One hundred and sixty-four F and Cl analyses of silicic welded tuffs and lavas and glass separates are presented. Comparison of the F and Cl contents of crystallized rocks with those of nonhydrated glass and hydrated glassy rocks from the same rock units shows that most of the halogens originally present were lost on crystallization. An average of about half of the F and four-fifths of the Cl originally present was lost. Analyses of hydrated natural glasses and of glassy rocks indicate that in some cases significant amounts of halogens may be removed from or added to hydrated glass through prolonged contact with ground water.
The data show that the original halogen contents of the groundmass of a silicic volcanic rock can be reliably determined only from nonhydrated glass.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0016-7037(67)80045-0","issn":"00167037","usgsCitation":"Noble, D.C., Smith, V.C., and Peck, L.C., 1967, Loss of halogens from crystallized and glassy silicic volcanic rocks: Geochimica et Cosmochimica Acta, v. 31, no. 2, p. 215-223, https://doi.org/10.1016/S0016-7037(67)80045-0.","productDescription":"9 p.","startPage":"215","endPage":"223","numberOfPages":"9","costCenters":[],"links":[{"id":219238,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a49dae4b0c8380cd68931","contributors":{"authors":[{"text":"Noble, D. C.","contributorId":60627,"corporation":false,"usgs":true,"family":"Noble","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, V. C.","contributorId":74027,"corporation":false,"usgs":true,"family":"Smith","given":"V.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359026,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peck, L. C.","contributorId":74871,"corporation":false,"usgs":true,"family":"Peck","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359027,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5220015,"text":"5220015 - 1966 - Trichinosis in Maryland raccoons","interactions":[],"lastModifiedDate":"2018-02-12T11:33:51","indexId":"5220015","displayToPublicDate":"2010-06-16T12:17:35","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1140,"text":"Bulletin of the Wildlife Disease Association","active":true,"publicationSubtype":{"id":10}},"title":"Trichinosis in Maryland raccoons","docAbstract":"During recent studies of experimental Chagas’ disease, trichinosis was found in 2 out of a total of 44 Maryland raccoons (Procyon lotor) examined histologically following necropsy. All raccoons were trapped near the towns of Beltsville or Laurel. The raccoons found to have trichinosis were trapped in the area of the Agricultural Research Center, Beltsville. Cysts containing larvae of Trichinella spiralis were found in sections of diaphragm in one raccoon and in sections of diaphragm, skeletal muscle, and ocular muscle in the other. Three to five cysts could he seen in sections of skeletal muscle or diaphragm within a single low-power (scanning lens X 40) field. There was little if any inflammatory reaction to most of these cysts, but inflammatory cells were present adjacent to an occasional cyst (Fig. 1). Foci of calcification were found in some sections of muscle and may represent old calcified cysts.
","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-2.3.81","usgsCitation":"Winslow, D., Price, D., Neafie, R., and Herman, C.M., 1966, Trichinosis in Maryland raccoons: Bulletin of the Wildlife Disease Association, v. 2, no. 3, p. 81-82, https://doi.org/10.7589/0090-3558-2.3.81.","productDescription":"2 p.","startPage":"81","endPage":"82","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","city":"Beltsville, Laurel","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.93416595458984,\n 38.997841307500714\n ],\n [\n -76.84061050415038,\n 38.997841307500714\n ],\n [\n -76.84061050415038,\n 39.06811345122598\n ],\n [\n -76.93416595458984,\n 39.06811345122598\n ],\n [\n -76.93416595458984,\n 38.997841307500714\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"2","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624687","contributors":{"authors":[{"text":"Winslow, D.J.","contributorId":26385,"corporation":false,"usgs":true,"family":"Winslow","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":331199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, D.L.","contributorId":94399,"corporation":false,"usgs":true,"family":"Price","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":331201,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Neafie, R.C.","contributorId":67607,"corporation":false,"usgs":true,"family":"Neafie","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":331200,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":331202,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":5221290,"text":"5221290 - 1966 - Acid-fast intranuclear inclusion bodies in the kidneys of mallards fed lead shot","interactions":[],"lastModifiedDate":"2023-11-08T23:12:33.650804","indexId":"5221290","displayToPublicDate":"2010-06-16T12:17:35","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1140,"text":"Bulletin of the Wildlife Disease Association","active":true,"publicationSubtype":{"id":10}},"title":"Acid-fast intranuclear inclusion bodies in the kidneys of mallards fed lead shot","docAbstract":"Acid-fast intranuclear inclusion bodies were found in the cells of the proximal convoluted tubules of the kidneys of mallards fed one, two, three or eight number 6 lead shot and maintained on cracked or whole corn and on grain-duck pellet diets. No acid-fast inclusion bodies were found in mallards fed one or three lead shot but maintained on a duck pellet ration. Dietary factors may be responsible for the failure of mallards fed a duck pellet ration to develop lead Inclusion bodies when treated with one or three lead shot. The authors suggest these inclusion bodies can be used as presumptive evidence for lead intoxication in mallards.","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-2.4.127","usgsCitation":"Locke, L.N., Bagley, G.E., and Irby, H., 1966, Acid-fast intranuclear inclusion bodies in the kidneys of mallards fed lead shot: Bulletin of the Wildlife Disease Association, v. 2, no. 4, p. 127-131, https://doi.org/10.7589/0090-3558-2.4.127.","productDescription":"5 p.","startPage":"127","endPage":"131","numberOfPages":"5","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194068,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3656","contributors":{"authors":[{"text":"Locke, L. N.","contributorId":73539,"corporation":false,"usgs":true,"family":"Locke","given":"L.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":333503,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bagley, George E.","contributorId":46589,"corporation":false,"usgs":true,"family":"Bagley","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":333502,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Irby, H.D.","contributorId":106996,"corporation":false,"usgs":true,"family":"Irby","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":333504,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":52564,"text":"ofr6737 - 1966 - Water-surface profiles of Raccoon River at Des Moines, Iowa","interactions":[],"lastModifiedDate":"2016-02-22T10:40:41","indexId":"ofr6737","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"67-37","title":"Water-surface profiles of Raccoon River at Des Moines, Iowa","docAbstract":"This investigation was undertaken as a part of the cooperative program with the Iowa Institute of Hydraulic Research, the City of Des Moines, and the U.S. Geological Survey. The purpose of this report is twofold:
\n1. To present water-surface profiles and rating curves for existing channel conditions in the 4-mile reach of Raccoon River upstream from the mouth, and
\n2. To show the effect upon water-surface profiles of raising the Fleur Drive roadway to eliminate road overflow.
\nThe Raccoon River., having a drainage area of 3,630 square miles, borders the south edge of the Des Moines downtown business district before flowing into the Des Moines River at mile 201.6. A large residential area and the city airport are separated from downtown Des Moines by the Raccoon River (fig. 1). Five highway bridges and one railroad bridge span the river between the mouth and mile 205.75, the limits of this report (fig. 1). The river is confined to a narrow channel from the mouth to the Chicago, Burlington, and Quincy Railroad bridge (mile 202.6); upstream of this bridge the river is not confined and during high water spreads over a wide flood plain. Fleur Drive, a principal traffic artery to the downtown area, is the only roadway of the five that crosses this wide flood plain. It has been flooded 15 times during the period 1903, 1918-1965.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr6737","usgsCitation":"Carpenter, P.J., and Appel, D.H., 1966, Water-surface profiles of Raccoon River at Des Moines, Iowa: U.S. Geological Survey Open-File Report 67-37, Report: 15 p.; 2 Plates: 48.06 x 36.38 inches and 32.10 x 22.10 inches, https://doi.org/10.3133/ofr6737.","productDescription":"Report: 15 p.; 2 Plates: 48.06 x 36.38 inches and 32.10 x 22.10 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":174700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr6737.jpg"},{"id":310400,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0037/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310401,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0037/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":310402,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0037/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Iowa","city":"Des Moines","otherGeospatial":"Raccoon River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.77311706542969,\n 41.52657175967685\n ],\n [\n -93.77311706542969,\n 41.671116673793016\n ],\n [\n -93.50120544433594,\n 41.671116673793016\n ],\n [\n -93.50120544433594,\n 41.52657175967685\n ],\n [\n -93.77311706542969,\n 41.52657175967685\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d4c","contributors":{"authors":[{"text":"Carpenter, Philip J.","contributorId":85034,"corporation":false,"usgs":true,"family":"Carpenter","given":"Philip","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":245555,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Appel, David H.","contributorId":45290,"corporation":false,"usgs":true,"family":"Appel","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":245554,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221300,"text":"70221300 - 1966 - Crustal study of a continental strip from the Atlantic Ocean to the Rocky Mountains","interactions":[],"lastModifiedDate":"2021-06-10T12:10:03.272124","indexId":"70221300","displayToPublicDate":"1966-12-01T08:37:06","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Crustal study of a continental strip from the Atlantic Ocean to the Rocky Mountains","docAbstract":"Twenty aeromagnetic profiles over a 100-mile-wide strip along the arc of a great circle passing through Denver, Colorado, and Washington, D. C, reveal large anomalies of major crustal significance. Contoured data disclose several areas of distinct magnetic patterns reflecting basement lithology and structure. The mafic rocks of the Blue Ridge and Piedmont and the Keweenawan mafic belt in Iowa and Nebraska give rise to strong linear trends. Areas with a more random pattern of closely spaced magnetic anomalies appear in central Ohio, eastern Iowa, and central and western Nebraska. Except in the Blue Ridge and Piedmont areas, crystalline basement rocks are covered by a thick blanket of virtually nonmagnetic sedimentary rocks, and lithology must be inferred from correlations of the magnetic data with scattered drill-hole data and regional gravity data. The area of highly magnetic rocks in central Ohio has a sharp western boundary that coincides with the western limit of metamorphism associated with the probable extension into Ohio of the Grenville province of Canada. This area and a similar one in eastern Iowa are linked by an arcuate, nearly continuous belt of positive gravity anomalies that extends north into Wisconsin and northern Michigan and then swings southeast across central Michigan. This horseshoe-shaped feature is associated with lithologically diverse but highly magnetic basement rocks. A group of linear magnetic anomalies in western Iowa and eastern Nebraska correlates with the well-known midcontinent gravity high. In Nebraska the magnetic data provide a basis for grouping the extremely complex drill-hole data into three over all lithologic terranes. An analysis of the long-wavelength (>40 miles) variations of the profiles shows that they form a number of large coherent anomalies, many of which show little relation to the major tectonic trends and lithologic patterns of the basement surface. The very broad and less numerous anomalies in the east, which have more or less north-south trends, are significantly different from the more numerous anomalies in the western part of the strip, which tend to trend east-west. One linear anomaly extends for nearly 500 miles across Nebraska and Iowa and may mark a zone of rifting. Heat-flow data show that rocks at the Curie point, which determines the depth below which rock magnetization cannot occur, may be deep enough, at least in shield and other stable parts of the continent, to include a part of the upper mantle. The concentration of the large magnetic features in Iowa and Nebraska may indicate that the thickness of magnetized rock is greater in this area and that perhaps some of these features originate in the upper mantle.