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,{"id":67028,"text":"i786E - 1972 - Map showing approximate locations, depths, and estimated yields of water wells in the Evergreen Quadrangle, Jefferson County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:18","indexId":"i786E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"786","subseriesTitle":"NONE","chapter":"E","title":"Map showing approximate locations, depths, and estimated yields of water wells in the Evergreen Quadrangle, Jefferson County, Colorado","language":"ENGLISH","doi":"10.3133/i786E","usgsCitation":"Schmidt, P.W., and Reed, J.C., 1972, Map showing approximate locations, depths, and estimated yields of water wells in the Evergreen Quadrangle, Jefferson County, Colorado: U.S. Geological Survey IMAP 786, 1 map :col. ;58 x 45 cm. on sheet 73 x 100 cm. folded to 26 x 20 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/i786E.","productDescription":"1 map :col. ;58 x 45 cm. on sheet 73 x 100 cm. folded to 26 x 20 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":256408,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0786e/plate-1.pdf","size":"6675","linkFileType":{"id":1,"text":"pdf"}},{"id":256409,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0786e/report.pdf","size":"39","linkFileType":{"id":1,"text":"pdf"}},{"id":256410,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0786e/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.36749999999999,39.6175 ], [ -105.36749999999999,39.75 ], [ -105.25,39.75 ], [ -105.25,39.6175 ], [ -105.36749999999999,39.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db659316","contributors":{"authors":[{"text":"Schmidt, P. W.","contributorId":28303,"corporation":false,"usgs":true,"family":"Schmidt","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":275476,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, J. C. Jr.","contributorId":97063,"corporation":false,"usgs":true,"family":"Reed","given":"J.","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":275477,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":1120,"text":"wsp2021 - 1972 - Evaluation of yields of wells in consolidated rocks, Virginia to Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp2021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"2021","title":"Evaluation of yields of wells in consolidated rocks, Virginia to Maine","docAbstract":"In the North Atlantic region, Virginia to Maine, yields of industrial and municipal wells are the most reliable indicators of the water-yielding potential of consolidated rocks. Generally, such wells represent efforts to develop a maximum supply of water, they are 350 to 500 feet deep, and they utilize 60 to 150 feet of drawdown. In multiple-well developments, average yields of wells per 100 feet of drawdown range from less than 75 gallons per minute in the least favorable rocks such as shale or granite gneiss to as much as 300 gallons per minute in limestone. In any one rock type, substantially greater than average sustained yields are possible in structurally deformed areas or in areas where recharge potential is especially favorable.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2021","usgsCitation":"Cederstrom, D.J., 1972, Evaluation of yields of wells in consolidated rocks, Virginia to Maine: U.S. Geological Survey Water Supply Paper 2021, iv, 38 p. :2 fold. illus. (in pocket) ;24 cm., https://doi.org/10.3133/wsp2021.","productDescription":"iv, 38 p. :2 fold. illus. (in pocket) ;24 cm.","costCenters":[],"links":[{"id":138012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2021/report-thumb.jpg"},{"id":25883,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2021/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25884,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2021/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25885,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9d4e","contributors":{"authors":[{"text":"Cederstrom, Dagfin John","contributorId":90287,"corporation":false,"usgs":true,"family":"Cederstrom","given":"Dagfin","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":143209,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56708,"text":"wdrNM712 - 1972 - Water resources data for New Mexico, water year 1971; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2020-12-07T19:54:13.837704","indexId":"wdrNM712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"NM-71-2","title":"Water resources data for New Mexico, water year 1971; Part 2, Water quality records","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNM712","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for New Mexico, water year 1971; Part 2, Water quality records: U.S. Geological Survey Water Data Report 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,{"id":2764,"text":"wsp1873F - 1972 - Determination of mass balance and entrainment in the stratified Duwamish River Estuary, King County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1873F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1873","chapter":"F","title":"Determination of mass balance and entrainment in the stratified Duwamish River Estuary, King County, Washington","docAbstract":"During a study of the effects of waste-water input on the stratified Duwamish River estuary, intensive water-velocity and salinity measurements were made in both the lower salt wedge and the upper fresher water layer for tidal-cycle periods. The net movement of water and salt mass past a cross section during a tidal cycle was determined from integration of the measured rates of movement of water and salt past the section. The net volume of water that moved downstream past the section during the cycle agreed with the volume of fresh-water inflow at the head of the estuary within (1) 3.8 and 7.2 percent, respectively, for two studies made during periods of maximum