What is left of Kuwai forms part of the modern island of Epi.
In all
cultures there are legends of great cataclysms, of Gods angry and the
world as man knows it turned into a hellish nightmare beyond human
comprehension. Vanuatu has known many such eruptions, one poignantly
described
by missionaries.
But two or
three times every 10,000 years a volcano erupts with such profound
violence as to make the awesome disasters of Tambourine and Krakatoa
seem like mere sneezes in comparison. Such were the famed eruptions
of Santorini in Greece and that which formed Crater Lake in the
U.S.
And such an
eruption, little known because it took place in a small South Pacific
archipelago, was Kuwai.
Once upon a
time, sometime between the years 1420 and 1430 AD, a magnificent
tropical island called Kuwai formed part of the Vanuatu group of
islands. It was a big island, of towering peaks and cascading
jungles. On its summit, a volcano steamed. Then one day, no doubt
preceded by days or even weeks of increasing earthquake activity and
ash eruptions, Kuwai blew itself off the face of the planet, taking a
significant chunk of the island with it. An estimated 32 cubic
kilometers of magma - a volume simply too large to fully comprehend -
shot into the atmosphere, cooling the planet and creating magnificent
sunsets during the next few years.
The impact of the eruption was profound. Those inhabitants who
somehow survived, were left scattered on the remnants of
Kuwai. Some remained on the larger fragment - Epi Island
while others were left scattered across the fragments of
southern Kuwai, now called the Shepherd Islands.
The largest of these islands is called Tongoa. Yet still more left
their island home forever and made the journey by canoe to the
northern parts of Efate Island.
Today, those
settlers of almost six hundred years ago still pay an annual
ceremonial tribute to the traditional landowners of North Efate from
whom they leased land, generations before. The settlers retained
their language and unique aspects of their culture. On a few, very
clear days, they can look north and glimpse what once remained of
their ancestral home.
This eruption
of Kuwai was dated in many ways. In a society where written language
does not exists, oral traditions are important - and accurate. The
legend of Kuwai is based solidly in fact. Arctic ice
cores*
have dated the eruption to within 10 years of what has traditionally
been estimated.
Being
submerged has not quenched Kuwai's fire. It has erupted at least 12
times since 1452, most recently 'officially' in 1974. In fact it has
also erupted in 1977, 79 and 1980 on a moderate (VE1=0-2) scale, with
aircraft pilots reporting steam and bubbling and on one occasion a
small land mass above the surface of the water.
The 1897-1901
eruption built an island 1km long by 15m high, however the ocean
eroded it within 6 months.
The collapsed
underwater Calera (see previous page) is 12 kilometers wide and 6
kilometers long. The eruption that cause the Calera in the fifteen
century probably began as a hydromagmatic eruption over the course of
a year or more, with two major pyroclastic flows (see
Tanna volcano
for an explanation of terms) followed by the collapse of the Calera.
Kuwai is
monitored regularly for it is still considered a very active and
potentially dangerous volcano. However it is today becoming more
famous as a world class dive site. the legendary Tongoa Wall, a dive
site off the south western side of the Calera, is famous for it's
extraordinary diversity of life and colour. Upwelling warmth from the
heart of the active vents have resulted in a veritable underwater
garden of Eden. Like all volcanoes, Kuwai, as destructive as it has
and will be again, is also the harbinger of life.
*Dating With Arctic Core Samples
All volcanoes
have individual 'signatures' for they are composed of a unique
combination of elements that can pinpoint them as accurately as any
finger print. When a volcano erupts, it shoots tons (or in the case
of Kuwai, cubic kilometers) of earth into the atmosphere. This
circles the globe and eventually falls to the earth, including places
like the Arctic, as dust. Over time, more ice covers this dust,
keeping it locked in, rather than mixed up with other direct, or
eroded away.
Arctic core
samples are obtained when scientists drill deep into the accumulated
layers ice, removing a 'core' of ice that a its base, can be hundreds
of thousands of years old. By dating small fragments found in these
ice cores, using radiocarbon and potassium-argon methods, it is
possibly to accurately date when particular events
occurred.
Knowing a
date and knowing that certain kinds of volcanic ash belong to
specific volcanoes, means prehistoric volcanic eruptions can be dated
very accurately.
Next: Ambae (Bali Hai) Island Volcanoes