Development of a rockfall hazard rating matrix for the State of Ohio : executive summary report.
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2005-06-30
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Edition:Executive summary report.
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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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