{"pageNumber":"5416","pageRowStart":"135375","pageSize":"25","recordCount":184776,"records":[{"id":65848,"text":"i1295 - 1981 - Shaded relief map of the Coprates Northwest Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:17","indexId":"i1295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1295","subseriesTitle":"NONE","title":"Shaded relief map of the Coprates Northwest Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1295","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Shaded relief map of the Coprates Northwest Quadrangle of Mars: U.S. Geological Survey IMAP 1295, 1 remote-sensing image :col. ;30 x 60 cm. on sheet 86 x 67 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1295.","productDescription":"1 remote-sensing image :col. ;30 x 60 cm. on sheet 86 x 67 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101202,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1295/plate-1.pdf","size":"8324","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f473a","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":534203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8759,"text":"ofr811125 - 1981 - Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective","interactions":[],"lastModifiedDate":"2022-08-31T19:15:57.552529","indexId":"ofr811125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1125","title":"Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective","docAbstract":"<p>The channels of the Platte River and its major tributaries, the South Platte and North Platte Rivers in Colorado, Wyoming, and Nebraska, have undergone major changes in hydrologic regime and morphology since 1860. These changes are attributed here to agricultural, municipal, and industrial water use.</p><p>Although water-resource development varied temporally throughout the basin, the history of development along the Platte River and tributaries followed four stages: (1) Construction of small, crude ditches to irrigate flood plains; (2) construction of larger canals to irrigate bench lands; (3) construction of reservoirs to store snowmelt runoff; and (4) accelerated development of ground-water resources. Despite differences in rates of development, diversion and storage of water for irrigation, municipal, and industrial use have changed streamflow patterns throughout the basin. At some stations, significant changes in flood peaks, annual mean discharges, and shapes of flow-duration curves have been recorded.</p><p>Changes in streamflow patterns are manifested by changes in appearance of channels of the Platte River. Prior to water development in the 19th century, the Platte was a wide (-2 kilometers), shallow (1.8 to 2.4 meters) river characterized by bankfull spring flows and low summer flows. Although timber generally was scarce in the valley, the Platte channels contained hundreds of small, timbered islands. Since development, the channels have changed radically. Comparing surveyor's maps (General Land Office), drawn during the 1860's, with six sets of aerial photographs, taken between 1938 and 1979, for six 5-kilometer reaches of the river shows that the channels have narrowed considerably above the confluence with the Loup River. The width of the channels in 1979 ranged from 8 to 50 percent of the channel width in 1860. Below the confluence with the Loup River, the width of the river in 1979 was about 92 percent of the channel width in 1860. Above the confluence with the Loup River, width reduction has occurred by progressive encroachment of vegetation and consequent vertical and horizontal accretion on sand bars in the channel. Vegetative encroachment on sand bars has occurred because (1) the present hydrologic regime provides more favorable conditions for germination and growth on sand bars, and (2) since development of the basin, flood peaks are no longer capable of scouring vegetation from the sand bars. Overbank flows evidently have become more common, probably because channel narrowing and vegetative encroachment have increased the hydraulic roughness of the channels. Moreover, the magnitude of low flows has increased and the days of no flows has decreased giving the channels a more perennial character.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811125","usgsCitation":"Eschner, T., Hadley, R.F., and Crowley, K., 1981, Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective: U.S. Geological Survey Open-File Report 81-1125, v, 57 p., https://doi.org/10.3133/ofr811125.","productDescription":"v, 57 p.","costCenters":[],"links":[{"id":406027,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1125/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1125/report-thumb.jpg"}],"country":"United States","state":"Colorado, Nebraska, Wyoming","otherGeospatial":"Platte River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.67675781249999,\n              39.57182223734374\n            ],\n            [\n              -95.9326171875,\n              39.57182223734374\n            ],\n            [\n              -95.9326171875,\n              43.99281450048989\n            ],\n            [\n              -108.67675781249999,\n              43.99281450048989\n            ],\n            [\n              -108.67675781249999,\n              