Posted
on January 23, 2017
I
think of volcanoes erupting over a matter of minutes or hours – not
for the better part of a year!
But
that's because I think of volcanic eruptions as violent explosive
outbursts of lava and gas and steam. Mauna Loa, in Hawaii, is the
largest volcano on the planet partly because its lava tends to be
silica poor, and therefore the lava eruptions tend to be very fluid,
non-explosive, gentler and slower-moving than many other volcano's eruptions, although often still quite
destructive.
So...why
does having silica-poor lava relate to being a large volcano? Simply
stated, Mauna Loa doesn't blow off its top!
These pictures of another volcano, Mt. St. Helens, shows that some volcanos DO blow their tops off! Check out the lovely cone that is Mauna Loa, below: |
The
slopes of Mauna Loa are generally gentle. The cooling lava makes the
volcano larger – and, incidentally, makes the island of Hawaii
larger. The volume of the volcano is estimated to be about 18
thousand cubic miles (75 thousand cubic kilometers).
By
the way, even though Mauna Loa is the largest volcano on Earth, we
are talking about that huge volume, not its height. It isn't the highest
volcano on Earth, and even its island neighbor, Mauna Kea, is higher
by about 120 feet (37 meters).
Now,
about that 300-day eruption!
On
this date in 1859, Mauna Loa had a brief summit eruption. Then a
stream of lava broke out from the volcano's flank (side), high up but
not at the top. This outbreak of lava created a 32-mile-long lava
flow, the longest in the state of Hawaii.
On
the evening of January 30 the lava began to destroy the village of
Wainanali'i on the west coast of the island. I gather that no lives
were lost, but some people lost everything they owned as well as
their homes. However, since Mauna Loa's lava moves relatively
slowly, many people were able to gather their most precious belongings
and personal effects before escaping to higher ground.
By
January 31 the lava reached the ocean. This was eight days after the
eruption started – and, amazingly, the eruption continued another
292 days! As the lava continued to flow, it filled fishponds and of
course impacted the economy of several communities.
The
science of volcanology was extended during this eruption, since a'a and pahoehoe lava flows could be studied
and compared. It turns out that the two kinds of lava are identical
chemically; the difference is in their temperature. A'a lava flows
become cool enough that they cannot flow, and so a more broken-up,
rougher rock forms, compared to the smooth-flowing pahoehoe lava flows.
A'a lava forming, above, and cool a'a lava, below. |
Pahoehoe lava forming, above, and cool pahoehoe lava, below. |
Also
on this date:
Anniversary of a Record-Setting Dive
Plan ahead:
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