布萊斯峽谷國(guó)家公園 布萊斯峽谷國(guó)家公園的冬天 當(dāng)考慮到猶他州西南部被嚴(yán)重侵蝕的峽谷時(shí)，首先想到的可能不是雪。但是，遙遠(yuǎn)的布萊斯峽谷國(guó)家公園有很多白色的東西，因?yàn)樗诰薮蟮膱A形劇場(chǎng)邊緣海拔8000多英尺。寒冷不僅提供了美麗的雪景和偉大的越野滑雪，它的原因是引人注目的紅巖頂峰，被稱為胡桃，使公園如此獨(dú)特。高在海平面以上，布萊斯峽谷國(guó)家公園的冬天經(jīng)常會(huì)出現(xiàn)冰凍和高于冰點(diǎn)的溫度變化。盡管它的名字，布萊斯峽谷不是一個(gè)真正的峽谷，而是一個(gè)自然圓形劇場(chǎng)的集合。當(dāng)水滲入巨大的石質(zhì)高原，然后凍結(jié)并膨脹，使大塊的巖石破碎，公園里的樹(shù)冠就形成了。在這一天的沉積過(guò)程中，最薄的一天已經(jīng)在峽谷留下了濃密的痕跡。

原文:

When considering the dramatically eroded canyons of southwestern Utah, snow may not be the first thing that comes to mind. But far-flung Bryce Canyon National Park gets plenty of the white stuff, owing to its elevation of 8,000-plus feet at the massive amphitheater's rim. The cold not only provides scenic snowy views and great cross-country skiing, it's responsible for the striking red-rock pinnacles—known as hoodoos—that make the park so unique.High above sea level, winter in Bryce Canyon often sees daily shifts between freezing and above-freezing temperatures. Despite its name, Bryce Canyon isn't a true canyon, but is instead a collection of natural amphitheaters. The park's hoodoos formed as water seeped into massive stone plateaus, then froze and expanded to break away chunks of rock. Repeated day after day for eons, this process has left slim sections of sediment standing throughout Bryce Canyon—now the largest concentration of hoodoos in the world.

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