{"pageNumber":"4571","pageRowStart":"114250","pageSize":"25","recordCount":166004,"records":[{"id":70184472,"text":"70184472 - 1985 - Atlantic Flyway review: Region V: Laurel, Prince Georges County, MD (390-0765)","interactions":[{"subject":{"id":70184472,"text":"70184472 - 1985 - Atlantic Flyway review: Region V: Laurel, Prince Georges County, MD (390-0765)","indexId":"70184472","publicationYear":"1985","noYear":false,"title":"Atlantic Flyway review: Region V: Laurel, Prince Georges County, MD (390-0765)"},"predicate":"IS_PART_OF","object":{"id":5221999,"text":"5221999 - 1985 - Atlantic Flyway review: Region V","indexId":"5221999","publicationYear":"1985","noYear":false,"title":"Atlantic Flyway review: Region V"},"id":1}],"isPartOf":{"id":5221999,"text":"5221999 - 1985 - Atlantic Flyway review: Region V","indexId":"5221999","publicationYear":"1985","noYear":false,"title":"Atlantic Flyway review: Region V"},"lastModifiedDate":"2017-03-09T17:18:40","indexId":"70184472","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2881,"text":"North American Bird Bander","active":true,"publicationSubtype":{"id":10}},"title":"Atlantic Flyway review: Region V: Laurel, Prince Georges County, MD (390-0765)","docAbstract":"

My being away nearly all of September and on half the October weekends cut deeply into this season's banding. Totals for permanent residents and winter residents were close to normal, but numbers of the transient species are not at all comparable with other years. The only species that seemed more common than usual was the Northern Cardinal, for which my total of 28 was the second highest in ten years. The Veery and Common Yellowthroat were missed for the first time. I had only 36 returns, of 9 species. The oldest was a 5-year-old White-throated Sparrow. A Yellow Warbler was the 113th species and the 31st species of warbler banded at this station.

","language":"English","publisher":"Western, Inland, and Eastern Bird Banding Associations","usgsCitation":"Robbins, C.S., 1985, Atlantic Flyway review: Region V: Laurel, Prince Georges County, MD (390-0765): North American Bird Bander, v. 10, no. 2, p. 56-56.","productDescription":"1 p.","startPage":"56","endPage":"56","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":337269,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":337268,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.westernbirdbanding.org/nabb.html","text":"Journal's Website"}],"country":"United States","state":"Maryland","county":"Prince George's County","city":"Laurel","volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c277f9e4b014cc3a3e7708","contributors":{"authors":[{"text":"Robbins, Chandler S. crobbins@usgs.gov","contributorId":4275,"corporation":false,"usgs":true,"family":"Robbins","given":"Chandler","email":"crobbins@usgs.gov","middleInitial":"S.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":681633,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180829,"text":"70180829 - 1985 - A model for estimating deficits in the size of spawning stocks for spring Chinook salmon in tributaries of the upper Columbia River basin","interactions":[],"lastModifiedDate":"2017-02-03T14:10:20","indexId":"70180829","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"A model for estimating deficits in the size of spawning stocks for spring Chinook salmon in tributaries of the upper Columbia River basin","docAbstract":"

No abstract available 

","language":"English","publisher":"U.S. Fish and Wildlife Service ","publisherLocation":"Portland, OR","usgsCitation":"McIntyre, J., 1985, A model for estimating deficits in the size of spawning stocks for spring Chinook salmon in tributaries of the upper Columbia River basin.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334711,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d6e4b0fa1e59bc1ee3","contributors":{"authors":[{"text":"McIntyre, J.D.","contributorId":27006,"corporation":false,"usgs":true,"family":"McIntyre","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":662538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29669,"text":"wri844128 - 1985 - A conceptual ground-water-quality monitoring network for San Fernando Valley, California","interactions":[],"lastModifiedDate":"2023-04-06T18:23:59.479672","indexId":"wri844128","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4128","title":"A conceptual ground-water-quality monitoring network for San Fernando Valley, California","docAbstract":"

A conceptual groundwater-quality monitoring network was developed for San Fernando Valley to provide the California State Water Resources Control Board with an integrated, basinwide control system to monitor the quality of groundwater. The geology, occurrence and movement of groundwater, land use, background water quality, and potential sources of pollution were described and then considered in designing the conceptual monitoring network. The network was designed to monitor major known and potential point and nonpoint sources of groundwater contamination over time. The network is composed of 291 sites where wells are needed to define the groundwater quality. The ideal network includes four specific-purpose networks to monitor (1) ambient water quality, (2) nonpoint sources of pollution, (3) point sources of pollution, and (4) line sources of pollution. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844128","usgsCitation":"Setmire, J.G., 1985, A conceptual ground-water-quality monitoring network for San Fernando Valley, California: U.S. Geological Survey Water-Resources Investigations Report 84-4128, Report: iv, 49 p.; 6 Plates: 35.96 x 24.93 inches or smaller, https://doi.org/10.3133/wri844128.","productDescription":"Report: iv, 49 p.; 6 Plates: 35.96 x 24.93 inches or smaller","costCenters":[],"links":[{"id":415361,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36006.htm","linkFileType":{"id":5,"text":"html"}},{"id":58497,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4128/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58498,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4128/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58496,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4128/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58495,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4128/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58494,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4128/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58493,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4128/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58492,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4128/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122748,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4128/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Fernando Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -118.669,\n 34.375\n ],\n [\n -118.669,\n 34.083\n ],\n [\n -118.196,\n 34.083\n ],\n [\n -118.196,\n 34.375\n ],\n [\n -118.669,\n 34.375\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6b000d","contributors":{"authors":[{"text":"Setmire, J. G.","contributorId":16818,"corporation":false,"usgs":true,"family":"Setmire","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":201927,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28861,"text":"wri854055 - 1985 - Investigation of selected streamflow characteristics of the Alabama River upstream from Selma, Alabama","interactions":[],"lastModifiedDate":"2022-06-06T17:50:01.378241","indexId":"wri854055","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4055","title":"Investigation of selected streamflow characteristics of the Alabama River upstream from Selma, Alabama","docAbstract":"Available data for floods in the vicinity of Montgomery since the late 1800 's indicate that the flood of 1886 is the highest since settlement of the area in 1814. Profiles for floods in 1948, 1961, 1976, and 1979 were defined using floodmarks and recorded peak stages at gaging stations at Selma and Montgomery. The floods in 1948 and 1961 occurred before construction of Robert F. Henry Lock and Dam (formerly Jones Bluff Lock and Dam and Millers Ferry Lock and Dam). Considerable water-surface differences are indicated between the profiles for periods before and after construction of the dams. The investigation included a step-backwater model to reproduce profiles based on the actual flood profiles. After the actual flood profiles were reproduced, the model was used to compute additional profiles showing the effects of varying tributary inflow. The profiles were computed for discharges ranging from 80,000 ft3/s to 500 ,000 ft3/s. Stage-discharge relations were then developed for five sites upstream from Selma. Discharge coefficient curves for prevalent types of flow over the spillway at Robert F. Henry Lock and Dam were developed using discharges obtained from current-meter measurements and standard discharge equations for flow through gate-controlled spillways. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854055","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers, Mobile District","usgsCitation":"Nelson, G.H., Ming, C.O., and Psinakis, W.L., 1985, Investigation of selected streamflow characteristics of the Alabama River upstream from Selma, Alabama: U.S. Geological Survey Water-Resources Investigations Report 85-4055, vi, 44 p., https://doi.org/10.3133/wri854055.","productDescription":"vi, 44 p.","costCenters":[],"links":[{"id":401757,"rank":6,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4055/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57740,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4055/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57739,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4055/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57737,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4055/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159334,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4055/report-thumb.jpg"},{"id":57738,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4055/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alabama","city":"Selma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.154541015625,\n 32.22906629627297\n ],\n [\n -86.22894287109375,\n 32.22906629627297\n ],\n [\n -86.22894287109375,\n 32.51207789841144\n ],\n [\n -87.154541015625,\n 32.51207789841144\n ],\n [\n -87.154541015625,\n 32.22906629627297\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4783e4b07f02db483979","contributors":{"authors":[{"text":"Nelson, G. H. Jr.","contributorId":23562,"corporation":false,"usgs":true,"family":"Nelson","given":"G.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":200521,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ming, C. O.","contributorId":9266,"corporation":false,"usgs":true,"family":"Ming","given":"C.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":200520,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Psinakis, W. L.","contributorId":104074,"corporation":false,"usgs":true,"family":"Psinakis","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200522,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28827,"text":"wri844190 - 1985 - Geohydrology of the aquifer in the Santa Fe Group, northern West Mesa of the Mesilla Basin near Las Cruces, New Mexico","interactions":[],"lastModifiedDate":"2023-03-23T20:08:00.059709","indexId":"wri844190","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4190","title":"Geohydrology of the aquifer in the Santa Fe Group, northern West Mesa of the Mesilla Basin near Las Cruces, New Mexico","docAbstract":"

