Pseudotachylyte Vredefort Impact Structure South Africa

Rare Pseudotachylyte Vredefort South Africa

Discover the extraordinary with this rare pseudotachylyte specimen from the renowned Vredefort Impact Structure, South Africa. Formed during the intense heat and pressure of an asteroid impact, pseudotachylyte is created by the immense kinetic energy released in such events. The temperatures are so extreme that they melt the target rocks, forming this rare and stunning material.

Why is Pseudotachylyte Special?

Pseudotachylyte is a significant marker used to identify and study impact structures. While it can also form through tectonic faulting, pseudotachylyte from impact craters is far less common, making it a coveted piece for geology enthusiasts.

Unique Visual and Scientific Appeal

The smooth, flowing textures and intricate vein patterns of pseudotachylyte provide insights into its formation under high-stress conditions. Flow bands, formed during rapid cooling and solidification, are a distinctive and fascinating feature.

Features of This Specimen

Key Highlights

• Distinct Flow Banding: Beautifully preserved textures showcasing rapid cooling processes.
• Metallic Inclusions: Tiny metallic features lining small crevices, adding unique visual interest.
• Exceptional Quality: Well-preserved veins from the world’s most famous impact site.

Specifications

Size: 75 mm (L) x 36 mm (W) x 14 mm (D)

Weight: 59 grams

What is Included?

• Certificate of Authenticity
• Informative tag and tag stand
• Detailed information about pseudotachylyte and its formation

Why Add This to Your Collection?

The Vredefort Impact Structure, the largest confirmed impact crater on Earth. This pseudotachylyte was legally collected by a geologist in 1998. Owning a pseudotachylyte from this site allows you to connect with Earth’s ancient and dramatic history.

Why Pseudotachylyte is Important For Geology Collections

Add this one-of-a-kind pseudotachylyte to your geology collection and marvel at this unique, ancient rock formed during a 2 billion year old impact event during the Paleoproterozoic Era, South Africa.