The U.S. Geological Survey collected 98 line kilometers of single-channel seismic-reflection profiles and sidescan sonar records on the inner shelf of eastern Cape Cod, Massachusetts, during April 1979. The data were obtained during cruise NE-1-79 of the R/V NEECHO. The purposes of the survey were: (1) to study the development of barrier islands; (2) to document the frequency and rate of migration of inlets that breach barrier islands; and (3) to define the characteristics of shoreface ridges on a barrier island.
he survey uti I ized two acoustic systems. Information about the bottom was obtained by using an EDO Western model 606 sidescan-sonar system (100 kHz). Profiles of the subbottom were collected by an EG&G Uni boom transducer (400-4,000 Hz) and a Del Norte streamer. Positional control for al I track! ines was provided by a shore-based Miniranger system and by LORAN-C.
The quality of the records generally is very good. However, subbottom penetration did vary somewhat from place to place during the survey due to the nature of the bottom sediments and to the presence or absence of buried channels.
The original records may be examined at the U.S. Geological Survey, Woods Hole, MA 02543. Microfilm copies of the data are avai I able for purchase from the National Geophysical pnd Solar-Terrestrial Data Center, NOAA/EDIS/NGSDC, Code D621, 325 Broadway, Boulder, CO 80303 (303-497-6338).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr81184","usgsCitation":"Knebel, H.J., 1981, Seismic-reflection and sidescan-sonar data collected off eastern Cape Cod, Massachusetts, during April 1979: U.S. Geological Survey Open-File Report 81-184, 3 p., https://doi.org/10.3133/ofr81184.","productDescription":"3 p.","numberOfPages":"3","costCenters":[{"id":680,"text":"Woods Hole Science Center","active":false,"usgs":true}],"links":[{"id":141851,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259859,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0184/ofr1981184.pdf","text":"Report","size":"5.02 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1998-184"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.0,41.0 ], [ -71.0,42.0 ], [ -69.5,42.0 ], [ -69.5,41.0 ], [ -71.0,41.0 ] ] ] } } ] }","contact":"Coastal and Marine Geology Program
U.S. Geological Survey
384 Woods Hole Road
Woods Hole, MA 02543
This report provides a record of the flood of September 16, 1975, and associated hydrologic data. These data can be used in making rational decisions in formulating effective flood-plain regulations that would minimize flood problems in the Tallaboa Valley.
The Tallaboa Valley (fig. 1) lies on the southwestern coast of Puerto Rico about 12 km (7.5 mi) west of the city of Ponce. The climate is semiarid with a mean annual precipitation of about 1,020 mm (40 in). It is a relatively small valley which until the late fifties was dedicated mainly to the product ion of sugarcane. Since then, the economy started changing from agriculture to industry. At present the lower part of the valley is completely industrialized. The upper part of the valley is used for agriculture--mostly as pastureland. The reach from Highway 132 downstream to the new Highway 2 is mainly agricultural with a few scattered communities. The lower part of the valley that includes the area from the Highway 2 bridge to the mouth is covered with heavy industry concerned with the refinement of oil, and associated industries.
The continuous growth of industry and consequently of the urban area of Peñuelas has encouraged growth onto the
flood plain. The study area is subject to flooding by the Rio Tallaboa and the Rio Guayanes, its main tributary. The Rio Guayanes is the- cause of flooding in the urban area of Penuelas, encompassing the reach from the northern edge of town downstream to Highway 132 where it joins the Rio Tallaboa.
Data are generally referred to in SI (International System) units followed by corresponding inch-pound units in parentheses. The SI units.may be converted to inch-pound units by multiplying the units given by the factors shown.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri801283","usgsCitation":"Johnson, K.G., 1981, Floods of September 16, 1975 in the Tallaboa Valley, Puerto Rico (WRI/OFR): U.S. Geological Survey Water-Resources Investigations Report 80-1283, 5 Plates: 17.00 x 22.00 inches, https://doi.org/10.3133/wri801283.","productDescription":"5 Plates: 17.00 x 22.00 inches","costCenters":[],"links":[{"id":175251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1283/report-thumb.jpg"},{"id":360551,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360552,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360553,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360554,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360550,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1283/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"state":"Puerto Rico","otherGeospatial":"Tallaboa Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -66.7690658569336,\n 17.96567026450932\n ],\n [\n -66.67808532714842,\n 17.96567026450932\n ],\n [\n -66.67808532714842,\n 18.116160664342022\n ],\n [\n -66.7690658569336,\n 18.116160664342022\n ],\n [\n -66.7690658569336,\n 17.96567026450932\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cde4b07f02db5448fb","contributors":{"authors":[{"text":"Johnson, Karl G.","contributorId":7680,"corporation":false,"usgs":true,"family":"Johnson","given":"Karl","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":247905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53614,"text":"wri81409 - 1981 - Assessment of water quality in streams draining coal-producing areas in Ohio","interactions":[],"lastModifiedDate":"2017-02-28T13:28:41","indexId":"wri81409","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-409","title":"Assessment of water quality in streams draining coal-producing areas in Ohio","docAbstract":"Water quality in the coal-producing areas of eastern Ohio was studied in a two-phase investigation between May 1975 and August 1976. Results of phase one, a reconnaissance of water quality at 150 sites, indicated that acid mine drainage generally occurred where abandoned drift or strip mines were located, whereas areas characterized by reclaimed or active strip mines showed few instances of acid drainage. Phase two was a detailed study of four small basins: One contained abandoned drift mines; the second, abandoned strip mines; the third, reclaimed strip mines; the last, active strip mines. Results of phase two were similar to those of phase one. