No abstract available.
","language":"English","publisher":"Southeastern Association","usgsCitation":"Sincock, J.L., 1962, Estimating consumption of food by wintering waterfowl populations: Proceedings of the Annual Conference of the Southeastern Association of Game and Fish Commissioners, v. 16, p. 217-221.","productDescription":"5 p.","startPage":"217","endPage":"221","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":372543,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":372542,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.seafwa.org/publications/proceedings/?id=66076"}],"country":"United States","state":"North Carolina, Virginia","otherGeospatial":"Back Bay, Currituck Sound","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.90591430664062,\n 36.6640126988417\n ],\n [\n -75.94436645507812,\n 36.737783602451906\n ],\n [\n -75.99105834960938,\n 36.717971509608496\n ],\n [\n -76.014404296875,\n 36.61442534338386\n ],\n [\n -76.00479125976562,\n 36.56590907528833\n ],\n [\n -76.0638427734375,\n 36.61442534338386\n ],\n [\n -76.058349609375,\n 36.54384614538856\n ],\n [\n -76.0858154296875,\n 36.52067329034796\n ],\n [\n -76.08444213867188,\n 36.470993797486535\n ],\n [\n -76.04324340820312,\n 36.488661268293136\n ],\n [\n -75.99517822265625,\n 36.37817351148144\n ],\n [\n -75.93338012695312,\n 36.34167804918315\n ],\n [\n -75.88668823242188,\n 36.25867019438799\n ],\n [\n -75.79879760742188,\n 36.0779620797358\n ],\n [\n -75.72738647460938,\n 36.09682839442643\n ],\n [\n -75.75897216796875,\n 36.20106624342554\n ],\n [\n -75.80291748046875,\n 36.29077703961915\n ],\n [\n -75.81527709960936,\n 36.31291199724548\n ],\n [\n -75.81253051757812,\n 36.33725319397006\n ],\n [\n -75.85235595703125,\n 36.43896124085945\n ],\n [\n -75.86883544921875,\n 36.52398412328937\n ],\n [\n -75.90591430664062,\n 36.6640126988417\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"16","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sincock, John L.","contributorId":111418,"corporation":false,"usgs":false,"family":"Sincock","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":782905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220787,"text":"70220787 - 1962 - Flume studies of the transport of pebbles and cobbles on a sand bed","interactions":[],"lastModifiedDate":"2021-05-25T18:06:23.791591","indexId":"70220787","displayToPublicDate":"1962-11-01T13:03:05","publicationYear":"1962","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":"Flume studies of the transport of pebbles and cobbles on a sand bed","docAbstract":"During experiments on sediment transport and resistance to flow with a uniform 0.33-mm sand, data were recorded on the movement of individual rocks having intermediate diameters from about 0.1 to 0.5 foot. The experiments were conducted in a flume 2 feet wide by 60 feet long and for most runs, depth was held constant at 0.5 foot. The experiments showed that rocks on the sand bed moved downstream consistently only if the flow was in the upper regime - that is, only if the bed forms were plane bed, standing waves, or antidunes. The rocks moved at velocities that were approximately half the average velocity of the water. On all bed forms in the lower flow regime (ripples, ripples superimposed upon dunes, and dunes), the rocks moved upstream and down into the bed. That is, the rocks moved into a scour pocket that formed at the upstream side of the rock. The movement upstream and down into the bed is limited by and approximately equal to the distance below the original rock position of the minimum bed elevation plus approximately half the rock diameter. The data indicate that cross-bedded sand deposits formed by the ripple or dune phases of transport would contain few, if any, pebbles or cobbles. Because the flow, in at least the downstream reaches, of most rivers is in the lower regime, the upstream movement and scour into the bed demonstrated in these experiments is an important factor in the sorting process.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[1431:FSOTTO]2.0.CO;2","usgsCitation":"Fahnestock, R.K., and Haushild, W., 1962, Flume studies of the transport of pebbles and cobbles on a sand bed: Geological Society of America Bulletin, v. 73, no. 11, p. 1431-1436, https://doi.org/10.1130/0016-7606(1962)73[1431:FSOTTO]2.0.CO;2.","productDescription":"6 p.","startPage":"1431","endPage":"1436","costCenters":[],"links":[{"id":480371,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/10217/196127","text":"External Repository"},{"id":385952,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fahnestock, Robert K.","contributorId":100381,"corporation":false,"usgs":true,"family":"Fahnestock","given":"Robert","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":816465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haushild, W.L.","contributorId":48953,"corporation":false,"usgs":true,"family":"Haushild","given":"W.L.","affiliations":[],"preferred":false,"id":816466,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220656,"text":"70220656 - 1962 - Studies of fluid inclusions I: Low temperature application of a dual-purpose freezing and heating stage","interactions":[],"lastModifiedDate":"2021-05-24T12:29:26.087514","indexId":"70220656","displayToPublicDate":"1962-11-01T07:26:21","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Studies