A kinematic model for the structure of the lee-side deposit of a dune-like bedform, Gilbert-type delta, or similar step is developed, based on the assumptions that initial deposition is entirely by grainfall, that the rate of deposition decreases as a power function of distance downflow from the brink of the slipface, and that the resulting steepening of the slipface is periodically interrupted by avalanching. The parameters used in the model are: (1) the deposition rate at a given distance from the brink, (2) the exponent in the equation relating the deposition rate to distance from the brink, (3) the bedform migration rate, (4) the bedform height, (5) the avalanche speed, (6) the angle of initial yield, and (7) the residual angle after avalanching. From these parameters can be calculated structural characteristics such as the proportions of bottomset and foreset deposits, the proportions of avalanche and grainfall deposits in the foreset deposit, and the spacing of avalanche-grainfall couplets.
The model correctly predicts the trends of changing avalanche activity and changing structural character with changes in flow character, grain size, and bedform height in both air and water. Moreover, the model correctly predicts certain consistent structural differences between aeolian and subaqueous lee-side deposits. Quantitative evaluation of the model requires more accurate data on the values of the input parameters than are presently available.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-3091.1985.tb00520.x","issn":"00370746","usgsCitation":"Hunter, R., 1985, A kinematic model for the structure of lee-side (dune-like) deposits: Sedimentology, v. 32, no. 3, p. 409-422, https://doi.org/10.1111/j.1365-3091.1985.tb00520.x.","productDescription":"14 p.","startPage":"409","endPage":"422","costCenters":[],"links":[{"id":220186,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-06-14","publicationStatus":"PW","scienceBaseUri":"5059e42ce4b0c8380cd4647a","contributors":{"authors":[{"text":"Hunter, Ralph E.","contributorId":53759,"corporation":false,"usgs":true,"family":"Hunter","given":"Ralph E.","affiliations":[],"preferred":false,"id":365586,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012972,"text":"70012972 - 1985 - Structure, porosity and stress regime of the upper oceanic crust: Sonic and ultrasonic logging of DSDP Hole 504B","interactions":[],"lastModifiedDate":"2025-08-26T16:35:03.910107","indexId":"70012972","displayToPublicDate":"2003-04-11T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Structure, porosity and stress regime of the upper oceanic crust: Sonic and ultrasonic logging of DSDP Hole 504B","docAbstract":"The layered structure of the oceanic crust is characterized by changes in geophysical gradients rather than by abrupt layer boundaries. Correlation of geophysical logs and cores recovered from DSDP Hole 504B provides some insight into the physical properties which control these gradient changes. Borehole televiewer logging in Hole 504B provides a continuous image of wellbore reflectivity into the oceanic crust, revealing detailed structures not apparent otherwise, due to the low percentage of core recovery. Physical characteristics of the crustal layers 2A, 2B and 2C such as the detailed sonic velocity and lithostratigraphic structure are obtained through analysis of the sonic, borehole televiewer and electrical resistivity logs. A prediction of bulk hydrated mineral content, consistent with comparison to the recovered material, suggests a change in the nature of the alteration with depth. Data from the sonic, borehole televiewer, electrical resistivity and other porosity-sensitive logs are used to calculate the variation of porosity in the crustal layers 2A, 2B and 2C. Several of the well logs which are sensitive to the presence of fractures and open porosity in the formation indicate many zones of intense fracturing. Interpretation of these observations suggests that there may be a fundamental pattern of cooling-induced structure in the oceanic crust.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(85)90153-2","issn":"00401951","usgsCitation":"Newmark, R., Anderson, R.N., Moos, D., and Zoback, M.D., 1985, Structure, porosity and stress regime of the upper oceanic crust: Sonic and ultrasonic logging of DSDP Hole 504B: Tectonophysics, v. 118, no. 1-2, p. 1-42, https://doi.org/10.1016/0040-1951(85)90153-2.","productDescription":"42 p.","startPage":"1","endPage":"42","costCenters":[],"links":[{"id":220117,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"118","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9c6ae4b08c986b31d3f2","contributors":{"authors":[{"text":"Newmark, Robin","contributorId":177284,"corporation":false,"usgs":false,"family":"Newmark","given":"Robin","email":"","affiliations":[],"preferred":false,"id":364963,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Roger N.","contributorId":95618,"corporation":false,"usgs":true,"family":"Anderson","given":"Roger","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":364964,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moos, Daniel","contributorId":105048,"corporation":false,"usgs":true,"family":"Moos","given":"Daniel","affiliations":[],"preferred":false,"id":364965,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zoback, Mark D.","contributorId":80275,"corporation":false,"usgs":true,"family":"Zoback","given":"Mark","middleInitial":"D.","affiliations":[],"preferred":false,"id":364962,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":14953,"text":"ofr85412 - 1985 - Post-Eruption Changes in Channel Geometry of Streams in the