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,{"id":22334,"text":"ofr698 - 1969 - Water supplies for Coulee Dam National Recreation Area, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:03","indexId":"ofr698","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-8","title":"Water supplies for Coulee Dam National Recreation Area, Washington","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, Water Resources Division,","doi":"10.3133/ofr698","issn":"0094-9140","usgsCitation":"Anderson, H.W., 1969, Water supplies for Coulee Dam National Recreation Area, Washington: U.S. Geological Survey Open-File Report 69-8, vi, 141 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr698.","productDescription":"vi, 141 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":155970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f015d","contributors":{"authors":[{"text":"Anderson, H. W. Jr.","contributorId":11187,"corporation":false,"usgs":true,"family":"Anderson","given":"H.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":188057,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23083,"text":"ofr69100 - 1969 - Hydrologic conditions during 1967 in Dade County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:13","indexId":"ofr69100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-100","title":"Hydrologic conditions during 1967 in Dade County, Florida","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, Water Resources Division,","doi":"10.3133/ofr69100","issn":"0094-9140","usgsCitation":"Galliher, C., and Hull, J., 1969, Hydrologic conditions during 1967 in Dade County, Florida: U.S. Geological Survey Open-File Report 69-100, 48 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr69100.","productDescription":"48 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":156952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611604","contributors":{"authors":[{"text":"Galliher, C.F.","contributorId":19971,"corporation":false,"usgs":true,"family":"Galliher","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":189402,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hull, J.E.","contributorId":56264,"corporation":false,"usgs":true,"family":"Hull","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":189403,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23375,"text":"ofr69128 - 1969 - An appraisal of the ground-water resources of the Susquehanna River basin in New York State","interactions":[],"lastModifiedDate":"2012-02-02T00:08:13","indexId":"ofr69128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-128","title":"An appraisal of the ground-water resources of the Susquehanna River basin in New York State","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/ofr69128","issn":"0094-9140","usgsCitation":"Hollyday, E., 1969, An appraisal of the ground-water resources of the Susquehanna River basin in New York State: U.S. Geological Survey Open-File Report 69-128, 97 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr69128.","productDescription":"97 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0128/report-thumb.jpg"},{"id":52664,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0128/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52665,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0128/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685680","contributors":{"authors":[{"text":"Hollyday, E. F.","contributorId":95062,"corporation":false,"usgs":true,"family":"Hollyday","given":"E. F.","affiliations":[],"preferred":false,"id":190001,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12479,"text":"ofr6914 - 1969 - Foraminiferal zonation and carbonate facies of the Mississippian and Pennsylvanian Lisburne Group, central and eastern Brooks Range, Arctic Alaska","interactions":[{"subject":{"id":12479,"text":"ofr6914 - 1969 - Foraminiferal zonation and carbonate facies of the Mississippian and Pennsylvanian Lisburne Group, central and eastern Brooks Range, Arctic Alaska","indexId":"ofr6914","publicationYear":"1969","noYear":false,"title":"Foraminiferal zonation and carbonate facies of the Mississippian and Pennsylvanian Lisburne Group, central and eastern Brooks Range, Arctic Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70043189,"text":"70043189 - 1970 - Foraminiferal zonation and carbonate facies of Carboniferous (Mississippian and Pennsylvanian) Lisburne group, central and eastern Brooks range, Arctic Alaska","indexId":"70043189","publicationYear":"1970","noYear":false,"title":"Foraminiferal zonation and carbonate facies of Carboniferous (Mississippian and Pennsylvanian) Lisburne group, central and eastern Brooks range, Arctic Alaska"},"id":1}],"supersededBy":{"id":70043189,"text":"70043189 - 1970 - Foraminiferal zonation and carbonate facies of Carboniferous (Mississippian and Pennsylvanian) Lisburne group, central and eastern Brooks range, Arctic Alaska","indexId":"70043189","publicationYear":"1970","noYear":false,"title":"Foraminiferal zonation and carbonate facies of Carboniferous (Mississippian and Pennsylvanian) Lisburne group, central and eastern Brooks range, Arctic Alaska"},"lastModifiedDate":"2024-05-20T17:27:43.389365","indexId":"ofr6914","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-14","title":"Foraminiferal zonation and carbonate facies of the Mississippian and Pennsylvanian Lisburne Group, central and eastern Brooks Range, Arctic Alaska","docAbstract":"<p>The Lisburne Group carbonates of the central and eastern Brooks Range contain foraminiferal assemblages assigned to zones of Osage [late Tournaisian], Early Mississippian, to Atoka [early Moscovian], Middle Pennsylvanian age. 