{"pageNumber":"4416","pageRowStart":"110375","pageSize":"25","recordCount":184880,"records":[{"id":29634,"text":"wri894159 - 1990 - A statistical processor for analyzing simulations made using the Modular Finite-Difference Ground-water Flow Model","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri894159","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-4159","title":"A statistical processor for analyzing simulations made using the Modular Finite-Difference Ground-water Flow Model","docAbstract":"Many hydrologic studies of ground-water systems are conducted using a digital computer model as an aid to understanding the flow system. One of the most commonly used ground-water modeling programs is the Modular Three-Dimensional Ground-water Flow Model (Modular Model) by McDonald and Harbaugh. This report presents a computer program to summarize the data input to and output from the Modular Model. The program is named the Modular Model Statistical Processor and is designed to be run following the Modular Model.\r\nThe Modular Model Statistical Processor provides ground-water modelers with the capabilities to easily read data input to and output from the Modular Model, calculate descriptive statistics, generate histograms, perform logical tests using relational operators, calculate data arrays using arithmetic operators, and calculate flow vectors for use in a graphical-display program.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri894159","usgsCitation":"Scott, J.C., 1990, A statistical processor for analyzing simulations made using the Modular Finite-Difference Ground-water Flow Model: U.S. Geological Survey Water-Resources Investigations Report 89-4159, v. 218 p. :ill. ;28 cm., https://doi.org/10.3133/wri894159.","productDescription":"v. 218 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119412,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4159/report-thumb.jpg"},{"id":58454,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4159/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a62b5","contributors":{"authors":[{"text":"Scott, J. C.","contributorId":75901,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201851,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26283,"text":"wri894063 - 1990 - Potential hazards from floodflows in Grapevine Canyon, Death Valley National Monument, California and Nevada","interactions":[],"lastModifiedDate":"2023-01-05T22:01:02.712872","indexId":"wri894063","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-4063","title":"Potential hazards from floodflows in Grapevine Canyon, Death Valley National Monument, California and Nevada","docAbstract":"

Grapevine Canyon is on the western slope of the Grapevine Mountains in the northern part of Death Valley National Monument , California and Nevada. Grapevine Canyon Road covers the entire width of the canyon floor in places and is a frequently traveled route to Scotty 's Castle in the canyon. The region is arid and subject to flash flooding because of infrequent but intense convective storms. When these storms occur, normally in the summer, the resulting floods may create a hazard to visitor safety and property. Historical data on rainfall and floodflow in Grapevine Canyon are sparse. Data from studies made for similar areas in the desert mountains of southern California provide the basis for estimating discharges and the corresponding frequency of floods in the study area. Results of this study indicate that high-velocity flows of water and debris , even at shallow depths, may scour and damage Grapevine Canyon Road. When discharge exceeds 4,900 cu ft/sec, expected at a recurrence interval of between 25 and 50 years, the Scotty 's Castle access road and bridge may be damaged and the parking lot partly inundated. A flood having a 100-year or greater recurrence interval probably would wash out the bridge and present a hazard to the stable and garage buildings but not to the castle buildings, whose foundations are higher than the predicted maximum flood level. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894063","usgsCitation":"Bowers, J.C., 1990, Potential hazards from floodflows in Grapevine Canyon, Death Valley National Monument, California and Nevada: U.S. Geological Survey Water-Resources Investigations Report 89-4063, Report: iv, 19 p.; 1 Plate: 25.50 x 22.74 inches, https://doi.org/10.3133/wri894063.","productDescription":"Report: iv, 19 p.; 1 Plate: 25.50 x 22.74 inches","costCenters":[],"links":[{"id":411455,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47177.htm","linkFileType":{"id":5,"text":"html"}},{"id":55092,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4063/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55091,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4063/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124288,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4063/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Death Valley National Monument, Grapevine Canyon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.3425,\n 37.0333\n ],\n [\n -117.3425,\n 37.0267\n ],\n [\n -117.3358,\n 37.0267\n ],\n [\n -117.3358,\n 37.0333\n ],\n [\n -117.3425,\n 37.0333\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db68319e","contributors":{"authors":[{"text":"Bowers, J. C.","contributorId":57106,"corporation":false,"usgs":true,"family":"Bowers","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":196111,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":49160,"text":"ofr90286 - 1990 - Reconnaissance wadi-sediment geochemical survey of the Bi'r Jarbuah area, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-07T14:28:20","indexId":"ofr90286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-286","title":"Reconnaissance wadi-sediment geochemical survey of the Bi'r Jarbuah area, Kingdom of Saudi Arabia","docAbstract":"

