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,{"id":33130,"text":"b1235 - 1969 - Bibliography of North American geology, 1965","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"b1235","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1235","title":"Bibliography of North American geology, 1965","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1235","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Bibliography of North American geology, 1965: U.S. Geological Survey Bulletin 1235, 1144 p., https://doi.org/10.3133/b1235.","productDescription":"1144 p.","costCenters":[],"links":[{"id":247375,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1235/report.pdf","size":"55408","linkFileType":{"id":1,"text":"pdf"}},{"id":251822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1235/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db629489","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":529456,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34098,"text":"b1292 - 1969 - The Geologic Story of Mount Rainier","interactions":[],"lastModifiedDate":"2018-02-22T15:44:26","indexId":"b1292","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1292","title":"The Geologic Story of Mount Rainier","docAbstract":"<p>Ice-clad Mount Rainier, towering over the landscape of western Washington, ranks with Fuji-yama in Japan, Popocatepeti in Mexico, and Vesuvius in Italy among the great volcanoes of the world. At Mount Rainier, as at other inactive volcanoes, the ever-present possibility of renewed eruptions gives viewers a sense of anticipation, excitement, and apprehension not equaled by most other mountains. Even so, many of us cannot imagine the cataclysmic scale of the eruptions that were responsible for building the giant cone which now stands in silence. We accept the volcano as if it had always been there, and we appreciate only the beauty of its stark expanses of rock and ice, its flower-strewn alpine meadows, and its bordering evergreen forests.</p><p>Mount Rainier owes its scenic beauty to many features. The broad cone spreads out on top of a major mountain range - the Cascades. The volcano rises about 7,000 feet above its 7,000-foot foundation, and stands in solitary splendor - the highest peak in the entire Cascade Range. Its rocky ice-mantled slopes above timberline contrast with the dense green forests and give Mount Rainier the appearance of an arctic island in a temperate sea, an island so large that you can see its full size and shape only from the air. The mountain is highly photogenic because of the contrasts it offers among bare rock, snowfields, blue sky, and the incomparable flower fields that color its lower slopes, shadows cast by the multitude of cliffs, ridges, canyons, and pinnacles change constantly from sunrise to sunset, endlessly varying the texture and mood of the mountain. The face of the mountain also varies from day to day as its broad snowfields melt during the summer. The melting of these frozen reservoirs makes Mount Rainier a natural resource in a practical as well as in an esthetic sense, for it ensures steady flows of water for hydroelectric power in the region, regardless of season.</p><p>Seen from the Puget Sound country to the west, Mount Rainier has an unreal quality - its white summit, nearly 3 miles high, seems to float among the clouds. We share with the populace of the entire lowland a thrill as we watch skyward the evening's setting sun reddens the volcano's western snowfields. When you approach the mountain in its lovely setting, you may find something that appeals especially to you - the scenery, the wildlife, the glaciers, or the wildflowers. Or you may feel challenged to climb to the summit. Mount Rainier and its neighboring mountains have a special allure for a geologist because he visualizes the event - some ordinary, some truly spectacular - that made the present landscape. Such is the fascination of geology. A geologist becomes trained to see 'in his mind's eye' geologic events of thousands or even millions of years ago. And, most remarkable, he can 'see' these events by studying rocks in a cliff or roadcut, or perhaps by examining earthy material that looks like common soil beneath pastureland many miles away from the volcano.</p><p>Our key to understanding the geology of Mount Rainier is that each geologic event can be reconstructed - or imagined - from the rocks formed at the time of the event. With this principle as our guide, we will review the geologic ancestry of this majestic volcano and learn what is behind its scenery.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b1292","usgsCitation":"Crandell, D.R., 1969, The Geologic Story of Mount Rainier (Revised 1983): U.S. Geological Survey Bulletin 1292, 43 p., https://doi.org/10.3133/b1292.","productDescription":"43 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":164037,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1292/report-thumb.jpg"},{"id":96253,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1292/report.pdf","size":"10911","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Mt. Ranier","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.29980468749999,\n              46.532413816559455\n            ],\n            [\n              -121.168212890625,\n              46.532413816559455\n            ],\n            [\n              -121.168212890625,\n              47.2307596483469\n            ],\n            [\n              -122.29980468749999,\n              47.2307596483469\n            ],\n            [\n              -122.29980468749999,\n              46.532413816559455\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Revised 1983","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c65d","contributors":{"authors":[{"text":"Crandell, Dwight Raymond","contributorId":6440,"corporation":false,"usgs":true,"family":"Crandell","given":"Dwight","email":"","middleInitial":"Raymond","affiliations":[],"preferred":false,"id":212451,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39683,"text":"pp650A - 1969 - Geological Survey research 1969, Chapter A","interactions":[],"lastModifiedDate":"2012-02-02T00:10:18","indexId":"pp650A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"650","chapter":"A","title":"Geological Survey research 1969, Chapter A","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1969","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp650A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Geological