No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2483","isbn":"0607888539","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1997, Revised shaded relief map and controlled color photomosaic of the Arabia Quadrangle (MC-12) of Mars: U.S. Geological Survey IMAP 2483, 2 Plates: 26.65 x 24.76 inches and 25.78 x 19.12 inches, https://doi.org/10.3133/i2483.","productDescription":"2 Plates: 26.65 x 24.76 inches and 25.78 x 19.12 inches","costCenters":[],"links":[{"id":115070,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2483/plate-2.pdf","size":"3790","linkFileType":{"id":1,"text":"pdf"}},{"id":190483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2483/report-thumb.jpg"},{"id":115069,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2483/plate-1.pdf","size":"6065","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602e56","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":534141,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29352,"text":"wri974190 - 1997 - August median streamflows in Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri974190","displayToPublicDate":"1998-07-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"97-4190","title":"August median streamflows in Massachusetts","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nU.S. Geological Survey, Branch of Information Services [distributor],","doi":"10.3133/wri974190","usgsCitation":"Ries, K., 1997, August median streamflows in Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 97-4190, iv, 27 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri974190.","productDescription":"iv, 27 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4190/report-thumb.jpg"},{"id":58204,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4190/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668104","contributors":{"authors":[{"text":"Ries, Kernell G. III kries@usgs.gov","contributorId":1913,"corporation":false,"usgs":true,"family":"Ries","given":"Kernell G.","suffix":"III","email":"kries@usgs.gov","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":false,"id":201394,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30189,"text":"wri974187 - 1997 - Glacier ice-volume modeling and glacier volumes on Redoubt Volcano, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri974187","displayToPublicDate":"1998-07-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"97-4187","title":"Glacier ice-volume modeling and glacier volumes on Redoubt Volcano, Alaska","docAbstract":"Assessment of ice volumes and hydrologic hazards on Redoubt Volcano began four months before the 1989-90 eruptions removed 0.29 cubic kilometer of perennial snow and ice from Drift glacier. A volume model was developed for evaluating glacier volumes on Redoubt Volcano. The volume model is based on third-order polynomial simulations of valley cross sections. The third-order polynomial is an interpolation from the valley walls exposed above glacier surfaces and takes advantage of ice-thickness measurements. The fortuitous 1989-90 eruptions removed the ice from a 4.5-kilometer length of Drift glacier, providing a unique opportunity for verification of the volume model. A 2.5-kilometer length was chosen in the denuded glacier valley and the ice volume was measured by digitally comparing two new maps: one derived from the most recent pre-eruption 1979 aerial photographs and the other from post-eruption 1990 aerial photographs. The measured volume in the reference reach was 99 x 106 cubic meters, about 1 percent less than was estimated by the volume model. The volume estimate produced by this volume model was much closer to the measured volume than was the volume estimated by other techniques. The verified volume model was used to evaluate the total volume of perennial snow and glacier ice on Redoubt Volcano, which was estimated to be 4.1?0.8 cubic kilometers. Substantial snow and ice covers on volcanoes exacerbate the hydrologic hazards associated with eruptions. The volume on Redoubt Volcano is about 23 times the volume that was present on Mount St. Helens before its 1980 eruption, which generated lahars and floods.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri974187","usgsCitation":"Trabant, D.C., and Hawkins, D.B., 1997, Glacier ice-volume modeling and glacier volumes on Redoubt Volcano, Alaska: U.S. Geological Survey Water-Resources Investigations Report 97-4187, iv, 29 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri974187.","productDescription":"iv, 29 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124875,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4187/report-thumb.jpg"},{"id":58985,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679bcb","contributors":{"authors":[{"text":"Trabant, Dennis C.","contributorId":13965,"corporation":false,"usgs":true,"family":"Trabant","given":"Dennis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":202831,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hawkins, Daniel