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,{"id":28641,"text":"wri844239 - 1985 - Potential effects of surface coal mining on the hydrology of the Horse Creek area, Sheridan and Moorhead coal fields, southeastern Montana","interactions":[],"lastModifiedDate":"2022-01-06T22:58:50.636271","indexId":"wri844239","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4239","title":"Potential effects of surface coal mining on the hydrology of the Horse Creek area, Sheridan and Moorhead coal fields, southeastern Montana","docAbstract":"The Horse Creek area of the Sheridan and Moorhead coal fields, 16 miles east of the Decker Coal Mines near the Tongue River, contains large reserves of Federally owned coal that have been identified for potential lease sale. A hydrologic study was conducted in the area to describe existing hydrologic systems and to assess potential impacts of surface coal mining on local water resources. Hydrologic data collected from private wells, observation wells, test holes, and springs indicate that the aquifers are primarily coal and sandstone beds in the upper part of the Tongue River Member of the Fort Union Formation (Paleocene age) and sand and gravel of valley alluvium (Pleistocene and Holocene age). Surface-water resources are mostly limited to a few stock ponds receiving discharge from springs in the higher ports of the area. Two stock wells, one spring, and three stock ponds receiving discharge from springs supply most of the water used within the Horse Creek basin; the only use is watering of livestock. Mining of the Anderson and Dietz coal beds would destroy one stock well and two ponds receiving discharge from springs, and would lower the potentiometric surface within the coal and sandstone aquifers. Although mining would alter existing hydrologic systems, alternative deeper water supplies are available. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844239","usgsCitation":"McClymonds, N.E., 1985, Potential effects of surface coal mining on the hydrology of the Horse Creek area, Sheridan and Moorhead coal fields, southeastern Montana: U.S. Geological Survey Water-Resources Investigations Report 84-4239, v, 61 p., https://doi.org/10.3133/wri844239.","productDescription":"v, 61 p.","costCenters":[],"links":[{"id":57476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4239/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4239/report-thumb.jpg"},{"id":393996,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36088.htm"}],"country":"United States","state":"Montana","otherGeospatial":"Horse Creek area, Sheridan and Moorhead coal fields","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.492,\n              45.075\n            ],\n            [\n              -106.305,\n              45.075\n            ],\n            [\n              -106.305,\n              45.158\n            ],\n            [\n              -106.492,\n              45.158\n            ],\n            [\n              -106.492,\n              45.075\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a83d1","contributors":{"authors":[{"text":"McClymonds, N. E.","contributorId":94653,"corporation":false,"usgs":true,"family":"McClymonds","given":"N.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":200160,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15734,"text":"ofr86302 - 1985 - Permitted water use in Iowa, 1985","interactions":[],"lastModifiedDate":"2016-03-04T14:40:27","indexId":"ofr86302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"86-302","title":"Permitted water use in Iowa, 1985","docAbstract":"<p>This report summarizes where, how much and for what purpose water is allocated for use in Iowa with permits issued by the Department of Water, Air and Waste Management. In Iowa, from a total permitted water use of 855,175.45 million gallons per year, about 58 percent is from surface-water sources and about 42 percent is from ground-water sources. Streams are 80.5 percent of the total surface-water use and wells make up 80.1 percent of the total ground-water use, with 65.4 percent of ground water coming from surficial aquifers. Power generation is the use category that is permitted the largest amount of total water use, 46.6 percent, with surface water being the source of 96.7 percent and 77.9 percent of the surface water is from streams. The public water suppliers' category is the next largest use type with 15.7 percent of the total permitted water. Ground water constitutes 74.4 percent of the public water supplier category with 51.7 percent from surficial aquifers. Surface water makes up 25.6 percent of this category with 83.0 percent of the surface water withdrawn from streams. Mining comprises 13.4 percent of the total water use and is the third largest water-use category. Ground water is the source of 63.3 percent of permitted mining water use with 94.3 percent of this from quarries and sand and gravel pits. Surface water is the source of 36.7 percent of the permitted mining water use with 97.6 percent from streams. Irrigation is the fourth largest permitted use type using 12.0 percent of the total water use. Eighty-eight percent of irrigation is from ground-water sources where surficial aquifers account for 94.7 percent. Streams are 81.1 percent of irrigational surface-water use. Self-supplied industrial users are permitted 10.6 percent of the total permitted water use with 85.5 percent of this from ground-water sources and 14.5 percent from surface-water sources. Of the self-supplied industrial ground-water use, 47.9 percent comes from surficial aquifers and of the self-supplied industrial surface-water use 86.1 percent is from streams. Self-supplied commercial use is allocated 1.5 percent of the total permitted water. Surface-water is the source of 37.7 percent of this and 62.3 percent is from ground-water sources. Agricultural (non-irrigation) use is 0.3 percent of the total permitted water with 73.3 percent from groundwater sources and 26.7 percent from surface-water sources. The areas that are allocated the most water permits are east-central Iowa and west-central Iowa.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr86302","collaboration":"Prepared in cooperation with Iowa Department of Water, Air and Waste Management, and the Iowa Geological Survey","usgsCitation":"Runkle, D., Newman, J., and Shields, E., 1985, Permitted water use in Iowa, 1985: U.S. Geological Survey Open-File Report 86-302, 24 p.: ill., maps; 22 x 28 cm., https://doi.org/10.3133/ofr86302.","productDescription":"24 p.: ill., maps; 22 x 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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L.","contributorId":57081,"corporation":false,"usgs":true,"family":"Runkle","given":"D. L.","affiliations":[],"preferred":false,"id":171615,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newman, J.L.","contributorId":103294,"corporation":false,"usgs":true,"family":"Newman","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":171617,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shields, E.M.","contributorId":73620,"corporation":false,"usgs":true,"family":"Shields","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":171616,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28424,"text":"wri854146 - 1985 - Summary of northern Atlantic Coastal Plain hydrology and its relation to disposal of high-level radioactive waste in buried crystalline rock – A preliminary appraisal","interactions":[],"lastModifiedDate":"2021-12-14T22:25:16.309266","indexId":"wri854146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4146","title":"Summary of northern Atlantic Coastal Plain hydrology and its relation to disposal of high-level radioactive waste in buried crystalline rock – A preliminary appraisal","docAbstract":"Interpretation of available hydrologic data suggests that some areas beneath the Coastal Plain in the States of Delaware, Maryland, New Jersey, North Carolina, and Virginia might have some potential for the disposal of nuclear waste in crystalline rock that is buried beneath the Coastal Plain sediments. The areas of major interest occur where the top of the basement rock lies between 1,000 and 4,000 feet below sea level, the aquifer(s) immediately above the basement rock are saturated with saline water, confining material overlies the saline water bearing aquifer(s), and groundwater flow in the saline water aquifer(s) can be established. Preliminary data on (1) the distribution and thickness of the lowermost aquifers and confining beds, (2) the distribution of hydraulic conductivity in the lowermost aquifers, (3) estimated hydraulic heads and inferred direction of lateral groundwater flow for 1980, and (4) the distribution of saline water and brine, indicate eastern parts of the study area relatively best meet most of the criteria proposed for sediments that would overlie any potential buried crystalline-rock disposal site.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854146","usgsCitation":"Lloyd, O., Larson, J.D., and Davis, R.W., 1985, Summary of northern Atlantic Coastal Plain hydrology and its relation to disposal of high-level radioactive waste in buried crystalline rock – A preliminary appraisal: U.S. Geological Survey Water-Resources Investigations Report 85-4146, vi, 132 p., https://doi.org/10.3133/wri854146.","productDescription":"vi, 132 p.","costCenters":[],"links":[{"id":392912,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36309.htm"},{"id":57227,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4146/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159230,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4146/report-thumb.jpg"}],"country":"United States","state":"Delaware, Maryland, New Jersey, North Carolina, Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.5,\n              33.833\n            ],\n            [\n              -74,\n              33.833\n            ],\n            [\n              -74,\n              40.5\n            ],\n            [\n              -79.5,\n              40.5\n            ],\n            [\n              -79.5,\n              33.833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a55ea","contributors":{"authors":[{"text":"Lloyd, O. B.","contributorId":75189,"corporation":false,"usgs":true,"family":"Lloyd","given":"O. B.","affiliations":[],"preferred":false,"id":199771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larson, J. D.","contributorId":83084,"corporation":false,"usgs":true,"family":"Larson","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":199772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199773,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28232,"text":"wri854155 - 1985 - A preliminary assessment of land-surface subsidence in the El Paso area, Texas","interactions":[],"lastModifiedDate":"2018-10-30T12:49:42","indexId":"wri854155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4155","title":"A preliminary assessment of land-surface subsidence in the El Paso area, Texas","docAbstract":"<p>The northeast and southeast parts of the El Paso area are underlain by Hueco bolson deposits as much as 9,000 feet thick. The deposits consist of lenses of gravel, sand, silt, and clay. In the Rio Grande Valley, about 400 to 450 feet of these deposits have been eroded and replaced with as much as 200 feet of alluvium. Ground water in the shallow alluvial aquifer in the Rio Grande Valley and in the Hueco bolson aquifer outside the valley is under water-table conditions, whereas ground water in the bolson aquifer in the valley is under leaky artesian conditions. Maximum water-level declines in the Hueco bolson aquifer are 110 feet east of the Franklin Mountains and 150 feet in the downtown El Paso area. For the shallow aquifer, the maximum declines have been 125 feet in the downtown area. Compressable materials in the freshwater zone of the aquifer range from 50 to 450 feet.