{"pageNumber":"1594","pageRowStart":"39825","pageSize":"25","recordCount":40783,"records":[{"id":26660,"text":"wri7354 - 1973 - Stratigraphy of an archeological site, Ocmulgee flood plain, Macon, Georgia","interactions":[],"lastModifiedDate":"2018-10-31T09:27:08","indexId":"wri7354","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-54","title":"Stratigraphy of an archeological site, Ocmulgee flood plain, Macon, Georgia","docAbstract":"<p>Archeological excavations on the Ocmulgee River flood plain at Ocmulgee National Monument revealed eight sedimentary units of Holocene age. Types of deposits found are natural levee, oberbank deposit, and a probable point bar. Since the 18th century, locally more than 10 feet of sediment has been deposited. These modern sediments are similar to those on other flood plains in the southeastern United States and probably resulted from erosion that began when extensive areas were laid bare for farming. They are red to reddish brown in contrast to underlying sediment, which is various shades of gray, brown, and yellow. Earliest traces of man are \"spinner-type\" projectiles in the lower sand member (Qls). Marrow mountain-type points are found in mottled silty sandy clay (Qmssc). Triangular stemmed Savannah River points were found throughout the intermediate sand (Qis). Fiber tempered pottery shards and steatite bowls were found in upper one half of the intermediate sand member (Qis).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7354","usgsCitation":"Cosner, O.J., 1973, Stratigraphy of an archeological site, Ocmulgee flood plain, Macon, Georgia: U.S. Geological Survey Water-Resources Investigations Report 73-54, vi, 27 p., https://doi.org/10.3133/wri7354.","productDescription":"vi, 27 p.","costCenters":[],"links":[{"id":359009,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0054/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158212,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0054/report-thumb.jpg"}],"country":"United States","state":"Georgia","otherGeospatial":"Ocmulgee Flood Plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.6337661743164,\n              32.82161450042075\n            ],\n            [\n              -83.57909202575684,\n              32.82161450042075\n            ],\n            [\n              -83.57909202575684,\n              32.855652799756534\n            ],\n            [\n              -83.6337661743164,\n              32.855652799756534\n            ],\n            [\n              -83.6337661743164,\n              32.82161450042075\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6538","contributors":{"authors":[{"text":"Cosner, Oliver J.","contributorId":38533,"corporation":false,"usgs":true,"family":"Cosner","given":"Oliver","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":196791,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41943,"text":"ofr73138 - 1973 - Analog-model studies of the effects of recharge wells along the Houston Ship Channel on potentiometric surfaces of the Chicot and Evangeline aquifers, Houston, Texas","interactions":[],"lastModifiedDate":"2016-08-23T16:37:52","indexId":"ofr73138","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-138","title":"Analog-model studies of the effects of recharge wells along the Houston Ship Channel on potentiometric surfaces of the Chicot and Evangeline aquifers, Houston, Texas","docAbstract":"<p>Because of increasing concern about the continuing decline of water levels in the Houston area, an electric analog model was used to determine the effects on the potentiometric surfaces resulting from recharging water through wells along the Houston Ship Channel into the two major aquifers, the Chicot and Evangeline.</p><p>The model conditions simulated for this study are too complex to be described in detail. The upper model layer simulated the hydrologic conditions in the lower unit of the Chicot aquifer undifferentiated. The simulation included clay compaction and vertical leakage as well as transmissivity and storage. The lower model layer simulated the hydrologic conditions in the Evangeline aquifer which underlies the Chicot aquifer.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73138","collaboration":"Prepared in cooperation with the City of Houston and Texas Water Development Board","usgsCitation":"Jorgensen, D.G., 1973, Analog-model studies of the effects of recharge wells along the Houston Ship Channel on potentiometric surfaces of the Chicot and Evangeline aquifers, Houston, Texas: U.S. Geological Survey Open-File Report 73-138, 2 Plates: 15.48 x 21.26 inches x 15.78 x 21.23 inches, https://doi.org/10.3133/ofr73138.","productDescription":"2 Plates: 15.48 x 21.26 inches x 15.78 x 21.23 inches","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327758,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr73138.JPG"},{"id":79670,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0138/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79671,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0138/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683991","contributors":{"authors":[{"text":"Jorgensen, D. G.","contributorId":104527,"corporation":false,"usgs":true,"family":"Jorgensen","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":225753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46353,"text":"ofr73334 - 1973 - Atlas of Mars, MC-18, Coprates Quadrangle","interactions":[],"lastModifiedDate":"2024-03-25T18:51:59.275031","indexId":"ofr73334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-334","title":"Atlas of Mars, MC-18, Coprates Quadrangle","docAbstract":"<p>This mosaic was made with Mariner 9 pictures provided by the Jet Propulsion Laboratory (JPL), California Institute of Technology. The Image Processing Laboratory (IPL) of JPL processed the digital pictures to remove image artifacts and geometric distortions, to enhance high-frequency topographic detail while subduing low-frequency albedo variation, and to transform the pictures to a Mercator projection. The U.S. Geological Survey performed further artifact removal and modified contrast and tone of each picture analytically on the digital magnetic tapes provided by IPL for uniformity of tone and contrast within the mosaic. Photographic reproductions of the pictures were generated from the magnetic tapes and mosaicked by the U.S. Geological Survey.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73334","collaboration":"Prepared in cooperation with the Jet Propulsion Laboratory, California Institute of Technology, and the National Aeronautics and Space Administration","usgsCitation":"United States Geological Survey, 1973, Atlas of Mars, MC-18, Coprates Quadrangle: U.S. Geological Survey Open-File Report 73-334, 1 Plate: 23.14 x 26.20 inches, https://doi.org/10.3133/ofr73334.","productDescription":"1 Plate: 23.14 x 26.20 inches","costCenters":[],"links":[{"id":427029,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0334/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171946,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0334/report-thumb.jpg"}],"scale":"5000000","projection":"Mercator Projection","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fab9","contributors":{"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":531676,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27037,"text":"wri7313 - 1973 - Ground-water hydrology of northern Napa Valley, California","interactions":[],"lastModifiedDate":"2020-08-08T00:26:00.663327","indexId":"wri7313","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-13","title":"Ground-water hydrology of northern Napa Valley, California","docAbstract":"<p><span>The alluvium of northern Napa Valley is the principal aquifer of the </span><span>area and is capable of yielding as much as 3,000 gallons per minute to wells. </span><span>Generally the larger-yielding wells are along the Napa River where the </span><span>alluvium is thickest and most permeable. Recharge to the alluvium is chiefly </span><span>by percolation from streams and infiltration of precipitation. Discharge is </span><span>chiefly flow to the Napa River, evapotranspiration, and pumpage from wells. </span><span>Both recharge to, and discharge from, the alluvial aquifer are sensitively </span><span>influenced by rainfall. About 190,000 acre-feet of water is presently (1972) </span><span>stored in the alluvium of northern Napa Valley. Future annual water use in </span><span>the project area will probably vary between 12,000 and 35,000 acre-feet and, </span><span>for most purposes, can be supplied by the alluvial aquifer even during </span><span>extended periods of limited rainfall. Generally low transmissivities in the </span><span>alluvium, however, limit the opportunity for obtaining sustained, large yields </span><span>from wells in much of the valley and require that large-scale development and </span><span>operation of wells in much of the area be planned and synchronized.</span></p><p><span>Sustained drought conditions in the Napa Valley accompanied by expected increases in the use of ground water will probably cause significant reductions in the base flow of the Napa River and cause many shallow wells in the area to dry up. </span></p><p><span>Sodium chloride ground water occurs near Calistoga and in the vicinity of Oakville and in some places is not suitable for irrigation. Model studies indicate that limited migration of sodium chloride water into intensively pumped parts of the aquifer probably will not be a serious problem.