{"pageNumber":"6280","pageRowStart":"156975","pageSize":"25","recordCount":184938,"records":[{"id":70009939,"text":"70009939 - 1972 - Appraisal of the future climate of the Holocene in the Rocky Mountains","interactions":[],"lastModifiedDate":"2025-07-11T15:57:31.67714","indexId":"70009939","displayToPublicDate":"2004-11-19T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Appraisal of the future climate of the Holocene in the Rocky Mountains","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>Consideration of the history of Holocene climate in the Rocky Mountains indicates that the over-all trend during the past 2500 yr has been toward increasing warmth, interrupted by cooler times of minor advances of cirque glaciers. Comparison of Holocene climatic history with the record of past interglacials in the region suggests that the present interglacial is not complete and that the climate may become first warmer and subsequently wetter before it is completed. Correlation of the timing of the regional glacial-interglacial record for the past 140,000 yr with the record of major sea level changes and with the calculated changes in the earth's insolation suggest that the present interglacial may be completed within a few millenia and that it may be followed by a significant cooling of the climate.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0033-5894(72)90051-8","issn":"00335894","usgsCitation":"Richmond, G., 1972, Appraisal of the future climate of the Holocene in the Rocky Mountains: Quaternary Research, v. 2, no. 3, p. 315-322, https://doi.org/10.1016/0033-5894(72)90051-8.","productDescription":"8 p.","startPage":"315","endPage":"322","costCenters":[],"links":[{"id":219115,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Rocky Mountain region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -126.51511131378889,\n              60.2309575319278\n            ],\n            [\n              -116.18429597454725,\n              42.750947322770955\n            ],\n            [\n              -108.87838224399725,\n              36.86506804817596\n            ],\n            [\n              -105.40760189448564,\n              35.35379898384873\n            ],\n            [\n              -104.83911650777394,\n              41.21864052034894\n            ],\n            [\n              -108.6656330679895,\n              48.208352104843684\n            ],\n            [\n              -121.0355086645085,\n              59.62239173453176\n            ],\n            [\n              -126.51511131378889,\n              60.2309575319278\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"2","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059ecd8e4b0c8380cd49509","contributors":{"authors":[{"text":"Richmond, G.M.","contributorId":104066,"corporation":false,"usgs":true,"family":"Richmond","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":357495,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010081,"text":"70010081 - 1972 - Pleistocene tectonic accretion of the continental slope off Washington","interactions":[],"lastModifiedDate":"2025-04-16T23:18:17.015983","indexId":"70010081","displayToPublicDate":"2003-04-07T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Pleistocene tectonic accretion of the continental slope off Washington","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>Interpretation of reflection profiles across the Washington continental margin suggests deformation of Cascadia basin strata against the continental slope. Individual reflecting horizons can be traced across the slope-basin boundary. The sense of offset along faults on the continental slope is predominantly, but not entirely, west side up. Two faults of small displacement are seen to be west-dipping reverse faults. Magnetic anomalies on the Juan de Fuca plate can be traced 40–100 km eastward under the slope, and structural interpretation combined with calculated rates of subduction suggests that approximately 50 km of the outer continental slope may have been formed in Pleistocene time. Rocks of Pleistocene age dredge from a ridge exposing acoustic “basement” on the slope, plus the results of deep-sea drilling off northern Oregon, are consistent with this interpretation. The question of whether or not subduction is occurring at present is unresolved because significant strain has not affected the upper 200 m of section in the Cascadia basin. However, deformation of the outer part of the slope has been episodic and may reflect episodic yield, deposition rate, subduction rate, or some combination of these factors.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(72)90053-9","issn":"00253227","usgsCitation":"Silver, E.A., 1972, Pleistocene tectonic accretion of the continental slope off Washington: Marine Geology, v. 13, no. 4, p. 239-249, https://doi.org/10.1016/0025-3227(72)90053-9.","productDescription":"11 p.","startPage":"239","endPage":"249","costCenters":[],"links":[{"id":219428,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -127.66113281249999,\n              45.644768217751924\n            ],\n            [\n              -121.2451171875,\n              45.644768217751924\n            ],\n            [\n              -121.2451171875,\n              48.545705491847464\n            ],\n            [\n              -127.66113281249999,\n              48.545705491847464\n            ],\n            [\n              -127.66113281249999,\n              45.644768217751924\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"13","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7c54e4b0c8380cd79919","contributors":{"authors":[{"text":"Silver, E. A.","contributorId":18491,"corporation":false,"usgs":true,"family":"Silver","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":357854,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010180,"text":"70010180 - 1972 - Influence of grounding ice on the Arctic shelf of Alaska","interactions":[],"lastModifiedDate":"2025-04-16T23:14:25.067807","indexId":"70010180","displayToPublicDate":"2003-04-02T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Influence of grounding ice on the Arctic shelf of Alaska","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id7\" class=\"abstract author\"><div id=\"aep-abstract-sec-id8\"><p>Alaska's Beaufort Sea shelf is characterized by small-scale relief with an average amplitude of 1–2 m and wavelength of 50–100 m. Diving observations confirm that much of the bottom roughness reflects the action of grounded ice. Except for areas in the shadow of islands, bars, and offshore bathymetric highs, the entire shelf surface from the beach to at least the 75-m contour is now or has been modified by ice gouging. Ice contact with the bottom is more common, and rates of sedimentation higher on the inner shelf than on the outer shelf; the density of gouge features is about equal in both areas. Therefore, the chances are that an area of gouging on the inner shelf contains younger gouges than a similar area on the outer shelf.