{"pageNumber":"3847","pageRowStart":"96150","pageSize":"25","recordCount":185189,"records":[{"id":25731,"text":"wri954110 - 1995 - Quantity and quality of ground-water discharge to the South Platte River, Denver to Fort Lupton, Colorado, August 1992 through July 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:08:13","indexId":"wri954110","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-4110","title":"Quantity and quality of ground-water discharge to the South Platte River, Denver to Fort Lupton, Colorado, August 1992 through July 1993","docAbstract":"Water-quality studies conducted by the Metro Wastewater Reclamation District have indicated that during low flow in segments of the South Platte River between Denver and Fort Lupton, concentrations of dissolved oxygen are less than minimum concen- trations set by the State of Colorado. Low dissolved-oxygen concentrations are observed in two reaches of the river-they are about 3.3 to 6.4 miles and 17 to 25 miles downstream from the Metro Waste- water Reclamation District effluent outfalls. Concentrations of dissolved oxygen recover between these two reaches. Studies conducted by the U.S. Geological Survey have indicated that ground-water discharge to the river may contribute to these low dissolved-oxygen concentrations. As a result, an assessment was made of the quantity and quality of ground-water discharge to the South Platte River from Denver to Fort Lupton. Measurements of surface- water and ground-water discharge and collections of surface water and ground water for water-quality analyses were made from August 1992 through January 1993 and in May and July 1993. The quantity of ground-water discharge to the South Platte River was determined indirectly by mass balance of surface-water inflows and outflows and directly by instantaneous measurements of ground-water discharge across the sediment/water interface in the river channel. The quality of surface water and ground water was determined by sampling and analysis of water from the river and monitoring wells screened in the alluvial aquifer adjacent to the river and by sampling and analysis of water from piezometers screened in sediments underlying the river channel. The ground-water flow system was subdivided into a large-area and a small-area flow system. The precise boundaries of the two flow systems are not known. However, the large-area flow system is considered to incorporate all alluvial sediments in hydrologic connection with the South Platte River. The small- area flow system is considered to incorporate the alluvial aquifer in the vicinity of the river. Flow-path lengths in the large-area flow system were considered to be on the order of hundreds of feet to more than a mile, whereas in the small-area flow system, they were considered to be on the order of feet to hundreds of feet. Mass-balance estimates of incremental ground-water discharge from the large- area flow system ranged from -27 to 17 cubic feet per second per mile in three reaches of the river; the median rate was 4.6 cubic feet per second per mile. The median percentage of surface-water discharge derived from ground-water discharge in the river reaches studied was 13 percent. Instantaneous measurements of ground-water discharge from the small-area flow system ranged from -1,360 to 1,000 cubic feet per second per mile, with a median value of -5.8 cubic feet per second per mile. Hourly measurements of discharge from the small-area flow system indicated that the high rates of discharge were transient and may have been caused by daily fluctuations in river stage due to changing effluent-discharge rates from the Metro Wastewater Reclamation District treatment plant. Higher river stages caused surface water to infiltrate bed sediments underlying the river channel, and lower river stages allowed ground water to discharge into the river. Although stage changes apparently cycled large quantities of water in and out of the small- area flow system, the process probably provided no net gain or loss of water to the river. In general, mass balance and instantaneous measurements of ground-water discharge indicated that the ground- water flow system in the vicinity of the river consisted of a large-area flow system that provided a net addition of water to the river and a small- area flow system that cycled water in and out of the riverbed sediments, but provided no net addition of water to the river. The small-area flow system was superimposed on the large-area flow system. The median values of pH and dissolved oxygen ","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954110","usgsCitation":"McMahon, P., Lull, K., Dennehy, K., and Collins, J., 1995, Quantity and quality of ground-water discharge to the South Platte River, Denver to Fort Lupton, Colorado, August 1992 through July 1993: U.S. Geological Survey Water-Resources Investigations Report 95-4110, v, 71 p. :ill., map ;28 cm., https://doi.org/10.3133/wri954110.","productDescription":"v, 71 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":157131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4110/report-thumb.jpg"},{"id":54491,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4110/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54492,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e4fe","contributors":{"authors":[{"text":"McMahon, P.B. 0000-0001-7452-2379","orcid":"https://orcid.org/0000-0001-7452-2379","contributorId":10762,"corporation":false,"usgs":true,"family":"McMahon","given":"P.B.","affiliations":[],"preferred":false,"id":194833,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lull, K.J.","contributorId":19591,"corporation":false,"usgs":true,"family":"Lull","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":194834,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dennehy, K.F.","contributorId":41841,"corporation":false,"usgs":true,"family":"Dennehy","given":"K.F.","affiliations":[],"preferred":false,"id":194835,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Collins, J.A.","contributorId":72412,"corporation":false,"usgs":true,"family":"Collins","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":194836,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5435,"text":"fs20795 - 1995 - USGS reference materials","interactions":[],"lastModifiedDate":"2014-04-03T11:23:23","indexId":"fs20795","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"207-95","title":"USGS reference materials","docAbstract":"Every year in the United States, millions \nof measurements are made on the chemical \ncomposition of items that affect us on a \ndaily basis. Determining the accuracy of \nthese measurements is based on the analysis \nof appropriate reference materials whose \ncomposition was previously determined \nthrough rigorous testing. Today, reference \nmaterials help us evaluate the composition \nof the food we eat, medicine we use, soil we \ngrow our crops in, and hundreds of other \nproducts that affect our everyday lives.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20795","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, USGS reference materials: U.S. Geological Survey Fact Sheet 207-95, 2 p., https://doi.org/10.3133/fs20795.","productDescription":"2 p.","numberOfPages":"2","costCenters":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"links":[{"id":139467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs20795.jpg"},{"id":285424,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/0207-95/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f928","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528577,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23884,"text":"ofr95426 - 1995 - Potential hazards from flood in part of the Chalone Creek and Bear Valley drainage basins, Pinnacles National Monument, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:07","indexId":"ofr95426","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-426","title":"Potential hazards from flood in part of the Chalone Creek and Bear Valley drainage basins, Pinnacles National Monument, California","docAbstract":"Areas of Chalone Creek and Bear Valley drainage basins in Pinnacles National Monument, California, are subject to frontal storms that can cause major flooding from November to April in areas designated for public use. To enhance visitor safety and to protect cultural and natural resources, the