The Tulare Formation and other continental deposits of Pliocene to Holocene age crop out over most of the area near Kettleman City in the San Joaquin Valley of California. The deposits range in thickness from 0 to more than 4,000 feet and overlie the upper Mya zone of the San Joaquin Formation of Pliocene age. Some features of their base reflect structural deformation during Quaternary time. Many freshwater fossils occur in the Tulare Formation itself, including the largest fossil assemblage of clams and snails known on the Pacific Coast. Sediments in the Tulare Formation and other continental deposits consist mainly of unconsolidated deposits of clay, silt, sand, and gravel. Texture maps of the Tulare Formation and other continental deposits show the distribution, both laterally and vertically, of the coarse- and fine-grained sediment in the area. Such maps can be used by water managers for selecting areas for recharge and discharge operations and by ground-water modelers for assigning relative values of hydraulic conductivity and storage coefficient.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834000","usgsCitation":"Page, R.W., 1983, Geology of the Tulare Formation and other continental deposits, Kettleman City area, San Joaquin Valley, California, with a section on ground-water management considerations and use of texture maps: U.S. Geological Survey Water-Resources Investigations Report 83-4000, Report: iv, 24 p.; 2 Plates: 21.67 x 24.81 inches and 18.84 x 19.65 inches, https://doi.org/10.3133/wri834000.","productDescription":"Report: iv, 24 p.; 2 Plates: 21.67 x 24.81 inches and 18.84 x 19.65 inches","costCenters":[],"links":[{"id":411591,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35648.htm","linkFileType":{"id":5,"text":"html"}},{"id":57860,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4000/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57859,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4000/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57858,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4000/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118805,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4000/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Kettleman City area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.098,\n 36.158\n ],\n [\n -119.25,\n 36.158\n ],\n [\n -119.25,\n 35.5\n ],\n [\n -120.098,\n 35.5\n ],\n [\n -120.098,\n 36.158\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e40f","contributors":{"authors":[{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26841,"text":"wri824056 - 1983 - Geology of the \"20-foot\" clay and Gardiners clay in southern Nassau and southwestern Suffolk counties, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri824056","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4056","title":"Geology of the \"20-foot\" clay and Gardiners clay in southern Nassau and southwestern Suffolk counties, Long Island, New York","docAbstract":"Data from 1978-79 drilling was compiled with information from previous reports and historical records to prepare surface contour and isopach maps of the ' 20-foot ' clay and Gardiners Clay in southern Nassau and southwestern Suffolk Counties. These units are major confining layers in the upper part of the groundwater reservoir along Long Island 's south shore. Where present, they influence the groundwater flow patterns locally. The ' 20-foot ' clay, previously mapped in Nassau County only, was found in test borings in Suffolk County also. Its surface altitude ranges from 20 to 40 ft below NGVD (National Geodetic Vertical Datum of 1929); thickness ranges from 0 to 30 ft. The surface altitude of the Gardiners Clay ranges from 40 to 120 ft below NGVD; thickness ranges from 0 to 90 ft. Previously known discontinuities in both formations are more accurately delineated, and several new discontinuities have been inferred from the new data. The Matawan Group-Magothy Formation undifferentiated the Monmouth Group, and the Jameco Gravel directly underlie the Gardiners Clay. Revised surface altitudes of these formations are depicted on maps and cross sections of the south-shore area. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824056","usgsCitation":"Doriski, T., and Wilde-Katz, F., 1983, Geology of the \"20-foot\" clay and Gardiners clay in southern Nassau and southwestern Suffolk counties, Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 82-4056, iv, 21 p. :maps ;28 cm., https://doi.org/10.3133/wri824056.","productDescription":"iv, 21 p. :maps ;28 cm.","costCenters":[],"links":[{"id":123765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4056/report-thumb.jpg"},{"id":55724,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4056/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55725,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4056/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55726,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4056/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55727,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4056/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55728,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4056/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55729,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4056/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55730,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4056/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55731,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4056/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55732,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db6808e7","contributors":{"authors":[{"text":"Doriski, T.P.","contributorId":108150,"corporation":false,"usgs":true,"family":"Doriski","given":"T.P.","affiliations":[],"preferred":false,"id":197101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilde-Katz, Franceska","contributorId":71587,"corporation":false,"usgs":true,"family":"Wilde-Katz","given":"Franceska","email":"","affiliations":[],"preferred":false,"id":197100,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28692,"text":"wri834016 - 1983 - Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri834016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4016","title":"Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico","docAbstract":"Geohydrologic data have been collected in the Los Medanos area at the U.S. Department of Energy 's proposed Waste Isolation Pilot Plant (WIPP) site in southeastern New Mexico since 1975 as part of an intensive study evaluating the feasibility of storing defense-associated nuclear wastes within the bedded salt of the Salado Formation of Permian age. Drilling and hydrologic testing have identified three principal water-producing zones above the salt, including the Rustler-Salado Formational contact and the Culebra and Magenta Dolomite Members of the Permian Rustler Formation. Below the bedded salt there is another water-bearing zone, the channel sandstones of the Bell Canyon formation of the Permian Delaware Mountain Group. Most data collected from 33 hydrologic test holes indicate that the water-bearing zones are characterized by low transmissivities and contain slightly saline to briny water. Data collected from drill-stem tests in the Bell Canyon Formation indicate the channel sandstones have hydraulic conductivities ranging from 0.02 to 0.36 feet per day grade vertically and laterally into siltstones and shales of very low permeability. The Rustler Formation contains the principal water-producing zones identified at the WIPP site. The Rustler-Salado formational contact has the least transmissivity, ranging from 0.00003 to 0.003 feet squared per day. The Culebra Dolomite is the most productive unit at the WIPP site with transmissivities ranging from 0.001 to 73 feet squared per day; the greater values result from fracturing in the dolomite created by dissolution of underlying halite. Minute vertical permeabilities prevent movement of water between hydrologic units. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834016","usgsCitation":"Mercer, J.W., 1983, Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 83-4016, viii, 121 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834016.","productDescription":"viii, 121 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4016/report-thumb.jpg"},{"id":57535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4016/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8824","contributors":{"authors":[{"text":"Mercer, Jerry W.","contributorId":32534,"corporation":false,"usgs":true,"family":"Mercer","given":"Jerry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18409,"text":"ofr8324 - 1983 - Two newly discovered submarine canyons on Alaskan continental margin of Bering Sea","interactions":[],"lastModifiedDate":"2021-11-19T21:16:27.102062","indexId":"ofr8324","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-24","title":"Two newly discovered submarine canyons on Alaskan continental margin of Bering Sea","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8324","usgsCitation":"Carlson, P.R., Fischer, J., and Karl, H., 1983, Two newly discovered submarine canyons on Alaskan continental margin of Bering Sea: U.S. Geological Survey Open-File Report 83-24, Report: 37 p.; 1 Plate: 28.97 × 42.01 inches, https://doi.org/10.3133/ofr8324.","productDescription":"Report: 37 p.; 1 Plate: 28.97 × 42.01 inches","costCenters":[],"links":[{"id":47747,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0024/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47746,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0024/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151217,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0024/report-thumb.jpg"},{"id":391951,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13950.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -178,\n 59.25\n ],\n [\n -175.25,\n 59.25\n ],\n [\n -175.25,\n 57.10\n ],\n [\n -178,\n 57.10\n ],\n [\n -178,\n 59.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623aba","contributors":{"authors":[{"text":"Carlson, Paul R.","contributorId":81469,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":179071,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fischer, Jeffrey M. 0000-0003-2996-9272 fischer@usgs.gov","orcid":"https://orcid.org/0000-0003-2996-9272","contributorId":573,"corporation":false,"usgs":true,"family":"Fischer","given":"Jeffrey M.","email":"fischer@usgs.gov","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":false,"id":179069,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Karl, Herman A.","contributorId":55796,"corporation":false,"usgs":true,"family":"Karl","given":"Herman A.","affiliations":[],"preferred":false,"id":179070,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10564,"text":"ofr821013 - 1983 - Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","interactions":[{"subject":{"id":10564,"text":"ofr821013 - 1983 - Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","indexId":"ofr821013","publicationYear":"1983","noYear":false,"title":"Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":2420,"text":"wsp2227 - 1987 - Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico","indexId":"wsp2227","publicationYear":"1987","noYear":false,"title":"Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico"},"id":1}],"supersededBy":{"id":2420,"text":"wsp2227 - 1987 - Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico","indexId":"wsp2227","publicationYear":"1987","noYear":false,"title":"Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico"},"lastModifiedDate":"2022-09-07T15:44:24.905824","indexId":"ofr821013","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-1013","title":"Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","docAbstract":"An evaluation of the water resources of the Zuni Tribal lands in west-central New Mexico was made to determine the yield, variability, and quality of water available to the Pueblo of Zuni. This study is needed to aid in orderly development of these resources.
