The 1980 eruptions of Mount St. Helens in southeast Washington resulted in a pronounced effect on the surface and ground water resources of the state. In response to the volcanic activity, the U.S. Geological Survey intensified statewide surface and ground water sampling programs to determine the nature and magnitude of the volcanic-induced variations. Streams to the east of Mount St. Helens received the major ash fallout. Chemical effects were best noted in smaller streams sampled 60 to 70 miles northeast of Mount St. Helens. The chemical variations observed were pronounced but short lived. Sulfate and chloride increases in anionic composition were prevalent immediately following the eruption however, the original bicarbonate predominance was again attained within several days. Suspended iron and aluminum concentrations were similarly elevated during the period of greatest ash deposition (highest turbidity) however, the dissolved concentrations remained relatively constant. Depressions of pH were minor and short lived. Streams draining to the south, tributaries to the Columbia river, showed little observable changes in water chemistry. Streams draining to the west (Toutle river and its tributaries) were compositionally affected by the various volcanic activities. Chloride and sulfate anion percentage exceeded the bicarbonate percentage up to one month following the eruption period. Streams and lakes sampled in the immediate vicinity of Mount St. Helens, in addition to trace metals, contained organic compounds derived from decomposing wood buried in the debris deposits. This organic material may constitute a significant source of organic compounds to surface and ground water for some time to come.
","language":"English","publisher":"U.S. Department of Energy","usgsCitation":"Bonelli, J.E., Taylor, H.E., and Klein, J., 1982, Impact of Mount St. Helens eruption on hydrology and water quality: Technical Report N-8311538, 4 p.","productDescription":"4 p.","startPage":"261","endPage":"264","costCenters":[],"links":[{"id":342794,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.9425048828125,\n 45.71385093029221\n ],\n [\n -121.51702880859374,\n 45.71385093029221\n ],\n [\n -121.51702880859374,\n 46.69089949154197\n ],\n [\n -122.9425048828125,\n 46.69089949154197\n ],\n [\n -122.9425048828125,\n 45.71385093029221\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594cd743e4b062508e3951f7","contributors":{"authors":[{"text":"Bonelli, J. E.","contributorId":35064,"corporation":false,"usgs":true,"family":"Bonelli","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":699775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":699776,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klein, J.M.","contributorId":44550,"corporation":false,"usgs":true,"family":"Klein","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":699777,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70176179,"text":"70176179 - 1981 - Assessing the risk of earthquakes in the eastern United States","interactions":[],"lastModifiedDate":"2016-08-31T11:52:18","indexId":"70176179","displayToPublicDate":"2016-03-15T00:00:00","publicationYear":"1981","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":"Assessing the risk of earthquakes in the eastern United States","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"1981, Assessing the risk of earthquakes in the eastern United States: Earthquake Information Bulletin (USGS), v. 13, no. 5, p. 175-178.","productDescription":"4 p.","startPage":"175","endPage":"178","numberOfPages":"4","costCenters":[],"links":[{"id":328122,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Central and eastern United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.55859375,\n 49.03786794532644\n ],\n [\n -90.966796875,\n 49.1242192485914\n ],\n [\n -86.7041015625,\n 48.10743118848039\n ],\n [\n -81.5185546875,\n 45.27488643704894\n ],\n [\n -81.474609375,\n 42.97250158602597\n ],\n [\n -78.1787109375,\n 44.33956524809713\n ],\n [\n -69.43359375,\n 47.635783590864854\n ],\n [\n -67.4560546875,\n 47.517200697839414\n ],\n [\n -66.796875,\n 44.77793589631623\n ],\n [\n -69.3896484375,\n 41.475660200278234\n ],\n [\n -75.3662109375,\n 34.95799531086792\n ],\n [\n -78.79394531249999,\n 30.14512718337613\n ],\n [\n -79.716796875,\n 25.20494115356912\n ],\n [\n -82.0458984375,\n 24.16680208530324\n ],\n [\n -85.4296875,\n 28.304380682962783\n ],\n [\n -88.5498046875,\n 28.497660832963472\n ],\n [\n -93.55957031249999,\n 28.57487404744697\n ],\n [\n -95.8447265625,\n 27.800209937418252\n ],\n [\n -96.50390625,\n 27.644606381943326\n ],\n [\n -97.55859375,\n 49.03786794532644\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"13","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c7ffafe4b0f2f0cebfc222","contributors":{"editors":[{"text":"Spall, Henry","contributorId":77933,"corporation":false,"usgs":true,"family":"Spall","given":"Henry","email":"","affiliations":[],"preferred":false,"id":647620,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":70162203,"text":"70162203 - 1981 - Shorebirds of the eastern Bering Sea","interactions":[],"lastModifiedDate":"2018-12-21T13:19:12","indexId":"70162203","displayToPublicDate":"2016-01-15T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"41","title":"Shorebirds of the eastern Bering Sea","docAbstract":"Largely on the basis of work conducted in western Alaska since 1975, we present an overview of the shorebird resources of the region and discuss their relationship to the littoral and supralittoral habitats of the area. Thirty species of shorebirds occur regularly and comprise an important component of the eastern Bering Sea ecosystem. For a third of these species the region supports the main Alaska population-for several species, the main North American population. In winter and spring littoral areas are generally ice-fast and little used by shorebirds. After breeding, there is a pronounced movement of shorebirds to coastal areas throughout the region. Populations regularly swell into the millions, many relying entirely on littoral habitats while undergoing molt and premigratory fat deposition. The extensive intertidal of the Yukon Delta and lagoons of the Alaska Peninsula are used by more species, in greater numbers, and for longer periods than other areas within the region. The timing of fall migration shows considerable variation by area, species, and age. The susceptibility of the most common shorebird species to disturbances from petroleum development is discussed.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Eastern Bering Sea Shelf: Oceanography and Resources","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"U.S. Deptartment of Commerce, National Oceanic and Atmospheric Administration, Office of Marine Pollution Assessment","publisherLocation":"Seattle, WA","doi":"10.5962/bhl.title.61718","usgsCitation":"Calder, J., and Hood, D.W., 1981, Shorebirds of the eastern Bering Sea, chap. 41 of The Eastern Bering Sea Shelf: Oceanography and Resources, p. 719-738, https://doi.org/10.5962/bhl.title.61718.","productDescription":"20 p.","startPage":"719","endPage":"738","numberOfPages":"20","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":480278,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.biodiversitylibrary.org/item/125430","text":"External Repository"},{"id":314427,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Eastern Bearing Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -186.15234374999997,\n 52.32191088594773\n ],\n [\n -186.15234374999997,\n 67.87554134672945\n ],\n [\n -150.205078125,\n 67.87554134672945\n ],\n [\n -150.205078125,\n 52.32191088594773\n ],\n [\n -186.15234374999997,\n 52.32191088594773\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569a182de4b0ec051295ef9d","contributors":{"authors":[{"text":"Calder, J.A.","contributorId":152283,"corporation":false,"usgs":false,"family":"Calder","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":646081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hood, Donald W.","contributorId":111881,"corporation":false,"usgs":false,"family":"Hood","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":646082,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70038303,"text":"70038303 - 1981 - Water resources inventory of Connecticut Part 7: upper Connecticut River basin","interactions":[],"lastModifiedDate":"2014-06-27T14:07:44","indexId":"70038303","displayToPublicDate":"2012-04-29T10:03:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"24","title":"Water resources inventory of Connecticut Part 7: upper Connecticut River basin","docAbstract":"The 508 square miles of the upper Connecticut River basin in north-central Connecticut include the basins of four major tributaries: the Scantic, Park, and Hockanum Rivers, and the Farmington River downstream from Tariffville. Precipitation over this area averaged 44 inches per year during 1931-60. In this period, an additional 3,800 billion gallons of water per year entered the basin in the main stem of the Connecticut River at the Massachusetts state line, about 230 billion gallons per year in the Farmington River at Tariffville, and about 10 billion gallons per year in the Seantic River at the Massachusetts state line. Some water was also imported from outside the basin by water-supply systems. About half the precipitation, 22.2 inches, was lost from the basin by evapotranspiration; the remainder flowed out of the study area in the Connecticut River at Portland.
