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Mergel

[lightbrown mergel]

'Mergel' is the regional name for the soft chalk rock which in most parts of southern Limburg is found in isolated outcrops or under a thin soil cover. Depending on the amount of iron oxide (rust) which it contains, the colour varies from light white to light yellow or light brown. The 'mergel' consists almost entirely of fragments of animals that lived here at the end of the Cretaceous era, when the area was flooded by the sea. In fact, it represents an extremely thick pile of fossils.

The Limburg 'mergel' is subdivided into various formations: those of Aken (Aken Sands), Vaals (Vaals Greensands), Gulpen (Gulpen Chalks), Kunrade (Kunrade Chalks) and Maastricht (Maastricht Chalks). The largest number of fossils has been found in the youngest 'mergel' unit of the Maastricht Formation. The quarrying of 'mergel' in southern Limburg probably started during Roman times, when a first settlement was built.

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