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri81409","usgsCitation":"Pfaff, C., Helsel, D., Johnson, D., and Angelo, C., 1981, Assessment of water quality in streams draining coal-producing areas in Ohio (WRI/OFR): U.S. Geological Survey Water-Resources Investigations Report 81-409, vi, 240 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri81409.","productDescription":"vi, 240 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":174506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":336349,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0409/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf5f","contributors":{"authors":[{"text":"Pfaff, C.L.","contributorId":47777,"corporation":false,"usgs":true,"family":"Pfaff","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":247915,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Helsel, D.R.","contributorId":57448,"corporation":false,"usgs":false,"family":"Helsel","given":"D.R.","email":"","affiliations":[{"id":7242,"text":"Wisconsin Department of Natural Resources, Madison, WI, USA","active":true,"usgs":false}],"preferred":false,"id":247916,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, D.P.","contributorId":76297,"corporation":false,"usgs":true,"family":"Johnson","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":247917,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Angelo, C.G.","contributorId":27434,"corporation":false,"usgs":true,"family":"Angelo","given":"C.G.","affiliations":[],"preferred":false,"id":247914,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":43278,"text":"ofr81895 - 1981 - Geophysical data collected on the continental margin midway between Washington State and Vancouver Island, B.C., along line 19, USGS R/V S.P. Lee cruise 3-76","interactions":[],"lastModifiedDate":"2021-09-20T20:48:42.326941","indexId":"ofr81895","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-895","title":"Geophysical data collected on the continental margin midway between Washington State and Vancouver Island, B.C., along line 19, USGS R/V S.P. Lee cruise 3-76","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81895","usgsCitation":"Snavely, P.D., 1981, Geophysical data collected on the continental margin midway between Washington State and Vancouver Island, B.C., along line 19, USGS R/V S.P. Lee cruise 3-76: U.S. Geological Survey Open-File Report 81-895, 1 Plate: 58.00 × 29.00 inches, https://doi.org/10.3133/ofr81895.","productDescription":"1 Plate: 58.00 × 29.00 inches","costCenters":[],"links":[{"id":172522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":389505,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12198.htm"},{"id":20204,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0895/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Canada, United States","state":"British Columbia, Washington","otherGeospatial":"Vancouver Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -126.75,\n 48.0\n ],\n [\n -124.9170,\n 48.0\n ],\n [\n -124.9170,\n 48.6330\n ],\n [\n -126.75,\n 48.6330\n ],\n [\n -126.75,\n 48.0\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c18a","contributors":{"authors":[{"text":"Snavely, Parke Detweiler Jr.","contributorId":48535,"corporation":false,"usgs":true,"family":"Snavely","given":"Parke","suffix":"Jr.","email":"","middleInitial":"Detweiler","affiliations":[],"preferred":false,"id":227971,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":22129,"text":"ofr8160 - 1981 - Sample mine-site permit application (hydrologic assessment)","interactions":[],"lastModifiedDate":"2017-06-27T11:17:49","indexId":"ofr8160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-60","title":"Sample mine-site permit application (hydrologic assessment)","docAbstract":"Hydrologic data are presented that may be useful in the permitapplication procedure required under current Office of Surface Mining regulations. The material is presented in a format which may serve as a guide for subsequent permit applications. Data on the quality and quantity of surface water and ground water for the mine plan, adjacent, and general areas are presented. The data are presented in three general categories: measured and estimated current conditions, estimated annual variations, and predicted effects of mining and reclamation. Current surface-water, ground-water, and biological conditions are the easiest to define. Seasonal variations in surface-water flow can be estimated with some confidence, but seasonal variations in surface-water quality, biological quality, and ground-water levels and quality are difficult to estimate with the insufficient field data available. The effects of mining and reclamation cannot be predicted through the use of the scant data collected and current predictive tools.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8160","issn":"0094-9140","usgsCitation":"Herb, W.J., Brown, D., Carswell, L., and Lietman, P., 1981, Sample mine-site permit application (hydrologic assessment): U.S. Geological Survey Open-File Report 81-60, 57 p. ill., charts, maps ;28 cm., https://doi.org/10.3133/ofr8160.","productDescription":"57 p. ill., charts, maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":154960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0060/report-thumb.jpg"},{"id":51578,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaee4b07f02db66c845","contributors":{"authors":[{"text":"Herb, William J.","contributorId":79454,"corporation":false,"usgs":true,"family":"Herb","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":187239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, D.M.","contributorId":80657,"corporation":false,"usgs":true,"family":"Brown","given":"D.M.","affiliations":[],"preferred":false,"id":187240,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carswell, L.D.","contributorId":6435,"corporation":false,"usgs":true,"family":"Carswell","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":187237,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lietman, P. L.","contributorId":63040,"corporation":false,"usgs":true,"family":"Lietman","given":"P. L.","affiliations":[],"preferred":false,"id":187238,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":24974,"text":"pp1203 - 1981 - Ground temperature measurements","interactions":[],"lastModifiedDate":"2012-02-02T00:08:27","indexId":"pp1203","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1203","title":"Ground temperature measurements","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/pp1203","usgsCitation":"Norton, D.R., Friedman, I., and Olmsted, F.H., 1981, Ground temperature measurements: U.S. Geological Survey Professional Paper 1203, 39 p., https://doi.org/10.3133/pp1203.","productDescription":"39 p.","costCenters":[],"links":[{"id":118975,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1203/report-thumb.jpg"},{"id":53960,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1203/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dc9d","contributors":{"authors":[{"text":"Norton, Daniel R.","contributorId":64265,"corporation":false,"usgs":true,"family":"Norton","given":"Daniel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":192924,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Irving","contributorId":90664,"corporation":false,"usgs":true,"family":"Friedman","given":"Irving","email":"","affiliations":[],"preferred":false,"id":192925,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Olmsted, F. H.","contributorId":24765,"corporation":false,"usgs":true,"family":"Olmsted","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":192923,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8746,"text":"ofr81880 - 1981 - Measurement and analysis of the near surface stress field in the vicinity of active faults in Southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr81880","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-880","title":"Measurement