Etna: A History of the Mountain and of its EruptionsRodwell, G. F. (George Farrer)
History
Etna: A History of the Mountain and of its Eruptions
Rodwell, G. F. (George Farrer)
Etna, Mount (Italy)
[Illustration: Sections of Etna]
The "natural boundaries" of Etna are the rivers Alcantara and Simeto on
the North, West, and South, and the sea on the East to the extent of 23
miles of coast, along which lava streams have been traced, sometimes
forming headlands several hundred feet in height. The base of the
mountain, as defined by these natural boundaries, is said to have a
circumference of "at least 120 miles," an examination of the new map,
however, proves that this is over-estimated.
If we take the sea as the eastern boundary, the river Alcantara,
(immediately beyond which Monte di Mojo, the most northerly minor cone
of Etna is situated), as the northern boundary, and the river Simeto as
the boundary on the west and south, we obtain a circumference of 91
miles for the base of Etna. In this estimate the small sinuosities of
the river have been neglected, and the southern circuit has been
completed by drawing a line from near Paterno to Catania, because the
Simeto runs for the last few miles of its course through the plain of
Catania, quite beyond the most southerly stream of lava. The Simeto
(anciently _Simæthus_) is called the Giaretta along the last three miles
of its course, after its junction with the Gurna Longa.
The area of the region enclosed by these boundaries is approximately 480
square miles. Reclus gives the area of the mountain as 1,200 square
kilometres--461 square miles. (_Nouvelle Geographie Universelle_, 1875.)
The last edition of a standard Gazetteer states it as "849 square
miles;" but this estimate is altogether absurd. This would require a
circle having a radius of between sixteen and seventeen miles. If a
circle be drawn with a radius of sixteen miles from the crater, it will
pass out to sea to a distance of 4-1/2 miles on the East, while on the
West and North it will pass through limestone and sandstone formations
far beyond the Alcantara and the Simeto, and beyond the limit of the
lava streams.
Public-domain text, read in full here on John Shaqi.
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