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Pozzo del Merro

Pozzo del Merro, Italy
Pozzo del Merro / Francesco Cervoni, Wikimedia Commons / CC BY-SA 4.0

WorldBlue  In short

The second deepest known water-filled sinkhole – cave system is located in the vicinities of Rome. Recently none expected that the small lake in Pozzo del Merro might be almost 400 m deep.

4.4 out of 10 stars 43.8%

GPS coordinates
42.039228 N 12.6805 E
Location, address
Europe, Italy, Lazio, some 23 km north-east from the centre of Rome, 3 km east from Mentana
Sinkholes, Caves, Lakes and streams, Geographical extremes
Alternate names
Pozza del Merro, Merro Well
Known – 472 m, waterbody – 392 m

Map of the site

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WorldYellow In detail

Sinkhole with small pond

Pozzo del Merro is located in a comparatively plain place some 140 – 150 m above sea level. It starts as a large, some 120 m long and 70 m wide hole in the ground. Steep, rocky walls of the sinkhole are covered with thick vegetation. The water level is located 80 m below the surrounding area.

Down, to the water, lead stairs built of stones. Here stand also abandoned constructions left by Rome water supply company – sometime in the past they had a project to supply the city with the clean water of Pozzo del Merro.

Lake at the bottom of this sinkhole is small, a maximum of 27 m wide. It is covered with a thick blanket of water plants Lemna.

This unsightly lake was considered to be fairly deep – some thought that it might be 50 m deep, some – that even 90 m deep.

There were told stories about people who got drowned in unexpected eddies in Pozzo del Merro – their corpses were found later in the sea. There is no reason to believe in these tales.

Crossection of Pozzo Merro, Italy
Crossection of Pozzo Merro / Francesco Cervoni, Wikimedia Commons / CC BY-SA 4.0

Unexpected depth

Group of Italian cave divers and scientists (Giorgio Caramanna, Riccardo Malatesta, and others) decided to find out the true depth of the cave in the late 1990s. In spring 1999 they reached 100 m depth – but the sinkhole continued down into the unknown depth. It was decided to continue exploration with remote-controlled submarines – ROV.

These devices were provided by a special unit of Italian firefighters and there was arranged complex expedition with helicopters and other heavy equipment.

In 2000 – 2002 a submarine "Mercurio" reached the depth of 210 m – it could not go further due to the length of connection cable. The sinkhole continued deeper without signs of ending.

Next submarine – "Hyball 300" had a longer connection cable and it reached the depth of 310 m. Finally, on March 19, 2002, there was used the ultimate minor submarine – "Prometeo" which reached the depth of 392 m. Here the abyss changes direction and continues horizontally into the unexplored passage. It is quite possible that Pozzo del Merro is even deeper.

Thus Pozzo del Merro surpasses the more famous, incredible Mexican sinkhole El Zacatón, which is "only" 319 m deep.

Only in the late September 2016 lake in one Czech cave – Hranice Abyss – surpassed the depth of Pozzo del Merro. This lake was dived up to 404 m depth.

Karst landscape

Pozzo del Merro is located in protected natural area – "Riserva Macchia del Barco e Macchia di Gattaceca", near the Cornicolani Hills. This location is far from true wilderness – but it is comparatively wild if we remember that just 23 km from it is located the centre of the eternal city of Rome.

Here, at the base of Apennines are located numerous interesting karst features – sinkholes, karst caves, travertine formations. South from Pozzo del Merro is located ancient, enormous mines of travertine, used up to this day. The beautiful town of Tivoli has developed around powerful springs with beautiful waterfalls falling over travertine formations.

Sinkhole has formed in lower Triassic limestone layers buried deep below later sand, clay sediments, and comparatively new, Quarternary tufa formed by eruptions of nearby volcanoes.

Groundwater and volcano

Bottom of Pozzo del Merro lake is located 322 m below sea level. Such geological formation simply could not form in common karst processes.

Most likely volcanic heat and chemistry of nearby Vulcano Albano have helped to create this exceptional abyss. Groundwater deep in Triassic limestone was heated by volcanic heat and saturated with sulfur. This warm, acidic water rather quickly dissolved the limestone, and there formed underground voids. The ceiling of the void collapsed, debris was dissolved, the ceiling of the void collapsed again and again until it reached the daylight.

Similar processes have created the amazing Sistema Zacatón in Mexico.

Narrow well

Contrary to El Zacatón, Pozzo del Merro is narrow and skewed. The lake above is up to 27 m wide but then it narrows down to 4 – 5 m width. Water is rather chilly: 16° C.

In a few meters depth due to the dense cover of water plants there is total darkness. Soon the water becomes very clear and transparent.

Along the path downwards there can be noticed side passages, some up to 70 m long, dissolved by the warm, acidic water in the past. Sometimes the cave has several parallel vertical shafts and the diver (rather – robot) can select which one to take.

Only at the bottom does the sinkhole expand to 30 m in width. The bottom is covered with silty reddish deposits – insoluble particles of limestone.

Niphargus cornicolanus - dweller of Pozzo Merro
Niphargus cornicolanus – dweller of Pozzo Merro / Francesco Cervoni, Wikimedia Commons / CC BY-SA 4.0

Cave biology

At the depth of 73 m there has been sampled small creature – a crustacean Niphargus cornicolanus Iannilli & Vigna-Tagl 2005. Most likely this is the only place in the world where this small crustacean lives.

Unfortunately here have been found invasive species as well – turtle from America (Trachemys) and a dangerous fern Salvinia molesta D.Mitch. Such small ecosystems are very fragile and slight changes can erase unique communities of endemic species.


  1. Il Pozzo del Merro. Accessed on July 12, 2010
  2. Giorgio Caramanna, Speleologia subacquea e ricerca scientifica. Un caso de studio: il "Posso del Merro" a i sinkholes della Piana di Tivoli.
  3. Cross section of Il Pozzo del Merro. Accessed on July 12, 2010

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