Interpretive illustration of a typical Dolmen

Dolmen

Anta de Curral dos Mouros

Also known asanta de Curral dos Mouros

Portugal

DatedEst. 4000–3000 BCE

No licensed photograph yetWe have no photograph we may publish for this site, so the interpretive 3D view leads instead.

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Overview

About this site

Overview

The Anta de Curral dos Mouros, also called the Dolmen de Sobreda, is a dolmen at Sobreda in the parish of Seixo da Beira, in the municipality of Oliveira do Hospital, district of Coimbra, Portugal. The catalogue dates it by typological estimate to between 4000 and 3000 BCE. It was classified as an Immovable Cultural Heritage of Public Interest in 1959.

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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. 4000–3000 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

Anta de Curral dos Mouros

2 min read278 wordsRead on Wikipedia

The monument has lost all the roof slabs over the burial chamber and the covered passage, and more than half of the supporting orthostates of the passage are missing.

Anta de Curral dos Mouros

Description

Sources for this section

The monument has lost all the roof slabs over the burial chamber and the covered passage, and more than half of the supporting orthostates of the passage are missing. The supporting stones of the chamber form an oval room, probably paved, which was entered by a long, wide passage. At the end of the nineteenth century traces of red paint were still visible on one of the chamber stones.

Finds

Sources for this section

The dolmen, said to be about 6 000 years old, contained a variety of stone tools, including nearly 150 arrowheads, broken pottery from about 500 vessels, and even wood and bone. The organic material is easily degraded and hard to detect because of the high acidity of the soil.