{"pageNumber":"5336","pageRowStart":"133375","pageSize":"25","recordCount":165252,"records":[{"id":70233096,"text":"70233096 - 1977 - The quantitative determination of chlorophylls A and B from freshwater algae without interference from degradation products","interactions":[],"lastModifiedDate":"2022-07-15T17:08:20.113298","indexId":"70233096","displayToPublicDate":"1977-03-01T12:02:17","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The quantitative determination of chlorophylls <i>A</i> and <i>B</i> from freshwater algae without interference from degradation products","title":"The quantitative determination of chlorophylls A and B from freshwater algae without interference from degradation products","docAbstract":"<p>Chlorophyll was efficiently extracted from freshwater algae with dimethyl sulfoxide. The extract was chromatographed on commercially available thin-layer cellulose sheets, 2 percent methanol and 98 percent petroleum ether being used as the solvent. Chlorophylls <i>a</i> and <i>b</i>, and phaeophytins <i>a</i> and <i>b</i> were cleanly separated from each other and other degradation products. No artifacts were formed. Recoveries of chlorophylls <i>a</i> and <i>b</i> were 98 and 96 percent as measured by spectrophotometry or fluorometry. </p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Shoaf, W.T., and Lium, B.W., 1977, The quantitative determination of chlorophylls A and B from freshwater algae without interference from degradation products: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 263-264.","productDescription":"2 p.","startPage":"263","endPage":"264","costCenters":[],"links":[{"id":403840,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403839,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Shoaf, W. Thomas","contributorId":21631,"corporation":false,"usgs":true,"family":"Shoaf","given":"W.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":846701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lium, Bruce W.","contributorId":75907,"corporation":false,"usgs":true,"family":"Lium","given":"Bruce","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":846702,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70170909,"text":"70170909 - 1977 - Geology and water-supply potential of the Anoka Sand Plain aquifer, Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T11:56:02","indexId":"70170909","displayToPublicDate":"1977-03-01T12:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":293,"text":"Technical Paper","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"6","title":"Geology and water-supply potential of the Anoka Sand Plain aquifer, Minnesota","docAbstract":"<p>Intensified land development on the Anoka sand plain necessitates a better understanding of the hydrogeology of the surficial outwash deposits of the area. The Anoka sand-plain aquifer consists of outwash attributable to two different ice lobes. Predominant grain size of the upper outwash decreases and sorting coefficient increases from west to east. Till or lake deposits underlie most of the surficial outwash. In some areas, these deposits are absent and the aquifer is directly underlain by bedrock, mainly sandstone. Preliminary study indicates that parts of the aquifer may yield several hundred to more than 1,000 gallons of water per minute to properly developed large-diameter wells. Storage in the aquifer is estimated to be 2,000 billion gallons and annual withdrawals approaching 250 billion gallons may be sustained. More detailed analysis is essential for proper management and optimum use of the resource.</p>","language":"English","publisher":"Minnesota Department of Natural Resources","publisherLocation":"St. Paul, MN","collaboration":"Prepared cooperatively by the Minnesota Department of Natural Resources and the U.S. Department of the Interior, Geological Survey","usgsCitation":"Helgesen, J.O., and Lindholm, G.F., 1977, Geology and water-supply potential of the Anoka Sand Plain aquifer, Minnesota: Technical Paper 6, 17 p.","productDescription":"17 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321084,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332588,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.leg.state.mn.us/edocs/edocs?oclcnumber=05392091"}],"country":"United States","state":"Minnesota","otherGeospatial":"Anoka Sand Plain aquifer","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57330630e4b0dae0d5dcd1c5","contributors":{"authors":[{"text":"Helgesen, J. O.","contributorId":62600,"corporation":false,"usgs":true,"family":"Helgesen","given":"J.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":629047,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindholm, G. F.","contributorId":88763,"corporation":false,"usgs":true,"family":"Lindholm","given":"G.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":629048,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70233087,"text":"70233087 - 1977 - Possibility of triggering earthquakes by injection of radioactive wastes in shale at Oak Ridge National Laboratory, Tenn.","interactions":[],"lastModifiedDate":"2022-07-15T16:49:42.579737","indexId":"70233087","displayToPublicDate":"1977-03-01T11:40:46","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Possibility of triggering earthquakes by injection of radioactive wastes in shale at Oak Ridge National Laboratory, Tenn.","docAbstract":"<p>Most investigators generally agree that the conditions for producing earthquakes by fluid injection through wells and by reservoir construction are (1) the presence of an underlying rock that is stressed to the verge of fracturing by tectonic stresses and (or) is on the brink of sliding on pre-existing fault planes, (2) the presence of potentially active faults(s), and (3) an increase of pore pressure in the rock caused by fluid injection or seepage from reservoir (s), which is probably the triggering force. The mechanism of disposal of radioactive wastes in shale by grout injection and hydraulic fracturing, which has been used at ORNL (Oak Ridge National Laboratory, Tenn.) is different from injection of fluid. The injected grout is in its liquid phase only during the injection period and, it is to be hoped, is confined in the hydraulically induced bedding-plane fractures. The grout is then allowed to solidify under pressure after termination of the injection, and, after solidification, it becomes an integral part of the shale. Significant characteristics of the disposal method and the site are as follows: (1) Because of the low permeability of shale and high viscosity of the injection grout, pore pressure in the rock, beyond the region of induced fractures, does not increase due to the injections; the injected grout enters newly formed bedding-plane fractures, (2) the injection site is free of local faults and of major interconnected joints and fractures; accordingly, injected grout in its liquid state is expected to be confined principally in the induced nearly horizontal bedding-plane fractures, and (3) due to low tensile strength along shale bedding planes, the energy needed to induce bedding-plane fractures is small; experiments made at ORNL indicate that the energy released during hydraulic fracturing in shale is so small that seismic signals generated by grout injections cannot be differentiated from ambient ground vibrations. In view of the fact 'that an increase of pore pressure in rock (the triggering force) and association with potentially active fault (s) do not occur at the proposed site at ORNL and that the disposal method does not produce an increase in pore pressure, it can reasonably be concluded that neither the method nor the site has the characteristics for triggering earthquakes during and after grout injections.</p>","language":"English","publisher":"U. S. Geological Survey","collaboration":"Work done in cooperation with the U.S. Energy Research and Development Administration","usgsCitation":"Sun, R.J., 1977, Possibility of triggering earthquakes by injection of radioactive wastes in shale at Oak Ridge National Laboratory, Tenn.: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 253-262.","productDescription":"10 p.","startPage":"253","endPage":"262","costCenters":[],"links":[{"id":403835,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403833,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Tennessee","otherGeospatial":"Oak Ridge National Laboratory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.33036804199219,\n              35.927980690382704\n            ],\n            [\n              -84.20539855957031,\n              35.927980690382704\n            ],\n            [\n              -84.20539855957031,\n              36.0624217151089\n            ],\n            [\n              -84.33036804199219,\n              36.0624217151089\n            ],\n            [\n              -84.33036804199219,\n              35.927980690382704\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sun, R. J.","contributorId":100403,"corporation":false,"usgs":true,"family":"Sun","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":846696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70233084,"text":"70233084 - 1977 - Effects of dredged channels on trace-metal migration in an estuary","interactions":[],"lastModifiedDate":"2022-07-15T16:40:07.685295","indexId":"70233084","displayToPublicDate":"1977-03-01T11:33:22","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Effects of dredged channels on trace-metal migration in an estuary","docAbstract":"<p>Determination of trace-metal levels in the sediments of the Matagorda Bay system revealed anomalously high mercury values. The distribution of the mercury-rich sediment deposits is the result of the sedimentological regime of the bay system produced by the tidal currents in the dredged channel. According to this model, the oxygenated open gulf water pushed into the bay by tidal currents activates the mercury and reintroduces it into the sediment regime of the bay in an area where the turbidity maximum is most prevalent. Within this region, the absorption sites are at a maximum, tying up the mercury. The mercury-enriched suspended material is then transported and deposited according to the hydraulic regime within the bay system.