We had a good climb: the total ascent being eleven hundred and thirty
feet. Our native friends, used to hills, coolly walked right up the
steep side, and thought nothing of it. Others of us took the more gentle
ascent or were carried by our men, who enjoyed the holiday, as much as
ourselves. The prospect from the summit was truly beautiful. Ivoko, we
saw, was a vast crater, a quarter of a mile across; the encircling wall
was complete, except at the south where the opening was fifty feet wide.
The western wall is higher than the eastern. Beneath us, half a mile to
the east, was another crater, Iatsífitra, second only to Ivoko, with its
opening to the north. Long narrow mounds of volcanic rocks, running out
from each of these hills showed the course taken by the molten lava
streams. Both hills were covered inside and out with living grass. On
the north-west shoulder of Ivoko were two other large craters,
overhanging Betafo: two more were close by at the north-east: and others
were conspicuous ten miles to the north. On the south again were several
others, the horse-shoe shape being very marked in all. While ten miles
to the south, was the round crater of Tritriva, with a green lake, deep
down within. Far away to the east were other craters near and to the
north of Sirabe.
Our survey of the country had now been carried along the western
districts of Imerina, and thence to the south; and it had embraced the
whole country lying between the Ankárat mountains and the great ridges
and peaks of Ménabé. On our former journey we had laid down the inner
portions of the Vákin Ankárat; Mr. Cameron had determined the latitude
of Betafo, Sirabe and Votovorona, nearly in a line; and we had examined
the whole eastern side of the upper plateau from the capital to the
south border of the Betsileo. At Ivoko we stood midway between these
separate lines of observations: a large number of the principal peaks
and positions were in sight; and we enjoyed an excellent opportunity of
comparing them together, and testing the accuracy of our own work. When
duly worked out, it was satisfactory to find that the sets of
observations were consistent with one another, and that the
discrepancies were few and within small compass. It is from these
observations that our Maps have been constructed.
Public-domain text, read in full here on John Shaqi.
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