Survey research 1969, Chapter A: U.S. Geological Survey Professional Paper 650, p. A1-A425, https://doi.org/10.3133/pp650A.","productDescription":"p. A1-A425","costCenters":[],"links":[{"id":119844,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0650a/report-thumb.jpg"},{"id":67409,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0650a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649734","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":529922,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38936,"text":"pp437B - 1969 - Land subsidence due to ground-water withdrawal Tulare-Wasco, area California","interactions":[{"subject":{"id":43258,"text":"ofr6094 - 1960 - Land subsidence in the Tulare-Wasco area, California, 1957-1959","indexId":"ofr6094","publicationYear":"1960","noYear":false,"title":"Land subsidence in the Tulare-Wasco area, California, 1957-1959"},"predicate":"SUPERSEDED_BY","object":{"id":38936,"text":"pp437B - 1969 - Land subsidence due to ground-water withdrawal Tulare-Wasco, area California","indexId":"pp437B","publicationYear":"1969","noYear":false,"chapter":"B","title":"Land subsidence due to ground-water withdrawal Tulare-Wasco, area California"},"id":1},{"subject":{"id":43259,"text":"ofr6277 - 1962 - Land subsidence in the Tulare-Wasco area, California, 1959-62","indexId":"ofr6277","publicationYear":"1962","noYear":false,"title":"Land subsidence in the Tulare-Wasco area, California, 1959-62"},"predicate":"SUPERSEDED_BY","object":{"id":38936,"text":"pp437B - 1969 - Land subsidence due to ground-water withdrawal Tulare-Wasco, area California","indexId":"pp437B","publicationYear":"1969","noYear":false,"chapter":"B","title":"Land subsidence due to ground-water withdrawal Tulare-Wasco, area California"},"id":2}],"lastModifiedDate":"2022-02-22T19:55:56.832525","indexId":"pp437B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"437","chapter":"B","title":"Land subsidence due to ground-water withdrawal Tulare-Wasco, area California","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Studies of land subsidence","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp437B","usgsCitation":"Lofgren, B.E., and Klausing, R., 1969, Land subsidence due to ground-water withdrawal Tulare-Wasco, area California: U.S. Geological Survey Professional Paper 437, vii, 101 p., https://doi.org/10.3133/pp437B.","productDescription":"vii, 101 p.","costCenters":[],"links":[{"id":65979,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0437b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396270,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92915.htm"},{"id":120520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0437b/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Tulare-Wasco area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.5858,\n              35.5858\n            ],\n            [\n              -119,\n              35.5858\n            ],\n            [\n              -119,\n              36.2256\n            ],\n            [\n              -119.5858,\n              36.2256\n            ],\n            [\n              -119.5858,\n              35.5858\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b416c","contributors":{"authors":[{"text":"Lofgren, B. E.","contributorId":42579,"corporation":false,"usgs":true,"family":"Lofgren","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":220694,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klausing, R.L.","contributorId":73205,"corporation":false,"usgs":true,"family":"Klausing","given":"R.L.","affiliations":[],"preferred":false,"id":220695,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32678,"text":"pp543H - 1969 - Erosion and deposition on a beach raised by the 1964 earthquake Montague Island, Alaska","interactions":[{"subject":{"id":32678,"text":"pp543H - 1969 - Erosion and deposition on a beach raised by the 1964 earthquake Montague Island, Alaska","indexId":"pp543H","publicationYear":"1969","noYear":false,"chapter":"H","title":"Erosion and deposition on a beach raised by the 1964 earthquake Montague Island, Alaska"},"predicate":"IS_PART_OF","object":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"id":1}],"isPartOf":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"lastModifiedDate":"2022-02-16T20:17:09.532739","indexId":"pp543H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"H","title":"Erosion and deposition on a beach raised by the 1964 earthquake Montague Island, Alaska","docAbstract":"During the 1964 Alaska earthquake, tectonic deformation uplifted the southern end of Montague Island as much as 33 feet or more. The uplifted shoreline is rapidly being modified by subaerial and marine processes. The new raised beach is formed in bedrock, sand, gravel, and deltaic bay-head deposits, and the effect of each erosional process was measured in each material. Fieldwork was concentrated in two areas—MacLeod Harbor on the northwest side and Patton Bay on the southeast side of Montague Island. In the unconsolidated deltaic deposits of MacLeod Harbor, 97 percent of the erosion up to June 1965, 15 months after the earthquake, was fluvial, 2.2 percent was by rainwash, and only 0.8 percent was marine; 52 percent of the total available raised beach material had already been removed. The volume removed by stream erosion was proportional to low-flow discharge raised to the power of 0.75 to 0.95, and this volume increased as the bed material became finer. Stream response to the relative fall in base level was very rapid, most of the downcutting in unconsolidated materials occurring within 48 hours of the uplift for streams with low flows greater than 10 cubic feet per second. Since then, erosion by these streams has been predominantly lateral. Streams with lower discharges, in unconsolidated materials, still had knickpoints after 15 months. No response to uplift could be detected in stream courses above the former preearthquake sea level.\n\nWhere the raised beach is in bedrock, it is being destroyed principally by marine action but at such a low rate that no appreciable erosion of bedrock was found 15 months after the earthquake. A dated rock platform raised earlier has eroded at a mean rate of 0.49 foot per year. In this area the factor limiting the rate of erosion was rock resistance rather than the transporting capacity of the waves.