{"pageNumber":"1759","pageRowStart":"43950","pageSize":"25","recordCount":46603,"records":[{"id":8688,"text":"ofr75663 - 1975 - Notes on some experiments on the application of subtractive compensation to USGS seismic magnetic tape recording and playback systems","interactions":[],"lastModifiedDate":"2012-06-02T01:01:38","indexId":"ofr75663","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-663","title":"Notes on some experiments on the application of subtractive compensation to USGS seismic magnetic tape recording and playback systems","docAbstract":"The purpose of these experiments is to lay the groundwork for the implementation of subtractive compensation of the USGS seismic network tape playbacks utilizing the Develco model 6203 discriminators at a x1 playback speed. Although the Develco discriminators were designed for this application and a matching Develco compensation discriminator was purchased, effective use of this system for subtractive compensation has been blocked by the inadequate (frequency dependent) matching of the phase of the compensation signal to that of the data signal at the point compensation is carried out in the data discriminators. John Van Schaack has ameliorated the phase mismatch problem by an empirical alteration of the compensation discriminator input bandpass filter. We have selected a set (of eight) Develco discriminators and adjusted their compensation signal input levels to minimize spurious signals (noise) originating from tape speed irregularities. The sensitivity of the data discriminators was adjusted so that deviations of +125 Hz and -125 Hz produced output signals of +2.00 volts and -2.00 volts, respectively. The eight data discriminators are driven by a multiplex signal on a single tape track (subcarriers 680, 1020, 1360, 1700, 2040, 2380, 2720, and 3060 Hz). The Develco-supplied compensation discriminator requires an unmodulated 3125 Hz signal on a separate tape track.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr75663","usgsCitation":"Eaton, J.P., 1975, Notes on some experiments on the application of subtractive compensation to USGS seismic magnetic tape recording and playback systems: U.S. Geological Survey Open-File Report 75-663, ii, 36 p., https://doi.org/10.3133/ofr75663.","productDescription":"ii, 36 p.","onlineOnly":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":379,"text":"Menlo Park Science Center","active":false,"usgs":true}],"links":[{"id":142676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_75_663.gif"},{"id":257112,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1975/0663/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6969dc","contributors":{"authors":[{"text":"Eaton, Jerry P.","contributorId":22341,"corporation":false,"usgs":true,"family":"Eaton","given":"Jerry","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":158158,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6352,"text":"pp877 - 1975 - The Black Hills-Rapid City flood of June 9-10, 1972: A description of the storm and flood","interactions":[],"lastModifiedDate":"2017-10-15T12:29:41","indexId":"pp877","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"877","title":"The Black Hills-Rapid City flood of June 9-10, 1972: A description of the storm and flood","docAbstract":"<p>On June 9, 1972, an almost stationary group of thunderstorms formed over the eastern Black Hills of South Dakota near Rapid City and produced record amounts of rainfall and flood discharges. Nearly 15 inches of rain fell in about 6 hours near Nemo, S. Dak., and more than 10 inches of rain fell over a 60-square-mile area. The resulting floods were the highest ever recorded in South Dakota. At least 18 of the 27 streams where peak flows were computed experienced flows that exceeded the 50-year flood.</p>\n<p>At least 237 people died in the Black Hills flood and 8 people were still listed as missing 6 months after the flood. Another 3,057 people were injured, and total damage is estimated to have exceeded $160 million.</p>\n<p>As documented by radar and' satellite images and by radiosonde observations, as well as by much other weather data, the unusual and excessive rainfall was partly the result of a strong, low-level, easterly airflow that forced moist air upslope over the Black Hills. This sustained orographic effect helped the air to rise, cool, become very unstable, and release its moisture in repeating -thunderstorms. Another important contributing factor was the unusually light winds at higher levels. Those light winds did not disperse the moist air or move the thunderstorms along to prevent the extreme concentration of rainfall. Instead, these conditions allowed heavy rainfall to remain almost stationary along the eastern slopes of the Black Hills.</p>\n<p>Rainfall data from 24 observing stations and from over 200 miscellaneous sites show that all reported rains greater than 4 inches fell on the eastern slopes of the Black Hills. At least 6 inches of rain fell over a 300-square-mile area that lies primarily between 4,000 and 5,000 feet elevation.</p>\n<p>Almost all the flood peaks occurred between 2230 MDT on June 9 and 0100 MDT on June 10, 1972, in a flood belt about 40 miles long and 20 miles wide along the eastern slopes of the Black Hills. This belt extended from Sturgis, S. Dak., on the north to Hermosa, S. Dak., on the south, with Rapid City near the center. To document the flood, peak discharge determinations were made at 49 sites. Records show that about 13,000 acre-feet of water flowed through Rapid City during the 2 days of flooding. At one point during the night of June 9, the floodwaters rose about 3.5 feet in 15 minutes. Coming off the slopes of the Black Hills, the flood peak traveled the 22 miles between Deer Creek and Rapid City in about 3.5 hours.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp877","usgsCitation":"Schwarz, F.K., Hughes, L., Hansen, E., Petersen, M., and Kelly, D.B., 1975, The Black Hills-Rapid City flood of June 9-10, 1972: A description of the storm and flood: U.S. Geological Survey Professional Paper 877, vi, 47 p., https://doi.org/10.3133/pp877.","productDescription":"vi, 47 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":117608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0877/report-thumb.jpg"},{"id":33704,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0877/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Dakota","city":"Rapid City","otherGeospatial":"Black Hills","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.05975341796875,\n              43.723474896114816\n            ],\n            [\n              -104.05975341796875,\n              44.55329208318493\n            ],\n            [\n              -102.99407958984375,\n              44.55329208318493\n            ],\n            [\n              -102.99407958984375,\n              43.723474896114816\n            ],\n            [\n              -104.05975341796875,\n              43.723474896114816\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db6823d7","contributors":{"authors":[{"text":"Schwarz, Francis K.","contributorId":100832,"corporation":false,"usgs":true,"family":"Schwarz","given":"Francis","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":152564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hughes, L.A.","contributorId":8840,"corporation":false,"usgs":true,"family":"Hughes","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":152561,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hansen, E.M.","contributorId":106479,"corporation":false,"usgs":true,"family":"Hansen","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":152565,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Petersen, M.S.","contributorId":41818,"corporation":false,"usgs":true,"family":"Petersen","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":152562,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kelly, Donovan B.","contributorId":56205,"corporation":false,"usgs":true,"family":"Kelly","given":"Donovan","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":152563,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":10068,"text":"ofr75669 - 1975 - Audio-magnetotelluric data log and station location map for Gerlach Known Geothermal Resource Area, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr75669","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-669","title":"Audio-magnetotelluric data log and station location map for Gerlach Known Geothermal Resource Area, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr75669","usgsCitation":"Long, C.L., Senterfit, R.M., and Kaufmann, H., 1975, Audio-magnetotelluric data log and station location map for Gerlach Known Geothermal Resource Area, Nevada: U.S. Geological Survey Open-File Report 75-669, 6 leaves :map ;28 cm., https://doi.org/10.3133/ofr75669.","productDescription":"6 leaves :map ;28 cm.","costCenters":[],"links":[{"id":144461,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669321","contributors":{"authors":[{"text":"Long, Carl L.","contributorId":32128,"corporation":false,"usgs":true,"family":"Long","given":"Carl","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senterfit, R. Michael","contributorId":10791,"corporation":false,"usgs":true,"family":"Senterfit","given":"R.