A Short History of the WorldWells, H. G. (Herbert George)
History
A Short History of the World
Wells, H. G. (Herbert George)
World history
Slowly by degrees as one million of years followed another, this fiery
scene would lose its eruptive incandescence. The vapours in the sky
would rain down and become less dense overhead; great slaggy cakes of
solidifying rock would appear upon the surface of the molten sea, and
sink under it, to be replaced by other floating masses. The sun and
moon growing now each more distant and each smaller, would rush with
diminishing swiftness across the heavens. The moon now, because of its
smaller size, would be already cooled far below incandescence, and
would be alternately obstructing and reflecting the sunlight in a
series of eclipses and full moons.
ANOTHER SPIRAL NEBULA
ANOTHER SPIRAL NEBULA
_Photo: G. W. Ritchey_
And so with a tremendous slowness through the vastness of time, the
earth would grow more and more like the earth on which we live, until
at last an age would come when, in the cooling air, steam would begin
to condense into clouds, and the first rain would fall hissing upon the
first rocks below. For endless millenia the greater part of the
earth’s water would still be vaporized in the atmosphere, but there
would now be hot streams running over the crystallizing rocks below and
pools and lakes into which these streams would be carrying detritus and
depositing sediment.
LANDSCAPE BEFORE LIFE
LANDSCAPE BEFORE LIFE
“Great lava-like masses of rock without traces of soil”
At last a condition of things must have been attained in which a man
might have stood up on earth and looked about him and lived. If we
could have visited the earth at that time we should have stood on great
lava-like masses of rock without a trace of soil or touch of living
vegetation, under a storm-rent sky. Hot and violent winds, exceeding
the fiercest tornado that ever blows, and downpours of rain such as our
milder, slower earth to-day knows nothing of, might have assailed us.
The water of the downpour would have rushed by us, muddy with the
spoils of the rocks, coming together into torrents, cutting deep gorges
and canyons as they hurried past to deposit their sediment in the
earliest seas. Through the clouds we should have glimpsed a great sun
moving visibly across the sky, and in its wake and in the wake of the
moon would have come a diurnal tide of earthquake and upheaval. And
the moon, which nowadays keeps one constant face to earth, would then
have been rotating visibly and showing the side it now hides so
inexorably.
The earth aged. One million years followed another, and the day
lengthened, the sun grew more distant and milder, the moon’s pace in
the sky slackened; the intensity of rain and storm diminished and the
water in the first seas increased and ran together into the ocean
garment our planet henceforth wore.
But there was no life as yet upon the earth; the seas were lifeless,
and the rocks were barren.
III
THE BEGINNINGS OF LIFE
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account