39.57182223734374\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6117ba","contributors":{"authors":[{"text":"Eschner, T.R.","contributorId":45700,"corporation":false,"usgs":true,"family":"Eschner","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":158281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":158280,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crowley, K.D.","contributorId":86769,"corporation":false,"usgs":true,"family":"Crowley","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":158282,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30250,"text":"wri8090 - 1981 - Geology and hydrology for environmental planning in Marquette County, Michigan","interactions":[],"lastModifiedDate":"2017-07-12T11:01:07","indexId":"wri8090","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"80-90","title":"Geology and hydrology for environmental planning in Marquette County, Michigan","docAbstract":"<p>Marquette County, in the glaciated area of the Upper Peninsula of Michigan, includes 1,878 square miles. Precipitation averages 32 inches per year. </p><p>Bedrock and glacial deposits contain materials that are good aquifers. Sedimentary bedrock units generally yield sufficient water for domestic supply and, in places, may yield more than 100 gallons per minute to large-diameter wells. In the glacial deposits, sand and gravel beds are the principal aquifers; yields to wells range from less than 10 to 200 gallons per minute. Igneous and metamorphic rocks yield little or no water to wells. </p><p>Suitable sewage and refuse disposal sites are not readily available because of the abundance of wetlands, streams, and lakes susceptible to infiltrating leachate.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reson, VA","doi":"10.3133/wri8090","usgsCitation":"Twenter, F.R., 1981, Geology and hydrology for environmental planning in Marquette County, Michigan: U.S. Geological Survey Water-Resources Investigations Report 80-90, viii, 44 p., https://doi.org/10.3133/wri8090.","productDescription":"viii, 44 p.","numberOfPages":"55","costCenters":[{"id":382,"text":"Michigan Water Science 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sgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6852a5","contributors":{"authors":[{"text":"Twenter, F. R.","contributorId":81080,"corporation":false,"usgs":true,"family":"Twenter","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202932,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61407,"text":"mf860 - 1981 - Preliminary geologic map of the McCarthy Gulch Quadrangle, Rio Blanco and Garfield Counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"mf860","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"860","title":"Preliminary geologic map of the McCarthy Gulch Quadrangle, Rio Blanco and Garfield Counties, Colorado","language":"ENGLISH","doi":"10.3133/mf860","usgsCitation":"O'Sullivan, R.B., Wahl-Pierce, F., and Arbelbide, S., 1981, Preliminary geologic map of the McCarthy Gulch Quadrangle, Rio Blanco and Garfield Counties, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 860, 1 map ;57 x 45 cm. on sheet 81 x 129 cm., https://doi.org/10.3133/mf860.","productDescription":"1 map ;57 x 45 cm. on sheet 81 x 129 cm.","costCenters":[],"links":[{"id":104327,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4046.htm","linkFileType":{"id":5,"text":"html"},"description":"4046"},{"id":187421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":88962,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1981/0860/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.11749999999999,39.6175 ], [ -108.11749999999999,39.75 ], [ -108,39.75 ], [ -108,39.6175 ], [ -108.11749999999999,39.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b098","contributors":{"authors":[{"text":"O'Sullivan, R. B.","contributorId":57858,"corporation":false,"usgs":true,"family":"O'Sullivan","given":"R.","middleInitial":"B.","affiliations":[],"preferred":false,"id":265596,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wahl-Pierce, Frances","contributorId":12931,"corporation":false,"usgs":true,"family":"Wahl-Pierce","given":"Frances","email":"","affiliations":[],"preferred":false,"id":265594,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arbelbide, S.J.","contributorId":32610,"corporation":false,"usgs":true,"family":"Arbelbide","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":265595,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":65436,"text":"i1399 - 1981 - Controlled photomosaic of the Cebrenia Southeast Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:14","indexId":"i1399","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1399","subseriesTitle":"NONE","title":"Controlled photomosaic of the Cebrenia Southeast Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1399","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Controlled photomosaic of the Cebrenia Southeast Quadrangle of Mars: U.S. Geological Survey IMAP 1399, 1 map ;53 x 60 cm., https://doi.org/10.3133/i1399.","productDescription":"1 map ;53 x 60 cm.","costCenters":[],"links":[{"id":114923,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1399/report.pdf","size":"26","linkFileType":{"id":1,"text":"pdf"}},{"id":114924,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1399/plate-1.pdf","size":"8063","linkFileType":{"id":1,"text":"pdf"}},{"id":190464,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1399/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688bee","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":533823,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5842,"text":"pp1202 - 1981 - Deformation of host rocks and flow of magma during growth of minette dikes and breccia-bearing intrusions near Ship Rock, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp1202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1202","title":"Deformation of host rocks and flow of magma during growth of minette dikes and breccia-bearing intrusions near Ship Rock, New Mexico","docAbstract":"We have studied a small group of minette dikes and plugs that crop out within a flat-lying sequence of siltstone and shale near Ship Rock, a prominent volcanic throat of tuff breccia in northwestern New Mexico. Seven dikes form a radial pattern about Ship Rock we describe in detail the northeastern dike, which has an outcrop length of about 2,900 m, an average thickness of 2.3 m, and a maximum thickness of 7.2 m. The dike is composed of 35 discrete segments arranged in echelon; orientation. of dike segments ranges systematically from N. 52? E. to N. 66? E. A prominent joint set strikes parallel to the segments and is localized within several tens of meters of the dike. Regional joint patterns display no obvious relation to dike orientation. Small offsets of segment contacts, as well as wedge-shaped bodies of crumpled host rock within segments mark the sites of coalescence of smaller segments during dike growth. Bulges in the dike contact, which represent a nondilational component of growth, indicate that wall rocks were brecciated and eroded during the flow of magma. Breccias make up about 9 percent of the 7,176-m 2 area of the dike, are concentrated in its southwest half, and are commonly associated with its thickest parts. We also describe three subcircular plugs; each plug is smaller than 30 m in diameter, is laterally associated with a dike, and contains abundant breccias. Field evidence indicates that these plugs grew from the dikes by brecciation and erosion of wallrocks and that the bulges in the contact of the northeastern dike represent an initial stage of this process. \r\n\r\nFrom continuum-mechanical models of host-rock deformation, we conclude that dike propagation was the dominant mechanism for creating conduits for magma ascent where the host rock was brittle and elastic. At a given driving pressure, dikes dilate to accept greater volumes of magma than plugs, and for a given dilation, less work is done on the host rocks. In addition, the pressure required for dike growth decreases with dike length. From numerical solutions for dilation of cracks oriented like segments of the northeastern dike, we find that we can best model the form of the dike by treating it as composed of 10 cracks rather than 35. We attribute this result to coalescence of adjacent segments below the present outcrop and to inelastic deformation at segment ends. Using a driving pressure of 2 MPa (20 bars), we estimate a shear modulus of about 10^3 MPa for the host rocks, in agreement with laboratory tests on soft shale. A propagation criterion based on stress intensity at the segment ends indicates a fracture toughness of the host rocks of about 100 MPa-m^? , a hundredfold greater than values reported from laboratory tests. Segmentation of fractures is common in many materials and has been observed during fissure eruptions at Kilauea Volcano in Hawaii. At the northeastern dike, we attribute segmentation to local rotation of the direction of least principal compressive stress. \r\n\r\nFrom continuum-mechanical models of magma and heat flow in idealized conduits, we conclude that magma flows far more rapidly and with less relative heat loss in plugs than in dikes. Although dikes are the preferred form for emplacement, plugs are the preferred form for the flow of magma. We present a numerical solution for volumetric flow rate and wall heat flux for the northeastern dike and find that although the flow rate is extremely sensitive to conduit geometry, the rate of heat loss to wall rocks is not. During emplacement of the northeastern dike, local flow rate increased where wall rocks were eroded and reached a maximum of about 45 times the mean initial rate, whereas the maximum rate of heat loss to wallrocks increased to only 1.6 times the mean initial rate. An inferred progression from continuous magma flow along a dike to flow from a plug agrees well with observations of volcanic eruptions that begin from fissures and later are localized at discrete vents. 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,{"id":65442,"text":"i1358 - 1981 - Controlled photomosaic of the Diacria Southwest Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:16","indexId":"i1358","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1358","subseriesTitle":"NONE","title":"Controlled photomosaic of the Diacria Southwest Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1358","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Controlled photomosaic of the Diacria Southwest Quadrangle of Mars: U.S. Geological Survey IMAP 1358, 1 map ;52 x 60 cm., https://doi.org/10.3133/i1358.","productDescription":"1 map ;52 x 60 cm.","costCenters":[],"links":[{"id":189853,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260765,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1358/plate-1.pdf"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688bb3","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":533829,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9696,"text":"ofr81140 - 1981 - Fluoride concentrations in water from four principal coastal plain aquifer systems, South Carolina","interactions":[],"lastModifiedDate":"2022-03-14T16:24:46.592512","indexId":"ofr81140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-140","title":"Fluoride concentrations in water from four principal coastal plain aquifer systems, South Carolina","docAbstract":"<p>Ample supplies of ground water are available throughout most of the Coastal Plain of South Carolina, but in many places the fluoride concentrations far exceed (as high as 5.8 mg/L, milligrams per liter) the MCL (maximum concentration limit) established for drinking water by the EPA (U.S. Environmental Protection Agency) and SCDHEC (South Carolina Department of Health and Environmental Control).</p><p>Fluoridation of drinking water for the prevention of dental caries is a well known practice in many parts of the country. Low concentrations of fluoride have an apparent beneficial effect whereas high concentrations may cause dental fluorosis (mottled teeth enamel) in young children. The recommended concentration of fluoride, as established by EPA (1975) in South Carolina ranges from 1.4 to about 2.4 mg/L depending on the daily air temperature (tables 1 and 2). A lower fluoride concentration in drinking water is considered optimum in areas of high air temperature because generally more water is consumed by individuals in these areas. The total fluoride intake in a warm area where the concentration is low, therefore, will be approximately the same as in a cooler area where the concentration is higher. However, it has been established by SCDHEC that the MCL for fluoride in public drinking water in the coastal areas will be 1.6 mg/L (R. Lewis Shaw, written commun., 1976).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81140","collaboration":"Prepared in cooperation with the South Carolina Department of Health and Environmental Control","usgsCitation":"Johnson, P.W., and Rhett, J., 1981, Fluoride concentrations in water from four principal coastal plain aquifer systems, South Carolina: U.S. Geological Survey Open-File Report 81-140, iii, 11 p., https://doi.org/10.3133/ofr81140.","productDescription":"iii, 11 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":397057,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0140/report-thumb.jpg"}],"country":"United States","state":"South 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,{"id":65470,"text":"i1348 - 1981 - Controlled photomosaic of the Mare Acidalium Northeast Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:08","indexId":"i1348","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1348","subseriesTitle":"NONE","title":"Controlled photomosaic of the Mare Acidalium Northeast Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1348","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Controlled photomosaic of the Mare Acidalium Northeast Quadrangle of Mars: U.S. Geological Survey IMAP 1348, 1 map ;53 x 59 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1348.","productDescription":"1 map ;53 x 59 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":114947,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1348/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":114948,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1348/plate-1.pdf","size":"7852","linkFileType":{"id":1,"text":"pdf"}},{"id":189596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1348/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688208","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":533857,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10411,"text":"ofr81315 - 1981 - Vegetation mapping of the National Petroleum Reserve in Alaska using Landsat digital data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr81315","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-315","title":"Vegetation mapping of the National Petroleum Reserve in Alaska using Landsat digital data","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81315","usgsCitation":"Morrissey, L., and Ennis, R., 1981, Vegetation mapping of the National Petroleum Reserve in Alaska using Landsat digital data: U.S. Geological Survey Open-File Report 81-315, 27 p.  ;28 cm., https://doi.org/10.3133/ofr81315.","productDescription":"27 p.  ;28 cm.","numberOfPages":"27","costCenters":[],"links":[{"id":143859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0315/report-thumb.jpg"},{"id":38271,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0315/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602528","contributors":{"authors":[{"text":"Morrissey, L.A.","contributorId":34136,"corporation":false,"usgs":true,"family":"Morrissey","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":161341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ennis, R.A.","contributorId":69151,"corporation":false,"usgs":true,"family":"Ennis","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":161342,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9268,"text":"ofr8143 - 1981 - Preliminary results of coal exploratory drilling in the Book Cliffs coal field, Grand County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr8143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-43","title":"Preliminary results of coal exploratory drilling in the Book Cliffs coal field, Grand County, Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8143","usgsCitation":"Gualtieri, J.L., 1981, Preliminary results of coal exploratory drilling in the Book Cliffs coal field, Grand County, Utah: U.S. Geological Survey Open-File Report 81-43, 2 well logs ;on sheets 301 x 31 and 239 x 31 cm. +legend on sheet 78 x 78 cm. and text (ii, 26 leaves ; 28 cm.); (28 p., 3 over-size sheets, scale 1:50,000 - PGS), https://doi.org/10.3133/ofr8143.","productDescription":"2 well logs ;on sheets 301 x 31 and 239 x 31 cm. +legend on sheet 78 x 78 cm. and text (ii, 26 leaves ; 28 cm.); (28 p., 3 over-size sheets, scale 1:50,000 - PGS)","costCenters":[],"links":[{"id":141213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0043/report-thumb.jpg"},{"id":36963,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0043/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36964,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0043/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36965,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0043/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36966,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0043/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"50000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b376","contributors":{"authors":[{"text":"Gualtieri, James Louis","contributorId":46491,"corporation":false,"usgs":true,"family":"Gualtieri","given":"James","email":"","middleInitial":"Louis","affiliations":[],"preferred":false,"id":159390,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61371,"text":"mf855 - 1981 - Reconnaissance bedrock geologic map of the Ashfield quadrangle, Franklin County, Massachusetts","interactions":[],"lastModifiedDate":"2022-04-11T18:42:53.817121","indexId":"mf855","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"855","title":"Reconnaissance bedrock geologic map of the Ashfield quadrangle, Franklin County, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf855","usgsCitation":"Hatch, N.L., 1981, Reconnaissance bedrock geologic map of the Ashfield quadrangle, Franklin County, Massachusetts: U.S. Geological Survey Miscellaneous Field Studies Map 855, 1 Plate: 42.94 × 30.49 inches, https://doi.org/10.3133/mf855.","productDescription":"1 Plate: 42.94 × 30.49 inches","costCenters":[],"links":[{"id":187171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":276315,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0855/plate-1.pdf"},{"id":398497,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4035.htm"}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Franklin County","otherGeospatial":"Ashfield quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.875,\n              42.5\n            ],\n            [\n              -72.75,\n              42.5\n            ],\n            [\n              -72.75,\n              42.625\n            ],\n            [\n              -72.875,\n              42.625\n            ],\n            [\n              -72.875,\n              42.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db64479d","contributors":{"authors":[{"text":"Hatch, N. L. Jr.","contributorId":58663,"corporation":false,"usgs":true,"family":"Hatch","given":"N.","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":265529,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67714,"text":"l154 - 1981 - Land use and land cover, 1974-75, Medford, Oregon; California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"l154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":321,"text":"Land Use and Land Cover","code":"L","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"154","title":"Land use and land cover, 1974-75, Medford, Oregon; California","language":"ENGLISH","doi":"10.3133/l154","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Land use and land cover, 1974-75, Medford, Oregon; California: U.S. Geological Survey Land Use and Land Cover 154, -, https://doi.org/10.3133/l154.","productDescription":"-","costCenters":[],"links":[{"id":186292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":261021,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/154/plate-1.pdf"}],"scale":"1","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,42 ], [ -123,42.5 ], [ -122,42.5 ], [ -122,42 ], [ -123,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae339","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":534460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67629,"text":"l192 - 1981 - Land use and land cover, 1971-75, Madison, Wisconsin","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"l192","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":321,"text":"Land Use and Land Cover","code":"L","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"192","title":"Land use and land cover, 1971-75, Madison, Wisconsin","language":"ENGLISH","doi":"10.3133/l192","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Land use and land cover, 1971-75, Madison, Wisconsin: U.S. Geological Survey Land Use and Land Cover 192, -, https://doi.org/10.3133/l192.","productDescription":"-","costCenters":[],"links":[{"id":188302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260934,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/192/plate-1.