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":160761,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaufmann, Harold","contributorId":86774,"corporation":false,"usgs":true,"family":"Kaufmann","given":"Harold","affiliations":[],"preferred":false,"id":160763,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4218,"text":"cir712 - 1975 - Earth science data in urban and regional information systems; a review","interactions":[],"lastModifiedDate":"2012-02-02T00:05:47","indexId":"cir712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"712","title":"Earth science data in urban and regional information systems; a review","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir712","usgsCitation":"Adams, V.W., 1975, Earth science data in urban and regional information systems; a review: U.S. Geological Survey Circular 712, iii,29 p. :ill., maps ; 26 cm., https://doi.org/10.3133/cir712.","productDescription":"iii,29 p. :ill., maps ; 26 cm.","costCenters":[],"links":[{"id":118233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1975/0712/report-thumb.jpg"},{"id":31332,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1975/0712/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c164","contributors":{"authors":[{"text":"Adams, Victor W.","contributorId":50884,"corporation":false,"usgs":true,"family":"Adams","given":"Victor","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":148431,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9485,"text":"ofr75581 - 1975 - A compilation of data from the 1973 Long Valley, California, seismic-refraction experiment","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr75581","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-581","title":"A compilation of data from the 1973 Long Valley, California, seismic-refraction experiment","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr75581","usgsCitation":"Hill, D.P., and McHugh, S., 1975, A compilation of data from the 1973 Long Valley, California, seismic-refraction experiment: U.S. Geological Survey Open-File Report 75-581, 35 leaves :ill., map ;28 cm.; (21 p. - PGS), https://doi.org/10.3133/ofr75581.","productDescription":"35 leaves :ill., map ;28 cm.; (21 p. - PGS)","costCenters":[],"links":[{"id":141930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0581/report-thumb.jpg"},{"id":37193,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0581/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0f26","contributors":{"authors":[{"text":"Hill, David P. hill@usgs.gov","contributorId":2600,"corporation":false,"usgs":true,"family":"Hill","given":"David","email":"hill@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":false,"id":159771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McHugh, Stuart","contributorId":8852,"corporation":false,"usgs":true,"family":"McHugh","given":"Stuart","email":"","affiliations":[],"preferred":false,"id":159772,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8577,"text":"ofr75411 - 1975 - Sediments, structural framework, petroleum potential, environmental conditions, and operational considerations of the United States South Atlantic Outer Continental Shelf","interactions":[],"lastModifiedDate":"2022-07-20T19:29:33.761823","indexId":"ofr75411","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-411","title":"Sediments, structural framework, petroleum potential, environmental conditions, and operational considerations of the United States South Atlantic Outer Continental Shelf","docAbstract":"<p>The area designated for possible oil and gas lease sale in Bureau of Land Management memorandum 3310 #43 (722) and referred to therein as part of the United States South Atlantic Outer Continental Shelf (OCS) contains about 98,000 square kilometres of the continental margin seaward of the 3 mile offshore limit and within the 600 metre isobath. The designated area, offshore of North Carolina, South Carolina, Georgia, and Florida, encompasses parts of three physiographic provinces: the Continental Shelf, the Florida-Hatteras Slope, and the Blake Plateau. </p><p>The structural framework of the U.3. South Atlantic region is dominated by the Southeast Georgia Embayment --an east-plunging depression recessed into the Atlantic Coastal Plain and shelf between Cape Fear, North Carolina and Jacksonville, Florida. The embayment is bounded to the north by the Cape Fear Arch and to southeast by the Peninsular Arch. </p><p>Refraction data indicate a minor basement(?) ridge beneath the outer shelf between 30° and 32°N at 80°W. Drill hole data also suggest a gentle fold or accretionary structure (reef?) off the east coast of Florida. Several other structural features have been identified by refraction and reflection techniques and drilling. These are the Yamacraw Uplift, Burton High, Stone Arch, and the Suwannee Channel. </p><p>Gravity and magnetic anomalies within the area probably result from emplacement of magma bodies along linear features representing fundamental crustal boundaries. Of these anomalies, the most prominent, is a segment of the East Coast Magnetic Anomaly which crosses the coast at Brunswick, Georgia. This anomaly has been interpreted as representing an ancient continental boundary where two formerly separate continental plates collided and were welded together. </p><p>There may be as much as 5,000 m of sedimentary rocks in the Southeast Georgia Embayment out to the 600 m isobath. Basement rocks beneath the Southeast Georgia Embayment are expected to be similar to those exposed in the Appalachian Piedmont province. Triassic deposits are likely to exist beneath the inner Continental Shelf, and probably consist of nonmarine arkosic sandstones, shales, basalt flows, and diabase intrusions deposited in relatively narrow northeast-trending grabens. Jurassic marine carbonates in the Bahamas grade northward to carbonates, shales, sand, and arkose in North Carolina. Salt may be present in the basal Jurassic section in the Southeast Georgia Embayment. Up to 4,000 m of Jurassic-Lower Cretaceous rocks are expected out to the 600 m water depth. Lower Cretaceous rocks in southern Florida are shallow-water marine limestone and dolomites with beds of anhydrite. In coastal North Carolina the Lower Cretaceous is a marine section made up of shales, sand, and sandy limestone. The Upper Cretaceous is composed almost entirely of marine carbonates in southern Florida grading northward to nonmarine to marginal marine, sandstones and shales with minor amounts of carbonates. In general, Upper Cretaceous rocks will probably maintain a fairly constant thickness (600 m) on the Continental Shelf and grade downdip from terrigeneous sands and shales to more marine chalks, limestones, and dolomites. The Cenozoic rocks are predominantly shallow-water marine carbonates in Florida grading northward into a marginal marine to marine clastic facies composed of sands, marls, and limestones. The offshore Cenozoic section is expected to range in thickness from 600 to 1100 m. </p><p><br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75411","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Sediments, structural framework, petroleum potential, environmental conditions, and operational considerations of the United States South Atlantic Outer Continental Shelf: U.S. Geological Survey Open-File Report 75-411, Report: vii, 262 p.; 1 Sheet: 16.88 x 32.94 inches, https://doi.org/10.3133/ofr75411.","productDescription":"Report: vii, 262 p.; 1 Sheet: 16.88 x 32.94 inches","costCenters":[],"links":[{"id":36147,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0411/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36148,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0411/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0411/report-thumb.jpg"},{"id":404154,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15175.