Old Mackinaw; Or, The Fortress of the Lakes and its SurroundingsStrickland, W. P. (William Peter)
History
Old Mackinaw; Or, The Fortress of the Lakes and its Surroundings
Strickland, W. P. (William Peter)
Great Lakes (North America); Mackinac Island (Mich. : Island) -- History; Michigan -- History
The first thing we shall notice as a natural attraction on the island,
is what is called "The Arch Rock." This is a natural arch projecting
from the precipice on the northeastern side of the island, about a
mile from the fort, and elevated about one hundred and forty feet
above the level of the water. Its abutments are formed of calcareous
rock, and have been produced by the falling down of great masses of
rock, leaving a chasm of eighty or ninety feet in height, and covered
by the arch which spans it of fifty or sixty feet sweep. The scene
presented by cliff and chasm is one of wild grandeur. Like the Natural
Bridge of Virginia, it possesses an attraction to all fond of natural
curiosities, sufficient of itself to justify a visit to the northern
lakes. The view from the beach is particularly grand. Before you is a
magnificent arch suspended in mid air. Indian tradition says that this
wonderful arch was formed by the giant spirits who inhabited this
island. Geological tradition, however, indicates that it was formed by
the action of the waters, which were at a remote period much higher
than at the present time.
The next object which strikes the attention of the visitors is the
"Sugar Loaf Rock," a high, isolated, conical rock which, resting upon
the elevated plateau that forms the next highest point of the island
from that of Fort Holmes, exhibits a rise of some sixty to eighty
feet. This is but little less than the elevation of the ridge which
forms the crowning plan of the island, and upon which the dismantled
post of Fort Holmes is seen, being separated therefrom by a distance
not exceeding one hundred and fifty yards. By what violent throe of
nature it has become severed from the adjacent ridge, of which it no
doubt, formed a part, is matter of curious inquiry. Has nature done
this by gradual recession, or by the slow upheaval of the land? On
inspection, this rock is found cavernous, slightly crystalline, with
its strata distorted in every conceivable direction. In its crevices
grow a few cedars and vines. As the visitor approaches it by the road
side its effect is grand and imposing; still more so, perhaps, when
beheld from the top of the ridge, where its isolated position with its
bold form, breaking the outline of the island, strikes the beholder
with wonder and admiration.
Public-domain text, read in full here on John Shaqi.
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