{"pageNumber":"355","pageRowStart":"8850","pageSize":"25","recordCount":11004,"records":[{"id":24977,"text":"pp1245 - 1983 - Historical surface deformation near Oildale, California","interactions":[],"lastModifiedDate":"2017-04-25T14:33:04","indexId":"pp1245","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1245","title":"Historical surface deformation near Oildale, California","docAbstract":"<p>Historical surface deformation recognized in the southern San Joaquin Valley and adjacent Sierra Nevada foothills near Oildale, Calif., includes: normal and apparently aseismic dip slip along four faults; subsidence within or adjacent to the Kern Front, Poso Creek, Mount Poso, and Fruitvale oil fields; and uplift of much of the area within and north of the Kern River oil field. As much as 0.34 m of vertical separation has been observed along a 5.2-km segment of the Kern Front fault, the structural barrier separating the Kern Front oil field on the west from the Kern River field to the east. Similar separations of as much as 0.15 m and 0.32 m, respectively, have also been identified along the surface traces of two en echelon faults between the Premier and Enas areas of the Poso Creek oil field and the fault that defines the southeast flank of the Premier area. The measured height changes are based on both unadjusted observed elevations and minimally constrained adjusted elevations developed from repeated control levelings referred to a relatively stable local bench mark; measurement error in the reported vertical movements probably is less than 0.05 m. Differential subsidence of at least 0.31 m (1903-68) and 0.05 m (1926/27/30/31-59) has occurred within the Kern Front and Fruitvale oil fields, respectively; subsidence of as much as 0.33 m (1903-53) and 0.19 m (1931-63) has also been measured along the north edge of the Premier area of the Poso Creek oil field and the south edge of the Main area of the Mount Poso field, respectively. Differential uplift of as much as 0.11 m and 0.13 m occurred within and immediately north of the Kern River oil field between 1903 and 1968, and similar uplift of as much as 0.19 m was measured along the north edge of the Dominion area of the Mount Poso field between 1931 and 1963. </p><p>Differential subsidence within the Kern Front and Fruitvale oil fields and along the edges of the Poso Creek and Mount Poso fields is attributable to subsurface compaction owing to fluid withdrawal; absence of subsidence within the much larger Kern River field probably is the result of either production from compaction-resistant materials or natural water flooding that has acted to preserve reservoir fluid pressures in the generally shallow producing beds. Contemporary displacements on the Kern Front fault and those along the faults within and adjacent to the Poso Creek oil field are attributable largely or entirely to changes in the subsurface stress regime associated with reservoir compaction; accumulated elastic strain of tectonic derivation conceivably contributed to the development of these displacements. The apparent uplift within and north of the Kern River oil field and along the north edge of the Mount Poso field probably is due in part to compaction of as much as 0.055 m beneath the reference bench mark; most of this apparent uplift, however, is interpreted as an effect of tectonic tilting.</p>","language":"English","publisher":"U.S. Government Publishing Office","doi":"10.3133/pp1245","usgsCitation":"Castle, R.O., Church, J.P., Yerkes, R.F., and Manning, J.C., 1983, Historical surface deformation near Oildale, California: U.S. Geological Survey Professional Paper 1245, Report: iv, 42 p.; 2 Plates: 25.12 x 36.22 inches and 29.04 x 39.66 inches, https://doi.org/10.3133/pp1245.","productDescription":"Report: iv, 42 p.; 2 Plates: 25.12 x 36.22 inches and 29.04 x 39.66 inches","costCenters":[],"links":[{"id":104580,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4766.htm","linkFileType":{"id":5,"text":"html"},"description":"4766"},{"id":126340,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1245/report-thumb.jpg"},{"id":53963,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1245/report.pdf","text":"Report","size":"4.09 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":340319,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1245/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":340320,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1245/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.2,\n              35.3\n            ],\n            [\n              -118.8,\n              35.3\n            ],\n            [\n              -118.8,\n              35.7\n            ],\n            [\n              -119.2,\n              35.7\n            ],\n            [\n              -119.2,\n              35.3\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c2a7","contributors":{"authors":[{"text":"Castle, Robert O.","contributorId":22741,"corporation":false,"usgs":true,"family":"Castle","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":192930,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Church, Jack P.","contributorId":6480,"corporation":false,"usgs":true,"family":"Church","given":"Jack","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":192928,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yerkes, Robert F.","contributorId":64239,"corporation":false,"usgs":true,"family":"Yerkes","given":"Robert","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":192931,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Manning, John C.","contributorId":10460,"corporation":false,"usgs":true,"family":"Manning","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":192929,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7624,"text":"ofr83157 - 1983 - Proceedings of Conference XVIII: a workshop on \"Continuing actions to reduce losses from earthquakes in the Mississippi Valley area,\" 24-26 May, 1982, St. Louis, Missouri","interactions":[],"lastModifiedDate":"2018-09-19T18:47:58","indexId":"ofr83157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-157","title":"Proceedings of Conference XVIII: a workshop on \"Continuing actions to reduce losses from earthquakes in the Mississippi Valley area,\" 24-26 May, 1982, St. Louis, Missouri","docAbstract":"<p>The U.S. Geological Survey and the Federal Emergency Management Agency \nsponsored a workshop on, \"Continuing Actions to Reduce Losses from Earthquakes \nin the Mississippi Valley area,\" in St. Louis, Missouri, on May 24-26, 1982. \nSeventy individuals (see Appendix A) representing local, State, and Federal \ngovernment; business and industry; and the research community participated in \nthe three day workshop. Collectively, the participants had backgrounds in \ndisaster preparedness, disaster response and recovery, geology, geophysics, \nseismology, engineering, architecture, social science, law, insurance, and \nland-use planning. Two-thirds of them came from the Mississippi Valley area\nabout one half of these had also attended an earlier USGS-FEMA workshop held \nin Knoxville, Tennessee on September 16-18, 1981 (Hays, 1982).</p>\n<br/>\n<p>The St. Louis workshop is the 18th in the continuing series of \nconferences and workshops which the Geological Survey initiated in 1977 to \nimprove the transfer and application of research results throughout the \nNation. It is the second workshop to focus on dealing with the earthquake \nthreat in the Eastern United States. The first one, \"Preparing for and \nResponding to a Damaging Earthquake in the Eastern United States,\" was held in \nKnoxville, Tennessee, and emphasized the development of a draft 5-year plan to \nimprove the state-of-earthquake-preparedness. The Knoxville workshop \ndemonstrated that policymakers and members of the scientific-technical \ncommunity can assimilate and synthesize a great deal of information and work \ntogether to devise practical plans. The St. Louis workshop, a sequel to the \nKnoxville workshop, identified those actions out of the range of possible \nactions which are most achievable; that is, the actions having the highest\npayoff and trre lowest cost and effort requirements. These action plans, which \nidentify steps that can be undertaken immediately to reduce losses from \nearthquakes in each of the seven States in the Mississippi Valley area, are \ncontained in this report. The draft 5-year plan for the Central United \nStates, prepared in the Knoxville workshop, was the starting point of the \nsmall group discussions in the St. Louis workshop which lead to the action \nplans contained in this report. For completeness, the draft 5-year plan for \nthe Central United States is reproduced as Appendix B.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83157","usgsCitation":"Hays, W., and Kitzmiller, C., 1983, Proceedings of Conference XVIII: a workshop on \"Continuing actions to reduce losses from earthquakes in the Mississippi Valley area,\" 24-26 May, 1982, St. Louis, Missouri: U.S. Geological Survey Open-File Report 83-157, 140 p., https://doi.org/10.3133/ofr83157.","productDescription":"140 p.","numberOfPages":"169","costCenters":[{"id":414,"text":"National Earthquake Hazards Reduction Program","active":false,"usgs":true}],"links":[{"id":139730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0157/report-thumb.jpg"},{"id":277916,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0157/report.pdf"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660813","contributors":{"editors":[{"text":"Gori, Paula L.","contributorId":75520,"corporation":false,"usgs":true,"family":"Gori","given":"Paula","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":745696,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Hays, Walter W.","contributorId":66669,"corporation":false,"usgs":true,"family":"Hays","given":"Walter W.","affiliations":[],"preferred":false,"id":156330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kitzmiller, Carla (compiler)","contributorId":27852,"corporation":false,"usgs":true,"family":"Kitzmiller","given":"Carla","suffix":"(compiler)","email":"","affiliations":[],"preferred":false,"id":156329,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46247,"text":"ofr82116 - 1983 - Map showing ground-water conditions in the Tonto basin area, Gila County, Arizona; 1978-79","interactions":[],"lastModifiedDate":"2022-04-20T22:40:32.0983","indexId":"ofr82116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-116","title":"Map showing ground-water conditions in the Tonto basin area, Gila County, Arizona; 1978-79","docAbstract":"<p>The Tonto basin area includes about 955 mi<sup>2</sup> in central Arizona. The area is bounded on the north by the Mogollon Rim, on the east by the Sierra Ancha Mountains, on the west by the Mazatzal Mountains, and on the south by Theodore Roosevelt Lake. The area is drained by Tonto Creek, which flows north to south and discharges into Theodore Roosevelt Lake.