{"pageNumber":"437","pageRowStart":"10900","pageSize":"25","recordCount":10951,"records":[{"id":1708,"text":"wsp154 - 1906 - The geology and water resources of the eastern portion of the Panhandle of Texas","interactions":[],"lastModifiedDate":"2022-11-29T21:46:10.52536","indexId":"wsp154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"154","title":"The geology and water resources of the eastern portion of the Panhandle of Texas","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp154","usgsCitation":"Gould, C.N., 1906, The geology and water resources of the eastern portion of the Panhandle of Texas: U.S. Geological Survey Water Supply Paper 154, 64 p., https://doi.org/10.3133/wsp154.","productDescription":"64 p.","costCenters":[],"links":[{"id":137195,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0154/report-thumb.jpg"},{"id":26785,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0154/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409827,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24450.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -101.558,\n 36.5\n ],\n [\n -101.558,\n 34.767\n ],\n [\n -100,\n 34.767\n ],\n [\n -100,\n 36.5\n ],\n [\n -101.558,\n 36.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d965","contributors":{"authors":[{"text":"Gould, Charles Newton","contributorId":37309,"corporation":false,"usgs":true,"family":"Gould","given":"Charles","email":"","middleInitial":"Newton","affiliations":[],"preferred":false,"id":143998,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39528,"text":"pp53 - 1906 - Geology and water resources of the Bighorn Basin, Wyoming","interactions":[],"lastModifiedDate":"2023-01-09T21:11:54.005352","indexId":"pp53","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"53","title":"Geology and water resources of the Bighorn Basin, Wyoming","docAbstract":"

This paper is the result of field work done during the seasons of 1904 and 1905 It is designed mainly to furnish information regarding geologic structure and the prospects for underground water. The description of the formations of the Bighorn Mountain area is chiefly the work of N. H. Darton, under whose direction the exploration ·was made.

\n

A general account of the surface waters is given, including a statement of their present and proposed uses for irrigation, and the economic products of a geologic nature are also described. The region considered comprises the Bighorn basin, a part of the Clark Fork basin, and the slopes of the adjoining mountain ranges, the entire area comprising 8,500 square miles. As shown on fig. 1, it is situated mainly in Bighorn County, in the northwestern part of Wyoming, and includes the greater portion of the area lying between meridians 107° 15' and 109° 15' and parallels 43° 40' and 45°. It is bounded on the north by Montana, on the east by the Bighorn Mountains, on the south by Bighorn and Owl Creek mountains, and on the west by Shoshone, Absaroka, and Beartooth mountains.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp53","usgsCitation":"Fisher, C., 1906, Geology and water resources of the Bighorn Basin, Wyoming: U.S. Geological Survey Professional Paper 53, Report: vi, 72 p.; 1 Plate: 28.03 x 25.85 inches, https://doi.org/10.3133/pp53.","productDescription":"Report: vi, 72 p.; 1 Plate: 28.03 x 25.85 inches","numberOfPages":"97","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":264260,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0053/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120279,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0053/report-thumb.jpg"},{"id":67134,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0053/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411589,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4575.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","county":"Big Horn County","otherGeospatial":"Big Horn Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.2622,\n 43.6475\n ],\n [\n -109.2622,\n 45\n ],\n [\n -107.2378,\n 45\n ],\n [\n -107.2378,\n 43.6475\n ],\n [\n -109.2622,\n 43.6475\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684132","contributors":{"authors":[{"text":"Fisher, C.A.","contributorId":44218,"corporation":false,"usgs":true,"family":"Fisher","given":"C.A.","affiliations":[],"preferred":false,"id":221577,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":34459,"text":"b298 - 1906 - Record of deep-well drilling for 1905","interactions":[],"lastModifiedDate":"2017-09-12T07:56:19","indexId":"b298","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"298","title":"Record of deep-well drilling for 1905","docAbstract":"

The present is the second of the series of reports on the collection of deep-well samples, the first of which, covering the period from the beginning of the work July 1, 1904, to December 31, 1904, was published as Bulletin No. 264. This report presents the records of a large number of wells from which more or less complete sets of samples have been secured and placed on file at the Survey, and. also many additional records not represented by samples.

The work has been conducted by the eastern section, division of hydrology, the expense being shared with the western section of hydrology and the geologic branch. The writer has continued in charge of the investigations and has been assisted by Messrs. E. F. Lines and Samuel Sanford. The burden of executive details has fallen mainly on Mr. Sanford since his assignment to the work on its relinquishment by Mr. Lines April 1. The methods followed are in most particulars those formulated by Mr. A. C. Veatch on the inauguration of the work in 1904, but to Mr. Sanford is due the credit for materially increasing the usefulness of the work to the driller, especially in furnishing geologic information.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b298","usgsCitation":"Fuller, M.L., and Sanford, S., 1906, Record of deep-well drilling for 1905: U.S. Geological Survey Bulletin 298, 299 p., https://doi.org/10.3133/b298.","productDescription":"299 p.","numberOfPages":"299","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":167766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0298/report-thumb.jpg"},{"id":22493,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0298/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a91be","contributors":{"authors":[{"text":"Fuller, Myron Leslie","contributorId":106091,"corporation":false,"usgs":true,"family":"Fuller","given":"Myron","email":"","middleInitial":"Leslie","affiliations":[],"preferred":false,"id":213001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanford, Samuel","contributorId":45687,"corporation":false,"usgs":true,"family":"Sanford","given":"Samuel","email":"","affiliations":[],"preferred":false,"id":213000,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32884,"text":"pp46 - 1906 - Geology and underground water resources of northern Louisiana and southern Arkansas","interactions":[],"lastModifiedDate":"2015-11-12T12:38:49","indexId":"pp46","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"46","title":"Geology and underground water resources of northern Louisiana and southern Arkansas","docAbstract":"

In the fall of 1902 arrangements were made with the Geological Survey of Louisiana for the writer to prepare a report on the geology and underground water resources of northern Louisiana. In the prosecution of this work it was found necessary, in order that the questions involved might be more thoroughly understood, to include that portion of the Coastal Plain in southern Arkansas southwest of Arkansas River, and the portion of northeastern Texas not discussed in Hill's exhaustive report on the artesian-water conditions of the Black and Grand prairies a After the Arkansas work was well in hand and before the Texas investigation had advanced beyond a few preliminary letters the writer was detailed to the Long Island, New York, investigation, which consumed the field and office time from February, 1903, to July, 1904.b The present report is thus based on the'field work of the fall and winter of 1902 and 1903, supplemented by several years' field work with the Geological Survey of Louisiana and private work in eastern Texas. It covers southern Arkansas and northern Louisiana and small portions of adjacent areas in Mississippi and Texas.

