{"pageNumber":"4844","pageRowStart":"121075","pageSize":"25","recordCount":184582,"records":[{"id":26148,"text":"wri864204 - 1986 - Capacity of the diversion channel below the flood-control dam on the Big Lost River at the Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2023-01-12T21:15:58.985273","indexId":"wri864204","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4204","title":"Capacity of the diversion channel below the flood-control dam on the Big Lost River at the Idaho National Engineering Laboratory, Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864204","usgsCitation":"Bennett, C.M., 1986, Capacity of the diversion channel below the flood-control dam on the Big Lost River at the Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 86-4204, iv, 25 p., https://doi.org/10.3133/wri864204.","productDescription":"iv, 25 p.","costCenters":[],"links":[{"id":411807,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36625.htm","linkFileType":{"id":5,"text":"html"}},{"id":121979,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4204/report-thumb.jpg"},{"id":54942,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4204/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Big Lost River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113,\n              43.525\n            ],\n            [\n              -113,\n              43.417\n            ],\n            [\n              -113.111,\n              43.417\n            ],\n            [\n              -113.111,\n              43.525\n            ],\n            [\n              -113,\n              43.525\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f6917","contributors":{"authors":[{"text":"Bennett, C. M.","contributorId":15648,"corporation":false,"usgs":true,"family":"Bennett","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":195902,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3507,"text":"cir977 - 1986 - Principles of logic and the use of digital geographic information systems","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"cir977","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"977","title":"Principles of logic and the use of digital geographic information systems","docAbstract":"Digital geographic information systems allow many different types of data to be spatially and statistically analyzed. Logical operations can be performed on individual or multiple data planes by algorithms that can be implemented in computer systems. Users and creators of the systems should fully understand these operations. This paper describes the relationships of layers and features in geographic data bases and the principles of logic that can be applied by geographic information systems and suggests that a thorough knowledge of the data that are entered into a geographic data base and of the logical operations will produce results that are most satisfactory to the user. Methods of spatial analysis are reduced to their primitive logical operations and explained to further such understanding.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir977","usgsCitation":"Robinove, C.J., 1986, Principles of logic and the use of digital geographic information systems: U.S. Geological Survey Circular 977, iii, 19 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir977.","productDescription":"iii, 19 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":122960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1986/0977/report-thumb.jpg"},{"id":21962,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1986/0977/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db66103d","contributors":{"authors":[{"text":"Robinove, Charles Joseph","contributorId":71153,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":147056,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27245,"text":"wri864153 - 1986 - Hydrogeology, ground-water flow, and tritium movement at low-level radioactive-waste disposal site near Sheffield, Illinois","interactions":[],"lastModifiedDate":"2023-01-05T21:29:02.151914","indexId":"wri864153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4153","title":"Hydrogeology, ground-water flow, and tritium movement at low-level radioactive-waste disposal site near Sheffield, Illinois","docAbstract":"<p>Groundwater flow and tritium movement are described at and near a low-level radioactive waste disposal site near Sheffield, Illinois. Flow in the shallow aquifer is confined to three basins that ultimately drain into a stripmine lake. Most of the flow from the site is through a buried, pebbly sandfilled channel. Remaining flow is toward alluvium of an existing stream. Conceptual flow models for the two largest basins are used to improve definition of flow velocity and direction. Flow velocities range from about 25 to 2,500 ft/yr. Tritium was found in all three basins. The most extensive migration of tritium is coincident with buried channel. Tritium concentrations ranged from detection level to more than 300 nanocuries/L.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864153","usgsCitation":"Garklavs, G., and Healy, R.W., 1986, Hydrogeology, ground-water flow, and tritium movement at low-level radioactive-waste disposal site near Sheffield, Illinois: U.S. Geological Survey Water-Resources Investigations Report 86-4153, v, 35 p., https://doi.org/10.3133/wri864153.","productDescription":"v, 35 p.","costCenters":[],"links":[{"id":411452,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36580.htm","linkFileType":{"id":5,"text":"html"}},{"id":56108,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4153/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158749,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4153/report-thumb.jpg"}],"country":"United States","state":"Illinios","city":"Sheffield","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.796,\n              41.343\n            ],\n            [\n              -89.796,\n              41.3360\n            ],\n            [\n              -89.782,\n              41.3360\n            ],\n            [\n              -89.782,\n              41.343\n            ],\n            [\n              -89.796,\n              41.343\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614875","contributors":{"authors":[{"text":"Garklavs, George","contributorId":87139,"corporation":false,"usgs":true,"family":"Garklavs","given":"George","email":"","affiliations":[],"preferred":false,"id":197789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, R. W.","contributorId":89872,"corporation":false,"usgs":true,"family":"Healy","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":197790,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25887,"text":"wri844119 - 1986 - Geohydrology and potential for artificial recharge in the western part of the U.S. Marine Corps Base, Twentynine Palms, California, 1982-83","interactions":[],"lastModifiedDate":"2018-02-14T17:30:40","indexId":"wri844119","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"84-4119","title":"Geohydrology and potential for artificial recharge in the western part of the U.S. Marine Corps Base, Twentynine Palms, California, 1982-83","docAbstract":"<p>A recent gravity survey indicates that sedimentary deposits in the Deadman Lake area of the Twentynine Palms Marine Corps Base, California, are as much as 10,500 feet thick. These deposits fill an ancient valley in the bedrock complex. This valley is alined east-west in the Surprise Spring area and north-south in the Deadman Lake area.</p><p>Water levels in the Ames Dry Lake area of the Surprise Spring subbasin have changed little between earliest measurements in 1952-53 and in 1982. Water levels in three Marine Corps Base supply wells in the same subbasin near Surprise Spring declined an average of 78 feet during the past 30 years. Water levels in the same timespan in Deadman subbasin and water quality in the base supply wells, drilled in 1952-53 and 1978, have remained virtually unchanged.