Article: Geology of the parliament buildings 6. Geology of the British Columbia parliament buildings, Victoria.(SERIES)(Report)

SUMMARY

The British Columbia parliament buildings were constructed in two stages: the first building was started in 1893 and officially opened in 1898; the addition was started in 1912 and completed in 1915. The primary external building stone is a fine-grained, light grey, dacitic volcanic rock, commonly called Haddington Island andesite. The foundation and lower courses are medium-grained, grey, salt-and-pepper granodiorite, called Nelson Island granite. The Haddington Island andesite was also used for exterior architectural ornaments and statues. A variety of marbles from the USA and Italy decorate the interior of the buildings. Several monuments and fountains ...

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