File:Ct farmington quarry.jpg
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Summary
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English: Farmington traprock quarry near Plainville, Connecticut. The quarry is mainly within basalt (‘traprock’) of the Talcott Formation of the Hartford Basin. This basalt is underlain by red siliciclastics of the Shuttle Meadow Formation. Both formations are lowest Jurassic in age and belong to the Newark Supergroup. |
| Date | |
| Source | Transferred from en.wikipedia to Commons. |
| Author | 5ju989nfhs50 at English Wikipedia (Paul Gagnon) |
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5ju989nfhs50 at English Wikipedia, the copyright holder of this work, hereby publishes it under the following licenses:
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Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License. |
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Original upload log
The original description page was here. All following user names refer to en.wikipedia.
- 2007-12-20 20:27 5ju989nfhs50 571×763× (451435 bytes) Traprock quarry near Plainville, Connecticut. 2000, Paul Gagnon
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 21:28, 25 August 2009 | | 571 × 763 (441 KB) | Gemini1980 | {{Information |Description={{en|Traprock quarry near Plainville, Connecticut. 2000, Paul Gagnon}} |Source=Transferred from [http://en.wikipedia.org en.wikipedia] |Date={{Date|2007|12|20}} (original upload date) |Author=Original uploader was [[:en:User:5ju |
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