[48]. They are described on p. [322].
[49]. This absence of a healthy forest-growth, such as occurs on the level summit of the neighbouring Soloa Levu and in all like situations, has probably some geological significance.
[50]. These tuffs are probably submarine. They will be found described with tuffs of the same character on p. [333].
[51]. The track attains an elevation of about 1,300 feet, but the top of the watershed is two or three hundred feet lower.
[52]. It belongs to the 3rd order of the hornblende-hypersthene-andesites described on p. [299].
[53]. Occasional views of its summit only are obtained from the eastward, as from the Ndrandramea mountains and their vicinity.
[54]. Alluvial gold has long been known to occur in the bed of the Yanawai below Vatu Kaisia; but it has never been found in paying quantity.
[55]. Under the microscope it is shown to be granular in structure, exhibiting a mosaic of irregular quartz grains.
[56]. The blocks of the agglomerate in this last locality are from one to three feet across.
[57]. It displays in the groundmass augite prisms in flow-arrangement, and is referred to genus 20 of the augite-andesites.