Interpretations were drawn on paper maps, which displayed the sun-illuminated topography with the locations of sediment grain size, with textural analysis, and video/photo stations. These paper maps were printed at a scale of 1:25000 on a large format HP plotter. The interpretation was based on seabed samples to determine sediment grain size distribution, photo and video imagery to identify small seabed features, multibeam sonar data to identify large seabed features and relative reflectivity (hardness and softness) of seabed sediments. The paper interpretations were transferred to ArcGIS visually based on background data layers in the GIS. The process was an iterative one, with the interpretation then printed on the paper maps with underlying bathymetry or backscatter, and interpretation lines adjusted based on the other data printed on the maps.
The following information was used as guidelines to derive individual units.
Individual sediment samples were aggregated into substrate types by comparing their textural composition, with special emphasis placed on:
(1) mean grain size in phi units;
(2) standard deviation from the mean of grain size distribution (degree of sorting) in phi units;
(3) significant grain size(s) in phi units;
(4) mud, sand and gravel contents in weight percents of the sample;
(5) sand fraction subdivided into fine grained sand (3 and 4 phi) and coarse grained sand (0, 1, and 2 phi) in weight percents of the sample;
(6) gravel fraction subdivided into G1 (-1 and -2 phi) and G2 (-3, -4, and -5 phi) in weight percents of the sample.
Gravel pebbles larger than -5 phi (6.4 cm) were not collected in this study, although larger pebbles, cobbles, and boulders were observed in seabed imagery.
Mobility of sediments was determined by the presence or absence of sand ripples, as viewed in video and photographic imagery.
Substrate layering was determined by the presence of a layer of finer sediment overlying (but not completely covering) coarser sediment, as viewed in video and photographic imagery.
This process took place over a number of years, 2005-2010.