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90,43 ], [ -90,44 ], [ -88,44 ], [ -88,43 ], [ -90,43 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae9f6","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":534375,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28236,"text":"wri80116 - 1981 - User's guide for a general purpose dam-break flood simulation model (K-634)","interactions":[],"lastModifiedDate":"2020-05-22T17:40:39.359024","indexId":"wri80116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"80-116","title":"User's guide for a general purpose dam-break flood simulation model (K-634)","docAbstract":"An existing computer program for simulating dam-break floods for forecast purposes has been modified with an emphasis on general purpose applications. The original model was formulated, developed and documented by the National Weather Service. This model is based on the complete flow equations and uses a nonlinear implicit finite-difference numerical method. The first phase of the simulation routes a flood wave through the reservoir and computes an outflow hydrograph which is the sum of the flow through the dam 's structures and the gradually developing breach. The second phase routes this outflow hydrograph through the stream which may be nonprismatic and have segments with subcritical or supercritical flow. The results are discharge and stage hydrographs at the dam as well as all of the computational nodes in the channel. From these hydrographs, peak discharge and stage profiles are tabulated. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri80116","usgsCitation":"Land, L.F., 1981, User's guide for a general purpose dam-break flood simulation model (K-634): U.S. Geological Survey Water-Resources Investigations Report 80-116, iv, 101 p., https://doi.org/10.3133/wri80116.","productDescription":"iv, 101 p.","numberOfPages":"110","costCenters":[],"links":[{"id":367496,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/80/0116/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/80/0116/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603b98","contributors":{"authors":[{"text":"Land, Larry F.","contributorId":60612,"corporation":false,"usgs":true,"family":"Land","given":"Larry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26510,"text":"wri818 - 1981 - Selected hydrologic relationships for Soldier Creek, northeastern Kansas","interactions":[],"lastModifiedDate":"2017-12-06T13:05:19","indexId":"wri818","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-8","title":"Selected hydrologic relationships for Soldier Creek, northeastern Kansas","docAbstract":"<p>Hydrologic data from Soldier Creek basin were compared with relations from statewide data. The quantity and quality of streamflow were affected mostly by soils, slopes, and land use. Average annual precipitation during the study (196476) was 35.12 inches, or 2.3 percent greater than the long-term (1929-76) average. The average streamflow in Soldier Creek at Topeka, Kansas, was 23 percent greater than the long-term average.</p><p>In general, frequency curves of annual peak discharges compared poorly with curves from statewide relations due to the absence of extremely low peaks during the short period. A comparison of low-flow frequency for drainage areas of more than 100 square miles indicated that reasonable results will not be obtained for estimates of 7-day and 30-day average annual minimum discharges by linear extrapolation to basins of less than 100 square miles. Comparison of flow-duration curves confirms the extrapolation for basins of less than 100 square miles, although the percentage duration of mean flow is variable.</p><p>Water surveys showed that calcium, bicarbonate, and sulfate were the predominant ions and dissolved solids were derived mostly from limestones and shales. Suspended sediment at gaged sites ranged from 9.94 to 848 tons per day; yield per unit area increased significantly between sites due to changes in hillside slopes and land use.<br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri818","usgsCitation":"Carswell, W., 1981, Selected hydrologic relationships for Soldier Creek, northeastern Kansas: U.S. Geological Survey Water-Resources Investigations Report 81-8, 68 p., https://doi.org/10.3133/wri818.","productDescription":"68 p.","numberOfPages":"71","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":349788,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0008/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157849,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0008/report-thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"Soldier Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.05072021484375,\n              39.04265287290379\n            ],\n            [\n              -95.67169189453125,\n              39.04265287290379\n            ],\n            [\n              -95.67169189453125,\n              39.66914219401813\n            ],\n            [\n              -96.05072021484375,\n              39.66914219401813\n            ],\n            [\n              -96.05072021484375,\n              39.04265287290379\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5ddf31","contributors":{"authors":[{"text":"Carswell, William J. Jr. carswell@usgs.gov","contributorId":1787,"corporation":false,"usgs":true,"family":"Carswell","given":"William J.","suffix":"Jr.","email":"carswell@usgs.gov","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":false,"id":196517,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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