This collection of 60 short papers on subjects in the fields of geology, hydrology, topography, and related sciences is the third of a series to be released during the year as chapters of Professional Paper 450. The papers in this chapter report on the scientific and economic results of current work by members of the Geologic, Water Resources, and Topographic Divisions of the United States Geologicai Survey. Some of the papers announce new discoveries or present observations on problems of limited scope; other papers draw conclusions from more extensive or continuing investigations that in large part will be discussed in greater detail in reports to be published in the future.
Chapter A of this series, to be published later in the year, will present a synopsis of results from a wide range of work done during the present fiscal year.
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the Erda area, Tooele Valley, Utah","linkFileType":{"id":5,"text":"html"}},{"id":480878,"rank":24,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28319.htm","text":"Restudy of the Arrowhead fault, Muddy Mountains, Nevada","linkFileType":{"id":5,"text":"html"}},{"id":480879,"rank":25,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28320.htm","text":"Correlation of granitic plutons across faulted Owens Valley, California","linkFileType":{"id":5,"text":"html"}},{"id":480880,"rank":26,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28321.htm","text":"Structural control of interior drainage, southern San Joaquin Valley, California","linkFileType":{"id":5,"text":"html"}},{"id":480881,"rank":27,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28322.htm","text":"Zinc occurrence in the Serpent Mound structure of southern Ohio","linkFileType":{"id":5,"text":"html"}},{"id":480882,"rank":28,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28323.htm","text":"Faulted Pleistocene strata near Jackson, northwestern Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":480883,"rank":29,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28324.htm","text":"Potential yield of deep water wells in the southern part of the Jicarilla Apache Indian Reservation and vicinity, San Juan Basin, New Mexico","linkFileType":{"id":5,"text":"html"}},{"id":480859,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28300.htm","text":"Precambrian(?) and Cambrian stratigraphy in Esmeralda County, Nevada","linkFileType":{"id":5,"text":"html"}},{"id":480860,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28301.htm","text":"Age and sequence of metasedimentary and metavolcanic formations northwest of New Haven, Connecticut","linkFileType":{"id":5,"text":"html"}},{"id":480861,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28302.htm","text":"The Eagle Valley Evaporite and its relation to the Minturn and Maroon Formations, northwest Colorado","linkFileType":{"id":5,"text":"html"}},{"id":480862,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28303.htm","text":"Jurassic stratigraphy in the McCarthy C-5 quadrangle, Alaska","linkFileType":{"id":5,"text":"html"}},{"id":480863,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28304.htm","text":"Some Late Cretaceous strand lines in southern Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":480864,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28305.htm","text":"Tertiary volcanic and related rocks of the Republic area, Ferry County, Washington","linkFileType":{"id":5,"text":"html"}},{"id":480865,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28306.htm","text":"Geology of Tertiary rocks in Escambia and Santa Rosa Counties, western Florida","linkFileType":{"id":5,"text":"html"}},{"id":480866,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28307.htm","text":"Stratigraphy and hydrology of the Juana Diaz Formation in the Yauco area, Puerto Rico","linkFileType":{"id":5,"text":"html"}},{"id":480867,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28308.htm","text":"Pyroclastic deposits of recent age at Mount Rainier, Washington","linkFileType":{"id":5,"text":"html"}},{"id":480868,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28309.htm","text":"The Pine Mountain overthrust at the northeast end of the Powell Valley anticline, Virginia","linkFileType":{"id":5,"text":"html"}},{"id":480869,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28310.htm","text":"Gravity and magnetic anomalies in Gem Valley, Carbon County, Idaho","linkFileType":{"id":5,"text":"html"}},{"id":480871,"rank":17,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28312.htm","text":"Precambrian gabbro in the central Front Range, Colorado [Keyser Creek area]","linkFileType":{"id":5,"text":"html"}},{"id":480872,"rank":18,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28313.htm","text":"Precambrian gabbro in the central Front Range, Colorado [Apex area]","linkFileType":{"id":5,"text":"html"}},{"id":480873,"rank":19,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28314.htm","text":"Configuration of the bedrock beneath the channel of the lower Merrimack River, Massachusetts","linkFileType":{"id":5,"text":"html"}},{"id":480874,"rank":20,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28315.htm","text":"Geology of Pleistocene deposits of Lake County, Indiana","linkFileType":{"id":5,"text":"html"}},{"id":480875,"rank":21,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28316.htm","text":"Geology of the Vermilion end moraine, Nett Lake Indian Reservation, Minnesota","linkFileType":{"id":5,"text":"html"}},{"id":480884,"rank":30,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93398.htm","text":"The pre-Bull Lake tills in the Wind River Mountains, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":480885,"rank":31,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93399.htm","text":"Cambrian Carrara Formation, Bonanza King Formation, and Dunderberg Shale east of Yucca Flat, Nye County, Nevada","linkFileType":{"id":5,"text":"html"}},{"id":480886,"rank":32,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93405.htm","text":"Age of the Leadville Limestone in the Glenwood Canyon, western Colorado","linkFileType":{"id":5,"text":"html"}},{"id":480887,"rank":33,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_100150.htm","text":"New members of the Bloyd Formation of Pennsylvanian