and minimum tidal-prism thickness and identical inflow rates .of 312 cfs (cubic feet per second), and (2) 15 percent for one study made during a period of average tidal-prism thickness and an inflow rate of 1,280 cfs. For the three studies, the difference between salt mass transported upstream and downstream during the cycles ranged from 0.8 to 19 percent of the respective mean salt-mass transport. Water was entrained from the .salt-water wedge into the overlying layer of mixed fresh and salt water at tidal-cycle-average rates of 30 and 69 cfs per million square feet of interface for the inflow rates of 312 cfs, and 99 cfs per million square feet of interface for an inflow rate of 1,280 cfs. At a constant inflow rate, the rate of entrainment of salt-wedge water in the Duwamish River estuary more than doubled for a doubling of tidal-prism thickness. It also doubled for a quadrupling of inflow rate at about constant tidal-prism thickness.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1873F","usgsCitation":"Stoner, J., 1972, Determination of mass balance and entrainment in the stratified Duwamish River Estuary, King County, Washington: U.S. Geological Survey Water Supply Paper 1873, iii, 17 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1873F.","productDescription":"iii, 17 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":138598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1873f/report-thumb.jpg"},{"id":29199,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1873f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6677b3","contributors":{"authors":[{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":145743,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43020,"text":"ofr7250 - 1972 - Simple Bouguer gravity map of Connecticut","interactions":[],"lastModifiedDate":"2025-07-31T16:40:55.265502","indexId":"ofr7250","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"72-50","title":"Simple Bouguer gravity map of Connecticut","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7250","usgsCitation":"Bromery, R.W., Davis, M., and Ahmad, F., 1972, Simple Bouguer gravity map of Connecticut: U.S. Geological Survey Open-File Report 72-50, 1 Plate: 58.00 x 42.00 inches, https://doi.org/10.3133/ofr7250.","productDescription":"1 Plate: 58.00 x 42.00 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,{"id":13103,"text":"ofr7271 - 1972 - Placer deposits of Alaska","interactions":[{"subject":{"id":13103,"text":"ofr7271 - 1972 - Placer deposits of Alaska","indexId":"ofr7271","publicationYear":"1972","noYear":false,"title":"Placer deposits of Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":34073,"text":"b1374 - 1973 - Placer deposits of Alaska","indexId":"b1374","publicationYear":"1973","noYear":false,"title":"Placer deposits of Alaska"},"id":1}],"supersededBy":{"id":34073,"text":"b1374 - 1973 - Placer deposits of Alaska","indexId":"b1374","publicationYear":"1973","noYear":false,"title":"Placer deposits of Alaska"},"lastModifiedDate":"2024-03-15T20:50:23.380388","indexId":"ofr7271","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"72-71","title":"Placer deposits of Alaska","docAbstract":"<p>Placer deposits, in addition to their intrinsic value, serve as indicators of areas of potential development of lode deposits. Any possibility that Alaska may again become an important source of metallic mineral commodities depends in part on an inventory of placer deposits and a knowledge of the geology of their source areas.</p><p>Information on Alaska's placer deposits is far from complete. Many mining camps have been at best the subject of only cursory examination by geologists or mining engineers at liberty to publish the results of their studies. Many placers are vaguely known from unconfirmed reports that someone was working on a creek, in many instances a creek bearing a name that cannot now be identified with any particular stream. Such data are, of course, practically valueless and were generally ignored in preparing the report. Other major gaps in our knowledge result from the lack of bedrock exposures in many areas where valuable placer deposits were mined, a circumstance that made impossible the determination of lode sources and their mode of occurrence during reconnaissance studies of mining districts. And the reluctance of many prospectors to divulge data on their claims has undoubtedly caused some deposits to be \"lost\" or overlooked.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7271","usgsCitation":"Cobb, E.H., 1972, Placer deposits of Alaska: U.S. Geological Survey Open-File Report 72-71, Report: iii, 132 p.; 1 Plate: 15.83 x 35.32 inches, https://doi.org/10.3133/ofr7271.","productDescription":"Report: iii, 132 p.; 1 Plate: 15.83 x 35.32 inches","costCenters":[],"links":[{"id":426714,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0071/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144533,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0071/report-thumb.jpg"},{"id":426712,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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Edward Huntington","contributorId":25916,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward","email":"","middleInitial":"Huntington","affiliations":[],"preferred":false,"id":167245,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1946,"text":"wsp1873E - 1972 - Movement and dispersion of soluble pollutants in the Northeast Cape Fear Estuary, North Carolina","interactions":[{"subject":{"id":55881,"text":"ofr68327 - 1968 - Interim report on sea-water encroachment into the Cape Fear River Estuary, North Carolina","indexId":"ofr68327","publicationYear":"1968","noYear":false,"title":"Interim report on sea-water encroachment into the Cape Fear River Estuary, North Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":1946,"text":"wsp1873E - 1972 - Movement