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THE OLD MAN OF VERONA.

BLE

FROM THE GREEK OF CLAUDIAN.*

LEST is the man who in his father's fields

Has past an age of quiet. The same roof That screened his cradle yields a shelter now To his gray hairs. He leans upon a staff

Where as a child he crept along the ground,

And in one cottage he has numbered o'er
A length of years. Him fortune has not
drawn

Into her whirl of strange vicissitudes,
Nor has he drunk, with ever-changing home,
From unknown rivers. Never on the deep,
A merchant, has he trembled at the storm,
Nor as a soldier started at the blare
Of trumpets, nor endured the noisy strife
Of the hoarse-clamoring bar, of the great
world

Simply unconscious. To the neighboring town.
A stranger, he enjoys the free expanse
Of open heaven. The old man marks his year,
Not by the names of consuls, but computes
Time by his various crops; by apples notes
The autumn; by the blooming flower, the
spring.

From the same field he sees his daily sun
Go down and lift again its reddening orb,
And by his own contracted universe
The rustic measures the vast light of day.
He well remembers that broad massive oak
An acorn, and has seen the
grove grow old
Coeval with himself. Verona seems
To him more distant than the swarthy Ind;
He deems the lake Benacus like the shores
Of the red gulf. But, his a vigor hale
And unabated, he has now outlived
Three ages; though a grandsire, green in

years,

*Born in Egypt about 365 A. D.

With firm and sinewy arms. The traveller May roam to farthest Spain: he more has known

Of earthly space; the old man, more of life.

THE EFFIGY OF LOVE.

FROM THE LATIN OF SEXTUS AURELIUS PROPERTIUS†

HAD he not hands of rare device whoe er

First painted Love in figure of a boy? He saw what thoughtless beings lovers were Who blessings lose, whilst lightest cares employ.

Nor added he those airy wings in vain,

And bade through human hearts the godhead fly;

For we are tost upon a wavering main:

Our gale, inconstant, veers around the sky. Nor without cause he grasps those barbed darts,

The Cretan quiver o'er his shoulder cast; Ere we suspect a foe he strikes our hearts,

And those inflicted wounds for ever last. In me are fix'd those arrows-in my breast: But sure his wings are shorn, the boy re

mains;

For never takes he flight, nor knows he rest; Still, still I feel him warring through my

veins.

In these scorch'd vitals dost thou joy to dwell? Oh, shame! To others let thy arrows flee; Let veins untouch'd with all thy venom swell;

Not me thou torturest, but the shade of me. Destroy me who shall then describe the fair?

This my light Muse to thee high glory brings,

When the nymph's tapering fingers, flowing hair, And eyes

of jet and gliding feet she sings.

Translation of ELTON.. Born at Umbria about B. c. 52.

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THE SILURIAN BEACH.

ITH what interest do we look upon any relic of early human history! The monument that tells of a civilization whose hieroglyphic records we cannot even decipher, the slight

est trace of a nation that vanished and left no sign of its life except the rough tools and utensils buried in the old site of its towns or villages, arouses our imagination and excites our curiosity. Men gaze with awe at the inscription on an ancient. Egyptian or Assyrian stone; they hold with reverential touch the yellow parchment-roll whose dim, defaced characters record the meagre learning of a buried nationality; and the announcement that for centuries the tropical forests of Central America have hidden within their tangled growth the ruined homes and temples of a past race stirs the civilized world with a strange, deep wonder. To me it seems that to look on the first land that was ever lifted above the waste of waters, to follow the shore where the earliest animals and plants were created when the thought of God first expressed itself in organic forms, to hold in one's hand a bit of stone from an old sea-beach hardened into rock thousands of centuries ago and studded with the beings that once crept upon its surface or were stranded there by some retreating wave,-is even of deeper interest to men than the relics of their own race, for these things tell

more directly of the thoughts and creative. acts of God.

Standing in the neighborhood of Whitehall, near Lake George, one may look along such a seashore and see it stretching westward and sloping gently southward as far as the eye can reach. It must have had a very gradual slope, and the waters must have been very shallow; for at that time no great mountains had been uplifted, and deep oceans are always the concomitants of lofty heights. We do not, however, judge of this by inference merely we have an evidence of the shallowness of the sea in those days in the character of the shells found in the Silurian deposits, which shows that they belonged in shoal waters.

Indeed, the fossil remains of all times tell us almost as much of the physical condition of the world at different epochs as they do of its animal and vegetable population. When Robinson Crusoe first caught sight of the footprint on the sand, he saw in it more than the mere footprint; for it spoke to him of the presence of men on his desert island. We walk on the old geological shores like Crusoe along his beach, and the footprints we find there tell us too more than we actually see in them. The crust of our earth is a great cemetery where the rocks are tombstones on which the buried dead have written their own epitaphs. They tell us not only who they were and when and where they lived, but much also of the circumstances under which they lived. We

But, although the animals of the early geological deposits indicate shallow seas by their similarity to our shoal-water animals, it must not be supposed that they are by any means the same. On the contrary, the old shells, crustacea, corals, etc., represent types which have existed in all times with the same essential structural elements, but under different specific forms in the several geological periods. And here it may not be amiss to say something of what are called by naturalists representative types.

ascertain the prevalence of certain physical | oceans-a register, in fact, of all the imconditions at special epochs by the presence portant physical changes the earth has unof animals and plants whose existence and dergone. maintenance required such a state of things more than by any positive knowledge respecting it. Where we find the remains of quadrupeds corresponding to our ruminating animals we infer not only land, but grassy meadows also, and an extensive vegetation; where we find none but marine animals we know the ocean must have covered the earth; the remains of large reptiles, representing, though in gigantic size, the half-aquatic, half-terrestrial reptiles of our own period, indicate to us the existence of spreading marshes still soaked by the retreating waters; while the traces of such animals as live now in sand and shoal waters or in mud speak to us of shelving sandy beaches and of mud-flats. The eye of the trilobite tells us that the sun shone on the old beach where he lived, for there is nothing in nature without a purpose; and when so complicated an organ was made to receive the light, there must have been light to enter it. The immense vegetable deposits in the Carboniferous period announce the introduction of an extensive terrestrial vegetation, and the impressions left by the wood and leaves of the trees show that these first forests must have grown in a damp soil and a moist atmosphere. In short, all the remains of animals and plants hidden in the rocks have something to tell of the climatic conditions and the general circumstances under which they lived, and the study of fossils is to the naturalist a thermometer by which he reads the variations of temperature in past times, a plummet by which he sounds the depths of the ancient

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The statement that different sets of animals and plants have characterized the successive epochs is often understood as indicating a difference of another kind than that which distinguishes animals now living in different parts of the world. This is a mistake. They are so-called representative types all over the globe, united to each other by structural relations and separated by specific differences of the same kind as those that unite and separate animals of different geological periods. Take, for instance, mudflats or sandy shores in the same latitudes of Europe and America: we find living on each animals of the same structural character and of the same general appearance, but with certain specific differences, as of color, size, external appendages, etc. They represent each other on the two continents. American wolves, foxes, bears, rabbits, are not the same as the European, but those of one continent are as true to their respective types as those of the other; under a somewhat different aspect they represent the same groups of animals. In certain latitudes or

The

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