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,{"id":39591,"text":"pp813R - 1979 - Summary appraisals of the nation's ground-water resources – Lower Colorado region","interactions":[],"lastModifiedDate":"2021-12-14T21:44:27.647319","indexId":"pp813R","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"813","chapter":"R","title":"Summary appraisals of the nation's ground-water resources – Lower Colorado region","docAbstract":"<p>This report summarizes ground-water availability in the lower Colorado region and discusses the potential for greater ground-water development and increased efficiency of water use.</p>\n<p>The climate in the most highly developed southwestern part of the region is warm and dry and that in the northeastern part is cool and moist to dry. Although the regional average annual precipitation is only about 14 inches and most streambeds are dry during most of the year, about 1.5 billion acre-feet of ground water of moderate to good chemical quality is stored in aquifers of the region. Much of the water use is founded on pumped withdrawal of ground water. However, in most of the southwestern part of the region pumpage and consumptive use are in excess of replenishment, resulting in declining water levels. In the southwestern part of the region, water levels generally are from 200-500 feet below land surface and in large areas are less than 200 feet. Large-diameter water wells in this part of the region commonly produce 500-1 ,500 gallons per minute of water. In the northeastern part of the region, water levels generally are more than 500 feet below land surface, but in some large areas water levels are from 200-500 feet, and locally are less than 200 feet below the surface. In the northeastern part of the region, water wells generally have lower yields than those to the southwest. The yields range from a few to 2,000 gallons per minute, but most wells yield from 10 to less than 500 gallons per minute. In the southwestern part of the region about 1 billion acre-feet of ground water is recoverable from storage from the water table to a depth of 700 feet below the land surface. In the northeast about 150 million acre-feet can be recovered by dewatering a 100-foot-thick section of a typical aquifer (16 million-acre area). The estimated current annual rate of ground-water depletion, occurring almost entirely in the southwestern part of the region, is 2.4-3.2 million acre-feet per year. Almost 6 million acre-feet is pumped each year-about 90 percent for agriculture, 6 percent for public supply, and 3 percent for industrial use. The percentage of use for public supply and industry is increasing each year.</p>\n<p>The potential for greater development of ground water in the southwestern part of the region is constrained by land subsidence, earth cracks, increasing costs of pumping and transportation, and moderate to poor chemical quality of water. More ground water can be developed in the northeastern part of the region, where the major constraint is pumping cost owing to low to moderate well yields and depth to water. Some benefits can be realized everywhere in the region through changes in current use and greater efficiencies of use. Additional supplies may be made available by capture of natural evapotranspiration. Increasing the efficiency of use is possible hydrologically but, in the near term, is more expensive than increasing groundwater development. Decrease of irrigation, change to water-saving methods of irrigation, use of saline water, decrease of per capita public- supply use, and more reuse of water in almost every type of use could help extend the supply and thereby reduce the current rate of ground-water depletion. Financial problems have not yet caused an overall decrease in pumpage, but, locally, operating costs or partial dewatering of the aquifer has eliminated or decreased withdrawal. Current water laws in all States of the region, except Arizona, control or allocate the use of ground water.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813R","usgsCitation":"Davidson, E., 1979, Summary appraisals of the nation's ground-water resources – Lower Colorado region: U.S. Geological Survey Professional Paper 813, Report: v, 23 p.; 3 Plates: 31.50 x 38.65 inches or smaller, https://doi.org/10.3133/pp813R.","productDescription":"Report: v, 23 p.; 3 Plates: 31.50 x 38.65 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":392893,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5072.htm"},{"id":67177,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813r/plate-2.pdf","text":"Plate 2","size":"19.62 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,{"id":39590,"text":"pp813O - 1979 - Summary appraisals of the nation's ground-water resources– South Atlantic-Gulf region","interactions":[],"lastModifiedDate":"2021-12-09T22:02:45.374578","indexId":"pp813O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"813","chapter":"O","title":"Summary appraisals of the nation's ground-water resources– South Atlantic-Gulf region","docAbstract":"<p>Precipitation in the 270,000-square-mile South Atlantic-Gulf Region ranges from 44 to 80 inches, and the average runoff is about 15 inches. The ground-water discharge that forms the base flow of streams is conservatively estimated to be about 78,000 million gallons per day the equivalent of about 6 inches of precipitation. On this basis, the regional sustained ground-water supply is about 286,000 gallons per day per square mile. Projected water use through 2020 indicates that about 10 percent of the supply will meet the region's requirement for ground water.