Geology in Belgium
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GigaPans of interesting geological structures in Belgium.
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Complex kink folds in the Lower Devonian fine-grained, siliciclastic metasediments of the core of the High-Ardenne Slate Belt (Belgium).
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Kink folds in the Lower Devonian fine-grained, siliciclastic metasediments of the core of the High-Ardenne Slate Belt (Belgium); northern part of the La Fortelle outcrop (Van Baelen 2010).
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Kink folds in the Lower Devonian fine-grained, siliciclastic metasediments of the core of the High-Ardenne Slate Belt (Belgium).
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Folded Upper-Carboniferous series in the frontal area of the Rhenohercynian foreland fold-and-thrust betl at the northern extremity of the Pan-European Variscan orogen. World-class outcrops at the Namur Citadel (Belgium). Classic example of a N-verging antiform.
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Folded Upper-Carboniferous series in the frontal area of the Rhenohercynian foreland fold-and-thrust belt at the northern extremity of the Pan-European Variscan orogen. World-class outcrops at the Namur Citadel (Belgium).
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The famous unconformity at the northwestern border of the Lower Palaeozoic Stavelot-Venn basement inlier in the valley of the Ninglinspo (Belgium). The layers are overturned and dip to the south. On the outcrop the basal conglomerate and reddish claystone is exposed; both are of Lochkovian age. The slates below the unc...
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