Talk:Newark Supergroup

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Untitled

Inexpertly, many of the magmatic provinces, associated with the rifting breakup of Pangea c.260-200Ma, occurred at the foothills of mountains uplifted, during the prior assembly of Pangea. For example, the Urals were uplifted c.300-250Ma by the collision of Baltica and Siberia; then the Siberian traps eruptions occurred along the Siberian foothills of those very mountains. Likewise, the Appalachians were uplifted during the collision of North America and Gondwana c.350-250Ma; then the Central Atlantic Magmatic Province erupted, along the same suture. Ipso facto, plates join & rift along similar axes (?).66.235.38.214 (talk) 19:05, 26 October 2012 (UTC)[reply]

Rename to Supergroup

I've been working on the Falling Creek Formation, which led me to create the Taylorsville Basin and I noticed that when I linked 'Newark Supergroup' it redirected to 'Newark Group'. This entry for Newark in the USGS GEOLEX database shows that the Group was renamed to Supergroup some time ago and on looking through GoogleScholar I notice that there is virtually no usage of 'Group' after the 1970s. I therefore propose that this article is renamed to 'Newark Supergroup' as I believe that is unequivocally current usage. Mikenorton (talk) 14:30, 24 November 2012 (UTC)[reply]

External links modified

Hello fellow Wikipedians,

I have just added archive links to one external link on Newark Supergroup. Please take a moment to review my edit. If necessary, add {{cbignore}} after the link to keep me from modifying it. Alternatively, you can add {{nobots|deny=InternetArchiveBot}} to keep me off the page altogether. I made the following changes:

Added archive https://web.archive.org/20050217093417/http://www.geowords.com:80/histbooknetscape/g22.htm to http://geowords.com/histbooknetscape/g22.htm

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