of fluid inclusions I: Low temperature application of a dual-purpose freezing and heating stage","docAbstract":"The design and operation of a microscope freezing stage developed for use at magnifications up to 500X are described. It makes possible studies of low-temperature phase changes such as the freezing of a saline water phase, and hence an estimate of the total salt concentration, in fluid inclusions as small as 10 microns (10-6 milligram in weight). The crystal or polished mineral plate containing the inclusions is viewed while immersed in a thermostated heat exchange medium (acetone) circulating rapidly in order to minimize thermal gradients. The stage permits easy operation at temperatures down to -35° C, with electrical control to ±0.05° C, and to much lower temperatures with manual control. With substitution of silicone oil for acetone, the same stage can be used for heating experiments up to +250° C. Calibration points in the low range indicate the accuracy of freezing temperature determinations on optimum material to be better than ±0.1° C. The low relief of ice crystals in water solution places considerable importance on sample selection, preparation, and lighting. As a result of almost ubiquitous and drastic supercooling (meta-stability), -35° C is inadequate to freeze most inclusions. Holding at -78.5° C (acetone + solid CO 2) for thirty minutes is generally adequate, although a few samples require extended immersion in liquid nitrogen at -196° C to cause freezing of even a part of their inclusions. Such extensive supercooling is not possible with most surface waters owing to the presence of abundant extraneous solid nuclei for the crystallization of ice.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.57.7.1045","usgsCitation":"Roedder, E., 1962, Studies of fluid inclusions I: Low temperature application of a dual-purpose freezing and heating stage: Economic Geology, v. 57, no. 1, p. 1045-1061, https://doi.org/10.2113/gsecongeo.57.7.1045.","productDescription":"17 p.","startPage":"1045","endPage":"1061","costCenters":[],"links":[{"id":385882,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"1","noUsgsAuthors":false,"publicationDate":"1962-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Roedder, E.","contributorId":100986,"corporation":false,"usgs":true,"family":"Roedder","given":"E.","affiliations":[],"preferred":false,"id":816308,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1003296,"text":"1003296 - 1962 - Evaluation of some heparinized capillaries for microhematocrit determinations of warm-water fishes","interactions":[],"lastModifiedDate":"2025-08-01T15:39:53.140727","indexId":"1003296","displayToPublicDate":"1962-10-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of some heparinized capillaries for microhematocrit determinations of warm-water fishes","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1962)24[188:EOSHCF]2.0.CO;2","usgsCitation":"Mairs, D., and Kennedy, T., 1962, Evaluation of some heparinized capillaries for microhematocrit determinations of warm-water fishes: Progressive Fish-Culturist, v. 24, no. 4, p. 188-189, https://doi.org/10.1577/1548-8659(1962)24[188:EOSHCF]2.0.CO;2.","productDescription":"2 p.","startPage":"188","endPage":"189","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":131317,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fab53","contributors":{"authors":[{"text":"Mairs, D.F.","contributorId":40936,"corporation":false,"usgs":true,"family":"Mairs","given":"D.F.","affiliations":[],"preferred":false,"id":313084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennedy, T.E.","contributorId":101604,"corporation":false,"usgs":true,"family":"Kennedy","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":313085,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220657,"text":"70220657 - 1962 - The origin of jasperoid in limestone","interactions":[],"lastModifiedDate":"2021-05-24T12:37:43.054398","indexId":"70220657","displayToPublicDate":"1962-09-01T07:33:31","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The origin of jasperoid in limestone","docAbstract":"The name jasperoid has been applied to rocks that consist mainly of silica and that have formed by replacement. This paper considers only those jasperoids formed by replacement of limestone. Major problems involved in the origin of such jasperoid include: source of the silica; nature of solutions that dissolve, transport, and precipitate silica; and the mechanism of replacement of limestone by silica. The answers to these problems are of practical as well as scientific interest because many jasperoid bodies are closely related to mineralization. Silica may be derived from: juvenile silica of magmatic origin; silica leached from underlying rocks by hydrothermal solutions; silica locally derived from enclosing rocks by circulating solutions; and silica carried downward in ground water from the weathering of overlying rocks. The nature and the concentration of other substances in solutions influence,in a complex manner, the ability of these solutions to dissolve, transport, and precipitate silica. Nevertheless, the following generalizations can be made. The solubility and rate of solution of silica in water at moderate pressure increase slowly with temperature up to 200 degrees