{"pageNumber":"58","pageRowStart":"1425","pageSize":"25","recordCount":2263,"records":[{"id":27218,"text":"wri864056 - 1987 - Effects of coal strip mining on stream water quality and biology, southwestern Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:43","indexId":"wri864056","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4056","title":"Effects of coal strip mining on stream water quality and biology, southwestern Washington","docAbstract":"Strip mining for coal in southwestern Washington may be affecting the water quality of streams. To investigate these possible effects, five streams were selected for study of water quality in each of the two coal bearing areas: the Centralia-Chehalis coal district, and Kelso-Castle Rock coal area. In the Centralia-Chehalis coal district, three of the streams have drainage basins in which mines are active. Water in streams that drain unmined basins is typical of western Washington streams and is characterized as a mixed water because calcium, magnesium, sodium, and bicarbonate ions predominate. A change in anionic composition from bicarbonate to sulfate in streams draining mined areas was not sufficient to change the general water composition and thus make the streams acidic. The largest downstream changes in water quality in both mined and unmined drainage basins were observed during summer low-flow conditions, when minimal dilution, increased water temperatures, and low dissolved oxygen concentrations occurred. High dissolved solids were found in the mined drainage basins during this period. High concentrations of iron, manganese, and zinc were present in the bottom sediments of the mined basins. Moderate concentrations of chromium, cobalt, copper, and zinc were also found in the bottom sediments of a few unmined basins. Streams with substrates of gravel-cobble or gravel-coarse sand had the most diverse benthic fauna and a higher number of ubiquitous taxa than streams with sand-silt substrates, which had the most dissimilar fauna. Mayflies, stoneflies, and caddisflies were rare at the site most affected by mining. The erosion potential of a basin appears to be related to the average basin slope and the amount of forested areas. Strip mining for coal in steep basins may lead to massive movements of unconsolidated spoils after vegetal cover is removed if the land disturbed is graded to pre-mining slopes. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864056","usgsCitation":"Fuste, L.A., and Meyer, D.F., 1987, Effects of coal strip mining on stream water quality and biology, southwestern Washington: U.S. Geological Survey Water-Resources Investigations Report 86-4056, vi, 124 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864056.","productDescription":"vi, 124 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":125108,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4056/report-thumb.jpg"},{"id":56089,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68453a","contributors":{"authors":[{"text":"Fuste, L. A.","contributorId":85631,"corporation":false,"usgs":true,"family":"Fuste","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":197751,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, D. F.","contributorId":21167,"corporation":false,"usgs":true,"family":"Meyer","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197750,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13971,"text":"ofr87149 - 1987 - Data tables for microprobe analyses of garnets from skarns at Copper Basin in the Battle Mountain Mining District, Lander County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr87149","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-149","title":"Data tables for microprobe analyses of garnets from skarns at Copper Basin in the Battle Mountain Mining District, Lander County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87149","usgsCitation":"Hammarstrom, J.M., 1987, Data tables for microprobe analyses of garnets from skarns at Copper Basin in the Battle Mountain Mining District, Lander County, Nevada: U.S. Geological Survey Open-File Report 87-149, 103 p. :map ;28 cm., https://doi.org/10.3133/ofr87149.","productDescription":"103 p. :map ;28 cm.","costCenters":[],"links":[{"id":148014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0149/report-thumb.jpg"},{"id":42621,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0149/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679c62","contributors":{"authors":[{"text":"Hammarstrom, J. M.","contributorId":34513,"corporation":false,"usgs":true,"family":"Hammarstrom","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":168720,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26094,"text":"wri874023 - 1987 - Preliminary assessment of water quality and its relation to hydrogeology and land use: Potomac-Raritan-Magothy aquifer system, New Jersey","interactions":[],"lastModifiedDate":"2021-12-20T22:20:14.978269","indexId":"wri874023","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4023","title":"Preliminary assessment of water quality and its relation to hydrogeology and land use: Potomac-Raritan-Magothy aquifer system, New Jersey","docAbstract":"<p>The relation of water quality to hydrogeology and land use was evaluated using analysis of water samples from 71 wells in the northern part of the Potomac-Raritan-Magothy aquifer system in New Jersey. The sampling network was evaluated for variations in hydrogeology. Well depths, pumping rates, and the number of wells in the confined and unconfined parts of the aquifer system did not differ among land-use groups. The influences of hydrogeologic factors on water quality were evaluated without considering land use. Shallow wells had the highest specific conductance and major ion concentrations. Water from wells in the unconfined part of the aquifer system had the highest dissolved organic carbon concentration. Dissolved oxygen and nitrate concentrations were lowest, trace metals concentrations were highest, and phenols were detected most frequently in groundwater from undeveloped land. Major ions and trace metals concentrations were lowest, dissolved oxygen and copper concentrations were highest, and pesticides were most frequently detected in groundwater from agricultural land. Nitrate concentrations were highest and orthophosphate, nitrite, and purgeable organics were detected most frequently in groundwater from urban land. These water quality data were compared to data from the same aquifer system in southern New Jersey. Frequencies of detection of purgeable organics among land-use groups were similar in the northern and southern areas.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874023","usgsCitation":"Barton, C., Vowinkel, E., and Nawyn, J., 1987, Preliminary assessment of water quality and its relation to hydrogeology and land use: Potomac-Raritan-Magothy aquifer system, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 87-4023, vi, 79 p., https://doi.org/10.3133/wri874023.","productDescription":"vi, 79 p.","costCenters":[],"links":[{"id":393165,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46709.htm"},{"id":54873,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4023/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4023/report-thumb.jpg"}],"country":"United States","state":"New Jersey","otherGeospatial":"Potomac-Raritan-Magothy aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.875,\n              40.125\n            ],\n            [\n              -74.125,\n              40.125\n            ],\n            [\n              -74.125,\n              40.625\n            ],\n            [\n              -74.875,\n              40.625\n            ],\n            [\n              -74.875,\n              40.125\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66957c","contributors":{"authors":[{"text":"Barton, Cynthia 0000-0001-8505-4347 cbarton@usgs.gov","orcid":"https://orcid.org/0000-0001-8505-4347","contributorId":3675,"corporation":false,"usgs":true,"family":"Barton","given":"Cynthia","email":"cbarton@usgs.gov","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195790,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vowinkel, E. F.","contributorId":90737,"corporation":false,"usgs":true,"family":"Vowinkel","given":"E. F.","affiliations":[],"preferred":false,"id":195792,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nawyn, J. P.","contributorId":29016,"corporation":false,"usgs":true,"family":"Nawyn","given":"J. P.","affiliations":[],"preferred":false,"id":195791,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":12273,"text":"ofr87178 - 1987 - Rock geochemistry in the Mahd adh Dhahab district, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-07T14:03:37","indexId":"ofr87178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-178","title":"Rock geochemistry in the Mahd adh Dhahab district, Kingdom of Saudi Arabia","docAbstract":"<p>Ten sets of geochemical samples from country rock, altered country rock, and quartz veins were collected to determine metal abundances and distributions in the Mahd adh Dhahab district. Gold, silver, copper, lead, and zinc are present throughout the district in veins and altered country rock. Although four generations of quartz veins are defined, there is complete gradation between types. The metals present are the same in all four, only the abundances vary. The concentrations of gold, silver, copper, lead, and zinc in altered country rock are zoned around known or projected mineralized-vein zones. Similarities in metal populations of all quartz veins, altered rock, and mineralized zones, plus the distribution of metals and some major elements, suggest that all formed as part of a single hydrothermal system.