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Areas of limestone terrain characterized by sinkholes are indicated in basins where they have been determined. Each location is referenced by U.S. Geological Survey station number (where assigned), latitude, longitude, county code, topographic quadrangle, river distance, and in some cases by nearby town or landmark. All values are given in both English and metric units and an alphabetical index by stream name is provided. 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No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81796","usgsCitation":"Bohannon, R.G., 1981, Geologic map, tectonic map, and structure sections of the Muddy and northern Black Mountains, Clark County, Nevada: U.S. Geological Survey Open-File Report 81-796, 3 Plates: 45.15 x 40.54 inches or smaller, https://doi.org/10.3133/ofr81796.","productDescription":"3 Plates: 45.15 x 40.54 inches or 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Ground water is available in Kiowa County, Colo., in quantities suitable for municipal or irrigation uses from at least two aquifers, the Big Sandy-Rush Creek alluvial aquifer and the Ogallala aquifer. The Dakota Sandstone and the Cheyenne Sandstone Member of the Purgatoire Formation may provide marginally sufficient water for municipal or irrigation purposes. Whil e wells in parts of the Ogallala aquifer have shown significant water-level declines in recent years, the Dakota Sandstone and Cheyenne Sandstone Member of the Purgatoire Formation are virtually undeveloped in the county , primarily because of the depth to the top of these formations (500-1,00 feet). Where water is not available from the Big Sandy-Rush Creek and Ogallala aquifers in the county, supplies sufficient for domestic or stock use may be obtained from shallow wells in several minor aquifers. The quality of ground water in the county varies widely, but dissolved-solids concentrations are usually greater than 500 milligrams per liter, except in parts of the Ogallala aquifer. The water is generally very hard and sulfate concentrations are usually greater than 250 milligrams per liter, except in parts of the Ogallala aquifer. High concentrations of selenium (greater than 10 micrograms per liter) in three-fourths of the wells sampled and locally high concentrations of fluoride, nitrate, iron, and manganese limit the suitability of the ground water for municipal and domestic use. (USGS)

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811023","usgsCitation":"Mustard, M.H., and Cain, D., 1981, Hydrology and chemical quality of ground water in Kiowa County, Colorado: U.S. Geological Survey Open-File Report 81-1023, 2 Sheets: 44.36 x 35.95 inches and 44.65 x 31.99 inches, https://doi.org/10.3133/ofr811023.","productDescription":"2 Sheets: 44.36 x 35.95 inches and 44.65 x 31.99 inches","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":169336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr811023.JPG"},{"id":309453,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1023/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":309452,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1023/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Kiowa","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-102.0454,38.6138],[-102.0443,38.2676],[-102.1749,38.2668],[-102.2858,38.2665],[-102.396,38.2662],[-102.5075,38.2662],[-102.6154,38.2661],[-102.741,38.2654],[-103.0571,38.2647],[-103.1691,38.2647],[-103.2787,38.2649],[-103.3972,38.2647],[-103.5004,38.2646],[-103.5019,38.3408],[-103.5066,38.3409],[-103.508,38.4366],[-103.5089,38.5159],[-103.5086,38.5236],[-103.3897,38.5239],[-103.2809,38.5224],[-103.1714,38.5236],[-103.1716,38.6111],[-103.1079,38.6133],[-103.0601,38.6135],[-102.9493,38.614],[-102.8386,38.6135],[-102.729,38.6133],[-102.6194,38.6131],[-102.5086,38.6128],[-102.4415,38.6122],[-102.3996,38.6128],[-102.2888,38.6132],[-102.1779,38.6134],[-102.073,38.6137],[-102.0695,38.6136],[-102.0454,38.6138]]]},\"properties\":{\"name\":\"Kiowa\",\"state\":\"CO\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49a5e4b07f02db5c1491","contributors":{"authors":[{"text":"Mustard, Martha H.","contributorId":91157,"corporation":false,"usgs":true,"family":"Mustard","given":"Martha","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":228392,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cain, Doug","contributorId":101655,"corporation":false,"usgs":true,"family":"Cain","given":"Doug","email":"","affiliations":[],"preferred":false,"id":228393,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9701,"text":"ofr81195 - 1981 - Pattern-recognition program modified and applied to southeastern United States seismicity","interactions":[],"lastModifiedDate":"2022-05-09T18:38:10.259916","indexId":"ofr81195","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":"81-195","title":"Pattern-recognition program modified and applied to southeastern United States seismicity","docAbstract":"

