Tessellated pavement

Tessellated Pavement is a rock formation along the coast of Eaglehawk Neck that consists of rectangular blocks separated by natural cracks, creating a mosaic-like effect. The surface displays two distinct patterns: shallow depressions in the pan formation and raised areas in the loaf formation.

This siltstone formation originated during the Permian period roughly 300 million years ago through sediment accumulation and subsequent compaction into solid rock. The visible rectangular pattern was then created by seawater erosion working over extended periods.

The site draws photographers and nature lovers wanting to capture how the ocean and stone interact over time. People return to observe how tides and waves shape the rocks differently throughout the day.

The location is reachable by car in roughly one hour from Hobart, with a parking area marking the starting point of your visit. Short walking paths from there lead to viewing points where you can see the rock formation clearly.

The rock displays weathering patterns that resemble naturally carved grooves, which fascinate scientists studying how stone fractures and erodes. These unintentional formations resemble human-made structures, making it a compelling study site for geologists interested in natural pattern formation.

GPS coordinates: -43.00816,147.93429

Latest update: December 7, 2025 10:05