accordingly, as if taking
her dispositions for his conduct after her death, asked her what she
thought of his marrying, in that contingency, a certain lady, whose
name he mentioned, whereupon she rose in her bed in such a rage at the
suggestion (the woman being her especial detestation) that she threw
off all the symptoms of illness, and the next day went about the house
as usual. This cure proved a grave misfortune to the whole family.
In spite of my aversion I was sent back to New York the next autumn
for another winter's schooling. I landed from the steamer at the foot
of Cortlandt Street two or three days after a great fire in New York,
and I saw the ruins still smoking and the firemen playing on them.
My baggage--a biscuit box, with my scanty wardrobe and a bag of
hickory-nuts for my city cousins--I carried on my shoulders and walked
the length of the city, my brother living in what was then farther New
York, in Seventh Street, near the East River. At that time Fourteenth
Street was the extreme limit of the city's growth, except for a few
scattering residences. Beyond, and, on the East River side, even most
of what lay beyond Seventh Street, was unreclaimed land. I sailed my
toy boats on the salt marshes where Tompkins Square now is, and I used
to shoot, botanize, and hunt for crystals all over the island beyond
Thirty-Second Street, the land being sparsely inhabited. I discovered
a little wild cactus growing freely amongst the rocks, and carried
a handkerchief full of it home, getting myself well pricked by the
spines, but to my botanical enthusiasm this was nothing in view of the
discovery. Only here and there patches of arable land maintained small
farmhouses, but the greater part of the surface of Manhattan Island
was composed of a poor grazing land, interspersed with rolling ledges
of bare granite, on which were visible what were then known as
"diluvial scratches," which my brother Charles, who was an ardent
naturalist, explained to me as the grooves made by the irruption of
the deluge, which carried masses of stone across the broad ledges and
left these scratches, then held widely as testimony to the actuality
of the great deluge of Genesis. I think that we had to wait for
Agassiz to show us that the "diluvial scratches" were really glacial
abrasions, caused by the great glacier which came down the valley of
the Hudson and went to sea off Sandy Hook. At this time my brother was
making conchology his special
|