Mixing models and evaluation of SiO2 contents of warm-water manifestations in the Jordan—Dead Sea Rift Valley indicate that these waters are fed by aquifers with estimated temperatures of up to 68°C. These calculations and Na/K ratios, concentrations of Na, K and Ca, concentrations of atmospheric Ne, Ar, Kr and Xe; and concentrations of the stable hydrogen and oxygen isotopes all indicate below-boiling temperatures.
\nNo indications are available for the existence of above-boiling geothermal systems in the Jordan Rift Valley. Slightly higher than observed temperatures are concluded for a deep component at the springs of Hammat Gader (67°C), Gofra (68°C), the Russian Garden (40°C), and the Yesha well (53–65°C). These temperatures may encourage further developments for spas and bathing installations and, to a limited extent, for space heating, but are not favorable for geothermal power generation.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(80)90002-5","issn":"00221694","usgsCitation":"Mazor, E., Levitte, D., Truesdell, A., Healy, J., and Nissenbaum, A., 1980, Mixing models and ionic geothermometers applied to warm (up to 60°C) springs: Jordan Rift Valley, Israel: Journal of Hydrology, v. 45, no. 1-2, p. 1-19, https://doi.org/10.1016/0022-1694(80)90002-5.","productDescription":"19 p.","startPage":"1","endPage":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":222350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5b86e4b0c8380cd6f5fb","contributors":{"authors":[{"text":"Mazor, E.","contributorId":18104,"corporation":false,"usgs":true,"family":"Mazor","given":"E.","email":"","affiliations":[],"preferred":false,"id":363416,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Levitte, D.","contributorId":102630,"corporation":false,"usgs":true,"family":"Levitte","given":"D.","email":"","affiliations":[],"preferred":false,"id":363419,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address: TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":363417,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Healy, J.","contributorId":80822,"corporation":false,"usgs":true,"family":"Healy","given":"J.","affiliations":[],"preferred":false,"id":363418,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nissenbaum, A.","contributorId":103008,"corporation":false,"usgs":true,"family":"Nissenbaum","given":"A.","email":"","affiliations":[],"preferred":false,"id":363420,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70012317,"text":"70012317 - 1980 - Water resources of the People's Republic of China","interactions":[],"lastModifiedDate":"2023-12-19T00:37:28.23101","indexId":"70012317","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Water resources of the People's Republic of China","docAbstract":"At the invitation of the Society of Hydraulic Engineers of the People's Republic of China (PRC), a delegation of U.S. hydrologists and hydraulic engineers visited the PRC in the fall of 1978.* From discussions with officials of both the Society and the Ministry of Water Conservancy and Power (MWCP), and from visits to research and academic institutions and water projects, the delegation gained a general understanding of the country's surface water resources. The reported statistics, supplemented with others from published sources, provide a quantitative description of the PRC's water resources in relation to those of the United States.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/EO061i046p00891","issn":"00963941","usgsCitation":"Matalas, N., and Nordin, C., 1980, Water resources of the People's Republic of China: Eos, Transactions, American Geophysical Union, v. 61, no. 46, p. 891-901, https://doi.org/10.1029/EO061i046p00891.","productDescription":"11 p.","startPage":"891","endPage":"901","numberOfPages":"11","costCenters":[],"links":[{"id":222005,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"China","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[110.33919,18.6784],[109.47521,18.1977],[108.65521,18.50768],[108.62622,19.36789],[109.11906,19.82104],[110.2116,20.10125],[110.78655,20.07753],[111.01005,19.69593],[110.57065,19.25588],[110.33919,18.6784]]],[[[127.65741,49.76027],[129.39782,49.4406],[130.58229,48.72969],[130.98728,47.79013],[132.50667,47.78897],[133.3736,48.18344],[135.02631,48.47823],[134.50081,47.57844],[134.11236,47.21247],[133.76964,46.11693],[133.09713,45.14407],[131.88345,45.32116],[131.02521,44.96795],[131.28856,44.11152],[131.14469,42.92999],[130.63387,42.90301],[130.64002,42.39501],[129.99427,42.98539],[129.59667,42.42498],[128.05222,41.99428],[128.20843,41.46677],[127.34378,41.50315],[126.86908,41.81657],[126.18205,41.10734],[125.07994,40.56982],[124.26562,39.92849],[122.86757,39.63779],[122.13139,39.17045],[121.05455,38.89747],[121.58599,39.36085],[121.37676,39.75026],[122.1686,40.42244],[121.64036,40.94639],[120.76863,40.59339],[119.6396,39.89806],[119.02346,39.25233],[118.04275,39.20427],[117.5327,38.73764],[118.0597,38.06148],[118.87815,37.89733],[118.91164,37.44846],[119.7028,37.15639],[120.82346,37.87043],[121.71126,37.48112],[122.35