No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf581A","usgsCitation":"Pease, M.H., 1974, Map showing unconsolidated materials, Stafford Springs quadrangle, Connecticut: U.S. Geological Survey Miscellaneous Field Studies Map 581, 1 Plate: 22.46 × 33.24 inches, https://doi.org/10.3133/mf581A.","productDescription":"1 Plate: 22.46 × 33.24 inches","costCenters":[],"links":[{"id":180098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":398426,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3690.htm"},{"id":272634,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0581a/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Connecticut","otherGeospatial":"Stafford Springs quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.375,\n 41.875\n ],\n [\n -72.25,\n 41.875\n ],\n [\n -72.25,\n 42\n ],\n [\n -72.375,\n 42\n ],\n [\n -72.375,\n 41.875\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ce4b07f02db69e84d","contributors":{"authors":[{"text":"Pease, M. H. Jr.","contributorId":15213,"corporation":false,"usgs":true,"family":"Pease","given":"M.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":263919,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2846,"text":"wsp2027 - 1974 - Analog model study of the ground-water basin of the Upper Coachella Valley, California","interactions":[{"subject":{"id":47981,"text":"ofr71287 - 1971 - Analog model study of the ground-water basin of the upper Coachella Valley, California","indexId":"ofr71287","publicationYear":"1971","noYear":false,"title":"Analog model study of the ground-water basin of the upper Coachella Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":2846,"text":"wsp2027 - 1974 - Analog model study of the ground-water basin of the Upper Coachella Valley, California","indexId":"wsp2027","publicationYear":"1974","noYear":false,"title":"Analog model study of the ground-water basin of the Upper Coachella Valley, California"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"wsp2027","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2027","title":"Analog model study of the ground-water basin of the Upper Coachella Valley, California","docAbstract":"An analog model of the ground-water basin of the upper Coachella Valley was constructed to determine the effects of imported water on ground-water levels. The model was considered verified when the ground-water levels generated by the model approximated the historical change in water levels of the ground-water basin caused by man's activities for the period 1986-67. The ground-water basin was almost unaffected by man's activities until about 1945 when ground-water development caused the water levels to begin to decline. The Palm Springs area has had the largest water-level decline, 75 feet since 1986, because of large pumpage, reduced natural inflow from the San Gorgonio Pass area, and diversions of natural inflows at Snow and Falls Creeks and Chino Canyon starting in 1945. The San Gorgonio Pass inflow had been reduced from about 18,000 acre-feet in 1986 to about 9,000 acre-feet by 1967 because of increased ground-water pumpage in the San Gorgonio Pass area, dewatering of the San Gorgonio Pass area that took place when the tunnel for the Metropolitan Water District of Southern California was drilled, and diversions of surface inflow at Snow and Falls Creeks. In addition, 1944-64 was a period of below-normal precipitation which, in part, contributed to the declines in water levels in the Coachella Valley. The Desert Hot Springs, Garnet Hill, and Mission Creek subbasins have had relatively little development; consequently, the water-level declines have been small, ranging from 5 to 15 feet since 1986. In the Point Happy area a decline of about 2 feet per year continued until 1949 when delivery of Colorado River water to the lower valley through the Coachella Canal was initiated. Since 1949 the water levels in the Point Happy area have been rising and by 1967 were above their 1986 levels. \r\n\r\nThe Whitewater River subbasin includes the largest aquifer in the basin, having sustained ground-water pumpage of about 740,000 acre-feet from 1986 to 1967, and will probably continue to provide the most significant supply of ground water for the upper valley. The total ground-water storage depletion for the entire upper valley for 1986-67 was about 600,000 acre-feet, an average storage decrease of about 25,000 acre-feet per year since 1945. \r\n\r\nTransmissivity for the Whitewater River subbasin ranges from 860,000 gallons per day per foot (near Point Happy) to 50,000 gallons per day per foot, with most of the subbasin about 800,000 gallons per day per foot. In contrast, the transmissivities of the Desert Hot Springs, Mission Creek, and Garnet Hill subbasins generally range from 2,000 to 100,000, but the highest value, beneath the Mission Creek streambed deposits, is 200,000 gallons per day per foot; the transmissivity for most of the area of th6 three subbasins is 80,000 gallons per day per foot.