Basalt Headlands: Difference between revisions
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{{other uses|Basalt (disambiguation)}} |
{{other uses|Basalt (disambiguation)}} |
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The '''Basalt Headlands''' are a chain of intermittent high-cliffed bluffs and islands that fringe the northern edge of the [[Minas Basin]], [[Nova Scotia]], [[Canada]]. Its name comes from the [[basalt]]ic outcrops that formed about 200 million years ago when this region was volcanically active by [[continent]]ial [[rift]]ing.<ref>[http://www.fundyshoreecotour.ns.ca/eco04.htm Fundy Shore Ecotour, The Eco-Nones, The Basalt Headlands]</ref> |
The '''Basalt Headlands''' are a chain of intermittent high-cliffed bluffs and islands that fringe the northern edge of the [[Minas Basin]], [[Nova Scotia]], [[Canada]]. Its name comes from the [[basalt]]ic outcrops that formed about 200 million years ago when this region was volcanically active by [[continent]]ial [[rift]]ing.<ref>[http://www.fundyshoreecotour.ns.ca/eco04.htm Fundy Shore Ecotour, The Eco-Nones, The Basalt Headlands] {{wayback|url=http://www.fundyshoreecotour.ns.ca/eco04.htm |date=20080621055016 }}</ref> |
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==See also== |
==See also== |
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Revision as of 22:40, 27 October 2016
The Basalt Headlands are a chain of intermittent high-cliffed bluffs and islands that fringe the northern edge of the Minas Basin, Nova Scotia, Canada. Its name comes from the basaltic outcrops that formed about 200 million years ago when this region was volcanically active by continential rifting.[1]
See also
References
- ^ Fundy Shore Ecotour, The Eco-Nones, The Basalt Headlands Archived 2008-06-21 at the Wayback Machine
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