</p>\n<p>Enormous quantities of ground water are available in the South Atlantic-Gulf States in the extensive aquifers that underlie the Coastal Plain province. Large supplies of ground water can be developed also in places in the Cumberland Plateau and the Valley and Ridge provinces. In the Piedmont and Blue Ridge provinces ground water is available only in modest quantities.</p>\n<p>The principal Coastal Plain aquifers consist largely of deltaic sand and gravel deposits of Cretaceous to Quaternary age; however, a notable exception is the highly permeable Tertiary limestone aquifer, which underlies parts of four States. Ground water in the Blue Ridge and the Valley and Ridge provinces is available from openings along fissures and joints in consolidated rocks and from the unconsolidated sand and gravel in the residuum and alluvium that overlie the bedrock. In parts of these areas faulting and folding has created favorable conditions for the development of moderate supplies of ground water. In the Piedmont province modest quantities of water are available from joints and fractures. Solution cavities in massive limestone units in some areas underlying the Cumberland Plateau section yield very large quantities of ground water.</p>\n<p>Most of the major Coastal Plain aquifers are recharged where they are exposed and water moves downdip to the south. The general direction of ground-water movement in the Coastal Plain aquifers is seaward. There is, however, movement of water vertically and laterally that affects pressure and quality in every aquifer.</p>\n<p>Ground water of good chemical and physical quality is available generally except in a small area in western Alabama and eastern Mississippi and in some small coastal areas. Freshwater extends to depths of slightly more than 3,000 feet in some areas. In many areas, water can be produced that does not require any treatment for general use. The more common objectionable constituents or properties are excessive iron, fluoride, hardness, color, and acidity. Contamination or pollution of ground water is not a major regional problem, but it is significant in local areas. Many of these local problems of contamination were the result of earlier improper disposal of oil-field and industrial waste. Saltwater intrusion either directly from the sea or from estuaries has been reported in every State in the region, and the potential for the proliferation of this problem is very large.</p>\n<p>The relationship of ground water and surface water is significant at many places in the region where large ground-water withdrawals affect swamps, lakes, and the flow of streams and springs. There is a potential in some areas for using ground water during dry periods for low-flow augmentation of stream supplies. In other areas it is feasible to recharge ground-water reservoirs artificially by means of injection wells, pits, and water spreading.</p>\n<p>Although large water-level declines caused by withdrawals have occurred locally, water-level changes have been small or modest when considered on a regional basis owing to the abundant rainfall and favorable recharge conditions.</p>\n<p>The saline-water resources of the region are known to be extremely large. In some areas where the availability of freshwater is limited, saline ground water is available for desalinization to supplement freshwater supplies. Also, the saline aquifers are potential storage sites for injected freshwater.</p>\n<p>Ground-water problems generally are not severe. Critical situations are restricted to areas where large quantities of ground water are being withdrawn or where aquifers are contaminated by oil-field or industrial waste. Large withdrawals in coastal areas have caused some saltwater intrusion. In other localities, highly mineralized water may have migrated along fault zones to freshwater aquifers. Many of the present problems can be resolved or ameliorated by redistributing withdrawals or developing alternative water sources.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813O","usgsCitation":"Cedarstrom, D., Boswell, E.H., and Tarver, G.R., 1979, Summary appraisals of the nation's ground-water resources– South Atlantic-Gulf region: U.S. Geological Survey Professional Paper 813, vi, 35 p., https://doi.org/10.3133/pp813O.","productDescription":"vi, 35 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":392704,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5070.htm"},{"id":22045,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813o/report.pdf","text":"Report","size":"8.79 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H.","contributorId":38954,"corporation":false,"usgs":true,"family":"Boswell","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":221725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tarver, G. R.","contributorId":46160,"corporation":false,"usgs":true,"family":"Tarver","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":221726,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":36945,"text":"fwsobs77_02 - 1979 - Nesting and migration areas of birds of the U.S. Great Lakes","interactions":[],"lastModifiedDate":"2012-02-02T00:09:51","indexId":"fwsobs77_02","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"77/02","title":"Nesting and migration areas of birds of the U.S. Great Lakes","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Scharf, W.C., Chamberlain, M., Erdman, T., and Shugart, G., 1979, Nesting and migration areas of birds of the U.S. Great Lakes: FWS/OBS 77/02, 1 v.