glacial erosion

The north face shows much evidence of glacial erosion.

Eventually, this hollow may become large enough that glacial erosion intensifies.

Glacial erosion created steep walls on the sides of the fjord.

However, the lake is actually the result of glacial erosion, and in no way an ancient volcanic crater.

Glacial erosion is represented in deep valleys which dissect the area.

These periods of glacial erosion were separated by warming trends and continue to present day.

The hard diabase layer resisted the glacial erosion of the last ice age.

The land surrounding Stirling has been most affected by glacial erosion and deposition.

Glacial erosion in this area is to be effective in large and small lakes are numerous.

Cyclopean stairs form as a result of glacial erosion.

Glacial erosion has contributed to such features by creating depressions in which standing water can collect.

Linga is made up of sandstone, subjected to ancient glacial erosion.

The valley was originally not only made through glacial erosion but by the high pressure melting water which pushed its way beneath the ice.

The central lowlands had been formed by glacial erosion in the Pleistocene ice age.

A cirque is an amphitheatre-like valley formed by glacial erosion.

The mountain has several cirques from glacial erosion.

Near Kantishna, it is the result of both glacial erosion and ice-block melting.

The lake was created by glacial erosion.

This glacial erosion resulted in the very steep northern and eastern faces which the hill possesses.

Glacial erosion was likewise responsible for scooping out the shallow lakebed.

From about 900,000 years ago to the present, numerous andesitic volcanic centers in the area have come and disappeared through glacial erosion.

His views on glacial erosion opposed the mainstream theories of the time, but have later been adopted in the geological sciences.

Most were created by glacial erosion.

It occupies a basin formed by glacial erosion.

The mesas that the townsite resides on were created by glacial erosion during the last ice age.