How far did the Scandinavian Ice Sheet extend during major glacial periods?

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Map showing the extent of the Laurentide, Cordilleran, and Greenland ice sheets during the Wisconsin glaciation, roughly 100,000 to 11,000 years ago. The Laurentide Ice Sheet covers most of present-day Canada and parts of the northern United States in light blue, the Cordilleran Ice Sheet covers the Pacific Northwest in teal, and the Greenland Ice Sheet is marked in purple. Modern international and state or provincial boundaries are outlined for reference. — Pleistocene Epoch Ice sheets during the Wisconsin glacial episode penetrated deep into North America.

During the Pleistocene Epoch, the Scandinavian Ice Sheet—also known as the Fennoscandian Ice Sheet—was the largest contiguous mass of ice in Eurasia. At its maximum extent, this massive glacial formation reached nearly to latitude 48° N.12

Geographically, the ice sheet originated in the Jostedalsbreen area of Norway and expanded significantly in all directions. Its reach included:1

West: The British Isles.3
South: Central Germany and Poland.1
East: Extending nearly to Moscow and covering parts of north-central Siberia.13

At its peak, the ice sheet is estimated to have covered approximately 6,600,000 square km (2,500,000 square miles) and reached a thickness of up to 3,000 meters (9,800 feet).12