Coal test drilling in the Thar Desert of southeast Pakistan was conducted as part of the Coal Exploration and Assessment Program (COALREAP) involving the United States Agency for International Development (USAID), the Geological Survey of Pakistan (GSP), and the U.S. Geological Survey. Drilling was performed in the Thar Desert, or Great Indian Desert, approximately 175 km northeast of Karachi. Twenty five exploration holes were drilled between January 1992 and May 1994. Drill core was described by geologists of the Pakistan Geological Survey and coal samples were analyzed in both the United States and Pakistan. U.S. Geological Survey geologists offered technical assistance, trained GSP personnel, and managed the drilling program according to an agreement with USAID under the Energy Planning and Development Project.
Drilling was performed by the Geological Survey of Pakistan. During drilling, the first 50 m was rotary drilled and cuttings collected every 2 m for examination. Average depth for all coal beds is 214 m with a total average thickness of 10 m of coal per drill hole. Core was described, boxed, and stored at the Geological Survey of Pakistan core library at Sonda, near Hyderabad. Approximately 6,412 m of Paleocene to Eocene rock was drilled of which 3,990 m was cored and 1,113 m was rotary drilled.
There was 1,309 m of core loss. Geophysical logging of each drill hole permitted detailed thicknesses of coal to be determined. Analysis of the coal indicated a rank of lignite B with an as-received heating value over 5,000 Btu.
This report presents data collected at the drill sites and should be used in
conjunction with the published interpretive report (Fassett and Durrani, 1994) and the USGS Open-File Report 94-167, which contains analysis of the coal samples. Tables provide quick reference to numeric data and results. Detailed index maps and specific data, for each drill hole are included. This report covers drill holes TP-5 to TP-31. Drill holes TP-16, 17, 21, 26, 27, and 29 were planned but not drilled due to time restraints and (or) a determination that those drill sites were not needed to effectively delineate the coal deposit. The basic data for drill holes TP-1 through TP-4 are included in SanFilipo and others, 1994 however, some data for these drill holes are included for consistency.
Ground-water level measurements from 30 wells in the Brightseat-upper Potomac aquifer in the Coastal Plain Physiographic Province of Virginia in 1993 were used to prepare a map of the potentiometric surface of the aquifer. The map shows the potentiometric surface of the Brightseat-upper Potomac aquifer indicating a regional trend toward the Chesapeake Bay and Atlantic Ocean. The potentiometric-surface data indicate that cones of depression are apparent around West Point and in southeastern Isle of Wight County near Franklin, Virginia. The highest ground-water-level measurement was 4 feet above sea level in northern Accomack County, and the lowest ground-water-level measurement was 117 feet below sea level in Franklin, Virginia.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94370","usgsCitation":"Hammond, E.C., McFarland, E.R., and Focazio, M., 1994, Potentiometric surface of the Brightseat-upper Potomac Aquifer in Virginia, 1993: U.S. Geological Survey Open-File Report 94-370, 1 p., https://doi.org/10.3133/ofr94370.","productDescription":"1 p.","costCenters":[],"links":[{"id":160995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0370/report-thumb.jpg"},{"id":390985,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12510.htm"},{"id":59992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0370/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Virginia","otherGeospatial":"Brightseat-upper Potomac aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78,\n 36.48\n ],\n [\n -75.119,\n 36.48\n ],\n [\n -75.119,\n 39\n ],\n [\n -78,\n 39\n ],\n [\n -78,\n 36.48\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683061","contributors":{"authors":[{"text":"Hammond, E. C.","contributorId":34544,"corporation":false,"usgs":true,"family":"Hammond","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":206936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McFarland, E. R.","contributorId":65109,"corporation":false,"usgs":true,"family":"McFarland","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":206938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Focazio, M. J.","contributorId":62997,"corporation":false,"usgs":true,"family":"Focazio","given":"M. J.","affiliations":[],"preferred":false,"id":206937,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28553,"text":"wri944053 - 1994 - Iodine-129 in the Snake River Plain aquifer at and near the Idaho National Engineering Laboratory, Idaho, 1990-91","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri944053","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-4053","title":"Iodine-129 in the Snake River Plain aquifer at and near the Idaho National Engineering Laboratory, Idaho, 1990-91","docAbstract":"From 1953 to 1990, an estimated 0.56 to 1.18 curies of iodine-129 were contained in wastewater generated by the Idaho Chemical Processing Plant (ICPP) at the Idaho National Engineering Laboratory. The waste- water was discharged directly to the Snake River Plain aquifer through a deep disposal well prior to February 1984 and through unlined disposal ponds in 1984-90. The wastewater did not contain measurable concentrations