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","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/wri924056","usgsCitation":"Lieblich, D., Haeni, F., and Lane, J., 1992, Integrated use of surface-geophysical methods to indicate subsurface fractures at Milford, New Hampshire: U.S. Geological Survey Water-Resources Investigations Report 92-4056, iv, 38 p. , https://doi.org/10.3133/wri924056.","productDescription":"iv, 38 p. ","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":123094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4056/report-thumb.jpg"},{"id":57171,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Hampshire","county":"Hillsborough County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-72.009,43.1875],[-71.9136,43.2069],[-71.8616,43.1234],[-71.8566,43.1152],[-71.8522,43.1157],[-71.6791,43.1497],[-71.6678,43.1525],[-71.6412,43.0538],[-71.6243,43.0556],[-71.5183,43.0684],[-71.5127,43.048],[-71.4901,43.0507],[-71.4857,43.0452],[-71.4851,43.0416],[-71.4738,43.0348],[-71.455,43.0438],[-71.4494,43.0197],[-71.4124,43.0134],[-71.3924,43.0084],[-71.375,42.9388],[-71.4513,42.9306],[-71.4513,42.9293],[-71.427,42.8247],[-71.3864,42.8228],[-71.3752,42.8124],[-71.3746,42.8115],[-71.3608,42.7987],[-71.3665,42.7914],[-71.364,42.7901],[-71.3627,42.7828],[-71.3577,42.7851],[-71.354,42.7828],[-71.3528,42.7801],[-71.354,42.7778],[-71.3503,42.7746],[-71.3515,42.7719],[-71.3085,42.7641],[-71.3022,42.7632],[-71.2629,42.7563],[-71.2469,42.7432],[-71.2524,42.7404],[-71.2561,42.7377],[-71.2599,42.7349],[-71.2674,42.7277],[-71.2743,42.7191],[-71.2824,42.71],[-71.2968,42.6978],[-71.3854,42.6988],[-71.6293,42.7042],[-71.8651,42.711],[-71.8994,42.7121],[-71.9287,42.713],[-71.9448,42.7885],[-71.9748,42.7888],[-71.9942,42.8833],[-72.0065,42.9437],[-72.0629,42.9444],[-72.059,43.0045],[-72.0585,43.0186],[-72.0433,43.0755],[-72.0427,43.0818],[-72.0439,43.0818],[-72.0343,43.1283],[-72.038,43.1287],[-72.0238,43.1601],[-72.0366,43.1824],[-72.009,43.1875]]]},\"properties\":{\"name\":\"Hillsborough\",\"state\":\"NH\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e4532","contributors":{"authors":[{"text":"Lieblich, D.A.","contributorId":73645,"corporation":false,"usgs":true,"family":"Lieblich","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":199673,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":199674,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lane, J.W. Jr.","contributorId":66723,"corporation":false,"usgs":true,"family":"Lane","given":"J.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":199672,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28093,"text":"wri914145 - 1992 - Time of travel and dispersion in a selected reach of Roberts Creek, Clayton County, Iowa","interactions":[],"lastModifiedDate":"2016-03-11T15:49:30","indexId":"wri914145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"91-4145","title":"Time of travel and dispersion in a selected reach of Roberts Creek, Clayton County, Iowa","docAbstract":"Time of travel and dispersion were determined in a 9.4-river-mile reach of Roberts Creek in northwestern Clayton County, Iowa, in the spring of 1990. Time of travel was determined so that a discrete parcel of water could be sampled through the study area during medium to low streamflow conditions. Dispersion characteristics were determined to identify solute-transport differences under two streamflow conditions.
