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Edward Huntington","contributorId":13629,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward","email":"","middleInitial":"Huntington","affiliations":[],"preferred":false,"id":167203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23313,"text":"ofr69122 - 1969 - Floods in Gravois Creek Basin, St. Louis County, Missouri","interactions":[],"lastModifiedDate":"2025-08-13T19:42:45.419348","indexId":"ofr69122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-122","title":"Floods in Gravois Creek Basin, St. Louis County, Missouri","docAbstract":"

The rapid growth of suburban St. Louis presents problems in the social and economic development of flood plains within the area. The U.S. Geological Survey, in cooperation with the Metropolitan St. Louis Sewer District, is conducting a study of the hydrology of five major drainage basins within the area of responsibility of the Sewer District.

This interim report presents stage and inundation data along Gravois Creek and its tributaries for the historic flood of June 1957, and the flood of January 1969. These data can be useful in studies leading to the proper utilization of the basin to minimize future flood problems. Other useful hydrologic data such as flood discharges and frequencies are being gathered, but were not available for this report.

Spencer and Hauth (1969) described the flood situation in Maline Creek basin, St. Louis County, Mo. Areas covered by both reports are shown in figure 1.

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This compilation briefly describes the objectives and purpose of a reconnaissance geochemical survey of Missouri, the results of the survey for the first 6 months, and the expenditures in funds and personnel for the present fiscal year and, as anticipated, for the fiscal year beginning on July 1, 1970. It is prepared primarily for the information of the Environmental Health Center of the University of Missouri in the interest of continuing communication at both the administrative and scientific levels.

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development","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir619","usgsCitation":"McKelvey, V., Tracey, J.I., Stoertz, G., and Vedder, J.G., 1969, Subsea mineral resources and problems related to their development: U.S. Geological Survey Circular 619, v, 26 p. :illus., maps. ;27 cm., https://doi.org/10.3133/cir619.","productDescription":"v, 26 p. :illus., maps. ;27 cm.","costCenters":[],"links":[{"id":30698,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0619/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121285,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0619/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b47","contributors":{"authors":[{"text":"McKelvey, V.E.","contributorId":85161,"corporation":false,"usgs":true,"family":"McKelvey","given":"V.E.","email":"","affiliations":[],"preferred":false,"id":147355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracey, J. I.","contributorId":35718,"corporation":false,"usgs":true,"family":"Tracey","given":"J.","middleInitial":"I.","affiliations":[],"preferred":false,"id":147353,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoertz, G.E.","contributorId":64230,"corporation":false,"usgs":true,"family":"Stoertz","given":"G.E.","affiliations":[],"preferred":false,"id":147354,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":147356,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":3726,"text":"cir620 - 1969 - Quantitative comparison of some aesthetic factors among rivers","interactions":[],"lastModifiedDate":"2017-03-29T10:55:17","indexId":"cir620","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"620","title":"Quantitative comparison of some aesthetic factors among rivers","docAbstract":"

It is difficult to evaluate the factors contributing to aesthetic or nonmonetary aspects of a landscape. In contrast, aspects which lend themselves to cost-benefit comparisons are now treated in a routine way. As a result, nonmonetary values are described either in emotion-loaded words or else are mentioned and thence forgotten.

The present report is a preliminary attempt to quantify some elements of aesthetic appeal while eliminating, insofar as possible, value judgments or personal preferences. If methods of recording such factors can be developed, the results promise to be a useful, new kind of basic data needed in many planning and decision-making circumstances. Such data would be especially useful when choices must be made among alternative courses of action. Such data would tend to provide a more prominent consideration of the nonmonetary aspects of a landscape.

Assignment of quantitative estimates to aesthetic factors leads not so much to ratios of value as to relative rank positions. In fact, value itself tends to carry a connotation of preference, whereas ranking can more easily be used for categorization without attribution of preference and thus it tends to a void the introduction at too early a stage of differences in preference.

Because the Federal Power Commission has been studying an application for a permit to construct one or more additional hydropower dams in the vicinity of Hells Canyon of the Snake River, the localities studied for the present discussion are in that region of Idaho. Hopefully, the data collected will provide some useful information on factors related to nonmonetary values in the region. 

