{"pageNumber":"1328","pageRowStart":"33175","pageSize":"25","recordCount":46734,"records":[{"id":70171330,"text":"70171330 - 1995 - Surface electromagnetic geophysical exploration of the ground-water resources of Isla de Mona, Puerto Rico, a caribbean carbonate island","interactions":[],"lastModifiedDate":"2016-05-26T16:21:44","indexId":"70171330","displayToPublicDate":"1995-07-12T14:30:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1184,"text":"Carbonates and Evaporites","active":true,"publicationSubtype":{"id":10}},"title":"Surface electromagnetic geophysical exploration of the ground-water resources of Isla de Mona, Puerto Rico, a caribbean carbonate island","docAbstract":"<p class=\"Para\">Two electromagnetic surface geophysical techniques were used to explore the ground-water resources of Isla de Mona, Puerto Rico&mdash;a 55-square-kilometer island located between Puerto Rico and Hispa&ntilde;iola, Isla de Mona is a tectonically uplifted carbonate plateau of Neogene age that has an average elevation of about 50 meters above mean sea level. This plateau is bounded by vertical cliffs except on the southwest where there is a narrow, 3-square-kilometer coastal plain. The coastal plain is composed of Quaternary carbonate deposits, and has a maximum elevation of less than 10 meters above mean sea level. No large-scale surface-water features are found on the plateau or on the coastal plain. To better understand the aquifer characteristics of the island, terrain conductivity and transient electromagnetic data were collected on the coastal plain and on the plateau. Computer programs were used to analyze quantitatively the electromagnetic data. Geoelectric models were produced to approximate the depth below land surface of the saline-freshwater interface underlying both the coastal plain and the plateau. Because the geophysical methods could not discern the water-table, it was assumed that it was near sea level. The thickness of the freshwater lens was estimated by subtracting the elevation of the land surface above mean sea level from the depth to the saline-freshwater interface as determined from the geophysical data. Results from the geophysical methods and water-level observations indicate that a freshwater lens with a maximum thickness of about 10 meters exists under the coastal plain. This lens thins towards the ocean, and it also thins away from the ocean toward the plateau. The model produced from the transient electromagnetic data indicates that the freshwater lens under the plateau has a maximum thickness of about 14 meters, which is a much thinner lens than previously estimated. A freshwater lens thickness of 14 meters is similar to direct measurements by divers in Cueva de Agua at Punta los Ingleses (located on the southeast coast), and observations by divers of freshwater seeps into the ocean at depths of 8 to 10 meters along the north coast cliffs after a major rainstorm.</p>\n<p class=\"Para\">Ground-water flow in the coastal plain appears to be radial from the center of the freshwater mound. At the intersection between the coastal plain and the plateau, the flow is parallel to the coastline. The direction of flow on the rest of the plateau could not be determined accurately with the available data.</p>","publisher":"Springer Netherlands","doi":"10.1007/BF03175403","issn":"1878-5212","usgsCitation":"Martinez, M., Troester, J.W., and Richards, R.T., 1995, Surface electromagnetic geophysical exploration of the ground-water resources of Isla de Mona, Puerto Rico, a caribbean carbonate island: Carbonates and Evaporites, v. 10, no. 2, p. 184-192, https://doi.org/10.1007/BF03175403.","productDescription":"9 p.","startPage":"184","endPage":"192","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"links":[{"id":321785,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationDate":"1995-09-01","publicationStatus":"PW","scienceBaseUri":"57481e3be4b07e28b664dc08","contributors":{"authors":[{"text":"Martinez, M.I.","contributorId":12895,"corporation":false,"usgs":true,"family":"Martinez","given":"M.I.","email":"","affiliations":[],"preferred":false,"id":630597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Troester, Joseph W.","contributorId":46544,"corporation":false,"usgs":true,"family":"Troester","given":"Joseph","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":630598,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richards, Ronald T.","contributorId":23592,"corporation":false,"usgs":true,"family":"Richards","given":"Ronald","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":630599,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70226727,"text":"70226727 - 1995 - Surface seismic and electrical methods to detect fluids related to faulting","interactions":[],"lastModifiedDate":"2021-12-07T17:37:46.507905","indexId":"70226727","displayToPublicDate":"1995-07-10T11:33:54","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Surface seismic and electrical methods to detect fluids related to faulting","docAbstract":"<p><span>In the absence of drilling, surface-based geophysical methods are necessary to observe fault zones and fault zone physical properties at seismogenic depths. These in situ physical properties can then be used to infer the presence and distribution of fluids along faults, although such observations are by nature indirect and become less exact with greater depth. Multiple observations of a range of such geophysical properties as compressional and shear seismic velocity (</span><i>V<sub>p</sub></i><span>&nbsp;and&nbsp;</span><i>V<sub>s</sub></i><span>),&nbsp;</span><i>V<sub>p</sub></i><span>/V5 ratio (related to Poisson's ratio), resistivity and attenuation in and adjacent to fault zones offer the greatest hope of making inferences of the fault zone geometry, fluids in the fault zone, and fluid reservoirs in the surrounding crust. For simple geometries, fault zone guided waves can provide information on fault zone width and velocities for faults of the order of 200 m wide. To address the question of whether a narrow fault zone can be imaged well enough at depths of seismic rupture to infer the presence of anomalously high fluid/rock ratios, we present synthetic seismic tomography and magnetotelluric examples for an ideal case of a narrow fault zone with a simple geometry, large changes in material properties, and numerous earthquakes within the fault zone. A synthetic 0.5-km wide fault zone with 20% velocity reduction is well imaged using local earthquake tomography. When sequential velocity inversions are done, the true fault width is found, even to 9 km depth, although the calculated amplitude of the velocity reduction is lower than the actual amplitude.&nbsp;</span><i>V<sub>p</sub></i><span>/</span><i>V<sub>s</sub></i><span>&nbsp;is as well determined as&nbsp;</span><i>V<sub>p</sub></i><span>. Magnetotelluric imaging of a synthetic fault zone shows that a conductive fault zone can be well imaged within the upper 10 km. Further, a narrow (1 km) very low resistivity (3 ohm m) fault core can be imaged within a broad (5 km) low resistivity (10 ohm m) fault zone, illustrating that regions of a fault containing large quantities of interconnected fluids within a broader, conductive fault zone should be detectable. Thus variations in fluid content and fluid pressure can be inferred from electrical and seismic methods but there will always be uncertainty in these inferences due to the trade-off with other factors, such as intrinsic variations in porosity, mineralogy, and pore geometry. The best approach is combined modeling of varied seismic and electrical data.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/94JB03256","usgsCitation":"Eberhart-Phillips, D., Stanley, W., Rodriguez, B.D., and Lutter, W.J., 1995, Surface seismic and electrical methods to detect fluids related to faulting: Journal of Geophysical Research Solid Earth, v. 100, no. B7, p. 12919-12936, https://doi.org/10.1029/94JB03256.","productDescription":"18 p.","startPage":"12919","endPage":"12936","costCenters":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":392579,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"100","issue":"B7","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Eberhart-Phillips, Donna","contributorId":192926,"corporation":false,"usgs":false,"family":"Eberhart-Phillips","given":"Donna","affiliations":[],"preferred":false,"id":827998,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanley, William D.","contributorId":23274,"corporation":false,"usgs":true,"family":"Stanley","given":"William D.","affiliations":[],"preferred":false,"id":827999,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rodriguez, Brian D. 0000-0002-2263-611X brod@usgs.gov","orcid":"https://orcid.org/0000-0002-2263-611X","contributorId":836,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Brian","email":"brod@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":828000,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lutter, William J.","contributorId":74366,"corporation":false,"usgs":true,"family":"Lutter","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":828001,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5222735,"text":"5222735 - 1995 - Banding reference areas and survival rates of green-winged teal, 1950-1989","interactions":[],"lastModifiedDate":"2024-12-09T17:07:00.058522","indexId":"5222735","displayToPublicDate":"1995-07-03T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Banding reference areas and survival rates of green-winged teal, 1950-1989","docAbstract":"<p>The green-winged teal (<i>Anas crecca carolinensis</i>) is an important harvest species, yet we know relatively little about its population ecology. We investigated aspects of green-winged teal population ecology of potential importance to waterfowl managers. We used recoveries of green-winged teal banded during winter (1950-89) to establish banding reference areas and estimate survival and band recovery rates. We used cluster analysis based on similarities in recovery patterns to group banding degree blocks into 8 minor and 5 major reference areas describing the principal wintering range of green-winged teal in North America. We then estimated survival and recovery rates of green-winged teal banded in these areas. Mean annual survival rate estimates across years and reference areas were similar (P &gt; 0.05) for males (0.55, SE = 0.022) and females (0.51, SE = 0.057). Mean annual recovery rate estimates were larger for males (0.033, SE = 0.0017) than for females (0.024, SE = 0.0024) (<i>P</i> &lt; 0.01). There was little evidence of temporal variation in survival or recovery rates for most datasets. There was evidence of geographic variation in survival rates among major reference areas for males (<i>P</i> = 0.04) but not for females (<i>P</i> = 0.30). We recommend that analyses be conducted on greenwinged teal banded during preseason to further investigate possible sex specificity of survival rates and to address questions about the relationship between harvest rates and survival.