U.S. Geological Survey in cooperation with the National Park Service studied flood-hazard potentials within the boundaries of the Pinnacles National Monument. This study area extends from about a quarter of a mile north of Chalone Creek Campground to the mouth of Bear Valley and from the east monument entrance to Chalone Creek. Historical data of precipitation and floodflow within the monument area are sparse to nonexistent, therefore, U.S. Soil Conservation Service unit-hydrograph procedures were used to determine the magnitude of a 100-year flood. Because of a lack of specific storm-rainfall data, a simulated storm was applied to the basins using a digital-computer model developed by the Soil Conservation Service. A graphical relation was used to define the regionally based maximum flood for Chalone Creek and Bear Valley. Water-surface elevations and inundation areas were determined using a conventional step-backwater program. Flood-zone boundaries were derived from the computed water-surface elevations. The 100-year flood plain for both streams would be inundated at all points by the regional maximum flood. Most of the buildings and proposed building sites in the monument area are above the elevation of the 100-year flood, except the proposed building sites near the horse corral and the east monument entrance. The 100-year flood may cause reverse flow through a 12-inch culvert embedded in the embankment of Old Pinnacles Campground Road in the center of Chalone Creek Campground. The likelihood of this occurring is dependant upon the amount of aggradation that occurs upstream; therefore, the campground area also is considered to be within the 100-year flood zone.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95426","issn":"0094-9140","usgsCitation":"Meyer, R.W., 1995, Potential hazards from flood in part of the Chalone Creek and Bear Valley drainage basins, Pinnacles National Monument, California: U.S. Geological Survey Open-File Report 95-426, iv, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95426.","productDescription":"iv, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0426/report-thumb.jpg"},{"id":19487,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0426/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19488,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0426/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db6832d8","contributors":{"authors":[{"text":"Meyer, Robert W.","contributorId":69601,"corporation":false,"usgs":true,"family":"Meyer","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":190907,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31920,"text":"ofr95624 - 1995 - Earthquakes in Alaska","interactions":[],"lastModifiedDate":"2023-11-03T16:48:43.857774","indexId":"ofr95624","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-624","title":"Earthquakes in Alaska","docAbstract":"Earthquake risk is high in much of the southern half of Alaska, but it is not the same everywhere. This map shows the overall geologic setting in Alaska that produces earthquakes. The Pacific plate (darker blue) is sliding northwestward past southeastern Alaska and then dives beneath the North American plate (light blue, green, and brown) in southern Alaska, the Alaska Peninsula, and the Aleutian Islands. Most earthquakes are produced where these two plates come into contact and slide past each other. Major earthquakes also occur throughout much of interior Alaska as a result of collision of a piece of crust with the southern margin.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95624","usgsCitation":"Haeussler, P.J., and Plafker, G., 1995, Earthquakes in Alaska: U.S. Geological Survey Open-File Report 95-624, Report: 1 p.; 1 Plate: 40.72 x 21.29 inches, https://doi.org/10.3133/ofr95624.","productDescription":"Report: 1 p.; 1 Plate: 40.72 x 21.29 inches","numberOfPages":"1","additionalOnlineFiles":"Y","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":3215,"rank":4,"type":{"id":15,"text":"Index 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Peter J. 0000-0002-1503-6247 pheuslr@usgs.gov","orcid":"https://orcid.org/0000-0002-1503-6247","contributorId":503,"corporation":false,"usgs":true,"family":"Haeussler","given":"Peter","email":"pheuslr@usgs.gov","middleInitial":"J.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":207236,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":207237,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30259,"text":"wri954113 - 1995 - Ground-Water Availability from the Hawi Aquifer in the Kohala Area, Hawaii","interactions":[],"lastModifiedDate":"2012-03-08T17:16:15","indexId":"wri954113","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-4113","title":"Ground-Water Availability from the Hawi Aquifer in the Kohala Area, Hawaii","docAbstract":"A ground-water study consisting of test-well drilling, aquifer tests, and numerical simulation was done to investigate ground-water availability in the basal part of the Hawi aquifer between the western drainage divide of Pololu Valley and Upolu Point in Kohala, Hawaii. The test-well drilling provided information on geology, water levels, water quality, vertical extent of the freshwater, and the thickness of the freshwater-saltwater transition zone in that aquifer. A total of 12 test wells were drilled at eight locations. Aquifer tests were done at five locations to estimate the hydraulic conductivity of the aquifer. Using information on the distribution of recharge, vertical extent of freshwater, hydraulic conductivity, and geometry of the basal aquifer, a numerical model was used to simulate the movement of water into, through, and out of the basal aquifer, and the effect of additional pumping on the water levels in the aquifer.\r\n\r\nResults of the modeling indicate that ground-water withdrawal of 20 million gallons per day above the existing withdrawal of 0.6 million gallons per day from the basal aquifer is hydrologically feasible, but that spacing, depth, and pumping rates of individual wells are important. If pumping is concentrated, the likelihood of saltwater intrusion is increased. The additional withdrawal of 20 million gallons per day would result in a reduction of ground-water discharge to the ocean by an amount equal to pumpage. Although model-calculated declines in water-level outside the area of pumping are small, pumping could cause some reduction of streamflow near the mouth of Pololu Stream.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri954113","usgsCitation":"Underwood, M.R., Meyer, W., and Souza, W.R., 1995, Ground-Water Availability from the Hawi Aquifer in the Kohala Area, Hawaii: U.S. Geological Survey Water-Resources Investigations Report 95-4113, vi, 57 p., https://doi.org/10.3133/wri954113.","productDescription":"vi, 57 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":123867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4113/report-thumb.jpg"},{"id":59048,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4113/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db5457af","contributors":{"authors":[{"text":"Underwood, Mark R.","contributorId":45354,"corporation":false,"usgs":true,"family":"Underwood","given":"Mark","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":202950,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Souza, William R.","contributorId":90295,"corporation":false,"usgs":true,"family":"Souza","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202951,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27863,"text":"wri954183 - 1995 - Geology, Streamflow, and Water Chemistry of the Talufofo Stream Basin, Saipan, Northern Mariana Islands","interactions":[],"lastModifiedDate":"2012-03-08T17:16:15","indexId":"wri954183","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-4183","title":"Geology, Streamflow, and Water Chemistry of the Talufofo Stream Basin, Saipan, Northern Mariana Islands","docAbstract":"A study of the geology, streamflow, and water chemistry of Talufofo Stream Basin, Saipan, Commonwealth of the Northern Mariana Islands, was undertaken to determine the flow characteristics of Talufofo Stream and the relation to the geology of the drainage basin. The Commonwealth government is exploring the feasibility of using water from Talufofo Stream to supplement Saipan's stressed municipal water supply.