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Inside this cavelet in the Broadwell Natural Arch formation is a ribbed ceiling

7626-natural-arch.jpg The gravelly road toward Foshay Pass rises slowlyThumbnailsThe erosion from flowing torrents of water in this little side wash is significantThe gravelly road toward Foshay Pass rises slowlyThumbnailsThe erosion from flowing torrents of water in this little side wash is significantThe gravelly road toward Foshay Pass rises slowlyThumbnailsThe erosion from flowing torrents of water in this little side wash is significantThe gravelly road toward Foshay Pass rises slowlyThumbnailsThe erosion from flowing torrents of water in this little side wash is significantThe gravelly road toward Foshay Pass rises slowlyThumbnailsThe erosion from flowing torrents of water in this little side wash is significant

Presumably, the thinner parts of the ceiling are weaker. Weak enough to break under the weight of a human body (I'm not about to test this)? Pieces of rock have broken off over time and are sliding down the slope.