Because of the heterogeneity of the Santa Fe Group, New Mexico, the hydrologic characteristics of the aquifer vary substantially from place to place. Hydraulic conductivities of 12 and 30 feet per day were estimated from aquifer tests for two wells in the eastern one-half of the study area. Well yields in the western one-half of the study area generally are less than 5 gallons per minute. Some of the well yields in the eastern one-half of the study area are greater than 1,000 gallons per minute. Ground water flows southeastward across the western one-half of the study area at a gradient of about 50 feet per mile. Across the eastern one-half of the study area, ground water flows southeastward at a gradient of less than 5 feet per mile. Dissolved-solids concentrations in groundwater range from 906 to 1,470 milligrams per liter in the western one-half of the study area and from 378 to 556 milligrams per liter in the eastern one-half. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844190","usgsCitation":"Myers, R.G., and Orr, B.R., 1985, Geohydrology of the aquifer in the Santa Fe Group, northern West Mesa of the Mesilla Basin near Las Cruces, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 84-4190, v, 37 p., https://doi.org/10.3133/wri844190.","productDescription":"v, 37 p.","costCenters":[],"links":[{"id":414655,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36053.htm","linkFileType":{"id":5,"text":"html"}},{"id":57687,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4190/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123396,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4190/report-thumb.jpg"}],"country":"United States","state":"New Mexico","city":"Las Cruces","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -106.83843928636912,\n 32.292037090742866\n ],\n [\n -107.03898267215521,\n 32.292037090742866\n ],\n [\n -107.03898267215521,\n 32.093231573912306\n ],\n [\n -106.83843928636912,\n 32.093231573912306\n ],\n [\n -106.83843928636912,\n 32.292037090742866\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a888c","contributors":{"authors":[{"text":"Myers, R. G.","contributorId":30642,"corporation":false,"usgs":true,"family":"Myers","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":200468,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Orr, B. R.","contributorId":46545,"corporation":false,"usgs":true,"family":"Orr","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":200469,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30582,"text":"wri854292 - 1985 - Limnology of nine small lakes, Matanuska-Susitna Borough, Alaska, and the survival and growth rates of rainbow trout","interactions":[],"lastModifiedDate":"2023-03-14T21:16:27.755353","indexId":"wri854292","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4292","title":"Limnology of nine small lakes, Matanuska-Susitna Borough, Alaska, and the survival and growth rates of rainbow trout","docAbstract":"

The survival and growth rates of rainbow trout (Salmo gairdnieri) were concurrently measured with selected limnological characteristics in nine small (surface area < 25 sq hectometers) lakes in the Matanuska-Susitna Borough. The project goal was to develop empirical models for predicting rainbow trout growth rates from the following variables: total phosphorus concentration, chlorophyll a concentration, Secchi disc transparency, or the morphoedaphic index--a means of characterizing potential biological productivity. No suitable model could be developed from the data collected during 1982 and 1983. The lack of significant correlation was attributed in part to the wide variation in survival of rainbow trout. Winterkills, caused by severe depletion of dissolved oxygen, were suspected in four of the lakes. Varied levels of fishing pressure and competition with threespine stickleback (Gasterosteus aculeatus) also influenced survival of rainbow trout but their effects were overshadowed by winterkill. Predictive capability was also reduced because of inconsistencies in rankings generated by each of the four limnological variables chosen as indicators of potential biological productivity. A lake ranked low in productivity by one variable was commonly ranked high in productivity by another variable. The survivability of rainbow trout stocked in lakes such as these nine may be a more important indicator of potential biomass production than are indicators of lake fertility. Assessments of a lake 's susceptibility to winterkill and the degree of competition with threespine stickleback are suggested as important topics for additional research. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854292","usgsCitation":"Woods, P.F., 1985, Limnology of nine small lakes, Matanuska-Susitna Borough, Alaska, and the survival and growth rates of rainbow trout: U.S. Geological Survey Water-Resources Investigations Report 85-4292, iv, 32 p., https://doi.org/10.3133/wri854292.","productDescription":"iv, 32 p.","costCenters":[],"links":[{"id":414141,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36430.htm","linkFileType":{"id":5,"text":"html"}},{"id":59341,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4292/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123988,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4292/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Matanuska-Susitna Borough, Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -149.817,\n 61.833\n ],\n [\n -149.817,\n 61.45\n ],\n [\n -148.267,\n 61.45\n ],\n [\n -148.267,\n 61.833\n ],\n [\n -149.817,\n 61.833\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a50f9","contributors":{"authors":[{"text":"Woods, P. F.","contributorId":97509,"corporation":false,"usgs":true,"family":"Woods","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":203490,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29912,"text":"wri854087 - 1985 - Ground-water flow in the Prairie du Chien-Jordan aquifer related to contamination by coal-tar derivatives, St. Louis Park, Minnesota","interactions":[],"lastModifiedDate":"2023-03-13T19:17:59.193897","indexId":"wri854087","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4087","title":"Ground-water flow in the Prairie du Chien-Jordan aquifer related to contamination by coal-tar derivatives, St. Louis Park, Minnesota","docAbstract":"

A three-dimensional, ground-water-flow model of the Prairie du Chien-Jordan aquifer and associated hydrogeologic units was developed to evaluate the movement of coal-tar derivatives from a coal-tar distillation and wood-preserving plant in St. Louis Park, Minnesota. A finite-difference grid was superimposed on the modeled area, which includes most of eastern Hennepin County. The individual cells are 400-foot squares in the center of the grid (St. Louis Park area); the cells increase in dimension toward the outside limits of the grid. Five geologic units are represented by four layers in the model. These units include the Jordan Sandstone, the Prairie du Chien Group (dolomite and sandy dolomite), the basal confining unit of the St. Peter Sandstone (silty and sandy shale), the St. Peter Sandstone, and glacial deposits in bedrock valleys.

