Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
An exploratory well, located at 388 feet above sea level in Kipahulu Valley on Maui, Hawaii, was completed and tested in October 1980. The 410-foot well penetrates a series of very dense basaltic lava flows of the Hana Formation. At an elevation of 10 feet above mean sea level, the well penetrated a water-bearing zone of permeable basaltic rock. Water from this zone had a head of about 76 feet above sea level. In October of 1980, the well was pump tested for 9 hours at various discharge rates up to 350 gallons per minute with a maximum drawdown of about 12 feet. Based on the test data, the well should produce water at a rate of 200 gallons per minute with a drawdown of less than 3 feet. The water level in the well was continuously monitored from October 1980 to mid-November 1981, during which period a maximum decline of 20 feet was recorded. Water level fluctuations in the well can be correlated to the flow in nearby Palikea Stream. The long-term water level in the well should stabilize at about 75 feet above sea level. Water quality was excellent. The total dissolved-solids content was 49 milligrams per liter and the chloride content was 4.2 milligrams per liter.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834066","usgsCitation":"Souza, W.R., 1983, Exploratory drilling and aquifer testing at the Kipahulu District, Haleakala National Park, Maui, Hawaii: U.S. Geological Survey Water-Resources Investigations Report 83-4066, v, 26 p., https://doi.org/10.3133/wri834066.","productDescription":"v, 26 p.","costCenters":[],"links":[{"id":58671,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4066/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123551,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4066/report-thumb.jpg"},{"id":411586,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35701.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawaii","otherGeospatial":"Haleakala National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -156.25717163085938,\n 20.580081709180345\n ],\n [\n -156.01547241210938,\n 20.580081709180345\n ],\n [\n -156.01547241210938,\n 20.78693059257028\n ],\n [\n -156.25717163085938,\n 20.78693059257028\n ],\n [\n -156.25717163085938,\n 20.580081709180345\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f78f4","contributors":{"authors":[{"text":"Souza, W. R.","contributorId":102114,"corporation":false,"usgs":true,"family":"Souza","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202254,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30562,"text":"wri824089 - 1983 - Hydrogeology of the Sarasota-Port Charlotte area, Florida","interactions":[],"lastModifiedDate":"2023-01-04T20:59:48.947233","indexId":"wri824089","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4089","title":"Hydrogeology of the Sarasota-Port Charlotte area, Florida","docAbstract":"The surficial and intermediate aquifers are the major source of public water supplies in the Sarasota-Port Charlotte, Florida, area because of the relatively poor quality of Floridan aquifer water. The hydrogeologic framework consists of the surficial aquifer, intermediate aquifers (Tamiami-upper Hawthorn and lower Hawthorn-upper Tampa aquifers) and confining beds, Floridan aquifer, and lower confining bed (or base of the Floridan aquifer). The quality of ground water in the surficial and intermediate aquifers is generally good, except in the western (coastal) and southern parts where saltwater intrusion or incomplete flushing of connate water has occurred. The mineral content of ground water generally increases with depth and areally from the northeast towards the west and south. A water budget for the study area shows that an average annual rainfall of 51.0 inches minus an evapotranspiration of 38.0 inches per year and streamflow of 12.5 inches per year leaves 0.5 inch per year of recharge to the surficial aquifer. Combined pumpage from the aquifers is 1.06 inches per year. A preliminary quasi-time dimensional model has been applied to the study area to check the reasonableness of the hydrogeologic framework defined and of aquifer parameters. The model was considered calibrated when the final head matrix was within plus or minus 5 feet of the starting head.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824089","usgsCitation":"Wolansky, R., 1983, Hydrogeology of the Sarasota-Port Charlotte area, Florida: U.S. Geological Survey Water-Resources Investigations Report 82-4089, vi, 48 p., https://doi.org/10.3133/wri824089.","productDescription":"vi, 48 p.","costCenters":[],"links":[{"id":411383,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35600.htm","linkFileType":{"id":5,"text":"html"}},{"id":59327,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4089/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123470,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4089/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Sarasota-Port Charlotte area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.55,\n 27.383\n ],\n [\n -82.55,\n 26.75\n ],\n [\n -81.667,\n 26.75\n ],\n [\n -81.667,\n 27.383\n ],\n [\n -82.55,\n 27.383\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc39a","contributors":{"authors":[{"text":"Wolansky, R. M.","contributorId":89163,"corporation":false,"usgs":true,"family":"Wolansky","given":"R. M.","affiliations":[],"preferred":false,"id":203459,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28692,"text":"wri834016 - 1983 - Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri834016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4016","title":"Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico","docAbstract":"Geohydrologic data have been collected in the Los Medanos area at the U.S. Department of Energy 's proposed Waste Isolation Pilot Plant (WIPP) site in southeastern New Mexico since 1975 as part of an intensive study evaluating the feasibility of storing defense-associated nuclear wastes within the bedded salt of the Salado Formation of Permian age. Drilling and hydrologic testing have identified three principal water-producing zones above the salt, including the Rustler-Salado Formational contact and the Culebra and Magenta Dolomite Members of the Permian Rustler Formation. Below the bedded salt there is another water-bearing zone, the channel sandstones of the Bell Canyon formation of the Permian Delaware Mountain Group. Most data collected from 33 hydrologic test holes indicate that the water-bearing zones are characterized by low transmissivities and contain slightly saline to briny water. Data collected from drill-stem tests in the Bell Canyon Formation indicate the channel sandstones have hydraulic conductivities ranging from 0.02 to 0.36 feet per day grade vertically and laterally into siltstones and shales of very low permeability. The Rustler Formation contains the principal water-producing zones identified at the WIPP site. The Rustler-Salado formational contact has the least transmissivity, ranging from 0.00003 to 0.003 feet squared per day. The Culebra Dolomite is the most productive unit at the WIPP site with transmissivities ranging from 0.001 to 73 feet squared per day; the greater values result from fracturing in the dolomite created by dissolution of underlying halite. Minute vertical permeabilities prevent movement of water between hydrologic units. