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  2. Heimaey - Wikipedia

    en.wikipedia.org/wiki/Heimaey

    Heimaey harbour in 2014. View from the Helgafell, looking north-west. Heimaey (Icelandic pronunciation: [ˈheiːmaˌeiː] ⓘ), is an Icelandic island. At 13.4 square kilometres (5.2 sq mi), it is the largest island in the Vestmannaeyjar archipelago, and the largest and most populated island off the Icelandic coast.

  3. Google Map Maker - Wikipedia

    en.wikipedia.org/wiki/Google_map_maker

    Changes to Google Map Maker were intended to appear on Google Maps only after sufficient review by Google moderators. Google Map Maker was used at Google Mapathon events held annually. In November 2016, Google announced that Google Map Maker would be retired and merged with Google Maps. [3] Google Map Maker was officially shut down on March 31 ...

  4. Google Maps Navigation - Wikipedia

    en.wikipedia.org/wiki/Google_Maps_Navigation

    Google Maps Navigation is a mobile application developed by Google for the Android and iOS operating systems that later integrated into the Google Maps mobile app. The application uses an Internet connection to a GPS navigation system to provide turn-by-turn voice-guided instructions on how to arrive at a given destination. [1]

  5. Keflavík - Wikipedia

    en.wikipedia.org/wiki/Keflavík

    Keflavík (pronounced [ˈcʰɛplaˌviːk] ⓘ, meaning Driftwood Bay) is a town in the Reykjanes region in southwest Iceland. It is included in the municipality of Reykjanesbær whose population as of 2016 is 15,129.

  6. Sandy Island, New Caledonia - Wikipedia

    en.wikipedia.org/wiki/Sandy_Island,_New_Caledonia

    Sandy Island (sometimes labelled in French Île de Sable, and in Spanish Isla Arenosa) is a phantom island that was charted for over a century as being located near the French territory of New Caledonia between the Chesterfield Islands and Nereus Reef in the eastern Coral Sea. [1]

  7. Bárðarbunga - Wikipedia

    en.wikipedia.org/wiki/Bárðarbunga

    Bárðarbunga was a little-known volcano in Iceland due to its remote location and infrequent eruptions approximately once every 50 years, but recent studies have shown that many tephra layers originally thought to be from other volcanoes were ejected from Bárðarbunga, [1] and that lateral dyke intrusions may trigger eruptions in adjacent ...

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