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The first settlers arrived in Iceland around AD 870, when the edge of the tongue of Breiðamerkurjökull glacier was about 20 km (12 mi) further north of its present location. During the Little Ice Age between 1600 and 1900, with lower temperatures prevailing in these latitudes, the glacier had grown by up to about 1 km (0.62 mi) from the coast ...
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A 1992 to 1998 observation of the Chacaltaya Glacier in Bolivia and Antizana Glacier in Ecuador indicate that between 0.6 m (2.0 ft) and 1.9 m (6.2 ft) of ice was lost per year on each glacier. Figures for Chacaltaya show a loss of 67% of its volume and 40% of its thickness over the same period.
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Snæfellsjökull (Icelandic pronunciation: [ˈs(t)naiːˌfɛlsˌjœːkʏtl̥] ⓘ, snow-fell glacier) is a 700,000-year-old glacier-capped stratovolcano in western Iceland. [3] It is situated on the westernmost part of the Snæfellsnes peninsula. Sometimes it may be seen from the city of Reykjavík over Faxa Bay, at a distance of 120 km (75 mi).
The mountain is located north of the Alpine crest within the municipal area of Kaprun, Salzburg.It was first climbed in 1828 by local mountaineer Johann Entacher. Today the summit can be easily reached using the Glacier Aerial Tramway from the valley station at 911 m (2,989 ft), including the highest cable car pylon in the world, being 113.6 m (373 ft) tall with a diameter of 2.2 m (7 ft 3 in).