Remmarna

World famous varves of clay

In the early 1900s scientists were visiting Ragunda to try to determine the time of the end of the latest ice age. At Remmarna they studied the layers of clay that the flowing water had brought here since the time when the inland ice melted. The varves of clay in Ragunda have been selected as one of a hundred geological heritage sites in the world.

Melting water brought sand and clay here

About 20,000 years ago the thick inland ice covered the land that today is Sweden. In due course the ice melted. Geologists are not entirely certain but Ragunda was probably free from ice some 10,000 years ago.

When the inland ice was melting the water gushed into the bay in the Baltic Sea at the time reaching into the valley of the River Indalsälven. At the time Sweden was pushed down by the heavy ice and the Baltic Sea had a different layout compared to the present.

The melting water carried along large quantities of sand and clay. The material was deposited on the bottom of the lake. One light, a little thicker layer was added every summer, and a dark, thinner layer was added every winter.

This process repeated every year until the point when no more material from the melting ice could reach here. At that point the land uplift had continued and the Baltic Sea retreated. What remained in the area was Lake Ragundasjön.

Varves of varying grain sizes at Remmarna. Photo: Souleiko Abdi Olade.

De Geer discovered the time when the ice age came to an end

Gerard De Geer was a famous professor of geology at Stockholm University. Early in the 1900s De Geer and his students came to Ragunda to count varves – layers – and attempt to determine the point in time when the latest ice age had come to an end. He knew that Lake Ragundasjön had been emptied of water which meant that the varves were easy to study.

The uppermost layer dated from 1796, the year when the lake was emptied and the bottom layer was approximately 7 000 years old. Since the varves are unique they were able to make comparisons with other, corresponding layers in other places, where they could count more layers back in time.

When De Geer had finished counting, his conclusion was that the end of the latest ice age should have happened about 12,000-13,000 years ago. Nowadays, geologists believe that Ragunda was ice-free about 10,000 years ago.

Varves in Ragunda in the early 1900s. Source: Svenska Turistföreningen.

One of the one hundred designated geological heritage sites

The varves in Ragunda have been selected as 1 of 100 geological heritage sites; sites of major importance for the development of geological science. The organisation behind The First 100 Heritage Sites is IUGS, International Union of Geological Sciences, one of the world’s largest scientific organisations.


More information

Theme Scientific Breakthrough

The First 100 IUGS Geological Heritage Sites


More site photos

Strandpromenad vid utställning där man kan se varv av olika kornstorlek. Foto: Lovis Uhlgrén.
Utsikt över Indalsälven och Vättaberget från Remmarna. Foto: Lovis Uhlgrén.
Utsikt över Indalsälven och bron i Hammarstrand vid Hammarforsen. Foto: Katarina Söderlund.

Places to visit nearby


Practicalities

Accessibility

See Accessibility.

Activities

Take a walk along the River Indalsälven. See also Activities in Ragunda.

Eating and drinking

The nearest grocery store, café and eatery are in Hammarstrand. See also Eating and drinking in Ragunda.

Accommodation

Missing on site, but various options are available nearby. See Accommodation in Ragunda.

Getting here

SWEREF 99 TM N: 6 999 624 E: 568 473
WGS84 N: 63,119471° E: 16,357442°

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