No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNJ791","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water-resources data for New Jersey, water year 1979, Volume 1. 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Jersey\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9d72","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":532389,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66212,"text":"i1181 - 1980 - Geologic map of the Argyre quadrangle of Mars","interactions":[],"lastModifiedDate":"2023-07-10T13:41:44.82202","indexId":"i1181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1181","title":"Geologic map of the Argyre quadrangle of Mars","docAbstract":"The geology of the Argyre quadrangle of Mars is dominated by the conspicuous Argyre basin, defined by a rim of rugged mountain blocks that surround a nearly circular expanse of plains 800 km across. Of the large (greater than 500 km in diameter) basins identified on Mars, Argyre is the best preserved and possibly youngest. Basins appear to be traps for eolian debris and evidently are source areas for some of the dust storms that periodically envelop the planet.
The quadrangle lies within the densely cratered province that characterizes the southern hemisphere, contrasting with sparsely cratered plains generally confined to the northern hemisphere. Northwest of Argyre an outlier of sparsely cratered, ridged plains extends into the quadrangle from the Coprates region. Northeast of the basin are the cratered uplands, parts of which are presumed to represent remnants of the earliest martian crust (Wilhelms, 1974). South of the quadrangle the cratered plateau is replaced by the pitted, etched, layered, and mantled terrains that characterize the south polar region (Sharp, 1973a; Condit and Soderblom, 1978). Constructional volcanic landforms were not recognized within the map area.
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Jersey\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4f15","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":532390,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5919,"text":"pp1126AJ - 1980 - Shorter contributions to stratigraphy and structural geology, 1979","interactions":[],"lastModifiedDate":"2024-11-18T19:41:27.730858","indexId":"pp1126AJ","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1126","chapter":"A-J","title":"Shorter contributions to stratigraphy and structural geology, 1979","docAbstract":"PART A: A system of anticlines lies along the trend of the sinuous course of the Colorado River for a distance of 97 km in the central Grand Canyon. Similar anticlines occur in some perennially wet side canyons. The anticlines are most abundant and well developed along northeast-trending reaches of the main canyon where it is floored by the Cambrian Muav Limestone. Dips of the folded strata are as great as 60?, and the folding locally extends more than 250 m from the river. Low-angle thrust faults in the limbs of the anticlines parallel the river and have formed in response to folding of the comparatively brittle carbonate strata. High-angle reverse kink bands, along which rocks are displaced up toward the river, also parallel the anticlines and have develop2d in response to the upward bulging of the canyon floor. \r\n\r\nThe river anticlines are an unloading phenomenon. They result from lateral squeezing toward the river of saturated shaly parts of the Muav Limestone and underlying Bright Angel Shale. The driving mechanism for the deformation is a stress gradient that results from a difference in lithostatic load between the heavily loaded rocks under the 650-m-high canyon walls and the unloaded canyon floor. Saturation appears to weaken the shaly rocks sufficiently to allow deformation to take place. River anticlines are not present in the eastern Grand Canyon, where the Cambrian rocks also occur at river level. Their absence is explained by a lack of shaly rocks that could flow when saturated. \r\n\r\nPART B: The current interest in contemporary tectonic processes in the Eastern United States is turning up abundant evidence of crustal movements in late geologic time. Topographic analysis of the highland areas from the southern Blue Ridge to the Adirondack Mountains indicates that most of the landforms owe their origin to erosion of rocks of different resistance rather than to tectonic processes. Most areas of high relief and high altitude have been formed on resistant rocks. The Cambrian and Ordovician belt, containing mostly shale and carbonate rock, on the other hand, forms an extensive lowland from Alabama to the Canadian border and girdles the Adirondack Mountains. Differences in altitude can be explained by the presence of resistant rocks outside the belt; these resistant rocks form local base levels on the streams that drain the belt. A few areas may have undergone local uplift at a higher rate than areas nearby--for example, the Piedmont region northwest of Chesapeake Bay. Most estimates of erosion rates, based on the load transported by streams and of uplift rates, based on removal during a known period of time, are of the same order of magnitude, averaging almost 4x 10^-2 millimeters per year. Rates of uplift, based on study of tilted Pleistocene beaches and repeated geodetic traverses, are at least an order of magnitude higher for comparable areas. Tectonic uplift of the highlands has been slow and involves mostly warping or tilting on a large scale. Erosion rates keep up with or exceed the rate of uplift and have been sufficient to mask evidence of faulting or other differential movements. The high rates of uplift that are inferred on tilted water planes in the glaciated regions or that are measured by differences in repeated geodetic traverses cannot have been sustained for long periods of time.