{"pageNumber":"4854","pageRowStart":"121325","pageSize":"25","recordCount":184582,"records":[{"id":27768,"text":"wri854281 - 1986 - Hydrogeology and simulation of water flow in strata above the Bearpaw Shale and equivalents of eastern Montana and northeastern Wyoming","interactions":[],"lastModifiedDate":"2022-01-12T21:14:23.478786","indexId":"wri854281","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4281","title":"Hydrogeology and simulation of water flow in strata above the Bearpaw Shale and equivalents of eastern Montana and northeastern Wyoming","docAbstract":"

The Powder River, Bull Mountains, and Williston basins of Montana and Wyoming were investigated to understand the geohydrology and subsurface water flow. Rocks were separated into: Fox Hills-lower Hell Creek aquifer (layer 1), upper Hell Creek confining layer (layer 2), Tullock aquifer (layer 3), Lebo confining layer (layer 4), and Tongue River aquifer (layer 5). Aquifer transmissivities were estimated from ratios of sand and shale and adjusted for kinematic viscosity and compaction. Vertical hydraulic conductance per unit area between layers was estimated. Potentiometric surface maps were drawn from limited data. A three-dimensional finite-difference model was used for simulation. Five stages of simulation decreased and standard error of estimate for hydraulic head from 135 to 110 feet for 739 observation nodes. The resulting mean transmissivities for layers 1-5 were 443, 191, 374, 217, and 721 sq ft/d. The corresponding mean vertical hydraulic conductances per unit area between the layers were simulated; they ranged from 0.000140 to 0.0000150. Mean annual recharge across the study area was about 0.26 percent of average annual precipitation. Large volumes of interlayer flow indicate the vertical flow may be significant.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854281","usgsCitation":"Hotchkiss, W.R., and Levings, J.F., 1986, Hydrogeology and simulation of water flow in strata above the Bearpaw Shale and equivalents of eastern Montana and northeastern Wyoming: U.S. Geological Survey Water-Resources Investigations Report 85-4281, v, 72 p., https://doi.org/10.3133/wri854281.","productDescription":"v, 72 p.","costCenters":[],"links":[{"id":394280,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36419.htm"},{"id":56613,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4281/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123489,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4281/report-thumb.jpg"}],"country":"United States","state":"Montana, Wyoming","otherGeospatial":"Bearpaw Shale","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.733,\n 42.817\n ],\n [\n -104.033,\n 42.817\n ],\n [\n -104.033,\n 47.7830\n ],\n [\n -108.733,\n 47.7830\n ],\n [\n -108.733,\n 42.817\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685505","contributors":{"authors":[{"text":"Hotchkiss, W. R.","contributorId":61820,"corporation":false,"usgs":true,"family":"Hotchkiss","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Levings, J. F.","contributorId":94675,"corporation":false,"usgs":true,"family":"Levings","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":198665,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13235,"text":"ofr862 - 1986 - Application of the aerial profiling of terrain system","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr862","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-2","title":"Application of the aerial profiling of terrain system","docAbstract":"Test well Ch-Bf 146 was drilled to 1,650 ft below land surface to explore and evaluate the Patapsco Formation aquifers deeper than 1,000 ft in the Waldorf/La Plata area of Charles County, Maryland. The test hole penetrated two major aquifer systems above a depth of 1,000 ft and another major aquifer system and aquifer below 1,000 ft. The deepest aquifer system found in the test drilling, the Lower Patapsco aquifer system, is comprised of a group of sands which lie between 1,140 ft and the base of the Patapsco Formation at 1,417 ft. The Waldorf aquifer system, overlies the Upper Patapsco aquifer system and includes sands in the Waldorf/La Plata area that are referred to as the ' Magothy aquifer ' by other. At the test well site, the Waldorf aquifer system consists solely of sands in the Magothy and Monmouth Formations. The three major aquifer systems and the Middle Patapsco aquifer are correlative along the regional strike for at least 10 miles in the Waldorf/La Plata area. Correlations of geophysical logs indicate that individual sands 15 to 25 ft thick can be traced between wells. Geophysical log correlations also indicate that, at some well sites, the Waldorf aquifer system and the Upper Patapsco aquifer system are in sand-on-sand contact and function as one major hydrologic system at these sites. A production well (Ch-Bf 147) was drilled at the site of the test well (Ch-Bf 146). The initial static water level of these aquifers was 9.8 ft below sea level. Evaluation of the 24-hr pumping test of Ch-Bf 147 resulted in a transmissivity of 14,000 gpd/ft (gallons per day per foot) for the first 2 hours of the test and 7,300 gpd/ft for the remainder of the test. The decrease of 6,700 gpd/ft in the transmissivity indicates that the well 's expanding cone of depression intersected a transmissivity boundary after 2 hours of pumping. The Patapsco sands tested in Ch-Bf 147 have a storage coefficient of 0.0016. The hydraulic conductivity of the producing sands in Ch-Bf 147 is 127 gpd/sq ft. The quality of groundwater from the Lower Patapsco aquifer system and the Middle Patapsco aquifer is suitable for most purposes. The water is nearly neutral (pH = 7.4), low in dissolved solids (about 200 mg/L), low in specific conductance, slightly warm (22 C), very soft, naturally fluoridated, and moderately high in dissolved silica. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr862","usgsCitation":"Cyran, E., 1986, Application of the aerial profiling of terrain system: U.S. Geological Survey Open-File Report 86-2, iii, 15 p. :maps ;28 cm., https://doi.org/10.3133/ofr862.","productDescription":"iii, 15 p. :maps ;28 cm.","costCenters":[],"links":[{"id":145878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0002/report-thumb.jpg"},{"id":41620,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0002/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e482ce4b07f02db4e878e","contributors":{"authors":[{"text":"Cyran, E.J.","contributorId":39792,"corporation":false,"usgs":true,"family":"Cyran","given":"E.J.","affiliations":[],"preferred":false,"id":167448,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12813,"text":"ofr86144 - 1986 - Hydrologic reconnaissance and summary of existing data on surface and ground-water resources in the Missouri River valley in Woodbury and Monona counties, Iowa, 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:06:53","indexId":"ofr86144","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-144","title":"Hydrologic reconnaissance and summary of existing data on surface and ground-water resources in the Missouri River valley in Woodbury and Monona counties, Iowa, 1985","docAbstract":"A hydrologic reconnaissance of the Missouri River valley in western Iowa was begun in 1985. The study area is about 400 sq mi of Missouri River flood plain used mainly for agricultural purposes and is located mostly in parts of Woodbury and Monona Counties, Iowa. The reconnaissance was conducted to determine the extent of hydrologic information available for the study area and to determine if the existing data base is sufficient to support an interpretive investigation to quantify the groundwater/surface water relationships in the area. Extensive information concerning the surface water resources of the area, particularly the Missouri River, is available. Very little information concerning the geometry, hydraulic characteristics and groundwater flow relationships in the alluvial aquifer is available. Information needs to be collected to create an adequate data base for future simulation of groundwater flow and to calibrate any estimates of flow. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86144","usgsCitation":"Buchmiller, R., 1986, Hydrologic reconnaissance and summary of existing data on surface and ground-water resources in the Missouri River valley in Woodbury and Monona counties, Iowa, 1985: U.S. Geological Survey Open-File Report 86-144, iv, 21 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr86144.","productDescription":"iv, 21 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":147407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0144/report-thumb.jpg"},{"id":41229,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0144/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605675","contributors":{"authors":[{"text":"Buchmiller, R.C.","contributorId":59458,"corporation":false,"usgs":true,"family":"Buchmiller","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":166759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12931,"text":"ofr86340 - 1986 - Calibration and acceptance testing of the DE-200 digital seismograph with S-6000 and L-4C seismometers","interactions":[],"lastModifiedDate":"2012-02-02T00:06:56","indexId":"ofr86340","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-340","title":"Calibration and acceptance testing of the DE-200 digital seismograph with S-6000 and L-4C seismometers","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86340","usgsCitation":"Carver, D.L., Cunningham, D., and King, K.W., 1986, Calibration and acceptance testing of the DE-200 digital seismograph with S-6000 and L-4C seismometers: U.S. Geological Survey Open-File Report 86-340, ii, 28 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86340.","productDescription":"ii, 28 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":146949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0340/report-thumb.jpg"},{"id":41379,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0340/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f95d1","contributors":{"authors":[{"text":"Carver, D. L.","contributorId":55808,"corporation":false,"usgs":true,"family":"Carver","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":166976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cunningham, D.R.","contributorId":94316,"corporation":false,"usgs":true,"family":"Cunningham","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":166977,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"King, K. W.","contributorId":105729,"corporation":false,"usgs":true,"family":"King","given":"K.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":166978,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":60776,"text":"mf1831 - 1986 - Isopach map of interval between top of the Pictured Cliffs Sandstone and the Huerfanito Bentonite bed of the Lewis Shale, La Plata County, Colorado, and Rio Arriba and San Juan counties, New Mexico","interactions":[],"lastModifiedDate":"2016-08-23T09:22:08","indexId":"mf1831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1831","title":"Isopach map of interval between top of the Pictured Cliffs Sandstone and the Huerfanito Bentonite bed of the Lewis Shale, La Plata County, Colorado, and Rio Arriba and San Juan counties, New Mexico","docAbstract":"

