The accompanying map shows the location of the principal deposits of titanium minerals in the United States (excluding Alaska and Hawaii). Four broad geologic categories of deposits have been distinguished on the map by the shapes of the symbols, and relative importance is indicated by their size. The smaller deposits and the deposits for which adequate data are lacking can only be rated as \"potential, unevaluated, or small\". The deposits placed in the next category have been characterized by modest production or can be described as having \"significant potential\". The larger deposits, for which, more information is available, arc divided into two categories, based on estimated production plus reserves: those containing 1,000,000 to 10,000,000 tons of TiO2, and those having more than 10,000,000 tons of TiO2.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mr29","usgsCitation":"Rogers, C.L., and Jaster, M.C., 1962, Titanium in the United States, exclusive of Alaska and Hawaii: U.S. Geological Survey Mineral Investigations Resource Map 29, Report: 18 p.; 1 Plate: 63.97 x 40.50 inches, https://doi.org/10.3133/mr29.","productDescription":"Report: 18 p.; 1 Plate: 63.97 x 40.50 inches","costCenters":[],"links":[{"id":180500,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mr/29/report-thumb.jpg"},{"id":486413,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mr/29/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":260488,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/29/plate-1.pdf"}],"scale":"3168000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.25,24.25 ], [ -127.25,49.25 ], [ -66.5,49.25 ], [ -66.5,24.25 ], [ -127.25,24.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699a4c","contributors":{"authors":[{"text":"Rogers, Cleaves Lincoln","contributorId":12858,"corporation":false,"usgs":true,"family":"Rogers","given":"Cleaves","email":"","middleInitial":"Lincoln","affiliations":[],"preferred":false,"id":266767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jaster, Marion Charlotte","contributorId":27117,"corporation":false,"usgs":true,"family":"Jaster","given":"Marion","email":"","middleInitial":"Charlotte","affiliations":[],"preferred":false,"id":266768,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36026,"text":"b1122E - 1962 - Geology and fluorspar deposits of the Levias-Keystone and Dike-Eaton areas, Crittenden County, Kentucky","interactions":[{"subject":{"id":55418,"text":"ofr4415 - 1944 - Preliminary notes on the geology of the Levias fault system, Crittenden County, Kentucky","indexId":"ofr4415","publicationYear":"1944","noYear":false,"title":"Preliminary notes on the geology of the Levias fault system, Crittenden County, Kentucky"},"predicate":"SUPERSEDED_BY","object":{"id":36026,"text":"b1122E - 1962 - Geology and fluorspar deposits of the Levias-Keystone and Dike-Eaton areas, Crittenden County, Kentucky","indexId":"b1122E","publicationYear":"1962","noYear":false,"chapter":"E","title":"Geology and fluorspar deposits of the Levias-Keystone and Dike-Eaton areas, Crittenden County, Kentucky"},"id":1}],"lastModifiedDate":"2022-07-22T18:41:11.031816","indexId":"b1122E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1122","chapter":"E","title":"Geology and fluorspar deposits of the Levias-Keystone and Dike-Eaton areas, Crittenden County, Kentucky","docAbstract":"The fault systems of the Levias-Keystone and Dike-Eaton areas, in the \r\nKentucky-Illinois fiuorspar district, are a complex northeastward-trending sys- \r\ntem and a simple northwestward-trending system of steeply dipping normal \r\nfaults, associated in part with a lamprophyre dike. Fluorspar mining started \r\nin the area about 1900 and, as of 1945, more than 200,000 tons of crude ore \r\nprobably has been mined; most of the ore was from the Levias-Keystone area. \r\nA small quantity of zinc and lead ore also is present in the Dike-Eaton area.\r\n\r\nThe deposits are localized along faults that displace fiat-lying or low-dipping \r\nlimestones, sandstones, and shales of the Meramec and Chester series of Missis- \r\nsippian age. Movement along most of the faults was principally vertical, with \r\ndisplacement as much as 600 feet. Some horizontal movement occurred along \r\nat least one fault. Geologic mapping of the surface and data from underground \r\nworkings have revealed 13 faults in an area of four-fifths of a square mile. \r\nOnly a few of these faults are known to contain economically important deposits \r\nof fiuorspar.