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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 110,
F02002,
doi:10.1029/2004JF000217,
2005
Nearshore wave-induced cyclical flexing of sea cliffs
Peter N. Adams
Department of Earth Sciences, University of California, Santa Cruz, California, USA
Curt D. Storlazzi
U.S. Geological Survey, Santa Cruz, California, USA
Robert S. Anderson
Department of Geological Sciences and INSTAAR, University of Colorado, Boulder, Colorado, USA
Abstract
Evolution of a tectonically active coast is driven by geomorphically destructive energy supplied by ocean waves. Wave energy
is episodic and concentrated; sea cliffs are battered by the geomorphic wrecking ball every 4–25 s. We measure the response
of sea cliffs to wave assault by sensing the ground motion using near-coastal seismometers. Sea cliffs respond to waves in
two distinct styles. High-frequency motion (20 Hz) reflects the natural frequency of the sea cliff as it rings in response
to direct wave impact. Low-frequency motion in the 0.1–0.05 Hz (10–20 s) band consistently agrees with the dominant nearshore
wave period. Integrating microseismic velocities suggests 50 μm and 10 μm displacements in horizontal and vertical directions,
respectively. Displacement ellipsoids exhibit simultaneous downward and seaward sea cliff motion with each wave. Video footage
corroborates the downward sea cliff flex in response to the imposed water load on the wave cut platform. Gradients in displacement
amplitudes documented using multiple seismometers suggest longitudinal and shear strain of the flexing sea cliff on the order
of 0.5–4 μ strains during each wave loading cycle. As this sea cliff flexure occurs approximately 3 million times annually,
it has the potential to fatigue the rock through cyclical loading. Local sea cliff retreat rates of 10 cm/yr imply that a
given parcel of rock is flexed through roughly 109 cycles of increasing amplitude before exposure to direct wave attack at the cliff face.
Received 4
August
2004;
accepted 6
January
2005;
published 23
April
2005.
Keywords: coastal;
erosion;
strain.
Index Terms: 4546 Oceanography: Physical: Nearshore processes; 4560 Oceanography: Physical: Surface waves and tides (1222); 5112 Physical Properties of Rocks: Microstructure; 1815 Hydrology: Erosion.
Read Full Article (file size: 2048728 bytes) Cited by
Citation: Adams, P. N., C. D. Storlazzi, and R. S. Anderson
(2005),
Nearshore wave-induced cyclical flexing of sea cliffs,
J. Geophys. Res.,
110,
F02002,
doi:10.1029/2004JF000217.
Copyright 2005 by the American Geophysical Union.
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