The pattern-recognition technique of Bongard and others (1966), Gelfand and others (1976), and Briggs and others (1977) was modified and applied in Southeastern United States to try to detect combinations or interactions of geologic, geophysical, and topographic parameters characteristic of areas with moderate and large earthquakes. The modification involved replacing the operator-defined criteria for significance of association of parameters and earthquakes with statistical estimates of significance. This was done in order to decrease the probability of random associations and to increase the flexibility of the pattern-recognition technique. The binomial distribution was used to determine the probability that each particular association could have occurred by chance. Bonferroni's inequality was invoked to determine a conservative significance level for each of the binomial tests. However, without being able to quantify the dependence among the associations, it is not possible to statistically evaluate the group of binomial tests as a whole. Preliminary results identify four independent associations characterizing spatially independent earthquake epicenters, or \"dangerous\" points, and seven independent associations characterizing the intervening \"safe\" points. When all points were reclassified using these traits, all epicenters were correctly classified as dangerous. In addition, three \"safe\" points were reclassified as dangerous and appear to be potential sites for future earthquakes. However, it is not possible to determine the degree of dangerousness of the points using this reclassification scheme. Two dangerous zones emerge in the northeast and southwest portions of the study area. Epicenters outside of these zones, including those of the large historic earthquakes (MMI > VIII) in Giles County, Virginia, and Charleston, South Carolina, have not been well characterized by the significant associations and may have fundamentally different causes.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81195","usgsCitation":"Jones-Cecil, M., Wheeler, R.L., and Dewey, J.W., 1981, Pattern-recognition program modified and applied to southeastern United States seismicity: U.S. Geological Survey Open-File Report 81-195, iv, 137 p., https://doi.org/10.3133/ofr81195.","productDescription":"iv, 137 p.","costCenters":[],"links":[{"id":400344,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0195/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0195/report-thumb.jpg"}],"country":"United States","otherGeospatial":"southeastern United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.84765625,\n 35.06597313798418\n ],\n [\n -84.28710937499999,\n 31.466153715024294\n ],\n [\n -80.2880859375,\n 32.21280106801518\n ],\n [\n -77.607421875,\n 34.488447837809304\n ],\n [\n -75.673828125,\n 36.491973470593685\n ],\n [\n -76.9482421875,\n 38.41055825094609\n ],\n [\n -79.189453125,\n 38.85682013474361\n ],\n [\n -81.82617187499999,\n 38.272688535980976\n ],\n [\n -83.84765625,\n 35.06597313798418\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4880","contributors":{"authors":[{"text":"Jones-Cecil, Meridee","contributorId":68313,"corporation":false,"usgs":true,"family":"Jones-Cecil","given":"Meridee","email":"","affiliations":[],"preferred":false,"id":160154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wheeler, Russell L. wheeler@usgs.gov","contributorId":858,"corporation":false,"usgs":true,"family":"Wheeler","given":"Russell","email":"wheeler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":160152,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dewey, James W. 0000-0001-8838-2450 jdewey@usgs.gov","orcid":"https://orcid.org/0000-0001-8838-2450","contributorId":5819,"corporation":false,"usgs":true,"family":"Dewey","given":"James","email":"jdewey@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":160153,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9983,"text":"ofr811194 - 1981 - A finite-element model study of the impact of the proposed I-326 crossing on flood stages of the Congaree River near Columbia, South Carolina","interactions":[],"lastModifiedDate":"2016-12-14T12:05:54","indexId":"ofr811194","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":"81-1194","title":"A finite-element model study of the impact of the proposed I-326 crossing on flood stages of the Congaree River near Columbia, South Carolina","docAbstract":"A two-dimensional finite element surface water model was used to study the hydraulic impact of the proposed Interstate Route 326 crossing of the Congaree River near Columbia, SC. The finite element model was assessed as a potential operational tool for analyzing complex highway crossings and other modifications of river flood plains. Infrared aerial photography was used to define regions of homogeneous roughness in the flood plain. Finite element networks approximating flood plain topography were designed using elements of three roughness types. High water marks established during an 8-yr flood that occurred in October 1976 were used to calibrate the model. The maximum flood of record, an approximately 100-yr flood that occurred in August 1908, was modeled in three cases: dikes on the right bank, dikes on the left bank, and dikes on both banks. In each of the three cases, simulations were performed both without and with the proposed highway embankments in place. Detailed information was obtained about backwater effects upstream from the proposed highway embankments, changes in flow distribution resulting from the embankments, and local velocities in the bridge openings. On the basis of results from the model study, the South Carolina Department of Highways and Public Transportation changed the design of several bridge openings. A simulation incorporating the new design for the case with dikes on the left bank indicated that both velocities in the bridge openings and backwater were reduced. A major problem in applying the model was the difficulty in predicting the network detail necessary to avoid local errors caused by roughness discontinuities and large depth gradients. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811194","usgsCitation":"Lee, J.K., and Bennett, C.S., 1981, A finite-element model study of the impact of the proposed I-326 crossing on flood stages of the Congaree River near Columbia, South Carolina: U.S. Geological Survey Open-File Report 81-1194, 65 p., 8 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr811194.","productDescription":"65 p., 8 over-size sheets, ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":143521,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1194/report-thumb.jpg"},{"id":37783,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1194/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37784,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1194/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37785,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1194/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37786,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1194/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37787,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1194/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37788,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1194/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37789,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1194/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37790,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1194/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37791,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1194/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","otherGeospatial":"Congaree River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.48422241210938,\n 33.552840110956154\n ],\n [\n -81.48422241210938,\n 34.32188946052673\n ],\n [\n -80.66436767578124,\n 34.32188946052673\n ],\n [\n -80.66436767578124,\n 33.552840110956154\n ],\n [\n -81.48422241210938,\n 33.552840110956154\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6c2","contributors":{"authors":[{"text":"Lee, J. K.","contributorId":28233,"corporation":false,"usgs":true,"family":"Lee","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":160616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, C. S. III","contributorId":49793,"corporation":false,"usgs":true,"family":"Bennett","given":"C.","suffix":"III","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":160617,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":46435,"text":"ofr81722 - 1981 - Map showing acoustic anomalies and near-surface faulting, Norton Sound, Alaska, 1981","interactions":[],"lastModifiedDate":"2022-10-17T20:32:25.387327","indexId":"ofr81722","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":"81-722","title":"Map showing acoustic anomalies and near-surface faulting, Norton Sound, Alaska, 1981","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81722","usgsCitation":"Steffy, D.A., and Hoose, P.J., 1981, Map showing acoustic anomalies and near-surface faulting, Norton Sound, Alaska, 1981: U.S. Geological Survey Open-File Report 81-722, 1 Plate: 47.00 × 42.00 inches, https://doi.org/10.3133/ofr81722.","productDescription":"1 Plate: 47.00 × 42.00 inches","costCenters":[],"links":[{"id":134763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20165,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0722/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":108172,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12128.htm","linkFileType":{"id":5,"text":"html"},"description":"12128"}],"country":"United States","state":"Alaska","otherGeospatial":"Norton Sound","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -167,\n 63.15\n ],\n [\n -163,\n 63.15\n ],\n [\n -163,\n 64.25\n ],\n [\n -167,\n 64.25\n ],\n [\n -167,\n 63.15\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658e53","contributors":{"authors":[{"text":"Steffy, David A.","contributorId":91075,"corporation":false,"usgs":true,"family":"Steffy","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":233310,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoose, Peter J.","contributorId":106076,"corporation":false,"usgs":true,"family":"Hoose","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":233311,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":21018,"text":"ofr81888 - 1981 - Earthquake hazard studies in southeastern Missouri","interactions":[],"lastModifiedDate":"2025-09-11T16:51:36.990664","indexId":"ofr81888","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":"81-888","title":"Earthquake hazard studies in southeastern Missouri","docAbstract":"

This report is intended to be a compact review of the current \"state of the art\" of operating a seismic telemetry network as applied to the New Madrid area, and incidentally, to the Adak, Alaska network because of the author's position as technical director of that network under a joint agreement with CIRES of the University of Colorado. The experiences and opinions expressed herein are necessarily those of the author and as such are limited to his acquaintance with the matter, and should not be construed to contradict or diminish the efforts of others operating telemetry networks under considerably different circumstances.