","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp46","usgsCitation":"Veatch, A.C., 1906, Geology and underground water resources of northern Louisiana and southern Arkansas: U.S. Geological Survey Professional Paper 46, 422 p., https://doi.org/10.3133/pp46.","productDescription":"422 p.","numberOfPages":"480","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":119703,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0046/report-thumb.jpg"},{"id":60807,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0046/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas, Lousiana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.33959960937499,\n 31.034108344903512\n ],\n [\n -94.33959960937499,\n 35.24561909420681\n ],\n [\n -90.867919921875,\n 35.24561909420681\n ],\n [\n -90.867919921875,\n 31.034108344903512\n ],\n [\n -94.33959960937499,\n 31.034108344903512\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68421d","contributors":{"authors":[{"text":"Veatch, A. C.","contributorId":84814,"corporation":false,"usgs":true,"family":"Veatch","given":"A.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":209344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32886,"text":"pp52 - 1906 - Geology and underground waters of the Arkansas Valley in eastern Colorado","interactions":[],"lastModifiedDate":"2017-04-25T14:37:34","indexId":"pp52","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"52","title":"Geology and underground waters of the Arkansas Valley in eastern Colorado","docAbstract":"

In the valley of Arkansas River in southeastern Colorado there is an area of considerable extent in which artesian flows are available. During the last ten years numerous wells have been sunk to develop this important resource and, in most cases in the lower lands, abundant water supplies have been obtained. The principal water-bearing bed is the \"Dakota\" formation, which consists of two sheets of porous sandstone separated by a small body of clay and overlain in the greater portion of the area by a mass of impervious shales. The sandstones receive their waters from, rainfall and from the sinking of streams along the foothills of the Rocky Mountains and on some of the higher slopes south of the Arkansas Valley. In the passage of this sandstone underground, the waters which it contains are held down by the overlying shales, but, as some of the sandstone outcrops are at relatively low levels to the east only a moderate head or pressure is sustained. On account of this low head, artesian flows are available only in the lower lands, and one of the principal objects of this investigation has been the determination of the area in which flows are to be expected. The \"Dakota\" sandstone and associated formations do not lie level, or even slope regularly to the east, but are flexed into low arches and shallow troughs of considerable complexity of configuration. Accordingly, in investigating this source of water supply, it has been necessary to ascertain the structure and distribution of the various formations in order to indicate the variations in depth to the water-bearing stratum. The principal results of these investigations are set forth: (1) In the geologic map (Pl. VI), which shows the distribution of the formations on the surface; (2) in the map, Pl. XXV, which shows the depth to the water-bearing horizon, the area in which flows are expected, the head of the underground waters, and other features, and (3) in the cross sections (Pls. VII and XXIII), which show the principal underground features. The investigation has been in progress for several years and is an extension of the preliminary examination of the region by G. K. Gilbert in 1894 and 1895.

For the western portion of the area the maps and texts of the Pueblo, Elmoro, Walsenburg, Spanish Peaks, and Pikes Peak folios have been utilized as far as practicable. For the central and eastern portions the larger features of the geology have been specially mapped, and considerable detailed mapping has been done in the region south and southeast of Canyon and Colorado Springs. In the field work I have been assisted by Mr. C. A. Fisher, who has examined in detail the Nepesta quadrangle and contributed numerous other data. Dr. W. S. Tangier Smith and Messrs. C. E. Sicbenthal and W. T. Lee have made observations in certain areas. Much valuable information respecting wells has been furnished by Mr. William Archer, of the Atchison, Topeka and Santa Fe Railway Company, and Mr. C. H. McVay, well driller at Rocky Ford.

","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp52","usgsCitation":"Darton, N.H., 1906, Geology and underground waters of the Arkansas Valley in eastern Colorado: U.S. Geological Survey Professional Paper 52, Report: iv, 90 p.; 2 Plates: 33.18 x 27.43 inches and 32.29 x 27.27 inches, https://doi.org/10.3133/pp52.","productDescription":"Report: iv, 90 p.; 2 Plates: 33.18 x 27.43 inches and 32.29 x 27.27 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":340321,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0052/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0052/report-thumb.jpg"},{"id":340322,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0052/plate-25.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60809,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0052/report.pdf","text":"Report","size":"7.41 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Colorado","otherGeospatial":"Arkansas Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.5,\n 39.5\n ],\n [\n -102,\n 39.5\n ],\n [\n -102,\n 37\n ],\n [\n -105.5,\n 37\n ],\n [\n -105.5,\n 39.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6841c9","contributors":{"authors":[{"text":"Darton, N. H.","contributorId":71523,"corporation":false,"usgs":true,"family":"Darton","given":"N.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":209348,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39504,"text":"pp50 - 1906 - The Montana lobe of the Keewatin ice sheet","interactions":[],"lastModifiedDate":"2019-06-11T15:31:29","indexId":"pp50","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"50","title":"The Montana lobe of the Keewatin ice sheet","docAbstract":"

Just south of the forty-ninth parallel and east of the Rocky Mountains is an area that is of much interest to glacialists. It is the area which lay between the Keewatin ice sheet and the mountain glaciers coming from the west. Although it has been known for nearly twenty years that the bodies of drift deposited by the ice coming from opposite directions were closely associated, little detailed field work has been done in this region. As early as 1881 Sir James Geikie prophesied that a careful study of the region would clear up many important points in glaciology.  In 1885, Dr. T. C. Chamberlin and Prof E. D. Salisbury, in a reconnaissance of the region, determined roughly the course of the terminal moraine of the eastern ice sheet and obtained data concerning the character and extent of the mountain glaciation. In 1890 Mr. G. E. Culver, while a member of the military party under the command of Lieutenant Ahern, U. S. Army, gathered many data concerning the geology of the region, publishing the results of his investigations in the Transactions of the Wisconsin Academy of Sciences, in 1891. Doctor Dawson and Mr McConnell, of the Canadian Survey, have worked out the geology of the region north of the boundary line. Their reports are unusually complete, but the area to the south offers better opportunity for study, and somewhat different conclusions were reached from a study of that region.

The work on which the following discussion is based was done during the field seasons of 1901, 1902, and 1903. During the first season the writer was accompanied by Mr. Bruce McLeish, then a student at the University of Chicago. The second year Mr. Porter Graves, of the Kansas City High School, rendered valuable assistance. The writer is most deeply indebted to Dr. T. C. Chamberlin and Prof. R. D. Salisbury, of the University of Chicago, for friendly interest shown while superintending the compiling of this manuscript. Professor Salisbury also personally directed a portion of the field work and made many practical suggestions. Thanks are also due Dr. G. K. Gilbert for careful criticism of the report.

The area covered by this investigation lies along the eastern front of the Montana Rockies, between longitude 108° and 113° 40', and latitude 47° 15' and 49° 30'. Over the eastern and northern part of this area the ice from the northeast deposited its drift. Over the western part the ice from the Rockies pushed down the mountain valleys and, deploying on the plain, deposited large and well-defined terminal moraines. Extending from the Canadian line to the Missouri there is a strip of country, varying greatly in width, which the ice did not cover.

