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Italiano: La morfologia erosiva, a calanchi e camini delle fate, del canyon del Cedar Breaks National Monument, nello Utah. Questo anfiteatro naturale era chiamato, dai Paiute, “un-cap-i-un-ump” («cerchio delle scogliere dipinte») per la brillante colorazione rossa, gialla, arancione e porpora delle sue rocce, a causa dell'elevata presenza di ossidi di ferro e di manganese.
Magyar: Erózió által létrehozott sziklaformációk, “kémények” a Cedar Breaks Canyon nemzeti emlékparkban (Utah állam, USA). A sziklák vörös, sárga, narancs és lila színeit a bennük lévő vas-oxid és a mangán okozza
Nederlands: Ingang naar een kloof met hoodoo's (aardpiramides) van het Cedar Breaks National Monument nabij het stadje Cedar City in de Amerikaanse staat Utah. De rotsformaties van het Cedar Breaks National Monument zijn enigszins vergelijkbaar met die van het iets oostelijker gelegen Bryce Canyon.
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Captions
Entrance to a ravine with hoodoos in the Cedar Breaks National Monument, Utah, United States
{{Information |Description={{en|1=Entrance to a Chine in the Cedar Breaks National Monument.}} {{de|1=Eingang zu einer Schlucht im [[:de:Cedar Breaks National Monument|Cedar Breaks Nati