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Heavitree stone is a type of red sandstone that was formerly quarried in the area and was used to construct many of Exeter's older buildings, including Exeter Guildhall. The Heavitree Gap , a pass through the MacDonnell Ranges in Australia, was named after Heavitree by the surveyor William Mills , [ 14 ] who had attended Heavitree School in England.
quality, with small bits of Heavitree Stone mixed in with inferior local material. Heavitree Stone in the 21st Century Although Heavitree Stone was a high-quality material, it is prone to weathering, after 800 years of exposure. Older buildings would've had no damp course, so water rises up from the ground, then oozes out and weathers it.
Heavitree Stone's heyday was in the 15th and 16th centuries. Churches dating from the period indicate that it was the preferred choice in Exeter. St Mary Steps is built from grand Heavitree Stone ashlar, as is St Stephen's, and the tower of St Martin's; Heavitree's St Clare's Chapel is a lovely example.
Heavitree stone is a type of breccia stone, red in colour, of very coarse texture [1] and prone to weathering, which occurs naturally in the parish of Heavitree near the City of Exeter in Devon, England.
Significantly, there is no Heavitree stone in their construction. Major quarrying of the distinctive red breccia known as Heavitree stone took place in nearby areas, including the parish of Heavitree from whence the stone derived its name, from the mid-14th century onwards.
Heavitree Stone is Exeter's stone. Many of its most interesting and historic buildings are built of it. It is a deep, Devonian red, with a character all its own. Q is for Quarries is an A-Z trail for mobiles. Click on the sites on the map and swipe through them to find out more. There are audio versions too. Please add your own comments and photos. Join us on a journey around the 'bullocks ...
Q Quarries. 1 April 2018. The Heavitree quarries are where our stories begin, in the Permian geological time period. Between 250 and 300 million years ago, Devon was a tropical desert. Occasional storms caused flash floods, which dumped large amounts of loose rock, sand and mud. Over time this gravelly sediment built up and was compacted together.
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