{"pageNumber":"5909","pageRowStart":"147700","pageSize":"25","recordCount":165658,"records":[{"id":61912,"text":"gq604 - 1966 - Geologic map of the Caledonia quadrangle, Trigg and Christian Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:12:38","indexId":"gq604","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"604","title":"Geologic map of the Caledonia quadrangle, Trigg and Christian Counties, Kentucky","language":"ENGLISH","doi":"10.3133/gq604","usgsCitation":"Ulrich, G.E., and Klemic, H., 1966, Geologic map of the Caledonia quadrangle, Trigg and Christian Counties, Kentucky: U.S. Geological Survey Geologic Quadrangle 604, 1 map :col. ;77 x 89 cm., https://doi.org/10.3133/gq604.","productDescription":"1 map :col. ;77 x 89 cm.","costCenters":[],"links":[{"id":103331,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1917.htm","linkFileType":{"id":5,"text":"html"},"description":"1917"},{"id":248200,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0604/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":253026,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0604/report-thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d54d","contributors":{"authors":[{"text":"Ulrich, George E.","contributorId":23550,"corporation":false,"usgs":true,"family":"Ulrich","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":266546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klemic, Harry","contributorId":49767,"corporation":false,"usgs":true,"family":"Klemic","given":"Harry","email":"","affiliations":[],"preferred":false,"id":266547,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38849,"text":"pp543D - 1966 - Geologic effects of the March 1964 earthquake and associated seismic sea waves on Kodiak and nearby islands, Alaska","interactions":[],"lastModifiedDate":"2022-02-17T19:34:30.778879","indexId":"pp543D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"543","chapter":"D","title":"Geologic effects of the March 1964 earthquake and associated seismic sea waves on Kodiak and nearby islands, Alaska","docAbstract":"Kodiak Island and the nearby islands constitute a mountainous landmass with an aggregate area of 4,900 square miles that lies at the western border of the Gulf of Alaska and from 20 to 40 miles off the Alaskan mainland. Igneous and metamorphic rocks underlie most of the area except for a narrow belt of moderately to poorly indurated rocks bordering the Gulf of Alaska coast and local accumulations of unconsolidated alluvial and marine deposits along the streams and coast. The area is relatively undeveloped and is sparsely inhabited. About 4,800 of the 5,700 permanent residents in the area live in the city of Kodiak or at the Kodiak Naval Station.\n\nThe great earthquake, which occurred on March 27, 1964, at 5:36 p.m. Alaska standard time (March 28,1964, 0336 Greenwich mean time), and had a Richter magnitude of 8.4-8.5, was the most severe earthquake felt on Kodiak Island and its nearby islands in modern times. Although the epicenter lies in Prince William Sound 250 miles northeast of Kodiak—the principal city of the area—the areal distribution of the thousands of aftershocks that followed it, the local tectonic deformation, and the estimated source area of the subsequent seismic sea wave, all suggest that the Kodiak group of islands lay immediately adjacent to, and northwest of, the focal region from which the elastic seismic energy was radiated. The duration of strong ground motion in the area was estimated at 2½ minutes. Locally, the tremors were preceded by sounds audible to the human ear and were reportedly accompanied in several places by visible ground waves.\n\nIntensity and felt duration of the shocks during the main earthquake and aftershock sequence varied markedly within the area and were strongly influenced by the local geologic environment. Estimated Mercalli intensities in most areas underlain by unconsolidated Quaternary deposits ranged from VIII to as high as IX. In contrast, intensities in areas of upper Tertiary rock ranged from VII to VIII, and in areas of relatively well indurated lower Tertiary and Mesozoic rocks, from VI to VII.\n\nLocal subsidence of as much as 10 feet was widespread in noncohesive granular deposits through compaction, flow, and sliding that resulted from vibratory loading during the earthquake. This phenomenon, which was largely restricted to saturated beach and alluvial deposits or artificial fill, was locally accompanied by extensive cracking of the ground and attendant ejection of water and water-sediment mixtures.\n\nNumerous landslides, including a wide variety of rockfalls, rockslides, and flows along steep slopes, were triggered by the long-duration horizontal and vertical accelerations during the earthquake. The landslides are most numerous in a narrow belt along the southeast coast of Kodiak Island and the nearby offshore islands. Their abundance appears to be related to an area underlain predominantly by Tertiary rocks.\n\nTemporary and permanent changes of level occurred after the earthquake in some wells, lakes, and streams throughout the area; ice was cracked, and the salinity of a few wells increased. Permanent change of water level at some localities appears to be related to readjustments of fracture porosity by earthquake-induced movements of bedrock blocks. Increased salinity of wells in coastal areas resulted from encroachment of seawater into aquifiers after subsidence during the earthquake, and to flooding of watersheds by seismic sea waves.