{"pageNumber":"6238","pageRowStart":"155925","pageSize":"25","recordCount":184918,"records":[{"id":48257,"text":"ofr741094 - 1973 - Derivation of homogeneous streamflow records in the upper Kentucky River basin, southeastern Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:10:48","indexId":"ofr741094","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"74-1094","title":"Derivation of homogeneous streamflow records in the upper Kentucky River basin, southeastern Kentucky","language":"ENGLISH","doi":"10.3133/ofr741094","usgsCitation":"Shearman, J., and Swisshelm, R., 1973, Derivation of homogeneous streamflow records in the upper Kentucky River basin, southeastern Kentucky: U.S. Geological Survey Open-File Report 74-1094, v, 34 leaves : ill., map ; 28 cm., https://doi.org/10.3133/ofr741094.","productDescription":"v, 34 leaves : ill., map ; 28 cm.","costCenters":[],"links":[{"id":171189,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab1e4b07f02db66dec7","contributors":{"authors":[{"text":"Shearman, J.O.","contributorId":33373,"corporation":false,"usgs":true,"family":"Shearman","given":"J.O.","email":"","affiliations":[],"preferred":false,"id":237048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swisshelm, R.V. Jr.","contributorId":71229,"corporation":false,"usgs":true,"family":"Swisshelm","given":"R.V.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":237049,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":49272,"text":"ofr73362 - 1973 - Catalog of earthquakes along the San Andreas fault system in Central California, July-September 1972","interactions":[],"lastModifiedDate":"2014-06-18T10:41:26","indexId":"ofr73362","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-362","title":"Catalog of earthquakes along the San Andreas fault system in Central California, July-September 1972","docAbstract":"

Numerous small earthquakes occur each day in the coast ranges of Central California. The detailed study of these earthquakes provides a tool for gaining insight into the tectonic and physical processes responsible for the generation of damaging earthquakes. This catalog contains the fundamental parameters for earthquakes located within and adjacent to the seismograph network operated by the National Center for Earthquake Research (NCER), U.S. Geological Survey, during the period July - September, 1972.

\n
\n

The motivation for these detailed studies has been described by Pakiser and others (1969) and by Eaton and others (1970). Similar catalogs of earthquakes for the years 1969, 1970 and 1971 have been prepared by Lee and others (1972 b, c, d). Catalogs for the first and second quarters of 1972 have been prepared by Wessan and others (1972 a & b). The basic data contained in these catalogs provide a foundation for further studies.

\n
\n

This catalog contains data on 1254 earthquakes in Central California. Arrival times at 129 seismograph stations were used to locate the earthquakes listed in this catalog. Of these, 104 are telemetered stations operated by NCER. Readings from the remaining 25 stations were obtained through the courtesy of the Seismographic Stations, University of California, Berkeley (UCB), the Earthquake Mechanism Laboratory, National Oceanic and Atmospheric Administration, San Francisco (EML); and the California Department of Water Resources, Sacramento.

\n
\n

The Seismographic Stations of the University of California, Berkeley, have for many years published a bulletin describing earthquakes in Northern California and the surrounding area, and readings at UCB Stations from more distant events. The purpose of the present catalog is not to replace the UCB Bulletin, but rather to supplement it, by describing the seismicity of a portion of central California in much greater detail.