Rocks of Permian to Quaternary age supply stock, irrigation, and domestic water to the Zuni Indians. The Glorieta Sandstone and San Andres Limestone (Glorieta-San Andres aquifer) of Permian age and sandstones in the Chinle Formation of Triassic age provide most of this water supply.
Water in the Glorieta-San Andres aquifer is confined by minimal-permeability shales and is transmitted through the aquifer along interconnected solution channels and fractures. Water-level and water-quality information indicate greater hydraulic conductivities along the southern boundaries of Zuni Tribal lands.
Well yields from the Glorieta-San Andres aquifer are as much as 150 gallons per minute and aquifer transmissivity ranges from 30 to 1,400 feet squared per day. Long-term, water-level declines of as much as 29 feet have been measured near pumping centers at Black Rock. Multiple-well aquifer tests are needed to further define aquifer properties (storage, transmissivity, and leakage from confining units) and the effects of well design on well yields. Dissolved-solids concentrations in water from the aquifer ranged from 331 to 1,068 milligrams per liter. Calcium and sulfate are the predominant ions.
Water in sandstones of the Chinle Formation is confined by adjacent shales and is transmitted along interconnected fractures. Well yields range from 5 to 125 gallons per minute and aquifer transmissivity ranges from 40 to 1,400 feet squared per day. Water-level declines of as much as 27 feet have been measured near Zuni Village. Dissolved-solids concentrations in water from the aquifer ranged from 215 to 1,980 milligrams per liter. Sodium and bicarbonate are the predominant ions.
Other sources of ground water are used primarily for livestock watering by means of windmills, with the exception of buried alluvial channel deposits along the Rio Pescado. These deposits provide domestic and irrigation water through springs and wells to Pescado and Black Rock.
The Bidahochi Formation of Miocene and Pliocene age could potentially provide an additional supply of water chemically suitable for most uses. Seismic-reflection techniques are being used to locate buried channels eroded in the rocks underlying the Bidahochi Formation. These buried channels may contain thicker sections of saturated sands and gravels that could be developed for stock and domestic use.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821013","collaboration":"Prepared in cooperation with the Pueblo of Zuni","usgsCitation":"Orr, B.R., 1983, Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico: U.S. Geological Survey Open-File Report 82-1013, Report: 179 p.; 2 Plates: 23.21 x 19.52 inches and 20.83 x 30.61 inches, https://doi.org/10.3133/ofr821013.","productDescription":"Report: 179 p.; 2 Plates: 23.21 x 19.52 inches and 20.83 x 30.61 inches","costCenters":[],"links":[{"id":406315,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1013/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406314,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1013/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406313,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1013/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1013/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Cibola County, McKinley County","otherGeospatial":"Zuni Tribal Lands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.061279296875,\n 34.134541681937364\n ],\n [\n -107.0068359375,\n 34.134541681937364\n ],\n [\n -107.0068359375,\n 35.96022296929667\n ],\n [\n -109.061279296875,\n 35.96022296929667\n ],\n [\n -109.061279296875,\n 34.134541681937364\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f03be","contributors":{"authors":[{"text":"Orr, Brennon R.","contributorId":18747,"corporation":false,"usgs":true,"family":"Orr","given":"Brennon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10588,"text":"ofr83762 - 1983 - January 1983 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr83762","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-762","title":"January 1983 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"Water-level measurements were made, mostly in January 1983, in about 1,540 wells in western and south-central Kansas. The measurements were made in mid-winter when pumping was minimal and water levels had recovered, for the most part, from the effects of pumping during the previous irrigation season. Annual hydrologic data are provided for relating water-level changes from a ' base-reference year ' (predevelopment year), a year of abnormally high rainfall and minimum pumpage (1966 or 1974) and each of seen consecutive years of measurement (1977-83). The ' base-reference year ' is designated as 1940 for the southwestern area, 1944 for the south-central area, and 1950 for the northwestern and west-central areas. Water levels for the ' base-reference year ' are established by measurements made during that year and by interpretation of maps showing water-level altitudes. Data also are provided for relating the average annual water-level changes, saturated thicknesses of the deposits, and percentage changes in saturated thicknesses. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83762","usgsCitation":"Pabst, M.E., 1983, January 1983 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 83-762, iv, 168 p. :maps ;28 cm., https://doi.org/10.3133/ofr83762.","productDescription":"iv, 168 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0762/report-thumb.jpg"},{"id":38414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0762/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fe6","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161638,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10272,"text":"ofr83286 - 1983 - A hydrogeochemical survey in east-central Nevada","interactions":[],"lastModifiedDate":"2022-07-22T21:20:44.950179","indexId":"ofr83286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-286","title":"A hydrogeochemical survey in east-central Nevada","docAbstract":"A hydrogeochemical survey utilizing waters from springs and wells was conducted in east-central Nevada. None of the trace elements commonly associated with mineralization were found to be highly anomalous in the study area. Slightly anomalous values for some elements were found in the southern valleys of the study area and in a few scattered areas that contained old mines. Data from this study revealed no new areas of significant mineralization.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83286","usgsCitation":"McHugh, J., Miller, W.R., and Ficklin, W.H., 1983, A hydrogeochemical survey in east-central Nevada: U.S. Geological Survey Open-File Report 83-286, i, 28 p., https://doi.org/10.3133/ofr83286.","productDescription":"i, 28 p.","costCenters":[],"links":[{"id":404396,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13966.htm","linkFileType":{"id":5,"text":"html"}},{"id":38129,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0286/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0286/report-thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.49,\n 37.874\n ],\n [\n -114,\n 37.874\n ],\n [\n -114,\n 38.5\n ],\n [\n -114.49,\n 38.5\n ],\n [\n -114.49,\n 37.874\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae468","contributors":{"authors":[{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":161115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. Roger","contributorId":60191,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"Roger","affiliations":[],"preferred":false,"id":161114,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ficklin, Walter H.","contributorId":52565,"corporation":false,"usgs":true,"family":"Ficklin","given":"Walter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161113,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10260,"text":"ofr83396 - 1983 - Seismic-reflection data collected in the Baltimore Canyon and Cape Hatteras areas during 1982, Gyre cruise 82-G-10B","interactions":[],"lastModifiedDate":"2024-11-25T22:57:27.956903","indexId":"ofr83396","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-396","title":"Seismic-reflection data collected in the Baltimore Canyon and Cape Hatteras areas during 1982, Gyre cruise 82-G-10B","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83396","usgsCitation":"McGregor, B.A., 1983, Seismic-reflection data collected in the Baltimore Canyon and Cape Hatteras areas during 1982, Gyre cruise 82-G-10B: U.S. Geological Survey Open-File Report 83-396, 5 p., https://doi.org/10.3133/ofr83396.","productDescription":"5 p.","costCenters":[],"links":[{"id":143135,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0396/report-thumb.jpg"},{"id":368900,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0396/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":464510,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14008.htm","text":"Baltimore Canyon","linkFileType":{"id":5,"text":"html"}},{"id":464511,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14009.htm","text":"Cape Hatteras","linkFileType":{"id":5,"text":"html"}}],"country":"United States","otherGeospatial":"Baltimore Canyon, Cape Hatteras","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.514543627322,\n 38.37922375578077\n ],\n [\n -75.60111811259628,\n 38.37922375578077\n ],\n [\n -75.60111811259628,\n 35.36603278137427\n ],\n [\n -74.514543627322,\n 35.36603278137427\n ],\n [\n -74.514543627322,\n 38.37922375578077\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb627","contributors":{"authors":[{"text":"McGregor, Bonnie A.","contributorId":61022,"corporation":false,"usgs":true,"family":"McGregor","given":"Bonnie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161091,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10254,"text":"ofr83817 - 1983 - $ANBA; a rapid, combined data acquisition and correction program for the SEMQ electron microprobe","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr83817","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-817","title":"$ANBA; a rapid, combined data acquisition and correction program for the SEMQ electron microprobe","docAbstract":"$ANBA is a program developed for rapid data acquisition and correction on an automated SEMQ electron microprobe. The program provides increased analytical speed and reduced disk read/write operations compared with the manufacturer's software, resulting in a doubling of analytical throughput. In addition, the program provides enhanced analytical features such as averaging, rapid and compact data storage, and on-line plotting. The program is described with design philosophy, flow charts, variable names, a complete program listing, and system requirements. A complete operating example and notes to assist in running the program are included.