{"pageNumber":"243","pageRowStart":"6050","pageSize":"25","recordCount":37001,"records":[{"id":51483,"text":"ofr0351 - 2003 - Stratigraphic inferences derived from borehole data of Tertiary basin-filling rocks of the Pahrump Valley basin, Nevada and California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr0351","displayToPublicDate":"2003-03-01T00:00:00","publicationYear":"2003","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":"2003-51","title":"Stratigraphic inferences derived from borehole data of Tertiary basin-filling rocks of the Pahrump Valley basin, Nevada and California","docAbstract":"This report summarizes the results from the compilation and interpretation of lithologic information from 266 driller?s logs from the Pahrump Valley, NV-CA. Borehole records for the Pahrump Valley were selected from a total of several thousand available well logs as those having lithologic data and high confidence in the well locations. Driller?s descriptions were reduced into one of 14 lithologic categories to produce a set of subsurface data that were internally consistent and amenable to contouring. Using the lithologic descriptors, the aggregate thickness of general lithologic types (coarse grained material, fine grained material, limestone, and volcanic material) were computed for each borehole. These data were used to compute ratios such as percent coarse-grained component of sedimentary rocks penetrated in each borehole that could be contoured.","language":"ENGLISH","doi":"10.3133/ofr0351","usgsCitation":"Sweetkind, D., Taylor, E., and Putnam, H., 2003, Stratigraphic inferences derived from borehole data of Tertiary basin-filling rocks of the Pahrump Valley basin, Nevada and California (Version 1.0): U.S. Geological Survey Open-File Report 2003-51, 30 p., https://doi.org/10.3133/ofr0351.","productDescription":"30 p.","costCenters":[],"links":[{"id":178250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4484,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-051/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae70e","contributors":{"authors":[{"text":"Sweetkind, Donald S.","contributorId":18732,"corporation":false,"usgs":true,"family":"Sweetkind","given":"Donald S.","affiliations":[],"preferred":false,"id":243708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Emily","contributorId":41474,"corporation":false,"usgs":true,"family":"Taylor","given":"Emily","affiliations":[],"preferred":false,"id":243709,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Putnam, Heather","contributorId":64722,"corporation":false,"usgs":true,"family":"Putnam","given":"Heather","email":"","affiliations":[],"preferred":false,"id":243710,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":51487,"text":"ofr0344 - 2003 - Economics of undiscovered oil in Federal Lands on the National Petroleum Reserve, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:11:30","indexId":"ofr0344","displayToPublicDate":"2003-03-01T00:00:00","publicationYear":"2003","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":"2003-44","title":"Economics of undiscovered oil in Federal Lands on the National Petroleum Reserve, Alaska","language":"ENGLISH","doi":"10.3133/ofr0344","usgsCitation":"Attanasi, E., 2003, Economics of undiscovered oil in Federal Lands on the National Petroleum Reserve, Alaska (Version 1.0): U.S. Geological Survey Open-File Report 2003-44, 67 p., https://doi.org/10.3133/ofr0344.","productDescription":"67 p.","costCenters":[],"links":[{"id":179152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4487,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-044/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6259d8","contributors":{"authors":[{"text":"Attanasi, Emil 0000-0001-6845-7160 attanasi@usgs.gov","orcid":"https://orcid.org/0000-0001-6845-7160","contributorId":1809,"corporation":false,"usgs":true,"family":"Attanasi","given":"Emil","email":"attanasi@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":243720,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51479,"text":"ofr0360 - 2003 - Primary causes of wetland loss at Madison Bay, Terrebonne Parish, Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:11:33","indexId":"ofr0360","displayToPublicDate":"2003-03-01T00:00:00","publicationYear":"2003","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":"2003-60","title":"Primary causes of wetland loss at Madison Bay, Terrebonne Parish, Louisiana","language":"ENGLISH","doi":"10.3133/ofr0360","usgsCitation":"Morton, R., Tiling, G., and Ferina, N.F., 2003, Primary causes of wetland loss at Madison Bay, Terrebonne Parish, Louisiana: U.S. Geological Survey Open-File Report 2003-60, ii, 44 p. : col. ill., col. maps ; 28 cm., https://doi.org/10.3133/ofr0360.","productDescription":"ii, 44 p. : col. ill., col. maps ; 28 cm.","costCenters":[],"links":[{"id":178246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4480,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-060/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668eb4","contributors":{"authors":[{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":243700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tiling, Ginger","contributorId":82787,"corporation":false,"usgs":true,"family":"Tiling","given":"Ginger","email":"","affiliations":[],"preferred":false,"id":243699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ferina, Nicholas F.","contributorId":14047,"corporation":false,"usgs":true,"family":"Ferina","given":"Nicholas","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":243698,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":51484,"text":"ofr0350 - 2003 - Map showing alpine debris flows triggered by a July 28, 1999 thunderstorm in the central Front Range of Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr0350","displayToPublicDate":"2003-03-01T00:00:00","publicationYear":"2003","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":"2003-50","title":"Map showing alpine debris flows triggered by a July 28, 1999 thunderstorm in the central Front Range of Colorado","docAbstract":"This 1:24,000-scale map shows an inventory of debris flows that were triggered above timberline by a thunderstorm in the central Front Range of Colorado. We have classified the debris flows into two categories based on the style of initiation processes in the debris-flow source areas: 1) soil slip, and 2) non-soil slip erosive processes. This map and associated digital data are part of a larger study of the debris-flow event, results of which we plan to present in a forthcoming paper.","language":"ENGLISH","doi":"10.3133/ofr0350","usgsCitation":"Godt, J.W., and Coe, J.A., 2003, Map showing alpine debris flows triggered by a July 28, 1999 thunderstorm in the central Front Range of Colorado (Version 1.0): U.S. Geological Survey Open-File Report 2003-50, map and text (4 p.), https://doi.org/10.3133/ofr0350.","productDescription":"map and text (4 p.)","costCenters":[],"links":[{"id":110392,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54494.htm","linkFileType":{"id":5,"text":"html"},"description":"54494"},{"id":176999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4485,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-050/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658e5e","contributors":{"authors":[{"text":"Godt, Jonathan W. 0000-0002-8737-2493 jgodt@usgs.gov","orcid":"https://orcid.org/0000-0002-8737-2493","contributorId":1166,"corporation":false,"usgs":true,"family":"Godt","given":"Jonathan","email":"jgodt@usgs.gov","middleInitial":"W.","affiliations":[{"id":508,"text":"Office of the AD Hazards","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":243711,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coe, Jeffrey A. 0000-0002-0842-9608 jcoe@usgs.gov","orcid":"https://orcid.org/0000-0002-0842-9608","contributorId":1333,"corporation":false,"usgs":true,"family":"Coe","given":"Jeffrey","email":"jcoe@usgs.gov","middleInitial":"A.","affiliations":[{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":243712,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":40090,"text":"ofr02490 - 2003 - Correlation of the Klamath Mountains and Sierra Nevada","interactions":[],"lastModifiedDate":"2023-06-23T15:21:04.454118","indexId":"ofr02490","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2002-490","title":"Correlation of the Klamath Mountains and Sierra Nevada","docAbstract":"This report graphically portrays the broadly parallel tectonic development of the Klamath Mountains and Sierra Nevada from early Paleozoic to Early Cretaceous time. It is dedicated to J.S. Diller of the U.S. Geological Survey who, during his pioneer field studies a century ago, recognized significant similarities between these two important provinces. The report is based mainly on the numerous published reports of the field and laboratory studies by various geologists and students during the last century, and to a lesser extent on my own field work which has been substantial in the Klamath Mountains but minimal in the Sierra Nevada. For brevity, required by the format