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Holmes, C.W., 1977, Effects of dredged channels on trace-metal migration in an estuary: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 243-251.","productDescription":"9 p.","startPage":"243","endPage":"251","costCenters":[],"links":[{"id":403831,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403829,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Gulf of Mexico, Matagorda Bay, Matagorda Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.8939208984375,\n              28.023500048883022\n            ],\n            [\n              -95.592041015625,\n              28.023500048883022\n            ],\n            [\n              -95.592041015625,\n              28.827831607445855\n            ],\n            [\n              -96.8939208984375,\n              28.827831607445855\n            ],\n            [\n              -96.8939208984375,\n              28.023500048883022\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Holmes, Charles W.","contributorId":31071,"corporation":false,"usgs":true,"family":"Holmes","given":"Charles","email":"","middleInitial":"W.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":846694,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70233080,"text":"70233080 - 1977 - Removal of fluorine and lithium from hectorite by solutions spanning a wide range of pH","interactions":[],"lastModifiedDate":"2022-07-15T16:32:56.038882","indexId":"70233080","displayToPublicDate":"1977-03-01T11:25:32","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Removal of fluorine and lithium from hectorite by solutions spanning a wide range of pH","docAbstract":"<p>One-gram samples of hectorite were treated with 40 millilitres each of hydrochloric acid (6 <i>N</i>), acetic acid (4.5 <i>N</i>), distilled water, natural seawater, sodium chloride (0.6 <i>N</i>), and sodium hydroxide (2.5 <i>N</i>) for 10 days in stoppered plastic centrifuge tubes. X-ray diffraction patterns show that the structure was virtually destroyed by the hydrochloric and acetic acids. Analyses of the supernatant liquids were made to determine amounts of the elements removed by the various treatments. All treatments removed at least some SiO<sub>2</sub>, MgO, CaO, Li<sub>2</sub>O, and F. The acids removed most of the lithium and magnesium after 3 days. The fluorine and the magnesium released by the acetic acid began to form sellaite (MgF<sub>2</sub> ). After 5 days, sufficient sellaite was produced to be discernible by X-ray diffraction. The loss of silica from the sample when it was treated with sodium hydroxide amounted to about 10 percent of the total sample. </p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Starkey, H., Mountjoy, W., and Gardner, J.M., 1977, Removal of fluorine and lithium from hectorite by solutions spanning a wide range of pH: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 235-242.","productDescription":"8 p.","startPage":"235","endPage":"242","costCenters":[],"links":[{"id":403828,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403827,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Starkey, Harry C.","contributorId":102074,"corporation":false,"usgs":true,"family":"Starkey","given":"Harry C.","affiliations":[],"preferred":false,"id":846691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mountjoy, Wayne","contributorId":21973,"corporation":false,"usgs":true,"family":"Mountjoy","given":"Wayne","email":"","affiliations":[],"preferred":false,"id":846692,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gardner, Johnnie M.","contributorId":293201,"corporation":false,"usgs":false,"family":"Gardner","given":"Johnnie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":846693,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70233078,"text":"70233078 - 1977 - Activity-product constants of brucite from 10 degrees to 90 degrees C","interactions":[],"lastModifiedDate":"2022-07-15T16:24:17.246885","indexId":"70233078","displayToPublicDate":"1977-03-01T11:15:22","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Activity-product constants of brucite from 10° to 90°C","title":"Activity-product constants of brucite from 10 degrees to 90 degrees C","docAbstract":"<p>The activity-product constant of brucite, <i>K<sub>B</sub></i>= [Mg<sup>2+</sup>][OH<sup>-</sup>]<sup>2</sup> (where the brackets denote activities), was determined experimentally at 10°, 25°, 40°, 55°, 70°, and 90°C. The values obtained for -log <i>K<sub>B</sub></i> are 10.89±0.16 (10°), 10.88±0.10 (25°), 10.90±0.10 (40°), 10.90±0.10 (55°), 10.99±0.14 (70°), and 11.10±0.14 (90°). Using National Bureau of Standards Technical Note 270 data for the ions, the free energy of formation (Δ<i>G</i>°<i><sub>t</sub></i>) at 25° for brucite is 831.486 joules per mole ( 198,730 cal mol<sup>-1</sup>). Using data compiled by R. A. Robie and D. R. Waldbaum in 1968 for the ions, this Δ<i>G</i>°<i><sub>t</sub></i> is -823,323 J mol<sup>-1</sup> (-198,930 cal mol<sup>-1</sup>).</p><p>Values of log KB are also calculated for the temperature range 0° to 200°C, by using thermochemical data listed by V. B. Parker, D. D. Wagman, and W. H. Evans in 1971 and E. G. King, M. J. Ferrante, and L. B. Pankratz in 1975 and the partial molal heat capacities estimated by C. M. Criss and J. W. Cobble in 1965. The experimental values are similar to the calculated values, especially at lower temperatures.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"McGee, K., and Hostetler, P.B., 1977, Activity-product constants of brucite from 10 degrees to 90 degrees C: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 227-233.","productDescription":"7 p.","startPage":"227","endPage":"233","costCenters":[],"links":[{"id":403824,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403823,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McGee, K.A.","contributorId":6059,"corporation":false,"usgs":true,"family":"McGee","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":846687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hostetler, P. B.","contributorId":107849,"corporation":false,"usgs":false,"family":"Hostetler","given":"P.","email":"","middleInitial":"B.","affiliations":[{"id":13719,"text":"Department of Geology, University of Missouri","active":true,"usgs":false}],"preferred":false,"id":846688,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70233074,"text":"70233074 - 1977 - Mercury in oil shale from the mahogany zone of the Green River formation, eastern Utah and western Colorado","interactions":[],"lastModifiedDate":"2022-07-15T16:14:25.497854","indexId":"70233074","displayToPublicDate":"1977-03-01T11:06:46","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Mercury in oil shale from the mahogany zone of the Green River formation, eastern Utah and western Colorado","docAbstract":"<p>Mercury has been reported in concentrations as high as 4 parts per million from oil shale in the Green River Formation near the Federal oil-shale prototype lease-tracts U-a and U-b in eastern Utah. This high concentration of mercury if present throughout a minable zone, would be of concern in commercial oil-shale operations processing large volumes of shale. Using an improved analytical method, surface samples from eastern Utah previously reported to contain high concentrations of mercury were reanalyzed, and an additional 183 drill core samples from the Mahogany zone and adjacent beds were analyzed. The reanalyzed samples averaged slightly more than 0.35 ppm mercury and the drill-core samples averaged 0.37 ppm. The products from a Fischer assay of 100-gram sample of oil shale, found to yield 35 gallons pier ton of oil and 43 ppm of mercury, were analyzed for their mercury content. The spent shale contained only 2 percent of the total mercury in the assay products and the gas fraction contained about 58 percent. </p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Donnell, J., and Shaw, V.E., 1977, Mercury in oil shale from the mahogany zone of the Green River formation, eastern Utah and western Colorado: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 221-226.","productDescription":"6 p.","startPage":"221","endPage":"226","costCenters":[],"links":[{"id":403821,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403820,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Green River Formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.7314453125,\n              39.29179704377487\n            ],\n            [\n              -107.3638916015625,\n              39.29179704377487\n            ],\n            [\n              -107.3638916015625,\n              41.025499378313754\n            ],\n            [\n              -109.7314453125,\n              41.025499378313754\n            ],\n            [\n              -109.7314453125,\n              39.29179704377487\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Donnell, John R.","contributorId":84330,"corporation":false,"usgs":true,"family":"Donnell","given":"John R.","affiliations":[],"preferred":false,"id":846685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaw, Van E.","contributorId":146896,"corporation":false,"usgs":true,"family":"Shaw","given":"Van","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":846686,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70232982,"text":"70232982 - 1977 - Land use and land cover changes: A framework for monitoring","interactions":[],"lastModifiedDate":"2022-07-14T15:46:14.365889","indexId":"70232982","displayToPublicDate":"1977-03-01T10:40:44","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Land use and land cover changes: A framework for monitoring","docAbstract":"<p>Information on the rate and kind of change in the use of land resources is essential to-the proper planning, management, and regulation of the use of such resources. Starting in 1975, the U.S. Geological Survey has been engaged in mapping and inventory of land use and land cover at a scale of 1:250000 with plans to change to new 1:100000 base maps as they become available. Such scales are-appropriate for acquiring benchmark or baseline data on land use and land cover on a nationwide basis with a reasonable degree of standardization and accuracy, within a practical time frame of 6 to 7 years, and at a reasonable level of detail in categorization. Changes in land use and land cover occur at highly variable rates from place to place. Thus variations, in the intervals between updates of land use and land cover data should be carefully evaluated in order to provide an appropriate frame of reference for the systematic updating of such data. A methodological framework is needed for monitoring changes in land use and land cover that will be timely, relatively inexpensive, and appropriate for widely varying needs at national, interstate-regional, state, multicounty, county, and city levels. In this article a partial framework for monitoring land use and land cover changes is provided with opportunity to extend its use to greater levels of detail in categorization and shorter intervals of frequency when needed for selected areas.