\r\n\r\nPART C: The Hanson Creek Formation southwest of Eureka, Nev., in the Bellevue Peak Quadrangle is composed of three lithostratigraphic members: (1) a basal dark-gray dolomite, (2) a middle silty thin- to thick-bedded, locally nodular, dark-gray, light-yellow-mottled limestone topped by light-gray dolomite, and (3) an upper dark-gray dolomite, which is herein named the Combs Canyon Dolomite Member. Detailed geologic mapping and accompanying fossil collecting prove that the same lithostratigraphic and biostratigraphic sequence is present in the Mountain Boy Range and 11 km to the south near Wood Cone Peak. 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(59 p., 2 over-size sheets - PGS)","costCenters":[],"links":[{"id":149687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0532/report-thumb.jpg"},{"id":45380,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0532/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45381,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0532/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45382,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0532/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaee4b07f02db66c866","contributors":{"authors":[{"text":"Walker, George Walton","contributorId":14801,"corporation":false,"usgs":true,"family":"Walker","given":"George","email":"","middleInitial":"Walton","affiliations":[],"preferred":false,"id":172807,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5913,"text":"pp1164 - 1980 - Effects of coal mine subsidence in the Sheridan, Wyoming, area","interactions":[{"subject":{"id":8650,"text":"ofr78473 - 1978 - Effects of coal mine subsidence in the western Powder River basin, Wyoming","indexId":"ofr78473","publicationYear":"1978","noYear":false,"title":"Effects of coal mine subsidence in the western Powder River basin, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":5913,"text":"pp1164 - 1980 - Effects of coal mine subsidence in the Sheridan, Wyoming, area","indexId":"pp1164","publicationYear":"1980","noYear":false,"title":"Effects of coal mine subsidence in the Sheridan, Wyoming, area"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:41","indexId":"pp1164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1164","title":"Effects of coal mine subsidence in the Sheridan, Wyoming, area","docAbstract":"Analyses of the surface effects of past underground coal mining in the Sheridan, Wyoming, area suggest that underground mining of strippable coal deposits may damage the environment more over long periods of time than would modern surface mining, provided proper restoration procedures are followed after surface mining. Subsidence depressions and pits are a continuing hazard to the environment and to man's activities in the Sheridan, Wyo., area above abandoned underground mines in weak overburden less than about 60 m thick and where the overburden is less than about 10-15 times the thickness of coal mined. In addition, fires commonly start by spontaneous ignition when water and air enter the abandoned mine workings via subsidence cracks and pits. The fires can then spread to unmined coal as they create more cavities, more subsidence, and more cracks and pits through which air can circulate. \r\n\r\nIn modern surface mining operations the total land surface underlain by minable coal is removed to expose the coal. The coal is removed, the overburden and topsoil are replaced, and the land is regraded and revegetated. The land, although disturbed, can be more easily restored and put back into use than can land underlain by abandoned underground mine workings in areas where the overburden is less than about 60 m thick or less than about 10-15 times the thickness of coal mined. The resource recovery of modern surface mining commonly is much greater than that of underground mining procedures. Although present-day underground mining technology is advanced as compared to that of 25-80 years ago, subsidence resulting from underground mining of thick coal beds beneath overburden less than about 60 m thick can still cause greater damage to surface drainage, ground water, and vegetation than can properly designed surface mining operations. \r\n\r\nThis report discusses (11 the geology and surface and underground effects of former large-scale underground coal mining in a 50-km 2 area 5-20 km north of Sheridan, Wyo., (2) a ground and aerial reconnaissance study of a 5-km^2 coal mining area 8-10 km west of Sheridan, and (31 some environmental consequences and problems caused by coal mining.