C.; from 200 degrees to 360 degrees C. they increase rapidly; above 360 degrees C. solubility is pressure dependent, increasing steadily at high pressure and decreasing slightly at moderate pressure due to the formation of a vapor phase. The pH has slight effect on the ionic solubility of silica in the range from pH 1 to ph 9 at low temperature. The effect of other components on the solubility of silica is probably subordinate to that of temperature above 200 degrees C., but becomes increasingly important as the temperature falls below that point. Most jasperoid bodies form by both replacement and silica deposition in voids, with replacement dominant during the early phase, and precipitation dominant during later phases. Replacement of limestone by silica is favored by relatively low temperature acid solutions, and the presence of CO 2 . As limestone dissolves, Ca ions are released to promote the precipitation of colloidal silica. Acid solutions then diffuse through this gelatinous film to continue dissolving limestone behind it; the Ca ions diffusing outward cause the precipitation of more colloidal silica at the solution-gel interface. As the gel mass ages, it shrinks, hardens, and ruptures. More silica is then deposited in the fractures. Eventually the gel crystallizes to a dense mass of aphanitic quartz and chalcedony, with shrinkage cracks and vugs filled or coated with younger coarse-grained quartz and other minerals that have been deposited directly from solution. The theory that relatively low temperature favors the formation of jasperoid replacement bodies in carbonate rocks, and high temperature inhibits their formation, offers an explanation for the gap that is observed in some districts between contact metasomatic lime silicates and siliceous replacement of limestone. This gap is characterized by the lack of any reaction between limestone and silica-bearing solutions moving through it.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.57.6.861","usgsCitation":"Lovering, T., 1962, The origin of jasperoid in limestone: Economic Geology, v. 57, no. 6, p. 861-889, https://doi.org/10.2113/gsecongeo.57.6.861.","productDescription":"29 p.","startPage":"861","endPage":"889","costCenters":[],"links":[{"id":385883,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"6","noUsgsAuthors":false,"publicationDate":"1962-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Lovering, T.G.","contributorId":91098,"corporation":false,"usgs":true,"family":"Lovering","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":816309,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213475,"text":"70213475 - 1962 - Water Research by the Geological Survey","interactions":[],"lastModifiedDate":"2020-09-17T20:02:10.732335","indexId":"70213475","displayToPublicDate":"1962-08-24T15:00:01","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Water Research by the Geological Survey","docAbstract":"No abstract available.
","language":"English","publisher":"AAAS","doi":"10.1126/science.137.3530.571-a","usgsCitation":"Nolan, T.B., 1962, Water Research by the Geological Survey: Science, v. 137, no. 3530, p. 571-573, https://doi.org/10.1126/science.137.3530.571-a.","productDescription":"3 p.","startPage":"571","endPage":"573","costCenters":[],"links":[{"id":378540,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"137","issue":"3530","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Nolan, Thomas B.","contributorId":102477,"corporation":false,"usgs":true,"family":"Nolan","given":"Thomas","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":799124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70176598,"text":"70176598 - 1962 - Controlled induced recharge tests at Kalamazoo, Mich","interactions":[],"lastModifiedDate":"2025-01-07T16:20:23.799877","indexId":"70176598","displayToPublicDate":"1962-07-18T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2136,"text":"Journal - American Water Works Association","active":true,"publicationSubtype":{"id":10}},"title":"Controlled induced recharge tests at Kalamazoo, Mich","docAbstract":"This article discusses the results of a controlled field testing program, which indicated that definite hydraulic and other advantages may be gained from induced recharging as practiced at Kalamazoo, Michigan. Results include the following: water levels and artesian pressures can be maintained at high stages, the results are lower pumping lifts and substantial reductions in the amount of power used for pumping; the high water levels permit increased rates of withdrawal during periods of peak demand; encroachment of poor quality water from other aquifers is minimized; the surface water induced into the aquifer is filtered naturally through great thicknesses of earth materials; natural underground storage is used to conserve and protect water, which otherwise would flow largely to waste; and, significant supplemental benefits, including flood control, have been derived. The tests demonstrated that it is possible to manipulate the regimen of a complex hydrologic system for definite hydraulic benefits with predictable results. Furthermore with current methods, quantitative evaluations may be made of the effects of induced recharge. The results of the tests, therefore, are applicable in other areas of similar hydrogeologic environments.