&nbsp;</p><p>Because the Tonta basin area is entirely within the Tonto National Forest, only about 3 percent of the land is privately owned and, for the most part, wells inventoried were on private land. Only selected wells are shown on the map because of the high well density on the private land.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82116","collaboration":"Prepared in cooperation with the Arizona Department of Water Resources","usgsCitation":"Denis, E., 1983, Map showing ground-water conditions in the Tonto basin area, Gila County, Arizona; 1978-79: U.S. Geological Survey Open-File Report 82-116, 1 Plate: 31.41 x 36.54 inches, https://doi.org/10.3133/ofr82116.","productDescription":"1 Plate: 31.41 x 36.54 inches","costCenters":[],"links":[{"id":399364,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0116/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0116/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Gila County","otherGeospatial":"Tonto basin area","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"98\",\"properties\":{\"name\":\"Gila\",\"state\":\"AZ\"},\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-111.543,34.4692],[-111.541,34.4719],[-111.536,34.4719],[-111.537,34.4696],[-111.529,34.4705],[-111.526,34.4751],[-111.522,34.4778],[-111.52,34.4827],[-111.522,34.4878],[-111.521,34.4991],[-111.518,34.4991],[-111.519,34.4955],[-111.508,34.4981],[-111.501,34.4977],[-111.51,34.4936],[-111.511,34.4895],[-111.512,34.4868],[-111.509,34.4782],[-111.512,34.4795],[-111.512,34.4732],[-111.519,34.4664],[-111.521,34.4628],[-111.522,34.4637],[-111.53,34.4619],[-111.537,34.4592],[-111.54,34.4565],[-111.534,34.4542],[-111.523,34.4551],[-111.521,34.4573],[-111.518,34.4559],[-111.512,34.4555],[-111.501,34.459],[-111.487,34.4622],[-111.486,34.464],[-111.481,34.4621],[-111.472,34.4626],[-111.474,34.4598],[-111.472,34.4571],[-111.476,34.4594],[-111.48,34.4549],[-111.477,34.4508],[-111.484,34.4535],[-111.489,34.454],[-111.49,34.4504],[-111.494,34.4517],[-111.496,34.4463],[-111.499,34.4463],[-111.503,34.4436],[-111.502,34.4418],[-111.507,34.4377],[-111.508,34.4404],[-111.513,34.4436],[-111.519,34.4459],[-111.517,34.44],[-111.52,34.4378],[-111.518,34.431],[-111.522,34.4269],[-111.525,34.4301],[-111.529,34.4224],[-111.537,34.4247],[-111.54,34.4283],[-111.544,34.4229],[-111.551,34.4197],[-111.547,34.4174],[-111.546,34.4147],[-111.543,34.4165],[-111.54,34.4151],[-111.537,34.4119],[-111.528,34.411],[-111.519,34.4128],[-111.512,34.4159],[-111.511,34.4191],[-111.505,34.4218],[-111.5,34.4272],[-111.498,34.4209],[-111.494,34.4186],[-111.493,34.4231],[-111.495,34.4345],[-111.489,34.4304],[-111.485,34.4304],[-111.484,34.4349],[-111.481,34.4335],[-111.478,34.4312],[-111.468,34.4366],[-111.472,34.4303],[-111.479,34.4253],[-111.479,34.414],[-111.466,34.4139],[-111.46,34.4239],[-111.454,34.4261],[-111.451,34.4311],[-111.441,34.437],[-111.436,34.446],[-111.426,34.4478],[-111.418,34.4446],[-111.409,34.4427],[-111.408,34.4468],[-111.403,34.444],[-111.398,34.4431],[-111.4,34.4404],[-111.406,34.4386],[-111.405,34.43],[-111.407,34.4272],[-111.412,34.4336],[-111.416,34.4323],[-111.418,34.435],[-111.424,34.4351],[-111.422,34.4291],[-111.426,34.4196],[-111.423,34.4083],[-111.423,34.4028],[-111.425,34.3942],[-111.423,34.3887],[-111.418,34.381],[-111.413,34.3819],[-111.409,34.3773],[-111.403,34.3786],[-111.398,34.3818],[-111.387,34.3876],[-111.384,34.3908],[-111.389,34.3917],[-111.39,34.3945],[-111.387,34.3972],[-111.394,34.3981],[-111.412,34.4091],[-111.406,34.4086],[-111.401,34.4109],[-111.4,34.4154],[-111.401,34.4259],[-111.397,34.4286],[-111.396,34.4254],[-111.392,34.424],[-111.388,34.4253],[-111.386,34.4308],[-111.379,34.4317],[-111.374,34.4384],[-111.368,34.4393],[-111.365,34.4384],[-111.363,34.4356],[-111.358,34.4397],[-111.354,34.4402],[-111.352,34.4324],[-111.355,34.4292],[-111.353,34.4238],[-111.337,34.4237],[-111.326,34.4227],[-111.321,34.4272],[-111.314,34.4299],[-111.296,34.4366],[-111.281,34.4388],[-111.268,34.4424],[-111.259,34.4468],[-111.252,34.4527],[-111.245,34.449],[-111.249,34.4427],[-111.246,34.4413],[-111.239,34.4313],[-111.235,34.4299],[-111.228,34.4312],[-111.225,34.4257],[-111.223,34.4257],[-111.222,34.4166],[-111.199,34.4097],[-111.19,34.4073],[-111.178,34.4086],[-111.177,34.404],[-111.17,34.4031],[-111.159,34.3976],[-111.15,34.3871],[-111.151,34.3789],[-111.147,34.3752],[-111.142,34.3811],[-111.138,34.387],[-111.13,34.3869],[-111.128,34.3905],[-111.121,34.3846],[-111.115,34.3845],[-111.106,34.3885],[-111.1,34.3939],[-111.094,34.3966],[-111.08,34.3892],[-111.076,34.3865],[-111.077,34.3801],[-111.06,34.3782],[-111.043,34.3794],[-111.037,34.3716],[-111.043,34.3703],[-111.057,34.3536],[-111.054,34.3536],[-111.045,34.3426],[-111.03,34.3411],[-111.032,34.3493],[-111.029,34.3511],[-111.034,34.3625],[-111.026,34.3638],[-111.025,34.3688],[-111.02,34.3715],[-111.021,34.3619],[-111.01,34.3596],[-111.008,34.3623],[-111.004,34.3573],[-111.005,34.3518],[-110.998,34.3513],[-110.996,34.3499],[-110.997,34.3445],[-110.989,34.3421],[-110.975,34.3366],[-110.968,34.3251],[-110.963,34.3183],[-110.955,34.3128],[-110.953,34.3186],[-110.945,34.3172],[-110.943,34.3113],[-110.928,34.3107],[-110.906,34.3],[-110.898,34.3027],[-110.894,34.2995],[-110.896,34.2958],[-110.884,34.2903],[-110.888,34.2862],[-110.884,34.2803],[-110.877,34.2757],[-110.858,34.2701],[-110.847,34.2686],[-110.844,34.269],[-110.826,34.2784],[-110.835,34.278],[-110.838,34.2803],[-110.831,34.282],[-110.825,34.2865],[-110.821,34.2878],[-110.824,34.2942],[-110.83,34.2975],[-110.844,34.304],[-110.846,34.3072],[-110.839,34.308],[-110.834,34.3048],[-110.818,34.2992],[-110.812,34.295],[-110.807,34.3109],[-110.804,34.3109],[-110.803,34.2972],[-110.797,34.299],[-110.795,34.3067],[-110.788,34.3098],[-110.788,34.2975],[-110.782,34.3079],[-110.783,34.2993],[-110.779,34.2983],[-110.759,34.284],[-110.757,34.2781],[-110.762,34.2732],[-110.765,34.2682],[-110.758,34.2599],[-110.751,34.2621],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E.E.","contributorId":53756,"corporation":false,"usgs":true,"family":"Denis","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":232939,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59810,"text":"mf1231D - 1983 - Map showing aeromagnetic interpretation of the Golden Trout Wilderness, Tulare and Inyo counties, California","interactions":[],"lastModifiedDate":"2016-08-22T14:02:14","indexId":"mf1231D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1231","chapter":"D","title":"Map showing aeromagnetic interpretation of the Golden Trout Wilderness, Tulare and Inyo counties, California","docAbstract":"<p>The Golden Trout Wilderness covers 457 mi<sup>2</sup><sup>&nbsp;</sup>in the rugged forested part of the southern Sierra Nevada. &nbsp;It is bounded on the east by Owens Valley, on the north by Sequoia National Park, and on the west and south by U.S. Forest Service multiple-use lands. &nbsp;The east side of the area is accesible from U.S. Highway 395, while the remainder is reached by state, county, and Forest Service roads from the San Joaquin Valley.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1231D","usgsCitation":"Jachens, R.C., and Elder, W.P., 1983, Map showing aeromagnetic interpretation of the Golden Trout Wilderness, Tulare and Inyo counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 1231, 57.03 x 40.42 inches, https://doi.org/10.3133/mf1231D.","productDescription":"57.03 x 40.42 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1231D.PNG"},{"id":327286,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1231-D/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","county":"Inyo County, Tulare County","otherGeospatial":"Golden Trout Wilderness","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.75,36.083333333333336 ], [ -118.75,36.5 ], [ -118,36.5 ], [ -118,36.083333333333336 ], [ -118.75,36.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658e59","contributors":{"authors":[{"text":"Jachens, Robert C. jachens@usgs.gov","contributorId":1180,"corporation":false,"usgs":true,"family":"Jachens","given":"Robert","email":"jachens@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":262634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elder, William P.","contributorId":61058,"corporation":false,"usgs":true,"family":"Elder","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":262635,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59808,"text":"mf1540B - 1983 - Aeromagnetic map and interpretation of geophysical data from the Condrey Mountain Roadless Area, Siskiyou County, California","interactions":[],"lastModifiedDate":"2016-08-22T14:06:01","indexId":"mf1540B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1540","chapter":"B","title":"Aeromagnetic map and interpretation of geophysical data from the Condrey Mountain Roadless Area, Siskiyou County, California","docAbstract":"<p>The Condrey Mountain Roadless Area lies within the Klamath Mountains geologic province, a province composed of four eastward-dipping imbricate thrust slices or belts consisting predominantly of marine arc-related volcanic and sedimentary rocks, but also including significant amounts of ultramafic and other ophiolitic rocks (Irwin, 1981). From west to east the four Klamath Mountains thrust slices are called the western Jurassic belt, the western Paleozoic and Triassic belt, the central metamorphic belt, and the eastern Klamath belt. The Condrey Mountain Road less Area is located within a structural window in the western Paleozoic and Triassic belt, a window in which the structural dome comprised of the Condrey Mountain Schist is exposed (Coleman and others, 1983). North, east and south of the roadless area, the Condrey Mountain Schist is separated from the overlying western Paleozoic and Triassic belt by a low-angle regional thrust, whereas to the west the two units are in high-angle fault contact (Coleman and others, 1983).