MATERIALIZATION AND ALIVE IN SOLID ROCK

When digging marble from the quarry at Oreston, England, in the 19th century, a startling discovery was made. This marble is finely grained and quite pure. The only defect is that here and there wide seams of clay wandered through the 400-million year old stone, sometimes giving way to partially-filled caverns. In one of the caverns, the fossil bones of three rhinoceroses was found, which were common in the area 65 million to 2 million years ago. The cave was 15 feet wide, 45 feet long, and lay 70 feet down. There were no stalactites, no stalagmites, and no indication that there had ever been an opening in the rock, and no indication on how the Rhino’s got there.


A horned lizard was found inside a block of stone, in New Mexico, in 1853. The stone was “so solid as to preclude the entrance of the smallest insect”. The lizard was sent to the Smithsonian Institute, where it died 2 days later.

AND CONCERNING evidence of a recent poleshift

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