Toutle River Drainage Basin, 1980-82, Mount St. Helens, Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"ofr85412","displayToPublicDate":"2001-09-01T00:00:00","publicationYear":"1985","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":"85-412","title":"Post-Eruption Changes in Channel Geometry of Streams in the Toutle River Drainage Basin, 1980-82, Mount St. Helens, Washington","docAbstract":"The May 18, 1980, eruption of Mount St. Helens, Washington, generated a debris avalanche, lateral blast, lahars, and tephra deposits that altered mainstem and tributary channels within the Toutle River drainage basin. Channel cross sections were monumented and surveyed on North Fork Toutle River and its tributaries, on South Fork Toutle River, on Green River, and on Toutle River in 1980 and 1981. These streams drain the north and west flanks of the volcano. The network of channel cross sections was surveyed more frequently following periods of higher flow. The repetitive cross-section surveys provide measurements of bank erosion or accretion and of channel erosion or aggradation. These data can be used to determine erosion rates, and to identify sources and storage sites of sediment in sediment budget computations. This report presents channel cross-section profiles constructed from the survey data collected during water years 1980 through 1982.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr85412","usgsCitation":"Meyer, D.F., Nolan, K.M., and Dodge, J., 1985, Post-Eruption Changes in Channel Geometry of Streams in the Toutle River Drainage Basin, 1980-82, Mount St. Helens, Washington: U.S. Geological Survey Open-File Report 85-412, vi, 128 p. **PUBLICATION PAGES ARE IN INCORRECT ORDER**, https://doi.org/10.3133/ofr85412.","productDescription":"vi, 128 p. **PUBLICATION PAGES ARE IN INCORRECT ORDER**","temporalStart":"1980-01-01","temporalEnd":"1982-12-31","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":145949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0412/report-thumb.jpg"},{"id":43768,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0412/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,46 ], [ -123,46.5 ], [ -122,46.5 ], [ -122,46 ], [ -123,46 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683ae6","contributors":{"authors":[{"text":"Meyer, D. F.","contributorId":21167,"corporation":false,"usgs":true,"family":"Meyer","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":170309,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nolan, K. Michael","contributorId":71943,"corporation":false,"usgs":true,"family":"Nolan","given":"K.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":170310,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dodge, J.E.","contributorId":21133,"corporation":false,"usgs":true,"family":"Dodge","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":170308,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70189805,"text":"wdrMI841 - 1985 - Water resources data, Michigan, water year 1984","interactions":[],"lastModifiedDate":"2017-08-10T14:46:52","indexId":"wdrMI841","displayToPublicDate":"1999-12-26T00:00:00","publicationYear":"1985","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":"MI-84-1","title":"Water resources data, Michigan, water year 1984","docAbstract":"Water resources data for the 1984 water year for Michigan consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water temperature of ground water. This report contains discharge records for 142 gaging stations; stage only records for 2 gaging stations; stage and contents for 5 lakes and reservoirs; water quality for 27 continuous-record stations; and water levels for 53 observation wells. Also included are 56 crest-stage partial-record stations and 22 low-flow partial-record stations.A Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Michigan.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMI841","collaboration":"Prepared in cooperation with the State of Michigan and with other agencies","usgsCitation":"Miller, J.B., Oberg, J.L., and Sieger, T., 1985, Water resources data, Michigan, water year 1984: U.S. Geological Survey Water Data Report MI-84-1, ix, 276, https://doi.org/10.3133/wdrMI841.","productDescription":"ix, 276","onlineOnly":"Y","temporalStart":"1983-10-01","temporalEnd":"1984-09-30","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":344736,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/mi-84-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":344331,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/mi-84-1/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5979aa59e4b0ec1a488b8c53","contributors":{"authors":[{"text":"Miller, John B.","contributorId":37304,"corporation":false,"usgs":true,"family":"Miller","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":706432,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oberg, John L.","contributorId":195162,"corporation":false,"usgs":false,"family":"Oberg","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":706433,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sieger, Theodore Jr.","contributorId":195163,"corporation":false,"usgs":false,"family":"Sieger","given":"Theodore","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":706434,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":60341,"text":"mf1246J - 1985 - Maps showing distribution of tungsten in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-12-22T19:26:09.570433","indexId":"mf1246J","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"J","title":"Maps showing distribution of tungsten in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.
Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.
Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.
The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246J","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of tungsten in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 35.98 x 27.39 inches, https://doi.org/10.3133/mf1246J.","productDescription":"1 Plate: 35.98 x 27.39 inches","costCenters":[],"links":[{"id":182847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246j.jpg"},{"id":393329,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-J/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390902,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6854.htm"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057bd","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263578,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263580,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":60340,"text":"mf1246I - 1985 - Maps showing distribution of tin in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T19:06:12.463908","indexId":"mf1246I","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"I","title":"Maps showing distribution of tin in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.
Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.
Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.
The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246I","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of tin in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 36.15 x 27.85 inches, https://doi.org/10.3133/mf1246I.","productDescription":"1 Plate: 36.15 x 27.85 inches","costCenters":[],"links":[{"id":182846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246i.jpg"},{"id":390901,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6853.htm"},{"id":283657,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-I/plate-1.pdf"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057ba","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263577,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":60339,"text":"mf1246H - 1985 - Maps showing distribution of thorium in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T19:04:27.687858","indexId":"mf1246H","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"H","title":"Maps showing distribution of thorium in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.
Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.
Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.
The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246H","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of thorium in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 36.21 x 27.70 inches, https://doi.org/10.3133/mf1246H.","productDescription":"1 Plate: 36.21 x 27.70 inches","costCenters":[],"links":[{"id":390900,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6852.htm"},{"id":283656,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-H/plate-1.pdf"},{"id":179801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246h.jpg"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057b4","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263572,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263574,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":60338,"text":"mf1246G - 1985 - Maps showing distribution of lead in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T19:01:20.256061","indexId":"mf1246G","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"G","title":"Maps showing distribution of lead in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.
Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.
Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.
The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246G","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of lead in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 36.38 x 27.85 inches, https://doi.org/10.3133/mf1246G.","productDescription":"1 Plate: 36.38 x 27.85 inches","costCenters":[],"links":[{"id":179800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246g.jpg"},{"id":283655,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-G/plate-1.pdf"},{"id":390898,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6851.htm"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605779","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263569,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263571,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":60337,"text":"mf1246F - 1985 - Maps showing distribution of copper in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T18:59:37.497209","indexId":"mf1246F","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"F","title":"Maps showing distribution of copper in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.
Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.
Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.
