postglacial

Understanding postglacial rebound is also important to our ability to monitor recent global change.

It may not have been able to move north in the postglacial warming, due to poor dispersal abilities.

Most of the island consists of forests and postglacial hills.

This lakes take a shape of the cross made of postglacial channels.

Great Langton shows signs of human activity throughout much of its postglacial history.

It is known for having large postglacial boulders.

This young postglacial uranium anomaly continues to be studied and modelled in detail.

Native distribution was driven by postglacial melt from the Mississippi River.

All geological formations are quite recent, dating from the Ice Age and postglacial times.

Postglacial volcanism in the Mývatn district may be divided into three cycles.

After a glacier retreats the end moraine may be destroyed by postglacial erosion.

The sea level became lower over time due to postglacial rebound, and it became increasingly difficult to approach the castle by boat.

The diverse forms of postglacial relief serve as a shelter for plenty of animal species.

Thus, the observations of postglacial rebound provide a natural experiment to measure mantle rheology.

When the sea level lowered, the area was submerged under a postglacial delta which deposited large volumes of sand.

The Gulf of Utica was formed during the postglacial transgression about 6,000 years ago.

It is a relict of a postglacial warm period where there had been a much warmer climate around the Kaiserstuhl.

It is a postglacial land of lakes, hills and forests, bordering Soviet Lithuania.

The lake is postglacial, having formed about 500 B.C. when an underground cave collapsed.

Moreover, populations that survived on icefree land have probably in most cases been genetically flooded by postglacial immigrants.

Some interstadial and postglacial pollen diagams from eastern Canada.

In numerous places there is evidence of the glacio-isostatic structures that survived the postglacial eustatic advances during the last 15,000 years.

Similarly extensive spreads of peat have developed across parts of the plateau surface in the postglacial period.

Conditions favourable for human settlement occurred in the present Wyrzysk Region in the postglacial period.

I. A postglacial climatic chronology for southern New England.