{"pageNumber":"5814","pageRowStart":"145325","pageSize":"25","recordCount":184582,"records":[{"id":20271,"text":"ofr78959 - 1978 - Hydrologic information for land-use planning, Fairbanks vicinity, Alaska","interactions":[],"lastModifiedDate":"2021-12-17T22:40:18.314429","indexId":"ofr78959","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-959","title":"Hydrologic information for land-use planning, Fairbanks vicinity, Alaska","docAbstract":"The flood plain on the Chena and Tanana Rivers near Fairbanks, Alaska, has abundant water in rivers and in an unconfined alluvial aquifer. The principal source of ground water is the Tanana River, from which ground water flows northwesterly to the Chena River. Transmissivity of the aquifer commonly exceed 100 ,000 sq ft. The shallow water table (less than 15 ft below land surface), high hydraulic conductivity of the sediments and cold soil give the flood plain a high susceptibility to pollution by onsite sewerage systems. The Environmental Protection Agency recommended maximum concentrations for drinking water may be exceeded in surface water for manganese and bacteria and in ground water for iron, manganese, and bacteria. Residents of the uplands obtain water principally from a widely-distributed fractured schist aquifer. The aquifer is recharged by local infiltration of precipitation and is drained by springs on the lower slopes and by ground-water flow to alluvial aquifers of the valleys. The annual base flow from basins in the uplands ranged from 3,000 to 100,000 gallons per acre; the smallest base flows occur in basins nearest the city of Fairbanks. The thick silt cover and great depth to the water table give much of the uplands a low susceptibility to pollution by onsite sewage disposal. Ground water is locally high in nitrate, arsenic, iron , and manganese. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78959","usgsCitation":"Nelson, G.L., 1978, Hydrologic information for land-use planning, Fairbanks vicinity, Alaska: U.S. Geological Survey Open-File Report 78-959, vi, 47 p., https://doi.org/10.3133/ofr78959.","productDescription":"vi, 47 p.","costCenters":[],"links":[{"id":152287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94448,"rank":800,"type":{"id":15,"text":"Index Page"},"url":"https://dggs.alaska.gov/pubs/id/11192"},{"id":393068,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14970.htm"}],"country":"United States","state":"Alaska","city":"Fairbanks","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -148.326416015625,\n              64.73429692356085\n            ],\n            [\n              -147.3211669921875,\n              64.73429692356085\n            ],\n            [\n              -147.3211669921875,\n              65.00026079026213\n            ],\n            [\n              -148.326416015625,\n              65.00026079026213\n            ],\n            [\n              -148.326416015625,\n              64.73429692356085\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606a25","contributors":{"authors":[{"text":"Nelson, Gordon L.","contributorId":55443,"corporation":false,"usgs":true,"family":"Nelson","given":"Gordon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":182362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7591,"text":"ofr78586 - 1978 - Uranium and phosphate resources in the Cooper Formation of the Charleston region, South Carolina","interactions":[{"subject":{"id":7591,"text":"ofr78586 - 1978 - Uranium and phosphate resources in the Cooper Formation of the Charleston region, South Carolina","indexId":"ofr78586","publicationYear":"1978","noYear":false,"title":"Uranium and phosphate resources in the Cooper Formation of the Charleston region, South Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":70047792,"text":"70047792 - 1977 - Uranium and phosphate resources in Cooper Formation in the Charleston region, South Carolina","indexId":"70047792","publicationYear":"1977","noYear":false,"title":"Uranium and phosphate resources in Cooper Formation in the Charleston region, South Carolina"},"id":1}],"supersededBy":{"id":70047792,"text":"70047792 - 1977 - Uranium and phosphate resources in Cooper Formation in the Charleston region, South Carolina","indexId":"70047792","publicationYear":"1977","noYear":false,"title":"Uranium and phosphate resources in Cooper Formation in the Charleston region, South Carolina"},"lastModifiedDate":"2023-02-21T22:12:39.367211","indexId":"ofr78586","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-586","title":"Uranium and phosphate resources in the Cooper Formation of the Charleston region, South Carolina","docAbstract":"<p>Phosphate deposits formerly exploited in the Charleston district were formed by weathering and reworking of the Cooper Formation (Eocene and Oliogcene). Previous workers have shown that unusual concentrations of uranium occur in phosphate-rich nodular material formed during subareal weathering. We found that the old mining district is on an erosional high of the Cooper Formation and in a topographic depression, but that the process of weathering enrichment of the Cooper Formation extends beyond the mining district.