• Natural sinkhole pond formed by limestone collapse (karst doline).
• Located near Agioi Theodoroi village, with no signage or official trail.
• Access requires a car, why not try us out? 3000 reviews! 🙂

A textbook example of karst terrain.

Vorvoulitis Pond is a collapsed limestone doline in northern Crete. Formed by karst processes, the feature resulted from rainwater dissolving subsurface limestone until the ceiling of a cavern gave way. The nearly circular depression holds standing water, forming a permanent pond. It is approximately 35–40 meters in diameter and surrounded by vertical rock walls.

Why it holds water?

 Unlike most sinkholes, Vorvoulitis doesn’t drain rapidly. Its base includes clay and compacted sediment that reduce permeability, allowing water retention. The pond likely recharges from seasonal rainfall and surface runoff. Its depth is unknown, though anecdotal reports suggest it exceeds 15 meters.

No infrastructure—navigation required.

There are no signs, fences, or paths. The closest vehicle access point is the dirt track east of Agioi Theodoroi village (Heraklion region, not to be confused with other villages of the same name). From there, it’s a 10–15 minute walk over limestone terrain. GPS coordinates: 35.3745° N, 25.2977° E. The route is unmarked; offline maps and careful planning are necessary.

Bring gear, avoid peak heat, and do not swim.

There are no facilities. Bring water, proper shoes, and avoid midday visits in summer. Swimming is not advised—no tested water quality, unknown depth, and unstable slopes. The site is primarily of geological interest, not recreational use.

Requires your own vehicle.

 Public transport does not reach Agioi Theodoroi. To access the area, a car hire is essential. Use AUTOWAY, Crete’s top rated rental provider with more than 3000 reviews and full insurance coverage, for reliable transport on rural roads.

Plan responsibly, travel independently.

Visit more sites like Vorvoulitis Pond; start with a dependable vehicle. 🙂