\nVariations in streamflow at 41 long-term continuous-record gaging stations are summarized in standardized graphs and tables that can be used to estimate streamflow characteristics at other sites. For example, mean-flow and two low-flow characteristics: (1) the 7-day annual minimum flow for 2-year and (2) 10-year recurrence intervals, have been determined for many partial-record stations throughout the basin.
\nOf the 30 principal lakes, ponds, and reservoirs, two have usable storage capacities of more than 1 billion gallons. The maximum safe draft rate (regulated flow) of the largest of these, Shenipsit Lake at Rockville, is 6.5 million gallons per day for the 2-year and 30-year recurrence intervals (median and lowest annual flow).
\nFloods have occurred within each month of the year but in different years. The greatest known flood on the Connecticut River was in March 1936; it had a peak flow of 130,000 cubic feet per second at Hartford. Since then, major floods have been reduced by flood-control measures.
\nThe major aquifers underlying the basin are composed of unconsolidated materials (stratified drift and till) and bedrock. Stratified drift overlies till and bedrock in valleys and lowlands in the eastern and western parts and in most of the broad central valley. The stratified drift generally ranges in thickness from 10 feet in small valleys to more than 200 feet in the Connecticut River Valley. Bedrock underlies the entire basin and is composed of (1) interbedded sedimentary and igneous rocks and (2) crystalline rocks.
\nGround-water sources yield from several million gallons per day from large well fields to 1 gallon per minute from single wells. Yields of 100 gal/min or more are most commonly obtained from screened wells tapping stratified-drift aquifers; amounts can be calculated by use of a series of graphs in conjunction with estimates of aquifer transmissivity and thickness. Eighteen areas underlain by good aquifers are selected as the most favorable locations for large-scale development of ground water. Selection of these areas is based on estimates of aquifer characteristics and the amount of water potentially available from induced infiltration of streamflow at low-flow conditions.
\nSmall to moderate water supplies can generally be obtained from any of the aquifers. Wells in bedrock yield at least a few gallons per minute at most sites. The probability of obtaining an adequate yield for domestic supply is greater in sedimentary than in crystalline bedrock and is also greater in stratified-drift overburden than in till.
\nWhere unaffected by man's activities, the water is of the calcium magnesium bicarbonate type, is generally low to moderate in dissolved-solids concentration, and ranges from soft to hard. In general, streamflow is less mineralized than ground water, particularly when it consists largely of direct runoff. However, streams become more highly mineralized during low-flow conditions, when most flow consists of more highly mineralized water discharged from aquifers. The median dissolved-solids concentration in water from 25 stream sites was 113 mg/L (milligrams per liter) during high flow, and 148 mg/L during low flow within the study period. Iron and manganese occur naturally in objectionable concentrations in some streams draining swamps and in some waters draining from sedimentary bedrock which contains iron- and manganese-bearing minerals.
\nMan's activities have affected the water quality of streams in much of the area, particularly in the Hockanum and Park River basins. The degradation in quality in these streams is shown by wide and erratic changes in dissolved-solids concentration, excessive amounts of trace elements, a low dissolved-oxygen content, and abnormally high temperatures. Ground water within this area is degraded principally by induced infiltration of surface water that contains chemical wastes, by leachate from wastes stored or disposed of on the ground, and by effluents discharged from septic tanks.
\nThe quantity and quality of water are satisfactory for a wide variety of uses, and, with suitable treatment, the water may be used for most purposes. The total amount of water used in 1968 was more than 100 billion gallons. About 80 percent of this was used for industrial purposes, and 90 percent of the industrial water was obtained from surface-water sources. About 85 percent of the population was supplied with water for domestic use by 15 major public and municipal systems and 25 private associations. Analyses of water from the 13 largest systems show generally good quality.
","language":"English","publisher":"Connecticut Department of Environmental Protection","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Ryder, R.B., Thomas, M.P., and Weiss, L.A., 1981, Water resources inventory of Connecticut Part 7: upper Connecticut River basin: Connecticut Water Resources Bulletin 24, Report: vii, 76 p.; 4 Plates: 37.33 x 50.45 inches and smaller.","productDescription":"Report: vii, 76 p.; 4 Plates: 37.33 x 50.45 inches and smaller","numberOfPages":"83","costCenters":[],"links":[{"id":258813,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0024/report.pdf","size":"17112","linkFileType":{"id":1,"text":"pdf"}},{"id":258814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0024/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Connecticut River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.833333,41.533333 ], [ -72.833333,42.058333 ], [ -72.366667,42.058333 ], [ -72.366667,41.533333 ], [ -72.833333,41.533333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc907e4b08c986b32cc15","contributors":{"authors":[{"text":"Ryder, Robert B. rryder@usgs.gov","contributorId":68294,"corporation":false,"usgs":true,"family":"Ryder","given":"Robert","email":"rryder@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":463828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463830,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiss, Lawrence A.","contributorId":102528,"corporation":false,"usgs":true,"family":"Weiss","given":"Lawrence","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463829,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5221635,"text":"5221635 - 1981 - Eustrongylides and pesticide levels in a great blue heron shot in Wisconsin","interactions":[],"lastModifiedDate":"2022-11-03T16:39:56.804404","indexId":"5221635","displayToPublicDate":"2010-06-16T12:19:18","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3111,"text":"Prairie Naturalist","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Eustrongylides and pesticide levels in a great blue heron shot in Wisconsin","title":"Eustrongylides and pesticide levels in a great blue heron shot in Wisconsin","docAbstract":"The parasitic roundworm, Eustrongylides ignotus Jagersk, has been known to cause mortality and morbidity in members of the heron family in the eastern states of North America. To date no previous records exist for this nematode in Wisconsin. Even though eustrongylidiosis was first detected in the District of Columbia in 1926 by Chapin (1926), it was not until 1976 that this parasite was found in the midwest, in central Indiana (Winterfield and Kazacos 1977). The purpose of this report is to document the occurrence of this nematode even further westward in Wisconsin, and to show the debilitating effect it can have on herons.