This thickness map of a Late Cretaceous interval in the northwestern part of the San Juan Basin is part of a study of the relationship between ancient shore 1ines and coal-forming swamps during the filial regression of the Cretaceous epicontinental sea. The top of the thickness interval is the top of the Pictured Cliffs Sands tone. The base of the interval is a thin time marker, the Huerfanito Bentonite Bed of the Lewis Shale. The interval includes all of the Pictured Cliffs Sandstone and the upper part of the Lewis Shale. The northwest boundary of the map area is the outcrop of the Pictured Cliffs Sandstone and the Lewis Shale.

\n

Data used for the isopach map are mostly from interpretation of geophysical logs of oil and gas wells, southeast of the outcrop in parts of the Cortez, Durango, Farmington, and Navajo Reservoir 1: 100,000-scale quadrangles, Colorado and New Mexico. Cross sections A-A’ and B-B' give examples of geophysical logs that show some of the variations in the isopach interval.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1831","usgsCitation":"Sandberg, D., 1986, Isopach map of interval between top of the Pictured Cliffs Sandstone and the Huerfanito Bentonite bed of the Lewis Shale, La Plata County, Colorado, and Rio Arriba and San Juan counties, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1831, 2 Plates: 37.83 x 52.35 inches and 40.54 x 39.40 inches, https://doi.org/10.3133/mf1831.","productDescription":"2 Plates: 37.83 x 52.35 inches and 40.54 x 39.40 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326168,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1831.JPG"},{"id":327474,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1831/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327475,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1831/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Colorado, New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.5,36.75 ], [ -108.5,37.25 ], [ -107.5,37.25 ], [ -107.5,36.75 ], [ -108.5,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667123","contributors":{"authors":[{"text":"Sandberg, D.T.","contributorId":91123,"corporation":false,"usgs":true,"family":"Sandberg","given":"D.T.","email":"","affiliations":[],"preferred":false,"id":264380,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40602,"text":"ofr86388 - 1986 - China oil and gas, geologic evaluation of potential for exploration and development","interactions":[],"lastModifiedDate":"2012-02-02T00:10:33","indexId":"ofr86388","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-388","title":"China oil and gas, geologic evaluation of potential for exploration and development","language":"ENGLISH","doi":"10.3133/ofr86388","usgsCitation":"Masters, C., Lee, K.Y., Ulmishek, G., and Robinson, K., 1986, China oil and gas, geologic evaluation of potential for exploration and development: U.S. Geological Survey Open-File Report 86-388, 1 map :photocopy ;87 x 101 cm., on sheet 98 x 107 cm., https://doi.org/10.3133/ofr86388.","productDescription":"1 map :photocopy ;87 x 101 cm., on sheet 98 x 107 cm.","costCenters":[],"links":[{"id":173381,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":77126,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0388/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a3cf","contributors":{"authors":[{"text":"Masters, C.D.","contributorId":96664,"corporation":false,"usgs":true,"family":"Masters","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":223592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, K. Y.","contributorId":74351,"corporation":false,"usgs":true,"family":"Lee","given":"K.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":223589,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ulmishek, Gregory","contributorId":88361,"corporation":false,"usgs":true,"family":"Ulmishek","given":"Gregory","email":"","affiliations":[],"preferred":false,"id":223591,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robinson, Keith","contributorId":80277,"corporation":false,"usgs":true,"family":"Robinson","given":"Keith","affiliations":[],"preferred":false,"id":223590,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":60641,"text":"mf1855 - 1986 - Map showing areas of visible land disturbances caused by two military training operations in the Mojave Desert, California","interactions":[],"lastModifiedDate":"2016-08-23T09:04:34","indexId":"mf1855","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1855","title":"Map showing areas of visible land disturbances caused by two military training operations in the Mojave Desert, California","docAbstract":"

