Slag Hill: Difference between revisions
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'''Slag Hill''' is a [[subglacial volcano|subglacial mound]] in the [[Mount Cayley|Mount Cayley Volcanic Field]] in [[British Columbia]], [[Canada]]. It consists of glassy, [[augite]]-phyric [[basalt]]ic [[andesite]] in steep-sided, glassy, finely jointed domes and one small, flat-topped [[bluff]]. The finely jointed domes are similar to those of [[Ember Ridge]]. There are quench features at Slag Hill, which is suggesting that the volcanic activity was [[subglacial eruption|subglacial]]. It is believed Slag Hill last erupted in the Pleistocene age.<ref>[http://gsc.nrcan.gc.ca/volcanoes/cat/volcano_e.php?id=gvb_shl_021 Catalogue of Canadian Volcanoes] Retrieved on [[2007-05-28]] </ref> |
'''Slag Hill''' is a [[subglacial volcano|subglacial mound]] in the [[Mount Cayley|Mount Cayley Volcanic Field]] in [[British Columbia]], [[Canada]]. It consists of glassy, [[augite]]-phyric [[basalt]]ic [[andesite]] in steep-sided, glassy, finely jointed domes and one small, flat-topped [[Hill|bluff]]. The finely jointed domes are similar to those of [[Ember Ridge]]. There are quench features at Slag Hill, which is suggesting that the volcanic activity was [[subglacial eruption|subglacial]]. It is believed Slag Hill last erupted in the Pleistocene age.<ref>[http://gsc.nrcan.gc.ca/volcanoes/cat/volcano_e.php?id=gvb_shl_021 Catalogue of Canadian Volcanoes] Retrieved on [[2007-05-28]] </ref> |
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==References== |
==References== |
Revision as of 21:55, 5 July 2007
Slag Hill is a subglacial mound in the Mount Cayley Volcanic Field in British Columbia, Canada. It consists of glassy, augite-phyric basaltic andesite in steep-sided, glassy, finely jointed domes and one small, flat-topped bluff. The finely jointed domes are similar to those of Ember Ridge. There are quench features at Slag Hill, which is suggesting that the volcanic activity was subglacial. It is believed Slag Hill last erupted in the Pleistocene age.[1]
References
- ^ Catalogue of Canadian Volcanoes Retrieved on 2007-05-28