</p><p>Ground water in storage, suitable for domestic use, in the top 200 feet of saturated sediments in Surprise Spring subbasin was estimated to be 810,000 acre-feet in the early 1950's. About 60,000 acre-feet of this has been removed, mostly for use at the Marine Corps Base, which leaves about 750,000 acre-feet of recoverable water of good quality still stored in the 200-foot interval considered. For planning purposes, it would be safe to use a conservative figure of 300,000 acre-feet for storage in the Deadman subbasin, which contains water having fluoride concentrations greater than the U.S. Environmental Protection Agency's standards for drinking water.</p><p>Three sites in the general area of the present well fields seem favorable for recharging the ground-water system in the Surprise Spring subbasin. Further exploration of these sites is suggested.</p>","language":"English","publisher":"U.S.Geological Survey","publisherLocation":"Sacramento, CA","doi":"10.3133/wri844119","collaboration":"Prepared in cooperation with the U.S. Marine Corps, Department of the Navy","usgsCitation":"Akers, J.P., 1986, Geohydrology and potential for artificial recharge in the western part of the U.S. Marine Corps Base, Twentynine Palms, California, 1982-83: U.S. Geological Survey Water-Resources Investigations Report 84-4119, Report: iv, 18 p.; 2 Plates: 32.07 x 35.21 inches and 32.18 x 34.70 inches, https://doi.org/10.3133/wri844119.","productDescription":"Report: iv, 18 p.; 2 Plates: 32.07 x 35.21 inches and 32.18 x 34.70 inches","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":54649,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4119/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Ground-water-level contours, 1982; well locations, and potential recharge areas; U.S. Marine Corps Base, Twentynine Palms, California"},{"id":54650,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4119/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120070,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4119/report-thumb.jpg"},{"id":54648,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4119/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Configuration of surface on bedrock complex at base of sediments, and area used for estimating ground-water storage, U.S. Marine Corps Base, Twentynine Palms, California"}],"country":"United States","state":"California","city":"Twentynine Palms","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.5,\n              34.5\n            ],\n            [\n              -116.2,\n              34.5\n            ],\n            [\n              -116,\n              34.25\n            ],\n            [\n              -116,\n              34.08333\n            ],\n            [\n              -116.25,\n              34.08333\n            ],\n            [\n              -116.25,\n              34.16667\n            ],\n            [\n              -116.5,\n              34.16667\n            ],\n            [\n              -116.5,\n              34.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8cac","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195425,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57318,"text":"wdrFL854 - 1986 - Water resources data, Florida, water year 1985. Volume 4: Northwest Florida","interactions":[],"lastModifiedDate":"2024-06-05T20:17:14.91391","indexId":"wdrFL854","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-85-4","title":"Water resources data, Florida, water year 1985. Volume 4: Northwest Florida","docAbstract":"<p>Water resources data for the 1985 water year in Florida consist of continuous or daily discharge for 285 streams, periodic discharge for 38 streams, miscellaneous discharge for 110 streams, continuous or daily stage for 124 streams, periodic stage for 32 streams, peak discharge for 98 streams and peak stage for 87 streams; continuous or daily elevations for 89 lakes, periodic elevations for 82 lakes; ground-water levels for 473 wells, periodic ground-water levels for 550 wells, and miscellaneous water-level measurements for 2,588 wells; quality-of-water data for 239 surface-water sites and 699 wells.</p><p>The data for northwest Florida include continuous or daily discharge for 46 streams, periodic discharge for 3 streams, miscellaneous discharge for 30 streams, continuous or daily stage for 1 stream, peak discharge for 34 streams, and peak stage for 34 streams; continuous elevations for 5 lakes and periodic elevations for 4 lakes; continuous groundwater levels for 12 wells, and periodic ground-water levels for 165 wells; quality of water for 25 surface-water sites and 20 wells.</p><p>These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, state and federal agencies in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL854","programNote":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Meadows, P., Martin, J., and Mixson, P., 1986, Water resources data, Florida, water year 1985. Volume 4: Northwest Florida: U.S. Geological Survey Water Data Report FL-85-4, xiii, 317 p., https://doi.org/10.3133/wdrFL854.","productDescription":"xiii, 317 p.","costCenters":[],"links":[{"id":429524,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/fl-85-4/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182134,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1985/fl-85-4/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"northwest Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -87.71648433687562,\n              30.960738174150208\n            ],\n            [\n              -87.71648433687562,\n              29.51793579845939\n            ],\n            [\n              -82.47514993530945,\n              29.51793579845939\n            ],\n            [\n              -82.47514993530945,\n              30.960738174150208\n            ],\n            [\n              -87.71648433687562,\n              30.960738174150208\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbcbb","contributors":{"authors":[{"text":"Meadows, P.E.","contributorId":10841,"corporation":false,"usgs":true,"family":"Meadows","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":256690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, J.B.","contributorId":32923,"corporation":false,"usgs":true,"family":"Martin","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":256691,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mixson, P.R.","contributorId":89556,"corporation":false,"usgs":true,"family":"Mixson","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":256692,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57319,"text":"wdrFL851A - 1986 - Water resources data, Florida, water year 1985, Volume 1A: Northeast Florida-surface water","interactions":[],"lastModifiedDate":"2024-05-15T19:37:06.488164","indexId":"wdrFL851A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-85-1A","title":"Water resources data, Florida, water year 1985, Volume 1A: Northeast Florida-surface water","docAbstract":"<p>Water resources data for the 1985 water year in Florida consist of continuous or daily discharge for 285 streams, periodic discharge for 38 streams, miscellaneous discharge for 110 streams, continuous or daily stage for 124 streams, periodic stage for 32 streams, peak discharge for 98 streams, and peak stage for 87 streams; continuous or daily elevations for 89 lakes, periodic elevations for 82 lakes; continuous groundwater levels for 473 wells, periodic ground-water levels for 550 wells, and miscellaneous water-level measurements for 2,588 wells; quality-of-water data for 239 surface-water sites and 699 wells.</p><p>The data for northeast Florida include continuous or daily discharge for 75 streams, periodic discharge for 9 streams, miscellaneous discharge for 21 streams, continuous or daily stage for 22 streams, periodic stage for 21 streams, peak discharge for 17 streams, and peak stage for 25 streams; continuous or daily elevations for 20 lakes, periodic elevations for 35 lakes; continuous ground-water levels for 40 wells, periodic ground-water levels for 103 wells, and miscellaneous water-level measurements for 590 wells; quality-of-water data for 19 surface-water sites and 82 wells.