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We therefore considered the reliability of predictions of boulder size.
Predicted boulder size ranged from 0.18 to 4.00 m measured on the longest axis.
We investigate some of the geological controls on boulder size, using a heterogeneous outcrop of Blue Lias limestone.
Discontinuity and predicted boulder size data were collected on different layers of Blue Lias limestone on a shore platform in Wales, United Kingdom.
The orbiting rocky grains gradually coalesced into objects of pebble size, boulder size, kilometer size, and larger another bottom-up scenario.
Our results demonstrate that in locations where repeated entrainment, transport and boulder breakdown are observed, loose boulder size may not be a reliable means of reconstructing wave energies required to detach, entrain and transport boulders.
Similar(38)
For two layers examined (layers 19 and 24), predicted boulder sizes were compared with boulders recently detached by storm waves (i.e. within 2.5 months of detachment) from the same layer.
Boulder sizes were found to be in the range 4.2 to 5.5 m, which is within the range of boulder sizes observed on Lanyu Island.
The results suggest that boulder sizes decreased with distance from the shore.
The heights were obtained by applying the Pignatelli et al. (2009) equation starting from the boulder sizes.
The use of the TLS techniques allows an accurate evaluation of the boulders size and weight whose accuracy is fundamental in order to test the reliability of the known hydrodynamic equations.
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