The flagship Helman Tor Reserve. © Ilaria Selvaggio / Selvaic

Geological nature reserves

Cornwall Wildlife Trust has two geological nature reserves in Cornwall, St Erth Pits Nature Reserve and Tresayes Quarry Nature Reserve. Many of CWT's nature reserves (there are over fifty) have some geological interest: an example is the flagship Helman Tor Reserve (see image above, by Ilaria Selvaggio / Selvaic).

Geological nature reserves are sites that have been acquired or leased by Cornwall Wildlife Trust and are important for geological and biological reasons. They illustrate the close links that exist between the geology of an area and its wildlife habitats.

St Erth Pits Nature Reserve

St Erth Pits were originally worked for moulding sand and clay of Pliocene age. The St Erth Pits Nature Reserve is of national importance and this is recognised by its designation as a Site of Special Scientific Interest (SSSI). It provides evidence of the climate and geography of this part of west Cornwall some two million years ago when the sea level was about 45m higher than today and the sea water was slightly warmer. An information board about the site can be found on the wall of the Star Inn in the village of St Erth and a St Erth Pits Nature Reserve information leaflet is also available. The moulding sand was used by Harvey's of Hayle, and the clay was used for puddling the dry-dock in Penzance in 1834, and also by Bernard Leach who had his pottery in St Ives in the 20th century. Well-preserved fossil molluscs, foraminifera and ostracods were found in the clay, as well as plant material. The microfossil fauna is particularly diverse, reflecting the range of habitats from brackish to open marine. Only one of the pits at St Erth is now a CWT reserve - and only sand is found in it, and much of that is probably spoil. The Turritella gastropods in the clay beds are typically 5-7cm long while the ostracods and foraminifera are much smaller (e.g. Leptocythere sp - an ostracod - typically 0.4-0.8mm. There are fossils from St Erth on display in the Royal Cornwall Museum, Truro).

Molluscan fossils found in clay layers of the St Erth Beds, exploited for puddling clay in Victorian times. Scale bar: 1 cm

St Erth Pits info board outside the Star Inn. The lowest fossil is an ostracod of the genus Leptocythere - it is 0.4-0.8mm long. The clay was used in waterproofing ('puddling') the new dry-dock in Penzance in 1834; the Ross Bridge was installed in 1881 to allow access for ships to the dry-dock after the road was built across the mouth of the old harbour.

Tresayes Quarry Nature Reserve

Tresayes Quarry, also known as ‘the Glass Mine’, is an old feldspar working in a pegmatite vein in the metamorphic aureole of the St Austell granite. The feldspar was used in glazes for pottery and in the glass making industry and is reputed to have been used to make Spitfire windscreens during the war. The quarry is a County Geology Site and also an EarthCache (https://www.geocaching.com/geocache/GC32BDK_tresayes-quarry-roche-glass-mine).

The nature reserve has on-site interpretation panels that tell more about the exciting geology and history of this quarry. The site also features in the Roche Rock and the Tresayes Trail leaflet. The quarry is now a wetland - with a boardwalk to take you dry-footed (at most times!) to the quarry face.

Tresayes Quarry. © Neil Lindsay

Tresayes Quarry. © Neil Lindsay

Other nature reserves with geological interest

Several other Cornwall Wildlife Trust nature reserves have geological interest, although this is not the main reason for their designation. These include Baker's Pit Nature Reserve near St Ives, Churchtown Farm Community Nature Reserve in Saltash, Ropehaven Cliffs Nature Reserve near St Austell and North Predannack Downs Nature Reserve and Windmill Farm Nature Reserve on The Lizard. But one of the prime geological sites in a larger reserve is the granite Helman Tor, rising up out of a post-industrial landscape due to tin-streaming, Helman Tor is a County Geology Site, and also now included in the Mid Cornwall Moors SSSI.

Baker's Pit is a disused claypit, Churchtown Farm has a couple of County Geology Sites, both disused quarries (for dolerite and low-grade slate), Ropehaven has old quarries too and, unusually, thin limestones in its Lower Devonian slates. Both North Predannack and Windmill Hill are mostly on serpentine.