of this report, little of the extensive literature pertaining to these two provinces is referenced. This report is preliminary in nature and was prepared as an aid to further study of the tectonic relations between the Klamath Mountains and Sierra Nevada. This report consists of two sheets: Sheet 1, Map showing accreted terranes and plutons of the Klamath Mountains and Sierra Nevada, and Sheet 2, Successive accretionary episodes of the Klamath mountains and northern part of Sierra Nevada, showing related plutonic, volcanic, and metamorphic events. The map on Sheet 1 was compiled and modified from two Open-File maps (Irwin and Wooden, 1999 and 2001) which had been compiled and modified mainly from Jennings (1977), Harwood (1992), Irwin (1994), Jayko (1988), Graymer and Jones (1994), Edelman and Sharp (1989), Schweickert and others (1999), Saucedo and Wagner(1992), Saleeby and Sharp (1980), Wagner and others (1981), and various other sources. For detailed lists of the sources for the isotopic age data used in Sheets 1 and 2, see Irwin and Wooden (1999 and 2001). On Sheet 2, the accretionary episodes are shown sequentially from left to right in two tiers of figures. Episodes for the Klamath Mountains are in the upper tier; correlative episodes of the Sierra Nevada are directly below in the lower tier. The sequence shown for the Klamath Mountains is modified from Irwin and Mankinen (1998) and Irwin and Wooden (1999). The episodes are named for the accreting terranes of the Klamath Mountains, but those names may not be suitable for reference to the correlative episodes of the Sierra Nevada. In the figure for each episode, a heavy black line represents the active suture that separated oceanic crustal rocks on the left from the earlier accreted terranes on the right. Plutons are particularly useful for timing the accretionary episodes. The preaccretionary plutons, which commonly represent the roots of oceanic volcanic arcs, are shown in the accreting oceanic crustal rocks to the left of the heavy black line. The accretionary plutons consist of rock that has been subducted and remobilized as magma during the accretionary process and injected into an overlying earlier accreted terrane on the right of the heavy black line. Thus, isotopic dating of the accretionary plutons (preferably U/Pb dates measured on zircon extracted from the plutonic rock) provides a useful basis for assigning ages to the accretionary episodes. Many plutons are rootless at depth, as they tend to be truncated by the subduction zone sutures of younger accreting terranes. Volcanic deposits resulting from accretionary episodes apparently are uncommon except for those deposited on the backstop terranes. In the Klamath Mountains, the Eastern Klamath terrane, which consists of the Yreka, Trinity and Redding subterranes, was the backstop for the Central Metamorphic and younger accretionary episodes, and displays a remarkable record of sedimentation, volcanism and plutonism from Silurian-Devonian to Jurassic time. In the Sierra Nevada, the correlative backstop was the Northern Sierra terrane which shows a similar long record of volcanism in the Taylorsville, Permian, and Jurassic volcanic arc sequences. During some accretionary episodes the subducting oceanic rocks were dynamically metamorphosed to schist along the suture zone beneath the overriding accreted terranes. Examples of this in the Klamath Mountains are the Devonian Salmon and Abrams Schists of the Central Metamorphic terrane, the Triassic(?) schist of the Fort Jones terrane , and the Early Cretaceous South Fork Mountain Schist that structurally underlies Klamath Mountains terranes along much of the western edge of the province. The Fort Jones terrane and South Fork Mountains Schist were metamorphosed under blueschist-facies conditions. In the Sierra Nevada, schist that is correlative with the Central Metamorphic terrane is present in patches along the Feather River terrane (see Hacker and Peacock, 1990); the Triassic(?) Red Ant Schist is correlative with the Fort Jones terrane; but a correlative of the South Fork Mountain Schist is not present. In addition to the similarities in the sequences of accretion, plutonism, volcanism, and metamorphism, strong ties between the two provinces are also provided by paleontologic data. The Permian McCloud fusulinid fauna of the Redding subterrane also is present in the Northern Sierra terrane. Rare Tethyan fusulinids are found in Permian limestone of the Eastern Hayfork terrane of the Klamath Mountains and also in limestone blocks in the Central Belt of the Sierra Nevada. Ichthyosaur fossils have been collected from the Triassic of both the Redding subterrane and Northern Sierra terrane. Jurassic ammonites and the pelecypod Buchia concentrica occur in both the Galice Formation of the western Klamath Mountains and the Mariposa Formation of the western Sierra Nevada. Events that preceded the Central Metamorphic episode prior to Silurian-Devonian time are not clearly understood and are not shown in the succession of diagrams on Sheet 2. The oldest rocks of the Klamath Mountains are Neoproterozic and they predate the Central Metamorphic episode by possibly a hundred million years or more. They include ophiolitic rocks of the Trinity subterrane and the Antelope Mountain Quartzite of the Yreka subterrane (see Mankinen and others, 2002). In the Sierra Nevada, correlatives of the ancient ophiolitic rocks may be part of the Feather River terrane. Although Neoproterozoic fossils have not yet been found in the Sierra Nevada, petrologic study shows the quartzite of the Lang sequence is closely similar to the Antelope Mountain Quartzite (see Bond and Devay, 1980). Correlation of the two quartzite formations is also suggested by the similarity of their positions in the accretionary sequence.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02490","usgsCitation":"Irwin, W., 2003, Correlation of the Klamath Mountains and Sierra Nevada: U.S. Geological Survey Open-File Report 2002-490, 2 Plates: 39.10 x 38.30 inches and 39.35 x 33.80 inches, https://doi.org/10.3133/ofr02490.","productDescription":"2 Plates: 39.10 x 38.30 inches and 39.35 x 33.80 inches","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":169671,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02490.jpg"},{"id":285188,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0490/of02-490_s2.eps"},{"id":285187,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0490/of02-490_s1.eps"},{"id":3542,"rank":6,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0490/","linkFileType":{"id":5,"text":"html"}},{"id":110383,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54412.htm","linkFileType":{"id":5,"text":"html"},"description":"54412"},{"id":285185,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0490/pdf/of02-490_s1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":285186,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0490/pdf/of02-490_s2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","otherGeospatial":"Klamath Mountains, Sierra Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.0,34.75 ], [ -124.0,43.0 ], [ -117.0,43.0 ], [ -117.0,34.75 ], [ -124.0,34.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684563","contributors":{"authors":[{"text":"Irwin, William P.","contributorId":12889,"corporation":false,"usgs":true,"family":"Irwin","given":"William P.","affiliations":[],"preferred":false,"id":222964,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51495,"text":"ofr0334 - 2003 - Rainfall and groundwater level monitoring data (1981-1984) at Weeks Creek landslide, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:30","indexId":"ofr0334","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2003-34","title":"Rainfall and groundwater level monitoring data (1981-1984) at Weeks Creek landslide, California","language":"ENGLISH","doi":"10.3133/ofr0334","usgsCitation":"Wieczorek, G.F., 2003, Rainfall and groundwater level monitoring data (1981-1984) at Weeks Creek landslide, California (Version 1.0): U.S. Geological Survey Open-File Report 2003-34, table of data, https://doi.org/10.3133/ofr0334.","productDescription":"table of data","costCenters":[],"links":[{"id":179234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4494,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-034/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649880","contributors":{"authors":[{"text":"Wieczorek, Gerald F.","contributorId":81889,"corporation":false,"usgs":true,"family":"Wieczorek","given":"Gerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":243736,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51507,"text":"ofr0321 - 2003 - Geochemistry of Permian rocks from the margins of the Phosphoria Basin: Lakeridge core, western Wyoming","interactions":[],"lastModifiedDate":"2023-06-23T15:22:09.929093","indexId":"ofr0321","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2003-21","title":"Geochemistry of Permian rocks from the margins of the Phosphoria Basin: Lakeridge core, western Wyoming","docAbstract":"

