With the exception of values from one borehole drilled at Palm Spring and three boreholes drilled around Saline Valley dry lake, eight new heat-flow values in Saline Valley, California, are within or somewhat below the range one would expect for this region of the Basin and Range heat-flow province. The lack of recent volcanism in the area and the apparently normal Basin and Range heat flow suggest that geothermal systems within the valley are stable stationary phases supported by high regional heat flow and forced convection.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791136","usgsCitation":"Mase, C.W., Galanis, S., and Munroe, R.J., 1979, Near-surface heat flow in Saline Valley, California: U.S. Geological Survey Open-File Report 79-1136, iii, 52 p., https://doi.org/10.3133/ofr791136.","productDescription":"iii, 52 p.","costCenters":[],"links":[{"id":423052,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1136/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143086,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1136/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Saline Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.8896135173155,\n 36.85646154756819\n ],\n [\n -117.8896135173155,\n 36.583462201942794\n ],\n [\n -117.58439478156708,\n 36.583462201942794\n ],\n [\n -117.58439478156708,\n 36.85646154756819\n ],\n [\n -117.8896135173155,\n 36.85646154756819\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f0e","contributors":{"authors":[{"text":"Mase, Charles W.","contributorId":8724,"corporation":false,"usgs":true,"family":"Mase","given":"Charles","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galanis, S.P.","contributorId":64242,"corporation":false,"usgs":true,"family":"Galanis","given":"S.P.","affiliations":[],"preferred":false,"id":160977,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Munroe, Robert J.","contributorId":12039,"corporation":false,"usgs":true,"family":"Munroe","given":"Robert","email":"","middleInitial":"J.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":160976,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10510,"text":"ofr791565 - 1979 - Annotated geologic bibliography for the Richfield 1° x 2° Quadrangle, Utah","interactions":[],"lastModifiedDate":"2024-02-26T18:15:49.299728","indexId":"ofr791565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1565","title":"Annotated geologic bibliography for the Richfield 1° x 2° Quadrangle, Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791565","usgsCitation":"Nelson, M., and Bromfield, C.S., 1979, Annotated geologic bibliography for the Richfield 1° x 2° Quadrangle, Utah: U.S. Geological Survey Open-File Report 79-1565, 66 p., https://doi.org/10.3133/ofr791565.","productDescription":"66 p.","costCenters":[],"links":[{"id":145542,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1565/report-thumb.jpg"},{"id":426008,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1565/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Richfield Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,38 ], [ -114,39 ], [ -112,39 ], [ -112,38 ], [ -114,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bd1d","contributors":{"authors":[{"text":"Nelson, M.G.","contributorId":86346,"corporation":false,"usgs":true,"family":"Nelson","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":161520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bromfield, Calvin Stanton","contributorId":12048,"corporation":false,"usgs":true,"family":"Bromfield","given":"Calvin","email":"","middleInitial":"Stanton","affiliations":[],"preferred":false,"id":161519,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8420,"text":"ofr791496 - 1979 - Effects of uranium development on erosion and associated sedimentation in southern San Juan Basin, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr791496","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1496","title":"Effects of uranium development on erosion and associated sedimentation in southern San Juan Basin, New Mexico","docAbstract":"A reconnaissance was made of some of the effects of uranium development on erosion and associated sedimentation in the southern San Juan Basin, where uranium development is concentrated. In general, the effects of exploration on erosion are minor, although erosion may be accelerated by the building of access roads, by activities at the drilling sites, and by close concentration of drilling sites. Areas where the greatest effects on erosion and sedimentation from mining and milling operations have occurred are: (1) in the immediate vicinity of mines and mills, (2) near waste piles, and (3) in stream channels where modifications, such as changes in depth have been caused by discharge of excess mine and mill water. Collapse of tailings piles could result in localized but excessive erosion and sedimentation.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791496","usgsCitation":"Cooley, M.E., 1979, Effects of uranium development on erosion and associated sedimentation in southern San Juan Basin, New Mexico: U.S. Geological Survey Open-File Report 79-1496, iii, 25 p. :map, photos. ;28 cm., https://doi.org/10.3133/ofr791496.","productDescription":"iii, 25 p. :map, photos. ;28 cm.","costCenters":[],"links":[{"id":141504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1496/report-thumb.jpg"},{"id":35991,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1496/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db60ff5f","contributors":{"authors":[{"text":"Cooley, Maurice E.","contributorId":8077,"corporation":false,"usgs":true,"family":"Cooley","given":"Maurice","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157682,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8222,"text":"ofr79414 - 1979 - Ground-water resources of Monroe County, Pennsylvania","interactions":[{"subject":{"id":8222,"text":"ofr79414 - 1979 - Ground-water resources of Monroe County, Pennsylvania","indexId":"ofr79414","publicationYear":"1979","noYear":false,"title":"Ground-water resources of Monroe County, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047444,"text":"70047444 - 1979 - Geology and groundwater resources of Monroe County, Pennsylvania","indexId":"70047444","publicationYear":"1979","noYear":false,"title":"Geology and groundwater resources of Monroe County, Pennsylvania"},"id":1}],"supersededBy":{"id":70047444,"text":"70047444 - 1979 - Geology and groundwater resources of Monroe County, Pennsylvania","indexId":"70047444","publicationYear":"1979","noYear":false,"title":"Geology and groundwater resources of Monroe County, Pennsylvania"},"lastModifiedDate":"2018-04-09T13:37:26","indexId":"ofr79414","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-414","title":"Ground-water resources of Monroe County, Pennsylvania","docAbstract":"Monroe County is on the eastern border of Pennsylvania and includes much of the area popularly called the Poconos. It is an area long used for outdoor recreation and includes a part of the Delaware Water Gap National Recreation Area.
