Nature is capable of unrepeatable wonders that can amaze you day after day. Here are some of the places worth visiting in the area:

• Balaton-Uplands National Park,
• lookout towers, hiking trails in the Keszthely Hills,
• Kis-Balaton Visitor Centre,
• Kányavár Island - Kis-Balaton,
• Csodabogyós (Butcher’s-broom) Cave - Balatonederics,
• Kotsy Water Mill - Zalaszántó,
• Buffalo Reserve - Balatonmagyaród,
• Szent György Hill basalt organs,
• Balaton Museum permanent exhibition - Keszthely,
• House of Nature - Gyenesdiás,
• Festetics Imre Zoo - Gyenesdiás,
• Szépkilátó (Lookout point) - Balatongyörök,
• Africa Museum - Balatonederics,
• Tapolca Lake Cave - Tapolca,
• Levendula House - Tihany

The western tip of Lake Balaton is rich in castle ruins. From the remains of the castles on Rezi, Tátika and Csobánc hills, you can enjoy a fantastic panorama of Lake Balaton and the buttes. In Szigliget and Sümeg, knights’ tournaments and jousting events are held several times a week. The Festetics Palace in Keszthely is not only one of the most beautiful and largest palaces in Hungary, but its exhibitions (carriages, hunting trophies, model railways, travels of the aristocrats, palm house) provide varied programmes for several days, should the weather take a turn for the worse. Festetics Palace - Helikon Palace Museum - Keszthely, Szigliget Castle - Szigliget, Sümeg Castle - Sümeg, Rezi Castle - Rezi Hill, Tátika Castle - Tátika Hill, Csobánc Castle - Csobánc Hill, Star Castle - Balatonszentgyörgy

Museums aren't the first thing you think of when you are on holiday. However, a good museum is a nice alternative when the weather turns unfavourable. Some museums are worth visiting even in good weather. The exhibitions at Festetics Palace are well worth a visit, and the permanent exhibition on the history of Lake Balaton at the Balaton Museum is surprisingly interesting for children and adults alike. In Keszthely, there are several smaller museums in the town centre, from the Erotic Wax-Works to the Snail Parliament. These small exhibitions can be visited during a walk around the town. For those who are more interested in nature, we recommend the House of Nature, in the neighbourhood of which you can also find the Imre Festetics Animal Park. And while cycling along the Balaton bike path, you can visit the Water Mill and Spice Garden in Gyenesdiás.

• Festetics Palace - Helikon Palace Museum permanent and temporary exhibitions - Keszthely,
• Balaton Museum permanent and temporary exhibitions - Keszthely,
• Balaton Museum escape room,
• Museums in the Town Centre / Doll Museum, Snail Parliament, Erotic Wax-Works, Retro Toy Museum / - Keszthely,
• House of Nature - Gyenesdiás,
• Mill of Gyenesdiás, Baker's Museum, Herbarium and Spice Garden - Gyenesdiás,
• Festetics Helikon Taverna wine and gastronomy exhibition space - Vonyarcvashegy,
• Africa Museum - Balatonederics,
• Star Castle - Balatonszentgyörgy

• Balaton Theatre - Keszthely,
• Escape Room at the Balaton Museum - Keszthely,
• Marina, scheduled boat trips and themed boat excursions - Keszthely,
• Municipal Beach and Island Beach Keszthely,
• J&A Ceramics House - Gyenesdiás,
• Darnay Cellar - Gyenesdiás,
• Diás Play Beach - Gyenesdiás,
• Paintball - Gyenesdiás,
• Water Mill - Gyenesdiás,
• St Michael’s Chapel - Vonyarcvashegy,
• Lido Beach - Vonyarcvashegy,
• Tavirózsa Adventure Park - Keszthely-Kertváros,
• Zala Springs Golf Club - Zalacsány,
• Rezi Dino and Adventure Park - Rezi,
• Bobo Fun Park - Alsópáhok,
• Peace Stupa - Zalaszántó

Keszthely | 6 kms from Hévíz

• Festetics Castle - Helikon Castle Museum temporary and permanent exhibitions
• Balaton Museum temporary and permanent exhibitions
• Museums of Keszthely
• Balaton Port, leisure boat trips, scheduled boat trips between cities
• City Beach and Island Bath

Gyenesdiás | 8 kms from Hévíz

• House of Nature visitor Center
• Festetics Imre Experience Centre
• Festetics Herb Garden & Herbarium at the Diás Water Mill
• J&A Ceramics House and Pottery
• Darnay Cellar
• Diási Beach
• Paintball

