Hranice Abyss

Hranice Abyss (Hranická propast) is the deepest flooded pit cave in the world. It is a karst sinkhole near the town of Hranice, Czech Republic. The greatest confirmed depth is 519.5 m, of which 450 m is underwater. In 2020, a scientific expedition to the cave revealed that part of the system apparently reaches 1 kilometre deep, albeit with the lowest reaches sediment-filled. Analysis of the water found carbon and helium isotopes which implied that the cave has been formed by acidic waters, heated by the mantle, welling up from below.

Description
It is located near the Zbrašov Aragonite Caves, which are open to the public. The total depth of the abyss (at least 473.5 m) is unknown, as the lower part of the abyss is flooded by the Hranice Lake. The abyss has an elliptical shape and is situated in the SE-SW direction. It is approximately 110 metres long at its longest point and 50 metres wide at its widest point. For most visitors the most interesting figure is the depth of the abyss including the flooded part, but in reality it is a rather rugged karst system. Karst phenomena (e.g. sinkholes) can also be observed in the immediate vicinity of the abyss.

At a depth of 48 metres below the surface of the lake, after crossing the siphon called Zubatice (after its jagged shape), it is possible to ascend to the dry caves (Rotunda Dry, Heaven I-III, Monika). These are continuously monitored, including water and air temperature measurements. In addition, the Dry Rotunda is known as a roosting site for bats, which enter it through a very narrow passage from the Jezírka area. They have to cross about 7 metres of rock mass. The occurrence of bats is monitored and studied by experts from the Institute of Biology of the Academy of Sciences of the Czech Republic.

Below the Zubatice is narrow neck opening to the deep underwater cave called Lift. The bottom of the Lift in the depth of 219 m is covered by sunken trees and branches making every further movement complicated and dangerous. The area is therefore called Mikado (a reference to the popular game). Behind this obstacle is the neck leading to another deep cave whose depth remains still uncertain.

Depth
The dry part of the abyss is 69.5 m deep. There is a small lake at the bottom. Below the surface, the abyss was mapped to a depth of -170 m (Pavel Říha, 2005), followed by a dive to a depth of -181 m (Starnawski, 2000) and a 21 June 2012 dive to a depth of -217 m (Starnawski with a team of six Czech and Polish divers). Robot (R.O.V.) Hyball was at a depth of -205 m (1995). The bottom was not reached because further investigations revealed a configuration of topography preventing further progress of the robot.



The measurement of the depth of the abyss was made on 1 October 2012, when Krzysztof Starnawski launched a probe from a depth of 217 m to a depth of 373 m during a caving action from the organization ZO ČSS 7-02 Hranický kras Olomouc. He then briefly descended to a depth of 225 m himself, which is the deepest depth reached by a diver in this location.

On 12 October 2014, Krzysztof Starnawski again measured the new maximum depth of the submerged part of the Hranice Abyss – 384 m. On 27 September 2016, the ROV made by GRALmarine reached a depth of 404 m without reaching the bottom. This surpassed the depth of Italy's Pozzo del Merro, which until then had been considered the deepest submerged chasm in the world with a maximum measured depth of 392 m. In 2022 the UNEXMIN Georobotics Ltd reached 450 m water depth with the UX1-Neo robot and set the new word record.

The total confirmed depth in 2022 was 519.5 m – 69.5 m above water, and 450 m below. It is estimated that the depth of the abyss could be between 800-1200 m, as indicated by the temperature and chemical composition of the water. This is confirmed by other studies published in the scientific press in 2022.

The report of Jiří Pogoda states that he launched a specially designed probe (glider) from Zubatice to a total depth of 260 m on 13 April 1980, during a solitary dive, without reaching the bottom. However, his measurements are incomplete and considered unreliable, as they have not been further verified. In terms of current knowledge, Pogoda's measurements are true, but due to the constriction at -205 m metres, it would have to be a huge coincidence for his probe to sink lower and, more importantly, to be able to pull it back through a tangle of logs, branches and other obstacles at that level.