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida, Georgia, South Carolina","otherGeospatial":"South Atlantic Outer Continental Shelf","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.55224609374999,\n              33.8430453147447\n            ],\n            [\n              -79.12353515625,\n              33.4039312002347\n            ],\n            [\n              -79.22241210937499,\n              33.09614359735857\n            ],\n            [\n              -79.837646484375,\n              32.713355353177555\n            ],\n            [\n              -81.1285400390625,\n              31.522361470421437\n            ],\n            [\n              -81.419677734375,\n              30.755998458321667\n            ],\n            [\n              -81.243896484375,\n              29.850173125689896\n            ],\n            [\n              -80.76599121093749,\n              28.86872905602898\n            ],\n            [\n              -80.452880859375,\n              28.70986084394286\n            ],\n            [\n              -79.07958984375,\n              28.748396571187406\n            ],\n            [\n              -78.6895751953125,\n              29.176145182559758\n            ],\n            [\n              -74.937744140625,\n              33.137551192346145\n            ],\n            [\n              -75.6793212890625,\n              33.82023008524739\n            ],\n            [\n              -76.92626953125,\n              33.87041555094183\n            ],\n            [\n              -78.02490234375,\n              33.8339199536547\n            ],\n            [\n              -78.55224609374999,\n              33.8430453147447\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbad0","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":528874,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5715,"text":"pp924 - 1975 - Hurricane Agnes rainfall and floods, June-July 1972","interactions":[],"lastModifiedDate":"2024-06-17T20:00:45.580721","indexId":"pp924","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"924","title":"Hurricane Agnes rainfall and floods, June-July 1972","docAbstract":"<p>Hurricane Agnes originated in the Caribbean Sea region in mid-June. Circulation barely reached hurricane intensity for a brief period in the Gulf of Mexico. The storm crossed the Florida Panhandle coastline on June 19, 1972, and followed an unusually extended overland trajectory combining with an extratropical system to bring very heavy rain from the Carolinas northward to New York. This torrential rain followed the abnormally wet May weather in the Middle Atlantic States and set the stage for the subsequent major flooding. The record-breaking floods occurred in the Middle Atlantic States in late June and early July 1972. Many streams in the affected area experienced peak discharges several times the previous maxima of record. Estimated recurrence intervals of peak flows at many gaging stations on major rivers and their tributaries exceeded 100 years. The suspended-sediment concentration and load of most flooded streams were also unusually high. The widespread flooding from this storm caused Agnes to be called the most destructive hurricane in United States history, claiming 117 lives and causing damage estimated at $3.1 billion in 12 States. Damage was particularly high in New York, Pennsylvania, Maryland, and Virginia. The detailed life history of Hurricane Agnes, including the tropical depression and tropical storm stages, is traced. Associated rainfalls are analyzed and compared with climatologic recurrence values. These are followed by a detailed description of the flood and streamflows of each affected basin. A summary of peak stages and discharges and comparison data for previous floods at 989 stations are presented. Deaths and flood damage estimates are compiled. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp924","usgsCitation":"Bailey, J.F., Patterson, J.L., and Paulhus, J.L., 1975, Hurricane Agnes rainfall and floods, June-July 1972: U.S. Geological Survey Professional Paper 924, Report: vii, 403 p.; 1 Plate: 30.00 x 42.00 inches, https://doi.org/10.3133/pp924.","productDescription":"Report: vii, 403 p.; 1 Plate: 30.00 x 42.00 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":118423,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0924/report-thumb.jpg"},{"id":32286,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0924/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32285,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0924/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104754,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5110.htm","linkFileType":{"id":5,"text":"html"},"description":"5110"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -79.17353337473213,\n              43.938644324808564\n            ],\n            [\n              -80.88780186579464,\n              35.83761262246428\n            ],\n            [\n              -75.21324700938271,\n              35.862166390663944\n            ],\n            [\n              -70.44403607851471,\n              42.89279462125202\n            ],\n            [\n              -79.17353337473213,\n              43.938644324808564\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a4f9","contributors":{"authors":[{"text":"Bailey, James F.","contributorId":91834,"corporation":false,"usgs":true,"family":"Bailey","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":151478,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patterson, James Lee","contributorId":24329,"corporation":false,"usgs":true,"family":"Patterson","given":"James","email":"","middleInitial":"Lee","affiliations":[],"preferred":false,"id":151476,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paulhus, Joseph Louis Hornore","contributorId":33705,"corporation":false,"usgs":true,"family":"Paulhus","given":"Joseph","email":"","middleInitial":"Louis Hornore","affiliations":[],"preferred":false,"id":151477,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7919,"text":"ofr7536 - 1975 - Rutile and sphene in blueschist and related high-pressure facies rocks","interactions":[],"lastModifiedDate":"2024-07-15T18:57:01.351591","indexId":"ofr7536","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-36","title":"Rutile and sphene in blueschist and related high-pressure facies rocks","docAbstract":"<p>Sphene and rutile are characteristic accessory minerals of blueschist facies metamorphic rocks. However, only sphene is present in the lowerr grade blueschist assemblages. In many areas of the world these blueschists pass into, or are in fault contact with, higher grade glaucophane schists, rutile-bearing amphibolites, and eclogites. The origin of the rutile may be related to a prograde metamorphic reaction that involves the alteration of sphene to rutile, but few data are available to support this hypothesis. It seems more probable that the rutile crystallized directly from ilmenite or titanium-rich clinopyroxene and magnetite in basalts and gabbros during the conversion of these rocks to amphibolites and eclogites containing omphacite, amphibolite, and garnet. Rutile in the higher grade blueschists, regardless of its origin, is a potential titanium resource and is currently being mined from eclogite and glaucophane-eclogite rocks in the Soviet Union. Resources are likely to be up to millions of tons contained Ti0<span style=\"font-size: 11.6667px;\">2</span>.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7536","usgsCitation":"Blake, M., and Morgan, B.A., 1975, Rutile and sphene in blueschist and related high-pressure facies rocks: U.S. Geological Survey Open-File Report 75-36, i, 20 p., https://doi.org/10.3133/ofr7536.","productDescription":"i, 20 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":140705,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0036/report-thumb.jpg"},{"id":431101,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cafa","contributors":{"authors":[{"text":"Blake, M.C.","contributorId":8470,"corporation":false,"usgs":true,"family":"Blake","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":156832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, Benjamin A.","contributorId":32158,"corporation":false,"usgs":true,"family":"Morgan","given":"Benjamin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":156833,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7819,"text":"ofr75619 - 1975 - Surface current observations--Beaufort Sea, 1972","interactions":[],"lastModifiedDate":"2021-10-19T10:56:34.357712","indexId":"ofr75619","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-619","title":"Surface current observations--Beaufort Sea, 1972","docAbstract":"Sediment transport via water and ice in the Beaufort Sea off northern Alaska is related to the movement of the surficial waters. As development proceeds along the north slope of alaska, a knowledge of the potential drift trajectories of water, ice, sediment and pollutants will be needed. In an attempt to better define the probable paths and rates of transport, 4200 surface drift cards were dropped during the U.S. Coast Guard WEBSEC cruise of August and September, 1972. The results of this release are the subject of this report. Because the data presented here will be used primarily by those interested in solving problems of transport, the emphasis has been placed on data presentation rather than a detailed analysis of the circulation. (Sinha-OEIS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75619","usgsCitation":"Barnes, P., and Garlow, R., 1975, Surface current observations--Beaufort Sea, 1972: U.S. Geological Survey Open-File Report 75-619, Report: 10 p.; 1 Plate: 42.06 × 18.00 inches, https://doi.org/10.3133/ofr75619.","productDescription":"Report: 10 p.; 1 Plate: 42.06 × 18.00 inches","costCenters":[],"links":[{"id":140953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0619/report-thumb.jpg"},{"id":35316,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0619/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35317,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0619/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":108640,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15218.htm","linkFileType":{"id":5,"text":"html"},"description":"15218"}],"country":"United