\n\nVertical displacements, both downward and upward, occurred throughout the area as a result of crustal warping along a northeast-trending axis. Most of Kodiak and all of Afognak, Shuyak, and adjacent islands are within a regional zone of subsidence whose trough plunges gently northeastward and approximately coincides with the mountainous backbone of Kodiak Island. Subsidence in excess of 6 feet occurred throughout the northern part of the zone-a maximum subsidence of 6½ feet having occurred on Marmot and, eastern Afognak Islands. Southeast of the axis of tectonic tilting, uplift of at least 2lh feet occurred in a narrow zone that includes most of the southeasterly capes of Kodiak Island, the southeastern half of Sitkalidak Island, and Sitkinak Island. The uplift is inferred to extend offshore over much or all of the continental shelf adjacent to the Kodiak group of islands. Within the affected area, tectonic subsidence, which was locally augmented by surficial subsidence of unconsolidated. deposits, caused widespread inundation of shorelines and attendant damage to intertidal organisms, nearshore terrestrial vegetation, and salmon-spawning areas.\n\nThe most devastating effect of the earthquake on Kodiak Island and nearby islands resulted from seismic sea waves that probably originated along a linear zone of differential uplift in the Gulf of Alaska. A train of at least seven seismic sea waves, having initial periods of 50–55 minutes, struck along all the southeast coast of the island group from 38 to 63 minutes after the earthquake. The southeast shores were repeatedly washed by destructive waves having runup heights along exposed coasts of perhaps as much as 40 feet above existing tide level, and of 8–20 feet along protected shores. Runup heights of the waves were much less on the northwest and southwest sides of the islands, and no wave damage was incurred there. Locally, high-velocity currents that accompanied the waves caused intense erosion and redistribution of unconsolidated natural and artificial shore deposits and of shallow sea-floor deposits.\n\nThe Alaska earthquake was the greatest natural catastrophe to befall the Kodiak Island area in historic time. The combination of seismic shock and the earthquake-related tectonic deformation and seismic sea waves took 18 lives, destroyed property worth about $45 million, and resulted in estimated losses of income to the fishing industry of an additional $5 million.\n\nMost of the damage and all of the loss of life were directly attributable to the seismic sea waves that crippled the city of Kodiak, wiped out the village of Kaguyak, and destroyed most of the village of Old Harbor and parts of the villages of Afognak and Uzinki. Bridges and segments of the highways in the vicinity of the city of Kodiak were washed out, and parts of the Kodiak Naval Station were inundated and damaged. Especially serious to all the damaged communities was the loss of fishing boats, seafood processing plants, and other waterfront installations, which had been the mainstay of the economy.\n\nAdditional heavy losses resulted from the combined regional tectonic and local surficial subsidence that occurred during the earthquake. Widespread shoreline flooding by high tides necessitated raising, protecting, or removing many installations otherwise undamaged by the earthquake or waves.\n\nStructural damage attributable to seismic shock during the earthquake was relatively light and was restricted to areas underlain by saturated unconsolidated deposits. The chief structural failure in the area as a result of shaking was the collapse of part of a cannery built on saturated beach deposits that were partially liquefied during the earthquake. Minor structural damage resulted from differential settlement and cracking of the ground on natural granular deposits and artificial fills. The overwhelming majority of structures are constructed on indurated bedrock; none of these sustained damage other than small losses resulting from shifting about and breakage of their contents.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Regional effects (Professional Paper 543)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp543D","usgsCitation":"Plafker, G., and Kachadoorian, R., 1966, Geologic effects of the March 1964 earthquake and associated seismic sea waves on Kodiak and nearby islands, Alaska: U.S. Geological Survey Professional Paper 543, vi, 46 p., https://doi.org/10.3133/pp543D.","productDescription":"vi, 46 p.","numberOfPages":"58","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":277742,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp543D.gif"},{"id":65810,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0543d/pp543d_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396126,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_99029.htm"},{"id":277741,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0543d/index.html"}],"country":"United States","state":"Alaska","otherGeospatial":"Afognak Island, Kodiak Island, Marmot Island, Rasberry Island, Shuyak Island, Sitkalidak Island, Sitkinak Island, Spruce Island, Tugidak Island, Uganik Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155,\n              56.3778\n            ],\n            [\n              -151.6917,\n              56.3778\n            ],\n            [\n              -151.6917,\n              58.6444\n            ],\n            [\n              -155,\n              58.6444\n            ],\n            [\n              -155,\n              56.3778\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a633d","contributors":{"authors":[{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":220538,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kachadoorian, Reuben","contributorId":24336,"corporation":false,"usgs":true,"family":"Kachadoorian","given":"Reuben","email":"","affiliations":[],"preferred":false,"id":220539,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40870,"text":"ofr66101 - 1966 - Preliminary geologic map and coal deposits of the northeast quarter of the Gunsight Butte quadrangle, Kane County, Utah","interactions":[{"subject":{"id":40870,"text":"ofr66101 - 1966 - Preliminary geologic map and coal deposits of the northeast quarter of the Gunsight Butte quadrangle, Kane County, Utah","indexId":"ofr66101","publicationYear":"1966","noYear":false,"title":"Preliminary geologic map and coal deposits of the northeast quarter of the Gunsight Butte quadrangle, Kane