Assemblages of drumlins, crag‐and‐tail features, giant glacial grooves, and megaflutes—collectively termed “drumlin fields"—are described along the southwestern shorelines of the Kara Sea, i.e., southernmost Novaya Zemlya, Vaygach Island, the Yugorskiy Peninsula, and the Pay‐Khoy ridge. All these landforms were formed during one of the latest stages in glaciation in the Eurasian Arctic, radiocarbon dated at about 8.5 thousand years ago. At that late stage, the ice kept spreading out of the Kara Sea center, which is strongly suggested by the NE‐SW orientation of the landforms. This is consistent with the model of a continuous marine Eurasian ice sheet and contradicts the concepts of “restricted” and “diachronous” glaciation. The Kara center of glaciation turns out to be one of the most stable and long‐lived features of the Northern Hemisphere's glaciation.