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,{"id":62434,"text":"gq1181 - 1974 - Geologic map of the Spurlington quadrangle, Marion and Taylor Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:51","indexId":"gq1181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1181","title":"Geologic map of the Spurlington quadrangle, Marion and Taylor Counties, Kentucky","language":"ENGLISH","doi":"10.3133/gq1181","usgsCitation":"Moore, S.L., 1974, Geologic map of the Spurlington quadrangle, Marion and Taylor Counties, Kentucky: U.S. Geological Survey Geologic Quadrangle 1181, 1 map., https://doi.org/10.3133/gq1181.","productDescription":"1 map.","costCenters":[],"links":[{"id":107612,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10720.htm","linkFileType":{"id":5,"text":"html"},"description":"10720"},{"id":248603,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1181/report.pdf","size":"38","linkFileType":{"id":1,"text":"pdf"}},{"id":253747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1181/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.36749999999999,37.3675 ], [ -85.36749999999999,37.5 ], [ -85.25,37.5 ], [ -85.25,37.3675 ], [ -85.36749999999999,37.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68aa60","contributors":{"authors":[{"text":"Moore, Samuel L.","contributorId":88727,"corporation":false,"usgs":true,"family":"Moore","given":"Samuel","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":267374,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3602,"text":"cir690 - 1974 - Seismic hazards and land-use planning","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"cir690","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"690","title":"Seismic hazards and land-use planning","docAbstract":"Basic earth-science data are necessary for a realistic assessment of seismic hazards and as a basis for limiting corrective land-use controls only to those areas of greatest hazard. For example, the location, character, and amount of likely displacement and activity of surface faulting can be predicted if detailed geologic maps and seismic data are available and are augmented by field studies at critical localities. Because few structures can withstand displacement of their foundations, they should be located off active fault traces, the distance varying with the character of faulting, the certainty with which fault traces are known, and the importance of the structure. Recreational activities and other nonoccupancy land uses should be considered for fault zone areas where land is under pressure for development; elsewhere, such areas should remain as open space. \r\n\r\nTwo methods of predicting ground shaking effects have applications to land-use decisions: (1) Relative earthquake effects can be related to firmness of the ground and can be used in a gross way to allocate population density in the absence of more sophisticated analyses; and (2) intensity maps, based on, (a) damage from former earthquakes, or (b) a qualitative analyses of geologic units added to a design earthquake, can be helpful both for general and specific plans. Theoretical models are used with caution to predict ground motion for critical structures to be located at specific sites with unique foundation conditions. Fully adequate methods of assessing possible shaking remain to be developed. Where land-use decisions do not reflect likely ground shaking effects, stringent building codes are needed, particularly for important structures. \r\n\r\nGround failure (landsliding, ground cracking and lurching, differential settlement, sand boils, and subsidence) commonly results from liquefaction, loss of soil strength, or compaction. Areas suspected of being most likely to fail should not be developed unless detailed site studies can demonstrate the hazard does not exist or can be overcome. Various methods can be used to reduce the high, long-term public costs that follow development of unstable ground. However, areas subject to tectonic deformation generally cannot be predicted nor can effects of such deformation be minimized. \r\n\r\nLarge water waves, such as produced by tsunamis, seiches, and dam failure or overtopping, can be anticipated in many places. Their effects can be lessened by land-use regulations similar to flood-plain zoning, restrictions on location of critical structures, and appropriate warning systems. \r\n\r\nMany local, state, and federal government agencies, universities, and private consultants may be able to assist planners by advising them of pertinent data and where those data can be obtained. Interpretation of the data for an evaluation of seismic risk commonly requires a team of planners, geologists, and soil and structural engineers.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir690","usgsCitation":"Nichols, D.R., and Buchanan-Banks, J.M., 1974, Seismic hazards and land-use planning: U.S. Geological Survey Circular 690, iv, 33 p. :ill. ;27 cm., https://doi.org/10.3133/cir690.","productDescription":"iv, 33 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":124619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1974/0690/report-thumb.jpg"},{"id":30637,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1974/0690/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a879b","contributors":{"authors":[{"text":"Nichols, Donald R.","contributorId":83129,"corporation":false,"usgs":true,"family":"Nichols","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":147239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buchanan-Banks, Jane M.","contributorId":29421,"corporation":false,"usgs":true,"family":"Buchanan-Banks","given":"Jane","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":147238,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26895,"text":"wri7417 - 1974 - Hydrologic analysis of the Mojave River, California, using a mathematical model","interactions":[],"lastModifiedDate":"2018-10-29T14:32:18","indexId":"wri7417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-17","title":"Hydrologic analysis of the Mojave River, California, using a mathematical model","docAbstract":"<p>The channel of the Mojave Rive'r in California is normally dry and is highly permeable over much of its length, and large quantities of water from natural floodflows in the channel infiltrate through the channel bed to the underlying ground-water body. From 1930 to 1972 only 18 floods at The Forks produced flow at Barstow, 55 miles (88 kilometres) downstream from The Forks. Peak discharges at Barstow from these floods ranged from 180 cubic feet per second (5 cubic metres per second) in 1967 to 64,300 cubic feet per second (1,820 cubic metres per second) in 1938. Total stream infiltration, primarily as ground-water recharge, ranged from 3,600 acre-feet (4.40 cubic hectometres) in 1935 to 50,400 acre-feet (62.1 cubic hectometres) in 1969 between The Forks and Victorville and from about 7,000 acre-feet (8.61 cubic hectometres) in 1935 to 128,000 acre-feet (158 cubic hectometres) in 1969 between Victorville and Barstow.