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Off.,","doi":"10.3133/wsp1987","usgsCitation":"Davis, R.W., Lambert, T.W., and Hansen, A.J., 1973, Subsurface geology and ground-water resources of the Jackson Purchase region, Kentucky: U.S. Geological Survey Water Supply Paper 1987, 1 portfolio (v, 66 p., 11 fold. leaves of plates) :ill. ;23 cm., https://doi.org/10.3133/wsp1987.","productDescription":"1 portfolio (v, 66 p., 11 fold. leaves of plates) :ill. ;23 cm.","costCenters":[],"links":[{"id":94700,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1987/plate-03.pdf","size":"3609","linkFileType":{"id":1,"text":"pdf"}},{"id":94698,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1987/plate-01.pdf","size":"4652","linkFileType":{"id":1,"text":"pdf"}},{"id":94699,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1987/plate-02.pdf","size":"1464","linkFileType":{"id":1,"text":"pdf"}},{"id":94701,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1987/plate-04.pdf","size":"1597","linkFileType":{"id":1,"text":"pdf"}},{"id":94702,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1987/plate-05.pdf","size":"4878","linkFileType":{"id":1,"text":"pdf"}},{"id":94703,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1987/plate-06.pdf","size":"3320","linkFileType":{"id":1,"text":"pdf"}},{"id":94704,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1987/plate-07.pdf","size":"3007","linkFileType":{"id":1,"text":"pdf"}},{"id":94705,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1987/plate-08.pdf","size":"1116","linkFileType":{"id":1,"text":"pdf"}},{"id":94706,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1987/plate-09.pdf","size":"818","linkFileType":{"id":1,"text":"pdf"}},{"id":94707,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1987/plate-10.pdf","size":"5377","linkFileType":{"id":1,"text":"pdf"}},{"id":94708,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1987/plate-11.pdf","size":"807","linkFileType":{"id":1,"text":"pdf"}},{"id":137431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1987/report-thumb.jpg"},{"id":26212,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1987/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699a9e","contributors":{"authors":[{"text":"Davis, R. 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No abstract available. 

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No abstract available. 

