A concrete staircase leads down into
the skylight that forms the entrance to the caves. The section of the caves
open to the public stretches for approximately 2 miles. Many areas near the
entrance are lit by sunlight, but the cave is damp, cool and often muddy, with
lots of vines, ferns and roots hanging down from the entranceway and the
ceiling. Visitors can observe a wide variety of lava formations, including some
rock that is red because it cooled so fast during the 1881 flow that it
retained its color.
The Kaumana lava tube was formed by
lava flow from Hawaii 's Mauna
Loa in 1881. The eruption of the giant volcano actually occurred
on Nov. 5, 1880, but the lava continued its slow approach on Hilo through the first few months of 1881. By
late June, it was within 5 miles of the town and began picking up speed. Legend
has it that Hawaii's Princess Ruth, sent from Honolulu, is responsible for
saving the then-tiny village because she was carried into the hills in late
July and took up a position in front of the lava, praying to Pele, the Hawaiian
goddess of religion and fire, to spare the town. The flow began slowing, and finally
stopped in early August, just 1.5 miles from Hilo Bay .
Dan and I didn't venture too far into
the tube, maybe just 1/4 mile in each direction, but far enough to notice that without our flashlights we would be in
absolute darkness. For the serious spelunker, long pants, headlamps, and closed
toed shoes are recommended to traverse all of the accessible parts of this
cave.
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