Flint's Letters from America, 1818-1820Flint, James, active 19th century
History
Flint's Letters from America, 1818-1820
Flint, James, active 19th century
Ohio River Valley -- Description and travel; United States -- Description and travel
For several miles the road is over a ridge, sixty or eighty feet in
breadth, about eight feet higher than the plain, and five or six feet
higher than the flat ground immediately to the southward. This ridge
or step runs in a winding line, forming a convexity towards the lake,
where it crosses the higher parts of the prairie, and recedes to the
southward, forming a concave curve round hollows in the ground, thus
preserving a horizontal position. A doubt of this having been once the
margin of the lake can scarcely be entertained.
The ridge just mentioned is dry and of a gravelly soil. It is preferred
by the settlers for the sites of their houses. Some patches of the
prairie are inclosed by worn fences, and produce large crops of maize.
Cattle range in the prairies, and are larger and fatter than those
reared by the Ohio River. A few stacks of coarse natural hay stand on
the ground that produced them.
Bloomingtown is a town consisting of about ten houses, and is situated
on a sandy eminence in the edge of the prairie:--a small place, but
deserving of notice from its abortive Bank. A company was formed,
plates engraved, and the bank notes brought to the spot. At the time
when this happened, the people had just become jealous of unchartered
banks. The company applied to the Legislature of the State for a
charter, which was refused. The bankers not venturing to sign the
pictures, but unwilling to lose the expense of manufacturing them,
sold them by auction. They were afterwards subscribed by a fictitious
president and cashier, and fraudulently put into circulation.
{284} Near the lake the shell limestone appears. This seems to be
the base on which the strata of the higher country rests. The higher
country, near Pittsburg, the Muskingum, and Sciota rivers, the
Silver-Creek hills, and the high land, over which I have recently come,
has strata of sandstone, slate-clay, bituminous shale, and, in various
places, coal.
Portland is a town situated on the shore of the indenture in the
south-western extremity of Lake Erie, called Sandusky Bay.[157] It is
only three years since it was founded, and contains thirty dwelling
houses, four warehouses, and has four temporary wharfs. At present
the trade is in salt, brought from Onondago in New York State, and in
imported goods. There is a boat at one of the wharfs, which carries
ten and a half tons; it was built in Connecticut, and was carried by
land over several portages in the way; and I have been told that there
is a vessel of fifty feet keel on the lake, that was carried over the
same obstructions, which lie between Hudson River and Lake Erie. A
steam-boat which sails between Detroit and Buffalo touches at this
place.
Public-domain text, read in full here on John Shaqi.
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