What archaeology says
The cautious mainstream position is that the 'monolith' is probably natural. Sceptical geologists and archaeologists note that the block is local sedimentary calcirudite, radiocarbon-dated from included shell to about 40,000 years old, consistent with the surrounding beachrock formations; that elongated, joint-bounded slabs with surprisingly straight edges are exactly what fractured, wave-worked beachrock produces; and that circular holes in coastal limestone are routinely bored by marine molluscs, scoured by pebbles rotating in currents, or dissolved along weaknesses. A 2024 reassessment in the Journal of Marine Science and Engineering examined the Sicilian Channel cases and concluded the features are natural, suggesting the block is a slab of neighbouring eroded beachrock broken off and shifted by storm waves or a tsunami around 9,500–9,200 years ago, and criticising the original dating argument as resting on sea-level assumptions rather than archaeological evidence.
The wider context also gives pause. No stone tools, hearths, bones or any other unambiguous trace of human presence has been recovered from the bank, and a Mesolithic monument of this scale would be exceptional: mainland megalith-building traditions are millennia younger, and moving a 15-tonne stone would be a remarkable feat for small foraging bands, though defenders note Göbekli Tepe proves pre-agricultural societies could work megaliths.
Notably, the discoverers themselves have grown more measured. In a 2023 Scientific Reports paper on two enigmatic rock ridges nearby — one almost exactly ten times the length of the other, meeting at close to a right angle — Lodolo and colleagues wrote plainly that their data 'do not conclusively reveal either a natural or anthropogenic origin', while observing that such a concentration of geometrically regular structures in one small area is curious. That is how the question currently stands: intriguing geometry, no artefacts, verdict open but leaning natural in most published assessments.
- The block is local-type calcirudite beachrock c. 40,000 years old, matching nearby natural formations
- Straight-edged slabs and rounded holes are known products of jointing, mollusc boring and current scour
- No stone tools, bones, hearths or other archaeological material found anywhere on the bank
- A 2024 Journal of Marine Science and Engineering reassessment concluded the features are natural, storm- or tsunami-moved beachrock
- The discoverers' own 2023 paper on nearby ridges concedes the evidence is inconclusive