and dispersion of soluble pollutants in the Northeast Cape Fear Estuary, North Carolina","indexId":"wsp1873E","publicationYear":"1972","noYear":false,"chapter":"E","title":"Movement and dispersion of soluble pollutants in the Northeast Cape Fear Estuary, North Carolina"},"id":1}],"lastModifiedDate":"2019-12-30T10:14:20","indexId":"wsp1873E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1873","chapter":"E","title":"Movement and dispersion of soluble pollutants in the Northeast Cape Fear Estuary, North Carolina","docAbstract":"This report presents the results of a fluorescent-dye-tracing study to determine the concentrations of a pollutant that would be present in the Northeast Cape Fear Estuary at various rates of continuous waste injection and freshwater inflow. Rhodamine WT dye was introduced into the estuary at a constant rate over a 24.8-hour period (two tidal cycles) at a point 6.4 miles upstream from the mouth in Wilmington, N.C., and concentrations were monitored at several selected sections in the tide-affected part of the river for 17 days. The range between high and low tide in this reach of the estuary averages at-rut 3.5 feet, and there is usually strong flow in both directions. \r\n\r\nResults of the dye study indicate that if a pollutant were injected at a rate of 100 pounds per day under the conditions of relatively low inflow existing' at the time, concentrations would ultimately build up to 20 micrograms of dye per liter of water 1,000 feet downstream. The flushing time during the study is estimated to be 17 days. These results are extrapolated to include periods of lower or higher inflow. For example, at average intervals of 10 years, it is estimated that inflow is so low that 100 days are required for a pollutant to travel the 6.4 miles from the point of waste release to the mouth of the river. Under these conditions it is expected that 1,000 feet downstream from the point of waste discharge, daily maximum concentrations will average about 130 micrograms per liter for each 100 pounds of pollutant injected per day. \r\n\r\nResults of a continuous discharge measurement of flow made by current meter during a complete tidal cycle are presented as a part of this report. Data from this measurement and other evidence indicate that net upstream flow in the estuary is possible over a period of several days.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1873E","usgsCitation":"Hubbard, E., and Stamper, W.G., 1972, Movement and dispersion of soluble pollutants in the Northeast Cape Fear Estuary, North Carolina: U.S. Geological Survey Water Supply Paper 1873, v, 31 p. , https://doi.org/10.3133/wsp1873E.","productDescription":"v, 31 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":138417,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1873e/report-thumb.jpg"},{"id":27277,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1873e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Cape Fear Estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.3599853515625,\n              33.77458136371689\n            ],\n            [\n              -77.7227783203125,\n              33.77458136371689\n            ],\n            [\n              -77.7227783203125,\n              34.5020297944346\n            ],\n            [\n              -78.3599853515625,\n              34.5020297944346\n            ],\n            [\n              -78.3599853515625,\n              33.77458136371689\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b47ea","contributors":{"authors":[{"text":"Hubbard, E. F.","contributorId":66666,"corporation":false,"usgs":true,"family":"Hubbard","given":"E. F.","affiliations":[],"preferred":false,"id":144416,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stamper, William G.","contributorId":58259,"corporation":false,"usgs":true,"family":"Stamper","given":"William","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144415,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2791,"text":"wsp1999A - 1972 - Geohydrology of the lower Verdigris River valley between Muskogee and Catoosa, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1999A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1999","chapter":"A","title":"Geohydrology of the lower Verdigris River valley between Muskogee and Catoosa, Oklahoma","docAbstract":"Alluvium is the principal aquifer along the Verdigris River between Muskogee and Catoosa, Okla. Yields of 1 to 10 gallons of water per minute, adequate for most domestic and stock uses, are available in almost all areas underlain by alluvium. In places where the proportion of gravel to fine material is high, yields ranging from 10 to 30 gallons per minute are possible from large-diameter wells. Terrace deposits yield small amounts of water (1 to 10 gallons per minute), adequate for most domestic and stock uses. \r\n\r\nWater-level fluctuations, in response to seasonal changes in recharge and discharge, range from 1 to 5 feet. Long-term fluctuations, measured as changes in seasonal high or low water levels during 8 years of record, are about 10 feet in the alluvium and less than 5 feet in the terrace deposits. \r\n\r\nRecharge to the alluvium is mainly by precipitation. Recharge maintains groundwater levels above the level of the Verdigris River, which, in turn, is the natural drain of the aquifer. Discharge from the alluvium is by seepage into the river and its tributaries and by evapotranspiration. \r\n\r\nGenerally, the quality of the water in the alluvium and terrace deposits is suitable for domestic, stock, and irrigation uses.