A reconnaissance wadi-sediment geochemical survey for gold was conducted in the Bi'r Jarbuah Area (lat 20° 45' 00\"-21 ° 00' 00\" N., long 43° 30' 00\"- 43° 41' 00\" K). The area is located in the northern part of a regional concentration of gold occurrences, the Jabal Ishmas-Wadi Tathlith gold belt. Panned concentrates and minus-80-mesh fractions were obtained from 300 samples collected from a 320 km2 area and analysed by atomic-absorption spectroscopy. Analyses of the pannedconcentrate samples proved to be more definitive than sieved samples in delineating areas of mineralization. Most of the anomalous gold-and arsenic-bearing wadi-sediment samples are located along an irregular contact between gneissic and dioritic rocks in the center of an area characterized by the presence of subparallel dacitic dike swarms.

\n

Most of the ancient gold mines are also located along this contact. Gold is associated with arsenic but not with silver. Five areas containing gold-anomalies areas and 6 areas containing tellurium anomalies and the contact zone between the diorite and the paragneiss are recommended for further investigation of precious-metals resources.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr90286","usgsCitation":"Samater, R.M., Christian, R.P., and Walker, B.M., 1990, Reconnaissance wadi-sediment geochemical survey of the Bi'r Jarbuah area, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 90-286, iii, 32 p. : ill. ; 28 cm., https://doi.org/10.3133/ofr90286.","productDescription":"iii, 32 p. : ill. ; 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":176737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0286/report-thumb.jpg"},{"id":85939,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0286/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Saudi Arabia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 43,\n 20\n ],\n [\n 43,\n 21\n ],\n [\n 44,\n 21\n ],\n [\n 44,\n 20\n ],\n [\n 43,\n 20\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db6361bf","contributors":{"authors":[{"text":"Samater, Rashid M.","contributorId":85251,"corporation":false,"usgs":true,"family":"Samater","given":"Rashid","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":239172,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christian, Ralph P.","contributorId":91739,"corporation":false,"usgs":true,"family":"Christian","given":"Ralph","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":239173,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walker, Bruce M.","contributorId":64684,"corporation":false,"usgs":true,"family":"Walker","given":"Bruce","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":239171,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":41105,"text":"ofr90557 - 1990 - Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, May 1990","interactions":[],"lastModifiedDate":"2021-11-24T19:28:50.125551","indexId":"ofr90557","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-557","title":"Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, May 1990","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90557","usgsCitation":"Murray, L., 1990, Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, May 1990: U.S. Geological Survey Open-File Report 90-557, 1 Plate: 27.00 × 46.00 inches, https://doi.org/10.3133/ofr90557.","productDescription":"1 Plate: 27.00 × 46.00 inches","costCenters":[],"links":[{"id":392098,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17974.htm"},{"id":21405,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0557/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":176406,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"St, Johns River Water Management District and vicinity","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.583984375,\n 26.49024045886963\n ],\n [\n -79.95849609375,\n 26.49024045886963\n ],\n [\n -79.95849609375,\n 30.939924331023445\n ],\n [\n -83.583984375,\n 30.939924331023445\n ],\n [\n -83.583984375,\n 26.49024045886963\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682b08","contributors":{"authors":[{"text":"Murray, Louis C.","contributorId":53022,"corporation":false,"usgs":true,"family":"Murray","given":"Louis C.","affiliations":[],"preferred":false,"id":224503,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38596,"text":"pp1200US - 1990 - The National Gazetteer of the United States of America; United States concise 