</p>\n<p>The Condrey Mountain schist consists mainly of sedimentary and volcanic rocks metamorphosed to greenschist facies. Metasedimentary rocks are exposed over most of the eastern and central parts of the structural window. Metavolcanic rocks occupy the western part of the window but also occur in small exposures within the metasedimentary rocks and along the eastern and southern margins of the window. Tabular bodies of metaserpentinite, the largest of which crops out near White Mountain, are contained within the metasedimentary rocks. Densities of hand samples from 11 sites scattered throughout the Condrey Mountain window average 2.66&plusmn;0.05 g/cm<sup>3</sup>. The four samples of metavolcanic rocks yielded a higher average density than the seven samples of metasedimentary rocks (2.71&plusmn;0.04 g/cm<sup>3</sup> versus 2.63&plusmn;0.03 g/cm<sup>3</sup>).</p>\n<p>Along the western edge of the Condrey Mountain Road less Area, numerous narrow north-trending zones of mineralized schist extend from near Copper Butte on the south, northward to Elliot Creek (Coleman and others, 1983). These zones contain abundant pyrite mineralization associated with pyrrhotite, chalcopyrite, qalena, and sphalerite. The Blue Ledge mine area, 2 mi north-northeast of Copper Butte, is located in a zone of mineralized schist.</p>\n<p>The western Paleozoic and Triassic belt that nearly surrounds the Condrey Mountain Schist is a melange of sedimentary, volcanic, and ultramafic rocks metamorphosed to amphibolite facies (Coleman and others, 1983). Only two samples of the metamorphic melange were collected near the Condrcy Mountain Road less Area, but extensive sampling of this unit southwest of the roadless area yielded an average sample density of 2.86&plusmn;0.15 g/cm<sup>3</sup> (112 samples) (Jachens and others, 1983).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1540B","usgsCitation":"Jachens, R., and Elder, W., 1983, Aeromagnetic map and interpretation of geophysical data from the Condrey Mountain Roadless Area, Siskiyou County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1540, Plate: 47.54 x 29.96 inches, https://doi.org/10.3133/mf1540B.","productDescription":"Plate: 47.54 x 29.96 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1540B.JPG"},{"id":327288,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1540-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","county":"Siskiyou County","otherGeospatial":"Condrey Mountain Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.25,41.833333333333336 ], [ -123.25,42 ], [ -122.75,42 ], [ -122.75,41.833333333333336 ], [ -123.25,41.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69835b","contributors":{"authors":[{"text":"Jachens, R.C.","contributorId":55433,"corporation":false,"usgs":true,"family":"Jachens","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":262631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elder, W.P.","contributorId":65467,"corporation":false,"usgs":true,"family":"Elder","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":262632,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61514,"text":"mf1554 - 1983 - Environmental-stratigraphic cross sections of the Cretaceous Fox Hills Sandstone and Hell Creek Formation and Paleocene Fort Union Formation, Richland and Roosevelt Counties, Montana","interactions":[],"lastModifiedDate":"2016-08-23T10:42:11","indexId":"mf1554","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1554","title":"Environmental-stratigraphic cross sections of the Cretaceous Fox Hills Sandstone and Hell Creek Formation and Paleocene Fort Union Formation, Richland and Roosevelt Counties, Montana","docAbstract":"<p>This study was conducted to determine the stratigraphic, lithofacies, and deopsitional relationships of the Cretaceous Fox Hills Sandstone and Hell Creek Formation and The Paleocene Fort Union Formation. These relationships, shown in sections A-A', B-B', C-C', and D-D', we established form nearly continuous exposures in the Missouri River valley in Richland and Roosevelt Counties, Mont. The river valley topography is characterized by badlands, which permitted detailed description and construction of the stratigraphic framework of the formations within a 30-mi-long belt of exposures paralleling the Missouri River. This area of study is on the western flank of the Williston Basin and east of the Poplar Dome. The latter structure imparted a northeasterly regional dip to the rocks, which averages 25 ft per mi and is as much as 100 ft per mi according to Spencer (1980). The regional dip resulted in exposure of older rocks (Cretaceous) in the west to younger rocks (Tertiary) in the east.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1554","isbn":"0607812842","usgsCitation":"Flores, R.M., and Lepp, C., 1983, Environmental-stratigraphic cross sections of the Cretaceous Fox Hills Sandstone and Hell Creek Formation and Paleocene Fort Union Formation, Richland and Roosevelt Counties, Montana: U.S. Geological Survey Miscellaneous Field Studies Map 1554, 42.07 x 49.32 in, https://doi.org/10.3133/mf1554.","productDescription":"42.07 x 49.32 in","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1554.PNG"},{"id":327610,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1554/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","country":"United States","state":"Montana","otherGeospatial":"Missouri River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105,48.083333333333336 ], [ -105,48.166666666666664 ], [ -104.35111111111111,48.166666666666664 ], [ -104.35111111111111,48.083333333333336 ], [ -105,48.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602208","contributors":{"authors":[{"text":"Flores, R. M.","contributorId":106899,"corporation":false,"usgs":true,"family":"Flores","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":265852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lepp, C.L.","contributorId":76821,"corporation":false,"usgs":true,"family":"Lepp","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":265851,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44509,"text":"wri834200 - 1983 - Hydrogeologic and water-quality characteristics of the St. Peter aquifer, Southeast Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T11:27:11","indexId":"wri834200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4200","title":"Hydrogeologic and water-quality characteristics of the St. Peter aquifer, Southeast Minnesota","docAbstract":"<p>Quality of water in the St. Peter aquifer is generally acceptable for most uses. Sulfate concentrations increase toward the southwestern part of the aquifer because of highly mineralized leakage from overlying Cretaceous deposits. Concentrations of sodium, magnesium, and sulfate generally increase to the west, and those of calcium, bicarbonate, and chloride generally increase toward the margins of the aquifer. Calcium magnesium bicarbonate water is the most common type in the aquifer. The aquifer is well protected from surface sources of Contaminants by the overlying Decorah-Platteville-Glenwood confining bed, which overlies about 80 percent of the St. Peter aquifer. Thin drift, which overlies the east side of the aquifer, provides much less protection than the confining bed. Water in the aquifer generally flows toward the Mississippi River and its tributaries. Some water flows southward into Iowa from a ground-water divide in Dodge and Steele Counties, Well yields from the aquifer, which are generally between 100 and 250 gallons per minute, are generally adequate for most uses.</p>\n<p>This report is one of a series on the hydrogeology and water quality of the 14 principal aquifers in Minnesota prepared by the U.S. Geological Survey. The U. S. Environmental Protection Agency requested these studies because of the need for information to develop its Underground Injection Control Program.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri834200","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Ruhl, J.F., and Wolf, R.J., 1983, Hydrogeologic and water-quality characteristics of the St. Peter aquifer, Southeast Minnesota: U.S. Geological Survey Water-Resources Investigations Report 83-4200, 2 Plates: 39.91 x 34.63 inches and 39.75 x 34.64 inches, https://doi.org/10.3133/wri834200.","productDescription":"2 Plates: 39.91 x 34.63 inches and 39.75 x 34.64 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":170402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81890,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4200/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81891,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4200/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"St. Peter aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.8619384765625,\n              45.71385093029221\n            ],\n            [\n              -93.3837890625,\n              45.706179285330855\n            ],\n            [\n          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-92.8729248046875,\n              45.6178796835697\n            ],\n            [\n              -92.8619384765625,\n              45.71385093029221\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628d25","contributors":{"authors":[{"text":"Ruhl, J. F.","contributorId":81866,"corporation":false,"usgs":true,"family":"Ruhl","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":229906,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolf, R. J.","contributorId":21518,"corporation":false,"usgs":true,"family":"Wolf","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229905,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62063,"text":"mf1555B - 1983 - Aeromagnetic map of the West Clear Creek roadless area, Coconino and Yavapai Counties, Arizona","interactions":[],"lastModifiedDate":"2016-08-23T10:42:17","indexId":"mf1555B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1555","chapter":"B","title":"Aeromagnetic map of the West Clear Creek roadless area, Coconino and Yavapai Counties, Arizona","docAbstract":"<p>The West Clear Creek Roadless Area lies within the Coconino National Forest in central Arizona (fig. 1) and includes parts of Yavapai and Coconino Counties. Camp Verde, the nearest population center, is approximately 7 miles (11 km) west of the area. West Clear Creek canyon begins on the east at the confluence of the incised gorges of Willow Valley and of Clover Creek and is joined toward the west by Black Mountain Canyon. The canyon of West Clear Creek is very rugged; in several places it is more than 1,900 ft (580 m) deep. Creek elevation ranges from 6,100 ft (1,860 m) near the junction with Clover Creek to 3,200 ft (975 m) at the mouth of the canyon. The elevation of peaks and ridges near the canyon range from 4,000 ft (1,220 m) to 7,000 ft (2,135 m). Uplands at the head of Willow Valley and Clover Creek reach elevations up to 7,100 ft (2,165 m) above sea level.