","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp50","usgsCitation":"Calhoun, F., 1906, The Montana lobe of the Keewatin ice sheet: U.S. Geological Survey Professional Paper 50, 62 p., https://doi.org/10.3133/pp50.","productDescription":"62 p.","numberOfPages":"62","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":120437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0050/report-thumb.jpg"},{"id":67112,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0050/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Rocky Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.3232421875,\n 45.30580259943578\n ],\n [\n -116.3232421875,\n 49.009050809382046\n ],\n [\n -111.81884765624999,\n 49.009050809382046\n ],\n [\n -111.81884765624999,\n 45.30580259943578\n ],\n [\n -116.3232421875,\n 45.30580259943578\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b8f9","contributors":{"authors":[{"text":"Calhoun, F.H.H.","contributorId":94724,"corporation":false,"usgs":true,"family":"Calhoun","given":"F.H.H.","email":"","affiliations":[],"preferred":false,"id":221540,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32883,"text":"pp44 - 1906 - Underground water resources of Long Island, New York","interactions":[],"lastModifiedDate":"2019-03-11T14:51:32","indexId":"pp44","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"44","title":"Underground water resources of Long Island, New York","docAbstract":"

As Long Island is the largest island on the eastern coast of the United States, and is of such size, 120 miles long and 23 miles wide, that it is a more or less noticeable feature on even very small-scale maps, little need be said of its general geographic position.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp44","usgsCitation":"Veatch, A.C., Slichter, C.S., Bowman, I., Crosby, W., and Horton, R., 1906, Underground water resources of Long Island, New York: U.S. Geological Survey Professional Paper 44, Report: 394 p.; 3 Plates: 63.30 x 26.74 inches or smaller, https://doi.org/10.3133/pp44.","productDescription":"Report: 394 p.; 3 Plates: 63.30 x 26.74 inches or smaller","numberOfPages":"422","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":333185,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0044/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":333186,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0044/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":333187,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0044/plate-24.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0044/report-thumb.jpg"},{"id":60806,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.87805175781249,\n 41.1290213474951\n ],\n [\n -72.2076416015625,\n 41.23031465959445\n ],\n [\n -72.6361083984375,\n 41.12281462734397\n ],\n [\n -73.4930419921875,\n 40.97575093157534\n ],\n [\n -73.71826171874999,\n 40.90313381465847\n ],\n [\n -74.08355712890625,\n 40.63688312646408\n ],\n [\n -74.04510498046875,\n 40.549287249082035\n ],\n [\n -73.76220703125,\n 40.53050177574321\n ],\n [\n -72.9052734375,\n 40.65772237175813\n ],\n [\n -72.27081298828125,\n 40.86783384138491\n ],\n [\n -71.97967529296874,\n 40.971603532799115\n ],\n [\n -71.83135986328124,\n 41.05035951931887\n ],\n [\n -71.87805175781249,\n 41.1290213474951\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f72f","contributors":{"authors":[{"text":"Veatch, A. C.","contributorId":84814,"corporation":false,"usgs":true,"family":"Veatch","given":"A.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":209343,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slichter, Charles Sumner","contributorId":102464,"corporation":false,"usgs":true,"family":"Slichter","given":"Charles","email":"","middleInitial":"Sumner","affiliations":[],"preferred":false,"id":209340,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowman, Isaiah","contributorId":57052,"corporation":false,"usgs":true,"family":"Bowman","given":"Isaiah","email":"","affiliations":[],"preferred":false,"id":209342,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crosby, W.O.","contributorId":16882,"corporation":false,"usgs":true,"family":"Crosby","given":"W.O.","email":"","affiliations":[],"preferred":false,"id":209339,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Horton, R.E.","contributorId":24760,"corporation":false,"usgs":true,"family":"Horton","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":209341,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":39505,"text":"pp51 - 1906 - Geology of the Bighorn Mountains","interactions":[],"lastModifiedDate":"2023-01-09T21:14:23.549553","indexId":"pp51","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"51","title":"Geology of the Bighorn Mountains","docAbstract":"

This report is the result of studies made in the field during the seasons of 1901, 1902, 1903, 1904, and 1905. It relates to an area of about 9,000 square miles, situated mainly in the north-central portion of Wyoming and extending northward into Montana. Its location and general surroundings are shown on PL II. It covers the greater portion of the Bighorn uplift, together with an adjoining area of the Great Plains on the east. It also includes a small part of the Bighorn Basin and the eastern end of the Bridger Range. The report describes the various rocks, their structure, history, and mineral resources, including underground water, coal, gypsum, and various other products. It also contains information as to surface waters available for irrigation.

\n

Throughout the work assistance has been rendered by Mr. C. A. Fisher, who mapped portions of the area, measured numerous sections, collected fossils, and examined most of the crystalline rocks; and the author is indebted to Mr. Albert Johannsen for some of the petrographic descriptions.

\n

Previous observers have given but little information regarding the geology of the Bighorn Mountains, though Dr. F. V. Hayden ascertained the general relations of the uplift in his exploration of the Northwest, and Mr. George H. Eldridge, who crossed the range near Bald Mountain and southwest of Buffalo during the summer of 1893, described 0 some of the broader features of the geologic succession and structure in a remarkably comprehensive manner, considering how small an area he had the opportunity to examine. The Bighorn region is very thinly settled, there being no permanent habitations among the mountains, and it is but little visited by others than hunters, prospectors, and herders. There have recently been established two summer resorts in the mountains, and each year a larger number of persons visit the region. Unfortunately the mineral prospects have proved disappointing to the prospectors, and there appears to be but little promise that the area will become important on account of its mineral resources. In the Bridger uplift promising prospects of gold and copper have recently been discovered, which may prove of value.

\n

There are extensive, forests in the mountains, which are now included in a Government forest reserve, but their timber is not of great value. Much of the area below timber line contains an abundance of luxuriant grasses and other plants, which afford excellent pasturage for stock, and large herds of sheep and cattle are ranged in the region during the short summer season. Game is moderately abundant, and most of the streams contain large numbers of trout. The region is one of great interest geologically on account of its variety of sedimentary rocks, interesting structure, and remarkably instructive glacial features. The central area, with its high peaks, presents alpine scenery of notable character. Doubtless in the future the region will be extensively visited by tourists, hunters, and geologists.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp51","usgsCitation":"Darton, N.H., 1906, Geology of the Bighorn Mountains: U.S. Geological Survey Professional Paper 51, 129 p., https://doi.org/10.3133/pp51.","productDescription":"129 p.","numberOfPages":"173","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":120438,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0051/report-thumb.jpg"},{"id":67113,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0051/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411590,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4527.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.68798828125,\n 45.251688256117646\n ],\n [\n -107.95166015624999,\n 45.398449976304086\n ],\n [\n -108.468017578125,\n 45.390735154248894\n ],\n [\n -108.5009765625,\n 45.058001435398296\n ],\n [\n -108.292236328125,\n 44.824708282300236\n ],\n [\n -107.830810546875,\n 44.535674532413196\n ],\n [\n -107.479248046875,\n 44.11125397357153\n ],\n [\n -107.391357421875,\n 43.82660134505384\n ],\n [\n -107.40234375,\n 43.34914966389313\n ],\n [\n -106.76513671875,\n 43.84245116699036\n ],\n [\n -106.72119140625,\n 44.11125397357153\n ],\n [\n -106.72119140625,\n 44.49650533109348\n ],\n [\n -106.995849609375,\n 44.793530904744074\n ],\n [\n -107.68798828125,\n 45.251688256117646\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683275","contributors":{"authors":[{"text":"Darton, N. H.","contributorId":71523,"corporation":false,"usgs":true,"family":"Darton","given":"N.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":221541,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39501,"text":"pp45 - 1906 - The geography and geology of Alaska; a summary of existing knowledge, with a section on climate, and a topographic map and description thereof","interactions":[],"lastModifiedDate":"2015-11-12T12:56:33","indexId":"pp45","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"45","title":"The geography and geology of Alaska; a summary of existing knowledge, with a section on climate, and a topographic map and description thereof","docAbstract":"

Alaska, the largest outlying possession of the United States, is that great land mass forming the northwestern extremity of the North American continent, whose western point is within 60 miles of the Asiatic coast (PI. II). About one-quarter of this area lies within the Arctic Circle, and from the standpoint of geographic position must be regarded as an arctic province; but the southern seaboard, exposed to the warm winds and waters of the Pacific, gives to the entire southern portion of the territory\" a comparatively warm climate. It is not generally realized that the range of climate in Alaska is greater than that between Florida and Maine. At the southernmost point of the Pacific coast the mean annual temperature is not far from that of the city of Washington, the winters being warmer and characterized by less snowfall; the Yukon Valley on the other hand has a winter climate similar to that of northern Montana and Dakota; while in the extreme northern part of the territory the meteorologic conditions are invariably arctic.