\r\n\r\nStreamflow records from gaging stations on the principal forks of Talufofo Stream indicate that peak streamflows and long-term average flow are higher at the South Fork gaging station than at the Middle Fork gaging station because the drainage area of the South Fork gaging station is larger, but persistent base flow from ground-water discharge during dry weather is greater in the Middle Fork gaging station. The sum of the average flows at the Middle Fork and South Fork gaging stations, plus an estimate of the average flow at a point in the lower reaches of the North Fork, is about 2.96 cubic feet per second or 1.91 million gallons per day. Although this average represents the theoretical maximum long-term draft rate possible from the Talufofo Stream Basin if an adequate reservoir can be built, the actual amount of surface water available will be less because of evaporation, leaks, induced infiltration, and reservoir-design constraints. \r\n\r\nBase-flow characteristics, such as stream seepage and spring discharge, are related to geology of the basin. Base flow in the Talufofo Stream Basin originates as discharge from springs near the base of limestones located in the headwaters of Talufofo Stream, flows over low-permeability volcanic rocks in the middle reaches, and seeps back into the high-permeability limestones in the lower reaches. \r\n\r\nWater sampled from Talufofo Stream during base flow had high dissolved-calcium concentrations (between 35 and 98 milligrams per liter), characteristic of water from a limestone aquifer. Concentrations of potassium, sodium, and chloride ions in water samples from Talufofo Stream are characteristic of water draining a heavily vegetated basin near the ocean.\r\n\r\nThe streamflow and water-chemistry data indicate that discharge from springs is in hydraulic connection with the limestone aquifer near the headwaters of the basin. The base flow therefore is subject to stresses placed on the nearby limestone ground-water system. Pumping from wells in the limestones at the headwaters of Talufofo Stream Basin may decrease spring flow in Talufofo Stream.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri954183","usgsCitation":"Izuka, S.K., and Ewart, C.J., 1995, Geology, Streamflow, and Water Chemistry of the Talufofo Stream Basin, Saipan, Northern Mariana Islands: U.S. Geological Survey Water-Resources Investigations Report 95-4183, iv, 26 p., https://doi.org/10.3133/wri954183.","productDescription":"iv, 26 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":123759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4183/report-thumb.jpg"},{"id":56688,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4183/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ee81","contributors":{"authors":[{"text":"Izuka, Scot K. 0000-0002-8758-9414 skizuka@usgs.gov","orcid":"https://orcid.org/0000-0002-8758-9414","contributorId":2645,"corporation":false,"usgs":true,"family":"Izuka","given":"Scot","email":"skizuka@usgs.gov","middleInitial":"K.","affiliations":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"preferred":true,"id":198803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ewart, Charles J. III","contributorId":76361,"corporation":false,"usgs":true,"family":"Ewart","given":"Charles","suffix":"III","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198804,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5062,"text":"fs21695 - 1995 - Mercury contamination of aquatic ecosystems","interactions":[],"lastModifiedDate":"2020-04-11T16:39:50.948014","indexId":"fs21695","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"216-95","title":"Mercury contamination of aquatic ecosystems","docAbstract":"<p>Mercury has been well known as an environmental pollutant for several decades. As early as the 1950's it was established that emissions of mercury to the environment could have serious effects on human health. These early studies demonstrated that fish and other wildlife from various ecosystems commonly attain mercury levels of toxicological concern when directly affected by mercury-containing emissions from human-related activities. Human health concerns arise when fish and wildlife from these ecosystems are consumed by humans. During the past decade, a new trend has emerged with regard to mercury pollution. Investigations initiated in the late 1980's in the northern-tier states of the U.S., Canada, and Nordic countries found that fish, mainly from nutrient-poor lakes and often in very remote areas, commonly have high levels of mercury. More recent fish sampling surveys in other regions of the U.S. have shown widespread mercury contamination in streams, wet-lands, reservoirs, and lakes. To date, 33 states have issued fish consumption advisories because of mercury contamination. These continental to global scale occurrences of mercury contamination cannot be linked to individual emissions of mercury, but instead are due to widespread air pollution. When scientists measure mercury levels in air and surface water, however, the observed levels are extraordinarily low. In fact, scientists have to take extreme precautions to avoid direct contact with water samples or sample containers, to avert sample contamination (Fig 3). Herein lies an apparent discrepancy: Why do fish from some remote areas have elevated mercury concentrations, when contamination levels in the environment are so low?</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs21695","usgsCitation":"Krabbenhoft, D.P., and Rickert, D.A., 1995, Mercury contamination of aquatic ecosystems: U.S. Geological Survey Fact Sheet 216-95, 4 p., https://doi.org/10.3133/fs21695.","productDescription":"4 p.","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science 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,{"id":31913,"text":"ofr95432 - 1995 - Records of wells and water levels from the statewide observation-well network in Montana from October 1985 through October 1992","interactions":[],"lastModifiedDate":"2022-07-11T18:48:56.885905","indexId":"ofr95432","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-432","title":"Records of wells and water levels from the statewide observation-well network in Montana from October 1985 through October 1992","docAbstract":"A statewide observation-well network was developed in Montana in 1947 by the U.S. Geological Survey in cooperation with other Federal and State agencies to provide a long-term record of water levels in selected wells. This report summarized well records and water levels for the network and shows the locations of the wells. Data for 360 wells are tabulated in this report, generally for the period 1985-92. The well records include altitude of land surface, principal aquifer, year of construction, depth of well, primary use of site, primary use of water, casing type,casing depth, casing diameter, top of and bottom of open interval, year water-level data collection began, frequency of water-level data collection, year water-quality data collection began, type of analysis, year water-quality parameter measured, analyzing agency, and type of logs available. The water-level data include date of measurement, water level, method of measurement, and site status. Data for wells equipped with recorders include well number, site identification, name of source agency, well depth, principal aquifer, altitude of land surface, and water level. Well location is shown on a map at a scale of 1:1,000,000.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95432","usgsCitation":"Chambers, C.L., 1995, Records of wells and water levels from the statewide observation-well network in Montana from October 1985 through October 1992: U.S. Geological Survey Open-File Report 95-432, 153 p., https://doi.org/10.3133/ofr95432.","productDescription":"153 p.","costCenters":[],"links":[{"id":403426,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18474.htm","linkFileType":{"id":5,"text":"html"}},{"id":60082,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0432/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0432/report-thumb.jpg"}],"country":"United 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,{"id":6726,"text":"fs18295 - 1995 - USGS ensures quality of acid rain network","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"fs18295","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"182-95","title":"USGS ensures quality of acid rain network","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs18295","usgsCitation":"Nilles, M.A., and Gordon, J.D., 1995, USGS ensures quality of acid rain network: U.S. Geological Survey Fact Sheet 182-95, [2] p. : ill. ; 28 cm. ill., https://doi.org/10.3133/fs18295.","productDescription":"[2] p. : ill. ; 28 cm. ill.","costCenters":[],"links":[{"id":117638,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_182_95.jpg"},{"id":760,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://bqs.usgs.gov/precip/reports/fs18295/qafactpg.htm","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610f07","contributors":{"authors":[{"text":"Nilles, Mark A. manilles@usgs.gov","contributorId":3171,"corporation":false,"usgs":true,"family":"Nilles","given":"Mark","email":"manilles@usgs.gov","middleInitial":"A.