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No abstract available.

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No abstract available.

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1969 - Bedrock geologic map of the Blue Hills quadrangle, Norfolk, Suffolk, and Plymouth Counties, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq796","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":"796","title":"Bedrock geologic map of the Blue Hills quadrangle, Norfolk, Suffolk, and Plymouth Counties, Massachusetts","language":"ENGLISH","doi":"10.3133/gq796","usgsCitation":"Chute, N.E., 1969, Bedrock geologic map of the Blue Hills quadrangle, Norfolk, Suffolk, and Plymouth Counties, Massachusetts: U.S. Geological Survey Geologic Quadrangle 796, 1 map., https://doi.org/10.3133/gq796.","productDescription":"1 map.","costCenters":[],"links":[{"id":103512,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2098.htm","linkFileType":{"id":5,"text":"html"},"description":"2098"},{"id":249341,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0796/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0796/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.11749999999999,42.1175 ], [ -71.11749999999999,42.25 ], [ -71,42.25 ], [ -71,42.1175 ], [ -71.11749999999999,42.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db6363bd","contributors":{"authors":[{"text":"Chute, Newton Earl","contributorId":97119,"corporation":false,"usgs":true,"family":"Chute","given":"Newton","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":268517,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63151,"text":"gq835 - 1969 - Geologic map of the Mellen Hill quadrangle, Rio Blanco and Moffat Counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:43","indexId":"gq835","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":"835","title":"Geologic map of the Mellen Hill quadrangle, Rio Blanco and Moffat Counties, Colorado","language":"ENGLISH","doi":"10.3133/gq835","usgsCitation":"Cullins, H.L., 1969, Geologic map of the Mellen Hill quadrangle, Rio Blanco and Moffat Counties, Colorado: U.S. Geological Survey Geologic Quadrangle 835, 1 map :col. ;58 x 44 cm., on sheet 84 x 101 cm., folded to 28 x 21 cm., in envelope 30 x 24 cm., https://doi.org/10.3133/gq835.","productDescription":"1 map :col. ;58 x 44 cm., on sheet 84 x 101 cm., folded to 28 x 21 cm., in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":103551,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2137.htm","linkFileType":{"id":5,"text":"html"},"description":"2137"},{"id":180392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89041,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gq/0835/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109,40.1175 ], [ -109,40.25 ], [ -108.86749999999999,40.25 ], [ -108.86749999999999,40.1175 ], [ -109,40.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696a3f","contributors":{"authors":[{"text":"Cullins, Henry L.","contributorId":23149,"corporation":false,"usgs":true,"family":"Cullins","given":"Henry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":268411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65231,"text":"i576 - 1969 - Bedrock geologic map of the Marenisco-Watersmeet area, Gogebic and Ontonagon Counties, Michigan","interactions":[],"lastModifiedDate":"2012-02-10T00:11:07","indexId":"i576","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":"576","subseriesTitle":"NONE","title":"Bedrock geologic map of the Marenisco-Watersmeet area, Gogebic and Ontonagon Counties, Michigan","language":"ENGLISH","doi":"10.3133/i576","usgsCitation":"Fritts, C., 1969, Bedrock geologic map of the Marenisco-Watersmeet area, Gogebic and Ontonagon Counties, Michigan: U.S. Geological Survey IMAP 576, 1 map :col. ;58 x 120 cm. folded in envelope 30 x 24 cm. +1 text., https://doi.org/10.3133/i576.","productDescription":"1 map :col. ;58 x 120 cm. folded in envelope 30 x 24 cm. +1 text.","costCenters":[],"links":[{"id":106845,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9361.htm","linkFileType":{"id":5,"text":"html"},"description":"9361"},{"id":255362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0576/report.pdf","size":"600","linkFileType":{"id":1,"text":"pdf"}},{"id":255363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0576/report-thumb.jpg"}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.75,46.25 ], [ -89.75,46.5 ], [ -89,46.5 ], [ -89,46.25 ], [ -89.75,46.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db63635f","contributors":{"authors":[{"text":"Fritts, C.E.","contributorId":47450,"corporation":false,"usgs":true,"family":"Fritts","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":272881,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66678,"text":"i580 - 1969 - Geologic map of the Mackay quadrangle, south-central Idaho","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"i580","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":"580","subseriesTitle":"NONE","title":"Geologic map of the Mackay quadrangle, south-central Idaho","language":"ENGLISH","doi":"10.3133/i580","usgsCitation":"Nelson, W.H., and Ross, C.P., 1969, Geologic map of the Mackay quadrangle, south-central Idaho: U.S. Geological Survey IMAP 580, 1 map :col. ;45 x 33 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i580.","productDescription":"1 map :col. ;45 x 33 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106849,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9365.htm","linkFileType":{"id":5,"text":"html"},"description":"9365"},{"id":188647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,43.5 ], [ -114,44 ], [ -113.5,44 ], [ -113.5,43.5 ], [ -114,43.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d02","contributors":{"authors":[{"text":"Nelson, W. H.","contributorId":100336,"corporation":false,"usgs":true,"family":"Nelson","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":274904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, C. P.","contributorId":91545,"corporation":false,"usgs":true,"family":"Ross","given":"C.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":274903,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":62955,"text":"gq815 - 1969 - Geologic map of the Equality quadrangle, western Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq815","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":"815","title":"Geologic map of the Equality quadrangle, western Kentucky","language":"ENGLISH","doi":"10.3133/gq815","usgsCitation":"Goudarzi, G.H., 1969, Geologic map of the Equality quadrangle, western Kentucky: U.S. Geological Survey Geologic Quadrangle 815, 1 map :col. ;76 x 90 cm., https://doi.org/10.3133/gq815.","productDescription":"1 map :col. ;76 x 90 cm.","costCenters":[],"links":[{"id":103531,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2117.htm","linkFileType":{"id":5,"text":"html"},"description":"2117"},{"id":249094,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0815/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":251931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0815/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.11749999999999,37.3675 ], [ -87.11749999999999,37.5 ], [ -87,37.5 ], [ -87,37.3675 ], [ -87.11749999999999,37.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db69992b","contributors":{"authors":[{"text":"Goudarzi, Gus H.","contributorId":44923,"corporation":false,"usgs":true,"family":"Goudarzi","given":"Gus","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":268101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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