794,37.45448],[122.51999,36.93061],[121.10416,36.65133],[120.63701,36.11144],[119.66456,35.60979],[119.15121,34.90986],[120.22752,34.36033],[120.62037,33.37672],[121.22901,32.46032],[121.90815,31.69217],[121.89192,30.94935],[121.26426,30.67627],[121.50352,30.14291],[122.09211,29.83252],[121.93843,29.01802],[121.68444,28.22551],[121.12566,28.13567],[120.39547,27.05321],[119.5855,25.74078],[118.65687,24.54739],[117.28161,23.6245],[115.89074,22.78287],[114.76383,22.66807],[114.15255,22.22376],[113.80678,22.54834],[113.24108,22.05137],[111.84359,21.55049],[110.78547,21.39714],[110.44404,20.34103],[109.88986,20.28246],[109.62766,21.00823],[109.86449,21.39505],[108.52281,21.71521],[108.05018,21.55238],[107.04342,21.8119],[106.56727,22.2182],[106.7254,22.79427],[105.81125,22.97689],[105.32921,23.35206],[104.47686,22.81915],[103.50451,22.70376],[102.70699,22.7088],[102.17044,22.46475],[101.65202,22.3182],[101.80312,21.17437],[101.27003,21.20165],[101.18001,21.43657],[101.15003,21.84998],[100.41654,21.55884],[99.98349,21.74294],[99.2409,22.11831],[99.53199,22.94904],[98.89875,23.14272],[98.66026,24.06329],[97.60472,23.8974],[97.72461,25.08364],[98.67184,25.9187],[98.71209,26.74354],[98.68269,27.50881],[98.24623,27.74722],[97.91199,28.33595],[97.32711,28.26158],[96.24883,28.41103],[96.58659,28.83098],[96.11768,29.4528],[95.4048,29.03172],[94.56599,29.27744],[93.41335,28.64063],[92.50312,27.89688],[91.69666,27.77174],[91.25885,28.04061],[90.73051,28.06495],[90.01583,28.29644],[89.47581,28.04276],[88.81425,27.29932],[88.73033,28.08686],[88.12044,27.87654],[86.95452,27.97426],[85.82332,28.20358],[85.01164,28.64277],[84.23458,28.83989],[83.89899,29.32023],[83.33712,29.46373],[82.32751,30.11527],[81.5258,30.42272],[81.11126,30.18348],[79.72137,30.88271],[78.73889,31.51591],[78.45845,32.61816],[79.17613,32.48378],[79.20889,32.99439],[78.81109,33.5062],[78.91227,34.32194],[77.83745,35.49401],[76.19285,35.8984],[75.8969,36.66681],[75.15803,37.13303],[74.98,37.41999],[74.82999,37.99001],[74.86482,38.37885],[74.25751,38.60651],[73.92885,38.50582],[73.67538,39.43124],[73.96001,39.66001],[73.82224,39.89397],[74.77686,40.36643],[75.46783,40.56207],[76.52637,40.42795],[76.90448,41.06649],[78.1872,41.18532],[78.54366,41.58224],[80.11943,42.12394],[80.25999,42.35],[80.18015,42.92007],[80.86621,43.18036],[79.96611,44.91752],[81.94707,45.31703],[82.45893,45.53965],[83.18048,47.33003],[85.16429,47.00096],[85.72048,47.45297],[85.76823,48.45575],[86.59878,48.54918],[87.35997,49.21498],[87.75126,49.2972],[88.01383,48.59946],[88.8543,48.06908],[90.28083,47.69355],[90.97081,46.88815],[90.58577,45.71972],[90.94554,45.28607],[92.13389,45.11508],[93.48073,44.97547],[94.68893,44.35233],[95.30688,44.24133],[95.76245,43.31945],[96.3494,42.72564],[97.45176,42.74889],[99.51582,42.52469],[100.84587,42.6638],[101.83304,42.51487],[103.31228,41.90747],[104.52228,41.90835],[104.96499,41.59741],[106.12932,42.13433],[107.74477,42.48152],[109.2436,42.51945],[110.4121,42.87123],[111.12968,43.40683],[111.82959,43.74312],[111.66774,44.07318],[111.34838,44.45744],[111.87331,45.10208],[112.43606,45.01165],[113.46391,44.80889],[114.46033,45.33982],[115.9851,45.72724],[116.71787,46.3882],[117.4217,46.67273],[118.87433,46.80541],[119.66327,46.69268],[119.77282,47.04806],[118.86657,47.74706],[118.06414,48.06673],[117.29551,47.69771],[116.30895,47.85341],[115.74284,47.72654],[115.48528,48.13538],[116.1918,49.1346],[116.6788,49.88853],[117.87924,49.51098],[119.28846,50.14288],[119.27937,50.58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N.C.","contributorId":25173,"corporation":false,"usgs":true,"family":"Matalas","given":"N.C.","affiliations":[],"preferred":false,"id":363264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nordin, C.F. Jr.","contributorId":100852,"corporation":false,"usgs":true,"family":"Nordin","given":"C.F.","suffix":"Jr.","affiliations":[],"preferred":false,"id":363265,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70012356,"text":"70012356 - 1980 - Geochemical exploration for uranium in playas","interactions":[],"lastModifiedDate":"2025-04-10T14:08:10.947951","indexId":"70012356","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical exploration for uranium in playas","docAbstract":"Monitoring of snow and ice on the Earth's surface will require increasing use of satellite remote sensing techniques. These techniques are evolving rapidly. Active and passive sensors operating in the visible, near infrared, thermal infrared, and microwave wavelengths are described in regard to general applications and in regard to specific USA or USSR satellites. Meteorological satellites (frequent images of relatively crude resolution) and Earth resources satellites such as Landsat (less frequent images of higher resolution) have been used to monitor the areal extent of seasonal snow, but problems exist with cloud cover or dense forest canopies. Snow mass (water equivalent) can be measured from a low-flying aircraft using natural radioactivity, but cannot yet be measured from satellite altitudes. A combination of active and