{"pageNumber":"4751","pageRowStart":"118750","pageSize":"25","recordCount":165605,"records":[{"id":70010326,"text":"70010326 - 1983 - Maps for the nation: The current federal mapping establishment","interactions":[],"lastModifiedDate":"2023-11-29T16:43:32.147923","indexId":"70010326","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1851,"text":"Government Publications Review","active":true,"publicationSubtype":{"id":10}},"title":"Maps for the nation: The current federal mapping establishment","docAbstract":"

The U.S. Government annually produces an estimated 53,000 new maps and charts and distributes about 160 million copies. A large number of these maps are produced under the national mapping program, a decentralized Federal/State cooperative approach to mapping the country at standard scales. Circular A-16, issued by the Office of Management and Budget in 1953 and revised in 1967, delegates the mapping responsibilities to various federal agencies. The U.S. Department of the Interior's Geological Survey is the principal federal agency responsible for implementing the national mapping program. Other major federal map producing agencies include the Departments of Agriculture, Commerce, Defense, Housing and Urban Development, and Transportation, and the Tennessee Valley Authority. To make maps and mapping information more readily available, the National Cartographic Information Center was established in 1974 and an expanded National Map Library Depository Program in 1981. The most recent of many technological advances made under the mapping program are in the areas of digital cartography and video disc and optical disc information storage systems. Future trends and changes in the federal mapping program will involve expanded information and customer service operations, further developments in the production and use of digital cartographic data, and consideration of a Federal Mapping Agency.

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}\n }\n ]\n}","volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a50ace4b0c8380cd6b84f","contributors":{"authors":[{"text":"North, Gary W.","contributorId":28587,"corporation":false,"usgs":true,"family":"North","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":358648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014009,"text":"1014009 - 1983 - Benefits to trout growers from U.S. Fish and Wildlife Service Research: an overview of recent advances","interactions":[],"lastModifiedDate":"2012-02-02T00:04:17","indexId":"1014009","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3330,"text":"Salmonid","active":true,"publicationSubtype":{"id":10}},"title":"Benefits to trout growers from U.S. Fish and Wildlife Service Research: an overview of recent advances","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Salmonid","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"520/FH","usgsCitation":"Wolf, K., 1983, Benefits to trout growers from U.S. Fish and Wildlife Service Research: an overview of recent advances: Salmonid, v. 6, no. 5, p. 6-10, 21.","productDescription":"p. 6-10, 21","startPage":"6","endPage":"10, 21","numberOfPages":"5","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b880","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":319612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011250,"text":"70011250 - 1983 - The nature of carbon dioxide waters in Snaefellsnes, western Iceland","interactions":[],"lastModifiedDate":"2024-04-19T18:38:31.995449","indexId":"70011250","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1828,"text":"Geothermics","active":true,"publicationSubtype":{"id":10}},"title":"The nature of carbon dioxide waters in Snaefellsnes, western Iceland","docAbstract":"

Over 20 occurrences of thermal and non-thermal waters rich in carbon dioxide are known in the Snaefellsnes Peninsula of western Iceland. On the basis of the thermal, chemical and isotopic characteristics of these waters, and hydrological considerations, it is concluded that they represent meteoric waters which have seeped to variable depths into the bedrock. Ascending carbon dioxide gas originating from intrusions or the mantle mixes with the meteoric waters to produce carbon dioxide waters: at considerable depth in the case of the thermal carbon dioxide waters but close to the surface in the case of cold carbon dioxide waters. The occurrence of carbon dioxide waters cannot be regarded as evidence for underground geothermal reservoirs.

","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6505(83)90027-5","issn":"03756505","usgsCitation":"Arnorsson, S., and Barnes, I., 1983, The nature of carbon dioxide waters in Snaefellsnes, western Iceland: Geothermics, v. 12, no. 2-3, p. 171-176, https://doi.org/10.1016/0375-6505(83)90027-5.","productDescription":"6 p.","startPage":"171","endPage":"176","numberOfPages":"6","costCenters":[],"links":[{"id":221652,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Iceland","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -25.048828125,\n 63.11463763252091\n ],\n [\n -12.919921874999998,\n 63.11463763252091\n ],\n [\n -12.919921874999998,\n 66.8265202749748\n ],\n [\n -25.048828125,\n 66.8265202749748\n ],\n [\n -25.048828125,\n 63.11463763252091\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"12","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae03e4b08c986b323eb6","contributors":{"authors":[{"text":"Arnorsson, S.","contributorId":96828,"corporation":false,"usgs":true,"family":"Arnorsson","given":"S.","email":"","affiliations":[],"preferred":false,"id":360662,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, I.","contributorId":23678,"corporation":false,"usgs":true,"family":"Barnes","given":"I.","affiliations":[],"preferred":false,"id":360661,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010304,"text":"70010304 - 1983 - Stability of streams and lakes on Mars","interactions":[],"lastModifiedDate":"2024-02-16T12:20:34.967206","indexId":"70010304","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Stability of streams and lakes on Mars","docAbstract":"

Under present climatic conditions streams and lakes on Mars will freeze. Freezing is slow and would have a negligible effect in impeding flow of the large floods that are believed to have eroded the outflow channels. Valley networks are more difficult to form under current climatic conditions since they appear to have formed by slow erosion by streams of modest discharges. Freezing of small Martian streams was modeled for a variety of climatic conditions on the supposition that the Martian atmosphere may have been considerably thicker in the past when the valley networks formed. The modeling involves examination of the energy balance at the upper and lower surfaces of ice on streams to determine the rate at which the ice thickens with time. The results indicate that freezing rates are not strongly dependent on atmospheric pressure. With no wind, increasing the pressure by a factor of 10 cuts the time taken to freeze solid only by about a factor of about 2. Under windy conditions dependence on atmospheric pressure is even weaker. The distance that water could travel in a stream before flow is arrested by freezing is also calculated. The distances depend on the initial temperature of the stream and when icings develop, but in general, if a stream deeper than 2 m can be initiated and sustained, the water within it can survive long enough to cut most of the valley networks observed. The main problem with forming the valley is initiating the flow. Groundwater seepage alone appears inadequate because of the difficulty of recharging the groundwater system. Melting of ice precipitated onto the surface following injection of water into the atmosphere by large impacts is a possible source of water, but the climatic conditions under which the ice could melt and the water be collected into streams that can survive long enough to cut the valley is uncertain.




","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(83)90168-9","issn":"00191035","usgsCitation":"Carr, M.H., 1983, Stability of streams and lakes on Mars: Icarus, v. 56, no. 3, p. 476-495, https://doi.org/10.1016/0019-1035(83)90168-9.","productDescription":"20 p.","startPage":"476","endPage":"495","numberOfPages":"20","costCenters":[],"links":[{"id":219443,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b965ce4b08c986b31b46d","contributors":{"authors":[{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":358584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011251,"text":"70011251 - 1983 - Distribution of differentiated tholeiitic basalts on the lower east rift zone of Kilauea Volcano, Hawaii: A possible guide to geothermal exploration","interactions":[],"lastModifiedDate":"2024-01-31T01:38:15.121082","indexId":"70011251","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of differentiated tholeiitic basalts on the lower east rift zone of Kilauea Volcano, Hawaii: A possible guide to geothermal exploration","docAbstract":"

Geologic mapping of the lower east rift zone of Kilauea Volcano, Hawaii, indicates that more than 100 eruptions have extruded an estimated 10 km3 of basalt during the past 2,000 yr. Six eruptions in the past 200 yr have extruded about 1 km3. The eruptive recurrence interval has ranged from 1 to 115 yr since the middle 18th century and has averaged 20 yr or less over the past 2,000 yr.

