Water resources data for the 1983 water year for Pennsylvania consist of records of discharge and water quality of streams; contents of lakes and reservoirs; and water levels, and water quality of ground-water wells. This volume contains records for water discharge at 84 stations; contents at 13 lakes and reservoirs, water quality at 18 gaging stations; and water levels at 26 network observation wells. Also included are data for 12 crest-stage, 98 low flow, and 3 water-quality, and 85 ground water-quality partial-record stations. Locations of these sites are shown on figures 7-10. Additional water data were collected at various sites not involved in-the systematic data-collection program and are published as miscellaneous measurements and analysis. These data together with the data in Volumes 1 and 3 represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in Pennsylvania.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrPA832","collaboration":"Prepared in cooperation with the Pennsylvania Department of Environmental Resources, the U.S. Army Corps of Engineers, Baltimore District, The Susquehanna River Basin Commission, and with other State, municipal, and Federal agencies","usgsCitation":"Buchanan, J., Loper, W., Schaffstall, W., and Hainly, R., 1984, Water resources data, Pennsylvania, water year 1983. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1284","usgsCitation":"Baird, A.K., and Miesch, A., 1984, Batholithic rocks of Southern California: A model for the petrochemical nature of their source materials: U.S. Geological Survey Professional Paper 1284, iii, 42 p., https://doi.org/10.3133/pp1284.","productDescription":"iii, 42 p.","costCenters":[],"links":[{"id":407185,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74524.htm","linkFileType":{"id":5,"text":"html"}},{"id":65320,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1284/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1284/report-thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.3236,\n 32.9\n ],\n [\n -115.7917,\n 32.9\n ],\n [\n -115.7917,\n 34.5667\n ],\n [\n -118.3236,\n 34.5667\n ],\n [\n -118.3236,\n 32.9\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640b33","contributors":{"authors":[{"text":"Baird, A. K.","contributorId":65148,"corporation":false,"usgs":true,"family":"Baird","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":220042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miesch, A.T.","contributorId":88726,"corporation":false,"usgs":true,"family":"Miesch","given":"A.T.","affiliations":[],"preferred":false,"id":220043,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":38561,"text":"pp1295 - 1984 - Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age","interactions":[{"subject":{"id":49319,"text":"ofr77544 - 1977 - Seismic refraction time-distance curves, Carolina, Hope Valley, and Kingston quadrangles, Rhode Island","indexId":"ofr77544","publicationYear":"1977","noYear":false,"title":"Seismic refraction time-distance curves, Carolina, Hope Valley, and Kingston quadrangles, Rhode Island"},"predicate":"SUPERSEDED_BY","object":{"id":38561,"text":"pp1295 - 1984 - Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age","indexId":"pp1295","publicationYear":"1984","noYear":false,"title":"Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age"},"id":1}],"lastModifiedDate":"2022-12-21T20:09:55.708609","indexId":"pp1295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1295","title":"Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age","docAbstract":"The Glastonbury dome is a long, narrow structure trending approximately 70 km north-northeast through Connecticut and Massachusetts along the west side of the Bronson Hill anticlinorium. Structurally and stratigraphically the dome is analogous to the Oliverian domes of New Hampshire. It is cored by Glastonbury Gneiss and is mantled by Ammonoosuc Volcanics and Partridge Formation (or their equivalents) of Ordovician age. The Glastonbury Gneiss intrudes the Ammonoosuc and, thereby, establishes the relative age of the two units. Monson Gneiss, which unconformably underlies the Ammonoosuc Volcanics in the Monson anticline to the east, is not in contact with Glastonbury Gneiss except near Stafford Springs, Conn., where the contact may be gradational. In some places, Monson Gneiss shows evidence of plastic flow and potential anatexis. The northern part of the Glastonbury Gneiss typically is leucocratic, granoblastic, relatively potassium-poor gneiss that appears