</p>\n<p>Gold in abundances greater than 1 ppm does not correlate with any other element and its distribution is very erratic. The variance in gold values between replicate samples collected in 0.5 m square panels is very high. Radio-element analyses (radium-equivalent uranium, thorium, and potassium) for 40 widely distributed sample localities indicate little variation in these elements throughout the district. If the hydrothermal system had an effect on the distribution of these elements, the system must have extended beyond the limits of the sampled area.</p>\n<p>Anomalous values of gold, silver, lead, and to a lesser extent copper and zinc in surface rock samples clearly delineated the northern mineralized zone in the upper agglomerate, and an east-vein area and west-vein area of the southern mineralized zone in the lower agglomerate. A third geochemically anomalous area occurs farther to the west in the lower agglomerate, suggesting that mineralization may have extended at least to this area along the lower agglomerate-lower tuff contact, and possibly even further to the west.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr87178","usgsCitation":"Worl, R.G., Doebrich, J., Allen, M.S., Afifi, A., and Ebens, R., 1987, Rock geochemistry in the Mahd adh Dhahab district, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 87-178, iv, 59 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87178.","productDescription":"iv, 59 p. :ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":143168,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0178/report-thumb.jpg"},{"id":40451,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0178/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0178/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Saudi Arabia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              39,\n              20\n            ],\n            [\n              39,\n              27\n            ],\n            [\n              45,\n              27\n            ],\n            [\n              45,\n              20\n            ],\n            [\n              39,\n              20\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0fe4b07f02db5fe9fb","contributors":{"authors":[{"text":"Worl, R. G.","contributorId":13984,"corporation":false,"usgs":true,"family":"Worl","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":165724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doebrich, J. L. 0009-0009-3427-0985","orcid":"https://orcid.org/0009-0009-3427-0985","contributorId":61422,"corporation":false,"usgs":true,"family":"Doebrich","given":"J. L.","affiliations":[],"preferred":false,"id":165727,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allen, M. S.","contributorId":63001,"corporation":false,"usgs":true,"family":"Allen","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":165728,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Afifi, A.M.","contributorId":39375,"corporation":false,"usgs":true,"family":"Afifi","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":165725,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ebens, R.J.","contributorId":46952,"corporation":false,"usgs":true,"family":"Ebens","given":"R.J.","affiliations":[],"preferred":false,"id":165726,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":57057,"text":"b1674B - 1987 - A resource assessment of copper and nickel sulfides within the Mountain View area of the Stillwater Complex, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:12:03","indexId":"b1674B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"1674","chapter":"B","title":"A resource assessment of copper and nickel sulfides within the Mountain View area of the Stillwater Complex, Montana","language":"ENGLISH","doi":"10.3133/b1674B","usgsCitation":"Attanasi, E.D., and Bawiec, W., 1987, A resource assessment of copper and nickel sulfides within the Mountain View area of the Stillwater Complex, Montana: U.S. Geological Survey Bulletin 1674, p. B1-B27, https://doi.org/10.3133/b1674B.","productDescription":"p. B1-B27","costCenters":[],"links":[{"id":181870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1674b/report-thumb.jpg"},{"id":88233,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1674b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a83a5","contributors":{"authors":[{"text":"Attanasi, E. D. 0000-0001-6845-7160","orcid":"https://orcid.org/0000-0001-6845-7160","contributorId":107672,"corporation":false,"usgs":true,"family":"Attanasi","given":"E.","middleInitial":"D.","affiliations":[],"preferred":false,"id":256193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bawiec, W.J.","contributorId":71540,"corporation":false,"usgs":true,"family":"Bawiec","given":"W.J.","affiliations":[],"preferred":false,"id":256192,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40333,"text":"ofr87153 - 1987 - Comparison of multiple-year analyses of clay mineralogy of the Copper River system and the Gulf of Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr87153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-153","title":"Comparison of multiple-year analyses of clay mineralogy of the Copper River system and the Gulf of Alaska","language":"ENGLISH","doi":"10.3133/ofr87153","usgsCitation":"Luepke, G., Molnia, B.F., and Hein, J.R., 1987, Comparison of multiple-year analyses of clay mineralogy of the Copper River system and the Gulf of Alaska: U.S. Geological Survey Open-File Report 87-153, 5 maps on 1 sheet :photocopy ;59 x 27 cm. and smaller, sheet 99 x 108., https://doi.org/10.3133/ofr87153.","productDescription":"5 maps on 1 sheet :photocopy ;59 x 27 cm. and smaller, sheet 99 x 108.","costCenters":[],"links":[{"id":135439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":72778,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0153/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae22f","contributors":{"authors":[{"text":"Luepke, Gretchen","contributorId":91827,"corporation":false,"usgs":true,"family":"Luepke","given":"Gretchen","email":"","affiliations":[],"preferred":false,"id":223283,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Molnia, B. F.","contributorId":29386,"corporation":false,"usgs":true,"family":"Molnia","given":"B.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":223282,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hein, James R. 0000-0002-5321-899X jhein@usgs.gov","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":2828,"corporation":false,"usgs":true,"family":"Hein","given":"James","email":"jhein@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":223281,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013839,"text":"1013839 - 1987 - In situ striped bass (Morone saxatilis) contaminant and water quality studies in the Potomac River","interactions":[],"lastModifiedDate":"2023-03-03T19:26:20.780068","indexId":"1013839","displayToPublicDate":"1987-06-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":874,"text":"Aquatic Toxicology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"In situ striped bass (<i>Morone saxatilis</i>) contaminant and water quality studies in the Potomac River","title":"In situ striped bass (Morone saxatilis) contaminant and water quality studies in the Potomac River","docAbstract":"<p><span>The objectives of this study were to evaluate survival of striped bass (</span><i>Morone saxatilis</i><span>) prolarvae and yearlings in the Potomac River by using in situ test chambers; correlate survival of both striped bass life stages with the presence of water quality conditions, inorganic contaminants, and organic contaminants and conduct histological examinations of surviving yearling striped bass. Survival of striped bass prolarvae ranged from 4.5–22.5% at three field locations during three 96-h experiments; control survival was ≥81%. Yearling survival ranged from 0–77.5% at three river stations during two 7-d experiments; highest mortality occurred at the upriver station. Control survival was 100%. Poor survival of striped bass prolarvae was likely related to the presence of inorganic contaminants (monomeric aluminum, cadmium, and copper) acting singly or synergistically and sudden decreases in water temperature (&lt; 11°C). Yearling mortality at the upriver station was likely correlated with high pH conditions from a point source discharge and perhaps inorganic contaminants. Histological examinations of yearlings suggested that test organisms exposed to Potomac River water exhibited adverse changes in the kidney.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0166-445X(87)90016-6","usgsCitation":"Hall, L.W., Hall, W.S., Bushong, S.J., and Herman, R.L., 1987, In situ striped bass (Morone saxatilis) contaminant and water quality studies in the Potomac River: Aquatic Toxicology, v. 10, p. 73-99, https://doi.org/10.1016/0166-445X(87)90016-6.","productDescription":"27 p.","startPage":"73","endPage":"99","numberOfPages":"27","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132054,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland, Virginia","otherGeospatial":"Potomac River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77.35,\n              38.60009214319618\n            ],\n            [\n              -77.35,\n              38.4\n            ],\n            [\n              -77.20508958745842,\n              38.4\n            ],\n            [\n              -77.20508958745842,\n              38.60009214319618\n            ],\n            [\n              -77.35,\n              38.60009214319618\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5bc0","contributors":{"authors":[{"text":"Hall, L. W. Jr.","contributorId":6010,"corporation":false,"usgs":false,"family":"Hall","given":"L.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":319318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hall, W. S.","contributorId":14773,"corporation":false,"usgs":false,"family":"Hall","given":"W.