</p><p>When ice grounds, it becomes an important agent in the sedimentary and morphologic environment of the Arctic shelf, directly by deforming bottom deposits and secondarily by affecting the current regime near the sediment/ice contact. While bulldozing action and rafting do not seem to contribute significantly to the direct transport of sediment, re-suspension of bottom material during bulldozing, which makes sediment available for transport, may be significant.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(72)90014-X","issn":"00253227","usgsCitation":"Reimnitz, E., Barnes, P., Forgatsch, T., and Rodeick, C., 1972, Influence of grounding ice on the Arctic shelf of Alaska: Marine Geology, v. 13, no. 5, p. 323-334, https://doi.org/10.1016/0025-3227(72)90014-X.","productDescription":"12 p.","startPage":"323","endPage":"334","costCenters":[],"links":[{"id":218631,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -146.44775390625,\n              69.89256519285392\n            ],\n            [\n              -145.04150390625,\n              69.89256519285392\n            ],\n            [\n              -145.04150390625,\n              70.18510275498964\n            ],\n            [\n              -146.44775390625,\n              70.18510275498964\n            ],\n            [\n              -146.44775390625,\n              69.89256519285392\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"13","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b3de4b0c8380cd62358","contributors":{"authors":[{"text":"Reimnitz, E.","contributorId":61557,"corporation":false,"usgs":true,"family":"Reimnitz","given":"E.","affiliations":[],"preferred":false,"id":358221,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, P.","contributorId":73331,"corporation":false,"usgs":true,"family":"Barnes","given":"P.","affiliations":[],"preferred":false,"id":358222,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forgatsch, T.","contributorId":15335,"corporation":false,"usgs":true,"family":"Forgatsch","given":"T.","email":"","affiliations":[],"preferred":false,"id":358219,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rodeick, C.","contributorId":19280,"corporation":false,"usgs":true,"family":"Rodeick","given":"C.","affiliations":[],"preferred":false,"id":358220,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70188907,"text":"70188907 - 1972 - An inventory of suspended sediment stations and type of data analysis for Pennsylvania streams, 1947-1970","interactions":[],"lastModifiedDate":"2017-07-12T15:17:55","indexId":"70188907","displayToPublicDate":"2000-03-11T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"An inventory of suspended sediment stations and type of data analysis for Pennsylvania streams, 1947-1970","docAbstract":"<p>Data concerning suspended sediment concentrations and loads, frequency of occurrence of suspended sediment concentrations, and long-term trends of annual suspended sediment loads are important tools for today's environmental manager. These data are required background for those concerned with establishing and enforcing erosion and sedimentation control regulations and sediment concentration or turbidity standards for water-quality criteria, or those concerned with designing for adequate long-term water storage in reservoirs (sediment load), for efficient municipal and industrial plant operation (sediment concentration frequency), etc.<br></p><p>This is a compilation of the location, period of record, sampling frequency and type of data synthesis for suspended sediment carried by Pennsylvania streams. Figures 1 and 2 show the approximate locations of sediment sampling stations in Pennsylvania. All of the sediment data listed were collected by the U. S. Geological Survey mainly in cooperation with the following Federal, State, and local agencies.<br></p><p style=\"padding-left: 60px;\" data-mce-style=\"padding-left: 60px;\">Pennsylvania Department of Environmental Resources<br>&nbsp; &nbsp; &nbsp;Bureau of Engineering and Construction<br>&nbsp; &nbsp; &nbsp;Soil and Water Conservation Commission<br>Pennsylvania Department of Transportation<br>City of Philadelphia<br>Brandywine Valley Association<br>Delaware Geological Survey<br>Conestoga Valley Association<br>Lehigh County Soil and Water Conservation District<br>Corps of Engineers, U. S. 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,{"id":65715,"text":"i711 - 1972 - Geologic map of Yellowstone National Park","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i711","displayToPublicDate":"1995-11-01T00:00:00","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":"711","subseriesTitle":"NONE","title":"Geologic map of Yellowstone National Park","language":"ENGLISH","doi":"10.3133/i711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Geologic map of Yellowstone National Park: U.S. Geological Survey IMAP 711, 1 map :col. ;87 x 86 cm. on sheet 98 x 104 cm. folded in envelope 31 x 24 cm., https://doi.org/10.3133/i711.","productDescription":"1 map :col. ;87 x 86 cm. on sheet 98 x 104 cm. folded in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":106926,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9475.htm","linkFileType":{"id":5,"text":"html"},"description":"9475"},{"id":189430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.16666666666667,44.13333333333333 ], [ -111.16666666666667,45.11666666666667 ], [ -109.8,45.11666666666667 ], [ -109.8,44.13333333333333 ], [ -111.16666666666667,44.13333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2b02","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":534087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70202873,"text":"70202873 - 1972 - Water quality at Miami International Airport, Miami, Florida, 1971–72","interactions":[],"lastModifiedDate":"2025-04-24T18:44:36.007127","indexId":"70202873","displayToPublicDate":"1994-04-01T14:44:18","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"FL 72-023","displayTitle":"Water quality at Miami International Airport, Miami, Florida, 1971–72","title":"Water quality at Miami International Airport, Miami, Florida, 1971–72","docAbstract":"<p>The quality of water, sediment, and biota was determined at four sites in canals and drainage ditches at Miami International