","language":"English","publisher":"Great Plains Natural Science Society","usgsCitation":"Windingstad, R.M., and Swineford, D.M., 1981, Eustrongylides and pesticide levels in a great blue heron shot in Wisconsin: Prairie Naturalist, v. 13, no. 2, p. 161-162.","productDescription":"2 p.","startPage":"161","endPage":"162","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":409097,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://digitalcommons.unl.edu/tpn/"}],"country":"United States","state":"Wisconsin","county":"Oneida County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.0477,45.8953],[-89.047,45.8097],[-89.0469,45.7265],[-89.0475,45.6391],[-89.0468,45.5518],[-89.0467,45.4668],[-89.174,45.4681],[-89.3013,45.4692],[-89.4274,45.4707],[-89.4286,45.5553],[-89.5489,45.5562],[-89.6725,45.5556],[-89.7961,45.5559],[-89.9197,45.5551],[-90.0433,45.5551],[-90.0434,45.6443],[-90.0434,45.7302],[-90.0448,45.8176],[-90.0428,45.8972],[-89.9846,45.8974],[-89.9212,45.8981],[-89.8199,45.8984],[-89.797,45.898],[-89.7571,45.8985],[-89.6741,45.8987],[-89.5498,45.8988],[-89.4256,45.8987],[-89.3628,45.8987],[-89.3007,45.9014],[-89.3008,45.8606],[-89.1754,45.859],[-89.1752,45.8993],[-89.1091,45.8973],[-89.0477,45.8953]]]},\"properties\":{\"name\":\"Oneida\",\"state\":\"WI\"}}]}","volume":"13","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fb126","contributors":{"authors":[{"text":"Windingstad, R. M.","contributorId":71124,"corporation":false,"usgs":true,"family":"Windingstad","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":334325,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swineford, D. M.","contributorId":106839,"corporation":false,"usgs":true,"family":"Swineford","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":334326,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011738,"text":"70011738 - 1981 - Canyon Creek: A late Pleistocene vertebrate locality in interior Alaska","interactions":[],"lastModifiedDate":"2025-07-10T16:29:25.653401","indexId":"70011738","displayToPublicDate":"2004-11-19T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Canyon Creek: A late Pleistocene vertebrate locality in interior Alaska","docAbstract":"The Canyon Creek vertebrate-fossil locality is an extensive road cut near Fairbanks that exposes sediments that range in age from early Wisconsin to late Holocene. Tanana River gravel at the base of the section evidently formed during the Delta Glaciation of the north-central Alaska Range. Younger layers and lenses of fluvial sand are interbedded with arkosic gravel from Canyon Creek that contains tephra as well as fossil bones of an interstadial fauna about 40,000 years old. Solifluction deposits containing ventifacts, wedge casts, and rodent burrows formed during a subsequent period of periglacial activity that took place during the maximum phase of Donnelly Glaciation about 25,000–17,000 years ago. Overlying sheets of eolian sand are separated by a 9500-year-old paleosol that may correlate with a phase of early Holocene spruce expansion through central Alaska. The Pleistocene fauna from Canyon Creek consists of rodents (indicated by burrows), Mammuthus primigenius (woolly mammoth), Equus lambei (Yukon wild ass), Camelops hesternus (western camel), Bison sp. cf. B. crassicornis (large-horned bison), Ovis sp. cf.O. dalli (mountain sheep), Canis sp. cf. C. lupus (wolf), Lepus sp. cf. L. othus or L. arcticus (tundra hare), and Rangifer sp. (caribou). This assemblage suggests an open landscape in which trees and tall shrubs were either absent or confined to sheltered and moist sites. Camelops evidently was present in eastern Beringia during the middle Wisconsin interstadial interval but may have disappeared during the following glacial episode. The stratigraphic section at Canyon Creek appears to demonstrate that the Delta Glaciation of the north-central Alaska Range is at least in part of early Wisconsin age and was separated from the succeeding Donnelly Glaciation by an interstadial rather than interglacial episode.
","language":"English","publisher":"Elsevier","doi":"10.1016/0033-5894(81)90043-0","issn":"00335894","usgsCitation":"Weber, F.R., Hamilton, T.D., Hopkins, D., Repenning, C., and Haas, H., 1981, Canyon Creek: A late Pleistocene vertebrate locality in interior Alaska: Quaternary Research, v. 16, no. 2, p. 167-180, https://doi.org/10.1016/0033-5894(81)90043-0.","productDescription":"14 p.","startPage":"167","endPage":"180","costCenters":[],"links":[{"id":220787,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"north-central Alaska Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -150.32186007264718,\n 65.94098893598314\n ],\n [\n -150.32186007264718,\n 64.33338352969466\n ],\n [\n -145.35284620275706,\n 64.33338352969466\n ],\n [\n -145.35284620275706,\n 65.94098893598314\n ],\n [\n -150.32186007264718,\n 65.94098893598314\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"16","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059f347e4b0c8380cd4b6eb","contributors":{"authors":[{"text":"Weber, F. R.","contributorId":105303,"corporation":false,"usgs":true,"family":"Weber","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":361847,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamilton, T. D.","contributorId":36921,"corporation":false,"usgs":true,"family":"Hamilton","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":361844,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hopkins, D.M.","contributorId":103646,"corporation":false,"usgs":true,"family":"Hopkins","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":361846,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Repenning, C.A.","contributorId":56700,"corporation":false,"usgs":true,"family":"Repenning","given":"C.A.","affiliations":[],"preferred":false,"id":361845,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Haas, H.","contributorId":27192,"corporation":false,"usgs":true,"family":"Haas","given":"H.","email":"","affiliations":[],"preferred":false,"id":361843,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70011989,"text":"70011989 - 1981 - Contemporary doming of the Adirondack Mountains: Further evidence from releveling","interactions":[],"lastModifiedDate":"2025-08-28T16:33:24.753325","indexId":"70011989","displayToPublicDate":"2003-04-08T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Contemporary doming of the Adirondack Mountains: Further evidence from releveling","docAbstract":"The Adirondack Mountains constitute an anomalously large, domical uplift on the Appalachian foreland. The dome has a NNE—SSW axis about 190 km long, and an east—west dimension of about 140 km. It has a structural relief of at least 1600 m, and a local topographic relief of up to 1200 m. First-order leveling in 1955, and again in 1973 along a north—south line at the eastern margin of the Adirondack shows an uplift rate of 2.2 mm/yr at the latitude of the center of the dome and a subsidence rate of 2.8 mm/yr at the northern end of the line near the Canadian border. The net amount of arching along this releveled line is 9 cm ± 2 cm (Isachsen, 1975). To test the idea that this arching represented an “edge effect” of contemporary doming of the Adirondacks as a whole, the National Geodetic Survey was encouraged to relevel a 1931 north—south line between Utica and Fort Covington (near the Canadian border) which crosses the center of the dome. The releveling showed that the mountain mass is undergoing contemporary domical uplift at a rate which reaches 3.7 mm/yr near the center of the dome (compare with 1 mm/yr for the Swiss Alps). Three other releveled lines in the area support this conclusion.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(81)90051-2","issn":"00401951","usgsCitation":"Isachsen, Y., 1981, Contemporary doming of the Adirondack Mountains: Further evidence from releveling: Tectonophysics, v. 71, no. 1-4, p. 95-96, https://doi.org/10.1016/0040-1951(81)90051-2.","productDescription":"2 p.","startPage":"95","endPage":"96","costCenters":[],"links":[{"id":220732,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Adirondack Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -75.08632613930284,\n 44.849722542694394\n ],\n [\n -75.68357029846126,\n 44.12534350539521\n ],\n [\n -75.11834401539436,\n 43.137593153404055\n ],\n [\n -73.6455352174284,\n 43.04799214874441\n ],\n [\n -73.31377725183206,\n 44.32023495222312\n ],\n [\n -73.6455352174284,\n 44.89509467289085\n ],\n [\n -75.08632613930284,\n 44.849722542694394\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"71","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fa4ce4b0c8380cd4da21","contributors":{"authors":[{"text":"Isachsen, Y.W.","contributorId":100528,"corporation":false,"usgs":true,"family":"Isachsen","given":"Y.W.","affiliations":[],"preferred":false,"id":362460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68748,"text":"oc113 - 1981 - Stratigraphic sections of Middle Jurassic Entrada Sandstone and related rocks from Salt Valley to Dewey Bridge in east-central Utah","interactions":[],"lastModifiedDate":"2019-12-26T07:46:24","indexId":"oc113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"113","title":"Stratigraphic sections of Middle Jurassic Entrada Sandstone and related