The model was calibrated for steady-state conditions for a period before significant ground-water development (1885-1930) and for a period of significant pumping stress (winter conditions, 1970 fs). A transient calibration was accomplished by simulation of a period during which seasonal changes in potentiometric head in the Prairie du Chien-Jordan aquifer were significant (1977-80). Sensitivity testing indicated that leakage to the upper model layer and the vertical hydraulic conductivity of the basal confining unit of the St. Peter Sandstone were the model hydrologic properties which, when changed, resulted in the greatest changes in model-calculated water levels. The calibrated model generally calculates water levels that are within 10 feet of measured values.

Model simulations indicate that the potentiometric surface of the Prairie du Chien-Jordan aquifer would be raised by as much as 3 feet in the area of the plant site by water introduced into the aquifer through wells open to more than one aquifer system. The cones of impression created at these wells could have a significant impact on the transport of contaminants in the Prairie du Chien-Jordan.

The presence of coal-tar derivatives in the aquifer has been difficult to explain in wells located upgradient from the plant site to the north, west, and southwest. Simulations suggest that, during periods of heavy withdrawal from certain of these wells (SLP10, SLP15, and SLP5), local hydraulic gradients may have been altered, resulting in the potential for the movement of contaminants from the area of the plant site to the wells. Cones of impression at multiaquifer wells near the plant site contributed to the alteration of local gradients.

Simulation of a proposed gradient-control plan, in which lateral homogeneity and isotropy of individual hydro geologic units was assumed, indicates that the actions would be effective in limiting expansion of the contaminated volume in the Prairie du Chien-Jordan aquifer. The plan includes the control of withdrawal from five wells. The simulations also show, however, that modelcalculated potentiometric surfaces are sensitive to changes in withdrawal rates at wells not intended to be under the control of the plan. Management of discharge from these wells also will be important to overall effectiveness of the remedial-action plan.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri854087","usgsCitation":"Stark, J., and Hult, M.F., 1985, Ground-water flow in the Prairie du Chien-Jordan aquifer related to contamination by coal-tar derivatives, St. Louis Park, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 85-4087, v, 57 p., https://doi.org/10.3133/wri854087.","productDescription":"v, 57 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":414036,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36260.htm","linkFileType":{"id":5,"text":"html"}},{"id":119515,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4087/report-thumb.jpg"},{"id":58730,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4087/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","city":"St. Louis Park","otherGeospatial":"Prairie du Chien-Jordan aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -93.167,\n 45.083\n ],\n [\n -93.583,\n 45.083\n ],\n [\n -93.583,\n 44.783\n ],\n [\n -93.167,\n 44.783\n ],\n [\n -93.167,\n 45.083\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cd74","contributors":{"authors":[{"text":"Stark, J. R.","contributorId":100406,"corporation":false,"usgs":true,"family":"Stark","given":"J. R.","affiliations":[],"preferred":false,"id":202343,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hult, M. F.","contributorId":29817,"corporation":false,"usgs":true,"family":"Hult","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":202342,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25586,"text":"wri854183 - 1985 - Hydrologic and geochemical monitoring in Long Valley caldera, Mono County, California, 1982-1984","interactions":[],"lastModifiedDate":"2023-04-13T20:24:01.164925","indexId":"wri854183","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4183","title":"Hydrologic and geochemical monitoring in Long Valley caldera, Mono County, California, 1982-1984","docAbstract":"

The Long Valley caldera is a potentially active volcanic area on the eastern side of the Sierra Nevada in east-central California. Hydrologic and geochemical monitoring of surface and subsurface features began in July 1982 to determine if changes were occurring in response to processes causing earthquakes and crustal deformation. Differences since 1982 in fluid chemistry of springs has been minor except at Casa Diablo, where rapid fluctuations in chemistry result from near surface boiling and mixing. Ratios of 3He/4He and 13C/12C in hot springs and fumaroles are consistent with a magnetic source for some of the carbon and helium discharged in thermal areas, and observed changes in 3He/4He between 1978 and 1984 suggest changes in the magmatic component. Significant fluctuations in hot spring discharge recorded at several sites since 1982 closely followed earthquake activity.