This map shows areas that retain visible land disturbances produced during two military armored-vehicle training operations in the Mojave Desert, California. The map documents the lasting visual effects these operations have on this arid region and provides a data base for monitoring changes in the extent of visual disturbances in the future.

\n

The first training operation was initiated in April 1942, by General George S. Patton, Jr., to ready armored-vehicle divisions for desert warfare in North Africa (Meller, 1946). The Desert Training Center (DTC) encompassed 17,500 mi2 of arid lands in California, Nevada, and Arizona, and for two years, more than one million soldiers trained under simulated battle conditions. Troops were stationed at 12 main base camps, each housing as many as 15,000 soldiers in canvas tents. From these camps, armored units would radiate into the broad valleys of the Mojave and Sonoran Deserts. Thousands of tanks, trucks, jeeps, and aircraft were used in the war games. When the DTC was inactivated in May 1944, most man-made structures were removed or buried by the U.S. Army.

\n

The second operation, called Operation Desert Strike, was held for two weeks in May 1964 (Moenk, 1964) in the same general area as the DTC. However, no temporary camps were established, and the tanks used were much larger than their World War II counterparts. Over 89,000 troops participated in this exercise.

\n

Land disturbances caused by these training exercises are still evident today throughout the designated training areas (Lathrop, 1983; Prose, 1985; Prose and Metzger, 1985). The World War II base-camp locations are easily identified because the networks of dirt roads are still used by campers, hunters, artifact seekers, and other visitors. Vehicle trails and single tracks remain on many relatively stable surfaces and are most conspicuous on surfaces composed of a veneer of stones (desert pavement).

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1855","usgsCitation":"Prose, D., 1986, Map showing areas of visible land disturbances caused by two military training operations in the Mojave Desert, California: U.S. Geological Survey Miscellaneous Field Studies Map 1855, Plate: 29.51 x 43.22 inches, https://doi.org/10.3133/mf1855.","productDescription":"Plate: 29.51 x 43.22 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326126,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1855.JPG"},{"id":327434,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1855/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","otherGeospatial":"Mojave Desert","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116,32.75 ], [ -116,35.5 ], [ -114,35.5 ], [ -114,32.75 ], [ -116,32.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db659419","contributors":{"authors":[{"text":"Prose, D.V.","contributorId":92682,"corporation":false,"usgs":true,"family":"Prose","given":"D.V.","email":"","affiliations":[],"preferred":false,"id":264123,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43332,"text":"ofr83105 - 1986 - Land use and land cover and associated maps for Marquette, Michigan","interactions":[],"lastModifiedDate":"2012-02-02T00:04:53","indexId":"ofr83105","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"83-105","title":"Land use and land cover and associated maps for Marquette, Michigan","language":"ENGLISH","doi":"10.3133/ofr83105","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Land use and land cover and associated maps for Marquette, Michigan: U.S. Geological Survey Open-File Report 83-105, maps :photocopy ;41 x 62 cm., https://doi.org/10.3133/ofr83105.","productDescription":"maps :photocopy ;41 x 62 cm.","costCenters":[],"links":[{"id":134918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0e1a","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":531119,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60626,"text":"mf1794 - 1986 - Map showing slope movements in the Oak Forest Quadrangle, Greene County, southwestern Pennsylvania","interactions":[],"lastModifiedDate":"2016-08-23T08:56:58","indexId":"mf1794","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1794","title":"Map showing slope movements in the Oak Forest Quadrangle, Greene County, southwestern Pennsylvania","docAbstract":"