One hundred new chemical analyses indicate that the erupted tholeiites commonly are differentiated beyond olivine control or are hybrid mixtures of differentiates with more mafic (olivine-controlled) summit magmas. The distribution of vents for differentiated lavas indicates that several large magma chambers underlie the lower east rift zone. Several workers have recognized that a chamber underlies the area near a producing well, HGP-A; petrologic and 14C data indicate that it has existed for at least 1,300 yr. Stratigraphy, petrology, and surface deformation patterns suggest that two other areas, Heiheiahulu and Kaliu, also overlie large magma chambers and appear to be favorable geothermal prospects.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1983)11<136:DODTBO>2.0.CO;2","issn":"00917613","usgsCitation":"Moore, R.B., 1983, Distribution of differentiated tholeiitic basalts on the lower east rift zone of Kilauea Volcano, Hawaii: A possible guide to geothermal exploration: Geology, v. 11, no. 3, p. 136-140, https://doi.org/10.1130/0091-7613(1983)11<136:DODTBO>2.0.CO;2.","productDescription":"5 p.","startPage":"136","endPage":"140","numberOfPages":"5","costCenters":[],"links":[{"id":221653,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a02c8e4b0c8380cd501d9","contributors":{"authors":[{"text":"Moore, R. B.","contributorId":98720,"corporation":false,"usgs":true,"family":"Moore","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":360663,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011253,"text":"70011253 - 1983 - INTERACTIVE NAME PLACEMENT FOR PROVISIONAL MAPS.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:08","indexId":"70011253","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"INTERACTIVE NAME PLACEMENT FOR PROVISIONAL MAPS.","docAbstract":"Computer generation and placement of map type has been refined into a production mode at Mid-Continent Mapping Center (MCMC) for USGS 1:24,000- and 1:25,000-scale Provisional maps. The map collar program is written in FORTRAN using batch processing that allows the program to work in the background.","largerWorkTitle":"Technical Papers of the American Congress of Surveying and Mapping","conferenceTitle":"Technical Papers of the 43rd Annual Meeting of the American Congress on Surveying and Mapping.","conferenceLocation":"Washington, DC, USA","language":"English","publisher":"American Congress on Surveying & Mapping","publisherLocation":"Falls Church, VA, USA","usgsCitation":"Goldberg, J.L., and Miller, T.C., 1983, INTERACTIVE NAME PLACEMENT FOR PROVISIONAL MAPS., in Technical Papers of the American Congress of Surveying and Mapping, Washington, DC, USA, p. 314-321.","startPage":"314","endPage":"321","numberOfPages":"8","costCenters":[],"links":[{"id":221742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a37d0e4b0c8380cd611b7","contributors":{"authors":[{"text":"Goldberg, Jeffrey L.","contributorId":59947,"corporation":false,"usgs":true,"family":"Goldberg","given":"Jeffrey","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":360666,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Thomas C.","contributorId":13752,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":360665,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011246,"text":"70011246 - 1983 - Clay mineral formation and transformation in rocks and soils","interactions":[],"lastModifiedDate":"2020-01-19T11:27:27","indexId":"70011246","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3047,"text":"Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Clay mineral formation and transformation in rocks and soils","docAbstract":"Three mechanisms for clay mineral formation (inheritance, neoformation, and transformation) operating in three geological environments (weathering, sedimentary, and diagenetic-hydrothermal) yield nine possibilities for the origin of clay minerals in nature. Several of these possibilities are discussed in terms of the rock cycle. The mineralogy of clays neoformed in the weathering environment is a function of solution chemistry, with the most dilute solutions favoring formation of the least soluble clays. After erosion and transportation, these clays may be deposited on the ocean floor in a lateral sequence that depends on floccule size. Clays undergo little reaction in the ocean, except for ion exchange and the neoformation of smectite; therefore, most clays found on the ocean floor are inherited from adjacent continents. Upon burial and heating, however, dioctahedral smectite reacts in the diagenetic environment to yield mixed-layer illite-smectite, and finally illite. With uplift and weathering, the cycle begins again. Refs.","language":"English","publisher":"Royal Society of London","doi":"10.1098/rsta.1984.0026","usgsCitation":"Eberl, D.D., 1983, Clay mineral formation and transformation in rocks and soils: Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, v. 311, no. 1517, p. 241-257, https://doi.org/10.1098/rsta.1984.0026.","productDescription":"17 p.","startPage":"241","endPage":"257","numberOfPages":"17","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"311","issue":"1517","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f2d0e4b0c8380cd4b3c5","contributors":{"authors":[{"text":"Eberl, D. D.","contributorId":66282,"corporation":false,"usgs":true,"family":"Eberl","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":360653,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011254,"text":"70011254 - 1983 - Kinetic analysis of strontium and potassium sorption onto sands and gravels in a natural channel","interactions":[],"lastModifiedDate":"2020-01-26T09:40:18","indexId":"70011254","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Kinetic analysis of strontium and potassium sorption onto sands and gravels in a natural channel","docAbstract":"

A kinetic, first-order mass transfer model was used to describe the sorption of strontium onto sand- and gravel-sized streambed sediments. Rate parameters, empirically determined for strontium, allowed for the prediction of potassium sorption with moderate success. The model parameters varied significantly with particle size. The sorption data were collected during an experimental injection of several elements into a small mountain pool-and-riffle stream. The sorption process onto sand- and gravel-sized sediment was relatively slow compared to changes in the dissolved concentrations.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR019i003p00725","usgsCitation":"Bencala, K.E., Jackman, A.P., Kennedy, V.C., Avanzino, R.J., and Zellweger, G.W., 1983, Kinetic analysis of strontium and potassium sorption onto sands and gravels in a natural channel: Water Resources Research, v. 19, no. 3, p. 725-731, https://doi.org/10.1029/WR019i003p00725.","productDescription":"7 p.","startPage":"725","endPage":"731","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505a40a3e4b0c8380cd64f07","contributors":{"authors":[{"text":"Bencala, Kenneth E. kbencala@usgs.gov","contributorId":1541,"corporation":false,"usgs":true,"family":"Bencala","given":"Kenneth","email":"kbencala@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":360671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackman, Alan P.","contributorId":28239,"corporation":false,"usgs":true,"family":"Jackman","given":"Alan","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":360669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kennedy, Vance C.","contributorId":102063,"corporation":false,"usgs":true,"family":"Kennedy","given":"Vance","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":360668,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Avanzino, Ronald J.","contributorId":24355,"corporation":false,"usgs":true,"family":"Avanzino","given":"Ronald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":360667,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zellweger, Gary W.","contributorId":71171,"corporation":false,"usgs":true,"family":"Zellweger","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":360670,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70011255,"text":"70011255 - 1983 - Influence of the Onion Creek salt diapir on the late Cenozoic history of Fisher Valley, southeastern Utah","interactions":[],"lastModifiedDate":"2024-01-31T01:35:29.538671","indexId":"70011255","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Influence of the Onion Creek salt diapir on the late Cenozoic history of Fisher Valley, southeastern Utah","docAbstract":"