Vonyarcvashegy | 11 kms from Hévíz

• St. Michael's Chapel
• Festetics Helikon Tavern
• Lido Beach

Balatongyörök | 14 kms from Hévíztől

• Szépkilátó - Panorama View Point
• Africa Museum

Szigliget | 25 kms from Hévíz

Sümeg | 25 kms from Hévíz

Cave Lake of Tapolca | 30 kms from Hévíz

Badacsony - Badacsonytomaj | 30 kms from Hévíz

Tihany | 67 kms from Hévíz

• Tihany Abbey
• Lavender House and Visitor Centre

Zalacsány - Zala Springs Golf Resort | 10 kms from Hévíz

The Life-Giving Winds of the Ice Age: How Loess Shaped the Land

Did you know that Transdanubia’s rich, golden soils are actually a gift from the winds of the Ice Age? Loess isn’t just a dry geological term — it’s an ancient natural recipe that gave rise to some of the most fertile soils in the Carpathian Basin. Where vineyards grow today and birds nest in loess cliffs, strong winds once carried yellow dust across the landscape — for thousands of years. Learn how this unique sediment shaped the land and why loess is still essential for sustainable farming today.

What Is Loess and How Did It Form?

The term loess comes from the German word lose, meaning "loose." Loess is a fine-grained, yellowish sediment that was deposited during the Pleistocene epoch (2.58–0.01 million years ago), particularly during glacial periods. It formed in periglacial environments south of the great Scandinavian ice sheet — cold, dry landscapes with little or no vegetation.

The dust was carried by strong Ice Age winds from floodplains and barren steppes, and slowly accumulated over tens of thousands of years. Eventually, calcium carbonate cemented these layers into loess, which developed characteristic vertical fissures.

It’s important to note that the Pleistocene wasn't a single “Ice Age,” but a period that included alternating cold and warm phases — some even warmer than today.

Loess and the Landscape

Loess gave the Carpathian Basin — especially Transdanubia — its distinct terrain.

Steep loess cliffs (sometimes up to 10 meters high), caves that provide nesting sites for bee-eaters and sand martins, centuries-old sunken roads carved into hillsides, and exposed root systems are all part of the landscape’s geological legacy.

Together, they define the unique character of this region — shaped by time, wind, and stone.

Fertility and Water Retention

Loess-rich areas have produced some of the most fertile soils in the region. Many local producers farm on land that sits atop loess. This creates an excellent foundation for agriculture — not just because of the high humus content, but also because loess has outstanding water-holding capacity. Its vertical pores allow moisture to penetrate deeply and remain in the soil, even during dry periods.

A Modern Echo — Dust from the Sahara

Interestingly, the fine Saharan dust that now reaches Central Europe more frequently can be seen as a modern counterpart to loess-forming material. It’s a reminder that the powerful natural forces that shaped the land long ago are still at work today — just on a different scale.

Imagine a vast body of water — over 1,000 meters deep and more than 400 times the size of Lake Balaton — once rippling across this land. The story of the Pannonian Lake is not just a fascinating chapter of geological history, but a legacy that continues to shape the region: it left behind mineral resources, fertile soils, and even inspired legends. Discover how an ancient lake transformed Transdanubia — and why its impact is still felt today.

An Inland Sea for Millions of Years

At its greatest extent, the Pannonian Lake covered an enormous area, far surpassing the size of today’s Balaton. For millions of years (approximately 12 to 8.5 million years ago), it dominated the region. As surrounding mountain ranges gradually rose, the lake became cut off from the world’s oceans. Its water slowly turned fresh, and its basin began to fill with sediments. Because of its isolation, the lake developed a unique ecosystem with many endemic species.

The Lake Didn’t Appear Overnight

The Pannonian Lake didn’t simply “appear” in the Carpathian Basin. Its formation was the result of millions of years of tectonic activity and shifting climate. It emerged as an independent, enclosed body of water — no longer connected to the open seas.

Deep Waters, Varied Shores

In some areas, the lake reached depths of over 1,000 meters. Elsewhere, shallower zones supported lagoons, river deltas, and small, isolated lakes. During high water periods, rocky shorelines formed along the mountain fringes — traces of which can still be found today in the Keszthely Hills and the Mecsek Mountains.

The Lake’s Retreat — and Sediment Legacy

Despite its size, the lake was eventually filled in by immense volumes of sediment, carried mainly by rivers flowing from the Alps and the Carpathians. Over the course of 6.5 million years, it gradually disappeared from the landscape.

