No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr70189","issn":"0094-9140","usgsCitation":"Knutilla, R., 1970, Statistical summaries of Michigan streamflow data, duration hydrographs and summaries of flow duration, low flow, high flow, and monthly and annual mean discharge through September 1967: U.S. Geological Survey Open-File Report 70-189, 283 p., https://doi.org/10.3133/ofr70189.","productDescription":"283 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":154890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United 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L.","affiliations":[],"preferred":false,"id":190397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23018,"text":"ofr70121 - 1970 - Geohydrology of the Cross-Florida Barge Canal area, with special reference to the Ocala vicinity","interactions":[],"lastModifiedDate":"2012-02-02T00:07:52","indexId":"ofr70121","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-121","title":"Geohydrology of the Cross-Florida Barge Canal area, with special reference to the Ocala vicinity","docAbstract":"The Cross-Florida Barge Canal route commences at Palatka on the St. Johns River, about 75 miles upstream from the Atlantic Ocean, and extends 110 miles southwestward across Peninsular Florida into deep water in the Gulf of Mexico near Yankeetown. The canal will be equipped with five locks, each 600 feet long and 84 feet wide, and the channel will be a minimum of 12 feet deep and 150 feet wide. From near Ocala northeastward, the canal channel will replace much of the natural channel of the Oklawaha River, and will be excavated into beds of the so-called shallow sand aquifer of Miocene and younger age, which overlies limestone of the Floridan aquifer. Westward from Ocala most of the canal will be excavated below the potentiometric surface into limestone and dolomite of the Floridan aquifer. Water levels of Rodman, Eureka, and Inglis Pools will be controlled by dams and spillways with limited exchange of water between the pools and the aquifers. The water levels in the Summit Pool will fluctuate with the natural changes in the ground-water level of the Floridan aquifer, although the stage of the pool will be partially controlled by the stage held in the Eureka Pool. A dynamic inflow-outflow relationship will exist between the Sun, nit Pool and the Floridan aquifer. \r\n\r\nThe Floridan aquifer in the canal area is 1,000 to 1,200 feet thick and consists of limestone and dolomite of middle Eocene to Miocene age, including, from older to younger the Lake City, Avon Park and Ocala limestones plus permeable sandy, dolomitic limestone in the lower part of the Hawthorn Formation. It is possible that most of the flow to the two major springs in the area occurs in the upper 100 feet or so of the aquifer in the Ocala Limestone. The aquifer is underlain by the Oldsmar Limestone of early Eocene age and is overlain by sand, clayey sand, clay and shell beds of Miocene through Holocene age, ranging from a few feet to two or three hundred feet thick. The permeable beds overlying the Floridan aquifer constitute the shallow aquifer, while the poorly permeable ones act as confining beds where the Floridan aquifer is under artesian conditions. \r\n\r\nA north-south line drawn separating the head of Silver Springs on the west from the Oklawaha River on the east marks the approximate westward limit of a continuous blanket of Miocene-Pliocene(?) age materials covering the rocks of the Floridan aquifer. East of the line much of the aquifer is under artesian conditions, particularly in the Oklawaha River valley, although in some areas east of the valley direct recharge through thick permeable Miocene-Pliocene(?) sands occurs. West of the line, only scattered remnants of a once continuous Miocene-Pliocene(?) cover remains. Lack of the cover is a result of erosion on the crest and flanks of the Ocala Uplift, a broad northwest-southeast trending anticlinal upwarp, the axis of which is crossed by the canal route in the Dunnellon area. Over most of this area the Floridan aquifer is unconfined, and receives direct recharge through a cover of a few tens of feet of sand and clayey sand of Quaternary age. \r\n\r\nTensional stresses during the structural evolution of the Ocala Uplift produced an intersecting system of fractures and normal faults in rocks of the Florida Aquifer. The fractures and faults are important controls for orientation of solution channels, and, therefore, for development of ground-water circulation patterns. When the system of surface streams which once drained the Barge Canal area eroded the poorly permeable Miocene-Pliocene(?) cover from the flanks of the Ocala Uplift, surface runoff was reduced and precipitation began to directly infiltrate the underlying limestones. Now only principal rivers, such as the Oklawaha and Withlacoochee Rivers, and a few short tributaries remain, while one of the most highly developed subsurface drainage systems in the world has evolved in the cavernous limestones of the Floridan aquifer. Two of the larger fresh water spr","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/ofr70121","issn":"0094-9140","usgsCitation":"Faulkner, G.L., 1970, Geohydrology of the Cross-Florida Barge Canal area, with special reference to the Ocala vicinity: U.S. Geological Survey Open-File Report 70-121, xii, 229 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr70121.","productDescription":"xii, 229 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154732,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0121/report-thumb.jpg"},{"id":52403,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0121/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a89d8","contributors":{"authors":[{"text":"Faulkner, Glen