The Geology of Minnesota volume 6
The Geology of Minnesota volume 6
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In our eReader you can find the full English version of the book. Read The Geology of Minnesota volume 6 Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book The Geology of Minnesota volume 6
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Such shale is the effect of cotemporary volcanic eruption of the Manitou igneous epoch.
*The most northern point at which these rocks are known in this county is in the north part of sec. 25, T. 45-17, nearly on the divide between the highest sources of the Willow river and thc_' Nemadji.
PLATE C A H L T O N COUNTY GEOLOGICAL AM) NATURAL HISTORY Sl'RVEYOK MINNESOTA IM N E C O UN TV BY WARREN UPHAM l-:xplanation.
I MotffnedJ}ri/i, flaiai iwduiatwo ... -fife.
/;// uiultiliJli. 'iti or roltin, 7>H..., km>U\' and hill\, Terminal Moraines Utttckle-vSt C H I S A G O COUNTY ( OnlOUI' Lines arc drawn appro* irruUflv for each >(' feet a&ow the . Fffi PINE COUNTY, 1888. WARREN UPHAM.
The drift in the main was derived from the region to the. Northeastward. It is less thick than in most of the country to the west, averaging about seventy-five feet. But south of Snake river the drift contains limestone boulders and gravel, evidently from the west or northwest. A distinctly morainic tract about six miles wide enters the county from Chisago county, and another from Aitkin county of about the same width.
What to read after The Geology of Minnesota volume 6?
You can find similar books in the "Read Also" column, or choose other free books by Geological And Natural History Survey of Minnesota to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Such shale is the effect of cotemporary volcanic eruption of the Manitou igneous epoch.
*The most northern point at which these rocks are known in this county is in the north part of sec. 25, T. 45-17, nearly on the divide between the highest sources of the Willow river and thc_' Nemadji.
PLATE C A H L T O N COUNTY GEOLOGICAL AM) NATURAL HISTORY Sl'RVEYOK MINNESOTA IM N E C O UN TV BY WARREN UPHAM l-:xplanation.
I MotffnedJ}ri/i, flaiai iwduiatwo ... -fife.
/;// uiultiliJli. 'iti or roltin, 7>H..., km>U\' and hill\, Terminal Moraines Utttckle-vSt C H I S A G O COUNTY ( OnlOUI' Lines arc drawn appro* irruUflv for each >(' feet a&ow the . Fffi PINE COUNTY, 1888. WARREN UPHAM.
The drift in the main was derived from the region to the. Northeastward. It is less thick than in most of the country to the west, averaging about seventy-five feet. But south of Snake river the drift contains limestone boulders and gravel, evidently from the west or northwest. A distinctly morainic tract about six miles wide enters the county from Chisago county, and another from Aitkin county of about the same width.
What to read after The Geology of Minnesota volume 6?
You can find similar books in the "Read Also" column, or choose other free books by Geological And Natural History Survey of Minnesota to read onlineMoreLess
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