The Green River-Moab area encompasses about 7,800 square kilometers or about 25 percent of the Paradox basin. The entire Paradox basin is a part of the Colorado Plateaus that is underlain by a thick sequence of evaporite (salt) beds of Pennsylvanian age. The rock units that underlie the area have been grouped into hydrogeologic units based on their water-transmitting ability. Confining beds consist of evaporite beds of mostly salt, and over- lying and underlying thick sequences of rocks with minimal permeability; above and below these confining beds are aquifers. The upper Mesozoic sand- stone aquifer, probably is the most permeable hydrogeologic unit of the area and is the subject of this investigation. The principal component of ground- water outflow from this aquifer probably is subsurface flow to regional streams (the Green and Colorado Rivers) and is about 100 million cubic meters per year. All other components of outflow are relatively small. The average annual recharge to the aquifer is about 130 million cubic meters, of which about 20 million cubic meters is from local precipitation. For the lower aquifer, all recharge and discharge probably is by subsurface flow and was not estimated.
The aquifers are generally isolated from the evaporite beds by the bounding confining beds; as a result, most ground water has little if any contact with the evaporites. Brines are present in the confining beds, but solution of beds o£ salt probably is very slow in most parts of the area. No brine discharges' have been identified.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr82107","collaboration":"Prepared in cooperaiton with the U.S. Department of Energy","usgsCitation":"Rush, F., Whitfield, M., and Hart, I.M., 1982, Regional hydrology of the Green River-Moab area, northwestern Paradox basin, Utah: U.S. Geological Survey Open-File Report 82-107, Report: vii, 86 p.; Table: 2 Plates: 26.00 in. x 28.00 inches, https://doi.org/10.3133/ofr82107.","productDescription":"Report: vii, 86 p.; Table: 2 Plates: 26.00 in. x 28.00 inches","numberOfPages":"92","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":392017,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13639.htm"},{"id":20448,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0107/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing generalized hydrology of the Green River-Moab area, Northwestern Paradox Basin, Utah"},{"id":20447,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0107/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing generalized hydrogeology of the Green River-Moab area, Northwestern Paradox Basin, Utah"},{"id":20449,"rank":402,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1982/0107/plate-3.pdf","text":"Table 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Rock and hydrogeologic units in the Green River-Moab area and vicinity"},{"id":153242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0107/report-thumb.jpg"},{"id":50276,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Green River - Moab area, Paradox Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.25,\n 38\n ],\n [\n -110.5,\n 38\n ],\n [\n -110.5,\n 39.283\n ],\n [\n -109.25,\n 39.283\n ],\n [\n -109.25,\n 38\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634869","contributors":{"authors":[{"text":"Rush, F. E.","contributorId":56234,"corporation":false,"usgs":true,"family":"Rush","given":"F. E.","affiliations":[],"preferred":false,"id":183122,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitfield, M.S.","contributorId":69547,"corporation":false,"usgs":true,"family":"Whitfield","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":183123,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hart, I. M.","contributorId":24806,"corporation":false,"usgs":true,"family":"Hart","given":"I.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":183121,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8777,"text":"ofr82775 - 1982 - Hydrology of the Arbuckle Mountain area, south-central Oklahoma","interactions":[{"subject":{"id":8777,"text":"ofr82775 - 1982 - Hydrology of the Arbuckle Mountain area, south-central Oklahoma","indexId":"ofr82775","publicationYear":"1982","noYear":false,"title":"Hydrology of the Arbuckle Mountain area, south-central Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70046124,"text":"70046124 - 1990 - Hydrology of the Arbuckle Mountains area, south-central Oklahoma","indexId":"70046124","publicationYear":"1990","noYear":false,"title":"Hydrology of the Arbuckle Mountains area, south-central Oklahoma"},"id":1}],"supersededBy":{"id":70046124,"text":"70046124 - 1990 - Hydrology of the Arbuckle Mountains area, south-central Oklahoma","indexId":"70046124","publicationYear":"1990","noYear":false,"title":"Hydrology of the Arbuckle Mountains area, south-central Oklahoma"},"lastModifiedDate":"2017-09-29T07:50:47","indexId":"ofr82775","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-775","title":"Hydrology of the Arbuckle Mountain area, south-central Oklahoma","docAbstract":"Rocks that make up the Arbuckle-Simpson aquifer crop out over about 500 square miles in the Arbuckle Mountains province in south-central Oklahoma. The aquifer consists of limestone, dolomite, and sandstone of the Arbuckle and Simpson Groups of Late Cambrian to Middle Ordovician age and is about 5,000 to 9,000 feet thick. The rocks were subjected to intensive folding and faulting associated with major uplift of the area during Early to Late Pennsylvanian time.
