About: Hampton Park, New Zealand     Goto   Sponge   NotDistinct   Permalink

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Hampton Park is one of the volcanoes in the Auckland volcanic field. A small scoria cone reaching 35 metres (114 ft 10 in) above sea level, with a shallow crater around 50 metres (164 ft 1 in) wide, which has been modified by quarrying. The scoria cone sits in the centre of a much larger explosion crater, the eastern arc of the surrounding tuff ring is still present. Stone from the volcano was used to build dry-stone walls and the nearby St John's Church built on the tuff ring crest.

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  • Hampton Park, New Zealand (en)
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  • Hampton Park is one of the volcanoes in the Auckland volcanic field. A small scoria cone reaching 35 metres (114 ft 10 in) above sea level, with a shallow crater around 50 metres (164 ft 1 in) wide, which has been modified by quarrying. The scoria cone sits in the centre of a much larger explosion crater, the eastern arc of the surrounding tuff ring is still present. Stone from the volcano was used to build dry-stone walls and the nearby St John's Church built on the tuff ring crest. (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Hampton_Park_scoria_cone_Auckland.jpg
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  • -36.950925 174.89544
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  • Hampton Park is one of the volcanoes in the Auckland volcanic field. A small scoria cone reaching 35 metres (114 ft 10 in) above sea level, with a shallow crater around 50 metres (164 ft 1 in) wide, which has been modified by quarrying. The scoria cone sits in the centre of a much larger explosion crater, the eastern arc of the surrounding tuff ring is still present. Stone from the volcano was used to build dry-stone walls and the nearby St John's Church built on the tuff ring crest. (en)
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  • POINT(174.89544677734 -36.950923919678)
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