1. References

The Kaigas glaciation was a hypothesized snowball earth event in the Neoproterozoic Era, preceding the Sturtian glaciation. Its occurrence was inferred based on the interpretation of Kaigas Formation conglomerates in the stratigraphy overlying the Kalahari Craton as correlative with pre-Sturtian Numees formation glacial diamictites. However, the Kaigas formation was later determined to be non-glacial, and a Sturtian age was assigned to the Numees diamictites. Thus, there is no longer any evidence for a Neoproterozoic glaciation prior to the Sturtian snowball earth event.^[1]

References

• University of the Arts Bremen
• University Of The Arts London
• University of the Assumption
• University of the Atlantic
• University of the Auvergne
• University of the Bahamas
• University of the Balearic Islands
• University of the Basque Country
• University of the Bosporus
• University of the Cape
• University of the Cape of Good Hope
• University of the Chinese Academy of Sciences
• University of the City of Manila, District Colleges
• University of the City of Manila, Open University
• University of the city of New York
• University of the Cloister of Sor Juana
• University of the Cordilleras
• University of the district of columbia
• University of the east
• University of the East Caloocan
• University of the East Chorale
• University of the East Chorale (UEC)
• University of the East College of Business Administration
• University of the East College of Computer Studies and System
• University of the East College of Dentistry