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":319319,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bushong, S. J.","contributorId":71927,"corporation":false,"usgs":false,"family":"Bushong","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":319321,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Herman, Roger L.","contributorId":106184,"corporation":false,"usgs":true,"family":"Herman","given":"Roger","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319320,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70209769,"text":"70209769 - 1987 - Geology of the Mount St. Helens area: Record of discontinuous volcanic and plutonic activity in the Cascade Arc of southern Washington","interactions":[],"lastModifiedDate":"2020-04-24T19:03:36.749267","indexId":"70209769","displayToPublicDate":"1987-04-24T13:46:20","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Geology of the Mount St. Helens area: Record of discontinuous volcanic and plutonic activity in the Cascade Arc of southern Washington","docAbstract":"<p><span>The Quaternary edifice of Mount St. Helens volcano was built upon a deeply eroded terrane of gently folded and altered volcanic and plutonic rocks that represent the core of the Tertiary Cascade magmatic arc. These rocks constitute an east dipping homoclinal sequence, several kilometers thick, of subaerially erupted mafic to silicic flows and volcaniclastic strata; K‐Ar ages from this section range from about 28 to 23 Ma (late Oligocene and earliest Miocene), which corresponds to an apparent lull in Cascade volcanism to the north of Mount Rainier. Volcanism was essentially continuous during this period of time, and neither a well‐defined base nor top of the section is exposed within the mapped area. Basalt and basaltic andesite dominate the lower part of the mid‐Tertiary section, whereas andesitic and dacitic rocks comprise most of the upper part. This section was intruded by numerous mafic to silicic dikes, sills, and irregular plutonic bodies, most no more than a few million years younger than their host rocks, and subjected to pervasive burial metamorphism and widespread hydrothermal alteration. Large areas of hornfelsed rock surrounding even relatively small intrusions indicate that the proportion of plutonic rock becomes significantly greater at shallow depth beneath the existing erosion surface. A large granitic pluton intruded the mid‐Tertiary section north of Spirit Lake at about 21 Ma. The Earl porphyry copper deposit occurs within the pluton but appears too young (17 Ma) to be genetically related to it. In contrast to the rather continuous and voluminous Oligocene to early Miocene activity, volcanism since then in the Mount St. Helens area has been localized and Volumetrically minor. Products of three younger eruptive periods have been recognized: a sequence of 15 m.y. old pyroxene andesite flows resting unconformably on mid‐Tertiary strata south of Mount St. Helens, widespread shallow dikes and sills of pyroxene andesite between 10 and 8 m.y. old, and compositionally diverse rocks erupted during the past 3 m.y. The Quaternary lavas are more potassic than the Tertiary lavas and typically contain phenocrysts of hornblende and biotite, which are absent from the older rocks. A number of Tertiary structures define a broad NNE trending zone that may reflect a deep‐seated lithospheric flaw that has controlled the locus of Cascade magmatism in southern Washington for the past 25 m.y. Mount St. Helens lies within this zone at the intersection of the NNW striking St. Helens seismic zone (SHZ) and an ENE trending alignment of Pleistocene silicic plug‐domes. No surface breakage has been detected along the SHZ, which is apparently very young. The linear zone of silicic vents is probably controlled by a fault that has been interpreted from seismic records to occur directly beneath the volcano. This zone parallels the directions of regional maximum horizontal compressive stress and North America/Juan de Fuca plate convergence. Mount St. Helens is an example of a low‐volume tectonically controlled magmatic system in an early stage of development.</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/JB092iB10p10155","usgsCitation":"Evarts, R.C., Ashley, R.P., and Smith, J., 1987, Geology of the Mount St. Helens area: Record of discontinuous volcanic and plutonic activity in the Cascade Arc of southern Washington: Journal of Geophysical Research B: Solid Earth, v. 92, no. B10, p. 10155-10169, https://doi.org/10.1029/JB092iB10p10155.","productDescription":"15 p.","startPage":"10155","endPage":"10169","costCenters":[],"links":[{"id":374268,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.75048828124999,\n              47.15984001304432\n            ],\n            [\n              -122.56347656249999,\n              46.51351558059737\n            ],\n            [\n              -122.40966796874999,\n              46.01222384063236\n            ],\n            [\n              -121.75048828124999,\n              45.874712248904764\n            ],\n            [\n              -120.69580078125001,\n              46.800059446787316\n            ],\n            [\n              -120.673828125,\n              47.234489635299184\n            ],\n            [\n              -121.17919921875001,\n              47.264320080254805\n            ],\n            [\n              -121.75048828124999,\n              47.15984001304432\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"92","issue":"B10","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Evarts, Russell C. revarts@usgs.gov","contributorId":1974,"corporation":false,"usgs":true,"family":"Evarts","given":"Russell","email":"revarts@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":787936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ashley, Roger P. ashley@usgs.gov","contributorId":2749,"corporation":false,"usgs":true,"family":"Ashley","given":"Roger","email":"ashley@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":787937,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, J.G.","contributorId":224359,"corporation":false,"usgs":false,"family":"Smith","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":787938,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70198602,"text":"70198602 - 1987 - Inhibition of aqueous copper and lead adsorption onto goethite by dissolved carbonate species","interactions":[],"lastModifiedDate":"2018-08-13T10:25:00","indexId":"70198602","displayToPublicDate":"1987-01-01T09:59:07","publicationYear":"1987","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Inhibition of aqueous copper and lead adsorption onto goethite by dissolved carbonate species","docAbstract":"<p>No abstract available.&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Chemical quality of water and the hydrologic cycle","language":"English","publisher":"Lewis","publisherLocation":"Chlesea, Michigan","isbn":"0873710819","usgsCitation":"Smith, K.S., and Langmuir, D., 1987, Inhibition of aqueous copper and lead adsorption onto goethite by dissolved carbonate species, chap. <i>of</i> Chemical quality of water and the hydrologic cycle, p. 351-358.","productDescription":"8 p.","startPage":"351","endPage":"358","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":356377,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c113532e4b034bf6a8279a3","contributors":{"editors":[{"text":"Averett, R. C.","contributorId":35709,"corporation":false,"usgs":true,"family":"Averett","given":"R. C.","affiliations":[],"preferred":false,"id":742278,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"McKnight, D.M.","contributorId":189736,"corporation":false,"usgs":false,"family":"McKnight","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":742279,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Smith, Kathleen S. 0000-0001-8547-9804 ksmith@usgs.gov","orcid":"https://orcid.org/0000-0001-8547-9804","contributorId":182,"corporation":false,"usgs":true,"family":"Smith","given":"Kathleen","email":"ksmith@usgs.gov","middleInitial":"S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":742117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langmuir, D.","contributorId":87303,"corporation":false,"usgs":false,"family":"Langmuir","given":"D.","email":"","affiliations":[],"preferred":false,"id":742118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015719,"text":"70015719 - 1987 - Cadmium, copper, lead, and zinc determination in precipitation: A comparison of inductively coupled plasma atomic emission spectrometry and graphite furnace atomization atomic absorption spectrometry","interactions":[],"lastModifiedDate":"2012-03-12T17:18:54","indexId":"70015719","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2742,"text":"Mikrochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Cadmium, copper, lead, and zinc determination in precipitation: A comparison of inductively coupled plasma atomic emission spectrometry and graphite furnace atomization atomic absorption spectrometry","docAbstract":"Selected trace element analysis for cadmium, copper, lead, and zinc in precipitation samples by inductively coupled plasma atomic emission Spectrometry (ICP) and by atomic absorption spectrometry with graphite furnace atomization (AAGF) have been evaluated. This task was conducted in conjunction with a longterm study of precipitation chemistry at high altitude sites located in remote areas of the southwestern United States. Coefficients of variation and recovery values were determined for a standard reference water sample for all metals examined for both techniques. At concentration levels less than 10 micrograms per liter AAGF analyses exhibited better precision and accuracy than ICP. Both methods appear to offer the potential for cost-effective analysis of trace metal ions in precipitation. ?? 