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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b8b6","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":528383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5637,"text":"pp1052 - 1979 - A study of global sand seas","interactions":[{"subject":{"id":8927,"text":"ofr78405 - 1978 - Techniques for the evaluation of surface wind data in terms of eolian sand drift","indexId":"ofr78405","publicationYear":"1978","noYear":false,"title":"Techniques for the evaluation of surface wind data in terms of eolian sand drift"},"predicate":"SUPERSEDED_BY","object":{"id":5637,"text":"pp1052 - 1979 - A study of global sand seas","indexId":"pp1052","publicationYear":"1979","noYear":false,"title":"A study of global sand seas"},"id":1}],"lastModifiedDate":"2018-01-12T14:20:03","indexId":"pp1052","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1052","title":"A study of global sand seas","docAbstract":"The birth of the idea that led to this publication on \"Global Sand Seas\" dates back to the late 1920's. At that time I was engaged in a study of the Coconino Sandstone of Arizona's Grand Canyon. Considerable controversy existed then as to whether this sandstone was a subaqueous deposit or was composed of wind-formed dunes. It became apparent that definitive literature was sparse or lacking on types of dunes, global distribution of these types, the mechanics of their development, the precise nature of their internal structure of cross-stratificiation, and the relation of wind systems to these sand forms. Especially lacking were data on criteria that could confidently be used in the recognition of ancient dunes.
The common denominator in this publication is eolian sand bodies. Although the book is concerned primarily with desert sand seas, the subject matter is not restricted to deserts; it includes many references to deposits of coastal sand and to sand bodies in humid climates. Nor does the book deal exclusively with dunes, which, according to most definitions, involve mounds or hills. Many references are made to sand sheets, sand stringers, and other types of sand deposits that have no prominent topographic expression. All sand bodies accumulated by the action of wind are discussed.
Chapters A-J of this publication are primarily topical. Chapters cover the grain texture, the color, and the structure of modern dunes and other eolian sands. Special treatment is given to the relation of wind data to dune interpretation, the evolution of form in current-deposited sand bodies as determined from experimental studies, and the discriminant analysis technique for differentiating between coastal and inland desert sands. This topical part of the publication also includes an analysis of criteria used in ancient deposits to interpret their eolian genesis and a consideration of economic application of the principles described, including a discussion of potentials and problems associated with eolian hydrocarbon reservoirs. The final chapters present a discussion of the morphology and distribution of dunes as determined largely from Landsat images.
Chapter K of the publication is devoted to descriptions of major sand seas based largely on thematic maps derived from Landsat (ERTS) mosaics. Although inclusion herein of the actual mosaics proved to be impractical, the maps derived from them do show the distribution and abundance of various dune types and the relations of these types to certain associated features, such as bedrock, water bodies, and juxtaposed dunes. Furthermore, sand roses included with each of these maps enable the user to draw conclusions on the probable relations of wind strength and direction to dune type in a particular area.
Regional studies (chapter K) were a team effort. Analysis of the Landsat (ERTS) mosaics and mapping boundaries of individual dune types were by Carol Breed. Synthesis of the rather voluminous literature and preparation of abstracts covering it was by Camilla MacCauley. Actual preparation of maps was by Franci Lennartz and later by Sarah Andrews. The gathering of data on wind, the calculation of wind roses, and the interpretation of their relations to sand bodies were by Steven Fryberger, assisted by Gary Dean.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp1052","usgsCitation":"1979, A study of global sand seas: U.S. Geological Survey Professional Paper 1052, ix, 429 p., https://doi.org/10.3133/pp1052.","productDescription":"ix, 429 p.","numberOfPages":"439","costCenters":[],"links":[{"id":122640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1052/report-thumb.jpg"},{"id":32135,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a61c2","contributors":{"editors":[{"text":"McKee, Edwin D.","contributorId":60207,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":725490,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":5645,"text":"pp1044C - 1979 - The waters of Hot Springs National Park, Arkansas — Their nature and origin","interactions":[{"subject":{"id":47999,"text":"ofr7119 - 1970 - The thermal springs of Hot Springs National Park, Arkansas; factors affecting their environment and management","indexId":"ofr7119","publicationYear":"1970","noYear":false,"title":"The thermal springs of Hot Springs National Park, Arkansas; factors affecting their environment and management"},"predicate":"SUPERSEDED_BY","object":{"id":5645,"text":"pp1044C - 1979 - The waters of Hot Springs National Park, Arkansas — Their nature and origin","indexId":"pp1044C","publicationYear":"1979","noYear":false,"chapter":"C","title":"The waters of Hot Springs National Park, Arkansas — Their nature and origin"},"id":1},{"subject":{"id":48219,"text":"ofr741009 - 1974 - The waters of Hot Springs National Park, Arkansas : their origin, nature and management","indexId":"ofr741009","publicationYear":"1974","noYear":false,"title":"The waters of Hot Springs National Park, Arkansas : their origin, nature and management"},"predicate":"SUPERSEDED_BY","object":{"id":5645,"text":"pp1044C - 1979 - The waters of Hot Springs National Park, Arkansas — Their nature and origin","indexId":"pp1044C","publicationYear":"1979","noYear":false,"chapter":"C","title":"The waters of Hot Springs National Park, Arkansas — Their nature and origin"},"id":2}],"lastModifiedDate":"2025-04-17T16:37:02.824343","indexId":"pp1044C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1044","chapter":"C","title":"The waters of Hot Springs National Park, Arkansas — Their nature and origin","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geohydrology of geothermal systems","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1044C","usgsCitation":"Bedinger, M.S., Pearson, F.J., Reed, J., Sniegocki, R., and Stone, C.G., 1979, The waters of Hot Springs National Park, Arkansas — Their nature and origin: U.S. Geological Survey Professional Paper 1044, Report: iii, 33 p.; 1 Plate: 21.38 × 21.86 inches, https://doi.org/10.3133/pp1044C.","productDescription":"Report: iii, 33 p.; 1 Plate: 21.38 × 21.86 inches","costCenters":[],"links":[{"id":104541,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4696.htm","linkFileType":{"id":5,"text":"html"},"description":"4696"},{"id":112533,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":112532,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1044c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139866,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1044c/report-thumb.jpg"}],"country":"United States","state":"Arkansas","otherGeospatial":"Hot Springs National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.12355041503905,\n 34.487881874939866\n ],\n [\n -93.0047607421875,\n 34.487881874939866\n ],\n [\n -93.0047607421875,\n 34.56990638085636\n ],\n [\n -93.12355041503905,\n 34.56990638085636\n ],\n [\n -93.12355041503905,\n 34.487881874939866\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62ebfd","contributors":{"authors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":151359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearson, F. J. Jr.","contributorId":7696,"corporation":false,"usgs":true,"family":"Pearson","given":"F.