Development of a rockfall hazard rating matrix for the State of Ohio : executive summary report.
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Development of a rockfall hazard rating matrix for the State of Ohio : executive summary report.

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      Executive summary report.
    • Abstract:
      The geology in Ohio is characterized by the

      presence of gently dipping, harder, more competent

      strata (siltstones, sandstones, limestones) alternating

      with softer, less competent strata (claystones,

      mudstones, sha les). This type of stratigraphy is

      highly susceptible to differential weathering which

      results in undercutting of the competent layers by

      erosion of the incompetent layers. Undercutting

      promotes a variety of slope movements such as

      rockfalls, plane failures, and wedge failures that

      may not occur otherwise. Many of the slope failures

      in Ohio initiate as plane failures and wedge failures

      in competent strata at higher elevations and descend

      as rockfalls. The frequency and size of these falls

      depend upon joint spacing within the competent

      unit and the extent by which it has been undercut.

      The undercutting- induced failures can be quite

      hazardous because of their instantaneous

      occurrence, high speed, and occasionally large

      volume of rock involved. There are many road cuts

      in Ohio, however, where closely jointed rock units

      lead to rockfalls without the presence of

      undercutting. This study was undertaken to develop

      a rating matrix that could be used to rank order the

      slopes in terms of their hazard potential with respect

      to rockfalls.

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