The Diabasbrottet Quarry (58°21′32.2″N 12°30′08.6″E / 58.358944°N 12.502389°E), located on Mt. Hunneberg, Västergötland, Sweden, is the location of the Global Boundary Stratotype Section and Point (GSSP) which marks the lower boundary of the Floian stage of the Lower Ordovician. The Floian stage is named after Flo Parish, a village 5 km to the southeast of the Diabasbrottet quarry. It was selected over "The Ledge" in western Newfoundland in 2000 and ratified as the GSSP by the International Union of Geological Sciences in 2002.
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| - Cantera Diabasbrottet (es)
- Diabasbrottet Quarry (en)
- Hunneberg (stratigrafisk referenspunkt) (sv)
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| - Hunneberg heter en av två GSSP:er som har blivit definierade i Sverige. I folkmun kallas platsen för Gyllene spiken och har koordinaterna 58.3589°N 12.5024°E. Den finns i Diabasbrottet vid Hunneberg, precis ovanför bädd E och definierar basen av den andra serien i den undre ordoviciska delen, som har fått namnet Flo efter Flo socken vid Hunneberg. Denna GSSP blev ratificerad av den International Commission on Stratigraphy 2002. (sv)
- The Diabasbrottet Quarry (58°21′32.2″N 12°30′08.6″E / 58.358944°N 12.502389°E), located on Mt. Hunneberg, Västergötland, Sweden, is the location of the Global Boundary Stratotype Section and Point (GSSP) which marks the lower boundary of the Floian stage of the Lower Ordovician. The Floian stage is named after Flo Parish, a village 5 km to the southeast of the Diabasbrottet quarry. It was selected over "The Ledge" in western Newfoundland in 2000 and ratified as the GSSP by the International Union of Geological Sciences in 2002. (en)
- La Cantera Diabasbrottet (58°21′32.2″N 12°30′08.6″E / 58.358944, 12.502389), se encuentra en el , Västergötland, Suecia, es la ubicación de la (GSSP) que marca el límite inferior de la etapa Floiense del Ordovícico Inferior. El límite inferior del Floiense se define con la primera aparición de , una especie de graptolito. La sección de roca, dominado por esquisto, es inusualmente fósiles iferous, incluyendo restos fósiles de graptolitos, conodontos, y trilobites. Está altamente comprimido, y la sección Ordovícico está a sólo 12 m de espesor. (es)
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| - 58.35894444444445 12.50238888888889
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| - The Diabasbrottet Quarry (58°21′32.2″N 12°30′08.6″E / 58.358944°N 12.502389°E), located on Mt. Hunneberg, Västergötland, Sweden, is the location of the Global Boundary Stratotype Section and Point (GSSP) which marks the lower boundary of the Floian stage of the Lower Ordovician. The lower boundary of the Floian is defined as the first appearance of Tetragraptus approximatus, a graptolite species. The rock section belongs to the and is dominated by shale. It is unusually fossiliferous, including fossilized remains of graptolites, conodonts, and trilobites. It is highly compressed, and the Ordovician section is only 12 m thick. The Floian stage is named after Flo Parish, a village 5 km to the southeast of the Diabasbrottet quarry. It was selected over "The Ledge" in western Newfoundland in 2000 and ratified as the GSSP by the International Union of Geological Sciences in 2002. (en)
- La Cantera Diabasbrottet (58°21′32.2″N 12°30′08.6″E / 58.358944, 12.502389), se encuentra en el , Västergötland, Suecia, es la ubicación de la (GSSP) que marca el límite inferior de la etapa Floiense del Ordovícico Inferior. El límite inferior del Floiense se define con la primera aparición de , una especie de graptolito. La sección de roca, dominado por esquisto, es inusualmente fósiles iferous, incluyendo restos fósiles de graptolitos, conodontos, y trilobites. Está altamente comprimido, y la sección Ordovícico está a sólo 12 m de espesor. El Floiense lleva el nombre de la parroquia de Flo, en Suecia, un pueblo a 5 km al sureste de la cantera Diabasbrottet. Fue seleccionado sobre "La Cornisa" en el oeste de Terranova en 2000 y ratificada como la GSSP por el Unión Internacional de Ciencias Geológicas en 2002. (es)
- Hunneberg heter en av två GSSP:er som har blivit definierade i Sverige. I folkmun kallas platsen för Gyllene spiken och har koordinaterna 58.3589°N 12.5024°E. Den finns i Diabasbrottet vid Hunneberg, precis ovanför bädd E och definierar basen av den andra serien i den undre ordoviciska delen, som har fått namnet Flo efter Flo socken vid Hunneberg. Denna GSSP blev ratificerad av den International Commission on Stratigraphy 2002. (sv)
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