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":153229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gordon, John D. 0000-0001-8396-8524 jgordon@usgs.gov","orcid":"https://orcid.org/0000-0001-8396-8524","contributorId":347,"corporation":false,"usgs":true,"family":"Gordon","given":"John","email":"jgordon@usgs.gov","middleInitial":"D.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153228,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31891,"text":"ofr95543A - 1995 - Map showing bedrock surface topography, bedrock outcrops, and areas of shallow bedrock in the northern sheet, New Jersey","interactions":[],"lastModifiedDate":"2023-09-14T19:40:58.589271","indexId":"ofr95543A","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-543","chapter":"A","title":"Map showing bedrock surface topography, bedrock outcrops, and areas of shallow bedrock in the northern sheet, New Jersey","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95543A","usgsCitation":"Stone, B.D., Stanford, S.D., and Witte, R.W., 1995, Map showing bedrock surface 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,{"id":23949,"text":"ofr95358 - 1995 - Estimated water use in Puerto Rico, 1986-87","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr95358","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-358","title":"Estimated water use in Puerto Rico, 1986-87","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95358","issn":"0094-9140","usgsCitation":"Molina-Rivera, W., and Dopazo, T., 1995, Estimated water use in Puerto Rico, 1986-87: U.S. Geological Survey Open-File Report 95-358, v, 31 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95358.","productDescription":"v, 31 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0358/report-thumb.jpg"},{"id":53148,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0358/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcc1e","contributors":{"authors":[{"text":"Molina-Rivera, W. L.","contributorId":84790,"corporation":false,"usgs":true,"family":"Molina-Rivera","given":"W. L.","affiliations":[],"preferred":false,"id":191029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dopazo, Teresa","contributorId":42246,"corporation":false,"usgs":true,"family":"Dopazo","given":"Teresa","affiliations":[],"preferred":false,"id":191028,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21715,"text":"ofr95469 - 1995 - Data on selected herbicides and two triazine metabolites in precipitation of the Midwestern and Northeastern United States, 1990-91","interactions":[],"lastModifiedDate":"2019-12-07T10:40:44","indexId":"ofr95469","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-469","title":"Data on selected herbicides and two triazine metabolites in precipitation of the Midwestern and Northeastern United States, 1990-91","docAbstract":"Weekly precipitation (rain and snow) samples were collected from 81 National Atmospheric Deposition Program/National Trends Network sites in the Midwestern and Northeastern United States for the analysis of herbicides. In addition, five high- elevation background sites along the Rocky Mountains and in Alaska were sampled to provide data on herbicides in precipitation at sites far from the study area. The study began in March 1990 and continued through September 1991. The precipitation samples were shipped to the Central Analytical Laboratory operated by the Illinois State Water Survey for analyses of inorganic compounds. Subsamples of the precipitation were shipped to the U.S. Geological Survey laboratory in Lawrence, Kansas, for the analysis of 11 herbicides and 2 triazines metabolites. This report provides descriptions of the study area, sample-collection methods, laboratory methods, and quality assurance. The report also includes a compilation of herbicide concentration data from both enzyme-linked immunosorbent assay and gas chromatography/mass spectrometry methods. Laboratory analyses consisted of 6,230 samples that were analyzed by enzyme-linked immunosorbent assay using alachlor and atrazine microtiter plates and 2,341 samples that were confirmed by gas chromatography/mass spectrometry analysis. Graphical and statistical comparisons of the two analytical methods are given in this report. Data from this study have been useful in determining the spatial and temporal distribution of herbicide concentrations and deposition in precipitation of over a 26-State area of the Midwestern and Northeastern United States. The data also provide evidence of long-range atmospheric transport of herbicides and triazine metabolites.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr95469","issn":"0566-8174","usgsCitation":"Goolsby, D.A., Scribner, E., Thurman, E., Pomes, M., and Meyer, M.T., 1995, Data on selected herbicides and two triazine metabolites in precipitation of the Midwestern and Northeastern United States, 1990-91: U.S. Geological Survey Open-File Report 95-469, iv, 341 p., https://doi.org/10.3133/ofr95469.","productDescription":"iv, 341 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":154557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0469/report-thumb.jpg"},{"id":51242,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0469/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.150390625,\n              48.80686346108517\n            ],\n            [\n              -101.865234375,\n              36.527294814546245\n            ],\n            [\n              -81.298828125,\n              35.02999636902566\n            ],\n            [\n              -67.587890625,\n              45.213003555993964\n            ],\n            [\n              -68.64257812499999,\n              47.39834920035926\n            ],\n            [\n              -82.353515625,\n              41.96765920367816\n            ],\n            [\n              -83.49609375,\n              46.13417004624326\n            ],\n            [\n              -88.330078125,\n              48.3416461723746\n            ],\n            [\n              -104.150390625,\n              48.80686346108517\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bdbc","contributors":{"authors":[{"text":"Goolsby, D. A.","contributorId":50508,"corporation":false,"usgs":true,"family":"Goolsby","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":185386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scribner, E.A.","contributorId":50925,"corporation":false,"usgs":true,"family":"Scribner","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":185387,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":185390,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pomes, M.L.","contributorId":84393,"corporation":false,"usgs":true,"family":"Pomes","given":"M.L.","affiliations":[],"preferred":false,"id":185388,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meyer, M. 