There is some reason to believe that Maui was originally two islands, the northern and southern parts being joined together by an immense sandy plain, so low that in misty weather it is hardly to be distinguished from the ocean; and some years ago a ship actually ran aground upon it, sailing for what the captain imagined to be an open passage.
Maui has also the famous Wailuku Valley, a picturesque gorge several miles deep, and giving you a very fair example of the broken, verdure-clad, and now lonely valleys of these islands; which are in reality steep, narrow canons, worn out of the mountains by the erosion of water. The old Hawaiians seem to have cared little how difficult a piece of country was; they not only made their taro patches in the streams which roar at the bottoms of such gorges, but they fought battles among the precipices which you find at the upper ends of these valleys, where the defeated usually met their deaths by plunging down into the stream far below.
After seeing a live or burning crater like Kilauea, Haleakala, I thought, would be but a dull sight; but it is, on the contrary, extremely well worth a visit. The islands have no sharp or angular volcanic peaks. Mauna Loa and Mauna Kea, on Hawaii, though 14,000 feet high, are mere bulbs—vast hills, not mountains; and the ascent to the summit of Haleakala, though you surmount 10,000 feet, is neither dangerous nor difficult. It is tedious, however, for it involves a ride of about twelve miles, mostly over lava, uphill. It is best to ride up during the day, and sleep at or near the summit, where there are one or two so-called caves in the lava, broken lava-bubbles in fact, sufficiently roomy to accommodate several persons. You must take with you a guide, provisions, and blankets, for the nights are cold; and you find near the summit water, wood enough for a small fire, and forage for your horses. Each person should have water-proof clothing, for it is very likely to rain, at least on the Makawao side.
[Illustration: CASCADE AND RIVER OF LAVA—FLOW OF 1869.]
The great crater is best seen at sunrise, and, if you are so fortunate as to have a tolerably clear sky, you may see, lying far away below you, almost all of the islands. Hawaii lies far enough away to reveal its entire outline, with Mauna Loa and Mauna Kea rising near either end, and the depression near which lies Kilauea in the middle. The cloud effects at sunrise and sunset are marvelous, and alone repay the ascent.
But the crater itself, clear of fog and clouds in the early morning, and lighted up by the rising sun, is a most surprising sight. It is ten miles in diameter, and the bottom lies 2000 feet below where you stand. The vast irregular floor contains more than a dozen subsidiary craters or great cones, some of them 750 feet high, and nearly as large as Diamond Head. At the Kaupo and Koolau gaps, indicated on the map, the lava is supposed to have burst through and made its way down the mountain sides. The cones are distinctly marked as you look down upon them; and it is remarkable that from the summit the eye takes in the whole crater, and notes all its contents, diminished of course by their great distance. Not a tree, shrub, or even tuft of grass obstructs the view.