More than 140 m of upper Cenozoic basin-fill sediments were deposited and then deformed in Fisher Valley between about 2.5 and 0.25 m.y. ago, in response to uplift of the adjacent Onion Creek salt diapir. In addition to these basin-fill sediments, minor amounts of eolian and fluvial sand were deposited in Holocene time. The sediments, whose relative ages are known from the stratigraphy, are predominantly sandy, second-cycle red beds derived from nearby Mesozoic rocks; most were deposited in a vertical sequence, filling a sedimentary basin now exposed by fluvial dissection. We have applied a variety of established and experimental dating methods to the sediments in Fisher Valley to establish their age and to provide time control for the recent history of the Onion Creek salt diapir.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1986)97<1422:DTUCSI>2.0.CO;2","issn":"00917613","usgsCitation":"Colman, S.M., 1983, Influence of the Onion Creek salt diapir on the late Cenozoic history of Fisher Valley, southeastern Utah: Geology, v. 11, no. 4, p. 240-243, https://doi.org/10.1130/0016-7606(1986)97<1422:DTUCSI>2.0.CO;2.","productDescription":"4 p.","startPage":"240","endPage":"243","numberOfPages":"4","costCenters":[],"links":[{"id":221744,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b87e4b0c8380cd625f9","contributors":{"authors":[{"text":"Colman, Steven M. 0000-0002-0564-9576","orcid":"https://orcid.org/0000-0002-0564-9576","contributorId":77482,"corporation":false,"usgs":true,"family":"Colman","given":"Steven","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":360672,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010557,"text":"70010557 - 1983 - Paleohydrological methods and some examples from Swedish fluvial environments I. Cobble and boulder deposits","interactions":[],"lastModifiedDate":"2023-12-19T00:53:07.339161","indexId":"70010557","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1767,"text":"Geografiska Annaler, Series A","active":true,"publicationSubtype":{"id":10}},"title":"Paleohydrological methods and some examples from Swedish fluvial environments I. Cobble and boulder deposits","docAbstract":"

This article establishes approximate empirical relations for determining the minimum unit stream power, bed shear stress and mean flow velocity capable of moving cobbles and boulders on streambeds. The derived equations then are used to estimate the minimum paleoflows that could have transported the boulders of two ancient fluvial deposits in Sweden. The flow estimates are compared with those made by more conventional hydraulic methods. Bankfull flows also are estimated for one of the two deposits, using various hydraulic equations.

","language":"English","publisher":"Taylor and Francis","doi":"10.1080/04353676.1983.11880088","usgsCitation":"Williams, G.P., 1983, Paleohydrological methods and some examples from Swedish fluvial environments I. Cobble and boulder deposits: Geografiska Annaler, Series A, v. 65 A, no. 3-4, p. 227-243, https://doi.org/10.1080/04353676.1983.11880088.","productDescription":"17 p.","startPage":"227","endPage":"243","numberOfPages":"17","costCenters":[],"links":[{"id":219018,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Sweden","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[22.18317,65.72374],[21.21352,65.02601],[21.36963,64.41359],[19.77888,63.60955],[17.84778,62.7494],[17.11955,61.34117],[17.83135,60.63658],[18.78772,60.08191],[17.86922,58.95377],[16.82919,58.71983],[16.44771,57.04112],[15.87979,56.1043],[14.66668,56.20089],[14.10072,55.40778],[12.94291,55.36174],[12.6251,56.30708],[11.78794,57.44182],[11.02737,58.85615],[11.46827,59.43239],[12.30037,60.11793],[12.63115,61.29357],[11.99206,61.80036],[11.93057,63.12832],[12.57994,64.06622],[13.57192,64.04911],[13.91991,64.44542],[13.55569,64.78703],[15.10841,66.19387],[16.10871,67.30246],[16.76888,68.01394],[17.72918,68.01055],[17.99387,68.56739],[19.87856,68.40719],[20.02527,69.06514],[20.64559,69.10625],[21.97853,68.61685],[23.53947,67.93601],[23.56588,66.39605],[23.90338,66.00693],[22.18317,65.72374]]]},\"properties\":{\"name\":\"Sweden\"}}]}","volume":"65 A","issue":"3-4","noUsgsAuthors":false,"publicationDate":"2017-08-08","publicationStatus":"PW","scienceBaseUri":"505a73f8e4b0c8380cd7736f","contributors":{"authors":[{"text":"Williams, G. P.","contributorId":97472,"corporation":false,"usgs":true,"family":"Williams","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":359165,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011272,"text":"70011272 - 1983 - The use of MAGSAT data to determine secular variation","interactions":[],"lastModifiedDate":"2024-06-28T16:51:26.602642","indexId":"70011272","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"The use of MAGSAT data to determine secular variation","docAbstract":"