1987 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mikrochimica Acta","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF01196608","issn":"00263672","usgsCitation":"Reddy, M., Benefiel, M., and Claassen, H., 1987, Cadmium, copper, lead, and zinc determination in precipitation: A comparison of inductively coupled plasma atomic emission spectrometry and graphite furnace atomization atomic absorption spectrometry: Mikrochimica Acta, v. 88, no. 3-4, p. 159-170, https://doi.org/10.1007/BF01196608.","startPage":"159","endPage":"170","numberOfPages":"12","costCenters":[],"links":[{"id":205402,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01196608"},{"id":223679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f2efe4b0c8380cd4b4bd","contributors":{"authors":[{"text":"Reddy, M.M.","contributorId":24363,"corporation":false,"usgs":true,"family":"Reddy","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":371612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benefiel, M.A.","contributorId":56382,"corporation":false,"usgs":true,"family":"Benefiel","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":371613,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Claassen, H.C.","contributorId":74028,"corporation":false,"usgs":true,"family":"Claassen","given":"H.C.","affiliations":[],"preferred":false,"id":371614,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70014805,"text":"70014805 - 1987 - Petrogenesis of gabbronorite at Yakobi and northwest Chichagof Islands, Alaska","interactions":[],"lastModifiedDate":"2023-12-28T01:02:44.900089","indexId":"70014805","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","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":"Petrogenesis of gabbronorite at Yakobi and northwest Chichagof Islands, Alaska","docAbstract":"<p><span>On Yakobi Island and at Mirror Harbor on the northwest coast of Chichagof Island, gabbronorite occurs as irregular bodies, as much as 5.5 km in maximum dimension, mostly within a 40 to 43 m.y. composite pluton consisting largely of tonalite. The gab-bronorites are the host rocks for a magmatic nickel-copper sulfide deposit consisting predominantly of pyrrhotite, pentlandite, and chalcopyrite. The gabbronorites characteristically have more orthopyroxene than augite and have a significant amount of hornblende. Rock types mapped as gabbronorite range from hornblende pyroxenite to hornblende-pyroxene gabbronorite to quartz-bearing norite and gabbronorite. The tonalite pluton is composed of hornblende diorite, biotite-hornblende diorite, hornblende quartz diorite, biotite-hornblende tonalite, and biotite granodiorite. Contacts between types of gabbronorite are generally gradational on a scale of centimetres to metres; contacts between gabbronorite and the tonalite pluton are gradational on a scale of metres to tens of metres. Rock textures, pyroxene-hornblende relations, and rock and mineral chemistry of the gabbronorites show systematic changes as the gabbronorites grade into the tonalites. The field, petrographic, and chemical data, including trace-element abundances, of the gabbronorites and tonalite pluton rocks can best be explained by either (1) crystallization of gabbronorite from a tholeiitic magma with subsequent assimilation by tonalite that was simultaneously undergoing fractional crystallization or (2) fractional crystallization of a quartz diorite parent magma yielding the range of gabbronorites and tonalite pluton rocks.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1987)98<265:POGAYA>2.0.CO;2","usgsCitation":"Himmelberg, G.R., Loney, R.A., and Nabelek, P., 1987, Petrogenesis of gabbronorite at Yakobi and northwest Chichagof Islands, Alaska: Geological Society of America Bulletin, v. 98, no. 3, p. 265-279, https://doi.org/10.1130/0016-7606(1987)98<265:POGAYA>2.0.CO;2.","productDescription":"15 p.","startPage":"265","endPage":"279","numberOfPages":"15","costCenters":[],"links":[{"id":226042,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"98","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a777fe4b0c8380cd784ee","contributors":{"authors":[{"text":"Himmelberg, G. R.","contributorId":27106,"corporation":false,"usgs":true,"family":"Himmelberg","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":369338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loney, R. A.","contributorId":90757,"corporation":false,"usgs":true,"family":"Loney","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":369340,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nabelek, P.I.","contributorId":71315,"corporation":false,"usgs":true,"family":"Nabelek","given":"P.I.","email":"","affiliations":[],"preferred":false,"id":369339,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70014238,"text":"70014238 - 1987 - Suspended sediment and metals removal from urban runoff by a small lake","interactions":[],"lastModifiedDate":"2018-01-30T20:57:03","indexId":"70014238","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"Suspended sediment and metals removal from urban runoff by a small lake","docAbstract":"A small lake in the Chicago Metropolitan Area was from 91 to 95 percent efficient in removing suspended sediment and from 76 to 94 percent efficient in removing copper, iron, lead, and zinc from urban runoff. Sediments accumulated in the lake in the form of an organic-rich mud at an average rate of 20 millimeters per year; this reduced lake storage and covered potential habitat for aquatic organisms. Copper, lead, and zinc concentrations were closely associated with suspended-sediment concentrations and with silt- and clay-sized fractions of lake sediment. Although concentrations of mercury and cadmium were near detection limits in runoff, measurable concentrations of these metals accumulated in the lake sediments.A small lake in the Chicago Metropolitan Area was from 91 to 95 percent efficient in removing suspended sediment and from 76 to 94 percent efficient in removing copper, iron, lead, and zinc from urban runoff. Sediments accumulated in the lake in the form of an organic-rich mud at an average rate of 20 millimeters per year; this reduced lake storage and covered potential habitat for aquatic organisms. Copper, lead, and zinc concentrations were closely associated with suspended sediment concentrations and with silt- and clay-sized fractions of lake sediment. Although concentrations of mercury and cadmium were near detection limits in runoff, measurable concentrations of these metals accumulated in the lake sediments.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Resources Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Water Resources Association","doi":"10.1111/j.1752-1688.1987.tb00848.x","issn":"00431370","usgsCitation":"Striegl, R.G., 1987, Suspended sediment and metals removal from urban runoff by a small lake: Water Resources Bulletin, v. 23, no. 6, p. 985-996, https://doi.org/10.1111/j.1752-1688.1987.tb00848.x.","startPage":"985","endPage":"996","costCenters":[],"links":[{"id":225240,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267766,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.1987.tb00848.x"}],"volume":"23","issue":"6","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"505ba300e4b08c986b31faf4","contributors":{"authors":[{"text":"Striegl, Robert G. 0000-0002-8251-4659 rstriegl@usgs.gov","orcid":"https://orcid.org/0000-0002-8251-4659","contributorId":1630,"corporation":false,"usgs":true,"family":"Striegl","given":"Robert","email":"rstriegl@usgs.gov","middleInitial":"G.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true}],"preferred":false,"id":367918,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70014110,"text":"70014110 - 1987 - Structural reinterpretation of the Ajo mining district, Pima County, Arizona, based on paleomagnetic and geochronologic studies","interactions":[],"lastModifiedDate":"2024-01-05T17:59:50.084117","indexId":"70014110","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","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":"Structural reinterpretation of the Ajo mining district, Pima County, Arizona, based on paleomagnetic and geochronologic studies","docAbstract":"<p><span>The Ajo mining district of southern Arizona is divided into two main structural blocks by the Gibson Arroyo fault. The eastern Camelback Mountain block contains the Late Cretaceous-early Tertiary porphyry copper deposit which has been previously thought to be associated with the displaced apex of a large intrusion exposed by deeper erosion in the western Cardigan Peak block. However, unpublished U-Pb data support a mid-Tertiary age for the western intrusion. Paleomagnetic and geologic evidence indicates that the ore deposit has been tilted to the south a total of approximately 120 degrees : 68 degrees before and another 55 degrees after emplacement of the overlying Locomotive Fanglomerate and Ajo Volcanics. The Ajo Volcanics have K-Ar ages (24-25 m.y.) slightly older than those from the large intrusion of the Cardigan Peak block (20-23 m.y.). Paleomagnetic directions are consistent with the southward tilting of the volcanic rocks, but they suggest that the remanent magnetization and perhaps the K-Ar dates of the western intrusion were reset by the emplacement of dikes younger than the Locomotive Fanglomerate and Ajo Volcanics. These and other geologic relations indicate the following sequence of mid-Tertiary events in the district: (1) emplacement of the western intrusion, (2) movement along the Gibson Arroyo fault, (3) unroofing and perhaps tilting of the pluton [asymp] 70 degrees to the south along with the Camelback Mountain block, (4) syntectonic depositions of the Locomotive Fanglomerate and the Ajo Volcanics, (5) continued uplift and tilting to the south totaling 40 degrees to 60 degrees , (6) intrusion of the youngest dikes with attendant alteration and remagnetization of the host rocks, and (7) minor (?) oblique movement along the Gibson Arroyo fault.