(various pagings) : ill., maps; 28 cm.","productDescription":"1 v.(various pagings) : ill., maps; 28 cm.","costCenters":[],"links":[{"id":165750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92228,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015012612399?urlappend=%3Bseq=141"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697c77","contributors":{"authors":[{"text":"Scharf, William C.","contributorId":96327,"corporation":false,"usgs":true,"family":"Scharf","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":217219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chamberlain, M.L.","contributorId":48231,"corporation":false,"usgs":true,"family":"Chamberlain","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":217216,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erdman, T.C.","contributorId":79438,"corporation":false,"usgs":true,"family":"Erdman","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":217218,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shugart, G.W.","contributorId":64708,"corporation":false,"usgs":true,"family":"Shugart","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":217217,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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,{"id":40314,"text":"ofr7981 - 1979 - Coal resource occurrence and coal development potential maps of the Box Elder Creek quadrangle, Powder River County, Montana","interactions":[],"lastModifiedDate":"2022-01-27T22:58:55.802357","indexId":"ofr7981","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-81","title":"Coal resource occurrence and coal development potential maps of the Box Elder Creek quadrangle, Powder River County, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7981","usgsCitation":"Colorado School of Mines, 1979, Coal resource occurrence and coal development potential maps of the Box Elder Creek quadrangle, Powder River County, Montana: U.S. Geological Survey Open-File Report 79-81, Report: iii, 22 p.; 16 Plates: 22.78 × 28.65 inches or smaller, https://doi.org/10.3133/ofr7981.","productDescription":"Report: iii, 22 p.; 16 Plates: 22.78 × 28.65 inches or smaller","costCenters":[],"links":[{"id":72353,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0081/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72352,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72351,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72350,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72349,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72348,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72347,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72346,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72345,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72344,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72343,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72342,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72341,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72340,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72339,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72338,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72337,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0081/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0081/report-thumb.jpg"},{"id":395029,"rank":19,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27643.htm"}],"country":"United States","state":"Montana","county":"Powder River County","otherGeospatial":"Box Elder Creek quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.75,\n              45.625\n            ],\n            [\n              -105.625,\n              45.625\n            ],\n            [\n              -105.625,\n              45.75\n            ],\n            [\n              -105.75,\n              45.75\n            ],\n            [\n              -105.75,\n              45.