rocks from Salt Valley to Dewey Bridge in east-central Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/oc113","usgsCitation":"O'Sullivan, R., 1981, Stratigraphic sections of Middle Jurassic Entrada Sandstone and related rocks from Salt Valley to Dewey Bridge in east-central Utah: U.S. Geological Survey Oil and Gas Investigation Chart 113, HTML, https://doi.org/10.3133/oc113.","productDescription":"HTML","costCenters":[],"links":[{"id":188260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":104771,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5139.htm","linkFileType":{"id":5,"text":"html"},"description":"5139"}],"scale":"5000","country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae694","contributors":{"authors":[{"text":"O'Sullivan, Robert Brett","contributorId":26695,"corporation":false,"usgs":true,"family":"O'Sullivan","given":"Robert Brett","affiliations":[],"preferred":false,"id":278870,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61158,"text":"mf1271B - 1981 - Oil and gas resources of the Cheat Mountain Further Planning Area (RARE II), Randolph County, West Virginia","interactions":[],"lastModifiedDate":"2016-08-23T10:09:28","indexId":"mf1271B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1271","chapter":"B","title":"Oil and gas resources of the Cheat Mountain Further Planning Area (RARE II), Randolph County, West Virginia","docAbstract":"The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and be submitted to the President and the Congress. This map presents an analysis of the oil and gas resources of the Cheat Mountain Further Planning Area in the Monongahela National Forest, Randolph County, West Virginia. The area was classified as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.
\nCheat Mountain Further Planning Area comprises about 7,720 acres in the Monongahela National Forest in east-central West Virginia, southeast of Elkins. The study area lies on a northeast-trending linear ridge bordered on the west by the Right Fork of Tygart River and on the east by Shavers Fork. It averages about 2 mi in length and 1½ mi in width. Altitudes on Cheat Mountain range from about 2,550 to 3,900 ft.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1271B","usgsCitation":"Weed, E.G., 1981, Oil and gas resources of the Cheat Mountain Further Planning Area (RARE II), Randolph County, West Virginia: U.S. Geological Survey Miscellaneous Field Studies Map 1271, 32.75 x 42.23 inches, https://doi.org/10.3133/mf1271B.","productDescription":"32.75 x 42.23 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1271B.PNG"},{"id":327558,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1271-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"West Virginia","county":"Randolph County","otherGeospatial":"Monongahela National Forest","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80,38.25 ], [ -80,39.25 ], [ -79.25,39.25 ], [ -79.25,38.25 ], [ -80,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d74","contributors":{"authors":[{"text":"Weed, E. G.","contributorId":55267,"corporation":false,"usgs":true,"family":"Weed","given":"E.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":265093,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46165,"text":"ofr81804 - 1981 - Maps showing ground-water conditions in the Agua Fria area, Yavapai and Maricopa Counties, Arizona","interactions":[],"lastModifiedDate":"2022-04-20T22:41:44.364897","indexId":"ofr81804","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-804","title":"Maps showing ground-water conditions in the Agua Fria area, Yavapai and Maricopa Counties, Arizona","docAbstract":"The Aqua Fria area includes about 1,500 mi2 in central Arizona. The area is bounded by the Prescott National Forest on the west, north, and east; by the Tonto National Forest on the southeast; and by the Bradshaw Mountains and Lake Pleasant on the southwest. Ground-water development has been slight, and in 1978 about 3,200 acre-ft of groundwater was withdrawn; of this, about 2,200 acres-ft was used for irrigation, 600 acre-ft for public supply, and 400 acre-ft for domestic and stock supplies. Public-supply use has increased nearly 30 percent (data in files of Arizona Corporation Commission Phoenix, Ariz.) Many small-capacity wells have been drilled in the area, and only selected areas are shown on the maps in areas of high well density.
The U.S. Geological Survey (USGS) made a reconnaissance geochemical survey of the Shining Rock Wilderness (fig. 1) to test for unidentified or unexposed mineral deposits that might be recognized by their geochemical halos. Similar geochemical survey based on trace-element analyses have been credited with the discovery of many types of mineral deposits (Hawkes and Webb, 1962). Although no metallic mineral deposits are known in the study area, the same sequence of rocks that is exposed there contains small deposits of copper-bearing sulfides 10-18 mi (16-28 km) west and southwest of the wilderness (Gair and Slack, 1979). Keith (1907, p. 8) reports minor amounts of copper sulfides and iron sulfides in schist and in quartz veins cutting schist near Retreat, 4 mi (6.5 km) northwest of the wilderness. An old gold mine, the Boylston mine, on Forge Mountain 10 mi (16 km) east of the wilderness (Nitze and Hanna, 1896, p. 181-191) is in metasedimentary rocks of the Great Smoky Group (Hadley and Nelson, 1971) which are probably younger than the rocks exposed in the wilderness.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1290B","usgsCitation":"Lesure, F.G., 1981, Geochemical survey of Shining Rock Wilderness, Heywood County, North Carolina: U.S. Geological Survey Miscellaneous Field Studies Map 1290, 42.00 x 55.52 inches, https://doi.org/10.3133/mf1290B.","productDescription":"42.00 x 55.52 inches","costCenters":[],"links":[{"id":358787,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1290-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180348,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1290-B/report-thumb.jpg"}],"scale":"0","country":"United States","state":"North Carolina","county":"Haywood County","otherGeospatial":"Shining Rock Wilderness","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.91666666666667,\n 35.333333333333336\n ],\n [\n -82.91666666666667,\n 35.416666666666664\n ],\n [\n -82.78416666666666,\n 35.416666666666664\n ],\n [\n -82.78416666666666,\n 35.333333333333336\n ],\n [\n -82.91666666666667,\n 35.333333333333336\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abb31","contributors":{"authors":[{"text":"Lesure, Frank G.","contributorId":20068,"corporation":false,"usgs":true,"family":"Lesure","given":"Frank","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":262999,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56286,"text":"wdrWA812 - 1981 - Water resources data, Washington, water year 1981: Vol. 2 - Eastern Washington","interactions":[],"lastModifiedDate":"2022-12-14T00:49:08.926242","indexId":"wdrWA812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"WA-81-2","title":"Water resources data, Washington, water year 1981: Vol. 2 - Eastern Washington","docAbstract":"Water-resources data for the 1981 water year for Washington 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 quality of ground-water. This report, in two volumes, contains records for water discharge at 229 gaging stations; stage only at 5 gaging stations; stage and contents at 39 lakes and reservoirs; water quality at 39 gaging stations (including 6 lakes and reservoirs) and 100 wells; and water levels at 164 observation wells. Also included are data for 14 crest-stage and 28 water-quality partial-record stations. Locations of sites in this volume are on figures 4, 5, 6, and 22. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data represent that part of the national Water Data system operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in Washington.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA812","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Water resources data, Washington, water year 1981: Vol. 2 - Eastern Washington: U.S. Geological Survey Water Data Report WA-81-2, x, 276 p., https://doi.org/10.3133/wdrWA812.","productDescription":"x, 276 p.","costCenters":[],"links":[{"id":174739,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/wa-81-2/report-thumb.jpg"},{"id":410428,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/wa-81-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0ad2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532477,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61399,"text":"mf1195 - 1981 - Map showing vegetation distribution in the central part of the East Tintic Mountains, Utah","interactions":[],"lastModifiedDate":"2016-08-23T10:31:33","indexId":"mf1195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1195","title":"Map showing vegetation distribution in the central part of the East Tintic Mountains, Utah","docAbstract":"With the development of remote sensing technology has come the capability of defining and mapping plant communities by means of their spectral properties. Such maps will be an important aid in resource evaluation and management, especially in densely vegetated and remote areas of the world.
