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,{"id":39642,"text":"pp1455 - 1988 - Palynological studies of Middle Pennsylvanian coal beds of the proposed Pennsylvania System stratotype in West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:09:56","indexId":"pp1455","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1455","title":"Palynological studies of Middle Pennsylvanian coal beds of the proposed Pennsylvania System stratotype in West Virginia","language":"ENGLISH","doi":"10.3133/pp1455","usgsCitation":"Kosanke, R., 1988, Palynological studies of Middle Pennsylvanian coal beds of the proposed Pennsylvania System stratotype in West Virginia: U.S. Geological Survey Professional Paper 1455, 73 p., https://doi.org/10.3133/pp1455.","productDescription":"73 p.","costCenters":[],"links":[{"id":119384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1455/report-thumb.jpg"},{"id":67310,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1455/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db68956c","contributors":{"authors":[{"text":"Kosanke, R.M.","contributorId":97517,"corporation":false,"usgs":true,"family":"Kosanke","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":221880,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39647,"text":"pp1447A - 1988 - Origins, behavior, and sedimentology of lahars and lahar-runout flows in the Toutle-Cowlitz River system","interactions":[{"subject":{"id":15876,"text":"ofr85500 - 1985 - Lahars and lahar-runout flows in the Toutle-Cowlitz River system, Mount St. Helens, Washington; origins, behavior, and sedimentology","indexId":"ofr85500","publicationYear":"1985","noYear":false,"title":"Lahars and lahar-runout flows in the Toutle-Cowlitz River system, Mount St. Helens, Washington; origins, behavior, and sedimentology"},"predicate":"SUPERSEDED_BY","object":{"id":39647,"text":"pp1447A - 1988 - Origins, behavior, and sedimentology of lahars and lahar-runout flows in the Toutle-Cowlitz River system","indexId":"pp1447A","publicationYear":"1988","noYear":false,"chapter":"A","title":"Origins, behavior, and sedimentology of lahars and lahar-runout flows in the Toutle-Cowlitz River system"},"id":1}],"lastModifiedDate":"2022-12-23T16:53:44.264053","indexId":"pp1447A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1447","chapter":"A","title":"Origins, behavior, and sedimentology of lahars and lahar-runout flows in the Toutle-Cowlitz River system","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1447A","usgsCitation":"Scott, K.M., 1988, Origins, behavior, and sedimentology of lahars and lahar-runout flows in the Toutle-Cowlitz River system: U.S. Geological Survey Professional Paper 1447, vi, 74 p., https://doi.org/10.3133/pp1447A.","productDescription":"vi, 74 p.","costCenters":[],"links":[{"id":67324,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1447a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119385,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1447a/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Toutle-Cowlitz River system","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.00914795227045,\n              46.55\n            ],\n            [\n              -123.00787788023842,\n              46.55\n            ],\n            [\n              -123.00787788023842,\n              46.01464105419163\n            ],\n            [\n              -122.00914795227045,\n              46.01464105419163\n            ],\n            [\n              -122.00914795227045,\n              46.55\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a5ad","contributors":{"authors":[{"text":"Scott, K. M.","contributorId":8119,"corporation":false,"usgs":true,"family":"Scott","given":"K.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":221898,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39651,"text":"pp1398 - 1988 - The Pintail coal bed and barrier bar G: A model for coal of barrier bar-lagoon origin, Upper Cretaceous Almond Formation, Rock Springs coal field, Wyoming","interactions":[],"lastModifiedDate":"2022-12-05T21:13:54.793867","indexId":"pp1398","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1398","title":"The Pintail coal bed and barrier bar G: A model for coal of barrier bar-lagoon origin, Upper Cretaceous Almond Formation, Rock Springs coal field, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1398","usgsCitation":"Roehler, H.W., 1988, The Pintail coal bed and barrier bar G: A model for coal of barrier bar-lagoon origin, Upper Cretaceous Almond Formation, Rock Springs coal field, Wyoming: U.S. Geological Survey Professional Paper 1398, Report: iv, 60 p.; 2 Plates: 43.00 × 29.00 inches and 33.00 × 32.00 inches, https://doi.org/10.3133/pp1398.","productDescription":"Report: iv, 60 p.; 2 Plates: 43.00 × 29.00 inches and 33.00 × 32.00 inches","costCenters":[],"links":[{"id":67339,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1398/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67338,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1398/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67337,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1398/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1398/report-thumb.jpg"},{"id":110592,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74206.htm","linkFileType":{"id":5,"text":"html"},"description":"74206"}],"country":"United