\n\nThe break in slope between the top of the raised beach and the former seacliff is being obliterated by debris which is accumulating at the base of the cliffs and which is no longer being removed by the sea. Current cliff retreat by rockfall, mudflows, and landslides was estimated at 0.7 to 2.0 feet per year, and in parts of Patton Bay the accumulation of debris has obliterated 78 percent of the original break in slope in 15 months.\n\nEvidence of two relative sea-level changes before 1964 was found in Patton Bay. At a high stand of sea level lasting until about 2000 B.P. (before present), an older raised beach was formed which, over a distance of 5 miles, shows 40 feet of deformation relative to the present sea level. Peat deposits exposed by the 1964 uplift also record a low sea level that lasted until at least 600 B.P.\n\nThe 1964 raised beach was used to test the accuracy of identification of former sea-level elevations from raised beach features. The Pre-1964 sea level could be accurately determined from the height of the former barnacle line, so an independent check on high-water level was available. The most reliable topographic indicator was the elevation of the break in slope at the top of a beach between a bedrock platform and a cliff. Even here, the former sea level could only be identified within 5 feet. The breaks in slope at the top of gravel beaches were found to be poor indicators of former sea level.\n\nOn Montague Island, evidence of former high sea levels appeared to be best preserved (1) as raised bedrock platforms on rocks of moderate resistance in slightly sheltered locations and (2) as raised storm beaches where the relief immediately inland was very low.","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/pp543H","usgsCitation":"Kirkby, M.J., and Kirkby, A.V., 1969, Erosion and deposition on a beach raised by the 1964 earthquake Montague Island, Alaska: U.S. Geological Survey Professional Paper 543, vi, 41 p., https://doi.org/10.3133/pp543H.","productDescription":"vi, 41 p.","numberOfPages":"49","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":277846,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0543h/index.html"},{"id":60590,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0543h/pp543h_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0543h/report-thumb.jpg"},{"id":396031,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_99031.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Montague Island","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -147.923,59.7643 ], [ -147.923,60.3825 ], [ -146.9077,60.3825 ], [ -146.9077,59.7643 ], [ -147.923,59.7643 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe045","contributors":{"authors":[{"text":"Kirkby, M. J.","contributorId":55322,"corporation":false,"usgs":true,"family":"Kirkby","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":208911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirkby, Anne V.","contributorId":108013,"corporation":false,"usgs":true,"family":"Kirkby","given":"Anne","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":208912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42026,"text":"ofr69289 - 1969 - Aeromagnetic map of the Cut Bank-Hungry Horse Reservoir area, northwestern Montana","interactions":[],"lastModifiedDate":"2022-12-07T11:57:10.047796","indexId":"ofr69289","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":"69-289","title":"Aeromagnetic map of the Cut Bank-Hungry Horse Reservoir area, northwestern Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69289","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Cut Bank-Hungry Horse Reservoir area, northwestern Montana: U.S. Geological Survey Open-File Report 69-289, 1 Plate: 28.88 × 19.94 inches, https://doi.org/10.3133/ofr69289.","productDescription":"1 Plate: 28.88 × 19.94 inches","costCenters":[],"links":[{"id":175437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79778,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0289/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":410132,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8415.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"Montana","otherGeospatial":"Cut Bank-Hungry Horse Reservoir area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114,\n              48.883\n            ],\n            [\n              -114,\n              47.667\n            ],\n            [\n              -111.917,\n              47.667\n            ],\n            [\n              -111.917,\n              48.883\n            ],\n            [\n              -114,\n              48.883\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696b30","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":530777,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39684,"text":"pp650C - 1969 - Geological Survey research 1969, Chapter C","interactions":[{"subject":{"id":15093,"text":"ofr68190 - 1968 - Aerial infrared images of The Geysers geothermal steam field and vicinity, Samoa County, California","indexId":"ofr68190","publicationYear":"1968","noYear":false,"title":"Aerial infrared images of The Geysers geothermal steam field and vicinity, Samoa County, California"},"predicate":"SUPERSEDED_BY","object":{"id":39684,"text":"pp650C - 1969 - Geological Survey research 1969, Chapter C","indexId":"pp650C","publicationYear":"1969","noYear":false,"chapter":"C","title":"Geological Survey research 1969, Chapter C"},"id":1},{"subject":{"id":15095,"text":"ofr68191 - 1968 - Aerial infrared surveys at The Geysers geothermal steam field, California","indexId":"ofr68191","publicationYear":"1968","noYear":false,"title":"Aerial infrared surveys at The Geysers geothermal steam field, California"},"predicate":"SUPERSEDED_BY","object":{"id":39684,"text":"pp650C - 1969 - Geological Survey research 1969, Chapter C","indexId":"pp650C","publicationYear":"1969","noYear":false,"chapter":"C","title":"Geological Survey research 1969, Chapter C"},"id":2}],"lastModifiedDate":"2023-09-25T20:40:31.988514","indexId":"pp650C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"650","chapter":"C","title":"Geological Survey research 1969, Chapter C","docAbstract":"<p>This collection of 38 short papers is the second published chapter of \"Geological Survey Research 1969.\" The papers report on scientific and economic results of current work by members of the Geologic, Topographic, and Water Resources Divisions of the U.S. Geological Survey.