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Rabbit Ears Pass (el. 9426 ft, 2873 m) is a high mountain pass in the Rocky Mountains of northern Colorado in the United States, where US highway 40 crosses the Continental Divide. North of the summit is Rabbit Ears Peak which has the shape of rabbit ears, which displays two large columns of basalt rock formations from the second volcanic episode. Rabbit Ears Peak is underlain by a pink tuff and the basalt immediately to the west is underlain by red, vesicular ash. Volcanic breccia occurs only at the Peak, which is a large stratified breccia pile. The three basal layers are cut by a basalt dike immediately beneath the peak. From petrographic evidence there appears to have been one period of lava flows and this surface can be seen at Rabbit Ears Peak.

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  • Rabbit Ears Pass (en)
  • Rabbit Ears Pass (pt)
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  • Rabbit Ears Pass (el. 9426 ft, 2873 m) is a high mountain pass in the Rocky Mountains of northern Colorado in the United States, where US highway 40 crosses the Continental Divide. North of the summit is Rabbit Ears Peak which has the shape of rabbit ears, which displays two large columns of basalt rock formations from the second volcanic episode. Rabbit Ears Peak is underlain by a pink tuff and the basalt immediately to the west is underlain by red, vesicular ash. Volcanic breccia occurs only at the Peak, which is a large stratified breccia pile. The three basal layers are cut by a basalt dike immediately beneath the peak. From petrographic evidence there appears to have been one period of lava flows and this surface can be seen at Rabbit Ears Peak. (en)
  • Rabbit Ears Pass (elevação de 2873 m) é uma passagem de alta montanha nas Rocky Mountains do Norte do Colorado, nos Estados Unidos. Seu cume tem a forma de orelhas de coelho (daí o seu nome), que exibe duas grandes colunas de formações rochosas de basalto do segundo episódio vulcânico. O Pico, chamado de Rabbit Ears Peak, é sustentado por um tufo rosa e o basalto imediatamente a oeste é coberto pelo vermelho, cinza vesicular. A brecha vulcânica ocorre apenas no Pico, que é uma grande pilha de brechas estratificadas. As três camadas basais são cortadas por um dique de basalto imediatamente abaixo do pico. De evidência petrográfica parece haver um período de fluxos de lava e esta superfície pode ser vista em Rabbit Ears Peak. (pt)
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  • Rabbit Ears Pass (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Continental_Divide.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Moose_Rabbit_Ears_Pass.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/MuleDeer_Rabbit_Ears_Pass.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/RabbitEarsPass.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Rabbit_Ears_pass_2014_.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Snowmobling_onrabbitearspass.jpg
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