</p><p>These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, state and federal agencies in Florida. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL851A","collaboration":"Prepared in cooperation with the State of Florida and other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Water resources data, Florida, water year 1985, Volume 1A: Northeast Florida-surface water: U.S. Geological Survey Water Data Report FL-85-1A, xi, 290 p., https://doi.org/10.3133/wdrFL851A.","productDescription":"xi, 290 p.","costCenters":[],"links":[{"id":428744,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/fl-85-1-a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182135,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1985/fl-85-1-a/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Northeast Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.06473632228511,\n              30.589394948252348\n            ],\n            [\n              -82.06473632228511,\n              28.624130221826974\n            ],\n            [\n              -80.82701366493133,\n              28.624130221826974\n            ],\n            [\n              -80.82701366493133,\n              30.589394948252348\n            ],\n            [\n              -82.06473632228511,\n              30.589394948252348\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbcbe","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533058,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27098,"text":"wri854202 - 1986 - Occurrence of nitrate and herbicides in ground water in the upper Conestoga River basin, Pennsylvania : water-quality study of the Conestoga River headwaters, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-05T11:28:02","indexId":"wri854202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4202","title":"Occurrence of nitrate and herbicides in ground water in the upper Conestoga River basin, Pennsylvania : water-quality study of the Conestoga River headwaters, Pennsylvania","docAbstract":"<p>Nitrate-nitrogen and herbicide ground-water data is being collected by the u.s. Geological Survey as part of the nationwide Rural Clean Water Program designed to determine the effects of agricultural-management practices on water quality. Data collected from September 1982 to October 1983 &middot; in the 188-square mile intensively farmed upper Conestoga River basin indicates high nitrate and detectable herbicide concentrations in ground water are closely associated with agricultural practices and carbonate geology. Maximum nitrate-nitrogen concentrations from 42 wells and one spring ranged from 37 to 40 milligrams per liter in the agricultural areas, and 12 to 19 milligrams per liter in the nonagricultural areas. Median concentrations of nitrate generally were three times higher in wells that penetrated carbonate rock than in wells that penetrated noncarbonate rocks. More than 40 percent of the wells in the carbonate and agricultural areas had dissolved-nitrate concentrations that exceeded 10 milligrams per liter as nitrogen, the criterion established by the U.S. Environmental Protection Agency as excessive for drinking water. Atrazine, simazine, alachlor, and metolachlor were found almost exclusively in the agricultural and carbonate areas.</p>\n<p>Water-quality data collected before and after installation of terraces, manure storage, and nutrient and herbicide management practices is valuable in determining the effectiveness of these agricultural practices, and will provide useful information to protect agricultural land, local water supplies, the Conestoga and Susquehanna Rivers and ultimately the Chesapeake Bay.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854202","usgsCitation":"Fishel, D.K., and Lietman, P.L., 1986, Occurrence of nitrate and herbicides in ground water in the upper Conestoga River basin, Pennsylvania : water-quality study of the Conestoga River headwaters, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 85-4202, iii, 8 p., https://doi.org/10.3133/wri854202.","productDescription":"iii, 8 p.","numberOfPages":"15","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":158657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri854202.jpg"},{"id":310314,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4202/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Conestoga River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.12838745117188,\n              40.333983227838104\n            ],\n            [\n              -75.85098266601562,\n              40.142139942215415\n            ],\n            [\n              -76.03775024414062,\n              39.9897471840457\n            ],\n            [\n              -76.431884765625,\n              40.24389506699777\n            ],\n            [\n              -76.12838745117188,\n              40.333983227838104\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db692369","contributors":{"authors":[{"text":"Fishel, David K.","contributorId":34967,"corporation":false,"usgs":true,"family":"Fishel","given":"David","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":197548,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lietman, Patricia L.","contributorId":64227,"corporation":false,"usgs":true,"family":"Lietman","given":"Patricia","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197549,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43093,"text":"ofr81323 - 1986 - Land use and land cover and associated maps for Pullman, Washington; Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr81323","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"81-323","title":"Land use and land cover and associated maps for Pullman, Washington; Idaho","language":"ENGLISH","doi":"10.3133/ofr81323","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Land use and land cover and associated maps for Pullman, Washington; Idaho: U.S. Geological Survey Open-File Report 81-323, maps ;45 x 63 cm., https://doi.org/10.3133/ofr81323.","productDescription":"maps ;45 x 63 cm.","costCenters":[],"links":[{"id":135554,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af628","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26958,"text":"wri864344 - 1986 - Sediment-data sources and estimated annual suspended-sediment loads of rivers and streams in Colorado","interactions":[],"lastModifiedDate":"2021-12-21T20:55:50.903688","indexId":"wri864344","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4344","title":"Sediment-data sources and estimated annual suspended-sediment loads of rivers and streams in Colorado","docAbstract":"Sources of sediment data collected by several government agencies through water year 1984 are summarized for Colorado. The U.S. Geological Survey has collected suspended-sediment data at 243 sites; these data are stored in the U.S. Geological Survey 's water data storage and retrieval system. The U.S. Forest Service has collected suspended-sediment and bedload data at an additional 225 sites, and most of these data are stored in the U.S. Environmental Protection Agency 's water-quality-control information system. Additional unpublished sediment data are in the possession of the collecting entities. Annual suspended-sediment loads were computed for 133 U.S. Geological Survey sediment-data-collection sites using the daily mean water-discharge/sediment-transport-curve method. Sediment-transport curves were derived for each site by one of three techniques: (1) Least-squares linear regression of all pairs of suspended-sediment and corresponding water-discharge data, (2) least-squares linear regression of data sets subdivided on the basis of hydrograph season; and (3) graphical fit to a logarithm-logarithm plot of data. The curve-fitting technique used for each site depended on site-specific characteristics. Sediment-data sources and estimates of annual loads of suspended, bed, and total sediment from several other reports also are summarized. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864344","usgsCitation":"Elliott, J.G., and DeFeyter, K.L., 1986, Sediment-data sources and estimated annual suspended-sediment loads of rivers and streams in Colorado: U.S. Geological Survey Water-Resources Investigations Report 86-4344, Report: vii, 148 p.; 2 Plates: 26.86 × 21.85 inches and 26.94 × 22.40 inches, https://doi.org/10.3133/wri864344.","productDescription":"Report: vii, 148 p.; 2 Plates: 26.86 × 21.85 inches and 26.94 × 22.40 inches","costCenters":[],"links":[{"id":55844,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4344/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55843,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4344/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55845,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4344/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4344/report-thumb.jpg"},{"id":393252,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36657.htm"}],"country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.039306640625,\n              37.01132594307015\n            ],\n            [\n              -102.06298828125,\n              37.01132594307015\n            ],\n            [\n              -102.06298828125,\n              41.00477542222947\n            ],\n            [\n              -109.039306640625,\n              41.00477542222947\n            ],\n            [\n              -109.039306640625,\n              37.01132594307015\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499fe4b07f02db5bd219","contributors":{"authors":[{"text":"Elliott, J. G.","contributorId":45341,"corporation":false,"usgs":true,"family":"Elliott","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":197315,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeFeyter, K. L.","contributorId":53425,"corporation":false,"usgs":true,"family":"DeFeyter","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197316,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15274,"text":"ofr86228 - 1986 - Physical and chemical data for northern San Francisco Bay, California, September through November, 1984","interactions":[],"lastModifiedDate":"2016-07-27T12:57:46","indexId":"ofr86228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-228","title":"Physical and chemical data for northern San Francisco Bay, California, September through November, 1984","docAbstract":"<p>This report presents physical and chemical data for northern San Francisco Bay waters. Samples were collected during the late summer and fall of 1984 during six cruises at near-two-week intervals. Bay waters were sampled at designated (historical) stations and selected salinitis along the deep channel of northern San Francisco Bay. Measurements included temperature, salinity, turbidity, in vivo fluorescence, chlorophyll a, alkalinity, suspended particulate matter, dissolved organic carbon, and dissolved inorganic nutrients: nitrite, nitrate + nitrite, ammonium, dissolved silica, and ortho-phosphate. Numerical results are tabulated and methods are described. (USGS)</p>","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86228","usgsCitation":"Ota, A.Y., Schemel, L., and Hager, S., 1986, Physical and chemical data for northern San Francisco Bay, California, September through November, 1984: U.S. Geological Survey Open-File Report 86-228, 32 p. :map ;28 cm., https://doi.org/10.3133/ofr86228.","productDescription":"32 p. :map ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":44205,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0228/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0228/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485e6","contributors":{"authors":[{"text":"Ota, Allan Y.","contributorId":85192,"corporation":false,"usgs":true,"family":"Ota","given":"Allan","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":170865,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schemel, L. E.","contributorId":89529,"corporation":false,"usgs":true,"family":"Schemel","given":"L. E.","affiliations":[],"preferred":false,"id":170866,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hager, S.W.","contributorId":51746,"corporation":false,"usgs":true,"family":"Hager","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":170864,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3587,"text":"cir948 - 1986 - Analytical methods used in geochemical exploration, 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"cir948","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"948","title":"Analytical methods used in geochemical exploration, 1984","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir948","usgsCitation":"O’Leary, R.M., and Meier, A.L., 1986, Analytical methods used in geochemical exploration, 1984: U.S. Geological Survey Circular 948, iii, 48 p. :ill. ;27 cm., https://doi.org/10.3133/cir948.","productDescription":"iii, 48 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":117125,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1986/0948/report-thumb.jpg"},{"id":30619,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1986/0948/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f672","contributors":{"authors":[{"text":"O’Leary, Richard M.","contributorId":19936,"corporation":false,"usgs":true,"family":"O’Leary","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":147212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meier, Allen L.","contributorId":14384,"corporation":false,"usgs":true,"family":"Meier","given":"Allen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147211,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27242,"text":"wri854147 - 1986 - Water-quality characteristics and nutrient and suspended-sediment loads, Carson River and Truckee Canal, western Nevada, water year 1980","interactions":[],"lastModifiedDate":"2022-08-23T19:38:27.291403","indexId":"wri854147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4147","title":"Water-quality characteristics and nutrient and suspended-sediment loads, Carson River and Truckee Canal, western Nevada, water year 1980","docAbstract":"<p>Lahontan Reservoir is a major recreational site in the Carson River basin in western Nevada. The reservoir is fed by the Carson River and by the Truckee Canal which transports water from the adjacent Truckee River. Water quality in both rivers is influenced by agriculture and urbanization. Specific conductance tended to increase in a downstream direction. Generally, pH values ranged from 7.0 to 8.8. Dissolved-oxygen concentrations were greater than 5 milligrams/L. Calcium and sodium were the dominant cations and bicarbonate the dominant anion. Suspended-sediment concentrations ranged from 3 to 1,790 milligrams/L. Ultimate carbonaceous biochemical oxygen demand ranged from 1.2 to 19.6 milligrams/L. The codominant algal groups were the blue-greens, greens, and diatoms. Background total nutrient and suspended-sediment loads were about 490 tons nitrogen, 130 tons phosphorus, and 200,000 tons suspended sediment. Total nutrient and suspended-sediment loads to Lahontan Reservoir were about 980 tons nitrogen, 300 tons phosphorus, and 300,000 tons suspended sediment. Loads to the lower Carson River from the reservoir were about 820 tons total nitrogen, 180 tons total phosphorus, and 26,000 tons suspended sediment.