ay be
that, if anything should befall me, your strong arm may succour Winnie;
mine has lost somewhat of its vigour," he whispered.

"Trust me--nothing but death shall sunder us," said the anxious youth in
a burst of enthusiasm.

It seemed as if death were indeed to be the immediate portion of all on
board the _Sunshine_, for a few minutes later there came a crash,
followed by a spout of smoke, fire, steam, and molten lava, compared to
which all that had gone before seemed insignificant!

The crash was indescribable! As we have said elsewhere, the sound of it
was heard many hundreds of miles from the seat of the volcano, and its
effects were seen and felt right round the world.

The numerous vents which had previously been noticed on Krakatoa must at
that moment have been blown into one, and the original crater of the old
volcano--said to have been about six miles in diameter--must have
resumed its destructive work. All the eye-witnesses who were near the
spot at the time, and sufficiently calm to take note of the terrific
events of that morning, are agreed as to the splendour of the electrical
phenomena displayed during this paroxysmal outburst. One who, at the
time, was forty miles distant speaks of the great vapour-cloud looking
"like an immense wall or blood-red curtain with edges of all shades of
yellow, and bursts of forked lightning at times rushing like large
serpents through the air." Another says that "Krakatoa appeared to be
alight with flickering flames rising behind a dense black cloud." A
third recorded that "the lightning struck the mainmast conductor five or
six times," and that "the mud-rain which covered the decks was
phosphorescent, while the rigging presented the appearance of St. Elmo's
fire."

It may be remarked here, in passing, that giant steam-jets rushing
through the orifices of the earth's crust constitute an enormous
hydro-electric engine; and the friction of ejected materials striking
against each other in ascending and descending also generates
electricity, which accounts to some extent for the electrical condition
of the atmosphere.

In these final and stupendous outbursts the volcano was expending its
remaining force in breaking up and ejecting the solid lava which
constituted its framework, and not in merely vomiting forth the
lava-froth, or pumice, which had characterised the earlier stages of the
eruption. In point of fact--as was afterwards clearly ascertained by
careful soundi