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from the 1979 imperial valley, California, earthquake","indexId":"70047764","publicationYear":"1981","noYear":false,"title":"Peak horizontal acceleration and velocity from strong-motion records including records from the 1979 imperial valley, California, earthquake"},"id":1}],"supersededBy":{"id":70047764,"text":"70047764 - 1981 - Peak horizontal acceleration and velocity from strong-motion records including records from the 1979 imperial valley, California, earthquake","indexId":"70047764","publicationYear":"1981","noYear":false,"title":"Peak horizontal acceleration and velocity from strong-motion records including records from the 1979 imperial valley, California, earthquake"},"lastModifiedDate":"2022-08-09T15:30:39.458696","indexId":"ofr81365","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":"81-365","title":"Peak horizontal acceleration and velocity from strong motion records including records from the 1979 Imperial Valley, California, earthquake","docAbstract":"

We have taken advantage of the recent increase in strong-motion data at close distances to derive new attenuation relations for peak horizontal acceleration and velocity. Acceleration data from 183 recordings of 24 earthquakes and velocity data from 62 recordings of 10 earthquakes have been used. This new analysis uses a magnitude-independent shape for the attenuation curve based on geometrical spreading and anelastic attenuation. A magnitude-dependent shape could be accommodated by the method, but the data do not support it. An innovation in technique is introduced that decouples the determination of the distance dependence of the data from the magnitude dependence.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81365","usgsCitation":"Joyner, W.B., Boore, D.M., and Porcella, R.L., 1981, Peak horizontal acceleration and velocity from strong motion records including records from the 1979 Imperial Valley, California, earthquake: U.S. Geological Survey Open-File Report 81-365, 46 p., https://doi.org/10.3133/ofr81365.","productDescription":"46 p.","costCenters":[],"links":[{"id":405015,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0365/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0365/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Imperial Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.58029174804686,\n 32.713355353177555\n ],\n [\n -114.67391967773436,\n 32.713355353177555\n ],\n [\n -114.67391967773436,\n 33.002905178377304\n ],\n [\n -115.58029174804686,\n 33.002905178377304\n ],\n [\n -115.58029174804686,\n 32.713355353177555\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6889cb","contributors":{"authors":[{"text":"Joyner, William B.","contributorId":39786,"corporation":false,"usgs":true,"family":"Joyner","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":160189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boore, David M. boore@usgs.gov","contributorId":2509,"corporation":false,"usgs":true,"family":"Boore","given":"David","email":"boore@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":160188,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Porcella, Ronald L.","contributorId":26674,"corporation":false,"usgs":true,"family":"Porcella","given":"Ronald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160190,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8936,"text":"ofr81399 - 1981 - In-situ measurements of seismic velocity at 19 locations in the Los Angeles, California, region","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr81399","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":"81-399","title":"In-situ measurements of seismic velocity at 19 locations in the Los Angeles, California, region","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81399","usgsCitation":"Fumal, T.E., Gibbs, J., and Roth, E.F., 1981, In-situ measurements of seismic velocity at 19 locations in the Los Angeles, California, region: U.S. Geological Survey Open-File Report 81-399, i, 123 p. ;28 cm., https://doi.org/10.3133/ofr81399.","productDescription":"i, 123 p. ;28 cm.","costCenters":[],"links":[{"id":141197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0399/report-thumb.jpg"},{"id":36543,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0399/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f594d","contributors":{"authors":[{"text":"Fumal, Thomas E.","contributorId":67882,"corporation":false,"usgs":true,"family":"Fumal","given":"Thomas","email":"","middleInitial":"E.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":158585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gibbs, James F.","contributorId":95880,"corporation":false,"usgs":true,"family":"Gibbs","given":"James F.","affiliations":[],"preferred":false,"id":158586,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roth, Edward F.","contributorId":12481,"corporation":false,"usgs":true,"family":"Roth","given":"Edward","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":158584,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":50766,"text":"ofr811004 - 1981 - Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980","interactions":[],"lastModifiedDate":"2017-12-06T14:00:43","indexId":"ofr811004","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":"81-1004","title":"Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980","docAbstract":"