The present discussion has been kept free of the preference judgments of the writer, and throughout the discussions observations are treated as facts.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir620","usgsCitation":"Leopold, L.B., 1969, Quantitative comparison of some aesthetic factors among rivers: U.S. Geological Survey Circular 620, iii, 16 p., https://doi.org/10.3133/cir620.","productDescription":"iii, 16 p.","numberOfPages":"22","costCenters":[],"links":[{"id":30787,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0620/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0620/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Hells Canyon, Snake River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.75,\n 45.75\n ],\n [\n -114.45,\n 45.75\n ],\n [\n -114.45,\n 43.7\n ],\n [\n -116.75,\n 43.7\n ],\n [\n -116.75,\n 45.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685eef","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":147490,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63453,"text":"gq821 - 1969 - Geologic map of the Buffalo Mountain quadrangle, Pershing and Churchill Counties, Nevada","interactions":[],"lastModifiedDate":"2018-06-19T17:06:05","indexId":"gq821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"821","title":"Geologic map of the Buffalo Mountain quadrangle, Pershing and Churchill Counties, Nevada","language":"ENGLISH","doi":"10.3133/gq821","usgsCitation":"Wallace, R.E., Silberling, N., Irwin, W., and Tatlock, D., 1969, Geologic map of the Buffalo Mountain quadrangle, Pershing and Churchill Counties, Nevada: U.S. Geological Survey Geologic Quadrangle 821, Map: 76.8 x 67.8 cm, https://doi.org/10.3133/gq821.","productDescription":"Map: 76.8 x 67.8 cm","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":249544,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0821/report.pdf","size":"30","linkFileType":{"id":1,"text":"pdf"}},{"id":103537,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2123.htm","linkFileType":{"id":5,"text":"html"},"description":"2123"},{"id":253109,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0821/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.25,40 ], [ -118.25,40.25 ], [ -118,40.25 ], [ -118,40 ], [ -118.25,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69d71c","contributors":{"authors":[{"text":"Wallace, R. E.","contributorId":6823,"corporation":false,"usgs":true,"family":"Wallace","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":268878,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silberling, N. J.","contributorId":34919,"corporation":false,"usgs":true,"family":"Silberling","given":"N. J.","affiliations":[],"preferred":false,"id":738410,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Irwin, W. P.","contributorId":82347,"corporation":false,"usgs":true,"family":"Irwin","given":"W. P.","affiliations":[],"preferred":false,"id":738411,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tatlock, D.B.","contributorId":22748,"corporation":false,"usgs":true,"family":"Tatlock","given":"D.B.","affiliations":[],"preferred":false,"id":738412,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":67381,"text":"i578 - 1969 - Geologic map of the Wheeler Peak and Garrison quadrangles, Nevada and Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i578","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"578","subseriesTitle":"NONE","title":"Geologic map of the Wheeler Peak and Garrison quadrangles, Nevada and Utah","language":"ENGLISH","doi":"10.3133/i578","usgsCitation":"Whitebread, D., 1969, Geologic map of the Wheeler Peak and Garrison quadrangles, Nevada and Utah: U.S. Geological Survey IMAP 578, 1 map :col. ;58 x 90 cm. on sheet 91 x 124 cm., https://doi.org/10.3133/i578.","productDescription":"1 map :col. ;58 x 90 cm. on sheet 91 x 124 cm.","costCenters":[],"links":[{"id":106847,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9363.htm","linkFileType":{"id":5,"text":"html"},"description":"9363"},{"id":188112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.5,38.75 ], [ -114.5,39 ], [ -114,39 ], [ -114,38.75 ], [ -114.5,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a07b","contributors":{"authors":[{"text":"Whitebread, D. H.","contributorId":96251,"corporation":false,"usgs":true,"family":"Whitebread","given":"D. H.","affiliations":[],"preferred":false,"id":276095,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68268,"text":"ha335 - 1969 - Water quality in the Delaware estuary for two years of drought: 1965 and 1966, from Trenton, New Jersey to Reedy Island, Delaware","interactions":[],"lastModifiedDate":"2022-12-29T21:42:52.735428","indexId":"ha335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"335","title":"Water quality in the Delaware estuary for two years of drought: 1965 and 1966, from Trenton, New Jersey to Reedy Island, Delaware","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha335","usgsCitation":"Keighton, W.B., 