{"pageNumber":"1086","pageRowStart":"27125","pageSize":"25","recordCount":36989,"records":[{"id":7342,"text":"ofr78142 - 1978 - Mineral resources of the Cranberry Wilderness Study Area, Pocahontas and Webster counties, West Virginia","interactions":[{"subject":{"id":7342,"text":"ofr78142 - 1978 - Mineral resources of the Cranberry Wilderness Study Area, Pocahontas and Webster counties, West Virginia","indexId":"ofr78142","publicationYear":"1978","noYear":false,"title":"Mineral resources of the Cranberry Wilderness Study Area, Pocahontas and Webster counties, West Virginia"},"predicate":"SUPERSEDED_BY","object":{"id":33372,"text":"b1494 - 1981 - Mineral resources of the Cranberry Wilderness study area, Webster and Pocahontas counties, West Virginia, with sections on peat resources, oil and gas potential, and geochemical survey","indexId":"b1494","publicationYear":"1981","noYear":false,"title":"Mineral resources of the Cranberry Wilderness study area, Webster and Pocahontas counties, West Virginia, with sections on peat resources, oil and gas potential, and geochemical survey"},"id":1}],"supersededBy":{"id":33372,"text":"b1494 - 1981 - Mineral resources of the Cranberry Wilderness study area, Webster and Pocahontas counties, West Virginia, with sections on peat resources, oil and gas potential, and geochemical survey","indexId":"b1494","publicationYear":"1981","noYear":false,"title":"Mineral resources of the Cranberry Wilderness study area, Webster and Pocahontas counties, West Virginia, with sections on peat resources, oil and gas potential, and geochemical survey"},"lastModifiedDate":"2022-10-04T21:18:49.726569","indexId":"ofr78142","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":"78-142","title":"Mineral resources of the Cranberry Wilderness Study Area, Pocahontas and Webster counties, West Virginia","docAbstract":"<p>Cranberry Wilderness Study Area comprises 14,702 ha in the Monongahela National Forest, Pocahontas and Webster Counties, east-central West Virginia. The area is in the Yew Mountains of the Appalachian Plateaus and is at the eastern edge of the central Appalachian coal fields. Cranberry Glades, a peatland of botanical interest lies at the southern end of the study area. All surface rights in the area are held by the U. S. Forest Service; nearly 90 percent of the mineral rights are privately-owned or subordinate to the surface rights.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78142","usgsCitation":"Meissner, C.R., Windolph, J.F., Mory, P.C., Harrison, D.K., Cameron, C.C., Grosz, A., Perry, W.J., and Lesure, F.G., 1978, Mineral resources of the Cranberry Wilderness Study Area, Pocahontas and Webster counties, West Virginia: U.S. Geological Survey Open-File Report 78-142, Report: vi, 77 p.; 5 Plates: 35.49 x 39.86 inches or smaller, https://doi.org/10.3133/ofr78142.","productDescription":"Report: vi, 77 p.; 5 Plates: 35.49 x 39.86 inches or smaller","costCenters":[],"links":[{"id":407914,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0142/plate-5-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407913,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0142/plate-5-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407912,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0142/plate-5-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407911,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0142/plate-5-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407910,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0142/plate-5-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407909,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0142/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0142/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              -80.5572509765625,\n              38.16911413556086\n            ],\n            [\n              -80.22216796875,\n              38.16911413556086\n            ],\n            [\n              -80.22216796875,\n              38.352426464461445\n            ],\n            [\n              -80.5572509765625,\n              38.352426464461445\n            ],\n            [\n              -80.5572509765625,\n              38.16911413556086\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b07e4b07f02db69adc0","contributors":{"authors":[{"text":"Meissner, Charles R. 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Jr.","contributorId":32498,"corporation":false,"usgs":true,"family":"Perry","given":"William","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":155320,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lesure, Frank Gardner","contributorId":70752,"corporation":false,"usgs":true,"family":"Lesure","given":"Frank","email":"","middleInitial":"Gardner","affiliations":[],"preferred":false,"id":155324,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":7767,"text":"ofr7871 - 1978 - Water-quality assessment of the Middle Fork Anderson River watershed, Crawford and Perry counties, Indiana","interactions":[],"lastModifiedDate":"2023-02-08T21:58:41.765456","indexId":"ofr7871","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":"78-71","title":"Water-quality assessment of the Middle Fork Anderson River watershed, Crawford and Perry counties, Indiana","docAbstract":"<p>Surface-water quality in the watershed is generally good except for problem-causing concentrations of bacteria, dissolved oxygen, and phosphorus at some sites along the main stem during low flow and manganese at most sites year-round.</p><p>Dissolved-solids concentration ranged from 76 to 248 milligrams per liter. Concentrations at sites upstream from reservoirs were greater than those at sites downstream during medium and low flows, but concentrations at sites upstream and downstream were similar during high flow.</p><p>Calcium and bicarbonate ions were dominant at most sites during low flows, whereas these ions were codominant with magnesium and sulfate at most sites during high flows.</p><p>Dissolved-oxygen concentration ranged from 2.1 to 11.6 milligrams per liter or from 21 to 124 percent of saturation. Low concentrations were associated with the main stem of the river during low flows when sluggish, pooled conditions prevailed.</p><p>Concentrations of certain inorganic constituents (including nutrients) were as follows: Dissolved-manganese concentration ranged from 0.02 to 7.3 milligrams per liter. The concentrations were generally higher at sites downstream from reservoirs than at sites upstream and was greater than the problem-causing level 0.05 milligrams per liter at most sites. The high manganese concentrations are probably associated with organic acids in the streams. Dissolved-nitrate concentration (as nitrogen) ranged from 0.03 to 3.3 milligrams per liter, the highest concentrations occurring during winter and spring in drainage from areas of the most intense cultivation. Dissolved-phosphorus concentrations were typically 0.03 milligrams per liter or less, except at one site in September 1975, when the concentration was 0.12 milligrams per liter, and at three sites in July 1976, when concentrations were 0.12, 0.41, and 0.58 milligrams per liter.</p><p>Chlorinated hydrocarbons were detected in bed material from two of the three sites sampled. Two micrograms or less per kilogram aldrin, DDT, DDD, DDE, dieldrin, and (or) chlordane and as much as 15 micrograms per kilogram PCB compounds were detected.</p><p>Suspended-sediment concentration ranged from 1 to 148 milligrams per liter. Concentrations in two sites downstream from reservoirs were higher for medium and low flows and, despite large changes in flow, were considerably more consistent than the concentrations at two sites unaffected by reservoirs.</p><p>Concentrations of fecal-coliform and fecal-streptococcal bacteria ranged from 5 to 9,900 and from 10 to 15,000 colonies per 100 milliliters, respectively. Source of high counts (more than 2,000 colonies per 100 milliliters) is probably livestock upstream from sampling sites.</p><p>Diversity indices (genera level) 2.7 and 2.5 at the two sites sampled for benthic invertebrates indicate healthy biologic communities at both sites.</p><p>Diversity indices (genera level) of the phytoplankton populations at seven sites ranged from 1.4 to 3.3. The phytoplankton populations were generally well balanced except for stressed communities at two mainstem sites during the September sampling.