of Wisconsin the pines were, even originally, restricted only to patches of the better soil, and the variability of the glacial topography has resulted in an interesting mixture of prairie marsh, swamp woodlot, and sand hill.
We did not acquire this farm because it had great potential for growing crops. Rather we were interested in the variety of ecologic and topographic types, which, even within the confines of our property, represented a condensed version of the many different types of land in the Wisconsin countryside. The farm also has a very peculiar aesthetic and historical interest. Marquette’s canoes once slipped quietly past our favorite fishing hole on the river; passenger pigeons once roosted in our great oaks; and the few remaining white pines silhouetted against the sky-glow of evening made one think of the Round River and the Blue Ox.
","language":"English","publisher":"American Water Works Association","doi":"10.1002/j.1551-8833.1959.tb21165.x","usgsCitation":"Leopold, L.B., 1959, Water resource development and management: Journal of the American Water Works Association, v. 51, no. 7, p. 821-827, https://doi.org/10.1002/j.1551-8833.1959.tb21165.x.","productDescription":"7 p.","startPage":"821","endPage":"827","costCenters":[],"links":[{"id":338133,"rank":2,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir414B","text":"USGS Circular 414-B: The challenge of water management","linkHelpText":"This transcript was also published as a USGS Circular"},{"id":338113,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"7","publicComments":"An address presented on March 11, 1959, at the Illinois Section Meeting, Chicago, Ill, by Luna B. Leopold, Chief Hydraulic Engr., USGS, Washington, D.C.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d38d66e4b0236b68f98f94","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":685787,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014485,"text":"1014485 - 1959 - Plasmoptysis and gelatin of erythrocytes in coagulation of blood of freshwater bony fishes","interactions":[],"lastModifiedDate":"2023-08-29T16:50:24.7837","indexId":"1014485","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1062,"text":"Blood","active":true,"publicationSubtype":{"id":10}},"title":"Plasmoptysis and gelatin of erythrocytes in coagulation of blood of freshwater bony fishes","docAbstract":"1. A clot-like material which results from very rapid plasmoptysis and hydrophyllic swelling of karyoplasm of erythrocytes from freshwater fish was reported. This attribute was found to a lesser degree in erythrocytes from an amphibian, but it was almost lacking in those of an aquatic reptile.
2. Rapid clotting of fish blood with the usual clinical methods was confirmed in this work. Fish blood clotted more quickly with the slide test than with the capillary tube test. In the presence of water, complete coagulation of fish blood occurred in only 65 per cent of the time required for clotting to be completed in air. This speed is attributed to the water-erythrocyte reaction, and not to a quality of the plasma.
3. An attempt was made to correlate the findings with the need for hemostasis and blood coagulation that is peculiar to aquatic vertebrates.
","language":"English","publisher":"American Society of Hematology","doi":"10.1182/blood.V14.12.1339.1339","usgsCitation":"Wolf, K., 1959, Plasmoptysis and gelatin of erythrocytes in coagulation of blood of freshwater bony fishes: Blood, v. 14, no. 12, p. 1339-1344, https://doi.org/10.1182/blood.V14.12.1339.1339.","productDescription":"6 p.","startPage":"1339","endPage":"1344","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":489761,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1182/blood.v14.12.1339.1339","text":"Publisher Index Page"},{"id":131729,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c46e","contributors":{"authors":[{"text":"Wolf, Ken","contributorId":106546,"corporation":false,"usgs":true,"family":"Wolf","given":"Ken","email":"","affiliations":[],"preferred":false,"id":320452,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010775,"text":"70010775 - 1959 - Australia and Gondwanaland","interactions":[],"lastModifiedDate":"2020-11-13T21:00:44.72793","indexId":"70010775","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1795,"text":"Geologische Rundschau","active":true,"publicationSubtype":{"id":10}},"title":"Australia and Gondwanaland","docAbstract":"Along the western margin of the Australian continent there exist four major sedimentary basins, filled with predominantly marine rocks from Cambrian to Tertiary in age, and up to 40,000 feet thick. Seaward these basins continue into depressions recognizable in the continental shelf and even the continental slope. Their very presence, the nature of their sediments and the composition and relationships of their fossil faunas indicate the existence of an open ocean to the west of Australia since early Paleozoic time. Composition of the Australian fossil land vertebrate faunas suggests isolation of the Australian continent since at least Permian time.