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,{"id":27283,"text":"wri954209 - 1995 - Regional water table (1994) and water-level changes in the Morongo Basin, San Bernardino County, California","interactions":[],"lastModifiedDate":"2022-03-29T17:21:41.312289","indexId":"wri954209","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-4209","title":"Regional water table (1994) and water-level changes in the Morongo Basin, San Bernardino County, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954209","collaboration":"Prepared in cooperation with the Mojave Water Agency, and the U.S. Marine Corps, Department of the Navy","usgsCitation":"Trayler, C.R., and Koczot, K.M., 1995, Regional water table (1994) and water-level changes in the Morongo Basin, San Bernardino County, California: U.S. Geological Survey Water-Resources Investigations Report 95-4209, 1 Plate: 47.42 x 33.03 inches, https://doi.org/10.3133/wri954209.","productDescription":"1 Plate: 47.42 x 33.03 inches","costCenters":[],"links":[{"id":397784,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4209/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159033,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4209/report-thumb.jpg"}],"country":"United States","state":"California","county":"San Bernardino County","otherGeospatial":"Morongo Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.1,\n              34.1\n            ],\n            [\n              -116,\n              34.1\n            ],\n            [\n              -116,\n              34.7\n            ],\n            [\n              -117.1,\n              34.7\n            ],\n            [\n              -117.1,\n              34.1\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634ded","contributors":{"authors":[{"text":"Trayler, Carolyn R.","contributorId":43818,"corporation":false,"usgs":true,"family":"Trayler","given":"Carolyn","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":197848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koczot, Kathryn M. 0000-0001-5728-9798 kmkoczot@usgs.gov","orcid":"https://orcid.org/0000-0001-5728-9798","contributorId":2039,"corporation":false,"usgs":true,"family":"Koczot","given":"Kathryn","email":"kmkoczot@usgs.gov","middleInitial":"M.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":197849,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23280,"text":"ofr94704 - 1995 - Ground-water data for the Suck Creek area of Walden Ridge, southern Cumberland Plateau, Marion County, Tennessee","interactions":[],"lastModifiedDate":"2026-04-08T15:36:03.854238","indexId":"ofr94704","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-704","title":"Ground-water data for the Suck Creek area of Walden Ridge, southern Cumberland Plateau, Marion County, Tennessee","docAbstract":"An investigation was made of the ground-water resources of the Suck Creek area, Marion County, Tennessee, 1990-91. Suck Creek is located on the Walden Ridge section of the Cumberland Plateau, and is about 16 miles northwest of Chattanooga. Eight wells were drilled into bedrock of Pennsylvania age. Drilling sites were chosen at or near fracture traces. Yields of the eight wells ranged from less than 1 to as much as 80 gallons of water per minute. Three wells had yields of 50 gallons per minute or more; two of these had estimated yields of 75 to 80 gallons per minute. These three wells produced water from a well- developed fracture within the Sewanee Conglomerate. Specific capacities for these three wells were 1.1, 1.3, 2.2 gallons per minute per foot of drawdown. Samples of water from six test wells and three domestic wells were analyzed for major inorganic constituents, nurients, major metals, trace elements, and bacteria. In addition, water samples from two of the test wells were analyzed for volatile organic compounds and scanned for the presence of semi-volatile organic compounds. Iron exceeded 300 micrograms per liter in five of the nine samples, and manganese exceeded 50 micrograms per liter in seven of the nine water samples. Toluene, a volatile organic compound, was detected in a concentration slightly above the reporting level; no other volatile organic compounds were detected.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94704","issn":"0094-9140","usgsCitation":"Hanchar, D., 1995, Ground-water data for the Suck Creek area of Walden Ridge, southern Cumberland Plateau, Marion County, Tennessee: U.S. Geological Survey Open-File Report 94-704, iv, 15 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94704.","productDescription":"iv, 15 p.","costCenters":[],"links":[{"id":156090,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1367,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1994/ofr_94-704/index.html","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Tennessee","county":"Marion County","otherGeospatial":"Cumberland 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,{"id":23762,"text":"ofr95423 - 1995 - Water-resources activities in Arkansas, 1992-94","interactions":[],"lastModifiedDate":"2012-02-02T00:08:11","indexId":"ofr95423","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-423","title":"Water-resources activities in Arkansas, 1992-94","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Report Section [distributor],","doi":"10.3133/ofr95423","issn":"0094-9140","usgsCitation":"Louthian, B.L., 1995, Water-resources activities in Arkansas, 1992-94: U.S. Geological Survey Open-File Report 95-423, iv, 44 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95423.","productDescription":"iv, 44 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0423/report-thumb.jpg"},{"id":52992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0423/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa147","contributors":{"authors":[{"text":"Louthian, Bobbie L. louthian@usgs.gov","contributorId":737,"corporation":false,"usgs":true,"family":"Louthian","given":"Bobbie","email":"louthian@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":190673,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23539,"text":"ofr95322 - 1995 - Vertical hydraulic conductivity of soil and potentiometric surface of the Missouri River alluvial aquifer at Kansas City, Missouri and Kansas — August 1992 and January 1993","interactions":[],"lastModifiedDate":"2021-12-30T20:32:31.733962","indexId":"ofr95322","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-322","title":"Vertical hydraulic conductivity of soil and potentiometric surface of the Missouri River alluvial aquifer at Kansas City, Missouri and Kansas — August 1992 and January 1993","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95322","issn":"0094-9140","usgsCitation":"Kelly, B.P., and Blevins, D.W., 1995, Vertical hydraulic conductivity of soil and potentiometric surface of the Missouri River alluvial aquifer at Kansas City, Missouri and Kansas — August 1992 and January 1993: U.S. Geological Survey Open-File Report 95-322, Report: v, 19 p.; 5 Plates: 41.00 × 23.00 inches, https://doi.org/10.3133/ofr95322.","productDescription":"Report: v, 19 p.; 5 Plates: 41.00 × 23.00 inches","costCenters":[],"links":[{"id":393699,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18452.htm"},{"id":52827,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0322/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19475,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0322/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19474,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0322/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19473,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0322/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19472,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0322/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19471,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0322/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154885,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0322/report-thumb.jpg"}],"country":"United States","state":"Kansas, Missouri","otherGeospatial":"Missouri River alluvial aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.899,\n              39.0590\n            ],\n            [\n              -94.126,\n              39.0590\n            ],\n            [\n              -94.126,\n              39.274\n            ],\n            [\n              -94.899,\n              39.274\n            ],\n            [\n              -94.899,\n              39.0590\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6020c4","contributors":{"authors":[{"text":"Kelly, B. P.","contributorId":30653,"corporation":false,"usgs":true,"family":"Kelly","given":"B.