","language":"English","publisher":"American Water Works Association","publisherLocation":"New York, NY","doi":"10.1002/j.1551-8833.1962.tb00831.x","usgsCitation":"Deutsch, M., 1962, Controlled induced recharge tests at Kalamazoo, Mich: Journal - American Water Works Association, v. 54, no. 2, p. 181-196, https://doi.org/10.1002/j.1551-8833.1962.tb00831.x.","productDescription":"16 p.","startPage":"181","endPage":"196","numberOfPages":"16","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":328865,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","city":"Kalamazoo","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -85.84304809570312,\n 42.09312731992276\n ],\n [\n -85.84304809570312,\n 42.416359972082866\n ],\n [\n -85.34042358398438,\n 42.416359972082866\n ],\n [\n -85.34042358398438,\n 42.09312731992276\n ],\n [\n -85.84304809570312,\n 42.09312731992276\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"54","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcff4e4b0824b2d17619a","contributors":{"authors":[{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":649336,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220776,"text":"70220776 - 1962 - Use of thermometry in hydrogeologic studies of glacial deposits at Worthington, Minnesota","interactions":[],"lastModifiedDate":"2021-05-25T17:37:15.261452","indexId":"70220776","displayToPublicDate":"1962-06-01T12:32:22","publicationYear":"1962","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":"Use of thermometry in hydrogeologic studies of glacial deposits at Worthington, Minnesota","docAbstract":"Precise measurements of fluctuations of ground-water temperature based on monthly readings in shallow glacial-outwash aquifers may be used to study ground-water movement and recharge. An increase in storage in the shallow basin of Okabena Lake, Worthington, Minnesota, permits the water to cover a much larger area and probably increases the opportunity for infiltration of lake water into aquifers connected with the lake. In a shallow artesian aquifer confined by relatively impervious glacial till, water moves toward the land surface in response to steep temperature gradients in the winter, and cool water descends to the aquifer when the upward temperature gradient is lowered or eliminated. Thermometry may also be used in hydrogeologic studies of limestone terrane.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[1305:UOTIHS]2.0.CO;2","usgsCitation":"Schneider, R., 1962, Use of thermometry in hydrogeologic studies of glacial deposits at Worthington, Minnesota: Geological Society of America Bulletin, v. 73, no. 10, p. 1305-1308, https://doi.org/10.1130/0016-7606(1962)73[1305:UOTIHS]2.0.CO;2.","productDescription":"4 p.","startPage":"1305","endPage":"1308","costCenters":[],"links":[{"id":385947,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","city":"Worthington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.78979492187499,\n 43.600284023536325\n ],\n [\n -95.350341796875,\n 43.600284023536325\n ],\n [\n -95.350341796875,\n 43.72744458647464\n ],\n [\n -95.78979492187499,\n 43.72744458647464\n ],\n [\n -95.78979492187499,\n 43.600284023536325\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schneider, R.J.","contributorId":97283,"corporation":false,"usgs":true,"family":"Schneider","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":816459,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220753,"text":"70220753 - 1962 - Paleozoic seas of central Idaho","interactions":[],"lastModifiedDate":"2021-05-26T12:04:10.351447","indexId":"70220753","displayToPublicDate":"1962-06-01T11:19:39","publicationYear":"1962","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":"Paleozoic seas of central Idaho","docAbstract":"Some recent paleogeographic maps indicate that central Idaho was part of a major geosyncline throughout Paleozoic time. This concept, apparently based on thick marine accumulations far apart on the margins of the region, is inconsistent with field data. Within the area of the Idaho batholith, Permian(?) volcanic rocks rest either on batholithic rocks or on the Belt Series. The Belt Series rocks have furnished the xenoliths in the batholith. To the west upper Paleozoic and Mesozoic strata are invaded. Along the eastern margin, south of lat. 45°, thick Paleozoic strata are intruded by the batholith. These locally exceed 30,000 feet in thickness and thin eastward. They have many variations. Those close to the batholith, especially those high in the sequence, are regarded as of near-shore origin. The Paleozoic strata in southeastern Idaho, more than 17,000 feet thick, are broadly similar except that Cambrian strata there are thicker and more widespread. The part of central Idaho north of the vicinity of lat. 45° has no known Paleozoic strata. Northern Idaho has only a few outcrops of beds of Cambrian age. The differences in thickness and character between Paleozoic strata in south-central and southeastern Idaho and those in western Montana and Wyoming (less than 7500 feet thick) suggest a hinge line near the eastern boundary between Idaho and Montana with a shelf to the east and a trough to the west. In south-central Idaho this trough had a maximum width of 90 miles and a western shore roughly at the east margin of the batholith. This trough wedged out northward a little beyond lat. 45°. Thus the area of the present Idaho batholith has been a positive block since Precambrian time, comparable to but apparently of longer duration than the geanticline in northern Nevada. Any invasion of the positive block in Idaho by marine waters during the Paleozoic was local and brief, except perhaps along the western border. Uncertain correlations within the area of the batholith leave open the possibility of some deposition there early in Paleozoic time.