County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70046202,"text":"70046202 - 1967 - Preliminary geologic map and coal deposits of the northeast quarter of the Gunsight Butte quadrangle, Kane County, Utah","indexId":"70046202","publicationYear":"1967","noYear":false,"title":"Preliminary geologic map and coal deposits of the northeast quarter of the Gunsight Butte quadrangle, Kane County, Utah"},"id":1}],"supersededBy":{"id":70046202,"text":"70046202 - 1967 - Preliminary geologic map and coal deposits of the northeast quarter of the Gunsight Butte quadrangle, Kane County, Utah","indexId":"70046202","publicationYear":"1967","noYear":false,"title":"Preliminary geologic map and coal deposits of the northeast quarter of the Gunsight Butte quadrangle, Kane County, Utah"},"lastModifiedDate":"2013-05-30T15:01:06","indexId":"ofr66101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-101","title":"Preliminary geologic map and coal deposits of the northeast quarter of the Gunsight Butte quadrangle, Kane County, Utah","language":"ENGLISH","doi":"10.3133/ofr66101","usgsCitation":"Peterson, F., and Horton, G., 1966, Preliminary geologic map and coal deposits of the northeast quarter of the Gunsight Butte quadrangle, Kane County, Utah: U.S. Geological Survey Open-File Report 66-101, 1 map + 1 data sheet, https://doi.org/10.3133/ofr66101.","productDescription":"1 map + 1 data sheet","costCenters":[],"links":[{"id":106363,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8117.htm","linkFileType":{"id":5,"text":"html"},"description":"8117"},{"id":170813,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c2dd","contributors":{"authors":[{"text":"Peterson, Fred fpeterson@usgs.gov","contributorId":1309,"corporation":false,"usgs":true,"family":"Peterson","given":"Fred","email":"fpeterson@usgs.gov","affiliations":[],"preferred":true,"id":224076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Horton, G.W.","contributorId":6321,"corporation":false,"usgs":true,"family":"Horton","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":224077,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24349,"text":"ofr67189 - 1966 - A preliminary evaluation of airborne and spaceborne remote sensing data for hydrologic uses","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"ofr67189","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"67-189","title":"A preliminary evaluation of airborne and spaceborne remote sensing data for hydrologic uses","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr67189","issn":"0094-9140","usgsCitation":"Robinove, C., 1966, A preliminary evaluation of airborne and spaceborne remote sensing data for hydrologic uses: U.S. Geological Survey Open-File Report 67-189, 1 v. 5 p.  ;28 cm., https://doi.org/10.3133/ofr67189.","productDescription":"1 v. 5 p.  ;28 cm.","costCenters":[],"links":[{"id":156767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6aad3f","contributors":{"authors":[{"text":"Robinove, C.J.","contributorId":68778,"corporation":false,"usgs":true,"family":"Robinove","given":"C.J.","affiliations":[],"preferred":false,"id":191736,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42737,"text":"ofr6628 - 1966 - Preliminary geologic map of the Mount Wrightson quadrangle, Santa Cruz and Pima Counties, Arizona","interactions":[{"subject":{"id":42737,"text":"ofr6628 - 1966 - Preliminary geologic map of the Mount Wrightson quadrangle, Santa Cruz and Pima Counties, Arizona","indexId":"ofr6628","publicationYear":"1966","noYear":false,"title":"Preliminary geologic map of the Mount Wrightson quadrangle, Santa Cruz and Pima Counties, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":65149,"text":"i614 - 1971 - Geologic map of the Mount Wrightson Quadrangle, southeast of Tucson, Santa Cruz, and Pima counties, Arizona","indexId":"i614","publicationYear":"1971","noYear":false,"title":"Geologic map of the Mount Wrightson Quadrangle, southeast of Tucson, Santa Cruz, and Pima counties, Arizona"},"id":1}],"supersededBy":{"id":65149,"text":"i614 - 1971 - Geologic map of the Mount Wrightson Quadrangle, southeast of Tucson, Santa Cruz, and Pima counties, Arizona","indexId":"i614","publicationYear":"1971","noYear":false,"title":"Geologic map of the Mount Wrightson Quadrangle, southeast of Tucson, Santa Cruz, and Pima counties, Arizona"},"lastModifiedDate":"2012-02-02T00:11:08","indexId":"ofr6628","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-28","title":"Preliminary geologic map of the Mount Wrightson quadrangle, Santa Cruz and Pima Counties, Arizona","language":"ENGLISH","doi":"10.3133/ofr6628","usgsCitation":"Drewes, H., 1966, Preliminary geologic map of the Mount Wrightson quadrangle, Santa Cruz and Pima Counties, Arizona: U.S. Geological Survey Open-File Report 66-28, 1 map, https://doi.org/10.3133/ofr6628.","productDescription":"1 map","costCenters":[],"links":[{"id":106374,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8134.htm","linkFileType":{"id":5,"text":"html"},"description":"8134"},{"id":176387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae29","contributors":{"authors":[{"text":"Drewes, Harald","contributorId":52567,"corporation":false,"usgs":true,"family":"Drewes","given":"Harald","affiliations":[],"preferred":false,"id":227030,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2183,"text":"wsp1613F - 1966 - Salt-water encroachment in southern Nassau and southeastern Queens Counties, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1613F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1613","chapter":"F","title":"Salt-water encroachment in southern Nassau and southeastern Queens Counties, Long Island, New York","docAbstract":"Test drilling, extraction of water from cores, electric logging, water sampling, and water-level measurements from 1958 to 1961 provided a suitable basis for a substantial refinement in the definition of the positions, chloride concentrations, and rates of movement of salty water in the intermediate and deep deposits of southern Nassau