\n

Though as yet only sparsely settled, Alaska's vast area and great resources make it one of the most important possessions of the United States and promise its rapid development. During the years 1890 to 1900 the population increased from 32,052* to 63,592. The mineral output, which in 1890 was valued at less than $800,000, exceeded $9,000,000 in 1904, and the fisheries show a corresponding growth. This rapid development has attracted public attention and led to urgent demand for explorations, surveys, and other investigations. So actively has this work been pushed, both by public and private enterprise, that exact knowledge of the geography, geology, and mineral resources of the interior has made greater strides within the last eight years than during the preceding thirty-one years since the acquisition of Alaska. The facts regarding the geography and geology, scattered as they are through the many books and reports of this period, are not always readily accessible, and the time seems ripe to present them in a summarized form.

\n

The topography of Alaska is varied and complex (see PI. I), and it is not easy to present briefly even the salient features. The limited number of pages here devoted to the subject precludes the possibility of detailed treatment, even if the facts were available. Much of the description has been taken from the results attained by other investigators, the writer being personally familiar with only a part of this large province. A list of the publications consulted is appended.

\n

The larger geographic features of Alaska are now fairly well known, though the detailed surveys which are demanded by the development of many localities have hardly been begun. Preliminary surveys have been completed of all but three 8 of the larger rivers. The most important mountain ranges have been at least outlined (fig. 3). Only three large areas remain almost entirely unmapped: One in southwestern Alaska, between Cook Inlet and the lower Kuskokwim, and the others in northern Alaska, embracing the Arctic watershed east and west of the Colville River. Nearly all the surveys of the interior, however, have been of a preliminary and exploratory character, and to meet the requirements of exact geography must be followed by more detailed mensuration.

\n

Though the coast line has been fairly well known for more than half a century, knowledge of the interior has been gained chiefly within the last two decades. This has not yet found its way into text-books and has too often been entirely ignored by cartographers. If facts are presented which may seem elementary, it is because even well-informed people have been known to harbor misconceptions in regard to the orographic features, climate, and general character of Alaska. Those who read of the perils and privations of winter travel and explorations are apt to picture a region of ice and snow; others, again, who have personal knowledge of the tourist route of southeastern Alaska, regard the whole district as one of rugged mountains and glaciers. In point of fact, glaciers are now nearly limited to the ranges bordering the Pacific and to the two slopes of the Alaska range; and even during the greatest development of glaciers but a small portion of Alaska was under ice (see map, PI. XXII).

\n

As a treatise on geography would hardly be complete without some discussion of the climate, meteorologic data have been compiled by Mr. Cleveland Abbe, jr., but the discussion of this does not pretend to be more than a cursory treatment of the subject.

\n

The scope of the paper seems to require also a brief summary of the development of geographic knowledge of Alaska. This subject, with its many ramifications, is of fascinating interest and offers a magnificent field for the trained historian. If the accompanying sketch of discovery and exploration awakens any measure of popular interest the writer will feel amply rewarded for having attacked a theme which hardly falls within the scope of his investigations.

\n

When this compilation was begun it was intended to be chiefly a description of the topography of Alaska, as illustrated by the accompanying map (PI. XXXIV, in pocket), which was compiled under the direction of the late R. U. Goode. In the course of the work there accumulated much geologic as well as geographic material which seemed worthy of inclusion in the report. As no comprehensive statement of the geology of Alaska has been made since the modern epoch of investigation was begun, an attempt will be made to give a summary of all results achieved. Since the writer has obtained much of his knowledge of the facts from the work of others, he disclaims any pretense of making an entirely original contribution to geologic science. He feels, however, that a personal familiarity with a considerable part of the province, gained during seven consecutive seasons of field work, will justify Mm in presenting conclusions which may in some cases be at variance with those in the reports on which he must draw for his facts.

\n

Throughout this report attempt will be made to credit borrowed material to the source from which it is drawn. Where such matter has been obtained entirely from published reports there is no difficulty in so doing; but as regards investigators of the Geological Survey, with whom the writer has collaborated both in field and in office, the case is somewhat different, for it is not always possible to know whether this or that theory originated with the writer or with one of his colleagues. It will, then, perhaps suffice to state that this report could not have been prepared without the explorations and researches of the geologists, F. C. Schrader, Walter C. Mendenhall, Arthur J. Collier, J. E. Spurr, and Arthur C. Spencer; and the surveys of the topographers, T. G. Gerdine, D. C. Witherspoon, D. L. Reaburn, W. J. Peters, and E. C. Barnard. Each of these men, in the course of from two to six years of field work, has made important contributions to the knowledge of the geography and geology of Alaska, and not all of these results have yet been put in print. In the last season (1903) L. M. Prindle, C. W. Wright, Arthur Hollick, G. C. Martin, F. L. Hess, and Fred H. Moffit have carried on geologic work in Alaska, and the writer has made use of their work now in course of publication. He has also been fortunate in having access to the manuscript reports of Walter C. Mendenhall and F. C. Schrader on the Copper River basin, to which references will be made. The matter here presented should be credited in a measure to all of these investigators, but for many of the theories advanced the writer alone is responsible.

\n

As this manuscript goes to press there has been opportunity to incorporate some of the results of the field work of 1904. As far as possible these have been embodied in the text, but in some instances it has been found advisable to add them only as footnotes. During the past summer F. E. and C. W. Wright extended the geologic reconnaissance in southeastern Alaska. In southwestern Alaska G. C. Martin and T. W. Stanton have determined the general Mesozoic section, while F. H. Moffit has made a reconnaissance of the northern part of the Kenai Peninsula. A. J. Collier has mapped the geology of the Cape Lisburne region, and L. M. Prindle and F. L. Hess have made contributions to the knowledge of the metamorphic terranes of the Yukon-Tanana district.

\n

It is the writer's purpose to describe in nontechnical language the larger geographic features and discuss their relation as far as the data available will permit. In the treatment of the geology, however, less effort will be made to make the matter acceptable to the lay reader. It is hoped, however, that a brief summary of the salient features of the geologic history' may be not without interest to the general public. If this paper serves in some measure to dispel the popular fallacies regarding Alaska and to disseminate more accurate knowledge of its geographic and geologic features, the purpose of its publication will be accomplished.

