Melting occurs at progressively greater depths and higher temperatures from west to east across the Cascades volcanic arc in northern California, as demonstrated by compositional variations observed in high-alumina olivine tholeiites. The lavas studied erupted from seven vents defining a 75-km-long, east-west transect across the arc, from near Mount Shasta to east of Medicine Lake volcano. The increase in melting depth across the arc parallels modeled isotherms in the mantle wedge and does not parallel the inferred dip of the slab. The depth of mantle melting at which the high-alumina olivine tholeiites were created is ∼36 km at the western end of the transect and 66 km at the eastern end. The very high temperatures of dry melting so close to the crust indicate a transitory condition of the mantle.
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","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coastal dynamics '01","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Fourth Conference on Coastal Dynamics","conferenceDate":"June 11-15, 2001","conferenceLocation":"Lund, Sweden","language":"English","publisher":"American Society of Civil Engineers","doi":"10.1061/40566(260)64","usgsCitation":"Ruggiero, P., Gelfenbaum, G., Thompson, D., and Kaminsky, G.M., 2001, Exploring the relationship between nearshore morphology and shoreline change, in Coastal dynamics '01, Lund, Sweden, June 11-15, 2001, p. 627-636, https://doi.org/10.1061/40566(260)64.","productDescription":"10 p.","startPage":"627","endPage":"636","costCenters":[],"links":[{"id":416822,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2012-04-26","publicationStatus":"PW","contributors":{"authors":[{"text":"Ruggiero, Peter","contributorId":15709,"corporation":false,"usgs":false,"family":"Ruggiero","given":"Peter","affiliations":[{"id":6680,"text":"Oregon State University","active":true,"usgs":false}],"preferred":false,"id":872020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gelfenbaum, Guy 0000-0003-1291-6107","orcid":"https://orcid.org/0000-0003-1291-6107","contributorId":217329,"corporation":false,"usgs":true,"family":"Gelfenbaum","given":"Guy","affiliations":[],"preferred":true,"id":872021,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, David","contributorId":68216,"corporation":false,"usgs":true,"family":"Thompson","given":"David","email":"","affiliations":[],"preferred":false,"id":872022,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kaminsky, George M","contributorId":221036,"corporation":false,"usgs":false,"family":"Kaminsky","given":"George","email":"","middleInitial":"M","affiliations":[{"id":25353,"text":"Washington State Department of Ecology","active":true,"usgs":false}],"preferred":false,"id":872023,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70243318,"text":"70243318 - 2001 - Coastal evolution and sediment budget at the mouth of the Columbia River, USA","interactions":[],"lastModifiedDate":"2023-05-08T16:30:12.631699","indexId":"70243318","displayToPublicDate":"2001-07-01T11:23:29","publicationYear":"2001","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Coastal evolution and sediment budget at the mouth of the Columbia River, USA","docAbstract":"The coastal morphology of the Mouth of the Columbia River (MCR) has changed dramatically over the past century. Since the construction of jetties in 1914 and 1917, the inlet deepened and stabilized, the outer ebb delta migrated northward and offshore several kilometers, and the adjacent shorelines to the north and south prograded several hundreds of meters. Recently, high rates of erosion along these adjacent shorelines affecting parklands have raised questions about the cause of the erosion. The purpose of the sediment budget analysis presented here is to address these questions by quantitatively examining the links between the morphology change of the shoreline and the ebb delta and historical changes in local and regional sediment supply.
