A summary of recent significant scientific and economic results accompanied by a list of geologic, hydrologic, and cartographic investigations in progress.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp1375","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Geological Survey research, fiscal year 1981: U.S. Geological Survey Professional Paper 1375, vii, 424 p., https://doi.org/10.3133/pp1375.","productDescription":"vii, 424 p.","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":65211,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1375/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1375/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673b2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529858,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38513,"text":"pp1342 - 1984 - The evolution of the southern California uplift, 1955 through 1976","interactions":[],"lastModifiedDate":"2017-04-25T15:11:50","indexId":"pp1342","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1342","title":"The evolution of the southern California uplift, 1955 through 1976","docAbstract":"The southern California uplift culminated in 1974 as a 150- km-wide crustal swell that extended about 600 km eastward and east-southeastward from Point Arguello to the Colorado River and Salton Sea, respectively; it was characterized by remarkably uniform height changes between 1959 and 1974 of 0.30-0.35 m over at least half of its 60,000-70,000 km2 area. At its zenith, the uplift included virtually the entire Transverse Ranges geologic province and parts of the Coast Ranges, San Joaquin Valley, Sierra Nevada, Basin and Range, Mojave Desert, Peninsular Ranges, and Salton Trough provinces. The alinement of the western part of the uplift closely paralleled the east-trending Transverse Ranges, whereas the southern flank of the eastern lobe roughly coincided with the west-northwest-trending San Andreas fault. The position and configuration of the uplift associate it with a singularly complex section of the boundary between the North American and Pacific plates that has certainly sustained major modification during the past 5 million years and probably during the past 1 million years.
Surface deformation can be categorized as tectonic or nontectonic. Nontectonic vertical displacements associated with the activities of man have overwhelmed natural compaction and areally significant soil expansion in the southern California area. Because tectonic displacements are implicitly defined as those that cannot be otherwise explained, those vertical movements that can be reasonably attributed to artificial processes have been subtracted from our reconstructed configurations of the uplift. Hence this reconstruction has necessarily included the assembly and evaluation of an enormous volume of data on oil-field operations, changes in ground-water levels, and measured subsidence (or rebound) associated with changes in the underground fluid regimen.
Measured changes in height at various stages in the evolution of the uplift have been based chiefly on first-order levelings carried out between 1953 and 1976. Exceptions to this generalization consist largely of the results of pre-1953 surveys through the western Transverse Ranges and the eastern Mojave Desert. Errors in measured height differences derive from blunders, systematic survey errors, random survey errors, improperly formulated orthometric corrections, and intrasurvey movement; the last of these has created the most serious problems encountered in our reconstruction of the basic data. A variety of independent tests indicate that survey error associated with the utilized levelings was generally small and fell largely within the predicted random-error range. Moreover, the redundancy and coherence displayed by the entire data set provide convincing evidence of survey accuracy and the virtual absence of height- and slope-dependent error in particular.
Our reconstructions of the changing configuration of the uplift derive chiefly from comparisons among sequentially developed observed elevations along the same route. Most of the observed elevations from which the vertical displacements were computed have been reconstructed with respect to bench mark Tidal 8, San Pedro, as invariant in height. Because the San Pedro tide station has been characterized by a history of modest relative uplift, vertical displacements referred to this station are biased slightly toward the appearance of subsidence. Where the observed elevations cannot be conveniently tied to Tidal 8, they have been referred to secondary control points whose history with respect to Tidal 8 can be independently established. Each of the lines of observed elevation changes provides, accordingly, a section athwart or along the axis of the uplift from which the changes in the configuration of the uplift can be roughly generalized. Because relatively few surveys were run in 1955, which we choose as a representative temporal datum, we have commonly incorporated the results of earlier or of somewhat later levelings as the equivalents of 1955 surveys. Although this procedure introduces a certain subjectivity, the probable equivalence between the results of these earlier or later surveys with those that would have been obtained had this leveling been carried out in 1955, usually can be independently tested. Wherever the calculated vertical displacements are based on comparisons between the results of levelings over different routes, the observed elevations have been orthometrically corrected to agree with those that would have been produced had each of these surveys been along the same route.
The growth of the southern California uplift consisted of two well-defined spasms of positive movement, the second of which was closely followed by partial collapse. Our reconstruction, although it clearly errs in detail, indicates that the uplift, together with marginal and apparently ephemeral tectonic subsidence, nucleated in the west-central Transverse Ranges near Ozena, sometime between the spring of 1959 and the spring of 1960. The uplift expanded rapidly eastward (and probably westward as well), and by the fall of 1961 much of the Transverse Ranges and the Mojave Desert at least as far east as Twentynine Palms had risen by as much as 0.25 m. Between 1962 and 1972 the area included by the initially developed (1959-61) uplift sustained additional but clearly decelerating uplift accompanied locally by oscillatory displacements. Between 1972/ 73 and 1974 a second crustal spasm extended the uplift eastward to the Colorado River and elevated much of the eastern Mojave Desert by values that equaled or exceeded those developed within the western lobe. Between 1974 and 1976, at least the central part of the uplift sustained partial collapse that nowhere amounted to less than 50 percent of the cumulative uplift since 1959. Whether this collapse affected the entire uplift is conjectural, but we now recognize well-defined evidence of major down-to-the-north tilting that must have occurred within the eastern part of the uplift at some time between 1974 and 1976.
Accumulating evidence indicates that nearly all the area included with the southern California uplift underwent similar uplift and partial collapse during the early part of the 20th century. Thus we infer that the recent uplift represents but a single event in an ongoing, more or less cyclic deformational process characterized by a period of about 50 years. Even though less than two full cycles are expressed in the geodetic record, the cumulative rate of uplift near the center of the recent uplift probably has averaged about 5 mm/yr, a value that is roughly consistent with the uplift rates that have been deduced for the late Quaternary emergent marine terraces along the south flank of the Transverse Ranges.
Although the evolution of the recent uplift is relatively well defined, its correlation with the regional seismicity is poorly defined. A comparison between the occurrence of southern California earthquakes of magnitude ≥4 during the period 1932 to 1976 with the 1974 configuration of the uplift demonstrates the existence of (1) relatively aseismic areas within the western lobe of the uplift (in the western Transverse Ranges), in the central part of the uplift (in the western Mojave Desert), and along an east-trending zone that extends into the eastern Mojave athwart the south flank of the uplift (north of the Salton Sea) and (2) localized concentrations of seismic activity along the flanks of the uplift. Moreover, 9 of the 10 largest earthquakes recorded within or around the area of the southern California uplift during the period 1932 to 1976 (the 1933 Long Beach, the 1941 Santa Barbara, the 1946 Walker Pass, the 1947 Manix, the 1948 Desert Hot Springs, and the four major 1952 Kern County shocks) occurred before the inception of the uplift in 1959 or 1960.