and analysis of the near surface stress field in the vicinity of active faults in Southern California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81880","usgsCitation":"Engelder, T., 1981, Measurement and analysis of the near surface stress field in the vicinity of active faults in Southern California: U.S. Geological Survey Open-File Report 81-880, 14 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr81880.","productDescription":"14 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":142684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0880/report-thumb.jpg"},{"id":36320,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0880/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610fae","contributors":{"authors":[{"text":"Engelder, T.","contributorId":99556,"corporation":false,"usgs":true,"family":"Engelder","given":"T.","affiliations":[],"preferred":false,"id":158255,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53613,"text":"wri81690 - 1981 - Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:11","indexId":"wri81690","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-690","title":"Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky","docAbstract":"This report provides water users with detailed information on the location, quantity, and quality of water available from underground coal mines in the Breathitt Formation of Pennsylvanian age in part of eastern Kentucky. The principal coal seams mined are the Van Lear in Johnson County and the Alma in Martin County. Coal mines that contained water were located by field inventory and coal-mine maps.\r\n\r\nThe principal factors that affect the occurrence of water in coal mines are the size of the recharge area overlying the mine, the intensity and duration of precipitation, and the altitude of the mine relative to that of the nearest perennial stream.\r\n\r\nTen above-drainage mines (that is, mines at higher elevations than that of the nearest perennial stream) are considered potential sources of water. Discharge from these mines ranged from 12 to 1,700 gallons per minute. The highest sustained discharge from a mine ranged from 750 to 1,200 gallons per minute.\r\n\r\nThe water in coal mines is part of the hydrologic system and varies seasonally with precipitation. Annual discharge from most above-drainage mines ranged from 3 to 10 percent of annual precipitation on the 1and-surface area above the mine.\r\n\r\nEight below-drainage mines are considered potential sources of water. Two were test-pumped at rates of 560 to 620 gallons per minute for as long as 6 hours. After test pumping the Warfield Mining No. 1 mine during September 1977 and March 1978, the recovery (or recharge) rates were significantly different. In September, the recharge rate was about 1,150 gallons per minute, but in March the recharge rate was 103,500 gallons per minute. This difference reflects the seasonal variations in the amount of water available to the ground-water system. Estimates of water stored in below-drainage mines ranged from 22 to 1,462 million gallons. This storage represents a safety factor sufficient to provide water through periods of limited recharge to the mine.\r\n\r\nMost mine water is of the calcium magnesium sulfate type. In general, water from below-drainage mines had lower concentrations of dissolved constituents and higher pH than water from mines above drainage. The hardness of water ranged from soft to very hard and pH ranged -from 3.1 to 8.0 units. Dissolved iron ranged from 0.01 to 64 milligrams per liter. Phenol concentrations in water from eight coal mines ranged from 0 to 5 micrograms per liter.\r\n\r\nThere seems to be a significant difference in the chemical quality of water from above- and below-drainage mines. The concentration of most constituents was lower in water from below-drainage mines than it was from above-drainage mines.\r\n\r\nThe better quality water from below-drainage mines may reflect (1) lower mineralization resulting from less atmospheric oxygen available to react with pyrite or, (2) the result of sampling only the upper zones of water in below-drainage mines where the water has been diluted by less mineralized surface water or inflow or recharge.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri81690","collaboration":"Prepared in cooperation with the Kentucky Geological Survey and the University of Kentucky","usgsCitation":"Mull, D.S., Cordivio1a, S., and Risser, D.W., 1981, Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky (WRI/OFR 81-690): U.S. Geological Survey Water-Resources Investigations Report 81-690, viii, 55 p.; Plates, https://doi.org/10.3133/wri81690.","productDescription":"viii, 55 p.; Plates","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":124648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0690/report-thumb.jpg"},{"id":91361,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0690/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83,37.666666666666664 ], [ -83,38 ], [ -82.58333333333333,38 ], [ -82.58333333333333,37.666666666666664 ], [ -83,37.666666666666664 ] ] ] } } ] }","edition":"WRI/OFR 81-690","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a85e4b07f02db64d4be","contributors":{"authors":[{"text":"Mull, D. S.","contributorId":43331,"corporation":false,"usgs":true,"family":"Mull","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":247913,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cordivio1a, Steven","contributorId":26357,"corporation":false,"usgs":true,"family":"Cordivio1a","given":"Steven","email":"","affiliations":[],"preferred":false,"id":247912,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Risser, Dennis W. 0000-0001-9597-5406 dwrisser@usgs.gov","orcid":"https://orcid.org/0000-0001-9597-5406","contributorId":898,"corporation":false,"usgs":true,"family":"Risser","given":"Dennis","email":"dwrisser@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247911,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":20144,"text":"ofr81579 - 1981 - Schematic drawing of a USGS high voltage D.C. resistivity transmitter","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr81579","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-579","title":"Schematic drawing of a USGS high voltage D.C. resistivity transmitter","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr81579","usgsCitation":"Mitchell, C.M., and Krizman, R.W., 1981, Schematic drawing of a USGS high voltage D.C. resistivity transmitter: U.S. Geological Survey Open-File Report 81-579, 2 p. ;28 cm., https://doi.org/10.3133/ofr81579.","productDescription":"2 p. ;28 cm.","costCenters":[],"links":[{"id":152827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0579/report-thumb.jpg"},{"id":49684,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0579/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd4c7","contributors":{"authors":[{"text":"Mitchell, C. M.","contributorId":106859,"corporation":false,"usgs":true,"family":"Mitchell","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":182142,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krizman, R. W.","contributorId":78304,"corporation":false,"usgs":true,"family":"Krizman","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":182141,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25041,"text":"pp1113 - 1981 - Metamorphic mineral assemblages of slightly calcic pelitic rocks in and around the Taconic Allochthon, southwestern Massachusetts and adjacent Connecticut and New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"pp1113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1113","title":"Metamorphic mineral assemblages of slightly calcic pelitic rocks in and around the Taconic Allochthon, southwestern Massachusetts and adjacent Connecticut and New York","docAbstract":"The mineral assemblages from metamorphosed slightly calcic pelitic rocks of the Taconic Range in southwestern Massachusetts and adjacent areas of Connecticut and New York were studied petrographically and chemically. These rocks vary in metamorphic grade from those below the chloritoid zone through the chloritoid and garnet zones into the kyanite-staurolite zone. Microprobe data on the ferromagnesian minerals show that the sequence of increasing Fe/ (Fe+Mg) value is, from the lowest, chlorite, biotite, hornblende, chloritoid, staurolite, garnet. Hornblende, epidote, garnet, and plagioclase are the most common minerals that carry significant calcium. Biotite is persistently deficient in alkali but is abnormally rich in octahedral aluminum to such an extent that the overall charge balance can be ascribed to an AI=K+ (Fe,Mg) diadochy. Muscovite contains small though persistent amounts of iron and magnesium in octahedral positions but has a variable K/Na ratio, which is potentially useful as a geothermometer. One low-grade muscovite is highly phengitic, but the white micas in rocks from metamorphic grades higher than chloritoid zone do not contain significant phengite components. Chlorite is persistently high in aluminum and so its ratio of divalent ions to aluminum is approximately that of garnet. Many garnets show pronounced zoning in manganese and less pronounced zoning in calcium. Garnet coexisting with hornblende contains a high proportion of the grossularitic component. The calcium content is significant in all the analyzed garnets, except those from a cummingtonite-bearing sample that is free of muscovite. This suggests that in slightly calcic pelitic rocks, calcium-free garnet cannot coexist with muscovite. \r\n\r\nMost of the mineral assemblages formed in the presence of excess quartz and muscovite. The phase-petrologic analysis, made with the aid of an eight-phase multisystematic model, shows the following major points: \r\n\r\n1. Chloritoid and staurolite coexist in a definite interval of prograde metamorphism. \r\n\r\n2. Biotite-chloritoid does not constitute an alternative assemblage to garnet-chlorite-muscovite, because the former combination is found predominantly in the presence of the latter combination. Because the garnet contains lime, all five phases are stable together in lowlime pelitic rocks. \r\n\r\n3. The first appearance of staurolite in the area does not correspond to the reaction leading to the first intrinsic stable existence of this phase. Inasmuch as the first appearanc,e of staurolite is always in chlorite-bearing as semblages, I suggest that the mapped staurolite zone marker corresponds to a reaction whereby staurolitechlorite becomes stable. The probable lower grade chemical equivalent, for example, chloritoid-aluminum silicate, however, has not been found in the area of study. Several staurolite-forming reactions discussed in the literature are ruled out because of the relative siderophility of the minerals. A second staurolite isograd involves the reaction, chloritoid+chlorite+muscovite= staurolite+biotite. A third isograd involves staurolite+ chlorite=biotite+kyanite; this reaction is postulated on the basis of the observed assemblage biotite-kyanitesta urolite-garnet-muscoviteplagioclase-quartzilmenite. \r\n\r\n4. In low-grade rocks, epidote is stable considerably before the first appearance of chloritoid. The nature of the high-aluminum phase in low-grade rocks that leads to the formation of chloritoid remains obscure. The epidote is always rich in ferric iron (pistacite content of about 1/ 4 to 1/3). Garnet-bearing assemblages (with or without epidote) are formed next as metamorphic grade increases. The next more calcium-rich silicate is hornblende, and despite the meager data on assemblages that include hornblende, the first intrinsic appearance of this phase has probably been recorded. At highstaurolite grade, the most calcium-rich assemblage in pelitic rocks is hornblende-garnet-biotite-plagioclase (bytownit","language":"ENGLISH","publisher":"G.P.O.,","doi":"10.3133/pp1113","usgsCitation":"Zen, E., 1981, Metamorphic mineral assemblages of slightly calcic pelitic rocks in and around the Taconic Allochthon, southwestern Massachusetts and adjacent Connecticut and New York: U.S. Geological Survey Professional Paper 1113, 128 p., https://doi.org/10.3133/pp1113.","productDescription":"128 p.","costCenters":[],"links":[{"id":118856,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1113/report-thumb.jpg"},{"id":54046,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1113/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db6287d1","contributors":{"authors":[{"text":"Zen, E-an","contributorId":38564,"corporation":false,"usgs":true,"family":"Zen","given":"E-an","affiliations":[],"preferred":false,"id":193120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24644,"text":"ofr801223 - 1981 - Data on ground-water quality with emphasis on radionuclides, Sarasota County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"ofr801223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1223","title":"Data on ground-water quality with emphasis on radionuclides, Sarasota County, Florida","docAbstract":"A compilation of analytical results are presented for selected radiochemical and chemical characteristics for 200 groundwater samples collected from 92 wells in Sarasota County, Fla. Radium-226 analysis was made on 160 of the water samples and 80 samples equaled or exceeded the 5 picocuries per liter maximum contaminant level established by the National Interim Primary Drinking Regulations. (USGS)","language":"ENGLISH","publisher":"U.S. Dept of the Interior, Geological Survey,","doi":"10.3133/ofr801223","issn":"0094-9140","usgsCitation":"Sutcliffe, H., and Miller, R.L., 1981, Data on ground-water quality with emphasis on radionuclides, Sarasota County, Florida: U.S. Geological Survey Open-File Report 80-1223, iii, 16 p. :maps ;28 cm., https://doi.org/10.3133/ofr801223.","productDescription":"iii, 16 p. :maps ;28 cm.","costCenters":[],"links":[{"id":157546,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1223/report-thumb.jpg"},{"id":53681,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1223/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c73f","contributors":{"authors":[{"text":"Sutcliffe, Horace","contributorId":28598,"corporation":false,"usgs":true,"family":"Sutcliffe","given":"Horace","affiliations":[],"preferred":false,"id":192312,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, R. L.","contributorId":54178,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":192313,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":43336,"text":"ofr811092 - 1981 - Geology of the Whitehorse Caldera and caldera-fill deposits, Malheur County, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:04:53","indexId":"ofr811092","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1092","title":"Geology of the Whitehorse Caldera and caldera-fill deposits, Malheur County, Oregon","language":"ENGLISH","doi":"10.3133/ofr811092","usgsCitation":"Rytuba, J.J., Minor, S., and McKee, E.H., 1981, Geology of the Whitehorse Caldera and caldera-fill deposits, Malheur County, Oregon: U.S. Geological Survey Open-File Report 81-1092, 1 map ;39 x 43 cm. +lithology on sheet 56 x 49 cm. and text (22 p. ; 28 cm.), https://doi.org/10.3133/ofr811092.","productDescription":"1 map ;39 x 43 cm. +lithology on sheet 56 x 49 cm. and text (22 p. ; 28 cm.)","costCenters":[],"links":[{"id":134921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1092/report-thumb.jpg"},{"id":81085,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1092/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81086,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1092/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81087,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c941","contributors":{"authors":[{"text":"Rytuba, James J. jrytuba@usgs.gov","contributorId":3043,"corporation":false,"usgs":true,"family":"Rytuba","given":"James","email":"jrytuba@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":228058,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Minor, S.A.","contributorId":65047,"corporation":false,"usgs":true,"family":"Minor","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":228060,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":228059,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":62511,"text":"gq1546 - 1981 - Geologic map of the Shady Spring quadrangle, Raleigh and Summers Counties, West Virginia","interactions":[{"subject":{"id":46645,"text":"ofr791512 - 1979 - Geologic map of the Shady Spring Quadrangle, Raleigh and Summers counties, West Virginia","indexId":"ofr791512","publicationYear":"1979","noYear":false,"title":"Geologic map of the Shady Spring Quadrangle, Raleigh and Summers counties, West Virginia"},"predicate":"SUPERSEDED_BY","object":{"id":62511,"text":"gq1546 - 1981 - Geologic map of the Shady Spring quadrangle, Raleigh and Summers Counties, West Virginia","indexId":"gq1546","publicationYear":"1981","noYear":false,"title":"Geologic map of the Shady Spring quadrangle, Raleigh and Summers Counties, West Virginia"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:01","indexId":"gq1546","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1546","title":"Geologic map of the Shady Spring quadrangle, Raleigh and Summers Counties, West Virginia","language":"ENGLISH","doi":"10.3133/gq1546","usgsCitation":"Meissner, C., 1981, Geologic map of the Shady Spring quadrangle, Raleigh and Summers Counties, West Virginia: U.S. Geological Survey Geologic Quadrangle 1546, 1 map :col. ;58 x 46 cm., https://doi.org/10.3133/gq1546.","productDescription":"1 map :col. ;58 x 46 cm.","costCenters":[],"links":[{"id":102641,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1091.htm","linkFileType":{"id":5,"text":"html"},"description":"1091"},{"id":248674,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1546/report.pdf","size":"71","linkFileType":{"id":1,"text":"pdf"}},{"id":253901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1546/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.11749999999999,37.6175 ], [ -81.11749999999999,37.75 ], [ -81,37.75 ], [ -81,37.6175 ], [ -81.11749999999999,37.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68ba58","contributors":{"authors":[{"text":"Meissner, Charles R.","contributorId":27863,"corporation":false,"usgs":true,"family":"Meissner","given":"Charles R.","affiliations":[],"preferred":false,"id":267478,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24989,"text":"pp716G - 1981 - Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan","interactions":[{"subject":{"id":21827,"text":"ofr80837 - 1980 - Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan","indexId":"ofr80837","publicationYear":"1980","noYear":false,"title":"Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan"},"predicate":"SUPERSEDED_BY","object":{"id":24989,"text":"pp716G - 1981 - Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan","indexId":"pp716G","publicationYear":"1981","noYear":false,"chapter":"G","title":"Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan"},"id":1}],"lastModifiedDate":"2016-12-09T12:21:14","indexId":"pp716G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"716","chapter":"G","title":"Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan","language":"ENGLISH","publisher":"U.S. Govt. Print. Off. ;\r\nfor sale by the Distribution Branch, U.S. Geological Service,","doi":"10.3133/pp716G","usgsCitation":"Calkins, J.A., Jamiluddin, S., Bhuyan, K., and Hussain, A., 1981, Geology and mineral resources of the Chitral-Partsan area, Hindu Kush Range, northern Pakistan: U.S. Geological Survey Professional Paper 716, 32 p.; 2 plates in pocket, https://doi.org/10.3133/pp716G.","productDescription":"32 p.; 2 plates in pocket","costCenters":[],"links":[{"id":118989,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0716g/report-thumb.jpg"},{"id":53974,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0716g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53975,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0716g/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53976,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0716g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264560,"rank":2,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/pp/0716g/plate-table_1.pdf","text":"Table 1","size":"1686","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684afd","contributors":{"authors":[{"text":"Calkins, James Alfred","contributorId":75504,"corporation":false,"usgs":true,"family":"Calkins","given":"James","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":192955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jamiluddin, S.","contributorId":29009,"corporation":false,"usgs":true,"family":"Jamiluddin","given":"S.","email":"","affiliations":[],"preferred":false,"id":192953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bhuyan, Kamaluddin","contributorId":70802,"corporation":false,"usgs":true,"family":"Bhuyan","given":"Kamaluddin","email":"","affiliations":[],"preferred":false,"id":192954,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hussain, Ahmad","contributorId":81523,"corporation":false,"usgs":true,"family":"Hussain","given":"Ahmad","email":"","affiliations":[],"preferred":false,"id":192956,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":9860,"text":"ofr82157 - 1981 - Discharge data at water-quality monitoring stations in Arkansas, 1980 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-157","title":"Discharge data at water-quality monitoring stations in Arkansas, 1980 water year","docAbstract":"Discharge data were computed for a network of water-quality monitoring stations operated by the Arkansas Department of Pollution Control and Ecology. Some of the sites are located at U.S. Geological Survey of U.S. Army Corps of Engineers daily-discharge stations, but most sites are at points where discharges are not regularly measured. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82157","usgsCitation":"Knott, R., 1981, Discharge data at water-quality monitoring stations in Arkansas, 1980 water year: U.S. Geological Survey Open-File Report 82-157, ii, 37 p., 28 cm., https://doi.org/10.3133/ofr82157.","productDescription":"ii, 37 p., 28 cm.","costCenters":[],"links":[{"id":142660,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0157/report-thumb.jpg"},{"id":37654,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0157/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aa2a","contributors":{"authors":[{"text":"Knott, R.K.","contributorId":102484,"corporation":false,"usgs":true,"family":"Knott","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":160419,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53612,"text":"ofr81690 - 1981 - Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:11","indexId":"ofr81690","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-690","title":"Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky","docAbstract":"This report provides water users with detailed information on the location, quantity, and quality of water available from underground coal mines in the Breathitt Formation of Pennsylvanian age in part of eastern Kentucky. The principal coal seams mined are the Van Lear in Johnson County and the Alma in Martin County. Coal mines that contained water were located by field inventory and coal-mine maps.\r\n\r\nThe principal factors that affect the occurrence of water in coal mines are the size of the recharge area overlying the mine, the intensity and duration of precipitation, and the altitude of the mine relative to that of the nearest perennial stream.\r\n\r\nTen above-drainage mines (that is, mines at higher elevations than that of the nearest perennial stream) are considered potential sources of water. Discharge from these mines ranged from 12 to 1,700 gallons per minute. The highest sustained discharge from a mine ranged from 750 to 1,200 gallons per minute.\r\n\r\nThe water in coal mines is part of the hydrologic system and varies seasonally with precipitation. Annual discharge from most above-drainage mines ranged from 3 to 10 percent of annual precipitation on the 1and-surface area above the mine.\r\n\r\nEight below-drainage mines are considered potential sources of water. Two were test-pumped at rates of 560 to 620 gallons per minute for as long as 6 hours. After test pumping the Warfield Mining No. 1 mine during September 1977 and March 1978, the recovery (or recharge) rates were significantly different. In September, the recharge rate was about 1,150 gallons per minute, but in March the recharge rate was 103,500 gallons per minute. This difference reflects the seasonal variations in the amount of water available to the ground-water system. Estimates of water stored in below-drainage mines ranged from 22 to 1,462 million gallons. This storage represents a safety factor sufficient to provide water through periods of limited recharge to the mine.\r\n\r\nMost mine water is of the calcium magnesium sulfate type. In general, water from below-drainage mines had lower concentrations of dissolved constituents and higher pH than water from mines above drainage. The hardness of water ranged from soft to very hard and pH ranged -from 3.1 to 8.0 units. Dissolved iron ranged from 0.01 to 64 milligrams per liter. Phenol concentrations in water from eight coal mines ranged from 0 to 5 micrograms per liter.\r\n\r\nThere seems to be a significant difference in the chemical quality of water from above- and below-drainage mines. The concentration of most constituents was lower in water from below-drainage mines than it was from above-drainage mines.\r\n\r\nThe better quality water from below-drainage mines may reflect (1) lower mineralization resulting from less atmospheric oxygen available to react with pyrite or, (2) the result of sampling only the upper zones of water in below-drainage mines where the water has been diluted by less mineralized surface water or inflow or recharge.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr81690","collaboration":"Prepared in cooperation with the Kentucky Geological Survey and the University of Kentucky","usgsCitation":"Mull, D.S., Cordivio1a, S., and Risser, D.W., 1981, Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky (WRI/OFR 81-690): U.S. Geological Survey Open-File Report 81-690, viii, 55 p.; Plates, https://doi.org/10.3133/ofr81690.","productDescription":"viii, 55 p.; Plates","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":175253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0690/report-thumb.jpg"},{"id":87487,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0690/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83,37.666666666666664 ], [ -83,38 ], [ -82.58333333333333,38 ], [ -82.58333333333333,37.666666666666664 ], [ -83,37.666666666666664 ] ] ] } } ] }","edition":"WRI/OFR 81-690","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64afa8","contributors":{"authors":[{"text":"Mull, D. S.","contributorId":43331,"corporation":false,"usgs":true,"family":"Mull","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":247910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cordivio1a, Steven","contributorId":26357,"corporation":false,"usgs":true,"family":"Cordivio1a","given":"Steven","email":"","affiliations":[],"preferred":false,"id":247909,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Risser, Dennis W. 0000-0001-9597-5406 dwrisser@usgs.gov","orcid":"https://orcid.org/0000-0001-9597-5406","contributorId":898,"corporation":false,"usgs":true,"family":"Risser","given":"Dennis","email":"dwrisser@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247908,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7662,"text":"ofr8145 - 1981 - Scanning electron micrographs of chrysomonad cysts from Lake Aloha, El Dorado County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr8145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-45","title":"Scanning electron micrographs of chrysomonad cysts from Lake Aloha, El Dorado County, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8145","usgsCitation":"Adam, D.P., and Mahood, A.D., 1981, Scanning electron micrographs of chrysomonad cysts from Lake Aloha, El Dorado County, California: U.S. Geological Survey Open-File Report 81-45, 15 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr8145.","productDescription":"15 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":141491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0045/report-thumb.jpg"},{"id":35137,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdb71","contributors":{"authors":[{"text":"Adam, David P.","contributorId":36132,"corporation":false,"usgs":true,"family":"Adam","given":"David","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":156390,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mahood, Albert D.","contributorId":97493,"corporation":false,"usgs":true,"family":"Mahood","given":"Albert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":156391,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8513,"text":"ofr81389 - 1981 - Interpretation of geophysical well-log measurements in drill holes UE25a-4, -5, -6, and -7, Yucca Mountain, Nevada Test Site","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr81389","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-389","title":"Interpretation of geophysical well-log measurements in drill holes UE25a-4, -5, -6, and -7, Yucca Mountain, Nevada Test Site","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81389","usgsCitation":"Daniels, J.J., Scott, J.H., and Hagstrum, J., 1981, Interpretation of geophysical well-log measurements in drill holes UE25a-4, -5, -6, and -7, Yucca Mountain, Nevada Test Site: U.S. Geological Survey Open-File Report 81-389, 31 p. :ill. ;28 cm., https://doi.org/10.3133/ofr81389.","productDescription":"31 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":142932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0389/report-thumb.jpg"},{"id":36085,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0389/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d2bb","contributors":{"authors":[{"text":"Daniels, Jeffrey J.","contributorId":87938,"corporation":false,"usgs":true,"family":"Daniels","given":"Jeffrey","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":157847,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, James H.","contributorId":73579,"corporation":false,"usgs":true,"family":"Scott","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":157845,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hagstrum, J.T.","contributorId":75922,"corporation":false,"usgs":true,"family":"Hagstrum","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":157846,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":65630,"text":"i1379 - 1981 - Controlled photomosaic of the Olympus Mons region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:10","indexId":"i1379","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1379","subseriesTitle":"NONE","title":"Controlled photomosaic of the Olympus Mons region of Mars","language":"ENGLISH","doi":"10.3133/i1379","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Controlled photomosaic of the Olympus Mons region of Mars: U.S. Geological Survey IMAP 1379, 1 map ;107 x 78 cm., https://doi.org/10.3133/i1379.","productDescription":"1 map ;107 x 78 cm.","costCenters":[],"links":[{"id":114989,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1379/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":114990,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1379/plate-1.pdf","size":"19469","linkFileType":{"id":1,"text":"pdf"}},{"id":190231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1379/report-thumb.jpg"}],"scale":"206000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686637","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":534018,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7757,"text":"ofr81421 - 1981 - Background hydrologic information in potential lignite mining areas in Mississippi, August 1980","interactions":[],"lastModifiedDate":"2022-11-04T17:29:59.898863","indexId":"ofr81421","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-421","title":"Background hydrologic information in potential lignite mining areas in Mississippi, August 1980","docAbstract":"The U.S. Geological Survey in cooperation with Mississippi Bureau of Geology is conducting a hydrologic data-collection program in the potential lignite-producing areas in Mississippi. During the week of August 25-28, 1980, hydrologic data on channel characteristics were collected at 15 sites on small streams draining potential lignite mining areas in east-central Mississippi. Streamflow measurements were made and water-quality samples were collected at 11 of the 15 sites.
Main channel widths at the 15 sampling sites in east-central Mississippi ranged from 126 feet on Sucarnoochee Creek to 15 feet on Houston Creek. Maximum water depth ranged from 7 feet on Pawticfaw Creek and Tallahatta Creek to one-half foot on Okatibbee Creek. The maximum stream discharge measured was 56 cubic feet per second on Pawticfaw Creek. Four sites had no discharge. Specific conductance at sampling sites ranged from 115 micromhos on Ponta Creek to 26 micromhos on Sucarnoochee Creek. The dissolved-oxygen concentration was 5.7 milligrams per liter or higher at all sites. The concentration of suspended sediment was not greater than 38 milligrams per liter at any site. Concentrations of calcium, magnesium, sodium, potassium, chloride, and sulfate were less than 10 milligrams per liter in all samples, but were highest at site 10 on Ponta Creek. Bottom-material samples commonly contained iron, manganese, and zinc.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81421","collaboration":"Prepared in cooperation with the Mississippi Department of Natural Resources, Bureau of Geology","usgsCitation":"Arthur, J.K., 1981, Background hydrologic information in potential lignite mining areas in Mississippi, August 1980: U.S. Geological Survey Open-File Report 81-421, 19 p., https://doi.org/10.3133/ofr81421.","productDescription":"19 p.","costCenters":[],"links":[{"id":409171,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0421/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142244,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0421/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69794b","contributors":{"authors":[{"text":"Arthur, J. K.","contributorId":56223,"corporation":false,"usgs":true,"family":"Arthur","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":156548,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7010,"text":"ofr81621 - 1981 - Arctic summary report: Outer Continental Shelf and onshore oil and gas activities and impacts in the Arctic : a summmary report, October 1981","interactions":[],"lastModifiedDate":"2024-02-08T21:44:18.761965","indexId":"ofr81621","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-621","title":"Arctic summary report: Outer Continental Shelf and onshore oil and gas activities and impacts in the Arctic : a summmary report, October 1981","docAbstract":"Due to the amount of Federal and State oil and gas activity in the Arctic subregion and the need for comprehensive planning, State and local officials requested coverage of all oil and gas activity in the area.
The first lease sale of offshore lands in the Beaufort Sea was held by the State of Alaska in 1969. The leasing process for oil and gas exploration on the Beaufort Sea Outer Continental Shelf (OCS) began in April 1976 with the first Federal lease sale in the subregion (Joint Federal/State Beaufort Sea Lease Sale) held in 1979. This sale was held jointly by the Department of the Interior and the State of Alaska because of conflicting jurisdictional claims to certain tracts in the sale area. The jurisdictional dispute will be resolved by the U.S. Supreme Court, but a decision is not expected for several years. The joint sale was held on December 11, 1979. However, bids on the Federal tracts were not accepted until July 1980 because of litigation. Of the 117 tracts offered, 86 were leased as a result of the sale. Of these 86 tracts, 24 are federally managed and 62 are State-managed.