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1164","usgsCitation":"Dunrud, C., and Osterwald, F.W., 1980, Effects of coal mine subsidence in the Sheridan, Wyoming, area: U.S. Geological Survey Professional Paper 1164, 49 p., https://doi.org/10.3133/pp1164.","productDescription":"49 p.","costCenters":[],"links":[{"id":124834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1164/report-thumb.jpg"},{"id":32798,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1164/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db615ca8","contributors":{"authors":[{"text":"Dunrud, C. Richard","contributorId":48964,"corporation":false,"usgs":true,"family":"Dunrud","given":"C. Richard","affiliations":[],"preferred":false,"id":151800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osterwald, Frank W.","contributorId":98301,"corporation":false,"usgs":true,"family":"Osterwald","given":"Frank","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":151801,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66180,"text":"i857I - 1980 - Well yields and chemical quality of water from water-table aquifers in the Colorado Springs-Castle Rock area, Front Range urban corridor, Colorado","interactions":[],"lastModifiedDate":"2021-10-13T22:04:18.552716","indexId":"i857I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"857","chapter":"I","title":"Well yields and chemical quality of water from water-table aquifers in the Colorado Springs-Castle Rock area, Front Range urban corridor, Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i857I","usgsCitation":"Hillier, D.E., and Hutchinson, E., 1980, Well yields and chemical quality of water from water-table aquifers in the Colorado Springs-Castle Rock area, Front Range urban corridor, Colorado: U.S. Geological Survey IMAP 857, 2 Plates: 18.60 × 37.04 inches and 30.62 × 37.24 inches, https://doi.org/10.3133/i857I.","productDescription":"2 Plates: 18.60 × 37.04 inches and 30.62 × 37.24 inches","costCenters":[],"links":[{"id":390509,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9757.htm"},{"id":255677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0857i/report-thumb.jpg"},{"id":255676,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0857i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255675,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0857i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255674,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0857i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Colorado Springs-Castle Rock area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.625,\n 38.625\n ],\n [\n -105.125,\n 38.625\n ],\n [\n -105.125,\n 39.375\n ],\n [\n -104.625,\n 39.375\n ],\n [\n -104.625,\n 38.625\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0a8a","contributors":{"authors":[{"text":"Hillier, D. E.","contributorId":78386,"corporation":false,"usgs":true,"family":"Hillier","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":274117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchinson, E. C.","contributorId":26373,"corporation":false,"usgs":true,"family":"Hutchinson","given":"E. C.","affiliations":[],"preferred":false,"id":274116,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":60880,"text":"mf1258 - 1980 - Maps showing composition of surficial sediments on the insular shelf of southwestern Puerto Rico","interactions":[],"lastModifiedDate":"2022-04-08T21:40:49.3541","indexId":"mf1258","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1258","title":"Maps showing composition of surficial sediments on the insular shelf of southwestern Puerto Rico","docAbstract":"The limited availability of onshore sand deposits for use in construction appears to be a future major problem in Puerto Rico (U.S. Bureau of Mines, 1972; Committee on Puerto Rico and the Sea, 1974). Consequently, the mining of offshore sand deposits as supplemental sources of construction aggregate may becom e necessary. For this reason, the U.S. Geological Survey and the Department of Natural Resources of the Commonwealth of Puerto Rico have conducted investigations of potential offshore sand deposits on the Puerto Rico insular shelf. This report provides information on the composition of surficial sediments on the southwestern Puerto Rico shelf (fig. 1), an area that may be one of the more favorable potential sites for offshore sand resources.