","language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF01800675","usgsCitation":"Teichert, C., 1959, Australia and Gondwanaland: Geologische Rundschau, v. 47, no. 2, p. 562-590, https://doi.org/10.1007/BF01800675.","productDescription":"29 p.","startPage":"562","endPage":"590","numberOfPages":"29","costCenters":[],"links":[{"id":218728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Australia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 108.017578125,\n -36.52729481454623\n ],\n [\n 129.6826171875,\n -36.52729481454623\n ],\n [\n 129.6826171875,\n -10.962764256386809\n ],\n [\n 108.017578125,\n -10.962764256386809\n ],\n [\n 108.017578125,\n -36.52729481454623\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"47","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eeece4b0c8380cd4a02b","contributors":{"authors":[{"text":"Teichert, C.","contributorId":17755,"corporation":false,"usgs":false,"family":"Teichert","given":"C.","email":"","affiliations":[{"id":6773,"text":"University of Kansas","active":true,"usgs":false}],"preferred":false,"id":359619,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010752,"text":"70010752 - 1959 - Free-radical concentrations and other properties of pile-irradiated coals","interactions":[],"lastModifiedDate":"2019-12-13T07:46:55","indexId":"70010752","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Free-radical concentrations and other properties of pile-irradiated coals","docAbstract":"Five coals reacted quite differently when they were exposed to pile-irradiation. Little or no change was found in free-radical content for the three coals of lowest carbon content, whereas the two coals of highest carbon content were found to have a considerable increase in free-radical content. The infrared spectra and the apparent hardness of the irradiated coals of higher carbon content indicate that polymerization occurred. Radiation of these coals in chemical reagents may promote reactivity.","language":"English","publisher":"Science","doi":"10.1126/science.130.3391.1762","issn":"00368075","usgsCitation":"Friedel, R., and Breger, I.A., 1959, Free-radical concentrations and other properties of pile-irradiated coals: Science, v. 130, no. 3391, p. 1762-1762, https://doi.org/10.1126/science.130.3391.1762.","productDescription":"1 p.","startPage":"1762","endPage":"1762","costCenters":[],"links":[{"id":219640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"130","issue":"3391","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a13c7e4b0c8380cd54794","contributors":{"authors":[{"text":"Friedel, R.A.","contributorId":17365,"corporation":false,"usgs":true,"family":"Friedel","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":359569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breger, Irving A.","contributorId":65205,"corporation":false,"usgs":true,"family":"Breger","given":"Irving","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359570,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000333,"text":"1000333 - 1959 - Burrowing activities of the larval lamprey","interactions":[],"lastModifiedDate":"2013-02-12T08:34:07","indexId":"1000333","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"Burrowing activities of the larval lamprey","docAbstract":"Since the appearance in 1950 of Applegate's work on the sea lamprey in Michigan (U. S. Fish and Wildl. Serv., Spec. Sci. Rept.; Fish, No. 55) and the subsequent development of means to control lampreys in the Great Lakes, biologists have accumulated much additional information on adult lampreys. Larval lampreys, however, are difficult animals to observe in the field, and many facets of their behavior are still unknown. While working with the U. S. Fish and Wildlife Service, I kept ammocetes in captivity, and was able to observe their burrowing activities.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Copeia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Society of Ichthyologists and Herpetologists","publisherLocation":"Lawrence, KS","doi":"10.2307/1440405","collaboration":"Out-of-print","usgsCitation":"Sawyer, P.J., 1959, Burrowing activities of the larval lamprey: Copeia, v. 1959, no. 3, p. 256-257, https://doi.org/10.2307/1440405.","productDescription":"2 p.","startPage":"256","endPage":"257","numberOfPages":"2","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":267263,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2307/1440405"},{"id":128857,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1959","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9936","contributors":{"authors":[{"text":"Sawyer, Philip J.","contributorId":105664,"corporation":false,"usgs":true,"family":"Sawyer","given":"Philip","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308409,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000334,"text":"1000334 - 1959 - Effects of certain chemicals on mucus-producing cells of Petromyzon marinus","interactions":[],"lastModifiedDate":"2016-02-08T11:56:57","indexId":"1000334","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","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":"Effects of certain chemicals on mucus-producing cells of Petromyzon marinus","docAbstract":"Tissue samples that contained slime-secreting cells were taken from the gills and epidermis of larval lampreys that had been poisoned by several compounds. Histochemical treatment of these pathological tissues helped delineate the fate of these mucus-producing areas of the ammocetes. It was shown that the slime-secreting cells, located at the tips of the gill filaments, lining the gill chamber, and scattered throughout the epidermis reacted differently to the same toxicant. The secretory cells of the gills were, without exception, the most sensitive to chemical attack.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1959)88[305:EOCCOM]2.0.CO;2","usgsCitation":"Sawyer, P.J., 1959, Effects of certain chemicals on mucus-producing cells of Petromyzon marinus: Transactions of the American Fisheries Society, v. 88, no. 4, p. 305-309, https://doi.org/10.1577/1548-8659(1959)88[305:EOCCOM]2.0.CO;2.","productDescription":"5 p.","startPage":"305","endPage":"309","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128858,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624750","contributors":{"authors":[{"text":"Sawyer, Philip J.","contributorId":105664,"corporation":false,"usgs":true,"family":"Sawyer","given":"Philip","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308410,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000103,"text":"1000103 - 1959 - Photoreception in the opossum shrimp, Mysis relicta Loven","interactions":[],"lastModifiedDate":"2023-08-25T16:19:41.352208","indexId":"1000103","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1014,"text":"Biological Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Photoreception in the opossum shrimp, Mysis relicta Loven","docAbstract":"No abstract available.
","language":"English","publisher":"Marine Biological Laboratory","doi":"10.2307/1539205","usgsCitation":"Beeton, A.M., 1959, Photoreception in the opossum shrimp, Mysis relicta Loven: Biological Bulletin, v. 116, no. 2, p. 204-216, https://doi.org/10.2307/1539205.","productDescription":"12 p.","startPage":"204","endPage":"216","numberOfPages":"12","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128471,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"116","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685daa","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":308083,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000478,"text":"1000478 - 1959 - Life history of the sea lamprey of Cayuga Lake, New York","interactions":[],"lastModifiedDate":"2012-03-02T17:16:04","indexId":"1000478","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Life history of the sea lamprey of Cayuga Lake, New York","docAbstract":"U. S. Fish and Wildlife Service Fishery Bulletin no. 154","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fishery Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Wigley, R.L., 1959, Life history of the sea lamprey of Cayuga Lake, New York: Fishery Bulletin, v. 59, p. 561-617.","productDescription":"p. 561-617","startPage":"561","endPage":"617","numberOfPages":"56","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":130317,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a53e6","contributors":{"authors":[{"text":"Wigley, Roland L.","contributorId":11559,"corporation":false,"usgs":true,"family":"Wigley","given":"Roland","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308601,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010687,"text":"70010687 - 1959 - Magnetostriction and palæomagnetism of igneous rocks","interactions":[],"lastModifiedDate":"2015-06-22T09:54:22","indexId":"70010687","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Magnetostriction and palæomagnetism of igneous rocks","docAbstract":"IN a recent communication, Stott and Stacey1 report on a “crucial experiment” from which they conclude: “This excellent agreement between the dip and the directions of artificial thermoremanent magnetization of the stressed and unstressed rocks indicates that large systematic errors due to magnetostriction are most improbable in igneous rocks of types normally used for palæomagnetic work”. This experiment was intended to test the proposals2 and measurements3 bearing on the role of magnetostriction in rock magnetism. We present here our reasons for believing that the experiment was not crucial and that the conclusion is not justified.