age, Washington County, Arkansas","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3f29","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":529442,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1115,"text":"wsp1535G - 1962 - Rainwater as a chemical agent of geologic processes; a review","interactions":[],"lastModifiedDate":"2013-08-12T12:37:51","indexId":"wsp1535G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1535","chapter":"G","title":"Rainwater as a chemical agent of geologic processes; a review","docAbstract":"Chemical analyses of the rainwater collected at several localities are given to show the variations of the principal constitutents. In rock weathering and soil-forming processes, the chemical composition of rainwater has an important effect which has been evaluated for only a few arid areas. In humid regions the important amounts of calcium, magnesium, sodium, and potassium added yearly by rain may be expected to influence the composition of the soil water and thereby the cations in the exchange positions of soil clay minerals. The acquisition of cations by clay minerals may slow down chemical weathering. The stability of soil clay minerals is influenced by the constant accession of cations from rainwater. Conversely, the clay minerals modify the amounts and kinds of cations that are leached out by drainage waters. The stability of micaceous minerals in soils may be partly due to accessions of K +1 ions from rainwater. \n\nThe pH of rainwater in any area varies considerably and seems to form a seasonal and regional pattern. The recorded pH values range from 3.0 to 9.8.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1535G","usgsCitation":"Carroll, D., 1962, Rainwater as a chemical agent of geologic processes; a review: U.S. Geological Survey Water Supply Paper 1535, 18 p., 1 leaf of plates ;23 cm. Reprinted 1965, https://doi.org/10.3133/wsp1535G.","productDescription":"18 p., 1 leaf of plates ;23 cm. Reprinted 1965","costCenters":[],"links":[{"id":138099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1535g/report-thumb.jpg"},{"id":25877,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1535g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":276517,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1535g/plate-1.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649593","contributors":{"authors":[{"text":"Carroll, Dorothy","contributorId":38534,"corporation":false,"usgs":true,"family":"Carroll","given":"Dorothy","email":"","affiliations":[],"preferred":false,"id":143201,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37554,"text":"ssrw66 - 1962 - Recent approaches to Canada goose management","interactions":[],"lastModifiedDate":"2012-02-02T00:10:00","indexId":"ssrw66","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"66","title":"Recent approaches to Canada goose management","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Nelson, H.K., 1962, Recent approaches to Canada goose management: Special Scientific Report - Wildlife 66, 25 p.","productDescription":"25 p.","costCenters":[],"links":[{"id":110882,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924055486744?urlappend=%3Bseq=7"},{"id":162814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485ac","contributors":{"authors":[{"text":"Nelson, Harvey K.","contributorId":101295,"corporation":false,"usgs":true,"family":"Nelson","given":"Harvey","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":218245,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37553,"text":"ssrw65 - 1962 - Waterfowl populations in the Upper Chesapeake region","interactions":[],"lastModifiedDate":"2016-07-11T07:35:32","indexId":"ssrw65","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"65","title":"Waterfowl populations in the Upper Chesapeake region","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Stewart, R., 1962, Waterfowl populations in the Upper Chesapeake region: Special Scientific Report - Wildlife 65, 208 p.; 3 maps.","productDescription":"208 p.; 3 maps","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":162813,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":110881,"rank":9999,"type":{"id":15,"text":"Index Page"},"url":"https://digital.library.unt.edu/ark:/67531/metadc100532/"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4b96","contributors":{"authors":[{"text":"Stewart, Robert E.","contributorId":84813,"corporation":false,"usgs":true,"family":"Stewart","given":"Robert E.","affiliations":[],"preferred":false,"id":218244,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1045,"text":"wsp1594B - 1962 - Experiments in water spreading at Newark, Delaware","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1594B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1594","chapter":"B","title":"Experiments in water spreading at Newark, Delaware","docAbstract":"Two experiments in water spreading were made at Newark, Del., to evaluate the prospects of using excess storm runoff to recharge the shallow water-table aquifer which serves the community. Water was diverted from 1 of the city's 3 production wells and released into an infiltration ditch near the municipal well field. \r\n\r\nAlthough slightly more than 65,000 cubic feet of water (nearly 500,000 gallons ) was spread in the infiltration ditch and allowed to seep into the subsurface, there was no indication that any appreciable amount of water reached the producing aquifer. Instead, a perched zone of saturation was created by the presence of an impermeable or slightly permeable bed above the water table. So effective is this barrier to the downward movement of water that within a period of less than 1 day, the apex of the perched zone rose about 10 feet to the level of the bottom of the infiltration ditch. As more water was added, the mound of saturation spread laterally. \r\n\r\nOn the basis of these experiments, it appears that the principal aquifer at Newark, Del., would not be benefited by spreading water in shallow infiltration ditches or basins. However, the absorptive capacity of the unsaturated materials which occur at a shallow depth, is sufficient to permit the disposal of large volumes of storm runoff.