This schematic outlines the principal openings and geological characteristics associated with the Great Sphinx. These include both ancient and later interventions, as well as natural fractures within the bedrock.
The current absence of clear evidence for a large internal chamber—often referred to as a “Hall of Records”—is typically noted in mainstream studies, though the question continues to attract speculation and further investigation.
For a more detailed analysis of these features, see the articles on this page beginning here.
Source: thegreatsphinxofgiza.com 2026