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7871","collaboration":"Prepared in cooperation with the U.S. Department of Agriculture Soil Conservation Service","usgsCitation":"Ayers, M.A., 1978, Water-quality assessment of the Middle Fork Anderson River watershed, Crawford and Perry counties, Indiana: U.S. Geological Survey Open-File Report 78-71, v, 31 p., https://doi.org/10.3133/ofr7871.","productDescription":"v, 31 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science 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Mark A.","contributorId":84730,"corporation":false,"usgs":true,"family":"Ayers","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":156564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7977,"text":"ofr78312 - 1978 - Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab and Millard counties, Utah","interactions":[{"subject":{"id":7977,"text":"ofr78312 - 1978 - Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab and Millard counties, Utah","indexId":"ofr78312","publicationYear":"1978","noYear":false,"title":"Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab and Millard counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043963,"text":"70043963 - 1978 - Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah","indexId":"70043963","publicationYear":"1978","noYear":false,"title":"Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah"},"id":1}],"supersededBy":{"id":70043963,"text":"70043963 - 1978 - Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah","indexId":"70043963","publicationYear":"1978","noYear":false,"title":"Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah"},"lastModifiedDate":"2022-09-30T22:58:27.004082","indexId":"ofr78312","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":"78-312","title":"Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab and Millard counties, Utah","docAbstract":"<p>The Fish Springs Flat area includes about 590 square miles (1,530 square kilometers) in western Utah. Total annual precipitation on the area averages about 7 inches (180 millimeters) and totals about 232,000 acre-feet (286 cubic hectometers). Fish Springs Wash is the major drainage in the area; and, along with numerous smaller washes, it flows only in direct response to precipitation. Runoff from the area is estimated to be about 2,000 acre-feet (2.5 cubic hectometers) per year.</p><p>The estimated amount of water recoverable from storage in the upper 100 feet (30 meters) of saturated valley fill is about 550,000 acre-feet (680 cubic hectometers), and most of this water is slightly to moderately saline.</p><p>The water in the Fish Springs Flat area ranges from slightly saline to briny, and the predominant ions in the water are sodium and chloride. The water that underlies the mudflats in the northwest part of the area is briny. Water that issues from Fish Springs is slightly saline.</p><p>The water in the Fish Springs Flat area is not suitable for drinking. The water that issues from Fish Springs is used for wildlife management, which includes ponding and irrigation of vegetation (chiefly saltgrass) in the Fish Springs National Wildlife Refuge. The water from the wells in the area is used for livestock and mining operations.</p><p>Ground-water recharge from precipitation is about 4,000 acre-feet (5 cubic hectometers) annually. Ground-water discharge is chiefly by springs and evapotranspiration. The largest springs in the Fish Springs group discharge about 26,000 acre-feet (32 cubic hectometers) annually. All other springs discharge about 600 acre-feet (0.74 cubic hectometer) per year, or only about 2 percent of the total spring discharge. Discharge by evapotranspiration is about 8,000 acre-feet (10 cubic hectometers) per year. Discharge by wells and by subsurface outflow is negligible. The difference between discharge and local recharge--approximately 31,000 acre-feet (38 cubic hectometers)--is assumed to enter the Fish Springs Flat area by interbasin flow.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78312","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Bolke, E., and Sumsion, C.T., 1978, Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab and Millard counties, Utah: U.S. Geological Survey Open-File Report 78-312, 46 p., https://doi.org/10.3133/ofr78312.","productDescription":"46 p.","costCenters":[],"links":[{"id":407755,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0312/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0312/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Juab County, Millard County, Tooele County,","otherGeospatial":"Fish Springs Flat area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.653564453125,\n              39.65539876418111\n            ],\n            [\n              -113.26492309570312,\n              39.65539876418111\n            ],\n            [\n              -113.26492309570312,\n              40.03918079694873\n            ],\n            [\n              -113.653564453125,\n              40.03918079694873\n            ],\n            [\n              -113.653564453125,\n              39.65539876418111\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605572","contributors":{"authors":[{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":156923,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sumsion, C. T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":156922,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9066,"text":"ofr78459 - 1978 - Progress report on Black Mesa monitoring program; 1977","interactions":[],"lastModifiedDate":"2023-02-13T17:21:38.661214","indexId":"ofr78459","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":"78-459","title":"Progress report on Black Mesa monitoring program; 1977","docAbstract":"<p>Monitoring activities of coal mine operations on Black Mesa were started in 1971 for the purpose of monitoring the effects of strip mining on the water resources of the area. Black Mesa is located in northeastern Arizona near the center of the Navajo Indian Reservation and is a prominent topographic high about 500 to 1,000 feet above the surrounding area. Monitoring on and near the mesa consists of measurements of ground-water levels, ground-water quality, and measurements of the quantity, sediment concentration, and chemical quality of surface water.</p><p>The surface-water monitoring consists of: (1) rainfall-runoff characteristics in the immediate vicinity of the mine, and (2) surface-flow conditions and water-quality characteristics at a site on Moenkopi Wash at the village of Moenkopi.</p><p>Three small watersheds of about 400 acres each are instrumented for the collection of flow data, precipitation data, and water samples for determination of chemical quality and sediment concentration. Each watershed is equipped with a data-collection platform that transmits the data via satellite to a computer that in turn provides near-real time information on rainfall and runoff.</p><p>Available data at this time are insufficient to assess the effects of mining on the quantity, sediment concentration, or chemical quality of surface-water runoff.</p><p>Water levels in seven wells, measured annually, have not shown significant declines. The water levels in some of the other wells in the network have declined as much as 7 feet, and others have fluctuated in response to seasonal pumping by nearby wells.</p><p><br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78459","collaboration":"Prepared in cooperation with the Arizona Water Commission","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Progress report on Black Mesa monitoring program; 1977: U.S. Geological Survey Open-File Report 78-459, vi, 38 p., https://doi.org/10.3133/ofr78459.","productDescription":"vi, 38 p.","costCenters":[],"links":[{"id":412997,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0459/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143553,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0459/report-thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Black Mesa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.06054687499999,\n              34.94899072578227\n            ],\n            [\n              -109.390869140625,\n              34.94899072578227\n            ],\n            [\n              -109.390869140625,\n              36.96744946416934\n            ],\n            [\n              -112.06054687499999,\n              36.96744946416934\n            ],\n            [\n              -112.06054687499999,\n              34.94899072578227\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65df2d","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":528894,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8039,"text":"ofr78430 - 1978 - Lithium in rocks from the Lincoln, Helena, and Townsend areas, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr78430","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":"78-430","title":"Lithium in rocks from the Lincoln, Helena, and Townsend areas, Montana","docAbstract":"In anticipation of increased demand for lithium for energy-related uses, the U.S. Geological Survey has been appraising the lithium resources of the United States and investigating occurrences of lithium. Analyses of samples of chiefly lacustrine rocks of Oligocene age collected by M. R. Mudge near Lincoln, Mont. showed as much as 1,500 ppm lithium. Since then we have sampled the area in greater detail, and have sampled rocks of similar ages in the Helena and Townsend valleys. \r\n\r\nThe lithium-rich beds crop out in a band about 1.3 km long by 0.3 km wide near the head of Beaver Creek, about 14 km northwest of Lincoln, Mont. These beds consist of laminated marlstone, oil shale, carbonaceous shale, limestone, conglomerate, and tuff. Some parts of this sequence average almost 0.1 percent lithium. The lithium-bearing rocks are too low in grade and volume to be economic. \r\n\r\nSamples of sedimentary rocks of Oligocene age from the Helena and Townsend valleys in the vicinity of Helena, Mont. were generally low in lithium (3-40 ppm). However, samples of rhyolites from the western side of the Helena valley and from the Lava Mountain area were slightly above average in lithium content (6-200 ppm).","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78430","usgsCitation":"Brenner-Tourtelot, E.F., Meier, A.L., and Curtis, C.A., 1978, Lithium in rocks from the Lincoln, Helena, and Townsend areas, Montana: U.S. Geological Survey Open-File Report 78-430, 27 leaves :fold. map (in pocket) ;30 cm.; (29 p., 1 sheet - PGS), https://doi.org/10.3133/ofr78430.","productDescription":"27 leaves :fold. map (in pocket) ;30 cm.; (29 p., 1 sheet - PGS)","costCenters":[],"links":[{"id":140542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0430/report-thumb.jpg"},{"id":35614,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0430/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0430/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a37f9","contributors":{"authors":[{"text":"Brenner-Tourtelot, Elizabeth F.","contributorId":103672,"corporation":false,"usgs":true,"family":"Brenner-Tourtelot","given":"Elizabeth","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":157033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meier, Allen L.","contributorId":14384,"corporation":false,"usgs":true,"family":"Meier","given":"Allen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157032,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Curtis, Craig A.","contributorId":103673,"corporation":false,"usgs":true,"family":"Curtis","given":"Craig","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":157034,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","interactions":[{"subject":{"id":8438,"text":"ofr78556A - 1978 - Drainage areas of surface water bodies of the Royal and Presumpscot River basins in southwestern Maine","indexId":"ofr78556A","publicationYear":"1978","noYear":false,"chapter":"A","title":"Drainage areas of surface water bodies of the Royal and Presumpscot River basins in southwestern Maine"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":1},{"subject":{"id":8439,"text":"ofr78556B - 1978 - Drainage areas of surface water bodies of the Saco River basin in southwestern Maine","indexId":"ofr78556B","publicationYear":"1978","noYear":false,"chapter":"B","title":"Drainage areas of surface water bodies of the Saco River basin in southwestern Maine"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":2},{"subject":{"id":8871,"text":"ofr78556I - 1982 - Drainage areas of surface water bodies of central Maine coastal river basins","indexId":"ofr78556I","publicationYear":"1982","noYear":false,"chapter":"I","title":"Drainage areas of surface water bodies of central Maine coastal river basins"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":3},{"subject":{"id":8872,"text":"ofr78556H - 1982 - Drainage areas of surface water bodies of eastern Maine coastal river basins","indexId":"ofr78556H","publicationYear":"1982","noYear":false,"chapter":"H","title":"Drainage areas of surface water bodies of eastern Maine coastal river basins"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":4},{"subject":{"id":8873,"text":"ofr78556E - 1980 - Drainage areas of surface water bodies of the Kennebec River basin in southwestern Maine","indexId":"ofr78556E","publicationYear":"1980","noYear":false,"chapter":"E","title":"Drainage areas of surface water bodies of the Kennebec River basin in southwestern Maine"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":5},{"subject":{"id":8875,"text":"ofr78556G - 1982 - Drainage areas of surface water bodies of the St. John River basin in northern Maine","indexId":"ofr78556G","publicationYear":"1982","noYear":false,"chapter":"G","title":"Drainage areas of surface water bodies of the St. John River basin in northern Maine"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":6},{"subject":{"id":23046,"text":"ofr78556D - 1979 - Drainage areas of surface water bodies of southern Maine coastal river basins","indexId":"ofr78556D","publicationYear":"1979","noYear":false,"chapter":"D","title":"Drainage areas of surface water bodies of southern Maine coastal river basins"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":7},{"subject":{"id":23047,"text":"ofr78556C - 1979 - Drainage areas of surface water bodies of the Androscoggin River basin in southwestern Maine","indexId":"ofr78556C","publicationYear":"1979","noYear":false,"chapter":"C","title":"Drainage areas of surface water bodies of the Androscoggin River basin in southwestern Maine"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":8},{"subject":{"id":23048,"text":"ofr78556F - 1981 - Drainage areas of surface water bodies of the Penobscot River basin in central Maine","indexId":"ofr78556F","publicationYear":"1981","noYear":false,"chapter":"F","title":"Drainage areas of surface water bodies of the Penobscot River basin in central Maine"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":9}],"lastModifiedDate":"2026-03-06T17:20:14.683526","indexId":"ofr78556","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered 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,{"id":40071,"text":"ofr78247 - 1978 - Correlations of coal beds in the Rock Springs Formation in measured sections on the east flank of the Rock Springs Uplift, Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:09:58","indexId":"ofr78247","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":"78-247","title":"Correlations of coal beds in the Rock Springs Formation in measured sections on the east flank of the Rock Springs Uplift, Sweetwater County, Wyoming","language":"ENGLISH","doi":"10.3133/ofr78247","usgsCitation":"Roehler, H.W., 1978, Correlations of coal beds in the Rock Springs Formation in measured sections on the east flank of the Rock Springs Uplift, Sweetwater County, Wyoming: U.S. Geological Survey Open-File Report 78-247, 1 map., https://doi.org/10.3133/ofr78247.","productDescription":"1 map.","costCenters":[],"links":[{"id":165781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":97489,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0247/plate-1.pdf","size":"4705","linkFileType":{"id":1,"text":"pdf"}},{"id":97490,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0247/plate-2.pdf","size":"2026","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6842b7","contributors":{"authors":[{"text":"Roehler, Henry W.","contributorId":48529,"corporation":false,"usgs":true,"family":"Roehler","given":"Henry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":222943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8721,"text":"ofr7813 - 1978 - A water-quality assessment of the Busseron Creek watershed, Sullivan, Vigo, Greene, and Clay counties, Indiana","interactions":[],"lastModifiedDate":"2022-09-19T22:19:47.65188","indexId":"ofr7813","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":"78-13","title":"A water-quality assessment of the Busseron Creek watershed, Sullivan, Vigo, Greene, and Clay counties, Indiana","docAbstract":"<p>Chemical quality of surface water in the 237-square mile Busseron Creek watershed is significantly affected by drainage from coal mines and municipalities. Drainage from coal mines is primarily a problem of higher than normal dissolved-solids concentration, whereas, drainage from municipalities is generally a problem of bacteria and phytoplankton. Generally, the water is calcium bicarbonate type, except in streams affected by drainage from coal mines, where the water is a mixed calcium and magnesium sulfate type.</p><p>Ranges of concentration (in milligrams per liter) of dissolved solids and of some of the chemical constituents dissolved in streams from September 1975 to July 2976 were: dissolved solids, from 104 to 2, 610; iron, from 0.00 to 150; sulfate, from 14 to 1,900; chloride, from 3.3 to 130; nitrate (as nitrogen), from 0.01 to 5.3; phosphate (as phosphorus), from 0.1 to 1.7; and total organic carbon, from 2.4 to 60. Range of pH was from 2.7 to 9.6. Highest concentrations of iron and sulfate and lowest pH values were measured at sites draining areas mined for coal. Highest concentrations of chloride, phosphate, and total organic carbon were at sites downstream from municipalities.</p><p>Ranges of concentration of chlorinated hydrocarbons (in micrograms per kilogram) detected in bed material of streams were: aldrin, from 0.2 to 0.4; chlordane, from 0 to 13; DDE, from 0.0 to 0.3; dieldrin, from 0.0 to 9.8; and heptachlor epoxide, from 0 to 1.0. Source of these materials is probably drainage from croplands.</p><p>Streams draining municipalities were affected by human wastes and had high populations of fecal coliform bacteria (as many as 46,000 colonies per 100 ml) and phytoplankton (as many as 190,000 cells per milliliter). Dissolved-oxygen concentration ranged from 2.8 to 15.0 milligrams per liter (from 26 to 194 percent of saturation).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7813","collaboration":"Prepared in cooperation with the U.S. Department of Agriculture Soil Conservation Service","usgsCitation":"Eikenberry, S.E., 1978, A water-quality assessment of the Busseron Creek watershed, Sullivan, Vigo, Greene, and Clay counties, Indiana: U.S. Geological Survey Open-File Report 78-13, v, 36 p., https://doi.org/10.3133/ofr7813.","productDescription":"v, 36 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science 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Stephen E.","contributorId":35309,"corporation":false,"usgs":true,"family":"Eikenberry","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":158210,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8723,"text":"ofr78811 - 1978 - Selected low-flow characteristics of streams in the vicinity of Warwick, Orange County, New York","interactions":[],"lastModifiedDate":"2023-09-12T21:44:55.403249","indexId":"ofr78811","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":"78-811","title":"Selected low-flow characteristics of streams in the vicinity of Warwick, Orange County, New York","docAbstract":"<p>Base flows were measured during 1971-76 at 10 partial-record sites and three continuous-record stations on major streams in and bordering the Town of Warwick. Discharge measurements at the partial-record sites were correlated with records from three suitable continuous-record gaging stations near the town to determine 7-day, 2-year low flows and 7-day, 10-year low flows. Measurement-site descriptions are included. The information presented provides a data base that planners and managers can use in making water-management decisions.