of iodine-129 in 1989-90. Samples were collected from 51 wells that obtain water from the Snake River Plain aquifer and 1 well that obtains water from a perched ground-water zone. The samples were analyzed for iodine-129 using an accelerator mass spectrometer which is two to six orders of magnitude more sensitive than neutron- activation methods. Therefore, iodine-129 was detectable in samples from a larger number of wells distributed over a larger area than previously was possible. Ground-water flow velocities calculated using iodine-129 data are estimated to be at least 6 feet per day. These velocities compare favorably with those of 4 to 10 feet per day calculated from tritium data and tracer studies at wells down- gradient from the ICPP. In 1990-91, concentrations of iodine-129 in water samples from wells that obtain water from the Snake River Plain aquifer ranged from less than 0.0000006+0.0000002 to 3.82.+0.19 picocuries per liter (pCi/L). The mean concentration in water from 18 wells was 0.81+0.19 pCi/L as compared with 1.30+0.26 pCi/L in 1986. The decrease in the iodine-l29 concentrations from 1986 to 1990-91 chiefly was the result of a decrease in the amount of iodine-129 disposed of annually, and changes in disposal techniques.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944053","usgsCitation":"Mann, L., and Beasley, T., 1994, Iodine-129 in the Snake River Plain aquifer at and near the Idaho National Engineering Laboratory, Idaho, 1990-91: U.S. Geological Survey Water-Resources Investigations Report 94-4053, iv, 27 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944053.","productDescription":"iv, 27 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4053/report-thumb.jpg"},{"id":57382,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4053/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667300","contributors":{"authors":[{"text":"Mann, L. J.","contributorId":39392,"corporation":false,"usgs":true,"family":"Mann","given":"L. J.","affiliations":[],"preferred":false,"id":200014,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beasley, T.M.","contributorId":74788,"corporation":false,"usgs":true,"family":"Beasley","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":200015,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28756,"text":"wri924013 - 1994 - Geohydrology and water quality of stratified-drift aquifers in the lower Connecticut River basin, southwestern New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri924013","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"92-4013","title":"Geohydrology and water quality of stratified-drift aquifers in the lower Connecticut River basin, southwestern New Hampshire","docAbstract":"Stratified-drift aquifers discontinuously underlie 116 square miles of the Lower Connecticut River basin in southwestern New Hampshire, which has a total drainage area of 1,163 square miles. Saturated thicknesses of stratified drift within the study area are locally greater than 400 feet but generally are less. Transmissivities 1ocally exceeds 4,000 feet squared per day but are generally much less. The 20.8 square mile, or 1.8 percent, of the study area identified as having transmissivity greater than 1,000 feet squared per day represents a valuable resource. The geohydrology of stratified- drift aquifers was investigated by focusing on basic aquifer properties, including aquifer boundaries; recharge, discharge, and direction of ground-water flow; saturated thickness and storage; and transmissivity. Surficial geologic mapping assisted in the determination of aquifer boundaries. Data from more than 2,300 wells, test borings, and springs were used to produce maps of water-table altitude, saturated thickness, and transmissivity of-stratified drift. Seismic-refraction profiles were completed at 29 locations in the study area. These profiles aided in the construction of the water-table and saturated-thickness maps. Seismic- reflection data were also collected along 60 miles of the Connecticut River. A stratified-drift aquifer in southern Croydon and northern Newport was analyzed for aquifer yield using transient simulations and a two-dimensional, finite-difference ground-water-flow model. The objective was to estimate the yield after a 180-day period of pumping. Two hypothetical wells were pumped at 1.0 Mgal/d and 0.5 Mgal/d for 180 days respectively. The amount of water available for infiltration was the limiting factor. Results of analysis of water samples from 22 wells and 8 spring show that, with some exceptions, water in the stratified-drift aquifer generally meets the U.S. Environmental Protection Agency's primary and secondary drinking-water regulations.