Milky Quartz Crystal Cluster | Rostowrack China Clay Pit, Cornwall |  No. 3

Milky Quartz Crystal Cluster | Rostowrack China Clay Pit, Cornwall | No. 3

£9.00
Sale price  £9.00 Regular price 
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Milky Quartz Crystal Cluster | Rostowrack China Clay Pit, Cornwall |  No. 3
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Milky Quartz Crystal Cluster | Rostowrack China Clay Pit, Cornwall | No. 3

£9.00
Sale price  £9.00 Regular price 
Product Information

A charming 45g Cornish milky quartz specimen featuring translucent white crystals, delicate champagne and blush-pink tones, and subtle iron-rich mineral staining, originating from Rostowrack China Clay Pit at Hendra Downs, near St Dennis, Cornwall.

This compact natural specimen displays an attractive combination of crystalline quartz growth, delicate mineral textures and the geological character of Cornwall's historic china clay district.

Specimen Description

This beautiful small specimen features a naturally irregular formation of milky quartz, with numerous intergrown crystals covering its exposed surfaces.

The most distinctive feature is a cluster of translucent quartz crystals extending from one side of the specimen. These display softly defined crystal faces, delicate glassy reflections and pale champagne colouration.

Some of the more prominent crystals exhibit well-developed terminations, while smaller crystals grow closely together across the surrounding surface.

The main body of the specimen displays a mixture of creamy-white and very pale blush-pink quartz, creating a subtle contrast between the more translucent crystal points and the denser, milky crystalline material.

Fine reddish-brown mineral staining is visible along several natural layers and fractures, adding warm earthy tones to the otherwise pale formation.

These coloured areas are consistent with iron-bearing mineral staining, although the precise mineral responsible has not been independently identified.

A small natural opening between the larger crystal formations provides additional depth and reveals the closely intergrown crystalline structure.

The reverse displays a more compact mineral surface, with delicate pinkish-beige tones and subtle variations in texture.

Despite its smaller size, this specimen offers plenty of interesting geological detail, particularly when examined closely under natural light.

Weighing 45g and measuring approximately 38.2mm × 50.7mm, it makes an attractive addition to a collection of Cornish minerals, British quartz specimens or smaller natural crystal formations.

About the Mineral

Quartz (SiO₂) is a silicon dioxide mineral belonging to the trigonal crystal system, with a Mohs hardness of 7.

Quartz is one of the most abundant minerals in the Earth's continental crust and occurs in a wide variety of geological environments.

It commonly forms when silica-rich fluids circulate through fractures, veins and cavities within rocks, gradually depositing crystalline silica as geological conditions change.

Milky Quartz is a variety of quartz characterised by its cloudy white or translucent appearance.

The characteristic milkiness is commonly caused by microscopic fluid inclusions within the crystal structure, which scatter incoming light and reduce transparency.

Milky quartz may occur as massive deposits, individual crystals, crystal clusters and mineralised veins.

In this specimen, the quartz displays a combination of closely intergrown crystal points and denser milky crystalline material.

The delicate champagne and blush-pink tones visible across the specimen may reflect subtle mineral inclusions, staining or variations in the way light passes through the crystalline structure.

The reddish-brown areas are consistent with iron-bearing alteration products.

Iron oxides and oxyhydroxides, including hematite and goethite, can produce yellow, orange, pinkish-red and rusty-brown staining on quartz surfaces.

However, the precise composition of the coloured material within this individual specimen has not been laboratory verified.

Rostowrack China Clay Pit & Cornish Heritage

Rostowrack China Clay Pit is located at Hendra Downs, near St Dennis, within Cornwall's historically important St Austell granite district.

The St Austell granite is internationally recognised for its extensive deposits of kaolin, commonly known as china clay.

These deposits developed through the alteration of feldspar-bearing granite, producing kaolin-rich material that became an important industrial resource.

China clay extraction has played a significant role in Cornwall's industrial heritage, supplying raw materials for porcelain, ceramics, paper manufacturing and other industries.

Unlike Cornwall's famous tin and copper mines, china clay workings concentrated on extracting altered granite rather than metallic ores.

However, the geological processes affecting the St Austell granite also produced quartz veins, mineralised fractures and a variety of associated mineral occurrences.

Rostowrack is particularly interesting because its exposed geological formations have been documented in published geological field studies.

In 1995, geologists C. M. Bristow and J. H. Howe published an account of a field excursion examining the Fal Valley and western St Austell granite.