The Permian Phosphoria Formation and interbedded units of the Park City Formation and Shedhorn Sandstone in western Wyoming represent deposition along a carbonate ramp at the eastern margin of the Phosphoria Basin, with portions of the Phosphoria units reflecting periods of upwelling and widespread phosphogenesis. Thickness-weighted slab-samples of these units were collected at a maximum interval of 3 m along an 80+ m-length of unweathered core and analyzed for major-, minor-, and trace-element contents. Interpretations of geochemistry were made within the confines of a previously recognized sequence stratigraphy framework. Major shifts in element ratios characteristic of terrigenous debris that occur at sequence boundaries at the base of the Meade Peak and Retort Members of the Phosphoria Formation are attributed to changing sediment sources. Inter-element relationships in the marine fraction indicate that bottom waters of the Phosphoria Basin were predominantly denitrifying during deposition of the Ervay, Grandeur, and Phosphoria sediments, although sulfate-reducing conditions may have existed during deposition of the lower Meade Peak sediments. Oxic conditions were prevalent during deposition of a large part of the Franson Member, which represents sedimentation in a shallow, inner- to back-ramp setting.

\n
\n

Variations in sediment facies and organic matter and trace element contents largely reflect changes in Permian sea level. Changes in sea level in basin-margin areas, such as represented by the study section, may have affected the oxidation of settling organic matter, the foci of intersection of upwelling bottom waters with the photic zone, the rate of terrigenous sedimentation, and, ultimately, the overall environment of deposition. Our study suggests that phosphogenesis can occur under lowstand, transgressive, and highstand conditions in marginal areas, assuming water depths sufficient for upwelling to occur. Formation of phosphorite layers under upwelling conditions appears to have been most dependent on a lack of dilution by terrigenous sedimentation and carbonate shoaling. Differences in the geochemistry between two similar environments represented by the upper and lower Phosphoria units are largely attributed to higher rates of diluting terrigenous sediment during deposition of the upper unit. This is consistent with prior interpretations of a more shoreward setting for the upper Phosphoria.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0321","usgsCitation":"Perkins, R.B., McIntyre, B., Hein, J.R., and Piper, D.Z., 2003, Geochemistry of Permian rocks from the margins of the Phosphoria Basin: Lakeridge core, western Wyoming: U.S. Geological Survey Open-File Report 2003-21, iv, 60 p., https://doi.org/10.3133/ofr0321.","productDescription":"iv, 60 p.","numberOfPages":"65","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":179209,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr0321.jpg"},{"id":4514,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0021/","linkFileType":{"id":5,"text":"html"}},{"id":285235,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0021/pdf/of03-21.pdf"},{"id":393796,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54231.htm"}],"country":"United States","state":"Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.475,\n 42.4833\n ],\n [\n -110.4625,\n 42.4833\n ],\n [\n -110.4625,\n 42.4917\n ],\n [\n -110.475,\n 42.4917\n ],\n [\n -110.475,\n 42.4833\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae46f","contributors":{"authors":[{"text":"Perkins, Robert B.","contributorId":106954,"corporation":false,"usgs":true,"family":"Perkins","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":243767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntyre, Brandie","contributorId":37796,"corporation":false,"usgs":true,"family":"McIntyre","given":"Brandie","affiliations":[],"preferred":false,"id":243766,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hein, James R. 0000-0002-5321-899X jhein@usgs.gov","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":2828,"corporation":false,"usgs":true,"family":"Hein","given":"James","email":"jhein@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":243765,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Piper, David Z. dzpiper@usgs.gov","contributorId":2452,"corporation":false,"usgs":true,"family":"Piper","given":"David","email":"dzpiper@usgs.gov","middleInitial":"Z.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":243764,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":50866,"text":"ofr0315 - 2003 - A Rapid Array Mobilization Procedure (RAMP) agreement for the central United States","interactions":[],"lastModifiedDate":"2012-02-02T00:11:29","indexId":"ofr0315","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2003-15","title":"A Rapid Array Mobilization Procedure (RAMP) agreement for the central United States","language":"ENGLISH","doi":"10.3133/ofr0315","usgsCitation":"Bodin, P., Pavlis, G., Schweig, E., and Gomberg, J., 2003, A Rapid Array Mobilization Procedure (RAMP) agreement for the central United States (Version 1.0): U.S. Geological Survey Open-File Report 2003-15, 21 p., https://doi.org/10.3133/ofr0315.","productDescription":"21 p.","costCenters":[],"links":[{"id":178311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4635,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-015","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4965e4b0b290850ef1f9","contributors":{"authors":[{"text":"Bodin, Paul","contributorId":104142,"corporation":false,"usgs":true,"family":"Bodin","given":"Paul","affiliations":[],"preferred":false,"id":242499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pavlis, Gary","contributorId":101319,"corporation":false,"usgs":true,"family":"Pavlis","given":"Gary","email":"","affiliations":[],"preferred":false,"id":242498,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schweig, Eugene","contributorId":21942,"corporation":false,"usgs":true,"family":"Schweig","given":"Eugene","affiliations":[],"preferred":false,"id":242496,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gomberg, Joan","contributorId":77919,"corporation":false,"usgs":true,"family":"Gomberg","given":"Joan","affiliations":[],"preferred":false,"id":242497,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":51503,"text":"ofr0325 - 2003 - A spatial database of bedding attitudes to accompany Geologic map of the greater Denver area, Front Range Urban Corridor, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:11:30","indexId":"ofr0325","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2003-25","title":"A spatial database of bedding attitudes to accompany Geologic map of the greater Denver area, Front Range Urban Corridor, Colorado","docAbstract":"This digital map shows bedding attitude symbols display over the geographic extent of surficial deposits and rock stratigraphic units (formations) as compiled by Trimble and Machette 1973-1977 and published in 1979 (U.S. Geological Survey Map I-856-H) under the Front Range Urban Corridor Geology Program. Trimble and Machette compiled their geologic map from published geologic maps and unpublished geologic mapping having varied map unit schemes. A convenient feature of the compiled map is its uniform classification of geologic units that mostly matches those of companion maps to the north (USGS I-855-G) and to the south (USGS I-857-F). Published as a color paper map, the Trimble and Machette map was intended for land-use planning in the Front Range Urban Corridor. This map recently (1997-1999), was digitized under the USGS Front Range Infrastructure Resources Project (see cross-reference).\r\n In general, the mountainous areas in the west part of the map exhibit various igneous and metamorphic bedrock units of Precambrian age, major faults, and fault brecciation zones at the east margin (5-20 km wide) of the Front Range. The eastern and central parts of the map (Colorado Piedmont) depict a mantle of unconsolidated deposits of Quaternary age and interspersed outcroppings of Cretaceous or Tertiary-Cretaceous sedimentary bedrock. The Quaternary mantle is comprised of eolian deposits (quartz sand and silt), alluvium (gravel, sand, and silt of variable composition), colluvium, and few landslides. At the mountain front, north-trending, dipping Paleozoic and Mesozoic sandstone, shale, and limestone bedrock formations form hogbacks and intervening valleys.","language":"ENGLISH","doi":"10.3133/ofr0325","usgsCitation":"Trimble, D.E., Machette, M., Brandt, T.R., Moore, D., and Murray, K., 2003, A spatial database of bedding attitudes to accompany Geologic map of the greater Denver area, Front Range Urban Corridor, Colorado (Version 1.0): U.S. Geological Survey Open-File Report 2003-25, map, 27 by 34 inches and accompanying text (9 p.), https://doi.org/10.3133/ofr0325.","productDescription":"map, 27 by 34 inches and accompanying text (9 p.)","costCenters":[],"links":[{"id":179311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4499,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-025/","linkFileType":{"id":5,"text":"html"}},{"id":110384,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54457.htm","linkFileType":{"id":5,"text":"html"},"description":"54457"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a63a3","contributors":{"authors":[{"text":"Trimble, Donald E.","contributorId":75910,"corporation":false,"usgs":true,"family":"Trimble","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":243756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Machette, Michael N.","contributorId":28963,"corporation":false,"usgs":true,"family":"Machette","given":"Michael N.","affiliations":[],"preferred":false,"id":243753,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brandt, Theodore R. 0000-0002-7862-9082 tbrandt@usgs.gov","orcid":"https://orcid.org/0000-0002-7862-9082","contributorId":1267,"corporation":false,"usgs":true,"family":"Brandt","given":"Theodore","email":"tbrandt@usgs.gov","middleInitial":"R.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":243752,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moore, David W.","contributorId":63835,"corporation":false,"usgs":true,"family":"Moore","given":"David W.","affiliations":[],"preferred":false,"id":243755,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murray, Kyle E.","contributorId":31825,"corporation":false,"usgs":true,"family":"Murray","given":"Kyle E.","affiliations":[],"preferred":false,"id":243754,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":51497,"text":"ofr0332 - 2003 - Water-quality, bed-sediment, and biological data, for streams in the upper Prickly Pear Creek watershed, Montana, 2001","interactions":[],"lastModifiedDate":"2016-12-05T10:49:24","indexId":"ofr0332","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2003-32","title":"Water-quality, bed-sediment, and biological data, for streams in the upper Prickly Pear Creek watershed, Montana, 2001","docAbstract":"

The upper Prickly Pear Creek watershed encompasses the upstream 15 miles of Prickly Pear Creek, south of Helena, Montana (fig. 1). The headwaters of Prickly Pear Creek and its tributaries (Beavertown Creek, Clancy Creek, Dutchman Creek, Golconda Creek, Lump Gulch, Spring Creek, and Warm Springs Creek) are primarily in the Helena National Forest, whereas the central part of the watershed primarily is within either Bureau of Land Management (BLM) or privately owned property. Three mining districts are present in the upper Prickly Pear Creek watershed: Alhambra, Clancy, and Colorado. Numerous prospects, adits, tailings piles, mills, dredge piles, and mines (mostly inactive) are located throughout the watershed. These districts contain polymetallic (Ag, Au, Cu, Pb, Zn) vein deposits and precious-metal (Au-Ag) vein and disseminated deposits that were exploited beginning in the 1860’s. Placer Au deposits in the major streams were extensively mined in the late 1800’s and early 1900’s.

As part of a cooperative effort with Federal land management agencies, the U.S. Geological Survey (USGS) is currently using an integrated approach to investigate two mining impacted watersheds in the western United States (the Animas River in Colorado and the Boulder River in Montana). These studies provide the USDA Forest Service and BLM scientific data for implementing informed land-management decisions regarding cleanup of abandoned mine lands within each watershed. A similar integrated-science approach will be used to characterize the upper Prickly Pear Creek watershed with respect to water and streambed sediment chemistry, aquatic biota, and geologic framework. This integrated database presents data that will be used to identify important pathways of metals movement and biological impacts, thereby guiding resource management decisions of land-managers in several publications that are in preparation. Watershed-level characterization in terms of water quality, streambed sediment chemistry, and fish health will facilitate determinations of whether removal of contaminated materials or other cleanup activities are necessary, planning of short- and long-term restoration efforts, and development of a monitoring plan to document cleanup effectiveness.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr0332","usgsCitation":"Klein, T.L., Thamke, J., Harper, D., Farag, A.M., Nimick, D.A., and Fey, D.L., 2003, Water-quality, bed-sediment, and biological data, for streams in the upper Prickly Pear Creek watershed, Montana, 2001: U.S. Geological Survey Open-File Report 2003-32, 103 p., https://doi.org/10.3133/ofr0332.","productDescription":"103 p.","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":179236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4495,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-032/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana","otherGeospatial":"Upper Prickly Pear Creek Watershed","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.148193359375,\n 45.21687321093267\n ],\n [\n -113.148193359375,\n 46.494610770689384\n ],\n [\n -110.731201171875,\n 46.494610770689384\n ],\n [\n -110.731201171875,\n 45.21687321093267\n ],\n [\n -113.148193359375,\n 45.21687321093267\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69928a","contributors":{"authors":[{"text":"Klein, Terry L. tklein@usgs.gov","contributorId":1244,"corporation":false,"usgs":true,"family":"Klein","given":"Terry","email":"tklein@usgs.gov","middleInitial":"L.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":243742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thamke, Joanna N. 0000-0002-6917-1946 jothamke@usgs.gov","orcid":"https://orcid.org/0000-0002-6917-1946","contributorId":1012,"corporation":false,"usgs":true,"family":"Thamke","given":"Joanna N.","email":"jothamke@usgs.gov","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":243740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harper, David D.","contributorId":102946,"corporation":false,"usgs":true,"family":"Harper","given":"David D.","affiliations":[],"preferred":false,"id":243743,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Farag, Aida M. 0000-0003-4247-6763 aida_farag@usgs.gov","orcid":"https://orcid.org/0000-0003-4247-6763","contributorId":1139,"corporation":false,"usgs":true,"family":"Farag","given":"Aida","email":"aida_farag@usgs.gov","middleInitial":"M.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":false,"id":243741,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nimick, David A. dnimick@usgs.gov","contributorId":421,"corporation":false,"usgs":true,"family":"Nimick","given":"David","email":"dnimick@usgs.gov","middleInitial":"A.","affiliations":[{"id":573,"text":"Special Applications Science Center","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":243738,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fey, David L. dfey@usgs.gov","contributorId":713,"corporation":false,"usgs":true,"family":"Fey","given":"David","email":"dfey@usgs.gov","middleInitial":"L.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":243739,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":50502,"text":"ofr02284 - 2003 - Hydrogeology of the Waverly-Sayre area in Tioga and Chemung Counties, New York and Bradford county, Pennsylvania","interactions":[],"lastModifiedDate":"2023-09-01T21:59:51.309676","indexId":"ofr02284","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2002-284","title":"Hydrogeology of the Waverly-Sayre area in Tioga and Chemung Counties, New York and Bradford county, Pennsylvania","docAbstract":"

The hydrogeology of a 135-square-mile area centered at Waverly, N.Y. and Sayre, Pa. is summarized in a set of five maps and a sheet of geologic sections, all at 1:24,000 scale, that depict locations of wells and test holes (sheet 1), surficial geology (sheet 2), altitude of the water table (sheet 3), saturated thickness of the surficial aquifer (sheet 4), thickness of the lacustrine confining unit (sheet 5), and geologic sections (sheet 6). The valley-fill deposits that form the aquifer system in the Waverly-Sayre area occupy an area of approximately 30 square miles, within the valleys of the Susquehanna River, Chemung River, and Cayuta Creek.