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(some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr0126.","productDescription":"20 p., :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":156097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0026/report-thumb.jpg"},{"id":51210,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e424e","contributors":{"authors":[{"text":"Herring, J. R.","contributorId":43348,"corporation":false,"usgs":true,"family":"Herring","given":"J. R.","affiliations":[],"preferred":false,"id":185155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Castle, C.J.","contributorId":88772,"corporation":false,"usgs":true,"family":"Castle","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":185157,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Z. A.","contributorId":82708,"corporation":false,"usgs":true,"family":"Brown","given":"Z.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":185156,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Briggs, Paul H.","contributorId":107691,"corporation":false,"usgs":true,"family":"Briggs","given":"Paul H.","affiliations":[],"preferred":false,"id":185158,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":31228,"text":"ofr0166 - 2001 - Benthic habitat and faunal surveys of Closed Area II, central Georges Bank, 1998 and 1999","interactions":[],"lastModifiedDate":"2017-01-18T10:12:29","indexId":"ofr0166","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-66","title":"Benthic habitat and faunal surveys of Closed Area II, central Georges Bank, 1998 and 1999","language":"ENGLISH","doi":"10.3133/ofr0166","usgsCitation":"Valentine, P.C., Malczyk, J., and Middleton, T.J., 2001, Benthic habitat and faunal surveys of Closed Area II, central Georges Bank, 1998 and 1999: U.S. Geological Survey Open-File Report 2001-66, One CD-ROM , https://doi.org/10.3133/ofr0166.","productDescription":"One CD-ROM ","costCenters":[],"links":[{"id":161073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":333321,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0066/ofr0166.zip","text":"Disc","linkFileType":{"id":6,"text":"zip"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b52b","contributors":{"authors":[{"text":"Valentine, P. C.","contributorId":46505,"corporation":false,"usgs":true,"family":"Valentine","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":205387,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Malczyk, J.T.","contributorId":10465,"corporation":false,"usgs":true,"family":"Malczyk","given":"J.T.","affiliations":[],"preferred":false,"id":205385,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Middleton, T. J.","contributorId":15669,"corporation":false,"usgs":true,"family":"Middleton","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":205386,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":33092,"text":"b2064W - 2001 - The geology and mineral deposits of part of the western half of the Hailey 1 degree x 2 degrees quadrangle, Idaho","interactions":[],"lastModifiedDate":"2021-08-17T21:08:20.187064","indexId":"b2064W","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2064","chapter":"W","title":"The geology and mineral deposits of part of the western half of the Hailey 1 degree x 2 degrees quadrangle, Idaho","docAbstract":"Rocks in the western half of the Hailey 1°x2° quadrangle of south-central Idaho include various units of the Atlanta lobe of the Idaho batholith (biotite granodiorite to two-mica granite) of Cretaceous age and plutons and dikes of Tertiary (Eocene to Miocene) age that intrude the batholith. Eocene plutonic rocks consist of a bimodal suite of anorogenic granite and tonalite-granodiorite and hypabyssal rhyolite and rhyodacite dikes. Rocks of the Eocene Challis Volcanics are scarce in the map area but are widespread to the east. Rhyolite ash flows of the Miocene Idavada Volcanics and basalt of the Snake River Plain crop out in the southern part of the area. Lacustrine rocks of probable Eocene to Holocene age are present in the vicinity of Anderson Ranch Reservoir. Quaternary basalts and gravels are widespread on the South Fork of the Boise River, and alluvial deposits are common along active drainages. Metasedimentary rocks of unknown age crop out on House Mountain, Chimney Peak, and on the ridges east of Anderson Ranch Reservoir.
Older structures in the Idaho batholith include a major fault beneath House Mountain that may be a decollement for one of the large thrust sheets in eastern Idaho or part of an extensional core complex. The southern part of the Atlanta lobe of the Idaho batholith is cut by northeast-striking faults (parallel with the Trans-Challis fault system) that are related to Eocene extension and by northwest-oriented faults that formed during basin and range extension in the Miocene. The basin and range faults have prominent scarps typical of basin and range topography. The combination of northeast and northwest faults has broken the batholith into a series of rhomboid blocks. Some of these northeast and northwest faults are older structures that were reactivated in the Eocene or Miocene, as indicated by Ar 40 /Ar 39 dates on mineralized rock contained in some of the structures.