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83817","usgsCitation":"McGee, J.J., 1983, $ANBA; a rapid, combined data acquisition and correction program for the SEMQ electron microprobe: U.S. Geological Survey Open-File Report 83-817, i, 47 p. ill. ;28 cm., https://doi.org/10.3133/ofr83817.","productDescription":"i, 47 p. ill. ;28 cm.","costCenters":[],"links":[{"id":143112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0817/report-thumb.jpg"},{"id":38118,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0817/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4901e4b0b290850eecd5","contributors":{"authors":[{"text":"McGee, James J.","contributorId":46535,"corporation":false,"usgs":true,"family":"McGee","given":"James","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161082,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47671,"text":"wri834058 - 1983 - Shallow ground water in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado, 1975-77","interactions":[],"lastModifiedDate":"2022-12-05T21:04:03.995944","indexId":"wri834058","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4058","title":"Shallow ground water in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado, 1975-77","docAbstract":"Shallow ground water may limit the location of construction and excavation projects in parts of the Front Range Urban Corridor. A shallow water table occurs from 0 to 50 feet below the land surface principally in the alluvial deposits along the streams and rivers in the Boulder-Fort Collins-Greeley area. This shallow water table underlies approximately 400 square miles and is maintained by natural recharge within the South Platte River basin and by the infiltration of irrigation water that is diverted into the basin from streams and reservoirs in the Colorado and the Laramie River basins. Return flow from irrigation, which is mostly ground water, helps maintain the flow of the South Platte River and its tributaries. The report includes a map from which depth to water table and the direction of ground-water movement can be determined. The map, compiled on a topographic base, shows the areal extent of the saturated materials and the altitude and configuration of the ground-water surface. The water-table contour map was prepared using data from approximately 400 wells. Monitoring of shallow ground-water within the study area shows depths to water have changed only slightly over the last 20 years, except for some seasonal and drought-related fluctuations. Gradients, computed from ground-water measurements, range from 27.7 feet per mile in Lone Tree-Spring Creek valley to 10.3 feet per mile in the South Platte River valley. The shallow ground-water underflow from the major tributaries in the basin is about 29,000 acre-feet per year, and underflow calculated at a cross section near Kersey is about 12,000 acre-feet per year.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834058","usgsCitation":"Schneider, P.A., 1983, Shallow ground water in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado, 1975-77: U.S. Geological Survey Water-Resources Investigations Report 83-4058, 1 Plate: 41.96 × 31.86 inches, https://doi.org/10.3133/wri834058.","productDescription":"1 Plate: 41.96 × 31.86 inches","costCenters":[],"links":[{"id":161788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410064,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35694.htm","linkFileType":{"id":5,"text":"html"}},{"id":84582,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4058/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","city":"Boulder, Fort Collins, Greeley","otherGeospatial":"Front Range urban corridor","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.46470339334677,\n 40.68848809489273\n ],\n [\n -105.46470339334677,\n 39.92665986663209\n ],\n [\n -104.58735150676397,\n 39.92665986663209\n ],\n [\n -104.58735150676397,\n 40.68848809489273\n ],\n [\n -105.46470339334677,\n 40.68848809489273\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f420a","contributors":{"authors":[{"text":"Schneider, Paul A. Jr.","contributorId":50183,"corporation":false,"usgs":true,"family":"Schneider","given":"Paul","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":235982,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38630,"text":"pp1049D - 1983 - Geology and description of thorium and rare-earth deposits in the southern Bear Lodge Mountains, northeastern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:36","indexId":"pp1049D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1049","chapter":"D","title":"Geology and description of thorium and rare-earth deposits in the southern Bear Lodge Mountains, northeastern Wyoming","docAbstract":"The Bear Lodge Mountains are a small northerly trending range approximately 16 km northwest of the Black Hills in the northeast corner of Wyoming. Thorium and rare-earth deposits occur over an area of 16 km 2 in the southern part of these mountains. These deposits occur in the core of the Bear Lodge dome in a large multiple intrusive body made up principally of trachyte and phonolite. Two types of deposits are recognized: disseminated deposits and veins. \r\n\r\nThe disseminated deposits are made up of altered igneous rocks cut by numerous crisscrossing veinlets. The disseminated deposits contain thorium and rare-earth minerals in a matrix consisting principally of potassium feldspar, quartz, and iron and manganese oxides. Total rare-earth content of these deposits is about 27 times that of the thorium content. \r\n\r\nThe general size and shape of the disseminated deposits were outlined by making a radiometric map using a scintillation counter of the entire Bear Lodge core, an area of approximately 30 km 2 . The most favorable part of this area, which was outlined by the 40 countJs (count-per-second) isograd on the radiometric map, was sampled in detail. A total of 341 samples were taken over an area of 10.6 km 2 and analyzed for as many as 60 elements. Rare earths and thorium are the principal commodities of interest in these deposits. Total rare-earth content of these samples ranged from 47 to 27,145 ppm (parts per million), and the thorium content from 9.3 to 990 ppm. The amount of total rare earths of individual samples shows little correlation with that of thorium. Contour maps were constructed using the analytical data for total rare earths, thorium, uranium, and