L.","contributorId":58302,"corporation":false,"usgs":true,"family":"Faulkner","given":"Glen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":189288,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56041,"text":"ofr70244 - 1970 - A proposed streamflow-data program for Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:11:50","indexId":"ofr70244","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-244","title":"A proposed streamflow-data program for Virginia","language":"ENGLISH","doi":"10.3133/ofr70244","usgsCitation":"Nuckels, E.H., 1970, A proposed streamflow-data program for Virginia: U.S. Geological Survey Open-File Report 70-244, 63 p., 3 figs., https://doi.org/10.3133/ofr70244.","productDescription":"63 p., 3 figs.","costCenters":[],"links":[{"id":174945,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8880","contributors":{"authors":[{"text":"Nuckels, E. H.","contributorId":15647,"corporation":false,"usgs":true,"family":"Nuckels","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":254682,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":22805,"text":"ofr7093 - 1970 - Water resources in the Big Lost River Basin, south-central Idaho","interactions":[],"lastModifiedDate":"2013-11-19T10:42:50","indexId":"ofr7093","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-93","title":"Water resources in the Big Lost River Basin, south-central Idaho","docAbstract":"The Big Lost River basin occupies about 1,400 square miles in south-central Idaho and drains to the Snake River Plain. The economy in the area is based on irrigation agriculture and stockraising. The basin is underlain by a diverse-assemblage of rocks which range, in age from Precambrian to Holocene. The assemblage is divided into five groups on the basis of their hydrologic characteristics. Carbonate rocks, noncarbonate rocks, cemented alluvial deposits, unconsolidated alluvial deposits, and basalt. The principal aquifer is unconsolidated alluvial fill that is several thousand feet thick in the main valley. The carbonate rocks are the major bedrock aquifer. They absorb a significant amount of precipitation and, in places, are very permeable as evidenced by large springs discharging from or near exposures of carbonate rocks. Only the alluvium, carbonate rock and locally the basalt yield significant amounts of water. \n\nA total of about 67,000 acres is irrigated with water diverted from the Big Lost River. The annual flow of the river is highly variable and water-supply deficiencies are common. About 1 out of every 2 years is considered a drought year. In the period 1955-68, about 175 irrigation wells were drilled to provide a supplemental water supply to land irrigated from the canal system and to irrigate an additional 8,500 acres of new land.\n\nAverage. annual precipitation ranged from 8 inches on the valley floor to about 50 inches at some higher elevations during the base period 1944-68. The estimated water yield of the Big Lost River basin averaged 650 cfs (cubic feet per second) for the base period. Of this amount, 150 cfs was transpired by crops, 75 cfs left the basin as streamflow, and 425 cfs left as ground-water flow. A map of precipitation and estimated values of evapotranspiration were used to construct a water-yield map. \n\nA distinctive feature of the Big Lost River basin, is the large interchange of water from surface streams into the ground and from the ground into the surface streams. Large quantities of water disappear in the Chilly, Darlington, and other sinks and reappear above Mackay Narrows, above Moore Canal heading, and in other reaches. A cumulative summary of water yield upstream from selected points in the basin is as follows :\n\nAbove Howell Ranch: water yield: 345 cfs; surface water: 310 cfs; ground water: 35 cfs\n\nAbove. Mackay Narrows water yield: 450 cfs; surface water: 325 cfs; ground water: 75 cfs; crop evapotranspiration: 50 cfs\n\nAbove Arco: water yield: 650 cfs; surface water: 75 cfs; ground water: 425 cfs; crop evapotranspiration: 150 cfs\n\nGround-water pumping affects streamflow in reaches , where the stream and water table are continuous, but the effects of pumping were not measured except locally. Pumping depletes the total water supply by the. amount of the pumped water that is evapotranspired by crops. The part of the pumped water that is not consumed percolates into the ground or runs off over the land surface to the stream. The estimated 425 cfs that leaves the basin as ground-water flow is more than adequate for present and foreseeable needs. However because much of the outflow occurs at considerable depth, the quantity that is salvageable is unknown.\n\nBoth the surface and ground waters are of good quality and are suitable for most uses. Although these waters are low in total dissolved solids, they tend to be hard or very hard.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7093","collaboration":"Prepared in cooperation with the Idaho Department of Reclamation","usgsCitation":"Crosthwaite, E., Thomas, C., and Dyer, K., 1970, Water resources in the Big Lost River Basin, south-central Idaho: U.S. Geological Survey Open-File Report 70-93, vi, 109 p., https://doi.org/10.3133/ofr7093.","productDescription":"vi, 109 p.","numberOfPages":"122","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":155707,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0093/report-thumb.jpg"},{"id":52236,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0093/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Big Lost River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.112216,43.516533 ], [ -113.112216,44.096 ], [ -114.119915,44.096 ], [ -114.119915,43.516533 ], [ -113.112216,43.516533 