This follows on my previous post here of a series started here.
A case of "AI to the rescue", it's listed on my blog's pinned post under 2026.
In my initial post of this series, I wrote (caps added):
That prompted me now to look up geophysical data (aeromagnetic anomalies, Wikipedia): will it allow to GLIMPSE terranes in the subsurface below the Great Lakes, as well as earlier Archean and later Phanerozoic features such as, respectively, the Wawa Lineament and the Niagara Escarpment? Lo-and-behold, I found aeromagnetic data (NOAA) and sketch-mapped them below on my desktop GIS (Esri)!
Was "glimpse" a subconscious play on words with GLIMPCE? A scant half decade after my thesis, it was a deep seismic refraction program to image the Mid-continent Rift underlying the Great Lakes (Perplexity). It followed earlier similar imaging the Grenville Front Tectonic Zone (Perplexity). That much I knew, tho not in time for my thesis early eighties of Geol. Surv. Canada work mid eighties
Imagine my surprise when the prompt "deep seismic survey Manitoulin Island Discontinuity under Lake Huron &/or Lake Michigan" in Perplexity yielded this:
The Manitoulin Island Discontinuity (MID) is a significant geological feature identified in deep seismic surveys beneath Lake Huron near Manitoulin Island. These surveys, part of the GLIMPCE project in the late 1980s, imaged crustal structures across Lakes Superior, Michigan, and Huron, including the MID labeled in seismic line maps.[prd-0420-geoontario-0000-blob-cge0eud7azhvfsf7.z01.azurefd]
GLIMPCE Seismic Surveys
GLIMPCE conducted multichannel seismic reflection and long-offset refraction surveys, collecting 1350 km of data along eight profiles, including lines in Lake Huron near Manitoulin Island. These deep surveys targeted structures like the early Proterozoic Huronian continental margin and middle Proterozoic Grenville front, with the MID marked as a key feature in the vicinity. High-resolution data revealed crustal velocities, rift basins, and Moho depths up to 55 km, though specific MID details relate to broader tectonic boundaries.[download-telecharger.services.geo]
Geological Significance
The MID appears in regional cross-sections as a fault or boundary along the southern margin of the Superior Province adjacent to Lake Huron, influencing Huronian megacycle sediment accumulation. Magnetotelluric surveys along GLIMPCE line J on Manitoulin Island and Bruce Peninsula detected conductive black shales masking the Grenville Front, limiting resolution of underlying structures. No direct evidence links it to Lake Michigan surveys, but GLIMPCE profiles extended through that basin.[ovid +3]
Related Studies
Shallow acoustic surveys on the Alpena-Amberley ridge under Lake Huron identified Paleoindian hunting structures but did not probe deep discontinuities like the MID. Recent 3D seismic work near Lake Huron focused on nuclear repository sites, not the MID specifically. For GIS or mapping applications, GLIMPCE data integrates with potential field anomalies for midcontinent rift modeling.[pnas +3]
Please go here to get the full text incl. list of references. In the "+3", my thesis paper was mis-attributed, and I contacted academia.edu to correct it. I add here the front page of the original paper [usgs].
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| click to enlarge, original here |
This closes my series... thanks for reading!


