{"pageNumber":"1465","pageRowStart":"36600","pageSize":"25","recordCount":40841,"records":[{"id":80340,"text":"fwsobs82_10_120 - 1986 - Habitat Suitability Index Models: Inland silverside","interactions":[],"lastModifiedDate":"2022-02-09T14:39:18.794677","indexId":"fwsobs82_10_120","displayToPublicDate":"2007-09-11T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.120","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Inland silverside","docAbstract":"<p>The systematics of the Meni di a complex have been evaluated by Johnson (1975), who could not distinguish biochemical differences between ~. beryllina and M. audens, and by Chernoff et al. (1981), who concluded that M. audens is conspecific with ~. beryllina. The two species have since been synonymized as ~. beryllina, the inland silverside. The result is a considerable extension of ~. beryllina's range into freshwater habitats.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Weinstein, M.P., 1986, Habitat Suitability Index Models: Inland silverside: FWS/OBS 82/10.120, vi, 25 p.","productDescription":"vi, 25 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":192090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64984c","contributors":{"authors":[{"text":"Weinstein, Michael P.","contributorId":63487,"corporation":false,"usgs":true,"family":"Weinstein","given":"Michael","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":292299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015563,"text":"70015563 - 1986 - Bajada de Rahue, Province of Neuquen, Argentina: An interstadial deposit in northern Patagonia","interactions":[],"lastModifiedDate":"2025-06-13T13:38:36.201694","indexId":"70015563","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Bajada de Rahue, Province of Neuquen, Argentina: An interstadial deposit in northern Patagonia","docAbstract":"<p><span>Pollen and diatom analyses of a radiocarbon dated lacustrine section in the temperate Andean region of Argentina (Rahue, Province Neuquen) suggest interglacial type climatic conditions between 27,000 and 33,000 yr B.P., with environments that resemble the modern conditions at the locality. This finding correlates with a woodland record from central Chile, interpreted as reflecting conditions substantially warmer and drier prior to 27,000 yr B.P. than during the following full-glacial period. It also appears to relate to the global paleoclimatic scheme derived from deep-sea records, suggesting interhemispheric synchroneity of such broad-scale palaeoclimatic phases.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(86)90097-0","issn":"00310182","usgsCitation":"Markgraf, V., Bradbury, J., and Fernandez, J., 1986, Bajada de Rahue, Province of Neuquen, Argentina: An interstadial deposit in northern Patagonia: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 56, no. 3-4, p. 251-258, https://doi.org/10.1016/0031-0182(86)90097-0.","productDescription":"8 p.","startPage":"251","endPage":"258","costCenters":[],"links":[{"id":224429,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Argentina","otherGeospatial":"northern Patagonia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -70.71610663693028,\n              -42.769406541950055\n            ],\n            [\n              -70.71610663693028,\n              -45.30671312372499\n            ],\n            [\n              -67.31859912003154,\n              -45.30671312372499\n            ],\n            [\n              -67.31859912003154,\n              -42.769406541950055\n            ],\n            [\n              -70.71610663693028,\n              -42.769406541950055\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"56","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059efa8e4b0c8380cd4a3a2","contributors":{"authors":[{"text":"Markgraf, Vera","contributorId":104228,"corporation":false,"usgs":false,"family":"Markgraf","given":"Vera","email":"","affiliations":[],"preferred":false,"id":371233,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradbury, J.P.","contributorId":14431,"corporation":false,"usgs":true,"family":"Bradbury","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":371231,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fernandez, J.","contributorId":46229,"corporation":false,"usgs":true,"family":"Fernandez","given":"J.","affiliations":[],"preferred":false,"id":371232,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70015724,"text":"70015724 - 1986 - Carbonate apron models: Alternatives to the submarine fan model for paleoenvironmental analysis and hydrocarbon exploration","interactions":[],"lastModifiedDate":"2025-07-24T15:02:10.799323","indexId":"70015724","displayToPublicDate":"2003-04-14T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3368,"text":"Sedimentary Geology","active":true,"publicationSubtype":{"id":10}},"title":"Carbonate apron models: Alternatives to the submarine fan model for paleoenvironmental analysis and hydrocarbon exploration","docAbstract":"<p><span>Sediment gravity flow deposition along the deep-water flanks of carbonate platforms typically does not produce submarine fans. Rather, wedge-shaped carbonate aprons develop parallel to the adjacent shelf/slope break. The major difference between submarine fans and carbonate aprons is a point source with channelized sedimentation on fans, versus a line source with sheet-flow sedimentation on aprons.</span></p><p><span>Two types of carbonate aprons may develop. Along relatively gentle (&lt; 4°) platform-margin slopes, aprons form immediately adjacent to the shallow-water platform and are referred to as&nbsp;<i>carbonate slope aprons</i>. Along relatively steep (4–15°) platform margin slopes, redeposited limestones accumulate in a base-of-slope setting, by-passing an upper slope via a multitude of small submarine canyons, and are referred to as&nbsp;<i>carbonate base-of-slope aprons</i>. Both apron types are further subdivided into inner and outer facies belts. Inner apron sediments consist of thick, mud-supported conglomerates and megabreccias (Facies F) as well as thick, coarse-grained turbidites (Facies A) interbedded with subordinate amounts of fine-grained, peri-platform ooze (Facies G). Outer apron sediments consist of thinner, grain-supported conglomerates and turbidites (Facies A) as well as classical turbidites (Facies C) with recognizable Bouma divisions, interbedded with approximately equal proportions of peri-platform ooze (Facies G). Seaward, aprons grade laterally into basinal facies of thin, base-cut-out carbonate turbidites (Facies D) that are subordinate to peri-platform oozes (Facies G).&nbsp;<i>Carbonate base-of-slope aprons</i>&nbsp;grade shelfward into an upper slope facies of fine-grained peri-platform ooze (Facies G) cut by numerous small canyons that are filled with coarse debris, as well as intraformational truncation surfaces which result from submarine sliding. In contrast,&nbsp;<i>slope aprons</i>&nbsp;grade shelfward immediately into shoal-water, platform-margin facies without an intervening by-pass slope. The two carbonate apron models presented here offer alternatives to the submarine-fan model for paleoenvironmental analysis and hydrocarbon exploration for mass-transported carbonate facies.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0037-0738(86)90080-1","issn":"00370738","usgsCitation":"Mullins, H., and Cook, H.E., 1986, Carbonate apron models: Alternatives to the submarine fan model for paleoenvironmental analysis and hydrocarbon exploration: Sedimentary Geology, v. 48, no. 1-2, p. 37-79, https://doi.org/10.1016/0037-0738(86)90080-1.","productDescription":"43 p.","startPage":"37","endPage":"79","costCenters":[],"links":[{"id":223735,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f36de4b0c8380cd4b7de","contributors":{"authors":[{"text":"Mullins, H.T.","contributorId":76881,"corporation":false,"usgs":true,"family":"Mullins","given":"H.T.","email":"","affiliations":[],"preferred":false,"id":371628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cook, H. E.","contributorId":18782,"corporation":false,"usgs":true,"family":"Cook","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":371627,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015106,"text":"70015106 - 1986 - Mechanical response of the south flank of Kilauea volcano, Hawaii, to intrusive events along the rift systems","interactions":[],"lastModifiedDate":"2025-08-25T16:41:37.724639","indexId":"70015106","displayToPublicDate":"2003-04-10T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Mechanical response of the south flank of Kilauea volcano, Hawaii, to intrusive events along the rift systems","docAbstract":"<div class=\"u-margin-s-bottom\">Increased earthquake activity and compression of the south flank of Kilauea volcano, Hawaii, have been recognized by previous investigators to accompany rift intrusions. We further detail the temporal and spatial changes in earthquake rates and ground strain along the south flank induced by six major rift intrusions which occurred between December 1971 and January 1981. The seismic response of the south flank to individual rift intrusions is immediate; the increased rate of earthquake activity lasts from 1 to 4 weeks. Horizontal strain measurements indicate that compression of the south flank usually accompanies rift intrusions and eruptions. Emplacement of an intrusion at a depth greater than about 4 km, such as the June 1982 southwest rift intrusion, however, results in a slight extension of the subaerial portion of the south flank.</div><div class=\"u-margin-s-bottom\"><br data-mce-bogus=\"1\"></div><div class=\"u-margin-s-bottom\">Horizontal strain measurements along the south flank are used to locate the January 1983 east-rift intrusion, which resulted in eruptive activity. The intrusion is modeled as a vertical rectangular sheet with constant displacement perpendicular to the plane of the sheet. This model suggests that the intrusive body that compressed the south flank in January 1983 extended from the surface to about 2.4 km depth, and was aligned along a strike of N66°E. The intrusion is approximately 11 km in length, extended beyond the January 1983 eruptive fissures, which are 8 km in length and is contained within the 14-km-long region of shallow rift earthquakes.