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"pp1200US","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"1200","chapter":"US","title":"The National Gazetteer of the United States of America; United States concise 1990","language":"ENGLISH","doi":"10.3133/pp1200US","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1990, The National Gazetteer of the United States of America; United States concise 1990: U.S. Geological Survey Professional Paper 1200, 526 p., https://doi.org/10.3133/pp1200US.","productDescription":"526 p.","costCenters":[],"links":[{"id":119150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1200us/report-thumb.jpg"},{"id":65408,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1200us/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b19d","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":529868,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60902,"text":"mf2115 - 1990 - Geologic map of the San Andreas Fault in the Parkfield 7.5-minute Quadrangle, Monterey and Fresno counties, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:33","indexId":"mf2115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"2115","title":"Geologic map of the San Andreas Fault in the Parkfield 7.5-minute Quadrangle, Monterey and Fresno counties, California","language":"ENGLISH","doi":"10.3133/mf2115","usgsCitation":"Sims, J., 1990, Geologic map of the San Andreas Fault in the Parkfield 7.5-minute Quadrangle, Monterey and Fresno counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 2115, 1 map ;58 x 47 cm., on sheet 106 x 112 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf2115.","productDescription":"1 map ;58 x 47 cm., on sheet 106 x 112 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":105245,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5715.htm","linkFileType":{"id":5,"text":"html"},"description":"5715"},{"id":180168,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.5,35.8675 ], [ -120.5,36 ], [ -120.36749999999999,36 ], [ -120.36749999999999,35.8675 ], [ -120.5,35.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61148c","contributors":{"authors":[{"text":"Sims, J.D.","contributorId":9230,"corporation":false,"usgs":false,"family":"Sims","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":264585,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40938,"text":"ofr90133 - 1990 - Potentiometric surface of the upper Floridan aquifer, west-central Florida, September 1989","interactions":[],"lastModifiedDate":"2021-08-17T20:26:05.522573","indexId":"ofr90133","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-133","title":"Potentiometric surface of the upper Floridan aquifer, west-central Florida, September 1989","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90133","usgsCitation":"Knochenmus, L.A., and Barr, G., 1990, Potentiometric surface of the upper Floridan aquifer, west-central Florida, September 1989: U.S. Geological Survey Open-File Report 90-133, 1 Plate: 24.06 × 35.03 inches, https://doi.org/10.3133/ofr90133.","productDescription":"1 Plate: 24.06 × 35.03 inches","costCenters":[],"links":[{"id":170906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":388055,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17865.htm"},{"id":78828,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0133/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.00,\n 26.5\n ],\n [\n -81.25,\n 26.5\n ],\n [\n -81.25,\n 30.00\n ],\n [\n -84.00,\n 30.00\n ],\n [\n -84.00,\n 26.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b11e4b07f02db6a23c4","contributors":{"authors":[{"text":"Knochenmus, Lari A. lari@usgs.gov","contributorId":301,"corporation":false,"usgs":true,"family":"Knochenmus","given":"Lari","email":"lari@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":224210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barr, G. L.","contributorId":22312,"corporation":false,"usgs":true,"family":"Barr","given":"G. L.","affiliations":[],"preferred":false,"id":224211,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2553,"text":"wsp2366 - 1990 - A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming","interactions":[{"subject":{"id":15559,"text":"ofr88337 - 1989 - A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming","indexId":"ofr88337","publicationYear":"1989","noYear":false,"title":"A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":2553,"text":"wsp2366 - 1990 - A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming","indexId":"wsp2366","publicationYear":"1990","noYear":false,"title":"A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"wsp2366","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"2366","title":"A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming","docAbstract":"A physically based point-infiltration model was developed for computing infiltration of rainfall into soils and the resulting runoff from small basins in Wyoming. The user describes a 'design storm' in terms of average rainfall intensity and storm duration. Information required to compute runoff for the design storm by using the model include (1) soil type and description, and (2) two infiltration parameters and a surface-retention storage parameter. Parameter values are tabulated in the report. Rainfall and runoff data for three ephemeral-stream basins that contain only one type of soil were used to develop the model. Two assumptions were necessary: antecedent soil moisture is some long-term average, and storm rainfall is uniform in both time and space. The infiltration and surface-retention storage parameters were determined for the soil of each basin. Observed rainstorm and runoff data were used to develop a separation curve, or incipient-runoff curve, which distinguishes between runoff and nonrunoff rainfall data. The position of this curve defines the infiltration and surface-retention storage parameters. \r\n\r\nA procedure for applying the model to basins that contain more than one type of soil was developed using data from 7 of the 10 study basins. For these multiple-soil basins, the incipient-runoff curve defines the infiltration and retention-storage parameters for the soil having the highest runoff potential. Parameters were defined by ranking the soils according to their relative permeabilities and optimizing the position of the incipient-runoff curve by using measured runoff as a control for the fit. Analyses of runoff from multiple-soil basins indicate that the effective contributing area of runoff is less than the drainage area of the basin. In this study, the effective drainage area ranged from 41.6 to 71.1 percent of the total drainage area. Information on effective drainage area is useful in evaluating drainage area as an independent variable in statistical analyses of hydrologic data, such as annual peak frequency distributions and sediment yield.A comparison was made of the sum of the simulated runoff and the sum of the measured runoff for all available records of runoff-producing storms in the 10 study basins. The sums of the simulated runoff ranged from 12.0 percent less than to 23.4 percent more than the sums of the measured runoff. A measure of the standard error of estimate was computed for each data set. These values ranged from 20 to 70 percent of the mean value of the measured runoff. \r\n\r\nRainfall-simulator infiltrometer tests were made in two small basins. The amount of water uptake measured by the test in Dugout Creek tributary basin averaged about three times greater than the amount of water uptake computed from rainfall and runoff data. Therefore, infiltrometer data were not used to determine infiltration rates for this study.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2366","usgsCitation":"Rankl, J.G., 1990, A point-infiltration model for estimating runoff from rainfall on small basins in semiarid areas of Wyoming: U.S. Geological Survey Water Supply Paper 2366, v, 29 p. :ill., maps ; 28 cm., https://doi.org/10.3133/wsp2366.","productDescription":"v, 29 p. :ill., maps ; 28 cm.","costCenters":[],"links":[{"id":138619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2366/report-thumb.jpg"},{"id":28801,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2366/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a91fd","contributors":{"authors":[{"text":"Rankl, James G.","contributorId":93026,"corporation":false,"usgs":true,"family":"Rankl","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23164,"text":"ofr90542 - 1990 - Preliminary geologic map of the Kanab 30- by 60-minute quadrangle, Utah-Arizona","interactions":[],"lastModifiedDate":"2022-09-12T19:40:40.041703","indexId":"ofr90542","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-542","title":"Preliminary geologic map of the Kanab 30- by 60-minute quadrangle, Utah-Arizona","docAbstract":"

