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The highest elevation is the Geiersberg at 586 metres NN.

According to a strictly geological definition, a small region south of the Main near Wertheim and another south of Gemünden can be considered part of the Spessart.

That definition would mean that part of the Spessart lies in the state of Baden-Württemberg.

The top layer of most of the Hochspessart and southern Spessart is made up of a slab of Buntsandstein or red sandstone, of up to 400 metres thickness.

It dates back about 250 million years and is prevalent especially around Miltenberg.

This is the best-known stone of the area, as it has been used in the past for many public buildings including the cathedrals of the Rhine valley, like Mainz Cathedral.

However, the north-south rift that follows the river Main along the western leg of the Maindreieck does not match exactly the geological divide between the sandstone and the Muschelkalk.

The highest elevation in the Hessian part of the Spessart is Hermannskoppe at 567 metres.

Since the admission of Croatia to the European Union (EU), the geographical centre of the EU is located in the village of Westerngrund, near Schöllkrippen, according to the Institut de Géographie in Paris.

The largest amount of precipitation falls in the elevated region of the Hochspessart, rising from the west to a maximum of 1,000 mm/year and then falling back on the lee side of the range (prevailing winds come from the west) to around 600 mm/year in the Main valley.

A snow cover of 10 centimetres or more is relatively rare, prevailing on average on fewer than 10 days per year in the Main valley, 15 to 20 days in the Vorspessart and 30 to 35 days in the Hochspessart.

These rock types are most visible in the Vorspessart.

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