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78811","collaboration":"Prepared in cooperation with the Town of Warwick","usgsCitation":"Eissler, B.B., 1978, Selected low-flow characteristics of streams in the vicinity of Warwick, Orange County, New York: U.S. Geological Survey Open-File Report 78-811, ii, 21 p., https://doi.org/10.3133/ofr78811.","productDescription":"ii, 21 p.","costCenters":[],"links":[{"id":420747,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0811/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141038,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0811/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Orange County","city":"Warwick","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -74.40317346376985,\n              41.276009317207354\n            ],\n            [\n              -74.40317346376985,\n              41.22899934354564\n            ],\n            [\n              -74.31350277830987,\n              41.22899934354564\n            ],\n            [\n              -74.31350277830987,\n              41.276009317207354\n            ],\n            [\n              -74.40317346376985,\n              41.276009317207354\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f8407","contributors":{"authors":[{"text":"Eissler, Benjamin B.","contributorId":77527,"corporation":false,"usgs":true,"family":"Eissler","given":"Benjamin","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":158212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7017,"text":"ofr78663 - 1978 - Availability of fresh and slightly saline ground water in the basins of westernmost Texas","interactions":[],"lastModifiedDate":"2016-08-11T09:33:45","indexId":"ofr78663","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":"78-663","title":"Availability of fresh and slightly saline ground water in the basins of westernmost Texas","docAbstract":"<p>Significant quantities of fresh ground water occur in the basin fill of the northern Hueco bolson and lower Mesilla Valley and in the Wildhorse Flat, Michigan Flat, Lobo Flat, and Ryan Flat areas of the Salt Basin; and may occur in Red Light Draw, Presidio bolson, and Green River valley. More than 20 million acre-feet of freshwater is estimated to be in storage in the basin fill of westernmost Texas. About 12 million acre-feet, or more than half, is in El Paso County in the Hueco bolson and Mesilla Valley. In addition, the basins contain about 7 million acre-feet of slightly saline water in basin fill, in Rio Grande alluvium in the Hueco bolson and lower Mesilla Valley, and in the Capitan Limestone in the northern Salt Basin. Ground-water pumping for municipal supply and industrial use in the El Paso area caused water-level declines of as much as 74 feet during 1903-73, and pumping for irrigation in the Salt Basin caused a maximum decline of 150 feet at Lobo Flat during 1949-73. Additional development of ground water in westernmost Texas will be accompanied by further declines in water levels, and will probably induce local migration of slightly saline or poorer quality water into freshwater areas. Land-surface subsidence could occur in local areas where water-level declines are large and the basin fill contains large amounts of compressible clay. (Kosco-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78663","usgsCitation":"Gates, J.S., Stanley, W.D., and Ackermann, H., 1978, Availability of fresh and slightly saline ground water in the basins of westernmost Texas: U.S. Geological Survey Open-File Report 78-663, vii, 173 p., https://doi.org/10.3133/ofr78663.","productDescription":"vii, 173 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":139554,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0663/report-thumb.jpg"},{"id":112893,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0663/report.pdf","size":"28391","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db616315","contributors":{"authors":[{"text":"Gates, Joseph Spencer","contributorId":108089,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph","email":"","middleInitial":"Spencer","affiliations":[],"preferred":false,"id":153925,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanley, W. D.","contributorId":86756,"corporation":false,"usgs":true,"family":"Stanley","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":153923,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ackermann, H.D.","contributorId":90711,"corporation":false,"usgs":true,"family":"Ackermann","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":153924,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7021,"text":"ofr78731 - 1978 - Bibliography of the available data on the solubility of silica in water substance","interactions":[],"lastModifiedDate":"2023-11-20T22:10:21.539417","indexId":"ofr78731","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":"78-731","title":"Bibliography of the available data on the solubility of silica in water substance","docAbstract":"<p>The following bibliography represents the currently available experimental data for the solubility of silica in water substance as a function of temperature and pressure. These references were compiled by the silica subcommittee of Working Group IV at the 1977 meeting of LAPS in Moscow. The data summarized in these references cover the temperature range of 0° to 900°C at pressures from atmospheric to 1000 mega pascals.</p><p>Preliminary examination of the data suggests that a good correlation of the solubility of silica can be obtained from temperature and log specific volume of water (Fig. 1). The available solubility data (log weight percent silica) tend to lie along smooth curves at constant temperature as a function of log specific volume of water. In addition the data appear to be reasonably consistent, such that a single equation can be derived that describes the solubility of quartz from 0° to 900°C at pressures up to 1000 mega pascals.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78731","usgsCitation":"Potter, R., Marshall, W., Fournier, R., and Martynova, O., 1978, Bibliography of the available data on the solubility of silica in water substance: U.S. Geological Survey Open-File Report 78-731, 7 p., https://doi.org/10.3133/ofr78731.","productDescription":"7 p.","costCenters":[],"links":[{"id":139559,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0731/report-thumb.jpg"},{"id":422747,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0731/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627d78","contributors":{"authors":[{"text":"Potter, Robert W.","contributorId":27045,"corporation":false,"usgs":true,"family":"Potter","given":"Robert W.","affiliations":[],"preferred":false,"id":153937,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marshall, W.L.","contributorId":59785,"corporation":false,"usgs":true,"family":"Marshall","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":153938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":153939,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Martynova, O.I.","contributorId":102467,"corporation":false,"usgs":true,"family":"Martynova","given":"O.I.","email":"","affiliations":[],"preferred":false,"id":153940,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":14676,"text":"ofr781076 - 1978 - Mineral resources of the Mill Creek, Mountain Lake, and Peters Mountain Wilderness Study Areas, Craig and Giles counties, Virginia and Monroe County, West Virginia","interactions":[{"subject":{"id":14676,"text":"ofr781076 - 1978 - Mineral resources of the Mill Creek, Mountain Lake, and Peters Mountain Wilderness Study Areas, Craig and Giles counties, Virginia and Monroe County, West Virginia","indexId":"ofr781076","publicationYear":"1978","noYear":false,"title":"Mineral resources of the Mill Creek, Mountain Lake, and Peters Mountain Wilderness Study Areas, Craig and Giles counties, Virginia and Monroe County, West Virginia"},"predicate":"SUPERSEDED_BY","object":{"id":34952,"text":"b1510 - 1982 - Mineral resources of the Mill Creek, Mountain Lake, and Peters Mountain Wilderness Study Areas, Craig and Giles Counties, Virginia, and Monroe County, West Virginia, with a section on oil and gas potential","indexId":"b1510","publicationYear":"1982","noYear":false,"title":"Mineral resources of the Mill Creek, Mountain Lake, and Peters Mountain Wilderness Study Areas, Craig and Giles Counties, Virginia, and Monroe County, West Virginia, with a section on oil and gas potential"},"id":1}],"supersededBy":{"id":34952,"text":"b1510 - 1982 - Mineral resources of the Mill Creek, Mountain Lake, and Peters Mountain Wilderness Study Areas, Craig and Giles Counties, Virginia, and Monroe County, West Virginia, with a section on oil and gas potential","indexId":"b1510","publicationYear":"1982","noYear":false,"title":"Mineral resources of the Mill Creek, Mountain Lake, and Peters Mountain Wilderness Study Areas, Craig and Giles Counties, Virginia, and Monroe County, West Virginia, with a section on oil and gas potential"},"lastModifiedDate":"2025-04-01T20:34:11.243667","indexId":"ofr781076","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":"78-1076","title":"Mineral resources of the Mill