The area embraced by the southern California uplift has been identified with geodetically defined horizontal strain, part of which may have accumulated as a major north-south contractional event that roughly coincided with the first spasm of uplift. Nonetheless, continuing contractional strain associated with regionally developed partial collapse argues that the uplift cannot be fully explained simply as the vertical expression of continuing north-south compression. Consideration of the two well-defined historical episodes of uplift and partial collapse indicate that the southern California uplift may be the product of decoupling and viscous flow beneath the seismogenic zone, presumably driven by continuing motion between the irregularly margined plates south of the great bend of the San Andreas fault. Because the magnitude of the maximum uplift associated with each episode was approximately the same, there may be some threshold value above which collapse (viscous flow) may ensue; the absence of total collapse may be a function of precollapse strain hardening within the postulated subseismogenic viscoelastic layer.
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Robert O.","contributorId":22741,"corporation":false,"usgs":true,"family":"Castle","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":219969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliot, Michael R.","contributorId":189355,"corporation":false,"usgs":true,"family":"Elliot","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":219967,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Church, Jack P.","contributorId":6480,"corporation":false,"usgs":true,"family":"Church","given":"Jack","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":219966,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wood, Spencer H. 0000-0002-5794-2619","orcid":"https://orcid.org/0000-0002-5794-2619","contributorId":16111,"corporation":false,"usgs":false,"family":"Wood","given":"Spencer","email":"","middleInitial":"H.","affiliations":[{"id":6934,"text":"University of 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Selected well data including: Water quality, quantity and depth to bedrock in the Havre 30' x 60' quadrangle, Montana","interactions":[],"lastModifiedDate":"2022-06-13T21:48:44.564005","indexId":"ofr84688","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-688","title":"Buried or abandoned drainage in the Havre 30' x 60' quadrangle, Montana. Selected well data including: Water quality, quantity and depth to bedrock in the Havre 30' x 60' quadrangle, Montana","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84688","usgsCitation":"Colton, R.B., and Patton, T.W., 1984, Buried or abandoned drainage in the Havre 30' x 60' quadrangle, Montana. Selected well data including: Water quality, quantity and depth to bedrock in the Havre 30' x 60' quadrangle, Montana: U.S. Geological Survey Open-File Report 84-688, 2 Plates: 36.32 × 26.29 inches and 36.62 × 26.90 inches, https://doi.org/10.3133/ofr84688.","productDescription":"2 Plates: 36.32 × 26.29 inches and 36.62 × 26.90 inches","costCenters":[],"links":[{"id":402130,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13525.htm","linkFileType":{"id":5,"text":"html"}},{"id":77744,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0688/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77743,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0688/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Havre 30' x 60' quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110,\n 48.5\n ],\n [\n -109,\n 48.5\n ],\n [\n -109,\n 49\n ],\n [\n -110,\n 49\n ],\n [\n -110,\n 48.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa10e","contributors":{"authors":[{"text":"Colton, Roger B.","contributorId":17967,"corporation":false,"usgs":true,"family":"Colton","given":"Roger","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":223662,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patton, Thomas W.","contributorId":65322,"corporation":false,"usgs":true,"family":"Patton","given":"Thomas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":223663,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36587,"text":"fwsobs82_10_68 - 1984 - Habitat Suitability Index Models: American black duck (wintering)","interactions":[],"lastModifiedDate":"2022-02-09T15:17:29.070511","indexId":"fwsobs82_10_68","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"82/10.68","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: American black duck (wintering)","docAbstract":"INTRODUCTION\r\n\r\nThe American black duck, commonly known as the black duck, is migratory and has a wide geographic range. American black ducks breed from Cape Hatteras, North Carolina, west to the Mississippi River and north through the eastern Canadian boreal forest (Bellrose 1976). The winter range extends from the Rio Grande River on the Texas coast, northeast to Lake Michigan, east to Nova Scotia, south to Florida, and west to Texas (Wright 1954).\r\n\r\nAmerican black ducks arrive on their wintering habitats between September and early December and remain there until February to April (Bellrose 1976). Their preferred habitat varies considerably through the wintering range. Habitat use appears related to food availability, freedom from disturbance, weather, and often upon the presence of large bodies of open water. These interrelated elements are essential for meeting the energy demands and other nutritional requirements of black ducks in response to the rigors of cold weather and migration.\r\n\r\nIn the Atlantic Flyway, winter populations of American black ducks concentrate in marine and estuarine wetlands (U.S. Fish and Wildlife Service 1979). They use salt marshes and small tidal bays for feeding and loafing areas. In wintering areas north of Chesapeake Bay, American black ducks frequently feed on tidal flats and rest in emergent wetlands or on ice-free bays, rivers, and coastal reservoirs. In the Chesapeake bay area, migrant and wintering American black ducks occupy a wide variety of habitats (Stewart 1962). They strongly favor brackish bays with extensive adjacent agricultural lands. Estuarine bays, coastal salt marshes, tidal fresh marshes, and adjacent impoundments receive high usage. American black ducks also concentrate in forested wetlands in and adjacent to estuaries in the South Atlantic Flyway, especially in Virginia and North Carolina.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Lewis, J., and Garrison, R.L., 1984, Habitat Suitability Index Models: American black duck (wintering): FWS/OBS 82/10.68, vi, 16 p.","productDescription":"vi, 16 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":165688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649e12","contributors":{"authors":[{"text":"Lewis, James C.","contributorId":88799,"corporation":false,"usgs":true,"family":"Lewis","given":"James C.","affiliations":[],"preferred":false,"id":216594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garrison, Russell L.","contributorId":107346,"corporation":false,"usgs":true,"family":"Garrison","given":"Russell","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":216595,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36578,"text":"fwsobs82_10_56 - 1984 - Habitat Suitability Index Models: Walleye","interactions":[],"lastModifiedDate":"2022-02-09T15:19:36.985384","indexId":"fwsobs82_10_56","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"82/10.56","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Walleye","docAbstract":"The wall eye is native to freshwater ri vers and 1akes of Canada and the United States, with rare occurrences in brackish water (Scott and Crossman 1973). In the United States, its native range occurs primarily in drainages east of the Rocky Mountains and west of the Appalachians; however, it has been widely introduced into reservoirs outside its native range (Colby et al. 1979). Walleye hybridize with sauger (S. canadense) and blue pike (S. v. glaucum) (Scott and Crossman 1973).
