Do the signs add a hint of an element of danger to this hike? |
This is most surely not a "gentle" slope. |
Source: U.S. Geological Survey |
We would expect older volcanoes to display a great deal more erosion, but that's only part of the story at Kohala. The rest of the volcano has no similar sea cliffs. Something else happened here. New technology for accurate mapping of the sea floor offshore of the Hawaiian Islands has provided a useful clue. There is chaotic debris on the ocean floor at distances reaching as much as a hundred miles. The islands have been falling apart!
It is difficult to imagine the scale of these events. The largest debris avalanche ever witnessed by humans was the one that came off the flank of Mt. St. Helens during the eruption of May 18,1980. It traveled about 12 miles. An avalanche off the side of Mt. Shasta in California traveled about 28 miles, but no one was about to see it happen, seeing as how it is more than 300,000 years old.
When the flanks of the Hawaiian Islands collapsed, the runout was more than 120 miles at Molokai, and 80 miles below the cliffs of the Pololu Coast. The sudden displacement of sea water by the rock generated devastating mega-tsunamis. One such event left chunks of coral reef 1,300 feet above sea level on the island of Lanai.
Don't worry too much about killer tsunamis on your vacation journey. As horrific as they are, they take place at intervals measured in the tens or hundreds of thousands of years, and there are no signs that any are imminent. The Pololu avalanche took place about 120,000 years ago.
A short but steep trail leads from the end of the road to the valley floor several hundred feet below. It travels farther out across the coastal cliffs providing a better view of the beach cliffs along the coast south of Pololu.
The floor of the Pololu Valley is surprisingly flat, and one might wonder that people aren't living and farming here. They once did in large numbers, but the taro fields were destroyed by a series of more "normal" tsunamis in the twentieth century, and the fields have been abandoned. There is a rich archaeological record of farming and housing sites all along the valley.
They collected rocks too. Not for their intrinsic beauty, mind you, but to construct an impressive heiau at Pu'ukoholā on the other side of the volcano, more than twenty miles away. Heiaus are large temple sites composed of hundreds of thousands of boulders that were passed hand-to-hand between thousands of "volunteers" working for King Kamehameha in the late 1700s. The workers could face punishment for dropping a stone and breaking up the rhythm of the line.
The beach is composed of black and gray sand. There is also a system of sand dunes higher up the beach. Dunes are relatively rare on the islands, but wind blew coastal sands into a series of dunes reaching an elevation of 100 feet. Enjoy the pools, beach and dunes, because the hike up is quite steep.
Waipi'o Valley along the Kohala Coast |
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