\r\n\r\nWater depths over most of the study area are less than 22 meters (m). The sea floor is composed of live and dead patch and fringing reefs, areas of rock exposures, and sedim ent-covered areas. The adjacent coastline includes prominent embaym ents and a conspicuous rock promontory (Cabo Rojo) connected by a tombolo to the mainland of Puerto Rico. The study area is in the belt of northeast trade winds. Waves approach the coast predominantly from the southeast, resulting in a predominantly westward littoral drift along the south coast (Grove and Trumbull, 1978). Local sand movement on the southern shelf is shown by an active sand wave field south of Bah1a Sucia in which the sand wave crests have migrated toward the southwest (Grove and Trumbull, 1978). The presence of the sand wave field suggests that large volumes of sand having potential for mining are locally present in the study area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1258","collaboration":"Prepared in cooperation with the Department of Natural Resources of the Commonwealth of Puerto Rico","usgsCitation":"Shideler, G.L., 1980, Maps showing composition of surficial sediments on the insular shelf of southwestern Puerto Rico: U.S. Geological Survey Miscellaneous Field Studies Map 1258, 1 Plate: 47.00 × 36.00 inches, https://doi.org/10.3133/mf1258.","productDescription":"1 Plate: 47.00 × 36.00 inches","costCenters":[],"links":[{"id":88874,"rank":300,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1980/1258/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398434,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6868.htm"},{"id":182500,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1980/1258/report-thumb.jpg"}],"scale":"93750","country":"United States","state":"Puerto Rico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -67.3333,\n 17.8583\n ],\n [\n -67.1167,\n 17.8583\n ],\n [\n -67.1167,\n 18.0583\n ],\n [\n -67.3333,\n 18.0583\n ],\n [\n -67.3333,\n 17.8583\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69bdd8","contributors":{"authors":[{"text":"Shideler, Gerald L.","contributorId":89137,"corporation":false,"usgs":true,"family":"Shideler","given":"Gerald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":264546,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43534,"text":"ofr801228 - 1980 - Geologic strip map of parts of Bar X Wash, Bryson Canyon, Jim Canyon, and San Arroyo Ridge quadrangles, Utah and Colorado, showing coal zones and adjacent rocks","interactions":[],"lastModifiedDate":"2022-02-01T22:32:58.194299","indexId":"ofr801228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1228","title":"Geologic strip map of parts of Bar X Wash, Bryson Canyon, Jim Canyon, and San Arroyo Ridge quadrangles, Utah and Colorado, showing coal zones and adjacent rocks","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801228","usgsCitation":"Gualtieri, J.L., 1980, Geologic strip map of parts of Bar X Wash, Bryson Canyon, Jim Canyon, and San Arroyo Ridge quadrangles, Utah and Colorado, showing coal zones and adjacent rocks: U.S. Geological Survey Open-File Report 80-1228, 1 Plate: 32.96 × 27.22 inches, https://doi.org/10.3133/ofr801228.","productDescription":"1 Plate: 32.96 × 27.22 inches","costCenters":[],"links":[{"id":172804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":395254,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11502.htm"},{"id":81183,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1228/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Bar X Wash, Bryson Canyon, Jim Canyon, and San Arroyo Ridge quadrangles","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 39.265\n ],\n [\n -109,\n 39.265\n ],\n [\n -109,\n 39.461\n ],\n [\n -109.25,\n 39.461\n ],\n [\n -109.25,\n 39.265\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881c8","contributors":{"authors":[{"text":"Gualtieri, James Louis","contributorId":46491,"corporation":false,"usgs":true,"family":"Gualtieri","given":"James","email":"","middleInitial":"Louis","affiliations":[],"preferred":false,"id":228339,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66206,"text":"i843C - 1980 - Delineation of flood hazards in the Biscuit Flat quadrangle and New River area, Maricopa County, Arizona","interactions":[],"lastModifiedDate":"2025-08-08T18:27:02.941935","indexId":"i843C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"843","chapter":"C","title":"Delineation of flood hazards in the Biscuit Flat quadrangle and New River area, Maricopa County, Arizona","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i843C","usgsCitation":"Hjalmarson, H., 1980, Delineation of flood hazards in the Biscuit Flat quadrangle and New River area, Maricopa County, Arizona: U.S. Geological Survey IMAP 843, 2 Plates: 29.16 x 40.40 inches and 22.61 x 30.85 inches, https://doi.org/10.3133/i843C.","productDescription":"2 Plates: 29.16 x 40.40 inches and 22.61 x 30.85 inches","costCenters":[],"links":[{"id":493886,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9670.htm","linkFileType":{"id":5,"text":"html"}},{"id":255699,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0843c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255698,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0843c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255697,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0843c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255700,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0843c/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Arizona","county":"Maricopa County","otherGeospatial":"Biscuit Flat quadrangle and New River area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.25,\n 