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"McMahon, T., Terrell, J.W., and Nelson, P.C., 1984, Habitat Suitability Index Models: Walleye: FWS/OBS 82/10.56, viii, 43 p.","productDescription":"viii, 43 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":165604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6497a2","contributors":{"authors":[{"text":"McMahon, Thomas E.","contributorId":93548,"corporation":false,"usgs":true,"family":"McMahon","given":"Thomas E.","affiliations":[],"preferred":false,"id":216576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terrell, James W. 0000-0001-5394-5663","orcid":"https://orcid.org/0000-0001-5394-5663","contributorId":92726,"corporation":false,"usgs":true,"family":"Terrell","given":"James","email":"","middleInitial":"W.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":216575,"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":216574,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":38557,"text":"pp1290 - 1984 - The Mid-Cretaceous Frontier Formation near the Moxa Arch, southwestern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"pp1290","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1290","title":"The Mid-Cretaceous Frontier Formation near the Moxa Arch, southwestern Wyoming","docAbstract":"The Frontier Formation in the Green River Basin of Wyoming, Utah, and Colorado, consists of sandstone, siltstone, and shale, and minor conglomerate, coal, and bentonite. These strata were deposited in several marine and nonmarine environments during early Late Cretaceous time. At north-trending outcrops along the eastern edge of the overthrust belt, the Frontier is of Cenomanian, Turonian, and early Coniacian age, and commonly is about 610 m (2,000 ft) thick. The formation in that area conformably overlies the Lower Cretaceous Aspen Shale and is divided into the following members, in ascending order: Chalk Creek, Coalville, Allen Hollow, Oyster Ridge Sandstone, and Dry Hollow. In west-trending outcrops on the northern flank of the Uinta Mountains in Utah, the Frontier is middle and late Turonian, and is about 60 m (200 ft) thick. These strata disconformably overlie the Lower Cretaceous Mowry Shale. In boreholes on the Moxa arch, the upper part of the Frontier is of middle Turonian to early Coniacian age and unconformably overlies the lower part of the formation, which is early Cenomanian at the south end and probably Cenomanian to early Turonian at the north end. The Frontier on the arch thickens northward from less than 100 m (328 ft) to more than 300 m (984 ft) and conformably overlies the Mowry. \r\n\r\nThe marine and nonmarine Frontier near the Uinta Mountains, marine and mnmarine beds in the upper part of the formation on the Moxa arch and the largely nonmarine Dry Hollow Member at the top of the Frontier in the overthrust belt are similar in age. Older strata in the formation, which are represented by the disconformable basal contact of the Frontier near the Uinta Mountains, thicken northward along the Moxa arch and westward between the arch and the overthrust belt. The large changes in thickness of the Frontier in the Green River Basin were caused mainly by differential uplift and truncation of the lower part of the formation during the early to middle Turonian and by the shoreward addition of progressively younger sandstone units at the top of the formation during the late Turonian and early Coniacian. \r\n\r\nThe sandstone in cores of the Frontier, from boreholes on the Moxa arch and the northern plunge of the Rock Springs uplift, consists of very fine grained and fine-grained litharenites and sublitharenites that were deposited in deltaic and shallow-water marine environments. These rocks consist mainly of quartz, chert, rock fragments, mixed-layer illite-smectite, mica-illite, and chlorite. Samples of the sandstone have porosities of 4.7 to 23.0 percent and permeabilities of 0.14 to 6.80 millidarcies, and seem to represent poor to fair reservoir beds for oil and gas. \r\n\r\nThe shale in cores of the Frontier Formation and the overlying basal Hilliard Shale, from the Moxa arch, Rock Springs uplift, and overthrust belt, was deposited in deltaic and offshore-marine environments. Samples of the shale are composed largely of quartz, micaillite, mixed-layer illite-smectite, kaolin, and chlorite. They also contain from 0.27 to 4.42 percent organic carbon, in humic and sapropelic organic matter. Most of the sampled shale units are thermally mature, in terms of oil generation, and a few probably are source rocks for oil and gas.","language":"ENGLISH","doi":"10.3133/pp1290","usgsCitation":"Mereweather, E., Blackmon, P., and Webb, J., 1984, The Mid-Cretaceous Frontier Formation near the Moxa Arch, southwestern Wyoming: U.S. Geological Survey Professional Paper 1290, 29 p., https://doi.org/10.3133/pp1290.","productDescription":"29 p.","costCenters":[],"links":[{"id":125139,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1290/report-thumb.jpg"},{"id":65326,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1290/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aeb2","contributors":{"authors":[{"text":"Mereweather, E.A.","contributorId":27524,"corporation":false,"usgs":true,"family":"Mereweather","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":220058,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blackmon, P.D.","contributorId":62210,"corporation":false,"usgs":true,"family":"Blackmon","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":220059,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Webb, J.C.","contributorId":13302,"corporation":false,"usgs":true,"family":"Webb","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":220057,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":38566,"text":"pp1302 - 1984 - Basic concepts of kinematic-wave models","interactions":[],"lastModifiedDate":"2018-03-09T14:00:28","indexId":"pp1302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1302","title":"Basic concepts of kinematic-wave models","docAbstract":"The kinematic-wave model is one of a number of approximations of the dynamic-wave model. The dynamic-wave model describes onedimensional shallow-water waves (unsteady, gradually varied, openchannel flow). This report provides a basic reference on the theory and applications of the kinematic-wave model and describes the limitations of the model in relation to the other approximations of the dynamic-wave model. In the kinematic-wave approximation, a number of the terms in the equation of motion are assumed to be insignificant. The equation of motion is replaced by an equation describing uniform flow. Thus, the kinematic-wave model is described by the continuity equation and a uniform-flow equation such as the wellknown Chezy or Manning formulas. Kinematic-wave models are applicable to overland flow where lateral inflow is continuously added and is a large part of the total flow. For channel-routing applications, the kinematic-wave model always predicts a steeper wave with less dispersion and attenuation than actually occurs. The effect of the accumulation of errors in the kinematic-wave model shows that the approximations made in the development of the kinematic-wave equations are not generally justified for most channel-routing applications. Modified flow-routing models can be used which help to stop the accumulation of errors that occur when the kinematic-wave model is applied.