A History of the Coldstream Guards, from 1815 to 1895Ross, J. (John)
History
A History of the Coldstream Guards, from 1815 to 1895
Ross, J. (John)
Great Britain -- History -- Victoria, 1837-1901; Great Britain. Army. Coldstream Guards
Kinglake, iii. 123, etc., 194, 347. Sir Edmond Lyons urged the
immediate assault of the Malakoff hill, “then unoccupied, and advised
the immediate construction of a battery there, which would make it
necessary for the fleet to take care of themselves” (_Ibid._, iii.,
Appendix, p. 491). The capture of the Malakoff in September, 1855,
caused the immediate fall of Sevastopol.
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The serious and very reasonable apprehension entertained by the Russian
chiefs did not, however, prevent them from taking every measure to
fortify their position, directly they understood that the Allies were
approaching the south side in force. The greatest activity prevailed day
and night in the garrison and among the inhabitants, the women and
children taking their share of the labour, and thus the works designed
by the Russian Engineer Officer, Todleben, were rapidly thrown up. The
Anglo-French Commanders never interrupted these operations, nor did they
make any demonstrations to try the quality of the defences; they
contented themselves with distant reconnaissances, so that in a short
time the entrenchments were greatly strengthened, especially the
Malakoff, and began to look more formidable than had been the case
before; the armament also was being changed, the lighter guns giving
place to heavier ordnance drawn from the ships and arsenal.
The upland of the Chersonese, on which the Allies had established
themselves, is a sloping plain, trending from a line of hills called the
Sapuné Ridge, 500 to 700 feet high, that bounds it on the east, from the
head of the roadstead of Sevastopol to a point on the coast some four
miles west of Balaklava. The upland is scored by numerous ravines,
running from the ridge in a general north-westerly direction to the town
and coast; but on the eastern side of the ridge the ground falls
abruptly and almost in a cliff-like manner into the valley of the
Tchernaya river, which discharges itself into the roadstead. The
distance from Balaklava to Sevastopol is nearly eight miles. Of the two
roads connecting them, one, the Woronzoff road, was metalled, and,
proceeding along the Causeway Heights, formed the main communication
with the south of the Crimean peninsula; the other, a mere cart-track or
pathway, more to the south, ascended the ridge over the “Col de
Balaklava,” three miles from that place, and joined the Woronzoff road
two miles further on, on the upland.
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