Is a Ship Canal Practicable?: Notes, Historical and Statistical, Upon the Projected Routes for an Interoceanic Ship Canal Between the Atlantic and Pacific Oceans, in Which is Included a Short Account of the Character and Influence of the Canal of Suez, and the Probable Effects Upon the Commerce of the World of the Two Canals, Regarded Either as Rivals, or as Parts of One System of Interoceanic NavigationAbert, S. T. (Silvanus Thayer)
History
Is a Ship Canal Practicable?: Notes, Historical and Statistical, Upon the Projected Routes for an Interoceanic Ship Canal Between the Atlantic and Pacific Oceans, in Which is Included a Short Account of the Character and Influence of the Canal of Suez, and the Probable Effects Upon the Commerce of the World of the Two Canals, Regarded Either as Rivals, or as Parts of One System of Interoceanic Navigation
Abert, S. T. (Silvanus Thayer)
Canals, Interoceanic
The Penaebach tunnel is the only one in England that is self-supporting.
It is driven through solid basalt. The Penmaenwhr tunnel, pierced
through hard green-stone, had to be lined throughout; and the Bangor
tunnel, supposed to be sufficiently firm, was afterward cased with
brick. It has been found necessary to line some of the tunnels of the
Washington aqueduct, which are driven through very hard gneiss.
Before taking leave of this instructive report, we have selected some
interesting portions of the narrative and scientific statements for
quotation:
“The great falls of the Hingador are grand and exceedingly romantic,
and equal in height and beauty to many of those in other countries
which elicit so much admiration from all lovers of magnificent scenery.
The valley itself is pleasant to gaze upon; many bright streams gush
into it, and impart additional charms to the already picturesque
landscape of falls and rapids, and rich tropical vegetation. Several
thermal springs were discovered at the foot of the great falls.
“As the party had to wade through the water, over smooth and slippery
rocks, and clamber up steep precipices, it took four days to accomplish
this section of the survey. Several fragments of rocks were broken
off at the head of the falls for subsequent analysis. According to
the report of the geologist, of which the following is an extract,
‘the rocky falls were found to be overcoated with a light, shaly
conglomerate of a cemented texture, and containing, imbedded in a
calcareous matrix, coarse sand and gravel. Higher up, in one of the
western head branches of this stream, a more consolidated semi-rock was
noticed, containing copiously interspersed fragments of little shells.
This rock seems also to be impregnated with carbonate of lime.’”
Public-domain text, read in full here on John Shaqi.
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