A combined spatial and secular variation model of the geomagnetic field, labeled M061581, is derived from a selection of Magsat data. Secular variation (SV) data computed from linear fits to midnight hourly values from 19 magnetic observatories were also included in the analysis but were seen to have little effect on the model. The SV patterns from this new model are compared with those from the 1980 IGRF and with those for 1970 computed by the DGRF and with the 1960 patterns computed using the GSFC(12/66) model. Most of the features of the M061581 are identical in location and level with those of the 1980 IGRF. Together they confirm that the reversals in sign of field change seen over Asia and North America between 1965 and 1975 are reverting to the pre-1965 states. The M061581 model gives −32 nT/yr for the dipole decay rate, larger than the 70% increase already reported since 1965. This abnormally high value is interpreted as being a defect of the model because it appears to result from a much larger (−100 nT/yr) drop in field over the polar regions not indicated by the 1980 IGRF. This north polar decrease is shown to be of external origin as the result of a combination of the seasonal effect of the north polar ionospheric (counterclockwise) afternoon Sqp cell increasing in intensity from the beginning (November 1979) to the end (June 1980) of the Magsat data collection period, coupled with an enhancement of its effect as the orbit lowered from the 350– 550 km initial altitudes to near 200 km just prior to burnup. This experiment indicates that secular variation can be obtained from satellite data for intervals of less than a full year if corrections can be made for seasonal effects and that ‘annual snapshots’ of the field by a satellite would allow easy and accurate models of secular change without the use of any surface data.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB088iB07p05903","issn":"01480227","usgsCitation":"Cain, J., Frayser, J., Muth, L., and Schmitz, D., 1983, The use of MAGSAT data to determine secular variation: Journal of Geophysical Research Solid Earth, v. 88, no. B7, p. 5903-5910, https://doi.org/10.1029/JB088iB07p05903.","productDescription":"8 p.","startPage":"5903","endPage":"5910","numberOfPages":"8","costCenters":[],"links":[{"id":220893,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"B7","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505bb15be4b08c986b3252eb","contributors":{"authors":[{"text":"Cain, J.C.","contributorId":68457,"corporation":false,"usgs":true,"family":"Cain","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":360720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frayser, J.","contributorId":83665,"corporation":false,"usgs":true,"family":"Frayser","given":"J.","affiliations":[],"preferred":false,"id":360721,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Muth, L.","contributorId":10035,"corporation":false,"usgs":true,"family":"Muth","given":"L.","email":"","affiliations":[],"preferred":false,"id":360718,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schmitz, D.","contributorId":45832,"corporation":false,"usgs":true,"family":"Schmitz","given":"D.","email":"","affiliations":[],"preferred":false,"id":360719,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70010555,"text":"70010555 - 1983 - CONTRIBUTION OF LAND USE DATA TO THE INVESTIGATION OF TRENDS IN FLOODING IN THE TUG FORK BASIN OF KENTUCKY, VIRGINIA, AND WEST VIRGINIA.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:17","indexId":"70010555","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"CONTRIBUTION OF LAND USE DATA TO THE INVESTIGATION OF TRENDS IN FLOODING IN THE TUG FORK BASIN OF KENTUCKY, VIRGINIA, AND WEST VIRGINIA.","docAbstract":"The U. S. Geological Survey, in cooperation with the U. S. Bureau of Mines and the Office of Surface Mining Reclamation and Enforcement, is investigating effects of mining on flood frequency and magnitude within the basin. Changing land use, particularly the acceleration of surface mining, may cause or contribute to flooding problems.","largerWorkTitle":"Technical Papers of the American Congress of Surveying and Mapping","conferenceTitle":"Technical Papers of the 43rd Annual Meeting of the American Congress on Surveying and Mapping.","conferenceLocation":"Washington, DC, USA","language":"English","publisher":"American Congress on Surveying & Mapping","publisherLocation":"Falls Church, VA, USA","usgsCitation":"Bowers, S.E., and Scott, A.G., 1983, CONTRIBUTION OF LAND USE DATA TO THE INVESTIGATION OF TRENDS IN FLOODING IN THE TUG FORK BASIN OF KENTUCKY, VIRGINIA, AND WEST VIRGINIA., in Technical Papers of the American Congress of Surveying and Mapping, Washington, DC, USA, p. 376-383.","startPage":"376","endPage":"383","numberOfPages":"8","costCenters":[],"links":[{"id":218964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f2dfe4b0c8380cd4b451","contributors":{"authors":[{"text":"Bowers, Sarah E.","contributorId":71311,"corporation":false,"usgs":true,"family":"Bowers","given":"Sarah","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, Arthur G.","contributorId":81885,"corporation":false,"usgs":true,"family":"Scott","given":"Arthur","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":359163,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1007644,"text":"1007644 - 1983 - Temporal patterns of seed use and availability in a guild of desert ants","interactions":[],"lastModifiedDate":"2023-09-29T15:49:23.408226","indexId":"1007644","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1455,"text":"Ecological Entomology","active":true,"publicationSubtype":{"id":10}},"title":"Temporal patterns of seed use and availability in a guild of desert ants","docAbstract":"","language":"English","publisher":"Royal Entomological Society","doi":"10.1111/j.1365-2311.1983.tb00484.x","usgsCitation":"Mehlhop, P., and Scott, N.J., 1983, Temporal patterns of seed use and availability in a guild of desert ants: Ecological Entomology, v. 8, p. 69-85, https://doi.org/10.1111/j.1365-2311.1983.tb00484.x.","productDescription":"17 p.","startPage":"69","endPage":"85","numberOfPages":"17","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130132,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","noUsgsAuthors":false,"publicationDate":"2008-03-14","publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685549","contributors":{"authors":[{"text":"Mehlhop, Patricia","contributorId":67046,"corporation":false,"usgs":true,"family":"Mehlhop","given":"Patricia","email":"","affiliations":[],"preferred":false,"id":315782,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, Norman J. Jr.","contributorId":91348,"corporation":false,"usgs":true,"family":"Scott","given":"Norman","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":315781,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011249,"text":"70011249 - 1983 - VARIATIONS IN MINERAL MATTER CONTENT OF A PEAT DEPOSIT IN MAINE RESTING ON GLACIO-MARINE SEDIMENTS.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:29","indexId":"70011249","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"VARIATIONS IN MINERAL MATTER CONTENT OF A PEAT DEPOSIT IN MAINE RESTING ON GLACIO-MARINE SEDIMENTS.","docAbstract":"The Great Heath, Washington County, Maine, is an excellent example of a multidomed ombrotrophic peatland resting on a gently undulating surface of glacio-marine sediments and towering above modern streams. A comprehensive study sponsored by the Geological Survey of Maine in cooperation with the U. S. Geological Survey included preparation of a contoured surficial geology map on which are located 81 core sites. Eight cross sections accompany the map showing occurrence and thickness of three types of organic material and locations of cored sample analyses. Refs.","largerWorkTitle":"Los Alamos National Laboratory (Report) LA","conferenceTitle":"Mineral Matter in Peat: Its Occurrence, Form, and Distribution.","conferenceLocation":"Los Alamos, NM, USA","language":"English","usgsCitation":"Cameron, C., and Schruben, P., 1983, VARIATIONS IN MINERAL MATTER CONTENT OF A PEAT DEPOSIT IN MAINE RESTING ON GLACIO-MARINE SEDIMENTS., in Los Alamos National Laboratory (Report) LA, Los Alamos, NM, USA, p. 63-76.","startPage":"63","endPage":"76","numberOfPages":"14","costCenters":[],"links":[{"id":221515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc0e5e4b08c986b32a3a0","contributors":{"authors":[{"text":"Cameron, Cornelia C.","contributorId":103002,"corporation":false,"usgs":true,"family":"Cameron","given":"Cornelia C.","affiliations":[],"preferred":false,"id":360660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schruben, Paul","contributorId":30249,"corporation":false,"usgs":true,"family":"Schruben","given":"Paul","email":"","affiliations":[],"preferred":false,"id":360659,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011261,"text":"70011261 - 1983 - A method of calculating quartz solubilities in aqueous sodium chloride solutions","interactions":[],"lastModifiedDate":"2024-03-19T15:53:17.532025","indexId":"70011261","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"A method of calculating quartz solubilities in aqueous sodium chloride solutions","docAbstract":"

The aqueous silica species that form when quartz dissolves in water or saline solutions are hydrated. Therefore, the amount of quartz that will dissolve at a given temperature is influenced by the prevailing activity of water. Using a standard state in which there are 1,000 g of water (55.51 moles) per 1,000 cm3 of solution allows activity of water in a NaCl solution at high temperature to be closely approximated by the effective density of water, pe, in that solution, i.e. the product of the density of the NaCl solution times the weight fraction of water in the solution, corrected for the amount of water strongly bound to aqueous silica and Na+ as water of hydration. Generally, the hydration of water correction is negligible.