Water in the aquifer is confined in some parts of the area, while in other parts it is unconfined. The average saturated thickness of the aquifer is about 3,500 feet in the outcrop area. Water levels measured in wells fluctuated from 8 to 53 feet each year, primarily in response to recharge from rainfall.
Recharge to the aquifer is estimated at about 4.7 inches per year.
The average storage coefficient of the aquifer is estimated at 0.008, and the average transmissivity is estimated at 15,000 feet squared per day. Based on an average saturated thickness of about 3,500 feet and a storage coefficient of 0.008, the volume of ground water contained in the 500-square-mile outcrop area is about 9 million acre-feet. An undetermined amount of fresh water probably exists in the aquifer around the periphery of the aquifer outcrop.
Base flow of streams that drain the aquifer accounts for about 60 percent of the total annual runoff from the outcrop area and is maintained by numerous springs. The close hydraulic connection between streams in the outcrop area and the aquifer is shown by a close correlation between base flow in Blue River and the fluctuation of ground-water levels in five wells in the Blue River basin. This correlation also exists between the discharge by Byrds Mill Spring and the fluctuation in water level in a nearby observation well; increase and decrease in spring discharge correspond to rise and fall of the water level in the well.
The chemical quality of water from the Arbuckle-Simpson aquifer is suitable for most industrial and municipal uses. The water is hard and of the bicarbonate type; the average hardness is about 340 milligrams per liter, and the average dissolved-solids concentration is about 360 milligrams per liter. Because springs issue from the aquifer and discharge to streams in the area, the quality of water from springs and base flow in streams is similar to that of ground water. The average dissolved-solids concentration of stream water is slightly less than that of water from wells and springs.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82775","usgsCitation":"Fairchild, R.W., Hanson, R.L., and Davis, R.E., 1982, Hydrology of the Arbuckle Mountain area, south-central Oklahoma: U.S. Geological Survey Open-File Report 82-775, 156 p., https://doi.org/10.3133/ofr82775.","productDescription":"156 p.","numberOfPages":"170","costCenters":[],"links":[{"id":346189,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0775/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0775/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.37182617187499,\n 34.16295449004889\n ],\n [\n -96.41189575195312,\n 34.16295449004889\n ],\n [\n -96.41189575195312,\n 34.73484137177769\n ],\n [\n -97.37182617187499,\n 34.73484137177769\n ],\n [\n -97.37182617187499,\n 34.16295449004889\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ee9","contributors":{"authors":[{"text":"Fairchild, Roy W.","contributorId":79155,"corporation":false,"usgs":true,"family":"Fairchild","given":"Roy","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158313,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanson, Ronald L.","contributorId":65054,"corporation":false,"usgs":true,"family":"Hanson","given":"Ronald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":158311,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":158312,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":43104,"text":"ofr82261 - 1982 - Ground-water levels in selected well fields and in west-central Florida, September 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr82261","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-261","title":"Ground-water levels in selected well fields and in west-central Florida, September 1981","docAbstract":"The water table in the surficial aquifer and the potentiometric surface of the Floridan aquifer in a 1,200-square-mile area in west-central Florida are mapped semiannually by the U.S. Geological Survey. Maps are based on water levels measured in wells each May to coincide with seasonal low levels and each September to coincide with seasonal high levels. The mapped area shows 14 well fields that supplied 140.3 million gallons to municipalities on September 21, 1981. The water is withdrawn from the Floridan aquifer, the major aquifer in Florida. The effect of localized withdrawal on ground water is shown on the maps as depressions in both the potentiometric and water-table surfaces. In September 1981, ground-water levels were significantly higher than those of May 1981 and were unchanged or within a few feet of those in September 1980. Seasonal recharge from summer rains and reduced pumpage are factors in the water-level recovery from record and near record low levels of May 1981. (USGS)","language":"ENGLISH","doi":"10.3133/ofr82261","usgsCitation":"Yobbi, D.K., and Barr, G., 1982, Ground-water levels in selected well fields and in west-central Florida, September 1981: U.S. Geological Survey Open-File Report 82-261, 33 maps on 2 sheets :photocopy ;sheets 86 x 61 cm., https://doi.org/10.3133/ofr82261.","productDescription":"33 maps on 2 sheets :photocopy ;sheets 86 x 61 