\r\n\r\nThe most abundant vein minerals are calcite and fiuorite with subordinate \r\nquantities of sphalerite, galena, barite, and quartz. Some weathering products \r\nof sphalerite and galena are present also. The veins are dominantly calcite \r\nthat contains fiuorite lenses but in places are mainly fiuorite having lesser \r\nquantities of calcite. Sphalerite- and galena-bearing deposits are present in the Dike-Eaton area. The ore bodies mainly are the result of fissure filling and replacement of calcite by fiuorite; in addition a small amount of limestone \r\nwallrock probably has been replaced. Residual concentrations of high-grade \r\nfluorspar in the overburden above faults have yielded some so-called gravel \r\nfiuorspar. The position of the veins within the faults may be related to one \r\nor more factors such as type of wallrock, change in dip of the fault, and amount of displacement.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to Economic Geology (1960)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1122E","usgsCitation":"Trace, R.D., 1962, Geology and fluorspar deposits of the Levias-Keystone and Dike-Eaton areas, Crittenden County, Kentucky: U.S. Geological Survey Bulletin 1122, Report: iv, 26 p.; 4 Plates: 28.00 × 8.50 inches or smaller, https://doi.org/10.3133/b1122E.","productDescription":"Report: iv, 26 p.; 4 Plates: 28.00 × 8.50 inches or smaller","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":63975,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1122e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63974,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63973,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63972,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63971,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166770,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1122e/report-thumb.jpg"},{"id":109364,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20826.htm","linkFileType":{"id":5,"text":"html"},"description":"20826"}],"country":"United States","state":"Kentucky","county":"Crittenden County","otherGeospatial":"Levias-Keystone and Dike-Eaton areas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.204,\n 37.333\n ],\n [\n -88.153,\n 37.333\n ],\n [\n -88.153,\n 37.287\n ],\n [\n -88.204,\n 37.287\n ],\n [\n -88.204,\n 37.333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68663e","contributors":{"authors":[{"text":"Trace, Robert Denny","contributorId":53866,"corporation":false,"usgs":true,"family":"Trace","given":"Robert","email":"","middleInitial":"Denny","affiliations":[],"preferred":false,"id":215636,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13687,"text":"ofr6248 - 1962 - Bedrock geology of the Mount Carmel and Southington quadrangles, Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:06:55","indexId":"ofr6248","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-48","title":"Bedrock geology of the Mount Carmel and Southington quadrangles, Connecticut","docAbstract":"New data concerning the geologic structure, stratigraphy, petrography, origin, and ages of bedrock formations in an area of approximately 111 square miles in south-central Connecticut were obtained in the course of detailed geologic mapping from 1957 to 1960. Mapping was done at a scale of 1:24,000 on topographic base maps having a 10-foot contour interval.\r\n\r\nBedrock formations are classified in two principal categories. The first includes metasedimentary, meta-igneous, and igneous rocks of Precambrian to Devonian age, which crop out in the western parts of both quadrangles. The second includes sedimentary and igneous rocks of the Newark Group of Late Triassic age, which crop out in the eastern parts of the quadrangles. Diabase dikes, which are Late Triassic or younger in age, intruded rocks in both the western and eastern parts of the map area.\r\n\r\nRocks in the western part of the area underwent progressive regional metamorphism in Middle to Late Devonian time. The arrangement of the chlorite, garnet, biotite, staurolite, and kyanite zones here is approximately the mirror-image of metamorphic zones in Dutchess County, New York. However, garnet appeared before biotite in politic rocks in the map area, because the ration MgO/FeO is low.\r\n\r\nWaterbury Gneiss and the intrusive Woodtick Gneiss are parts of a basement complex of Precambrian age, which forms the core of the Waterbury dome. This structure is near the southern end of a line of similar domes that lie along the crest of a geanticline east of the Green Mountain anticlinorium. The Waterbury Gneiss is believed to have been metamorphosed in Precambrian time as well as in Paleozoic time. The Woodtick Gneiss also may have been metamorphosed more than once.