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H.","contributorId":45681,"corporation":false,"usgs":true,"family":"Brooks","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":221535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abbe, Cleveland Jr.","contributorId":25039,"corporation":false,"usgs":true,"family":"Abbe","given":"Cleveland","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":221534,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goode, R.U.","contributorId":50951,"corporation":false,"usgs":true,"family":"Goode","given":"R.U.","email":"","affiliations":[],"preferred":false,"id":221536,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":39503,"text":"pp49 - 1906 - Geology and mineral resources of part of the Cumberland Gap coal field, Kentucky","interactions":[],"lastModifiedDate":"2015-11-12T11:52:14","indexId":"pp49","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1906","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":"49","title":"Geology and mineral resources of part of the Cumberland Gap coal field, Kentucky","docAbstract":"

The Cumberland Gap coal field lies in Bell and Harlan counties, in the southeast corner of Kentucky and in Claiborne and Campbell counties, Tenn., and extends in a general northeast-southwest direction between Pine and Cumberland mountains from Fork Mountain on the southwest to the heads of Poor and Clover forks of Cumberland River on the northeast. As defined in this paper, it has a total length of about 90 miles and a width of from 15 to 20 miles. (See Pl. II.)

\n

In this paper is described only the central part of the basin, or the area lying between Log Mountains at the head of Yell ow Creek of Cumberland and nearly north-south line about 10 miles east of Harlan, and while the data presented will give an idea of the general stratigraphy and structure of the whole field, they are not authoritative except within these limits.

","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp49","usgsCitation":"Ashley, G.H., and Glenn, L.C., 1906, Geology and mineral resources of part of the Cumberland Gap coal field, Kentucky: U.S. Geological Survey Professional Paper 49, 239 p., https://doi.org/10.3133/pp49.","productDescription":"239 p.","numberOfPages":"283","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":67111,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0049/report-thumb.jpg"}],"country":"United States","state":"Kentucky","county":"Boll County, Harlan County","otherGeospatial":"Cumberland Gap, Log Mountains, Yellow 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G. H.","contributorId":106857,"corporation":false,"usgs":true,"family":"Ashley","given":"G.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":221539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Glenn, L. C.","contributorId":86025,"corporation":false,"usgs":true,"family":"Glenn","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":221538,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":33656,"text":"b294 - 1906 - Zinc and lead deposits of the Upper Mississippi Valley","interactions":[],"lastModifiedDate":"2023-12-22T19:23:14.247663","indexId":"b294","displayToPublicDate":"1906-01-01T00:00:00","publicationYear":"1906","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":"294","title":"Zinc and lead deposits of the Upper Mississippi Valley","docAbstract":"

The zinc and lead mines of the upper Mississippi Valley are in the southwest portion of Wisconsin and in adjacent parts of Illinois mid Iowa. The boundaries of the region are in part indefinite, since sporadic occurrences of the minerals are found outside the mining region proper. It is usual to define the area as including Grant, Lafayette, and Iowa counties in Wisconsin, Jo Daviess County in Illinois, and an irregular narrow belt of territory in Clayton and Dubuque counties paralleling the Mississippi River in Iowa. In this report a slightly smaller area is discussed, the region being limited on the east by the meridian of 90° west longitude. East of this meridian there are a few scattered prospects, hut comparatively little mining has been done in recent years in the area beyond the boundary indicated, so that it is sufficiently accurate for present purposes.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b294","usgsCitation":"Bain, H.F., 1906, Zinc and lead deposits of the Upper Mississippi Valley: U.S. Geological Survey Bulletin 294, xi, 155 p., https://doi.org/10.3133/b294.","productDescription":"xi, 155 p.","numberOfPages":"200","costCenters":[],"links":[{"id":341576,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/294/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164118,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/294/report-thumb.jpg"},{"id":344142,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/294/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":344143,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/294/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":423867,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19831.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Illinois, Iowa, Wisconsin","otherGeospatial":"Upper Mississippi Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -90,\n 43.25\n ],\n [\n -91.167,\n 43.25\n ],\n [\n -91.167,\n 42.25\n ],\n [\n -90,\n 42.25\n ],\n [\n -90,\n 43.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49a1e4b07f02db5be47d","contributors":{"authors":[{"text":"Bain, Harry Foster","contributorId":61480,"corporation":false,"usgs":true,"family":"Bain","given":"Harry","email":"","middleInitial":"Foster","affiliations":[],"preferred":false,"id":211734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1248,"text":"wsp149 - 1905 - Preliminary list of deep borings in the United States","interactions":[],"lastModifiedDate":"2017-09-12T07:57:57","indexId":"wsp149","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1905","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":"149","title":"Preliminary list of deep borings in the United States","docAbstract":"

The first preliminary list of deep borings in the United States was issued as Water-Supply Papers Nos. 57 and 61. The present publication includes all of the wells listed in these two papers, together with many additional borings, mostly of recent date. Messrs. M. L. Fuller and A. C. Veatch, of the eastern section of hydrology, and other geologists of the Survey have contributed many new data. Descriptions of borings published in reports issued since 1901 have been incorporated as far as practicable. All the entries are by counties. The wells and borings reported in the paper are all more than 400 feet in depth. The information concerning them has been obtained partly from replies to circular letters sent to all parts of the United States and partly from geological reports and other published sources. Owing to the difficulty of obtaining replies to the circulars, to lack of knowledge on the part of correspondents, and to the incompleteness of published records, doubtless there are borings which have not been reported. In regions of oil and gas wells, where borings are numerous, the individual wells can not be listed here, but representative wells are given. References to logs or records of the wells or extended descriptions of them are given in footnotes, and after the list of wells in each State there is added a list of the principal publications relating to deep borings in that State.

The bearing of the information given in the columns of the lists probably is apparent unless, perhaps, in the one headed \"Height to which the water rises.\" In this column an entry such as \"-45\" indicates that the water rises to within 45 feet of the surface; \"+45\" indicates that it is a flowing well and has sufficient head to raise the water 45 feet above the surface in an open pipe 45 feet or more in height. The yield in gallons per minute usually is estimated. Depths and diameters often have been reported from memory and different sources of publication sometimes give different figures. Most wells which are not stated to be \"for oil,\" \"for gas,\" \"brine,\" \"abandoned,\" etc., in the remarks column, or \"not any\" in the yield column, generally afford more or less water. Many of the gas and oil wells, active or abandoned, yield salt water.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp149","usgsCitation":"Darton, N.H., 1905, Preliminary list of deep borings in the United States (2d ed. with additions.): U.S. Geological Survey Water Supply Paper 149, 175 p., https://doi.org/10.3133/wsp149.","productDescription":"175 p.","numberOfPages":"180","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":26178,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0149/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0149/report-thumb.jpg"}],"country":"United States","edition":"2d ed. with additions.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d96f","contributors":{"authors":[{"text":"Darton, Nelson Horatio","contributorId":78307,"corporation":false,"usgs":true,"family":"Darton","given":"Nelson","email":"","middleInitial":"Horatio","affiliations":[],"preferred":false,"id":143436,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67842,"text":"gf120 - 1905 - Silverton folio, Colorado","interactions":[],"lastModifiedDate":"2015-10-14T11:45:56","indexId":"gf120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1905","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":314,"text":"Folios of the Geologic Atlas","code":"GF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"120","title":"Silverton folio, Colorado","docAbstract":"

The term San Juan region, or simply \"the San Juan,\" used with variable meaning by early explorers, and naturally with indefinite limitation during the period of settlement, is now quite generally applied to a large tract of mountainous country in southwestern Colorado, together with an undefined zone of lower country bordering it on the north, west, and south.  The Continental Divide traverses this area in a great bow.  The principal part of the district is a deeply scored volcanic plateau, more than 3000 square miles in extent, drained on the north by the tributaties of the Gunnison River, on the west by those of the Dolores and San Miguel rivers, on the south by numerous branches of the San Juan, and on the east by the Rio Grande.  ALl but the latter drainage finds its way to the Gulf of California through the Colorado River.

