0 the large mass of rocks and dirt that is left by a melting glacier (= a large mass of ice) at its furthest point of movement
1 the large mass of rocks and dirt that is left by a melting glacier (= large mass of ice) at its farthest point of movement
The glacial debris, possibly terminal moraine, left behind by the receding ice, acted as dams, allowing lakes to form.
The lake is dammed by a high unconsolidated terminal moraine dam.
The glacier descends from approximately 8200 ft to a terminus near 7400 ft below which an old terminal moraine and proglacial lake exist.
These terminal moraine ridges mark the southernmost extreme of the prehistoric glacier expansion.
Till is deposited at the terminal moraine, along the lateral and medial moraines and in the ground moraine of a glacier.
It deposited materials and then melted, leaving a terminal moraine blocking the river, forming an earthen dam.
When the ice retreated, a deposit known as a terminal moraine was left behind, in the form of a ridge.
The striking arc of a terminal moraine marks the limit of the last ice advance in the area.
