CHAPTER XIII.
Michigan Agricultural Reports for 1854 — Professor Thomas's Report — Report of J. S. Dixon — Products of States — Climate — Army Meteorological Reports.
From the Agricultural Reports of the State of Michigan we take the following:—
"From old Fort Mackinaw to the Manistee River, the land immediately upon the lake shore, and not unfrequently extending back for many miles, is considerably elevated, and occasionally rises very abruptly to the height of from one hundred to three or four hundred feet. The country (more particularly the northern portion) continues to rise as we proceed into the interior, until it attains an elevation equal to any other portion of the peninsula.
"This is more particularly the case in the rear of Traverse Bay, where this elevation continues for many miles into the interior, giving to the landscape a very picturesque appearance when viewed from some of the small lakes, which abound in this as well as in the more southern portion of the State.
"The tract of country under consideration is based on limestone, sandstone, and shales, which are covered, excepting at a few points, with a deposit of red clay and sand, varying in thickness from a few inches to more than four hundred feet. The interior of the northern portion of the peninsula, west of the meridian, is generally more rolling than that on the east. It is interspersed with some extensive cedar swamps and marshes, on the alluvial lands, and in the vicinity of heads of streams and some of the lakes. The upland is generally rolling, has a soil of clay, loam and sand, and is clad with evergreen timber, intermixed with tracts of beech and maple, varying in extent from a few acres to several townships. Several of the most extensive of these tracts are in the vicinity of the Cheboygan and Tahweegon rivers, their lakes and tributary streams. There are also large tracts of beech and maple timber lying between the head of Grand Traverse Bay, and the Manistee and Muskeegon rivers.
"The elevated portion of land on the shore of Lake Michigan, known as the 'Sleeping Bear' as well as Manitou Island, (see latitude 45) which, when viewed from a distance, has the appearance of sand, is found to be composed of alternate layers of highly marly clay and sand. The clay is of a deep red color, and in many places its strata are much contorted.
"The hilly region, to which allusions have been made, is mostly heavily timbered with beech, maple, bass, oak, ash, elm, birch, etc., interspersed with an occasional cedar swamp. In the vicinity of Grand Traverse Bay, this character of country extends into the interior for many miles, bordering on a series of small and beautiful lakes, which vary in length from two to eighteen miles, and are generally free from marsh and swamp. This country, as also that in the interior from Little Traverse Bay, is well adapted to the purposes of agriculture.
"Passing south of this rolling district, the country becomes less elevated and more variable, the soil assuming a more sandy character, and being generally clad with evergreen timber. There are, however, exceptions to this in some fine tracts of beech and maple near the lake coast, also, in the vicinity of some of the streams in the interior.
"It is nevertheless true, that there are many extensive swamps and marshes in this part of the peninsula, but it is doubted whether, upon the whole, they exceed the quantity or extent of those of the more southern part of the State.