</p>\n<p>Recharge from the Rio Grande to the shallow alluvial aquifer has increased from an estimated 15,000 acre-feet during 1968 to 30,000 acre-feet during 1983, an increase of about 1,000 acre-feet per year. Leakage from the Rio Grande is expected to continually increase in the near future because of a continued decline in ground-water levels. The amount of leakages from the canals is much less than from the river.</p>\n<p>Releveling of bench marks along lines to the northeast and the southeast of the Rio Grande, and along its channel commonly show land subsidence of about 0.2 foot. The maximum measured subsidence is 0.41 foot along the river in the Chamizal zone. No subsidence was detected at the Riverside Diversion Dam. A comparison of subsidence, water-level declines, and clay thickness along the three survey lines shows the expected correlation of greater subsidence with thicker accumulated clay material for a given decline in water levels. The preconsolidation stress was expected to range from 85 to 115 feet of water-level decline on the basis of subsidence studies in Arizona and California. A study of specific-unit compaction along the three survey lines shows that the values usually range between 1.0 to 2.5 x 10-5 feet per feet squared. These values are comparable to the ones computed in the Tulare-Wasco, California, and Houston-Galveston, Texas, areas following the exceedance of the local preconsolidation stress. Because of this comparability, the specific-unit compaction for future periods in the El Paso area probably will not increase dramatically when the preconsolidation stress is exceeded, if it has not already been exceeded.</p>\n<p>In addition to regional subsidence, local subsidence is indicated by observable surface fractures but has not been verified by precise leveling. These local areas coincide with areas that historically were swamps along the Rio Grande.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri854155","collaboration":"Prepared in cooperation with the Bureau of Reclamation","usgsCitation":"Land, L.F., and Armstrong, C.A., 1985, A preliminary assessment of land-surface subsidence in the El Paso area, Texas: U.S. Geological Survey Water-Resources Investigations Report 85-4155, vi, 96 p., https://doi.org/10.3133/wri854155.","productDescription":"vi, 96 p.","numberOfPages":"108","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":57062,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4155/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4155/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"El Paso","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.32293701171874,\n              31.647536225797772\n            ],\n            [\n              -106.35314941406249,\n              31.701882151861714\n            ],\n            [\n              -106.37443542480469,\n              31.71122878128754\n            ],\n            [\n              -106.38198852539062,\n              31.73400724374667\n            ],\n            [\n              -106.45271301269531,\n              31.764369817056387\n            ],\n            [\n              -106.468505859375,\n              31.76145077153307\n            ],\n            [\n              -106.47468566894531,\n              31.750941445321764\n            ],\n            [\n              -106.48773193359375,\n              31.74918977495709\n            ],\n            [\n              -106.50421142578125,\n              31.756780107186728\n            ],\n            [\n              -106.51588439941406,\n              31.770791393089315\n            ],\n            [\n              -106.52961730957031,\n              31.783633207994736\n            ],\n            [\n              -106.53648376464844,\n              31.94633593313394\n            ],\n            [\n              -106.32980346679686,\n              31.94808386339691\n            ],\n            [\n              -106.32293701171874,\n              31.647536225797772\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6aaf25","contributors":{"authors":[{"text":"Land, L. F.","contributorId":17253,"corporation":false,"usgs":true,"family":"Land","given":"L.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199434,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60393,"text":"mf1573B - 1985 - Aeromagnetic maps of the Mazatzal Wilderness and contiguous roadless areas, Gila, Maricopa, and Yavapai counties, Arizona","interactions":[],"lastModifiedDate":"2016-08-23T08:22:42","indexId":"mf1573B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1573","chapter":"B","title":"Aeromagnetic maps of the Mazatzal Wilderness and contiguous roadless areas, Gila, Maricopa, and Yavapai counties, Arizona","docAbstract":"<p>The Mazatzal Wilderness and contiguous roadless areas are located in Tonto and Coconino National Forests, west and southwest of Payson, and are almost exactly in the geographic center of Arizona. This is a region of relatively small mining districts and few mines, but occurrences of many different metals are widespread.</p>\n<p>The Mazatzal Mountains constitute the dominant physiographic feature of the wilderness. The eastern slopes of these mountains rise steeply from about 3,500 ft in altitude along the valley of Rye Creek east of the range, to 7,903 ft at Mazatzal Peak. To the west, the range slopes steeply from the crest then more gently along the lower flanks to the Werde River, one of the main drainage channels of Arizona. In the northern part of the wilderness, the East Werde River, a tributary of the Verde, occupies a deep canyon that separates the Mazatzal Mountains from mesas to the north. The lowest parts of the wilderness have altitudes of about 2,200 ft and are located near Bartlett Reservoir in the southwestern part of the area studied.</p>\n<p>Two aeromagnetic surveys were flown and interpreted to aid in the delineation of subsurface lithology and structure: one survey was flown at a low level (1,000 ft above ground) and the other at a high level (9,000 ft above sea level). In addition, the results of a small-scale electromagnetic (EM) survey are briefly discussed; the surface EM survey took place in an area of copper concentrations and past exploration activity to look for evidence of massive sulfide mineralization.</p>\n<p>Studies of the geology, geochemistry (Marsh and others, 1983a, b, Erickson, 1984), mines and prospects (Ellis, 1982), and mineral resource potential (Wrucke and others, 1983) of the Mazatzal Wilderness and contiguous roadless areas have been published elsewhere.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1573B","isbn":"0607813288","usgsCitation":"Moss, C.K., and Abrams, G.A., 1985, Aeromagnetic maps of the Mazatzal Wilderness and contiguous roadless areas, Gila, Maricopa, and Yavapai counties, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1573, 2 Plates: 38.70 x 50.88 inches and 30.79 x 28.29 inches, https://doi.org/10.3133/mf1573B.","productDescription":"2 Plates: 38.70 x 50.88 inches and 30.79 x 28.29 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1573B.JPG"},{"id":327379,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1573-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327380,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1573-B/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Arizona","county":"Gila County, Maricopa County, Yavapai County","otherGeospatial":"Mazatzal Wilderness and contiguous roadless areas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.68333333333334,33.8675 ], [ -111.68333333333334,34.33416666666667 ], [ -111.38333333333334,34.33416666666667 ], [ -111.38333333333334,33.8675 ], [ -111.68333333333334,33.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d7e","contributors":{"authors":[{"text":"Moss, C. K.","contributorId":94661,"corporation":false,"usgs":true,"family":"Moss","given":"C.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":263672,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abrams, G. A.","contributorId":27047,"corporation":false,"usgs":true,"family":"Abrams","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":263671,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27937,"text":"wri854263 - 1985 - Transit losses and traveltimes for water-supply releases from Marion Lake during drought conditions, Cottonwood River, east-central Kansas","interactions":[],"lastModifiedDate":"2022-01-10T21:28:07.938796","indexId":"wri854263","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4263","title":"Transit losses and traveltimes for water-supply releases from Marion Lake during drought conditions, Cottonwood River, east-central Kansas","docAbstract":"<p>A streamflow routing model was used to calculate the transit losses and traveltimes. Channel and aquifer characteristics, and the model control parameters, were estimated from available data and then verified to the extent possible by comparing model simulated streamflow to observed streamflow at streamflow gaging stations. Transit losses and traveltimes for varying reservoir release rates and durations then were simulated for two different antecedent streamflow (drought) conditions. For the severe-drought antecedent-streamflow condition, it was assumed that only the downstream water use requirement would be released from the reservoir. For a less severe drought (LSD) antecedent streamflow condition, it was assumed than any releases from Marion Lake for water supply use downstream, would be in addition to a nominal dry weather release of 5 cu ft/sec. Water supply release rates of 10 and 25 cu ft/sec for the severe drought condition and 5, 10, and 25 cu ft/sec for the less severe drought condition were simulated for periods of 28 and 183 days commencing on July 1. Transit losses for the severe drought condition for all reservoir release rates and durations ranged from 12% to 78% of the maximum downstream flow rate and from 27% to 91% of the total volume of reservoir storage released. For the LSD condition, transit losses ranged from 7% to 29% of the maximum downstream flow rate and from 10% to 48% of the total volume of release. The 183-day releases had larger total transit losses, but losses on a percentage basis were less than the losses for the 28-day release period for both antecedent streamflow conditions. Traveltimes to full response (80% of the maximum downstream flow rate), however, showed considerable variation. For the release of 5 cu ft/sec during LSD conditions, base flow exceeded 80% of the maximum flow rate near the confluence; the traveltime to full response was undefined for those simulations. For the releases of 10 and 25 cu ft/sec during the same drought condition, traveltimes to full response ranged from 4.4 to 6.5 days. For releases of 10 and 25 cu ft/sec during severe drought conditions, traveltimes to full response near the confluence with the Neosho River ranged from 8.3 to 93 days.