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
[234] This metal has subsequently (namely, in 1844) been found to
constitute a percentage in the native copper of the Eagle River mines
of Lake Superior. Traces of it were found in a mass of native copper
found on the shores of Keweena Lake, by Mr. Moliday, in 1826. A mass
of pure silver was discovered in a boulder in the drift of Lake
Huron, west of White Rock, in 1824. These discoveries induce the
belief that this element will be found to be extensively present in
the eventual metallurgic operations of the Lake Superior basin.
b. _Silicious Minerals._
1. QUARTZ.
This interesting species being distributed in its numerous varieties
throughout the region visited, I shall confine my notices to a few
localities.
Subs. 1.--_Common Quartz._
Occurs in the form of large water-worn masses along the shores of Lakes
Huron, Michigan, and Superior. Also, in veins in the granite of Lake
Superior, and in the argillite of St. Louis River. These localities all
consist of the opaque varieties, with a slight degree of translucence
in some places. It exists in mass at Huron Bay, Lake Superior, and in
fragments of red jasper on Sugar Island, St. Mary's River.
1. _Radiated Quartz._--In detached masses on the Grange, and also at the
rapids of the River Desmoines, on the Upper Mississippi. At the Grange,
the crystals, which are usually minute, sometimes possess a cinnamon
color, or pass into a variety of crystallized ferruginous quartz.
2. _Tabular Quartz._--In small, flattened masses along the shores of
Lake Pepin. These masses are transparent, or only translucent. Their
color is generally white, but sometimes yellow. They appear to be
closely allied to chalcedony.
3. _Greasy Quartz._--In detached masses along the shores of Lake
Superior.
4. _Granular Quartz._--At the Falls of Puckaiguma, on the Upper
Mississippi, in large, compact beds rising through the soil. Also, in
some conditions of the cliffs commencing at the Falls of St. Anthony,
Carrer's Cave, &c.
5. _Arenaceous Quartz._--This is sometimes the condition of fine,
even-grained, translucent sand rock of the preceding localities.
Valuable as an ingredient of glass.
6. _Pseudomorphous Quartz._--On the shores of Lake Pepin, occasionally.
These masses appear to have taken their crystalline _impress_ from
rhomboidal crystals of carbonate of lime.
7. _Amethystine Quartz._--In the trap-rock of Lake Superior.
Subs. 2.--_Amethyst._
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