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":151356,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, J.E.","contributorId":41801,"corporation":false,"usgs":true,"family":"Reed","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":151358,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sniegocki, R. T.","contributorId":38546,"corporation":false,"usgs":true,"family":"Sniegocki","given":"R. T.","affiliations":[],"preferred":false,"id":151357,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stone, C. G.","contributorId":91094,"corporation":false,"usgs":true,"family":"Stone","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":151360,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":5903,"text":"pp1108 - 1979 - Impact of flow regulation and powerplant effluents on the flow and temperature regimes of the Chattahoochee River— Atlanta to Whitesburg, Georgia","interactions":[{"subject":{"id":8788,"text":"ofr78528 - 1978 - Impact of flow regulation and power plant effluents on the flow and temperature regimes of the Chattahoochee River - Atlanta to Whitesburg, Georgia","indexId":"ofr78528","publicationYear":"1978","noYear":false,"title":"Impact of flow regulation and power plant effluents on the flow and temperature regimes of the Chattahoochee River - Atlanta to Whitesburg, Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":5903,"text":"pp1108 - 1979 - Impact of flow regulation and powerplant effluents on the flow and temperature regimes of the Chattahoochee River— Atlanta to Whitesburg, Georgia","indexId":"pp1108","publicationYear":"1979","noYear":false,"title":"Impact of flow regulation and powerplant effluents on the flow and temperature regimes of the Chattahoochee River— Atlanta to Whitesburg, Georgia"},"id":1}],"lastModifiedDate":"2021-12-08T22:43:06.72437","indexId":"pp1108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1108","title":"Impact of flow regulation and powerplant effluents on the flow and temperature regimes of the Chattahoochee River— Atlanta to Whitesburg, Georgia","docAbstract":"A calibrated and verified transient flow-temperature model was used to evaluate the effects of flow regulation and powerplant loadings on the natural temperature regime of the Chattahoochee River in northeast Georgia. Estimates were made of both instantaneous and average natural temperatures in the river during an 8-day period in August 1976. Differences between the computed average natural temperature and an independent estimate of natural temperature based on observed equilibrium temperatures were less than 0.5°C. Downstream of the powerplants, the combined thermal effects of flow regulation and powerplant effluents resulted in mean daily river temperatures about equal to or less than computed mean natural temperatures. Thus the thermal impact of heated effluents was offset by the cooling effects of structural regulation. An independent analysis of historical river- and air-temperature data, although considerably less accurate than model computations, provided substantially the same result. The range and rates of change of computed natural diurnal temperature fluctuations were considerably less than those in the river at the time of this study in 1976. The models also were used to simulate summer river temperatures using estimated year 2000 flow conditions and meteorologic data collected during 1976. Except during periods of peak water-supply demand, differences between computed year 2000 river temperatures and observed 1976 temperatures were less than 2°C.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1110MDD","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, The Mississippian and Pennsylvanian (Carboniferous) systems in the United States: U.S. Geological Survey Professional Paper 1110, 487 p., https://doi.org/10.3133/pp1110MDD.","productDescription":"487 p.","costCenters":[],"links":[{"id":247324,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1110m-dd/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402239,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93477.htm","text":"Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":251797,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1110m-dd/report-thumb.jpg"},{"id":464250,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93478.htm","text":"Idaho","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b8d3","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":528705,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6057,"text":"pp1137 - 1979 - Comprehensive monitoring of meteorology, hydraulics, and thermal regime of the San Diego Aqueduct, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"pp1137","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1137","title":"Comprehensive monitoring of meteorology, hydraulics, and thermal regime of the San Diego Aqueduct, California","docAbstract":"Water temperature, as well as meteorologic and hydraulic variables which influence the energy budget of the San Diego Aqueduct in southern California, were continuously monitored for a 1-year period beginning July 24, 1973. Incoming solar and atmospheric radiation, windspeed and direction, water temperature, and wet- and dry-bulb air temperatures were recorded at 10-minute intervals at each end of the 26-kilometer concrete-lined canal, while flow-rates and stages were determined at hourly intervals for five locations. Although only daily averaged values are presented in this report, all information necessary for the use and interpretation of these data are presented. Windspeeds were minimum during the early morning hours and maximum during the late afternoon; however, they were variable spatially. On the other hand, incoming radiation and absolute vapor pressure varied little from point to point. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1137","usgsCitation":"Jobson, H.E., and Sturrock, A.M., 1979, Comprehensive monitoring of meteorology, hydraulics, and thermal regime of the San Diego Aqueduct, California: U.S. Geological Survey Professional Paper 1137, 29 p., https://doi.org/10.3133/pp1137.","productDescription":"29 p.","costCenters":[],"links":[{"id":123400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1137/report-thumb.jpg"},{"id":33057,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1137/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f8c","contributors":{"authors":[{"text":"Jobson, Harvey E.","contributorId":27032,"corporation":false,"usgs":true,"family":"Jobson","given":"Harvey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":152037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sturrock, Alex M.","contributorId":48948,"corporation":false,"usgs":true,"family":"Sturrock","given":"Alex","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":152038,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6058,"text":"pp1136 - 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}],"lastModifiedDate":"2017-01-05T12:46:45","indexId":"pp1136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1136","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. \r\n\r\nThe linear, implicit finite-difference flow model was calibrated by use of a depth profile obtained at steady low flow and unsteady flow data obtained in March 1976. During the calibration period, the model was generally able to reproduce observed stages to within 0.15 m and discharges at less than 100 m 3 /s, to within 5 percent. Peak discharges of about 200 m 3 /s were under-estimated by about 20 percent. During the verification period, October 1975, the flow model reproduced observed stage changes to within about 0.15 m, and its timing and over-all performance was considered to be very good. \r\n\r\nDye was added to the upstream end of the river reach at a constant rate while the river flow was highly unsteady. The numerical solution of either the conservative or nonconservative form of the mass-transport equation did an excellent job of simulating the observed concentrations of dye in the river. \r\n\r\nThe temperature model was capable of predicting temperature changes through this reach of as large as 5.8?C with a RMS (root-mean-square) error of 0.32?C in October 1975 and 0.20?C in March 1976. \r\n\r\nHydropulsation has a significant effect on the water temperature below Buford Dam. These effects are very complicated because they are quite dependent on the timing of the release with respect to both the time of day and past releases.","language":"ENGLISH","publisher":"U.S. Govt. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db69990c","contributors":{"authors":[{"text":"Jobson, Harvey E.","contributorId":27032,"corporation":false,"usgs":true,"family":"Jobson","given":"Harvey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":152039,"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":152040,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6162,"text":"pp1130 - 1979 - Hydrologic and human aspects of the 1976-77 drought","interactions":[],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp1130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1130","title":"Hydrologic and human aspects of the 1976-77 drought","docAbstract":"The drought of 1976-77 was the most severe in at least 50 years in many parts of the United States. Record low amounts of rainfall, snowfall, and runoff, and increased withdrawals of ground water were prevalent. The use of carry-over storage in reservoirs during 1976 maintained streamflow at near normal levels, but some reservoirs went dry or dropped below the outlet works in 1977. Carry-over storage in the fall of 1977 was very low. Ground-water levels were at or near record low levels in many aquifers, hundreds of wells went dry, and thousands of wells were drilled. Yet no wide-spread deterioration of ground-water quality was reported. Water-quality problems arose in some streams and lakes, but most were localized and of short duration. Water rationing became a way of life in numerous areas , and water was hauled in many rural areas and to a few towns. Water use was affected by legal agreements or decisions, some of which were modified for the duration of the drought, and by the inability of water managers to efficiently manage surface and ground waters as one resource under existing law. There are still many drought related problems to solve and many challenges to be met before the next drought occurs. The advancement of techniques in many fields of endeavor in recent years plus ongoing, planned, and proposed research on drought and the risks involved are promising thrusts that should make it easier to cope with the next drought. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1130","usgsCitation":"Matthai, H.F., 1979, Hydrologic and human aspects of the 1976-77 drought: U.S. Geological Survey Professional Paper 1130, 84 p., https://doi.org/10.3133/pp1130.","productDescription":"84 p.","costCenters":[],"links":[{"id":126668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1130/report-thumb.jpg"},{"id":33266,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1130/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687f83","contributors":{"authors":[{"text":"Matthai, Howard F.","contributorId":106491,"corporation":false,"usgs":true,"family":"Matthai","given":"Howard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":152222,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6187,"text":"pp1087 - 1979 - Maine coastal storm and flood of February 2, 1976","interactions":[],"lastModifiedDate":"2012-02-02T00:06:01","indexId":"pp1087","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1087","title":"Maine coastal storm and flood of February 2, 1976","docAbstract":"A business section of Bangor, Maine, was flooded with 12 feet (3.7 m) of water on February 2, 1976. The water surface elevation reached 17.46 feet (5.32 m) above national geodetic vertical datum of 1929 (NGVD), approximately 10.5 feet (3.2 m) above the predicted astronomical tide at Bangor. The unusually high water resulted from a tidal storm surge caused by prolonged strong, south-southeasterly winds which occurred near the time of astronomical high tide. Winds exceeded 64 knots off the New England coast. The resulting flood was the third highest since 1846 and is the first documented tidal flood at Bangor. This report documents the meteorological and hydrologic conditions associated with the flooding and also contains a brief description of storm damage from Eastport to Brunswick, Maine. Included are flood elevations in the city of Bangor and along the coast of Maine east of the Kennebec River. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1087","usgsCitation":"Morrill, R.A., Chin, E.H., and Richardson, W., 1979, Maine coastal storm and flood of February 2, 1976: U.S. Geological Survey Professional Paper 1087, 20 p., https://doi.org/10.3133/pp1087.","productDescription":"20 p.","costCenters":[],"links":[{"id":104548,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4716.htm","linkFileType":{"id":5,"text":"html"},"description":"4716"},{"id":117292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1087/report-thumb.jpg"},{"id":33319,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1087/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33320,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1087/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33321,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1087/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6496b0","contributors":{"authors":[{"text":"Morrill, Richard Arthur","contributorId":73200,"corporation":false,"usgs":true,"family":"Morrill","given":"Richard","email":"","middleInitial":"Arthur","affiliations":[],"preferred":false,"id":152256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chin, Edwin H.","contributorId":87921,"corporation":false,"usgs":true,"family":"Chin","given":"Edwin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":152257,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richardson, W.S.","contributorId":50150,"corporation":false,"usgs":true,"family":"Richardson","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":152255,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":6402,"text":"pp1147 - 1979 - Chemical correlation of some late Cenozoic tuffs of Northern and Central California by neutron activation analysis of glass and comparison with X-ray fluorescence analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:05:56","indexId":"pp1147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1147","title":"Chemical correlation of some late Cenozoic tuffs of Northern and Central California by neutron activation analysis of glass and comparison with X-ray fluorescence analysis","docAbstract":"Glasses separated from several dacitic and rhyolitic late Cenozoic tuffs of northern and central California were analyzed by neutron activation for more than 43 elemental abundances. Eighteen elements--scandiurn, manganese, iron, zinc, rubidium, cesium, barium, lanthanum, cerium, samarium, europium, terbiurn, dysprosiurn, ytterbiurn, hafniurn, tantalurn, thorium and uranium--were selected as most suitable for purposes of chemical correlation on the basis of their natural variability in silicic tuffs and the precision obtainable in analysis. Stratigraphic relations between tuffs and replicate chemical analyses on individual tuffs make it possib1e to calibrate a quantitative parameter, the similarity coefficient, which indicates the degree of correlation for the tuffs studied. The highest similarity coefficient (0.99) was obtained for analyses of two tuffs (potassium-argon dated at about' 6.0 m.y.) exposed in the Merced(?) and Petaluma Formations of Sonoma County, which represent different paleoenvironments, shallow-water marine and fresh water or brackish marine, respectively. Corre1ation of these formations on the basis of criteria other than tephrochronoloqy would be difficult. Results of neutron activation analysis in general confirm earlier correlations made on the basis of analysis by X-ray fluorescence but also make it possible to resolve small compositional differences between chemically simi1ar tuffs in stratigraphic proximity. The Lawlor Tuff (potassium-argon dated at about 4.0 m.y.) is identified at two new localities: in a core sample obtained from a bore hole east of Suisun Bay, and from the Kettleman Hills of western San Joaquin Valley. This identification permits correlation of the uppermost part of the marine Etchegoin Formation in the San Joaquin Valley with the continental Livermore Gravels of Clark, the Tassajara Formation, and the upper part of the Sonoma Volcanics in the cel1tral Coast Ranges of California. A younger tuff near the top of the marine San Joaquin Formation in the Kettleman Hills has been identified at both new 1oca1ities .","language":"ENGLISH","publisher":"for sale by the Supt. of Docs., U.S. Govt. Print. Off., 1979","doi":"10.3133/pp1147","usgsCitation":"Sarna-Wojcicki, A.M., Bowman, H.W., and Russell, P.C., 1979, Chemical correlation of some late Cenozoic tuffs of Northern and Central California by neutron activation analysis of glass and comparison with X-ray fluorescence analysis: U.S. Geological Survey Professional Paper 1147, 15 p., https://doi.org/10.3133/pp1147.","productDescription":"15 p.","costCenters":[],"links":[{"id":125077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1147/report-thumb.jpg"},{"id":33792,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1147/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3ec9","contributors":{"authors":[{"text":"Sarna-Wojcicki, Andrei M. 0000-0002-0244-9149 asarna@usgs.gov","orcid":"https://orcid.org/0000-0002-0244-9149","contributorId":1046,"corporation":false,"usgs":true,"family":"Sarna-Wojcicki","given":"Andrei","email":"asarna@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":152656,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowman, Harry W.","contributorId":93761,"corporation":false,"usgs":true,"family":"Bowman","given":"Harry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":152658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Russell, Paul C.","contributorId":87414,"corporation":false,"usgs":true,"family":"Russell","given":"Paul","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":152657,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":6452,"text":"pp1061 - 1979 - Clay mineralogy of Pleistocene Lake Tecopa, Inyo County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"pp1061","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1061","title":"Clay mineralogy of Pleistocene Lake Tecopa, Inyo County, California","docAbstract":"Pleistocene Lake Tecopa in southeastern Inyo County, Calif., was formed when the Amargosa River was blocked at the southern end of its valley. The lake acted as a settling basin for detrital material being transported by the river. This detritus consisted of clays, quartz, feldspars, and micas which became mudstones and siltstones. These mudstones and siltstones, much eroded and dissected after the draining of the lake, extend over the entire basin and are interbedded with tuffs formed by the intermittent deposition of volcanic ashfalls in the former lake waters. These lightcolored mudstones and siltstones are tough and well indurated and break with a conchoidal fracture. \r\n\r\nThe predominant clay mineral in these detrital beds is a lithiumbearing saponite, which is found not only in the lake beds but also in the area beyond the boundaries of the lake, especially in fluvial deposits in the drainage basin of the Amargosa River to the north. This saponite does not contain enough lithium to be classified as a hectorite, and we have observed no indications that this clay consists of a mixture of two phases, such as hectorite and a diluent. Some authigenic dioctahedral