</p><p>Fresh sediments from the Cooper Formation average 14.5 ppm uranium and 1.0 percent P<sub>2</sub>0<sub>5</sub> for Oliogcene samples and 5.6 ppm U and 0.15 percent P<sub>2</sub>0<sub>5</sub> for Eocene samples. Zones of secondary enrichment over undifferentiated Cooper Formation average 2 m thick and have average values of 60 ppm U and 5.4 percent P<sub>2</sub>0<sub>5</sub>. No deposits clearly of economic importance were found, although detailed studies may reveal such deposits.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78586","usgsCitation":"Force, E.R., Gohn, G.S., Force, L., and Higgins, B., 1978, Uranium and phosphate resources in the Cooper Formation of the Charleston region, South Carolina: U.S. Geological Survey Open-File Report 78-586, Report: 22 p.; 1 Plate: 41.09 x 34.02 inches, https://doi.org/10.3133/ofr78586.","productDescription":"Report: 22 p.; 1 Plate: 41.09 x 34.02 inches","costCenters":[],"links":[{"id":413245,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0586/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413244,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0586/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139871,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0586/report-thumb.jpg"}],"country":"United States","state":"South Carolina","city":"Charleston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.07845793912077,\n              32.896452667136515\n            ],\n            [\n              -80.07845793912077,\n              32.693957168154824\n            ],\n            [\n              -79.79328756668285,\n              32.693957168154824\n            ],\n            [\n              -79.79328756668285,\n              32.896452667136515\n            ],\n            [\n              -80.07845793912077,\n              32.896452667136515\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605d2e","contributors":{"authors":[{"text":"Force, Eric R.","contributorId":32916,"corporation":false,"usgs":true,"family":"Force","given":"Eric","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":156243,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gohn, G. S.","contributorId":25937,"corporation":false,"usgs":true,"family":"Gohn","given":"G.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":156242,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Force, L.M.","contributorId":7266,"corporation":false,"usgs":true,"family":"Force","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":156240,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Higgins, B.B.","contributorId":8091,"corporation":false,"usgs":true,"family":"Higgins","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":156241,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7526,"text":"ofr78801 - 1978 - A statistical summary and listing of the spectrographic analyses of heavy mineral concentrate and conventional, sieved stream-sediment samples, Silver City area, New Mexico","interactions":[],"lastModifiedDate":"2026-02-19T17:57:26.57247","indexId":"ofr78801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-801","title":"A statistical summary and listing of the spectrographic analyses of heavy mineral concentrate and conventional, sieved stream-sediment samples, Silver City area, New Mexico","docAbstract":"<p>Geochemical sampling of a tier of eight 7 1/2-minute quadrangles bordered by latitudes 32° 45'and 33° 00' N. and longitudes 108° 00' and 108° 30' W. was begun in the fall of 1974 and continued seasonally until completion in the fall of 1976. These quadrangles are in southwest New Mexico and include the well-known mineral deposits of the Silver City area. The sampling was designed to gain semidetailed information on the metal-anomaly characteristics of the strongly mineralized area surrounding Silver City, New Mexico, and to seek geochemical clues for the continuation of these mineral deposits beneath overlying Tertiary volcanic rocks to the north.&nbsp;</p><p>The data obtained within areas of known mineral deposits provide information on the metallogenic processes and metal suites that both relate and distinguish metal systems. Evaluation of this information relative to the regional geologic framework and the distribution of known mineral deposits will result in the identification of additional target areas for exploration, as well as further our understanding of the geochemical characteristics of mineralized areas. Extrapolation of models developed from the study of areas of known, exposed mineralization to areas covered by Tertiary volcanic rocks, such as the northern part of this tier of quadrangles, is a promising procedure for continuing research into geochemical-anomaly characteristics of covered mineral deposits.&nbsp;</p><p>Preliminary interpretation of the data indicates that the southern part of the area in which Paleozoic-Mesozoic rocks and mineral deposits are exposed, should be reassessed to the classification and genesis of some of the deposits and to the types of mineral commodities that may be present. Some wholly new exploration targets within these areas are also indicated by some of the data. In addition, geochemical clues to buried mineral deposits, possibly representing continuation northward of some features of the Silver City mining district, have been observed in data from the northern, Tertiary volcanic areas. The meanings of these clues are still speculative.