States","state":"Alaska","otherGeospatial":"Beaufort Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -157.236328125,\n              69.31832006949072\n            ],\n            [\n              -140.44921875,\n              69.31832006949072\n            ],\n            [\n              -140.44921875,\n              71.66366293141732\n            ],\n            [\n              -157.236328125,\n              71.66366293141732\n            ],\n            [\n              -157.236328125,\n              69.31832006949072\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698366","contributors":{"authors":[{"text":"Barnes, Peter","contributorId":66684,"corporation":false,"usgs":true,"family":"Barnes","given":"Peter","affiliations":[],"preferred":false,"id":156668,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garlow, Richard","contributorId":107697,"corporation":false,"usgs":true,"family":"Garlow","given":"Richard","email":"","affiliations":[],"preferred":false,"id":156669,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5911,"text":"pp827 - 1975 - Geology of the Sierra Foothills Melange and adjacent areas, Amador County, California","interactions":[],"lastModifiedDate":"2019-11-14T14:29:42","indexId":"pp827","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"827","title":"Geology of the Sierra Foothills Melange and adjacent areas, Amador County, California","docAbstract":"<p>Detailed outcrop mapping in the western Sierra foothills of Amador County, Calif., has resulted in some major changes in the interpretation of stratigraphy and structure. The Amador Group was originally defined at its type locality on the south bank of the Cosumnes River in Amador County to include the Cosumnes Formation and the conformably overlying Logtown Ridge Formation, but the new data indicate that the lower boundary of the type Logtown Ridge should be located 600 m farther west (downsection) than originally designated and that this boundary is a fault. The strata that were originally called the Cosumnes Formation are part of a lithologically diverse assemblage of tectonically intermixed rocks that constitute a newly recognized melange and thus are not a formational rock-stratigraphic unit as the earlier workers believed. Thus, the names Cosumnes Formation and Amador Group are both inappropriate in their type area and are abandoned.</p><p>The Logtown Ridge Formation is here divided into four members, some of which cross what earlier was considered to be a formational boundary of the Logtown Ridge with overlapping pyroclastic strata. The outcrop mapping requires additional changes, although of lesser importance, in the identification and correlation of other Mesozoic rocks in Amador County.</p><p>The newly recognized melange forms a 4-km-wide belt underlying the Logtown Ridge Formation. In addition to the type section of the abandoned Cosumnes Formation and scattered fault-bounded blocks of strata of Cosumnes lithology, the melange comprises rocks heretofore mapped as \"western belt of Calaveras Formation,\" considered to be of Paleozoic age. Single clasts of this huge tectonic breccia range from a few centimeters to a few kilometers in maximum dimension. Distinctive strata are generally disrupted, and pervasive shearing is common. In the absence of fossils, no age of original deposition can be assigned to any clast or matrix of the melange, but on the basis of indirect structural evidence, the intermixing that formed the melange probably took place during the Late Jurassic or before, and therefore the now sheared and faulted strata must originally have been at least this old.</p><p>Available data are ambiguous but suggest that rocks were intermixed to form the melange when the strata were horizontal or nearly so. Similarly, the overlying Logtown Ridge and Mariposa Formations were faulted when these rocks were essentially horizontal. The entire section was subsequently tilted to its present, nearly vertical position.</p><p>Traditional syntheses of the tectonic history of the Sierra foothills argue that the faults there have always been steeply dipping. Although this may be true for some faults, the new interpretation suggests that most faulting occurred before the section was steeply tilted. Neither suggestion can yet be proved, but we maintain that the highly deformed rocks mapped in Amador County represent primarily the effects of subduction at a continental margin, possibly augmented by gravity tectonics in a trough of sediment accumulation there. On the basis of the ages of affected strata, this period of subduction was Late Jurassic but possibly began at an earlier time. If this interpretation of the melange in Amador County is correct, a belt of&nbsp;similarly deformed rocks should extend far beyond the limits of the study area.&nbsp;</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp827","usgsCitation":"Duffield, W.A., and Sharp, R.V., 1975, Geology of the Sierra Foothills Melange and adjacent areas, Amador County, California: U.S. Geological Survey Professional Paper 827, Report: iii, 30 p.; 1 Plate: 40.99 x 56.88 inches, https://doi.org/10.3133/pp827.","productDescription":"Report: iii, 30 p.; 1 Plate: 40.99 x 56.88 inches","costCenters":[],"links":[{"id":139598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0827/report-thumb.jpg"},{"id":112646,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0827/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":369221,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0827/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","datum":"Mean sea level","country":"United States","state":"California","county":"Amador County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.93750000,\n              38.28333333\n            ],\n            [\n              -120.75,\n              38.28333333\n            ],\n            [\n              -120.75,\n              38.56666667\n            ],\n            [\n              -120.93750000,\n              38.56666667\n            ],\n            [\n              -120.93750000,\n              38.28333333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e50b","contributors":{"authors":[{"text":"Duffield, Wendell A.","contributorId":14363,"corporation":false,"usgs":true,"family":"Duffield","given":"Wendell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":151797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sharp, Robert V.","contributorId":89857,"corporation":false,"usgs":true,"family":"Sharp","given":"Robert","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":151798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1068,"text":"wsp1827F - 1975 - Reactions of aqueous aluminum species at mineral surfaces","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1827F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"1827","chapter":"F","title":"Reactions of aqueous aluminum species at mineral surfaces","docAbstract":"Aqueous aluminum solutions containing 4.5 ? 10 4 molar aluminum in 0.01 molar NaC104 were partly neutralized with NaOH to give OH:A1 mole ratios from 1.40 to 2.76. \r\n\r\nMeasured amounts of montmorillonite, kaolinite, volcanic ash, or feldspathic sand were added to provide an area of inert surface. Reactions that occurred during 100 days of aging were compared with those in similar solutions without added surfaces, studied in earlier work. \r\n\r\nAdsorption of monomeric species Al(H20)6+3, AlOH(H2O)5+2, and Al(OH)2(H2O 4? on the added surfaces follows a cation exchange mass law equilibrium model, and adsorption is essentially complete in 1 hour. Only minor changes in monomeric aluminum species occurred after that. \r\n\r\nRapid adsorption of polynuclear aluminum hydroxide species also occurs and follows the pattern of the Langmuir adsorption isotherm. In the absence of surfaces, the polynuclear ions slowly increase in size and become microcrystalline gibbsite during aging. Electron micrographs showed microcrystalline gibbsite was present or surfaces after aging only 2 days. However, the analytical data suggest this material must have been adsorbed after it had already attained a near-crystalline state. Adsorbed polynuclear aluminum hydroxide species were not extensively converted to microcrystalline gibbsite during 100 days of aging.