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.82.5.1348","issn":"03610128","usgsCitation":"Hagstrum, J., Cox, D.P., and Miller, R.J., 1987, Structural reinterpretation of the Ajo mining district, Pima County, Arizona, based on paleomagnetic and geochronologic studies: Economic Geology, v. 82, no. 5, p. 1348-1361, https://doi.org/10.2113/gsecongeo.82.5.1348.","productDescription":"14 p.","startPage":"1348","endPage":"1361","numberOfPages":"14","costCenters":[],"links":[{"id":226202,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","issue":"5","noUsgsAuthors":false,"publicationDate":"1987-08-01","publicationStatus":"PW","scienceBaseUri":"505b9c02e4b08c986b31d210","contributors":{"authors":[{"text":"Hagstrum, J.T.","contributorId":75922,"corporation":false,"usgs":true,"family":"Hagstrum","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":367605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cox, D. P.","contributorId":82689,"corporation":false,"usgs":true,"family":"Cox","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":367606,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, R. J.","contributorId":9225,"corporation":false,"usgs":true,"family":"Miller","given":"R.","middleInitial":"J.","affiliations":[],"preferred":false,"id":367604,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5222168,"text":"5222168 - 1987 - Environmental pollutant and necropsy data for ospreys from the eastern United States, 1975-1982","interactions":[],"lastModifiedDate":"2022-12-05T17:05:40.070542","indexId":"5222168","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Environmental pollutant and necropsy data for ospreys from the eastern United States, 1975-1982","docAbstract":"<p><span>Twenty-three ospreys (</span><i>Pandion haliaetus</i><span>) found dead or moribund in the eastern United States during 1975–1982 were necropsied and selected tissues were analyzed for organo-chlorines and metals. Major causes or factors contributing to death were trauma, impact injuries, and emaciation. DDE was detected in 96% of the osprey carcasses, DDD in 65%, DDT and heptachlor epoxide in 13%, dieldrin, oxychlordane, and&nbsp;</span><i>cis</i><span>-nonachlor in 35%,&nbsp;</span><i>cis</i><span>-chlordane in 52%,&nbsp;</span><i>trans</i><span>-nonachlor in 45%, and PCB's in 83%. Carcasses of immature ospreys from the Chesapeake Bay had significantly lower concentrations of DDE, DDD + DDT,&nbsp;</span><i>cis</i><span>-chlordane, and PCB's than carcasses of adults from the same area. Concentrations of some organochlorines in ospreys from the Chesapeake Bay declined significantly from 1971–1973 to 1975–1982. Significant differences in concentrations of certain metals in the ospreys' livers were noted between time periods, and sex and age groups for birds from the Chesapeake Bay. During 1975–1982, adults had significantly lower concentrations of chromium, copper, and arsenic than immatures and nestlings, and adult males had higher mercury concentrations than adult females. Adult females had lower zinc concentrations in 1975–1982 than in 1971–1973. Immatures and nestlings had higher concentrations of chromium and lead in 1975–1982 than in 1971–1973. A slightly elevated concentration of chromium (1.7 ppm) or arsenic (3.2 ppm) was found in the livers of individual ospreys. Several ospreys had elevated concentrations of mercury in their livers; two ospreys had more than 20 ppm which may have contributed to their deaths.</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-23.2.279","usgsCitation":"Wiemeyer, S.N., Schmeling, S.K., and Anderson, A., 1987, Environmental pollutant and necropsy data for ospreys from the eastern United States, 1975-1982: Journal of Wildlife Diseases, v. 23, no. 2, p. 279-291, https://doi.org/10.7589/0090-3558-23.2.279.","productDescription":"13 p.","startPage":"279","endPage":"291","numberOfPages":"13","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":480087,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-23.2.279","text":"Publisher Index Page"},{"id":198836,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Eastern United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.673828125,\n              36.38591277287651\n            ],\n            [\n              -74.8828125,\n              38.61687046392973\n            ],\n            [\n              -70.3125,\n              41.244772343082076\n            ],\n            [\n              -70.400390625,\n              42.74701217318067\n            ],\n            [\n              -66.533203125,\n              44.77793589631623\n            ],\n            [\n              -67.939453125,\n              46.49839225859763\n            ],\n            [\n              -69.345703125,\n              47.45780853075031\n            ],\n            [\n              -72.158203125,\n              45.521743896993634\n            ],\n            [\n              -77.783203125,\n              43.77109381775651\n            ],\n            [\n              -80.595703125,\n              42.032974332441405\n            ],\n            [\n              -81.123046875,\n              39.70718665682654\n            ],\n            [\n              -84.19921875,\n              38.61687046392973\n            ],\n            [\n              -82.08984375,\n              37.020098201368114\n            ],\n            [\n              -75.673828125,\n              36.38591277287651\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"23","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dc0a","contributors":{"authors":[{"text":"Wiemeyer, Stanley N.","contributorId":78279,"corporation":false,"usgs":true,"family":"Wiemeyer","given":"Stanley","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":335690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmeling, Shelia K.","contributorId":98673,"corporation":false,"usgs":false,"family":"Schmeling","given":"Shelia","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":335691,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, Allen","contributorId":167065,"corporation":false,"usgs":false,"family":"Anderson","given":"Allen","email":"","affiliations":[],"preferred":false,"id":335689,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2001203,"text":"2001203 - 1987 - Effects of contaminants on naiad mollusks (Unionidae): A review","interactions":[],"lastModifiedDate":"2019-11-13T14:24:27","indexId":"2001203","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"164","title":"Effects of contaminants on naiad mollusks (Unionidae): A review","docAbstract":"<p>Although the uptake, storage, and elimination of contaminants by naiad mollusks has been studied, relatively little information is available on toxicity. Contaminants appear to have destroyed some populations directly by exerting toxic effects, or indirectly by causing or contributing to the elimination of essential food organisms or host fish. The most frequently studied contaminants are Cd, Cu, Mn-Mn<sup>54</sup>, Pb-Pb<sup>210</sup>. and Zn-Zn<sup>65</sup>. Manganese seems to be most readily taken up and stored in tissues; no apparent damage has been reported from tissue concentrations of thousands of parts per million (ppm) and the element appears to be essential to metabolism. Zinc and cadmium also accumulate at high levels in tissues. Lead was never found to be lethal in the studies reviewed. Various common contaminants have been reported to be toxic at the following concentrations (ppm): cadmium. 2; copper sulfate, 2 to 18.7; ammonia, 5; potassium. 11; chromium, 12.4; arsenic trioxide, 16; copper, 19; and zinc, 66. In long-term exposures, concentrations of copper as low as 25 parts per billion (ppb) were lethal. Fry of fish infected with 20-35 glochidia were more sensitive than uninfected fish to toluene, naphthalene, and crude oil. Although few specific adverse impacts of contaminants have become clearly evident, circumstantial evidence leaves little doubt that contaminants have been responsible for decreases in population density, range, and diversity. Stresses that have been responsible for the disappearance of naiad mollusks in contaminated areas have not generally been identified, and the components of the stresses have seldom been quantitatively and qualitatively correlated with the composition and size of the naiad fauna. Often two or more factors appear to work in combination to produce the total stress that adversely affects populations. Naiad mollusks are important indicaters of contaminants in the environment; residues in soft tissue indicate recent or current exposure, and residues in shells indicate past exposure.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Havlik, M., and Marking, L.L., 1987, Effects of contaminants on naiad mollusks (Unionidae): A review: Resource Publication 164, ii, 20 p.","productDescription":"ii, 20 p.","numberOfPages":"20","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":197758,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":369175,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://fwslibrary.on.worldcat.org/oclc/15084166"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db616066","contributors":{"authors":[{"text":"Havlik, M.E.","contributorId":50490,"corporation":false,"usgs":true,"family":"Havlik","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":325557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marking, L. L.","contributorId":90661,"corporation":false,"usgs":true,"family":"Marking","given":"L.","middleInitial":"L.","affiliations":[],"preferred":false,"id":325558,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5222153,"text":"5222153 - 1986 - Reproductive success and heavy metal contamination in Rhode Island common terns","interactions":[],"lastModifiedDate":"2017-02-24T13:28:02","indexId":"5222153","displayToPublicDate":"2010-06-16T12:18:59","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1556,"text":"Environmental Pollution (Series A)","active":true,"publicationSubtype":{"id":10}},"title":"Reproductive success and heavy metal contamination in Rhode Island common terns","docAbstract":"Common tern cIutch size, reproductive success and growth of young recorded from an abandoned barge on the Providence River, an area of heavy metal contamination, were equal to, or greater than, .from less contaminated areas. Concentrations of copper and zinc were higher in livers of nestling terns from the Providence River than from other, less contaminated, areas. However, concentrations of magnesium, manganese, and iron and the frequency of nickel were equal, or lower, at Providence than other, less contaminated, locations. Among-colony trends in residues of copper, zinc and nickel in prey samples were similar to trends .found in nestling livers. Uric acid concentrations in nestling blood were twice as high in the Providence River than another colony and may have resulted from moderate levels of chromium in the diet.","language":"English","doi":"10.1016/0143-1471(86)90105-4","usgsCitation":"Custer, T., Franson, J.C., Moore, J.F., and Myers, J., 1986, Reproductive success and heavy metal contamination in Rhode Island common terns: Environmental Pollution (Series A), v. 41, no. 1, p. 33-52, https://doi.org/10.1016/0143-1471(86)90105-4.","productDescription":"20 p.","startPage":"33","endPage":"52","numberOfPages":"20","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true},{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":195947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b299","contributors":{"authors":[{"text":"Custer, T. W. 0000-0003-3170-6519","orcid":"https://orcid.org/0000-0003-3170-6519","contributorId":91802,"corporation":false,"usgs":true,"family":"Custer","given":"T. W.