States","state":"Wyoming","otherGeospatial":"Upper Cretaceous Almond Formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.805,\n              41.4492\n            ],\n            [\n              -108.805,\n              41.25\n            ],\n            [\n              -108.9458,\n              41.25\n            ],\n            [\n              -108.9458,\n              41.4492\n            ],\n            [\n              -108.805,\n              41.4492\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67adec","contributors":{"authors":[{"text":"Roehler, H. W.","contributorId":16072,"corporation":false,"usgs":true,"family":"Roehler","given":"H.","middleInitial":"W.","affiliations":[],"preferred":false,"id":221908,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39654,"text":"pp1403A - 1988 - Summary of the hydrology of the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama","interactions":[],"lastModifiedDate":"2025-04-17T18:08:44.491095","indexId":"pp1403A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1403","chapter":"A","title":"Summary of the hydrology of the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama","docAbstract":"The Floridan aquifer system is one of the major sources of ground-water supplies in the United States. This highly productive aquifer system underlies all of Florida, southern Georgia, and small parts of adjoining Alabama and South Carolina, for a total area of about 100,000 square miles. About 3 billion gallons of water per day is withdrawn from the aquifer for all uses, and, in many areas, the Floridan is the sole source of freshwater.\r\n\r\nThe aquifer system is a sequence of hydraulically connected carbonate rocks (principally limestone and some dolomite) that generally range in age from Late Paleocene to Early Miocene. The rocks vary in thickness from a featheredge where they crop out to more than 3,500 ft where the aquifer is deeply buried. The aquifer system generally consists of an upper aquifer and a lower aquifer, separated by a less permeable confining unit of highly variable properties. In parts of north Florida and southwest Georgia, there is little permeability contrast within the aquifer system. Thus in these areas the Floridan is effectively one continuous aquifer. The upper and lower aquifers are defined on the basis of permeability, and their boundaries locally do not coincide with those for either time-stratigraphic or rock-stratigraphic units.\r\n\r\nLow-permeability clastic rocks overlie much of the Floridan aquifer system. The lithology, thickness, and integrity of these low-permeability rocks have a controlling effect on the development of permeability and ground-water flow in the Floridan locally. \r\n\r\nThe Floridan aquifer system derives its permeability from openings that vary from fossil hashes and networks of many solution-widened joints to large cavernous openings in karst areas. Diffuse flow pre-dominates where the small openings occur, whereas conduit flow may occur where there are large cavernous openings. For the Upper Floridan aquifer, transmissivities are highest (greater than 1,000,000 ft squared per day) in the unconfined karst areas of central and northern Florida. Lowest transmissivities (less than 50,000 ft squared per day) occur in the Florida panhandle and southernmost Florida, where the Upper Floridan aquifer is confined by thick clay sections. The hydraulic properties of the Lower Floridan aquifer are not well known; however, this unit also contains intervals of very high transmissivity that have been attributed to paleokarst development.\r\n\r\nThe dominant feature of the Floridan flow system, both before and after ground-water development, is Upper Floridan aquifer springs, nearly all of which occur in unconfined and semiconfined parts of the aquifer in Florida. Before ground-water development, spring flow and point discharge to surface-water bodies was about 88 percent of the estimated 21,500 cubic ft per second total discharge. Current discharge (early 1980's) is about 24,100 cubic ft per second, 75 percent of which is spring flow and discharge to surface-water bodies, 17 percent is withdrawal from wells, and 8 percent is diffuse upward leakage.\r\n\r\nPumpage has been and continues to be supplied primarily by the diversion of natural outflow from the aquifer system and by induced recharge rather than by loss of water from aquifer storage. The approximately 3 billion gallons per day pumped from the Floridan aquifer system has resulted in long-term regional water-level declines of more than 10 ft in three broad areas of the flow system: (1) coastal Georgia and adjacent South Carolina and northeast Florida, (2) west-central Florida, and (3) the Florida panhandle. Saltwater has encroached as a result of pumping in a few coastal areas.