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7313","collaboration":"Prepared in cooperation with the Napa County Flood Control and Water Conservation District","usgsCitation":"Faye, R.E., 1973, Ground-water hydrology of northern Napa Valley, California: U.S. Geological Survey Water-Resources Investigations Report 73-13, Report: vi, 64 p.; 1 Figure: 32.18 x 21.92 inches, https://doi.org/10.3133/wri7313.","productDescription":"Report: vi, 64 p.; 1 Figure: 32.18 x 21.92 inches","costCenters":[],"links":[{"id":158580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0013/report-thumb.jpg"},{"id":377248,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/wri/1973/0013/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377247,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0013/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Napa Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.66666667,\n              38.33333333\n            ],\n            [\n              -122.25,\n              38.33333333\n            ],\n            [\n              -122.25,\n              38.61666667\n            ],\n            [\n              -122.66666667,\n              38.61666667\n            ],\n            [\n              -122.66666667,\n              38.33333333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d497","contributors":{"authors":[{"text":"Faye, Robert E.","contributorId":92221,"corporation":false,"usgs":true,"family":"Faye","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":197449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46351,"text":"ofr73332 - 1973 - Atlas of Mars, Memnonia quadrangle, MC-16","interactions":[{"subject":{"id":46351,"text":"ofr73332 - 1973 - Atlas of Mars, Memnonia quadrangle, MC-16","indexId":"ofr73332","publicationYear":"1973","noYear":false,"title":"Atlas of Mars, Memnonia quadrangle, MC-16"},"predicate":"SUPERSEDED_BY","object":{"id":65889,"text":"i1075 - 1978 - Shaded relief map of the Memnonia Quadrangle of Mars","indexId":"i1075","publicationYear":"1978","noYear":false,"title":"Shaded relief map of the Memnonia Quadrangle of Mars"},"id":1}],"supersededBy":{"id":65889,"text":"i1075 - 1978 - Shaded relief map of the Memnonia Quadrangle of Mars","indexId":"i1075","publicationYear":"1978","noYear":false,"title":"Shaded relief map of the Memnonia Quadrangle of Mars"},"lastModifiedDate":"2024-08-05T21:34:32.628744","indexId":"ofr73332","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-332","title":"Atlas of Mars, Memnonia quadrangle, MC-16","docAbstract":"<p>This mosaic was made with Mariner 9 pictures provided by the Jet Propulsion Laboratory (JPL), California Institute of Technology. The Image Processing Laboratory (IPL) of JPL processed the digital pictures to remove image artifacts and geometric distortions, to enhance high-frequency topographic detail while subduing low-frequency albedo variation, and to transform the pictures to a Mercator projection. The U.S. Geological Survey performed further artifact removal and modified contrast and tone of each picture analytically on the digital magnetic tapes provided by IPL for uniformity of tone and contrast within the mosaic. Photographic reproductions of the pictures were generated from the magnetic tapes and mosaicked by the U. S. Geological Survey.</p><p>Primary horizontal control points, where available, controlled the placement of pictures. Where these points were not available, picture placement was controlled by spacecraft tracking data and by matching images in overlap zones between pictures. Discrepancies in matching these images are less than 10 km over 90% of the mosaic. The number designations and positions of the primary control points, shown by broken crosses (-l-), are those given by Davies and Arthur (1973).</p><p>Aerographic latitudes are shown on this mosaic. The projection is based on a theoretical dynamical ellipticity of 1/192. The scale is based on an equatorial radius of 3393. 4 km.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73332","collaboration":"Prepared in cooperation with the Jet Propulsion Laboratory, California Insitute of Technology, and the Langley Research Center, National Aeronautics and Space Administration","usgsCitation":"United States Geological Survey, 1973, Atlas of Mars, Memnonia quadrangle, MC-16: U.S. Geological Survey Open-File Report 73-332, 1 Plate: 23.39 x 26.48 inches, https://doi.org/10.3133/ofr73332.","productDescription":"1 Plate: 23.39 x 26.48 inches","costCenters":[],"links":[{"id":432216,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0332/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171944,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0332/report-thumb.jpg"}],"scale":"5000000","projection":"Mercator Projection","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fa8c","contributors":{"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":531674,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46355,"text":"ofr73336 - 1973 - Atlas of Mars, Sinus Sabaeus Quadrangle, MC-20","interactions":[{"subject":{"id":46355,"text":"ofr73336 - 1973 - Atlas of Mars, Sinus Sabaeus Quadrangle, MC-20","indexId":"ofr73336","publicationYear":"1973","noYear":false,"title":"Atlas of Mars, Sinus Sabaeus Quadrangle, MC-20"},"predicate":"SUPERSEDED_BY","object":{"id":69660,"text":"i1296 - 1980 - Shaded relief map of the Sinus Sabaeus quadrangle of Mars :b MC-20, M 5M-15/338 RN","indexId":"i1296","publicationYear":"1980","noYear":false,"title":"Shaded relief map of the Sinus Sabaeus quadrangle of Mars :b MC-20, M 5M-15/338 RN"},"id":1}],"supersededBy":{"id":69660,"text":"i1296 - 1980 - Shaded relief map of the Sinus Sabaeus quadrangle of Mars :b MC-20, M 5M-15/338 RN","indexId":"i1296","publicationYear":"1980","noYear":false,"title":"Shaded relief map of the Sinus Sabaeus quadrangle of Mars :b MC-20, M 5M-15/338 RN"},"lastModifiedDate":"2024-08-05T22:06:38.46851","indexId":"ofr73336","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-336","title":"Atlas of Mars, Sinus Sabaeus Quadrangle, MC-20","docAbstract":"<p>This mosaic was made with Mariner 9 pictures provided by the Jet Propulsion Laboratory (JPL), California Institute of Technology. The Image Processing Laboratory (IPL) of JPL processed the digital pictures to remove image artifacts and geometric distortions, to enhance high-frequency topographic detail while subduing low-frequency albedo variation, and to transform the pictures to a Mercator projection. The U.S. Geological Survey performed further artifact removal and modified contrast and tone of each picture analytically on the digital magnetic tapes provided by IPL for uniformity of tone and contrast within the mosaic. Photographic reproductions of the pictures were generated from the magnetic tapes and mosaicked by the U.S. Geological Survey.</p><p>Primary horizontal control points, where available, controlled the placement of pictures. Where these points were not available, picture placement was controlled by spacecraft tracking data and by matching images in overlap zones between pictures. Discrepancies in matching these images are less than 10 km over 90% of the mosaic. The number designations and positions of the primary control points, shown by broken crosses (-l-), are those given by Davies and Arthur (1973).</p><p>Aerographic latitudes are shown on this mosaic. The projection is based on a theoretical dynamical ellipticity of 1/192. The scale is based on an equatorial radius of 3393. 4 km.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73336","usgsCitation":"United States Geological Survey, 1973, Atlas of Mars, Sinus Sabaeus Quadrangle, MC-20: U.S. Geological Survey Open-File Report 73-336, 1 Plate: 23.06 x 25.84 inches, https://doi.org/10.3133/ofr73336.","productDescription":"1 Plate: 23.06 x 25.84 inches","costCenters":[],"links":[{"id":171948,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0336/report-thumb.jpg"},{"id":432254,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0336/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","projection":"Mercator Projection","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fac1","contributors":{"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":531678,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46348,"text":"ofr73329 - 1973 - Atlas of Mars, Lunae Palus quadrangle, MC-10","interactions":[],"lastModifiedDate":"2024-08-05T21:38:07.129933","indexId":"ofr73329","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-329","title":"Atlas of Mars, Lunae Palus quadrangle, MC-10","docAbstract":"<p>This mosaic was made with Mariner 9 pictures provided by the Jet Propulsion Laboratory (JPL), California Institute of Technology. The Image Processing Laboratory (IPL) of JPL processed the digital pictures to remove image artifacts and geometric distortions, to enhance high-frequency topographic detail while subduing low-frequency albedo variation, and to transform the pictures to a Mercator projection. The U.S. Geological Survey performed further artifact removal and modified contrast and tone of each picture analytically on the digital magnetic tapes provided by IPL for uniformity of tone and contrast within the mosaic. Photographic reproductions of the pictures were generated from the magnetic tapes and mosaicked by the U.S. Geological Survey.