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,{"id":42230,"text":"ofr69138 - 1969 - Bouguer gravity map of the Cripple Creek mining district, Teller County, Colorado","interactions":[],"lastModifiedDate":"2025-07-28T17:27:56.500683","indexId":"ofr69138","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-138","title":"Bouguer gravity map of the Cripple Creek mining district, Teller County, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69138","usgsCitation":"Kleinkopf, M.D., and Peterson, D.L., 1969, Bouguer gravity map of the Cripple Creek mining district, Teller County, Colorado: U.S. Geological Survey Open-File Report 69-138, 1 Plate: 24.20 x 18.25 inches, https://doi.org/10.3133/ofr69138.","productDescription":"1 Plate: 24.20 x 18.25 inches","costCenters":[],"links":[{"id":493035,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8367.htm","linkFileType":{"id":5,"text":"html"}},{"id":79987,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0138/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168040,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"Colorado","county":"Teller County","otherGeospatial":"Cripple Creek mining district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -105.202,\n              38.812\n            ],\n            [\n              -105.202,\n              38.666\n            ],\n            [\n              -105.083,\n              38.666\n            ],\n            [\n              -105.083,\n              38.812\n            ],\n            [\n              -105.202,\n              38.812\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fcf33","contributors":{"authors":[{"text":"Kleinkopf, M. Dean","contributorId":37723,"corporation":false,"usgs":true,"family":"Kleinkopf","given":"M.","email":"","middleInitial":"Dean","affiliations":[],"preferred":false,"id":226135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, Donald L.","contributorId":28597,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":226134,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40925,"text":"ofr6922 - 1969 - Preliminary geologic map of the Black River quadrangle, east-central Alaska","interactions":[{"subject":{"id":40925,"text":"ofr6922 - 1969 - Preliminary geologic map of the Black River quadrangle, east-central Alaska","indexId":"ofr6922","publicationYear":"1969","noYear":false,"title":"Preliminary geologic map of the Black River quadrangle, east-central Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":64790,"text":"i601 - 1970 - Preliminary geologic map of the Black River quadrangle, east-central Alaska","indexId":"i601","publicationYear":"1970","noYear":false,"title":"Preliminary geologic map of the Black River quadrangle, east-central Alaska"},"id":1}],"supersededBy":{"id":64790,"text":"i601 - 1970 - Preliminary geologic map of the Black River quadrangle, east-central Alaska","indexId":"i601","publicationYear":"1970","noYear":false,"title":"Preliminary geologic map of the Black River quadrangle, east-central Alaska"},"lastModifiedDate":"2018-06-14T10:18:23","indexId":"ofr6922","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-22","title":"Preliminary geologic map of the Black River quadrangle, east-central Alaska","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6922","usgsCitation":"Brabb, E.E., and Churkin, M., 1969, Preliminary geologic map of the Black River quadrangle, east-central Alaska: U.S. Geological Survey Open-File Report 69-22, Map: 111.5 x 60.6 cm, https://doi.org/10.3133/ofr6922.","productDescription":"Map: 111.5 x 60.6 cm","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":171332,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":106442,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8400.htm","linkFileType":{"id":5,"text":"html"},"description":"8400"}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bcc5","contributors":{"authors":[{"text":"Brabb, Earl E.","contributorId":48939,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":224191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Churkin, Michael Jr.","contributorId":62566,"corporation":false,"usgs":true,"family":"Churkin","given":"Michael","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":738003,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12939,"text":"ofr6936 - 1969 - Recent surface movements in the Baldwin Hills, Los Angeles County, California","interactions":[{"subject":{"id":12939,"text":"ofr6936 - 1969 - Recent surface movements in the Baldwin Hills, Los Angeles County, California","indexId":"ofr6936","publicationYear":"1969","noYear":false,"title":"Recent surface movements in the Baldwin Hills, Los Angeles County, California"},"predicate":"SUPERSEDED_BY","object":{"id":5758,"text":"pp882 - 1976 - Recent surface movements in the Baldwin Hills, Los Angeles County, California","indexId":"pp882","publicationYear":"1976","noYear":false,"title":"Recent surface movements in the Baldwin Hills, Los Angeles County, California"},"id":1}],"supersededBy":{"id":5758,"text":"pp882 - 1976 - Recent surface movements in the Baldwin Hills, Los Angeles County, California","indexId":"pp882","publicationYear":"1976","noYear":false,"title":"Recent surface movements in the Baldwin Hills, Los Angeles County, California"},"lastModifiedDate":"2024-05-24T19:53:10.458712","indexId":"ofr6936","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-36","title":"Recent surface movements in the Baldwin Hills, Los Angeles County, California","docAbstract":"<p>The Baldwin Hills are located in the northwest part of the densely populated Los Angeles basin. They comprise one of several groups of isolated hills that extend along the northwest-trending Newport-Inglewood zone of folds and faults, a structural lineament identified with a series of very productive oil fields. In addition to being the site of the Inglewood oil field, these hills are the site of surface deformation that has been monitored for over 35 years. This record of deformation, which includes differential subsidence, horizontal displacements, and surface rupturing, forms one of the best documented examples of oilfield-associated surface deformation yet recognized. The deformation is described in detail, analyzed as to cause(s), and finally attributed largely or essentially entirely to the exploitation of the spatially-associated Inglewood oil field.</p><p>The Baldwin Hills are underlain by gently to moderately arched and conspicuously faulted Cenozoic sedimentary and volcanic rocks that overlie crystalline basement rocks at a depth of more than 10,000 feet. The Inglewood fault, a part of the northwest-trending Newport-Inglewood zone, diagonally transects the hills. Right-lateral displacements of 3,000-4,000 feet since middle or late Pliocene time and 1,500-2,000 feet during Quaternary time are indicated by offset structural and physio-graphic features; indications of vertical separations of up to about 200 feet during late Quaternary time occur locally.</p><p>Evidence of continuing deformation includes recognized seismicity and regional elevation changes. The M5-5 1/2 Inglewood earthquake of 1920, the largest local earthquake of record, is believed to have originated immediately southeast of the Baldwin Hills; it was apparently unassociated with surficial fault displacements. Leveling in and around the west and central Los Angeles basin has shown that lowland stations have been consistently subsiding, whereas foothill stations commonly have been rising. Several seemingly persistent basins of differential subsidence and a zone of positive movement, roughly coincident with the Newport-Inglewood zone, have also been identified in the northwest part of the basin.