</p><p>The Mojave Water Agency is considering the use of the channel of the river to convey water imported from northern California through Silverwood Reservoir (5 miles or 8 kilometres upstream from The Forks) downstream to the Barstow area. The imported water would be used to replenish aquifers underlying the Barstow area. A mathematical model was developed that simulates the advance of discharge down the initially dry channel of the Mojave River, and the model was used to evaluate the potential of the channel to move imported water downstream to Barstow.</p><p>Results of simulation by modeling indicate that the channel of the Mojave River can be used to efficiently convey imported water to Barstow only when the absorption capacity of the channel has been reduced by an antecedent flood. The volume of imported water that can reach Barstow depends on the volume and duration of the antecedent flood, on the volume of imported water released trom Silverwood Reservoir, and on the rate at which imported water is released. A release of 20,000 acre-feet (24.6 cubic hectometres) of imported water may produce at Barstow a maximum volume of imported water of 2,500, 8,000, 11,000, or 15,000 acre-feet (3.08, 9.86, 13.6, or 18.4 cubic hectometres) for a release rate of 500, 750, 1,000, or 2,000 cubic feet per second (14.2, 21.2, 28.3, or 56.8 cubic metres per second).</p><p>For planning purposes in evaluating some of the hydraulic effects of recharge on the aquifer, a simulation of the aquifer near the Barstow area using an electrical analog model showed that a combination of no pumping and a yearly recharge of 5,000 acre-feet (6.17 cubic hectometres) for 10 years could raise ground-water levels at least 10 feet (3 metres) over an area of about 10 square miles (25 square kilometres). To obtain the water-level changes due to the combined effects of pumping and recharge, the above water-level changes should be superimposed on the separate effects of pumping.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7417","usgsCitation":"Durbin, T.J., and Hardt, W.F., 1974, Hydrologic analysis of the Mojave River, California, using a mathematical model: U.S. Geological Survey Water-Resources Investigations Report 74-17, v, 50 p., https://doi.org/10.3133/wri7417.","productDescription":"v, 50 p.","costCenters":[],"links":[{"id":157467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0017/report-thumb.jpg"},{"id":358909,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0017/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Mojave River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.42187500000001,\n              34.26289150646404\n            ],\n            [\n              -117.00576782226562,\n              34.26289150646404\n            ],\n            [\n              -117.00576782226562,\n              34.91521472314689\n            ],\n            [\n              -117.42187500000001,\n              34.91521472314689\n            ],\n            [\n              -117.42187500000001,\n              34.26289150646404\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611900","contributors":{"authors":[{"text":"Durbin, Timothy J.","contributorId":63373,"corporation":false,"usgs":true,"family":"Durbin","given":"Timothy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hardt, W. F.","contributorId":12455,"corporation":false,"usgs":true,"family":"Hardt","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197203,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62336,"text":"gq1177 - 1974 - Geologic map of the Rudolph Hill quadrangle, Gunnison, Hinsdale, and Saguache Counties, Colorado","interactions":[{"subject":{"id":15256,"text":"ofr73213 - 1973 - Geologic map of the Rudolph Hill quadrangle, Gunnison, Hinsdale, and Saguache Counties, Colorado","indexId":"ofr73213","publicationYear":"1973","noYear":false,"title":"Geologic map of the Rudolph Hill quadrangle, Gunnison, Hinsdale, and Saguache Counties, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":62336,"text":"gq1177 - 1974 - Geologic map of the Rudolph Hill quadrangle, Gunnison, Hinsdale, and Saguache Counties, Colorado","indexId":"gq1177","publicationYear":"1974","noYear":false,"title":"Geologic map of the Rudolph Hill quadrangle, Gunnison, Hinsdale, and Saguache Counties, Colorado"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq1177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1177","title":"Geologic map of the Rudolph Hill quadrangle, Gunnison, Hinsdale, and Saguache Counties, Colorado","language":"ENGLISH","doi":"10.3133/gq1177","usgsCitation":"Olson, J.C., 1974, Geologic map of the Rudolph Hill quadrangle, Gunnison, Hinsdale, and Saguache Counties, Colorado: U.S. Geological Survey Geologic Quadrangle 1177, 1 map :col. ;58 x 46 cm. folded to 28 x 20 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/gq1177.","productDescription":"1 map :col. ;58 x 46 cm. folded to 28 x 20 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107914,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11025.htm","linkFileType":{"id":5,"text":"html"},"description":"11025"},{"id":248515,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1177/report.pdf","size":"71","linkFileType":{"id":1,"text":"pdf"}},{"id":253576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1177/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.11749999999999,38.1175 ], [ -107.11749999999999,38.25 ], [ -107,38.25 ], [ -107,38.1175 ], [ -107.11749999999999,38.