The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246F","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of copper in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 36.31 x 27.27 inches, https://doi.org/10.3133/mf1246F.","productDescription":"1 Plate: 36.31 x 27.27 inches","costCenters":[],"links":[{"id":179799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246f.PNG"},{"id":390897,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6850.htm"},{"id":283654,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-F/plate-1.pdf"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605711","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263566,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263568,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":55706,"text":"wdrND841 - 1985 - Water resources data, North Dakota, water year 1984","interactions":[],"lastModifiedDate":"2020-10-27T17:09:51.617667","indexId":"wdrND841","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"ND-84-1","title":"Water resources data, North Dakota, water year 1984","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrND841","usgsCitation":"Haffield, N., and Ryan, G., 1985, Water resources data, North Dakota, water year 1984: U.S. Geological Survey Water Data Report ND-84-1, ix, 358 p., https://doi.org/10.3133/wdrND841.","productDescription":"ix, 358 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":379806,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/nd-84-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/nd-84-1/report-thumb.jpg"}],"country":"United States","state":"North 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Southern Great Basin from Mexican border to Mono Lake basin, and Pacific slope basins from Tijuana River to Santa Maria River","interactions":[],"lastModifiedDate":"2012-06-23T01:01:39","indexId":"wdrCA841","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"CA-84-1","title":"Water resources data for California, water year 1984; Volume 1. Southern Great Basin from Mexican border to Mono Lake basin, and Pacific slope basins from Tijuana River to Santa Maria River","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA841","collaboration":"Prepared in cooperation with the California Department of Water Resources and with other agencies","usgsCitation":"Bowers, J.C., Butcher, M., Lamb, C.E., Polinoski, K.G., and Smith, G., 1985, Water resources data for California, water year 1984; Volume 1. Southern Great Basin from Mexican border to Mono Lake basin, and Pacific slope basins from Tijuana River to Santa Maria River (Legacy Report): U.S. Geological Survey Water Data Report CA-84-1, xii, 375 p., https://doi.org/10.3133/wdrCA841.","productDescription":"xii, 375 p.","temporalStart":"1983-10-01","temporalEnd":"1984-09-30","costCenters":[{"id":631,"text":"Water Resources Division-California District","active":false,"usgs":true}],"links":[{"id":257812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_ca_84_1.jpg"},{"id":184299,"rank":0,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/ca-84/WDR-1984-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Southern Great Basin;Mono Lake Basin;Pacific Slope Basins;Tijuana River;Santa Maria River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.4,32.5 ], [ -124.4,42 ], [ -114.13333333333334,42 ], [ -114.13333333333334,32.5 ], [ -124.4,32.5 ] ] ] } } ] }","edition":"Legacy Report","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1539","contributors":{"authors":[{"text":"Bowers, J. C.","contributorId":57106,"corporation":false,"usgs":true,"family":"Bowers","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":256463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butcher, M.T.","contributorId":47867,"corporation":false,"usgs":true,"family":"Butcher","given":"M.T.","email":"","affiliations":[],"preferred":false,"id":256461,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lamb, C. E.","contributorId":59793,"corporation":false,"usgs":true,"family":"Lamb","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":256464,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Polinoski, K. 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This report contains discharge records for 115 gaging stations; stage and contents for 7 lakes and reservoirs; water quality for 17 gaging stations; and water levels for 90 observation wells. Also included are 120 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements and analyses. The data represent that part of the National Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Iowa.
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This report contains discharge records for 48 gaging stations; stage only for 2 gaging stations; contents for 17 lakes and reservoirs; water quality for 11 gaging stations and 6 ground-waterwells; and water-levels for 17 ground-water wells. Additional water data were collectedat other sites, not part of the systematic data collection program, and are publishedas miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrME851","collaboration":"Prepared in cooperation with the State of Maine and with other agencies","usgsCitation":"Bartlett, W., Higgins, W., and Nichols, W., 1985, Water resources data, Maine, water year 1985: U.S. Geological Survey Water Data Report ME-85-1, vii, 158 p., https://doi.org/10.3133/wdrME851.","productDescription":"vii, 158 p.","costCenters":[],"links":[{"id":174490,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1985/me-85-1/report-thumb.jpg"},{"id":492560,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/me-85-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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Jr.","contributorId":85597,"corporation":false,"usgs":true,"family":"Bartlett","given":"W.P.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":252947,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Higgins, W.B.","contributorId":21627,"corporation":false,"usgs":true,"family":"Higgins","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":252946,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nichols, W.J. Jr.","contributorId":86030,"corporation":false,"usgs":true,"family":"Nichols","given":"W.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":252948,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":55230,"text":"wdrME841 - 1985 - Water resources data, Maine, water year 1984","interactions":[],"lastModifiedDate":"2025-07-29T15:09:17.026341","indexId":"wdrME841","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"ME-84-1","title":"Water resources data, Maine, water year 1984","docAbstract":"Water resources data for the 1984 water year for Maine consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of wells. This report contains discharge records for 53 gaging stations; stage only for 2 gaging stations; contents for 17 lakes and reservoirs; water quality for 11 gaging stations; and water levels for 17 observation wells. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies.