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834016","usgsCitation":"Mercer, J.W., 1983, Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 83-4016, viii, 121 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834016.","productDescription":"viii, 121 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4016/report-thumb.jpg"},{"id":57535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4016/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8824","contributors":{"authors":[{"text":"Mercer, Jerry W.","contributorId":32534,"corporation":false,"usgs":true,"family":"Mercer","given":"Jerry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30560,"text":"wri8257 - 1983 - Continuous seismic-reflection survey defining shallow sedimentary layers in the Charlotte Harbor and Venice areas, southwest Florida","interactions":[],"lastModifiedDate":"2019-11-01T11:59:59","indexId":"wri8257","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-57","title":"Continuous seismic-reflection survey defining shallow sedimentary layers in the Charlotte Harbor and Venice areas, southwest Florida","docAbstract":"A continuous marine seismic-reflection survey system was used to define the configuration of shallow sedimentary layers underlying the Charlotte Harbor and Venice areas, southwest Florida. Seismic profiling was conducted over a distance of about 57 miles of Charlotte Harbor, the Peace and Myakka Rivers, and the Intracoastal Waterway near Venice using a high resolution energy source capable of penetrating 200 feet of sediments with a resolution of 1 to 3 feet. Five stratigraphic units defined from the seismic records includes sediments to Holocene to early Miocene age. All seismic-profile records are presented, along with geologic sections constructed from the records. Seismic reflection amplitude, frequency, continuity, configuration, external form, and areal association were utilized to interpret facies and depositional environments of the stratigraphic units. The despositional framework of the units ranges from shallow shelf to prograded slope. The stratigraphic units are correlated with the surficial aquifer and intermediate artesian aquifers, and permeable zones of the aquifers are related to the seismic records. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8257","usgsCitation":"Wolansky, R., Haeni, F., and Sylvester, R., 1983, Continuous seismic-reflection survey defining shallow sedimentary layers in the Charlotte Harbor and Venice areas, southwest Florida: U.S. Geological Survey Water-Resources Investigations Report 82-57, v, 77 p. , https://doi.org/10.3133/wri8257.","productDescription":"v, 77 p. ","costCenters":[],"links":[{"id":160634,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0057/report-thumb.jpg"},{"id":368888,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","city":"Venice","otherGeospatial":"Charlotte Harbor","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.4908447265625,\n 26.75051574561839\n ],\n [\n -81.92779541015624,\n 26.75051574561839\n ],\n [\n -81.92779541015624,\n 27.088473156555896\n ],\n [\n -82.4908447265625,\n 27.088473156555896\n ],\n [\n -82.4908447265625,\n 26.75051574561839\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691b5b","contributors":{"authors":[{"text":"Wolansky, R. M.","contributorId":89163,"corporation":false,"usgs":true,"family":"Wolansky","given":"R. M.","affiliations":[],"preferred":false,"id":203456,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":203455,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sylvester, R.E.","contributorId":97951,"corporation":false,"usgs":true,"family":"Sylvester","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":203457,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30424,"text":"wri834098 - 1983 - Reconnaissance of the geohydrology of the Moab-Monticello area, western Paradox basin, Grand and San Juan Counties, Utah","interactions":[],"lastModifiedDate":"2022-12-15T21:30:07.603261","indexId":"wri834098","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4098","title":"Reconnaissance of the geohydrology of the Moab-Monticello area, western Paradox basin, Grand and San Juan Counties, Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834098","usgsCitation":"Weir, J.E., Maxfield, E., and Hart, I.M., 1983, Reconnaissance of the geohydrology of the Moab-Monticello area, western Paradox basin, Grand and San Juan Counties, Utah: U.S. Geological Survey Water-Resources Investigations Report 83-4098, Report: vii, 59 p.; 3 Plates: 23.69 × 25.03 inches or smaller, https://doi.org/10.3133/wri834098.","productDescription":"Report: vii, 59 p.; 3 Plates: 23.69 × 25.03 inches or smaller","costCenters":[],"links":[{"id":410582,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35723.htm","linkFileType":{"id":5,"text":"html"}},{"id":59195,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4098/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59193,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4098/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59194,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4098/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59192,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4098/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4098/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Grand County, San Juan County","otherGeospatial":"Moab-Monticello area, western Paradox basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.044,\n 38.808\n ],\n [\n -110.043,\n 38.808\n ],\n [\n -110.043,\n 37.82\n ],\n [\n -109.044,\n 37.82\n ],\n [\n -109.044,\n 38.808\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63af9f","contributors":{"authors":[{"text":"Weir, J. E. Jr.","contributorId":102476,"corporation":false,"usgs":true,"family":"Weir","given":"J.","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":203226,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maxfield, E. B.","contributorId":83967,"corporation":false,"usgs":true,"family":"Maxfield","given":"E. B.","affiliations":[],"preferred":false,"id":203225,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hart, I. M.","contributorId":24806,"corporation":false,"usgs":true,"family":"Hart","given":"I.