\nThis study in part of a broader program to determine the usefulness of multispectral scanner aircraft and satellite images for mapping lithologic units and vegetation communities (Rowan and others, 1974; 1977; Abrams and others, 1997; Rowan and Abrams, 1978a; 1978b; Kahle and Rowan, 1979, written commun.).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1195","usgsCitation":"Milton, N., and Madura, D.P., 1981, Map showing vegetation distribution in the central part of the East Tintic Mountains, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1195, 34.68 x 25.43 inches, https://doi.org/10.3133/mf1195.","productDescription":"34.68 x 25.43 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1195.PNG"},{"id":327594,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1195/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Utah","otherGeospatial":"Eastern Tintic Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.11749999999999,39 ], [ -112.11749999999999,40 ], [ -112,40 ], [ -112,39 ], [ -112.11749999999999,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ce4b07f02db69e473","contributors":{"authors":[{"text":"Milton, Nancy","contributorId":85188,"corporation":false,"usgs":true,"family":"Milton","given":"Nancy","affiliations":[],"preferred":false,"id":265580,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Madura, Daryl P.","contributorId":173056,"corporation":false,"usgs":false,"family":"Madura","given":"Daryl","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":265579,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":59612,"text":"mf1214C - 1981 - Map showing aeromagnetic interpretation of the Baker-Cypress BLM Instant Study Area and Timbered Crater Forest Service Further Planning Areas, Modoc, Shasta, and Siskiyou counties, California","interactions":[],"lastModifiedDate":"2018-12-06T14:40:41","indexId":"mf1214C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1214","chapter":"C","title":"Map showing aeromagnetic interpretation of the Baker-Cypress BLM Instant Study Area and Timbered Crater Forest Service Further Planning Areas, Modoc, Shasta, and Siskiyou counties, California","docAbstract":"The data for the aeromagnetic map of the Baker-Cypress and Timbered crater areas were collected in 1978 and compiled at a scale of 1 :62,500 (U,S, Geological Survey, 1979). East-west traverses were spaced at 0.8-km intervals at a constant altitude of 1370 m (4500 ft) above sea level, Contour interval is 20 and 100 gammas, depending upon the steepness of local gradients in the Earth's magnetic field. A regional magnetic field (the International Geomagnetic Reference Field - 1975, updated to the month flown) of approximately 5-6 gammas/km was removed from the data be fore con touring.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1214C","usgsCitation":"Griscom, A., 1981, Map showing aeromagnetic interpretation of the Baker-Cypress BLM Instant Study Area and Timbered Crater Forest Service Further Planning Areas, Modoc, Shasta, and Siskiyou counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 1214, 29.11 x 23.46 inches, https://doi.org/10.3133/mf1214C.","productDescription":"29.11 x 23.46 inches","costCenters":[],"links":[{"id":359992,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1214-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1214-C/report-thumb.jpg"}],"scale":"0","country":"United States","state":"California","county":"Modoc County, Shasta County, Siskiyou County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.58333333333333,41.083333333333336 ], [ -121.58333333333333,41.25 ], [ -121.33333333333333,41.25 ], [ -121.33333333333333,41.083333333333336 ], [ -121.58333333333333,41.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655511","contributors":{"authors":[{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":262319,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":58926,"text":"mf1271C - 1981 - Maps showing mines, quarries, prospects, and exposures in the Cheat Mountain Roadless Area, Randolph County, West Virginia","interactions":[],"lastModifiedDate":"2016-08-22T09:46:36","indexId":"mf1271C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1271","chapter":"C","title":"Maps showing mines, quarries, prospects, and exposures in the Cheat Mountain Roadless Area, Randolph County, West Virginia","docAbstract":"The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and be submitted to the President and the Congress. This report presents the results of a mineral survey of the Cheat Mountain Roadless Area in the Monongahela National Forest, Randolph County, West Virginia. The area was designated as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.
\nThe Cheat Mountain Roadless Area is in the Greenbrier Ranger District of the Monongahela National Forest, east-central West Virginia. It is located in Randolph County about 10 mi southeast of Elkins, W.Va., and is accessible there via U.S. 219-250 to Beverly, W.Va., and then southeastward along an improved country road. From the east, the study area can be reached via U.S. 33 and by a paved country road that extends from Alpena, W.Va. to the village of Bemis. Unimproved Forest service roads, abandoned logging railroad grades, and primitive trails provide access by foot or horseback into the interior of the study area.
