coast, between the island of Manaar and Karativoe, the natives,
in addition to fishing for chank shells[1] in the sea, dig them up in
large quantities from beneath the soil on the adjacent shores, in which
they are deeply imbedded[2], the land having since been upraised.
[Footnote 1: _Turbinella rapa_, formerly known as _Voluta gravis_ used
by the people of India to be sawn into bangles and anklets.]
[Footnote 2: In 1845 an antique iron anchor was found under the soil at
the northwestern point of Jaffna, of such size and weight as to show
that it must have belonged to a ship of much greater tonnage than any
which the depth of water would permit to navigate the channel at the
present day.]
The sand, which covers a vast extent of the peninsula of Jaffna, and in
which the coco-nut and Palmyra-palm grow freely, has been carried by the
currents from the coast of India, and either flung upon the northern
beach in the winter months, or driven into the lake during the
south-west monsoon, and thence washed on shore by the ripple, and
distributed by the wind.
The arable soil of Jaffna is generally of a deep red colour, from the
admixture of iron, and, being largely composed of lime from the
comminuted coral, it is susceptible of the highest cultivation, and
produces crops of great luxuriance. This tillage is carried on
exclusively by irrigation from innumerable wells, into which the water
rises fresh through the madrepore and sand; there being no streams in
the district, unless those percolations can be so called which make
their way underground, and rise through the sands on the margin of the
sea at low water.
_Wells in the Coral Rock_.--These phenomena occur at Jaffna, in
consequence of the rocks being magnesian limestone and coral, overlying
a bed of sand, and in some places, where the soil is light, the surface
of the ground is a hollow arch, so that it resounds as if a horse's
weight were sufficient to crush it inwards. This is strikingly
perceptible in the vicinity of the remarkable well at Potoor[1], on the
west side of the road leading from Jaffna to Point Pedro, where the
surface of the surrounding country is only about fifteen feet above the
sea-level. The well, however, is upwards of 140 feet in depth; the water
fresh at the surface, brackish lower down, and intensely salt below.
According to the universal belief of the inhabitants, it is an
underground pool, which communicates with the sea by a subterranean
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