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b42bc","contributors":{"authors":[{"text":"Colorado School of Mines","contributorId":127904,"corporation":true,"usgs":false,"organization":"Colorado School of Mines","id":530120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39635,"text":"pp1067A - 1979 - Upper Cenozoic deposits of the central Delmarva Peninsula, Maryland and Delaware","interactions":[],"lastModifiedDate":"2012-02-02T00:09:55","indexId":"pp1067A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"1067","chapter":"A","title":"Upper Cenozoic deposits of the central Delmarva Peninsula, Maryland and Delaware","docAbstract":"The surface and shallow subsurface sediments of the lower Delmarva Peninsula include beds ranging in age from Miocene to Holocene. The oldest beds appear to be typical shelf deposits of the Chesapeake Group (Calvert-Choptank age). These marine units are overlain by deltaic deposits, which range from fluviatile facies in the north (Pensauken Formation) to marginal marine and marine beds in the south ('Yorktown(?) and Cohansey(?)' Formations as used by Rasmussen and Slaughter in 1955). This large deltaic mass underlies most of the Delmarva Peninsula. Fossil age determinations supplemented by some radiometric dates indicate the delta to be largely late Miocene in age. The nonmarine facies of the delta, the Pensauken Formation, previously was considered to be Pleistocene in age. \r\n\r\nThe late Miocene delta and possibly the Yorktown Formation (lower to middle Pliocene) are overlain by a feldspathic sand, the Beaverdam, which is at least in part marginal marine. Microflora recovered from this formation include species no longer indigenous to the Delmarva region ('exotics'). On the basis of existing information, microfloral assemblages containing 'exotics' are pre-Pleistocene in age. The Beaverdam therefore is pre-Pleistocene in age, probably late Pliocene. A highly dissected and weathered unit, the Walston Silt, caps the uplands of the central Delmarva Peninsula, where it overlies the Beaverdam. The Walston has a microflora containing 'exotics' and therefore is considered to be the youngest Tertiary unit (uppermost Pliocene) in this area. \r\n\r\nSediments forming a barrier-back-barrier sequence fringe most of the southern Maryland-Delaware part of the Delmarva Peninsula and are found at altitudes of as much as 15 m (50 ft) above sea level. This sequence, the Omar Formation, is Sangamon in age and has been dated radiometrically as 60,000 to about 100,000 years old. The microflora in these beds contains no 'exotics,' and the assemblage suggests a warm-temperate environment. The Omar represents the highest stand of the Quaternary seas in the Delmarva region. \r\n\r\nThe Ironshire and Kent Island Formations overlie or cut into the Omar Formation and are probably late Sangamon and middle Wisconsin, respectively, in age. Near Ocean City, the Ironshire forms a seaward-facing scarp with a toe nearly 4.5 m (15 ft) above sea level. A warm-temperate microfloral assemblage from the fluviatile-estuarine facies of the Ironshire Formation in the Delaware Bay region suggests that the formation is interglacial, probably late Sangamon in age. \r\n\r\nThe Ironshire and Omar Formations are overlain unconformably by the Sinepuxent Formation. The top of this marine unit is slightly above present sea level and has been dated by radiocarbon as about 30,000 years old or middle Wisconsin. The microflora from this formation is a cold to cool-temperate assemblage (high proportion of spruce pollen). The outer fringes of the Delmarva Peninsula are being overlapped by deposits of a Holocene marine transgression.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1067A","usgsCitation":"Owens, J.P., and Denny, C.S., 1979, Upper Cenozoic deposits of the central Delmarva Peninsula, Maryland and Delaware: U.S. Geological Survey Professional Paper 1067, p. A1-A28, https://doi.org/10.3133/pp1067A.","productDescription":"p. A1-A28","costCenters":[],"links":[{"id":125036,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1067a/report-thumb.jpg"},{"id":67295,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1067a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a23e4b07f02db60d3ad","contributors":{"authors":[{"text":"Owens, James Patrick","contributorId":105706,"corporation":false,"usgs":true,"family":"Owens","given":"James","email":"","middleInitial":"Patrick","affiliations":[],"preferred":false,"id":221859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Denny, Charles Storrow","contributorId":86331,"corporation":false,"usgs":true,"family":"Denny","given":"Charles","email":"","middleInitial":"Storrow","affiliations":[],"preferred":false,"id":221858,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39633,"text":"pp1067B - 1979 - The Parsonsburg Sand in the central Delmarva Peninsula, Maryland and Delaware","interactions":[],"lastModifiedDate":"2012-02-02T00:09:55","indexId":"pp1067B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"1067","chapter":"B","title":"The Parsonsburg Sand in the central Delmarva Peninsula, Maryland and Delaware","docAbstract":"The Parsonsburg Sand, a surface sand largely of Wisconsin age, caps terraces east of some of the major streams and mantles broad areas on the uplands of the central Delmarva Peninsula, Maryland and Delaware. The main body of the formation east and south of Salisbury, Md., ranges from 1.25 to 6.00 m (4-20 ft) in thickness and is a medium-grained moderately feldspathic sand containing a relatively mature heavy-mineral suite. The sand is either stratified or massive, and in some areas contains peaty sand and silt-clay, typically at or near the base of the formation. The organic matter ranges in radiocarbon age from about 30,000 to about 13,000 years B.P. and contains microfloral assemblages suggesting that at the time the sand was deposited the climate was cooler and drier that it is at present. The region may have been a pine-birch barrens in which were small ponds, spruce bogs, and abundant shrubs. The distribution of the sand at or near the position of high stands of the Sangamon sea suggests that the Parsonsburg Sand was derived from sandy shore and nearshore deposits of Sangamon age. Deposition was in part eolian and in part fluvial and lacustrine, probably in small streams and ponds between sand dunes.