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854147","usgsCitation":"Garcia, K.T., and Carman, R.L., 1986, Water-quality characteristics and nutrient and suspended-sediment loads, Carson River and Truckee Canal, western Nevada, water year 1980: U.S. Geological Survey Water-Resources Investigations Report 85-4147, vii, 107 p., https://doi.org/10.3133/wri854147.","productDescription":"vii, 107 p.","costCenters":[],"links":[{"id":405483,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36310.htm","linkFileType":{"id":5,"text":"html"}},{"id":56105,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4147/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4147/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Carson River and Truckee Canal","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120,\n              38.717\n            ],\n            [\n              -119,\n              38.717\n            ],\n            [\n              -119,\n              39.6\n            ],\n            [\n              -120,\n              39.6\n            ],\n            [\n              -120,\n              38.717\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cce4b07f02db544586","contributors":{"authors":[{"text":"Garcia, K. T.","contributorId":52613,"corporation":false,"usgs":true,"family":"Garcia","given":"K.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":197784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carman, R. L.","contributorId":16460,"corporation":false,"usgs":true,"family":"Carman","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197783,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27100,"text":"wri854023 - 1986 - Results of a preimpoundment water-quality study of Swatara Creek, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-05T11:28:52","indexId":"wri854023","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4023","title":"Results of a preimpoundment water-quality study of Swatara Creek, Pennsylvania","docAbstract":"<p>The water quality of Swatara Creek prior to impoundment by the proposed Swatara Creek Reservoir in south-central Pennsylvania was studied from July 1981 through October 1982. The report, done in cooperation with the Pennsylvania Department of Environmental Resources (PaDER), Bureau of State Parks, presents information on existing water-quality conditions. A discussion of possible water-quality conditions in and downstream from the planned impoundment is also included.</p>\n<p>Precipitation measured near the study area at Lebanon, Pennsylvania from October 1981 through September 1982 was 8 percent below normal. Streamflow for the same period at Swatara Creek at Harper Tavern just downstream from the study area was 15 percent below the average annual flow. Swatara Creek above Highway 895 has been degraded by acid mine drainage. The main inflow to the planned impoundment has 2.1 times the discharge of Lower Little Swatara Creek--a forested and agricultural basin that is also tributary to the proposed impoundment. During the 1982 water year, 17,400 tons of suspended sediment were transported from the study area. About 46 percent of the annual load was transported during 3 days of high flow. Inflows to the planned impoundment from both Lower Little Swatara Creek and Swatara Creek above Highway 895 were poorly buffered. Measured concentrations of alkalinity and acidity were usually less than 10 mg/L (milligrams per liter) and 5 mg/L as CaCO3, respectively. The inflows contain high concentrations of nutrients and metals that would probably stratify in a reservoir. Maximum concentrations of dissolved nitrate and total phosphorus were 2.6 mg/L and 0.31 mg/L, respectively. At Lower Little Swatara Creek; these concentrations are well above those needed for growth of algae. Maximum observed concentrations for total recoverable iron, aluminum, and manganese at Swatara Creek above Highway 895 at Pine Grove were 100,000 ug/L (micrograms per liter), 66,000 ug/L, and 2,300 ug/L, respectively.</p>\n<p>Large increases in metal concentrations along with simultaneous decreases in pH and increases in acidity confirm that mine drainage continues to degrade the water quality of Swatara Creek and may have a large impact on water quality of the planned impoundment. Iron, lead, copper, and zinc concentrations periodically exceeded the U.S. Environmental Protection Agency (U.S. EPA) criteria for freshwater aquatic life. Concentrations of manganese and lead also exceeded the U.S. EPA criteria for domestic water supplies and human health, respectively.</p>\n<p>The water quality of the Swatara Creek Reservoir will depend on characteristics such as (1) the detention time of water in the lake, (2) the timing and extent of thermal and chemical stratification, (3) sedimentation, and (4) the chemical loading and concentrations in the lake. Each of these characteristics may depend in part, on streamflow.</p>\n<p>The impoundment will act as a sediment trap and thus reduce the concentrations of total phosphorus, iron, aluminum, lead, copper, and zinc immediately downstream from the impoundment. Large storm discharges and releases from the hypolimnion of the reservoir to attain the winter-pool level may contain low oxygen concentrations and elevated concentrations of iron, aluminum, lead, copper, and zinc. Unless conservation releases from the multi-level release gates are carefully controlled, low dissolved-oxygen levels and high metal concentrations may degrade the downstream water quality and be detrimental to the aquatic community.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/wri854023","usgsCitation":"Fishel, D.K., and Richardson, J., 1986, Results of a preimpoundment water-quality study of Swatara Creek, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 85-4023, vi, 84 p., https://doi.org/10.3133/wri854023.","productDescription":"vi, 84 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science 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,{"id":4308,"text":"cir1010 - 1986 - Goals of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"cir1010","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1010","title":"Goals of the U.S. Geological Survey","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir1010","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Goals of the U.S. Geological Survey: U.S. Geological Survey Circular 1010, v, 17 p. :ill. ;28 cm., https://doi.org/10.3133/cir1010.","productDescription":"v, 17 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":123270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1986/1010/report-thumb.jpg"},{"id":31419,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1986/1010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674201","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528176,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35462,"text":"b1587 - 1986 - Geology and mineral-resource potential of Seven Roadless Areas in the Apalachicola National Forest, Liberty County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:09:45","indexId":"b1587","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1587","title":"Geology and mineral-resource potential of Seven Roadless Areas in the Apalachicola National Forest, Liberty County, Florida","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1587","usgsCitation":"Patterson, S.H., Cameron, C.C., and Schmidt, W., 1986, Geology and mineral-resource potential of Seven Roadless Areas in the Apalachicola National Forest, Liberty County, Florida: U.S. Geological Survey Bulletin 1587, vi, 21 p. ill, maps ;28 cm., https://doi.org/10.3133/b1587.","productDescription":"vi, 21 p. ill, maps ;28 cm.","costCenters":[],"links":[{"id":164645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1587/report-thumb.jpg"},{"id":63359,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1587/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4733","contributors":{"authors":[{"text":"Patterson, Sam H.","contributorId":62996,"corporation":false,"usgs":true,"family":"Patterson","given":"Sam","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":214686,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cameron, Cornelia