Two exploration plans have been submitted for the federally managed joint lease sale (Sale BF) area. Both plans call for building a gravel island and exploratory drilling of several tracts, but no drilling permits have yet been filed. Three exploratory wells have been drilled on or into State-managed tracts. These include one well drilled directionally into Tract 75, one into Tract 76, and one well drilled from Challenge Island, a natural barrier island. Additional exploratory wells are planned for the 1981-82 drilling season on State-managed tracts.
The next OCS sale in the Beaufort Sea, Lease Sale 71, is proposed for September 1982. The first two sales in the National Petroleum Reserve in Alaska are being planned for December 1981 and the late spring or early summer of 1982 and will involve a total of 2 million acres (809,200 hectares). In anticipation of future leasing, plans for geophysical surveys in the Arctic National Wildlife Refuge are also being formulated.
Four State lease sales have been held in the Arctic, in addition to the Joint Federal/State Lease Sale. These onshore sales have resulted in the leasing of lands on which a number of commercial discoveries have been made, including the discovery of the largest hydrocarbon accumulation in North America at Prudhoe Bay. Exploration, development, and production are continuing on these State lands. The State of Alaska has plans for three future lease sales in the Arctic to be held in the spring of 1982 and 1983 and the fall of 1984. Leasing and exploration are also under way on Arctic Slope Regional Corporation lands.
Transportation systems in the Arctic have been developed to accommodate production on State lands. Some of the production from OCS tracts, as well as other Arctic lands, may be handled by the existing Trans-Alaska Pipeline System. However, a number of additional transportation strategies are being considered, including the Alaska Natural Gas Transportation System, additional oil pipelines, and tanker transport. The pace of oil and gas production in the Arctic will depend in part on the number and type of transportation modes available.
The support bases at Prudhoe Bay are expected to be used to some extent for future activities on the OCS. However, expanded and new facilities will also be required, depending on the location of discoveries on the OCS and on other Arctic lands. The impacts resulting from OCS activities in the Arctic will be particularly important because of their contribution to the regionwide and cumulative impacts arising from Federal onshore, State, and regional corporation oil and gas exploration, development, and production in the Arctic.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81621","usgsCitation":"Jackson, J.B., Golden, B., Stadnychenko, A., and Kolasinski, S., 1981, Arctic summary report: Outer Continental Shelf and onshore oil and gas activities and impacts in the Arctic : a summmary report, October 1981: U.S. Geological Survey Open-File Report 81-621, x, 137 p., https://doi.org/10.3133/ofr81621.","productDescription":"x, 137 p.","costCenters":[],"links":[{"id":425512,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0621/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139505,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0621/report-thumb.jpg"}],"country":"United 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Joanne Barnes","contributorId":31752,"corporation":false,"usgs":true,"family":"Jackson","given":"Joanne","email":"","middleInitial":"Barnes","affiliations":[],"preferred":false,"id":153899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Golden, B.F.","contributorId":45701,"corporation":false,"usgs":true,"family":"Golden","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":153901,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stadnychenko, Anne","contributorId":32515,"corporation":false,"usgs":true,"family":"Stadnychenko","given":"Anne","email":"","affiliations":[],"preferred":false,"id":153900,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kolasinski, Sharon","contributorId":46510,"corporation":false,"usgs":true,"family":"Kolasinski","given":"Sharon","affiliations":[],"preferred":false,"id":153902,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7873,"text":"ofr81879 - 1981 - Studies of the seismic and crustal deformation patterns of an active fault; Pinon Flat Observatory, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr81879","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-879","title":"Studies of the seismic and crustal deformation patterns of an active fault; Pinon Flat Observatory, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81879","usgsCitation":"Berger, J., and Brune, J.N., 1981, Studies of the seismic and crustal deformation patterns of an active fault; Pinon Flat Observatory, California: U.S. Geological Survey Open-File Report 81-879, 5 p. ill. ;28 cm., https://doi.org/10.3133/ofr81879.","productDescription":"5 p. ill. ;28 cm.","costCenters":[],"links":[{"id":140475,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0879/report-thumb.jpg"},{"id":35381,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0879/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dd3","contributors":{"authors":[{"text":"Berger, Jonathan","contributorId":83113,"corporation":false,"usgs":true,"family":"Berger","given":"Jonathan","email":"","affiliations":[],"preferred":false,"id":156763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brune, James N.","contributorId":76304,"corporation":false,"usgs":true,"family":"Brune","given":"James","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":156762,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7964,"text":"ofr81842 - 1981 - Chemical analyses of selected agricultural soils of Missouri","interactions":[],"lastModifiedDate":"2025-09-15T18:00:43.340655","indexId":"ofr81842","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-842","title":"Chemical analyses of selected agricultural soils of Missouri","docAbstract":"This report contains a compilation of chemical data for samples of the plow zone of agricultural soils that were collected in 1970 from each of the 114 counties of the State of Missouri. Most of the principal taxonomic soil types that occur in each county are represented by the 10 samples per county that were collected. There are numerous examples of soils that were developed from each of the several parent-material types in the State.
Each soil sample is a composite of several channel samples collected throughout a field from a depth 0-15cm. Soil material that passed a 2mm sieve was ground in a ceramic mill to -100 mesh and then analyzed for total concentrations of 70 elements. The methods of analysis and the lower limits of determination for each element are given in table 1. Most methods were described by Miesch (1976); delayed neutron counting for uranium and thorium was described by Millard (1976). The limits of determination for the methods did not always encompass the natural range of element concentrations in some samples, thus the elements may be classed into three groups: never detected, rarely detected, and frequently detected.
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