B.","contributorId":10842,"corporation":false,"usgs":true,"family":"Hawkins","given":"Daniel","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":202830,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24787,"text":"ofr97599 - 1997 - Estimated water use, by county, in North Carolina, 1995","interactions":[],"lastModifiedDate":"2017-01-05T11:26:19","indexId":"ofr97599","displayToPublicDate":"1998-07-01T00:00:00","publicationYear":"1997","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":"97-599","title":"Estimated water use, by county, in North Carolina, 1995","docAbstract":"Data on water use in North Carolina were compiled for 1995 as part of a cooperative agreement between the U.S. Geological Survey and the Division of Water Resources of the North Carolina Department of Environment and Natural Resources. Data were compiled from a number of Federal, State, and private sources for the offstream water-use categories of public supply, domestic, commercial, industrial, mining, livestock, irrigation, and thermoelectric-power generation. Data also were collected for instream use from hydroelectric facilities. Total withdrawals (fresh and saline) during 1995 were an estimated 9,286 million gallons per day for the offstream water-use categories. About 94 percent of the water withdrawn was from surface water. Thermoelectric-power generation accounted for 80 percent of all withdrawals. Instream water use for hydroelectric-power generation totaled about 56,400 million gallons per day. Each water-use category is summarized in this report by county and source of water supply.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/ofr97599","issn":"0094-9140","usgsCitation":"Walters, D.A., 1997, Estimated water use, by county, in North Carolina, 1995: U.S. Geological Survey Open-File Report 97-599, iv, 102 p. :col. ill., col. maps ;28 cm., https://doi.org/10.3133/ofr97599.","productDescription":"iv, 102 p. :col. ill., col. maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":53805,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0599/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0599/report-thumb.jpg"}],"country":"United States","state":"North 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Sediment was sampled at 31 sites for trace elements and 23 sites for synthetic organic compounds; biota were collected at a subset of sites. Some of the variability in trace elements and synthetic organic compounds was related to land use, and many differences in trace element concentration by land use category were statistically significant. The spatial distribution of some trace elements was related to a combination of land use and surficial deposits and (or) bedrock type. Urban land use was likely the dominant factor influencing high sediment concentrations of Cd, Cu, Hg, and Pb. Forested land use was related to high concentrations of As in sediment and biota and high Se in sediment; however, bedrock type was an additional factor for As and surficial deposits type was a factor for Se. Land use, surficial deposits, and bedrock type appeared to influence Ni and Zn concentrations, and Cr concentrations did not directly reflect any of these factors. Most occurrences of organochlorine compounds in sediment and biota were related to urban land use. DDT and related compounds were detected at sites spanning all land uses. PCBs were detected in sediment at large-river sites and at one urban site in the Milwaukee area; the highest concentrations of PCBs in fish were found at two of four large river sites. A larger number of SVOCs were detected at urban sites and large river sites compared to agricultural and forested sites.
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Director, Pennsylvania Water Science Center
U.S. Geological Survey
215 Limekiln Road
New Cumberland, PA 17070
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97703","usgsCitation":"Ratcliffe, N.M., 1997, Preliminary bedrock geologic map of the Chittenden quadrangle, Rutland County, Vermont: U.S. Geological Survey Open-File Report 97-703, Report; 36 p.; 3 Plates: 19.19 × 28.92 inches or smaller, https://doi.org/10.3133/ofr97703.","productDescription":"Report; 36 p.; 3 Plates: 19.19 × 28.92 inches or smaller","costCenters":[],"links":[{"id":161048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0703/report-thumb.jpg"},{"id":60188,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0703/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60187,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0703/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60186,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0703/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60189,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0703/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397798,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18830.