</p>\n<p>The greater part of the surface is underlain by late Tertiary volcanic rocks, mainly alkali olivine basalts. These overlie Lower Per i an sedimentary rocks consisting mostly of dolomite, limestone, and sandstone strata that dip gently westward. Late Tertiary and Quaternary sedimentary rocks and deposits mantle several ridges (terrace gravels) and cover basalt flows in Verde Valley at the west end of the area (Verde Formation). Quaternary alluvial deposits occur in the main West Clear Creek drainage and its larger tributaries at the west end of the area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1555B","usgsCitation":"Davis, W., and Ulrich, G.E., 1983, Aeromagnetic map of the West Clear Creek roadless area, Coconino and Yavapai Counties, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1555, 38.10 x 56.57 inches, https://doi.org/10.3133/mf1555B.","productDescription":"38.10 x 56.57 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":186936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1555B.JPG"},{"id":327611,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1555-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Arizona","county":"Coconino County, Yavapai County","otherGeospatial":"West Clear Creek Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.78416666666666,34.5 ], [ -111.78416666666666,34.6175 ], [ -111.33333333333333,34.6175 ], [ -111.33333333333333,34.5 ], [ -111.78416666666666,34.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68bea8","contributors":{"authors":[{"text":"Davis, Willard E.","contributorId":8549,"corporation":false,"usgs":true,"family":"Davis","given":"Willard E.","affiliations":[],"preferred":false,"id":266841,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ulrich, George E.","contributorId":23550,"corporation":false,"usgs":true,"family":"Ulrich","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":266842,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48833,"text":"ofr83671 - 1983 - Tens of successive, colossal Missoula floods at north and east margins of channeled scabland","interactions":[],"lastModifiedDate":"2022-12-28T22:56:03.490071","indexId":"ofr83671","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-671","title":"Tens of successive, colossal Missoula floods at north and east margins of channeled scabland","docAbstract":"In deposits of Pleistocene glacial lakes in northern Idaho and Washington, beds comprising 20 to 55 varves (average = 35-40) separate each successive graded gravel or sand bed that was swiftly emplaced by a catastrophic flood from glacial Lake Missoula. The floodlaid beds are similar to rhythmic successions of 40 or more graded beds in backflooded tributaries of the lower Columbia River. This new field evidence corroborates a controversial hypothesis that the great Pleistocene floods from glacial Lake Missoula were 40 or more colossal, separate joekulhlaups, and refutes the conventional notion that any two successive graded beds were deposited by one flood. \r\n\r\nThe only outlet of the 2000-km3 glacial Lake Missoula was through its great ice dam. Calculations show that each time the lake rose to about 600 m deep, it made the glacier buoyant and engendered a catastrophic discharge along the glacier bed (a joekulhlaup). A reconstructed water budget suggests that after a complete draining, the lake refilled in 3 to 6 decades; thus the hydrostatic prerequisites for a joekulhlaup were reestablished dozens of times during the late-Wisconsin episode of lake damming. \r\n\r\nVarious intercalated tephra layers, radiocarbon dates, varve successions, and the Bonneville flood deposits in the region suggest that late-Wisconsin glacial Lake Missoula existed for about 2 millennia within the period 15,000 to 12,700(?) yr ago. Varve beds indicate that the mean period between Missoula floods was about 4 decades, but became shorter during the last several floods. Between 20 and 30 of the Missoula joekulhlaups occurred after the single great flood from Lake Bonneville, which according to 14C dating in the Bonneville basin by W. E. Scott and associates and by D. R. Currey occurred some time between 15,000 and 14,000 yr ago.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83671","usgsCitation":"Waitt, R.B., 1983, Tens of successive, colossal Missoula floods at north and east margins of channeled scabland: U.S. Geological Survey Open-File Report 83-671, 29 p., https://doi.org/10.3133/ofr83671.","productDescription":"29 p.","costCenters":[],"links":[{"id":411160,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75698.htm","linkFileType":{"id":5,"text":"html"}},{"id":85666,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0671/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162658,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0671/report-thumb.jpg"}],"country":"United States","state":"Idaho, Montana, Oregon, Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -124,\n              49\n            ],\n            [\n              -124,\n              45\n            ],\n            [\n              -113.5,\n              45\n            ],\n            [\n              -113.5,\n              49\n            ],\n            [\n              -124,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db685155","contributors":{"authors":[{"text":"Waitt, Richard B. 0000-0002-6392-5604 waitt@usgs.gov","orcid":"https://orcid.org/0000-0002-6392-5604","contributorId":2343,"corporation":false,"usgs":true,"family":"Waitt","given":"Richard","email":"waitt@usgs.gov","middleInitial":"B.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":238384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48823,"text":"ofr83433A - 1983 - Nevada - basic data for thermal springs and wells as recorded in Geotherm; Part A","interactions":[],"lastModifiedDate":"2024-06-07T18:39:43.046879","indexId":"ofr83433A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-433","chapter":"A","title":"Nevada - basic data for thermal springs and wells as recorded in Geotherm; Part A","docAbstract":"<p>GEOTHERM, a computerized information system now off-line, was used to maintain data on the geology, geochemistry and hydrology of geothermal sites primarily within the United States. The system was proposed at the First Geothermal Implementation Conference in New Zealand in 1974 (Swanson, 1977) and was active until 1983. The primary mission was to provide a broad informational framework for the Geothermal Research Program (Duffield and Guffanti, 1981). GEOTHERM was used to support national geothermal assessments--in 1978 (Muffler, 1979) and 1982 (Reed, 1983). It was however a public system and provided data to both public and private sectors. A detailed discussion on databases in GEOTHERM and a general scheme of how the information system operated can be found in Bliss and Rapport (1983).</p><p>This report on Nevada is one of a series intended to preserve the data collected for GEOTHERM and make the data available to the public. This report will give summaries and sources of records for Nevada. The complete records for Nevada can be found in a companion report, U.S. Geological Survey Open-File Report 83-433B, which is issued as MICROFICHE ONLY. States with significant geochemical data for geothermal fluids will be covered in individual reports such as this. A report will also be issued to cover miscellaneous data collected for sites in the central and eastern United States. The data presented this series is also available as a data file on the internationally-available General Electric Mark III service, a timeshare network. Those interested in accessing that system should contact the Energy Resource Center, University of Oklahoma, Norman, Oklahoma 73070. It is anticipated that a portion of the data will also be available on magnetic tape from the National Technical Information Service, U. S. Department of Commerce, Springfield, VA 22161. It will not be available until after the completion of the open-file series.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83433A","usgsCitation":"Bliss, J.D., 1983, Nevada - basic data for thermal springs and wells as recorded in Geotherm; Part A: U.S. Geological Survey Open-File Report 83-433, 101 p., https://doi.org/10.3133/ofr83433A.","productDescription":"101 p.","costCenters":[],"links":[{"id":429671,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0433-a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161589,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0433-a/report-thumb.jpg"}],"country":"United 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,{"id":57247,"text":"wdrVA821 - 1983 - Water resources data--Virginia, water year 1982","interactions":[],"lastModifiedDate":"2020-11-25T18:41:31.061786","indexId":"wdrVA821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"VA-82-1","title":"Water resources data--Virginia, water year 1982","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrVA821","usgsCitation":"Prugh, B., Easton, F., and Lynch, D.D., 1983, Water resources data--Virginia, water year 1982: U.S. Geological Survey Water Data Report VA-82-1, xi, 460 p., https://doi.org/10.3133/wdrVA821.","productDescription":"xi, 460 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Jr.","contributorId":38226,"corporation":false,"usgs":true,"family":"Prugh","given":"B.