</p><p>A prominent, elliptically-shaped, northwest-trending subsidence bowl encompassing the northwest part of the Baldwin Hills, has been defined by repeated level circuits. Partial reconstruction of selected level circuits with respect to a common, relatively stable control point (Hollywood E-11), located on the edge of the subsidence bowl, has permitted evaluation of the subsidence since 1910 and 1911 at two points near the center of the bowl. Thus bench mark PBM 67 is estimated to have subsided approximately 4.324 feet between June 1910 and February 1963; and bench mark PBM 68 (the only bench mark within the subsidence bowl that was leveled prior to 1926 and has been repeatedly leveled since) subsided 3.846 feet between November 1911 and June 1962. Analysis of the available data indicates little if any elevation change at PBM 68 (or elsewhere throughout the Baldwin Hills-Inglewood area) associated with the Inglewood earthquake of 1920. Maximum subsidence of PBM 122 (which has remained very close to the center of subsidence since at . least 1950) between 1911 and 1963 is calculated to have been 5.67 feet.</p><p>Horizontal displacements (with respect to a north-south base line about 3 miles east of the hills) of six triangulation points within the subsidence bowl have been measured for various periods between 1934 and 1963. Displacements have been generally toward the center of subsidence and almost precisely perpendicular to the immediately adjacent isobases of equal elevation change. Maximum movement has been recorded at triangulation point Baldwin Aux, which was displaced 2.21 feet between 1934 and 1961; horizontal displacements of three additional points ranged from 0.95 foot to 1.85 feet between 1936 and 1961. Displacements of 0.10-0.29 foot were recorded at all six monuments during the period 1961-1963.</p><p>\"Earth cracks\" and surficial fault displacements were recognized in the Baldwin Hills at least as early as 1957. The cracks are relatively straight, generally continuous fractures confined to the structural block east of the Inglewood fault; they are concentrated in two areas centering on (1) the Baldwin Hills Reservoir and (2) the Stocker Street-LaBrea Avenue-Overhill Drive intersection. The cracks trend north to north-northeast and are nearly everywhere parallel to or coincident with minor faults and joints, and are generally orthogonal to radii emanating from the center of subsidence. Differential movement along the cracks has been almost entirely dip slip along steep to nearly vertical surfaces, and generally down-dropped toward the center of subsidence. Cumulative displacements have been as much as 6 or 7 inches. Rates of displacement have ranged widely, and the movement has generally occurred as creep or very small discrete jumps. A probable exception is the several inches of differential movement that is believed to have occurred along a crack through the floor of the Baldwin Hills Reservoir on or about December 14, 1963.</p><p>The contemporary surface movements are attributable to one or more of the following phenomena: (1). exploitation of the Inglewood oil field; (2) changes in the ground-water regimen; (3) compaction of sedimentary materials in response to surface loading; (4) tectonic activity.</p><p>The following considerations indicate that the differential subsidence is attributable largely or entirely to exploitation of the underlying Inglewood oil field: (1) the coincidence of the centers of the oil field, the producing structure, and the subsidence bowl; (2) the general correspondence between the pattern of subsidence and the outlines of the oil field; (3) the approximate coincidence between the initiation of production and the initiation of subsidence; (4) the generally linear relations between various measures of subsidence and liquid production from both the field as a whole and the exceptionally prolific Vickers zone in particular; (5) the sharp deceleration of subsidence in the eastern block of the field coincident with the initiation of full-scale water flooding there; (6) the many examples of oil fields In which both spatial and temporal associations between production and subsidence are recognized; (7) the many similarities of the subsidence-production relations in the Inglewood field to those in the Wilmington field, where the subsidence has been authoritatively attributed to oilfield&nbsp;operations; (8) the theoretical relation between subsidence or a tendency toward subsidence and increased effective pressure associated with underground fluid extraction.</p><p>Consideration of six possible explanations for the increasing rather than decreasing or constant rate of subsidence with respect to reservoir fluid pressure decline suggests that measured or calculated down-hole reservoir fluid pressure decline is non-representative of average or real fluid pressure decline away from producing wells. The near-linear relations between net-liquid production and subsidence are explained through analogy with a tightly confined artesian system of infinite areal extent, where production must derive from liquid expansion and/or reservoir compaction. Test data from compaction studies in two other oil fields yield estimates of ultimate compaction of the Vickers zone resulting from a total loss of fluid pressure; these estimates range over an order of magnitude. The best estimate, based on these data and considerations of late Cenozoic history in the Baldwin Hills area, is about 10 feet.</p><p>The centripetally-directed horizontal movements are considered attributable to exploitation of the Inglewood oil field on the basis of:<br>(1) their well-defined symmetrical and geometrical association with the differential subsidence; (2) the similarities between these associations and those developed in and around other subsiding oil fields; and (3) the mechanical compatibility of these movements with subsidence induced by the extraction of subsurface materials.