Creek, Mountain Lake, and Peters Mountain Wilderness Study Areas, Craig and Giles counties, Virginia and Monroe County, West Virginia","docAbstract":"<p>The Mill Creek, Mountain Lake, and Peters Mountain Wilderness Study Areas comprise about 8200 ha of steep wooded slopes in the Jefferson National Forest in west central Virginia and adjacent West Virginia. Mill Creek area contains about 1800 ha and Peters Mountain area about 1600 ha in Giles County, Va. Mountain Lake area contains about 3000 ha in Giles County, a little more than 570 ha in Craig County, Va., and nearly 1230 ha in Monroe County, W. Va. A small part of each study area is privately owned-- about 5 percent of Mill Creek, 20 percent of Mountain Lake and 2 percent of Peters Mountain. The U.S. Forest Service owns the mineral rights on all the Government land except for about 162 ha in the Peters Mountain arca. The three study areas are in the western part of the Valley and Ridge physiographic province and are therefore part of the folded Appalachians, which contain deformed sedimentary rocks of Paleozoic age. The same elastic marine and non—marine sedimentary rock formations ranging in age from Late Ordovician to Middle Devonian are exposed throughout the region. Sandstones of the Juniata, Tuscarora, and Keefer Formations form cliffs, ridges and steep dip slopes. The distinctive hematitic sandstone beds of the Rose Hill Formation cover any dip slopes with red sandstone blocks. Other formations are less well exposed and form lower slopes and valleys.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr781076","usgsCitation":"Lesure, F.G., Williams, B.B., Dunn, M., and Perry, W., 1978, Mineral resources of the Mill Creek, Mountain Lake, and Peters Mountain Wilderness Study Areas, Craig and Giles counties, Virginia and Monroe County, West Virginia: U.S. Geological Survey Open-File Report 78-1076, Report: iv, 69 p.; 8 Plates: 38.51 x 37.67 inches or smaller, https://doi.org/10.3133/ofr781076.","productDescription":"Report: iv, 69 p.; 8 Plates: 38.51 x 37.67 inches or smaller","costCenters":[],"links":[{"id":414034,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1076/plate-6-1.pdf","text":"Plate 6-1","linkFileType":{"id":1,"text":"pdf"}},{"id":414033,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1076/plate-6-2.pdf","text":"Plate 6-2","linkFileType":{"id":1,"text":"pdf"}},{"id":414032,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1076/plate-6-3.pdf","text":"Plate 6-3","linkFileType":{"id":1,"text":"pdf"}},{"id":414031,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1076/plate-6-4.pdf","text":"Plate 6-4","linkFileType":{"id":1,"text":"pdf"}},{"id":414030,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1076/plate-6-5.pdf","text":"Plate 6-5","linkFileType":{"id":1,"text":"pdf"}},{"id":414029,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1076/plate-6-6.pdf","text":"Plate 6-6","linkFileType":{"id":1,"text":"pdf"}},{"id":414028,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1076/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414027,"rank":3,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1978/1076/table-1.pdf","text":"Table 1","linkFileType":{"id":1,"text":"pdf"}},{"id":414026,"rank":2,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1978/1076/table-4.pdf","text":"Table 4","linkFileType":{"id":1,"text":"pdf"}},{"id":148871,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1076/report-thumb.jpg"}],"country":"United States","state":"Virginia, West Virginia","county":"Craig County, Giles County, Monroe County","otherGeospatial":"Mill Creek, Mountain Lake, Peters Mountain Wilderness Study Areas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.8845976961457,\n              37.17302183133792\n            ],\n            [\n              -80.20410471356774,\n              37.17302183133792\n            ],\n            [\n              -80.20410471356774,\n              37.71941663684228\n            ],\n            [\n              -80.8845976961457,\n              37.71941663684228\n            ],\n            [\n              -80.8845976961457,\n              37.17302183133792\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a20c","contributors":{"authors":[{"text":"Lesure, Frank Gardner","contributorId":70752,"corporation":false,"usgs":true,"family":"Lesure","given":"Frank","email":"","middleInitial":"Gardner","affiliations":[],"preferred":false,"id":169829,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Bradford B.","contributorId":6864,"corporation":false,"usgs":true,"family":"Williams","given":"Bradford","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":169826,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunn, Maynard L.","contributorId":40225,"corporation":false,"usgs":true,"family":"Dunn","given":"Maynard L.","affiliations":[],"preferred":false,"id":169828,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Perry, William J.","contributorId":30960,"corporation":false,"usgs":true,"family":"Perry","given":"William J.","affiliations":[],"preferred":false,"id":169827,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":8886,"text":"ofr78253 - 1978 - Petrographic and chemical data on Mesozoic granitic rocks of the Eagle quadrangle, Alaska","interactions":[],"lastModifiedDate":"2021-10-06T20:07:45.700936","indexId":"ofr78253","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":"78-253","title":"Petrographic and chemical data on Mesozoic granitic rocks of the Eagle quadrangle, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78253","usgsCitation":"Foster, H.L., Donato, M.M., and Yount, M.E., 1978, Petrographic and chemical data on Mesozoic granitic rocks of the Eagle quadrangle, Alaska: U.S. Geological Survey Open-File Report 78-253, Report: 29 p.; 5 Plates: 33.62 × 26.39 inches or smaller, https://doi.org/10.3133/ofr78253.","productDescription":"Report: 29 p.; 5 Plates: 33.62 × 26.39 inches or smaller","costCenters":[],"links":[{"id":36453,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0253/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36452,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0253/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36451,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0253/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36450,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0253/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0253/report-thumb.jpg"},{"id":36455,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0253/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36454,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0253/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Eagle quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -144,\n              64\n            ],\n            [\n              -141,\n              64\n            ],\n            [\n              -141,\n              65\n            ],\n            [\n              -144,\n              65\n            ],\n            [\n              -144,\n              64\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68807a","contributors":{"authors":[{"text":"Foster, Helen Laura","contributorId":21936,"corporation":false,"usgs":true,"family":"Foster","given":"Helen","email":"","middleInitial":"Laura","affiliations":[],"preferred":false,"id":158488,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Donato, Mary M.","contributorId":30962,"corporation":false,"usgs":true,"family":"Donato","given":"Mary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":158489,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yount, M. E.","contributorId":76748,"corporation":false,"usgs":true,"family":"Yount","given":"M.","middleInitial":"E.","affiliations":[],"preferred":false,"id":158490,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8881,"text":"ofr78427 - 1978 - Premetamorphic hydrothermal origin of the Tungsten Queen vein, Hamme District, North Carolina, as indicated by mineral textures and minor structures","interactions":[{"subject":{"id":8881,"text":"ofr78427 - 1978 - Premetamorphic hydrothermal origin of the Tungsten Queen vein, Hamme District, North Carolina, as indicated by mineral textures and minor structures","indexId":"ofr78427","publicationYear":"1978","noYear":false,"title":"Premetamorphic hydrothermal origin of the Tungsten Queen vein, Hamme District, North Carolina, as indicated by mineral textures and minor structures"},"predicate":"SUPERSEDED_BY","object":{"id":70047777,"text":"70047777 - 1980 - Textural and structural evidence for a predeformation hydrothermal origin of the Tungsten Queen Deposit, Hamme District, North Carolina","indexId":"70047777","publicationYear":"1980","noYear":false,"title":"Textural and structural evidence for a predeformation hydrothermal origin of the Tungsten Queen Deposit, Hamme District, North Carolina"},"id":1}],"supersededBy":{"id":70047777,"text":"70047777 - 1980 - Textural and structural evidence for a predeformation hydrothermal origin of the Tungsten Queen Deposit, Hamme District, North Carolina","indexId":"70047777","publicationYear":"1980","noYear":false,"title":"Textural and structural evidence for a predeformation hydrothermal origin of the Tungsten Queen Deposit, Hamme District, North Carolina"},"lastModifiedDate":"2023-02-14T22:46:17.122007","indexId":"ofr78427","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":"78-427","title":"Premetamorphic hydrothermal origin of the Tungsten Queen vein, Hamme District, North Carolina, as indicated by mineral textures and minor structures","docAbstract":"<p>The Hamme Tungsten district is a 13-km long, 2-km wide, northeast-trending belt located in northern Vance County, North Carolina and southern Mecklenburg County, Virginia (Fig. 1). The district contains the largest quartz-wolframite-type vein deposits in the United States. Over 50 tungsten-bearing veins occur in this area (Espenshade, 1947), from which more than 1 million short ton units of WO<sub>3</sub> have been produced since World War II Mining terminated in 1971 after a sharp drop in the price of tungsten; currently, the district is inactive.