\nPhysiographically, the Cheat Mountain Roadless Area is in the Allegheny Mountain section of the Appalachian Plateaus province and is situated at the eastern edge of the Appalachian coal region. Cheat Mountain, a northeast-trending ridge, is bordered on the west by the right fork of Files Creek and on the east by Shavers Fork and its tributaries. Most of the area occupies an elevated plateau capped by resistant sandstone and conglomerate. Altitudes range form 2,320 ft on Lime Kiln Run to more than 3,900 ft on Cheat Mountain. The topography ranges from relatively flat in the uplands to very steep in the canyons along tributaries of Shavers Fork. The area is heavily forested with vegetation varying from mixed hardwoods on the western slope of Cheat Mountain to thickets of conifers in the uplands. Hemlocks are sparsely interspersed and red spruce, the dominant tree at higher elevations prior to logging in the mid 1920's, is again reforesting upland areas. Rhododendron and laurel flourish in moist protected areas along drainage courses and in coves.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1271C","usgsCitation":"Behum, P.T., and Hammack, R.W., 1981, Maps showing mines, quarries, prospects, and exposures in the Cheat Mountain Roadless Area, Randolph County, West Virginia: U.S. Geological Survey Miscellaneous Field Studies Map 1271, 32.93 x 39.62 inches, https://doi.org/10.3133/mf1271C.","productDescription":"32.93 x 39.62 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183725,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1271C.PNG"},{"id":327160,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1271-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"West Virginia","county":"Randolph County","otherGeospatial":"Cheat Mountain Roadless Area, Monongahela National Forest","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.86749999999999,38.700833333333335 ], [ -79.86749999999999,38.8675 ], [ -79.70083333333334,38.8675 ], [ -79.70083333333334,38.700833333333335 ], [ -79.86749999999999,38.700833333333335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605ce1","contributors":{"authors":[{"text":"Behum, Paul T.","contributorId":86894,"corporation":false,"usgs":true,"family":"Behum","given":"Paul","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":261107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hammack, Richard W.","contributorId":150019,"corporation":false,"usgs":false,"family":"Hammack","given":"Richard","email":"","middleInitial":"W.","affiliations":[{"id":17887,"text":"National Energy Technology Laboratory, Department of Energy","active":true,"usgs":false}],"preferred":false,"id":261106,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":48721,"text":"ofr81458 - 1981 - Equal-area base map of the Bering Sea, plate 4: Aleutian east","interactions":[],"lastModifiedDate":"2021-10-22T16:32:10.686685","indexId":"ofr81458","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-458","title":"Equal-area base map of the Bering Sea, plate 4: Aleutian east","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81458","usgsCitation":"Jones, D., and Swenson, P.A., 1981, Equal-area base map of the Bering Sea, plate 4: Aleutian east: U.S. Geological Survey Open-File Report 81-458, 1 Plate: 40.44 × 34.36 inches, https://doi.org/10.3133/ofr81458.","productDescription":"1 Plate: 40.44 × 34.36 inches","costCenters":[],"links":[{"id":170308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":108152,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12046.htm","linkFileType":{"id":5,"text":"html"},"description":"12046"},{"id":85528,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0458/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -176,\n 52\n ],\n [\n -164,\n 52\n ],\n [\n -164,\n 58\n ],\n [\n -176,\n 58\n ],\n [\n -176,\n 52\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe34d","contributors":{"authors":[{"text":"Jones, D.R.","contributorId":80670,"corporation":false,"usgs":true,"family":"Jones","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":238111,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swenson, P. A.","contributorId":38632,"corporation":false,"usgs":true,"family":"Swenson","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":238110,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68690,"text":"ha650 - 1981 - Geologic structure, hydrology, and water quality of the Laramie-Fox Hills aquifer in the Denver basin, Colorado","interactions":[],"lastModifiedDate":"2022-08-25T20:15:42.86453","indexId":"ha650","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"650","title":"Geologic structure, hydrology, and water quality of the Laramie-Fox Hills aquifer in the Denver basin, Colorado","docAbstract":"The Denver ground-water basin underlies a 6,700-square-mile area extending from Greeley in the north to Colorado Springs in the south, and from the Front Range in the west to near Limon in the east. The four major bedrock aquifers that occur in the basin are the Laramie-Fox Hills aquifer (the deepest aquifer), the Arapahoe aquifer, the Denver aquifer, and the Dawson aquifer (the uppermost aquifer). The Laramie-Fox Hills aquifer, which is the subject of this report, underlies the entire area of the basin in east-central Colorado (index map, fig. 1) and is an important source of water for residents in the northern Denver suburban area and in the rural areas of eastern Jefferson, Arapahoe, and Elbert Counties, Adams County, and southern Weld and El Paso Counties. About 90 percent of the estimated 1,700 wells completed in the aquifer supply water to residents and livestock. The remaining wells supply water for commercial and industrial use and limited irrigation of commercial crops.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha650","usgsCitation":"Robson, S.G., 1981, Geologic structure, hydrology, and water quality of the Laramie-Fox Hills aquifer in the Denver basin, Colorado: U.S. Geological Survey Hydrologic Atlas 650, 3 Plates: 34.74 x 40.63 inches or smaller, https://doi.org/10.3133/ha650.","productDescription":"3 Plates: 34.74 x 40.63 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":90408,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/650/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405625,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16050.htm","linkFileType":{"id":5,"text":"html"}},{"id":187920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90409,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/650/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90410,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/650/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Colorado","otherGeospatial":"Denver basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.257,\n 38.661\n ],\n [\n -103.603,\n 38.661\n ],\n [\n -103.603,\n 40.425\n ],\n [\n -105.257,\n 40.425\n ],\n [\n -105.257,\n 38.661\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688117","contributors":{"authors":[{"text":"Robson, Stanley G.","contributorId":73187,"corporation":false,"usgs":true,"family":"Robson","given":"Stanley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":278754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56197,"text":"wdrNY801 - 1981 - Water resources data for New York, volume 1, eastern New York, excluding Long Island","interactions":[],"lastModifiedDate":"2020-11-23T21:04:14.619679","indexId":"wdrNY801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"NY-80-1","title":"Water resources data for New York, volume 1, eastern New York, excluding Long Island","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY801","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Water resources data for New York, volume 1, eastern New York, excluding Long Island: U.S. Geological Survey Water Data Report NY-80-1, ix, 310 p., https://doi.org/10.3133/wdrNY801.","productDescription":"ix, 310 p.","costCenters":[],"links":[{"id":380722,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1980/ny-80-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1980/ny-80-1/report-thumb.jpg"}],"country":"United States","state":"New 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York\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f248e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532445,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60711,"text":"mf1270 - 1981 - Bathymetric map of the continental slope and uppermost continental rise between Lindenkohl Canyon and South Toms Canyon, offshore Eastern United States","interactions":[],"lastModifiedDate":"2016-08-23T09:18:06","indexId":"mf1270","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1270","title":"Bathymetric map of the continental slope and uppermost continental rise between Lindenkohl Canyon and South Toms Canyon, offshore Eastern United States","docAbstract":"This map was prepared as part of a study of geologic hazards to resource exploration and development on the Continental Slope in the Baltimore Canyon Trough area, off southern New Jersey. Detailed bathymetric maps are required for enfineering studies of bottom stability and for geologic interpretation of the nature of the submarine topography. This map presents the morphology of the Continental Slope in greater detail than do other available bathymetic maps (Veatch and Smith, 1939; Uchupi, 1965, sheet 2; U.S. Coast and Geodetic Survey, 1967; Belding and Holland, 1970, sheet 1; National Ocean Survey, 1977).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1270","usgsCitation":"Robb, J.M., Kirby, J., and Hampson, J., 1981, Bathymetric map of the continental slope and uppermost continental rise between Lindenkohl Canyon and South Toms Canyon, offshore Eastern United States: U.S. Geological Survey Miscellaneous Field Studies Map 1270, 30.76 x 36.75 inches, https://doi.org/10.3133/mf1270.","productDescription":"30.76 x 36.75 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180590,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1270.PNG"},{"id":327469,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1270/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Lindenkohl Canyon, South Toms Canyon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73,\n 38.583333333333336\n ],\n [\n -73,\n 39.083333333333336\n ],\n [\n -72.28333333333335,\n 39.083333333333336\n ],\n [\n -72.28333333333335,\n 38.583333333333336\n ],\n [\n -73,\n 38.583333333333336\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640710","contributors":{"authors":[{"text":"Robb, James M.","contributorId":73272,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":264270,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirby, John R.","contributorId":91826,"corporation":false,"usgs":true,"family":"Kirby","given":"John R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":264268,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hampson, John C.","contributorId":173186,"corporation":false,"usgs":false,"family":"Hampson","given":"John C.","affiliations":[],"preferred":false,"id":264269,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":46430,"text":"ofr81333 - 1981 - Map of water table in Graham County, northwestern Kansas, March 1979","interactions":[],"lastModifiedDate":"2017-09-29T08:23:27","indexId":"ofr81333","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-333","title":"Map of water table in Graham County, northwestern Kansas, March 1979","docAbstract":"A map of the water table in Graham County, prepared in collaboration with the U.S. Bureau of Reclamation, provides current (1980) information on water levels in the unconsolidated deposits. Graham County, an area of 900 square miles in northwestern Kansas, is within the rolling, moderately to well-dissected terrain on the eastern edge of the High Plains. The eastward-flowing South Fork Solomon River separates the county into nearly equal parts.