","language":"English","publisher":"Nature Publishing Group","doi":"10.1038/1831318a0","issn":"00280836","usgsCitation":"Graham, J.W., Buddington, A.F., and Balsley, J.R., 1959, Magnetostriction and palæomagnetism of igneous rocks: Nature, v. 183, no. 4671, https://doi.org/10.1038/1831318a0.","startPage":"1318","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":480399,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1038/1831318a0","text":"Publisher Index Page"},{"id":219407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":204940,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/1831318a0"}],"volume":"183","issue":"4671","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4ba6e4b0c8380cd696d0","contributors":{"authors":[{"text":"Graham, John W.","contributorId":80008,"corporation":false,"usgs":true,"family":"Graham","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359429,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buddington, A. F.","contributorId":40211,"corporation":false,"usgs":true,"family":"Buddington","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":359428,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Balsley, James R.","contributorId":10010,"corporation":false,"usgs":true,"family":"Balsley","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359427,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1000389,"text":"1000389 - 1959 - Food of yellow perch, Perca flavescens (Mitchill), in Saginaw Bay, Lake Huron","interactions":[],"lastModifiedDate":"2016-02-08T11:25:01","indexId":"1000389","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","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":"Food of yellow perch, Perca flavescens (Mitchill), in Saginaw Bay, Lake Huron","docAbstract":"No abstract available.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1959)88[330:FOYPPF]2.0.CO;2","usgsCitation":"Tharratt, R.C., 1959, Food of yellow perch, Perca flavescens (Mitchill), in Saginaw Bay, Lake Huron: Transactions of the American Fisheries Society, v. 88, no. 4, p. 330-331, https://doi.org/10.1577/1548-8659(1959)88[330:FOYPPF]2.0.CO;2.","productDescription":"2 p.","startPage":"330","endPage":"331","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de508","contributors":{"authors":[{"text":"Tharratt, Robert C.","contributorId":76260,"corporation":false,"usgs":true,"family":"Tharratt","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":308493,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000148,"text":"1000148 - 1959 - Survival and retention of tags, and growth of tagged lake trout in a rearing pond","interactions":[],"lastModifiedDate":"2016-02-08T13:30:29","indexId":"1000148","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Survival and retention of tags, and growth of tagged lake trout in a rearing pond","docAbstract":"No abstract available.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1959)21[17:SAROTA]2.0.CO;2","usgsCitation":"Eschmeyer, P.H., 1959, Survival and retention of tags, and growth of tagged lake trout in a rearing pond: Progressive Fish-Culturist, v. 21, no. 1, p. 17-21, https://doi.org/10.1577/1548-8659(1959)21[17:SAROTA]2.0.CO;2.","productDescription":"5 p.","startPage":"17","endPage":"21","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faeeb","contributors":{"authors":[{"text":"Eschmeyer, Paul H.","contributorId":86719,"corporation":false,"usgs":true,"family":"Eschmeyer","given":"Paul","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308145,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3013,"text":"wsp1457 - 1959 - Ground-water conditions in the Avenal-McKittrick area, Kings and Kern Counties, California","interactions":[],"lastModifiedDate":"2023-03-13T19:07:27.707161","indexId":"wsp1457","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1457","title":"Ground-water conditions in the Avenal-McKittrick area, Kings and Kern Counties, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1457","usgsCitation":"Wood, P.R., and Davis, G.H., 1959, Ground-water conditions in the Avenal-McKittrick area, Kings and Kern Counties, California: U.S. Geological Survey Water Supply Paper 1457, Report: iv, 141 p.; 5 Plates: 35.00 x 36.25 inches, https://doi.org/10.3133/wsp1457.","productDescription":"Report: iv, 141 p.; 5 Plates: 35.00 x 36.25 inches","costCenters":[],"links":[{"id":139531,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1457/report-thumb.jpg"},{"id":29827,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1457/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29822,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1457/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29823,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1457/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29824,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1457/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29825,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1457/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29826,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1457/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414014,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24385.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","county":"Kern County, Kings County","otherGeospatial":"Avenal-McKittrick area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.25,\n 35.25\n ],\n [\n -119.375,\n 35.25\n ],\n [\n -119.375,\n 36\n ],\n [\n -120.25,\n 36\n ],\n [\n -120.25,\n 35.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d1bc","contributors":{"authors":[{"text":"Wood, Perry Rowley","contributorId":10787,"corporation":false,"usgs":true,"family":"Wood","given":"Perry","email":"","middleInitial":"Rowley","affiliations":[],"preferred":false,"id":146147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, G. H.","contributorId":40963,"corporation":false,"usgs":true,"family":"Davis","given":"G.