About: Benton Fault

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The Benton Fault is a geological fault in southern Pembrokeshire in Wales that was active as a normal fault during the deposition of the Old Red Sandstone during the Devonian period, forming a thick half graben. During the Carboniferous, the Benton Fault was strongly inverted as part of the Variscan Orogeny.

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  • The Benton Fault is a geological fault in southern Pembrokeshire in Wales that was active as a normal fault during the deposition of the Old Red Sandstone during the Devonian period, forming a thick half graben. During the Carboniferous, the Benton Fault was strongly inverted as part of the Variscan Orogeny. (en)
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  • The Benton Fault is a geological fault in southern Pembrokeshire in Wales that was active as a normal fault during the deposition of the Old Red Sandstone during the Devonian period, forming a thick half graben. During the Carboniferous, the Benton Fault was strongly inverted as part of the Variscan Orogeny. (en)
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  • Benton Fault (en)
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