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The San Bernardino basin lies near the eastern end of the valley of southern California.  Under the latter term is included that general lowland area which is definitely limited on the north by the San Gabriel and San Bernardino ranges and on the east by the latter range and the San Jacinto group, but whose southern boundary is irregular and difficult to define.  In this direction there is an interdigitation of ridges and valleys as the Sierra Madre Range of San Diego County dies out toward the north.  The more or less indefinite heights that represent its extension in this direction are separated by lowlands, which in turn are to be regarded as southwest lobes of the well-defined east-west valley that lies along the base of the San Gabriel Range.

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The present paper is a brief summary of the underground water conditions in eastern United States, prepared to meet the demands of drillers and others for information relating to the general water resources of the various States or of specified regions.

The detail with which the several regions or subjects are discussed depends mainly on their relative importance, although because of the greater amount of work done in certain localities, or on certain problems, it is possible to make more complete and definite statements in regard to the underground water supplies in some regions than in others. The included reports have been prepared by a number of geologists, each, in general, having charge of the investigations in a particular State or group of States. Because of the number of contributors there is necessarily considerable variation in the manner of treatment of the subject, but in most cases the same general plan has been followed.

In preparing the paper simplicity of treatment has been kept in mind, and elaborate geologic discussions have been omitted. Wherever possible maps have been given in preference to long and possibly obscure discussions. In some instances, however, it has been necessary to describe the various water-bearing formations under their geologic names. Where this has been necessary the aim has been to employ those terms which are oldest and best known to the people of the States to which the discussion relates.

For the purpose of presenting in a simple manner a few of the more important features relating to the nature and occurrence of subterranean waters and of making more intelligible the descriptions of the conditions in the various States, there is given a short paper on the general occurrence of underground waters.

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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp137","usgsCitation":"Mendenhall, W.C., 1905, Development of underground waters in the eastern coastal plain region of southern California: U.S. Geological Survey Water Supply Paper 137, Report: 140 p.; 5 Plates: 27.50 × 16.00 inches or smaller, https://doi.org/10.3133/wsp137.","productDescription":"Report: 140 p.; 5 Plates: 27.50 × 16.00 inches or smaller","costCenters":[],"links":[{"id":395959,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24349.htm"},{"id":28096,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0137/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28095,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0137/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28094,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0137/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28093,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0137/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247201,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0137/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247200,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0137/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137660,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0137/report-thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118,\n 33.5\n ],\n [\n -117.75,\n 33.5\n ],\n [\n -117.75,\n 34\n ],\n [\n -118,\n 34\n ],\n [\n -118,\n 33.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65ddea","contributors":{"authors":[{"text":"Mendenhall, Walter Curran","contributorId":57823,"corporation":false,"usgs":true,"family":"Mendenhall","given":"Walter","email":"","middleInitial":"Curran","affiliations":[],"preferred":false,"id":144966,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39497,"text":"pp39 - 1905 - Forest conditions in the Gila River Forest Reserve, New Mexico","interactions":[],"lastModifiedDate":"2015-09-17T09:53:53","indexId":"pp39","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1905","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":"39","title":"Forest conditions in the Gila River Forest Reserve, New Mexico","docAbstract":"

The Gila River Forest Reserve was established by proclamation of President McKinley on March 2, 1899. The following is a statement of the boundaries as laid down in the proclamation: \"Beginning at a point on the boundary line between New Mexico and Arizona, where it is intersected by the north line of township five (5) south, range twenty-one (21) west, New Mexico principle meridian, New Mexico; thence easterly along the township line to the northeast corner of township five (5) south, range sixteen (16) west; thence southerly along the range line between ranges fifteen (15) and sixteen (16) west, to the southeast corner of township eight (8) south, range sixteen (16) west; thence easterly along the township line to the northeast corner of township nine (9) south, range fifteen (15) west; thence southerly along the range line to the southeast corner of said township; thence easterly along the township line to the northeast corner of township ten (10) south, range ten (10) west; thence southerly along the first guide meridian west, between ranges nine (9) and ten (10) west, to its intersection with the third (3rd) standard parallel south, between townships fifteen (15) and sixteen (16) south; thence westerly along the said third (3rd) standard parallel south to the southwest corner of township fifteen (15) south, range sixteen (16) west; thence northerly along the range line to the northwest corner of said township; thence westerly along the township line to the northeast corner of township fifteen (15) south, range nineteen (19) west; thence southerly along the range line to its intersection with the third (3d) standard parallel south; thence westerly along the third (3rd) standard parallel south to its intersection with the boundary line between New Mexico and Arizona; thence northerly along said boundary line to the point where it intersects the north line of township five (5) south, range twenty-one (21) west, the place of beginning.\"

","language":"English","publisher":"Government Printing Office","publisherLocation":"Washington D.C.","doi":"10.3133/pp39","usgsCitation":"Rixon, T.F., 1905, Forest conditions in the Gila River Forest Reserve, New Mexico: U.S. Geological Survey Professional Paper 39, Report: 89 p.; 1 Plate: 20 x 19 inches, https://doi.org/10.3133/pp39.","productDescription":"Report: 89 p.; 1 Plate: 20 x 19 inches","numberOfPages":"95","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":67107,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0039/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67108,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104451,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4389.htm","linkFileType":{"id":5,"text":"html"},"description":"4389"},{"id":120434,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0039/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Gila Forest Reserve","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.06677246093749,\n 32.519026027827515\n ],\n [\n -109.06677246093749,\n 34.21634468843465\n ],\n [\n -107.1990966796875,\n 34.21634468843465\n ],\n [\n -107.1990966796875,\n 32.519026027827515\n ],\n [\n -109.06677246093749,\n 32.519026027827515\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de37e","contributors":{"authors":[{"text":"Rixon, T. F.","contributorId":107358,"corporation":false,"usgs":true,"family":"Rixon","given":"T.","email":"","middleInitial":"F.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":221529,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1443,"text":"wsp145 - 1905 - Contributions to the hydrology of Eastern United States, 1905","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1905","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":"145","title":"Contributions to the hydrology of Eastern United States, 1905","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp145","usgsCitation":"Fuller, M.L., 1905, Contributions to the hydrology of Eastern United States, 1905: U.S. Geological Survey Water Supply Paper 145, 220 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp145.","productDescription":"220 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":137063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0145/report-thumb.jpg"},{"id":26536,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a7a0","contributors":{"authors":[{"text":"Fuller, M. L.","contributorId":24326,"corporation":false,"usgs":true,"family":"Fuller","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":143737,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1442,"text":"wsp110 - 1905 - Contributions to the hydrology of eastern United States, 1904","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1905","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":"110","title":"Contributions to the hydrology of eastern United States, 1904","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp110","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1905, Contributions to the hydrology of eastern United States, 1904: U.S. Geological Survey Water Supply Paper 110, 211 p. ;23 cm., https://doi.org/10.3133/wsp110.","productDescription":"211 p. ;23 cm.","costCenters":[],"links":[{"id":137062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0110/report-thumb.jpg"},{"id":26535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691294","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527846,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39493,"text":"pp32 - 1905 - Preliminary report on the geology and underground water resources of the central Great Plains","interactions":[],"lastModifiedDate":"2017-04-25T15:20:08","indexId":"pp32","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1905","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":"32","title":"Preliminary report on the geology and underground water resources of the central Great Plains","docAbstract":"

The area to which this report relates is shown in Pl. II.  It comprises the greater portions of South Dakota, Nebraska, and Kansas, and the eastern portions of Colorado and of Wyoming, an area of about one-half million square miles. It is the result of my investigations during the past eight years, but includes also all available data from many sources. I have been aided by various field assistants, those deserving special mention being Messrs. C. A. Fisher, C. C. O'Harra, J.E. Todd, the late C. M. Hall, G. B. Eichardson, W. S. Tangier Smith, E. H. Barbour, and the late J. E. Macfarland.