 

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An area near Luray, Va., was studied to determine the thickness of the formation, its relationship to overlying and underlying rocks, and the original nature of the lavas from which the Catoctin greenstone was derived. There the Catoctin Formation lies unconformably on granitic rocks. Its basal sedimentary layer ranges from a few inches to 150 feet in thickness and contains pebbles of underlying basement rocks. The erosion surface beneath the Catoctin is irregular, and in several places, hills as much as 1,000 feet high were buried beneath the Catoctin lavas. No important time break is indicated between the deposition of the Catoctin Formation and the overlying Cambrian sediments.\r\n\r\nThe original Catoctin lavas were basaltic and were probably normal plateau basalts. Columnar joints, amygdules, sedimentary dikes, flow breccias low-dipping primary joints, and other primary structures are well preserved.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1265","usgsCitation":"Reed, J.C., 1969, Ancient lavas in Shenandoah National Park near Luray, Virginia: U.S. Geological Survey Bulletin 1265, Report: 43 p.; 1 Plate: 12.50 × 15.01 inches, https://doi.org/10.3133/b1265.","productDescription":"Report: 43 p.; 1 Plate: 12.50 × 15.01 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":408784,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21359.htm","linkFileType":{"id":5,"text":"html"}},{"id":63476,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1265/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247572,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1265/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1265/report-thumb.jpg"}],"country":"United States","state":"Virginia","city":"Luray","otherGeospatial":"Shenandoah National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.583,\n 38.5\n ],\n [\n -78.583,\n 38.75\n ],\n [\n -78.267,\n 38.75\n ],\n [\n -78.267,\n 38.5\n ],\n [\n -78.583,\n 38.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c243","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":214895,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68195,"text":"ha307 - 1969 - Water resources of the Buffalo River Watershed, West-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T09:59:47","indexId":"ha307","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":"307","title":"Water resources of the Buffalo River Watershed, West-central Minnesota","docAbstract":"

The Buffalo River watershed includes two general physiographic areas – a glacial lake plain and an glacial moraine.

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The lake plain, which was formed by Glacial lake Agassiz more than 9,000 years ago, is extremely flat – sloping only a few feet per mile westward near the Red River of the North. The moraine is largely an area of gently rolling hills, but in the eastern “tail” of the watershed the relief locally is over two hundred feet.

\n

The watershed has an area of about 1,690 square miles and includes most of Clay County and parts of Wilkin, Otter Tail, Becker, and Norman Counties. The population of the area is about 45,500 – 31,000 urban and 14,500 rural.

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The economy is largely agricultural. Sugar beet and wheat farming are dominant in the areas of clay and silt; potato farming is confined mainly to the sandy areas. Dairying and stock raising is important in the morainal area. The larger industries are located in Moorhead and consist of sugar beet, potato, and dairy product processing.