</p><p>Primary horizontal control points, where available, controlled the placement of pictures. Where these points were not available, picture placement was controlled by spacecraft tracking data and by matching images in overlap zones between pictures. Discrepancies in matching these images are less than 10 km over 90% of the mosaic. The number designations and positions of the primary control points, shown by broken crosses (-l-), are those given by Davies and Arthur (1973).</p><p>Aerographic latitudes are shown on this mosaic. The projection is based on a theoretical dynamical ellipticity of 1/192. The scale is based on an equatorial radius of 3393.4 km.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73329","usgsCitation":"United States Geological Survey, 1973, Atlas of Mars, Lunae Palus quadrangle, MC-10: U.S. Geological Survey Open-File Report 73-329, 1 Plate: 22.90 x 25.79 inches, https://doi.org/10.3133/ofr73329.","productDescription":"1 Plate: 22.90 x 25.79 inches","costCenters":[],"links":[{"id":171839,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0329/report-thumb.jpg"},{"id":432222,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0329/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","projection":"Mercator Projection","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fa5c","contributors":{"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":531671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48177,"text":"ofr73203 - 1973 - Water resources outlook for the Minneapolis-Saint Paul Metropolitan Area, Minnesota","interactions":[{"subject":{"id":49254,"text":"ofr72272 - 1972 - Hydrogeologic maps of the Minneapolis-St. Paul artesian basin, Minnesota","indexId":"ofr72272","publicationYear":"1972","noYear":false,"title":"Hydrogeologic maps of the Minneapolis-St. Paul artesian basin, Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":48177,"text":"ofr73203 - 1973 - Water resources outlook for the Minneapolis-Saint Paul Metropolitan Area, Minnesota","indexId":"ofr73203","publicationYear":"1973","noYear":false,"title":"Water resources outlook for the Minneapolis-Saint Paul Metropolitan Area, Minnesota"},"id":1}],"lastModifiedDate":"2018-03-19T10:38:07","indexId":"ofr73203","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-203","title":"Water resources outlook for the Minneapolis-Saint Paul Metropolitan Area, Minnesota","docAbstract":"<p>The water resources were studied within an area whose natural ground-water flow is largely towards the center of the metropolitan area. This area coincides with the extent of the Hinckley Sandstone aquifer. Thus, the general geohydrology of the area bounded by the extent of the Hinckley Sandstone (about 6,000 square miles) as it relates to the hydrology of the Minneapolis-St. Paul metropolitan area is described. Greater emphasis is placed on the area underlain by the Prairie du Chien-Jordan aquifer (about 2,000 square miles), from which approximately 75 percent of the ground-water for the metropolitan area is pumped.</p>\n<p>The study indicates that the surface-water resources of the Twin Cities metropolitan area are used to such an extent that a supply adequate for domestic and industrial needs as well as power plant and sanitary effluent assimilation will not be available during severe drought.</p>\n<p>Ground-water is obtained primarily from two aquifer systems: The Prairie du Chien-Jordan and the Mount Simon-Hinckley. In 1970, these aquifers supplied about 90 percent (175 mgd) of the ground-water used in the metropolitan part of the study area. The probable level of development that can be sustained by these two aquifers in the metropolitan area is estimated to be 1,100 mgd; thus, substantial additional ground-water supplies could be developed. However, considerable management and planning would be needed to sustain this level of development.</p>\n<p>Maps in this report can be used to select general well-field locations based on consideration of 1) aquifer, 2) depth needed for completion, 3) head availability, 4) location of natural recharge and discharge boundaries, and 5) distance from areas where over-development of ground-water resources is imminent. Because of complexities in the ground-water system, yield estimates, boundary effects, and effects of aquifer interaction may best be determined in a study incorporating the use of a hydrologic model.</p>\n<p>Future detailed studies might include elaboration on some of the topics described in this report and the acquisition and interpretation of new data. Major items on which future work might focus are 1) data collection, 2) geohydrologic mapping, 3) hydraulic characteristics of subsurface geohydrologic units, 4) hydrology of lakes, and 5) hydrologic systems modeling</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr73203","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities Area","usgsCitation":"Norvitch, R., Ross, T., and Brietkrietz, A., 1973, Water resources outlook for the Minneapolis-Saint Paul Metropolitan Area, Minnesota: U.S. Geological Survey Open-File Report 73-203, x, 219 p., https://doi.org/10.3133/ofr73203.","productDescription":"x, 219 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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R.F.","contributorId":107742,"corporation":false,"usgs":true,"family":"Norvitch","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":236923,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, T.G.","contributorId":34987,"corporation":false,"usgs":true,"family":"Ross","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":236922,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brietkrietz, Alex","contributorId":34111,"corporation":false,"usgs":true,"family":"Brietkrietz","given":"Alex","email":"","affiliations":[],"preferred":false,"id":236921,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":48174,"text":"ofr73193 - 1973 - Puerto Rico water resources planning model program description","interactions":[],"lastModifiedDate":"2012-02-02T00:10:46","indexId":"ofr73193","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-193","title":"Puerto Rico water resources planning model program description","docAbstract":"Because the use of the Mathematical Programming System -Extended (MPSX) to solve large linear and mixed integer programs requires the preparation of many input data cards, a matrix generator program to produce the MPSX input data from a much more limited set of data may expedite the use of the mixed integer programming optimization technique. \r\n\r\nThe Model Definition and Control Program (MODCQP) is intended to assist a planner in preparing MPSX input data for the Puerto Rico Water Resources Planning Model. The model utilizes a mixed-integer mathematical program to identify a minimum present cost set of water resources projects (diversions, reservoirs, ground-water fields, desalinization plants, water treatment plants, and inter-basin transfers of water) which will meet a set of future water demands and to determine their sequence of construction. While MODCOP was specifically written to generate MPSX input data for the planning model described in this report, the program can be easily modified to reflect changes in the model's mathematical structure.","language":"ENGLISH","doi":"10.3133/ofr73193","usgsCitation":"Moody, D., Maddock, T., Karlinger, M., and Lloyd, J., 1973, Puerto Rico water resources planning model program description: U.S. Geological Survey Open-File Report 73-193, 22 p. ill. ; 28 cm., https://doi.org/10.3133/ofr73193.","productDescription":"22 p. ill. ; 28 cm.","costCenters":[],"links":[{"id":170864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0193/report-thumb.jpg"},{"id":84906,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0193/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db65575d","contributors":{"authors":[{"text":"Moody, D.W.","contributorId":54642,"corporation":false,"usgs":true,"family":"Moody","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":236913,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maddock, Thomas","contributorId":79892,"corporation":false,"usgs":true,"family":"Maddock","given":"Thomas","affiliations":[],"preferred":false,"id":236914,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Karlinger, M.R.","contributorId":95039,"corporation":false,"usgs":true,"family":"Karlinger","given":"M.R.","affiliations":[],"preferred":false,"id":236915,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lloyd, J.J.","contributorId":106186,"corporation":false,"usgs":true,"family":"Lloyd","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":236916,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":48159,"text":"ofr73142 - 1973 - Handbook for Federal Insurance Administration: Flood-insurance studies","interactions":[],"lastModifiedDate":"2017-09-15T07:55:41","indexId":"ofr73142","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-142","title":"Handbook for Federal Insurance Administration: Flood-insurance studies","docAbstract":"<p>A flood insurance study, made for the Federal Insurance Administration (FIA) of the Department of Housing and Urban Development (HUD) is an analysis of flood inundation frequency for all flood plains within the corporate limits of the community being studied. The study is an application of surveying, hydrology, and hydraulics to determine flood insurance premium rates. Much of the surveying needed can be done by private firms, either by ground methods or photogrammetry. Contracts are needed to let large surveys but purchase orders can be used for small ones. Photogrammetric stereo models, digital regression models, and step-backwater models are needed for most studies. Damage survey data are not involved.