On account of its size, the region presents relatively diverse geologic conditions, but comprises comparatively few formations, most of which are widespread. The question of water supply, both overground and underground, is one of great interest to the people in this district, and although considerable progress has been made in some sections in developing well waters, there are vast areas in which the present supplies are inadequate, even for local domestic use. In order to understand the relations of the underground waters it has been necessary to investigate the geology, especially the structure and stratigraphy of the water-bearing and associated formations. This part of the work has required a very large amount of special field study, and the present results show that extended investigation will be required before many important questions of geology can be fully understood.

","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp32","usgsCitation":"Darton, N.H., 1905, Preliminary report on the geology and underground water resources of the central Great Plains: U.S. Geological Survey Professional Paper 32, Report: 433 p.; 2 Plates: 32.13 x 31.96 inches and 31.84 x 32.29 inches, https://doi.org/10.3133/pp32.","productDescription":"Report: 433 p.; 2 Plates: 32.13 x 31.96 inches and 31.84 x 32.29 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":67103,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0032/report.pdf","text":"Report","size":"66.05 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":120431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0032/report-thumb.jpg"},{"id":340373,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0032/plate-35.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":340372,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0032/plate-69.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Kansas, Nebraska, South Dakota, Wyoming","otherGeospatial":"Great Plains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {\n \"stroke\": \"#555555\",\n \"stroke-width\": 2,\n \"stroke-opacity\": 1,\n \"fill\": \"#555555\",\n \"fill-opacity\": 0.5\n },\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108,\n 43.2\n ],\n [\n -105.2,\n 42.2\n ],\n [\n -105.2,\n 37\n ],\n [\n -95.5,\n 37\n ],\n [\n -95.5,\n 45.5\n ],\n [\n -108,\n 45.5\n ],\n [\n -108,\n 43.2\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c908","contributors":{"authors":[{"text":"Darton, N. H.","contributorId":71523,"corporation":false,"usgs":true,"family":"Darton","given":"N.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":221523,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1441,"text":"wsp102 - 1904 - Contributions to the hydrology of eastern United States, 1903","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1904","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":"102","title":"Contributions to the hydrology of eastern United States, 1903","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp102","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1904, Contributions to the hydrology of eastern United States, 1903: U.S. Geological Survey Water Supply Paper 102, 522 p. ;23 cm., https://doi.org/10.3133/wsp102.","productDescription":"522 p. ;23 cm.","costCenters":[],"links":[{"id":137061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0102/report-thumb.jpg"},{"id":26534,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0102/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691272","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527845,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39525,"text":"pp22 - 1904 - Forest conditions in the San Francisco Mountains Forest Reserve, Arizona","interactions":[],"lastModifiedDate":"2015-09-15T13:06:55","indexId":"pp22","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1904","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":"22","title":"Forest conditions in the San Francisco Mountains Forest Reserve, Arizona","docAbstract":"

On April 12, 1902, President Roosevelt issued a proclamation \"for the purpose of consolidating into one reserve the lands heretofore embraced in the San Francisco Mountains Forest Reserves and of including therein the other adjacent lands within Francisco Mountains Forest Reserve, and is described by metes and bound as follows:

\n

''Beginning at the northwest corner of township twenty-two (22) north, range one (1) east, Gila and Salt River meridian, Arizona; thence southerly along the said meridian, allowing for the proper offset on the fifth (5th) standard parallel north, to the southwest corner of Township nineteen (19) south, range one (1) east; thence easterly along the surveyed and unsurveyed township line to the point for the northwest corner of township eighteen (18) north, range four (4) east; thence southerly along the unsurveyed range line to its intersection with the fourth (4th) standard' parallel north; thence easterly along said parallel to the point for the northwest corner of township sixteen (16) north, range five (5) east; thence southerly to the point for the southwest corner of said township; then easterly to the point for the northwest corne1· of township fifteen (15) north, range six (6) east; thence southerly to the point for the southwest corner of section eighteen (18), said township; thence easterly along the unsurveyed section line to the point for the northwest corner of section nineteen (19), township fifteen (15) north, range seven (7) east; thence southerly to the southwest corner of said section; thence easterly along the unsurveyed section lines to the southwest corner of section nineteen (19), township fifteen (15) north, range nine (9) east; thence northerly to the northwest corner of said section; thence easterly along the section line to the southeast corner of section thirteen (13), said township; thence northerly to the northeast corner of section twelve (12), said township; thence easterly along the section lines to the southeast corner of section one (1), township fifteen (15) north, range eleven (11) east; thence northerly along the range line to its intersection with the fourth (4th) standard parallel north; thence westerly along said parallel to the southeast corner of township seventeen (17) north, range eleven (11) east; thence northerly along the surveyed and unsurveyed range line to the point for the northeast corner of township eighteen (18) north, range eleven (11) east; thence westerly to the southeast corner of township nineteen (19) north, range ten (10) east; thence northerly along the range line to its intersection with the fifth (5th) standard parallel north; thence westerly along said parallel to the point for the southeast corner of township twenty-one (21) north, range nine (9) east; thence northerly along the unsurveyed range line, allowing for the proper offset on the sixth (6th) standard parallel north, to the point for the northeast cornet· of township twenty-five (25) north, range nine (9) east; thence westerly along the surveyed and unsurveyed township line to the point for the northwest corner of township twenty-five (25) north, range three (3) east; thence southerly along the surveyed and unsurveyed range line, allowing for the proper offset on the sixth (6th) standard parallel north, to the northeast corner of township twenty-two (22) north, range two (2) east; thence westerly along the township line to the northwest corner of township twenty-two (22) north, range one (1) east, to the place of beginning.\" 