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Anderson, J.R., 1977, Land use and land cover changes: A framework for monitoring: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 143-153.","productDescription":"11 p.","startPage":"143","endPage":"153","costCenters":[],"links":[{"id":403766,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403765,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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States\"}}]}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Anderson, James R.","contributorId":20213,"corporation":false,"usgs":true,"family":"Anderson","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":846613,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70233061,"text":"70233061 - 1977 - Blades of olivine in ultramafic rock from northern Sierra Nevada, California","interactions":[],"lastModifiedDate":"2022-07-15T16:05:59.833213","indexId":"70233061","displayToPublicDate":"1977-03-01T10:37:53","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Blades of olivine in ultramafic rock from northern Sierra Nevada, California","docAbstract":"<p>Blades of olivine in random arrangement crystallized in a small body of serpentine just north of the Grizzly pluton as a result of contact metamorphism. Interstitial minerals are talc, chlorite, and minor amount of cummingtonite.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Hietanen, A., 1977, Blades of olivine in ultramafic rock from northern Sierra Nevada, California: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 217-219.","productDescription":"3 p.","startPage":"217","endPage":"219","costCenters":[],"links":[{"id":403818,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403809,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Rock Creek, Sierra Nevada, Spring Valley Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.41875267028809,\n              39.989549903780365\n            ],\n            [\n              -121.35764122009277,\n              39.989549903780365\n            ],\n            [\n              -121.35764122009277,\n              40.01525729596965\n            ],\n            [\n              -121.41875267028809,\n              40.01525729596965\n            ],\n            [\n              -121.41875267028809,\n              39.989549903780365\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hietanen, Anna","contributorId":43841,"corporation":false,"usgs":true,"family":"Hietanen","given":"Anna","affiliations":[],"preferred":false,"id":846679,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70233059,"text":"70233059 - 1977 - Pleistocene fishes from Alameda County, California","interactions":[],"lastModifiedDate":"2022-07-15T15:36:36.362775","indexId":"70233059","displayToPublicDate":"1977-03-01T10:27:50","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Pleistocene fishes from Alameda County, California","docAbstract":"<p> Six types of freshwater fishes were recovered from an early Pleistocene (Irvingtonian) locality on the east side of San Francisco Bay, Alameda County, Calif. The fauna includes one centrarchid, one salmonid, three cyprinids, and one catostomid. The fauna indicates fluvial and slow-moving or lacustrine aquatic environments. One of the cyprinids and the catostomid are assigned to provisional genera because of the inadequate amount of material available for study and the obvious differences between these fossils and known fossil or recent fishes. They are new additions to the Pleistocene fish fauna of California. Paleogeographic distribution of some of these fishes indicates former fluvial or lacustrine connections between Utah, Idaho, Oregon, Washington, Nevada, and California. The Pliocene and Pleistocene fossil fish faunas indicate the widespread occurrence of genera now endemic to California. A similar picture is presented by the molluscan evidence. </p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Casteel, R.W., and Adam, D.P., 1977, Pleistocene fishes from Alameda County, California: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 209-215.","productDescription":"7 p.","startPage":"209","endPage":"215","costCenters":[],"links":[{"id":403806,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403805,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Alameda 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Richard W.","contributorId":28241,"corporation":false,"usgs":true,"family":"Casteel","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":846674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adam, David P.","contributorId":36132,"corporation":false,"usgs":true,"family":"Adam","given":"David","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":846675,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70233055,"text":"70233055 - 1977 - Electrical soundings near Yellow Creek, Rio Blanco County, Colorado","interactions":[],"lastModifiedDate":"2022-07-15T15:24:19.929894","indexId":"70233055","displayToPublicDate":"1977-03-01T10:15:21","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Electrical soundings near Yellow Creek, Rio Blanco County, Colorado","docAbstract":"<p>Ten vertical electrical soundings were made in the Piceance Creek Basin in October 1974-5 along Yellow Creek, 2 in Big Duck Creek, and 1 each along Corral Gulch, on the hill in sec. 20, 1 kilometre northwest of 84 Ranch, and along the White River between the mouths of Yellow and Piceance Creeks. Interpretations of these soundings indicate that the anisotropy of the upper oil shales decreases from 2 in the basin center to 1 at a location on its flank. This decrease could result from a greater number of vertical water-filled fractures in the upper shales near the edge of the basin. On the other hand, the anisotropy coefficient for the lower shales increases from 2 to around 9 along the same section, indicating the presence of an increasing number of isolated horizontal aquifers in the lower shales on the basin flank. It is speculated that this trend for the lower shales reverses nearer the basin edge in the area of recharge of these splintered horizontal aquifers.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Campbell, D.L., 1977, Electrical soundings near Yellow Creek, Rio Blanco County, Colorado: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 193-205.","productDescription":"13 p.","startPage":"193","endPage":"205","costCenters":[],"links":[{"id":403804,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403803,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Rio Blanco County","otherGeospatial":"Yellow Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.74542236328125,\n              39.6437675734185\n            ],\n            [\n              -108.18923950195312,\n              39.6437675734185\n            ],\n            [\n              -108.18923950195312,\n              40.23026664265011\n            ],\n            [\n              -108.74542236328125,\n              40.23026664265011\n            ],\n            [\n              -108.74542236328125,\n              39.6437675734185\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Campbell, David L.","contributorId":95447,"corporation":false,"usgs":true,"family":"Campbell","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":846673,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70233051,"text":"70233051 - 1977 - Geology and Rb-Sr age of Precambrian W Puritan Quartz Monzonite, northern Michigan","interactions":[],"lastModifiedDate":"2022-07-15T15:13:40.019423","indexId":"70233051","displayToPublicDate":"1977-03-01T10:01:07","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Geology and Rb-Sr age of Precambrian W Puritan Quartz Monzonite, northern Michigan","docAbstract":"<p>The Puritan Quartz Monzonite, in the western part of the Upper Peninsula of Michigan, composes a batholith at least 50 kilometres long and as much as 20 km wide on the south side of the Gogebic iron range. It is associated with subaqueous metavolcanic rocks assigned to the Precambrian W Ramsey Formation and with a complex gneissic unit of the same age. The quartz monzonite has a Rb-Sr isochron age of 2,710±140 million years and an initial <sup>87</sup>Sr/<sup>86</sup>Sr of 0.7015±0.0017. The scatter of data points in excess of analytical error is interpreted as indicating that minor cataclasis and retrograde metamorphism produced slight open-system behavior in Precambrian X (circa 1,800 m.y.) time. The Puritan Quartz Monzonite and associated volcanic rocks are equated with similar Precambrian W greenstone-granite complexes in northern Minnesota, and clearly are a part of the Precambrian W greenstone terrane, as defined previously for the Lake Superior region.