cm.","costCenters":[],"links":[{"id":135287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80919,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0261/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80920,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0261/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675f1","contributors":{"authors":[{"text":"Yobbi, D. K.","contributorId":56622,"corporation":false,"usgs":true,"family":"Yobbi","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":227730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barr, G. L.","contributorId":22312,"corporation":false,"usgs":true,"family":"Barr","given":"G. L.","affiliations":[],"preferred":false,"id":227729,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9881,"text":"ofr82307 - 1982 - Hydrotectonics; principles and relevance","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr82307","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-307","title":"Hydrotectonics; principles and relevance","docAbstract":"Hydrotectonics combines the principles of hydraulics and rock mechanics. The hypothesis assumes that: (1) no faults are truly planar, (2) opposing noncongruent wavy wallrock surfaces form chambers and bottlenecks along the fault, and (3) most thrusting occurs beneath the water table. These physical constraints permit the following dynamics. \r\n\r\nShear displacement accompanying faulting must constantly change the volume of each chamber. Addition of ground water liquefies dry fault breccia to a heavy incompressible viscous muddy breccia I call fault slurry. When the volume of a chamber along a thrust fault decreases faster than its fault slurry can escape laterally, overpressurized slurry is hydraulically injected into the base of near-vertical fractures in the otherwise impervious overriding plate. Breccia pipes commonly form where such fissures intersect. \r\n\r\nAlternating decrease and increase in volume of the chamber subjects this injection slurry to reversible surges that not only raft and abrade huge clasts sporadically spalled from the walls of the conduit but also act as a forceful hydraulic ram which periodically widens the conduit and extends its top. If the pipe perforates a petroleum reservoir, leaking hydrocarbons float to its top. \r\n\r\nSudden faulting may generate a powerful water hammer that can be amplified at some distal narrow ends of the anastomosing plumbing system, where the shock may produce shatter cones. If vented on the Earth's surface, the muddy breccia, now called extrusion slurry, forms a mud volcano. \r\n\r\nThis hypothesis suggests that many highly disturbed features presently attributed to such catastrophic processes as subsurface explosions or meteorite impacts are due to the rheology of tectonic slurry in an intermittently reactivated pressure-relief tube rooted in a powerful reciprocating hydrotectonic pump activated by a long-lived deep-seated thrust fault.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82307","usgsCitation":"Kopf, R.W., 1982, Hydrotectonics; principles and relevance: U.S. Geological Survey Open-File Report 82-307, 30 p., ill. ;28 cm., https://doi.org/10.3133/ofr82307.","productDescription":"30 p., ill. ;28 cm.","costCenters":[],"links":[{"id":140947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0307/report-thumb.jpg"},{"id":37669,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0307/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c928","contributors":{"authors":[{"text":"Kopf, R. W.","contributorId":69544,"corporation":false,"usgs":true,"family":"Kopf","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160450,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43931,"text":"ofr823 - 1982 - Land use and land cover and associated maps for Ritzville, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:11:05","indexId":"ofr823","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-3","title":"Land use and land cover and associated maps for Ritzville, Washington","language":"ENGLISH","doi":"10.3133/ofr823","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Land use and land cover and associated maps for Ritzville, Washington: U.S. Geological Survey Open-File Report 82-3, maps ;45 x 61 cm., https://doi.org/10.3133/ofr823.","productDescription":"maps ;45 x 61 cm.","costCenters":[],"links":[{"id":168484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af5a3","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":531479,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43826,"text":"ofr82214 - 1982 - Landsat image map of the Jabal Ibrahim Quadrangle, sheet 20E, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-12-11T14:13:02","indexId":"ofr82214","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-214","title":"Landsat image map of the Jabal Ibrahim Quadrangle, sheet 20E, Kingdom of Saudi Arabia","docAbstract":"Miscellaneous Map 13
Interagency Report 312
Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in Austin, Houston, and San Antonio.
The U.S. Geological Survey, in cooperation with the city of Houston, began studies in the Houston metropolitan area in 1964. The program was expanded in 1968 to include collection of water-quality data. The objectives of the Houston urban-hydrology study are as follows:
This report, the sixteenth in a series of reports to be published annually, is primarily applicable to objective 2. The report presents hydro!ogic data collected in the Houston urban area for the 1979 water year (October 1, 1978 to September 30, 1979).