33.944\n ],\n [\n -112.25,\n 33.75\n ],\n [\n -112.125,\n 33.75\n ],\n [\n -112.125,\n 33.944\n ],\n [\n -112.25,\n 33.944\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db67239d","contributors":{"authors":[{"text":"Hjalmarson, H. W.","contributorId":95872,"corporation":false,"usgs":true,"family":"Hjalmarson","given":"H. W.","affiliations":[],"preferred":false,"id":274168,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13381,"text":"ofr80663 - 1980 - Acid-extractable alumina and water-soluble sodium analyses and histograms of Eocene Green River Formation from U.S. Geological Survey coreholes CR-1 and CR-2, Piceance Creek basin, Rio Blanco County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:42","indexId":"ofr80663","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-663","title":"Acid-extractable alumina and water-soluble sodium analyses and histograms of Eocene Green River Formation from U.S. Geological Survey coreholes CR-1 and CR-2, Piceance Creek basin, Rio Blanco County, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80663","usgsCitation":"Donnell, J., and Smith, M.C., 1980, Acid-extractable alumina and water-soluble sodium analyses and histograms of Eocene Green River Formation from U.S. Geological Survey coreholes CR-1 and CR-2, Piceance Creek basin, Rio Blanco County, Colorado: U.S. Geological Survey Open-File Report 80-663, 50 p. :1 fold. ill. (in pocket), maps ;28 cm., https://doi.org/10.3133/ofr80663.","productDescription":"50 p. :1 fold. ill. (in pocket), maps ;28 cm.","costCenters":[],"links":[{"id":145185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0663/report-thumb.jpg"},{"id":41808,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0663/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41809,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0663/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2782","contributors":{"authors":[{"text":"Donnell, John R.","contributorId":84330,"corporation":false,"usgs":true,"family":"Donnell","given":"John R.","affiliations":[],"preferred":false,"id":167713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Marjorie C.","contributorId":78305,"corporation":false,"usgs":true,"family":"Smith","given":"Marjorie","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":167712,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68413,"text":"ha620 - 1980 - Water resources of the Cook Inlet Basin, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:13:24","indexId":"ha620","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"620","title":"Water resources of the Cook Inlet Basin, Alaska","docAbstract":"Ground-water and surface-water systems of Cook Inlet basin, Alaska, are analyzed. Geologic and topographic features that control the movement and regional availability of ground water are explained and illustrated. Five aquifer systems beneath the most populous areas are described. Estimates of ground-water yield were determined for the region by using ground-water data for the populated areas and by extrapolating known subsurface conditions and interpreting subsurface conditions from surficial features in the other areas. Area maps of generalized geology, Quaternary sediment thickness, and general availability of ground water are shown. Surface-water resources are summarized by describing how basin characteristics affect the discharge in streams. Seasonal trend of streamflow for three types of streams is described. Regression equations for 4 streamflow characteristics (annual, monthly minimum, and maximum discharge) were obtained by using gaging station streamflow characteristics and 10 basin characteristics. In the 24 regression equations presented, drainage area is the most significant basin characteristic, but 5 others are used. Maps of mean annual unit runoff and minimum unit yield for 7 consecutive days with a recurrence interval of 10 years are shown. Historic discharge data at gaging stations is tabulated and representative low-flow and flood-flow frequency curves are shown. (USGS)","language":"ENGLISH","doi":"10.3133/ha620","usgsCitation":"Freethey, G.W., and Scully, D.R., 1980, Water resources of the Cook Inlet Basin, Alaska: U.S. Geological Survey Hydrologic Atlas 620, 5 maps : col. ;55 x 41 cm. on 4 sheets 83 x 112 cm., https://doi.org/10.3133/ha620.","productDescription":"5 maps : col. ;55 x 41 cm. on 4 sheets 83 x 112 cm.","costCenters":[],"links":[{"id":188639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89931,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/620/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89932,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/620/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89933,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/620/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89934,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/620/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a4e4b07f02db496c05","contributors":{"authors":[{"text":"Freethey, Geoffrey