\n

Water-based recreation consists mostly of fishing in the larger lakes in the morainal area, and water-fowl hunting in the area of prairie potholes – the western part of the morainal area.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha307","collaboration":"Prepared in cooperation with the Minnesota Department of Conservation, Division of Waters, Soils and Minerals","usgsCitation":"Maclay, R.W., Bidwell, L.E., and Winter, T.C., 1969, Water resources of the Buffalo River Watershed, West-central Minnesota: U.S. Geological Survey Hydrologic Atlas 307, 3 Plates: 40.00 x 42.72 inches or smaller, https://doi.org/10.3133/ha307.","productDescription":"3 Plates: 40.00 x 42.72 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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W.","contributorId":13210,"corporation":false,"usgs":true,"family":"Maclay","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277822,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bidwell, L. E.","contributorId":100029,"corporation":false,"usgs":true,"family":"Bidwell","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":277824,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277823,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3657,"text":"cir619 - 1969 - Subsea mineral resources and problems related to their development","interactions":[],"lastModifiedDate":"2017-06-25T13:03:55","indexId":"cir619","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":"619","title":"Subsea mineral resources and problems related to their 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":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":3941,"text":"cir611 - 1969 - Asbestos occurrence in the Eagle C-4 quadrangle, Alaska","interactions":[],"lastModifiedDate":"2017-06-25T12:59:45","indexId":"cir611","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":"611","title":"Asbestos occurrence in the Eagle C-4 quadrangle, Alaska","docAbstract":"An asbestos occurrence was discovered in a remote part of the Eagle quadrangle, Alaska, in the summer of 1968 during geologic reconnaissance in connection with the U.S. Geological Survey's Heavy Metals program. The exposed part of the deposit consists of large joint blocks of serpentine which are cut by closely spaced subparallel veins. Most of the veins are about ? inch thick, and they consist of cross-fiber chrysotile asbestos. The asbestos appears to be of commercial quality, but the total quantity is unknown. \r\n\r\nThe asbestos occurs in a serpentinized ultramafic mass which appears to intrude metamorphic rocks. Many other serpentinized ultramafic masses are known in the Eagle quadrangle, but this is the first one in which considerable asbestos has been found. The deposit is of importance because it shows that geologic conditions are locally favorable for the formation of asbestos in the Yukon-Tanana Upland, and hope of finding commercial asbestos deposits thus seems possible.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir611","usgsCitation":"Foster, H.L., 1969, Asbestos occurrence in the Eagle C-4 quadrangle, Alaska: U.S. Geological Survey Circular 611, iii, 7 p. :maps. ;26 cm., https://doi.org/10.3133/cir611.","productDescription":"iii, 7 p. :maps. ;26 cm.","costCenters":[],"links":[{"id":139036,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0611/report-thumb.jpg"},{"id":31026,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0611/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c0d","contributors":{"authors":[{"text":"Foster, Helen Laura","contributorId":21936,"corporation":false,"usgs":true,"family":"Foster","given":"Helen","email":"","middleInitial":"Laura","affiliations":[],"preferred":false,"id":147866,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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. 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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":5935,"text":"pp670 - 1969 - John Wesley Powell and the anthropology of the Canyon Country","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"pp670","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":"670","title":"John Wesley Powell and the anthropology of the Canyon Country","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey; [for sale by the Supt. of Docs.] U.S. Govt. 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This map is one of a series prepared from photographs transmitted by Ranger IX (Jet Propulsion Lab., 1966., pls. A56-A58, B70-B82). It depicts the geology of some 724 sq km in the northeast part of the floor of Alphonsus (diameter about 115 km), a typical flat-floored old terra crater or basin with subdued rim. Similar basins abound in the south-central tarrae of the visible hemisphere and on the far side of the Moon. Alphonsus is of particular interest, however, because of a well-developed interior rille system and associated dark-halo craters.