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(86)90200-3","issn":"00401951","usgsCitation":"Dvorak, J., Okamura, A., English, T., Koyanagi, R.Y., Nakata, J.S., Sako, M., Tanigawa, W., and Yamashita, K., 1986, Mechanical response of the south flank of Kilauea volcano, Hawaii, to intrusive events along the rift systems: Tectonophysics, v. 124, no. 3-4, p. 193-209, https://doi.org/10.1016/0040-1951(86)90200-3.","productDescription":"17 p.","startPage":"193","endPage":"209","costCenters":[],"links":[{"id":224019,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -155.46126003973447,\n              19.32313934378122\n            ],\n            [\n              -155.46126003973447,\n              19.19866425187726\n            ],\n            [\n              -155.2306109623595,\n              19.19866425187726\n            ],\n            [\n              -155.2306109623595,\n              19.32313934378122\n            ],\n            [\n              -155.46126003973447,\n              19.32313934378122\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"124","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a535ce4b0c8380cd6ca13","contributors":{"authors":[{"text":"Dvorak, J.J.","contributorId":52597,"corporation":false,"usgs":true,"family":"Dvorak","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":370089,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Okamura, A.T.","contributorId":70400,"corporation":false,"usgs":true,"family":"Okamura","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":370092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"English, T.T.","contributorId":49799,"corporation":false,"usgs":true,"family":"English","given":"T.T.","email":"","affiliations":[],"preferred":false,"id":370087,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koyanagi, R. Y.","contributorId":35719,"corporation":false,"usgs":true,"family":"Koyanagi","given":"R.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":370086,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nakata, J. S.","contributorId":23940,"corporation":false,"usgs":true,"family":"Nakata","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":370085,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sako, M. K.","contributorId":50152,"corporation":false,"usgs":true,"family":"Sako","given":"M. K.","affiliations":[],"preferred":false,"id":370088,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tanigawa, W.T.","contributorId":56383,"corporation":false,"usgs":true,"family":"Tanigawa","given":"W.T.","email":"","affiliations":[],"preferred":false,"id":370091,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Yamashita, K.M.","contributorId":54603,"corporation":false,"usgs":true,"family":"Yamashita","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":370090,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70015687,"text":"70015687 - 1986 - River meanders and channel size","interactions":[],"lastModifiedDate":"2025-04-23T15:13:08.595739","indexId":"70015687","displayToPublicDate":"2003-03-27T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"River meanders and channel size","docAbstract":"<p>This study uses an enlarged data set to (1) compare measured meander geometry to that predicted by the Langbein and Leopold (1966) theory, (2) examine the frequency distribution of the ratio radius of curvature/channel width, and (3) derive 40 empirical equations (31 of which are original) involving meander and channel size features. The data set, part of which comes from publications by other authors, consists of 194 sites from a large variety of physiographic environments in various countries. The Langbein-Leopold sine-generated-curve theory for predicting radius of curvature agrees very well with the field data (78 sites). The ratio radius of curvature/channel width has a modal value in the range of 2 to 3, in accordance with earlier work; about one third of the 79 values is less than 2.0. The 40 empirical relations, most of which include only two variables, involve channel cross-section dimensions (bankfull area, width, and mean depth) and meander features (wavelength, bend length, radius of curvature, and belt width). These relations have very high correlation coefficients, most being in the range of 0.95-0.99. Although channel width traditionally has served as a scale indicator, bankfull cross-sectional area and mean depth also can be used for this purpose.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(86)90202-7","issn":"00221694","usgsCitation":"Williams, G.P., 1986, River meanders and channel size: Journal of Hydrology, v. 88, no. 1-2, p. 147-164, https://doi.org/10.1016/0022-1694(86)90202-7.","productDescription":"18 p.","startPage":"147","endPage":"164","costCenters":[],"links":[{"id":223999,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aadb1e4b0c8380cd86f5b","contributors":{"authors":[{"text":"Williams, G. P.","contributorId":97472,"corporation":false,"usgs":true,"family":"Williams","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":371528,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015711,"text":"70015711 - 1986 - A boundary element-Random walk model of mass transport in groundwater","interactions":[],"lastModifiedDate":"2025-04-18T16:20:17.386258","indexId":"70015711","displayToPublicDate":"2003-03-27T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"A boundary element-Random walk model of mass transport in groundwater","docAbstract":"<p>A boundary element solution to the convective mass transport in groundwater is presented. This solution produces a continuous velocity field and reduces the amount of data preparation time and bookkeeping. </p><p>By combining this solution and the random walk procedure, a convective-dispersive mass transport model is obtained. This model may be easily used to simulate groundwater contamination problems. </p><p>The accuracy of the boundary element model has been verified by reproducing the analytical solution to a two-dimensional convective mass transport problem. The method was also used to simulate a convective-dispersive problem.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(86)90062-4","issn":"00221694","usgsCitation":"Kemblowski, M., 1986, A boundary element-Random walk model of mass transport in groundwater: Journal of Hydrology, v. 85, no. 3-4, p. 305-318, https://doi.org/10.1016/0022-1694(86)90062-4.","productDescription":"14 p.","startPage":"305","endPage":"318","costCenters":[],"links":[{"id":224387,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e32ce4b0c8380cd45e69","contributors":{"authors":[{"text":"Kemblowski, M.","contributorId":54340,"corporation":false,"usgs":true,"family":"Kemblowski","given":"M.","affiliations":[],"preferred":false,"id":371582,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015068,"text":"70015068 - 1986 - Use of the chloride ion in determining hydrologic-basin water budgets - A 3-year case study in the San Juan Mountains, Colorado, U.S.A.","interactions":[],"lastModifiedDate":"2025-04-18T16:16:38.103513","indexId":"70015068","displayToPublicDate":"2003-03-27T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Use of the chloride ion in determining hydrologic-basin water budgets - A 3-year case study in the San Juan Mountains, Colorado, U.S.A.","docAbstract":"<p>Measurement of chloride concentration and water equivalent in precipitation and recharge at a site can be extrapolated to determine available moisture in a nearby basin. This method also may be extrapolated to a basin with similar climatic characteristics if precipitation, vegetation, and topographic data are available. The average accuracy of the total of evaporation, recharge, and runoff (assuming no storage) was about 10% of total precipitation. Soil-moisture measurements indicate the entire 10% error in moisture balance can be attributed to annual changes in storage. Data requirements for the method are considerably less than data requirements for energy-budget methods to determine available moisture. </p><p>Potential applications of the method to hydrologic problem-solving are: </p><p>1. (1) Estimating total available moisture from chloride concentrations in groundwater or surface water or both. </p><p>2. (2) Modeling paleoclimate scenarios and evaluating their correctness by comparison with paleo-groundwater chloride concentrations. </p><p>3. (3) Providing an independent comparison for water budgets obtained by energy-budget methods. Obviously the method cannot be applied readily to systems with a lithologic source of chloride. Most systems primarily consisting of tuff, intrusive volcanic rock, nonmarine sediments, quartzite, and other metamorphic rocks will be suitable for application of the model.