This article is within the scope of WikiProject Volcanoes, a collaborative effort to improve the coverage of volcanoes, volcanology, igneous petrology, and related subjects on Wikipedia. If you would like to participate, please visit the project page, where you can join the discussion and see a list of open tasks.VolcanoesWikipedia:WikiProject VolcanoesTemplate:WikiProject VolcanoesWikiProject Volcanoes articles
This article is within the scope of WikiProject Canada, a collaborative effort to improve the coverage of Canada on Wikipedia. If you would like to participate, please visit the project page, where you can join the discussion and see a list of open tasks.CanadaWikipedia:WikiProject CanadaTemplate:WikiProject CanadaCanada-related articles
Talk:Watts Point volcanic centre is part of WikiProject Geology, an attempt at creating a standardized, informative, comprehensive and easy-to-use geology resource. If you would like to participate, you can choose to edit this article, or visit the project page for more information.GeologyWikipedia:WikiProject GeologyTemplate:WikiProject GeologyGeology articles
If that's what it is, that's what it should be called; as with other parallels elsewhere, the name of this article currently refers to have a place. That it has a volcanic character can be mentioned as a geographic feature can be mentioned in the "place" article; if there's nothing else to encyclopedia about Watts Point e.g. re the highway, the railway, marine history, native culture, then this article's in need of a name change anyway; volcanic centre could use a definition too, since it obviously refers to something like a non-montane volcano - what do you call it, a subduction volcano? That is to say, a volcanic feature, though not a volcano.Skookum107:54, 18 January 2007 (UTC)[reply]
PS is tufa volcanic? - linking that so I can check it out. If it is there's a Rexmount Bluff in the Bridge River Country made out of the stuff (pic later).Skookum107:54, 18 January 2007 (UTC)[reply]
Aha it was tuff that I was thinking about, and that's what Rexmount Bluff is made out of. There's ash deposits throughout the upper Bridge basin, which I guess is where that came from, i.e the Bridge River cones, although this is a good sixty miles east, right under the west flank of the Shulaps Range, and quite a bit in the lower too, below the canyon; (canyon pic on Bridge River) makes me wonder about the conical shape of Rex Peak, and also Big Dog Mountain and Big Sheep Mountain in the [[Shulaps Range}Shulaps]]; and Poison Mountain and Red Mountain and....ever heard of Black Dome Mountain? linking that because there may be an article on it; it's some kind of chemical spring, maybe thermal, the last "peak" (summit really) in the Camelsfoot Range, in the angle of Churn Creek and the Fraser just by Big Bar Ferry; fossilized but something like an old geyser crystallization; staked out for some rare chemical in the mineral complex; google it for sure just out of interest; quite the curiosity; not as odd as the microbialitesinPavilion Lake, but getting up there.Skookum108:00, 18 January 2007 (UTC)[reply]
Done, though I haven't matched the precision of your coordinates, which are far too precise for a feature of this size. Deor (talk) 07:26, 5 November 2013 (UTC)[reply]