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854263","usgsCitation":"Jordan, P.R., and Hart, R.J., 1985, Transit losses and traveltimes for water-supply releases from Marion Lake during drought conditions, Cottonwood River, east-central Kansas: U.S. Geological Survey Water-Resources Investigations Report 85-4263, vi, 41 p., https://doi.org/10.3133/wri854263.","productDescription":"vi, 41 p.","costCenters":[],"links":[{"id":394144,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36405.htm"},{"id":56751,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4263/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4263/report-thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"Cottonwood River, Marion Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.083,\n              38.221\n            ],\n            [\n              -96.017,\n              38.221\n            ],\n            [\n              -96.017,\n              38.433\n            ],\n            [\n              -97.083,\n              38.433\n            ],\n            [\n              -97.083,\n              38.221\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f48","contributors":{"authors":[{"text":"Jordan, P. R.","contributorId":7282,"corporation":false,"usgs":true,"family":"Jordan","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198933,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hart, R. J.","contributorId":62607,"corporation":false,"usgs":true,"family":"Hart","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198934,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27260,"text":"wri844315 - 1985 - Estimated water and nutrient inflows and outflows Lake Cochituate, eastern Massachusetts, 1977-79","interactions":[],"lastModifiedDate":"2022-02-16T20:37:17.448552","indexId":"wri844315","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4315","title":"Estimated water and nutrient inflows and outflows Lake Cochituate, eastern Massachusetts, 1977-79","docAbstract":"<p>Streamflow was the major source of water and nutrients (nitrogen and phosphorus) to Lake Cochituate, followed by ground water, and then precipitation during April 1978 through March 1979. Compared to all sources during that period, streams contributed 7,217 million gallons (a little over 82 percent) of water, 63 ,000 pounds (between 50 and 60 percent) of nitrogen, and 3,000 pounds (94 percent) of phosphorus. A little over 60 percent of all the water that entered Lake Cochituate flowed from Fisk Pond. This single source transported about 38,000 pounds of nitrogen and 2,000 pounds of phosphorus. Ground-water inflow to Lake Cochituate occurs along its shoreline except at the north end of Lake Cochituate 's North Pond where natural seepage from the lake is occurring and at locations on the lake 's Middle and South Ponds where municipal wells induce infiltration of lake water amounting to 1,228 million gallons for that period. Discharge of ground water to the lake was estimated to range from 462 to 816 million gallons and transported from 31,000 to 55,000 pounds of nitrogen and from 46 to 82 pounds of phosphorus. Bulk precipitation was estimated to contribute about the same volume of water to the lake as ground water but double its phosphorus load. However, the load of nitrogen, 8000 pounds, from bulk precipitation was the smallest of any source.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri844315","usgsCitation":"Gay, F.B., 1985, Estimated water and nutrient inflows and outflows Lake Cochituate, eastern Massachusetts, 1977-79: U.S. Geological Survey Water-Resources Investigations Report 84-4315, Report: vi, 59 p.; 2 Plates: 21.50 × 29.50 inches and 17.00 × 18.00 inches, https://doi.org/10.3133/wri844315.","productDescription":"Report: vi, 59 p.; 2 Plates: 21.50 × 29.50 inches and 17.00 × 18.00 inches","costCenters":[],"links":[{"id":123985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4315/report-thumb.jpg"},{"id":56133,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4315/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56134,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4315/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56135,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4315/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396033,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36156.htm"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Lake Cochituate","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.458,\n              42.233\n            ],\n            [\n              -71.328,\n              42.233\n            ],\n            [\n              -71.328,\n              42.35\n            ],\n            [\n              -71.458,\n              42.35\n            ],\n            [\n              -71.458,\n              42.233\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcca3","contributors":{"authors":[{"text":"Gay, F. B.","contributorId":55002,"corporation":false,"usgs":true,"family":"Gay","given":"F.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":197815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59736,"text":"mf1765 - 1985 - Stratigraphic cross sections and correlation of lignites in the Sentinel Butte member and upper part of the Tongue River member of the Fort Union Formation between Amidon and Fryburg, North Dakota","interactions":[],"lastModifiedDate":"2018-09-26T15:00:08","indexId":"mf1765","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1765","title":"Stratigraphic cross sections and correlation of lignites in the Sentinel Butte member and upper part of the Tongue River member of the Fort Union Formation between Amidon and Fryburg, North Dakota","docAbstract":"<p>The Austin Farm bed was once mined form an adit in the SE1/4 sec, T. 136 N., R. 101 W. Its westerly outcrop extends from that point northward along the east side and north end of the valley of Third Creek at elevations between about 2740 and 2800 ft. It is the uppermost lignite bed preserved on Hanley and Cliffs Plateaus in T. 137 N., R. 101 W., where its thickness is generally from 2 to 4 ft. It is exposed at the NW corner of sec. 26, T. 138 N., R. 101 W., where it is 0.7 ft thick. The surface trace of the Austin Farm bed has not been mapped north of that location, and because of its thinness and local absence it is probably rarely exposed at the surface north of that point.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1765","isbn":"0607815965","usgsCitation":"Hinds, J.S., 1985, Stratigraphic cross sections and correlation of lignites in the Sentinel Butte member and upper part of the Tongue River member of the Fort Union Formation between Amidon and Fryburg, North Dakota: U.S. Geological Survey Miscellaneous Field Studies Map 1765, 41.89 x 57.39 inches, https://doi.org/10.3133/mf1765.","productDescription":"41.89 x 57.39 inches","costCenters":[],"links":[{"id":180076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1765/report-thumb.jpg"},{"id":357801,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1765/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"256000","country":"United States","state":"North Dakota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.36666666666666,46.45138888888889 ], [ -103.36666666666666,46.901111111111106 ], [ -103.0675,46.901111111111106 ], [ -103.0675,46.45138888888889 ], [ -103.36666666666666,46.45138888888889 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af757","contributors":{"authors":[{"text":"Hinds, Jim S.","contributorId":29800,"corporation":false,"usgs":true,"family":"Hinds","given":"Jim","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":262508,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59735,"text":"mf1766 - 1985 - Stratigraphic cross section and coal bed correlations of uppermost Cretaceous and Paleocene rocks between Painted Canyon and Davis Buttes, North Dakota","interactions":[],"lastModifiedDate":"2016-08-22T10:55:45","indexId":"mf1766","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1766","title":"Stratigraphic cross section and coal bed correlations of uppermost Cretaceous and Paleocene rocks between Painted Canyon and Davis Buttes, North Dakota","docAbstract":"<p>Recent detailed coal studies in the area between Havelock and Fryburg, N. Dak. (Hinds, 1983; 1985), have resulted in some revised coal-bed correlations that are, in places, in disagreement with previous work (Banet, 1980; Hares, 1928; Lewis, 1979; Menge, 1977; Owen, 1979; Rehbein, 1977; Royse, 1967). The strati graphically most important of these have been specifically discussed (Hinds, 1983; 1985), but many others, of more or less local significance, were not specifically mentioned.</p>\n<p>This report is an extension of the author's stratigraphic and coal -bed correlations from the vicinity of the Painted Canyon Overlook, at the south edge of Theodore Roosevelt National Memorial Park, eastward to the vicinity of Davis Buttes, near Dickinson, N. Dak.