montmorillonite, found only in small quantities close to the tuffs, was formed by alteration of the volcanic glass of the tuffs and was then admixed with the overlying or underlying detrital clays. \r\n\r\nThe only authigenic clay-type mineral found in any significant quantity is sepiolite, found near the edges of the lake basin and stratigraphically located mainly within a meter of the two uppermost tuffs. This sepiolite probably was precipitated when silica became available to the magnesium-bearing lake water through dissolution of the volcanic ash. Precipitation of sepiolite probably did not occur within the tuffs owing to the presence of alumina in solution. Zeolites were produced there and sepiolite formed outside the margins of the tuffs. \r\n\r\nAlso formed by the high-pH lake waters were water-soluble minerals, which were found widely dispersed in crusts or streaks on the clays. Much of the calcite was likely precipitated from the lake waters, especially near the north end of the lake where calciumbearing fresh water came into contact with the C02-rich lake waters. \r\n\r\nMagadiite, a sodium silicate mineral reported only twice previously in the United States, was found in small quantities in the southern end of the basin. This mineral is indicative of a minimum pH of 8.5. \r\n\r\nThe authigenic minerals formed in the lake reflect the presence of silica-rich tuffs and the high-pH, alkaline character of the lake waters.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1061","usgsCitation":"Starkey, H., and Blackmon, P.D., 1979, Clay mineralogy of Pleistocene Lake Tecopa, Inyo County, California: U.S. Geological Survey Professional Paper 1061, 34 p., https://doi.org/10.3133/pp1061.","productDescription":"34 p.","costCenters":[],"links":[{"id":124998,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1061/report-thumb.jpg"},{"id":33870,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1061/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de273","contributors":{"authors":[{"text":"Starkey, Harry C.","contributorId":102074,"corporation":false,"usgs":true,"family":"Starkey","given":"Harry C.","affiliations":[],"preferred":false,"id":152745,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blackmon, Paul D.","contributorId":56641,"corporation":false,"usgs":true,"family":"Blackmon","given":"Paul","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":152744,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6521,"text":"pp712E - 1979 - Geochemistry of ground water associated with tuffaceous rocks, Oasis Valley, Nevada","interactions":[],"lastModifiedDate":"2025-04-15T20:37:41.064608","indexId":"pp712E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"712","chapter":"E","title":"Geochemistry of ground water associated with tuffaceous rocks, Oasis Valley, Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp712E","usgsCitation":"White, A.F., 1979, Geochemistry of ground water associated with tuffaceous rocks, Oasis Valley, Nevada: U.S. Geological Survey Professional Paper 712, 24 p., https://doi.org/10.3133/pp712E.","productDescription":"24 p.","costCenters":[],"links":[{"id":33998,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0712e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121560,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0712e/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Oasis Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116.8333,\n 37.0833\n ],\n [\n -116.8333,\n 36.9\n ],\n [\n -116.6667,\n 36.9\n ],\n [\n -116.6667,\n 37.0833\n ],\n [\n -116.8333,\n 37.0833\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab5bb","contributors":{"authors":[{"text":"White, A. F.","contributorId":36546,"corporation":false,"usgs":true,"family":"White","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":152861,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7051,"text":"ofr79540 - 1979 - Chemical composition of water and gas from five nearshore subaqueous springs in Clear Lake, Northern California","interactions":[],"lastModifiedDate":"2022-10-19T21:47:21.664511","indexId":"ofr79540","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":"79-540","title":"Chemical composition of water and gas from five nearshore subaqueous springs in Clear Lake, Northern California","docAbstract":"In 1971 The Geysers-Clear Lake area was selected by the U.S. Geological Survey geothermal research program as a region for extensive investigation. Under this program thermal water samples were first collected in December, 1974 during a winter of normal rainfall; the last samples were collected in February, 1977 during a period of drought. The drought exposed many springs which normally are submerged by Clear Lake. The collection and analysis of these springs is reported in Thompson and others (this vol.).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79540","usgsCitation":"Thompson, J., Sims, J., Yadav, S., and Rymer, M.J., 1979, Chemical composition of water and gas from five nearshore subaqueous springs in Clear Lake, Northern California: U.S. Geological Survey Open-File Report 79-540, 14 p., https://doi.org/10.3133/ofr79540.","productDescription":"14 p.","costCenters":[],"links":[{"id":408553,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0540/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140565,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0540/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Clear Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.93838500976561,\n 38.91668153637508\n ],\n [\n -122.60879516601561,\n 38.91668153637508\n ],\n [\n -122.60879516601561,\n 39.144972625112224\n ],\n [\n -122.93838500976561,\n 39.144972625112224\n ],\n [\n -122.93838500976561,\n 38.91668153637508\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3faa","contributors":{"authors":[{"text":"Thompson, J. M.","contributorId":77142,"corporation":false,"usgs":true,"family":"Thompson","given":"J. M.","affiliations":[],"preferred":false,"id":154089,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sims, J.D.","contributorId":9230,"corporation":false,"usgs":false,"family":"Sims","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":154088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yadav, Sandhya","contributorId":8847,"corporation":false,"usgs":true,"family":"Yadav","given":"Sandhya","email":"","affiliations":[],"preferred":false,"id":154087,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rymer, M. J.","contributorId":90694,"corporation":false,"usgs":true,"family":"Rymer","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154090,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7096,"text":"ofr791139 - 1979 - Description of dredge samples from the Bering Sea continental margin","interactions":[],"lastModifiedDate":"2024-01-22T20:44:17.754546","indexId":"ofr791139","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":"79-1139","title":"Description of dredge samples from the Bering Sea continental margin","docAbstract":"During 1978 twenty dredge sites were occupied and successfully dredged from the R.V. S.P. LEE along the eastern Bering Sea continental margin (Fig. 1). A total of several tons of rock were collected using a chain-bag dredge. Samples were recovered in water depths ranging from 750 to 2,750 meters from exposures along the continental slope bordering the large Bering Sea shelf.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791139","usgsCitation":"Marlow, M.S., Cooper, A.K., Scholl, D.W., Vallier, T.L., and McLean, H., 1979, Description of dredge samples from the Bering Sea continental margin: U.S. Geological Survey Open-File Report 79-1139, 6 p., https://doi.org/10.3133/ofr791139.","productDescription":"6 p.","costCenters":[],"links":[{"id":141536,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1139/report-thumb.jpg"},{"id":424697,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -185.15090325261252,\n 57.09189815353466\n ],\n [\n -185.15090325261252,\n 50.777014004737026\n ],\n [\n -160.1657690351336,\n 50.777014004737026\n ],\n [\n -160.1657690351336,\n 57.09189815353466\n ],\n [\n -185.15090325261252,\n 57.09189815353466\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dbf5","contributors":{"authors":[{"text":"Marlow, Michael S.","contributorId":72775,"corporation":false,"usgs":true,"family":"Marlow","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":154280,"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":154278,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scholl, David W. 0000-0001-6500-6962 dscholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6500-6962","contributorId":3738,"corporation":false,"usgs":true,"family":"Scholl","given":"David","email":"dscholl@usgs.gov","middleInitial":"W.