A report by Johnson and Sayre (1973) utilized records collected from 1965 to 1969 to make a study of the effects of urbanization on floods in the Houston area. The report also summarizes various basin parameters. A report by Waddell, Massey, and Jennings (1979) presents data on computed runoff from the Houston area and computed concentrations and loads of selected waterquality constituents combined in the inflow to Galveston Bay. The study utilized a variation of the \"STORM\" model developed by the Hydro!ogic Engineering Center of the U.S. Army Corps of Engineers. A report prepared by Li scum and Massey (1980) presents a technique for estimating the magnitude and frequency of floods in the Houston area from drainage areas, bank-full conveyance, and percentage of urban development.
A definition of terms related to streamflow, water quality, and other hydrologic data, as used in this report, are defined in \"U.S. Geological Survey, Water-resources data for Texas, volume 2, 1979.\"
To facilitate the publication and distribution of this report at the earliest feasible time, some material has been included that does not conform to the formal publications standards of the U.S. Geological Survey.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82164","collaboration":"Prepared in cooperation with the City of Houston","usgsCitation":"Liscum, F., Weigel, J.F., and Bruchmiller, J., 1982, Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1979: U.S. Geological Survey Open-File Report 82-164, 308 p., https://doi.org/10.3133/ofr82164.","productDescription":"308 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":145609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0164/report-thumb.jpg"},{"id":37900,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0164/report.pdf","text":"Report","size":"6.18 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Houston","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.36819458007811,\n 30.039377605001338\n ],\n [\n -95.42587280273438,\n 30.039377605001338\n ],\n [\n -95.49179077148438,\n 30.03462216002981\n ],\n [\n -95.56320190429686,\n 30.0262995822237\n ],\n [\n -95.62774658203125,\n 30.001327656702326\n ],\n [\n -95.73348999023438,\n 29.969211659636663\n ],\n [\n -95.83648681640624,\n 29.92756435779241\n ],\n [\n -95.87493896484374,\n 29.888280933159265\n ],\n [\n -95.86257934570312,\n 29.80251790576445\n ],\n [\n -95.86944580078125,\n 29.75364773335698\n ],\n [\n -95.8447265625,\n 29.69640358280457\n ],\n [\n -95.79940795898438,\n 29.672542219068987\n ],\n [\n -95.69641113281249,\n 29.630771207229\n ],\n [\n -95.63186645507812,\n 29.60092416008231\n ],\n [\n -95.51513671875,\n 29.57106827738255\n ],\n [\n -95.40252685546875,\n 29.511330027309146\n ],\n [\n -95.28030395507812,\n 29.485034019181064\n ],\n [\n -95.17730712890625,\n 29.482643134466617\n ],\n [\n -95.086669921875,\n 29.499378142743375\n ],\n [\n -94.99740600585938,\n 29.532839863453397\n ],\n [\n -94.95483398437499,\n 29.551955878093022\n ],\n [\n -94.9493408203125,\n 29.604506272365295\n ],\n [\n -94.96719360351562,\n 29.653449050468925\n ],\n [\n -94.9822998046875,\n 29.680894340704334\n ],\n [\n -95.01800537109374,\n 29.71787396585316\n ],\n [\n -95.0372314453125,\n 29.744109309616487\n ],\n [\n -95.06881713867188,\n 29.76556948666697\n ],\n [\n -95.06744384765625,\n 29.797751134173065\n ],\n [\n -95.07705688476562,\n 29.837070205715218\n ],\n [\n -95.10314941406249,\n 29.871610558533725\n ],\n [\n -95.1361083984375,\n 29.925183985247404\n ],\n [\n -95.15396118164062,\n 29.972780616663897\n ],\n [\n -95.14572143554688,\n 29.997759725578906\n ],\n [\n -95.185546875,\n 30.01916538794235\n ],\n [\n -95.2294921875,\n 30.02511058549258\n ],\n [\n -95.2789306640625,\n 30.029866486852946\n ],\n [\n -95.33660888671875,\n 30.032244351965684\n ],\n [\n -95.36819458007811,\n 30.039377605001338\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db607de7","contributors":{"authors":[{"text":"Liscum, Fred","contributorId":95463,"corporation":false,"usgs":true,"family":"Liscum","given":"Fred","email":"","affiliations":[],"preferred":false,"id":160733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weigel, Jay F.","contributorId":19560,"corporation":false,"usgs":true,"family":"Weigel","given":"Jay","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160732,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bruchmiller, J.P.","contributorId":102490,"corporation":false,"usgs":true,"family":"Bruchmiller","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":160734,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10554,"text":"ofr82692 - 1982 - Data for wells at the low-level radioactive-waste burial site in the Palos Forest Preserve, Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82692","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-692","title":"Data for wells at the low-level radioactive-waste burial site in the Palos Forest Preserve, Illinois","docAbstract":"The U.S. Geological Survey is studying the geologic, hydrologic, and geochemical properties of the glacial drift and underlying bedrock at a low-level radioactive-waste burial site in the Palos Forest Preserve, 22 kilometers southwest of Chicago. Data collected from the 33 test wells drilled into the drift plus data from 4 wells drilled into the underlying dolomite bedrock are presented. Data include maps showing the location of the test wells, a general description of the drift, well-construction information, and lithologic descriptions of cores from the wells finished in the drift.