Martyria; or, Andersonville PrisonHamlin, Augustus C. (Augustus Choate)
History
Martyria; or, Andersonville Prison
Hamlin, Augustus C. (Augustus Choate)
Andersonville Prison; United States -- History -- Civil War, 1861-1865 -- Prisoners and prisons
The inequalities of the earth's surface are like the rugosities of the
human brain: the depths of the one contain the richest and most
inexhaustible treasures of mineral wealth, as the wrinkles of the other
collect the stores of mental lore. As the surface of the brain becomes
less marked and rugged, the strength and scope of the mind vanish, and
approach the standard of the lower animals; and likewise, as the elevated
lands of the earth shrink in form, and sink into the level of the plain,
so the characters of the races who inhabit them lose force and elevation.
Sometimes the minds of men are the reflections of the beauties and
sublimities of nature. Sometimes men become degraded, and nature then does
not inspire.
XXXI.
The lofty and diversified mountain range, or system of ranges, known as
the Appalachian or Alleghany, rises or reappears in the State of New York,
midway between the Atlantic coast and the shores of those fresh-water
seas, Erie and Ontario. It then stretches down south-westward, with its
adjacent spurs, through the great States of Pennsylvania and Virginia;
then, dividing, it forms, with its eastern range, the western and northern
limit of North and South Carolina and Georgia; and with the western it
intersects Tennessee, forming that beautiful basin known among the white
men as East Tennessee, but among the traditions of the red men as the
Garden of the Manitou--their God. In Northern Alabama, the separated
ranges seemingly unite; and passing southward, towards the central portion
of the State, the mountain summits gradually contract, and finally sink
into the level of the great alluvial plains, which stretch away, without
undulation, to the shores of the Gulf. These huge masses of rock,
dislocated and elevated like the Vosges and the Hartz Mountains at the
close of the carboniferous or devonian period of the earth's age, contain,
with the adjacent and connecting bands,--which are composed of the
silurian, primitive, and metamorphic ledges,--most of the accessible
mineral wealth of the republic. And the collective beds of iron, coal,
marble, zinc, copper, and gold are unsurpassed in similar extent and
richness by the mines of any country of the known world, with the
exception of those wonderful deposits of ores and minerals among the
unexplored and almost inaccessible recesses and plateaus of the Sierra
Nevada or the Andes.
Public-domain text, read in full here on John Shaqi.
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