passive microwave sensors may permit this kind of measurement, but not until more is known about radiation scattering in snow. Satellite observations are very useful in glacier inventories, correcting maps of glacier extent, estimating certain mass balance parameters, and monitoring calving or surging glaciers. Ground ice is virtually impossible to monitor from satellites; ice on rivers and lakes can be monitored only with very high-resolution sensors. Microwave sensors, due to their all-weather capability (the ability to see through clouds) provide exciting data on sea ice distribution. Analysis of digital tapes of satellite data requires the archiving and scanning of huge amounts of data. Simple methods for extracting quantitative data from satellite images are described.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626668009491937","issn":"03036936","usgsCitation":"Meier, M.F., 1980, Remote sensing of snow and ice: Hydrological Sciences Bulletin, v. 25, no. 3, p. 307-330, https://doi.org/10.1080/02626668009491937.","productDescription":"24 p.","startPage":"307","endPage":"330","numberOfPages":"24","costCenters":[],"links":[{"id":487066,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626668009491937","text":"Publisher Index Page"},{"id":222466,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"3","noUsgsAuthors":false,"publicationDate":"2009-12-25","publicationStatus":"PW","scienceBaseUri":"505aa704e4b0c8380cd8519b","contributors":{"authors":[{"text":"Meier, M. F.","contributorId":98713,"corporation":false,"usgs":true,"family":"Meier","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":363009,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012387,"text":"70012387 - 1980 - Heat flow and energetics of the San Andreas fault zone","interactions":[],"lastModifiedDate":"2024-07-16T16:35:20.182875","indexId":"70012387","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"Heat flow and energetics of the San Andreas fault zone","docAbstract":"Approximately 100 heat flow measurements in the San Andreas fault zone indicate (1) there is no evidence for local factional heating of the main fault trace at any latitude over a 1000-km length from Cape Mendocino to San Bernardino, (2) average heat flow is high (∼2 HFU, ∼80 mW m−2) throughout the 550-km segment of the Coast Ranges that encloses the San Andreas fault zone in central California; this broad anomaly falls off rapidly toward the Great Valley to the east, and over a 200-km distance toward the Mendocino Triple Junction to the northwest. As others have pointed out, a local conductive heat flow anomaly would be detectable unless the frictional resistance allocated to heat production on the main trace were ≲100 bars. Frictional work allocated to surface energy of new fractures is probably unimportant, and hydrologic convection is not likely to invalidate the conduction assumption, since the heat discharge by thermal springs near the fault is negligible. Explanations for the low dynamic friction fall into two intergradational classes: those in which the fault is weak all of the time and those in which it is weak only during earthquakes (possibly just large ones). The first class includes faults containing anomalously weak gouge materials and faults containing materials with normal frictional properties under near-lithostatic steady state fluid pressures. In the second class, weakening is caused by the event (for example, a thermally induced increase in fluid pressure, dehydration of clay minerals, or acoustic fluidization). In this class, unlike the first, the average strength and ambient tectonic shear stress may be large, ∼1 kbar, but the stress allocated to elastic radiation (the apparent stress) must be of similar magnitude, an apparent contradiction with seismic estimates. Unless seismic radiation is underestimated for large earthquakes, it is difficult to justify average tectonic stresses on the main trace of the San Andreas fault in excess of ∼200 bars. The development of the broad Coast Range heat flow anomaly southward from Cape Mendocino suggests that heat flow increases by a factor of 2 within 4 m.y. after the passage of the Mendocino Triple Junction. This passage leaves the San Andreas transform fault zone in its wake; the depth of the anomalous sources cannot be much greater than the depth of the seismogenic layer. Some of the anomalous heat may be supplied by conduction from the warmer mantle that must occur south of the Mendocino transform (where there is no subducting slab), and some might be supplied by shear heating in the fault zone. With no contribution from shear heating, extreme mantle upwelling would be required, and asthenosphere conditions should exist today at depths of only ∼20 km in the northernmost Coast Ranges. If there is an appreciable contribution from shear heating, the heat flow constraint implies that the seismogenic layer is partially decoupled at its base and that the basal traction is in the sense that resists right lateral motion on the fault(s). As a result of these basal tractions, the average shearing stress in the seismogenic layer would increase with distance from the main fault, and the seismogenic layer would offer substantial resistance to plate motion even though resistance on the main fault might be negligible. These speculative models have testable consequences.