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Fox Glacier

Fox Glacier / Te Moeka o Tuawe
Fox Glacier / Te Moeka o Tuawe is located in West Coast
Fox Glacier / Te Moeka o Tuawe
Fox Glacier / Te Moeka o Tuawe
Coordinates: 43°27′52″S 170°1′4″E / 43.46444°S 170.01778°E / -43.46444; 170.01778
Country New Zealand
Region West Coast
District Westland District
Population (2006)
 • Total 375

Fox Glacier / Te Moeka o Tuawe is a 13-kilometre-long (8.1 mi) temperate maritime glacier located in Westland Tai Poutini National Park on the West Coast of New Zealand's South Island. It was named in 1872 after a visit by then Prime Minister of New Zealand Sir William Fox. Following the passage of the Ngai Tahu Claims Settlement Act 1998, the name of the glacier was officially altered to Fox Glacier / Te Moeka o Tuawe.

Fed by four alpine glaciers, Fox Glacier falls 2,600 m (8,500 ft) on its 13 km journey from the Southern Alps down to the coast, with it having the distinction of being one of the few glaciers to end among lush rainforest only 300 metres (980 ft) above sea level. Although retreating throughout most of the last 100 years, it was advancing between 1985 and 2009. In 2006 the average rate of advance was about a metre a week. In January 2009, the terminal face of the glacier was still advancing and had vertical or overhanging faces which were continually collapsing. Since then there has been a significant retreat, with the 2009 high level clearly visible as vegetation line on the southern slope above what is left of the lower glacier today.

The outflow of the glacier forms the Fox River. During the last ice age, its ice reached beyond the present coastline, and the glacier left behind many moraines during its retreat. Lake Matheson formed as a kettle lake within one of these.

Like nearby Franz Josef Glacier, it is one of the most accessible glaciers in the world, with its terminal face an easy walk from Fox Glacier village/Weheka. It is a major tourist attraction and about 1000 people daily visit it during high tourist season. Though people are told not to, some go beyond the barriers and climb without guides onto the glacier, whose rapid advance creates dangers of sudden ice and rockfalls.


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