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Record #00499Nature archive

Largest Confirmed Terrestrial Impact Structure

South Africa's Vredefort impact structure formed about 2.023 billion years ago and is widely regarded as the largest confirmed terrestrial impact remnant. Geological reconstructions commonly estimate the original crater at roughly 250–300 km across, while UNESCO describes a broader structure with a radius of 190 km.

Verification status
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Last updated
2026-11-10
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Current Record

about250

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–300 (reconstructed range)

Current record value

Holder
Vredefort Dome
Location
— · Vredefort DomeSatellite view · Google Maps · South Africa
Start date
—
Record status
Evidence-backedView verification details ↗Report an issue
OverviewRecord historyRelated recordsSources

Overview

Archive Note

Billions of years of erosion have removed the crater's original rim and exposed the deeply uplifted central region now represented by the Vredefort Dome.

A 2022 JGR: Planets modelling study describes common original-crater estimates around 250–280 km, while a 2023 Meteoritics & Planetary Science study gives 250–300 km. UNESCO describes a broader structure with a radius of 190 km, which is not automatically equivalent to the modelled original crater diameter.

Key information

Original crater diameter
About 250–300 km, modelled range
Impact age
About 2.023 billion years
UNESCO broader scale
190 km stated structural radius
Preserved feature
Central uplift known as Vredefort Dome
Evidence
Shock metamorphism and impact melts

Record history

1 Milestones
  1. —about 250–300 (reconstructed range)Vredefort DomeCurrent Record

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Sources

Evidence & References

Verification basis and limitations

Evidence-backed

Credible sources support core facts; the comparison scope or corroboration remains incomplete.

Basis: corroborating reliable secondary materials

UNESCO calls Vredefort the largest known impact structure, using a broader 190 km radius. JGR (2022) and Meteoritics & Planetary Science (2023) estimate the original crater at about 250–300 km diameter. The numeric 300 is an explicitly qualified upper bound, not a directly observed exact diameter.

Ranking confidence
Uncertain

Comparison boundaries still under review

The original rim has been deeply eroded. Reconstructed crater diameters commonly fall around 250–300 km but broader estimates exist; UNESCO's radius must not be assumed equivalent. Developing status is retained.

Verification assessment
2026-11-10
Last editorial review
2026-11-10

Current Entry identifies the current entry in this archive; it does not establish that the record is still held today.

Source IDSourcePublisherLink
SRC-001A Revision of the Formation Conditions of the Vredefort CraterAcademicENCurrent recordJournal of Geophysical Research: PlanetsSRC-002Vredefort DomeOfficialENCurrent recordUNESCO World Heritage CentreSRC-003Decision 29 COM 8B.4OfficialENCurrent recordUNESCO World Heritage CommitteeSRC-004Genesis of the mafic impact melt rock in the northwest sector of the Vredefort DomeAcademicENCurrent recordMeteoritics & Planetary Science

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