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1966)77[1427:CSOACS]2.0.CO;2","usgsCitation":"Zietz, I., King, E.R., Geddes, W., and Lidiak, E., 1966, Crustal study of a continental strip from the Atlantic Ocean to the Rocky Mountains: Geological Society of America Bulletin, v. 77, no. 12, p. 1427-1447, https://doi.org/10.1130/0016-7606(1966)77[1427:CSOACS]2.0.CO;2.","productDescription":"21 p.","startPage":"1427","endPage":"1447","costCenters":[],"links":[{"id":386346,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"77","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zietz, I.","contributorId":59937,"corporation":false,"usgs":true,"family":"Zietz","given":"I.","email":"","affiliations":[],"preferred":false,"id":817271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Elizabeth R.","contributorId":40990,"corporation":false,"usgs":true,"family":"King","given":"Elizabeth","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":817272,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Geddes, Wilburt","contributorId":260105,"corporation":false,"usgs":false,"family":"Geddes","given":"Wilburt","email":"","affiliations":[],"preferred":false,"id":817273,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lidiak, E.G.","contributorId":101698,"corporation":false,"usgs":true,"family":"Lidiak","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":817274,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70221299,"text":"70221299 - 1966 - Magnetic data on the structure of the central Arctic Region","interactions":[],"lastModifiedDate":"2021-06-09T13:34:02.726064","indexId":"70221299","displayToPublicDate":"1966-12-01T08:29:47","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Magnetic data on the structure of the central Arctic Region","docAbstract":"A study of 23,000 miles of total intensity aeromagnetic profiles in the central Arctic has been made by the U. S. Geological Survey and the U. S. Coast and Geodetic Survey. The profiles were flown at 20,000 feet above sea level and cover approximately 1,350,000 square miles of the Arctic Ocean between the North Pole and the North American continent. When the profiles are smoothed to remove crustal anomalies, the resulting contoured values differ from the U. S. Hydrographic Office Chart 1703 N for 1955 corrected to 1951 by as much as 2000 gammas in the northern part of the Arctic Archipelago. A nondipole regional focus east of Greenland has decreased in amplitude but has changed very little in position since 1907.5. There is a profound difference in the magnetic characteristics of the rocks on either side of the underwater Lomonosov Ridge across the Arctic Ocean. In the Eurasian Basin the high-altitude profiles are relatively smooth or show only minor anomalies, but on the North American side of the ridge there is a large area of closely spaced, high-amplitude anomalies which has been designated the Central Magnetic Zone. Although the anomaly trends parallel the Alpha Rise, this zone is far more extensive, including nearly half of the Canadian Basin on one side and probably all the Central Arctic Basin on the other side of the rise. The Lomonosov Ridge is marked by a persistent anomaly of moderate size that indicates the presence of magnetic material in the ridge. Probable block-fault structures along the flanks of the Alpha Rise are associated with blocklike magnetic anomalies of comparable widths. A characteristic magnetic pattern occurs over an area of jagged bottom topography in the Eurasian Basin. A similar magnetic pattern over part of the Lena Trough may indicate another area of jagged topography. The belt of epicenters associated with the Mid-Atlantic Ridge continues through this rugged part of the Eurasian Basin, but the absence of the typical high magnetic anomaly makes it doubtful that the mid-oceanic ridge extends through this part of the Arctic. Magnetic data indicate that the thick sections of sedimentary rocks in the Paleozoic geosynclinal belts of northern Ellesmere Island and northern Greenland continue out under the adjacent continental shelves north of Greenland, west of the Arctic Archipelago, north of the part of Alaska east of Barrow, and under part of the Chukchi Shelf, and that they make up the bulk of the Nansen Swell off Spitsbergen. Thick sedimentary fill is indicated in the magnetically flat areas of the Eurasian Basin next to the Lomonosov Ridge and in the southern part of the Canadian Basin. The magnetic profiles on the Eurasian side of the Lomonosov Ridge closely resemble typical magnetic profiles over both Atlantic and Pacific oceans, where as the profiles of the Central Magnetic Zone on the North American side of the Lomonosov Ridge are completely unlike the oceanic data and show a striking similarity to typical profiles over the Precambrian rocks of the Canadian Shield and its buried equivalent under the Central Stable Region of the United States. Therefore, it is concluded that the Arctic region consists of a probable oceanic area on the Eurasian side and a basin formed by downdropped continental rocks, presumably a Precambrian complex similar to that of the Canadian Shield, on the North American side of the ridge.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1966)77[619:MDOTSO]2.0.CO;2","usgsCitation":"King, E.R., Zietz, I., and Alldredge, L., 1966, Magnetic data on the structure of the central Arctic Region: Geological Society of America Bulletin, v. 77, no. 6, p. 619-646, https://doi.org/10.1130/0016-7606(1966)77[619:MDOTSO]2.0.CO;2.","productDescription":"28 p.","startPage":"619","endPage":"646","costCenters":[],"links":[{"id":386345,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Arctic Circle","volume":"77","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"King, E. R.","contributorId":93482,"corporation":false,"usgs":true,"family":"King","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":817268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zietz, I.","contributorId":59937,"corporation":false,"usgs":true,"family":"Zietz","given":"I.","email":"","affiliations":[],"preferred":false,"id":817269,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alldredge, L.R.","contributorId":53457,"corporation":false,"usgs":true,"family":"Alldredge","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":817270,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5220439,"text":"5220439 - 1966 - Proportion of recovered goose and brant bands that are reported","interactions":[],"lastModifiedDate":"2025-02-07T17:16:28.262516","indexId":"5220439","displayToPublicDate":"1966-10-03T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Proportion of recovered goose and brant bands that are reported","docAbstract":"A few more than one-third of the goose and brant bands recovered by hunters were reported to the Bird Banding Laboratory (a rate of 0.361) during the 1962-64 hunting seasons. We calculated this band-reporting rate by comparing the estimated number of goose and brant bands recovered by hunters, based on a mail questionnaire survey, with the number of bands actually reported to the Bird Banding Laboratory. This band-reporting rate is probably representative only of the 1962-65 period. It is likely that, in earlier years, a greater proportion (perhaps about 0.60) of recovered goose and brant bands were reported.","language":"English","publisher":"Wiley","doi":"10.2307/3798300","usgsCitation":"Martinson, R.K., and McCann, J., 1966, Proportion of recovered goose and brant bands that are reported: Journal of Wildlife Management, v. 30, no. 4, p. 856-858, https://doi.org/10.2307/3798300.","productDescription":"3 p.","startPage":"856","endPage":"858","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193487,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649a8b","contributors":{"authors":[{"text":"Martinson, R. K.","contributorId":106983,"corporation":false,"usgs":true,"family":"Martinson","given":"R.","middleInitial":"K.","affiliations":[],"preferred":false,"id":331815,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCann, J.A.","contributorId":25499,"corporation":false,"usgs":true,"family":"McCann","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":331814,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010712,"text":"70010712 - 1966 - Airborne geophysical study in the Pensacola Mountains of Antarctica","interactions":[],"lastModifiedDate":"2026-02-10T15:49:56.691594","indexId":"70010712","displayToPublicDate":"1966-09-16T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Airborne geophysical study in the Pensacola Mountains of Antarctica","docAbstract":"A seismic reflection, gravity, and aeromagnetic reconnaissance was made in the Pensacola Mountains, Antarctica, during the 1965-66 austral summer. Prominent ice streams located between the Neptune and Patuxent Ranges and east of the Forrestal Range overlie channels in the rock surface 2000 meters below sea level which are probably of glacial origin. Seismic reflections show that the Filchner Ice Shelf is 1270 meters thick near its southern margin. Along the boundary between West and East Antarctica, Bouguer anomalies decrease from +60 milligals in West Antarctica to -80 milligals in East Antarctica. An abrupt change in crustal structure across this boundary is required to explain the 2 milligals per kilometer gradient. This may indicate a fault extending through the crust into the mantle. Aeromagnetic profiles delineate anomalies up to 1800 γ associated with the basic stratiform intrusion which comprises the Dufek and Forrestal ranges. A probable minimum area of 9500 square kilometers is calculated for the intrusive body on the basis of the magnetic anomalies, making it one of the largest bodies of its type. The extension of this magnetic anomaly across a fault forming the north border of the Pensacola Mountains probably precludes transcurrent movement.
Analyses of lead isotopes in galena in carbonate rock ore deposits collected from several mineralized districts in the Central and Eastern Interior of the United States support previous studies in establishing that the galena is anomalously radiogenic (\"J\"type\")- This study, using care-fully selected samples to test some géologie relationships, shows region-wide and distrietwide systematic variations in isotope ratios. The genetic implications of thèse variations are discussed. Two mechanisms of origin are considered to explain thèse variations in isotopic ratios. One involves mixing of leads from multiple sources, the other calls for variable lead-isotope ratios originating from a single source. Several source materials for the lead ores have been suggested; whether a single source has predominated, or two or more main sources have predominated is still unresolved. Slopes from Pb206/Pb204 versus Pb207/Pb204 plot are compatible with a contribution of lead by the 1300 ± 300 m.y. basement rocks that underlie the deposits. The spatial relationships of alkaline igneous rocks to several of the minerai districts in the Mississippi Valley région suggest a possible mag-matic source for the lead. Isotopic analyses of galenas closely associated with several of the intrusive rocks are similar in isotopic composition to adjacent ore leads, but genetic implications are ambiguous. Galena oc-curring in shales in the Mississippi Valley région outside mineralized districts contains ordinary lead. Théories that call upon such shales to be the major source of the lead in the depoaits of the Mississippi Valley type must explain this distinct différence in isotopic compositions. Galena collected from districts within the Appalachian Ridge and Valley Province contains notably less radiogenic lead than that from the Mississippi Valley minerai districts, and the lead is of the ordinary type.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.61.5.933","usgsCitation":"Heyl, A.V., Delevaux, M., Zartman, R., and Brock, M.R., 1966, Isotopic study of galenas from the upper Mississippi Valley, the Illinois-Kentucky, and some Appalachian Valley mineral districts: Economic Geology, v. 61, no. 5, p. 933-961, https://doi.org/10.2113/gsecongeo.61.5.933.","productDescription":"29 p.","startPage":"933","endPage":"961","costCenters":[],"links":[{"id":386283,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois, Kentucky","otherGeospatial":"Illinois-Kentucky border","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.0224609375,\n 37.84015683604136\n ],\n [\n -89.53857421875,\n 37.64903402157866\n ],\n [\n -89.36279296875,\n 37.09023980307208\n ],\n [\n -89.67041015625,\n 36.50963615733049\n ],\n [\n -87.4072265625,\n 36.686041276581925\n ],\n [\n -88.0224609375,\n 37.84015683604136\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"61","issue":"5","noUsgsAuthors":false,"publicationDate":"1966-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Heyl, A. V.","contributorId":70032,"corporation":false,"usgs":true,"family":"Heyl","given":"A.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":817146,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Delevaux, M.H.","contributorId":27853,"corporation":false,"usgs":true,"family":"Delevaux","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":817147,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zartman, R. E.","contributorId":15632,"corporation":false,"usgs":true,"family":"Zartman","given":"R. E.","affiliations":[],"preferred":false,"id":817148,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brock, M. R.","contributorId":96230,"corporation":false,"usgs":true,"family":"Brock","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":817149,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70221248,"text":"70221248 - 1966 - Digital computer methods for water‐quality data","interactions":[],"lastModifiedDate":"2021-06-08T15:28:33.090973","indexId":"70221248","displayToPublicDate":"1966-07-01T10:23:39","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Digital computer methods for water‐quality data","docAbstract":"The digital computer is used on a routine basis in the ground-water program in Kansas for tasks ranging from the listing of water-quality data in tabular and publishable form to statistically and graphically analyzing a mass of data.