\r\n\r\nThe storage coefficients are representative of water-table conditions, ranging from 0.18 beneath the Mission Creek stream deposits to 0.06 in the Palm Springs area. \r\n\r\nThe model indicated that the outflow at Point Happy decreased from 50,000 acre-feet in 1936 to 30,000 acre-feet by 1967 as a result of the rising water levels in the lower valley. \r\n\r\nThe most logical area to recharge the Colorado River water is the Windy Point-Whitewater area, where adequate percolation rates of 2-4 acre-feet per acre per day are probable. The Whitewater River bed may be the best location to spread the water if the largest part of the imported water can be recharged during low-flow periods. The area in sec. 21, T. 2 S., R. 4 E., would be adequate for the smaller quantities of recharge proposed for the Mission Creek area. \r\n\r\nProjected pumpage for the period 1968-2000 was programmed on the model with the proposed recharge of Colorado River water for the same period. The model indicated a maximum water-level increase of 200 feet above the 1967 water level at Windy Point, the proposed recharge site, by the year 2000, a 130-foot increase by 1990, and a 20-foot increas","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2027","usgsCitation":"Tyley, S.J., 1974, Analog model study of the ground-water basin of the Upper Coachella Valley, California: U.S. Geological Survey Water Supply Paper 2027, v, 77 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp2027.","productDescription":"v, 77 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138697,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2027/report-thumb.jpg"},{"id":29418,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2027/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6837f5","contributors":{"authors":[{"text":"Tyley, Stephen J.","contributorId":35355,"corporation":false,"usgs":true,"family":"Tyley","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145897,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56789,"text":"wdrLA731 - 1974 - Water resources data for Louisiana, water year 1973","interactions":[],"lastModifiedDate":"2025-02-10T17:12:13.467012","indexId":"wdrLA731","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"LA-73-1","title":"Water resources data for Louisiana, water year 1973","docAbstract":"Water resources data for the 1973 water year for West Virginia including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, records of water-quality data on the chemical and physical characteristics of surface water, and records of ground-water levels at index wells are given in this report. In Part 1, records are included for 126 gaging stations of which 119 are streamflow discharge stations, 1 is stage only streamflow station, and 6 are reservoir or lake stations; also included are records for 2 low-flow partial-record stations, 39 crest-stage partial-record stations and 7 miscellaneous sites. Locations of gaging stations are shown in Figure 1, and location of partial-record stations are shown in Figure 2. In Part 2, data on the quality of surface water (chemical, temperature, and sediment) were collected from designated sampling sites at predetermined intervals, such as once daily, weekly, monthly, or less frequently, and at some sites data were recorded on punched paper tape at 15-, 30-, or 60-minute intervals. Records are given for 28 sampling stations of which 18 are continuous record stations, and 10 are partial-record stations. Locations of water quality stations are shown in Figure 1. A few pertinent stations (not included above) in bordering States are also included in this report. In Part 3, records are included for 46 observation wells of which 8 are equipped with water-level recorders that give a continuous graph of the fluctuations, 3 are equipped with digital recorders that punch the water level on a tape at hourly intervals, at 35 manual reading are made with a steel tape by observers on the days indicated. Locations of index wells are shown in Figure 2. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Edwin E. Harris, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in West Virginia.
Beginning with the 1961 water year, streamflow records and related data have been released by the Geological Survey in annual reports on a State-boundary basis. Water-quality records beginning with the 1964 water year have been similarly released either in separate reports or in conjunction with streamflow records. These reports are for limited distribution and are designed primarily for rapid release of data shortly after the end of the water year.
Records of discharge and stage of streams, and contents and stage of lakes and reservoirs are published in a series of U.S. Geological Survey water-supply papers entitled, \"Surface Water Supply of the United States.\" Through September 30, 1960, these water-supply papers were in an annual series and since then are in a 5-year series. Records of chemical quality, water temperatures, and suspended sediment have been published since 1941 in an annual series of water-supply papers entitled, \"Quality of Surface Waters of the United States.\" More information is given under the headings \"Publications\" on page 21. Records of ground water levels are published in a series of water supply papers entitled, \"Ground-water Levels in the United States\". Through 1955 these were in an annual series but are now in a 5-year series. More information is given under the heading \"Publications\" on page 22.