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78427","usgsCitation":"Foose, M.P., and Slack, J.F., 1978, Premetamorphic hydrothermal origin of the Tungsten Queen vein, Hamme District, North Carolina, as indicated by mineral textures and minor structures: U.S. Geological Survey Open-File Report 78-427, iv, 34 p., https://doi.org/10.3133/ofr78427.","productDescription":"iv, 34 p.","costCenters":[],"links":[{"id":413063,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0427/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142654,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0427/report-thumb.jpg"}],"country":"United States","state":"North Carolina, Virginia","otherGeospatial":"Hamme District","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79,36.25 ], [ -79,36.75 ], [ -78.25,36.75 ], [ -78.25,36.25 ], [ -79,36.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6696fc","contributors":{"authors":[{"text":"Foose, Michael P. mfoose@usgs.gov","contributorId":4756,"corporation":false,"usgs":true,"family":"Foose","given":"Michael","email":"mfoose@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":158480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slack, John F. 0000-0001-6600-3130 jfslack@usgs.gov","orcid":"https://orcid.org/0000-0001-6600-3130","contributorId":1032,"corporation":false,"usgs":true,"family":"Slack","given":"John","email":"jfslack@usgs.gov","middleInitial":"F.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":158479,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8880,"text":"ofr78385 - 1978 - Preliminary geologic report on the Harris Lake area, northeastern Minnesota","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr78385","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":"78-385","title":"Preliminary geologic report on the Harris Lake area, northeastern Minnesota","docAbstract":"Intense faulting and fracturing in the Harris Lake area) northeastern Minnesota are documented by detailed field studies. Faults are identified chiefly by the disruption of mappable layers within sequences of plagioclase and plagioclase-olivine cumulates. Most layers grade from olivine-rich bottoms to plagioclase-rich tops and were probably deposited by density currents. Faults trend principally N35?E, N05?W, and N40?W. The recognition of intense faulting and fracturing in this region and an understanding of the currents responsible for cumulate deposition establish a basic geologic framework with important local and regional implications.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78385","usgsCitation":"Foose, M.P., and Cooper, R.W., 1978, Preliminary geologic report on the Harris Lake area, northeastern Minnesota: U.S. Geological Survey Open-File Report 78-385, [3], 24 leaves :ill., maps (1 fold. in envelope) ;28 cm.; (27 p., 1 sheet, scale 1:12,000 - PGS), https://doi.org/10.3133/ofr78385.","productDescription":"[3], 24 leaves :ill., maps (1 fold. in envelope) ;28 cm.; (27 p., 1 sheet, scale 1:12,000 - PGS)","costCenters":[],"links":[{"id":142653,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0385/report-thumb.jpg"},{"id":36444,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0385/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36445,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0385/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673efe","contributors":{"authors":[{"text":"Foose, M. P.","contributorId":97075,"corporation":false,"usgs":true,"family":"Foose","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":158478,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, Roger W.","contributorId":44546,"corporation":false,"usgs":true,"family":"Cooper","given":"Roger","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158477,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7003,"text":"ofr781092 - 1978 - Analytical results for 89 water samples from the Papago Indian Reservation, Arizona","interactions":[],"lastModifiedDate":"2022-10-12T18:56:25.28947","indexId":"ofr781092","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":"78-1092","title":"Analytical results for 89 water samples from the Papago Indian Reservation, Arizona","docAbstract":"Eighty-nine water samples were collected from the Papago Indian Reservation during 1977 and 1978 as a part of a mineral resource study. Each sample was analyzed for copper, zinc, molybdenum, arsenic, uranium, sodium, potassium, calcium, magnesium, bicarbonate, sulfate, chloride, fluoride, and silica. Temperature, pH, and specific conductance were also measured. The data are presented in accompanying tables. Also, included are the location and a description of each sample site.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr781092","usgsCitation":"Ficklin, W.H., Ashton, W., Preston, D.J., and Nowlan, G., 1978, Analytical results for 89 water samples from the Papago Indian Reservation, Arizona: U.S. Geological Survey Open-File Report 78-1092, 29 p., https://doi.org/10.3133/ofr781092.","productDescription":"29 p.","costCenters":[],"links":[{"id":408227,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14596.htm","linkFileType":{"id":5,"text":"html"}},{"id":34295,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1092/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1092/report-thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Papago Indian Reservation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.75,\n              31.583\n            ],\n            [\n              -111.333,\n              31.583\n            ],\n            [\n              -111.333,\n              32.75\n            ],\n            [\n              -112.75,\n              32.75\n            ],\n            [\n              -112.75,\n              31.583\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca1f","contributors":{"authors":[{"text":"Ficklin, Walter H.","contributorId":52565,"corporation":false,"usgs":true,"family":"Ficklin","given":"Walter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":153872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ashton, Wheeler","contributorId":82297,"corporation":false,"usgs":true,"family":"Ashton","given":"Wheeler","email":"","affiliations":[],"preferred":false,"id":153873,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Preston, D. J.","contributorId":22759,"corporation":false,"usgs":false,"family":"Preston","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":153871,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":153874,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":8911,"text":"ofr78825 - 1978 - Hydrologic and geomorphic data from the Piceance Basin, Colorado, 1972-77","interactions":[],"lastModifiedDate":"2023-11-24T19:26:15.060898","indexId":"ofr78825","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":"78-825","title":"Hydrologic and geomorphic data from the Piceance Basin, Colorado, 1972-77","docAbstract":"<p>This report is a compilation of erosion measurements made at 121 channel sites and 45 hillslope sites during the period 1972-77 in the Piceance basin of northwestern Colorado. The data were collected as part of channel-morphology, sediment-transport, and erosion-rate studies being conducted in conjunction with development of the oil-shale resource of the area. The channel measurements were made to determine rates of aggradation, degradation, and lateral movement. Hillslope measurements were obtained to determine rates of soil erosion in the area. No analyses, results, or conclusions are included in this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78825","usgsCitation":"Frickel, D.G., 1978, Hydrologic and geomorphic data from the Piceance Basin, Colorado, 1972-77: U.S. Geological Survey Open-File Report 78-825, 169 p., https://doi.org/10.3133/ofr78825.","productDescription":"169 p.","costCenters":[],"links":[{"id":422918,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0825/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141920,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0825/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Piceance Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.88085832876698,\n              40.155655360329575\n            ],\n            [\n              -108.88085832876698,\n              39.46787280884405\n            ],\n            [\n              -108.02667131704814,\n              39.46787280884405\n            ],\n            [\n              -108.02667131704814,\n              40.155655360329575\n            ],\n            [\n              -108.88085832876698,\n              40.155655360329575\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611812","contributors":{"authors":[{"text":"Frickel, Donald G.","contributorId":23524,"corporation":false,"usgs":true,"family":"Frickel","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":158533,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42904,"text":"ofr78491 - 1978 - Preliminary megafossil biostratigraphy and