Water levels in wells have been used as strain meters to detect rock deformation associated with magmatic and tectonic activity and to construct a water table contour map. Coseismic water level fluctuations of as much as 0.6 ft have been observed but no clear evidence of deformation caused by magmatic intrusions can be seen in the well records through 1984. Temperature profiles in wells, which can be used to delineate regionally continuous zones of lateral flow of hot water across parts of the caldera, have remained constant at all but two sites. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854183","usgsCitation":"Farrar, C.D., Sorey, M., Rojstaczer, S., Janik, C.J., Mariner, R.H., Winnett, T.L., and Clark, M.D., 1985, Hydrologic and geochemical monitoring in Long Valley caldera, Mono County, California, 1982-1984: U.S. Geological Survey Water-Resources Investigations Report 85-4183, Report: ix, 137 p.; 2 Plates: 30.75 x 21.36 inches and 30.63 x 21.71 inches, https://doi.org/10.3133/wri854183.","productDescription":"Report: ix, 137 p.; 2 Plates: 30.75 x 21.36 inches and 30.63 x 21.71 inches","costCenters":[],"links":[{"id":415732,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36337.htm","linkFileType":{"id":5,"text":"html"}},{"id":123638,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4183/report-thumb.jpg"},{"id":54328,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4183/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54326,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4183/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54327,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4183/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Mono County","otherGeospatial":"Long Valley caldera","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.079,\n 37.767\n ],\n [\n -119.079,\n 37.583\n ],\n [\n -118.645,\n 37.583\n ],\n [\n -118.645,\n 37.767\n ],\n [\n -119.079,\n 37.767\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683c71","contributors":{"authors":[{"text":"Farrar, C. D.","contributorId":71978,"corporation":false,"usgs":true,"family":"Farrar","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":194301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":194302,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rojstaczer, S.","contributorId":92709,"corporation":false,"usgs":true,"family":"Rojstaczer","given":"S.","email":"","affiliations":[],"preferred":false,"id":194304,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Janik, C. J.","contributorId":10795,"corporation":false,"usgs":true,"family":"Janik","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":194298,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mariner, Robert H.","contributorId":81075,"corporation":false,"usgs":true,"family":"Mariner","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":194303,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Winnett, T. L.","contributorId":27095,"corporation":false,"usgs":true,"family":"Winnett","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":194300,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Clark, M. D.","contributorId":25202,"corporation":false,"usgs":true,"family":"Clark","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":194299,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":26386,"text":"wri854010 - 1985 - Ground-water problems in Arkansas","interactions":[],"lastModifiedDate":"2023-04-11T20:56:55.59043","indexId":"wri854010","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4010","title":"Ground-water problems in Arkansas","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854010","usgsCitation":"Bryant, C.T., Ludwig, A.H., and Morris, E.E., 1985, Ground-water problems in Arkansas: U.S. Geological Survey Water-Resources Investigations Report 85-4010, Report: iv, 24 p.; 4 Plates: 15.58 x 10.06 inches or smaller, https://doi.org/10.3133/wri854010.","productDescription":"Report: iv, 24 p.; 4 Plates: 15.58 x 10.06 inches or smaller","costCenters":[],"links":[{"id":55178,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4010/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55176,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4010/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55175,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4010/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55179,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4010/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":415604,"rank":7,"type":{"id":36,"text":"NGMDB Index 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66062e","contributors":{"authors":[{"text":"Bryant, C. T.","contributorId":7263,"corporation":false,"usgs":true,"family":"Bryant","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":196296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ludwig, A. H.","contributorId":63007,"corporation":false,"usgs":true,"family":"Ludwig","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":196297,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morris, E. E.","contributorId":93493,"corporation":false,"usgs":true,"family":"Morris","given":"E.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":196298,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26047,"text":"wri854169 - 1985 - Major and trace-element analyses of acid mine waters in the Leviathan Mine drainage basin, California/Nevada; October, 1981 to October, 1982","interactions":[],"lastModifiedDate":"2023-04-17T19:47:15.067137","indexId":"wri854169","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4169","title":"Major and trace-element analyses of acid mine waters in the Leviathan Mine drainage basin, California/Nevada; October, 1981 to October, 1982","docAbstract":"

Water issuing from the inactive Leviathan open-pit sulfur mine has caused serious degradation of the water quality in the Leviathan/Bryant Creek drainage basin which drains into the East Fork of the Carson River. As part of a pollution abatement project of the California Regional Water Quality Control Board, the U.S. Geological Survey collected hydrologic and water quality data for the basin during 1981-82. During this period a comprehensive sampling survey was completed to provide information on trace metal attenuation during downstream transport and to provide data for interpreting geochemical processes. This report presents the analytical results from this sampling survey. Sixty-seven water samples were filtered and preserved on-site at 45 locations and at 3 different times. Temperature, discharge, pH, and Eh and specific conductance were measured on-site. Concentrations of 37 major and trace constituents were determined later in the laboratory on preserved samples. The quality of the analyses was checked by using two or more techniques to determine the concentrations including d.c.-argon plasma emission spectrometry (DCP), flame and flameless atomic absorption spectrophotometry, UV-visible spectrophotometry, hydride-generation atomic absorption spectrophotometry and ion chromatography. Additional quality control was obtained by comparing measured to calculated conductance, comparing measured to calculated Eh (from Fe-2 +/Fe-3+ determinations), charge balance calculations and mass balance calculations for conservative constituents at confluence points. Leviathan acid mine waters contain mg/L concentrations of As, Cr, Co, Cu, Mn, Ni, T1, V and Zn, and hundreds to thousands of mg/L concentrations of Al, Fe, and sulfate at pH values as low as 1.8. Other elements including Ba, B, Be, Bi, Cd , Mo, Sb, Se and Te are elevated above normal background concentrations and fall in the microgram/L range. The chemical and 34 S/32 S isotopic analyses demonstrate that these acid waters are derived from pyrite oxidation and not from the oxidation of elemental sulfur. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854169","usgsCitation":"Ball, J., and Nordstrom, D.K., 1985, Major and trace-element analyses of acid mine waters in the Leviathan Mine drainage basin, California/Nevada; October, 1981 to October, 1982: U.S. Geological Survey Water-Resources Investigations Report 85-4169, v, 46 p., https://doi.org/10.3133/wri854169.","productDescription":"v, 46 p.","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":415876,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36324.htm","linkFileType":{"id":5,"text":"html"}},{"id":54824,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4169/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123446,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4169/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Leviathan Mine drainage basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.722,\n 38.828\n ],\n [\n -119.722,\n 38.669\n ],\n [\n -119.583,\n 38.669\n ],\n [\n -119.583,\n 38.828\n ],\n [\n -119.722,\n 38.828\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649741","contributors":{"authors":[{"text":"Ball, J.W.","contributorId":67507,"corporation":false,"usgs":true,"family":"Ball","given":"J.W.","affiliations":[],"preferred":false,"id":195709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":195710,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25517,"text":"wri844192 - 1985 - Geochemical processes in the Gascoyne Lignite Mining Area, Bowman County, North Dakota","interactions":[],"lastModifiedDate":"2017-07-18T12:53:53","indexId":"wri844192","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4192","title":"Geochemical processes in the Gascoyne Lignite Mining Area, Bowman County, North Dakota","docAbstract":"