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[769:PSOCI]2.0.CO;2","usgsCitation":"Ross, C.P., 1962, Paleozoic seas of central Idaho: Geological Society of America Bulletin, v. 73, no. 6, p. 769-793, https://doi.org/10.1130/0016-7606(1962)73[769:PSOCI]2.0.CO;2.","productDescription":"25 p.","startPage":"769","endPage":"793","costCenters":[],"links":[{"id":385940,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"western-central Idaho","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.24609374999999,\n 43.26120612479979\n ],\n [\n -114.5654296875,\n 43.26120612479979\n ],\n [\n -114.5654296875,\n 45.398449976304086\n ],\n [\n -117.24609374999999,\n 45.398449976304086\n ],\n [\n -117.24609374999999,\n 43.26120612479979\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ross, Clyde P.","contributorId":10473,"corporation":false,"usgs":true,"family":"Ross","given":"Clyde","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":816449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000378,"text":"1000378 - 1962 - Temperature correction in conductivity measurements","interactions":[],"lastModifiedDate":"2025-05-01T15:42:14.299821","indexId":"1000378","displayToPublicDate":"1962-04-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Temperature correction in conductivity measurements","docAbstract":"Electrical conductivity has been widely used in freshwater research but usual methods employed by limnologists for converting measurements to conductance at a given temperature have not given uniformly accurate results. The temperature coefficient used to adjust conductivity of natural waters to a given temperature varies depending on the kinds and concentrations of electrolytes, the temperature at the time of measurement, and the temperature to which measurements are being adjusted. The temperature coefficient was found to differ for various lake and stream waters, and showed seasonal changes. High precision can be obtained only by determining temperature coefficients for each water studied. Mean temperature coefficients are given for various temperature ranges that may be used where less precision is required.","language":"English","publisher":"Association for the Sciences of Limnology and Oceanography","doi":"10.4319/lo.1962.7.3.0330","usgsCitation":"Smith, S.H., 1962, Temperature correction in conductivity measurements: Limnology and Oceanography, v. 7, no. 3, p. 330-334, https://doi.org/10.4319/lo.1962.7.3.0330.","productDescription":"5 p.","startPage":"330","endPage":"334","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":486857,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lo.1962.7.3.0330","text":"Publisher Index Page"},{"id":133095,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"3","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685741","contributors":{"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308482,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010570,"text":"70010570 - 1962 - Glass electrodes sensitive to divalent cations","interactions":[],"lastModifiedDate":"2026-02-25T16:37:12.820953","indexId":"70010570","displayToPublicDate":"1962-03-23T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Glass electrodes sensitive to divalent cations","docAbstract":"Glass electrodes suitable for measurement of divalent cations have been made and tested. Empirical and theoretical electrode equations have been presented to describe electrode behavior in a variety of aqueous solutions. Most electrodes show response interpretable as showing nearly ideal solid-solution behavior of the cations in the glass surface. The electrodes should be useful in the measurement of divalent-cation activities in natural waters and biological fluids, and useful in general analytical chemistry.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.135.3508.1045","issn":"00368075","usgsCitation":"Garrels, R., Sato, M., Thompson, M., and Truesdell, A., 1962, Glass electrodes sensitive to divalent cations: Ion exchange models for new electrode glasses simplify analyses for calcium and other ions: Science, v. 135, no. 3508, p. 1045-1048.","productDescription":"4 p.","startPage":"1045","endPage":"1048","costCenters":[],"links":[{"id":218972,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"135","issue":"3508","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2929e4b0c8380cd5a6f7","contributors":{"authors":[{"text":"Garrels, R.M.","contributorId":88804,"corporation":false,"usgs":true,"family":"Garrels","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":359195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sato, M.","contributorId":50201,"corporation":false,"usgs":true,"family":"Sato","given":"M.","email":"","affiliations":[],"preferred":false,"id":359193,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, M.E.","contributorId":98794,"corporation":false,"usgs":true,"family":"Thompson","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":359196,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address: TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":359194,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70010568,"text":"70010568 - 1962 - Hydrology","interactions":[],"lastModifiedDate":"2026-02-25T16:58:59.570241","indexId":"70010568","displayToPublicDate":"1962-03-02T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology","docAbstract":"An understanding of water in relation to earth processes requires the collaboration of many disciplines.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.135.3505.699","issn":"00368075","usgsCitation":"Hendricks, E.L., 1962, Hydrology: Science, v. 135, no. 3505, p. 699-705.","productDescription":"7 p.","startPage":"699","endPage":"705","costCenters":[],"links":[{"id":218970,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"135","issue":"3505","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a36b2e4b0c8380cd6091d","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171277,"text":"70171277 - 1962 - Valve position indicator for P-46 sampler","interactions":[],"lastModifiedDate":"2018-04-02T10:32:32","indexId":"70171277","displayToPublicDate":"1962-02-01T11:45:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"Valve position indicator for P-46 sampler","docAbstract":"No abstract available.