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":256457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Easton, F.J.","contributorId":61096,"corporation":false,"usgs":true,"family":"Easton","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":256458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lynch, D. D.","contributorId":12075,"corporation":false,"usgs":true,"family":"Lynch","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":256456,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60415,"text":"mf1537 - 1983 - Maps showing geology and shallow structure of western Rhode Island Sound, Rhode Island","interactions":[],"lastModifiedDate":"2022-04-08T20:10:19.843819","indexId":"mf1537","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1537","title":"Maps showing geology and shallow structure of western Rhode Island Sound, Rhode Island","docAbstract":"<p><span>This report presents the results of a high-resolution, seismic-reflection, and sidescan-sonar survey conducted in western Rhode Island Sound south of Narragansett Bay (fig. 1 inset) by the U.S. Geological Survey in 1980. The study defines the geologic framework of the Atlantic Inner Continental Shelf between lat. 41°09' and 41°32'N and long. 71°07' and 71°37'W. A total of 580 kilometers (km) of seismic-reflection profiles and 580 km of sidescan sonographs was collected aboard the RV Neecho. Trackline spacing was 1 to 2 km at the mouth of Narragansett Bay, and dip lines were 2 km apart with widely spaced strike lines in Rhode Island Sound (fig. 1). The maps in this report adjoin those for eastern Rhode Island Sound and Vineyard Sound, Massachusetts, of O'Hara and Oldale (1980).</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1537","usgsCitation":"Needell, S.W., O’Hara, C.J., and Knebel, H.J., 1983, Maps showing geology and shallow structure of western Rhode Island Sound, Rhode Island: U.S. Geological Survey Miscellaneous Field Studies Map 1537, 34 p., https://doi.org/10.3133/mf1537.","productDescription":"34 p.","temporalStart":"1980-01-01","temporalEnd":"1980-12-31","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":183285,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":398418,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7599.htm"},{"id":12764,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/1983/mf-1537/","linkFileType":{"id":5,"text":"html"}},{"id":398419,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1983/mf-1537/pdf/mf-1537.pdf"}],"country":"United States","state":"Rhode Island","otherGeospatial":"Rhode Island Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.6178,\n              41.2\n            ],\n            [\n              -71.1178,\n              41.2\n            ],\n            [\n              -71.1178,\n              41.5\n            ],\n            [\n              -71.6178,\n              41.5\n            ],\n            [\n              -71.6178,\n              41.2\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d29d","contributors":{"authors":[{"text":"Needell, Sally W.","contributorId":106874,"corporation":false,"usgs":true,"family":"Needell","given":"Sally","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":263707,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Hara, Charles J.","contributorId":11228,"corporation":false,"usgs":true,"family":"O’Hara","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":263705,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knebel, Harley J.","contributorId":25930,"corporation":false,"usgs":true,"family":"Knebel","given":"Harley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":263706,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":59340,"text":"mf1577D - 1983 - Aeromagnetic map of the Arnold Mesa Roadless Area, Yavapai County, Arizona","interactions":[],"lastModifiedDate":"2016-08-22T10:15:54","indexId":"mf1577D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1577","chapter":"D","title":"Aeromagnetic map of the Arnold Mesa Roadless Area, Yavapai County, Arizona","docAbstract":"<p><span>The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and be submitted to the President&nbsp;and the Congress. This report presents the results of an aeromagnetic survey of the&nbsp;Arnold Mesa Roadless Area (U.S. Forest Service number 03092) in the Prescott and Tonto National Forests,&nbsp;Yavapai County, Arizona. The&nbsp;Arnold Mesa Roadless Area was classified&nbsp;as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.</span></p>\n<p><span>The&nbsp;Arnold Mesa Roadless Area is within the transition zone between the Colorado Plateaus to the northeast and the Basin and Range province to the southwest. The transition zone is a belt about 701 miles (120 km) wide that extends diagonally from northwest to south east across central Arizona and parallels the topographic margin of the plateaus. The study area is underlain by Precambrian rocks and gently dipping Paleozoic strata that are largely covered by basaltic lavas and pyroclastic deposits of Miocene age ( McKee and Anderson, 1971). Dacite breccia and tuff are locally interbedded with the basaltic rocks. Sedimentary deposits of late Cenozoic age are dominant in the Verde Valley from about Chasm Creek north; they accumulated in a depositional basin bounded on the west by the Verde fault.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1577D","usgsCitation":"Davis, W., and Wolfe, E.W., 1983, Aeromagnetic map of the Arnold Mesa Roadless Area, Yavapai County, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1577, 49.43 x 35.85 inches, https://doi.org/10.3133/mf1577D.","productDescription":"49.43 x 35.85 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/MF1577D.PNG"},{"id":327199,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1577-D/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Arizona","county":"Yavapai County","otherGeospatial":"Arnold Mesa Roadless Area, Prescott National Forest, Tonto National Forest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112,\n              34.5\n            ],\n            [\n              -112,\n              34.2\n            ],\n            [\n              -111.6,\n              34.2\n            ],\n            [\n              -111.6,\n              34.5\n            ],\n            [\n              -112,\n              34.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6972f1","contributors":{"authors":[{"text":"Davis, Willard E.","contributorId":8549,"corporation":false,"usgs":true,"family":"Davis","given":"Willard E.","affiliations":[],"preferred":false,"id":261818,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolfe, Edward W.","contributorId":79878,"corporation":false,"usgs":true,"family":"Wolfe","given":"Edward","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":261817,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57348,"text":"wdrOR811 - 1983 - Water resources data Oregon, water year 1981: Volume 1. Eastern Oregon","interactions":[],"lastModifiedDate":"2020-09-25T16:22:15.514316","indexId":"wdrOR811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OR-81-1","title":"Water resources data Oregon, water year 1981: Volume 1. Eastern Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrOR811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Water resources data Oregon, water year 1981: Volume 1. 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Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53499,"text":"fwsobs82_10_45 - 1983 - Habitat Suitability Index Models: Fisher","interactions":[],"lastModifiedDate":"2016-09-16T10:10:29","indexId":"fwsobs82_10_45","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.45","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Fisher","docAbstract":"<p>The fisher (Martes pennanti) is the largest member of its genus and is found only i n North America (Powell 1982). Within the contiguous United States, indigenous and reintroduced populations presently inhabit portions of the Appalachian Mountains from New England south to West Virginia in the east; northern Wisconsin, Minnesota, and Michigan's upper peninsula in the Midwest; northern Idaho and western Montana in the Northwest; and as far south as northern California along the West Coast.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Allen, A.W., 1983, Habitat Suitability Index Models: Fisher: FWS/OBS 82/10.45, vi, 19 p.","productDescription":"vi, 19 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":8271,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/wdb/pub/hsi/hsi-045.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177823,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6498a6","contributors":{"authors":[{"text":"Allen, Arthur W.","contributorId":40648,"corporation":false,"usgs":true,"family":"Allen","given":"Arthur","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":247706,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59299,"text":"mf1495C - 1983 - Geochemical maps of the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli counties, Montana","interactions":[],"lastModifiedDate":"2016-08-22T10:18:25","indexId":"mf1495C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1495","chapter":"C","title":"Geochemical maps of the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli counties, Montana","docAbstract":"<p><span>The Selway-Bitterroot Wilderness covers almost 2,000 mi<sup>2</sup> in east-central Idaho and western Montana (fig. 1). The wilderness lies across the Bitterroot Range, which forms the boundary between Idaho and Montana, and includes large portions of the drainages of the Selway, Lochsa, and Bitterroot Rivers. Elevations range from 1,800 ft on the Selway River near the wilderness boundary to 10,157 ft at Trapper Peak in the Bitterroot Mountains. Specific areas within the wilderness mentioned in this report are shown in figure 1.