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(86)90076-4","issn":"00221694","usgsCitation":"Claassen, H., Reddy, M., and Halm, D., 1986, Use of the chloride ion in determining hydrologic-basin water budgets - A 3-year case study in the San Juan Mountains, Colorado, U.S.A.: Journal of Hydrology, v. 85, no. 1-2, p. 49-71, https://doi.org/10.1016/0022-1694(86)90076-4.","productDescription":"23 p.","startPage":"49","endPage":"71","costCenters":[],"links":[{"id":224288,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"San Juan Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.26236941271583,\n              37.973786790349635\n            ],\n            [\n              -108.26236941271583,\n              37.32252264711801\n            ],\n            [\n              -106.96577592186041,\n              37.32252264711801\n            ],\n            [\n              -106.96577592186041,\n              37.973786790349635\n            ],\n            [\n              -108.26236941271583,\n              37.973786790349635\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"85","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbf9de4b08c986b329c71","contributors":{"authors":[{"text":"Claassen, H.C.","contributorId":74028,"corporation":false,"usgs":true,"family":"Claassen","given":"H.C.","affiliations":[],"preferred":false,"id":369981,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reddy, M.M.","contributorId":24363,"corporation":false,"usgs":true,"family":"Reddy","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":369979,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Halm, D.R.","contributorId":54352,"corporation":false,"usgs":true,"family":"Halm","given":"D.R.","affiliations":[],"preferred":false,"id":369980,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70015631,"text":"70015631 - 1986 - Groundwater flow into Lake Michigan from Wisconsin","interactions":[],"lastModifiedDate":"2025-04-18T16:08:31.924749","indexId":"70015631","displayToPublicDate":"2003-03-27T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Groundwater flow into Lake Michigan from Wisconsin","docAbstract":"<p><span>Detailed hydrogeological study has been done at six sites along the Lake Michigan shoreline in Wisconsin. At each site a flux of groundwater to the lake has been calculated for both natural conditions and the existing conditions created by pumping. The values from each site have then been extrapolated to the entire portion of the total shoreline having similar hydrogeology in order to calculate a total flow of groundwater to the lake. Sensitivity analysis with a digital model was used to define limits on the similarity of hydrogeologic conditions.</span></p><p><span>The net flow calculated is 580–880 m<sup>3</sup>&nbsp;day<sup>−1</sup>&nbsp;km<sup>−1</sup>&nbsp;of shoreline, which falls within the previously published range of 110–8200 m<sup>3</sup>&nbsp;day<sup>−1</sup>&nbsp;km<sup>−1</sup>. Human activity may have reduced the natural flow as much as 15%. The estimated natural flow is between 7 and 11% of the surface water contribution to the lake from the study area.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(86)90126-5","issn":"00221694","usgsCitation":"Cherkauer, D., and Hensel, B., 1986, Groundwater flow into Lake Michigan from Wisconsin: Journal of Hydrology, v. 84, no. 3-4, p. 261-271, https://doi.org/10.1016/0022-1694(86)90126-5.","productDescription":"11 p.","startPage":"261","endPage":"271","costCenters":[],"links":[{"id":223832,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -87.29697155974961,\n              45.254760089058976\n            ],\n            [\n              -87.89261675173874,\n              45.254760089058976\n            ],\n            [\n              -87.89261675173874,\n              42.57857557165951\n            ],\n            [\n              -87.29697155974961,\n              42.57857557165951\n            ],\n            [\n              -87.29697155974961,\n              45.254760089058976\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"84","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2da2e4b0c8380cd5bf6d","contributors":{"authors":[{"text":"Cherkauer, D.S.","contributorId":62756,"corporation":false,"usgs":true,"family":"Cherkauer","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":371406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hensel, B.R.","contributorId":83669,"corporation":false,"usgs":true,"family":"Hensel","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":371407,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015667,"text":"70015667 - 1986 - Groundwater model of the Blue River basin, Nebraska-Twenty years later","interactions":[],"lastModifiedDate":"2025-04-18T16:25:32.00409","indexId":"70015667","displayToPublicDate":"2003-03-27T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Groundwater model of the Blue River basin, Nebraska-Twenty years later","docAbstract":"<p>Groundwater flow models have become almost a routine tool of the practicing hydrologist. Yet, surprisingly little attention has been given to true verification analysis of studies using these models. This paper examines predictions for 1982 of water-level declines and streamflow depletions that were made in 1965 using an electric analog groundwater model of the Blue River basin in southeastern Nebraska. Analysis of the model's predictions suggests that the analog model used too low an estimate of net groundwater withdrawals, yet overestimated water-level declines. The model predicted that almost all of the net groundwater pumpage would come from storage in the Pleistocene aquifer within the Blue River basin. It appears likely that the model underestimated the contributions of other sources of water to the pumpage, and that the aquifer storage coefficients used in the model were too low. There is some evidence that groundwater pumpage has had a greater than predicted effect on streamflow. Considerable uncertainty about the basic conceptualization of the hydrology of the Blue River basin greatly limits the reliability of groundwater models developed for the basin. The paper concludes with general perspectives on groundwater modeling gained from this post-audit analysis.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(86)90058-2","issn":"00221694","usgsCitation":"Alley, W., and Emery, P.A., 1986, Groundwater model of the Blue River basin, Nebraska-Twenty years later: Journal of Hydrology, v. 85, no. 3-4, p. 225-249, https://doi.org/10.1016/0022-1694(86)90058-2.","productDescription":"25 p.","startPage":"225","endPage":"249","costCenters":[],"links":[{"id":224384,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nebraska","otherGeospatial":"Blue River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -98.95009987605386,\n              41.428729545197314\n            ],\n            [\n              -98.95009987605386,\n              40.049780894036104\n            ],\n            [\n              -97.22563000651064,\n              40.049780894036104\n            ],\n            [\n              -97.22563000651064,\n              41.428729545197314\n            ],\n            [\n              -98.95009987605386,\n              41.428729545197314\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"85","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2daae4b0c8380cd5bf94","contributors":{"authors":[{"text":"Alley, W.M.","contributorId":6853,"corporation":false,"usgs":true,"family":"Alley","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":371485,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emery, P. A.","contributorId":49392,"corporation":false,"usgs":true,"family":"Emery","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":371486,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015650,"text":"70015650 - 1986 - A comparison of the coupled fresh water-salt water flow and the Ghyben-Herzberg sharp interface approaches to modeling of transient behavior in coastal aquifer systems","interactions":[],"lastModifiedDate":"2025-04-18T16:30:13.223878","indexId":"70015650","displayToPublicDate":"2003-03-27T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"A comparison of the coupled fresh water-salt water flow and the Ghyben-Herzberg sharp interface approaches to modeling of transient behavior in coastal aquifer systems","docAbstract":"<p>A quasi-three dimensional finite difference model which simulates coupled, fresh water and salt water flow, separated by a sharp interface, is used to investigate the effects of storage characteristics, transmissivity, boundary conditions and anisotropy on the transient responses of such flow systems. The magnitude and duration of the departure of aquifer response from the behavior predicted using the Ghyben-Herzberg, one-fluid approach is a function of the ease with which flow can be induced in the salt water region. In many common hydrogeologic settings short-term fresh water head responses, and transitional responses between short-term and long-term, can only be realistically reproduced by including the effects of salt water flow on the dynamics of coastal flow systems. The coupled fresh water-salt water flow modeling approach is able to reproduce the observed annual fresh water head response of the Waialae aquifer of southeastern Oahu, Hawaii.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(86)90012-0","issn":"00221694","usgsCitation":"Essaid, H., 1986, A comparison of the coupled fresh water-salt water flow and the Ghyben-Herzberg sharp interface approaches to modeling of transient behavior in coastal aquifer systems: Journal of Hydrology, v. 86, no. 1-2, p. 169-193, https://doi.org/10.1016/0022-1694(86)90012-0.","productDescription":"25 p.","startPage":"169","endPage":"193","costCenters":[],"links":[{"id":224165,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Oahu","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -158.2928500311901,\n              21.77866910239088\n            ],\n            [\n              -158.2928500311901,\n              21.230143945209946\n            ],\n            [\n              -157.626889717843,\n              21.230143945209946\n            ],\n            [\n              -157.626889717843,\n              21.77866910239088\n            ],\n            [\n              -158.2928500311901,\n              21.77866910239088\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"86","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e377e4b0c8380cd46047","contributors":{"authors":[{"text":"Essaid, H.I.","contributorId":22342,"corporation":false,"usgs":true,"family":"Essaid","given":"H.I.","email":"","affiliations":[],"preferred":false,"id":371450,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57994,"text":"pp1369 - 1986 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","interactions":[{"subject":{"id":9672,"text":"ofr84612 - 1984 