Brandungskliff am Steigerberg, Paleocliff formation at Steigerberg, Germany.
Brandungskliff am Steigerberg is a paleocliff located in Rhineland-Palatinate that displays the effects of ancient wave action on its rock face. The formation presents clear horizontal striations and erosion patterns visible across its exposed slope, which speaks to the powerful forces that shaped it over time.
The formation developed roughly 30 million years ago during the Early Oligocene when a warm sea covered the Mainz Basin region. Wave action and coastal processes from this ancient ocean carved the distinctive patterns that remain visible in the rock face today.
The geological survey of Rhineland-Palatinate discovered this formation in 1997, leading to its designation as a protected excavation site for research.
The site sits between Eckelsheim and Wendelsheim villages, southwest of Mainz, positioned on the western slope of Steigerberg. Visitors should wear sturdy footwear since the terrain is steep and conditions can vary depending on weather and ground moisture.
Scientists identified this formation in 1997, leading to its recognition as a protected research site for geological study. This status transforms it into a valuable reference point for understanding how ancient seas shaped the Rhine Valley landscape.
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