Airport (MIA) during high- and low-water periods and during summer and winter 1971–72. Concentrations of common ions, such as calcium, sodium, chloride, and magnesium, tended to be above average for fresh water because of periodic salt-water intrusion. Nitrogen, phosphorus, and pesticides were in higher concentrations than typical for undisturbed areas of south Florida, but not higher than usual for the urban coastal area, so it is not known to what extent these chemicals are attributable to surrounding urbanization. Heavy metals, oil and grease, and PCB's (polychlorinated biphenyls) were the best indicators of the effects of MIA on water quality. Concentations of the above were quite variable, high values for each were recorded and were probably associated with recent discharges from industrial sources. Arsenic, lead, iron, and chromium all exceeded, in one or more samples, the U.S. Public Health Service's recommended upper limits for metals in water. Only iron normally exceeds these standards in the natural waters of south Florida. PCB's were detected in most samples and were in concentrations up to 1,000 micrograms per kilogram in fish. In addition to pesticides and PCB's, another group of persistant chlorinated compounds, PCN's (polychlorinated naphthalenes) were detected in water, sediment, and fish. This is the first known detection of these compounds in the environment.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70202873","usgsCitation":"Freiberger, H.J., and McPherson, B.F., 1972, Water quality at Miami International Airport, Miami, Florida, 1971–72: Open-File Report FL 72-023, 50 p., https://doi.org/10.3133/70202873.","productDescription":"50 p.","numberOfPages":"50","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":362649,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70202873/ofr72023.pdf","text":"Report","size":"1.28 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":362648,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70202873/coverthb.jpg"}],"contact":"<p><a href=\"https://www.usgs.gov/locations/st-petersburg-coastal-and-marine-science-center\" data-mce-href=\"https://www.usgs.gov/locations/st-petersburg-coastal-and-marine-science-center\">St. Petersburg Coastal and Marine Science Center</a><br>U.S. Geological Survey<br>600 4th Street South<br>St. Petersburg, FL 33701</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Sampling sites</li><li>Methods</li><li>Streamflow</li><li>Rainfall</li><li>Water quality</li><li>Summary and conclusions</li><li>References</li></ul>","publishedDate":"1972-10-01","noUsgsAuthors":false,"publicationDate":"1972-10-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Freiberger, Herbert J.","contributorId":84404,"corporation":false,"usgs":true,"family":"Freiberger","given":"Herbert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":760363,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McPherson, Benjamin F.","contributorId":17965,"corporation":false,"usgs":true,"family":"McPherson","given":"Benjamin","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":760364,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12415,"text":"ofr722 - 1972 - Iron resources of Turkey","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr722","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":"72-2","title":"Iron resources of Turkey","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr722","usgsCitation":"Albers, J.P., and Capan, U., 1972, Iron resources of Turkey: U.S. Geological Survey Open-File Report 72-2, 12 leaves :ill., map ;27 cm., https://doi.org/10.3133/ofr722.","productDescription":"12 leaves :ill., map ;27 cm.","costCenters":[],"links":[{"id":144333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa6e4b07f02db6666e4","contributors":{"authors":[{"text":"Albers, John Patrick","contributorId":26669,"corporation":false,"usgs":true,"family":"Albers","given":"John","email":"","middleInitial":"Patrick","affiliations":[],"preferred":false,"id":166102,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Capan, Ussal","contributorId":106123,"corporation":false,"usgs":true,"family":"Capan","given":"Ussal","affiliations":[],"preferred":false,"id":166103,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12777,"text":"ofr7248 - 1972 - Evaluation of the Um Gerad barite deposits near Rabigh, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2014-07-10T09:40:58","indexId":"ofr7248","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":"72-48","title":"Evaluation of the Um Gerad barite deposits near Rabigh, Kingdom of Saudi Arabia","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr7248","usgsCitation":"Brobst, D.A., 1972, Evaluation of the Um Gerad barite deposits near Rabigh, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 72-48, 7 leaves ;27 cm., https://doi.org/10.3133/ofr7248.","productDescription":"7 leaves ;27 cm.","costCenters":[],"links":[{"id":145016,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0048/report-thumb.jpg"},{"id":289704,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0048/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa5f7","contributors":{"authors":[{"text":"Brobst, Donald Albert","contributorId":36117,"corporation":false,"usgs":true,"family":"Brobst","given":"Donald","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":166690,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12882,"text":"ofr7260 - 1972 - A preliminary study of peat resources in eastern Maine","interactions":[],"lastModifiedDate":"2026-04-22T16:51:58.002549","indexId":"ofr7260","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":"72-60","title":"A preliminary study of peat resources in eastern Maine","docAbstract":"<p>Nineteen peat deposits in southeastern Aroostook County (fig. 1) contain an estimated 4,987,000 tons of peat. The location, size and quality data for each deposit are given in tables 1, 2 and 3. Thirty-eight deposits in Washington County (fig. 2) contain an estimated 20,041,000 tons of peat. The location, size and quality data for each deposit are given in tables 4, 5 and 6. Twenty additional deposits containing estimated 3,802,000 tons in Washington County (fig. 2) were not sampled in detail but are described in tables 7 and 8. In addition to the deposits studied, it is estimated that there are at least as many more deposits of similiar size and quality in the area studied.