The Idaho batholith and associated rocks in the map area host several hundred mines and prospects in 18 mining districts. The deposits range in age from Cretaceous to Eocene, and many were developed for precious metals. Most of the deposits are in quartz veins in shear zones in granitic rocks of the batholith. Several districts were actively being explored for low-grade, bulk-minable, precious-metal deposits in the late 1980s and early 1990s.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2064W","usgsCitation":"Bennett, E.H., 2001, The geology and mineral deposits of part of the western half of the Hailey 1 degree x 2 degrees quadrangle, Idaho: U.S. Geological Survey Bulletin 2064, 39 p., https://doi.org/10.3133/b2064W.","productDescription":"39 p.","costCenters":[],"links":[{"id":160595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3294,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/b2064-w/","linkFileType":{"id":5,"text":"html"}},{"id":388065,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_38252.htm"}],"country":"United States","state":"Idaho","otherGeospatial":"Hailey 1° x 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.0000,\n 43.000\n ],\n [\n -114.7610,\n 43.000\n ],\n [\n -114.7610,\n 44.0000\n ],\n [\n -116.0000,\n 44.0000\n ],\n [\n -116.0000,\n 43.000\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4835","contributors":{"authors":[{"text":"Bennett, Earl H.","contributorId":97093,"corporation":false,"usgs":true,"family":"Bennett","given":"Earl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":209873,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30920,"text":"wri014080 - 2001 - Sediment oxygen demand in upper Klamath and Agency lakes, Oregon, 1999","interactions":[],"lastModifiedDate":"2016-06-24T08:53:40","indexId":"wri014080","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-4080","title":"Sediment oxygen demand in upper Klamath and Agency lakes, Oregon, 1999","docAbstract":"Sediment oxygen demand (SOD) was measured in two shallow, interconnected lakes in southern Oregon, Upper Klamath Lake and Agency Lake, in spring and late summer of 1999. Upper Klamath Lake contains populations of two endangered fishes, the shortnose sucker and the Lost River sucker, and low dissolved oxygen concentrations in summer are thought to be one factor affecting sucker populations.
\nThe distribution of SOD20 values (measured sediment oxygen demand values corrected to 20o C [degrees Celsius]) had a median value of 1.6 g/m2/day (grams per square meter per day) in the spring and 1.7 g/m2/day in the late summer. These values were well within the range of values in the literature for sites with similar sediment characteristics: primarily silty with at least a moderate amount of organic content.
\nLittle variation in SOD was observed--the interquartile range in values was 0.4 g/m2/day in the spring and 0.7 g/m2/day in the late summer. A significant exception was apparent in Ball Bay, where SOD in the late summer was greater than 10.2 g/m2/day. In the absence of primary production, an SOD of this magnitude could deplete the water column of oxygen in a few days. This measurement provided evidence that localized areas of very high SOD occur episodically in the bays, perhaps associated with large algal mats being trapped by the lake circulation patterns.
\nA statistical test for a spring to late summer difference in the median values of SOD confirmed that SOD in the late summer (median value 1.7 g/m2/day) was significantly higher than in the spring (median value 1.2 g/m2/day). The difference was primarily due to seasonal changes in temperature, however; when SOD values were corrected to 20o C, there was no seasonal difference in the median values.
