Interpretive illustration of a typical Dolmen

DolmenThe Copper Age

Nældemose

Denmark

DatedEst. 3500–2800 BCE

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Overview

About this site

Overview

The long dolmen (langdysse) of Nældemose, also called Nellermose, lies on the shore south-west of Nældemose on the island of Funen, Denmark. It is a megalithic monument of the Funnel Beaker culture, dating from the Neolithic, about 3500 to 2800 BCE. It stands very close to an eroding cliff.

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Where it sits in time

The site's dated range, placed against world reference points.

The scale is logarithmic: each step to the left is about ten times older than the last.

Est. 3500–2800 BCEHow this date was established: Type comparisonTypical for this type

What this badge meansThe published range for this kind of monument in this region. It is not a date for this site.
Source for this date

Article

Nældemose

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0 m north of the chamber in the forest floor, and two stones lie on the beach directly below the chamber.

Langdysse von Nældemose

Description

Sources for this section

The rectangular chamber is oriented west to east and sunk into the ground. It belongs to the closed type of early dolmen (Urdolmen) and is about 1.9 m long and 0.8 m wide. It is made of six stones, two on each long side and one at each end. The capstone or capstones are missing. After an excavation in 1951 the chamber floor lay about 0.7 m below ground level.

About 5.0 m west of the chamber three large stones form a north-south row about 4.0 m long; they are presumably kerbstones at the western end of a vanished long bed (Hünenbett). Another possible kerbstone lies about 5.0 m north of the chamber in the forest floor, and two stones lie on the beach directly below the chamber. About 5.0 m east of the chamber a recess can be seen in which an upright kerbstone with a split face directed to the south stands. This could be the remains of a second chamber.

Conservation

Sources for this section

In 1987 the chamber lay only about 4.0 m from the edge of the eroded cliff, which had receded by 6.0 m since 1954. With the erosion unchanged at 1.0 m every five years, a fall of the chamber within twenty years was expected in 1987. The existing state was nevertheless still found during a periodic inspection in 2018.