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f09e0","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":188905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, C.A.","contributorId":14385,"corporation":false,"usgs":true,"family":"Thomas","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":188904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dyer, K.L.","contributorId":100011,"corporation":false,"usgs":true,"family":"Dyer","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":188906,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":41041,"text":"ofr705 - 1970 - Physiographic diagrams of parts of the continental borderlands of California and Alaska: 12 physiographic diagrams: Southern California Borderland; Eastern Murray Fracture Zone and Transverse Ranges; Southern Monterey Bay; Monterey Canyon; Central San","interactions":[],"lastModifiedDate":"2012-02-02T00:05:01","indexId":"ofr705","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-5","title":"Physiographic diagrams of parts of the continental borderlands of California and Alaska: 12 physiographic diagrams: Southern California Borderland; Eastern Murray Fracture Zone and Transverse Ranges; Southern Monterey Bay; Monterey Canyon; Central San","language":"ENGLISH","doi":"10.3133/ofr705","usgsCitation":"Alpha, T.R., 1970, Physiographic diagrams of parts of the continental borderlands of California and Alaska: 12 physiographic diagrams: Southern California Borderland; Eastern Murray Fracture Zone and Transverse Ranges; Southern Monterey Bay; Monterey Canyon; Central San: U.S. Geological Survey Open-File Report 70-5, 12 maps, https://doi.org/10.3133/ofr705.","productDescription":"12 maps","costCenters":[],"links":[{"id":135268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98348,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-01.pdf","size":"2437","linkFileType":{"id":1,"text":"pdf"}},{"id":98349,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-02.pdf","size":"1549","linkFileType":{"id":1,"text":"pdf"}},{"id":98350,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-03.pdf","size":"4147","linkFileType":{"id":1,"text":"pdf"}},{"id":98351,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-04.pdf","size":"3695","linkFileType":{"id":1,"text":"pdf"}},{"id":98352,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-05.pdf","size":"2504","linkFileType":{"id":1,"text":"pdf"}},{"id":98354,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-07.pdf","size":"4064","linkFileType":{"id":1,"text":"pdf"}},{"id":98355,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-08.pdf","size":"6757","linkFileType":{"id":1,"text":"pdf"}},{"id":98356,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-09.pdf","size":"2621","linkFileType":{"id":1,"text":"pdf"}},{"id":98357,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-10.pdf","size":"2913","linkFileType":{"id":1,"text":"pdf"}},{"id":98358,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-11.pdf","size":"1178","linkFileType":{"id":1,"text":"pdf"}},{"id":98359,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-12.pdf","size":"912","linkFileType":{"id":1,"text":"pdf"}},{"id":98353,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0005/plate-06.pdf","size":"1267","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6859d0","contributors":{"authors":[{"text":"Alpha, Tau Rho","contributorId":63371,"corporation":false,"usgs":true,"family":"Alpha","given":"Tau","email":"","middleInitial":"Rho","affiliations":[],"preferred":false,"id":224372,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1003,"text":"wsp1869E - 1970 - Response of gas-purged manometers to oscillations in water level","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1869E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1869","chapter":"E","title":"Response of gas-purged manometers to oscillations in water level","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1869E","usgsCitation":"Beck, J., and Goodwin, C., 1970, Response of gas-purged manometers to oscillations in water level: U.S. Geological Survey Water Supply Paper 1869, iii, 24 p., https://doi.org/10.3133/wsp1869E.","productDescription":"iii, 24 p.","costCenters":[],"links":[{"id":136146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1869e/report-thumb.jpg"},{"id":25574,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1869e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6283ab","contributors":{"authors":[{"text":"Beck, J.R.","contributorId":46921,"corporation":false,"usgs":true,"family":"Beck","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":143001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodwin, Carl R.","contributorId":76284,"corporation":false,"usgs":true,"family":"Goodwin","given":"Carl R.","affiliations":[],"preferred":false,"id":143002,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23870,"text":"ofr70220 - 1970 - Phosphate rock at West Thaniyat, Sirhan-Turaif (Jawf-Sakakah) Basin Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:08:07","indexId":"ofr70220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-220","title":"Phosphate rock at West Thaniyat, Sirhan-Turaif (Jawf-Sakakah) Basin Kingdom of Saudi Arabia","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr70220","issn":"0094-9140","usgsCitation":"Meissner, C.R., 1970, Phosphate rock at West Thaniyat, Sirhan-Turaif (Jawf-Sakakah) Basin Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 70-220, 8 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr70220.","productDescription":"8 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":155480,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0220/report-thumb.jpg"},{"id":53085,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0220/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687728","contributors":{"authors":[{"text":"Meissner, Charles R. 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