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri924013","usgsCitation":"Moore, R.B., Johnson, C., and Douglas, E., 1994, Geohydrology and water quality of stratified-drift aquifers in the lower Connecticut River basin, southwestern New Hampshire: U.S. Geological Survey Water-Resources Investigations Report 92-4013, 1 v. (various paging) :ill., maps (some col.) ;28 cm. [PGS - 325 p.], https://doi.org/10.3133/wri924013.","productDescription":"1 v. (various paging) :ill., maps (some col.) ;28 cm. [PGS - 325 p.]","costCenters":[],"links":[{"id":123676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4013/report-thumb.jpg"},{"id":57616,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4013/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57617,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4013/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57618,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4013/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57619,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4013/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57620,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4013/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6880d5","contributors":{"authors":[{"text":"Moore, R. B.","contributorId":98720,"corporation":false,"usgs":true,"family":"Moore","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":200347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, C. D.","contributorId":8120,"corporation":false,"usgs":true,"family":"Johnson","given":"C. D.","affiliations":[],"preferred":false,"id":200345,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Douglas, E.M.","contributorId":60685,"corporation":false,"usgs":true,"family":"Douglas","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":200346,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30522,"text":"wri924187 - 1994 - Hydrology and geochemistry of a surface coal mine in northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri924187","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"92-4187","title":"Hydrology and geochemistry of a surface coal mine in northwestern Colorado","docAbstract":"The hydrology and geochemistry of a reclaimed coal mine in northwestern Colorado were monitored during water years 1988 and 1989. Some data also were collected in water years 1987 and 1990. This report describes (1) the sources of hydrologic recharge to and discharge from reclaimed spoil, (2) the relative contributions of recharge to the reclaimed spoil aquifer from identified source waters and the rate of water movement from those sources to the reclaimed spoil, and (3) the geochemical reactions that control water quality in reclaimed spoil. The study area was at a dip-slope coal mine encompassing about 7 square miles with land slopes of varying aspect. The area was instrumented and monitored at five sites; two sites had unmined and reclaimed- spoil areas adjacent to each other and three sites were unmined. The mined areas had been reclaimed. Instrumentation at the study sites included 1 climate station, 3 rain gages, 19 soil-water access tubes, 2 lysimeters, 18 wells completed in bedrock, 7 wells completed in reclaimed spoil, and 2 surface- water gaging stations. The results of the study indicate that the reclaimed spoil is recharged from surface recharge and underburden aquifers. Discharge, as measured by lysimeters, was about 3 inches per year and occurred during and after snowmelt. Hydraulic-head measurements indicated a potential for ground-water movement from deeper to shallower aquifers. Water levels rose in the reclaimed-spoil aquifer and spring discharge at the toe of the spoil slopes increased rapidly in response to snowmelt. Water chemistry, stable isotopes, geochemical models, and mass-balance calculations indicate that surface recharge and the underburden aquifers each contribute about 50 percent of the water to the reclaimed-spoil aquifers. Geochemical information indicates that pyrite oxidation and dissolution of carbonate and efflorescent sulfate minerals control the water chemistry of the reclaimed-spoil aquifer.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri924187","usgsCitation":"Williams, R., and Clark, G.M., 1994, Hydrology and geochemistry of a surface coal mine in northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 92-4187, vi, 61 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924187.","productDescription":"vi, 61 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124119,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4187/report-thumb.jpg"},{"id":59301,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604da8","contributors":{"authors":[{"text":"Williams, R.S. Jr.","contributorId":46102,"corporation":false,"usgs":true,"family":"Williams","given":"R.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":203394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, G. M.","contributorId":90325,"corporation":false,"usgs":true,"family":"Clark","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":203395,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29284,"text":"wri934233 - 1994 - Use of landsat thematic mapper data to identify crop types and estimate irrigated acreage, Uvalde and Medina counties, Texas, 1991","interactions":[],"lastModifiedDate":"2016-08-16T13:58:33","indexId":"wri934233","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"93-4233","title":"Use of landsat thematic mapper data to identify crop types and estimate irrigated acreage, Uvalde and Medina counties, Texas, 1991","docAbstract":"Landsat Thematic Mapper (TM) data were used to estimate that about 51,000 acres of crops were irrigated with water pumped from the Edwards aquifer in Uvalde and Medina Counties, Texas in 1991. Bands 2, 3,4, and 5 from a TM image for August 10,1991, were classified using the maximum-likelihood, unsupervised-classification procedure to identify the areas of crops irrigated in the two counties. Detailed vegetation distribution maps of two calibration sites in the study area, and boundaries of the areas probably irrigated in 1991, were used to interpret the results and to separate probable irrigated areas by county from the rest of the image.