1969, Water quality in the Delaware estuary for two years of drought: 1965 and 1966, from Trenton, New Jersey to Reedy Island, Delaware: U.S. Geological Survey Hydrologic Atlas 335, 3 Plates: 41.96 x 34.00 inches, https://doi.org/10.3133/ha335.","productDescription":"3 Plates: 41.96 x 34.00 inches","costCenters":[],"links":[{"id":188552,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411200,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15710.htm","linkFileType":{"id":5,"text":"html"}},{"id":89673,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/335/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89672,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/335/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89671,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/335/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Delaware, New Jersey","city":"Trenton","otherGeospatial":"Reedy Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.77593070250738,\n 40.282957430960124\n ],\n [\n -75.67504000078515,\n 40.282957430960124\n ],\n [\n -75.67504000078515,\n 39.20262224433091\n ],\n [\n -74.77593070250738,\n 39.20262224433091\n ],\n [\n -74.77593070250738,\n 40.282957430960124\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9ab7","contributors":{"authors":[{"text":"Keighton, Walter B.","contributorId":81877,"corporation":false,"usgs":true,"family":"Keighton","given":"Walter","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":277938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35589,"text":"b1286 - 1969 - Gold Veins near Great Falls, Maryland","interactions":[],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"b1286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1286","title":"Gold Veins near Great Falls, Maryland","docAbstract":"Small deposits of native gold are present along an anastomosing system of quartz veins and shear zones just east of Great Falls, Montgomery County, Md. The deposits were discovered in 1861 and were worked sporadically until 1951, yielding more than 5,000 ounces of gold.\r\n\r\nThe vein system and the principal veins within it strike a few degrees west of north, at an appreciable angle to foliation and fold axial planes in enclosing rocks of the Wissahickon Formation of late Precambrian (?) age. The veins cut granitic rocks of Devonian or pre-Devonian age and may be as young as Triassic.\r\n\r\nFurther development of the deposits is unlikely under present economic conditions because of their generally low gold content and because much of the vein system lies on park property, but study of the Great Falls vein system may be useful in the search for similar deposits elsewhere in the Appalachian Piedmont.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/b1286","usgsCitation":"Reed, J.C., and Reed, J., 1969, Gold Veins near Great Falls, Maryland: U.S. Geological Survey Bulletin 1286, 22 p., https://doi.org/10.3133/b1286.","productDescription":"22 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":93394,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1286/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93395,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1286/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93396,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1286/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166177,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1286/report-thumb.jpg"},{"id":12477,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/bul/1286/index.htm","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.26666666666667,38.916666666666664 ], [ -77.26666666666667,39.083333333333336 ], [ -77.05,39.083333333333336 ], [ -77.05,38.916666666666664 ], [ -77.26666666666667,38.916666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a48f7","contributors":{"authors":[{"text":"Reed, John Calvin Jr.","contributorId":8460,"corporation":false,"usgs":true,"family":"Reed","given":"John","suffix":"Jr.","email":"","middleInitial":"Calvin","affiliations":[],"preferred":false,"id":214899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, John C. jreed@usgs.gov","contributorId":1259,"corporation":false,"usgs":true,"family":"Reed","given":"John C.","email":"jreed@usgs.gov","affiliations":[],"preferred":true,"id":214898,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68085,"text":"ha337 - 1969 - Ground-water favorability areas and surficial geology of the lower Kennebec River basin, Maine","interactions":[],"lastModifiedDate":"2022-04-13T18:35:50.587891","indexId":"ha337","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"337","title":"Ground-water favorability areas and surficial geology of the lower Kennebec River basin, Maine","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha337","usgsCitation":"Prescott, G., 1969, Ground-water favorability areas