Summary Narrative of an Exploratory Expedition to the Sources of the Mississippi River, in 1820: Resumed and Completed, by the Discovery of its Origin in Itasca Lake, in 1832Schoolcraft, Henry Rowe
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Summary Narrative of an Exploratory Expedition to the Sources of the Mississippi River, in 1820: Resumed and Completed, by the Discovery of its Origin in Itasca Lake, in 1832
Schoolcraft, Henry Rowe
Great Lakes (North America); Mississippi River -- Sources; Northwest, Old -- Description and travel
Longitude of Detroit, calculated from above 82 54 53
Latitude of camp near head of Lake Michigan,
Aug. 31 and Sept. 1 41 38 48
Mean latitude of the extreme south point of Lake
Michigan, 4 sets of observations and meridian
observation 41 37 28
Latitude of camp next north of the St. Joseph's,
near Kekalamazo, Sept. 3 42 32 16
Latitude of camp at Maskegon River, Sept. 4 43 13 41
Latitude of camp near Point aux Salles, Lake
Michigan, Sept. 5 44 5 17
Latitude of camp at Grand Traverse Bay, Lake
Michigan, Sept. 7 45 34 24
[203] _Galet_, in the Canadian patois, means a smooth, flat
rock.--H. R. S.
[204] A little doubtful.
[205] A little doubtful.
[206] Or 20´´.
3. MINERALOGY AND GEOLOGY.
VI.
_Report on the Copper Mines of Lake Superior._ By HENRY R. SCHOOLCRAFT.
To the Hon. JOHN C. CALHOUN, _Secretary of War_.
VERNON (Oneida County, N. Y.), November 6, 1820.
SIR: I have now the honor to submit such observations as have occurred
to me, during the recent expedition under GOV. Cass, in relation to the
copper mines on Lake Superior; reserving, as the subject of a future
communication, the facts I have collected on the mineralogy and geology
of the country explored generally.
The first striking change in the mineral aspect of the country north of
Lake Huron, is presented near the head of the Island of St. Joseph, in
the River St. Mary, where the calcareous strata of secondary rocks are
succeeded by a formation of red sandstone, which extends northward to
the head of that river at Point Iroquois, producing the falls called the
_Sault de Ste. Marie_, fifteen miles below; and thence stretching
northwest, along the whole southern shore of Lake Superior, with the
interruptions noted, to Fond du Lac.
This extensive stratum is perforated at various points by upheaved
masses of sienitic granite and trap, which appear in elevated points on
the margin of the lake at Dead River, Keweena Point, Presque Isle, and
the Chegoimagon Mountains. It is overlaid, in other parts, by a stratum
of gray or neutral-colored sandstone, of uncommon thickness, which
appears in various promontories along the shore, and, at the distance of
ninety miles from Point Iroquois, constitutes a lofty perpendicular and
caverned wall, upon the water's edge, called the Pictured Rocks.
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