\nAreas calculated for irrigated crops were 31,000 acres for Uvalde County, about 35 percent less than the area calculated using Landsat multispectral scanner (MSS) data in 1989, and 20,000 acres for Medina County, about 13 percent less than in 1989, a total decrease of about 28 percent for the two counties. Quantities of water pumped from the Edwards aquifer to irrigate crops in 1991 were estimated as 65,000 acre-feet for Uvalde County and 18,000 acre-feet for Medina County, a total decrease of about 56 percent from the value calculated using crop acreages from MSS data for 1989. Differences were attributed primarily to greater precipitation in 1991 than in 1989, resulting in smaller irrigation water requirements and less supplemental irrigation in 1991. Differences between results from 1989 and 1991, and between results from Uvalde and Medina Counties in 1991, were attributed primarily to greater precipitation in 1991, particularly in Medina County.
\nThe total number of acres of irrigated crops estimated using Landsat TM data was about 9 percent lower in Uvalde County and about 13 percent lower in Medina County than the number of acres calculated from data reported by the U.S. Department of Agriculture, Agricultural Stabilization and Conservation Service (ASCS). The total quantity of water pumped from the Edwards aquifer for irrigation in the two counties in 1991, about 83,000 acre-feet, was about 5 percent greater than the quantity calculated from data reported by the ASCS.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri934233","collaboration":"Prepared in cooperation with the Edwards Underground Water District","usgsCitation":"Raymond, L., and McFarlane, S., 1994, Use of landsat thematic mapper data to identify crop types and estimate irrigated acreage, Uvalde and Medina counties, Texas, 1991: U.S. Geological Survey Water-Resources Investigations Report 93-4233, iii, 19 p., https://doi.org/10.3133/wri934233.","productDescription":"iii, 19 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":58129,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4233/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4233/report-thumb.jpg"}],"country":"United States","state":"Texas","county":"Medina County, Uvalde County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.8056,29.6968],[-98.8042,29.2513],[-98.8039,29.0884],[-99.4107,29.087],[-99.6813,29.0872],[-100.1119,29.0844],[-100.1112,29.3486],[-100.111,29.6236],[-100.0145,29.6237],[-99.6173,29.6257],[-99.6033,29.6257],[-99.4132,29.6253],[-99.0103,29.6187],[-98.9909,29.6185],[-98.982,29.6148],[-98.9794,29.6129],[-98.9789,29.6102],[-98.9779,29.606],[-98.9801,29.5983],[-98.9818,29.5909],[-98.9819,29.5804],[-98.9836,29.5717],[-98.9837,29.5671],[-98.9832,29.5625],[-98.9811,29.5589],[-98.978,29.5556],[-98.9765,29.5547],[-98.9712,29.5533],[-98.9676,29.5546],[-98.9633,29.5578],[-98.9607,29.5578],[-98.9513,29.5581],[-98.9429,29.5585],[-98.9318,29.5588],[-98.9282,29.5593],[-98.9245,29.562],[-98.9213,29.5665],[-98.8056,29.6968]]]},\"properties\":{\"name\":\"Medina\",\"state\":\"TX\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6858c5","contributors":{"authors":[{"text":"Raymond, L.H.","contributorId":23151,"corporation":false,"usgs":true,"family":"Raymond","given":"L.H.","email":"","affiliations":[],"preferred":false,"id":201279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McFarlane, S.I.","contributorId":57504,"corporation":false,"usgs":true,"family":"McFarlane","given":"S.I.","email":"","affiliations":[],"preferred":false,"id":201280,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30353,"text":"wri944071 - 1994 - Traveltime and reaeration characteristics for a reach of the Rio Grande, Albuquerque, New Mexico, October 1991","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri944071","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-4071","title":"Traveltime and reaeration characteristics for a reach of the Rio Grande, Albuquerque, New Mexico, October 1991","docAbstract":"Traveltime characteristics were determined using stream-velocity data and tracer-dye data for a reach of the Rio Grande. Traveltimes determined by the stream-velocity method were virtually the same as those determined by the tracer-dye and tracer-gas technique. The mean velocity of the stream was 1.12 miles per hour at a flow of about 300 cubic feet per second. Reaeration characteristics were determined using a propane tracer gas and a tracer-dye (rhodamine WT). Reaeration coefficients were adjusted for water temperature and the effects of wind movement on the water surface. The peak method-adjusted reaeration-coefficient mean value for the reach was 7.0 per day and