This is an amateur geologist's idea of how the natural bridge could have formed. If you know of a more plausible scenario, please let me know.
![]() | Original cross-section through natural bridge area, looking along the bridge. The cross-section is through the middle of the bridge. |
![]() | Some erosion due to the spring has now moved the surface back to expose the strong rock layer. |
![]() | Two possible scenarios: |
![]() | The cavity expands rapidly, either due to seep of water through the alluvium from above, or from flow toward the spring from below. |
![]() | The cavity has now broken through to the surface, and stream runoff now enters from above as well. |
![]() | The stream runoff from above erodes the uphill side rapidly. The downhill side of the cavity erodes at a lesser rate, leaving a more vertical wall. |
![]() | Two possible scenarios, corresponding to the two cases above: |
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Copyright © 1999 by Tom Chester.
Permission is freely granted to reproduce any or all of this page as long as credit is given to me at this source:
http://tchester.org/sgm/places/nat_bridge/model.html
Comments and feedback: Tom Chester
Updated 8 December 1999.