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1999A","usgsCitation":"Tanaka, H., 1972, Geohydrology of the lower Verdigris River valley between Muskogee and Catoosa, Oklahoma: U.S. Geological Survey Water Supply Paper 1999, iii, 23 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1999A.","productDescription":"iii, 23 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":138869,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1999a/report-thumb.jpg"},{"id":29275,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29276,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29277,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1999a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8838","contributors":{"authors":[{"text":"Tanaka, H.H.","contributorId":30610,"corporation":false,"usgs":true,"family":"Tanaka","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":145796,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42221,"text":"ofr7231 - 1972 - Bouguer gravity map of Colorado","interactions":[{"subject":{"id":42221,"text":"ofr7231 - 1972 - Bouguer gravity map of Colorado","indexId":"ofr7231","publicationYear":"1972","noYear":false,"title":"Bouguer gravity map of Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":64195,"text":"gp895 - 1974 - Bouguer gravity map of Colorado","indexId":"gp895","publicationYear":"1974","noYear":false,"title":"Bouguer gravity map of Colorado"},"id":1}],"supersededBy":{"id":64195,"text":"gp895 - 1974 - Bouguer gravity map of Colorado","indexId":"gp895","publicationYear":"1974","noYear":false,"title":"Bouguer gravity map of Colorado"},"lastModifiedDate":"2022-03-30T16:45:00.152672","indexId":"ofr7231","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"72-31","title":"Bouguer gravity map of Colorado","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7231","collaboration":"Prepared in cooperation with the Colorado Mining Industrial Development Board and the Colorado Geological Survey","usgsCitation":"Behrendt, J.C., and Bajwa, L.Y., 1972, Bouguer gravity map of Colorado: U.S. Geological Survey Open-File Report 72-31, 1 Plate: 63.80 x 42.11 inches, https://doi.org/10.3133/ofr7231.","productDescription":"1 Plate: 63.80 x 42.11 inches","costCenters":[],"links":[{"id":168558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United 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,{"id":56707,"text":"wdrNM711 - 1972 - Water resources data for New Mexico, water year 1971; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2013-07-08T13:23:28","indexId":"wdrNM711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"NM-71-1","title":"Water resources data for New Mexico, water year 1971; Part 1, Surface water records","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNM711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for New Mexico, water year 1971; Part 1, Surface water records: U.S. Geological Survey Water Data Report NM-71-1, 468 p., https://doi.org/10.3133/wdrNM711.","productDescription":"468 p.","costCenters":[{"id":627,"text":"Water Resources Data for New Mexico","active":false,"usgs":true}],"links":[{"id":180764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":270284,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/nm-71-1/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0502,31.3322 ], [ -109.0502,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.0502,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2742","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":532823,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":62458,"text":"gq1000 - 1972 - Geologic map of the Upton quadrangle, central Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:43","indexId":"gq1000","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1000","title":"Geologic map of the Upton quadrangle, central Kentucky","language":"ENGLISH","doi":"10.3133/gq1000","usgsCitation":"Moore, F.R., 1972, Geologic map of the Upton quadrangle, central Kentucky: U.S. Geological Survey Geologic Quadrangle 1000, 1 map., https://doi.org/10.3133/gq1000.","productDescription":"1 map.","costCenters":[],"links":[{"id":103236,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1822.htm","linkFileType":{"id":5,"text":"html"},"description":"1822"},{"id":248624,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1000/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":253851,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1000/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86,37.3675 ], [ -86,37.5 ], [ -85.86749999999999,37.5 ], [ -85.86749999999999,37.3675 ], [ -86,37.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a238","contributors":{"authors":[{"text":"Moore, Frank R.","contributorId":54582,"corporation":false,"usgs":false,"family":"Moore","given":"Frank","email":"","middleInitial":"R.","affiliations":[{"id":12981,"text":"Department of Biological Sciences, University of Southern Mississippi","active":true,"usgs":false}],"preferred":false,"id":267402,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63024,"text":"gq1004 - 1972 - Geologic map of the Ruedi quadrangle, Pitkin and Eagle Counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq1004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1004","title":"Geologic map of the Ruedi quadrangle, Pitkin and Eagle Counties, Colorado","language":"ENGLISH","doi":"10.3133/gq1004","usgsCitation":"Freeman, V.L., 1972, Geologic map of the Ruedi quadrangle, Pitkin and Eagle Counties, Colorado: U.S. Geological Survey Geologic Quadrangle 1004, 1 map :col. ;58 x 45 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1004.","productDescription":"1 map :col. ;58 x 45 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107451,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10552.htm","linkFileType":{"id":5,"text":"html"},"description":"10552"},{"id":249157,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1004/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":252158,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1004/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.86749999999999,39.25 ], [ -106.86749999999999,39.3675 ], [ -106.75,39.3675 ], [ -106.75,39.25 ], [ -106.86749999999999,39.