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":203224,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30425,"text":"wri834217 - 1983 - Regional hydrology of the Dolores River basin, eastern Paradox Basin, Colorado and Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri834217","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4217","title":"Regional hydrology of the Dolores River basin, eastern Paradox Basin, Colorado and Utah","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nOpen-File Service Section [distributor],","doi":"10.3133/wri834217","usgsCitation":"Weir, J.E., Maxfield, E.B., and Zimmerman, E.A., 1983, Regional hydrology of the Dolores River basin, eastern Paradox Basin, Colorado and Utah: U.S. Geological Survey Water-Resources Investigations Report 83-4217, vii, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834217.","productDescription":"vii, 53 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4217/report-thumb.jpg"},{"id":59196,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4217/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59197,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4217/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59198,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4217/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59199,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4217/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634ec2","contributors":{"authors":[{"text":"Weir, James E. Jr.","contributorId":47419,"corporation":false,"usgs":true,"family":"Weir","given":"James","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":203228,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maxfield, E. Blair","contributorId":91538,"corporation":false,"usgs":true,"family":"Maxfield","given":"E.","email":"","middleInitial":"Blair","affiliations":[],"preferred":false,"id":203229,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zimmerman, Everett Alfred","contributorId":18729,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Everett","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":203227,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28683,"text":"wri834028 - 1983 - Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri834028","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4028","title":"Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834028","usgsCitation":"Meisler, H., 1983, Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 83-4028, 76 p. :maps ;28 cm., https://doi.org/10.3133/wri834028.","productDescription":"76 p. :maps ;28 cm.","costCenters":[],"links":[{"id":121639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4028/report-thumb.jpg"},{"id":57523,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4028/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57524,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4028/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7662","contributors":{"authors":[{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":200226,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28674,"text":"wri824124 - 1983 - Water quality of Somerville Lake, south-central Texas","interactions":[],"lastModifiedDate":"2016-08-09T13:24:36","indexId":"wri824124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4124","title":"Water quality of Somerville Lake, south-central Texas","docAbstract":"Somerville Lake in south-central Texas is a shallow lake, with a mean depth of 14 feet. The maximum depth of the submerged channel of Yegua Creek is usually less than 35 feet and in most areas of the lake the depth is less than 10 feet.
\nSeveral factors including thermal circulation resulting from the cooling of surface water, wind action, and the large inflow volume in realtion to the lake volume combine to keep the lake well mixed throughout the year. The oxygen concentrations remain high areally and at depth because of good circulation of lake waters during most of the year. Even in summer most bottom oxygen concentrations were in excess of 50 percent of saturation.
\nDue to year-round high percent oxygen saturation from surface to bottom in most parts of the lake, caused by the frequent periods of circulation that occur during all seasons, concentrations of dissolved iron, and manganese reamin low. Dissovled iron concentrations were less than 50 micrograms per liter and dissolved manganese concentrations were less than 40 micrograms per liter. The total inorganic nitrogen concentrations varied little throughout the lake. During the summer, concentrations were 0.01 milligram per liter at the surface to 0.02 milligram per liter at the bottom; and during the winter 0.11 milligram per liter at the surface and 0.10 milligram per liter at the bottom. Concentrations in the headwaters were about double those in the lake. Surface and bottom total phosphorus concentrations, during summer and winter averaged about the same, 0.04 and 0.06 milligram per liter throughout the lake, except in the headwaters where the concentrations were about double those in the lake.
\nHomogeneous or near homogeneous concentrations of total phosphorus and inorganic nitrogen can occur at any time of the year throughout the lake. Total phosphorus concentrations did not increase during the year or during the study period. On the other hand total inorganic nitrogen concentrations did show an annual cycle and were highest in the spring and lowest in late summer or fall. During periods of large releases of water, the more soluble total inorganic nitrogen was flushed from the lake.
\nThe concentration of dissolved solids ranged from 139 to 292 milligrams per liter and averaged about 220 milligrams per liter. Dissolved chloride concentrations ranged from 20 to 68 milligrams per liter and averaged 43 milligrams per liter. Dissolved sulfate concentrations ranged from 30 to 130 milligrams per liter and averaged 63 milligrams per liter. The total hardness of the water ranged from 75 to 140 milligrams per liter, expressed as calcium carbonate, placing it in the moderately hard to hard (61 to 180 milligrams per liter) classification. The concentrations of principal dissolved constituents indicate that Somerville Lake is an excellent source of water for municipal, industrial, or agricultural use.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri824124","usgsCitation":"McPherson, E., and Mendieta, H., 1983, Water quality of Somerville Lake, south-central Texas: U.S. Geological Survey Water-Resources Investigations Report 82-4124, vi, 88 p., https://doi.org/10.3133/wri824124.","productDescription":"vi, 88 p.","numberOfPages":"94","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":57509,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4124/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158278,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4124/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f919","contributors":{"authors":[{"text":"McPherson, Emma","contributorId":85629,"corporation":false,"usgs":true,"family":"McPherson","given":"Emma","email":"","affiliations":[],"preferred":false,"id":200213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mendieta, H.B.","contributorId":38965,"corporation":false,"usgs":true,"family":"Mendieta","given":"H.B.","email":"","affiliations":[],"preferred":false,"id":200212,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28991,"text":"wri834000 - 1983 - Geology of the Tulare Formation and other continental deposits, Kettleman City area, San Joaquin Valley, California, with a section on ground-water management considerations and use of texture maps","interactions":[],"lastModifiedDate":"2023-01-09T21:31:47.454289","indexId":"wri834000","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4000","title":"Geology of the Tulare Formation and other continental deposits, Kettleman City area, San Joaquin Valley, California, with a section on ground-water management considerations and use of texture maps","docAbstract":"The Tulare Formation and other continental deposits of Pliocene to Holocene age crop out over most of the area near Kettleman City in the San Joaquin Valley of California. The deposits range in thickness from 0 to more than 4,000 feet and overlie the upper Mya zone of the San Joaquin Formation of Pliocene age. Some features of their base reflect structural deformation during Quaternary time. Many freshwater fossils occur in the Tulare Formation itself, including the largest fossil assemblage of clams and snails known on the Pacific Coast. Sediments in the Tulare Formation and other continental deposits consist mainly of unconsolidated deposits of clay, silt, sand, and gravel. Texture maps of the Tulare Formation and other continental deposits show the distribution, both laterally and vertically, of the coarse- and fine-grained sediment in the area. Such maps can be used by water managers for selecting areas for recharge and discharge operations and by ground-water modelers for assigning relative values of hydraulic conductivity and storage coefficient.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834000","usgsCitation":"Page, R.W., 1983, Geology of the Tulare Formation and other continental deposits, Kettleman City area, San Joaquin Valley, California, with a section on ground-water management considerations and use of texture maps: U.S. Geological Survey Water-Resources Investigations Report 83-4000, Report: iv, 24 p.; 2 Plates: 21.67 x 24.81 inches and 18.84 x 19.65 inches, https://doi.org/10.3133/wri834000.","productDescription":"Report: iv, 24 p.; 2 Plates: 21.67 x 24.81 inches and 18.84 x 19.65 inches","costCenters":[],"links":[{"id":411591,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35648.htm","linkFileType":{"id":5,"text":"html"}},{"id":57860,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4000/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57859,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4000/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57858,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4000/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118805,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4000/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Kettleman City area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.098,\n 36.158\n ],\n [\n -119.25,\n 36.158\n ],\n [\n -119.25,\n 35.5\n ],\n [\n -120.098,\n 35.5\n ],\n [\n -120.098,\n 36.158\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e40f","contributors":{"authors":[{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30442,"text":"wri834172 - 1983 - Statistical summary of daily values data and trend analysis of dissolved-solids data at National Stream Quality Accounting Network (NASQAN) stations","interactions":[],"lastModifiedDate":"2016-08-09T13:58:46","indexId":"wri834172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4172","title":"Statistical summary of daily values data and trend analysis of dissolved-solids data at National Stream Quality Accounting Network (NASQAN) stations","docAbstract":"A statistical summary is provided of the available continuous and once-daily discharge, specific-conductance, dissolved oxygen , water temperature, and pH data collected at NASQAN stations during the 1973-81 water years and documents the period of record on which the statistical calculations were based. In addition, dissolved-solids data are examined by regression analyses to determine the relation between dissolved solids and specific conductance and to determine if long-term trends can be detected in dissolved-solids concentrations. Statistical summaries, regression equations expressing the relation between dissolved solids and specific conductance, and graphical presentations of trend analyses of dissolved solids are presented for 515 NASQAN stations in the United States, Canada, Guam, and Puerto Rico.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834172","usgsCitation":"Wells, F., and Schertz, T., 1983, Statistical summary of daily values data and trend analysis of dissolved-solids data at National Stream Quality Accounting Network (NASQAN) stations: U.S. Geological Survey Water-Resources Investigations Report 83-4172, xx, 526 p., https://doi.org/10.3133/wri834172.","productDescription":"xx, 526 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":59223,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4172/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4172/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dce4b07f02db5e13f1","contributors":{"authors":[{"text":"Wells, F.C.","contributorId":25158,"corporation":false,"usgs":true,"family":"Wells","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":203260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schertz, T. L.","contributorId":65841,"corporation":false,"usgs":true,"family":"Schertz","given":"T. L.","affiliations":[],"preferred":false,"id":203261,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30443,"text":"wri834124 - 1983 - Geologic and well-construction data for the H-10 borehole complex near the proposed Waste Isolation Pilot Plant site, southeastern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"wri834124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4124","title":"Geologic and well-construction data for the H-10 borehole complex near the proposed Waste Isolation Pilot Plant site, southeastern New Mexico","docAbstract":"The H-10 borehole complex, a group of three closely spaced boreholes, is located 3 1/2 miles southeast of the proposed Waste Isolation Pilot Plant site in west-central Lea County, New Mexico. The geological data presented in this report are part of a site-characterization study for the possible storage of defense-associated radioactive wastes within salt beds of the Salado Formation of Permian age. Each borehole was designated to penetrate a distinct water-bearing zone: H-10a (total depth 1 ,318 feet) was completed just below the Magenta Dolomite Member of the Rustler Formation of Permian age; H-10b (total depth 1 ,398 feet) was completed just below the Culebra Dolomite Member of the Rustler Formation; and H-10c (total depth 1,538 feet) was completed below the Rustler Formation-Salado Formation contact. The geologic units penetrated in borehole H-10c are surficial alluvium and eolian sand of Holocene age (0-5 feet); the Mescalero caliche (5-9 feet) and the Gatuna Formation (9-90 feet) of Pleistocene age; formation in the Dockum Group (Chinle Formation, 90-482 feet and Santa Rosa Sandstone, 482-658 feet) of Late Triassic age; and the Dewey Lake Red Beds (658-1,204 feet), the Rustler Formation (1,204-1,501 feet), and part of the Salado Formation (1,501-1,538 feet), all of Permian age. The sections of the Rustler and Salado Formations penetrated by borehole H-10c are complete and contain little or no evidence of dissolution of halite and associated rocks, indicating that the eastward-moving dissolution on top of the Salado, found just to the west of the WIPP site, has not reached the H-10 site. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834124","usgsCitation":"Wells, J., and Drellack, S., 1983, Geologic and well-construction data for the H-10 borehole complex near the proposed Waste Isolation Pilot Plant site, southeastern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 83-4124, iv, 38 p. :ill., map ;28 cm., https://doi.org/10.3133/wri834124.","productDescription":"iv, 38 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":126882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4124/report-thumb.jpg"},{"id":59224,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4124/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4124/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4eec","contributors":{"authors":[{"text":"Wells, J.G.","contributorId":85198,"corporation":false,"usgs":true,"family":"Wells","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":203263,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drellack, S.L.","contributorId":19973,"corporation":false,"usgs":true,"family":"Drellack","given":"S.L.","affiliations":[],"preferred":false,"id":203262,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29005,"text":"wri834020 - 1983 - Initial assessment of time of travel and mixing through Gulf Island Pond and the lower Androscoggin River, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri834020","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4020","title":"Initial assessment of time of travel and mixing through Gulf Island Pond and the lower Androscoggin River, Maine","docAbstract":"Flow-stratification patterns were observed in Gulf Island Pond during time-of-travel studies in May and August 1980. The stratification patterns in this 70 million cubic-meter impoundment were due to a temperature differences between inflowing water and reservoir water. Separation was observed at temperature differences of 0.5 degrees C in May 1980 and 1.0 degrees C in August 1980. The pathway taken by inflowing water through the reservoir was governed by the temperature-related density forces acting between the two water masses. Data collected during August 1980 to define differences in dye concentrations with depth at two fixed profile points in Gulf Island Pond showed average water velocity to be seven times faster near the bottom than near the surface. A concept of mass flow was used to analyze data collected at sites downstream from Gulf Island Dam where flow varied rapidly with time. This report presents the mathematical derivation of controid traveltime, skewness, and percentage recovery of dye mass as determined from mass versus time curves. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834020","usgsCitation":"Parker, G., and Hunt, G., 1983, Initial assessment of time of travel and mixing through Gulf Island Pond and the lower Androscoggin River, Maine: U.S. Geological Survey Water-Resources Investigations Report 83-4020, vii, 60 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834020.","productDescription":"vii, 60 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4020/report-thumb.jpg"},{"id":57872,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4020/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49c1e4b07f02db5d33cb","contributors":{"authors":[{"text":"Parker, G.W.","contributorId":100374,"corporation":false,"usgs":true,"family":"Parker","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":200775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunt, G.S.","contributorId":20360,"corporation":false,"usgs":true,"family":"Hunt","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":200774,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29011,"text":"wri834084 - 1983 - Simulated effects of anticipated coal mining on dissolved solids in selected tributaries of the Yampa River, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri834084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4084","title":"Simulated effects of anticipated coal mining on dissolved solids in selected tributaries of the Yampa River, northwestern Colorado","docAbstract":"Identifying cumulative effects of coal mining on dissolved solids downstream from multipe coal-mining operations is particularly important in western basins. The problem of identifying cumulative effects is evident in the Trout Creek drainage, a tributary to the Yampa River in northwestern Colorado, where a number of mines are active and mine expansions are planned. As an evaluation tool, a model was developed and calibrated for the Trout Creek drainage and a reach of the Yampa River main stem. This model uses a series of nodes on the stream network to sum water quantity and quality through the network. The model operates on a monthly basis and uses data from water years 1976 to 1981. Output is mean monthly discharge, dissolved-solids concentration, and dissolved-solids load. Observed data are needed to initiate the model and for model calibration. Some data were extrapolated from records of nearby streamflow-gaging stations. Some nodes within the stream network were for inputs from anticipated mining and were inactive during calibrations. After calibration, these nodes were used to input water discharge at a given dissolved-solids concentration to reflect various future mine configurations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834084","usgsCitation":"Parker, R.S., and Norris, J.M., 1983, Simulated effects of anticipated coal mining on dissolved solids in selected tributaries of the Yampa River, northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 83-4084, vi, 72 p. :ill., map ;28 cm., https://doi.org/10.3133/wri834084.","productDescription":"vi, 72 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":159492,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4084/report-thumb.jpg"},{"id":57877,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4084/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64953e","contributors":{"authors":[{"text":"Parker, R. S.","contributorId":104510,"corporation":false,"usgs":true,"family":"Parker","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":200784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norris, J. M.","contributorId":87953,"corporation":false,"usgs":true,"family":"Norris","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":200783,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29151,"text":"wri834052 - 1983 - Ground water in the Redding Basin, Shasta and Tehama counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:45","indexId":"wri834052","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4052","title":"Ground water in the Redding Basin, Shasta and Tehama counties, California","docAbstract":"An appraisal of ground-water conditions in the Redding Basin was made by the U.S. Geological Survey and the California Department of Water Resources during 1979 and 1980. The basin covers about 510 square miles in the northern part of the Central Valley of California. Ground water in the basin is obtained principally from wells tapping continental deposits of Tertiary and/or Quaternary age. These deposits are arranged in a synclinal structure that trends and plunges southward. Recharge to the basin is from subsurface inflow; infiltration of precipitation and excess irrigation water; and percolation of certain reaches of streams and creeks. Ground-water movement is generally from the periphery of the basin towards the Sacramento River. Hydrographs for the period 1956 to 1970 show only a slight water-level decline and virtually no change between 1970 and 1979. The total estimated pumpage for 1976 was 82,000 acre-feet. Estimated usable storage capacity for the basin is about 5.5 million acre-feet. Chemical quality of ground water is rated good to excellent. Water type is a magnesium-calcium bicarbonate in character. The underlying Chico Formation contains saline marine water which is of poor quality. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834052","usgsCitation":"Pierce, M., 1983, Ground water in the Redding Basin, Shasta and Tehama counties, California: U.S. Geological Survey Water-Resources Investigations Report 83-4052, iv, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834052.","productDescription":"iv, 41 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4052/report-thumb.jpg"},{"id":58025,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d549","contributors":{"authors":[{"text":"Pierce, M.J.","contributorId":8893,"corporation":false,"usgs":true,"family":"Pierce","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":201030,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30470,"text":"wri834233 - 1983 - Problems of rising ground-water levels in urban areas with special reference to the Louisville, Kentucky area","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri834233","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4233","title":"Problems of rising ground-water levels in urban areas with special reference to the Louisville, Kentucky area","docAbstract":"Rising ground-water levels are a problem for cities such as San Bernadino, California; Greely and Fort Collins, Colorado; New York City boroughs of Brooklyn and Queens; and Louisville, Kentucky. Ground-water levels showed a steeply rising trend in the alluvial aquifer underlying Louisville during the early and middle 1970 's in response to above average precipitation and a decrease in ground-water withdrawals. This rising trend flattened in 1979 and the water levels are stabilizing at 25 to 45 feet below land surface in the downtown area. Basements are generally 20 to 25 feet below land surface and some utility lines are as much as 40 feet below land surface in this area. Because of the shallow depth to water, any resumption of the upward trend would require preventive measures such as selective dewatering to avoid damage to some structures. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834233","usgsCitation":"Whitesides, D.V., Faust, R., and Zettwoch, D., 1983, Problems of rising ground-water levels in urban areas with special reference to the Louisville, Kentucky area: U.S. Geological Survey Water-Resources Investigations Report 83-4233, v, 31 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834233.","productDescription":"v, 31 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4233/report-thumb.jpg"},{"id":59253,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4233/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62594f","contributors":{"authors":[{"text":"Whitesides, D. V.","contributorId":34553,"corporation":false,"usgs":true,"family":"Whitesides","given":"D.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":203304,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faust, R.J.","contributorId":80700,"corporation":false,"usgs":true,"family":"Faust","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":203306,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zettwoch, D.D.","contributorId":44950,"corporation":false,"usgs":true,"family":"Zettwoch","given":"D.D.","affiliations":[],"preferred":false,"id":203305,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":29019,"text":"wri834173 - 1983 - Trace metals in surface water and stream sediments of Healy and Lignite Creek basins, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri834173","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4173","title":"Trace metals in surface water and stream sediments of Healy and Lignite Creek basins, Alaska","docAbstract":"Water quality and streamflow in the Russian River basin during low-flow seasons (May to October), were studied for water years 1973-78 to document water-quality and streamflow conditions in the basin, and to determine the extent and cause of any water-quality impairment. The most important factors affecting surface-water quality and streamflow during the period of the study were wastewater discharges, their abatement beginning in 1975, and the drought during 1976 and 1977. Substantial decreases in fecal-coliform bacteria and nutrients occurred from 1975 through 1978, corresponding to regulations specifying no discharge of wastewater during the lowflow season. Generally, turbidity and nutrients were least during the 1977 lowflow season. However, specific conductance increased markedly during 1976 and 1977 in response to substantially decreased streamflow during the drought. Algal growth in the Russian River depends on the amount of nitrogen in the water and is not limited by the amount of phosphorus in the water. Cold water releases from Lake Mendocino seem to be important for maintaining downstream water temperatures at acceptable levels for survival of certain aquatic organisms, retarding aquatic community respiration, and preventing nuisance growths of photoplankton and periphyton. During August 1977, a diel study showed the Russian River was a heterotrophic system where photosynthetic production of oxygen was not sufficient to offset respiration. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834173","usgsCitation":"Parks, B., 1983, Trace metals in surface water and stream sediments of Healy and Lignite Creek basins, Alaska: U.S. Geological Survey Water-Resources Investigations Report 83-4173, iv, 30 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834173.","productDescription":"iv, 30 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4173/report-thumb.jpg"},{"id":57884,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4173/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f065f","contributors":{"authors":[{"text":"Parks, Bruce","contributorId":87542,"corporation":false,"usgs":true,"family":"Parks","given":"Bruce","email":"","affiliations":[],"preferred":false,"id":200800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29093,"text":"wri834219 - 1983 - Hydrogeology of parts of the Central Platte and Lower Loup Natural Resources Districts, Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri834219","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4219","title":"Hydrogeology of parts of the Central Platte and Lower Loup Natural Resources Districts, Nebraska","docAbstract":"Water-level declines of at least 15 feet have occurred in this heavily irrigated area of central Nebraska since the 1930's, and potential for additonal declines is high. To test the effects of additional irrigation development on water levels and streamflow , computer programs were developed that represent the surface-water system, soil zone, and saturated zone. A two-dimensional, finite-difference ground-water flow model of the 3,374 square-mile study area was developed and calibrated using steady-state and transient conditions. Three management alternatives were examined. First, 125,000 acre-feet of water would be diverted annually from the Platte River. During a water year in which flows are similar to those in 1957, months of zero streamflow at Grand Island increased from the historical 2, to 7. After 5 years of such low flows, in 36 nodes (997.4 acres per node) water levels declined more than 5 feet, with a maximum decline of 10.7 feet. A second alternative would allow no new ground-water development after 1980. The third alternative would allow irrigable but unirrigated land to be developed at an annual rate of 2, 5, and 8 percent and to apply irrigation water at 80, 100, and 120 percent of consumptive irrigation requirements. The maximum projected declines by 2020 are 119 and 139 feet, respectively, for the second and third alternatives. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834219","usgsCitation":"Peckenpaugh, J.M., and Dugan, J.T., 1983, Hydrogeology of parts of the Central Platte and Lower Loup Natural Resources Districts, Nebraska: U.S. Geological Survey Water-Resources Investigations Report 83-4219, 100 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834219.","productDescription":"100 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123624,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4219/report-thumb.jpg"},{"id":57945,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4219/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57946,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4219/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57947,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4219/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57948,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4219/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db625128","contributors":{"authors":[{"text":"Peckenpaugh, J. M.","contributorId":69559,"corporation":false,"usgs":true,"family":"Peckenpaugh","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":200940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dugan, J. T.","contributorId":67890,"corporation":false,"usgs":true,"family":"Dugan","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":200939,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29092,"text":"wri834090 - 1983 - Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey; 1981 annual report","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri834090","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4090","title":"Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey; 1981 annual report","docAbstract":"The U.S. Geological Survey maintains a quality-assurance program based on the analysis of reference samples for its two water-analysis laboratories located in Atlanta, Georgia and Denver, Colorado. Reference containing inorganic constituents are prepared at the U.S. Geological Survey 's Ocala, Florida, office and disguised as routine samples, and sent daily to each laboratory through other U.S. Geological Survey offices. The results are permanently stored in the National Water Data Storage and Retrieval System (WATSTORE), the U.S. Geological Survey 's data base for all water data. These data are analyzed statistically for precision and bias. The results of these statistical analyses are presented for data collected during the 1981 calendar year. In addition, one sample containing known concentrations of trihalomethanes and samples containing unknown concentrations of chlorophyll a were analyzed in both laboratories, and these results also are presented. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834090","usgsCitation":"Peart, D., and Thomas, N., 1983, Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey; 1981 annual report: U.S. Geological Survey Water-Resources Investigations Report 83-4090, viii, 120 p. :ill. ;28 cm., https://doi.org/10.3133/wri834090.","productDescription":"viii, 120 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":158928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4090/report-thumb.jpg"},{"id":57944,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4090/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db651417","contributors":{"authors":[{"text":"Peart, D.B.","contributorId":45304,"corporation":false,"usgs":true,"family":"Peart","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":200938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Nancy","contributorId":7657,"corporation":false,"usgs":true,"family":"Thomas","given":"Nancy","affiliations":[],"preferred":false,"id":200937,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":43362,"text":"ofr83111 - 1983 - Land use and land cover and associated maps for Lovelock, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:09","indexId":"ofr83111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-111","title":"Land use and land cover and associated maps for Lovelock, Nevada","language":"ENGLISH","doi":"10.3133/ofr83111","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use and land cover and associated maps for Lovelock, Nevada: U.S. Geological Survey Open-File Report 83-111, maps :photocopy ;44 x 68 cm., https://doi.org/10.3133/ofr83111.","productDescription":"maps :photocopy ;44 x 68 cm.","costCenters":[],"links":[{"id":162516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0e64","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531138,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43324,"text":"ofr83564 - 1983 - Land use series, Lund [quadrangle], Nevada-Utah","interactions":[],"lastModifiedDate":"2016-05-17T11:53:02","indexId":"ofr83564","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-564","title":"Land