</p><p>Chapter A, to be published later in the year, will present a summary of significant results of work done during fiscal year 1969, together with lists of investigations in progress, reports published, cooperating agencies, and Geological Survey offices.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1969","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp650C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Geological Survey research 1969, Chapter C: U.S. Geological Survey Professional Paper 650, iv, 247 p., https://doi.org/10.3133/pp650C.","productDescription":"iv, 247 p.","numberOfPages":"254","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":67410,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0650c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123061,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0650c/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6877bf","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":529923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38891,"text":"pp486D - 1969 - Lower Colorado River water supply - its magnitude and distribution","interactions":[],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"pp486D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"486","chapter":"D","title":"Lower Colorado River water supply - its magnitude and distribution","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water resources of Lower Colorado River-Salton Sea area","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp486D","usgsCitation":"Hely, A., 1969, Lower Colorado River water supply - its magnitude and distribution: U.S. Geological Survey Professional Paper 486, p. D1-D54, https://doi.org/10.3133/pp486D.","productDescription":"p. D1-D54","costCenters":[],"links":[{"id":119996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0486d/report-thumb.jpg"},{"id":65903,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0486d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648843","contributors":{"authors":[{"text":"Hely, A. G.","contributorId":14401,"corporation":false,"usgs":true,"family":"Hely","given":"A. G.","affiliations":[],"preferred":false,"id":220612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37268,"text":"rp76 - 1969 - Parasites and diseases of warm-water fishes","interactions":[],"lastModifiedDate":"2016-11-09T11:27:46","indexId":"rp76","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":"76","title":"Parasites and diseases of warm-water fishes","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Bureau Of Sport Fisheries And Wildlife, 1969, Parasites and diseases of warm-water fishes: Resource Publication 76, 20 p.","productDescription":"20 p.","costCenters":[],"links":[{"id":162017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6892fd","contributors":{"authors":[{"text":"Bureau Of Sport Fisheries And Wildlife","contributorId":128243,"corporation":true,"usgs":false,"organization":"Bureau Of Sport Fisheries And Wildlife","id":529634,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41695,"text":"ofr69293 - 1969 - Aeromagnetic map of parts of the Piney River and Shipman quadrangles, Amherst and Nelson Counties, Virginia","interactions":[],"lastModifiedDate":"2021-12-28T20:38:38.745679","indexId":"ofr69293","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":"69-293","title":"Aeromagnetic map of parts of the Piney River and Shipman quadrangles, Amherst and Nelson Counties, Virginia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69293","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of parts of the Piney River and Shipman quadrangles, Amherst and Nelson Counties, Virginia: U.S. Geological Survey Open-File Report 69-293, 1 Plate: 40.88 × 34.10 inches, https://doi.org/10.3133/ofr69293.","productDescription":"1 Plate: 40.88 × 34.10 inches","costCenters":[],"links":[{"id":176504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393543,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8417.htm"},{"id":79415,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0293/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Virginia","county":"Amherst County, Nelson County","otherGeospatial":"Piney River and Shipman quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.125,\n              37.622\n            ],\n            [\n              -78.867,\n              37.622\n            ],\n            [\n              -78.867,\n              37.75\n            ],\n            [\n              -79.125,\n              37.75\n            ],\n            [\n              -79.125,\n              37.622\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6974c3","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":530574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41716,"text":"ofr69295 - 1969 - Areal geologic and structural interpretation map of an area in the Sheep Creek Range, Lander County, Nevada","interactions":[],"lastModifiedDate":"2021-12-29T20:23:22.66978","indexId":"ofr69295","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":"69-295","title":"Areal geologic and structural interpretation map of an area in the Sheep Creek Range, Lander County, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69295","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Areal geologic and structural interpretation map of an area in the Sheep Creek Range, Lander County, Nevada: U.S. Geological Survey Open-File Report 69-295, 1 Plate: 22.00 × 53.00 inches, https://doi.org/10.3133/ofr69295.","productDescription":"1 Plate: 22.00 × 53.00 inches","costCenters":[],"links":[{"id":167869,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393621,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8419.htm"},{"id":98586,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0295/plate-1.pdf","size":"7077","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Nevada","county":"Lander County","otherGeospatial":"Sheep Creek Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.9040,\n              40.67\n            ],\n            [\n              -116.7780,\n              40.67\n            ],\n            [\n              -116.7780,\n              40.911\n            ],\n            [\n              -116.9040,\n              40.911\n            ],\n            [\n              -116.9040,\n              40.67\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6733fb","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":530581,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42351,"text":"ofr69287 - 1969 - Aeromagnetic map of the Barker and Neihart quadrangles, Judith