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":146148,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2336,"text":"wsp1375 - 1959 - Ground-water resources of Riverton irrigation project area, Wyoming, with a section on chemical quality of ground water","interactions":[{"subject":{"id":51092,"text":"ofr5211 - 1952 - Geology of Big Bottom dam site, Lewis River, Washington","indexId":"ofr5211","publicationYear":"1952","noYear":false,"title":"Geology of Big Bottom dam site, Lewis River, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":2336,"text":"wsp1375 - 1959 - Ground-water resources of Riverton irrigation project area, Wyoming, with a section on chemical quality of ground water","indexId":"wsp1375","publicationYear":"1959","noYear":false,"title":"Ground-water resources of Riverton irrigation project area, Wyoming, with a section on chemical quality of ground water"},"id":1},{"subject":{"id":51158,"text":"ofr52101 - 1952 - Progress report on the geology and ground-water hydrology of the Riverton irrigation project, Wyoming, with a section on the chemical quality of the water","indexId":"ofr52101","publicationYear":"1952","noYear":false,"title":"Progress report on the geology and ground-water hydrology of the Riverton irrigation project, Wyoming, with a section on the chemical quality of the water"},"predicate":"SUPERSEDED_BY","object":{"id":2336,"text":"wsp1375 - 1959 - Ground-water resources of Riverton irrigation project area, Wyoming, with a section on chemical quality of ground water","indexId":"wsp1375","publicationYear":"1959","noYear":false,"title":"Ground-water resources of Riverton irrigation project area, Wyoming, with a section on chemical quality of ground water"},"id":2},{"subject":{"id":52965,"text":"ofr5085 - 1950 - Progress report on the geology and ground-water hydrology of the Riverton Irrigation Project, Wyoming","indexId":"ofr5085","publicationYear":"1950","noYear":false,"title":"Progress report on the geology and ground-water hydrology of the Riverton Irrigation Project, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":2336,"text":"wsp1375 - 1959 - Ground-water resources of Riverton irrigation project area, Wyoming, with a section on chemical quality of ground water","indexId":"wsp1375","publicationYear":"1959","noYear":false,"title":"Ground-water resources of Riverton irrigation project area, Wyoming, with a section on chemical quality of ground water"},"id":3}],"lastModifiedDate":"2025-01-22T22:18:11.845204","indexId":"wsp1375","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1375","title":"Ground-water resources of Riverton irrigation project area, Wyoming, with a section on chemical quality of ground water","docAbstract":"The Riverton irrigation project area is in the northwestern part of the Wind River basin in west-central Wyoming. Because the annual precipitation is only about 9 inches, agriculture, which is the principal occupation in the area, is dependent upon irrigation. Irrigation by surface-water diversion was begum is 1906; water is now supplied to 77,716 acres and irrigation has been proposed for an additional 31,344 acres.
This study of the geology and ground-water resources of the Riverton irrigation project, of adjacent irrigated land, and of nearby land proposed for irrigation was begun during the summer of 1948 and was completed in 1951. The purpose of the investigation was to evaluate the ground-water resources of the area and to study the factors that should be considered in the solution of drainage and erosional problems within the area.
The Riverton irrigation project area is characterized by flat to gently sloping stream terraces, which are flanked by a combination of badlands, pediment slopes, and broad valleys. These features were formed by long-continued erosion in an arid climate of the essentially horizontal, poorly consolidated beds of the Wind River formation. The principal streams of the area flow south-eastward. Wind River and Fivemile Creek are perennial streams and the others are intermittent. Ground-water discharge and irrigation return flow have created a major problem in erosion control along Fivemile Creek. Similar conditions might develop along Muddy and lower Cottonwood Creeks when land in their drainage basins is irrigated.
The bedrock exposed in the area ranges in age from Late Cretaceous to early Tertiary (middle Eocene). The Wind River formation of early and middle Eocene age forms the uppermost bedrock formation in the greater part of the area. Unconsolidated deposits of Quaternary age, which consist of terrace gravel, colluvium, eolian sand and silt. and alluvium, mantle the Wind River formation in much of the area.
In the irrigated parts of the project, water from domestic use is obtained chiefly from the sandstone beds of the Wind River formation although some is obtained from the alluvium underlying the bottom land and from the unconsolidated deposits underlying the lower terraces along the Wind River. Although adequate quantities if water for domestic use are available from the Wind River formation, there quantities are not considered to be large enough to warrant pumping of ground water for irrigation. Only a few wells are in the nonirrigated part of the area. When this new land is irrigated, a body of ground water will gradually form in the terrace deposits and the alluvial and colluvial-alluvial deposits. Eventually, the terrace deposits may yield adequate quantities of water for domestic and stock use, but only locally are the alluvial and colluvial-alluvial deposits likely to become suitable aquifers.
In the Riverton irrigation project area, ground water occurs under water-table conditions near the surface and under artesian conditions in certain strata at both shallow and greater depths. Irrigation is the principal source of recharge to the shallow aquifers; the water level in wells that tap these aquifers fluctuates with irrigation. The depth to water in the shallow wells ranges from less than 1 foot to about 30 feet below the land surface, depending on the season of the year and on the length of time the land has been irrigated. The water level in the wells that tap the deep confined aquifers , which receive recharge indirectly from surface sources, fluctuates only slightly because the recharge and discharge are more constant. In most places the depth to water in wells penetrating the deep confined aquifers is mush greater than that in shallow wells. but in certain low areas water from the deep aquifers flows at the surface from wells. Ground water moves from the area of recharge in the direction of the hydraulic gradient and is discharges either by evapotranspiration; by inflow into streams, drains, or lakes; by pumping or flow of wells; or by flow of springs.
Waterlogging and the associated development of saline soils are common in parts of the Riverton irrigation project and adjacent irrigated land. The waterlogging is in part the result of the infiltration of irrigation water in excess of the capacity of the aquifers to store and transmit this added recharge. The solution of the drainage problems involves the consideration of a number of factors, some of which are inadequately known in some parts of the area and require further investigation before fully effective drainage measures can be designed.
The results of an aquifer test to determine the hydrologic characteristics of the Wind River formation at Riverton indicate a transmissibility of 10,000 gallons per day per foot (10,000 gpd per ft) and a storage coefficient of 2 x 10-4. The results of the test provide a part of the necessary foundation for the solution of present and future water-supply problems at Riverton and throughout the project area.