What did it leave behind?

Its sediments — composed mostly of sand, clay, and fine silt — became the so-called “Pannonian formations,” which today hold key mineral resources (such as petroleum) and aquifers. These formations define much of the surface geology of Transdanubia, including the Zala Hills.

Fertile soils later formed on the laminated silty and clay-rich deposits of the Somló Formation. Even the legendary “Tihany goat’s hoof” fossils — actually worn shell fragments of the Congeria ungulacaprae mollusk — can still be found embedded in these ancient layers.

The Final Lakes and a Gradual Goodbye

Because most of the sediment entered from the northwest, north, and northeast, the lake slowly retreated toward the south and southeast — as if it were “withdrawing” from what is now Hungary.

Small remnant lakes persisted for much longer in areas of present-day Slavonia (Croatia) and northern Serbia, but due to their different scale, character, and fauna, they are not considered true successors of the ancient Pannonian Lake.

The Life-Giving Winds of the Ice Age: How Loess Shaped the Land

Did you know that Transdanubia’s rich, golden soils are actually a gift from the winds of the Ice Age? Loess isn’t just a dry geological term — it’s an ancient natural recipe that gave rise to some of the most fertile soils in the Carpathian Basin. Where vineyards grow today and birds nest in loess cliffs, strong winds once carried yellow dust across the landscape — for thousands of years. Learn how this unique sediment shaped the land and why loess is still essential for sustainable farming today.

What Is Loess and How Did It Form?

The term loess comes from the German word lose, meaning "loose." Loess is a fine-grained, yellowish sediment that was deposited during the Pleistocene epoch (2.58–0.01 million years ago), particularly during glacial periods. It formed in periglacial environments south of the great Scandinavian ice sheet — cold, dry landscapes with little or no vegetation.

The dust was carried by strong Ice Age winds from floodplains and barren steppes, and slowly accumulated over tens of thousands of years. Eventually, calcium carbonate cemented these layers into loess, which developed characteristic vertical fissures.

It’s important to note that the Pleistocene wasn't a single “Ice Age,” but a period that included alternating cold and warm phases — some even warmer than today.

Loess and the Landscape

Loess gave the Carpathian Basin — especially Transdanubia — its distinct terrain.

Steep loess cliffs (sometimes up to 10 meters high), caves that provide nesting sites for bee-eaters and sand martins, centuries-old sunken roads carved into hillsides, and exposed root systems are all part of the landscape’s geological legacy.

Together, they define the unique character of this region — shaped by time, wind, and stone.

Fertility and Water Retention

Loess-rich areas have produced some of the most fertile soils in the region. Many local producers farm on land that sits atop loess. This creates an excellent foundation for agriculture — not just because of the high humus content, but also because loess has outstanding water-holding capacity. Its vertical pores allow moisture to penetrate deeply and remain in the soil, even during dry periods.

A Modern Echo — Dust from the Sahara

Interestingly, the fine Saharan dust that now reaches Central Europe more frequently can be seen as a modern counterpart to loess-forming material. It’s a reminder that the powerful natural forces that shaped the land long ago are still at work today — just on a different scale.

The Life-Giving Winds of the Ice Age: How Loess Shaped the Land

Did you know that Transdanubia’s rich, golden soils are actually a gift from the winds of the Ice Age? Loess isn’t just a dry geological term — it’s an ancient natural recipe that gave rise to some of the most fertile soils in the Carpathian Basin. Where vineyards grow today and birds nest in loess cliffs, strong winds once carried yellow dust across the landscape — for thousands of years. Learn how this unique sediment shaped the land and why loess is still essential for sustainable farming today.

What Is Loess and How Did It Form?

The term loess comes from the German word lose, meaning "loose." Loess is a fine-grained, yellowish sediment that was deposited during the Pleistocene epoch (2.58–0.01 million years ago), particularly during glacial periods. It formed in periglacial environments south of the great Scandinavian ice sheet — cold, dry landscapes with little or no vegetation.

The dust was carried by strong Ice Age winds from floodplains and barren steppes, and slowly accumulated over tens of thousands of years. Eventually, calcium carbonate cemented these layers into loess, which developed characteristic vertical fissures.

It’s important to note that the Pleistocene wasn't a single “Ice Age,” but a period that included alternating cold and warm phases — some even warmer than today.

Loess and the Landscape

Loess gave the Carpathian Basin — especially Transdanubia — its distinct terrain.