County and southeastern Queens County. \r\n\r\nFilter-press, centrifugal, and dilution methods were used to extract water from cores for chloride analysis at the test-drilling sites. Chloride analysis of water extracted by these methods, chloride analyses of water from wells, and the interpretation of electric logs helped to define the chloride content of the salty water. New concepts of environmental-water head and zerovels, developed during the investigation, proved useful for defining hydraulic gradients and ratee of flow in ground water of variable density in a vertical direction and in horizontal and inclined planes, respectively. Hydraulic gradients in and between fresh and salty water were determined from water levels from data at individual and multiple-observation wells. \r\n\r\nSalty ground water occurs in southern Nassau and southeastern Queens Counties as three wedgelike extensions that project landward in unconsolidated deposits from a main body of salty water that lies seaward of the barrier beaches in Nassau County and of Jamaica Bay in Queens County. Salty water occurs not only in permeable deposits but also in the shallow and deep clay deposits. The highest chloride content of the salty ground water in the main body and the wedges is about 16,000 ppm, which is about 1,000 to 2,000 ppm less than the chloride content of ocean water. \r\n\r\nThe shallow salty water in the Pleistocene and Recent deposits is connected freely with the bays, tidal estuaries, and ocean. The intermediate wedge is found only in the southwestern part of Nassau County in the upper part of the Magothy (?) Formation, in the Jamneco Gravel, and in the overlying clay deposits. It extends from the seaward areas inland about 2 miles into Island Park. The deep wedge extends into southeastern Queens County and southern Nassau County principally in the deeper parts of the Magothy (?) Formation and in the underlying clay member of the Raritan Formation. The leading edge of the deep wedge is at the base of the Magothy (?) Formation. This edge is apparently at the shoreline east of Lido Beach and extends inland about 4 miles to Woodmere and about 7 miles to South Ozone Park. Zones of diffusion as much as 6 miles wide and about 500 feet thick were delineated in the frontal part of the salty-water wedges. These thick and broad zones of diffusion were probably formed during the past 1,000 or more years in heterogeneous unconsolidated deposits by long- and short-term changes in sea level and in fresh-water outflow to the sea and by dispersion caused by the movements of the water and its salt mass. Changes in sea level and fresh-water outflow together produced appreciable advances and recessions of the salt-water front. The chemical compositions of the diffused water in all wedges are modified to some extent by base exchange and other physical and chemical processes and also by diffusion. \r\n\r\nThe intermediate wedge of salty water is moving landward at a rate of less than 20 feet a year in the vicinity of Island Park and, thus, has moved less than 1,000 feet since 1900. The leading edge of the deep wedge has advanced landward at about 300 feet a :ear in Woodmere in southwestern Nassau County and about 160 feet a year at South Ozone Park in southeastern Queens County, principally under the influence of local withdrawals near the toe of the wedge. Between Hewlett and Lido Beach, the deep wedge is moving inland at the rate of about 10 feet a year under the influence of regional withdrawals in inland areas. Regional encroachment of the deep wedge is apparently retarded appreciably by cyclic flow, that is, by the return seaward in the upper","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1613F","usgsCitation":"Lusczynski, N., and Swarzenski, W.V., 1966, Salt-water encroachment in southern Nassau and southeastern Queens Counties, Long Island, New York: U.S. Geological Survey Water Supply Paper 1613, iv, 76 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1613F.","productDescription":"iv, 76 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1613f/report-thumb.jpg"},{"id":27807,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27808,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27809,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613f/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27810,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613f/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27811,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613f/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27812,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1613f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c894","contributors":{"authors":[{"text":"Lusczynski, N.J.","contributorId":10779,"corporation":false,"usgs":true,"family":"Lusczynski","given":"N.J.","affiliations":[],"preferred":false,"id":144787,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swarzenski, Wolfgang V.","contributorId":30213,"corporation":false,"usgs":true,"family":"Swarzenski","given":"Wolfgang","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":144788,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40715,"text":"ofr66155 - 1966 - Flood-frequency of streams in Jackson, Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:10:50","indexId":"ofr66155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-155","title":"Flood-frequency of streams in Jackson, Mississippi","language":"ENGLISH","doi":"10.3133/ofr66155","usgsCitation":"Wilson, K., 1966, Flood-frequency of streams in Jackson, Mississippi: U.S. Geological Survey Open-File Report 66-155, 6 p., https://doi.org/10.3133/ofr66155.","productDescription":"6 p.","costCenters":[],"links":[{"id":171205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6fc8","contributors":{"authors":[{"text":"Wilson, K. V.","contributorId":51715,"corporation":false,"usgs":true,"family":"Wilson","given":"K. V.","affiliations":[],"preferred":false,"id":223843,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40711,"text":"ofr66157 - 1966 - Effect of treated effluent diversion on Yahara River flow, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-13T12:32:32","indexId":"ofr66157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-157","title":"Effect of treated effluent diversion on Yahara River flow, Wisconsin","docAbstract":"<p>Before December 1958 the treated sewage effluent from the Madison, Wisconsin, metropolitan area was discharged into the Yahara River at the north end of Lake Waubesa, which is upstream from the USGS gaging station on the Yahara River near McFarland, Wis. Since December 1958 the effluent has been diverted southward from the sewage treatment plant into Badfish Creek and enters the lower reach of Yahara River, thus byrpassing the gaging station. The purpose of this report is to demonstrate the effect that this diversion seems to have on the flow of the Yahara River near McFarland. Indirectly, it also demonstrates the effect on streamflow of withdrawing ground water for use in the Madison metropolitan area since the treated effluent is primarily the major portion of the used ground water.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr66157","usgsCitation":"Young, K., 1966, Effect of treated effluent diversion on Yahara River flow, Wisconsin: U.S. Geological Survey Open-File Report 66-157, 23 p., https://doi.org/10.3133/ofr66157.","productDescription":"23 p.","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":98243,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0157/report.pdf","size":"1509","linkFileType":{"id":1,"text":"pdf"}},{"id":171098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0157/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Yahara River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.36965942382812,\n              43.3101903843356\n            ],\n            [\n              -89.55230712890624,\n              43.17814279946058\n            ],\n            [\n              -89.65805053710938,\n              43.08995208151042\n            ],\n            [\n              -89.44244384765625,\n              42.943355168255806\n            ],\n            [\n              -89.25979614257812,\n              42.898100636939276\n            ],\n            [\n              -89.22821044921875,\n              42.819580715795915\n            ],\n            [\n              -89.15817260742188,\n              42.78129125156277\n            ],\n            [\n              -89.11148071289062,\n              42.78431496548022\n            ],\n            [\n              -89.07852172851562,\n              42.790361950280925\n            ],\n            [\n              -89.0716552734375,\n              42.81353658623225\n            ],\n            [\n              -89.0936279296875,\n              42.89105805581562\n            ],\n            [\n              -89.17739868164062,\n              42.99761672705504\n            ],\n            [\n              -89.32159423828125,\n              43.17513839170044\n            ],\n            [\n              -89.36141967773438,\n              43.26020603533185\n            ],\n            [\n              -89.36965942382812,\n              43.3101903843356\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62543f","contributors":{"authors":[{"text":"Young, K.B.","contributorId":77997,"corporation":false,"usgs":true,"family":"Young","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":223836,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41475,"text":"ofr6636 - 1966 - Precambrian geology of Iron Mountain SW quadrangle, Florence County, Wisconsin","interactions":[{"subject":{"id":41475,"text":"ofr6636 - 1966 - Precambrian geology of Iron Mountain SW quadrangle, Florence County, Wisconsin","indexId":"ofr6636","publicationYear":"1966","noYear":false,"title":"Precambrian geology of Iron Mountain SW quadrangle, Florence County, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":5849,"text":"pp633 - 1971 - Geology of the Florence area, Wisconsin and Michigan","indexId":"pp633","publicationYear":"1971","noYear":false,"title":"Geology of the Florence area, Wisconsin and Michigan"},"id":1}],"supersededBy":{"id":5849,"text":"pp633 - 1971 - Geology of the Florence area, Wisconsin and Michigan","indexId":"pp633","publicationYear":"1971","noYear":false,"title":"Geology of the Florence area, Wisconsin and Michigan"},"lastModifiedDate":"2012-02-02T00:10:53","indexId":"ofr6636","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-36","title":"Precambrian geology of Iron Mountain SW quadrangle, Florence County, Wisconsin","language":"ENGLISH","doi":"10.3133/ofr6636","usgsCitation":"Dutton, C.E., and Emerick, W., 1966, Precambrian geology of Iron Mountain SW quadrangle, Florence County, Wisconsin: U.S. Geological Survey Open-File Report 66-36, 1 map., https://doi.org/10.3133/ofr6636.","productDescription":"1 map.","costCenters":[],"links":[{"id":170623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680fd5","contributors":{"authors":[{"text":"Dutton, Carl E.","contributorId":27418,"corporation":false,"usgs":true,"family":"Dutton","given":"Carl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":225099,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emerick, W.L.","contributorId":64668,"corporation":false,"usgs":true,"family":"Emerick","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":225100,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":3037,"text":"wsp1610D - 1966 - Waterpower resources and reconnaissance geology of sites in the Alsea River basin, Oregon","interactions":[],"lastModifiedDate":"2022-05-06T21:25:35.386662","indexId":"wsp1610D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1610","chapter":"D","title":"Waterpower resources and reconnaissance geology of sites in the Alsea River basin, Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1610D","usgsCitation":"Young, L.L., Neal, D.W., and Gaskill, D.L., 1966, Waterpower resources and reconnaissance