\r\n\r\nIn Paleozoic time, sediments were deposited in geosynclines during two main cycles of sedimentation. The Straits, Southington Mountain, and Derby Hill Schists, which range in age from Cambrian to Ordovician, reflect a transition from relatively clean politic sediments to thinly layered sediments that contained rather high percentages of fine-grained volcanic debris. Metadiabase and metabasalt extrusives above Derby Hill Schist south of the map area represent more intense volcanic activity before or during the early stages of the Taconic disturbance in Late Ordovician time. Impure argillaceous, siliceous, and minor calcareous sediments of the Wepawaug Schist, which is Silurian and Devonian in age, were deposited unconformably on older rocks during renewed subsidence of a geosyncline. The Wepawaug now occupies the trough of a tight syncline, which formed before and during progressive regional metamorphism at the time of the Acadian orogeny in middle to Late Devonian time.\r\n\r\nFelsic igneous rocks were intruded into the metasedimentary formations of Paleozoic age before the climax of the latest progressive regional metamorphism. Intrusives that gave rise to the Prospect and Ansonia Gneisses were emplaced mainly in the Southington Mountain Schist, and the igneous rocks as well as the host rocks were metamorphosed in the staurolite zone. Although it is possible that these two intrusives were emplaced during the Taconic disturbance, the writer believes it more likely that the igneous rocks from which the Prospect and Ansonia Gneisses formed were emplaced during the Acadian orogeny. Woodbridge Granite, which intruded the Wepawaug Schist, is Devonian in age and undoubtedly was emplaced during the Acadian orogeny. In this area the granite is essentially unmetamorphosed, because it is in the chlorite, garnet, and biotite zones. Southwest of the map area, however, metamorphic equivalents of the Woodbridge are found in Wepawaug Schist in the staurolite zone. The Ansonia Gneiss, therefore, may be a metamorphic equivalent of the Woodbridge Granite.\r\n\r\nRocks of Late Triassic age formerly covered the entire map area, but were eroded from the western part after tilting and faulting in Late Triassic time. The New Haven Arkose of the Newark ","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6248","usgsCitation":"Fritts, C.E., 1962, Bedrock geology of the Mount Carmel and Southington quadrangles, Connecticut: U.S. Geological Survey Open-File Report 62-48, 161 p. ill., maps (some col.) ;30 cm., https://doi.org/10.3133/ofr6248.","productDescription":"161 p. ill., maps (some col.) ;30 cm.","costCenters":[],"links":[{"id":147018,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0048/report-thumb.jpg"},{"id":42237,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42238,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42239,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42240,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42241,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42242,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42243,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42244,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0048/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42245,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0048/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db63404e","contributors":{"authors":[{"text":"Fritts, Crawford Ellswroth","contributorId":102087,"corporation":false,"usgs":true,"family":"Fritts","given":"Crawford","email":"","middleInitial":"Ellswroth","affiliations":[],"preferred":false,"id":168232,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64962,"text":"i356 - 1962 - Preliminary geologic map of the Valdez-Tiekel Belt, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:13:13","indexId":"i356","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"356","subseriesTitle":"NONE","title":"Preliminary geologic map of the Valdez-Tiekel Belt, Alaska","language":"ENGLISH","doi":"10.3133/i356","usgsCitation":"Coulter, H., and Coulter, E., 1962, Preliminary geologic map of the Valdez-Tiekel Belt, Alaska: U.S. Geological Survey IMAP 356, 1 map ;59 x 63 cm. folded in envelope 31 x 24 cm., https://doi.org/10.3133/i356.","productDescription":"1 map ;59 x 63 cm. folded