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Sims, P., Peterman, Z.E., and Prinz, W.C., 1977, Geology and Rb-Sr age of Precambrian W Puritan Quartz Monzonite, northern Michigan: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 185-192.","productDescription":"8 p.","startPage":"185","endPage":"192","costCenters":[],"links":[{"id":403801,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403800,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan, Wisconsin","otherGeospatial":"Gogebic iron range, Lake Gogebic, Upper Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.53994750976562,\n              46.40093514439044\n            ],\n            [\n              -89.5111083984375,\n              46.44069599413034\n            ],\n            [\n              -89.52621459960938,\n              46.49082901981415\n            ],\n            [\n              -89.59075927734375,\n              46.5635815342227\n            ],\n            [\n              -89.53445434570312,\n              46.580574564531695\n            ],\n            [\n              -89.53994750976562,\n              46.60228013300284\n            ],\n            [\n              -89.89700317382812,\n              46.76620587423741\n            ],\n            [\n              -89.9945068359375,\n              46.707852594536355\n            ],\n            [\n              -90.03570556640624,\n              46.677710064644344\n            ],\n            [\n              -90.21560668945311,\n              46.638122462379656\n            ],\n            [\n              -90.30624389648438,\n              46.6088844501943\n            ],\n            [\n              -90.3350830078125,\n              46.612657984230204\n            ],\n            [\n              -90.42022705078125,\n              46.565469911631475\n            ],\n            [\n              -90.41473388671875,\n              46.34123949998618\n            ],\n            [\n              -90.11672973632812,\n              46.334602622976156\n            ],\n            [\n              -89.54544067382812,\n              46.22735299655779\n            ],\n            [\n              -89.53994750976562,\n              46.40093514439044\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":846670,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterman, Zell E. 0000-0002-5694-8082 peterman@usgs.gov","orcid":"https://orcid.org/0000-0002-5694-8082","contributorId":167699,"corporation":false,"usgs":true,"family":"Peterman","given":"Zell","email":"peterman@usgs.gov","middleInitial":"E.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":846671,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prinz, W. C.","contributorId":82670,"corporation":false,"usgs":true,"family":"Prinz","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":846672,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70233046,"text":"70233046 - 1977 - Metamorphic rocks of the Yakutat-St. Elias area, south-central Alaska","interactions":[],"lastModifiedDate":"2022-07-15T14:59:28.258206","indexId":"70233046","displayToPublicDate":"1977-03-01T09:51:22","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Metamorphic rocks of the Yakutat-St. Elias area, south-central Alaska","docAbstract":"<p>Metamorphic rocks in the Yakutat-St. Elias area range in grade from zeolite to amphibolite facies. Radiometric age determinations on selected metamorphic rocks have helped to identify two major metamorphic events, one in Late Cretaceous time that was characterized by penetrative deformation, and one in the Miocene Epoch that resulted in widespread recrystallization and igneous intrusions. Mapped facies units show many discontinuities across major faults, and their distribution indicates major differential uplift between several structurally bound crustal blocks within a strongly deformed mobile belt west of the Art Lewis fault. Late Cretaceous metamorphic gradients indicate that the blocks have been tilted to the west or northwest parallel to their general structural grain. As mineral assemblages that were recrystallized during Miocene time occur on both sides of the Fairweather fault, large-scale, post-Miocene strike-slip movement along the fault is not indicated.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Hudson, T., Plafker, G., and Turner, D.L., 1977, Metamorphic rocks of the Yakutat-St. Elias area, south-central Alaska: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 173-184.","productDescription":"12 p.","startPage":"173","endPage":"184","costCenters":[],"links":[{"id":403799,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403797,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"St. Elias, Yakutat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -141.0205078125,\n              60.32150850738404\n            ],\n            [\n              -141.13037109375,\n              59.772991625706695\n            ],\n            [\n              -140.745849609375,\n              59.701013531997326\n            ],\n            [\n              -140.3173828125,\n              59.68438118751815\n            ],\n            [\n              -139.74609375,\n              59.81168490365651\n            ],\n            [\n              -139.74609375,\n              59.85033331585688\n            ],\n            [\n              -139.70214843749997,\n              59.9054675732672\n            ],\n            [\n              -139.6142578125,\n              59.7619281579702\n            ],\n            [\n              -139.647216796875,\n              59.62332522313024\n            ],\n            [\n              -139.76806640625,\n              59.567723306212955\n            ],\n            [\n              -139.866943359375,\n              59.52317553544798\n            ],\n            [\n              -139.306640625,\n              59.338792483494494\n            ],\n            [\n              -138.746337890625,\n              59.147769484619786\n            ],\n            [\n              -138.482666015625,\n              59.085738569819505\n            ],\n            [\n              -137.999267578125,\n              58.90464570302001\n            ],\n            [\n              -137.999267578125,\n              59.439489583059725\n            ],\n            [\n              -138.66943359375,\n              59.81168490365651\n            ],\n            [\n              -138.702392578125,\n              59.91097597079679\n            ],\n            [\n              -139.075927734375,\n              60.01546201341472\n            ],\n            [\n              -139.19677734375,\n              60.10319489936693\n            ],\n            [\n              -139.06494140625,\n              60.354130331374286\n            ],\n            [\n              -139.70214843749997,\n              60.343260013555195\n            ],\n            [\n              -139.98779296875,\n              60.19615576604439\n            ],\n            [\n              -140.47119140625,\n              60.32150850738404\n            ],\n            [\n              -140.537109375,\n              60.23435742267943\n            ],\n            [\n              -141.0205078125,\n              60.32150850738404\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hudson, Travis","contributorId":90282,"corporation":false,"usgs":true,"family":"Hudson","given":"Travis","affiliations":[],"preferred":false,"id":846666,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":846667,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turner, Donald L.","contributorId":11604,"corporation":false,"usgs":true,"family":"Turner","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":846668,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70233036,"text":"70233036 - 1977 - Intrusive rocks of the Yakutat-St. Elias area, south-central Alaska","interactions":[],"lastModifiedDate":"2022-07-15T14:35:17.066585","indexId":"70233036","displayToPublicDate":"1977-03-01T09:23:16","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Intrusive rocks of the Yakutat-St. Elias area, south-central Alaska","docAbstract":"<p>Twenty-three plutons, exposed over a total area of nearly 1200 km<sup>2</sup>, have been studied in the Alaska part of the St. Elias Mountains between long 138° and 141°W. Results of potassium-argon age determinations combined with field relations, petrography, and major- and trace-element chemistry suggest six major intrusive events: (1) late Paleozoic gabbro to quartz diorite intruded Paleozoic metamorphic rocks that are probably equivalent to the Kaskawulsh Group in adjacent areas of Canada, (2) Triassic quartz diorite formed one small pluton in undated metamorphic rocks near Mt. St. Elias, (3) Jurassic tonalite and granite intruded upper Paleozoic(?) and lower Mesozoic(?) metamorphic rocks, (4) Late Cretaceous or Tertiary altered tonalite formed three widely separated plutons in metasedimentary rocks of Jurassic(?) and Cretaceous age in the Yakutat Group, (5) Eocene granodiorite and granite, and (6) late Cenozoic tonalite and granodiorite intruded both the Yakutat Group and upper Paleozoic(?) and lower Mesozoic(?) metamorphic rocks. The Paleozoic, Jurassic, and Cretaceous or Tertiary plutonic suites are restricted to particular geologic terranes, and the Jurassic and Eocene suites correlate with regional plutonic belts present elsewhere in southern Alaska. The distribution of the Tertiary plutons does not require large-scale horizontal displacements along the Fairweather and other major high-angle faults. The available data indicate that the mineral resource potential of the Yakutat-St. Elias area is low for those deposits that are generally related to magmatic processes. </p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Hudson, T., Plafker, G., and Lanphere, M.A., 1977, Intrusive rocks of the Yakutat-St. Elias area, south-central Alaska: Journal of Research of the U.S. Geological Survey, v. 5, no. 2, p. 155-172.","productDescription":"18 p.","startPage":"155","endPage":"172","costCenters":[],"links":[{"id":403791,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403789,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue2/report.pdf","size":"18181 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"St. Elias, Yakutat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -141.0205078125,\n              60.32150850738404\n            ],\n            [\n              -141.13037109375,\n              59.772991625706695\n            ],\n            [\n              -140.745849609375,\n              59.701013531997326\n            ],\n            [\n              -140.3173828125,\n              59.68438118751815\n            ],\n            [\n              -139.74609375,\n              59.81168490365651\n            ],\n            [\n              -139.74609375,\n              59.85033331585688\n            ],\n            [\n              -139.70214843749997,\n              59.9054675732672\n            ],\n            [\n              -139.6142578125,\n              