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3802455","usgsCitation":"Chu, D.S., Nichols, J.D., Hestbeck, J.B., and Hines, J.E., 1995, Banding reference areas and survival rates of green-winged teal, 1950-1989: Journal of Wildlife Management, v. 59, no. 3, p. 487-498, https://doi.org/10.2307/3802455.","productDescription":"12 p.","startPage":"487","endPage":"498","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194048,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Georgia, Kansas, Nevada, Ohio, Virginia, Washington","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-119.789798,34.05726],[-119.5667,34.053452],[-119.795938,33.962929],[-119.916216,34.058351],[-119.789798,34.05726]]],[[[-118.524531,32.895488],[-118.573522,32.969183],[-118.369984,32.839273],[-118.524531,32.895488]]],[[[-118.500212,33.449592],[-118.32446,33.348782],[-118.593969,33.467198],[-118.500212,33.449592]]],[[[-122.289533,42.007764],[-114.107428,41.993965],[-114.046838,36.194069],[-114.21369,36.015613],[-114.545789,36.152248],[-114.730435,36.031317],[-114.569238,35.18348],[-114.635176,34.875003],[-114.136671,34.274377],[-114.420499,34.103466],[-114.535965,33.569154],[-114.701732,33.408388],[-114.707896,33.097432],[-114.502871,33.011153],[-114.468971,32.845155],[-114.612697,32.734516],[-117.118868,32.534706],[-117.50565,33.334063],[-118.088896,33.729817],[-118.428407,33.774715],[-118.519514,34.027509],[-119.159554,34.119653],[-119.616862,34.420995],[-120.441975,34.451512],[-120.608355,34.556656],[-120.644311,35.139616],[-120.873046,35.225688],[-120.884757,35.430196],[-121.851967,36.277831],[-121.932508,36.559935],[-121.788278,36.803994],[-121.880167,36.950151],[-122.140578,36.97495],[-122.419113,37.24147],[-122.511983,37.77113],[-122.425942,37.810979],[-122.168449,37.504143],[-122.144396,37.581866],[-122.385908,37.908136],[-122.301804,38.105142],[-122.484411,38.11496],[-122.492474,37.82484],[-122.972378,38.020247],[-123.103706,38.415541],[-123.725367,38.917438],[-123.851714,39.832041],[-124.373599,40.392923],[-124.063076,41.439579],[-124.23972,41.7708],[-124.203402,41.940964],[-122.289533,42.007764]]],[[[-84.810477,34.987607],[-83.108714,35.000768],[-83.339029,34.683807],[-82.908365,34.485402],[-82.589245,34.000118],[-81.50203,33.015113],[-81.120034,32.153303],[-80.84313,32.024226],[-81.254218,31.55594],[-81.17831,31.52241],[-81.276862,31.254734],[-81.490586,30.984952],[-81.408484,30.977718],[-81.461065,30.753684],[-82.004973,30.791744],[-82.116385,30.367335],[-82.227254,30.561041],[-84.903122,30.751791],[-85.102052,31.184734],[-85.141831,31.839261],[-84.925427,32.221551],[-85.188741,32.889727],[-85.598781,34.944915],[-84.810477,34.987607]]],[[[-99.541116,36.999573],[-102.000447,36.993249],[-102.051744,40.003078],[-95.375257,40],[-94.869644,39.772894],[-95.113077,39.559133],[-94.615834,39.160003],[-94.617982,37.075077],[-94.699735,36.998805],[-99.541116,36.999573]]],[[[-81.725583,39.215835],[-81.756975,38.937152],[-81.889233,38.874279],[-82.068864,38.984878],[-82.318111,38.457876],[-82.569368,38.406258],[-82.923694,38.750076],[-83.301951,38.598178],[-83.512571,38.701716],[-83.679484,38.630036],[-84.212904,38.805707],[-84.445242,39.114461],[-84.812241,39.107102],[-84.806082,41.696089],[-83.504334,41.731547],[-82.513827,41.384257],[-81.69325,41.514161],[-80.533774,41.973475],[-80.518991,40.638801],[-80.667957,40.582496],[-80.619297,40.26517],[-80.88036,39.620706],[-81.725583,39.215835]]],[[[-75.242266,38.027209],[-75.962596,37.117535],[-75.981624,37.434116],[-75.712065,37.936082],[-75.242266,38.027209]]],[[[-77.041898,38.741514],[-77.240604,38.638917],[-77.317288,38.383576],[-77.08481,38.368297],[-76.251358,37.833072],[-76.443254,37.652347],[-76.722156,37.83668],[-76.252415,37.447274],[-76.475927,37.250543],[-76.300352,37.00885],[-76.780532,37.209336],[-76.482407,36.917364],[-76.058154,36.916947],[-75.867044,36.550754],[-83.645586,36.600002],[-82.895445,36.882145],[-82.722097,37.120168],[-81.968297,37.537798],[-81.896001,37.331967],[-81.560625,37.206663],[-81.367052,37.334504],[-81.225104,37.234874],[-80.332038,37.493744],[-79.649075,38.591515],[-79.291813,38.419627],[-79.023053,38.798613],[-78.869276,38.762991],[-78.439429,39.132146],[-78.346718,39.427618],[-77.828157,39.132329],[-77.687124,39.319914],[-77.46021,39.228359],[-77.47701,39.100331],[-77.1199,38.934311],[-77.041898,38.741514]]],[[[-122.519535,48.288314],[-122.66921,48.240614],[-122.400628,48.036563],[-122.419274,47.912125],[-122.744612,48.20965],[-122.664928,48.374823],[-122.519535,48.288314]]],[[[-122.800217,48.60169],[-122.883759,48.418793],[-123.173061,48.579086],[-122.949116,48.693398],[-122.743049,48.661991],[-122.800217,48.60169]]],[[[-122.418268,47.320614],[-122.336934,47.341421],[-122.407841,47.680119],[-122.230046,47.970917],[-122.425572,48.232887],[-122.358375,48.056133],[-122.512031,48.133931],[-122.424102,48.334346],[-122.689121,48.476849],[-122.425271,48.599522],[-122.796887,48.975026],[-117.032351,48.999188],[-117.046915,46.379577],[-116.923005,46.018293],[-118.941242,46.000574],[-121.120064,45.623134],[-121.631167,45.704657],[-122.262625,45.544321],[-122.691008,45.624739],[-122.904119,46.083734],[-124.029924,46.308312],[-124.06842,46.601397],[-123.97083,46.47537],[-123.84621,46.716795],[-124.022413,46.708973],[-124.108078,46.836388],[-123.86018,46.948556],[-124.138035,46.970959],[-124.425195,47.738434],[-124.672427,47.964414],[-124.727022,48.371101],[-123.981032,48.16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 \"}}]}","volume":"59","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db545d4d","contributors":{"authors":[{"text":"Chu, Diane S.","contributorId":7378,"corporation":false,"usgs":true,"family":"Chu","given":"Diane","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":337002,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nichols, James D. 0000-0002-7631-2890 jnichols@usgs.gov","orcid":"https://orcid.org/0000-0002-7631-2890","contributorId":200533,"corporation":false,"usgs":true,"family":"Nichols","given":"James","email":"jnichols@usgs.gov","middleInitial":"D.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":337003,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hestbeck, Jay B. jay_hestbeck@usgs.gov","contributorId":4247,"corporation":false,"usgs":true,"family":"Hestbeck","given":"Jay","email":"jay_hestbeck@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":337005,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hines, James E. 0000-0001-5478-7230 jhines@usgs.gov","orcid":"https://orcid.org/0000-0001-5478-7230","contributorId":146530,"corporation":false,"usgs":true,"family":"Hines","given":"James","email":"jhines@usgs.gov","middleInitial":"E.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":337004,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5222711,"text":"5222711 - 1995 - Use of solicited bands and separation of hunting and natural mortality: a comment","interactions":[],"lastModifiedDate":"2024-12-09T17:30:40.250164","indexId":"5222711","displayToPublicDate":"1995-07-03T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Use of solicited bands and separation of hunting and natural mortality: a comment","docAbstract":"We previously presented (Conroy 1985, Conroy et al. 1989) models for analysis of band recovery data stratified into those voluntarily reported and those obtained by solicitation, similar to models described by Pollock et al. (1994).  We discuss differences between the 2 modeling approaches and suggest designs and analyses involving overlapping samples of standard and reward bands to enable adjustment for temporal and geographic variation in reporting and solicitation rates,","language":"English","publisher":"Wiley","doi":"10.2307/3802471","usgsCitation":"Conroy, M.J., Hines, J., and Williams, B.K., 1995, Use of solicited bands and separation of hunting and natural mortality: a comment: Journal of Wildlife Management, v. 59, no. 3, p. 619-621, https://doi.org/10.2307/3802471.","productDescription":"3 p.","startPage":"619","endPage":"621","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197709,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604331","contributors":{"authors":[{"text":"Conroy, Michael J.","contributorId":20871,"corporation":false,"usgs":false,"family":"Conroy","given":"Michael","email":"","middleInitial":"J.","affiliations":[{"id":13266,"text":"Warnell School of Forestry and Natural Resources, The University of Georgia","active":true,"usgs":false}],"preferred":false,"id":336922,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hines, James E. jhines@usgs.gov","contributorId":3506,"corporation":false,"usgs":true,"family":"Hines","given":"James E.","email":"jhines@usgs.gov","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":336921,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williams, B. Kenneth","contributorId":107798,"corporation":false,"usgs":true,"family":"Williams","given":"B.","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":336923,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70246578,"text":"70246578 - 1995 - The relationship of habitat characteristics to the distribution of chironomidae (Diptera) as measured by pupal exuviae collections in a large river system","interactions":[],"lastModifiedDate":"2023-07-10T18:06:39.464942","indexId":"70246578","displayToPublicDate":"1995-07-01T12:57:56","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2299,"text":"Journal of Freshwater Ecology","active":true,"publicationSubtype":{"id":10}},"title":"The relationship of habitat characteristics to the distribution of chironomidae (Diptera) as measured by pupal exuviae collections in a large river system","docAbstract":"<p><span>Floating chironomid pupal exuviae were collected throughout the Yakima River (Washington, USA) and tributaries in 1989 and 1990. All samples were taken during the October-November low-flow season and most sites were visited once with a sampling effort of approximately 10 minutes. Sampled stream segments ranged from 3rd to 7th order and elevation ranged from 140–1200 m. The total number of taxa distinguished in 77 samples was 150 with a mean of 24 per site. Species richness was not highly correlated with stream order or elevation. An ecological gradient defined by ordinating the taxa by site data was highly correlated with site elevation (r=.93). Comparison with published attributes of chironomid genera suggested that temperature regime was a dominant environmental variable controlling chironomid distribution in this basin. However, since most measured habitat variables were associated with altitude, their effects could not be separated. Cluster analysis of taxa by site data resulted in groupings that distinguished montane from valley sites and agricultural drains from other valley sites. Differences in species composition between moderately enriched agricultural drains and less-impacted sites were minor compared with the underlying elevation gradient.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02705060.1995.9663457","usgsCitation":"Fend, S.V., and Carter, J.L., 1995, The relationship of habitat characteristics to the distribution of chironomidae (Diptera) as measured by pupal exuviae collections in a large river system: Journal of Freshwater Ecology, v. 10, no. 4, p. 343-359, https://doi.org/10.1080/02705060.1995.9663457.","productDescription":"17 p.","startPage":"343","endPage":"359","costCenters":[],"links":[{"id":418832,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Yakima River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.77239215353185,\n              46.7497418070713\n            ],\n            [\n              -120.897818239824,\n              46.68668212264748\n            ],\n            [\n              -120.91663215276789,\n              46.54309054910462\n            ],\n            [\n              -121.00024853298291,\n              46.457092841556204\n            ],\n            [\n              -120.91245027257827,\n              46.26377807784297\n            ],\n            [\n              -120.76829114616146,\n              46.04227268731577\n            ],\n            [\n              -120.53207201697792,\n              45.98855855863255\n            ],\n            [\n              -120.23523027941988,\n              46.03791943132424\n            ],\n            [\n              -119.71889289085051,\n              46.17415846720985\n            ],\n            [\n              -119.52866332664071,\n              46.234922402859326\n            ],\n            [\n              -119.38233289263326,\n              46.182843144398646\n            ],\n            [\n              -119.34052419720238,\n              46.15678499772375\n            ],\n            [\n              -119.20882680659568,\n              46.284063030963125\n            ],\n            [\n              -119.42414158806389,\n              46.321611442952445\n            ],\n            [\n              -119.6561798477043,\n              46.46002866647308\n            ],\n            [\n              -119.86731375962941,\n              46.48306407710115\n            ],\n            [\n              -119.90494158551718,\n              46.55786183190668\n            ],\n            [\n              -119.8505902814572,\n              46.619636045820414\n            ],\n            [\n              -120.17460767104537,\n              46.68420809304271\n            ],\n            [\n              -120.4902633215473,\n              46.7601607513713\n            ],\n            [\n              -120.61150853829633,\n              46.81025954953077\n            ],\n            [\n              -120.77239215353185,\n              46.7497418070713\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fend, Steven V. 0000-0002-4638-6602 svfend@usgs.gov","orcid":"https://orcid.org/0000-0002-4638-6602","contributorId":3591,"corporation":false,"usgs":true,"family":"Fend","given":"Steven","email":"svfend@usgs.gov","middleInitial":"V.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":877271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, James L. 0000-0002-0104-9776 jlcarter@usgs.gov","orcid":"https://orcid.org/0000-0002-0104-9776","contributorId":3278,"corporation":false,"usgs":true,"family":"Carter","given":"James","email":"jlcarter@usgs.gov","middleInitial":"L.