Water from shallow aquifers in irrigated tracts in the Riverton irrigation project area generally contains large amounts of dissolved solids that were leached from the soil and rocks by infiltrating irrigation water. However, wells tapping beds that receive considerable recharge from influent canal and drain seepage yield water of relatively low mineralizatoin. Dilute water is obtained also from some shallow wells in the alluvial bottom lands and on low stream terraces that border the Wind Rover. Water from deep aquifers generally is more dilute than that from shallow aquifers. However, ground water from the deep aquifers, unmixed with irrigation water, generally has a percent sodium greater than 80.
Analyses of salt crusts on the ground surface in low areas that are affected by effluent seepage and a high water table show predominance of sodium sulfate salinity, and from determinations of the water-soluble and acid-soluble substances in several samples of soil and shale it is apparent that harmful concentrations of salts are being deposited in poorly drained area. Although most of the soul in the Midvale irrigation district is of the normal arid type, analyses of soil samples show that saline, nonsaline alkaline, and saline alkaline types also are present.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington","doi":"10.3133/wsp1375","usgsCitation":"Morris, D.A., Hackett, O.M., Vanlier, K., Moulder, E.A., and Durum, W.H., 1959, Ground-water resources of Riverton irrigation project area, Wyoming, with a section on chemical quality of ground water: U.S. Geological Survey Water Supply Paper 1375, Report: vi, 205 p.; 3 Plates: 46.86 x 30.77 inches or smaller, https://doi.org/10.3133/wsp1375.","productDescription":"Report: vi, 205 p.; 3 Plates: 46.86 x 30.77 inches or smaller","numberOfPages":"215","costCenters":[],"links":[{"id":138573,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1375/report-thumb.jpg"},{"id":422309,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24357.htm","linkFileType":{"id":5,"text":"html"}},{"id":480957,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1375/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":480958,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1375/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":278839,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1375/plate-3.pdf"},{"id":28201,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1375/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","county":"Freemont County","otherGeospatial":"Wind River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0,41.0 ], [ -111.0,45.0 ], [ -104.0,45.0 ], [ -104.0,41.0 ], [ -111.0,41.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d744","contributors":{"authors":[{"text":"Morris, Donald Arthur","contributorId":13960,"corporation":false,"usgs":true,"family":"Morris","given":"Donald","email":"","middleInitial":"Arthur","affiliations":[],"preferred":false,"id":145033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":145035,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vanlier, K.E.","contributorId":24332,"corporation":false,"usgs":true,"family":"Vanlier","given":"K.E.","affiliations":[],"preferred":false,"id":145034,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moulder, E. A.","contributorId":78719,"corporation":false,"usgs":true,"family":"Moulder","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145037,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145036,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":2712,"text":"wsp1478 - 1959 - Ground-water resources of the middle Big Wood River-Silver Creek area, Blaine County, Idaho","interactions":[],"lastModifiedDate":"2023-03-13T21:01:13.193599","indexId":"wsp1478","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1478","title":"Ground-water resources of the middle Big Wood River-Silver Creek area, Blaine County, Idaho","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1478","usgsCitation":"Smith, R.O., 1959, Ground-water resources of the middle Big Wood River-Silver Creek area, Blaine County, Idaho: U.S. Geological Survey Water Supply Paper 1478, Report: iv, 64 p.; 4 Plates: 23.50 x 23.28 inches or smaller, https://doi.org/10.3133/wsp1478.","productDescription":"Report: iv, 64 p.; 4 Plates: 23.50 x 23.28 inches or smaller","costCenters":[],"links":[{"id":414051,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24421.htm","linkFileType":{"id":5,"text":"html"}},{"id":247238,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1478/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29095,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1478/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29096,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1478/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29094,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1478/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29093,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1478/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138962,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1478/report-thumb.jpg"}],"country":"United States","state":"Idaho","county":"Blaine County","otherGeospatial":"Big Wood River-Silver Creek area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -114.409,\n 43.536\n ],\n [\n -114.409,\n 43.261\n ],\n [\n -113.967,\n 43.261\n ],\n [\n -113.967,\n 43.536\n ],\n [\n -114.409,\n 43.536\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a1aa","contributors":{"authors":[{"text":"Smith, Rex Onis","contributorId":93889,"corporation":false,"usgs":true,"family":"Smith","given":"Rex","email":"","middleInitial":"Onis","affiliations":[],"preferred":false,"id":145648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15072,"text":"ofr5987 - 1959 - Stratigraphic sections, well logs, and soil-profile sections in the southern Carson Desert near Fallon, Nevada","interactions":[],"lastModifiedDate":"2023-04-04T21:21:29.595511","indexId":"ofr5987","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"59-87","title":"Stratigraphic sections, well logs, and soil-profile sections in the southern Carson Desert near Fallon, Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5987","usgsCitation":"Morrison, R.B., 1959, Stratigraphic sections, well logs, and soil-profile sections in the southern Carson Desert near Fallon, Nevada: U.S. Geological Survey Open-File Report 59-87, Report: 294 p.; 2 Plates: 17.81 x 25.18 inches and 17.06 x 23.68 inches, https://doi.org/10.3133/ofr5987.","productDescription":"Report: 294 p.; 2 Plates: 17.81 x 25.18 inches and 17.06 x 23.68 inches","costCenters":[],"links":[{"id":148700,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1959/0087/report-thumb.jpg"},{"id":43984,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1959/0087/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43985,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1959/0087/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43986,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1959/0087/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":106304,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7962.htm","linkFileType":{"id":5,"text":"html"},"description":"7962"}],"country":"United States","state":"Nevada","city":"Fallon","otherGeospatial":"Carson Desert","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119,\n 39.75\n ],\n [\n -119,\n 39.23\n ],\n [\n -118.5,\n 39.23\n ],\n [\n -118.5,\n 39.75\n ],\n [\n -119,\n 39.75\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abaeb","contributors":{"authors":[{"text":"Morrison, Roger B.","contributorId":52570,"corporation":false,"usgs":true,"family":"Morrison","given":"Roger","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":170523,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70185500,"text":"70185500 - 1959 - Climatology and the problems of western grasslands ","interactions":[],"lastModifiedDate":"2019-03-26T13:28:11","indexId":"70185500","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Climatology and the problems of western grasslands ","docAbstract":"Sixty years after Coronado, Don Juan de Onate wrote the first reasonably good description of the High Plains. He was near the present site of Wichita, Kansas, in 1601, when he arrived a t a large rancheria, or temporary Indian camp, containing more than 5000 souls. Onate's account expressed wonderment at the great extent of the level land, a t the numerous small streams bordered with luxuriant groves of trees, and, of course, at the large number of buffalo.