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Vermont","county":"Rutland County","otherGeospatial":"Chittenden quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.875,\n 43.625\n ],\n [\n -73,\n 43.625\n ],\n [\n -73,\n 43.75\n ],\n [\n -72.875,\n 43.75\n ],\n [\n -72.875,\n 43.625\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c646","contributors":{"authors":[{"text":"Ratcliffe, N. M.","contributorId":80691,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"N.","middleInitial":"M.","affiliations":[],"preferred":false,"id":207488,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70019706,"text":"70019706 - 1997 - Deep structure of Medicine Lake volcano, California","interactions":[],"lastModifiedDate":"2025-08-14T16:30:52.918813","indexId":"70019706","displayToPublicDate":"1998-06-25T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Deep structure of Medicine Lake volcano, California","docAbstract":"Medicine Lake volcano (MLV) in northeastern California is the largest-volume volcano in the Cascade Range. The upper-crustal structure of this Quaternary shield volcano is well known from previous geological and geophysical investigations. In 1981, the U.S. Geological Survey conducted a teleseismic tomography experiment on MLV to explore its deeper structure. The images we present, calculated using a modern form of the ACH-inversion method, reveal that there is presently no hint of a large (> 100 km3), hot magma reservoir in the crust. The compressional-wave velocity perturbations show that directly beneath MLV's caldera there is a zone of increased seismic velocity. The perturbation amplitude is +10% in the upper crust, +5% in the lower crust, and +3% in the lithospheric mantle. This positive seismic velocity anomaly presumably is caused by mostly subsolidus gabbroic intrusive rocks in the crust. Heat and melt removal are suggested as the cause in the upper mantle beneath MLV, inferred from petro-physical modeling. The increased seismic velocity appears to be nearly continuous to 120 km depth and is a hint that the original melts come at least partly from the lower lithospheric mantle. Our second major finding is that the upper mantle southeast of MLV is characterized by relatively slow seismic velocities (−1%) compared to the northwest side. This anomaly is interpreted to result from the elevated temperatures under the northwest Basin and Range Province.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0040-1951(97)00022-X","issn":"00401951","usgsCitation":"Ritter, J., and Evans, J., 1997, Deep structure of Medicine Lake volcano, California: Tectonophysics, v. 275, no. 1-3, p. 221-241, https://doi.org/10.1016/S0040-1951(97)00022-X.","productDescription":"21 p.","startPage":"221","endPage":"241","costCenters":[],"links":[{"id":228171,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Medicine Lake volcano","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -121.6253989653446,\n 41.59366233777956\n ],\n [\n -121.6253989653446,\n 41.57255366496153\n ],\n [\n -121.57877644244559,\n 41.57255366496153\n ],\n [\n -121.57877644244559,\n 41.59366233777956\n ],\n [\n -121.6253989653446,\n 41.59366233777956\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"275","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe2ae4b0c8380cd4eb6d","contributors":{"authors":[{"text":"Ritter, J.R.R.","contributorId":96848,"corporation":false,"usgs":true,"family":"Ritter","given":"J.R.R.","email":"","affiliations":[],"preferred":false,"id":383668,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, J.R.","contributorId":50526,"corporation":false,"usgs":true,"family":"Evans","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":383667,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70019705,"text":"70019705 - 1997 - Analysis of borehole televiewer measurements in the Vorotilov drillhole, Russia - First results","interactions":[],"lastModifiedDate":"2025-08-14T16:37:58.927983","indexId":"70019705","displayToPublicDate":"1998-06-25T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Analysis of borehole televiewer measurements in the Vorotilov drillhole, Russia - First results","docAbstract":"In the Eurasian part of the World Stress Map almost the whole region east of the Tornquist-Teisseyre line is terra incognita. The closure of this information gap is of fundamental importance to the understanding of the geodynamics of the Eurasian continent. A detailed analysis of stress-induced wellbore breakouts has been performed over a 4.1-km-long depth interval in the Vorotilov drillhole (VGS). The borehole is located in the central part of the Russian platform, right in the center of the Vorotilov meteorite impact crater 60 km to the NNE of the city of Nizni Novgorod. An ultrasonic borehole televiewer (BHTV) was used to obtain high-resolution acoustical images from the borehole wall. With an interactive system for analyzing BHTV data the azimuth and shape of borehole breakouts occurring in the depth range of 1.3–4.8 km were analyzed. A statistical analysis of the resulting orientation profile of the breakout azimuths yields an overall direction of the maximum horizontal principal stress SH of N 137°E ± 15°. Variations of breakout orientation with depth ranging from a few degrees up to more than 90° are seen on various depth scales.