Water resources in the county are derived from precipitation. The Lehigh and Delaware Rivers, bordering the northwestern and southeastern parts, respectively, are the drains for surface-water and ground-water discharge and are essentially unused for water supply.
Water budgets were calculated for average conditions when annual precipitation is 45 in. Sixty percent of this or 27 in. runs off and 65 percent of that runoff or 17 in. moves through the ground-water reservoir. Evapotranspiration varies little between wet and dry years and averages 18 in.
Bedrock consists of Silurian and Devonian sedimentary rocks, which are intensely deformed by folding in the southeastern third of the county and are moderately deformed in the remainder. During the Pleistocene Epoch, glaciers repeatedly advanced across most of the county. The last of these advances deposited a terminal moraine that extends across the southwestern part of the county. The glaciers eroded pre-existing deposits, veneered the upland, and filled valleys with unconsolidated deposits that changed surface-water drainage and altered ground-water gradients.
Water occurs in fractures and solution openings in the consolidated rocks and in intergranular openings in the unconsolidated rocks and weathered calcareous sandstones. Water that reaches the water table moves down the hydraulic gradient to points of discharge, moving both laterally and vertically away from ground-water divides and toward streams. The thickness of the fresh-water system is 800 ft or more, but little water is yielded to wells by aquifers more than 500 ft below land surface. Ground-water recharge is 600 to 650 (gal/min)/mi2; and about 1.6 billion gallons per square mile is stored in the ground-water reservoir.
Currently the most productive wells are in consolidated-rock aquifers; however, specific-capacity data suggest that wells in the unconsolidated deposits have potentially larger yields. Well yield is affected primarily by the distribution, size, and interconnection of the water-bearing openings and by topographic location, available recharge, well-depth, location within the flow system, pumping rate and duration of pumping, and interference from other pumping wells. Potential yields of properly located, drilled, and developed wells have been calculated for the aquifers. The median yields calculated from specific capacity data from the unconsolidated deposits, are 200 gal/min; from the Bloomsburg Formation, 100 gal/min; and from the Poplar Gap Member of the Catskill Formation, 70 gal/min. Median yields of the other units range from 15 to 40 gal/min. In general, enough water for domestic use can be obtained throughout the county. Large-scale development and consumptive use of the ground water will diminish baseflow of the streams.
The temperature of water measured in wells ranges from 44° to 57°F and is largely dependent on altitude of the land surface and depth to the producing zone. Hardness of water in the noncarbonate rocks averages 3 to 4 grains per gallon, or about half that of the carbonate rocks. Water from most of the bedrock aquifers is low in dissolved solids, acidic, and soft. In carbonate rocks, the water tends to be hard and slightly alkaline. Excessive amounts of iron and manganese are encountered in water from the unconsolidated deposits and, locally, from the Catskill and Shawangunk Formations.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79414","collaboration":"Prepared in cooperation with the Topographic and Geologic Survey, Pennsylvania Department of Environmental Resources","usgsCitation":"Carswell, L.D., and Lloyd, O.B., 1979, Ground-water resources of Monroe County, Pennsylvania: U.S. Geological Survey Open-File Report 79-414, Report: 100 p.; 2 Plates: 53.19 x 41.58 inches and 56.43 x 41.52 inches, https://doi.org/10.3133/ofr79414.","productDescription":"Report: 100 p.; 2 Plates: 53.19 x 41.58 inches and 56.43 x 41.52 inches","costCenters":[],"links":[{"id":353263,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0414/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353264,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0414/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":353265,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0414/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":141330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0414/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"Pennsylvania","county":"Monroe County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.75,\n 40.75\n ],\n [\n -74.9,\n 40.75\n ],\n [\n -74.9,\n 41.3\n ],\n [\n -75.75,\n 41.3\n ],\n [\n -75.75,\n 40.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d6ad","contributors":{"authors":[{"text":"Carswell, Louis D.","contributorId":17259,"corporation":false,"usgs":true,"family":"Carswell","given":"Louis","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":157368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lloyd, Orville B. Jr.","contributorId":47639,"corporation":false,"usgs":true,"family":"Lloyd","given":"Orville","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":157367,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8987,"text":"ofr79557 - 1979 - Hydrology and water resources of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport","interactions":[{"subject":{"id":8987,"text":"ofr79557 - 1979 - Hydrology and water resources of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport","indexId":"ofr79557","publicationYear":"1979","noYear":false,"title":"Hydrology and water resources of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport"},"predicate":"SUPERSEDED_BY","object":{"id":68395,"text":"ha616 - 1980 - Hydrology and water resources of the lower Merrimack River Basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport","indexId":"ha616","publicationYear":"1980","noYear":false,"title":"Hydrology and water resources of the lower Merrimack River Basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport"},"id":1}],"supersededBy":{"id":68395,"text":"ha616 - 1980 - Hydrology and water resources of the lower Merrimack River Basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport","indexId":"ha616","publicationYear":"1980","noYear":false,"title":"Hydrology and water resources of the lower Merrimack River Basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport"},"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr79557","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-557","title":"Hydrology and water resources of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79557","usgsCitation":"Gay, F.B., and Delaney, D.F., 1979, Hydrology and water resources of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport: U.S. Geological Survey Open-File Report 79-557, 52 p. :ill., maps (some fold. col.) ;28 cm., https://doi.org/10.3133/ofr79557.","productDescription":"52 p. :ill., maps (some fold. col.) ;28 cm.","costCenters":[],"links":[{"id":144258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e7a1","contributors":{"authors":[{"text":"Gay, Frederick B.","contributorId":102052,"corporation":false,"usgs":true,"family":"Gay","given":"Frederick","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":158669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Delaney, David