","language":"English","publisher":"American Water Resources Association","publisherLocation":"Herndon, VA","usgsCitation":"Scott, C., and Skinner, J.V., 1962, Valve position indicator for P-46 sampler: Water Resources Bulletin, v. February, p. 9-10.","productDescription":"2 p.","startPage":"9","endPage":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321725,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"February","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57481e3ee4b07e28b664dc1d","contributors":{"authors":[{"text":"Scott, C.H.","contributorId":101634,"corporation":false,"usgs":true,"family":"Scott","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":630418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skinner, J. V.","contributorId":32504,"corporation":false,"usgs":true,"family":"Skinner","given":"J.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":630419,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70176600,"text":"70176600 - 1962 - Phenol contamination of an artesian aquifer at Alma, Michigan, 1962","interactions":[],"lastModifiedDate":"2016-09-22T14:14:24","indexId":"70176600","displayToPublicDate":"1962-01-30T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5209,"text":"Proceedings of the Society for Water Treatment and Examination","active":true,"publicationSubtype":{"id":10}},"title":"Phenol contamination of an artesian aquifer at Alma, Michigan, 1962","docAbstract":"No abstract available.
","language":"English","publisher":"Society for Water Treatment and Examination","publisherLocation":"Sutton, England","usgsCitation":"Deutsch, M., 1962, Phenol contamination of an artesian aquifer at Alma, Michigan, 1962: Proceedings of the Society for Water Treatment and Examination, v. 11, p. 94-100.","startPage":"94","endPage":"100","numberOfPages":"7","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":328867,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","city":"Alma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.72656249999999,\n 43.33791397478761\n ],\n [\n -84.72656249999999,\n 43.415522593099915\n ],\n [\n -84.60090637207031,\n 43.415522593099915\n ],\n [\n -84.60090637207031,\n 43.33791397478761\n ],\n [\n -84.72656249999999,\n 43.33791397478761\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcff4e4b0824b2d17619c","contributors":{"authors":[{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":649338,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37556,"text":"37556 - 1962 - Waterfowl status report, 1962","interactions":[],"lastModifiedDate":"2014-07-15T14:30:01","indexId":"37556","displayToPublicDate":"1962-01-01T14:29:12","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"68","title":"Waterfowl status report, 1962","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Govt. Print. Off.","publisherLocation":"Washington, D.C.","usgsCitation":"Hansen, H., 1962, Waterfowl status report, 1962 (Revises and updates Special Scientific Report-Wildlife 61 (1961)): Special Scientific Report - Wildlife 68, iv, 127 p.","productDescription":"iv, 127 p.","numberOfPages":"131","costCenters":[],"links":[{"id":290180,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises and updates Special Scientific Report-Wildlife 61 (1961)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64deae4b0001bd51477d6","contributors":{"authors":[{"text":"Hansen, Henry A.","contributorId":15533,"corporation":false,"usgs":true,"family":"Hansen","given":"Henry A.","affiliations":[],"preferred":false,"id":218252,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70170554,"text":"70170554 - 1962 - Instructions for US P-61-A1 suspended-sediment sampler","interactions":[],"lastModifiedDate":"2018-03-05T12:28:54","indexId":"70170554","displayToPublicDate":"1962-01-01T13:45:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":66,"text":"Report","active":false,"publicationSubtype":{"id":1}},"title":"Instructions for US P-61-A1 suspended-sediment sampler","docAbstract":"No abstract available.
","language":"English","publisher":"Federal Interagency Sedimentation Project","publisherLocation":"Vickburg, MS","usgsCitation":"Colby, V., and Witzgman, F., 1962, Instructions for US P-61-A1 suspended-sediment sampler: Report, 9 p.","productDescription":"9 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":320513,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571f3fbee4b071321fe56a42","contributors":{"authors":[{"text":"Colby, V.C.","contributorId":168886,"corporation":false,"usgs":false,"family":"Colby","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":627601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witzgman, F.W.","contributorId":168892,"corporation":false,"usgs":false,"family":"Witzgman","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":627602,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70114641,"text":"70114641 - 1962 - Records of wells and ground-water quality in Burlington County, New Jersey","interactions":[],"lastModifiedDate":"2014-07-15T14:06:04","indexId":"70114641","displayToPublicDate":"1962-01-01T13:09:22","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"title":"Records of wells and ground-water quality in Burlington County, New Jersey","docAbstract":"The data in the following tables were abstracted from measurements of physical properties of evaporite minerals or of equivalent synthetic compounds. The compounds considered are the halide and sulfate salts which supposedly precipitated from evaporating ocean water and which form very extensive and thick \"rock salt\" beds. These beds are composed almost entirely of NaCl. In places where the beds are deeply buried and where fractures occur in the overlying rocks, the salt is plastically extruded upward as in a pipe to form the \"salt domes\".