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","indexId":"ofr84612","publicationYear":"1984","noYear":false,"title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":57994,"text":"pp1369 - 1986 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","indexId":"pp1369","publicationYear":"1986","noYear":false,"title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado"},"id":1}],"lastModifiedDate":"2012-02-02T00:12:14","indexId":"pp1369","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1369","title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","language":"ENGLISH","doi":"10.3133/pp1369","usgsCitation":"Jarrett, R.D., and Costa, J.E., 1986, Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado: U.S. Geological Survey Professional Paper 1369, vi, 78 p. : ill.; 29 cm.; 2 plates in pocket, https://doi.org/10.3133/pp1369.","productDescription":"vi, 78 p. : ill.; 29 cm.; 2 plates in pocket","costCenters":[],"links":[{"id":104610,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4820.htm","linkFileType":{"id":5,"text":"html"},"description":"4820"},{"id":120705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1369/report-thumb.jpg"},{"id":88298,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1369/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88299,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1369/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88300,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1369/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc732","contributors":{"authors":[{"text":"Jarrett, Robert D. rjarrett@usgs.gov","contributorId":2260,"corporation":false,"usgs":true,"family":"Jarrett","given":"Robert","email":"rjarrett@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":258117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Costa, John E.","contributorId":105743,"corporation":false,"usgs":true,"family":"Costa","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":258118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68462,"text":"ha678 - 1986 - Hydrologic characteristics of soils in parts of Arkansas, Colorado, Kansas, Missouri, Nebraska, New Mexico, Oklahoma, South Dakota, and Texas","interactions":[],"lastModifiedDate":"2017-02-21T10:40:14","indexId":"ha678","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"678","title":"Hydrologic characteristics of soils in parts of Arkansas, Colorado, Kansas, Missouri, Nebraska, New Mexico, Oklahoma, South Dakota, and Texas","docAbstract":"<p>Certain physical characteristics of soils, including permeability, available water capacity, thickness, and topographic position, have a definite effect on the hydrology of an area. They control the rate at which precipitation infiltrates or is transmitted through the soil, and thus they have a significant role in determining the rates both of ground-water recharge and surface runoff. In studies of ground-water hydrology, it commonly is useful to differentiate soils areally according to their physical characteristics and to assign values indicating the hydrologic responses of soils in the different areas.</p><p>In 1980 the U.S. Geologic Surey began a study termed the “Central Midwest Region Aquifer System Analysis,” Jorgensen and Signor, 1981). The regional aquifer system is defined as including all aquifers of Cretaceous age or older in all or parts of nine States included in this report. For part of this analysis, use of a soil-moisture model is planned to obtain estimates of actual evapotranspiraion and recharge to the regional aquifer system. Data for the hydrologic characteristics of the soils in the study area are required as input to this soil-moisture model.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha678","usgsCitation":"Dugan, J.T., 1986, Hydrologic characteristics of soils in parts of Arkansas, Colorado, Kansas, Missouri, Nebraska, New Mexico, Oklahoma, South Dakota, and Texas: U.S. Geological Survey Hydrologic Atlas 678, 1 Sheet: 40.5 x 44.5 inches, https://doi.org/10.3133/ha678.","productDescription":"1 Sheet: 40.5 x 44.5 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":185704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90002,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/678/plate-1.pdf","text":"Hydrologic Atlas HA-678","size":"9.92 MB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Arkansas, Colorado, Kansas, Missouri, Nebraska, New Mexico, Oklahoma, South Dakota, Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105,\n              38.5\n            ],\n            [\n              -89,\n              38.5\n            ],\n            [\n              -89,\n              44\n            ],\n            [\n              -105,\n              44\n            ],\n            [\n              -105,\n              38.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611636","contributors":{"authors":[{"text":"Dugan, Jack T.","contributorId":102456,"corporation":false,"usgs":true,"family":"Dugan","given":"Jack","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":278275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":80293,"text":"fwsobs82_10_122 - 1986 - Habitat Suitability Index Models and Instream Flow Suitability Curves: Chinook salmon","interactions":[],"lastModifiedDate":"2022-02-09T14:40:20.911393","indexId":"fwsobs82_10_122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.122","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models and Instream Flow Suitability Curves: Chinook salmon","docAbstract":"A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the Chinook salmon (Oncorhynchus tshawytscha). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum habitat). HSI models are designed to be used with Habitat Evaluation Procedures previously developed by the U.S. Fish and Wildlife Service.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Raleigh, R.F., Miller, W., and Nelson, P.C., 1986, Habitat Suitability Index Models and Instream Flow Suitability Curves: Chinook salmon: FWS/OBS 82/10.122, viii, 64 p.","productDescription":"viii, 64 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":192284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649e6f","contributors":{"authors":[{"text":"Raleigh, Robert F.","contributorId":49841,"corporation":false,"usgs":true,"family":"Raleigh","given":"Robert","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":292194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, William J.","contributorId":18069,"corporation":false,"usgs":true,"family":"Miller","given":"William J.","affiliations":[],"preferred":false,"id":292193,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, Patrick C.","contributorId":68799,"corporation":false,"usgs":true,"family":"Nelson","given":"Patrick","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":292195,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60970,"text":"mf1852 - 1986 - Seismicity map of the state of Arizona","interactions":[],"lastModifiedDate":"2017-05-10T11:32:30","indexId":"mf1852","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1852","title":"Seismicity map of the state of Arizona","docAbstract":"<p>This map is one of a series of seismicity maps produced by the U. S. Geological Survey that show earthquake data of individual states or groups of states at the scale of 1:1,000,000. This map shows only those earthquakes with epicenters located within the boundaries of Arizona, even though earthquakes in nearby states or countries may have been felt or may have caused damage in Arizona.</p><p>The data in table 1 were used to compile the seismicity map; these data are a corrected, expanded, and updated (through 1982) version of the data used by Algermissen (1969) for a study of seismic risk in the United States. The locations and intensities of some earthquakes were revised and intensities were assigned where none had been before. Many earthquakes were added to the original list from new data sources as well as from some old data sources that had not been previously used. The data in table 1 represent best estimates of the location of the epicenter, magnitude, and intensity of each earthquake on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed, but not all, especially for earthquakes that occurred before seismic instruments were universally used.</p><p>Table 1 includes earthquakes reported felt in Yuma, Arizona that had no corroborating reports from other areas. These events are listed with coordinates (32.7°N., 114.6° W.) near Yuma even though it is suspected that they may have actually occurred in the Imperial Valley, California or Baja California, Mexico. Very few earthquakes have been instrumentally located near Yuma and it is believed that most historical felt reports correspond to earthquakes that occurred in the seismic zone extending from the Gulf of California northward into California. It is known that some earthquakes located graphically from phase data prior to epicenter determinations by electronic computer were erroneously located in southern Arizona and actually had locations in the Gulf of California or northern Mexico.</p><p>For detailed descriptions of the effects of earthquakes in Arizona see Bulletin 193, Arizona earthquakes, 1776-1980 (reference 343) which lists the localities where the earthquakes were felt and the effects at each place. This publication also includes isoseismal maps for 41 events.</p><p>The latitude and longitude coordinates of each epicenter were rounded to the nearest tenth of a degree and sorted so that all identical locations were grouped and counted. These locations are represented on the map by a triangle. The number of earthquakes at each location is shown on the map by the arabic number to the right of the triangle. The Roman numeral to the left of the triangle is the maximum Modified Mercalli intensity (Wood and Neumann, 1931) of al 1 earthquakes with epicenters at that geographic location. The absence of an intensity value indicates that no intensities have been assigned to earthquakes at that location. The year shown below each triangle is the latest year for which the maximum intensity was recorded.