Honu'apo Park Resource Management Plan
Honu'apo Park Resource Management Plan
Honu'apo Park Resource Management Plan
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Honuÿapo <strong>Park</strong> Final <strong>Resource</strong>s <strong>Management</strong> <strong>Plan</strong><br />
flooding on the subject property. An irrigation system developed and formerly<br />
maintained by the sugar plantations of Kaÿü has affected the surface hydrology of<br />
the area and, according to verbal accounts, decreased the number of flooding<br />
events at Honuÿapo. With the shutting down of the sugar industry in Kaÿü and the<br />
subdivision of plantation lands into smaller parcels, the irrigation system is no<br />
longer maintained.<br />
2.3.3 Natural Hazards<br />
Volcanic hazard in the vicinity of Honuÿapo is assessed by the USGS as “6” in the<br />
southern and central portion of the park, and “3” in the northernmost zone of the<br />
park, on a scale of ascending risk from “9” to “1”. This moderate to high hazard<br />
designation is based on the fact that Mauna Loa is an active volcano, having last<br />
erupted in 1984.<br />
In terms of seismic risk, the entire Island of Hawai‘i is rated Zone 4 Seismic Hazard,<br />
which means it is at risk from major earthquake damage, especially to structures<br />
that are poorly designed or built. The most significant earthquake occurring in Kaÿü<br />
in recorded history was in March and April 1868. Written accounts of Kaÿü<br />
residents attest to the tremendous damage caused by the earthquakes and ensuing<br />
tsunami. A written account by C. J. Waialoha (Ka Nupepa Kuÿokoÿa, April 11,<br />
1868), a Hawaiian resident of Kaÿü describes the disaster (Handy et al. 1991:566):<br />
… The earthquakes were terrible from the 27 th [of March] to the<br />
30 th . The earth shook constantly. We had never before known<br />
anything like this. The stones on our beaches and the cliffs are<br />
scattered and broken… The famous cliffs of Pohina [at Honuÿapo]<br />
were broken in places and some of the natives there feared a<br />
similar fate… At three o’clock on Thursday, April 2, came a great<br />
quake which made it impossible for man and animals to stand<br />
upright. The earth below rose to the sky like a cloud, from the land<br />
slides; big trees toppled over; gulches were filled and houses<br />
collapsed… fifteen minutes after the earthquake, a tidal wave arose,<br />
which killed a number of people. Those who died numbered 46<br />
and those who barely escaped are not numbered… When the sea<br />
ebbed, all kinds of fish were left ashore, except the whale and the<br />
shark.<br />
The houses at Kaÿaluÿalu, Paiahaÿa, Honuÿapo, Hokukano,<br />
Kaÿalaiki, the two Hilea, Ninole, Wailau, Punaluÿu, and as far as<br />
Keauhou, were all swept away by the sea.<br />
The 1868 earthquake that caused the destructive tsunami was estimated to have<br />
had a magnitude of 7.9. Another tsunami in 1946, generated by an earthquake in<br />
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