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68c090","contributors":{"authors":[{"text":"Freeman, Val L.","contributorId":40570,"corporation":false,"usgs":true,"family":"Freeman","given":"Val","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":268213,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15001,"text":"ofr72256 - 1972 - Preliminary geologic map of the eastern Solomon and southeastern Bendeleben quadrangles, eastern Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2022-03-24T22:16:50.505652","indexId":"ofr72256","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"72-256","title":"Preliminary geologic map of the eastern Solomon and southeastern Bendeleben quadrangles, eastern Seward Peninsula, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72256","usgsCitation":"Miller, T.P., Grybeck, D., Elliott, R.L., and Hudson, T., 1972, Preliminary geologic map of the eastern Solomon and southeastern Bendeleben quadrangles, eastern Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 72-256, Report: 11 p.; 2 Plates: 14.36 × 29.40 inches and 23.19 × 14.54 inches, https://doi.org/10.3133/ofr72256.","productDescription":"Report: 11 p.; 2 Plates: 14.36 × 29.40 inches and 23.19 × 14.54 inches","costCenters":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"links":[{"id":148954,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0256/report-thumb.jpg"},{"id":397588,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8692.htm"},{"id":43829,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0256/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43830,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0256/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43831,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0256/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"eastern Solomon and southeastern Bendeleben quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -163.5,\n              64.25\n            ],\n            [\n              -162,\n              64.25\n            ],\n            [\n              -162,\n              65.5\n            ],\n            [\n              -163.5,\n              65.5\n            ],\n            [\n              -163.5,\n              64.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674324","contributors":{"authors":[{"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":170392,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grybeck, Donald","contributorId":8066,"corporation":false,"usgs":true,"family":"Grybeck","given":"Donald","affiliations":[],"preferred":false,"id":170393,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Elliott, Raymond L.","contributorId":82667,"corporation":false,"usgs":true,"family":"Elliott","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":170394,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hudson, Travis","contributorId":90282,"corporation":false,"usgs":true,"family":"Hudson","given":"Travis","affiliations":[],"preferred":false,"id":170395,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":62976,"text":"gq1040 - 1972 - Geologic map of the Morgantown quadrangle, Butler and Warren Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:44","indexId":"gq1040","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1040","title":"Geologic map of the Morgantown quadrangle, Butler and Warren Counties, Kentucky","language":"ENGLISH","doi":"10.3133/gq1040","usgsCitation":"Gildersleeve, B., 1972, Geologic map of the Morgantown quadrangle, Butler and Warren Counties, Kentucky: U.S. Geological Survey Geologic Quadrangle 1040, 1 map., https://doi.org/10.3133/gq1040.","productDescription":"1 map.","costCenters":[],"links":[{"id":107484,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10585.htm","linkFileType":{"id":5,"text":"html"},"description":"10585"},{"id":249114,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1040/report.pdf","size":"38","linkFileType":{"id":1,"text":"pdf"}},{"id":252115,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1040/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.75,37.1175 ], [ -86.75,37.25 ], [ -86.61749999999999,37.25 ], [ -86.61749999999999,37.1175 ], [ -86.75,37.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6967b0","contributors":{"authors":[{"text":"Gildersleeve, Benjamin","contributorId":14468,"corporation":false,"usgs":true,"family":"Gildersleeve","given":"Benjamin","email":"","affiliations":[],"preferred":false,"id":268125,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32489,"text":"wrr1 - 1972 - An analysis of the population dynamics of selected avian species, with special reference to changes during the modern pesticide era","interactions":[],"lastModifiedDate":"2012-02-02T00:09:09","indexId":"wrr1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":99,"text":"Wildlife Research Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"1","title":"An analysis of the population dynamics of selected avian species, with special reference to changes during the modern pesticide era","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Henny, C.J., 1972, An analysis of the population dynamics of selected avian species, with special reference to changes during the modern pesticide era: Wildlife Research Report 1, 99 p. illus. ; 26 cm.","productDescription":"99 p. illus. ; 26 cm.","costCenters":[],"links":[{"id":160648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68582d","contributors":{"authors":[{"text":"Henny, Charles J. 0000-0001-7474-350X hennyc@usgs.gov","orcid":"https://orcid.org/0000-0001-7474-350X","contributorId":3461,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"hennyc@usgs.gov","middleInitial":"J.