The solubility of quartz in pure water is well known over a large temperature-pressure range. An empirical formula expresses that solubility in terms of temperature and density of water and thus takes care of activity coefficient and pressure-effect terms. Solubilities of quartz in NaCl solutions can be calculated by using that equation and substituting pe, for the density of pure water. Calculated and experimentally determined quartz solubilities in NaCl solutions show excellent agreement when the experiments were carried out in non-reactive platinum, gold, or gold plus titanium containers. Reactive metal containers generally yield dissolved silica concentrations higher than calculated, probably because of the formation of metal chlorides plus NaOH and H2. In the absence of NaOH there appears to be no detectable silica complexing in NaCl solutions, and the variation in quartz solubility with NaCl concentration at constant temperature can be accounted for entirely by variations in the activity of water.

The average hydration number per molecule of dissolved SiO2 in liquid water and NaCl solutions decreases from about 2.4 at 200°C to about 2.1 at 350°C. This suggests that H4SiO4 may be the dominant aqueous silica species at 350°C, but other polymeric forms become important at lower temperatures.

","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(83)90279-X","issn":"00167037","usgsCitation":"Fournier, R., 1983, A method of calculating quartz solubilities in aqueous sodium chloride solutions: Geochimica et Cosmochimica Acta, v. 47, no. 3, p. 579-586, https://doi.org/10.1016/0016-7037(83)90279-X.","productDescription":"8 p.","startPage":"579","endPage":"586","numberOfPages":"8","costCenters":[],"links":[{"id":220759,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e45ae4b0c8380cd465e0","contributors":{"authors":[{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":360689,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011274,"text":"70011274 - 1983 - Role of fluid mixing and fault-related sulfide in the origin of the Ray Point uranium district, south Texas","interactions":[],"lastModifiedDate":"2024-01-11T16:42:28.609707","indexId":"70011274","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Role of fluid mixing and fault-related sulfide in the origin of the Ray Point uranium district, south Texas","docAbstract":"

The Lamprecht and Felder deposits are roll-type deposits hosted by the Miocene Oakville Sandstone. Four distinct stages of FeS 2 mineral formation are recognized: (1) a generation of isotopically light (delta 34 S < -20 per mil) preore pyrite, (2) a generation of isotopically light (delta 34 S < -20 per mil) marcasite that formed mostly before, but also during ore deposition, (3) a postore generation of isotopically heavy pyrite (delta 34 S > 0 per mil), and (4) a yet later generation of marcasite with isotopically light sulfur close to the values of stages 1 and 2. Complex zone of mixing between saline brines migrating up the fault from depth and oxygenated meteoric water recharging at the outcrop. Bacterial activity.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.78.6.1043","issn":"03610128","usgsCitation":"Goldhaber, M., Reynolds, R.L., and Rye, R.O., 1983, Role of fluid mixing and fault-related sulfide in the origin of the Ray Point uranium district, south Texas: Economic Geology, v. 78, no. 6, p. 1043-1063, https://doi.org/10.2113/gsecongeo.78.6.1043.","productDescription":"21 p.","startPage":"1043","endPage":"1063","numberOfPages":"21","costCenters":[],"links":[{"id":220895,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"78","issue":"6","noUsgsAuthors":false,"publicationDate":"1983-10-01","publicationStatus":"PW","scienceBaseUri":"505aae50e4b0c8380cd87083","contributors":{"authors":[{"text":"Goldhaber, M. B. 0000-0002-1785-4243","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":103280,"corporation":false,"usgs":true,"family":"Goldhaber","given":"M. B.","affiliations":[],"preferred":false,"id":360726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, R. L. 0000-0002-4572-2942","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":79885,"corporation":false,"usgs":true,"family":"Reynolds","given":"R.","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":360725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rye, R. O.","contributorId":66208,"corporation":false,"usgs":true,"family":"Rye","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":360724,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010554,"text":"70010554 - 1983 - A strategy for mineral and energy resource independence","interactions":[],"lastModifiedDate":"2013-02-20T20:55:04","indexId":"70010554","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":661,"text":"Advances in Space Research","active":true,"publicationSubtype":{"id":10}},"title":"A strategy for mineral and energy resource independence","docAbstract":"Data acquired by Landsats 1, 2, and 3, are beginning to provide the information on which an improved mineral and energy resource exploration strategy can be based. Landsat 4 is expected to augment this capability with its higher resolution (30 m) and additional spectral bands in the Thematic Mapper (TM) designed specifically to discriminate clay minerals associated with mineral alteration. In addition, a new global magnetic anomaly map, derived from the recent Magsat mission, has recently been compiled by the National Aeronautics and Space Administration (NASA), the U.S. Geological Survey (USGS), and others. Preliminary, extremely small-scale renditions of this map indicate that global coverage is nearly complete and that the map will improve upon a previous one derived from Polar Orbiting Geophysical Observatory (POGO) data. Digital processing of the Landsat image data and Magsat geophysical data can be used to create three-dimensional stereoscopic models for which Landsat images provide surface reference to deep structural anomalies. Comparative studies of national Landsat lineament maps, Magsat stereoscopic models, and metallogenic information derived from the Computerized Resources Information Bank (CRIB) inventory of U.S. mineral resources, provide a way of identifying and selecting exploration areas that have mineral resource potential. Landsat images and computer-compatible tapes can provide new and better mosaics and also provide the capability for a closer look at promising sites. ?? 1983.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Advances in Space Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0273-1177(83)90124-2","issn":"02731177","usgsCitation":"Carter, W.D., 1983, A strategy for mineral and energy resource independence: Advances in Space Research, v. 3, no. 2, p. 223-236, https://doi.org/10.1016/0273-1177(83)90124-2.","startPage":"223","endPage":"236","numberOfPages":"14","costCenters":[],"links":[{"id":218963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267879,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0273-1177(83)90124-2"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e5b5e4b0c8380cd46f22","contributors":{"authors":[{"text":"Carter, W. D.","contributorId":75633,"corporation":false,"usgs":true,"family":"Carter","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":359161,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011144,"text":"70011144 - 1983 - Gravity studies in the Cascade Range","interactions":[],"lastModifiedDate":"2023-07-12T18:49:09.945462","indexId":"70011144","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Gravity studies in the Cascade Range","docAbstract":"A compatible set of gravity data has been compiled for the entire Cascade Range. From this data set a series of interpretive color gravity maps have been prepared, including a free air anomaly map, Bouguer anomaly map at a principle, and an alternate reduction density, and filtered and derivative versions of the Bouguer anomaly map. The regional anomaly pattern and gradients outline the various geological provinces adjacent to the Cascade Range and delineate major structural elements in the range. The more local anomalies and gradients may delineate low density basin and caldera fill, faults, and shallow plutons. Refs.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Transactions - Geothermal Resources Council","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Geothermal Resources: Energy on Tap! Geothermal Resources Council 1983 Annual Meeting.","conferenceDate":"1983","conferenceLocation":"Portland, Oregon, United States","language":"English","publisher":"Geothermal Resources Council","publisherLocation":"Davis, CA, USA","issn":"01935933","isbn":"093441257X","usgsCitation":"Finn, C.A., and Williams, D., 1983, Gravity studies in the Cascade Range, in Transactions - Geothermal Resources Council, v. 7, Portland, Oregon, United States, 1983, p. 247-251.","productDescription":"5 p.","startPage":"247","endPage":"251","costCenters":[],"links":[{"id":220818,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Oregon, Washington","otherGeospatial":"Cascade Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.56484562362637,\n 40.5290042884144\n ],\n [\n -122.32275197558576,\n 40.52257003161097\n ],\n [\n -121.474514217935,\n 41.1287673203594\n ],\n [\n -121.474514217935,\n 42.08013935532142\n ],\n [\n -121.79092036563003,\n 42.67981755225486\n ],\n [\n -121.58895899476082,\n 43.407962341123465\n ],\n [\n -121.19176829871805,\n 44.46474435738827\n ],\n [\n -120.94268260797968,\n 45.285635278829716\n ],\n [\n -120.51183168345878,\n 45.846477078764195\n ],\n [\n -120.43777918080681,\n 46.37850392962855\n ],\n [\n -119.85209120528538,\n 46.75556849240482\n ],\n [\n -119.91941166224206,\n 47.59753664766524\n ],\n [\n -119.48182869202503,\n 48.3188429440041\n ],\n [\n -119.38758005228632,\n 48.994768779433485\n ],\n [\n -122.28909174710762,\n 48.99918566683198\n ],\n [\n -122.524713346455,\n 48.675723095781734\n ],\n [\n -122.24196742723805,\n 48.41276719804202\n ],\n [\n -121.93902537093442,\n 47.909835084653764\n ],\n [\n -122.14072629860917,\n 47.53097926013987\n ],\n [\n -121.9993533390009,\n 47.27581787315788\n ],\n [\n -122.30229539530455,\n 46.91375554777727\n ],\n [\n -122.7533429031046,\n 46.849335173305235\n ],\n [\n -122.87451972562613,\n 46.000158831216226\n ],\n [\n -122.47059698388682,\n 45.58662057756328\n ],\n [\n -122.6254340348865,\n 45.070740944306834\n ],\n [\n -123.06301700510309,\n 44.189237840604534\n ],\n [\n -123.38615519849431,\n 43.17602762303008\n ],\n [\n -123.42654747266815,\n 42.6038855060948\n ],\n [\n -123.2245861017989,\n 42.345686032794134\n ],\n [\n -122.90144790840814,\n 41.57981163343143\n ],\n [\n -122.82066336006048,\n 40.83021947976849\n ],\n [\n -122.56484562362637,\n 40.5290042884144\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1481e4b0c8380cd54a78","contributors":{"authors":[{"text":"Finn, Carol A. 0000-0002-6178-0405 cfinn@usgs.gov","orcid":"https://orcid.org/0000-0002-6178-0405","contributorId":1326,"corporation":false,"usgs":true,"family":"Finn","given":"Carol","email":"cfinn@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":360385,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, David","contributorId":33989,"corporation":false,"usgs":true,"family":"Williams","given":"David","affiliations":[],"preferred":false,"id":360386,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011257,"text":"70011257 - 1983 - Paleohydraulic reconstruction of flash- flood peaks from boulder deposits in the Colorado Front Range","interactions":[],"lastModifiedDate":"2024-01-03T12:32:31.770285","indexId":"70011257","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Paleohydraulic reconstruction of flash- flood peaks from boulder deposits in the Colorado Front Range","docAbstract":"