Steep loess cliffs (sometimes up to 10 meters high), caves that provide nesting sites for bee-eaters and sand martins, centuries-old sunken roads carved into hillsides, and exposed root systems are all part of the landscape’s geological legacy.

Together, they define the unique character of this region — shaped by time, wind, and stone.

Fertility and Water Retention

Loess-rich areas have produced some of the most fertile soils in the region. Many local producers farm on land that sits atop loess. This creates an excellent foundation for agriculture — not just because of the high humus content, but also because loess has outstanding water-holding capacity. Its vertical pores allow moisture to penetrate deeply and remain in the soil, even during dry periods.

A Modern Echo — Dust from the Sahara

Interestingly, the fine Saharan dust that now reaches Central Europe more frequently can be seen as a modern counterpart to loess-forming material. It’s a reminder that the powerful natural forces that shaped the land long ago are still at work today — just on a different scale.

Did you know the Zala River once flowed into the Drava and only later “found” Lake Balaton?
 The history of western Hungary’s water systems is not just a fascinating geological puzzle — it reads like an epic of Earth history: riverbeds shift, rivers “consume” one another, and even Lake Balaton doesn’t enter the scene until the final chapter. Discover how nature reshaped this landscape stroke by stroke — and how the Zala became Balaton’s most vital source of water.

The Quaternary Period and the Power of Landscape Formation

What sets the Quaternary Period (2.58 million years ago to the present) apart from earlier geological epochs is that the surface-shaping processes of this time — and the landforms they produced — continue to define our geographic environment today.

Pleistocene Changes: Riverbed Migrations and Terraces

One of the most pivotal surface processes during the Pleistocene (2.58 to 0.01 million years ago) was the migration of riverbeds and the formation of terraces and alluvial fans. These changes were closely tied to the slow retreat of the Pannonian Lake, which once filled much of the Carpathian Basin (see also: The Legacy of the Ancient Pannonian Lake).

The Ancient Danube Moves West

The early Danube initially flowed westward across what is now western Hungary, draining into the retreating Pannonian Lake. This westward course likely remained until the early Pleistocene.

A River’s Great Turning Point

The most dramatic hydrological change in the Carpathian Basin occurred between the Pliocene and Pleistocene: the formation of the Danube’s Visegrád Gorge (today’s Danube Bend), which diverted the river toward the center of the country and what is now the Pest Plain.

This shift profoundly affected all its former western tributaries — including the Zala.

The Story of the Zala: Migration and Capture

The river system of Central Transdanubia evolved in surprising ways, and the Zala’s journey is one of its most remarkable chapters. The Rába River already flowed northeastward toward the Little Hungarian Plain. The ancient Marcal, running northward, flowed into the Rába — and into it, in turn, flowed the ancient Zala.

But nature redrew the map — using the Zala as its brush. A now-vanished river flowing from north to south (its remnants visible today between Zalaszentgrót and Zalavár) cut into the landscape through a process called headward erosion — where rivers erode backward into the terrain, much like a hot knife slicing through butter. Eventually, it cut into the ancient Zala’s valley and “captured” the river, diverting it into its own course.

A New Path — and the Birth of Lake Balaton

From then on, the Zala made a sharp turn south at Türje and — with no Lake Balaton yet in existence — initially emptied into the Drava. Later, as the depression that would one day become Lake Balaton deepened, the Zala was gradually drawn toward it.

Lake Balaton, as a continuous body of water, is only about 5,000 years old — but for millions of years before, the Zala had already been on a winding journey that ultimately made it Balaton’s primary source of water, and the most life-giving river in the region today.

The Life-Giving Winds of the Ice Age: How Loess Shaped the Land

Did you know that Transdanubia’s rich, golden soils are actually a gift from the winds of the Ice Age? Loess isn’t just a dry geological term — it’s an ancient natural recipe that gave rise to some of the most fertile soils in the Carpathian Basin. Where vineyards grow today and birds nest in loess cliffs, strong winds once carried yellow dust across the landscape — for thousands of years. Learn how this unique sediment shaped the land and why loess is still essential for sustainable farming today.

What Is Loess and How Did It Form?

The term loess comes from the German word lose, meaning "loose." Loess is a fine-grained, yellowish sediment that was deposited during the Pleistocene epoch (2.58–0.01 million years ago), particularly during glacial periods. It formed in periglacial environments south of the great Scandinavian ice sheet — cold, dry landscapes with little or no vegetation.