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1594B","usgsCitation":"Boggess, D.H., and Rima, D.R., 1962, Experiments in water spreading at Newark, Delaware: U.S. Geological Survey Water Supply Paper 1594, 15 p. :illus., map., https://doi.org/10.3133/wsp1594B.","productDescription":"15 p. :illus., map.","costCenters":[],"links":[{"id":137901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1594b/report-thumb.jpg"},{"id":25708,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1594b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25709,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1594b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c21","contributors":{"authors":[{"text":"Boggess, Durward Haye","contributorId":102049,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"Haye","affiliations":[],"preferred":false,"id":143085,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rima, Donald Robert","contributorId":99535,"corporation":false,"usgs":true,"family":"Rima","given":"Donald","email":"","middleInitial":"Robert","affiliations":[],"preferred":false,"id":143084,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":64687,"text":"i359 - 1962 - Geologic map of lower Matanuska Valley, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:13:06","indexId":"i359","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"359","subseriesTitle":"NONE","title":"Geologic map of lower Matanuska Valley, Alaska","language":"ENGLISH","doi":"10.3133/i359","usgsCitation":"Barnes, F., 1962, Geologic map of lower Matanuska Valley, Alaska: U.S. Geological Survey IMAP 359, 1 map ;44 x 56 cm. on sheet 86 x 121 cm. folded in envelope 31 x 24 cm., https://doi.org/10.3133/i359.","productDescription":"1 map ;44 x 56 cm. on sheet 86 x 121 cm. folded in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":111252,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/13609","linkFileType":{"id":5,"text":"html"}},{"id":255117,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0359/plate-1.pdf","size":"20126","linkFileType":{"id":1,"text":"pdf"}},{"id":255118,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0359/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":255119,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0359/report-thumb.jpg"}],"scale":"63360","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2906","contributors":{"authors":[{"text":"Barnes, F.F.","contributorId":87198,"corporation":false,"usgs":true,"family":"Barnes","given":"F.F.","email":"","affiliations":[],"preferred":false,"id":271985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32744,"text":"pp382B - 1962 - Geologic effects of the high-explosive tests in the USGS Tunnel area, Nevada Test Site","interactions":[],"lastModifiedDate":"2012-02-02T00:09:10","indexId":"pp382B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"382","chapter":"B","title":"Geologic effects of the high-explosive tests in the USGS Tunnel area, Nevada Test Site","language":"ENGLISH","doi":"10.3133/pp382B","usgsCitation":"Cattermole, J.M., and Hansen, W.R., 1962, Geologic effects of the high-explosive tests in the USGS Tunnel area, Nevada Test Site: U.S. Geological Survey Professional Paper 382, p. B1-B31, https://doi.org/10.3133/pp382B.","productDescription":"p. B1-B31","costCenters":[],"links":[{"id":119249,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0382b/report-thumb.jpg"},{"id":60666,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0382b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60667,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0382b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60668,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0382b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60669,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0382b/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60670,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0382b/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60671,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0382b/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60672,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0382b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d88","contributors":{"authors":[{"text":"Cattermole, J. M.","contributorId":6909,"corporation":false,"usgs":true,"family":"Cattermole","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":209083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, W. R.","contributorId":59378,"corporation":false,"usgs":true,"family":"Hansen","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":209084,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":930,"text":"wsp1576B - 1962 - Geology and ground water of the Red Lake area, Navajo Indian Reservation, Arizona and New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1576B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1576","chapter":"B","title":"Geology and ground water of the Red Lake area, Navajo Indian Reservation, Arizona and New Mexico","docAbstract":"The Red Lake area in the Navajo Indian Reservation, Arizona and New \r\nMexico, was studied by the U.S. Geological Survey to determine if 1 mgd (mil- \r\nlion gallons per day) of water could be obtained for the requirements of a \r\nproposed sawmill. Geologic mapping and stratigraphic studies indicated three \r\nfavorable areas where ground water may be developed. Test holes were drilled \r\nunder contract in the areas, and pumping tests indicate that 500,000 gpd (gal- \r\nlons per day) is available from alluvium along Tohdildonih Wash near Frog \r\nRock, 100,000 gpd is available from the Shinarump member of the Chinle forma- \r\ntion and the De Chelly sandstone near Red Lake, and 800,000 gpd is available \r\nfrom alluvium and cinder beds in lapiUi tuff in Buell Park, an eroded diatreme. \r\nThe diatreme at Buell Park is about 2% miles in diameter. It was formed \r\nby several explosions in which lapilli tuff and cinders were erupted. These \r\nmaterials, together with later basaltic intrusive and extrusive rock, now fill \r\nthe diatreme. The tuff and cinders are water bearing, 'and they receive re- \r\ncharge from rainwater and snowmelt moving through overlying alluvium and \r\nfrom storage in the De Chelly sandstone which encloses the east half of the \r\ndiatreme. \r\nThe quality of water from all areas is suitable for domestic use. 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