geology of sites in the Alsea River basin, Oregon: U.S. Geological Survey Water Supply Paper 1610, Report: iv, 45 p.; 2 Plates: 21.00 × 19.21 inches and 19.00 × 20.82 inches, https://doi.org/10.3133/wsp1610D.","productDescription":"Report: iv, 45 p.; 2 Plates: 21.00 × 19.21 inches and 19.00 × 20.82 inches","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":400319,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24800.htm"},{"id":29875,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1610d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29874,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1610d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29876,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1610d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1610d/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"Oregon","otherGeospatial":"Alsea River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.802,\n              44.349\n            ],\n            [\n              -123.933,\n              44.349\n            ],\n            [\n              -123.933,\n              44.417\n            ],\n            [\n              -123.802,\n              44.417\n            ],\n            [\n              -123.802,\n              44.349\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f7517","contributors":{"authors":[{"text":"Young, Loyd L.","contributorId":14805,"corporation":false,"usgs":true,"family":"Young","given":"Loyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neal, D. W.","contributorId":76726,"corporation":false,"usgs":true,"family":"Neal","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":146190,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gaskill, David L.","contributorId":53369,"corporation":false,"usgs":true,"family":"Gaskill","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146189,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1994,"text":"wsp1532C - 1966 - Effects of agricultural conservation practices on the hydrology of Corey Creek basin, Pennsylvania, 1954-60","interactions":[],"lastModifiedDate":"2017-06-26T08:27:00","indexId":"wsp1532C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1532","chapter":"C","title":"Effects of agricultural conservation practices on the hydrology of Corey Creek basin, Pennsylvania, 1954-60","docAbstract":"Analyses of data collected from two small basins in northern Pennsylvania during the period May 1954 to September 1960 indicated that changes in land use and land treatment have affected suspended- sediment discharge from the basins. Extensive land use and land-treatment changes have taken place in the 12.2-square-mile Corey Creek study basin, whereas such changes in the 10.2-square-mile Elk Run basin, which is adjacent to the northeast, have been relatively slight. Elk Run basin, which is topographically and hydrologically similar to Corey Creek basin, was used as an external control for the Corey Creek basin study. \r\n\r\nMultiple-regression analysis showed that of all the variables, runoff correlated most highly with the sediment yield of each basin. \r\n\r\nSurveys at selected cross-sections of the two streams indicated that most channel changes were in the banks rather than in the bed. At points where the stream channel slope was greater than 70 feet per mile, the average annual change in cross-sectional area at the measured ranges was less than +--2.5 square feet. Filling of the stream channel occurred where the slope was 70 feet per mile or less, and such filling was greater in Corey Creek than in Elk Run. \r\n\r\nTrend analyses of data from both basins indicated no persistent changers in quantity of runoff, precipitation, or runoff intensity (peakedness), although similar analyses indicated significant changes in the rate of suspended-sediment discharge from both basins. During the period September 1957 to September 1960, sediment discharge from Corey Creek basin decreased by 11 percent relative to the sediment discharge from Elk Run. All, or most, of this decrease was the result of a decrease in sediment discharge during the May to October growing seasons. No significant trends were detected in data collected d-ring the November to April dormant season. \r\n\r\nA factor, termed the relative erosion potential, was formulated for evaluating the effects of changes in the hydrologic cover conditions. This factor was adjusted for- the effects of diversion terrace construction in the Corey Creek basin. A rank correlation test of the adjusted relative erosion potential versus the growing season Corey Creek-Elk Run suspended-sediment discharge ratio resulted in a correlation coefficient, r=0.71, significant at the 3 percent level. The least-squares regression equation derived from the .same data. was Y=0.276 X - 6.89. \r\n\r\nwhere Y was the Corey Creek-Elk Run sediment-discharge ratio and X was the adjusted relative erosion potential. The correlation coefficient was 0.65. significant at the 12 percent level. Standard error of estimate was 0.44. or about ?20 percent of the observed variation in the sediment-discharge ratio.