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":877272,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59940,"text":"mf2280 - 1995 - Maps and diagrams showing acoustic and textural characteristics and distribution of bottom sedimentary environments, Boston Harbor and Massachusetts Bay","interactions":[],"lastModifiedDate":"2025-06-10T20:45:17.76841","indexId":"mf2280","displayToPublicDate":"1995-07-01T07:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2280","title":"Maps and diagrams showing acoustic and textural characteristics and distribution of bottom sedimentary environments, Boston Harbor and Massachusetts Bay","docAbstract":"This report illustrates, describes, and briefly discusses the acoustic and textural characteristics and the distribution of bottom sedimentary environments in Boston Harbor and Massachusetts Bay. The study is an outgrowth of a larger research program designed to understand the regional processes that distribute sediments and related contaminants in the area. The report highlights the major findings presented in recent papers by Knebel and others (1991), Knebel, (1993), and Knebel and Circe (1995). The reader is urged to consult the full text of these earlier papers for a more definitive treatment of the data and for appropriate supporting references.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf2280","usgsCitation":"Knebel, H.J., and Circe, R.C., 1995, Maps and diagrams showing acoustic and textural characteristics and distribution of bottom sedimentary environments, Boston Harbor and Massachusetts Bay: U.S. Geological Survey Miscellaneous Field Studies Map 2280, 2 Plates: 53.54 x 39.70 inches and 35.39 x 41.42 inches, https://doi.org/10.3133/mf2280.","productDescription":"2 Plates: 53.54 x 39.70 inches and 35.39 x 41.42 inches","costCenters":[],"links":[{"id":490339,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5900.htm","linkFileType":{"id":5,"text":"html"}},{"id":284470,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2280/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":284471,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2280/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180111,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"150000","projection":"Transverse Mercator","country":"United States","otherGeospatial":"Boston Harbor, Massachusetts Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.0,42.1 ], [ -71.0,42.4 ], [ -70.3,42.4 ], [ -70.3,42.1 ], [ -71.0,42.1 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6617e4b0b29085100836","contributors":{"authors":[{"text":"Knebel, Harley J.","contributorId":25930,"corporation":false,"usgs":true,"family":"Knebel","given":"Harley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":262867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Circe, Ronald C.","contributorId":41592,"corporation":false,"usgs":true,"family":"Circe","given":"Ronald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":262868,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61350,"text":"mf2296 - 1995 - Detailed lithologic log of the Dow Chemical #1 B.L. Garrigan Drill Hole, Mississippi County, Arkansas","interactions":[],"lastModifiedDate":"2025-06-10T20:58:58.611046","indexId":"mf2296","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2296","title":"Detailed lithologic log of the Dow Chemical #1 B.L. Garrigan Drill Hole, Mississippi County, Arkansas","docAbstract":"The geology and tectonic setting of the New Madrid region in southeastern Missouri has received considerable attention because of the area's high seismic activity. The largest recorded earthquakes in this area occurred in the winter of 1811-1812. These earthquakes has estimated magnitudes as large as 8.0 on the Richter scale (Johnsonton and Kanter, 1990) and affected an area of about 1 million square miles (Fuller, 1912). Today, an area of continuously high seismic activity defines the New Madrid seismic zone, which extends from northeastern Arkansas into southeastern Missouri and northwestern Tennessee. Seismicity is locally concentrated along two subsurface archers--the Blytheville and Pascola (Hildenbrand and others, 1977; Crone and others, 1985; Hildenbrand, 1985; McKeown, 1988). The Padcola arch is not pertinent to this study and, therefore will not be discusses further. The Blytheville arch is located in and is subparallel to the axis of the northeast-southwest-trending Reelfoot structural basin, which formed during early Paleozoic rifting (Ervin and McGinnis, 1975; fig. 1). The Reelfoot basin is filled with Cambrian and Ordovician sedimentary rocks (Grohskopf, 1955; Howe, 1984; Houseknevht, 1989; Collins and others, 1992) that are uncomfortably overlain by Cretacaous and Tertiary sedimentary rocks and underlain by crystalline rocks of the eastern granite-rhyolite province (see Bickford and others, 1986). The presence of some Late Proterozoic sedimentary rocks in the Reelfoot basin currently cannot be ruled out. The Dow Chemical #1 B.L. Garrigan drill hole (hereafter, Garrigan) penetrated Paleozoic rocks on the Blytheville arch. The Garrigan is locted in the Reelfoot basin in the NW1/4, NW1/4 sec. 28, T. 15 N., R. 10 E., Mississippi County, Arkansas (fig. 1) and was completed to a total depth of 12,038 ft from a ground elevation of 239 ft on April 11, 1982 (Swolfs, 1991). The Garrigan is the only reported drill hole that penetrates the subsurface Blytheville arch and is an important source of core from the Reelfoot basin (Collins and others, 1992). Therefore, this drill hole is important for understanding structure and Paleozoic stratigraphy in a basin where stratigraphic and structural data are sparse. Rocks in the Garrigan were originally logged and described by J.R. Howe (personal communication to D.S. Collins, 1990) and published as a composite stratigraphic section along with the rock description for the Dow Chemical #1 Wilson drill hole (Howe, 1984). F.A. McKeown later relogged the rocks in the Garrigan and presented a generalized log in McKeown and others (1990). Swolfs (1991) presented another version of the Garrigan drill-hole geologic section (fig. 2). Aided by new biostratigraphic information, Taylor and others (1991) corrected major errors in the characterization and correlation of rocks in the Garrigan (fig. 2). Collins (1991) described the insoluble residues from the cuttings of the Garrigan, but could not correlate them with the insoluble resides from rocks of the carbonate platform west of the basin. However Taylor and others (1991), Collins and others (1992), and Collins and Bohm (1993) did correlate fossils from the Garrigan to other drill holes in the Reelfoot basin and adjacent areas. Using these correlated data, Collins and Bohm (1993) provided information on the structural relief across a part of the Reelfoot basin. Collins and others (1992) also interpreted the depositional setting for the Paleozoic rocks of the Garrigan. This report presents a detailed lithologic log of the Paleozoic rocks penetrated by the Garrigan that differs from the lithologic logs of previous workers (Howe, 1984; McKeown and others, 1990; see also Dart, 1992, p. 18-19). The lithologic descriptions of the Garrigan are derived from observations of well cuttings and core. Cored intervals used were 11,426-11,402 ft, 10,229-10,200 ft, and 8,002-7,979 ft. These intervals were the only intervals cored during the Garrigan drill project. Detailed analyses of the core will be described in a subsequent report.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf2296","usgsCitation":"Collins, D.S., and Skipp, G.L., 1995, Detailed lithologic log of the Dow Chemical #1 B.L. Garrigan Drill Hole, Mississippi County, Arkansas: U.S. Geological Survey Miscellaneous Field Studies Map 2296, 2 Plates: 40.99 x 60.03 inches and 40.84 x 58.40 inches, https://doi.org/10.3133/mf2296.","productDescription":"2 Plates: 40.99 x 60.03 inches and 40.84 x 58.40 inches","costCenters":[],"links":[{"id":490340,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5916.htm","linkFileType":{"id":5,"text":"html"}},{"id":282183,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2296/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":282184,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2296/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180126,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2296.jpg"}],"country":"United States","state":"Arkansas","county":"Mississippi County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.1,35.876944 ], [ -90.1,35.926111 ], [ -90.016667,35.926111 ], [ -90.016667,35.876944 ], [ -90.1,35.876944 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667cfa","contributors":{"authors":[{"text":"Collins, Donley S.","contributorId":93906,"corporation":false,"usgs":true,"family":"Collins","given":"Donley","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":265487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skipp, Gary L. 0000-0002-9404-0980 gskipp@usgs.gov","orcid":"https://orcid.org/0000-0002-9404-0980","contributorId":2102,"corporation":false,"usgs":true,"family":"Skipp","given":"Gary","email":"gskipp@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":265486,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21504,"text":"ofr9588 - 1995 - Preliminary Geologic Map of the Thousand Oaks 7.5' Quadrangle, Southern California: A Digital Database","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr9588","displayToPublicDate":"1995-07-01T00:00:00","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":"95-88","title":"Preliminary Geologic Map of the Thousand Oaks 7.5' Quadrangle, Southern California: A Digital Database","docAbstract":"Thousand Oaks is located in Arroyo Conejo, a region spanning both southeastern Ventura County and extreme northwest Los Angeles County in southern California. It was discovered in 1542 by Spanish explorer Juan Rodriquez Cabrillo and eventually became part of the Spanish Rancho El Conejo land grant (conejo means 'rabbit' in Spanish, of which there are many in the area). It is located in the Santa Monica Mountains in the northwestern part of the greater Los Angeles area. The area is bordered by the San Fernando Valley and the city of Los Angeles to the east, Simi Hills to the north, Las Posas Hills and the Santa Rosa Valley to the northwest, Conejo Mountain (also known as Conejo Hills) and Oxnard Plain to the west, and the Santa Monica Mountains and Malibu to the southwest. \r\n\r\nThe geology of the surrounding Santa Monica Mountains is dominated by a sequence of Tertiary sedimentary and volcanic rocks. These include the Tertiary Modelo Formation and the upper part of the Topanga Formation, other minor Tertiary rocks, and Miocene volcanic and intrusive rocks of the Conejo Formation. The basement units within the Santa Monica Mountains are a series of Jurassic and Cretaceous sedimentary rocks. \r\n\r\nThe volcanic rocks of the Conejo Formation underlies much of the surrounding watersheds. The younger Tertiary sedimentary Modelo and Upper Topanga Formations flank the Conejo to the north and south. On the north slope of the Santa Monica Mountains where the Arroyo Conejo and Thousand Oaks are located, the Tertiary formations are gently folded. The south flank of the Santa Monica Mountains is structurally dominated by the Malibu Coast Fault that runs along the foot of the mountains. This fault, and associated structures, creates a complex geologic setting on the south flank of the Santa Monica Mountains. The active nature of the Malibu Coast fault and associated structures accounts for the steep and rugged coastal topography. \r\n\r\nThe most widely exposed rock units in the area are the Plio-Pleistocene marine and nonmarine Pico and Saugus formations, which crop out on the southern flank of South Mountain-Oak Ridge and on the Las Posas uplands and Las Posas Hills. Locally, the Pico Formation consists of marine siltstone and silty shale with minor sandstone and pebbly sandstone. The Saugus Formation overlies and interfingers with the Pico Formation and is composed of interbedded shallow-marine to brackish water sandstone, siltstone, pebble-cobble conglomerate, and coquina beds that grade laterally and vertically into non-marine sandstone, siltstone, and conglomerate. A local member of the Saugus Formation is exposed in the southeast corner of the map area. It is predominantly a volcanic breccia conglomerate that resembles the Conejo Volcanics breccia, but is believed to represent remnants of landslide debris shed from the Conejo Formation into a local trough during Saugus time. \r\n\r\nEroded from, and overlying, these bedrock formations are a series of recent alluvial units. These alluvial units include Quaternary alluvium comprised of alluvium, stream deposits, alluvial fan and floodplain deposits, beach deposits, dissected older alluvial deposits. Also present are Quaternary landslides and colluvium composed of landslide deposits and colluvium deposits. The colluvium represents relatively thick continuous deposits of soil and rock fragments that are common on the steep slopes of the coastal canyons, and generally feed the many landslides, soil slips, and debris flows.