F.","contributorId":41797,"corporation":false,"usgs":false,"family":"Delaney","given":"David","email":"","middleInitial":"F.","affiliations":[{"id":27261,"text":"U.S. Army Construction Engineering Research Laboratory, Champaig","active":true,"usgs":false}],"preferred":false,"id":158668,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9392,"text":"ofr791249 - 1979 - Chemical analyses of deep core coal and shale samples from the Almond Formation, Washakie Basin, Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2018-08-29T12:20:14","indexId":"ofr791249","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1249","title":"Chemical analyses of deep core coal and shale samples from the Almond Formation, Washakie Basin, Sweetwater County, Wyoming","docAbstract":"During gas and oil exploration efforts in the Washakie Basin in Sweetwater County, Wyoming, undertaken by Ladd Petroleum Co. (a subsidiary of Utah International Inc.) core from the Upper Cretaceous Almond Formation of the Mesaverde Group was collected from their 1-22 Federal well. (See figure 1 for location.) From this core three coal and two carbonaceous shale samples, orginally at depths ranging from 3,091 to 3,116 m (see table 1 for descriptions), were selected and given to the U.S. Geological Survey for study. Results of chemical analyses on the samples and a comparison of these analyses with analyses of near-surface Almond Formation coal samples in Carbon County, Wyoming, are the topics of this report.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791249","usgsCitation":"Hatch, J.R., and Barclay, C.V., 1979, Chemical analyses of deep core coal and shale samples from the Almond Formation, Washakie Basin, Sweetwater County, Wyoming: U.S. Geological Survey Open-File Report 79-1249, 16 p., https://doi.org/10.3133/ofr791249.","productDescription":"16 p.","costCenters":[],"links":[{"id":356919,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1249/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1249/report-thumb.jpg"}],"country":"United States","county":"Sweetwater County","otherGeospatial":"Washakie Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108,\n 41\n ],\n [\n -107,\n 41\n ],\n [\n -107,\n 42\n ],\n [\n -108,\n 42\n ],\n [\n -108,\n 41\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ae4","contributors":{"authors":[{"text":"Hatch, Joseph R. 0000-0001-9257-0278 jrhatch@usgs.gov","orcid":"https://orcid.org/0000-0001-9257-0278","contributorId":722,"corporation":false,"usgs":true,"family":"Hatch","given":"Joseph","email":"jrhatch@usgs.gov","middleInitial":"R.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":159595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barclay, C.S. Venable","contributorId":89525,"corporation":false,"usgs":true,"family":"Barclay","given":"C.S.","email":"","middleInitial":"Venable","affiliations":[],"preferred":false,"id":159596,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9369,"text":"ofr79553 - 1979 - Magnitude and frequency of floods in western Oregon","interactions":[],"lastModifiedDate":"2017-02-07T09:24:39","indexId":"ofr79553","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-553","title":"Magnitude and frequency of floods in western Oregon","docAbstract":"A method for estimating the magnitude and frequency of floods is presented for unregulated streams in western Oregon. Equations relating flood magnitude to basin characteristics were developed for exceedance probabilities of 0.5 to 0.01 (2- to 100-year recurrence intervals). Separate equations are presented for four regions: Coast, Willamette, Rogue-Umpqua, and High Cascades. Also presented are values of flood discharges for selected exceedance probabilities and of basin characteristics for all gaging stations used in the analysis. Included are data for 230 stations in Oregon, 6 stations in southwestern Washington, and 3 stations in northwestern California. Drainage areas used in the analysis range from 0.21 to 7,280 square miles. Also included are maximum discharges for all western Oregon stations used in the analysis. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79553","usgsCitation":"Harris, D.D., Hubbard, L.L., and Hubbard, L.E., 1979, Magnitude and frequency of floods in western Oregon: U.S. Geological Survey Open-File Report 79-553, v, 51 p., 2 sheets :ill., maps (2 fold. in pocket) ;27 cm., https://doi.org/10.3133/ofr79553.","productDescription":"v, 51 p., 2 sheets :ill., maps (2 fold. in pocket) ;27 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":37082,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0553/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37080,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0553/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141432,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0553/report-thumb.jpg"},{"id":37081,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0553/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649622","contributors":{"authors":[{"text":"Harris, David Dell","contributorId":24338,"corporation":false,"usgs":true,"family":"Harris","given":"David","email":"","middleInitial":"Dell","affiliations":[],"preferred":false,"id":159557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubbard, Larry L.","contributorId":91492,"corporation":false,"usgs":true,"family":"Hubbard","given":"Larry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hubbard, Lawrence E.","contributorId":57848,"corporation":false,"usgs":true,"family":"Hubbard","given":"Lawrence","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159558,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9301,"text":"ofr79979 - 1979 - Hydrologic data for wells, springs, and streams in Boulder County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr79979","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-979","title":"Hydrologic data for wells, springs, and streams in Boulder County, Colorado","docAbstract":"Hydrologic data collected in 1975-77 as part of a comprehensive water-resources investigation of Boulder County, Colo., by the U.S. Geological Survey in cooperation with the Boulder County Health Department and the Colorado Geological Survey are presented in this report. The data, in tabular and graphic form, consist of water-quality analyses of selected constituents and geohydrologic-site, water-treatment, and sewage-treatment data for 609 wells and 48 springs; water-quality analyses for 102 of the wells and 9 of the springs; water-quality analyses of streamflow from 34 sites; and specific conductance and water-temperature measurements of streamflow from 3 sites. State and local officials in Boulder County may find these data useful in planning for residential, commercial, and industrial development. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79979","usgsCitation":"Hall, D.C., Boyd, E.L., and Cain, D., 1979, Hydrologic data for wells, springs, and streams in Boulder County, Colorado: U.S. Geological Survey Open-File Report 79-979, iv, 110 p. :ill., maps (1 fold. in pocket) ;28 cm., https://doi.org/10.3133/ofr79979.","productDescription":"iv, 110 p. :ill., maps (1 fold. in pocket) ;28 cm.","costCenters":[],"links":[{"id":110106,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30424.htm","linkFileType":{"id":5,"text":"html"},"description":"30424"},{"id":140898,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0979/report-thumb.jpg"},{"id":37015,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0979/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37016,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0979/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db607c22","contributors":{"authors":[{"text":"Hall, Dennis C.","contributorId":95473,"corporation":false,"usgs":true,"family":"Hall","given":"Dennis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":159446,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boyd, Elaine L.","contributorId":103277,"corporation":false,"usgs":true,"family":"Boyd","given":"Elaine","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159448,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cain, Doug","contributorId":101655,"corporation":false,"usgs":true,"family":"Cain","given":"Doug","email":"","affiliations":[],"preferred":false,"id":159447,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10181,"text":"ofr791210 - 1979 - Titaniferous magnetite in the layered intrusive complex at Lakathah, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr791210","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1210","title":"Titaniferous magnetite in the layered intrusive complex at Lakathah, Kingdom of Saudi Arabia","docAbstract":"The Lakathah layered intrusive complex about 90 km east of Qunfudhah contains significant resources of low-grade titanium-bearing rock. The complex is about 10 km in diameter and consists of three principal units: an outer syenite ring, an intermediate diorite-gabbro zone, and a central pyroxenite-hornblendite core. The principal mineralization zone is in the ultramafic core of the complex. \r\n\r\nThe titanium is mainly in titaniferous magnetite, but some is in ilmenite intergrown with magnetite and in the titanium-bearing hornblende, kaersutite. The titaniferous magnetite is in concordant lenses and veinlets and is disseminated throughout the host rock. The lenses and veins range from a few centimeters to 3 m in width and are as much as 50 m long. The layered disseminated bodies contain as much as 25 percent magnetite. \r\n\r\nExploratory drilling showed that an area 500 by 1000 m contains titaniferous rock averaging about 6.2 percent TiO2. This mineralized zone contains about 175,000,000 tons per 100 m depth. Material of this grade is not commercial at this time, but may be a future resource. Alluvial deposits along the Red Sea near Al Qunfudhah should be tested for possible deposits of titaniferous sand.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791210","usgsCitation":"Martin, C., Roberts, R.J., and Stoeser, D.B., 1979, Titaniferous magnetite in the layered intrusive complex at Lakathah, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 79-1210, ii, 39 p., 1 over-size sheet :ill.;28 cm., https://doi.org/10.3133/ofr791210.","productDescription":"ii, 39 p., 1 over-size sheet :ill.;28 cm.","costCenters":[],"links":[{"id":143045,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1210/report-thumb.jpg"},{"id":38027,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1210/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38028,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1210/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f96e2","contributors":{"authors":[{"text":"Martin, Conrad","contributorId":28245,"corporation":false,"usgs":true,"family":"Martin","given":"Conrad","email":"","affiliations":[],"preferred":false,"id":160953,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, Ralph Jackson","contributorId":63010,"corporation":false,"usgs":true,"family":"Roberts","given":"Ralph","email":"","middleInitial":"Jackson","affiliations":[],"preferred":false,"id":160954,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoeser, D. B.","contributorId":18735,"corporation":false,"usgs":true,"family":"Stoeser","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":160952,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10179,"text":"ofr791622 - 1979 - Rutile mineralization in the White Mountain andalusite deposit, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr791622","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1622","title":"Rutile mineralization in the White Mountain andalusite deposit, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791622","usgsCitation":"Marsh, S.P., 1979, Rutile mineralization in the White Mountain andalusite deposit, California: U.S. Geological Survey Open-File Report 79-1622, 9 p. :maps ;28 cm., https://doi.org/10.3133/ofr791622.","productDescription":"9 p. :maps ;28 cm.","costCenters":[],"links":[{"id":143176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1622/report-thumb.jpg"},{"id":38026,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1622/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cad5","contributors":{"authors":[{"text":"Marsh, Sherman P.","contributorId":42950,"corporation":false,"usgs":true,"family":"Marsh","given":"Sherman","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":160949,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10176,"text":"ofr791147 - 1979 - Multichannel seismic-reflection profiles collected in 1977 in the northern Bering Sea","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr791147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1147","title":"Multichannel seismic-reflection profiles collected in 1977 in the northern Bering Sea","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791147","usgsCitation":"Marlow, M.S., and Cooper, A.K., 1979, Multichannel seismic-reflection profiles collected in 1977 in the northern Bering Sea: U.S. Geological Survey Open-File Report 79-1147, 3 p. :map ;28 cm., https://doi.org/10.3133/ofr791147.","productDescription":"3 p. :map ;28 cm.","costCenters":[],"links":[{"id":111864,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/13583","linkFileType":{"id":5,"text":"html"}},{"id":143173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698c7f","contributors":{"authors":[{"text":"Marlow, Michael S.","contributorId":72775,"corporation":false,"usgs":true,"family":"Marlow","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":160945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, Alan K. acooper@usgs.gov","contributorId":2854,"corporation":false,"usgs":true,"family":"Cooper","given":"Alan","email":"acooper@usgs.gov","middleInitial":"K.