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  • A very COOL experience! Drinks are served in a Torne River ice glass of course. The ICEBAR in Copenhagen was the first ever to be launched by ICEHOTEL (April 2009). Here, lens fog appeared on the camera just after leaving the extreme cold of the ICEBAR, giving a dreamy feel to the photograph.
    ICEBAR-Copenhagen-1585.jpg
  • A very COOL experience! Drinks are served in a Torne River ice glass of course. The ICEBAR in Copenhagen was the first ever to be launched by ICEHOTEL (April 2009).
    ICEBAR-Copenhagen-1573.jpg
  • Along the roadside in Loudoun County, Virginia, prickly dried Teasel plants collect ice and snow creating beautiful "ice prickles."
    Prickly-Teasel-winter-2970.jpg
  • Seagulls sit atop the ice at Jökulsárlón, a large glacial lagoon in southeast Iceland bordering Vatnajökull National Park. The lagoon is situated at the head of Breiðamerkurjökull glacier.
    Jokulsarlon-lagoon-Iceland-9679.jpg
  • Although the lava flowed some 3,000 to 4,000 years ago, the Berserkjahraun (Berserkers Lava Field), near Stykkishomur, Iceland is young enough to retain all kinds of convoluted shapes, with fascinating color and textural contrasts in the rock and thick mosses. The berserkers, from whom "gone berserk" originates, were a faction of Norse mercenaries known for their savage battle frenzy.
    Lava-Berserkjahraun-Iceland-1555.jpg
  • Jökulsárlón is a large glacial lagoon in southeast Iceland bordering Vatnajökull National Park. The lagoon is situated at the head of Breiðamerkurjökull glacier.
    Jokulsarlon-lagoon-Iceland-9859.jpg
  • Jökulsárlón is a large glacial lagoon in southeast Iceland bordering Vatnajökull National Park. The lagoon is situated at the head of Breiðamerkurjökull glacier.
    Jokulsarlon-lagoon-Iceland-9863.jpg
  • A large glacial lagoon in southeast Iceland bordering Vatnajökull National Park, Jökulsárlón is situated at the head of Breiðamerkurjökull glacier. It evolved into a lagoon after the glacier started receding from the edge of the Atlantic Ocean.
    Jokulsarlon-lagoon-Iceland-9661.jpg
  • Kvíárjökull is one of the many outlet glaciers that are part of Vatnajökull, the largest glacier in Europe.
    Vatnajokull-glacier-Iceland-9569.jpg
  • A dusting of snow covers a small woodland of trees and the leaf-strewn ground below them in rural Loudoun County, Virginia.
    Snow-trees-woods-2975.jpg
  • A large glacial lagoon in southeast Iceland bordering Vatnajökull National Park, Jökulsárlón is situated at the head of Breiðamerkurjökull glacier. It evolved into a lagoon after the glacier started receding from the edge of the Atlantic Ocean.
    Jokulsarlon-lagoon-Iceland-9825.jpg
  • Bryce Canyon National Park in Southern Utah is distinctive due to geological structures called hoodoos, formed by wind, water and ice erosion of the river and lake bed sedimentary rocks. The intricate hoodoos, eroded from soft limestone, glow with warm shades of red, orange, pink, yellow and cream with the right light. This was taken from Sunset Point.
    Bryce-Canyon-hoodoos-UT-5410.jpg
  • Bryce Canyon National Park in Southern Utah is distinctive due to geological structures called hoodoos, formed by wind, water and ice erosion of the river and lake bed sedimentary rocks. The intricate hoodoos, eroded from soft limestone, glow with warm shades of red, orange, pink, yellow and cream with the right light. This was taken from Sunset Point.
    Bryce-Canyon-hoodoos-UT-5410.jpg
  • From Sunset Point overlook, a view of the climb down into Bryce Canyon through a series of switchbacks leading to the Navajo Loop and Queen's Garden hiking trails. Bryce Canyon National Park in Southern Utah is distinctive due to geological structures called hoodoos, formed by wind, water and ice erosion of the river and lake bed sedimentary rocks. The red, orange and white colors of the rocks provide spectacular vistas for park visitors.
    Bryce-Canyon-Utah-5224.jpg
  • Bryce Canyon National Park in Southern Utah is distinctive due to geological structures called hoodoos, formed by wind, water and ice erosion of the river and lake bed sedimentary rocks. The red, orange and white colors of the rocks provide spectacular vistas for park visitors. This was taken from Sunset Point.
    Bryce-Canyon-hoodoos-UT-5205.jpg
  • Bryce Canyon National Park in Southern Utah is distinctive due to geological structures called hoodoos, formed by wind, water and ice erosion of the river and lake bed sedimentary rocks. The red, orange and white colors of the rocks provide spectacular vistas for park visitors.
    Bryce-Canyon-hoodoos-UT-5423.jpg
  • A lone photographer walks among the hoodoos catching the morning's golden light in Bryce Canyon National Park, Utah. Bryce is distinctive due to these geological structures, formed by wind, water and ice erosion of the river and lake bed sedimentary rocks.
    Bryce-Canyon-hoodoos-UT-5430.jpg
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Rozanne Hakala Photography

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