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr9588","usgsCitation":"Yerkes, R., and Campbell, R., 1995, Preliminary Geologic Map of the Thousand Oaks 7.5' Quadrangle, Southern California: A Digital Database: U.S. Geological Survey Open-File Report 95-88, Report: 11 p.; ReadMe; GIS Files, https://doi.org/10.3133/ofr9588.","productDescription":"Report: 11 p.; ReadMe; GIS Files","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":154620,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0088/report-thumb.jpg"},{"id":7858,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-088/","linkFileType":{"id":5,"text":"html"}},{"id":51078,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0088/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e6ca","contributors":{"authors":[{"text":"Yerkes, R.F.","contributorId":105752,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.F.","affiliations":[],"preferred":false,"id":184556,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Russell H.","contributorId":91074,"corporation":false,"usgs":true,"family":"Campbell","given":"Russell H.","affiliations":[],"preferred":false,"id":184555,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21502,"text":"ofr9589 - 1995 - Preliminary geologic map of the Oat Mountain 7.5' quadrangle, southern California: A digital database","interactions":[{"subject":{"id":21501,"text":"ofr93525 - 1993 - Preliminary geologic map of the Oat Mountain 7.5' Quadrangle, southern California","indexId":"ofr93525","publicationYear":"1993","noYear":false,"title":"Preliminary geologic map of the Oat Mountain 7.5' Quadrangle, southern California"},"predicate":"SUPERSEDED_BY","object":{"id":21502,"text":"ofr9589 - 1995 - Preliminary geologic map of the Oat Mountain 7.5' quadrangle, southern California: A digital database","indexId":"ofr9589","publicationYear":"1995","noYear":false,"title":"Preliminary geologic map of the Oat Mountain 7.5' quadrangle, southern California: A digital database"},"id":1}],"lastModifiedDate":"2023-08-31T20:16:17.015601","indexId":"ofr9589","displayToPublicDate":"1995-07-01T00:00:00","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":"95-89","title":"Preliminary geologic map of the Oat Mountain 7.5' quadrangle, southern California: A digital database","docAbstract":"<p>This database, identified as \"Preliminary Geologic Map of the Oat Mountain 7.5' Quadrangle, southern California: A Digital Database,\" has been approved for release and publication by the Director of the USGS. Although this database has been reviewed and is substantially complete, the USGS reserves the right to revise the data pursuant to further analysis and review. This database is released on condition that neither the USGS nor the U. S. Government may be held liable for any damages resulting from its use.</p>\n<br/>\n<p>This digital map database is compiled from previously published sources combined with some new mapping and modifications in nomenclature. The geologic map database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U. S. Geological Survey. For detailed descriptions of the units, their stratigraphic relations and sources of geologic mapping consult Yerkes and Campbell (1993). More specific information about the units may be available in the original sources.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9589","usgsCitation":"Yerkes, R., and Campbell, R., 1995, Preliminary geologic map of the Oat Mountain 7.5' quadrangle, southern California: A digital database: U.S. Geological Survey Open-File Report 95-89, Readme; Metadata; Data Files, https://doi.org/10.3133/ofr9589.","productDescription":"Readme; Metadata; Data Files","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":7859,"rank":10,"type":{"id":16,"text":"Metadata"},"url":"https://geo-nsdi.er.usgs.gov/metadata/open-file/95-89/metadata.faq.html","linkFileType":{"id":5,"text":"html"}},{"id":109868,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22628.htm","linkFileType":{"id":5,"text":"html"},"description":"22628"},{"id":284025,"rank":6,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/of95-089/oatmtn.tar.gz"},{"id":154598,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":284030,"rank":7,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-089/"},{"id":284029,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/of95-089/om-topo.e00.gz"},{"id":284028,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/of95-089/om-wells.e00.gz"},{"id":284027,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/of95-089/om-strc.e00.gz"},{"id":284026,"rank":5,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/of95-089/om-geol.e00.gz"},{"id":284024,"rank":8,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/1995/of95-089/oatmtn.txt"}],"scale":"24000","country":"United States","state":"California","otherGeospatial":"Oat Mountain 7.5' quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.5,\n              34.25\n            ],\n            [\n              -118.5,\n              34.375\n            ],\n            [\n              -118.625,\n              34.375\n            ],\n            [\n              -118.625,\n              34.25\n            ],\n            [\n              -118.5,\n              34.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae66","contributors":{"authors":[{"text":"Yerkes, R.F.","contributorId":105752,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.F.","affiliations":[],"preferred":false,"id":184552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Russell H.","contributorId":91074,"corporation":false,"usgs":true,"family":"Campbell","given":"Russell H.","affiliations":[],"preferred":false,"id":184551,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20724,"text":"ofr95229 - 1995 - Active-, inactive-, and abandoned-mine information and selected geochemical data for the state of Montana","interactions":[],"lastModifiedDate":"2013-09-17T15:16:49","indexId":"ofr95229","displayToPublicDate":"1995-07-01T00:00:00","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":"95-229","title":"Active-, inactive-, and abandoned-mine information and selected geochemical data for the state of Montana","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr95229","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Ryder, J.L., 1995, Active-, inactive-, and abandoned-mine information and selected geochemical data for the state of Montana (Diskette version.): U.S. Geological Survey Open-File Report 95-229, 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr95229.","productDescription":"1 computer disk ;3 1/2 in.","costCenters":[],"links":[{"id":154167,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1148,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/ofr-95-0229/","linkFileType":{"id":5,"text":"html"}},{"id":277699,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1995/0229/application.zip"}],"edition":"Diskette version.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3306","contributors":{"authors":[{"text":"Ryder, Jean L.","contributorId":80709,"corporation":false,"usgs":true,"family":"Ryder","given":"Jean","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":183131,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21505,"text":"ofr9591 - 1995 - Preliminary Geologic Map of the Topanga 7.5' Quadrangle, Southern California: A Digital Database","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"ofr9591","displayToPublicDate":"1995-07-01T00:00:00","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":"95-91","title":"Preliminary Geologic Map of the Topanga 7.5' Quadrangle, Southern California: A Digital Database","docAbstract":"INTRODUCTION\r\n\r\nThis Open-File report is a digital geologic map database. This pamphlet serves to introduce and describe the digital data. There is no paper map included in the Open-File report.\r\n\r\nThis digital map database is compiled from previously published sources combined with some new mapping and modifications in nomenclature. The geologic map database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U. S. Geological Survey.  For detailed descriptions of the units, their stratigraphic relations and sources of geologic mapping consult Yerkes and Campbell (1994).  More specific information about the units may be available in the original sources. \r\n\r\nThe content and character of the database and methods of obtaining it are described herein. The geologic map  database itself, consisting of three ARC coverages and  one base layer, can be obtained over the Internet or by magnetic tape copy as described below.  The processes of extracting the geologic map database from the tar file, and importing the ARC export coverages (procedure described herein), will result in the creation of an ARC workspace (directory) called 'topnga.' \r\n\r\nThe database was compiled using ARC/INFO version 7.0.3, a commercial Geographic \r\nInformation System (Environmental Systems Research Institute, Redlands, California), with  version 3.0 of the menu interface ALACARTE (Fitzgibbon and Wentworth, 1991, Fitzgibbon, 1991, Wentworth and Fitzgibbon, 1991).  It is stored in uncompressed ARC export format (ARC/INFO version 7.x) in a compressed UNIX tar (tape archive) file.  The tar file was compressed with gzip, and may be uncompressed with  gzip, which is available free of charge via the Internet from the gzip Home Page (http://w3.teaser.fr/~jlgailly/gzip). A tar  utility is required to extract the database from  the  tar file.  This utility is included in most UNIX  systems, and can be obtained free of charge via the Internet from Internet Literacy's Common Internet File Formats Webpage http://www.matisse.net/files/formats.html).  ARC/INFO export files (files with the .e00 extension) can be converted into ARC/INFO coverages in ARC/INFO (see below) and can be read by some other Geographic Information Systems, such as MapInfo via ArcLink and ESRI's ArcView (version 1.0 for Windows 3.1 to 3.11 is available for free from ESRI's web site:  http://www.esri.com).\r\n\r\n1.  Different base layer - The original digital database included separates clipped out of the Los Angeles 1:100,000 sheet.  This release includes a vectorized scan of a scale-stable negative of the Topanga 7.5 minute quadrangle.\r\n\r\n2.  Map projection - The files in the original release were in polyconic projection.  The projection used in this release is state plane, which allows for the tiling of adjacent quadrangles.\r\n\r\n3.  File compression -  The files in the original release were compressed with UNIX compression.  The files in this release are compressed with gzip.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr9591","usgsCitation":"Yerkes, R., and Campbell, R.H., 1995, Preliminary Geologic Map of the Topanga 7.5' Quadrangle, Southern California: A Digital Database: U.S. Geological Survey Open-File Report 95-91, ReadMe; Data Files, https://doi.org/10.3133/ofr9591.","productDescription":"ReadMe; Data Files","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":10098,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-091/","linkFileType":{"id":5,"text":"html"}},{"id":153749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0091/report-thumb.jpg"},{"id":51079,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","projection":"Polyconic","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.63333333333334,34 ], [ -118.63333333333334,34.117777777777775 ], [ -118.61777777777777,34.117777777777775 ], [ -118.61777777777777,34 ], [ -118.63333333333334,34 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cbff","contributors":{"authors":[{"text":"Yerkes, R.F.","contributorId":105752,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.F.","affiliations":[],"preferred":false,"id":184558,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, R. H.","contributorId":52160,"corporation":false,"usgs":true,"family":"Campbell","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":184557,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17180,"text":"ofr9578 - 1995 - Geometeorological data collected by the USGS Desert Winds Project at Gold Spring, Great Basin desert, northeastern Arizona, 1979-1992","interactions":[],"lastModifiedDate":"2022-08-04T21:20:40.149997","indexId":"ofr9578","displayToPublicDate":"1995-07-01T00:00:00","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":"95-78","title":"Geometeorological data collected by the USGS Desert Winds Project at Gold Spring, Great Basin desert, northeastern Arizona, 1979-1992","docAbstract":"The primary purpose of the Desert Winds Project (DWP) is to obtain high-resolution meteorological data and related surface geological and vegetation data for natural (e.g., uncultivated) desert sites where wind is or has been a major erosive or depositional force. The objectives are twofold: (1) to provide the detailed field measurements needed to carry out quantitative studies of wind as an agent of surface geologic change; and (2) to establish a baseline for defining the 'normal' range of climatic conditions that can be expected to occur on a decadal time scale, in areas considered representative of the major American deserts. The Gold Spring locality was selected to represent that part of the Great Basin Desert that extends into northeastern Arizona. The long-term goal for acquiring and analyzing the Desert Winds Project data is to use them to address problems of land resource degradation by wind, whether resulting from climatic variation aridification) or human activities (desertification), or both (see techinfo.doc).