In the past year a number of computer programs in FORTRAN IV have been developed by Charles O. Morgan and Jesse M. McNellis using an IBM-7040 computer to store, retrieve, and manipulate water-quality data. These programs:
(1) Tabulate data at the rate of 40 chemical analyses of water per minute in a format similar to that found in the Kansas ground-water publications.
(2) Perform necessary calculations and print Stiff diagrams at the rate of 30 per minute.
(3) Perform necessary calculations and print Piper diagrams, including a square modification of the normally diamond-shaped cation-anion diagram, and trilinear diagrams of the cations and anions. The symbol representing the analyses located on the diagrams can be designated by either an analysis number or a geologic unit number. A cation-anion diagram showing the average chemical composition of water for an aquifer can also be printed. These diagrams for 50 analyses can be produced in 1.5 minutes.
(4) Plot maps of 42 individual, combined, or calculated parameters obtained from the data cards. These maps can be plotted to any specified scale and for as many as 10 designated geologic units. Computer time involved for one map with 50 plotted points is 15 seconds.
It is estimated that the use of these programs will save several man-months during a ground-water study, and the error inherent in the manual manipulation of data is greatly reduced. The present cost for running 50 analyses through the four water-quality programs on the computer is approximately $20.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1966.tb01605.x","usgsCitation":"Morgan, C., Dingman, R., and McNellis, J., 1966, Digital computer methods for water‐quality data: Groundwater, v. 4, no. 3, p. 35-42, https://doi.org/10.1111/j.1745-6584.1966.tb01605.x.","productDescription":"8 p.","startPage":"35","endPage":"42","costCenters":[],"links":[{"id":386295,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Morgan, C.O.","contributorId":24482,"corporation":false,"usgs":true,"family":"Morgan","given":"C.O.","email":"","affiliations":[],"preferred":false,"id":817165,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dingman, R.J.","contributorId":40645,"corporation":false,"usgs":true,"family":"Dingman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":817166,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McNellis, J.M.","contributorId":58662,"corporation":false,"usgs":true,"family":"McNellis","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":817167,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5220442,"text":"5220442 - 1966 - Proportion of recovered duck bands that are reported","interactions":[],"lastModifiedDate":"2025-02-12T15:25:10.156198","indexId":"5220442","displayToPublicDate":"1966-04-04T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Proportion of recovered duck bands that are reported","docAbstract":"Band-reporting rates (the proportion of duck bands recovered by hunters that are actually reported to the Bird Banding Laboratory) appear to have decreased between the late 1950's and early 1960's. About one-half the banded ducks bagged during the 1958-59 and 1959-60 hunting seasons were reported-a rate similar to those recorded in other studies conducted during the early and mid-1950's. Band-reporting rates were lower for the 1962-63 and 1962-64 hunting seasons; less than one-third of the banded ducks bagged were reported. This decrease in band-reporting rates was concurrent with significant changes in duck hunting regulations, the volume of duck banding, and the method used to relay information to the person who reports a band. Band-reporting rates differed for various species of ducks. In general, band-reporting rates were high on canvasbacks (Aythya valisineria), redheads (A. americana), and pintails (Anas acuta) and low for teals (Anas discors and A. carolinensis).
","language":"English","publisher":"Wiley","doi":"10.2307/3797812","usgsCitation":"Martinson, R.K., 1966, Proportion of recovered duck bands that are reported: Journal of Wildlife Management, v. 30, no. 2, p. 264-268, https://doi.org/10.2307/3797812.","productDescription":"5 p.","startPage":"264","endPage":"268","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198154,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"contiguous United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"geometry\": {\n \"type\": \"MultiPolygon\",\n \"coordinates\": [\n [\n [\n [\n -94.81758,\n 49.38905\n ],\n [\n -94.64,\n 48.84\n ],\n [\n -94.32914,\n 48.67074\n ],\n [\n -93.63087,\n 48.60926\n ],\n [\n -92.61,\n 48.45\n ],\n [\n -91.64,\n 48.14\n ],\n [\n -90.83,\n 48.27\n ],\n [\n -89.6,\n 48.01\n ],\n [\n -89.27292,\n 48.01981\n ],\n [\n -88.37811,\n 48.30292\n ],\n [\n -87.43979,\n 47.94\n ],\n [\n -86.46199,\n 47.55334\n ],\n [\n -85.65236,\n 47.22022\n ],\n [\n -84.87608,\n 46.90008\n ],\n [\n -84.77924,\n 46.6371\n ],\n [\n -84.54375,\n 46.53868\n ],\n [\n -84.6049,\n 46.4396\n ],\n [\n -84.3367,\n 46.40877\n ],\n [\n -84.14212,\n 46.51223\n ],\n [\n -84.09185,\n 46.27542\n ],\n [\n -83.89077,\n 46.11693\n ],\n [\n -83.61613,\n 46.11693\n ],\n [\n -83.46955,\n 45.99469\n ],\n [\n -83.59285,\n 45.81689\n ],\n [\n -82.55092,\n 45.34752\n ],\n [\n -82.33776,\n 44.44\n ],\n [\n -82.13764,\n 43.57109\n ],\n [\n -82.43,\n 42.98\n ],\n [\n -82.9,\n 42.43\n ],\n [\n -83.12,\n 42.08\n ],\n [\n -83.142,\n 41.97568\n ],\n [\n -83.02981,\n 41.8328\n ],\n [\n -82.69009,\n 41.67511\n ],\n [\n -82.43928,\n 41.67511\n ],\n [\n -81.27775,\n 42.20903\n ],\n [\n -80.24745,\n 42.3662\n ],\n [\n -78.93936,\n 42.86361\n ],\n [\n -78.92,\n 42.965\n ],\n [\n -79.01,\n 43.27\n ],\n [\n -79.17167,\n 43.46634\n ],\n [\n -78.72028,\n 43.62509\n ],\n [\n -77.73789,\n 43.62906\n ],\n [\n -76.82003,\n 43.62878\n ],\n [\n -76.5,\n 44.01846\n ],\n [\n -76.375,\n 44.09631\n ],\n [\n -75.31821,\n 44.81645\n ],\n [\n -74.867,\n 45.00048\n ],\n [\n -73.34783,\n 45.00738\n ],\n [\n -71.50506,\n 45.0082\n ],\n [\n -71.405,\n 45.255\n ],\n [\n -71.08482,\n 45.30524\n ],\n [\n -70.66,\n 45.46\n ],\n [\n -70.305,\n 45.915\n ],\n [\n -69.99997,\n 46.69307\n ],\n [\n -69.23722,\n 47.44778\n ],\n [\n -68.905,\n 47.185\n ],\n [\n -68.23444,\n 47.35486\n ],\n [\n -67.79046,\n 47.06636\n ],\n [\n -67.79134,\n 45.70281\n ],\n [\n -67.13741,\n 45.13753\n ],\n [\n -66.96466,\n 44.8097\n ],\n [\n -68.03252,\n 44.3252\n ],\n [\n -69.06,\n 43.98\n ],\n [\n -70.11617,\n 43.68405\n ],\n [\n -70.64548,\n 43.09024\n ],\n [\n -70.81489,\n 42.8653\n ],\n [\n -70.825,\n 42.335\n ],\n [\n -70.495,\n 41.805\n ],\n [\n -70.08,\n 41.78\n ],\n [\n -70.185,\n 42.145\n ],\n [\n -69.88497,\n 41.92283\n ],\n [\n -69.96503,\n 41.63717\n ],\n [\n -70.64,\n 41.475\n ],\n [\n -71.12039,\n 41.49445\n ],\n [\n -71.86,\n 41.32\n ],\n [\n -72.295,\n 41.27\n ],\n [\n -72.87643,\n 41.22065\n ],\n [\n -73.71,\n 40.9311\n ],\n [\n -72.24126,\n 41.11948\n ],\n [\n -71.945,\n 40.93\n ],\n [\n -73.345,\n 40.63\n ],\n [\n -73.982,\n 40.628\n ],\n [\n -73.95232,\n 40.75075\n ],\n [\n -74.25671,\n 40.47351\n ],\n [\n -73.96244,\n 40.42763\n ],\n [\n -74.17838,\n 39.70926\n ],\n [\n -74.90604,\n 38.93954\n ],\n [\n -74.98041,\n 39.1964\n ],\n [\n -75.20002,\n 39.24845\n ],\n [\n -75.52805,\n 39.4985\n ],\n [\n -75.32,\n 38.96\n ],\n [\n -75.07183,\n 38.78203\n ],\n [\n -75.05673,\n 38.40412\n ],\n [\n -75.37747,\n 38.01551\n ],\n [\n -75.94023,\n 37.21689\n ],\n [\n -76.03127,\n 37.2566\n ],\n [\n -75.72205,\n 37.93705\n ],\n [\n -76.23287,\n 38.31921\n ],\n [\n -76.35,\n 39.15\n ],\n [\n -76.54272,\n 38.71762\n ],\n [\n -76.32933,\n 38.08326\n ],\n [\n -76.99,\n 38.23999\n ],\n [\n -76.30162,\n 37.91794\n ],\n [\n -76.25874,\n 36.9664\n ],\n [\n -75.9718,\n 36.89726\n ],\n [\n -75.86804,\n 36.55125\n ],\n [\n -75.72749,\n 35.55074\n ],\n [\n -76.36318,\n 34.80854\n ],\n [\n -77.39763,\n 34.51201\n ],\n [\n -78.05496,\n 33.92547\n ],\n [\n -78.55435,\n 33.86133\n ],\n [\n -79.06067,\n 33.49395\n ],\n [\n -79.20357,\n 33.15839\n ],\n [\n -80.30132,\n 32.50935\n ],\n [\n -80.86498,\n 32.0333\n ],\n [\n -81.33629,\n 31.44049\n ],\n [\n -81.49042,\n 30.72999\n ],\n [\n -81.31371,\n 30.03552\n ],\n [\n -80.98,\n 29.18\n ],\n [\n -80.53558,\n 28.47213\n ],\n [\n -80.53,\n 28.04\n ],\n [\n -80.05654,\n 26.88\n ],\n [\n -80.08801,\n 26.20576\n ],\n [\n -80.13156,\n 25.81677\n ],\n [\n -80.38103,\n 25.20616\n ],\n [\n -80.68,\n 25.08\n ],\n [\n -81.17213,\n 25.20126\n ],\n [\n -81.33,\n 25.64\n ],\n [\n -81.71,\n 25.87\n ],\n [\n -82.24,\n 26.73\n ],\n [\n -82.70515,\n 27.49504\n ],\n [\n -82.85526,\n 27.88624\n ],\n [\n -82.65,\n 28.55\n ],\n [\n -82.93,\n 29.1\n ],\n [\n -83.70959,\n 29.93656\n ],\n [\n -84.1,\n 30.09\n ],\n [\n -85.10882,\n 29.63615\n ],\n [\n -85.28784,\n 29.68612\n ],\n [\n -85.7731,\n 30.15261\n ],\n [\n -86.4,\n 30.4\n ],\n [\n -87.53036,\n 30.27433\n ],\n [\n -88.41782,\n 30.3849\n ],\n [\n -89.18049,\n 30.31598\n ],\n [\n -89.59383,\n 30.15999\n ],\n [\n -89.41373,\n 29.89419\n ],\n [\n -89.43,\n 29.48864\n ],\n [\n -89.21767,\n 29.29108\n ],\n [\n -89.40823,\n 29.15961\n ],\n [\n -89.77928,\n 29.30714\n ],\n [\n -90.15463,\n 29.11743\n ],\n [\n -90.88022,\n 29.14854\n ],\n [\n -91.62678,\n 29.677\n ],\n [\n -92.49906,\n 29.5523\n ],\n [\n -93.22637,\n 29.78375\n ],\n [\n -93.84842,\n 29.71363\n ],\n [\n -94.69,\n 29.48\n ],\n [\n -95.60026,\n 28.73863\n ],\n [\n -96.59404,\n 28.30748\n ],\n [\n -97.14,\n 27.83\n ],\n [\n -97.37,\n 27.38\n ],\n [\n -97.38,\n 26.69\n ],\n [\n -97.33,\n 26.21\n ],\n [\n -97.14,\n 25.87\n ],\n [\n -97.53,\n 25.84\n ],\n [\n -98.24,\n 26.06\n ],\n [\n -99.02,\n 26.37\n ],\n [\n -99.3,\n 26.84\n ],\n [\n -99.52,\n 27.54\n ],\n [\n -100.11,\n 28.11\n ],\n [\n -100.45584,\n 28.69612\n ],\n [\n -100.9576,\n 29.38071\n ],\n [\n -101.6624,\n 29.7793\n ],\n [\n -102.48,\n 29.76\n ],\n [\n -103.11,\n 28.97\n ],\n [\n -103.94,\n 29.27\n ],\n [\n -104.45697,\n 29.57196\n ],\n [\n -104.70575,\n 30.12173\n ],\n [\n -105.03737,\n 30.64402\n ],\n [\n -105.63159,\n 31.08383\n ],\n [\n -106.1429,\n 31.39995\n ],\n [\n -106.50759,\n 31.75452\n ],\n [\n -108.24,\n 31.75485\n ],\n [\n -108.24194,\n 31.34222\n ],\n [\n -109.035,\n 31.34194\n ],\n [\n -111.02361,\n 31.33472\n ],\n [\n -113.30498,\n 32.03914\n ],\n [\n -114.815,\n 32.52528\n ],\n [\n -114.72139,\n 32.72083\n ],\n [\n -115.99135,\n 32.61239\n ],\n [\n -117.12776,\n 32.53534\n ],\n [\n -117.29594,\n 33.04622\n ],\n [\n -117.944,\n 33.62124\n ],\n [\n -118.4106,\n 33.74091\n ],\n [\n -118.51989,\n 34.02778\n ],\n [\n -119.081,\n 34.078\n ],\n [\n -119.43884,\n 34.34848\n ],\n [\n -120.36778,\n 34.44711\n ],\n [\n -120.62286,\n 34.60855\n ],\n [\n -120.74433,\n 35.15686\n ],\n [\n -121.71457,\n 36.16153\n ],\n [\n -122.54747,\n 37.55176\n ],\n [\n -122.51201,\n 37.78339\n ],\n [\n -122.95319,\n 38.11371\n ],\n [\n -123.7272,\n 38.95166\n ],\n [\n -123.86517,\n 39.76699\n ],\n [\n -124.39807,\n 40.3132\n ],\n [\n -124.17886,\n 41.14202\n ],\n [\n -124.2137,\n 41.99964\n ],\n [\n -124.53284,\n 42.76599\n ],\n [\n -124.14214,\n 43.70838\n ],\n [\n -124.02053,\n 44.6159\n ],\n [\n -123.89893,\n 45.52341\n ],\n [\n -124.07963,\n 46.86475\n ],\n [\n -124.39567,\n 47.72017\n ],\n [\n -124.68721,\n 48.18443\n ],\n [\n -124.5661,\n 48.37971\n ],\n [\n -123.12,\n 48.04\n ],\n [\n -122.58736,\n 47.096\n ],\n [\n -122.34,\n 47.36\n ],\n [\n -122.5,\n 48.18\n ],\n [\n -122.84,\n 49\n ],\n [\n -120,\n 49\n ],\n [\n -117.03121,\n 49\n ],\n [\n -116.04818,\n 49\n ],\n [\n -113,\n 49\n ],\n [\n -110.05,\n 49\n ],\n [\n -107.05,\n 49\n ],\n [\n -104.04826,\n 48.99986\n ],\n [\n -100.65,\n 49\n ],\n [\n -97.22872,\n 49.0007\n ],\n [\n -95.15907,\n 49\n ],\n [\n -95.15609,\n 49.38425\n ],\n [\n -94.81758,\n 49.38905\n ]\n ]\n ]\n ]\n },\n \"properties\": {\n \"name\": \"United States\"\n }\n }\n ]\n}","volume":"30","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d7f7","contributors":{"authors":[{"text":"Martinson, R. K.","contributorId":106983,"corporation":false,"usgs":true,"family":"Martinson","given":"R.","middleInitial":"K.","affiliations":[],"preferred":false,"id":331820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221246,"text":"70221246 - 1966 - Packer testing in water wells near Sarasota, Florida","interactions":[],"lastModifiedDate":"2021-06-08T15:03:04.793505","indexId":"70221246","displayToPublicDate":"1966-04-01T09:58:04","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Packer testing in water wells near Sarasota, Florida","docAbstract":"During February and March 1964, the U. S. Geological Survey ran caliper, conductance, and temperature logs on several wells in the Sarasota area. The Florida Geological Survey had previously run gamma ray and electric logs on the same wells. Two flowing wells were selected for packer testing. The two wells are about the same depth, penetrate essentially the same geologic horizons, and are about 16 miles apart. The packers were set in the wells between the producing horizons of the formations penetrated and each of the horizons was tested for head, amount of production, and quality of water. One of the tests produced excellent results, indicating that the various producing zones were effectively isolated by the packers and that different quality of water, quantity of water, and a different head was available from each zone. The other test did not show sharp differences but did indicate the extent of contamination of the producing horizons in a flowing well which had been capped for approximately two years. These tests indicate that packer testing can measurably add to knowledge of the separation of permeable zones.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1966.tb01595.x","usgsCitation":"Sutcliffe, H., and Joyner, B., 1966, Packer testing in water wells near Sarasota, Florida: Groundwater, v. 4, no. 2, p. 23-27, https://doi.org/10.1111/j.1745-6584.1966.tb01595.x.","productDescription":"5 p.","startPage":"23","endPage":"27","costCenters":[],"links":[{"id":386293,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","city":"Sarasota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.5732421875,\n 27.186242185608737\n ],\n [\n -82.408447265625,\n 27.186242185608737\n ],\n [\n -82.408447265625,\n 27.410785702577023\n ],\n [\n -82.5732421875,\n 27.410785702577023\n ],\n [\n -82.5732421875,\n 27.186242185608737\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Sutcliffe, Horace Jr.","contributorId":96725,"corporation":false,"usgs":true,"family":"Sutcliffe","given":"Horace","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":817162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Joyner, B.F.","contributorId":55899,"corporation":false,"usgs":true,"family":"Joyner","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":817163,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221267,"text":"70221267 - 1966 - The design and use of hydrogeologic maps","interactions":[],"lastModifiedDate":"2021-06-08T18:47:01.175646","indexId":"70221267","displayToPublicDate":"1966-01-01T13:44:15","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"The design and use of hydrogeologic maps","docAbstract":"A map should treat the critical problems in a way understandable to the intended reader. Some maps appropriately show only one or two pertinent hydrogeologic parameters. Point‐data maps make little or no interpretation of the data. Four‐dimensional maps‐those that include an elapsed span of time or projection of hydrogeologic variables into the future‐represent a high degree of interpretation of data; they are most useful to the map reader. The hydro‐geologist has an obligation to his reader to design maps that are as useful as possible.
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1966.tb01589.x","usgsCitation":"Warman, J., and Wiesnet, D., 1966, The design and use of hydrogeologic maps: Groundwater, v. 4, no. 1, p. 25-26, https://doi.org/10.1111/j.1745-6584.1966.tb01589.x.","productDescription":"2 p.","startPage":"25","endPage":"26","costCenters":[],"links":[{"id":386314,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Warman, J.C.","contributorId":92587,"corporation":false,"usgs":true,"family":"Warman","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":817193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiesnet, D.R.","contributorId":14057,"corporation":false,"usgs":true,"family":"Wiesnet","given":"D.R.","affiliations":[],"preferred":false,"id":817194,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5221296,"text":"5221296 - 1965 - Care of captive woodcocks","interactions":[],"lastModifiedDate":"2017-04-19T14:37:22","indexId":"5221296","displayToPublicDate":"2010-06-16T12:17:34","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Care of captive woodcocks","docAbstract":"Numbers of American woodcocks (Philohela minor) were held in cages for experimental work lasting several months. Injuries caused by birds attempting to flush were greatly reduced by clipping feathers from one wing, by making cage walls opaque, and by using high cages or false ceilings of fabric. Size of cage was found not to be important, to judge from weight changes, so long as ample food was unmistakably available. Birds were kept in both large and small cages without social conflicts. Cages on the ground proved too unsanitary for long-term use; small steel cages with removable floors were practical but did not solve the sanitation problem. Living earthworms (Lumbricus terrestris) were provided daily in amounts roughly equal to weights of birds. Birds gained on this food when worms were offered in suitable ways. The feeding tray recommended is a large roasting pan with a snap-on metal rim that retards loss of worms. Trays contained moist peat in which birds probed for worms. Two efforts to keep woodcocks on a diet of red worms (Eisenia foetide) were unsuccessful; use of this worm was considered responsible. Woodcocks were handled and transported for short periods with least injury to them when they were rolled individually in soft bags.