Basin, Cascade, and Meagher Counties, Montana","interactions":[],"lastModifiedDate":"2021-12-28T21:07:51.844825","indexId":"ofr69287","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":"69-287","title":"Aeromagnetic map of the Barker and Neihart quadrangles, Judith Basin, Cascade, and Meagher Counties, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69287","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Barker and Neihart quadrangles, Judith Basin, Cascade, and Meagher Counties, Montana: U.S. Geological Survey Open-File Report 69-287, 1 Plate: 19.47 × 45.92 inches, https://doi.org/10.3133/ofr69287.","productDescription":"1 Plate: 19.47 × 45.92 inches","costCenters":[],"links":[{"id":173578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80117,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0287/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393549,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8413.htm"}],"scale":"62500","country":"United States","state":"Montana","county":"Cascade County, Meagher County","otherGeospatial":"Barker and Neihart quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.7916259765625,\n              46.73233101286786\n            ],\n            [\n              -110.577392578125,\n              46.73233101286786\n            ],\n            [\n              -110.577392578125,\n              47.26804770458176\n            ],\n            [\n              -110.7916259765625,\n              47.26804770458176\n            ],\n            [\n              -110.7916259765625,\n              46.73233101286786\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db69723b","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":530916,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38817,"text":"pp543I - 1969 - Tectonics of the March 27, 1964, Alaska earthquake","interactions":[{"subject":{"id":38817,"text":"pp543I - 1969 - Tectonics of the March 27, 1964, Alaska earthquake","indexId":"pp543I","publicationYear":"1969","noYear":false,"chapter":"I","title":"Tectonics of the March 27, 1964, Alaska earthquake"},"predicate":"IS_PART_OF","object":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"id":1}],"isPartOf":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"lastModifiedDate":"2022-06-28T18:18:07.763935","indexId":"pp543I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"I","title":"Tectonics of the March 27, 1964, Alaska earthquake","docAbstract":"The March 27, 1964, earthquake was accomp anied by crustal deformation-including warping, horizontal distortion, and faulting-over probably more than 110,000 square miles of land and sea bottom in south-central Alaska. Regional uplift and subsidence occurred mainly in two nearly parallel elongate zones, together about 600 miles long and as much as 250 miles wide, that lie along the continental margin. From the earthquake epicenter in northern Prince William Sound, the deformation extends eastward 190 miles almost to long 142° and southwestward slightly more than 400 miles to about long 155°. It extends across the two zones from the chain of active volcanoes in the Aleutian Range and Wrangell Mountains probably to the Aleutian Trench axis.\n\nUplift that averages 6 feet over broad areas occurred mainly along the coast of the Gulf of Alaska, on the adjacent Continental Shelf, and probably on the continental slope. This uplift attained a measured maximum on land of 38 feet in a northwest-trending narrow belt less than 10 miles wide that is exposed on Montague Island in southwestern Prince William Sound. Two earthquake faults exposed on Montague Island are subsidiary northwest-dipping reverse faults along which the northwest blocks were relatively displaced a maximum of 26 feet, and both blocks were upthrown relative to sea level. From Montague Island, the faults and related belt of maximum uplift may extend southwestward on the Continental Shelf to the vicinity of the Kodiak group of islands. To the north and northwest of the zone of uplift, subsidence forms a broad asymmetrical downwarp centered over the Kodiak-Kenai-Chugach Mountains that averages 2½ feet and attains a measured maximum of 7½ feet along the southwest coast of the Kenai Peninsula. Maximum indicated uplift in the Alaska and Aleutian Ranges to the north of the zone of subsidence was l½ feet. Retriangulation over roughly 25,000 square miles of the deformed region in and around Prince William Sound shows that vertical movements there were accompanied by horizontal distortion, involving systematic shifts of about 64 feet in a relative seaward direction. Comparable horizontal movements are presumed to have affected those parts of the major zones of uplift and subsidence for which retriangulation data are unavailable.\n\nRegional vertical deformation generated a train of destructive long-period seismic sea waves in the Gulf of Alaska as well as unique atmospheric and ionospheric disturbances that were recorded at points far distant from Alaska. Warping resulted in permanent tilt of larger lake basins and temporary reductions in discharge of some major rivers. Uplift and subsidence relative to sea level caused profound modifications in shoreline morphology with attendant catastrophic effects on the nearshore biota and costly damage to coasta1 installations. Systematic horizontal movements of the land relative to bodies of confined or semiconfined water may have caused unexplained short-period waves—some of which were highly destructive—observed during or immediately after the earthquake at certain coastal localities and in Kenai Lake. Porosity increases, probably related to horizontal displacements in the zone of subsidence, were reflected in lowered well-water levels and in losses of surface water.\n\nThe primary fault, or zone of faults, along which the earthquake occurred is not exposed at the surface on land. Focal-mechanism studies, when considered in conjunction with the pattern of deformation and seismicity, suggest that it was a complex thrust fault (megathrust) dipping at a gentle angle beneath the continental margin from the vicinity of the Aleutian Trench. Movement on the megathrust was accompanied by subsidiary reverse faulting, and perhaps wrench faulting, within the upper plate. Aftershock distribution suggests movement on a segment of the megathrust, some 550–600 miles long and 110–180 miles wide, that underlies most of the major zone of uplift and the seaward part of the major zone of subsidence.