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1302","usgsCitation":"Miller, J., 1984, Basic concepts of kinematic-wave models: U.S. Geological Survey Professional Paper 1302, vi, 29 p., https://doi.org/10.3133/pp1302.","productDescription":"vi, 29 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":65341,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1302/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1302/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485f9","contributors":{"authors":[{"text":"Miller, J.E.","contributorId":63058,"corporation":false,"usgs":true,"family":"Miller","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":220079,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55178,"text":"wdrHI831 - 1984 - Water resources data for Hawaii and other Pacific areas, water year 1983: Volume 1. Hawaii","interactions":[],"lastModifiedDate":"2025-12-02T16:24:08.295975","indexId":"wdrHI831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"HI-83-1","title":"Water resources data for Hawaii and other Pacific areas, water year 1983: Volume 1. Hawaii","docAbstract":"Water resources data for the 1983 water year for Hawaii and other Pacific Areas consist of records of stage, discharge, and water quality of streams and springs; and water levels and water quality in wells. This report, volume 1, contains discharge records for 97 gaging stations; water quality for 13 gaging stations, 92 partial-record flow stations, and 159 wells; and water levels for 24 observation wells. Also included are 108 crest-stage partial-record stations and 24 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, Federal, and other agencies in Hawaii.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrHI831","collaboration":"Prepared in cooperation with the State of Hawaii Department of Land and Natural Resources, Division of Water and Land Development and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Water resources data for Hawaii and other Pacific areas, water year 1983: Volume 1. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a75e4b07f02db644a3f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532281,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55179,"text":"wdrHI832 - 1984 - Water resources data for Hawaii and other Pacific areas, water year 1983: Volume 2. Guam, Northern Mariana Islands, Federated States of Micronesia, Palau, and American Samoa","interactions":[],"lastModifiedDate":"2025-12-11T17:03:31.710338","indexId":"wdrHI832","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"HI-83-2","title":"Water resources data for Hawaii and other Pacific areas, water year 1983: Volume 2. Guam, Northern Mariana Islands, Federated States of Micronesia, Palau, and American Samoa","docAbstract":"Volume 2 of water resources data for the 1983 water year for other Pacific areas consists of records of stage, discharge, and water quality of streams and springs; stage of a lake and a reservoir; and water levels and water quality in wells. This report contains discharge records for 37 gaging stations; stage only record for 2 gaging stations; water quality for 9 gaging stations; 12 partial-record stations; water temperature for 36 gaging stations; and water levels for 30 observation wells and water quality for 78 ground-water sites. Also included are 43 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Governments and Federal agencies in other Pacific areas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrHI832","collaboration":"Prepared in cooperation with the Governments of Guam, Northern Mariana Islands, Federated States of Micronesia, Palau, American Samoa, and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Water resources data for Hawaii and other Pacific areas, water year 1983: Volume 2. Guam, Northern Mariana Islands, Federated States of Micronesia, Palau, and American Samoa: U.S. Geological Survey Water Data Report HI-83-2, viii, 162 p., https://doi.org/10.3133/wdrHI832.","productDescription":"viii, 162 p.","costCenters":[],"links":[{"id":497336,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/hi-83-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174381,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1983/hi-83-2/report-thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"American Samoa, Federated States of Micronesia, Guam, Northern Mariana Islands, 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6f4d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55530,"text":"wdrLA841 - 1984 - Water resources data, Louisiana, water year 1984","interactions":[],"lastModifiedDate":"2025-12-02T16:51:26.348549","indexId":"wdrLA841","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"LA-84-1","title":"Water resources data, Louisiana, water year 1984","docAbstract":"Water resources data for the 1984 water year for Louisiana consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground water. This report, in one volume, contains records for water discharge at 72 gaging stations (including stage for 71 of these stations); stage only for 40 gaging stations and 11 lakes; water quality for 80 surface-water stations (including 26 gaging stations), 17 miscellaneous sites, 10 lakes, and 145 wells; and water levels for 423 observation wells. Also included are data for 141 crest-stage and flood-profile partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Louisiana.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrLA841","collaboration":"Prepared in cooperation with the Louisiana Department of Transportation and Development and with other State and Federal agencies","usgsCitation":"Carlson, D., Stallworth, G., Dantin, L., and Stuart, C., 1984, Water resources data, Louisiana, water year 1984: U.S. Geological Survey Water Data Report LA-84-1, xi, 608 p., https://doi.org/10.3133/wdrLA841.","productDescription":"xi, 608 p.","costCenters":[],"links":[{"id":496994,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/la-84-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181503,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/la-84-1/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f12c8","contributors":{"authors":[{"text":"Carlson, D.D.","contributorId":10816,"corporation":false,"usgs":true,"family":"Carlson","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":253651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stallworth, G.R.","contributorId":107732,"corporation":false,"usgs":true,"family":"Stallworth","given":"G.R.","affiliations":[],"preferred":false,"id":253654,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dantin, L.J.","contributorId":61891,"corporation":false,"usgs":true,"family":"Dantin","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":253653,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stuart, C.G.","contributorId":58644,"corporation":false,"usgs":true,"family":"Stuart","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":253652,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":55712,"text":"wdrND831 - 1984 - Water resources data, North Dakota, water year 1983","interactions":[],"lastModifiedDate":"2025-12-02T17:00:40.938619","indexId":"wdrND831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ND-83-1","title":"Water resources data, North Dakota, water year 1983","docAbstract":"Water resources data for the 1983 water year for North Dakota consist of records of stage discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground water. This report contains discharge records for 112 gaging stations; stage only records for 17 gaging stations; stage and contents for 10 lakes and reservoirs; water quality for 109 gaging stations; 5 lakes, 29 wells, and water levels for 31 observation wells. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in North Dakota.