ranged from 4.6 to 8.3 per day. The area method-adjusted reaeration- coefficient mean value for the reach was 7.7 per day and ranged from 5.5 to 10.4 per day.","language":"ENGLISH","publisher":"U.S. Geological Survey, [Water Resources Division, New Mexico District] ;\r\nCan be purchased from U.S. Geological Survey, Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/wri944071","usgsCitation":"Waltemeyer, S., 1994, Traveltime and reaeration characteristics for a reach of the Rio Grande, Albuquerque, New Mexico, October 1991: U.S. Geological Survey Water-Resources Investigations Report 94-4071, iv, 19 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944071.","productDescription":"iv, 19 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159849,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4071/report-thumb.jpg"},{"id":59143,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626a1f","contributors":{"authors":[{"text":"Waltemeyer, S. D.","contributorId":65857,"corporation":false,"usgs":true,"family":"Waltemeyer","given":"S. D.","affiliations":[],"preferred":false,"id":203104,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18735,"text":"ofr94319 - 1994 - Compilation of selected hydrologic data, through water year 1992, Black Hills Hydrology Study, western South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:07:24","indexId":"ofr94319","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-319","title":"Compilation of selected hydrologic data, through water year 1992, Black Hills Hydrology Study, western South Dakota","docAbstract":"This report presents water-level, water-quailty, and springflow data that have been collected or compiled, through water year 1992, for the Black Hills Hydrology Study. This study is a long-term cooperative effort between the U.S. Geological Survey, the South Dakota Department of Environmental and Natural Resources, and the West Dakota Water Development District (which represents various local and county cooperators). Water-level data are presented for 32 observation wells and 2 cave sites in the Black Hills area of western South Dakota. The wells are part of a network of observation wells maintained by the South Dakota Department of Environment and Natural Resources and are completed in various bedrock formations that are utilized as aquifers in the Black Hills area. Both cave sites are located within outcrops of the Madison Limestone. Data presented include site descriptions, hydrographs, and tabular data. Water- quality data are presented for 12 surface-water sites and 5 ground-water sites. Data presented include field parameters, bacteria counts, and concentrations of common ions, solids, nutrients, trace elements, radiometrics, cyanide, phenols, dissolved organic carbon, and suspended sediment. Spring data are presented for 83 springs and 21 stream reaches with significant springflow components. Data presented include site information, discharge, and field water-quality parameters including temperature, specific conductance, dissolved oxygen, and pH.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94319","usgsCitation":"Driscoll, D.G., and Bradford, W., 1994, Compilation of selected hydrologic data, through water year 1992, Black Hills Hydrology Study, western South Dakota: U.S. Geological Survey Open-File Report 94-319, vi, 158 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94319.","productDescription":"vi, 158 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151286,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0319/report-thumb.jpg"},{"id":48096,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0319/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a50","contributors":{"authors":[{"text":"Driscoll, Daniel G. dgdrisco@usgs.gov","contributorId":1558,"corporation":false,"usgs":true,"family":"Driscoll","given":"Daniel","email":"dgdrisco@usgs.gov","middleInitial":"G.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":179647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradford, Wendell","contributorId":52987,"corporation":false,"usgs":true,"family":"Bradford","given":"Wendell","affiliations":[],"preferred":false,"id":179648,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18106,"text":"ofr94301 - 1994 - Hydrogeologic and water-quality data for the main site, Naval Surface Warfare Center, Dahlgren Laboratory, Dahlgren, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr94301","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-301","title":"Hydrogeologic and water-quality data for the main site, Naval Surface Warfare Center, Dahlgren Laboratory, Dahlgren, Virginia","docAbstract":"Hydrogeologic and water-quality