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] standing sixty-six feet (twenty meters) high and 240 feet (seventy-three meters) long, sits on the edge of the Giza Plateau (just west of Cairo, Egypt), east of the three great pyramids.Most Egyptologists currently attribute the carving of the Great Sphinx to King Chafre (Chephren) of the Old Kingdom's Fourth Dynasty, in approximately 2500 B. by various chronologies.[It is important to read the LAST PARAGRAPH of this paper and to understand the mindset of a geologist who was raised by his grandmother, she was a Rosicrucian - Robert Schoch looked specifically for any geological features that would 'prove' his theory, he was not neutral in his search of geological data when he told me his story of his interest in Egypt and Edgar Cayce and the Sphinx prior to joining JAW.Of course, it still rains at Giza on occasion, and thus precipitation-induced weathering can be said to exist on all structures on the Plateau to some small degree; here we are talking in generalities and attempting to look at the broad picture.In many places this precipitation-induced weathering mode has superimposed upon it wind-induced weathering.

The Sphinx is carved from local bedrock and faces directly east.Presumably the major portion of this precipitation-induced weathering occurred prior to the onset of the current and regime exhibited at Giza On the Sakkara Plateau, some ten miles (sixteen kilometers) to the south of Giza, there are fragile mud-brick structures, mastabas, that are indisputably dated to the First and Second dynasties-presumably several hundred years earlier than the standard dating of the Sphinx-that exhibit no evidence of the precipitation-weathering features seen in the Sphinx enclosure.As noted above, well-documented Old Kingdom tombs at Giza, cut from the identical sequence of limestones as the body of the Sphinx, exhibit well-developed wind-weathering features, but lack significant weathering which is precipitation-induced.In this mode of weathering, the original profiles of the carved faces of tombs and other structures are still clearly visible (sometimes containing easily legible hieroglyphic inscriptions); but the softer, less competent layers of rock have been "picked out" by wind and sand abrasion, with the consequent formation of deeply eroded "wind-tunnel" features.This wind-induced weathering is distinctly different in nature from the precipitation-induced weathering; it is well exemplified on various Old Kingdom tombs and structures south and west of the sphinx, which have been carved from the same sequence of limestones as the body of the great sculpture itself.

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