and surficial geology of the lower Kennebec River basin, Maine: U.S. Geological Survey Hydrologic Atlas 337, 2 Plates: 37.50 × 57.00 inches and 8.00 × 10.50 inches, https://doi.org/10.3133/ha337.","productDescription":"2 Plates: 37.50 × 57.00 inches and 8.00 × 10.50 inches","costCenters":[],"links":[{"id":189800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89346,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/337/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89345,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/337/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398652,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15712.htm"}],"scale":"62500","country":"United States","state":"Maine","otherGeospatial":"lower Kennebec River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.078,\n 43.929\n ],\n [\n -69.5,\n 43.929\n ],\n [\n -69.5,\n 44.674\n ],\n [\n -70.078,\n 44.674\n ],\n [\n -70.078,\n 43.929\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649777","contributors":{"authors":[{"text":"Prescott, Glenn C.","contributorId":38126,"corporation":false,"usgs":true,"family":"Prescott","given":"Glenn C.","affiliations":[],"preferred":false,"id":277617,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1078,"text":"wsp1859F - 1969 - Geohydrology and water utilization in the Willcox Basin, Graham and Cochise Counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1859F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"1859","chapter":"F","title":"Geohydrology and water utilization in the Willcox Basin, Graham and Cochise Counties, Arizona","docAbstract":"The Willcox basin is an area of interior drainage in the northern part of Sulphur Springs Valley, Cochise and Graham Counties, Ariz. The basin comprises about 1,500 square miles, of which the valley floor occupies about 950 square miles. \r\n\r\nThe basin probably formed during middle and late Tertiary time, when the area was subjected to large-scale faulting accompanied by the uplift of the mountain ranges that presently border it. During and after faulting, large quantities of alluvium were deposited in the closed basin. \r\n\r\nThe rocks in the basin are divided into two broad groups--the rocks of the mountain blocks, of Precambrian through Tertiary age, and the rocks of the basin, of Tertiary and Quaternary age. The mountain blocks consist of igneous, metamorphic, and sedimentary rocks; the water-bearing characteristics of these rocks depend primarily on their degree of weathering and fracturing. Even in areas where these rocks are fractured and jointed, only small amounts of water have been developed. The rocks of the basin consist of moderately consolidated alluvium, poorly consolidated alluvium, and unconsolidated alluvium. The water-bearing characteristics of the moderately and poorly consolidated alluvium are not well known. The unconsolidated alluvium underlies most of the valley floor and consists of two facies, stream deposits and lake beds associated with the old playa. The lenticular sand and gravel layers interbedded in silt- and clay-size material of the unconsolidated alluvium constitute the principal aquifer in the basin. The other aquifers, which yield less water, consist of beds of poorly to moderately consolidated sand- and gravel-size material; these beds occur in both the poorly consolidated and moderately consolidated alluvium. \r\n\r\nIn the Stewart area the median specific capacity of wells per 100 feet of saturated unconsolidated alluvium was 20 gallons per minute, and in the Kansas Settlement area the specific capacity of wells penetrating the poorly and moderately consolidated alluvium, undifferentiated, was only 7.4 gallons per minute per 100 feet of saturated material penetrated. The aquifer in the Kansas Settlement area is much less permeable but more homogeneous than the aquifer in the Stewart area. The coefficient of transmissibility of the aquifers, which was estimated from the specific-capacity data, ranged from 58,000 to 160,000 gal. tons per day per foot. \r\n\r\nPrior to extensive ground-water pumpage, the ground-water system probably was in equilibrium, with discharge equaling recharge. At that time, ground water moved toward the playa, where it was discharged by transpiration and evaporation. The estimate of the evapotranspiration in the playa area before large-scale development was about 75,000 acre-feet per year. On the basis of estimates of coefficients of transmissibility of the aquifer and on the basis of the water-table configuration, underflow toward the playa was computed to be about 54,000 acre-feet per year. \r\n\r\nBy 1963, large-scale pumping had caused marked changes in the shape of the piezometric surface; large cones of depression had developed, and ground-water movement was toward the centers of pumping. The cones of depression caused by large-scale pumping have since expanded, and