in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":111250,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/13608","linkFileType":{"id":5,"text":"html"}},{"id":254835,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0356/plate-1.pdf","size":"15848","linkFileType":{"id":1,"text":"pdf"}},{"id":254836,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0356/report.pdf","size":"31","linkFileType":{"id":1,"text":"pdf"}},{"id":254837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0356/report-thumb.jpg"}],"scale":"96000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aa54","contributors":{"authors":[{"text":"Coulter, H.W.","contributorId":34490,"corporation":false,"usgs":true,"family":"Coulter","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":272429,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coulter, E.B.","contributorId":78811,"corporation":false,"usgs":true,"family":"Coulter","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":272430,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":62113,"text":"gq154 - 1962 - Geology of the Marysvale quadrangle, Utah","interactions":[{"subject":{"id":42893,"text":"ofr58110 - 1958 - Preliminary geologic map of the Marysvale quadrangle, Piute County, Utah","indexId":"ofr58110","publicationYear":"1958","noYear":false,"title":"Preliminary geologic map of the Marysvale quadrangle, Piute County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":62113,"text":"gq154 - 1962 - Geology of the Marysvale quadrangle, Utah","indexId":"gq154","publicationYear":"1962","noYear":false,"title":"Geology of the Marysvale quadrangle, Utah"},"id":1},{"subject":{"id":46977,"text":"ofr5017 - 1950 - Geologic map of the Marysvale area, Utah","indexId":"ofr5017","publicationYear":"1950","noYear":false,"title":"Geologic map of the Marysvale area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":62113,"text":"gq154 - 1962 - Geology of the Marysvale quadrangle, Utah","indexId":"gq154","publicationYear":"1962","noYear":false,"title":"Geology of the Marysvale quadrangle, Utah"},"id":2}],"lastModifiedDate":"2021-11-10T20:36:08.647995","indexId":"gq154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"154","title":"Geology of the Marysvale quadrangle, Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq154","usgsCitation":"Willard, M.E., and Callaghan, E., 1962, Geology of the Marysvale quadrangle, Utah: U.S. Geological Survey Geologic Quadrangle 154, Report: 1 p.; Plate, https://doi.org/10.3133/gq154.","productDescription":"Report: 1 p.; Plate","costCenters":[],"links":[{"id":102154,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_603.htm","linkFileType":{"id":5,"text":"html"},"description":"603"},{"id":253204,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0154/report-thumb.jpg"},{"id":248310,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0154/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Utah","otherGeospatial":"Marysvale quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,38.25 ], [ -112.25,38.5 ], [ -112,38.5 ], [ -112,38.25 ], [ -112.25,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696c0c","contributors":{"authors":[{"text":"Willard, Max Emery","contributorId":46593,"corporation":false,"usgs":true,"family":"Willard","given":"Max","email":"","middleInitial":"Emery","affiliations":[],"preferred":false,"id":266929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Callaghan, Eugene","contributorId":79855,"corporation":false,"usgs":true,"family":"Callaghan","given":"Eugene","email":"","affiliations":[],"preferred":false,"id":266930,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5967,"text":"pp368 - 1962 - Geology and ore deposits of the Darwin quadrangle, Inyo County, California","interactions":[{"subject":{"id":13963,"text":"ofr5842 - 1958 - Structure and ore deposits of the Darwin quadrangle, Inyo County, California","indexId":"ofr5842","publicationYear":"1958","noYear":false,"title":"Structure and ore deposits of the Darwin quadrangle, Inyo County, California"},"predicate":"SUPERSEDED_BY","object":{"id":5967,"text":"pp368 - 1962 - Geology and ore deposits of the Darwin quadrangle, Inyo County, California","indexId":"pp368","publicationYear":"1962","noYear":false,"title":"Geology and ore deposits of the Darwin quadrangle, Inyo County, California"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:56","indexId":"pp368","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"368","title":"Geology and ore deposits of the Darwin quadrangle, Inyo County, California","language":"ENGLISH","publisher":"U.S. Govt. 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