homogeneous in outcrop, but proves to be chemically and modally inhomogeneous over short distances, as shown by variation diagrams and REE plots. The gneiss straddles the compositional fields of trondhjemite, tonalite, and granodiorite, and partly overlaps that of Monson Gneiss. The southern part of the Glastonbury Gneiss is consistently more potassic than the northern, having compositions ranging from granite to granodiorite. All of the Glastonbury Gneiss show pervasive, strong foliation, deformation, and local shearing related to the Acadian orogeny. \r\n\r\nField relations, textures, and chemistry of the northern part of the Glastonbury suggest an origin by anatexis of the premetamorphic Monson sequence at temperatures of about 690 DC to 750 DC and pressures of <3kbars. The southern part of the Glastonbury appears to have been generated contemporaneously but not comagmatically from calcalkaline crust. U-Pb zircon ages for both the northern and southern bodies are slightly discordant with 207PbfosPb ages of 445 to 467 m.y. At first these results seem to contradict the known stratigraphic position of the Glastonbury relative to the Monson, which yields distinctly younger zircon 207PbfosPb ages of 428 to 440 m.y. However, this apparent discrepancy in the radiometric ages-younger Monson, older Glastonbury-could be resolved by postulating either (1) a small component of old inherited zircon in the Glastonbury or (2) preferential metamorphic overprinting of the zircon in the Monson. In any case, the isotopic age discrepancy is not so large as to render the proposed Monson anatectic model implausible. Rb-Sr whole-rock data show a large amount of scatter on an isochron diagram and hence do not permit a reliable estimate of age. This condition may reflect inhomogeneities in the initial 87S r /8SS r ratio or may have been also induced by later Acadian or Alleghanian metamorphism. \r\n\r\nAn early Silurian to Middle Ordovician age of the Glastonbury Gneiss gives evidence of higher heat flow and more extensive plutonism in the Taconic than has generally been recognized. With certain qualifications, the Glastonbury and associated volcanic rocks are compatible with recent plate-tectonic models involving the Bronson Hill anticlinorium.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1295","usgsCitation":"Leo, G.W., Zartman, R., and Brookins, D.G., 1984, Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age (Supercedes OFR 77-544): U.S. Geological Survey Professional Paper 1295, iv, 45 p., https://doi.org/10.3133/pp1295.","productDescription":"iv, 45 p.","costCenters":[],"links":[{"id":410878,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74531.htm","linkFileType":{"id":5,"text":"html"}},{"id":65330,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1295/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1295/report-thumb.jpg"}],"country":"United States","state":"Connecticut, Massachusetts","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -72.25,\n 42.25\n ],\n [\n -72.625,\n 42.25\n ],\n [\n -72.625,\n 41.5772\n ],\n [\n -72.25,\n 41.5772\n ],\n [\n -72.25,\n 42.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Supercedes OFR 77-544","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abee4b07f02db674deb","contributors":{"authors":[{"text":"Leo, G. W.","contributorId":102899,"corporation":false,"usgs":true,"family":"Leo","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":220069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zartman, R. E.","contributorId":15632,"corporation":false,"usgs":true,"family":"Zartman","given":"R. E.","affiliations":[],"preferred":false,"id":220067,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brookins, D. G.","contributorId":93963,"corporation":false,"usgs":true,"family":"Brookins","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":220068,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":38564,"text":"pp1299AB - 1984 - Igneous activity and related ore deposits in the western and southern Tushar Mountains, Marysvale volcanic field, west-central Utah","interactions":[{"subject":{"id":8489,"text":"ofr82479 - 1982 - Multiple episodes of igneous activity, mineralization, and alteration in the western Tushar Mountains, Utah","indexId":"ofr82479","publicationYear":"1982","noYear":false,"title":"Multiple episodes of igneous activity, mineralization, and alteration in the western Tushar Mountains, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":38564,"text":"pp1299AB - 1984 - Igneous activity and related ore deposits in the western and southern Tushar Mountains, Marysvale volcanic field, west-central Utah","indexId":"pp1299AB","publicationYear":"1984","noYear":false,"chapter":"A,B","title":"Igneous activity and related ore deposits in the western and southern Tushar Mountains, Marysvale volcanic field, west-central Utah"},"id":1},{"subject":{"id":11337,"text":"ofr79527 - 1979 - Uranium potential of the Big John Caldera, Beaver County, Utah","indexId":"ofr79527","publicationYear":"1979","noYear":false,"title":"Uranium potential of the Big John Caldera, Beaver County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":38564,"text":"pp1299AB - 1984 - Igneous activity and related ore deposits in the western and southern Tushar Mountains, Marysvale volcanic field, west-central Utah","indexId":"pp1299AB","publicationYear":"1984","noYear":false,"chapter":"A,B","title":"Igneous activity and related ore deposits in the western and southern Tushar Mountains, Marysvale volcanic field, west-central Utah"},"id":2}],"lastModifiedDate":"2025-08-22T18:57:39.424056","indexId":"pp1299AB","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1299","chapter":"A,B","title":"Igneous activity and related ore deposits in the western and southern Tushar Mountains, Marysvale volcanic field, west-central Utah","docAbstract":"PART A: Igneous activity in the Marysvale volcanic field of western Utah can be separated into many episodes of extrusion, intrusion, and hydrothermal activity. The rocks of the western Tushar Mountains, near the western part of the volcanic field, include intermediate-composition, calc-alkalic volcanic rocks erupted from scattered volcanoes in Oligocene through earliest Miocene time and related monzonitic intrusions emplaced 24-23 m.y. ago. Beginning 22-21 m.y. ago and extending through much of the later Cenozoic, a bimodal basalt-rhyolite assemblage was erupted widely throughout the volcanic field. Only volcanic and intrusive rocks belonging to the rhyolitic end member of this bimodal assemblage are present in the western Tushar Mountains; most of these rocks either fill the Mount Belknap caldera (19 m.y. old) or are part of the rhyolite of Gillies Hill (9---8 m.y. old). Episodic hydrothermal activity altered and mineralized rocks at many places in the western Tushar Mountains during Miocene time. The earliest activity took place in and adjacent to monzonitic calcalkalic intrusions emplaced in the vicinity of Indian Creek and Cork Ridge. These rocks were widely propylitized, and gold-bearing quartz-pyrite-carbonate veins formed in local fractures. Hydrothermal activity associated with the Mount Belknap caldera mobilized and redeposited uranium contained in the caldera-fill rocks and formed primary concentrations of lithophile elements (including molybdenum and uranium) in the vicinity of intrusive bodies. Hydrothermal activity associated with the rhyolite of Gillies Hill altered and mineralized rocks at several places along the fault zone that marks the western margin of the Tushar Mountains; the zoned alunite and gold deposits at Sheep Rock, the gold deposit at the Sunday Mine, and an alunite deposit near Indian Creek were thus produced. Resetting of isotopic ages suggests that another center of hydrothermally altered rocks associated with a buried pluton about 16 m.y. old may exist near Indian Creek just west of the Mount Belknap caldera. Geophysical evidence confirms the probability of a buried pluton near Indian Creek, and also indicates that another buried pluton probably exists beneath the 9-m.y.-old mineralized area at Sheep Rock. The mineral potential of the different hydrothermal systems, and the types of minerals deposited probably vary considerably from one period of mineralization to another and from one depth environment to another within a given system.
