DescriptionDolostone breccia (Mackinac Breccia, Devonian; Interstate-75 exit near St. Ignace, Upper Peninsula of Michigan, USA) 2 (40975889854).jpg
Breccia from the Devonian of Michigan, USA. (public display, Geology Department, Wittenberg University, Springfield, Ohio, USA)
This rock is a Devonian-aged dolostone breccia called the Mackinac Breccia. It is exposed in the vicinity of Castle Rock, Michigan. In that area, the unit is a dolostone block breccia - it's principally a jumble of broken blocks of dolostone derived from the St. Ignace Dolomite (upper Upper Silurian). The breccia represents deposition from many collapse events in paleocaverns of dissolved-out Salina Group evaporites (Upper Silurian). Post-Silurian collapse of dissolved-out Salina evaporites was a widespread phenomenon throughout the Michigan-Ohio region.
Stratigraphy: Mackinac Breccia, upper Lower Devonian to lower Middle Devonian
Locality: outcrop attributed to an Interstate-75 exit near St. Ignace, Upper Peninsula of Michigan, USA
For info. on the Mackinac Breccia, see:
Landes (1959) - The Mackinac Breccia. pp. 19-24 in Geology of Mackinac Island and Lower and Middle Devonian South of the Straits of Mackinac. Michigan Basin Geological Society.
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