\nThere was no correlation between SOD20 and the sediment characteristics measured in this study: percent fines, organic carbon, and residue lost on ignition.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri014080","collaboration":"Prepared in cooperation with the Bureau of Reclamation","usgsCitation":"Wood, T.M., 2001, Sediment oxygen demand in Upper Klamath and Agency Lakes, Oregon, 1999:\nU.S. Geological Survey Water-Resources Investigations Report 01–4080, 13 p.","productDescription":"13 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":2882,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4080/wri01-4080.pdf","text":"Report","size":"420 KB","linkFileType":{"id":1,"text":"pdf"},"description":"PDF of report"},{"id":160292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4080/coverthb.jpg"}],"contact":"Director, Oregon Water Science Center
U.S. Geological Survey
2130 SW 5th Avenue
Portland, Oregon 97201
http://or.water.usgs.gov
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0140","usgsCitation":"Aycock, R.A., and Haugh, C.J., 2001, Ground-water hydrology and water-quality data for wells, springs, and surface-water sites in the Bradley-Brumalow creeks area near Arnold Air Force Base, Tennessee, September to December 1999: U.S. Geological Survey Open-File Report 2001-40, iv, 49 p., https://doi.org/10.3133/ofr0140.","productDescription":"iv, 49 p.","costCenters":[],"links":[{"id":160888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":390528,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37346.htm"},{"id":2746,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr01-040/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Tennessee","otherGeospatial":"Bradley-Brumalow Creeks area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.1386489868164,\n 35.294952147406576\n ],\n [\n -85.98037719726562,\n 35.294952147406576\n ],\n [\n -85.98037719726562,\n 35.47744667178578\n ],\n [\n -86.1386489868164,\n 35.47744667178578\n ],\n [\n -86.1386489868164,\n 35.294952147406576\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668d0e","contributors":{"authors":[{"text":"Aycock, Robert A.","contributorId":75976,"corporation":false,"usgs":true,"family":"Aycock","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haugh, Connor J. 0000-0002-5204-8271 cjhaugh@usgs.gov","orcid":"https://orcid.org/0000-0002-5204-8271","contributorId":3932,"corporation":false,"usgs":true,"family":"Haugh","given":"Connor","email":"cjhaugh@usgs.gov","middleInitial":"J.","affiliations":[{"id":581,"text":"Tennessee Water Science Center","active":true,"usgs":true}],"preferred":true,"id":205336,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":31200,"text":"ofr00600A - 2001 - Preliminary determination of epicenters; monthly listing, January-March 2000","interactions":[],"lastModifiedDate":"2012-02-02T00:09:05","indexId":"ofr00600A","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2000-600","chapter":"A","title":"Preliminary determination of epicenters; monthly listing, January-March 2000","language":"ENGLISH","doi":"10.3133/ofr00600A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2001, Preliminary determination of epicenters; monthly listing, January-March 2000: U.S. Geological Survey Open-File Report 2000-600, 40 p., https://doi.org/10.3133/ofr00600A.","productDescription":"40 p.","costCenters":[],"links":[{"id":160313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0600a/report-thumb.jpg"},{"id":59703,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0600a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c548","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":529266,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31205,"text":"ofr0119 - 2001 - Potentiometric surfaces of the intermediate aquifer system, west-central Florida, May 2000","interactions":[],"lastModifiedDate":"2012-02-02T00:09:05","indexId":"ofr0119","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-19","title":"Potentiometric surfaces of the intermediate aquifer system, west-central Florida, May 2000","language":"ENGLISH","doi":"10.3133/ofr0119","usgsCitation":"Duerr, A.D., 2001, Potentiometric surfaces of the intermediate aquifer system, west-central Florida, May 2000: U.S. Geological Survey Open-File Report 2001-19, 2 maps on one sheet ;41 x 42 cm. and 24 x 38 cm., on sheet 84 x 76 cm., folded to 22 x 23 cm., https://doi.org/10.3133/ofr0119.","productDescription":"2 maps on one sheet ;41 x 42 cm. and 24 x 38 cm., on sheet 84 x 76 cm., folded to 22 x 23 cm.","costCenters":[],"links":[{"id":160329,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":59705,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2001/0019/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db682525","contributors":{"authors":[{"text":"Duerr, A. D.","contributorId":29821,"corporation":false,"usgs":true,"family":"Duerr","given":"A.