The dust was carried by strong Ice Age winds from floodplains and barren steppes, and slowly accumulated over tens of thousands of years. Eventually, calcium carbonate cemented these layers into loess, which developed characteristic vertical fissures.

It’s important to note that the Pleistocene wasn't a single “Ice Age,” but a period that included alternating cold and warm phases — some even warmer than today.

Loess and the Landscape

Loess gave the Carpathian Basin — especially Transdanubia — its distinct terrain.

Steep loess cliffs (sometimes up to 10 meters high), caves that provide nesting sites for bee-eaters and sand martins, centuries-old sunken roads carved into hillsides, and exposed root systems are all part of the landscape’s geological legacy.

Together, they define the unique character of this region — shaped by time, wind, and stone.

Fertility and Water Retention

Loess-rich areas have produced some of the most fertile soils in the region. Many local producers farm on land that sits atop loess. This creates an excellent foundation for agriculture — not just because of the high humus content, but also because loess has outstanding water-holding capacity. Its vertical pores allow moisture to penetrate deeply and remain in the soil, even during dry periods.

A Modern Echo — Dust from the Sahara

Interestingly, the fine Saharan dust that now reaches Central Europe more frequently can be seen as a modern counterpart to loess-forming material. It’s a reminder that the powerful natural forces that shaped the land long ago are still at work today — just on a different scale.

Flavius Theodosius, the emperor who was a sickly child, or the best-known legend of the origin of Lake Hévíz

According to the ancient legend about the birth of the lake and its healing powers, Flavius, a Roman boy, was brought up by a Christian nurse here in Pannonia. The boy was weak and of poor health but his father was a great military leader so the nurse prayed to Virgin Mary to help him. The Holy Virgin, hearing her prayer, caused a spring to gush forth, in the healing water of which the child was bathed every day. The hot water of the spring and the steaming mud made the child's body grow stronger and stronger. Later, the boy became the Emperor of Eastern Rome, Flavius Theodosius, who made Christianity the state religion of his empire in 391. Since then, the water of the spring has been feeding Lake Hévíz and has brought healing to many.

When it comes to Hévíz and the Romans, there is no doubt that there were several places in the settlement and the surrounding area where people lived in Roman times. Local excavations show that there was a significant settlement in the period of the Roman empire in the present-day Egregy district. Several finds of the Villa Rustica - or villa farm - show that the settlement was inhabited from the 1st century until the 5th century. Roman artefacts were found not only in Egregy but also in other parts of Hévíz: Roman coins, earthenware, and an altar stone of Jupiter were found in the bed of Lake Hévíz.

The formation of Lake Hévíz in reality…

Lake Hévíz was born at the same time as Lake Balaton 20-22 thousand years ago. The origin of Lake Hévíz dates back to the time when the basalt mountains around Lake Balaton and Lake Balaton itself were born. At the end of the Pannonian period, volcanoes broke up the landscape of the Transdanubian region. The first signs of postvolcanic activity were the eruption of hot springs, such as the original Hévíz thermal spring. Archaeological excavations show that people lived here as early as the end of the Stone Age. In addition, many legends are dating back to different periods about the healing properties of the water here. According to Roman remains and finds, Hévíz was already a settlement 2,000 years ago, but even more surprisingly, water samples taken upon the discovery of the spring cave suggest that the cold water from the spring is 8,000 years old, while the hot medicinal water is 12,000 years old.

Opening hours

The central bath building located on the Hévíz Thermal Lake
(“A” building and “B” terrace = central covered section and large terrace)
will be temporarily closed from 18 March 2025 due to technical reasons.

The entrances to the Lake Bath and all other buildings remain open as usual.
Bathing in the thermal lake continues to be available without interruption, and all related spa facilities remain accessible.

Thank you for your understanding!
Lake Bath information desk:
Mobile: +36 30 959 1002
Email: spaheviz@spaheviz.hu

Hévíz Lake Bath reserve the right to change the opening hours and prices.

Hévíz Lake Bath Telephone:
+36 30 959 1002

Hévíz Lake Bath and Festetics Bathhouse price list

Valid from 01. April 2025. until withdrawn

Single-day tickets: Usable on the day of purchase only. Entitles the bearer to one-time entry. An additional charge will be levied if the allotted time limit is exceeded. Additional time extension cannot be purchased after the time limit has expired.

Lake passes: Deposits are refundable within 5 days of expiery. Refunds are payable in cash only, each day before the end of bathing time. Passes eintitle the bearer to enter the premises on two occasions per day. Following the bearer's first exit, a 15-minute wait period is required before return entry is permitted. Upon exiting the premises, locker number assignments are automatically cleared, after which we can accept no liability for contents. An additional charge will be levied if the alloted time limit is exceeded.