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1067B","usgsCitation":"Denny, C.S., Owens, J.P., Sirkin, L., and Rubin, M., 1979, The Parsonsburg Sand in the central Delmarva Peninsula, Maryland and Delaware: U.S. Geological Survey Professional Paper 1067, p. B1-B16, https://doi.org/10.3133/pp1067B.","productDescription":"p. B1-B16","costCenters":[],"links":[{"id":119379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1067b/report-thumb.jpg"},{"id":67293,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1067b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae55","contributors":{"authors":[{"text":"Denny, Charles Storrow","contributorId":86331,"corporation":false,"usgs":true,"family":"Denny","given":"Charles","email":"","middleInitial":"Storrow","affiliations":[],"preferred":false,"id":221853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Owens, J. P.","contributorId":50946,"corporation":false,"usgs":true,"family":"Owens","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":221852,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sirkin, L.A.","contributorId":40647,"corporation":false,"usgs":true,"family":"Sirkin","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":221851,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rubin, Meyer","contributorId":107283,"corporation":false,"usgs":true,"family":"Rubin","given":"Meyer","email":"","affiliations":[],"preferred":false,"id":221854,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":40234,"text":"ofr79820 - 1979 - Coal resource occurrence and coal development potential maps of the Castor Gulch quadrangle, Moffat County, Colorado","interactions":[],"lastModifiedDate":"2021-10-28T20:02:03.388991","indexId":"ofr79820","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-820","title":"Coal resource occurrence and coal development potential maps of the Castor Gulch quadrangle, Moffat County, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79820","usgsCitation":"Dames & Moore, 1979, Coal resource occurrence and coal development potential maps of the Castor Gulch quadrangle, Moffat County, Colorado: U.S. Geological Survey Open-File Report 79-820, Report: iii, 24 p.; 15 Plates: 28.99 × 23.01 inches or smaller, https://doi.org/10.3133/ofr79820.","productDescription":"Report: iii, 24 p.; 15 Plates: 28.99 × 23.01 inches or smaller","costCenters":[],"links":[{"id":71020,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0820/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71019,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71018,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71017,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71016,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71015,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71014,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71013,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71012,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71011,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71010,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71009,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71008,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71007,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71006,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71005,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0820/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":176898,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0820/report-thumb.jpg"},{"id":391107,"rank":18,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30305.htm"}],"country":"United States","state":"Colorado","county":"Moffat County","otherGeospatial":"Castor Gulch quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.625,\n              40.375\n            ],\n            [\n              -107.5,\n              40.375\n            ],\n            [\n              -107.5,\n              40.5\n            ],\n            [\n              -107.625,\n              40.5\n            ],\n            [\n              -107.625,\n              40.