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68beee","contributors":{"authors":[{"text":"Olson, Jerry Chipman","contributorId":57869,"corporation":false,"usgs":true,"family":"Olson","given":"Jerry","email":"","middleInitial":"Chipman","affiliations":[],"preferred":false,"id":267244,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62376,"text":"gq1151 - 1974 - Surficial geologic map of the Natick quadrangle, Middlesex and Norfolk Counties, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-10T00:10:47","indexId":"gq1151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1151","title":"Surficial geologic map of the Natick quadrangle, Middlesex and Norfolk Counties, Massachusetts","language":"ENGLISH","doi":"10.3133/gq1151","usgsCitation":"Nelson, A.E., 1974, Surficial geologic map of the Natick quadrangle, Middlesex and Norfolk Counties, Massachusetts: U.S. Geological Survey Geologic Quadrangle 1151, 1 map., https://doi.org/10.3133/gq1151.","productDescription":"1 map.","costCenters":[],"links":[{"id":107585,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10691.htm","linkFileType":{"id":5,"text":"html"},"description":"10691"},{"id":248551,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1151/report.pdf","size":"26","linkFileType":{"id":1,"text":"pdf"}},{"id":253695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1151/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.36749999999999,42.25 ], [ -71.36749999999999,42.3675 ], [ -71.25,42.3675 ], [ -71.25,42.25 ], [ -71.36749999999999,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688fbe","contributors":{"authors":[{"text":"Nelson, Arthur E.","contributorId":6035,"corporation":false,"usgs":true,"family":"Nelson","given":"Arthur","email":"","middleInitial":"E.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":267299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38998,"text":"pp352J - 1974 - Chemical weathering, soil development, and geochemical fractionation in a part of the White Mountains, Mono and Inyo counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:15","indexId":"pp352J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"352","chapter":"J","title":"Chemical weathering, soil development, and geochemical fractionation in a part of the White Mountains, Mono and Inyo counties, California","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Erosion and sedimentation in a semiarid environment","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp352J","usgsCitation":"Marchand, D.E., 1974, Chemical weathering, soil development, and geochemical fractionation in a part of the White Mountains, Mono and Inyo counties, California: U.S. Geological Survey Professional Paper 352, 45 p., https://doi.org/10.3133/pp352J.","productDescription":"45 p.","costCenters":[],"links":[{"id":120469,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0352j/report-thumb.jpg"},{"id":66111,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0352j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e31e6","contributors":{"authors":[{"text":"Marchand, D. E.","contributorId":86004,"corporation":false,"usgs":true,"family":"Marchand","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":220786,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":217,"text":"wsp2150 - 1974 - Quality of surface waters of the United States, 1969, Parts 12-16, North Pacific slope basins, Alaska, Hawaii, and other Pacific areas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp2150","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"2150","title":"Quality of surface waters of the United States, 1969, Parts 12-16, North Pacific slope basins, Alaska, Hawaii, and other Pacific areas","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/wsp2150","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Quality of surface waters of the United States, 1969, Parts 12-16, North Pacific slope basins, Alaska, Hawaii, and other Pacific areas: U.S. Geological Survey Water Supply Paper 2150, xiii, 480 p. :tables ;23 cm., https://doi.org/10.3133/wsp2150.","productDescription":"xiii, 480 p. :tables ;23 cm.","costCenters":[],"links":[{"id":137370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2150/report-thumb.jpg"},{"id":24828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2150/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6518dc","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":527246,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62761,"text":"gq1147 - 1974 - Geologic map of parts of the Dekoven and Saline Mines quadrangles, Crittenden and Union Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:42","indexId":"gq1147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1147","title":"Geologic map of parts of the Dekoven and Saline Mines quadrangles, Crittenden and Union Counties, Kentucky","language":"ENGLISH","doi":"10.3133/gq1147","usgsCitation":"Kehn, T.M., 1974, Geologic map of parts of the Dekoven and Saline Mines quadrangles, Crittenden and Union Counties, Kentucky: U.S. Geological Survey Geologic Quadrangle 1147, 1 map., https://doi.org/10.3133/gq1147.","productDescription":"1 map.","costCenters":[],"links":[{"id":107581,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10687.htm","linkFileType":{"id":5,"text":"html"},"description":"10687"},{"id":248916,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1147/report.pdf","size":"43","linkFileType":{"id":1,"text":"pdf"}},{"id":254391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1147/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.11749999999999,37.5 ], [ -88.11749999999999,37.6175 ], [ -88,37.6175 ], [ -88,37.5 ], [ -88.11749999999999,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a287f","contributors":{"authors":[{"text":"Kehn, Thomas M.","contributorId":64219,"corporation":false,"usgs":true,"family":"Kehn","given":"Thomas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":267824,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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