The Yankee and the Teuton in WisconsinSchafer, Joseph
History
The Yankee and the Teuton in Wisconsin
Schafer, Joseph
Germans -- Wisconsin; Wisconsin -- Social life and customs
Muscoda as a present-day railway station is inconspicuously located on
the Chicago, Milwaukee and St. Paul line, Prairie du Chien division,
at the distance of fifty-six miles almost due west from Madison, one
hundred and fifty-two from Milwaukee; it is forty-two miles east from
Prairie du Chien. The village was begun at the river bank on the south
side of Wisconsin River, in section 1, township 8 north, range 1 west
of the fourth principal meridian. It stretches south from the river
toward the flanking hills about three-fourths of a mile, the main
portion now clustering about the depot, whereas the “Old Town” lay
farther north and hugged the river bank.
The ground on which Muscoda stands is a portion of the sandy plain,
the outwash of the erosion process by which the Wisconsin and its
larger tributaries worked their way through the sandstone stratum. The
upper courses of these tributaries and the smaller streams which feed
them have laid down flood bottoms of rich alluvium. Often, too, the
bench land of their valleys is a fertile limestone soil intermingled
with clayey patches and occasional streaks of sand. These are all
characteristics of the “Driftless Area,” as the geologists have named
this region, because the various primordial movements of glacial
ice, so influential in modifying the topography elsewhere, passed
around instead of over it, leaving no “drift” upon it. The terrain
is just what the eroding waters in the course of countless ages made
it--a system of regular valleys perfectly drained and bounded by
symmetrically sculptured hills or bluffs, which exhibit a level sky
line and decrease in altitude steadily till at the heads of the streams
they merge in the great plateau or “prairie” of southern Wisconsin. The
valleys make natural and not ill-graded highways from the prairie to
the Wisconsin River, while the ranges of bluffs separating them appear
like promontories running out fingerwise from the main plateau and
terminating either where two smaller streams converge or at the edge of
the lower plain laid down by the Wisconsin.
Public-domain text, read in full here on John Shaqi.
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