</p><p>For this study, 917 stream-sediment and 921 stream-sediment concentrate samples were collected. The stream-sediment-concentrate samples, which consist of heavy minerals, were split into magnetic and nonmagnetic fractions, each of which was analyzed. This resulted in the analysis of 1,842 heavy-mineral and 917 sieved stream-sediment samples.&nbsp;</p><p>Analytical results for all of the sample types are summarized statistically on table 1 and tabulated in their entirety on table 2.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78801","usgsCitation":"Watts, K.C., Hassemer, J., Siems, D.F., and Nishi, J.M., 1978, A statistical summary and listing of the spectrographic analyses of heavy mineral concentrate and conventional, sieved stream-sediment samples, Silver City area, New Mexico: U.S. Geological Survey Open-File Report 78-801, i, 247 leaves ;28 cm., https://doi.org/10.3133/ofr78801.","productDescription":"i, 247 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,{"id":65889,"text":"i1075 - 1978 - Shaded relief map of the Memnonia Quadrangle of Mars","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}],"lastModifiedDate":"2012-02-02T00:13:18","indexId":"i1075","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1075","subseriesTitle":"NONE","title":"Shaded relief map of the Memnonia Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1075","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Shaded relief map of the Memnonia Quadrangle of Mars: U.S. Geological Survey IMAP 1075, 1 map ;37 x 53 cm. on sheet 86 x 69 cm., https://doi.org/10.3133/i1075.","productDescription":"1 map ;37 x 53 cm. on sheet 86 x 69 cm.","costCenters":[],"links":[{"id":190389,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260830,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1075/plate-1.pdf"}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f457d","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":534242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29276,"text":"wri7868 - 1978 - Comparison of the radioactive and modified techniques for measurement of stream reaeration coefficients","interactions":[],"lastModifiedDate":"2015-10-21T09:37:07","indexId":"wri7868","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-68","title":"Comparison of the radioactive and modified techniques for measurement of stream reaeration coefficients","docAbstract":"<p>The radioactive and modified tracer techniques were used to measure the reaeration coefficients of two reaches each of Black Earth Creek and the Madison Effluent Channel near Madison, Wis. Comparison of the results showed that coefficients measured with the modified technique ranged from -8.96 to +3.61 and from +15.7 to +32.2 percent different from the coefficient measured with the radioactive tracer technique on the two reaches of Black Earth Creek. The larger coefficients measured with the modified technique on the second reach were attributed to increased wind conditions during the latter part of the modified-technique experiment. Interpretation of the results of the Madison Effluent Channel study was complicated by an unsteady flow condition during the modified-technique experiment. It was necessary to estimate the part of the reduction in the area under the dye concentration-versus-time curve that was the result of dye loss and the part that was the result of the increase in water discharge. Using these estimated values, the coefficients measured with the modified technique ranged from +25.3 to +57.9 and from -4.74 to +2.94 percent different from the coefficient measured with the radioactive technique on the two reaches of the Madison Effluent Channel.</p>\n<p>Reaeration coefficients were predicted for the 4 stream reaches with 19 predictive equations from the literature. The range of the predicted coefficients for each of the reaches varied from about a 6-fold range for the first reach of the Madison Effluent Channel to an almost 11-fold range for the second reach of Black Earth Creek.</p>\n<p>There are advantages and disadvantages to both the radioactive and modified tracer techniques. The main advantage of the radioactive technique is that the tracer gas is chemically inert; the main disadvantage is that a radioactive isotope of the gas must be used to obtain the necessary analytical sensitivity. The main advantage of the modified technique is that radioactive tracers are not necessary; the main disadvantage is that the hydrocarbon tracer gases may be subject to biological degradation and sorption losses. Results of this comparison study suggest that the modified technique is a promising alternative to the use of radioactive tracers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7868","usgsCitation":"Rathbun, R.E., and Grant, R.S., 1978, Comparison of the radioactive and modified techniques for measurement of stream reaeration coefficients: U.S. Geological Survey Water-Resources Investigations Report 78-68, vii, 57 p., https://doi.org/10.3133/wri7868.","productDescription":"vii, 57 