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73142","usgsCitation":"Kennedy, E., 1973, Handbook for Federal Insurance Administration: Flood-insurance studies: U.S. Geological Survey Open-File Report 73-142, 54 p., https://doi.org/10.3133/ofr73142.","productDescription":"54 p.","costCenters":[],"links":[{"id":162758,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0142/report-thumb.jpg"},{"id":114391,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0142/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"tableOfContents":"<p><br data-mce-bogus=\"1\"></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a5c8","contributors":{"authors":[{"text":"Kennedy, E.J.","contributorId":87529,"corporation":false,"usgs":true,"family":"Kennedy","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":236893,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48158,"text":"ofr73139 - 1973 - A plan for study of water resources in the Platte River basin, Nebraska: with special emphasis on the stream-aquifer relations","interactions":[],"lastModifiedDate":"2018-11-01T14:40:55","indexId":"ofr73139","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-139","title":"A plan for study of water resources in the Platte River basin, Nebraska: with special emphasis on the stream-aquifer relations","docAbstract":"<p>A \"Level B\" study is being made of the Platte River basin in Nebraska. The basin (approximately 40,800 square miles) extends the full length of the State, a distance of nearly 470 miles. The study is a Federal and State interagency effort to formulate a comprehensive plan for the conservation, development, and management of the water and related land resources of the Platte River basin. The technical information for the study will be provided by 14 task forces. This report describes the work of the Level B Stream-Aquifer Hydrology Task Force (Task Force 13). The U.S. Geological Survey is the lead agency for this task force. </p><p>Task Force 13 will provide the agencies participating in the Level B study with a quantitative description of the operation of the hydrologic system with emphasis on the relation of ground water to surface water. A digital model will be developed to simulate the physical character and operation of the stream-aquifer system. After the model has been calibrated with field data, it will be used to evaluate the effect of proposed projects. Some of the uses of the model are evaluation of effects of proposed conjunctive use projects, effects of changes in water use, and study of future water problems such as water-logged areas, groundwater mining, and streamflow depletion.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73139","usgsCitation":"Keech, C., Moore, J., and Emery, P.A., 1973, A plan for study of water resources in the Platte River basin, Nebraska: with special emphasis on the stream-aquifer relations: U.S. Geological Survey Open-File Report 73-139, 36 p., https://doi.org/10.3133/ofr73139.","productDescription":"36 p.","numberOfPages":"39","costCenters":[],"links":[{"id":162757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0139/report-thumb.jpg"},{"id":359082,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nebraska","otherGeospatial":"Platte River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab77e","contributors":{"authors":[{"text":"Keech, C.F.","contributorId":67941,"corporation":false,"usgs":true,"family":"Keech","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":236892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, J.E.","contributorId":34927,"corporation":false,"usgs":true,"family":"Moore","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":236890,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Emery, P. A.","contributorId":49392,"corporation":false,"usgs":true,"family":"Emery","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":236891,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":48189,"text":"ofr73237 - 1973 - Comments on the use of numerical model by Kerr-McGee Corporation in appraising effects of subsurface liquid waste disposal","interactions":[],"lastModifiedDate":"2020-05-12T17:40:47.892257","indexId":"ofr73237","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-237","title":"Comments on the use of numerical model by Kerr-McGee Corporation in appraising effects of subsurface liquid waste disposal","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr73237","usgsCitation":"Robertson, J., 1973, Comments on the use of numerical model by Kerr-McGee Corporation in appraising effects of subsurface liquid waste disposal: U.S. Geological Survey Open-File Report 73-237, 5 p., https://doi.org/10.3133/ofr73237.","productDescription":"5 p.","costCenters":[],"links":[{"id":171829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0237/report-thumb.jpg"},{"id":374695,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0237/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae654","contributors":{"authors":[{"text":"Robertson, J.B.","contributorId":85173,"corporation":false,"usgs":true,"family":"Robertson","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":236943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46360,"text":"ofr73341 - 1973 - Atlas of Mars chart, Argyre Quadrangle, MC-26","interactions":[],"lastModifiedDate":"2024-08-05T21:58:13.797537","indexId":"ofr73341","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-341","title":"Atlas of Mars chart, Argyre Quadrangle, MC-26","docAbstract":"<p><span>This mosaic was made with Mariner 9 pictures provided by the Jet Propulsion Laboratory (JPL), California Institute of Technology. The Image Processing Laboratory (IPL) of JPL processed the digital pictures to remove image artifacts and geometric distortions, to enhance high-frequency topographic detail while subduing low-frequency albedo variation, and to transform the pictures to a Mercator projection. The U.S. Geological Survey performed further artifact removal and modified contrast and tone of each picture analytically on the digital magnetic tapes provided by IPL for uniformity of tone and contrast within the mosaic. Photographic reproductions of the pictures were generated from the magnetic tapes and mosaicked by the U.S. Geological Survey.</span></p><p><span>Primary horizontal control points, where available, controlled the placement of pictures. Where these points were not available, picture placement was controlled by spacecraft tracking data and by matching images in overlap zones between pictures. Discrepancies in matching these images are less than 10 km over 90% of the mosaic. The number designations and positions of the primary control points, shown by broken crosses (-l-), are those given by Davies and Arthur (1973).</span></p><p><span>Aerographic latitudes are shown on this mosaic. The projection is based on a theoretical dynamical ellipticity of 1/192. The scale is based on an equatorial radius of 3393. 4 km.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73341","usgsCitation":"United States Geological Survey, 1973, Atlas of Mars chart, Argyre Quadrangle, MC-26: U.S. Geological Survey Open-File Report 73-341, 1 Plate: 29.54 x 32.27 inches, https://doi.org/10.3133/ofr73341.","productDescription":"1 Plate: 29.54 x 32.27 inches","costCenters":[],"links":[{"id":168895,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0341/report-thumb.jpg"},{"id":432243,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0341/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"4336000","projection":"Lambert Conformal Projection","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fb10","contributors":{"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":531683,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48155,"text":"ofr73134 - 1973 - Hydrology and sediment transport, Moanalua Valley, Oahu, Hawaii","interactions":[],"lastModifiedDate":"2021-03-19T22:46:21.403504","indexId":"ofr73134","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-134","title":"Hydrology and sediment transport, Moanalua Valley, Oahu, Hawaii","docAbstract":"<p><span>The first 2 years of intensive data collection in Moanalua </span><span>Valley have resulted in some observations concerning the rainfall-</span><span>runoff and rainfall-sedimentation characteristics of the basin.</span></p><p><span>This initial study period has been concerned primarily with establishing a reliable hydrologic data-collection network. However, enough data have been collected to determine that rainfall within the valley shows extreme areal variations from one storm to another. An initial run on the U.S. Geological Survey small watershed model indicates some differences in basin characteristics in the two upper subregions. Results of model studies to date are encouraging. Flood routing with the Corps of Engineers' HEC-1 flood hydrograph package seems to be feasible. By preliminary estimates, the 50-year flood at gage 2282 would probably be between 5,500 and 6,000 cubic feet per second. </span></p><p><span>The narrow, steep nature of Moanalua Valley results in very rapid concentration of runoff, with extremely sharp hydrograph peaks. Stream channel width ranges from about 20 feet in the headwaters to 35 feet near the downstream limit of the study area. Mean slope of the main stem is about 0.027 foot/foot.1/ Where not identified, units for slope are ft/ft.