</p><p>The earth cracks and surficial fault displacements are considered largely or entirely attributable to the exploitation of the Inglewood oil field on the basis of: (1) their spatial and temporal relations to both oil-field operations and the differential subsidence; (2) the similarities of these cracks and displacements to those generated in and around other oil fields and areas of subsurface materials extraction; and (3) surface strain patterns predicted from the measured vertical and horizontal surface movements. The cracks and displacements can i)e explained by an exploitation-based, elastic-rebound model which requires elastic compression of the sedimentary section in response to compaction-induced downdrag within those blocks around the periphery of the subsidence bowl. The measured displacements have been about one-quarter to one-half those predicted for a purely elastic system.</p><p>Analysis of: (1) the history of ground-water extraction within and around the Baldwin Hills; and (2) subsidence associated with water-level declines in sediments comparable with those in the Baldwin Hills, indicate that the surface movements can be no more than incidentally attributed to changes in ground-water conditions. Similarly, analysis of the history of natural and artificial changes in surface loading indicate that these movements are generally unassociated with changes in surface loading conditions.</p><p>Considerations of local geologic history and various tectonic associations indicate that it is very unlikely that the differential subsidence and horizontal movements are due to tectonic downwarping. There exists a far stronger prima facie argument for tectonic involvement in the earth cracking and associated fault displacements. This argument is disputed by; (1) the spatial and temporal relations of the earth cracks to, and their mechanical compatibility with, the nontectonic differential subsidence; (2) the absence of displacements on the Inglewood fault in conjunction with those along the conjugate earth cracks; (3) the probability that purely tectonic displaceMents would be characterized by oblique or strike slip; and (4) the absence of any clear temporal relation between crack growth and local seismicity, However, because as much as 10 percent of the local isobase gradient may be unexplained' by oil-field exploitation, a small fraction of this gradient, and thus the displacements among the southern group of cracks, may be attributable to tectonic activity. This fraction should have been insignificant in the presence of the strain pattern produced by nontectonic compaction of the underlying oil measures.</p><p>Because nearly all of the observed and measured surface movements can be fully explained as the products of oil-field operations, yet can be no more than incidentally attributed to changes in ground-water conditions, surface loading, or tectonic activity, we conclude that these movements are attributable largely or essentially entirely to the exploitation of the Inglewood oil field.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6936","usgsCitation":"Castle, R.O., and Yerkes, R.F., 1969, Recent surface movements in the Baldwin Hills, Los Angeles County, California: U.S. Geological Survey Open-File Report 69-36, xviii, 185 p., https://doi.org/10.3133/ofr6936.","productDescription":"xviii, 185 p.","costCenters":[],"links":[{"id":429278,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146998,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0036/report-thumb.jpg"}],"country":"United States","state":"California","county":"Los Angeles County","otherGeospatial":"Baldwin Hills","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.38187677397389,\n              34.0348739886972\n            ],\n            [\n              -118.38187677397389,\n              33.97553856602411\n            ],\n            [\n              -118.30144514525205,\n              33.97553856602411\n            ],\n            [\n              -118.30144514525205,\n              34.0348739886972\n            ],\n            [\n              -118.38187677397389,\n              34.0348739886972\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648569","contributors":{"authors":[{"text":"Castle, Robert O.","contributorId":22741,"corporation":false,"usgs":true,"family":"Castle","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":166993,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yerkes, R. F.","contributorId":24754,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":166994,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":55939,"text":"ofr69255 - 1969 - Environment mapping with spacecraft photography: a central Australian example","interactions":[],"lastModifiedDate":"2014-07-14T09:59:38","indexId":"ofr69255","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-255","title":"Environment mapping with spacecraft photography: a central Australian example","docAbstract":"No abstract available.","language":"English","publisher":"University of Kansas Dept. of Geography and Center for Research in Engineering Science","publisherLocation":"Lawrence, KS","doi":"10.3133/ofr69255","usgsCitation":"Simonett, D., Cochrane, G., Morain, S., and Egbert, D., 1969, Environment mapping with spacecraft photography: a central Australian example: U.S. Geological Survey Open-File Report 69-255, 32 p., https://doi.org/10.3133/ofr69255.","productDescription":"32 p.","numberOfPages":"32","costCenters":[],"links":[{"id":100419,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0255/report.pdf","size":"3336","linkFileType":{"id":1,"text":"pdf"}},{"id":184195,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0255/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025bd","contributors":{"authors":[{"text":"Simonett, D.S.","contributorId":102499,"corporation":false,"usgs":true,"family":"Simonett","given":"D.S.","affiliations":[],"preferred":false,"id":254532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cochrane, G.R.","contributorId":104002,"corporation":false,"usgs":true,"family":"Cochrane","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":254533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morain, S.A.","contributorId":9275,"corporation":false,"usgs":true,"family":"Morain","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":254530,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Egbert, D.E.","contributorId":56305,"corporation":false,"usgs":true,"family":"Egbert","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":254531,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":37446,"text":"ssrw123 - 1969 - Woodcock research and management programs 1967 and 1968","interactions":[],"lastModifiedDate":"2012-02-02T00:09:39","indexId":"ssrw123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"123","title":"Woodcock research and management programs 1967 and 1968","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Goudy, W.H., 1969, Woodcock research and management programs 1967 and 1968 (Updates and revises Special Scientific Report-Wildlife 101 (1967).): Special Scientific Report  - Wildlife 123, iv, 32 p.","productDescription":"iv, 32 p.","costCenters":[],"links":[{"id":112089,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924055486793?urlappend=%3Bseq=9"},{"id":165859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Updates and revises Special Scientific Report-Wildlife 101 (1967).