In 1855 The Fourth Recorded Eruption Of Mauna Loa Occurred.

The lava flowed directly Hilo- wards, and for several months, spreading through the dense forests which belt the mountain, crept slowly shorewards, threatening this beautiful portion of Hawaii with the fate of the Cities of the Plain.

Mr. C. made several visits to the eruption, and on each return the simple people asked him how much longer it would last. For five months they watched the inundation, which came a little nearer every day. "Should they fly or not? Would their beautiful homes become a waste of jagged lava and black sand, like the neighbouring district of Puna, once as fair as Hilo?" Such questions suggested themselves as they nightly watched the nearing glare, till the fiery waves met with obstacles which piled them up in hillocks, eight miles from Hilo, and the suspense was over. Only gigantic causes can account for the gigantic phenomena of this lava- flow. The eruption travelled forty miles in a straight line, or sixty, including sinuosities. It was from one to three miles broad, and from five to two hundred feet deep, according to the contours of the mountain slopes over which it flowed. It lasted for thirteen months, pouring out a torrent of lava which covered nearly 300 square miles of land, and whose volume was estimated at thirty-eight thousand millions of cubic feet! In 1859 lava fountains 400 feet in height, and with a nearly equal diameter, played on the summit of Mauna Loa.

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