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1766","isbn":"0607815973","usgsCitation":"Hinds, J., 1985, Stratigraphic cross section and coal bed correlations of uppermost Cretaceous and Paleocene rocks between Painted Canyon and Davis Buttes, North Dakota: U.S. Geological Survey Miscellaneous Field Studies Map 1766, Plate: 40.74 x 57.14 inches, https://doi.org/10.3133/mf1766.","productDescription":"Plate: 40.74 x 57.14 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326205,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1766.JPG"},{"id":327247,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1766/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000","country":"United States","state":"North Dakota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.40083333333334,46.833333333333336 ], [ -103.40083333333334,46.9175 ], [ -102.70138888888889,46.9175 ], [ -102.70138888888889,46.833333333333336 ], [ -103.40083333333334,46.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af8c9","contributors":{"authors":[{"text":"Hinds, J.S.","contributorId":8881,"corporation":false,"usgs":true,"family":"Hinds","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":262507,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59695,"text":"mf1631D - 1985 - Aeromagnetic map of the Sandia Mountain Wilderness, Bernalillo and Sandoval counties, New Mexico","interactions":[],"lastModifiedDate":"2016-08-22T10:59:26","indexId":"mf1631D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1631","chapter":"D","title":"Aeromagnetic map of the Sandia Mountain Wilderness, Bernalillo and Sandoval counties, New Mexico","docAbstract":"<p>During 1981 and 1982 the U.S. Geological Survey and the U.S. Bureau of Mimes conducted field investigations to evaluate the mineral resource potential of the Sandia Mountain Wilderness, Bernalillo and Sandoval Counties, New Mexico. This report and map represent only the results of the aeromagnetic compilation from previous publications (U.S. geological Survey, 1975a,b,c). The wilderness encompasses 61 mi<sup>2</sup> (37,232 acres) within the Cibola National Forest, but the map area is about 145 mi<sup>2</sup> and includes areas adjacent to the wilderness boundary.</p>\n<p>The Sandia Mountains are a part of an eastward-tilted fault block that is about 18 mi long and 8-10 mi wide and that is continuous with the Manzanita-Manzano Mountain fault blocks to the south of Tijeras Canyon (fig. 1). The westward-facing Sandia range front of Precambrian crystalline rocks is capped by about 2,500 ft of Pennsylvanian and Permian limestone, sandstone, and siltstone strata that dip 15&deg;-20&deg; eastward to form the dip slope of the tilted fault block.</p>\n<p>About 40-50 percent of the rocks exposed in the Sandia Mountains are of Precambrian age and include an older group of greenstone, metarhyolite, quartzite, and gneiss that is intruded by the Sandia Granite (1,445 m.y.). Paleozoic strata, about 2,500 ft thick, comprise about 30 percent of the outcrop area and form an extensive dip slope on the tilted fault block. Mesozoic strata commonly occupy synclinal basins such as that near Placitas in the Santo Domingo basin. Tertiary strata are represented by the early Tertiary Galisteo Formation and the poorly consolidated basin-f111 sediments of the Santa Fe Group.</p>\n<p>The dominant structural element is the east-tilted Sandia fault block, which is bounded on the west by the Pliocene and Miocene Sandia and Rincon-Ranchos range-front faults. These faults have as much as 20,000-28,000 ft of throw. Numerous north-trending faults along the dip slope are considered coeval with the range-front faults and have had an important influence on the localization of barite-fluorite veins. The northeast- and east-northeast-striking Placitas-San Francisco, Tijeras, and Gutierrez faults are principally of Laramide age but probably had numerous periods of movement.</p>\n<p>Regional gravity data (Suits and Cordell, 1981) indicate no significant mass distribution anomalies within the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1631D","usgsCitation":"Hedlund, D.C., and Cordell, L.E., 1985, Aeromagnetic map of the Sandia Mountain Wilderness, Bernalillo and Sandoval counties, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1631, Plate: 18.12 x 30.63 inches, https://doi.org/10.3133/mf1631D.","productDescription":"Plate: 18.12 x 30.63 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326354,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1631D.JPG"},{"id":327250,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1631-D/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"New Mexico","county":"Bernalillo County, Sandoval County","otherGeospatial":"Sandia Mountain Wilderness","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.5,35.1175 ], [ -106.5,35.333333333333336 ], [ -106.36749999999999,35.333333333333336 ], [ -106.36749999999999,35.1175 ], [ -106.5,35.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6912a4","contributors":{"authors":[{"text":"Hedlund, D. C.","contributorId":101624,"corporation":false,"usgs":true,"family":"Hedlund","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":262440,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cordell, L. E.","contributorId":69213,"corporation":false,"usgs":true,"family":"Cordell","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":262439,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48859,"text":"ofr84145B - 1985 - Streamflow statistics and drainage-basin characteristics for the Southwestern and Eastern Regions, Washington: Volume II. Eastern Washington","interactions":[],"lastModifiedDate":"2021-10-28T19:11:25.560714","indexId":"ofr84145B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-145","chapter":"B","title":"Streamflow statistics and drainage-basin characteristics for the Southwestern and Eastern Regions, Washington: Volume II. Eastern Washington","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84145B","usgsCitation":"Williams, J.R., and Pearson, H.E., 1985, Streamflow statistics and drainage-basin characteristics for the Southwestern and Eastern Regions, Washington: Volume II. Eastern Washington: U.S. Geological Survey Open-File Report 84-145, Report: 662 p.; 1 Plate: 32.03 × 36.42 inches, https://doi.org/10.3133/ofr84145B.","productDescription":"Report: 662 p.; 1 Plate: 32.03 × 36.42 inches","costCenters":[],"links":[{"id":391100,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13292.htm"},{"id":85683,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0145b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85682,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0145b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170006,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0145b/report-thumb.jpg"}],"country":"United States","state":"Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.493,\n              45.643\n            ],\n            [\n              -116.903,\n              45.643\n            ],\n            [\n              -116.903,\n              49\n            ],\n            [\n              -121.493,\n              49\n            ],\n            [\n              -121.493,\n              45.643\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d3b","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":238447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearson, Harold E.","contributorId":18046,"corporation":false,"usgs":true,"family":"Pearson","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":238446,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12041,"text":"ofr84774 - 1985 - Emission spectrographic and atomic absorption analyses of rock, mineral occurrence, prospect, and deposit samples from the Mount Hayes quadrangle, eastern Alaska Range, Alaska","interactions":[],"lastModifiedDate":"2023-08-23T20:50:02.029457","indexId":"ofr84774","displayToPublicDate":"1985-12-31T00:00:00","publicationYear":"1985","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":"84-774","title":"Emission spectrographic and atomic absorption analyses of rock, mineral occurrence, prospect, and deposit samples from the Mount Hayes quadrangle, eastern Alaska Range, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84774","usgsCitation":"Zehner, R.E., O’Leary, R.M., Day, G., Sutley, S.J., Nokleberg, W., and Koch, R.D., 1985, Emission spectrographic and atomic absorption analyses of rock, mineral occurrence, prospect, and deposit samples from the Mount Hayes quadrangle, eastern Alaska Range, Alaska: U.S. Geological Survey Open-File Report 84-774, Report: 139 p.; 1 Plate: 25.56 x 21.90 inches, https://doi.org/10.3133/ofr84774.","productDescription":"Report: 139 p.; 1 Plate: 25.56 x 21.90 inches","costCenters":[],"links":[{"id":420088,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13554.htm","linkFileType":{"id":5,"text":"html"}},{"id":143744,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0774/report-thumb.jpg"},{"id":40046,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0774/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40047,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0774/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Mount Hayes quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -147,\n              64\n            ],\n            [\n              -147,\n              63\n            ],\n            [\n              -144,\n              63\n            ],\n            [\n              -144,\n              64\n            ],\n            [\n              -147,\n              64\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db60574b","contributors":{"authors":[{"text":"Zehner, R. E.","contributorId":67933,"corporation":false,"usgs":true,"family":"Zehner","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":164795,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Leary, R. M.","contributorId":44894,"corporation":false,"usgs":true,"family":"O’Leary","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":164793,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":164794,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sutley, S. J.","contributorId":91484,"corporation":false,"usgs":true,"family":"Sutley","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":164797,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nokleberg, W. J. 0000-0002-1574-8869","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":68312,"corporation":false,"usgs":true,"family":"Nokleberg","given":"W. J.","affiliations":[],"preferred":false,"id":164796,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Koch, R. D.","contributorId":106487,"corporation":false,"usgs":true,"family":"Koch","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":164798,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":5222001,"text":"5222001 - 1985 - Environmental contaminants in eastern Cooper's hawk eggs","interactions":[],"lastModifiedDate":"2024-11-06T16:23:07.10629","indexId":"5222001","displayToPublicDate":"1985-10-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Environmental contaminants in eastern Cooper's hawk eggs","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.2307/3801392","usgsCitation":"Pattee, O.H., Fuller, M.R., and Kaiser, T.E., 1985, Environmental contaminants in eastern Cooper's hawk eggs: Journal of Wildlife Management, v. 49, no. 4, p. 1040-1044, https://doi.org/10.2307/3801392.","productDescription":"5 p.","startPage":"1040","endPage":"1044","costCenters":[{"id":531,"text":"Patuxent Wildlife 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 \"}}]}","volume":"49","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602428","contributors":{"authors":[{"text":"Pattee, Oliver H.","contributorId":45412,"corporation":false,"usgs":true,"family":"Pattee","given":"Oliver","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":335222,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fuller, Mark R. 0000-0001-7459-1729 mark_fuller@usgs.gov","orcid":"https://orcid.org/0000-0001-7459-1729","contributorId":2296,"corporation":false,"usgs":true,"family":"Fuller","given":"Mark","email":"mark_fuller@usgs.gov","middleInitial":"R.