Large, overturned, rootless folds of bedrock and drift were thrust up forming ridges. View across Limfjord estuary toward Hanklit, a cliff exposure on the island of Mors, northern Denmark. The cliff is about 60 m high and cuts across the end of a large ice-shoved hill, visible behind the cliff. Hanklit reveals an overturned fold of Fur Fm. Ice movement was from left to right.
Narrow valleys alternate with ridges.
The Limfjord basin was presumably the source region for material now thrust into the ice-pushed ridges. Brandon Hills are a push moraine located on the Manitoba Escarpment of southwestern Manitoba. The hills contain a core of deformed stratified drift with a discordant cover of till. Composite-ridges covered by a thin veneer of till resemble a giant fishhook in overall plan. A conspicuous esker resting on till loops over the eastern end of the hills, and low kames and kettles are located to the southwest.