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1827F","usgsCitation":"Brown, D.W., and Hem, J.D., 1975, Reactions of aqueous aluminum species at mineral surfaces: U.S. Geological Survey Water Supply Paper 1827, iv, 48 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1827F.","productDescription":"iv, 48 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1827f/report-thumb.jpg"},{"id":25748,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1827f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648685","contributors":{"authors":[{"text":"Brown, David Wayne","contributorId":77124,"corporation":false,"usgs":true,"family":"Brown","given":"David","email":"","middleInitial":"Wayne","affiliations":[],"preferred":false,"id":143127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hem, John David","contributorId":42577,"corporation":false,"usgs":true,"family":"Hem","given":"John","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":143126,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2127,"text":"wsp1827G - 1975 - Effects of organic solutes on chemical reactions of aluminum","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1827G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"1827","chapter":"G","title":"Effects of organic solutes on chemical reactions of aluminum","docAbstract":"Concentrations of organic matter in the general range of 1-10 milligrams per litre organic carbon are common in natural water, and many naturally occurrin7 organic compounds form aluminum complexes. The aluminum concentrations in near-neutral pH solutions may be 10-100 times higher than the values predicted from solubility data if formation of such organic complexes is ignored. The processes of polymerization of aluminum hydroxide and precipitation of gibbsite are inhibited by the presence of the organic flavone compound quercetin in concentrations as low as 10 x -5.3 mole per litre. Quercetin forms a complex, with a probable molar ratio of 1:2 aluminum to quercetin, that has a formation constant (f12) of about 10 12. A complex with a higher aluminum-quercetin ratio also was observed, but this material tends to evolve into a compound of low solubility that removes aluminum from solution. \r\n\r\nIn the presence of both dissolved aluminum and aqueous silica, low concentrations of quercetin improved the yield of crystallized kaolinite and halloysite. Small amounts of well-shaped kaolinite and halloysite crystals were identified by electron microscopy in solutions with pH's in the range 6.5-8.5 after 155 days aging in one experimer t and 481 days aging in a repeated experiment. The bulk of the precipitated material was amorphous to X-rays, and crystalline material was too small a proportion of the total to give identifiable X-ray diffraction peaks. The precipitates had aluminum-silicon ratios near 1, and their solubility corresponded to that found by Hem, Roberson, Lind, and Polzer (1973) for similar aluminosilicate precipitated in the absence of organic solutes. The improved yield of crystalline material obtained in the presence of quercetin probably is the result of the influence of the organic compound on the aluminum hydroxide polymerization process. \r\n\r\nNatural water containing color imparted by organic material tends to be higher in aluminum than would be predicted by pH, silica concentrations, and solubility data for inorganic aluminum species.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1827G","usgsCitation":"Lind, C.J., and Hem, J.D., 1975, Effects of organic solutes on chemical reactions of aluminum: U.S. Geological Survey Water Supply Paper 1827, v, 83 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1827G.","productDescription":"v, 83 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1827g/report-thumb.jpg"},{"id":27727,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1827g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686720","contributors":{"authors":[{"text":"Lind, Carol J.","contributorId":36110,"corporation":false,"usgs":true,"family":"Lind","given":"Carol","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":144709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hem, John David","contributorId":42577,"corporation":false,"usgs":true,"family":"Hem","given":"John","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":144710,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7807,"text":"ofr75207 - 1975 - A geologic analysis of the Side-Looking Airborne Radar imagery of southern New England","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr75207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-207","title":"A geologic analysis of the Side-Looking Airborne Radar imagery of southern New England","docAbstract":"Analysis of the side looking airborn radar imagery of Massachusetts, Connecticut and Rhode Island indicates that radar shows the topography in great detail. Since bedrock geologic features are frequently expressed in the topography the radar lends itself to geologic interpretation. \r\n\r\nThe radar was studied by comparisons with field mapped geologic data first at a scale of approximately 1:125,000 and then at a scale of 1:500,000. The larger scale comparison revealed that faults, minor faults, joint sets, bedding and foliation attitudes, lithology and lithologic contacts all have a topographic expression interpretable on the imagery. Surficial geologic features were far less visible on the imagery over most of the area studied. The smaller scale comparisons revealed a pervasive, near orthogonal fracture set cutting all types and ages of rock and trending roughly N40?E and N30?W. In certain places the strike of bedding and foliation attitudes and some lithologic Contacts were visible in addition to the fractures. \r\n\r\nFracturing in southern New England is apparently far more important than has been previously recognized. This new information, together with the visibility of many bedding and foliation attitudes and lithologic contacts, indicates the importance of radar imagery in improving the geologic interpretation of an area.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr75207","usgsCitation":"Banks, P.T., 1975, A geologic analysis of the Side-Looking Airborne Radar imagery of southern New England: U.S. Geological Survey Open-File Report 75-207, 126, A23 leaves, 6 sheets :ill., maps ;29 cm., https://doi.org/10.3133/ofr75207.","productDescription":"126, A23 leaves, 6 sheets :ill., maps ;29 cm.","costCenters":[],"links":[{"id":94830,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0207/plate-1.pdf","size":"4004","linkFileType":{"id":1,"text":"pdf"}},{"id":94831,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0207/plate-2.pdf","size":"2843","linkFileType":{"id":1,"text":"pdf"}},{"id":94832,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0207/plate-3.pdf","size":"2358","linkFileType":{"id":1,"text":"pdf"}},{"id":94833,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0207/plate-4.pdf","size":"2618","linkFileType":{"id":1,"text":"pdf"}},{"id":94834,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0207/plate-5.pdf","size":"2627","linkFileType":{"id":1,"text":"pdf"}},{"id":94835,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0207/plate-6.pdf","size":"2915","linkFileType":{"id":1,"text":"pdf"}},{"id":140379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0207/report-thumb.jpg"},{"id":35305,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6a0","contributors":{"authors":[{"text":"Banks, Paul T.","contributorId":84362,"corporation":false,"usgs":true,"family":"Banks","given":"Paul","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":156642,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5728,"text":"pp941A - 1975 - Studies for seismic zonation of the San Francisco Bay region","interactions":[],"lastModifiedDate":"2018-06-12T12:04:33","indexId":"pp941A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"941","chapter":"A","title":"Studies for seismic zonation of the San Francisco Bay region","docAbstract":"<p>The analyses presented in the preceding six papers show that the geologic setting of the San Francisco Bay region has a dominant influence on potential earthquake hazards. The strong correlation between geologic conditions and the amount of earthquake damage in 1906 emphasizes the importance of this influence and demonstrates the need for seismic zonation. Seismic zonation can provide the logical basis for preparation of special-purpose land-use maps that, with appropriate public policy, would be a significant step toward reducing the currently expected catastrophic effects of another great earthquake (Algermissen, 1972). </p><p>Seismic zonation requires a set of integrated multidisciplinary predictions about the geologic effects of potential earthquakes. To illustrate a strategy for making such predictions, a demonstration profile has been chosen perpendicular to a segment of the San Andreas fault, along which a magnitude 6.5 earthquake has been postulated. This profile includes a wide variety of geologic conditions and provides a means for application of the analyses presented in the preceding six papers. </p><p>Earthquake hazards to life and property originate from (1) surface faulting, (2) ground shaking, (3) flooding, (4) liquefaction, and (5) landsliding. The extent to which each of these geologic effects can be predicted for an earthquake of a given magnitude and location depends on the current state of the art. To illustrate techniques and data currently available, each effect is considered for the postulated earthquake. </p><p>This paper does not provide final estimates for the total earthquake hazard along the demonstration profile. Such an objective would require analysis of individual manmade structures as well as consideration of earthquakes of other sizes and locations. Instead, this paper illustrates the extent to which the above effects can be predicted for an earthquake of this given size and location. Such an analysis demonstrates a methodology for seismic zonation based on available data. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp941A","usgsCitation":"Borcherdt, R.D., 1975, Studies for seismic zonation of the San Francisco Bay region: U.S. Geological Survey Professional Paper 941, 101 p., https://doi.org/10.3133/pp941A.","productDescription":"101 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":32308,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0941a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0941a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2d1","contributors":{"authors":[{"text":"Borcherdt, Roger D. 0000-0002-8668-0849 borcherdt@usgs.gov","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":2373,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Roger","email":"borcherdt@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":151492,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8550,"text":"ofr75219 - 1975 - Interpretation of Fischer assay data for the evaluation of analcime-bearing oil shale in the Green River Formation, Colorado and Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr75219","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-219","title":"Interpretation of Fischer assay data for the evaluation of analcime-bearing oil shale in the Green River Formation, Colorado and Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr75219","usgsCitation":"Desborough, G.A., and Pitman, J.K., 1975, Interpretation of Fischer assay data for the evaluation of analcime-bearing oil shale in the Green River Formation, Colorado and Utah: U.S. Geological Survey Open-File Report 75-219, 26 leaves :ill., map ;27 cm.; (30 p. - PGS), https://doi.org/10.3133/ofr75219.","productDescription":"26 leaves :ill., map ;27 cm.; (30 p. - PGS)","costCenters":[],"links":[{"id":141741,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e063b","contributors":{"authors":[{"text":"Desborough, George A.","contributorId":101661,"corporation":false,"usgs":true,"family":"Desborough","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":157921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pitman, Janet K. 0000-0002-0441-779X jpitman@usgs.gov","orcid":"https://orcid.org/0000-0002-0441-779X","contributorId":767,"corporation":false,"usgs":true,"family":"Pitman","given":"Janet","email":"jpitman@usgs.gov","middleInitial":"K.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":157920,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10062,"text":"ofr75585 - 1975 - Land subsidence and tectonism, Raft River Valley, Idaho","interactions":[],"lastModifiedDate":"2024-02-28T17:29:14.543073","indexId":"ofr75585","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-585","title":"Land subsidence and tectonism, Raft River Valley, Idaho","docAbstract":"<p>A comparison of 1974 leveling data with elevations established 40 years earlier reveals two types of vertical ground movement which have occurred in Raft River Valley, Idaho: (1) regional differential movement of about 0.22 ft (6.4 cm), apparently due to tectonism, and (2) extensive land subsidence of as much as 2.61 ft (0.80 m) caused by withdrawal of ground water. Data are too sparse to calculate the magnitude or areal extent of subsidence; however, tentative lines of equal subsidence suggest that the area affected by subsidence probably exceeds 100 mi<sup>2</sup> (260 km<sup>2</sup>).</p><p>In order to estimate historic subsidence or subsidence potential in Raft River Valley serious consideration should be given to a field program of basic-data collection. Leveling along a few carefully selected lines of existing control and the installation and operation of extensometer water-level recorders in areas of continuing water-level decline would provide useful data for evaluating past and estimating future subsidence.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75585","usgsCitation":"Lofgren, B.E., 1975, Land subsidence and tectonism, Raft River Valley, Idaho: U.S. Geological Survey Open-File Report 75-585, 21 p., https://doi.org/10.3133/ofr75585.","productDescription":"21 p.","costCenters":[],"links":[{"id":426078,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0585/report.pdf"},{"id":144435,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0585/report-thumb.jpg"}],"scale":"126720","country":"United States","state":"Idaho","otherGeospatial":"Raft River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113.5,\n              42.5\n            ],\n            [\n              -113.5,\n              42\n            ],\n            [\n              -113.25,\n              42\n            ],\n            [\n              -113.25,\n              42.5\n            ],\n            [\n              -113.5,\n              42.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b4168","contributors":{"authors":[{"text":"Lofgren, Ben Elder","contributorId":52973,"corporation":false,"usgs":true,"family":"Lofgren","given":"Ben","email":"","middleInitial":"Elder","affiliations":[],"preferred":false,"id":160752,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8355,"text":"ofr75587 - 1975 - Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Teller Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2024-04-05T20:57:51.782509","indexId":"ofr75587","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-587","title":"Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Teller Quadrangle, Alaska","docAbstract":"<p>This summary of references is designed to aid in library research on metallic and nonmetallic (other than mineral fuels and construction materials) mineral occurrences in the Teller quadrangle, Alaska. All references to published and open-filed reports of the Geological Survey, to most published and open-filed reports of the U.S. Bureau of Mines, and to most published reports of the State of Alaska Division of Geological and Geophysical Surveys and its predecessor State and Territorial agencies released before January 1, 1975, are summarized. Certain, mainly statistical, reports such as the annual Minerals Yearbook of the U.S. Bureau of Mines and the biennial and annual reports of the State of Alaska Division of Gedlogical and Geophysical Surveys and its predecessor State and Territorial agencies are not included.</p><p>This summary is divided into three parts: a section made up of summaries of references arranged alphabetically by occurrence name; a section that lists synonyms for names in the first section, claim names, and the names of operators and owners of mines and prospects; and a section that lists, by author, all references summarized in the first section and cited in introductory paragraphs. Pages are not numbered because users may wish to add data from other sources.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75587","usgsCitation":"Cobb, E.H., 1975, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Teller Quadrangle, Alaska: U.S. Geological Survey Open-File Report 75-587, 148 p., https://doi.org/10.3133/ofr75587.","productDescription":"148 p.","costCenters":[],"links":[{"id":427523,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0587/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140258,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0587/report.thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Teller Quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -169.15,\n              64.955\n            ],\n            [\n              -165,\n              64.955\n            ],\n            [\n              -165,\n              66\n            ],\n            [\n              -169.15,\n              66\n            ],\n            [\n              -169.15,\n              64.955\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698bd7","contributors":{"authors":[{"text":"Cobb, Edward Huntington","contributorId":25916,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward","email":"","middleInitial":"Huntington","affiliations":[],"preferred":false,"id":157587,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8993,"text":"ofr75150 - 1975 - Age and tectonic significance of volcanic rocks on St. Matthew Island, Bering Sea, Alaska","interactions":[{"subject":{"id":8993,"text":"ofr75150 - 1975 - Age and tectonic significance of volcanic rocks on St. Matthew Island, Bering Sea, Alaska","indexId":"ofr75150","publicationYear":"1975","noYear":false,"title":"Age and tectonic significance of volcanic rocks on St. Matthew Island, Bering Sea, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":58767,"text":"mf642 - 1975 - Reconnaissance geologic map of St. Matthew Island, Bering Sea, Alaska","indexId":"mf642","publicationYear":"1975","noYear":false,"title":"Reconnaissance geologic map of St. Matthew Island, Bering Sea, Alaska"},"id":1}],"supersededBy":{"id":58767,"text":"mf642 - 1975 - Reconnaissance geologic map of St. Matthew Island, Bering Sea, Alaska","indexId":"mf642","publicationYear":"1975","noYear":false,"title":"Reconnaissance geologic map of St. Matthew Island, Bering Sea, Alaska"},"lastModifiedDate":"2023-12-08T18:44:52.063774","indexId":"ofr75150","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-150","title":"Age and tectonic significance of volcanic rocks on St. Matthew Island, Bering Sea, Alaska","docAbstract":"<p>Reconnaissance investigations of the heretofore little known volcanic assemblage on St. Matthew Island provide significant information on the tectonic history of the Bering Sea shelf. St. Matthew Island is made up of approximately 500 m of subaerial calc-alkaline volcanic rocks ranging in composition from high-alumina basalt to rhyolite. Four K-Ar analyses of samples from this volcanic sequence give Late Cretaceous ages of 65-77 m.y., and intercalated carbonaceous tuff layers yield Cretaceous pollen assemblages. Along the northeast coast of St. Matthew Island the volcanic rocks are intruded by granodiorite that gives an early Tertiary K-Ar age of 61 m.y.