</p><p>Data in this study were obtained by conducting pace and compass traverses across swamps, marshes and heaths. Auger holes were put down by hand using a Davis sampler and Macaulay peat borer along the traverses to collect samples of the peat and to determine the thickness and stratigraphy of the deposits and the configuration of the depression in which they lie. The amount of peat was estimated from auger hole data and from the surface area measured on topographic and air photo maps. In calculating tonnages, 1 acre-foot of peat in place was considered equivalent to 200 tons of air-dried peat. Samples from all of the deposits were analyzed under the supervision of Irving May in the laboratories of the U.S. Geological Survey for moisture, ash, organic content, water-holding capacity, fiber size (exceeding 0.15mm),and acidity.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7260","usgsCitation":"Cameron, C.C., 1972, A preliminary study of peat resources in eastern Maine: U.S. Geological Survey Open-File Report 72-60, 25 leaves :maps ;29 cm., https://doi.org/10.3133/ofr7260.","productDescription":"25 p.","costCenters":[],"links":[{"id":503314,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0060/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147083,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0060/report-thumb.jpg"}],"country":"United 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,{"id":21119,"text":"ofr72377 - 1972 - Geology and geochemistry of a part of the Abla Formation at Jabal Rumur, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr72377","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":"72-377","title":"Geology and geochemistry of a part of the Abla Formation at Jabal Rumur, Kingdom of Saudi Arabia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr72377","usgsCitation":"Theobald, P., and Thompson, C., 1972, Geology and geochemistry of a part of the Abla Formation at Jabal Rumur, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 72-377, 15, [7] leaves (some folded) :ill. ;28 cm., https://doi.org/10.3133/ofr72377.","productDescription":"15, [7] leaves (some folded) :ill. ;28 cm.","costCenters":[],"links":[{"id":154118,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0377/report-thumb.jpg"},{"id":50707,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0377/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50708,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0377/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50709,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0377/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50710,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0377/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db686165","contributors":{"authors":[{"text":"Theobald, P. K.","contributorId":45293,"corporation":false,"usgs":true,"family":"Theobald","given":"P. K.","affiliations":[],"preferred":false,"id":183874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, Charles E.","contributorId":35333,"corporation":false,"usgs":true,"family":"Thompson","given":"Charles E.","affiliations":[],"preferred":false,"id":183873,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22987,"text":"ofr72108 - 1972 - The hydraulic geometry of some Alaskan streams south of the Yukon River","interactions":[],"lastModifiedDate":"2024-02-14T22:23:45.085047","indexId":"ofr72108","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":"72-108","title":"The hydraulic geometry of some Alaskan streams south of the Yukon River","docAbstract":"<p>Channel geometry surveys were conducted to determine bankfull stage, discharge, and other hydraulic parameters at 22 locations along the proposed route of the trans-Alaska pipeline corridor south of the Yukon River. Combined with the records from gaging stations located at some of the sites, the data are sufficient to describe some of the channel and flow characteristics typical of each of two major hydrologic areas, the Yukon River Region and the South-Central Region. Although each region follows general hydrologic trends, least squares relations indicate each exhibits its own particular deviations.</p><p>Average values of the hydraulic and geometric properties of rivers were used to illustrate their application to practical engineering problems, namely the computation of depth of channel scour and of bedload discharge. For design purposes, caution is recommended when making computations based on average values. 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,{"id":48022,"text":"ofr7297 - 1972 - Ground-water outflow, San Timoteo-Smiley Heights area, upper Santa Ana Valley, southern California, 1927 through 1968","interactions":[],"lastModifiedDate":"2022-09-16T19:31:03.070135","indexId":"ofr7297","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":"72-97","title":"Ground-water outflow, San Timoteo-Smiley Heights area, upper Santa Ana Valley, southern California, 1927 through 1968","docAbstract":"The San Timoteo-Smiley Heights area is in the upper Santa Ana Valley, San Bernardino and Riverside Counties, Calif., where the Yucaipa and San Timoteo-Beaumont ground-water basins border Bunker .Hill basin on the south between the San Jacinto and San Andreas faults. The area is broken by numerous faults, the topography is rough, and in a large part of the area few wells had been drilled prior to 196S. \r\n\r\nThe alluvial deposits, which constitute the aquifers in the area, range in thickness from 0 where they lap onto exposed bedrock hills to about 1,000 feet. Beneath the southern part of the area near the San Jacinto fault the total thickness of alluvial and lacustrine deposits may be as much as 6,000 feet. \r\n\r\nThe purpose of this study was to estimate ground-water outflow by an indirect method not involving balancing of the hydrologic budget. For this purpose it was necessary to estimate the permeability of the aquifer materials, the average annual hydraulic gradient, and the cross-sectional area through which the flow occurs; these values were estimated for five segments along a line of section between the San Jacinto fault and Crafton Hills. \r\n\r\nTo provide data for the outflow estimates, several miles of reflection and refraction seismic traverses were made along and across the outflow section. Nineteen deep and shallow test holes were drilled; one of the deep test holes and several existing wells were pumped to obtain data on aquifer permeability.\r\n\r\nThe estimated average permeabilities of the aquifer materials range from 5 gallons per day per square foot for the lower part of the San Timoteo beds of Frick (1921) and 40 gallons per day per square foot for the older alluvium to 220 gallons per day per square foot for the upper part of the San Timoteo beds. \r\n\r\nThe estimated outflow in 1927 was 8,150 acre-feet. By 1967 the estimated total outflow was 5,350 acre-feet, a reduction of approximately 34 percent. During the 12-year period 1956 through 1967, however, the annual outflow decline has been considerably less than the average for the 41-year period 1927 through 1967, and the decline as of 1968 was probably about 30-35 acre-feet per year.