A funny thing happened when I showed my last blog post to my mom: "what is that blob right above where it says 'Atlantic Ocean'?". Widow and mother to geologists, she learned to read maps: she spotted the Rockhall Rise as it shows in the zoomed-in view below; it's also known as Rockhall Plateau (Perplexity), briefly a piece of crust left behind in the spreading of the North Atlantic. The tectonic plate margins, incl. the mid-Atlantic Ridge top right, are highlighted in cyan below. Same as the second-last blogpost showed interesting geomorphology only seen in North polar view, this portion of the far North Atlantic also shows better than in a normal or equatorial map view shown at right.
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| click to enlarge (can be slow), original |
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| click to enlarge (can be slow), original |
- the Reykjanes Ridge portion of the mid-Atlantic Ridge shows a spread at a slight angle (dashed line) to the median itself (cyan), with matching original continental shelf margins (brown)
- the Rockhall Plateau is however separated from the UK Ireland mass by a trough with matching continental shelf outlines (blue), not unlike the original brown ones
- if the mid-oceanic ridge were the motor, the plateau would have been pressed against not separated from the NW Europe continental mass
- the small offset orphaned ridge next to the Faroe Islands further underscores the pull you rather than the push me aspect
- this is a patent example on geomorphology alone, and a keen eye, of the slab pull driver of plate tectonics, rather than ridge push or mantle drag theories detailed in the Perplexity link above.
Thanks to @John Nelson LinkedIn post here, w far superior cartography on global plate tectonics, inspired in turn by his daughter - this rattled about in my brain and y'all prompted me to post it - aptly enough, our posts bridge International Women's Day!