The observed stress direction of N 137°E agrees very well with the average SH orientation of N 145°E in Central Europe. If this measurement is taken as representative for the Russian platform, the stress field in Russia is only slightly rotated in comparison to Central Europe. This can possibly be interpreted as indicative for the stress field to be governed by broad scale tectonic forces, such as a strong contribution from the forces exerted by the collision zone in the Alpine-Himalayan belt and by the Mid-Atlantic ridge.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0040-1951(97)00031-0","issn":"00401951","usgsCitation":"Huber, K., Fuchs, K., Palmer, J., Roth, F., Khakhaev, B., Van-Kin, L.E., Pevzner, L., Hickman, S., Moos, D., Zoback, M.D., and Schmitt, D., 1997, Analysis of borehole televiewer measurements in the Vorotilov drillhole, Russia - First results: Tectonophysics, v. 275, no. 1-3, p. 261-272, https://doi.org/10.1016/S0040-1951(97)00031-0.","productDescription":"12 p.","startPage":"261","endPage":"272","costCenters":[],"links":[{"id":228132,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia","otherGeospatial":"Vorotilov drillhole","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 43.85361151516585,\n 56.377878378335424\n ],\n [\n 43.85361151516585,\n 56.24665273409747\n ],\n [\n 44.20560894507008,\n 56.24665273409747\n ],\n [\n 44.20560894507008,\n 56.377878378335424\n ],\n [\n 43.85361151516585,\n 56.377878378335424\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"275","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eb0ae4b0c8380cd48b92","contributors":{"authors":[{"text":"Huber, K.","contributorId":18230,"corporation":false,"usgs":true,"family":"Huber","given":"K.","email":"","affiliations":[],"preferred":false,"id":383658,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fuchs, K.","contributorId":89666,"corporation":false,"usgs":true,"family":"Fuchs","given":"K.","email":"","affiliations":[],"preferred":false,"id":383664,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Palmer, J.","contributorId":25040,"corporation":false,"usgs":true,"family":"Palmer","given":"J.","affiliations":[],"preferred":false,"id":383660,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roth, F.","contributorId":92929,"corporation":false,"usgs":true,"family":"Roth","given":"F.","email":"","affiliations":[],"preferred":false,"id":383665,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Khakhaev, B.N.","contributorId":17101,"corporation":false,"usgs":true,"family":"Khakhaev","given":"B.N.","email":"","affiliations":[],"preferred":false,"id":383657,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Van-Kin, L. E.","contributorId":52043,"corporation":false,"usgs":true,"family":"Van-Kin","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":383661,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Pevzner, L.A.","contributorId":6327,"corporation":false,"usgs":true,"family":"Pevzner","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":383656,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hickman, S.","contributorId":79995,"corporation":false,"usgs":true,"family":"Hickman","given":"S.","email":"","affiliations":[],"preferred":false,"id":383662,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Moos, Daniel","contributorId":105048,"corporation":false,"usgs":true,"family":"Moos","given":"Daniel","affiliations":[],"preferred":false,"id":383666,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Zoback, Mark D.","contributorId":80275,"corporation":false,"usgs":true,"family":"Zoback","given":"Mark","middleInitial":"D.","affiliations":[],"preferred":false,"id":383663,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Schmitt, D.","contributorId":19395,"corporation":false,"usgs":true,"family":"Schmitt","given":"D.","email":"","affiliations":[],"preferred":false,"id":383659,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}} ,{"id":70020093,"text":"70020093 - 1997 - Reinterpretation of the peninsular Florida Oligocene: An integrated stratigraphic approach","interactions":[],"lastModifiedDate":"2025-07-22T15:01:08.608335","indexId":"70020093","displayToPublicDate":"1998-06-15T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3368,"text":"Sedimentary Geology","active":true,"publicationSubtype":{"id":10}},"title":"Reinterpretation of the peninsular Florida Oligocene: An integrated stratigraphic approach","docAbstract":"A very thick (> 300 m) nearly continuous Oligocene section exists in southern peninsular Florida, as revealed by lithostratigraphic, biostratigraphic (mollusks and dinocysts), chronostratigraphic (Sr isotopes) and petrographic analyses of twelve cores and two quarries. The Oligocene deposits in the subsurface of southern Florida are the thickest documented in the southeastern U.S., and they also may represent the most complete record of Oligocene deposition in this region. No major unconformities within the Oligocene section are detected in the southern portion of the peninsula; hiatuses at the Eocene-Oligocene boundary, the early Oligocene-late Oligocene boundary, and the late Oligocene-Miocene boundary, are of limited duration if they exist at all. No significant disconformity