The principal source of water for domestic, stock, municipal, and irrigation use if from wells in the shallow unconsolidated deposits. The aquifers occur chiefly in the Ogallala Formation of Miocene age and in deposits of Quaternary age.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81333","usgsCitation":"Spinazola, J.M., 1981, Map of water table in Graham County, northwestern Kansas, March 1979: U.S. Geological Survey Open-File Report 81-333, 23.85 x 20.34 inches., https://doi.org/10.3133/ofr81333.","productDescription":"23.85 x 20.34 inches.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":134661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0333/report-thumb.jpg"},{"id":346212,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0333/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kansas","county":"Graham County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-99.6019,39.5672],[-99.6024,39.4806],[-99.6035,39.3949],[-99.6039,39.3074],[-99.6044,39.2194],[-99.6054,39.1329],[-99.7027,39.1329],[-99.7157,39.1323],[-99.8142,39.1322],[-99.8279,39.132],[-99.9251,39.1323],[-99.9388,39.1326],[-100.0355,39.1324],[-100.0521,39.1326],[-100.1488,39.1318],[-100.1642,39.1321],[-100.1638,39.2187],[-100.1635,39.3062],[-100.1637,39.3927],[-100.1639,39.4793],[-100.1635,39.5673],[-100.0788,39.5675],[-100.0507,39.5674],[-99.9642,39.5671],[-99.9373,39.5669],[-99.852,39.5665],[-99.8251,39.5668],[-99.7398,39.5672],[-99.7135,39.567],[-99.6282,39.5674],[-99.6019,39.5672]]]},\"properties\":{\"name\":\"Graham\",\"state\":\"KS\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db6586b0","contributors":{"authors":[{"text":"Spinazola, Joseph M.","contributorId":102044,"corporation":false,"usgs":true,"family":"Spinazola","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":233303,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60612,"text":"mf1201B - 1981 - Aeromagnetic map of the Mokelumne Wilderness and contiguous Rare II further planning areas, central Sierra Nevada, California","interactions":[],"lastModifiedDate":"2014-04-25T06:45:57","indexId":"mf1201B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1201","chapter":"B","title":"Aeromagnetic map of the Mokelumne Wilderness and contiguous Rare II further planning areas, central Sierra Nevada, California","docAbstract":"The aeromagnetic map consists of parts of two surveys flown at an altitude of 300 m above the average ground surface. One survey (west park of the map_ centered over the Mokelumne Wilderness was flowing in a northeast-southwest direction along slight lines spaced at a horizontal interval of about 800 m (U>S> Geological Survey, 1979b). The survey to the east is part of a regional survey flown in an east-west direction along flight lines spaced at an interval of about 1,600 m (U.S. Geological Survey, 1979a). The join of the aeromagnetic contours along the border between the two surveys is generally conformable. The contour datum of the eastern regional survey, however, is about 650 nT (nanotesla) lower than the Mokelumne Wilderness survey because of difference in data reduction.
\nThe aeromagnetic pattern reflects variations of magnetization within the underlying rocks, but the pattern is complicated by strong topographic effects. That is, magnetic anomaly maxima tend to occur over ridges and hilltops and minima over canyons and depressions. The topographic effect exists mostly because a constant ground clearance could not be maintained at normal aircraft speeds in this area of rugged topographic relief. The recorded flight altitude varied from 30 m to nearly 1,500 m above the ground with local changes that approard 1,000 m in distances of less than 5,000 m.
\nFour magnetic anomalies that can be related to geologic features are discusses., Magnetic highs or lows cause by topography are not discussed.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1201B","usgsCitation":"Plouff, D., and McKee, E.H., 1981, Aeromagnetic map of the Mokelumne Wilderness and contiguous Rare II further planning areas, central Sierra Nevada, California: U.S. Geological Survey Miscellaneous Field Studies Map 1201, Map: 37.01 x 33.97 inches, https://doi.org/10.3133/mf1201B.","productDescription":"Map: 37.01 x 33.97 inches","costCenters":[],"links":[{"id":286554,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":286553,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1201-B/plate-1.pdf"}],"scale":"62500","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"California","otherGeospatial":"Sierra Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.25,38.416667 ], [ -120.25,38.75 ], [ -119.75,38.75 ], [ -119.75,38.416667 ], [ -120.25,38.416667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d73","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":264079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":264078,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":60919,"text":"mf1311 - 1981 - Structure contours and overburden on the top of the Mahogany bed, Green River Formation, eastern part of the Uinta Basin, Uintah, Duchesne, and Carbon Counties, Utah, and Rio Blanco County, Colorado","interactions":[],"lastModifiedDate":"2022-08-26T21:33:34.328288","indexId":"mf1311","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1311","title":"Structure contours and overburden on the top of the Mahogany bed, Green River Formation, eastern part of the Uinta Basin, Uintah, Duchesne, and Carbon Counties, Utah, and Rio Blanco County, Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1311","usgsCitation":"Smith, M.C., 1981, Structure contours and overburden on the top of the Mahogany bed, Green River Formation, eastern part of the Uinta Basin, Uintah, Duchesne, and Carbon Counties, Utah, and Rio Blanco County, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 1311, 1 Plate: 34.00 × 33.00 inches, https://doi.org/10.3133/mf1311.","productDescription":"1 Plate: 34.00 × 33.00 inches","costCenters":[],"links":[{"id":183705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":405734,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6938.htm","linkFileType":{"id":5,"text":"html"}},{"id":88894,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1981/1311/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","county":"Carbon County, Duchesne County, Rio Blanco County, Uintah County","otherGeospatial":"Green River Formation, Uinta Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110,\n 39.625\n ],\n [\n -109,\n 39.625\n ],\n [\n -109,\n 40.25\n ],\n [\n -110,\n 40.25\n ],\n [\n -110,\n 39.625\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d0fb","contributors":{"authors":[{"text":"Smith, M. C.","contributorId":97116,"corporation":false,"usgs":true,"family":"Smith","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":264617,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":59455,"text":"mf1348A - 1981 - Geologic map of the Beaver Creek Wilderness, McCreary County, Kentucky","interactions":[],"lastModifiedDate":"2025-09-24T16:51:26.969392","indexId":"mf1348A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1348","chapter":"A","title":"Geologic map of the Beaver Creek Wilderness, McCreary County, Kentucky","docAbstract":"The Beaver Creek Wilderness comprises approximately 4,800 acres and is principally within the cliffline bordering the Beaver Creek drainage basin in McCreary County, southeastern Kentucky. It is part of the Beaver Creek Cooperative Wildlife management Area in the Daniel Boone National Forest, which is managed by the U.S. Forest Service and the Kentucky Department of Fish and Wildlife Resources. The wilderness is about 11 mi southeast of Burnside, Ky., and is accessible from thr north and south via U.S. Route 27 and Forest Service Road 50, at its northwest border (fig. 1). From the east the area can be reached via State Route 90 and Forest Service Road 46, at the eastern end of the wilderness. The interiors is accessible by foot along an abandoned Forest Service road and by several primitive trails that extend along the major streams. The Beaver Creek Wilderness is centrally located at the western edge of the Appalachian coal regions and is within the highly dissected Cumberland Plateau section of the Appalachian Plateaus physiographic province (fig. 2). It is drained by Beaver Creek and tributaries, which flow northeastward into Cumberland Lake, a reservoir on the Cumberland River about 1 mi north of the wilderness. Altitudes range from about 730 ft on the lower part of Beaver Creek to about 1,200 ft at its headwaters.