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":335223,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaiser, T. Earl","contributorId":84826,"corporation":false,"usgs":true,"family":"Kaiser","given":"T.","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":335224,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70113380,"text":"70113380 - 1985 - Comparison of fire fuel maps produced using MSS and AVHRR data","interactions":[],"lastModifiedDate":"2022-04-18T14:56:19.187034","indexId":"70113380","displayToPublicDate":"1985-08-20T15:02:46","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Comparison of fire fuel maps produced using MSS and AVHRR data","docAbstract":"<p>The fuel information, in support of the Bureau of Land Management's (BLM) national fire program, has been obtained through the manila interpretation of Landsat multi-spectral scanner images and digital image analysis of Advanced Very High Resolution Radiometer (AVHRR) data.  The BLM, in cooperation with the Earth Resources Observation Systems Data Center, determined that the accuracy (approximately 90 percent overall) was similar for deriving fire fuel information for Malheur County in eastern Oregon using either approach, and for an area the size of Malheur County (6.4 million acres), the costs were about the same (0.19 cents per acre).  But the cost per acre was substantially lower (0.04 cents) where digital analysis of AVHRR data were used to derive fire fuel information for a 42-million-acre area in eastern Oregon.  Based on these results, the BLM is using digital analysis of AVHRR data to support its operational fire fuel mapping program.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Pecora 10 Symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","publisherLocation":"Falls Church, VA","usgsCitation":"Miller, W.A., and Johnston, D.C., 1985, Comparison of fire fuel maps produced using MSS and AVHRR data, <i>in</i> Pecora 10 Symposium, p. 305-314.","productDescription":"10 p.","startPage":"305","endPage":"314","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288935,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","county":"Malheur County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.2336,41.997 ], [ -118.2336,44.4445 ], [ -116.8941,44.4445 ], [ -116.8941,41.997 ], [ -118.2336,41.997 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7658e4b0abf75cf2bf3a","contributors":{"authors":[{"text":"Miller, Wayne A. wamiller@usgs.gov","contributorId":1123,"corporation":false,"usgs":true,"family":"Miller","given":"Wayne","email":"wamiller@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":495083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnston, David C.","contributorId":98636,"corporation":false,"usgs":true,"family":"Johnston","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":495084,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221986,"text":"5221986 - 1985 - Organochlorine concentrations, whole body weights, and lipid content of black skimmers wintering in Mexico and in south Texas, 1983","interactions":[],"lastModifiedDate":"2020-02-19T10:43:16","indexId":"5221986","displayToPublicDate":"1985-06-16T12:18:59","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1103,"text":"Bulletin of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Organochlorine concentrations, whole body weights, and lipid content of black skimmers wintering in Mexico and in south Texas, 1983","docAbstract":"<p>Since 1978, a large proportion of the black skimmers (Rynchops niger) nesting along the Texas coast have had high concentrations of DDE in their eggs. Of 284 eggs collected from 5 sites during 1978-81, 99.5% contained detectable (&gt; 0.i0 ppm) w levels of DDE, ranging up to 86 ppm wet-weight; 36% of the eggs contained &gt; i0 ppm DDE (White et al., 1984). During the 4-year period, geometric mean concentrations of DDE remained strikingly similar, with no significant decline in egg contaminant levels. The sources of DDE contamination in skimmers are unknown. Recoveries of juvenile skimmers banded in Texas, Louisiana, and Mississippi indicate that a large proportion of the birds (60%) spend the winter on the east and west coasts of Mexico. Therefore, it is possible that the DDE exposure to Texas skimmers occurs in Mexico during the winter, although some birds remain along the Gulf Coast year-round.\\</p><p> This study was conducted to determine the degree of DDE and other organochlorine contamination in black skimmers and their food items from sites in Mexico and Texas, and to statistically compare residue concentrations and body condition in individuals from the 2 areas. </p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Environmental Contamination and Toxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","doi":"10.1007/BF01609769","usgsCitation":"White, D.H., Mitchell, C.A., and Stafford, C.J., 1985, Organochlorine concentrations, whole body weights, and lipid content of black skimmers wintering in Mexico and in south Texas, 1983: Bulletin of Environmental Contamination and Toxicology, v. 34, no. 4, p. 513-517, https://doi.org/10.1007/BF01609769.","productDescription":"5 p.","startPage":"513","endPage":"517","numberOfPages":"5","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197594,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":17680,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.springerlink.com/content/l08u2454r31p0770/","linkFileType":{"id":5,"text":"html"}}],"country":"Mexico, United States","state":"Texas, Veracruz","otherGeospatial":"Chachalacas, Veracruz, Port Mansfield, Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.47962951660156,\n              26.512976738763484\n            ],\n            [\n              -97.3828125,\n              26.512976738763484\n            ],\n            [\n              -97.3828125,\n              26.65175460663639\n            ],\n            [\n              -97.47962951660156,\n              26.65175460663639\n            ],\n            [\n              -97.47962951660156,\n              26.512976738763484\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.3387680053711,\n              19.389615012409525\n            ],\n            [\n              -96.3057231903076,\n              19.389615012409525\n            ],\n            [\n              -96.3057231903076,\n              19.444255598188818\n            ],\n            [\n              -96.3387680053711,\n              19.444255598188818\n            ],\n            [\n              -96.3387680053711,\n              19.389615012409525\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68aa0c","contributors":{"authors":[{"text":"White, Donald H.","contributorId":97868,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":335199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mitchell, C. A.","contributorId":54543,"corporation":false,"usgs":true,"family":"Mitchell","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":335197,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stafford, C. J.","contributorId":65429,"corporation":false,"usgs":true,"family":"Stafford","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":335198,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70210572,"text":"70210572 - 1985 - Origin and tectonic evolution of the Maclaren and Wrangellia terranes, eastern Alaska Range, Alaska","interactions":[],"lastModifiedDate":"2020-06-09T19:50:48.233035","indexId":"70210572","displayToPublicDate":"1985-06-09T14:41:27","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Origin and tectonic evolution of the Maclaren and Wrangellia terranes, eastern Alaska Range, Alaska","docAbstract":"<p>Major portions of the eastern Alaska Range, south of the Denali fault, in the McCarthy, Nabesna, Mount Hayes, and eastern Healy quadrangles, consist predominantly of the Maclaren and Wrangellia tectono-stratigraphic terranes. The Maclaren terrane consists of the Maclaren Glacier metamorphic belt and the regionally deformed and metamorphosed East Susitna batholith. The Maclaren Glacier metamorphic belt is composed of argillite, metagraywacke, and sparse andesite flows that are progressively regionally metamorphosed from lower greenschist facies to middle amphibolite facies near the East Susitna batholith. The East Susitna batholith is composed of gabbro, quartz diorite, granodiorite, and sparse quartz monzonite. Isotopic ages are as old as a K-Ar hornblende age of 87.5 m.y., possibly reset, and a U-Pb zircon age of 70 m.y. The batholith is intensely deformed and regionally metamorphosed under conditions of the middle amphibolite facies.</p><p>The Wrangellia terrane is divided into two subterranes: (1) the Slana River subterrane, composed of late Paleozoic andesite to dacite flows, tuff, limestone, and argillite, unconformably overlying massive basalt flows of the Triassic Nikolai Greenstone, Late Triassic limestone, and younger Mesozoic flysch; and (2) the Tangle subterrane, a deeper-water equivalent of the Slana River subterrane, composed of late Paleozoic and Early Triassic aquagene tuff, chert, minor andesite tuff and flows, limestone, unconformably overlying pillow basalt and massive basalt flows of the Triassic Nikolai Greenstone, and Late Triassic limestone. Both subterranes are intruded by locally extensive gabbro and diabase dikes and by cumulate mafic and ultramafic sills.