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Date: Sat, 10 Jan 2026 08:43:54 +0100
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miswil tracksite preserves fossil tracks of sauropod dinosaurs from the Late Jurassic epoch. The site is located in the Jura Mountains of Switzerland, north of the village of Lommiswil and near the city of Solothurn, in limestones of the Reuchenette Formation. The site consists of around 450 individual tracks on a steeply inclined (70°) surface measuring 7,000 m2 (75,000 sq ft) in area. Discovered in 1988 in an active quarry, it was the first Jurassic dinosaur tracksite to be discovered in Switzerland. The tracks provided evidence that the area, which was thought to have been a shallow sea, was above sea level. The site was scientifically documented by rock climbing and the use of a helicopter. The tracks are large, with hind foot impressions up to 80 cm (31 in) in length. At least 10 trackways can be seen, one of which showing a pronounced right turn. The site is protected as a geoheritage site (geotope) and accessible to the public.
Locality and discovery
The tracksite is located in the Steingrueben quarry, ca. 1 km north of the village of Lommiswil, in the canton of Solothurn, Switzerland. Geologically, it is part of the Weissenstein anticline, a major fold in the southernmost extent of the Swiss Jura mountains. The sediments are part of the Reuchenette Formation and date to the late Kimmeridgian. The track surface is inclined by about 70°. The Steingrueben quarry extracted packstones that contained a large amount of snail shells (Nerineidae) for use as building stones. The tracks were located directly beneath this packstone layer and were exposed as the stone was quarried away. Besides the abundant snail shells, macroscopic fossils are rare in the quarry, but the hermit crab Orhomalus virgulinus, a tooth of the fish Macrodon, fragments of turtle shells (Plesiochelys), tooth plates of sharks (Asteracanthus), and fragments of the marine crocodile Steneosaurus have been discov
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<div style="font-size:8px;color:#ffffff;">miswil tracksite preserves fossil tracks of sauropod dinosaurs from the Late Jurassic epoch. The site is located in the Jura Mountains of Switzerland, north of the village of Lommiswil and near the city of Solothurn, in limestones of the Reuchenette Formation. The site consists of around 450 individual tracks on a steeply inclined (70°) surface measuring 7,000 m2 (75,000 sq ft) in area. Discovered in 1988 in an active quarry, it was the first Jurassic dinosaur tracksite to be discovered in Switzerland. The tracks provided evidence that the area, which was thought to have been a shallow sea, was above sea level. The site was scientifically documented by rock climbing and the use of a helicopter. The tracks are large, with hind foot impressions up to 80 c</div>
<div style="font-size:8px;color:#ffffff;">m (31 in) in length. At least 10 trackways can be seen, one of which showing a pronounced right turn. The site is protected as a geoheritage site (geotope) and accessible to the public. Locality and discovery The tracksite is located in the Steingrueben quarry, ca. 1 km north of the village of Lommiswil, in the canton of Solothurn, Switzerland. Geologically, it is part of the Weissenstein anticline, a major fold in the southernmost extent of the Swiss Jura mountains. The sediments are part of the Reuchenette Formation and date to the late Kimmeridgian. The track surface is inclined by about 70°. The Steingrueben quarry extracted packstones that contained a large amount of snail shells (Nerineidae) for use as building stones. The tracks were located directly beneath this packstone layer and were exposed as the stone was quarried away. Besides the abundant snail shells, macroscopic fossils are rare in the quarry, but the hermit crab Orhomalus virgulinus, a tooth of the fish Macrodon, fragments of turtle shells (Plesiochelys), tooth plates of sharks (Asteracanthus), and fragments of the marine crocodile Steneosaurus have been discov</div>
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