The Mięguszowiecki Glacieret, also known as the Mięguszowiecki Snowfield, is a genuine curiosity of the Polish Tatras — the largest firn-ice patch remaining in the Polish High Tatras, hidden within the dramatic rocky cirque of Bańdzioch. This is a place where winter never truly lets go, even in the height of summer.

The glacieret sits in the upper part of the Mięguszowiecki Cirque, at an altitude of 1973-2035 m, beneath the Mięguszowiecka Pass under Chłopek. Its size fluctuates from year to year, but it remains impressive — the cone-shaped upper section forms mainly from avalanche and snow-slide accumulation rather than direct precipitation. The sight of this icy tongue surrounded by the sheer rock walls of Bańdzioch is one of the wildest, most rugged scenes in the High Tatras, especially striking in early summer when white snow contrasts with dark granite cliffs.

How to get there

• Morskie Oko or Rybi Potok Valley — demanding terrain, accessible only as part of off-trail mountaineering routes, mountain experience required
• Bańdzioch (Mięguszowiecki Cirque) — approach for those experienced in high-mountain terrain, off marked trails

Practical information

• The glacieret lies beyond marked tourist trails, in terrain requiring mountaineering skills
• The area is protected within the Tatra National Park
• Beneath the glacieret a variable melt tunnel forms, along with a bergschrund up to 32 meters deep — approaching these is dangerous

It was here, in September 1924, that mountaineer Stanisław Krystyn Zaremba arrived, leaving behind one of the earliest descriptions of this icy phenomenon — a witness to an era when Tatra glaciers still endured.