Clermont","contributorId":20737,"corporation":false,"usgs":true,"family":"Cameron","given":"Cornelia","email":"","middleInitial":"Clermont","affiliations":[],"preferred":false,"id":214684,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schmidt, Walter","contributorId":21612,"corporation":false,"usgs":true,"family":"Schmidt","given":"Walter","email":"","affiliations":[],"preferred":false,"id":214685,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25922,"text":"wri844148 - 1986 - Hydrogeology and leachate movement near two chemical-waste sites in Oswego County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri844148","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"84-4148","title":"Hydrogeology and leachate movement near two chemical-waste sites in Oswego County, New York","docAbstract":"Forty-five observation wells and test holes were installed at two chemical waste disposal sites in Oswego County, New York, to evaluate the hydrogeologic conditions and the rate and direction of leachate migration. At the site near Oswego groundwater moves northward at an average velocity of 0.4 ft/day through unconsolidated glacial deposits and discharges into White Creek and Wine Creek, which border the site and discharge to Lake Ontario. Leaking barrels by chemical wastes have contaminated the groundwater within the site, as evidenced by detection of 10 ' priority pollutant ' organic compounds, and elevated values of specific conductance, chloride, arsenic, lead, and mercury. At the site near Fulton, where 8,000 barrels of chemical wastes are buried, groundwater in the sandy surficial aquifer bordering the landfill on the south and east moves southward and eastward at an average velocity of 2.8 ft/day and discharges to Bell Creek, which discharges to the Oswego River, or moves beneath the landfill. Leachate is migrating eastward, southeastward, and southwestward, as evidenced by elevated values of specific conductance, temperature, and concentrations of several trace metals at wells east, southeast, and southwest of the site. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844148","usgsCitation":"Anderson, H., and Miller, T.S., 1986, Hydrogeology and leachate movement near two chemical-waste sites in Oswego County, New York: U.S. Geological Survey Water-Resources Investigations Report 84-4148, v, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844148.","productDescription":"v, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4148/report-thumb.jpg"},{"id":54680,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4148/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625438","contributors":{"authors":[{"text":"Anderson, H. R.","contributorId":67487,"corporation":false,"usgs":true,"family":"Anderson","given":"H. R.","affiliations":[],"preferred":false,"id":195485,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Todd S.","contributorId":85623,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":195486,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61018,"text":"mf1867 - 1986 - Map showing landslides in California that have caused fatalities or at least $1,000,000 in damages from 1906 to 1984","interactions":[],"lastModifiedDate":"2016-08-23T10:03:24","indexId":"mf1867","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1867","title":"Map showing landslides in California that have caused fatalities or at least $1,000,000 in damages from 1906 to 1984","docAbstract":"<p>Understanding where landslide processes in California have been most severe is helpful in determining priorities for landslide mapping, mitigation measures, and preparedness planning. Although a few studies of landslide damage and fatalities have been published (see sources of data 12, 17, 34, 36, 40), and many more reports mention landslide damage and fatalities incidentally, our map is the first to show where the problem is most severe for the entire state.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1867","usgsCitation":"Taylor, F., and Brabb, E.E., 1986, Map showing landslides in California that have caused fatalities or at least $1,000,000 in damages from 1906 to 1984: U.S. Geological Survey Miscellaneous Field Studies Map 1867, Plate: 40.87 x 50.33 inches, https://doi.org/10.3133/mf1867.","productDescription":"Plate: 40.87 x 50.33 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326123,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1867.JPG"},{"id":327549,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1867/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,33 ], [ -124,42 ], [ -115,42 ], [ -115,33 ], [ -124,33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a92e4b07f02db657794","contributors":{"authors":[{"text":"Taylor, Fred","contributorId":50165,"corporation":false,"usgs":true,"family":"Taylor","given":"Fred","affiliations":[],"preferred":false,"id":264842,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brabb, E. E.","contributorId":43780,"corporation":false,"usgs":true,"family":"Brabb","given":"E.","middleInitial":"E.","affiliations":[],"preferred":false,"id":264841,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27076,"text":"wri864063 - 1986 - Machine-readable files developed for the High Plains Regional Aquifer-System analysis in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:46:47","indexId":"wri864063","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4063","title":"Machine-readable files developed for the High Plains Regional Aquifer-System analysis in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","docAbstract":"Machine-readable files were developed for the High Plains Regional Aquifer-System Analysis project are stored on two magnetic tapes available from the U.S. Geological Survey. The first tape contains computer programs that were used to prepare, store, retrieve, organize, and preserve the areal interpretive data collected by the project staff. The second tape contains 134 data files that can be divided into five general classes: (1) Aquifer geometry data, (2) aquifer and water characteristics , (3) water levels, (4) climatological data, and (5) land use and water use data. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864063","usgsCitation":"Ferrigno, C., 1986, Machine-readable files developed for the High Plains Regional Aquifer-System analysis in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 86-4063, iii, 23 p. ;28 cm., https://doi.org/10.3133/wri864063.","productDescription":"iii, 23 p. ;28 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":123722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4063/report-thumb.jpg"},{"id":55946,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4063/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6490bf","contributors":{"authors":[{"text":"Ferrigno, C.F.","contributorId":27092,"corporation":false,"usgs":true,"family":"Ferrigno","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":197515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61006,"text":"mf1897 - 1986 - Logs of trenches across the Beatty Scarp, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"mf1897","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1897","title":"Logs of trenches across the Beatty Scarp, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/mf1897","isbn":"0607817585","usgsCitation":"Swadley, W.C., Huckins, H.E., and Taylor, E.M., 1986, Logs of trenches across the Beatty Scarp, Nye County, Nevada: U.S. Geological Survey Miscellaneous Field Studies Map 1897, 4 sections on 1 sheet ;sheet 104 x 101 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1897.","productDescription":"4 sections on 1 sheet ;sheet 104 x 101 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":106132,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7560.htm","linkFileType":{"id":5,"text":"html"},"description":"7560"},{"id":182782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"40","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.75055555555555,36.83444444444444 ], [ -116.75055555555555,36.8675 ], [ -116.73333333333333,36.8675 ], [ -116.73333333333333,36.83444444444444 ], [ -116.75055555555555,36.83444444444444 