59.7619281579702\n            ],\n            [\n              -139.647216796875,\n              59.62332522313024\n            ],\n            [\n              -139.76806640625,\n              59.567723306212955\n            ],\n            [\n              -139.866943359375,\n              59.52317553544798\n            ],\n            [\n              -139.306640625,\n              59.338792483494494\n            ],\n            [\n              -138.746337890625,\n              59.147769484619786\n            ],\n            [\n              -138.482666015625,\n              59.085738569819505\n            ],\n            [\n              -137.999267578125,\n              58.90464570302001\n            ],\n            [\n              -137.999267578125,\n              59.439489583059725\n            ],\n            [\n              -138.66943359375,\n              59.81168490365651\n            ],\n            [\n              -138.702392578125,\n              59.91097597079679\n            ],\n            [\n              -139.075927734375,\n              60.01546201341472\n            ],\n            [\n              -139.19677734375,\n              60.10319489936693\n            ],\n            [\n              -139.06494140625,\n              60.354130331374286\n            ],\n            [\n              -139.70214843749997,\n              60.343260013555195\n            ],\n            [\n              -139.98779296875,\n              60.19615576604439\n            ],\n            [\n              -140.47119140625,\n              60.32150850738404\n            ],\n            [\n              -140.537109375,\n              60.23435742267943\n            ],\n            [\n              -141.0205078125,\n              60.32150850738404\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hudson, Travis","contributorId":90282,"corporation":false,"usgs":true,"family":"Hudson","given":"Travis","affiliations":[],"preferred":false,"id":846657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":846658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lanphere, Marvin A. alder@usgs.gov","contributorId":2696,"corporation":false,"usgs":true,"family":"Lanphere","given":"Marvin","email":"alder@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":846659,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70009955,"text":"70009955 - 1977 - Delaware River: Evidence for its former extension to Wilmington Submarine Canyon","interactions":[],"lastModifiedDate":"2026-01-16T16:29:17.544502","indexId":"70009955","displayToPublicDate":"1977-02-04T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Delaware River: Evidence for its former extension to Wilmington Submarine Canyon","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>Seismic-reflection profiles indicate that during the Pleistocene the Delaware River flowed across the continental shelf east of Delaware Bay and emptied into Wilmington Submarine Canyon. The ancestral valley (width, 3 to 8 kilometers; relief, 10 to 30 meters) is buried, is not reflected in the surface topography, and probably predates the formation of the present canyon head.</span></span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.195.4277.483","issn":"00368075","usgsCitation":"Twichell, D., Knebel, H., and Folger, D.W., 1977, Delaware River: Evidence for its former extension to Wilmington Submarine Canyon: Science, v. 195, no. 4277, p. 483-485, https://doi.org/10.1126/science.195.4277.483.","productDescription":"3 p.","startPage":"483","endPage":"485","costCenters":[],"links":[{"id":219204,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Delaware","otherGeospatial":"Delaware Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.77418738436643,\n              39.7369030436918\n            ],\n            [\n              -75.77418738436643,\n              38.43058282173703\n            ],\n            [\n              -74.88970281894306,\n              38.43058282173703\n            ],\n            [\n              -74.88970281894306,\n              39.7369030436918\n            ],\n            [\n              -75.77418738436643,\n              39.7369030436918\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"195","issue":"4277","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe5be4b0c8380cd4ecc6","contributors":{"authors":[{"text":"Twichell, D.C.","contributorId":84304,"corporation":false,"usgs":true,"family":"Twichell","given":"D.C.","affiliations":[],"preferred":false,"id":357520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knebel, H.J.","contributorId":79092,"corporation":false,"usgs":true,"family":"Knebel","given":"H.J.","affiliations":[],"preferred":false,"id":357519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Folger, D. W.","contributorId":97126,"corporation":false,"usgs":true,"family":"Folger","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":357521,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70233962,"text":"70233962 - 1977 - Reflection and refraction of type-II S waves in elastic and anelastic media","interactions":[],"lastModifiedDate":"2022-07-28T13:33:48.462327","indexId":"70233962","displayToPublicDate":"1977-02-01T08:29:23","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7571,"text":"Bulletin of Seismological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Reflection and refraction of type-II S waves in elastic and anelastic media","docAbstract":"<p>The general theory of viscoelasticity, which accounts for elastic as well as anelastic linear behavior of materials, predicts that two types of&nbsp;<i>S</i>&nbsp;waves propagate in anelastic earth materials. The particle motion for an inhomogeneous plane&nbsp;<i>S</i>&nbsp;wave of type I is elliptical in the plane defined by the directions of propagation and attenuation, while the particle motion for an inhomogeneous plane&nbsp;<i>S</i>&nbsp;wave of type II is linear perpendicular to this plane. The general theory predicts that an&nbsp;<i>S</i>-wave incident upon a plane boundary perpendicular to the plane defined by the directions of propagation and attenuation generates&nbsp;<i>S</i>&nbsp;waves only of the same type. General characteristics of the type-II&nbsp;<i>S</i> waves reflected and refracted at plane anelastic boundaries are:</p><p>(a) velocities and maximum attenuations which depend on the angle of incidence and frequency,</p><p>(b) maximum energy flow at a different velocity and in a different direction than phase propagation,</p><p>(c) energy flow across the boundary due to interaction of the incident and reflected waves.</p><p>The general theory predicts these characteristics for the waves whenever a plane type-II&nbsp;<i>S</i>&nbsp;wave interacts with a plane anelastic boundary such as a soil-bedrock, crust-mantle, or core-mantle interface. None of these characteristics are predicted for the plane&nbsp;<i>SH</i>&nbsp;waves described by elasticity theory.</p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/BSSA0670010043","usgsCitation":"Borcherdt, R.D., 1977, Reflection and refraction of type-II S waves in elastic and anelastic media: Bulletin of Seismological Society of America, v. 67, no. 1, p. 43-67, https://doi.org/10.1785/BSSA0670010043.","productDescription":"25 p.","startPage":"43","endPage":"67","costCenters":[],"links":[{"id":404537,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"1","noUsgsAuthors":false,"publicationDate":"1977-02-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Borcherdt, Roger D. 0000-0002-8668-0849 borcherdt@usgs.gov","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":2373,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Roger","email":"borcherdt@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":847753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014096,"text":"1014096 - 1977 - A new host for Pleistophora ovariae (Microsporida)","interactions":[],"lastModifiedDate":"2025-04-30T16:46:00.307974","indexId":"1014096","displayToPublicDate":"1977-02-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2414,"text":"Journal of Parasitology","active":true,"publicationSubtype":{"id":10}},"title":"A new host for Pleistophora ovariae (Microsporida)","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Allen Press","doi":"10.2307/3280131","usgsCitation":"Nagel, M., and Hoffman, G.L., 1977, A new host for Pleistophora ovariae (Microsporida): Journal of Parasitology, v. 63, no. 1, p. 160-162, https://doi.org/10.2307/3280131.","productDescription":"3 p.","startPage":"160","endPage":"162","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129579,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -93.71886924701124,\n              38.21707405441765\n            ],\n            [\n              -93.71886924701124,\n              38.01677745033331\n            ],\n            [\n              -93.22851637945013,\n              38.116981579409384\n            ],\n            [\n              -92.60145591442377,\n              38.01677745033331\n            ],\n            [\n              -92.60145591442377,\n              38.21707405441765\n            ],\n            [\n              -93.1719550805126,\n              38.29853798647787\n            ],\n            [\n              -93.71886924701124,\n              38.21707405441765\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -94.60877016070945,\n              36.49683346433352\n            ],\n            [\n              -94.46299084589886,\n              35.31175006694599\n            ],\n            [\n              -94.60877016070945,\n              32.97770683603406\n            ],\n            [\n              -91.03596143698991,\n              32.98536507540483\n            ],\n            [\n              -90.79442609239385,\n              33.9672727871569\n            ],\n            [\n              -90.06981486394116,\n              35.30430729339946\n            ],\n            [\n              -89.75080285062971,\n              35.99297747345833\n            ],\n            [\n              -90.3751487519523,\n              36.02777812812913\n            ],\n            [\n              -90.10626391024843,\n              36.460196165165016\n            ],\n            [\n              -94.60877016070945,\n              