correlation of stratigraphic sections in the Gulf of Alaska Tertiary province","interactions":[],"lastModifiedDate":"2022-02-23T21:09:24.408504","indexId":"ofr78491","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":"78-491","title":"Preliminary megafossil biostratigraphy and correlation of stratigraphic sections in the Gulf of Alaska Tertiary province","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78491","usgsCitation":"Addicott, W.O., Winkler, G.R., and Plafker, G., 1978, Preliminary megafossil biostratigraphy and correlation of stratigraphic sections in the Gulf of Alaska Tertiary province: U.S. Geological Survey Open-File Report 78-491, 2 Plates: 43.00 × 61.00 inches, https://doi.org/10.3133/ofr78491.","productDescription":"2 Plates: 43.00 × 61.00 inches","costCenters":[],"links":[{"id":168160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":396391,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14744.htm"},{"id":99009,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0491/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":99008,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0491/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Gulf of Alaska Tertiary province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147,\n              58\n            ],\n            [\n              -137,\n              58\n            ],\n            [\n              -137,\n              60.5\n            ],\n            [\n              -147,\n              60.5\n            ],\n            [\n              -147,\n              58\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696696","contributors":{"authors":[{"text":"Addicott, Warren O.","contributorId":80668,"corporation":false,"usgs":true,"family":"Addicott","given":"Warren","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":227375,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winkler, G. R.","contributorId":17964,"corporation":false,"usgs":true,"family":"Winkler","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":227374,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":227373,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":42900,"text":"ofr78341 - 1978 - Preliminary geologic map of the west half of Owyhee County, Idaho","interactions":[{"subject":{"id":42900,"text":"ofr78341 - 1978 - Preliminary geologic map of the west half of Owyhee County, Idaho","indexId":"ofr78341","publicationYear":"1978","noYear":false,"title":"Preliminary geologic map of the west half of Owyhee County, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":67534,"text":"i1256 - 1981 - Geologic map of Owyhee County, Idaho, west of longitude 116 degrees W.","indexId":"i1256","publicationYear":"1981","noYear":false,"title":"Geologic map of Owyhee County, Idaho, west of longitude 116 degrees W."},"id":1}],"supersededBy":{"id":67534,"text":"i1256 - 1981 - Geologic map of Owyhee County, Idaho, west of longitude 116 degrees W.","indexId":"i1256","publicationYear":"1981","noYear":false,"title":"Geologic map of Owyhee County, Idaho, west of longitude 116 degrees W."},"lastModifiedDate":"2022-04-12T21:36:52.998485","indexId":"ofr78341","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":"78-341","title":"Preliminary geologic map of the west half of Owyhee County, Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78341","usgsCitation":"Ekren, E.B., McIntyre, D.H., and Bennett, E.H., 1978, Preliminary geologic map of the west half of Owyhee County, Idaho: U.S. Geological Survey Open-File Report 78-341, 2 Plates: 40.72 x 65.57 inches and 39.55 x 31.07 inches, https://doi.org/10.3133/ofr78341.","productDescription":"2 Plates: 40.72 x 65.57 inches and 39.55 x 31.07 inches","costCenters":[],"links":[{"id":398605,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0341/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398604,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0341/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0341/report-thumb.jpg"},{"id":397087,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14692.htm"}],"scale":"125000","country":"United States","state":"Idaho","county":"Owyhee County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.8333,\n              42\n            ],\n            [\n              -116,\n              42\n            ],\n            [\n              -116,\n              43.583\n            ],\n            [\n              -117.8333,\n              43.583\n            ],\n            [\n              -117.8333,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674196","contributors":{"authors":[{"text":"Ekren, E. B.","contributorId":14371,"corporation":false,"usgs":true,"family":"Ekren","given":"E.","middleInitial":"B.","affiliations":[],"preferred":false,"id":227358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntyre, D. H.","contributorId":45726,"corporation":false,"usgs":true,"family":"McIntyre","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":227359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bennett, Earl H.","contributorId":97093,"corporation":false,"usgs":true,"family":"Bennett","given":"Earl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":227360,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8811,"text":"ofr78864 - 1978 - Release of trace elements from a burning bituminous culm bank","interactions":[],"lastModifiedDate":"2026-02-19T15:09:11.247603","indexId":"ofr78864","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":"78-864","title":"Release of trace elements from a burning bituminous culm bank","docAbstract":"<p>A burning bituminous coal waste-bank at Mather, PA was studied in order to determine if trace elements are being released into the environment in substantial concentrations. Samples of the minerals forming on the surface of the bank, the gases escaping from vents, and the water and sediment from a nearby stream were analyzed to determine the presence of these elements.&nbsp;</p><p>The output of trace elements from the Mather bank, as is evidenced by the minerals forming on the surface, is relatively low compared to the output from actively burning anthracite culm-banks.&nbsp;</p><p>Copper was the only element of potential environmental significance found accumulating on the Mather bank. However, the sediment &nbsp;in the vicinity of the bank and the waters immediately downstream did not have anomolously high concentrations of copper. &nbsp;</p><p>Relatively high concentrations of arsenic were found in the organic matter at the base of the bank but no evidence of high As values &nbsp;were found downstream. &nbsp;</p><p>No potentially toxic elements, other than sulfur, were detected in the gases being emitted from the culm-bank.&nbsp;</p><p>Because of the quiescent condition of the Mather culm-bank the question of the fate of trace elements released in the burning process remains unanswered.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78864","usgsCitation":"Finkelman, R.B., 1978, Release of trace elements from a burning bituminous culm bank: U.S. Geological Survey Open-File Report 78-864, 37 p., https://doi.org/10.3133/ofr78864.","productDescription":"37 p.","costCenters":[],"links":[{"id":500182,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0864/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142752,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0864/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db63444f","contributors":{"authors":[{"text":"Finkelman, Robert B.","contributorId":85951,"corporation":false,"usgs":true,"family":"Finkelman","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":158367,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42901,"text":"ofr78533 - 1978 - Preliminary geologic map of the west half of the Pocatello 1° x 2° quadrangle, Idaho","interactions":[],"lastModifiedDate":"2024-10-30T21:49:22.493996","indexId":"ofr78533","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":"78-533","title":"Preliminary geologic map of the west half of the Pocatello 1° x 2° quadrangle, Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78533","usgsCitation":"Armstrong, R.L., Smith, J.F., Covington, H., and Williams, P.L., 1978, Preliminary geologic map of the west half of the Pocatello 1° x 2° quadrangle, Idaho: U.S. Geological Survey Open-File Report 78-533, 1 Plate: 41.32 × 27.44 inches, https://doi.org/10.3133/ofr78533.","productDescription":"1 Plate: 41.32 × 27.44 inches","costCenters":[],"links":[{"id":108558,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14776.htm","linkFileType":{"id":5,"text":"html"},"description":"14776"},{"id":168063,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80715,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0533/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Idaho","otherGeospatial":"Pocatello 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113,\n              42\n            ],\n            [\n              -114,\n              42\n            ],\n            [\n              -114,\n              43\n            ],\n            [\n              -113,\n              43\n            ],\n            [\n              -113,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674081","contributors":{"authors":[{"text":"Armstrong, Richard L.","contributorId":58701,"corporation":false,"usgs":true,"family":"Armstrong","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":227362,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, J. F. Jr.","contributorId":54650,"corporation":false,"usgs":true,"family":"Smith","given":"J.