\n\nAccording to the postulated model, the observed and inferred tectonic displacements that accompanied the earthquake resulted primarily from (1) relative seaward displacement and uplift of the seaward part of the block by movement along the dipping megathrust and subsidiary faults that break through the upper plate to the surface, and (2) simultaneous elastic horizontal extension and vertical attenuation (subsidence) of the crustal slab behind the upper plate. Slight uplift inland from the major zones of deformation presumably was related to elastic strain changes resulting from the overthrusting; however, the data are insufficient to permit conclusions regarding its cause.\n\nThe belt of seismic activity and major zones of tectonic deformation associated with the 1964 earthquake, to a large extent, lie between and parallel to the Aleutian Volcanic Arc and the Aleutian Trench, and are probably genetically related to the arc. Geologic data indicate that the earthquake-related tectonic movements were but the most recent pulse in an episode of deformation that probably began in late Pleistocene time and has continued intermittently to the present. Evidence for progressive coastal submergence in the deformed region for several centuries preceding the earthquake, in combin1ation with transverse horizontal shortening indicated by the retriangulation data, suggests pre-earthquake strain directed at a gentle angle downward beneath the arc. The duration of strain accumulation in the epicentral region, as interpreted from the time interval during which the coastal submergence occurred, probably is 930–1,360 years.","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/pp543I","usgsCitation":"Plafker, G., 1969, Tectonics of the March 27, 1964, Alaska earthquake: U.S. Geological Survey Professional Paper 543, Report: viii, 74 p.; 2 Plates: 27.08 x 21.87 inches and 16.09 x 20.66 inches, https://doi.org/10.3133/pp543I.","productDescription":"Report: viii, 74 p.; 2 Plates: 27.08 x 21.87 inches and 16.09 x 20.66 inches","numberOfPages":"88","costCenters":[{"id":380,"text":"Menlo ParkCalif. 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,{"id":41733,"text":"ofr69291 - 1969 - Aeromagnetic map of the Menominee-Northland area, Dickinson, Marquette, and Menominee Counties, Michigan, and Marinette County, Wisconsin.","interactions":[{"subject":{"id":41733,"text":"ofr69291 - 1969 - Aeromagnetic map of the Menominee-Northland area, Dickinson, Marquette, and Menominee Counties, Michigan, and Marinette County, Wisconsin.","indexId":"ofr69291","publicationYear":"1969","noYear":false,"title":"Aeromagnetic map of the Menominee-Northland area, Dickinson, Marquette, and Menominee Counties, Michigan, and Marinette County, Wisconsin."},"predicate":"SUPERSEDED_BY","object":{"id":63898,"text":"gp711 - 1970 - Aeromagnetic map of the Menominee-Northland area, Dickinson, Marquette, and Menominee Counties, Michigan, and Marinette County, Wisconsin","indexId":"gp711","publicationYear":"1970","noYear":false,"title":"Aeromagnetic map of the Menominee-Northland area, Dickinson, Marquette, and Menominee Counties, Michigan, and Marinette County, Wisconsin"},"id":1}],"supersededBy":{"id":63898,"text":"gp711 - 1970 - Aeromagnetic map of the Menominee-Northland area, Dickinson, Marquette, and Menominee Counties, Michigan, and Marinette County, Wisconsin","indexId":"gp711","publicationYear":"1970","noYear":false,"title":"Aeromagnetic map of the Menominee-Northland area, Dickinson, Marquette, and Menominee Counties, Michigan, and Marinette County, Wisconsin"},"lastModifiedDate":"2022-05-31T21:41:20.862063","indexId":"ofr69291","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":"69-291","title":"Aeromagnetic map of the Menominee-Northland area, Dickinson, Marquette, and Menominee Counties, Michigan, and Marinette County, Wisconsin.","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69291","collaboration":"Prepared in cooperation with the Michigan Department of Conservation, Geological Survey Division","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Menominee-Northland area, Dickinson, Marquette, and Menominee Counties, Michigan, and Marinette County, Wisconsin.: U.S. Geological Survey Open-File Report 69-291, 2 Plates: 28.40 x 40.41 inches and 37.53 x 52.71 inches, https://doi.org/10.3133/ofr69291.","productDescription":"2 Plates: 28.40 x 40.41 inches and 37.53 x 52.71 inches","costCenters":[],"links":[{"id":401465,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0291/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401464,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0291/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0291/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"Michigan, Wisconsin","otherGeospatial":"Menominee-Northland area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.62969970703125,\n              45.09364075696455\n            ],\n            [\n              -87.5888442993164,\n              45.09364075696455\n            ],\n            [\n              -87.5888442993164,\n              45.150811140066864\n            ],\n            [\n              -87.62969970703125,\n              45.150811140066864\n            ],\n            [\n              -87.62969970703125,\n              45.09364075696455\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691db2","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":530595,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42051,"text":"ofr69290 - 1969 - Aeromagnetic map of Gladstone and vicinity, Delta, Alger, Menominee, and Marquette Counties, Michigan.","interactions":[],"lastModifiedDate":"2012-02-02T00:05:06","indexId":"ofr69290","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":"69-290","title":"Aeromagnetic map of Gladstone and vicinity, Delta, Alger, Menominee, and Marquette Counties, Michigan.","language":"ENGLISH","doi":"10.3133/ofr69290","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of Gladstone and vicinity, Delta, Alger, Menominee, and Marquette Counties, Michigan.: U.S. Geological Survey Open-File Report 69-290, 4 maps, https://doi.org/10.3133/ofr69290.","productDescription":"4 