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1348A","usgsCitation":"Englund, K., and Teaford, N.K., 1981, Geologic map of the Beaver Creek Wilderness, McCreary County, Kentucky: U.S. Geological Survey Miscellaneous Field Studies Map 1348, 1 Plate: 22.98 x 30.08 inches, https://doi.org/10.3133/mf1348A.","productDescription":"1 Plate: 22.98 x 30.08 inches","costCenters":[],"links":[{"id":496034,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7005.htm","linkFileType":{"id":5,"text":"html"}},{"id":284426,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1348-A/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180325,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1348a.jpg"}],"scale":"24000","country":"United States","state":"Kentucky","county":"Mccreary County","otherGeospatial":"Beaver Creek Wilderness","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.5,\n 36.95\n ],\n [\n -84.5,\n 36.833\n ],\n [\n -84.375,\n 36.833\n ],\n [\n -84.375,\n 36.95\n ],\n [\n -84.5,\n 36.95\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5c1ae4b0b290850fa4fa","contributors":{"authors":[{"text":"Englund, Kenneth J.","contributorId":105371,"corporation":false,"usgs":true,"family":"Englund","given":"Kenneth J.","affiliations":[],"preferred":false,"id":262040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Teaford, Nancy K.","contributorId":73919,"corporation":false,"usgs":true,"family":"Teaford","given":"Nancy","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":262039,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":48530,"text":"ofr80965 - 1981 - Potentiometric-surface map for the Cretaceous aquifer, Virginia coastal plain, 1978","interactions":[],"lastModifiedDate":"2021-09-24T14:37:57.637933","indexId":"ofr80965","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-965","title":"Potentiometric-surface map for the Cretaceous aquifer, Virginia coastal plain, 1978","docAbstract":"The Atlantic Coastal Plain of Virginia includes 9,600 square miles--all or part of 40 counties east of the Fall Line. The undifferentiated Cretaceous sediments underlying this area are the most productive and extensive source of ground water, from which large withdrawals have been made over the past 40 years. In 1978, withdrawals exceeded 100 million gallons per day. To determine the effect of continued withdrawals, annual synoptic water levels for 1978 were used to prepare a map showing the approximate configuration of the potentiometric surface. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80965","usgsCitation":"Hopkins, H.T., Bower, R.F., Abe, J.M., and Harsh, J.F., 1981, Potentiometric-surface map for the Cretaceous aquifer, Virginia coastal plain, 1978: U.S. Geological Survey Open-File Report 80-965, 1 Plate: 36.60 × 26.36 inches, https://doi.org/10.3133/ofr80965.","productDescription":"1 Plate: 36.60 × 26.36 inches","costCenters":[],"links":[{"id":161673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":389717,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75436.htm"},{"id":85347,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0965/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Virginia","otherGeospatial":"Cretaceous aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.83,\n 36.55\n ],\n [\n -76,\n 36.55\n ],\n [\n -76,\n 38.75\n ],\n [\n -77.83,\n 38.75\n ],\n [\n -77.83,\n 36.55\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683186","contributors":{"authors":[{"text":"Hopkins, Herbert T.","contributorId":59423,"corporation":false,"usgs":true,"family":"Hopkins","given":"Herbert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":237686,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bower, R. F.","contributorId":96736,"corporation":false,"usgs":true,"family":"Bower","given":"R.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":237688,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Abe, J. M.","contributorId":18420,"corporation":false,"usgs":true,"family":"Abe","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":237685,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harsh, J. F.","contributorId":77535,"corporation":false,"usgs":true,"family":"Harsh","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":237687,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":50766,"text":"ofr811004 - 1981 - Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980","interactions":[],"lastModifiedDate":"2017-12-06T14:00:43","indexId":"ofr811004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1004","title":"Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980","docAbstract":"The High Plains aquifer in Kansas is part of a regional system that extends into Colorado, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming. The aquifer in Kansas underlies an area of 31,000 square miles in the western and south-central part of the State. This aquifer is a hydraulically connected assemblage of unconsolidated water-bearing deposits. In western Kansas, the High Plains aquifer consists principally of the Ogallala Formation of late Tertiary age and the overlying deposits of Quaternary age. In south-central Kansas, the aquifer consists of unconsolidated deposits principally of the Quaternary age. Valley alluvium of Quaternary age also is included in the deposits in both areas. The High Plains aquifer is delimited on the east by outcrops of Permian or Cretaceous rocks and by unsaturated deposits of Quaternary age.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811004","usgsCitation":"Pabst, M.E., and Stullken, L.E., 1981, Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980: U.S. Geological Survey Open-File Report 81-1004, 43.21 x 31.20 inches, https://doi.org/10.3133/ofr811004.","productDescription":"43.21 x 31.20 inches","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":349811,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1004/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175854,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1004/report-thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"High Plains Aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102,\n 40\n ],\n [\n -102,\n 37\n ],\n [\n -97,\n 37\n ],\n [\n -97,\n 39\n ],\n [\n -99,\n 39\n ],\n [\n -99,\n 40\n ],\n [\n -102,\n 40\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686ac3","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":242258,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stullken, Lloyd E.","contributorId":60609,"corporation":false,"usgs":true,"family":"Stullken","given":"Lloyd","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":242259,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}