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":335656,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Franson, J. C. 0000-0002-0251-4238","orcid":"https://orcid.org/0000-0002-0251-4238","contributorId":99071,"corporation":false,"usgs":true,"family":"Franson","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":335658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, John F.","contributorId":30185,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":335655,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Myers, J.E.","contributorId":92770,"corporation":false,"usgs":true,"family":"Myers","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":335657,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":32606,"text":"pp1134E - 1986 - Geochemical variability of soils and biogeochemical variability of plants in the Piceance Basin, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:09:19","indexId":"pp1134E","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":"1134","chapter":"E","title":"Geochemical variability of soils and biogeochemical variability of plants in the Piceance Basin, Colorado","docAbstract":"Geochemical baselines for native soils and biogeochemical baselines for plants in the Piceance basin provide data that can be used to assess geochemical and biogeochemical effects of oil-shale development, monitor changes in the geochemical and biogeochemical environment during development, and assess the degree of success of rehabilitation of native materials after development. Baseline values for 52 properties in native soils, 15 properties in big sagebrush, and 13 properties in western wheatgrass were established. Our Study revealed statistically significant regional variations of the following properties across the basin: in soil&-aluminum, cobalt, copper, iron, manganese, sodium, nickel, phosphorus, lead, scandium, titanium, vanadium, zinc, organic and total carbon, pH, clay, dolomite, sodium feldspar, and DTPA-extractable calcium, cadmium, iron, potassium, manganese, nickel, phosphorus, yttrium, and zinc; in big sagebrush-barium, calcium, copper, magnesium, molybdenum, sodium, strontium, zinc, and ash; and in western wheatgrass-boron, barium, calcium, magnesium, manganese, molybdenum, strontium, zinc, and ash. These variations show up as north-south trends across the basin, or they reflect differences in elevation, hydrology, and soil parent material. Baseline values for properties that do not have statistically significant regional variations can be represented by geometric means and deviations calculated from all values within the basin. \r\n\r\nChemical and mineralogical analyses of soil and chemical analyses of western wheatgrass samples from Colorado State University's experimental revegetation plot at Anvil Points provide data useful in assessing potential effects on soil and plant properties when largescale revegetation operations begin. The concentrations of certain properties are related to the presence of topsoil over spent shale in the lysimeters. In soils, calcium, fluorine, lithium, magnesium, sodium, phosphorus, strontium, carbonate and total carbon, and DTPA-extractable boron, copper, iron, magnesium, and nickel have lower concentrations in topsoil than in the spent oil shale; whereas, silicon, titanium, ytterbium, clay, quartz, and DTPA-extractable potassium have greater concentrations in the topsoil than in the spent oil shale. In western wheatgrass, molybdenum has a lower concentration in grasses growing on the topsoil than in grasses on the spent oil shale; whereas, barium, calcium, manganese, strontium, zinc, and ash have greater concentrations in grasses growing on the topsoil than on the spent oil shale. When compared to baseline values, soils in the revegetation plot are significantly higher in concentrations of lead, zinc, organic and total carbon, and DTP A-extractable cadmium, iron, manganese, nickel, phosphorus, and zinc. Whereas, western wheatgrass grown within the revegetation plot has concentrations which fall within the baseline values established in the regional study. \r\n\r\nThe equations used in predicting concentrations of elements in plants from native and altered sites are cumbersome because of the large number of variables required to adequately predict expected concentrations and are of limited use because many explained only a small proportion of the total variation.","language":"ENGLISH","doi":"10.3133/pp1134E","usgsCitation":"Tuttle, M.L., Severson, R.C., Dean, W., and Klusman, R., 1986, Geochemical variability of soils and biogeochemical variability of plants in the Piceance Basin, Colorado: U.S. Geological Survey Professional Paper 1134, p. E1-E46, https://doi.org/10.3133/pp1134E.","productDescription":"p. E1-E46","costCenters":[],"links":[{"id":125089,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1134e/report-thumb.jpg"},{"id":60463,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1134e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6ab97e","contributors":{"authors":[{"text":"Tuttle, M. L.","contributorId":71992,"corporation":false,"usgs":true,"family":"Tuttle","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":208773,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Severson, R. C.","contributorId":46498,"corporation":false,"usgs":true,"family":"Severson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":208772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dean, W.E.","contributorId":97099,"corporation":false,"usgs":true,"family":"Dean","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":208775,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Klusman, R.W.","contributorId":93108,"corporation":false,"usgs":true,"family":"Klusman","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":208774,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":17045,"text":"ofr86408 - 1986 - Description and interpretation of geologic materials from shotholes drilled for the Trans-Alaska Crustal Transect project, Copper River basin, Alaska, May 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:07:13","indexId":"ofr86408","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":"86-408","title":"Description and interpretation of geologic materials from shotholes drilled for the Trans-Alaska Crustal Transect project, Copper River basin, Alaska, May 1985","docAbstract":"This map shows the potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, for May 1986. The Upper Floridan aquifer is the principal source of potable water in the area. Water level measurements were made on approximately 1,000 wells and on several springs. The potentiometric surface is shown mostly by 5-foot contour intervals. In the Fernandina Beach area of Nassau County, a 30-ft. interval is used to show a deep cone of depression. The potentiometric surface ranged from 125 feet above sea level in Polk County to 75 feet below sea level in Nassau County. Water levels in most key wells ranged from 1 to 9 feet below the May average in response to the lack of recharge from rainfall and an attendant increase in pumpage. Many levels in the district were equal to or lower than the below average levels of May 1985. Declines of about a foot from May 1985 levels were common in the eastern half of the district. However, the largest declines from May 1985 levels, as much as 7 to 9 feet, were mostly in well fields along the coastline. Levels in many wells approached, and in a few wells exceeded, record lows. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86408","usgsCitation":"Odum, J.K., Yehle, L., Schmoll, H., and Gilbert, C., 1986, Description and interpretation of geologic materials from shotholes drilled for the Trans-Alaska Crustal Transect project, Copper River basin, Alaska, May 1985: U.S. Geological Survey Open-File Report 86-408, i, 18 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr86408.","productDescription":"i, 18 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":149742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0408/report-thumb.jpg"},{"id":46184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0408/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f757e","contributors":{"authors":[{"text":"Odum, J. K.","contributorId":105705,"corporation":false,"usgs":true,"family":"Odum","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":174724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yehle, L. A.","contributorId":44536,"corporation":false,"usgs":true,"family":"Yehle","given":"L. A.","affiliations":[],"preferred":false,"id":174722,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schmoll, H. R.","contributorId":71543,"corporation":false,"usgs":true,"family":"Schmoll","given":"H. R.","affiliations":[],"preferred":false,"id":174723,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gilbert, Chuck","contributorId":13484,"corporation":false,"usgs":true,"family":"Gilbert","given":"Chuck","email":"","affiliations":[],"preferred":false,"id":174721,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":30245,"text":"wri844258 - 1986 - Quality of ground water in the Puget Sound region, Washington, 1981","interactions":[],"lastModifiedDate":"2022-10-17T20:54:41.24328","indexId":"wri844258","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":"84-4258","title":"Quality of ground water in the Puget Sound region, Washington, 1981","docAbstract":"<p>Groundwater from more than 100 sites in the Puget Sound region, Washington, was sampled and analyzed in 1981 for pH, specific conductance, and concentrations of fecal coliform bacteria, major ions, and dissolved iron, manganese, and nitrate. 