</span></p><p><span>Observations indicate that the stream transports very large </span><span>particles (in excess of 2 </span><span>feet </span><span>in diameter) quite frequently. Detached </span><span>fragments from old stone-arch bridges have been marked in the channel </span><span>fill for use as tracers.</span></p><p><span>Only one storm has been analyzed for suspended-sediment discharge, but rough calculations indicate a possible suspended-sediment load of 12,000 tons for a storm similar to the design flow at gage 2282. This compares with a computed bedload discharge of 2,600 tons for the same flow.</span></p><p><span>Accumulation in the debris basin between October 2, 1969 and </span><span>July 26, 1971, as measured by level survey, was 48,000 cubic feet </span><span>or about 2,900 tons. </span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr73134","usgsCitation":"Jones, B., and Ewart, C., 1973, Hydrology and sediment transport, Moanalua Valley, Oahu, Hawaii: U.S. Geological Survey Open-File Report 73-134, 124 p., https://doi.org/10.3133/ofr73134.","productDescription":"124 p.","costCenters":[],"links":[{"id":384517,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0134/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0134/report-thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Oahu","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -157.90306091308594,\n              21.362132196021925\n            ],\n            [\n              -157.87919998168942,\n              21.362132196021925\n            ],\n            [\n              -157.87919998168942,\n              21.372363370512762\n            ],\n            [\n              -157.90306091308594,\n              21.372363370512762\n            ],\n            [\n              -157.90306091308594,\n              21.362132196021925\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e887","contributors":{"authors":[{"text":"Jones, B.L.","contributorId":6498,"corporation":false,"usgs":true,"family":"Jones","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":236886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ewart, C.J.","contributorId":76339,"corporation":false,"usgs":true,"family":"Ewart","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":236887,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48105,"text":"ofr739 - 1973 - Electrical-analog model study of a hydrologic system in Southeast Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:04","indexId":"ofr739","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-9","title":"Electrical-analog model study of a hydrologic system in Southeast Florida","language":"ENGLISH","doi":"10.3133/ofr739","usgsCitation":"Appel, C.A., 1973, Electrical-analog model study of a hydrologic system in Southeast Florida: U.S. Geological Survey Open-File Report 73-9, 57 p. ill., maps ; 27 cm., https://doi.org/10.3133/ofr739.","productDescription":"57 p. ill., maps ; 27 cm.","costCenters":[],"links":[{"id":162111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606e1f","contributors":{"authors":[{"text":"Appel, Charles A.","contributorId":14376,"corporation":false,"usgs":true,"family":"Appel","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":236819,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46359,"text":"ofr73340 - 1973 - Atlas of Mars chart, Thaumasia Quadrangle, MC-25","interactions":[],"lastModifiedDate":"2024-08-05T21:59:31.126593","indexId":"ofr73340","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-340","title":"Atlas of Mars chart, Thaumasia Quadrangle, MC-25","docAbstract":"<p><span>This mosaic was made with Mariner 9 pictures provided by the Jet Propulsion Laboratory (JPL), California Institute of Technology. The Image Processing Laboratory (IPL) of JPL processed the digital pictures to remove image artifacts and geometric distortions, to enhance high-frequency topographic detail while subduing low-frequency albedo variation, and to transform the pictures to a Mercator projection. The U.S. Geological Survey performed further artifact removal and modified contrast and tone of each picture analytically on the digital magnetic tapes provided by IPL for uniformity of tone and contrast within the mosaic. Photographic reproductions of the pictures were generated from the magnetic tapes and mosaicked by the U.S. Geological Survey.</span></p><p><span>Primary horizontal control points, where available, controlled the placement of pictures. Where these points were not available, picture placement was controlled by spacecraft tracking data and by matching images in overlap zones between pictures. Discrepancies in matching these images are less than 10 km over 90% of the mosaic. The number designations and positions of the primary control points, shown by broken crosses (-l-), are those given by Davies and Arthur (1973).</span></p><p><span>Aerographic latitudes are shown on this mosaic. The projection is based on a theoretical dynamical ellipticity of 1/192. The scale is based on an equatorial radius of 3393. 4 km.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73340","collaboration":"Prepared in cooperation with the Jet Propulsion Laboratory, California Insititute of Technology and the National Aeronautics and Space Administration","usgsCitation":"United States Geological Survey, 1973, Atlas of Mars chart, Thaumasia Quadrangle, MC-25: U.S. Geological Survey Open-File Report 73-340, 1 Plate: 30.03 x 31.21 inches, https://doi.org/10.3133/ofr73340.","productDescription":"1 Plate: 30.03 x 31.21 inches","costCenters":[],"links":[{"id":432246,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0340/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171952,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0340/report-thumb.jpg"}],"scale":"4336000","projection":"Lambert Conformal Projection","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fb04","contributors":{"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":531682,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28990,"text":"wri736 - 1973 - Geology and quality of water in the Modesto-Merced area, San Joaquin Valley, California, with a brief section on hydrology","interactions":[],"lastModifiedDate":"2019-09-05T12:53:57","indexId":"wri736","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-6","title":"Geology and quality of water in the Modesto-Merced area, San Joaquin Valley, California, with a brief section on hydrology","docAbstract":"<p>The Modesto-Merced area includes about 1,800 square miles on the northeast side of the San Joaquin Valley. The physiographic units in the area are (1) Sierra Nevada, (2) dissected uplands, (3) low alluvial plains and fans, (4) river flood plains and channels, and (5) overflow lands.</p><p>Geologic units consist of consolidated rocks and unconsolidated deposits. The dominant structure of the geologic units is that of a homocline, which reflects the southwestward-tilted fault block of the Sierra Nevada. The consolidated rocks include: (1) basement complex (pre-Tertiary), (2) marine sandstone and shale (Cretaceous), (3) Ione Formation and other sedimentary rocks (Eocene), (4) Valley Springs Formation (late? Miocene), and (5) the Mehrten Formation (Miocene and Pliocene). In the eastern part of the area, the consolidated rocks generally yield small quantities of water to wells except for the Mehrten Formation which is an important aquifer.</p><p>The unconsolidated deposits include: (1) continental deposits (Pliocene and Pleistocene?), (2) lacustrine and marsh deposits (Pleistocene), (3) older alluvium (Pleistocene and Holocene?), (4) younger alluvium (Holocene), and (5) flood-basin deposits (Holocene). The continental deposits and older alluvium are the main water-yielding units in the unconsolidated deposits. The lacustrine and marsh deposits (E-clay) and the flood-basin deposits yield little water to wells, and the younger alluvium in most places probably yields only moderate quantities of water to wells.</p><p>There are three ground-water bodies in the Modesto-Merced area: (1) the unconfined water body, (2) the confined water body, and (3) the water body in consolidated rocks. The unconfined water body occurs in the unconsolidated deposits above and east of the E-clay, except in the western and southern parts of the area where clay lenses occur and semiconfined conditions exist. The confined water body occurs in the unconsolidated deposits below the E-clay and extends downward to the base of fresh water. The water body in consolidated rocks occurs under both perched and confined conditions.</p><p>Ground-water movement in the unconfined and the confined water bodies is generally westward toward the valley trough. In the unconfined water body, the water also moves toward the major rivers, and toward pumping depressions at Modesto and near El Nido. Because of the higher head in the unconfined water body, water slowly moves from it through the E-clay to the underlying confined water body.