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":160944,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8419,"text":"ofr791291 - 1979 - Hydrogeologic features of the alluvial deposits in the Nowood River drainage area, Bighorn Basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr791291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1291","title":"Hydrogeologic features of the alluvial deposits in the Nowood River drainage area, Bighorn Basin, Wyoming","docAbstract":"In the Nowood River drainage area, Wyoming, the principal deposits comprising the alluvial aquifer include the flood-plain and younger (generally undissected) alluvial-fan deposits and a unique boulder-fan gravel. Other deposits mapped, but virtually nonwater yielding, are the older (dissected) alluvial-fan, pediment, and terrace deposits. Terraces are capped by gravel and form levels at 30-40, 45-100, 120-150, 200-260, and 280-330 feet above the Nowood River. The thickness of the alluvial aquifer indicated from the sparse well-log data and 42 surface resistivity measurements is between 25 and 50 feet along the Nowood River and more than 60 feet along Tensleep and Paint Rock Creeks. The resistivity measurements indicate a buried bedrock ridge below the boulder-fan gravel between Paint Rock and Medicine Lodge Creeks and a buried channel filled by alluvium along Tensleep Creek. Well yields from the alluvial aquifer are estimated to be low. The most favorable areas for ground-water development are from the flood-plain alluvium along Tensleep Creek and from the boulder-fan gravel and adjoining flood-plain alluvium along Paint Rock and Medicine Creeks. Along the Nowood River the flood-plain alluvium, although its yields are small, has the best potential for ground-water development. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791291","usgsCitation":"Cooley, M.E., and Head, W.J., 1979, Hydrogeologic features of the alluvial deposits in the Nowood River drainage area, Bighorn Basin, Wyoming (WRI/OFR): U.S. Geological Survey Open-File Report 79-1291, v, 60 p. :ill., maps (4 fold. in pocket) ;27 cm., https://doi.org/10.3133/ofr791291.","productDescription":"v, 60 p. :ill., maps (4 fold. in pocket) ;27 cm.","costCenters":[],"links":[{"id":141485,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1291/report-thumb.jpg"},{"id":35988,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1291/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35989,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1291/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35990,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1291/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627df4","contributors":{"authors":[{"text":"Cooley, M. E.","contributorId":89868,"corporation":false,"usgs":true,"family":"Cooley","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Head, William J.","contributorId":96686,"corporation":false,"usgs":true,"family":"Head","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":157681,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8418,"text":"ofr79912 - 1979 - Geophysical and lithologic logs for 1978 coal drilling in Mountrail, Renville, Ward, and Williams counties, North Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr79912","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-912","title":"Geophysical and lithologic logs for 1978 coal drilling in Mountrail, Renville, Ward, and Williams counties, North Dakota","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79912","usgsCitation":"Cook, S.M., and Spencer, J.M., 1979, Geophysical and lithologic logs for 1978 coal drilling in Mountrail, Renville, Ward, and Williams counties, North Dakota: U.S. Geological Survey Open-File Report 79-912, i, 124 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr79912.","productDescription":"i, 124 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0912/report-thumb.jpg"},{"id":35987,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0912/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c24b","contributors":{"authors":[{"text":"Cook, Susan M.","contributorId":95058,"corporation":false,"usgs":true,"family":"Cook","given":"Susan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":157679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spencer, John M.","contributorId":79883,"corporation":false,"usgs":true,"family":"Spencer","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":157678,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9524,"text":"ofr791100 - 1979 - Coal exploratory drilling; a cost percentage comparison of three methods","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr791100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1100","title":"Coal exploratory drilling; a cost percentage comparison of three methods","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791100","usgsCitation":"Hobbs, R., 1979, Coal exploratory drilling; a cost percentage comparison of three methods: U.S. Geological Survey Open-File Report 79-1100, 11 p. :graphs, ill. ;28 cm., https://doi.org/10.3133/ofr791100.","productDescription":"11 p. :graphs, ill. ;28 cm.","costCenters":[],"links":[{"id":142055,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1100/report-thumb.jpg"},{"id":37241,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1100/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5dde98","contributors":{"authors":[{"text":"Hobbs, Robert G.","contributorId":44542,"corporation":false,"usgs":true,"family":"Hobbs","given":"Robert G.","affiliations":[],"preferred":false,"id":159832,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10174,"text":"ofr791667 - 1979 - Hydrocarbon prospects for the Navarin and the Aleutian Basin provinces","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr791667","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1667","title":"Hydrocarbon prospects for the Navarin and the Aleutian Basin provinces","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791667","usgsCitation":"Marlow, M.S., and Cooper, A.K., 1979, Hydrocarbon prospects for the Navarin and the Aleutian Basin provinces: U.S. Geological Survey Open-File Report 79-1667, iii, 64 p. ;28 cm., https://doi.org/10.3133/ofr791667.","productDescription":"iii, 64 p. ;28 cm.","costCenters":[],"links":[{"id":143156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1667/report-thumb.jpg"},{"id":38021,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1667/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db6292f2","contributors":{"authors":[{"text":"Marlow, Michael S.","contributorId":72775,"corporation":false,"usgs":true,"family":"Marlow","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":160941,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, Alan K. acooper@usgs.gov","contributorId":2854,"corporation":false,"usgs":true,"family":"Cooper","given":"Alan","email":"acooper@usgs.gov","middleInitial":"K.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":160940,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10159,"text":"ofr79348 - 1979 - Water budget and mathematical model of the Coconino Aquifer, southern Navajo County, Arizona","interactions":[],"lastModifiedDate":"2018-01-29T11:51:09","indexId":"ofr79348","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-348","title":"Water budget and mathematical model of the Coconino Aquifer, southern Navajo County, Arizona","docAbstract":"The main source of water in the 3,400-square-mile area of southern Navajo County is the large volume of ground water in storage in the Coconino aquifer, which consists of the Coconino Sandstone, the uppermost part of the underlying Supai Formation, and the overlying Kaibab Limestone. The amount of water withdrawn from the aquifer increased from about 13,800 acre-feet in 1960 to 38,400 acre-feet in 1972. As industrial and agricultural development continues, the amount of withdrawal probably will increase greatly.
