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No abstract available.

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No abstract available.

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Lunar surface materials are classed into units on the basis of visual observations and data from telescopic and Lunar Orbiter photographs. Each unit has a distinctive range of physical characteristics, such as topography and albedo (reflectivity under full-Moon illumination), and is considered analogous to a terrestrial rock-stratigraphic formation.  These characteristics rather than lithologic properties must, of necessity, suffice to define the units; however, the morphologic nature of most mappable units on the Moon, is, of itself, suggestive of a certain lithologic composition, based on analogous terranes on Earth.  

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Glacial drift and Cretaceous sedimentary rocks are the major aquifers in the Yellow Medicine River watershed unit.

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The Yellow Medicine and Minnesota Rivers are the major sources of surface water. For physiographic regions – Upland Plain, Slope, Lowland Plain, and Minnesota River Flood Plain – influence surface drainage, and the flow of ground water through the aquifers. The watershed comprises 1070 square miles, including the drainage basin of the Yellow Medicine River (665 square miles) and 405 square miles drained by small streams tributary to the Minnesota River.

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- 1969 - Geochemical abundance and distribution of nine metals in rocks and soils of the Coeur d'Alene district, Shoshone County, Idaho","interactions":[],"lastModifiedDate":"2026-01-21T16:58:24.499136","indexId":"ofr69107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"69-107","title":"Geochemical abundance and distribution of nine metals in rocks and soils of the Coeur d'Alene district, Shoshone County, Idaho","docAbstract":"

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The land surface of the Pine River basin, an area of 194 square miles, is a relatively flat or gently undulating northwest to southeast trending glacial lake plain.

The plain is interrupted by small streams and by a series of former glacial lake beaches. Other irregularities are the morainal hills in the headwaters and the morainal areas that form a large part of the basin divide. Altitudes range from 850 feet above mean sea level in the northwest corner of the basin to 578 feet at the mouth of the Pine river.

Drainage is not well developed in the basin. Many stream courses are poorly defined, having cut only from 3 to 10 feet below the adjacent plain. For this reason, ditches and drains are necessary to effectively drain parts of the basin. There are a few small scattered ponds, but no lakes within the basin.

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No abstract available.