&nbsp;</span></p>","language":"English","publisher":"U. S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1495C","usgsCitation":"Coxe, B.W., and Toth, M.I., 1983, Geochemical maps of the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli counties, Montana: U.S. Geological Survey Miscellaneous Field Studies Map 1495, 55.66 x 41.70 inches and 54.51 x 41.51 inches, https://doi.org/10.3133/mf1495C.","productDescription":"55.66 x 41.70 inches and 54.51 x 41.51 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":185314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1495C.PNG"},{"id":327201,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1495-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327202,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1495-C/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Idaho, Montana","county":"Idaho, Missoula, Ravalli","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.6533203125,\n              46.54563867035857\n            ],\n            [\n              -114.62585449218749,\n              46.594731356000686\n            ],\n            [\n              -114.55718994140625,\n              46.6588624401289\n            ],\n            [\n              -114.44183349609375,\n              46.70408569832255\n            ],\n            [\n              -114.31549072265625,\n              46.72480037466717\n            ],\n            [\n              -114.19189453125,\n              46.72480037466717\n            ],\n            [\n              -114.16168212890625,\n              46.685247274319565\n            ],\n            [\n        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I.","contributorId":18365,"corporation":false,"usgs":true,"family":"Toth","given":"Margo","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":261744,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60559,"text":"mf1529A - 1983 - Geochemical map of the Mount Eddy and Castle Crags Roadless Areas, Shasta, Siskiyou, and Trinity counties, California","interactions":[],"lastModifiedDate":"2016-08-23T08:36:33","indexId":"mf1529A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1529","chapter":"A","title":"Geochemical map of the Mount Eddy and Castle Crags Roadless Areas, Shasta, Siskiyou, and Trinity counties, California","docAbstract":"<p>The Mount Eddy and Castle , Crags Roadless Areas occupy 9,600 acres (39 km<sup>2</sup>) and 3,300 acres (13 km<sup>2</sup>), respectively, in Shasta, Siskiyou, and Trinity Counties, Calif., approximately 8 mi (13 km) west of the towns of Mount Shasta City and Dunsmuir (fig. 1). Access is provided by secondary roads and trails from Interstate Highway 5, which passes through Mount Shasta City and Dunsmuir. The areas are located in rugged terrane in the easternmost part of the Klamath Mountains where altitudes range from about 2,500 ft (7.62 m) in the southern Castle Crags area to 9,025 ft (2,751 m) on Mount Eddy. Manzanita and other brush are ubiquitous at lower elevations whereas vegetation is lacking at higher elevations except for occasional gnarled conifers and ground-level plants.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1529A","usgsCitation":"Peterson, J., and Caress, M., 1983, Geochemical map of the Mount Eddy and Castle Crags Roadless Areas, Shasta, Siskiyou, and Trinity counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 1529, Plate: 34.89 x 28.90 inches, https://doi.org/10.3133/mf1529A.","productDescription":"Plate: 34.89 x 28.90 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":182689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1529A.JPG"},{"id":327398,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1529-A/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","county":"Shasta County, Siskiyou County, Trinity County","otherGeospatial":"Mount Eddy and Castle Crags Roadless Areas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.5,41 ], [ -122.5,41.333333333333336 ], [ -122.33333333333333,41.333333333333336 ], [ -122.33333333333333,41 ], [ -122.5,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae1e1","contributors":{"authors":[{"text":"Peterson, J.A.","contributorId":76308,"corporation":false,"usgs":true,"family":"Peterson","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":263980,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Caress, M.E.","contributorId":99104,"corporation":false,"usgs":true,"family":"Caress","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":263981,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60610,"text":"mf1365B - 1983 - Aeromagnetic and gravity maps of the east part of the Raymond Peak Roadless Area, Alpine County, California","interactions":[],"lastModifiedDate":"2018-10-18T13:35:44","indexId":"mf1365B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1365","chapter":"B","title":"Aeromagnetic and gravity maps of the east part of the Raymond Peak Roadless Area, Alpine County, California","docAbstract":"<p>The Raymond Peak Roadless Area, 60 mi<sup>2</sup><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"> (153 km<sup>2</sup><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\">) in area, is located at the crest of the Sierra Nevada approximately 13 min (21 km) south-southeast of Lake Tahoe.&nbsp; Markleeville, the seat of Alpine County, lies about 1.5 mi (2km) outside the northeast boundary of the area.&nbsp; The rugged topography of this area is dominated by Raymond and Reynolds Peaks at the south end, and Hawkins Peak at the north end.</span></span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1365B","usgsCitation":"Plouff, D., 1983, Aeromagnetic and gravity maps of the east part of the Raymond Peak Roadless Area, Alpine County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1365, 41.34 x 24.26 inches, https://doi.org/10.3133/mf1365B.","productDescription":"41.34 x 24.26 inches","costCenters":[],"links":[{"id":183042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1365-B/report-thumb.jpg"},{"id":358531,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1365-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","county":"Alpine County","otherGeospatial":"Raymond Peak Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.91666666666667,38.583333333333336 ], [ -119.91666666666667,38.75 ], [ -119.75,38.75 ], [ -119.75,38.583333333333336 ], [ -119.91666666666667,38.583333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698578","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":264076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60611,"text":"mf1322B - 1983 - Aeromagnetic and gravity maps of the Freel and Dardanelles Roadless Areas, Alpine and El Dorado counties, California","interactions":[],"lastModifiedDate":"2016-08-23T08:59:44","indexId":"mf1322B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1322","chapter":"B","title":"Aeromagnetic and gravity maps of the Freel and Dardanelles Roadless Areas, Alpine and El Dorado counties, California","docAbstract":"<p>The Freel and Dardanelles Roadless Areas comprise 51 mi<sup>2</sup> (132 km<sup>2</sup>) in the central Sierra Nevada south of Lake Tahoe. &nbsp;The Sierra Nevada crest passes through the eastern part of the area. &nbsp;Prominent mountains include Stevens Peak (elev 10,061 ft), Waterhouse Peak (elev 9,497 ft), and Freel Peak (elev 10,881 ft).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1322B","usgsCitation":"Plouff, D., 1983, Aeromagnetic and gravity maps of the Freel and Dardanelles Roadless Areas, Alpine and El Dorado counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 1322, 41.79 x 23.48 inches, https://doi.org/10.3133/mf1322B.","productDescription":"41.79 x 23.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1322B.PNG"},{"id":327422,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1322-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","county":"Alpine County, El Dorado County","otherGeospatial":"Freel and Dardaneel Roadless Areas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.16666666666667,38.666666666666664 ], [ -120.16666666666667,38.916666666666664 ], [ -119.83333333333333,38.916666666666664 ], [ -119.83333333333333,38.666666666666664 ], [ -120.16666666666667,38.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6984c8","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":264077,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59038,"text":"mf1542C - 1983 - Mineral resource potential map of the Spanish Peaks Wilderness Study Area, Huerfano and Las Animas counties, Colorado","interactions":[],"lastModifiedDate":"2015-10-22T13:51:38","indexId":"mf1542C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1542","chapter":"C","title":"Mineral resource potential map of the Spanish Peaks Wilderness Study Area, Huerfano and Las Animas counties, Colorado","docAbstract":"<p>A geologic and geochemical investigation and a survey of mines and prospects have been conducted to evaluate the mineral resource potential of the Spanish Peaks Wilderness Study Area, Huerfano and Las Animas Counties, in south-central Colorado. The&middot;study area is underlain by sedimentary rocks of Paleozoic to Tertiary age (Johnson, 1969). Stocks and dikes were emplaced between 20 and 25 m.y. ago (Smith, 1979) forming East and West Spanish Peaks and the White Peaks.</p>\n<p>Most of the study area lacks significant geochemical anomalies and has a low mineral potential. Anomalous concentrations of gold, silver, copper, lead, and zinc in the rocks and drainage basins in the vicinity of the old mines and prospects on West Spanish Peak indicate a moderate potential for small mineralized veins in this area. Ore-bearing veinlets have been worked in the past, primarily for silver and lead; however, the sparsity, small size, and low grade of the veins diminish their significance.</p>\n<p>The depth of several thousand feet at which coal may underlie the surface rocks of the study area makes it a resource with little likelihood of development. The potential for oil and gas appears low because of the apparent lack of structural traps and the intense igneous activity in the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1542C","usgsCitation":"Budding, K.E., and Kluender, S.E., 1983, Mineral resource potential map of the Spanish Peaks Wilderness Study Area, Huerfano and Las Animas counties, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 1542, Report: 5 p.; Plate: 35.17 x 22.37 inches, https://doi.org/10.3133/mf1542C.","productDescription":"Report: 5 p.; Plate: 35.17 x 22.37 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183243,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1542C.jpg"},{"id":310525,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1542-C/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310526,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1542-C/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Huerfano County, Las Animas County","otherGeospatial":"Spanish Peaks Wilderness Study Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.11749999999999,37.333333333333336 ], [ -105.11749999999999,37.416666666666664 ], [ -104.86749999999999,37.416666666666664 ], [ -104.86749999999999,37.333333333333336 ], [ -105.11749999999999,37.