\nTime of travel was determined by dye tracing, using rhodamine WT as the tracer. One dyeinjection site and three sampling sites were used to measure time of travel. Two dye-tracing tests were conducted at discharges having flow-duration values of 48 and 80 percent. The discharges at the time of the two dye-tracing tests approximated medium- and low-flow conditions. The average stream velocity in the study area was 0.23 foot per second during medium-flow conditions, March 20 to 22,1990, and 0.07 foot per second during low-flow conditions, April 30 to May 12, 1990. The injected dye dispersed in a plume that lasted about 18 hours during medium flow and about 64 hours during low flow at the downstream site.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri914145","collaboration":"Prepared in cooperation with the Iowa Department of Natural Resources, Geological Survey Bureau","usgsCitation":"Kolpin, D., and Kalkhoff, S., 1992, Time of travel and dispersion in a selected reach of Roberts Creek, Clayton County, Iowa: U.S. Geological Survey Water-Resources Investigations Report 91-4145, iv, 16 p.: ill.; 28 cm., https://doi.org/10.3133/wri914145.","productDescription":"iv, 16 p.: ill.; 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":159007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4145/report-thumb.jpg"},{"id":56912,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Iowa","county":"Clayton County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-91.604,43.0816],[-91.4892,43.0817],[-91.37,43.0807],[-91.2546,43.0802],[-91.1944,43.08],[-91.178,43.0798],[-91.1777,43.0732],[-91.1782,43.0655],[-91.1776,43.0584],[-91.1766,43.0506],[-91.1756,43.0415],[-91.1716,43.0291],[-91.1677,43.0192],[-91.1624,43.0071],[-91.1589,42.9989],[-91.1579,42.9966],[-91.1566,42.9934],[-91.1563,42.9894],[-91.1568,42.9839],[-91.1585,42.9784],[-91.1566,42.9747],[-91.1559,42.9739],[-91.152,42.9695],[-91.1506,42.9678],[-91.1464,42.9609],[-91.1455,42.9518],[-91.1457,42.9445],[-91.1454,42.9395],[-91.1453,42.9372],[-91.1438,42.9268],[-91.1445,42.9168],[-91.1444,42.9104],[-91.1411,42.905],[-91.1372,42.9007],[-91.1311,42.8965],[-91.1218,42.8927],[-91.1132,42.8885],[-91.1047,42.8824],[-91.0999,42.875],[-91.0995,42.874],[-91.0971,42.8678],[-91.0944,42.8596],[-91.0924,42.8542],[-91.0908,42.8498],[-91.089,42.8462],[-91.086,42.8443],[-91.0847,42.8437],[-91.0823,42.8424],[-91.0796,42.8398],[-91.0775,42.8373],[-91.0776,42.8339],[-91.0781,42.8294],[-91.078,42.8214],[-91.0776,42.8103],[-91.0763,42.8],[-91.0735,42.7913],[-91.0713,42.7826],[-91.0696,42.7771],[-91.0688,42.7736],[-91.0667,42.7698],[-91.0649,42.767],[-91.0629,42.7645],[-91.062,42.762],[-91.0621,42.7591],[-91.0634,42.7561],[-91.0639,42.7545],[-91.0638,42.754],[-91.0632,42.7523],[-91.0613,42.75],[-91.0587,42.7487],[-91.0582,42.7485],[-91.0563,42.7478],[-91.0549,42.746],[-91.0549,42.7446],[-91.0543,42.7428],[-91.0517,42.7397],[-91.0492,42.7383],[-91.0467,42.7379],[-91.0447,42.7376],[-91.0417,42.7375],[-91.0392,42.7375],[-91.0354,42.7371],[-91.0323,42.7358],[-91.0305,42.7341],[-91.03,42.7314],[-91.0301,42.7291],[-91.0283,42.7263],[-91.0264,42.7249],[-91.0259,42.7245],[-91.0226,42.7227],[-91.0182,42.7205],[-91.0075,42.7161],[-90.998,42.7121],[-90.9903,42.7074],[-90.9841,42.7036],[-90.98,42.6995],[-90.9734,42.6956],[-90.9677,42.6929],[-90.9601,42.6898],[-90.9542,42.6872],[-90.9482,42.6858],[-90.9413,42.685],[-90.9382,42.685],[-90.9332,42.6856],[-90.9276,42.6856],[-90.9226,42.6843],[-90.9169,42.6821],[-90.9108,42.68],[-90.9065,42.6785],[-90.8985,42.6761],[-90.896,42.6753],[-90.8962,42.6697],[-90.8978,42.6447],[-91.0181,42.6452],[-91.1334,42.6451],[-91.2519,42.6445],[-91.3691,42.6437],[-91.4876,42.6442],[-91.606,42.6437],[-91.6055,42.731],[-91.605,42.8169],[-91.6045,42.9056],[-91.6046,42.9915],[-91.604,43.0816]]]},\"properties\":{\"name\":\"Clayton\",\"state\":\"IA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b70f","contributors":{"authors":[{"text":"Kolpin, D.W.","contributorId":87565,"corporation":false,"usgs":true,"family":"Kolpin","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":199206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kalkhoff, S. J.","contributorId":28967,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"S. J.","affiliations":[],"preferred":false,"id":199205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28365,"text":"wri924012 - 1992 - Integrated use of surface-geophysical methods to indicate subsurface fractures at Tibbetts Road, Barrington, New Hampshire","interactions":[],"lastModifiedDate":"2019-10-15T07:35:37","indexId":"wri924012","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-4012","title":"Integrated use of surface-geophysical methods to indicate subsurface fractures at Tibbetts Road, Barrington, New Hampshire","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/wri924012","usgsCitation":"Lieblich, D., Haeni, F., and Cromwell, R., 1992, Integrated use of surface-geophysical methods to indicate subsurface fractures at Tibbetts Road, Barrington, New Hampshire: U.S. Geological Survey Water-Resources Investigations Report 92-4012, iv, 33 p. , https://doi.org/10.3133/wri924012.","productDescription":"iv, 33 p. 