is recognized between the Suwannee Limestone and the Arcadia Formation in southern Florida. However, on the east coast of Florida a hiatus of more than 12 m.y., spanning from at least the middle of the early Oligocene to early Miocene is present. The Suwannee Limestone was deposited during the early Oligocene. The top of the Suwannee Limestone appears to be diachronous across the platform. The 'Suwannee' Limestone, previously identified incorrectly as a late Oligocene unit, is herein documented to be early Oligocene and is encompassed in the lower Oligocene Suwannee Limestone. An unnamed limestone, found on the east coast of the peninsula is, at least in part, correlative with the Suwannee Limestone. The Arcadia Formation, basal Hawthorn Group, accounts for a large portion of the Oligocene deposition in southern Florida, spanning the interval from the middle of the early Oligocene to at least the early Miocene. Comparisons of the depositional patterns, and the distribution of dolomite and phosphate within the Suwannee Limestone and the Arcadia Formation, suggest fluctuating sea levels and that the paleo-Gulf Stream played a role in determining the nature and extent of Oligocene deposition in peninsular Florida.","language":"English","publisher":"Elsevier","doi":"10.1016/S0037-0738(96)00055-3","issn":"00370738","usgsCitation":"Wingard, G.L., Scott, T., Edwards, L.E., Weedman, S., and Simmons, K.R., 1997, Reinterpretation of the peninsular Florida Oligocene: An integrated stratigraphic approach: Sedimentary Geology, v. 108, no. 1-4, p. 207-228, https://doi.org/10.1016/S0037-0738(96)00055-3.","productDescription":"22 p.","startPage":"207","endPage":"228","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":227910,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.5390625,\n 30.939924331023445\n ],\n [\n -87.51708984375,\n 30.334953881988564\n ],\n [\n -85.8251953125,\n 29.99300228455108\n ],\n [\n -84.17724609375,\n 29.075375179558346\n ],\n [\n -83.1884765625,\n 28.34306490482549\n ],\n [\n -82.4853515625,\n 26.05678288577881\n ],\n [\n -80.57373046875,\n 24.627044746156027\n ],\n [\n -79.7607421875,\n 26.41155054662258\n ],\n [\n -80.04638671875,\n 27.89734922968426\n ],\n [\n -80.9912109375,\n 30.031055426540206\n ],\n [\n -81.40869140625,\n 30.713503990354965\n ],\n [\n -81.82617187499999,\n 30.80791068136646\n ],\n [\n -84.814453125,\n 30.789036751261136\n ],\n [\n -84.990234375,\n 31.109388560814963\n ],\n [\n -87.5390625,\n 30.939924331023445\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"108","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a60ce4b0e8fec6cdc08a","contributors":{"authors":[{"text":"Wingard, G. Lynn 0000-0002-3833-5207 lwingard@usgs.gov","orcid":"https://orcid.org/0000-0002-3833-5207","contributorId":605,"corporation":false,"usgs":true,"family":"Wingard","given":"G.","email":"lwingard@usgs.gov","middleInitial":"Lynn","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":385003,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, T.M.","contributorId":66694,"corporation":false,"usgs":true,"family":"Scott","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":385001,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edwards, Lucy E. 0000-0003-4075-3317 leedward@usgs.gov","orcid":"https://orcid.org/0000-0003-4075-3317","contributorId":2647,"corporation":false,"usgs":true,"family":"Edwards","given":"Lucy","email":"leedward@usgs.gov","middleInitial":"E.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":384999,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Weedman, S.D.","contributorId":23961,"corporation":false,"usgs":true,"family":"Weedman","given":"S.D.","affiliations":[],"preferred":false,"id":385000,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Simmons, K. R.","contributorId":68771,"corporation":false,"usgs":true,"family":"Simmons","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":385002,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70019954,"text":"70019954 - 1997 - Slope-apron deposition in an Ordovician arc-related setting: The Vuelta de Las Tolas Member (Suri Formation), Famatina Basin, northwest Argentina","interactions":[],"lastModifiedDate":"2025-07-22T15:15:15.199943","indexId":"70019954","displayToPublicDate":"1998-06-15T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3368,"text":"Sedimentary Geology","active":true,"publicationSubtype":{"id":10}},"title":"Slope-apron deposition in an Ordovician arc-related setting: The Vuelta de Las Tolas Member (Suri Formation), Famatina Basin, northwest Argentina","docAbstract":"The Ordovician Suri Formation is part of the infill of the Famatina Basin of northwest Argentina, which formed in an active setting along the western margin of early Paleozoic Gondwana. The lower part of this formation, the Vuelta de Las Tolas Member, records sedimentation on a slope apron formed in an intra-arc basin situated on a flooded continental arc platform. The coincidence of a thick Arenig-Llanvirn sedimentary succession and volcanic-plutonic arc rocks suggests an extensional or transtensional arc setting, and is consistent with evidence of an extensional regime within the volcanic arc in the northern Puna region.