The High Plains aquifer in Kansas is part of a regional system that extends into Colorado, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming.  The aquifer in Kansas underlies an area of 31,000 square miles in the western and south-central part of the State.  This aquifer is a hydraulically connected assemblage of unconsolidated water-bearing deposits.  In western Kansas, the High Plains aquifer consists principally of the Ogallala Formation of late Tertiary age and the overlying deposits of Quaternary age.  In south-central Kansas, the aquifer consists of unconsolidated deposits principally of the Quaternary age.  Valley alluvium of Quaternary age also is included in the deposits in both areas.  The High Plains aquifer is delimited on the east by outcrops of Permian or Cretaceous rocks and by unsaturated deposits of Quaternary age.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811004","usgsCitation":"Pabst, M.E., and Stullken, L.E., 1981, Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980: U.S. Geological Survey Open-File Report 81-1004, 43.21 x 31.20 inches, https://doi.org/10.3133/ofr811004.","productDescription":"43.21 x 31.20 inches","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":349811,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1004/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175854,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1004/report-thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"High Plains Aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102,\n 40\n ],\n [\n -102,\n 37\n ],\n [\n -97,\n 37\n ],\n [\n -97,\n 39\n ],\n [\n -99,\n 39\n ],\n [\n -99,\n 40\n ],\n [\n -102,\n 40\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686ac3","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":242258,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stullken, Lloyd E.","contributorId":60609,"corporation":false,"usgs":true,"family":"Stullken","given":"Lloyd","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":242259,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9331,"text":"ofr811100 - 1981 - Remote-site data entry for the Gospel-Hump Wilderness Area, Idaho; experimental use of a microcomputer on RASS (Rock Analysis Storage System) data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr811100","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":"81-1100","title":"Remote-site data entry for the Gospel-Hump Wilderness Area, Idaho; experimental use of a microcomputer on RASS (Rock Analysis Storage System) data","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811100","usgsCitation":"Hanley, J.T., 1981, Remote-site data entry for the Gospel-Hump Wilderness Area, Idaho; experimental use of a microcomputer on RASS (Rock Analysis Storage System) data: U.S. Geological Survey Open-File Report 81-1100, ii, 49 p. ill. ;28 cm., https://doi.org/10.3133/ofr811100.","productDescription":"ii, 49 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1100/report-thumb.jpg"},{"id":37052,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1100/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf53","contributors":{"authors":[{"text":"Hanley, J. Thomas","contributorId":85594,"corporation":false,"usgs":true,"family":"Hanley","given":"J.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":159491,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9731,"text":"ofr811069 - 1981 - Quality of water and time of travel in Little Copiah Creek near Crystal Springs, Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr811069","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":"81-1069","title":"Quality of water and time of travel in Little Copiah Creek near Crystal Springs, Mississippi","docAbstract":"An intensive quality of water study was conducted on Little Copiah Creek in the vicinity of Crystal Springs, Miss., from August 19 to August 21, 1980. The quality of water in Little Copiah Creek improved 7 miles downstream of a source of wastewater inflow. The mean total nitrogen concentration decreased from 17 to 1.1 milligrams per liter and the mean total phosphorus concentrations decreased from 5.8 to 0.39 milligrams per liter. The maximum five-day biochemical oxygen demand decreased from 14 to 1.4 milligrams per liter while the dissolved-oxygen concentration increased from 2.0 to 6.9 milligrams per liter. The maximum fecal coliform and fecal streptococcus densities at the upstream sampling site were 2,200 and 6,700 colonies per 100 milliliter, respectively, and were observed to decrease downstream to 160 and 1,500 colonies per 100 milliliters. The mean stream temperatures decreased downstream only slightly from 26.5 to 25.0 Celsius and the pH of the water ranged from 7.2 to 7.4 units upstream and 6.5 to 7.0 units at the downstream site. The average rate of dye travel through the upstream 2.3 mile reach was 0.08 miles per hour during the study. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811069","usgsCitation":"Kalkhoff, S., 1981, Quality of water and time of travel in Little Copiah Creek near Crystal Springs, Mississippi: U.S. Geological Survey Open-File Report 81-1069, v, 36 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr811069.","productDescription":"v, 36 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143057,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1069/report-thumb.jpg"},{"id":37475,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1069/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db65176e","contributors":{"authors":[{"text":"Kalkhoff, S. J.","contributorId":28967,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"S. J.","affiliations":[],"preferred":false,"id":160201,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9537,"text":"ofr81695 - 1981 - Floods of March 1978, in the Maumee River basin, northeastern Indiana","interactions":[],"lastModifiedDate":"2016-05-25T12:18:03","indexId":"ofr81695","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":"81-695","title":"Floods of March 1978, in the Maumee River basin, northeastern Indiana","docAbstract":"

