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dc.contributor.authorJoseph, P.E.
dc.date.accessioned2018-09-29T02:13:56Z
dc.date.available2018-09-29T02:13:56Z
dc.date.issued1916-12-12
dc.identifier.urihttp://hdl.handle.net/10150/629795
dc.descriptionWith the exception of aluminum, iron is the most abundant metallic element constituting the earth's crust. According to Clarke, the average of analyses of igneous rocks made in the laboratories of the United States Geological Survey showed 4.47 per cent iron. It occurs in nature native and in many compounds, giving rise to numerous minerals. Its most important ores are hematite, limonite, magnetite, and siderite. Goethite and turgite are commercially included with limonite under the name of brown hematite. 13 p.
dc.language.isoen
dc.publisherUniversity of Arizona Bureau of Mines
dc.relation.ispartofseriesBulletin No. 43
dc.relation.ispartofseriesMineral Technology Series No. 15
dc.relation.urlhttps://library.azgs.arizona.edu/item/AGSB-1552427060347-890
dc.rightsPublic Domain: This material has been identified as being free of known restrictions under U.S. copyright law, including all related and neighboring rights.
dc.subjectArizona Geological Survey Bulletins
dc.subjectRecent
dc.subjectUnited States of America
dc.subjectcommercial interests
dc.subjectiron ore
dc.subjectturgite
dc.subjectgoethite
dc.subjectsiderite
dc.subjectmagnetite
dc.subjectlimonite
dc.subjecthematite
dc.subjectmetallic element
dc.subjectMetal
dc.subjectiron
dc.titleIron
csdgm.bounding.west-125.332
csdgm.bounding.east-68.2031
csdgm.bounding.north48.9967
csdgm.bounding.south25.1084
dc.description.collectioninformationDocuments in the AZGS Document Repository collection are made available by the Arizona Geological Survey (AZGS) and the University Libraries at the University of Arizona. For more information about items in this collection, please contact azgs-info@email.arizona.edu.
refterms.dateFOA2018-09-29T02:13:56Z


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