About: Pignola-Abriola stratigraphic section

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The Pignola-Abriola section is a ~63 m long stratigraphic sequence of cherty limestones deposited in the Lagonegro Basin during the latest Norian and the early Rhaetian Stages (Late Triassic Period). The main outcrop (40°33′23.50″N 15°47′1.71″E / 40.5565278°N 15.7838083°E) is on the western side of Mount Crocetta along the SP5 road connecting the villages of Pignola and Abriola (Province of Potenza, Basilicata, southern Italy). A smaller outcrop (~7 m thick), overlapping the central part of the main section, is located near a former railway tunnel, few meters below the road level. The Pignola-Abriola section has been recently proposed as GSSP (Global boundary Stratotype Section and Point) of the Rhaetian Stage.

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  • The Pignola-Abriola section is a ~63 m long stratigraphic sequence of cherty limestones deposited in the Lagonegro Basin during the latest Norian and the early Rhaetian Stages (Late Triassic Period). The main outcrop (40°33′23.50″N 15°47′1.71″E / 40.5565278°N 15.7838083°E) is on the western side of Mount Crocetta along the SP5 road connecting the villages of Pignola and Abriola (Province of Potenza, Basilicata, southern Italy). A smaller outcrop (~7 m thick), overlapping the central part of the main section, is located near a former railway tunnel, few meters below the road level. The Pignola-Abriola section has been recently proposed as GSSP (Global boundary Stratotype Section and Point) of the Rhaetian Stage. (en)
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  • Pignola-Abriola section (en)
  • Location of the Pignola-Abriola section in Basilicata Region (en)
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  • The Pignola-Abriola section is a ~63 m long stratigraphic sequence of cherty limestones deposited in the Lagonegro Basin during the latest Norian and the early Rhaetian Stages (Late Triassic Period). The main outcrop (40°33′23.50″N 15°47′1.71″E / 40.5565278°N 15.7838083°E) is on the western side of Mount Crocetta along the SP5 road connecting the villages of Pignola and Abriola (Province of Potenza, Basilicata, southern Italy). A smaller outcrop (~7 m thick), overlapping the central part of the main section, is located near a former railway tunnel, few meters below the road level. The Pignola-Abriola section has been recently proposed as GSSP (Global boundary Stratotype Section and Point) of the Rhaetian Stage. (en)
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  • Pignola-Abriola stratigraphic section (en)
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