20% of the samples were analyzed for concentrations of dissolved trace metals including aluminum, arsenic, barium, cadmium, chromium, copper, lead, mercury, selenium, silver, and zinc. The predominant water types were calcium bicarbonate and calcium-magnesium bicarbonate. Some wells in San Juan and Island Counties contained sodium chloride as a result of seawater intrusion. Dissolved solids concentrations were generally &lt; 150 mg/L. Iron concentrations &gt; 300 micrograms/L in 14% of all samples. Manganese concentrations &gt; 50 micrograms/L in 40% of all samples. Trace-metal concentrations were generally &lt; 10 mg/L , except for barium, copper, lead, and zinc. Nitrate concentrations were &lt; 1.0 mg/L in water for over 75% of the sites. Concentrations &gt; 1.0 mg/L in samples from Skagit, Whatcom , and Pierce Counties, were probably due to agricultural activities or septic tanks. Fecal coliform bacteria were detected in isolated instances. EPA drinking water regulations were exceeded only in isolated instances, except for widespread excessive iron and manganese concentrations. The historical data for the region were also evaluated for the same constituents. There are quantitative differences between historical and 1981 data, but they may be due to inconsistencies in data collection and analytical methods.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844258","usgsCitation":"Turney, G.L., 1986, Quality of ground water in the Puget Sound region, Washington, 1981: U.S. Geological Survey Water-Resources Investigations Report 84-4258, Report: v, 170 p.; 2 Plates: 45.03 × 27.49 inches and 45.24 × 27.60 inches, https://doi.org/10.3133/wri844258.","productDescription":"Report: v, 170 p.; 2 Plates: 45.03 × 27.49 inches and 45.24 × 27.60 inches","costCenters":[],"links":[{"id":59033,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4258/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":408435,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36104.htm","linkFileType":{"id":5,"text":"html"}},{"id":59032,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4258/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59034,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4258/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4258/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Puget Sound region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.733,\n              46.596\n            ],\n            [\n              -121,\n              46.596\n            ],\n            [\n              -121,\n              49\n            ],\n            [\n              -124.733,\n              49\n            ],\n            [\n              -124.733,\n              46.596\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624dd0","contributors":{"authors":[{"text":"Turney, G. L.","contributorId":95070,"corporation":false,"usgs":true,"family":"Turney","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":202924,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30244,"text":"wri854320 - 1986 - Quality of ground water in the Columbia Basin, Washington, 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri854320","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":"85-4320","title":"Quality of ground water in the Columbia Basin, Washington, 1983","docAbstract":"Groundwater from 188 sites in the Columbia Basin of central Washington was sampled and analyzed in 1983 for pH, specific conductance, and concentrations of fecal coliform bacteria, major dissolved ions, and dissolved iron, manganese, and nitrate. Twenty of the samples were also analyzed for concentrations of dissolved trace metals including aluminum, arsenic, barium, cadmium, chromium, copper, lead, mercury, selenium, silver, and zinc. The predominant water types were sodium bicarbonate and calcium bicarbonate. The sodium bicarbonate water samples had higher pH, fluoride, and sodium:adsorption ratio values than samples with other water types. Dissolved solids concentrations were generally between 250 and 500 mg/L. Iron and manganese concentrations were usually &lt; 10 micrograms/L (ug/L). Most trace metal concentrations were also &lt; 10 ug/L except for barium and zinc, which had maximum concentrations of 170 and 600 ug/L, respectively. Nitrate concentrations were &lt; 1.0 mg/L in water from more than half the wells sampled. Concentrations exceeded 1.0 mg/L in large areas of Lincoln, eastern Adams, Franklin and southern Grant Counties. No fecal coliform bacteria were detected. U.S. EPA drinking water regulations were exceeded in several samples, most commonly involving pH and concentrations of fluoride, nitrate, and dissolved solids in samples from Adams and Grant Counties. Generally, the historical data lead to similar conclusions about the quality of groundwater in the Columbia Basin region. However , historical samples had higher dissolved solids concentrations in Douglas County. Historical samples also included fewer sodium bicarbonate type waters in the region as a whole than the 1983 samples. These differences may be due to inconsistencies in data collection or analytical methods. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854320","usgsCitation":"Turney, G.L., 1986, Quality of ground water in the Columbia Basin, Washington, 1983: U.S. Geological Survey Water-Resources Investigations Report 85-4320, v, 172 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854320.","productDescription":"v, 172 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4320/report-thumb.jpg"},{"id":59026,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4320/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59027,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4320/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59028,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4320/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59029,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4320/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59030,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4320/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59031,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4320/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c043","contributors":{"authors":[{"text":"Turney, G. L.","contributorId":95070,"corporation":false,"usgs":true,"family":"Turney","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":202923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30243,"text":"wri844262 - 1986 - Quality of ground water in southeastern and south-central Washington, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri844262","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":"84-4262","title":"Quality of ground water in southeastern and south-central Washington, 1982","docAbstract":"In 1982 groundwater was sampled at over 100 sites in the southeastern-south central region of Washington and analyzed for pH, specific conductance, and concentrations of fecal-coliform bacteria, major dissolved irons, and dissolved iron, manganese, and nitrate. Twenty percent of the samples were analyzed for concentrations of dissolved aluminum, arsenic, barium, cadmium, chromium, cooper, lead, mercury, selenium, silver, and zinc. The predominant water type was calcium bicarbonate. Some sodium bicarbonate water was found in samples from the Lower Yakima, Horse Heaven Hills, and Walla Walla-Tucannon subregions. Dissolved solids concentrations were typically less than 500 mg/L (milligrams per liter). Median iron and manganese concentrations were less than 20 micrograms/L except in the Palouse subregion, where the median concentration of iron was 200 micrograms/L and the median concentrations of manganese was 45 micrograms/L. Generally, trace-metal concentrations were also less than 10 micrograms/L except for barium, copper, and zinc. Nitrate concentrations were less than 1.0 mg/L in waters from half the wells sampled. Concentrations greater than 5.0 mg/L were found in areas of the Lower Yakima, Walla Walla-Tucannon and Hanford subregions. No fecal-coliform bacteria were detected. U.S. Environmental Protection Agency drinking water regulation limits were generally not exceeded, except for occasional high concentrations of nitrate or dissolved solids. The historical data for the region were evaluated for these same constituents. Quantitative differences were found, but the historical and 1982 data led to similar qualitative conclusions. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844262","usgsCitation":"Turney, G.L., 1986, Quality of ground water in southeastern and south-central Washington, 1982: U.S. Geological Survey Water-Resources Investigations Report 84-4262, v, 158 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844262.","productDescription":"v, 158 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159823,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4262/report-thumb.jpg"},{"id":59020,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4262/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59021,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4262/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59022,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4262/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59023,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4262/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59024,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4262/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59025,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4262/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c012","contributors":{"authors":[{"text":"Turney, G. L.","contributorId":95070,"corporation":false,"usgs":true,"family":"Turney","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":202922,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66343,"text":"i1509C - 1986 - Geochemical map showing distribution of stream-sediment samples that contain anomalous concentrations of antimony, bismuth, cadmium, copper, lead, silver, and zinc in the Wallace 1° x 2° quadrangle, Montana and Idaho","interactions":[],"lastModifiedDate":"2021-10-22T20:52:05.723666","indexId":"i1509C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1509","chapter":"C","title":"Geochemical map showing distribution of stream-sediment samples that contain anomalous concentrations of antimony, bismuth, cadmium, copper, lead, silver, and zinc in the Wallace 1° x 2° quadrangle, Montana and Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1509C","usgsCitation":"Leach, D.L., and Hopkins, D., 1986, Geochemical map showing distribution of stream-sediment samples that contain anomalous concentrations of antimony, bismuth, cadmium, copper, lead, silver, and zinc in the Wallace 1° x 2° quadrangle, Montana and Idaho: U.S. Geological Survey IMAP 1509, Report: 6 p.;  Plates: 37.50 × 23.50 inches or smaller, https://doi.org/10.3133/i1509C.","productDescription":"Report: 6 p.;  Plates: 37.50 × 23.50 inches or smaller","costCenters":[],"links":[{"id":106779,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9276.htm","linkFileType":{"id":5,"text":"html"}},{"id":91551,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1509c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91550,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1509c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":188064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1509c/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Idaho, Montana","otherGeospatial":"Wallace 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116,47 ], [ -116,48 ], [ -114,48 ], [ -114,47 ], [ -116,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4865e4b07f02db506dc9","contributors":{"authors":[{"text":"Leach, D. L.","contributorId":18758,"corporation":false,"usgs":true,"family":"Leach","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":274378,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hopkins, D.M.","contributorId":103646,"corporation":false,"usgs":true,"family":"Hopkins","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":274379,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66344,"text":"i1509D - 1986 - Geochemical map showing distribution of stream-sediment samples that contain anomalous concentrations of partially-extractable antimony, bismuth, copper, lead, silver, and zinc in the Wallace 1° x 2° quadrangle, Montana and Idaho","interactions":[],"lastModifiedDate":"2021-10-22T20:55:06.649829","indexId":"i1509D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1509","chapter":"D","title":"Geochemical map showing distribution of stream-sediment samples that contain anomalous concentrations of partially-extractable antimony, bismuth, copper, lead, silver, and zinc in the Wallace 1° x 2° quadrangle, Montana and Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1509D","usgsCitation":"Leach, D.L., and Hopkins, D., 1986, Geochemical map showing distribution of stream-sediment samples that contain anomalous concentrations of partially-extractable antimony, bismuth, copper, lead, silver, and zinc in the Wallace 1° x 2° quadrangle, Montana and Idaho: U.S. Geological Survey IMAP 1509, Report: 6 p.; 1 Plate: 37.50 × 23.50 inches, https://doi.org/10.3133/i1509D.","productDescription":"Report: 6 p.; 1 Plate: 37.50 × 23.50 inches","costCenters":[],"links":[{"id":106780,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9277.htm","linkFileType":{"id":5,"text":"html"}},{"id":91553,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1509d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91552,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1509d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":188065,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1509d/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Idaho, Montana","otherGeospatial":"Wallace 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116,47 ], [ -116,48 ], [ -114,48 ], [ -114,47 ], [ -116,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486ae4b07f02db50a374","contributors":{"authors":[{"text":"Leach, D. L.","contributorId":18758,"corporation":false,"usgs":true,"family":"Leach","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":274380,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hopkins, D.M.","contributorId":103646,"corporation":false,"usgs":true,"family":"Hopkins","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":274381,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66342,"text":"i1509B - 1986 - Geochemical map showing distribution of samples of nonmagnetic heavy-mineral concentrates that contain anomalous concentrations of antimony, arsenic, copper, lead, silver, and zinc in the Wallace 1° x 2° quadrangle, Montana and Idaho","interactions":[],"lastModifiedDate":"2021-10-22T20:48:42.447509","indexId":"i1509B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1509","chapter":"B","title":"Geochemical map showing distribution of samples of nonmagnetic heavy-mineral concentrates that contain anomalous concentrations of antimony, arsenic, copper, lead, silver, and zinc in the Wallace 1° x 2° quadrangle, Montana and Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1509B","usgsCitation":"Leach, D.L., and Domenico, J.A., 1986, Geochemical map showing distribution of samples of nonmagnetic heavy-mineral concentrates that contain anomalous concentrations of antimony, arsenic, copper, lead, silver, and zinc in the Wallace 1° x 2° quadrangle, Montana and Idaho: U.S. Geological Survey IMAP 1509, Report: 6 p.; 1 Plate: 37.50 × 23.50 inches, https://doi.org/10.3133/i1509B.","productDescription":"Report: 6 p.; 1 Plate: 37.50 × 23.50 inches","costCenters":[],"links":[{"id":106778,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9275.htm","linkFileType":{"id":5,"text":"html"},"description":"9275"},{"id":91548,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1509b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91549,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1509b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":188063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1509b/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Idaho, Montana","otherGeospatial":"Wallace 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116,47 ], [ -116,48 ], [ -114,48 ], [ -114,47 ], [ -116,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e484ee4b07f02db4fc8bb","contributors":{"authors":[{"text":"Leach, D. L.","contributorId":18758,"corporation":false,"usgs":true,"family":"Leach","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":274377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Domenico, J. A.","contributorId":12028,"corporation":false,"usgs":true,"family":"Domenico","given":"J.","middleInitial":"A.","affiliations":[],"preferred":false,"id":274376,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66129,"text":"i1509F - 1986 - Resource appraisal map for stratabound copper-silver deposits in the Wallace 1° x 2° quadrangle, Montana and Idaho","interactions":[],"lastModifiedDate":"2021-10-12T19:19:47.258197","indexId":"i1509F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1509","chapter":"F","title":"Resource appraisal map for stratabound copper-silver deposits in the Wallace 1° x 2° quadrangle, Montana and Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1509F","usgsCitation":"Harrison, J.E., Domenico, J.A., and Leach, D.L., 1986, Resource appraisal map for stratabound copper-silver deposits in the Wallace 1° x 2° quadrangle, Montana and Idaho: U.S. Geological Survey IMAP 1509, Report: 4 p. ;  Plate: 40.50 × 23.50 inches, https://doi.org/10.3133/i1509F.","productDescription":"Report: 4 p. ;  Plate: 40.50 × 23.50 inches","costCenters":[],"links":[{"id":106782,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9279.htm","linkFileType":{"id":5,"text":"html"},"description":"9279"},{"id":91506,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1509f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91505,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1509f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":189605,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1509f/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Idaho, Montana","otherGeospatial":"Wallace 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116,47 ], [ -116,48 ], [ -114,48 ], [ -114,47 ], [ -116,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629dea","contributors":{"authors":[{"text":"Harrison, J. E.","contributorId":54532,"corporation":false,"usgs":true,"family":"Harrison","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":274021,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Domenico, J. A.","contributorId":12028,"corporation":false,"usgs":true,"family":"Domenico","given":"J.","middleInitial":"A.","affiliations":[],"preferred":false,"id":274019,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leach, D. L.","contributorId":18758,"corporation":false,"usgs":true,"family":"Leach","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":274020,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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