","language":"English","publisher":"Wiley","doi":"10.2307/3798645","usgsCitation":"Stickel, W.H., Sheldon, W.G., and Stickel, L.F., 1965, Care of captive woodcocks: Journal of Wildlife Management, v. 29, no. 1, p. 161-172, https://doi.org/10.2307/3798645.","productDescription":"12 p.","startPage":"161","endPage":"172","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487041,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3798645","text":"Publisher Index Page"},{"id":194005,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5efdef","contributors":{"authors":[{"text":"Stickel, William H.","contributorId":178252,"corporation":false,"usgs":false,"family":"Stickel","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":333514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sheldon, William G.","contributorId":35411,"corporation":false,"usgs":true,"family":"Sheldon","given":"William","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":333515,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stickel, Lucille F.","contributorId":76598,"corporation":false,"usgs":true,"family":"Stickel","given":"Lucille","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":333516,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5220413,"text":"5220413 - 1965 - The roosting behavior of the red-winged blackbird in the southern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:14:38","indexId":"5220413","displayToPublicDate":"2010-06-16T12:17:34","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"The roosting behavior of the red-winged blackbird in the southern United States","docAbstract":"This report concerns the roosting behavior of the Red-winged blackbird and associated species ; and is based on observations made over a 14-year period mainly in the Southern United States....Th e greatest concentrations of Red-winged Blackbirds in the southern states occur in the Coastal Plain Province in or near major grain growing regions.....Roosts are formed during every month of the year. The largest roosts are usually found in winter; the smallest during the breeding season. Composition of roosts may vary from place to place and from season to season.....The general locality in which roosts are found is probably influenced by food supply. The precise location is determined by the character of the habitat. Wetland situations are preferred by Red-winged Blackbirds. Most of the roosts in the Coastal Plain Province are located in marshes and swamps. Rice fields are important in the southern rice producing area. Coniferous stands and bamboo are frequently used in the Piedmont Province.....Blackbirds move out of roosts each morning at about dawn or shortly after, and return in the evening usually before sunset. Some birds may travel 35 miles or more from the starting point in the course of a day?s feeding activity. On cloudy days blackbirds move into the roost earlier than on sunny days. At a Maryland roost subadult male Redwinged Blackbirds were the first to arrive at the roost. Females and then juveniles followed. Adult males were sporadic in their time of arrival. Stratification in a roost flight was observed where birds were flying downstream to a river marsh roost. Bobolinks flew at the greatest elevations; next in order of height were Starlings, Common Grackles, Brown-headed Cowbirds, and Red-winged Blackbirds. The exodus of a large roosting population is usually of shorter duration that the movement into the roost..... In virtually all roosts some segments of the population are segregated. Stratification by species and by sexes of some species has been noted in roosts. Blackbirds may roost on partly submerged vegetation in a marsh, on the ground in grassy fields, in branches of trees, or in various other sites. In deciduous thickets with high bird densities they may roost at elevations of 1 foot to 30 feet or more. In one Arkansas roost Red-winged Blackbirds were roosting along branches at an average of about three birds per foot.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wilson Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Meanley, B., 1965, The roosting behavior of the red-winged blackbird in the southern United States: The Wilson Bulletin, v. 77, no. 3, p. 217-228.","productDescription":"217-228","startPage":"217","endPage":"228","numberOfPages":"12","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":15776,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://elibrary.unm.edu/sora/Wilson/v077n03/p0217-p0228.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"77","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640d8e","contributors":{"authors":[{"text":"Meanley, B.","contributorId":43867,"corporation":false,"usgs":true,"family":"Meanley","given":"B.","email":"","affiliations":[],"preferred":false,"id":331783,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6042,"text":"pp478 - 1965 - Geology of the Coeur d'Alene district, Shoshone County, Idaho","interactions":[{"subject":{"id":12748,"text":"ofr5426 - 1954 - Geologic map of the Wallace and vicinity quadrangle, Shoshone County, Idaho","indexId":"ofr5426","publicationYear":"1954","noYear":false,"title":"Geologic map of the Wallace and vicinity quadrangle, Shoshone County, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":6042,"text":"pp478 - 1965 - Geology of the Coeur d'Alene district, Shoshone County, Idaho","indexId":"pp478","publicationYear":"1965","noYear":false,"title":"Geology of the Coeur d'Alene district, Shoshone County, Idaho"},"id":1},{"subject":{"id":46653,"text":"ofr5329 - 1953 - Geologic map of the Smelterville and vicinity quadrangle, Idaho","indexId":"ofr5329","publicationYear":"1953","noYear":false,"title":"Geologic map of the Smelterville and vicinity quadrangle, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":6042,"text":"pp478 - 1965 - Geology of the Coeur d'Alene district, Shoshone County, Idaho","indexId":"pp478","publicationYear":"1965","noYear":false,"title":"Geology of the Coeur d'Alene district, Shoshone County, Idaho"},"id":2},{"subject":{"id":47270,"text":"ofr52162 - 1952 - Geologic map of the Pottsville quadrangle, northern Idaho","indexId":"ofr52162","publicationYear":"1952","noYear":false,"title":"Geologic map of the Pottsville quadrangle, northern Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":6042,"text":"pp478 - 1965 - Geology of the Coeur d'Alene district, Shoshone County, Idaho","indexId":"pp478","publicationYear":"1965","noYear":false,"title":"Geology of the Coeur d'Alene district, Shoshone County, Idaho"},"id":3},{"subject":{"id":51221,"text":"ofr5330 - 1953 - Geologic map of the Kellogg and vicinity quadrangle, Shoshone County, Idaho","indexId":"ofr5330","publicationYear":"1953","noYear":false,"title":"Geologic map of the Kellogg and vicinity quadrangle, Shoshone County, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":6042,"text":"pp478 - 1965 - Geology of the Coeur d'Alene district, Shoshone County, Idaho","indexId":"pp478","publicationYear":"1965","noYear":false,"title":"Geology of the Coeur d'Alene district, Shoshone County, Idaho"},"id":4}],"lastModifiedDate":"2025-09-22T18:29:49.053294","indexId":"pp478","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"478","title":"Geology of the Coeur d'Alene district, Shoshone County, Idaho","docAbstract":"The Coeur d'Alene district, near the base of the northern panhandle of Idaho, is one of the world's larger lead- zinc and silver-producing areas. The greater part of the dis~rict i~ included within five map areas, from east to west the Pottsville, Mullan, Wallace, Kellogg, and Smelterville, which were geologically mapped during this study. These quadrangles encompass an area about 26 miles long in an east-west direction and about 9 miles wide. The district lies wholly within the Coeur d'Alene Mountains, the part of the Bitterroot Range that is drained by the Coeur d'Alene River. The Bitterroot Range is a rugged, deeply dissected mountain mass which extends on both sides of the Idaho-Montana boundary for more than 200 miles and is a part of the Northern Rocky Mountains; within the district the range has a relief of 3,000-4,000 feet. The westward-flowing South Fork of the Coeur d'Alene River bisects the district, and roads along this river and its major tributaries generally provide easy access to the communities and many mines.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp478","usgsCitation":"Hobbs, S., Griggs, A., Wallace, R.E., and Campbell, A., 1965, Geology of the Coeur d'Alene district, Shoshone County, Idaho: U.S. Geological Survey Professional Paper 478, Report: v, 139 p.; 10 Plates: 45.04 x 36.56 inches or smaller, https://doi.org/10.3133/pp478.","productDescription":"Report: v, 139 p.; 10 Plates: 45.04 x 36.56 inches or smaller","numberOfPages":"145","costCenters":[],"links":[{"id":112695,"rank":12,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0478/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":495859,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4483.htm","linkFileType":{"id":5,"text":"html"}},{"id":140260,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0478/report-thumb.jpg"},{"id":330374,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0478/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330373,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0478/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330372,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0478/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330371,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0478/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330370,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0478/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330369,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0478/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330368,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0478/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330367,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0478/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330366,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0478/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330365,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0478/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Shoshone County","otherGeospatial":"Coeur d'Alene