We shall never see the wonderland of the blossoming prairie which he described as follows: Grazing for the horses \"had been lacking for several days, as there had been none for many leagues, for the fields there were covered with flowers of a thousand different kinds, so thick that they choked the pasture \" (1, p. 256).
We who fly from Chicago to Denver in a few hours cannot get the same view of the western grasslands as those who, with rifle or sword in hand, moved at the rate of 10 to 15 miles a day.
The tall- and short-grass prairies of the West comprise more than 700,000 square miles in the United States alone, not to mention the great prong extending northward into Canada. Such an area represents nearly a quarter of the United States. There are areas other than prairie where grass is an important natural resource. Among these should be mentioned the grass openings in woodland and along the borders of desert shrub associations in the plateau and basin-and-range provinces. So considered, the western grassed areas constitute even a larger proportion of our country.
This vast domain has problems commensurate in complexity with its geographic scope, and these are in part related to the changes which have occurred since settlement. I shall attempt to state the most important current problems as I see them, and then will discuss briefly the role of the climatologist in their solution.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Grasslands: A symposium presented at the New York meeting of the American Association for the Advancement of Science","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"A symposium presented at the New York meeting of the American Association for the Advancement of Science","conferenceDate":"December 27-30, 1956","conferenceLocation":"New York, NY","language":"English","publisher":"American Association for the Advancement of Science","usgsCitation":"Leopold, L.B., 1959, Climatology and the problems of western grasslands , in Grasslands: A symposium presented at the New York meeting of the American Association for the Advancement of Science, v. 53, New York, NY, December 27-30, 1956, p. 281-287.","productDescription":"7 p.","startPage":"281","endPage":"287","costCenters":[],"links":[{"id":338100,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d38d66e4b0236b68f98f96","contributors":{"editors":[{"text":"Sprague, Howard B.","contributorId":189708,"corporation":false,"usgs":false,"family":"Sprague","given":"Howard","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":685775,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":685774,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009820,"text":"70009820 - 1959 - New occurrences of ferroselite (FeSe2)","interactions":[],"lastModifiedDate":"2020-11-13T21:09:50.402244","indexId":"70009820","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"displayTitle":"New occurrences of ferroselite (FeSe2)","title":"New occurrences of ferroselite (FeSe2)","docAbstract":"Iron selenide from the uranium-vanadium ores of the Colorado Plateau was under investigation when ferroselite was described as a new mineral in Russia by Bur'yanova and Komkov (1955). Association of ferroselite with selenian pyrite and marcasite within discrete areas of these uranium-vanadium deposits suggests an unusual environment of formation. Its association with apparent low temperature assemblages in the United States and Bussia indicates that its minimum temperature of formation is quite low. Chemical analyses of ferroselite agree well with the theoretical formula FeSe2; material from the Virgin no. 3 mine, Montrose County, Colorado, gives the formula FeSe2.07 and that from the A.E.C. no. 8 mine, Temple Mountain, Utah, gives the formula (Fe, Co)Se2.08. The similarity of hastite and ferroselite suggests that a complete series FeSe2-CoSe2 may exist. In contrast to this, pyrite associated with ferroselite apparently will camouflage only 4 per cent (molecular) FeSe2 within its structure. Ferroselite cannot be distinguished from rammelsbergite (FeAs2) by X-ray or in polished section; therefore, the exact identification of these two minerals can be made only by specific tests for As or Se. As hastite (CoSe2) and marcasite are in the same structure group as ferroselite and rammelsbergite, identification of these minerals should include qualitative chemical determinations.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(59)90116-4","usgsCitation":"Coleman, R.G., 1959, New occurrences of ferroselite (FeSe2): Geochimica et Cosmochimica Acta, v. 16, no. 4, p. 296-301, https://doi.org/10.1016/0016-7037(59)90116-4.","productDescription":"6 p.","startPage":"296","endPage":"301","numberOfPages":"6","costCenters":[],"links":[{"id":219037,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a65f3e4b0c8380cd72cb0","contributors":{"authors":[{"text":"Coleman, R. G.","contributorId":75170,"corporation":false,"usgs":true,"family":"Coleman","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":357222,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009819,"text":"70009819 - 1959 - Data of rock analyses-VI: Bibliography and index of rock analyses in the periodical and serial literature of Scotland","interactions":[],"lastModifiedDate":"2020-11-13T21:07:47.301123","indexId":"70009819","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Data of rock analyses-VI: Bibliography and index of rock analyses in the periodical and serial literature of Scotland","docAbstract":"While Hutton fortified his convictions by constant appeals to the rocks themselves, his disciple Hall tested their truth in the laboratory. It is the boast of Scotland to have led the way in the application of chemical and physical experiment to the elucidation of geological history.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(59)90083-3","usgsCitation":"Woodland, M., 1959, Data of rock analyses-VI: Bibliography and index of rock analyses in the periodical and serial literature of Scotland: Geochimica et Cosmochimica Acta, v. 17, no. 1-2, p. 136-147, https://doi.org/10.1016/0016-7037(59)90083-3.","productDescription":"12 p.","startPage":"136","endPage":"147","numberOfPages":"12","costCenters":[],"links":[{"id":219036,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fd8de4b0c8380cd4e89a","contributors":{"authors":[{"text":"Woodland, M.V.","contributorId":35065,"corporation":false,"usgs":true,"family":"Woodland","given":"M.V.","email":"","affiliations":[],"preferred":false,"id":357221,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009821,"text":"70009821 - 1959 - Leaching of clay minerals in a limestone environment","interactions":[],"lastModifiedDate":"2020-11-13T21:11:30.187278","indexId":"70009821","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Leaching of clay minerals in a limestone environment","docAbstract":"Water saturated with CO2 at about 25°C was percolated through mixed beds of limestone or marble fragments and montmorillonite, “illite” and kaolinite in polyethylene tubes for six and fortyfive complete runs. The leachates were analysed for SiO2, A12O3 and Fe2O3, but only SiO2 was found. The minerals lost SiO2 in this order: montmorillonite > kaolinite > “illite”. The differential removal of SiO2 during the short period of these experiments suggests a mechanism for the accumulation of bauxite deposits associated with limestones.