Notice

The publication has been withdrawn because it contained errors or contained information that could not be verified for accuracy.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844192","collaboration":"The publication has been withdrawn because it contained errors or contained information that could not be verified for accuracy.","usgsCitation":"Fisher, D.W., Thorstenson, D.C., Croft, M.G., and Houghton, R.L., 1985, Geochemical processes in the Gascoyne Lignite Mining Area, Bowman County, North Dakota: U.S. Geological Survey Water-Resources Investigations Report 84-4192, v, 80 p., https://doi.org/10.3133/wri844192.","productDescription":"v, 80 p.","costCenters":[],"links":[{"id":343981,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf01","contributors":{"authors":[{"text":"Fisher, D. W.","contributorId":127082,"corporation":false,"usgs":true,"family":"Fisher","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":522983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thorstenson, D. C.","contributorId":127190,"corporation":false,"usgs":true,"family":"Thorstenson","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":522984,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Croft, M. G.","contributorId":127310,"corporation":false,"usgs":true,"family":"Croft","given":"M.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":522986,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Houghton, R. L.","contributorId":127282,"corporation":false,"usgs":true,"family":"Houghton","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":522985,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":28183,"text":"wri854039 - 1985 - Water quality in the Blue Creek arm of Lake Eufaula and Blue Creek, Oklahoma, March-October 1978","interactions":[],"lastModifiedDate":"2023-04-05T20:14:39.064405","indexId":"wri854039","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4039","title":"Water quality in the Blue Creek arm of Lake Eufaula and Blue Creek, Oklahoma, March-October 1978","docAbstract":"Based on samples collected bimonthly for major inorganic and trace elements and monthly for biota and bacteria, water from the Blue Creek arm of Lake Eufaula and Blue Creek is suitable for most uses when compared to water-quality standards or criteria. Concentrations of most chemical constituents gradually increased from spring to fall. The concentrations generally were within established drinking-water standards, with the exception of iron and manganese.\r\nUsing water-quality determinations and biologic indicators, the water from Blue Creek arm of Lake Eufaula and Blue Creek is: (1) Soft and acidic with little mineral content and conductivity; (2) calm or very slowly moving; and (3) warm and enriched with organic matter.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854039","usgsCitation":"Kurklin, J., 1985, Water quality in the Blue Creek arm of Lake Eufaula and Blue Creek, Oklahoma, March-October 1978: U.S. Geological Survey Water-Resources Investigations Report 85-4039, v, 91 p., https://doi.org/10.3133/wri854039.","productDescription":"v, 91 p.","costCenters":[],"links":[{"id":415295,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36223.htm","linkFileType":{"id":5,"text":"html"}},{"id":57021,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4039/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159239,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4039/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Blue Creek, Lake Eufaula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -95.64,\n 35.083\n ],\n [\n -95.64,\n 35\n ],\n [\n -95.539,\n 35\n ],\n [\n -95.539,\n 35.083\n ],\n [\n -95.64,\n 35.083\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9ae5","contributors":{"authors":[{"text":"Kurklin, J. K.","contributorId":59032,"corporation":false,"usgs":true,"family":"Kurklin","given":"J. K.","affiliations":[],"preferred":false,"id":199348,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27238,"text":"wri844348 - 1985 - Effects of increased pumpage on a fractured-bedrock aquifer system in central Orange County, New York","interactions":[],"lastModifiedDate":"2023-04-07T20:39:49.294109","indexId":"wri844348","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4348","title":"Effects of increased pumpage on a fractured-bedrock aquifer system in central Orange County, New York","docAbstract":"

The bedrock in central Orange County consists of highly indurated siltstone, shale, and conglomerate containing two major fault systems and extensive fracturing; it is overlain by 50 to 100 feet of till. The fracturing permits unusually high well yields. Wells tapping the bedrock yield 75 to 200 gallons per minute; those tapping bedrock in adjacent areas yield only a few tens of gallons per minute. The bedrock aquifer is recharged mainly by percolation of water from precipitation through the till. In 1983, the U.S. Geological Survey studied the hydrologic effects of increased pumpage on the fractured bedrock aquifer system near the Village of Kiryas Joel, in the Town of Monroe. Water levels were measured in several wells in the village 's two well fields from February to October 1983, and pumpage data from the same period were tabulated. Water levels responded to variations in both pumpage and precipitation. Pumping tests and water levels in the southeastern well field in 1983 had no effect on the northwestern well field. An observation well between the two fields shows about 20 feet of seasonal fluctuation from recharge and the effects of pumping at the northwestern well field. Aquifer-test data indicate a transmissivity of 900 feet squared per day and a storage coefficient of 0.0001. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844348","usgsCitation":"Garber, M., 1985, Effects of increased pumpage on a fractured-bedrock aquifer system in central Orange County, New York: U.S. Geological Survey Water-Resources Investigations Report 84-4348, v, 27 p., https://doi.org/10.3133/wri844348.","productDescription":"v, 27 p.","costCenters":[],"links":[{"id":415469,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36182.htm","linkFileType":{"id":5,"text":"html"}},{"id":126634,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4348/report-thumb.jpg"},{"id":56102,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4348/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","county":"Orange County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.187,\n 41.356\n ],\n [\n -74.187,\n 41.324\n ],\n [\n -74.149,\n 41.324\n ],\n [\n -74.149,\n 41.356\n ],\n [\n -74.187,\n 41.356\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611e84","contributors":{"authors":[{"text":"Garber, Murray","contributorId":81951,"corporation":false,"usgs":true,"family":"Garber","given":"Murray","affiliations":[],"preferred":false,"id":197779,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26965,"text":"wri844072 - 1985 - A summary of urban runoff studies in the Denver Metropolitan area, Colorado","interactions":[],"lastModifiedDate":"2023-04-06T18:58:59.018095","indexId":"wri844072","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4072","title":"A summary of urban runoff studies in the Denver Metropolitan area, Colorado","docAbstract":"

The Denver metropolitan area has been the subject of urban-runoff studies for several years. The first studies, started in about 1968, usually were concerned only with the quantity of urban runoff. In 1974, studies were begun that included both quantity and quality of urban runoff. In 1979, Denver was selected as one of the cities to be included in the Nationwide Urban Runoff Program. The Denver study was called the Denver Regional Urban Runoff Program and was a cooperative study between the Denver Regional Council of Governments and the U.S. Geological Survey. This report presents the major conclusions of the pre-Denver Regional Urban Runoff Program studies and a summary of the various elements of the Denver Regional Urban Runoff Program. The report summarizes and references urban-runoff studies in the Denver metropolitan area and is a reference guide for planners and other persons interested in urban runoff. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844072","usgsCitation":"Ellis, S.R., and Mustard, M.H., 1985, A summary of urban runoff studies in the Denver Metropolitan area, Colorado: U.S. Geological Survey Water-Resources Investigations Report 84-4072, iv, 31 p., https://doi.org/10.3133/wri844072.","productDescription":"iv, 31 p.","costCenters":[],"links":[{"id":55850,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4072/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119009,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4072/report-thumb.jpg"},{"id":415369,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35968.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","city":"Denver","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.2543190060805,\n 39.84789864180311\n ],\n [\n -105.2543190060805,\n 39.55675228729626\n ],\n [\n -104.80765821242575,\n 39.55675228729626\n ],\n [\n -104.80765821242575,\n 39.84789864180311\n ],\n [\n -105.2543190060805,\n 39.84789864180311\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5f42","contributors":{"authors":[{"text":"Ellis, S. R.","contributorId":103278,"corporation":false,"usgs":true,"family":"Ellis","given":"S.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":197329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mustard, M. H.","contributorId":18385,"corporation":false,"usgs":true,"family":"Mustard","given":"M.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":197328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28497,"text":"wri844351 - 1985 - A preliminary evaluation of hydrology and water quality near the Tacoma landfill, Pierce County, Washington","interactions":[],"lastModifiedDate":"2023-04-06T18:37:41.574409","indexId":"wri844351","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4351","title":"A preliminary evaluation of hydrology and water quality near the Tacoma landfill, Pierce County, Washington","docAbstract":"

