We had now reached the south border of the Betsileo country. Indeed we
might say that we were close to three boundaries which enclose its
southern end. And when in the afternoon, my colleague and I climbed the
ridge of Kinanga, which overhangs the town, we had these chains of hills
prominent and near. On the west and south-west was the granite ridge of
Kipaseha, towering over the country. Within it were two lower groups of
gneiss hills, with the forest close by, bounding the Ambohimandroso
valley. To the east was the lofty mountain of Ambóndrombé, covered with
dense wood. Directly south was a line of hills crossing the country from
the one set of ridges to the other and shutting us completely in. Beyond
the town to the south we noted several villages, and ten miles away,
upon a spur of these hills, with the green forest just beyond, was the
village of Angalampona, the last village peopled by the Betsileo in that
direction. This was the boundary of the Hova dominion; and of the sphere
which the Mission has yet occupied. Imahazony is on the line of Lat. 22°
S.
It must not be supposed that on the other side of the southern forest
there is no population. Population does not cease, but it changes its
character. What change there may be in the ground no one could clearly
describe. One thing however we had ourselves observed with deep
interest. The fall in the ground of fourteen hundred feet, immediately
south of Ivato-avo, as well as the profusion of red clay outside the
gneiss hills, indicated that in the basin of Ambohimandroso we had
descended on to the first terrace toward the south. We were no longer on
the high level of the Imerina and Betsileo plateau. It is exceedingly
probable that some few miles beyond another and lower terrace is
reached, as in the north of the island. From the top of Iody Mr. Pillans
observed that the country seemed to be falling and to be more open: and
the natives were unanimous in declaring that in the south the country
was more level and more easy to travel than the Betsileo. As on the
eastern and western slopes, so towards the south also, the ground
doubtless falls in broad, well-watered terraces, till it reaches the
great, level plains observed near the extreme end of the island. It is
hoped that in due time some members of the Mission may solve these
questions by a personal examination of the district.
Public-domain text, read in full here on John Shaqi.
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