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The area was formed from a series of large moraines during the last ice age.
Where the moraines met away from the end of the ice also helped deposits.
These three moraines occur on the western slope of the bay.
These terminal moraines covered all of what is now Denmark.
It can be found on moraines, plains, and mountain slopes.
Its black moraines showed quite clear against the snow.
Moraines which are found far off from existing glaciers were created during a past ice age.
Glacial moraines are exposed on both sides of the water.
In addition moraines have been left behind by various glacial periods.
These moraines are most clearly seen southwest of Chicago.
Lateral moraines are formed on the sides of the glacier.
Thus the glacier did not create any moraines, which could have created larger lakes.
It left low rolling hills with steep sides called moraines.
The ice sheets shaped the terrain over 100,000 years ago with their ground moraines.
For one thing, the glaciers left moraines - great piles of debris.
These moraines formed long ribbons of rubble on the surface as they moved along the current.
Boulder clay is also abundant and moraines cover substantial areas.
It is a 588 hectare region at which the two moraines merge.
Surrounding the low plain are bands of moraines in the south and west suburbs.
Large lateral moraines can be seen below the glacier.
Sweden has many lakes and moraines, legacies of the ice age.
Rock flows or moraines are another characteristic left by glaciation.
There are two types of end moraines; terminal and recessional.
'Take a rest from moraines for a bit,' he says.
The moraines are low hills that were built as the glaciers receded over 12,000 years ago.