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Carolina\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e753a","contributors":{"authors":[{"text":"Tarr, Arthur C. atarr@usgs.gov","contributorId":1925,"corporation":false,"usgs":true,"family":"Tarr","given":"Arthur","email":"atarr@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":172428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Kenneth W.","contributorId":54213,"corporation":false,"usgs":true,"family":"King","given":"Kenneth","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":172429,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12517,"text":"ofr74331 - 1974 - Summary appraisals of the Nation's ground-water resources; Texas Gulf region","interactions":[],"lastModifiedDate":"2016-08-10T16:11:59","indexId":"ofr74331","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-331","title":"Summary appraisals of the Nation's ground-water resources; Texas Gulf region","docAbstract":"Ground water in the Texas-Gulf Region is a large and important resource that can provide a more significant percentage of the total water supply of the region. Total water requirements within the region are projected to rise sharply from 14 million acre-feet (17 cubic kilometres) in 1970 to nearly 26 million acre-feet (32.cubic kilometres) in 2020. About half of the water used in 1970 was ground water.
\nAn estimated total of 1.04 billion acre-feet (1,280 cubic kilometres) of recoverable water containing less than 3,000 milligrams per litre dissolved solids is stored above a depth of 400 feet (122 metres) in the aquifers of the region. In addition, part of an estimated 3.28 billion acre-feet (4,040 cubic kilometres) of water in storage below 400 feet (122 metres) is recoverable. Although not all of the ground water in storage is recoverable, a significant amount is available for development, and an enormous quantity is accessible should occasions prompt its use on a time-limited basis.
\nThe total steady-state yield (amount of water that approximates the maximum perennial replenishment from precipitation) of the region's aquifers is about 4.6 million acre-feet (5.7 cubic kilometres) annually, or about 2.3 times the ground-water usage in 1970 if the large mining draft on the High Plains is not considered as part of the total steady-state yield. Because of the large quantity of recoverable ground water in storage, the steady-state yield can be augmented for a very long time on a 'deferred' basis, whereby the economic use of the water that is withdrawn from storage in excess of the steady-state yield may result in a strengthened economy.
\nAn important goal in programs for meeting future water needs should be to identify the full potential of the available ground-water resources. The subsurface reservoirs may be utilized not only as sources of fresh and treatable water, but as storage facilities for other fresh-water-supplies and as possible sources of geothermal energy. Some saline-water reservoirs may be suitable for liquid-waste storage or disposal.
\nLarge-scale and unregulated ground-water pumping may result in hydrologic problems such as declining water levels, streamflow depletion, and land-surface subsidence; but studies on proper development of the groundwater reservoirs could provide solutions to many of the problems. Water rights and other legal concepts should be based on sound hydrologic principles to assist development of water resources in an orderly and efficient manner.
\nBecause significant amounts of ground water are available, the opportunities for expanded and conjunctive use of ground water and surface water should be considered in regional plans for water development and conservation. The complexities of water management and the difficulties of achieving an integrated system of total water management will require additional technical information.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74331","usgsCitation":"Baker, E.T., and Wall, J.R., 1974, Summary appraisals of the Nation's ground-water resources; Texas Gulf region: U.S. Geological Survey Open-File Report 74-331, Report: iv, 61 p.; 11 Figures: 30.32 x 41.39 inches or smaller, https://doi.org/10.3133/ofr74331.","productDescription":"Report: iv, 61 p.; 11 Figures: 30.32 x 41.39 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":146488,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0331/report-thumb.jpg"},{"id":40760,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-01.pdf","text":"Figure 1","size":"950.37 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 1"},{"id":40761,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-02.pdf","text":"Figure 10","size":"735.75 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 10"},{"id":40762,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-03.pdf","text":"Figure 11","size":"325.46 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 11"},{"id":40763,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-04.pdf","text":"Figure 2","size":"935.74 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 2"},{"id":40764,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-05.pdf","text":"Figure 3","size":"457.42 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 3"},{"id":40765,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-06.pdf","text":"Figure 4","size":"2.30 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 4"},{"id":40766,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-07.pdf","text":"Figure 5","size":"2.23 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 5"},{"id":40767,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-08.pdf","text":"Figure 5","size":"2.23 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 5"},{"id":40768,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-09.pdf","text":"Figure 6","size":"2.56 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 6"},{"id":40769,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-10.pdf","text":"Figure 7","size":"821.78 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 7"},{"id":40770,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-11.pdf","text":"Figure 8","size":"310.10 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 8"},{"id":40771,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-12.pdf","text":"Figure 9","size":"3.01 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 9"},{"id":40772,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0331/report.pdf","text":"Report","size":"1.