Nioghalvfjerdsbrae

Nioghalvfjerdsbrae is a glacier in Northeast Greenland and spreads across vast ice fields that form part of the Greenland ice sheet. The ice displays visible cracks and edges where it constantly moves and breaks apart into the fjord below.

The glacier formed thousands of years ago as part of the continental ice sheet during the last ice age. Its ice preserves a detailed record of climate shifts over many centuries and shows how the Arctic environment has changed.

Scientific research stations near the glacier facilitate international cooperation among researchers who study Arctic environments and glacial movements throughout the year.

Visits are best during the warmer months from June to September, when weather is more stable and daylight lasts much longer. Specialized tours with local guides and proper equipment are necessary, as the terrain is challenging and conditions can change quickly.

The glacier continuously releases massive icebergs that drift into surrounding waters, influencing the marine ecosystem and water circulation of the region. You can watch this calving process from the fjord, where breaking ice reveals deep cracks and fractured surfaces.