· 6. the ridge and swale topography was created as lake michigan levels receded from its...

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Page 1:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 2:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 3:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 4:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 5:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 6:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 7:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 8:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 9:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 10:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 11:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 12:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 13:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 14:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 15:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 16:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 17:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 18:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 19:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 20:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 21:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 22:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 23:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 24:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 25:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled
Page 26:  · 6. The ridge and swale topography was created as Lake Michigan levels receded from its post-glacial high from about 12,000 years ago to approximately 6,000 years ago (Jansen prefiled