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9578","usgsCitation":"Helm, P.J., Breed, C.S., Tigges, R., and Garcia, P.A., 1995, Geometeorological data collected by the USGS Desert Winds Project at Gold Spring, Great Basin desert, northeastern Arizona, 1979-1992 (Version 3.0): U.S. Geological Survey Open-File Report 95-78, HTML Document; CD-ROM, https://doi.org/10.3133/ofr9578.","productDescription":"HTML Document; CD-ROM","costCenters":[],"links":[{"id":151063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":404854,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13250.htm","linkFileType":{"id":5,"text":"html"}},{"id":1056,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-078","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona","otherGeospatial":"Gold Spring, Great Basin Desert","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.26953125,\n              35.64836915737426\n            ],\n            [\n              -111.00311279296875,\n              35.64836915737426\n            ],\n            [\n              -111.00311279296875,\n              35.94910642813857\n            ],\n            [\n              -111.26953125,\n              35.94910642813857\n            ],\n            [\n              -111.26953125,\n              35.64836915737426\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 3.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c5a9","contributors":{"authors":[{"text":"Helm, P. J.","contributorId":72813,"corporation":false,"usgs":true,"family":"Helm","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":175284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breed, C. S.","contributorId":39809,"corporation":false,"usgs":true,"family":"Breed","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":175283,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tigges, R. K.","contributorId":74769,"corporation":false,"usgs":true,"family":"Tigges","given":"R. K.","affiliations":[],"preferred":false,"id":175285,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Garcia, P. A.","contributorId":36954,"corporation":false,"usgs":true,"family":"Garcia","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":175282,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":17760,"text":"ofr94365 - 1995 - Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska; results of investigations, 1987-90","interactions":[{"subject":{"id":17760,"text":"ofr94365 - 1995 - Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska; results of investigations, 1987-90","indexId":"ofr94365","publicationYear":"1995","noYear":false,"title":"Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska; results of investigations, 1987-90"},"predicate":"SUPERSEDED_BY","object":{"id":253,"text":"wsp2451 - 1996 - Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Results of investigations, 1987-90","indexId":"wsp2451","publicationYear":"1996","noYear":false,"title":"Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Results of investigations, 1987-90"},"id":1}],"supersededBy":{"id":253,"text":"wsp2451 - 1996 - Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Results of investigations, 1987-90","indexId":"wsp2451","publicationYear":"1996","noYear":false,"title":"Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Results of investigations, 1987-90"},"lastModifiedDate":"2021-01-07T18:02:39.813916","indexId":"ofr94365","displayToPublicDate":"1995-07-01T00:00:00","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":"94-365","title":"Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska; results of investigations, 1987-90","docAbstract":"<p>Surface-water-quality conditions and trends were assessed in the lower Kansas River Basin, which drains about 15,300 square miles of mainly agricultural land in southeast Nebraska and northeast Kansas. On the basis of established water-quality criteria, most streams in the basin were suitable for uses such as public-water supply, irrigation, and maintenance of aquatic life. However, most concerns identified from a previous analysis of available data through 1986 are substantiated by analysis of data for May 1987 through April 1990. Less-than-normal precipitation and runoff during 1987-90 affected surface-water quality and are important factors in the interpretation of results.</p><p>Dissolved-solids concentrations in the main stem Kansas River during May 1987 through April 1990 commonly exceeded 500 milligrams per liter, which may be of concern for public-water supplies and for the irrigation of sensitive crops. Large concentrations of chloride in the Kansas River are derived from ground water discharging in the Smoky Hill River Basin west of the study unit. Trends of increasing concentrations of some dissolved major ions were statistically significant in the northwestern part of the study unit, which could reflect substantial increases in irrigated acreage.</p><p>The largest concentrations of suspended sediment in streams during May 1987 through April 1990 were associated with high-density cropland in areas of little local relief and medium-density irrigated cropland in more dissected areas. The smallest concentrations were measured downstream from large reservoirs and in streams draining areas having little or no row-crop cultivation. Mean annual suspended-sediment transport rates in the main stem Kansas River increased substantially in the downstream direction. No conclusions could be reached concerning the relations of suspended-sediment transport, yields, or trends to natural and human factors.</p><p>The largest sources of nitrogen and phosphorus in the study unit were fertilizer and livestock. Nitrate-nitrogen concentrations in stream-water samples did not exceed 10 milligams per liter; relatively large concentrations in the northwestern part of the study unit were associated with fertilizer application. Concentrations of total phosphorus generally were largest in the northwestern part of the study unit, which probably relates to the prevalence of cultivated land, fertilizer application, and livestock wastes.</p><p>Deficiencies in dissolved-oxygen concentrations in streams occurred locally, as a result of discharges from wastewater-treatment plants, algal respiration, and inadequate reaeration associated with small streamflow. Large densities of a fecal-indicator bacterium, Escherichia coli, were associated with discharges from municipal wastewater-treatment plants and, especially in the northwestern part of the study unit, with transport of feca</p><p>The largest concentrations of the herbicide atrazine generally were measured where the largest quantities of atrazine were applied to the land. Large atrazine concentrations, 10 to 20 micrograms per liter, were measured most&nbsp;frequently in unregulated principal streams during May and June. Downstream of reservoirs, the seasonal variability of atrazine concentrations was decreased compared to that of inflowing streams.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94365","usgsCitation":"1995, Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska; results of investigations, 1987-90: U.S. Geological Survey Open-File Report 94-365, viii, 129 p., https://doi.org/10.3133/ofr94365.","productDescription":"viii, 129 p.","numberOfPages":"141","costCenters":[],"links":[{"id":150575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0365/report-thumb.jpg"},{"id":359241,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0365/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kansas, Nebraska","otherGeospatial":"Kansas River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99,\n              38.75\n            ],\n            [\n              -94.6,\n              38.75\n            ],\n            [\n              -94.6,\n              41.1\n            ],\n            [\n              -99,\n              41.1\n            ],\n            [\n              -99,\n              38.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a445","contributors":{"editors":[{"text":"Helgesen, J. O.","contributorId":62600,"corporation":false,"usgs":true,"family":"Helgesen","given":"J.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":725471,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":17228,"text":"ofr94305 - 1995 - Hydrochemical data base for the Death Valley Region, California and Nevada","interactions":[],"lastModifiedDate":"2013-09-18T07:37:48","indexId":"ofr94305","displayToPublicDate":"1995-07-01T00:00:00","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":"94-305","title":"Hydrochemical data base for the Death Valley Region, California and Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey :Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94305","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Perfect, D.L., Faunt, C., Steinkampf, W., and Turner, A.K., 1995, Hydrochemical data base for the Death Valley Region, California and Nevada: U.S. Geological Survey Open-File Report 94-305, 2 computer disks ;3 1/2 in. +1 user guide (iii, 10 p. : ill., map ; 28 cm.), https://doi.org/10.3133/ofr94305.","productDescription":"2 computer disks ;3 1/2 in. +1 user guide (iii, 10 p. : ill., map ; 28 cm.)","costCenters":[],"links":[{"id":149282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0305/report-thumb.jpg"},{"id":46377,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0305/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":277766,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1994/0305/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628ec3","contributors":{"authors":[{"text":"Perfect, Diana L.","contributorId":102741,"corporation":false,"usgs":true,"family":"Perfect","given":"Diana","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":175506,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faunt, C.C. 0000-0001-5659-7529","orcid":"https://orcid.org/0000-0001-5659-7529","contributorId":103314,"corporation":false,"usgs":true,"family":"Faunt","given":"C.C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":175507,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Steinkampf, W.C.","contributorId":8137,"corporation":false,"usgs":true,"family":"Steinkampf","given":"W.C.","affiliations":[],"preferred":false,"id":175504,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Turner, A. K.","contributorId":82351,"corporation":false,"usgs":true,"family":"Turner","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":175505,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":18047,"text":"ofr9577 - 1995 - A bibliography of some geophysical computer programs, data bases, and maps from the U.S. Geological Survey, 1971-1994","interactions":[],"lastModifiedDate":"2012-02-02T00:07:18","indexId":"ofr9577","displayToPublicDate":"1995-07-01T00:00:00","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":"95-77","title":"A bibliography of some geophysical computer programs, data bases, and maps from the U.S. Geological Survey, 1971-1994","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9577","usgsCitation":"Bankey, V., and Anderson, W.L., 1995, A bibliography of some geophysical computer programs, data bases, and maps from the U.S. Geological Survey, 1971-1994: U.S. Geological Survey Open-File Report 95-77, 30 p. ;28 cm., https://doi.org/10.3133/ofr9577.","productDescription":"30 p. ;28 cm.","costCenters":[],"links":[{"id":150194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0077/report-thumb.jpg"},{"id":8088,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/ofr-95-0077/of-95-77.html","linkFileType":{"id":5,"text":"html"}},{"id":47291,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0077/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4975e4b0b290850ef30a","contributors":{"authors":[{"text":"Bankey, Viki viki@usgs.gov","contributorId":1238,"corporation":false,"usgs":true,"family":"Bankey","given":"Viki","email":"viki@usgs.gov","affiliations":[],"preferred":true,"id":178436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Walter L.","contributorId":99133,"corporation":false,"usgs":true,"family":"Anderson","given":"Walter","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":178437,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29455,"text":"wri944199 - 1995 - Water resources of the Grand Portage Indian Reservation, northeastern Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T11:28:06","indexId":"wri944199","displayToPublicDate":"1995-07-01T00:00:00","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":"94-4199","title":"Water resources of the Grand Portage Indian Reservation, northeastern Minnesota","docAbstract":"<p>The Grand Portage Indian Reservation Tribal Council needs information about the availability and quality of the ground water in the Reservation to develop, protect, and manage this resource for future use. The U.S. Geological Survey, in cooperation with the Grand Portage Indian Reservation Tribal Council, did a three-year study of the ground water in the Reservation to provide this needed information. This report presents the results of that study.