. Annual report. Geological and Natural History Survey of Minnesota; Geology; Natural history. STATE GEOLOGIST. 19 about W NW, in harmony with the structure which is seen on the south shore of Oak lake. In some places a thin, even slaty structure is evinced in the fine-grained parts; and on making search farther north about two rods there is an appearance of fragments of the fine in the coarse. 2033 represents the rock thus included in the granite (?). 2034. At 15 rods east of Oak portage, on the Canadian side of Saganaga lake, a light-colored, feldspathic rock with quartzes, perhaps fragmenta
. Annual report. Geological and Natural History Survey of Minnesota; Geology; Natural history. STATE GEOLOGIST. 19 about W NW, in harmony with the structure which is seen on the south shore of Oak lake. In some places a thin, even slaty structure is evinced in the fine-grained parts; and on making search farther north about two rods there is an appearance of fragments of the fine in the coarse. 2033 represents the rock thus included in the granite (?). 2034. At 15 rods east of Oak portage, on the Canadian side of Saganaga lake, a light-colored, feldspathic rock with quartzes, perhaps fragmental,butitcan hardly be distinguished from a massive crystalline granite. It lacks, however, the dark elements of granite, and is not fresh and sharp. It shows pyrites and Fig. 2. Wave Marks in Recomposed Granite near Oak Portage, Saganaga Lake. At a point about 20 rods east of Oak portage, on the Can- adian side of Saganaga lake, is a curiously marked surface of this supposed "granite," a structure which is quite unlike any. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Geological and Natural History Survey of Minnesota. St. Paul : Geological and Natural History Survey of Minnesota
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Keywords: ., bookcentury1800, bookdecade1870, booksubjectgeology, booksubjectn