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1532C","usgsCitation":"Jones, B.L., 1966, Effects of agricultural conservation practices on the hydrology of Corey Creek basin, Pennsylvania, 1954-60: U.S. Geological Survey Water Supply Paper 1532, v, 55 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1532C.","productDescription":"v, 55 p. :ill. ;24 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":27395,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532c/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624b61","contributors":{"authors":[{"text":"Jones, Benjamin L.","contributorId":78313,"corporation":false,"usgs":true,"family":"Jones","given":"Benjamin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144491,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41472,"text":"ofr6637 - 1966 - Precambrian geology of Florence East quadrangle, Florence County, Wisconsin, and Iron County, Michigan","interactions":[{"subject":{"id":41472,"text":"ofr6637 - 1966 - Precambrian geology of Florence East quadrangle, Florence County, Wisconsin, and Iron County, Michigan","indexId":"ofr6637","publicationYear":"1966","noYear":false,"title":"Precambrian geology of Florence East quadrangle, Florence County, Wisconsin, and Iron County, Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":5849,"text":"pp633 - 1971 - Geology of the Florence area, Wisconsin and Michigan","indexId":"pp633","publicationYear":"1971","noYear":false,"title":"Geology of the Florence area, Wisconsin and Michigan"},"id":1}],"supersededBy":{"id":5849,"text":"pp633 - 1971 - Geology of the Florence area, Wisconsin and Michigan","indexId":"pp633","publicationYear":"1971","noYear":false,"title":"Geology of the Florence area, Wisconsin and Michigan"},"lastModifiedDate":"2019-11-22T14:46:34","indexId":"ofr6637","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-37","title":"Precambrian geology of Florence East quadrangle, Florence County, Wisconsin, and Iron County, Michigan","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr6637","usgsCitation":"Dutton, C.E., James, H.L., Johnson, R.W., and Wier, K.L., 1966, Precambrian geology of Florence East quadrangle, Florence County, Wisconsin, and Iron County, Michigan: U.S. Geological Survey Open-File Report 66-37, 2 Plates: 33.86 x 49.58 inches and 26.07 x 20.82 inches, https://doi.org/10.3133/ofr6637.","productDescription":"2 Plates: 33.86 x 49.58 inches and 26.07 x 20.82 inches","costCenters":[],"links":[{"id":369489,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0037/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170620,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0037/report-thumb.jpg"},{"id":369490,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0037/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan, Wisconsin","county":"Iron County, Florence County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.28475952148438,\n              45.90052165380744\n            ],\n            [\n              -88.16802978515625,\n              45.90052165380744\n            ],\n            [\n              -88.16802978515625,\n              45.9683336020637\n            ],\n            [\n              -88.28475952148438,\n              45.9683336020637\n            ],\n            [\n              -88.28475952148438,\n              45.90052165380744\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db6809d5","contributors":{"authors":[{"text":"Dutton, Carl E.","contributorId":27418,"corporation":false,"usgs":true,"family":"Dutton","given":"Carl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":225091,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"James, H. L.","contributorId":96732,"corporation":false,"usgs":true,"family":"James","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":225092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, R. W. Jr.","contributorId":18331,"corporation":false,"usgs":true,"family":"Johnson","given":"R.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":225090,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wier, K. L.","contributorId":106864,"corporation":false,"usgs":true,"family":"Wier","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":225093,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2565,"text":"wsp1767 - 1966 - Delaware water","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"wsp1767","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1767","title":"Delaware water","language":"ENGLISH","publisher":"U. S. Dept of the Interior, Geological Survey; for sale by the Superintendent of Documents, U.S. Govt. Print. Off.,","doi":"10.3133/wsp1767","usgsCitation":"Rasmussen, W., Odell, J.W., and Beamer, N.H., 1966, Delaware water: U.S. Geological Survey Water Supply Paper 1767, vii, 106 p. :illus. (part col.) maps (part col.) ;24 cm., https://doi.org/10.3133/wsp1767.","productDescription":"vii, 106 p. :illus. (part col.) maps (part col.) ;24 cm.","costCenters":[],"links":[{"id":138584,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1767/report-thumb.jpg"},{"id":28831,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1767/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db672361","contributors":{"authors":[{"text":"Rasmussen, William Charles","contributorId":12021,"corporation":false,"usgs":true,"family":"Rasmussen","given":"William Charles","affiliations":[],"preferred":false,"id":145407,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Odell, John W.","contributorId":100364,"corporation":false,"usgs":true,"family":"Odell","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145409,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beamer, Norman Howard","contributorId":43738,"corporation":false,"usgs":true,"family":"Beamer","given":"Norman","email":"","middleInitial":"Howard","affiliations":[],"preferred":false,"id":145408,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23326,"text":"ofr6661 - 1966 - Floods of November and December 1965 in southern California","interactions":[],"lastModifiedDate":"2019-03-08T12:23:23","indexId":"ofr6661","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-61","title":"Floods of November and December 1965 in southern California","docAbstract":"<p>Severe flooding occurred in southern California in late November and late December 1965 as a result of three heavy storms. Rain occurred on most days during the period November 13-26 and December 28-31, with major amounts distributed in three periods: November 13-19, 21-26, and December 28-31. More than 12 inches of precipitation was reported at Mount Baldy and Big Bear Lake on November 23, 1965; and more than 15 inches was reported at Mount Baldy on December 29, 1965.</p><p>Peak discharges at streamflow stations were generally the highest since 1943. The Los Angeles River at Sepulveda Dam and the Santa Clara River at the Los Angeles-Ventura County line had peak discharges greater than those of March 1938, the highest previously known.