This map is the first example in the eastern United States of a 1:24,000-scale 7.5– minute quadrangle map that identifies areas with slope—stability problems in detail. Such a map enables the user to make a rapid evaluation of the potential for mass movement. Furthermore, detailed slope movement inventory of this type can serve as a framework for statistical analyses of several factors that cause slope failures, such as the effects of bedrock lithology, soil and slope characteristics, and precipitation. Planners, engineers, soil scientists, geologists, and elected officials should find the map useful in the assessment of slope hazards and planning for future land use. Final evaluation of any site within the quadrangle should be based on an examination by a soils engineer or an engineering geologist.

\n

Field investigations in the springs of 1981 and 1982 and the fall of 1981 involved nearly 60 days of traverses. The foot traverses were supplemented by the interpretation of the land surface on vertical black-and-white aerial photography flown in January and February of 1973 at a scale of nearly 1:24,000. Earlier aerial photography flown in June and July 1939 at a scale of 1:20,000 and more recent but significantly smaller scale photography (1:80,000) flown in June 1977 supplied additional documentation. More than 1,200 active or recently active and 900 older slope movements were identified.

\n

The geologic map of the Oak Forest quadrangle (Roen, 1972) is one of several geologic maps at a scale of 1:24,000 in eastern and central Greene County. Stone (1932) wrote an earlier report of the geology and mineral resources of Greene County. A series of reconnaissance landslide maps at 1:24,000 scale based mainly on aerial photographic interpretation included Greene and adjacent counties (Hackman and Thomas, 1978).

\n

Selection of the Oak Forest quadrangle for a more comprehensive study of the slope movements was based on the existence of a recent geologic map (Roen, 1972), sizeable tracts of both forested and non-forested land, nearby precipitation record stations, a large number of pipelines which could offer pertinent data, and good accessibility of terrain from secondary roads. Finally, Hackman and Thomas (1978) showed that the area was representative of any quadrangle in the northern part of the Dunkard basin in its distribution and density of slope movements.

\n

The quadrangle is located about 65 km southwest of Pittsburgh, Penn. (fig. 1). Three distinct drainage systems (north, east, and south trending) are represented within the quadrangle (fig. 2).

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Correlation of coal beds in the Fruitland Formation (Upper Cretaceous) in the subsurface, from interpretation of geophysical logs, is an outgrowth of unpublished studies of deep coal on the Navajo Reservation by the author in the Toadlena 30 x 60 minute quadrangle, New Mexico, and by W. J. Mapel in the Farmington 30 x 60 minute quadrangle, New Mexico.  The lines of sections of this report extend eastward from the reservation into east-central San Juan County, which is in the western part of the San Juan Basin.  In this area, the rocks dip gently northeast toward the central part of the basin.  The thick coal is less than 1,500 feet beneath the surface.  Of the 53 logs in the sections, 48 are from oil- and gas-test holes, and 5 are from coal-test holes (see table 1).  Stratigraphic relations of the Upper Cretaceous Lewis Shale, Pictured Cliffs Sandstone, and Fruitland Formation, shown on the cross sections and briefly reviewed below, have been previously described for this or other parts of the San Juan Basin by Hayes and Zapp (1955), Beaumont (1971), Fassett and hinds (1971), O;Sullivan and other (1972), and Molenaar (1983), among others.