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":154282,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vallier, Tracy L.","contributorId":28857,"corporation":false,"usgs":true,"family":"Vallier","given":"Tracy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":154279,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McLean, Hugh","contributorId":73977,"corporation":false,"usgs":true,"family":"McLean","given":"Hugh","affiliations":[],"preferred":false,"id":154281,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":7129,"text":"ofr791572 - 1979 - Examples of deep-water-bottom multiple dereverberation techniques applied to seismic-reflection data from the Atlantic Outer Continental Shelf","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr791572","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":"79-1572","title":"Examples of deep-water-bottom multiple dereverberation techniques applied to seismic-reflection data from the Atlantic Outer Continental Shelf","docAbstract":"Seismic-reflection data recorded in deep water over the Atlantic Outer Continental Shelf are often dominated by multiply-reflected seismic energy. This energy reverberates between the surface of the water and the seafloor (or other strong reflectors), and makes portions of the seismic data completely useless. Several different data-processing techniques can be applied to partially suppress these multiples and enhance the interpretability of the data. These techniques include (1) the three-point operator, (2) predictive deconvolution, (3) near-trace muting, (4) spatially variant bandpass filters, (5) Nth root stack, and (6) trace distance weighting. Application of these methods to several seismic lines indicates that trace distance weighting is the most useful method studied for suppressing deep-water-bottom multiples for data from the Atlantic Outer Continental Shelf.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791572","usgsCitation":"Peterson, S.D., Balch, A.H., Patterson, W., and Taylor, D.J., 1979, Examples of deep-water-bottom multiple dereverberation techniques applied to seismic-reflection data from the Atlantic Outer Continental Shelf: U.S. Geological Survey Open-File Report 79-1572, iii, 42 p. :ill. ;27 cm., https://doi.org/10.3133/ofr791572.","productDescription":"iii, 42 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":139982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1572/report-thumb.jpg"},{"id":34442,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1572/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9490","contributors":{"authors":[{"text":"Peterson, Steven D.","contributorId":90717,"corporation":false,"usgs":true,"family":"Peterson","given":"Steven","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":154400,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Balch, A. H.","contributorId":104892,"corporation":false,"usgs":true,"family":"Balch","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":154401,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patterson, W.C.","contributorId":73994,"corporation":false,"usgs":true,"family":"Patterson","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":154399,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Taylor, D. J.","contributorId":50849,"corporation":false,"usgs":true,"family":"Taylor","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154398,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7217,"text":"ofr791625 - 1979 - Helium in soil-gas and helium/radon in ground water in the vicinity of a south Texas uranium roll-type deposit","interactions":[],"lastModifiedDate":"2024-06-07T18:36:23.033698","indexId":"ofr791625","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":"79-1625","title":"Helium in soil-gas and helium/radon in ground water in the vicinity of a south Texas uranium roll-type deposit","docAbstract":"A survey was run in the vicinity of a south Texas uranium roll-type deposit to determine the general concentration of helium in the soil gas and helium/radon ratios in the ground water for deposits of this nature. The helium in soil-gas concentrations are typical of the concentrations found associated with other low-grade uranium deposits in other areas. The distribution of the values probably reflects local structure and is influenced by surface activities such as farming and mining. The helium/radon ratios in water strikingly reveal the known orebody, and some samples taken for background information may indicate the presence of nearby mineralized areas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791625","usgsCitation":"Reimer, G.M., Bowles, C., Murrey, D., and Been, J., 1979, Helium in soil-gas and helium/radon in ground water in the vicinity of a south Texas uranium roll-type deposit: U.S. Geological Survey Open-File Report 79-1625, i, 10 p., https://doi.org/10.3133/ofr791625.","productDescription":"i, 10 p.","costCenters":[],"links":[{"id":429669,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1625/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140830,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1625/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"south Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -98.38414338122332,\n 28.745222690320517\n ],\n [\n -98.38414338122332,\n 28.021417695428653\n ],\n [\n -97.76942585212466,\n 28.021417695428653\n ],\n [\n -97.76942585212466,\n 28.745222690320517\n ],\n [\n -98.38414338122332,\n 28.745222690320517\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635da3","contributors":{"authors":[{"text":"Reimer, G. Michael","contributorId":95875,"corporation":false,"usgs":true,"family":"Reimer","given":"G.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":154797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowles, C.G.","contributorId":14369,"corporation":false,"usgs":true,"family":"Bowles","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":154794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murrey, D.G.","contributorId":51740,"corporation":false,"usgs":true,"family":"Murrey","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":154796,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Been, J.M.","contributorId":26685,"corporation":false,"usgs":true,"family":"Been","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":154795,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7218,"text":"ofr79700 - 1979 - Hexavalent chromium in the ground and surface waters near Telluride, Colorado; preliminary data report","interactions":[],"lastModifiedDate":"2022-07-12T16:42:11.666303","indexId":"ofr79700","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":"79-700","title":"Hexavalent chromium in the ground and surface waters near Telluride, Colorado; preliminary data report","docAbstract":"Data showing results of 38 groundwater and 25 surface-water samples analyzed for hexavalent chromium are presented. Most samples were taken within the Telluride, Colo., city limits during October 1978. Twenty-four of the 38 groundwater samples (63%) contained more than 50 micrograms per liter of hexavalent chromium. Excluding the mill tailings pond 6 of the 23 surface-water samples (26%) contained more than 50 micrograms per liter of hexavalent chromium. Hexavalent chromium concentrations in groundwaters ranged from 0 to 2700 micrograms per liter and in surface waters from 0 to 160 micrograms per liter.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79700","usgsCitation":"Grove, D.B., Miller, R.L., Konikow, L.F., and O’Boyle, P.S., 1979, Hexavalent chromium in the ground and surface waters near Telluride, Colorado; preliminary data report: U.S. Geological Survey Open-File Report 79-700, ii, 18 p., https://doi.org/10.3133/ofr79700.","productDescription":"ii, 18 p.","costCenters":[],"links":[{"id":403541,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0700/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0700/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Telluride","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.81244277954102,\n 37.93296060989755\n ],\n [\n -107.80137062072752,\n 37.93296060989755\n ],\n [\n -107.80137062072752,\n 37.93661617256258\n ],\n [\n -107.81244277954102,\n 37.93661617256258\n ],\n [\n -107.81244277954102,\n 37.93296060989755\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62ec79","contributors":{"authors":[{"text":"Grove, David B.","contributorId":74750,"corporation":false,"usgs":true,"family":"Grove","given":"David","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":154801,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Ronald L.","contributorId":225052,"corporation":false,"usgs":false,"family":"Miller","given":"Ronald","email":"","middleInitial":"L.","affiliations":[{"id":41028,"text":"NASA GISS and Columbia University","active":true,"usgs":false}],"preferred":false,"id":154799,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Konikow, Leonard F. 0000-0002-0940-3856 lkonikow@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-3856","contributorId":158,"corporation":false,"usgs":true,"family":"Konikow","given":"Leonard","email":"lkonikow@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":154798,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"O’Boyle, P. S.","contributorId":55820,"corporation":false,"usgs":true,"family":"O’Boyle","given":"P.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":154800,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7224,"text":"ofr791493 - 1979 - Hydrologic and climatologic data, southeastern Uinta Basin, Utah and Colorado, water year 1977","interactions":[],"lastModifiedDate":"2017-09-02T14:13:37","indexId":"ofr791493","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":"79-1493","title":"Hydrologic and climatologic data, southeastern Uinta Basin, Utah and Colorado, water year 1977","docAbstract":"No abstract available.