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postglacial geologic history of Isle Royale National Park, Michigan","docAbstract":"Isle Royale was overridden by glacial ice during each of the four major glaciations of the Pleistocene Epoch, and each successive glaciation essentially obliterated all direct evidence of preceding glaciations on the island. In the waning phase of the last major glaciation, the Wisconsin Glaciation, the frontal ice margin retreated northward from at least the greater part of the Lake Superior basin, then readvanced into the basin during Valders time, about 11,000 years ago. We can attribute to the Valders ice the final aspect of glaciation on Isle Royale, including both erosional and depositional features.\r\n\r\nIt is impossible to estimate the quantity of glacial debris or other surficial materials that might have been present on Isle Royale prior to the Valders readvance, but the readvancing ice appears to have removed most of what might have been present, as judged by the thin surficial cover on the eastern two-thirds of the island today. During the Valders retreat, a series of lakes formed in the Lake Superior basin in front of the retreating ice margin.\r\n\r\nThe retreating ice opened successively lower outlets, and thus the general trend of lake elevations is downward. Distinct lake stages reflect periods of relative stability during which well- defined shoreline features developed. The ice front forming the north margin of the earlier lakes probably remained south of Isle Royale until about the time of glacial Lake Beaver Bay, when it retreated to a position straddling Isle Royale west of Lake Desor. Abundant deposits of glacial debris were left upon the newly deglaciated west end of the island, and the ice front remained stable long enough to build a complex of ice-margin deposits across the island. Shorelines formed by the glacial lake associated with this ice front are found on the western part of the island about 200 feet above present Lake Superior.\r\n\r\nSubsequent renewed and complete retreat of the ice margin from Isle Royale was rapid enough that only a minor amount of glacial debris was deposited on the central and eastern parts of the island. When the ice margin reached the north edge of the Lake Superior basin, Lake Minong was formed, and the entire basin was filled for the first time since the Valders advance. Lake Minong marked a relatively stable episode in the history of the basin, and its beaches are among the best developed of the abandoned shoreline features on Isle Royale. Lake Minong beaches and later lower beaches are best developed on the southwest end of Isle Royale, where abundant glacial debris provided easily worked materials for beach construction.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"GEOLOGY OF ISLE ROYALE NATIONAL PARK, MICHIGAN","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp754A","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Huber, N.K., 1973, Glacial and postglacial geologic history of Isle Royale National Park, Michigan: U.S. Geological Survey Professional Paper 754, Report: iii, 15 p.; Plate: 30.0 x 21.5 inches, https://doi.org/10.3133/pp754A.","productDescription":"Report: iii, 15 p.; Plate: 30.0 x 21.5 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true},{"id":595,"text":"U.S. Geological 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A large southward-flowing ground-water system beneath the southern flank of the Horse Heaven Hills discharges to the Columbia River in the westward-trending reach downstream from Wallula Gap.","language":"ENGLISH","doi":"10.3133/ofr73153","usgsCitation":"La Sala, A.M., Doty, G., and Pearson, F.J., 1973, A preliminary evaluation of regional ground-water flow in south-central Washington: U.S. Geological Survey Open-File Report 73-153, 55 p. ill., maps ; 28 cm., https://doi.org/10.3133/ofr73153.","productDescription":"55 p. ill., maps ; 28 cm.","costCenters":[],"links":[{"id":162761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0153/report-thumb.jpg"},{"id":84891,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0153/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6aacd8","contributors":{"authors":[{"text":"La Sala, A. M. 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Jr.","contributorId":7696,"corporation":false,"usgs":true,"family":"Pearson","given":"F.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":236896,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":64991,"text":"i721 - 1973 - Metallogenic map of Puerto Rico","interactions":[{"subject":{"id":46951,"text":"ofr7178 - 1971 - Geologic and metallogenic maps of Puerto Rico","indexId":"ofr7178","publicationYear":"1971","noYear":false,"title":"Geologic and metallogenic maps of Puerto Rico"},"predicate":"SUPERSEDED_BY","object":{"id":64991,"text":"i721 - 1973 - Metallogenic map of Puerto Rico","indexId":"i721","publicationYear":"1973","noYear":false,"title":"Metallogenic map of Puerto Rico"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:10","indexId":"i721","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"721","subseriesTitle":"NONE","title":"Metallogenic map of Puerto Rico","language":"ENGLISH","doi":"10.3133/i721","usgsCitation":"Cox, D.P., and Briggs, R., 1973, Metallogenic map of Puerto Rico: U.S. Geological Survey IMAP 721, 1 map :col. ;39 x 128 cm., on sheet 83 x 134 cm. folded in envelope 30 x 24 cm. +1 text., https://doi.org/10.3133/i721.","productDescription":"1 map :col. ;39 x 128 cm., on sheet 83 x 134 cm. folded in envelope 30 x 24 cm. +1 text.","costCenters":[],"links":[{"id":6094,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pr.water.usgs.gov/public/online_pubs/map_i_721/index.html","linkFileType":{"id":5,"text":"html"}},{"id":190190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"240000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -67.75,18 ], [ -67.75,18.5 ], [ -65.25,18.5 ], [ -65.25,18 ], [ -67.75,18 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db6286b9","contributors":{"authors":[{"text":"Cox, Dennis