| Everyone
has heard about Krakatoa - its got such a lovely name. And in 1883,
people living 3,000 miles from the volcano heard the sound as Krakatoa
exploded - the loudest sound ever made. Most people thought it was a
naval bombardment. And for years afterwards, the colourful sunsets
caused by the volcano's dust were much admired. And in New York State
a fire crew set off to fight a fire which turned out to be a
particularly vivid setting of the sun!
But we, as geologists, are not concerned with such ephemera. We
need to know the causes of the eruption and what it means in the
context of plate tectonics. Simon Winchester aims to satisfy both
markets. The book is full of the background of the Dutch East Indies
(for, of course, Krakatoa was a Dutch colony at the time). Not only
this but everything else about the East Indies is incorporated. If you
want to know about the Wallace Line, you can find out about it here.
Actually the Wallace Line (Australian fauna to the east, Indian to the
west) is a consequence of the geology, but at some remove from the
essentials of the story.
But it does allow him a good way of introducing Wegener and
Continental Drift - and a series of entertaining stories. I
particularly liked his tale about Harry Hess, one of the Godfathers of
Plate Tectonics.
Winchester was Chairman of the Oxford University Geological
Society. In a magnificent coup they had managed to get Hess to lecture
to them and all the scientific big-wigs were to attend the lecture.
But first the committee had to dine (and wine) the speaker. On the way
back from a country restaurant the car broke down, they had a long
walk to a pub, where Hess had a few whiskies, eventually a taxi turned
up, but not before Hess had had a few more whiskies. They got to the
Lecture Theatre at 10, and the audience was still there. Hess later
said it was one of the most amusing and satisfying evenings of his
life, but the big-wigs were not very amused by the late start, slurred
speech, maps falling down, people falling over and projectors fusing.
All in all it makes our taking our speakers to Browns sound very tame.
The heart of the book is the account of what happened when Krakatoa
erupted and there is certainly a lot about that. I liked the picture
of a Dutch gun boat stranded 2 miles from the sea, upright and not
much damaged but the crew dead. The stories of people trying to outrun
the tsunamis are frightening. It was these “tidal waves” which were
the mass killers of the eruption.
The geological explanation of the explosion could not be given at
the time of the eruption. Why the volcano was where it was is now
easily explained by Plate Tectonics and this Winchester does - but so
subtly that the explanation needs to be sought out.
If you want a detailed exposition of the geology of the Sunda
Straits, this is not the place to look. But for a picture of life
before and after the eruption in and about Java the book is a treasure
trove.
The reporting of the eruption is used to illustrate the
connectedness of the world brought about by the new submarine
telegraphs - enabled by the discovery of the insulating gutta percha
in the East Indies! The news was around the world in a few hours.
This book could have been a lot shorter and covered the subject of
its title adequately. But it is all the better for being longer and
discursive. One sometimes thinks that not a note made by Winchester
goes to waste - everything gets thrown into the mix. But mostly it is
a very entertaining mix.
A good book which hides its learning well and which will tell you
lots of things you did not know - or even think that you wanted to
know.
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