The saturated thickness of the surficial aquifer, which consists of alluvium, valley-train outwash, and underlying ice-contact deposits, ranges from zero to 90 feet and is greatest in areas where (1) the outwash is underlain by ice-contact sand and gravel or (2) the outwash is overlain by alluvium and alluvial fans. Estimated transmissivity of the surficial aquifer ranges from 5,600 to 100,270 feet squared per day, and estimated hydraulic conductivity ranges from 50 feet per day for ice-contact deposits to 1,300 feet per day for well-sorted, valley-train outwash.

The surficial aquifer is underlain by deposits of lacustrine sand, silt, and clay in the main valleys; these deposits reach thicknesses of as much as 150 ft and form a thick confining unit. Beneath the lacustrine silt and clay confining unit is a thin, discontinuous sand and gravel aquifer whose thickness averages 5 feet but may be as much as 30 feet locally. This confined aquifer supplies many domestic well in the area; yields average about 22 gallons per minute for 6-inch-diameter, open-ended wells. Average annual recharge to the aquifer system is estimated to be approximately 52.5 Mgal/d (million gallons per day), of which 29.7 Mgal/d is from direct precipitation, 7.6 Mgal/d is from unchanneled upland runoff that infiltrates the stratified drift along the valley wall, and 15.2 Mgal/d is from infiltration from tributary streams on the valley floor.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02284","collaboration":"Prepared in cooperation with New York State Department of Environmental Conservation","usgsCitation":"Reynolds, R.J., 2003, Hydrogeology of the Waverly-Sayre area in Tioga and Chemung Counties, New York and Bradford county, Pennsylvania: U.S. Geological Survey Open-File Report 2002-284, 6 Plates: 38.00 x 32.00 inches, https://doi.org/10.3133/ofr02284.","productDescription":"6 Plates: 38.00 x 32.00 inches","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":110381,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54232.htm","linkFileType":{"id":5,"text":"html"},"description":"54232"},{"id":323091,"rank":6,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2002/0284/sheets/ofr20020284_sheet5.pdf","text":"Sheet 5: Thickness of lacustrine confining unit","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2002-0284"},{"id":323097,"rank":5,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2002/0284/sheets/ofr20020284_sheet4.pdf","text":"Sheet 4: Saturated thickness of the surficial aquifer","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2002-0284"},{"id":323096,"rank":4,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2002/0284/sheets/ofr20020284_sheet3.pdf","text":"Sheet 3: Altitude of the water table","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2002-0284"},{"id":323089,"rank":3,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2002/0284/sheets/ofr20020284_sheet2.pdf","text":"Sheet 2: Surficial geology","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2002-0284"},{"id":323088,"rank":2,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2002/0284/sheets/ofr20020284_sheet1.pdf","text":"Sheet 1: Location of wells and test holes","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2002-0284"},{"id":323893,"rank":9,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2002/0284/readme.txt","linkFileType":{"id":2,"text":"txt"},"description":"OFR 2002-0284"},{"id":176181,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0284/coverthb.jpg"},{"id":323093,"rank":7,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2002/0284/sheets/ofr20020284_sheet6.pdf","text":"Sheet 6: Geological sections","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2002-0284"}],"country":"United States","state":"New York, Pennsylvania","county":"Tioga County, Chemung County, Bradford 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Director, New York Water Science Center
U.S. Geological Survey
425 Jordan Rd
Troy, NY 12180
(518) 285-5695 
http://ny.water.usgs.gov/

","tableOfContents":"","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db69137a","contributors":{"authors":[{"text":"Reynolds, Richard J. 0000-0001-5032-6613 rjreynol@usgs.gov","orcid":"https://orcid.org/0000-0001-5032-6613","contributorId":1082,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rjreynol@usgs.gov","middleInitial":"J.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241625,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51500,"text":"ofr0329 - 2003 - Design and construction of a gamma-ray spectrometer system for determining natural radioelement concentrations in geological samples at the U.S. Geological Survey in Reston, Virginia","interactions":[],"lastModifiedDate":"2018-11-26T08:46:57","indexId":"ofr0329","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2003-29","title":"Design and construction of a gamma-ray spectrometer system for determining natural radioelement concentrations in geological samples at the U.S. Geological Survey in Reston, Virginia","language":"ENGLISH","doi":"10.3133/ofr0329","usgsCitation":"Snyder, S.L., and Duval, J.S., 2003, Design and construction of a gamma-ray spectrometer system for determining natural radioelement concentrations in geological samples at the U.S. Geological Survey in Reston, Virginia: U.S. Geological Survey Open-File Report 2003-29, Online Only, https://doi.org/10.3133/ofr0329.","productDescription":"Online Only","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":179239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4497,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-029/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667ed4","contributors":{"authors":[{"text":"Snyder, Stephen L. ssnyder@usgs.gov","contributorId":4753,"corporation":false,"usgs":true,"family":"Snyder","given":"Stephen","email":"ssnyder@usgs.gov","middleInitial":"L.","affiliations":[{"id":5068,"text":"Midwest Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":243746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duval, Joseph S.","contributorId":22314,"corporation":false,"usgs":true,"family":"Duval","given":"Joseph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":243747,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":50867,"text":"ofr0317 - 2003 - Preliminary soil-slip susceptibility maps, southwestern California","interactions":[],"lastModifiedDate":"2023-06-23T15:17:41.159722","indexId":"ofr0317","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2003-17","title":"Preliminary soil-slip susceptibility maps, southwestern California","docAbstract":"

This group of maps shows relative susceptibility of hill slopes to the initiation sites of rainfall-triggered soil slip-debris flows in southwestern California. As such, the maps offer a partial answer to one part of the three parts necessary to predict the soil-slip/debris-flow process. A complete prediction of the process would include assessments of “where”, “when”, and “how big”. These maps empirically show part of the “where” of prediction (i.e., relative susceptibility to sites of initiation of the soil slips) but do not attempt to show the extent of run out of the resultant debris flows. Some information pertinent to “when” the process might begin is developed. “When” is determined mostly by dynamic factors such as rainfall rate and duration, for which local variations are not amenable to long-term prediction. “When” information is not provided on the maps but is described later in this narrative. The prediction of “how big” is addressed indirectly by restricting the maps to a single type of landslide process—soil slip-debris flows.

\n
\n

The susceptibility maps were created through an iterative process from two kinds of information. First, locations of sites of past soil slips were obtained from inventory maps of past events. Aerial photographs, taken during six rainy seasons that produced abundant soil slips, were used as the basis for soil slip-debris flow inventory. Second, digital elevation models (DEM) of the areas that were inventoried were used to analyze the spatial characteristics of soil slip locations. These data were supplemented by observations made on the ground. Certain physical attributes of the locations of the soil-slip debris flows were found to be important and others were not. The most important attribute was the mapped bedrock formation at the site of initiation of the soil slip. However, because the soil slips occur in surficial materials overlying the bedrocks units, the bedrock formation can only serve as a surrogate for the susceptibility of the overlying surficial materials.

\n
\n

The maps of susceptibility were created from those physical attributes learned to be important from the inventories. The multiple inventories allow a model to be created from one set of inventory data and evaluated with others. The resultant maps of relative susceptibility represent the best estimate generated from available inventory and DEM data.