Data obtained during a hydrologic reconnaissance in 1975-77 in the Wasatch Plateau-Book Cliffs coal area of Utah were correlated with existing long-term data. Maps were prepared showing average precipitation, average streamflow, stream temperature, ground- and surface-water quality, sediment yield, and geology. Recommendations were made for additional study and suggested approaches for continued monitoring in the coal areas.
During the 1931-75 water years, the minimum discharges for the five major streams that head in the area ranged from about 12,000 to 26,000 acre-feet per year, and the maximum discharges ranged from about 59,000 to 315,000 acre-feet per year. Correlations indicate that 3 years of low-flow records at stream sites in the Wasatch Plateau would allow the development of relationships with long-term sites that can be used to estimate future low-flow records within a standard error of about 20 percent.
Most water-quality degradation in streams occurs along the flanks of the Wasatch Plateau and Book Cliffs. In the uplands, dissolved-solids concentrations generally ranged from less than 100 to about 250 milligrams per liter, and in the lowlands the concentrations ranged from about 250 to more than 6,000 milligrams per liter.
In the lowland areas, the Ferron Sandstone Member of the Mancos Shale appears to have the most potential for subsurface development of water of suitable chemical quality for human consumption. Three wells in the Ferron yielded water with dissolved-solids concentrations ranging from about 650 to 1,230 milligrams per liter.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79988","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management and the U.S. Environmental Protection Agency","usgsCitation":"Waddell, K., Contratto, P., Sumsion, C.T., and Butler, J.R., 1979, Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah: U.S. Geological Survey Open-File Report 79-988, Report: 85 p. ; 15 Figures: 40.36 x 26.85 inches or smaller; 8 Tables, https://doi.org/10.3133/ofr79988.","productDescription":"Report: 85 p. ; 15 Figures: 40.36 x 26.85 inches or smaller; 8 Tables","costCenters":[],"links":[{"id":484732,"rank":25,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-20.pdf","text":"Figure 20","linkFileType":{"id":1,"text":"pdf"}},{"id":484731,"rank":24,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-19-2.pdf","text":"Figure 19-2","linkFileType":{"id":1,"text":"pdf"}},{"id":484730,"rank":23,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-19-1.pdf","text":"Figure 19-1","linkFileType":{"id":1,"text":"pdf"}},{"id":484729,"rank":22,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-18-2.pdf","text":"Figure 18-2","linkFileType":{"id":1,"text":"pdf"}},{"id":484728,"rank":21,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-18-1.pdf","text":"Figure 18-1","linkFileType":{"id":1,"text":"pdf"}},{"id":484727,"rank":20,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-16.pdf","text":"Figure 16","linkFileType":{"id":1,"text":"pdf"}},{"id":484726,"rank":19,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-15.pdf","text":"Figure 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6","linkFileType":{"id":1,"text":"pdf"}},{"id":484720,"rank":13,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":484719,"rank":12,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-2-2.pdf","text":"Figure 2-2","linkFileType":{"id":1,"text":"pdf"}},{"id":484718,"rank":11,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-2-1.pdf","text":"Figure 2-1","linkFileType":{"id":1,"text":"pdf"}},{"id":484717,"rank":10,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1979/0988/table-9-2.pdf","text":"Table 9-2","linkFileType":{"id":1,"text":"pdf"}},{"id":484716,"rank":9,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1979/0988/table-9-1.pdf","text":"Table 9-1","linkFileType":{"id":1,"text":"pdf"}},{"id":484715,"rank":8,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1979/0988/table-8.pdf","text":"Table 8","linkFileType":{"id":1,"text":"pdf"}},{"id":484714,"rank":7,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1979/0988/table-7.pdf","text":"Table 7","linkFileType":{"id":1,"text":"pdf"}},{"id":484713,"rank":6,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1979/0988/table-6-2.pdf","text":"Table 6-2","linkFileType":{"id":1,"text":"pdf"}},{"id":484712,"rank":5,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1979/0988/table-6-1.pdf","text":"Table 6-1","linkFileType":{"id":1,"text":"pdf"}},{"id":484711,"rank":4,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1979/0988/table-5.pdf","text":"Table 5","linkFileType":{"id":1,"text":"pdf"}},{"id":484710,"rank":3,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1979/0988/table-2.pdf","text":"Table 2","linkFileType":{"id":1,"text":"pdf"}},{"id":484709,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0988/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139829,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0988/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Wasatch Plateau-Book Cliffs","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.21245898457167,\n 38.91116861217185\n ],\n [\n -111.21245898457167,\n 38.85223901594625\n ],\n [\n -111.17155403404577,\n 38.85223901594625\n ],\n [\n -111.17155403404577,\n 38.91116861217185\n ],\n [\n -111.21245898457167,\n 38.91116861217185\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6054b7","contributors":{"authors":[{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":154855,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Contratto, P.K.","contributorId":78733,"corporation":false,"usgs":true,"family":"Contratto","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":154856,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sumsion, C. T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":154853,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Butler, John R.","contributorId":36540,"corporation":false,"usgs":true,"family":"Butler","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":154854,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7299,"text":"ofr791069 - 1979 - Major sources of ground-water contamination in Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:06:06","indexId":"ofr791069","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":"79-1069","title":"Major sources of ground-water contamination in Connecticut","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791069","usgsCitation":"Handman, E.H., Grossman, I., Bingham, J., and Rolston, J., 1979, Major sources of ground-water contamination in Connecticut: U.S. Geological Survey Open-File Report 79-1069, xiii, 73 p. :ill., maps ;26 cm., https://doi.org/10.3133/ofr791069.","productDescription":"xiii, 73 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":141317,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1069/report-thumb.jpg"},{"id":34690,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1069/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6497d3","contributors":{"authors":[{"text":"Handman, Elinor H.","contributorId":31748,"corporation":false,"usgs":true,"family":"Handman","given":"Elinor","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":155120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grossman, I.G.","contributorId":52574,"corporation":false,"usgs":true,"family":"Grossman","given":"I.G.","email":"","affiliations":[],"preferred":false,"id":155122,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bingham, J.W.","contributorId":35295,"corporation":false,"usgs":true,"family":"Bingham","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":155121,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rolston, J.L.","contributorId":86766,"corporation":false,"usgs":true,"family":"Rolston","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":155123,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7300,"text":"ofr79581 - 1979 - Makah Formation--a deep marginal basin sedimentary sequence of Late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","interactions":[{"subject":{"id":7300,"text":"ofr79581 - 1979 - Makah Formation--a deep marginal basin sedimentary sequence of Late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","indexId":"ofr79581","publicationYear":"1979","noYear":false,"title":"Makah Formation--a deep marginal basin sedimentary sequence of Late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":4804,"text":"pp1162B - 1980 - Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","indexId":"pp1162B","publicationYear":"1980","noYear":false,"chapter":"B","title":"Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington"},"id":1}],"supersededBy":{"id":4804,"text":"pp1162B - 1980 - Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","indexId":"pp1162B","publicationYear":"1980","noYear":false,"title":"Makah Formation — A deep-marginal-basin sequence of late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington"},"lastModifiedDate":"2022-06-28T18:12:44.914956","indexId":"ofr79581","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":"79-581","title":"Makah Formation--a deep marginal basin sedimentary sequence of Late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington","docAbstract":"The Makah Formation of the Twin River Group crops out in a north-west-trending linear belt in the northwesternmost part of the Olympic Peninsula, Wash. This marine sequence consists of 2,800 meters of predominantly thin-bedded siltstone and sandstone that encloses six distinctive members. The named members include four packets of thick-bedded amalgamated turbidite sandstone, an olistostromal shallow-water marine sandstone and conglomerate member, and a thin-bedded water-laid tuff member. A local unconformity of submarine origin occurs within the lower part of the Makah Formation except in the central part of the study area, where it forms the contact between the older Hoko River Formation and the Makah. Foraminiferal faunas indicate that the Makah Formation ranges in age from late Eocene (late Narizian Stage) to late Oligocene (Zemorrian Stage) and was deposited in a predominantly lower to middle bathyal environment.
The Makah strata are part of a deep marginal basin facies that crops out in the western part of the Olympic Peninsula, in southwesternmost Washington and coastal embayments in northwestern Oregon, and along the central part of the coast of western Vancouver Island. On the basis of limited subsurface data from exploratory wells, correlative deepmarginal-basin deposits underlie the inner continental shelf of Oregon and the continental shelf (Tofino Basin) along the southwestern side of Vancouver Island.
Directional structures in the Makah Formation indicate that the predominantly lithic arkosic sandstone that forms the turbidite packets was derived from the northwest. A possible source of the clastics is the dioritic, granitic, and volcanic terranes in the vicinity of the Hesquiat Peninsula on the west coast of Vancouver Island. Vertical and lateral variations of turbidite facies suggest that the four packets of sandstone were formed as depositional lobes on an outer submarine fan. The thin-bedded strata between the turbidite packets have characteristics of basin-plain and outer-fan fringe deposits.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79581","usgsCitation":"Snavely, P.D., Niem, A.R., MacLeod, N.S., Pearl, J.E., and Rau, W.W., 1979, Makah Formation--a deep marginal basin sedimentary sequence of Late Eocene and Oligocene age in the northwestern Olympic Peninsula, Washington: U.S. Geological Survey Open-File Report 79-581, iv, 75p., https://doi.org/10.3133/ofr79581.","productDescription":"iv, 75p.","costCenters":[],"links":[{"id":141318,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0581/report-thumb.jpg"},{"id":402607,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0581/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Northwestern Olympic Peninsula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.79370117187499,\n 47.80577611936809\n ],\n [\n -122.78320312499999,\n 47.80577611936809\n ],\n [\n -122.78320312499999,\n 48.436489955944154\n ],\n [\n -124.79370117187499,\n 48.436489955944154\n ],\n [\n -124.79370117187499,\n 47.80577611936809\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db628787","contributors":{"authors":[{"text":"Snavely, P. D.","contributorId":13971,"corporation":false,"usgs":true,"family":"Snavely","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":155124,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Niem, A. R.","contributorId":54984,"corporation":false,"usgs":true,"family":"Niem","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":155125,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"MacLeod, N. S.","contributorId":55816,"corporation":false,"usgs":true,"family":"MacLeod","given":"N.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155126,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pearl, J. E.","contributorId":89883,"corporation":false,"usgs":true,"family":"Pearl","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155128,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rau, W. W.","contributorId":71963,"corporation":false,"usgs":true,"family":"Rau","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":155127,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":7310,"text":"ofr79530 - 1979 - Metals in Devonian kerogenous marine strata at Gibellini and Bisoni properties in southern Fish Creek Range, Eureka County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr79530","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":"79-530","title":"Metals in Devonian kerogenous marine strata at Gibellini and Bisoni properties in southern Fish Creek Range, Eureka County, Nevada","docAbstract":"A kerogen-rich sequence of siliceous mudstone, siltstone, and chert as much as 60 m thick on ridge 7129 in the southern Fish Creek Range, referred to as Gibellini facies of the Woodruff Formation, has been evaluated on the surface and in drill holes principally for its potential resources of vanadium, zinc, selenium, molybdenum, and syncrude oil content. The strata are part of a strongly deformed allochthonous mass of eugeosynclinal Devonian marine rocks that overlie deformed allochthonous Mississippian siliceous rocks and relatively undeformed autochthonous Mississippian Antler flysch at this locality. The vanadium in fresh black rocks obtained from drill holes and fresh exposures in trenches and roadcuts occurs chiefly in organic matter. Concentrations of vanadium oxide (V2O5) in unoxidized samples range from 3,000 to 7,000 ppm. In oxidized and bleached rock that is prevalent at the surface, concentrations of vanadium oxide range from 6,000 to 8,000 ppm, suggesting a tendency toward enrichment due to surficial weathering and ground-water movement. Zinc occurs in sphalerite, and selenium occurs in organic matter; molybdenum appears to occur both in molybdenite and in organic matter. Concentrations of zinc in unoxidized rock range from 4,000 to 18,000 ppm, whereas in oxidized rock they range from 30 to 100 ppm, showing strong depletion due to weathering. Concentrations of selenium in unoxidized rock range from 30 to 200 ppm, whereas in oxidized rock they range from 200 to 400 ppm, indicating some enrichment upon weathering. Concentrations of molybdenum in unoxidized rock range from 70 to 960 ppm, whereas in oxidized rock they range from 30 to 80 ppm, indicating strong depletion upon weathering. Most fresh black rock is low-grade oil shale, and yields as much as 12 gallons/short ton of syncrude oil. Metahewettite is the principal vanadium mineral in the oxidized zone, but it also occurs sparsely as small nodules and fillings of microfractures in unweathered strata. In fresh rock, bluish-white opaline-like silica (chalcedonic quartz) fills microfractures, and is believed to have originated by diagenetic mobilization of opaline silica from radiolarian tests and sponge spicules. \r\n\r\nAs revealed by microscopic study, the Gibellini facies originally consisted of siliceous muds, slimes, and oozes high in organic constituents. The organic