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d770","contributors":{"authors":[{"text":"Swadley, W. C.","contributorId":46940,"corporation":false,"usgs":true,"family":"Swadley","given":"W.","middleInitial":"C.","affiliations":[],"preferred":false,"id":264815,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huckins, H. E.","contributorId":105330,"corporation":false,"usgs":true,"family":"Huckins","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":264817,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, E. M.","contributorId":55842,"corporation":false,"usgs":true,"family":"Taylor","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":264816,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60997,"text":"mf1856 - 1986 - Seismicity map of the state of Utah","interactions":[],"lastModifiedDate":"2017-05-11T14:38:38","indexId":"mf1856","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1856","title":"Seismicity map of the state of Utah","docAbstract":"<p>This map is one of a series of seismicity maps produced by the U. S. Geological Survey that show earthquake data of individual states or groups of states at the scale of 1:1,000,000. This map shows only those earthquakes with epicenters located within the boundaries of Utah, even though earthquakes in nearby states or countries may have been felt or may have caused damage in Utah.</p><p>The data in table 1 were used to compile the seismicity map; these data are a corrected, expanded, and updated (through 1982) version of the data used by Algermissen (1969) for a study of seismic risk in the United States. The locations and intensities of some earthquakes were revised and intensities were assigned where none had been before. Many earthquakes were added to the original list from new data sources as well as from some old data sources that had not been previously used. The data in table 1 represent best estimates of the location of the epicenter, magnitude, and intensity of each earthquake on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed, but not all, especially for earthquakes that occurred before seismic instruments were universally used.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1856","usgsCitation":"Stover, C.W., Reagor, B., and Algermissen, S.T., 1986, Seismicity map of the state of Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1856, 57.79 x 38.29 inches, https://doi.org/10.3133/mf1856.","productDescription":"57.79 x 38.29 inches","costCenters":[],"links":[{"id":341151,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1856/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1856/mf1856.JPG"}],"country":"United States","state":"Utah","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"47\",\"properties\":{\"name\":\"Utah\",\"nation\":\"USA  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,{"id":25889,"text":"wri854178 - 1986 - Ground water in the Long Meadow area and its relation with that in the General Sherman Tree area, Sequoia National Park, California","interactions":[],"lastModifiedDate":"2018-02-15T12:01:33","indexId":"wri854178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4178","title":"Ground water in the Long Meadow area and its relation with that in the General Sherman Tree area, Sequoia National Park, California","docAbstract":"<p>Westward movement of ground water from the Long Meadow area of Sequoia National Park, California, to the General Sherman Tree area is prevented by an eastward hydraulic gradient and low fracture permeability of a granodiorite ridge separating the two areas. Clay beds present in the alluvium in the Long Meadow area would hinder, but not preclude, recharge to the ground-water system beneath Long Meadow from streams. </p><p>A dependable ground-water supply of about 50 gallons per minute (72,000 gallons per day) can be developed from the Long Meadow area. The withdrawal of this quantity of ground water from the Long Meadow area should not affect ground or surface water in the General Sherman Tree area. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Sacramento, CA","doi":"10.3133/wri854178","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Akers, J.P., 1986, Ground water in the Long Meadow area and its relation with that in the General Sherman Tree area, Sequoia National Park, California: U.S. Geological Survey Water-Resources Investigations Report 85-4178, Report: iv, 15 p.; 1 Plate: 20.19 x 17.62 inches, https://doi.org/10.3133/wri854178.","productDescription":"Report: iv, 15 p.; 1 Plate: 20.19 x 17.62 inches","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":121514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4178/report-thumb.jpg"},{"id":54651,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4178/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Long Meadow Area, Sequoia National Park, California, showing locations of test-hole, stream-measuring, and water-sampling sites"},{"id":54652,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4178/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Sequoia National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.75456809997559,\n              36.572319932849254\n            ],\n            [\n              -118.71500015258789,\n              36.572319932849254\n            ],\n            [\n              -118.71500015258789,\n              36.599542913631645\n            ],\n            [\n              -118.75456809997559,\n              36.599542913631645\n            ],\n            [\n              -118.75456809997559,\n              36.572319932849254\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d999","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57994,"text":"pp1369 - 1986 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","interactions":[{"subject":{"id":9672,"text":"ofr84612 - 1984 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","indexId":"ofr84612","publicationYear":"1984","noYear":false,"title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":57994,"text":"pp1369 - 1986 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","indexId":"pp1369","publicationYear":"1986","noYear":false,"title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado"},"id":1}],"lastModifiedDate":"2012-02-02T00:12:14","indexId":"pp1369","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1369","title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","language":"ENGLISH","doi":"10.3133/pp1369","usgsCitation":"Jarrett, R.D., and Costa, J.E., 1986, Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado: U.S. Geological Survey Professional Paper 1369, vi, 78 p. : ill.; 29 cm.; 2 plates in pocket, https://doi.org/10.3133/pp1369.","productDescription":"vi, 78 p. : ill.; 29 cm.; 2 plates in pocket","costCenters":[],"links":[{"id":104610,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4820.htm","linkFileType":{"id":5,"text":"html"},"description":"4820"},{"id":120705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1369/report-thumb.jpg"},{"id":88298,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1369/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88299,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1369/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88300,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1369/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc732","contributors":{"authors":[{"text":"Jarrett, Robert D. rjarrett@usgs.gov","contributorId":2260,"corporation":false,"usgs":true,"family":"Jarrett","given":"Robert","email":"rjarrett@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":258117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Costa, John E.","contributorId":105743,"corporation":false,"usgs":true,"family":"Costa","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":258118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26205,"text":"wri864193 - 1986 - Comparison of flume and towing methods for verifying the calibration of a suspended-sediment sampler","interactions":[],"lastModifiedDate":"2018-03-05T11:08:38","indexId":"wri864193","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4193","title":"Comparison of flume and towing methods for verifying the calibration of a suspended-sediment sampler","docAbstract":"<p>Suspended-sediment samplers must sample isokinetically (at stream velocity) in order to collect representative water samples of rivers. Each sampler solo by the Federal Interagency Sedimentation Project or by the U.S. Geological Survey Hydrologic Instrumentation Facility has been adjusted to sample isokinetically and tested in a flume to verify the calibration. The test program for a modified U.S. P-61 sampler provided an opportunity to compare flume and towing tank tests. Although the two tests yielded statistically distinct results, the difference between them was quite small. The conclusion is that verifying the calibration of any suspended-sediment sampler by either the flume or towing method should give acceptable results.