\n
\n

Slope and aspect values used in the susceptibility analysis were 10-meter DEM cells at a scale of 1:24,000. For most of the area 10-meter DEMs were available; for those quadrangles that have only 30-meter DEMs, the 30-meter DEMS were resampled to 10-meters to maintain resolution of 10-meter cells. Geologic unit values used in the susceptibility analysis were five-meter cells. For convenience, the soil slip susceptibility values are assembled on 1:100,000-scale bases. Any area of the 1:100,000-scale maps can be transferred to 1:24,000-scale base without any loss of accuracy. Figure 32 is an example of part of a 1:100,000-scale susceptibility map transferred back to a 1:24,000-scale quadrangle.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/ofr0317","collaboration":"Prepared in cooperation with the California Geological Survey","usgsCitation":"Morton, D.M., Alvarez, R.M., Campbell, R., Bovard, K.R., Brown, D.T., Corriea, K.M., and Lesser, J.N., 2003, Preliminary soil-slip susceptibility maps, southwestern California: U.S. Geological Survey Open-File Report 2003-17, Report: 14 p.; 7 Plates: 41.0 x 36.0 inches or smaller; Readme; Metadata, https://doi.org/10.3133/ofr0317.","productDescription":"Report: 14 p.; 7 Plates: 41.0 x 36.0 inches or smaller; Readme; Metadata","numberOfPages":"46","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":178312,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr0317.jpg"},{"id":4636,"rank":12,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0017/","linkFileType":{"id":5,"text":"html"}},{"id":110376,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54144.htm","linkFileType":{"id":5,"text":"html"},"description":"54144"},{"id":285239,"rank":11,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2003/0017/README.doc"},{"id":285250,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0017/pdf/plate7.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"}},{"id":285249,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0017/pdf/plate6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"}},{"id":285248,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0017/pdf/plate5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"}},{"id":285247,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0017/pdf/plate4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":285246,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0017/pdf/plate3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":285245,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0017/pdf/plate2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":285244,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0017/pdf/plate1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":285240,"rank":3,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2003/0017/sus_met.txt"},{"id":285238,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0017/pdf/of03-17.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","projection":"Universal Transverse Mercator projection","country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.0,32.5 ], [ -121.0,35.5 ], [ -115.0,35.5 ], [ -115.0,32.5 ], [ -121.0,32.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c0ae","contributors":{"authors":[{"text":"Morton, Douglas M. scamp@usgs.gov","contributorId":4102,"corporation":false,"usgs":true,"family":"Morton","given":"Douglas","email":"scamp@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":242500,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alvarez, Rachel M.","contributorId":74451,"corporation":false,"usgs":true,"family":"Alvarez","given":"Rachel","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":242503,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Campbell, Russell H.","contributorId":91074,"corporation":false,"usgs":true,"family":"Campbell","given":"Russell H.","affiliations":[],"preferred":false,"id":242505,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bovard, Kelly R.","contributorId":49009,"corporation":false,"usgs":true,"family":"Bovard","given":"Kelly","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":242502,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Brown, D. T.","contributorId":34196,"corporation":false,"usgs":true,"family":"Brown","given":"D.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":242501,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Corriea, K. M.","contributorId":81981,"corporation":false,"usgs":true,"family":"Corriea","given":"K.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":242504,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lesser, J. N.","contributorId":102563,"corporation":false,"usgs":true,"family":"Lesser","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":242506,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":51504,"text":"ofr0324 - 2003 - A spatial database of bedding attitudes to accompany Geologic Map of Boulder-Fort Collins-Greeley area, Colorado","interactions":[],"lastModifiedDate":"2022-08-17T18:46:39.404796","indexId":"ofr0324","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2003-24","title":"A spatial database of bedding attitudes to accompany Geologic Map of Boulder-Fort Collins-Greeley area, Colorado","docAbstract":"This digital map shows bedding attitude data displayed over the geographic extent of rock stratigraphic units (formations) as compiled by Colton in 1976 (U.S.Geological Survey Map I-855-G) under the Front Range Urban Corridor Geology Program. Colton used his own mapping and published geologic maps having varied map unit schemes to compile one map with a uniform classification of geologic units. The resulting published color paper map was intended for planning for use of land in the Front Range Urban Corridor. In 1997-1999, under the USGS Front Range Infrastructure Resources Project, Colton's map was digitized to provide data at 1:100,000 scale to address urban growth issues(see cross-reference). In general, the west part of the map shows a variety of Precambrian igneous and metamorphic rocks, major faults and brecciated zones along an eastern strip (5-20 km wide) of the Front Range. The eastern and central part of the map (Colorado Piedmont) depicts a mantle of Quaternary unconsolidated deposits and interspersed Cretaceous or Tertiary-Cretaceous sedimentary rock outcrops. The Quaternary mantle is comprised of eolian deposits (quartz sand and silt), alluvium (gravel, sand, and silt of variable composition), colluvium, and few landslides. At the mountain front, north-trending, dipping Paleozoic and Mesozoic sandstone and shale formations (and sparse limestone) form hogbacks, intervening valleys, and in range-front folds, anticlines, and fault blocks. Localized dikes and sills of Tertiary rhyodacite and basalt intrude rocks near the range front, mostly in the Boulder area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0324","usgsCitation":"Colton, R.B., Brandt, T.R., Moore, D., and Murray, K., 2003, A spatial database of bedding attitudes to accompany Geologic Map of Boulder-Fort Collins-Greeley area, Colorado (Version 1.0): U.S. Geological Survey Open-File Report 2003-24, HTML Document, https://doi.org/10.3133/ofr0324.","productDescription":"HTML Document","costCenters":[],"links":[{"id":179312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110385,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54458.htm","linkFileType":{"id":5,"text":"html"},"description":"54458"},{"id":4500,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-024/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","city":"Boulder, Fort Collins, Greeley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.4302978515625,\n 39.98132938627215\n ],\n [\n -104.61181640625,\n 39.98132938627215\n ],\n [\n -104.61181640625,\n 40.58475654701271\n ],\n [\n -105.4302978515625,\n 40.58475654701271\n ],\n [\n -105.4302978515625,\n 39.98132938627215\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6391","contributors":{"authors":[{"text":"Colton, Roger B.","contributorId":17967,"corporation":false,"usgs":true,"family":"Colton","given":"Roger","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":243758,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brandt, Theodore R. 0000-0002-7862-9082 tbrandt@usgs.gov","orcid":"https://orcid.org/0000-0002-7862-9082","contributorId":1267,"corporation":false,"usgs":true,"family":"Brandt","given":"Theodore","email":"tbrandt@usgs.gov","middleInitial":"R.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":243757,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, David W.","contributorId":63835,"corporation":false,"usgs":true,"family":"Moore","given":"David W.","affiliations":[],"preferred":false,"id":243760,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Murray, Kyle E.","contributorId":31825,"corporation":false,"usgs":true,"family":"Murray","given":"Kyle E.","affiliations":[],"preferred":false,"id":243759,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":50580,"text":"ofr2002483 - 2003 - Map and digital database of sedimentary basins and indications of petroleum in the Central Alaska Province","interactions":[{"subject":{"id":50580,"text":"ofr2002483 - 2003 - Map and digital database of sedimentary basins and indications of petroleum in the Central Alaska Province","indexId":"ofr2002483","publicationYear":"2003","noYear":false,"title":"Map and digital database of sedimentary basins and indications of petroleum in the Central Alaska Province"},"predicate":"SUPERSEDED_BY","object":{"id":69768,"text":"mf2428 - 2003 - Maps showing sedimentary basins, surface thermal maturity, and indications of petroleum in the Central Alaska Province","indexId":"mf2428","publicationYear":"2003","noYear":false,"title":"Maps showing sedimentary basins, surface thermal maturity, and indications of petroleum in the Central Alaska Province"},"id":1}],"supersededBy":{"id":69768,"text":"mf2428 - 2003 - Maps showing sedimentary basins, surface thermal maturity, and indications of petroleum in the Central Alaska Province","indexId":"mf2428","publicationYear":"2003","noYear":false,"title":"Maps showing sedimentary basins, surface thermal maturity, and indications of petroleum in the Central Alaska Province"},"lastModifiedDate":"2012-02-10T00:10:10","indexId":"ofr2002483","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2002-483","title":"Map and digital database of sedimentary basins and indications of petroleum in the Central Alaska Province","docAbstract":"This database and accompanying text depict historical and modern reported \r\n\r\n occurrences of petroleum both in wells and at the surface within the \r\n\r\n boundaries of the Central Alaska Province. These data were compiled from \r\n\r\n previously published and unpublished sources and were prepared for use in \r\n\r\n the 2002 U.S. Geological Survey petroleum assessment of Central Alaska, \r\n\r\n Yukon Flats region. Indications of petroleum are described as oil or gas \r\n\r\n shows in wells, oil or gas seeps, or outcrops of oil shale or oil-bearing \r\n\r\n rock and include confirmed and unconfirmed reports. The scale of the \r\n\r\n source map limits the spatial resolution (scale) of the database to \r\n\r\n 1:2,500,000 or smaller. \r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr2002483","usgsCitation":"Troutman, S.M., and Stanley, R.G., 2003, Map and digital database of sedimentary basins and indications of petroleum in the Central Alaska Province: U.S. Geological Survey Open-File Report 2002-483, 1 map, 66 by 36 inches, https://doi.org/10.3133/ofr2002483.","productDescription":"1 map, 66 by 36 inches","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":110382,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54257.htm","linkFileType":{"id":5,"text":"html"},"description":"54257"},{"id":176227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8869,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-483/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -168.2405,58.5998 ], [ -168.2405,68.1017 ], [ -138.8511,68.1017 ], [ -138.8511,58.5998 ], [ -168.2405,58.5998 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db6548c7","contributors":{"authors":[{"text":"Troutman, Sandra M.","contributorId":46601,"corporation":false,"usgs":true,"family":"Troutman","given":"Sandra","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":241889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanley, Richard G. 0000-0001-6192-8783 rstanley@usgs.gov","orcid":"https://orcid.org/0000-0001-6192-8783","contributorId":1832,"corporation":false,"usgs":true,"family":"Stanley","given":"Richard","email":"rstanley@usgs.gov","middleInitial":"G.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":241888,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":50513,"text":"ofr02335 - 2003 - Economic drivers of mineral supply","interactions":[],"lastModifiedDate":"2012-02-02T00:11:16","indexId":"ofr02335","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2003","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":"2002-335","title":"Economic drivers of mineral supply","docAbstract":"The debate over the adequacy of future supplies of mineral resources continues in light of the\r\ngrowing use of mineral-based materials in the United States. According to the U.S. Geological\r\nSurvey, the quantity of new materials utilized each year has dramatically increased from 161\r\nmillion tons2 in 1900 to 3.2 billion tons in 2000. Of all the materials used during the 20th\r\ncentury in the United States, more than half were used in the last 25 years.\r\nWith the Earth?s endowment of natural resources remaining constant, and increased demand for\r\nresources, economic theory states that as depletion approaches, prices rise. This study shows\r\nthat many economic drivers (conditions that create an economic incentive for producers to act in\r\na particular way) such as the impact of globalization, technological improvements, productivity\r\nincreases, and efficient materials usage are at work simultaneously to impact minerals markets and supply. As a result of these economic drivers, the historical price trend of mineral prices3 in\r\nconstant dollars has declined as demand has risen. When price is measured by the cost in human\r\neffort, the price trend also has been almost steadily downward.\r\nAlthough the United States economy continues its increasing mineral consumption trend, the\r\nsupply of minerals has been able to keep pace. This study shows that in general supply has\r\ngrown faster than demand, causing a declining trend in mineral prices.","language":"ENGLISH","doi":"10.3133/ofr02335","usgsCitation":"Wagner, L.A., Sullivan, D.E., and Sznopek, J.L., 2003, Economic drivers of mineral supply (Version 1.0): U.S. Geological Survey Open-File Report 2002-335, p. 274, illus., 65 refs, https://doi.org/10.3133/ofr02335.","productDescription":"p. 274, illus., 65 refs","costCenters":[],"links":[{"id":176254,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4326,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-335/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625b0e","contributors":{"authors":[{"text":"Wagner, Lorie A.","contributorId":95457,"corporation":false,"usgs":true,"family":"Wagner","given":"Lorie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":241651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sullivan, Daniel E.","contributorId":62198,"corporation":false,"usgs":true,"family":"Sullivan","given":"Daniel","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":241650,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sznopek, John L.","contributorId":23936,"corporation":false,"usgs":true,"family":"Sznopek","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":241649,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":53655,"text":"ofr2003444 - 2003 - Wilderness experience in Rocky Mountain National Park 2002; report to respondents","interactions":[],"lastModifiedDate":"2025-06-06T13:06:03.759245","indexId":"ofr2003444","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","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":"2003-444","title":"Wilderness experience in Rocky Mountain National Park 2002; report to respondents","docAbstract":"