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82692","usgsCitation":"Olimpio, J., 1982, Data for wells at the low-level radioactive-waste burial site in the Palos Forest Preserve, Illinois: U.S. Geological Survey Open-File Report 82-692, iii, 101 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82692.","productDescription":"iii, 101 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":142500,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0692/report-thumb.jpg"},{"id":38392,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0692/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c902","contributors":{"authors":[{"text":"Olimpio, J.C.","contributorId":36137,"corporation":false,"usgs":true,"family":"Olimpio","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":161584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10236,"text":"ofr82179 - 1982 - Metal distribution in the Battle Lake area, Grand Encampment mining district, Carbon County, Wyoming, with comparisons to deposits in the New Rambler mine district, Albany and Carbon Counties, Wyoming","interactions":[],"lastModifiedDate":"2022-08-01T21:50:41.167541","indexId":"ofr82179","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-179","title":"Metal distribution in the Battle Lake area, Grand Encampment mining district, Carbon County, Wyoming, with comparisons to deposits in the New Rambler mine district, Albany and Carbon Counties, Wyoming","docAbstract":"
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82179","usgsCitation":"McCallum, M.E., and Menzer, F.J., 1982, Metal distribution in the Battle Lake area, Grand Encampment mining district, Carbon County, Wyoming, with comparisons to deposits in the New Rambler mine district, Albany and Carbon Counties, Wyoming: U.S. Geological Survey Open-File Report 82-179, 20 p., https://doi.org/10.3133/ofr82179.","productDescription":"20 p.","costCenters":[],"links":[{"id":404616,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75623.htm","linkFileType":{"id":5,"text":"html"}},{"id":144214,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0179/report-thumb.jpg"},{"id":38105,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0179/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","county":"Albany County, Carbon County,","otherGeospatial":"Battle Lake area, Grand Encampment mining district, New Rambler mine district","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.138671875,\n 41.03585891144301\n ],\n [\n -106.20071411132812,\n 41.03585891144301\n ],\n [\n -106.20071411132812,\n 41.29328546081616\n ],\n [\n -107.138671875,\n 41.29328546081616\n ],\n [\n -107.138671875,\n 41.03585891144301\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625927","contributors":{"authors":[{"text":"McCallum, M. E.","contributorId":34119,"corporation":false,"usgs":true,"family":"McCallum","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Menzer, F. J.","contributorId":36005,"corporation":false,"usgs":true,"family":"Menzer","given":"F.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161057,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10055,"text":"ofr82446 - 1982 - Preliminary data for northern Great Plains test well 1, quarter NE quarter Sec. 11, T.55N., R.77W., Sheridan County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr82446","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-446","title":"Preliminary data for northern Great Plains test well 1, quarter NE quarter Sec. 11, T.55N., R.77W., Sheridan County, Wyoming","docAbstract":"This report documents the preliminary data obtained from Northern Great Plains test well 1 and describes the preliminary results and future testing plans. The intended audience includes hydrologists, local water users, drilling contractors, and water managers. The test well was drilled as part of the study to determine the water resource potential of the regional aquifer system in the Northern Great Plains, an area of about 250,000 sq mi. The well is 4,485 ft deep; nine cores were drilled totaling 182 ft; 157.42 ft of core were recovered. Sidewall cores were obtained from 24 horizons. Gamma and density scans of the cores were made, and selected parts were tested for density, porosity, and vertical and horizontal permeability. Eight zones were perforated and tested using conventional drill-stem tests and swabbing. Water samples were obtained from seven zones. No major potential sources of groundwater were penetrated by the test well. Estimated yields from selected zones range from about 240 gal/min with 400 ft of drawdown to about 5 gal/min flow at the surface. Dissolved-solids concentrations ranged from about 1,800 to 3,000 mg/l. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82446","usgsCitation":"Lobmeyer, D., Anna, L.O., and Busby, J., 1982, Preliminary data for northern Great Plains test well 1, quarter NE quarter Sec. 11, T.55N., R.77W., Sheridan County, Wyoming: U.S. Geological Survey Open-File Report 82-446, 80 p., 3 logs, ill., maps ;28 cm., https://doi.org/10.3133/ofr82446.","productDescription":"80 p., 3 logs, ill., maps ;28 cm.","costCenters":[],"links":[{"id":145632,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0446/report-thumb.jpg"},{"id":37904,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0446/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aee5","contributors":{"authors":[{"text":"Lobmeyer, D.H.","contributorId":106502,"corporation":false,"usgs":true,"family":"Lobmeyer","given":"D.H.","affiliations":[],"preferred":false,"id":160740,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anna, L. O.","contributorId":65472,"corporation":false,"usgs":true,"family":"Anna","given":"L.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":160738,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Busby, J.F.","contributorId":105300,"corporation":false,"usgs":true,"family":"Busby","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":160739,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10555,"text":"ofr8278 - 1982 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium","interactions":[{"subject":{"id":10555,"text":"ofr8278 - 1982 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium","indexId":"ofr8278","publicationYear":"1982","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium"},"predicate":"SUPERSEDED_BY","object":{"id":2414,"text":"wsp2226 - 1984 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","indexId":"wsp2226","publicationYear":"1984","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium"},"id":1}],"supersededBy":{"id":2414,"text":"wsp2226 - 1984 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","indexId":"wsp2226","publicationYear":"1984","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium"},"lastModifiedDate":"2019-11-07T11:35:12","indexId":"ofr8278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-78","title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr8278","usgsCitation":"Olimpio, J., 1982, Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium: U.S. Geological Survey Open-File Report 82-78, v, 57 p., https://doi.org/10.3133/ofr8278.","productDescription":"v, 57 p.","costCenters":[],"links":[{"id":142501,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0078/report-thumb.jpg"},{"id":369038,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0078/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Illinois","otherGeospatial":"Palos Forest Preserve","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.9290771484375,\n 41.66162721430806\n ],\n [\n -87.83294677734375,\n 41.66162721430806\n ],\n [\n -87.83294677734375,\n 41.72213058512578\n ],\n [\n -87.9290771484375,\n 41.72213058512578\n ],\n [\n -87.9290771484375,\n 41.66162721430806\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64880f","contributors":{"authors":[{"text":"Olimpio, J.C.","contributorId":36137,"corporation":false,"usgs":true,"family":"Olimpio","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":161585,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10126,"text":"ofr82850 - 1982 - Guidebook to the late Cenozoic geology of the Beaver Basin, south-central Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr82850","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-850","title":"Guidebook to the late Cenozoic geology of the Beaver Basin, south-central Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82850","usgsCitation":"Machette, M.N., 1982, Guidebook to the late Cenozoic geology of the Beaver Basin, south-central Utah: U.S. Geological Survey Open-File Report 82-850, 44 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82850.","productDescription":"44 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":145681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0850/report-thumb.jpg"},{"id":37973,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0850/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64af2f","contributors":{"authors":[{"text":"Machette, M. N.","contributorId":19561,"corporation":false,"usgs":true,"family":"Machette","given":"M.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":160855,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10829,"text":"ofr82588 - 1982 - High rates of bedload transport measured from infilling rate of large strudelscour craters in the Beaufort Sea, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr82588","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-588","title":"High rates of bedload transport measured from infilling rate of large strudelscour craters in the Beaufort Sea, Alaska","docAbstract":"Strudel scours are craters as much as 20 m wide and 4 m deep, that are excavated by vertical drainage flow during the yearly spring flooding of vast reaches of fast ice surrounding arctic deltas; they form at a rate of about 2.5 km^-2 yr^-1. Monitoring two such craters in the Beaufort Sea, we found that in relatively unprotected sites they fill in by deposition from bedload in 2 to 3 years. Net westward sediment transport results in sand layers dipping at the angle of repose westward into the strudel-scour crater, whereas the west wall of the crater remains steep to vertical. Initially the crater traps almost all bedload: sand, pebbles, and organic detritus; as infilling progresses, the materials are increasingly winnowed, and bypassing must occur. Over a 20-m-wide sector, an exposed strudel scour trapped 360 m3 of bedload during two seasons; this infilling represents a bedload transport rate of 9 m3 