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The Smithsonian Institution's travel program will offer a new collection of trips, Smithsonian Active Journeys, in 2024.
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).
Arctic exploration is the physical exploration of the Arctic region of the Earth. It refers to the historical period during which mankind has explored the region north of the Arctic Circle. Historical records suggest that humankind have explored the northern extremes since 325 BC, when the ancient Greek sailor Pytheas reached a frozen sea while ...
Hofsjökull. Snæfellsjökull. Ljósufjöll. Þeistareykjabunga. Bárðarbunga. Fagradalsfjall. Svartsengi. Map all coordinates using OpenStreetMap. There are too many presumed extinct or now inactive volcanic features to list all of these below, so most monogenetic volcanoes can not be mentioned individually.
Surtsey. Vestmannaeyjar. 2008. 1267; ix (natural) Surtsey is a volcanic island that formed in a series of eruptions from 1963 to 1967, around 32 kilometres (20 mi) off the south coast of Iceland. Since 1964, it has served as a site to study colonisation from founder populations that arrived from outside.
Silfra. Rocks and boulders that have piled up in the fissure due to earthquakes. Silfra (Icelandic pronunciation: [ˈsɪl (v)ra]) is a rift formed in the Mid-Atlantic Ridge – the divergent tectonic boundary between the North American and Eurasian plates – and is located in the Þingvallavatn Lake in the Þingvellir National Park in Iceland.
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