File:Folded-faulted banded iron formation (Temagami Iron-Formation, Neoarchean, ~2.736 Ga; Temagami North roadcut, Temagami, Ontario, Canada) 23 (46899078415).jpg
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[edit]DescriptionFolded-faulted banded iron formation (Temagami Iron-Formation, Neoarchean, ~2.736 Ga; Temagami North roadcut, Temagami, Ontario, Canada) 23 (46899078415).jpg |
Folded-faulted magnetite-quartz banded iron formation in the Precambrian of Ontario, Canada. Whitish = quartz-rich Dark gray = magnetite-rich The outcrop seen here consists of BIFs - banded iron formations. BIFs are unusual, dense sedimentary rocks consisting of alternating layers of iron-rich oxides and iron-rich silicates. Most BIFs are Proterozoic in age (although some are Late Archean), and do not form today - they're “extinct”! Many specific varieties of iron formation are known, and some are given special rock names. For example, jaspilite is an attractive reddish & silvery gray banded rock consisting of hematite, red chert (“jasper”), and specular hematite or magnetite. This outcrop has magnetite-quartz BIF. Because of their age, most BIFs have been around long enough to have been subjected to one or more orogenic (mountain-building) events. As such, most BIFs are folded, faulted, and/or metamorphosed to varying degrees. BIFs are known from around the world, but some of the most famous & extensive BIF deposits are found in the vicinity of North America’s Lake Superior Basin. Many BIFs have economic concentrations of iron and are mined. BIFs are the most important variety of iron ore on Earth. The rocks at this locality have small-scale folds and faults. Published literature refers to the folding here as soft-sediment deformation. The outcrop surface here was glacially eroded and smoothed during the Pleistocene Ice Age. Stratigraphy: Temagami Iron-Formation, lower Neoarchean, ~2.736 Ga Locality: Temagami North Outcrop - roadcut on the eastern side of Route 11, immediately north of town of Temagami, eastern Ontario, southeastern Canada (47° 04’ 08.32” North latitude, 79° 47’ 25.34” West longitude) |
Date | |
Source | Folded-faulted banded iron formation (Temagami Iron-Formation, Neoarchean, ~2.736 Ga; Temagami North roadcut, Temagami, Ontario, Canada) 23 |
Author | James St. John |
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/46899078415 (archive). It was reviewed on 10 October 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
10 October 2019
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current | 00:46, 10 October 2019 | 4,000 × 3,000 (9.65 MB) | Ser Amantio di Nicolao (talk | contribs) | Transferred from Flickr via #flickr2commons |
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Date and time of data generation | 08:46, 15 July 2012 |
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File change date and time | 23:30, 9 May 2019 |
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Exif version | 2.21 |
Date and time of digitizing | 08:46, 15 July 2012 |
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Date metadata was last modified | 19:30, 9 May 2019 |
Unique ID of original document | EB98A548AB6ACB2B6E70AC54523B92DF |