</p><p>Less extensive terranes (two) are the Clearwater terrane, a sequence of intensely deformed chlorite schist, muscovite schist, marble, and greenstone of Late Triassic age; and an unnamed terrane of ultramafic and associated rocks of presumable Paleozoic or Mesozoic age. Each terrane or subterrane generally has (1) a distinctive time-stratigraphic sequence reflecting a unique geologic history; (2) a missing provenance for bedded sedimentary or volcanic rocks; and (3) bounding thrust or strike-slip faults, interpreted as accretionary sutures.</p><p>The Maclaren and Wrangellia terranes are juxtaposed along the Broxson Gulch thrust, which consists of an imbricate series of north-dipping thrust faults. Paralleling the Broxson Gulch thrust, a few kilometres to the south, is the north-dipping Eureka Creek thrust, along which are juxtaposed the Slana River and Tangle subterranes. The Maclaren terrane is correlated with the Kluane Schist and the Ruby Range batholith in the southern Yukon Territory, which represent the northward extension of the Taku and Tracy Arm terranes. If correct, this correlation defines a minimum displacement of the Maclaren terrane along the Denali fault of ∼400 km.</p><p>The Maclaren terrane is interpreted to have formed in a synorogenic Andean-type arc setting on the west margin of Mesozoic North America in the middle to late Mesozoic and early Cenozoic. The Wrangellia terrane is interpreted to have initially formed in an island-arc setting during the late Paleozoic. Subsequently in the Late Triassic, the Wrangellia terrane underwent rifting near the paleoequator, with formation of the Nikolai Greenstone and associated mafic and ultra-mafic igneous rocks. In the middle and late Mesozoic, Wrangellia migrated toward, and was accreted during, the middle Cretaceous to the Maclaren terrane along the Broxson Gulch thrust. Subsequent dispersion of both the Maclaren and Wrangellia terranes along the Denali fault and the Broxson Gulch thrust commenced during the early Tertiary and continues through the present.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1985)96<1251:OATEOT>2.0.CO;2","usgsCitation":"Nokleberg, W.J., Jones, D.L., and Silberling, N.J., 1985, Origin and tectonic evolution of the Maclaren and Wrangellia terranes, eastern Alaska Range, Alaska: GSA Bulletin, v. 96, no. 10, p. 1251-1270, https://doi.org/10.1130/0016-7606(1985)96<1251:OATEOT>2.0.CO;2.","productDescription":"20 p.","startPage":"1251","endPage":"1270","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":375479,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Maclaren and Wrangellia terranes","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -151.962890625,\n              61.227957176677876\n            ],\n            [\n              -141.064453125,\n              61.227957176677876\n            ],\n            [\n              -141.064453125,\n              64.1297836764257\n            ],\n            [\n              -151.962890625,\n              64.1297836764257\n            ],\n            [\n              -151.962890625,\n              61.227957176677876\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"96","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Nokleberg, Warren J. 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":2077,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":790640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, D. L.","contributorId":65045,"corporation":false,"usgs":true,"family":"Jones","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":790641,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Silberling, Norman J.","contributorId":102438,"corporation":false,"usgs":true,"family":"Silberling","given":"Norman","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":790642,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70210571,"text":"70210571 - 1985 - Geologic setting, petrology, and geochemistry of stratiform sphalerite-galena-barite deposits, Red Dog Creek and Drenchwater Creek areas, northwestern Brooks Range, Alaska","interactions":[],"lastModifiedDate":"2020-06-11T15:17:53.269547","indexId":"70210571","displayToPublicDate":"1985-06-09T14:31:59","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Geologic setting, petrology, and geochemistry of stratiform sphalerite-galena-barite deposits, Red Dog Creek and Drenchwater Creek areas, northwestern Brooks Range, Alaska","docAbstract":"<p><span>Similar stratiform sphalerite-galena-barite deposits occur in the Red Dog Creek area, De Long Mountains quadrangle, and in the Drenchwater Creek area, Howard Pass quadrangle, northwestern Brooks Range, Alaska. The deposits, located approximately 180 km apart, are hosted by Mississippian and Pennsylvanian strata of the Kagvik structural sequence of late Paleozoic and early Mesozoic age. This sequence is situated in the lowermost structural plate of a series of predominantly east-striking, shallow-dipping thrust plates that characterize the regional structure. The deposits occur in shale, tuff, tuffaceous sandstone, altered chert, and quartz exhalite. These units are in places interlayered with or adjacent to bedded or nodular barite or submarine keratophyre flows. Chert and shale commonly contain abundant highly altered, fine-grained feldspar, pumice lapilli, and mafic volcanic rock fragments.The main types of occurrences at Red Dog Creek are: (1) disseminated and stratiform sulfides thinly bedded in organic-rich Mississippian and Pennsylvanian shale and chert, (2) massive sulfide veins and breccia fillings in silicified Mississippian and Pennsylvanian shale, and (3) stratiform sulfide-bearing lenses subdivided into (3a) quartz-exhalite with up to several percent sulfides and barite, (3b) massive sulfide-quartz lenses with up to several percent barite, and (3c) barite-quartz lenses with up to several percent sulfides.At Drenchwater Creek sulfides and barite occur as: (1) disseminations in shale, chert, tuff, and tuffaceous sandstone; (2) disseminations to aggregates in quartz exhalite; and (3) occurrences in veins crosscutting cleavages in brecciated chert and shale.The stratiform sulfides occur in zones up to several thousand meters long and several tens of meters thick. Preliminary grades at Red Dog Creek are 17.1 percent zinc, 5.0 percent lead, and 2.4 oz silver per ton contained in at least 85 million tons.The range of sulfide sulfur isotope values at Red Dog Creek is -16.6 per mil to +3.6 per mil. Sphalerite averages 0.8 per mil. Pyrite is isotopically lighter than coexisting sphalerite in quartz exhalite and massive sulfide lenses. This isotopic relationship is compatible with paragenetic relationships which show pyrite crystallized both earlier and later than other sulfides. Galena is isotopically lighter than coexisting sphalerite. Three groups of geologically and isotopically distinct barites exist including isotopic values appropriate for derivation from late Paleozoic seawater sulfate.Early in the depositional sequence isotopically light pyrite formed from organically reduced seawater sulfate. Sphalerite, galena, late pyrite, and some barite precipitated from two sulfur-bearing solutions that mixed at the mineralization site. Isotopically light barite associated with sulfides precipitated from oxidized H&nbsp;</span><sub>2</sub><span>&nbsp;S without seawater sulfate contribution. Lead isotope data from Red Dog and Drenchwater Creeks are compatible with generation of lead in a Phanerozoic mature island-arc setting, a typical orogene, or possibly a back-arc type intracratonic basin.The stratiform sphalerite-galena-barite deposits probably formed in an incipient island-arc environment near a continental margin, containing magmas of keratophyric and andesitic composition, where metal-laden hydrothermal fluids discharged into a deep (?) water, low-energy environment. Later intense deformation, associated with plate docking and thrusting, disrupted and partly remobilized and stratiform deposits.</span></p>","language":"English","publisher":"SPEM","doi":"10.2113/gsecongeo.80.7.1896","usgsCitation":"Lange, I.M., Nokleberg, W.J., Plahuta, J., Krouse, H., and Doe, B.R., 1985, Geologic setting, petrology, and geochemistry of stratiform sphalerite-galena-barite deposits, Red Dog Creek and Drenchwater Creek areas, northwestern Brooks Range, Alaska: Economic Geology, v. 80, no. 7, p. 1896-1926, https://doi.org/10.2113/gsecongeo.80.7.1896.","productDescription":"31p.","startPage":"1896","endPage":"1926","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":375478,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Northwestern Brooks Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -157.8955078125,\n              66.38155976071747\n            ],\n            [\n              -149.7216796875,\n              66.38155976071747\n            ],\n            [\n              -149.7216796875,\n              68.87143872335129\n            ],\n            [\n              -157.8955078125,\n              68.87143872335129\n            ],\n            [\n              -157.8955078125,\n              66.38155976071747\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"80","issue":"7","noUsgsAuthors":false,"publicationDate":"1985-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Lange, Ian M.","contributorId":149316,"corporation":false,"usgs":false,"family":"Lange","given":"Ian","email":"","middleInitial":"M.","affiliations":[{"id":5097,"text":"University of Montana, Division of Biological Sciences","active":true,"usgs":false}],"preferred":false,"id":790635,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nokleberg, Warren J. 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":2077,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":790636,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plahuta, J.T.","contributorId":225176,"corporation":false,"usgs":false,"family":"Plahuta","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":790637,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Krouse, H.R.","contributorId":63067,"corporation":false,"usgs":true,"family":"Krouse","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":790638,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Doe, B. 