Nine watersheds in the Colorado Front Range with steep bedrock channels were used to test the accuracy of paleohydraulic reconstruction of large flash floods using boulder deposits. The nine basins consist of eight small ungauged basins ranging in size from 1.6 to 29 km2 and the Big Thompson River at the mouth of the Big Thompson Canyon, draining 790 km2. Between 1923 and 1976, all nine basins had had one catastrophic flash flood, the magnitude of which has been estimated by the conventional slope-area method.

In each basin, coarse boulder deposits of the large flash floods were identified, and three axes of the five largest boulders were measured, along with at least two profiles of the valley cross section. A simple arithmetic average of two theoretical and two empirical relationships was used to estimate average flood velocity using boulder size and shape. Average depth was estimated as the arithmetic average of four values computed from the Manning equation, a regression equation for boulder size and unit stream power, a relative smoothness equation, and a modified Shields' relationship. The appropriate flood width for the estimated average depth was found by iteration, using the valley cross sections.

The paleohydraulic discharges thus computed generally underestimate conventional slope-area discharge estimates on small streams by as much as 75%, although the average amount is only 28% too low, and the reconstructed discharge in one stream was 31% too large. The Big Thompson River flood of 1976 was overestimated by 76%. Reasons for discrepancy in reconstructed peaks could include (1) the possibility that floods may have been able to move boulders larger than those available to be moved; (2) overestimation of the slope-area discharge because high-water marks were set prior to erosion of the channel; (3) underestimation of original roughness coefficients; and (4) macroturbulent effects during fast, deep flows.

