Occurrence of Attributes in Original Text
The text related to the cultural heritage 'Ilulissat Icefjord' has mentioned 'Fjord' in the following places:
| Occurrence Sentence | Text Source |
|---|---|
| For the fjord in eastern Greenland, see Isfjord. | WIKI |
| Ilulissat Icefjord (Greenlandic: Ilulissat Kangerlua) is a fjord in western Greenland. | WIKI |
| The glacier flows at a rate of 20xe2x80x9335xc2xa0m (66xe2x80x93115xc2xa0ft) per day, resulting in around 20xc2xa0billion tonnes of icebergs calved off and passing out of the fjord every year. | WIKI |
| Icebergs breaking from the glacier are often so large xe2x80x94up to a kilometer (3,300xc2xa0ft) in heightxe2x80x94 that they are too tall to float down the fjord and lie stuck on the bottom of its shallower areas, sometimes for years, until they are broken up by the force of the glacier and icebergs further up the fjord. | WIKI |
| Located on the west coast of Greenland, 250 km north of the Arctic Circle, Greenlandxe2x80x99s Ilulissat Icefjord is a tidal fjord covered with floating brash and massive ice, as it is situated where the Sermeq Kujalleq glacier calves ice into the sea. | UNESCO |
| 10% of all Greenland calf ice, is more than any other glacier outside Antarctica, and it is still actively eroding the fjord bed. | UNESCO |
| The combination of a huge ice-sheet and the dramatic sounds of a fast-moving glacial ice-stream calving into a fjord full of icebergs make for a dramatic and awe-inspiring natural phenomenon. | UNESCO |
| 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. | UNESCO |
| 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. | UNESCO |
| The property is of sufficient size to adequately represent the geological process of the ice fjord, i.e. | UNESCO |
| the fast-moving ice-stream, the relevant portion of the inland icecap, the glacial front and the fjord. | UNESCO |