data were collected at the Naval Surface Warfare Center, Dahlgren Laboratory at Dahlgren, Virginia, as part of a hydrogeologic assessment of the shallow aquifer system begun in 1992. The U.S. Geological Survey conducted this study to provide the Navy with hydrogeologic data to meet the requirements of a Spill Contingency Plan. This report describes the ground-water observation-well network, hydro- geologic, and water-quality data collected between August 1992 and September 1993. The report includes a description of the locations and con- struction of 35 observation wells on the Main Site. Hydrologic data include lithologic core samples, geophysical logs, and vertical hydraulic conductivity measurements of selected core intervals. Hydrologic data include synoptic and hourly measurements of ground-water levels, observation-well slug tests to determine horizontal hydraulic conductivity, and tide data. Water-quality data include analyses of major dissolved constituents in ground water and surface water.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94301","usgsCitation":"Bell, C.F., Bolles, T.P., and Harlow, G., 1994, Hydrogeologic and water-quality data for the main site, Naval Surface Warfare Center, Dahlgren Laboratory, Dahlgren, Virginia: U.S. Geological Survey Open-File Report 94-301, iv, 81 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94301.","productDescription":"iv, 81 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0301/report-thumb.jpg"},{"id":21589,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0301/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47462,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0301/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628c54","contributors":{"authors":[{"text":"Bell, Clifton F.","contributorId":79905,"corporation":false,"usgs":true,"family":"Bell","given":"Clifton","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":178560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bolles, Thomas P.","contributorId":22374,"corporation":false,"usgs":true,"family":"Bolles","given":"Thomas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":178559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harlow, George E. Jr. geharlow@usgs.gov","contributorId":383,"corporation":false,"usgs":true,"family":"Harlow","given":"George E.","suffix":"Jr.","email":"geharlow@usgs.gov","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":178558,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":18273,"text":"ofr94329 - 1994 - Hydrogeologic and water-quality data from wells near the Hueco Bolson Recharge Project area, El Paso, Texas, 1990 and 1991","interactions":[],"lastModifiedDate":"2019-12-08T13:58:17","indexId":"ofr94329","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-329","title":"Hydrogeologic and water-quality data from wells near the Hueco Bolson Recharge Project area, El Paso, Texas, 1990 and 1991","docAbstract":"Tertiary-treated wastewater currently (1991) is being injected into the Hueco bolson aquifer at a site in northeastern El Paso, Texas, to supplement the quantity of available freshwater. Hydrologic data were compiled and water-quality and bacterial data were collected from existing wells near the Hueco Bolson Recharge Project (HBRP) in August and September 1990 and 1991.
\nBorehole tracer tests indicated upward ground-water flow in nearly all tested intervals of several observation wells. The cumulative volume of injected water was less than the volume produced from wells adjacent to the HBRP area. Water levels in three production wells, located more than 1.5 miles from the injection wells, declined at rates comparable to those observed before injection operations. Water levels in wells located within 0.75 mile of the injection-well pipeline declined at a slower rate after HBRP injection operations had begun. Between 1985 and 1991, water levels in observation wells located within 700 feet of an injection well either did not appreciably decline, or declined at smaller rates than water levels in more distant production wells.
\nTrihalomethane compounds were detected in water from 8 of the 16 observation and production wells sampled in 1990 and in 10 of the 17 wells sampled in 1991. Concentrations of trihalomethane compounds in these samples ranged from 0.05 to 1.9 |lg/L (micrograms per liter) in 1990 and from 0.05 to 1.4 |ig/L in 1991. Concentrations of trihalomethane compounds in samples of injected water from two wells were 27.8 and 34.6 |J,g/L respectively, in 1991. Dibromomethane and dichloromethane were detected in water from injection wells and from observation wells within about 700 feet of the injection wells.
