ground moraine

The ice sheets shaped the terrain over 100,000 years ago with their ground moraines.

Ground moraine may be modified into drumlins by the overriding ice.

The municipality is located in the Wasseramt district, on a ground moraine.

It is embedded in the ground moraines of Niederbarnimer.

Kettle lakes may be formed within the ground moraine region behind the terminal moraines.

Terminal moraines sweep in a giant arc around the ground moraine zone to the south.

All intermediate rock had eroded away before the till was deposited in a ground moraine by continental glaciers.

In alpine glaciers, ground moraines are often found between the two lateral moraines.

The low, rolling, ground moraine landscape is fertile and supports highly-productive arable farming.

The entire, gently rolling terrain in the southeast is composed partly of peat deposits and a ground moraine.

At the base there is a locally derived ground moraine that may be a remnant glacial deposit of much greater antiquity.

The ground moraine landscape of the Uelzen Basin is predominantly used for agriculture.

The ground moraine landscape consists predominantly in flat to gently rolling terrain, on which the ice mass deposited till.

A common variation, for example, is the spillage of younger meltwaters over older ground moraine beds.

Ground moraines are formed when the till melts out of the glacier in irregular heaps, forming rolling hills.

Near Hänigsen a loamy ground moraine rises close to the surface which improves the soil quality.

The Teltow Plateau is a flatly undulating ground moraine landscape.

Ground moraines are till covered areas with irregular topography and no ridges, often forming gently rolling hills or plains.

The Strange Till Plain is a flat ground moraine with underlying glacial till.

In Minnesota, the majority of kettles lakes reside in ground moraine and terminal moraine areas.

The marl dating from the diluvian times, when the ground moraines formed, contains, as we know, calcium carbonate.

Less apparent are ground moraines, also called glacial drift, which often blankets the surface underneath the glacier downslope from the equilibrium line.

This left a terminal moraine where the glacier halted, and a ground moraine in other areas once covered by the continental glacier.

There aer flat sander areas, undulating ground moraines and elongated end moraines.

Ground moraine with uncharacteristic reddish iron-rich sediments extended from St. Cloud, Minnesota, back northeastward.