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df8a2","contributors":{"authors":[{"text":"Goudy, William H. (compiler)","contributorId":58693,"corporation":false,"usgs":true,"family":"Goudy","given":"William","suffix":"(compiler)","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":218094,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55956,"text":"ofr69296 - 1969 - Compilation of hydrologic data, Honey Creek, Trinity River basin, Texas, 1966","interactions":[],"lastModifiedDate":"2021-12-23T15:26:11.192535","indexId":"ofr69296","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-296","title":"Compilation of hydrologic data, Honey Creek, Trinity River basin, Texas, 1966","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69296","collaboration":"Prepared in cooperation with Texas Water Development Board and Soil Conservation Service","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Compilation of hydrologic data, Honey Creek, Trinity River basin, Texas, 1966: U.S. Geological Survey Open-File Report 69-296, v, 125 p., https://doi.org/10.3133/ofr69296.","productDescription":"v, 125 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":393359,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0296/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0296/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Honey Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9c97","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":532421,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12930,"text":"ofr6935 - 1969 - Maps showing locations of holes drilled in 1952 to 1954 by U.S. Geological Survey, La Sal Creek area, Paradox district, Montrose County, Colorado","interactions":[],"lastModifiedDate":"2021-09-16T19:02:48.365613","indexId":"ofr6935","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-35","title":"Maps showing locations of holes drilled in 1952 to 1954 by U.S. Geological Survey, La Sal Creek area, Paradox district, Montrose County, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6935","usgsCitation":"Carter, W.D., and Gualtieri, J.L., 1969, Maps showing locations of holes drilled in 1952 to 1954 by U.S. Geological Survey, La Sal Creek area, Paradox district, Montrose County, Colorado: U.S. Geological Survey Open-File Report 69-35, Report: 3 p.; 4 Plates: 37.32 × 30.06 inches or smaller, https://doi.org/10.3133/ofr6935.","productDescription":"Report: 3 p.; 4 Plates: 37.32 × 30.06 inches or smaller","costCenters":[],"links":[{"id":41376,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0035/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":389357,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8432.htm"},{"id":41377,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0035/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41374,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0035/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0035/report-thumb.jpg"},{"id":41375,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0035/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41378,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","county":"Montrose County","otherGeospatial":"La Sal Creek area, Paradox district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.1236,\n              38.2931\n            ],\n            [\n              -109,\n              38.2931\n            ],\n            [\n              -109,\n              38.3667\n            ],\n            [\n              -109.1236,\n              38.3667\n            ],\n            [\n              -109.1236,\n              38.2931\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605be0","contributors":{"authors":[{"text":"Carter, William Douglas","contributorId":93892,"corporation":false,"usgs":true,"family":"Carter","given":"William","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":166975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gualtieri, James Louis","contributorId":46491,"corporation":false,"usgs":true,"family":"Gualtieri","given":"James","email":"","middleInitial":"Louis","affiliations":[],"preferred":false,"id":166974,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":55883,"text":"ofr691 - 1969 - Ground water in the Scotts Valley area, Santa Cruz County, California","interactions":[],"lastModifiedDate":"2018-06-04T12:06:57","indexId":"ofr691","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-1","title":"Ground water in the Scotts Valley area, Santa Cruz County, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr691","usgsCitation":"Akers, J.P., 1969, Ground water in the Scotts Valley area, Santa Cruz County, California: U.S. Geological Survey Open-File Report 69-1, 13 p., https://doi.org/10.3133/ofr691.","productDescription":"13 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":182228,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California","county":"Santa Cruz County","otherGeospatial":"Scotts Valley area","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d878","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":254413,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55931,"text":"ofr69227 - 1969 - Areas and use of water by phreatophytes in Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:12:22","indexId":"ofr69227","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-227","title":"Areas and use of water by phreatophytes in Nevada","language":"ENGLISH","doi":"10.3133/ofr69227","usgsCitation":"Robinson, T.W., 1969, Areas and use of water by phreatophytes in Nevada: U.S. Geological Survey Open-File Report 69-227, 25 p., https://doi.org/10.3133/ofr69227.","productDescription":"25 p.","costCenters":[],"links":[{"id":183956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673108","contributors":{"authors":[{"text":"Robinson, T. W.","contributorId":82285,"corporation":false,"usgs":true,"family":"Robinson","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":254510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12797,"text":"ofr6926 - 1969 - Isopach maps of upper Paleozoic and Mesozoic rocks, northern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:55","indexId":"ofr6926","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-26","title":"Isopach maps of upper Paleozoic and Mesozoic rocks, northern Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6926","usgsCitation":"Brosge, W.P., and Tailleur, I.L., 1969, Isopach maps of upper Paleozoic and Mesozoic rocks, northern Alaska: U.S. Geological Survey Open-File Report 69-26, 13 p. :11 maps ;27 cm., https://doi.org/10.3133/ofr6926.","productDescription":"13 p. :11 maps ;27 cm.","costCenters":[],"links":[{"id":146829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0026/report-thumb.jpg"},{"id":41207,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6670e6","contributors":{"authors":[{"text":"Brosge, William Peters","contributorId":40191,"corporation":false,"usgs":true,"family":"Brosge","given":"William","email":"","middleInitial":"Peters","affiliations":[],"preferred":false,"id":166729,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tailleur, Irvin L.","contributorId":105304,"corporation":false,"usgs":true,"family":"Tailleur","given":"Irvin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":166730,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13007,"text":"ofr6939 - 1969 - The talc, soapstone, and asbestos deposits of Massachusetts","interactions":[],"lastModifiedDate":"2025-07-28T20:31:43.140339","indexId":"ofr6939","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-39","title":"The talc, soapstone, and asbestos deposits of Massachusetts","docAbstract":"Several talc and soapstone deposits were worked in Massachusetts from about 1810 to 1922.  Most of these deposits are in the Chester Amphibolite, or in serpentine lenses in or adjacent to the amphibolite along a belt that extends north-south across the State from Rowe to West Granville; it appears to be a continuation of the Vermont talc belt.  The only deposits outside of this belt that have been worked are a talc and soapstone deposit in the north-west corner of Hinsdale and soapstone deposits on the east side of Soapstone Hill in the western part of Petersham.\r\n\r\nVery little asbestos has been produced in Massachusetts.  A small amount of anthophyllite asbestos was obtained from the deposit in Hinsdale, and from a deposit in southwestern Pelham.\r\n\r\nThe talc and soapstone deposits of Massachusetts were formed from serpentine and possibly from amphibolite, schist, and dolomitic limestone.  Those fromed from serpentine are mainly at the ends of the serpentine bodies, and those that appear to have been formed from amphibolite or schist are on the faults and folds.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6939","usgsCitation":"Chute, N.E., 1969, The talc, soapstone, and asbestos deposits of Massachusetts: U.S. Geological Survey Open-File Report 69-39, Report: iv, 42 p.; 8 Plates: 13.88 x 23.44 inches or smaller, https://doi.org/10.3133/ofr6939.","productDescription":"Report: iv, 42 p.; 8 Plates: 13.88 x 23.44 inches or smaller","costCenters":[],"links":[{"id":41470,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0039/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41469,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0039/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41468,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0039/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":493056,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8434.htm","linkFileType":{"id":5,"text":"html"}},{"id":41471,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0039/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41472,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0039/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41473,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41467,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0039/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41466,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0039/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41465,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0039/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146229,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0039/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.174,\n              42.746\n            ],\n            [\n              -73.174,\n              42.0610\n            ],\n            [\n              -72.186,\n              42.0610\n            ],\n            [\n              -72.186,\n              42.746\n            ],\n            [\n              -73.174,\n              42.746\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a50e6","contributors":{"authors":[{"text":"Chute, Newton Earl","contributorId":97119,"corporation":false,"usgs":true,"family":"Chute","given":"Newton","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":167124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37262,"text":"rp70 - 1969 - Recreational use patterns at Flaming Gorge Reservoir, 1963-65","interactions":[],"lastModifiedDate":"2016-11-09T11:22:07","indexId":"rp70","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"70","title":"Recreational use patterns at Flaming Gorge Reservoir, 1963-65","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Hewston, J.G., and Franklin, D.R., 1969, Recreational use patterns at Flaming Gorge Reservoir, 1963-65: Resource Publication 70, viii, 80 p.","productDescription":"viii, 80 p.","costCenters":[],"links":[{"id":162912,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca6e","contributors":{"authors":[{"text":"Hewston, John G.","contributorId":8523,"corporation":false,"usgs":true,"family":"Hewston","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":217757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Franklin, Donald R.","contributorId":78380,"corporation":false,"usgs":true,"family":"Franklin","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":217758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":37719,"text":"wl483 - 1969 - Wildlife imported into the United States in 1968.","interactions":[],"lastModifiedDate":"2012-02-02T00:10:02","indexId":"wl483","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"483","title":"Wildlife imported into the United States in 1968.","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Division Of Management And Enforcement, 1969, Wildlife imported into the United States in 1968. (Revises Wildlife Leaflet 480 (1968).): Wildlife Leaflet 483, 4 p.","productDescription":"4 p.","costCenters":[],"links":[{"id":162821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises Wildlife Leaflet 480 (1968).