","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1968","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp614C","usgsCitation":"Moore, J., and Koyanagi, R.Y., 1969, The October 1963 eruption of Kilauea Volcano, Hawaii: U.S. Geological Survey Professional Paper 614, Report: iii, 13 p.; 1 Plate: 37.00 × 21.00 inches, https://doi.org/10.3133/pp614C.","productDescription":"Report: iii, 13 p.; 1 Plate: 37.00 × 21.00 inches","costCenters":[],"links":[{"id":104690,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4941.htm","linkFileType":{"id":5,"text":"html"},"description":"4941"},{"id":67392,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0614c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67393,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0614c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122067,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0614c/report-thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea Volcano","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -155.1886,\n 19.3472\n ],\n [\n -154.9867,\n 19.3472\n ],\n [\n -154.9867,\n 19.4472\n ],\n [\n -155.1886,\n 19.4472\n ],\n [\n -155.1886,\n 19.3472\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aeda","contributors":{"authors":[{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":221947,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koyanagi, R. Y.","contributorId":35719,"corporation":false,"usgs":true,"family":"Koyanagi","given":"R.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":221946,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15362,"text":"ofr69197 - 1969 - Predicting the dye layer densities of color infrared transparencies","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr69197","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"69-197","title":"Predicting the dye layer densities of color infrared transparencies","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr69197","usgsCitation":"Pease, R.W., 1969, Predicting the dye layer densities of color infrared transparencies: U.S. Geological Survey Open-File Report 69-197, 33 p. ill. ;29 cm., https://doi.org/10.3133/ofr69197.","productDescription":"33 p. ill. ;29 cm.","costCenters":[],"links":[{"id":95297,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0197/report.pdf","size":"1455","linkFileType":{"id":1,"text":"pdf"}},{"id":148578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0197/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e7ff","contributors":{"authors":[{"text":"Pease, Robert W.","contributorId":43760,"corporation":false,"usgs":true,"family":"Pease","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":171009,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1515,"text":"wsp1918 - 1969 - Surface water supply of the United States 1961-65: Part 6, Missouri River basin: Volume 3. Missouri River basin from Sioux City, Iowa to Nebraska City, Nebraska","interactions":[],"lastModifiedDate":"2022-11-02T19:10:57.406604","indexId":"wsp1918","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1918","title":"Surface water supply of the United States 1961-65: Part 6, Missouri River basin: Volume 3. Missouri River basin from Sioux City, Iowa to Nebraska City, Nebraska","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1918","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Surface water supply of the United States 1961-65: Part 6, Missouri River basin: Volume 3. Missouri River basin from Sioux City, Iowa to Nebraska City, Nebraska: U.S. Geological Survey Water Supply Paper 1918, Report: ix, 751 p.; 1 Plate: 30.00 × 16.25 inches, https://doi.org/10.3133/wsp1918.","productDescription":"Report: ix, 751 p.; 1 Plate: 30.00 × 16.25 inches","costCenters":[],"links":[{"id":26579,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1918/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26578,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1918/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136967,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1918/report-thumb.jpg"},{"id":409072,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25142.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado, Iowa, Nebraska, South Dakota, Wyoming","otherGeospatial":"Missouri River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -95,\n 38.804\n ],\n [\n -95,\n 43.65\n ],\n [\n -109,\n 43.65\n ],\n [\n -109,\n 38.804\n ],\n [\n -95,\n 38.804\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697263","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527881,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1027,"text":"wsp1873B - 1969 - Estuarine studies in upper Grays Harbor, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1873B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1873","chapter":"B","title":"Estuarine studies in upper Grays Harbor, Washington","docAbstract":"Improved management of the water resources of Grays Harbor, Wash., requires more data on the water quality of the harbor and a better understanding of the influences of industrial and domestic wastes on the local fisheries resources. To provide a more comprehensive understanding of these influences, the U.S. Geological Survey joined other agencies in a cooperative study of Grays Harbor. This report summarizes the Survey's study of circulation patterns, description of water-quality conditions, and characterization of bottom material in the upper harbor. \r\n\r\nSalt water was found to intrude at least as far as Montesano, 28.4 nautical miles from the mouth of the harbor. Longitudinal salinity distributions were used to compute dispersion (diffusivity) coefficients ranging from 842 to 3,520 square feet per second. These values were corroborated by half-tidal-cycle dye studies. The waters of the harbor were found to be well mixed after extended periods of low fresh-water flow but stratified at high flows. Salinity data were used lo define the cumulative 'mean age' of the harbor water, which may be used to approximate a mean 'flushing time.' \r\n\r\nVelocity-time curves for the upper harbor are distorted from simple harmonic functions owing to channel geometry and frictional effects. Surface and bottom velocity data were used to estimate net tidal 'separation' distance, neglecting vertical mixing. Net separation distances between top and bottom water ranged from 1.65 nautical miles when fresh-water inflow was 610 cubic feet per second to 13.4 miles when inflow was 15,900 cubic feet per second. The cumulative mean age from integration of the fresh-water velocity equation was about twice that obtained from the salinity distribution. \r\n\r\nExcursion distances obtained with dye over half-tidal cycles exceeded those estimated from longitudinal salinity distributions and those obtained by earlier investigators who used floats. Net tidal excursions were as much as twice those obtained with floats. \r\n\r\nThe carbon content of bottom materials was related to channel fine material: \r\n\r\nC= 0.315+0.0238 F \r\n\r\nwhere C is in percent by dry weight, and F is percent by weight finer than 0.062 millimeter. Carbon content was low upstream and downstream of the upper harbor area, and high in the Cow Point-Rennie Island reach. The high-carbon-content reach coincides with the general area of a dissolved-oxygen sag. \r\n\r\nThe logarithm of the fresh-water discharge gave a high degree of correlation with daily maximum specific conductance at Cosmopolis. The regression equation is: \r\n\r\nKc max---- 76.4-- 17.7 logl0 Qf \r\n\r\nwhere Kc max is in millimhos at 25 ? Celsius (centigrade), and Qf is the estimated daily fresh-water discharge, in cubic feet per second. \r\n\r\nDissolved oxygen is the most critical water-quality parameter in Grays Harbor. At Cosmopolis, the daily minimum dissolved oxygen content, DOc min, correlated well with discharge and tidal range, delta H. The regression equation relating the variables is: \r\n\r\nDOc min---- 6.03 + 0.00096 Qf - 0.291 delta H \r\n\r\nin which DOc min is in milligrams per liter and delta H is in feet. The upper harbor was found to contain 250 million cubic feet less water than average during the critical low-flow period, on the basis of the frequency distribution of predicted tides. About 78,000 pounds of dissolved oxygen is thus unavailable for oxidation of waste during summer.