denudation

The denudation of the land was upon a grand scale.

I am more struck with his remarks on denudation than you seem to be.

Denudation (removal of matter to a lower level) is caused mainly by air and water movement.

The reservoir's life is estimated at 107 years due to silt from denudation.

The third denudation event took place during the Early Cenozoic.

It is also good to take into consideration the effects of denudation (processes that wear away the earth's surface).

These are produced by denudation of the successive flows.

Denudation can involve the removal of both solid particles and dissolved material.

Denudation rates are usually much lower than the rates of uplift.

The timing, magnitude, and rate of denudation can be estimated using pressure-temperature studies.

There is an enormous difference between mean and maximum denudation and deposition.

Early studies prompted the formation of denudation cycle hypotheses to describe land formations.

In medicine, denudation refers to the loss of surface layers, such as the epithelium.

This effect was likely due to epithelial denudation.

Volcanoes can thus provide important test cases for estimates of rates of denudation (see Section 15.4.1.2).

After the eruptions, an intense uplifting and consequent regional denudation took place.

If denudation is insufficient as a thinning mechanism then sub-crustal processes must be considered.

Deposition and denudation as measure of time.

Only the unnatural denudation of turf in this vicinity impeded its progress even slightly.

There are no "craters of denudation" at Galapagos.

Modern denudation estimates are usually based on stream load measurements taken at gauging stations.

During the Cretaceous period (65-145 Ma), two separate denudation events occurred.

Forest denudation, particularly in the hilly areas, has caused soil erosion, compounded by wind and water action.

Man is many more times more powerful, as an agent of denudation, than all the atmospheric denuding forces combined.

Denudation exposes deep sub-volcanic structures on the present surface of the area where volcanic activity once occurred.