36.49683346433352\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"63","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6ac142","contributors":{"authors":[{"text":"Nagel, M.L.","contributorId":56181,"corporation":false,"usgs":true,"family":"Nagel","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":319780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319781,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207916,"text":"70207916 - 1977 - Composition and phase chemistry of sulfide globules in basalt from the Mid-Atlantic Ridge rift valley near 37°N lat","interactions":[],"lastModifiedDate":"2020-01-20T11:36:05","indexId":"70207916","displayToPublicDate":"1977-01-20T11:26:42","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Composition and phase chemistry of sulfide globules in basalt from the Mid-Atlantic Ridge rift valley near 37°N lat","docAbstract":"<p>The electron microprobe was used to determine the bulk composition of immiscible sulfide globules trapped in the glass phase of 25 fresh submarine basalt samples from the Mid-Atlantic Ridge. Twenty-three samples represent a spectrum of primitive through differentiated tholeiites from the FAMOUS dive area; two are differentiated basalts from the Reykjanes Ridge. The analyzed globules range in diameter from 11 to 233 µm. On the average, they constitute only 0.0022 volume percent of the rocks and contain less than 1.5 percent of the sulfur. Compositions of the globules change with differentiation as measured by Fe/(Fe+Mg) or TiO<sub>2</sub><span>&nbsp;</span>content of the host glass. Globules in glass containing 0.66 to 1.0 wt percent TiO<sub>2</sub><span>&nbsp;</span>typically contain 20 to 26 wt percent Ni + Cu and have an average atomic Ni/Cu of 1.6. With differentiation toward 1.6 wt percent TiO<sub>2</sub>, Ni + Cu content of the globules falls to less than 10 wt percent and atomic Ni/Cu falls to 0.4.</p><p>Sulfur content of the host glasses shows a strong correlation with FeO content, increasing from 840 ppm to 1,370 ppm as FeO content increases from 8.0 to 12.6 wt percent. Reference to experimental studies shows that this relationship is consistent with sulfur saturation of the host glass at liquidus temperatures. Crystal fractionation is considered to be the dominant factor in keeping the differentiating melt at sulfur saturation.</p><p>The sulfide globules may have persisted in the basaltic melt from its place of formation by partial melting in the mantle, or they may have exsolved from the melt as it became sulfur-saturated in a high-level magma chamber. Globule abundance and composition indicate adjustment to the composition of the melt in which they were trapped. Material balance calculations suggest that one-third of the Cu and commensurate amounts of S, Ni, and Fe have settled from the magma as immiscible globules.</p><p>The sulfide globules contain less than 4 wt percent magnetite, compatible with low f<sub>o2</sub><span>&nbsp;</span>in the magma. Three sulfide phases coexisted in the globules at about 600 °C: monosulfide solid solution, intermediate solid solution, and pentlandite. At lower temperatures, the intermediate solid solution has broken down, and the monosulfide solid solution has exsolved a second generation of pentlandite.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1977)88<587:CAPCOS>2.0.CO;2","usgsCitation":"Czamanske, G., and Moore, J.G., 1977, Composition and phase chemistry of sulfide globules in basalt from the Mid-Atlantic Ridge rift valley near 37°N lat: GSA Bulletin, v. 88, no. 4, p. 587-599, https://doi.org/10.1130/0016-7606(1977)88<587:CAPCOS>2.0.CO;2.","productDescription":"13 p.","startPage":"587","endPage":"599","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":371371,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mid-Atlantic Ridge rift valley near 37°N lat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -44.736328125,\n              29.22889003019423\n            ],\n            [\n              -30.322265625000004,\n              29.22889003019423\n            ],\n            [\n              -30.322265625000004,\n              35.31736632923788\n            ],\n            [\n              -44.736328125,\n              35.31736632923788\n            ],\n            [\n              -44.736328125,\n              29.22889003019423\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"88","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Czamanske, G.","contributorId":61185,"corporation":false,"usgs":true,"family":"Czamanske","given":"G.","affiliations":[],"preferred":false,"id":779770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, James G. 0000-0002-7543-2401 jmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-7543-2401","contributorId":2892,"corporation":false,"usgs":true,"family":"Moore","given":"James","email":"jmoore@usgs.gov","middleInitial":"G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":779771,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207915,"text":"70207915 - 1977 - Compositional variations of young basalts in the Mid-Atlantic Ridge rift valley near lat 36°49′N","interactions":[],"lastModifiedDate":"2020-01-20T11:25:57","indexId":"70207915","displayToPublicDate":"1977-01-20T11:08:30","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Compositional variations of young basalts in the Mid-Atlantic Ridge rift valley near lat 36°49′N","docAbstract":"<p>Fifty acoustically positioned samples of fresh basalt were collected by the submersible<span>&nbsp;</span><i>Alvin</i><span>&nbsp;</span>from the median valley of the Mid-Atlantic Ridge during the French American Mid-Ocean Undersea Study (FAMOUS) in the summer of 1974. The samples show regular compositional variations from the center of the rift valley (central lava flows) out to the rift valley walls (flank lava flows). The central lava samples show higher ratios of olivine relative to clinopyroxene and plagioclase phenocrysts and contain chrome spinel. Glasses of the flank lava samples are enriched in SiO<sub>2</sub>, TiO<sub>2</sub>, K<sub>2</sub>O, H<sub>2</sub>O, and FeO/MgO relative to central lava samples.</p><p>Studies of the thickness of palagonite and manganese crusts indicate that the flank lava flows are considerably younger than the inferred spreading age of the crust on which they occur. Flank lavas are generally older than central lavas, but notable exceptions occur.</p><p>The composition of the flank lava glass can be derived by the removal of approximately 29 wt percent of analyzed phenocrysts (in the ratio 5.7 plagioclase, 2.5 olivine, 1.8 clinopyroxene) from the central lava glass. In addition, other processes (possibly involving volatile transfer) must enrich the flank lavas in K<sub>2</sub>O, TiO<sub>2</sub>, and H<sub>2</sub>O.</p><p>A model is proposed whereby this crystal fractionation occurs in a shallow, narrow (6-km-wide) magma chamber underlying the median valley. The chamber is compositionally zoned, and central lavas are fed from dikes tapping its hotter axial zone, whereas flank lavas are fed from the cooler, differentiated melt on the margins. The nature of the chemical variations in the lavas permits an estimate of the composition and thickness of the cumulates forming at the base of the chamber.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1977)88<556:CVOYBI>2.0.CO;2","usgsCitation":"Bryan, W., and Moore, J.G., 1977, Compositional variations of young basalts in the Mid-Atlantic Ridge rift valley near lat 36°49′N: GSA Bulletin, v. 88, no. 4, p. 556-570, https://doi.org/10.1130/0016-7606(1977)88<556:CVOYBI>2.0.CO;2.","productDescription":"15 p.","startPage":"556","endPage":"570","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":371370,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mid-Atlantic Ridge rift valley near lat 36°49′N","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -44.736328125,\n              29.22889003019423\n            ],\n            [\n              -30.322265625000004,\n              29.22889003019423\n            ],\n            [\n              -30.322265625000004,\n              35.31736632923788\n            ],\n            [\n              -44.736328125,\n              35.31736632923788\n            ],\n            [\n              -44.736328125,\n              29.22889003019423\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"88","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bryan, W.B.","contributorId":100412,"corporation":false,"usgs":true,"family":"Bryan","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":779768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, James G. 0000-0002-7543-2401 jmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-7543-2401","contributorId":2892,"corporation":false,"usgs":true,"family":"Moore","given":"James","email":"jmoore@usgs.gov","middleInitial":"G.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":779769,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207883,"text":"70207883 - 1977 - Sheeted dikes, gabbro, and pillow basalt in flysch of coastal southern Alaska","interactions":[],"lastModifiedDate":"2020-01-16T14:02:08","indexId":"70207883","displayToPublicDate":"1977-01-16T13:56:49","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sheeted dikes, gabbro, and pillow basalt in flysch of coastal southern Alaska","docAbstract":"<p><span>A Paleocene to Eocene(?) mafic sequence of igneous rocks on Knight Island and a Cretaceous mafic and ultramafic sequence of the Resurrection Peninsula in coastal southern Alaska are characterized by pillow basalts, sheeted dikes, and gabbro intrusions. At both localities, pillow basalts are interbedded with flysch, and the gabbros intrude both the sheeted dikes and the immediately overlying sedimentary rocks. At the Resurrection Peninsula, small bodies of serpentinized dunite are present in the gabbro, and overlying low-grade metasedimentary rocks and mafic tuffs are interbedded with sedimentary rocks. At Knight Island the sheeted dikes intrude Paleocene and Eocene(?) sedimentary rocks. These igneous rocks have petrographic features similar to those of oceanic tholeiites and have some of the characteristics of ophiolites. They apparently were formed near the continental margin, because both sequences intrude and are interlayered with flysch. We believe the igneous rocks were intruded along faults (perhaps leaky transform faults) of ocean floor that happened to be near the continental margin; the faults were oriented parallel to the depositional strike and subsequent deformational strike of the Valdez(?) and Orca Groups.