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":208592,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59231,"text":"mf437 - 1972 - Metallic mineral resources map of the Prince Rupert quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:10:16","indexId":"mf437","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"437","title":"Metallic mineral resources map of the Prince Rupert quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/mf437","usgsCitation":"Cobb, E.H., 1972, Metallic mineral resources map of the Prince Rupert quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 437, map ;60 x 61 cm. fold. in envelope 25 x 31 cm., https://doi.org/10.3133/mf437.","productDescription":"map ;60 x 61 cm. fold. in envelope 25 x 31 cm.","costCenters":[],"links":[{"id":111315,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/13215","linkFileType":{"id":5,"text":"html"}},{"id":185225,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -132,54 ], [ -132,55 ], [ -130,55 ], [ -130,54 ], [ -132,54 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db628479","contributors":{"authors":[{"text":"Cobb, Edward Huntington","contributorId":25916,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward","email":"","middleInitial":"Huntington","affiliations":[],"preferred":false,"id":261626,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60442,"text":"mf321 - 1972 - Preliminary photointerpretation map of landslide and other surficial deposits of parts of the Altamont and Carbona 15-minute quadrangles, Alameda County, California","interactions":[],"lastModifiedDate":"2013-01-24T09:54:40","indexId":"mf321","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"321","title":"Preliminary photointerpretation map of landslide and other surficial deposits of parts of the Altamont and Carbona 15-minute quadrangles, Alameda County, California","language":"ENGLISH","doi":"10.3133/mf321","usgsCitation":"Nilsen, T.H., 1972, Preliminary photointerpretation map of landslide and other surficial deposits of parts of the Altamont and Carbona 15-minute quadrangles, Alameda County, California: U.S. Geological Survey Miscellaneous Field Studies Map 321, 1 map., https://doi.org/10.3133/mf321.","productDescription":"1 map.","costCenters":[],"links":[{"id":180595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":266373,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0321/plate-1.pdf"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.75,37.5 ], [ -121.75,37.75 ], [ -121.5,37.75 ], [ -121.5,37.5 ], [ -121.75,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cd12","contributors":{"authors":[{"text":"Nilsen, T. H.","contributorId":93057,"corporation":false,"usgs":true,"family":"Nilsen","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":263759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61950,"text":"gq984 - 1972 - Surficial geologic map of the Thomaston quadrangle, Litchfield, New Haven, and Hartford Counties, Connecticut","interactions":[],"lastModifiedDate":"2012-02-10T00:10:49","indexId":"gq984","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"984","title":"Surficial geologic map of the Thomaston quadrangle, Litchfield, New Haven, and Hartford Counties, Connecticut","language":"ENGLISH","doi":"10.3133/gq984","usgsCitation":"Warren, C.R., 1972, Surficial geologic map of the Thomaston quadrangle, Litchfield, New Haven, and Hartford Counties, Connecticut: U.S. Geological Survey Geologic Quadrangle 984, 1 map., https://doi.org/10.3133/gq984.","productDescription":"1 map.","costCenters":[],"links":[{"id":103697,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2283.htm","linkFileType":{"id":5,"text":"html"},"description":"2283"},{"id":248235,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0984/report.pdf","size":"38","linkFileType":{"id":1,"text":"pdf"}},{"id":253061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0984/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.11749999999999,41.6175 ], [ -73.11749999999999,41.75 ], [ -73,41.75 ], [ -73,41.6175 ], [ -73.11749999999999,41.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb487","contributors":{"authors":[{"text":"Warren, Charles Reynolds","contributorId":46964,"corporation":false,"usgs":true,"family":"Warren","given":"Charles","email":"","middleInitial":"Reynolds","affiliations":[],"preferred":false,"id":266597,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16672,"text":"ofr72454 - 1972 - Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards","interactions":[],"lastModifiedDate":"2024-03-27T17:56:09.862376","indexId":"ofr72454","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"72-454","title":"Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards","docAbstract":"<p>A program to study the engineering geology of most of the larger Alaska coastal communities and to evaluate their earthquake and other geologic hazards was started promptly after the 1964 Alaska earthquake; this report is a product of that program. Field-study methods were largely reconnaissance, and thus the interpretations in the report are subject to revision as further information becomes available. The report provides broad guidelines for planners and engineers when considering geologic factors during preparation of land-use plans. The use of this information should lead to minimizing future loss of life and property, especially during major earthquakes.</p><p>Skagway was established in 1897 as a seaport near the head of Taiya Inlet fiord in the northern part of southeastern Alaska. Rugged mountains, steep-walled valleys, fiords, and numerous glaciers and icefields characterize the landscape of the area. Valley floors are narrow and most carry large streams, which end in tidewater deltas. Skagway is situated on the delta and lower valley floor of the Skagway River.</p><p>Glaciers became vastly enlarged during the Pleistocene Epoch and presumably covered the area at least several times. The last major deglaciation probably occurred about 10,000 years ago. Subsequently, there was minor expansion and then partial retreat of glaciers; land rebound because of glacial melting is still going on today.