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Lake Ontario Shoreline


ttantalo

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Horn coral. Cross section on the right in the first photo. A more oblique section in the second.

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The fossils are rugosan corals. Such fossils are common in certain rock formations exposed at places along the Lake Erie shore. For example if you visit Rock Point Provincial Park you will see an excellent example of a Devonian coral reef in the Onondaga Formation rocks exposed there. Also such fossils can be found in rocks from glacial deposits, which were scraped from the bedrock surface and transported (generally from North to South) across considerable distances. If you found this at the Lake Ontario shore it was transported (likely by a glacier) as there are no outcrops of Devonian age on that shore (only Ordovician), and the internal structure of the corals suggests they are Silurian or Devonian but not Ordovician.

Don

Edited by FossilDAWG
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