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB085iB11p06185","issn":"01480227","usgsCitation":"Lachenbruch, A., and Sass, J., 1980, Heat flow and energetics of the San Andreas fault zone: Journal of Geophysical Research Solid Earth, v. 85, no. B11, p. 6185-6223, https://doi.org/10.1029/JB085iB11p06185.","productDescription":"39 p.","startPage":"6185","endPage":"6223","numberOfPages":"39","costCenters":[],"links":[{"id":222413,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"B11","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a2ff7e4b0c8380cd5d26e","contributors":{"authors":[{"text":"Lachenbruch, A.H.","contributorId":76737,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"A.H.","affiliations":[],"preferred":false,"id":363427,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":363426,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":46216,"text":"ofr80441 - 1980 - Maps showing hydrologic conditions in the San Francisco River area, Greenlee County, Arizona, 1978: A reconnaissance study","interactions":[],"lastModifiedDate":"2022-12-09T21:01:32.102478","indexId":"ofr80441","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"80-441","title":"Maps showing hydrologic conditions in the San Francisco River area, Greenlee County, Arizona, 1978: A reconnaissance study","docAbstract":"The San Francisco River area includes about 950 square miles in Greenlee County in east-central Arizona. Water-resources development has been slight compared with that in many areas in Arizona. In 1978 about 500 acre-feet of water was diverted for irrigation from the San Francisco and Blue Rivers, and about 550 acre-feet of ground water was withdrawn from wells for municipal use at Clifton. Surface water and ground water generally contained less than 500 milligrams per liter of dissolved solids; however, in the San Francisco River the dissolved-solids concentration increased from 263 to 885 milligrams per liter as the water moved downstream. The increase in dissolved solids was caused by inflow from springs near Clifton, one of which contained 11,700 milligrams per liter of dissolved solids. Information shown on the maps includes altitude of the water level, depth to water, well depth, streamflow characteristics of the San Francisco and Blue Rivers, and dissolved-solids and fluoride concentrations.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80441","usgsCitation":"Mann, L.J., 1980, Maps showing hydrologic conditions in the San Francisco River area, Greenlee County, Arizona, 1978: A reconnaissance study (WRI/OFR): U.S. Geological Survey Open-File Report 80-441, 2 Plate: 27.50 × 33.00 inches and 27.92 × 33.53 inches, https://doi.org/10.3133/ofr80441.","productDescription":"2 Plate: 27.50 × 33.00 inches and 27.92 × 33.53 inches","costCenters":[],"links":[{"id":170844,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410221,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11635.htm","linkFileType":{"id":5,"text":"html"}},{"id":83191,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0441/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83190,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0441/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Greenlee county","otherGeospatial":"San Francisco River area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.464,\n 33.75\n ],\n [\n -109.464,\n 33\n ],\n [\n -109.05,\n 33\n ],\n [\n -109.05,\n 33.75\n ],\n [\n -109.464,\n 33.75\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605ad4","contributors":{"authors":[{"text":"Mann, Larry J.","contributorId":48531,"corporation":false,"usgs":true,"family":"Mann","given":"Larry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":232852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70046237,"text":"70046237 - 1979 - White Marsh quadrangle: Geology, hydrology, and mineral resources","interactions":[{"subject":{"id":46945,"text":"ofr74347 - 1974 - Environmental geohydrology, folio No.1 (White Marsh 7 1/2-minute quadrangle)","indexId":"ofr74347","publicationYear":"1974","noYear":false,"title":"Environmental geohydrology, folio No.1 (White Marsh 7 1/2-minute quadrangle)"},"predicate":"SUPERSEDED_BY","object":{"id":70046237,"text":"70046237 - 1979 - White Marsh quadrangle: Geology, hydrology, and mineral resources","indexId":"70046237","publicationYear":"1979","noYear":false,"title":"White Marsh quadrangle: Geology, hydrology, and mineral resources"},"id":1}],"lastModifiedDate":"2026-05-27T15:09:24.06341","indexId":"70046237","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":279,"text":"Quadrangle Atlas","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"4","title":"White Marsh quadrangle: Geology, hydrology, and mineral resources","docAbstract":"No abstract available.