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7297","usgsCitation":"Dutcher, L., and Fenzel, F., 1972, Ground-water outflow, San Timoteo-Smiley Heights area, upper Santa Ana Valley, southern California, 1927 through 1968: U.S. Geological Survey Open-File Report 72-97, Report: ii, 30 p.; 2 Plates: 35.22 × 22.43 inches and 33.72 × 22.76 inches, https://doi.org/10.3133/ofr7297.","productDescription":"Report: ii, 30 p.; 2 Plates: 35.22 × 22.43 inches and 33.72 × 22.76 inches","costCenters":[],"links":[{"id":110340,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52161.htm","linkFileType":{"id":5,"text":"html"},"description":"52161"},{"id":84797,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0097/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84796,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0097/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84795,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0097/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0097/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Timoteo-Smiley Heights area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.2431,\n              33.9756\n            ],\n            [\n              -117.0681,\n              33.9756\n            ],\n            [\n              -117.0681,\n              34.0778\n            ],\n            [\n              -117.2431,\n              34.0778\n            ],\n            [\n              -117.2431,\n              33.9756\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66741d","contributors":{"authors":[{"text":"Dutcher, L.C.","contributorId":42191,"corporation":false,"usgs":true,"family":"Dutcher","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":236685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fenzel, F. W.","contributorId":94742,"corporation":false,"usgs":true,"family":"Fenzel","given":"F. W.","affiliations":[],"preferred":false,"id":236686,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15289,"text":"ofr72281 - 1972 - Reconnaissance geology of the Precambrian rocks in the Ayn Qunay quadrangle, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:47","indexId":"ofr72281","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":"72-281","title":"Reconnaissance geology of the Precambrian rocks in the Ayn Qunay quadrangle, Kingdom of Saudi Arabia","docAbstract":"The Aya Qunay quadrangle covers an area of 2833 sq km in central Saudi Arabia, Only the western edge of the quadrangle is underlain by Precambrian rocks, which were the subject of this investigation. Toward the east the Precambrian rocks are unconformably overlain by Permian and younger sedimentary rocks. \r\n\r\nThe Permian rocks at the west edge of the Ayn Qunay quadrangle consist mainly of a granitic intrusive complex of batholithic dimensions. Parts of the eastern edge of the granitic complex are exposed just west of the overlying Khuff Formation of Permian age, where biotite-hornblende granite of the complex intrudes chlorite-sericite schist of the Precambrian Bi'r Khountina Group. The biotite-hornblende granite of the complex also intrudes plutons of diorite, gabbro, and pyroxenite and is itself intruded by granite porphyry, thereby indicating some difference in age between the granitic rocks in the complex. A sequence of metamorphosed volcanic rocks composed mainly of andesite, rhyolite, and kindred rocks, and called the Halaban Group, is older than the Bi'r Khountina Group. Relations between the Halaban and a gray hornblende-biotite granite gneiss are uncertain, but the gneiss may be older than the Halaban. The few observed contacts disclosed parallel foliation in the two units, but the foliation may have been imposed after the Halaban was deposited on the granite gneiss. \r\n\r\nTwo major left-lateral faults extend west-northwest across the Precambrian rocks but are not in the Permian rocks. These faults parallel to the Najd fault zone found farther south. Seemingly they correlate in time with early movements on the Najd fault zone, but not with the latest. \r\n\r\nSaprolitic material-of variable thickness is present on the upper surface of the Precambrian rocks beneath the Khuff Formation at many places. Where the Khuff Formation has been removed by erosion, the saprolite is also stripped away. The weathering probably took place in pre-Khuff time. \r\n\r\nNo ancient mines or prospects were seen in the Precambrian rocks; however, a notable positive anomaly for tungsten in concentrates is associated with a small prominence of granite porphyry 35 km southwest of Ayn Qunay. Further investigation of the porphyry should be undertaken to learn the amount of scheelite at this locality.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr72281","usgsCitation":"Overstreet, W.C., Whitlow, J.W., and Ankary, A.O., 1972, Reconnaissance geology of the Precambrian rocks in the Ayn Qunay quadrangle, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 72-281, ii, 26 leaves :col. ill., folded map ;27 cm., https://doi.org/10.3133/ofr72281.","productDescription":"ii, 26 leaves :col. ill., folded map ;27 cm.","costCenters":[],"links":[{"id":146411,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0281/report-thumb.jpg"},{"id":44210,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0281/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44211,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0281/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db62811c","contributors":{"authors":[{"text":"Overstreet, William C.","contributorId":73586,"corporation":false,"usgs":true,"family":"Overstreet","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":170893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitlow, Jesse William","contributorId":18366,"corporation":false,"usgs":true,"family":"Whitlow","given":"Jesse","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":170891,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ankary, Abdullah O.","contributorId":30991,"corporation":false,"usgs":true,"family":"Ankary","given":"Abdullah","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":170892,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38690,"text":"pp800D - 1972 - Geological Survey research 1972","interactions":[],"lastModifiedDate":"2025-08-22T20:26:27.572414","indexId":"pp800D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"800","chapter":"D","title":"Geological Survey research 1972","docAbstract":"<p>This collection of 30 short papers is the third published chapter of \"Geological Survey Research 1972.