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The Geology and Mining of Cligga Head - A Report by Jack Knight The Royal Geological Society of Cornwall, RGSC, organised a field trip on Saturday 12th August 2023 to Cligga Head, St Agnes, Cornwall, UK. The visit was all about the mining and minerals of Cligga Head and was led by Professor Frances Wall of the University of Exeter, Camborne School of Mines. Professor Frances led us on an exploration of the St Agnes Area of Outstanding Natural Beauty to explain what minerals are present, the geology and formation of the igneous rocks in the area and how the landscape was mined. Picture of Jack Knight on the left
Igneous Rocks and Greisens All rocks can be split into three categories: igneous, sedimentary and metamorphic. The rocks at Cligga Head are igneous, formed when molten magma intruded the Devonian clay slate country rock around 290 million years ago. The magma cooled five kilometres below the ground and formed a small coarse granite batholith (nearly two kilometres squared). The granite contains quartz, feldspars and micas. The micas are so abundant it is called ‘muscovite granite’. 15 million years later, water heated to around 200 to 400°C that was carrying the elements boron and fluorine, entered the granite through fissures (cracks in the rock). The heated water dissolved the feldspar in the granite which reacted with the other minerals in the fluids to form wolframite and cassiterite. This process is called greisenisation and is what forms the distinctive veins at Cligga Head. Left photo shows the Greisen veins and the right photo a closer view
The Mining Industry of Cligga Head Wolframite contains the rare metal tungsten whereas cassiterite contains tin. Both metals are important for industry, hence the mining at Cligga Head. The first location that Professor Frances took us to was the very windy remains of a 20th century building (left photo) and abandoned mineshaft (right photo). The building was an extraction and processing site for tungsten during the Second World War.
The wolframite (left photo) was mined from the Greisen and then crushed. The crushed dust was left to settle in the buddle tanks. This separated the heavy tungsten ore from the rest of the less dense minerals of the wolframite. Sometimes this process may have to have been repeated multiple times to extract the tungsten ore, which was very expensive and time consuming. The Cligga Head mine began decreasing production in 1944 when Britain started importing American tungsten, which was much cheaper than the tungsten produced at Cligga Head. Eventually after the war ended Cligga mine closed with a grand total of around 300 tons of tungsten produced.
The Granite Cliffs The next location that Professor Frances took us to was a perfect viewpoint of the granite and the Greisen veins (photos left and right). From where we stood we could see many adits in the cliff face demonstrating how vast the mine workings at Cligga were. It also showed how the greisenisation had affected all the granite of the area around Cligga Head with the unique landscape and excellent veins resulting in it being designated a Site of Special Scientific
The Elvan Dyke The final location that Professor Frances took us to was a small quarry. Here a dyke had intruded the metasediments of the surrounding country rock. The dyke comprises a fine grained rock called quartz porphyry, which has a composition much like granite. Elvan is a Cornish word that means a rock that is very good for building material. In contrast to Cligga Head, which had been mined for minerals, this dyke had been quarried for building stone. On breaking an elvan specimen with a piece of rock as a hammer we were able to see the fine grained quartz crystals. These quartz crystals make up the majority of the minerals in the elvan dyke. After seeing the fine grained elvan, Professor Frances asked us to examine the margin between the dyke and the rock above it (right photo). The rock had some joints and looked like the same slaty rock that made up the rest of the country rock. Then Professor Frances asked us whether the rock had been baked when the dyke intruded or was deposited there after the dyke had cooled and been eroded. On closer examination of the margin I believed it had been baked as the dyke appeared to have finer grains next to the boundary. This implied that when it had intruded, the outer edge of the dyke had cooled quicker on the colder country rock forming a chilled margin in the dyke and a baked margin on the country rock. Conclusion I would like to thank Professor Frances Wall for leading this fascinating field trip and the Royal Geological Society of Cornwall for arranging and organising the event. I learned so much I never knew about minerals and mining during this trip and it showed me how much there is to discover in the ever-growing field of geology. I highly suggest that you join your local geological society for the engaging and eye-opening content from field trips and talks.
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