A substantial amount of backcountry (about 250,000 acres) in Rocky Mountain National Park [RMNP of the Park] may be designated as wilderness areas in the coming years. Currently, over 3 million visitors drives through the park on Trail Ridge Road, camp in designated campgrounds, day hike, etc. each year. Many of those visitors also report using the backcountry-wilderness areas that are not easily accessible by roads or trails. Use of the backcountry is growing at RMNP and is accompanied by changing visitor expectations and preferences for wilderness management. For these reasons it is of great importance for the Park to periodically assess what types of environments and conditions wilderness users seek to facilitate a quality experience.

To assist in this effort, the Political Analysis and Science Assistance [PSAS] program / Fort Collins Center / U.S. Geological Survey, in close collaboration with personnel and volunteers from RMNP, as well as the Natural Resource Recreation and Tourism [NRRT] Department at Colorado State University, launched a research effort in the summer of 2002 to investigate visitors wilderness experiences in the Park.

Specifically, the purpose of this research was: (1) To determine what constitutes a wilderness experience; (2) To identify important places, visual features, and sounds essential to a quality wilderness experience and; (3) To determine what aspects may detract from wilderness experience. Thus, answers to these questions should provide insight for Park managers about visitors expectation for wilderness recreation and the conditions they seek for quality wilderness experiences. Ultimately, this information can be used to support wilderness management decisions within RMNP.

The social science technique of Visitor Employed Photography [VEP] was used to obtain information from visitors about wilderness experiences. Visitors were selected at random from Park-designated wilderness trails, in proportion to their use, and asked to participate in the survey. Respondents were given single use, 10-exposure cameras and photo-log diaries to record experiences. A total of 293 cameras were distributed, with a response rate of 87%. Following the development of the photos, a copy of the photos, two pertinent pages from the photo-log, and a follow-up survey were mailed to respondents. Fifty-six percent of the follow-up surveys were returned. Findings from the two surveys were analyzed and compared.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2003444","usgsCitation":"Schuster, E., Johnson, S.S., and Taylor, J.G., 2003, Wilderness experience in Rocky Mountain National Park 2002; report to respondents: U.S. Geological Survey Open-File Report 2003-444, 32 p., https://doi.org/10.3133/ofr2003444.","productDescription":"32 p.","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":490188,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0444/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175093,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2003/0444/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Rocky Mountain National Park","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49cae4b07f02db5d7b41","contributors":{"authors":[{"text":"Schuster, Elke","contributorId":63462,"corporation":false,"usgs":true,"family":"Schuster","given":"Elke","email":"","affiliations":[],"preferred":false,"id":248024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, S. Shea","contributorId":93122,"corporation":false,"usgs":true,"family":"Johnson","given":"S.","email":"","middleInitial":"Shea","affiliations":[],"preferred":false,"id":248025,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, Jonathan G.","contributorId":37378,"corporation":false,"usgs":true,"family":"Taylor","given":"Jonathan","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":248023,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":53199,"text":"ofr2003288 - 2003 - The Role of stocking in the reestablishment and augmentation of native fish in the Lower Colorado River mainstream (1998-2002)","interactions":[],"lastModifiedDate":"2016-05-23T15:18:51","indexId":"ofr2003288","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","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":"2003-288","title":"The Role of stocking in the reestablishment and augmentation of native fish in the Lower Colorado River mainstream (1998-2002)","docAbstract":"

The Colorado River has experienced dramatic physical and biological change. Rated as the fifth largest river in the USA by volume, today its waters seldom reach the sea. Water diversions gradually reduce its flow to a point where its last remaining waters are diverted at Morales Dam leaving nearly 100 km of historic channel dry. In contrast, lower basin storage reservoirs cover 36% of the historic channel. Remaining portions of the flowing river have been channelized and straightened to a point where it now resembles a large canal. Levees, mechanical dredging, and the natural forces of erosion have degraded the river channel nearly 2 m in some locations, isolating it from its floodplain and affecting local water tables. The river no longer functions as a natural stream system characteristic of spring run-off, summer spates, and droughts. Today it serves as a water storage and conveyance system to meet human needs.

\n

Physical change has been severe, but not as devastating as the biological pollution. More than 80 nonnative fish species have been introduced to the lower basin. Today, over 20 fish species have established, many forming economically important sport fisheries. As these alien species expanded their range, native communities rapidly declined and disappeared from much of their historic range. By 1930, most had become rare. The last remnant populations of bonytail, razorback sucker, and Colorado pikeminnow in the lower basin were taken downstream of Davis Dam during the 1960’s and 1970’s. Today, Colorado pikeminnow, and it appears, wild bonytail are extirpated downstream of Glen Canyon Dam, and wild razorback suckers are extremely rare. The Colorado River and its fish assemblage is a totally different ecosystem than it was a century ago.

\n

State and federal agencies have been attempting to reestablish native communities for nearly three decades. More than 12 million razorback suckers, most of them small, were stocked between 1981 and 1991. Few of these fish survived and during the past decade managers have switched to stocking larger suckers to improve survival. Since 1995, nearly 18,000 bonytail and 30,000 large razorback suckers have been stocked in Lake Havasu. There was also a single stocking (611) of flannelmouth suckers in 1976. These programs have produced mixed results. The single introduction of flannelmouth sucker has resulted in a thriving community, estimated at more than 4,000 fish. This success spirited hopes by many that other natives would respond similarly but unfortunately, that has not occurred.

\n

Initial stocking returns suggest that stocking survival of bonytail and razorback sucker is relatively poor (<12%) and the absence of any detectable recruitment indicates present reintroduction efforts are falling short of anticipated survival or potential recovery. In contrast, the single introduction of wild flannelmouth sucker, out-performed millions of hatchery produced razorback sucker. This suggests hatchery reared fish may be inferior to wild fish in terms of survival skills, which has been found to be the case for terrestrial animal introductions. A review of culturing, stocking, and repatriation techniques is warranted which examines ways to better prepare fish to convert to natural foods, recognize predators, and be physically conditioned to cope with currents and hopefully avoid or escape predators.

\n

Comparison of flannelmouth sucker success and the razorback sucker’s failure provides compelling evidence that helps explain the dramatic physical habitat changes that have occurred and the possible role of habitat selection and predator communities. It mimics conditions observed in portions of the upper basin where flannelmouth suckers are still common but razorback suckers have been extirpated. Both sucker species are successfully spawning in the lower basin, however, recruitment can only be detected for flannelmouth. Habitat preference and associated predation pressure of those habitats appear to be the primary factors responsible for recruitment. Flannelmouth suckers prefer channel habitat that supports a fraction of the predators found in off-channel habitats where razorback suckers reside. The dependence of razorback sucker young on slack water habitat puts the species at a much higher predation risk.

\n

Through a process of trial and error during the past two decades, managers are now stocking large natives to increase their survival. Small native fish simply have not survived. While this improves short-term stocking survival, it ignores or at least delays dealing with the predation issue. Current stocking programs have reestablished or augmented relatively small populations of bonytail, razorback, and flannelmouth suckers between Davis and Parker Dams. All three species are better off than they were a decade ago in this section of the river. Unfortunately, bonytail and razorback sucker will only maintain a presence in the Colorado River main stem through continued stocking and it remains to be seen if management agencies will make that long-term commitment.