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":190282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blevins, D. W.","contributorId":75940,"corporation":false,"usgs":true,"family":"Blevins","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":190283,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23277,"text":"ofr95386 - 1995 - Hydrogeologic and water-quality data for the explosive experimental area, Naval Surface Warfare Center, Dahlgren Site, Dahlgren, Virginia","interactions":[],"lastModifiedDate":"2022-07-20T19:54:53.940777","indexId":"ofr95386","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-386","title":"Hydrogeologic and water-quality data for the explosive experimental area, Naval Surface Warfare Center, Dahlgren Site, Dahlgren, Virginia","docAbstract":"Hydrogeologic and water-quality data were collected at the Explosive Experimental Area, Naval Surface Warfare Center, Dahlgren Site at Dahlgren, Virginia, as part of a hydrogeologic assessment of the shallow aquifer system begun in 1993. The U.S. Geological Survey conducted this study to provide the U.S. Navy with hydrogeologic data to aid in the evaluation of the effects from remediation of contaminated sites and to protect against additional contamination. This report describes the ground-water observation- well network, hydrogeologic, and water-quality data collected between October 1993 and April 1995. The report includes a description of the locations and construction of 28 observation wells on the Explosive Experimental Area. Hydrogeologic data include lithologic logs, geophysical logs, and vertical hydraulic conductivity measurements of selected core intervals. Hydrologic data include synoptic and hourly measurements of ground-water levels, and observation-well slug tests to determine horizontal hydraulic conductivity. Water-quality data include analyses of major dissolved constituents in ground water and surface water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95386","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Hammond, E.C., and Bell, C.F., 1995, Hydrogeologic and water-quality data for the explosive experimental area, Naval Surface Warfare Center, Dahlgren Site, Dahlgren, Virginia: U.S. Geological Survey Open-File Report 95-386, Report: iv, 68 p.; 1 Plate: 19.00 × 17.00 inches; Application Site, https://doi.org/10.3133/ofr95386.","productDescription":"Report: iv, 68 p.; 1 Plate: 19.00 × 17.00 inches; Application Site","costCenters":[],"links":[{"id":404158,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18470.htm","linkFileType":{"id":5,"text":"html"}},{"id":277684,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1995/0386/application.zip"},{"id":52564,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0386/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19444,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0386/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0386/report-thumb.jpg"}],"country":"United States","state":"Virginia","city":"Dahlgren","otherGeospatial":"Naval Surface Warfare Center, Dahlgren Site","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.070,\n              38.284\n            ],\n            [\n              -77.009,\n              38.284\n            ],\n            [\n              -77.009,\n              38.319\n            ],\n            [\n              -77.070,\n              38.319\n            ],\n            [\n              -77.070,\n              38.284\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628caf","contributors":{"authors":[{"text":"Hammond, E. C.","contributorId":34544,"corporation":false,"usgs":true,"family":"Hammond","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":189800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bell, C. F.","contributorId":14449,"corporation":false,"usgs":true,"family":"Bell","given":"C.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":189799,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21972,"text":"ofr95210 - 1995 - National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 1","interactions":[],"lastModifiedDate":"2012-02-02T00:07:45","indexId":"ofr95210","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-210","title":"National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 1","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"National Earthquake Hazards Reduction Program, annual project summaries, XXXVI","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr95210","issn":"0094-9140","usgsCitation":"Jacobson, M.L., 1995, National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 1 (Volume 1): U.S. Geological Survey Open-File Report 95-210, Volume 1 - Total: 592 p.; Report: Pages 1-574; Index: I1-I13, https://doi.org/10.3133/ofr95210.","productDescription":"Volume 1 - Total: 592 p.; Report: Pages 1-574; Index: I1-I13","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":152892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0210/report-thumb.jpg"},{"id":51448,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0210/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Volume 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69894b","contributors":{"authors":[{"text":"Jacobson, Muriel L. (compiler)","contributorId":42965,"corporation":false,"usgs":true,"family":"Jacobson","given":"Muriel","suffix":"(compiler)","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":186501,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26584,"text":"wri954097 - 1995 - Geochemical processes in ground water resulting from surface mining of coal at the Big Sky and West Decker Mine areas, southeastern Montana","interactions":[],"lastModifiedDate":"2025-01-08T21:55:11.888669","indexId":"wri954097","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-4097","title":"Geochemical processes in ground water resulting from surface mining of coal at the Big Sky and West Decker Mine areas, southeastern Montana","docAbstract":"A potential hydrologic effect of surface mining of coal in southeastern Montana is a change in the quality of ground water. Dissolved-solids concen- trations in water in spoils aquifers generally are larger than concentrations in water in the coal aquifers they replaced; however, laboratory experiments have indicated that concentrations can decrease if ground water flows from coal-mine spoils to coal. This study was conducted to determine if decreases in concentrations occur onsite and, if so, which geochemical processes caused the decreases. Solid-phase core samples of spoils, unmined over- burden, and coal, and ground-water samples were collected from 16 observation wells at two mine areas. In the Big Sky Mine area, changes in ground- water chemistry along a flow path from an upgradient coal aquifer to a spoils aquifer probably were a result of dedolomitization. Dissolved-solids concentrations were unchanged as water flowed from a spoils aquifer to a downgradient coal aquifer. In the West Decker Mine area, dissolved-solids concentrations apparently decreased from about 4,100 to 2,100 milligrams per liter as water moved along an inferred flow path from a spoils aquifer to a downgradient coal aquifer. Geochemical models were used to analyze changes in water chemistry on the basis of results of solid-phase and aqueous geochemical characteristics. Geochemical processes postulated to result in the apparent decrease in dissolved-solids concentrations along this inferred flow path include bacterial reduction of sulfate, reverse cation exchange within the coal, and precipitation of carbonate and iron-sulfide minerals.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954097","usgsCitation":"Clark, D., 1995, Geochemical processes in ground water resulting from surface mining of coal at the Big Sky and West Decker Mine areas, southeastern Montana: U.S. Geological Survey Water-Resources Investigations Report 95-4097, vi, 80 p., https://doi.org/10.3133/wri954097.","productDescription":"vi, 80 p.","costCenters":[],"links":[{"id":123515,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4097/report-thumb.jpg"},{"id":55453,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4097/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":465912,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48202.htm","text":"Big Sky Mine area","linkFileType":{"id":5,"text":"html"}},{"id":465913,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48203.htm","text":"West Decker Mine area","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana","otherGeospatial":"Big Sky and West Decker Mine areas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107,\n              46\n            ],\n            [\n              -107,\n              45\n            ],\n            [\n              -106,\n              45\n            ],\n            [\n              -106,\n              46\n            ],\n            [\n              -107,\n              46\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adefa","contributors":{"authors":[{"text":"Clark, D.W.","contributorId":22765,"corporation":false,"usgs":true,"family":"Clark","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":196660,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26733,"text":"wri944253 - 1995 - Geochemistry of ground water in the Gallup, Dakota, and Morrison aquifers, San Juan Basin, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri944253","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-4253","title":"Geochemistry of ground water in the Gallup, Dakota, and Morrison aquifers, San Juan Basin, New Mexico","docAbstract":"Ground water was sampled from wells completed in the Gallup,\r\nDakota, and Morrison aquifers in the San Juan Basin, New Mexico,\r\nto examine controls on solute concentrations. Samples were \r\ncollected from 38 wells primarily from the Morrison aquifer (25 \r\nwells) in the northwestern part of the basin. A series of samples\r\nwas collected along ground-water flow paths; dissolved \r\nconstituents varied horizontally and vertically.