p.","numberOfPages":"66","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":123417,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0068/report-thumb.jpg"},{"id":58124,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0068/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Dane","city":"Madison, Mazomanie","otherGeospatial":"Black Earth Creek","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.0094,43.286],[-89.0084,43.2555],[-89.0094,43.2],[-89.01,43.1131],[-89.0109,43.0849],[-89.0107,43.0271],[-89.0132,42.9353],[-89.013,42.8762],[-89.0119,42.8471],[-89.132,42.8479],[-89.2488,42.8478],[-89.3689,42.8484],[-89.3688,42.8575],[-89.4832,42.858],[-89.6026,42.8575],[-89.7196,42.8587],[-89.8377,42.8598],[-89.8375,42.9471],[-89.8386,43.0317],[-89.8384,43.1181],[-89.8394,43.205],[-89.8325,43.2123],[-89.825,43.2187],[-89.8175,43.226],[-89.8125,43.2342],[-89.8088,43.2369],[-89.8012,43.2365],[-89.7874,43.2356],[-89.771,43.237],[-89.7579,43.2379],[-89.7529,43.2443],[-89.7485,43.2507],[-89.7391,43.2548],[-89.7259,43.2644],[-89.7171,43.2739],[-89.714,43.2821],[-89.7165,43.2867],[-89.7235,43.2935],[-89.7209,43.2935],[-89.6008,43.2932],[-89.4819,43.2942],[-89.3617,43.2954],[-89.3624,43.2832],[-89.246,43.2834],[-89.1271,43.2827],[-89.0094,43.286]]]},\"properties\":{\"name\":\"Dane\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf29","contributors":{"authors":[{"text":"Rathbun, R. 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,{"id":63298,"text":"gq1464 - 1978 - Geologic map of the Creekville quadrangle, Clay and Leslie Counties, Kentucky","interactions":[{"subject":{"id":47163,"text":"ofr77877 - 1977 - Geologic map of the Creekville Quadrangle, Clay and Leslie counties, Kentucky","indexId":"ofr77877","publicationYear":"1977","noYear":false,"title":"Geologic map of the Creekville Quadrangle, Clay and Leslie counties, Kentucky"},"predicate":"SUPERSEDED_BY","object":{"id":63298,"text":"gq1464 - 1978 - Geologic map of the Creekville quadrangle, Clay and Leslie Counties, Kentucky","indexId":"gq1464","publicationYear":"1978","noYear":false,"title":"Geologic map of the Creekville quadrangle, Clay and Leslie Counties, Kentucky"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq1464","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"1464","title":"Geologic map of the Creekville quadrangle, Clay and Leslie Counties, Kentucky","language":"ENGLISH","doi":"10.3133/gq1464","usgsCitation":"Bryant, B., 1978, Geologic map of the Creekville quadrangle, Clay and Leslie Counties, Kentucky: U.S. Geological Survey Geologic Quadrangle 1464, 1 map : col. ;58 x 47 cm. on sheet 80 x 88 cm., https://doi.org/10.3133/gq1464.","productDescription":"1 map : col. ;58 x 47 cm. on sheet 80 x 88 cm.","costCenters":[],"links":[{"id":107887,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10998.htm","linkFileType":{"id":5,"text":"html"},"description":"10998"},{"id":249402,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1464/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":252801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1464/report-thumb.jpg"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.61749999999999,37 ], [ -83.61749999999999,37.1175 ], [ -83.5,37.1175 ], [ -83.5,37 ], [ -83.61749999999999,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69c051","contributors":{"authors":[{"text":"Bryant, Bruce bbryant@usgs.gov","contributorId":1355,"corporation":false,"usgs":true,"family":"Bryant","given":"Bruce","email":"bbryant@usgs.gov","affiliations":[],"preferred":false,"id":268630,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11739,"text":"ofr781073 - 1978 - Mineral exploration, Mahd adh Dhahab District, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr781073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-1073","title":"Mineral exploration, Mahd adh Dhahab District, Kingdom of Saudi Arabia","docAbstract":"Mahd adh Dhahab is the largest of numerous ancient gold mines scattered through the Precambrian shield of Saudi Arabia and the only one with recent production. During the period 1939-54, 765,768 fine ounces of gold and 1,002,029 ounces of silver were produced from the mines by the Saudi Arabian Mining Syndicate. \r\n\r\nOre minerals at Mahd adh Dhahab include free gold and silver, tellurides, sphalerite, and chalcopyrite in and associated with a system of north-trending quartz veins and quartz veinlet stockworks. Pyrite is a common sulfide gangue mineral. Country rocks are a north dipping sequence of pyroclastic and transported pyroclastic rocks of the Hulayfah Group that are locally highly silicified and potassium-feldspathized. The prime target for this exploration program was a north-trending zone of quartz veins and breccias, faults, alteration, and metalization approximately 400 m wide and 1000 m long. The ancient and recent mine workings are located in the northern part of this zone. Although the quartz veins and alteration cut all lithologies, the major metalization is confined to the intersection of veins and agglomerate. Ten holes were diamond drilled to explore geochemical, geological, and geophysical targets in the area.