Topic: Tura Limestone

The Khafre pyramid at Giza exhibits physical evidence of a massive oceanic inundation in the form of a tidal band near its summit. While the very top retains intact Tura limestone, the middle section shows parabolic erosion caused by sustained sea levels approximately 576 feet higher than current levels. The presence of 55,000 tons of travertine detritus at the base suggests the limestone casing stones were dissolved by carbonic acid in ocean water rather than being scavenged by later civilizations.

The guest describes a specific "bric-a-brac" erosion pattern on the Khafren pyramid in Egypt, located just below its remaining limestone cap. Drawing on 40 years of sailing experience, he identifies this as a horizontal band caused by standing ocean water. He concludes that the pyramid was once partially submerged, which explains the loss of its outer casing stones, and argues that this evidence is being suppressed to maintain the current historical narrative.