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A.","contributorId":10838,"corporation":false,"usgs":true,"family":"Sylvester","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285736,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18993,"text":"ofr92395 - 1992 - Preliminary results of coring surficial deposits in the Winchester 30 x 60 minute Quadrangle, West Virginia and Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr92395","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-395","title":"Preliminary results of coring surficial deposits in the Winchester 30 x 60 minute Quadrangle, West Virginia and Virginia","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr92395","usgsCitation":"Froelich, A., Hoffman, M., Taunton, S., and Phelan, D.J., 1992, Preliminary results of coring surficial deposits in the Winchester 30 x 60 minute Quadrangle, West Virginia and Virginia: U.S. Geological Survey Open-File Report 92-395, 46 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr92395.","productDescription":"46 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0395/report-thumb.jpg"},{"id":48404,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0395/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b30d","contributors":{"authors":[{"text":"Froelich, A.J.","contributorId":13593,"corporation":false,"usgs":true,"family":"Froelich","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":180108,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, M.F.","contributorId":20599,"corporation":false,"usgs":true,"family":"Hoffman","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":180110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taunton, S.S.","contributorId":22193,"corporation":false,"usgs":true,"family":"Taunton","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":180111,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Phelan, D. J.","contributorId":17635,"corporation":false,"usgs":true,"family":"Phelan","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":180109,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":64695,"text":"i1960 - 1992 - Pre-Tertiary bedrock geologic map of the Mariposa 1 degree by 2 degrees Quadrangle, Sierra Nevada, California; Nevada","interactions":[{"subject":{"id":12598,"text":"ofr87670 - 1988 - Pre-Tertiary bedrock geologic map of the Mariposa 1 degree x 2 degrees Quadrangle","indexId":"ofr87670","publicationYear":"1988","noYear":false,"title":"Pre-Tertiary bedrock geologic map of the Mariposa 1 degree x 2 degrees Quadrangle"},"predicate":"SUPERSEDED_BY","object":{"id":64695,"text":"i1960 - 1992 - Pre-Tertiary bedrock geologic map of the Mariposa 1 degree by 2 degrees Quadrangle, Sierra Nevada, California; Nevada","indexId":"i1960","publicationYear":"1992","noYear":false,"title":"Pre-Tertiary bedrock geologic map of the Mariposa 1 degree by 2 degrees Quadrangle, Sierra Nevada, California; Nevada"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:00","indexId":"i1960","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1960","subseriesTitle":"NONE","title":"Pre-Tertiary bedrock geologic map of the Mariposa 1 degree by 2 degrees Quadrangle, Sierra Nevada, California; Nevada","language":"ENGLISH","doi":"10.3133/i1960","usgsCitation":"Bateman, P.C., 1992, Pre-Tertiary bedrock geologic map of the Mariposa 1 degree by 2 degrees Quadrangle, Sierra Nevada, California; Nevada: U.S. Geological Survey IMAP 1960, 1 map :col. ;45 x 71 cm., on sheet 90 x 132 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1960.","productDescription":"1 map :col. ;45 x 71 cm., on sheet 90 x 132 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107218,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10040.htm","linkFileType":{"id":5,"text":"html"},"description":"10040"},{"id":187207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,37 ], [ -120,38 ], [ -118,38 ], [ -118,37 ], [ -120,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684388","contributors":{"authors":[{"text":"Bateman, P. 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Precipitation, temperature, Palmer Drought Severity Indices, and ground- and surface-water levels from water years 1988 and 1989 were compared to the historical record to evaluate severity, extent, and duration of the 1988 drought in Indiana.
\nThree types of drought-climatological, hydrologic, and agricultural--occurred in most of Indiana during water years 1988 and 1989. The drought began toward the end of calendar year 1987 as annual precipitation decreased to 4.6 inches below the long term mean. By the end of September 1988, statewide precipitation deficits had increased to almost 8 inches below normal. High temperatures during the summer months increased the stress on crops, livestock, and people. Northwest Indiana experienced the second warmest June-August on record. Palmer Drought Severity Indices indicated that a moderate-to-severe drought had occurred in Indiana during most of 1988.
\nGround-water levels were affected substantially in many areas of the State. Record low-water levels were observed at 12 of the 20 monitoring wells included in this report. A go-day ground-water emergency was declared in parts of northwestern Indiana. Streamflow throughout the State was affected to varying degrees by the drought. Annual mean discharge in some rivers was only slightly less than the mean annual discharge, while others flowed at less than half that value. The effects of low streamflows were felt by many as electric power plants reduced or ceased production and public-water utilities requested conservation measures by their customers. Major reservoirs in the State approached or reached record low levels, causing water supplies as well as recreational activities to be diminished.
\nMost major crops produced in Indiana were affected by the dry conditions. Average yields in 1988 ranged from 50 to 86 percent of 1987 yields.
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It is located off the Carolinas on the continental rise in approximately 1,200-5,500 m water depth and extends downslope for over 300 km (Popenoe, 1982). These maps show the bathymetry at the head of the Cape Fear Slide as interpreted from single-channel 3.5 kHz seismic-reflection profiles and mid-range Sea Marc I sidescan sonar imagery (Popenoe, 1985; Popenoe and others, 1991; Schmuck, 1991). The 3.5 kHz data consist of over 1000 km of profiles that were collected in 1988 for the University of North Carolina, Department of Geology. The UNC 3.5 kHz data were used as the main data set in interpreting the bathymetry. The sidescan sonar data were collected in 1980 by the U.S. Geological Survey in cooperation with the Lamont-Doherty Geological Observatory for the U.S. Bureau of Land Management Environmental Studies Program. 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