</p><p>Surface water is used extensively for irrigation in most of the study area; consequently, shallow water in the unconfined water body has to be controlled by pumping. Nevertheless, water levels near Modesto declined about 6 feet between 1958 and 1962, for the most part during the dry years 1959-61. Near El Nido, water levels declined about 70 feet between 1942 and 1967. In the confined water body, water levels were high in the winter and spring and low in the summer and fall, reflecting irrigation practices. In the southwestern part of the area, water levels in the confined water body declined about 14 feet from 1962 to 1968 and rose slightly after 1968, whereas in the northwestern part water levels remained fairly constant.</p><p>Water from the upper reaches of the Stanislaus, Tuolumne, Merced, and Chowchilla Rivers is calcium bicarbonate in chemical type and is of excellent quality. As those rivers cross the valley floor, their water quality is generally degraded by return flows from irrigated land, and in the Tuolumne River by saline water discharged from abandoned gas wells. Average dissolvedsolids content in the major rivers, as indicated by chemical analyses, do not exceed 400 mg/1 (milligrams per liter) except in the San Joaquin River where average dissolved-solids content has not exceeded 1,050 mg/l.</p><p>Water from minor streams in the area is bicarbonate in chemical type with dissolved-solids content ranging from 56 mg/1 to about 350 mg/l.</p><p>Although chloride-type fresh ground water occurs in the unconfined and confined water bodies and in the water body in consolidated rocks, most of the fresh ground water is a bicarbonate type that has a dissolved-solids content of less than 500 mg/l.</p><p>Water having dissolved solids in excess of about 2,000 mg/1 is considered to be saline. Saline water extends below the base of fresh water to the basement complex and, except in the extreme eastern part, underlies most of the study area. Saline water also occurs as lenses above the base of fresh water in the unconfined and confined water bodies. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri736","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Page, R.W., and Balding, G.O., 1973, Geology and quality of water in the Modesto-Merced area, San Joaquin Valley, California, with a brief section on hydrology: U.S. Geological Survey Water-Resources Investigations Report 73-6, v, 85 p., https://doi.org/10.3133/wri736.","productDescription":"v, 85 p.","costCenters":[],"links":[{"id":367180,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0006/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.5,\n              37\n            ],\n            [\n              -120,\n              37\n            ],\n            [\n              -120,\n              38\n            ],\n            [\n              -121.5,\n              38\n            ],\n            [\n              -121.5,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6842bf","contributors":{"authors":[{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Balding, Gary O.","contributorId":25210,"corporation":false,"usgs":true,"family":"Balding","given":"Gary","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":200747,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30114,"text":"wri737 - 1973 - Magnitude and frequency of floods in small drainage basins in Idaho","interactions":[],"lastModifiedDate":"2018-11-16T09:53:15","indexId":"wri737","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-7","title":"Magnitude and frequency of floods in small drainage basins in Idaho","docAbstract":"<p>A method is presented in this report for determining magnitude and frequency of floods on streams with drainage areas between 0.5 and 200 square miles. The method relates basin characteristics, including drainage area, percentage of forest cover, percentage of water area, latitude, and longitude, with peak flow characteristics. </p><p>Regression equations for each of eight regions are presented for determination of QIQ/ the peak discharge, which, on the average, will be exceeded once in 10 years. Peak flows, Q25 and Q 50 , can then be estimated from Q25/Q10 and Q-50/Q-10 ratios developed for each region. Nomographs are included which solve the equations for basins between 1 and 50 square miles. </p><p>The regional regression equations were developed using multiple regression techniques. Annual peaks for 303 sites were analyzed in the study. These included all records on unregulated streams with drainage areas less than about 500 square miles with 10 years or more of record or which could readily be extended to 10 years on the basis of nearby streams. The log-Pearson Type III method as modified and a digital computer were employed to estimate magnitude and frequency of floods for each of the 303 gaged sites. A large number of physical and climatic basin characteristics were determined for each of the gaged sites. The multiple regression method was then applied to determine the equations relating the floodflows and the most significant basin characteristics. For convenience of the users, several equations were simplified and some complex characteristics were deleted at the sacrifice of some increase in the standard error. Standard errors of estimate and many other statistical data were computed in the analysis process and are available in the Boise district office files. The analysis showed that QIQ was the best defined and most practical index flood for determination of the Q25 and 0,50 flood estimates.</p><p>Regression equations are not developed because of poor definition for areas which total about 20,000 square miles, most of which are in southern Idaho. These areas are described in the report to prevent use of regression equations where they do not apply. They include urbanized areas, streams affected by regulation or diversion by works of man, unforested areas, streams with gaining or losing reaches, streams draining alluvial valleys and the Snake Plain, intense thunderstorm areas, and scattered areas where records indicate recurring floods which depart from the regional equations. Maximum flows of record and basin locations are summarized in tables and maps. </p><p>The analysis indicates deficiencies in data exist. To improve knowledge regarding flood characteristics in poorly defined areas, the following data-collection programs are recommended. Gages should be operated on a few selected small streams for an extended period to define floods at long recurrence intervals. Crest-stage gages should be operated in representative basins in urbanized areas, newly developed irrigated areas and grasslands, and in unforested areas. Unusual floods should continue to be measured at miscellaneous sites on regulated streams and in intense thunderstorm-prone areas. The relationship between channel geometry and floodflow characteristics should be investigated as an alternative or supplement to operation of gaging stations. Documentation of historic flood data from newspapers and other sources would improve the basic flood-data base. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri737","usgsCitation":"Thomas, C., Harenberg, W., and Anderson, J., 1973, Magnitude and frequency of floods in small drainage basins in Idaho: U.S. Geological Survey Water-Resources Investigations Report 73-7, Report: iv, 61 p.; 3 Plates: 22.54 x 31.64 inches or smaller, https://doi.org/10.3133/wri737.","productDescription":"Report: iv, 61 p.; 3 Plates: 22.54 x 31.64 inches or 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A.","contributorId":78743,"corporation":false,"usgs":true,"family":"Harenberg","given":"W. A.","affiliations":[],"preferred":false,"id":202702,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, J.M.","contributorId":49830,"corporation":false,"usgs":true,"family":"Anderson","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":202701,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":48230,"text":"ofr741031 - 1973 - A conceptual model of the hydrologic system supplying the large springs in the Ozarks","interactions":[],"lastModifiedDate":"2012-02-02T00:10:38","indexId":"ofr741031","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"74-1031","title":"A conceptual model of the hydrologic system supplying the large springs in the Ozarks","language":"ENGLISH","doi":"10.3133/ofr741031","usgsCitation":"Feder, G.L., 1973, A conceptual model of the hydrologic system supplying the large springs in the Ozarks: U.S. Geological Survey Open-File Report 74-1031, [2], v, [2], 148 leaves : ill., maps ; 28 cm., https://doi.org/10.3133/ofr741031.","productDescription":"[2], v, [2], 148 leaves : ill., maps ; 28 cm.","costCenters":[],"links":[{"id":172598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6afb7a","contributors":{"authors":[{"text":"Feder, Gerald Leon","contributorId":71242,"corporation":false,"usgs":true,"family":"Feder","given":"Gerald","email":"","middleInitial":"Leon","affiliations":[],"preferred":false,"id":237004,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48035,"text":"ofr72163 - 1973 - Low-flow characteristics of streams in the Puget Sound region, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"ofr72163","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"72-163","title":"Low-flow characteristics of streams in the Puget Sound region, Washington","docAbstract":"Periods of low streamflow are usually the most critical factor in relation to most water uses. The purpose of this report is to present data on low-flow characteristics of streams in the Puget Sound