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":205321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31242,"text":"ofr0188 - 2001 - Geologic map of the Ontonagon and part of the Wakefield 30' X 60' quadrangles, Michigan; a digital representation of Map I-2499 (1995)","interactions":[],"lastModifiedDate":"2012-02-02T00:09:07","indexId":"ofr0188","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-88","title":"Geologic map of the Ontonagon and part of the Wakefield 30' X 60' quadrangles, Michigan; a digital representation of Map I-2499 (1995)","language":"ENGLISH","doi":"10.3133/ofr0188","usgsCitation":"Cannon, W., Nicholson, S.W., Woodruff, L.G., Hedgman, C.A., Schultz, K., and Pimley, S., 2001, Geologic map of the Ontonagon and part of the Wakefield 30' X 60' quadrangles, Michigan; a digital representation of Map I-2499 (1995): U.S. Geological Survey Open-File Report 2001-88, One CD-ROM., https://doi.org/10.3133/ofr0188.","productDescription":"One CD-ROM.","costCenters":[],"links":[{"id":160760,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af6e4b07f02db692aff","contributors":{"authors":[{"text":"Cannon, W.F. 0000-0002-2699-8118","orcid":"https://orcid.org/0000-0002-2699-8118","contributorId":70382,"corporation":false,"usgs":true,"family":"Cannon","given":"W.F.","affiliations":[],"preferred":false,"id":205446,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nicholson, S. W.","contributorId":79504,"corporation":false,"usgs":true,"family":"Nicholson","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":205447,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodruff, L. G.","contributorId":46999,"corporation":false,"usgs":true,"family":"Woodruff","given":"L.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":205445,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hedgman, C. A.","contributorId":82795,"corporation":false,"usgs":true,"family":"Hedgman","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205448,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schultz, K.J.","contributorId":14248,"corporation":false,"usgs":true,"family":"Schultz","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":205444,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pimley, S.G.","contributorId":99424,"corporation":false,"usgs":true,"family":"Pimley","given":"S.G.","email":"","affiliations":[],"preferred":false,"id":205449,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":31212,"text":"ofr0135 - 2001 - Hydraulic and mechanical properties affecting ground-water flow and aquifer-system compaction, San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:09:06","indexId":"ofr0135","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-35","title":"Hydraulic and mechanical properties affecting ground-water flow and aquifer-system compaction, San Joaquin Valley, California","docAbstract":"This report summarizes hydraulic and mechanical properties affecting ground-water flow and aquifer-system compaction in the San Joaquin Valley, a broad alluviated intermontane structural trough that constitutes the southern two-thirds of the Central Valley of California. These values will be used to constrain a coupled ground-water flow and aquifer-system compaction model of the western San Joaquin Valley called WESTSIM. A main objective of the WESTSIM model is to evaluate potential future land subsidence that might occur under conditions in which deliveries of imported surface water for agricultural use are reduced and ground-water pumping is increased. Storage values generally are components of the total aquifer-system storage and include inelastic and elastic skeletal storage values of the aquifers and the aquitards that primarily govern the potential amount of land subsidence. Vertical hydraulic conductivity values generally are for discrete thicknesses of sediments, usually aquitards, that primarily govern the rate of land subsidence. The data were compiled from published sources and include results of aquifer tests, stress-strain analyses of borehole extensometer observations, laboratory consolidation tests, and calibrated models of aquifer-system compaction.","language":"ENGLISH","doi":"10.3133/ofr0135","usgsCitation":"Sneed, M., 2001, Hydraulic and mechanical properties affecting ground-water flow and aquifer-system compaction, San Joaquin Valley, California: U.S. Geological Survey Open-File Report 2001-35, 26 p., https://doi.org/10.3133/ofr0135.","productDescription":"26 p.","costCenters":[],"links":[{"id":2745,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr01035","linkFileType":{"id":5,"text":"html"}},{"id":160887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629b78","contributors":{"authors":[{"text":"Sneed, Michelle 0000-0002-8180-382X micsneed@usgs.gov","orcid":"https://orcid.org/0000-0002-8180-382X","contributorId":155,"corporation":false,"usgs":true,"family":"Sneed","given":"Michelle","email":"micsneed@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":205335,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31201,"text":"ofr00600B - 2001 - Preliminary determination of epicenters; monthly listing, April-June 