\" The papers report on scientific and economic results of current work by members of the Geologic and Water Resources Divisions of the U.S. Geological Survey.</p><p>Chapter A, to be published later in the year, will present a summary of significant results of work done in fiscal year 1972, together with lists of investigations in progress, cooperating agencies, and Geological Survey offices.</p><p>\"Geological Survey Research 1972\" is the thirteenth and last volume of the annual series Geological Survey Research. The short-papers chapters (B, C, and D) will be replaced in 197 3 by the \"Journal of Research of the U.S. Geological Survey,\" and the summary chapter (A) will be published as a separate professional paper. The twelve volumes already published are listed below, with their series designations. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1972 (Professional Paper 800)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp800D","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Geological Survey research 1972: U.S. Geological Survey Professional Paper 800, iv, 227 p., https://doi.org/10.3133/pp800D.","productDescription":"iv, 227 p.","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":494633,"rank":17,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31404.htm","text":"Land-use effect on the water regimen of the U.S. Virgin Islands","linkFileType":{"id":5,"text":"html"}},{"id":494632,"rank":16,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31403.htm","text":"Fremont Lake, Wyoming - preliminary survey of a large mountain lake","linkFileType":{"id":5,"text":"html"}},{"id":494621,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31389.htm","text":"Late Pleistocene glaciation and pollen stratigraphy in northwestern New Jersey","linkFileType":{"id":5,"text":"html"}},{"id":494620,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31388.htm","text":"Significance of Lower Ordovician exotic blocks in the Hamburg klippe, eastern Pennsylvania","linkFileType":{"id":5,"text":"html"}},{"id":494631,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31402.htm","text":"Staurolite, kyanite, and sillimanite from Narragansett basin of Rhode Island","linkFileType":{"id":5,"text":"html"}},{"id":494630,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31401.htm","text":"Genesis of mesozonal granitic rocks below the base of the Stillwater complex in the Beartooth Mountains, Montana","linkFileType":{"id":5,"text":"html"}},{"id":494629,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31400.htm","text":"Investigation of the occurrence and transport of arsenic in the upper Sugar Creek watershed, Charlotte, North Carolina","linkFileType":{"id":5,"text":"html"}},{"id":494628,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31399.htm","text":"Nitrogen content of ground water in Kings County, Long Island, New York","linkFileType":{"id":5,"text":"html"}},{"id":494627,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31398.htm","text":"The hydrologic balance of Lake Sallie, Becker County, Minnesota","linkFileType":{"id":5,"text":"html"}},{"id":494626,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31394.htm","text":"Potassium-argon ages from whole-rock analyses of igneous rocks in the area of the National Reactor Testing Station, Idaho","linkFileType":{"id":5,"text":"html"}},{"id":494625,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31393.htm","text":"Potassium-argon ages from areas of hydrothermal alteration in South Carolina","linkFileType":{"id":5,"text":"html"}},{"id":494624,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31392.htm","text":"Strontium isotopic composition of some early Miocene rhyolite tuffs and lavas from northwestern part of the Great Basin","linkFileType":{"id":5,"text":"html"}},{"id":494623,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31391.htm","text":"Distribution of earthquakes related to mobility of the south flank of Kilauea Volcano, Hawaii","linkFileType":{"id":5,"text":"html"}},{"id":494622,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31390.htm","text":"Unconformities within the Frontier Formation, northwestern Carbon County, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":65539,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0800d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119911,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0800d/report-thumb.jpg"},{"id":421034,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31387.htm","text":"Gravina-Nutzotin belt-tectonic significance of an Upper Mesozoic sedimentary and volcanic sequence in southern and southeastern Alaska"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6876bc","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":529875,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13787,"text":"ofr72130 - 1972 - Earthquakes in the oil field at Rangely, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"ofr72130","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":"72-130","title":"Earthquakes in the oil field at Rangely, Colorado","docAbstract":"<p>Seven years of seismic data recorded at the Uinta Basin Observatory were searched for earthquakes originating near an oil field at Rangely, Colorado, located 65 km ESE of the observatory. Changes in the number of earthquakes recorded per year appear to correlate with changes in the quantity of fluid injected per year. Between November 1962 and January 1970, 976 earthquakes were detected near the oil field by the UBO station; 320 earthquakes were larger than magnitude 1.</p> <p>Richter magnitudes are estimated from both S-wave and P-wave measurements and a method based on the duration of the seismic signal is used to estimate the magnitude of the larger shocks. The two largest shocks had magnitudes of 3.4 and 3.3. The total seismic energy released was l0<sup>l7</sup> ergs. During this same period the energy used for water injection, measured at the wellhead, was 10<sup>21</sup> ergs.