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8441","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Land use series, Boise [quadrangle], Idaho-Oregon: U.S. Geological Survey Open-File Report 84-41, 3 Sheets: 39.82 x 28.16 inches or smaller, https://doi.org/10.3133/ofr8441.","productDescription":"3 Sheets: 39.82 x 28.16 inches or smaller","costCenters":[],"links":[{"id":499068,"rank":4,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1984/0041/sheet-3.pdf","text":"Sheet 3","linkFileType":{"id":1,"text":"pdf"}},{"id":499067,"rank":3,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1984/0041/sheet-2.pdf","text":"Sheet 2","linkFileType":{"id":1,"text":"pdf"}},{"id":499066,"rank":2,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1984/0041/sheet-1.pdf","text":"Sheet 1","linkFileType":{"id":1,"text":"pdf"}},{"id":172822,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0041/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Boise quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -118,\n 44\n ],\n [\n -118,\n 43\n ],\n [\n -116,\n 43\n ],\n [\n -116,\n 44\n ],\n [\n -118,\n 44\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a10c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531051,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55626,"text":"wdrMARI821 - 1984 - Water resources data, Massachusetts and Rhode Island, water year 1982","interactions":[],"lastModifiedDate":"2025-09-24T20:51:07.454327","indexId":"wdrMARI821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MA-RI-82-1","title":"Water resources data, Massachusetts and Rhode Island, water year 1982","docAbstract":"Water-resources data for the 1982 water year for Massachusetts and Rhode Island consist of records of stage, discharge, and water quality of streams; contents of lakes and reservoirs; and ground-water levels. This report contains discharge records for 97 gaging stations, monthend contents for 30 lakes and reservoirs, water quality for 10 gaging stations, and water levels for 107 observation wells. Also included are data for 3 low-flow and 18 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. A few pertinent stations (not included above) in bordering States are also included in this report. These data represent that portion of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Massachusetts and Rhode Island.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMARI821","collaboration":"This report was prepared in cooperation with the States of Massachusetts and Rhode Island and with other agencies","usgsCitation":"Gadoury, R.A., Girouard, G., and Letty, D., 1984, Water resources data, Massachusetts and Rhode Island, water year 1982: U.S. Geological Survey Water Data Report MA-RI-82-1, vii, 237 p., https://doi.org/10.3133/wdrMARI821.","productDescription":"vii, 237 p.","costCenters":[],"links":[{"id":174499,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/mari-82-1/report-thumb.jpg"},{"id":496059,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/mari-82-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts, Rhode Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -73.50297488831188,\n 42.97016577848564\n ],\n [\n -73.50297488831188,\n 41.11994266161375\n ],\n [\n -69.8918541821574,\n 41.11994266161375\n ],\n [\n -69.8918541821574,\n 42.97016577848564\n ],\n [\n -73.50297488831188,\n 42.97016577848564\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f123c","contributors":{"authors":[{"text":"Gadoury, R. A.","contributorId":26334,"corporation":false,"usgs":true,"family":"Gadoury","given":"R.","middleInitial":"A.","affiliations":[],"preferred":false,"id":253848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Girouard, G.G.","contributorId":88017,"corporation":false,"usgs":true,"family":"Girouard","given":"G.G.","affiliations":[],"preferred":false,"id":253850,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Letty, D.F.","contributorId":36996,"corporation":false,"usgs":true,"family":"Letty","given":"D.F.","affiliations":[],"preferred":false,"id":253849,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30809,"text":"ofr84466 - 1984 - Movement and fate of creosote waste in ground water, Pensacola, Florida; U.S. Geological Survey toxic waste--ground-water contamination program","interactions":[{"subject":{"id":30809,"text":"ofr84466 - 1984 - Movement and fate of creosote waste in ground water, Pensacola, Florida; U.S. Geological Survey toxic waste--ground-water contamination program","indexId":"ofr84466","publicationYear":"1984","noYear":false,"title":"Movement and fate of creosote waste in ground water, Pensacola, Florida; U.S. Geological Survey toxic waste--ground-water contamination program"},"predicate":"SUPERSEDED_BY","object":{"id":130,"text":"wsp2285 - 1986 - Movement and fate of creosote waste in ground water, Pensacola, Florida; U.S. Geological Survey toxic waste-ground-water contamination program","indexId":"wsp2285","publicationYear":"1986","noYear":false,"title":"Movement and fate of creosote waste in ground water, Pensacola, Florida; U.S. Geological Survey toxic waste-ground-water contamination program"},"id":1}],"supersededBy":{"id":130,"text":"wsp2285 - 1986 - Movement and fate of creosote waste in ground water, Pensacola, Florida; U.S. Geological Survey toxic waste-ground-water contamination program","indexId":"wsp2285","publicationYear":"1986","noYear":false,"title":"Movement and fate of creosote waste in ground water, Pensacola, Florida; U.S. Geological Survey toxic waste-ground-water contamination program"},"lastModifiedDate":"2018-10-22T17:55:31","indexId":"ofr84466","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-466","title":"Movement and fate of creosote waste in ground water, Pensacola, Florida; U.S. Geological Survey toxic waste--ground-water contamination program","docAbstract":"In 1983, the U.S. Geological Survey, Office of Hazardous Waste Hydrology, selected the former American Creosote Works site near Pensacola, Florida as a national research demonstration area. Seventy-nine years (1902-81) of seepage from unlined discharge impoundments had released creosote, diesel fuel, and pentachlorophenol (since 1950) wastes into the ground-water system. A cluster of from 2 to 5 wells constructed at different depths at 9 sites yielded water which revealed contamination 600 feet downgradient and to a depth of 100 feet below land surface near the site. The best cross-sectional representation of the contaminant plume was obtained from samples collected and analyzed for oxidation-reduction sensitive inorganic chemical constituents. Energy dispersive x-ray fluorescence detected recently formed iron carbonate in soil samples from highly reducing ground-water zones. Approximately eighty specific organic contaminants were isolated from ground-water samples by gas-chromotography/mass spectrometry. Column studies indicate the dimethyl phenols are not sorbed or degraded by the sand-and-gravel aquifer materials. Five of nineteen individual phenolic and related compounds are biodegradable based on anaerobic digestor experiments with ACW site bacterial populations. The potential impacts in the nearby Pensacola Bay biotic community are being evaluated. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84466","usgsCitation":"Franks, B., 1984, Movement and fate of creosote waste in ground water, Pensacola, Florida; U.S. Geological Survey toxic waste--ground-water contamination program: U.S. Geological Survey Open-File Report 84-466, x, 93 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84466.","productDescription":"x, 93 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":275864,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0466/report.pdf"},{"id":161041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0466/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698ca0","contributors":{"editors":[{"text":"Mattraw, H.C. Jr.","contributorId":81957,"corporation":false,"usgs":true,"family":"Mattraw","given":"H.C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":749251,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Franks, B.J.","contributorId":107739,"corporation":false,"usgs":true,"family":"Franks","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":204014,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25394,"text":"wri844159 - 1984 - Analysis of urban storm-runoff data and the effects on the South Platte River, Denver metropolitan area, Colorado","interactions":[],"lastModifiedDate":"2026-01-22T18:48:01.342746","indexId":"wri844159","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4159","title":"Analysis of urban storm-runoff data and the effects on the South Platte River, Denver metropolitan area, Colorado","docAbstract":"Denver was selected for inclusion in the Nationwide Urban Runoff Program, sponsored by the U.S. Environmental Protection Agency and the U.S. Geological Survey. This report, prepared in cooperation with the Denver Regional council of governments, contains a synopsis of previous urban runoff studies in the Denver metropolitan area. The report includes a description of the monitored basins, a summary of storm runoff-to-rainfall ratios and estimates of impervious retention, and constituent loads and concentrations from seven small basins. The data from six small and five tributary basins to the South Platte River are analyzed using regression analysis, resulting in two sets of regression equations to predict storm runoff volume and selected constituent loads. The regression equations may be used to estimate storm-runoff volume and constituent loads from unmonitored basins from 15 to 16,000 acres with effective impervious areas of 15 to 90 percent. The effects of urban runoff on the South Platte River in the Denver area are described in three ways. The three methods indicated that storm runoff was a significant contributor of total suspended solids, total organic carbon, total lead, and total zinc to the South Platte River.