","language":"English","publisher":"Maryland Geological Survey","publisherLocation":"Baltimore, MD","usgsCitation":"Cleaves, E.T., Kuff, K.R., Otton, E.G., Crowley, W.P., and Reinhardt, J., 1979, White Marsh quadrangle: Geology, hydrology, and mineral resources: Quadrangle Atlas 4.","costCenters":[],"links":[{"id":273119,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.6,39.3 ], [ -76.6,39.6 ], [ -76.3,39.6 ], [ -76.3,39.3 ], [ -76.6,39.3 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51adbaece4b07c214e64bd5a","contributors":{"authors":[{"text":"Cleaves, Emery T.","contributorId":80249,"corporation":false,"usgs":true,"family":"Cleaves","given":"Emery","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":479256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kuff, Karen R.","contributorId":30896,"corporation":false,"usgs":true,"family":"Kuff","given":"Karen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":479254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Otton, Edmond G.","contributorId":96989,"corporation":false,"usgs":true,"family":"Otton","given":"Edmond","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":479258,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crowley, William P.","contributorId":60521,"corporation":false,"usgs":true,"family":"Crowley","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":479255,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Reinhardt, Juergen","contributorId":88714,"corporation":false,"usgs":true,"family":"Reinhardt","given":"Juergen","email":"","affiliations":[],"preferred":false,"id":479257,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70043066,"text":"70043066 - 1979 - A digital model for simulation of ground-water hydrology in the Houston area, Texas","interactions":[{"subject":{"id":10320,"text":"ofr79677 - 1979 - A digital model for simulation of ground-water hydrology in the Houston area, Texas","indexId":"ofr79677","publicationYear":"1979","noYear":false,"title":"A digital model for simulation of ground-water hydrology in the Houston area, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":70043066,"text":"70043066 - 1979 - A digital model for simulation of ground-water hydrology in the Houston area, Texas","indexId":"70043066","publicationYear":"1979","noYear":false,"title":"A digital model for simulation of ground-water hydrology in the Houston area, Texas"},"id":1}],"lastModifiedDate":"2017-06-14T12:23:14","indexId":"70043066","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":262,"text":"Limited Printing Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"103","title":"A digital model for simulation of ground-water hydrology in the Houston area, Texas","docAbstract":"This report documents the construction and calibration of a digital model for the simulation of hydrologic conditions in the Chicot and Evangeline aquifers in the Houston area of southeastern Texas. The model is a five-layer finite-difference model, with a grid pattern of 63 x 67 nodes representing an area of 27,000 square miles, for simulation of three- dimensional ground-water flow. The hydrologic properties and processes modeled were ground-water withdrawals, transmissivities, storage coefficients of the aquifers and clays, quantity of water derived from storage in the clays, and vertical hydraulic conductivity and vertical leakage. The model, which simulates water-level declines, changes in storage in the clay layers, and land-surface subsidence, was calibrated by use of historical records from 1890 to 1975. It is very sensitive to variations in transmissivities and to variations in water-table and artesian storage. It is less sensitive to variations in clay storage.
","language":"English","publisher":"Texas Department of Water Resources","publisherLocation":"Austin, TX","collaboration":"Prepared in cooperation with the Texas Department of Water Resources and the City of Houston","usgsCitation":"Meyer, W., and Carr, J.E., 1979, A digital model for simulation of ground-water hydrology in the Houston area, Texas: Limited Printing Report 103, v, 27, I-1, II-1, III-73 p.","productDescription":"v, 27, I-1, II-1, III-73 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":266908,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266906,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.twdb.texas.gov/publications/reports/limited_printing/doc/LP-103/LP-103%20a.pdf","text":"Report","size":"26.14 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Houston","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.361572265625,\n 30.95876857077987\n ],\n [\n -97.7783203125,\n 30.798474179567823\n ],\n [\n -97.349853515625,\n 28.603814407841327\n ],\n [\n -96.94335937499999,\n 27.89734922968426\n ],\n [\n -96.844482421875,\n 27.994401411046148\n ],\n [\n -96.52587890625,\n 28.17855984939698\n ],\n [\n -95.657958984375,\n 28.65203063036226\n ],\n [\n -94.28466796874999,\n 29.53522956294847\n ],\n [\n -94.361572265625,\n 30.95876857077987\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"510e4371e4b09f303997b281","contributors":{"authors":[{"text":"Meyer, Walter R.","contributorId":63283,"corporation":false,"usgs":true,"family":"Meyer","given":"Walter R.","affiliations":[],"preferred":false,"id":472904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carr, Jerry E.","contributorId":47758,"corporation":false,"usgs":true,"family":"Carr","given":"Jerry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":472903,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70042633,"text":"70042633 - 1979 - Better utilization of ground water in the Piedmont and mountain region of the southeast","interactions":[{"subject":{"id":19287,"text":"ofr79262 - 1979 - Better utilization of ground water in the Piedmont and mountain region of the Southeast","indexId":"ofr79262","publicationYear":"1979","noYear":false,"title":"Better utilization of ground water in the Piedmont and mountain region of the Southeast"},"predicate":"SUPERSEDED_BY","object":{"id":70042633,"text":"70042633 - 1979 - Better utilization of ground water in the Piedmont and mountain region of the southeast","indexId":"70042633","publicationYear":"1979","noYear":false,"title":"Better utilization of ground water in the Piedmont and mountain region of the southeast"},"id":1}],"lastModifiedDate":"2016-11-30T12:41:04","indexId":"70042633","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Better utilization of ground water in the Piedmont and mountain region of the southeast","docAbstract":"The development of water supplies for domestic consumption, and for those commercial and industrial uses requiring relatively pure water, has followed a pattern in the Piedmont and mountain areas of the southeast similar to that in most other humid areas. The first settlers utilized seepage springs on hillsides. Such springs occur along steep slopes where the water table intersects the land surface. As the population of the region grew, it became increasingly necessary to resort to shallow dug wells for domestic water supplies. Such wells also served as sources of water for the villages that developed, in time, around crossroad taverns. Seepage springs and dug wells are a satisfactory source of water in a virgin environment but are quickly polluted by careless waste-disposal practices. Thus disposal of domestic wastes in shallow pits resulted in epidemics of water-borne diseases as the villages grew into towns. This resulted in the third phase of water-supply development, which consisted of installing water lines and supplying water to homes from town-owned wells. In time, some of these wells became polluted and others failed to supply adequate water for the increasing needs of the larger urban areas. In the fourth phase these areas met their needs by drawing water from nearby streams. By the early years of this century it was possible to make this water palatable and relatively safe as a result of improvement in filtration methods. Streams, of course, have highly variable rates of flow and, as towns grew into small cities, the minimum flow of many streams was not adequate to meet the water-supply needs. This problem was solved in the fifth phase by building dams on the streams. We are still in this phase as we build larger and larger reservoirs to meet our growing water needs. Thus, through five phases of growth in the Piedmont and mountains we have advanced from the point where ground water was the sole source of supply to the point where it is the forgotten resource. For reasons to be explained below, a sixth phase can be foreseen in which ground water and surface water are recognized as parts of the hydrologic system with advantages in their conjunctive development and use.