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Minneapolis, MN","doi":"10.3133/wri864193","collaboration":"Prepared in cooperation with the U.S. Agricultural Research Service, U.S. Bureau of Reclamation, U.S. Forest Service, U.S. Bureau of Land Management, and the U.S. Federal Highways Admininstration","usgsCitation":"Beverage, J., and Futrell, J., 1986, Comparison of flume and towing methods for verifying the calibration of a suspended-sediment sampler: U.S. Geological Survey Water-Resources Investigations Report 86-4193, v, 12 p., https://doi.org/10.3133/wri864193.","productDescription":"v, 12 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":55000,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4193/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126635,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4193/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3b9","contributors":{"authors":[{"text":"Beverage, J.P.","contributorId":44120,"corporation":false,"usgs":true,"family":"Beverage","given":"J.P.","affiliations":[],"preferred":false,"id":195978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Futrell, J.C.","contributorId":32953,"corporation":false,"usgs":true,"family":"Futrell","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":195977,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25861,"text":"wri844079 - 1986 - Water resources of Weston County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri844079","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"84-4079","title":"Water resources of Weston County, Wyoming","docAbstract":"Surface water is scarce in Weston County, Wyoming. Groundwater has been developed from rocks ranging in age from Mississippian to Holocene. Adequate supplies for domestic or stock use can be developed from wells generally less than 1,000 ft deep, except in the area underlain by a thick sequence of predominantly marine shale that will yield only small quantities of very mineralized water. In the early 1960 's decreases in artesian pressures occurred in some wells completed in the Lakota Formation of Early Cretaceous age and Pahasapa Limestone of Early Mississippian age. Only the decrease in the Lakota was attributed to development of water from the formation. Extensive development of either of these aquifers, however, may result in significant interference between nearby wells completed within the same aquifer. There are other aquifers within a few hundred feet of the overlying Lakota Formation that could be developed as an alternative to the Lakota to help limit the loss of pressure. The much deeper Pahasapa Limestone generally is developed because of the large supplies that are possible. Because there are no other large yield aquifers, there are no alternatives to limit the loss of pressure of the Pahasapa in the event of increased development. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844079","usgsCitation":"Lowry, M., Head, W.J., Rankl, J., and Busby, J., 1986, Water resources of Weston County, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 84-4079, iv, 33 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844079.","productDescription":"iv, 33 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123493,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4079/report-thumb.jpg"},{"id":54612,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4079/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54613,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4079/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fcfb2","contributors":{"authors":[{"text":"Lowry, M.E.","contributorId":55807,"corporation":false,"usgs":true,"family":"Lowry","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":195379,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Head, W. J.","contributorId":33719,"corporation":false,"usgs":true,"family":"Head","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":195378,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rankl, J.G.","contributorId":107733,"corporation":false,"usgs":true,"family":"Rankl","given":"J.G.","affiliations":[],"preferred":false,"id":195381,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Busby, J.F.","contributorId":105300,"corporation":false,"usgs":true,"family":"Busby","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":195380,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25876,"text":"wri854230 - 1986 - Reconnaissance of ground-water resources in the North Fork Gunnison River basin, southwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri854230","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4230","title":"Reconnaissance of ground-water resources in the North Fork Gunnison River basin, southwestern Colorado","docAbstract":"Aquifers of large areal extent in the North Fork Gunnison River basin are found in the alluvium and bedrock. Alluvial aquifers yielded water with dissolved solids concentrations ranging from 43 to 2,300 mg/L. Dissolved solids concentrations of water samples from the Mesaverde Formation of Late Cretaceous age and the Dakota Sandstone and Burro Canyon Formations of Late and Early Cretaceous age ranged from 56 to 3,200 mg/L. Dissolved solids concentrations of water samples from Mancos Shale ranged from 1,800 to 8,200 mg/L. Most wells in the North Fork Gunnison River basin are at altitudes below 7,500 ft, yield from 2 to 40 gal/min and are completed in alluvial sand and gravel, sandstone , or fractured bedrock. Springs generally are at altitudes above 7,000 ft, discharge from perched water tables at geologic contacts, have calcium magnesium bicarbonate water types, and are much less saline than water from wells. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854230","usgsCitation":"Ackerman, D.J., and Brooks, T., 1986, Reconnaissance of ground-water resources in the North Fork Gunnison River basin, southwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 85-4230, v, 21 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854230.","productDescription":"v, 21 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4230/report-thumb.jpg"},{"id":54630,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4230/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54631,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4230/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54632,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4230/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e817","contributors":{"authors":[{"text":"Ackerman, D. J.","contributorId":53380,"corporation":false,"usgs":true,"family":"Ackerman","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":195408,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooks, Tom","contributorId":76356,"corporation":false,"usgs":true,"family":"Brooks","given":"Tom","email":"","affiliations":[],"preferred":false,"id":195409,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}