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844159","usgsCitation":"Ellis, S.R., Doerfer, J., Mustard, M.H., Blakely, S.R., and Gibbs, J.W., 1984, Analysis of urban storm-runoff data and the effects on the South Platte River, Denver metropolitan area, Colorado: U.S. Geological Survey Water-Resources Investigations Report 84-4159, vi, 66 p., https://doi.org/10.3133/wri844159.","productDescription":"vi, 66 p.","costCenters":[],"links":[{"id":414376,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36032.htm","linkFileType":{"id":5,"text":"html"}},{"id":123692,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4159/report-thumb.jpg"},{"id":54126,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4159/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","city":"Denver","otherGeospatial":"South Platte River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.25,\n 39.842\n ],\n [\n -105.25,\n 39.5\n ],\n [\n -104.75,\n 39.5\n ],\n [\n -104.75,\n 39.842\n ],\n [\n -105.25,\n 39.842\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae29b","contributors":{"authors":[{"text":"Ellis, S. 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W.","contributorId":66699,"corporation":false,"usgs":true,"family":"Gibbs","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":193511,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":25652,"text":"wri834118B - 1984 - Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri834118B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4118","chapter":"B","title":"Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834118B","usgsCitation":"Brady, B.T., Mulvihill, D.A., Hart, D., and Langer, W.H., 1984, Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 83-4118, 6 p. :maps ;28 cm., https://doi.org/10.3133/wri834118B.","productDescription":"6 p. :maps ;28 cm.","costCenters":[],"links":[{"id":121726,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4118b/report-thumb.jpg"},{"id":54421,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4118b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54422,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4118b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54423,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4118b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605a4f","contributors":{"authors":[{"text":"Brady, B. T.","contributorId":93047,"corporation":false,"usgs":true,"family":"Brady","given":"B.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":194520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mulvihill, D. A.","contributorId":73644,"corporation":false,"usgs":true,"family":"Mulvihill","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hart, D.L.","contributorId":13239,"corporation":false,"usgs":true,"family":"Hart","given":"D.L.","affiliations":[],"preferred":false,"id":194517,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":194518,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":26377,"text":"wri844175 - 1984 - Hydrologic effects of impoundments in Sherburne National Wildlife Refuge, Minnesota","interactions":[],"lastModifiedDate":"2018-03-05T11:33:26","indexId":"wri844175","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4175","title":"Hydrologic effects of impoundments in Sherburne National Wildlife Refuge, Minnesota","docAbstract":"The hydrologic effects of proposed impoundments in Sherburne National Wildlife Refuge were found to be insignificant with respect to both ground- and surface-water flow patterns and water quality. Monitoring of water levels in 23 observation wells and of discharge in the St. Francis River during 1980 and 1981 has shown that ground water in the surf icial aquifer responds quickly to areal recharge and subsequently discharges to the St. Francis River. The impoundment of surface water in the refuge was not found to affect water levels in the refuge significantly. The impoundments may affect ground-water-flow systems beneath and adjacent to the impoundments. Quality of ground and surface water was found to be similar except ground water contained higher concentrations of dissolved nitrite plus nitrate nitrogen than surface water. Phytoplankton removed dissolved nitrite plus nitrate nitrogen from surface water. The effects of impoundments on water quality are expected to be minor.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri844175","collaboration":"Prepared in cooperation with the U.S. Fish and Wildlife Service","usgsCitation":"Brown, R.G., 1984, Hydrologic effects of impoundments in Sherburne National Wildlife Refuge, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 84-4175, iv, 20 p., https://doi.org/10.3133/wri844175.","productDescription":"iv, 20 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":55169,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4175/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4175/report-thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Sherburne county","otherGeospatial":"Sherburne National Wildlife Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.85482788085938,\n 45.36854917415683\n ],\n [\n -93.85482788085938,\n 45.58425087527735\n ],\n [\n -93.50875854492188,\n 45.58425087527735\n ],\n [\n -93.50875854492188,\n 45.36854917415683\n ],\n [\n -93.85482788085938,\n 45.36854917415683\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606ff3","contributors":{"authors":[{"text":"Brown, R. G.","contributorId":106118,"corporation":false,"usgs":true,"family":"Brown","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":196282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25695,"text":"wri844186 - 1984 - Partial compilation and revision of basic data in the WATEQ programs","interactions":[],"lastModifiedDate":"2018-03-21T15:28:32","indexId":"wri844186","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4186","title":"Partial compilation and revision of basic data in the WATEQ programs","docAbstract":"Several portions of the basic data in the WATEQ series of computer programs (WATEQ, WATEQF, WATEQ2, WATEQ3, and PHREEQE) are compiled. The density and dielectric constant of water and their temperature dependence are evaluated for the purpose of updating the Debye-Huckel solvent parameters in the activity coefficient equations. The standard state thermodynamic properties of the Fe2+ and Fe3+ aqueous ions are refined. The main portion of this report is a comprehensive listing of aluminum hydrolysis constants, aluminum fluoride, aluminum sulfate, calcium chloride, magnesium chloride, potassium sulfate and sodium sulfate stability constants, solubility product constants for gibbsite and amorphous aluminum hydroxide, and the standard electrode potentials for Fe (s)/Fe2+(aq) and Fe2 +(aq)/Fe3+(aq). (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844186","usgsCitation":"Nordstrom, D.K., Valentine, S., Ball, J., Plummer, N., and Jones, B., 