\r\n\r\nA significant new zone of metalization was discovered 700 m south of the ancient and recent mine workings and within the same major zone of quartz veins, alteration, and faults. Metalization in this southern mineralized zone is at the intersection of the quartz veins and a distinctive and highly altered agglomerate. The total zone of vein and agglomerate intercept is potentially metalized and comprises a block of ground 40 m thick and 400 m wide along the strike of the agglomerate and projected downdip 250 m. Tonnage of this block is 17.2 million tons. The explored zone, approximately 25 percent of the potentially metalized rock, has a potential resource of 1.1 million tons containing 27 g/t gold and 73 g/t silver.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr781073","usgsCitation":"Worl, R., 1978, Mineral exploration, Mahd adh Dhahab District, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 78-1073, iii, 85 p. :ill., maps (some fold. in pocket) ;27 cm.; (89 p., 3 sheets - PGS), https://doi.org/10.3133/ofr781073.","productDescription":"iii, 85 p. :ill., maps (some fold. in pocket) ;27 cm.; (89 p., 3 sheets - PGS)","costCenters":[],"links":[{"id":145544,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1073/report-thumb.jpg"},{"id":39629,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1073/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39630,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1073/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39631,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635a3f","contributors":{"authors":[{"text":"Worl, Ronald G.","contributorId":87143,"corporation":false,"usgs":true,"family":"Worl","given":"Ronald G.","affiliations":[],"preferred":false,"id":163646,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40455,"text":"ofr78637 - 1978 - Coal resource occurrence and coal development potential maps of the Miller Creek NW Quadrangle, Rosebud and Custer counties, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:11:05","indexId":"ofr78637","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-637","title":"Coal resource occurrence and coal development potential maps of the Miller Creek NW Quadrangle, Rosebud and Custer counties, Montana","language":"ENGLISH","doi":"10.3133/ofr78637","usgsCitation":"Colorado School of Mines Research Institute, 1978, Coal resource occurrence and coal development potential maps of the Miller Creek NW Quadrangle, Rosebud and Custer counties, Montana: U.S. Geological Survey Open-File Report 78-637, 5 maps and 2 data sheets ;59 x 40 cm.; 17 p., https://doi.org/10.3133/ofr78637.","productDescription":"5 maps and 2 data sheets ;59 x 40 cm.; 17 p.","costCenters":[],"links":[{"id":168681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0637/report-thumb.jpg"},{"id":74975,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0637/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74976,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0637/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74977,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0637/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74978,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0637/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74979,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0637/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74980,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0637/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74981,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0637/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74982,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0637/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0fd1","contributors":{"authors":[{"text":"Colorado School of Mines Research Institute","contributorId":128082,"corporation":true,"usgs":false,"organization":"Colorado School of Mines Research Institute","id":530240,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20132,"text":"ofr78662 - 1978 - Analysis of urban storm-water quality for seven basins near Portland, Oregon","interactions":[],"lastModifiedDate":"2016-07-08T09:24:04","indexId":"ofr78662","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-662","title":"Analysis of urban storm-water quality for seven basins near Portland, Oregon","docAbstract":"<p>Over a 1.5-year period, water-quality data were collected for seven small drainage basins in urban aeas of Portland, Oreg. Analysis of the data followed three approaches. First, the constituent concentrations were analyzed. Average concentrations of suspended sediment, settleable solids, and fecal coliform bacteria generally exceeded levels expected for secondary waste-treatment plant effluent, whereas biochemical oxygen demand concentrations were lower than expected. The second analytical approach established correlations and bivariate regression relationships between constituents for individual storms in each basin, for all storms in each basin, and for all storms in all basins. Generally, correlation coefficients decreased when progressing from data for individual storms in each basin, to data for all storms in each basin, to data for all storms in all basins. In the third approach, storm yields for 10 constituents were related to basin and precipitation characteristics by use of multiple-linear-regression techniques. Storm yields for suspended sediment varied by about four orders of magnitude. Generally, results of the multiple-regression analysis indicated that variations in storm yields were highly dependent on precipitation characteristics, with total rainfall of the storm frequently explaining most of the variation of the dependent variable.