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Louisiana, New Mexico, Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.32617187499999,\n 31.989441837922904\n ],\n [\n -103.798828125,\n 31.541089879585808\n ],\n [\n 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T. Jr.","contributorId":88366,"corporation":false,"usgs":true,"family":"Baker","given":"E.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":166264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wall, James Ray","contributorId":14830,"corporation":false,"usgs":true,"family":"Wall","given":"James","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":166263,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42744,"text":"ofr74141 - 1974 - Preliminary geologic map of the Nereidum Montes region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:11:08","indexId":"ofr74141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-141","title":"Preliminary geologic map of the Nereidum Montes region of Mars","language":"ENGLISH","doi":"10.3133/ofr74141","usgsCitation":"Granata, G., 1974, Preliminary geologic map of the Nereidum Montes region of Mars: U.S. Geological Survey Open-File Report 74-141, 1 map; scale = 1:1000000, https://doi.org/10.3133/ofr74141.","productDescription":"1 map; scale = 1:1000000","costCenters":[],"links":[{"id":176488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"1000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67af32","contributors":{"authors":[{"text":"Granata, George","contributorId":106751,"corporation":false,"usgs":true,"family":"Granata","given":"George","email":"","affiliations":[],"preferred":false,"id":227042,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12622,"text":"ofr7122 - 1974 - Aeromagnetic map of the Gbanka quadrangle, Liberia","interactions":[{"subject":{"id":12622,"text":"ofr7122 - 1974 - Aeromagnetic map of the Gbanka quadrangle, Liberia","indexId":"ofr7122","publicationYear":"1974","noYear":false,"title":"Aeromagnetic map of the Gbanka quadrangle, Liberia"},"predicate":"SUPERSEDED_BY","object":{"id":64733,"text":"i776B - 1974 - Aeromagnetic map of the Gbanka Quadrangle, Liberia","indexId":"i776B","publicationYear":"1974","noYear":false,"chapter":"B","title":"Aeromagnetic map of the Gbanka Quadrangle, Liberia"},"id":1}],"supersededBy":{"id":64733,"text":"i776B - 1974 - Aeromagnetic map of the Gbanka Quadrangle, Liberia","indexId":"i776B","publicationYear":"1974","noYear":false,"title":"Aeromagnetic map of the Gbanka Quadrangle, Liberia"},"lastModifiedDate":"2018-03-15T14:18:24","indexId":"ofr7122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"71-22","title":"Aeromagnetic map of the Gbanka quadrangle, Liberia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7122","usgsCitation":"Behrendt, J.C., and Wotorson, C.S., 1974, Aeromagnetic map of the Gbanka quadrangle, Liberia: U.S. Geological Survey Open-File Report 71-22, 5 [i.e. 8] leaves :col. map ;27 cm. +map 44 x 45 cm. fold. in envelope 30 x 24 cm.; (5 p. - PGS); 3 sheets, scale 1:250,00, https://doi.org/10.3133/ofr7122.","productDescription":"5 [i.e. 8] leaves :col. map ;27 cm. +map 44 x 45 cm. fold. in envelope 30 x 24 cm.; (5 p. - PGS); 3 sheets, scale 1:250,00","costCenters":[],"links":[{"id":145510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69632d","contributors":{"authors":[{"text":"Behrendt, John C. jbehrendt@usgs.gov","contributorId":25945,"corporation":false,"usgs":true,"family":"Behrendt","given":"John","email":"jbehrendt@usgs.gov","middleInitial":"C.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true},{"id":213,"text":"Crustal Imaging and Characterization Team","active":false,"usgs":true}],"preferred":false,"id":166429,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wotorson, Cletus S.","contributorId":106854,"corporation":false,"usgs":true,"family":"Wotorson","given":"Cletus","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":166430,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15371,"text":"ofr7448 - 1974 - Time-dependent spectral analysis of thirty-one strong-motion earthquake records","interactions":[],"lastModifiedDate":"2024-05-08T18:25:48.635523","indexId":"ofr7448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-48","title":"Time-dependent spectral analysis of thirty-one strong-motion earthquake records","docAbstract":"Velocity response spectral analysis as a function of time for 5 percent critical damping is presented for the horizontal components of thirty-one earthquake records (61 components). A nomograph that allows conversion of the velocity response envelope to a displacement response envelope and a pseudo-absolute acceleration response envelope spectrum is also presented. Included among the records analyzed are such important accelerograms as those from El Centro, 1940, Olympia, 1949, Taft, 1952, San Francisco, 1957, Park-field, 1966, San Fernando, 1971 and Managua, 1972. Time-duration spectra showing the number of cycles for a particular period of the response envelope above different levels are presented. The effects of peak ground acceleration on the response envelope are examined.
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