\n\nMost of the tables are for NaCl, both the natural (halite) and the synthetic salt, polycrystalline and single crystals. These measurements have been collected for use 1) in studies on storage of radioactive wastes in salt domes or beds, 2) in calculations concerned with nuclear tests in salt domes and beds, and 3) in studies of phenomena in salt of geologic interest.
\n\nRather than an exhaustive compilation of physical property measurements, there tables represent a summary of data from accessible sources. As limitations of time have presented making a more systematic and comprehensive selection, the data given may seem arbitrarily chosen. Some of the data listed are old, and newer, more accurate data are undoubtedly available.
\nHalite (an synthetic NaCl) has been very thoroughly studied because of its relatively simple and highly symmetrical crystal structure, its easy availability naturally or synthetically, both in single crystals and polycrystalline, its useful and scientifically interesting properties, and its role as a compound of almost purely ionic bonding. The measurements of NaCl in the tables, however, represent only a small part of the total number of observations; discrimination was necessary to keep the size of the tabulations manageable. The physical properties of the evaporite minerals other than halite and sylvite have received only desultory attention of experiementalists, and appear in only a few tables.
\nThe effects of temperature, hydrostatic pressure, stress difference, and other mechanical, eletrical, and optical conditions on the physical properties have probably been observed more completely on NaCl than on any other solid substance, which makes it a unique and important substance. Several new and important phenomena have been observed first on it. The mechanical properties of NaCl, for example, depend very strongly on the condition and the composition of the gas or liquid in contact with the sample surface; the data are sparse as yet and are not reported here.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei821","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Robertson, E.C., 1962, Physical properties of evaporite minerals: U.S. Geological Survey Trace Elements Investigations 821, 90 p., https://doi.org/10.3133/tei821.","productDescription":"90 p.","numberOfPages":"90","costCenters":[],"links":[{"id":288266,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288265,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0821/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5385b3fbe4b09e18fc023a7b","contributors":{"authors":[{"text":"Robertson, Eugene C.","contributorId":71139,"corporation":false,"usgs":true,"family":"Robertson","given":"Eugene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":284738,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220665,"text":"70220665 - 1962 - Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah","interactions":[],"lastModifiedDate":"2021-05-24T13:58:30.40077","indexId":"70220665","displayToPublicDate":"1962-01-01T08:53:59","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah","docAbstract":"Uranium-vanadium deposits in the Salt Wash Member of the Morrison Formation in Montezuma Canyon, San Juan County, Utah, exhibit zoning that is interpreted as a result of metal transport by diffusion. The concentric zones consist of a brown nonmineralized core, an olive-gray mineralized shell, and a gray nonmineralized outer zone. The brown zone is iron-stained, porous sandstone commonly containing abundant carbonaceous material. The curved mineralized layer completely encloses the brown zone, and is composed of oxidized uranium-vanadium minerals that impregnate sandstone. The gray zone is light-gray sandstone tightly cemented with calcite and commonly freckled with limonitic specks.Formation of the deposits most likely took place during Late Cretaceous or early Tertiary time when the ore-bearing sandstones were deeply buried and saturated with connate waters. The concentration of organic material in the brown zone suggests that this zone was once saturated with a reducing solution containing soluble organic compounds like alcohols and aldehydes derived from the organic material. The gray zone, on the other hand, was probably saturated with an oxidizing solution containing uranium and vanadium. Where these two solutions were in contact, oxidation-reduction reactions took place that caused the precipitation of low-valent uranium and vanadium minerals.The ellipsoidal shape of the ore layer and the lack of any exit or entrance for flowing solutions indicates that the dissolved metals moved through the gray zone by diffusion and were precipitated at the periphery of the reducing zone. Recent weathering and oxidation have altered the primary low-valent minerals to high-valent forms without noticeable leaching of the ore metals.