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr78662","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers, Columbia Region Association of Governments","usgsCitation":"Miller, T.L., and McKenzie, S.W., 1978, Analysis of urban storm-water quality for seven basins near Portland, Oregon: U.S. Geological Survey Open-File Report 78-662, vii, 81 p., https://doi.org/10.3133/ofr78662.","productDescription":"vii, 81 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":153234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr78662.jpg"},{"id":324876,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0662/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","city":"Portland","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.84500122070311,\n              45.35407536661815\n            ],\n            [\n              -122.84500122070311,\n              45.54675503088241\n            ],\n            [\n              -122.46597290039062,\n              45.54675503088241\n            ],\n            [\n              -122.46597290039062,\n              45.35407536661815\n            ],\n            [\n              -122.84500122070311,\n              45.35407536661815\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea2b","contributors":{"authors":[{"text":"Miller, Timothy L.","contributorId":9263,"corporation":false,"usgs":true,"family":"Miller","given":"Timothy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":182118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKenzie, Stuart W.","contributorId":27841,"corporation":false,"usgs":true,"family":"McKenzie","given":"Stuart","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":182119,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68652,"text":"ha582 - 1978 - Water resources of the Lake Superior watershed, northeastern Minnesota","interactions":[{"subject":{"id":9593,"text":"ofr77415 - 1976 - Geohydrology of Cheyenne River Indian Reservation, South Dakota","indexId":"ofr77415","publicationYear":"1976","noYear":false,"title":"Geohydrology of Cheyenne River Indian Reservation, South Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":68652,"text":"ha582 - 1978 - Water resources of the Lake Superior watershed, northeastern Minnesota","indexId":"ha582","publicationYear":"1978","noYear":false,"title":"Water resources of the Lake Superior watershed, northeastern Minnesota"},"id":1},{"subject":{"id":17899,"text":"ofr76276 - 1976 - Water resources of the Lake Superior Watershed, northeastern Minnesota","indexId":"ofr76276","publicationYear":"1976","noYear":false,"title":"Water resources of the Lake Superior Watershed, northeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":68652,"text":"ha582 - 1978 - Water resources of the Lake Superior watershed, northeastern Minnesota","indexId":"ha582","publicationYear":"1978","noYear":false,"title":"Water resources of the Lake Superior watershed, northeastern Minnesota"},"id":2}],"lastModifiedDate":"2018-03-19T10:41:45","indexId":"ha582","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"582","title":"Water resources of the Lake Superior watershed, northeastern Minnesota","docAbstract":"<p>The Lake Superior watershed is mostly a highland, generally 1,200 feet (366 meters) to 2,000 feet (610 meters) above mean sea level. It extends from Duluth to the Canadian border.</p>\n<p>Both maximum and minimum altitudes for Minnesota occur in the watershed; 2.301 ft (701 ) at Eagle Mountain, about 12 mi (19 km) northwest of Grand Marais, and 602 ft (184 m), the normal level of Lake Superior. Total relief is nearly 1,700 ft (518 m). The North Shore area (Duluth to the Canadian border) has a southeastward slope that is especially precipitous adjacent to Lake Superior.</p>\n<p>Conforming to this topography, the drainage includes a series of 17 southeastward-flowing streams averaging 23 mi (36 km) in length, with an average gradient from headwaters to mouth of about 57 ft/mi (10.8 m/km). The streams are deeply entrenched and characterized by swift flows, many rapids and waterfalls, and especially steep gradients in the 3 to 5 mi (4.8 to 8.0 km) before entering Lake Superior.</p>\n<p>The Pigeon River drains the extreme northern part of the watershed and forms the international border between the United States and Canada. More than half of the 610 mi<sup>2</sup> (1580 km<sup>2</sup>) drainage basin of the Pigeon River lies in Canada.</p>\n<p>The Nemadji River and tributaries drain the Nemadji Basin, the southern detached part of the watershed. Topographically, the Nemadji Basin is roughly spoon shaped with maximum total relief in Minnesota of about 800 ft (244 m). More than half of the approximately 55-mi (88-km) long river flows northeastward through Wisconsin before reaching Lake Superior.