The studied stratigraphic sections consist of volcanic rocks and six sedimentary facies. The facies can be clustered into four facies associations. Association 1, composed of facies A (laminated siltstones and mudstones) and B (massive mudstones and siltstones), is interpreted to have accumulated from silty-muddy high-and low-density turbidity currents and highly fluid, silty debris flows, with subsequent reworking by bottom currents, and to a lesser extent, hemipelagic suspension in an open-slope setting. Facies association 2 is dominated by facies C (current-rippled siltstones) strata. These deposits are interpreted to record overbank sedimentation from fine-grained turbidity currents. Facies E (matrix-supported volcanic breccias) interbedded with andesitic lava units comprises facies association 3. Deposition was contemporaneous with subaqueous volcanic activity, and accumulated from cohesive debris flows in a coarse-grained wedge at the base of slope. Facies association 4 is typified by facies D (vitric fine-grained sandstones and siltstones) and F (channelized and graded volcanic conglomerates and breccias) deposits. These strata commonly display thinning-and fining-upward trends, indicating sedimentation from highly-concentrated volcaniclastic turbidity currents in a channelized system. The general characteristics of these deposits of fresh pyroclastic detritus suggest that their accumulation was contemporaneous with, or post-dated shallow-water or subaereal explosive volcanism.
The Vuelta de Las Tolas Member tends to show an overall random facies patterns reflecting the strong influence of non-cyclical episodic processes related to arc volcanism and slope sedimentation. The scarcity of resident ichnofaunas and the presence of thick packages of uniform mudstones suggest deposition under oxygen-depleted conditions in a topographically confined, ponded sub-basin. Interbasinal correlations favor comparison with Middle Arenig slope-apron successions formed in the northern Puna Basin and suggest a southward prolongation of the Arenig volcanic arc.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0037-0738(96)00043-7","issn":"00370738","usgsCitation":"Mangano, M., and Buatois, L., 1997, Slope-apron deposition in an Ordovician arc-related setting: The Vuelta de Las Tolas Member (Suri Formation), Famatina Basin, northwest Argentina: Sedimentary Geology, v. 109, no. 1-2, p. 155-180, https://doi.org/10.1016/S0037-0738(96)00043-7.","productDescription":"26 p.","startPage":"155","endPage":"180","costCenters":[],"links":[{"id":228221,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Argentina","otherGeospatial":"Famatina Basin, northwest Argentina","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -67.23482147385482,\n -23.944258309430438\n ],\n [\n -68.40438488382345,\n -24.909066517371013\n ],\n [\n -68.3703898071458,\n -27.179130872784455\n ],\n [\n -67.1457598578472,\n -27.655241469128985\n ],\n [\n -66.16083769868202,\n -27.276718312457376\n ],\n [\n -66.10573738389476,\n -23.944258309430438\n ],\n [\n -67.23482147385482,\n -23.944258309430438\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"109","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b916de4b08c986b3198c8","contributors":{"authors":[{"text":"Mangano, M.G.","contributorId":7432,"corporation":false,"usgs":true,"family":"Mangano","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":384486,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buatois, L.A.","contributorId":40740,"corporation":false,"usgs":true,"family":"Buatois","given":"L.A.","affiliations":[],"preferred":false,"id":384487,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70020020,"text":"70020020 - 1997 - Correlation of Miocene sequences and hydrogeologic units, New Jersey Coastal Plain","interactions":[],"lastModifiedDate":"2025-07-22T15:07:43.001694","indexId":"70020020","displayToPublicDate":"1998-06-15T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3368,"text":"Sedimentary Geology","active":true,"publicationSubtype":{"id":10}},"title":"Correlation of Miocene sequences and hydrogeologic units, New Jersey Coastal Plain","docAbstract":"We have developed a Miocene sequence stratigraphic framework using data from recently drilled boreholes in the New Jersey Coastal Plain. Sequences