yr^-1 m^-1. This rate should be applicable to a 4.5-km-wide zone with equal exposure and similar or shallower depth. Within this zone, the transport rate is 40,500 m3 yr^-1, similar to estimated longshore transport rates on local barrier beaches. On the basis of the established rate of cut and fill, all the delta-front deposits should consist of strudel-scour fill. Vibracores typically show dipping interbedded sand and lenses of organic material draped over very steep erosional contacts, and an absence of horizontal continuity of strata--criteria that should uniquely identify high-latitude deltaic deposits. Given a 2- to 3-year lifespan, most strudel scours seen in surveys must be old. The same holds true for ice gouges and other depressions not adjusted to summer waves and currents, although these features record events of only the past few years. In view of such high rates of bottom reworking of the shallow shelf, any human activities creating turbidity, such as dredging, would have little effect on the environment. However, huge amounts of transitory material trapped by long causeways planned for offshore development would result in major changes in the environment.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82588","usgsCitation":"Reimnitz, E., and Kempema, E., 1982, High rates of bedload transport measured from infilling rate of large strudelscour craters in the Beaufort Sea, Alaska: U.S. Geological Survey Open-File Report 82-588, 19 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr82588.","productDescription":"19 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":145562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0588/report-thumb.jpg"},{"id":38629,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0588/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6359f7","contributors":{"authors":[{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":162038,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kempema, E. 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1982 - Knik Glacier, Alaska; summary of 1979, 1980, and 1981 data and introduction of new surveying techniques","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr82685","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-685","title":"Knik Glacier, Alaska; summary of 1979, 1980, and 1981 data and introduction of new surveying techniques","docAbstract":"Knik Glacier in south-central Alaska has the potential to reform Lake George, Alaska 's largest glacier-dammed lake. Measurements of surface altitude, snow depth, terminus position, glacier speed, and ice depth are being made in an attempt to determine the mechanisms that could cause a significant re-advance of the glacier. New surveying and data reduction techniques were developed by the authors and employed successfully at Knik Glacier. These include precise geodetic surveying by the ' trisection ' technique, calculation of surface altitude at a specially-fixed ' index point ' from three point measurements on a rough, moving glacier surface, and calculation of ice thickness from low frequency radar measurements. In addition, this report summarizes the data collected from 1979 to 1981 in support of this goal. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82685","usgsCitation":"Mayo, L., and Trabant, D., 1982, Knik Glacier, Alaska; summary of 1979, 1980, and 1981 data and introduction of new surveying techniques: U.S. Geological Survey Open-File Report 82-685, vi, 32 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82685.","productDescription":"vi, 32 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":144323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0685/report-thumb.jpg"},{"id":38099,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0685/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48fe","contributors":{"authors":[{"text":"Mayo, L.R.","contributorId":21541,"corporation":false,"usgs":true,"family":"Mayo","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":161046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trabant, D.C.","contributorId":42209,"corporation":false,"usgs":true,"family":"Trabant","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":161047,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10318,"text":"ofr82475 - 1982 - Geophysical logs of nine holes drilled in 1978 in the Yampa coal field, Hamilton and Pagoda quadrangles, Moffat County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82475","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-475","title":"Geophysical logs of nine holes drilled in 1978 in the Yampa coal field, Hamilton and Pagoda quadrangles, Moffat County, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82475","usgsCitation":"Meyer, R.F., and Brown, R., 1982, Geophysical logs of nine holes drilled in 1978 in the Yampa coal field, Hamilton and Pagoda quadrangles, Moffat County, Colorado: U.S. Geological Survey Open-File Report 82-475, i, 34 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82475.","productDescription":"i, 34 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0475/report-thumb.jpg"},{"id":38171,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0475/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b58b","contributors":{"authors":[{"text":"Meyer, R. 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