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,{"id":5222030,"text":"5222030 - 1985 - An aerial photographic census of Chesapeake Bay and North Carolina canvasbacks","interactions":[],"lastModifiedDate":"2024-11-06T16:52:48.957349","indexId":"5222030","displayToPublicDate":"1985-04-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"An aerial photographic census of Chesapeake Bay and North Carolina canvasbacks","docAbstract":"<p>We used conventional 35-mm photography to conduct an aerial photographic census of canvasbacks (<i>Aythya valisineria</i>) throughout Chesapeake Bay (tidal Maryland and Virginia) and coastal North Carolina, 26-30 January 1981. Flock size and sex ratio characteristics were determined from examination of color transparencies of 165 canvasback flocks totaling over 95,000 birds. A sex ratio of 2.91 males/female was determined from 68,769 birds, 80% of the birds in 150 flocks. Sex ratio for the Atlantic Flyway was projected as 2.90 males/female. We recorded the greatest number of canvasbacks and the widest range of flock size in Maryland waters; the fewest canvasbacks and the smallest average flock size in Virginia; and the fewest but on average the largest flocks of canvasbacks in North Carolina. Sex ratio varied latitudinally in the flyway with a tendency for males to occupy more northern and females more southern latitudes in winter. Sex ratio (males/female) was highest in Maryland (3.98), slightly lower in Virginia (3.71), and lowest in North Carolina (1.70). Locally, sex ratio varied with flock size. In Chesapeake Bay, small flocks (&lt;100 birds) had lower sex ratio (P &lt; 0.05) than medium (100-1,000) or large (&gt;1,000) flocks. By providing large- sample sex ratio information, as well as exact counts of birds, we conclude that low-level 35-mm aerial photography is the most efficient and accurate means of determining canvasback population status in eastern coastal habitats.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3801550","usgsCitation":"Haramis, G., Goldsberry, J., McAuley, D., and Derleth, E., 1985, An aerial photographic census of Chesapeake Bay and North Carolina canvasbacks: Journal of Wildlife Management, v. 49, no. 2, p. 449-454, https://doi.org/10.2307/3801550.","productDescription":"6 p.","startPage":"449","endPage":"454","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487094,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3801550","text":"Publisher Index 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 \"}}]}","volume":"49","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db686049","contributors":{"authors":[{"text":"Haramis, G.M.","contributorId":101212,"corporation":false,"usgs":true,"family":"Haramis","given":"G.M.","email":"","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":335318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldsberry, J.R.","contributorId":33013,"corporation":false,"usgs":true,"family":"Goldsberry","given":"J.R.","affiliations":[],"preferred":false,"id":335317,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McAuley, D.G. 0000-0003-3674-6392","orcid":"https://orcid.org/0000-0003-3674-6392","contributorId":15296,"corporation":false,"usgs":true,"family":"McAuley","given":"D.G.","affiliations":[],"preferred":false,"id":335315,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Derleth, E.L.","contributorId":31483,"corporation":false,"usgs":true,"family":"Derleth","given":"E.L.","affiliations":[],"preferred":false,"id":335316,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5222023,"text":"5222023 - 1985 - Recent Red-shouldered Hawk range expansion north into Oregon including first specimen record","interactions":[],"lastModifiedDate":"2024-10-09T16:00:10.979016","indexId":"5222023","displayToPublicDate":"1985-04-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2793,"text":"Murrelet","active":true,"publicationSubtype":{"id":10}},"title":"Recent Red-shouldered Hawk range expansion north into Oregon including first specimen record","docAbstract":"<p> In this paper we review 46 Red-shouldered Hawk (<i>Buteo lineatus</i>) observation records from Oregon between 1971 and 1983. The literature contained only two records prior to 1971: Johnson's (1880) record without a specific date or locality from the Willamette Valley of western Oregon, and Bendire's (1892) two nests located in 1878 near Camp Harney in eastern Oregon. Gabrielson and Jewett (1940) placed the species on the Oregon hypothetical list because they doubted the validity of the previous identifications. However, Browning (1973) measured the eggs collected by Bendire, reviewed his field notes, and concluded that there was ample evidence the species had occurred in Oregon despite the absence of records for nearly 100 years.</p>","language":"English","publisher":"Society for Northwestern Vertebrate Biology","doi":"10.2307/3535467","usgsCitation":"Henny, C.J., and Cornely, J.E., 1985, Recent Red-shouldered Hawk range expansion north into Oregon including first specimen record: Murrelet, v. 66, no. 1, p. 29-31, https://doi.org/10.2307/3535467.","productDescription":"3 p.","startPage":"29","endPage":"31","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":18558,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.jstor.org/stable/3535467","linkFileType":{"id":5,"text":"html"}},{"id":196781,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70009928,"text":"70009928 - 1985 - Global geologic mapping of Mars: The western equatorial region","interactions":[],"lastModifiedDate":"2013-02-20T20:50:01","indexId":"70009928","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":661,"text":"Advances in Space Research","active":true,"publicationSubtype":{"id":10}},"title":"Global geologic mapping of Mars: The western equatorial region","docAbstract":"Global geologic mapping of Mars was originally accomplished following acquisition of orbital spacecraft images from the Mariner 9 mission. The mapping program represented a joint enterprise by the U.S. Geological Survey and other planetary scientists from universities in the United States and Europe. Many of the Mariner photographs had low resolution or poor albedo contrast caused by atmospheric haze and high-sun angles. Some of the early geologic maps reflect these deficiencies in their poor discrimination and subdivision of rock units. New geologic maps made from higher resolution and better quality Viking images also represent a cooperative effort, by geologists from the U.S. Geological Survey, Arizona State University, and the University of London. This second series of global maps consists of three parts: 1) western equatorial region, 2) eastern equatorial region, and 3) north and south polar regions. These maps, at 1:15 million scale, show more than 60 individual rock-stratigraphic units assigned to three Martian time-stratigraphic systems. The first completed map of the series covers the western equatorial region of Mars. Accompanying the map is a description of the sequence and distribution of major tectonic, volcanic, and fluvial episodes as recorded in the stratigraphic record. ?? 1985.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Advances in Space Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0273-1177(85)90243-1","issn":"02731177","usgsCitation":"Scott, D.H., 1985, Global geologic mapping of Mars: The western equatorial region: Advances in Space Research, v. 5, no. 8, p. 71-82, https://doi.org/10.1016/0273-1177(85)90243-1.","startPage":"71","endPage":"82","numberOfPages":"12","costCenters":[],"links":[{"id":218923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267876,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0273-1177(85)90243-1"}],"volume":"5","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2948e4b0c8380cd5a80c","contributors":{"authors":[{"text":"Scott, D. H.","contributorId":73565,"corporation":false,"usgs":true,"family":"Scott","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":357477,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013365,"text":"70013365 - 1985 - 40Ar/39Ar and K-Ar data bearing on the metamorphic and tectonic history of western New England","interactions":[],"lastModifiedDate":"2023-12-28T13:24:02.293607","indexId":"70013365","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"40Ar/39Ar and K-Ar data bearing on the metamorphic and tectonic history of western New England","docAbstract":"<p><sup>40</sup>Ar/<sup>39</sup>Ar ages of coexisting biotite and hornblende from Proterozoic Y gneisses of the Berkshire and Green Mountain massifs, as well as<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar and K-Ar mineral and whole-rock ages from Paleozoic metamorphic rocks, suggest that the thermal peak for the dominant metamorphic recrystallization in western New England occurred 465 ± 5 m.y. ago (Taconian). Although textural data indicate a complex metamorphic-tectonic history for Paleozoic rocks, no evidence in rocks at least as high as kyanite grade dictates an Acadian age for the Barrovian metamorphism. Available<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar and K-Ar data suggest that the low-grade metamorphism and cleavage formation in Taconic allochthons and the higher-grade metamorphism and emplacement of the Berkshire massif allochthon are Taconian.</p><p><sup>40</sup>Ar/<sup>39</sup>Ar age data from a poorly defined terrane beginning near the east margin of the Green Mountain massif and extending along the eastern one-third of the Berkshire massif as far south as Otis, Massachusetts, suggest that the area has been retrograded during a metamorphism that peaked at least 376 ± 5 m.y. ago (Acadian).</p><p>Available age and petrologic data from western New England indicate the presence of at least three separate metamorphic-structural domains of Taconian age: (1) a small area of relict high-pressure and low-temperature metamorphism in northern Vermont (T-1 domain), (2) a broad area in Vermont and eastern New York of normal Barrovian metamorphism from chlorite to garnet grade and characterized by a gentle metamorphic gradient (T-2 domain), and (3) a rather narrow belt of steep-gradient, Barrovian series metamorphic rocks extending from near the Cortlandt Complex northeastward through Dutchess County, New York, to the Berkshire massif in western Massachusetts (T-3 domain). Areas of maximum metamorphic intensity within the T-3 domain coincide with areas of maximum crustal thickening resulting from imbricate thrusting (Berkshire massif) or from recumbent folding (Manhattan Prong) of remobilized North American continental crust in the later stages of the Taconic orogeny.