potassium. The total rare-earth and thorium maps can be used to define the size of the deposits based on what cut-off grade may be needed during mining. The size is large as the 2,000 ppm total rare-earth isograd encloses several areas that total 3.22 km 2 in size, and the 200 ppm thorium isograd encloses several areas that total 1.69 km 2 . These deposits could be mined by open pit. The Bear Lodge disseminated deposits have one of the largest resources of both total rare earths and thorium in the United States, and although the grade of both commodities is lower than some other deposits, their large size and relative cheapness of mining make them an important future resource. \r\n\r\nVein deposits in the Bear Lodge Mountains include all tabular bodies at least 5 cm thick. Twenty-six veins were noted in this area. These veins are thin and short; the longest vein was traced for only 137 m. Minerals vary greatly in the amount present. Gangue minerals are commonly potassium feldspar, quartz, or cristobalite intermixed with varying amounts of limonite, hematite, and various manganese oxides. Rare earths and thorium occur in the minerals monazite, brockite, and bastnaesite. Thorium content of 35 samples ranged from 0.01 to 1.2 percent, and the total rare-earth content of 21 samples from 0.23 to 9.8 percent. Indicated reserves were calculated to a depth of one-third the exposed length of the vein. Inferred reserves lie in a block surrounding indicated reserves. Indicated reserves of all veins are only 50 t of Th0 2 and 1,360 t of total rare-earth oxides; inferred reserves are 250 t of Th0 2 and 6,810 t of total rare-earth oxides. \r\n\r\nThe Bear Lodge dome, which underlies the greater part of this area, is formed by multiple intrusive bodies of Tertiary age that dome up the surrounding sedimentary rocks. In the southern part of the core, the younger intrusive bodies surround and partly replace a granite of Precambrian age. This granite is approximately 2.6 b.y. old. The sedimentary rocks around the core are (from oldest to youngest): Deadwood Formation of Late Cambrian and Early Ordovician age, Whitewood Limestone of Late Ordovician age, Pahasapa Limestone of Early Mississippian age, Minnelusa Sandstone of Pennsylvanian and Early Permian age, Opeche Formation of Permian age, Minnek","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology and resources of thorium in the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp1049D","usgsCitation":"Staatz, M., 1983, Geology and description of thorium and rare-earth deposits in the southern Bear Lodge Mountains, northeastern Wyoming: U.S. Geological Survey Professional Paper 1049, p. D1-D52; 2 plates in pocket, https://doi.org/10.3133/pp1049D.","productDescription":"p. D1-D52; 2 plates in pocket","costCenters":[],"links":[{"id":104542,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4702.htm","linkFileType":{"id":5,"text":"html"},"description":"4702"},{"id":120497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1049d/report-thumb.jpg"},{"id":65454,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1049d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65455,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1049d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65456,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1049d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686276","contributors":{"authors":[{"text":"Staatz, M.H.","contributorId":14411,"corporation":false,"usgs":true,"family":"Staatz","given":"M.H.","affiliations":[],"preferred":false,"id":220190,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19153,"text":"ofr83733 - 1983 - Analytical results and sample locality maps for stream-sediment, oxalic-acid-leachate, panned-concentrate, and rock samples from the Kalmiopsis Wilderness, Curry and Josephine Counties, Oregon","interactions":[],"lastModifiedDate":"2022-08-17T21:25:10.872563","indexId":"ofr83733","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-733","title":"Analytical results and sample locality maps for stream-sediment, oxalic-acid-leachate, panned-concentrate, and rock samples from the Kalmiopsis Wilderness, Curry and Josephine Counties, Oregon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83733","usgsCitation":"Grimes, D.J., Leinz, R.W., and Speckman, W.S., 1983, Analytical results and sample locality maps for stream-sediment, oxalic-acid-leachate, panned-concentrate, and rock samples from the Kalmiopsis Wilderness, Curry and Josephine Counties, Oregon: U.S. Geological Survey Open-File Report 83-733, Report: 95 p.; 2 Plates: 27.78 × 40.49 inches and 28.43 × 40.19 inches, https://doi.org/10.3133/ofr83733.","productDescription":"Report: 95 p.; 2 Plates: 27.78 × 40.49 inches and 28.43 × 40.19 inches","costCenters":[],"links":[{"id":405286,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14200.htm","linkFileType":{"id":5,"text":"html"}},{"id":48624,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0733/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48623,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0733/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48622,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0733/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151532,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0733/report-thumb.jpg"}],"country":"United States","state":"Oregon","county":"Curry County, Josephine County","otherGeospatial":"Kaliopsis Wilderness","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.167,\n 42.467\n ],\n [\n -123.767,\n 42.467\n ],\n [\n -123.767,\n 43.017\n ],\n [\n -124.167,\n 43.017\n ],\n [\n -124.167,\n 42.467\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e413","contributors":{"authors":[{"text":"Grimes, D. J.","contributorId":73575,"corporation":false,"usgs":true,"family":"Grimes","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":180403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leinz, R. W.","contributorId":89885,"corporation":false,"usgs":true,"family":"Leinz","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":180404,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Speckman, W. S.","contributorId":105296,"corporation":false,"usgs":true,"family":"Speckman","given":"W.