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha582","usgsCitation":"Olcott, P.G., Ericson, D., Felsheim, P., and Broussard, W., 1978, Water resources of the Lake Superior watershed, northeastern Minnesota: U.S. Geological Survey Hydrologic Atlas 582, 2 Plates: 58.00 x 41.96 inches, https://doi.org/10.3133/ha582.","productDescription":"2 Plates: 58.00 x 41.96 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":189791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90341,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/582/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90342,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/582/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Minnesota","otherGeospatial":"Lake Superior watershed","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.21810913085938, 47.3136897998641 ], [ -91.24008178710938, 47.291339409457294 ], [ -91.27166748046875, 47.26711582310954 ], [ -91.30599975585938, 47.249406957888446 ], [ -91.3348388671875, 47.226096795477204 ], [ -91.36642456054688, 47.200910301521674 ], [ 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,{"id":7808,"text":"ofr78660 - 1978 - Lithologic and geophysical logs of holes drilled during 1977 in the Savery Quadrangle and southeastern part of the Baggs Quadrangle, Carbon County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr78660","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-660","title":"Lithologic and geophysical logs of holes drilled during 1977 in the Savery Quadrangle and southeastern part of the Baggs Quadrangle, Carbon County, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78660","usgsCitation":"Barclay, C.V., and Shoaff, L.A., 1978, Lithologic and geophysical logs of holes drilled during 1977 in the Savery Quadrangle and southeastern part of the Baggs Quadrangle, Carbon County, Wyoming: U.S. Geological Survey Open-File Report 78-660, iii, 50 leaves :ill. (some fold.), maps ;32 cm., https://doi.org/10.3133/ofr78660.","productDescription":"iii, 50 leaves :ill. (some fold.), maps ;32 cm.","costCenters":[],"links":[{"id":94836,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0660/plate-1.pdf","size":"1132","linkFileType":{"id":1,"text":"pdf"}},{"id":140398,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0660/report-thumb.jpg"},{"id":35306,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0660/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3fc0","contributors":{"authors":[{"text":"Barclay, C.S. Venable","contributorId":89525,"corporation":false,"usgs":true,"family":"Barclay","given":"C.S.","email":"","middleInitial":"Venable","affiliations":[],"preferred":false,"id":156644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shoaff, Larry A.","contributorId":69545,"corporation":false,"usgs":true,"family":"Shoaff","given":"Larry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":156643,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29175,"text":"wri797 - 1978 - A preliminary appraisal of the impact of agriculture on ground-water availability in southwest Georgia","interactions":[],"lastModifiedDate":"2023-02-17T21:12:44.134681","indexId":"wri797","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"79-7","title":"A preliminary appraisal of the impact of agriculture on ground-water availability in southwest Georgia","docAbstract":"<p>Irrigated acreage in the study area in southwest Georgia increased from 130,000 acres in 1976 to 261,000 in 1977. Acreage irrigated entirely by ground water increased 85 percent for the same period. The largest quantity of ground water used for irrigation was in the Dougherty Plain district, where 92 percent of supplemental irrigation water comes from wells. In the Tifton Upland district, ground water is the source for only 16 percent of the irrigation water used. The major ground-water reservoir supplying the irrigation water is the principal artesian aquifer.</p><p>The Dougherty Plain, because of the gently rolling land surface and large fields, is suitable for the use of large self-propelled center-pivot irrigation systems requiring 1,200 to 1,500 gallons per minute. The installed pump capacity of the irrigation systems in the Dougherty Plain using ground water was 1.8 billion gallons per day in 1977. The total amount of water pumped for irrigation in the Dougherty Plain in 1977 was more than 42 billion gallons, 30 billion gallons more than in 1976. This quantity could be considerably higher in 1978 as preparations were being made to irrigate more than 214,000 acres during the 1978 growing season.</p><p>There were no concentrations of selected organic compounds or trace metals used in agricultural chemicals above the recommended limits for public consumption in water analyzed from 19 wells. However, concentrations of total nitrite plus nitrate ranged from 0.3 to 7.8 milligrams per liter in wells in the Dougherty Plain, and this could indicate that the downward percolation of water through sandy soils has carried soluble nitrate, a byproduct of fertilizer, into the ground-water reservoir.