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1852","usgsCitation":"Stover, C.W., Reagor, B., and Algermissen, S.T., 1986, Seismicity map of the state of Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1852, 49.25 x 37.11 inches, https://doi.org/10.3133/mf1852.","productDescription":"49.25 x 37.11 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326144,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1852.JPG"},{"id":327507,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1852/plate-1.pdf","text":"Plate ","size":"15.66 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faae8","contributors":{"authors":[{"text":"Stover, C. 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,{"id":80288,"text":"fwsobs82_10_118 - 1986 - Habitat Suitability Index Models: Brown thrasher","interactions":[],"lastModifiedDate":"2022-02-09T14:40:47.261651","indexId":"fwsobs82_10_118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.118","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Brown thrasher","docAbstract":"A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the brown thrasher (Toxostoma rufum). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum habitat). HSI models are designed to be used with Habitat Evaluation Procedures previously developed by the U.S. Fish and Wildlife Service.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Cade, B.S., 1986, Habitat Suitability Index Models: Brown thrasher: FWS/OBS 82/10.118, vi, 14 p.","productDescription":"vi, 14 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":195610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649a69","contributors":{"authors":[{"text":"Cade, Brian S. 0000-0001-9623-9849 cadeb@usgs.gov","orcid":"https://orcid.org/0000-0001-9623-9849","contributorId":1278,"corporation":false,"usgs":true,"family":"Cade","given":"Brian","email":"cadeb@usgs.gov","middleInitial":"S.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":292184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":80297,"text":"fwsobs82_10_123 - 1986 - Habitat Suitability Index Models: White-tailed deer in the Gulf of Mexico and South Atlantic Coastal Plains","interactions":[],"lastModifiedDate":"2022-02-09T14:39:51.489502","indexId":"fwsobs82_10_123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.123","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: White-tailed deer in the Gulf of Mexico and South Atlantic Coastal Plains","docAbstract":"A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the white-tailed deer (Odocoileus virginianus). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum habitat). HSI models are designed to be used with Habitat Evaluation Procedures previously developed by the U.S. Fish and Wildlife Service.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Short, H.L., 1986, Habitat Suitability Index Models: White-tailed deer in the Gulf of Mexico and South Atlantic Coastal Plains: FWS/OBS 82/10.123, vi, 36 p.","productDescription":"vi, 36 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":192957,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64972d","contributors":{"authors":[{"text":"Short, Henry L.","contributorId":58695,"corporation":false,"usgs":true,"family":"Short","given":"Henry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":292202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68224,"text":"ha691 - 1986 - Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":43378,"text":"ofr84452 - 1984 - Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon","indexId":"ofr84452","publicationYear":"1984","noYear":false,"title":"Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":68224,"text":"ha691 - 1986 - Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon","indexId":"ha691","publicationYear":"1986","noYear":false,"title":"Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2013-11-12T15:07:25","indexId":"ha691","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"691","title":"Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon","docAbstract":"Prompted by the need for a current, accurate, and repeatable delineation of irrigated acreage on the Snake River Plain, the U.S. Geological Survey entered into a cooperative agreement with the Idaho Department of Water Resources Image Analysis Facility and the U.S. Bureau of Reclamation to delineate 1980 land use form Landsat data. Irrigated acreage data were needed as input to groundwater flow models developed by the U.S. Geological Survey in a study of the regional aquifer system underlying the Snake River Plain. Single-date digital multispectral scanner data analyzed to delineate land-use classes. Source of irrigation water (surface water, ground water, and combined) was determined from county maps of 1975 water-related land use, data from previous investigations, and field checking. Surface-water diversions for irrigation on the Snake River Plain began in the 1840's. With the stimulus of Federal aid authorized by the Desert Land Act, Carey Act, and Reclamation Act, irrigated area increased rapidly in the early 1900's. By 1929, 2.2 million acres were irrigated. Ground water became and important source of irrigation water after World War II. In 1980, about 3.1 million acres of the Snake River Plain were irrigate: 2.0 million acres with surface water, 1.0 million with ground water, and 0.1 million with combined surface and ground water. About 5.2 million acres (half of the plain) are undeveloped rangeland, 1.0 million acres (one-tenth) are classified as barren. The remaining land is a mixture of dryland agriculture, water bodies, wetland, forests, and urban areas.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha691","usgsCitation":"Lindholm, G.F., and Goodell, S.A., 1986, Irrigated acreage and other land uses on the Snake River Plain, Idaho and eastern Oregon: U.S. Geological Survey Hydrologic Atlas 691, 1 Plate: 43.90 x 33.00 inches, https://doi.org/10.3133/ha691.","productDescription":"1 Plate: 43.90 x 33.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":187949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89581,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/691/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"Idaho;Oregon","otherGeospatial":"Snake River Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.25,42.0 ], [ -117.25,44.5 ], [ -111.5,44.5 ], [ -111.5,42.0 ], [ -117.25,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667289","contributors":{"authors":[{"text":"Lindholm, Gerald F.","contributorId":18374,"corporation":false,"usgs":true,"family":"Lindholm","given":"Gerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":277869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodell, S. A.","contributorId":38168,"corporation":false,"usgs":true,"family":"Goodell","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277870,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57019,"text":"b1737F - 1986 - Mineral Resources of the Warm Springs Wilderness Study Area, Mohave County, Arizona","interactions":[{"subject":{"id":20854,"text":"ofr90250 - 1990 - GSDEDIT and GSMEDIT, screen edit programs for GSDRAW and GSMAP data bases using a microcomputer (IBM PC or compatible)","indexId":"ofr90250","publicationYear":"1990","noYear":false,"title":"GSDEDIT and GSMEDIT, screen edit programs for GSDRAW and GSMAP data bases using a microcomputer (IBM PC or compatible)"},"predicate":"SUPERSEDED_BY","object":{"id":57019,"text":"b1737F - 1986 - Mineral Resources of the Warm Springs Wilderness Study Area, Mohave County, Arizona","indexId":"b1737F","publicationYear":"1986","noYear":false,"chapter":"F","title":"Mineral Resources of the Warm Springs Wilderness Study Area, Mohave County, Arizona"},"id":1},{"subject":{"id":57019,"text":"b1737F - 1986 - Mineral Resources of the Warm Springs Wilderness Study Area, Mohave County, Arizona","indexId":"b1737F","publicationYear":"1986","noYear":false,"chapter":"F","title":"Mineral Resources of the Warm Springs Wilderness Study Area, Mohave County, Arizona"},"predicate":"IS_PART_OF","object":{"id":39795,"text":"b1737 - 1989 - Mineral resources of wilderness study areas: Black Mountains region, Arizona","indexId":"b1737","publicationYear":"1989","noYear":false,"title":"Mineral resources of wilderness study areas: Black Mountains region, Arizona"},"id":2}],"isPartOf":{"id":39795,"text":"b1737 - 1989 - Mineral resources of wilderness study areas: Black Mountains region, Arizona","indexId":"b1737","publicationYear":"1989","noYear":false,"title":"Mineral resources of wilderness study areas: Black Mountains region, Arizona"},"lastModifiedDate":"2017-08-09T08:51:41","indexId":"b1737F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1737","chapter":"F","title":"Mineral Resources of the Warm Springs Wilderness Study Area, Mohave County, Arizona","docAbstract":"At the request of the U.S. Bureau of Land Management, approximately 113,500 acres of the Warm Springs Wilderness Study Area (AZ-020-028/029) were evaluated for mineral resources and mineral resource potential. In this report, the area studied is referred to as the 'wilderness study area' or 'study area'; any reference to the Warm Springs Wilderness Study Area refers only to that part of the wilderness study area for which a mineral survey was requested. This study area is located in west-central Arizona. The U.S. Geological Survey and the U.S. Bureau of Mines conducted geological, geochemical, and geophysical surveys to appraise the identified mineral resources (known) and assess the mineral resource potential (undiscovered) of the study area. fieldwork for this report was carried out largely in 1986-1989. There is a 1-million short ton indicated subeconomic resource of clinoptilolite-mordenite zeolite and an additional inferred resource of 2 million short tons near McHeffy Butte, approximately 2 miles west of the study area. A perlite deposit in the southeast corner of the study area contains an inferred subeconomic resource totaling 13 million short tons. An inferred subeconomic resource of gold in 225 short tons of quartz having a grade of 0.01 8 troy ounces per short ton is present at the Cook mine, 0.5 miles west of the study area. The northwestern part of the Warm Springs Wilderness Study Area has high mineral resource potential for gold and silver. The south-central part of the study area has one area of moderate and one area north of this south-central part has low mineral resource potential for gold and silver in and near Warm Springs Canyon; the mineral resource potential for gold is also moderate in three small areas in the southern part and one area in the northeastern part of the study area. The mineral resource potential for zeolite is high for the area surrounding the McHeffy Butte prospect and for one area in the southern part of the study area. Two areas inside the south and southeast boundaries of the study area have high mineral resource potential for perlite. The potential for ka: olinite resources is moderate in two areas in the southern part of the study area. The southern part of the study area has low resource potential for perlite and zeolite. Geothermal energy resource potential of the study area is low. The study area has no resource potential for oil and gas.