District","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-116.324,47.889],[-116.322,48.0176],[-116.32,48.0204],[-116.311,48.032],[-116.301,48.0363],[-116.296,48.0391],[-116.293,48.0433],[-116.288,48.0489],[-116.284,48.0517],[-116.277,48.0555],[-116.262,48.0631],[-116.241,48.0679],[-116.233,48.068],[-116.226,48.0649],[-116.216,48.0586],[-116.205,48.0486],[-116.198,48.0408],[-116.185,48.0368],[-116.178,48.0337],[-116.162,48.0251],[-116.147,48.0262],[-116.135,48.0259],[-116.127,48.032],[-116.119,48.0316],[-116.107,48.0281],[-116.103,48.0221],[-116.1,48.0162],[-116.074,47.9939],[-116.064,47.9889],[-116.056,47.978],[-116.052,47.9748],[-116.047,47.973],[-116.045,47.9714],[-116.043,47.9705],[-116.041,47.9696],[-116.033,47.9673],[-116.027,47.9668],[-116.022,47.965],[-116.022,47.9645],[-116.021,47.9639],[-116.017,47.96],[-116.011,47.9536],[-116.008,47.9487],[-116.008,47.9476],[-116.001,47.9375],[-116,47.9362],[-115.995,47.9275],[-115.991,47.9245],[-115.984,47.9182],[-115.982,47.9168],[-115.981,47.9163],[-115.977,47.9148],[-115.976,47.9143],[-115.966,47.9078],[-115.965,47.9072],[-115.964,47.9045],[-115.961,47.8969],[-115.957,47.8936],[-115.949,47.8882],[-115.942,47.8837],[-115.937,47.8782],[-115.926,47.8657],[-115.919,47.8587],[-115.914,47.8533],[-115.909,47.851],[-115.908,47.8498],[-115.904,47.8475],[-115.903,47.8468],[-115.902,47.845],[-115.9,47.8425],[-115.898,47.8427],[-115.896,47.8434],[-115.894,47.8443],[-115.89,47.8464],[-115.889,47.8468],[-115.883,47.8474],[-115.879,47.8449],[-115.878,47.8428],[-115.876,47.8402],[-115.874,47.8362],[-115.868,47.8333],[-115.85,47.8209],[-115.848,47.8154],[-115.848,47.8148],[-115.848,47.8108],[-115.848,47.8044],[-115.848,47.8015],[-115.848,47.7988],[-115.848,47.7936],[-115.848,47.7864],[-115.846,47.7823],[-115.844,47.7785],[-115.843,47.7779],[-115.838,47.7719],[-115.836,47.7675],[-115.836,47.7651],[-115.835,47.7615],[-115.833,47.7565],[-115.833,47.7547],[-115.831,47.7523],[-115.828,47.7508],[-115.823,47.7521],[-115.819,47.7548],[-115.814,47.7554],[-115.806,47.7563],[-115.799,47.7553],[-115.787,47.7478],[-115.785,47.7463],[-115.783,47.7432],[-115.784,47.7394],[-115.785,47.7338],[-115.785,47.7326],[-115.783,47.7249],[-115.782,47.7245],[-115.775,47.7179],[-115.771,47.7163],[-115.77,47.7163],[-115.764,47.7165],[-115.755,47.7158],[-115.753,47.7149],[-115.744,47.7119],[-115.743,47.7115],[-115.733,47.7063],[-115.729,47.7028],[-115.725,47.7],[-115.724,47.6963],[-115.724,47.6883],[-115.724,47.6866],[-115.725,47.6828],[-115.726,47.678],[-115.727,47.6763],[-115.729,47.6702],[-115.732,47.6654],[-115.733,47.662],[-115.734,47.6597],[-115.734,47.658],[-115.733,47.6558],[-115.732,47.6491],[-115.731,47.647],[-115.728,47.6425],[-115.722,47.6395],[-115.719,47.6378],[-115.716,47.6369],[-115.701,47.6307],[-115.697,47.6269],[-115.697,47.626],[-115.696,47.6234],[-115.696,47.6154],[-115.696,47.6143],[-115.696,47.6119],[-115.696,47.6101],[-115.695,47.6065],[-115.695,47.6051],[-115.693,47.6035],[-115.692,47.6019],[-115.691,47.6008],[-115.691,47.5988],[-115.69,47.5956],[-115.69,47.5926],[-115.693,47.5916],[-115.695,47.5911],[-115.697,47.5905],[-115.703,47.587],[-115.704,47.5844],[-115.705,47.5821],[-115.71,47.5805],[-115.713,47.5796],[-115.715,47.5792],[-115.716,47.5788],[-115.721,47.5756],[-115.723,47.5723],[-115.725,47.5715],[-115.725,47.5709],[-115.729,47.5699],[-115.73,47.5696],[-115.733,47.5683],[-115.736,47.5667],[-115.737,47.5661],[-115.744,47.5608],[-115.749,47.557],[-115.75,47.5561],[-115.752,47.5539],[-115.754,47.5494],[-115.754,47.5488],[-115.754,47.5453],[-115.75,47.5413],[-115.748,47.5407],[-115.743,47.5395],[-115.736,47.5377],[-115.734,47.5368],[-115.731,47.536],[-115.726,47.5339],[-115.721,47.5336],[-115.719,47.5335],[-115.711,47.534],[-115.706,47.534],[-115.701,47.5322],[-115.7,47.5298],[-115.702,47.5276],[-115.705,47.5249],[-115.709,47.5218],[-115.709,47.521],[-115.709,47.5174],[-115.709,47.5163],[-115.706,47.5122],[-115.705,47.5104],[-115.703,47.5088],[-115.7,47.5058],[-115.698,47.5046],[-115.697,47.5034],[-115.695,47.5015],[-115.694,47.5002],[-115.691,47.4965],[-115.691,47.4955],[-115.69,47.4897],[-115.69,47.4875],[-115.689,47.487],[-115.684,47.4848],[-115.682,47.4848],[-115.679,47.4852],[-115.668,47.4877],[-115.666,47.4866],[-115.663,47.4834],[-115.66,47.4795],[-115.659,47.479],[-115.658,47.4777],[-115.656,47.4774],[-115.655,47.4774],[-115.652,47.4773],[-115.641,47.478],[-115.637,47.4785],[-115.635,47.4774],[-115.635,47.4746],[-115.635,47.474],[-115.639,47.4659],[-115.644,47.4606],[-115.645,47.4591],[-115.646,47.4588],[-115.652,47.4567],[-115.659,47.4549],[-115.661,47.4542],[-115.665,47.4538],[-115.669,47.4534],[-115.677,47.455],[-115.682,47.4558],[-115.684,47.4561],[-115.691,47.456],[-115.705,47.4545],[-115.719,47.4518],[-115.72,47.4512],[-115.729,47.4477],[-115.732,47.4464],[-115.741,47.442],[-115.747,47.4394],[-115.752,47.4367],[-115.754,47.435],[-115.76,47.4256],[-115.758,47.4233],[-115.757,47.4231],[-115.752,47.4223],[-115.75,47.4222],[-115.744,47.423],[-115.74,47.4236],[-115.735,47.4247],[-115.733,47.425],[-115.73,47.4253],[-115.725,47.4258],[-115.72,47.4222],[-115.718,47.4202],[-115.714,47.4168],[-115.713,47.4168],[-115.708,47.4171],[-115.708,47.4172],[-115.698,47.4163],[-115.695,47.4153],[-115.692,47.4142],[-115.684,47.4113],[-115.682,47.4094],[-115.68,47.4077],[-115.678,47.4063],[-115.671,47.4037],[-115.667,47.4021],[-115.662,47.4001],[-115.657,47.3966],[-115.654,47.3921],[-115.653,47.3883],[-115.649,47.383],[-115.648,47.3827],[-115.647,47.3829],[-115.643,47.3833],[-115.632,47.3846],[-115.623,47.3835],[-115.619,47.3829],[-115.616,47.382],[-115.613,47.3811],[-115.609,47.3799],[-115.604,47.3787],[-115.603,47.378],[-115.596,47.3742],[-115.589,47.3689],[-115.586,47.3667],[-115.585,47.3659],[-115.581,47.3622],[-115.579,47.359],[-115.577,47.3567],[-115.574,47.3557],[-115.573,47.3555],[-115.57,47.3542],[-115.566,47.3529],[-115.561,47.3514],[-115.554,47.3468],[-115.554,47.3459],[-115.55,47.3382],[-115.549,47.3363],[-115.545,47.3293],[-115.545,47.328],[-115.538,47.319],[-115.537,47.318],[-115.531,47.3105],[-115.53,47.3093],[-115.527,47.3044],[-115.525,47.3026],[-115.521,47.2992],[-115.515,47.2944],[-115.51,47.2905],[-115.503,47.2873],[-115.502,47.2871],[-115.491,47.2848],[-115.485,47.2834],[-115.483,47.2834],[-115.478,47.2835],[-115.477,47.2835],[-115.471,47.2836],[-115.469,47.2837],[-115.468,47.2833],[-115.464,47.282],[-115.463,47.2812],[-115.462,47.2807],[-115.458,47.2785],[-115.456,47.2772],[-115.453,47.2769],[-115.448,47.2763],[-115.443,47.2771],[-115.44,47.2775],[-115.439,47.2781],[-115.432,47.2801],[-115.431,47.2802],[-115.427,47.2801],[-115.425,47.2798],[-115.421,47.2756],[-115.421,47.275],[-115.419,47.2723],[-115.413,47.2671],[-115.412,47.2667],[-115.408,47.2653],[-115.405,47.265],[-115.401,47.2648],[-115.4,47.2648],[-115.394,47.266],[-115.391,47.2666],[-115.386,47.2673],[-115.385,47.2674],[-115.379,47.2669],[-115.377,47.2666],[-115.375,47.2658],[-115.372,47.2648],[-115.363,47.2622],[-115.358,47.2618],[-115.355,47.2617],[-115.352,47.2617],[-115.345,47.2626],[-115.343,47.2625],[-115.338,47.262],[-115.332,47.2612],[-115.331,47.261],[-115.326,47.26],[-115.32,47.2581],[-115.319,47.2555],[-115.319,47.2535],[-115.32,47.2528],[-115.322,47.249],[-115.322,47.2446],[-115.321,47.2431],[-115.319,47.2387],[-115.318,47.2379],[-115.31,47.2313],[-115.31,47.231],[-115.3,47.227],[-115.297,47.2248],[-115.296,47.2243],[-115.293,47.2206],[-115.292,47.2163],[-115.292,47.2148],[-115.292,47.2118],[-115.292,47.2107],[-115.293,47.2093],[-115.293,47.2068],[-115.295,47.2039],[-115.299,47.2001],[-115.3,47.198],[-115.301,47.1941],[-115.299,47.1918],[-115.296,47.1886],[-115.29,47.1864],[-115.288,47.186],[-115.285,47.1856],[-115.279,47.1846],[-115.271,47.1834],[-115.27,47.1833],[-115.261,47.1799],[-115.26,47.1794],[-115.257,47.1748],[-115.257,47.1741],[-115.257,47.1716],[-115.256,47.167],[-115.256,47.1654],[-115.256,47.1639],[-115.254,47.162],[-115.252,47.16],[-115.251,47.1588],[-115.248,47.1572],[-115.239,47.1535],[-115.236,47.1531],[-115.226,47.1519],[-115.226,47.1515],[-115.219,47.1478],[-115.216,47.1463],[-115.214,47.1455],[-115.211,47.1441],[-115.209,47.1429],[-115.195,47.1366],[-115.192,47.1345],[-115.189,47.1319],[-115.184,47.128],[-115.184,47.1276],[-115.177,47.1187],[-115.175,47.1159],[-115.174,47.1151],[-115.168,47.1075],[-115.167,47.1066],[-115.163,47.1057],[-115.156,47.1043],[-115.155,47.1043],[-115.151,47.1039],[-115.148,47.1035],[-115.141,47.1019],[-115.14,47.1013],[-115.139,47.0996],[-115.14,47.0954],[-115.14,47.0947],[-115.142,47.0894],[-115.141,47.0846],[-115.14,47.0825],[-115.139,47.0812],[-115.137,47.0787],[-115.133,47.0739],[-115.132,47.0725],[-115.126,47.0666],[-115.119,47.0609],[-115.116,47.0588],[-115.109,47.0533],[-115.109,47.0531],[-115.1,47.0485],[-115.099,47.0483],[-115.093,47.0466],[-115.088,47.0455],[-115.084,47.0439],[-115.082,47.0417],[-115.08,47.0395],[-115.08,47.0349],[-115.078,47.0311],[-115.078,47.0304],[-115.073,47.0266],[-115.071,47.0247],[-115.07,47.017],[-115.07,47.0134],[-115.069,47.0091],[-115.068,47.0056],[-115.067,47.0052],[-115.066,47.0014],[-115.065,46.9974],[-115.065,46.9937],[-115.062,46.9897],[-115.057,46.986],[-115.054,46.9833],[-115.052,46.9817],[-115.052,46.9808],[-115.051,46.9777],[-115.051,46.9754],[-115.05,46.9715],[-115.047,46.97],[-115.043,46.9701],[-115.039,46.9703],[-115.037,46.9704],[-115.03,46.9723],[-115.025,46.9745],[-115.023,46.9748],[-115.019,46.9754],[-115.015,46.9752],[-115.01,46.9739],[-115.007,46.9726],[-114.998,46.9666],[-114.997,46.9655],[-114.989,46.9571],[-114.987,46.9532],[-114.986,46.9506],[-114.984,46.9488],[-114.981,46.9465],[-114.98,46.9459],[-114.978,46.9445],[-114.975,46.9426],[-114.97,46.9391],[-114.969,46.9388],[-114.963,46.9374],[-114.96,46.9332],[-115.049,46.9331],[-115.069,46.933],[-115.132,46.9328],[-115.259,46.9321],[-115.386,46.9314],[-115.6,46.9307],[-115.72,46.9311],[-115.764,46.9311],[-115.785,46.9314],[-115.807,46.9312],[-115.849,46.9313],[-115.871,46.9315],[-115.934,46.9313],[-116.016,46.9323],[-116.12,46.9329],[-116.14,46.9327],[-116.328,46.9326],[-116.327,46.9478],[-116.326,46.9625],[-116.326,46.9772],[-116.327,46.9919],[-116.326,47.007],[-116.327,47.0231],[-116.325,47.1081],[-116.325,47.1356],[-116.325,47.1503],[-116.325,47.1802],[-116.325,47.1944],[-116.325,47.2101],[-116.325,47.2394],[-116.325,47.2537],[-116.325,47.2684],[-116.325,47.2978],[-116.326,47.313],[-116.326,47.3199],[-116.325,47.3277],[-116.325,47.3424],[-116.325,47.3571],[-116.324,47.37],[-116.324,47.3838],[-116.325,47.3985],[-116.325,47.4137],[-116.325,47.4284],[-116.324,47.4422],[-116.324,47.4555],[-116.324,47.485],[-116.324,47.4997],[-116.324,47.5149],[-116.322,47.5857],[-116.324,47.889]]]},\"properties\":{\"name\":\"Shoshone\",\"state\":\"ID\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db6830fe","contributors":{"authors":[{"text":"Hobbs, S. Warren","contributorId":36420,"corporation":false,"usgs":true,"family":"Hobbs","given":"S. Warren","affiliations":[],"preferred":false,"id":152005,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Griggs, Allan B.","contributorId":21929,"corporation":false,"usgs":true,"family":"Griggs","given":"Allan B.","affiliations":[],"preferred":false,"id":152004,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wallace, Robert E.","contributorId":15570,"corporation":false,"usgs":true,"family":"Wallace","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":152002,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Campbell, Arthur B.","contributorId":29035,"corporation":false,"usgs":true,"family":"Campbell","given":"Arthur B.","affiliations":[],"preferred":false,"id":152003,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1132,"text":"wsp1809P - 1965 - Water-supply potential from an asphalt-lined catchment near Holualoa Kona, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1809P","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"P","title":"Water-supply potential from an asphalt-lined catchment near Holualoa Kona, Hawaii","docAbstract":"The Jenkins-Whitesburg area includes approximately 250 square miles In Letcher and Pike Counties in the southeastern part of the Eastern Coal Field. In this area ground water is the principal source of water for nearly all rural families, most public supplies, several coal mines and coal processing plants, and one bottling plant. \r\n\r\nThe major aquifers in the Jenkins-Whitesburg area are the Breathitt and Lee Formations of Pennsylvanian age. Other aquifers range in age from Devonian to Quaternary but are not important in this area because they occur at great depth or yield little or no water. The Breathitt Formation occurs throughout the area except along the crest and slopes of Pine Mountain and where it is covered by unconsolidated material of Quaternary age. The Breathitt Formation consists of shale, sandstone, and lesser amounts of coal and associated underclay. The yield of wells penetrating the Breathitt Formation ranges from less than 1 to 330 gallons per minute. Well yield is controlled by the type and depth of well, character of the aquifer, and topography of the well site. Generally, deep wells drilled in valleys of perennial streams offer the best potential for high yields. Although enough water for a minimum domestic supply (more than 100 gallons per day) may be obtained from shale, all high-yielding wells probably obtain water from vertical joints and from bedding planes which are best developed in sandstone. About 13 percent of the wells inventoried in the Breathitt Formation failed to supply enough water for a minimum domestic supply. Most of these are shallow dug wells or drilled wells on hillsides or hilltops. Abandoned coal mines are utilized as large infiltration galleries and furnish part of the water for several public supplies. \r\n\r\nThe chemical quality of water from the Breathitt Formation varies considerably from place to place, but the water generally is acceptable for most domestic and industrial uses. Most water is a calcium magnesium bicarbonate or sodium bicarbonate type, and nearly all sampled water contained enough iron to stain cooking and laundry utensils. The water ranged from soft to very hard, and only one well in the Breathitt Formation produced salty water. The absence of salty water may be due to abundant fractures which are associated with the Pine Mountain fault and which have allowed fresh water to enter the formation. The Lee Formation underlies the Cumberland Mountain section and is exposed along the crest and southeast slope of Pine Mountain. The Lee Formation consists of massive sandstone and conglomerate with thin beds of shale and a few thin coal seams.