The paleohydraulic technique is applied to two other streams in Colorado with sedimentological evidence of large flash floods, but no conventional indirect discharge estimates. A small tributary to the Big Thompson River draining 1.8 km2 has a paleohydraulic reconstructed flood peak of about 60 m3/s from a flood in 1976. Using boulders excavated from a foundation site in Holocene alluvium along Boulder Creek in Boulder, Colorado, a paleohydraulic reconstructed flood peak of between 860 and 1,512 m3/s is calculated. This is 1.4 to 2.4 times the magnitude of the estimated 500-yr flood.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1983)94<986:PROFPF>2.0.CO;2","usgsCitation":"Costa, J.E., 1983, Paleohydraulic reconstruction of flash- flood peaks from boulder deposits in the Colorado Front Range: Geological Society of America Bulletin, v. 94, no. 8, p. 986-1004, https://doi.org/10.1130/0016-7606(1983)94<986:PROFPF>2.0.CO;2.","productDescription":"19 p.","startPage":"986","endPage":"1004","numberOfPages":"19","costCenters":[],"links":[{"id":220694,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a73f4e4b0c8380cd7734b","contributors":{"authors":[{"text":"Costa, J. E.","contributorId":28977,"corporation":false,"usgs":true,"family":"Costa","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":360676,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011237,"text":"70011237 - 1983 - FINDINGS ON THE USE OF LANDSAT-3 RETURN BEAM VIDICON IMAGERY FOR DETECTING LAND USE AND LAND COVER CHANGES.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:32","indexId":"70011237","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"FINDINGS ON THE USE OF LANDSAT-3 RETURN BEAM VIDICON IMAGERY FOR DETECTING LAND USE AND LAND COVER CHANGES.","docAbstract":"The spatial resolution of imagery from the return beam vidicon (RBV) camera aboard the Landsat-3 satellite suggested that such data might prove useful in inspecting land use and land cover maps. In this study, a 1972 land use and land cover map derived from aerial photographs is compared with a 1978 Landsat RBV image to delineate areas of change. Findings indicate RBV imagery useful in establishing the fact of change and in identifying gross category changes.","largerWorkTitle":"Technical Papers of the American Congress of Surveying and Mapping","conferenceTitle":"Technical Papers of the 43rd Annual Meeting of the American Congress on Surveying and Mapping.","conferenceLocation":"Washington, DC, USA","language":"English","publisher":"American Congress on Surveying & Mapping","publisherLocation":"Falls Church, VA, USA","usgsCitation":"Milazzo, V.A., 1983, FINDINGS ON THE USE OF LANDSAT-3 RETURN BEAM VIDICON IMAGERY FOR DETECTING LAND USE AND LAND COVER CHANGES., in Technical Papers of the American Congress of Surveying and Mapping, Washington, DC, USA, p. 366-375.","startPage":"366","endPage":"375","numberOfPages":"10","costCenters":[],"links":[{"id":221100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0e76e4b0c8380cd53477","contributors":{"authors":[{"text":"Milazzo, Valerie A.","contributorId":88717,"corporation":false,"usgs":true,"family":"Milazzo","given":"Valerie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360635,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011262,"text":"70011262 - 1983 - Distribution of oceanic and continental leads in the Arabian-Nubian Shield","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011262","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of oceanic and continental leads in the Arabian-Nubian Shield","docAbstract":"New common lead data for feldspar, whole-rock, and galena samples from the Arabian-Nubian Shield, together with data from previous work, can be divided into two main groups. Group I leads have oceanic (mantle) characteristics, whereas group II leads have incorporated a continental-crustal component of at least early Proterozoic age. The group I leads are found in rocks from the Red Sea Hills of Egypt and the western and southern parts of the Arabian Shield. Group II leads are found in rocks from the northeastern and eastern parts of the Arabian Shield, as well as from the southeastern Shield near Najran. They are also found in rocks to the south in Yemen, to the east in Oman, and to the west at Aswan, Egypt. This distribution of data suggests that the Arabian-Nubian Shield has an oceanic core flanked by rocks that have developed, at least in part, from older continental material. Two mechanisms are suggested by which this older lead component could have been incorporated into the late Proterozoic rocks, and each may have operated in different parts of the Shield. The older lead component either was derived directly from an underlying early Proterozoic basement or was incorporated from subducted pelagic sediments or sediments derived from an adjacent continent. New U-Pb zircon data indicate the presence of an early Proterozoic basement southeast of Jabal Dahul in the eastern Arabian Shield. These data, together with 2,000-Ma-old zircons from the Al Amar fault zone, verify the implication of the common lead data that at least a part of the eastern Arabian Shield has an older continental basement. Because continental margins are particularly favorable locations for development of ore deposits, these findings may have important economic implications, particularly for tin, tungsten, and molybdenum exploration. ?? 1983 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF01132334","issn":"00107999","usgsCitation":"Stacey, J.S., and Stoeser, D.B., 1983, Distribution of oceanic and continental leads in the Arabian-Nubian Shield: Contributions to Mineralogy and Petrology, v. 84, no. 1, p. 91-105, https://doi.org/10.1007/BF01132334.","startPage":"91","endPage":"105","numberOfPages":"15","costCenters":[],"links":[{"id":205061,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01132334"},{"id":220760,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"84","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a02ebe4b0c8380cd5026b","contributors":{"authors":[{"text":"Stacey, J. S.","contributorId":72785,"corporation":false,"usgs":true,"family":"Stacey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":360691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoeser, D. B.","contributorId":18735,"corporation":false,"usgs":true,"family":"Stoeser","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":360690,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011267,"text":"70011267 - 1983 - Major and trace elements in Mahogany zone oil shale in two cores from the Green River Formation, piceance basin, Colorado","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011267","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Major and trace elements in Mahogany zone oil shale in two cores from the Green River Formation, piceance basin, Colorado","docAbstract":"The Parachute Creek Member of the lacustrine Green River Formation contains thick sequences of rich oil-shale. The richest sequence and the richest oil-shale bed occurring in the member are called the Mahogany zone and the Mahogany bed, respectively, and were deposited in ancient Lake Uinta. The name \"Mahogany\" is derived from the red-brown color imparted to the rock by its rich-kerogen content. Geochemical abundance and distribution of eight major and 18 trace elements were determined in the Mahogany zone sampled from two cores, U. S. Geological Survey core hole CR-2 and U. S. Bureau of Mines core hole O1-A (Figure 1). The oil shale from core hole CR-2 was deposited nearer the margin of Lake Uinta than oil shale from core hole O1-A. The major- and trace-element chemistry of the Mahogany zone from each of these two cores is compared using elemental abundances and Q-mode factor modeling. The results of chemical analyses of 44 CR-2 Mahogany samples and 76 O1-A Mahogany samples are summarized in Figure 2. The average geochemical abundances for shale (1) and black shale (2) are also plotted on Figure 2 for comparison. The elemental abundances in the samples from the two cores are similar for the majority of elements. Differences at the 95% probability level are higher concentrations of Ca, Cu, La, Ni, Sc and Zr in the samples from core hole CR-2 compared to samples from core hole O1-A and higher concentrations of As and Sr in samples from core hole O1-A compared to samples from core hole CR-2. These differences presumably reflect slight differences in depositional conditions or source material at the two sites. The Mahogany oil shale from the two cores has lower concentrations of most trace metals and higher concentrations of carbonate-related elements (Ca, Mg, Sr and Na) compared to the average shale and black shale. During deposition of the Mahogany oil shale, large quantities of carbonates were precipitated resulting in the enrichment of carbonate-related elements and dilution of most trace elements as pointed out in several previous studies. Q-mode factor modeling is a statistical method used to group samples on the basis of compositional similarities. Factor end-member samples are chosen by the model. All other sample compositions are represented by varying proportions of the factor end-members and grouped as to their highest proportion. The compositional similarities defined by the Q-mode model are helpful in understanding processes controlling multi-element distributions. The models for each core are essentially identical. A four-factor model explains 70% of the variance in the CR-2 data and 64% of the O1-A data (the average correlation coefficients are 0. 84 and 0. 80, respectively). Increasing the number of factors above 4 results in the addition of unique instead of common factors. Table I groups the elements based on high factor-loading scores (the amount of influence each element has in defining the model factors). Similar elemental associations are found in both cores. Elemental abundances are plotted as a function of core depth using a five-point weighted moving average of the original data to smooth the curve (Figure 3 and 4). The plots are grouped according to the four factors defined by the Q-mode models and show similar distributions for elements within the same factor. Factor 1 samples are rich in most trace metals. High oil yield and the presence of illite characterize the end-member samples for this factor (3, 4) suggesting that adsorption of metals onto clay particles or organic matter is controlling the distribution of the metals. Precipitation of some metals as sulfides is possible (5). Factor 2 samples are high in elements commonly associated with minerals of detrital or volcanogenic origin. Altered tuff beds and lenses are prevalent within the Mahogany zone. The CR-2 end-member samples for this factor contain analcime (3) which is an alteration product within the tuff beds of the Green River Formation. Th","largerWorkTitle":"Preprints Symposia","language":"English","issn":"05693799","usgsCitation":"Tuttle, M.L., Dean, W., and Parduhn, N.L., 1983, Major and trace elements in Mahogany zone oil shale in two cores from the Green River Formation, piceance basin, Colorado, in Preprints Symposia, v. 28, no. 1, p. 85-90.","startPage":"85","endPage":"90","numberOfPages":"6","costCenters":[],"links":[{"id":220827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4c0ae4b0c8380cd69972","contributors":{"authors":[{"text":"Tuttle, M. L.","contributorId":71992,"corporation":false,"usgs":true,"family":"Tuttle","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":360707,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dean, W.E.","contributorId":97099,"corporation":false,"usgs":true,"family":"Dean","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":360708,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parduhn, N. L.","contributorId":69136,"corporation":false,"usgs":true,"family":"Parduhn","given":"N.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":360706,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70170285,"text":"70170285 - 1983 - Was seismology lucky to acquire John Milne?","interactions":[],"lastModifiedDate":"2016-04-15T15:37:30","indexId":"70170285","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Was seismology lucky to acquire John Milne?","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Herbert-Gustar, L., and Nott, P.A., 1983, Was seismology lucky to acquire John Milne?: Earthquake Information Bulletin (USGS), v. 15, no. 5, p. 164-176.","productDescription":"13 p.","startPage":"164","endPage":"176","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320075,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571210bbe4b0ef3b7ca64464","contributors":{"authors":[{"text":"Herbert-Gustar, L.","contributorId":168613,"corporation":false,"usgs":false,"family":"Herbert-Gustar","given":"L.","email":"","affiliations":[],"preferred":false,"id":626760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nott, P. A.","contributorId":168614,"corporation":false,"usgs":false,"family":"Nott","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":626761,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047930,"text":"70047930 - 1983 - Off-road vehicular destabilization of hill slopes: the major contributing factor to destructive debris flows in Ogden, Utah, 1979","interactions":[{"subject":{"id":10474,"text":"ofr81258 - 1981 - Off-road vehicular destabilization of hillslopes: The major contributing factor to destructive debris flows in Ogden, Utah, 1979","indexId":"ofr81258","publicationYear":"1981","noYear":false,"title":"Off-road vehicular destabilization of hillslopes: The major contributing factor to destructive debris flows in Ogden, Utah, 1979"},"predicate":"SUPERSEDED_BY","object":{"id":70047930,"text":"70047930 - 1983 - Off-road vehicular destabilization of hill slopes: the major contributing factor to destructive debris flows in Ogden, Utah, 1979","indexId":"70047930","publicationYear":"1983","noYear":false,"title":"Off-road vehicular destabilization of hill slopes: the major contributing factor to destructive debris flows in Ogden, Utah, 1979"},"id":1}],"lastModifiedDate":"2015-01-16T14:43:30","indexId":"70047930","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Off-road vehicular destabilization of hill slopes: the major contributing factor to destructive debris flows in Ogden, Utah, 1979","docAbstract":"