The Tacoma landfill, located in western Pierce County, Washington, has been used for the disposal of waste since about 1960. Disposal operations are planned to continue at this site until at least 1990. Data were compiled and interpreted to help understand the possible effects of the landfill on water quality in the surrounding area. Data were collected from published and unpublished reports of the U.S. Geological Survey, and from predominantly unpublished data in the files of other government agencies. The Tacoma landfill is underlain by unconsolidated, glacially derived deposits that consist of a wide variety of mixtures of clay to boulder-sized materials. Ground water is mostly the result of rainfall on the land surface, and moves through artesian aquifers (under the landfill) that are tapped for both domestic and municipal use. Hazardous liquid and dissolved wastes are probably present in the landfill, and potential flow paths for waste migration exist. An undetermined number of single-family domestic wells and 18 public-supply wells are within 3 miles of the landfill, three as close as 0.2 miles. There is only limited evidence indicating ground- and surface-water contamination. Further investigations of the geology, hydrology and water quality are needed to characterize the impact the landfill has on ground- and surface-water of the surrounding area.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844351","usgsCitation":"Lum, W., and Turney, G.L., 1985, A preliminary evaluation of hydrology and water quality near the Tacoma landfill, Pierce County, Washington: U.S. Geological Survey Water-Resources Investigations Report 84-4351, v, 35 p., https://doi.org/10.3133/wri844351.","productDescription":"v, 35 p.","costCenters":[],"links":[{"id":57299,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4351/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122670,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4351/report-thumb.jpg"},{"id":415365,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36184.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","city":"Tacoma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.543,\n 47.239\n ],\n [\n -122.543,\n 47.185\n ],\n [\n -122.457,\n 47.185\n ],\n [\n -122.457,\n 47.239\n ],\n [\n -122.543,\n 47.239\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4964e4b0b290850ef1eb","contributors":{"authors":[{"text":"Lum, W. E.","contributorId":57847,"corporation":false,"usgs":true,"family":"Lum","given":"W. E.","affiliations":[],"preferred":false,"id":199913,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turney, G. L.","contributorId":95070,"corporation":false,"usgs":true,"family":"Turney","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":199914,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27088,"text":"wri844094 - 1985 - Nonpoint-source discharges and water quality of the Elk Creek basin, west-central Wisconsin","interactions":[],"lastModifiedDate":"2023-03-31T18:28:59.552368","indexId":"wri844094","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4094","title":"Nonpoint-source discharges and water quality of the Elk Creek basin, west-central Wisconsin","docAbstract":"

The Elk Creek basin in west-central Wisconsin was studied during the 1980 water year to define the water quality in relation to streamflow. Agricultural nonpoint-source discharges were suspected of contributing significantly to degraded water quality. Two water quality and streamflow gaging stations were established--one on Elk Creek near Independence and the other on Bruce Valley Creek near Pleasantville.

Streamflow for the 1980 water year was about 28% greater than average, and precipitation was about 36% greater than average. At Elk Creek, base flow was about 68% of the total stream discharge and, at Bruce Valley Creek, base flow was about 56% of the total stream discharge. Streamflow at Elk Creek during the study ranged from 43 to 1,020 cu ft/sec; Bruce Valley Creek discharges ranged from 2.8 to 306 cu ft/sec. The low flow discharges are significantly greater than the 2-year, 7-day low flow, whereas the peak discharges were between a 2-year and a 5-year flood recurrence interval.

Suspended-sediment yields were greatest at Bruce Valley Creek, and was 215 ton/sq mi/yr compared with 184 ton/sq mi/yr for Elk Creek. Double mass-accumulation curves, however, indicated that loading rates were similar for both stations. Suspended sediment and nutrient yields were slightly above the long-term average.

Total phosphorus , ammonia nitrogen, and organic nitrogen yields also were highest at Bruce Valley Creek. Phosphorus yields at Bruce Valley Creek were 1,6000 lb/sq mi/yr compared with 1,350 lb/sq mi/yr at Elk Creek. Because base flow was a greater percentage of total discharge, nitrite plus nitrate nitrogen yields and loads were highest at Elk Creek.

All phosphorus concentrations at Bruce Valley and Elk Creeks exceeded levels recommended by EPA to prevent the formation of biological nuisance growths. Only one sample, collected on March 18, 1980, at Bruce Valley Creek may have exceeded the Wisconsin Department of Natural Resources criterion of toxic levels for un-ionized ammonia (0.04 mg/L). No samples from Elk Creek extended the criteria. (

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844094","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Field, S.J., 1985, Nonpoint-source discharges and water quality of the Elk Creek basin, west-central Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 84-4094, vi, 38 p., https://doi.org/10.3133/wri844094.","productDescription":"vi, 38 p.","numberOfPages":"45","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":415016,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35985.htm","linkFileType":{"id":5,"text":"html"}},{"id":124908,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4094/report-thumb.jpg"},{"id":55954,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4094/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Trempealeau County","otherGeospatial":"Bruce Valley Creek, Elk Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -91.5,\n 44.5\n ],\n [\n -91.5,\n 44.25\n ],\n [\n -91.217,\n 44.25\n ],\n [\n -91.217,\n 44.5\n ],\n [\n -91.5,\n 44.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e480ae4b07f02db4d2c43","contributors":{"authors":[{"text":"Field, S. J.","contributorId":50540,"corporation":false,"usgs":true,"family":"Field","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197534,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26538,"text":"wri844068 - 1985 - Geology of the surficial aquifer system Broward County, Florida: Lithologic logs","interactions":[],"lastModifiedDate":"2023-04-11T18:47:46.100693","indexId":"wri844068","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4068","title":"Geology of the surficial aquifer system Broward County, Florida: Lithologic logs","docAbstract":"