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.57.2.226","usgsCitation":"Huff, L., and Lesure, F., 1962, Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah: Economic Geology, v. 57, no. 2, p. 226-237, https://doi.org/10.2113/gsecongeo.57.2.226.","productDescription":"12 p.","startPage":"226","endPage":"237","costCenters":[],"links":[{"id":385897,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Montezuma Canyon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.654541015625,\n 37.02886944696474\n ],\n [\n -109.061279296875,\n 37.02886944696474\n ],\n [\n -109.061279296875,\n 38.53957267203905\n ],\n [\n -109.654541015625,\n 38.53957267203905\n ],\n [\n -109.654541015625,\n 37.02886944696474\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"57","issue":"2","noUsgsAuthors":false,"publicationDate":"1962-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Huff, L.C.","contributorId":32919,"corporation":false,"usgs":true,"family":"Huff","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":816355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lesure, F. G.","contributorId":7694,"corporation":false,"usgs":true,"family":"Lesure","given":"F. G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":816356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185558,"text":"70185558 - 1962 - Rivers","interactions":[],"lastModifiedDate":"2017-03-23T16:17:35","indexId":"70185558","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":743,"text":"American Scientist","active":true,"publicationSubtype":{"id":10}},"title":"Rivers","docAbstract":"Rivers are both the means and the routes by which the products of continental weathering are carried to the oceans of the world. Except in the most arid areas more water falls as precipitation than is lost by evaporation and transpiration from the land surface to the atmosphere. Thus there is an excess of water, which must flow to the ocean. Rivers, then, are the routes by which this excess water flows to the ultimate base level. The excess of precipitation over evaporation and transpiration provides the flow of rivers and springs, recharges ground-water storage, and is the supply from which man draws water for his needs.
","language":"English","publisher":"Sigma Xi, The Scientific Research Society","usgsCitation":"Leopold, L.B., 1962, Rivers: American Scientist, v. 50, no. 4, p. 511-537.","productDescription":"27 p.","startPage":"511","endPage":"537","costCenters":[],"links":[{"id":338231,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338230,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.americanscientist.org/issues/past.aspx","text":"Journal's Website"}],"volume":"50","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d4df19e4b05ec79911d20b","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":685951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70195893,"text":"70195893 - 1962 - Artesian water from glacial drift near Lehr, Logan and McIntosh Counties, North Dakota","interactions":[],"lastModifiedDate":"2018-03-08T09:28:58","indexId":"70195893","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5646,"text":"North Dakota Ground Water Studies","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"38","title":"Artesian water from glacial drift near Lehr, Logan and McIntosh Counties, North Dakota","docAbstract":"No abstract available.
","language":"English","publisher":"North Dakota State Water Conservation Commission","usgsCitation":"Adolphson, D.G., 1962, Artesian water from glacial drift near Lehr, Logan and McIntosh Counties, North Dakota: North Dakota Ground Water Studies 38, 22 p.","productDescription":"22 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352287,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6345e4b0da30c1bfdf0a","contributors":{"authors":[{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":730411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171159,"text":"70171159 - 1962 - Microorganic constituents of water of the Great Lakes","interactions":[],"lastModifiedDate":"2017-11-14T10:16:23","indexId":"70171159","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Microorganic constituents of water of the Great Lakes","docAbstract":"No abstract available.
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","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Garza, S., 1962, Chemical analysis of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas: Edwards Underground Water District Bulletin 1, 56 p.","productDescription":"56 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326718,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ac0e4b03bcb0104bb6e","contributors":{"authors":[{"text":"Garza, Sergio","contributorId":88713,"corporation":false,"usgs":true,"family":"Garza","given":"Sergio","email":"","affiliations":[],"preferred":false,"id":645896,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70185611,"text":"70185611 - 1962 - The Vigil Network","interactions":[],"lastModifiedDate":"2017-03-24T14:24:10","indexId":"70185611","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"The Vigil Network","docAbstract":"Those of us who seek to explain the variations in hydrologic phenomena such as may be observed in the occurrence of floods or in changes in the shape of river channels are painfully aware of the lack of adequate data. Our existing data, collected mainly to serve immediate practical needs for water-resources development, usually are deficient in providing information useful for many kinds of scientific inquiry. Hydrologic records are usually obtained on streams that are highly regulated or otherwise put to use, to the neglect of headwater streams better suited to studies of the details of hydrologic processes.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666209493250","usgsCitation":"Leopold, L.B., 1962, The Vigil Network: International Association of Scientific Hydrology - Bulletin , v. 7, no. 2, p. 5-9, https://doi.org/10.1080/02626666209493250.","productDescription":"5 p.","startPage":"5","endPage":"9","costCenters":[],"links":[{"id":338317,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d6304ce4b05ec799131147","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}