matter is amorphous flaky and stringy sapropel, and probably includes remains of bacteria, phytoplankton, zooplankton, and minor higher plants. Recognizable organic remnants include radiolarian tests, sponge spicules, conodonts, brachiopod shells, algae, and humic debris. Diagnostic radiolarians indicate a Late Devonian age for the Gibellini facies of the Woodruff Formation. Some pyrite is disseminated through the rock and may be primary (syngenetic) but significant pyrite and marcasite occur in chalcedonic quartz veinlets and appear to be diagenetic. In fresh rock, black solid bitumen and liquid oil fill voids and microfractures. These early phase hydrocarbons probably were released during diagenesis from complex nonhydrocarbon molecular structures originating from living organisms, and formed without any major thermal degradation of the kerogen. Gas chromatographic analysis of the saturated hydrocarbon fraction indicates a very complex mixture dominated by branched and cyclic compounds. Conodont and palynomorph color alteration, vitrinite reflectance, and other organic geochemical data suggest that the organic matter in the rock is thermally immature and has not been subjected to temperatures greater than 60?C since deposition in Devonian time. All of these characteristics are consistent with the interpretation of a relatively low temperature and a shallow-burial history for the Gibellini facies on ridge 7129.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79530","usgsCitation":"Desborough, G.A., Poole, F.G., Hose, R.K., and Radtke, A.S., 1979, Metals in Devonian kerogenous marine strata at Gibellini and Bisoni properties in southern Fish Creek Range, Eureka County, Nevada: U.S. Geological Survey Open-File Report 79-530, iii, 35 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr79530.","productDescription":"iii, 35 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0530/report-thumb.jpg"},{"id":34700,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0530/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db62875c","contributors":{"authors":[{"text":"Desborough, George A.","contributorId":101661,"corporation":false,"usgs":true,"family":"Desborough","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":155168,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poole, F. G. 0000-0001-8487-0799","orcid":"https://orcid.org/0000-0001-8487-0799","contributorId":104883,"corporation":false,"usgs":true,"family":"Poole","given":"F.","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":155169,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hose, R. K.","contributorId":63388,"corporation":false,"usgs":true,"family":"Hose","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":155167,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Radtke, A. S.","contributorId":16408,"corporation":false,"usgs":true,"family":"Radtke","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155166,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7365,"text":"ofr791062 - 1979 - A one-dimensional, steady-state dissolved-oxygen model and waste-load assimilation study for Cedar Creek, Dekalb and Allen counties, Indiana","interactions":[],"lastModifiedDate":"2023-11-24T19:31:09.75019","indexId":"ofr791062","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":"79-1062","title":"A one-dimensional, steady-state dissolved-oxygen model and waste-load assimilation study for Cedar Creek, Dekalb and Allen counties, Indiana","docAbstract":"The Indiana State Board of Health is developing a State water-quality management plan that includes the establishing of limits for wastewater effluents discharged into Indiana streams. A digital model calibrated to conditions in Cedar Creek was used to develop alternatives for future waste loadings that would be compatible with Indiana stream water-quality standards defined for two critical hydrologic conditions, summer and winter low flows. All point-source waste loads affecting Cedar Creek are in the four incorporated municipalities of Auburn, Garrett, Huntertown, and Waterloo, in a primarily agricultural area. Avilla, because of its distance from Cedar Creek, does not significantly affect the water quality of the modeled segment.
The model indicates that the dissolved-oxygen concentration of the Auburn wastewater effluent and nitrification are the most significant factors affecting the dissolved-oxygen concentration in Cedar Creek during summer low flows. The observed dissolved-oxygen concentration of the Auburn wastewater effluent was low, and averaged 30 percent of saturation. Whether the effluent is aerated before discharge will ultimately define the waste-load assimilative capacity of Cedar Creek. Projected nitrogenous biochemical-oxygen demand loads, from the Indiana State Board of Health, for the Auburn and Waterloo wastewater-treatment facilities will result in violations of the current instream dissolved-oxygen standard (5 milligrams per liter), even with an effluent dissolved-oxygen concentration of 80 percent saturation.
Natural streamflow for Cedar Creek upstream from the confluence of Willow and Little Cedar Creeks is small compared with the waste discharge, so benefits of dilution for Waterloo and Auburn are minimal. Stream reaeration capacity is not sufficient to maintain an average dissolved-oxygen concentration of at least 5 milligrams per liter, the State's water-quality standard for streams.
The model also indicates that, during winter low flows, ammonia toxicity, rather than dissolved oxygen, is the limiting water-quality criterion in the reach of Cedar Creek downstream from the wastewater-treatment facility at Auburn and the confluence of Garrett ditch. Ammonia-nitrogen concentrations predicted for 2978 through 2000 downstream from the Waterloo wastewater-treatment facility do not exceed Indiana water-quality standards for streams.
Calculations of the stream's assimilative capacity indicate that future waste discharge in the Cedar Creek basin will be limited to the reaches between the Auburn wastewater-treatment facility and County Road 68.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791062","collaboration":"Prepared in cooperation with the Indiana State Board of Health","usgsCitation":"Wilber, W.G., Peters, J.G., Ayers, M.A., and Crawford, C.G., 1979, A one-dimensional, steady-state dissolved-oxygen model and waste-load assimilation study for Cedar Creek, Dekalb and Allen counties, Indiana: U.S. Geological Survey Open-File Report 79-1062, viii, 79 p., https://doi.org/10.3133/ofr791062.","productDescription":"viii, 79 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":422925,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1062/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140364,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1062/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Allen County, Dekalb County","otherGeospatial":"Cedar Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -85.38216090798966,\n 41.60787742256892\n ],\n [\n -85.38216090798966,\n 41.14208690200232\n ],\n [\n -84.81087184548976,\n 41.14208690200232\n ],\n [\n -84.81087184548976,\n 41.60787742256892\n ],\n [\n -85.38216090798966,\n 41.60787742256892\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abb2c","contributors":{"authors":[{"text":"Wilber, William G. wgwilber@usgs.gov","contributorId":297,"corporation":false,"usgs":true,"family":"Wilber","given":"William","email":"wgwilber@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":155417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peters, James G.","contributorId":69137,"corporation":false,"usgs":true,"family":"Peters","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":155420,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ayers, Mark A.","contributorId":84730,"corporation":false,"usgs":true,"family":"Ayers","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":155419,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crawford, Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":155418,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}