1984, Partial compilation and revision of basic data in the WATEQ programs: U.S. Geological Survey Water-Resources Investigations Report 84-4186, iii, 40 p. :ill. ;28 cm., https://doi.org/10.3133/wri844186.","productDescription":"iii, 40 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":54460,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4186/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122708,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4186/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf81","contributors":{"authors":[{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":194695,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Valentine, S.D.","contributorId":19194,"corporation":false,"usgs":true,"family":"Valentine","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":194691,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ball, J.W.","contributorId":67507,"corporation":false,"usgs":true,"family":"Ball","given":"J.W.","affiliations":[],"preferred":false,"id":194693,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":194694,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jones, B.F.","contributorId":52156,"corporation":false,"usgs":true,"family":"Jones","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":194692,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":25638,"text":"wri834119E - 1984 - Map showing outcrops of pre-Quaternary ash-flow tuffs and volcaniclastic rocks, Basin and Range Province, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri834119E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4119","chapter":"E","title":"Map showing outcrops of pre-Quaternary ash-flow tuffs and volcaniclastic rocks, Basin and Range Province, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834119E","usgsCitation":"Sargent, K.A., and Roggensack, K., 1984, Map showing outcrops of pre-Quaternary ash-flow tuffs and volcaniclastic rocks, Basin and Range Province, Nevada: U.S. Geological Survey Water-Resources Investigations Report 83-4119, 54 p. :maps ;28 cm., https://doi.org/10.3133/wri834119E.","productDescription":"54 p. :maps ;28 cm.","costCenters":[],"links":[{"id":118834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4119e/report-thumb.jpg"},{"id":54393,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4119e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54394,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4119e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54395,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4119e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3775","contributors":{"authors":[{"text":"Sargent, K. A.","contributorId":58630,"corporation":false,"usgs":true,"family":"Sargent","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roggensack, Kurt","contributorId":35771,"corporation":false,"usgs":true,"family":"Roggensack","given":"Kurt","email":"","affiliations":[],"preferred":false,"id":194491,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26383,"text":"wri824049 - 1984 - Flow routing in the Susquehanna River basin: Part V – Flow-routing models for the West Branch Susquehanna River basin, Pennsylvania","interactions":[],"lastModifiedDate":"2022-01-04T20:02:21.811502","indexId":"wri824049","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"82-4049","title":"Flow routing in the Susquehanna River basin: Part V – Flow-routing models for the West Branch Susquehanna River basin, Pennsylvania","docAbstract":"Digital-computer, daily-flow routing models were developed for four consecutive reaches of the West Branch Susquehanna River between Curwensville and Lewisburg, Pennsylvania. These models will enable water-resources managers to evaluate efficiently the effect of present and future water-resources developments on streamflows at six locations along the West Branch Susquehanna River. The models utilize a unit-response, convolution technique of flowrouting based on diffusion analogy and multilinearization. Estimates of streamflow from the intervening areas of each reach, wave celerity, and wave-dispersion coefficients are the model parameters. These were adjusted until simulated outflow hydrographs and flow statistics adequately approximated those for observed flow data. The overall accuracy of the models is considered good. Average, absolute, daily flow errors between observed and simulated flows ranged from 8.82 to 13.70 percent for the periods that were evaluated. Volume errors for the same periods were between -0.01 and 1.61 percent. Estimates of the 7-day, 10-year low flows for simulated conditions were within 5 percent of those computed for observed flows.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824049","usgsCitation":"Brua, S.A., 1984, Flow routing in the Susquehanna River basin: Part V – Flow-routing models for the West Branch Susquehanna River basin, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 82-4049, v, 42 p., https://doi.org/10.3133/wri824049.","productDescription":"v, 42 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":119099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4049/report-thumb.jpg"},{"id":55172,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4049/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393872,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35573.htm"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Susquehanna River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.881,\n 40.6720\n ],\n [\n -76.4,\n 40.6720\n ],\n [\n -76.4,\n 41.717\n ],\n [\n -78.881,\n 41.717\n ],\n [\n -78.881,\n 40.6720\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de832","contributors":{"authors":[{"text":"Brua, S. A.","contributorId":53844,"corporation":false,"usgs":true,"family":"Brua","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196291,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25654,"text":"wri834116B - 1984 - Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Southern California","interactions":[],"lastModifiedDate":"2020-03-27T14:22:19","indexId":"wri834116B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4116","chapter":"B","title":"Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Southern California","docAbstract":"This report on ground-water levels, springs and depth to ground water in the Basin and Range province of southern California (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing program guidelines defined in Sargent and Bedinger (1984). Also included in this report are selected references on pertinent geologic and hydrologic studies of the region. Other map reports in this series contain detailed data on ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834116B","usgsCitation":"Langer, W.H., Moyle, W., Woolfenden, L.R., and Mulvihill, D.A., 1984, Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Southern California: U.S. Geological Survey Water-Resources Investigations Report 83-4116, Report: 6 p.; 2 Plates: 41.09 x 53.96 inches and 41.37 x 53.85 inches, https://doi.org/10.3133/wri834116B.","productDescription":"Report: 6 p.; 2 Plates: 41.09 x 53.96 inches and 41.37 x 53.85 inches","costCenters":[],"links":[{"id":373616,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4116b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118965,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4116b/report-thumb.jpg"},{"id":373615,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4116b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54425,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4116b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.87158203125,\n 32.509761735919426\n ],\n [\n -114.14794921875,\n 32.509761735919426\n ],\n [\n -114.14794921875,\n 38.805470223177466\n ],\n [\n -120.87158203125,\n 38.805470223177466\n ],\n [\n -120.87158203125,\n 32.509761735919426\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605a5d","contributors":{"authors":[{"text":"Langer, William H. blanger@usgs.gov","contributorId":1241,"corporation":false,"usgs":true,"family":"Langer","given":"William","email":"blanger@usgs.gov","middleInitial":"H.