</p><p>Bedrock is composed predominantly of plutonic intrusive rocks, chiefly quartz diorite and granodiorite, some metamorphic rocks and a few dikes are present. Most bedrock is of Jurassic and Cretaceous age.</p><p>An assortment of surficial deposits of Quaternary age form the valley bottoms and locally part of the valley walls. Thick deposits of sand and gravel have accumulated as deltas at the heads of fiords and as alluvium in the main stream valleys; deposits may be as much as S8S feet thick at Skagway. Locally, thin deposits mantle some of the steep bedrock slopes and also form some moderately to gently sloping ground. Manmade fill covers much of the top of the delta and floor of the Skagway valley. The fill is composed chiefly of gravel and sand. Quarried blocks of granodiorite are used as riprap to face river dikes and on fill areas exposed to waves of Taiya Inlet.</p><p>The geologic structure of the area is imperfectly known. However, it appears that plutonic rocks intruded metamorphic rocks in Jurassic and Cretaceous time. Extensive faulting is strongly indicated by the strikingly linear or curvilinear pattern of fiords and many large and small valleys, but no major faults have been positively identified because of concealment by water or surficial deposits. Inferred faults include those coincident with the lower Skagway valley, Taiya Inlet-Taiya valley, and the Katzehin River delta-Upper Dewey Lake. Principal fault movements probably occurred in middle Tertiary time but some movement might have been in late Tertiary or possibly early Quaternary time. Local faults appear to join the Chilkat River fault, a segment of the important Denali fault system, one of the major tectonic elements of southeastern Alaska. One fault segment of this system shows evidence of movement within the last several hundred years. Southeastern Alaska's other major fault system is the active Fairweather-Queen Charlotte Islands fault system'near the coast of the Pacific Ocean. This fault system passes to within about 100 miles of Skagway. At its northwest end the fault system merges with the Chugach-St. Elias fault.</p><p>One hundred twenty-two earthquakes, some of them strong, have been felt or possibly felt at Skagway during the years 1898 through 1969. The closest large earthquake (magnitude about 8) causing some damage at Skagway occurred July 10, 1958. Its epicenter was about 100 miles to the southwest. Other earthquakes, as much as 150 miles away, also have caused slight to moderate damage. The closest instrumentally recorded earthquake (magnitude 6) had its epicenter about 30 miles to the west of Skagway.</p><p>Most earthquakes in southeastern Alaska have occurred southwest, west, or northwest of Skagway, near the coast of the Pacific Ocean. They appear to be related to movement along the Fairweather-Queen Charlotte Islands fault system or the Chugach-St. Elias fault. Most have had their epicenters offshore. Some earthquakes may be related to movement at depth along the Denali fault system.</p><p>The probability of destructive earthquakes at Skagway is unknown because the tectonics of the region have not been studied in detail. However, on the basis of the seismic record and limited tectonic evidence, we suggest that sometime in the future an earthquake of at least magnitude 6 probably will occur very close to the city, a magnitude 7 earthquake might occur in the general area, and an earthquake of magnitude 8 probably will occur at some distance to the southwest, west, or northwest.</p><p>Effects from nearby large earthquakes could cause extensive damage at Skagway. Nine principal effects are considered.</p><p>1. Surface&nbsp;displacement. Displacement of ground caused by fault movement would affect only structures built athwart the fault. However, a sudden tectonic uplift of land of as much as a few feet might affect a wide area and necessitate extensive dredging and wharf rebuilding. On the other hand, a subsidence of several feet would allow tidewater to reach inland and flood part of the harbor facilities and the business district.</p><p>2. Ground shaking. Because intensity of ground shaking during earthquakes largely depends on type and water content of the geologic material being shaken, the geologic materials are separated into three categories. Those considered susceptible to strongest shaking are grouped into category 1 (containing materials that are saturated, loose, and of medium- to fine-grain sizes); those of intermediate susceptibility in category 2; and those least susceptible to shaking in category 3.</p><p>3. Compaction of some medium-grained sediments during strong earthquake shaking could cause local settling of alluvial and deltaic surfaces. Also, some manmade fills near the harbor might undergo marked differential settling.</p><p>4. Liquefaction of saturated beds of uniform, fine sand commonly occurs during strong earthquakes. Few such beds, however, are positively identified at Skagway; some may occur within deltaic and alluvial deposits. If present, these beds might liquefy and cause local settling or trigger landslides.</p><p>5. Ejection of water-sediment mixtures from earthquake-induced fractures or from point sources, plus some associated ground subsidence, is common during major earthquakes where saturated sand and fine gravel deposits are confined beneath generally impermeable beds. Some alluvial and deltaic deposits at Skagway probably are susceptible to these processes. Locally, ejecta might cover roads and areas between buildings and fill low-lying areas. Associated ground fracturing might damage roadways, foundations of buildings, and other facilities.