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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8643","usgsCitation":"Ratcliffe, N.M., Burton, W., Anderson, R., and Moos, D., 1986, Preliminary results of coring of the Furlong Fault near Lake Aquetong, New Hope, Pennsylvania: U.S. Geological Survey Open-File Report 86-43, ii, 23 p., https://doi.org/10.3133/ofr8643.","productDescription":"ii, 23 p.","costCenters":[],"links":[{"id":147502,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0043/report-thumb.jpg"},{"id":44536,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0043/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":464668,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16917.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Pennsylvania","city":"New Hope","otherGeospatial":"Furlong Fault near Lake Aquetong","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.917,\n 40.413\n ],\n [\n -75.125,\n 40.413\n ],\n [\n -75.125,\n 40.25\n ],\n [\n -74.917,\n 40.25\n ],\n [\n -74.917,\n 40.413\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b363","contributors":{"authors":[{"text":"Ratcliffe, N. 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1986 - Geomorphic map of the Kyle Canyon alluvial fan, Clark County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:13","indexId":"ofr86210","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-210","title":"Geomorphic map of the Kyle Canyon alluvial fan, Clark County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86210","usgsCitation":"Sowers, J., 1986, Geomorphic map of the Kyle Canyon alluvial fan, Clark County, Nevada: U.S. Geological Survey Open-File Report 86-210, ii, 9 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr86210.","productDescription":"ii, 9 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0210/report-thumb.jpg"},{"id":45008,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0210/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45009,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0210/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45010,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0210/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c507","contributors":{"authors":[{"text":"Sowers, J.M.","contributorId":89546,"corporation":false,"usgs":true,"family":"Sowers","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":172201,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13335,"text":"ofr86364 - 1986 - Mineral resource potential of National Forest RARE II and wilderness areas in Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr86364","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-364","title":"Mineral resource potential of National Forest RARE II and wilderness areas in Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86364","usgsCitation":"Dickerson, R.P., 1986, Mineral resource potential of National Forest RARE II and wilderness areas in Colorado: U.S. Geological Survey Open-File Report 86-364, vi, 178 p. :map ;28 cm., https://doi.org/10.3133/ofr86364.","productDescription":"vi, 178 p. :map ;28 cm.","costCenters":[],"links":[{"id":147985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0364/report-thumb.jpg"},{"id":41755,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0364/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41756,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0364/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db62863d","contributors":{"authors":[{"text":"Dickerson, R. 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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 geophysical survey of the Winchester Roadless Area in the Coronado National Forest, Cochise County, Arizona. The Winchester Roadless Area (03122) 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.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1851","usgsCitation":"Martin, R., 1986, Geophysical maps of the Winchester Roadless Area, Cochise County, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1851, 56.23 x 37.81 inches, https://doi.org/10.3133/mf1851.","productDescription":"56.23 x 37.81 inches","costCenters":[],"links":[{"id":357800,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1851/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1851/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Cochise County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.16666666666667,32.333333333333336 ], [ -110.16666666666667,32.416666666666664 ], [ -110.08333333333333,32.416666666666664 ], [ -110.08333333333333,32.333333333333336 ], [ -110.16666666666667,32.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b47b","contributors":{"authors":[{"text":"Martin, R.A.","contributorId":53379,"corporation":false,"usgs":true,"family":"Martin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":263343,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16062,"text":"ofr86460 - 1986 - Principle facts for gravity stations along lines 4A and 4B of the Quebec-western Maine seismic reflection profile, west-central Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr86460","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-460","title":"Principle facts for gravity stations along lines 4A and 4B of the Quebec-western Maine seismic reflection profile, west-central Maine","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86460","usgsCitation":"Snyder, S.L., and Phillips, J., 1986, Principle facts for gravity stations along lines 4A and 4B of the Quebec-western Maine seismic reflection profile, west-central Maine: U.S. Geological Survey Open-File Report 86-460, 20 p. :maps ;28 cm., https://doi.org/10.3133/ofr86460.","productDescription":"20 p. :maps ;28 cm.","costCenters":[],"links":[{"id":150319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0460/report-thumb.jpg"},{"id":44994,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0460/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66711c","contributors":{"authors":[{"text":"Snyder, S. L.","contributorId":25132,"corporation":false,"usgs":true,"family":"Snyder","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":172173,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, J. D. 0000-0002-6459-2821","orcid":"https://orcid.org/0000-0002-6459-2821","contributorId":22366,"corporation":false,"usgs":true,"family":"Phillips","given":"J. D.","affiliations":[],"preferred":false,"id":172172,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}