region, Washington, and to briefly explain some of the factors that influence low flow in the various basins. \r\n\r\nPresented are data on low-flow frequencies of streams in the Puget Sound region, as gathered at 150 gaging stations. Four indexes were computed from the flow-flow-frequency curves and were used as a basis to compare the low-flow characteristics of the streams. The indexes are the (1) low-flow-yield index, expressed in unit runoff per square mile; (2) base-flow index, or the ratio of the median 7-day low flow to the average discharge; (3) slope index, or slope of annual 7-day low-flow-frequency curve; and (4) spacing index, or spread between the 7-day and 183-day low-flow-frequency curves. The indexes showed a wide variation between streams due to the complex interrelation between climate, topography, and geology. \r\n\r\nThe largest low-flow-yield indexes determined--greater than 1.5 cfs (cubic feet per second) per square mile--were for streams that head at high altitudes in the Cascade and Olympic Mountains and have their sources at glaciers. The smallest low-flow-yield indexes--less than 0.5 cfs per square mile--were for the small streams that drain the lowlands adjacent to Puget Sound. Indexes between the two extremes were for nonglacial streams that head at fairly high altitudes in areas of abundant precipitation. \r\n\r\nThe base-flow index has variations that can be attributed to a basin's hydrogeology, with very little influence from climate. The largest base-flow indexes were obtained for streams draining permeable unconsolidated glacial and alluvial sediments in parts of the lowlands adjacent to Puget Sound. Large volume of ground water in these materials sustain flows during late summer. The smallest indexes were computed for streams draining areas underlain by relatively impermeable igneous, sedimentary, and metamorphic rocks or by relatively impermeable glacial till. Melt water from snow and ice influences the index for streams which originate at glaciers, and result in fairly large indexes--0.25 or greater. \r\n\r\nThe slope index is influenced principally by the character of the geologic materials that underlie the basin. The largest slope indexes were computed for small streams that drain areas underlain by compact glacial till or consolidated sedimentary rocks. In contrast, lowland streams that flow through areas underlain by unconsolidated alluvia and glacial deposits have the smallest indexes. Small slope indexes also are characteristic of glacial streams and show the moderating effect of the snow and ice storage in the high mountain basins. \r\n\r\nThe spacing indexes are similar to the slope indexes in that they are affected by the character of the geologic materials underlying a basin. The largest spacing indexes are characteristic of small streams whose basins are underlain by glacial till or by consolidated sedimentary rocks. The smallest indexes were computed for some lowland streams draining areas underlain by permeable glacial and alluvial sediments. \r\n\r\nThe indexes do not appear to have a definite relation to each other. The low-flow-yield indexes are not related to either the slope or spacing indexes because snow and ice storage has a great influence on the low-flow-yield index, while the character of the geologic materials influences the slope and spacing indexes. A relation exists between the slope and spacing indexes but many anomalies occur that cannot be explained by the geology of the basins.","language":"ENGLISH","doi":"10.3133/ofr72163","usgsCitation":"Hidaka, F., 1973, Low-flow characteristics of streams in the Puget Sound region, Washington: U.S. Geological Survey Open-File Report 72-163, 162 p. ill., maps (1 col.) ; 27 cm., https://doi.org/10.3133/ofr72163.","productDescription":"162 p. ill., maps (1 col.) ; 27 cm.","costCenters":[],"links":[{"id":170224,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0163/report-thumb.jpg"},{"id":84804,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0163/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84805,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0163/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6486e8","contributors":{"authors":[{"text":"Hidaka, F.T.","contributorId":48542,"corporation":false,"usgs":true,"family":"Hidaka","given":"F.T.","email":"","affiliations":[],"preferred":false,"id":236708,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28181,"text":"wri734 - 1973 - Data requirements for modeling a ground-water system in an arid region","interactions":[],"lastModifiedDate":"2019-07-10T09:49:57","indexId":"wri734","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-4","title":"Data requirements for modeling a ground-water system in an arid region","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri734","usgsCitation":"Kunkel, F., 1973, Data requirements for modeling a ground-water system in an arid region: U.S. Geological Survey Water-Resources Investigations Report 73-4, iii, 21 p., https://doi.org/10.3133/wri734.","productDescription":"iii, 21 p.","costCenters":[],"links":[{"id":365425,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0004/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158957,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0004/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679c83","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":199346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46354,"text":"ofr73335 - 1973 - Atlas of Mars, Margaritifer Sinus Quadrangle, MC-19","interactions":[],"lastModifiedDate":"2024-08-05T21:53:35.503048","indexId":"ofr73335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-335","title":"Atlas of Mars, Margaritifer Sinus Quadrangle, MC-19","docAbstract":"<p>This mosaic was made with Mariner 9 pictures provided by the Jet Propulsion Laboratory (JPL), California Institute of Technology. The Image Processing Laboratory (IPL) of JPL processed the digital pictures to remove image artifacts and geometric distortions, to enhance high - frequency topographic detail while subduing low-frequency albedo variation, and to transform the pictures to a Mercator projection. The U.S. Geological Survey performed further artifact removal and modified contrast and tone of each picture analytically on the digital magnetic tapes provided by IPL for uniformity of tone and contrast within the mosaic. Photographic reproductions of the pictures were generated from the magnetic tapes and mosaicked by the U. S. Geological Survey.</p><p>Primary horizontal control points, where available, controlled the placement of pictures. Where these points were not available, picture placement was controlled by spacecraft tracking data and by matching images in overlap zones between pictures. Discrepancies in matching these images are less than 10 km over 90% of the mosaic. The number designations and positions of the primary control points, shown by broken crosses (-l-), are those given by Davies and Arthur (1973).</p><p>Aerographic latitudes are shown on this mosaic. The projection is based on a theoretical dynamical ellipticity of 1/192. The scale is based on an equatorial radius of 3393. 4 km.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73335","usgsCitation":"United States Geological Survey, 1973, Atlas of Mars, Margaritifer Sinus Quadrangle, MC-19: U.S. Geological Survey Open-File Report 73-335, 1 Plate: 22.92 x 26.05 inches, https://doi.org/10.3133/ofr73335.","productDescription":"1 Plate: 22.92 x 26.05 inches","costCenters":[],"links":[{"id":432234,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0335/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171947,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0335/report-thumb.jpg"}],"scale":"5000000","projection":"Mercator Projection","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fac0","contributors":{"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":531677,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46358,"text":"ofr73339 - 1973 - Atlas of Mars chart, Aeolis Quadrangle, MC-23","interactions":[],"lastModifiedDate":"2024-08-05T22:00:55.820486","indexId":"ofr73339","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-339","title":"Atlas of Mars chart, Aeolis Quadrangle, MC-23","docAbstract":"<p><span>This mosaic was made with Mariner 9 pictures provided by the Jet Propulsion Laboratory (JPL), California Institute of Technology. The Image Processing Laboratory (IPL) of JPL processed the digital pictures to remove image artifacts and geometric distortions, to enhance high-frequency topographic detail while subduing low-frequency albedo variation, and to transform the pictures to a Mercator projection. The U.S. Geological Survey performed further artifact removal and modified contrast and tone of each picture analytically on the digital magnetic tapes provided by IPL for uniformity of tone and contrast within the mosaic. Photographic reproductions of the pictures were generated from the magnetic tapes and mosaicked by the U.S. Geological Survey.</span></p><p><span>Primary horizontal control points, where available, controlled the placement of pictures. Where these points were not available, picture placement was controlled by spacecraft tracking data and by matching images in overlap zones between pictures. Discrepancies in matching these images are less than 10 km over 90% of the mosaic. The number designations and positions of the primary control points, shown by broken crosses (-l-), are those given by Davies and Arthur (1973).