P. dcox@usgs.gov","contributorId":2766,"corporation":false,"usgs":true,"family":"Cox","given":"Dennis","email":"dcox@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":272474,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briggs, Reginald P.","contributorId":51388,"corporation":false,"usgs":true,"family":"Briggs","given":"Reginald P.","affiliations":[],"preferred":false,"id":272475,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13423,"text":"ofr7363 - 1973 - Summary of seismic activity and its relation to geology and mining in the Sunnyside mining district, Carbon and Emery Counties, Utah, during 1967-1970","interactions":[],"lastModifiedDate":"2012-02-02T00:06:50","indexId":"ofr7363","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-63","title":"Summary of seismic activity and its relation to geology and mining in the Sunnyside mining district, Carbon and Emery Counties, Utah, during 1967-1970","docAbstract":"In the Sunnyside mining district, Utah, coal is mined under thick and variable overburden which is locally weakened by faults and other structural discontinuities. Stress changes and local stress concentrations produced by mining under these conditions often cause sudden and violent ruptures in the coal and surrounding rock mass. The strain energy released by this type of failure, which can produce shock waves and may discharge coal and rock with explosive force, is often a serious threat to life and property. These releases of strain energy are called bumps or bounces by miners if they occur in the coal, and rock bursts if they occur in the surrounding rock mass. Many of these releases are so violent that they generate seismic waves that can be felt, or at least detected by seismic instruments, miles from the site of the rupture, whereas others are smaller and can be detected only by those sensitive seismic instruments within a few thousand feet of the site of the rupture. \r\n\r\nIn 1969 and 1970, about 27,000 and about 15,000 earth tremors, respectively, were recorded by the five-station seismic monitoring network that is located at the surface and encompasses most of the mine workings in the district. Of these totals, 512 and 524 earth tremors, respectively, were of sufficient magnitude (greater than 1. 5 on the Richter scale) so that the hypocenters could be accurately located. In 1968 about 20,000 tremors were recorded, with 281 large enough to plot, but in 1967 over 50,000 were recorded, of which 540 were plotted. \r\n\r\nIn this report we discuss the way in which seismic activity, geology, and mining are related or seem to be related for the period 1967 through 1970, with emphasis on the period 1969-70. We also suggest certain mining procedures which, based on studies during the period, might increase the safety and efficiency of mining operations in the Sunnyside district. A complete tabulation of the larger magnitude earth tremors which occurred during 1969-70 and descriptions of how they relate to mining are given in the appendix. Similar tabulations and descriptions for 1967 and 1968 are available in earlier reports (Barnes and others, 1969; Dunrud and others, 1970).","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr7363","usgsCitation":"Dunrud, C., Osterwald, F.W., and Hernandez, J., 1973, Summary of seismic activity and its relation to geology and mining in the Sunnyside mining district, Carbon and Emery Counties, Utah, during 1967-1970: U.S. Geological Survey Open-File Report 73-63, iii, 86 p. :ill., maps ;29 cm., https://doi.org/10.3133/ofr7363.","productDescription":"iii, 86 p. :ill., maps ;29 cm.","costCenters":[],"links":[{"id":106564,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8836.htm","linkFileType":{"id":5,"text":"html"},"description":"8836"},{"id":146175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0063/report-thumb.jpg"},{"id":41861,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0063/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41862,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0063/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41863,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0063/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41864,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0063/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41865,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0063/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41866,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0063/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41867,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0063/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41868,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0063/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41869,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0063/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697da8","contributors":{"authors":[{"text":"Dunrud, C. Richard","contributorId":48964,"corporation":false,"usgs":true,"family":"Dunrud","given":"C. Richard","affiliations":[],"preferred":false,"id":167786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osterwald, Frank W.","contributorId":98301,"corporation":false,"usgs":true,"family":"Osterwald","given":"Frank","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":167787,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hernandez, Jerome","contributorId":48188,"corporation":false,"usgs":true,"family":"Hernandez","given":"Jerome","affiliations":[],"preferred":false,"id":167785,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":48017,"text":"ofr7259 - 1973 - Salt-water movement in the lower Withlacoochee River-Cross-Florida Barge Canal complex","interactions":[{"subject":{"id":48017,"text":"ofr7259 - 1973 - Salt-water movement in the lower Withlacoochee River-Cross-Florida Barge Canal complex","indexId":"ofr7259","publicationYear":"1973","noYear":false,"title":"Salt-water movement in the lower Withlacoochee