\r\n\r\nIn general, the water chemistry in the Upper Floridan is related to flow and proximity to the freshwater-saltwater interface. In the unconfined or semiconfined areas where flow is vigorous, dissolved-solids concentrations are low (less than 250 milligrams per liter). Where the system is more tightly confined, flow is more sluggish and concentrations are higher (grea","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1403A","usgsCitation":"Summary of the hydrology of the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama; 1988; PP; 1403-A; Johnston, Richard H.; Bush, Peter W.","productDescription":"Report: 24 p.; 4 Plates: 20.00 x 26.00 inches or smaller","numberOfPages":"24","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":67366,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1403a/report.pdf","text":"Report","size":"5.46 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1403-A"},{"id":67362,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1403a/plate-1.pdf","size":"1.22 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-81.1614990234375,\n              25.37380917154398\n            ],\n            [\n              -81.18896484375,\n              25.24469595130604\n            ],\n            [\n              -81.1285400390625,\n              25.11544539706194\n            ],\n            [\n              -81.9854736328125,\n              24.78673454198888\n            ],\n            [\n              -82.9522705078125,\n              24.84656534821976\n            ],\n            [\n              -82.97973632812499,\n              24.577099744289427\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"1988-10-01","noUsgsAuthors":false,"publicationDate":"1988-10-01","publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980f5","contributors":{"authors":[{"text":"Johnston, Richard H.","contributorId":95860,"corporation":false,"usgs":true,"family":"Johnston","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":221917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bush, Peter W.","contributorId":57820,"corporation":false,"usgs":true,"family":"Bush","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":221916,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39782,"text":"pp1467 - 1988 - Floods of March 1982 in Indiana, Ohio, Michigan, and Illinois","interactions":[],"lastModifiedDate":"2016-05-24T10:12:36","indexId":"pp1467","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1467","title":"Floods of March 1982 in Indiana, Ohio, Michigan, and Illinois","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/pp1467","collaboration":"National Oceanic and Atmospheric Administration","usgsCitation":"Glatfelter, D., and Chin, E., 1988, Floods of March 1982 in Indiana, Ohio, Michigan, and Illinois: U.S. Geological Survey Professional Paper 1467, iv, 36 p., https://doi.org/10.3133/pp1467.","productDescription":"iv, 36 p.","startPage":"1","endPage":"36","numberOfPages":"43","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":67650,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1467/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122286,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1467/report-thumb.jpg"}],"country":"United States","state":"Illinois, Indiana, Ohio, 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,{"id":39783,"text":"pp1459 - 1988 - Geology of the Silsilah ring complex and associated tin mineralization, Kingdom of Saudi Arabia","interactions":[{"subject":{"id":13403,"text":"ofr85253 - 1985 - Geology of the Silsilah ring complex, Kingdom of Saudi Arabia","indexId":"ofr85253","publicationYear":"1985","noYear":false,"title":"Geology of the Silsilah ring complex, Kingdom of Saudi Arabia"},"predicate":"SUPERSEDED_BY","object":{"id":39783,"text":"pp1459 - 1988 - Geology of the Silsilah ring complex and associated tin mineralization, Kingdom of Saudi Arabia","indexId":"pp1459","publicationYear":"1988","noYear":false,"title":"Geology of the Silsilah ring complex and associated tin mineralization, Kingdom of Saudi Arabia"},"id":1}],"lastModifiedDate":"2012-02-02T00:10:15","indexId":"pp1459","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1459","title":"Geology of the Silsilah ring complex and associated tin mineralization, Kingdom of Saudi Arabia","language":"ENGLISH","doi":"10.3133/pp1459","usgsCitation":"Du Bray, E., 1988, Geology of the Silsilah ring complex and associated tin mineralization, Kingdom of Saudi Arabia: U.S. Geological Survey Professional Paper 1459, 47 p., 3 plates in pocket, https://doi.org/10.3133/pp1459.","productDescription":"47 p., 3 plates in pocket","costCenters":[],"links":[{"id":120425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1459/report-thumb.jpg"},{"id":67651,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1459/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67652,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1459/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67653,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1459/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67654,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1459/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e5b1","contributors":{"authors":[{"text":"Du Bray, E. A.","contributorId":22333,"corporation":false,"usgs":true,"family":"Du Bray","given":"E. A.","affiliations":[],"preferred":false,"id":222154,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39784,"text":"pp1452 - 1988 - Geology and paleoenvironment of the Oligocene Jebel Qatrani Formation and adjacent rocks, Fayum