water-level declines have been measured in the recharge areas along the mountain fronts. \r\n\r\nGround water has been used for irrigation since 1910. In 1928, about 4,000 acre-feet of ground water was pumped, and by 1963 180,000 acre-feet per year was being pumped. An estimated 1,860,000 acre-feet of water has been pumped for irrigation in the Willcox basin through 1963; 680,000 acre-feet from the Stewart area, 990,000 acre-feet from the Kansas Settlement area, and 190,000 acre-feet from the Pearce-Cochise area. In the Sierra Bonita Ranch area and the north playa area, ground-water withdrawal for irrigation through 1963 was small. From the spring of 1952 to the spring of 1964 water-level declines resulting from the ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1859F","usgsCitation":"Brown, S., and Schumann, H.H., 1969, Geohydrology and water utilization in the Willcox Basin, Graham and Cochise Counties, Arizona: U.S. Geological Survey Water Supply Paper 1859, 32 p. :maps (3 fold. in pocket), https://doi.org/10.3133/wsp1859F.","productDescription":"32 p. :maps (3 fold. in pocket)","costCenters":[],"links":[{"id":138054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1859f/report-thumb.jpg"},{"id":25785,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1859f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25786,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1859f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25787,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1859f/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25788,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1859f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b50","contributors":{"authors":[{"text":"Brown, S. G.","contributorId":46914,"corporation":false,"usgs":true,"family":"Brown","given":"S. G.","affiliations":[],"preferred":false,"id":143141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schumann, Herbert H.","contributorId":30964,"corporation":false,"usgs":true,"family":"Schumann","given":"Herbert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143140,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3780,"text":"cir612 - 1969 - Gold in minerals and the composition of native gold","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"cir612","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"612","title":"Gold in minerals and the composition of native gold","docAbstract":"Gold occurs in nature mainly as the metal and as various alloys. It forms complete series of solid solutions with silver, copper, nickel, palladium, and platinum. In association with the platinum metals, gold occurs as free gold as well as in solid solution. \r\n\r\nThe native elements contain the most gold, followed by the sulfide minerals. Several gold tellurides are known, but no gold selenides have been reported, and only one sulfide, the telluride-sulfide mineral nagyagite, is known. \r\n\r\nThe nonmetallic minerals carry the least gold, and the light-colored minerals generally contain less gold than the dark minerals. \r\n\r\nSome conclusions in the literature are conflicting in regard to the relation of fineness of native gold to its position laterally and vertically within a lode, the nature of the country rocks, and the location and size of nuggets in a streambed, as well as to the variation of fineness within an individual nugget.","language":"ENGLISH","publisher":"[U.S. Dept. of the Interior, Geological Survey],","doi":"10.3133/cir612","usgsCitation":"Jones, R.S., and Fleischer, M., 1969, Gold in minerals and the composition of native gold: U.S. Geological Survey Circular 612, 17 p. ;26 cm., https://doi.org/10.3133/cir612.","productDescription":"17 p. ;26 cm.","costCenters":[],"links":[{"id":117870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0612/report-thumb.jpg"},{"id":30851,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0612/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674115","contributors":{"authors":[{"text":"Jones, Robert Sprague","contributorId":41814,"corporation":false,"usgs":true,"family":"Jones","given":"Robert","email":"","middleInitial":"Sprague","affiliations":[],"preferred":false,"id":147586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleischer, Michael","contributorId":65835,"corporation":false,"usgs":true,"family":"Fleischer","given":"Michael","email":"","affiliations":[],"preferred":false,"id":147587,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4919,"text":"pp606 - 1969 - Revision of some of Girty's invertebrate fossils from the Fayetteville Shale (Mississippian) of Arkansas and Oklahoma","interactions":[],"lastModifiedDate":"2015-10-21T10:16:21","indexId":"pp606","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"606","title":"Revision of some of Girty's invertebrate fossils from the Fayetteville Shale (Mississippian) of Arkansas and Oklahoma","docAbstract":"