Floods in the Maumee River basin in northeastern Indiana in March 1978 resulted in heavy damage in Fort Wayne and surrounding areas. Flood damage in Fort Wayne was estimated by the Mayor to be 11 million dollars. Approximately 15 percent of the city was inundated, and 2,400 of its 190,000 residents were forced to leave their homes. The estimate of damage in Adams and Allen Counties by Civil Defense officials was 44 million dollars. The Maumee River at New Haven exceeded the peak stage of record, 21.4 feet, by 2.2 feet. The peak discharge at this stream-gaging station, 22,400 cubic feet per second, was about equal to that of a 75-year flood. Recurrence intervals of peak flows on streams tributary to the Maumee River ranged from 5 to 50 years. Records of peak and daily discharges and some precipitation data are given in this report. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr81695","usgsCitation":"Hoggatt, R.E., 1981, Floods of March 1978, in the Maumee River basin, northeastern Indiana: U.S. Geological Survey Open-File Report 81-695, iv, 18 p. ill., map ;28 cm., https://doi.org/10.3133/ofr81695.","productDescription":"iv, 18 p. ill., map ;28 cm.","startPage":"1","endPage":"18","numberOfPages":"21","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":142828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94513,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015046045863?urlappend=%3Bseq=1"}],"country":"United States","state":"Indiana, Ohio","county":"Adams, Allen","city":"New Haven","otherGeospatial":"Maumee River Basin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.8026,40.9221],[-84.8027,40.9187],[-84.8026,40.9074],[-84.8023,40.7281],[-84.8025,40.7051],[-84.8025,40.7],[-84.8037,40.5723],[-84.8782,40.571],[-84.992,40.5697],[-85.0689,40.5688],[-85.074,40.9181],[-85.1087,40.9181],[-85.2218,40.9174],[-85.3349,40.9172],[-85.3347,41.0034],[-85.3346,41.0061],[-85.3381,41.0901],[-85.3397,41.1781],[-85.3111,41.1788],[-85.309,41.265],[-85.1935,41.2643],[-85.078,41.2658],[-84.9636,41.2676],[-84.8487,41.2698],[-84.8049,41.2702],[-84.8047,41.2536],[-84.8047,41.2527],[-84.8035,41.0133],[-84.8033,40.989],[-84.8026,40.9221]]]},\"properties\":{\"name\":\"Adams\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cde4b07f02db544f97","contributors":{"authors":[{"text":"Hoggatt, Richard Earl","contributorId":25929,"corporation":false,"usgs":true,"family":"Hoggatt","given":"Richard","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":159855,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9540,"text":"ofr81857 - 1981 - Fisheries resource evaluation, Cache Creek EIS, Wyoming","interactions":[],"lastModifiedDate":"2025-09-15T13:58:50.086116","indexId":"ofr81857","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":"81-857","title":"Fisheries resource evaluation, Cache Creek EIS, Wyoming","docAbstract":"

The U.S. Forest Service and U.S. Geological Survey are preparing an Environmental Impact Statement on proposed oil exploration in the Cache Creek area of the Teton National Forest, near Jackson, Wyoming. This fishery study represents a portion of the EIS data gathering effort by the U.S. Forest Service. The objective of this study was to provide a complete evaluation of the fisheries that would be potentially impacted by the proposed oil development, primarily related to the construction of access roads to proposed drilling sites.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81857","usgsCitation":"Holden, P.B., and Campbell, J.R., 1981, Fisheries resource evaluation, Cache Creek EIS, Wyoming: U.S. Geological Survey Open-File Report 81-857, Report: 25 p.; 1 Plate: 35.61 x 49.77 inches, https://doi.org/10.3133/ofr81857.","productDescription":"Report: 25 p.; 1 Plate: 35.61 x 49.77 inches","costCenters":[],"links":[{"id":495489,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0857/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":495490,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0857/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142831,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0857/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef47c","contributors":{"authors":[{"text":"Holden, Paul B.","contributorId":48180,"corporation":false,"usgs":true,"family":"Holden","given":"Paul","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":159859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, James R. 0000-0002-2760-3149","orcid":"https://orcid.org/0000-0002-2760-3149","contributorId":50156,"corporation":false,"usgs":true,"family":"Campbell","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":159860,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9733,"text":"ofr81406 - 1981 - Quality of water in Tibbee Creek and tributaries near West Point, Mississippi","interactions":[],"lastModifiedDate":"2022-08-10T13:46:14.777396","indexId":"ofr81406","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":"81-406","title":"Quality of water in Tibbee Creek and tributaries near West Point, Mississippi","docAbstract":"

