Note 5 — XVII

Comparison with Javan Mountain district.The country here is strikingly similar to the remarkable mountain district of the Gelungúng, described by Junghuhn;5 yet the origin of these rising grounds differs in some degree from that of those in Java. The latter were due to the eruption of 1822, and the great fissure in the wall of the crater of the Gelungúng, which is turned towards them, shows unmistakably whence the materials for their formation were derived; but the great chasm of the Isaróg opens towards the east, and therefore has no relation to the numberless hillocks on the north-west of the mountain. Behind Maguiring they run more closely together, their summits are flatter, and their sides steeper; and they pass gradually into a gently inclined slope, rent into innumerable clefts, in the hollows of which as many brooks are actively employed in converting the angular outlines of the little islands into these rounded hillocks. The third river behind Maguiring is larger than those preceding it; on the sixth lies the large Visita of Borobod; and on the tenth, that of Ragay. The rice fields cease with the hill country, and on the slope, which is well drained by deep channels, only wild cane and a few groups of trees grow. Passing by many villages, whose huts were so isolated and concealed that they might remain unobserved, we arrived at five o’clock at Tagunton; from which a road, practicable for carabao carts, and used for the transport of the abacá grown in the district, leads to Goa; and here, detained by sickness, I hired a little house, in which I lay for nearly four weeks, no other remedies offering themselves to me but hunger and repose.