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Water conservation and alternative water supplies: proceedings of a southeast regional conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Georgia Institute of Technology","publisherLocation":"Atlanta, GA","usgsCitation":"Heath, R., 1979, Better utilization of ground water in the Piedmont and mountain region of the southeast, in Water conservation and alternative water supplies: proceedings of a southeast regional conference, p. 145-160.","productDescription":"16 p.; ill.; map","startPage":"145","endPage":"160","numberOfPages":"16","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":265708,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Piedmont","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.6525,24.52 ], [ -91.6525,42.2694 ], [ -73.9025,42.2694 ], [ -73.9025,24.52 ], [ -91.6525,24.52 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f6887fe4b0f5392eb7e77c","contributors":{"authors":[{"text":"Heath, Ralph C.","contributorId":53359,"corporation":false,"usgs":true,"family":"Heath","given":"Ralph C.","affiliations":[],"preferred":false,"id":471942,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039032,"text":"70039032 - 1979 - United States Geological Survey Yearbook, fiscal year 1978","interactions":[],"lastModifiedDate":"2017-03-08T16:45:01","indexId":"70039032","displayToPublicDate":"2012-01-01T11:39:03","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":392,"text":"Yearbook","active":false,"publicationSubtype":{"id":6}},"title":"United States Geological Survey Yearbook, fiscal year 1978","docAbstract":"Fiscal year 1978 saw the U.S. Geological Survey continuing to perform its basic historical missions of collecting, analyzing, and disseminating information about the Earth, its processes, and its water and mineral resources. Classifying Federal lands and supervising lessee mineral extraction operations on those lands were also major Survey concerns during the year. In addition, substantial progress was made in the exploration and assessment of the petroleum potential of the National Petroleum Reserve in Alaska, a recently assigned mission. These basic missions found expression in a wide range of program activities and interests as diverse as the sands of Mars and the volcanoes of Hawaii. Programs included assessment of numerous potential energy and mineral resources, study of earthquakes and other geologic hazards, appraisal of the magnitude and quality of the Nation's water resources, and supervision of lease operations on Federal lands. The Survey also was involved in developing data on land use and producing topographic, geologic, and hydrologic maps for public and private use. In cooperation with other Federal agencies, the Survey participated in studies under the U.S. Climate Program and continued its analysis of data received from the two Viking landers on the surface of Mars. On April 3, 1978, Dr. H. William Menard became the 10th Director of the U.S. Geological Survey. Dr. Menard, who, until his appointment, was Professor of Geology at the Scripps Institution of Oceanography, San Diego, Calif., brings to the Director's post the experience gained in a long and successful career as a marine geologist and oceanographer. He succeeds Dr. Vincent E. McKelvey, who continues with the Survey as a senior research scientist.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039032","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, United States Geological Survey Yearbook, fiscal year 1978: Yearbook, vi, 208 p., https://doi.org/10.3133/70039032.","productDescription":"vi, 208 p.","costCenters":[],"links":[{"id":261269,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039032/report.pdf","text":"Report","size":"73.02 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":261270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039032/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc90e4b08c986b328ce9","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":535201,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70040787,"text":"70040787 - 1979 - Hydrologic and water-quality appraisal of southeast Nassau County, Long Island, New York","interactions":[],"lastModifiedDate":"2012-11-16T11:52:20","indexId":"70040787","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":263,"text":"Long Island Water Resources Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"LIWR-13","title":"Hydrologic and water-quality appraisal of southeast Nassau County, Long Island, New York","language":"English","publisher":"Nassau County Department of Public Works","publisherLocation":"Mineola, NY","usgsCitation":"Ku, H., and Sulam, D., 1979, Hydrologic and water-quality appraisal of southeast Nassau County, Long Island, New York: Long Island Water Resources Bulletin LIWR-13, 129 p.","productDescription":"129 p.","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263240,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a76ec7e4b0e93eb366ee99","contributors":{"authors":[{"text":"Ku, H.F.H.","contributorId":53012,"corporation":false,"usgs":true,"family":"Ku","given":"H.F.H.","email":"","affiliations":[],"preferred":false,"id":469012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sulam, D.J.","contributorId":99610,"corporation":false,"usgs":true,"family":"Sulam","given":"D.J.","affiliations":[],"preferred":false,"id":469013,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":45785,"text":"wri79111 - 1979 - River mileages and drainage areas for Illinois streams—Volume 2, Illinois River basin","interactions":[],"lastModifiedDate":"2020-04-30T16:04:39.371965","indexId":"wri79111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-111","displayTitle":"River Mileages and Drainage Areas for Illinois Streams—Volume 2, Illinois River Basin","title":"River mileages and drainage areas for Illinois streams—Volume 2, Illinois River basin","docAbstract":"River mileages are presented for points of interest on Illinois streams draining 10 square miles or more. Points of interest include bridges, dams, gaging stations, county lines, hydrologic unit boundaries, and major tributaries. Drainage areas are presented for selected sites, including total drainage area for any stream draining at least 100 square miles. The report is contained in two volumes. This volume (Volume II) includes Illinois River basin.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri79111","collaboration":"Prepared in cooperation with the U.S. Army of Engineers","usgsCitation":"Healy, R.W., 1979, River mileages and drainage areas for Illinois streams—Volume 2, Illinois River basin: U.S. Geological Survey Water-Resources Investigations Report 79-111, v. 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405 North Goodwin
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No abstract available.
