Criterion (vii): The combination of a huge ice sheet and a fast moving glacial ice-stream calving into a fjord covered by icebergs is a phenomenon only seen in Greenland and Antarctica. Ilulissat offers both scientists and visitors easy access for a close view of the calving glacier front as it cascades down from the ice sheet and into the ice-choked fjord. The wild and highly scenic combination of rock, ice and sea, along with the dramatic sounds produced by the moving ice, combine to present a memorable natural spectacle.
Criterion (viii): The Ilulissat Icefjord is an outstanding example of a stage in the Earth’s history: the last ice age of the Quaternary Period. The ice-stream is one of the fastest (40 m per day) and most active in the world. Its annual calving of over 46 km3 of ice accounts for 10% of the production of all Greenland calf ice, more than any other glacier outside Antarctica. The glacier has been the object of scientific attention for 250 years and, along with its relative ease of accessibility, has significantly added to the understanding of ice-cap glaciology, climate change and related geomorphic processes.
Integrity
The property is of sufficient size to adequately represent the geological process of the ice fjord, i.e. the fast-moving ice-stream, the relevant portion of the inland icecap, the glacial front and the fjord. The boundaries of the property are clearly defined in relation to the logical topographic criteria of the natural watershed, and the settlements of the nearby villages of Ilimanaq and Ilulissat are excluded from the property. Along with climatic limitations and the fact that no roads exist at the site, the area’s physical features retain a high degree of natural integrity.
The property has effective legal protection and a sound planning framework, including the prohibition of any mining in the protected area. However, increased management will be required as pressures from tourism and resource harvesting continue to grow.