Danubius Health Spa Resort Hévíz

Danubius Health Spa Resort Hévíz
(former Thermal Hotel Hévíz) - Hévíz

The thermal lake

How was the Lake of Hévíz formed?

The answer lies in the past, in the history of our Earth looking back to several million years. At the beginning of the Mesozic era, during the Triassic period (about 200 million years ago) crystal-clear sea water covered this region as well as the site of the present day Transdanubian Mountains. Out of this sea snow-white dolomite and limestone formed a deposit around Hévíz.

During the other two Mesozic periods, the Jurassic and the Cretaceous (about 180-170 million years ago) the sea withdrew from this area. In the territory of the present day Bakony Hills, at the end of the Cretaceous period and the during the first epoch of the Tertiary period, the Palaeocene bauxite deposits formed in a tropical environment, then redeposited due to surface impacts. These natural forces caused erosion in the softer layers of the ground surface, at some spots totally destroying them. Then started the karstification of limestone and dolomite.

During the Tertiary period even the Eocene, the Oligocene and the Miocene epochs following the Palaeocene did not leave layers behind, the region of Hévíz remained a 'mainland'. The last epoch of the period, the Pliocene, however, was very eventful.

At the end of the Pliocene and at the beginning of the Pleistocene (about 2 to 4 million years ago) the wind and water streams carried the majority of the material of the Pannonian layers southwards. The welling up of hot springs, and thus the Primordial Spring were the first sign of postvolcanic activities. Due to earth movements and the crustal collapse two trench systems were formed in the middle of the Pleistocene epoch. Moisture accumulated in them: Lake Balaton was formed about 22 thousand years ago. This was the time when the history of the Lake of Hévíz also started.

There are several pieces of evidence proving that the thermal water of the Lake of Hévíz did not well up at the level in the geological past it does today but much higher. The water of the Hévíz Lake welled up at its present site about 20-22 thousand years ago, simultaneously with the formation of Lake Balaton. The warm water rushing up first flowed into Lake Balaton. Due to the changes in the climate the water level of Lake Balaton dropped. A peat-moor formed from the once lush flora in the former basin of the lake.

The boggy, peaty, flat surface of the Hévíz valley extends 1-1.5 km eastwards of the lake as far as Mt. Dobogó at the eastern part of the valley and the mountain range of Cserszegtomaj surrounding the valley from the east. The peaty area extends southwards as far as river Zala and northwards as well as the country tavern of Gyöngyös.

The water of the Hévíz Lake is 'heated' by geothermal energy. The deep-seated waters enclosed in underground storage systems formed during the Triassic and the Pannonian periods are heated by heat conducted and radiated from deep-lying layers of the crust of the earth.

Based on the amount of carbon isotope in the water scientists have found out that the cold rill of the spring - from the period of penetration till the date of welling up - is 5-7 thousand years old, while the warm-water spring is 10-12 thousand years of age. Waters infiltrating into the depth from the surface come from a quite extensive area: from the Bakony Hills, the Keszthely Mountains and the Zala Hills. A part of the water does not permeate too deep into the ground (as far as the Pannonian layer) - this is the so-called karst water zone - and from here it gets into the 'mixing cave' of the Lake of Hévíz through the cold rill. The majority of the water gets much deeper, into the Triassic dolomite layers where it gets warmed up. During its journey it dissolves various metals and minerals, then it flows towards the surface again to arrive finally at the spring cave.

If we keep a close watch on the surface of the Hévíz Lake, we can see that it does not stand still.