\n

While the gains for the bonytail and razorback sucker have been difficult, the successful reintroduction of flannelmouth sucker highlights the ecological changes that have taken place and suggests this, and possibly other channel oriented species (i.e., Gila robusta) could be established. In contrast, there is no evidence to suggest we can expect similar recruitment or expansions for bonytail and razorback sucker. Their dependence on slack water habitat leaves their young vulnerable to overwhelming predation.

\n

Recovery in the main stem will only be accomplished with a dramatic decrease and possibly a total removal of nonnative species. After ten years and over $6 million in expenditures to remove nonnative fish it appears this philosophy is neither technically nor politically viable. In the meantime, stocking is the only alternative available to insure these species don’t disappear. The only viable option appears the creation and maintenance of small, isolated refuge communities where these species have shown they can produce young.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr2003288","collaboration":"Prepared in cooperation with the Bureau of Reclamation, Arizona State University, U.S. Fish and Wildlife Service, and California Fish and Game Department","usgsCitation":"Mueller, G., 2003, The Role of stocking in the reestablishment and augmentation of native fish in the Lower Colorado River mainstream (1998-2002): U.S. Geological Survey Open-File Report 2003-288, vi, 43 p., https://doi.org/10.3133/ofr2003288.","productDescription":"vi, 43 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":177921,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr2003288.PNG"},{"id":320295,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0288/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona, California, Nevada","otherGeospatial":"Colorado River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.60937499999999,\n 35.263561862152095\n ],\n [\n -114.60662841796875,\n 35.14237113713991\n ],\n [\n -114.6697998046875,\n 35.10193405724606\n ],\n [\n -114.63409423828125,\n 35.068221159859256\n ],\n [\n -114.6533203125,\n 35.03224538129597\n ],\n [\n -114.6697998046875,\n 34.872411827691025\n ],\n [\n -114.49676513671875,\n 34.687427949314845\n ],\n [\n -114.41436767578124,\n 34.522398580663314\n ],\n [\n -114.43634033203125,\n 34.447688696497444\n ],\n [\n -114.17816162109375,\n 34.29579932143427\n ],\n [\n -114.3402099609375,\n 34.15499986715356\n ],\n [\n -114.3017578125,\n 34.125447565116126\n ],\n [\n -114.1094970703125,\n 34.261756524459805\n ],\n [\n -114.0765380859375,\n 34.30714385628804\n ],\n [\n -114.32373046875,\n 34.4793919710481\n ],\n [\n -114.35943603515625,\n 34.54049998801135\n ],\n [\n -114.40887451171875,\n 34.617387052407175\n ],\n [\n -114.45281982421875,\n 34.732584206123626\n ],\n [\n -114.49676513671875,\n 34.856636719051735\n ],\n [\n -114.60113525390625,\n 34.89043681762452\n ],\n [\n -114.58740234375,\n 35.05698043137265\n ],\n [\n -114.55169677734375,\n 35.11766197360177\n ],\n [\n -114.54620361328125,\n 35.22767235493586\n ],\n [\n -114.56268310546874,\n 35.26580442886754\n ],\n [\n -114.60937499999999,\n 35.263561862152095\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ac4d","contributors":{"authors":[{"text":"Mueller, Gordon","contributorId":7729,"corporation":false,"usgs":true,"family":"Mueller","given":"Gordon","affiliations":[],"preferred":false,"id":246889,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53273,"text":"ofr2003222 - 2003 - Reconnaissance-level application of physical habitat simulation in the evaluation of physical habitat limits in the Animas Basin, Colorado","interactions":[],"lastModifiedDate":"2016-05-23T11:17:50","indexId":"ofr2003222","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","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":"2003-222","title":"Reconnaissance-level application of physical habitat simulation in the evaluation of physical habitat limits in the Animas Basin, Colorado","docAbstract":"

The Animas River is in southwestern Colorado and flows mostly to the south to join the San Juan River at Farmington, New Mexico (Figure 1). The Upper Animas River watershed is in San Juan County, Colorado and is located in the San Juan Mountains. The lower river is in the Colorado Plateau country. The winters are cold with considerable snowfall and little snowmelt in the mountains in the upper part of the basin. The lower basin has less snow but the winters are still cold. The streamflows during the winter are low and reasonably stable.

\n

The native trout in the Animas Basin is the cutthroat trout. Few native trout remain and the trout found in the upper watershed are brook trout with rainbow and brown trout in the lower river. There is considerable metal contamination in the upper basin near Silverton but a brook trout fishery does exist in the Animas River from just above Howardsville to where the Animas joins Cement Creek in Silverton.

\n

There are two principle objectives of the habitat studies in the Animas Basin: (1) to improve understanding of the fate of sediment from mining operations from the view point of physical habitat impacts, and (2) to determine if reconnaissance level physical habitat studies can be useful in understanding the impacts of mining on the aquatic ecosystem.

\n

Part of the project was to apply the Physical Habitat Simulation System (PHABSIM) to selected locations in the Upper Animas River Basin, Colorado in order to demonstrate the importance of physical habitat in evaluating the efficacy of mined land remediation activities. Physical habitat analysis included the use of sedimentation variables in physical habitat simulations. A map of the Upper Animas Basin is presented in Figure 2.

\n

The project involves collecting data for the following locations: Animas River above Magee Creek; Animas River above Howardsville; Animas River below Howardsville; Animas River above Silverton at Hillsdale Cemetery; Animas River at Silverton; Cement Creek above Silverton; Cement Creek at Silverton; Mineral Creek at Powerline above Silverton; Mineral Creek at Campground; South Mineral Creek at Overflow Campground; Mineral Creek above Bear Creek; Mineral Creek at Silverton; Animas River below Silverton; and Animas River at Elk Park.

\n

Bed material samples were collected at each site. These included samples of the armour, the substrate, and sand and fines deposited on the surface. At selected sites the stream morphology was measured. These measurements included one to three cross sections, stream discharge, and water surface elevations. The data are located in the files of the Fort Collins Science Center.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr2003222","usgsCitation":"Milhous, R.T., 2003, Reconnaissance-level application of physical habitat simulation in the evaluation of physical habitat limits in the Animas Basin, Colorado: U.S. Geological Survey Open-File Report 2003-222, v, 16 p., https://doi.org/10.3133/ofr2003222.","productDescription":"v, 16 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":177987,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr2003222.PNG"},{"id":320296,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0222/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, New Mexico","otherGeospatial":"Animas River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.21807861328125,\n 36.697053200100335\n ],\n [\n -107.940673828125,\n 36.82247761166621\n ],\n [\n -107.74566650390625,\n 37.2587521486561\n ],\n [\n -107.53692626953125,\n 37.861844098370945\n ],\n [\n -107.611083984375,\n 37.93553306183642\n ],\n [\n -107.82257080078125,\n 37.85750715625203\n ],\n [\n -107.99835205078124,\n 37.54022177661216\n ],\n [\n -108.03131103515625,\n 37.24782120155428\n ],\n [\n -108.0670166015625,\n 37.00035919622158\n ],\n [\n -108.21807861328125,\n 36.697053200100335\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623b5f","contributors":{"authors":[{"text":"Milhous, Robert T.","contributorId":28646,"corporation":false,"usgs":true,"family":"Milhous","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":247141,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53727,"text":"ofr2003476 - 2003 - Effects of channel modification on fish habitat in the upper Yellowstone River: Final report to the USACE, Omaha","interactions":[],"lastModifiedDate":"2016-05-23T11:31:18","indexId":"ofr2003476","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","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":"2003-476","title":"Effects of channel modification on fish habitat in the upper Yellowstone River: Final report to the USACE, Omaha","docAbstract":"

A two-dimensional hydrodynamic simulation model was coupled with a geographic information system (GIS) to produce a variety of habitat classification maps for three study reaches in the upper Yellowstone River basin in Montana. Data from these maps were used to examine potential effects of channel modification on shallow, slow current velocity (SSCV) habitats that are important refugia and nursery areas for young salmonids. At low flows, channel modifications were found to contribute additional SSCV habitat, but this contribution was negligible at higher discharges. During runoff, when young salmonids are most vulnerable to downstream displacement, the largest areas of SSCV habitat occurred in side channels, point bars, and overbank areas. Because of the diversity of elevations in the existing Yellowstone River, SSCV habitat tends to be available over a wide range of discharges. Based on simulations in modified and unmodified sub-reaches, channel simplification results in decreased availability of SSCV habitat, particularly during runoff. The combined results of the fish population and fish habitat studies present strong evidence that during runoff, SSCV habitat is most abundant in side channel and overbank areas and that juvenile salmonids use these habitats as refugia. Channel modifications that result in reduced availability of side channel and overbank habitats, particularly during runoff, will probably cause local reductions in juvenile abundances during the runoff period. Effects of reduced juvenile abundances during runoff on adult numbers later in the year will depend on (1) the extent of channel modification, (2) patterns of fish displacement and movement, (3) longitudinal connectivity between reaches that contain refugia and those that do not, and (4) the relative importance of other limiting factors.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr2003476","usgsCitation":"Bowen, Z.H., Bovee, K.D., and Waddle, T.J., 2003, Effects of channel modification on fish habitat in the upper Yellowstone River: Final report to the USACE, Omaha: U.S. Geological Survey Open-File Report 2003-476, 80 p., https://doi.org/10.3133/ofr2003476.","productDescription":"80 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":179438,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr2003476.PNG"},{"id":320297,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0476/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","county":"Park County","otherGeospatial":"Yellowstone River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.74905395507812,\n 45.32704768567264\n ],\n [\n -110.61721801757812,\n 45.41966030640988\n ],\n [\n -110.54855346679686,\n 45.596743928454124\n ],\n [\n -110.49636840820312,\n 45.69850658738848\n ],\n [\n -110.52932739257812,\n 45.71097418682748\n ],\n [\n -110.59112548828125,\n 45.64092778836502\n ],\n [\n -110.60623168945312,\n 45.55444852652113\n ],\n [\n -110.64468383789062,\n 45.487094732298374\n ],\n [\n -110.65704345703124,\n 45.433153642271414\n ],\n [\n -110.69549560546874,\n 45.42737117898911\n ],\n [\n -110.77239990234375,\n 45.346354488594436\n ],\n [\n -110.74905395507812,\n 45.32704768567264\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db61629c","contributors":{"authors":[{"text":"Bowen, Zachary H. 0000-0002-8656-1831 bowenz@usgs.gov","orcid":"https://orcid.org/0000-0002-8656-1831","contributorId":821,"corporation":false,"usgs":true,"family":"Bowen","given":"Zachary","email":"bowenz@usgs.gov","middleInitial":"H.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":248241,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bovee, Ken D.","contributorId":100447,"corporation":false,"usgs":true,"family":"Bovee","given":"Ken","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":248243,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waddle, Terry J.","contributorId":43430,"corporation":false,"usgs":true,"family":"Waddle","given":"Terry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":248242,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":51954,"text":"ofr0354 - 2003 - U.S. Geological Survey Greater Everglades Science Program: 2002 Biennial Report","interactions":[],"lastModifiedDate":"2024-02-06T13:59:38.599699","indexId":"ofr0354","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","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":"03-54","title":"U.S. Geological Survey Greater Everglades Science Program: 2002 Biennial Report","docAbstract":"

