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Most of these sedimentary rock fragments are coarse arenites or fine diamictites.
The composition of the arenites is given in Table 2.
Arenite is a sedimentary clastic rock with sand grain size between 0.0625 mm (0.00246 in) and 2 mm (0.08 in).
In sections from a proximal position relative to the palaeo-shoreline, the lower parts of this limestone are dolomitized and contain thin intercalations of quartz arenite.
Beds of very fine to very coarse, rarely gravelly, sandstone (volcanic lithic arenite) and mudstone dominate the succession with subordinate beds of lithic and vitric tuff.
Beds of very fine to very coarse, sandstone (volcanic lithic arenite) and mudstone dominate the succession with a bed of lithic and vitric tuff occurring at one horizon.
Beds of very fine to very coarse, rarely gravelly, sandstone (volcanic lithic arenite) and mudstone dominate the succession with beds of lithic and vitric tuff occurring at two horizons.
The term quartzose sandstone can also be used for a quartz arenite.
Sand composition is largely quartz arenite and a small percentage of monomineralic components dominated by quartz and some accessory minerals (zircon, feldspar, hematite, and rutile).
The arenite can contain calcareous concretions, fossils and hardgrounds with shell fragments.
Six sandstone names are possible using descriptors for grain composition (quartz-, feldspathic-, and lithic-) and amount of matrix (wacke or arenite).
The sediment is mostly quartz arenite.