</span></p><p><span>Aerographic latitudes are shown on this mosaic. The projection is based on a theoretical dynamical ellipticity of 1/192. The scale is based on an equatorial radius of 3393. 4 km.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73339","collaboration":"Prepared in cooperation with the Jet Propulsion Laboratory, California Insititute of Technology and the National Aeronautics and Space Administration","usgsCitation":"United States Geological Survey, 1973, Atlas of Mars chart, Aeolis Quadrangle, MC-23: U.S. Geological Survey Open-File Report 73-339, 1 Plate: 23.20 x 26.49 inches, https://doi.org/10.3133/ofr73339.","productDescription":"1 Plate: 23.20 x 26.49 inches","costCenters":[],"links":[{"id":432248,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0339/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171951,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0339/report-thumb.jpg"}],"scale":"5000000","projection":"Mercator Projection","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60faf3","contributors":{"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":531681,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39113,"text":"pp306E - 1973 - Geology and paleontology of Canal Zone and adjoining parts of Panama: Description of Tertiary mollusks (additions to gastropods, scaphopods, pelecypods Nuculidae to Malleidae)","interactions":[],"lastModifiedDate":"2017-11-29T09:21:36","indexId":"pp306E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"306","chapter":"E","title":"Geology and paleontology of Canal Zone and adjoining parts of Panama: Description of Tertiary mollusks (additions to gastropods, scaphopods, pelecypods Nuculidae to Malleidae)","docAbstract":"<p>Chapter E adds 112 described species and subspecies (a few briefly described) to the some 440 covered in preceding chapters : 27 additional gastropods, 18 scaphopods, and 67 pelecypods in 10 families. It is estimated that about 125 species are to be added in chapter F, the final chapter.</p><p>The Arcidae is by far the largest family in the pelecypods so far studied : 30 species in six genera. The genus <i>Anadara</i> is the largest in that family : 25 species, representing the subgenera <i>Hawaiarca?</i>, <i>Rasia, Tosarca, Grandiarca, Potiarca</i>, and <i>Cunearca</i>. <i>Potiarca</i>, based on a living western Pacific species, is adopted for many American species heretofore assigned to <i>Cunearca</i>.</p><p>Eighteen of the 27 additional gastropods were found at a new locality in the late Eocene part of the Gatuncillo formation. They 'are assigned to 16 genera, 14 of which are not represented at other Gatuncillo localities. The genera include <i>Faunus, Turnpanotonos</i>, and <i>Bezaneonia</i>, which are rare in America, and the rare endemic American genus <i>Harrisianella</i>.</p><p>The marine member of the Bohio (?) formation is now assigned to the late Eocene, instead of late Eocene or early Oligocene—the only change in age assignment. Eocene affinities are especially strengthened by the presence of <i>Samanoetia samanensis</i> and <i>Volvariella?</i>, if indeed the unnamed species represents that genus, as seems likely. Both the marine member of the Bohio( ?) and the late Oligocene part of the Bohio contain early small species of <i>Anadara</i>, subgenus <i>Rasia</i>.</p><p>The fossils from the moderately deep-water facies of the late Oligocene Caimito formation include the earliest hexagonal <i>Dentalium</i> of the subgenus <i>Dentalium</i> s.s., from the American mainland, and a widespread and abundant species of the essentially deep-water subgenus <i>Fissidentalium</i>.</p><p><i>Anadara chiriquiensis chiriquiensis</i>, a relatively small form of the subgenus <i>Grandiarca</i> that is widely distributed in the Miocene Caribbean province, occurs in the Culebra formation. For the most part it indicates brackish water.</p><p>Among the fossils from the La Boca formation proper, <i>Cyphoma</i> aff. <i>C. intermedia</i> is the earliest representative of an endemic American genus, and <i>Isognomon mimeticus</i>, a remarkable, narrowly mytiliform species is the type of the new subgenus <i>Mimonion</i>. Both the Culebra and La Boca, both of early Miocene age, contain predecessors of Gatun species.</p><p>As in other chapters, the largest number of species is from the middle Miocene Gatun formation: 50 species. <i>Bailya crossata</i> is the first Tertiary species of the genus from the Caribbean region, and the earliest now known. A bizarre, incomplete gastropod is described as xancid?, genus?. The Gatun contains 13&nbsp;of the 24 species of <i>Anadara</i> and half of the 12 species of the subgenus <i>Rasia</i> of that genus. In consideration of two battered and worn specimens of a large form of the subgenus <i>Grandiarca</i>, identified as <i>Anadara grandis patricia?</i>, the similar Tertiary forms in the Caribbean region are reviewed and divided into a brackish-water group and a marine group. The Gatun fauna now totals some 330 species.&nbsp;</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp306E","usgsCitation":"Woodring, W., 1973, Geology and paleontology of Canal Zone and adjoining parts of Panama: Description of Tertiary mollusks (additions to gastropods, scaphopods, pelecypods Nuculidae to Malleidae): U.S. Geological Survey Professional Paper 306, iii, 86 p., https://doi.org/10.3133/pp306E.","productDescription":"iii, 86 p.","startPage":"453","endPage":"539","numberOfPages":"128","costCenters":[],"links":[{"id":120014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0306e/report-thumb.jpg"},{"id":66572,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0306e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Panama","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6843e6","contributors":{"authors":[{"text":"Woodring, W. P.","contributorId":48230,"corporation":false,"usgs":true,"family":"Woodring","given":"W. P.","affiliations":[],"preferred":false,"id":220980,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46357,"text":"ofr73338 - 1973 - Alas of Mars chart, Mare Tyrrhenum Quadrangle, MC-22","interactions":[{"subject":{"id":46357,"text":"ofr73338 - 1973 - Alas of Mars chart, Mare Tyrrhenum Quadrangle, MC-22","indexId":"ofr73338","publicationYear":"1973","noYear":false,"title":"Alas of Mars chart, Mare Tyrrhenum Quadrangle, MC-22"},"predicate":"SUPERSEDED_BY","object":{"id":65886,"text":"i1123 - 1978 - Shaded relief map of the Mare Tyrrhenum Quadrangle of Mars","indexId":"i1123","publicationYear":"1978","noYear":false,"title":"Shaded relief map of the Mare Tyrrhenum Quadrangle of Mars"},"id":1}],"supersededBy":{"id":65886,"text":"i1123 - 1978 - Shaded relief map of the Mare Tyrrhenum Quadrangle of Mars","indexId":"i1123","publicationYear":"1978","noYear":false,"title":"Shaded relief map of the Mare Tyrrhenum Quadrangle of Mars"},"lastModifiedDate":"2024-08-05T22:04:08.165867","indexId":"ofr73338","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-338","title":"Alas of Mars chart, Mare Tyrrhenum Quadrangle, MC-22","docAbstract":"<p><span>This mosaic was made with Mariner 9 pictures provided by the Jet Propulsion Laboratory (JPL), California Institute of Technology. The Image Processing Laboratory (IPL) of JPL processed the digital pictures to remove image artifacts and geometric distortions, to enhance high-frequency topographic detail while subduing low-frequency albedo variation, and to transform the pictures to a Mercator projection. The U.S. Geological Survey performed further artifact removal and modified contrast and tone of each picture analytically on the digital magnetic tapes provided by IPL for uniformity of tone and contrast within the mosaic. Photographic reproductions of the pictures were generated from the magnetic tapes and mosaicked by the U.S. Geological Survey.</span></p><p><span>Primary horizontal control points, where available, controlled the placement of pictures. Where these points were not available, picture placement was controlled by spacecraft tracking data and by matching images in overlap zones between pictures. Discrepancies in matching these images are less than 10 km over 90% of the mosaic. The number designations and positions of the primary control points, shown by broken crosses (-l-), are those given by Davies and Arthur (1973).</span></p><p><span>Aerographic latitudes are shown on this mosaic. The projection is based on a theoretical dynamical ellipticity of 1/192. The scale is based on an equatorial radius of 3393. 4 km.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73338","usgsCitation":"United States Geological Survey, 1973, Alas of Mars chart, Mare Tyrrhenum Quadrangle, MC-22: U.S. Geological Survey Open-File Report 73-338, 1 Plate: 23.87 x 26.82 inches, https://doi.org/10.3133/ofr73338.","productDescription":"1 Plate: 23.87 x 26.82 inches","costCenters":[],"links":[{"id":432250,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0338/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171950,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0338/report-thumb.jpg"}],"scale":"5000000","projection":"Mercator Projection","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fae8","contributors":{"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":531680,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}