\nAerobic bacteria were determined to be the only bacteria type present in ground water except for samples from two wells, which also contained denitrifying bacteria. The populations of aerobic bacteria determined in ground water ranged from 80 to more than 160,000 most probable number of organisms per milliliter of sample.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94329","usgsCitation":"Brock, R.D., Buszka, P.M., and Godsy, E.M., 1994, Hydrogeologic and water-quality data from wells near the Hueco Bolson Recharge Project area, El Paso, Texas, 1990 and 1991: U.S. Geological Survey Open-File Report 94-329, v, 85 p., https://doi.org/10.3133/ofr94329.","productDescription":"v, 85 p.","numberOfPages":"90","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":151165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0329/report-thumb.jpg"},{"id":47626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0329/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"El Paso","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.64154052734374,\n 31.5668353078939\n ],\n [\n -106.15814208984374,\n 31.5668353078939\n ],\n [\n -106.15814208984374,\n 32.010404958190534\n ],\n [\n -106.64154052734374,\n 32.010404958190534\n ],\n [\n -106.64154052734374,\n 31.5668353078939\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628c2d","contributors":{"authors":[{"text":"Brock, Robert D.","contributorId":27875,"corporation":false,"usgs":true,"family":"Brock","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":178829,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buszka, Paul M. 0000-0001-8218-826X pmbuszka@usgs.gov","orcid":"https://orcid.org/0000-0001-8218-826X","contributorId":1786,"corporation":false,"usgs":true,"family":"Buszka","given":"Paul","email":"pmbuszka@usgs.gov","middleInitial":"M.","affiliations":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":178828,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godsy, Edward M.","contributorId":66278,"corporation":false,"usgs":true,"family":"Godsy","given":"Edward","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":178830,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":17763,"text":"ofr94308 - 1994 - Surface-water-quality assessment of the Yakima River basin in Washington: major-and minor-element data for sediment, water, and aquatic biota, 1987-91","interactions":[],"lastModifiedDate":"2017-02-07T09:54:13","indexId":"ofr94308","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-308","title":"Surface-water-quality assessment of the Yakima River basin in Washington: major-and minor-element data for sediment, water, and aquatic biota, 1987-91","docAbstract":"Major- and minor-element concentrations are presented for streambed and suspended sediment, filtered- and unfiltered-water, and aquatic-biota samples collected during 1987-91 from the Yakima River Basin in south-central Washington. The samples were collected as part of the U.S. Geological Survey's National Water-quality Assessment (NAWQA) program which is designed to provide results that are useful in understanding and managing the Nation's water resources. This report includes the sampling approach, field collection and processing techniques, and methods of chemical analysis, as well as a compilation of chemical data, statistical summaries, and quality- control data. These data may be used by scientists and resource managers to describe (1) spatial distribution of selected major and minor elements in sediment, water, and aquatic biota of the Yakima River Basin; (2) temporal variation for element concentrations in filtered water and in suspended sediment at selected sites; (3) suita- bility of surface water for preservation of aquatic life and protection of human health; and (4) major natural and anthropogenic sources of major and minor elements in the Yakima River Basin that affect observed water-quality conditions.