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1985)96<123:AAKDBO>2.0.CO;2","usgsCitation":"Sutter, J.F., Ratcliffe, N.M., and Mukasa, S., 1985, 40Ar/39Ar and K-Ar data bearing on the metamorphic and tectonic history of western New England: Geological Society of America Bulletin, v. 96, no. 1, p. 123-136, https://doi.org/10.1130/0016-7606(1985)96<123:AAKDBO>2.0.CO;2.","productDescription":"14 p.","startPage":"123","endPage":"136","numberOfPages":"14","costCenters":[],"links":[{"id":220304,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.71683860031261,\n              43.14936147487742\n            ],\n            [\n              -73.71683860031261,\n              41.42652808796893\n            ],\n            [\n              -72.88187766281217,\n              41.42652808796893\n            ],\n            [\n              -72.88187766281217,\n              43.14936147487742\n            ],\n            [\n              -73.71683860031261,\n              43.14936147487742\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"96","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e264e4b0c8380cd45b3a","contributors":{"authors":[{"text":"Sutter, J. F.","contributorId":59779,"corporation":false,"usgs":true,"family":"Sutter","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":365907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ratcliffe, N. M.","contributorId":80691,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"N.","middleInitial":"M.","affiliations":[],"preferred":false,"id":365908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mukasa, S.B.","contributorId":89568,"corporation":false,"usgs":true,"family":"Mukasa","given":"S.B.","email":"","affiliations":[],"preferred":false,"id":365909,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":16562,"text":"ofr84145A - 1985 - Streamflow statistics and drainage-basin characteristics for the southwestern and eastern regions, Washington: Volume I. Southwestern Washington","interactions":[],"lastModifiedDate":"2023-11-27T20:58:06.945985","indexId":"ofr84145A","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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":"84-145","chapter":"A","title":"Streamflow statistics and drainage-basin characteristics for the southwestern and eastern regions, Washington: Volume I. Southwestern Washington","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84145A","usgsCitation":"Williams, J.R., and Pearson, H.E., 1985, Streamflow statistics and drainage-basin characteristics for the southwestern and eastern regions, Washington: Volume I. Southwestern Washington: U.S. Geological Survey Open-File Report 84-145, Report: iii, 424 p.; 26.52 x 35.91 inches, https://doi.org/10.3133/ofr84145A.","productDescription":"Report: iii, 424 p.; 26.52 x 35.91 inches","costCenters":[],"links":[{"id":422980,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13291.htm","linkFileType":{"id":5,"text":"html"}},{"id":45554,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0145a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149750,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0145a/report-thumb.jpg"},{"id":45555,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0145a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -123.03705855355781,\n              46.774202263516884\n            ],\n            [\n              -123.5782106152086,\n              47.30518349691528\n            ],\n            [\n              -123.68822513785824,\n              47.628171560775456\n            ],\n            [\n              -124.33385568765746,\n              48.083836939231304\n            ],\n            [\n              -124.7276057487826,\n              48.35430242614737\n            ],\n            [\n              -124.88498659891658,\n              47.92306035281257\n            ],\n            [\n              -124.5333696302558,\n              47.461391797419\n            ],\n            [\n              -124.2895212396597,\n              46.97997528940809\n            ],\n            [\n              -124.0659132725674,\n              46.300094884791406\n            ],\n            [\n              -123.53295368644481,\n              46.23954551851912\n            ],\n            [\n              -123.31979382077077,\n              46.15021551425289\n            ],\n            [\n              -123.15538395788386,\n              46.17329159005263\n            ],\n            [\n              -122.7904450153109,\n              46.03945192780412\n            ],\n            [\n              -122.71565663774024,\n              45.605413714316995\n            ],\n            [\n              -122.3869618215725,\n              45.545950312640656\n            ],\n            [\n              -121.6733248794553,\n              45.70866420289531\n            ],\n            [\n              -121.6051531956781,\n              46.72146991229192\n            ],\n            [\n              -122.3094933178835,\n              46.68352499136691\n            ],\n            [\n              -123.03705855355781,\n              46.774202263516884\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d3a","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":173062,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearson, Harold E.","contributorId":18046,"corporation":false,"usgs":true,"family":"Pearson","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":173061,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013093,"text":"70013093 - 1985 - Interannual streamflow variability in the United States based on principal components","interactions":[],"lastModifiedDate":"2018-02-12T18:02:29","indexId":"70013093","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Interannual streamflow variability in the United States based on principal components","docAbstract":"<p><span>Interannual modes of streamflow variation at 106 locations across the United States during the period 1931–1978 are defined by using principal components. Five statistically significant components are found to account for more than 56% of the total streamflow variance. The first principal component represents a nationwide tendency for either above- or below-mean streamflow. The second component represents a north-south opposition in departures from mean flow, and the third, an east-west opposition. Higher-order components (fourth and fifth) geographically depict regional patterns of opposition in the sign of streamflow departures between coastal-continental areas and between the northern and southern plains, respectively. Analyses using spatially and temporally modified data sets indicate that the first three components (which explain 45% of the variance) are quite stable spatially, while only the first component is stable temporally. Time series analysis of principal component scores indicates that all but the fourth component are first-order autoregressive processes, as is mean annual nationwide streamflow. The fourth component is an autoregressive (AR)(2) process. In general, the principal components of streamflow are found to exhibit more persistence over annual time scales than the mean annual flow data themselves.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i005p00691","usgsCitation":"Lins, H.F., 1985, Interannual streamflow variability in the United States based on principal components: Water Resources Research, v. 21, no. 5, p. 691-701, https://doi.org/10.1029/WR021i005p00691.","productDescription":"11 p.","startPage":"691","endPage":"701","costCenters":[],"links":[{"id":219777,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"21","issue":"5","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"505a3ce6e4b0c8380cd63139","contributors":{"authors":[{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":365266,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013055,"text":"70013055 - 1985 - Character and regional significance of Great Falls tectonic zone, east-central Idaho and west-central Montana","interactions":[],"lastModifiedDate":"2023-01-12T17:01:30.219496","indexId":"70013055","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Character and regional significance of Great Falls tectonic zone, east-central Idaho and west-central Montana","docAbstract":"<p><span>The Great Falls tectonic zone, here named, is a belt of diverse northeast-trending geologic features that can be traced from the Idaho batholith in the Cordilleran miogeocline, across thrust-belt structures and basement rocks of west-central and southwestern Montana, through cratonic rocks of central Montana, and into southwesternmost Saskatchewan, Canada. Geologic mapping in east-central Idaho and west-central Montana has outlined a continuous zone of high-angle faults and shear zones. These structures (1) extend more than 150 km (93 mi) northeastward from near Salmon, Idaho, toward Anaconda, Montana, (2) had recurrent movement from middle Proterozoic to Holocene time, (3) controlled the intrusion and orientation of Late Cretaceous to early Tertiary dike swarms, and (4) ontrolled the uplift and orientation of the Anaconda-Pintlar Range. Recurrent fault movement in this zone and strong structural control over igneous intrusion suggest a fundamental tectonic feature that has influenced the tectonic development of the Idaho-Montana area from at least middle Proterozoic time to the present.</span></p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/AD462506-16F7-11D7-8645000102C1865D","usgsCitation":"O’Neill, J.M., and Lopez, D.A., 1985, Character and regional significance of Great Falls tectonic zone, east-central Idaho and west-central Montana: American Association of Petroleum Geologists Bulletin, v. 69, no. 3, p. 437-447, https://doi.org/10.1306/AD462506-16F7-11D7-8645000102C1865D.","productDescription":"11 p.","startPage":"437","endPage":"447","numberOfPages":"11","costCenters":[],"links":[{"id":220229,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho, Montana","otherGeospatial":"Great Falls tectonic zone","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.94970703125,\n              44.62175409623324\n            ],\n            [\n              -111.20361328125,\n              44.62175409623324\n            ],\n            [\n              -111.20361328125,\n              46.76996843356982\n            ],\n            [\n              -115.94970703125,\n              46.76996843356982\n            ],\n            [\n              -115.94970703125,\n              44.62175409623324\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"69","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f2cae4b0c8380cd4b38e","contributors":{"authors":[{"text":"O’Neill, J. Michael jmoneill@usgs.gov","contributorId":99522,"corporation":false,"usgs":true,"family":"O’Neill","given":"J.","email":"jmoneill@usgs.gov","middleInitial":"Michael","affiliations":[],"preferred":false,"id":365185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lopez, David A.","contributorId":79445,"corporation":false,"usgs":true,"family":"Lopez","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":365184,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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