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b4149","contributors":{"authors":[{"text":"Dames & Moore","contributorId":127975,"corporation":true,"usgs":false,"organization":"Dames & Moore","id":530069,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40275,"text":"ofr7921 - 1979 - Coal resource occurrence and coal development potential maps of the White Tail Butte Quadrangle, Campbell County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:34","indexId":"ofr7921","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-21","title":"Coal resource occurrence and coal development potential maps of the White Tail Butte Quadrangle, Campbell County, Wyoming","language":"ENGLISH","doi":"10.3133/ofr7921","usgsCitation":"IntraSearch Inc., 1979, Coal resource occurrence and coal development potential maps of the White Tail Butte Quadrangle, Campbell County, Wyoming: U.S. Geological Survey Open-File Report 79-21, 38 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,{"id":40235,"text":"ofr795 - 1979 - Coal resource occurrence and coal development potential maps of the Chalky Point Quadrangle, Big Horn and Rosebud counties, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:11:09","indexId":"ofr795","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-5","title":"Coal resource occurrence and coal development potential maps of the Chalky Point Quadrangle, Big Horn and Rosebud counties, Montana","language":"ENGLISH","doi":"10.3133/ofr795","usgsCitation":"Colorado School of Mines Research Institute, 1979, Coal resource occurrence and coal development potential maps of the Chalky Point Quadrangle, Big Horn and Rosebud counties, Montana: U.S. Geological Survey Open-File Report 79-5, 8 maps and 1 data sheet ;58 x 41 cm.; 20 p., https://doi.org/10.3133/ofr795.","productDescription":"8 maps and 1 data sheet ;58 x 41 cm.; 20 p.","costCenters":[],"links":[{"id":175762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0005/report-thumb.jpg"},{"id":71021,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0005/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71022,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0005/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71023,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0005/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71024,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0005/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71025,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0005/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71026,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0005/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71027,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0005/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71028,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0005/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71029,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0005/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71030,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0005/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b414e","contributors":{"authors":[{"text":"Colorado School of Mines Research Institute","contributorId":128082,"corporation":true,"usgs":false,"organization":"Colorado School of Mines Research Institute","id":530070,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38151,"text":"ofr79329 - 1979 - Particle size of sediments collected from the bed of the Amazon River and its tributaries in May and June 1977","interactions":[],"lastModifiedDate":"2014-01-30T12:03:00","indexId":"ofr79329","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-329","title":"Particle size of sediments collected from the bed of the Amazon River and its tributaries in May and June 1977","docAbstract":"One-hundred-eight samples of bed material were collected from the Amazon River and its major tributaries between Belem, Brazil , and Iquitos, Peru. Samples were taken with a standard BM-54 sampler or with pipe dredges from May 18 to June 5, 1977. Most of the samples have median diameters in the size range of fine to medium sand and contain small percentages of fine gravel. Complete size distributions are tabulated. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79329","issn":"0094-9140","usgsCitation":"Nordin, C.F., Meade, R., Curtis, W.F., Bosio, N., and Delaney, B.M., 1979, Particle size of sediments collected from the bed of the Amazon River and its tributaries in May and June 1977: U.S. Geological Survey Open-File Report 79-329, iii, 27 p. ;29 cm., https://doi.org/10.3133/ofr79329.","productDescription":"iii, 27 p. ;29 cm.","costCenters":[],"links":[{"id":162713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0329/report-thumb.jpg"},{"id":281747,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0329/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689117","contributors":{"authors":[{"text":"Nordin, Carl F.","contributorId":68297,"corporation":false,"usgs":true,"family":"Nordin","given":"Carl","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":219218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meade, R.H.","contributorId":27449,"corporation":false,"usgs":true,"family":"Meade","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":219214,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Curtis, W. F.","contributorId":61432,"corporation":false,"usgs":true,"family":"Curtis","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":219216,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bosio, N.J.","contributorId":67940,"corporation":false,"usgs":true,"family":"Bosio","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":219217,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Delaney, B. M.","contributorId":42217,"corporation":false,"usgs":true,"family":"Delaney","given":"B.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":219215,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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