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":false,"id":194526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moyle, W. R.","contributorId":27421,"corporation":false,"usgs":true,"family":"Moyle","given":"W. R.","affiliations":[],"preferred":false,"id":194524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woolfenden, L. R. 0000-0003-3500-4709","orcid":"https://orcid.org/0000-0003-3500-4709","contributorId":36945,"corporation":false,"usgs":true,"family":"Woolfenden","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":194525,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mulvihill, D. A.","contributorId":73644,"corporation":false,"usgs":true,"family":"Mulvihill","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194527,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":25449,"text":"wri834160 - 1984 - A digital model for streamflow routing by convolution methods","interactions":[],"lastModifiedDate":"2012-02-02T00:08:19","indexId":"wri834160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4160","title":"A digital model for streamflow routing by convolution methods","docAbstract":"U.S. Geological Survey computer model, CONROUT, for routing streamflow by unit-response convolution flow-routing techniques from an upstream channel location to a downstream channel location has been developed and documented. Calibration and verification of the flow-routing model and subsequent use of the model for simulation is also documented. Three hypothetical examples and two field applications are presented to illustrate basic flow-routing concepts. Most of the discussion is limited to daily flow routing since, to date, all completed and current studies of this nature involve daily flow routing. However, the model is programmed to accept hourly flow-routing data. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/wri834160","usgsCitation":"Doyle, W., Shearman, H., Stiltner, G., and Krug, W., 1984, A digital model for streamflow routing by convolution methods: U.S. Geological Survey Water-Resources Investigations Report 83-4160, vi, 136 p. :ill., charts ;28 cm., https://doi.org/10.3133/wri834160.","productDescription":"vi, 136 p. :ill., charts ;28 cm.","costCenters":[],"links":[{"id":124901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4160/report-thumb.jpg"},{"id":54183,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aed4c","contributors":{"authors":[{"text":"Doyle, W.H. Jr.","contributorId":59029,"corporation":false,"usgs":true,"family":"Doyle","given":"W.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":193741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shearman, H.O.","contributorId":40630,"corporation":false,"usgs":true,"family":"Shearman","given":"H.O.","email":"","affiliations":[],"preferred":false,"id":193739,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stiltner, G.J.","contributorId":56668,"corporation":false,"usgs":true,"family":"Stiltner","given":"G.J.","affiliations":[],"preferred":false,"id":193740,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Krug, W.O.","contributorId":77964,"corporation":false,"usgs":true,"family":"Krug","given":"W.O.","email":"","affiliations":[],"preferred":false,"id":193742,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":26559,"text":"wri844339 - 1984 - Tides, tidal and residual currents in San Francisco Bay California — Results of measurements, 1979–1980","interactions":[],"lastModifiedDate":"2022-01-26T20:24:13.835979","indexId":"wri844339","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4339","title":"Tides, tidal and residual currents in San Francisco Bay California — Results of measurements, 1979–1980","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844339","usgsCitation":"Cheng, R.T., and Gartner, J.W., 1984, Tides, tidal and residual currents in San Francisco Bay California — Results of measurements, 1979–1980: U.S. Geological Survey Water-Resources Investigations Report 84-4339, 1778 p., https://doi.org/10.3133/wri844339.","productDescription":"1778 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":394910,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36174.htm"},{"id":157321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4339/report-thumb.jpg"},{"id":55426,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4339/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.62939453125001,\n 37.33522435930639\n ],\n [\n -121.62963867187499,\n 37.33522435930639\n ],\n [\n -121.62963867187499,\n 38.30718056188316\n ],\n [\n -122.62939453125001,\n 38.30718056188316\n ],\n [\n -122.62939453125001,\n 37.33522435930639\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b76d","contributors":{"authors":[{"text":"Cheng, R. T.","contributorId":23138,"corporation":false,"usgs":false,"family":"Cheng","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":196616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gartner, J. W.","contributorId":81903,"corporation":false,"usgs":false,"family":"Gartner","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":196617,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25898,"text":"wri824073 - 1984 - Runoff, sediment transport, and water quality in a northern Illinois agricultural watershed before urban development, 1979-81","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri824073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"82-4073","title":"Runoff, sediment transport, and water quality in a northern Illinois agricultural watershed before urban development, 1979-81","docAbstract":"A study designed to quantify and evaluate changes in runoff and sediment transport attributable to construction activities during urban development of a watershed required identification of pre-construction hydrologic conditions. Data collected before construction on a 2.81 sq m (7.28 sq km) agricultural watershed (upper Spring Creek) near Rockford, IL, show that during a 2-year period ending June 30, 1981, 2,890 tons (2,620 Mg) of suspended sediment were transported from the watershed. Of the 2 ,890 tons (2,620 Mg), 2,690 tons (2,440 Mg) or 93.1 % were transported during a storm in a 46.6-hour period of June 13-14, 1981. Runoff from a 0.031 sq m (0.080 sq km) subbasin (Spring Creek tributary) transported 33.9 tons (30.9 Mg) of suspended sediment during a 3.2-hour storm period on June 13, 1981. Regression models relating storm suspended-sediment yields and peak-water discharge per square mile for upper Spring Creek and Spring Creek tributary have average standard errors of 57 and 24 %, respectively. Trace amounts of currently banned pesticides, including Aldrin and DDT, were detected in streambed material samples. Documented sediment yields, chemical quality, and relations between runoff and sediment discharge provide baseline information for future evaluation of hydrologic conditions in the watershed. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824073","usgsCitation":"Allen, H., and Gray, J.R., 1984, Runoff, sediment transport, and water quality in a northern Illinois agricultural watershed before urban development, 1979-81: U.S. Geological Survey Water-Resources Investigations Report 82-4073, vii, 55 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824073.","productDescription":"vii, 55 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158136,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4073/report-thumb.jpg"},{"id":54658,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5face6","contributors":{"authors":[{"text":"Allen, H.E. Jr.","contributorId":63054,"corporation":false,"usgs":true,"family":"Allen","given":"H.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":195440,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gray, J. R.","contributorId":63372,"corporation":false,"usgs":true,"family":"Gray","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":195441,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}