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This data file has been recompiled and updated through 1981. Some revisions of epicenters and intensities in the original file have been made, and intensities have been assigned to earthquakes that previously had none assigned. Only earthquakes that had epicenters within the boundary of the state are listed in table 1, even though earthquakes that had epicenters in bordering states or countries may have been felt or may have caused damage in the state. Intensity values were updated from data sources that were not available at the time or original compilation. Some epicenters were relocated on the basis of new information. The data shown in table 1 represent best estimates of the epicenter, magnitude, and intensity of each earthquake on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed, but not all, especially for the earthquakes that occurred before seismic instruments were universally used.
\nThe data in table 1 were used to compile the seismicity map. The latitude and longitude coordinates of each epicenter were rounded to the nearest tenth of a degree. The triangles on the map represent epicenters plotted to the nearest tenth of a degree. The number of earthquakes at each location is shown on the map by the number to the right of the triangle. A Roman numeral to the left of a triangle is the maximum Modified Mercalli (MM) intensity (Wood and Neumann, 1931) of al earthquakes at that geographic location. The absence of an intensity value indicates that no intensities have been assigned to earthquakes at that location. The four-digit number shown below each triangle is the latest year for which the maximum intensity was recorded.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1798","usgsCitation":"Reagor, B., Stover, C.W., and Algermissen, S.T., 1985, Seismicity map of the State of Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 1798, Plate: 55.71 x 41.76 inches, https://doi.org/10.3133/mf1798.","productDescription":"Plate: 55.71 x 41.76 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326198,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1798.JPG"},{"id":327438,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1798/plate-1.pdf","text":"Plate","size":"23.53 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"}],"scale":"0","country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,41 ], [ -111,45 ], [ -104,45 ], [ -104,41 ], [ -111,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fae70","contributors":{"authors":[{"text":"Reagor, B.G.","contributorId":99121,"corporation":false,"usgs":true,"family":"Reagor","given":"B.G.","affiliations":[],"preferred":false,"id":264191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stover, C. W.","contributorId":70369,"corporation":false,"usgs":true,"family":"Stover","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":264190,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Algermissen, S. T.","contributorId":39790,"corporation":false,"usgs":true,"family":"Algermissen","given":"S.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":264189,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":60662,"text":"mf1819 - 1985 - Seismicity map of the State of Montana","interactions":[],"lastModifiedDate":"2017-05-10T11:33:23","indexId":"mf1819","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1819","title":"Seismicity map of the State of Montana","docAbstract":"This map is one of a series of seismicity maps produced by the U. S. Geological Survey that show earthquake data of individual states or groups of states at the scale of 1:1,000,000. This map shows only those earthquakes with epicenters located within the boundaries of Montana, even though earthquakes in bordering states or countries may have been felt or may have caused damage in Montana.
\nThe data in table 1 were used to compile the seismicity map; these data are a corrected, expanded, and updated (through 1981) version of the data used by Algermissen (1969) for a study of seismic risk in the United States. The locations and intensities of some earthquakes were revised and intensities were assigned where none had been before. Many earthquakes were added to the original list from new data sources as well as from some old data sources that had not been previously used. No earthquakes with magnitudes greater than 2.5 were located in Montana during 1981. The data in table 1 represent best estimates of the location of the epicenter, magnitude, and intensity of each earthquake on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed, but not all, especially for earthquakes that occurred before seismic instruments were universally used.
\nSpecial criteria used in compiling the list of earthquake in the State of Montana include the following: (1) All earthquakes with epicenters along the Montana-Wyoming border with a latitude of 45° N are listed in Montana. (2) Aftershocks of the 1925 and 1935 earthquakes were assigned the same geographic locations as the main shocks. (3) Instrumental epicenters for the 1959 Hebgen Lake earthquake and its aftershocks were 1ocated in Idaho, Montana, and Wyoming; only the ones located in Montana are included on this map. All non-instrumental locations were given the location of the main shock with an accuracy code that includes the community reporting the maximum intensity.
\nThe latitude and longitude coordinates of each epicenter were rounded to the nearest tenth of a degree and sorted so that all identical locations were grouped and counted. These locations are represented on the map by a triangle. The number of earthquakes at each location is shown on the map by the number to the right of the triangle. A Roman numeral to the left of a triangle is the maximum Modified Mercalli intensity (Wood and Neumann, 1931) of all earthquakes at that geographic location. The absence of an intensity value indicates that no intensities have been assigned to earthquakes at that location. The year shown below each triangle is the latest year for which the maximum intensity was recorded.