</p><p>6. Subaerial and subaqueous slides occur frequently during earthquakes. Saturated loose sediments on steep slopes are especially susceptible to sliding. During a major earthquake, surficial deposits forming such slopes along the southeast side of the Skagway valley probably would be subject to sliding or earthflowing on an extensive scale. Some sliding might extend onto the valley floor and damage or destroy buildings and part of the railroad. Rockfalls would be numerous and locally very large rockslides might occur.</p><p>Subaqueous sliding of the Skagway delta is potentially the most damaging of earthquake effects. Sliding may have occurred there during the earthquake of September 16, 1899; any future major earthquake close to the city would cause extensive sliding, possibly triggered in part by liquefaction. If shaking continued for several minutes, successive slides might progressively remove large portions of the delta and allow extensive land spreading and fracturing of Skagway River alluvium as much as several thousand feet landward from the shoreline.</p><p>7. Glacier surfaces commonly receive extensive snow avalanches and rockslides during seismic shaking. In the Skagway area, glaciers may be disrupted at their margins, and resulting blocked streams might form lakes in a few places. If these lakes drained suddenly, downstream areas would he flooded. No long-term effects, such as glacier expansion, are expected.</p><p>8. Ground- and surface-water levels often are affected during and after strong earthquake shaking. At Skagway, ground-water levels probably would be lowered, but there would be no permanent change in water quality. Earthquake-triggered landslides could dam the Skagway River; the sudden failure of the dams might cause severe flooding.</p><p>9. Waves generated by earthquakes include tsunamis, seiche waves, and waves caused by subaerial and submarine sliding and tectonic displacement of land. Damage in the Skagway area would depend on wave height, tidal stage, and warning time. Some waves triggered by subaerial and subaqueous slides have a strong possibility of reaching heights of as much as 60 feet--or possibly even higher. Tsunamis from the open ocean must travel 160 miles of fiords before reaching Skagway, which allows sufficient time for appraisal of expectable wave height and, if necessary, evacuation of the harbor area and other low-lying ground.</p><p>Geologic hazards other than those hazards associated with earthquakes include nonearthquake-induced subaerial and subaqueous slides, floods, and slow uplift (rebound) of land. Landslides of moderate size are known to have occurred from time to time during heavy rains such as those of September 1967. Subaqueous slides happen intermittently during the normal growth of deltas. Submarine cables on the floor of northern Taiya Inlet presumably were broken by such slides on September 10, 1927. Flooding by the Skagway River has inundated parts of the city many times, usually during heavy rains in the fall. Two floods were reported to have been caused by the sudden draining of glacier-dammed lakes. Dikes protect the city from many smaller floods, but heightening and broadening is needed to give full protection. Slow land uplift at Skagway, because of regional glacioisostatic rebound, averages 0.059 foot per year. On this basis, the shoreline theoretically shifted seaward 500 feet and the harbor shoaled 4.4 feet between 1897 and 1972.</p><p>It is recommended that future geologic study of the Skagway area include: detailed geologic mapping and collection of data on geologic materials, joints, faults, and slope stability; complete evaluation of earthquake probability and response of materials to shaking; and collection and evaluation of periodic soundings and sediment data from Skagway and Taiya deltas to assist in forecasting the stability of the delta front.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72454","usgsCitation":"Yehle, L.A., and Lemke, R.W., 1972, Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Open-File Report 72-454, Report: iv, 108 p.; 4 Plates: 35.77 x 18.67 inches or smaller, https://doi.org/10.3133/ofr72454.","productDescription":"Report: iv, 108 p.; 4 Plates: 35.77 x 18.67 inches or smaller","costCenters":[],"links":[{"id":427161,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427160,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427159,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427158,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427153,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0454/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150379,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0454/report-thumb.jpg"}],"scale":"9600","country":"United States","state":"Alaska","city":"Skagway","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -135.3463249696411,\n              59.48810534833572\n            ],\n            [\n              -135.3463249696411,\n              59.40680330286153\n            ],\n            [\n              -135.22164285027563,\n              59.40680330286153\n            ],\n            [\n              -135.22164285027563,\n              59.48810534833572\n            ],\n            [\n              -135.3463249696411,\n              59.48810534833572\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db6443d4","contributors":{"authors":[{"text":"Yehle, Lynn A. yehle@usgs.gov","contributorId":3794,"corporation":false,"usgs":true,"family":"Yehle","given":"Lynn","email":"yehle@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":173260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lemke, Richard Walter","contributorId":105280,"corporation":false,"usgs":true,"family":"Lemke","given":"Richard","email":"","middleInitial":"Walter","affiliations":[],"preferred":false,"id":173261,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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