2000","interactions":[],"lastModifiedDate":"2012-02-02T00:09:05","indexId":"ofr00600B","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2000-600","chapter":"B","title":"Preliminary determination of epicenters; monthly listing, April-June 2000","language":"ENGLISH","doi":"10.3133/ofr00600B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2001, Preliminary determination of epicenters; monthly listing, April-June 2000: U.S. Geological Survey Open-File Report 2000-600, 31 p., https://doi.org/10.3133/ofr00600B.","productDescription":"31 p.","costCenters":[],"links":[{"id":160325,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0600b/report-thumb.jpg"},{"id":59704,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0600b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c571","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":529267,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31262,"text":"ofr01118 - 2001 - Magnetotelluric data across the Battle Mountain-Eureka and Carlin trends, south of Cortez, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:04","indexId":"ofr01118","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-118","title":"Magnetotelluric data across the Battle Mountain-Eureka and Carlin trends, south of Cortez, Nevada","language":"ENGLISH","doi":"10.3133/ofr01118","usgsCitation":"Williams, J.M., Rodriguez, B.D., and Klein, D.P., 2001, Magnetotelluric data across the Battle Mountain-Eureka and Carlin trends, south of Cortez, Nevada (Version 1.0): U.S. Geological Survey Open-File Report 2001-118, 109 p., https://doi.org/10.3133/ofr01118.","productDescription":"109 p.","costCenters":[],"links":[{"id":160367,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2891,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0118/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649422","contributors":{"authors":[{"text":"Williams, Jackie M.","contributorId":11217,"corporation":false,"usgs":true,"family":"Williams","given":"Jackie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":205513,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodriguez, Brian D. 0000-0002-2263-611X brod@usgs.gov","orcid":"https://orcid.org/0000-0002-2263-611X","contributorId":836,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Brian","email":"brod@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":205512,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klein, Douglas P.","contributorId":50896,"corporation":false,"usgs":true,"family":"Klein","given":"Douglas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":205514,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31270,"text":"ofr2001135 - 2001 - Basin-centered gas systems of the U.S.","interactions":[],"lastModifiedDate":"2021-11-23T23:24:02.073468","indexId":"ofr2001135","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-135","title":"Basin-centered gas systems of the U.S.","docAbstract":"Basin-center accumulations, a type of continuous accumulation, have spatial dimensions equal to or exceeding those of conventional oil and gas accumulations, but unlike conventional fields, cannot be represented in terms of discrete, countable units delineated by downdip hydrocarbon-water contacts. Common geologic and production characteristics of continuous accumulations include their occurrence downdip from water-saturated rocks, lack of traditional trap or seal, relatively low matrix permeability, abnormal pressures (high or low), local interbedded source rocks, large in-place hydrocarbon volumes, and low recovery factors.\r\n\r\nThe U.S. Geological Survey, in cooperation with the U.S. Department of Energy, National Energy Technology Laboratory, Morgantown, West Virginia, is currently re-evaluating the resource potential of basin-center gas accumulations in the U.S. in light of changing geologic perceptions about these accumulations (such as the role of subtle structures to produce sweet spots), and the availability of new data. Better geologic understanding of basin-center gas accumulations could result in new plays or revised plays relative to those of the U.S. Geological Survey 1995 National Assessment (Gautier and others, 1995).\r\n\r\nFor this study, 33 potential basin-center gas accumulations throughout the U.S. were identified and characterized based on data from the published literature and from well and reservoir databases (Figure 1). However, well-known or established basin-center accumulations such as the Green River Basin, the Uinta Basin, and the Piceance Basin are not addressed in this study.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2001135","usgsCitation":"Popov, M.A., Nuccio, V.F., Dyman, T.S., Gognat, T.A., Johnson, R.C., Schmoker, J.W., Wilson, M.S., and Bartberger, C.E., 2001, Basin-centered gas systems of the U.S.: U.S. Geological Survey Open-File Report 2001-135, 506 p., https://doi.org/10.3133/ofr2001135.","productDescription":"506 p.","temporalStart":"1998-04-01","temporalEnd":"2000-11-30","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":392085,"rank":3,"type":{"id":36,"text":"NGMDB Index 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