PART B: The Big John caldera, on the western flank of the Tushar Mountains in the Marysvale volcanic field in west-central Utah, formed 23-22 m.y. ago in response to ash-flow eruptions of the Delano Peak Tuff Member of the Bullion Canyon Volcanics. These eruptions were near the end of the period of Oligocene-early Miocene calc-alkalic igneous activity that built a broad volcanic plateau in this part of Utah. About 22 m.y. ago, the composition of rocks erupted changed to a bimodal assemblage of mafic and silicic volcanics that was erupted episodically through the remainder of Cenozoic time. The alkali rhyolites are uranium rich in part, and are associated with all the known uranium deposits in the Marysvale volcanic field. The Big John caldera was a broad drained basin whose floor was covered by a layer of stream gravels when ash flows from the western source area of the Mount Belknap Volcanics filled the caldera with the Joe Lott Tuff Member about 19 m.y. ago. Devitrified and zeolitized rocks in the caldera fill have lost one-quarter to one-half of the uranium contained in the original magma. This mobilized uranium probably moved into the hydrologic regime, and some may have been redeposited in stream gravels underlying the Joe Lott within the caldera, or in gravels filling the original drainage channel that extended south from the caldera.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1299AB","usgsCitation":"1984, Igneous activity and related ore deposits in the western and southern Tushar Mountains, Marysvale volcanic field, west-central Utah (Supercedes OFR 82-479 and OFR 79-527): U.S. Geological Survey Professional Paper 1299, 33 p., https://doi.org/10.3133/pp1299AB.","productDescription":"33 p.","costCenters":[],"links":[{"id":402244,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74533.htm","text":"Multiple episodes of igneous activity, mineralization, and alteration in the western Tushar Mountains, Utah","linkFileType":{"id":5,"text":"html"}},{"id":173143,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1299a-b/report-thumb.jpg"},{"id":65339,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1299a-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":494549,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74534.htm","text":"Geologic history and uranium potential of the Big John caldera, southern Tushar Mountains, Utah","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"Tushar Mountains, Marysvale volcanic field","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.54119873046875,\n 38.225235239076824\n ],\n [\n -112.25006103515625,\n 38.225235239076824\n ],\n [\n -112.25006103515625,\n 38.50948995925553\n ],\n [\n -112.54119873046875,\n 38.50948995925553\n ],\n [\n -112.54119873046875,\n 38.225235239076824\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Supercedes OFR 82-479 and OFR 79-527","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c72c","contributors":{"editors":[{"text":"Steven, Thomas A.","contributorId":57529,"corporation":false,"usgs":true,"family":"Steven","given":"Thomas A.","affiliations":[],"preferred":false,"id":749871,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":38567,"text":"pp1303 - 1984 - The Schultze granite, the Tea Cup granodiorite, and the Granite Basin porphyry: A geochemical comparison of mineralized and unmineralized stocks in southern Arizona","interactions":[],"lastModifiedDate":"2021-09-14T19:28:48.891796","indexId":"pp1303","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1303","title":"The Schultze granite, the Tea Cup granodiorite, and the Granite Basin porphyry: A geochemical comparison of mineralized and unmineralized stocks in southern Arizona","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1303","usgsCitation":"Creasey, S., 1984, The Schultze granite, the Tea Cup granodiorite, and the Granite Basin porphyry: A geochemical comparison of mineralized and unmineralized stocks in southern Arizona: U.S. Geological Survey Professional Paper 1303, Report: iii, 41 p.; 1 Plate: 16.82 × 14.07 iinches, https://doi.org/10.3133/pp1303.","productDescription":"Report: iii, 41 p.; 1 Plate: 16.82 × 14.07 iinches","costCenters":[],"links":[{"id":97391,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1303/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1303/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121994,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1303/report-thumb.jpg"},{"id":389229,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4793.htm"}],"country":"United States","state":"Arizona","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.29150390625,\n 33.1329513125159\n ],\n [\n -110.9344482421875,\n 33.1329513125159\n ],\n [\n -110.9344482421875,\n 33.47727218776036\n ],\n [\n -111.29150390625,\n 33.47727218776036\n ],\n [\n -111.29150390625,\n 33.1329513125159\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aa30","contributors":{"authors":[{"text":"Creasey, S.C.","contributorId":36109,"corporation":false,"usgs":true,"family":"Creasey","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":220080,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}