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/b1737F","usgsCitation":"Gray, F., Jachens, R.C., Miller, R.J., Turner, R.L., Knepper, D.H., Pitkin, J.A., Keith, W.J., Mariano, J., Jones, S.L., and Korzeb, S.L., 1986, Mineral Resources of the Warm Springs Wilderness Study Area, Mohave County, Arizona: U.S. Geological Survey Bulletin 1737, Report: vi, F1-F26; 1 plate in pocket, https://doi.org/10.3133/b1737F.","productDescription":"Report: vi, F1-F26; 1 plate in pocket","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":88214,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1737f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1737f/report-thumb.jpg"},{"id":88215,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1737f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.75,34.5 ], [ -114.75,35.25 ], [ -114,35.25 ], [ -114,34.5 ], [ -114.75,34.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6357df","contributors":{"authors":[{"text":"Gray, Floyd 0000-0002-0223-8966 fgray@usgs.gov","orcid":"https://orcid.org/0000-0002-0223-8966","contributorId":603,"corporation":false,"usgs":true,"family":"Gray","given":"Floyd","email":"fgray@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":256095,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jachens, Robert C. jachens@usgs.gov","contributorId":1180,"corporation":false,"usgs":true,"family":"Jachens","given":"Robert","email":"jachens@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":256096,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, Robert J. rjmiller@usgs.gov","contributorId":2516,"corporation":false,"usgs":true,"family":"Miller","given":"Robert","email":"rjmiller@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":256098,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Turner, Robert L.","contributorId":45283,"corporation":false,"usgs":true,"family":"Turner","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":256101,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Knepper, Daniel H. dknepper@usgs.gov","contributorId":1242,"corporation":false,"usgs":true,"family":"Knepper","given":"Daniel","email":"dknepper@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":256097,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pitkin, James A.","contributorId":96651,"corporation":false,"usgs":true,"family":"Pitkin","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":256104,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Keith, William J.","contributorId":21146,"corporation":false,"usgs":true,"family":"Keith","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":256099,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Mariano, John","contributorId":69949,"corporation":false,"usgs":true,"family":"Mariano","given":"John","email":"","affiliations":[],"preferred":false,"id":256102,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Jones, Stephanie L.","contributorId":41012,"corporation":false,"usgs":true,"family":"Jones","given":"Stephanie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":256100,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Korzeb, Stanley L.","contributorId":71569,"corporation":false,"usgs":true,"family":"Korzeb","given":"Stanley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":256103,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":58783,"text":"mf1863 - 1986 - Seismic-reflection profiles of the New Madrid seismic zone-data along the Mississippi River near Caruthersville, Missouri","interactions":[],"lastModifiedDate":"2016-08-19T11:35:33","indexId":"mf1863","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1863","title":"Seismic-reflection profiles of the New Madrid seismic zone-data along the Mississippi River near Caruthersville, Missouri","docAbstract":"<p>The tectonic setting and the earthquake hazards of the New Madrid seismic zone in the northern Mississippi embayment have been the subject of intensive study the past several years as part of the Earthquake Hazard Reduction Program of the USGS (U.S. Geological Survey). These efforts have improved our knowledge of the geologic history, general tectonic setting, and patterns of modern seismicity (see McKeown and Pakiser, 1982) in the New Madrid seismic zone. Identifying and characterizing the specific structures that may be responsible for the seismicity is the focus of continuing research. Unfortunately, these structures are buried by the veneer of poorly consolidated Upper Cretaceous and Tertiary sediments that overlie competent rocks in the embayment. In such a geologic setting, seismic-reflection profiling is one of the most valuable techniques available to obtain useful information on the distribution of faults, and on the local and regional structure.</p>\n<p>Three major seismic-reflection programs have been conducted by the USGS in the New Madrid seismic zone. The first program consisted of 32 km of conventional Vibroseis profiling designed to investigate the subsurface structure associated with scarps and lineaments in northwestern Tennessee (Zoback, 1979). A second, more extensive Vibroseis program collected about 250 km of data from all parts of the New Madrid seismic zone in Missouri, Arkansas, and Tennessee (Hamilton and Zoback, 1979, 1982; Zoback and others, 1980). The profiles presented here are part of the third program that collected about 240 km of high-resolution seismic-reflection data from a boat along the Mississippi River between Osceola, Ark., and Wickliffe, Ky. (fig. 1). The data for profiles A, B, C, and D were collected between river miles 839-1/2 and 850-1/2 from near the Interstate-155 bridge to upstream of Caruthersville, Mo. (fig. 2). Profiles on this part of the river are important for three reasons: (1) they connect many of the land-based profiles on either side of the river, (2) they are near the northeast termination of a linear, 120km-long, northeast-southwest zone of seismicity that extends from northeast Arkansas to Caruthersville, Mo. (Stauder, 1982; fig. 1), and (3) they cross the southwesterly projection of the Cottonwood Grove fault (fig. 1), a fault having a substantial amount of vertical Cenozoic offset (Zoback and others, 1980).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1863","isbn":"0607817208","usgsCitation":"Crone, A.J., Harding, S., Russ, D.P., and Shedlock, K.M., 1986, Seismic-reflection profiles of the New Madrid seismic zone-data along the Mississippi River near Caruthersville, Missouri: U.S. Geological Survey Miscellaneous Field Studies Map 1863, 4 Plates: 40.82 x 57.37 inches or smaller, https://doi.org/10.3133/mf1863.","productDescription":"4 Plates: 40.82 x 57.37 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326124,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1863.JPG"},{"id":327013,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1863/plate-2.pdf"},{"id":327012,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1863/plate-1.pdf"},{"id":327014,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1863/plate-3.pdf"},{"id":327015,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1863/plate-4.pdf"}],"scale":"90000","country":"United States","state":"Missouri","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.73333333333333,36.084722222222226 ], [ -89.73333333333333,36.25 ], [ -89.56805555555555,36.25 ], [ -89.56805555555555,36.084722222222226 ], [ -89.73333333333333,36.084722222222226 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e0df","contributors":{"authors":[{"text":"Crone, A. J.","contributorId":84363,"corporation":false,"usgs":true,"family":"Crone","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":260787,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harding, S.T.","contributorId":99565,"corporation":false,"usgs":true,"family":"Harding","given":"S.T.","email":"","affiliations":[],"preferred":false,"id":260788,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Russ, D. P.","contributorId":38538,"corporation":false,"usgs":true,"family":"Russ","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":260785,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shedlock, K. M.","contributorId":72805,"corporation":false,"usgs":true,"family":"Shedlock","given":"K.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":260786,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":80270,"text":"fwsobs82_10_126 - 1986 - Habitat Suitability Index Models: Bald eagle (breeding season)","interactions":[],"lastModifiedDate":"2022-02-09T14:41:14.921701","indexId":"fwsobs82_10_126","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.126","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Bald eagle (breeding season)","docAbstract":"A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the bald eagle (Haliaeetus leucocephalus). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum habitat). HSI models are designed to be used with Habitat Evaluation Procedures previously developed by the U.S. Fish and Wildlife Service.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Peterson, A., 1986, Habitat Suitability Index Models: Bald eagle (breeding season): FWS/OBS 82/10.126, vi, 23 p.","productDescription":"vi, 23 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":192039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649df8","contributors":{"authors":[{"text":"Peterson, Allen","contributorId":95574,"corporation":false,"usgs":true,"family":"Peterson","given":"Allen","email":"","affiliations":[],"preferred":false,"id":292147,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15903,"text":"ofr86307 - 1986 - Guide to user modification of a three-dimensional digital ground-water model for Salt Lake Valley, Utah","interactions":[],"lastModifiedDate":"2022-11-01T19:07:57.514397","indexId":"ofr86307","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-307","title":"Guide to user modification of a three-dimensional digital ground-water model for Salt Lake Valley, Utah","docAbstract":"<p>A digital-computer model was calibrated to simulate, in three dimensions, the ground-water flow in the principal and shallow-unconfined aquifers in Salt Lake Valley, Utah. The model can be used to predict water-level and waterbudget changes that would be caused by changes in well recharge or discharge. This report shows how a user can revise the input data so that recharging or discharging wells may be simulated and how stress-period intervals can be varied to simulate different periods of recharge or discharge. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr86307","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources","usgsCitation":"Seiler, R.L., and Waddell, K., 1986, Guide to user modification of a three-dimensional digital ground-water model for Salt Lake Valley, Utah: U.S. Geological Survey Open-File Report 86-307, Report: iv, 13 p.; Plate: 17.58 in. x 21.55 inches, https://doi.org/10.3133/ofr86307.","productDescription":"Report: iv, 13 p.; Plate: 17.58 in. x 21.55 inches","numberOfPages":"16","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":44885,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0307/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44886,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0307/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409007,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16998.htm","linkFileType":{"id":5,"text":"html"}},{"id":150214,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0307/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Salt Lake Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.19540041154342,\n              40.88370704900959\n            ],\n            [\n              -112.19540041154342,\n              40.399033913978286\n            ],\n            [\n              -111.78769401167678,\n              40.399033913978286\n            ],\n            [\n              -111.78769401167678,\n              40.88370704900959\n            ],\n            [\n              -112.19540041154342,\n              40.88370704900959\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a83e4b07f02db64b76d","contributors":{"authors":[{"text":"Seiler, R. L.","contributorId":87546,"corporation":false,"usgs":true,"family":"Seiler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":171908,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25616,"text":"wri864329 - 1986 - Investigation of possible effects of surface coal mining on hydrology and landscape stability in part of the Powder River structural basin, northeastern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"wri864329","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4329","title":"Investigation of possible effects of surface coal mining on hydrology and landscape stability in part of the Powder River structural basin, northeastern Wyoming","docAbstract":"The effects of surface coal mining on the surface- and groundwater systems in a 5,400 sq mi area in the Powder River Basin, Wyoming, that includes 20 major coal mines were evaluated using three approaches: A surface water model, a landscape-stability analysis, and a groundwater model. A surface water model was developed for the Belle Fourche River basin. The Hydrological Simulation Program-Fortran model was used to simulate changes in streamflow and changes in dissolved-solids and sulfate concentrations. Simulated streamflows resulting from less than average rainfall were small, changes in flow from premining to during-mining and postmining conditions were less than 2.5%, and changes in mean dissolved-solids and sulfate concentrations ranged from 1 to 7%. A landscape-stability analysis resulted in regression relations to aid in the reconstruction of reclaimed drainage networks. Hypsometric analyses indicate the larger basins are relatively stable, and statistical data from these basins may be used to design the placement of material within a mined basin to approximate natural, stable landscapes in the area. The attempt to define and simulate the groundwater system in the area using a groundwater-flow model was unsuccessful. The steady-state groundwater-flow model could not be calibrated. The modeling effort failed principally because of insufficient quantity and quality of data to define the spatial distribution of aquifer properties; the hydraulic-head distribution within and between aquifers; and the rates of groundwater recharge and discharge, especially for steady-state conditions. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864329","usgsCitation":"Bloyd, R., Daddow, P., Jordon, P., and Lowham, H., 1986, Investigation of possible effects of surface coal mining on hydrology and landscape stability in part of the Powder River structural basin, northeastern Wyoming: U.S. Geological Survey Water-Resources Investigations Report 86-4329, vi, 101 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864329.","productDescription":"vi, 101 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4329/report-thumb.jpg"},{"id":54362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4329/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e479de4b07f02db49212b","contributors":{"authors":[{"text":"Bloyd, R. M.","contributorId":34549,"corporation":false,"usgs":true,"family":"Bloyd","given":"R. M.","affiliations":[],"preferred":false,"id":194423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daddow, P. B.","contributorId":26700,"corporation":false,"usgs":true,"family":"Daddow","given":"P. B.","affiliations":[],"preferred":false,"id":194422,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jordon, P.R.","contributorId":69605,"corporation":false,"usgs":true,"family":"Jordon","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":194424,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lowham, H. W.","contributorId":8111,"corporation":false,"usgs":true,"family":"Lowham","given":"H. W.","affiliations":[],"preferred":false,"id":194421,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":12707,"text":"ofr85571 - 1986 - Sources of coal-mine drainage and their effects on surface-water chemistry in the Claybank Creek basin and vicinity, north-central Missouri, 1983-84","interactions":[{"subject":{"id":12707,"text":"ofr85571 - 1986 - Sources of coal-mine drainage and their effects on surface-water chemistry in the Claybank Creek basin and vicinity, north-central Missouri, 1983-84","indexId":"ofr85571","publicationYear":"1986","noYear":false,"title":"Sources of coal-mine drainage and their effects on surface-water chemistry in the Claybank Creek basin and vicinity, north-central Missouri, 1983-84"},"predicate":"SUPERSEDED_BY","object":{"id":1039,"text":"wsp2305 - 1989 - Sources of coal-mine drainage and their effects on surface-water chemistry in the Claybank Creek basin and vicinity, north-central Missouri, 1983-84","indexId":"wsp2305","publicationYear":"1989","noYear":false,"title":"Sources of coal-mine drainage and their effects on surface-water chemistry in the Claybank Creek basin and vicinity, north-central Missouri, 1983-84"},"id":1}],"supersededBy":{"id":1039,"text":"wsp2305 - 1989 - Sources of coal-mine drainage and their effects on surface-water chemistry in the Claybank Creek basin and vicinity, north-central Missouri, 1983-84","indexId":"wsp2305","publicationYear":"1989","noYear":false,"title":"Sources of coal-mine drainage and their effects on surface-water chemistry in the Claybank Creek basin and vicinity, north-central Missouri, 1983-84"},"lastModifiedDate":"2018-11-06T15:31:11","indexId":"ofr85571","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-571","title":"Sources of coal-mine drainage and their effects on surface-water chemistry in the Claybank Creek basin and vicinity, north-central Missouri, 1983-84","docAbstract":"<p>Eighteen sources of drainage related to past coal-mining activity were identified in the Claybank Creek, Missouri, study area, and eight of thew were considered large enough to have detectable effects on receiving streams. However, only three sources, coal wastes at Keota and Binkley, and drainage from underground coal mines near Keota, significantly affected the chemistry of water in receiving streams. </p><p>Coal wastes in the Claybank Creek basin contributed large quantities of acid drainage to receiving streams during storm runoff; pH of coal-waste runoff ranged from 2.1 to 2.8. At these small pH values, concentrations of some dissolved metals and dissolved sulfate were a few to several hundred times larger than Federal and State water-quality standards established for these constituents. Effects of acid storm runoff were detected near the mouth of North Fork Claybank Creek where the pH during a small storm was 