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3ed3","contributors":{"authors":[{"text":"Division Of Management And Enforcement","contributorId":127883,"corporation":true,"usgs":false,"organization":"Division Of Management And Enforcement","id":529684,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3796,"text":"cir630 - 1969 - Hydrogeologic information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and adjoining areas as related to underground waste disposal","interactions":[],"lastModifiedDate":"2022-09-02T21:59:54.813067","indexId":"cir630","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"630","title":"Hydrogeologic information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and adjoining areas as related to underground waste disposal","docAbstract":"<p>The Oklahoma Panhandle and adjacent areas in Texas, Kansas, Colorado, and New Mexico have prospered because of the development of supplies of fresh water and of oil and gas. The Ogallala and, in places, Cretaceous rocks produce fresh water for irrigation, public supply, and domestic and stock use through approximately 9,000 irrigation and public supply wells and a large but undetermined number of other wells. Disposal of oil-field brine and other wastes into the Glorieta Sandstone is of concern to many local residents because of the possibility of pollution of the overlying fresh-water aquifers, particularly the Ogallala Formation. Permits for 147 disposal wells into the Glorieta have been issued in this area. This report summarizes the data on geology, hydrology, and water development currently available to the U.S. Geological Survey. Geologic information indicates that, in the report area, the Glorieta Sandstone lies at depths ranging from about 500 to 1,600 feet below the base of the Ogallala Fox, nation. The rocks between those two formations are of relatively impermeable types, but solution and removal of salt has resulted in collapse of the rocks in some places. Collapse and fracturing of the rocks could result in increased vertical permeability. This might result in movement of brine under hydrostatic head from the Glorieta Sandstone into overlying fresh-water aquifers, in places where an upward hydraulic gradient exists or is created by an increase in pressure within the Glorieta. Abandoned or inadequately sealed boreholes also are possible conduits for such fluids. The mixing of water in the fresh-water aquifers with brines injected into the Glorieta is not known to have occurred anywhere in the report area, but the information available is not adequate to show positively whether or not this may have occurred locally. Much additional information on the stratigraphy and hydrology--particularly, data on the potentiometric surface of water in the Glorieta--needs to be collected and analyzed before conclusions can be drawn regarding the possibility of vertical movement of oil-field brines from the Glorieta to fresh-water aquifers above.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir630","usgsCitation":"Irwin, J.H., and Morton, R.B., 1969, Hydrogeologic information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and adjoining areas as related to underground waste disposal: U.S. Geological Survey Circular 630, Report: iii, 26 p.; 4 Plates: 41.62 x 21.27 inches or smaller, https://doi.org/10.3133/cir630.","productDescription":"Report: iii, 26 p.; 4 Plates: 41.62 x 21.27 inches or smaller","numberOfPages":"34","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311912,"rank":304,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":406196,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23973.htm","linkFileType":{"id":5,"text":"html"}},{"id":311911,"rank":303,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":30866,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0630/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":311910,"rank":302,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":124418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0630/report-thumb.jpg"},{"id":311909,"rank":301,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Kansas, New Mexico, Oklahoma, Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.388,\n              35.242\n            ],\n            [\n              -104.388,\n              38.25\n            ],\n            [\n              -99.25,\n              38.25\n            ],\n            [\n              -99.25,\n              35.242\n            ],\n            [\n              -104.388,\n              35.242\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627989","contributors":{"authors":[{"text":"Irwin, James Haskell","contributorId":56633,"corporation":false,"usgs":true,"family":"Irwin","given":"James","email":"","middleInitial":"Haskell","affiliations":[],"preferred":false,"id":147617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morton, Robert B.","contributorId":50899,"corporation":false,"usgs":true,"family":"Morton","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":147616,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44169,"text":"ofr69278 - 1969 - Surface distribution of selected elements around the Copper Canyon copper-gold-silver open pit mine, Lander County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"ofr69278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-278","title":"Surface distribution of selected elements around the Copper Canyon copper-gold-silver open pit mine, Lander County, Nevada","language":"ENGLISH","doi":"10.3133/ofr69278","usgsCitation":"Theodore, T., 1969, Surface distribution of selected elements around the Copper Canyon copper-gold-silver open pit mine, Lander County, Nevada: U.S. Geological Survey Open-File Report 69-278, 21 maps, https://doi.org/10.3133/ofr69278.","productDescription":"21 