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":180405,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":41056,"text":"ofr83310 - 1983 - Preliminary chart of stratigraphic nomenclature of Paleocene and Eocene lignite-bearing and associated strata of the Gulf Coast Plain-Mississippi Embayment","interactions":[],"lastModifiedDate":"2012-02-02T00:10:53","indexId":"ofr83310","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-310","title":"Preliminary chart of stratigraphic nomenclature of Paleocene and Eocene lignite-bearing and associated strata of the Gulf Coast Plain-Mississippi Embayment","language":"ENGLISH","doi":"10.3133/ofr83310","usgsCitation":"Hackman, B.S., and Meissner, C.R., 1983, Preliminary chart of stratigraphic nomenclature of Paleocene and Eocene lignite-bearing and associated strata of the Gulf Coast Plain-Mississippi Embayment: U.S. Geological Survey Open-File Report 83-310, 1 chart ;76 x 117 cm., https://doi.org/10.3133/ofr83310.","productDescription":"1 chart ;76 x 117 cm.","costCenters":[],"links":[{"id":172213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78926,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0310/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c77e","contributors":{"authors":[{"text":"Hackman, Bettie S.","contributorId":83187,"corporation":false,"usgs":true,"family":"Hackman","given":"Bettie","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":224403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meissner, Charles R. 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1983 - Residual aeromagnetic map of the Hat Mountain Quadrangle, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:10:30","indexId":"ofr83292","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-292","title":"Residual aeromagnetic map of the Hat Mountain Quadrangle, Arizona","language":"ENGLISH","doi":"10.3133/ofr83292","usgsCitation":"Klein, D.P., 1983, Residual aeromagnetic map of the Hat Mountain Quadrangle, Arizona: U.S. Geological Survey Open-File Report 83-292, 1 map :photocopy ;45 x 38 cm., https://doi.org/10.3133/ofr83292.","productDescription":"1 map :photocopy ;45 x 38 cm.","costCenters":[],"links":[{"id":173351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80404,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0292/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b9df","contributors":{"authors":[{"text":"Klein, Douglas P.","contributorId":50896,"corporation":false,"usgs":true,"family":"Klein","given":"Douglas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":226853,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41054,"text":"ofr83624D - 1983 - Preliminary chart D-D' showing electric log correlation, facies, and test data of some Cretaceous and Tertiary rocks, Wind River basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:53","indexId":"ofr83624D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-624","chapter":"D","title":"Preliminary chart D-D' showing electric log correlation, facies, and test data of some Cretaceous and Tertiary rocks, Wind River basin, Wyoming","language":"ENGLISH","doi":"10.3133/ofr83624D","usgsCitation":"Fox, J.E., and Priestley, R.L., 1983, Preliminary chart D-D' showing electric log correlation, facies, and test data of some Cretaceous and Tertiary rocks, Wind River basin, Wyoming: U.S. Geological Survey Open-File Report 83-624, 5 well logs on 1 sheet :photocopy ;sheet 337 x 108 cm., https://doi.org/10.3133/ofr83624D.","productDescription":"5 well logs on 1 sheet :photocopy ;sheet 337 x 108 cm.","costCenters":[],"links":[{"id":172211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20955,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0624d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c779","contributors":{"authors":[{"text":"Fox, J. 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The peat #s chiefly sphagnum moss with some reed-sedge of high quality according to ASTM standards for agricultural and horticultural use. This same volume of peat may be considered for use as fuel because BTO per pound ranges from 8,600 to 10,500 with low sulfur and high hydrogen contents.","language":"ENGLISH","doi":"10.3133/ofr834","usgsCitation":"Cameron, C.C., and Mullen, M., 1983, Surficial geology map of the Great Heath, Washington County, Maine: U.S. Geological Survey Open-File Report 83-4, 1 map ;41 x 47 cm. +1 text (26 p. ; 28 cm.), https://doi.org/10.3133/ofr834.","productDescription":"1 map ;41 x 47 cm. +1 text (26 p. ; 28 cm.)","costCenters":[],"links":[{"id":170542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0004/report-thumb.jpg"},{"id":81493,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0004/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81494,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0004/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688ae6","contributors":{"authors":[{"text":"Cameron, Cornelia Clermont","contributorId":20737,"corporation":false,"usgs":true,"family":"Cameron","given":"Cornelia","email":"","middleInitial":"Clermont","affiliations":[],"preferred":false,"id":229166,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mullen, Michael