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| Author | : Terrance F. Anstett |
| Publisher | : |
| Total Pages | : 192 |
| Release | : 1977 |
| Genre | : Geology |
| ISBN | : |
| Author | : Glen Steven Tanck |
| Publisher | : |
| Total Pages | : 366 |
| Release | : 1977 |
| Genre | : Geology |
| ISBN | : |
| Author | : |
| Publisher | : |
| Total Pages | : 160 |
| Release | : 1978 |
| Genre | : Geology |
| ISBN | : |
| Author | : Patrick J. Julig |
| Publisher | : University of Ottawa Press |
| Total Pages | : 331 |
| Release | : 2002-01-01 |
| Genre | : Social Science |
| ISBN | : 1772821551 |
First excavated in the early 1950s, the Sheguiandah site had remained enigmatic for half a century. This volume details controversial early claims that the site had been occupied before the last Ice Age, then covers more recent studies of the geological and botanical history of the area – including new evidence that the site was uninhabited until after the retreat of the glaciers.
| Author | : John J. Mortenson |
| Publisher | : |
| Total Pages | : 308 |
| Release | : 1981 |
| Genre | : Geology |
| ISBN | : |
| Author | : Mark D. Myers |
| Publisher | : |
| Total Pages | : 304 |
| Release | : 1981 |
| Genre | : Sandstone |
| ISBN | : |
| Author | : Lee Clayton |
| Publisher | : |
| Total Pages | : 84 |
| Release | : 1990 |
| Genre | : Geology |
| ISBN | : |
| Author | : Wisconsin Geological and Natural History Survey |
| Publisher | : |
| Total Pages | : 84 |
| Release | : 1990 |
| Genre | : Geology |
| ISBN | : |
| Author | : |
| Publisher | : |
| Total Pages | : 288 |
| Release | : 1988 |
| Genre | : Geology |
| ISBN | : |
| Author | : Richard A. Davis Jr. |
| Publisher | : Geological Society of America |
| Total Pages | : 92 |
| Release | : 2016-08-10 |
| Genre | : Nature |
| ISBN | : 0813700434 |
"Primarily for students, this guidebook on, and road log to, the Baraboo, Wisconsin, area offers insight into a wide range of geologic features. Precambrian, Cambrian, and Quaternary times are represented in a range of lithologies, structures, stratigraphy, and geomorphology. This notable area lies at the boundary of the glacial and driftless regions of the Quaternary"--