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(59)90048-1","usgsCitation":"Carroll, D., and Starkey, H., 1959, Leaching of clay minerals in a limestone environment: Geochimica et Cosmochimica Acta, v. 16, no. 1-3, p. 83-87, https://doi.org/10.1016/0016-7037(59)90048-1.","productDescription":"5 p.","startPage":"83","endPage":"87","numberOfPages":"5","costCenters":[],"links":[{"id":219038,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a45a0e4b0c8380cd6744a","contributors":{"authors":[{"text":"Carroll, D.","contributorId":84495,"corporation":false,"usgs":true,"family":"Carroll","given":"D.","email":"","affiliations":[],"preferred":false,"id":357223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Starkey, H.C.","contributorId":88728,"corporation":false,"usgs":true,"family":"Starkey","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":357224,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010776,"text":"70010776 - 1959 - Composition of monazites from pegmatites in eastern Minas Gerais, Brazil","interactions":[],"lastModifiedDate":"2020-11-13T21:20:43.492334","indexId":"70010776","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Composition of monazites from pegmatites in eastern Minas Gerais, Brazil","docAbstract":"Two zoned pegmatites in south-eastern Minas Gerais were sampled in detail for their content of monazite and xenotime and the monazite was analysed for certain of the rare-earth elements and thorium.
The ratio of xenotime to monazite increases in both pegmatites from the wall toward the quartz core. The content of the less basic rare-earth elements and of thorium in monazite rises in the same direction. These variation trends suggest that during the crystallization of these pegmatites there was a fractionation of the elements leading to a more or less steady enrichment of the less basic rare-earth elements and of thorium in the residual fluids. One mode of explaining these observed effects postulates that the rare-earth elements and thorium were present in pegmatitic fluids as co-ordination complexes rather than as simple cations.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(59)90043-2","usgsCitation":"Murata, K.J., Dutra, C.V., Costa, D., and Branco, J., 1959, Composition of monazites from pegmatites in eastern Minas Gerais, Brazil: Geochimica et Cosmochimica Acta, v. 16, no. 1-3, p. 1-14, https://doi.org/10.1016/0016-7037(59)90043-2.","productDescription":"14 p.","startPage":"1","endPage":"14","numberOfPages":"14","costCenters":[],"links":[{"id":218729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Brazil","state":"Minas Gerais","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -46.142578125,\n -22.75592068148639\n ],\n [\n -43.06640625,\n -21.53484700204879\n ],\n [\n -40.166015625,\n -17.72775860985227\n ],\n [\n -40.078125,\n -15.792253570362446\n ],\n [\n -43.9453125,\n -14.264383087562637\n ],\n [\n -45.439453125,\n -14.859850400601037\n ],\n [\n -46.142578125,\n -22.75592068148639\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"16","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f92ae4b0c8380cd4d48d","contributors":{"authors":[{"text":"Murata, K. J.","contributorId":18759,"corporation":false,"usgs":true,"family":"Murata","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dutra, C. V.","contributorId":37884,"corporation":false,"usgs":false,"family":"Dutra","given":"C.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":359621,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Costa, da","contributorId":48306,"corporation":false,"usgs":true,"family":"Costa","given":"da","email":"","affiliations":[],"preferred":false,"id":359622,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Branco, J.J.R.","contributorId":84894,"corporation":false,"usgs":true,"family":"Branco","given":"J.J.R.","email":"","affiliations":[],"preferred":false,"id":359623,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":81381,"text":"81381 - 1959 - Recommended treatment for fish parasite diseases","interactions":[],"lastModifiedDate":"2012-02-02T00:15:02","indexId":"81381","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"486","title":"Recommended treatment for fish parasite diseases","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"715/FH","usgsCitation":"Hoffman, G.L., 1959, Recommended treatment for fish parasite diseases: Fishery Leaflet 486, 4 p.","productDescription":"4 p.","startPage":"0","endPage":"4","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db64473d","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":295311,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000161,"text":"1000161 - 1959 - The goldeye, Amphiodon alosoides (Rafinesque), in the commercial fishery of the Red Lakes Minnesota","interactions":[],"lastModifiedDate":"2012-03-02T17:16:04","indexId":"1000161","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"The goldeye, Amphiodon alosoides (Rafinesque), in the commercial fishery of the Red Lakes Minnesota","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fishery Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Grosslein, M.D., and Smith, L., 1959, The goldeye, Amphiodon alosoides (Rafinesque), in the commercial fishery of the Red Lakes Minnesota: Fishery Bulletin, v. 60, no. 157, p. 33-41.","productDescription":"p. 33-41","startPage":"33","endPage":"41","numberOfPages":"8","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":130362,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"157","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d51c","contributors":{"authors":[{"text":"Grosslein, Marvin D.","contributorId":46900,"corporation":false,"usgs":true,"family":"Grosslein","given":"Marvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":308167,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Lloyd L.","contributorId":34859,"corporation":false,"usgs":true,"family":"Smith","given":"Lloyd L.","affiliations":[],"preferred":false,"id":308166,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70009818,"text":"70009818 - 1959 - Determination of uranium in zircon","interactions":[],"lastModifiedDate":"2020-11-13T20:54:43.737203","indexId":"70009818","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Determination of uranium in zircon","docAbstract":"A routine fluorimetric procedure is described for the determination of trace amounts of uranium in zircon. It employs the direct extraction of uranyl nitrate with ethyl acetate using phosphate as a retainer for zirconium. Submicrogram amounts or uranium are separated in the presence of 100,000 times the amount of zirconium. The modified procedure has been worked out using synthetic mixtures of known composition and zircon. Results of analyses have an accuracy of 97–98% of the contained uranium and a standard deviation of less than 2.5%.