\r\n\r\n     The understanding of the flow system changed as a result of\r\nthe geochemical analyses. The conceptual model of the flow system in\r\nthe Morrison aquifer prior to the study reported here assumed the\r\nWestwater Canyon Member of the Morrison aquifer as the only \r\nsignificant regional aquifer; flow was assumed to be two \r\ndimensional; and vertical leakage was assumed to be negligible.\r\nThe geochemical results indicate that the Westwater Canyon Member\r\nis not the only major water-yielding zone and that the flow\r\nsystem is three dimensional. The data presented in this report \r\nsuggest an upward component of flow into the Morrison aquifer. The \r\nentire section above and below the Morrison aquifer appears to be \r\ncontrolled by a three-dimensional flow regime where saline brine\r\nleaks near the San Juan River discharge area.\r\n\r\n     Predominant ions in the Gallup aquifer were calcium\r\nbicarbonate in recharge areas and sodium sulfate in discharge areas.  \r\nIn the Dakota aquifer, predominant ions were sodium bicarbonate and\r\nsodium sulfate. Water in the Morrison aquifer was predominantly sodium \r\nbicarbonate in the recharge area, changing to sodium sulfate \r\ndowngradient.\r\n\r\n     Chemical and radioisotopic data indicate that water from \r\noverlying and underlying units mixes with recharge water in the \r\nMorrison aquifer. Recharge water contained a large ratio of \r\nchlorine-36 to chlorine and a small ratio of bromide to chloride.\r\nApproximately 10 miles downgradient, samples from four wells \r\ncompleted in the Morrison aquifer were considerably different in\r\ncomposition compared to recharge samples. Oxygen stable isotopes\r\ndecreased by 2.8 per mil and deuterium decreased 26 per mil, \r\nrelative to recharge. Carbon-14 radioisotope activities were not\r\ndetectable. Chloride-36 radioisotope ratios were small and\r\nbromide to chloride concentration ratios were large. These results\r\nsuggest two potentially viable processes: ion filtration or trapping of\r\nancient dilute water recharged under a humid climate. For water\r\nsamples near the San Juan River, pH decreased to about 8.0, \r\nchloride concentrations increased to more than 100 milligrams per\r\nliter, and ratios of chlorine-36 to chlorine and bromide to \r\nchloride were small. Leakage of deep basin brine into the fresher\r\nwater of the Morrison aquifer appears to control ion concentrations.","language":"ENGLISH","publisher":"U.S. Geological Survey, [Water Resources Division, New Mexico District] ;\r\nCan be purchased from U.S.G.S. Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/wri944253","usgsCitation":"Dam, W.L., 1995, Geochemistry of ground water in the Gallup, Dakota, and Morrison aquifers, San Juan Basin, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 94-4253, vii, 76 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944253.","productDescription":"vii, 76 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":125156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4253/report-thumb.jpg"},{"id":55609,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4253/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6aaeb3","contributors":{"authors":[{"text":"Dam, W. L.","contributorId":100890,"corporation":false,"usgs":true,"family":"Dam","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196906,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19871,"text":"ofr95395 - 1995 - Report on the U.S. Geological Survey's evaluation program for standard reference samples distributed in May 1995 : T-135 (trace constituents), M-134 (major constituents), N-45 (nutrients), N-46 (nutrients), P-24 (low ionic strength), Hg-20 (mercury), and SED-5 (bed material)","interactions":[],"lastModifiedDate":"2012-02-02T00:07:42","indexId":"ofr95395","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-395","title":"Report on the U.S. Geological Survey's evaluation program for standard reference samples distributed in May 1995 : T-135 (trace constituents), M-134 (major constituents), N-45 (nutrients), N-46 (nutrients), P-24 (low ionic strength), Hg-20 (mercury), and SED-5 (bed material)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr95395","usgsCitation":"Long, H., and Farrar, J., 1995, Report on the U.S. Geological Survey's evaluation program for standard reference samples distributed in May 1995 : T-135 (trace constituents), M-134 (major constituents), N-45 (nutrients), N-46 (nutrients), P-24 (low ionic strength), Hg-20 (mercury), and SED-5 (bed material): U.S. Geological Survey Open-File Report 95-395, iii, 135 p. :ill. ;28 cm., https://doi.org/10.3133/ofr95395.","productDescription":"iii, 135 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":153392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0395/report-thumb.jpg"},{"id":49381,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0395/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62f64d","contributors":{"authors":[{"text":"Long, H.K.","contributorId":50547,"corporation":false,"usgs":true,"family":"Long","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":181667,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrar, J.W.","contributorId":26715,"corporation":false,"usgs":true,"family":"Farrar","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":181666,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21879,"text":"ofr95813 - 1995 - Hydrologic effects associated with the January 17, 1994 Northridge, California, earthquake","interactions":[],"lastModifiedDate":"2019-09-06T15:49:42","indexId":"ofr95813","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-813","title":"Hydrologic effects associated with the January 17, 1994 Northridge, California, earthquake","docAbstract":"<p>This report compiles hydrologic observations in southern California associated with the 1994 Mw = 6.7 Northridge, California earthquake. In southern California, the largest ground water level change was a drop of 52 cm at Crystalaire. Most of the steplike water-level changes recorded following the Northridge earthquake agreed in direction with the sign of the calculated coseismic volume strain field. A spring discharge increase at Southern Pacific Springs was reported to have preceded the earthquake by several days. Outside of southern California, water-level changes were also observed, but are not consistent in sign or size with the static strain field of the earthquake sequence.