Their report includes Rostowrack China Stone Quarry and China Clay Pit, documenting altered granite and quartz vein mineralisation.

Further geological documentation published for EUROGRANITES 2014 describes Rostowrack as an important exposure of topaz-bearing granite affected by structurally controlled kaolinisation.

The field guide also records a prominent multistage quartz-hematite vein within the Rostowrack workings.

This documented association of quartz and iron-bearing mineralisation provides useful geological context for specimens displaying quartz crystallisation and iron-rich staining.

Mineralogical locality records document quartz, hematite, fluorite, kaolinite and other minerals from Rostowrack.

These occurrences reflect the complex geological processes that affected the granite and its associated mineralised structures.

Rostowrack also has historical connections with Cornwall's china stone industry.

China stone, a feldspar-bearing granitic material, was historically used alongside china clay in the manufacture of porcelain and other ceramic products.

The Wheal Martyn Trust preserves and interprets the industrial heritage of Cornwall's china clay district.

Specimens attributed to Rostowrack therefore offer an interesting connection to both Cornwall's geological history and its important china clay industry.

Intention & Associated Chakras

In traditional crystal healing practices, milky quartz is associated with gentle, balancing and restorative symbolic qualities.

  • Clarity: Traditionally associated with clear thinking, reflection and mental focus.
  • Calm: Symbolically connected with emotional balance, tranquillity and peaceful surroundings.
  • Spiritual Growth: Associated with personal awareness, reflection and the exploration of intention.
  • Protection: Traditionally used as a symbolic reminder of stability and energetic boundaries.

Associated Chakras: Crown Chakra and Root Chakra.

Intention: Calm and Spiritual Growth.

These associations belong to crystal healing traditions and are not scientifically established properties of quartz.

Natural Formation & Symbolism

As a naturally formed raw quartz specimen, this piece retains its irregular shape, exposed crystalline surfaces and subtle mineral staining.

The closely intergrown quartz crystals provide a beautiful example of natural crystallisation, with individual points developing alongside one another to create a complex textured formation.

The combination of milky-white crystals, delicate blush-pink tones and earthy mineral staining creates a soft, understated appearance.

Raw quartz formations are traditionally associated with authenticity, clarity and connection to the natural world.

The pale crystalline surfaces can be interpreted symbolically as representing renewal and clarity, while the natural iron-rich staining provides a visual connection to grounding and stability.

Beyond its symbolic associations, this specimen is an appealing natural geological object, particularly for collectors interested in Cornwall's mineralogical and industrial heritage.

Specimen Details

  • Mineral: Milky Quartz
  • Chemical Formula: SiO₂
  • Crystal System: Trigonal
  • Mohs Hardness: 7
  • Mine: Rostowrack China Clay Pit
  • Locality: Hendra Downs, St Dennis, Cornwall, England
  • Weight: 45g
  • Measurements: 38.2mm × 50.7mm
  • Formation: Natural raw quartz cluster with intergrown crystals
  • Colour: Milky white, cream, translucent champagne and pale blush pink
  • Associated Features: Subtle iron-rich mineral staining and natural crystalline matrix
  • Finish: Natural, unpolished
  • Condition: Natural crystalline surfaces, irregular edges, mineral staining and visible geological textures
  • Quantity: One individual specimen

You will receive the exact specimen photographed. Natural mineral specimens may contain fractures, uneven surfaces, delicate crystal points, inclusions and variations resulting from their geological formation.

Wooden display plinth and decorative flowers shown in the photographs are not included.

Sources & References

The following resources provide geological, mineralogical and historical information relating to Rostowrack China Clay Pit and the surrounding St Austell granite district:

  1. Mindat – Rostowrack China Clay Pit, Cornwall. Mineral locality database documenting the locality and recorded mineral occurrences, including quartz and hematite.
  2. Bristow & Howe (1995) – Field Excursion to the Fal Valley, Western St Austell Granite. Geological field account describing Rostowrack, altered granite and quartz vein mineralisation.
  3. EUROGRANITES 2014 – Granites and Mineralisation of South West England. Geological field guide discussing Rostowrack's kaolinised granite, multistage quartz-hematite vein and associated mineralisation.
  4. Wheal Martyn Trust – China Stone. Museum resource documenting Cornwall's china stone heritage and its relationship with the china clay industry.

Historical and geological references relate to the recorded Rostowrack locality. The provenance of this individual specimen is based on supplied collection information. The mineral identification and precise composition of the coloured staining have not been independently laboratory verified.

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