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Northern California, Oregon, and the Sandwich Islands by Charles Nordhoff
page 53 of 346 (15%)
caused by earthquakes and lava flows, on the Puna coast. Near and at
Kaimu, for instance, there has been an apparent subsidence of the land,
which is supposed in reality, however, I believe, to have been caused
rather by the breaking off of a vast lava ledge or overhang, on which,
covered as it was with earth and trees, a considerable population had long
lived. In front of the native house in which you will sleep, at Kaimu,
part of a large grove of cocoa-nut-trees was thus submerged, and you may
see the dead stumps still sticking up out of the surf.

Kaimu is twenty-five miles from the Volcano House. The native house
at which you will pass the night is clean, and you may there enjoy the
novelty of sleeping on Hawaiian mats, and under the native cover of tapa.
You must bring with you tea or coffee, sugar, and bread, and such other
food as is necessary to your comfort. Sweet-potatoes and bananas, and
chickens caught after you arrive, with abundant cocoa-nuts, are the
supplies of the place. The water is not good, and you will probably drink
only cocoa-nut milk, until, fifteen miles farther on, at Captain Eldart's,
you find a pleasant and comfortable resting-place for the second night,
with a famous natural warm bath, very slightly mineral. Thence a ride of
twenty-three miles brings you back to Hilo, all of it over lava, most of
it through a sterile country, but with one small burst of a real paradise
of tropical luxuriance, a mile of tall forest and jungle, which looks more
like Brazil than Hawaii.

One advantage of returning by way of the Puna coast, rather than by the
direct route from Kilauea, is that you have clear, bright weather all the
way. The configuration of the coast makes Puna sunny while Hilo is rainy.

If you desire a longer ride than that by the Puna coast, you can cross
the island, from the Volcano House, by way of Waiahino and Kapapala to
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