are shallowing upward, unconformity-bounded units; fine-grained shelf and prodelta sediments grade upward to delta front and shallow-marine sands, corresponding to confining bed-aquifer couplets. By dating Miocene sequences using Sr-isotope stratigraphy, and mapping with borehole data and geophysical logs, we can predict the continuity and effectiveness of the confining beds and aquifers. The following are illustrated on a 90-km basinward dip section: (1) the composite confining bed is comprised of the KwO and lower Kw1a (ca. 23.8-20.5 Ma) sequences downdip at Atlantic City, and the Kw1b, Kw1a and older sequences updip (ca. 69.3-20.6 Ma), and is continuous throughout most of the coastal plain; (2) the major confined aquifer, the Atlantic City 800-foot sand, is comprised of the upper Kw1a and Kw1b sequences (ca. 20.5-20.2 Ma) and is an areally continuous sand that is interconnected with the Kirkwood-Cohansey aquifer system updip of Mays Landing; (3) the confining bed above the Atlantic City 800-foot sand is comprised of the Kw2a, Kw2b, and Kw3 sequences (18.1-13.3 Ma) and is an extensive confining bed that pinches out updip. These sequences and aquifer-confining bed couplets are linked to global sea-level changes evinced by the ??18O record. We conclude that sequence stratigraphy is a powerful tool when applied to regional hydrogeologic problems, although basinal tectonic differences and localized variations in sediment supply can affect aquifer thickness and permeability.","language":"English","publisher":"Elsevier","doi":"10.1016/S0037-0738(96)00046-2","issn":"00370738","usgsCitation":"Sugarman, P.J., and Miller, K., 1997, Correlation of Miocene sequences and hydrogeologic units, New Jersey Coastal Plain: Sedimentary Geology, v. 108, no. 1-4, p. 3-18, https://doi.org/10.1016/S0037-0738(96)00046-2.","productDescription":"16 p.","startPage":"3","endPage":"18","costCenters":[],"links":[{"id":228033,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.37244133572423,\n 40.47663791572276\n ],\n [\n -75.57270968879646,\n 39.523620061399654\n ],\n [\n -75.05109120457679,\n 38.84727608756319\n ],\n [\n -74.7877049538744,\n 38.86305997864855\n ],\n [\n -74.04324209964783,\n 39.76554809333294\n ],\n [\n -73.88624305883334,\n 40.42262654169221\n ],\n [\n -74.37244133572423,\n 40.47663791572276\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"108","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fc32e4b0c8380cd4e182","contributors":{"authors":[{"text":"Sugarman, P. J.","contributorId":81154,"corporation":false,"usgs":true,"family":"Sugarman","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":384730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, K.G.","contributorId":18094,"corporation":false,"usgs":true,"family":"Miller","given":"K.G.","email":"","affiliations":[],"preferred":false,"id":384729,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70019840,"text":"70019840 - 1997 - Southern Laurentide ice lobes were created by ice streams: Des Moines Lobe in Minnesota, USA","interactions":[],"lastModifiedDate":"2025-07-22T15:24:14.797677","indexId":"70019840","displayToPublicDate":"1998-06-15T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3368,"text":"Sedimentary Geology","active":true,"publicationSubtype":{"id":10}},"title":"Southern Laurentide ice lobes were created by ice streams: Des Moines Lobe in Minnesota, USA","docAbstract":"Regional mapping in southern Minnesota has illuminated a suite of landforms developed by the Des Moines Lobe that delimit the position of the lobe at its maximum and at lesser readvances. The ice lobe repeatedly advanced, discharged its subglacial water, and subsequently stagnated. Recent glaciological research on Antarctic ice streams has led some glacial geologists to postulate that ice streams drained parts of the marine-based areas of the Laurentide Ice Sheet. I postulate that such ice streams may develop in land-based areas of an ice sheet as well, and that the Des Moines Lobe, 200 km wide and 900 km long, was an outlet glacier of an ice stream. It appears to have been able to advance beyond the Laurentide Ice Sheet as long as adequate water pressure was maintained. However, the outer part of the lobe stagnated because subglacial water that facilitated the flow was able to