morainic

Hill River was so named for the morainic hills in the area.

There was a period when these two morainic systems marked a continuous ice margin.

Ridgetown is located in the middle of a low morainic ridge.

It is of ice age origin and lies embedded between low morainic hills.

North of it there are several morainic plateaux or Ländchen.

Its sources are in the morainic lakes in northern Minnesota.

However, the morainic belts are of small relief in comparison to the great area of the ice.

Sand martins settle on the steep coast of the morainic core.

Associated with rougher morainic deposits are numerous small sloughs and ponds.

The Marseilles moraine was preceded by the Bloomington morainic system.

Here it joins with the Morainic system of the Erie Lobe.

Young Drift morainic landscapes by contrast have new landforms that are still recognisable as glacial forms.

This morainic debris gave rise to forest and plants making possible a settled life for man, his skills and his animals.

It is made up of morainic material from the west margin of the Koettlitz Glacier.

Morainic drift is the movement of rock debris (talus) (see also Moraine) left by glaciers.

Features such as the morainic hills, gravel sandar and lakes have left a record of various glaciation stages in this region.

They are rather unique formations of their kind which originate from morainic rocks of glacial origin.

Dylewska Góra is a morainic hill, with its eastern and northern slopes covered by beech forest.

Actually Titisee, we were told, is a settlement along a famous morainic lake, a glacier left over from the last Ice Age.

This older bedrock and loose morainic debris is mostly obscured by a covering of wind-blown loess.

There are no lateral moraines, but there are a few morainic patches along the terminus.

Located along the shores of Lake Iseo, vineyards are planted in well-drained morainic soils.

On the far side of the morainic zone is the gravel outwash plain, which was piled up by the meltwaters of the ice mass.

In some places the Arkona beaches stand by the outer border of the Port Huron morainic system.

The valley formed by this stream is U-shaped with a river bed scattered with boulders and glacial morainic deposits.