The Geology of Minnesota volume 1
The Geology of Minnesota volume 1
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In our eReader you can find the full English version of the book. Read The Geology of Minnesota volume 1 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 1
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Rolling glacial drift thus traced from Iowa into Minnesota was probably accumulated as a terminal moraine at the end of the ice-lobe which extended southeastward from the Leaf hills and the Head of the Coteau des Prairies, as more fully explained on page 406; but at a late part of the epoch, after two distinct recessions of the ice had taken place in south- western Minnesota. When this lobe of the ice-sheet attained its greatest area it terminated on the south in the vicinity of Des Moines, and... was bounded on its sides by the outermost belt of hilly and knolly drift deposits. On its east side only two morainic belts are found, but on its west side three are clearly distinguished in the west edge of this state and the east edge of Dakota. * At the time of accumulation of the second belt of morainic drift, the end of this ice-lobe had receded to Mineral ridge in the north part of Boone county, Iowa; and when the third belt was formed, its extremity appears to have been in Hancock county, Iowa.
What to read after The Geology of Minnesota volume 1?
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:
Rolling glacial drift thus traced from Iowa into Minnesota was probably accumulated as a terminal moraine at the end of the ice-lobe which extended southeastward from the Leaf hills and the Head of the Coteau des Prairies, as more fully explained on page 406; but at a late part of the epoch, after two distinct recessions of the ice had taken place in south- western Minnesota. When this lobe of the ice-sheet attained its greatest area it terminated on the south in the vicinity of Des Moines, and... was bounded on its sides by the outermost belt of hilly and knolly drift deposits. On its east side only two morainic belts are found, but on its west side three are clearly distinguished in the west edge of this state and the east edge of Dakota. * At the time of accumulation of the second belt of morainic drift, the end of this ice-lobe had receded to Mineral ridge in the north part of Boone county, Iowa; and when the third belt was formed, its extremity appears to have been in Hancock county, Iowa.
What to read after The Geology of Minnesota volume 1?
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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