W.","contributorId":25570,"corporation":false,"usgs":true,"family":"Freethey","given":"Geoffrey","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":278176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scully, David R.","contributorId":6857,"corporation":false,"usgs":true,"family":"Scully","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":278175,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4289,"text":"cir715K - 1980 - Evaluation of planning alternatives for maintaining desirable dissolved-oxygen concentrations in the Willamette River, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:53:54","indexId":"cir715K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"715","chapter":"K","title":"Evaluation of planning alternatives for maintaining desirable dissolved-oxygen concentrations in the Willamette River, Oregon","docAbstract":"For nearly half a century the Willamette River in Oregon experienced severe dissolved-oxygen problems related to large loads of organically rich waste waters from industries and municipalities. Since the mid-1950 's dissolved oxygen quality has gradually improved owing to low-flow augmentation, the achievement of basinwide secondary treatment, and the use of other waste-management practices. As a result, summer dissolved-oxygen levels have increased, salmon runs have returned, and the overall effort is widely regarded as a singular water-quality success. To document the improved dissolved-oxygen regimen, the U.S. Geological Survey conducted intensive studies of the Willamette during the summer low-flow seasons of 1973 and 1974. During each summer the mean daily dissolved-oxygen levels were found to be higher than 5 milligrams per liter throughout the river. Because of the basinwide secondary treatment, carbonaceous deoxygenation rates were low. In addition, almost half of the biochemical oxygen demand entering the Willamette was from diffuse (nonpoint) sources rather than outfalls. These results indicated that point-source biochemical oxygen demand was no longer the primary cause of dissolved-oxygen depletion. Instead, the major causes of deoxygenation were nitrification in a shallow ' surface active ' reach below Salem and an anomalous oxygen demand (believed to be primarily of benthal origin) in Portland Harbor. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir715K","usgsCitation":"Rickert, D.A., Rinella, F.A., Hines, W.G., and McKenzie, S.W., 1980, Evaluation of planning alternatives for maintaining desirable dissolved-oxygen concentrations in the Willamette River, Oregon: U.S. Geological Survey Circular 715, vii, p K1-K30; ill., map ; 26 cm., https://doi.org/10.3133/cir715K.","productDescription":"vii, p K1-K30; ill., map ; 26 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":117202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0715k/report-thumb.jpg"},{"id":31400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0715k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fac76","contributors":{"authors":[{"text":"Rickert, David A.","contributorId":80247,"corporation":false,"usgs":true,"family":"Rickert","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":148733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rinella, F. A.","contributorId":89120,"corporation":false,"usgs":true,"family":"Rinella","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":148735,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hines, W. G.","contributorId":84742,"corporation":false,"usgs":true,"family":"Hines","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":148734,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McKenzie, S. W.","contributorId":66240,"corporation":false,"usgs":true,"family":"McKenzie","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":148732,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":35225,"text":"b1503 - 1980 - Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, Northern California","interactions":[{"subject":{"id":10325,"text":"ofr78827 - 1978 - Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, northern California","indexId":"ofr78827","publicationYear":"1978","noYear":false,"title":"Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, northern California"},"predicate":"SUPERSEDED_BY","object":{"id":35225,"text":"b1503 - 1980 - Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, Northern California","indexId":"b1503","publicationYear":"1980","noYear":false,"title":"Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, Northern California"},"id":1}],"lastModifiedDate":"2017-02-09T13:00:04","indexId":"b1503","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1503","title":"Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, Northern California","docAbstract":"Mount Shasta has erupted, on the average, at least once per 800 years during the last 10,000 years, and about once per 600 years during the last 4,500 years. The last known eruption occurred about 200 radiocarbon years ago. Eruptions during the last 10,000 years produced lava flows and domes on and around the flanks of Mount Shasta, and pyroclastic flows from summit and flank vents extended as far as 20 kilometers