The geologic framework of the surficial aquifer system, of which the Biscayne aquifer is the major component in Broward County, Florida, is presented in eight geologic cross sections. The cross sections are based on detailed lithologic logs of 27 test wells that were drilled, in the summer of 1981, through the sediments overlying the relatively impermeable units of the Hawthorn Formation, of Miocene age. The cross sections show the aquifer system as a wedge-shaped sequence of Cenozoic sediments. The aquifer thickness gradually decreases from more than 400 feet along the coast to about 160 feet in the west and southwest parts of Broward County. The sediments that comprise the aquifer system range in age from Pliocene to Pleistocene and are assigned to the following stratigraphic units from bottom to top: Tamiami Formation, Caloosahatchee Marl, Fort Thompson Formation, Key Largo Limestone, Anastasia Formation, Miami Oolite, and Pamlico Sand. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844068","usgsCitation":"Causaras, C., 1985, Geology of the surficial aquifer system Broward County, Florida: Lithologic logs: U.S. Geological Survey Water-Resources Investigations Report 84-4068, Report: 167 p.; 2 Plates: 43.55 x 31.77 inches and 41.19 x 33.19 inches, https://doi.org/10.3133/wri844068.","productDescription":"Report: 167 p.; 2 Plates: 43.55 x 31.77 inches and 41.19 x 33.19 inches","costCenters":[],"links":[{"id":415586,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35964.htm","linkFileType":{"id":5,"text":"html"}},{"id":123469,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4068/report-thumb.jpg"},{"id":55400,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4068/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55401,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4068/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55402,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4068/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Broward County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.117,\n 26.351\n ],\n [\n -80.875,\n 26.351\n ],\n [\n -80.875,\n 25.967\n ],\n [\n -80.117,\n 25.967\n ],\n [\n -80.117,\n 26.351\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c763","contributors":{"authors":[{"text":"Causaras, C. R.","contributorId":66679,"corporation":false,"usgs":true,"family":"Causaras","given":"C. R.","affiliations":[],"preferred":false,"id":196574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40625,"text":"ofr791379 - 1985 - Federal coal resource occurrence and coal development potential maps of the Pillar 3 SE 7 1/2-minute quadrangle, San Juan and McKinley Counties, New Mexico","interactions":[],"lastModifiedDate":"2023-05-09T19:54:35.336224","indexId":"ofr791379","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1379","title":"Federal coal resource occurrence and coal development potential maps of the Pillar 3 SE 7 1/2-minute quadrangle, San Juan and McKinley Counties, New Mexico","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791379","usgsCitation":"Berge Exploration Inc., 1985, Federal coal resource occurrence and coal development potential maps of the Pillar 3 SE 7 1/2-minute quadrangle, San Juan and McKinley Counties, New Mexico: U.S. Geological Survey Open-File Report 79-1379, Report: ii, 21 p.; 22 Plates: 28.96 x 22.78 inches or smaller, https://doi.org/10.3133/ofr791379.","productDescription":"Report: ii, 21 p.; 22 Plates: 28.96 x 22.78 inches or smaller","costCenters":[],"links":[{"id":416873,"rank":25,"type":{"id":36,"text":"NGMDB Index 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1983","interactions":[],"lastModifiedDate":"2023-09-01T20:49:26.854725","indexId":"ofr84726","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-726","title":"Map of Antelope Valley-East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and lines of equal depth to water for spring 1983","docAbstract":"

No abstract available.

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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8040","usgsCitation":"Berge Exploration Inc., 1985, Federal coal resource occurrence and coal development potential maps of the Pinehaven 7 1/2-minute quadrangle, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 80-40, Report: ii, 19 p.; 9 Plates: 29.79 x 23.48 inches or smaller, https://doi.org/10.3133/ofr8040.","productDescription":"Report: ii, 19 p.; 9 Plates: 29.79 x 23.48 inches or smaller","costCenters":[],"links":[{"id":416875,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75179.htm","linkFileType":{"id":5,"text":"html"}},{"id":77395,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0040/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77394,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0040/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77393,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0040/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77392,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0040/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77391,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0040/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77390,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0040/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77389,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0040/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77388,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0040/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77387,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0040/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77386,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173137,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0040/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"McKinley County","otherGeospatial":"Pinehaven 7 1/2-minute quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -108.75,\n 35.25\n ],\n [\n -108.625,\n 35.25\n ],\n [\n -108.625,\n 35.375\n ],\n [\n -108.75,\n 35.375\n ],\n [\n -108.75,\n 35.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6c23","contributors":{"authors":[{"text":"Berge Exploration Inc.","contributorId":128031,"corporation":true,"usgs":false,"organization":"Berge Exploration Inc.","id":530368,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40511,"text":"ofr8041 - 1985 - Federal coal resource occurrence and coal development potential maps of the Upper Nutria 7 1/2-minute quadrangle, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2023-05-09T21:39:48.723528","indexId":"ofr8041","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-41","title":"Federal coal resource occurrence and coal development potential maps of the Upper Nutria 7 1/2-minute quadrangle, McKinley County, New Mexico","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8041","usgsCitation":"Berge Exploration Inc., 1985, Federal coal resource occurrence and coal development potential maps of the Upper Nutria 7 1/2-minute quadrangle, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 80-41, Report: i, 29 p.; 5 Plates: 23.66 x 28.34 inches or smaller, https://doi.org/10.3133/ofr8041.","productDescription":"Report: i, 29 p.; 5 Plates: 23.66 x 28.34 inches or smaller","costCenters":[],"links":[{"id":416882,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75180.htm","linkFileType":{"id":5,"text":"html"}},{"id":75908,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0041/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":75907,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0041/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":75906,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0041/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":75905,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0041/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":75904,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0041/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":75903,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168767,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0041/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"McKinley County","otherGeospatial":"Upper Nutria 7 1/2-minute quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -108.625,\n 35.375\n ],\n [\n -108.625,\n 35.25\n ],\n [\n -108.5,\n 35.25\n ],\n [\n -108.5,\n 35.375\n ],\n [\n -108.625,\n 35.375\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5fa2","contributors":{"authors":[{"text":"Berge Exploration Inc.","contributorId":128031,"corporation":true,"usgs":false,"organization":"Berge Exploration Inc.","id":530289,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012275,"text":"70012275 - 1985 - LIQUEFACTION POTENTIAL OF SEDIMENT IN THE NORTHERN BERING SEA.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:06","indexId":"70012275","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"LIQUEFACTION POTENTIAL OF SEDIMENT IN THE NORTHERN BERING SEA.","docAbstract":"The liquefaction potential of sediment in Norton Sound and the northern Bering Sea was evaluated by estimating the liquefaction susceptibility of the material from in-situ and laboratory tests in terms of earthquake and wave loads required to liquefy the material, and then comparing estimated behavior with anticipated loadings caused by frequent storm waves in the relatively shallow water depths and infrequent earthquakes. In-situ cone penetration tests (CPT) were performed at 13 stations. After the CPT data were transformed into equivalent standard penetration test (SPT) blow counts, analyses were performed that determined earthquake accelerations and sustained relative storm wave heights that would cause liquefaction. Vibratory core samples, up to 6 m long, were obtained in silty sand grading to sandy silt near many of the CPT locations. Results of cyclic triaxial tests performed on those samples were used to calculate earthquake accelerations and sustained storm wave heights that would liquefy the sediment.","largerWorkTitle":"ASTM Special Technical Publication","conferenceTitle":"Strength Testing of Marine Sediments: Laboratory and In-Situ Measurements.","conferenceLocation":"San Diego, CA, USA","language":"English","publisher":"ASTM","publisherLocation":"Philadelphia, PA, USA","issn":"00660558","isbn":"0803104316","usgsCitation":"Winters, W.J., 1985, LIQUEFACTION POTENTIAL OF SEDIMENT IN THE NORTHERN BERING SEA., in ASTM Special Technical Publication, San Diego, CA, USA, p. 454-472.","startPage":"454","endPage":"472","numberOfPages":"19","costCenters":[],"links":[{"id":222343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a40e9e4b0c8380cd65130","contributors":{"editors":[{"text":"Chaney Ronald C.Demars Kenneth R.","contributorId":128443,"corporation":true,"usgs":false,"organization":"Chaney Ronald C.Demars Kenneth R.","id":536247,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Winters, William J. bwinters@usgs.gov","contributorId":522,"corporation":false,"usgs":true,"family":"Winters","given":"William","email":"bwinters@usgs.gov","middleInitial":"J.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":363157,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1013926,"text":"1013926 - 1985 - Toxic materials, fishing, and environmental variation: Simulated effects on striped bass population trends","interactions":[],"lastModifiedDate":"2026-04-09T17:06:29.026728","indexId":"1013926","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Toxic materials, fishing, and environmental variation: Simulated effects on striped bass population trends","docAbstract":"