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri797","collaboration":"Prepared in cooperation with the Georgia Department of Natural Resources","usgsCitation":"Pollard, L., Grantham, R., and Blanchard, H., 1978, A preliminary appraisal of the impact of agriculture on ground-water availability in southwest Georgia: U.S. Geological Survey Water-Resources Investigations Report 79-7, Report: v, 22 p.; 4 Plates: 35.12 x 28.88 inches or smaller, https://doi.org/10.3133/wri797.","productDescription":"Report: v, 22 p.; 4 Plates: 35.12 x 28.88 inches or smaller","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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,{"id":8995,"text":"ofr78215 - 1978 - Analyses and description of geochemical samples, Cranberry Wilderness Study Area, Pocahontas and Webster counties, West Virginia","interactions":[],"lastModifiedDate":"2022-09-30T22:56:24.505298","indexId":"ofr78215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-215","title":"Analyses and description of geochemical samples, Cranberry Wilderness Study Area, Pocahontas and Webster counties, West Virginia","docAbstract":"<p>Semiquantitative spectrographic and other analyses on 104 stream sediment and 100 rock and mineral samples are reported here in detail. Location for all samples are in universal Transverse Mercator (UTM) coordinates. Brief descriptions of rock and mineral samples are included. Rocks analyzed include sandstone and shale; two samples of pyrite from sandstone are included. No obviously anomalous values related to mineralized rock are present in the data.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78215","usgsCitation":"Motooka, J.M., Negri, J., Sharkey, J.D., and Lesure, F., 1978, Analyses and description of geochemical samples, Cranberry Wilderness Study Area, Pocahontas and Webster counties, West Virginia: U.S. Geological Survey Open-File Report 78-215, 23 p., https://doi.org/10.3133/ofr78215.","productDescription":"23 p.","costCenters":[],"links":[{"id":407754,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0215/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144124,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0215/report-thumb.jpg"}],"country":"United States","state":"West Virginia","county":"Pocahontas County, Webster County","otherGeospatial":"Cranberry Wilderness Study Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.54763793945311,\n              38.22847167526397\n            ],\n            [\n              -80.2716064453125,\n              38.22847167526397\n            ],\n            [\n              -80.2716064453125,\n              38.31903340948611\n            ],\n            [\n              -80.54763793945311,\n              38.31903340948611\n            ],\n            [\n              -80.54763793945311,\n              38.22847167526397\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6839f2","contributors":{"authors":[{"text":"Motooka, J. M.","contributorId":8834,"corporation":false,"usgs":true,"family":"Motooka","given":"J.","middleInitial":"M.","affiliations":[],"preferred":false,"id":158687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Negri, J.C.","contributorId":36565,"corporation":false,"usgs":true,"family":"Negri","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":158688,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sharkey, J. D.","contributorId":85578,"corporation":false,"usgs":true,"family":"Sharkey","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":158689,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lesure, F. G.","contributorId":7694,"corporation":false,"usgs":true,"family":"Lesure","given":"F. G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":158686,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":10834,"text":"ofr78961 - 1978 - An abbreviation key for the DASCH System: A lithostratigraphic information storage and retrieval system","interactions":[],"lastModifiedDate":"2023-02-28T23:16:01.8293","indexId":"ofr78961","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-961","title":"An abbreviation key for the DASCH System: A lithostratigraphic information storage and retrieval system","docAbstract":"<p>DASCH is a computer-based information storage and retrieval system which accepts lithostratigraphic information and produces both graphic and tabular compilations. This system has been modified for use on the U.S.G.S. MULTICS computer.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78961","usgsCitation":"Reinhardt, J., and Van Driel, J.N., 1978, An abbreviation key for the DASCH System: A lithostratigraphic information storage and retrieval system: U.S. Geological Survey Open-File Report 78-961, 26 p., https://doi.org/10.3133/ofr78961.","productDescription":"26 p.","costCenters":[],"links":[{"id":145703,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0961/report-thumb.jpg"},{"id":413498,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0961/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6864f2","contributors":{"authors":[{"text":"Reinhardt, Juergen","contributorId":88714,"corporation":false,"usgs":true,"family":"Reinhardt","given":"Juergen","email":"","affiliations":[],"preferred":false,"id":162048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Driel, J. Nicholas","contributorId":80688,"corporation":false,"usgs":true,"family":"Van Driel","given":"J.","email":"","middleInitial":"Nicholas","affiliations":[],"preferred":false,"id":162047,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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