Engineering Wonders of the World
Volume III
Forfatter: Archibald Williams
År: 1945
Serie: Engineering Wonders of the World
Forlag: Thomas Nelson and Sons
Sted: London, Edinburgh, Dublin and New York
Sider: 407
UDK: 600 eng- gl
With 424 Illustrations, Maps, and Diagrams
Søgning i bogen
Den bedste måde at søge i bogen er ved at downloade PDF'en og søge i den.
Derved får du fremhævet ordene visuelt direkte på billedet af siden.
Digitaliseret bog
Bogens tekst er maskinlæst, så der kan være en del fejl og mangler.
242 ENGINEERING WONDERS OF THE WORLD.
THE SOLANI AQUEDUCT, WHICH CARRIES THE GANGES CANAL OVER THE SOLANI RIVER.
It has 15 arches of 50 feet span, is 195 feet broad, and passes a stream of water 172 feet across and 9 feet deep.
into the cribs till its top is at the level of the
water which, during construction, had been
flowing over it.
The boulder dam when complete is, of course,
very leaky. This is remedied partially by sink-
ing grass mattresses on the up-stream face, and
throwing on to them boulders, shingle, and
soil until an almost watertight embankment
has been formed, to direct the river into the
channel feeding the canal. It may seem
strange that so primitive a structure should
be a mainstay of the prosperity of a large
tract of country. But so it is, and the canal
has worked effectively for half a century.
The Ganges Canal has a maximum capacity
of 7,000 cubic feet a second. This great vol-
ume of water is carried by level crossings
through some rivers, over
The Solani an(j jn aqueducts, the
Aqueduct.
most notable of which—that
over the Solani—has fifteen arches of 50-foot
span, is 195 feet broad, and gives passage to
a stream 172 feet broad and 9 feet deep. We
may notice that in some cases a river is led
over a canal; for instance, a river 400 feet
The Forma-
tion of
Deltas.
broad and 9 feet deep in flood crosses the
Sirhind Canal at a height of 24 feet.
On the eastern coast the rivers, as they
approach the sea, become deltaic. In their
lower reaches the reduced velocity of the stream
causes the matter eroded in
swifter upper reaches ,to be
deposited, and so raises the bed
until the water overflows. The
silt is then deposited on the land, the general
level of which rises until the water is once
more confined. This process is repeated
along the banks and at the river’s mouth
until a great fan-shaped body of land has
been pushed out into the sea, traversed by
the several branches into which the river has
divided. These branches run along the ridges
of the country, a condition of affairs which is
ideal for irrigation.
In the delta of the Godaveri a weir spans
the river at Dowlaishweran, holds up the level
of the water, and compels the stream to flow
into three main canals. These supply many
branch canals, which feed many more dis-