","language":"English","publisher":"Elsevier","doi":"10.1016/0003-2670(59)80094-5","usgsCitation":"Cuttitta, F., and Daniels, G.J., 1959, Determination of uranium in zircon: Analytica Chimica Acta, v. 20, p. 430-434, https://doi.org/10.1016/0003-2670(59)80094-5.","productDescription":"5 p.","startPage":"430","endPage":"434","numberOfPages":"5","costCenters":[],"links":[{"id":219035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ffe6e4b0c8380cd4f471","contributors":{"authors":[{"text":"Cuttitta, F.","contributorId":33837,"corporation":false,"usgs":true,"family":"Cuttitta","given":"F.","affiliations":[],"preferred":false,"id":357219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daniels, G. J.","contributorId":95193,"corporation":false,"usgs":true,"family":"Daniels","given":"G.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":357220,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70171147,"text":"70171147 - 1959 - Life history of the sea lamprey of Cayugaf Lake, New York","interactions":[],"lastModifiedDate":"2016-05-24T09:20:38","indexId":"70171147","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1664,"text":"Fishery Bulletin of the U.S. Fish and Wildlife Service","active":true,"publicationSubtype":{"id":10}},"title":"Life history of the sea lamprey of Cayugaf Lake, New York","docAbstract":"A life history study of the sea lamprey, Petromyson marinus Linnaeus, in Cayuga Lake, N.Y., was conducted during 1950, 1951, and 1952. One of the major objectives was to obtain biological data concerning this endemic stock of sea lampreys for comparison with the newly established stocks in the Great Lakes. Sexually mature sea lampreys captured on their spawning migration in Cayuga Inlet were the basis of much of this study. Such items as meristic counts, body proportions, body color, sex ratios, lengths and weights, fecundity, rate of upstream travel, effect of dams in retarding upstream movement, nesting habits, parasites, predators, estimates of abundance, and morphological changes were based on mature upstream migrants. Sea lampreys were procured by weir and trap operations and captured by hand. Tagging and marking' programs each spring made it possible to determine movements and morphological changes of individual lampreys, in addition to estimating the number of upstream migrants. Growth of parasitic-phase sea lampreys was estimated from measurements of specimens captured in Cayuga Inlet and Cayuga Lake proper. The incubation period of lamprey eggs and the habits of ammocoetes and transforming lampreys were ascertained from specimens kept in hatchery troughs and raceways. Length-frequency and weight-frequency distributions, together with the length-weight regression, of ammocoetes from Cayuga Inlet were utilized for estimating the duration of their larval life. Lake trout, Salvelinus n. namayc\"Ush (Walbaum), from Cayuga Lake and Seneca Lake were the subject of an inquiry into the effects of sea lamprey attacks. Incidence of sea lamprey attacks on the white sucker, Catosto7llus c. commerson/: (LacepMe), was investigated. Three methods are suggested for reducing the number of sea lampreys in Cayuga Lake.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Wigley, R.L., 1959, Life history of the sea lamprey of Cayugaf Lake, New York: Fishery Bulletin of the U.S. Fish and Wildlife Service, p. 561-617.","productDescription":"17 p.","startPage":"561","endPage":"617","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321582,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":321581,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.fisherybulletin.nmfs.noaa.gov/59-1/591toc.html"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d65a6e4b07e28b66845ec","contributors":{"authors":[{"text":"Wigley, Roland L.","contributorId":11559,"corporation":false,"usgs":true,"family":"Wigley","given":"Roland","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70182492,"text":"70182492 - 1959 - Some serological, cytological and histopathological aspects of the immune response in rainbow trout (Salmo gairdneri Walbaum)","interactions":[],"lastModifiedDate":"2017-02-23T12:40:21","indexId":"70182492","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":21,"text":"Thesis"},"publicationSubtype":{"id":28,"text":"Thesis"},"title":"Some serological, cytological and histopathological aspects of the immune response in rainbow trout (Salmo gairdneri Walbaum)","docAbstract":"No abstract available
","language":"English","usgsCitation":"Klontz, G., 1959, Some serological, cytological and histopathological aspects of the immune response in rainbow trout (Salmo gairdneri Walbaum).","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":336104,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publicComments":"Master's Thesis","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58b002dfe4b01ccd54fb284b","contributors":{"authors":[{"text":"Klontz, G.W.","contributorId":113429,"corporation":false,"usgs":true,"family":"Klontz","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":671252,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}