Depression, Egypt","interactions":[],"lastModifiedDate":"2012-02-02T00:10:15","indexId":"pp1452","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1452","title":"Geology and paleoenvironment of the Oligocene Jebel Qatrani Formation and adjacent rocks, Fayum Depression, Egypt","language":"ENGLISH","doi":"10.3133/pp1452","usgsCitation":"Bown, T.M., and Kraus, M.J., 1988, Geology and paleoenvironment of the Oligocene Jebel Qatrani Formation and adjacent rocks, Fayum Depression, Egypt: U.S. Geological Survey Professional Paper 1452, 60 p., https://doi.org/10.3133/pp1452.","productDescription":"60 p.","costCenters":[],"links":[{"id":120426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1452/report-thumb.jpg"},{"id":67655,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1452/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6843b8","contributors":{"authors":[{"text":"Bown, T. M.","contributorId":106858,"corporation":false,"usgs":true,"family":"Bown","given":"T.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":222156,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kraus, M. J.","contributorId":44605,"corporation":false,"usgs":false,"family":"Kraus","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":222155,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39785,"text":"pp1336C - 1988 - Landslides triggered by earthquakes in the central Mississippi Valley, Tennessee and Kentucky","interactions":[],"lastModifiedDate":"2022-11-28T23:04:58.553907","indexId":"pp1336C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1336","chapter":"C","title":"Landslides triggered by earthquakes in the central Mississippi Valley, Tennessee and Kentucky","docAbstract":"We mapped 221 large (more than 200 ft across) landslides of three morphologically distinct types on the bluffs bordering the Mississippi alluvial plain in western Tennessee and Kentucky Old coherent slides (146 landslides, or 66 percent of the total) include translational block slides and single and multiple-block rotational slumps, all of which are covered by mature vegetation and have eroded features; no active analogs exist in the area. Earth flows (51 landslides, or 23 percent of the total) are also largely revegetated and eroded, though a few active earth flows are present on bluffs that have been cleared of vegetation. Young rotational slumps (24 landslides, or 11 percent of the total) form solely along actively eroding near-river bluffs and are the only active or recently active landslides in the area. \r\n\r\nTwo investigations conducted around 1900 indicate that the old coherent slides, in at least part of the area, formed during the 1811-12 earthquakes. The present investigation uses dendrochronology, geomorphology, historic topographic maps, local historical accounts, and comparisons with landslides triggered by other earthquakes to show that most or all of the old coherent slides and earth flows formed during the 1811-12 New Madrid earthquakes. Evidence clearly indicates that the only large, aseismic landslide activity in the area results from fluvial undercutting of near-river bluffs. This erosion of the base of the bluffs triggers slumps that are morphologically distinct from the old slumps on bluffs away from the river. \r\n\r\nOur conclusions are consistent with the findings of other recent investigations of the same landslides that indicate extensive seismic triggering of coherent slides and earth flows during the 1811-12 New Madrid earthquakes.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1336C","usgsCitation":"Jibson, R.W., and Keefer, D.K., 1988, Landslides triggered by earthquakes in the central Mississippi Valley, Tennessee and Kentucky: U.S. Geological Survey Professional Paper 1336, Report: iv, 24 p.; 1 Plate: 33.00 × 50.50 inches, https://doi.org/10.3133/pp1336C.","productDescription":"Report: iv, 24 p.; 1 Plate: 33.00 × 50.50 inches","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":104604,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4806.htm","linkFileType":{"id":5,"text":"html"},"description":"4806"},{"id":67656,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1336c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67657,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1336c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":125031,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1336c/report-thumb.jpg"}],"country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"central Mississippi Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.075,\n              37.065\n            ],\n            [\n              -90.1333,\n              37.065\n            ],\n            [\n              -90.1333,\n              34.9464\n            ],\n            [\n              -89.075,\n              34.9464\n            ],\n            [\n              -89.075,\n              37.065\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a91c4","contributors":{"authors":[{"text":"Jibson, Randall W. 0000-0003-3399-0875 jibson@usgs.gov","orcid":"https://orcid.org/0000-0003-3399-0875","contributorId":2985,"corporation":false,"usgs":true,"family":"Jibson","given":"Randall","email":"jibson@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":222157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keefer, David