maps","costCenters":[],"links":[{"id":136740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98780,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0290/plate-1.pdf","size":"9267","linkFileType":{"id":1,"text":"pdf"}},{"id":98781,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0290/plate-2.pdf","size":"6286","linkFileType":{"id":1,"text":"pdf"}},{"id":98782,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0290/plate-3.pdf","size":"10402","linkFileType":{"id":1,"text":"pdf"}},{"id":98783,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0290/plate-4.pdf","size":"8397","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db69218f","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":530800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32763,"text":"pp417F - 1969 - A water budget of the Carson Valley, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"pp417F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"417","chapter":"F","title":"A water budget of the Carson Valley, Nevada","language":"ENGLISH","doi":"10.3133/pp417F","usgsCitation":"Piper, A.M., 1969, A water budget of the Carson Valley, Nevada: U.S. Geological Survey Professional Paper 417, p. F1-F8, https://doi.org/10.3133/pp417F.","productDescription":"p. F1-F8","costCenters":[],"links":[{"id":119270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0417f/report-thumb.jpg"},{"id":60699,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0417f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60700,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0417f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a51c0","contributors":{"authors":[{"text":"Piper, A. M.","contributorId":102865,"corporation":false,"usgs":true,"family":"Piper","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":209117,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37449,"text":"ssrw126 - 1969 - Catalogue of helminths of waterfowl (Anatidae)","interactions":[],"lastModifiedDate":"2012-02-02T00:09:40","indexId":"ssrw126","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":"126","title":"Catalogue of helminths of waterfowl (Anatidae)","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"McDonald, M., 1969, Catalogue of helminths of waterfowl (Anatidae): Special Scientific Report  - Wildlife 126, viii, 692 p.","productDescription":"viii, 692 p.","costCenters":[],"links":[{"id":112092,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924055486801?urlappend=%3Bseq=9"},{"id":166817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6fb0","contributors":{"authors":[{"text":"McDonald, Malcolm E.","contributorId":68373,"corporation":false,"usgs":true,"family":"McDonald","given":"Malcolm E.","affiliations":[],"preferred":false,"id":218098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38718,"text":"pp650B - 1969 - Geological Survey research 1969, Chapter B","interactions":[],"lastModifiedDate":"2025-08-22T20:37:13.467108","indexId":"pp650B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"650","chapter":"B","title":"Geological Survey research 1969, Chapter B","docAbstract":"<p>This collection of 40 short papers is the first published chapter of \"Geological Survey Research 1969.\" The papers report on scientific and economic results of current work by members of the Conservation, Geologic, and Water Resources Divisions of the U.S. Geological Survey.</p>\n<p>Chapter A, to be published later in the year, will present a summary of significant results of work done during fiscal year 1969, together with lists of investigations in progress, reports published, cooperating agencies, and Geological Survey offices.</p>\n<p>&nbsp;</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1969","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp650B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Geological Survey research 1969, Chapter B: U.S. Geological Survey Professional Paper 650, 211 p., https://doi.org/10.3133/pp650B.","productDescription":"211 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":494648,"rank":18,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92914.htm","text":"The ages of three uranium minerals, Mojave Desert, California","linkFileType":{"id":5,"text":"html"}},{"id":411254,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30395.htm","text":"Origin of some amphibolites in western North Carolina","linkFileType":{"id":5,"text":"html"}},{"id":494647,"rank":17,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30409.htm","text":"Effects of reservoir filling on a buried aquifer of glacial origin in Campbell County, South Dakota","linkFileType":{"id":5,"text":"html"}},{"id":494646,"rank":16,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30408.htm","text":"Correlation of carbonate rock units in northwest Ohio by natural gamma logging","linkFileType":{"id":5,"text":"html"}},{"id":494645,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30407.htm","text":"Occurrence and movement of ground water in the Brunswick Shale at a site near Trenton, New Jersey","linkFileType":{"id":5,"text":"html"}},{"id":494644,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30406.htm","text":"Seismic investigations on Cape Cod, Martha's Vinyard, and Nantucket, Massachusetts, and a topographic map of the basement surface from Cape Cod Bay to the islands","linkFileType":{"id":5,"text":"html"}},{"id":494643,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30405.htm","text":"Hawaiian seismic events during 1966","linkFileType":{"id":5,"text":"html"}},{"id":494642,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30404.htm","text":"Distribution of mercury in the Navajo Sandstone, Colorado Plateau region","linkFileType":{"id":5,"text":"html"}},{"id":494641,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30403.htm","text":"The time interval between stabilization of alpine glacial deposits and establishment of tree seedlings","linkFileType":{"id":5,"text":"html"}},{"id":494640,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30402.htm","text":"Possible exploration targets for uranium deposits, south end of the Uravan mineral belt, Colorado - Utah","linkFileType":{"id":5,"text":"html"}},{"id":494639,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30401.htm","text":"White clay deposits near Mount Holly Springs, Cumberland County, Pennsylvania","linkFileType":{"id":5,"text":"html"}},{"id":494638,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30400.htm","text":"New evidence on age relationships of possible Eocene rocks in southwestern North Dakota","linkFileType":{"id":5,"text":"html"}},{"id":494637,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30399.htm","text":"Larger fossil mammals and Mylagaulid rodents from the Troublesome Formation of