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Amethyst Crystal Point Brazil Natural Purple Quartz Mineral Terminated Crystal

Original price was: £10.20.Current price is: £9.18.

(Actual as seen)

Only 1 left in stock

SKU: RP0736 Category:

Description

Natural Amethyst Crystal Point from Brazil

This Amethyst Crystal Point is a natural quartz mineral specimen sourced from Brazil, one of the world’s most well-known regions for producing high-quality amethyst crystals. The specimen displays the distinctive purple coloration that makes amethyst one of the most recognisable varieties of quartz.

The crystal terminates in a natural point, formed during geological growth within mineral-rich cavities. Such points occur when crystal growth continues freely in open space, allowing the characteristic pyramidal termination faces to develop.

The listing photographs show the exact specimen you will receive, allowing collectors and buyers to clearly observe the colour, natural crystal form, and internal features before purchase.

This crystal is a genuine specimen and includes a Certificate of Authenticity lifetime guarantee generic card, confirming authenticity.

Please refer to the photographs for full sizing and scale.


Mineral Identification – Amethyst (Quartz Variety)

Amethyst is the purple variety of quartz, a silicon dioxide mineral that forms some of the most common and well-defined crystals in the Earth’s crust. Quartz belongs to the silicate mineral group and develops distinctive hexagonal crystal structures.

Key mineralogical details include:

  • Mineral Name: Quartz

  • Variety: Amethyst

  • Chemical Formula: SiO₂ (Silicon Dioxide)

  • Mineral Class: Silicate

  • Crystal System: Trigonal

  • Mohs Hardness: 7

  • Transparency: Transparent to translucent

  • Lustre: Vitreous

The purple colour seen in amethyst results from trace amounts of iron impurities within the quartz crystal lattice, combined with natural irradiation within the surrounding geological environment. This process alters the structure of the crystal and produces the violet colouration.


Geological Formation of Amethyst Crystals

Amethyst crystals commonly form within volcanic rock cavities, particularly inside geodes and vesicles in basaltic lava flows. When silica-rich fluids circulate through these cavities, quartz crystals begin to grow on the cavity walls.

Over long geological periods, successive layers of silica crystallise to form well-developed quartz crystals with sharply defined faces and pointed terminations. Iron present in the surrounding rock contributes to the purple coloration that distinguishes amethyst from other quartz varieties.

These environments typically form under hydrothermal conditions where mineral-rich fluids move through fractures and voids in volcanic rock.

Minerals commonly associated with amethyst deposits include:

  • Quartz varieties

  • Calcite

  • Chalcedony

  • Agate

  • Hematite

  • Goethite

These associated minerals reflect the chemical composition of the fluids present during crystal growth.


Brazilian Amethyst Deposits

Brazil is globally recognised for producing large quantities of high-quality amethyst. Major deposits occur in volcanic basalt formations in regions such as Rio Grande do Sul, Minas Gerais, and Bahia.

Brazilian amethyst often forms within large geodes where quartz crystals grow inward from the cavity walls. These geodes may contain clusters of crystals ranging from small points to large crystal groups.

Specimens from Brazil are valued for:

  • Strong purple colour tones

  • Well-formed crystal points

  • Natural geological formations

  • Consistent crystal quality

Brazil remains one of the primary global sources of natural amethyst mineral specimens.


Natural Crystal Form and Structure

This specimen features a natural crystal point, meaning the termination developed naturally during the crystal’s geological growth. Quartz crystals commonly display six-sided prism structures with pointed pyramid terminations.

Features that may be visible in natural amethyst crystals include:

  • Hexagonal crystal structure

  • Natural termination faces

  • Internal mineral inclusions

  • Colour zoning or banding

  • Slight natural surface variations

These characteristics are normal features of naturally formed quartz crystals and provide insight into the mineral’s formation history.


Mineral Collecting and Display

Amethyst crystal points are popular among mineral collectors due to their distinctive colour and well-defined crystal form. Natural points are particularly desirable because they demonstrate how quartz crystals develop within geological environments.

This specimen may be suitable for:

  • Mineral and crystal collections

  • Quartz variety collections

  • Geological study displays

  • Decorative mineral displays

  • Unique natural gift items

In some traditions, amethyst crystals have been traditionally associated with symbolic or spiritual interpretations, although these interpretations are belief-based rather than scientific descriptions.

Because the listing photographs show the actual specimen, collectors can purchase confidently knowing the exact crystal they will receive.


Authentic Natural Mineral Specimen

This Amethyst Crystal Point from Brazil is a genuine natural quartz mineral specimen carefully selected for its colour and crystal structure.

The specimen includes a Certificate of Authenticity lifetime guarantee generic card, confirming the authenticity of the mineral.

Please review the listing photographs for full sizing and scale, as they form part of the description and clearly show the exact specimen you will receive.

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