\r\n\r\nAlthough the Lee Formation is tapped by only a few wells in this area, it is potentially an important aquifer. Wells penetrating the Lee Formation in the Cumberland Mountain section would probably yield water under artesian pressure.\r\n\r\nUnlike most water from the Lee Formation in other part.3 of eastern Kentucky, all water from the Lee Formation in the Jenkins-Whitesburg area is fresh. All water from the Lee Formation contained more than 0.3 parts per million of iron and ranged from soft to moderately hard.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1809P","usgsCitation":"Chinn, S.S., 1965, Water-supply potential from an asphalt-lined catchment near Holualoa Kona, Hawaii: U.S. Geological Survey Water Supply Paper 1809, iv, 25 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1809P.","productDescription":"iv, 25 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809p/report-thumb.jpg"},{"id":25912,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809p/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4bd7","contributors":{"authors":[{"text":"Chinn, Salwyn S.W.","contributorId":91082,"corporation":false,"usgs":true,"family":"Chinn","given":"Salwyn","email":"","middleInitial":"S.W.","affiliations":[],"preferred":false,"id":143231,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1231,"text":"wsp1809D - 1965 - An evaluation of aquifer and well characteristics of municipal well fields in Los Alamos and Guaje Canyons, near Los Alamos, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1809D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"D","title":"An evaluation of aquifer and well characteristics of municipal well fields in Los Alamos and Guaje Canyons, near Los Alamos, New Mexico","docAbstract":"The Jenkins-Whitesburg area includes approximately 250 square miles In Letcher and Pike Counties in the southeastern part of the Eastern Coal Field. In this area ground water is the principal source of water for nearly all rural families, most public supplies, several coal mines and coal processing plants, and one bottling plant. \r\n\r\nThe major aquifers in the Jenkins-Whitesburg area are the Breathitt and Lee Formations of Pennsylvanian age. Other aquifers range in age from Devonian to Quaternary but are not important in this area because they occur at great depth or yield little or no water. The Breathitt Formation occurs throughout the area except along the crest and slopes of Pine Mountain and where it is covered by unconsolidated material of Quaternary age. The Breathitt Formation consists of shale, sandstone, and lesser amounts of coal and associated underclay. The yield of wells penetrating the Breathitt Formation ranges from less than 1 to 330 gallons per minute. Well yield is controlled by the type and depth of well, character of the aquifer, and topography of the well site. Generally, deep wells drilled in valleys of perennial streams offer the best potential for high yields. Although enough water for a minimum domestic supply (more than 100 gallons per day) may be obtained from shale, all high-yielding wells probably obtain water from vertical joints and from bedding planes which are best developed in sandstone. About 13 percent of the wells inventoried in the Breathitt Formation failed to supply enough water for a minimum domestic supply. Most of these are shallow dug wells or drilled wells on hillsides or hilltops. Abandoned coal dunes are utilized as large infiltration galleries and furnish part of the water for several public supplies. \r\n\r\nThe chemical quality of water from the Breathitt Formation varies considerably from place to place, but the water generally is acceptable for most domestic and industrial uses. Most water is a calcium magnesium bicarbonate or sodium bicarbonate type, and nearly all sampled water contained enough iron to stain cooking and laundry utensils. The water ranged from soft to very hard, and only one well in the Breathitt Formation produced salty water. The absence of salty water may be due to abundant fractures which are associated with the Pine Mountain fault and which have allowed fresh water to enter the formation. The Lee Formation underlies the Cumberland Mountain section and is exposed along the crest and southeast slope of Pine Mountain. The Lee Formation consists of massive sandstone and conglomerate with thin beds of shale and a few thin coal seams.\r\n\r\nAlthough the Lee Formation is tapped by only a few wells in this area, it is potentially an important aquifer. Wells penetrating the Lee Formation in the Cumberland Mountain section would probably yield water under artesian pressure.\r\n\r\nUnlike most water from the Lee Formation in other part.3 of eastern Kentucky, all water from the Lee Formation in the Jenkins-Whitesburg area is fresh. All water from the Lee Formation contained more than 0.3 parts per million of iron and ranged from soft to moderately hard.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1809D","usgsCitation":"Cushman, R., 1965, An evaluation of aquifer and well characteristics of municipal well fields in Los Alamos and Guaje Canyons, near Los Alamos, New Mexico: U.S. Geological Survey Water Supply Paper 1809, v, 50 p. :ill., maps ;24 cm. + plates folded in pocket., https://doi.org/10.3133/wsp1809D.","productDescription":"v, 50 p. :ill., maps ;24 cm. + plates folded in pocket.","costCenters":[],"links":[{"id":138069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809d/report-thumb.jpg"},{"id":26149,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26150,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26151,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26152,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26153,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684a57","contributors":{"authors":[{"text":"Cushman, Robert L.","contributorId":22751,"corporation":false,"usgs":true,"family":"Cushman","given":"Robert L.","affiliations":[],"preferred":false,"id":143410,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":934,"text":"wsp1809J - 1965 - Water-resources reconnaissance of the Ouachita Mountains, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1809J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"J","title":"Water-resources reconnaissance of the Ouachita Mountains, Arkansas","docAbstract":"The Jenkins-Whitesburg area includes approximately 250 square miles in Letcher and Pike Counties in the southeastern part of the Eastern Coal Field. In this area ground water is the principal source of water for nearly all rural families, most public supplies, several coal mines and coal processing plants, and one bottling plant. \r\n\r\nThe major aquifers in the Jenkins-Whitesburg area are the Breathitt and Lee Formations of Pennsylvanian age. Other aquifers range in age from Devonian to Quaternary but are not important in this area because they occur at great depth or yield little or no water. The Breathitt Formation occurs throughout the area except along the crest and slopes of Pine Mountain and where it is covered by unconsolidated material of Quaternary age. The Breathitt Formation consists of shale, sandstone, and lesser amounts of coal and associated underclay. The yield of wells penetrating the Breathitt Formation ranges from less than 1 to 330 gallons per minute. Well yield is controlled by the type and depth of well, character of the aquifer, and topography of the well site. Generally, deep wells drilled in valleys of perennial streams offer the best potential for high yields. Although enough water for a minimum domestic supply (more than 100 gallons per day) may be obtained from shale, all high-yielding wells probably obtain water from vertical joints and from bedding planes which are best developed in sandstone. About 13 percent of the wells inventoried in the Breathitt Formation failed to supply enough water for a minimum domestic supply. Most of these are shallow dug wells or drilled wells on hillsides or hilltops. Abandoned coal mines are utilized as large infiltration galleries and furnish part of the water for several public supplies. \r\n\r\nThe chemical quality of water from the Breathitt Formation varies considerably from place to place, but the water generally is acceptable for most domestic and industrial uses. Most water is a calcium magnesium bicarbonate or sodium bicarbonate type, and nearly all sampled water contained enough iron to stain cooking and laundry utensils. The water ranged from soft to very hard, and only one well in the Breathitt Formation produced salty water. The absence of salty water may be due to abundant fractures which are associated with the Pine Mountain fault and which have allowed fresh water to enter the formation. The Lee Formation underlies the Cumberland Mountain section and is exposed along the crest and southeast slope of Pine Mountain. The Lee Formation consists of massive sandstone and conglomerate with thin beds of shale and a few thin coal seams.\r\n\r\nAlthough the Lee Formation is tapped by only a few wells in this area, it is potentially an important aquifer. Wells penetrating the Lee Formation in the Cumberland Mountain section would probably yield water under artesian pressure. \r\n\r\nUnlike most water from the Lee Formation in other parts of eastern Kentucky, all water from the Lee Formation in the Jenkins-Whitesburg area is fresh. All water from the Lee Formation contained more than 0.3 parts per million of iron and ranged from soft to moderately hard.","language":"ENGLISH","publisher":"United States. Government Printing Office,","doi":"10.3133/wsp1809J","usgsCitation":"Albin, D.R., 1965, Water-resources reconnaissance of the Ouachita Mountains, Arkansas: U.S. Geological Survey Water Supply Paper 1809, iii, 14 p. :maps (part fold., in pocket) ;24 cm., https://doi.org/10.3133/wsp1809J.","productDescription":"iii, 14 p. :maps (part fold., in pocket) ;24 cm.","costCenters":[],"links":[{"id":137015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809j/report-thumb.jpg"},{"id":25407,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25408,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485a0","contributors":{"authors":[{"text":"Albin, Donald R.","contributorId":67486,"corporation":false,"usgs":true,"family":"Albin","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":142880,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70197612,"text":"70197612 - 1965 - Ordovician, Silurian, and Devonian biostratigraphy of east-central Alaska","interactions":[],"lastModifiedDate":"2023-02-01T14:25:21.059833","indexId":"70197612","displayToPublicDate":"1965-12-31T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Ordovician, Silurian, and Devonian biostratigraphy of east-central Alaska","docAbstract":"A predominantly shale and chert sequence has been mapped from the Canadian border at Latitude 65°00′ N. to the Nation River about 25 miles northwest. It has Ordovician and Silurian graptolites in the lower half, and Middle Devonian corals and Upper Devonian spores in the upper half.