</p><p>Correlations with on-land geology in northeast Siberia and marine geophysical data from the western Bering Sea strongly suggest that St. Matthew Island represents a southeastward extension of the Okhotsk-Chukotsk belt, a Late Cretaceous and early Tertiary volcanic arc that borders the Pacific margin of Siberia for 3,000 km. The apparent continuation of this volcanic arc along the margin of the Bering shelf at least as far east as St. Matthew Island supports suggestions by Burk and by Scholl and others that in late Mesozoic time the Pacific plate margin coincided with the present-day Bering shelf margin and did not shift to the Aleutian trench until the end of Cretaceous or the beginning of Tertiary time.</p><p>During the summer of 1971 the U.S. Geological Survey conducted a reconnaissance expedition to St. Matthew Island in the central Bering Sea aboard the Survey research vessel Don J. Miller II. The purpose of the expedition was to obtain basic geologic information on the age and lithologic character of the volcanic rocks on St. Matthew as part of a broad program of onshore and offshore investigations of the energy and mineral resources of the Bering Sea shelf. St. Matthew Island had not been mapped previously and available geologic information was confined to brief notes from early exploratory surveys of the Bering Sea region published more than 50 years ago (Dawson, 1894; Emerson, 1910).</p><p>St. Matthew Island together with two small neighboring islands, Hall and Pinnacle, is situated 400 km west of mainland Alaska on the broad continental shelf that connects Alaska and Siberia (fig. 1). Although these islands have a combined area of only 350<sup>2</sup> km, they are important because they provide a rare subaerial exposure of the geology of the shelf and furnish new information on the tectonic history of the Bering Sea region.</p><p>This report briefly describes the geology of the island and suggests how the island fits into the tectonic framework of the Bering Sea region.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75150","usgsCitation":"Patton, W.W., Lanphere, M.A., Miller, T.P., and Scott, R., 1975, Age and tectonic significance of volcanic rocks on St. Matthew Island, Bering Sea, Alaska: U.S. Geological Survey Open-File Report 75-150, 18 p., https://doi.org/10.3133/ofr75150.","productDescription":"18 p.","costCenters":[],"links":[{"id":423344,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0150/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144105,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0150/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea, St. Matthew Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -173.19656898891907,\n              60.72952223911312\n            ],\n            [\n              -173.19656898891907,\n              60.248433293048976\n            ],\n            [\n              -172.1421533581664,\n              60.248433293048976\n            ],\n            [\n              -172.1421533581664,\n              60.72952223911312\n            ],\n            [\n              -173.19656898891907,\n              60.72952223911312\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6896f3","contributors":{"authors":[{"text":"Patton, William Wallace Jr.","contributorId":72346,"corporation":false,"usgs":true,"family":"Patton","given":"William","suffix":"Jr.","email":"","middleInitial":"Wallace","affiliations":[],"preferred":false,"id":158681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lanphere, Marvin A. alder@usgs.gov","contributorId":2696,"corporation":false,"usgs":true,"family":"Lanphere","given":"Marvin","email":"alder@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":158678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":158679,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scott, Richard A.","contributorId":14414,"corporation":false,"usgs":true,"family":"Scott","given":"Richard A.","affiliations":[],"preferred":false,"id":158680,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":10044,"text":"ofr75565 - 1975 - Data summary of June-July 1975 floods in eastern North Dakota and northwestern Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T14:09:08","indexId":"ofr75565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-565","title":"Data summary of June-July 1975 floods in eastern North Dakota and northwestern Minnesota","docAbstract":"<p>Torrential rains during late June and early July 1975, combined with wet antecedent conditions, caused severe flooding, mainly along the lower reaches of the Sheyenne and Maple Rivers and their tributaries in North Dakota, and in the Buffalo and Wild Rice River basins in Minnesota. The Red River of the North from the Fargo-Moorhead area to the Halstad, Minnesota area was also severely flooded. Because much of the region is extremely flat, large areas of the two States were inundated by flood waters. Damage, mostly agricultural, was widespread and damage estimates exceeded a quarter of a billion dollars.</p>\n<p>Local, State, and Federal officials need factual information to evaluate, coordinate, and manage programs concerned with flood losses. The purpose of this report is to provide quickly a summary of some of the basic data collected on the June-July 1975 floods. Only a part of the information collected by the U.S. Geological Survey on the extent and magnitude of the floods is presented. This information includes the magnitude and frequency of the instantaneous maximum stages (water-surface elevations) and flow rates for 62 sites, measured sediment loads at 7 sites, and hydrographs of daily mean flow at 6 sites. Additional streamflow information associated with the floods will be provided subsequently in annual data releases of the Geological Survey. The report also describes availability of graphic or photographic data depicting the areal extent of inundation. Those data may be obtained from the Applications Assistance Branch, EROS Data Center, U.S. Geological Survey, Sioux Falls, S. Dak. 57198.</p>\n<p>Only a minimal amount of rainfall data are summarized in this report to aid in documenting the flood event. These data were provided by the National Oceanic and Atmospheric Administration (NOAA), U.S. Department of Commerce, and by the Minnesota State Office of Climatology. This assistance in providing the data and in reviewing the form of its presentation is appreciated.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr75565","usgsCitation":"Lindskov, K., 1975, Data summary of June-July 1975 floods in eastern North Dakota and northwestern Minnesota: U.S. Geological Survey Open-File Report 75-565, v, 15 p., https://doi.org/10.3133/ofr75565.","productDescription":"v, 15 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science 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,{"id":4721,"text":"twri01D1 - 1975 - Water temperature-influential factors, field measurement, and data presentation","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"twri01D1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"01-D1","title":"Water temperature-influential factors, field measurement, and data presentation","docAbstract":"This manual contains suggested procedures for collecting and reporting of water-temperature data on streams, lakes and reservoirs, estuaries, and ground water.  Among the topics discussed are the selection of equipment and measuring sites, objectives and accuracy of measurements, and data processing and presentation.  