Forget it, jw: the ice shelf was sea ice!
Ice packs on land may get to 2 miles thick, and depress the land below it with their weight of billions of tonnes, as it does on the continent of Antarctica.
A floating sea ice shelf, though, in permanent contact with salt water, never gets to 2 miles thick! A couple hundred meters max.
Have a look at e.g. the Ross Ice Shelf.
A couple hundred (200) meters is about 199.5 meters thicker than the Arctic areas where traditional Inuit men recently hunted seals. But, there are other options, e.g. hunting them directly in water, or while they bask on ice floes. And, since the Antarctic ice today is home to a few species of seals, I’ll concede that there might have been seals on the edge of the Atlantic ice shelf, if an ice shelf existed between Europe and North America. That seems to be in question now.
Based on a LGM model of a permanent ice shelf connection between Europe and North America, Stanford once suggested that Solutreans walked across solid ice to North America in a few weeks. When challenged, he modified it to a marine-adapted people from Iberia following the Atlantic ice shelf to America, living off the sea like recent traditional Arctic people of the last 3000 years. Most of us, including myself, have based our arguments, both pro and con, on Stanford’s suggestion that Solutreans started at the Iberian peninsula and ended up near the coast of Virginia, implying a connecting ice shelf at least somewhere near those latitudes.
But, newer information on glacial oceanography durring the LGM indicates Atlantic ice only in winter, and farther north than previously believed, with an open water channel between Europe and North America. In summer, according to the newer data, there was no Atlantic ice sheet. Land in northern Europe and northern North America on both sides of the Atlantic remained heavily glaciated and uninhabitable year round, except for parts of Iberia in Europe and land south of modern New Jersey and Pennsylvania in North America.
More information about the LGM ecosystem for this model is still being collected. Too soon to support or oppose the idea that a marine people from Europe would or could have followed an ice edge route from Iberia to 25 or 30 degrees north, crossed the open water channel, and then followed it 30 to 40 degrees south again on the North American side. Or that they crossed the open North Atlantic in a directly western route from Iberia to Virginia without following an ice shelf at all.
The following study discusses the newer, developing model. It's in technical jargon that’s beyond most of us (me, anyway), but the excerpt below from page 7 is more understandable. The CLIMAP Project that it mentions is the source of the old model.
http://courses.washington.edu/proxies/S ... 003.pdfink on the Antarctic ecosystem.
Applications of these threshold values to a set of more
than 60 well-dated sediment cores shows that the glacial
North Atlantic was characterized by an extreme seasonal
variability of climate. During glacial summers, sea ice
retreated up to the Arctic ocean and the western Fram Strait,
in contrast to the CLIMAP Project Members [1981] reconstruction
that postulated a complete perennial sea ice cover.
Accordingly, most of the Nordic Seas remained ice free,
leading to conditions that could support at least modest deepwater
convection. During glacial winters, sea ice extended to
the south of the Iceland Faroe Ridge. A small patch of ice
may also have lain near the (modern and glacial) center of
the Azores High. During the winter season, a broad meridional
ice-free channel 50_ to 60_N may have formed the site
of intensive upper North Atlantic Deep Water formation.
These new sea ice data sets will contribute to the initiation
and/or testing of paleoceanographic ocean circulation models
[cf. Paul and Scha¨ fer-Neth, 2003].