K.","contributorId":77930,"corporation":false,"usgs":true,"family":"Keefer","given":"David","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":222158,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39793,"text":"b1713D - 1988 - Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California","interactions":[{"subject":{"id":7331,"text":"ofr82956 - 1982 - Mineral-resource potential of the Whipple Mountains Wilderness Study Area(CDCA-312), San Bernardino County, California","indexId":"ofr82956","publicationYear":"1982","noYear":false,"title":"Mineral-resource potential of the Whipple Mountains Wilderness Study Area(CDCA-312), San Bernardino County, California"},"predicate":"SUPERSEDED_BY","object":{"id":39793,"text":"b1713D - 1988 - Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California","indexId":"b1713D","publicationYear":"1988","noYear":false,"chapter":"D","title":"Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California"},"id":1}],"lastModifiedDate":"2017-07-05T12:49:41","indexId":"b1713D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1713","chapter":"D","title":"Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California","docAbstract":"<p>At the request of the U.S. Bureau of Land Management, approximately 85,100 acres of the Whipple Mountains Wilderness Study Area (CDCA-312) and 1,380 acres of the Whipple Mountains Addition Wilderness Study Area (AZ-050-010) were evaluated for identified mineral resources (known) and mineral resource potential (undiscovered). In this report, the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas are referred to as simply \"the study area.\" </p><p>Most of the mines and prospects with identified resources in the Whipple Mountains Wilderness Study Area are within areas designated as having mineral resource potential. The area in and around the Turk Silver mine and the Lucky Green group and the area near the northwest boundary of the study area have high mineral resource potential for copper, lead, zinc, gold, and silver. An area along the west boundary of the study area has moderate resource potential for copper lead, zinc, gold, and silver. An area in the east adjacent to the Whipple Mountains Addition Wilderness Study Area has moderate resource potential for copper, gold, and silver resources. One area on the north boundary and one on the southeast boundary of the study area have low mineral resource potential for copper, lead, zinc, gold, and silver. Two areas, one on the north boundary and one inside the east boundary of the study area, have moderate resource potential for manganese. A small area inside the south boundary of the study area has high resource potential for decorative building stone, and the entire study area has low resource potential for&nbsp;sand and gravel and other rock products suitable for construction. Two areas in the eastern part of the study area have low resource potential for uranium. There is no resource potential for oil and gas or geothermal resources in the Whipple Mountains Wilderness Study Area. </p><p>Sites within the Whipple Mountains Wilderness Study Area with identified resources of copper, gold, silver, manganese and (or) decorative building stone are located at the Stewart mine, New American Eagle mine, Turk Silver mine, Twin Lode mine, decorative stone property, Lucky Green group, Blue Cloud mine, Nickel Plate mine, Crescent mine, Quadrangle Copper group, and the Copper Basin mine. </p><p>The Whipple Mountains Addition Wilderness Study Area has moderate resource potential for copper, gold, and silver resources and low resource potential for sand and gravel and other rock products. There is no resource potential for oil and gas or for geothermal energy in the Whipple Mountains Addition Wilderness Study Area. </p><p>Although there are no identified resources in the Whipple Mountains Addition Wilderness Study Area, sites within and immediately adjacent warrant further study because of gold assays from widespread, numerous samples.</p>","largerWorkTitle":"Mineral resources of Wilderness Study Areas: Eastern California Desert Conservation Area","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1713D","usgsCitation":"Marsh, S.P., Raines, G.L., Diggles, M.F., Howard, K.A., Simpson, R.W., Hoover, D.B., Ridenour, J., Moyle, P.R., and Willett, S.L., 1988, Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California: U.S. Geological Survey Bulletin 1713, Report: vi, 36 p.; Plate: 36.50 x 25.00 inches, https://doi.org/10.3133/b1713D.","productDescription":"Report: vi, 36 p.; Plate: 36.50 x 25.00 inches","startPage":"D1","endPage":"D36","costCenters":[],"links":[{"id":67672,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1713d/report.pdf","text":"Report","size":"2.02 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":173394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1713d/report-thumb.jpg"},{"id":67671,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1713d/plate-1.pdf","text":"Plate","size":"5.14 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"}],"country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.378662109375,\n              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