Northern California, Oregon, and the Sandwich Islands by Charles Nordhoff
page 60 of 346 (17%)
page 60 of 346 (17%)
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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. To describe such a scene is impossible. A study of the map, with the figures showing elevations, will give you a better idea of it than a long verbal description. It is an extraordinarily desolate scene. A few wild goats scramble over the rocks, or rush down the nearly perpendicular cliff; occasionally a solitary bird raises its harsh note; the wind howls fiercely; and as you lie under the lee of a mass of lava, taking in the scene and picking out the details as the rising sun brings them out one by one, presently the mist begins to pour into the crater, and often by ten o'clock fills it up completely. The natives have no tradition of Haleakala in activity. There are signs of several lava flows, and of one in particular, clearly much more recent than the others. It must have presented a magnificent and terrible sight when it was in full activity. I did not ride into the crater, but it is possible to do so, and the natives have a trail, not much used, by which they pass. If you descend, be careful not to leave or lose this trail, for in many parts your horse will not be able to get back to it if you suffer him to stray off even a few yards, the lava is so sharp and jagged. As you descend the mountain on the Makawao side you will notice two finely shaped craters on the side of the mountain, which also in their time spewed out |
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