</p>\n<p>Presently, ground water from bedrock is the principal source of supply for municipal, commercial, and residential water use. The bedrock aquifers are the (1) North Shore Volcanic Group basalt, (2) Keweenawan Volcanic and intrusive rocks, which are gabbro and diabase, and (3) Rove Formation argillite, slate, and graywacke. Sand and gravel aquifers are a small source of ground water.</p>\n<p>The storage coefficient of the bedrock aquifers was estimated to be 1 x 10<sup>-4</sup>, which is a small value typical of confined, fractured rock aquifers. The median estimate of transmissivity determined from data for 17 wells completed in bedrock was 20 feet squared per day; the range was from 3 to 500 feet squared per day. Reported yield of 19 wells completed in bedrock had a range of 1 to 100 gallons per minute and a median of 7 gallons per minute. The median yield of 11 wells completed in the North Shore Volcanic Group was 16 gallons per minute; the median yield of 8 wells completed in the Keweenawan Volcanic and intrusive rocks and Rove Formation was 4 gallons per minute.</p>\n<p>Geophysical logs and televiewer images of two wells completed in bedrock indicated the boreholes penetrated many fractures. Hydrofracturing of the two wells increased their yield from about 0.05 and 0.25 gallons per minute to about 1.5 and 1.2 gallons per minute, respectively. Although the estimated yield from the two wells was increased by 30 and by nearly 5 times after hydrofracturing, the well yield after hydrofracturing was still small.</p>\n<p>Water types determined from analyses of water from nine wells completed in bedrock were sodium-chloride, calcium-chloride, sodium-bicarbonate, and calcium-bicarbonate. Water from three wells had concentrations of dissolved solids (800 to 3,110 milligrams per liter) and dissolved chloride (410 to 1,600 milligrams per liter) that were higher than their respective Secondary Maximum Contaminant Levels of 500 and 250 milligrams per liter established by the U.S. Environmental Protection Agency. Water from two wells had concentrations of dissolved iron (1,600 and 1,300 micrograms per liter) that were higher than the Secondary Maximum Contaminant Level of 300 micrograms per liter. Water from an observation well located about 200 feet downgradient from an abandoned landfill and screened from 79 to 84 feet below land surface in a gravel aquifer had a trace amount of toluene (0.2 micrograms per liter). The presence of toluene suggested possible contamination.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/wri944199","collaboration":"Prepared in cooperation with the Grand Portage Indian Reservation Tribal Council","usgsCitation":"Ruhl, J.F., 1995, Water resources of the Grand Portage Indian Reservation, northeastern Minnesota: U.S. Geological Survey Water-Resources Investigations Report 94-4199, vi, 28 p., https://doi.org/10.3133/wri944199.","productDescription":"vi, 28 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":124164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4199/report-thumb.jpg"},{"id":58300,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4199/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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F.","contributorId":81866,"corporation":false,"usgs":true,"family":"Ruhl","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":201550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29626,"text":"wri924171 - 1995 - Selected hydrogeologic and water-quality data from Jones Beach Island, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"wri924171","displayToPublicDate":"1995-07-01T00:00:00","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":"92-4171","title":"Selected hydrogeologic and water-quality data from Jones Beach Island, Long Island, New York","docAbstract":"A data-collection site was instrumented on Jones Beach Island, a barrier island south of Long Island, N.Y., to study local freshwater/ saltwater relations in the shallow ground-water system.   A geologic test boring revealed about 88 feet of well-sorted glacial outwash sand above about 15 feet of Gardiners Clay, which directly overlies silty sand of the Magothy Formation.   Tidal effects on water levels in Great South Bay, the upper glacial aquifer, and the Magothy aquifer were observed and quantified with a tidal gage in the bay and analog water-level recorders in the wells.Chloride concentrations in the upper Magothy aquifer were higher than expected--about 270 mg/L (milligrams per liter), and those in the upper glacial aquifer were 17,000 to 19,000 mg/L, about the same as in Great South Bay. Estimates of pressure and freshwater equivalent heads indicate that, at the data-collection site, freshwater is discharging upward from the Magothy aquifer into the salty upper glacial aquifer, but dilution by this freshwater is undetectable. The reason for the elevated chloride concentration in the Magothy aquifer cannot be determined from available hydrogeologic information.","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/wri924171","usgsCitation":"Scorca, M., Reilly, T.E., and Franke, O., 1995, Selected hydrogeologic and water-quality data from Jones Beach Island, Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 92-4171, iv, 21 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924171.","productDescription":"iv, 21 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":160014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4171/report-thumb.jpg"},{"id":58447,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4171/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1eb4","contributors":{"authors":[{"text":"Scorca, M. P.","contributorId":21997,"corporation":false,"usgs":true,"family":"Scorca","given":"M. P.","affiliations":[],"preferred":false,"id":201838,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reilly, T. E.","contributorId":79460,"corporation":false,"usgs":true,"family":"Reilly","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":201840,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Franke, O.L.","contributorId":57082,"corporation":false,"usgs":true,"family":"Franke","given":"O.L.","affiliations":[],"preferred":false,"id":201839,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28664,"text":"wri944128 - 1995 - Water quality of the Boca Raton canal system and effects of the Hillsboro Canal inflow, southeastern Florida, 1990-91","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri944128","displayToPublicDate":"1995-07-01T00:00:00","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":"94-4128","title":"Water quality of the Boca Raton canal system and effects of the Hillsboro Canal inflow, southeastern Florida, 1990-91","docAbstract":"The City of Boca Raton in southeastern Palm Beach County, Florida, is an urban residential area that has sustained a constant population growth with subsequent increase in water use. The Boca Raton network of canals is controlled to provide for drainage of excess water, to maintain proper coastal ground-water levels to prevent saltwater intrusion, and to recharge the surficial aquifer system from which the city withdraws potable water. Most of the water supplied to the Boca Raton canal system and the surficial aquifer system, other than rainfall and runoff, is pumped from the Hillsboro Canal. The Biscayne aquifer, principal hydrogeologic unit of the surficial aquifer system, is highly permeable and there is a close relation between water levels in the canals and the aquifer. The amount of water supplied by seepage from the conservation areas is unknown. Because the Hillsboro Canal flows from Lake Okeechobee and Water Conservation Areas 1 and 2, which are places of more highly mineralized ground water and surface water, the canal is a possible source of contamination. Water samples were collected at 10 canal sites during wet and dry seasons and analyzed for major inorganic ions and related characteristics, nutrients, and trace elements. All concentrations were generally within or less than the drinking-water standards established by the Florida Department of Environmental Protection. The high concentrations of sodium and chloride that were detected in samples from the Boca Raton canal system are probably from the more mineralized water of the Hillsboro Canal. Other water-quality data, gathered from various sources from 1982 through 1991, did not indicate any significant changes nor trends. The effects of the Hillsboro Canal on the water quality of the Boca Raton canal system are indicated by increased concentrations of sodium, chloride, dissolved solids, and total organic carbon. Concentrations of the constituents in the canal water generally decrease with distance from the Hillsboro Canal pumping station and are the result of dilution by receiving canal waters.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944128","usgsCitation":"McKenzie, D., 1995, Water quality of the Boca Raton canal system and effects of the Hillsboro Canal inflow, southeastern Florida, 1990-91: U.S. Geological Survey Water-Resources Investigations Report 94-4128, iv, 14 p. :ill., map ;28 cm. [PGS - 18 p.], https://doi.org/10.3133/wri944128.","productDescription":"iv, 14 p. :ill., map ;28 cm. [PGS - 18 p.]","costCenters":[],"links":[{"id":2258,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri944128","linkFileType":{"id":5,"text":"html"}},{"id":158337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae85","contributors":{"authors":[{"text":"McKenzie, D.J.","contributorId":75134,"corporation":false,"usgs":true,"family":"McKenzie","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":200196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29463,"text":"wri944094 - 1995 - Surface-water-quality assessment of the upper Illinois River Basin in Illinois, Indiana, and Wisconsin: Analysis of relations between fish-community structure and environmental conditions in the Fox, Des Plaines, and Du Page River basins in Illinois, 1982-84","interactions":[],"lastModifiedDate":"2022-09-13T19:30:12.180562","indexId":"wri944094","displayToPublicDate":"1995-07-01T00:00:00","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":"94-4094","title":"Surface-water-quality assessment of the upper Illinois River Basin in Illinois, Indiana, and Wisconsin: Analysis of relations between fish-community structure and environmental conditions in the Fox, Des Plaines, and Du Page River basins in Illinois, 1982-84","docAbstract":"Multivariate analyses of fish-community, water- quality, streambed-sediment-quality, and habitat data collected from 1982 through 1984 in the Fox, Des Plaines, and Du Page River Basins in northeastern Illinois indicate that fish-community structure was strongly related to water-quality gradients commonly associated with differences between agricultural and urban land uses. Detrended correspondence analysis (DCA) and the Alternate Index of Biotic Integrity (AIBI) tended to group fish communities by river basin. Streams in the predominantly agricultural Fox River Basin tended to have similar DCA scores, the highest AIBI scores, and relatively diverse fish communities that usually included several intolerant species. Streams in the more heavily urbanized Chicago, Little Calumet, Des Plaines, and Du Page River Basins tended to have lower AIBI scores and fish communities dominated by fewer; more tolerant species. Correlative (Spearman's rho) and graphical analyses showed that DCA and AIBI scores for nonwadable sites were more strongly related to water qualiity and streambed- sediment quality than to habitat conditions. DCA and AIBI scores for wadable sites were most strongly related to water quality, were not related to streambed-sediment quality, and were moderately related to habitat variables indicative of stream size. Streams in the Fox River Basin had the smallest concentrations of chemical constituents commonly associated with anthropogenic sources. Streams in the heavily urbanized Des Plaines and Du Page River Basins had larger concentrations of chemical constituents associated with urban runoff and point-sourca discharges. Although fish-community structure was strongly related to the water quality, U.S. Environmental Protection Agency acute and chronic criteria for the protection of freshwater aquatic life were exceeded at few stations. These fish communities may have been responding either to concentrations below the U.S. Environmental Protection Agency criteria or to cumulative or synergistic effects of overall water quality.