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Jersey\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ee9","contributors":{"authors":[{"text":"Bauersfeld, W.R.","contributorId":72451,"corporation":false,"usgs":true,"family":"Bauersfeld","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":254152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moshinsky, E.W.","contributorId":104972,"corporation":false,"usgs":true,"family":"Moshinsky","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":254154,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pustay, E.A.","contributorId":62604,"corporation":false,"usgs":true,"family":"Pustay","given":"E.A.","affiliations":[],"preferred":false,"id":254151,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schaefer, F. L.","contributorId":91085,"corporation":false,"usgs":true,"family":"Schaefer","given":"F. L.","affiliations":[],"preferred":false,"id":254153,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":60392,"text":"mf1570C - 1985 - Aeromagnetic maps of the Latir Peak and Wheeler Peak Wildernesses and the Columbine-Hondo Wilderness Study Area, Taos County, New Mexico","interactions":[],"lastModifiedDate":"2016-08-23T08:23:56","indexId":"mf1570C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1570","chapter":"C","title":"Aeromagnetic maps of the Latir Peak and Wheeler Peak Wildernesses and the Columbine-Hondo Wilderness Study Area, Taos County, New Mexico","docAbstract":"This report interprets data from a helicopter-borne magnetic survey to help delineate subsurface geology. Such data, acquired near the ground, reflect greater magnetic detail than do data acquired at higher altitude. Data from a high-altitude reconnaissance aeromagnetic survey (U.S. Geological Survey, 1976) are used selectively to assist in the interpretation of the helicopter data.
\nInterpretations are chiefly empirical, wherein magnetic anomalies characterizing known geologic features in the region are used as interpretive criteria for identifying such features where they are concealed. Identifying geologic environments favorable for mineral deposits is a primary objective of this report.
\nGeophysical interpretations of a broader and more general scope are made from other geophysical data by Cordell and Jones (in press).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1570C","usgsCitation":"Moss, C.K., and Abrams, G.A., 1985, Aeromagnetic maps of the Latir Peak and Wheeler Peak Wildernesses and the Columbine-Hondo Wilderness Study Area, Taos County, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1570, 2 Plates: 58.65 x 38.74 inches and 29.90 x 24.69 inches, https://doi.org/10.3133/mf1570C.","productDescription":"2 Plates: 58.65 x 38.74 inches and 29.90 x 24.69 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326366,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1570C.JPG"},{"id":327381,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1570-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327382,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1570-C/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"New Mexico","county":"Taos County","otherGeospatial":"Columbine-Hondo Wilderness Study Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.61749999999999,36.5 ], [ -105.61749999999999,36.8675 ], [ -105.36749999999999,36.8675 ], [ -105.36749999999999,36.5 ], [ -105.61749999999999,36.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d72","contributors":{"authors":[{"text":"Moss, C. K.","contributorId":94661,"corporation":false,"usgs":true,"family":"Moss","given":"C.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":263670,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abrams, G. A.","contributorId":27047,"corporation":false,"usgs":true,"family":"Abrams","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":263669,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":60342,"text":"mf1246K - 1985 - Maps showing distribution of zinc in heavy-mineral concentrates, Richfield 1° by 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2019-06-11T12:31:17","indexId":"mf1246K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1246","chapter":"K","title":"Maps showing distribution of zinc in heavy-mineral concentrates, Richfield 1° by 2° quadrangle, Utah","docAbstract":"These maps are part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Coterminous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.
Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.
Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related instrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.
The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of zinc in two fractions of heavy-mineral concentrates of drainage sediments.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1246K","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of zinc in heavy-mineral concentrates, Richfield 1° by 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, Plate: 35.92 x 27.30 in., https://doi.org/10.3133/mf1246K.","productDescription":"Plate: 35.92 x 27.30 in.","costCenters":[],"links":[{"id":364157,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-K/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":" https://pubs.usgs.gov/mf1246K/report-thumb.jpg"}],"scale":"500000","country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057c3","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263581,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263583,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}