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Jr.","contributorId":83887,"corporation":false,"usgs":true,"family":"Frazee","given":"James","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":228467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laughlin, Charles P.","contributorId":6490,"corporation":false,"usgs":true,"family":"Laughlin","given":"Charles","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":228466,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26821,"text":"wri7963 - 1979 - Environmental features, general hydrology, and external sources of nutrients affecting Wilderness Lake, King County, Washington","interactions":[],"lastModifiedDate":"2019-08-05T11:26:57","indexId":"wri7963","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-63","title":"Environmental features, general hydrology, and external sources of nutrients affecting Wilderness Lake, King County, Washington","docAbstract":"A water budget prepared for Wilderness Lake, a candidate for lake-quality restoration, indicates that of the 530 acre-feet of water that enters the lake each year, 170 acre-feet is from precipitation and 360 acre-feet is from groundwater inflow. An equal amount leaves the lake, and of this, 380 acre-feet is by surface runoff, 8 acre-feet is by groundwater seepage, and 140 acre-feet is by evaporation. Based on these amounts of inflow and outflow, the theoretical water-renewal time of the lake is calculated to be 2.6 years. The annual contributions of nitrogen and phosphorus to the lake from precipitation, natural ground water, and septic-tank leachate are about 920 kilograms nitrogen and 38 kilograms phosphorus. Nitrogen and phosphorus contributions from other sources were not assessed but could be significant. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7963","usgsCitation":"Dion, N.P., 1979, Environmental features, general hydrology, and external sources of nutrients affecting Wilderness Lake, King County, Washington: U.S. Geological Survey Water-Resources Investigations Report 79-63, v, 27 p. , https://doi.org/10.3133/wri7963.","productDescription":"v, 27 p. ","costCenters":[],"links":[{"id":366246,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0063/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0063/report-thumb.jpg"}],"country":"United States","state":"Washington","county":"King County","otherGeospatial":"Wilderness Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.03922271728514,\n 47.36929191683155\n ],\n [\n -122.0313262939453,\n 47.36929191683155\n ],\n [\n -122.0313262939453,\n 47.38021933437073\n ],\n [\n -122.03922271728514,\n 47.38021933437073\n ],\n [\n -122.03922271728514,\n 47.36929191683155\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6023ec","contributors":{"authors":[{"text":"Dion, N. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79338","usgsCitation":"Frazee, J.M., and Laughlin, C.P., 1979, Hydrologic overlay maps of the Cocoa Beach quadrangle, Florida: U.S. Geological Survey Open-File Report 79-338, 5 Plates: 23.79 x 36.27 inches, https://doi.org/10.3133/ofr79338.","productDescription":"5 Plates: 23.79 x 36.27 inches","costCenters":[],"links":[{"id":399033,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0338/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399032,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0338/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399031,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0338/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399030,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0338/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399029,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0338/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397090,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28378.htm"},{"id":172740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0338/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Florida","otherGeospatial":"Cocoa Beach quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.5,\n 28.25\n ],\n [\n -80.625,\n 28.25\n ],\n [\n -80.625,\n 28.375\n ],\n [\n -80.5,\n 28.375\n ],\n [\n -80.5,\n 28.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688414","contributors":{"authors":[{"text":"Frazee, James M. Jr.","contributorId":83887,"corporation":false,"usgs":true,"family":"Frazee","given":"James","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":228522,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laughlin, Charles P.","contributorId":6490,"corporation":false,"usgs":true,"family":"Laughlin","given":"Charles","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":228521,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29551,"text":"wri78118 - 1979 - Ground-water conditions and potential for artificial recharge in Lucerne Valley, San Bernardino County, California","interactions":[],"lastModifiedDate":"2017-07-11T10:50:55","indexId":"wri78118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"78-118","title":"Ground-water conditions and potential for artificial recharge in Lucerne Valley, San Bernardino County, California","docAbstract":"The water level in two areas of Lucerne Valley has declined more than 100 feet since 1917, including 60 feet from 1954 to 1976. These declines are the result of pumping for the irrigation of alfalfa. The lowering of water levels has caused many shallow domestic wells to go dry.
Well yields in the valley generally are between 10 and 1,000 gallons per minute. About 240,000 acre-feet of ground water was extracted between 1950 and 1976. About 1,750,000 acre-feet remains in storage.
Water of poor quality underlies the valley around Lucerne Lake. There was no definable movement of this water from 1954 to 1976, but the possibility exists for future movement toward centers of pumping.
