Nearly 50% of the shoreline is dominated by the calving ice fronts of the large outlet glaciers.
For a given water depth, as em increases, so does the delta length and, correspondingly, the shoreline sediment flux required to maintain progradation.
The isolated exposures of the accretionary lapilli-bearing facies along the coastline may alternatively record shoreline or water interaction of pyroclastic flows.
And it's very noisy, only if you're camping by the shoreline will you notice it.
To capture accurately the small-time shoreline behavior, we use a logarithmic temporal discretization.
Alternative explanations for the observed pattern of shoreline vegetation distribution are possible but less plausible than the action of wind and waves.
During and immediately following monsoon periods, some species of fish may concentrate closer to the shoreline.
The shoreline can be envisioned as an internal moving boundary of the fluvio-deltaic system.