</p><p>Eleven deaths were attributed to the storm and the resulting floods, and preliminary estimates indicate damage in excess of $11 million in the foothill and valley areas. Flood-control, water-conservation, and power-production reservoirs effected a substantial reduction in the magnitude of the floods in many areas and thus prevented more extensive damage.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6661","issn":"0094-9140","usgsCitation":"Hedman, E.R., and Pearson, E., 1966, Floods of November and December 1965 in southern California: U.S. Geological Survey Open-File Report 66-61, v, 90 p., https://doi.org/10.3133/ofr6661.","productDescription":"v, 90 p.","costCenters":[],"links":[{"id":156198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0061/report-thumb.jpg"},{"id":361895,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0061/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121,\n              32.5\n            ],\n            [\n              -116,\n              32.5\n            ],\n            [\n              -116,\n              35.75\n            ],\n            [\n              -121,\n              35.75\n            ],\n            [\n              -121,\n              32.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df91a","contributors":{"authors":[{"text":"Hedman, E. R.","contributorId":71527,"corporation":false,"usgs":true,"family":"Hedman","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":189909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearson, E.G.","contributorId":66295,"corporation":false,"usgs":true,"family":"Pearson","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":189908,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1043,"text":"wsp1819I - 1966 - Ground-water development in the high plains of Colorado, with a section on chemical quality of the ground water","interactions":[],"lastModifiedDate":"2023-01-12T22:18:35.442921","indexId":"wsp1819I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1819","chapter":"I","title":"Ground-water development in the high plains of Colorado, with a section on chemical quality of the ground water","docAbstract":"The High Plains of Colorado includes all or part of 11 counties and has an area of about 9,500 square miles. The land surface slopes eastward and in most areas is gently rolling owing to erosion by ephemeral streams. The Ogallala Formation, of Pliocene age, is the principal aquifer. In pierces it is overlain by dune sand, alluvium, or loess. The Ogallala is semiconsolidated and consists of sand, gravel, silt, clay, and caliche. \r\n\r\nThe Ogallala Formation is recharged by precipitation at a rate of about 0.85 inch per year. The water table slopes generally eastward. The major use of ground water is for irrigation. About 72,500 acre-feet of water was pumped from 428 wells to irrigate about 56,600 acres in 1962. Estimates of consumptive use made by the Blaney-Criddle method show that the optimum amount of water is being used to irrigate parts of the High Plains. At the end of the 1963 irrigation season, 525 irrigation wells each pumped more than 300 gallons per minute. Water levels decline as much as 10 feet in some places during the irrigation season but return almost to normal at the completion of pumping. By prorating transmissibility on the basis of lithologic descriptions from well logs, the average permeability of the Ogallala Formation in various places can be estimated. Most water from the Ogallala Formation in the High Plains is a calcium bicarbonate solution having a dissolved-solids content ranging from 100 to 600 parts per million. The water is generally hard; its calcium carbonate hardness ranges from 100 to 350 parts per million. Except for some ground water in the area south of the Cheyenne-Kiowa County line, the ground water analyzed was suitable for all uses.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1819I","usgsCitation":"Boettcher, A.J., and Brennan, R., 1966, Ground-water development in the high plains of Colorado, with a section on chemical quality of the ground water: U.S. Geological Survey Water Supply Paper 1819, Report: iv, 22 p.; 3 Plates: 30.50 x 29.00 inches or smaller, https://doi.org/10.3133/wsp1819I.","productDescription":"Report: iv, 22 p.; 3 Plates: 30.50 x 29.00 inches or smaller","costCenters":[],"links":[{"id":411813,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25027.htm","linkFileType":{"id":5,"text":"html"}},{"id":25700,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25699,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819i/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25698,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25697,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138008,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819i/report-thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -102.11372229864088,\n              40.977920576752354\n            ],\n            [\n              -104.87143967673825,\n              40.977920576752354\n            ],\n            [\n              -104.87143967673825,\n              37.00029750496559\n            ],\n            [\n              -102.11372229864088,\n              37.00029750496559\n            ],\n            [\n              -102.11372229864088,\n              40.977920576752354\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ced3","contributors":{"authors":[{"text":"Boettcher, Arnold J.","contributorId":93025,"corporation":false,"usgs":true,"family":"Boettcher","given":"Arnold","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":143081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brennan, Robert","contributorId":105695,"corporation":false,"usgs":true,"family":"Brennan","given":"Robert","email":"","affiliations":[],"preferred":false,"id":143082,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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