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr72130","usgsCitation":"Gibbs, J., Healy, J., Raleigh, C.B., and Coakley, J.M., 1972, Earthquakes in the oil field at Rangely, Colorado: U.S. Geological Survey Open-File Report 72-130, 26 p.; Appendix, https://doi.org/10.3133/ofr72130.","productDescription":"26 p.; Appendix","onlineOnly":"Y","temporalStart":"1962-11-01","temporalEnd":"1970-01-31","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":116805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_72_130.gif"},{"id":111130,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1972/0130/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","city":"Rangely","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.75,40 ], [ -109.75,40.5 ], [ -108.75,40.5 ], [ -108.75,40 ], [ -109.75,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db629424","contributors":{"authors":[{"text":"Gibbs, James F.","contributorId":95880,"corporation":false,"usgs":true,"family":"Gibbs","given":"James F.","affiliations":[],"preferred":false,"id":168386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, John H.","contributorId":19562,"corporation":false,"usgs":true,"family":"Healy","given":"John H.","affiliations":[],"preferred":false,"id":168384,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Raleigh, C. Barry","contributorId":103683,"corporation":false,"usgs":true,"family":"Raleigh","given":"C.","email":"","middleInitial":"Barry","affiliations":[],"preferred":false,"id":168387,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Coakley, John M.","contributorId":61436,"corporation":false,"usgs":true,"family":"Coakley","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":168385,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":39023,"text":"pp387B - 1972 - Recent activity of glaciers of Mount Rainier, Washington","interactions":[],"lastModifiedDate":"2025-05-20T13:43:37.038244","indexId":"pp387B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"387","chapter":"B","title":"Recent activity of glaciers of Mount Rainier, Washington","docAbstract":"Knowing the ages of trees growing on recent moraines at Mount Rainier, Wash., permits the moraines to be dated. Moraines which are ridges of boulders, gravel, sand, and dust deposited at the margins of a glacier, mark former limits of a receding glacier. Knowing past glacial activity aids our understanding of past climatic variations.\r\n\r\nThe report documents the ages of moraines deposited by eight glaciers. Aerial photographs and planimetric maps show areas where detailed field studies were made below seven glaciers. Moraines, past ice positions, and sample areas are plotted on the photographs and maps, along with trails, roads, streams, and landforms, to permit critical areas to be identified in the future. Ground photographs are included so that sample sites and easily accessible moraines can be found along trails. Tables present data about trees sampled in areas near the glaciers of Mount Rainier, Wash.\r\n\r\nThe data in the tables show there are modern moraines of different age around the mountain; some valleys contain only one modern moraiine; others contain as many as nine. The evidence indicates a sequence of modern glacial advances terminating at about the following A.D. dates: 1525, 1550, 1625-60, 1715, 1730-65, 1820-60, 1875, and 1910. Nisqually River valley near Nisqually Glacier contains one moraine formed before A.D. 1842; Tahoma Creek valley near South Tahoma Glacier contains three moraines formed before A.D. 1528; 1843, and 1864; South Puyallup River valley near Tahoma Glacier, six moraines A.D. 1544, 1761, 1841, 1851, 1863, 1898; Puyallup Glacier, one moraine, A.D. 1846; Carbon Glacier, four moraines, 1519, 1763, 1847, 1876; Winthrop Glacier, four moraines, 1655, 1716, 1760, amid 1822; Emmons Glacier, nine moraines, 1596, 1613, 1661, 1738, 1825, 1850, 1865, 1870, 1901; and Ohanapecosh Glacier, three moraines, 1741, 1846, and 1878.\r\n\r\nAbandoned melt-water and flood channels were identified within moraine complexes below three glaciers, and their time of abandonment was dated. Outwash in three areas was deposited by melt-water of Tahoma Glacier before A.D. 1862, 1873, and 1910, respectively. Flood channels or melt-water channels on either side of Carbon River near Carbon Glacier dated from about 1901 to 1907. Melt-water channels of three different ages cut through Emmons Glacier moraines were dated as being abandoned before 1865, 1871, and 1917, respectively.\r\n\r\nAlthough the evidence at Mount Rainier indicates a sequence of glacial advance and retreat and of melt-water flow through different channels at different times, their climatic and hydrologic significance is not yet known.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp387B","usgsCitation":"Sigafoos, R.S., and Hendricks, E.L., 1972, Recent activity of glaciers of Mount Rainier, Washington: U.S. Geological Survey Professional Paper 387, Report: vi, 24 p.; 7 Plates: 35.00 x 33.00 inches or smaller, https://doi.org/10.3133/pp387B.","productDescription":"Report: vi, 24 p.; 7 Plates: 35.00 x 33.00 inches or smaller","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":66160,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0387b/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124857,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0387b/report-thumb.jpg"},{"id":66155,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0387b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66157,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0387b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66158,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0387b/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66161,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0387b/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":486132,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4385.htm","linkFileType":{"id":5,"text":"html"}},{"id":66162,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0387b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66156,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0387b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66159,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0387b/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Mount Rainier","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.9659158058002,\n              47.00544610953378\n            ],\n            [\n              -121.9659158058002,\n              46.74731525709666\n            ],\n            [\n              -121.55292944619455,\n              46.74731525709666\n            ],\n            [\n              -121.55292944619455,\n              47.00544610953378\n            ],\n            [\n              -121.9659158058002,\n              47.00544610953378\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db643aac","contributors":{"authors":[{"text":"Sigafoos, Robert S.","contributorId":82379,"corporation":false,"usgs":true,"family":"Sigafoos","given":"Robert","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":220820,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hendricks, E. 