River-Cross-Florida Barge Canal complex"},"predicate":"SUPERSEDED_BY","object":{"id":26438,"text":"wri725 - 1973 - Salt-water movement in the lower Withlacoochee River-Cross Florida Barge Canal Complex","indexId":"wri725","publicationYear":"1973","noYear":false,"title":"Salt-water movement in the lower Withlacoochee River-Cross Florida Barge Canal Complex"},"id":1}],"supersededBy":{"id":26438,"text":"wri725 - 1973 - Salt-water movement in the lower Withlacoochee River-Cross Florida Barge Canal Complex","indexId":"wri725","publicationYear":"1973","noYear":false,"title":"Salt-water movement in the lower Withlacoochee River-Cross Florida Barge Canal Complex"},"lastModifiedDate":"2013-02-05T14:41:53","indexId":"ofr7259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"72-59","title":"Salt-water movement in the lower Withlacoochee River-Cross-Florida Barge Canal complex","language":"ENGLISH","doi":"10.3133/ofr7259","usgsCitation":"Bush, P.W., 1973, Salt-water movement in the lower Withlacoochee River-Cross-Florida Barge Canal complex: U.S. Geological Survey Open-File Report 72-59, 44 p. ill., maps ; 27 cm., https://doi.org/10.3133/ofr7259.","productDescription":"44 p. ill., maps ; 27 cm.","costCenters":[],"links":[{"id":161660,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdef7","contributors":{"authors":[{"text":"Bush, Peter W.","contributorId":57820,"corporation":false,"usgs":true,"family":"Bush","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":236678,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18297,"text":"ofr7335 - 1973 - Erosion processes, fluvial sediment transport, and reservoir sedimentation in a part of the Newell and Zayante Creek basins, Santa Cruz County, California","interactions":[],"lastModifiedDate":"2025-07-31T19:41:15.704749","indexId":"ofr7335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-35","title":"Erosion processes, fluvial sediment transport, and reservoir sedimentation in a part of the Newell and Zayante Creek basins, Santa Cruz County, California","docAbstract":"The drainage basins upstream from Loch Lomond, a water-supply reservoir on Newell Creek, and a proposed reservoir site on Zayante Creek were investigated for their characteristics with respect to the erosion, transportation, and deposition of sediment. The study area is underlain predominantly by sandstone, siltstone, and shale of Tertiary age that decompose readily into moderately deep soils, friable colluvium, and easily transported sediment particles. The Rices Mudstone and Twobar, Shale Members of the San Lorenzo Formation of Brabb (1964) underlie steep dip slopes in the study area, and probably are the most highly erodible of the several geologic units present there. However, nearly all of the geologic units have shown a propensity for accelerated erosion accompanying the disturbance of the land surface by the roadbuilding practices that predominate over other types of sediment-producing land-use activities in the study area. \r\n\r\nSediment transport in the study area was estimated from (1) a reservoir survey of Loch Lomond in 1971 that was compared with a preconstruction survey of 1960, and (2) sampling of sediment transported in suspension by Zayante Creek during the 1970 and 1971 water years. At least 46 acre-feet of sediment accumulated in Loch Lomond in a 10-year period, and an unmeasured quantity of very fine sediment in the form of a thin layer over much of the reservoir bottom was observed. The measured quantity of deposited sediment in a 10-year period represented a sediment yield of about 1,100 tons annually per square mile of drainage basin upstream from the reservoir arms where the major deposition occurred. This sediment occupied less than i percent of the original capacity of Loch Lomond, but the volume of measured sediment deposition is probably conservative in view of the unmeasured deposits observed and a reservoir trap efficiency of about 95 percent. \r\n\r\nSediment sampling on Zayante Creek indicated suspended-sediment yields of about 4,570 and 570 tons per square mile for the 1970 and 1971 water years. These values were considered excessive with respect to the relatively low flows during which they were measured, and probably reflect the intensive and current roadbuilding practices in the central and upstream parts of the Zayante Creek drainage in the study area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7335","usgsCitation":"Brown, W.M., 1973, Erosion processes, fluvial sediment transport, and reservoir sedimentation in a part of the Newell and Zayante Creek basins, Santa Cruz County, California: U.S. Geological Survey Open-File Report 73-35, Report: iv, 31 p.; 2 Plates: 16.98 x 19.55 inches and 24.96 x 19.75 inches, https://doi.org/10.3133/ofr7335.","productDescription":"Report: iv, 31 p.; 2 Plates: 16.98 x 19.55 inches and 24.96 x 19.75 inches","costCenters":[],"links":[{"id":493280,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8825.htm","linkFileType":{"id":5,"text":"html"}},{"id":47651,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47650,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0035/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47649,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0035/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151101,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0035/report-thumb.jpg"}],"country":"United States","state":"California","county":"Santa Cruz County","otherGeospatial":"Newell and Zayante Creek basins","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -121.972,\n 37.258\n ],\n [\n -122.105,\n 37.258\n ],\n [\n -122.105,\n 37.083\n ],\n [\n -121.972,\n 37.083\n ],\n [\n -121.972,\n 37.258\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdf38","contributors":{"authors":[{"text":"Brown, W. M. III","contributorId":27060,"corporation":false,"usgs":true,"family":"Brown","given":"W.","suffix":"III","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":178871,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}