J.n 1910, G. H. Girty published a paper on the fauna of the Fayetteville Shale of northern Arkansas and northeastern Oklahoma in which he described 110 new taxa of fossil invertebrates. He did not, however, designate any type specimens or divulge the localities at which •the fossils were collected, nor did he illustrate the species. The present study is designed to fill the gaps in information on some of these species and to bring them as far as possible up to date and in line with the modern scheme of classification.

\n

This report deals with the corals, pelecypods, _gastropods, trilobites, and ostracodes. It does not include the brachiopods and bryozoans. The study has been performed by specialists of the U.S. Geological Survey who are contributing separate parts to the volume.

\n

 

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp606","usgsCitation":"Gordon, M., Sando, W.J., Pojeta, J., Yochelson, E.L., and Sohn, I.G., 1969, Revision of some of Girty's invertebrate fossils from the Fayetteville Shale (Mississippian) of Arkansas and Oklahoma: U.S. Geological Survey Professional Paper 606, iii, 59 p.; 8 Plates; 1 Map: 21.62 x 12.87 inches, https://doi.org/10.3133/pp606.","productDescription":"iii, 59 p.; 8 Plates; 1 Map: 21.62 x 12.87 inches","numberOfPages":"94","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":251792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0606/report-thumb.jpg"},{"id":247317,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0606/report.pdf","size":"9886","linkFileType":{"id":1,"text":"pdf"}},{"id":310255,"rank":301,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0606/plate-9.pdf","text":"Plate 9","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas, Oklahoma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.1630859375,\n 35.65729624809628\n ],\n [\n -97.1630859375,\n 37.00255267215955\n ],\n [\n -92.6806640625,\n 37.00255267215955\n ],\n [\n -92.6806640625,\n 35.65729624809628\n ],\n [\n -97.1630859375,\n 35.65729624809628\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602b54","contributors":{"authors":[{"text":"Gordon, Mackenzie Jr.","contributorId":13225,"corporation":false,"usgs":true,"family":"Gordon","given":"Mackenzie","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":576292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sando, William J.","contributorId":47851,"corporation":false,"usgs":true,"family":"Sando","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":576293,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pojeta, John Jr.","contributorId":44514,"corporation":false,"usgs":true,"family":"Pojeta","given":"John","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":576294,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yochelson, Ellis L.","contributorId":90802,"corporation":false,"usgs":true,"family":"Yochelson","given":"Ellis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":576295,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sohn, I. G.","contributorId":70751,"corporation":false,"usgs":true,"family":"Sohn","given":"I.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":576296,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":3824,"text":"cir617 - 1969 - Results of geological and geochemical investigations in an area northwest of the Chulitna River, central Alaska Range","interactions":[],"lastModifiedDate":"2017-06-25T13:03:47","indexId":"cir617","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"617","title":"Results of geological and geochemical investigations in an area northwest of the Chulitna River, central Alaska Range","docAbstract":"Sedimentary and volcanic rock units of Paleozoic and Mesozoic age, faults, and elongate bodies of intrusive rock, particularly serpentinites, have a dominant northeasterly trend in an area northwest of the Chulitna River between Eldridge Glacier and Bull River. The serpentinites locally contain abnormal (as much as 0.5 percent) concentrations of nickel, have one newly identified occurrence of chromite, and are hosts to small epigenetic lodes containing copper, gold, and silver. Other epigenetic concentrations of copper or other metals occur in interlayered basalt and limestone at Partin and Canyon Creeks in the southwestern part of the area and in porphyry near Costello Creek in the northern part of the area. Tin occurs in greisen on upper Ohio Creek, and abnormal concentrations of tin also characterize mineralized rocks along Canyon Creek and at a prospect near Long Creek. Mineralized rocks characterized by silver, lead, and zinc crop out near Lookout Mountain. \r\n\r\nAnomalous concentrations of gold and other metals occur in stream sediments at isolated sites in upper Long Creek and at Coal Creek, as well as in several areas near known lode mineral occurrences. Shotgun and McCallie Creeks both contain stream sediments with anomalous concentrations of metals and both head into the basalt-limestone unit which is the host rock at Partin and Canyon Creeks; these facts suggest that other concentrations may be found.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir617","usgsCitation":"Hawley, C.C., Clark, A.L., Herdrick, M., and Clark, S.H., 1969, Results of geological and geochemical investigations in an area northwest of the Chulitna River, central Alaska Range: U.S. Geological Survey Circular 617, iii, 19 p. :maps. ;27 cm., https://doi.org/10.3133/cir617.","productDescription":"iii, 19 p. :maps. ;27 cm.","costCenters":[],"links":[{"id":30893,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0617/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0617/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db60635f","contributors":{"authors":[{"text":"Hawley, C. C.","contributorId":102070,"corporation":false,"usgs":true,"family":"Hawley","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":147681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, A. L.","contributorId":89502,"corporation":false,"usgs":true,"family":"Clark","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147679,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Herdrick, M.A.","contributorId":33307,"corporation":false,"usgs":true,"family":"Herdrick","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":147678,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clark, S. H. B.","contributorId":95052,"corporation":false,"usgs":true,"family":"Clark","given":"S.","email":"","middleInitial":"H. B.","affiliations":[],"preferred":false,"id":147680,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":63933,"text":"gp674 - 1969 - Aeromagnetic map of the Framingham quadrangle, Middlesex and Worcester Counties, Massachusetts","interactions":[],"lastModifiedDate":"2025-06-20T19:45:27.871777","indexId":"gp674","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"674","title":"Aeromagnetic map of the Framingham quadrangle, Middlesex and Worcester Counties, Massachusetts","docAbstract":"

No abstract available.

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No abstract available.

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