Aquifer tests indicate that the hydraulic conductivity of the aquifer ranges from 8 to 40 feet per day; however, a flow-net analysis indicates that the hydraulic conductivity may be as much as 80 feet per day in the north-central part of the area. In the southern and central parts of the area the aquifer is unconfined, and the storage coefficient is estimated to be about 0.15. In the northern and eastern parts the aquifer is confined, and the storage coefficient ranges from 0.00013 to 0.0014.
A mathematical model was developed to simulate the groundwater system and to provide a management tool for estimating the effects of present and future ground-water withdrawals. The model indicates that the inflow to and outflow from the aquifer were about 105,600 acre-feet in 1960 prior to extensive ground-water development and that about 192,000 acre-feet of water was derived from groundwater storage between 1960 and 1972. The mathematical model provides an approximation of the Coconino aquifer and can be used to estimate the future response of the aquifer.
Water samples were collected from 31 wells and springs in eastern Idaho and western Wyoming to help evaluate the potential geothermal resources in the Teton River area, Idaho. The water analyses included the common anions and cations, oxygen-18, deuterium, and several minor elements. Actual temperatures of the sampled thermal waters ranged from 23° to 49°C. Estimated aquifer temperatures, as derived from geochemical thermometers, ranged from 45° to 145°C based on silica concentrations and 45° to 205°C based on sodium-potassium-calcium ratios. Using the cation thermometer, two analyses indicated aquifer temperatures that were lower than the actual measured temperatures. Estimated temperatures using a mixing-model method ranged from 205° to 320°C, the higher temperature being of questionable value. The different methods used to estimate aquifer temperatures showed little correlation. On the basis of isotope data, the warm waters may be of local meteoric origin and have not been heated enough to react significantly with the aquifer rocks, or they originated as precipitation at high altitude and great distance from the area.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79687","collaboration":"Prepared in cooperation with the U.S. Department of Energy","usgsCitation":"Crosthwaite, E., 1979, Chemical analyses of ground water related to geothermal investigations in the Teton River area, eastern Idaho: U.S. Geological Survey Open-File Report 79-687, i, 14 p., https://doi.org/10.3133/ofr79687.","productDescription":"i, 14 p.","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":403546,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0687/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0687/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Teton River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.912434,43.755291 ], [ -111.912434,43.962399 ], [ -111.591358,43.962399 ], [ -111.591358,43.755291 ], [ -111.912434,43.755291 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a9c","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":157767,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10149,"text":"ofr79971 - 1979 - Late Pleistocene chrysomonad cysts from core 7, Clear Lake, Lake County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr79971","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-971","title":"Late Pleistocene chrysomonad cysts from core 7, Clear Lake, Lake County, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79971","usgsCitation":"Mahood, A.M., and Adam, D.P., 1979, Late Pleistocene chrysomonad cysts from core 7, Clear Lake, Lake County, California: U.S. Geological Survey Open-File Report 79-971, 16 p., 4 over-size sheets :ill., map ;28 cm., https://doi.org/10.3133/ofr79971.","productDescription":"16 p., 4 over-size sheets :ill., map ;28 cm.","costCenters":[],"links":[{"id":143481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0971/report-thumb.jpg"},{"id":37992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0971/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b7f","contributors":{"authors":[{"text":"Mahood, Albert M.","contributorId":75150,"corporation":false,"usgs":true,"family":"Mahood","given":"Albert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adam, David P.","contributorId":36132,"corporation":false,"usgs":true,"family":"Adam","given":"David","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":160895,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10148,"text":"ofr791431 - 1979 - Techniques used for the cleaning, concentration, and observation of chrysomonad cysts from sediments","interactions":[],"lastModifiedDate":"2023-08-22T20:59:05.993808","indexId":"ofr791431","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1431","title":"Techniques used for the cleaning, concentration, and observation of chrysomonad cysts from sediments","docAbstract":"This report documents the techniques that we use to clean and concentrate chrysomonad cysts prior to examining them under a scanning electron microscope. Like diatoms, chrysomonad cysts are composed of opaline silica; the method we use is basically the same as one of the methods commonly used to prepare diatoms.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791431","usgsCitation":"Mahood, A.D., and Adam, D.P., 1979, Techniques used for the cleaning, concentration, and observation of chrysomonad cysts from sediments: U.S. Geological Survey Open-File Report 79-1431, 5 p., https://doi.org/10.3133/ofr791431.","productDescription":"5 p.","costCenters":[],"links":[{"id":143480,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1431/report-thumb.jpg"},{"id":420040,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1431/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685a7d","contributors":{"authors":[{"text":"Mahood, Albert D.","contributorId":97493,"corporation":false,"usgs":true,"family":"Mahood","given":"Albert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":160894,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adam, David P.","contributorId":36132,"corporation":false,"usgs":true,"family":"Adam","given":"David","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":160893,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10147,"text":"ofr791649 - 1979 - Two oil types on the North Slope of Alaska: implications for future exploration","interactions":[{"subject":{"id":10147,"text":"ofr791649 - 1979 - Two oil types on the North Slope of Alaska: implications for future exploration","indexId":"ofr791649","publicationYear":"1979","noYear":false,"title":"Two oil types on the North Slope of Alaska: implications for future