The Wasatch Mountains in northern Utah are a north-south trending range with steep slopes caused by faulting less than 10,000 years ago. Through the natural processes of rain, frost-wedging, gravity, and earthquakes these slopes are slowly being eroded. A geologic history of instability is recorded at the base of the range in the form of landslide deposits, debris flows, and rock-fall deposits.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Environmental Effects of Off-Road Vehicles","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","doi":"10.1007/978-1-4612-5454-6_18","usgsCitation":"Nakata, J.K., 1983, Off-road vehicular destabilization of hill slopes: the major contributing factor to destructive debris flows in Ogden, Utah, 1979, chap. of Environmental Effects of Off-Road Vehicles, v. Part IV, p. 343-353, https://doi.org/10.1007/978-1-4612-5454-6_18.","productDescription":"11 p.","startPage":"343","endPage":"353","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":277195,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","city":"Ogden","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.12371826171875,\n 41.05087733907939\n ],\n [\n -112.12371826171875,\n 41.340215943707705\n ],\n [\n -111.84288024902344,\n 41.340215943707705\n ],\n [\n -111.84288024902344,\n 41.05087733907939\n ],\n [\n -112.12371826171875,\n 41.05087733907939\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"Part IV","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5221bee6e4b001cbb8a34f1f","contributors":{"editors":[{"text":"Webb, Robert H. rhwebb@usgs.gov","contributorId":1573,"corporation":false,"usgs":false,"family":"Webb","given":"Robert H.","email":"rhwebb@usgs.gov","affiliations":[{"id":12625,"text":"School of Natural Resources and the Environment, University of Arizona, Tucson, AZ, 85721, USA","active":true,"usgs":false}],"preferred":false,"id":538773,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Wilshire, Howard G.","contributorId":68346,"corporation":false,"usgs":true,"family":"Wilshire","given":"Howard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":538774,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Nakata, John K.","contributorId":32518,"corporation":false,"usgs":true,"family":"Nakata","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":483321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10355,"text":"ofr83444 - 1983 - Analytical results of a geochemical survey utilizing heavy-mineral fractions and the less-than-180-micrometer fraction of stream sediments, Tushar Mountains and adjoining areas, Marysvale volcanic field, Utah","interactions":[],"lastModifiedDate":"2023-03-21T21:15:43.766329","indexId":"ofr83444","displayToPublicDate":"1983-01-01T00:00:00","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":"83-444","title":"Analytical results of a geochemical survey utilizing heavy-mineral fractions and the less-than-180-micrometer fraction of stream sediments, Tushar Mountains and adjoining areas, Marysvale volcanic field, Utah","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83444","usgsCitation":"Miller, W.R., and Motooka, J.M., 1983, Analytical results of a geochemical survey utilizing heavy-mineral fractions and the less-than-180-micrometer fraction of stream sediments, Tushar Mountains and adjoining areas, Marysvale volcanic field, Utah: U.S. Geological Survey Open-File Report 83-444, i, 108 p., https://doi.org/10.3133/ofr83444.","productDescription":"i, 108 p.","costCenters":[],"links":[{"id":414509,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75685.htm","linkFileType":{"id":5,"text":"html"}},{"id":38199,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0444/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143374,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0444/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Marysvale volcanic field, Tushar Mountains and adjoining areas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -112,\n 38.7081\n ],\n [\n -112,\n 38.25\n ],\n [\n -112.625,\n 38.25\n ],\n [\n -112.625,\n 38.7081\n ],\n [\n -112,\n 38.7081\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c746","contributors":{"authors":[{"text":"Miller, W. Roger","contributorId":60191,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"Roger","affiliations":[],"preferred":false,"id":161245,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, J. M.","contributorId":8834,"corporation":false,"usgs":true,"family":"Motooka","given":"J.","middleInitial":"M.","affiliations":[],"preferred":false,"id":161244,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}