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,{"id":14354,"text":"ofr72197 - 1972 - Report on field trip to the Jabal As Sawrah and Wadi Al'Ays areas, northwestern Hijaz quadrangle, Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:01","indexId":"ofr72197","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":"72-197","title":"Report on field trip to the Jabal As Sawrah and Wadi Al'Ays areas, northwestern Hijaz quadrangle, Saudi Arabia","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr72197","usgsCitation":"Johnson, R.F., and Trent, V.A., 1972, Report on field trip to the Jabal As Sawrah and Wadi Al'Ays areas, northwestern Hijaz quadrangle, Saudi Arabia: U.S. Geological Survey Open-File Report 72-197, i, 4 leaves ;27 cm., https://doi.org/10.3133/ofr72197.","productDescription":"i, 4 leaves ;27 cm.","costCenters":[],"links":[{"id":147686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bc59","contributors":{"authors":[{"text":"Johnson, Robert Francis","contributorId":8864,"corporation":false,"usgs":true,"family":"Johnson","given":"Robert","email":"","middleInitial":"Francis","affiliations":[],"preferred":false,"id":169313,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trent, Virgil A.","contributorId":47381,"corporation":false,"usgs":true,"family":"Trent","given":"Virgil","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":169314,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13457,"text":"ofr7299 - 1972 - Preliminary bedrock geologic map of the Middle Haddam quadrangle, Middlesex County, Connecticut","interactions":[],"lastModifiedDate":"2022-03-24T18:24:40.396181","indexId":"ofr7299","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":"72-99","title":"Preliminary bedrock geologic map of the Middle Haddam quadrangle, Middlesex County, Connecticut","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7299","usgsCitation":"Eaton, G.P., and Rosenfeld, J.L., 1972, Preliminary bedrock geologic map of the Middle Haddam quadrangle, Middlesex County, Connecticut: U.S. Geological Survey Open-File Report 72-99, Report: 9 p.; 1 Plate: 19.46 × 27.07 inches, https://doi.org/10.3133/ofr7299.","productDescription":"Report: 9 p.; 1 Plate: 19.46 × 27.07 inches","costCenters":[],"links":[{"id":41900,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0099/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41899,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0099/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145442,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0099/report-thumb.jpg"},{"id":397537,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8752.htm"}],"scale":"24000","country":"United States","state":"Connecticut","county":"Middlesex County","otherGeospatial":"Middle Haddam quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.625,\n              41.5\n            ],\n            [\n              -72.5,\n              41.5\n            ],\n            [\n              -72.5,\n              41.625\n            ],\n            [\n              -72.625,\n              41.625\n            ],\n            [\n              -72.625,\n              41.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c933","contributors":{"authors":[{"text":"Eaton, Gordon P.","contributorId":67077,"corporation":false,"usgs":true,"family":"Eaton","given":"Gordon","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":167834,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenfeld, John L.","contributorId":57079,"corporation":false,"usgs":true,"family":"Rosenfeld","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":167833,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":13648,"text":"ofr72122 - 1972 - Analyses of stream-sediment and rock samples from parts of the Eagle quadrangle, east-central Alaska","interactions":[],"lastModifiedDate":"2021-11-04T21:28:14.28466","indexId":"ofr72122","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":"72-122","title":"Analyses of stream-sediment and rock samples from parts of the Eagle quadrangle, east-central Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72122","usgsCitation":"Foster, H.L., and Yount, M.E., 1972, Analyses of stream-sediment and rock samples from parts of the Eagle quadrangle, east-central Alaska: U.S. Geological Survey Open-File Report 72-122, Report: 102 p.; 2 Plates: 25.50 × 23.07 inches and 24.93 × 22.85 inches, https://doi.org/10.3133/ofr72122.","productDescription":"Report: 102 p.; 2 Plates: 25.50 × 23.07 inches and 24.93 × 22.85 inches","costCenters":[],"links":[{"id":42170,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0122/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42169,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0122/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391403,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8668.htm"},{"id":147297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0122/report-thumb.jpg"},{"id":42168,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0122/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Eagle quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -142,\n              64\n            ],\n            [\n              -141,\n              64\n            ],\n            [\n              -141,\n              65\n            ],\n            [\n              -142,\n              65\n            ],\n            [\n              -142,\n              64\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680156","contributors":{"authors":[{"text":"Foster, Helen Laura","contributorId":21936,"corporation":false,"usgs":true,"family":"Foster","given":"Helen","email":"","middleInitial":"Laura","affiliations":[],"preferred":false,"id":168171,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yount, M. E.","contributorId":76748,"corporation":false,"usgs":true,"family":"Yount","given":"M.","middleInitial":"E.","affiliations":[],"preferred":false,"id":168172,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":56712,"text":"wdrVA711 - 1972 - Water resources data for Virginia, water year 1971","interactions":[],"lastModifiedDate":"2020-12-31T22:04:56.496925","indexId":"wdrVA711","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":"VA-71-1","title":"Water resources data for Virginia, water year 1971","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrVA711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Virginia, water year 1971: U.S. Geological Survey Water Data Report VA-71-1, Report: ix, 305 p.; 1 Plate: 19.06 x 9.87 inches, 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