Introduction

The U.S. Geological Survey (USGS) conducts scientific investigations in south Florida to improve society’s understanding of the environment and assist in the sustainable use, protection, and restoration of the Everglades and other ecosystems within the region. The investigations summarized in this document have been carried out under the Greater Everglades Science Program (previously known as the South Florida Ecosystem Program), which is part of the USGS Place-Based Studies initiative.

The USGS Placed-Based Studies initiative is a nationwide program that concentrates on areas with severe environmental problems. Through interdisciplinary investigations the Program provides sound scientific information on which to base informed resource management decisions. Individuals from all the USGS programs (hydrology, geology, biology, mapping) work together with other scientists to cover the diverse scientific disciplines involved in this complex and challenging task. The Greater Everglades Science Program began in 1995 as one of the initial Place-Based Studies programs and serves as a model for similar future collaborative studies. Placed-Based Studies are also being conducted in the San Francisco Bay area, Chesapeake Bay, the Platte River, Greater Yellowstone, Salton Sea, and the Mojave Desert.

The South Florida Ecosystem Program is part of a coordinated federal effort, under the South Florida Ecosystem Restoration Task Force. The Task Force was started in 1993, through interagency agreement, to coordinate the efforts of the agencies within six federal departments. In 1996, statutory authority formalized the Task Force and expanded it to include tribal, state, and local governments. The Task Force conducts its activities through the South Florida Ecosystem Working Group and teams, such as the Science Coordination Team. A Science Plan and Integrated Financial Plans are established to focus efforts and prevent duplicative efforts by the agencies.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0354","usgsCitation":"Torres, A.E., Higer, A.L., Henkel, H., Mixson, P.R., Eggleston, J., Embry, T.L., and Clement, G., 2003, U.S. Geological Survey Greater Everglades Science Program: 2002 Biennial Report: U.S. Geological Survey Open-File Report 03-54, 291 p., https://doi.org/10.3133/ofr0354.","productDescription":"291 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":4503,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0054/ofr03-54.pdf","text":"Report","size":"78.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 03-54"},{"id":179089,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2003/0054/coverthb.jpg"}],"contact":"

Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314

Contact Pubs Warehouse

","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613a90","contributors":{"authors":[{"text":"Torres, Arturo E. aetorres@usgs.gov","contributorId":1397,"corporation":false,"usgs":true,"family":"Torres","given":"Arturo","email":"aetorres@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":244527,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Higer, Aaron L.","contributorId":52163,"corporation":false,"usgs":true,"family":"Higer","given":"Aaron","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":244530,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Henkel, Heather S. hhenkel@usgs.gov","contributorId":2869,"corporation":false,"usgs":true,"family":"Henkel","given":"Heather S.","email":"hhenkel@usgs.gov","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":244528,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mixson, Patsy R.","contributorId":79550,"corporation":false,"usgs":true,"family":"Mixson","given":"Patsy","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":244532,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Eggleston, Jane R.","contributorId":48956,"corporation":false,"usgs":true,"family":"Eggleston","given":"Jane R.","affiliations":[],"preferred":false,"id":244529,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Embry, Teresa L.","contributorId":61503,"corporation":false,"usgs":true,"family":"Embry","given":"Teresa","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":244531,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Clement, Gail","contributorId":84000,"corporation":false,"usgs":true,"family":"Clement","given":"Gail","email":"","affiliations":[],"preferred":false,"id":244533,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":53682,"text":"ofr03123 - 2003 - User's manual for the National Water Information System of the U.S. Geological Survey: Automated Data Processing System (ADAPS)","interactions":[{"subject":{"id":31447,"text":"ofr97635 - 1997 - User's manual for the National Water Information System of the U.S. Geological Survey; Chapter 3, Automated data processing system","indexId":"ofr97635","publicationYear":"1997","noYear":false,"title":"User's manual for the National Water Information System of the U.S. Geological Survey; Chapter 3, Automated data processing system"},"predicate":"SUPERSEDED_BY","object":{"id":53682,"text":"ofr03123 - 2003 - User's manual for the National Water Information System of the U.S. Geological Survey: Automated Data Processing System (ADAPS)","indexId":"ofr03123","publicationYear":"2003","noYear":false,"title":"User's manual for the National Water Information System of the U.S. Geological Survey: Automated Data Processing System (ADAPS)"},"id":1}],"lastModifiedDate":"2012-02-02T00:11:25","indexId":"ofr03123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-123","title":"User's manual for the National Water Information System of the U.S. Geological Survey: Automated Data Processing System (ADAPS)","docAbstract":"The Automated Data Processing System (ADAPS) was developed for the processing, storage, and retrieval of water data, and is part of the National Water Information System (NWIS) developed by the U.S. Geological Survey. NWIS is a distributed water database in which data can be processed over a network of computers at U.S. Geological Survey offices throughout the United States. NWIS comprises four subsystems: ADAPS, the Ground-Water Site Inventory System (GWSI), the Water-Quality System (QWDATA), and the Site-Specific Water-Use Data System (SWUDS).\r\n\r\nThis section of the NWIS User's Manual describes the automated data processing of continuously recorded water data, which primarily are surface-water data; however, the system also allows for the processing of water-quality and ground-water data.\r\n\r\nThis manual describes various components and features of the ADAPS, and provides an overview of the data processing system and a description of the system framework. The components and features included are: (1) data collection and processing, (2) ADAPS menus and programs, (3) command line functions, (4) steps for processing station records, (5) postprocessor programs control files, (6) the standard format for transferring and entering unit and daily values, and (7) relational database (RDB) formats.","language":"ENGLISH","doi":"10.3133/ofr03123","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2003, User's manual for the National Water Information System of the U.S. Geological Survey: Automated Data Processing System (ADAPS) (Version 4.3; Supercedes OFR 97-635): U.S. Geological Survey Open-File Report 2003-123, 413 p., https://doi.org/10.3133/ofr03123.","productDescription":"413 p.","costCenters":[],"links":[{"id":5001,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03123/","linkFileType":{"id":5,"text":"html"}},{"id":178756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 4.3; Supercedes OFR 97-635","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49afe4b07f02db5c8791","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":532198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":54020,"text":"ofr03454 - 2003 - Water temperature, streamflow, and ground-water elevation in and adjacent to the Russian river between Hopland and Guerneville, California from 1998-2002","interactions":[],"lastModifiedDate":"2020-02-11T07:19:47","indexId":"ofr03454","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-454","title":"Water temperature, streamflow, and ground-water elevation in and adjacent to the Russian river between Hopland and Guerneville, California from 1998-2002","docAbstract":"Temperature, water level elevation, stage height, and river discharge data for this report were collected in and adjacent to the Russian River from Hopland to Guerneville, CA over a four-year period from 1998 to 2002 to establish baselines for long-term water quality, water supply and habitat. Data files presented in this report were collected by the USGS and the Sonoma County Water Agency's Engineering Resource and Planning, and Natural Resource Divisions. Temperature data were collected in single-channel submersible microloggers or temperature data were collected simultaneously with water-elevation data in dual-channel down-hole data loggers. Stream stage and streamflow data were collected at USGS stream gaging stations located near Hopland, Healdsburg, and Guerneville over a 130 km reach of the Russian River. During the period of record stream flow ranged from 3 to 1458 m3/s. Stream temperature ranged from 8 to 29 oC while groundwater temperature ranged from 10 to 38 oC. Stream stage varied 5 m seasonly, while ground-water level varied 19 m over the same time scale.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr03454","usgsCitation":"Cox, M.H., and Hatch, C., 2003, Water temperature, streamflow, and ground-water elevation in and adjacent to the Russian river between Hopland and Guerneville, California from 1998-2002: U.S. Geological Survey Open-File Report 2003-454, 39 p., https://doi.org/10.3133/ofr03454.","productDescription":"39 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":182038,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5460,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03-454/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","county":"Mendocino County, Sonoma County","city":"Hopland, 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