\nStreambed-sediment samples were collected once from 27 sites in the basin during 1987-91. Suspended-sediment and filtered-water samples were collected monthly and during hydrologic events (including snowmelt and winter rainstorms) at seven sites, and filtered-water samples were collected at least once at an additional 37 sites during synoptic samplings. Unfiltered-water samples were collected at seven sites on a quarterly basis during 1987 only. Samples of aquatic plants were collected once in 1989, and aquatic insects, fish, and clams were collected from 34 sites three times during 1989-90.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr94308","usgsCitation":"Fuhrer, G.J., Fluter, S.L., McKenzie, S.W., Rinella, J.F., Crawford, J.K., Cain, D.J., Hornberger, M.I., Bridges, J.L., and Skach, K.A., 1994, Surface-water-quality assessment of the Yakima River basin in Washington: major-and minor-element data for sediment, water, and aquatic biota, 1987-91: U.S. Geological Survey Open-File Report 94-308, vi, 222 p., https://doi.org/10.3133/ofr94308.","productDescription":"vi, 222 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1987-01-01","temporalEnd":"1991-12-31","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":46993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0308/report.pdf","text":"Report","size":"3.90 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":150597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0308/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Yakima River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.717529296875,\n 46.10561307998295\n ],\n [\n -121.717529296875,\n 47.42251265435723\n ],\n [\n -119.28955078124999,\n 47.42251265435723\n ],\n [\n -119.28955078124999,\n 46.10561307998295\n ],\n [\n -121.717529296875,\n 46.10561307998295\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a4d2","contributors":{"authors":[{"text":"Fuhrer, Gregory J. gjfuhrer@usgs.gov","contributorId":944,"corporation":false,"usgs":true,"family":"Fuhrer","given":"Gregory","email":"gjfuhrer@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":177724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fluter, Shelley L.","contributorId":36419,"corporation":false,"usgs":true,"family":"Fluter","given":"Shelley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":177727,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKenzie, Stuart W.","contributorId":27841,"corporation":false,"usgs":true,"family":"McKenzie","given":"Stuart","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":177730,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rinella, Joseph F. jrinella@usgs.gov","contributorId":1371,"corporation":false,"usgs":true,"family":"Rinella","given":"Joseph","email":"jrinella@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":177732,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Crawford, J. Kent","contributorId":54176,"corporation":false,"usgs":true,"family":"Crawford","given":"J.","email":"","middleInitial":"Kent","affiliations":[],"preferred":false,"id":177725,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cain, Daniel J. 0000-0002-3443-0493 djcain@usgs.gov","orcid":"https://orcid.org/0000-0002-3443-0493","contributorId":1784,"corporation":false,"usgs":true,"family":"Cain","given":"Daniel","email":"djcain@usgs.gov","middleInitial":"J.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":177731,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hornberger, Michelle I. 0000-0002-7787-3446 mhornber@usgs.gov","orcid":"https://orcid.org/0000-0002-7787-3446","contributorId":1037,"corporation":false,"usgs":true,"family":"Hornberger","given":"Michelle","email":"mhornber@usgs.gov","middleInitial":"I.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":177726,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Bridges, Jennifer L.","contributorId":42480,"corporation":false,"usgs":true,"family":"Bridges","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":177729,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Skach, Kenneth A. kaskach@usgs.gov","contributorId":1894,"corporation":false,"usgs":true,"family":"Skach","given":"Kenneth","email":"kaskach@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":177728,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":18932,"text":"ofr94450 - 1994 - Geochemical data of drill core samples of carbonatites and associated igneous rocks, Benton, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr94450","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-450","title":"Geochemical data of drill core samples of carbonatites and associated igneous rocks, Benton, Arkansas","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94450","usgsCitation":"Flohr, M.J., and Howard, J.M., 1994, Geochemical data of drill core samples of carbonatites and associated igneous rocks, Benton, Arkansas: U.S. Geological Survey Open-File Report 94-450, 21 leaves :map ;28 cm., https://doi.org/10.3133/ofr94450.","productDescription":"21 leaves :map ;28 cm.","costCenters":[],"links":[{"id":151719,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0450/report-thumb.jpg"},{"id":48331,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0450/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae467","contributors":{"authors":[{"text":"Flohr, Marta J.","contributorId":8127,"corporation":false,"usgs":true,"family":"Flohr","given":"Marta","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":180005,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howard, J. Michael","contributorId":74770,"corporation":false,"usgs":true,"family":"Howard","given":"J.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":180006,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18957,"text":"ofr94287 - 1994 - The 1992 Basin & Range Province GPS survey; 3, Data processing and results","interactions":[],"lastModifiedDate":"2012-02-02T00:07:26","indexId":"ofr94287","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-287","title":"The 1992 Basin & Range Province GPS survey; 3, Data processing and results","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94287","usgsCitation":"Foulger, G., 1994, The 1992 Basin & Range Province GPS survey; 3, Data processing and results: U.S. Geological Survey Open-File Report 94-287, ii, 39 p. :ill. ;28 cm., https://doi.org/10.3133/ofr94287.","productDescription":"ii, 39 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":150656,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0287/report-thumb.jpg"},{"id":48362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0287/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683613","contributors":{"authors":[{"text":"Foulger, G.R.","contributorId":14439,"corporation":false,"usgs":false,"family":"Foulger","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":180052,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}