","language":"English","publisher":"Government Printing Office","publisherLocation":"Washington D.C.","doi":"10.3133/pp22","usgsCitation":"Leiberg, J.B., Rixon, T.F., Dodwell, A., and Plummer, F.G., 1904, Forest conditions in the San Francisco Mountains Forest Reserve, Arizona: U.S. Geological Survey Professional Paper 22, 95 p., https://doi.org/10.3133/pp22.","productDescription":"95 p.","numberOfPages":"104","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":123269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0022/report-thumb.jpg"},{"id":67131,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","otherGeospatial":"San Francisco 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de35c","contributors":{"authors":[{"text":"Leiberg, J. B.","contributorId":14034,"corporation":false,"usgs":true,"family":"Leiberg","given":"J.","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":221570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rixon, T. F.","contributorId":107358,"corporation":false,"usgs":true,"family":"Rixon","given":"T.","email":"","middleInitial":"F.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":221572,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dodwell, Arthur","contributorId":9315,"corporation":false,"usgs":true,"family":"Dodwell","given":"Arthur","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":221569,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Plummer, F. G.","contributorId":96749,"corporation":false,"usgs":true,"family":"Plummer","given":"F.","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":221571,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":32878,"text":"pp31 - 1904 - Preliminary report on the geology of the Arbuckle and Wichita mountains in Indian Territory and Oklahoma","interactions":[],"lastModifiedDate":"2021-09-16T19:06:02.513093","indexId":"pp31","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1904","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":"31","title":"Preliminary report on the geology of the Arbuckle and Wichita mountains in Indian Territory and Oklahoma","docAbstract":"

The Arbuckle Mountains consist of a moderately elevated table -land or plateau in the east-central part of the Chickasaw Nation, Indian Territory. The plateau ranges in elevation from 1,300 feet above sea, in its contracted western part, to 750 feet, at the east end, where it coalesces with the bordering plain. Geologically the Arbuckle Mountain region consists of a great thickness of rocks, composed chiefly of limestones, which range in age from middle Cambrian to Devonian, and which are succeeded on the borders by an almost equal thickness of Carboniferous conglomerates, shales, and sandstones. In the central part of the district, unconformably beneath the Cambrian strata, there is a mass of granite, granite-porphyry, diabase, and associated crystalline rocks. The uplifting and folding of the region occurred previous to the deposition of the Permian \"Red Beds,\" which were deposited across it on the' west. The bearing of the Arbuckle uplift is approximately N. 70° W.

","language":"English","publisher":"Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp31","usgsCitation":"Taff, J.A., and Bain, H.F., 1904, Preliminary report on the geology of the Arbuckle and Wichita mountains in Indian Territory and Oklahoma: U.S. Geological Survey Professional Paper 31, 97 p., https://doi.org/10.3133/pp31.","productDescription":"97 p.","numberOfPages":"117","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":104426,"rank":699,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4292.htm","linkFileType":{"id":5,"text":"html"},"description":"4292"},{"id":268926,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0031/report.pdf"},{"id":163542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0031/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Arbuckle Mountains, Wichita Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -99.97558593749999,\n 33.94335994657882\n ],\n [\n -99.97558593749999,\n 35.8356283888737\n ],\n [\n -96.591796875,\n 35.8356283888737\n ],\n [\n -96.591796875,\n 33.94335994657882\n ],\n [\n -99.97558593749999,\n 33.94335994657882\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c8ef","contributors":{"authors":[{"text":"Taff, J. A.","contributorId":81467,"corporation":false,"usgs":true,"family":"Taff","given":"J.","email":"","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":209330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bain, H. F.","contributorId":30309,"corporation":false,"usgs":true,"family":"Bain","given":"H.","email":"","middleInitial":"F.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":209329,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32875,"text":"pp24 - 1904 - Zinc and lead deposits of northern Arkansas","interactions":[],"lastModifiedDate":"2021-08-19T18:43:57.096158","indexId":"pp24","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1904","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":"24","title":"Zinc and lead deposits of northern Arkansas","docAbstract":"

The field work on which this report is based was carried on during the months of July, August, and September, 1902. The writer was assisted by Prof. A. H. Purdue, of the University of Arkansas, and Mr. Ernest F. Burchard. The larger portion of the time was used in the detailed examination and study of the Yellville quadrangle, which is between 36° and 36° 30' and meridians 92° 30' and 93°, and embraces Marion County, the northern border of Searcy County, the eastern border of Boone County, and the northeastern corner of Newton County. The adjacent country, which is usually recognized as mineral bearing, was examined in a general way. Mr. E. O. Ulrich was in the field two weeks collecting fossils and studying the rocks for the purpose of correlation, and Dr. George H. Girty devoted a week to a portion of the section in an adjacent area.

","language":"English","publisher":"Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp24","usgsCitation":"Adams, G., Purdue, A., Burchard, E.F., and Ulrich, E.O., 1904, Zinc and lead deposits of northern Arkansas: U.S. Geological Survey Professional Paper 24, 118 p., https://doi.org/10.3133/pp24.","productDescription":"118 p.","numberOfPages":"173","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":388179,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4227.htm"},{"id":271250,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0024/report.pdf"},{"id":164278,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0024/report-thumb.jpg"}],"country":"United States","state":"Arkansas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.0,\n 36.0\n ],\n [\n -92.5,\n 36.0\n ],\n [\n -92.5,\n 36.5\n ],\n [\n -93.0,\n 36.5\n ],\n [\n -93.0,\n 36.0\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de3cb","contributors":{"authors":[{"text":"Adams, George I.","contributorId":64985,"corporation":false,"usgs":true,"family":"Adams","given":"George I.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":209324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Purdue, A. H.","contributorId":37631,"corporation":false,"usgs":true,"family":"Purdue","given":"A. H.","affiliations":[],"preferred":false,"id":209323,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burchard, E. F.","contributorId":104020,"corporation":false,"usgs":true,"family":"Burchard","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":209326,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ulrich, E. O.","contributorId":90167,"corporation":false,"usgs":true,"family":"Ulrich","given":"E.","email":"","middleInitial":"O.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":209325,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":998,"text":"wsp106 - 1904 - Water resources of the Philadelphia district","interactions":[],"lastModifiedDate":"2017-07-07T09:27:01","indexId":"wsp106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1904","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":"106","title":"Water resources of the Philadelphia district","docAbstract":"

The area included in the Philadelphia district lies between 39° 45' and 40° 15' north latitude and 75° and 75° 30' west longitude. It has a length of 34.50 miles from north to south and a width of 26.53 miles from east to west, and covers one-fourth of a square degree, which is equivalent, in that latitude, to, about 915.25 square miles. It is mapped on the Germantown, Norristown, Philadelphia, and Chester atlas sheets of the United States Geological Survey. a Each of these sheets represents a tract fifteen minutes in extent each way. This district is in Pennsylyania, New Jersey, and Delaware, and comprises, in whole or in part, ten counties-Bucks, Montgomery, Philadelphia, Delaware, and Chester counties in Pennsylvania; Burlington, Camden, Gloucester, and Salem counties in New Jersey; and Newcastle County in Delaware. A population of nearly 2,000,000 is embraced within these limits. The location and general relations of the district are shown in fig. 1, on the next page. In this paper will be discussed the topography, rainfall, run-off, and stream discharges of the chief hydrographic basins, the geology and water-bearing horizons, and the water power and water supply in relation to its present and future utilization.

","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp106","usgsCitation":"Bascom, F., 1904, Water resources of the Philadelphia district: U.S. Geological Survey Water Supply Paper 106, 75 p. :illus., 4 pl. (incl. map) ;23 cm., https://doi.org/10.3133/wsp106.","productDescription":"75 p. :illus., 4 pl. (incl. map) ;23 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":136015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0106/report-thumb.jpg"},{"id":25569,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0106/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602b8a","contributors":{"authors":[{"text":"Bascom, Florence","contributorId":107668,"corporation":false,"usgs":true,"family":"Bascom","given":"Florence","email":"","affiliations":[],"preferred":false,"id":142993,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}