Colorado","linkFileType":{"id":5,"text":"html"}},{"id":494636,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30398.htm","text":"Notes on the geology and paleohydrology of the Boulder City pluton, southern Nevada","linkFileType":{"id":5,"text":"html"}},{"id":494635,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30397.htm","text":"Tuffaceous epiclastic breccia and sandstone near Hahns Peak, Colorado, and their genetic implications","linkFileType":{"id":5,"text":"html"}},{"id":494634,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30396.htm","text":"Lawsonite blueschist from north-central Oregon","linkFileType":{"id":5,"text":"html"}},{"id":119562,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0650b/report-thumb.jpg"},{"id":65575,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0650b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6877ea","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":529876,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38733,"text":"pp627B - 1969 - Effects of urban development on direct runoff to East Meadow Brook, Nassau County, Long Island, New York","interactions":[],"lastModifiedDate":"2025-04-15T19:29:23.002453","indexId":"pp627B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"627","chapter":"B","title":"Effects of urban development on direct runoff to East Meadow Brook, Nassau County, Long Island, New York","docAbstract":"<p>The study described in this report is concerned with the effects of intensive urban development on direct runoff to East Meadow Brook, a southward-flowing stream in central Nassau County, N.Y., during the period 1937-66. The specific objectives of the study were (a) to relate indices of urban development to increases in the volume of annual direct runoff to the stream; (b) to compare hydrograph features at different periods during the transition of the drainage basin from rural to urban conditions; and (c) to compare the rainfall-runoff relations for periods before and after urban development.</p><p>Periods of housing and street construction in the drainage basin correspond to three distinct periods of increased direct runoff after the base period 1937-43-namely, 1944-51, 1952-59, and 1960-62. During each period, the average annual direct runoff increased because of an increase in the area served by storm sewers that discharged into East Meadow Brook. The amount of land served by sewers increased from about 570 acres in 1943 to about 3,600 acres in 1962, or about 530 percent. During this same period, the average annual direct runoff increased from about 920 acre-feet per year to about 3,400 acre-feet per year, or about 270 percent.</p><p>The shape of direct-runoff unit hydrographs of East Meadow Brook also changed during the period of study. The average peak discharge of a 1-hour-duration unit hydrograph increased from 313 cubic feet per second, for storms in 1937-43, to 776 cubic feet per second, for storms in 1960-62, or about 2.5 times. In addition, the widths of the unit hydrographs for 1960-62 at values of 50 and 75 percent of the peak discharge were 38 and 28 percent, respectively, the comparable widths of the unit hydrographs for 1937-43.</p><p>An analysis of the rainfall-runoff relations for both preurban and urban conditions indicates that the direct runoff for both periods increased with the magnitude of the storm. However, the direct runoff during a period of urbanized conditions (1964- 66) was from 1.1 to 4.6 times greater than the corresponding runoff during the preurban period 1937-43, depending on the size of the individual storm.</p><p>The volume of direct runoff from the parts of the subarea equipped with storm sewers that discharged into East Meadow Brook is estimated to have been roughly 3,000 acre-feet per year in 1960-62, or about 20 percent of the precipitation on those parts of the area.</p><p>The increase in direct runoff probably represents a loss of ground-water recharge. However, because data changes in evapo-transpiration are insufficient and because the effects of recharge basins are unknown, adequate quantitative estimates of groundwater recharge can not be made.</p><p>On the basis of the present zoning regulations and on assumption that an additional 320 acres in the Hempstead subarea will be serviced by storm sewers that discharge into East Meadow Brook, direct runoff from the subarea is expected to increase in the future to an estimated 4,000-4,500 acre-feet per year.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology and some effects of urbanization on Long Island, New York (Professional Paper 627)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp627B","collaboration":"Prepared in cooperation with the New York State Department of Conservation, Division of Water Resources; the Nassau County Department of Public Works; the Suffolk County Board of Supervisors; and the Suffolk County Water Authority","usgsCitation":"Seaburn, G., 1969, Effects of urban development on direct runoff to East Meadow Brook, Nassau County, Long Island, New York: U.S. Geological Survey Professional Paper 627, Report: iii, 14 p.; 1 Plate: 25.54 x 35.52 inches, https://doi.org/10.3133/pp627B.","productDescription":"Report: iii, 14 p.; 1 Plate: 25.54 x 35.52 inches","costCenters":[],"links":[{"id":484611,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4955.htm","linkFileType":{"id":5,"text":"html"}},{"id":65592,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0627b/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":340354,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0627b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122210,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0627b/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Nassau County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.75,\n              40.65\n            ],\n            [\n              -73.5,\n              40.65\n            ],\n            [\n              -73.5,\n              40.8\n            ],\n            [\n              -73.75,\n              40.8\n            ],\n            [\n              -73.75,\n              40.65\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db60feb1","contributors":{"authors":[{"text":"Seaburn, G.E.","contributorId":42193,"corporation":false,"usgs":true,"family":"Seaburn","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":220362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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