East their control fades out as you get into the continental interior.

They are typically found in continental interiors some distance from large bodies of water.

In the 19th century, the Portuguese began a more serious program of advancing into the continental interior.

On his left the land rose to the distant hills, fading into the continental interior.

The second age, centered in the 19th century, focused on the exploration of the continental interiors.

This would change in the later half of the 17th and 18th centuries as French settlement penetrated further into the continental interior.

Full colonization of the continental interior was not established until the end of the 19th century.

In the continental interior the climate swung wildly between killing heat and dry freezing.

A major river drained the continental interior and passed eastwards at Parkes.

This is a typical plot for continental interiors.

They tend to be sparser in continental interiors.

The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior.

This shear zone is associated with one of the largest gravity anomalies known from continental interiors.

The continental interiors are the driest areas.

The waterway was the major one connecting the eastern seaboard of the United States to the continental interior.

Well south, a continental interior.

Rather, magmatism occurs in response to thickening of crust in the continental interior.

Across from where they landed on the beach was the waterfall where they would start their journey into the continental interior.

"Death rates in earthquakes within continental interiors have often exceeded five percent and can be as high as 30 percent," they warn.

A moderating influence of the nearby ocean water prevents winter temperatures from falling to the extreme lows found in the continental interior.

There are those who see the drying out of the continental interiors as a more significant consequence of climate change than sea-level rises.

A chevron is a wedge-shaped sediment deposit observed on coastlines and continental interiors around the world.

The greatest warming has occurred in the continental interiors of the northern hemisphere, whereas the coasts have warmed more slowly or even cooled.

As on Earth, the state eventually appeared, both sedentary (along the fortunate seashores) and nomadic (in the grim continental interiors).

In their analysis, maximum warming occurred in winter in high latitudes and in continental interiors.