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  2. Tourism in Antarctica - Wikipedia

    en.wikipedia.org/wiki/Tourism_in_Antarctica

    Tourism started in Antarctica by the sea in the 1960s. Air overflights started in the 1970s with sightseeing flights by airliners from Australia and New Zealand, and were resumed in the 1990s. The (summer) tour season lasts from November to March. Most of the estimated 14,762 visitors to Antarctica from 1999–2000 were on sea cruises. [1]

  3. Historic Sites and Monuments in Antarctica - Wikipedia

    en.wikipedia.org/wiki/Historic_Sites_and...

    Upload another image HSM-2 Fukushima's Rock Cairn Rock cairn and plaques at Syowa Station in memory of Shin Fukushima, a member of the 4th Japanese Antarctic Research Expedition, who died in October 1960 while performing official duties. The cairn was erected on 11 January 1961, by his colleagues. Some of his ashes repose in the cairn. (1972) Rec VII-9 69°00′00″S 39°35′00″E ...

  4. Antarctic gateway cities - Wikipedia

    en.wikipedia.org/wiki/Antarctic_gateway_cities

    Each of the gateway cities accommodate both planes and ships traveling to Antarctica, and generally service the areas of the continent closest to them. The cities are used by both national Antarctic programs and Antarctic commercial tourism companies, although they differ in how much of each they facilitate. As a result of their status as ...

  5. It's not for everyone: 3 things to know about Antarctica ...

    www.aol.com/news/not-everyone-3-things-know...

    More than 71,200 people visited Antartica during the 2022-2023 season. Expedition cruises can offer travel experiences unlike any other.

  6. End of the World Route - Wikipedia

    en.wikipedia.org/wiki/End_of_the_World_Route

    1 Tourist attractions. 2 Gallery. 3 References. ... Ruta del Fin del Mundo) is a Chilean touristic scenic route located in the Magallanes and Chilean Antarctic Region

  7. Lists of places in Antarctica - Wikipedia

    en.wikipedia.org/wiki/Lists_of_places_in_Antarctica

    Nearly all of Antarctica's surface is covered by ice to an average depth of 1.9 km (1.2 mi; 6,200 ft). [2] As such, a number of notable ice features have been described on the continent. Ice shelves

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