Lucerne Valley may be hydrologically suitable for artificial-recharge operations. Preliminary data suggest an area in T. 4 N., R. 1 E. as suitable for artificial recharge that would benefit most of the areas affected by the water-level declines. Detailed investigation is needed before recharge operations are begun.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri78118","collaboration":"Prepared in cooperation with the Mohave Water Agency","usgsCitation":"Schaefer, D.H., 1979, Ground-water conditions and potential for artificial recharge in Lucerne Valley, San Bernardino County, California: U.S. Geological Survey Water-Resources Investigations Report 78-118, iv, 37 p., https://doi.org/10.3133/wri78118.","productDescription":"iv, 37 p.","numberOfPages":"48","costCenters":[],"links":[{"id":343482,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0118/wri78118.pdf","text":"Report","size":"3 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 78-118"},{"id":159953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0118/coverthb.jpg"}],"country":"United States","state":"California","county":"San Bernardino County","otherGeospatial":"Lucerne 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79501","usgsCitation":"Frazee, J.M., and Laughlin, C.P., 1979, Hydrologic overlay maps of the Sebastian quadrangle, Florida: U.S. Geological Survey Open-File Report 79-501, 5 Plates: 23.77 x 36.35 inches or smaller, https://doi.org/10.3133/ofr79501.","productDescription":"5 Plates: 23.77 x 36.35 inches or smaller","costCenters":[],"links":[{"id":398993,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0501/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398992,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0501/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398991,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0501/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398990,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0501/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398989,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0501/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397125,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_29158.htm"},{"id":168551,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0501/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Florida","otherGeospatial":"Sebastian quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.5,\n 27.75\n ],\n [\n -80.375,\n 27.75\n ],\n [\n -80.375,\n 27.875\n ],\n [\n -80.5,\n 27.875\n ],\n [\n -80.5,\n 27.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605722","contributors":{"authors":[{"text":"Frazee, James M. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1481","usgsCitation":"Wright, A.F., 1979, Bibliography of geology and hydrology, San Juan Basin, New Mexico, Colorado, Arizona, and Utah: U.S. Geological Survey Bulletin 1481, iii, 123 p., https://doi.org/10.3133/b1481.","productDescription":"iii, 123 p.","costCenters":[],"links":[{"id":64252,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1481/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1481/report-thumb.jpg"},{"id":409755,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21574.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona, Colorado, New Mexico, Utah","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.333,\n 37.333\n ],\n [\n -109.333,\n 34.667\n ],\n [\n -107,\n 34.667\n ],\n [\n -107,\n 37.333\n ],\n [\n -109.333,\n 37.333\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db6294a1","contributors":{"authors":[{"text":"Wright, Ann Finley","contributorId":99196,"corporation":false,"usgs":true,"family":"Wright","given":"Ann","email":"","middleInitial":"Finley","affiliations":[],"preferred":false,"id":216116,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":45932,"text":"ofr79519 - 1979 - Hydrologic overlay maps of the Melbourne East Quadrangle, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:58","indexId":"ofr79519","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-519","title":"Hydrologic overlay maps of the Melbourne East Quadrangle, Florida","language":"ENGLISH","doi":"10.3133/ofr79519","usgsCitation":"Frazee, J.M., and Laughlin, C.P., 1979, Hydrologic overlay maps of the Melbourne East Quadrangle, Florida: U.S. Geological Survey Open-File Report 79-519, 7 maps ;80 x 56 cm., https://doi.org/10.3133/ofr79519.","productDescription":"7 maps ;80 x 56 cm.","costCenters":[],"links":[{"id":168626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606471","contributors":{"authors":[{"text":"Frazee, James M. Jr.","contributorId":83887,"corporation":false,"usgs":true,"family":"Frazee","given":"James","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":232324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laughlin, Charles P.","contributorId":6490,"corporation":false,"usgs":true,"family":"Laughlin","given":"Charles","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":232323,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27615,"text":"wri79110 - 1979 - River mileages and drainage areas for Illinois streams—Volume 1, Illinois except Illinois River basin","interactions":[],"lastModifiedDate":"2021-01-11T18:42:19.337486","indexId":"wri79110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-110","displayTitle":"River mileages and drainage areas for Illinois streams—Volume 1, Illinois except Illinois River basin","title":"River mileages and drainage areas for Illinois streams—Volume 1, Illinois except Illinois River basin","docAbstract":"River mileages are presented for points of interest on Illinois streams draining 10 square miles or more. Points of interest include bridges, dams, gaging stations, county lines, hydrologic unit boundaries, and major tributaries. Drainage areas are presented for selected sites, including total drainage area for any stream draining at least 100 square miles. The report is contained in two volumes. This volume (Volume I) includes Illinois except Illinois River basin.
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Brevard County is an area of some 1,300 square miles located on the east coast of central Florida. The Cape Canaveral quadrangle, in central Brevard, includes part of the Merritt Island National Wildlife Refuge, John F. Kennedy Space Center (NASA), and Cape Canaveral Air Force Station. The eastern part of the quadrangle is occupied by the Atlantic Ocean and the western part by estuarine waters of the Banana River. Topography is characterized by numerous elongate sand dumes, with altitudes up to 10 feet or greater, which roughly parallel the estuary and ocean.
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