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1873B","usgsCitation":"Beverage, J.P., and Swecker, M.N., 1969, Estuarine studies in upper Grays Harbor, Washington: U.S. Geological Survey Water Supply Paper 1873, vi, 90 p., https://doi.org/10.3133/wsp1873B.","productDescription":"vi, 90 p.","costCenters":[],"links":[{"id":137896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1873b/report-thumb.jpg"},{"id":25656,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1873b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fb152","contributors":{"authors":[{"text":"Beverage, Joseph P.","contributorId":48943,"corporation":false,"usgs":true,"family":"Beverage","given":"Joseph","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":143049,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swecker, Milton N.","contributorId":57826,"corporation":false,"usgs":true,"family":"Swecker","given":"Milton","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":143050,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":55889,"text":"ofr6921 - 1969 - Photogrammetric calibration of Apollo film cameras","interactions":[],"lastModifiedDate":"2014-07-14T10:15:33","indexId":"ofr6921","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"69-21","title":"Photogrammetric calibration of Apollo film cameras","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr6921","collaboration":"Prepared under NASA Contract no. T65253G","usgsCitation":"Borgeson, W., and Batson, R.M., 1969, Photogrammetric calibration of Apollo film cameras: U.S. Geological Survey Open-File Report 69-21, iii, 14 p., https://doi.org/10.3133/ofr6921.","productDescription":"iii, 14 p.","numberOfPages":"17","costCenters":[],"links":[{"id":181531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685e64","contributors":{"authors":[{"text":"Borgeson, W.T.","contributorId":47519,"corporation":false,"usgs":true,"family":"Borgeson","given":"W.T.","email":"","affiliations":[],"preferred":false,"id":254423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Batson, Raymond M.","contributorId":13989,"corporation":false,"usgs":true,"family":"Batson","given":"Raymond","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":254422,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68298,"text":"ha369 - 1969 - Hydrologic significance of 1966 flood levels at Lake Jackson near Tallahassee, Florida","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha369","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"369","title":"Hydrologic significance of 1966 flood levels at Lake Jackson near Tallahassee, Florida","language":"ENGLISH","doi":"10.3133/ha369","usgsCitation":"Hughes, G., 1969, Hydrologic significance of 1966 flood levels at Lake Jackson near Tallahassee, Florida: U.S. Geological Survey Hydrologic Atlas 369, 1 col. map., https://doi.org/10.3133/ha369.","productDescription":"1 col. map.","costCenters":[],"links":[{"id":186621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89725,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/369/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.36749999999999,30.467499999999998 ], [ -84.36749999999999,30.6 ], [ -84.26666666666667,30.6 ], [ -84.26666666666667,30.467499999999998 ], [ -84.36749999999999,30.467499999999998 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60547e","contributors":{"authors":[{"text":"Hughes, G.H.","contributorId":73975,"corporation":false,"usgs":true,"family":"Hughes","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":277985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36133,"text":"b1214G - 1969 - Element distribution in some Paleozoic black shales and associated rocks","interactions":[],"lastModifiedDate":"2012-02-02T00:09:36","indexId":"b1214G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1214","chapter":"G","title":"Element distribution in some Paleozoic black shales and associated rocks","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to geochemistry, 1964-68","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1214G","usgsCitation":"Vine, J.D., 1969, Element distribution in some Paleozoic black shales and associated rocks: U.S. Geological Survey Bulletin 1214, p. G1-G32, illus., map. ;24 cm., https://doi.org/10.3133/b1214G.","productDescription":"p. G1-G32, illus., map. ;24 cm.","costCenters":[],"links":[{"id":97226,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1214g/report.pdf","size":"2921","linkFileType":{"id":1,"text":"pdf"}},{"id":166319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1214g/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606c1b","contributors":{"authors":[{"text":"Vine, James David","contributorId":52147,"corporation":false,"usgs":true,"family":"Vine","given":"James","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":215820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37001,"text":"ifc32 - 1969 - Toxicity of Hyamine 3500 to fish","interactions":[],"lastModifiedDate":"2012-02-02T00:09:57","indexId":"ifc32","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":39,"text":"Investigations in Fish Control","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"32","title":"Toxicity of Hyamine 3500 to fish","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Hogan, J.W., 1969, Toxicity of Hyamine 3500 to fish: Investigations in Fish Control 32, 9 p. ; 26 cm.","productDescription":"9 p. ; 26 cm","costCenters":[],"links":[{"id":164538,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ifc/032/report-thumb.jpg"},{"id":64331,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ifc/032/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69884c","contributors":{"authors":[{"text":"Hogan, James W.","contributorId":24402,"corporation":false,"usgs":true,"family":"Hogan","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":217334,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":34896,"text":"b1203E - 1969 - The effect of two-dimensinal topography on superficial thermal gradients","interactions":[],"lastModifiedDate":"2012-02-02T00:09:30","indexId":"b1203E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1203","chapter":"E","title":"The effect of two-dimensinal topography on superficial thermal gradients","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1203E","usgsCitation":"Lachenbruch, A.H., 1969, The effect of two-dimensinal topography on superficial thermal gradients: U.S. Geological Survey Bulletin 1203, p. E1-E86, ill., (2 fold in pocket) ;24 cm., https://doi.org/10.3133/b1203E.","productDescription":"p. E1-E86, ill., (2 fold in pocket) ;24 cm.","costCenters":[],"links":[{"id":167371,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1203e/report-thumb.jpg"},{"id":62854,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1203e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62855,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1203e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62856,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1203e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6281ca","contributors":{"authors":[{"text":"Lachenbruch, Arthur H.","contributorId":27850,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"Arthur","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":213774,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}