Background information on the influence of temperature on water quality and the factors influencing water temperature are also presented.","language":"ENGLISH","publisher":"U.S. Government Printing Office,","doi":"10.3133/twri01D1","issn":"0565-596X","usgsCitation":"Stevens, H., Ficke, J.F., and Smoot, G.F., 1975, Water temperature-influential factors, field measurement, and data presentation: U.S. Geological Survey Techniques of Water-Resources Investigations 01-D1, vi, 65 p. :ill. ;26 cm. Reprinted in 1978., https://doi.org/10.3133/twri01D1.","productDescription":"vi, 65 p. :ill. ;26 cm. Reprinted in 1978.","costCenters":[],"links":[{"id":139092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":349,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri1-d1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9fdd","contributors":{"authors":[{"text":"Stevens, Herbert H.","contributorId":86752,"corporation":false,"usgs":true,"family":"Stevens","given":"Herbert H.","affiliations":[],"preferred":false,"id":149679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ficke, John F.","contributorId":86750,"corporation":false,"usgs":true,"family":"Ficke","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":149678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smoot, George F.","contributorId":34116,"corporation":false,"usgs":true,"family":"Smoot","given":"George","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":149677,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60577,"text":"mf668C - 1975 - Map showing construction materials in the Fairbanks D-2 NW Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2023-04-10T17:27:58.153971","indexId":"mf668C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"668","chapter":"C","title":"Map showing construction materials in the Fairbanks D-2 NW Quadrangle, Alaska","docAbstract":"<p>This map is based on data presented on the Geologic map of the Fairbanks D-2 quadrangle (Map I-907, Pewe and others, 1975), the Map showing distribution of permafrost in the Fairbanks D-2 quadrangle (Map MF-668A, Pewe and Bell, 1975a), the map showing ground-water conditions in the Fairbanks D-2 quadrangle (Map MF-668B, Pewe and Bell, 1975b), and the Map showing foundation conditions in the Fairbanks D-2 quadrangle (Map MF-668D, Pewe and Bell, 1975c). Additional information, especially detailed subsurface data, can be obtained from these maps.&nbsp;</p><p>This map provides basic information on where construction materials may be obtained near the surface. The map units are defined on the basis of type of material and distribution of permafrost.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf668C","usgsCitation":"Pewe, T., and Bell, J.W., 1975, Map showing construction materials in the Fairbanks D-2 NW Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 668, 1 Plate: 37.99 x 30.92 inches, https://doi.org/10.3133/mf668C.","productDescription":"1 Plate: 37.99 x 30.92 inches","costCenters":[],"links":[{"id":415502,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0668-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182907,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0668-C/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Alaska","otherGeospatial":"Fairbanks D-2 NW Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -148,64.86749999999999 ], [ -148,65 ], [ -147.75,65 ], [ -147.75,64.86749999999999 ], [ -148,64.86749999999999 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d549","contributors":{"authors":[{"text":"Pewe, Troy L.","contributorId":30283,"corporation":false,"usgs":true,"family":"Pewe","given":"Troy L.","affiliations":[],"preferred":false,"id":264018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bell, John W.","contributorId":61411,"corporation":false,"usgs":true,"family":"Bell","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":264019,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60578,"text":"mf669C - 1975 - Map showing construction materials in the Fairbanks D-2 SE Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2023-04-11T22:34:45.391373","indexId":"mf669C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"669","chapter":"C","title":"Map showing construction materials in the Fairbanks D-2 SE Quadrangle, Alaska","docAbstract":"<p>This map is based on data presented on the Geologic map of the Fairbanks D-2 SE quadrangle (Map I-942, Pewe and others, in press), the Map showing distribution of permafrost in the Fairbanks D-2 SE quadrangle (Map MF-669A, Pewe and Bell, 1975a), the map showing ground-water conditions in the Fairbanks D-2 SE quadrangle (Map MF-669B, Pewe and Bell, 1975b), and the Map showing foundation conditions in the Fairbanks D-2 SE quadrangle (Map MF-669D, Pewe and Bell, 1975c). Additional information, especially detailed subsurface data, can be obtained from these maps.&nbsp;</p><p>This map provides basic information on where construction materials may be obtained near the surface. The map units are defined on the basis of type of material and distribution of permafrost.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf669C","usgsCitation":"Pewe, T., and Bell, J.W., 1975, Map showing construction materials in the Fairbanks D-2 SE Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 669, 1 Plate: 39.94 x 30.94 inches, https://doi.org/10.3133/mf669C.","productDescription":"1 Plate: 39.94 x 30.94 inches","costCenters":[],"links":[{"id":415618,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0669-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182999,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0669-C/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Alaska","otherGeospatial":"Fairbanks D-2 SE Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -147.75,64.75 ], [ -147.75,64.86749999999999 ], [ -147.5,64.86749999999999 ], [ -147.5,64.75 ], [ -147.75,64.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d582","contributors":{"authors":[{"text":"Pewe, Troy L.","contributorId":30283,"corporation":false,"usgs":true,"family":"Pewe","given":"Troy L.","affiliations":[],"preferred":false,"id":264020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bell, John W.","contributorId":61411,"corporation":false,"usgs":true,"family":"Bell","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":264021,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56694,"text":"wdrTX741 - 1975 - Water resources data for Texas, water year 1974; Part 1, surface water records","interactions":[],"lastModifiedDate":"2020-02-04T13:33:42","indexId":"wdrTX741","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"TX-74-1","title":"Water resources data for Texas, water year 1974; Part 1, surface water records","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrTX741","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Water resources data for Texas, water year 1974; Part 1, surface water records: U.S. Geological Survey Water Data Report TX-74-1, xviii, 609 p., 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,{"id":60587,"text":"mf671B - 1975 - Map showing ground water conditions in the Fairbanks D-1 SW quadrangle, Alaska","interactions":[],"lastModifiedDate":"2023-04-11T22:42:23.303556","indexId":"mf671B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"671","chapter":"B","title":"Map showing ground water conditions in the Fairbanks D-1 SW quadrangle, Alaska","docAbstract":"<p>The primary controlling factors determining ground-water conditions in the Fairbanks D-1 SW quadrangle are (1) topographic position, (2) water-bearing characteristics of the rocks, and (3) distribution of permafrost. These interrelated factors generally limit the conditions in any particular area.&nbsp;</p><p>Basic data from the geologic map of the Fairbanks D-1 SW quadrangle (Map I-949, Pewe and others, in press), the map showing distribution of permafrost in the Fairbanks D-1 SW quadrangle (Map MF-671A, Pewe and Bell, 1975a), and the map showing foundation conditions in the Fairbanks D-1 SW quadrangle (Map MF 671D, Pewe and Bell, 1975c) have been used in conjunction with well data to establish generalized potential ground-water conditions.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf671B","usgsCitation":"Pewe, T., and Bell, J.W., 1975, Map showing ground water conditions in the Fairbanks D-1 SW quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 671, 1 Plate: 38.05 x 31.12 inches, https://doi.org/10.3133/mf671B.","productDescription":"1 Plate: 38.05 x 31.12 inches","costCenters":[],"links":[{"id":415622,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0671-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180537,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0671-B/report-thumb.jpg"},{"id":391112,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3805.htm","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Alaska","otherGeospatial":"Fairbanks D-1 SW quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147.25,\n              64.75\n            ],\n            [\n              -147.5,\n              64.75\n            ],\n            [\n              -147.5,\n              64.875\n            ],\n            [\n              -147.25,\n              64.875\n            ],\n            [\n              -147.25,\n              64.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656d01","contributors":{"authors":[{"text":"Pewe, Troy L.","contributorId":30283,"corporation":false,"usgs":true,"family":"Pewe","given":"Troy L.","affiliations":[],"preferred":false,"id":264038,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bell, John W.","contributorId":61411,"corporation":false,"usgs":true,"family":"Bell","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":264039,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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