maps","costCenters":[],"links":[{"id":113807,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0278/plate-figure_01.pdf","size":"7938","linkFileType":{"id":1,"text":"pdf"}},{"id":113808,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0278/plate-figure_02_and_03.pdf","size":"1196","linkFileType":{"id":1,"text":"pdf"}},{"id":113809,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0278/plate-figure_04_and_05.pdf","size":"1106","linkFileType":{"id":1,"text":"pdf"}},{"id":113810,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0278/plate-figure_06_and_07.pdf","size":"1208","linkFileType":{"id":1,"text":"pdf"}},{"id":113811,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0278/plate-figure_08_and_09.pdf","size":"1197","linkFileType":{"id":1,"text":"pdf"}},{"id":113812,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0278/plate-figure_10_and_11.pdf","size":"1255","linkFileType":{"id":1,"text":"pdf"}},{"id":113813,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0278/plate-figure_12_and_13.pdf","size":"1209","linkFileType":{"id":1,"text":"pdf"}},{"id":113814,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0278/plate-figure_14_and_15.pdf","size":"1159","linkFileType":{"id":1,"text":"pdf"}},{"id":113815,"rank":419,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0278/plate-figure_16_and_17.pdf","size":"1304","linkFileType":{"id":1,"text":"pdf"}},{"id":113816,"rank":420,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0278/plate-figure_18_and_19.pdf","size":"1165","linkFileType":{"id":1,"text":"pdf"}},{"id":113817,"rank":421,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0278/plate-figure_20_and_21.pdf","size":"1312","linkFileType":{"id":1,"text":"pdf"}},{"id":161524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0278/report-thumb.jpg"},{"id":81563,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0278/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626c42","contributors":{"authors":[{"text":"Theodore, Ted G.","contributorId":57840,"corporation":false,"usgs":true,"family":"Theodore","given":"Ted G.","affiliations":[],"preferred":false,"id":229274,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3243,"text":"cir616 - 1969 - Sensor detection capabilities study","interactions":[],"lastModifiedDate":"2017-06-25T13:10:11","indexId":"cir616","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"616","title":"Sensor detection capabilities study","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir616","usgsCitation":"Wilson, J.E., 1969, Sensor detection capabilities study: U.S. Geological Survey Circular 616, iv, 26 p. :illus. ;26 cm., https://doi.org/10.3133/cir616.","productDescription":"iv, 26 p. :illus. ;26 cm.","costCenters":[],"links":[{"id":30239,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0616/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117774,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0616/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f78dd","contributors":{"authors":[{"text":"Wilson, John Emery 0000-0001-6752-4069 jtwilson@usgs.gov","orcid":"https://orcid.org/0000-0001-6752-4069","contributorId":25921,"corporation":false,"usgs":true,"family":"Wilson","given":"John","email":"jtwilson@usgs.gov","middleInitial":"Emery","affiliations":[],"preferred":false,"id":146499,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3244,"text":"cir529B - 1969 - Movement of a solute in the Potomac River estuary at Washington, D.C., at low inflow conditions","interactions":[],"lastModifiedDate":"2022-12-13T19:39:12.270831","indexId":"cir529B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"529","chapter":"B","title":"Movement of a solute in the Potomac River estuary at Washington, D.C., at low inflow conditions","docAbstract":"<p>The movement of a solute, as represented by a soluble fluorescent dye, was observed in the Potomac River estuary at Washington, D.C. The average net rate of downstream movement of the solute centroid was less than 0.6 mile per day. The movement of a solute is highly dependent on the nontidal inflow to the estuary. During the study, the average inflow was 900 cubic feet per second a very low value, equaled or exceeded 98 percent of the time. Using a storage equation, the average movement of a solute was estimated for nontidal inflow of 3,100 and 6,500 cubic feet per second; these inflows are equaled or exceeded 75 and 50 percent of the time, respectively. The study showed that tidal action was fairly efficient in dispersing the solute longitudinally. The solute, which was dumped 1,000 feet upstream from the 14th Street Bridge, was observed as far upstream as Roosevelt Island. A transient longitudinal dispersion coefficient at the end of 150 hours was determined to be 210 square feet per second. On the other hand, the lateral diffusion was a slow process and the lateral distribution of the solute was far from uniform at the end of 6½ days after the release.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir529B","usgsCitation":"Wilson, J.F., Cobb, E.D., and Yotsukura, N., 1969, Movement of a solute in the Potomac River estuary at Washington, D.C., at low inflow conditions: U.S. Geological Survey Circular 529, iii, 14 p., https://doi.org/10.3133/cir529B.","productDescription":"iii, 14 p.","costCenters":[],"links":[{"id":410382,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23901.htm","linkFileType":{"id":5,"text":"html"}},{"id":30240,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0529b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0529b/report-thumb.jpg"}],"country":"United States","state":"Washington D.C.","otherGeospatial":"Potomac River estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77.05946773907127,\n              38.8983597413571\n            ],\n            [\n              -77.05946773907127,\n              38.71400631838506\n            ],\n            [\n              -77.00136231593808,\n              38.71400631838506\n            ],\n            [\n              -77.00136231593808,\n              38.8983597413571\n            ],\n            [\n              -77.05946773907127,\n              38.8983597413571\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b480b","contributors":{"authors":[{"text":"Wilson, James F.","contributorId":84737,"corporation":false,"usgs":true,"family":"Wilson","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":146502,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cobb, Ernest D.","contributorId":25139,"corporation":false,"usgs":true,"family":"Cobb","given":"Ernest","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":146500,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yotsukura, Nobuhiro","contributorId":81884,"corporation":false,"usgs":true,"family":"Yotsukura","given":"Nobuhiro","email":"","affiliations":[],"preferred":false,"id":146501,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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