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0091-7613(1977)5<377:SDGAPB>2.0.CO;2","usgsCitation":"Tysdal, R.G., Case, J.E., Winkler, G.R., and Clark, S.H., 1977, Sheeted dikes, gabbro, and pillow basalt in flysch of coastal southern Alaska: Geology, v. 5, no. 6, p. 377-383, https://doi.org/10.1130/0091-7613(1977)5<377:SDGAPB>2.0.CO;2.","productDescription":"7 p.","startPage":"377","endPage":"383","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":371320,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Coastal southern Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -154.86328125,\n              55.87531083569679\n            ],\n            [\n              -143.61328125,\n              55.87531083569679\n            ],\n            [\n              -143.61328125,\n              62.02152819100765\n            ],\n            [\n              -154.86328125,\n              62.02152819100765\n            ],\n            [\n              -154.86328125,\n              55.87531083569679\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Tysdal, Russell G.","contributorId":1700,"corporation":false,"usgs":true,"family":"Tysdal","given":"Russell","email":"","middleInitial":"G.","affiliations":[],"preferred":true,"id":779628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Case, J. E.","contributorId":56625,"corporation":false,"usgs":true,"family":"Case","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":779629,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winkler, G. R.","contributorId":17964,"corporation":false,"usgs":true,"family":"Winkler","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":779630,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clark, S. H. B.","contributorId":95052,"corporation":false,"usgs":true,"family":"Clark","given":"S.","email":"","middleInitial":"H. B.","affiliations":[],"preferred":false,"id":779631,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70207857,"text":"70207857 - 1977 - Mechanical twinning in diopside Ca(Mg,Fe)Si2O6: Structural mechanism and associated crystal defects","interactions":[],"lastModifiedDate":"2020-07-09T15:44:07.275704","indexId":"70207857","displayToPublicDate":"1977-01-15T16:48:14","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3066,"text":"Physics and Chemistry of Minerals","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Mechanical twinning in diopside Ca(Mg,Fe)Si<sub>2</sub>O<sub>6</sub>: Structural mechanism and associated crystal defects","title":"Mechanical twinning in diopside Ca(Mg,Fe)Si2O6: Structural mechanism and associated crystal defects","docAbstract":"<p>iopside twins mechanically on two planes, (100) and (001), and the associated macroscopic twinning strains are identical (Raleigh and Talbot, 1967). An analysis based on crystal structural arguments predicts that both twin mechanisms involve shearing of the (100) octahedral layers (containing Ca<sup>2+</sup>, Mg<sup>2+</sup><span>&nbsp;</span>and Fe<sup>2+</sup><span>&nbsp;</span>ions) by a magnitude of<span>&nbsp;</span><i>c</i>/2. Small adjustments or shuffles occur in the adjacent layers containing the [SiO<sub>4</sub>]<sup>4−</sup><span>&nbsp;</span>tetrahedral chains. While the (100) twins are conventional with shear parallel to the composition plane, this analysis predicts that (001) twins form by a mechanism closely related to kinking.</p><p>A polycrystalline diopside specimen was compressed 8% at a temperature of 400° C, a pressure of 16 kilobars, and a compressive strain rate of about 10<sup>−4</sup>/s. Transmission electron microscopy on this specimen has revealed four basic lamellar features:</p><ol class=\"u-list-style-none\"><li><span class=\"u-custom-list-number\">1)</span><p>(100) mechanical twin lamellae;</p></li><li><span class=\"u-custom-list-number\">2)</span><p>(100) glide bands containing unit dislocations;</p></li><li><span class=\"u-custom-list-number\">3)</span><p>(001) twin lamellae;</p></li><li><span class=\"u-custom-list-number\">4)</span><p>(101) lamellar features, not as yet identified.</p></li></ol><p>The (001) twins often contain remnant (100) lamellae of untwinned host. Twinning dislocations occur in these (100) lamellae and in the (001) twin boundaries with very high densities. Diffraction contrast experiments indicate that the twinning dislocations associated with both twin laws glide on (100) with Burgers vector<span>&nbsp;</span><strong>b</strong>=<i>X</i><span>&nbsp;</span>[001] where<span>&nbsp;</span><i>X</i><span>&nbsp;</span>is probably equal to 1/2 on the basis of the structural analysis.</p><p>Parallels are drawn between mechanical twinning in clinopyroxenes and clinoamphiboles. The exclusive natural occurrence of basal twins in shock-loaded clinopyroxenes and of analogous (<span class=\"mathjax-tex\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mrow class=&quot;MJX-TeXAtom-ORD&quot;><mover><mn>1</mn><mo stretchy=&quot;false&quot;>&amp;#x00AF;</mo></mover></mrow></math>\"><span id=\"MathJax-Span-1\" class=\"math\"><span><span id=\"MathJax-Span-2\" class=\"mrow\"><span id=\"MathJax-Span-3\" class=\"texatom\"><span id=\"MathJax-Span-4\" class=\"mrow\"><span id=\"MathJax-Span-5\" class=\"munderover\"><span id=\"MathJax-Span-6\" class=\"mn\">1</span><span id=\"MathJax-Span-7\" class=\"mo\">¯</span></span></span></span></span></span></span><span class=\"MJX_Assistive_MathML\">1¯</span></span></span>01) twins in clinoamphiboles is given a simple explanation in terms of the relative difficulty of the “kinking” mechanism as compared to direct glide parallel to the composition plane.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF00307315","usgsCitation":"Kirby, S.H., and Christie, J., 1977, Mechanical twinning in diopside Ca(Mg,Fe)Si2O6: Structural mechanism and associated crystal defects: Physics and Chemistry of Minerals, v. 1, p. 137-163, https://doi.org/10.1007/BF00307315.","productDescription":"27 p.","startPage":"137","endPage":"163","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":371286,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kirby, Stephen H. 0000-0003-1636-4688 skirby@usgs.gov","orcid":"https://orcid.org/0000-0003-1636-4688","contributorId":2752,"corporation":false,"usgs":true,"family":"Kirby","given":"Stephen","email":"skirby@usgs.gov","middleInitial":"H.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":779546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christie, J.M.","contributorId":21672,"corporation":false,"usgs":true,"family":"Christie","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":779547,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70198917,"text":"70198917 - 1977 - Geology of the Waynesboro East and Waynesboro West Quadrangles, Virginia","interactions":[],"lastModifiedDate":"2019-05-21T10:43:21","indexId":"70198917","displayToPublicDate":"1977-01-03T15:27:31","publicationYear":"1977","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Geology of the Waynesboro East and Waynesboro West Quadrangles, Virginia","docAbstract":"<p>The Waynesboro East and Waynesboro West Quadrangles comprise an area of approximately 117 square miles (304 sq km) in portions of Albemarle, Augusta, and Nelson counties in north-central Virginia. Included in the quadrangles are portions of the Piedmont, Blue Ridge, and Valley and Ridge physiographic provinces and two major regional structures - the Blue Ridge anticlinoriurm and the Massanutten synclinorium.</p><p>The rocks of the Blue Ridge anticlorium are complexly folded and faulted and consist of five sequences, the oldest being the Precambrian gneisses that include the Lovingston and Pedlar formations. Unconformably overlying these rocks or in fault contact with them is a sequence of Precambrian(?) stratified rock units including the metamorphosed, fluvial, sedimentary, and basic volcanic strata of the Swift Run and Catoctin formations. These are overlain by a sequence of Cambrian clastic rocks that include the Weverton, Harpers, and Antietarn formations. The Massanutten synclinorium within the study area is formed from the overlying Cambrian and Ordovician carbonate sequence that includes the Shady, Waynesboro, Elbrook, Conococheague, Chepultepec, Beekmantown, New Market, and Lincolnshire formations. These carbonate rocks are overlain by the Ordovician clastic sequence of the Martinsburg Formation. Many of these rock units are locally intruded by diabase dikes of Triassic age and are IocalIy covered by alluvial Quaternary sediments.</p><p>The intensity of deformation increases from northwest to southeast with recumbent folds, thrust faults, and zones of cataclastic rocks present in the southeastern half of the area. All of the rocks are altered with the metamorphic rank being somewhat greater to the southeast.</p><p>Sources of agricultural limestone, limestone aggregate, and in limited quantities high-calcium Iimestone are present. Ceramic clay, crushed stone. sand and gravel, and iron and manganese have been produced in small quantities.</p><p>Fourteen environmental geologic units having similar geologic factors - bedrock, residuum, and soil properties - affecting land modification have been delineated. Each is briefly evaluated with respect to slope stability, erodibility, and response to excavation or other types of land modification. Rockfall, karst. cave areas, and floodprone regions have been delineated.