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The Pyramid is on a promontory on the west side of Koettlitz Glacier between Renegar Glacier to the southwest and Walcott Bay to the northeast. Dromedary Glacier is to the northwest. Nearby features include The Almond, Pyramid Trough and The Bulwark. [2] The Alph River flows north through the Pyramid Trough. [3]
Stephenson Nunatak) is a prominent, pyramid-shaped rock nunatak, rising to about 640 m, which rises 300 m above the surrounding ice at the northwest side of Kirwan Inlet in the southeast part of Alexander Island, Antarctica
Charpentier Pyramid) is a pyramid-shaped peak rising to 1,080 metres (3,540 ft) in the northwest part of the Herbert Mountains, Shackleton In association with the names of glacial geologists grouped in this area, it was named by the UK Antarctic Place-Names Committee in 1971 after Jean de Charpentier , a Swiss engineer and mineralogist who in ...
Fake news websites are those which intentionally, but not necessarily solely, publish hoaxes and disinformation for purposes other than news satire.Some of these sites use homograph spoofing attacks, typosquatting and other deceptive strategies similar to those used in phishing attacks to resemble genuine news outlets.
Snopes: focuses on, but is not limited to, validating and debunking urban legends and other stories in American popular culture. RealClearPolitics's Fact Check Review: aspires to offer quaternary-level critiquing of such tertiary-level efforts at fact-checking as those listed above.
Nunataks in Antarctica Cântaro Magro, Serra da Estrela, Portugal, formed as a nunatak during the last ice age and now exposed [1]. A nunatak (from Inuit nunataq) is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge.
Solitaire: Pyramid Challenge. Play five solitaire hands in a row to see how you rank. By Masque Publishing
Location Map of the Ellsworth Mountains Topographic Map of Ellsworth Mountains with an interval of 100 metres (330 ft). The geology of the Ellsworth Mountains, Antarctica, is a rock record of continuous deposition that occurred from the Cambrian to the Permian periods, with basic igneous volcanism and uplift occurring during the Middle to Late Cambrian epochs, deformation occurring in the Late ...