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3f3a","contributors":{"authors":[{"text":"Budding, Karin E.","contributorId":32164,"corporation":false,"usgs":true,"family":"Budding","given":"Karin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":261308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kluender, Steven E.","contributorId":49842,"corporation":false,"usgs":true,"family":"Kluender","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":261307,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59031,"text":"mf1424 - 1983 - Structure maps and seismic stratigraphy of the Yakataga segment of the continental margin, northern Gulf of Alaska","interactions":[],"lastModifiedDate":"2015-10-20T11:19:54","indexId":"mf1424","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1424","title":"Structure maps and seismic stratigraphy of the Yakataga segment of the continental margin, northern Gulf of Alaska","docAbstract":"<p>Multichannel seismic-reflection data show the late Cenozoic structure, seismic stratigraphy, and geologic history of the Yakataga segment of the continental margin, between Icy Bay and Kayak Island, northern Gulf of Alaska. The structure of the Yakataga segment consists of broad folds and associated thrust faults beneath the continental shelf and slope, trending generally northeast in the eastern part of the s~gment to east-west in the western part. Anticlines are generally asymmetric and doubly plunging and are commonly bounded on the seaward side by high-angle thrust faults. The degree of deformation is less intense than is observed in adjacent onshore areas. The age of deformation decreases seaward and the deformation shows an overall southeastward migration with time. Structures of similar age define three structural zones; structural growth was roughly contemporaneous in each structural zone, although the local growth pattern is complex in detail. Deformation within each structural zone was followed by subsidence and burial by rapidly deposited marine sediment. Deformation appears to have been continuous during the late Cenozoic, rather than a series of discrete events, because subsidence of a particular structural zone is accompanied by initiation of growth on a younger, more seaward zone. Varying degrees of reactivation of the older structures within recent time have resulted in renewed uplift of these structures. Average sedimentation, uplift, and subsidence rates are all extremely high, and generally range from about 1 to 2 m/1,000 yr; these rates can locally be much higher. The average strike of structures in the Yakataga segment indicates northwest-southeastward compression and is consistent with the current convergence direction between the Pacific and North America plates. Observed shortening within the segment is much less than required by the late Cenozoic convergence rate (about 6 cm/yr), and the major deformation is taken up elsewhere, primarily onshore. Thus, the deformation of the Yakataga segment is caused by minor shortening of the continental margin between Cross Sound and Kayak Island, which together comprise the Yakutat block, as the margin moves northwestward with the Pacific plate and collides with the North America plate.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1424","usgsCitation":"Bruns, T., and Schwab, W.C., 1983, Structure maps and seismic stratigraphy of the Yakataga segment of the continental margin, northern Gulf of Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 1424, Report: 20 p.; 4 Plates: 43.68 x 35.60 inches or smaller, https://doi.org/10.3133/mf1424.","productDescription":"Report: 20 p.; 4 Plates: 43.68 x 35.60 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1424.jpg"},{"id":105852,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7167.htm","linkFileType":{"id":5,"text":"html"},"description":"7167"},{"id":310127,"rank":701,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1424/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310128,"rank":702,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1424/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":310129,"rank":703,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1424/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":310130,"rank":704,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1424/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":310131,"rank":705,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1424/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -145,59 ], [ -145,60.5 ], [ -141,60.5 ], [ -141,59 ], [ -145,59 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d017","contributors":{"authors":[{"text":"Bruns, T.R.","contributorId":96683,"corporation":false,"usgs":true,"family":"Bruns","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":261298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwab, W. 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,{"id":60643,"text":"mf1269 - 1983 - Index of faults of Cretaceous and Cenozoic age in the eastern United States","interactions":[],"lastModifiedDate":"2016-08-23T09:03:39","indexId":"mf1269","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1269","title":"Index of faults of Cretaceous and Cenozoic age in the eastern United States","docAbstract":"<p>The information in this report was collected between 1974 and 1982 as part of the Reactor Hazards Program of the U.S. Geological Survey (USGS). This program was initiated to delineate and assess geologic hazards that could be particularly detrimental to major constructions, especially nuclear reactors. Faults are of principal interest to the program because earthquakes associated with them can cause major damage in short periods of time.&nbsp;</p>\n<p>Prior to 1970, very little was known about Cenozoic faulting in the eastern United States. the most abundant data were available in the western gulf Coastal Plain where oil exploration had generated a considerable amount of subsurface stratigraphic information. The Atlantic coastal Plain was considered to be generally devoid of faults, although scientists such as McGee (1888) and Darton (1891, 1951) had proposed major faulting or uplift along the Fall Line. The Piedmont and Blue Ridge Provinces of the eastern United States contained numerous mapped faults, abut the recency of fault movement was unknown because of the absence of Cenozoic strata.</p>\n<p>One of the initial efforts of the Reactor Hazards Program was a compilation and evaluation of Cretaceous and younger faults in the East. Topical studies were initiated in areas of particular interest, and these studies in turn generated a broader scientific interest in the problem of Cenozoic deformation. A preliminary literature investigation of Cretaceous and younger faulting was published by York and Oliver (1976), and was followed by an interpretive map of young faults by Howard and others (1978).</p>\n<p>The data in this report represent the presently available knowledge of fault characteristics and distribution. Clearly, as current investigations progress and as geologists become more aware of the evidence for Cenozoic faulting, the number of known Cenozoic faults will increase substantially. Until such time, the data that are shown here must be viewed conservatively because I believe they are not a totally representative collection of information at this scale. the data are useful in characterizing basic fault patterns in the region, but certain factors limit the usefulness of the map. Limitations of this information are discussed in the following text, and the reader should give them major consideration when using the map and fault table.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1269","usgsCitation":"Prowell, D.C., 1983, Index of faults of Cretaceous and Cenozoic age in the eastern United States: U.S. Geological Survey Miscellaneous Field Studies Map 1269, 2 Plates: 33.97 x 47.57 inches and 46.18 x 37.79 inches, https://doi.org/10.3133/mf1269.","productDescription":"2 Plates: 33.97 x 47.57 inches and 46.18 x 37.79 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1269.PNG"},{"id":327432,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1269/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327431,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1269/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.388671875,\n              45.02695045318546\n            ],\n            [\n              -71.279296875,\n              45.1510532655634\n            ],\n            [\n              -69.9169921875,\n              43.03677585761058\n            ],\n            [\n              -69.9609375,\n              42.42345651793833\n            ],\n            [\n              -69.60937499999999,\n              41.64007838467894\n            ],\n            [\n              -69.9609375,\n              40.91351257612758\n            ],\n            [\n              -71.89453125,\n              40.58058466412764\n            ],\n            [\n              -73.564453125,\n              39.774769485295465\n            ],\n            [\n              -75.0146484375,\n              37.75334401310656\n            ],\n            [\n              -75.498046875,\n              36.24427318493909\n            ],\n            [\n              -75.322265625,\n              34.92197103616377\n            ],\n            [\n              -77.3876953125,\n              34.016241889667015\n            ],\n            [\n              -79.0576171875,\n              32.80574473290688\n            ],\n            [\n              -80.2880859375,\n              31.989441837922904\n            ],\n            [\n              -81.298828125,\n              30.751277776257812\n            ],\n            [\n              -81.6064453125,\n              29.76437737516313\n            ],\n            [\n              -83.232421875,\n              29.38217507514529\n            ],\n            [\n              -85.341796875,\n              29.305561325527698\n            ],\n            [\n              -87.62695312499999,\n              29.305561325527698\n            ],\n            [\n              -88.72558593749999,\n              29.305561325527698\n            ],\n            [\n              -89.12109375,\n              29.267232865200878\n            ],\n            [\n              -90.791015625,\n              29.34387539941801\n            ],\n            [\n              -90.263671875,\n              31.203404950917395\n            ],\n            [\n              -89.12109375,\n              34.161818161230386\n            ],\n            [\n              -87.6708984375,\n              35.31736632923788\n            ],\n            [\n              -85.078125,\n              37.16031654673677\n            ],\n            [\n              -83.408203125,\n              38.89103282648846\n            ],\n            [\n              -80.2880859375,\n              40.51379915504413\n            ],\n            [\n              -79.40917968749999,\n              42.16340342422401\n            ],\n            [\n              -77.95898437499999,\n              43.004647127794435\n            ],\n            [\n              -75.4541015625,\n              44.49650533109348\n            ],\n            [\n              -73.388671875,\n              45.02695045318546\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4300","contributors":{"authors":[{"text":"Prowell, David C.","contributorId":46956,"corporation":false,"usgs":true,"family":"Prowell","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":264125,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58338,"text":"mf1548 - 1983 - Biostratigraphic correlation chart of some Upper Cretaceous rocks from the Lost Soldier area, Wyoming to west of Craig, Colorado","interactions":[],"lastModifiedDate":"2018-03-26T15:24:45","indexId":"mf1548","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1548","title":"Biostratigraphic correlation chart of some Upper Cretaceous rocks from the Lost Soldier area, Wyoming to west of Craig, Colorado","docAbstract":"<p>This chart depicts the time-stratigraphic relations of some Upper Cretaceous rocks along the eastern and southeastern margins of the Greater Green River Basin, south-central Wyoming and northwestern Colorado. The purpose of this report is to release a preferred set of correlations based upon marine mollusk biostratigraphy. The senior author, with the help of B. E. Law, has acquired, synthesized, compiled, and interpreted data from various sources. These include selected published documents (see \"References Cited\") and unpublished reports of fossil identifications by W. A. Cobban who examined collections made by the late J. R. Gill. Numerous measured sections of Gill's were also utilized. It must be emphasized that all interpretations on this chart are based on information obtained from these sources and the senior author has yet to substantiate these correlations in the field. Not all data from the area of this study is included herein because it is either repetitive in nature or its reliability is uncertain. This uncertainty is due to the ambiguity inherent in both fossil identification and stratigraphic interpretation. Questionable unpublished material has been omitted while published data which is inconsistent with the senior author's correlations may be found in the footnotes portion of this report. The rock units are assigned to a range of ammonites that have been related to an absolute time scale. The ammonite zonation and age boundaries are adapted from Obradovich and Cobban (1975). \"D\" numbers are provided for each geographic locality where fossils were collected and described by personnel of the U.S. Geological Survey. These fossils may be accessed at the offices of the Survey in Lakewood, Colorado.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1548","isbn":"0607812788","usgsCitation":"Bader, J., Gill, J.R., Cobban, W.A., and Law, B.E., 1983, Biostratigraphic correlation chart of some Upper Cretaceous rocks from the Lost Soldier area, Wyoming to west of Craig, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 1548, Plate: 50.26 x 37.13 inches, https://doi.org/10.3133/mf1548.","productDescription":"Plate: 50.26 x 37.13 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326970,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1548/plate-1.pdf"},{"id":326972,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1548.JPG"}],"scale":"1","country":"United States","state":"Colorado, Wyoming","otherGeospatial":"Lost Soldier area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.25,40 ], [ -108.25,42.5 ], [ -106.8,42.5 ], [ -106.8,40 ], [ -108.25,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db622ff1","contributors":{"authors":[{"text":"Bader, J.W.","contributorId":68281,"corporation":false,"usgs":true,"family":"Bader","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":258786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, J. R.","contributorId":8125,"corporation":false,"usgs":true,"family":"Gill","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":258783,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cobban, W. A.","contributorId":21577,"corporation":false,"usgs":true,"family":"Cobban","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":258785,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Law, B. E.","contributorId":17586,"corporation":false,"usgs":true,"family":"Law","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":258784,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":61519,"text":"mf1577C - 1983 - Geochemical map of the Arnold Mesa Roadless Area, Yavapai County, Arizona","interactions":[],"lastModifiedDate":"2016-08-23T10:40:39","indexId":"mf1577C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1577","chapter":"C","title":"Geochemical map of the Arnold Mesa Roadless Area, Yavapai County, Arizona","docAbstract":"<p><span>The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and be submitted to the President&nbsp;and the Congress. This report presents the results of a geochemical survey of the&nbsp;Arnold Mesa Roadless Area (U.S. Forest Service number 03092) in the Prescott and Tonto National Forests,&nbsp;Yavapai County, Arizona. The&nbsp;Arnold Mesa Roadless Area was classified&nbsp;as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.</span></p>\n<p><span>During 1980 the&nbsp;U.S. Geological Survey and the&nbsp;U.S. Bureau of Mines (USBM) conducted field investigations to evaluate the mineral resource potential of the&nbsp;Arnold Mesa Roadless Area,&nbsp;Yavapai County, Arizona. Field studies included geologic mapping (Wolrfe, 1983), aeromagnetic mapping (Davis and Wolfe, 1983), geochemical sampling (this report), and a survey of known mines and prospects (McColly and Korzeb, 1981).</span></p>\n<p>The&nbsp;Arnold Mesa Roadless Area comprises about 28,000 acres (11,300 hectares) in and along the flanks of the Black Hills south of Camp Verde, Arizona. The Black Hills form a northwest-trending drainage divide, between the Agua Fria drainage on the west and Verde River on the east, that extends through the roadless area. The crest and southwest flank of the divide within the study area are moderately dissected, gently rolling uplands. The northeast flank is steep terrain that forms the western wall of the Verde Valley. The northeast flank has a total relief within the study area of almost 4,000 ft (more than 1,200 m) and is deeply incised by the canyons of Gap and Chasm Creeks. Unpaved roads provide access to much of the perimeter of the Arnold Mesa Roadless Area, but the interior is accessible only by foot, horse, or helicopter.</p>\n<p>&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1577C","usgsCitation":"Wolfe, E.W., 1983, Geochemical map of the Arnold Mesa Roadless Area, Yavapai County, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1577, 58.63 x 40.35 inches, https://doi.org/10.3133/mf1577C.","productDescription":"58.63 x 40.35 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":182475,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1577C.PNG"},{"id":327607,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1577-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Arizona","county":"Yavapai County","otherGeospatial":"Arnold Mesa Roadless Area, Prescott National Forest, Tonto National Forest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112,\n              34.5\n            ],\n            [\n              -112,\n              34.2\n            ],\n            [\n              -111.6,\n              34.2\n            ],\n            [\n              -111.6,\n              34.5\n            ],\n            [\n              -112,\n              34.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae229","contributors":{"authors":[{"text":"Wolfe, Edward W.","contributorId":79878,"corporation":false,"usgs":true,"family":"Wolfe","given":"Edward","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265862,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61069,"text":"mf1495B - 1983 - Reconnaissance geologic map of the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli counties, Montana","interactions":[],"lastModifiedDate":"2025-09-24T17:41:14.495224","indexId":"mf1495B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1495","chapter":"B","title":"Reconnaissance geologic map of the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli counties, Montana","docAbstract":"<p>The Selway-Bitterroot Wilderness covers about 1.25 million acres in east-central Idaho and western Montana (fig. 1). The wilderness lies across the Bitterroot Range, which forms the boundary between Idaho and Montana, and includes large portions of the drainages of the Selway, Lochsa, and Bitterroot Rivers. Elevations range from 1,800 ft on the Selway River near the wilderness boundary to 10,157 ft at Trapper Peak in the Bitterroot Mountains. Cities within 50 min of the wilderness include Missoula, Hamilton, and Salmon on the east, and Orofino and Grangeville on the west. Access to trailheads near the edge of the wilderness is limited to dirt roads.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1495B","usgsCitation":"Toth, M.I., 1983, Reconnaissance geologic map of the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli counties, Montana: U.S. Geological Survey Miscellaneous Field Studies Map 1495, 1 Plate: 39.49 x 57.80 inches, https://doi.org/10.3133/mf1495B.","productDescription":"1 Plate: 39.49 x 57.80 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179812,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1495B.PNG"},{"id":327544,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1495-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":496038,"rank":3,"type":{"id":36,"text":"NGMDB Index 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