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944094","usgsCitation":"Ruhl, P.M., 1995, Surface-water-quality assessment of the upper Illinois River Basin in Illinois, Indiana, and Wisconsin: Analysis of relations between fish-community structure and environmental conditions in the Fox, Des Plaines, and Du Page River basins in Illinois, 1982-84: U.S. Geological Survey Water-Resources Investigations Report 94-4094, v, 50 p., https://doi.org/10.3133/wri944094.","productDescription":"v, 50 p.","costCenters":[],"links":[{"id":406634,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47985.htm","linkFileType":{"id":5,"text":"html"}},{"id":58308,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4094/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160434,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4094/report-thumb.jpg"}],"country":"United States","state":"Illinois, Indiana, Wisconsin","otherGeospatial":"Fox, Des Plaines, and Du Page River basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.1081,\n              41.3\n            ],\n            [\n              -87.3567,\n              41.3\n            ],\n            [\n              -87.3567,\n              43.1833\n            ],\n            [\n              -89.1081,\n              43.1833\n            ],\n            [\n              -89.1081,\n              41.3\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a3ec","contributors":{"authors":[{"text":"Ruhl, P. M.","contributorId":30251,"corporation":false,"usgs":true,"family":"Ruhl","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":201561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29188,"text":"wri944077 - 1995 - Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Dissolved oxygen and Escherichia coli bacteria in streams during low flow, July 1988 through July 1989","interactions":[],"lastModifiedDate":"2022-09-07T21:36:00.154359","indexId":"wri944077","displayToPublicDate":"1995-07-01T00:00:00","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":"94-4077","title":"Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Dissolved oxygen and Escherichia coli bacteria in streams during low flow, July 1988 through July 1989","docAbstract":"The 15,300-square-mile lower Kansas River Basin in Kansas and Nebraska was investigated, as one of the pilot study units of the U.S. Geological Survey's National Water-Quality Assessment (NAWQA) Program, to address a variety of water-quality issues. This report describes sanitary quality of streams as defined by concentrations of dissolved oxygen (DO) and densities of a fecal-indicator bacterium, Escherichia coli (E. coli).  Sixty-one surface-water sampling sites were chosen for this investigation. Synoptic surveys were conducted in July 1988, November 1988, March 1989, and May 1989 to define the concentrations and diel and seasonal variability in concentrations of DO. Synoptic surveys were conducted in July 1988 and July 1989 to define densities of E. coli. Ancillary data included measurements of specific conductance, pH, water temperature. barometric pressure, and concentrations of nutrients, total organic carbon, chlorophyll, and suspended sediment. Surveys were conducted during stable-flow, dry-weather conditions.  During the July 1988 synoptic survey for DO, emphasis was placed on the measurement of DO under maximum stress (high water temperature, low streamflow, and predawn conditions). Of 31 sites sampled just before dawn, 5 had DO concentrations less than the 5.0-milligrams-perliter, l-day minimum warmwater criterion for early life stages as established by the U.S. Environmental Protection Agency (USEPA), and 4 of these 5 sites had concentrations less than the 3.0-milligrams-per-liter criterion for all other life stages. For all four synoptic surveys, a total of 392 DO determinations were made, and 9 (2.3 percent) were less than water-quality criteria. Concentrations of DO less than water-quality criteria in the study unit are localized occurrences and do not reflect regional differences in DO. The most severe DO deficiencies are the result of discharges from wastewater-treatment plants into small tributary streams with inadequate assimilation capacity. Algal respiratory demand in combination with reduced physical reaeration associated with extreme low flow probably also contributes to temporary, localized deficiencies.  Densities of E. coli were determined at 57 surface-water sampling sites during the syn- optic survey in July 1988. Results indicate large regional differences in E. coli densities within the study unit. Densities orE. coli in water at 19 sites in the Big Blue River subbasin, exclusive of the Little Blue River subbasin, ranged from 120 to 260,000 col/100 mL (colonies per 100 milliliters), with a median density of 2,400 col/100 mL. Densities at the 11 sites in the Little Blue River ranged from 100 to 30,000 col/100 mL, with a median density of 940 col/100 mL. Densities at the 27 sites in the Kansas River subbasin ranged from less than 1 to 1,000 col/100 mL, with a median density of 88 col/100 mL. Densities at 84 percent of the sites in the Big Blue River subbasin exceeded the USEPA E. coli criterion of 576 col/100 mL for infrequently used full-body contact recreation, and 53 percent exceeded the 2,000 cot/I00 mL fecal coliform criterion for uses other than full-body contact established by the Kansas Department of Health and Environment. Densities at 73 percent of the sites in the Little Blue River subbasin exceeded the 576 col/100 mL E. coli criterion, and 36 percent exceeded the 2,000 col/100 mL fecal coliform criterion. Densities at one of the sites in the Kansas River subbasin exceeded the 576 col/100 mL E. coli criterion, and none exceeded the 2,000 col/100 mL fecal-coliform criterion.  The largest densities of E. coli in the study unit were the result of discharges from municipal wastewater-treatment plants; however, densities in the Big Blue and Little Blue River subbasins were generally larger than those in the Kansas River subbasin. These larger densities in the Big Blue and Little Blue River subbasins may have been the result of irrigation return flow from fields where manure was used as a soil","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944077","usgsCitation":"Pope, L.M., 1995, Surface-water-quality assessment of the lower Kansas River basin, Kansas and Nebraska: Dissolved oxygen and Escherichia coli bacteria in streams during low flow, July 1988 through July 1989: U.S. Geological Survey Water-Resources Investigations Report 94-4077, vi, 102 p., https://doi.org/10.3133/wri944077.","productDescription":"vi, 102 p.","costCenters":[],"links":[{"id":58054,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4077/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159408,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4077/report-thumb.jpg"},{"id":406352,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47973.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kansas, Nebraska","otherGeospatial":"Kansas River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99,\n              38.650\n            ],\n            [\n              -94.5597,\n              38.650\n            ],\n            [\n              -94.5597,\n              41.2583\n            ],\n            [\n              -99,\n              41.2583\n            ],\n            [\n              -99,\n              38.650\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a43a","contributors":{"authors":[{"text":"Pope, L. M.","contributorId":71939,"corporation":false,"usgs":true,"family":"Pope","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":201111,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31874,"text":"ofr9526 - 1995 - Map showing potential metal-mine drainage hazards in Colorado, based on mineral-deposit geology","interactions":[],"lastModifiedDate":"2020-09-24T14:44:20.800501","indexId":"ofr9526","displayToPublicDate":"1995-07-01T00:00:00","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":"95-26","title":"Map showing potential metal-mine drainage hazards in Colorado, based on mineral-deposit geology","docAbstract":"This map, compiled by the U.S. Geological Survey (USGS) in cooperation with the Colorado Geological Survey (CGS) and the U. S. Bureau of Land Management (BLM), shows potential mine-drainage hazards that may exist in Colorado metal-mining districts, as indicated by the geologic characteristics of the mineral deposits that occur in the respective districts. It was designed to demonstrate how geologic and geochemical information can be used on a regional scale to help assess the potential for mining-related and natural drainage problems in mining districts, unmined mineralized areas, and surrounding watersheds. The map also provides information on the distribution of different mineral deposit types across Colorado. A GIS (Geographic Information System) format was used to integrate geologic, geochemical, water-quality, climate, landuse, and ecological data from diverse sources. Likely mine-drainage signatures were defined for each mining district based on: (1) a review of the geologic characteristics of the mining district, including mineralogy, trace-element content, host-rock lithology, and wallrock alteration, and; (2) results of site specific studies on the geologic controls on mine-drainage composition.","language":"English","doi":"10.3133/ofr9526","usgsCitation":"Plumlee, G.S., Streufert, R.K., Smith, K.S., Smith, S.M., Wallace, A.R., Toth, M.I., Nash, J.T., Robinson, R.A., Ficklin, W.H., and Lee, G.K., 1995, Map showing potential metal-mine drainage hazards in Colorado, based on mineral-deposit geology (Version 1.0): U.S. Geological Survey Open-File Report 95-26, Report: 11 p.; 1 Sheet: 44.00 x 34.00 inches, https://doi.org/10.3133/ofr9526.","productDescription":"Report: 11 p.; 1 Sheet: 44.00 x 34.00 inches","costCenters":[],"links":[{"id":160234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":378689,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/ofr-95-26/OFR95-26text508.pdf","text":"Pamphlet","size":"86 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 95-26 map pamphlet"},{"id":378690,"rank":3,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1995/ofr-95-26/ofr95-26.pdf","text":"Map","size":"1.3 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 95-26 map sheet"}],"scale":"750000","country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.06298828125,\n              40.93011520598305\n            ],\n            [\n              -109.05029296875,\n              40.97989806962013\n            ],\n            [\n              -109.05029296875,\n              36.94989178681327\n            ],\n            [\n              -101.9970703125,\n              37.00255267215955\n            ],\n            [\n              -102.06298828125,\n              40.93011520598305\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659c88","contributors":{"authors":[{"text":"Plumlee, Geoffrey S. 0000-0002-9607-5626 gplumlee@usgs.gov","orcid":"https://orcid.org/0000-0002-9607-5626","contributorId":960,"corporation":false,"usgs":true,"family":"Plumlee","given":"Geoffrey","email":"gplumlee@usgs.gov","middleInitial":"S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":207142,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Streufert, Randall K.","contributorId":45353,"corporation":false,"usgs":true,"family":"Streufert","given":"Randall","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":207149,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Kathleen S. 0000-0001-8547-9804 ksmith@usgs.gov","orcid":"https://orcid.org/0000-0001-8547-9804","contributorId":182,"corporation":false,"usgs":true,"family":"Smith","given":"Kathleen","email":"ksmith@usgs.gov","middleInitial":"S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":207141,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Steven M. 0000-0003-3591-5377 smsmith@usgs.gov","orcid":"https://orcid.org/0000-0003-3591-5377","contributorId":1460,"corporation":false,"usgs":true,"family":"Smith","given":"Steven","email":"smsmith@usgs.gov","middleInitial":"M.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":207144,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wallace, Alan R.","contributorId":6024,"corporation":false,"usgs":true,"family":"Wallace","given":"Alan","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":207145,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Toth, Margo I.","contributorId":18365,"corporation":false,"usgs":true,"family":"Toth","given":"Margo","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":207146,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Nash, J. Thomas","contributorId":26306,"corporation":false,"usgs":true,"family":"Nash","given":"J.