The lower half of the sequence consists of about 400 to 900 feet of predominantly dark gray graptolitic shale with lesser amounts of grayish black laminated chert. This unit has been traced by Green and Roddick from the international border southeastward into the Dawson area of the Yukon Territory and northeastward into the Ogilvie and Richardson Mountains where it has been mapped by Jackson & Lenz, Norris, and others as the Road River Formation. In the Tatonduk-Nation Rivers area the Road River Formation rests disconformably on a sequence of Middle and Upper Cambrian limestone that locally may include Lower Ordovician (Tremadoc) beds at its top. The sequence of graptolite faunas from the Road River Formation in Alaska is essentially the same as the graptolite zones established by Elles and Wood in Great Britain. All the standard series of the Ordovician and Silurian are probably represented in the formation with the exception of the Tremadoc and possibly the Arenig and Wenlock.
Overlying the Road River Formation is a formation, 200 to 800 feet thick, consisting predominantly of thinly bedded and laminated light gray to black chert and siliceous shale that is here named the McCann Hill Chert. This new formation disconformably overlies the Road River Formation, and its lower boundary is at the base of a distinctive limestone and shale member. The basal limestone and shale member of the McCann Hill Chert contains a remarkably varied fauna including corals, brachiopods, trilobites, conodonts, ostracods, and fish of Eifelian (early Middle Devonian) age. Spores from the upper part of the formation resemble those from the overlying Nation River Formation and indicate a Late Devonian age. The McCann Hill Chert is conformably overlain by the Nation River Formation—a thick succession of inter-bedded graywacke, chert conglomerate, and silty shale of Late Devonian age.
In the vicinity of Jones Ridge, only 7 miles north of exposures of the Road River Formation, Upper Cambrian limestone is overlain by a pure limestone section containing Ordovician, Middle Devonian, and perhaps Silurian shelly faunas contemporaneous with the Road River Formation and the thinner basal limestone and shale member of the McCann Hill Chert. The rapid change from graptolitic shale to limestone probably reflects changes in conditions of sedimentation, but could be a result of thrust faulting.
The Tatonduk-Nation Rivers area seems to lie in a transitional zone between an early Paleozoic eugeosynclinal belt south of the Yukon River and a contemporaneous miogeosynclinal belt along the Porcupine River. One puzzling feature of the lower Paleozoic sequence in the Tatonduk-Nation Rivers area is its thinness in contrast to the much thicker volcanic and detrital sequence on the south and the considerably thicker carbonate sequence on the north.
","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/A6633526-16C0-11D7-8645000102C1865D","usgsCitation":"Churkin, M., and Brabb, E.E., 1965, Ordovician, Silurian, and Devonian biostratigraphy of east-central Alaska: American Association of Petroleum Geologists Bulletin, v. 49, no. 2, p. 172-185, https://doi.org/10.1306/A6633526-16C0-11D7-8645000102C1865D.","productDescription":"14 p.","startPage":"172","endPage":"185","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355007,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Nation-Tatonduk Rivers area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -142.38695878694335,\n 65.46836165464507\n ],\n [\n -142.38695878694335,\n 64.62502455781637\n ],\n [\n -141.00230856836862,\n 64.62502455781637\n ],\n [\n -141.00230856836862,\n 65.46836165464507\n ],\n [\n -142.38695878694335,\n 65.46836165464507\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"49","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Churkin, Michael Jr.","contributorId":62566,"corporation":false,"usgs":true,"family":"Churkin","given":"Michael","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":737908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brabb, Earl E.","contributorId":8545,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":737909,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221187,"text":"70221187 - 1965 - Solubility measurements in the system CaSO4-NaCL-H2O at 35°, 50°, and 70°cand one atmosphere pressure","interactions":[],"lastModifiedDate":"2021-06-04T18:15:18.43742","indexId":"70221187","displayToPublicDate":"1965-12-01T13:11:47","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Solubility measurements in the system CaSO4-NaCL-H2O at 35°, 50°, and 70°cand one atmosphere pressure","docAbstract":"The solubilities in the system CaSO4-NaCl-H2O, at 1 atm pressure and 35°, 50°, and 70°C, have been determined by approaching the solubility curves from both the undersaturation and supersaturation sides. The experimental runs are of long duration, as much as 3 months; these rates should be commensurate with those of the appropriate geological processes, and so the results should be directly applicable to the interpretation of evaporite deposits.
","language":"English","publisher":"Oxford University Press","doi":"10.1093/petrology/6.1.124","usgsCitation":"Zen, E., 1965, Solubility measurements in the system CaSO4-NaCL-H2O at 35°, 50°, and 70°cand one atmosphere pressure: Journal of Petrology, v. 6, no. 1, p. 124-164, https://doi.org/10.1093/petrology/6.1.124.","productDescription":"41 p.","startPage":"124","endPage":"164","costCenters":[],"links":[{"id":386232,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zen, E-An","contributorId":47064,"corporation":false,"usgs":true,"family":"Zen","given":"E-An","email":"","affiliations":[],"preferred":false,"id":817019,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5222228,"text":"5222228 - 1965 - Epizootiologic studies on filarioids of the raccoon","interactions":[],"lastModifiedDate":"2025-02-07T16:26:50.198695","indexId":"5222228","displayToPublicDate":"1965-10-11T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Epizootiologic studies on filarioids of the raccoon","docAbstract":"Filarioid worms (Dirofilaria immitis, D. tenuis, Dipetalonema procyonis, and D. llewellyni) were discovered in raccoons (Procyon lotar) in Maryland. Raccoons were trapped in lowland, upland, and agricultural-residential areas, which were further classified as stream borders, poorly drained, and well drained. Data on incidence of D. llewellyni were analyzed on basis of host distribution within these areas to indicate type of habitat in which one might seek the vector. It was concluded that exposure takes place in the spring of the year. The arthropod found associated most often with the raccoon in spring was Ixodes texanus. Larvae of this tick which were fed on infected raccoons presented no evidence of development of the microfilariae. Feeding experiments were also conducted with mosquitoes: Aedes aegypti, A. canadensis, A. sollicitans, A. triseriatus, A. vexans, Culex pipiens, Anopheles punctipennis, and A. quadrimaculatus. Although microfilariae remained alive and active in the gut contents of all these mosquitoes for 2 days, only in Aedes aegypti did they enter the hemocele, but no developmental changes were noted and all microfilariae were dead by the eighth day. Although the intermediate host of D. llewellyni was not determined, evaluation of the accumulated data provides criteria for seeking the vector. It appeared unlikely that exposure of the raccoons took place in the den or that the filarioids were transmitted by an ectoparasite commonly found in raccoon dens. The data suggest that the vector is available only early in spring, although there are infected raccoons throughout the year. Prevalence in juveniles was 21 percent; in subadults, 64 percent; in adults, 87 percent.
","language":"English","publisher":"Wiley","doi":"10.2307/3798544","usgsCitation":"Herman, C.M., and Price, D., 1965, Epizootiologic studies on filarioids of the raccoon: Journal of Wildlife Management, v. 29, no. 4, p. 694-699, https://doi.org/10.2307/3798544.","productDescription":"6 p.","startPage":"694","endPage":"699","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196000,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent Wildlife Research Center","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.82499365611099,\n 39.06403824922501\n ],\n [\n -76.82499365611099,\n 39.05470892556758\n ],\n [\n -76.81260696233649,\n 39.05470892556758\n ],\n [\n -76.81260696233649,\n 39.06403824922501\n ],\n [\n -76.82499365611099,\n 39.06403824922501\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"29","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d601","contributors":{"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":335856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, D.L.","contributorId":94399,"corporation":false,"usgs":true,"family":"Price","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":335855,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}