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95813","issn":"0566-8174","usgsCitation":"Quilty, E., Farrar, C.D., Galloway, D., Hamlin, S.N., Laczniak, R.J., Roeloffs, E., Sorey, M., and Woodcock, D., 1995, Hydrologic effects associated with the January 17, 1994 Northridge, California, earthquake: U.S. Geological Survey Open-File Report 95-813, ii, 47 p., https://doi.org/10.3133/ofr95813.","productDescription":"ii, 47 p.","numberOfPages":"49","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":51367,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0813/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0813/report-thumb.jpg"}],"country":"United States","state":"California, Nevada, Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -125.41992187499999,\n              31.615965936476076\n            ],\n            [\n              -113.99414062499999,\n              31.615965936476076\n            ],\n            [\n              -113.99414062499999,\n              43.100982876188546\n            ],\n            [\n              -125.41992187499999,\n              43.100982876188546\n            ],\n            [\n              -125.41992187499999,\n              31.615965936476076\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607120","contributors":{"authors":[{"text":"Quilty, E.G.","contributorId":87160,"corporation":false,"usgs":true,"family":"Quilty","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":186096,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrar, C. D.","contributorId":71978,"corporation":false,"usgs":true,"family":"Farrar","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":186094,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Galloway, D. L. 0000-0003-0904-5355","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":31383,"corporation":false,"usgs":true,"family":"Galloway","given":"D. L.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":false,"id":186091,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hamlin, S. N.","contributorId":46560,"corporation":false,"usgs":true,"family":"Hamlin","given":"S.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":186093,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Laczniak, R. J.","contributorId":46104,"corporation":false,"usgs":true,"family":"Laczniak","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":186092,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Roeloffs, E.A.","contributorId":88742,"corporation":false,"usgs":true,"family":"Roeloffs","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":186097,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":186095,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Woodcock, D.E.","contributorId":8499,"corporation":false,"usgs":true,"family":"Woodcock","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":186090,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":22248,"text":"ofr95596 - 1995 - USGS spectral response maps and their relationship with seismic design forces in building codes","interactions":[],"lastModifiedDate":"2012-02-02T00:07:57","indexId":"ofr95596","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-596","title":"USGS spectral response maps and their relationship with seismic design forces in building codes","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95596","issn":"0094-9140","usgsCitation":"Leyendecker, E.V., Perkins, D.M., Algermissen, S.T., Thenhaus, P., and Hanson, S., 1995, USGS spectral response maps and their relationship with seismic design forces in building codes (Online only, Version 1.0): U.S. Geological Survey Open-File Report 95-596, vii, 60 p. (some folded) :ill., maps; data files, https://doi.org/10.3133/ofr95596.","productDescription":"vii, 60 p. (some folded) :ill., maps; data files","onlineOnly":"Y","costCenters":[],"links":[{"id":108956,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18522.htm","linkFileType":{"id":5,"text":"html"},"description":"18522"},{"id":1333,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/596/","linkFileType":{"id":5,"text":"html"}},{"id":155166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0596/report-thumb.jpg"},{"id":51675,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0596/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f8d4","contributors":{"authors":[{"text":"Leyendecker, E. V.","contributorId":87162,"corporation":false,"usgs":true,"family":"Leyendecker","given":"E.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":187768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perkins, D. M.","contributorId":83922,"corporation":false,"usgs":true,"family":"Perkins","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":187767,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Algermissen, Sylvester Theodore","contributorId":94300,"corporation":false,"usgs":true,"family":"Algermissen","given":"Sylvester","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":187769,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thenhaus, P.C.","contributorId":46089,"corporation":false,"usgs":true,"family":"Thenhaus","given":"P.C.","affiliations":[],"preferred":false,"id":187765,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hanson, S.L.","contributorId":47361,"corporation":false,"usgs":true,"family":"Hanson","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":187766,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":22941,"text":"ofr95417 - 1995 - Flood magnitude and frequency of Hollow Brook at the culvert on New Jersey route 35, at Neptune Township, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:55","indexId":"ofr95417","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-417","title":"Flood magnitude and frequency of Hollow Brook at the culvert on New Jersey route 35, at Neptune Township, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95417","issn":"0094-9140","usgsCitation":"Dunne, P., 1995, Flood magnitude and frequency of Hollow Brook at the culvert on New Jersey route 35, at Neptune Township, New Jersey: U.S. Geological Survey Open-File Report 95-417, iv, 5 p. :map ;28 cm., https://doi.org/10.3133/ofr95417.","productDescription":"iv, 5 p. :map ;28 cm.","costCenters":[],"links":[{"id":154282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0417/report-thumb.jpg"},{"id":52342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0417/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef015","contributors":{"authors":[{"text":"Dunne, Paul","contributorId":86794,"corporation":false,"usgs":true,"family":"Dunne","given":"Paul","email":"","affiliations":[],"preferred":false,"id":189167,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21863,"text":"ofr9575G - 1995 - Hydrocarbon source rock characterization and maturity based on rock-eval pyrolysis and vitrinite reflectance of Eocene strata, southern Oregon Coast Range, Douglas and Coos Counties, southwest Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr9575G","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-75","chapter":"G","title":"Hydrocarbon source rock characterization and maturity based on rock-eval pyrolysis and vitrinite reflectance of Eocene strata, southern Oregon Coast Range, Douglas and Coos Counties, southwest Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9575G","issn":"0566-8174","usgsCitation":"Lillis, P.G., Daws, T., Pawlewicz, M., Niem, A.R., and Ryu, I., 1995, Hydrocarbon source rock characterization and maturity based on rock-eval pyrolysis and vitrinite reflectance of Eocene strata, southern Oregon Coast Range, Douglas and Coos Counties, southwest Oregon: U.S. Geological Survey Open-File Report 95-75, 27 p.; 30 leaves :ill., map ;28 cm., https://doi.org/10.3133/ofr9575G.","productDescription":"27 p.; 30 leaves :ill., map ;28 cm.","costCenters":[],"links":[{"id":153025,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0075g/report-thumb.jpg"},{"id":51349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0075g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db6296a1","contributors":{"authors":[{"text":"Lillis, Paul G. 0000-0002-7508-1699 plillis@usgs.gov","orcid":"https://orcid.org/0000-0002-7508-1699","contributorId":1817,"corporation":false,"usgs":true,"family":"Lillis","given":"Paul","email":"plillis@usgs.gov","middleInitial":"G.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":186025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daws, T.A.","contributorId":56651,"corporation":false,"usgs":true,"family":"Daws","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":186027,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pawlewicz, M. J.","contributorId":75111,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"M. J.","affiliations":[],"preferred":false,"id":186029,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Niem, A. R.","contributorId":54984,"corporation":false,"usgs":true,"family":"Niem","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":186026,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ryu, In-Chang","contributorId":69584,"corporation":false,"usgs":true,"family":"Ryu","given":"In-Chang","email":"","affiliations":[],"preferred":false,"id":186028,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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