Decreased survival of larval striped bass Morone saxatilis resulting from toxic chemicals in the environment and decreased survival of adults caused by fishing both are suspected as agents contributing to the decline in the Chesapeake Bay stock since the mid‐1970s. The relative power of each type of mortality to cause population declines was evaluated with simulation techniques. Equivalent levels of added mortality induced qualitatively identical and quantitatively similar trends in population simulations for all conditions examined except if strong density‐dependent mortality preceded the contaminant toxicity. In this case the contaminant effect caused a greater reduction in yield, but the population did not tend toward extinction. The results indicate that the observed downward trend in the Chesapeake Bay population can be halted or reversed by a reduction in fishing mortality, even if contaminant toxicity is the proximate cause for the decline.

","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1985)114<107:TMFAEV>2.0.CO;2","usgsCitation":"Goodyear, C., 1985, Toxic materials, fishing, and environmental variation: Simulated effects on striped bass population trends: Transactions of the American Fisheries Society, v. 114, no. 1, p. 107-113, https://doi.org/10.1577/1548-8659(1985)114<107:TMFAEV>2.0.CO;2.","productDescription":"7 p.","startPage":"107","endPage":"113","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130776,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Chesapeake Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.45137515753754,\n 39.490431843405645\n ],\n [\n -76.58379606562652,\n 38.66690029793358\n ],\n [\n -76.4943486933714,\n 37.089918804712\n ],\n [\n -75.96462427284425,\n 37.121312200179204\n ],\n [\n -75.86444692063253,\n 37.54276135963376\n ],\n [\n -75.6426165939144,\n 37.91879819208148\n ],\n [\n -75.7857193310846,\n 39.6502389229056\n ],\n [\n -76.45137515753754,\n 39.490431843405645\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"114","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db628142","contributors":{"authors":[{"text":"Goodyear, C.P.","contributorId":11538,"corporation":false,"usgs":true,"family":"Goodyear","given":"C.P.","email":"","affiliations":[],"preferred":false,"id":319449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013112,"text":"70013112 - 1985 - Vp/Vs ratios in the Yellowstone National Park region, Wyoming","interactions":[],"lastModifiedDate":"2012-03-12T17:18:39","indexId":"70013112","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Vp/Vs ratios in the Yellowstone National Park region, Wyoming","docAbstract":"In this paper we study the variation of Vp/Vs and Poisson's ratio (??) in the Yellowstone National Park region, using earthquakes which were well recorded by a local seismic network. We find that the average Vp/Vs value within the geothermally active Yellowstone caldera is about 7% lower than in the area outside the caldera. Within the caldera itself there may be a further 2-7% reduction of Vp/Vs in the hydrothermally active Norris Geyser Basin, the Upper and Lower Geyser Basins, and the Yellowstone Lake and Mud Volcano regions. After considering various possible causes for Vp/Vs changes, such as geologic and structural differences, thermal effects, partial melting, and hydrothermal activity, we conclude that the most plausible explanation for the observed Vp/Vs reduction is the presence of hot-water at temperatures and pore-pressures near the water steam transition in the caldera geothermal reservoirs. ?? 1985.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Chatterjee, S., Pitt, A., and Iyer, H.M., 1985, Vp/Vs ratios in the Yellowstone National Park region, Wyoming: Journal of Volcanology and Geothermal Research, v. 26, no. 3-4, p. 213-230.","startPage":"213","endPage":"230","numberOfPages":"18","costCenters":[],"links":[{"id":220015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc373e4b08c986b32b1ad","contributors":{"authors":[{"text":"Chatterjee, S.N.","contributorId":28742,"corporation":false,"usgs":true,"family":"Chatterjee","given":"S.N.","email":"","affiliations":[],"preferred":false,"id":365322,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pitt, A.D.","contributorId":41440,"corporation":false,"usgs":true,"family":"Pitt","given":"A.D.","affiliations":[],"preferred":false,"id":365323,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Iyer, H. M.","contributorId":17997,"corporation":false,"usgs":true,"family":"Iyer","given":"H.","middleInitial":"M.","affiliations":[],"preferred":false,"id":365321,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70012177,"text":"70012177 - 1985 - THEORETICAL TECHNIQUE FOR DETERMINING THE CUMULATIVE IMPACT OF IRON AND MANGANESE OXIDATION IN STREAMS RECEIVING COAL-MINE DISCHARGE.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:05","indexId":"70012177","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"THEORETICAL TECHNIQUE FOR DETERMINING THE CUMULATIVE IMPACT OF IRON AND MANGANESE OXIDATION IN STREAMS RECEIVING COAL-MINE DISCHARGE.","docAbstract":"Two U. S. Geological Survey computer programs are modified and linked to predict the cumulative impact of iron and manganese oxidation in coal-mine discharge on the dissolved-chemical quality of a receiving stream. The coupled programs calculate the changes in dissolved-iron, dissolved-manganese, and dissolved-oxygen concentrations, and the pH of surface water downstream from the discharge. The cumulative impact of representative discharges from several coal mines on stream quality in a small watershed in southwestern Indiana was simulated to determine the effectiveness and sensitivity of the coupled programs.","largerWorkTitle":"University of Kentucky, Office of Engineering Services, (Bulletin) UKY BU","conferenceTitle":"Proceedings - 1985 Symposium on Surface Mining, Hydrology, Sedimentology, and Reclamation.","conferenceLocation":"Lexington, KY, USA","language":"English","publisher":"Univ of Kentucky","publisherLocation":"Office of Engineering Services, Lexington, KY, USA","issn":"02706504","isbn":"0897790642","usgsCitation":"Bobay, K.E., and Banaszak, K.J., 1985, THEORETICAL TECHNIQUE FOR DETERMINING THE CUMULATIVE IMPACT OF IRON AND MANGANESE OXIDATION IN STREAMS RECEIVING COAL-MINE DISCHARGE., in University of Kentucky, Office of Engineering Services, (Bulletin) UKY BU, Lexington, KY, USA, p. 105-114.","startPage":"105","endPage":"114","numberOfPages":"10","costCenters":[],"links":[{"id":221932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba386e4b08c986b31fd38","contributors":{"editors":[{"text":"Graves Donald H.","contributorId":128374,"corporation":true,"usgs":false,"organization":"Graves Donald H.","id":536244,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Bobay, Keith E.","contributorId":66733,"corporation":false,"usgs":true,"family":"Bobay","given":"Keith","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":362929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Banaszak, Konrad J.","contributorId":88880,"corporation":false,"usgs":true,"family":"Banaszak","given":"Konrad","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":362930,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}