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i586","usgsCitation":"McCauley, J., 1969, (RLC-15) Geologic map of the Alphonsus GA region of the moon: U.S. Geological Survey IMAP 586, 1 map, https://doi.org/10.3133/i586.","productDescription":"1 map","costCenters":[],"links":[{"id":439066,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9FLIU6G","text":"USGS data release","linkHelpText":" (RLC-15) Geologic map of the Alphonsus GA region of the moon"},{"id":439065,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9OIQ6EJ","text":"USGS data release","linkHelpText":"Interactive Map: USGS IMAP 586 Geologic map of the Alphonsus GA region of the moon (RLC-15)"},{"id":189480,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101341,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0586/plate-1.pdf","size":"9863","linkFileType":{"id":1,"text":"pdf"}}],"scale":"50000","otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4906e4b0b290850eed1f","contributors":{"authors":[{"text":"McCauley, J.F.","contributorId":26310,"corporation":false,"usgs":true,"family":"McCauley","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":274642,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55903,"text":"ofr69117 - 1969 - Availability of ground water in the lower Wisconsin River valley, Wisconsin","interactions":[{"subject":{"id":55903,"text":"ofr69117 - 1969 - Availability of ground water in the lower Wisconsin River valley, Wisconsin","indexId":"ofr69117","publicationYear":"1969","noYear":false,"title":"Availability of ground water in the lower Wisconsin River valley, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":68310,"text":"ha479 - 1974 - Water resources of Wisconsin: Lower Wisconsin River basin","indexId":"ha479","publicationYear":"1974","noYear":false,"title":"Water resources of Wisconsin: Lower Wisconsin River basin"},"id":1}],"supersededBy":{"id":68310,"text":"ha479 - 1974 - Water resources of Wisconsin: Lower Wisconsin River basin","indexId":"ha479","publicationYear":"1974","noYear":false,"title":"Water resources of Wisconsin: Lower Wisconsin River basin"},"lastModifiedDate":"2015-10-13T12:22:23","indexId":"ofr69117","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":"69-117","title":"Availability of ground water in the lower Wisconsin River valley, Wisconsin","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69117","usgsCitation":"Hamilton, L., 1969, Availability of ground water in the lower Wisconsin River valley, Wisconsin: U.S. Geological Survey Open-File Report 69-117, 45 p., https://doi.org/10.3133/ofr69117.","productDescription":"45 p.","numberOfPages":"45","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":184897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Wisconsin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.23870849609375,\n 42.92827401776912\n ],\n [\n -91.23870849609375,\n 43.667871610117494\n ],\n [\n -89.39849853515625,\n 43.667871610117494\n ],\n [\n -89.39849853515625,\n 42.92827401776912\n ],\n [\n -91.23870849609375,\n 42.92827401776912\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8b7","contributors":{"authors":[{"text":"Hamilton, L.J.","contributorId":102917,"corporation":false,"usgs":true,"family":"Hamilton","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":254444,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55901,"text":"ofr69111 - 1969 - Geology and ground-water conditions in parts of Grant, Adams, and Franklin Counties, east-central Washington","interactions":[],"lastModifiedDate":"2013-08-19T10:20:13","indexId":"ofr69111","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":"69-111","title":"Geology and ground-water conditions in parts of Grant, Adams, and Franklin Counties, east-central Washington","language":"ENGLISH","doi":"10.3133/ofr69111","usgsCitation":"Grolier, M., and Bingham, J., 1969, Geology and ground-water conditions in parts of Grant, Adams, and Franklin Counties, east-central Washington: U.S. Geological Survey Open-File Report 69-111, 302 p., 5 figs., https://doi.org/10.3133/ofr69111.","productDescription":"302 p., 5 figs.","costCenters":[],"links":[{"id":184895,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6275cb","contributors":{"authors":[{"text":"Grolier, M. 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1969 - Flood of July 27-28, 1969, in southeastern New York","interactions":[{"subject":{"id":55898,"text":"ofr6980 - 1969 - Flood of July 27-28, 1969, in southeastern New York","indexId":"ofr6980","publicationYear":"1969","noYear":false,"title":"Flood of July 27-28, 1969, in southeastern New York"},"predicate":"SUPERSEDED_BY","object":{"id":2580,"text":"wsp2030 - 1975 - Summary of floods in the United States during 1969","indexId":"wsp2030","publicationYear":"1975","noYear":false,"title":"Summary of floods in the United States during 1969"},"id":1}],"supersededBy":{"id":2580,"text":"wsp2030 - 1975 - Summary of floods in the United States during 1969","indexId":"wsp2030","publicationYear":"1975","noYear":false,"title":"Summary of floods in the United States during 1969"},"lastModifiedDate":"2012-02-02T00:12:01","indexId":"ofr6980","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":"69-80","title":"Flood of July 27-28, 1969, in southeastern New York","language":"ENGLISH","doi":"10.3133/ofr6980","usgsCitation":"Dunn, B., and Robinson, F., 1969, Flood of July 27-28, 1969, in southeastern New York: U.S. Geological Survey Open-File Report 69-80, 11 p., 7 figs., https://doi.org/10.3133/ofr6980.","productDescription":"11 p., 7 figs.","costCenters":[],"links":[{"id":181643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eedd2","contributors":{"authors":[{"text":"Dunn, Bernard","contributorId":61423,"corporation":false,"usgs":true,"family":"Dunn","given":"Bernard","email":"","affiliations":[],"preferred":false,"id":254438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, F.L.","contributorId":56720,"corporation":false,"usgs":true,"family":"Robinson","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":254437,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}