Description
Pink Agate Slice (2.5–3″) – Banded Quartz Mineral Specimen
This Pink Agate Slice measuring approximately 2.5–3 inches is a genuine quartz mineral specimen, cut and polished to reveal its beautiful banded structure and distinctive colour. Carefully selected for its pattern clarity and visual appeal, this piece offers a striking example of layered chalcedony formation. The photograph shows the exact specimen you will receive. Please refer to the listing photos for full sizing and scale.
This crystal is a genuine specimen and includes a Certificate of Authenticity lifetime guarantee generic card.
Mineral Type & Scientific Classification
Agate is a variety of Chalcedony, which is a microcrystalline form of Quartz (SiO₂ – silicon dioxide). It belongs to the tectosilicate mineral group and crystallises in the trigonal crystal system, although the crystal fibres are microscopic and tightly intergrown rather than forming large visible crystals.
The microcrystalline composition gives Agate its smooth texture, dense structure, and ability to take a high polish. With a Mohs hardness of approximately 6.5–7, Agate is durable and well-suited for display, collection, and decorative use.
Pink Colouration & Banding Characteristics
This Agate slice displays pink tones layered within natural banding patterns. Agate’s characteristic bands form through rhythmic silica deposition inside volcanic cavities. In pink varieties, colour may result from trace mineral inclusions or, in some cases, enhancement through dyeing to intensify the hue. The layered structure remains natural chalcedony quartz regardless of colour intensity.
Banding may appear as:
• Concentric rings
• Fortification-style angular patterns
• Flowing layered structures
• Semi-translucent and opaque zones
Some areas may allow light to pass through thinner sections, highlighting the internal layering, while denser bands remain more opaque. Each slice is unique in pattern distribution and tonal variation.
Geological Formation
Agate forms primarily in volcanic environments, especially within basaltic lava flows. As lava cools, trapped gas bubbles create cavities known as vesicles. Over time, silica-rich groundwater enters these cavities and deposits successive layers of microcrystalline quartz.
Changes in mineral chemistry, temperature, and pressure during deposition create the distinctive layered bands. Over millions of years, these deposits solidify into nodules, which are later cut and sliced to reveal the intricate internal structure.
Some Agate nodules may contain crystalline quartz centres, though many slices are fully composed of banded chalcedony.
Cut, Finish & Display Use
This Agate has been sliced to expose its internal banding and polished on both flat faces to enhance colour contrast and pattern visibility. The outer edge may retain a natural contour, reflecting the original nodule form.
Agate slices are popular as:
• Mineral and crystal display pieces
• Decorative home or office accents
• Educational geological specimens
• Collector’s quartz variety examples
• Unique natural gifts
Pink Agate is traditionally associated with love and emotional balance in spiritual symbolism. These associations are cultural and symbolic rather than scientific.
Authenticity & Individual Selection
• Genuine Agate (Chalcedony – Quartz SiO₂)
• Mineral class: Tectosilicate
• Microcrystalline quartz structure
• Natural banded formation
• Size: Approximately 2.5–3 inches
• Exact specimen shown in photographs
• Includes Certificate of Authenticity lifetime guarantee generic card
Formed through volcanic and hydrothermal processes over extensive geological timescales, this Pink Agate slice represents a distinctive and collectible example of banded quartz mineralisation.






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