peneplain , auch: peneplane

The larger part of the country is covered by a peneplain.

The central area of the park is an undulating peneplain.

The whole land area at the time of flooding was virtually a peneplain.

This contact is regarded to be a classic example of an ancient peneplain.

The peneplain is no longer in the cycle of erosion that witnessed its production.

The chain, once split open, continued to erode until it formed a peneplain.

A peneplain can be mistaken for a depositional plain.

Because of long and continuous erosion, the whole region has been transformed into an undulating peneplain.

Notwithstanding dramatic local differences in elevation, much of the state is a gently rolling peneplain.

On the pliocene peneplain, today's drainage system was firmly established.

The peaks of these mountains are all remnant features of this peneplain.

So also, forms which are not classified together may be superficially similar; for example, a young coastal plain and a peneplain.

To the southeast, the transition to the Congo basin takes place on a gently sloping peneplain.

The plateau and peneplain are mostly wooded.

A peneplain topography argues permanence for hundreds of millions of years."

Caille is built on a rocky outcrop in a glacial peneplain.

It is situated in the peneplain at the South of Toros Mountains.

During the Pliocene period the Coast Mountains did not exist and a level peneplain extended to the sea.

Naparima Plains, the peneplain which occupies part of western south Trinidad.

This process over 30 million years resulted in an elevated and highly eroded peneplain where the San Luis Valley is today.

This latter formation basically corresponds to the post-Hercynian peneplain characteristic of the Primary era.

At the base-line of these hills lie the landscapes of the 'peneplain' and 'charro' field.

A peneplain with the occasional moderately high monadnocks left behind during the peneplanation of the rest of the surface.

These incised meanders have been interpreted to have formed by downward erosion after uplift of an older peneplain surface.

Jameson Land mainly consists of a tilted peneplain of jurassic sandstone, highest in the east.