drain away through tunnel valleys. Stagnation of the lobe is not equivalent to stoppage of the ice stream, because ice repeatedly advanced into and onto the stagnant margins, stacking ice and debris. Similar landforms are also seen in other lobes of the upper midwestern United States.","language":"English","publisher":"Elsevier","doi":"10.1016/S0037-0738(97)00018-3","issn":"00370738","usgsCitation":"Patterson, C.J., 1997, Southern Laurentide ice lobes were created by ice streams: Des Moines Lobe in Minnesota, USA: Sedimentary Geology, v. 111, no. 1-4, p. 249-261, https://doi.org/10.1016/S0037-0738(97)00018-3.","productDescription":"13 p.","startPage":"249","endPage":"261","costCenters":[],"links":[{"id":227731,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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F.","contributorId":87153,"corporation":false,"usgs":true,"family":"Miller","given":"K.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":190928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atkins, J.T.","contributorId":39403,"corporation":false,"usgs":true,"family":"Atkins","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":190927,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25985,"text":"wri974006 - 1997 - A comparison of drainage basin nutrient inputs with instream nutrient loads for seven rivers in Georgia and Florida, 1986-90","interactions":[],"lastModifiedDate":"2017-01-31T09:15:53","indexId":"wri974006","displayToPublicDate":"1998-06-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"97-4006","title":"A comparison of drainage basin nutrient inputs with instream nutrient loads for seven rivers in Georgia and Florida, 1986-90","docAbstract":"Instream nutrient loads of the Altamaha, Suwannee, St. Johns, Satilla, Ogeechee, Withlacoochee, and Ochlockonee River Basins were computed and compared with nutrient inputs for each basin for the period 1986-90. Nutrient constituents that were considered included nitrate, ammonia, organic nitrogen, and total phosphorus. Sources of nutrients considered for this analysis included atmospheric deposition, fertilizer, animal waste, wastewater-treatment plant discharge, and septic discharge. The mean nitrogen input ranged from 2,400 kilograms per year per square kilometer (kg/yr)km2 in the Withlacoochee River Basin to 5,470 (kg/yr)km2 in the Altamaha River Basin. The Satilla and Ochlockonee River Basins also had large amounts of nitrogen input per unit area, totaling 5,430 and 4,920 (kg/yr)km2, respectively.Fertilizer or animal waste, as sources of nitrogen, predominated in all basins. Atmospheric deposition contributed less than one-fourth of the mean total nitrogen input to all basins and was consistently the third largest input in all but the Ogeechee River Basin, where it was the second largest.The mean total phosphorus input ranged from 331 (kg/yr)km2 in the Withlacoochee River Basin to 1,380 (kg/yr)km2 in both the Altamaha and Satilla River Basins. The Ochlockonee River Basin had a phosphorus input of 1,140 (kg/yr)km2.Per unit area, the Suwannee River discharged the highest instream mean total nitrogen and phosphorus loads and also discharged higher instream nitrate loads per unit area than the other six rivers. Phosphorus loads in stream discharge were highest in the Suwannee and Ochlockonee Rivers.The ratio of nutrient outputs to inputs for the seven studied rivers ranged from 4.2 to 14.9 percent, with the St. Johns (14.9 percent) and Suwannee (12.1 percent) Rivers having significantly higher percentages than those from the other basins. The output/input percentages for mean total phosphorus ranged from 1.0 to 7.0 percent, with the St. Johns (6.2 percent) and Suwannee (7.0 percent) Rivers exporting the highest percentage of phosphorus.Although instream nutrient loads constitute only one of the various pathways nutrients may take in leaving a river basin, only a relatively small part of nutrient input to the basin leaves the basin in stream discharge for the major coastal rivers examined in this study. The actual amount of nutrient transported in a river basin depends on the ways in which nutrients are physically handled, geographically distributed, and chemically assimilated within a river basin. 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