Now you know why we call it KAMA.
700 foot diabase -capped mesas and cuestas rising out of Superior.
Sibley sedimentary rocks.
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| Peregrine Falcons now nest in these cliffs. |
A sequence of flat-laying, pale sandstone beds
alternating with thin strata of brick-red impure dolomites
and dolomite limestones.
The dark colours are fine grained diabase sills.
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| Lying in wait. |
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| A quiet afternoon on the shore of Mozakama Bay, Aug 25,2011. |
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| I guess I was trying to see around this rare reed-bed and tilted my camera. |
Geology information from:
Geology and Scenery North Shore of Lake Superior
by E.G. Pye
Geological Guide Book No. 2
Ontario Department of Mines 1969
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