No abstract available.

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No abstract available.

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The Bonneville region of the Basin and Range province in westcentral Utah and adjacent Nevada includes several basins lying south of the Great Salt Lake Desert. Physiographically, the region consists of linear, north-trending mountain ranges separated by valleys, many of which are closed basins underlain by thick sequences of fill. Surface drainage of open basins and ground-water flow is to the Great Salt Lake Desert. In structure and composition the ranges are faulted Paleozoic rocks, locally intruded by Mesozoic and Tertiary plugs and stocks. In the southern and northeastern parts of the region, volcanic rocks are widespread and form large parts of some mountain ranges. The Paleozoic sedimentary rocks include great thicknesses of carbonate rocks which compose a significant aquifer in the region

Media considered to have potential for isolation of high-level radioactive waste in the region include intrusive rocks, such as granite; ash-flow tuff; and basalt and basaltic andesite lava flows. These rock types, basin fill, and possibly other rock types, may have potential as host media in the unsaturated zone. Quaternary tectonism in the region is evidenced by seismic activity, local areas of above-normal geothermal heat flow, Quaternary faulting, late Cenozoic volcanic activity, and active vertical crustal movement.

The Bonneville region is part of a large ground-water flow system that is integrated partly through basin-fill deposits, but largely through an underlying carbonate-rock sequence. The region includes: (1) several topographically closed basins with virtually no local surface discharge that are drained by the underlying carbonate-rock aquifer; (2) closed basins with local surface discharge by evapotranspiration; and (3) basins open to the Great Salt Lake Desert that discharge by groundwater underflow and evapotranspiration. The carbonate-rock aquifer discharges to large springs in the Desert and in basins tributary to the Desert. The climate is arid to semiarid with the greatest precipitation in the mountain ranges. Most recharge probably occurs by infiltration of runoff as it leaves the mountains, although some recharge probably occurs directly to the carbonate rocks in the mountain areas. The concentration of dissolved solids in ground water is generally less than 500 milligrams per liter. Dissolved-solids concentrations increase in the Great Salt Lake Desert and in major valleys adjoining the Desert. The predominant chemical constituents in ground water are calcium, magnesium, and sodium bicarbonate. Chloride-type water is associated with the higher dissolved-solids content of water in and near the Great Salt Lake Desert.

The majority of the mineral occurrences containing base- and precious-metal deposits in the Bonneville region are of Tertiary age. Fluorspar is the primary industrial mineral. Coal, oil, and gas have not been produced in significant amounts.

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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90309","usgsCitation":"Cooper, A.K., and Webb, P., 1990, International workshop on Antarctic offshore acoustic stratigraphy (Antostrat); overview and extended abstracts, June 7 to 10, 1990: U.S. Geological Survey Open-File Report 90-309, 290 p., https://doi.org/10.3133/ofr90309.","productDescription":"290 p.","costCenters":[],"links":[{"id":152634,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0309/report-thumb.jpg"},{"id":48968,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0309/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0708","contributors":{"authors":[{"text":"Cooper, A. K.","contributorId":50149,"corporation":false,"usgs":true,"family":"Cooper","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":181040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Webb, P.-N.","contributorId":44180,"corporation":false,"usgs":true,"family":"Webb","given":"P.-N.","email":"","affiliations":[],"preferred":false,"id":181039,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":55003,"text":"wdrTX892 - 1990 - Water resources data Texas, water year 1989, volume 2. San Jacinto River basin, Brazos River basin, San Bernard River basin, and intervening coastal basins","interactions":[],"lastModifiedDate":"2020-12-17T20:20:25.087967","indexId":"wdrTX892","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"TX-89-2","title":"Water resources data Texas, water year 1989, volume 2. San Jacinto River basin, Brazos River basin, San Bernard River basin, and intervening coastal basins","docAbstract":"

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This report contains records of discharge for 17\nstream-gaging stations, stage for 6 stream stations, stage and contents for 1 reservoir\nwater quality for 3 streams and 5 observation wells, and water levels for 80 lakes and\n91 observation wells. Also included are records of peak flows for 23 crest-stage\npartial-record stations. Additional water data were collected at various sites, no\npart of the systematic data-collection program, and are shown as miscellaneous measurements. These data represent that part of the National Water Data System operated by the\nU.S. Geological Survey in Indiana in cooperation with State and Federal agencies.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrIN891","collaboration":"Prepared in cooperation with the State of Indiana and with other agencies","usgsCitation":"Thompson, R.E., and Nell, G.E., 1990, Water resources data, Indiana, water year 1989: U.S. Geological Survey Water Data Report IN-89-1, xv, 336 p., https://doi.org/10.3133/wdrIN891.","productDescription":"xv, 336 p.","numberOfPages":"355","temporalStart":"1988-10-01","temporalEnd":"1989-09-30","costCenters":[],"links":[{"id":288346,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288345,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1989/in-89-1/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faff2","contributors":{"authors":[{"text":"Thompson, Ronald E. 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No abstract available.

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