from the summit. Most of these eruptions also produced large mudflows, many of which reached more than several tens of kilometers from Mount Shasta. Future eruptions like those of the past could endanger the communities of Weed, Mount Shasta, McCloud, and Dunsmuir, located at or near the base of Mount Shasta. Such eruptions will most likely produce deposits of lithic ash, lava flows, domes, and pyroclastic flows. Lava flows and pyroclastic flows may affect low-and flat-lying ground almost anywhere within about 20 kilometers of the summit of Mount Shasta, and mudflows may cover valley floors and other low areas as much as several tens of kilometers from the volcano. On the basis of its past behavior, Mount Shasta is not likely to erupt large volumes of pumiceous ash in the future; areas subject to the greatest risk from air-fall tephra are located mainly east and within about 50 kilometers of the summit of the volcano. The degree of risk from air-fall tephra decreases progressively as the distance from the volcano increases.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/b1503","usgsCitation":"Miller, C.D., 1980, Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, Northern California: U.S. Geological Survey Bulletin 1503, Report: vii, 43 p.; 3 Plates: 35.50 x 40.0 inches or smaller, https://doi.org/10.3133/b1503.","productDescription":"Report: vii, 43 p.; 3 Plates: 35.50 x 40.0 inches or smaller","numberOfPages":"54","additionalOnlineFiles":"Y","costCenters":[{"id":157,"text":"Cascades Volcano Observatory","active":false,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":295349,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/b1503.jpg"},{"id":63103,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1503/pdf/b1503_plate1.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":280569,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/1503/"},{"id":63104,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1503/pdf/b1503_plate2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":63105,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1503/pdf/b1503_plate3.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":63106,"rank":302,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1503/pdf/b1503_report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Mount Shasta","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.499586,41.097215 ], [ -122.499586,41.608364 ], [ -121.749498,41.608364 ], [ -121.749498,41.097215 ], [ -122.499586,41.097215 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e77c4","contributors":{"authors":[{"text":"Miller, C. Dan","contributorId":38145,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"Dan","affiliations":[],"preferred":false,"id":214280,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7548,"text":"ofr82398 - 1980 - Summary of regional geology, petroleum potential, resource assessment and environmental considerations for oil and gas lease sale area #56","interactions":[],"lastModifiedDate":"2022-09-26T19:10:40.19118","indexId":"ofr82398","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"82-398","title":"Summary of regional geology, petroleum potential, resource assessment and environmental considerations for oil and gas lease sale area #56","docAbstract":"This report summarizes our general knowledge of the petroleum potential, as well as problems and hazards associated with development of petroleum resources in the area proposed for nominations for lease sale number 56. This area includes the U.S. eastern continental margin from the North Carolina-Virginia border south to approximately Cape Canaveral, Florida and from three miles from shore, seaward to include the upper Continental Slope and inner Blake Plateau. The area for possible sales is shown in figure 1; major physiographic features of the region are shown in figure 2.
No wells have been drilled for petroleum within this proposed lease area and no significant commercial production has been obtained onshore in the Southeast Georgia Embayment. The COST GE-1 stratigraphic test well, drilled on the Continental Shelf off Jacksonville, Fla. (fig- 1), reached basement at 3,300 m. The bottom third of the section consists of dominantly continental rocks that are typically poor sources of petroleum (Scholle, 1979) and the rocks that contain organic carbon adequate for generation of petroleum at the well are seen in seismic profiles always at shallow subbottom depths, so they probably have not reached thermal maturity. However, seismic profiles indicate that the sedimentary deposits thicken markedly in a seaward direction where more of the section was deposited under marine conditions; therefore, commercial accumulations of petroleum offshore are more likely.