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":207148,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Robinson, Rob A.","contributorId":22391,"corporation":false,"usgs":true,"family":"Robinson","given":"Rob","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":207147,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ficklin, Walter H.","contributorId":52565,"corporation":false,"usgs":true,"family":"Ficklin","given":"Walter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":207150,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Lee, Gregory K. glee@usgs.gov","contributorId":1220,"corporation":false,"usgs":true,"family":"Lee","given":"Gregory","email":"glee@usgs.gov","middleInitial":"K.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":207143,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":4986,"text":"fs15395 - 1995 - Review of sediment data in the South Platte River Basin, Colorado, 1980-92","interactions":[],"lastModifiedDate":"2017-04-20T16:50:39","indexId":"fs15395","displayToPublicDate":"1995-07-01T00:00:00","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":"153-95","title":"Review of sediment data in the South Platte River Basin, Colorado, 1980-92","docAbstract":"<p>Suspended-sediment transport and its relation to water quality are important issues in the South Platte River Basin. Most sediment enters the South Platte River during snowmelt runoff from March to June. The suspended sediment varies by particle size, concentration, and load. Suspended-sediment data in the South Platte River for water years 1980-92 are limited; therefore, only generalizations can be made concerning land use and its effects on suspended-sediment concentrations and loads in the South Platte River. More data are needed before detailed comparisons can be made.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs15395","usgsCitation":"Heiny, J.S., 1995, Review of sediment data in the South Platte River Basin, Colorado, 1980-92: U.S. Geological Survey Fact Sheet 153-95, 2 p., https://doi.org/10.3133/fs15395.","productDescription":"2 p.","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"links":[{"id":200,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0153/fs15395.pdf","text":"Report","size":"148 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 153-95"},{"id":121272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0153/coverthb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db603fd2","contributors":{"authors":[{"text":"Heiny, Janet S.","contributorId":93468,"corporation":false,"usgs":true,"family":"Heiny","given":"Janet","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":150242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4868,"text":"ds31rel1 - 1995 - Profiles of gamma-ray and magnetic data for aerial surveys over parts of the Western United States from longitude 108 to 126 degrees W. and from latitude 34 to 49 degrees N.","interactions":[],"lastModifiedDate":"2012-02-10T00:10:06","indexId":"ds31rel1","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"31","title":"Profiles of gamma-ray and magnetic data for aerial surveys over parts of the Western United States from longitude 108 to 126 degrees W. and from latitude 34 to 49 degrees N.","docAbstract":"This CD-ROM contains images generated from geophysical data, software for displaying and analyzing the images and software for displaying and examining profile data from aerial surveys flown as part of the National Uranium Resource Evaluation (NURE) Program of the U.S. Department of Energy. The images included are of gamma-ray data (uranium, thorium, and potassium channels), Bouguer gravity data, isostatic residual gravity data, aeromagnetic anomalies, topography, and topography with bathymetry. This publication contains image data for the conterminous United States and profile data for the conterminous United States within the area longitude 108 to 126 degrees W. and latitude 34 to 49 degrees N. The profile data include apparent surface concentrations of potassium, uranium, and thorium, the residual magnetic field, and the height above the ground. The images on this CD-ROM include graytone and color images of each data set, color shaded-relief images of the potential-field and topographic data, and color composite images of the gamma-ray data. The image display and analysis software can register images with geographic and geologic overlays. The profile display software permits the user to view the profiles as well as obtain data listings and export ASCII versions of data for selected flight lines.","language":"ENGLISH","publisher":"U.S. Geological Survey :USGS Information Services,","doi":"10.3133/ds31rel1","isbn":"0607624418","usgsCitation":"Duval, J.S., 1995, Profiles of gamma-ray and magnetic data for aerial surveys over parts of the Western United States from longitude 108 to 126 degrees W. and from latitude 34 to 49 degrees N. (Release 1): U.S. Geological Survey Data Series 31, 1 computer laser optical disc :col. ;4 3/4 in., https://doi.org/10.3133/ds31rel1.","productDescription":"1 computer laser optical disc :col. ;4 3/4 in.","costCenters":[],"links":[{"id":139687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -126,34 ], [ -126,49 ], [ -108,49 ], [ -108,34 ], [ -126,34 ] ] ] } } ] }","edition":"Release 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649f6a","contributors":{"authors":[{"text":"Duval, Joseph S.","contributorId":22314,"corporation":false,"usgs":true,"family":"Duval","given":"Joseph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":149981,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70018833,"text":"70018833 - 1995 - Source parameters and crustal Q for four earthquakes in South Carolina","interactions":[],"lastModifiedDate":"2025-07-29T16:47:27.902508","indexId":"70018833","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Source parameters and crustal Q for four earthquakes in South Carolina","docAbstract":"<p><span>Two three-component seismometers (one surface and one borehole) were re-installed on the Savannah River Site (SRS), South Carolina in July 1992 to determine attenuation in the Coastal Plain sediment wedge and source parameters of local earthquakes. Four earthquakes&nbsp;</span><strong>M</strong><span>&nbsp;∼ 1.8 to 3.6 were recorded during the next 6 months. The largest event was located near Summerville within the meizoseismal area for the 1886 Charleston earthquake. Two shocks were located 50 km to the east near Neeses, and one was located 20 km north of the SRS near Aiken. Although source parameters have been determined from strong motion data and short-period regional networks for east coast earthquakes, such as the Saguenay, Nahanni, and Mt. Laurier earthquakes (e.g.,&nbsp;</span><a class=\"link link-ref xref-bibr\" data-modal-source-id=\"REF3\">Atkinson, 1993</a><span>), these are some of the first source parameters determined from broad-band digital recorders. Seismograms for the Summerville event are also available from Chapel Hill, North Carolina and Blacksburg, Virginia, providing estimates of&nbsp;</span><i>t</i><span>* beyond 200 km. Here we determine source parameters such as moment, stress drop, and the attenuation parameter&nbsp;</span><i>t</i><span>* using a non-linear least-squares algorithm. We do not correct for site response because the deepest borehole is not below the Coastal Plain sediments (about 300m thick at this site) and because only one station is available for most of the data. Values of&nbsp;</span><i>t*</i><span>&nbsp;are marginally higher from seismograms recorded at the surface when compared to records from the 91m depth borehole seismograph. A value of 170-200 bars was determined for the Brune stress drop of the Summerville event using the borehole data, which is high compared to a value of 50 bars usually specified for modeling strong motion in western North America, but similar to other estimates for eastern North America. A higher stress drop leads to a higher seismic risk because peak acceleration is approximately proportional to stress drop. Moreover, mid- to upper-crustal Qs are in the range of 2,000 to 3,000, which would permit the propagation of high frequency seismic waves. A comparison of the surface records from the SRS with a record from the USGS dense array at Parkfield, CA for an event at about the same distance range and moment as the Summerville event-SRS case shows that the peak acceleration of the Summerville event is 16 times higher than that for the event from California (stress drop of 21 bars).</span></p>","language":"English","publisher":"GeoScienceWorld","doi":"10.1785/gssrl.66.4.44","issn":"08950695","usgsCitation":"Fletcher, J.B., 1995, Source parameters and crustal Q for four earthquakes in South Carolina: Seismological Research Letters, v. 66, no. 4, p. 44-61, https://doi.org/10.1785/gssrl.66.4.44.","productDescription":"18 p.","startPage":"44","endPage":"61","costCenters":[],"links":[{"id":226661,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South 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,{"id":70205368,"text":"70205368 - 1995 - Wind shear stress measurements in a coastal marsh during Hurricane Andrew","interactions":[],"lastModifiedDate":"2019-09-17T08:31:34","indexId":"70205368","displayToPublicDate":"1995-06-30T11:15:51","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"Wind shear stress measurements in a coastal marsh during Hurricane Andrew","docAbstract":"<p><span>Hurricane Andrew produced changes to the Louisiana wetlands not normally observed after lesser, more common storms. For example, the &lt;25 m/s wind speeds generated by cold fronts and winter storms, and any accompanying storm surge, do not cause substantial, wide-spread alteration of marsh vegetation. During Hurricane Andrew, however, the wind, the wind-driven storm surge, or both produced severe, wide-spread wetland alteration, especially in areas that primarily consisted of densely vegetated floating mats. In a few hours, vegetated brackish marsh was severely torn and large areas were converted to open water, a process that takes decades when driven by geologic subsidence, human intervention, and lesser storms. During the passage of Hurricane Andrew, wind measurements were taken inside an impoundment within a brackish part of Louisiana's coastal wetlands system. At its closest point, the site lay 50 km to the right of the north-trending storm track, placing it in or near the zone of maximum wind (the eye wall). As the hurricane approached, the wind blew from the north; after it passed, the wind direction swung around to the southeast. Several hours after the eye passed, the southeasterly wind drove a 1.5-m storm surge through the area, causing the collapse of the meteorology tower. Wind shear stress calculations, based on data from two vertically stacked sensors, showed a direct correlation between wind shear stress and wind speed. The greatest increase in wind shear stress occurred when wind speed exceeded 20 m/s. Overall, wind shear stress increased more than three orders of magnitude — from approximately 0.01 N/m² at a wind speed of 6 m/s through 1 N/m² at 20 m/s to 18 N/m² at the maximum sustained speed of 43 m/s. Drag-coefficient calculations show that the open-ocean CD formulations, such as the popular WAMDI model, cannot be employed for wetland use because it overestimates CD for velocities less than approximately 20 m/s and underestimates it for higher velocities.</span></p>","language":"English","publisher":"Coastal Education and Research Foundation Inc","usgsCitation":"Dingler, J.R., Hsu, S., and Foote, A.L., 1995, Wind shear stress measurements in a coastal marsh during Hurricane Andrew: Journal of Coastal Research, p. 295-305.","productDescription":"11 p.","startPage":"295","endPage":"305","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":367434,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":367447,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/25736016"}],"country":"United States","state":"Louisiana","otherGeospatial":"Jug Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.0081672668457,\n              29.34582065193874\n            ],\n            [\n              -90.90568542480469,\n              29.34582065193874\n            ],\n            [\n              -90.90568542480469,\n              29.397131972809856\n            ],\n            [\n              -91.0081672668457,\n              29.397131972809856\n            ],\n            [\n              -91.0081672668457,\n              29.34582065193874\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dingler, J. R.","contributorId":79043,"corporation":false,"usgs":true,"family":"Dingler","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":770951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hsu, S.A.","contributorId":94161,"corporation":false,"usgs":true,"family":"Hsu","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":770952,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foote, A. Lee","contributorId":216145,"corporation":false,"usgs":false,"family":"Foote","given":"A.","email":"","middleInitial":"Lee","affiliations":[],"preferred":false,"id":770953,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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