An intensive water-quality study was conducted on Tibbee Creek and two of its tributaries, Town Creek and Catalpa Creek, on June 19-22, 1979. The data were collected during a period of low discharge and high air temperatures. The water in Tibbee Creek and Catalpa Creek was of much better quality than water in Town Creek. Large quantities of nitrogen, phosphorus, and dissolved solids and high densities of fecal coliform were present in Town Creek. The five-day biochemical oxygen demand values averaged 14 mg/L, and the mean total nitrogen concentration was 56 mg/L. The mean concentrations of ammonia, nitrate plus nitrite nitrogen, and organic nitrogen were 1.8 mg/L, 50 mg/L, and 3.7 mg/L, respectively. A total phosphorus load of more than 400 pounds per day, more than 91 percent of the total phosphorus load leaving the study area, was carried by Town Creek into Tibbee Creek. Total phosphorus concentrations averaged 14 mg/L in Town Creek and 0.11 and 0.12 mg/L in Tibbee and Catalpa Creeks respectively. Bacterial densities were higher at site 2 in Town Creek than at sites 1 and 3 in Tibbee and Catalpa Creeks respectively. The median fecal coliform bacterial density was 25,000 col/100 mL (colonies per 100 milliliters) in Town Creek and less than 200 col/100 mL in Tibbee and Catalpa Creeks. Median fecal streptococcal densities were 1,000 col/100 mL in Town Creek, 210 col/100 mL in Tibbee Creek, and 800 col/100 mL in Catalpa Creek. Fecal coliform to fecal streptococcal ratios were greater than 4.0 in Town Creek, indicating wastes of human origin were probably present during the study. Ratios were less than 0.7 in Tibbee and Catalpa Creeks, indicating human wastes were probably absent during the study.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81406","collaboration":"Prepared in cooperation with the Mississippi Department of Natural Resources Bureau of Pollution Control","usgsCitation":"Kalkhoff, S.J., 1981, Quality of water in Tibbee Creek and tributaries near West Point, Mississippi: U.S. Geological Survey Open-File Report 81-406, v, 42 p., https://doi.org/10.3133/ofr81406.","productDescription":"v, 42 p.","costCenters":[],"links":[{"id":405069,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75487.htm","linkFileType":{"id":5,"text":"html"}},{"id":143076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0406/report-thumb.jpg"},{"id":405013,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0406/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Mississippi","city":"West Point","otherGeospatial":"Tibbee Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.71734619140625,\n 33.57687060377715\n ],\n [\n -88.58551025390624,\n 33.57687060377715\n ],\n [\n -88.58551025390624,\n 33.6283419913718\n ],\n [\n -88.71734619140625,\n 33.6283419913718\n ],\n [\n -88.71734619140625,\n 33.57687060377715\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bc87a","contributors":{"authors":[{"text":"Kalkhoff, Stephen J. 0000-0003-4110-1716 sjkalkho@usgs.gov","orcid":"https://orcid.org/0000-0003-4110-1716","contributorId":1731,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"Stephen","email":"sjkalkho@usgs.gov","middleInitial":"J.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true},{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":160203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9833,"text":"ofr81909 - 1981 - A method of estimating flood-frequency parameters for streams in Idaho","interactions":[],"lastModifiedDate":"2023-03-10T23:06:10.358969","indexId":"ofr81909","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":"81-909","title":"A method of estimating flood-frequency parameters for streams in Idaho","docAbstract":"Skew coefficients for the log-Pearson type III distribution are generalized on the basis of some similarity of floods in the Snake River basin and other parts of Idaho. Generalized skew coefficients aid in shaping flood-frequency curves because skew coefficients computed from gaging stations having relatively short periods of peak flow records can be unreliable. Generalized skew coefficients can be obtained for a gaging station from one of three maps in this report. The map to be used depends on whether (1) snowmelt floods are domiant (generally when more than 20 percent of the drainage area is above 6,000 feet altitude), (2) rainstorm floods are dominant (generally when the mean altitude is less than 3,000 feet), or (3) either snowmelt or rainstorm floods can be the annual miximum discharge. For the latter case, frequency curves constructed using separate arrays of each type of runoff can be combined into one curve, which, for some stations, is significantly different than the frequency curve constructed using only annual maximum discharges. For 269 gaging stations, flood-frequency curves that include the generalized skew coefficients in the computation of the log-Pearson type III equation tend to fit the data better than previous analyses. Frequency curves for ungaged sites can be derived by estimating three statistics of the log-Pearson type III distribution. The mean and standard deviation of logarithms of annual maximum discharges are estimated by regression equations that use basin characteristics as independent variables. Skew coefficient estimates are the generalized skews. The log-Pearson type III equation is then applied with the three estimated statistics to compute the discharge at selected exceedance probabilities. Standard errors at the 2-percent exceedance probability range from 41 to 90 percent. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81909","usgsCitation":"Kjelstrom, L., and Moffatt, R.L., 1981, A method of estimating flood-frequency parameters for streams in Idaho: U.S. Geological Survey Open-File Report 81-909, Report: iv, 101 p.; 4 Plates: 26.90 × 25.97 inches or smaller, https://doi.org/10.3133/ofr81909.","productDescription":"Report: iv, 101 p.; 4 Plates: 26.90 × 25.97 inches or 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629f57","contributors":{"authors":[{"text":"Kjelstrom, L.C.","contributorId":89104,"corporation":false,"usgs":true,"family":"Kjelstrom","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":160380,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moffatt, R. L.","contributorId":79889,"corporation":false,"usgs":true,"family":"Moffatt","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160379,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9405,"text":"ofr81454 - 1981 - 1980 annual index of current earthquake literature","interactions":[],"lastModifiedDate":"2022-08-10T17:40:24.044637","indexId":"ofr81454","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":"81-454","title":"1980 annual index of current earthquake literature","docAbstract":"

In the past several years earthquake research has been greatly accelerated in China, Japan, the USSR, and the United States. Presently about 3,000 earthquake-related publications (including meeting abstracts) are produced yearly. In order to keep up with this current literature, a computer-based bibliographic system was implemented as part of a research project called \"Worldwide Earthquake Research Databases\" under the direction of W.H.K. Lee. This bibliographic system is called the Current Earthquake Literature (CEL) Database. From this database, a quarterly Author Index and an Annual Index (including author, keyword and address listings) are prepared. The CEL Index will no longer be distributed on a bimonthly basis, it will be published quarterly in order to save on cost. Because there are large amounts of data entries, errors are unavoidable and any corrections from the readers are welcome.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81454","usgsCitation":"Hayashida, B., Kauffmann, M.L., and Lee, W., 1981, 1980 annual index of current earthquake literature: U.S. Geological Survey Open-File Report 81-454, 386 p., https://doi.org/10.3133/ofr81454.","productDescription":"386 p.","costCenters":[],"links":[{"id":405085,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0454/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0454/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4912e4b0b290850eedc3","contributors":{"authors":[{"text":"Hayashida, B.S.","contributorId":42212,"corporation":false,"usgs":true,"family":"Hayashida","given":"B.S.","email":"","affiliations":[],"preferred":false,"id":159628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kauffmann, Mari L.","contributorId":42594,"corporation":false,"usgs":true,"family":"Kauffmann","given":"Mari","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159629,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, William Hung Kan","contributorId":83502,"corporation":false,"usgs":true,"family":"Lee","given":"William Hung Kan","affiliations":[],"preferred":false,"id":159630,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":50764,"text":"ofr81126 - 1981 - Manchester quadrangle, Carroll County, Maryland: Hydrogeology","interactions":[{"subject":{"id":50764,"text":"ofr81126 - 1981 - Manchester quadrangle, Carroll County, Maryland: Hydrogeology","indexId":"ofr81126","publicationYear":"1981","noYear":false,"title":"Manchester quadrangle, Carroll County, Maryland: Hydrogeology"},"predicate":"SUPERSEDED_BY","object":{"id":70047498,"text":"70047498 - 1981 - Hydrogeologic atlas, Manchester quadrangle, Carroll County, Maryland","indexId":"70047498","publicationYear":"1981","noYear":false,"title":"Hydrogeologic atlas, Manchester quadrangle, Carroll County, Maryland"},"id":1}],"supersededBy":{"id":70047498,"text":"70047498 - 1981 - Hydrogeologic atlas, Manchester quadrangle, Carroll County, Maryland","indexId":"70047498","publicationYear":"1981","noYear":false,"title":"Hydrogeologic atlas, Manchester quadrangle, Carroll County, Maryland"},"lastModifiedDate":"2013-08-08T08:53:13","indexId":"ofr81126","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":"81-126","title":"Manchester quadrangle, Carroll County, Maryland: Hydrogeology","language":"ENGLISH","doi":"10.3133/ofr81126","usgsCitation":"Otton, E., 1981, Manchester quadrangle, Carroll County, Maryland: Hydrogeology: U.S. Geological Survey Open-File Report 81-126, 68 p., https://doi.org/10.3133/ofr81126.","productDescription":"68 p.","costCenters":[],"links":[{"id":175744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ac66","contributors":{"authors":[{"text":"Otton, E. G.","contributorId":22311,"corporation":false,"usgs":true,"family":"Otton","given":"E. G.","affiliations":[],"preferred":false,"id":242256,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}