3.9. </p><p>Coal wastes in the streambeds and seepage from coal wastes also had significant effects on receiving streams during base flows. The receiving waters had pH values between 2.8 and 3.5 and concentrations of some dissolved metals and dissolved sulfate were a few to several hundred times larger than Federal and State water-quality standards. </p><p>Most underground mines in the North Fork Claybank Creek basin are hydraulically connected and about 80 percent of their discharge surfaced at one site. Drainage from the underground mines contributed most of the dissolved constituents in North Fork Claybank Creek during dry weather. Underground-mine water always had a pH near 5.9, was well-buffered, had a dissolved-sulfate concentration of about 2,400 milligrams per liter, dissolved-manganese concentrations ranging from 4.0 to 5.3 milligrams per liter, and large concentrations of ferrous iron. Iron was in the ferrous state due to reducing conditions in the mines. When underground-mine drainage reached the ground surface, the ferrous iron was oxidized and precipitated to form large, orange deposits of ferric hydroxide around the site and in streambeds. </p><p>Generally, drainage from strip mines had dissolved-sulfate concentrations several times larger than drainage from unmined areas. However, effects of drainage from strip mines on receiving streams were minimal when compared to the drainage from coal wastes and underground mines. </p><p>No appreciable effects of mine-related drainage were detected in the water of the Claybank Creek arm of Thomas Hill Reservoir at the time of sampling because beaver bogs upstream had trapped suspended coal wastes and moderated the effects. However, the concentration of coal in the bottom material was 60 percent of the coal concentration in coal wastes at Keota, indicating that the reservoir had received these wastes during the past.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85571","usgsCitation":"Blevins, D.W., 1986, Sources of coal-mine drainage and their effects on surface-water chemistry in the Claybank Creek basin and vicinity, north-central Missouri, 1983-84: U.S. Geological Survey Open-File Report 85-571, Report: viii, 74 p.; 3 Plates: 35.23 x 28.19 inches or smaller, https://doi.org/10.3133/ofr85571.","productDescription":"Report: viii, 74 p.; 3 Plates: 35.23 x 28.19 inches or smaller","costCenters":[],"links":[{"id":359246,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0571/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359247,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0571/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359248,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0571/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0571/report-thumb.jpg"},{"id":359244,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0571/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Missouri","otherGeospatial":"Claybank Creek Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.6667,\n              39.75\n            ],\n            [\n              -92.5417,\n              39.75\n            ],\n            [\n              -92.5417,\n              39.625\n            ],\n            [\n              -92.6667,\n              39.625\n            ],\n            [\n              -92.6667,\n              39.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e766b","contributors":{"authors":[{"text":"Blevins, Dale W. dblevins@usgs.gov","contributorId":2729,"corporation":false,"usgs":true,"family":"Blevins","given":"Dale","email":"dblevins@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":166575,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15324,"text":"ofr86565 - 1986 - Red-Sea rift magmatism near Al Lith, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-07T14:20:00","indexId":"ofr86565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-565","title":"Red-Sea rift magmatism near Al Lith, Kingdom of Saudi Arabia","docAbstract":"<p>A newly recognized Tertiary dike complex and comagmatic volcanic rocks exposed on the central Saudi Arabian coastal plain record early stages of magmatism related to Red Sea rifting. Intrusive and stratigraphic relationships, and new potassium-argon dating indicate episodic magmatism from about 30 Ma to the present. Additional stratigraphic and radiometric evidence suggests that limited rift-related magmatism may have began as early as about 50 Ma ago. An early phase of crustal extension in the region was accompanied by faulting and graben formation and by dike-swarm intrusion. The style of extension and intrusion changed approximately 20 Ma ago. Localized volcanism and sheeted dike injection ceased and were replaced by the intrusion of thick gabbro dikes. This change may mark the onset of sea-floor spreading in the central Red Sea.</p>\n<p>The dikes and volcanic rocks consist of a bimodal mafic-felsic suite with transitional subalkaline to alkaline chemistry. Although no unique petrogenetic model can be developed for the suite, the following observations and conclusions are apparent from the available reconnaissance geochemistry: 1) Strontium isotopic initial ratios overlap in the range 0.7031 to 0.7047 and are not clearly related to alkalinity or silica content. Therefore, the bimodality and alkalinity of the suite are not products of contamination by the radiogenic Precambrian upper-crustal granitic rocks exposed in the region. 2) Several of the evolved rocks (rhyolites and comendite) show large to extreme negative europium anomalies and heavy rare-earth element (HREE) enrichment, features that cannot be explained by low-pressure crystal fractionation of potential parent magmas. An intriguing possibility is that HREE enrichments and large negative Eu anomalies of some peraluminous rhyolites (and granites) may result from the complete melting of garnet from middle or lower crustal rocks. 3) Most of the basalts are light rare-earth element (LREE)-enriched, consistent with derivation from fertile mantle in a continental-rift setting, however, interaction of the mafic melts with lower continental crust cannot be ruled out.</p>\n<p>A model of poly-baric mantle-melt derivation, producing several alkalinesubalkaline cycles, best explains magmatism in the Red Sea region. Differences in the depths and dynamics of mantle-melt extraction and transport brought about through changes in crust and mantle structure as the rift and paar developed may account for the transition from mixed alkaline-subalkaline bimodal magmatism of the pre-20 Ma rift basin to exclusively subalkaline (tholeiitic) magmatism at the Red Sea spreading axis and to predominantly alkali basalt volcanism within the Arabian Shield.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr86565","usgsCitation":"Pallister, J., 1986, Red-Sea rift magmatism near Al Lith, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 86-565, i, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr86565.","productDescription":"i, 41 p. :ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":146458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0565/report-thumb.jpg"},{"id":44254,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0565/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              39,\n              20\n            ],\n            [\n              39,\n              21\n            ],\n            [\n              41,\n              21\n            ],\n            [\n              41,\n              20\n            ],\n            [\n              39,\n              20\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63534a","contributors":{"authors":[{"text":"Pallister, J.S.","contributorId":46534,"corporation":false,"usgs":true,"family":"Pallister","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":170957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12359,"text":"ofr8671 - 1986 - Water resources activities in Kentucky, 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr8671","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-71","title":"Water resources activities in Kentucky, 1986","docAbstract":"The U.S. Geological Survey, Water Resources Division, conducts three major types of activities in Kentucky in order to provide hydrologic information and understanding needed for the best management of Kentucky 's and the Nation 's water resources. These activities are: (1) Data collection and dissemination; (2) Water-resources appraisals (interpretive studies); and (3) Research. Activities described in some detail following: (1) collection of surface - and groundwater data; (2) operation of stations to collect data on water quality, atmospheric deposition, and sedimentation; (3) flood investigations; (4) water use; (5) small area flood hydrology; (6) feasibility of disposal of radioactive disposal in deep crystalline rocks; (7) development of a groundwater model for the Louisville area; (8) travel times for streams in the Kentucky River Basin; (9) the impact of sinkholes and streams on groundwater flow in a carbonate aquifer system; (10) sedimentation and erosion rates at the Maxey Flats Radioactive Waste Burial site; and (11) evaluation of techniques for evaluating the cumulative impacts of mining as applied to coal fields in Kentucky. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8671","usgsCitation":"Faust, R.J., 1986, Water resources activities in Kentucky, 1986: U.S. Geological Survey Open-File Report 86-71, iv, 58 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr8671.","productDescription":"iv, 58 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0071/report-thumb.jpg"},{"id":40595,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623b38","contributors":{"authors":[{"text":"Faust, R. J. (compiler)","contributorId":83128,"corporation":false,"usgs":true,"family":"Faust","given":"R.","suffix":"(compiler)","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":166003,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}