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":227361,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Covington, H. R.","contributorId":92671,"corporation":false,"usgs":true,"family":"Covington","given":"H. R.","affiliations":[],"preferred":false,"id":227364,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, P. L.","contributorId":79109,"corporation":false,"usgs":true,"family":"Williams","given":"P.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":227363,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":8858,"text":"ofr78488 - 1978 - Relative concentrations of lanthanides in minerals of the bastnaesite group","interactions":[],"lastModifiedDate":"2026-03-06T16:53:17.307862","indexId":"ofr78488","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":"78-488","title":"Relative concentrations of lanthanides in minerals of the bastnaesite group","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78488","usgsCitation":"Fleischer, M., 1978, Relative concentrations of lanthanides in minerals of the bastnaesite group: U.S. Geological Survey Open-File Report 78-488, 20 leaves ;28 cm., https://doi.org/10.3133/ofr78488.","productDescription":"22 p.","costCenters":[],"links":[{"id":500866,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0488/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141109,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0488/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db6344b5","contributors":{"authors":[{"text":"Fleischer, Michael","contributorId":65835,"corporation":false,"usgs":true,"family":"Fleischer","given":"Michael","email":"","affiliations":[],"preferred":false,"id":158446,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8580,"text":"ofr7844 - 1978 - Coal resource occurrence and coal development potential maps of the Carbon quadrangle, Carbon County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr7844","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":"78-44","title":"Coal resource occurrence and coal development potential maps of the Carbon quadrangle, Carbon County, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7844","usgsCitation":"Texas Instruments Incorporated, 1978, Coal resource occurrence and coal development potential maps of the Carbon quadrangle, Carbon County, Wyoming: U.S. Geological Survey Open-File Report 78-44, iv, 27 leaves, 4 leaves of ill. :ill., maps ;28 cm., https://doi.org/10.3133/ofr7844.","productDescription":"iv, 27 leaves, 4 leaves of ill. :ill., maps ;28 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,{"id":7166,"text":"ofr7875 - 1978 - Geochronologic data for the Arabian Shield","interactions":[],"lastModifiedDate":"2014-05-29T08:38:46","indexId":"ofr7875","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":"78-75","title":"Geochronologic data for the Arabian Shield","docAbstract":"The radiometric ages reported below were completed during the period 1957-1936. the rock samples were provided and examined petrographically by Glen F. Brown and his associates at the U.S. Geological Survey. The 25 Rb-Sr ages of biotites and feldspars and the 25 K-Ar ages of biotites, hornblendes, and total rock samples constituted the initial suite of ages for the Arabian Shield. Zircons in the quantity required for analysis were not found in any of the rocks examined.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7875","usgsCitation":"Aldrich, L.T., Brown, G.F., Hedge, C., and Marvin, R., 1978, Geochronologic data for the Arabian Shield: U.S. Geological Survey Open-File Report 78-75, 20 p., https://doi.org/10.3133/ofr7875.","productDescription":"20 p.","numberOfPages":"29","costCenters":[],"links":[{"id":287779,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287778,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0075/report.pdf"}],"country":"Saudi Arabia","otherGeospatial":"Arabian Shield","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 34.9,17.05 ], [ 34.9,29.25 ], [ 45.25,29.25 ], [ 45.25,17.05 ], [ 34.9,17.05 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6a9e99","contributors":{"authors":[{"text":"Aldrich, Lyman Thomas","contributorId":108105,"corporation":false,"usgs":true,"family":"Aldrich","given":"Lyman","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":154576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Glen F.","contributorId":23943,"corporation":false,"usgs":true,"family":"Brown","given":"Glen","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":154575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hedge, Carl","contributorId":15610,"corporation":false,"usgs":true,"family":"Hedge","given":"Carl","email":"","affiliations":[],"preferred":false,"id":154574,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marvin, Richard","contributorId":12473,"corporation":false,"usgs":true,"family":"Marvin","given":"Richard","affiliations":[],"preferred":false,"id":154573,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":20000,"text":"ofr781024 - 1978 - On the development of strong-motion instrument networks in the United States","interactions":[],"lastModifiedDate":"2023-03-13T18:51:22.842395","indexId":"ofr781024","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":"78-1024","title":"On the development of strong-motion instrument networks in the United States","docAbstract":"<p>This report outlines a plan for the distribution of strong-motion instrumentation throughout the United States. The present \"national\" network of strong-motion instrumentation has evolved through the merger of several programs initiated by different agencies and organizations with objectives ranging from research to regulation. It is the result of the coordination of instrument maintenance and record archival currently provided by the Seismic Engineering Branch of the U.S. Geological Survey (formerly the Seismological Field Survey of the U.S. Coast &amp; Geodetic Survey, or the National Ocean Survey, or the National Oceanic and Atmospheric Administration). The USGS operates the program under funding from the National Science Foundation (NSF) in cooperation with other federal, state, and local agencies.</p><p>NSF supports a data management function and the operation of a network of about 200 accelerographs and 300 seismoscopes utilized for studies of ground motion and building response. The State of California is developing its own strong-motion instrumentation program (CSMIP), which includes measurements of ground motion as well as the response of representative types of structures. The CSMIP network is the largest network operated by a single agency anywhere in the world. Eventually it will contain a total of about 1000 accelerographs. The Army Corps of Engineers (COE) is developing a program for monitoring the response of earth dams, which eventually will include as many as 400 instruments on over 100 dams. Other agencies and organizations are developing networks appropriate to their missions or objectives. At present the number of instruments owned by these other agencies is less than 100 in each case, although several agencies are still expanding their networks. The present distribution of accelerographs in the United States is indicated in Figure 1 (see: USGS, 1977, also).</p><p>In 1964 the cities of Los Angeles and Beverly Hills, California passed ordinances which required 3 accelerographs to be installed in all high-rise buildings. Initially, these instruments were installed and maintained as a part of the strong-motion program of the Seismological Field Survey (SFS). As the number of installations required by such codes increased, it became apparent that the maintenance of these instruments placed an inordinate burden on and created an imbalance in the SFS operated program (in 1972, 50 percent of the \"national\" program was concentrated in Los Angeles). With the transfer of the SFS program responsibility to the NSF and with the development of the CSMIP, the responsibility for maintenance of code required instruments has reverted to the city building officials and the building owners.</p><p>As the coordinated network of strong-motion instruments has grown, the maintenance of the instruments has required a larger staff than the USGS could provide under existing personnel ceilings. This situation has been resolved by the agencies with the larger networks performing their own installation and maintenance. The USGS maintains an archive of first class copies of all records, whereas other agencies maintain archives of their own records, only. In addition, the USGS coordinates the routine processing of all of the significant records, although other agencies will process their own data if they consider it to have a higher priority than does the USGS. In response to a recent change in their legislated charter, the CSMIP is beginning to develop a capability to process the data collected under that program.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr781024","usgsCitation":"Matthiesen, R., 1978, On the development of strong-motion instrument networks in the United States: U.S. Geological Survey Open-File Report 78-1024, iii, 91 p., https://doi.org/10.3133/ofr781024.","productDescription":"iii, 91 p.","costCenters":[],"links":[{"id":152473,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1024/report-thumb.jpg"},{"id":414025,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1024/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"geometry\": {\n        \"type\": \"MultiPolygon\",\n        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