K.","contributorId":9257,"corporation":false,"usgs":true,"family":"Mullen","given":"Michael K.","affiliations":[],"preferred":false,"id":229165,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42171,"text":"ofr8360 - 1983 - Aeromagnetic map of the Sangre de Cristo Mountains, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:10:29","indexId":"ofr8360","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-60","title":"Aeromagnetic map of the Sangre de Cristo Mountains, Colorado","language":"ENGLISH","doi":"10.3133/ofr8360","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Aeromagnetic map of the Sangre de Cristo Mountains, Colorado: U.S. Geological Survey Open-File Report 83-60, 1 map ;180 x 106 cm., on 3 sheets 108 x 93 cm. or smaller., https://doi.org/10.3133/ofr8360.","productDescription":"1 map ;180 x 106 cm., on 3 sheets 108 x 93 cm. or smaller.","costCenters":[],"links":[{"id":173346,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79906,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0060/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79907,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0060/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79908,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0060/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691320","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":530884,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48799,"text":"ofr8353 - 1983 - Preliminary report on near-surface lignite occurrences, Cleveland County, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"ofr8353","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-53","title":"Preliminary report on near-surface lignite occurrences, Cleveland County, Arkansas","docAbstract":"Four cross sections were constructed from lithologic descriptions of 43 drill holes in Cleveland County, Ark., in order to illustrate the occurrence of lignite and to relate the lignite beds to the regional stratigraphic framework. Of 43 holes drilled, 8 contained beds of lignite, but only two had beds greater than 30 in. thick. These beds are apparently lenticular and are restricted to the upper 60 ft. of the Cockfield Formation of the Claiborne Group of Middle Eocene age. The Cockfield Formation is at or near the surface west of the Saline River.","language":"ENGLISH","doi":"10.3133/ofr8353","usgsCitation":"Heermann, S.E., 1983, Preliminary report on near-surface lignite occurrences, Cleveland County, Arkansas: U.S. Geological Survey Open-File Report 83-53, 9 p., 5 over-size sheets, https://doi.org/10.3133/ofr8353.","productDescription":"9 p., 5 over-size sheets","costCenters":[],"links":[{"id":169780,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0053/report-thumb.jpg"},{"id":85629,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0053/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85630,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0053/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85631,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0053/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85632,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0053/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85627,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0053/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85628,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0053/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cacc","contributors":{"authors":[{"text":"Heermann, Stephen E.","contributorId":97969,"corporation":false,"usgs":true,"family":"Heermann","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":238282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37153,"text":"rp151 - 1983 - Avian use of forest habitats in the Pembina Hills of northeastern North Dakota","interactions":[],"lastModifiedDate":"2016-11-16T13:33:48","indexId":"rp151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"151","title":"Avian use of forest habitats in the Pembina Hills of northeastern North Dakota","docAbstract":"North Dakota has the least extensive total area of forested habitats of any of the 50 United States. Although occurring in limited area, forest communities add considerably to the total ecological diversity of the State. The forests of the Pembina Hills region in northeastern North Dakota are one of only three areas large enough to be considered of commercial value. During 1981 we studied the avifauna of the upper valley of the Pembina River in the Pembina Hills. Field work extended from 20 April to 23 July; breeding bird censuses were conducted 7 June to 2 July. Of the 120 bird species recorded during the study period, 79 species were recorded during the breeding season. The total breeding population was estimated at nearly 76,000 breeding pairs. The wood warblers (Parulidae) were the most numerous family, accounting for about 28,000 breeding pairs. The yellow warbler (Dendroica petechia) was the most abundant breeding species, making up 19.4% of the population. American redstart (Setophaga ruticilla) was second in abundance, accounting for 10.5% of the breeding population. Largest breeding densities occurred in the willow (Salix sp.) shrub community. Although supporting the lowest mean breeding density, quaking aspen (Populus tremuloides) forests supported the highest species diversity. First State breeding records were recorded for alder flycatcher (Empidonax alnorum) and golden-winged warbler (Vermivora chrysoptera). Records were obtained for 12 species considered rare or unusual in North Dakota during the breeding season. The status of all species known to have occurred in the study area is described in an annotated species list.
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