General information

• Valid from 09.05.2020 until withdrawal.
• The depth of the medicinal lake is 2-38 meters.
• Free use of changing rooms (included in the entrance fee)
• A sauna sheet is provided free of charge if you buy a ticket that entitles you to the use of the wellness facilities.
• The services of the wellness area are only available to persons over 12 years of age.
• Children under 6 years of age are admitted free of charge.
• The deposit is refundable within 72 hours of expiry.
• Daily tickets are valid only on the day of purchase.
• All tickets are valid for one entry a day only.
• We are not able to refund the price of the purchased tickets.
• We reserve the right to change prices and opening hours.
• An ATM is available during the opening hours in the building accessed from the Schulhof Promenade.

You can have more information about our special offers at the cash desks or on our website.
Hévíz Lake Baths phone number: 06 83 30 959 1002

To whom are Kinesio-Lab services recommended?

Younger people, even children, as a preventive measure, adults, to identify or assess musculoskeletal and spinal problems, athletes, to get an accurate picture of the condition of joints and muscles that are under above-average strain, or of the whole body either to prevent sports injuries or to follow up on existing injuries.

Tests that are available at the Kinesio-Lab:

Functional examination of the gait (45 minutes)
Functional examination of the spine (30 minutes)
Body composition analysis (20 minutes)
Functional examination of the foot (30 minutes)

Kinesio - Lab packages

Where can you find it?

The Kinesio Movement Analysis Lab is located on the second floor of the Festetics Bathhouse.

It is a facility of Hévíz Spa and St Andrew’s Hospital for Rheumatic Diseases. However, it is not located in the hospital. The Kinesio Lab can be accessed through the main entrance of the Lake Baths in Ady Endre Street. To make an appointment for a test in the laboratory, you don't need to have a doctor's referral or purchase a ticket to the Lake Baths. However, it is essential to book an appointment in advance. At the same time, you can also discuss which tests you would like to take.

Appointment

During opening hours in person on the spot: Festetics Bathhouse, Therapy Department
Via telephone: + 36 83 501-700 / extension 530 or 528 (during opening hours)
Via e-mail: mozgaslabor@spaheviz.hu

Opening hours

The central bath building located on the Hévíz Thermal Lake
(“A” building and “B” terrace = central covered section and large terrace)
will be temporarily closed from 18 March 2025 due to technical reasons.

The entrances to the Lake Bath and all other buildings remain open as usual.
Bathing in the thermal lake continues to be available without interruption, and all related spa facilities remain accessible.

Thank you for your understanding!
Lake Bath information desk:
Mobile: +36 30 959 1002
Email: spaheviz@spaheviz.hu

Hévíz Lake Bath reserve the right to change the opening hours and prices.

Hévíz Lake Bath Telephone:
+36 30 959 1002

Hévíz Lake Bath and Festetics Bathhouse price list

Valid from 01. April 2025. until withdrawn

Single-day tickets: Usable on the day of purchase only. Entitles the bearer to one-time entry. An additional charge will be levied if the allotted time limit is exceeded. Additional time extension cannot be purchased after the time limit has expired.

Lake passes: Deposits are refundable within 5 days of expiery. Refunds are payable in cash only, each day before the end of bathing time. Passes eintitle the bearer to enter the premises on two occasions per day. Following the bearer's first exit, a 15-minute wait period is required before return entry is permitted. Upon exiting the premises, locker number assignments are automatically cleared, after which we can accept no liability for contents. An additional charge will be levied if the alloted time limit is exceeded.

General information

• Valid from 09.05.2020 until withdrawal.
• The depth of the medicinal lake is 2-38 meters.
• Free use of changing rooms (included in the entrance fee)
• A sauna sheet is provided free of charge if you buy a ticket that entitles you to the use of the wellness facilities.
• The services of the wellness area are only available to persons over 12 years of age.
• Children under 6 years of age are admitted free of charge.
• The deposit is refundable within 72 hours of expiry.
• Daily tickets are valid only on the day of purchase.
• All tickets are valid for one entry a day only.
• We are not able to refund the price of the purchased tickets.
• We reserve the right to change prices and opening hours.
• An ATM is available during the opening hours in the building accessed from the Schulhof Promenade.

You can have more information about our special offers at the cash desks or on our website.
Hévíz Lake Baths phone number: 06 83 30 959 1002