</p>","largerWorkTitle":"Virginia Division of Mineral Resources Publication","publisher":"Commonwealth of Virginia, Dept. of Conservation and Economic Development, Division of Mineral Resources","publisherLocation":"Charlottesville, VA","usgsCitation":"Gathright, T.M., Henika, W.S., and Sullivan, J.L., 1977, Geology of the Waynesboro East and Waynesboro West Quadrangles, Virginia, v. 3, 53 p.","productDescription":"53 p.","costCenters":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"links":[{"id":356748,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":356747,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.dmme.virginia.gov/commercedocs/PUB_3.pdf","text":"Document"}],"country":"United States","state":"Virginia","county":"Albemarle County, Augusta County, Nelson County","city":"Waynesboro","otherGeospatial":"Waynesboro East quadrangle, Waynesboro West Quadrangle","volume":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gathright, Thomas M. II","contributorId":207266,"corporation":false,"usgs":false,"family":"Gathright","given":"Thomas","suffix":"II","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":743415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henika, William S.","contributorId":178188,"corporation":false,"usgs":false,"family":"Henika","given":"William","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":743416,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sullivan, John L.","contributorId":207277,"corporation":false,"usgs":false,"family":"Sullivan","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":743417,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26246,"text":"wri7733 - 1977 - Saline-water intrusion related to well construction in Lee County, Florida","interactions":[],"lastModifiedDate":"2022-01-05T19:02:45.909337","indexId":"wri7733","displayToPublicDate":"1977-01-01T21:30:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-33","title":"Saline-water intrusion related to well construction in Lee County, Florida","docAbstract":"<p>Ground water is the principle source of water supply in Lee County, Florida where an estimated 30,000 wells have been drilled since 1990. These wells ranges in depth from about 10 to 1,240 feet and tap the water table aquifer or one or more of the artesian water-bearing units or zones in the Tamiami Formation, the upper part of the Hawthorn Formation, the lower part of the Hawthorn Formation and the Tampa Limestone and the Suwannee Limestone. Before 1968, nearly all wells were constructed with galvanized or black iron pipe. Many of these wells are sources of saline-water intrusion into freshwater-bearing zones.</p><p>The water-bearing zones in the lower part of the Hawthorn Formation, Tampa Limestone, and Suwannee Limestone are artesian-they have higher water levels and usually contain water with a higher concentration of dissolved solids than do the aquifers occurring at shallower depths. The water from these deeper aquifers generally range in dissolved solids concentration from about 1,500 to 2,400 mg/L, and in chloride from about 500 to 1,00 mg/L. A maximum chloride concentration of 15,200 mg/L has been determined. Few of the 3,00 wells estimated to have been drilled to these zones contain sufficient casing to prevent upward flow into overlaying water-bearing zones. Because of water-level differentials, upward movement and lateral intrusion of saline water occurs principally into the upper part of the Hawthorn Formation where the chloride concentrations in water unaffected by saline-water intrusion ranges from about 80 to 150 mg/L. Where intrusion from deep artesian zones has occurred, the chloride concentration in water from the upper part of the Hawthorn Formation ranges from about 300 to more than 2,100 mg/L.</p><p>Surface discharges of the saline water from wells tapping the lower part of the Hawthorn Formation and the Suwannee Limestone also had affected the water-table aquifer which normally contains water with 10 to 50 mg/L of chloride. In one area, the chloride concentration in water from the water table aquifer ranged from 200 to 590 mg/L as a result of intrusion.</p><p>In areas adjacent to tidal-water bodies, the water table aquifer contains water that is very saline, Where the wells in such areas have been constructed with metal casings, the metal corrodes when exposed to the saline water, and many ultimately develop holes. This permits saline water to leak into the well where the water level in the well is lower than the water table. The intrusion of saline water from the water-table aquifer into the upper part of the Hawthorn Formation is a major problem in parts of Cape Coral. Withdrawal of water from the upper part of the Hawthorn Formation has caused water levels to decline below the lowest annual position of the water table, so that downward leakage is perennial. In some coastal areas, wells that tap the upper part of the Hawthorn Formation contain water whose chloride concentration is as much as 9,500 mg/L.</p><p>Upward leakage of saline water from the deep artesian aquifers and downward leakage of saline water from the water-table aquifer can be prevented by proper well construction.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7733","collaboration":"Prepared in cooperation with the Board of County Commissioners of Lee County","usgsCitation":"Boggess, D.H., Missimer, T., and O’Donnell, T., 1977, Saline-water intrusion related to well construction in Lee County, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-33, iv, 29 p., https://doi.org/10.3133/wri7733.","productDescription":"iv, 29 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":157182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0033/coverthb.jpg"},{"id":1961,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0033/wri7733.pdf","text":"Report","size":"980 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Florida","county":"Lee 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href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c9a6","contributors":{"authors":[{"text":"Boggess, Durward Hoye","contributorId":13243,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"Hoye","affiliations":[],"preferred":false,"id":196053,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Missimer, T.M.","contributorId":41839,"corporation":false,"usgs":true,"family":"Missimer","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":196054,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Donnell, T.H.","contributorId":69970,"corporation":false,"usgs":true,"family":"O’Donnell","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":196055,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30043,"text":"wri7761 - 1977 - The effect of the Faka Union Canal system on water levels in the Fakahatchee Strand, Collier County, Florida","interactions":[],"lastModifiedDate":"2022-01-06T16:35:14.160273","indexId":"wri7761","displayToPublicDate":"1977-01-01T21:30:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-61","title":"The effect of the Faka Union Canal system on water levels in the Fakahatchee Strand, Collier County, Florida","docAbstract":"<p>The Faka Union Canal system, constructed in the western Big Cypress Swamp, Fla., in the early 1970's, lies about 3.5 miles west of the centerline of the Fakahatchee Strand, a forested water course which the State of Florida has designated as an Area of Critical State Concern in order to conserve natural resources. Between 1970 and 1975 the canal system annually discharged to the Gulf of Mexico from 143,200 to 275,600 acre-feet of freshwater. Discharge lowered ground-water levels as much as 4 feet near the eastern canal and created a water-level gradient that indicates water flowed from the Fakahatchee Strand west toward the canal during most of the year. In June 1975, water from early summer rains was impounded in the eastern canal upstream of the control structure at Janes Scenic Drive, and, as water levels rose in this reach, water flowed from the canal into the aquifer and around the control structure.</p><p>The annual low-water level in the center of the Fakahatchee Strand declined from nearly 3 feet above mean sea level in 1972 to 1 foot above mean sea level in 1974. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7761","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Swayze, L.J., and McPherson, B.F., 1977, The effect of the Faka Union Canal system on water levels in the Fakahatchee Strand, Collier County, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-61, iii, 19 p., https://doi.org/10.3133/wri7761.","productDescription":"iii, 19 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":2477,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0061/wri7761.pdf","text":"Report","size":"885 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":159292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0061/coverthb.jpg"}],"country":"United States","state":"Florida","county":"Collier County","otherGeospatial":"Fakahatchee Strand, Faka Union Canal","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.25326538085938,\n              25.75413552707459\n            ],\n            [\n              -81.20407104492188,\n              25.75413552707459\n            ],\n            [\n              -81.20407104492188,\n              26.606946521203206\n            ],\n            [\n              -82.25326538085938,\n              26.606946521203206\n            ],\n            [\n              -82.25326538085938,\n              25.75413552707459\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62f633","contributors":{"authors":[{"text":"Swayze, Leo J.","contributorId":55437,"corporation":false,"usgs":true,"family":"Swayze","given":"Leo","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202585,"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":202584,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70007446,"text":"70007446 - 1977 - The U.S. Geological Survey's Central Region headquarters, Denver, Colorado","interactions":[],"lastModifiedDate":"2012-02-17T00:10:14","indexId":"70007446","displayToPublicDate":"1977-01-01T17:27:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"The U.S. Geological Survey's Central Region headquarters, Denver, Colorado","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/70007446","usgsCitation":"U.S. Geological Survey, 1977, The U.S. Geological Survey's Central Region headquarters, Denver, Colorado, 24 p., ill., 23 cm., https://doi.org/10.3133/70007446.","productDescription":"24 p., ill., 23 cm.","startPage":"1","endPage":"24","numberOfPages":"24","costCenters":[],"links":[{"id":258785,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70007446/report.pdf","size":"7520","linkFileType":{"id":1,"text":"pdf"}},{"id":258786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70007446/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba945e4b08c986b32215a"}
]}