What are my risks?
Oahu Volcanoes
Oahu has been formed from two principle volcanoes:
Waianae and Koolau. Waianae is about 2.2-3.8 million years old
and Koolau is about 1.8-2.6 million years old. Both volcanoes
are now considered extinct.
The island is also riddled in spots by smaller volcanic
features such as Diamond Head, Punchbowl, Salt Lake Crater, Koko
Head and Koko Crater. These smaller volcanoes formed in more recent
times, although the age determinations on them are not very good.
In general, these "post-erosional" volcanoes are believed to be
between 70,000 and 500,000 years old.
Is there a threat of a volcano
erupting on Oahu again?
It is always possible, but the odds are extremely
slim. Vulcanologists (people who study volcanoes) predict volcanic
activity for places such as Oahu by looking at the area's historical
record. Although data is limited, it suggests Oahu's post-erosional
volcanoes erupted every couple of 10,000 years or so. Since it
has been longer than that since the last eruption, it indicates
volcanic activity has finished for Oahu.
Dr. Ken Rubin, Assistant Professor
Department of Geology and Geophysics
University of Hawaii, Honolulu, HI 96822
Vog and Laze Hazards on Oahu
Although volcanoes on Oahu are extinct, volcanic
hazards do affect the island. Volcanoes spew noxious plumes of
acidic gases. The resulting vog and laze effect many communities
across the State, including Oahu.
When a volcanic erupts, sulfur dioxide within the
molten rock is converted to sulfuric acid. The resulting plume
is known as vog (volcanic fog).
Gases are also produced at the ocean. When the lava
enters the ocean, hydochloric acid is produced - called laze
(lava haze). Both of these gases can contain particulate matter,
such as volcanic glass or trace metals.
Vog and laze are carried by winds across the county.
The impacts include:
- obscured views;
- lower agricultural yields for certain crops;
- adverse health effects for people with respiratory or heart
conditions; and
- acidified rainwater catchment tanks (which, in turn, produces
a secondary hazard of leached lead in local water supplies).