Several potential sources of environmental hazard exist. Among the most important are hurricanes, the Gulf Stream, and earthquakes. The potential danger from high wind, waves, storm surges, and storm-driven currents associated with hurricanes is obvious. Evidence for significant bottom scour by the Gulf Stream is abundant; such scour is a threat to the stability of bottom-mounted structures. The fast-flowing water also will hamper floating drill rigs and control of drill strings. A major earthquake of about magnitude 6.8 struck Charleston in 1886; it may have been associated with a zone of active seismicity that crosses South Carolina. The likelihood of a repetition of the 1886 event is presently not predictable but a seismic hazard must be assumed to exist.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82398","usgsCitation":"Dillon, W.P., Klitgord, K.D., Paull, C.K., Grow, J.A., Ball, M.M., Dolton, G., Powers, R.B., Khan, A.S., Popenoe, P., and Robb, J.M., 1980, Summary of regional geology, petroleum potential, resource assessment and environmental considerations for oil and gas lease sale area #56: U.S. Geological Survey Open-File Report 82-398, 61 p., https://doi.org/10.3133/ofr82398.","productDescription":"61 p.","costCenters":[],"links":[{"id":407344,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13718.htm","linkFileType":{"id":5,"text":"html"}},{"id":35009,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0398/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":140845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0398/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.5,\n 29\n ],\n [\n -72,\n 29\n ],\n [\n -72,\n 38\n ],\n [\n -81.5,\n 38\n ],\n [\n -81.5,\n 29\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698b9a","contributors":{"authors":[{"text":"Dillon, William P. bdillon@usgs.gov","contributorId":79820,"corporation":false,"usgs":true,"family":"Dillon","given":"William","email":"bdillon@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klitgord, Kim D.","contributorId":82307,"corporation":false,"usgs":true,"family":"Klitgord","given":"Kim","email":"","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704560,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paull, Charles K. 0000-0001-5940-3443","orcid":"https://orcid.org/0000-0001-5940-3443","contributorId":55825,"corporation":false,"usgs":false,"family":"Paull","given":"Charles","email":"","middleInitial":"K.","affiliations":[{"id":7043,"text":"University of North Carolina","active":true,"usgs":false}],"preferred":true,"id":704561,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grow, John A.","contributorId":25943,"corporation":false,"usgs":true,"family":"Grow","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":704562,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ball, Mahlon M.","contributorId":27472,"corporation":false,"usgs":true,"family":"Ball","given":"Mahlon","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704563,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dolton, Gordon","contributorId":50509,"corporation":false,"usgs":true,"family":"Dolton","given":"Gordon","email":"","affiliations":[],"preferred":false,"id":704564,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Powers, Richard B.","contributorId":52248,"corporation":false,"usgs":true,"family":"Powers","given":"Richard","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":704565,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Khan, Abdul S.","contributorId":194534,"corporation":false,"usgs":false,"family":"Khan","given":"Abdul","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":704566,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704567,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Robb, James M.","contributorId":73272,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":704568,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":61078,"text":"mf1232 - 1980 - Maps showing geology of East and West Flower Garden Banks, northwest Gulf of Mexico","interactions":[],"lastModifiedDate":"2019-11-14T16:25:25","indexId":"mf1232","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1232","title":"Maps showing geology of East and West Flower Garden Banks, northwest Gulf of Mexico","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1232","usgsCitation":"Trippet, A.R., 1980, Maps showing geology of East and West Flower Garden Banks, northwest Gulf of Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1232, HTML, https://doi.org/10.3133/mf1232.","productDescription":"HTML","costCenters":[],"links":[{"id":180318,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":105586,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6669.htm","linkFileType":{"id":5,"text":"html"},"description":"6669"}],"scale":"70000","otherGeospatial":"Northwest Gulf of Mexico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -96.9873046875,\n 19.68397023588844\n ],\n [\n -92.021484375,\n 30.14512718337613\n ],\n [\n -96.15234375,\n 30.334953881988564\n ],\n [\n -98.4375,\n 27.644606381943326\n ],\n [\n -98.4375,\n 22.471954507739227\n ],\n [\n -96.9873046875,\n 19.68397023588844\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6058f6","contributors":{"authors":[{"text":"Trippet, Anita R.","contributorId":67159,"corporation":false,"usgs":true,"family":"Trippet","given":"Anita","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":264943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}