use series, Lund [quadrangle], Nevada-Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83564","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use series, Lund [quadrangle], Nevada-Utah: U.S. Geological Survey Open-File Report 83-564, 3 Sheets: 35.60 x 22.93 inches or smaller, https://doi.org/10.3133/ofr83564.","productDescription":"3 Sheets: 35.60 x 22.93 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":134537,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr83564.PNG"},{"id":321265,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0564/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":321266,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0564/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":321264,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0564/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada, Utah","otherGeospatial":"Lund Quadrangle","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae001","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531111,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43760,"text":"ofr83551 - 1983 - Land use and land cover and associated maps for Eau Claire, Wisconsin; Minnesota","interactions":[],"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr83551","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-551","title":"Land use and land cover and associated maps for Eau Claire, Wisconsin; Minnesota","language":"ENGLISH","doi":"10.3133/ofr83551","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use and land cover and associated maps for Eau Claire, Wisconsin; Minnesota: U.S. Geological Survey Open-File Report 83-551, maps :photocopy ;45 x 65 cm., https://doi.org/10.3133/ofr83551.","productDescription":"maps :photocopy ;45 x 65 cm.","costCenters":[],"links":[{"id":161994,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1452","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531348,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43087,"text":"ofr83106 - 1983 - Land use and land cover and associated maps for Prescott, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr83106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-106","title":"Land use and land cover and associated maps for Prescott, Arizona","language":"ENGLISH","doi":"10.3133/ofr83106","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use and land cover and associated maps for Prescott, Arizona: U.S. Geological Survey Open-File Report 83-106, maps :photocopy ;45 x 67 cm., https://doi.org/10.3133/ofr83106.","productDescription":"maps :photocopy ;45 x 67 cm.","costCenters":[],"links":[{"id":135548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af635","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48747,"text":"ofr811056B - 1983 - Summary of available data on surface water, State of Hawaii - Volume 3: Station location maps for the Islands of Oahu, Molokai, Maui and Hawaii","interactions":[],"lastModifiedDate":"2022-06-27T18:53:00.308537","indexId":"ofr811056B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"81-1056","chapter":"B","title":"Summary of available data on surface water, State of Hawaii - Volume 3: Station location maps for the Islands of Oahu, Molokai, Maui and Hawaii","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811056B","collaboration":"Prepared in cooperation with the Hawaii State Department of Land and Natural Resources, Division of Water and Land Development","usgsCitation":"Matsuoka, I., 1983, Summary of available data on surface water, State of Hawaii - Volume 3: Station location maps for the Islands of Oahu, Molokai, Maui and Hawaii: U.S. Geological Survey Open-File Report 81-1056, 12 Plates: 39.00 × 24.00 inches, https://doi.org/10.3133/ofr811056B.","productDescription":"12 Plates: 39.00 × 24.00 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":161889,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20258,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20257,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20256,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20251,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20250,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20249,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20248,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20259,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-12-preview.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20255,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20254,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20253,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20252,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20247,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1056b/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402543,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11876.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawaii","otherGeospatial":"Hawaii, Maui, Molokai, Oahu","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -155.63232421875,\n 18.812717856407776\n ],\n [\n -154.698486328125,\n 19.497664168139053\n ],\n [\n -155.753173828125,\n 20.365227537412434\n ],\n [\n -155.98388671875,\n 20.879342971957897\n ],\n [\n -156.763916015625,\n 21.320080964008206\n ],\n [\n -157.379150390625,\n 21.320080964008206\n ],\n [\n -158.00537109375,\n 21.80030805097259\n ],\n [\n -158.389892578125,\n 21.58593511478851\n ],\n [\n -158.016357421875,\n 21.15623836610943\n ],\n [\n -157.21435546875,\n 20.992214250886114\n ],\n [\n -156.73095703125,\n 20.992214250886114\n ],\n [\n -156.6650390625,\n 20.73556590521864\n ],\n [\n -156.42333984375,\n 20.540221355754728\n ],\n [\n -155.928955078125,\n 20.107523268824004\n ],\n [\n -156.148681640625,\n 19.766703551716976\n ],\n [\n -156.016845703125,\n 19.01019029439606\n ],\n [\n -155.63232421875,\n 18.812717856407776\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69954e","contributors":{"authors":[{"text":"Matsuoka, Iwao","contributorId":34966,"corporation":false,"usgs":true,"family":"Matsuoka","given":"Iwao","email":"","affiliations":[],"preferred":false,"id":238149,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43299,"text":"ofr83565 - 1983 - Land use series, Aztec [quadrangle], New Mexico-Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr83565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-565","title":"Land use series, Aztec [quadrangle], New Mexico-Colorado","language":"ENGLISH","doi":"10.3133/ofr83565","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use series, Aztec [quadrangle], New Mexico-Colorado: U.S. Geological Survey Open-File Report 83-565, maps :photocopy ;45 x 73 cm., on sheets 77 x 107 cm., https://doi.org/10.3133/ofr83565.","productDescription":"maps :photocopy ;45 x 73 cm., on sheets 77 x 107 cm.","costCenters":[],"links":[{"id":161607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a109","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531103,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}