exploration"},"predicate":"SUPERSEDED_BY","object":{"id":70011728,"text":"70011728 - 1981 - Two oil types on North slope of Alaska: Implications for exploration","indexId":"70011728","publicationYear":"1981","noYear":false,"title":"Two oil types on North slope of Alaska: Implications for exploration"},"id":1}],"supersededBy":{"id":70011728,"text":"70011728 - 1981 - Two oil types on North slope of Alaska: Implications for exploration","indexId":"70011728","publicationYear":"1981","noYear":false,"title":"Two oil types on North slope of Alaska: Implications for exploration"},"lastModifiedDate":"2023-08-28T16:46:37.403394","indexId":"ofr791649","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1649","title":"Two oil types on the North Slope of Alaska: implications for future exploration","docAbstract":"Forty oil samples from across the North Slope of Alaska have been analyzed by the U.S. Bureau of Mines and the U.S. Geological Survey. Results of these analyses suggest two separate genetic oil types. The first type, the Simpson-Umiat oil type, occurs in reservoir rocks of Cretaceous and Quaternary age and includes oils from seeps in the Skull Cliff, Cape Simpson, Manning Point, and Ungoon Point areas; the Wolf Creek test well 3, and the Umiat oil field. These are higher gravity, low-sulfur oils with no, or slight, odd-numbered n-alkane predominance and pristane to phytane ratios greater than 1.5. The second type, the Barrow-Prudhoe oil type, occurs in reservoir rocks of Carboniferous to Cretaceous age and includes oils from South Barrow gas field, Prudhoe Bay oil field, and the Fish Creek test well 1. Physical properties of Barrow-Prudhoe oils are variable, but in general the oils are medium-gravity, high-sulfur oils with a slight even-numbered n-alkane predominance and pristane to phytane ratios of less than 1.5. The two types are believed to originate from different source rocks; the Barrow-Prudhoe type may have originated from a carbonate or other iron-deficient source rock, and the Simpson-Umiat type from a siliciclastic source rock. Occurrences of the two oil types, when outlined on a map, indicate at least two exploration fairways. The fairway for the Barrow-Prudhoe type is along the Barrow arch, and the fairway for the Simpson-Umiat type is the area of the best reservoir development for the Nanushuk Group.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791649","usgsCitation":"Magoon, L.B., and Claypool, G.E., 1979, Two oil types on the North Slope of Alaska: implications for future exploration: U.S. Geological Survey Open-File Report 79-1649, 13 p., https://doi.org/10.3133/ofr791649.","productDescription":"13 p.","costCenters":[],"links":[{"id":420193,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1649/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143479,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1649/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"North Slope","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -44.26437145587704,\n -17.892934656589816\n ],\n [\n -44.26437145587704,\n -19.132095555888\n ],\n [\n -42.65007384041027,\n -19.132095555888\n ],\n [\n -42.65007384041027,\n -17.892934656589816\n ],\n [\n -44.26437145587704,\n -17.892934656589816\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -170.4186309255835,\n 71.2434612382597\n ],\n [\n -170.4186309255835,\n 68.56040199188811\n ],\n [\n -141.06065965042941,\n 68.56040199188811\n ],\n [\n -141.06065965042941,\n 71.2434612382597\n ],\n [\n -170.4186309255835,\n 71.2434612382597\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db62399c","contributors":{"authors":[{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":160891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Claypool, George Edwin","contributorId":99972,"corporation":false,"usgs":true,"family":"Claypool","given":"George","email":"","middleInitial":"Edwin","affiliations":[],"preferred":false,"id":160892,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10146,"text":"ofr79548 - 1979 - Petroleum geology of Cook Inlet basin, Alaska: An exploration model","interactions":[],"lastModifiedDate":"2022-10-07T19:46:41.79808","indexId":"ofr79548","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-548","title":"Petroleum geology of Cook Inlet basin, Alaska: An exploration model","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79548","usgsCitation":"Magoon, L.B., and Claypool, G.E., 1979, Petroleum geology of Cook Inlet basin, Alaska: An exploration model: U.S. Geological Survey Open-File Report 79-548, 44 p., https://doi.org/10.3133/ofr79548.","productDescription":"44 p.","costCenters":[],"links":[{"id":111853,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/11278","linkFileType":{"id":5,"text":"html"}},{"id":143478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":408121,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75005.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Cook Inlet basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -154.423828125,\n 58.88194208135912\n ],\n [\n -149.4580078125,\n 58.88194208135912\n ],\n [\n -149.4580078125,\n 61.501734289732326\n ],\n [\n -154.423828125,\n 61.501734289732326\n ],\n [\n -154.423828125,\n 58.88194208135912\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687e99","contributors":{"authors":[{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":160889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Claypool, George E.","contributorId":76312,"corporation":false,"usgs":true,"family":"Claypool","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160890,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9682,"text":"ofr79270 - 1979 - Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia","interactions":[{"subject":{"id":9682,"text":"ofr79270 - 1979 - Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia","indexId":"ofr79270","publicationYear":"1979","noYear":false,"title":"Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":6058,"text":"pp1136 - 1979 - Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia","indexId":"pp1136","publicationYear":"1979","noYear":false,"title":"Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia"},"id":1}],"supersededBy":{"id":6058,"text":"pp1136 - 1979 - Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia","indexId":"pp1136","publicationYear":"1979","noYear":false,"title":"Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia"},"lastModifiedDate":"2019-04-29T11:39:38","indexId":"ofr79270","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-270","title":"Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia","docAbstract":"A coupled flow-temperature model has been developed and verified for a 27.9-km reach of the Chattahoochee River between Buford Dam and Norcross, Ga. Flow in this reach of the Chattahoochee is continuous but highly regulated by Buford Dam, a flood-control and hydroelectric facility located near Buford, Ga. Calibration and verification utilized two sets of data collected under highly unsteady discharge conditions. Existing solution techniques, with certain minor improvements, were applied to verify the existing technology of flow and transport modeling. A linear, implicit finite-difference flow model was coupled with implicit, finite-difference transport and temperature models. Both the conservative and nonconservative forms of the transport equation were solved, and the difference in the predicted concentrations of dye were found to be insignificant. The temperature model, therefore, was based on the simpler nonconservative form of the transport equation. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr79270","usgsCitation":"Jobson, H.E., and Keefer, T.N., 1979, Modeling highly transient flow, mass, and heat transport in the Chattahoochee River near Atlanta, Georgia: U.S. Geological Survey Open-File Report 79-270, xv, 139 p. , https://doi.org/10.3133/ofr79270.","productDescription":"xv, 139 p. ","numberOfPages":"160","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":363251,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0270/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140966,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":" https://pubs.usgs.gov/of/1979/0270/report-thumb.jpg"}],"country":"United States","state":"Georgia","city":"Atlanta, Buford, Norcross","otherGeospatial":" Buford Dam, Chattahoochee River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {\n \"stroke\": \"#555555\",\n \"stroke-width\": 2,\n \"stroke-opacity\": 1,\n \"fill\": \"#555555\",\n \"fill-opacity\": 0.5\n },\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.71307373046874,\n 34.496370914707285\n ],\n [\n -83.66363525390625,\n 34.45448326886294\n ],\n [\n -83.64852905273438,\n 34.40464357107094\n ],\n [\n -83.64715576171875,\n 34.35137289731883\n ],\n [\n -83.70208740234375,\n 34.25494631082515\n ],\n [\n -83.80508422851564,\n 34.226564487211114\n ],\n [\n -83.87512207031251,\n 34.15727269301868\n ],\n [\n -84.01107788085938,\n 34.008273470938335\n ],\n [\n -84.28024291992188,\n 33.792843773631844\n ],\n [\n -84.5343017578125,\n 33.7597402884442\n ],\n [\n -84.58786010742188,\n 33.80197351806589\n ],\n [\n -84.59609985351562,\n 33.865854454071865\n ],\n [\n -84.5672607421875,\n 33.950195282756994\n ],\n [\n -84.45877075195312,\n 34.07882486401267\n ],\n [\n -84.30221557617188,\n 34.24813554589752\n ],\n [\n -84.13330078125,\n 34.37517887533528\n ],\n [\n -84.08660888671875,\n 34.43862840686652\n ],\n [\n -83.96987915039061,\n 34.48957975202644\n ],\n [\n -83.88473510742186,\n 34.49750272138159\n ],\n [\n -83.71307373046874,\n 34.496370914707285\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699951","contributors":{"authors":[{"text":"Jobson, Harvey E.","contributorId":27032,"corporation":false,"usgs":true,"family":"Jobson","given":"Harvey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keefer, Thomas N.","contributorId":43752,"corporation":false,"usgs":true,"family":"Keefer","given":"Thomas","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":160118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9526,"text":"ofr791522 - 1979 - Guidelines for logging, describing, and sampling cores and cuttings of coal and associated rocks at the drill site","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr791522","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1522","title":"Guidelines for logging, describing, and sampling cores and cuttings of coal and associated rocks at the drill site","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791522","usgsCitation":"Hobbs, R., 1979, Guidelines for logging, describing, and sampling cores and cuttings of coal and associated rocks at the drill site: U.S. Geological Survey Open-File Report 79-1522, [i], 23 p. :ill. ;28 cm., https://doi.org/10.3133/ofr791522.","productDescription":"[i], 23 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":142073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1522/report-thumb.jpg"},{"id":37243,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1522/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aeef","contributors":{"authors":[{"text":"Hobbs, Robert G.","contributorId":44542,"corporation":false,"usgs":true,"family":"Hobbs","given":"Robert G.","affiliations":[],"preferred":false,"id":159836,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8973,"text":"ofr79955 - 1979 - High-resolution seismic profiling data from the upper continental slope of the northern Gulf of Mexico","interactions":[],"lastModifiedDate":"2024-06-03T16:45:29.20895","indexId":"ofr79955","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-955","title":"High-resolution seismic profiling data from the upper continental slope of the northern Gulf of Mexico","docAbstract":"From July 28 through December 20, 1975, the U.S. Geological Survey conducted a high-resolution geophysical survey on the Upper Continental Slope in the Gulf of Mexico north of Latitude 26°N. The survey was limited to water depths between 100 m and 1000 m with seismic lines spaced from 7.5 to 18.5 km apart in a reconnaissance grid pattern. The data were collected by Western Geophysical Company of America under an exclusive contract with the Geological Survey.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79955","usgsCitation":"Garrison, L.E., 1979, High-resolution seismic profiling data from the upper continental slope of the northern Gulf of Mexico: U.S. Geological Survey Open-File Report 79-955, 8 p., https://doi.org/10.3133/ofr79955.","productDescription":"8 p.","costCenters":[],"links":[{"id":429454,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0955/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142382,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0955/report-thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Louisiana, Mississippi, Texas","otherGeospatial":"northern Gulf of Mexico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -96.13190153946888,\n 30.008342872844068\n ],\n [\n -96.13190153946888,\n 28.500366711147066\n ],\n [\n -82.70271628013394,\n 28.500366711147066\n ],\n [\n -82.70271628013394,\n 30.008342872844068\n ],\n [\n -96.13190153946888,\n 30.008342872844068\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f5cd","contributors":{"authors":[{"text":"Garrison, Louis E.","contributorId":91793,"corporation":false,"usgs":true,"family":"Garrison","given":"Louis","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":158647,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}